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LIBRARI ES” SMITHSONIAN” INSTITUTION ss N oO ae w = w oa Aa = > e] = A > > - > -— = - e = 2 = ei = m 4 m n°’ pea ” = z r ” _ Ww — w — op SMITHSONIAN INSTITUTION NOILNLILSNI_ NVINOSHLIWS, S3 iyvudit =” = a = 7 x = , = ¥ =a al an = 5 \ = LS ve fe} = AS S “2 O £ = 2a NK Zz, = = _ z Wie 3 4 ; —NVINOSHLINS S3 iy¥Vuag I7_LIBRARI ES SMITHSONIAN _INSTITUTION rb ig ena a a Sa a nn PROCEEDINGS of the Biological Society of Washington VOLUME 102 1989 Vol. 102(1) published 29 March 1989 Vol. 102(3) published 18 October 1989 Vol. 102(2) published 28 June 1989 Vol. 102(4) published 19 December 1989 WASHINGTON PRINTED FOR THE SOCIETY EDITOR C. BRIAN ROBBINS ASSOCIATE EDITORS Classical Languages Invertebrates GEORGE C. STEYSKAL STEPHEN D. CAIRNS FRANK D. FERRARI RAYMOND B. MANNING Plants Vertebrates DAvip B. LELLINGER G. DAviID JOHNSON Insects WAYNE N. MATHIS All correspondence should be addressed to the Biological Society of Washington, Smithsonian Institution Washington, D.C. 20560 ALLEN PREss INC. LAWRENCE, KANSAS 66044 OFFICERS AND COUNCIL of the BIOLOGICAL SOCIETY OF WASHINGTON FOR 1988-1989 OFFICERS President KRISTIAN FAUCHALD President-Elect LESLIE W. KNAPP Secretary G. DAVID JOHNSON Treasurer DON E. WILSON COUNCIL Elected Members GARY R. GRAVES MEREDITH L. JONES W. RONALD HEYER RAYMOND B. MANNING W. DUANE HOPE WAYNE N. MATHIS TABLE OF CONTENTS Volume 102 Alvarez, Fernando. Smalleyus tricristatus, new genus, new species, and Pseudothelphusa parabelliana, new species (Brachyura: Pseudothelphusidae) from Los Tuxtlas, Vera- Feng AMM) a) 4 66 no ea NCS 9 AT Sn Ae Cee Le on SNe eA ies One Anderson, William D., Jr. and Phillip C. Heemstra. Ellerkeldia, a junior synonym of Hypoplectrodes, with redescription of the type species of the genera (Pisces: Serranidae: AN Tut EDR) sa ee eee aa vee eee Barnard, J. L. Rectification of Halirages regis and H. huxleyanus (Crustacea: Amphip- oda), from marine Antarctica, with description of a new genus, Austroregid..................... Barnard, J. L. and James Darwin Thomas. Four species of Synopiidae from the Carib- bean region (Crustacea: Amphipoda) 1. = ee ee eee, Barnard, J. L. and James Darwin Thomas. A new species, Ampelisca burkei, (Crustacea, Amphipoda) from, Plorida..22.000 2.00..) -S eee ee ene Barr, Douglas J. and Susumu Ohtsuka. Pseudocyclops lepidotus, a new species of demersal copepod (Calanoida: Pseudocyclopidae) from the northwestern Pacific... Bieri, Robert. Krohnittellidae and Bathybelidae, new families in the Phylum Chaetog- natha; the rejection of the family Tokiokaispadellidae and the generea Tokiokaispa- della, Zahonya, and: Aberrospadella: 2a ee ee ee eee Boeger, Walter A., Delane C. Kritsky, and Joaber Pereira, Jr. Neotrpical Monogena. 14. Revision of Callorhynchocotyle Suriano and Incorvaia, 1982 (Hexabothriidae) with the description of C.amatol....... See eee ee ee ee Bowman, Thomas E. The high frequency of errors in format in manuscripts submitted to. Proceedings of the Biological Societyiof Washinelon === ne a ae Bowman, Thomas E. and Robert Bieri. Paraspadella anops, new species, from Sao anus Cave, Grand Bahama Island, the second troglobitic chaetognath Brinkhurst, Ralph O. Varichaetradrilus angustipenis (Brinkhurst and Cook, 1966), new combination for Limnodrilus angustipenis (Oligochaeta: Tubificidae)... Brownell, Robert L., Jr. and James G. Mead. Taxonomic status of the delphinid (Mam- malia: Cetacea) Mursio? panope: Pinilippis SO 5) eee eae ce Browning, M. Ralph. The type specimens of Hekstra’s OW]S 2... eect Bullock, Robert C. Rhyssoplax baliensis, a new species of chiton from Indonesia (Mol- Iusea:: Pobyplacophora: Chitomicac) 2.25 ee ee Campbell, Jonathan A. A new species of colubrid snake of the genus Coniophanes from the ‘highlands of Chiapas) Mexico 2: —) 2 a ee ee Campbell, Jonathan A., William W. Lamar, and David M. Hillis. A new species of diminutive Eleutherodactylus (Leptodactylidae) from Oaxaca, Mexico... Carvacho, Alberto. Cancer johngarthi, n. sp. and Cancer porteri (Bell) (Crustacea, De- capoda): comparisons.and hypothesis-=<2).. ee eee Chace, Fenner A., Jr. The holotype of Heterocarpus alexandri A. Milne-Edwards (Crus- tacea: Decapoda: :Pandalidae) (1.3520 5 Pee ee eee Child, C. Allan. Pycnogonida of the Western Pacific Islands VI. Sericosura cochleifovea, a new hydrothermal vent species from the Marianas back-arc Dasani eeeeeeeeees Chirino-Galvez, Luis A. and Raymond B. Manning. A new deep-sea crab of the genus Chaceon from Chile (Crustacea, Decapoda, Geryonidae) Colbath, G. Kent. Revision of the family Lysaretidae, and recognition of the family Ocnonidac Kinberg; 1865 (Eunicida: Polychacta)a == ee Colbath, G. Kent. A revision of Arabella mutans (Chamberlin, 1919) and related species (Polychaeta: Arabelln@ac): 20 on ae a TC Cutler, Edward B. and Norma J. Cutler. A revision of the genus Aspidosiphon (Sipuncula: Aspidosiphonidae). ee a ee ken nee ee e Desbruyéres, Daniel and Lucien Laubier. Paralvinella hessleri, new species of Alvinel- lidae (Polychaeta) from the Mariana back-arc basin hydrothermal vents... 45-49 1001-1017 701-715 362-374 375-384 331-338 973-976 264-271 1067-1068 586-589 311-312 532-534 515-519 808-819 1036-1044 491-499 613-619 84-88 732-737 401-404 116-123 283-299 826-865 761-767 Erséus, Christer. Phallodrilus hessleri, new species (Oligochaeta: Tubificidae), from abys- Sang OHEHS Mat He sWweSstenm ur aCiNe \OCCAn soe ne Slash pe as Erséus, Christer. Phallodrilus vescus, new species (Oligochaeta, Tubificidae) from the STS EN a cat Le See 8 SOS PE Re ee Erséus, Christer. Four new west Atlantic species of Tubificoides (Oligochaeta, TEETER ES 0 CS) OS ee ee eens cc eS a de Ee ee ce ae ae Erséus, Christer and Michael R. Milligan. Three new species of Tubificidae (Oligochaeta) from an oil seepage area on the continental slope of the northern Gulf of Mexico....... Etnier, David A. and James D. Williams. Etheostoma (Nothonotus) wapiti (Osteichthyes: Percidae), a new darter from the southern bend of the Tennessee River system in BLS TEATS NEE oy ea ne oe ee A es de Ee Re Oe Se ne ee Fauchald, Kristian. The Second Annual Riser Lecture: Eclecticism and the study of a UOM ES A i sd ee i a et zs Fautin, Daphne G. and Robert R. Hessler. Marianactis bythios, a new genus and species of actinostolid sea anemone (Coelenterata: Actiniaria) from the Mariana vents... Fitzpack, J. F., Jr. and Craig A. Busack. Hobbseus yalobushensis, a new crawfish from posers Mississippi (Decapoda: Cambaridae) 2.0 0s Flint, Oliver S., Jr. and D. G. Denning. Studies of neotropical caddisflies, XL: new species of Smicridea (Smicridea) from middle America and the West Indies (Tri- Sanaa eo ol ETAL OPS VC IGAC) ee, nto ae sd a ea Formas, J. Ramon. A new species of Eupsophus (Amphibia: Anura: Leptodactylidae) ODSE QE TET Sen CB rl RE Be ee Cee ere aS ene ae eee ae Sa, SO a ee ee Froeschner, Richard C. A small collection of Heteroptera from the Galapagos Islands, with the description of the new species Niesthrea ashlocki and a list of Niesthrea SPETOSY CRNGCR NG A1e) RO es a cae ee ed ee ee Froeschner, Richard C. Three new species of Colombian lace bugs of the genera Le- wamenya and Lepropharsa (Heteroptera: Tingidac) 22-25 Gardner, Alfred L. and G. Ken Creighton. A new generic name for Tate’s (1933) Mi- crotarsus group of South American mouse opossums (Marsupialia: Didelphidae).. Giere, Olav. The First Annual Riser Lecture: Meiofauna and Microbes—the interactive relations of annelid hosts with their symbiotic bacteria eect Gillet, Patrick. Axiothella crozetensis, a new species of maldanid polychaete from Crozet re RMSE GRE EVE CO) Ce ANT ee see i oe St Goeke, Gary D. Stenorhynchus yangi, a new western Atlantic species of Arrow Crab (Crustacea, Brachyura, Majidae) and a redescription Of S. SCtiCOM IIS i.e Grabe, Stephen A. Some aspects of the biology of Rhopalophthalmus tatersallae Pillai, 1961 (Crustacea, Mysidacea) and extension of range into the Khor Al Sabiya, Kuwait meats i APAE Cen ITN | seen eee Mice tenn i 8 ee Tere lees 2 OS ee BON ee Grygier, Mark J. Three new species of Myzostoma (Myzostomida) eee Hardy, Laurence M. The karyotype of Exilliboa placata Bogert (Tropidopheidae), and comparisons with the family Boidae (Reptilia: Serpentes) Hensley, Dannie A. and Kunio Amaoka. A redescription of Pseudorhombus megalops, with comments on Cephalopsetta ventrocellata (Osteichthyes: Pleuronectiformes: ee eee IGG tees ee mH itin Pie Mi fete acl Te i ad Hershler, Robert. Springsnails (Gastropoda: Hydrobiidae) of Owens and Amargosa Riv- er (exclusive of Ash Meadows) drainages, Death Valley System, California-Nevada.. Heyer, W. Ronald and Alan J. Wolf. Physalaemus crombiei (Amphibia: Leptodactyli- dae), a new frog species from Espirito Santo, Brazil with comments on the P. signifer Hobbs, Horton H., Jr. and Daniel J. Peters. New records of entocytherid ostracods infesting burrowing crayfishes, with the description of a new species, Ascetocythere BEE LE Se ne ree oad Ree ee OR ee Hobbs, Horton H., Jr. and Henry W. Robison. On the crayfish genus Fallicambarus (Decapoda: Cambaridae) in Arkansas, with notes on the fodiens complex and descrip- HISICHALIV CT HEIVES PECIC Smale. 2 divert ihe pth Th fee Holsinger, John R. Allocrangonyctidae and Pseudocrangonyctidae, two new families of 131-133 134-136 877-886 887-893 987-1000 742-752 815-825 637-643 418-433 568-576 609-612 968-972 3-7 109-115 866-869 620-636 726-731 793-804 1045-1049 577-585 176-248 500-506 324-330 651-697 holarctic subterranean amphipod crustaceans (Gammaridea), with comments on their pliylopenetic and zoogeographic-relationships:.<... es ee es Holt, Perry C. A new species of the cambarincolid genus Sathodrilus from Missouri, with the proposal of a replacement name for Adenodrilus Holt, 1977 (Clitellata: Branchiobdellida) 0 2-2) FS NE eB RE ee ee ee a A RON eee Humes, Arthur G. Acontiophorus excavatus, new species (Copepoda: Siphonostoma- toida) associated with the soft coral Dendronephthya (Alcyonacea) in the Indo- PACHIG son OIE hee EST RPE OE eat eee ee ROAR Oe OU nN) Oa ee Jara, Carlos G. Aegla denticulata lacustris, new subspecies, from Lake Rupanco, Chile (Crustacea: ‘Decapoda: Anomira Acelidae) es eee 2 ee eee ee Johnson, G. David and Edward B. Brothers. Acanthemblemaria paula, a new diminutive chaenopsid (Pisces: Blennioidei) from Belize, with comments on life history... Kensley, Brian. New genera in the thalassinidean families Calocarididae and Axiidae... Keppner, Edwin J. Four new species of free-living marine nematodes in the genus Pareurystomina (Nematoda: Enoplida) with observations on other members of the Kornicker, Louis S. The adult male of the troglobitic ostracode Spelaeoecia bermudensis Angel and Iliffe, 1987, from an anchialine cave in Bermuda (Crustacea: Ostracoda: Halocypridoidea) 2.) Jo3 4) 2, As SE Sa ee ene ee ene ee ee Kornicker, Louis and Thomas M. Iliffe. Dantya ferox, a new species of mydocopid ostracode from Niue, central South Pacific (Crustacea: Ostracoda: Sarsiellidae)....... Lowry, James K. and Gary C. B. Poore. First ingolfiellids from the southwest Pacific (Crustacea: Amphipoda) with a discussion of their Systematics... eeeeeeeecccsneeeeeeeeeeeneeeee Manning, Raymond B. Sanquerus, a replacement name for Posidon Herklots, 1851 (Crustacea, 'Decapoda-Portumidae) sot cn tle eee ee Manning, Raymond B. and David K. Camp. Additional records for an Atlantic reef lobster, Enoplometopus antillensis Liitken, 1865 (Crustacea, Decapoda, Enoplometopidae) 2.4.22 4 22 See ee eee OE 8 tence O38 es ee ee Manning, Raymond B. and L. B. Holthuis. Two new genera and nine new species of geryonid crabs (Crustacea; Decapoda,'Geryoniddae) eee eee Manning, Raymond B., Marcos Siqueira Taveres, and Elaine Figueiredo Albuquerque. Chaceon ramosae, a new deep-water crab from Brazil (Crustacea: Decapoda: CHEF VOL AG) ote Osan mee ePaper Se he Sac leah ene ghee iA aS Martin, Joel W. and Denton Belk. Eulimnadia ovilunata and E. ovisimilis, new species of clam shrimps (Crustacea, Branchiopoda, Spinicaudata) from South America... Mathis, Wayne N. A review of the beach flies of the Caribbean and Gulf of Mexico (Diptera: Canacidae) 2020 ee ee SF Sioa ee ae Ok, ROO Ee Ae Mathis, Wayne N. and Jin Zuyin. A review of the shore-fly genus Polytrichophora Cresson: fromeAsia (Diptera: Ephydridae) = eee ee ee ee McCranie, James R., Jay M. Savage, and Larry David Wilson. Description of two new species of the Eleutherodactylus milesi group (Amphibia: Anura: Leptodactylidae) from: northern: Honduras = 20 Sees SU Se ea eet oy eee ne Se nee eee McLelland, Jerry A. Eukrohnia calliops, a new species of Chaetognatha from the northern Gulf of Mexico‘withmiotes on related: specie sees ee eee Miller, John E. and David L. Pawson. Hansenothuria benti, new genus, new species (Echinodermata: Holothuroidea) from the troptical western Atlantic: a bathyal, epi- benthic holothurian’ with swimming) abilitics 2 = eee eee Miller, Scott E. Paleontological type specimens in the Santa Barbara Museum of Natural Monniot, Claude and Francoise Monniot. Ascidians collected around the Galapagos Islands using the Johnson-Sea-Link research submersible... cece Munroe, Thomas A. and Madhu N. Mahadeva. Symphurus callopterus (Cynoglossidae, Pleuronectiformes), a new deepwater tonguefish from the eastern Pacific. Ohwada, Takashi. Redescription of Nephtys squamosa Ehlers (Polychaeta: Nee polity ihe) es ee koe Th hea eel ad Ns Si ene le Olson, Storrs L. Two overlooked holotypes of the Hawaiian flycatcher Chasiempis described by Leonhard Stemneger (Aves: Miyacuticac) ree eet ee 947-959 738-741 916-923 385-393 1018-1030 960-967 249-263 313-323 901-911 933-946 698-700 411-417 50-77 646-650 894-900 590-608 434-446 483-490 33-44 977-986 1-2 14-32 458-467 124-130 555-558 Ortiz, Juan Carlos, Héctor Ibarra- Vidal, and J. Ramon Formas. A new species of Eupso- phus (Anura: Leptodactylidae) from Contulmo, Nahuelbuta Range, southern Chile... Ota, Hidetoshi and Ronald I. Crombie. A new lizard of the genus Lepidodactylus (Rep- tilia: Gekkonidae) from Batan Island, Philippines. Perkins, Philip D. Adelphydraena, new genus, and two new species from Venezuela, and remarks on phylogenetic relationships within the subtribe Hydraenina (Coleoptera: SCE 21e) aa eerie ce aio) ev eae 8 ee Re OL PS 2 Pettibone, Marian H. New species of scale-worms (Polychaeta: Polynoidae) from the hydrothermal rift-area of the Mariana back-arc basin in the western central Pacific... Pettibone, Marian H. Polynoidae and Sigalionidae (Polychaeta) from the Guaymas Basin, with descriptions of two new species, and additional records from hydrothermal vents of the Galapagos Rift, 21°N, and seep-sites in the Gulf of Mexico (Florida and eS EEE Sees EEE oes ee eee ee mMRRNT SS | ns Sr ene Oe vee Pettibone, Marian H. A new species of Benhamipolynoe (Polychaeta: Polynoidae: Lep- idastheniinae) from Australia, associated with the unattached stylasterid coral Co- RUPIRIRPERPEIIOL Besos Secon se es 2 atic Pk 2h Pettibone, Marian H. Two new species of Harmothoinae (Polychaeta: Polynoidae) from the East Pacific Rise, collected by Alvin dives 2000 and 2003 nee Rickart, Eric A., Lawrence R. Heaney, and Mark J. Rosenfeld. Chromosomes of ten species of Philippine fruit bats (Chiroptera: Pteropodidae) oe eeeeeeeceeeeeeeeeeeeeeeee Rodriguez, Gilberto and Horton H. Hobbs, Jr. Freshwater crabs associated with caves in southern Mexico and Belize, with descriptions of three new species (Crustacea: ae, Sennen mee Ee ee es rr ee ee ee Romero, Raul Castro and Hernan Baeza Kuroki. Neobrachiella anisotremi (Copepoda: Lernaeopodidae), a new species parasitic on an inshore fish, Anisotremus scapularis, PEEVE CEE SOR OY a a ee ear Mn ee Romero, Raul Castro and Hernan Baeza K. Lamelliform structures on the proboscis of Peniculus and Metapeniculus (Copepoda: Penmellidae) cece eeeeeeeceeeneeeeeeeeeene Roper, Clyde F. E. and C. C. Lu. Systematic status of Lepidoteuthis, Pholidoteuthis, and Neranvenoieuins (Cephalopoda: Ocgopsida)... Rossman, Douglas A., Ernest A. Liner, Carlos H. Trevino, and Alan H. Chaney. Re- description of the garter snake Thamnophis exsul Rossman, 1969 (Serpentes: IPE ASS a ee a Fe Ruff, R. Eugene and Betsy Brown. A new species of Euchone (Polychaeta: Sabellidae) from the northwest Atlantic with comments on ontogenetic variability. Russell, David E. A new species of Odontosyllis (Polychaeta: Syllidae) from Twin Cays, San Martin, Guillermo and Carmen Alos. Paraprocerastea crocantinae, a new genus and species (Polychaeta: Syllidae: Autolytinae) from the Spanish Mediterranean... Schotte, Marilyn. Two new species of wood-boring Limnoria (Crustacea: Isopoda) from Rene ane ARIE eP ICICSE ATG E- RCPILCULIES se Sheavly, Seba B. and Harold G. Marshall. Plytoplankton composition in a borrow pit EE CE OSIRIS ere a Soils-Weiss, Vivianne and Kristian Fauchald. Orbiniidae (Annelida: Polychaeta) from mangrove root-mats in Belize, with a revision of protoariciin genera Stauffer, J. R., Jr. and J. M. Boltz. Description of a rock-dwelling cichlid (Teleostei: Mieaneac)ironirake Malawi Alricn |... te. Noe Steadman, David W. New species and records of birds (Aves: Megapodiidae, Colum- bidae) from an archaeological site on Lifuka, Tongo. Storer, Robert W. Geographic variation in the Yellow-rumped Tanager (Aves: Thrau- Thomas, James Darwin and J. L. Barnard. Gammaropsis arawakia, a new species of macine Atmphipoda (Crustacea) from Jamaica Vari, Richard P. and Ann Williams Vari. Systematics of the Steindachnerina hypostoma complex (Pieces, Ostariophysi, Curimatidae), with the description of three new SEE ES te ae eee Wagele, Johann Wolfgang and Niel L Bruce. Natatolana pastorei (Giambiagi, 1925) 1031-1035 559-567 447-457 137-153 154-168 300-304 305-310 520-531 394-400 106-108 912-915 805-807 507-514 753-760 768-771 870-876 716-725 272-279 772-792 8-13 537-552 553-554 89-94 468-482 (Crustacea, Isopoda, Cirolanidae) from the Straits of Magellan, South America: Re- description and notes on functional morphology ee Warén, Anders and Robert Moolenbeek. A new eulimid gastropod, Trochostilifer eu- cidaricola, parasitic on the pencil urchin Eucidaris tribuloides from the southern Caribbean 2-45 aden ewer I perett watunensomthcpent fn bs orte wee Bomets Bh EE Wicksten, Mary K. Synalpheus arostris and Philocheras lapillus, two new species of caridean shrimp (Crustacea) from the tropical eastern Pacific ee Wicksten, Mary K. Hippolyte zostericola (Crustacea: Decapoda) in the eastern Pacific. Williams, Austin B. and P. J. B. Scott. Upogebia corallifora, a new species of coral- boring shrimp from the West Indies (Decapoda: Upogebiidae) Wilson, George D. F., Oleg G. Kussakin, and Galina S. Vasina. A revision of the genus Microprotus Richardson with descriptions of two new species, M. acutispinatus and M. lobispinatus.(Asellota, Isopoda,. Crustacea) 2s. 2.8 ac eo Bi eS Zullo, Victor A. and Anna V. Buising. An unusual species of the Balanus amphitrite Darwin complex (Cirripedia, Balanidae) from the ancestral Colorado River delta in western Arizona .and ‘southeastern California: 2c. 28 2 aioe ee 95-105 169-175 78-83 644-645 405-410 339-361 924-932 INDEX TO NEW TAXA Volume 102 (New taxa are indicated in italics; new combinations designated n.c.) COELENTERATA Anthozoa Si OE SE IS tee tN ga a Ite Pd Bt Fl a Co ee Se EST IS te se ae a A i IRA RAS Ew REE eS PLATYHELMINTHES Trematoda ea ES TSO SD GON GLC ate ca AS ROPE EAE RE IES SERA ADSI A TH EEN AS RE RA En DE DOTS G1) TSC a scat Ra a a ee re de Sa a NEMATODA ies Oe aM SE CHER DEEN INCE) PIT ICE eee etme Nt ee PAPEETE EDEL (Se ee re cl PT a orcas Met eee Ree ee SDT EI TITAS eat el i DAR MR eS NE EEe A eAO ALE SoA Ra A Al Se LIES SY DE, sac cncenpet ntl det ee et tS NO ee Ret MOLLUSCA Polyplacophora MUIR CREME IIIT COTES 1 Simmer ae Sf a ad ae en eee tee a 2 TEED OTE SES: PUPIL OSS id a ceed eae eh al oR Sn EET EET EGIL SOO, OG, SS RTS SO NNER Tee GN UDP er ae PMMOM TON TTL LEOE EN We? 2 / CREE SCALES Scere oe CB De Ree ea IR ch ne Ee eS ELE YDS I SS os I STS RIT AS Sena til a ele a RE a es ET Os EOE CETTE LEIS, sata i ct DR NR td Me IE eA CS Atel a LA FEO GE ST sen ep Bi I a TU at A i le 8 AE ea ce 7A der ant Bes AP Sot Ra dla DUEL SIC ee oa PT SM RE is ED ER UE AR aN BL SCE OE eT ade eR at A SEVERE OT Ca AO) a cost a ce a tS I Oe es RE A TA ee ES ERE T PUTED Bsr oe eh ta Ne ah PS RA Se RE A EE ETL TT ee eee ee ete en ter ee oe PONG SOE a nane PSs P Rs i PE Ik e e l A SR e RE ANNELIDA Polychaeta DNTPS SUL EL POTATO se te pr EST Ee ees enn SOC UCTRE REDS oS OES IS eS eee ee EMR OE CENE EER EL ACE CNIS Ii err nes ee ees Beshamipotynoe carpsi 2 * 2 A 2a ee ee ee ee 301 Branchmmolopiutmia DUrKenses ee 144 EE VACENCATRS PRIA SR a a ne ee nc 753 EXURrieee IVETE a a Ree et ee 308 E¥arinrothine WHat ee ee a ey EO ee cee 305 ELEEPTDAST FOEIIN VAP aa a a e 2 300 Lepidonotopockivarm: ryanritetunreg os esa A ee eh te ee me ee 5 142 Pevemsteinielica aise. a a ee ee 139 Macellicephaloides a@ivirer 13 og ee eee ee a Se 162 Qdots Gls LW Pricey CHS IS a a ec 768 COPISTHO UO CHOPOCUS FTTCTIES a re 149 Paralvinella Resslerd 2 eo Ea NE aI ate erro ene oe SD ent cen 761 Paraprocerdstea oe eee ee eee er 872 CFOCGNUIN GG. a ee Ea Tice a ee ne ef ee 874 Bararteia: OCIEZCVISIS ne a ee 789 Petfibonelia on a ee ee 785 VVC TUUTACT ILL oa oh 785 RGEOAUICIA PECTIICIIE AEG: cc Fg 783 Oligochaeta Tmnodriloides OLCGritis 2 he De no 887 hve raha: eS SE CHU an se es 131 VESCUS 2 aS Ss EEN Dee a 134 Tubificoides 6) gL | | | eam een ue een Merete Ere a ee ne 882 OCPINIUS eee 883 BOLO ss yh 2M re 880 PO ATRLTIICTASIS aa FN a as a 878 PORCH UMTS a Ses ee ee 889 DDCOUCENO AC a on! NR NI oe I a 891 Branchiobdellida Sea EERO ETN US 1B OKO PULOV EUS a I 738 ARTHROPODA Pycnogonida Odontothelphusa wiOnOdOntis xh ee eee ee ee 396 Potamocarcinusleptoriel ies a a ee eee 394 SeriGostina COCHICHOVCG sc. te as a eo 732 Pyphlopseudothelphusa (ya ar 398 Crustacea AACONTIOPHOFS CXCOVOTLUS isso BO ED BR ei aa ET a Sn 916 A@eia demticurlatanLaCi stra ooh te Se A eS ee eee 385 AL ELOGRANGONY CT LDAE be lana Dato Bl aE Os SF 9 ee 947 Ampelisca burkei. o2 3 I ie oe ee 375 Aseelocy there Stocker hi: 8 BE De 325 PAUSES OV COV 5 ee ot ls nD 703 BSetb ASUS COTO US on See SE op lk Pt 926 GCOISTOCOFIS a Fe EO See hy a oo ee ed 961 Caner JOMMGOTEN xe 2 I ee 613 CCC ON i ie Te ce Lae a Re 51 CAL OPUS as Nhe NS Sr an LN RDN AO EE 53 DS 6) (0) ee oe ee ae ee eee eT ae eee Pee 55 CVAPN ASB Si i Ss IS ac a SEE 401 OCU DSW CU a oh lh te es Se a7 CUM OT A Oo a i tage aH Ta ea eo 61 OORT EET NEE Me ee aaa ae 66 EARS ied Ne ace kB ee SR ee oc ae eee ee 69 POP DN Gee SS DE 2s TN De 646 REGIE DING TG oS NI ae Ee NO ee et 70 we SEE (ERODE Se See TD oi i et 902 CEOS SOPECE EGE DOTTIE lS I De BIE ek ee 894 POOR Sa a ah OE ed a 898 Pat STATA TTI (CO GC ASCUETINES 77) 90 100 a 684 Emaecimnards (balliGamibanuS)) DCHINCONDUS = 661 SOO ART ARTS PAORESSESSECET PR RE CD AUD cecil an ra A i E 89 ODA IE TS SERDS LOVES eS aCe Ss Se IE PT Se eo ee NNN PT ALND ee Te 370 ORES MOE Ps COEME SIT CHEN Sete ae wae ae es ee Pe 637 LL EEE, DOU R ITT Sa Sa SE el li SM PO Se eee a 933 ee EEE 7 em cn nS 2D 938 paid aM ek Sele E ONL GA ETC ECD) nf CGS Ii a ee) FLT PEE IUD AS tush Bee te AR a ANTE ED SENST ST g IRE OENS AOU ORO PERN PEI PETS 720 NEP IE IEE TEs Pan ae reas Nok ak a ee eo SN ae hk ites 2 962 DMEDIES FAT Dies SS UN) SEI i pe ne POR eh ONT WSN AOS eae Be IE Le or NE REI set UO 963 WAP UPMRCRPMERE ASIN S PRCT YC TIEUZCL LIS ene eh a Sok kd a Be eed thn 354 SUS DEAT OL Sn oa 2 aa Sa MR geet a ee ee eh GS ge ht SE ane eee 349 SET PPS CPS LS COTO OG (y i ct 2 F ea aatot Se RG aOR ct EAE Aa eae A a D 106 SSRmOR TAIT TPITE CS ns Ra toa ls YB De 80 PELE DOTA ce sce Oe ES I ae a 2 A ae eee We Re A Seas eel Seti le 964 ene Ore G Oe TD Ab ees oer eee eee eee 953 PSEC SUES VERT ONO No een ace et eaten a a che ea lee eae oe 0 el Merge nee ear se A oe ane 331 EPEUZIE LEE SVS) GUAT OG TOT sal ee ES eR A Pi cite 46 oo DAE TDG EIS. cent ais ss Ne ae eNO APR Ce a REE SE PSE DETR PET SSRI) AG LM ta SoA 964 ner aneaTie WATT cet ener ete ae ee ere ee ee ee eee eee 698 EE et eR Ss Een SB oa A Ee, eee le ie a. 45 SFLU TILT a re a ot Ot i a lg ee CL eee RDO eRe RA 46 2 EDR ES Tet ETS Te ag a ee Sc Rn 631 LTE SLD ETS GOR ee al oie a OSE Oe ee Oe reek Cee eee, 5 78 a CARTE ED 1) 0) mee ae ee enenne Tr en enn se rte ee ee eee 405 EEN BOVE ac cess a eg ah AN en see a EES AS, a A 2 INLET a Sa a elec Ee Se 73 Insecta ALP BIL SURE GD) ast So EG yd 5 ns Ne ea a rr 448 Di LG ET Se et a SRE Ws te Se A le ts 450 SORIA ee TS EN Beso UES ae a elt Le ERR oe) 448 RI GI SARI TIAGGICS Eanes ek Beek Oe eee ee Re WA Soho 968 UBD RESS RAPES CTP TICIOIITS e RRN So! Se aig SSCS I EB Re nr re 969 TEES OT! soso SE IE 3 I ES cll NS See I EE 970 “TESS EPSR) EQ DGl Te NA Se ee Sa DS eee Tee oe te a Ne ee Are ELT Pee PU ea 609 Co DEE GSES LOE TTT LE Ss a a a aa nS 599 Ae 8 ey OER RSN yaa sh Sahl ala, AIR 598 TEE SRYESE OS TENCE LEAD CUI 0 a2 Aaa eo 419 CESSES GI Fac Sanat ess dln Micah pees As ll cil te A AO 421 POD Apr wens alan TS cays ba toe les sea estate cel a Me Nimes A a REL a 423 EPP T BOSS Sn I Sc ET Sa I SP 421 SOP TINT 6 a Rs a 429 EAE Tt 2 eee ee ene emnn ane nn ent ne erie fy ee er et 423 APIO ea cee an te Sue ea ea ee A a eS A 426 ELLE TEN ETT a ent gt eg a LL LOE EEA ATT LIE AE 431 ed gn PI PP Baca cs TRC Eh 43] CRETE sa cau eels Ta Mesh ge SON ae a eel ree . 426 COLES TN a yal SUT Re OS OL) eA ee BS 423 CELE POE IF) oe a8 pe on ne EO a eR ee 419 CHAETOGNATHA RATELY BE DA es hs Ee ee eT hE eee Seen ee te ee ee ee eee JESUS oN ga ee ator? 11110) 2) eae Od OO RRR tld MOR gO Ce ROA! cs aan bea Pact adie sac Wire vn tae adode lh, KRONE ERE TE PAT 5 oe i hd Rs Ie eee eae pie ee RIE ONE ee Set ae LT Paraspadellainops.2 ee ee Se ee ee ECHINODERMATA Holothuroidea TUNICATA Ascidiacea PSC1G NA FAS Cg ha et rm nln dn ere A OVEN OITA OVA ain se ct as een Peco yeh ir ts OF IAS ONT i eB SSL EM G1.) [1] {| a ac ara enone ee mnsee onese stot ene eves ree 0) See eee Styler SOLfOT IS ccc ce a hh Pn Nee CHORDATA Pisces Acanthemiblemaria paul 2.50253 ey, ey he he I Bll er ln eee EGE OSUOMNA WPI scsi 8 ha os es es i eo es re ge rose Seek Pseudotropheus XnstOnta Chis snc. se a ee on verso she pee aa Stcindachnherima o7acilis. 22-54.) oh oa. bank ile ee pa ee ee tren te on ee DUGTUIVONUTAS 25s oo sn pe ey SE ates lah SA ee W Ret ae eee GUGSUIIOU ON 2.58 Sn ee Es Pi set OE Nall tlhe sa ind ae Syanplrs: CaM Ope eras saa spe 0 Sem Se a a ig eer decane ne DOU IUUIAU Sea i a Be gd nee eH EIPSOPHUS COMI OCTISIS 2 an 5 ape eee aC a CHNIMOPUGIT ia ee gc TE ee Pi ySala@unvuns: CROWD CL ceo 0 sla me ae One Cm Oplanies aI V ee 0 ats i Nr ae age oc Wepidodacty lus: DaQliOD isis tao. A es oo inh settled Se a cla Megapodius alimentum Gracilinanus TRUOA OB OV ON 5 5 5 8 ol pf AD LA a ce carriebowensis ramosissima ERRATA Hobbs, H. H., & H. W. Robison. 1989. 102(3):651-697. For Fig. 2 (p. 657) and Fig. 7 (p. 673), the same maps were inadvertently printed. The correct map and caption for Fig. 2 is shown below. Fig. 2. Distribution of Fallicambarus (F.) dissitus (encircled stars), F. (F.) jeanae (encircled dots), F. (F.) petilicarpus (triangle) and F. (F.) strawni (dots) in Arkansas. (Some localities listed in text too close to others to be shown.) g 4. ww Ye THE BIOLOGICAL SOCIETY OF WASHINGTON 1988-1989 Officers President: Kristian Fauchald Secretary: G. David Johnson President-elect: Leslie W. Knapp : Treasurer: Don E. Wilson Elected Council Gary R. Graves Meredith L. Jones W. Ronald Heyer Raymond B. Manning W. Duane Hope Wayne N. Mathis Custodian of Publications: David L. Pawson PROCEEDINGS Editor: C. Brian Robbins Associate Editors Classical Languages: George C. Steyskal Invertebrates: Stephen D. Cairns Frank D. Ferrari Plants: David B. Lellinger Raymond B. Manning Insects: Wayne N. Mathis Vertebrates: G. David Johnson Membership in the Society is open to anyone who wishes to join. There are no prerequisites. Annual dues of $15.00 ($20.00 to non-USA addresses) include subscription to the Proceedings of the Biological Society of Washington. Library subscriptions to the Proceedings are: $25.00 within the U.S.A., $30.00 elsewhere. The Proceedings of the Biological Society of Washington (USPS 404-750) is issued quarterly. Back issues of the Proceedings and the Bulletin of the Biological Society of Washington (issued sporadically) are available. Correspondence dealing with membership and subscriptions should be sent to The Treasurer, Biological Society of Washington, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560. Manuscripts, corrected proofs, editorial questions should be sent to the Editor, Biological Society of Washington, National Museum of Natural History, Smithsonian Institution, Wash- ington, D.C. 20560. Known office of publication: National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560. Printed for the Society by Allen Press, Inc., Lawrence, Kansas 66044 Second class postage paid at Washington, D.C., and additional mailing office. POSTMASTER: Send address changes to PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON, National Museum of Natural History, Washington, D.C. 20560. THIS PUBLICATION IS PRINTED ON ACID-FREE PAPER. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 1-2 PALEONTOLOGICAL TYPE SPECIMENS IN THE SANTA BARBARA MUSEUM OF NATURAL HISTORY Scott E. Miller Abstract.—In accordance with Recommendation 72G of the International Code of Zoological Nomenclature, which recommends that institutions publish lists of the type specimens in their collections, this paper lists primary paleon- tological type specimens in the Santa Barbara Museum of Natural History, Santa Barbara, California (SBMNH). This list does not include paratypes and plesiotypes, which include those of Bremner (1933), Chaney and Mason (1933), and Orr (1968). Kingdom Plantae Family Rosaceae Pyrus hoffmannii Chaney and Mason, 1933:61, pl. 7, figs. 9, 10, 13; syntypes flow- er, fruit, and leaf, SBMNH Pal. 277-279 (SBMNH Pal. Bot. Types 26-28); Late Pleistocene, “Carpinteria Formation’’; Car- pinteria Asphalt Deposit, Santa Barbara County, California. Synonymized under Amelanchier pallida Greene by Miller (1979). Kingdom Animalia Class Aves Family Pseudodontornithidae Osteodontornis orri Howard, 1957:3, figs. 2-8; holotype nearly complete skeleton in 2 shale slabs, SBMNH Pal. 309; Miocene, Monterey Formation; Flagstone quarry of G. Antolini and Sons, west side of Tepus- quet Creek, Santa Barbara County, Califor- nia. Family Phalacrocoracidae Phalacrocorax rogersi Howard, 1932:118, fig. 19; holotype coracoid, SBMNH Pal. 131 (SBMNH Pal. Orn. 32.1); Early Pleistocene, Santa Barbara Formation; Veronica Springs Stone Quarry (depth 50 feet), Santa Bar- bara, Santa Barbara County, California. Class Mammalia Family Otariidae Imagotaria downsi Mitchell, 1968:1844, figs. 1-14; holotype partial skeleton, SBMNH Pal. 342; Early Pliocene or Late Miocene, Sisquoc Formation; Quarry of Great Lakes Carbon Company, near Lom- poc, Santa Barbara County, California. Literature Cited Bremner, C.S.J. 1933. Geology of San Miguel Island, Santa Barbara County, California.— Santa Bar- bara Museum of Natural History Occasional Pa- per 2:1-23. Chaney, R. W., & H. L. Mason. 1933. A Pleistocene flora from the asphalt deposits at Carpinteria, California.— Carnegie Institute of Washington Publication 415:45-79. Howard, H. 1932. A new species of cormorant from Pliocene deposits near Santa Barbara, Califor- nia.—Condor 34:118-120. . 1957. A gigantic “toothed” marine bird from the Miocene of California.—Santa Barbara Mu- seum of Natural History, Department of Ge- ology Bulletin 1:1-23. Miller, S. E. 1979. Reevaluation of Pyrus hoffmannii (Rosaceae) from the Pleistocene Carpinteria As- phalt Deposit, California.—Madrono 26:190- 191. Mitchell, E. D., Jr. 1968. The Mio-Pliocene pinniped Imagotaria.—Journal of the Fisheries Research Board of Canada 25:1843-1900. Orr, P. C. 1968. Prehistory of Santa Rosa Island.— Santa Barbara Museum of Natural History, San- ta Barbara, California. xxi + 253 pp. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Santa Barbara Museum of Natural His- tory, 2559 Puesta Del Sol Road, Santa Bar- bara, California 93105; Present address: Bishop Museum, Box 19000-A, Honolulu, Hawaii 96817. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 3-7 A NEW GENERIC NAME FOR TATE’S (1933) MICROTARSUS GROUP OF SOUTH AMERICAN MOUSE OPOSSUMS (MARSUPIALIA: DIDELPHIDAE) Alfred L. Gardner and G. Ken Creighton Abstract. — Until recently, all mouse opossums were considered as belonging to the genus Marmosa, as revised by Tate (1933). Today, however, we recognize that Marmosa (s.1.) contains several distinctive species groups whose relation- ships are best expressed by dividing this complex into five genera as follows: Marmosa (s.s.), Marmosops, Micoureus, Thylamys, and a complex of species for which we propose a new name Gracilinanus because no genus-group name is available. Systematists have differed in their inter- pretation of the generic and subgeneric tax- onomy of the smaller mouse-sized marsu- pials of the family Didelphidae. Thomas (1888) grouped the known taxa of mouse opossums under the subgenus Micoureus in the genus Didelphys. Matschie (1916) dis- tributed these taxa among five subgenera of Didelphis: Marmosa, Grymaeomys, Mar- mosops, Thylamys, and Caluromys. Ca- brera (1919) grouped mouse opossums into two subgenera (Varmosa and Thylamys) under the genus Marmosa. Tate’s (1933) re- vision was the most comprehensive. Tate (1933:22) believed that the genus Marmosa was a “““good,’ natural genus of didelphids”’ that included all Neotropical mouse opos- sums. Although Tate acknowledged natural subunits in his concept of Marmosa, he did not recognize subgenera and, instead, used the following names to indicate five infor- mal groups: cinerea, murina, noctivaga, mi- crotarsus, and elegans. He also expressed the opinion (p. 22) that “‘there is always the chance that subgenera may be later con- verted into full genera, and thus, in the case of Marmosa the undoubted unity of the ge- nus be obscured.” Over the ensuing half-century, however, new information has made the division of Marmosa (sensu Tate 1933) into several genera a desirable and necessary step to bet- ter reflect relationships and natural assem- blages. Gilmore (1941) again divided Mar- mosa into the subgenera Marmosa and Thylamys but did not list species. Cabrera (1958) used Marmosa and Thylamys as sub- genera as he had earlier (Cabrera 1919) and followed the species associations of Tate (1933) except that he divided Tate’s micro- tarsus group, assigning the microtarsus sec- tion to Thylamys and the /epida section to Marmosa. Marshall (1981) listed the names Marmosa (“murine opossums’’), Micoureus (‘large murine opossums’’), and Thylamys (‘small murine opossums’’), as genera among other didelphids and attributed this arrangement to a manuscript by Reig et al. subsequently published in 1985. Reig et al. (1985) assigned Tate’s (1933) murina and noctivaga groups to the genus Marmosa along with the more recently described taxa M. andersoni, M. cracens (incorrectly spelled crascens), and M. xerophila. They allocated Tate’s (1933) cinerea group to Micoureus. They also assigned the 14 species listed by Kirsch & Calaby (1977) along with Mar- mosa lepida, M. emiliae, and M. contrerasi, to Thylamys. Creighton (1984) also recog- nized five groups in his revision of the genus 4 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Marmosa (s.1.). He placed four of these (ci- nerea, murina, noctivaga, and microtarsus) in the subgenus Marmosa and the fifth (e/e- gans) in the subgenus Thylamys. Despite Creighton’s (1984) conservative treatment of Marmosa (s.l.), each of the groups he recognized corresponds to a genus in the sense used by Kirsh & Calaby (1977) and Reig et al. (1985, 1987). Creighton’s elegans-group equals Thylamys and corre- sponds closely to Tate’s elegans group, but is more restrictive than construed by Ca- brera (1958), Kirsch & Calaby (1977), and Reig et al. (1985, 1987). We recognize Thy- lamys Gray, 1843 as a genus that includes the species 7. elegans (genotype), 7. ma- crura (Olfers, 1818:205; Didelphis grisea Desmarest, 1827, is a Junior synonym), T. pallidior, T. pusillus, and T. velutinus. Creighton’s cinerea-group corresponds to that of Tate (1933) as used by Reig et al. (1985, 1987) under the generic name M7- coureus Lesson, 1842 (Micoures Reig et al. 1987, is an incorrect subsequent spelling), to which we assign the species Micoureus cinereus (genotype), M. constantiae, M. re- gina, and M. alstoni. Creighton’s murina- group is similar to Tate’s (1933) group by the same name except that Creighton also included M. lepida. The earliest available name for Creighton’s murina-group is Mar- mosa Gray, 1821, which we use here as a genus in a narrower sense than treated by Reig et al. (1985, 1987). As we understand it, Marmosa (s.s.) includes Marmosa an- dersoni, M. canescens, M. lepida, M. mex- icana, M. murina (genotype), M. robinsoni, M. rubra, M. tyleriana, and M. xerophila. Reig et al. (1985, 1987) combined Tate’s noctivaga and murina groups under Mar- mosa. However, Creighton (1984) showed that Tate’s (1933) noctivaga group, with the addition of M. parvidens (which Tate had included in his microtarsus group), and the more recently described taxa M. cracens and M. handleyi, is a natural unit of closely re- lated species for which the name Marmo- sops Matschie, 1916, is available. Marmo- sops includes the species M. cracens, M. dorothea, M. fuscatus, M. handleyi, M. im- pavidus, M. incanus (genotype), M. invictus, M. noctivagus, and M. parvidens. This is similar to Reig et al.’s (1987:7) composition of Marmosops, which they ranked as a sub- genus of Marmosa. Creighton’s (1984) fifth taxon, the micro- tarsus-group, is nearly identical to Tate’s microtarsus section with the addition of the more recently described M. agricolai. How- ever, Kirsch & Calaby (1977) and Reig et al. (1985, 1987) followed Cabrera (1958) in combining Tate’s (1933) elegans group and microtarsus section under Thylamys, along with some other taxa that Creighton (1984) showed belong elsewhere. Creighton includ- ed nine species in his microtarsus-group, although here we recognize only six. No ge- nus-group name is available for this species complex for which we propose the name: Gracilinanus, new genus Type species. —Didelphys microtarsus Wagner, 1842:359; type locality ““Ypane- ma’”’ (=Bacaetava), Sao Paulo, Brazil. Etymology. —From the Latin gracilis (thin, slender) and Greek nanos (dwarf) combined to reflect the small size and slen- der or gracile form of the species included in this genus. Distribution. —Gracilinanus contains six living species whose composite geographic range is below 3000 m in the tropical and subtropical zone east of the Andean Cor- dillera of South America. Diagnosis and description.—A genus of small mouse opossums (head and body, 85.0—130.0 mm; tail, 90.0-—150.0 mm). The ratio of tail length to head-and-body length is always greater than 1.3 and usually less than 1.5. Dorsal pelage ranges from bright reddish brown to dull brownish gray. The tail has small (more than 40 per cm) round- ed to square scales, arranged in annular rows. Triplet interscalar hairs are subequal in length with the middle hair about three scale rows long. The diameter of the middle hair VOLUME 102, NUMBER 1 is about twice that of the lateral hairs, but not as stout and petiolate as in Marmosops. The tail is weakly bicolored in some species (G. agilis and G. marica) and unicolored fuscous in others (G. aceramarcae, G. dryas, and G. microtarsus). Claws on the manus do not extend beyond terminal digital pads. The central palmar surfaces lack the gran- ular appearance of those of Thylamys and Monodelphis. All palmar and plantar tu- bercles (description by Creighton 1984) are present and separated by at least a double row of granules. Sparse granules are present on the central plantar surface. Granules on the proximal ventral surfaces of the digits are fused into transverse bars. The skull lacks postorbital processes; however, the su- praorbital margin of the frontals may be beaded in larger individuals of some species. The lambdoidal crest is weakly developed or absent except in the largest individuals. The hard palate is highly fenestrated, usu- ally with three pairs of medial fenestrae (medial, posteromedial, and mesolateral— described in Creighton 1984). The postero- lateral fenestrae are moderate in size, usu- ally about a third to half the breadth of the last upper molar in length. The nasals are moderately expanded laterally at the max- illo-frontal suture. The auditory bullae are relatively large compared with those of Marmosa, Micoureus, and Marmosops, but proportionately smaller than in Thylamys. A slender anteromedial process of the ali- sphenoid portion of the auditory bulla is always present, although frequently dam- aged during specimen preparation. The sec- ond upper premolar is always larger than the third. The incisors increase slightly in size from 12 through I5. The lower canines are relatively short compared with those of Marmosa, Micoureus, and Thylamys, but are not as short or premolariform as in Mar- mosops. Species of Gracilinanus are distinguish- able from those of Marmosops by the shape and arrangement of tail scales and bristles, the non-premolariform lower canine, and the presence of pectoral mammae. They can be separated from species of Thylamys by the absence of seasonal fat deposits in the tail (thus non-incrassate), absence of dense- ly granular central palmar and plantar sur- faces, and relatively longer digits and broad- er interdigital pads on manus and pes. Gracilinanus can be distinguished from Marmosa and Micoureus by the lack of postorbital processes on the frontals and by the annular arrangement of minute scales on the tail. Included species. — Gracilinanus aceramarcae (Marmosa ac- eramarcae Tate, 1931:12; type locality ‘Rio Aceramarca, tributary of Rio Un- duavi, Yungas,”’ La Paz, Bolivia). Gracilinanus agilis (Grymaeomys agilis Burmeister, 1854:139; type locality ““La- goa Santa,’ Minas Gerais, Brazil). Synonyms: Marmosa beatrix Thomas, 1910:502; type locality ““Ipu,”’ Ceara, Brazil. Marmosa muscula Shamel, 1930a:83; type locality ““Kilometro 182” (=Ria- cho Pilaga, 10 miles northwest of Km 182), Formosa, Argentina. Marmosa formosa Shamel, 1930b:311; renaming of M. muscula Shamel, 1930a, preoccupied by Didelphis (Mar- mosa) musculus Cabanis, 1848. Marmosa agilis chacoensis Tate, 1931:10; type locality ““Sapucay,” Paraguay. Marmosa agilis buenavistae Tate, 1931: 10; type locality ““Buenavista, Depart- ment of Santa Cruz, Bolivia.” Marmosa agilis peruana Tate, 1931:11; type locality ““Tingo Maria, Rio Hua- llaga,”” Huanuco, Peru.” Marmosa unduaviensis Tate, 1931:11; type locality ““Pitiguaya, Rio Unduavi, Yungas,”’ La Paz, Bolivia. Marmosa blaseri Miranda-Ribeiro, 1936: 373; type locality “S. Bento,” Goias, Brazil. Thylamys rondoni Miranda-Ribeiro, 6 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 1936:387; type locality “‘salto do Se- potuba e S. Joao da Serra do Norte,” Mato Grosso, Brazil. Gracilinanus dryas (Marmosa dryas Thom- as, 1898:456; type locality ““Culata, Me- rida, Venezuela’’). Gracilinanus emiliae (Marmosa emiliae Thomas, 1909:379; type locality “Para, Brazil’). Synonym: Marmosa agricolai Moojen, 1943:2; type locality ““Crato, Ceara,” Brazil. Gracilinanus marica (Marmosa marica Thomas, 1898:455; type locality ““R. Al- barregas, Merida, Venezuela’’). Gracilinanus microtarsus (Didelphys micro- tarsus Wagner, 1842:359; type locality ‘““Ypanema,”’ Sao Paulo, Brazil). Synonyms: Marmosa microtarsus guahybae Tate, 1931:10; type locality “‘Island of Gua- hyba near Porto Alegre, Rio Grande do Sul,”’ Brazil. Marmosa herhardti Miranda-Ribeiro, 1936:382; type locality ““Humboldt,” Santa Catarina, Brazil. Literature Cited Burmeister, H. 1854. Systematische Uebersicht der Thiere Brasiliens, welche wahrend einer Reise durch die Provinzen von Rio de Janeiro und Minas Geraés gesammelt oder beobachtat wur- den von Dr. Hermann Burmeister. I. Sauge- thiere (Mammalia). G. Reimer, Berlin, x + 342 pp. Cabanis, J. 1848. Saeugethiere. Pp. 766-786 in R. Schomburgk, ed., Versuch einer Fauna und Flora von Britisch-Guiana, in Reisen in Britisch- Guiana in den jahren 1840-1844. J. J. Weber, Leipzig, 3:vi1l + 531-1260. Cabrera, A. 1919. Genera Mammalium. Museo Na- cional de Ciencias Naturales, Madrid, 177 pp., 17 pls. . 1958. Catalogo de los mamiferos de America del Sur.— Revista del Museo Argentino de Cien- cias Naturales “Bernardino Rivadavia,”’ Cien- cias Zoologicas 4(1):iv + 307 pp. Creighton, G. K. 1984. Systematic studies on opos- sums (Didelphidae) and rodents (Cricetidae). Unpublished Ph.D. dissertation, University of Michigan, xi + 220 pp. Desmarest, A. G. 1827. Sarigue. Pp. 392-399, Vol. 47 inF. G. Cuvier, ed., Dictionnaire des sciences naturelles, dans lequel on traite méthodique- ment des différens étres de la nature considérés soit en eux-mémes, d’apres |’état actuel de nos connoissances, soit relativement a l’utilité qu’en peuvent retirer la médecine, l’agriculture, le commerce et les arts. F. G. Levrault, Strasbourg; Le Normant, Paris, 1816-1845, 61 Vols., 12 Vols. pls. Gilmore, R. M. 1941. Zoology. Pp. 314-319 in J. C. Bugher, J. Boshell-Manrique, M. Roca-Garcia, and R. M. Gilmore, eds., The susceptibility to yellow fever of the vertebrates of eastern Co- lombia.—American Journal of Tropical Medi- cine 21:309-333. Gray, J. E. 1821. On the natural arrangement of ver- tebrose animals.—London Medical Repository 15:297-311. . 1843. List of the specimens of Mammalia in the collection of the British Museum. British Museum (Natural History), London, xxviii + 216 pp. Kirsch, J. A. W., & J. H. Calaby. 1977. The species of living marsupials: An annotated list. Pp. 9- 26 in B. Stonehouse and D. Gilmore, eds., The biology of marsupials, University Park Press, Baltimore, viii + 486 pp. Lesson, R. P. 1842. Nouveau tableau do Régne An- imal. Mammiféres. Arthus-Bertrand, Paris, 204 pp. Marshall, L. G. 1981. The families and genera of Marsupialia. — Fieldiana: Geology, new series 8: 1-65. Matschie, P. 1916. Bemerkungen iiber die Gattung Didelphis L.—Sitzungsberichte der Gesellschaft Naturforschender Freunde, Berlin 1916(1): 259- 272; Miranda-Ribeiro, A. 1936. Didelphia ou Mamma— lia—ovovivipara.— Revista do Museu Paulista, Sao Paulo 20:245-427. Moojen, J. 1943. Algunos mamiferos colecionados do nordeste do Brasil com a descriaao de duas especies novas e notas de campo.— Boletim do Museu Nacional, Rio de Janeiro, Zoologia 5:1— 14. Olfers, I. von. 1818. Bemerkungen zu Illiger’s Ue- berblik der Saugthiere nach ihrer Vertheilung uber die Welttheile, riicksichtlich Siidamerican- ischen Arten [chapter 10]. Pp. 192-237 in W. L. Eschwege, Journal von Brasilien, oder ver- mischte Nachrichten aus Brasilien, auf wissenschaftlichen Reisen gesammelt. Vol. 15, heft 2 in F. T. Bertuch, ed., Neue Bibliotek des wichtigsten Reisen-beschreibungen zur Erwei- terung der Erd- und Volkerkunde; in Verbin- VOLUME 102, NUMBER 1 dung mit einigen anderen Gelehrten gesammelt und herausgegeben .... Gr. H. S. pr. Landes- industries-comptoirs, Weimar. Reig, O. A., J. A. W. Kirsch, & L. G. Marshall. 1985. New conclusions on the relationships of the opossum-like marsupials, whith [sic] an anno- tated classification of the Didelphimorphia.— Ameghiniana 21(2-4):335-343. —.. ,& . 1987. Systematic relation- ships of the living and Neocenozoic American ““opossum-like”” marsupials (suborder Didel- phimorphia), with comments on the classifica- tion of these and of the Cretaceous and Paleo- gene New World and European metatherians. Pp. 1-90 in Possums and opossums: Studies in evolution. Surrey Beatty & Sons PTY Limited, New South Wales, frontispiece, 1xxii + 400 pp.., 4 pls. Shamel, H. H. 1930a. A new murine opossum from Argentina.—Journal of the Washington Acad- emy of Sciences 20:83. 1930b. A new name for Marmosa muscula Shamel.—Journal of Mammalogy 11:311. Tate, G. H. H. 1931. Brief diagnoses of twenty-six apparently new forms of Marmosa (Marsupi- alia) from South America.— American Museum Novitates 493:1-14. . 1933. Asystematic revision of the marsupial genus Marmosa.—Bulletin of the American Museum of Natural History 66:1-250, 26 pls., 1 table (9 sections, pocketed). Thomas, O. 1888. Catalogue of the Marsupialia and Monotremata in the collection of the British Museum (Natural History). British Museum (Natural History), London, xiv + 401 pp., 33 pls. . 1898. On seven new mammals from Ecuador and Venezuela. — Annals and Magazine of Nat- ural History, Series 7 1:451-457. . 1909. New species of Oecomys and Marmosa from Amazonia. — Annals and Magazine of Nat- ural History, Series 8 3:378-380. . 1910. On mammals collected in Ceara, N. E. Brazil by Fraulein Dr. Snethlage.— Annals and Magazine of Natural History, Series 8 6:500- 503. Wagner, A. 1842. Diagnosen neuer Arten Brasilischer Saugethiere.— Archiv fiir Naturgeschichte 8(1): 359-360. (ALG) Biological Survey Field Station, National Ecology Research Center, U.S. Fish and Wildlife Service, National Museum of Natural History, Washington, D.C. 20560; (GKC) Division of Mammals, National Museum of Natural History, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 8-13 DESCRIPTION OF A ROCK-DWELLING CICHLID (TELEOSTEI: CICHLIDAE) FROM LAKE MALAWI, AFRICA J. R. Stauffer, Jr. and J. M. Boltz Abstract. —A new species of cichlid fish of the Pseudotropheus zebra complex, P. xanstomachus, is described from Lake Malawi, Africa. The species is en- demic to the Maleri Islands. The species is morphologically similar to the sympatric Pseudotropheus barlow McKaye & Stauffer, but the species are dis- tinguishable in both coloration and shape. The rock-dwelling cichlids (“mbuna’’) which inhabit the rocky shores and rock outcroppings of Lake Malawi are repre- sented by many species which are endemic to particular islands. Ribbink et al. (1983) published a survey of this group and Lewis et al. (1986) published a guide to the fishes of the Lake Malawi National Park, which discussed the distribution of many of the mbuna. The purpose of this paper is to de- scribe a new species closely related to Pseu- dotropheus zebra (Boulenger) endemic to a group of islands collectively referred to as the Maleri Islands, located in Lake Malawi, Malawi, Africa. Ribbink et al. (1983) rec- ognized this form and referred to it as P. zebra “yellow throat.” Methods and materials. —Standard length (SL) is used throughout. External counts and measurements follow Barel et al. (1977). Scale counts in the lateral line series do not include scales in the overlapping portion of the lower lateral line. Except for gill raker meristics, which were recorded from the right side, all counts and measurements were made on the left side of the fish. Vertebral counts were made from radiographs. All specimens were collected at Nakantenga Is- land (34°39’E, 13°55’S), Lake Malawi, Af- rica (Apr 1984 and Aug 1987). The new species is compared with P. bar- lowi by color descriptions of fresh speci- mens, meristic differences, and shape dif- ferences. Body shape differences were compared using sheared principal compo- nent analysis (Humphries et al. 1981, Book- stein et al. 1985). This analysis quantifies shape differences between the two popula- tions independent of size of the individuals (Reyment et al. 1984). Pseudotropheus xanstomachus, new species Figs. 1, 2; Tables 1, 2 Pseudotropheus zebra, Ribbink et al., 1983: 162 (an part). Holotype. —National Museum of Natural History (USNM) 297268, adult male, 63.3 mm, Nakantenga Island, Lake Malawi, 3- 7m, 4 Aug 1987. Paratypes.—USNM 297269, 11 (47.0- 70.8 mm), data as for holotype; USNM 297270, 4 (63.5-—78.5 mm), Nakantenga Is- land, Lake Malawi, 12 m, 19 Apr 1984. Diagnosis. —This species fits the descrip- tion of the genus Pseudotropheus as given by Regan (1921) in that: 1) its jaws have several rows of teeth, with the ones in the outer row bicuspid and those in the inner rows tricuspid; 2) it has 16-18 dorsal-fin spines, 7—8 dorsai-fin rays, 3 anal-fin spines, and 6-7 anal-fin rays. However, as noted by Ribbink et al. (1983), Fryer (1957:350) regarded the genus Pseudotropheus as being ‘“‘rather ill-defined.’ Pseudotropheus xan- VOLUME 102, NUMBER 1 Fig: 1. stomachus differs from other members of the group in coloration. It differs from the only described sympatric member of the group in the number of anal-fin rays, shape of the lower pharyngeal bone, the length of the dentigerous surface of the lower pha- ryngeal bone, and in body shape. Description.— Morphometric ratios and P. barlowi Fig. 2. Lower pharyngeal bones of the holotypes of Pseudotropheus barlowi and Pseudotropheus xansto- machus. ies fe", ag : 2 eA OS eee he ES it ES Holotype (USNM 297268) of Pseudotropheus xanstomachus. meristics are presented in Table 1. Body moderately compressed and elongate; jaws isognathous (Fig. 1). Teeth on lower jaw in 3-4 rows, those on premaxilla in 4 rows; teeth in outer rows bicuspid, with occasion- al conical lateral tooth in some individuals; teeth in inner rows tricuspid; 12 teeth in outer row of left lower jaw of holotype, 9- HAA 7) 4 3 ee” h lineal Ate, P xanstomachus 10 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Table 1.—Morphometric characters and meristics of Pseudotropheus xanstomachus. Range includes holotype and 15 paratypes. 12 in paratyes. Pectoral fins with 13 rays in holotype and 10-14 in paratypes; anal fin with 7 rays in holotype and 6-7 in para- types; caudal fin emarginate. Vertebrae of holotype 14 + 14 (abdominal + caudal); paratypes 12-14 + 14-15. Lower pharyn- geal bone of holotype triangular in outline, length of dentigerous surface 59% of lower pharyngeal bone length; pharyngeal teeth in left posterior row 23, those in left median row, 13. Holotype with 5 scale rows on cheek, paratypes with 5-6; pored scales along Holotype Mean SD Range Standard length, mm 63.3 62.9 Tell 47.0-78.5 Head length, mm DOS 20.4 2.4 15.3-26.0 Percent Standard Length Head length 32.4 32.4 0.7 31.5-33.4 Snout to dorsal By) 33.3 1.2 30.9-35.0 Snout to pelvic 43.4 43.1 3 40.8-45.2 Greatest Body depth 36.7 34.2 1.4 31.8-36.5 Caudal peduncle length 12.8 13.5 i) 11.2-15.5 Least caudal peduncle depth 13.0 12.9 0.3 12.3-13.4 Pectoral-fin length 26.5 25.6 1.8 22.4-28.2 Pelvic-fin length 31.8 ihe 4.5 21.6-36.4 Dorsal-fin base length 60.7 60.4 1.1 58.6-62.2 Percent Head Length Horizontal eye diameter 30.7 313 1.1 28.5-32.8 Vertical eye diameter 30.2 30.9 123 28.1-—33.3 Snout length 33.7 35.1 1.4 33.2-37.7 Postorbital head length 40.5 40.0 0.8 38.5-41.2 Preorbital depth DAES) 20.3 12 18.2-22.6 Lower jaw length 34.6 33.6 12 32.0-36.5 Interorbital width 28.3 28.3 2.4 25.3-33.6 Cheek depth 30y 30.0 2.8 24.5-34.4 Head depth 98.5 95.1 3.0 91.1-100.1 Counts Lateral line scales 30 29.9 0.5 29-31 Scale rows on cheek 5 5.4 0.5 5-6 Dorsal-fin spines i 7s 0.5 16-18 Dorsal-fin rays 8 7.9 0.4 7-8 Pectoral-fin rays 13 13.3 1.0 10-14 Anal-fin rays 7 6.9 0.3 6-7 Gillrakers on first ceratobranchial 12 10.8 0.9 9-12 Gillrakers on first epibranchial 3 2.5 0.5 2-3 Teeth in outer row of left lower jaw 12 10.7 ital 9-12 Abdominal vertebrae 14 13.6 0.8 12-15 Caudal vertebrae 14 14.7 0.5 14-15 lateral line of holotype 30, and of paratypes 29-31; pored scales posterior to hypural plate 2, with exception of two paratypes which had scales missing from this area. Gill rakers simple, first gill arch of holotype with 12 on ceratobranchial (9-12 in para- types); 3 on epibranchial of holotype and 2-3 in paratypes; and | between epibran- chial and ceratobranchial. Body coloration in freshly collected males light blue with six black vertical bars; head dark blue with one light blue interorbital VOLUME 102, NUMBER 1 11 Table 2.—Sheared principal components (shape factors) of the untransformed morphometric data for Pseu- dotropheus xanstomachus (n = 16) and Pseudotropheus barlowi (n = 10). Sheared Size PC 2 PC 3 Standard length O.215 —0.021 —0.082 Head length 0.207 =O —0.108 Horizontal eye diameter 0.183 0.095 —0.154 Vertical eye diameter 0.189 0.048 —0.048 Snout length 0.231 —0.088 eros Postorbital head length 0.193 —0.107 —0.048 Preorbital depth 0.282 == Ue ly 0.042 Lower jaw length 0.210 0.070 —0.048 Interorbital width 0.275 —0.065 —0.014 Snout to dorsal fin origin 0.212 0.052 —0.149 Snout to pelvic fin origin 0.261 —0.064 etsy Body depth 0.231 0.136 —0.050 Cheek depth 0.169 —0.594 0.447 Head depth 0.229 0.010 —0.067 Caudal peduncle length 0.219 —0.459 0.206 Least caudal peduncle depth 0.215 0.048 —0.050 Pectoral-fin length 0.258 O55 —0.158 Pelvic-fin length 0.311 0521 0.728 Dorsal-fin base length 0.215 —0.009 —0.069 bar, yellow gular and branchiostegal rays; dorsal fin medium blue with grey flecks and light blue marginal band; pectoral fins black; pelvic fins black anteriorly fading to yellow- brown posteriorly; anal fin blue; males with three to five yellow ocelli on anal fin. Body coloration of females similar, but some in- dividuals have light brown body coloration with brownish cast to fins. The description of the coloration and the color plate of the males in Ribbink et al. (1983:162; plate 2a) agree with the above description, except that they noted between 1-5 ocelli on the anal fin. Ribbink et al. (1983:162) note that the females are “‘dark brown sometimes almost black with darker bars ....’” The differences in color of the females may be associated with breeding coloration and may be influenced by the time of the year when the fish were ob- served. However, all descriptions of the fe- male coloration note a yellow chin and gular region. Etymology.—The specific epithet is de- rived from the Greek “‘xanthos” and “‘sto- machus”’ meaning yellow throat, which char- acterizes the yellow gular region present in both sexes. Discussion. —Pseudotropheus xanstoma- chus is morphologically similar to the P. zebra complex in that it has a terminal mouth, has three or four rows of teeth, of which the outer rows are bicuspid, with the occasional conical lateral tooth, and the in- ner rows are tricuspid (see Ribbink et al. 1983). The only sympatric species of this complex which is described is P. barlowi, from which P. xanstomachus differs in col- oration. P. barlowi males are bright gold, and the females are uniformly brown (McKaye & Stauffer 1986). Differences in color patterns among cichlids, especially the male’s, generally are recognized to be suf- ficient to delimit valid species (Greenwood 1981, Hoogerhoud & Witte 1981). In addition to coloration differences, P. xanstomachus has six or seven anal rays while P. barlowi has eight. The shape of the lower pharyngeal bone between the two species also differs. The angle of the suture 12 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON SHRD_PC3 -0.025 -0.050 -0.075 -0.100 =O. 125 =O2030 “0.260 ""-0.15>,°-0.10 -0.05 0.00 @ 0.05 SHRD_PC2 Fig. 3. Plot of the sheared principal components of Pseudotropheus xanstomachus (solid) and Pseudotropheus barlowi (open). of the two posterior halves of the lower pha- ryngeal bone is more acute and the resultant depression is greater in P. barlowi (Fig. 2). Moreover, the length of the dentigerous sur- face of the lower pharyngeal bone of P. bar- lowi was 76% (range = 74—78%) of the length of the bone (n = 3; USNM 274782; USNM 274783), while the length of the dentigerous surface of the lower pharyngeal bone of P. xanstomachus was 62% (n = 4; range = 57— 67%). An attempt was made to determine if there were differences in body shape between the two described sympatric species of the P. zebra complex using a sheared principal component analysis. Data for P. barlowi were obtained from the original data sheets used by McKaye & Stauffer (1986). Sheared principal component analysis demonstrated that there was no overlap between species when the first sheared principal component was plotted against the second sheared prin- cipal component (Fig. 3). The first principal component is interpreted as a size compo- nent and the sheared components as shape, independent of size (See Humphries et al. 1981, Bookstein et al. 1985). Thus, these data were calculated using the untrans- formed values of the morphometrics rather than percent standard length or percent head length. Those morphometrics which have the highest loadings on the first sheared principal component are cheek depth, pel- vic-fin length, and caudal peduncle length, while those which have the highest loadings on the second sheared principal component are pelvic-fin length, cheek depth, and snout length (Table 2). All of the specimens reported herein were captured at a depth between 7—12 m at Na- kantenga Island. Ribbink et al. (1983) re- ported this form from all three Maleri Is- lands: Namkoma, Maleri, and Nakantenga. They stated that it was most common be- tween depths of 2-8 m, and was rare in water deeper than 12 m. Conversely McKaye & Stauffer (1986) stated that P. barlowi occurred primarily at depths greater than 10 m and hypothesized that the oc- currence of these brightly colored forms in VOLUME 102, NUMBER 1 deeper water may be an adaptation related to avoidance of surface predators (i.e., birds and otters). Therefore, even though P. xan- stomachus and P. barlowi are indigenous to the same islands, they are in effect allotopic. Acknowledgments We thank the government of Malawi for providing the facilities to make this research possible. We thank L. Knapp of the Smith- sonian Institution who arranged for ship- ment of specimens from Malawi to the USNM. We benefited from discussions with K. R. McKaye. We are especially thankful to D. Swofford who provided the SAS pro- gram to conduct the sheared principal com- ponent analysis. The original art work was completed by M. Katz. Literature Cited Barcel ©. Dp N.. M. J. O. Van Oyen, F. Witte, & E. L. M. Witte-Mass. 1977. An introduction to the taxonomy and morphology of the haplochro- mine Cichlidae from Lake Victoria. Part A. Text. — Netherlands Journal of Zoology 27:333- 389. Bookstein, F., B. Chernoff, R. Elder, J. Humphries, G. Smith, & R. Strauss. 1985. Morphometrics in evolutionary biology. Special Publication 15. The Academy of Natural Sciences of Philadelphia. Philadelphia, Pennsylvania. 277 pp. Fryer, G. 1957. A new species of Gephyrochromis (Pisces: Cichlidae) from Lake Nyasa, with notes 13 on its ecology and affinities.—Revue de Zool- ogie et de Botanique Africaines 55:347-352. Greenwood, P. H. 1981. The haplochromine fishes of East African lakes. Cornell University Press, Ithaca, New York. 839 pp. Hoogerhoud, R. J. C., & F. Witte. 1981. Revision of species from the “Haplochromis” empodisma group. Revision of the haplochromine species (Teleostei, Cichlidae), from Lake Victoria, Part II.—Netherlands Journal of Zoology 31:232- 274. Humphries, J. M., F. L. Bookstein, B. Chernoff, G. R. Smith, R. L. Elder, & S.G. Poss. 1981. Multi- variate discrimination by shape in relation to size.—Systematic Zoology 30:291-308. Lewis, D., P. Reinthal, & J. Trendall. 1986. A guide to the fishes of Lake Malawi National Park. World Wildlife Fund, Gland, Switzerland. 72 pp. McKaye, K.R., & J. R. Stauffer, Jr. 1986. Description ofa gold cichlid (Teleostei: Cichlidae) from Lake Malawi, Africa.—Copeia 1986:870-875. Regan, C. T. 1921. The cichlid fishes of Lake Nyara.— Proceedings of the Zoological Society of London 1921:675-727. Reyment, R. A., R. E. Blackith, & N. A. Campbell. 1984. Multivariate morphometrics. Academic Press, New York, New York. 233 pp. Ribbink, A. J., B. A. Marsh, A. C. Marsh, A. C. Rib- bink, & B. J. Sharp. 1983. A preliminary sur- vey of the cichlid fishes of the rocky habitats in Lake Malawi.—South African Journal of Sci- ence 18:149-310. School of Forest Resources, The Penn- sylvania State University, University Park, Pennsylvania 16802. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 14-32 ASCIDIANS COLLECTED AROUND THE GALAPAGOS ISLANDS USING THE JOHNSON-SEA-LINK RESEARCH SUBMERSIBLE Claude Monniot and Francoise Monniot Abstract.—Ascidians were collected for the first time by a manned sub- mersible on ocean-bottoms between 300 and 800 meters around the Galapagos Islands. Solitary forms dominate; among the eight species collected, five are new ones: Polyclinum johnsoni, Ciona pomponiae, Situla rineharti, Ascidia fusca, and Styela psoliformis. They belong to surprisingly diverse families and several have deep-sea characteristics. The fauna of the eastern part of the trop- ical Pacific Ocean is poorly known, espe- cially the ascidians. Tokioka (1972) report- ed on a small collection of ascidians from the coast of Costa Rica, and recently Millar (1988) identified some specimens from the Galapagos and Ecuador. Nothing else is re- ported about ascidians between Baja Cali- fornia and Chile. In November 1986, an expedition to the Galapagos Islands collected deep-water or- ganisms for pharmacological studies. Over 600 animals were collected by the R/V Sew- ard Johnson and Johnson-Sea-Link- I manned submersible (Harbor Branch Oceanographic Institution, Fort Pierce, FL) using a manipulator arm equipped with a claw, a suction tube, and a grab sampler. Among this collection there are eight species of ascidians, five of which are new species. The material is particularly interesting because the specimens were collected un- damaged on rocky bottoms, where a dredge or any blunt device monitored from a sur- face boat cannot operate. The animals are unusually large compared to the size of the ascidians collected in shallow water by SCUBA during the same cruise and relative to the deep-water ascidians on soft bottoms elsewhere. Observation from the submersible during several dives suggests that ascidians are not evenly distributed on the bottom, but live in patches in restricted areas. They grow attached to vertical walls, in small caves, or on large cobbles; they are directly in contact with loose sediment. The solitary forms seem more abundant in deep water than colonial ones, a situation opposite to that in shallow water areas out- side of the Galapagos Islands. This may be due to the collecting method: solitary ascid- 1ans, especially large ones, are easily seen from the submersible and can be collected, but colonial ascidians normally live in crusts on the undersides of rocks or pebbles, or in deep crevices, and so escape notice. The col- onies reported here were attached to cob- bles. Of the eight species collected, two are co- lonial. They both belong to the family Poly- clinidae (order Aplousobranchiata). One is a new species of the genus Polyclinum, named P. johnsoni after the submersible and ship. The other species is probably Aplidium californicum (Ritter & Forsyth 1917), one of the most common Polyclinidae on the shore nearby, but the samples are too small and not fully enough developed to verify their identity. The other ascidians belong to surprisingly diverse families: one Cionidae, two Ascidiidae, and one Octacnemidae among the order Phlebobranchiata; and one Styelidae and one Pyuridae in the Stolido- VOLUME 102, NUMBER 1 branchiata. Several of these solitary ascid- ians have deep-sea characteristics: Ciona pomponiae, n. sp. has a particularly solid, noncontractile tunic, and a very small gut compared to the branchial sac; Situla rine- harti, n. sp. belongs to a typical bathyal fam- ily (Octacnemidae); Styela psoliformis, n. sp. has the same characteristics as other deep-water species of that genus. The presence of a deep-water ascidian fauna around the Galapagos, different from the shore species collected by SCUBA, is not surprising. The bottom temperature at 500-700 m was between 7°C and 5.5°C. The water near the bottom was rich in suspend- ed particles, but it is not known whether the particles were plankton except for the nu- merous crustacean larvae observed. Type specimens are deposited at the Smithsonian Institution, National Museum of Natural History (USNM). Sorted sam- ples received a Sea Pharm number (SP), in- dicated here for each specimen. Polyclinidae Polyclinum johnsoni, new species - Fig. 1A, B, C, D Holotype. —USNM 18249; SP 25-XI-86- 35 iif: Description. —Two colonies were collect- ed close to Punta Espinosa, Fernandina Is- land, at 306 m depth, attached to a sponge underneath a large piece of rock. The colony retained as a taxonomic voucher is a cush- ion 2.5 cm in diameter. Color in life pale yellow with translucent tunic through which yellow zooids were clearly visible. Branchial sac and internal papillae obscured by an or- ange-yellow pigment. Zooids situated on either side of cloacal canals that converge towards the center of the colony where col- ony’s sole common cloacal aperture opens. The zooids have a large size range. Tho- rax large compared to the abdomen and the post-abdomen (Fig. 1A). Oral siphon star- shaped with six triangular pointed lobes above a strong sphincter that closes the si- 15 phon into a narrowed tube. Oral tentacles vary in number with the zooids and are in- serted in at least three circles, with three or four orders of length, the largest being dor- sal. At least 40 oral tentacles can be counted ‘in the largest zooids. The peripharyngeal band lined with two high laminae and not curved at the level of the dorsal tubercle. Cloacal aperture close to the oral siphon and provided with a sphincter which may make the aperture into a tube when contracted. Dorsal lappet (Fig. 1A) well developed and inserted on a large base; not wide but its length, which varies according to the loca- tion of the zooid in the colony, can reach at least the length of the thorax; has two lon- gitudinal muscular bands (Fig. 1A). There is a rounded button under the cloacal ap- erture, as is usual in the genus. Thoracic musculature is weak; longitudinal fibers from the oral siphon stop very quickly and do not pass the level of the first row of stig- mata; there is an average of eight muscles on each side. Branchial sac, in both the live and pre- served animals, visible by transparency; the transverse vessels underlain by muscular fi- bers and bear high papillae (Fig. 1B) con- taining an orange-yellow opaque pigment. The number of rows of stigmata is variable according to size of zooids, and divisions of stigmatal rows commonly seen. In the col- ony studied there is a maximum of 16-17 rows of stigmata. In this example the fourth row 1s divided as follows: 25 stigmata on the right and 23 on the left side with 16 papillae on the right and 15 on the left on the fourth transverse vessel. Branchial sac not perforated along the endostyle or under the rapheal papillae. Dorsal languets short and wide, only slightly displaced to the left side. The whole branchial sac has a rect- angular shape with a right angle at the base of the endostyle (Fig. 1A). Abdomen slightly twisted; esophagus short; the stomach placed anteriorly is sud- denly cut in its pyloric part (Fig. 1C). There is a ring-like post-stomach; intestine not 16 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON |) ane e A (\ — ae j at Fig. 1. Polyclinum johnsoni: A, Zooid; B, Detail of the branchial sac; C, Digestive tract; D, Larva. Ciona pomponiae: E, Animal without tunic, right side; F, Neural region; G, Gonads on the digestive loop; H, Extremities of gonoducts. VOLUME 102, NUMBER 1 further differentiated into regions (Fig. 1C). Anus opens at the level of the 7th or 8th row of stigmata and has two lips. Post-abdomen egg-shaped, linked to the abdomen by a thin peduncle (Fig. 1A); ovary is anterior followed by a cluster of testes. The heart is terminal. One or two vascular appendices extend from the post-abdomen into the test. Larvae (Fig. 1D) incubated in the cloacal cavity. The zooids contain 1-3 larvae. The trunks measure 550 wm. They have 3 ad- hesive papillae, 7 pairs of thick epidermal papillae arranged on a line on each side of the body except for one pair which is lightly displaced inside, and there are two areas of epidermal vesicles on each side, one dorsal and the other ventral (Fig. 1D). Remarks.—This species differs from all other Polyclinum with more than 15 stig- mata rows in having higher papillae on the transverse bars, a large number of stigmata per row, and a peculiar distribution of the pigments in the colony. The genus Polycii- num is very homogeneous and the anatom- ical differences between the species are slight, sO it is not surprising that deep-water species do not differ substantially from shallow- water species. | There is only one Polyclinum species known to live deeper than P. johnsoni, n. sp.; P. neptunium Hartmeyer, 1912, col- lected at 106 m and 318 m off the Cape of Good Hope. The species is named after the submers- ible from which it was collected. Cionidae Ciona pomponiae, new species Figs. LE, F, G, H,, 2A, B Holotype. —USNM 18247, SP 21-XI-86- 2-1. Description. —The unique specimen mea- sures 15 cm in length; attached by the left posterior side; oral siphon terminal; cloacal aperture located '3 the way down the dorsal 17 side (Fig. 2A). Both siphons sessile. Test soft, gelatinous, colorless in life and free of for- eign particles; is at least 5 mm thick and does not appear to consist of several layers as in Ciona intestinalis. Body contracted in- side tunic and no longer attached to it, even at the level of the siphons; size of body re- duced to 6.9 cm. Tunic much less retractile than in other Ciona species. Musculature on each side (Fig. 1E) forms four muscular ribbons initiated from the oral siphon and two ribbons from the cloacal siphon. The two most dorsal muscles of the oral siphon and the one most ventral muscle from the cloacal siphon gather to form one ribbon in the posterior part of the body. The two ventral muscular bands issuing from the oral siphon become narrow before reaching the posterior part of the body and two muscles reach the bottom of the bran- chial sac (Fig. 1E). There is a network of transverse fibers. This small number of muscular bands is peculiar to this species. There are few oral tentacles (16 large ones and several very small) placed without or- der on acrest. The length of some tentacles allows them to protrude through the oral aperture. The peripharyngeal band consists of two unequal laminae; the anterior thin and high, the posterior low and thick. There is a marked dorsal V in which the neural duct opens as a simple slit (Fig. 1F). Neural gland close to the nerve ganglion. Dorsal languets have an increased length poste- riorly, measuring 6 mm in the anterior 4 and 18 mm near the esophagus. Branchial sac (Fig. 2B) thin, the trabec- ulae connecting it to the body wall long. Transverse vessels of several orders regu- larly distributed; those of the first order wide and protrude into the branchial cavity, those of the third or fourth orders are thin laminae protruding into the branchial cavity. They bear large papillae that are flattened longi- tudinally and form hooks above the longi- tudinal bars. Longitudinal bars thin; stig- mata elongated, generally numbering six to 18 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Ciona pomponiae: A, Group of in situ individuals (from a submersible videotape); B, Part of branchial sac. C: Ascidia clementea part of the branchial sac with dorsal lamina. Situla rineharti: D, Part of the branchial sac; E, Habitus left side; F, The same without tunic. (Scales: A = 10 cm; B, C, D = 1 mm; E, F = 1 cm.) VOLUME 102, NUMBER 1 eight in a mesh; most crossed by a high parastigmatic vessel bearing papillae (Fig. 2B); often divided under this vessel. If the division is complete, the stigmata on each side of the vessel are shorter than the others, and a very thin new parastigmatic vessel without papillae can occur above them. Digestive tract clearly situated under the branchial sac; enlarged stomach has internal plications visible by transparency; most posterior fold prolonged and ends in a small ampulla at its junction with the intestine; intestinal wall thin and gut contents can be seen through it. Rectum elongated and ends in a non-lobated narrow anus; posterior in- testine encircled by a well developed pyloric gland. The pear-shaped ovary is located under the intestinal loop (Fig. 1E, G). Testis dif- fuse, consisting of numerous acini which coat the intestinal wall; ducts join to form a com- mon sperm duct at the level of the anterior part of the ovary; i.e., oviduct and common sperm duct originate at the same point. Gonoducts contain large numbers of eggs (400 wm in diameter) and spermatozoa, and pass beyond the anus; oviduct opens in a flat horseshoe-shaped papillae (Fig. 1H). Male papilla has several small apertures; there is no pigment spot at this level. Remarks.—This species is very uncom- mon for a Ciona. Although very few species occur in shallow waters, the genus is better differentiated deeper on the continental slope. In the northeast Atlantic is found Ciona gelatinosa Bonnevie, 1896 and Ciona imperfecta Monniot & Monniot, 1977, and in the northeast Pacific Ciona mollis Ritter, 1907. Ciona mollis, known from California at 2011 m depth off San Nicolas Island, differs from the new species in several important characters: C. mollis’s size is smaller (3 cm maximum) and its tunic is very soft. There are 6 muscle bands on each side of the body, all of them reaching the posterior part where they fuse. There is circular musculature only on the siphons. The oral tentacles are very 19 numerous, more than 200, while the present specimen, much larger, has only 16. This difference is perhaps not as significant as the reduction of the number of oral tentacles even with increased size in Ascidia translu- cida according to Millar (1960) and in Cnemidocarpa verrucosa according to Mon- niot (1978). In C. mollis, furthermore, the digestive tract does not have the same shape as in this specimen, C. mollis’s intestine curves immediately after the stomach, and its gonoducts do not open near the anus. Ciona mollis seems closer to the Atlantic species C. gelatinosa Bonnevie 1896, re- described by C. Monniot (1970), in the mus- culature (7 bands), the shape of the gut, and the location of the genital papillae. The species is named after Shirley Pom- poni, co-chief scientist of the cruise. Octacnemidae Situla rineharti, new species Figs. 2D, E,;F, 3A, B, C, D Holotype. —USNM 18244; paratype USNM 18245; SP 14-XI-86-1-2 and 18- XI-86-2-11. Description. —Among several samples collected, two specimens have been exam- ined: one was designated as the holotype, collected north of Floreana (Santa Maria Is- land) at 790 m depth, and another (para- type) collected south of Genovesa (Tower Island) at 695 m depth. All specimens col- lected are approximately the same size, al- most spherical, with a cartilaginous white tunic that is translucent more than trans- parent (Fig. 2E). Holotype ovoid, attached by the small ventral end (7 x 5 xX 5.2 cm). The part of the tunic attached to the sub- stratum torn but represents a narrow area of attachment; in other specimens there is no particular differentiation of the attach- ment area. Oral aperture a gaping transverse slit, made of two large lips located at half the height of the body (Figs. 2F, 3A). Dorsal lip protrudes more than ventral one. Cloacal 20 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON aperture not obvious; it is a simple hole at the upper part of the body slightly displaced to the dorsal side (Fig. 3A). Tunic on the two lips of the oral siphon is thin, cartilag- inous, and glossy, radially wrinkled, and dif- ferent from the thick test (at least 3 mm) around the rest of the body. Border between the two kinds of tunic marked by a groove at the limit of the lips. Removed from the tunic, the body ap- pears composed of three parts: the oral si- phon formed of two well developed lips, a branchial cavity widely spread separated from the oral siphon by a ring of tentacles, and a “‘nucleus” containing the gut and go- nads. The musculature is complex (Fig. 3A, B). The muscles of the oral siphon, independent of the body musculature, include radial fi- bers regularly distributed on both lips; these end at the circle of oral tentacles and the peripharyngeal groove. The oral siphon’s circular fibers are also regularly placed, spread over both lips and gathered at the lip corners. At each of those corners is a fan of fibers belonging to the radial muscula- ture, connecting the corners to the large muscle located at the level of the ring of oral tentacles. Musculature of the cloacal siphon con- sists of radial and circular fibers, weakly de- veloped and anastomosed. It is limited to the immediate vicinity of the siphon. A large, strong ribbon of muscle fibers encircles the body above the ring of oral tentacles, and has a horseshoe shape opened on each side of the endostyle at the level where the body attaches to the substratum (Fig. 3A). A muscular string binds the rib- bon’s two free extremities. There are also two areas of transverse muscles dorsally, and ventrally two bundles more or less parallel to the endostyle, connected to the “‘string”’ linking the posterior extremities of the large horseshoe muscle ribbon. Oral tentacles (Fig. 3C, D) situated on a rim located posterior to the horseshoe mus- cle-band. Dorsally the rim is low; its height increases ventrally where it is lined by a flat muscular band. Tentacles have a unique leaf- shaped structure, narrowed at their inser- tion on the rim. On the anterior side of each tentacle is an ampulla which stains very deeply with hemalum. The tentacles are of two regularly alternating sizes (Fig. 3C). The peripharyngeal groove is far from the ring of tentacles in the dorsal half of the body but comes close to it in the ventral part. Dorsally, a series of irregular crests separate the peripharyngeal groove and the tentacles and they may be considered as the anterior rim of the peripharyngeal groove. Dorsally the peripharyngeal groove is deep- ly incurved (Fig. 3D) to reach the dorsal tubercle. The latter is rather far from the neural ganglion; its aperture is a simple hole. The neural gland is located on the left pos- terior side of the neural ganglion. There is no differentiated dorsal lamina. The restricted space between the dorsal tu- bercle and the opening of the esophagus is marked by transverse elevations continuous with more or less regular internal transverse crests on the branchial sac; these elevations can be considered as transverse vessels. There is a short endostyle originating near the oral tentacles and ending far from the entrance of the esophagus (Fig. 3A, B). At its posterior extremity, on the left, is a ret- ropharyngeal groove which initially consists of a single rim but divides in two wide and flat ridges. The entire surface placed between the peripharyngeal band and the branchial stig- mata is covered with small papillae. Bran- chial cavity cup-shaped with the bottom close to the digestive tract. The perfora- tions, limited to two small areas in the flat bottom of the cup on each side of the re- tropharyngeal band, lie in thick tissue. The perforations are oval (Fig. 2D) and generally grouped in pairs; they are not ciliated, and are larger than in the other known species of Octacnemidae. The digestive tract forms a simple loop (Fig. 3B); esophagus opens by a simple hole VOLUME 102, NUMBER 1 21 om Fig. 3. Situla rineharti: A, Right side of the animal without tunic; B, Postero-dorsal side; C, Oral tentacles; D, Peripharyngeal groove indentation,tentacles and neural ganglion. Ascidia clementea: E, Left side of the body, tunic removed; F, Dorsal part of the tentacle ring and peripharyngeal groove; G, Intestinal loop with ovary and oviduct. a2 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON in the branchial sac; stomach is wide and has a glandular wall which appears some- what wrinkled but has no internal plications (Fig. 3A, B); its external oblique ridges may be due to contraction. The intestine is thin and transparent, ending in a plain-edged anus placed beside the esophageal entrance. The digestive tract and gonads are embed- ded in a thick mesenchyme. The retro- pharyngeal groove lies beside the middle of the gut loop and indicates that the stomach is on the right side. The gonads (Fig. 3A, B) consist of a mas- sive and protrusive ovary located between the two branches of the digestive loop; testis is composed of numerous acini; it is flat and covers the ventral part of the ovary and each side of the intestine. The oviduct opens on the medial side of the intestine a short dis- tance before the anus. The spermduct, full of spermatozoa, opens next to the oviducal aperture on a small papilla. The heart lies alongside the intestine. Remarks. —Octacnemidae having an oral aperture with two large lips belong to four genera: Dicopia Sluiter, 1905; Megalodico- pia Oka, 1918; Situla Vinogradova, 1969; and Cibacapsa Monniot & Monniot, 1983. Cibacapsa is characterized by the total ab- sence of a branchial sac. The distinctions between the other genera are less obvious. The difference between Dicopia and Meg- alodicopia is the presence in the latter of a peduncle, which in our opinion is not a dif- ference of much importance. Dicopia differs from Situla by the presence in Dicopia of a true branchial cavity with a conical perfo- rated area and oral tentacles forming a ring of a smaller diameter than that of the bran- chial cavity. In Situ/a the branchial cavity opens widely and the perforated area is in a flat disk around the digestive tract. The Galapagos species is closer to Situla. The main differences between the species of Di- copia and Situla are summarized in Table 1. The new species is the only one having a large imperforate space between the peripharyngeal groove and the branchial tis- sue, and its oral tentacles have a very orig- inal structure. Ritter (1907) has incompletely described a species of Octacnemidae collected off San Diego, California: Benthascidia michael- seni. His account suggests he did not un- derstand the anatomy of the animal very well. The two specimens of that species pre- served at the Smithsonian Institution are dissected and their organs isolated, and so it is impossible to reconstitute their original disposition in the animal. In any case Rit- ter’s material cannot be of the same species as the new Galapagos one. The species is named after Kenneth Rine- hart, co-chief scientist of the cruise. Ascidiidae Ascidia clementea, Ritter, 1907 Figs. 2C, 3E, F, G SP 23-XI-86-3-27. Description. —One specimen was collect- ed north of Isabella Island at 335 m depth. The ovoid body is attached to the substra- tum by the posterior part of the left side. The maximum length of the animal is 6.8 cm. Oral aperture terminal; cloacal aperture located at the anterior 14, the distance be- tween the siphons being 2.9 cm. The tunic in life is yellowish, covered with small cy- lindro-conical papillae. Papillae and grooves of the tunic are pigmented with ochre; both apertures are 6-lobed. The test is partially covered with epibionts: foraminifera, poly- chaete tubes, bryozoans and molluscan egg- capsules. One of the cheilostome bryozoans consists of thecal rows, each zooid having a long ventral extension penetrating deeply into the ascidian’s tunic; the bryozoan col- ony is raised above the tunic surface by these extensions. Thickness of the tunic averages 2 mm; its internal side is soft and translu- cent. Body wall thin and transparent; the mus- culature forms 2 bands of transverse parallel fibers—a well developed dorsal band, and a smaller ventral band—and longitudinal 23 VOLUME 102, NUMBER 1 dno ev jo W10}10q 941 18 Svole ie Z SULI poyel -Ojiod A[[ny yey SULI po}el -ojiod Any 1ey SULI poi! -Ojiod Any 1ey po -je1oj.iod Aye -191e] “SULI 1eYy podeys 9u09 SULI polel -Ojiod Aq[ny yey podeys 9u09 podeys su09 podeys ouo0o oes [eIpourig suo] yoys yoys suo] yoys wos yoys yoys yoys yoys Bore Jeno -19Qni Log A][es1op oes jeryouriq wod 1Ry ‘sg[deB]UD}] WIOIY 1ey S9[Oe} -U9} WOIJ Ie} ‘oes jetyoueig 0} 9so[9D oes [eryoursg 0} 9so[9 *‘so[0e]U9} WO IRj A][VUusA 1e9U ynq ovs [eTyouRIq wo Jey AT[es1op oes jeryoursqg 0} 9sojO oes jeryouviq pue S$9]OR]UD} 0} 9SOO oes [eryoursq 0} 9sojo ovs [eryouRrlq pur $9[O1UD} 0} 9SOTO ovs [eryouRrlqg pur S9[9"1UD} 0} BSO]O oes [eIyouRIg pur S9JOR1UD} 0} BSO]O 9A0018 [eaduAIeYdog oes [eryoursq pue dA0018 [vod -uAreydiiod us9M10q 9AO00I3 [Od -uAreydiiod pur $9[9e1U9} U99M19q 9AO00I3 [e938 -uAieydiiod pur $9[9B1U9} U99M19q Poquiosop 10U 9A00I18 [vod -uAreyduod pur $9[9e]U9} U99M10q $9[9P1UD}] 0} JOLIOJUR 9AOOI3 [v93 -uAieydiuod pue S9[0e1U9} U99M19q 9A00I18 [e938 -uAieydiiod pur $9[9B1U9} U99M19q uogos 10U uoos JOU aei[ided A1osuag 90119 posies SUOIXO]J “Ur qi oul] podoyyeos o1un} Yory) YIOOWS ‘sdij woys ‘oroyds o1uny Asrey uryy ‘sy odie] ‘ojouNnpod y10Ys oun} YJOOUS sosedrey (purjs] pre -uOqoeP) uvIDg uerpuy YINos ‘ds ‘u ‘1JADYOULA JONG LL6I “A “SD loruu0yy IpjDUuOpIDUL DNS CL6| “eAopeia SUI] [BAO ‘sdij odie] ‘ojounpod BOS BI}IONS -OULA ISUIDGAd DINTIS cL6l o1un} YIOOWS UI} ‘BAOPRISOULA DID] oul] [BAO ‘sdij ou ‘ojounpod BIS BITIONS -NIDIUAININU VINIIS SUOIXO]J orun} “Ur ¢ YIM Arey uty} ‘sdiy IN0kRW €L61 “A 7 “OD 101U oul] B UO odie] ‘oyounpod y10Ys odoing -UO| VSOUD] VINIIS oruny Arey sul urIy} ‘sdi] o91K] ZL6I “OC 1OTUUO|J posie1 Be uO ‘Q[ISssos 10 pojounpod odoing WMnUIYyAdUD DIdOJIG oruny 6961 sult YyIoows ury}) ‘sdiy ‘BAOPPIZOUI A, posrel e UO odie] ‘opounpod y10Ys youol olny psojnoijjad vjinj1s orun} Airey ‘sdiy odie] BIS [[J9PPIM 6961 ‘NOY uedef EC6I ‘PAOLJOL ouly podoy o1un} YIOOUIS SI6I ‘RAO -[eos B UO ‘sdij 110Ys ‘ojounpod uvdes suvly vidoo1pojvsapw sd odie] Z E161 “BAO j Juosqe ‘oeyjided yim o1oyds uvdese poniuodnvl vidovig sdtj S061 “191INIS u99S 10U odie] 7 ‘o1oyds Arey BISoUOpU] vIpiuquy vidoriq soit L odeys Apog uonngiNsiq osWIeN ‘e1ouos DIdoIIpojvsay pue vidoIIG ‘vINIIS UI sotdads dy} Ud9MI0q SUOSLIRdWIOD—"]| 91qB 24 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON muscle fibers extend from the oral siphon. On the right side all the muscles spread and intermingle to make a loose network. On the left side the longitudinal fibers extend only a short way from the oral siphon, and most of the left body wall is devoid of mus- culature. Seventy oral tentacles arise from an ele- vated rim that has a muscular ring. The tentacles are of at least four orders of size, regularly alternated although the smallest ones are not developed everywhere. Peri- pharyngeal groove made of two unequal laminae, the anterior one being larger, is close to the tentacles, and the space between is covered with thin papillae (Fig. 3F). It does not make a deep ‘V’ dorsally; the dorsal tubercle is low, J-shaped. Neural ganglion distant from the dorsal tubercle; neural duct is twice the length of the neural ganglion. Rapheal band consists of two laminae which measure five times the length of the dorsal tubercle. Posteriorly, its edge is higher and carries teeth that coincide with the trans- verse vessels (Fig. 2C). After passing around the esophageal entrance it becomes irregu- lar. On the right side close to the esophagus the transverse vessels end without differ- entiation. Branchial sac thin and flat (Fig. 2C). At the level of the top of the intestinal loop there are 100 longitudinal vessels. Main pa- pillae are located at the junctions of the lon- gitudinal and transverse vessels, and almost everywhere in the branchial sac there are smaller intermediate papillae, which are not linked to the presence of parastigmatic ves- sels. These vessels exist only where there is duplication of a stigmata row. There are four to six stigmata in a mesh, except on the right side, where the meshes located near the esophagus have more than 20 stigmata. The gut forms an open loop with an ac- centuated secondary curve (Fig. 3E). The stomach appears plicated externally (Fig. 3E, G). The intestine is deeply embedded in a mass of large renal vesicles which spread over the body wall. The anus is attached to the body wall and has two slightly scalloped lips. The specimen was not sexually mature. The ovary, a network of tubes inside the intestinal loop, does not spread out onto the intestine (Fig. 3G). We have not found the testicular acini that Ritter (1907) shows against the stomach. Remarks. —A. clementea has not been re- ported since its description in 1907 based on eight specimens: one collected by the A/- batross near San Clemente Island at 654— 704 fathoms (station 4405), and seven spec- imens at 21.8 miles to the south of San Nic- olas Island, 1100 fathoms (station 4425). There are a few small differences from Rit- ter’s description: he does not mention the tunic papillae and counts eight lobes at the oral siphon instead of six. His figure 33 shows more than 75 small oral tentacles all of equal size. He describes “‘deep narrow plications” of the branchial sac, but his fig. 34 does not show this. In his discussion, he recognizes that these plications do not al- ways exist. All the other characters of our specimen are identical to his description. Ascidia fusca, new species Fig. 4A, B, C, D Holotype.—USNM 18248; SP 20-XI-86- 1-25. Description. — The sole specimen was tak- en at 375 m depth southeast of San Salvador (James) Island. Maximum length 5.6 cm; it was lying on its left side. Apertures distant from each other (4.6 cm); have an undeter- mined number of external large soft swell- ings. Tunic dark brown in life (thus the species name fusca) and its surface wrin- kled. Some foraminifera and sedimentary particles adhere to the settlement surface; elsewhere on the tunic are small epibionts, mostly bryozoans. The test is soft and its internal layer is colorless. Musculature strong and lies entirely on the right side; is interrupted before it reach- es the endostyle and dorsal lamina; com- prises one ventral and one dorsal field, which intermix in the middle of the right side. The fields’ fibers are close together and nearly VOLUME 102, NUMBER 1 joined; siphonal musculature weak. On the right side of the oral aperture an array of about 10 bands blends into both transverse fields and disappears in the first 4% of the body. Oral tentacles arise from posterior part of a velum linked by a muscular ring; there are about 40 large ones and as many very small ones alternating and irregularly developed; bases crooked; peripharyngeal groove made of two unequal laminae: anterior high and thin and the posterior forming a flat ribbon. There is a large space between the tentacle ring and the peripharyngeal groove which is indented into a deep dorsal V (Fig. 4B). Dorsal tubercle is urn-shaped, opening with a simple aperture (Fig. 4B). Neural ganglion far from the dorsal tubercle at a distance of 3 times its length (0.6 cm in the type spec- imen). Dorsal lamina has 2 rims which ex- tend to the posterior part of the neural gan- glion and then form a single lamina that is thin and high. This carries digitiform pa- pillae which prolong the transverse sinuses. The lamina becomes progressively lower and somewhat irregular as it nears the esopha- gus, where it forms a low, toothed crest. At this level on the right side, one of two trans- verse vessels ends in a large lanceolate pa- pilla. Branchial sac flat; at the level of the top of the intestinal loop there are 70 longitu- dinal vessels on the right and 55 on the left, the left side being much more narrow than the right side. Longitudinal vessels very thin and carry fingerlike main papillae where they intersect transverse vessels. There are nei- ther secondary papillae nor parastigmatic vessels. The meshes are elongate and con- tain 2 to 3 stigmata. Gut (Fig. 4A, C, D) small; stomach, clear- ly enlarged, has some plications only visible on its medial side. Intestine inserted inside the wall of the mantle. The 2 lips of the anus have many small lobes. In this specimen a translucent swelling is located close to the anus. It has no discernable internal structure and we do not know if it is a specific char- acter or an artefact. 25 The ovary (Fig. 4C, D) consists of a mass of tubes projecting internally, with edges growing partly over the inside of the intes- tine. The testicular lobules lie on the 2 sides of the gut. The gonoducts open together next to the anus. The renal vesicles are small, almost invisible. Remarks. —Ascidia fusca differs from A.vermiformis (Ritter 1913), another deep- water Ascidia in the East Pacific, by the for- mer’s external shape, the length ofits cloacal siphon and the long posterior extension of its branchial sac. As in several of the rare Ascidia known from the continental and is- land slopes, Ascidia fusca has a relatively small gut compared to the branchial sac, an open primary gut loop, and a flat branchial sac. The species name refers to the dark tunic of the animal. Styelidae Styela psoliformis, new species Fig. 4E, F, G Holotype. -USNM 18246, SP 16-XI- 86-1. Description. —The sole specimen was found in a cavity of a basaltic cobble near Espanola island at 567 m depth. The visible part of the still attached body is an oval disk, 14 x 11 mm, white, covered with low, round, plate-like papillae which have a vas- cular dilation full of blood granules. Around the disk the tunic is thinner and also has vascular ampullae; it strongly attaches the animal to the substratum. Both apertures protrude a distance of 6 mm, but they are located in depressions, so they do not ex- tend beyond the body surface after contrac- tion. Tunic of the central disk opaque and internally pearly. The rest of the body has a thinner tunic that is soft and transparent. Inside the tunic the body is flattened against the substrate. The dorsal part of the body wall is opaque and muscular, the ventral side thin and transparent without muscu- lature. At the boundary between the dorsal and ventral side the mantle has a ring of 26 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 4. Ascidia fusca: A, Left side of the body, tunic removed; B, Dorsal tubercle; C, External side of the gut and gonads; D, Internal side of the gut and gonads. Styela psoliformis: E, Ventral side of the body, tunic removed; F, Internal side of the body, branchial side removed; G, Gonad. tissue rich in tan blood lacunae clearly seen velum. There are at least four different sizes by transparency. which regularly alternate. The oral tentacles About 30 oral tentacles are attached toa are wide and transversally flattened. The thin crest located posteriorly to a large oral peripharyngeal groove has 2 equally pro- VOLUME 102, NUMBER 1 truding rims. It is far from the tentacles on the ventral part, nearer on the sides, and dorsally makes a little but distinct V; it is only curved around branchial folds number 1 and 2. The opening of the dorsal tubercle has the shape of a C opened on the left. The neural ganglion is in contact with it. The dorsal lamina is high and smooth. Branchial sac has 4 folds on each side in the anterior part only; fold number 4 dis- appears in the posterior *4 of the branchial sac. Longitudinal vessels very numerous and difficult to count; there are as many as 15 vessels between the folds and more than 20 on folds 1 and 3. Fold 4 has more than 15 longitudinal vessels anteriorly. The folds are high and the longitudinal vessels close to each other, with only one or two elongated stigmata per mesh. Parastigmatic vessels are generally present. Gut a narrow loop (Fig. 4E, F). Stomach and intestine weakly linked to the ventral side of the body wall but rectum strongly united to dorsal side. The globular stomach has 14 obvious plications. A very small cae- cum is located near the gastric aperture of the pyloric gland. Intestine long; the short rectum opens by a wide, lobed anus. There are two gonads on each side (Fig. 4E, F), weakly linked to the body wall; each is made of a double series of testes (Fig. 4G). The central ovary of each gonad spreads onto the internal part of these lobes, which makes this structure intermediate between the genera Styela and Cnemidocarpa. The gonoducts open together at the margin of the dorsal disk of the body wall. Endocarps are evenly distributed on the ventral side of the body (Fig. 4F). They are very numerous and protrude along the ring of tissue rich in tan blood lacunae which marks the boundary between dorsal and ventral halves of the body. The dorsal part is devoid of endocarps. The cloacal aperture is circled by thin cloacal tentacles arising from a crest (Fig. 4F). Remarks. — This species has several char- acters which are similar to Styela milleri Ritter, 1907, collected frequently from 900 27 to 4000 m depth along the Pacific coast from California to Chile and also recorded in the south Atlantic and the Indian Oceans. The oral tentacles, dorsal tubercle, dorsal lami- na, branchial sac, and gut are similar in both species. In contrast, S. milleri has only one gonad on each side and they are different in structure from those of S. psoliformis. The new species has the same appearance as S. similis C. Monniot, 1969 from the conti- nental slope of Europe and West Africa, and these species have many anatomical char- acters in common due to their similar body shape. S. similis also has only one gonad on each side, but its structure differs. The gonad of S. psoliformis is morpho- logically intermediate between typical Sty- ela gonads and the very peculiar gonad of Cnemidocarpa pfefferi (Michaelsen, 1904) shown in Millar 1960; that large (5 cm), round species lives on the slope of South Georgia and South Shetland Islands. It has two gonads on each side, each consisting of a lobed ovary with each lobe encircled by testes. The structure of the gonad of S. pso- liformis resembles that of species of Pyura, but this is only a convergence: all other char- acteristics of the present species are typical of the Styelidae family. The animal looks like a psolid holothu- rian after which it is named. Pyuridae Halocynthia hispida Herdman, 1881 Pig; 5 Synonymy: see Kott, 1985:342, fig. 169, pl. 7F, Millar (1988). SP 24-XI-86-3-9 and 27-XI-86-1-9. Description.—This species has two dif- ferent types of morphology on the Gala- pagos Islands: a hard form with a thick tunic collected in shallow water by SCUBA and a larger form with a soft hairy tunic collected from deep water by the submersible. The two forms also differ in internal structure, and only a very careful analysis of all char- acters has convinced us that they belong to the same species. A reduction of the organs 28 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON linked to increased depth and decreased food supply has been described in ascidians (Monniot & Monniot 1978), but the case of H. hispida in the Galapagos is extreme. The shallow-water form was collected at Bainbridge Rocks, east of San Salvador Is- land, at a depth of 17 m. It was firmly at- tached by its ventral side; both apertures are erect, at almost the same level. The spec- imen measures 10 X 7 X 5 cm, the aper- tures separated by 4 cm. The side facing the light is dark red in life. The tunic is wrinkled and covered with small smooth spines that become larger near the siphons, the largest grouped on tubercles. Around the apertures there are large branched spines 3 to 4 mm in length. The thickness of the cartilaginous tunic reaches 5 mm. The body wall is 2—3 mm thick and fleshy. The muscles are well developed: the exter- nal circular ones make a continuous layer, the internal radial muscles are gathered to- gether in strong bands. The oral tentacles are located behind a strong sphincter; they number about 20 in three orders and are only weakly pinnate. The peripharyngeal groove has 2 equal rims and shows a clear dorsal V. The dorsal tubercle is large, com- plex and protruding (Fig. 5D). The dorsal lamina has a double series of languets. The middle level of the branchial sac has 10 high folds on each side. Anteriorly and posteriorly, additional ventral folds appear, so the maximum number of folds in this specimen is 13 on the right and 12 on the left side. The distance between 2 longitu- dinal vessels is the same on the folds as between them, so it is difficult to distinguish the base of a fold. In the ventral part of the branchial sac there are only 2 or 3 longi- tudinal vessels between folds, the meshes are larger there and they may have a dozen stigmata. The gut (Fig. 5C) is voluminous and oc- cupies most of the left side. The esophagus is long and the stomach is covered with a hepatic gland of two parts: the anterior la- mellar and the posterior cauliflower-like. The intestine is attached to the body wall and has a smooth edged bilobed anus. The gonads are very numerous (13 on the right and 10 on the left) and so massed and interpenetrated (Fig. 5C) that they can only be counted by their genital papillae. On the left side they cover the descending limb of the intestine. Each gonad consists of an ovary surrounded by lobes of testes. There are numerous endocarps on the body wall, inside the gut loop and even pro- truding from the anterior part of the stom- ach (Fig. 5C). The deep-water form is rounded; the larg- est specimen measures 7 X 5 X 4cm with a distance of 4 cm between the apertures. The color in life is tan-brown with some amounts of red near the siphons. The entire tunic bears short branched spines with much larger ones on the siphons; between the branched spines there are smaller simple ones, often placed in rings. The test is thin (1 mm) and flexible. Internal organs are vis- ible through the thin, transparent body wall. The external layer of circular muscles is thin. The internal radial muscles are gathered to- gether in weak ribbons. When the tunic is removed, the oral ap- erture has 4 low lobes with undulated edges. There is a small plain velum at the base of the oral siphon. The oral tentacles are not numerous (36) and occur in at least 4 orders. Between the largest tentacles on the tentacle crest there are numerous small digitiform ones. The largest tentacles measure up to 13 mm but only have about 20 primary branchings, which are themselves thin and poorly branched in turn. The peripharyn- geal groove has 2 equal laminae; it is curved around each branchial fold and makes a large dorsal V. The dorsal tubercle is round and has a C-shaped aperture open on the ante- rior left side (Fig. 5A). The neural ganglion is elongated (15 mm), and thin. Nerves from it are clearly visible: 2 anterior and 2 pos- terior ones. The visceral nerve follows the dorsal lamina and is accompanied by a neat dorsal band; it originates on the right pos- Fig. 5. Halocynthia hispida: A, Deep-water form, internal side of the body, branchial sac removed; B, Detail of the right gonad; C, Shallow-water form, internal side of the body; D, Dorsal tubercle of the shallow-water specimen. 30 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON terior side of the neural ganglion. In its an- terior part the dorsal lamina consists of a double row of languets; the left line has true languets and is more developed than the right line, which is made of prolongations of the right transverse branchial vessels. The branchial sac has 10 folds on each side. The branchial formula is: R.E.2(8)2(13)2(15)3(17)2(18)2(20)2(22)2 (21)3(20)3(16)2.DL L.DL.2(17)2(21)2(22)3(22)2(21)2(19)3(15) 2(13)2(11)1(10)O.R The 10th (most ventral) fold on the left is only present in the anterior part of the bran- chial sac. The folds are very high and largely cover each other. The longitudinal vessels are raised, and there are only two or three between the folds. We counted 24 stigmata in a median mesh between two folds and 8 to 10 in meshes close to the base of the folds. It is only at the crest of the fold that the number of stigmata in a mesh go down to five or six. We have not observed spiral stigmata at the crests of folds. The stigmata are not very elongated; they are crossed by parastigmatic vessels only when a division begins in a transverse row. Between the folds the transverse vessels are inflated into am- pullae attaining several millimeters, much like endocarps. Gut short; a long esophagus leads to a stomach with a 2-part liver (Fig. 5A), the anterior one with parallel ridges and the posterior with papillae on crests. The two parts of the gland are separated by a nar- rowing, but they remain united. At the nar- rowing level there are parallel riges, each dividing in two in the anterior part (Fig. 5A). At the pyloric end of the stomach the hepatic gland stops abruptly. The intestine is short and translucent. Rectum long; at- tached along the dorsal lamina, and the anus has two lobed lips. On each side there is a cluster of four parallel ovaries united at their proximal ends. Each cylindrical ovary is surrounded by ramified testes (Fig. 5B). Each ovary and its testes are wrapped in a common mem- brane. The testes give off long thin ducts which join at the atrial surface of the ovary to form a common spermduct. The com- mon spermduct consists of canals coming from both sides of the ovary. The sperm- duct opens just behind the oviduct on a common protruding papilla. The four left Ovaries originate inside the gut loop and open onto the intestine (Fig. 5A). The entire body wall is provided with en- docarps. The cloacal siphon has a short ve- lum similar to the oral siphon. We have not seen cloacal tentacles. Remarks. — This species is recorded from the Galapagos by Millar (1988) and the specimens he describes are intermediate be- tween our two forms. If we examine point by point the differences between our shallow and deep populations, we find that they are almost all quantitative ones: thickness of the tunic and body wall, gonad number, size of the gut, and number of branchial folds. The difference in the number of oral ten- tacles has no taxonomic significance. The most important contrast is the reduction of the gut in deep-water specimens, and its po- sition at the posterior part of the body. The gonads are also posteriorly displaced in deep- water animals. The thinning of the tissues in deep-water animals is probably linked to decreased food supply. The species of Halocynthia have a highly evolved branchial sac which is very efficient in filtering phytoplankton, but the deep samples certainly have less food avail- able. In fact, the branchial sac is the only organ not reduced; on the contrary, the number of stigmata per mesh increases with depth. The reduction in size of the gut is correlated with this nutritional phenome- non; it is a common characteristic for as- cidians living on the slope such as in Ascidia (see below). A similar but less accentuated situation has been described for Ascidia VOLUME 102, NUMBER 1 challengeri and Corella eumyota (Monniot & Monniot 1983) on the slope in the Ant- arctic Ocean and at Kerguelen. The shifting of the gut and gonads pos- teriorly may be a consequence of the loss of tunic rigidity. In 1973 we reported that deep- sea ascidians show a tendency to equilibrate their visceral masses to keep their balance on the substratum. In other species of Halo- cynthia the disposition of the gonads on the right side seems linked to the tunic rigidity: H. ritteri from Japan has a hard tunic and gonads located in the middle of the right side, while H. papillosa, H. aurantium and H. pyriformis, with thin tunics, have gonads located posteriorly. Except for two Arctic species, the tropical and temperate Halocynthia are found in very shallow water not deeper than 30 meters. Is the presence of deep specimens in the Ga- lapagos exceptional? We cannot answer be- cause the deep rocky bottoms have not been sampled enough, but this species represents the most extreme case of ecological dimor- phism known in an ascidian. Conclusions The bathyal ascidian fauna of the Gala- pagos does not provide any evidence in sup- port of an archaic fauna. All species belong to genera and more advanced families which are well represented in other oceans and which show adaptations here to deep-sea life. The origin of the fauna is unknown. Rel- atively few collections have been made along the South American Pacific coast; we cannot determine if the new species described here are endemic or if they have been carried north by the Humboldt Current. The Ga- lapagos ascidian fauna differs greatly from the assemblage of Antarctic ascidians known from the south coast of Chile. Among the eight species recorded from the Galapagos, only three were previously known: Apii- dium californicum, a tropical shallow-water 31 shallow-water species probably at its depth limit here, Halocynthia hispida, widely dis- tributed and known in shallow water from both the Galapagos and Australia; and As- cidia clementea, a north Pacific species. Sit- ula and Ciona are genera which are well represented in bathyal areas in other parts of the world. It seems unlikely that the Humboldt Current contributes to the oc- currence or distribution of ascidian fauna around the Galapagos islands. Observations from the Johnson-Sea-Link have shown that ascidians are a very small part of the bathyal biomass which is mainly comprised of sponges, cnidarians and echi- noderms. Other filter-feeding animals, such as bivalves or bryozoans, were also very seldom seen. Except for Situ/a, which is phytophagous and carnivorous, the other ascidians we report have the same diet as sponges: small suspended particles and dis- solved substances. Sponges in Galapagos deep-water habitats are large, abundant, and diversified, but ascidians remain scarce even though they are relatively large. Acknowledgments The R/V Seward Johnson and Johnson- Sea-Link-1 cruise was funded by Harbor Branch Oceanographic Institution, the U.S. National Cancer Institute, Natural Products Branch (contract no. NO1-CM-67919), and SeaPharm Inc. Francoise Monniot is par- ticularly thankful to the chief scientist of the cruise, K. L. Rinehart and to Shirley A. Pomponi who gave her the opportunity to participate in the submersible dives and in SCUBA collecting. In gratitude two of the species reported here are named after them. Literature Cited Bonnevie, K. 1896. Ascidiae simplices og Asciidae compositae fra Nordhavs-Expeditionen. — Norske Nordhavs-Expeditionen 1876-78 23:1- 16. Kott, P. 1969. Antarctic Ascidiacea.— Antarctic Re- search Series 13:1—239. 32 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 1985. The Australian Ascidiacea. Part I, Phlebobranchiata and Stolidobranchiata. — Memoirs of the Queensland Museum 23:1-440. Hartmeyer, R. 1912. Die Ascidien der deutschen Tiefsee-Expedition.— Deutschen Tiefsee-Expe- dition 7:223-392. Herdman, W. A. 1881. Preliminary report on the Tunicata of the Challenger expedition.—Pro- ceedings of the Royal Society of Edinburgh, part 3 Cynthiadae 11:233-240. Millar, R. H. 1960. Ascidiacea.— Discovery Reports 30:1-160. 1988. Ascidians collected during the South- east Pacific Biological Oceanographic Program (SEPBOP).—Journal of Natural History 22:225- 240. Monniot, C. 1969. Ascidies récoltées par la ““Tha- lassa” sur la pente du plateau continental du golfe de Gascogne: (3-12 Adut 1967).— Bulletin du Muséum National d’Histoire Naturelle, Paris (2),41(1):155-186. 1970. Ascidies récoltées par la ““Thalassa”’ sur la pente du plateau continental du golfe de Gascogne (18-25 Octobre 1968).—Bulletin du Muséum National d’Histoire Naturelle, Paris (2),41(5):1131-1145. 1972. Dicopia antirrhinum n. sp. ascidie de la pente du plateau continental du golfe de Gas- cogne. Interprétation nouvelle de la famille des Octacnemidae.— Cahiers de Biologie Marine 13: 9-20. 1978. Ascidies phlébobranches et stolidob- ranches du sud de Il’Océan Indien.— Annales de l'Institut Océanographique, Paris 54(2):171-—224. —., & F. Monniot. 1973. Ascidies abyssales ré- coltées au cours de la campagne océanogra- phique Biacores par le “Jean Charcot”.—Bul- letin du Muséum National d’Histoire Naturelle, Paris (3), 121 Zoologie 93:289-475. ———,,& . 1977a. Quelques ascidies abyssales du Sud-Ouest de l’Océan Indien.—Comité Na- tional Francais de Recherches Antarctiques 42: 305-327. ——., & 1977b. Tuniciers benthiques pro- fonds du Nord-Est Atlantique. Résultats des campagnes Biogas.— Bulletin du Muséum Na- tional d’Histoire Naturelle, Paris (3), 466 Zoo- logie 323:695-720. ———., & 1978. Recent work on the deep- sea tunicates. Oceanography and marine biol- ogy, annual review, 16:181-—228. ——., & . 1983. Ascidies antarctiques et sub- antarctiques. Morphologie et biogéographie. — Mémoires du Muséum National d’ Histoire Na- turelle, Paris (A), Zoologie 125:1-168. Oka, A. 1913. Zur Kenntnis der zwei aberranten As- cidiengattungen Dicopia Sluit. und Hexacroby- lus Sluit.— Zoologischer Anzeiger 43(1):1-10. 1918. Megalodicopia hians n. g., n. sp., eine sehr merkwurdige Ascidie aus dem japanischen Meere. — Annotationes Zoologicae Japonense 9: 399-407. Ritter, W. E. 1907. The ascidians collected by the United States Fisheries Bureau Steamer Alba- tross on the coast of California during the sum- mer of 1904. University of California, Publi- cations in Zoology, Berkeley 4(1):1—-52. 1913. The simple ascidians from the North- eastern Pacific in the collection of the United States National Museum.— Proceedings of the United States National Museum 45:427-505. —., & R.A. Forsyth. 1917. Ascidians of the lit- toral zone of southern California. University of California Publications in Zoology 16:439-512. Sluiter, C. P. 1905. Die Tunicaten der Siboga-Ex- pedition. Supplement zu der I. Abteilung: die socialen und holosomen Ascidien.—Siboga Ex- pedition Monographie 56A:129-139. Tokioka, T. 1953. Ascidians of Sagami Bay collected by His Majesty the Emperor of Japan. — Tokyo: Iwanami Shoten 1-315. . 1972. Onasmall collection of ascidians from the Pacific coast of Costa Rica. Publications of the Seto Marine Biological Laboratory 19(6): 383-404. Vinogradova, N. G. 1969. On the finding of a new aberrant ascidian in the ultrabyssal of the Ku- rile-Kamchatka trench.—Bulletin of the Mos- kovit Society of Natural History, Biological Part 3:27-42. 1975. On the discovery of two new species of an aberrant deep-water ascidiacean genus Sit- ula in the South-Sandwich trench.—Transac- tions of the P. P. Shirshov Institute of Oceano- logia 103:289-303. Museum national d’Histoire naturelle, Laboratoire de Biologie des Invertébrés Marins et Malacologie, 55 rue Buffon, 75005 Paris, France. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 33-44 EUKROHNIA CALLIOPS, A NEW SPECIES OF CHAETOGNATHA FROM THE NORTHERN GULF OF MEXICO WITH NOTES ON RELATED SPECIES Jerry A. McLelland Abstract. —Eukrohnia calliops, a new species of Chaetognatha, was discov- ered in deep-water plankton collections made at four stations in the northern Gulf of Mexico in August 1987, and in February 1988. The new species appears to occur in bottom water over the upper continental slope at depths between 200 and 700 m. Its large pigmented eyes easily distinguish it from other Eu- krohnia species occurring in the Gulf of Mexico. It differs from the closely related E. kitoui Kuroda, 1981, a species from Japanese waters, chiefly by the size and shape of the eyes. Thirteen specimens of EF. calliops are studied and compared with specimens of E. kitoui, E. proboscidea, and E. fowleri, all of which possess pigmented eyes. The first record of E. proboscidea in the Gulf of Mexico is documented and affinities within the proposed “‘proboscidea group” are discussed. Distribution records of four species of Eukrohnia reported from the Gulf of Mexico prior to this study are presented with a key separating the Six species now known. Members of the chaetognath genus Eu- krohnia typically inhabit deep-water plank- ton communities throughout the world (Al- varino 1965, 1969 for zoogeography). Of the nine currently described species of Eu- krohnia (Casanova 1986), only three are known to possess pigmented eyes: E. fowleri Ritter-Zahony, 1909, E. proboscidea Fur- nestin & Ducret, 1965, and EF. kitoui Ku- roda, 1981. Eukrohnia fowleri has a well known cosmopolitan distribution, while the latter two species appear restricted to deep coastal waters of the Atlantic Ocean and the Pacific coast of Japan, respectively. One hundred and eighty three specimens ofan undescribed species of Eukrohnia with large pigmented eyes were discovered in plankton samples collected at four study areas in the northern Gulf of Mexico in Au- gust 1987 and February 1988 by personnel of the Gulf Coast Research Laboratory aboard the R/V Tommy Munro (Fig. 1, Ta- ble 1). Quantitative samples were obtained by towing horizontally at depths of 200-500 meters using a Niskin double-trip system with 1 m diameter, 333 wm mesh nets. Qualitative samples were obtained near the bottom with 0.3 m diameter, 183 um mesh nets attached to crab traps and allowed to passively filter the bottom current. Only material from the February 1988 cruise was used in this work because specimens in the August 1987 samples were in poor condi- tion. Class Sagittoidea Claus and Grobben, 1905 Order Phragmophora Tokioka, 1965 Family Eukrohniidae Tokioka, 1965 Genus Eukrohnia Ritter-Zahony, 1909 Diagnosis. —One pair of lateral fins emerging at or near ventral ganglion; one pair of tooth rows; apical gland cell com- plex, or papillae tuft, at anteroventral point of head; ventral transverse musculature in trunk segment extending from neck to at least posterior edge of ventral ganglion. 34 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON GULF OF MEXICO YUCATAN vs 90° 89° 88° 87° Fig. 1. 86° 35° 84° 83° 82° g1° 80° 79° Map showing locations of five study areas along the continental slope in the northern Gulf of Mexico from which deep-water plankton collections were made in August 1987, and February 1988. Eukrohnia calliops, new species Figs. 2, 3, Tables 1—4 Material. —Holotype, 21.5 mm (USNM 119293), R/V Tommy Munro, Area 3, (29°21'N, 86°57'W) northern Gulf of Mex- ico, 200-500 m, 16 Feb 1988, 1910 CDT, 11 paratypes as follows: 1 specimen, 18.2 mm (USNM 119296), from type locality; 2 specimens 18.4, 15.0 mm (USNM 119294), from Area 1 (29°00'N, 88°26'W), 677 m, 28 Feb 1988, 1930 CDT; 5 specimens, 14.4, 12.6, 11.7, 10.4, 8.4 mm (USNM 119295), from Area 2 (29°18'N, 87°32’W), 200-500 m; 13 Feb) 1988; 1035 CDT; ‘bspeciment 16.6 mm (GCRL 1131), from Area 4 (27°50’N, 85°24'W), 400-485 m, 25 Feb 1988, 2345 CDT; 3 specimens, 16.2, 13.0, 11.3 mm (GCRL 1132), from =Arear (27°50'N, 85°24’W), 677 m, 26 Feb 1988, 1910 CDT. Description. — Based on type material with five stages of sexual maturity described in Table 2. Body firm, translucent, with well- developed dorsal and ventral longitudinal muscle bands; widest at trunk-caudal sep- tum, tapering slightly toward the head; maximum length recorded 21.5 mm. Tail length 21.7-29.3% of total body length. Head wider than long with distinct constric- tion at neck. Corona ciliata not observed. Collarette (alveolar tissue) absent. Eyes large, bulbous, sub-oval to tear-drop shaped (Figs. 3C, 5B); widely separated on VOLUME 102, NUMBER 1 35 Table 1.—Station and hydrographic data for Eukrohnia species in the northern Gulf of Mexico. : Number of Bottom Sampling Length Bottom Bottom specimens depth depth oftow salinity temp. Station Position Date Time (m) (m) (min) (ppt) (°C) Ec. Ef. Ep. mgea! 29°02’N, 088°27'W 08/02/87 2007 494 200-400* 33 36.0 8.4 mm (Oe OD 29°00'N, 088°26’W 02/28/88 1930 677 Offa ees hr 36.0 - 6.5 = es 8 Area2 29°18'N, 087°34'W 08/04/87 1910 494 200-400* 44 33:0 “8.60 son 0. 0 29°18'N, 087°32'W 02/13/88" 1035 °*677 (200-500 30 34.0 6.3 a Oo 0 29°18'N, 087°32'W 02/14/88 0730 677 Giizze= 23hr (34.0 6.3 2) SU @) Area3 29°21'N, 086°57'W 08/06/87 0838 677 200-500 54 39.0 6.4 is 0 0 29°21'N, 086°57’'W 02/16/88 1910 677 200-500 94 5602, 6:7 DEW Nera, © 29°21'N, 086°57'W 02/17/88 1840 677 Site acne. 36.0 ‘6:7 Te On oO Area4 27°54'N, 085°16'W 08/08/87 1150 494 200-400 31 58:0) 7 1 0 27°50'N, 085°24'W 02/25/88 2345 494 400-485 27 38.0 8.4 040 27°50'N, 085°24'W 02/26/88 1910 677 CUI WeaMinr: S810". 6:5 37 0). 0 Area5 27°00'N, 084°57'W 02/24/88 0720 677 G71 24 hrs 38:0: 6:6 0 4 1 * Net accidentally dragged bottom. ** Passive sampling by 0.3 m diameter nets attached to crab traps. Ec. = E. calliops, Ef. = E. fowleri, Ep. = E. proboscidea. dorsal surface of the head. Pigment cups lunate to hemispherical, dark-brown to black in color; oriented parallel to longitudinal body axis with apex of cup on inner median edge of eyes. Apical gland cell complex bilobate, pro- truding anteriorly. Two less conspicuous gland cell complexes, a smaller anterior one and a larger posterior one, both with small, densely packed papillae, situated anterior to mouth between vestibular ridges (Fig. 3A). Hooks 12-13 on each side of head; long, slender, and somewhat straight, with sharp- ly bent tips (Fig. 3D, E); no denticulate hooks observed. Anterior teeth absent. Posterior teeth 9-21 (17-21 in stage HII and IV in- dividuals); thin, pointed, set close together (Fig. 3B); located midway between hooks and apical gland cell complex. Up to 20 vestibular palps in one or two rows on ves- tibular ridge, beginning ahead of and run- ning parallel to entire length of tooth row; those adjacent to teeth elongate, highly transparent with cup-like terminal ends (Fig. 3B). Gut extending from mouth to anus, flat- tened laterally into thin ribbon, appears im- pregnated with fine darkened granular ma- terial; usually with distinctly thickened area directly beneath ventral ganglion (Fig. 2B). Intestinal diverticulae absent. Ventral ganglion located at anterior fourth of body on ventral surface of trunk; small, rectangular to oval in shape, with fine nerve fibers emerging at corners. Ventral trans- verse musculature extending from neck re- gion past posterior edge of ventral ganglion by a distance of up to one-fourth the length of ganglion (Fig. 2B). Lateral fins extending along body from posterior third of tail segment to about an- terior third of ventral ganglion; broadly rounded at posterior end and tapering an- teriorly to delicate ridge; posterior portions entirely rayed to about level of trunk-caudal septum, rays continuing anteriorly along distal edge for about half fin length; inner and anterior portions containing laminar material and fine fibrils. Tail fin distinc- tively large, broadly triangular, completely rayed. Ovaries short, club shaped, 10-17 ova per Ovary; Ova arranged in two rows when viewed laterally (Fig. 2C). Seminal vesicles 36 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON = = = = \ RWI AW WOH 1cehhs Woy Ni) | si \ || Gos Bne Reid Neko ¥, age a _— AL hy LOU DUVAA GA eT NLEAR DEL LASALLE WH OOo ATH HA HN Fig. 2. Eukrohnia calliops from the northern Gulf of Mexico. A, ventral view of a mature specimen; B, lateral view of ventral ganglion area with cut-away showing thickened area of gut tube underlying trans- verse musculature; C, lateral view of ovary at maturity stage III; D, detail of mature seminal vesicle. oval to elongate, about a third their length overlapped by posterior edges of lateral fins; separated from tail fin by about a fourth their length (Fig. 2D). Etymology.—The specific name is de- rived from the Greek words “‘kallos”’ (beau- ty) and “‘ops”’ (pertaining to the eyes), and is a noun 1n apposition. Comparative material examined (Table 3).— Eukrohnia kitoui, 10 specimens, 4.7—25.4 mm; Tokyo Bay, Japan (35°08'N, 139°46’E), 13 Feb 1981, 0-240 m; from Kazunori Kuroda, Tokai Regional Fish- eries Research Laboratory, Tokyo, Japan. Eukrohnia proboscidea, 2 specimens, one 18.0 mm; origin unknown; from Jean- Paul Casanova, Laboratorie de Biologie animal (Plancton), Marseille, France. Eukrohnia proboscidea, 1 specimen, 10.6 mm; Gulf of Mexico (27°00'N, 84°57'W), 14 Feb 1988, 677 m; from Area 5, R/V Tommy Munro (Table 1). Eukrohnia fowleri, 7 specimens co-occur- ring with E. calliops and E. proboscidea in the northern Gulf of Mexico (Table 1). Results and Discussion Affinities. —Morphological characteris- tics of the four species of Eukrohnia pos- sessing eye pigmentation are compared in Table 4 which combines personal obser- vations with published data. Eukrohnia calliops is most closely related to E. kitoui (Figs. 4B; 5C, D). The two species are very similar in all respects including eye pigment configuration. In fact, they were at first considered synonymous until a detailed comparison was made between non-con- tracted E. calliops specimens collected in February 1988 and material of similar con- dition from Tokyo Bay, Japan. Results of this comparison appear in Table 3 and Fig. 6. Eukrohnia calliops has greater numbers of posterior teeth and higher tail segment percentages in specimens of comparable size. Obvious differences between the two species are eye size and the appearance of the pig- VOLUME 102, NUMBER 1 a0 Fig. 3. Head details of Eukrohnia calliops, holotype: A, ventral view of head; B, vestibular ridge showing rows of palps and teeth; C, dorsal view of eyes; D, mature hook; E, hook tip variations. (Abbreviations for Fig. 3A, B: gc = gland cell complex, m = mouth, pt = posterior teeth, vp = vestibular palps.) ment cup within the eye. The pigment cups of E. calliops are darker in color, larger in relation to the total area of the eye, and have a greater three-dimensional aspect causing them to “‘bulge’’ from the surface of the head. The larger eye size of E. calliops is dem- onstrated in Fig. 6 which compares ratios of eye length to total body length (EL/TL x 100) between the two species. Eukrohnia calliops was found to differ from E. kitoui at the 95% level of significance using a t-test on the mean ratios with variances pooled. Eukrohnia proboscidea (Figs. 4C; 5E, F), originally described from tropical African waters by Furnestin & Ducret (1965), is ap- parently a close relative of E. calliops and E. kitoui as demonstrated by their morpho- logical similarities (Table 4) and similar habitats. As such, the three might be loosely separated from the rest of the genus to form the “‘proboscidea group.” This grouping would further subdivide the “‘fowleri group” proposed by Casanova (1986:827), an ar- tificial arrangement of five species of Eu- krohnia based on the presence of similar light sensitive cells in the eyes, pigmenta- tion in the digestive tube, and numbers and coloration of hooks. 38 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Table 2.—Maturity stages for Eukrohnia calliops in February 1988 collections from the Gulf of Mexico. Stage TL (mm) Male gonads Female gonads I 8.4-12.6 Testes are small rods originating in anterio- Ovaries short, club-shaped; no ova lateral corners of tail segment and not ex- formed but oocyte clusters present. tending over half the length of the seg- ment; spermatids not enlarged; seminal vesicles not formed. II 11.7-14.4 Testes elongated to full length of caudal seg- § Ovaries longer (4% TL); ova small, ment; spermatids enlarging; seminal vesi- uniform in size, arranged in 2 rows cles emerging but not enlarged. or clustered. II = 15.0 Testes completely fill tail segment; sperm Ovaries longer and thicker (S—7% TL); cells enlarged; seminal vesicles enlarged, some ova enlarged (3-5 per ovary), fully formed. arranged in 2 rows. IV >15.0 Tail segment partially empty; seminal vesi- Ovaries at maximum length (10-11% cles ruptured. TL); all ova enlarged (10-14 per Ovary), arranged in 2 rows. Vv > 18.0 Tail segment empty (spent). Ovaries contracted, empty (spent) or The pigment of E. proboscidea, which is situated in the posterior portion of the eye, differs considerably from that of E. calliops and E. kitoui. It is light-brown in color with a distinct black edge along the inner border which lends a ““U”’-shaped appearance when viewed dorsally. An interesting affinity within the “‘pro- boscidea group”’ is the posterior extent from the neck of the ventral transverse muscu- lature. Casanova (1986:831) found that for E. proboscidea the musculature exceeded the position of the ventral ganglion by half the length of the ganglion. He considered this to be a unique feature of that species and stated that in all other members of the genus Eukrohnia, the musculature extends only to the edge of the ganglion. The overreaching of the musculature by a fourth the length of the ganglion in E. calliops, while not as great an extent as that of E. proboscidea, does demonstrate a similarity. In the largest spec- imen of the EF. kitoui material (25.4 mm), the extent of transverse musculature was similar to that of E. calliops; however, this characteristic was reported by Kuroda (1981: 181) as “extending from the neck to the posterior edge of the ventral ganglion.” with | or 2 large ova; oviducts swol- len. The hooks of the “‘proboscidea group” species are nearly identical. The hook tips (Fig. 3E), abruptly deflected inward at 45- 90°, are similar to those of E. hamata and E. bathypelagica. Denticulate hooks, a com- mon characteristic in juveniles of Eukroh- nia and Heterokrohnia (Kapp & Hagen 1985:58), were not found on small speci- mens of the “proboscidea group” in this study nor were any reported by Kuroda (1981) for E. kitoui or by Furnestin (1965) for E. proboscidea. Owre (1973:957), how- ever, reported that the ventral-most hooks on 13.0 and 16.5 mm specimens of E. pro- boscidea from the Caribbean Sea were “‘ser- rated with 10-18 small hooks.” The single specimen of E. proboscidea ob- tained from the bottom sample at Area 5 represents a new record for the Gulf of Mex- ico. At 10.6 mm, it is the smallest specimen yet recorded for the species. Meristic counts were similar to those reported by Owre (1973) for a 13.0 mm specimen from the Caribbean Sea but the Gulf specimen had fewer number of hooks and teeth than the smallest specimen (13.3 mm) of the type material from tropical African waters (Du- cret 1965). The Gulf of Mexico specimen VOLUME 102, NUMBER 1 Table 3.—Meristic values of Eukrohnia comparison material. 39 TL mm % Tail Hooks Teeth Eukrohnia calliops, n. sp. from the Gulf of Mexico Eye Lmm Mat. St. Source 0.26 IV-—V A3, 200-500 m 0.28 III Al, bottom 0.24 Vv A3, 200-500 m 0.22 III A4, 400-440 m 0.24 IV A4, bottom O27 IV Al, bottom 0.24 II A2, 200-500 m 0.20 II A4, bottom 0.20 I A2, 200-500 m 0.19 II A2, 200-500 m NA II A4, bottom 0.18 I A2, 200-500 m 0.14 I A2, 200-500 m 2a 24.9 12 21 18.4 27.0 12 17, 18.2 25.6 12 15-17 16.6 26.6 12 17-19 LG? 24.8 12-13 16 15:0 29:3 NA NA 14.4 2335 13 12 13.0 26.4 12 13 12.6 217 12 12-13 ELT 2555 12 7-11 £13 31.0 13 15 10.4 223 11-12 10 8.4 26.7 11 9-10 Eukrohnia kitoui from Tokyo Bay, Japan (35°08'N, 139°46’E), 0-240 m 25.4 24.6 13 16-17 18.4 222 12 14 16.6 23:6 10-11 14 15.0 DEES) i 13 13.4 22.8 11 9-10 10.4 25.4 10 q) 7.9 D522) 10 5 7.0 253 9 4 5.0 26.2 8 5 4.7 27.4 i 1 Eukrohnia proboscidea 18.0 23.0 12 13 NA NA 12 15 10.6 24.2 10 8 Eukrohnia fowleri from the Gulf of Mexico 28.5 23.0 18} 27 28.5 Des 11-13 27 26.6 22.0 11 20 14.4 2333 11 12 14.0 24.0 1hi@)F 12 11.8 20.0 12 (4)* 10 10.7 20.9 12 (4)* 12 * Denticulate hooks (number). lacked denticulations on the ventral-most hooks. Eukrohnia fowleri (Figs. 4D; 5G, H), a cosmopolitan, mesoplanktonic species, dif- fers from the “‘proboscidea”’ group in nearly all morphological features and armature meristics. The eye pigment is a dark, vari- ably shaped fleck in the center of the eye. The hooks are robust, red in color, and have 0.20 IV Kazunori Kuroda O17 Ill Kazunori Kuroda 0.14 III Kazunori Kuroda 0.14 II Kazunori Kuroda On II Kazunori Kuroda 0.10 II Kazunori Kuroda 0.08 I Kazunori Kuroda 0.07 I Kazunori Kuroda 0.06 I Kazunori Kuroda 0.07 I Kazunori Kuroda II J. P. Casanova II J. P. Casanova I A5, Gulf of Mex. II A5, bottom II AS, bottom II A3, 200-500 m I A3, 200-500 m I A3, 200-500 m I A5, bottom I A5, bottom straight tips. The ventral-most three or four hooks of small specimens are strongly den- ticulate (Table 3). Ecology and distribution.—Based on avail- able data, the three species of the “‘probos- cidea group” appear to occupy similar hab- itats in deep-water areas adjacent to coastal regions, although E. proboscidea has so far been found at greater depths, with occur- 40 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON e Fig. 4. Dorsal views of heads of the four species of Eukrohnia possessing pigmented eyes. A, E. calliops, holotype; B, E. kitoui Kuroda, 1981; C, E. proboscidea Furnestin & Ducret, 1965; D, E. fowleri Ritter-Zahony, 1909. Scales: A, B, and D = 0.5 mm; C = 0.2 mm. rences below 1000 m, off the west African coast (Ducret 1965) and in samples collect- ed between 750 and 1100 m in the Carib- bean Sea (Owre 1973, Michel et al. 1976). Eukrohnia kitoui and E. calliops were col- lected at similar depths (0-400 and 200- 677 m) in Tokyo Bay and the northern Gulf of Mexico, respectively, near undersea can- yon areas where upwelling of water from deeper regions occurs. It is worthy to note that at the Area 5 station (Table 1), no specimens of E. cal- liops were present, but in the February bot- tom net samples, one immature specimen of E. proboscidea was found, indicating the northward extension of a deep-dwelling Ca- ribbean population of that species. More ex- tensive sampling near the bottom in these areas may identify boundaries between these two species in the Gulf of Mexico. In the August 1987 cruise, the nets acci- dentally dragged bottom at the Area 2 sta- tion near the Desoto Canyon, resulting in a sample containing a large number (131) of E. calliops (Table 1). This suggests a pos- sible hypo-planktonic distribution for the species in the Gulf of Mexico. The genus Evkrohnia was not mentioned in any of the major studies of the chaeto- gnath fauna of coastal areas of the Gulf of VOLUME 102, NUMBER 1 41 Table 4.—Characteristics of the four species of Eukrohnia with pigmented eyes from descriptions published by Ducret (1965), Alvarino (1967), Kuroda (1981), Michel (1984), and from personal observations by the author. E. fowleri E. proboscidea Furnestin & Character Ritter-Zahony, 1909 Ducret, 1965 E. kitoui Kuroda, 1981 E. calliops, n. sp. Total length 40 25 24.5 PAGS (mm) % Tail length 22-25 21.5-31 22-24 24-29 Eye shape Elliptical Elongate Circular to sub- Oval to tear-drop oval shaped Eye pigment Apical gland Hooks Posterior teeth Transverse musculature extent Epidermal col- larette tissue Lateral fins Mature ova- ries Seminal vesi- cles Variably shaped rectangular fleck in center of eye, black Single mass of cells, not protruding 11-13, robust, strongly curved, reddish, tips straight Up to 30 Level with poste- rior edge of ven- tral ganglion Thick band around body at ventral ganglion Extending from an- terior 4 of ven- tral ganglion to middle of tail segment Short (13% TL); ova large, in two rows Ovoid; adjacent to posterior fins and separated from tail fin a distance greater than their length Elongate to U-shaped in pos- terior part of eye, light-brown Bilobate, protrud- ing anteriorly 10-13, slender, gently curved, light-brown, transparent, tips curved sharply inward Upto 25 Past ventral gan- gion by up to '2 length of gan- glion Absent Extending from base of ventral ganglion to mid- dle of tail seg- ment Short (15% TL); Ova in 2 rows, about 14 per ovary Ovoid, elongate; adjacent to inser- tion of lateral fins with anterior '4 overlapped by posterior edge of fins, separated from tail fin by about 4 their length Semi-circular in center of eye, dark brown to black Bilobate, protrud- ing anteriorly 8-13, slightly curved, light- brown, transpar- ent, tips curved sharply inward Up to 17 Usually level with posterior edge of ventral ganglion Absent Extending from slightly anterior to ventral gan- glion to posterior third of tail seg- ment Shont(13-5% DE): Ova in 2 rows, 10-15 per ovary Ovoid; adjacent to insertion of later- al fins with ante- rior 4 over- lapped by posterior edge of fins, separated from tail fin by about '/ their length Large, lunate, in cen- ter of eye, dark brown to black Bilobate, protruding anteriorly 11-13, slightly curved, light- brown, transpar- ent, tips curved sharply inward Up to 21 Past ventral ganglion by up to % length of ganglion Absent Extending from ante- rior third of ven- tral ganglion to posterior third of tail segment Short (7.5—10.5% TL); ova in two rows, 10-14 per ovary Ovoid, elongate; ad- jacent to insertion of lateral fins with anterior '/3 over- lapped by posterior edge of fins, sepa- rated from tail fin by about '2 their length 42 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 5. Eyes of the four species of Eukrohnia possessing pigmented eyes. A, C, E, and G show relative distances between eyes and B, D, F, and H show detail of individual eyes. A and B, E. calliops, holotype; C and D,-E. kitoui Kuroda, 1981; E and F, E. proboscidea Furnestin & Ducret, 1964; G and H, E. fowleri Ritter- Zahony, 1909. All scales = 0.1 mm. VOLUME 102, NUMBER 1 30 O E. kitoui Sa r= 0.989 y = 139.35 x -3.645 BODY LENGTH mm, ® €. calliops r= 0.865 y = 79.23 x —2.931 EYE LENGTH mm. 05 -10 -15 -20 25 -30 Fig. 6. Comparative relationships of body length to eye length for Eukrohnia kitoui and E. calliops. Mexico (Pierce 1951, 1962; Suarez-Caabro 1955; Vega-Rodriguez 1965; McLelland 1984) because sufficient depths were either not present or not sampled. Deep-water studies from areas further removed from the continental slopes that did include four species of Eukrohnia are presented in Table 5. Based on personal observations and on characteristics of mature specimens report- ed in the literature, the following key sep- arating the species of Eukrohnia occurring in the Gulf of Mexico is presented. 43 Key to the Species of Eukrohnia of the la. 1b. 2a. 2D: 3a. 3b. 4a. 4b. Sa. Sb. Gulf of Mexico Byes with. plement.) is/ye. se. 2 Eyes non-pigmented Apical gland bilobate and protrud- ing, causing head to appear point- ed. Hook tips bent inward at 45 to 90 degree angles. Transverse mus- culature extending past posterior edge of ventral ganglion ........ 3 Apical gland not prominent, a sin- gle lobed mass. Hook tips straight, transverse musculature even with posterior edge of ganglion E. fowleri Eye pigment small, elongate or ‘““U’’-shaped, in posterior region of BNE cuterh hertinn Se ai. E. proboscidea Eye pigment large, lunate, encom- passing most of the median por- tion of the eye .... E. calliops, n. sp. Number of hooks greater than 11, hook tips straight E. bathyantarctica Number of hooks less than 11, heok tips bent mward, | «2. .)..-+). . s Hooks stout, nearly straight; tail less than 25% of body length be (iee abies eet tas lout 9 te, £ E. hamata Hooks long, gently curved; tail greater than 25% of body length manent rite l is 2 1 | E. bathypelagica Table 5.— Distribution records of the genus Evkrohnia in the Gulf of Mexico. Species E. hamata Mobius, 1875 E. fowleri Ritter- Zahony, 1909 E. bathyantarctica Area Central Gulf Central Gulf Central Gulf SW Gulf Central Gulf Position 27°15'N, 029°09'W 27°21'N, 088°42'W 24°39'N, 093°09'W 2 ASN; 095725" W 24°39'N, 093°09'W David, 1958 Central Gulf 27°08'N, 089°55’W Central Gulf 26°16'N, 087°52’W Central Gulf 23°41'N, 090°08’W SW Gulf 21°55’N, 095°25'W E. bathypelagica Alvarino, 1962 Central Gulf Central Gulf 25°59'N, 086°11'W 25°59’'N, 086°11'W Sampling depth (m) Abundance Source 495-749 Common Pierce (1954) 1100 Common Every (1968) 2000 1 specimen Fagetti (1968) 509-1000 1 specimen Fagetti (1968) 2000 2 specimens Fagetti (1968) 1032-2000 1 specimen Fagetti (1968) 2002-2400 2 specimens Fagetti (1968) 1971-2800 1 specimen Fagetti (1968) 509-1900 2 specimens Fagetti (1968) 580-2000 15 specimens Owre (1973) 580 8 specimens Owre (1973) 44 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Acknowledgments This work was developed with materials collected under Grant No. NA87WC-H- 06142, Marine Fisheries Initiative (MAR- FIN), NMFS, NOAA, U.S. Department of Commerce. I wish to thank Harriet Perry for providing the MARFIN plankton col- lections, Dr. Richard Heard and Sara Le- croy for their review and suggestions on the manuscript, and Dr. Robin Overstreet, Mary Ann Pavlov, and Debbie Jackson for their help in producing the photographs. All of the above are from the Gulf Coast Research Laboratory. Dr. Kazunori Kuroda of the Tokai Regional Fisheries Laboratory (To- kyo, Japan) and Dr. Jean-Paul Casanova of the Laboratorie de Biologie animal-planc- ton (Marseille, France) kindly provided me with some of the specimens of Eukrohnia used in this study. Literature Cited Alvarino, A. 1965. Chaetognaths. Pp. 115-194 in Harold Barnes, ed., Oceanography and marine biology, annual revue, Vol. 3. George Allen & Unwin Ltd., London. 1967. The Chaetognatha of the NAGA ex- pedition (1959-1961) in the South China Sea and the Gulf of Thailand. Part 1—systemat- ics. -NAGA Reports, University of California, Scripps Institute of Oceanography 4(2):1-197. . 1969. Los quetognatos del Atlantico. Distri- bucion y notas esenciales de sistematica. Tra- bajos del Instituto Espanol de Oceanografia 37, 290 pp. Casanova, J. P. 1986. Deux nouvelles espéces d’Eu- krohnia (Chaetognathes) de l’Atlantique sud- tropical africain.— Bulletin du Muséum Natio- nal d’Histoire Naturelle, Paris (4)8(A no. 4):819- 8355 Ducret, F. 1965. Les espéces du genre Eukrohnia dans les eaux équatoriales et tropicales afri- caines.—Cahiers O.R.S.T.O.M.—Océanogra- phie 3(2):63-78. Every, M. G. 1968. The taxonomy and areal distri- bution of the Chaetognatha in the oceanic Gulf of Mexico. M.S. Thesis, Texas A&M Univer- sity, College Station, 67 pp. Fagetti, G. E. 1968. New record of Eukrohnia bathy- antarctica David, 1958, from the Gulf of Mex- ico and Caribbean Sea. — Bulletin of Marine Sci- ence 18(2):383-387. Furnestin, M. L. 1965. Variations morphologiques des crochets au cours du développement dans le genre Eukrohnia.—Revue des Travaux. In- stitut des Péches Maritimes 29(3):275-284. —., & F. Ducret. 1965. Eukrohnia proboscidea, nouvelle espéce de Chaetognathe.— Revue des Travaux. Institut des Péches Maritimes 29(3): 271-273. Kapp, H., & W. Hagen. 1985. Two new species of Heterokrohnia (Chaetognatha) from Antarctic waters. — Polar Biology 4:53-59. Kuroda, K. 1981. A new chaetognath, Eukrohnia kitoui n. sp., from the entrance to Tokyo Bay. — Publications of the Seto Marine Biological Lab- oratory 26 (1/3):177-185. McLelland, J. A. 1984. Observations on chaetognath distributions in the northeastern Gulf of Mexico during the summer of 1974.—Northeast Gulf Science 7(1):49-59. Michel, H. B. 1984. Chaetognatha of the Caribbean Sea and adjacent areas. NOAA Technical Re- port NMFS 15, United States Department of Commerce, National Technical Information Service, Springfield, Virginia, 33 pp. —., M. Foyo, & D. A. Haagensen. 1976. Carib- bean Zooplankton. Office of Naval Research, Department of the Navy, U.S. Government Printing Office, Washington, D.C., 712 pp. Owre, H. B. 1973. A new chaetognath genus and species, with remarks on the taxonomy and dis- tribution of others. — Bulletin of Marine Science 23(4):948-963. Pierce, E. L. 1951. The Chaetognatha of the west coast of Florida.— Biological Bulletin (Woods Hole) 100:206-228. . 1954. Notes on Chaetognatha of the Gulf of Mexico.—Fishery Bulletin of the U.S. Fish & Wildlife Service 55:327-329. . 1962. Chaetognatha from the Texas coast. — Publications of the Institute of Marine Science, University of Texas 8:147-152. Suarez-Caabro, J. A. 1955. Quetognatos de los mares Cubanos. — Memorias de la Sociedad Cubana de Historia Natural 22:125-180. Vega-Rodriguez, F. 1965. Distribucion de Chaetog- natha en Veracruz, Ver.—Anales del Instituto de Biologia, Universidad Nacional Autonoma de México 36(1/2):229-247. Gulf Coast Research Laboratory, P.O. Box 7000, Ocean Springs, Mississippi 39564. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 45-49 SMALLEYUS TRICRISTATUS, NEW GENUS, NEW SPECIES, AND PSEUDOTHELPHUSA PARABELLIANA, NEW SPECIES (BRACHYURA: PSEUDOTHELPHUSIDAE) FROM LOS TUXTLAS, VERACRUZ, MEXICO. Fernando Alvarez Abstract.—One new genus and species, Smalleyus tricristatus, and a new species of Pseudothelphusa, P. parabelliana, are described from the Los Tuxtlas region in the State of Veracruz, Mexico. The new species described here belong to the Tribe Pseudothelphusini. The distribution patterns of both genera are discussed. The Los Tuxtlas region of Veracruz lies adjacent to the coast of the Gulf of Mexico, and comprises the area between 18°10’N to 18°40'N and 94°45'W to 95°25'W. This re- gion encompasses a small mountain range of volcanic origin, where the highest vol- canic cone is more than 1700 m high. In this area four genera and six species of pseu- dothelphusid crabs co-occur: Odontothel- phusa maxillipes (Rathbun, 1898), Te- huana veracruzana (Rodriguez & Smalley, 1969), 7. poglayenorum (Pretzmann, 1980), T. diabolis (Pretzmann, 1980), Smalleyus tricristatus, and Pseudothelphusa parabel- liana (described below). Topographic het- erogeneity, the presence of tropical rainfor- est, and the fact that this is an isolated mountain range situated on the coastal plain, may account for much of the observed di- versity. Future collections in southern Ve- racruz and Tabasco will confirm if, in fact, pseudothelphusid crabs are absent from these coastal lowlands. This suggests that Los Tuxtlas may have served as a refuge in the past and that its brachyuran fauna has been preserved. The sites where collections were made are at altitudes that range be- tween 200 and 1000 m. All the organisms are deposited in the Carcinologic Collec- tion, Instituto de Biologia, Universidad Na- cional Autonoma de México (IBUNAM). Smalleyus, new genus Diagnosis.--In cephalic view, proximal half of gonopod thinner than distal half. In mesial view, middle portion, along longi- tudinal axis, narrower than rest. In caudal view, lateral process also exhibiting con- striction in middle portion. In lateral view, proximal half straight with constant thick- ness; distal half slightly curved caudally. Apex of gonopod bearing 3 lobes: mesial, cephalolateral, and lateral. Mesial lobe with basal *4 of crest disposed at 90° angle to longitudinal axis of gonopod; distal portion sloping proximally; small field of spines along mesial surface of crest; apical margin of crest serrate, spine size increasing distal- ly. In cephalic view, mesial process with cephalic serrate projection, lying oblique to longitudinal axis of gonopod. Cephalolater- al lobe with median ridge in apical cavity, cephalic blade-like projection oriented cephalolaterally. Apical median ridge rounded, bearing spines. Cephalolateral projection with 3 strong teeth. Lateral lobe forming lateral wall of apical cavity. Field of spines along lateral crest and lateral sur- face; spine size increasing laterally and ce- phalically. Field of terminal pore setae sit- uated between median ridge and lateral crest. Sperm channel opening situated caudal to median ridge. 46 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Type species. —Smalleyus tricristatus. Etymology.—This genus is named after Dr. Alfred E. Smalley. Gender is masculine. Smalleyus tricristatus, new species Fig. 1 Material examined. —Camino Izquierdo, Sierra de Santa Marta, Veracruz (18°26’N, 94°57'W), Jul 1985, collector Mardocheo Palma: male holotype, c.b. 23.4 mm, c.l. (5-tmm: 2. females. cbs. 272.2232 ine c.l. 17.0, 14.9 mm, IBUNAM EM-7030. The large female had 19 juveniles in the abdo- men. Gonopod description. —Same as of genus. Description.—Carapace slightly convex. Superior frontal border formed by sloping of carapace; inclined towards median re- gion. Inferior frontal border well marked, formed by diffuse tubercles; sinuous in fron- tal view, arched in dorsal view. Median groove short, deep between front and post- frontal lobes. Cervical grooves straight. Notch on anterolateral margin between or- bit and cervical groove. Anterolateral mar- gin with 17-19 small blunt denticles be- tween cervical groove and epibranchial region. Pterygostomian region, around third maxillipeds, covered with setae. Third max- illiped with ischium/exopod ratio of 0.71. Five rows of spines on dactylus of walking legs. Strong heterochely in males, in females obvious size differences. Cutting margins of propodus and dactylus of major chelae with alternating large and small teeth, when closed large teeth opposing small ones on opposite finger. Type.—The holotypic male is deposited in the Carcinologic Collection, Instituto de Biologia, Universidad Nacional Autonoma de México (Catalog No. EM-7029). Etymology. — From the Latin “‘tri’”’ (three) and “crista’’ (crest), referring to the three crests on the apex of the male’s gonopod. Remarks. —Smalleyus belongs to the Tribe Pseudothelphusini because it exhibits a curved sperm channel, a reniform mesial process, and a discernible lateral lobe. A new genus is created due to the presence of: a mesial process whose shape is not com- pletely reniform as in Pseudothelphusa or Tehuana and bearing spines along its su- perior margin; a cephalic serrate projection of the mesial process; three ridges (crests) on the apex of the gonopod, the median one partly filling what would otherwise be the apex cavity; a cephalolateral lobe, which seems to be a continuation of the median apical ridge; a lateral lobe, which corre- sponds to the lateral lobe in the genus Pseu- dothelphusa, but in this crab occupying a more caudal position; and three spine fields, one on each one of the three apical ridges. The relationships of this genus with the oth- er genera of the tribe are not clear. However, this aberrant form, together with Spirothel- phusa, Lobithelphusa, Odontothelphusa, and Disparithelphusa constitute a belt of mono- typic genera dispersed along the Isthmus of Tehuantepec. Even though these taxa be- long to three different tribes, the factors in- fluencing the origin of these five genera may be similar. In this case, the isthmus repre- sents a barrier that these crabs could not cross (Rodriguez 1987). Epithelphusa with two species, occurring in the same area, has more distinct affinities. Rodriguez (1982) places the genus linking the tribes Hypo- lobocerini and Pseudothelphusini. The af- finities of the monotypic genera mentioned are obscure, with the exception of Odon- tothelphusa which derives from the genus Potamocarcinus. Pseudothelphusa parabelliana, new species Fig.’ 2 Material examined. —Cerro El Vigia, Los Tuxtlas Biological Station, Veracruz (18°35'N, 95°03’W), 7 Jul 1986: male ho- lotype, c.b. 24.5 mm, c.l. 15.8 mm; 1 male paratype, c.b. 21.4 mm, c.l._13-0 sami females, c.b..34.1, 19.2,.c.l. 21.3, Pi Seana IBUNAM EM-7031. Same locality, 30 Aug 1984, collector Mardocheo Palma: 1 male VOLUME 102, NUMBER 1 47 Fig. 1. Left gonopod and major chela of Smalleyus tricristatus: a, Total mesial view; b, Cephalic view of apex; c, Lateral view of apex; d, Caudal view of apex; e, Apical view; f, Right chela. paratype, c.b. 23.9 mm, c.l. 14.8, IBUNAM in abdomen, c.b. 28.0 mm, c.l. 16.9 mm, EM-7032; 5 females c.b. 32.3, 29.2, 27.7, IBUNAM EM-7034. Ue) 20.9 mim, cl. 18.8. 17.6, 16.8, 14.0, Description. —Carapace slightly convex. 13.6 mm, IBUNAM EM-7033. Same lo- Superior frontal border absent, but front cality, 7 Jul 1986, 1 female with 8 juveniles limited by edge. Front inclined in dorsal 48 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Left gonopod of Pseudothelphusa parabelliana: a, Total mesial view; b, Cephalic view of apex; c, Lateral view of apex; d, Caudal view of apex. view. Inferior frontal border smooth, some- frontal lobes. Cervical grooves shallow, what bilobed in dorsal and frontal views. wide, straight; not reaching anterolateral Median groove narrow, deep, dividing su- margin. Anterolateral margin with slender perior edge of front and separating post- notch lateral to orbit. Anterolateral margin VOLUME 102, NUMBER 1 with 16-19 denticles between cervical groove and epibranchial region. Ratio is- chium/exopod of third maxilliped 0.91. Pterygostomian region covered with setae. Major chelae right, fingers not gaping. Gonopod description.—Well developed reniform mesial process. Marginal process reduced to acute spine. Mesial crest round- ed. Lateral lobe completely closing apical cavity cephalically and ending in 2 tips dis- tally; inferior sharper than superior. Lateral lobe with mesial surface triangular. Ter- minal pore setae 19. Setal field restricted to lateral portion of cavity. Mesial crest higher than lateral. Opening of sperm channel cau- dal. Type.—The holotypic male is deposited in the Carcinologic Collection, Instituto de Biologia, Universidad Nacional Autonoma de México (Catalog No. EM-7028). Etymology. —From the Latin “‘para’’ (be- side) and “‘belliana”’ a freshwater crab spe- cific name. Remarks.—Before this species was de- scribed the genus Pseudothelphusa was known only from the central part and Pa- cific slope of Mexico. The presence of P. parabelliana now widens this distribution to the 95°W meridian. This species seems to be closely related to P. belliana Rathbun, 1898, which occurs in the states of Guer- rero, Michoacan, and México. The gonopod of P. parabelliana has a lateral lobe with two acute distal tips, a straight mesial crest, and the mesial process is much larger in relation to the marginal process. In P. bel- liana the lateral lobe bears only one distal tip, the mesial crest is broadly rounded, and the mesial process is slightly larger than the 49 marginal process. The occurrence of P. parabelliana in the Gulf coast of Mexico agrees well with the morphocline proposed recently by Rodriguez (1987). He places on a west-east axis, across central Mexico, a succession of species (including Tehuana veracruzana, P. guerreroensis Rathbun, 1933, P. belliana, P. americana de Saussure, 1857, and P. peyotensis Rodriguez & Smal- ley, 1969) in which a progressive reduction of the lateral lobe can be seen. Acknowledgments I wish to thank Mardocheo Palma for col- lecting most of the crabs included in this study, and Dr. Alfred E. Smalley for pro- viding much helpful advice and reviewing the manuscript. This study was supported by a grant from the Mesoamerican Ecology Institute of Tulane University. Literature Cited Pretzmann, G. 1980. Von Dr. Ivo Poglayen-Neuwall 1975 in Mittelamerika gesammelte Krabben. — Annalen Naturhistorisches Museum Wien 83: 651-666. Rodriguez, G. 1982. Les crabes d’eau douce d’Amé- rique. Famille des Pseudothelphusidae. — Faune Tropicale 22:1-223. . 1987. Centers of radiation of freshwater crabs in the Neotropics. Pp. 51-67 in R. H. Gore & K. L. Heck, eds., Crustacean issues 3: Biogeog- raphy of the crustacea. A. A. Balkema, Rotter- dam. Department of Biology, Tulane Univer- sity, New Orleans, Louisiana, 70118. Pres- ent address: Department of Zoology, Uni- versity of Maryland, College Park, Maryland 20742. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 50-77 TWO NEW GENERA AND NINE NEW SPECIES OF GERYONID CRABS (CRUSTACEA, DECAPODA, GERYONIDAE) Raymond B. Manning and L. B. Holthuis Abstract. —The family Geryonidae Colosi, 1923 is restricted to three genera: Geryon Kroyer, 1837, containing two species, G. trispinosus (Herbst, 1803), and G. longipes A. Milne Edwrds, 1882; Chaceon, new genus, containing 21 species, eight of which are newly described; and Zariquieyon, new genus, con- taining one new Mediterranean species, Z. inflatus. The new species of Chaceon and their ranges are: C. atopus, Saint Helena Island; C. bicolor, central Pacific Ocean; C. crosnieri, Madagascar; C. eldorado, northern South America; C. inglei, northeastern Atlantic; C. mediterraneus, western Mediterranean Sea; C. notialis, Uruguay and Argentina; and C. sanctaehelenae, Saint Helena Island. In addition to results published elsewhere (see Manning & Holthuis 1984, 1986, 1987, 1988), our studies on deep-sea crabs of the family Geryonidae have revealed the exis- tence of nine other undescribed species from various localities that can be assigned to two new genera. These taxa are named herein. Specimens have been deposited in the British Museum (Natural History), London (BMNH), the Muséum National d’Histoire Naturelle, Paris (MNHN), the Rijksmu- seum van Natuurlijke Historie, Leiden (RMNH), the National Museum of Natural History, Smithsonian Institution, Washing- ton (USNM), and the Zoological Museum, Copenhagen (ZMC). We use the following abbreviations: cb, carapace breadth, measured between the tips of the posterior pair of anterolateral teeth; cl, carapace length, measured on the mid- line; fm, fathoms; leg, collector; m, meter(s); mm, millimeter(s); P5, fifth leg (fourth walking leg); sta, station. Family Geryonidae Colosi, 1923 Geryonidae Colosi, 1923:249. Diagnosis. —Carapace hexagonal, with three or five anterolateral teeth on each side. Suborbital margin with inner tooth only. Chelipeds unequal, merus with subdistal dorsal spine, carpus with strong inner spine. Chelae portunid-like. Walking legs with na- ked dactyli, lacking segments expanded for swimming. Abdomens of male and female with seven free.segments. Remarks. —The status of the family Ger- yonidae and of the genera assigned to it have long posed problems for students of the group, as we already have pointed out (Manning & Holthuis 1981:109). That the family Geryonidae deserves recognition as a family distinct from the Xanthidae s.]. and the Goneplacidae s.l. and that its affinities are with the Portunidae no longer seem to be in question. Several genera of uncertain affinities have been placed in the family Geryonidae (see Guinot 1971:1077—1078), e.g., Paragalene Kossmann, 1878, Bathyplax A. Milne Ed- wards, 1880, Platypilumnus Alcock, 1894, Progeryon Bouvier, 1922, and Platychelo- nion Crosnier & Guinot, 1969. In spite of Guinot’s (1969:692) observa- tion, “Les deux genres monospécifiques Progeryon and Platypilumnus nous parais- sent étroitement apparentés a Geryon, in- séparables de celui-ci,’’ we do not believe VOLUME 102, NUMBER 1 that these or any of the genera other than Geryon and the two new genera established here belong in the Geryonidae. We believe that for the moment all other Recent genera formerly assigned to the Geryonidae should be placed in the Xanthidae s.l. Several of them, including Paragalene and Progeryon, may well belong in a new family. Members of all of the genera here ex- cluded from the Geryonidae lack the por- tunid-like chelipeds and the characteristic subdistal dorsal spine on the merus of the chelipeds found in the geryonids proper as well as in some portunids, and they all can be distinguished from geryonids as restrict- ed here by these features alone. Further, all of the geryonids as restricted here have na- ked dactyli on the walking legs and lack black fingers on the chelae, other features that will distinguish them from members of Para- galene and Progeryon. As restricted here, the Geryonidae com- prise three genera and 24 species: Geryon Krgyer, with 2 species; Chaceon, new genus, with 21 species; and Zariquieyon, new ge- nus, with | species. Geryon Kroyer, 1837 Geaven, Kroyer, 1837:10, 20, 21 [type species, by original designation and monotypy, Geryon tridens Kroyer, 1837, a subjective junior synonym of Cancer trispinosus Herbst, 1803]. Chalaepus Gerstaecker, 1856:118 [type species, by monotypy, Cancer trispinosus Herbst, 1803]. Definition. —Geryonid crabs with three anterolateral teeth on each side of the car- apace. Carapace length half to two-thirds width. Branchial regions not markedly in- flated. Frontal teeth poorly developed, small. Orbits shallow, rounded. Included species. —Two, both from the northeastern Atlantic Ocean: Geryon longipes A. Milne Edwards (1882: FG:,39); Geryon trispinosus (Herbst) (1803:43) 51 (=Geryon tridens Kre@yer, 1837, see Man- ning & Holthuis 1987). Remarks. —Geryon differs from both Chaceon and Zariquieyon in having three rather than five anterolateral teeth on each side of the carapace, and the two submedian frontal teeth are smaller than in the repre- sentatives of either of the other two genera. Geryon agrees with Chaceon and differs from Zariquieyon in having the orbits shallow and rounded rather than rectangular, and Ger- yon and Chaceon lack the swollen branchial regions that are characteristic of the only known species of Zariquieyon. Chaceon, new genus Type species.—Geryon fenneri Manning & Holthuis, 1984. Name.—The name is given in honor of our colleague Fenner A. Chace, Jr. The suf- fix -on is used to make the name similar to Geryon. This sufhx should not be consid- ered to be the Greek neuter ending -on. The gender of the name Chaceon is masculine, like that of Geryon. Definition. —Geryonid crabs with five an- terolateral teeth on each side of the cara- pace. Carapace length half to two-thirds width. Branchial regions not markedly in- flated. Frontal teeth well-developed, large. Orbits shallow, rounded. Included species. —Twenty-one, of which eight are described herein. Nominal species include the following: Chaceon affinis (A. Milne Edwards & Bou- vier, 1894:41), northeastern Atlantic. Chaceon chuni (Macpherson, 1983:23), Na- mibia and South Africa. Chaceon erytheiae (Macpherson, 1984:86), Valdivia Bank, southeastern Atlantic. Chaceon fenneri (Manning & Holthuis, 1984:666), northwestern Atlantic. Chaceon gordonae (Ingle, 1985:90), West Africa. Chaceon granulatus (Sakai, 1978:11), Ja- pan. 52 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Chaceon inghami (Manning & Holthuis, 1986:367), Bermuda. Chaceon macphersoni (Manning & Hol- thuis, 1988:83), southwestern Indian Ocean and South Africa. Chaceon maritae (Manning & Holthuis, 1981:112), West Africa. Chaceon atopus, male holotype, cb 124 mm, Saint Helena, dorsal view. Fig. 1. Chaceon paulensis (Chun, 1903:531), cen- tral Indian Ocean. Chaceon quinquedens (Smith, 1879:35), northwestern Atlantic. Two other species originally described in Geryon, Geryon incertus Miers, 1886, and VOLUME 102, NUMBER 1 Geryon ischurodous Stebbing, 1923, were incorrectly assigned to the genus. Manning & Holthuis (1986:369) showed that G. in- certus is a synonym of the portunid Bathy- nectes longispina Stimpson, 1871, and Manning & Holthuis (1988:78) showed that G. ischurodous is a species of the goneplacid genus Carcinoplax. Remarks. — Accounts of two other species, one from Chile, and one from Brazil are in preparation. These 2 species, the 11 known species, and the 8 new species described be- low raise the known number of species to 2 Members of Chaceon agree with Zari- quieyon and differ from Geryon in having five anterolateral teeth on each side of the carapace. Chaceon atopus, new species Figs. 1-2 Material. —Off Rupert’s Bay, Saint He- lena Island [15°58’S, 5°43'W], 130 fm (238 m), 5 Aug 1983, leg A. J. Edwards: one male (holotype, RMNH). Diagnosis. —A large Chaceon, cl 90 mm, cb more than 120 mm in only known spec- imen, with well-developed anterolateral teeth on the carapace in adults and with laterally compressed dactyli on the walking legs. Carapace 1.4 times broader than long, very inflated, strongly convex from front to back, appearing smooth. Median pair of frontal teeth long and sharp, separated by a narrow, V-shaped emargination, medians extending further forward than laterals; out- er margin of lateral frontal tooth with slight convex projection, indicating position of in- ner orbital angle. Anterolateral teeth well- developed, all sharp, fourth smallest but sharp and distinct. Distance from first to second tooth about the same as from third to fourth, distance from first to third tooth less than distance between third to fifth. Carapace surface finely granular postero- laterally. Suborbital tooth strong and sharp- ly pointed, visible in dorsal view, extending about to level of lateral frontal tooth; sub- orbital margin evenly curved, tuberculate. 53 Fig.2. Chaceon atopus, male holotype, cb 124 mm, Saint Helena: a, Ventral view of orbit; b, P5 dactylus, posterior view; c, P5 dactylus, dorsal view. Cheliped merus with sharp spine subdistally and with distal dorsal spine; carpus rough- ened dorsally, with distal outer spine, den- ticulate anterior margin, and strong and slender distal spine; propodus with distal dorsal spine broken in left chela, right chela with distal angled projection. Meri of walk- ing legs with distinct distal dorsal spine. Dactyli of walking legs laterally com- pressed, height at midlength greater than width. P5: merus 6.5 times longer than high, length 0.58 cb; carpus with line of erect spi- nules dorsally; propodus longer than dac- tylus, length 5.8 times height. Size. —Unique male holotype, cl 90 mm, cb 124 mm. Remarks. —This species resembles C. gordonae, from the Cape Verde Islands and Sierra Leone, in many features, including the large size, the well-developed frontal and anterolateral teeth on the carapace, and the compressed dactyli of the walking legs. It differs from C. gordonae in having much 54 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 3. Chaceon bicolor, male paratype, cb 158 mm, Passe de Saint Vincent: a, Dorsal view; 6; Carapace. VOLUME 102, NUMBER 1 longer walking legs, with the merus more than 6 times longer than high, and in its habitat. Chaceon gordonae, in which the P5 merus is less than 6 times longer than high, generally occurs in depths in excess of 2000 m, whereas the present new species occurs in less than 250 m. This species can be distinguished on sight from C. sanctaehelenae, described below, by the long, slender walking legs, the distal meral spine on the walking legs, and the well-developed anterolateral spines of the. carapace. Name.—The specific name is from the Greek, atopos, out of place, strange, our re- action when we learned this. specimen was specifically distinct from the holotype of C. sanctaehelenae, described below. Distribution.—Known only from Saint. Helena Island, in 238 m. - Chaceon bicolor, new species Figs. 3-4 Geryon affinis. —Griffiin & Brown, 1976:256, figs. 7-9.—Sakai, 1978:9, figs. 18-19, pl. 2, fig. D (color). [Not Geryon affinis A. Milne Edwards & Bouvier, 1894.] Geryon quinquedens.—Intés, 1978:7, figs. 5B, 8.— Guinot & Richer de Forges, 1981: 249.—King, 1984:186. [Not Geryon quinquedens Smith, 1879.] Geryon.—Intés, 1978: fig. 10.—Guinot & Richer de Forges, 1981:249. Previous _records.—Emperor Seamount Chain: North of Nintoku Seamount, 42°20'N, 170°50’E, 800 m; Jingu Seamount [38°50’N, 171°15’E], 890-930 m; Kinmei Seamount, 35°34’N, 171°41’E, 600-640 m, and 500-700 m; south of Kinmei Sea- mount, 34°42’N, 171°48’E, 980-1100 m (Sakai 1978). Southwestern Pacific: in depths greater than 600 m (King 1984). Loyalty Islands [21°00'S, 167°00’E]: (Intés 1978). New Caledonia [21°30’S, 165°30’E]: 600- 55 Fig.4. Chaceon bicolor, male paratype, cb 148 mm, Passe de Saint Vincent: a, Ventral view of orbit; b, P5 dactylus, posterior view; c, P5 dactylus, dorsal view. 1000 m (Intés 1978; Guinot & Richter de Forges 1981). New South Wales, Australia: Southeast - of Grafton, 29°49’S, 153°42’E to 29°59’S, 153°38’E, 369 m; east of Broken Bay, 33°40’S,.151°53’E to 33°22’S, 152°09’E, 450 m=33°40'S,. 151°53’E 10 33°35’S, 151°58’E, 450-810 m, and 33°38’S, 151°57’E to 33°34 891152701 E)..774—792) m;: north of Sydney, 33°43’S, 151°55’E to 33°37’S, 1:52°02'E)}. 675:-m;.. off Sydney, 33°52'S, 152°50’'E to 33°48'S, 152°54’E, 765 m (Grif- fin & Brown 1976). Material. —Emperor Seamount Chain: Kinmei Seamount, 35°17.50'N, 171°25.98’E, 150 fm (275 m), Townsend Cromwell cruise 56 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Cromwell cruise 82-05, sta 57, 11 Nov 1982: three females (USNM 205974). New Caledonia: 23°44’S, 166°58’E, 1490- 1620 m, BIOCAL, Jean Charcot sta CP 57, 1 Sep 1985: one juvenile male, one female (MNHN), one female (USNM 205975).— 23°07'S, 166°51’E, BIOCAL, Jean Charcot sta CP 32, 825 m, 29 Aug 1985: one male (MNHN).—Passe de Saint Vincent [22°02’S, 165°57’'E], 800 m, traps, leg B. Richer de Forges: four males (3 MNHN, 1 USNM 205976). Australia: Southeast of Newcastle, New South Wales, 33°11—09’S, 152°24—25’E, 732 m, leg D. E. Brown on FRV Kapala, sta K77-23-10, 7 Dec 1977: one male (USNM 205978).—East of Broken Bay, New South Wales, 33°35—33’'S, 152°00-02’E, 823 m, leg D. E. Brown on FRV Kapala, sta K77-23- 12, 8 Dec 1977: one male, one female (USNM 205977). The holotype is the male, cl 144 mm, cb 165 mm, from New Caledonia, Jean Char- cot sta CP 32 (MNHN). All of the other specimens are paratypes. Diagnosis. —A very large Chaceon, cl to more than 140 mm, cb to 180 mm in adults, with small, blunt anterolateral teeth on the carapace in adults and with laterally-com- pressed dactyli on the walking legs. Cara- pace 1.1-1.2 times broader than long in adults, 1.4 times broader than long in ju- veniles. Median pair of frontal teeth nar- rower than laterals, separated by U-shaped emargination, medians extending further forward than laterals. Second and fourth an- terolateral teeth reduced, fourth often ob- solete. Distance from first to second an- terolateral tooth less than that from third to fourth, distance from first to third sub- equal to that from third to fifth. Carapace with distinct granulation mesial to fifth tooth and on protogastric, cardiac, and branchial regions; hepatic region smooth; protogastric region inflated in large specimens, especially in females. Suborbital tooth short and blunt in males, longer and sharper in females and juveniles, scarcely or not at all visible in dorsal view, suborbital margin evenly curved, tuberculate. Cheliped lightly tuber- culate dorsally; upper margin of merus with sharp subdistal spine; carpus lacking outer spine in adult, blunt projection present in some specimens, with distinct spine in ju- venile; propodus unarmed distally. Meri of posterior walking legs with distinct distal dorsal angled projection, spined in juve- niles. Dactyli of walking legs laterally com- pressed, height at midlength greater than width. P5: merus 4.3—5.1 (mean 4.6) times longer than high in females, 5.2—5.6 (mean 5.4) times longer than high in males, and 7.0—7.5 times longer than high in juveniles, usually with blunt distal dorsal projection in adults, distinct distal spine in juveniles; merus length 0.49-0.56 cb in females, 0.61- 0.64 cb in males; carpus smoothly tuber- culate dorsally; propodus distinctly longer than dactylus, 3.6-4.6 (mean 4.1) times longer than high in adults, 5.6-6.0 times longer than high in juveniles. Size. — Males, cl 116-147 mm, cb 134— 165 mm; females, cl 21-110 mm, cb 30- 122.5 mm; juvenile, cl 7 mm, cb 10 mm. The largest specimens recorded in the lit- erature are: male, cl 141 mm, cb 155 mm (Sakai 1978); a specimen with cb 176 mm (Griffin & Brown 1976); a specimen with cb 180 mm (Intés 1978). Color.—Anterior part of carapace pre- dominantly purple, branchial regions tan, legs yellowish. Sakai (1978: pl. 2, fig. D) gave a figure in color. Remarks. —Chaceon bicolor differs from all other species of the genus in color pat- tern, with the anterior part of the body pur- plish rather than reddish or tan, set off from the tan branchial regions. Remnants of this distinctive color pattern are visible in one of the juveniles from deep water off New Caledonia. In addition to color pattern, C. bicolor also differs from the only other species known to occur in the central Pa- cific, C. granulatus, in having compressed rather than depressed dactyli on the walking legs; also, the hepatic region of the carapace VOLUME 102, NUMBER 1 in C. granulatus is coarsely granular, where- as it is smooth in C. bicolor. The juvenile specimens taken in 1490- 1620 m off New Caledonia differ from the adults in many features: the teeth of the carapace are much larger and sharper, there is a sharp outer spine on the carpus of the cheliped and a sharp distal spine on the me- rus of each walking leg, and the legs are much longer and slenderer. As mentioned above, one specimen shows traces of the typical color pattern of the adults, suggest- ing that these small specimens are juveniles that occur in much deeper water than do the adults. Adult females differ from males in having much sharper anterolateral teeth on the car- apace, sharper suborbital spines, and much shorter legs, with less trace of a distal dorsal projection on the merus. Also, the carapace of females is more strongly arched from front to back and the protogastric regions are no- ticeably more inflated. Our specimens were taken in depths of 275, 732, 800, 823, 825, and 1490-1620 m; the juveniles were collected at the latter depth. Depth records in the literature in- clude: 369 to 774-792 m (Grifin & Brown 1976); 500-700 to 980-1 100 m (Sakai 1978); 600-1000 m (Intés 1978, Guinot & Richer de Forges 1981); and in depths greater than 600 m (King 1984). Name.—The specific name is from the Latin, the prefix bi- and color, referring to the purple and tan color pattern of this species in life. Distribution. —Widely distributed in the central Pacific, from the Emperor Seamount Chain (42°20'N) to eastern Australia, off Sydney (33°52’S), in depths between 275 and about 1600 (1490-1620) m. Chaceon crosnieri, new species Figs. 5-6 Material.— Madagascar: 22°21'S, 43°05.5’E, 450-420 m, sta 27, 15 Jan 1986: two males, three females (MNHN).—22°13.5’S, 57 43°05’E, 530 m, mud, chalutage 62, leg Rudo von Cosel, 19 Oct 1986: one female (MNHN).—22°26.1'S, 43°04.6’E, 520 m, mud, chalutage 65, leg Rudo von Cosel, 1986: one male, four females (MNHN).— PPV S45 02.5 FE, 560 m, mud, chalu- tage 75, leg Rudo von Cosel, 23 Oct 1986: two females (MNHN).—22°24.7’S, 43°04.2’E, 535 m, mud, chalutage 91, leg Rudo von Cosel, 4 Nov 1986: one male, two females (USNM 205979).—22°24.6’'S, 43°03.7’E, 590 m, mud, chalutage 93, leg Rudo von Cosel, 7 Nov 1986: one male, one female (MNHN).—22°S, 43°E, 790 m, mud, chalutage 102, leg Rudo von Cosel, 24 Nov 1986: one male, one female (MNHN).—22°24.7'S, 43°03.7’E, 630 m, mud, chalutage 115, leg Rudo von Cosel, 28 Nov 1986: one female (MNHN). The holotype is the male, cl 116 mm, cb 140 mm, from chalutage 93; all other spec- imens are paratypes. Diagnosis.—A very large Chaceon, cl to 127 mm, cb to 155 mm in adults, with low, blunt anterolateral teeth on the carapace in adults and with laterally compressed dactyli on the walking legs. Carapace 1.2 times broader than long, very inflated dorsally, especially at protogastric regions Median pair of frontal teeth narrower than laterals, not set ahead of laterals, both pairs extend- ing about to same level. All five anterolat- eral teeth reduced, distance from first to sec- ond equal to distance from third to fourth, distance from first to third equal to distance from third to fifth. Carapace relatively smooth, with small granules and pits on branchial, cardiac, and gastric regions, he- patic regions smooth. Suborbital tooth sharp in females, very short and blunt in males, scarcely visible in dorsal view, suborbital margin concave, tuberculate. Cheliped lightly granular, not conspicuously rough- ened, merus with sharp subdistal spine; car- pus irregular dorsally, with sharp inner tooth, lacking any trace of outer tooth; prop- odus with some small tubercles dorsally, lacking distal spine. Meri of walking legs, Fig. 5. Chaceon crosnieri, male holotype, cb 140 mm, Madagascar: a, Dorsal view; b, Carapace. Female paratype, cb i27 mm, Madagascar: c, Carapace, lateral view. VOLUME 102, NUMBER 1 especially posterior ones, with distal, dorsal spine. Dactyli of walking legs laterally com- pressed, height at midlength greater than width. PS: merus 4.1—5.0 (mean 4.7 in males, 4.5 in females) times longer than high, with distal dorsal spine, length 0.47-0.55 cb (mean 0.51) in females, 0.57-0.63 cb (mean 0.59) in males; carpus lacking erect spinules dorsally; propodus length 3.6-4.4 times height (mean 3.9 in males, 4.0 in females), usually longer than dactylus, subequal to dactylus in large females. Size. —Males, cl 83-127 mm, cb 101-155 mm; females, cl 82-127 mm, cb 97-148 mm. Color.—In preservative, some males show tips of fingers of chela with red band proxi- mally, apices whitish. Color in life un- known. Remarks. —Chaceon crosnieri differs from C. affinis in that the carapace is much more inflated, the outer orbital and the suborbital teeth are stronger, the subdistal tooth on the merus of the cheliped is stronger and the cheliped is smoother dorsally, the carpus of the walking legs lacks dorsal spinules, and the merus of the walking legs, especially the posterior ones, has a strong distal dorsal spine. This new species differs from C. chuni in being much larger, cb to 155 mm, the carapace is much more inflated, especially at the protogastric region, the gap between the first and second anterolateral tooth of the carapace is larger (equal to distance from third to fourth in C. crosnieri, less in C. chuni), the frontal teeth of the carapace are stronger, the suborbital spine is smaller, and the carpus of the cheliped lacks an outer spine. Chaceon crosnieri is a much smoother species than C. bicolor, with much shorter, stouter legs, the suborbital spine is much lower and blunter, and the distal projection on the merus of the walking legs is much less developed in larger specimens. A male of C. paulensis in the USNM, cl so mm), ‘cb 113 mm; ‘from: 38°24.92'S, 77°25.15'E, in 1050-1110 m off Amster- dam Island in the southern Indian Ocean, a9 Fig. 6. Chaceon crosnieri, male paratype, cb 155 mm, Madagascar: a, Ventral view of orbit; b, PS dac- tylus, posterior view; c, P5 dactylus, dorsal view. is available for comparison. It shares the compressed dactyli of the walking legs with C. crosnieri, and little else. It differs in many features, especially in having strongly de- veloped, sharp anterolateral teeth on the carapace and on the meri of the walking legs, and in having a large, sharp outer spine on the carpus of the cheliped. Chaceon crosnieri was taken together with C. macphersoni at sta 27 and at chalutages 62, 65, 91, and 93. The two species can be distinguished immediately, as C. macpher- soni is much rougher dorsally and has the dactyli of the walking legs depressed, not laterally compressed. Our specimens were taken in depths of 420-450 to 790 m, with five samples being taken in depths between 520 and 590 m. Name.—We are pleased to dedicate this 60 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig..7: Chaceon eldorado, male holotype, cb 109 mm, Venezuela: a, Dorsal view; b, Carapace. VOLUME 102, NUMBER 1 species to our colleague Alain Crosnier, Mu- séum National d’Histoire Naturelle, Paris, who made special efforts to save specimens of geryonids whenever they were encoun- tered in the field. Distribution. —Known only from locali- ties around Madagascar, in depths between 420-450 and 790 m. Chaceon eldorado, new species Figs. 7-8 Geryon quinquedens. — Takeda, 1983:15, 18, 31, 164, color fig. on p. 164. [Not Geryon quinquedens Smith, 1879.] Previous records. —Off Suriname and French Guiana, 310-790 m (Takeda 1983). Material.—Colombia: 12°06'N, 72°55'W, 350-500 fm (641-915 m), Oregon sta 4912, 31 May 1964: one male (USNM 205980). Venezuela: 12°55'N, 70°16’W, 340 fm (622 m), Oregon IT sta 11307, 26 Nov 1970: one female (USNM 205981).—11°53'N, 69°25'W, 350 fm (641 m), Oregon sta 4413, 3 Oct 1963: one male (USNM 205982).— 11°36'N, 62°46'W, 290 fm (531 m), Oregon sta 2777, 19 Apr 1960: two males (USNM 205983). French Guiana: 7°37'N, 53°32’'W, 395 fm (723 m), Oregon IT sta 10616, 13 May 1969: one male (USNM 205984). The male, cl 89.5 mm, cb 109 mm, from Oregon sta 4413, is the holotype (USNM 205982); the other specimens are paratypes. Diagnosis. —A moderately large Cha- ceon, cl to 89.5 mm, cb to 109 mm in ma- terial examined, with low, blunt anterolat- eral teeth on the carapace in adults and with dorsoventrally depressed dactyli on the walking legs. Carapace 1.2—1.3 times broad- er than long, inflated dorsally, especially at protogastric regions. Median pair of frontal teeth about as wide as and extending farther forward than laterals. Second and fourth an- terolateral teeth usually reduced, much smaller and lower than remainder. Distance from first to second tooth equal to or less 61 Fig. 8. Chaceon eldorado, male holotype, cb 109 mm: a, Ventral view of orbit; 6, PS dactylus, posterior view; c, P5 dactylus, dorsal view. than that from third to fourth tooth, dis- tance from first to third tooth less than that from third to fifth. Carapace granular pos- terolaterally and on cardiac and protogastric regions, hepatic region smooth. Suborbital tooth short, broad, visible in dorsal view, lower margin of orbit evenly curved, tuber- culate. Cheliped lightly granular; merus with sharp subdistal spine; carpus with sharp in- ner tooth and distinct angled projection or 62 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON low tooth on outer margin; propodus un- armed distally. Meri of walking legs, espe- cially posterior ones, with distal dorsal tu- bercle, lacking distinct distal spine. Dactyli of walking legs dorsoventrally depressed, height at midlength less than width. P35: merus 5.3—5.9 (mean 5.5) times longer than high, length 0.56 cb in female, 0.61-0.67 (mean 0.63) cb in males; carpus with line of erect spinules dorsally; propodus length 4.5-5.1 (mean 4.8) times height, longer than dactylus. Size. — Males, cl 46-89.5 mm, cb 56-109 mm; only female examined, cl 48 mm, cb 64 mm. Color. —Takeda’s (1983:164) colored fig- ure shows a dark red crab. Remarks. —This species resembles C. quinquedens in having depressed dactyli on the walking legs, but differs in that the legs are shorter (P5 propodus 5-7 times longer than high) and lack a strong distal spine on the merus, the propodus of the chela lacks a distal dorsal spine, and the carapace is more granular. The specimens from stations 4912 (male, cl 47 m), 11,307 (female, cl 48 mm), and 10,616 (male, cl 46 mm) have much stron- ger anterolateral spines on the carapace than those from stations 2777 (males, cl 53.5 and 55 mm) and 4413 (female, cl 89.5 mm). Takeda (1983) reported this species from depths between 310 and 790 m. Our spec- imens were taken in depths of 531, 622, 641, 641-915, and 723 m. Name. —The name refers to the mythical land of gold, El Dorado, thought by six- teenth century Spanish explorers to be in northern South America. Distribution. —Northern coast of South America, from Colombia to French Guiana, in depths between 531 and 641-915 m. Chaceon inglei, new species Figs. 9-11 Geryon affinis. —Hansen, 1908:19, pl. 1, fig. la, b. [Not Geryon affinis A. Milne Ed- wards & Bouvier, 1894.] Geryon gordonae Ingle, 1985:90, figs. 3, 4 [part, not material from Sierra Leone and Cape Verde Islands]. Previous records.—Northeastern Atlan- tic: 61°33'N, 19°0’W, 1089 fm (1993 m) and 61°30'N, 22°30’W, 975 fm (1784 m) (Han- sen 1908).—56°49’-56°48'’N, 09°51’— 09°57'W, 2000 m; 51°6.8’-51°6.9'N, 13°16.7'-13°24.4'W, 1817-1930 m; 51°05.3’— 51°06.5'N, 13°04.5’-12°59.5'W, 1925-1960 m; 49°39.5'N, 12°36.9'W, 1857-1910 m; 49°38.6’N, 12°40.9’'W, 1860-1875 m; 49°32.6'-49°33.5'N, 13°7.1'-13°5.9'W, 1630- 1640 m; 49°30.1'’-49°27.7'N, 13°19.9'— 13°17.2'W, 1794-1785 m; and 49°27.3’— 49°30.1’N, 13°21.1'-13°26.8'W, 2045-2110 m (Ingle 1985). Material.—North Atlantic: 61°33’N, 19°00'W, 1089 fm (1993 m), Ingolf sta 65: one male (ZMC).—61°30'N, 22°30'W, 975 fm (1784 m), Ingolf sta 67: one ovigerous female (ZMC).—56°49’—-56°48'N, 09°51’-09°57'W, 2000 m, Challenger sta 12, leg R. W. Ingle: one female (BM 1978.102).—55°07.7'N, 15°11.2'W to 55°10.3’N, 15°09.3"W, 2215— 2233 m, COB NORATLANTIQUE, PR 0006, sta CH04, Blake trawl, 10 Aug 1969: two males (USNM 205986).—49°27.3’— 49°30.1’N, 13°21.1’-13°26.8'W, 2045-2110 m, Challenger sta 50518, 7 Jun 1979: one male (BMNH).—48°45’N, 11°19.8’W to 48°46.6’N, 11°21.8’W, 1830-1870 m, Thal- assa sta 2448, 1973: one female (MNHN B.15835).—48°34'N, 10°51.6’W to 48°32.9’N, 10°49’W, 1975-2070 m, Thalassa sta 2453, 1973: one female, two juveniles (MNHN B.15834).—47°34.6’N, 08°38.8’W, 2245 m, BIOGAS IV, Jean Charcot sta CP 01, 25 Feb 1974: one male, one female (MNHN B.7215).—47°34.5'’N, 08°34.2’W, 2180 m, CENTOB BIOGAS, sta 011, CV 08: one fe- male (MNHN _B.17207).—47°34.1'N, 08°40.5'W, 2175 m, CENTOB BIOGAS XI, sta 1, CP 37: one female (MNHN B.17583).— 47°34'N, 8°41'W, 2100 m, CENTOB, EPITV, sta 1, CP 40, 3 Sep 1985: one juvenile female (MNHN B.17585).—47°33.2'N, 08°38.5'W, 2177 m, CENTOB BIOGAS, PR 08, CP: VOLUME 102, NUMBER 1 63 Fig. 9. Chaceon inglei, male paratype, cb 61 mm, North Atlantic: a, Dorsal view; 5, Carapace, enlarged. 64 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 10. Chaceon inglei, male paratype, cb 34 mm, North Atlantic: a, Carapace; b, Ventral view of orbit; c, Cheliped, dorsal view; d, Chela, outer view; e, P5; f, P5 dactylus, dorsal view; g, PS dactylus, posterior view. one female (MNHN B.15821).—47°32.8'N, 08°33.5'W, 2115 m, BIOGAS VI, CP 26: two males, one female (USNM 205987). — 47°32.7'N, 08°34.2'W, 2034 m, BIOGAS II, CV 23: one ovigerous female (MNHN B.17208).—47°31.4'’N, 8°42.7'W, 2100 m, CENTOB, EPIIV, sta 1, CP 41, 4 Sep 1985: one male (MNHN B.17586).—47°31'N, 08°16'W, 2200 m, BIOGAS I, CV 06: 2 females (MNHN B.15820).—47°28.1'N, 08°25.1'W to 47°29.6'N, 08°22.6’W, 2149- 2047 m, COB NORATLANTIQUE, CHOO4, PR 124, BO19, sta 48, Blake Trawl, 31 Oct 1969: one male, one female (MNHN B.15822).—42°32'N, 08°39.4'W, 2100 m, CENTOB, EPI I, sta 1, CP 39, 30 Mar 1984: one female (MNHN B.17584).—39°04.5'N, 32°43.5'W, 2120 m, Blake trawl, BIA- CORES 1971, sta 131, 24 Oct 1971: one male, one female (MNHN B.15836). The female from Challenger sta 12, cl 43 mm, cb 62 mm, is the holotype (BM 1978.102). The other specimens are para- types. Diagnosis.—A small Chaceon, cl to 54 mm, cb to 72 mm in adults, with sharp, well-developed anterolateral spines on the carapace in adults and with laterally com- pressed dactyli on the walking legs. Cara- pace 1.3—1.5 times broader than long. Me- dian pair of frontal teeth strong, sharp, separated by U-shaped sinus, medians nar- rower and extending farther forward than laterals. Second lateral tooth small, fourth usually obsolete or even totally absent, fifth usually largest. Distance from first to second VOLUME 102, NUMBER 1 65 Rigs 11. 28 mm, dorsal view. tooth subequal to or less than distance from third to fourth tooth, distance from first to third tooth subequal to or less than distance from third to fifth tooth. Suborbital tooth large, extending at least to level of outer frontal tooth, visible in dorsal view, sub- orbital margin evenly concave. Cheliped roughened dorsally; merus with sharp sub- distal and smaller distal spine; carpus with long inner spine and shorter outer spine; propodus with distal dorsal spine or angled projection. Meri of walking legs, especially fourth and fifth, with distal, dorsal spine. Dactyli of walking legs laterally com- pressed, height at midlength greater than width. P5: merus more than 6 times longer than high, 6.5—7.2 (mean 6.8) times in males, 6.3-7.5 (mean 6.7) times in females. 8.0— 9.0 times in juveniles, with distal dorsal spine, length 0.52—0.61 cb (mean 0.56 cb) in females, 0.53—0.66 cb (mean 0.60 cb) in males; carpus with line of erect spinules dor- sally; propodus 5.1—6.7 (mean 5.7 in both sexes) times longer than high, longer than dactylus. Chaceon inglei, North Atlantic: a, Male paratype, cb 18 mm, dorsal view; b, Male paratype, cb ca. Size.—Males, cl 22-54 mm, cb 34-72 mm; females, cl 15—45 mm, cb 24-62 mm; ovigerous females, cl 43 and 44 mm, cb 61 mm; juveniles cl 9 mm. Hansen (1908) re- ported a male with cl 40 mm, an ovigerous female with cl 42 mm. Ingle (1985) studied males with cl 11.5—49.5 mm, females with cl 7-43 mm. Remarks.—The long anterolateral teeth of the carapace, the long, slender legs, with the merus of the fifth leg more than 6 times longer than high, the sharp outer spine on the carpus of the claw and the merus of the walking legs, all will serve to differentiate this species from C. affinis, the only other species of Chaceon known to occur in the northeastern Atlantic off the coast of Eu- rope. Chaceon affinis, which, like this species, has compressed dactyli on the walking legs, differs from C. inglei of the same size in the features mentioned above and in having smaller and blunter frontal teeth on the car- apace and a much smaller suborbital spine. A small male, cl 30 mm, cb 42 mm, of C. 66 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 12. Chaceon mediterraneus, male holotype, cb 65 mm, Mediterranean, dorsal view. affinis available for comparison (USNM) has a much shorter fifth leg, with the merus less than 6 times as long as high and the prop- odus less than 5 times as long as high. The merus shows no trace of the distal, dorsal spine that is so prominent in members of C. ingle. Chaceon gordonae, a species that occurs off West Africa, is a much larger species, cb to at least 161 mm (male from the Cape Verde Islands, MNHN B.6432) rather than less than 75 mm, that has much shorter legs, with the merus less than 6 times longer than high. In C. gordonae the fourth anterolateral tooth of the carapace is present, whereas it usually is obsolete in C. inglei. This species differs from Chaceon medi- terraneus, described below, in having com- pressed rather than depressed dactyli on the walking legs. That species also inhabits rel- atively deep water. Small specimens that lack the second and fourth anterolateral teeth of the carapace could be mistaken for Geryon longipes; both species occur together in the northeastern Atlantic. The frontal teeth of G. /ongipes are much smaller than those of C. ing/ei at the same carapace length. This species occurs in relatively deep water, with all records coming from depths in excess of 1600 m. The specimens re- ported by Hansen (1908) were taken in 1784 and 1993 m, and Ingle (1985) saw material from depths ranging from 1630-1640 to 2045-2110 m. Our specimens were taken in depths between 1784 and 2245 m, with most lots coming from depths in excess of 2000 m. Name.—We are pleased to dedicate this species to our colleague R. W. Ingle, British Museum (Natural History). Distribution. —Northeastern Atlantic, from about 61°N, south of Iceland, to 39°N, off the Azores, in depths between 1630-1640 m to 2245 m. Chaceon mediterraneus, new species Figs. 12-13 Geryon gordonae. —Della Croce, Drago, & Flocchini, 1988:6, 7, 8 [not Geryon gor- donae Ingle, 1985]. VOLUME 102, NUMBER 1 ZOD Fig. 13. Chaceon mediterraneus, male holotype, cb 65 mm, Mediterranean: a, Ventral view of orbit; b, P5 dactylus, posterior view; c, P5 dactylus, dorsal view. Previous records. —Mediterranean Sea, north of Sardinia, 1990-2008 m (Della Croce, Drago, & Flocchini, 1988). Material.— Mediterranean Sea, 37°56.7'N, 07°31.6’E, 2830 m, POLYMED sta CV 04, 18 May 1970: one male (holotype, MNHN B.15824). Off Sardinia, 1990-2016 m; N. Drago: one male (USNM); one male, one female (BMNH). Diagnosis. —A moderately large Cha- ceon, cl to 78 mm, cb to 103 mm, with well- developed anterolateral teeth on the cara- pace and with dorsoventrally depressed dactyli on the walking legs. Carapace 1.3 times broader than long. Median pair of frontal teeth broad and short, separated by V-shaped emargination, medians extending further forward than laterals. Orbit broadly concave, with low swelling on margin of inner orbital tooth. First, third, and fifth anterolateral spines stronger than remain- der, fifth strongest, slender; gap between first and second tooth very small. Distance from first to second tooth subequal to distance from third to fourth tooth, distance from first to third tooth less than distance from 67 third to fifth tooth. Raised areas of carapace pitted and eroded, but not tuberculate. Sub- orbital tooth strong, sharp, extending about to level of lateral frontal tooth, suborbital margin tuberculate, evenly rounded. Che- liped sparsely tuberculate dorsally; upper margin of merus with sharp subdistal spine and distal angled lobe; carpus with strong inner spine and distinct but smaller outer spine; propodus with distinct distal spine. Meri of walking legs broad, upper margin distinctly convex, with distal, dorsal spine. Dactyli of walking legs dorsoventrally de- pressed, width near midlength slightly larg- er than height. P5: merus 4.5-5.4 times longer than high, with distal dorsal spine, length about half cb; carpus with line of sharp spinules dorsally; propodus 4.1-4.3 times longer than high, slightly longer than dactylus. Size.—Males. cl 50-78 mm, cb 65-103 mm; female, cl 59 mm, cb 82 mm. Remarks. —This species resembles C. maritae and differs from both C. affinis and C. inglei in having relatively broad, de- pressed dactyli on the walking legs. It differs from C. maritae in having much stronger anterolateral spines on the carapace (even when specimens of the same size are com- pared), in having distal dorsal spines on the meri of the walking legs, and in having slen- derer walking legs. The merus of the fifth leg is more than 5 times longer than high in C. mediterraneus, about 4 times longer than high in C. maritae. Although the dactyli of the walking legs of C. mediterraneus are not as conspicu- ously flattened as in C. maritae, they are distinctly broader than the dactyli in C. gor- donae or C. inglei. It is more than a little surprising to find an undescribed Chaceon from the Mediter- ranean. Even more surprising is that this species was collected together with the new genus and species described below. The only eastern and central Atlantic species with strong anterolateral spines on the carapace in adults are C. atopus, C. gor- donae, and C. inglei, and all of them have 68 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 14. Chaceon notialis, ovigerous female paratype, cb 110 mm, Argentina: a, Dorsal view; b, Carapace. VOLUME 102, NUMBER 1 distinctly compressed dactyli on the walk- ing legs. Name.—Derived from the type locality in the Mediterranean Sea. Distribution. —Known only from the western Mediterranean Sea, in 1990-2830 m. Chaceon notialis, new species Figs. 14-15 Geryon quinquedens.—Juanico, 1973:145, fig. on p. 147.—Scelzo & Valentini, 1974: 561, figs. 1-2 [part, not specimens from Brazil].—Boschi, 1976:66, 67; 1979: 140.—Boschi et al., 1981:247.—Barea & Defeo, 1985:189, fig. 1; 1986:38, fig. 1. [Not Geryon quinquedens Smith, 1879.] Previous records.—Uruguay and Argen- tina: 34°40’—-36°45’S, 250-800 m (Barea & Defeo 1985).—34°40’—39°04’S, 250-800 m (Barea & Defeo 1986).—33°56’'—36°25'S, 52°35'-54°51'W (Juanico 1973).—Uru- guay: 33°38’S, 50°38’W, 790 m; 34°48’S, 52°02'W, 400 m; 35°04'S, 52°06’W, 800 m; 35°04'S, 52°15'W, 600 m (Scelzo & Val- entini 1974).— Argentina: 36°24’S, 53°58'W, 120 m; 37°45’S, 54°55’'W, 300 m; and 38°55'S, 55°35'W, 170 m (Scelzo & Val- entini 1974).— Buenos Aires Province, 36° 41°S (Boschi, 1976, 1979).—35°40’S, 52°47'W, 260 m (Boschi et al. 1981). Material. — Argentina: 37°45'S, 54°55'W, 280-320 m, R/V Cruz del Sur, 17-18 May 1973: one ovigerous female, paratype (USNM 205702).—38°55’S, 55°35'W, 170 m, R/V Cruz del Sur, 16 Apr 1973: one male, holotype (USNM 205701). Diagnosis. — A large Chaceon, cl to about 120 mm, cb to 135 mm in adults, with low, blunt anterolateral spines on the carapace and with dorsoventrally depressed dactyli on the walking legs. Carapace 1.1-1.2 times broader than long. Median pair of frontal teeth sharp, projecting forward, separated by U-shaped sinus, extending farther for- ward than laterals. Anterolateral teeth low, 69 Fig. 15. Chaceon notialis, male holotype, cb 104 mm, Argentina: a, Ventral view of orbit; b, P5 dactylus, posterior view; c, PS dactylus, dorsal view. blunt, fourth tooth very small, almost ob- solete. Distance from first to second an- terolateral tooth less than distance from third to fourth, distance from first to third an- terolateral tooth less than distance from third to fifth. Carapace surface strongly granular posterolaterally. Suborbital tooth low, blunt, falling short of level of lateral frontal tooth, suborbital margin evenly curved. Cheliped with blunt tooth subdistally and with distal angled lobe on merus; carpus roughened dorsally, lacking distal outer spine, anterior margin denticulate; propodus lacking distal spine or angled projection. Meri of walking legs with at most a distal dorsal tubercle, lacking a distinct distal dorsal spine. Dactyli of walking legs depressed, width at mid- length much greater than height. PS: merus less than 5 times longer than high, length 0.60 cb; carpus with line of low but sharp spinules dorsally; propodus length less than 4 times height, slightly longer than dactylus. 70 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Size. — Male, cl 94 mm, cb 104 mm; ovig- erous female, cl 99 mm, cb 110 mm. Jua- nico (1973) reported a male with cl 61 mm, cb 73 mm; Boschi et al. (1981) studied a male cl 30 mm. Scelzo & Valentini (1974) studied 18 specimens, measuring as follows: males, cl 88-116 mm, cb 97-124 mm; fe- males, cl 72-99 mm, cb 82-110 mm. Barea & Defeo (1985) reported catching males with cb 32-135 mm, females with cb 48-124 mm. Color.—Scelzo & Valentini (1974) re- ported that this species is reddish in color. Remarks.—Chaceon notialis resembles both C. quinquedens, from the northeastern Atlantic, and C. maritae, from West Africa, in having depressed dactyli on the walking legs, but it differs from both in numerous features. It is a much shorter-legged species than C. guinquedens: the merus of the fifth leg is about three-fifths the width of the car- apace as opposed to three-fourths the car- apace width in C. quinquedens, and the propodus of the fifth leg is less than 4 times as long as high instead of 5—7 times as long as high. In C. quinquedens there is a sharp outer spine on the carpus and a distal dorsal spine on the propodus of the cheliped, and each walking leg has a distinct distal dorsal spine. These spines are not present on the cheliped of G. notialis, and in this latter species the meri of the walking legs are armed with at most a distal dorsal tubercle. The surface of the carapace also is much coarser in C. notialis, especially posterolaterally. Chaceon notialis differs from C. maritae as follows: the frontal teeth are sharper and are not as close together; the anterolateral teeth of the carapace all are sharper, and the fourth tooth is much more distinct; the sub- orbital teeth are sharper and longer; and the walking legs are slightly longer. The merus of the fifth leg is about 5 rather than 4 times as long as high, and is about three-fifths rather than two-thirds of the carapace width. Barea & Defeo (1985, 1986) provided de- tails of the occurrence and biology of this species on joint fishing grounds off Uruguay and Argentina. Boschi (1976, 1979) char- acterized it as a cold-temperate species of the Buenos Aires Province (36—41° South latitude). The specimen from off Brazil identified with Geryon quinquedens by Rathbun (1937: 270) and material from Brazil identified by Scelzo & Valentini (1974:560) with the same species is referable to a new species, the de- scription of which is in preparation. Scelzo & Valentini reported that their Brazilian specimens were cream-colored, whereas their material from Uruguay and Argentina was reddish. Further, the length/height ratio of the propodus of the walking legs of their specimens from Brazil was 4.3—4.5, longer than that of C. notialis. The range in the length/height ratio observed by Scelzo & Valentini for their specimens from Uruguay and Argentina, with one exception, is as we found in our material of C. notialis. Our specimens were taken in depths of 170 and 280-320 m. Boschi et al. (1981) recorded a specimen from 260 m. Scelzo & Valentini (1974) reported specimens from depths of 120, 170, 300, 400, 600, 790, and 800 m, and Barea & Defeo (1985, 1986) reported this species from fishing grounds in depths between 250 and 800 m. Name.—The specific name is from the Latin, notialis, southern. Distribution. —Known from the coasts of Uruguay and Argentina, from about 33°S to about 41°S, in depths between 120 and 800 m. Chaceon sanctaehelenae, new species Figs. 16-17 Material. —Sandy Bay, St. Helena Island [15°58’S, 5°43’W], trap, 8 Oct 1968, leg F. N. Martin: one male (holotype, USNM 125510). Diagnosis. — A large Chaceon, cl 113 mm, cb 134 mm in adult, with low, blunt an- terolateral teeth on the carapace in adults and with laterally compressed dactyli on the walking legs. Carapace about 1.2 times broader than long. Median pair of frontal VOLUME 102, NUMBER 1 be Fig. 16. Chaceon sanctaehelenae, male holotype, cb 134 mm, Saint Helena: a, Dorsal view; b, Carapace. teeth broad, obtuse, separated by shallow U-shaped emargination, medians extending farther forward than laterals. Second and fourth anterolateral teeth obsolete, present as low lobes in adults. Distance from first to second anterolateral tooth subequal to distance from third to fourth tooth, distance from first to third tooth subequal to distance h2 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON yo jn ¢ b Fig. 17. Chaceon sanctaehelenae, male holotype, cb 134 mm, Saint Helena: a, Ventral view of orbit; 5, P5 dactylus, posterior view; c, P5 dactylus, dorsal view. from third to fifth. Carapace surface finely granular, hepatic regions largely smooth. Suborbital tooth short, blunt, scarcely vis- ible in dorsal view, falling short of level of lateral frontal tooth, suborbital margin evenly rounded. Cheliped with blunt tooth subdistally on merus; carpus roughened dorsally, lacking outer spine, anterior mar- gin smooth; propodus lacking distal angled projection. Meri of walking legs lacking dis- tal, dorsal spine. Dactyli of walking legs compressed, height at midlength greater than width. P5: merus 4.5 times longer than high, length 0.6 cb; propodus slightly longer than dactylus, length 3.3 times height. Size. —Male, cl 113 mm, cb 134 mm. Remarks. — This new species differs from both C. affinis and C. atopus in having much lower and blunter frontal and anterolateral teeth on the carapace; in C. affinis the sec- ond and fourth teeth are well-developed in large specimens, but in C. sanctaehelenae the second and fourth teeth are almost com- pletely obsolete. In addition, in C. sanctae- helenae the orbit appears to be shallower, the suborbital tooth is shorter and more ob- tuse, and the carpus of the walking legs is much smoother dorsally than in C. affinis. This new species further differs from C. ato- pus in having much shorter walking legs (P5 merus 4.5 times rather than 6.5 times longer than high), and in having the distance from the first to third anterolateral teeth on the carapace subequal to the distance from the third to the fifth tooth; in C. atopus the dis- tance from the first to third tooth is shorter. Chaceon sanctaehelenae differs from C. fenneri in some of these same features. All marginal teeth of the carapace are lower than in C. fenneri; in that species the frontal teeth are much sharper and more prominent, and the first, third, and fifth anterolateral teeth are much more prominent. The carapace is smoother than in C. fenneri, with lower and fewer granules, and the dorsal ridge on the carpus of the walking legs is much smooth- cle Chaceon chuni, from the southeastern At- lantic, differs in having a larger suborbital spine and in having a distinct distal dorsal spine on the merus of each walking leg. Name.—The specific name is derived from the type locality. Distribution. —Known only from the type locality. Zariquieyon, new genus Type species. — Zariquieyon inflatus, new species. Name. —The name is dedicated to the late Spanish carcinologist, Ricardo Zariquiey Alvarez, whose studies of Mediterranean decapods added so much to our knowledge of the group. As in Chaceon, the ending -on is added to make the name similar to Geryon. The gender is masculine. Definition. —Geryonid crabs with five an- terolateral spines on each side of the cara- VOLUME 102, NUMBER 1 pace. Carapace length about seven-tenths width. Branchial regions markedly inflated. Frontal teeth well-developed, large. Orbits deep, rectangular. Included species. —One, Zariquieyon in- flatus, n. sp. Remarks. —Zariquieyon shares with Chaceon and Geryon the portunid-like che- lipeds, with the subdistal dorsal spine on the merus, the strong inner spine on the carpus, the portunid-like chela, the single inner suborbital tooth, the slender walking legs with their naked dactyli, and the seven- segmented abdomen in both sexes. Zari- quieyon differs from those genera in having a comparatively broader carapace, with the posterolateral margins convex, strongly in- flated branchial regions, and rectangular rather than rounded orbits. It also shows far more pebbling dorsally, visible only under magnification, than any species of Chaceon or Geryon. Zariquieyon inflatus, new species Figs. 18-19 Material. —Mediterranean Sea, 37°56.7°N, 07°31.6’E, 2830 m, POLYMED sta CV 04, 18 May 1970: one male, two females (MNHN;; one female USNM 205985). The holotype is the female, cl 22 mm, cb 35 mm, in the collection of the Muséum National d’Histoire Naturelle, Paris; the other specimens are paratypes. Diagnosis.— A very small geryonid, cl 19— 22 mm, cb 27-35 mm, with strongly de- veloped anterolateral teeth on the carapace in adults and with laterally compressed dac- tyli on the walking legs. Body, except ab- domen, covered with fine granules, coarser and larger on posterior branchial regions. Regions of carapace well-marked, proto- gastric region, area adjacent to fifth antero- lateral spine, and branchial regions very in- flated. Intestinal region with two prominences. Posterolateral margins strongly convex. Carapace 1.4—1.6 (mean 1.5) times broader than long. Median pair 73 Fig. 18. Zariquieyon inflatus, female holotype, cb 35 mm, Mediterranean, dorsal view. of frontal teeth slender, separated by V-shaped emargination. Second and fourth anterolateral teeth reduced, fourth smallest; other teeth progressively increasing in size posteriorly, fifth much the largest. Distance from first to second tooth short, about the same as from third to fourth tooth, distance from first to third tooth much less than dis- tance from third to fifth. Orbits rectangular. Suborbital tooth strong, extending to level of outer frontal tooth, suborbital margin denticulate. Cheliped finely granular dor- sally; merus with sharp subdistal spine, dis- tal angled projection spinulose; carpus peb- bled dorsally, with long, sharp inner spine and distinct outer spine or crest of spinules; propodus pebbled dorsally, with distal dor- sal projection. Meri of walking legs with dis- tinct distal dorsal spine. Dactyli of walking legs laterally compressed, height near mid- length greater than width. P5: merus 6.3- 6.6 times longer than high, pebbled dorsal- ly, with distal dorsal spine, length 0.45 times cb; carpus with line of spinules dorsally; 74 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 19. Zariquieyon inflatus, female holotype, cb 35 mm, Mediterranean: a, Dorsal view; b, Ventral view of orbit; c, Third maxilliped; d, Carpus of cheliped; e, P5; f PS dactylus, dorsal view. propodus length about 5 times height, much longer than dactylus. Size.— Male, cl 19 mm, cb 28 mm; fe- males, cl 20—22 mm, cb 27-35 mm. Color. —Not recorded. Remarks.—This species was taken to- gether with Chaceon mediterraneus at a depth of 2830 m in the western Mediter- ranean basin. We know of no deeper record for a brachyuran crab from the Mediterra- nean. Name.—The specific name is from the Latin, inflatus, swollen. Distribution. —Known only from the type locality, in 2830 m. Remarks The genus Chaceon has proven to be much more speciose than even we imagined when we began studying its members, and much additional work remains to be done on the genus. The geographic ranges of most species remain to be determined; in general, ranges of each species are restricted latitudinally, although some species, like C. bicolor, have relatively wide ranges. Chaceon paulensis from the southern Indian Ocean should be redescribed, and the status of the species reported from off Travancore, India, in 224— 284 fm (410-520 m) by Alcock (1899:85) needs to be determined. A particularly in- teresting problem that remains to be solved is whether the types of Chaceon quinque- dens, one of which is an ovigerous female only 22 mm long (Smith, 1879:36), are con- specific with the large, commercially im- portant species now identified as C. quin- quedens. For most species there is no information available on growth changes, especially as it pertains to proportions of the walking legs VOLUME 102, NUMBER 1 13 Table 1.—Characteristics of known species of Chaceon. Abbreviations are as follows: ? (not known); Color: B (bicolor, tan and purple), R (red), T (tan), W (whitish); Size (maximum cb in mm); PS dactylus: C (laterally compressed), D (dorsoventrally depressed); Distal spine on P5 merus: + (large, well developed), — (small, reduced or absent); Anterolateral teeth of carapace: + (large, well-developed in adults), — (small, reduced or absent). Color Northwestern Atlantic C. eldorado R C. fenneri ih C. inghami R C. quinquedens R Southwestern Atlantic C. notialis R n. sp. Brazil T Northeastern Atlantic C. affinis Gi C. inglei R C. mediterraneus 2 Central South Atlantic C. atopus ? C. sanctaehelenae 2 Southeastern Atlantic C. chuni T C. erytheiae Rp C. gordonae v C. maritae Ae Western Indian Ocean C. crosnieri ? C. macphersoni ? C. paulensis R Western and Central Pacific C. bicolor B C. granulatus ac Eastern Pacific n. sp. Chile W and spination of the carapace and walking legs. In the case of C. bicolor, for example, we have identified a small, spiny, long-legged specimen from deep water with the much larger adult found in the same area, but the possibility remains that more than one species is involved. Certainly additional species remain to be recognized, and we believe that a key to the species now known would be premature and perhaps even confusing. As the species of Dactylus Merus Carapace Size P5 PS spines 109 D = a 190 € = = 110 C <5 =F 178 D 35 = 135 D = = 158 D = a 210 GC = = 2 € + == 103 D a 55 (124 € =e + 134 € = = 114 ( se = 125 (G =F = 161 C =F =e 172 D = = 155 C == =F 126 D + -- 113 Cc ata 2s 180 C = = 146 D == = A/S) ‘S = 7 Chaceon may be difficult to distinguish in the absence of comparative material, we provide here, by broad geographic region, a summary of the species found in each region and their major characteristics (Table 1). Acknowledgments Many people contributed to this study. We thank all of those who provided us with material or access to their collections: E. E. Boschi, Instituto Nacional de Investigacion 76 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON y Desarollo Pesquero, Mar del Plata, Ar- gentina; Diane E. Brown, Australian Mu- seum, Sydney; Alain Crosnier and D. Gui- not, Muséum National d’Histoire Naturelle, Paris; Reginald M. Gooding, then of the NOAA/NMEFS Southwest Fisheries Center, Honolulu Laboratory; R. W. Ingle, British Museum (Natural History), London; En- rique Macpherson, Instituto de Ciencias del Mar, Barcelona; Torben Wolff, Zoological Museum, Copenhagen; and Nicolino Dra- go, Universita di Genova, Italy, who al- lowed us to add reference to his material from the Mediterranean in galley. Our studies on geryonid crabs have been supported in part by the Food and Agri- culture Organization of the United Nations (FAO); that support is gratefully acknowl- edged. This paper also was supported in part by the Smithsonian Institution, through its Research Opportunities Fund. We thank Roy K. Kropp for taking the photographs used in Figs. 14 and 16. Fig. 1 was taken by the staff photographer of the Riksmuseum van Natuurlijke Historie, Leiden, and Figs. 3 and 5 were taken by the staff photographer of the Muséum National d’ Histoire Naturelle, Paris. Lilly King Man- ning drew the line drawings and prepared all of the figures for publication. We thank Fenner A. Chace, Jr., Enrique Macpherson, and Marilyn Schotte for read- ing a draft of the manuscript. Literature Cited Alcock, A. 1899. An account of the deep-sea Brachy- ura collected by the Royal Indian Marine Survey Ship Investigator, pp. 1-85, 1-2, pls. 1-4. Cal- cutta: Indian Museum. Barea, L., & O. Defeo. 1985. Primeros ensayos de captura del crustaceo batial Geryon quinquedens Smith en el area comun de pesca Argentino- Uruguaya.—Contribucion, Departamento de Oceanografia (F.H.C.), Montevideo 2(3):189- 203: ——,, & . 1986. Aspectos de la pesqueria del cangrejo rojo (Geryon quinquedens) en la zona comun de pesca Argentino-Uruguaya.— Publi- caciones de la Comision Técnica Mixta del Frente Maritimo 1(1):38—46. Boschi, E. E. 1976. Nuevos aportes al conocimiento de la distribucion geografica de los crustaceos decapodos del Mar Argentino.—Physis (A)35(90):59-68. 1979. Geographic distribution of Argenti- nian marine decapod crustaceans. — Bulletin of the Biological Society of Washington 3:134—143. , M. I. Iorio, & K. Fischbach. 1981. Distri- bucion e abundancia de los crustaceos decapo- dos capturados en las campanas de los B/I “Wal- ther Herwig” y “Shinkai Maru” en el Mar Argentino, 1978-1979. In Campanas de inves- tigacion pesquera realizadas en el Mar Argen- tino por los B/I “Shinkai Maru” y “Walther Herwig” y el B/P “Marburg,” Anos 1978 y 1979.—Contribuciones del Instituto Nacional de Investigacion y Desarrollo Pesquero 383:233- 253. Chun, C. 1903. Aus den Tiefen der Weltmeeres, 2nd edition. Gustav Fischer, 592 pp. Colosi,G. 1923. Una specie fossile de Gerionide (De- capodi brachiuri).— Bolettino della Societa dei Naturalisti in Napoli, 35 (series 2, volume 15), 37:248-255. Della Croce, N., N. Drago, & G. Flocchini. 1988. Ricerche biologiche e geofisiche. Campagna oceanografica N/R “Minerva” (14-31.8.1987).— Istituto di Scienze Ambientali Marine, Univ- ersita di Genova, Rapporto Tecnico 24:1-10. Gerstaecker, A. 1856. Carcinologische Beitrage.— Archiv fur Naturgeschichte 22(1):101-—162, pls. 4-6. Grifin, D. J. G., & D. E. Brown. 1976. Deepwater decapod Crustacea from eastern Australia: Brachyuran crabs.—Records of the Australian Museum 30(11):248-271. Guinot, D. 1969. Les Goneplacidae (suite et fin). Re- cherches préliminaires sur les groupements na- turels chez les Crustacés Décapodes Brachy- oures, VII.—Bulletin du Muséum National d’Histoire Naturelle (2)41(3):688—724. pls. 3-5. . 1971. Synthése et bibliographie. Recherches préliminaires sur les groupements naturels chez les Crustacés Décapodes Brachyoures, VIII.— Bulletin du Muséum National d’Histoire Na- turelle (2)42(5):1063—-1090. —, & B. Richer de Forges. 1981. Crabes de pro- fondeur, nouveaux ou rares, de l’Indo-Pacifique (Crustacea, Decapoda, Brachyura) (Deuxiéme partie).— Bulletin du Muséum National d’His- toire Naturelle, Paris (4)3(A1):227—260, pls. 3-7. Hansen, H. J. 1908. Crustacea Malacostraca, I.—The Danish Ingolf-Expedition 3(2):1—120, pls. 1-5. Herbst, J. F. W. 1799-1804. Versuch einer Natur- geschichte des Krabben und Krebse, nebst einer systematischen Beschreibung ihrer verschiede- nen Arten, 3:215 pp. Berlin and Stralsund. Ingle, R. W. 1985. Geryon gordonae sp. nov. (Decap- VOLUME 102, NUMBER 1 oda Brachyura, Geryonidae) from the north- eastern Atlantic Ocean. —Crustaceana 48(1):88- 98. Intés, A. 1978. Péche profonde aux casiers en Nou- velle Calédonie et iles adjacentes. Essais préli- minaires. ORSTOM, Centre de Nouméa, Rap- ports Scientifiques et Techniques 2:1-10, figs. 1-10. Juanico, M. 1973. Hallazgo de Geryon quinquedens Smith, 1879 (Crustacea Decapoda), en aguas Uruguayas.— Revista de Biologia del Uruguay 1(2):145-149. King, M.G. 1984. The species and depth distribution of deepwater caridean shrimps (Decapoda, Ca- ridea) near some southwest Pacific islands.— Crustaceana 47(2):174-191. Kroyer, H. 1837. Geryon tridens, en ny Krabbe.— Naturhistorisk Tidsskrift 1:10—21, pl. 1. Macpherson, E. 1983. Crustaceos decapodos captu- rados en las costas de Namibia. — Resultados Ex- pediciones Cientificas (supplement to Investi- gacion Pesquera, Barcelona) 11:3-80. 1984. Crustaceos decapodos del Banco Val- divia (Atlantico sudoriental).— Resultados Ex- pediciones Cientificas (supplement to Investi- gacion Pesquera, Barcelona) 12:39-10S. Manning, R. B., & L. B. Holthuis. 1981. West African brachyuran crabs.—Smithsonian Contributions to Zoology 306:379 pp. ——,,& . 1984. Geryon fenneri, a new deep- water crab from Florida (Crustacea: Decapoda: Geryonidae).—Proceedings of the Biological Society of Washington 97(3):666-673. ——, & 1986. Notes on Geryon from Ber- muda, with the description of Geryon inghami, new species (Crustacea: Decapoda: Geryoni- dae).— Proceedings of the Biological Society of Washington 99(2):366-373. , & 1987. The status of Geryon tri- spinosus (Herbst) (Geryonidae). — Investigacion Pesquera, Barcelona 51 (supplement 1):57-62. ,& . 1988. South African species of the genus Geryon (Crustacea, Decapoda, Geryoni- ve | dae).—Annals of the South African Museum 98(3):77-92. Milne Edwards, A. 1882. Rapport sur les travaux de la Commission chargée par M. le Ministre de l’Instruction Publique d’étudier la faune sous- marine dans les grandes profondeurs de la Médi- terranée et de l’Océan Atlantique. — Archives des Missions Scientifiques et Litteraires, Paris (3)9: 1-59. —., & E.-L. Bouvier. 1894. Brachyoures et ano- moures. Crustacés décapodes provenant des campagnes du yacht I’Hirondelle (1886, 1887, 1888). Premiére partie.—Résultats des cam- pagnes scientifiques accomplies sur son yacht par Albert Is", Prince Souverain de Monaco 7: 1-112. Rathbun, M. J. 1937. The oxystomatous and allied crabs of America. — United States National Mu- seum Bulletin 166, vi + 278 pp. Sakai, T. 1978. Decapod Crustacea from the Emperor Seamount Chain.—Researches on Crustacea 8 (supplement): 1-39, pls. 1-4. Scelzo, M. A., & A. Valentini. 1974. Presencia de - Geryon quinquedens Smith en aguas del Oceano Atlantico sudoccidental (Decapoda, Brachyura, Geryonidae).—Physis, Buenos Aires (A)33(87): 557-567. Smith, S. I. 1879. The stalk-eyed crustaceans of the Atlantic coast of North America north of Cape Cod.—Transactions of the Connecticut Acade- my of Arts and Sciences 5(1):27-136. Takeda, M. 1983. Crustaceans. Pp. 19-185 in Crus- taceans and mollusks trawled off Suriname and French Guiana. Japan Marine Fishery Research Center, Tokyo. (RBM) Department of Invertebrate Zo- ology, National Museum of Natural His- tory, Smithsonian Institution, Washington, DC 20560; (LBH) Rijksmuseum van Na- tuurlijke Historie, Postbus 9517, 2300 RA Leiden, The Netherlands. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 78-83 SYNALPHEUS AROSTRIS AND PHILOCHERAS LAPILLUS, TWO NEW SPECIES OF CARIDEAN SHRIMP (CRUSTACEA) FROM THE TROPICAL EASTERN PACIFIC Mary K. Wicksten Abstract.—Two new species of shrimp (Decapoda: Caridea) are described from the eastern Pacific. Synalpheus arostris is described from specimens from western Colombia. Philocheras lapillus is the first species of its genus to be reported in the area. During examination of specimens from western Colombia and the Galapagos Is- lands, I discovered two undescribed species of shrimp. The new species of Philocheras is the first report of the genus from the trop- ical eastern Pacific. I thank Gabriel Ramos, Universidad del Valle (UV); Raymond Manning, United States Museum of Natural History (USNM); and Janet Haig, Allan Hancock Foundation, University of South- ern California (AHF) for their interest and assistance during this study. The figures are by Gabriel Ramos and Joseph Goy, Texas A&M University. This project was aided by a Visiting Fellowship of the Smithsonian Institution. Family Alpheidae Synalpheus arostris, new species Fig. 1 Type material. —Holotype: female, total length 10.5 mm. Morro de Los Agujeros, Bahia de Malaga, Colombia (3°55’N, 77°20'W), rocky intertidal zone, 28 Nov 1981, collector not reported, AHF no. 8111. Paratype: female, same site and date, UV. Description. — Rostrum lacking, a slight raised area present between orbital teeth. Orbital teeth reaching less than 0.5 x length of first segment of antennular peduncle, longer than broad. Visible part of first antennular segment 1.3 x as long as second antennular article, third article shorter. Stylocerite reaching just beyond first antennular segment. Scapho- cerite with lateral tooth reaching beyond end of antennular peduncle and exceeding car- pocerite. Squamous part of scaphocerite reaching or almost reaching end of anten- nular peduncle. Inferior tooth of basicerite reaching as far forward as stylocerite, su- perior tooth well developed and acute. Large chela 3 x as long as wide, with fin- gers occupying about 0.3 entire length. Superior margin of palm bearing blunt knob proximal to dactylus. Merus 2x long as broad, superior margin blunt. Small chela 2.4 x long as wide, with fin- gers occupying about 0.4 entire length. Merus almost 3x long as wide, bearing 3 teeth on superior margin. Carpal articles of second leg with ratio 10: 3:3:3:4. Merus of third leg 4 x long as broad, with- out spines. Carpus without teeth or spines. Propodus 7 X long as wide, straight, bearing 7-8 spines on inferior margin and a pair of terminal spines. Dactyl biunguiculate, 0.3 x propodus, relatively straight; superior and inferior ungui slender and almost equal in size and shape. Fourth and fifth legs similar to third. Telson only slightly longer than width of anterior margin, tapering to posterior mar- gin. Two to three dorsolateral spines per VOLUME 102, NUMBER 1 79 Pig: 1: cheliped; E, Large cheliped; F, Third pereopod. side, pair long spines at distolateral margin, distolateral margin produced into small tooth. Posterior margin of telson rounded. Discussion. —Coutiére (1909) established six groups in the genus Synalpheus, based on features of the rostrum, orbital teeth, se- tae of the smaller chela, ungui of the dactyls, and other features. Banner & Banner (1975) reexamined these groups and found that perhaps only two of them were of taxonom- ic validity—the others contained such a range of variation or overlapped other groups to such an extent that the group cer- tainly was artificial. The new species illus- trates the difficulties in finding relationships among the species of Synalpheus; lacking a Synalpheus arostris, A, Holotype in lateral view; B, Anterior end in dorsal view; C, Telson; D, Small rostrum, it cannot easily be compared with many other species. The short orbital teeth and equal, slender ungui of the dactyls of S. arostris are found in species of Coutiére’s ““Brevicarpus” group, known only from American waters. Three species, S. minus (Say), S. obtusifrons Chace, and S. brevicarpus Coutiére are found in the Caribbean region. All of these species have short rostra. Synalpheus minus has a sty- locerite that greatly exceeds the first article of the antennular peduncle, but the spine of the scaphocerite does not reach the end of the carpocerite. Synalpheus obtusifrons has a rounded stylocerite and a short scapho- cerite that does not reach the end of the 80 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Philocheras lapillus, paratype: A, Entire animal in lateral view; B, Carapace in dorsal view; C, Carapace in lateral view; D, Telson and uropods. antennular peduncle. The eastern Pacific species, S. digueti Coutiére, is common in rocky intertidal areas. Aside from lacking a rostrum, S. arostris can be distinguished from S. digueti by having a shorter stylo- cerite, reaching barely beyond the end of the first article of the antennular peduncle rather than to the middle of the second ar- ticle; and having a longer spine on the scaphocerite, reaching proportionally far- ther beyond the blade than in S. digueti. Only S. arostris has three teeth on the su- perior margin of the merus of the small che- liped. Synalpheus arostris can be distinguished easily from S. /ockingtoni Coutiére by the lack of the rostrum (seen in both specimens of the new species). Should one encounter a specimen of S. lockingtoni missing a ros- trum, the species can be distinguished by the sharp spine at the anterior margin of the palm of the major chela, above the articu- lation of the dactyl, in S. arostris. In S. lock- ingtoni, the anterior margin of the major chela ends in a knob or tubercle. The pos- terior margins of the telson of S. arostris are sharply triangular, those of S. lockingtoni are weakly pointed. Adult S. /ockingtoni can be larger than the specimens of S. arostris: Schmitt (1921) gives a length of 30 mm for a large female S. lockingtoni. Family Crangonidae Philocheras lapillus, new species Figs. 2-4 Type material. —Holotype male, total length 13.7 mm. Off Gardner Bay, Hood Island (Isla Espanola), Galapagos (Archi- pelago de Colon) 1°22’S, 90°40’W), 46-65 m, rock, 31 Jan 1934, Velero III sta. 201- 34, USNM 234435. VOLUME 102, NUMBER 1 81 Fig. 3. Philocheras lapillus: A, Antennule; B, Scaphocerite; C, Mandible; D, First maxilla; E, Second maxilla; F, First maxilliped: G, Second maxilliped; H, Third maxilliped. Paratypes.—Tagus Cove, Albemarle Is- land (Isla Isabela) (0°17'S, 91°23'’W), 37 m, rock and nullipores, 11 Jan 1934, Velero III sta. 149-34, one specimen. Stephens Bay, Chatham Island (Isla San Cristobal), (0°48’S, 89°31'W), 59 m, fine sand and coralline al- gae, Velero III sta. 170-34, 21 Jan 1934, three specimens. Off Cartago Bay, Albe- marle Island (0°35’S, 90°54’W), 59 m, mud, 25 Jan 1934, Velero IIT sta. 185-34, five specimens. Off Cartago Bay, Albemarle Is- land (0°34’S, 90°53’W), 59 m, sand and nul- lipores, 25 Jan 1934, Velero IIT sta. 186-34, two specimens. Off Gardner Bay, Hood Is- land (same station as holotype), Velero III sta. 201-34 (four specimens USNM, two specimens AHF). All specimens USNM ex- cept as noted. Description. —Rostrum exceeding or nearly exceeding end of cornea, distal end wide. Anterior margin of carapace with teeth, one suborbital tooth, pair near base of second antenna and two pterygostomial teeth. One large tooth on dorsal midline. Abdominal pleura rounded. Sixth ab- dominal segment about 1.5 x length of fifth, slightly shorter than length of telson. Telson narrow, with two pair dorsolateral, three pair terminal spines and sharp posteromesial tip. Basal article of antennular peduncle not reaching as far as end of cornea. Stylocerite not as long as basal article of antennular peduncle, broad and quadrangular. Last two articles of antennular peduncle short. Scaphocerite longer than antennular pe- duncle, outer margin straight, blade longer than spine. Basicerite short. Third maxilliped exceeding scaphocerite. Ultimate segment longer than penultimate, 0.6X antepenultimate. Exopod present. Other mouthparts as figured. First pereopod stout, subchelate. Dactyl about 0.3 X propodus length, subchelar spine narrow and simple. Carpus 0.25 propo- dus, with one or no spines. Merus shorter than chela, with two teeth on distal end near articulation with carpus and one large tooth on lower margin. Ischium and basis short, without teeth. No exopods or epipods on pereopods. Second pereopod short, chelate. Dactyl 0.5 X propodus, carpus about equal to chela, 82 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON (Tk Ati ‘) Fig. 4. Philocheras lapillus: A, First pereopod; B, Second pereopod; C, Third pereopod; D, Fourth pereopod; E, Fifth pereopod; F, Second pleopod of female. 0.5 merus. Merus longer than ischium. Third pereopod slender, thread-like. Dactyl thin, 0.7 X propodus. Propodus 0.6 car- pus, carpus 1.8x merus, merus 0.6% is- chium. Fourth and fifth pereopods similar. Dactyl long and simple, 0.8 propodus. Carpus 0.8 X propodus, merus 1.2 X carpus, ischium 0.8 X merus. Second pleopod with appendix interna, male with appendix masculina. Uropods long, outer uropod shorter than inner. Outer uropod with small posterolateral tooth. Color in life. —Carapace almost all white, body Van Dyke brown, speckled. (Field note for specimen at sta. 149-34, by Waldo L. Schmitt.) Discussion. —1 follow the revision of Chace (1984) in considering Philocheras to be distinct from Pontophilus. Philocheras lapillus most closely resembles P. gorei (Dardeau, 1980) from the Gulf of Mexico and Georgia. In P. gorei, however, there are always teeth on the distal margins of the carpus of the first pereopod. The outer fla- gellum of the antennular peduncle of P. /a- pillus is much thicker than that of P. gorei. The tip of the rostrum of P. /apillus is round- ed, not spatulate. Pontophilus lapillus also may be larger than P. gorei: the carapace length of the holotype is 3.3 mm, that of the type of P. gorei is 2.5 mm. The habitat and living color of P. /apillus suggest that the animal’s mode of life is sim- ilar to that of species of Crangon and Lis- socrangon along the coast of California. These species have a speckled, cryptic color pattern, which provides camouflage when the shrimp dig into sand (Kuris & Carlton 1977; Ricketts et al. 1985). The species epithet means “‘pebble,”’ which the resting animal resembles. The name is a noun in apposition. VOLUME 102, NUMBER 1 Literature Cited Banner, D. M., & A. H. Banner. 1975. The alpheid shrimp of Australia. Part 2: the genus Synal- pheus.—Records of the Australian Museum 29(12):267-389. Chace, F. A., Jr. 1984. The caridean shrimps (Crus- tacea: Decapoda) of the A/batross Philippine Ex- pedition, 1907-1910, Part 2: Families Glypho- crangonidae and Crangonidae.— Smithsonian Contributions to Zoology No. 397:1-63. Coutiére, H. 1909. The American species of snapping shrimps of the genus Synalpheus. — Proceedings of the United States National Museum 36(1659): 1-93. Dardeau, M. 1980. A new species of Pontophilus (Crustacea: Natantia: Crangonidae) from the Gulf of Mexico and the western Atlantic. — Pro- 83 ceedings of the Biological Society of Washington 93(3):563-572. Kunis, A. M., & J. T. Carlton. 1977. Description of a new species, Crangon handi, and new genus, Lissocrangon, of crangonid shrimps (Crustacea: Caridea) from the California coast, with notes on adaptation in body shape and coloration. — Biological Bulletin 153:540-559. Ricketts, E. F., J. Calvin, J. W. Hedgpeth, & D. W. Phillips. 1985. Between Pacific tides, 5th ed. Stanford University Press, Stanford, Califor- nia, 652 pp. Schmitt, W. L. 1921. Marine decapod Crustacea of California.— University of California Publica- tions in Zoology 23:1—470. Department of Biology, Texas A&M Uni- versity, College Station, Texas 77843. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 84-88 THE HOLOTYPE OF HETEROCARPUS ALEXANDRI A. MILNE-EDWARDS (CRUSTACEA: DECAPODA: PANDALIDAE) Fenner A. Chace, Jr. Abstract.—The ovigerous female holotype of Heterocarpus alexandri from off Havana, Cuba, is described and reillustrated. A male of presumably the same species is recorded from the Bahamas, and probably two related species are recorded and diagnosed from the Pacific region: H. nesisi Burukovsky from Baja California and an undescribed species previously recorded as H. alexandri from Hawaii. The systematic status of H. alexandri is discussed but not con- summated. This paper was prompted by the discov- ery in the collection of the Museum of Com- parative Zoology, Harvard University, of the holotype of Heterocarpus alexandri, which had been rather inadequately de- scribed and was feared lost. This opportu- nity was made especially significant by the revelation that A. Milne-Edwards’ (1883) original illustration (there was no written description) was erroneous in several im- portant characters, thereby precluding as- surance of the identification of the species from other material. Although I have of- fered comparisons of H. alexandri with specimens of related species from the Pacific and have discussed the possible systematic status of those species, my objective in this contribution has been to record the typical features of H. alexandri for future reference, not to define its hierarchical position in the family. Family Pandalidae Genus Heterocarpus A. Milne-Edwards Heterocarpus alexandri A. Milne-Edwards, 1883 Fig. 1 Heterocarpus Alexandri A. Milne-Edwards, 1883 [unnumbered plate] [type locality: Blake dredging no. 2; north of Havana; 23°14’00’N, 82°25'00”W; 805 fms (1472 m)].—De Man, 1920:108, 153, 154. Heterocarpus alexandri. —Faxon, 1896: 161.—Chace, 1985:19, 20, fig. 135. —Bu- rukovsky, 1986:64, 67, 69. Description of holotype.—Ovigerous fe- male with postorbital carapace length of 12.8 mm. Rostrum (Fig. 1a) incomplete, existent portion nearly three-fourths as long as post- orbital carapace, overreaching antennal scale, with sharp lateral carina arising from orbital margin, armed dorsally with eight strong teeth, four on carapace posterior to orbital margin, posteriormost arising slight- ly anterior to midlength of carapace, bearing denticle on posterior slope, armed ventrally with four teeth. Carapace with middorsal carina extending over anterior two-thirds of length, posterior one-third smoothly round- ed; antennal spine flaring sinuously laterad from origin below orbit, slightly smaller than anteriorly directed branchiostegal spine, latter buttressed by submarginal carina ex- tending to near midlength of carapace; low, broad elevation, accentuated by rather deep dorsal and ventral depressions, extending posteriorly from orbital region and indis- tinctly joining somewhat more distinct su- prabranchial ridge reaching nearly to pos- terior margin of carapace. VOLUME 102, NUMBER 1 Pig. 1. aspect; b, Same, dorsal aspect; c, Abdomen, lateral aspect; d, third abdominal somite, dorsal aspect; e, Sixth abdominal somite, telson, and uropods, dorsal aspect; f Juncture of sixth abdominal somite and telson, lateral aspect; g, Right second pereopod. (Magnifications: a, c, x3; b, d, e, g, x6; ff x12.) Abdomen (Fig. lc) with tergum of first somite rather severely distorted, second so- mite with distinct, anteriorly convex, pos- teriorly setose transverse groove crossing tergum posterior to midlength, third somite with sharply defined middorsal boss on ter- gum (Fig. 1d); sixth somite fully one and three-fourths times as long as fifth somite, slightly more than twice as long as high, Heterocarpus alexandri, ovigerous female holotype: a, Carapace and anterior appendages, lateral dorsal surface shallowly convex and bluntly distinct from lateral surface (Fig. le), armed posteroventrally with small but discrete tooth (Fig. 1f); pleura of four anterior so- mites with irregularly convex margins, pleu- ron of fifth somite with sharp posteroventral tooth. Telson (Fig. le) deeply sulcate mid- dorsally on anterior half of length, armed with five pairs of dorsolateral spines, in- 86 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON cluding pair lateral to long, intermediate posterior spines. Eye with subspherical cornea slightly broader than stalk, without ocellus (Fig. 15). Antennule with stylocerite narrowly taper- ing to sharp point near level of second third of second antennular segment. Antennal scale with lateral margin nearly straight, ter- minating in strong distolateral tooth not reaching level of distal oblique margin of blade. Third maxilliped overreaching an- tennal scale by length of terminal segment, exopod reaching to about midlength of an- tepenultimate segment. Pereopods with epipods on four anterior pairs. First pereopods missing or incom- plete. Right second pereopod (Fig. 1g) over- reaching antennal scale by length of chela and about one-third of carpus, carpus com- posed of 18 articles; left second pereopod missing. All three pairs of posterior pereo- pods missing. Uropod (Fig. le) with branches subequal in length, slightly overreaching telson, not including posterior spines. Eggs measuring about 0.4 x 0.6 mm. Remarks.—The unique holotype differs from A. Milne-Edwards’ original illustra- tion in having the margin of the pleuron of the fourth abdominal somite rounded in- stead of posteroventrally acute, the telson armed with five rather than four pairs of dorsolateral spines, the blade of the anten- nal scale oblique rather than transversely truncate, and the carpus of the right second pereopod composed of 18 rather than 25 articles. The specimen assigned to H. alexandri by Faxon (1896:161) from Blake dredge no. 196; off Martinique; 1030 fms (1884 m) ap- parently has been temporarily misplaced in the MCZ collections, but there is a male of that species in the Smithsonian collections, taken by the Albatross at station 2629; mouth of Exuma Sound, Bahamas; 23°48'40"N, 75°10'40’W; 1169 fms (2138 m); 8 Mar 1886. That specimen has a post- orbital carapace length of 11.0 mm; the an- terior part of the rostrum is missing beyond the seventh dorsal and the posterior ventral teeth. It differs otherwise from the holotype in having the submarginal carina that but- tresses the branchiostegal spine less sharp; the tergum of the first abdominal somite traversed by a distinct, anteriorly convex groove similar to the one on the second so- mite; the margins of the dorsal boss on the third somite curving laterad more strongly at the anterior end; the sixth somite nearly twice as long as the fifth and about two and one-half times as long as high; the telson armed with five pairs of dorsolateral spines on the left side but only four on the right, including the pair lateral to the intermediate posterior spines; the stylocerite not over- reaching the acute lateral projection of the first antennular segment; the blade of the antennal scale slightly narrower beyond the base of the distolateral spine than in the holotype (but not quite as distinctly so as indicated in Chace (1985:fig. 135)); the first pereopod overreaching the antennal scale by about one-half the length of the chela; and the appendix interna on the second pleopod overreaching the appendix mas- culina by at least one-fourth of its length. In virtually all other characters, the male agrees with the ovigerous female holotype. The Hawaiian specimen recorded as H. alexandri by Rathbun (1906:918) from A/- batross station 4181; near Kauai Island; 81 1— 671 fms (1483-1227 m) is an ovigerous fe- male with a postorbital carapace length of 9.7 mm. It almost certainly represents a dis- tinct species. The rostrum reaches only about as far as the distal end of the antennular peduncle, does not reach the level of the distal end of the antennal scale, and has a rostral formula of 4+ 6/4; although the car- apace is very like that of H. alexandri, the transverse grooves on the first and second abdominal somites are much less distinct, that on the second being~ virtually non- existent, and there is no suggestion of a boss on the tergum of the third somite; the sixth somite is two and one-fourth times as long VOLUME 102, NUMBER 1 as the fifth and fully two and one-half times as long as high; the telson is deeply sulcate anteriorly, but the posterior one-half is missing. Another Smithsonian specimen, identi- fied by Waldo L. Schmitt as H. alexandri, from “D. 5682,” which almost certainly refers to an Albatross station by that num- ber in San Lucas Bay, Baja California; 22° 48'20’N, 109°52'40”W; 491 fms (898 m); 24 Mar 1911, is a large female with a post- orbital carapace length of 31.5 mm; the rostrum far overreaches the antennal scale and has a rostral formula of 4+7/7; the middorsal postrostral carina reaches poster- iorly to about the posterior one-sixth of the postorbital carapace length, and the lateral postorbital ridge is very like the one in the holotype of H. alexandri, but the branchio- stegal spine is situated closer to the antennal spine and is not supported by a long, cari- nate buttress; the two anterior abdominal somites lack transverse grooves; the third abdominal somite is produced posteriorly in the midline, but it is without a dorsal boss on the tergum, except for a vestige sug- gested by a short, mesially convex furrow on each side of the midline; the sixth ab- dominal somite is somewhat transversely convex dorsally, nearly two and one-fourth times as long as the fifth, and one and two- thirds times as long as high; the telson is rather deeply sulcate dorsally, especially an- teriorly, armed. with five pairs of dorsolat- eral spines, including the pair lateral to the intermediate posterior spines; the eyestalk widens distally to a nearly hemispherical cornea; the pereopods have well-developed epipods on the four anterior pairs; the first pair slightly overreaching the antennal scale; the right second pereopod reaches at least to the distal one-fourth of the antennal scale, the carpus is composed of five articles; the left second pereopod overreaches the an- tennal scale by the length of the chela and the distal carpal article, and the carpus com- posed of 15 articles; the third pereopod overreaching the antennal scale by the 87 lengths of the dactyl and propodus, the dac- tyl bearing four spines on the flexor margin proximal to the distal tooth; the uropod with the lateral branch reaching to the level of the posterior margin of the telson, not in- cluding the posterior spines. It seems probable that the specimen from the southern tip of Baja California may be identifiable as H. nesisi Burukovsky, 1986, previously known only from the male ho- lotype, with an apparent postorbital cara- pace length of about 27 mm, found about 1600 kms southwest of the A/batross station at 13°34'N, 120°33’W, on an apparent sea- mount in 800 m in an area where total depths are near 4300 m. Although the Hawaiian specimen agrees with the one from Baja Cal- ifornia and disagrees with H. alexandri in the indistinct or nonexistent grooves on the first and second abdominal tergites and the absence of a dorsal boss on the third tergite, it differs so clearly from H. nesisi in its much smaller size, shorter rostrum, and much longer sixth abdominal somite as to suggest that-it represents an undescribed species. There is little doubt that Crosnier (1986a: 368) had ample reason to remove H. /aevis A. Milne-Edwards, 1883, from the genus Heterocarpus and to transfer it and its Pa- cific analogue Plesionika chacei Crosnier, 1986 (renamed P. fenneri Crosnier, 1986b), to the genus Plesionika because of their sim- ilarity to P. bifurca Alcock & Anderson, 1894, and P. spinidorsalis (Rathbun, 1906). Similarly, the three species discussed above probably belong to the same genus as the four assigned to Plesionika by Crosnier (1986a), because they lack strong postor- bital or postantennal carinae and have the carapace transversely convex rather than carinate in the dorsal midline of the pos- terior one-fourth or more of its length. I am not proposing that change here, however, because these seven species seem to form a rather homogeneous group quite different from Plesionika uniproducta Bate, 1888 (=Acanthephyra ensis A. Milne-Edwards, 1881), the type species of Plesionika. The 88 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON family Pandalidae displays cosiderable morphological diversity, but some of the genera are so obscurely differentiated as to engender the possibility that a group of species clustered around Heterocarpus lae- vis and H. alexandri might eventually con- stitute a valid separate genus. The danger of prematurely accepting potential generic characters in the family, however, 1s man- ifested by the occurrence of a well-defined boss on the tergum of the third abdominal somite in those two Atlantic species and the virtually complete absence of such a boss in the Pacific species that are obviously closely related to them: Plesionika fenneri, Heterocarpus nesisi, and the Hawaiian spec- imen assigned to H. alexandri by Rathbun (1906). Acknowledgments But for the serendipity provided by Ardis Johnston of the Museum of Comparative Zoology in response to my inquiry about the specimen identified by Faxon (1896:161) as Heterocarpus alexandri, the holotype of that species would have remained “‘lost”’ in- definitely. Iam most grateful to her for that welcome information and for making the type specimen available to me. I also thank Alain Crosnier of the Muséum national d’Histoire naturelle in Paris and my Smith- sonian colleague Brian Kensley for reading the manuscript. Literature Cited Alcock, A., & A. R. Anderson. 1894. Natural history notes from H. M. Indian Marine Survey Steam- er ““Investigator,’’» Commander C. F. Oldham, R.N., commanding, series 2(14); An account of a recent collection of deep sea Crustacea from the Bay of Bengal and Laccadive Sea.— Journal of the Asiatic Society of Bengal. new series, 63: 141-185, pl. 9. Bate, C. S. 1888. Report of the Crustacea Macrura collected by H.M.S. Challenger during the years 1873-76.— Report on the scientific results of the voyage of H.M.S. Challenger during the years 1873-76 24:i-xc, 1-942, figs. 1-76, 157 pl. Burukovsky, R.N. 1986. [Anew shrimp species from the genus Heterocarpus (Crustacea: Decapoda: Pandalidae) and a brief review of the genus.]— Byulleten Moskovskogo Obshchestva Ispytate- ley Prirody Otdel Bioloogicheskiy 91(5):62-73, figs. 1-4. [Russian with English summary.] Chace, F. A., Jr. 1985. The caridean shrimps (Crus- tacea: Decapoda) of the A/batross Philippine Ex- pedition, 1907-1910, part 3: Families Thalas- socarididae and Pandalidae.—Smithsonian Contributions to Zoology 411:1—143, 62 fig. Crosnier, A. 1986a. Crevettes de la famille des Pan- dalidae récoltées durant ces derniéres années en Polynésie francaise. Description de Plesionika chacei et P. carsini spp. nov.—Bulletin du Mu- seum National d’Histoire Naturelle, sér. 4, 8, sect. A(2):361-377, figs. 1-4. . 1986b. Plesionika fenneri, nouveau nom pour Plesionika chacei Crosnier, 1986.— Bulletin du Muséum National d’Histoire Naturelle, sér. 4, 8, sect. A(3):691. de Man, J. G. 1920. The Decapoda of the Siboga Expedition, IV: Families Pasiphaeidae, Stylo- dactylidae, Hoplophoridae, Nematocarcinidae, Thalassocaridae, Pandalidae, Psalidopodidae, Gnathophyllidae, Processidae, Glyphocrango- nidae and Crangonidae.—Siboga-Expeditie Monographie 39a:1-318, pl. 1-25. Faxon, W. 1896. Reports on the results of dredging, under the supervision of Alexander Agassiz, in the Gulf of Mexico and the Caribbean Sea, and on the east coast of the United States 1877 to 1880, to the U.S. Coast Survey Steamer “Blake,” Lieut.-Commander C. D. Sigsbee, U.S.N., and Commander J. R. Bartlett, U.S.N., command- ing. 37. Supplementary notes on the Crusta- cea.— Bulletin of the Museum of Comparative Zoology at Harvard College 30(3):153-166. Milne-Edwards, A. 1881. Description de quelques Crustacés Macroures provenant des grandes profondeurs de la mer des Antilles. —Annales des Science Naturelles, Zoologie, sér. 6, 11(4): 1-16. 1883. Recueil de figures de Crustacés nou- veaux Ou peu connus, Paris, 3 pp, 44 pls. Rathbun, M. J. 1906. The Brachyura and Macrura of the Hawaiian Islands. — Bulletin of the United States Fish Commission (1903) 23(3):827—930 [reprint with index pages i—vili], figs. 1-79, pl. 1-24. Department of Invertebrate Zoology, Na- tional Museum of Natural History, Smith- sonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 89-94 GAMMAROPSIS ARAWAKIA, A NEW SPECIES OF MARINE AMPHIPODA (CRUSTACEA) FROM JAMAICA James Darwin Thomas and J. L. Barnard Abstract.—One of the dominant amphipods in algal turf communities at Discovery Bay, Jamaica, is a new species, Gammaropsis arawakia, character- ized by long peduncle of uropod 3, small coxa 1, 3-articulate accessory flagellum, extremely setose gnathopod 2, one pair of dorsal teeth on urosomite 1, pointed ocular lobe, and oblique upper margin of cephalic sinus for antenna 2. Gammaropsis arawakia is very abundant in the algal turf that now (1986) covers the heavily disturbed reef at Discovery Bay, Ja- maica. The living coral was damaged by the hurricane of 1980 and any regenerants al- most completely exterminated by algal turf in 1984-1986. This turf developed follow- ing the death of the herbivorous urchins Diadema antillarum (information from Di- rector Dr. Jeremy Woodley). A nearby load- ing dock for bauxite may also be a factor in the disturbance, although we are informed that the coral damage and turf development are common to most of the north coast of Jamaica. Discovery Bay is also character- ized by the presence of large, cold fresh- water seeps. Other amphipod genera pres- ent in this turf mat are Lembos, Elasmopus and Hyale. Isaeidae Gammaropsis arawakia, new species Figs. 1-3 Etymology. —Named for the Arawak, former Indian tribe of the central Carib- bean. Diagnosis. —Ocular lobe projecting mod- erately, bearing sharp anterior cusp, lower antennal sinus with oblique dorsal margin; eyes of medium size, with irregular mass of purple pigment surrounded sparsely by clear ommatidia. Accessory flagellum 3-articu- late, articles 1-2 long, apical article minute. Epistome sharply produced into long an- terior spike. Mandibular palp article 3 cla- vate, with subdistal anterior notch, heavily setose. Inner plate of maxilla 1 naked, outer plate with 9 spines. Plates of maxilla 2 broad, inner with oblique facial row of 6 setae. Anterior coxae short, coxa | less than half as wide as coxa 2, rounded-quadrate an- teroventrally, coxa 3 narrower than coxa 2, coxa 5 as long as coxa 4. Carpus of gnatho- pod 1 longer than propodus, dactyl strongly overreaching oblique palm. Article Z of gnathopod 2 densely setose mediodistally, carpus short, propodus greatly enlarged, palm oblique, convex, defined by tooth lacking spine, densely setose medially and anteriorly, these setae projecting dorsally and medially. Locking spines of pereopods 3—4 absent, of pereopods 5-7 forming unequal pair. Pereopods 5-7 of similar structure but increasingly longer, article 2 very narrow and smooth posteriorly. Epimera 1-3 similar, each with small pos- teroventral tooth and setule-notch, poste- rior margins weakly convex. Urosomite | with pair of weak dorsal teeth side by side. Uropod 1 with medium interramal tooth, lacking on uropod 2; each ramus of uropods 1-2 with elongate apical spine. Peduncle of uropod 3 elongate, rami lanceolate but al- most rod-like, subequal to each other but longer than peduncle, outer ramus with 90 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON P|) \ ye Ny L) OK PRE VOLUME 102, NUMBER 1 elongate apical spine-setae about as long as peduncle of uropod 2. Telson ordinary. Description of male “‘a’’ 2.09 mm. —Left mandibular incisor with four teeth, lacinia mobilis with four teeth, main rakers three. Apex of palp on maxilla 1 with four spines, one apicolateral spine-seta, 3 subdistal fa- cial setae; inner plate short, softly triangu- lar. Inner plate of maxilliped with 3 medial setae, 7 apical setae, three stout apical spines, one ventral facial locking spine and one ventral seta; outer plate with four thick ser- rate medial spines, two similar but thinner apical spines and 2 apical setae, ventral sur- face with 11 scattered setae; dactyl elongate, nail of medium length, with three accessory setules (Figs. 1-3). Apices of rami on uropods 1-2 as in en- larged illustration, with medial elongate spine and short lateral spine, except inner ramus of uropod 2 with long and short spines reversed. Description of female “‘b’” 2.47 mm.— Oostegites 2 and 5 short, slender, with 2 and 6 setae each, oostegites 3 and 4 twice as long and wide, with 10 setae each; gills 2-3 and 6-7 sac-like, slender, 3 times as long as broad, gills 4 and 5 about 4 times as long as broad, scarcely broader than others. Holotype. —USNM No. 195175, male “‘a”’ 2.09 mm. Type locality.—Jamaica station 1B, Dis- covery Bay, backreef, 1 m, 6 Sep 1986, on Acropora palmata rubble mound near chan- nel marker, formaldehyde wash of algal turf, coll. J. D. Thomas and J. Clark. Material.—Type locality, female “‘b’”’ 2.47 mm, female “‘c’? 2.14 mm, male ‘“‘d”’ 2.03 mm and 15 other specimens. Numerous — Fig. 1. 91 specimens from many other similar samples also deposited in Smithsonian crustacean collections. Relationship. —There are 105 species of Gammaropsis so that it was a laborious task to distinguish our species from the score of species that it resembles. To avoid a lengthy discussion we have eliminated those species not fitting significant parts in the following diagnosis: Ocular lobe pointed, short; eyes small; antennae of medium length; coxae 1-5 short and almost evenly extended; carpus of gnathopod 1 long; carpus of gnathopod 2 short, propodus evenly rectangular, palm shorter than posterior margin of propodus, regular, poorly sculptured, defined, medial surface of hand heavily setose; epimeron 3 with point; urosome with only one pair of dorsal teeth; peduncle and rami of uropod 3 elongate, armaments of rami very sparse and simple. Gammaropsis (=Eurystheus, Kermys- theus, Podoceropsis, Megamphopus, Se- gamphopus, Pseudeurystheus, see Barnard 1973) contains a diversity of species not yet organized cladistically. Note that Paranae- nia Chilton (1884) is being revived by Bar- nard & Karaman (1989). Gammaropsis ara- wakia resembles Segamphopus and Pseudeurystheus in the elongate carpus of gnathopod 1 and such species as G. exser- tipes and G. spinosa in the elongate peduncle of uropod 3. It also resembles several species with densely setose gnathopod 2 such as G. setifera, G. tonichi, and G. tawahi. The nar- row coxa | suggests certain species of Me- gamphopus but most members of that “‘ge- nus” have other anomalies in gnathopods Gammaropsis arawakia, unattributed figures = holotype male “‘a”’ 2.09 mm; d = male “‘d” 2.03 mm. Capital letters denote main parts in the following list; lower case letters to right of capital letters or in body of figure indicate modifications as follows; lower case letters to left of capital letters indicate specimens described in captions: B, body; D, dactyl of thoracic leg; E, prebuccal lateral; G, gnathopod; H, head; M, mandible; N, mandibular molar; O, outer ramus; P, pereopod; R, uropod; S, maxilliped; T, telson; V, palp; W, pleon; X, maxilla; r, right; s, setae removed; t, left. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 92 fj “a”? 2.09 mm. Letter codes see Fig. 1. Fig. 2. Gammaropsis arawakia, holotype male VOLUME 102, NUMBER 1 93 Fig. 3. Gammaropsis arawakia, holotype male ‘“‘a” 2.09 mm. Letter codes see Fig. 1. or other coxae. We have ignored species of *“‘Podoceropsis”’ and “‘Kermystheus’”? which have severely reduced accessory flagella. Gammaropsis tawahi Barnard (1972), from New Zealand, has an elongate pedun- cle on uropod 3 and densely setose gnatho- pod 2 but the palm bears a tooth near the hinge, the apical armaments on uropods 1- 3 are all short, mandibular palp article 3 lacks a notch and the antennae are short- ened and sparsely setose. Our species is close to G. averus Reid (1951) from West Africa, but differs in the broader hand of gnathopod 2 and less sculp- tured palm. Our species differs: From G. sutherlandi Nelson (1981), North Carolina, in the small even coxae 1-5, strongly subchelate gnatho- pod 2 and simpler spination of uropod 3; From G. hirsuta Reid (1951), West Africa, in the more sculptured palm and long prop- odus of male gnathopod 2 and the longer carpus of gnathopod 1; From G. tonichi Bar- nard (1969), Pacific Mexico, in the presence of only one pair of teeth on the urosome, and the lack of radical transformations oc- curring in male gnathopod 2 and coxa 7; From G. spinosa Shoemaker (1942), Pacific Mexico, in the small coxae 1—5 and medium (versus very short) antennae; From G. chil- toni and G. haswelli Thomson (1897), New Zealand, in the sharp ocular lobes, small coxae 5-6 and the ordinary, not grotesque, male gnathopod 2; From the pan-tropical G. atlantica Stebbing (1888) in the normal and small eyes and longer carpus of gnatho- pod 1; From G. thomsoni Stebbing (1888), New Zealand, in the more simplified ar- maments on the more elongate rami of uro- pod 3; From G. exsertipes Stebbing (1888), Kerguelen, in the ordinary condition of cox- ae 1—5 (versus enlarged), male gnathopod 2 (versus grotesque or elephantine), epimeron 3, regular length of antennae and sharp ocu- lar lobes; From G. anomala Chevreux (1926), warm eastern Atlantic, in the nor- mal gnathopod 2 and pereopod 5 which in the Lusitanian species are respectively weakly palmate and elephantine. The following species also have many 94 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON similarities to ours but differ in two or more of the characters in the diagnosis presented just above: G. dilatata and G. pseudoden- ticulata Ledoyer (1982) from Madagascar; G. pacifica and G. setifera Schellenberg (1938) from the middle Pacific Ocean; G. crenulata and G. ulrici Krapp-Schickel & Myers (1979) from the Mediterranean Sea; G. palmata (Stebbing & Robertson, 1891) from Europe; G. e/lisi Conlan (1983) from cold-temperate eastern Pacific; and G. lo- bata Chevreux (1920) from Europe. Acknowledgments We thank Janice Clark for her assistance in the field in Jamaica and Kimberly R. Cleary for her assistance in our laboratories at the Smithsonian Institution. Dr. Jeremy Woodley, Director of the Discovery Bay Marine Laboratory, and his staff gave us considerable help in our survey studies. Literature Cited Barnard, J. L. 1969. A biological survey of Bahia de Los Angeles Gulf of California, Mexico, IV. Benthic Amphipoda (Crustacea).—Transac- tions of the San Diego Society of Natural His- tory 15:175-228. 1972. The marine fauna of New Zealand: Algae-living littoral Gammaridea (Crustacea Amphipoda).—New Zealand Oceanographic Institute Memoir 62:1-216. 1973. Revision of Corophiidae and related families (Amphipoda).—Smithsonian Contri- butions to Zoology 151:1-27. , & G. S. Karaman. 1989. The families and genera of Gammaridean Amphipoda (except marine Gammaroids).—Smithsonian Contri- butions to Zoology (In press). Chevreux, E. 1920. Sur quelques amphipodes nou- veaux OU peu connus provenant des cdtes de Bretagne. — Bulletin de la Société Zoologique de France 45:75-87. 1926. Amphipodes I.—Gammariens (suite). Voyage de la goélette Melita aux Canaries et au Senegal 1889-1890.—Bulletin de la Société Zoologique de France 50:365-398. Chilton, C. 1884. Additions to the sessile-eyed Crus- tacea of New Zealand.—Transactions and Pro- ceedings of the New Zealand Institute 16:249- 265. Conlan, K. 1983. The amphipod superfamily Coro- phioidea in the northeastern Pacific region 3. Family Isaeidae: Systematics and distributional ecology. — Publications in Natural Sciences, Na- tional Museum of Natural Sciences, Canada 4: 1-75. Krapp-Schickel, G., & A. A. Myers. 1979. The Med- iterranean species of Gammaropsis Liljeborg (Crustacea, Amphipoda).—Bollettino del Mu- seo Civico di Storia Naturale, Verona 6:441- 467. Ledoyer, M. 1982. Crustaces amphipodes gamma- riens familles des Acanthonotozomatidae a Gammaridae.—Faune de Madagascar 59(1):1— 598. Nelson, W. 1981. A new species of the marine am- phipod genus Gammaropsis from the south- eastern United States (Photidae).— Proceedings of the Biological Society of Washington 93:1223- 1229, 3 figs. Reid, D. M. 1951. Report on the Amphipoda (Gam- maridea and Caprellidea) of the coast of tropical West Africa.—Atlantide Report 2:189-291. Schellenberg, A. 1938. Litorale Amphipoden des tro- pischen Pazifiks.—Kungliga Svenska Veten- skapsakademiens Handlingar (3)16(6):105 pp. Shoemaker, C. R. 1942. Amphipod crustaceans col- lected on the Presidential Cruise of 1938.— Smithsonian Miscellaneous Collections 101(1 1): 1-52. Stebbing, T. R. R. 1888. Report on the Amphipoda collected by H.M.S. Challenger during the years 1873-—76.—Report on the Scientific Results of the Voyage of H.M.S. Challenger During the Years 1873-1876, Zoology 29:xxiv and 1737 pp. —, & D. Robertson. 1891. On four new British Amphipoda.—Transactions of the Zoological Society of London 13:31-42. Thomson, G. M. 1897. On two new gammarids from New Zealand.—Annals and Magazine of Nat- ural History, ser. 6, 20:447-451. (JDT) The Reef Foundation, P.O. Box 170, Big Pine Key, Florida 33043; (JLB) Department of Invertebrate Zoology, Na- tional Museum of Natural History, NHB- 163, Smithsonian Institution, Washington, DCs 20560. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 95-105 NATATOLANA PASTOREI (GIAMBIAGI, 1925) (CRUSTACEA, ISOPODA, CIROLANIDAE) FROM THE STRAITS OF MAGELLAN, SOUTH AMERICA: REDESCRIPTION AND NOTES ON FUNCTIONAL MORPHOLOGY Johann Wolfgang Wagele and Niel L. Bruce Abstract. —Cirolanids caught with baited traps in the Straits of Magellan and identified as Natatolana pastorei (Giambiagi) are described. Observations on living specimens suggest that several features, such as the broadened merus of the anterior pereopods, the arrangement of spines and setae are adaptations to digging and respiration in sand. Giambiagi (1925) described briefly from “San Sebastian, Tierra del Fuega,” south of the eastern entrance of the Straits of Ma- gellan, a cirolanid named Cirolana pastorei. No other figures than those published by Giambiagi exist; they are not adequate to distinguish this species from the many sim- ilar cirolanids known today. Another ciro- lanid from the Straits of Magellan was men- tioned by Pfeffer (1887) in a list of species collected during a German expedition to South Georgia (1882-1883). Of this Ciro- lana magellanica no illustrations or de- scriptions were ever published. The name was therefore listed as nomen nudum by Bruce (1986). During an expedition to Antarctica (1985— 1986) with R/V Polarstern a large number of cirolanids were caught in a baited trap in the Straits of Magellan. Most of these ani- mals were kept in aquaria for bionomic studies. Later the same species was found in collections of the Zoologisches Museum Hamburg, in vials labelled ““Cirolana ma- gellanica, cf. types,” which possibly contain the specimens studied by Pfeffer (1887). Further material was kindly sent to the first author by Dr. Gruner from the Zoologisches Museum Berlin, also with the label “‘Ciro- lana cf. magellanica.”’ The species clearly belongs to the genus Natatolana Bruce, 1981 and is related to a group of large species, the Natatolana valida group, that have an exclusively southern hemisphere distribution (Bruce 1986). The species was compared to drawings of the types of Natatolana rossi, N. hirtipes and all subantarctic species and found to be dis- tinct. The species here described is identical with the Cirolana pastorei of Giambiagi (1925); no differences from the original de- scription or the type specimens could be found. The species is not identical with the Cirolana pastorei from South Georgia men- tioned by Monod (1931). Natatolana pastorei (Giambiag1) Figs. 1-7 Cirolana pastorei Giambiagi, 1925:4—7, pl. 1, pl. 3, fig. 3, not Cirolana pastorei sensu Monod, 1931:22. Cirolana magellanica Pfeffer, 1887:58, no- men nudum.—Bruce, 1986:218. Material examined.—Male, length 33 mm, partly dissected, Magellan Straits, 52°17.49'S, 69°8.96'W, 35 m; 15 Nov 1984; four adult specimens, 27-36 mm, from the same locality, Zoological Museum Ham- burg, K-33324. Further material: Zoologi- cal Museum Hamburg, K-19219, Magellan 96 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON X) Q) Q ee ae SS Gon on en ", > p 1) WHA, By) SA) TE vv td Vr VXyt . \\\ Wh \| S Fig. 1. Natatolana pastorei: A, Male in dorsal view; B, Ventral aspect of cephalothorax; C, Posterior segments, ventral. Arrow: respiratory current passing through filter of pereopods 5—7. Abbreviations.—A1, A2: antenna 1,2; La: labrum; Md: mandible; MdP: palp of Md; Mx1, Mx2: maxilla 1,2; Mxp: maxilliped; PJ-7: pereopods 1- 7; Plp1-5: pleopods 1-5; Tel: telson; Urp: uropod. mens, 13-15 mm, leg. Prof. Carlos Grethe, Magellan Str., 19 Nov 1908; further mate- rial collected by Kpt. Paessler: K-23268 (about 52°20’S, 69°W), K-23287 (51°54’S, Straits, labelled ““Cirolana magellanica, cf. types,” leg. Kpt. R. Paessler 1886: 44 spec- imens, 13-29 mm, one male of 30.5 mm, no mature females; also included: 5 speci- VOLUME 102, NUMBER 1 97 ___0.5mm__, Fig. 2. Natatolana pastorei, male in lateral view; arrows: respiratory current passing through setal combs of basipodites, antennule with detail of flagellar setation. For abbreviations see Fig. 1. 98 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 73°42'W), K-23281 (about 47°S, Golfo de Penas), K-23278 (Hale Cove, Patagonia); with number K-23242 two samples are de- posited: leg. Dr. Gassmann, Magellan Str., 1 Nov 1895, and leg. Umbach, off Punta Arenas, Chile (53°10’S, 70°54’W), 1 Jan 1903. Zoological Museum Berlin, Nr. 8118, Magellan Str., leg. Pohl: three small speci- mens (10-18 mm); one further specimen was sent to the Copenhagen Museum, prob- ably for H. J. Hansen. Museo Argentino de Ciencias Naturales ‘“‘Bernardino Rivadavia,’’ Buenos Aires, Nr. 12690: nine syntypes, San Sebastian, Tierra del Fuego. Description. —Body about 2.5 times as long as broad. Cephalothorax and eyes as in Figs. 1 & 2; beneath eye a deep groove for antennae. Coxae one to three with curved carina running from frontal area of coxa to posterolateral point; coxae four to seven with more pronounced, less curved medial ca- rina; coxa seven reaching beyond epimeral plate of pleonite 1 (Fig. 2). Epimeral plate of pleonite 3 narrower than preceding plate, posteriorly acute. Outline of telson as in Fig. 7, distal margin with six to seven sensory spines on each side and between them rows of four to five setae. Antennule peduncle of 4 articles (3 in the sense of Wagele 1983), article 3 longest (Fig. 2); article 4 short, with three plumose setae; flagellum not much longer than peduncle, with 17 articles, articles short and broad, with rows of aesthetascs and each 2nd or 3rd article with a group of short simple se- tae, last article with simple setae and one plumose seta (Fig. 2). Antenna peduncle ar- ticle 2 very short, article 5 longest; fourth article with lateral row of seven simple se- tae; flagellum long, extending to pereonite 3, of about 30 articles; last articles more slender and relatively longer than basal ar- ticles (Fig. 3). Mandible palp setation as in Fig. 3. Lat- eral endite of maxillule gnathal surface with 13 stout spines, medial endite short, with three stout apical teeth and subapically a smaller, slender trifurcate spine (Fig. 2). Maxilla of three lobes; proximal endite with two rows of setae, first row with 11, second with 17 setae; medial (second) endite with 15 long setae and a second row with 11 shorter setae; distal lobe bearing 5 setae. Maxilliped endite with two coupling hooks; all palp articles bearing large numbers of simple setae (Fig. 4). Pereopod 1 merus posterior margin with 14 acute spines; carpus posterodistal margin with 2 long and 2 short acute spines: pro- podal palm with 4 large acute and 5 small acute spines and stout spine opposite base of dactylus. Pereopods 2 and 3 similar to 1 but spines of merus and carpus larger, pe- reopod propodal palm with 3 spines, is- chium posterodistal margin with additional spines. Pereopod 3 with only 2 small spines on propodal palm. Pereopods 4—7 essen- tially similar but basis widening and all ar- ticles increasing in length towards posterior. Pereopod 7 basis about 1.8 times as long as greatest width, posterior margin shallowly convex, anterior margin feebly sinuate; is- chium, merus and carpus with clusters of spines at distal angles and along posterior margins; propodus with three groups of 2— 4 spines on posterior margin and a group of 4 spines opposite base of dactylus. Pleopods conform to the generic condi- tion; pleopod 2 of male with appendix mas- culina, apex narrowed, slightly angled, slightly extending beyond apex of endopod. Uropod endopod medial margin convex with six spines and a further apical spine, lateral margin with two large and two small spines, apex narrow. Exopod lanceolate, lat- eral margin with eight spines and a further small apical spine, medial with four. Variations of spine armature of tail fan in adult specimens (25-36 mm): Distal mar- gin of telson with 6 to 8 spines on each side (generally 6), lateral margin of uropod ex- opod with 9 to 11 (usually 10, including apical spine), medial margin always with 4 (including apical spine of this side), lateral VOLUME 102, NUMBER 1 99 Fig. 3. Natatolana pastorei, male: Last articles of antenna and apical part of 5th peduncular article (inset, bottom) of immature adult; Right mandible (r. Md) with detail of setal lobe. For abbreviations see Fig. 1. 100 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 4. Natatolana pastorei, male: Maxilliped with detail of endite; several setae and sensory spines cut off. For abbreviations see Fig. 1. VOLUME 102, NUMBER 1 101 XQ \ =S Ulta, an Ago rttege » Set Fig. 5. Natatolana pastorei, male: Pereopods 2-5, several setae and sensory spines cut off. For abbreviations see Fig. 1. 102 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Yj Y MG Wh ~—— — _—-—~_— —— Soe oe —— \ é \S \ NY Ys he SY nh LZ WY we” . AY at\ a \ fina x \ wus ‘ a fee > \v vie OU \ ne y ® VY ae _ S= A a P AIL a ——— hid a = ~U 5 fez Y Take Wa \ =— ere ON) j Se A \ g™ Wit iy f A eee 227111 ar Fig. 6. Natatolana pastorei, male: Several setae and sensory spines cut off; setae of pleopods shown as simple setae; dashed line (Plp 2): range of setae. For abbreviations see Fig. 1. VOLUME 102, NUMBER 1 Tel , 225 mm _, 103 Urp Wepre at steal Fig. 7. Natatolana pastorei, male: Setae of pleopods shown as simple setae, dashed line indicating length of setae; detail of Plp 5 showing apex of endopod; detail of uropod showing a sensory spine. For abbreviations see Fig. 1. margin of endopod always with 4, medial with 4 to 7 spines (including apical spine). Color.—Purple brown, chromatophore pattern shown in Fig. 1. Size. —Immature adults 27-34 mm, males 30.5-—33 mm. Remarks. —Natatolana pastorei belongs to the N. valida group of species character- ized by Bruce (1986). It can be distinguished from all of those species listed by having a slightly wider basis to pereopod 7, narrow apices on the uropod rami, and also differ- ences in the spination of the uropod rami. Other large Natatolana species include those found in the subantarctic region such as N. meridionalis Hodgson, N. nitida Hale or N. obtusata VanhOffen (these species were list- ed by Bruce, 1986). All of these species are 104 characterized by large penial processes, broad or elongate appendix masculina and acute upturned posterolateral margins on pleonite 4. The present material differs from the ma- terial discovered in South Georgia and men- tioned by Monod (1931) as ““Cirolana pas- torei.”’ An examination of Monod’s material (collection of the Senckenberg Institute, Frankfurt) revealed the following differ- ences: Lateral margin of uropod endopod with six spines (instead of four in N. pas- torei); telson narrower; antennule shorter with only 12 flagellar articles; groove be- neath the eyes not present; eyes longer and less wide (number of ommatidia in N. pas- torei (17.5 mm): longitudinal line with 11- 12, vertical line with 12; in the specimen from South Georgia: longitudinal line with 14-15, vertical line with 8-9). So the pop- ulation from South Georgia must belong to a different species. Distribution. —Known from Straits of Magellan and between Hale Cove, Argen- tina to Punta Arenas, Chile, and from San Sebastian, Argentina. Occurs in shallow sublittoral sediments. Observations on biology and functional morphology. —About 20 specimens were observed in aquaria kept at 1—2°C together with other Antarctic isopods. At this low temperature the animals were inactive for many weeks, only sporadically feeding on pieces of krill and fish. All specimens bur- rowed in sand; when resting only the tips of the antennae and sometimes the eyes could be seen. In coarse sand burrowing is diffi- cult, as the grains keep rolling back into the groove, but in fine sand the specimens dis- appear within 1—2 min. The sand is pushed with the first pereopods laterally and cau- dally, the broad merus with its setae being a very effective broom; the posterior pe- reopods push the sand caudally, their effec- tiveness is increased due to the lateral spines (Fig. 1, bottom). The pleopods help when the animals dig fast; with their beat a strong current sweeps away the grains loosened by PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON the pereopods. In a depth of 2—5 cm the animals stop digging. After feeding the an- imals can obviously remain inactive for about two months; in aquaria the animals were fed only once a week and mostly the food was not consumed. Though the low temperature affects the metabolism, in na- ture this species is probably also able to sur- vive several weeks without food, living as an opportunistic carrion feeder. Some isopods living in sand possess a protective operculum to cover the respira- tory pleopods (Chaetiliidae, Bathynatali- idae, Serolidae, Anthuridae). The cirolanid genera Conilera and Oncilorpheus also have such structures, but operculate pleopods are absent from other cirolanid genera. In Na- tatolana the setae of the pereopods are ar- ranged in such a way, that sand grains are kept away from the thin pleopods. While on the ventral side gravity will keep many grains in their place, the sides of the animal are protected against sand; the marginal se- tae of the pereopods cover the slits between the basipodites, where the respiratory cur- rent passes (Fig. 2). Directly in front of the pleopods, the setae of the frontal margins of the basis and ischium of PS5—7 form a fan- like filter, to intercept grains and detritus. The pereopods are not used for swim- ming, animals swim with their dorsum downwards, propelled only by the beating pleopods. The broadened merus of P1-3, flattened basis with the marginal setae of P5-7, the arrangement of the sensory spines are adaptations to digging in fine sand. Acknowledgments We are grateful to Prof. G. Hartmann (Hamburg), Dr. M. Turkay (Frankfurt), and Prof. H. E. Gruner (Berlin, G.D.R.) for the loan of specimens. Mrs. S. Willig kindly fed and cultured the living animals. Mr. A. Pompecki helped to prepare the plates. This study was supported by the German Science Foundation (DFG Nr. Wa-530) to J.-W. Wagele, and a Queen’s Fellowship in Marine Science to N. L. Bruce. VOLUME 102, NUMBER 1 Literature Cited Bruce, N. L. 1981. Cirolanidae (Crustacea: Isopoda) of Australia: Diagnoses of Cirolana Leach, Me- tacirolana Nierstrasz, Neocirolana Hale, An- opsilana Paulian & Deboutteville, and three new genera—Natatolana, Politolana and Carteto- lana. — Australian Journal of Marine and Fresh- water Research 32:945-966. 1986. Cirolanidae (Crustacea: Isopoda) of Australia.— Records of the Australian Museum Supplement 6:1—240. Giambiagi, D. 1925. Resultados de la primera ex- pedicion a Tierra del Fuego (1921). Crustaceos IsoOpodos. — Anales de la Sociedad Cientifica Ar- gentina, Buenos Aires 1925:229-245. Monod, T. 1931. Tanaidacés et isopodes subantarc- 105 tiques de la collection Kohl-Larsen du Senck- enberg Museum.—Senckenbergiana 13:10-30. Pfeffer,G. 1887. Die Krebse von Siid-Georgien nach der Ausbeute der Deutschen Station 1882/83. I.—Jahrbuch der Hamburger Wissenschaftli- chen Anstalten 4:41-150. Wagele, J. W. 1983. On the homology of antennal articles in Isopoda.—Crustaceana 45:3 1-37. (JWW) Arbeitsgruppe Zoomorphologie, Fachbereich 7, Universitat Oldenburg, P.O.B. 2503, 2900 Oldenburg, FRG; (NLB) Australian Museum, Division of Inverte- brate Zoology, P.O.B. A285, Sydney South, N.S.W. 2000, Australia. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 106-108 NEOBRACHIELLA ANISOTREMI (COPEPODA: LERNAEOPODIDAE), A NEW SPECIES PARASITIC ON AN INSHORE FISH, ANISOTREMUS SCAPULARIS, OFF THE CHILEAN COAST Raul Castro Romero and Hernan Baeza Kuroki Abstract. — Neobrachiella anisotremi, parasitic on Anisotremus scapularis, an inshore fish of the northern coast of Chile, is described and illustrated. The new species can be distinguished from all the species in the genus by a com- bination of characters including second maxilla, trunk-cephalothorax length ratio, and specially the posterior processes. The existing literature contains very little information on the genus Neobrachiella Ka- bata, 1979, in Chilean waters. Only five species have been recorded. Krgyer (1863) gave a sketchy decription of Anchorella (=Neobrachiella) appendiculata, without recording its host. Ho (1983) described Neo- brachiella amphipacifica, a species occur- ring in both the North and South Pacific. In the latter it was found on Psichrolutes sio Nelson, a deep water fish, in northern Chile. Castro & Baeza (1986) added to the list Neo- brachiella exilis (Shiino, 1956) parasitic on Mugil cephalus L., 1758; N. chevreuxii (van Beneden, 1891), from Paralonchurus peru- anus (Steindachner, 1785) and N. paralich- hyos, Castro & Baeza, 1986. Recently we decribed four other species collected from sciaenid hosts from the Chilean coast (Cas- tro & Baeza 1987). In the course of our studies of the parasitic copepods of Chilean fishes, we discovered another species of Neobrachiella, parasitic on an inshore fish, Anisotremus scapularis (Tschudi). This species is described and il- lustrated below. Terminology used is that proposed by Kabata (1979). Neobrachiella anisotremi, new species Figs. 1-7 Material examined. —Four ovigerous fe- males (8 Jan 1982); one female (12 Mar 1982) and three females (14 Jul 1982). Types deposited in National Museum of Natural History (USNM), Smithsonian Institution. Holotype USNM 210517; Paratype USNM 210158. Habitat.—Branchial arches of A. scapu- laris, collected by beach seining. Locality. —Isla Santa Maria, Antofagasta (2327-5, FO225 Why: Description. —Female (Fig. 1). Cephalo- thorax subcylindrical, arching with slightly expanded cephalic region, mean length 2636 um (range 2242-2908 um), width 455 wm (range 364-545 um); dorsal shield well de- limited, subrectangular. Trunk much longer than wide, mean length 2909 um (range 2121-3636 um), width 1136 wm (range 909- 1333 um); its length varying from 75 to 123% of that of cephalothorax; posterior extrem- ity with two pairs of processes (Fig. 7A, B); first pair ventral to egg sacs, mean length 736 um (range 606-805 um); its length 20— 38% that of trunk; second pair dorsal to egg sacs and shorter, mean length 570 um (range 483-606); its length 73-83% that of first; genital process of varying length, mean 186 um (range 113-145 um); poorly developed in some specimens. Egg sacs subcylindrical, multiseriate, mean length 2651 um (range 1818-3515 um); their length 71—112% that of trunk. First antenna (Fig. 2A, B) apparently 4— VOLUME 102, NUMBER 1 107 Figs. 1-4. Neobrachiella anisotremi: 1, Female, lat- eral view; 2A, First antenna; 2B, First antenna, detail of apical armament; 3A, Second antenna; 3B, Second antenna, detail of apical armament; 4, Mandible. segmented; first and second segments in- distinctly separated, second armed with spine on distoventral margin; third short, unarmed; fourth segment with apical ar- mament as follows: tubercles 1 and 3 well developed, 4a centrally situated, digitiform seta; 6a single slender seta, and 5a complex, consisting of a bifid seta and an additional simple process; gibber absent. Second an- tenna (Fig. 3A, B) strongly sclerotized, its long axis running through sympod and ex- opod; sympod bearing short robust spine on its distoventral border; exopod bulbous, apex spinulose on dorsal side; endopod 2-segmented, distal segment with apical spi- niform process (reduced hook one, see Ka- bata 1979) and two setae (spinulation on ventral surface of distal segment can be seen on distended cuticle in Fig. 3B). Mandible (Fig. 4) with dental formula P1,P1,S1,P1, S1,B3. First maxilla (Fig. 5) with papilli- Figs. 5-7. Neobrachiella anisotremi: 5, First max- illa, ventral; 6A, Maxilliped; 6B, Maxilliped, detail of myxal area and claw; 7A, Posterior end of trunk, fe- male; 7B, Lateral view of same, showing processes and egg sacs. form exopod situated ventrally, bearing single seta; endopod armed with two sub- cylindrical, setiferous papillae, ventral papilla stouter than dorsal; no spinulation observed. Second maxilla (Fig. 1) fused only at tip, slender, less than half length of ceph- alothorax; mean length 1051 wm (range 909- 1273 um); without conspicuous collars (bul- la with short manubrium and anchor of nar- row diameter). Maxilliped (Fig. 6A, B) corpus strong, slightly tapering, with spiniform process and denticulate pad in myxal area; patch of spi- nules near maxilla with subchela; shaft of subchela with barb and spinulose pad on distomedial part, claw gently curved, with two accessory teeth. Male. —Unknown. Etymology. —The specific name anisotre- mi, is derived from the generic name of the host. 108 Discussion. —To establish the identity of Neobrachiella anisotremi it must be com- pared with all the species of the genus pos- sessing two pairs of posterior processes. A comparison within this group must be based on a combination of gross morphological characters (cephalothorax length; trunk length; relationships between the length of posterior process and other parts of the body), since descriptions of the appendages are not available for all species. Using these criteria, the present species can be distin- guished from all of them by a combination of characters. It resembles most closely N. gulosa (Wilson, 1915) but can be differen- tiated from this species by the posterior pro- cesses. Wilson’s species has ventral processes as long as the trunk, whereas in N. anisotremi they are only 20-38% of the trunk length. Slight differences exist also in the structure of the second maxilla, that of N. gulosa, in contrast to N. anisotremi, having a promi- nent swelling accommodating the excretory glands. Another difference can be found in the cephalothorax-trunk length ratio. In N. gu- losa the cephalothorax is considerably long- er than the trunk, whereas in anisotremi the trunk is longer than the cephalothorax. A unique feature of N. anisotremi is the presence of a short spine on the distolateral border of the sympod of the second antenna. The four recently described species, para- sitic on host fishes of the genus Sciaena (N. oralis, N. auriculata, N. fasciata, and N. dis- par), which are included in the same group as the present one, can be differentiated by PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON a combination of characters that clearly dis- tinguish between each one and N. anisotre- mi. Their differences are given in the key to the species of Neobrachiella (Castro & Baeza 1987). Acknowledgments The authors wish to thank Dr. Z. Kabata for his review of the manuscript and spe- cially for inviting the first author to spend some time at the Pacific Biological station, Nanaimo, B.C., Canada where this paper was completed. They are also grateful to the Universidad de Antofagasta for making the journey to Canada possible. Literature Cited Castro, R., & Baeza, H. 1986. Some species of Neo- brachiella Kabata, 1979 (Copepoda, Lernaeo- podidae), parasitic on Chilean fishes, with de- scription of Neobrachiella paralichthyos sp. nov. from Paralichthys adspersus (Steindachner).— Crustaceana 51(3):245-253. ——., & 1987. Four new species of Neo- brachiella (Copepoda: Lernaeopodidae), para- sitic on Sciaena genus (Teleostei: Sciaenidae) in the South Pacific. — Estudios Oceanologicos 6(1): 1-24. Ho, J. S. 1982. Copepod parasites of Psychrolutes (Pisces: Scorpaeniformes) from deep waters in the eastern Pacific.— Parasitology 85:451-458. Kabata, Z. 1979. Parasitic copepoda of British fish- es.— The Ray Society, London, No. 152:1-469. Kroyer, H. 1863. Bidrag til Kundskab om snyltek- rebsene. — Naturhistorisk Tiddsskrift, ser. 3(2): 75-426, pls. 1-18. Universidad de Antofagasta, Instituto de Investigaciones Oceanologicas, Casilla 170, Antofagasta, Chile. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 109-115 THE FIRST ANNUAL RISER LECTURE: MEIOFAUNA AND MICROBES— THE INTERACTIVE RELATIONS OF ANNELID HOSTS WITH THEIR SYMBIOTIC BACTERIA Olav Giere Abstract.—The gutless marine tubificid Phallodrilus leukodermatus (Oligo- chaeta) harbors two kinds of chemoautotrophic sulfur bacteria beneath its cuticle. The annelid hosts live predominantly around the redox potential dis- continuity layer in calcareous sediments, providing their bacterial endosym- bionts with access to both oxygen and reduced sulfur compounds. The bacteria produce energy by oxidation of these sulfur compounds, and use this energy for the fixation of CO, and production of carbohydrates. The worms utilize the exudates of the bacteria and also ingest a portion of the bacterial population in the epidermal cytoplasm. Further interactions in this apparently obligate symbiosis are discussed. The transmittance of the bacteria through the host generations by “infection” of freshly deposited eggs is correlated with a modified reproductive biology. The studies on this symbiosis reveal a well-coordinated balance between the annelid hosts and their extracellular bacterial partners. Serendipity let us find a new species of small (2-3 cm long) white annelid worms in the calcareous sands of Bermudian reefs. These tubificid oligochaetes, described as Phallodrilus leukodermatus (Giere, 1979), were unique among known annelids. They lacked mouth, gut and anus and had no ex- cretory organs. But the most striking feature was a thick, subcuticular ‘mantle’ of extra- cellular bacteria living between extensions of the epidermal cells (Fig. 1). This bacterial association, present in each worm, even in the youngest, apparently The Riser Lecture Series.—In 1985 the annual Riser Lecture was initiated by members, alumni and friends of the Marine Science Center, Northeastern University at Nahant, Massachusetts. The occasion was the official retirement of Professor Nathan W. Riser. As teacher, biologist and founder of the facility, ‘““Pete’’ Riser en- dowed the laboratory with a legacy—the importance of considering the whole organism regardless of one’s special focus. We dedicate these annual lectures to that principle. consists of two different gram-negative pro- karyotes (Fig. 2), a smaller, rod-shaped form (maximally 1.9 x 0.4 wm) with a thick cell envelope, and a larger oval one (about 3 x 2 wm) characterized by a thinner body wall and, more conspicuously, by the rich supply of vesicles in its cytoplasm (Giere et al. 1984). This peculiar bacterial layer raises ques- tions about the nutrition of these worms and about the structural implications of com- plete reduction of the gut in worms from sands that otherwise are richly populated by other meiofauna, including oligochaetes with normal guts. Also the microdistribution of these exceptional worms is quite unusual (Giere et al. 1982). We found rich popula- tions in an area where, despite strong cur- rents, anoxic horizons occurred at 5 cm sed- iment depth. Only a few worms were present in the upper, oxygenated strata, while the bulk of the population always occurred in the deeper layers where they were exposed to considerable amounts of toxic hydrogen 110 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Doi am 7 Avance me VOLUME 102, NUMBER 1 sulfide (around 100 uM S~-) with oxygen present only in minimal concentrations. What promotes this exceptional distri- bution? How are the bacteria involved in this scenario? The answers require integra- tion of morphological studies with ecolog- ical, physiological and microbiological analyses, i.e., consideration of the whole animal’s biology. These studies were per- formed by a multidisciplinary team during several research periods at the Bermuda Bi- ological Station for Research and in mem- bers’ respective home laboratories. Structural and ecological similarities sug- gest that the symbiotic prokaryotes are sul- fur bacteria similar to those found in the giant vestimentiferan Riftia (Cavanaugh et al. 1981) from hydrothermal vents. The bacteria obtain energy by oxidation of re- duced-sulfur compounds, enabling them to fix ambient CO, with subsequent produc- tion of carbohydrates. For Phallodrilus leukodermatus, confir- mation of this pathway results from phys- 10logical analyses: Ribulosebiphosphate- carboxylase in high activities in the bacteria enables a notable incorporation of CO, with a most rapid transfer into the malate pool (Felbeck et al. 1983). The high activity of enzymes like ATP-sulfurylase and sulfite oxidase, involved in the sulfur metabolism, indicates more specifically that sulfur com- pounds become metabolized by the sym- biotic bacteria. Moreover, it can be shown that the products of this metabolism get stored in the numerous bacterial vesicles: —_— Lit Energy-dispersive X-ray microanalysis demonstrates high sulfur peaks in mem- brane-bound bacterial vesicles, suggesting deposition of polysulfanes or polythionates as easily available reserve products (Steudel 1985, Steudel et al. 1987). Sulfur also is found in the internal tissues of the worms where it accumulates in the ““chloragosomes,” annelid structures known to store xenobiotic substances. Thus, sulfur is transported from the ambient pore water (perhaps via the symbiotic bacteria?) to the internal worm tissues. Sulfate, the end prod- uct of oxidative sulfur metabolism, is ex- creted by the worms into the ambient sea water (Giere et al. 1988). Bacteria oxidizing sulfur compounds are micro-aerophilic, gram-negative microor- ganisms thriving in those horizons where they have access to both reduced sulfur and oxygen, 1.e., around the redox potential dis- continuity layer. Microdistribution of the worm population presents ecological con- firmation of these sulfur-based chemoau- totrophic processes in the annelid sym- bionts. The bulk of the worm population is always concentrated around this transition- al zone between the oxygenated surface lay- er and the anoxic depth with its poisonous hydrogen sulfide. In this zone the prokary- otic symbionts can synthesize their reserve substances. In addition to reduced-sulfur compounds, the bacterial cytoplasm abounds with unwalled globules (Fig. 2) filled with polyhydroxybutyric acid. Thus, in in- cident light worms from this zone have well- Figs. 1-3. Phallodrilus leuakodermatus: 1, Cross section through the gutless worm with “mantle” of subcu- ticular bacteria, scale bar = 50 um; chl = chloragocytes, coe = coelomic cavity, cu = cuticle, ep = epidermis, mu = musculature, ne = ventral nerve cord, scu = subcuticular space filled with bacteria; 2, The two kinds of bacteria endosymbionts; note difference in thickness of cell envelope, scale bar = 0.5 um; Iba = large bacterium, phb = vesicle filled with polyhydroxybutyric acid, sba = small bacterium, sve = sulfur vesicle; 3, Typical zonation pattern of subcuticular bacteria with free, active bacteria in peripheral position and enclosed, lytic bacteria in innermost position, scale bar = 5 wm; blys = bacteria in lysis, zba = zone of (free) bacteria, zint = intermediate zone bacteria become enclosed by epidermal strands, zlys = zone of bacterial lysis: bacteria are enclosed in vacuoles of epidermal cells and become digested (Fig. 1: light microscopy; Figs. 2+3: transmission electron microscopy). 112 fed bacteria and appear shiny white due to the rich content of light-refractile sub- stances in the bacterial cytoplasm, which can be almost 6% of the worm’s dry weight (Giere et al. 1988). When kept in pure, ox- ygenated seawater, the worms (through their bacteria) continue to take up CO, for a while from the environment, using up energy stored in the reserve substances. However, this uptake decreases soon, the worms be- come (after about 24 h) transparent pale- grayish, indicating rapid loss of their re- serves, which in these “pale worms” is only 1.7% of their dry weight (Giere et al. 1988). These results emphasize the biological in- teractions between the oligochaete host and its prokaryotic symbionts and lead to ques- tions for the biological function of the bac- teria/host system. The presence of bacteria in all members of the population and the ubiquity of bacterial incorporation in gut- less oligochaete species—several species mainly from the Caribbean, but also from Australian reefs have been examined—sug- gests an obligate symbiosis with mutual benefits. What are the benefits to the microorgan- isms of this incorporation into the worms’ bodies? -In a changing sedimentary system with steep, overlapping gradients of oxygen, sul- fide, thiosulfate and CO,, the highly motile worms are able to quickly adjust position relative to environmental fluctuations, maintaining an optimal combination of gradients required for growth of sulfur-ox- idizing bacteria. —It is conceivable that the prokaryotes take up organic substances excreted by their host which, in turn, has lost its excretory or- gans. The highly vesiculate epidermal cy- toplasm of the worms and the multitude of membrane-bound secretory granules found extracellularly in their subcuticular lumen suggest this physiological pathway. —The favorable position of the bacteria un- derneath the cuticle affords both shelter and easy access to nutrients from the am- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON bient pore water through the highly perme- able cuticle. On the other hand, what benefits might the oligochaetes derive from close associa- tion with bacteria? —Since the bacterial oxidation of reduced sulfur combines production of energy with detoxification of poisonous hydrogen sul- fide, the microorganisms enhance the chances of the worms to invade a biotope of high ecological potential, rich in dis- solved nutrients, but with little competi- tion or predation. Our physiological ex- periments demonstrate that the worms can actively and selectively take up dissolved hexoses (particularly glucose and galac- tose) and acidic free amino acids (partic- ularly glutamic acid and aspartate). These purely transcuticular absorption processes seem so intensive that, compared to cor- responding figures from pogonophorans of the same size, they “contribute signifi- cantly” to the nutrition of P. leukoder- matus (Liebezeit et al. 1983, Liebezeit, pers. comm.). —Exuded bacterial products could serve as a valuable and ever-present source of fur- ther dissolved organic matter. —Digestion of a certain portion of the inter- nal bacterial population would provide an additional trophic pathway. Comparison of bacteria in the deeper layer of the epi- dermis with those in the subcuticular areas reveals a zonation pattern (Fig. 3): Periph- eral bacteria are extracellular in a subcu- ticular lumen, where they accumulate re- serve substances and multiply intensively by division. In the middle zone they tend to be surrounded by strands of the epider- mal cells. the innermost bacteria are al- ways found enclosed in intracellular vac- uoles, apparently “‘engulfed’’ by the epidermal cells, and clearly undergoing lysis (Giere and Langheld 1987). This coordinated system, combining bac- terial growth and multiplication with lysis and digestion, is similar to those described VOLUME 102, NUMBER 1 Lh3 Figs. 4-5. Phallodrilus leukodermatus: 4, Cross section through genital pad in clitellar region, scale bar = 50 um; cl = clitellar glands in epidermis, gepa = genital pad filled with bacteria, ne = ventral nerve cord; 5, Cross section through young embryo with some free subcuticular bacteria (both kinds) and many lytic bacteria enclosed in host cells, scale bar = 1 um; balys = bacteria enclosed in embryonic cells, mostly in lysis, foa = free bacteria in peripheral layer (Fig. 4: light microscopy; Fig. 5: transmission electron microscopy). for some thyasirid bivalves (Southward 1986), for the vestimentiferans Riftia pachyptila (Bosch & Grassé 1984a, b) and Tevnia sp. (Bassaglia 1986) and is compa- rable to the processes found in the root nod- ules of Leguminosae (Sprent 1979). Thus, it seems that by their symbiosis with sulfur-oxidizing bacteria the worms have acquired a tripartite nutritional basis via transepidermal uptake of dissolved or- ganic matter, utilization of bacterial meta- bolic products, and digestion of bacterial cells. This flexible trophic pattern seems to allow for the complete loss of digestive and excretory organs. Moreover, the worms gained access to a new habitat, the sulfidic sediments. Examination of four additional species within the approximately 40 species of gutless marine tubificids showed that in each case associations with subcuticular bacteria are established, suggesting that this symbiosis is geographically as ubiquitous as it is evolutionarily favorable. An intricate, mutualistic and well-estab- lished symbiosis as seen in P. leukoder- matus might be predicted to have evolved a fairly secure method of transmitting the bacterial partners through the generations of their hosts rather than depending on more or less randomly repeated de-novo-infec- tions of the worms. A regular transmission would require specific adaptative trends in the reproductive biology of these oligo- chaetes (Giere & Langheld 1987). In fact, investigation of fully mature worms reveals formation of a ventral “‘gen- ital pad’’ (Fig. 4), a blister-like structure packed with masses of fully active bacteria ensheathed only by a thin cuticular enve- lope. In a few cases deposition of single eggs was observed. They are covered by a sticky mucus, but not enclosed in a cocoon as would be typical for oligochaetes. These eggs were already infected by the characteristic bacteria. These first bacteria are mostly in- tracellular, within the cleavage cells, and 114 clearly in a lytic stage (Fig. 5). Only a few peripheral bacteria maintain their subcutic- ular, extracellular position and have a healthy appearance. Probably the latter stock is the source of the rich supply of extracel- lular, active prokaryotes in adult worms. In fortuitous sections of freshly laid eggs, still adhering to the body, the bacteria appear to be just about to enter the egg membrane through deep invaginations. Since we found free bacteria only during egg deposition and the earliest developmental stages, we con- clude that prokaryotic symbionts are re- leased by rupture or, more probably, by lysis of the genital pad adjacent to the oviducal pore. Subsequently, they are transmitted by invasion of the freshly deposited egg. Although some microbiological and zoo- logical details are not yet fully understood, we envisage the following scenario: While in early stages a defense mechanism initially causes intracellular lysis of the bacterial-in- truders, a balance between production of extracellular bacteria and their intracellular digestion becomes established in the grow- ing worms, resulting in a coordinated sym- biotic relationship between these aberrant marine tubificids and chemoautotrophic sulfur bacteria. Acknowledgments As pointed out, this lecture is based on a series of studies performed by a group of colleagues from various institutes and dis- ciplines. I owe sincere thanks for intensive collaboration and stimulating discussions to R. Dawson, now Chesapeake Biological Laboratory, University of Maryland, Sol- omons, Maryland, USA; H. Felbeck, Scripps Institution of Oceanography, La Jolla, Cal- ifornia, USA; H. Jannasch and C. Wirsen, both Woods Hole Oceanographic Institu- tion, Woods Hole, Massachusetts, USA; C. Langheld, G. Liebezeit and C. Schmidt, all University of Hamburg, Hamburg, FRG. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Literature Cited Bassaglia, Y. 1986. Le trophosome d’un Vestimen- tifére. Structure et physiologie d’une symbiose. — Université Paul & Marie Curie, D.E.A. d’O- cénologie Biologique Paris, 42 pp. + 18 pp. of appendices and bibliography + 8 pls. Bosch, C., & P.-P. Grassé. 1984a. Cycle partiel des bactéries chimiautotrophes symbiotiques et leurs rapports avec les bactériocytes chez Riftia pachyptila Jones (Pogonophore Vestimentifére). I. Le trophosome et les bactériocytes. Comptes Rendus de l’Académie des Sciences, Paris 299 (sér. 3):371-376. 1984b. Cycle partiel des bactéries chimiau- totrophes symbiotiques et leurs rapports avec les bactériocytes chez Riftia pachyptila (Pogono- phore Vestimentifére). II. L’évolution des bac- téries symbiotiques et des bactériocytes.— Comptes Rendus de l’Académie des Sciences, Paris 299 (sér. 3):413-419. Cavanaugh, C. M., S. L. Gardiner, M. L. Jones, H. W. Jannasch, & J. B. Waterbury. 1981. Prokary- otic cells in the hydrothermal vent tube worm Riftia pachyptila Jones: Possible chemoauto- trophic symbionts.—Science 213 (4505):340- 34) _ Felbeck,.H., G. Liebezeit, R. Dawson, & O. Giere. 1983. CO, fixation in tissues of marine oligo- chaetes (Phallodrilus leukodermatus and P. planus) containing symbiotic, chemoautotro- phic bacteria.— Marine Biology 75:187-191. Giere, O. 1979. Studies on marine Oligochaeta from Bermuda, with emphasis on new Phallodrilus- species (Tubificidae).— Cahiers de Biologie Ma- rine 20:301-314. — ; H. Felbeck, R. Dawson, & G. Liebezeit. 1984. The gutless oligochaete Phallodrilus leukoder- matus Giere, a tubificid of structural, ecological and physiological relevance.— Hydrobiologia 115:83-89. —,&C. Langheld. 1987. Structural organisation, transfer and biological fate of endosymbiotic bacteria in gutless oligochaetes.— Marine Biol- ogy 93:641-650. — ., G. Liebezeit, & R. Dawson. 1982. Habitat conditions and distribution pattern of the gut- less oligochaete Phallodrilus leukodermatus. — Marine Ecology Progress Series 8:291-299. —., C. O. Wirsen, C. Schmidt, & H. W. Jannasch. 1988. Contrasting effects of sulfide and thio- sulfate on symbiotic CO,-assimilation of Phal- lodrilus leukodermatus (Annelida). — Marine Bi- ology 97:413-419. Liebezeit, G., H. Felbeck, R. Dawson, & O. Giere. 1983. Transepidermal uptake of dissolved car- VOLUME 102, NUMBER 1 bohydrates by the gutless marine oligochaete Phallodrilus leukodermatus (Annelida).— Océanis 9:205-211. Southward, E. C. 1986. Gill symbionts in thyasirid and other bivalve molluscs. — Journal of the Ma- rine Biological Association of the United King- dom 66:889-914. Sprent, J. I. 1979. The biology of nitrogen-fixing or- ganisms. McGraw-Hill Book Company, Lon- don, 196 pp. Steudel, R. 1985. Neue Entwicklungen in der Chemie des Schwefels und des Selens.— Nova Acta Leo- poldina, N.F. 59, No. 264:231-246. 115 —,G. Holdt, T. Gobel, & W. Hazeu. 1987. Chro- matographische Trennung hoherer Polythionate S,0O,2> (n = 3... 22) und deren Nachweis in Kulturen von Thiobacillus ferrooxidans; molek- ulare Zusammensetzung bakterieller Schwefe- lausscheidungen. — Angewandte Chemie 99:143- 146. Zoologisches Institut und Zoologisches Museum, Universitat Hamburg, Martin- Luther-King-Platz 3, D-2000 Hamburg 13, Federal Republic of Germany. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 116-123 REVISION OF THE FAMILY LYSARETIDAE, AND RECOGNITION OF THE FAMILY OENONIDAE KINBERG, 1865 (EUNICIDA: POLYCHAETA) G. Kent Colbath Abstract.— As recognized by previous authors, the family Lysaretidae Kin- berg, 1865 includes genera with dissimilar jaw morphology and composition. Lysaretidae is restricted here to include only Lysarete Kinberg, characterized by jaws mineralized with calcite and relatively short carriers with transverse musculature. Oenone Savigny, Halla Costa and Tainokia Knox & Green are removed into the family Oenonidae Kinberg, 1865. These genera are charac- terized by heavily sclerotized jaws which are not mineralized, and by long carriers with oblique-longitudinal musculature. Hartman (1944) published a family-level revision of the eunicoid polychaetes which was widely accepted. Drawing on the work of Kinberg (1865) and Ehlers (1868), she placed heavy emphasis on the configuration of the jaws as a taxonomic character. Hartman recognized three basic maxil- lary jaw patterns within the superfamily Eu- nicea: the labidognath pattern ascribed to the Eunicidae, Onuphidae, and Lumbriner- idae; the prionognath pattern in the Arabellidae and Lysaretidae; and a third pattern (later named ctenognath by Kielan- Jaworowska 1966) found only in the Dor- villeidae. Labidognath jaws are character- ized by having two relatively short, broad carriers, in contrast to the two long, slender carriers with a ventral median ligament (or “third carrier’’) which characterize priono- gnath jaw apparatuses. In the ctenognath condition the maxillae consist of two to four rows of numerous separate denticles. During a study of the composition and fossilization potential of polychaete jaws, I divided eunicoid jaws into three groups based on their composition (Colbath 1986). Labidognath jaws are mineralized with cal- cium carbonate in the form of aragonite in the Onuphidae and Eunicidae, and calcite in the Lumbrineridae. Labidognath jaws are also weakly sclerotized, and the outer pro- tein wall is readily leached in 2% KOH (Hartmann-Schroder 1967, Colbath 1986). In contrast, prionognath and ctenognath jaws are amorphous to x-rays, do not react with HCl, and are relatively resistant to leaching in KOH (Colbath 1986). The jaws of species of Lysarete Kinberg, 1865 are mineralized with calcite (Colbath 1986), and exhibit other labidognath mor- phological characters. Other genera previ- ously included within the Lysaretidae have jaws of the prionognath type, prompting a revision of the family, and recognition of the family Oenonidae Kinberg, 1865. History of Study Early classifications of the eunicoid poly- chaetes were based exclusively on features of the external anatomy, and produced ar- bitrary groupings of genera which are dis- similar internally (Hartman 1944:1). First to emphasize the importance of jaw parts in classification was Kinberg (1865). Kin- berg recognized ten families which he di- vided into four major groups (labeled in- formally as A-D). He defined group C by the presence of mandibles with separated right and left halves (an ontogenetically variable feature), and included only La- VOLUME 102, NUMBER 1 randa Kinberg, 1865, which was considered unrecognizable by Hartman (1944:10, 1948: 98). Kinberg’s other groups correspond to the labidognath (A), prionognath (B), and ctenognath (D) jaw types presently recog- nized. Kinberg considered the Lysaretae (sic) and Oenonidea (sic) distinct, including the former in group A and the latter in group B. Ehlers (1868:280—282) also emphasized the importance of jaw configuration in clas- sifying these polychaetes, but did not for- malize the distinctions. Instead, he recog- nized a single family Eunicea (sic), which he informally divided into the Eunicea lab- idognatha and Eunicea prionognatha. Eh- lers (1868) did not stress the morphology of maxillary carriers as strongly as did Kin- berg, but rather subdivided the eunicoids according to whether the anterior maxillae are arranged in a semicircle (labidognatha) or in parallel rows (prionognatha). In contrast to Kinberg, Ehlers (1868) placed the genus Lysarete close to Aglau- rides Ehlers (~Oenone Savigny) in the prionognath subdivision. He later (Ehlers 1887:107-108) acknowledged the close similarity between the jaws of Lysarete and those of Lumbriconereis Grube (=Lumbri- neris Blainville), but did not emend his ear- lier taxonomic treatment. Hartman (1944:2) essentially formalized the 1868 scheme of Ehlers using the family- level nomenclature of Kinberg. She retained six of the ten families recognized by Kin- berg, placing the Oenonidae into synonymy with the Lysaretidae. Fauchald (1970:118) removed Iphitime Marenzeller from the Lysaretidae, and erected the family Iphitimidae. He later (Fauchald 1977) erected the order Eunicida to include the seven families within the su- perfamily Eunicea, plus two additional fam- ilies (Histriobdellidae, Ichthyotomidae) which were not assigned to a superfamily. Materials and Methods All lysaretids in the collection of the U.S. Museum of Natural History (USNM) were | GF examined for the present study, and selected specimens were dissected for examination of the jaws. Additional specimens of Ly- sarete were obtained on loan from the Flor- ida Department of Natural Resources (FSBC). The holotype of L. brasiliensis Kin- berg, 1865 was obtained from the Swedish National Museum, Stockholm. One specimen of Lysarete brasiliensis with jaws in excellent condition (USNM 55884) was used for the chemical and mineralogical analyses, and for scanning electron micros- copy. The maxillary apparatus was re- moved, dehydrated in an alcohol series, and prepared for SEM by critical point drying. The specimen was initially coated with car- bon only, and chemically analyzed using x-ray dispersion. The specimen was then coated with gold palladium for routine scan- ning electron microscopy. The mandibles were removed, photographed with a Wild 400 wide-field optical microscope, and ana- lyzed with the Gandalfi x-ray spectrometer in the Department of Mineralogy, Smith- sonian Institution. Taxonomic Characters Jaw morphology and composition. — X-ray dispersion analysis of the maxillae of Ly- sarete brasiliensis indicates the presence of abundant calcium carbonate. The mandi- bles are mineralized with calcite, as are jaws in the lumbrinerids (Colbath 1986). Calci- fication is also evident in L. australiensis Benham, 1915, in that the blades of the mandibles are white, and the maxillae are dark brown rather than black. The presence of calcite is inferred by comparison with L. brasiliensis. In contrast to Lysarete, jaws in species of Oenone Savigny, Halla Costa and Tainokia Knox & Green (commonly included in the Lysaretidae) are not mineralized, but rather are composed almost exclusively of sclero- protein. As a consequence, both maxillae and mandibles are jet black in color. The distinction between heavily sclerotized and calcified jaws is apparent upon inspection, 118 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON and was described by Benham (1915:233, 236-237). Benham made no comment about the utility of this distinction above the species level, however. Other aspects of jaw morphology are cor- related with the difference in mineraliza- tion. In Lysarete the maxillary carriers are relatively short (approximately equal to the length of the maxillae) and broad (Fig. 1b), with no ventral ligament (=“‘third carrier’). A thick band of transverse muscles joins the carriers dorsally (Fig. 2f), allowing them to be pulled closed in the “trap”? motion de- scribed by Wolf (1980) for other labido- gnath jaws. The MI (maxilla I) elements in the maxillary apparatus are the same length (Fig. 2c), which allows the anterior tips to come together in a pincer-like fashion as part of the trap motion. The posterior dorsal surfaces of the MIs exhibit an interlocking ridge and furrow system (Fig. 2e), which may help to lock the apparatus in a closed position (Wolf 1980). In species of Oenone, Halla and Tainokia the carriers are narrow and much longer than the combined length of the maxillae, and are not equiped with a transverse muscle band. Instead, a series of long, oblique-lon- gitudinal muscles are attached along the length of the carriers. A ventral ligament is present. The right and left MI elements may be of different lengths (Crossland 1924; Hartman 1944; Kielan-Jaworowska 1966), and no basal ridge and furrow system is present to lock the jaws in a closed position. Such jaws are presumably incapable of per- forming a trap motion, as Wolf (1980) also concluded for the arabellids. Soft-part morphology.—The genera tra- ditionally included within the Lysaretidae share an elongated post-setal lobe and prominent dorsal cirrus on posterior para- podia. The morphology of the head, how- ever, is distinctly different in each of the four genera under discussion. Although the difference between Lysarete and the other genera may not merit consideration as a family-level character, the anterior mor- phology is none-the-less a useful key char- acter. In Lysarete, three antennae emerge from the posterior margin of the prostomium, and may lie flat in a V-shaped notch (Fig. 1a). In adult specimens the notch extends pos- teriorly across the peristomial rings, and in some cases across the first one or two seti- gers. Halla has three antennae which may lie back in a semicircular notch in the two peristomial rings (Fig. le). Tainokia has a single antennae, and a slight invagination which extends posteriorly only partially across the first of two peristomial rings (Knox & Green 1972, fig. 1). In Oenone, three antennae are tucked into a nuchal fold (Fig. 1d), no notch is present, and dorsally the peristomium has only one distinct ring. Setae and acicula.—All of the worms considered here have simple geniculate se- tae. In addition, bifid hooks have been re- ported in Oenone and Halla. In Lysarete, Oenone, and Tainokia the geniculate setae are smooth (Knox & Green 1972, figs. 6, 7; pers. observ.). In Halla, however, the dorsal setae are denticulate, and the ventral setae are marked by distinctive oblique striae (Fig. 2a, b; Fauvel 1923:427, fig. 169 g, h). Both described species of Lysarete have black acicula. In Oenone fulgida (Savigny, 1818) and Halla parthenopeia (Chiaje, 1828) the acicula are amber, while Knox & Green (1972:433) described the acicula in Taino- kia iridescens as colorless. Black acicula are thus useful for distinguishing Lysarete from the other three genera, supporting the fam- ily-level distinction based on jaw morphol- ogy. Systematics Order Eunicida Fauchald, 1977 Family Lysaretidae Kinberg, 1865 Emended diagnosis. —Eunicoid poly- chaetes with jaws mineralized with calcite. Mandibles flat with semicircular growth rings anteriorly (Fig. 2d). Maxillary carriers no longer than combined length of maxillae, VOLUME 102, NUMBER 1 119 Fig. 1. a-c, Lysarete brasiliensis, holotype, Brazil; a, Dorsal view, anterior end, illustrating V-shaped notch in peristomium; b, Dorsal view, MI elements and carriers, muscle attachment stippled; c, Labial view, MIIL- MVL. d, Oenone fulgida, USNM 17729, Dry Tortugas, dorsal view, anterior end, note tips of antennae protruding from nuchal fold. e, Halla parthenopeia, USNM 5147, Bay of Naples, dorsal view, anterior end, note semicircular notch in peristomium. All scale bars = 1 mm. articulated by prominent transverse mus- cular bundle, no ventral ligament. Maxillary jaws symmetrical. MI elements of identical length, distally falcate with prominent sec- ondary fang, additional small denticles may be present at base. Three short antennae arise from base of prostomium. Elongate post-setal lobe and flattened dorsal cirrus (or notopodium) developed in posterior parapodia. Simple geniculate setae present, bifid hooks absent. Comparison.—The Lysaretidae are dis- tinguished from the Oenonidae based on jaw morphology and mineralogy. Lysarete, the only genus presently recognized within the family, is further distinguished from the Oenonidae in having black acicula, and a V-shaped notch in the dorsal surface of the peristomium. The Lysaretidae are similar to the Lum- brineridae in having: 1) jaws mineralized with calcite; 2) flat mandibles with a semi- circular blade; 3) symmetrical maxillary jaws; 4) transverse musculature on the car- riers. The Lysaretidae are distinguished from the Lumbrineridae by: 1) well-developed PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. a, b, Halla parthenopeia, USNM 5147, Bay of Naples; a, SEM dentate setae from dorsal bundle, posterior parapodium, scale bar = 10 um; b, SEM striate setae from ventral bundle, scale bar = 50 um. c-g, Lysarete brasiliensis, USNM 55884, Gulf of Mexico; c, SEM maxillary apparatus, dorsal view, scale bar = 1 mm; d, Light photomicrograph mandibles, ventral view, scale bar = 1 mm; e, SEM MI elements, oblique-lateral view, note ridges and grooves on bases of MIs, scale bar = 0.5 mm; f, SEM carriers, oblique-lateral view, carriers canted at an angle to MIs, note transverse muscle band, scale bar = 0.2 mm; g, SEM anterior maxillary jaws, oblique-lateral view, scale bar = 0.2 mm. dorsal cirri; 2) a prominent secondary fang on the MI elements of the maxillae; 3) the absence of hooded hooks. Kuwaita Moham- mad, 1973 is intermediate between the Ly- saretidae and Lumbrineridae in having an- tennae on the prostomium, but clearly belongs in the Lumbrineridae based on the 3 criteria above (Mohammad 1973:34, 36, figs. 6, 7). Distribution.—Lysarete includes one VOLUME 102, NUMBER 1 species recorded from the east coast of North and South America in low latitudes, and a second species from a single locality east of Australia. Larymna Kinberg, 1865 may also belong in the Lysaretidae based on jaw mor- phology (Hartman 1948:99). The type and only specimen (from Mozambique) is so poorly preserved that, according to Hart- man, attribution cannot be made below the family level, and Larymna should be re- garded as unrecognizable. Genus Lysarete Kinberg, 1865 Type species.—L. brasiliensis Kinberg, 1865:570. Lysarete brasiliensis Kinberg, 1865 Figs. la—c, 2c-g Lysarete brasiliensis Kinberg 1865:570; 1910:49, pl. 17, fig. 30.—Ehlers 1887:107- 108, pl. 33, figs. 1-8.—Rioja 1944:130- 131, figs. 47-50.—Hartman 1951:65, pl. 14, figs. 7, 8.—Orensanz 1975:106-108, fig. 8.— Gardiner 1976:213, figs. 29b-e. — Gilbert 1984:43-6—43-7, figs. 43-3, 43-4. ?Oenone brevimaxillata. —Treadwell 1931: 1-3, figs. 4-8. Remarks.—In her re-appraisal of Kin- berg’s type material, Hartman (1948:8) did not consider the holotype of Lysarete bra- siliensis, but instead referred to an earlier revision by Ehlers (1887:107-108, pl. 33). Ehlers did not figure the Brazilian type of L. brasiliensis, but rather figured a specimen collected from Florida. The posthumous publication of Kinberg’s plates (Kinberg 1910) did not include illustrations of the jaws of the holotype. The maxillae are there- fore illustrated here (Fig. 1b, c). On the holotype, maxillary jaws III and IV each have a prominent anterior denticle, with two progressively smaller denticles posteriorly. The jaws in a specimen from Argentina (Rioja 1944, fig. 50) are similar, except that the MIII elements have four denticles instead of three. Most specimens examined from the east 121 coast of the United States have five to six denticles on the MIII and four to seven den- ticles on the MIV elements (Fig. 2g). The anterior three denticles on the MIII element are sub-equal in length, unlike those of the type. One specimen from Florida (FSBC I 31008) has MIII jaws like the type, how- ever, and a specimen from Argentina illus- trated by Orensanz (1975, fig. 8-3) has MIIIs and IVs indistinguishable from most of the North American specimens. There is thus some overlap in jaw morphology between the North and South American populations. The number and shape of denticles on an- terior jaws is variable in eunicoid poly- chaetes, and the two populations are ten- tatively considered conspecific in spite of their disjunct geographic ranges. The type and only specimen of Oenone brevimaxillata Treadwell, 1931 was never deposited (H. S. Feinberg, AMNH, pers. comm. 1985), and is presumed lost. Tread- well’s (1931, fig. 8) illustration of the max- illae 1s schematic, and insufficient for de- tailed comparison. Family Oenonidae Kinberg, 1865 Emended diagnosis. —Jaws jet black, composed primarily of scleroprotein, no crystalline mineral phases present. Mandi- bles H-shaped. Maxillary carriers much longer than anterior jaws, attached to bun- dles of oblique-longitudinal muscles, ven- tral ligament present. Maxillae commonly asymmetrical, MIs differ slightly to mark- edly in length. One or three antennae arise from base of prostomium. Elongate post- setal lobe and prominent dorsal cirri de- veloped on posterior parapodia. Geniculate setae present, bifid hooks present or absent. Key to the genera of Oenonidae la. One or 3 antennae recline in notch in peristomium, 2 peristomial rings dorsally, bifid hooks present or ab- sent lb. Three antennae tucked into nuchal 122 fold, 1 peristomial ring dorsally, bifid hooks present. 424.222 -: Oenone 2a. One antenna, peristomial notch weakly developed, bifid hooks ab- sent, setae smooth Tainokia 2b. Three antennae, distinct semicir- cular peristomial notch, bifid hooks present (small individuals only), dorsal setae dentate, ventral setae SUGIALCE toot aes 2s Re eR he Halla o) = @ e je @ = © Genus Halla A. Costa, 1844 Type species.—Halla_ parthenopeia (Chiaje) Costa, 1844:63.—Lysidice parthe- nopeia Chiaje, 1828:175. Remarks. —Fauvel (1923:427, fig. 169f) described Halla parthenopeia as having bi- fid hooks, in addition to the setae figured here (Fig. 2a, b). Hooks are absent in para- podia from the large specimen of H. par- thenopeia examined here (USNM 5147), nor were hooks recorded from the large speci- men figured by Ehlers (1868:28, figs. 27, 28). The type of Halla okudai Imajima (1967:437) is also a large worm, and lacks hooks (Imajima & Hartman 1964:267-—268). Individuals of Halla which attain large size may lose their bifid hooks. A similar con- dition prevails in several large species with- in the Eunicidae (K. Fauchald, pers. comm. 1985). Distribution. — All western hemisphere specimens deposited in the USNM collec- tion as Halla proved to be misidentified members of Oenone or Lysarete. Halla may be restricted to the Old World, with docu- mented reports from the Mediterranean (Fauvel 1923) and Japan (Imajima 1967). Acknowledgments I thank Kristian Fauchald for extensive discussions about the taxonomy of eunicoid polychaetes, and for critically reading the manuscript. Thomas H. Perkins arranged the loan of material from the Florida De- partment of Natural Resources. H. S. Fein- berg, American Museum of Natural His- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON tory, provided information concerning the type of Oenone brevimaxillata Treadwell. This research was supported by a post-doc- toral fellowship, Smithsonian Institution. Literature Cited Benham, W. B. 1915. Report on the Polychaeta ob- tained by the F. I. S. “Endeavour” on the coasts of New South Wales, Victoria, Tasmania and South Australia, part I.—Biological Results of the Fishing Experiments carried on by the F. I. S. “Endeavour,” 1909-14:173-273. Chiaje, S. delle. 1828. Memorie sulla storia a notomia degli animali senza vertebre del regno di Napoli, 3. Napoli, 232 pp. Colbath, G. K. 1986. Jaw mineralogy in eunicean polychaetes (Annelida).— Micropaleontology 32: 186-189. Costa, A. 1844. Cerni intorno alle osservazioni zool- ogiche fatte durante intre mesi vernali del 1844.—Annales Accademia aspirantes Natu- rales Napoli 2:40-68. Crossland, C. 1924. Polychaeta of tropical East Af- rica, the Red Sea and Cape Verde Islands. The Lumbriconereidae and Staurocephalidae. — Proceedings of the Zoological Society of London 1924:1-106. Ehlers, E. 1864-1868. Die Bornstenwiirmer (Anne- lida, Chaetopoda). Leipzig, 748 pp. 1887. Reports on the results of dredging in the U.S. Coast steamer “Blake.” XX XI. Report on the annelids.—Memoirs of the Museum of Comparative Zoology, Harvard 15:1-335. Fauchald, K. 1970. Polychaetous annelids of the fam- ilies Eunicidae, Lumbrineridae, Iphitimidae, Arabellidae, Lysaretidae and Dorvilleidae from western Mexico.— Allan Hancock Monographs in Marine Biology 5:1-335. . 1977. The polychaete worms.— Natural His- tory Museum of Los Angeles, Science Series 28: 1-188. Fauvel, P. 1923. Faune de France 5, polychetes er- rantes.—Office Central de Faunistique, Paris, 488 pp. Gardiner, S. L. 1976. Errant polychaete annelids from North Carolina. — Journal of the Elisha Mitchell Scientific Society 91:77—220. Gilbert, K. M. 1984. Family Lysaretidae Kinberg, 1865. Pp. 43-1-43-7 in J. M. Uebelacker & P. G. Johnson, eds., Taxonomic guide to the poly- chaetes of the Northern Gulf of Mexico, Volume 6. Barry A. Vittor and Associates, Mobile, Al- abama. Hartman, O. 1944. Polychaetous annelids. Part V. Eunicea.— Allan Hancock Pacific Expedition 10: 1-339. VOLUME 102, NUMBER 1 1948. The marine annelids erected by Kin- berg, with notes on some other types in the Swedish State Museum.—Arkiv For Zoologi 42A:1-137. . 1951. The littoral marine annelids of the Gulf of Mexico.—Publications of the Institute for Marine Science, University of Texas 2:7-124. Hartmann-Schroder, G. 1967. Feinbau und Funktion des Kieferapparates der Euniciden am Beispiel von Eunice (Palola) siciliensis Grube (Poly- chaeta).— Mitteilungen aus dem Hamburg Zool- ogischen Museum und Institut 64:5—27. Imajima,M. 1967. Errant polychaetousannelids from Tsukumo Bay and vicinity of Noto Peninsula, Japan.— Bulletin of the National Science Mu- seum, Tokyo 10:403-441. , & O. Hartman. 1964. The polychaetous an- nelids of Japan.—Allan Hancock Foundation Occasional Papers 26:1-452. Kielan-Jaworowska, Z. 1966. Polychaete jaw appa- ratuses from the Ordovician and Silurian of Po- land and a comparison with modern forms.— Paleontologica Polonica 16:1—152. Kinberg, J. G. H. 1865. Annulata nova.—Ofversigt af Svenska Kongliga Vetenskaps-Akademiens Forhandlingar 21:559-574. 1910. Kongliga Svenska Fregatten Eugenies 123 Resa omkrig jorden. Vetenskapliga Iakttagelser. II. Zoologi. 3. Annulater, Uppsala, 78 pp. Knox, G. A., & K. M. Green. 1972. The polychaetes of New Zealand part 3: Lysaretidae.— Journal of the Royal Society of New Zealand 2:43 1-434. Mohammad, M.-B. 1973. New species and records of polychaete annelids from Kuwait, Arabian Gulf. — Zoological Journal of the Linnean So- ciety 52:23-44. Orensanz, J. M. 1975. Los anelidos poliquetos de la provincia biogeographica Argentina. VII. Eu- nicidae y Lysaretidae.— Physis 34:85-111. Rioja, E. 1944. Estudios anelidologicos. X. Estudio de algunos poliquetos del Museo Argentino de Ciencias Naturales.—Anales del Instituto de Biologia, México 15:115-138. Treadwell, A. L. 1931. New species of polychaetous annelids from California, Mexico, Puerto Rico, and Jamaica.—American Museum Novitates (N.Y.) 1023:1-7. Wolf, G. 1980. Morphologische Untersuchungen an den Kieferapparaten einiger rezenter und fos- siler Eunicoidea (Polychaeta). —Senckenber- giana Maritima 12:1—182. 2195 Deborah Way, Upland, California 91786, USA. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 124-130 REDESCRIPTION OF NEPHTYS SQUAMOSA EHLERS (POLYCHAETA: NEPHTYIDAE) Takashi Ohwada Abstract. —Confusion about the identity of Nephtys squamosa Ehlers, 1887 requires redescription of the species based on the syntypes. A lectotype is designated. Comparisons are made with similar species. Nephtys squamosa was originally de- scribed by Ehlers (1887) as having scale-like structures on both dorsum and ventrum, a character unique to the family Nephtyidae. Many subsequent authors have described N. squamosa on the basis of specimens from temperate and tropical waters of the Atlan- tic and the East Pacific (Augener 1918; Monro 1933; Fauvel 1936; Hartman 1940, 1950; Pettibone 1963; Nonato & Luna 1970; Fauchald 1972, 1976; Gardiner 1976; Tay- lor 1984; Lana 1986). Although all agree on the presence of the scale-like lamellae, dis- crepancies exist among descriptions in the parapodial morphology. None of these de- scriptions after that of Augener (1918) men- tioned the presence of infrapreacicular la- mellae on neuropodia, which is clearly stated in the original description (Ehlers 1887). Types of N. squamosa have been exam- ined in the present study to clarify its iden- tity. The presence of infrapreacicular la- mellae has been confirmed on neuropodia, and suprapreacicular lamellae have been also found on notopodia. The present exami- nation has further shown the presence of tiny, slender dorsal cirri on the first noto- podia, overlooked by previous workers. Nephtys squamosa Ehlers, 1887 Figs. 1-3 Nephthys squamosa Ehlers, 1887:128-131, pl. 37, figs. 7-10. Material examined. — Original specimens collected from Florida during the U.S. Coast Survey 1868-1869, L. F. Pourtales, assist.: off French Reef, Cast No. 6, 103 fms, 3 Apr 1869, paralectotype (MCZ 735).—off French Reef, Cast No. 4, 50 fms, 3 Apr 1869, para- lectotype (MCZ 740).—off Alligator Reef, Cast No. 9, 113 fms, 8 May 1869, paralec- totype (MCZ 836).—off American Shoal, 55 fms, lectotype (MCZ 1202). Measurements. —Lectotype complete, 48.4 mm long, 3.4 mm wide including para- podia with 120 setigers. Paralectotypes (MCZ 735, 740, 836) incomplete posterior- ly, respectively, 21.7 mm long, 3.5 mm wide with 47 setigers, 54.4 mm long, 2.9 mm wide with 105 setigers, 30.7 mm long, 2.4 mm wide with 96 setigers. Description. —Body creamy white to brown, lacking pigmentation in alcohol. Eyes absent. Prostomium pentagonal with anterior margin convex, thin, spatulate (Fig. la, b); lateral margins rounded, broadest between second antennae (Fig. 2a), posterior margin with V-shaped middorsal projection ex- tending to posterior border of setiger 1. An- terior part between first antennae translu- cent, marked by an intricate pattern of opaque tissue (Figs. 1b, 2a). First antennae small, flattened, attached obliquely, ap- pearing as raised lobes originating some dis- tance from and fused with frontal prosto- mial margin (Figs. 1b, 2a). Second antennae large, basally flattened and distally conical, slightly constricted at bases, much larger than lst antennae, directed laterally at mid- dle of ventral surface of prostomium, well VOLUME 102, NUMBER 1 125 a @' = i Soe O QR * = PANNE RE PAT Hy cana lL : | Fig. 1. Nephtys squamosa (setae omitted): a, c, d, lectotype (MCZ 1202), b, paralectotype (MCZ 735): a, Anterior end, dorsal view, ventrally dissected and somewhat flattened, dorsal cirrus missing and preacicular lobe twisted outside on Ist right notopodium (acL~acicular lobe; prL—preacicular lobe); b, Same, ventral view, 3rd right ventral cirrus missing (notopodia omitted); c, 72nd to 76th setiger, dorsal view (neuropodia omitted); d, 74th to 78th setiger, ventral view (notopodia omitted). behind Ist antennae and slightly anterior to podia reduced, with triangularly pointed Ist neuropodia (Figs. la, b; 2a, b). Mouth acicular lobes, short preacicular and post- covered with two thick lateral lips and thick acicular lobes (preacicular lobes concealed rugose midventral lip at level of setiger 1 behind acicular lobes and usually not rec- (Fig. 1b); rugose area extending to setiger 5. ognizable from above); dorsal cirri (barely Setiger 1 modified (Figs. la, 2b); noto- visible unless stained) tiny, slender, point- 126 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Nephtys squamosa: a, c, paralectotype (MCZ 735), b, lectotype (MCZ 1202): a, Anterior half of prostomium, dorsal view (setae omitted); b, Ist left parapodium, dorsal view, preacicular lobe obscured by acicular lobe (acL—acicular lobe; dc—-dorsal cirrus; tips of setae omitted); c, 12th right neuropodium, dorsal view (setae omitted). ed, arising from outer side of acicular lobes near their base between preacicular and postacicular setal fascicles (Fig. 2b). Neu- ropodia of setiger 1 on anterior margin, lat- eral to prostomium, with slender rudimen- tary acicular lobes projecting anteriorly (Figs. la, 2b); acicular lobes supported by thin acicula whose tip curves inward. Ven- tral cirri large, similar to or smaller than 2nd antennae, digitate but tips may be con- ical, lateral to neuropodia and continuous with anterior setigerous margins, directed laterally or bent backward (Figs. la, 2b). Notosetae of setiger 1 including preacicular barred (laddered) capillaries and very finely serrated slender postacicular capillaries; neurosetae long, thin, smooth capillaries, surrounding acicular lobes (Fig. 2b). Parapodia similar throughout from se- tiger 2; both rami with preacicular and post- acicular setal fascicles; branchiae (interra- mal cirri) may be lacking on setiger 2. Both notopodial and neuropodial acicular lobes conical (Fig. 3a—c), becoming acutely coni- cal and pointed posteriorly (Fig. 3e). No- topodial presetal lamellae thin, rather broad and slightly bilobed, distally rounded, ex- tending from lower margins of notopodia, as long as acicular lobes on anterior para- podia (Fig. 3a—c), posteriorly reduced and much shorter than acicular lobes (Fig. 3e). Small lamellae dorsal to notopodial presetal lobes, thinner than presetal lobes except on middle parapodia, rounded on anterior no- topodia (Fig. 3a, b), posteriorly reduced and becoming much thinner and smaller (Fig. 3c, e), barely recognizable on posterior se- tigers (Fig. 3e). Preacicular setae appearing mostly beyond dorsal margins of presetal lamellae and usually partially covering small suprapreacicular lamellae (Fig. 3a—c, e). Neuropodial presetal lamellae thin, larger than notopodial presetal lamellae, extend- ing from upper margins of neuropodia rath- er triangularly on middle parapodia (Fig. 3b, c), distally rounded on all but especially on anterior and posterior parapodia (Fig. 3a, e), as long as acicular lobes on anterior VOLUME 102, NUMBER 1 127 Fig. 3. Nephtys squamosa (tips of setae omitted): a, b, paralectotype (MCZ 735), c-e, lectotype (MCZ 1202): a, Left parapodium, setiger 6, anterior view; b, Same, setiger 32, anterior view; c, Same, setiger 40, anterior view; d, Same, posterior view (preacicular setae omitted); e, Right parapodium, setiger 79, anterior view. neuropodia (Fig. 3a, b), posteriorly reduced and much shorter than acicular lobes (Fig. 3e). Lamellae ventral to neuropodial pre- setal lobes, broad, thin, shorter than presetal lobes, slightly bilobed on anterior parapodia (Fig. 3a, b), posteriorly reduced and becom- ing narrower and much thinner, thinner than presetal lobes, hardly recognizable on pos- terior setigers (Fig. 3e). Preacicular setae ap- pearing mainly beyond ventral margins of 128 presetal lamellae and usually partially cov- ering infrapreacicular lamellae (Fig. 3a-c, e). Notopodial postsetal lamellae thin, lig- ulate, extending dorsolaterally from seg- mental wall above and longer than acicular lobes, distally rather rounded on anterior setigers (Fig. 3a), posteriorly becoming more or less pointed (Fig. 3b—e). Neuropodial postsetal lamellae large, thin, extending from behind and longer than acicular lobes (Fig. 3a-e), posteriorly extending much further (Fig. 3c, e), but degree of extension variable between specimens (Fig. 3b, c), with rather pointed tips except on anterior parapodia where distally rounded (Fig. 3a). Small, short lobe on superior edge of neuropodia be- tween presetal and postsetal lamellae (Figs. 2c, 3a, d, e) except on setiger 1, distinct on anterior neuropodia but posteriorly reduced and barely recognizable. Dorsal cirri flat- tened, thin, triangularly elongate with rather pointed tips, smaller than notopodial post- setal lamellae, extending laterally from bas- al part of branchiae behind acicular lobes (Fig. 3a—e). Ventral cirri digitiform on an- terior several parapodia (Figs. 1b, 3a), thereafter foliaceous, constricted at bases (Figs. 1b, 3b-d). Branchiae first present on setigers 2-3 usually as processes slightly curved out- ward, completely recurved within a few se- tigers (Fig. 3a), thereafter gradually increas- ing in size and fully developed by setigers 25-27 (Fig. 3c-e), then (in lectotype) de- creasing gradually in size after setigers 89- 92, and not recurved after setigers 106-107, still present as very small rudimentary ridge on setiger 116, completely absent on last 4 setigers. Scale-like dorsal lamellae broad, folia- ceous (Fig. Ic), originating from dorsolat- eral wall of body (Fig. 3b-e), extending mainly posterolaterally over notopodia, partially overlapping successive segments in shingle-like arrangement (Fig. lc), begin- ning on setigers 5-9, becoming larger more posteriorly but not fully developed until PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON middle setigers (Fig. 3c, d), gradually de- creasing in size (in lectotype) over posterior several setigers but still recognizable on se- tiger 117, absent on last 3 setigers. Similar but much smaller lamellae present on ven- trolateral surface of body (Figs. 1d, 3c, d), foliaceous, extending somewhat postero- laterally, only slightly covering neuropodia and successive segments (Fig. 1d), begin- ning on setiger 2, increasing in size more posteriorly but not fully developed until middle setigers (Fig. 3c, d), gradually re- duced (in lectotype) over posterior several setigers but still recognizable on setiger 117, absent on last 3 setigers. Both preacicular and postacicular setae occurring in spreading fascicles, with post- acicular fascicles wider than preacicular ones (Fig. 3a—c, e); preacicular setae much shorter and fewer than postacicular setae. Most preacicular setae consisting of barred cap- illaries; a few, similarly long, very finely ser- rated capillaries at upper and lower end of preacicular fascicles. Postacicular setae con- sisting of finely serrated long capillaries. No lyrate seta found. Acicula single in rami, completely embedded in conical acicular lobes (Fig. 3b-e). Proboscis not everted in specimens ex- amined. Proboscis in lectotype previously dissected, damaged, incomplete, with ter- minal circlet of 20 bifid papillae and simple middorsal papilla, with at least 20 rows of 5-6 cirriform papillae subterminally, and more distal cirriform middorsal papilla; middorsal papilla not noticeably larger nor longer than others. Pair of horny jaws pres- ent inside proboscis. Pharyngeal trepans ab- sent. Remarks.—In the original description, Ehlers (1887:130) stated that dorsal cirri were about half as long as notopodial post- setal lamellae. This is the case in the middle parapodia of the lectotype (Fig. 3c, d). In two paralectotypes (MCZ 735, 836), how- ever, notopodial postsetal lamellae do not extend beyond dorsal cirri (Fig. 3a, b). The VOLUME 102, NUMBER 1 relative length of notopodial postsetal la- mellae to dorsal cirri is thought to vary greatly between specimens. There are obvious problems with descrip- tions of Nephtys squamosa. Although the presence of suprapreacicular lamellae on notopodia has been clearly recognized in the lectotype and paralectotypes in the present study, neither the original description (Eh- lers 1887) nor any subsequent description mentioned this structure, whereas Ehlers described infrapreacicular lamellae on neu- ropodia (p. 130, Taf. 37, fig. 8). Examina- tion of the lectotype and paralectotypes also revealed some other structures such as tiny, slender dorsal cirri on Ist notopodia and small, short lobes on the superior edge of neuropodia between presetal and postsetal lamellae, which had been overlooked by previous workers. Descriptions subsequent to Augener (1918) did not mention the presence of in- frapreacicular lamellae on neuropodia. Hartman’s figure (1940: pl. 41, fig. 98) of the 25th parapodium of N. sguamosa from the Gulf of California showed only preacic- ular lamellae both on the notopodium and the neuropodium, and she stated (p. 237) that the prostomium of her specimens dif- fered from that originally described for the species. Neither is an additional preacicular lamella shown on either the notopodium or the neuropodium in Taylor’s figure (1984: fig. 35-8b) of the 20th parapodium of N. squamosa from the Gulf of Mexico. Taylor also stated (p. 11) that dorsal cirri were lack- ing on the Ist notopodia of his specimens, whereas dorsal cirri, although tiny and slen- der, are present on Ist notopodia of the lec- totype and paralectotypes. Additional pre- acicular lamellae are neither described nor figured also in Lana’s description (1986:139, figs. 4, 5) of N. squamosa from Brazil. Since additional preacicular lamellae, especially suprapreacicular lamellae on notopodia, are difficult to observe in some specimens, the lack of description may not necessarily im- 129 ply absence in specimens concerned. Never- theless, it seems to be necessary to reex- amine these specimens for certain identification. Nephtys squamosa is closely related to N. acrochaeta Hartman, 1950, N. imbricata Grube, 1857 and N. serratifolia Ehlers, 1897 in the possession of scale-like dorsal la- mellae. Nephtys squamosa, however, differs from N. acrochaeta in that branchiae are present from setigers 2—3 in the former and 9-10 (Hartman 1950, Fauchald 1976) in the latter. Neuropodial postsetal lamellae are lacinated in N. acrochaeta (Hartman 1950) and N. serratifolia (Ehlers 1897), whereas they are entire in N. squamosa. Capillary setae with a large spur are present in post- acicular fascicles both in N. acrochaeta (Hartman 1950) and N. serratifolia (Hart- man-Schroder 1965), but absent in N. squa- mosa. Nephtys imbricata is ‘too incomplete- ly known for certain identification’ (Hartman 1950:111), but according to the original description (Ehlers 1887), N. squa- mosa differs from N. imbricata in parapo- dial morphology. I have examined types of both species, however further study will be needed to fully characterize N. imbricata. Acknowledgments I am grateful to Dr. Ardis B. Johnston, Museum of Comparative Zoology, Harvard University (MCZ) for the loan of the spec- imens. The manuscript benefited from the helpful suggestions by Dr. Mary E. Petersen, Zoological Museum, University of Copen- hagen, Denmark and the critical review by Dr. Thomas H. Perkins, Florida Depart- ment of Natural Resources. Literature Cited Augener, H. 1918. Polychaeta.—Beitrage zur Kennt- nis des Meeresfauna West-Afrikas 2:67-625, 6 pls. Ehlers, E. 1887. Report on the annelids of the dredg- ing expedition of the U.S. coast survey steamer Blake.—Memoirs of the Museum of Compar- 130 ative Zoology of Harvard College 15:vi + 335 pp., 60 pls. 1897. Polychaeten.—Hamburger Magalla- nische Sammelreise. Hamburg, Friedrichsen & Co. 148 pp., 9 pls. Fauchald, K. 1972. Benthic polychaetous annelids from deep water off western Mexico and adja- cent areas in the eastern Pacific Ocean.— Allan Hancock Monographs in Marine Biology No. 7: 1-575. 1976. Some Nephtyidae (Polychaeta) from Ubatuba, Brasil.— Bulletin of the Southern Cal- ifornia Academy of Sciences 75:16-19. Fauvel, P. 1936. Contribution a la fauna des Anné- lides polychétes du Moroc. — Mémoires de la So- ciété des Sciences Naturelles du Moroc 43:1- 143. Gardiner, S. L. 1976. Errant polychaete annelids from North Carolina. — Journal of the Elisha Mitchell Scientific Society 91:77—220. Grube, E. 1857. Annulata Orstediana Enumeratio Annulatorum, quae in itinere per Indiam occi- dentalem et Americam centralem annis 1845- 1848 suscepto legit cl. A. S. Orsted, adjectis spe- ciebus nonnullis a cl. H. Kréyero in itinere ad Americam meridionalem collectis.— Videnska- belige Meddelelser fra Dansk naturhistorisk Forening i Kjgbenhavn 1857:1-29. Hartman, O. 1940. Polychaetous annelids. Part 2. Chrysopetalidae to Goniadidae.—Allan Han- cock Pacific Expeditions 7:173-—287. 1950. Polychaetous annelids. Goniadidae, Glyceridae, Nephtyidae.—Allan Hancock Pa- cific Expeditions 15:1-181. Hartmann-Schroder, G. 1965. Zur Kenntnis des Sub- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON litorals der chilenischen Kiiste unter besonderer Beriicksichtigung der Polychaeten und Ostra- coden. Teil II. Die Polychaeten des Sublito- rals.— Mitteilungen aus dem Hamburgischen Zoologischen Museum und Institut 62 (Supple- ment):59-305. Lana, P.C. 1986. Nephtyidae (Annelida; Polychaeta) do litoral do estado do Parana (Brazil). — Neri- tica 1:135-154. Monro, C. C. A. 1933. The Polychaeta Errantia col- lected by Dr. C. Crossland at Colon, in the Pan- ama region, and the Galapagos Islands during the expedition of the S. Y. ‘St. George’.— Pro- ceeding of the Zoological Society of London 1933:1-96. Nonato, E. F., & J. A. C. Luna. 1970. Anelideos poliquetas do nordeste do Brasil. 1. Poliquetas bent6nicos da costa de Alagoas e Sergipe.— Boletim do Instituto Oceanografico, Sao Paulo 19:57-130. Pettibone, M. H. 1963. Marine polychaete worms of the New England Region. 1. Aphroditidae through Trochochaetidae.— United States Na- tional Museum Bulletin No. 227:1-356. Taylor, J. L. 1984. Family Nephtyidae Grube, 1850. Pp. 1-20 in J. M. Uebelacker & P. G. Johnson, eds., Taxonomic guide to the polychaetes of the Northern Gulf of Mexico, Vol. 5, Chapt. 35. Barry A. Vittor & Associates, Inc., Mobile, Al- abama. Ocean Research Institute, University of Tokyo, 15-1, 1-Chome, Minamidai, Na- kano-ku, Tokyo 164 Japan. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 131-133 PHALLODRILUS HESSLERI, NEW SPECIES (OLIGOCHAETA: TUBIFICIDAE), FROM ABYSSAL DEPTHS IN THE WESTERN PACIFIC OCEAN Christer Erséus Abstract.—Phallodrilus hessleri is described from abyssal clay at 5916 m depth east of the Philippines. It is characterized by (1) slender, sharply pointed somatic setae with very thin (or absent?) upper teeth, (2) somewhat sigmoid penial setae in segment XI, 2 per bundle, and (3) very small, spindle-shaped atria. The species represents the second deepest record of marine oligochaetes in the world. In a collection of benthic invertebrates from a deep-sea area near the Philippine Trench in the western Pacific Ocean, de- posited in the National Museum of Natural History (USNM), Washington, D.C., the author found one well preserved individual of a new species of Phallodrilus Pierantoni, 1902 from a station almost 6000 m deep. Oligochaetes from such great depths are in- deed rare. It was therefore considered ap- propriate to describe the species on the basis of this specimen. The worm was stained in paracarmine and mounted whole in Canada balsam. Phallodrilus hessleri, new species Fig. 1 Holotype. —USNM_ 104128, whole- mounted specimen from E of the Philippine Trench, West Pacific Ocean, 9°06.0'N, 127°43.6’E, 5916 m, abyssal red clay (13 Mar 1975). Etymology. —Named for Dr. Robert R. Hessler (Scripps Institution of Oceanogra- phy, La Jolla, California), who collected the sample. Description. —Length more than 2.5 mm, more than 16 segments (worm not com- plete). Width at XI (compressed) 0.22 mm. Prostomium large, rounded. Body wall bearing scattered, very small particles. Cli- tellum extending over '2X—XII. Somatic se- tae (Fig. 1A, B) bifid, with teeth almost par- allel, upper tooth shorter and much thinner than lower, sometimes not visible (or ab- sent?; cf. right bundle in Fig. 1B). Bifids 50— 85 um long, 1.5—2.5 wm thick at node, three to four per bundle anteriorly, two (or three) per bundle in postclitellar segments. Penial setae (Fig. 1C, D, ps) two per bundle, some- what sigmoid, sharply single-pointed, 65— 75 um long, about 3 wm thick at node, di- rected in an almost antero-posterior direc- tion. Male pores inconspicuous, paired ven- trally and posteriorly in XI. Spermathecal pores paired, in line with ventral setae(?) in anteriormost X. Pharyngeal glands in IV—VII. Male gen- italia (Fig. 1D) paired. Vas deferens 8-10 um wide, coiled, much longer than atrium, entering apical end of latter. Atrium pear- shaped, about 60 um long, 28-33 um wide, with very thin outer lining and ciliated inner epithelium; latter densely granulated in ec- tal, wide part of atrium. Prostate glands compact, round, one at each end of atrium. Atrium opening to exterior through simple pore; penis or pseudopenis absent. Sper- mathecae (Fig. 1D, s) not seen in their full length (hidden behind gut), but consisting of short, narrow duct, and slender ampulla. Remarks. —The diagnostic characters of this species are (1) the slender, sharply pointed somatic setae with very thin upper 132 B C A ae ec) Fig. 1. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Phallodrilus hessleri: A, Free-hand drawing of tip of somatic seta; B, Two bundles of somatic setae (from postclitellar segments); C, Penial setae; D, Horizontal view of spermathecae (only parts visible) and male genitalia in segments X—XI. Abbreviations: a, atrium; pr 1, anterior prostate gland; pr 2, posterior prostate gland; ps, penial seta; s, spermatheca; sf, sperm funnel; vd, vas deferens. teeth (or sometimes absent?), (2) the bisetal penial bundles, and (3) the small atria. Oth- er species within the genus with similar fea- tures are all deep-sea forms, viz. P. profun- dus Cook, 1970 (N Atlantic), P. remus Erséus, 1979 (NW Atlantic), P. altus Erséus, 1980 (Beaufort Sea, Arctic), and P. segon- zaci Erséus, 1986 (S Indian Ocean), and they are probably the closest relatives of P. hess- leri. However, in all these other species, the penial setae are clearly longer than the so- matic setae (setae about equally long in hess- leri). The new species is further distin- guished from all of them except P. remus by its very short atria (atria not very large, but elongate in the others), from P. remus by the shape of its penial setae (those of remus oar-shaped, with wide inner ends), and from P. profundus and P. segonzaci by its lack of modified genital setae in segments IX and X. Distribution and habitat.—Known only from the type-locality E of the Philippines, W Pacific Ocean. Abyssal clay, 5916 m. Discussion More than 30 species of Tubificidae have been described from the deep sea, all within the last 20 years (Cook 1970a, b; Erséus 1979a, b, 1980, 1982a, b, 1983a—c, 1984, 1986, 1988; see also review by Erséus 1985). Most of them are bathyal forms, but four are known from depths greater than 4000 m: the North Atlantic Bathydrilus at- lanticus Erséus, 1979 (depth range 1600- 4632 m; Erséus 1983), the two Indian Ocean species Phallodrilus segonzaci and P. stilus Erséus, 1986, both from a single station at 4910 m (Erséus 1986), and the North Pacific B. hadalis Erséus, 1979, which was collected at 7298 m in the Aleutian Trench (Erséus 1979a). Phallodrilus hessleri (from 5916 m) thus represents the second deepest record of marine oligochaetes in the world. Acknowledgments I am indebted to Dr. K. Fauchald for bringing my attention to the Philippine Trench collection in the USNM, and for the loan of the specimen studied; to Dr. R. R. Hessler for providing station data; and to Ms. Barbro Lofnertz and Mrs. Aino Falck- Wahlstrom for technical assistance. Literature Cited Cook, D.C. 1970a. Peloscolex dukei n. sp. and P. aculeatus n. sp. (Oligochaeta, Tubificidae) from the N.W. Atlantic, the latter being from abyssal VOLUME 102, NUMBER 1 depths. — Transactions of the American Micro- scopical Society 88(1969):492-497. . 1970b. Bathyal and abyssal Tubificidae (An- nelida, Oligochaeta) from the Gay Head-Ber- muda transect, with descriptions of new genera and species.— Deep-Sea Research 17:973-981. Erséus, C. 1979a. Taxonomic revision of the marine genera Bathydrilus Cook and Macroseta Erséus (Oligochaeta, Tubificidae), with descriptions of six new species and subspecies.— Zoologica Scripta 8:139-151. 1979b. Taxonomic revision of the marine genus Phallodrilus Pierantoni (Oligochaeta, Tubificidae), with descriptions of thirteen new species. — Zoologica Scripta 8:187—208. 1980. New species of Phallodrilus (Oligo- chaeta, Tubificidae) from the Arctic deep sea and Norwegian fjords.—Sarsia 65:57—60. . 1982a. Atlantidrilus, a new genus of deep-sea Tubificidae (Oligochaeta).—Sarsia 67:43-46. 1982b. Taxonomic revision of the marine genus Limnodriloides (Oligochaeta: Tubifici- dae).— Verhandlungen des Naturwissenschaft- lichen Vereins in Hamburg (Neue Folge) 25: 207-277. 1983a. New records of Adelodrilus (Oligo- chaeta, Tubificidae), with descriptions of two new species from the Northwest Atlantic. — Hy- drobiologia 106:73-83. . 1983b. Deep-sea Phallodrilus and Bathydri- 133 lus (Oligochaeta, Tubificidae) from the Atlantic Ocean, with descriptions of ten new species. — Cahiers de Biologie Marine 24:125-146. . 1983c. A new bathyal species of Coralliodri- lus (Oligochaeta, Tubificidae) from the S.E. At- lantic.— Proceedings of the Biological Society of Washington 96:273-275. . 1984. New and little-known species of deep- sea Tubificidae (Oligochaeta) from the North- west Atlantic.— Zoologica Scripta 13:101-106. . 1985. Distribution and biogeography of Oli- gochaeta. Pp. 365-367 in L. Laubier and C. Monniot, eds., Peuplements profonds du Golfe de Gascogne. Institut Francais de Recherche pour V’Exploitation de la Mer (IFREMER), Brest. . 1986. Two new abyssal species of Phallodri- lus (Oligochaeta, Tubificidae) from the South Indian Ocean.— Bulletin du Muséum National d’Histoire Naturelle (4° sér.) 8 (section A, n° 3): 567-572. —. 1988. Deep-sea Tubificidae (Oligochaeta) from the Gulf of Mexico.— Proceedings of the Biological Society of Washington 101:67-71. Zoo-Tax, Swedish Museum of Natural History, Stockholm, and (postal address): Department of Zoology, University of G6- teborg, Box 25059, S-400 31 Goteborg, Sweden. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 134-136 PHALLODRILUS VESCUS, NEW SPECIES (OLIGOCHAETA, TUBIFICIDAE) FROM THE GULF OF MEXICO Christer Erséus Abstract.—Phallodrilus vescus (subfamily Phallodrilinae) is described from the continental slope of the northern part of the Gulf of Mexico. The species is distinguished from the closely related P. davisi Erséus, 1984 by (1) its fewer setae, (2) its very small anterior prostate glands, (3) its very short penial papillae, and (4) the markedly narrow inner part of its spermathecal ampullae. Species of Phallodrilinae from the north- ern Gulf of Mexico continental slope, orig- inating from a project at LGL Ecological Research Associates, Inc. (Bryan, Texas), were recently described by Erséus (1988). Subsequently, further material was sent to this author for identification. Three worms proved to represent an additional new species of Phallodrilus Pierantoni, 1902, which is described herein. The specimens, weakly stained in Rose Bengal, were mounted whole in Canada bal- sam by the author. They are deposited in the United States National Museum of Nat- ural History (USNM), Smithsonian Insti- tution, Washington, D.C. Phallodrilus vescus, new species Fig. 1 Holotype.—USNM 118716, from south of Louisiana, 27°49'36’”N, 90°07'06’W, 841 m (12 Apr 1984). Paratypes.—USNM 118717, 118718, one from type locality, and one from 27°49'24”’N, 90°07'00’"W, 840 m (12 Apr 1984). Etymology. —The epithet vescus is Latin for “thin, slender,” a feature of the new species. Description. —Length (two complete, fixed specimens) 3.4—-5.6 mm, 31-38 segments. Width at XI (compressed, whole-mounted specimens) 0.08-0.13 mm. Prostomium rounded triangular, pygidium blunt-ended, clitellum extending over 2X—XII. Setae (Fig. 1A) bifid, with upper tooth slightly thinner and shorter than lower. Setae 35-50 um long, 1—1.5 um thick, three per bundle anteriorly, two per bundle in postclitellar segments. Ventral setae absent from XI. Male pores paired in line with ventral setae, posterior to middle of segment X. Pharyngeal glands poorly developed. Male genitalia (Fig. 1B) paired. Vas deferens about 5 wm wide, long and coiled, entering apical end of atrium. Atrium comma-shaped, about 30 um long, about 15 um wide, with thin outer (muscular) lining and thick, gran- ulated inner epithelium; ciliation not seen. Anterior prostate gland small, inconspic- uous, located near junction between vas def- erens and atrium. Posterior prostate gland large, conspicuous, attached to ectal part of atrium. Atrium terminating in small penial papilla, about as long as wide (10-15 um), enclosed in simple penial sac. Spermathecae (Fig. 1B, s) slender, 65-90 um long, con- sisting of short, 11-13 wm wide ducts, and 11-18 wm wide ampullae; latter with inner end very narrow in (at least) two of the spec- imens studied. Lumen of ampullae incon- spicuously and irregularly incised in a few places. A few spermatozoa, arranged in a bundle, present in each ampulla. Remarks. —This species is distinguished VOLUME 102, NUMBER 1 Fig. 1. 135 | 50 pm Phallodrilus vescus: A, Free-hand drawing of somatic seta; B, Lateral view of spermatheca and male genitalia in segments X—XI. Abbreviations: a, atrium; p, penial papilla; pr 1, anterior prostate gland; pr 2, posterior prostate gland; s, spermatheca; vd, vas deferens. from the closely related P. davisi, described by Erséus (1984) from sublittoral depths (78- 80 m) off Massachusetts, by: (1) having only two setae per bundle in postclitellar seg- ments (up to four setae in davisi), (2) its very small anterior prostate glands (in davisi, these glands are conspicuous and in fact larger than the posterior prostates), (3) its very short penial papillae (penes slender and conspicuously hollow in davisi), and (4) the narrow inner end of its spermathecal am- pullae (these ends rounded, not markedly narrow in davisi). The genitalia of P. vescus bear resem- blance to those of P. constrictus Erséus, 1988, which also occurs on the upper continental slope in the northern Gulf of Mexico (Erséus 1988). The latter species, however, pos- sesses a very thick muscular lining on the atria, copulatory sacs and spermathecae; penial setae in segment XI; and a very dis- tinct constriction on the male ducts between the atria and the copulatory sacs; these fea- tures are all absent in P. vescus. The spermathecal ampullae are markedly incised or compartmented in P. davisi (Er- seus 1984:fig. 6B) and P. constrictus (Erséus 1988:fig. 1C). A similar, but less developed, compartmentalization is present in the spermathecae of P. vescus (Fig. 1B). Distribution and habitat. —N Gulf of Mexico. Upper continental slope sediment, 840-841 m. Acknowledgments The LGL specimens reported on in this publication were collected through funding by the U.S. Department of Interior, Min- erals Management Service, Gulf of Mexico Regional OCS Office under Contract Num- ber 14-12-0001-30046 and 14-12-0001- 30212. I am indebted to Dr. Linda H. Pe- quegnat (LGL) for placing the material at my disposal, and to Ms. Barbro Lofnertz and Mrs. Aino Falck-Wahlstrom for tech- nical assistance. Literature Cited Erséus, C. 1984. Taxonomy of some species of Phal- lodrilus (Oligochaeta: Tubificidae) from the 136 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Northwest Atlantic, with description of four new species. — Proceedings of the Biological Society of Washington 97:812-826. —. 1988. Deep-sea Tubificidae (Oligochaeta) from the Gulf of Mexico.— Proceedings of the Biological Society of Washington 101:67-71. Zoo-Tax, Swedish Museum of Natural History, Stockholm, and (postal address): Department of Zoology, University of G6- teborg, Box 25059, S-400 31 Goteborg, Sweden. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 137-153 NEW SPECIES OF SCALE-WORMS (POLYCHAETA: POLYNOIDAE) FROM THE HYDROTHERMAL RIFT-AREA OF THE MARIANA BACK-ARC BASIN IN THE WESTERN CENTRAL PACIFIC Marian H. Pettibone Abstract. —Polynoid polychaetes collected by the Mariana Back-Arc Basin Expedition in the western Central Pacific in 1987 are described. They include four new species belonging to three subfamilies and four genera of Polynoidae: Macellicephalinae: Levensteiniella raisae,; Lepidonotopodiinae: Lepidonoto- podium minutum,; and Branchinotogluminae: Branchinotogluma burkensis and Opisthotrochopodus marianus. Included also is a brief summary of the subfam- ilies, genera, and species associated with deep-sea hydrothermal vents, deep seep-sites, trenches, abyssal basins, experimental deep wood panels, and caves. In her revision of the genera and species that had been grouped in Macellicephalinae Hartmann-Schroder, 1971, containing mostly abyssal species, Pettibone (1976) separated Macellicephalinae and five ad- ditional subfamilies: Macellicephaloidinae (four species), Macelloidinae, Bathyedithi- nae, Polaruschakovinae (two species), and Bathymacellinae. In the remaining Macel- licephalinae, in addition to Macellicephala (seven species), six new genera were added: Bathykermadeca, Bathyeliasona (three species), Bathyvitiazia, Bathyfauvelia, Bathycatalina, and Bathykurila. Subsequently, additional new subfami- lies, genera, and species have been added. Pettibone (1979) emended and added to Macellicephalinae Bruunilla natalensis (Hartman, 1971). Levenstein (1975) added two new species of Macellicephala from the deep-sea trenches in the Antarctic: M. tri- cornis and M. grandelytris. The latter species was later transferred to Bathyfauvelia by Levenstein (1978a:77). Levenstein (1975) also added the new species Macellicepha- loides sandvichensis. Levenstein (1978b) added the new species Macellicephala alia from the Palau trench and the new genus Bathymariana for B. zebra from the Ryuku trench. The latter genus was placed in Bathyedithinae by Levenstein (1984). From the deep Canadian basin in the Arc- tic Ocean, Levenstein (1981) added the new genus Bathypolaria for B. carinata in Ma- cellicephalinae; the new species Bathyedi- thia tuberculata in Bathyedithinae; and the new genera Bathymiranda for B. microceph- ala and Bathycanadia for B. diaphana in Polaruschakovinae. In the same subfamily, Loshamn (1981) added the new genus Di- placonotum for D. paucidentatum (Eliason, 1962) from the Skagerrak. From the Japanese trench, Levenstein (1982a) added a new species of Macelli- cephaloides, M. villosa. From the Tasman trench, Levenstein (1982b) included a key to the genera of Macellicephalinae and added two new genera: Bathytasmania for B. in- solita, and Bathynotalia for B. perplexa. The latter genus and species were referred to Harmothoinae by Pettibone (1985a:130), based on the figure of the prostomium showing long lateral antennae (not men- tioned in the text): the prostomium is har- mothoid, with cephalic peaks; prostomial lateral antennae are lacking in Macelli- 138 cephalinae. From the Kurile-Kamchatka trench, Levenstein (1983) added a new species of Macellicephaloides, M. improvi- sa, and included a key to the seven species of the genus. Levenstein (1984) summarized the dis- tributional patterns for the 19 genera and 38 species of polynoid polychaetes belong- ing to the six deep-sea subfamilies covered in Pettibone (1976), along with the addi- tional genera and species indicated above. They were widely distributed on the abyssal plains and in the deep-sea trenches. The Macellicephalinae had the greatest number of genera (10) and species (21). Three subfamilies were represented by fewer gen- era and species: Macellicephaloidinae (one genus, seven species), Bathyedithinae (two genera, three species), and Polaruschako- vinae (four genera, five species). Two subfamilies were monotypic: Macelloidinae and Bathymacellinae. These groups were defined as ancient or primary abyssal be- cause all the representatives lived only in abyssal depths except for a few that ascend- ed secondarily. Members of the Macelli- cephalinae showed the greatest vertical range and panoceanic distributions, mostly in the Northern Hemisphere. This group appeared to be the most ancient of the abyssal poly- noids. Since the summary of the group by Lev- enstein (1984), additional new subfamilies, genera, and species have been added, chiefly in connections with studies on the hydro- thermal vents in the northeastern Pacific, deep seep-sites in the Gulf of Mexico, and deep wood panel and cave studies in the northwestern Atlantic. From the hydrothermal rift-area off west- ern Mexico at 21°N, Pettibone (1983) added the new subfamily Lepidonotopodiinae for Lepidonotopodium fimbriatum. From the Galapagos vent, the new subfamily Bran- chipolynoinae for Branchipolynoe symmy- tilida, commensal with the deep-sea mussel, was added by Pettibone (1984a). Also from the vents, Pettibone (1984b) added two new PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON species of Lepidonotopodium: L. riftense and L. williamsae and included a key to the species of the genus. From the North Atlantic, Pettibone (1985a) added to Macellicephalinae two new genera: Pelagomacellicephala for P. iliffei, from a cave in the Bahamas, and Bathy- bahamas for B. charleneae from off the Ba- hamas, associated with experimental wood panels, and a new species of Bathykerma- deca, B. turnerae, from off the Virgin Is- lands, also associated with wood panels. Pettibone (1985b) added the new subfam- ily Branchiplicatinae for Branchiplicatus cupreus from the vents off western Mexico at 21°N. From the vents off the Galapagos and western Mexico, Pettibone (1985c) added the third new subfamily having ar- borescent branchiae, Branchinotogluminae for two new genera: Branchinotogluma, with three new species: B. hessleri, B. sandersi, and B. grasslei; and Opisthotrochopodus for O. alvinus. A key to the three branchiate subfamilies was included. Pettibone (1985d) added to Macelli- cephalinae the new genus Levensteiniella for L. kincaidi, and the new species Macelli- cephala galapagensis from the Galapagos, and from the Santa Catalina Channel, the new genus Natopolynoe for N. kensmithi. Included also was a summary of the poly- noid polychaetes collected by DSRV Alvin in the Galapagos Rift in 1979 and East Pa- cific Rise at 21°N in 1982, along with a key to the subfamilies, genera, and species. From the deep seep-sites at the Florida escarpment in the Gulf of Mexico, Petti- bone (1986) added a new species of Bran- chipolynoe, B. seepensis, commensal in the mantle cavities of the Gulf of Mexico mus- sels, along with a key to the two species of the genus. From the hydrothermal vents in the Northeast Pacific Explorer and Juan de Fuca Ridges, Pettibone (1988) added two new species: Lepidonotopodium piscesae in the Lepidonotopodiinae, and Opisthotrochop- odus tunnicliffeae in Branchinotogluminae. VOLUME 102, NUMBER 1 A new species of Macellicephala from the Antarctic, M. australis, was added by Wu and Wang (1987). Thus to the summary by Levenstein (1984), four new subfamilies have been added (total 10), nine new genera (total 28), and 20 new species (total 58). Four of the new genera were added to Macellicephali- nae (total 14) and seven new species (total 28). Two of the new species were referred to Macellicephala, one to Bathykermadeca. Additional polynoids were collected by the Mariana Back-Arc Basin Expedition during April and May 1987, where active hydrothermal vents were found in the west- ern Pacific off the Mariana Islands about 18°N and 144°E. The polynoid polychaetes were collected during dives of DSRV Alvin and sent to me for study by Robert Hessler, along with information on the collecting sites. Four species of polynoids were col- lected on two A/vin dives: dive 1836, re- ferred to as Snail Pits in Burke Field (1 species), and dive 1843, designated as Alice Springs (3 species). The polynoids agree with some of the subfamilies and genera that were previously described from the hydrother- mal vents in the eastern Pacific. Burke Field (Alvin dive 1836, 27 Apr, 18°10.9'N, 144°43.2’E, 3660 m) was an ex- tensive area of low temperature vents at the southern end of an active spreading zone and dominated by pillow basalts. The Snail Pits vent had a water temperature of 15°C, with small, dense aggregations of “hairy” snails that clogged the vent openings. The hot vent water was crystal clear. The single polynoid collected is described below under Branchinotogluminae: Branchinotogluma burkensis, new species. Alice Springs (A/vin dive 1843, 4 May, 18°12.6'N, 144°42.4’E, 3640 m) was an ex- tensive area dominated by pillow basalts with sharp cliffs up to 40 m high. Some low temperature vent sites (10—25°C) were char- acterized by cloudy, particle-filled water and dense concentrations of white anemones. Some high temperature vents (up to 250°C) 139 had dense aggregations of “hairy” snails, crabs, and shrimps, with emerging crystal clear water. The three species of polynoids collected are described below under three subfamilies: Macellicephalinae: Levenstei- niella raisae, new species (1 specimen): Lep- idonotopodinae: Lepidonotopodium minu- tum, new species (9 specimens); and Branchinotogluminae: Opisthotrochopodus marianus, new species (12 specimens). The types are deposited in the National Museum of Natural History, Smithsonian Institution (USNM). Subfamily Macellicephalinae Hartmann-Schroder, 1971 emended Pettibone, 1976 Levensteiniella Pettibone, 1985 Levensteiniella was erected for the single species L. kincaidi from off western Mexico at 21°N and the Galapagos Rift (Pettibone 1985d:741). An additional species is added from the Mariana Back-Arc Basin. Levensteiniella raisae, new species Figs. 1, 2 Material examined. —Western Central Pacific in Mariana Back-Arc Basin, Alvin dive 1843, 4 May 1987, Alice Springs, 18°12.6'N, 144°42.4’E, 3640 m, R. Hessler, collector, holotype (USNM 118362). Description. —Length of holotype 21 mm, width 11 mm with setae, segments 27, last one very small (Fig. 1D). Body flattened, tapering anteriorly and more so posteriorly, with parapodia about as long as body width. Elytra 11 pairs, on segments 2, 4, 5, 7, con- tinuing on alternate segments to 21, large, covering dorsum, oval to subreniform; most of surface covered with unusual type of macro- and micro-tubercle-papillae, with chitinous bases and bulbous papillar tips, larger ones on posterior border; bases cov- ered with brownish foreign material and bacterial ‘‘hairs” (Fig. 1G). Elytrophores large and prominent (Figs. 1A, C, 2A, D). Dorsal cirri on segments lacking elytra, with cylindrical cirrophores on posterodorsal 140 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig: 1. —— ee Levensteiniella raisae, holotype, USNM 118362: A, Dorsal view of anterior end; B, Ventral view of anterior end, bases of palps only shown; C, Dorsal view of left half of segments 8 (cirrigerous) and 9 (elytragerous); D, Dorsal view of posterior end, including parapodia of segments 24-27, last one very small; E, Ventral view of left side of segments 1 1-13 showing ventral papillae on segments 11 and 12, tip of long papilla on segment 12 hidden from view; F, Dorsal row of border papillae and jaws of pharynx (cut open), inner view; G, Left elytron, with detail of macro- and micro-tubercle-papillae (not to scale). Scales = 1.0 mm for A-E; 0.5 mm for F; 2.0 mm for G. faces of notopodia; long styles extending be- yond neurosetae, with filamentous tips; dor- sal tubercles prominent, nodular to truncate (Figs. 1C, D, 2B, C). Dorsal transverse cil- lated ridges, up to five per segment, con- tinuing onto bases of elytrophores and dor- sal tubercles (Fig. 1A, C, D). Prostomium oval, deeply bilobed: lobes projecting anteriorly, with frontal filaments; ceratophore of median antenna short, oval, inserted in anterior notch, with style short, tapered, shorter than palps; palps stout, long, tapered; lateral antennae and eyes lacking (pair of tannish spots resembling “eyes’’) VOLUME 102, NUMBER 1 141 E Fig. 2. Levensteiniella raisae, holotype, USNM 118362: A, Right elytragerous parapodium of segment 2, anterior view, acicula dotted; B, Right cirrigerous parapodium of segment 3, posterior view; C, Same, from segment 8; D, Right elytragerous parapodium of segment 9, anterior view, acicula dotted; E, Notosetae; F, Supraacicular neuroseta, with detail of parts; G, Subacicular neurosetae. Scales = 1.0 mm for A—D; 0.1 mm for E-G. (Fig. 1A). Tentacular segment not distinct dorsally; tentaculophores lateral to prosto- mium, lacking setae; each with pair of ten- tacular cirri, dorsal one about as long as palps, ventral one shorter, both with long slender tips; large bilobed facial tubercle medial to palps (Fig. 1A, B). Second or buccal segment bearing first pair of elytrophores, biramous parapodia, with notopodium shorter than neuropodium; ventral buccal cirri similar to tentacular cir- ri, longer than following ventral cirri (Figs. 1A, B, 2A). Pharynx not extended (cut open); seven pairs of border papillae, none elon- gated; two pairs of light amber-colored, en- tire jaws (not denticled) (Fig. 1F). Both rami of biramous parapodia well de- veloped, notopodium on dorsoposterior side of larger neuropodium, rounded basally with projecting acicular process on lower side; neuropodium with conical presetal lobe with projecting acicular process, postsetal lobe shorter, rounded, deeply cut on dorsal side (Fig. 2B-D). Notosetae very numerous, forming radiating bundle, short to longer, much stouter than neurosetae, straight to slightly curved, tapering to bare blunt tips, with widely spaced spines along one side, variable in number (1-18) (Fig. 2E); tips often covered with reddish-brown foreign material and bacterial “‘hairs.’? Neurosetae slender, numerous, forming fan-shaped bundle; supraacicular neurosetae very slen- der, with longer spinous regions, consisting 142 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 3. Lepidonotopodium minutum, A-F, holotype, USNM 118363; G, paratype, USNM 118364: A, Dorsal view of anterior end, right dorsal and left ventral tentacular cirri missing; B, Right 1st elytron from segment 2, with detail of micropapillae; C, Right 2nd elytron from segment 4; D, Right 6th elytron from segment 11, with detail of micropapillae; E, Right 10th elytron from segment 19; F, Right 11th elytron from segment 21; G, Ventral view of extended pharynx. Scales = 0.5 mm for A; 1.0 mm for B—F; 0.2 mm for G. of two rows of long, widely spaced spines along borders, and with shorter spines near tapered tips (Fig. 2F); subacicular neuro- setae with shorter spinous regions, stouter, with minute, close-set spines along one bor- der, and with slightly hooked bare tips (Fig. 2G). Ventral cirri short, tapered, attached on middle of neuropodia (Fig. 2C, D). Anus dorsal, medial to parapodia of last two segments (26, 27); pygidium small, rect- angular, with pair of long anal cirri (Fig. 1E). Two pairs of long ventral papillae on seg- ments 11 and 12, their tips sometimes ex- tending dorsally between parapodia (Fig. LE). Etymology.—The species, as well as the genus, is named for Raisa J. Levenstein in recognition of her numerous contributions to the study of the deep-sea polychaetes. Remarks. —Levensteiniella raisae differs from L. kincaidi in the form of the elytra, where the surfaces are nearly covered with unusual macro- and micro-tubercle-pa- pillae; in L. kincaidi the elytra are more delicate with only scattered micropapillae. The notosetae differ in having more distinct and fewer spines along the border, rather than more numerous spinous rows in L. kincaidi. Subfamily Lepidonotopodiinae Pettibone, 1983 Lepidonotopodium Pettibone, 1983 Lepidonotopodium was erected for L. fim- briatum Pettibone, 1983 from the East Pa- cific Rise at 21°N. Two additional species were added by Pettibone (1984b) from the Galapagos Rift, as well as 21°N: L. william- sae and L. riftense, and a fourth species from the North East Pacific Explorer and Juan de Fuca Ridges by Pettibone (1988), L. pisce- sae. An additional species is added from the Mariana Back-Arc Basin. Lepidonotopodium minutum, new species Figs. 3, 4 Material.—Western Central Pacific in Mariana Back-Arc Basin, A/vin dive 1843, 4 May 1987, Alice Springs, 18°12.6'N, 144°42.4’E, 3640 m, R. Hessler, collector, holotype (USNM 118363) and 8 paratypes (USNM 118364, 118365). Description. —Holotype 7.5 mm long, 3.5 mm wide with setae, with 23 segments; slightly smaller paratypes 6—6.5 mm long, 3-4 mm wide, with 22—23 segments; small- est paratype 5.2-5.5 mm long, 3-3.2 mm wide, with 21-22 segments. Body short, VOLUME 102, NUMBER 1 143 See | H Fig. 4. Lepidonotopodium minutum, holotype, USNM 118363: A, Right elytragerous parapodium from segment 2, anterior view; B, Right cirrigerous parapodium from segment 3, posterior view; C, Right elytragerous parapodium from segment 9, anterior view; D, Right cirrigerous parapodium from segment 10, posterior view; E, Right elytragerous parapodium from segment 11, posterior view, notopodium and neuropodium separated, acicula dotted; F, Upper, middle and lower notosetae; G, Short anterior notosetae; H, Upper and lower neurosetae. Scales = 0.2 mm for A—-E; 0.1 mm for F—H. suboval in outline, flattened dorsoventrally and slightly tapered anteriorly and poste- riorly. Elytra 11 pairs, on segments 2, 4, 5, 7, continuing on alternate segments to 21, attached eccentrically on prominent elyt- rophores (Figs. 3A, 4A, C, E). Elytra oval to subreniform, imbricated, covering dor- sum, variable in size, last pair very small, Opaque, smooth, with branching “‘veins’’ emanating from place of attachment to elyt- rophores. Surface of first pair of elytra and posterior half on rest of elytra covered with scattered micropapillae, globular with short to longer tapered or cylindrical bases (Fig. 3B-F). Elytral surface and borders covered with foreign material and bacterial “‘hairs.”’ Dorsal cirri witih cylindrical cirrophores at- tached on dorsoposterior sides of notopo- dia; styles tapered, extending beyond tips of neurosetae: dorsal tubercles elongated, in- flated (Fig. 4B, D). Prostomium deeply bilobed, anterior lobes subtriangular with small frontal fila- ments; ceratophore of median antenna in anterior notch, short, bulbous, with short, subulate style; palps cylindrical, with ta- pered tips, nearly two times longer than pro- stomium; lateral antennae and eyes lacking (Fig. 3A). Tentacular segment not visible dorsally; tentaculophores lateral to prosto- mium, achaetous, each with pair of tenta- cular cirri, dorsal ones nearly as long as palps, ventral ones slightly shorter, both with long tapering tips (Fig. 3A). Without distinct fa- cial tubercle. Second or buccal segment with first pair of elytrophores, biramous parapodia, and ventral or buccal cirri attached basally on prominent cirrophores lateral to ventral mouth, with styles similar to tentacular cir- ri, longer than following ventral cirri (Figs. 3A, 4A). Opening of extended pharnyx en- 144 Table 1.—Comparison of Lepidonotopodium rif- tense and L. minutum. L. riftense L. minutum Borders of with short pa- lack papillae notopodi- pillae al bracts Papillae of 7-9 pairs, none 7 pairs, unequal, pharynx elongated some elongated Jaws of with numerous smooth, without pharynx teeth teeth Long ven- 2 pairs on seg- not present tral pa- ments 11 & pillae 12 (on some specimens) circled with seven pairs of unequal-sized pa- pillae; dorsal with three medial ones long, tapered, and two short lateral pairs; ventral with three middle ones and lateral pair short, next to lateral pair long, tapered; two pairs of hooked jaws, without teeth or serrations (Fig. 3G). Biramous parapodia with shorter noto- podia on anterodorsal sides of longer neu- ropodia (Fig. 4A—D). Notopodia subconi- cal, with projecting acicular lobe, hidden anteriorly by very numerous notosetae; well- developed flaring bracts enclosing bases of notosetae; ventro-anterior and dorso-pos- terior bracts attached basally to acicular lobe (Fig. 4A, C, E). Neuropodia with conical presetal acicular lobe and shorter, rounded postsetal lobe (Fig. 4B—E); distal borders with bacterial “‘hairs.”’ Notosetae very numer- ous, forming thick radiating bundle, stouter than neurosetae, with widely spaced spines along one side; notosetae arranged in four groups: upper (about 8), middle (11), lower (8) (Fig. 4F), and short anterior group (Fig. 4G). Notosetae covered with foreign ma- terial and bacterial “‘hairs.’’ Neurosetae nu- merous, forming fan-shaped bundle; neu- rosetae with two rows of numerous spines along one side and slightly hooked bare tips; upper neurosetae longer, with longer spi- nous regions (Fig. 4H). Ventral cirri at- tached on middle of posterior face of neu- ropoda, short, tapered (Fig. 4B—E). PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Segmental or nephridial papillae not ob- vious. Without elongated ventral papillae on segments 11 and 12. Pygidium small, rectangular, between posterior parapodia, with pair of long anal cirri. Etymology.—The specific name minu- tum refers to the relatively small size of the species. Remarks.— Lepidonotopodium minutum is closest to L. riftense. Both are of small size with relatively few segments (up to 7 mm in length and 23 segments). The elytra lack macrotubercles and micro-tubercles but have clavate micropapillae, differing from the other species of Lepidonotopodium. The notosetae have widely spaced spines along one side (also found in L. fimbriatum). The two species may be separated by the char- acters indicated in Table 1. Subfamily Branchinotogluminae Pettibone, 1985 Branchinotogluma Pettibone, 1985 Branchinotogluma was established by Pettibone (1985c) for three species from the hydrothermal vents off western Mexico at 21°N and the Galapagos: B. hessleri, B. san- dersi, and B. grasslei, with B. hessleri as the type species. B. grassleiand B. sandersi were also reported from the North Pacific Ex- plorer and Juan de Fuca Ridges by Petti- bone (1988). An additional species is added from the Mariana Back-Arc Basin. Branchinotogluma burkensis, new species Figs. 5, 6 Material. —Western Central Pacific in Mariana Back-Arc Basin, Alvin dive 1836, 27 Apr 1987, Burke Field, Snail Pits, 18°10.9’N, 144°43.2’E, 3660 m, R. Hessler, collector, holotype (USNM 118366). Description. — Length of holotype 30 mm, width with setae 16 mm, segments 21, with additional small parapodium on right side (Fig. 5B). Body flattened, tapering anteriorly and posteriorly, with parapodia longer than body width. No color except for golden-col- ored setae. Dorsum with transverse ciliated VOLUME 102, NUMBER 1 145 ~ —— G Fig. 5. Branchinotogluma burkensis, holotype. USNM 118366: A. Dorsal view of anterior end: B, Dorsal view of posterior end including segments 18-21: C, Ventral view of left side of segments 1 1—13, showing small segmental ventral papillae: D. Right 1st elytron from segment 2: E, Right 7th elytron from segment 13; F, Dorsal view of left side of cirrigerous segment 14, only base of style of dorsal cirrus shown: G. One of jaws removed from body: H, Right elytragerous parapodium from segment 2, anterior view, acicula dotted. Scales = 2.0 mm for A—E- 0.5 mm for F. G: 1.0 mm for H. bands, 2-4 per segment, extending onto elytrophores. dorsal tubercles. and bran- chial bases (Fig. 5A, B, F). Elytra 10 pairs, attached on large bulbous elytrophores on segments 2. 4. 5. 7. con- tinuing on alternate segments to 19 (Figs. 5A, B, H, 6B). Elytra large. overlapping. covering dorsum, round to oval. delicate. with branched “‘veins.”” without tubercles or papillae (Fig. 5D. E). Dorsal cirm on non- elytragerous segments, with cylindrical cir- rophores on posterodorsal sides of noto- podia. and long smooth styles with slender tips extending beyond tips of neurosetae: dorsal tubercles nodular. projecting (Figs. 5B, F, 6A, C). Branchiae arborescent, in two groups: on dorsal bases of notopodia and on lateral sides of elytrophores and dorsal tubercles (Figs. 5F, 6B). Branchiae begin- ning on segment 3 as two small groups (Fig. 6A). becoming larger (Figs. 5F, 6B. C), con- tinuing to posterior end and becoming very small (Fig. 5B). Bilobed prostomium with prominent cy- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 146 (4 D 46 y i sense Z | LF i 2 Z E | an B / / g . i | i \ \ { f \ } i : iy, * ema oe F |; Y ~ i \ ; ; \ I = Sy j f | ¥ ; Y, SS I} : } | E 2S j | £ SSG j | j So | ¢ / gs o~ Z ! | é — ———S- bs —— | [ Cc —— = Sg = E Ee Fig. 6. Branchinotogluma burkensis, holotype. USNM 118366: A, Right cirrigerous parapodium from seg- ment 3, posterior view; B, Right elytragerous parapodium from segment 9, anterior view, acicula dotted; C, Right cirrigerous parapodium from segment 10, posterior view; D, notosetae; E, Tip of long supraacicular neuroseta, with detail of parts; F. Subacicular neuroseta, with detail of parts. Scales = 1.0 mm for A-C; 0.1 mm for D-F. smooth, about three times length of prosto- mium; without eyes, but non-ocular paired oval shaded areas present (Fig. 5A). Ten- tacular segment not distinct dorsally; ten- lindrical anterior lobes with terminal fila- ments; median antenna with bulbous cer- atophore in anterior notch and short style tapered to slender tip: palps long, tapered, VOLUME 102, NUMBER 1 taculophores lateral to prostomium, achae- tous, each with pair of dorsal and ventral tentacular cirri about as long as palps, dorsal tentacular cirri slightly longer than ventral ones (Fig. 5A). Second or buccal segment with first pair of large elytrophores, bira- mous parapodia, and long, slender buccal cirri similar to tentacular cirri, longer than following ventral cirri; notopodium with prominent bract fused with acicular lobe (not distinct, as usual in genus) and small bundle of stout notosetae; neuropodium similar to following (Fig. 5A, H). Pharynx not everted (cut out), with five border papillae around opening: three dorsal and two ventral; two pairs of prominent dark reddish amber-col- ored jaws, minutely denticled on inner bor- der (about 50) (Fig. 5G). Biramous parapodia with notopodia shorter than neuropodia, both rami with golden-colored setae (Figs. 5H, 6A—C). No- topodia conical, with prominent projecting acicular processes, without notopodial bracts except on segment 2 with bract fused to acic- ular process. Notosetae numerous, forming radiating bundles, not as long as but much stouter than neurosetae, straight, tapered, acicular, shorter ones smooth, longer ones with some spines near distal tips (Fig. 6D). Larger and longer neuropodium with sub- conical presetal acicular lobe with project- ing acicular process and shorter rounded postsetal lobe, lobes deeply separated dor- sally and ventrally. Neurosetae very nu- merous, forming fan-shaped bundles, slen- der, with slightly hooked tips. Supraacicular neurosetae with two rows of widely spaced prominent spines and finely spinous hood on slightly hooked tip (Fig. 6E).Subacicular neurosetae finely spinous along border, with slightly hooked tip (Fig. 6F). Ventral cirri short, tapering, attached on middle of neu- ropodia (Fig. 6A-C). Posterior end not modified or com- pressed. Pygidium small lobe between para- podia of last segment (21), with dorsal anus and pair of anal cirri (Fig. 5B). Segmental ventral papillae seven pairs, small squarish, 147 on ventral bases of parapodia of segments 11-17, none elongated (Fig. 5C). Etymology. —The species is named bur- kensis for the collecting area, Burke Field on the Mariana Back-Arc Basin. Remarks.—B. burkensis is closest to B. grasslei Pettibone (1985c). Both species have a pair of anal cirri and posterior segments that are not compressed or modified; bran- chiae are present on all segments from 3 on; and both lack elongated ventral papillae. B. burkensis has seven pairs of small segmental ventral papillae on segments 11-17, com- pared to five pairs on segments 11-15 in B. grasslei. In B. burkensis, the notopodial bract on segment 2 is fused with the acicular lobe and not distinct, as in B. grasslei, where the notopodial bract encloses the acicular lobe and notosetae (Pettibone 1985c, fig. 6A). The long notosetae in B. burkensis have dis- tal spines, whereas they are smooth in B. grasslei. Opisthotrochopodus Pettibone, 1985, emended Opisthotrochopodus was established by Pettibone (1985c) for O. alvinus from the hydrothermal vents off western Mexico at 21°N and the Galapagos. O. tunnicliffeae, from the hydrothermal vents of the Ex- plorer and Juan de Fuca Ridges, was added by Pettibone (1988). A third species is added from the Mariana Back-Arc Basin and the genus 1s emended. Diagnosis.—Body short, with 21 seg- ments, first achaetous. Elytra 10 pairs, on segments 2, 4, 5, continuing on alternate segments to 19. Dorsal cirri with short cir- rophores and long style, and dorsal tuber- cles, in line with elytrophores, on segments 3, 6, continuing on alternate segments to 20 and 21. Arborescent branchiae two pairs per segment, attached to lateral sides of elyt- rophores, dorsal tubercles, and dorsal side of notopodia, beginning on segment 3 and continuing to segment 15-18. Prostomium bilobed, with triangular anterior lobes bear- 148 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 7. Opisthotrochopodus marianus, A-I, paratype, USNM 118369; J, holotype, USNM 118367: A, Dorsal view of anterior end; B, Ventral view of segments 12-18; C, Right Ist elytron from segment 2; D, Right 2nd elytron from segment 4; E, Right 4th elytron from segment 7; F, Right 6th elytron from segment 11; G, Right 9th elytron from segment 17; H, Right 10th elytron from segment 19; I, Ventral view of extended pharynx; J, Dorsal jaws, inner view. Scales = 0.5 mm for A, B, I; 0.5 mm for C—H; 0.1 mm for J. ing frontal filaments, with ceratophore of median antenna in anterior notch, with paired ventral palps, without lateral anten- nae or eyes. First or tentacular segment not visible dorsally; tentaculophores lateral to prostomium, achaetous, each with dorsal and ventral tentacular cirri. Second or buc- cal segment with first pair of elytra, bira- mous parapodia, and ventral or buccal cirri attached to basal parts of parapodia lateral to mouth; styles longer than following ven- tral cirri. Parapodia biramous, with noto- podia shorter than neuropodia. Notopodia of elytragerous segments 2-17 with promi- nent rounded bracts enclosing conical acic- ular lobes and notosetae, only on segment 2 or lacking. Neuropodia with longer con- ical presetal and shorter rounded postsetal lobes. Notosetae stouter than neurosetae, straight, acicular, smooth or with spines. Neurosetae long, slender, finely spinous, with slightly hooked tips. Ventral cirri short, tapered. Posterior 3 to 6 segments modified, including wheel organs on segment 20 or lateral lamellae on segment 21. Pharynx with 5 to 8 border papillae; 2 pairs of dorsal and ventral hooked jaws, with or without den- ticles. Elongated ventral papillae on seg- ment 12 and rounded ventral lamellae on some following segments. Pygidium with or without pair of anal cirri. Opisthotrochopodus marianus, new species Figs. 7-9 Material.—West Central Pacific, Mar- iana Back-Arc Basin, A/vin dive 1843, 4 May 1987, Alice Springs, 18°12.6'N, 144°22.4’E, 3640 m, holotype (USNM 118367), para- type (USNM 118369), paratype (USNM 118368), 9 paratypes (3 small, USNM 118370). Description. —Holotype 6 mm long, 3 mm wide, with 21 segments. Two adult para- types 5—5.5 mm long, 3 mm wide, with 21 segments. Two young paratypes 2.5—3 mm long, 2-3 mm wide, with 13-14 segments plus small growing zone. Body flattened, ta- pering slightly anteriorly, anterior parapo- dia (segments 2-13) longer, tapering grad- ually (segments 14-18), narrowing and projecting posteriorly with extra long setae (segments 19-21) (Figs. 7B, 9H, I). Dorsum with transverse ciliated bands, 1—2 per seg- VOLUME 102, NUMBER 1 149 Fig. 8. Opisthotrochopodus marianus, paratype, USNM 118369: A, Right elytragerous parapodium from segment 2, anterior view, acicula dotted; B, Right cirrigerous parapodium from segment 3, posterior view, style of dorsal cirrus broken off; C, Left elytragerous parapodium from segment 9, anterior view, acicula dotted; D, Left cirrigerous parapodium from segment 10, posterior view; E, Short and long notosetae; F, Supraacicular neuroseta; G, Subacicular neurosetae; H, Right elytragerous parapodium from segment 15, anterior view; I, Right cirrigerous parapodium from segment 16, posterior view; J, Right elytragerous parapodium from segment 17, posterior view; K, same, anterior view. Scales = 0.3 mm for A-D, H-J; 0.1 mm for E—G; 0.2 mm for K. ment, extending onto elytrophores and dor- sal tubercles (Figs. 7A, 9H). Elytra and prominent bulbous elytro- phores 10 pairs (Figs. 7A, 8A, C, H, J, K, 9H). Elytra large, overlapping, covering dorsum, except for posterior modified par- apodia, round to oval, larger on middle ely- tra, very small on segments 17 and 19, del- icate, showing branched “‘veins”’ emanating from scars of attachment to elytrophores, without tubercles or papillae (Figs. 7C—H, 9H). Dorsal cirri with cylindrical cirro- phores on posterodorsal sides of notopodia, long smooth styles with slender tips ex- tending beyond setae; dorsal tubercles elon- gate, tapered, with long cilia (Fig. 8B, D, I). Branchiae delicate, arborescent, on lateral bases of elytrophores and dorsal tubercles and dorsal bases of notopodia, beginning on segment 3 as two small groups (Fig. 8B), becoming larger (Fig. 8C, D), and continu- ing to segment 15 as single small group (Fig. 8H). Prostomium bilobed, anterior lobes tri- angular with slender frontal filaments; me- dian antenna with bulbous ceratophore in anterior notch, with slender short style; palps stout, tapered, about two times longer than prostomium; without eyes (Fig. 7A). Ten- taculophores lateral to prostomium, achae- tous, with 2 pairs of tentacular cirri, dorsal pair longer than palps, ventral pair shorter (Fig. 7A). Second or buccal segment with first pair of prominent elytrophores, bira- mous parapodia, similar to but smaller than following: ventral buccal cirri similar to ten- tacular cirri, longer than following ventral cirri; notopodium without notopodial bract 150 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 9. Opisthotrochopodus marianus, A—G, paratype, USNM 118369; H-I, paratype, USNM 118368: A, Right cirrigerous parapodium from segment 18, anterior view, acicula dotted; B, Right elytragerous parapodium from segment 19, anterior view, acicula dotted, elytrophore not shown; C, Right cirrigerous parapodium from segment 20, anterior view, acicula dotted; D, Tips of long notosetae from same; E, Neuroseta from same; F, Left cirrigerous parapodium from segment 21, anterior view, acicula dotted; G, Same, cirrigerous parapodium from segment 21, anterior view, acicula dotted; G, Same, enlarged: H, Dorsal view of posterior end including segments 19-21, acicula dotted: I, same, ventral view. Scales = 0.3 mm for A-C, F; 0.1 mm for D, E, G; 0.2 mm for H, I. (Figs. 7A, 8A). Notosetae stout, similar to those of following segments; lower neuro- setae with capillary tips, rest similar to up- per neurosetae of following segments. Ex- tended pharynx encircled with four pairs of papillae, dorsal with two medial ones larger and lateral ones smaller: ventral with four small papillae; two pairs of curved reddish jaws occupying most of opening, without denticles on inner border (Fig. 7I, J). Parapodia of segments 2-16 biramous, with notopodia shorter than neuropodia, both rami with light yellow amber-colored setae (Fig. 8A—D, H, I). Notopodia rather long, conical, without notopodial bracts en- closing acicular lobe and notosetae (as in O. alvinus). Notosetae numerous, stouter than neurosetae, short, smooth and longer, smooth or with faint spinous rows, tapered to blunt tips (Fig. 8E). Larger neuropodia with presetal lobe long, subconical, with projecting acicular process, postsetal lobe Shorter, rounded. Neurosetae numerous, long, slender, wider basally, with slightly hooked tips. Supraacicular neurosetae more slender, with longer spinous regions (Fig. VOLUME 102, NUMBER 1 Table 2:—Comparison of three species of Opisthotrochopodus. 151 O. alvinus Pettibone, 1985c (Figs. 7-9) O. tunnicliffeae Pettibone, 1988 (Figs. 6-9) O. marinus n. sp. (Figs. 7-9) Notopodial bracts on elytragerous parapo- dia Branchiae on segments Pharynx: Papillae Jaws Segment 20: Notopodia Neuropodia segments 2-17 (Figs. 7A, G) 3-17 5 small: 3 dorsal, 2 ventral with minute denticles (Fig. 8H, I) achaetous (Fig. 9B, F—L) with “wheel” organ, incl. stout, acicular segment 2 only (Fig. 6A, C) short notosetae (Figs. 8B, C, 9A-F) with “balloon” organ including stout har- without 3-15 8: 4 dorsal, 2 medial larger; 4 ventral small without denticles (Fig. 7I, J) long notosetae (Fig. 9C-E) long, slender, acicular lobe & short capillary & slender spinous neurosetae _. Ventral cirrus without Segment 21: Lamellae small notopodial & neuropodial (Fig. 9M, N). Neurosetae few, short Ventral cirrus without 8F). Subacicular neurosetae decreasing in length ventrally, finely spinous more basal- ly, with longer spines distally; few shorter lower ones with capillary tips (Fig. 8G). Ventral cirri short, tapered, attached on middle of neuropodia (Fig. 8B—D, H, I). Elongated ventral papillae on segment 12, extending posteriorly to segment 15 (Fig. 7B); 6 pairs of short, flat ventral lamellae on segments 13-18, ciliated on upper side (Figs. 7B, 8H, J, K). Parapodia from segment 15 on more or less modified. Parapodium 15 with only small branchia on lateral side of elytro- phore; notopodium almost as long as neu- ropodium; supraacicular neurosetae with capillary tips (Fig. 8H). Parapodium 16, and following parapodia, without branchiae; all neurosetae with capillary tips (Fig. 81). Par- apodium 17 with small neuropodium short- er than ventral cirrus, with bundle of long poon & slender spi- neurosetae nous neurosetae present without without (Fig. 9C) large lateral neuro- podia (Fig. 9G-—I) same present long capillary without slender capillary neurosetae; notopodium small, with three shorter and seven longer stout notosetae extending to tip of neuro- podium (Fig. 8J, K). Parapodium 18 with small notopodial acicular lobe fused to cirrophore of dorsal cirrus, ciliated on lower side, with few (4) short stout notosetae on upper side; conical neuropodium shorter than ventral cirrus, ciliated on upper side, with small bundle of long capillary neurosetae (Fig. 9A). Parapodium 19 with elytrophore and small elytron, inflated oval notopodium with short acicular lobe and few (3-4) short stout notosetae near tip, ciliated on underside; neuropodium similar to preceding parapo- dium, with small bundle of long capillary neurosetae (Fig. 9B, H, I). Parapodium 20 directed posteriorly, with small notopodial acicular lobe fused to cir- rophore of dorsal cirrus; neuropodium with £52 long slender acicular lobe nearly as long as dorsal cirrus, with short ventral cirrus (Fig. 9C, H, I). Long notosetae wider subdistally, spinous, tapering to slender tips (Fig. 9D). Shorter neurosetae slender, wider subdis- tally, spinous, tapering to capillary tips (Fig. 9E). Parapodium 21 directed posteriorly, with notopodial acicular lobe fused to cirrophore of dorsal cirrus, without notosetae; neuro- podial conical acicular lobe with slender capillary neurosetae and large, oval, delicate lateral lamella; without ventral cirrus (Fig. 9F-I). Pygidium small rounded lobe with dorsal anus medial to parapodia of segment 21, and pair of long anal cirri (Fig. 9H, I). Etymology.—The specific name mari- anus is based on the collecting site of the Mariana Back-Arc Basin. Remarks. —O. marianus can be separated from the other two species of Opisthotro- chopodus according to Table 2. Acknowledgments My thanks go to the members of the Mar- iana Back-Arc Basin Expedition, the crew of the Alvin, and especially Robert R. Hes- sler and Michel A. Boudrias, who sent me the polynoid specimens and furnished sta- tion data and information on the collecting area. The manuscript benefited from the re- views by James A. Blake and Jerry D. Ku- denov. Literature Cited Levenstein, R. J. 1975. [The polychaetous annelids of the deep-sea trenches of the Atlantic sector of the Antarctic Ocean.]—Trudy Institut Okeanologii P.P. Shirshov Academii Nauk SSSR 103:119-142 [in Russian, English summary]. . 1978a. [Annelida (Polychaeta) from the deep waters of the Pacific region of Antarctica.]— Trudy Institut Okeanologii P.P. Shirshov Aca- demii Nauk SSSR 113:73-87 [in Russian, En- glish summary]. . 1978b. [Polychaetes of the family Polynoidae (Polychaeta) from the deep-water trenches of the western part of the Pacific.|—Trudy Institut PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Okeanologii P.P. Shirshov Academii Nauk SSSR 112:162-174 [in Russian, English summary]. 1981. [Some pecularities in the distribution of polychaetes of the family Polynoidae in the Canadian basin of the Arctic Ocean.]—Trudy Institut Okeanologii P.P. Shirshov Academii Nauk SSSR 115:26-36 [in Russian, English summary]. . 1982a. [On the polychaete fauna of the family Polynoidae from the trench of Japan.]— Trudy Institut Okeanologii P.P. Shirshov Academii Nauk SSSR 117:59-62 [in Russian, English summary]. 1982b. [New genera of the subfamily Ma- cellicephalinae (Polychaeta, Polynoidae) from the Tasman Trench]—Zoologichesky Zhurnal 61(9):1291-1296 [in Russian, English summa- ry] 1983. [Macellicephaloides improvisa sp. n. (Polychaeta, Polynoidae) from the Kurile-Kam- chatka Trench]—Zoologichesky Zhurnal 62(9): 1419-1421 [in Russian, English summary]. . 1984. On the ways of formation of the deep- sea polychaete fauna of the family Polynoidae. Pp. 72-85, in P.A. Hutchings, ed., Proceedings of the First International Polychaete Confer- ence, Sydney, Australia, 1983. The Linnean So- ciety of New South Wales. Loshamn, A.-A. 1981. Descriptions of five polynoid species (Polychaeta) from the coasts of Norway and Sweden, including three new species, one new genus and one new generic name.—Zoo- logica Scripta 10(1):5—13. Pettibone, M. H. 1976. Revision of the genus Ma- cellicephala McIntosh and the subfamily Ma- cellicephalinae Hartmann-Schroder (Polychae- ta: Polynoidae). —Smithsonian Contributions to Zoology 229:1-71. 1979. Redescription of Bruunilla natalensis Hartman (Polychaeta: Polynoidae), originally referred to Fauveliopsidae. — Proceedings of the Biological Society of Washington 92(2):384-388. 1983. A new scale worm (Polychaeta: Poly- noidae) from the hydrothermal rift area off Western Mexico at 21°N.—Proceedings of the Biological Society of Washington 96(3):392-399. 1984a. A new scale-worm commensal with deep-sea mussels on the Galapagos hydrother- mal vent (Polychaeta: Polynoidae).— Proceed- ings of the Biological Society of Washington 97(1):226-239. 1984b. Two new species of Lepidonotopo- dium (Polychaeta: Polynoidae: Lepidonotopo- dinae) from hydrothermal vents off the Gala- pagos and East Pacific Rise at 21°N.— Proceedings of the Biological Society of Wash- ington 97(4):847-863. VOLUME 102, NUMBER 1 . 1985a. Polychaete worms from a cave in the Bahamas and from experimental wood panels in deep water of the North Atlantic (Polynoidae: Macellicephalinae, Harmothoinae).—Proceed- ings of the Biological Society of Washington 98(1):127-149. 1985b. An additional new scale worm (Po- lychaeta: Polynoidae) from the hydrothermal rift- area off Western Mexico at 21°N.— Proceedings of the Biological Society of Washington 98(1): 157-164. 1985c. Additional branchiate scale-worms (Polychaeta: Polynoidae) from Galapagos hy- drothermal vent and rift-area off Western Mex- ico at 21°N.— Proceedings of the Biological So- ciety of Washington 98(2):447-469. 1985d. New genera and species of deep-sea Macellicephalinae and Harmothoinae (Poly- chaeta: Polynoidae) from the hydrothermal rift areas of the Galapagos and western Mexico at 21°N and from the Santa Catalina Channel. — Proceedings of the Biological Society of Wash- ington 98(3):740-757. 153 1986. A new scale-worm commensal with deep-sea mussels in the seep-sites at the Florida Escarpment in the eastern Gulf of Mexico (Poly- chaeta: Polynoidae: Branchipolynoinae).—Pro- ceedings of the Biological Society of Washington 99(3):444-451. . 1988. New species and new records of scaled polychaetes (Polychaeta: Polynoidae) from hy- drothermal vents of the Northeast Pacific Ex- plorer and Juan de Fuca Ridges. — Proceedings of the Biological Society of Washington 101(1): 192-208. Wu, B. & Wang, Y.-H. 1987. Two new species of Polychaeta from South Ocean.—Acta Zootax- onomica Sinica 12(1):23—29 [in Chinese and En- glish]. Department of Invertebrate Zoology, Na- tional Museum of Natural History, Smith- sonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 154-168 POLY NOIDAE AND SIGALIONIDAE (POLYCHAETA) FROM THE GUAYMAS BASIN, WITH DESCRIPTIONS OF TWO NEW SPECIES, AND ADDITIONAL RECORDS FROM HYDROTHERMAL VENTS OF THE GALAPAGOS RIFT, 21°N, AND SEEP-SITES IN THE GULF OF MEXICO (FLORIDA AND LOUISIANA) Marian H. Pettibone Abstract. —Eight species of scaled polychaetes are reported from hydrother- mal vents of the Guaymas Basin in the Gulf of California: Neoleanira racemosa in the Sigalionidae and seven species of Polynoidae, including two new species, Bathykurila guaymasensis, in Macellicephalinae, and Macellicephaloides alvini, in Macellicephaloidinae. The latter genus and subfamily are reviewed, and a Key to the seven species in the genus is provided. Included are additional records of some species of Polynoidae from hydrothermal vents from the Ga- lapagos and 21°N in the eastern Pacific, as well as seep-sites in the Gulf of Mexico Florida Escarpment and off Louisiana. A small collection of scaled polychaetes from the Guaymas Basin in the Gulf of Cal- ifornia or the Sea of Cortez was sent to me for study by J. F. Grassle. Hot vents and hydrocarbon seeps were discovered in this area in 1980 and sampled in 1982 during dives of the submersible DSRV Alvin (Lons- dale 1984, Grassle 1986). The area, a con- tinuation of the East Pacific Rise into the Gulf of California, is covered by a thick layer of pelagic muddy sulfide sediment. The study site consists of mounds of hydrother- mal precipitates in the spreading center troughs at about 2000 meters. The fauna included large numbers of the giant vesti- mentiferans, Riftia, giant clams, such as Ca- lyptogena pacifica, nuculanid bivalves, al- vinellid polychaetes, as Paralvinella grasslei, and fluffy mats of the large bacterium Beg- giatoa. Eight species of scaled polychaetes are re- ported herein from the Guaymas Basin, sev- en of them belonging to the Polynoidae and one to the Sigalionidae: Neoleanira race- mosa (Fauchald), previously reported from the Guaymas Basin by Fauchald (1972, as Sthenolepis). Of the polynoid species, five were previously described by me from other vent areas: one, Branchiplicatus cupreus, from the tropical eastern Pacific at 21°N; one, Lepidonotopodium riftense, the same area and the Galapagos Rift; and three, Branchinotogluma grasslei, B. sandersi, and Levensteiniella kincaidi, from the above two areas and also the Explorer and Juan de Fuca Ridges. The other two polynoid species are described below as new species: Bathy- kurila guaymasensis, in Macellicephalinae, and Macellicephaloides alvini, in Macelli- cephaloidinae. The specimens were collect- ed during A/vin dives in 1982 and 1985, in washings from rock with worms, Bead Ex- periment washings, washings from Rock Chimney, washings from Riftia, Calypto- gena, and alvinellid polychaetes, from Box cores taken on the slopes of the mounds, some with numerous nuculanid bivalves. Some additional records of previously de- scribed vent fauna are included in this re- port, such as Branchipolynoe symmytilida, removed from some Galapagos mussels and sent to me in July 1985 by J. F. Grassle. VOLUME 102, NUMBER 1 Also, specimens of Branchipolynoe seepen- sis were removed by Ruth Turner from Gulf of Mexico mussels collected in the seep-sites at the Florida Escarpment and sent to me in October 1986, by Barbara Hecker. An additional specimen of this species was col- lected in May 1987, by the US Navy sub- marine NR-1 and R/V Gyre and sent to me by T. H. Perkins. Additional vent polynoids from the Galapagos and the eastern Pacific Rise at 21°N, collected during A/vin dives in 1979 and 1982, chiefly among fauna in washings from mussels and crab traps, were sent to the Smithsonian Sorting Center for further sorting and transferred to me in De- cember 1987. They supplement my pre- vious studies on this group. Types and additional specimens are de- posited in the collections of the Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution (USNM). Family Polynoidae Subfamily Branchipolynoinae Pettibone, 1984 Genus Branchipolynoe Pettibone, 1984, emended Pettibone, 1986 Branchipolynoe symmytilida Pettibone Branchipolynoe symmytilida Pettibone, 1984a:227, figs. 1-8.—Kenk & Wilson, 1985:264.—Desbruyéres et al. 1985:104, 113, 114.—Grassle, 1986:325, 327, 336. Material. —East Central Pacific, from dives of the A/vin on three vent areas along the Galapagos Rift in 1979, associated with deep-sea mussels, Branchimodiolus ther- mophilus Kenk & Wilson: Mussel Bed, 00°47.89'N, 86°09.21'W: Dive 880, 21 Jan, 2493 m, from 9 mussels, 9 specimens (USNM 98577). Dive 888, 13 Feb, 2493 m, from mussel, 1 specimen (USNM 98578). Dive 986, 3 Dec, 2494 m, mussel bucket washings, 1 specimen (USNM 118168). Dive 989, 6 Dec, 2482 m, from small mus- sels, 5 specimens (USNM 118171). Dive 991, 8 Dec, 2490 m, washings from 68 mus- 155 sels in mesh-lined milk crates, 5 specimens, (USNM 118170). Garden of Eden, 00°47.69'N, 86°07.74'W: Dive 883, 25 Jan, 2482 m, from mussel, 1 specimen (USNM 98579). Dive 884, 25 Jan, 2482 m, from 6 mussels, 7 specimens (USNM 98580) and 3 young specimens (USNM 118172). Dive 993, 10 Dec, 2518 m, slurp sample from base of vestimentiferans, 1 specimen (USNM 118166). Rose Garden, 00°48.25’N, 86°13.48'W: Dive 892, 17 Feb, 2454 m, from 3 mussels, 3 specimens (USNM 98581). Dive 894, 19 Feb, 2457 m, from 12 mussels, 12 specimens (USNM 98582). Dive 983, 30 Nov, 2457 m, mussel bucket residue, 2 young specimens (USNM 118167). Dive 984, 1 Dec, 2451 m, mussel washings left in clam bucket overnight, 13 specimens (USNM 118169); residue from retrieved box containing vestimentiferans, 1 small specimen (USNM 118173). Remarks.—Branchipolynoe symmytilida has been found living commensally in the mantle cavities of the giant deep-sea vent mussels, Branchimodiolus thermophilus Kenk & Wilson (Pettibone 1984a, Kenk & Wilson 1985). Of the 37 polynoids taken from 36 mussels (USNM 98577-98582), 1 had a length of 40 mm; 14, lengths of 29- 33 mm; 9, lengths of 21—25 mm; 10, lengths of 15-20 mm; 2, lengths of 11 mm; and 1, length of 6 mm. The two polynoids taken from a single mussel had lengths of 25 and 15 mm. The additional 31 specimens from 8 Alvin dives, taken mostly from mussel washings (USNM 118166-73), consisted of smaller worms: adults up to 1 1 mm in length, 3 mm in width, with 20 segments and 10 pairs of elytra; juveniles 3—4 mm in length, 1.5—2.2 mm in width, with 14-17 segments; and very young specimens 1.2—2 mm in length, 1 mm in width, with 11-12 seg- ments. According to observations by Desbru- yéres et al. (1985:104) on B. symmytilida, gut contents included pieces of mussel gills, coccoid and filamentous bacteria-like cells, and a mixture of crustacean molts, uniden- 156 tifiable worm setae, diatom frustules, and amorphous organic matter consistent with a mixed diet including living tissue and pseudofeces of mussels. Special features are their red blood, segmental arborescent branchiae, 10 pairs of elytra, and 20-21 seg- ments. Distribution. —East Central Pacific along Galapagos Rift, associated with Galapagos deep-sea mussels, in 2451-2518 m. Re- ported for 13°N by Desbruyéres et al. (1985: 114). Branchipolynoe seepensis Pettibone Branchipolynoe seepensis Pettibone, 1986: 445, figs. 1-4. Branchipolynoe sp. Hecker, 1985:470. Material. —Gulf of Mexico, from dives of the A/vin in Oct 1986, Florida Escarpment, 26°01'46’"N, 84°54'36”"W, 3270 m: Dive 1753, commensal with mussels, 15 speci- mens (USNM 10151). Dive 1755, with mussels, 19 specimens (USNM 101503). Dive 1756, in washings and from broken mussels, 25 specimens (USNM 101502). Dive 1758, with mussels, 2 juveniles (USNM 101504). Gulf of Mexico off Louisiana, 27°47'N, 91°30'’W, 1097 m, Fla. Dept. Nat. Res., 5 Mar, EJ 87-127, 1987, Bush Hill Box 1, among mussels, collected by US Navy sub- marine NR-1, recovered on surface by R/V Gyre, cruise 87-G-2, one specimen (USNM 102844). Remarks. — The additional 61 specimens from 4 Alvin dives (USNM 10151-4), as- sociated with the unnamed Gulf of Mexico giant mussels (to be described and named by Ruth Turner and Barry Wilson) include adults and juveniles; some are larger than previously reported. Larger adults are 31- 40 mm long, 14-17 mm wide, with 21 seg- ments; smaller adults, 9-17 mm long, 4-8 wide, with 21 segments; larger juveniles, 5- 9 mm long, 3-4.5 mm wide, with 17-19 segments; smaller juveniles, 3-4.5 mm long, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 2-2.5 mm wide, with 15-16 segments; and the smallest juvenile, 2 mm long, 1.5 mm wide, with 14 segments. The single speci- men from Bush Hill off Louisiana (USNM 102844) is 20 mm long, 8 mm wide, with 21 segments; it differs by having long ven- tral papillae on segment 12 only, not on both segments 11 and 12. The smaller ju- veniles lack both pairs of ventral papillae. Distribution. —Gulf of Mexico, near hy- persaline seeps at base of Florida Escarp- ment, associated with Gulf of Mexico mus- sels, in 3266-3270 m and off Louisiana, in 1097 m. Subfamily Lepidonotopodiinae Pettibone, 1983 Genus Lepidonotopodium Pettibone, 1983 — Lepidonotopodium riftense Pettibone Lepidonotopodium riftense Pettibone, 1984b:852, figs. 2-4. Material. —East Central Pacific, from dives of the A/vin on 3 vent areas along the Galapagos Rift in 1979: Mussel Bed, 00°47.89'N, 86°09.21'W: Dive 986, 3 Dec, 2494 m, mussel bucket washings, one spec- imen (USNM 118180). Garden of Eden, 00°47.09’N, 86°07.74'W: Dive 993, 10 Dec, 2518 m, slurp sample from base of vesti- mentiferans, three specimens (USNM 118181). Rose Garden, 00°48.25'N, 86°13.48'W: Dive 896-4, 21 Feb, 2460 m, six specimens (USNM 118184). Dive 983, 30 Nov, 2457 m, mussel bucket washings and crab trap residue, 13 specimens (USNM 118183). Dive 990, 7 Dec, 2451 m, wash- ings from crab trap, 1 specimen (USNM 118185). East Pacific Rise off western Mexico, 20°50’N, 109°06’W, Oasis Alvin dives in 1982: Dive 1220, 26 Apr, 2617 m, Riftia and Calyptogena washings, nine specimens (USNM 118182). Dive 1229, 14 May, 2615 m, Riftia, Calyptogena and Alvinella wash- ings, eight specimens (USNM 118186). Gulf of California, Guaymas Basin, dive VOLUME 102, NUMBER 1 of the A/vin in Jan 1982, 27°01'N, 111°25'W, 2020 m. Dive 1170, rock sample, two small specimens (USNM 118708). Dives of the Alvin in 1985, 27°00'N, 111°24’'W, 2000- 2009 m: Dive 1603, 25 Jul, Angel Rock, bacterial mat, Riftia washings, three spec- imens (USNM 118707). Dive 1607, 29 Jul, Lutz 2, bacterial mat, washings from rocks worms, one specimen (USNM 118706). Dive 1609, 1 Aug, Lutz 2, sediment, bottom of bucket of Bead Exp. no. 1, one minute specimen (USNM 118705). Dive 1615, 7 Aug, smoker in hydrothermal area, Riftia washings, 16 specimens (USNM 118709). Remarks.—Some specimens from the Guaymas Basin are larger than previously reported: up to 19 mm long, 9 mm wide, with 26 segments, compared to 13 mm long, 7 mm wide, with 25 segments. Distribution. —Gulf of California, East Pacific Rise at 21°N, and East Central Pacific in the Galapagos Rift, in 2020- 2633 m. Lepidonotopodium williamsae Pettibone Lepidonotopodium williamsae Pettibone, 1984b:857, figs. 5-7. Material. —East Central Pacific, from dives of the A/vin on two vent areas along the Galapagos Rift in 1979: Mussel Bed, 00°47.89'N, 86°21'W: Dive 991, 8 Dec, 2490 m, washings from mussels in mesh-lined milk crates and slurp samples from mussel wall, eight specimens (USNM 118118-—90). Rose Garden, 00°48.25'N, 86°13.48'W: Dive 990, 7 Dec, 2451 m, residue from re- trieval box containing vestimentiferans, two specimens (USNM 118187). East Pacific Rise off western Mexico, 20°50’N, 109°06’W, Oasis Alvin dive in 1982: Dive 1220, 26 Apr, 2617 m, Riftia and Calyptogena washings, three specimens (USNM 118188). Distribution. —Hydrothermal vents of Tropical East Pacific, Galapagos Rift and East Pacific Rise at 21°N, in 2451-2633 m. £SZ Subfamily Branchinotogluminae Pettibone, 1985 Genus Branchinotogluma Pettibone, 1985 Branchinotogluma grasslei Pettibone Branchinotogluma grasslei Pettibone, 1985b:457, figs. 5, 6; 1988: 215. Material. —East Central Pacific, Galapa- gos Rift, Alvin dives in 1979: Mussel Bed, 00°47.89'N, 86°09.21'W: Dive 991, 8 Dec, 2490 m, two slurp samples from mussel wall, three specimens (USNM 118151). Rose Garden, 00°48.25’N, 86°13.48’W: Dive 983, 30 Nov, 2457 m, mussel bucket washings, three specimens (USNM 118152). East Pacific Rise off western Mexico, Oa- sis Alvin dive in 1982, 20°50'N, 109°06’W: Dive 1220, 26 Apr, 2617 m, Riftia and Ca- lyptogena washings, one specimen (USNM 118150). Gulf of California, A/vin dive in Guaymas Basin in Jan 1982, 27°01'N, 111°25'W: Dive 1172, 2010 m, Box core no. 1, on slope of mound in area of sulfides, sediment covered with white material, one specimen (USNM 118699). Distribution. —Hydrothermal vents of Tropical East Pacific, Galapagos Rift and East Pacific Rise at 21°N; Gulf of California; Northeast Pacific, Explorer and Juan de Fuca Ridges, in 1495-2633 m. Branchinotogluma sandersi Pettibone Branchinotogluma sandersi Pettibone, 1985b:453, figs. 3, 4; 1988: 217. Material. —East Central Pacific, Galapa- gos Rift, Alvin dives in 1979: Mussel Bed, 00°47.89'N, 86°09.21'W: Dive 991, 8 Dec, 2490 m, two slurp samples from mussel wall, two specimens (USNM 118157). Rose Gar- den, 00°48.25'N, 86°13.48’W: Dive 983, 30 Nov, 2457 m, mussel bucket washings, one specimen (USNM 118156). Dive 988, 5 Dec, 2450 m, slurp sample from base of vesti- mentiferans, one specimen (USNM 118158). 158 East Pacific Rise off western Mexico, Oa- sis Alvin dive in 1982, 20°50'N, 109°06'W: Dive 1220, 26 Apr, 2617 m, Riftia and Ca- lyptogena washings, three specimens (USNM 118159). Gulf of California, A/vin dive in Guaymas Basin in 1985, 27°00'N, 111°24’W: Dive 1599, 13 Jul, 2009 m, Lutz 2, bacterial mat, washing from Rock Chimney, one specimen (USNM 118700). Distribution. —Hydrothermal vents of Tropical East Pacific, Galapagos Rift and East Pacific Rise at 21°N; Gulf of California; Northeast Pacific, Explorer and Juan de Fuca Ridges, in 1592-2633 m. Branchinotogluma hessleri Pettibone Branchinotogluma _ hessleri Pettibone, 1985b:450, figs. 1, 2. Material. —East Central Pacific, Galapa- gos Rift, dives of A/vin in 1979: Mussel Bed, 00°47.89'N, 86°09.21'W: Dive 991, 8 Dec, 2490 m, two slurp samples from mussel wall, three specimens (USNM 118164). Garden of Eden, 00°47.69°N, 86°07.74'W: Dive 993, 10 Dec, 2518 m, slurp sample from base of vestimentiferans, four specimens (USNM 118162). Rose Garden, 00°48.25’N, 86°13.48'W: Dive 983, 30 Nov, 2457 m, mussel bucket washings, three specimens (USNM 118161). Dive 988, 5 Dec, 2450 m, slurp sample from base of vestimenti- ferans, one specimen (USNM 118163). East Pacific Rise off western Mexico, Oa- sis A/vin dives in 1982, 20°50'N, 109°06'W: Dive 1220, 26 Apr, 2617 m, Riftia and Ca- lyptogena washings, 13 specimens (USNM 118160). Dive 1229, 14 May, 2615 m, Rif- tia, Calyptogena and Alvinella washings, 2 specimens (USNM 118165). Distribution. —Hydrothermal vents of Tropical East Pacific, Galapagos Rift and East Pacific Rise at 21°N, in 2450-2633 m. Opisthotrochopodus Pettibone, 1985 Opisthotrochopodus alvinus Pettibone Opisthotrochopodus alvinus Pettibone, 1985b:459, figs. 7-9. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Material. —East Central Pacific, Galapa- gos Rift, dives of A/vin in 1979: Mussel Bed, 00°47.89'N, 86°09.21'’W: Dive 991, 8 Dec, 2490 m, two slurp samples from mussel wall, one specimen (USNM 118179). Garden of Eden, 00°47.69'N, 86°07.74'W: Dive 993, 10 Dec, 2518 m, slurp sample from base of vestimentiferans, 2 specimens (USNM 118177). Rose Garden, O0°48225 Ne 86°13.48’W: Dive 983, 30 Nov, 2457 m, mussel bucket washings, 11 specimens (USNM 118174), crab trap residue, 2 spec- imens (USNM 118176). East Pacific Rise off western Mexico, Oa- sis Alvin dive in 1982, 20°50'N, 109°06’W: Dive 1220, 26 Apr, 2617 m, Riftia and Ca- lyptogena washings two specimens (USNM 118178). Distribution. —Hydrothermal vents of Tropical East Pacific, Galapagos Rift and East Pacific Rise at 21°N, in 2451-2633 m. Branchinotogluma sp. A [Young of B. hessleri or O. alvinus] Branchinotogluma sp. A Pettibone, 1985b: 466. Material. —East Central Pacific, from dives of A/vin along Galapagos Rift in 1979: Mussel Bed: Dive 991, 8 Dec, 2490 m, slurp sample from mussel wall, nine young spec- imens (USNM 118154). Garden of Eden: Dive 993, 10 Dec, 2518 m, slurp sample from base of vestimentiferans, two young specimens (USNM 118155). Rose Garden: Dive 983, 30 Nov, 2457 m, mussel bucket washings, 10 young specimens (USNM 118153). Remarks. —Adults of the above two species were collected on the same dives. Branchinotogluma sp. B [Young of B. grasslei or B. sandersi| Branchinotogluma sp. B Pettibone, 1985b: 466. Material. —East Central Pacific, from dives of Alvin along Galapagos Rift in 1979: Rose Garden: Dive 983, 30 Nov, 2457 m, VOLUME 102, NUMBER 1 mussel bucket washings, 11 young speci- mens (USNM 118149). Gulf of California, A/vin dive in Guaymas Basin in 1985, 27°00’N, 111°24’W: Dive 1603, 25 Jul, 2004 m, Angel Rock, bacterial mat, Riftia washings, one small specimen (USNM 118701). Remarks. —Adults of the above two species were collected on the same dives. Subfamily Branchiplicatinae Pettibone, 1985 Genus Branchiplicatus Pettibone, 1985 Branchiplicatus cupreus Pettibone Branchiplicatus cupreus Pettibone, 1985a: 151, figs. 1-4. Material. —Gulf of California, Alvin dive in Guaymas Basin in 1982, 27°01'N, 111°25’W: Dive 1169-001, 11-20 Jan, 2020 m, rock sample, one specimen (USNM 118702). Alvin dive in 1985, 27°00’N, 111°24’W: Dive 1615, 7 Aug, 2000 m, smoker 1, hydrothermal area, Riftia wash- ings, one specimen (USNM 118703). Distribution. —Hydrothermal vents in Gulf of California and East Pacific Rise at 21°N, in 2000-2633 m. Subfamily Macellicephalinae Hartmann- Schroder, 1971, emended Pettibone, 1976 Genus Levensteiniella Pettibone, 1985 Levensteiniella kincaidi Pettibone Levensteiniella kincaidi Pettibone, 1985c: 471, figs. 1-3; 1988:215. Material. —East Central Pacific, Galapa- gos Rift, dives of A/vin in 1979: Mussel Bed, 00°47.89'N, 86°09.21'W: Dive 986, 3 Dec, 2494 m, mussel bucket washings, three specimens (USNM 118196). Dive 991, 8 Dec, 2490 m, slurp samples from mussel wall, four young specimens (USNM 118194). Garden of Eden, 00°47.69'W, 86°07.74'W: Dive 993, 10 Dec, 2518 m, slurp sample from base of vestimentiferans, 29 young specimens (USNM 118191). Rose Garden, 00°48.25'W, 86°13.48'W: Dive 983, 159 30 Nov, mussel bucket washings, 20 young specimens (USNM 118197). Dive 988, 5 Dec, 2450 m, slurp sample from base of vestimentiferans, one specimen (USNM 118192). East Pacific Rise off western Mexico, 20°50’N, 109°06’W, Oasis Alvin dives in 1982: Dive 1220, 26 Apr, 2617 m, Riftia and Calyptogena washings, 10 specimens (4 young, USNM 118195). Dive 1229, 14 May, 2616 m, Riftia, Calyptogena and Alvinella washings, small specimen (USNM 118193). Distribution. —Hydrothermal vents of Tropical East Pacific: Galapagos Rift and East Pacific Rise at 21°N; Northeast Pacific, Explorer and Juan de Fuca Ridges, in 1818- 2633 m. Genus Bathykurila Pettibone, 1976 Bathykurila guaymasensis, new species Bigs. h.2 Material. —Gulf of California, Alvin dive in Guaymas Basin in Jan 1982, 27°01'N, 111°25’°W: Dive 1176, 2020 m, Box core 2, taken over vent, with numerous nuculanid bivalves, 2d, holotype (USNM 118694) and paratype (USNM 118695); sec. B, paratype (USNM 118696). Alvin dive in 8 Aug 1985, 27°00’N, 111°24’W: Dive 1614, 2004 m, Angel Rock, bacterial mat, Box core 5, sub- core B, 0-5 cm, paratype (USNSM 118697), subcore, C, 0-3 cm, paratype (USNM 118698). Description. —Length of holotype 8 mm, width with setae 5 mm, segments 15; length of two larger paratypes 7 mm, width 5 mm, segments 14; length of two smaller para- types 3-4 mm, width 3-3.5 mm, segments 15. Body fusiform, flattened, with parapo- dia and setae very long, projecting, longer than body width (Fig. 1A, B). Elytra (mostly missing) and large, bul- bous elytrophores (Figs. 1A, B, 2A) seven pairs, on segments 2, 4, 5, 7, 9, 11, and 13. Elytra large, oval, covering dorsum, deli- cate, with larger conical to rounded tuber- cles variable in size on posterior and lateral borders, with smaller ones scattered on sur- 160 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig-T. Bathykurila guaymasensis, A, B, holotype, USNM 118694; C, paratype, USNM 118698; D, paratype, USNM 118695: A, Dorsal view of anterior end, acicula in tentaculophores of lst segment dotted; B, Dorsal view of posterior end (segments 12-15); C, Ventral view of posterior end (segments 10-14), anal cirri and most of ventral cirri broken off; D, Border papillae on dorsal side of pharynx (dissected). Scales = 0.5 mm for A, B; 1.0 mm for C; 0.1 mm for D. face (Fig. 2F): larger tubercles not usual type, not chitinous, not sharply set off from sur- face. Dorsal tubercles on cirrigerous seg- ments large, bulbous to nodular (Figs. 1A, B, 2B). Prostomium oval, deeply bilobed; trian- gular anterior continuations of prostomium with small frontal filaments; median anten- na with small ceratophore in anterior notch, with short subulate style; without lateral an- tennae and eyes; palps stout, tapered, about two times longer than prostomium (Fig. 1A). First or tentacular segment fused to prosto- mium, not visible dorsally; tentaculophores lateral to prostomium, each with prominent acicular lobe on inner side, without setae, and pair of subulate tentacular cirri, shorter than palps; upper lip large, bilobed (Fig. 1A). Second or buccal segment with first pair of elytrophores, biramous parapodia and ven- tral or buccal cirri lateral to ventral mouth, longer than following ventral cirri (Fig. 1A). Parapodia biramous, with notopodia shorter and smaller than neuroodia (Fig. 2A, B.) Notopodium rounded basally, with pro- jecting acicular lobe on lower side; neuro- podium with conical projecting presetal acicular lobe and shorter, rounded postsetal lobe. Notosetae numerous, short to longer, forming radiating bundles, stouter than neurosetae, with row of widely spaced teeth (4-11) along one side and blunt tips (Fig. 2C). Neurosetae very numerous, forming fan-shaped bundles; supraacicular neuro- setae with longer spinous regions and two rows of long spines, tapering to bluntly pointed bare tips (Fig. 2D); subacicular neu- rosetae with shorter spinous regions, close- set short spines, and tapered bare tips (Fig. 2E). Dorsal cirri with cylindrical cirro- phores on posterior sides of notopodia, shorter than notopodia, with styles wider basally and long slender tips extending to tips of setae or beyond (Figs. 1A, B, 2B). VOLUME 102, NUMBER 1 161 ¢ c c ¢ is € © ¢ ie ee ee ee SSS) Mm C D Fig. 2. Bathykurila guaymasensis, holotype, USNM 118694: A, Right elytragerous parapodium, anterior view, acicula dotted; B, Right cirrigerous parapodium, posterior view; C, Notosetae; D, Supraacicular neuroseta; E, Subacicular neuroseta; F, Right elytron. Scales = 0.5 mm for A, B; 0.1 mm for C-E; 0.5 mm for F. Ventral cirri attached on middle of neuro- podia, short, tapered (Fig. 2A, B). Pair of long ventral papillae usually pres- ent on segment 11 (present on four of five specimens), sometimes extending far be- yond posterior end, with yellowish secretion inside (Fig. 1C). Posterior 2 segments (14, 15) smaller, enclosed in elytragerous seg- ment 13 (Fig. 1B); segment 14 with dorsal cirri; segment 15 smaller, without dorsal cirri (Fig. 1B), or segment absent (Fig. 1C); py- gidium long, slender, wedged between par- apodia of segment 15, with pair of slender, short anal cirri (Fig. 1B). Pharynx (dissected) with opening encir- cled by eight pairs of border papillae (Fig. 1D), and two pairs of heavy, hooked jaws. Etymology.—The species is named for the collecting site, the Guaymas Basin. Remarks.—Bathykurila guaymasensis is close to B. zenkevitchi (Uschakov 1955, fig. la-—c; Pettibone 1976, fig. 24a—d), the type species of Bathykurila, from the Kurile- Kamchatka Trench in the northwest Pacific, in 8100 m. They differ as indicated in Ta- ble 1. Subfamily Macellicephaloidinae Pettibone, 1976 Genus Macellicephaloides Uschakov, 1955 Type species.—Macellicephaloides gran- dicirrus Uschakov, 1955 (as grandicirra). Gender: masculine (according to the Code, Art. 30.a.i1, names ending in -oides should be masculine, not feminine, as indicated by Pettibone 1976:42). Table 1.— Differences between Bathykurila zenkevit- chi (Uschakov) and Bathykurila guaymasensis, n. sp. Character B. zenkevitchi B. guaymasensis Tentacular about as long as _ shorter than palps cirri palps Notopodia as long as or shorter than neu- longer than ropodia neuropodia Cirrophore longer than no- shorter than no- of dorsal topodia topodia cirri Ventral pa- 4 pairs on seg- | pair on segment pillae ments 10-13 11 Length 15-21 mm 3-8 mm Width 12 mm 3-5 mm Segments 1S 14-15 162 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 3. Macellicephaloides alvini, holotype, USNM 118704: A, Dorsal view of anterior end, styles of median antenna, tentacular cirri, and dorsal cirri of segment 3 missing, right parapodia of segments 2 and 3 damaged or not developed; B, Ventral view of anterior end, ventral cirri missing; C, Dorsal view of posterior end (segments 13-17), elytra and styles of dorsal cirri missing. Scale = 1.0 mm for A-C. Macellicephaloides alvini, new species Figs. 3, 4 Material. —Gulf of California, Alvin dive in Guaymas Basin, F. Grassle, collector, Dive 1614, 6 Aug 1985, 27°00’N, 111°24'W: 2004 m, Angel Rock, bacterial mat, Box core 5, subcore D, holotype (USNM 118704). Description. — Length of holotype 7.5 mm, width with setae 4 mm, segments 17. Body flattened dorsoventrally, tapering slightly anteriorly and more so posteriorly, with parapodia of 5 posterior segments directed posteriorly (Fig. 3C). Integument smooth, not papillate. Elytra (all missing) and large, bulbous elytrophores eight pairs, on seg- ments 2; 4,5, 7,9, 115 13sand 15 (Figs.3A, C, 4A). Dorsal tubercles on cirrigerous seg- ments indistinct. Prostomium (poor condition) withdrawn and fused to tentacular segment, oval, slightly bilobed; ceratophore of median an- tenna in middle of prostomium, style miss- ing; palps on short palpophores, rather short, tapering; without lateral antennae and eyes (Fig. 3A, B). Tentacular segment distinct dorsally, ventrally forming upper, lateral, and posterior lips of ventral mouth; tenta- culophores of dorsal and ventral cirri short, lateral to prostomium, styles missing (Fig. 3A, B). Segment 2 with first pair of elytro- phores and elongate parapodia; ventral cirri missing; deep depression in middle of ven- tral surface, covered by large, oval flap at- tached to segment 3 (Fig. 3A, B). Parapodia subbiramous; notopodium bulbous basally, with projecting, stout, am- ber-colored notoaciculum, without noto- setae (Fig. 4A—C); neuropodium elongated, with projecting acicular lobe; neurosetae numerous, delicate, slender, slightly wider basally, tapering to slender tips, with two rows of delicate spines (Fig. 4A, B, D). Pos- terior five segments with notoacicula stou- ter, projecting beyond neuropodia (Fig. 3C). Dorsal cirri with rather long, thick, cylin- drical cirrophores on posterior dorsal sides of notopodia; styles missing (Fig. 4B). Ven- tral cirri missing. Pygidium rounded, enclosed in parapo- dia of last segment (Fig. 3C). Pharynx (dis- sected) large, muscular; anterior end encir- cled with papillae, number and arrangement not evident but with longer lateral pair (not extra long as in M. vitiazi); two pairs of long V-shaped hooked jaws; dorsal pair fused medially, with additional median piece (Fig. VOLUME 102, NUMBER 1 163 Fig. 4. Macellicephaloides alvini, holotype, USNM 118704: A, Right elytragerous parapodium from segment 7, anterior view, acicula dotted, elytron and ventral cirri missing; B, Right cirrigerous parapodium of segment 8, posterior view, styles of dorsal and ventral cirri missing; C, Notoaciculum from same; D, Neuroseta from same, with detail of parts; E, Dorsal jaws, outer view; F, Same, inner view; G, Ventral jaws, outer view; H, Same, inner view. Scales = 0.5 mm for A, B; 0.1 mm for C—H. 4E, F); ventral pair denticulate on inner side (Fig. 4G, H). Etymology.—The species is named for the collecting submersible, DSRV Alvin. Remarks on the genus Macellicephaloides Uschakov, 1955, and the subfamily Macel- licephaloidinae Pettibone, 1976: Of partic- ular interest is the find of a single specimen from the Guaymas Basin that seems to fit into the genus Macellicephaloides, estab- lished by Uschakov (1955) for three ultra-abyssal species, M. grandicirrus, M. verrucosus, and M. vitiazi, from the Kurile- Kamchatka Trench in 7210-9950 m. Us- chakov placed the genus under Aphroditi- dae: Polynoinae. An additional species, M. uschakovi, was added to the genus from the same area in 8120 m by Levenstein (1971). In her catalogue, Hartman (1959:93) placed Macellicephaloides under Polynoi- dae: Lepidonotinae, and selected M. gran- dicirrus as the type species. Hartmann- Schroder (1974), in her revision of the subfamily Macellicephalinae Hartmann- Schroder, 1971, included Macellicepha- loides in the subfamily. As a part of my revision of the genus Macellicephala and the subfamily Macellicephalinae Hartmann- Schroder, I established the new subfamily Macellicephaloidinae for Macellicepha- 164 loides and the above four species, with sup- plementary descriptions, based on speci- mens sent in exchange by P. Uschakov and R. Levenstein. Levenstein (1975) added an additional species, M. sandvichensis, from the South Sandwich Trench in 7200-7934 m. Another species, M. villosus, was added by Leven- stein (1982) from the Japan Trench in 7370- 7380 m. Levenstein (1983) added a seventh species, M. improvisus, from the Kurile- Kamchatka Trench in 8035-8120 m and included a Key to the seven species of Ma- cellicephaloides. It probably should be not- ed that Uschakov (1982) did not recognize the subfamily Macellicephaloidinae and other subfamilies proposed by Pettibone but included the genus under Macellicephali- nae. In her review of the genera and species of the deep-sea polynoid subfamilies in the world oceans, Levenstein (1984:83, fig. 4) indicated that the distributional pattern of the Macellicephaloidinae showed a western Pacific origin, since six of the seven species of the genus Macellicephaloides were known to inhabit trenches of the western Pacific and only one species was known to inhabit the Atlantic sector of the Antarctic Ocean, the South Sandwich Trench. She suggested that representatives of this genus (or its ancestor) were probably widely distributed in the abyssal region of the Pacific Ocean and gave rise to species adapted to life in the oceanic trenches, producing the ultra- abyssal fauna of this subfamily. The pres- ence of M. sandvichensis in the South Sand- wich Trench could be explained on the basis of a close connection between the deep-sea faunas of the Pacific and Atlantic sectors of the Antarctic. The new species, M. alvini from 4000-5000 m shallower waters in the Gulf of California, might be considered to be close to the ancestor of the genus. It is considerably smaller than representatives from the other areas. All eight species have a relatively small number of segments (16-21, 1st achaetous) and eight pairs of elytrophores (elytra all PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON missing) on segments 2, 4, 5, 7, 9, 11, 13, and 15. The prostomium is relatively small, bilobed, with the ceratophore of the median antenna in the middle of the prostomium and with palps but without lateral antennae or eyes. The first or tentacular segment en- closes the prostomium and is distinct dor- sally, with two pairs of tentacular cirri on tentaculophores, but without acicular lobes or setae; ventrally the tentacular segment forms the upper, lateral, and posterior lips of the ventral mouth. The second segment has the first pair of elytrophores, large par- apodia, and ventral cirri, with a deep mid- ventral depression covered by a large oval flap attached to segment 3 (as in M. alvini, Fig. 3B) or a rectangular flap (as in M. gran- dicirrus, Pettibone, 1976, fig. 25b). Para- podia are elongate, subbiramous, the no- topodium represented by a conical lobe with a more or less projecting, stout notoacicu- lum, without notosetae; the neuropodium is conical, with numerous, slender neuro- setae. Dorsal cirri on the non-elytragerous segments have moderately to very long, cy- lindrical cirrophores and short styles; dorsal tubercles are indistinct or rarely nodular, as in M. verrucosus. Ventral cirri are short. The pygidium is enclosed in the long parapodia of a variable number of posterior segments, and without anal cirri. The integument is smooth, rarely papillate dorsally, as in M. villosus, or with middorsal nodular tuber- cles, asin M. verrucosus. The large muscular pharynx has two pairs of hooked jaws and distal papillae, the lateral pair of papillae longer than the others. Lateral papillae sometimes very long, as in M. vitiazi (Pet- tibone, 1976, fig. 26c) and M. sandvichensis (Levenstein, 1975, fig. 3a), and similar to those of the pelagic polychaete family AI- ciopidae. Key to the Species of Macellicephaloides b. Segments '6tor 7.22 eae 2 =) ‘Segments tS: 071 20-21), 2a eee 6 2. Segments. 16) b. &. HO) See 3 =, Segments l7is 24. Bi ee ee 4 VOLUME 102, NUMBER 1 165 SS Cle oS “et WSss = = D Fig. 5. Neoleanira racemosa, USNM 118714: A, Dorsal view of anterior end, ventral tentacular cirri not visible; left dorsal cirrus on segment 3 broken off; B, Right tentacular parapodium, outer view, aciculum dotted; C, Right elytragerous parapodium from segment 2, anterior view, acicula dotted; D, Right cirrigerous parapodium from segment 3, posterior view; E, Right elytragerous parapodium from segment 4, anterior view, acicula dotted. Scales = 1.0 mm for A; 0.5 mm for B—E. au, auricle; br, branchia; ct, ctenidium; dc, dorsal cirrus; dtc, dorsal tentacular cirrus; itl, inner tentacular lobe; lan, lateral antenna; man, median antenna; pa, palp; st, stylode; vtc, ventral tentacular cirrus. 3. With paired, nodular dorsal tuber- ments. Pharynx with lateral papillae cles on cirrigerous segments 6-14 MISE ERA IOs ee cen age NE ee 3 and middorsal tubercles on seg- 5. Cirrophores of dorsal cirri extend- ments 3-15 (Uschakov 1955, fig. 3; ing far beyond tips of neuropodia 1982, pl. 12; Pettibone 1976, fig. 27 (Uschakov 1955, fig. 2; 1982, pl. 11: oe eee M. verrucosus Uschakov Petibone, 197.6. fie.25)=...: -h4 enn —wymnout Gorsal tubercles On. Gifi- .... | 6 nk beet eus- M. grandicirrus Uschakov gerous segments and middorsal tu- — Cirrophores of dorsal cirri not as bercles (Uschakov 1955S, fig. 4; 1982, long, extending to tips of neuropo- pl 13; Pettibone 1976, fig. 26)... dia or shorter (Figs. 3, 4) ........ a ee M. vitiazi Uschakov ieee tegen lla VINE HCW SPeGiEs 4. Notoacicula not extra stout or long. 6. Segments 18. Cirrophores of dorsal Cirrophores of dorsal cirri extend- cirri very short. Notopodia with ing to about tips of neuropodia. flexible, thin acicula (Levenstein Pharynx with pair of very long lat- POSS ie Ae) ee Sy ae Bee peal papillae (Pevensicein lOVS AGS... 6) on de Suan woe ce M. improvisus Levenstein SW Rha ve: 2. M. sandvichensis Levenstein — Segments 20-21. Notopodia other- — Notoacicula stout, extending far be- WISE darian Paces ss ari Sa, Se 7 yond neuropodia in posterior seg- 7. Dorsal side of body with conical pa- 166 LL PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Zz SS —— ———- 7 (Dec 1 pair lost; — _ 1986) F 4.0 mm, M 2.6 mm, eggs (ZMA Moll. 3.88.007— 008, left on host) 6 (Dec O 2.0 mm, — — 1986) O 2.0 mm (ZMA Moll. 3.88.009— 010) vaCDee O27 nim. — — 1986) O 2.2 mm (ZMA Moll. 3.88.01 1- 012) —_—_—_—_—_—_—_—_—_—_—_—_—_—_—_—_——_—_ Table 1.—Continued. Specimen mid number T. eucidaricola S. troglodytes n. sp 8 (Dec O 1.6 mm, — — 1986) O 0.6 mm (ZMA Moll. 3.88.013- 014) 9 (Dec F 3.6 mm, empty gall 2 1986) M 2.0 mm (USNM 859313); F 4.8 mm (holotype), M 2.6 mm (allotype) (ZMA Moll. 3.88.004 and 005) 10 (Dec — O 0.6 mm, on — 1986) spine 11 (Dec — 1 gall with — 1986) M 2.2 mm, M 2.2 mm, M 1.8 mm, M 1.8 mm (Fig. 15). prosocline. Outer lip thickened, with the most protruding part situated one-seventh of total height from suture. Inner lip thick- ened, reflected over columella. Height of holotype 4.68 mm (larval shell broken). Soft parts (based on rehydrated speci- mens): Head-foot can be almost completely retracted into pallial cavity. Animal pig- mented with bright red, especially along right side of visceral mass. Tentacles short, flat- tened, with subcutaneous eyes situated somewhat laterally to center of bases, meet- ing above snout to form a “V.”’ Snout large, cylindrical, with distal attachment disc with anterior notch and central proboscis open- ing. Foot smaller than snout, shapeless but with distinct opercular lobes and large oper- culum. One large pedal fold on each side of foot. Body of holotype consisting of 2.5 whorls, of which pallial cavity occupies 0.5. Holotype female with large closed pallial Oviduct, no penis. Gill with about 25 low VOLUME 102, NUMBER 1 Figs. 1-6. 1, Trochostilifer eucidaricola new species, recently settled larva, from host 8, 0.67 mm; 2, Sabinella troglodytes, recently settled larva from host 10, 0.67 mm; 3-6, Trochostilifer eucidaricola new species; 3, apex of allotype, 0.65 mm of larval shell visible; 4, holotype, 4.68 mm; 5, female paratype from host 2, 3.6 mm; 6, male paratype from host 2, 2.6 mm. We Figs. 7-8. Trochostilifer eucidaricola, operculum, female and male, maximum diameter 1.4 and 0.79 mm respectively. leaflets, occupying almost all space between osphradium and oviduct. Hypobranchial gland anteriorly occupying small, short, tri- angular area between gill and oviduct, pos- Figs. 9-11. respectively. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON teriorly forming a very narrow band. Os- phradium a simple low ridge in shallow furrow to the left of and along whole length of gill. Operculum (Figs. 7—8) yellowish, thin, paucispiral with thickened part inside the nucleus serving as a muscular attachment. Male: In fully grown pairs it is less than 0.6 the size of the female. Shell consisting of up to 2.5 teleoconch whorls of shape identical to corresponding whorls of female. Soft parts similar to those of female, but with a simple tentacle-like penis curving forwards, to the right and then backwards along right side of pallial cavity. No trace of female reproductive organs seen. Height of allotype 2.72 mm. Remarks. —Specimens of T. eucidaricola and Sabinella troglodytes can easily be dis- tinguished by the apical teleoconch whorls which are strongly shouldered in 7. euci- daricola and evenly convex in S. troglo- Sabinella troglodytes, female (Fig. 9) and two males from host 3, height 4.6, 2.2, and 2.3 mm VOLUME 102, NUMBER 1 173 Figs. 12-15. 12, Epidermal fold formed by the host, normally covering distal part of snout of Sabinella troglodytes, detail of lower left scar in Fig. 13; 13, Spine of Eucidaris tribuloides with deformed (cf. Fig. 15) gall caused by S. troglodytes, apical view. The spine has formed 3 “‘secondary”’ spines at a right angle to the axis of the original spine. Four attachment scars of epidermal tissue visible. Maximum diameter of spine 5 mm; 14, Eucidaris tribuloides, host 1, with male and female of Trochostilifer eucidaricola. Primary spine just to the right and dorsal to the pair has been removed to show the pair better. Diameter of test 20 mm; 15, normally formed gall caused by Sabinella troglodytes, host 11, length 9.7 mm. dytes. Monogamus minibulla (Olsson & much smaller species, ca. 1.5 mm; it has a McGinty, 1958) bears some resemblance to larval shell of about 1.0 whorl and is para- T. eucidaricola in having the first part ofthe _ sitic on the sea urchin Echinometra lucunter teloconch distinctly shouldered, but is a (L.) (Warén, unpub. data). 174 Among the described species of Trochos- tilifer only T. striatus bears any resemblance to T. eucidaricola. The other species of the genus have a shell of typical ““7rochus shape” and live in galls in the spines of their hosts. Trochostilifer striatus can, however, easily be distinguished by having a much more distinct spiral sculpture, a larval shell of 1.5 whorls and by having evenly convex apical whorls. The newly settled larva (Fig. 1) is virtually indistinguishable from that of Sabinella troglodytes (Fig. 2), but it 1s possible that they can be distinguished by the preferred site on the host, because the specimen in Fig. 2 had already started to deform the spine where it was found. This is also the basis for our determination of these two specimens. These determinations are not contradicted by the shape and size of the larval shells of specimens with enough post- larval growth to allow identification by the shape of the teleoconch. Several dozen specimens of the host ur- chin were examined and of these 8 were parasitized by this new species. These spec- imens are enumerated in Table 1. During the examination two more species of eu- limids were found on Eucidaris, viz. Sabi- nella troglodytes (Thiele, 1925) (Figs. 9-13, 15) and specimens of an undescribed, small, slender, straight-sided species. Because of problems with generic assignment of such species, and because they seemed juvenile, the latter are left undescribed. A few years ago the senior author ex- amined all material of Eucidaris tribuloides in USNM and found several specimens par- asitized by Sabinella troglodytes from the Caribbean area. No specimens of Trochos- tilifer eucidaricola were then noticed and we assume it to be a more rare and/or locally distributed species. Sabinella troglodytes lives in galls of the spines of the host and has been reported in the literature several times (Warén 1984). We figure the latter species for comparison, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON together with two galls. These specimens are also listed in Table 1. Trochostilifer eucidaricola lives attached to the test of the host by the disc-shaped distal part of the snout, and it seems very unlikely that it is able to move. In the center of the scar on the test of the host there is a very narrow hole, probably caused by the proboscis, but in these dried specimens it proved impossible to trace the proboscis to find the precise way of parasitism. The spec- imens were almost always attached in cou- ples, between a row of primary spines and the peristome. In two cases also the egg cap- sules, small globular sacs, were present, at- tached to the test by a short stalk. Each capsule contained 100-300 eggs, embryos, or veliger larvae ready to hatch. The di- ameter of the shell of the veligers, consisting of about 0.5 whorls is about 90 wm. This clearly shows that the species has plankto- trophic development. In the five cases when the sex of the spec- imens in a pair could be determined, the couples consisted of a small male and a larg- er female. In one case the sex could not be determined, because the specimens had not begun to develop a penis or pallial oviduct. A single specimen was found only on one host, which clearly shows that the distri- bution is not random, but that larvae prefer to settle on a host already parasitized by a single specimen. Acknowledgments We thank Mrs. Ineke Peeters, Aruba, who collected the sea urchins and most kindly allowed us to describe their molluscan fau- na, and Frere Fredericus, who forwarded the material to ZMA. Literature Cited Hedley, C. 1900. Studies on Australian Mollusca. 2.—Proceedings of the Linnean Society of New South Wales 26:16-25. Olsson, A. A., & T. L. McGinty. 1958. Recent marine VOLUME 102, NUMBER 1 mollusks from the Caribbean coast of Panama with the description of some new genera and species.— Bulletins of American Paleontology 39(177):1-58. Thiele, J. 1925. Gastropoda der deutschen Tiefsee- Expedition. II. Teil. — Wissenschaftliche Ergeb- nisse der deutschen Tiefsee-Expedition auf dem Dampfer “Valdivia” 1898-1899 7(2):36—-382. Warén, A. 1980. Descriptions of new taxa of Eulim- idae (Mollusca, Prosobranchia) with notes on some previously described genera.— Zoologica Scripta 9:283-306. Wes) . 1984. A generic revision of the family Eulim- idae (Gastropoda, Prosobranchia).—The Jour- nal of Molluscan Studies, Supplement 13. 96 pp. (AW) Swedish Museum of Natural His- tory, Box 50007, S-10405 Stockholm, Swe- den; (RM) Zoological Museum, Postbus 20125, 1000 HC Amsterdam, The Neth- erlands. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 176-248 SPRINGSNAILS (GASTROPODA: HYDROBIIDAE) OF OWENS AND AMARGOSA RIVER (EXCLUSIVE OF ASH MEADOWS) DRAINAGES, DEATH VALLEY SYSTEM, CALIFORNIA-NEVADA Robert Hershler Abstract. — Thirteen springsnail species (9 new) belonging to Pyrgulopsis Call & Pilsbry, 1886, and Tryonia Stimpson, 1865 are recorded from the region encompassing pluvial Owens and Amargosa River (exclusive of Ash Meadows) drainages in southeastern California and southwestern Nevada. Discriminant analyses utilizing shell morphometric data confirmed distinctiveness of the nine new species described herein, as: Pyrgulopsis aardahli, P. amargosae, P. owenensis, P. pertubata, P. wongi, Tyronia margae, T. robusta, T. rowlandsi, and 7. salina. Of the 22 springsnails known from Death Valley System, 17 have very localized distributions, with endemic fauna concentrated in Owens Valley, Death Valley, and Ash Meadows. A preliminary analysis showed only partial correlation between modern springsnail zoogeography and configuration of inter-connected Pleistocene lakes comprising the Death Valley System. This constitutes the second part of a sys- tematic treatment of springsnails from the Death Valley System, a large desert region in southeastern California and southwest- ern Nevada integrated by a series of lakes during Pleistocene times. An earlier paper (Hershler & Sada 1987) dealt with the Ash Meadows faunule, while this document pro- vides descriptions of fauna collected during 1985-1987 survey of much of remaining portions of the System, including waters in Mono, Adobe, Long, Owens, Indian Wells, Panamint, and Death Valleys; Amargosa River drainage; and some areas adjacent to the above (Fig. 1). A brief discussion of springsnail zoogeography also is provided, although a more extensive treatment will be given following survey of remaining por- tions of Death Valley System (notably Mo- jave River drainage) and additional periph- eral areas. List of Recognized Taxa Pyrgulopsis aardahli, new species. P. amargosae, new species. P. micrococcus (Pilsbry, 1893). P. owensensis, new species. P. perturbata, new species. P. cf. stearnsiana (Pilsbry, 1899). P. wongi, new species. Tryonia margae, new species. T. protea (Gould, 1855). T. robusta, new species. T. rowlandsi, new species. T. salina, new species. T. variegata Hershler & Sada, 1987. Materials and Methods Localities visited, consisting of low- to mid-elevation (<2500 m) springs and pe- rennial streams, are shown in Figs. 2—7 and listed in the Appendix. Snails were found VOLUME 102, NUMBER 1 Deep Springs Valley oO (e) = rs) = o 50 Kilometers Fig. 1. area. Stippled areas indicate mountain ranges. in springs of varying sizes and appearance as well as low- to moderate-energy (spring- fed) streams. Photographs of representative sites are in Figs. 8 and 9. Snails were relaxed in the field with men- thol crystals, fixed in 4% buffered formalin and preserved in 70% ETOH. Material was collected by author unless otherwise indi- 177 Map showing desert basins of southeastern California and southwestern Nevada comprising study cated. Water temperature and conductivity were measured with a temperature-com- pensated, HACH 16300 conductivity me- ter. Methods of anatomical study and pho- tography of shells and other morphologic features are routine (Hershler & Sada 1987). Generalized radular formulae are based on 178 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Table 1.—Selected shell parameters for Pyrgulopsis species. Shell height (SH) and width (SW) are given in mm. Data for each population include mean values (upper line) and standard deviations (lower). Number of populations and specimens for which data were obtained are given in parentheses. NW = number of whorls, T = translation rate, D = distance of generating curve from coiling axis, AS = aperture shape, W = whorl expansion rate. Species NW SH P. aardahli 3.98 2.90 Ci To) G5 O21 P. amargosae 3.86 L977, (3, 45) 0.20 0.28 P. crystalis S51 2.02 €.3) 0.29 0.24 P. erythropoma 3.46 2.00 (5, 68) O27 0.31 P. fairbanksensis 3:29 2.67 (1, 14) 0.34 O21 P. isolata 4.00 245 (1; 13) 0.14 0.13 P. micrococcus 4.16 2.16 (27, 362) 0.33 0.31 P. nanus 5555) 1.74 (3, 42) 0.24 1.74 P. owensensis 3.61 2.16 (6, 86) 0.26 0.28 P. perturbata 4.37 3:29 (3,39) 0.19 0.39 P. pisteri 3.97 2-3 (2; 31) O:27 0.18 P. cf. stearnsiana 4.14 22 (25) 0.15 0.18 P. wongi 3.86 ZA (19, 286) 0.27 0.39 Parameter SW a D AS W 2.20 4.24 0.56 es 2A 0.20 0.54 0.04 0.04 0.19 1.45 4.43 0.57 1.14 2.03 0.25 0.67 0.05 0.06 0.21 £95 3.44 0.50 1.18 2.56 0.18 0.32 0.05 ~ 0.06 0.76 1.82 S332 0.56 Ici 2.13 0.24 0.64 0.05 0.06 0.87 2.28 4.23 0.61 1.09 2.80 0.15 1.03 0.09 0.13 0.07 2.18 3.81 0.58 Le 2.09 0.11 0.36 0.03 0.04 0.20 1.42 S17 0.62 1.19 1.89 0.17 1.05 0.06 0.08 0.28 53 S252 0.55 1.09 2.44 1253 3.52 0.55 1.09 0.34 1.62 4.56 0.59 1.16 2.08 0.18 0.98 0.05 0.05 0.24 apap 5.26 0.62 1.18 2.01 0.31 0.85 0.62 1.18 0.19 1.99 3.46 0.54 1.10 Dest, 0.13 0.45 0.04 0.04 0.31 1.68 I 0.61 1.24 |S 0.12 1s | 0.05 0.06 0.21 ey, 4.10 0:59 | be 2.28 0.24 0.70 0.05 0.05 0.29 examination of SEM micrographs from varying numbers of populations, and are presented in following order of tooth types: centrals, laterals, inner marginals, outer marginals. Whorl counts, standard measurements, and Raupian parameters were obtained from selected series of live-collected, adult spec- imens, recognizable by their complete and thickened inner shell lips. After whorls were counted (NW), shells were imbedded in clay with aperture facing up and coiling axis per- pendicular to the observer’s line of sight. Shell outlines were traced using camera lu- cida (25 x or 50) and points on these dig- itized for calculation of the following pa- rameters (largely following Kohn & Riggs 1975): shell height (SH), shell width (SW), length of body whorl (LBW), width of body whorl (WBW), aperture length (AL), aper- ture width (AW), translation rate (T), whorl expansion rate (W), distance of generating curve from coiling axis (D), and aperture shape (SA). In order to facilitate compari- sons, these parameters were also obtained from the entire set of shells of Ash Meadows springsnails used in an earlier morphomet- ric study (which involved generation of a subset of the above parameters using a somewhat different methodology; Hershler VOLUME 102, NUMBER 1 iZ9 Table 2.—Selected shell parameters for 7ryonia species. Shell height (SH) and width (SW) are given in mm. Data for each population include mean values (upper line) and standard deviations (lower). Number of popu- lations and specimens for which data were obtained are given in parentheses. NW = number of whorls, T = translation rate, D = distance of generating curve from coiling axis, AS = aperture shape, W = whorl expansion rate. Parameter Species NW SH SW T D AS WwW T. angulata 5:10 3.24 1.56 1.99 0.58 1.50 1.66 39) 0.52 O37 0.19 29 0.07 0.08 O22 T. elata noo 1.96 0.82 8.96 0.59 1.34 1.42 (2, 30) 0.53 0.29 0.07 ts 0.05 0.08 0.11 T. ericae 4.71 1.40 0.76 6.42 0.57 125 1.65 (2, 19) 0.66 0.19 0.06 1.06 0.06 0.06 0.11 T. margae 6.21 218 0.98 10.80 0.59 1.48 | Bes (1;°6) 0.10 Qeh2 0.02 0.93 0.59 0.03 0.19 T. protea 5233 3.53 eg 9.45 0.66 1.38 L351 (1, 6) 0.52 0.45 0.13 0.86 0.04 0.05 0.19 T. robusta 4.22 1.63 1.06 5.03 0.60 1225 1.81 C28) 0.34 0.31 0.18 0.83 0.04 0.04 OT T. rowlandsi 4.34 1295 1.19 Al 0.62 IH | 1.69 Cl, 16) 0.18 0.16 0.07 1205 0.06 0.08 0.15 T. salina 4.83 2.89 1.70 5212 0.53 1225 1.64 (1,15) 0.20 0.14 0.08 0.60 0.04 0.03 0.09 T. variegata 6.81 4.27 1.69 8.93 0.56 1.50 1.44 Gi 79226) 0.91 1.18 0.32 2.02 0.07 Oat O15 & Sada 1987). Digitizing was done using CONCH (methodology described in Chap- man et al., in prep) and a GI'CO Micro- Digi Pad 12 x 12 linked toa KAYPRO 2000 microcomputer. Descriptive statistics for all morpholog- ical variables were obtained for each pop- ulation and species, and a selection of these are summarized (by species) in Tables 1 and 2. Discriminant analysis (DA) incorporated all of the shell morphometric parameters and were constructed using all specimens measured for each species (considered as separate groups). All computations were performed using SYSTAT (Wilkinson 1986) on an IBM-AT. Systematics Generic diagnoses are in Hershler & Sada (1987). Species accounts include common name, synonomy, material examined (lo- calities numbered [in parentheses] as in Ap- pendix), diagnosis, description, remarks, type locality, distribution and habitat, etymology, and remarks. Asterisked (*) lots were used for shell measurements. Descrip- tions emphasize distinctive features from Shell, radula, body pigmentation, and re- productive systems of both sexes. Family Hydrobiidae Troschel, 1857 Genus Pyrgulopsis Call & Pilsbry, 1886 Pyrgulopsis aardahli, new species Benton Valley springsnail Figs. 10-14 Material examined.—California: Mono Co.; Spring at Bramlette Ranch (87), USNM 860406 (holotype), *857951 (paratypes), 21 Apr 1987. Diagnosis.—A large-sized species with broadly conical shell. Penis with elongate filament, very small lobe, and ventral swell- ing. Penial glandular ridges, 1-3. Description. —Shell (Fig. 10) 2.6-3.4 mm 180 Fig. 2. Sampling localities in southern Owens Val- ley and western Indian Wells Valley. Solid lines indi- cate selected elevation contours (light) and modern drainage (dark; stipple indicates lakes); dashed lines indicate historic drainage, including dry lake beds. high, height/width, 140-—170%. Whorls, 3.75—4.25, moderately convex, moderately shouldered. Body whorl inflated, height 76- 82% of that of shell. Aperture ovate, aper- tural plane near-parallel to coiling axis (Fig. 10c). Inner lip thickened, slightly reflected, adnate to small portion of or slightly sep- arated from body whorl. Outer lip straight, thin. Umbilicus moderately open. Dark, grey-black epithelial (melanic) pig- ment on most of snout (to just posterior of cephalic tentacles), along anterior edge of foot, on operculigerous lobe (Fig. 11). Cen- tral portions of sides of head/foot lightly PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 3. Sampling localities in northern Owens Val- ley. dusted or unpigmented. Tentacles unpig- mented except for dark ring along bases. Brown-black subepithelial pigment gran- ules sometimes forming dark band along posterior edge of “‘neck.” Radular (Fig. 12) formula: 5—1—-5/1-1, 2(3)-1-3, 22-24, 28-32 (from paratypes). Central tooth broadly trapezoidal; basal process moderately excavated. Penis (Fig. 13b-e) large (extending beyond mantle col- lar), thin, considerably longer than wide. Filament slender, moderate in length. Lobe reduced or absent, with blunt distal edge. Large, elongate glandular ridge borne on elongate swelling of ventral penial surface. Single, smaller ridges sometimes found on VOLUME 102, NUMBER 1 Oke WM Ag ON 4 Mono Valley Fig. 4. Sampling localities in Mono, Long, and Adobe Valleys. tip of lobe, and on dorsal penial surface proximal to base of filament. Filament darkly pigmented with subepithelial gran- ules (Fig. 13b). Capsule gland sub-equal to albumen gland (Fig. 13a). Seminal recep- tacle minute, positioned entirely anterior to bursa copulatrix. Bursa pear-shaped, mod- erate in size relative to pallial oviduct, po- sitioned partly posterior to albumen gland. Type locality. —Spring at Bramlette Ranch in Benton Valley, Mono County, California. Distribution and habitat.—Endemic to type locality (Fig. 14). Common in dense watercress in uppermost portion of outflow of small, highly degraded spring (20°C, 190 micromhos/cm). Etymology. —Named after Jeffrey B. Aar- dahl, Bureau of Land Management (Cali- fornia Desert District), who provided di- verse forms of assistance throughout the tenure of this project. Remarks. — Distinguished from similar P. perturbata by shell appearance and highly reduced penial lobe. 181 Fig. 5. Sampling localities in Saline, Eureka, and Deep Springs Valleys. Pyrgulopsis amargosae, new species Amargosa springsnail Figs. 15.46. b7a. bs ks. 19 Material Examined. —California: San Bernardino Co.; Saratoga Spring (204), USNM 860401 (holotype), *853515 (para- types), 7 Feb 1985; 857972, 10 Jul 1986.— Inyo Co.; Spring crossing path on south side of Amargosa Gorge (208), *853516, 13 Mar 1986; 857973, 16 Mar 1987.—Spring feed- ing Amargosa River in Amargosa Gorge (208), 853517, 13 Mar 1985.—Spring in marsh east of Grimshaw Lake (209), *853518, 13 Mar 1985. Diagnosis.—A small-sized species with globose to low conical shell. Penis large rel- ative to head/foot; penial lobe reduced; fil- ament long, wide. Penial glandular ridges, 0-2. Description. —Shell (Fig. 15) 1.5-2.7 mm high, height/width, 1 10-160%. Whorls, 3.5- 182 Fig. 6. Sampling localities in Panamint and north- ern Indian Wells Valleys. 4.25, convex, moderately shouldered. Body whorl 74-85% of shell height. Apex, parts of teleoconch whorls often appearing white due to erosion. Aperture broadly ovate, apertural plane near-parallel to coiling axis (Fig. 15b). Inner lip thickened, reflected above, adnate to small portion of or slightly separated from body whorl. Outer lip straight, thin. Umbilicus chink-like to broadly open. Spiral striations sometimes prominent on teleoconch. Dark, brown-black epithelial pigment on most of snout (except distal tip), along an- terior and posterior edges of “‘neck”’ (central area lighter), on part or all of operculigerous lobe. Tentacles lightly pigmented. Radular (Fig. 16) formula: 5(6)—1—5(6)/ 1-1, 3-1-4, 27-28, 24—26 (from paratypes). Central tooth broadly trapezoidal; basal process moderately excavated. Penis (Figs. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 17a, b, 18b—-e) thickened, longer than wide. Filament much longer than lobe, about equal to remaining penis length. Lobe narrow, variable in shape (Fig. 18b—e). Filament having highly muscular appearance; surface lined with weak striations. One or two small glandular ridges sometimes present at tip of lobe. Dark, grey-black subepithelial pig- ment filling filament length almost to distal tip as well as portions of remaining distal penis (Fig. 18b). Albumen and capsule glands about equal in length (Fig. 18a). Sem- inal receptacle minute, positioned well an- terior to bursa copulatrix. Bursa copulatrix club-shaped, small, positioned partly pos- terior to albumen gland. Type locality. —Saratoga Spring, southern Death Valley, San Bernardino Co., Califor- nia. Distribution and habitat. — Found in a few near-brackish springs along lower course of Amargosa River at Saratoga Spring, Amar- gosa Gorge, and Grimshaw Lake area (Fig. 19). Type locality an extensive marsh area (with several large, open pools) fed by sev- eral small springs. Snails were common in westernmost spring, both on rocks and sub- mergent macrophytes in small springpool (28°C, 5000 micromhos/cm), and on emer- gent sedges and firm bottom in shallow stream outflow. At other localities, consist- ing of small rheocrenes (16-—27°C, 2000-10, 150 micromhos/cm), snails were common on all substrates. Etymology. —Referring to distribution along Amargosa River. Remarks. — Distinguished from P. micro- coccus by globose shell; large penis; large penial filament; small, narrow penial lobe; and highly reduced glandular ridge. Ranges of these very similar snails (previously con- fused by Hershler and Sada 1987:788) are contiguous. Pyrgulopsis micrococcus (Pilsbry, 1893) Oasis Valley springsnail Figs. 17c, d, 20-25 Amnicola micrococcus Pilsbry in Stearns, 1893:277. VOLUME 102, NUMBER 1 183 Fig. 7. Sampling localities in Death Valley and Amargosa Basin. Material examined. —Nevada: Nye Co.; Spring in Oasis Valley (204), USNM *850297, 18 Nov 1985; 857961, 16 Mar 1987.—Cane Spring (239), *857936, 10 July 1986:— California: Inyo Co.; Northernmost of Tecopa Hot Springs (210), *853502, 12- 13 Mar 1985; 857962, 16 Mar 1987.— Shoshone Spring (211), *853501, 12 Mar 1985; 857962, 16 Mar 1987.—Grapevine Springs (241): northwest-most spring in complex, 853503, 1 Mar 1985; Spring emerging below limestone bench northwest of ranch, 853504, 26 Feb 1985; Spring on bench above ranch, 853505, 25 Feb 1985; Spring at ranch, *853506, 25 Feb 1985; 857964, 14 Mar 1985.—Spring 1.6-km east of Scotty’s Castle (242), *853507, 26 Feb 1985; 857965, 14 Mar 1987.—Hanaupah Sprime (222), *8§53508, 16 Feb 1985; 857966, 21 Mar 1987.—Lower spring in Johnson Canyon (220), *853509, 18 Feb 1985; 857967, 21 Mar 1987.—Stream in Jail Canyon (196), *853513, 14 Feb 1985; 857970, 19 Mar 1987.—Stream in Surprise Canyon (194), *857937, 19 Mar 1987; Stream in Pleasant Canyon (190), *857940, 19 Mar 1987.—China Garden Spring (184), 853511, 9 Feb 1985.—Stream below Dar- win Falls (184), 857969, 23 Mar 1987.— Spring above Darwin Falls (184), *853512, 10 Feb 1985.—Stream in Snow Canyon (182), *857938, 16 Sep 1987, J. Aardahl! — Stream in Knight Canyon (180), *857939, 14 Apr 1987.—Tennessee Spring (178), *S 53014, 04Mart, 1985: 5/971, 13, May 1987.—Saline Marsh (152), *853510, 10 Feb 1985; 857968, 28 Mar 1987. Diagnosis. —A small-sized species, with 184 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 8. Photographs of selected springsnail localities: a, stream in Cottonball Marsh, Death Valley, type locality of T. salina (3-10-87: photo by P. Rowlands); b, Grapevine Springs, Death Valley, type locality of T. margae and T. rowlandsi is on the large travertine mound (3-14-87); c, Saline Marsh, Saline Valley (3-29-87); d, Sand Canyon stream, Indian Wells Valley (3-26-87); e, Fish Slough, Owens Valley, spring sources (including type locality of P. perturbata) visible in lower portion of photograph (ca. 1975; aerial photo by P. Pister); f, ““NE” Spring at Fish Slough (2-7-85). globose to ovate-conic shell. Penis with moderate-sized lobe; distal edge of lobe usu- ally ornamented with glanduiar ridge. Description. —Shell (Figs. 20, 21) 1.1-3.1 mm high, height/width, 99-190%. Whorls, 3.25-5.0, well-rounded, with slight shoul- ders. Spire often irregularly convex due to bulging of whorls. Body whorl 65-89% of shell height. Aperture ovate, apertural plane near-parallel to coiling axis (Fig. 21b). Inner lip moderately thickened and reflected, usu- ally slightly separated from body whorl. Outer lip straight, thin. Umbilicus chink- like to moderately open. VOLUME 102, NUMBER 1 185 Fig. 9. Photographs of springsnail localities: a, Warm Springs, Owens Valley (4-19-87); b, Small spring S of Warren Lake, Owens Valley (4-18-87); c, Spring in Owens Gorge, Owens Valley (5-7-87); d, Hot Creek, Long Valley (4-23-87). 186 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 10. SEM micrographs of P. aardahli from spring at Bramlette Ranch: a, Holotype, USNM 860406 (shell height, 3.26 mm); b—d, Paratypes, USNM 857951 (scale of “‘b” and “‘c”’ as in “‘a”’; bar = 150 um). VOLUME 102, NUMBER 1 Head/foot epithelial pigment ranging from absent to near-uniformly black (lighter on central portions of sides of “‘neck’’). Radular (Figs. 22, 23) formula: (4—7)-1- (4-7)/1-1, (2-4)-1-(3-6), 17-26, 19-32 (from numerous populations). Central tooth moderately to broadly trapezoidal; basal process moderately excavated. Penis (Figs. 17c, d, 24b—1) barely extend- ing beyond mantle collar, moderately thick- ened, longer than wide. Filament slender, usually extending well beyond edge of lobe. Lobe highly variable in size and shape, ta- pering slightly distally. Glandular ridge (rarely absent) small, positioned on or near distal edge of lobe. Capsule gland smaller than albumen gland (Fig. 24a). Seminal re- ceptacle small, positioned largely anterior to bursa copulatrix. Bursa pear-shaped, small to fairly large relative to pallial ovi- duct, most of length positioned on albumen gland. Type locality. —Small spring in Oasis Val- ley, Nye County, Nevada (precise location unknown). Distribution and habitat.—A widespread form (contrary to Taylor 1985:317) found in small springs and stream outflows (see Figs. 8b, c) of Amargosa River drainage as well as interior drainage in Death, Pana- mint, and Saline Valleys (5—32°C, 300—4000 micromhos/cm) (Fig. 25). Typically com- mon on stone, bits of travertine, watercress, and plant debris. Pyrgulopsis owensensis, new species Owens Valley springsnail Figs. 26a—-d, 27-32 Material examined. —California: Inyo Co.; Spring ca. 1.6 km south of Mule Spring (92), USNM 853541, 5 Dec 1987, D. Giu- liani.— Mule Spring (93), *853540, 19 Nov 1985, D. Wong; 857983, 20 Apr 1987.— Spring at Graham Ranch (94), *853543, 8 Feb 1985; 857985, 19 Apr 1987.—Wilk- erson Springs (96), *853542, 8 Feb 1985; 857984, 18 Apr 1987.—Spring at Toll House 187 Fig. 11. Right lateral view of head-foot of P. aar- dahli, USNM 857951, spring at Bramlette Ranch. Stip- ples indicate pigmented areas. (97), *857950, 26 Apr 1987.— Warm Springs (98), Main spring, *853544, 7 Feb 1985, 857988, 19 Apr 1987; Small spring north of above, 853545, 7 Feb 1985; 857989, 19 Apr 1987. Mono Co.: Stream in canyon S of Piute Creek (104), 860404 (holotype), *857955 (paratypes), 8 May 1987.—Springs on bench south of Piute Creek (103), North spring, 857986, 21 Apr 1987; South spring, 857987, 22 Apr 1987. Diagnosis.—A small- to moderate-sized species with globose to ovate-conic shell. Penis large relative to head/foot, filament short, lobe enlarged, ventral swelling pres- ent. Penial glandular ridges, 2-6. Description. —Shell (Figs. 26a—d, 27, 28) 1.5-—2.8 mm high, height/width, 110-160%. Whorls, 3.0—4.25, well-rounded, sutures slightly impressed. Protoconch sometimes slightly tilted. Body whorl inflated, height 74-90% of that of the shell. Apical whorls sometimes eroded, shell often covered by deposits. Aperture ovate, angled above; moderate to large in size. Aperture plane near-parallel to somewhat tilted relative to coiling axis (Figs. 27b, 28b). Inner lip slight- ly to considerably thickened and reflected, adnate to or (more commonly) slightly sep- arated from body whorl. Outer lip thin, straight or slightly sinuate. Umbilicus chink- like to moderately open. Dark brown or grey-black epithelial pig- ment on snout, peripheral portions of 188 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ‘ ee is : By 4 ‘ = ad 1% 4 ri is %, oe) = ; a) is ~ 4 2 = : ¥ an . at J a Fig. 12. Radula of P. aardahli, USNM 857951, spring at Bramlette Ranch: a, Centrals (bar = 12 wm); b, Laterals (bar = 8.6 um); c, Inner marginal (bar = 6.7 um); d, Outer marginals (bar = 6.0 um). “‘neck,”’ and dorsal surfaces of tentacles. Radular (Figs. 29, 30) formula: 5(6)—1- Dark subepithelial granules prominent in 5(6)/1-1, 3-1-3(4), 18-23, 25-37 (from central areas of sides and sometimes along three populations). Central tooth broadly posterior edges of “‘neck.”’ trapezoidal; basal process well-excavated. VOLUME 102, NUMBER 1 Penis (Fig. 31b—1) extending well beyond mantle collar, elongate. Narrow filament shorter than lobe. Lobe massive, tapering only slightly, distal edge blunt. Edge of lobe ornamented with single elongate or two shorter glandular ridges. Dorsal penis some- times having small glandular ridges on lobe and/or near base of filament. Ventral swell- ing small, located filament base. Ridge or- namenting swelling variably-sized. Fila- ment darkly pigmented with sub-epithelial granules along most of length (Fig. 31b). Capsule gland equal to (Fig. 31a) or slightly smaller than albumen gland. Seminal re- ceptacle minute, positioned largely or en- tirely anterior to bursa. Bursa pear-shaped, small- to moderate-sized, with about half of length posterior to albumen gland. Type locality.—Stream in canyon S of Piute Creek, Mono Co., California. Distribution and habitat.—Found along escarpments of White and Inyo Mountains east side of Owens Valley (Fig. 32). Habitat consisting of small springbrooks (10—29°C, 300-780 micromhos/cm) (Fig. 9a) where snails typically common in watercress and/ or on bits of travertine and stone. Syntopic with P. wongi in spring at Toll House. Etymology—Referring to occurrence in Owens Valley. Remarks. — Distinguished from similar P. perturbata by shell appearance. more en- larged penial lobe, and (usually) more nu- merous penial glandular ndges. Pyrgulopsis perturbata, new species Fish Slough springsnail Figs. 26e-g, 33-36 Material examined.—California: Mono Co.; Fish Slough: “Northwest Springs.” South spring (76), USNM 860407 (holo- type), *853546 (paratypes). 7 Feb 1985: 857990, 24 Apr 1987: “Northwest Springs.” North spring (76), 853547, 7 Feb 1985: 857991, 20 Apr 1987; ““NE Spring” (77), *853548, 7 Feb 1985: 857992. 20 Apr 1987: “BLM Spring” (75), *853549, 7 Feb 1985. Fig. 13. Reproductive anatomy of P. aardahli, USNM 857951, spring at Bramlette Ranch: a, Left lateral view of pallial oviduct complex: b-e, Penes (b. c, dorsal: d, e. ventral). Stippled areas on penes indicate glandular ridges (enclosed stipples) and pigmented re- gions (open). Ag = albumen gland: Bu = bursa copu- latrix; Cg = capsule gland: Cga = capsule gland open- ing: Emc = posterior end of pallial cavity; Ov = oviduct: Pf =penial filament: Plo = penial lobe: Sr = seminal receptacle: Vc = ventral channel of capsule gland. Diagnosis.—A large-sized species with thickened, low-conical shell. Penis large, lobe and filament small, ventral swelling present. Penial glandular ridges. 3 or 4. Description. — Shell (Figs. 26e-g. 33) 2.7- 4.00 mm high, height/width. 130—-180%. Whorls, 4.25—5.0, only slightly convex, with pronounced sub-sutural angulations. Body whorl inflated. 71—85% of shell height. Ap- erture broadly ovate. Apertural plane tilted relative to coiling axis (Fig. 33b). Inner lip usually well-thickened and reflected, broad- ly adnate to body whorl. Outer lip straight, thin or moderately thickened. Umbilicus chink-like. Dark brown-black epithelial pigment prominent on snout, tentacles, and periph- eral portions of sides of head/foot. Pigment 190 Kilometers Fig. 14. Map showing distribution of P. aardahii. either light or absent on central portions of sides of head/foot. Radular (Fig. 34) formula: 5—1—5/1-1, 3- 1-4(5), 18-19, 29-31 (from paratypes). Central tooth broadly trapezoidal, basal process well-excavated. Penis (Fig. 35b—e) extending well beyond edge of mantle collar, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON thin, considerably longer than wide. Fila- ment both narrow and short, barely extend- ing beyond tip of lobe. Lobe tapering only slightly distally, bearing elongate glandular ridge along distal edge. Dorsal surface of penis with small ridge proximal to base of filament. Ventral swelling arising slightly VOLUME 102, NUMBER 1 191 Fig. 15. SEM micrographs of P. amargosae from Saratoga Spring: a, Holotype, USNM 860401 (2.28 mm); b, c (bar = 136 um), Paratypes, USNM 853515. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ¥ ab \ Fig. 16. Radula of P. amargosae, USNM 853515, Saratoga Spring: a, Centrals (bar = 12 wm); b, Laterals (bar = 8.6 um); c, Inner marginals (bar = 8.6 wm); d, Outer marginal (bar = 3.8 wm). proximal to base of filament; ridge (rarely two) on swelling elongate. Filament dark- ened along much of length by sub-epithelial pigment granules. Capsule gland sub-equal to albumen gland (Fig. 35a). Bursa small, with ca. 50% of length posterior to albumen gland. Seminal receptacle minute, posi- tioned entirely anterior to bursa. VOLUME 102, NUMBER 1 Fig. 17. SEM micrographs of head-foot and dorsal penes of P. amargosae and P. micrococcus: a (bar = 0.43 mm), b (bar = 0.38 mm), P. amargosae, USNM 853515, Saratoga Spring; c (bar = 0.3 mm), d (bar = 200 um), P. micrococcus, USNM 857961, spring in Oasis Valley. 194 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Type locality. —‘‘Northwest Springs,”’ south springpool, Fish Slough, Mono Co., California. Distribution and habitat. — Found in three of the four main springs in Fish Slough (ex- tinct in ““BLM Spring’) (Figs. 8e, f, 36). Springs issuing relatively cool (22—26°C), soft (200-360 micromhos/cm) water. Snails found only in small vestiges of rheocrene habitat at various small orifices in north- west springs (rare at both sites on vegetation and stones), and at beginning of outflow from “NE Spring” (common in Chara). Etymology. — Referring to various distur- bances to endemic locale, including severe reduction of original rheocrene habitat as unanticipated side effect of efforts to con- serve Owens pupfish (Miller and Pister 1971). Pyrgulopsis cf. stearnsiana (Pilsbry, 1899) Figs. 37-40 Paludestrina stearnsiana Pilsbry, 1899:124. Fontelicella stearnsiana. —Gregg & Taylor 1965:108. Pyrgulopsis stearnsiana.—Hershler & Thompson 1987:30. Material examined. —California: Kern Co.; Stream in Sage Canyon (1), USNM *853520, 26 Mar 1987; 857975, 10 Nov 1987.—Stream in Sand Canyon (6), *853519, 26 Mar 1987; 857974, 22 Dec 1987, J. Aardahl. Diagnosis. —A small-sized species with low conical shell. Penis small relative to head/foot, penial lobe reduced, filament elongate, ventral swelling present. Penial glandular ridges, 1-3. Description. — Pertaining only to popula- tions in study area. Shell (Fig. 37) 2.0-2.9 mm high, height/width, 130—170%. Whorls, 4.0-4.5, convex. Body whorl ca. 75% of shell height. Shell surface encrusted with thick, black deposits. Aperture broadly ovate, somewhat angled above, about half as tall Fig. 18. Reproductive anatomy of P. amargosae: a, Left lateral view of pallial oviduct complex, USNM 853515, Saratoga Spring; b, c, Dorsal penes, USNM 853515, Saratoga Spring; d, e, Dorsal penes, USNM 857973, spring in Amargosa Gorge. “‘b” through “e”’ drawn to same scale. as body whorl. Inner lip slightly thickened and reflected, adnate to small portion of or slightly separated from body whorl. Outer lip straight, thin; apertural plane slightly tilted relative to coiling axis (Fig. 37b). Dark, grey-black epithelial pigment on most of snout (except distal tip), proximal portion of cephalic tentacles, along anterior and posterior edges of “neck,” part or all of operculigerous lobe. Pigment on central portions of sides of neck absent to dark (sub- epithelial pigment cluster dense in area). Radular (Fig. 38) formula: 5(6)—1—5(6)/ 1-1, 2(3,4)-1-3(4,5), 23-24, 23-29 (from single population). Central tooth broadly trapezoidal; basal process moderately ex- cavated. Penis (Fig. 39b—e) rarely protrud- ing beyond edge of mantle collar, longer than wide. Filament slender, sub-equal to re- maining penis length. Reduced lobe scarcely VOLUME 102, NUMBER 1 Kilometers 118° Fig. 19. Map showing distribution of P. amargosae. projecting distal to base of filament. Tip of lobe often ornamented with small glandular ridge; similar, single ridges on dorsal penial surface about halfway from base of penis to base of filament, on ventral surface near (sometimes on) inner edge. The latter ridge enlarged, borne on low swelling (Fig. 39e). 195 Wu Filament with dark sub-epithelial pigment streak (Fig. 39b). Albumen gland sub-equal to capsule gland (Fig. 39a). Seminal recep- tacle small, positioned anterior to bursa copulatrix. Bursa copulatrix small relative to capsule gland, positioned partly posterior to gland. 196 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 20. Camera lucida drawings of shells of P. micrococcus: a, USNM 857936, Cane Spring (2.24 mm); b, USNM 853501, Shoshone Spring (1.96 mm); c, USNM 853502, Tecopa Hot Springs (1.90 mm); d, USNM 853506, Grapevine Springs (2.16 mm); e, USNM 853508, Hanaupah Spring (2.26 mm); f, USNM 853510, Saline Marsh (1.96 mm); g, USNM 853512, spring above Darwin Falls (1.94 mm); h, USNM 857937, Surprise Canyon stream (1.88 mm). Type locality. —Near Oakland, Alameda County, California. Distribution and habitat. —Distribution given by Taylor (1981:152) as ““Central Cal- ifornia, from Sonoma County to Monterey County along the coast, and inland in the foothills of the Sierra Nevada.” Found in the study area in two moderate-sized, cool streams (16—20°C, 550 micromhos/cm) sep- arated by 25 km along eastern slope of Sier- ra Nevada in Indian Wells Valley (Fig. 40). Snails common in watercress and Chara. Remarks.—Shells of the Indian Wells Valley snails closely resemble P. stearnsiana from the San Francisco Bay area and their penes conform to a general description for the species provided by Gregg and Taylor (1965:107). Additional study, including ex- amination of anatomy of topotypes or near- topotypes, will be necessary to confirm identity of the snails from Indian Wells Val- ley. Pyrgulopsis wongi, new species Wong’s springsnail Figs. 41-47 Material examined. —California: Inyo. Co.; Spring at Little Lake, east of HW 395 (10), USNM *853521, 9 Feb 1985.—Hog- back Creek (Monache Mtn. quad.) (20), *853522, 28 Jun 1985, D. Wong.—Summit Creek (21), 853523, 12 Apr 1987.—Spring ca. 3.0 km north of Summit Creek (21), *853524, 12 Apr 1987.—Spring at Cabin Bar Ranch (25), 853525, 12 Oct 1987, J. Goldberg and M. Shumway.—Lubkin Creek (34), 853526, 16 Apr 1987.—Spring feeding Lubkin Creek (34), 857942, 25 Apr 1987.— Spring along east side of Tuttle Creek (35), VOLUME 102, NUMBER 1 197 Fig. 21. SEM micrographs of P. micrococcus: a, USNM 853502, Tecopa Hot Springs (1.98 mm); b, USNM 853512, spring above Darwin Falls: c, USNM 853512. Tecopa Hot Springs (bar = 120 um). 198 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON f™ i —_ — i i Fig. 22. Central radular teeth of P. micrococcus: a, USNM 857936, Cane Spring (bar = 7.5 um); b, USNM 857963, Tecopa Hot Springs (bar = 7.5 um); c, USNM 857965, spring E of Scotty’s Castle (bar = 7.5 um); d, USNM 857968, Saline Marsh (bar = 8.6 um). 857943, 30 Apr 1987.—Hogback Creek Giuliani.—Spring on hill south of Warren (Lone Pine quad.) (36), *853527, 8 Feb 1985; Lake (57), *853530, 18 Apr 1987.—Spring 857976, 16 Apr 1987.—Boron Springs (40), in canyon south of Shannon Canyon (59), *853528, 17 Apr 1987.—Stream in Charlie 857944, 20 Apr 1987.—Spring along north Canyon (43), *853529, 12 Jun 1987, D. side of upper Pine Creek (69), *853531, 24 VOLUME 102, NUMBER 1 Fig. 23. Lateral and marginal radular teeth of P. micrococcus: a, Laterals, USNM 857936, Cane Spring (bar = 6.0 um); b, Laterals, USNM 857966, Hanaupah Spring (bar = 7.5 um); c, Inner marginals, USNM 857937, Surprise Canyon stream (bar = 5.0 um); d, Outer marginals, USNM 857963, Tecopa Hot Springs (bar = 4.3 pm). Apr 1987; 857977, 15 Sep 1987,D. Wong.— 857945, 3 May 1987.—Spring in Owens West spring in Birchim Canyon (70), 860403 Gorge (74), *853532, 14 May 1985, D. (holotype), *857941 (paratypes), 3 May Wong; 857978, 8 May 1987.—French Spring 1987.—East spring in Birchim Canyon (70), (89), *857947, 4 May 1987.—Barrel Springs 200 Fig. 24. Reproductive anatomy of P. micrococcus: a, Left lateral view of pallial oviduct complex, USNM 857961, spring in Oasis Valley; b—-i, Penes (all dorsal except “1’’) (b, 1, USNM 857936, Cane Spring; c, USNM 853505, Grapevine Springs; d, USNM 857962, Shosh- one Spring; e, USNM 857963, Tecopa Hot Springs; f, USNM 857967, Johnson Canyon spring; g, USNM 857971, Tennessee Spring; h, USNM 853512, spring above Darwin Falls). (91), *857948, 18 Aug 1987.—Spring at Toll House (97), *857949, 26 Apr 1987.—Corral Springs (160), *853535, 8 Feb 1985; 857979, 29 Mar 1987.—Antelope Spring (162), *853536, 8 Feb 1985. Mono Co.; Spring along Marble Creek (82), *853533, 22 Apr 1987.—Springs at north end of Blind Spring Valley (86); North Spring, *857946, 21 Apr 1987; South spring, 853534, 21 Apr 1987.— Layton Springs (122), *853537, 6 Feb 1985; 857980, 23 Apr 1987.—River Springs (132), *853538, 6 Feb 1985; 857981, 21 Apr 1987. Diagnosis. —A small- to moderate-sized species with globose to low conical shell. Penis massive, with large filament and mod- erate-sized lobe. Ventral penis with two prominent swellings bearing glandular ridges. Glandular ridges, 7-12. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Description. —Shell (Figs. 41, 42) 1.2—3.0 mm high, height/width, 100—160%. Whorls, 3.25—4.5, well rounded, with slightly an- gulated shoulders. Body whorl 76-87% of shell height. Aperture broadly ovate, angled above. Apertural plane slightly tilted rela- tive to coiling axis (Fig. 42c). Inner lip slightly thickened, usually only minimally reflected, either adnate to portion of or slightly separated from body whorl. Outer lip straight, thin. Umbilicus chink-like to moderately open. Dark grey-black epithelial pigment on snout, proximal tentacles, and peripheral portions of sides of head/foot. Entirety of head/foot often very dark. Central portions of sides of head/foot usually with densely clustered dark, subepithelial pigment gran- ules. Radular (Figs. 43, 44) formula: (4—7)—1- (4-7)/1-1, (2-—5)—1-(3-6), 17-26, 20-34 (from numerous populations). Central tooth relatively square-shaped; basal process well- excavated. Penis (Figs. 45b-—l, 46) flattened, longer than wide. Filament fairly broad, short relative to length of remaining penis. Lobe slightly shorter than filament, broad, often widening distally. Glandular ridge ar- rangement typically as follows: 1) elongate ridge lining edge of lobe; 2) similar, stalked ridge on ventral surface just proximal to lobe; 3) similar ridge (rarely very reduced) on fleshy projection of ventral surface prox- imal to above; 4) elongate ridge covering proximal-most two-thirds of dorsal fila- ment; 5) very elongate ridge on dorsal sur- face curving from just proximal to filament to lobe; 6) shorter ridges on dorsal surface along right side of (5) and in area between base of filament and edge of lobe. Modifi- cations of above include addition of a few small ridges on central dorsal surface, ad- dition of a single small ridge (sometimes stalked) on ventral surface, apparent frag- mentation of ridges (particularly “1,” ““5’’); apparent merging of adjacent ridges on dor- sal surface. Filament darkened with sub-ep- ithelial pigment along most of length. Cap- sule gland sub-equal to albumen gland (Fig. VOLUME 102, NUMBER 1 (@) Kilometers Fig. 25. 45a). Seminal receptacle small, positioned lateral to anterior bursa copulatrix. Bursa pear-shaped, massive, with about one-third of length posterior to albumen gland. Type locality.—Spring in Birchim Can- yon north of Bishop, Inyo Co., California. Distribution and habitat. — Widespread in Owens Valley along eastern escarpment of Sierra Nevada from Pine Creek south to 201 Map showing distribution of P. micrococcus. Snail occurs at 15 localities in Ash Meadows. Little Lake, and along western side of val- ley from French Spring to Marble Creek. Also found in a few sites in Long, Adobe, and Deep Springs Valleys (Fig. 47). Habitat includes seeps and spring-fed streams of small-moderate size (9.5-—22°C, 85-450 micromhos/cm) (Fig. 9b, c). Snails typically common in watercress and/or on small bits of travertine and stone. 202 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 26. Camera lucida drawings of shells of P. owensensis and P. perturbata: a—d, P. owensensis (a, USNM 853540, Mule Spring [2.1 mm]; b, USNM 857950, spring at Toll House [2.3 mm]; c, USNM 857955, stream in canyon S of Piute Creek [2.08 mm]; d, USNM 853543, spring at Graham Ranch [2.16 mm]); e-g, P. perturbata (e, USNM 853546, Fish Slough, ““Northwest Springs,” [3.93 mm]; f, USNM 853549, Fish Slough, ““BLM Spring,” [3.22 mm]; g, USNM 853548, Fish Slough, ““NE Spring” [3.97 mm]). Etymology. —Named after Darrell Wong, California Fish and Game, for his assistance during the project and interest in conserving Owens Valley springsnails. Remarks. —Similar in penial morphology to P. californiensis (Gregg & Taylor) from western California (Taylor 1981:154). Dis- tinguished from above by globose shell, and more numerous stalked glandular ridges on ventral penial surface. Genus Tryonia Stimpson, 1865 Tryonia margae, new species Grapevine Springs elongate tryonia Figs. 48-50, 5la, 52 Material examined. —California: Inyo Co.; Grapevine Springs (241); (upper) Warm spring on limestone bench, USNM 860408 (holotype), *857952 (paratypes), 14 Mar 1987; Spring on limestone bench above ranch 853555, 25 Feb 1987; 857996, 14 Mar 1987. Diagnosis.—A small-sized species with narrow, turriform shell. Penis small, with 3 papillae on inner curvature, and a single papilla (sometimes absent) on outer cur- vature. Distal tip of penis with elongate swelling on inner side. Description. — Shell (Fig. 48) 1.5-—2.9 mm high, height/width, 250—300%. Whorls, 4.5- 6.25, rounded, with angulated shoulders. Sutures often deeply impressed. Apex blunt, protoconch slightly depressed (Fig. 48g). VOLUME 102, NUMBER 1 203 Fig. 27. SEM micrographs of P. owensensis from stream in canyon S of Piute Creek: a, Holotype, USNM 860404 (2.0 mm); b-d, Paratypes, USNM 857955 (bars = 120 um, 176 um). Body whorl 45-55% of shell height. Marl frequently covering apical whorls, with near- entirety of shell sometimes blanketed. Ap- erture narrowly ovate. Inner lip well-reflect- ed, slightly thickened, adnate to or slightly separated from body whorl. Outer lip sin- uate, thin (Fig. 48d, f). Umbilicus chink- like. Protoconch near-smooth (Fig. 48g). Collabral growth lines well developed on teleoconch, often elevated at irregular in- tervals. Spiral sculpture consisting of weak striations. Dark brown-black epithelial pigment covering most of head/foot, although some- times absent on tentacles, and lighter on snout and central portion of sides of ‘“‘neck.” Radular (Figs. 49, 50) formula: 4(5)}-1- 4(5)/1(2)-1(2), 2(3}-1-3(4), 20-21, 22-28. 204 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 28. SEM micrographs of P. owensensis from Warm Springs: a (1.92 mm), b, d, USNM 853544, main spring; c, USNM 853545, spring N of above (bar = 136 um). Central tooth broadly trapezoidal, basal cusps large, basal process well excavated. Central cusps of lateral tooth only slightly enlarged (Fig. 49c, d). Penis (Fig. 51a) ex- tending only slightly beyond edge of mantle collar. Enlarged papilla located on outer edge of penis at base. Two smaller papillae po- sitioned along distal half on inner edge; sim- ilar small papilla usually found near base on inner edge. Brown-black epithelial pig- ment usually prominent near distal tip, at bases of two distal papillae. Lighter pigment dusting much of dorsal surfaces of penis and 2 proximal papillae. Type locality. —Warm spring on lime- stone bench in Grapevine Springs complex, northern Death Valley, Inyo Co., Califor- nia. VOLUME 102, NUMBER 1 205 Fig. 29. Radula of P. owensensis, USNM 857955, stream in canyon S of Piute Creek: a, Centrals (bar = 10 um); b, Laterals (bar = 6.7 um); c, Inner marginal (bar = 6.0 wm); d, Outer marginals (bar = 6.0 um). Distribution and habitat.— Found in two sites (Separated by about 1 km) among Grapevine Springs in northern Death Val- ley (Fig. 52). Habitat consists of upper por- tions of shallow spring brooks flowing over travertine (Fig. 8b), on which snails were moderately common. Springs were highly mineralized (1050-1075 micromhos/cm), but differed considerably in temperature (west spring, 26—27°C; east, 36—37°C). Syn- topic with 7. rowlandsi in the thermal spring. Etymology. —From Latin marga, mean- ing marl, and referring to occurrence of snail in travertine springs. 206 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 30. Radula of P. owensensis, USNM 857988, Warm Springs (main spring): a, Centrals (bar = 6.7 um); b, Laterals (bar = 6.0 um); c, Inner marginal (bar = 6.0 wm); d, Outer marginals (bar = 3.8 um). VOLUME 102, NUMBER 1 Tryonia protea (Gould, 1855) Desert tryonia Figs. 52-54 Amnicola protea Gould 1855:129. Melania exigua Conrad 1855:269. Pyrgulopsis blakeana Taylor 1950:30. Pyrgulopsis cahuillarum Taylor 1950:31. Material examined. —California: Mono Co.; Hot Creek, USNM *857954, 23 Apr 1987. Diagnosis.—A moderate to large-sized species (shell height typically 3-7 mm) with elongate-conic to turriform shell. Shell smooth or with spiral and/or collabral sculpture varying from faint striations to elevated ridges. Description of Hot Creek population. — Shell (Fig. 53) 3.0-4.5 mm high, height/ width, 210—242%. Whorls, 4.75-6.25, rounded. Sutures moderately impressed. Body whorl 55-61% of shell height. Pro- toconch slightly depressed (Fig. 53b), apex of adults invariably highly eroded. Aperture ovate, apertural plane tilted relative to coil- ing axis. Inner lip only slightly thickened and reflected, broadly adnate to body whorl. Outer lip thin, slightly sinuate. Umbilicus chink-like, near-absent. Smooth surface of protoconch lined with well-spaced rows of numerous, shallow perforations (Fig. 53b, c). Teleoconch with strong growth lines; 10- 20 spiral lines prominent on middle whorls, sometimes extending to aperture. Brown epithelial pigment dense on most of snout. Black patches of subepithelial pig- ment along edges of sides of head/foot. Pal- lial roof with paired, black pigment patches extending along length of ctenidium. Radular (Fig. 54) formula: 5(6)—1-5(6)/ 2(3)—2(3), (3-5)—1-(6-8), 35-36, 28-31 (from single population). Central tooth broadly trapezoidal; basal cusps large, basal process moderately excavated. No males found among the more than 100 specimens collected. Type locality.—Colorado Desert (proba- 207 1.0 mm Fig. 31. Reproductive anatomy of P. owensensis: a, Left lateral view of pallial oviduct complex, USNM 857955, stream in canyon S of Piute Creek; b—i, Penes (b [dorsal], i [ventral], USNM 857955, stream in can- yon S of Piute Creek; c [dorsal], f [ventral], USNM 857983, Mule Spring; d [dorsal], g [ventral], h [ventral], USNM 857988, Warm Spring (main spring); e [ven- tral], USNM 857989, Warm Springs [spring N of above]). ““b’’ through “i” drawn to same scale. bly in Riverside County, California [based on Blake 1857]). Distribution and habitat. —‘‘Western Utah to southeastern California, adjacent Baja California, and southeastern Arizona’”’ (Taylor 1981:155), with only two living populations known from California: that of Hot Creek (Fig. 52) and Dos Palmas Spring in Riverside County (Taylor 1981:154). At Hot Creek (Fig. 9d), snails were rare on var- ious submergent macrophytes lining sides 208 Kilometers Fig. 32. Map showing distribution of P. owensensis. of the swiftly flowing thermal stream (32°C, 480 micromhos/cm). Remarks. —The taxonomic concept of this form is vague (Taylor 1966:53—54) and sta- tus of the few living (and mostly widely sep- arated) populations (Taylor 1985:fig. 35) re- mains unclear. The Hot Creek population is referable to 7. protea on basis of shell form, size, and sculpture, but confirmation PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON by anatomical comparison with snails from Dos Palmas Spring (that represent near to- potypes) would be desirable. Tryonia robusta, new species Robust tryonia Figs. 51d, 52, 55-58 Material examined. —California: Inyo Co.; Nevares Springs (230); Spring on trav- VOLUME 102, NUMBER 1 209 Fig. 33. SEM micrographs of P. perturbata from Fish Slough, ““Northwest Springs,” south spring: a, b, Holotype, USNM 860407 (3.57 mm); c, Paratype, USNM 853456 (bar = 200 um). ertine mound, USNM 860411 (holotype), 1985—Travertine Springs; South spring, *853557 (paratypes), 2 Feb 1985; 857999, *853559, 2 Feb 1985; 857959, 12 Mar 1987; 16 Nov 1985; 857958, 12 Mar 1987;Spring North spring, 857960, 12 Mar 1987. issuing from base of mound, 853558, 2 Feb Diagnosis.—A small-sized species with PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 34. Radula of P. perturbata, USNM 857990, Fish Slough, “‘“Northwest Springs,” south spring: a, Centrals (bar = 13.6 wm); b, Laterals (bar = 10 wm); c, Laterals and inner marginals (bar = 12 wm); d, Outer marginals (bar = 10 wm). unusually broadly conical shell for genus. high, height/width, 140-170%. Whorls, Penis moderate-sized, with single papillaon 3.75-4.75, rounded, with pronounced outer curvature. shoulders. Sutures impressed. Body whorl Description. —Shell (Fig. 55) 1.1-2.1mm 68-80% of shell height. Protoconch (Figs. VOLUME 102, NUMBER 1 56a-c) simple, sometimes eroded. Aperture near-ovate, sometimes sharply angled above; apertural plane slightly tilted relative to coiling axis. Inner lip thickened, mod- erately reflected, usually slightly separated from body whorl. Outer lip thin, near- straight. Umbilicus chink-like. Protoconch surface wrinkled (Figs. 56a—c). Teleoconch often with weak spiral striations, particu- larly on upper whorls. Operculum (Fig. 56d) thin, paucispiral, with 2.5—3.0 rapidly expanding whorls. Brown-black melanic pigment dark on snout and posterior edge of “‘neck,”’ variable on central portions of sides of head/foot; - sub-epithelial pigment granules prominent in latter. Mantle roof epithelial pigment typ- ically uniformly dark brown-black. Radular (Fig. 57) formula: (5—7)-1-(5-7)/ 1-1, 3(4)-1-5(6), 24, 22—27 (from two pop- ulations). Central tooth relatively square- shaped; central cusps elongate, basal cusps small, basal process highly excavated. Ce- phalic tentacles covered with sparse, irreg- ular patches of hypertrophied cilia, rarely forming short tracts. Penis (Figs. 51d, 58) considerably longer than wide, moderately thickened. Attachment area broad, with rest of narrow length coiled in tight, clockwise fashion. Papilla small, conical, positioned along outer curvature just proximal to mid- length. Distal tip blunt, with inner side slightly swollen; surface of tip densely cov- ered with elongate cilia. Distal tip of papilla simple, lightly ciliated (Fig. 58b). Type locality.—Nevares Springs, Death Valley, Inyo County, California. Distribution and habitat.— Found at Ne- vares and Travertine Springs along base of Funeral Mountains in mid-eastern Death Valley (Fig. 52). Snails found commonly on plant debris and travertine in shallow out- flows of four thermal springs (30—37°C, 900-— 975 micromhos/cm). Extinct at Texas Springs (located between above complexes). Etymology. —Referring to unusually broad shell for genus. Remarks. —Shell form and penial shape 211 Fig. 35: Reproductive anatomy of P. perturbata from Fish Slough, “‘ Northwest Springs”: a, Left lateral view of pallial oviduct complex, USNM 857990, south spring; b-e, Penes (b [dorsal], c [dorsal], d [ventral], USNM 857990, south spring; e [ventral], USNM 857991, north spring). and lobation pattern are highly distinctive, and relationship between this local endemic and other congeners in region is unclear. Species closely conforms to typical Tryonia in other features (including details of female reproductive morphology). Tryonia rowlandsi, new species Grapevine Springs squat tryonia Figs. 51b, 52, 59, 60 Material examined. —California: Inyo Co.; Grapevine Springs (241); (upper) Warm spring on limestone bench, USNM 860409 (holotype), *857953 (paratypes), 14 Mar 1987; (lower) Warm spring on limestone bench, 857997, 14 Mar 1987. Diagnosis.—A small-sized species with elongate-conic shell. Penis large, with single papilla on outside curvature and 2 papillae on inside curvature. Description. —Shell (Fig. 59) 1.7—2.3 mm 212 50 Kilometers Fig. 36. Map showing distribution of P. perturbata. high, height/width, 140—190%. Whorls, 4.0— 4.75, rounded, somewhat shouldered. Su- tures impressed. Body whorl 62-74% of shell height. Protoconch tilted relative to teleo- conch. Aperture ovate, apertural plane slightly tilted relative to coiling axis. Inner lip thin, only very slightly reflected, adnate to or slightly separate from body whorl. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Outer lip thin, near-straight. Umbilicus nar- row, chink-like. Protoconch mottled with series of short, predominantly spiral stria- tions (Fig. 59e). Teleoconch with weakly de- veloped spiral lines, particularly on upper whorls. Head/foot and visceral coil usually uni- formly coated with dark brown epithelial VOLUME 102, NUMBER 1 213 Fig. 37. SEM micrographs of P. cf. stearnsiana, USNM 853519, Sand Canyon (a, 3.04 mm; bar = 136 um). pigment. Central portions of sides of head/ foot consisting of either a thin band or broad patch, often lighter or unpigmented. Radular formula (Fig. 60): 4(5)—1-4/1(2)}+ 1, 2(3)}-1-2(3), 16, 20 (from paratypes). Central tooth broadly trapezoidal; basal cusps small, basal process only moderately excavated. Lateral tooth having unusual ““claw-like’’ appearance, with cusps few and widely separated. Penis (Fig. 51b) elongate, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 38. Radula of P. cf. stearnsiana, USNM 857974, Sand Canyon: a, Centrals (bar = 10 wm); b, Laterals (bar = 6.0 um); c, Inner marginal (bar = 8.6 wm); d, Outer marginals (bar = 6.0 wm). distal tip with slightly swollen inner edge. Attachment area broad, with remaining pe- nis near-totally uncoiled. Single, small pa- pillae located on outer curvature near mid- point, and on inner curvature near distal tip. Inner curvature also bearing enlarged, basal papilla. Penial pigmentation consist- ing of small, dark patch near distal tip and/ or light dusting on broad area near base. Type locality.—Grapevine Springs, VOLUME 102, NUMBER 1 Grapevine Mountains, Death Valley, Inyo Co., California. Distribution and habitat. — Found in two thermal, highly mineralized springs on limestone bench in northeast portion of Grapevine Spring complex (32-—36°C, 1 100- 1050 micromhos/cm) (Fig. 52). Etymology.—Named after Peter Row- lands, Resources Management Division, National Park Service, Death Valley, for his efforts in both assisting this study and con- serving local aquatic gastropods in the Mon- ument. Tryonia salina, new species Cottonball Marsh tryonia Figs. 5le, 52, 61, 62 Tryonia sp.— Taylor in LaBounty and Dea- con 1972:775. Material examined.—California: Inyo Co.; Spring in Cottonball Marsh (231), USNM 860410 (holotype), .*853556 (para- types), 22 Feb 1985; *857998, 11 Mar 1987. Diagnosis. —A moderate-sized-species. with elongate-conic shell bearing well-de- veloped spiral striae. Penis with three pa- pillae on inner curvature and single papilla on outer curvature. Description. —Shell (Fig. 61) 2.4—3.1 mm high, height/width, 150—190%. Whorls, 4.5- 5.25, well-rounded, shouldered above. Su- _.tures impressed. Shell loosely coiled, with slight separation of upper whorls common. Body whorl 61-68% of shell. height. Pro- toconch tilted relative to teleoconch. Ap- erture ovate, apertural plane slightly tilted relative to coiling axis. Inner lip thin, only slightly reflected, narrowly adnate to or slightly separated from body whorl. Outer lip thin, near-straight. Umbilicus chink-like to moderately. open. Protoconch smooth (Fig. 61c). Teleoconch with strong, regular- ly-spaced spiral striations, usually continu- ing onto body whorl, interacting with oc- casionaHy highly pronounced growth: lines to produce a weakly cancellate appearance. Brown epithelial pigment dark on snout, 2AS 0.5 mm Fig. 39. Reproductive anatomy of P. cf. stearn- siana, USNM 857974, Sand Canyon: a, Left lateral view of pallial oviduct complex; b-e, Penes (b, c, dorsal aspects; d, e, ventral aspects). dorsal tentacles, and all but narrow central strip of head/foot. Radular (Fig. 62) formula: 5(6)—1-5(6)/ 2(3)—2(3), 3(4)-1-4(5), 19-26, 26-28 (from paratypes). Central tooth broadly trapezoi- dal, basal cusps small, basal process weakly excavated. Penis (Fig. 5le) longer than wide, - moderately thickened. Distal tip with prominent swelling of inner side. Inner cur- vature with two small papillae positioned on inner curvature near tip, and larger basal papilla. Outer curvature with enlarged basal papilla. Dorsal penis variably pigmented by brown epithelial melanin, with especially dark cover on basal penis and papillae. Type locality.—Spring brook in Cotton- ball Marsh, near base of Panamint Moun- tains at west side of salt pan in Death Valley, Inyo Co., California. Distribution and habitat. — Found in a few small, cool, brackish (17°C, >5000 mi- cromhos/cm) spring brooks emerging in 216 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 50 Kilometers Fig. 40. Map showing distribution of P. cf. stearnsiana in the study area. Cottonball Marsh, ca. 1.6 km out onto salt oped shell sculpture, penial lobation pat- pan east of Salt Springs. Snails common on __ tern, and morphology of lateral radular teeth. large, actively growing tufa blocks. Highly remote area in near-pristine condition. Etymology. —Referring to highly miner- alized spring habitat. Amargosa Se Remarks.—Very similar to T. rowlandsi Figs. 51c, 52, 63, 64 from northern Death Valley, but distin- Zryonia variegata Hershler & Sada 1987: guished by larger size, more highly devel- 817. Tryonia variegata Hershler and Sada, 1987 VOLUME 102, NUMBER 1 217 Fig. 41. Camera lucida drawings of shells of P. wongi: a, USNM 853531, spring alongside upper Pine Creek (2.18 mm); b, USNM 853524, spring N of Summit Creek (2.24 mm); c, USNM, 853527, Hogback Creek (Lone Pine) (1.74 mm); d, USNM 853530, spring S of Warren Lake (2.08 mm); e, USNM 853521, spring at Little Lake (1.44 mm); f, USNM 857947, French Spring (2.32 mm); g, USNM 857949, spring at Toll House (1.66 mm); h, USNM 857946, spring (north) at N end of Blind Spring Valley (2.34 mm); 1, USNM 853536, Antelope Spring (1.90 mm); j, USNM 853535, Corral Springs (1.80 mm); k, USNM 853538, River Springs (2.66 mm); 1, USNM 853537, Layton Spring (1.78 mm). Material examined. —California: San Bernardino Co.; Saratoga Spring (204), USNM *853554, 27 Feb 1985; 857995, 10 Jul 1986. Inyo Co.; Spring crossing path on south side of Amargosa Gorge (208), 853553 (empty shell).—Spring in marsh east of Grimshaw Lake (209), *853551, 13 Mar 1985; 857994, 22 Mar 1987.—Shoshone Sprme (11); *853550, 12 Mar 1985; 857993, 16 Mar 1987.—Resting Spring (212). .853552,.13 Mar 1985. Diagnosis.—A variably-sized species with turriform-aciculate shell. Penis large, with 3 or 4 papillae on inner curvature and single 218 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON > Fig. 42. SEM micrographs of P. wongi from west spring in Birchim Canyon: a, Holotype, USNM 860403 (2.14 mm); b, c, Paratypes, USNM 857941 (bar = 136 um). papilla (sometimes absent) on outer cur- 4.75-9.75, slightly to moderately rounded, vature. sometimes slightly shouldered. Sutures im- Description. —Shell (Fig. 63) 1.2-7.5 mm __ pressed. Body whorl 37-63% of shell height. high, height/width, 170-—350%. Whorls, Aperture narrowly ovate, apertural plane VOLUME 102, NUMBER 1 219 Phe ay rhe. Fig. 43. Central radular teeth of P. wongi: a, USNM 857941, west spring in Birchim Canyon (bar = 10 um); b, USNM 853521, spring at Little Lake (bar = 7.5 um); c, USNM 853536, Antelope Spring (bar = 7.5 wm); d, USNM 857981, River Springs (bar = 12 um). near-parallel with coiling axis. Inner lip Umbilicus chink-like to moderately open. slightly thickened and reflected, adnate to Protoconch smooth to irregularly wrinkled or slightly separated from body whorl. Out- (Fig. 63d). Growth lines often highly pro- er lip thin, slightly to moderately sinuate. nounced. 220 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON " ‘ 35 . “a 7 Fig.44. Lateral and marginal teeth of P. wongi: a (laterals), c (laterals and inner marginals), d (outer marginals), USNM 857941, west spring in Birchim Canyon (bars = 6.0 um); b, Laterals, USNM 853536, Antelope Spring (bar = 6.0 um). VOLUME 102, NUMBER 1 Fig. 45. 221 Reproductive anatomy of P. wongi: a, Left lateral view of pallial oviduct complex, USNM 857941, west spring in Birchim Canyon; b-—l, Dorsal penes (b, USNM 857941, west spring in Birchim Canyon; c, USNM 853530, spring S of Warren Lake; d, USNM 857981, River Springs; e, USNM 857979, Corral Springs; f, USNM 857980, Layton Spring; g, USNM 857947, French Spring; h, USNM 857949, spring at Toll House; i, USNM 853534, spring (north) at northern end of Blind Spring Valley; 3, USNM 857978, spring in Owens Gorge; k, USNM 857942, spring alongside Lubkin Creek; 1, USNM 853523, Summit Creek). “‘c’—“‘l’? drawn to same scale. ‘ Radular (Fig. 64) formula: (4—7)—1-(4-7)/ 2(3)—2(3), 3(4)-1-4(5), 17-30, 22-33 (from numerous populations). Central tooth typ- ically broadly trapezoidal; basal cusps mod- erate to large-sized, basal process moder- ately excavated. Epithelial pigment usually dark brown- black on snout and sides of head/foot, with lighter cover on central portions of latter. Type locality. —Five Springs, Ash Mead- ows, Nye County, Nevada. Distribution and habitat. —Amargosa River drainage, from Ash Meadows south to Saratoga Spring. Snails typically common 222 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 46. Penes (ventral aspects) of P. wongi: a, USNM 857941, west spring in Birchim Canyon; b, USNM 857947, French Spring; c, USNM 853536, Antelope Spring; d, USNM 857942, spring alongside Lublin Creek; e, USNM 853534, spring (north) at northern end of Blind Spring Valley; f, USNM 857981, River Springs; g, USNM 857949, spring at Toll House; h, USNM 857979, Corral Spring; 1, USNM 853523, Summit Creek. “a’— ““e” and “‘g’—“‘1” drawn to same scale. on various substrates in small springpools and upper portions of outflows (7—-32°C, 430-10,150 micromhos/cm). Remarks. —Populations from lower Amargosa River drainage are clearly as- signable to 7. variegata on basis of shell, radular, and penial features. Morphometrics Discriminant analyses were performed on each of three groups of congeners from giv- en portions of the study area: a) P. amar- gosae and P. micrococcus, very similar forms with contiguous ranges; b) Pyrgulopsis fau- na of Owens Valley (P. aardahli, P. owen- sensis, P. perturbata, P. cf. stearnsiana, P. wongl); and c) small-sized Tryonia spp., in- cluding those of northern Death Valley (T. salina, T. rowlandsi, T. margae) and Ash Meadows (T. ericae, T. elata). Results (Summarized in Tables 3-5) sup- port taxonomy presented herein, insofar as high correct classifications (81-87% [over- all]) indicate that these snails are well-dif- ferentiated in shell features. In the analysis involving P. amargosae and P. micrococcus, correct classification was 89% (40/45) and 80% (291/362) for each species, respective- ly. Correct classification for two populations of P. amargosae (Amargosa Gorge, Grim- shaw Lake) from Tecopa area (where the ranges abut) was high (83%), as was that (92%) for two nearby populations of P. mi- VOLUME 102, NUMBER 1 Kilometers Fig. 47. Map showing distribution of P. wongi. crococcus (Tecopa Hot Springs, Shoshone Spring). Misclassified specimens of P. mi- crococcus were concentrated in a few pop- ulations in northern Death, Panamint, and Saline Valleys (well separated from the range of P. amargosae), and indicate local differ- entiation of this relatively widespread form. 223 In this analysis, discrimination was based largely on height of shell and aperture. For the Owens Valley Pyrgulopsis, correct classification was 84% overall (382/451), and ranged from 79-87% by species. The sole species having <80% correct classifi- cation, P. owensensis, was most frequently 224 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 48. SEM micrographs of T. margae: a—d, Grapevine Springs, upper warm spring (a, holotype, USNM 860408, [3.52 mm]; b-d, Paratypes, USNM 857952); e-g, USNM 853555, Grapevine Springs, spring above shack (bar = 86 um). VOLUME 102, NUMBER 1 225 Fig. 49. Central and lateral radular teeth of T. margae: a,c, USNM 857953, Grapevine Springs, upper warm spring (a, centrals, bar = 6.7 um; c, laterals and inner marginals, bar = 6.7 um); b, d, USNM 857996, Grapevine Springs, spring above shack (b, centrals, bar = 6.7 um; d, laterals, bar = 6.7 um). (10/14) misclassified as P. wongi, which nant function were related to size and width cannot be confused with the former when of shell and aperture. penial morphology is considered. Parame- Classification of each of the three small- ters weighing heavily on the first discrimi- sized Tryonia spp. from northern Death PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 50. Marginal radular teeth of T. margae: a, c, USNM 857953, Grapevine Springs, upper warm spring (a, laterals and inner marginals, bar = 10.0 um; c, outer marginal, bar = 3.8 um); b, d, USNM 857996, Grapevine Springs, spring above shack (b, laterals and inner marginals, bar = 7.5 um; d, outer marginal, bar = 3.8 um). Valley was 100%, while that of 7. elata and T. ericae from Ash Meadows was 93% and 95%, respectively. Despite their general similarity in form, 7. margae and T. elata were well-discriminated, with only a single specimen (of the latter) misclassified (as the former). Parameters weighing heavily on the first discriminant function were shell height, VOLUME 102, NUMBER 1 0.5 mm 1.0 mm Fig. 51. Penes (dorsal aspects) of Tryonia spp.: a, T. margae, USNM 857952, Grapevine Springs, upper warm spring; b, 7. rowlandsi, USNM 857953, Grape- vine Springs, upper warm spring; c, 7. variegata, USNM 857994, spring at Grimshaw Lake; d, T. robusta, USNM 857999, Nevares Springs, upper spring; e, 7. salina, USNM 857998, Cottonball Marsh. “a,” “b,”’ “‘d,”’ “‘e”’ drawn to same scale. width of body whorl, and aperture size and shape. Discussion Modern drainage in the Death Valley area includes Owens, Amargosa, and Mojave Rivers, the latter two of which are dry along most of their courses. Although now iso- lated from one another, these river systems were integrated during wetter, pluvial times during the Pleistocene as a series of lakes overflowed along their courses to terminate in Death Valley. This Death Valley System (named by Miller 1943:69) was initially proposed by Gale (1914) and Blackwelder (1933), and has been discussed in detail by many others (Hubbs & Miller 1948; Miller 1946, 1948; Smith 1978; Soltz & Naiman 227 Table 3.—Results of discriminant function analysis on Pyrgulopsis amargosae and P. micrococcus. Also given are the canonical correlation, number of speci- mens used (by species, ordered as above), and percent correct classification (overall). Standardized Variables coefficients Correlations WH 0.365 0.554 SH 1.194 0.354 SW 0.398 —0.094 LBW =—§: 717 0.176 WBW 0.749 0.146 AL 1-928 0.055 AW —0.067 —0.108 WwW 0.176 ==§:292 D 0.798 0.536 a: —0.390 0.425 SA 0.871 0.351 C. correlation 0.475 N 45,362 % correct classification 81 1978; Smith & Street-Perrott 1983; Minck- ley et al. 1986; Taylor 1986). Configuration of the System is portrayed in Fig. 65 as pre- lude to discussion of springsnail zoogeog- raphy. Springsnail distributions reflect pro- nounced local endemism of the modern fau- na. Twenty of 22 species known from Death Valley System area are restricted to its con- fines. Of these, 10 are endemic to single springs or spring complexes, and another seven occur in relatively small portions of single modern drainage basins. Locally en- demic Pyrgulopsis are concentrated in Ow- ens Valley and Ash Meadows, while endem- ic 7ryonia occur in the latter and northern Death Valley. Three forms are relatively widespread in the system: P. wongi, of plu- vial Owens River drainage (Long, Adobe, Owens Valleys); P. micrococcus, widely dis- tributed from Amargosa Valley west to Pan- amint Valley; and 7. variegata, of pluvial Amargosa River drainage (Ash Meadows, Tecopa Basin, Saratoga Spring [southern Death Valley]). Endemic Pyrgulopsis of Owens Valley and 228 Kilometers Fig. 52. Map showing distribution of 7Jryonia spp. in Ash Meadows. Amargosa Basin are sharply differentiated on basis of penial morphology and represent separate local radiations. Owens. Valley forms, characterized in part by possession of a ventral penial swelling bearing glan- dular ridge (absent in forms endemic to PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON T. margae o T. protea a T. robusta = -T. rowlandsi o T. salina a i _T. variegatae = — in study area. Tyronia variegata occurs at 18 localities Amargosa drainage), include a group com- prising P. cf. stearnsiana and similar, en- demic forms (P. aardahli, P. owensensis, P. perturbata); and P. wongi, which has no close relatives in the study area. Ash Meadows (Amargosa Basin) endemics represent at VOLUME 102, NUMBER 1 Fig. 53. SEM micrographs of T. protea, USNM 857954, Hot Creek. Shell “a” 229 7 sj ] - - 7s s 3 . . j ~ 7 j}° * * ‘ > . 7 . - - . _ A pe + afr A > - 7 4 ; s Ps . 2s - — * > J 7 “ is 3.64 mm tall. “b,” “‘c” show sculpture on protoconch of embryonic shell (bars = 60, 17.6 um). least two lineages (both including Flumin- icola-like representatives): snails with re- duced or absent penial lobes and a glandular ridge on mid-ventral penial surface (P. erythropoma, P. crystalis, P. pisteri); and those having a ridge on terminal portion of moderate-large sized penial lobes (P. fair- banksensis, P. nanus, P. isolatus). The latter may be related to the probable sister species pair of widespread P. micrococcus and P. amargosae from southern Amargosa River drainage. Relationships among regional 7ryonia are more speculative. Endemic 7Jryonia in Table 4.—Results of discriminant function analysis on Owens Valley Pyrgulopsis (P. aardahli, P. owensensis, P. perturbata, P. cf. stearnsiana, P. wongi). Also given are canonical correlations, number of specimens used (by species, ordered as above), and percent correct classification (overall). Standardized coefficients Variable Function | WH 0.580 SH Sie T/he SW 1.037 LBW O51S WBW 1.367 AL 2.937 AW een WwW 0.075 D 0.285 T —0.143 SA —0.810 C. correlation 0.771 N 15, 86, 39, 25, 286 % correct classification 84 Correlations Function 2 Function 1 Function 2 —0.841 Se | ee (7 =—O714 0.489 —0.708 —0.534 2.483 —0.549 —0.466 2 501 —0.641 == | Ta PA =29 —0.558 0.333 =0:550 i553 —0.424 1.822 —0.617 —0.387 =@.3f7 0.255 —0.068 0.453 OOS —0.120 0.904 =0-397 —0.042 0.600 0.085 —0.164 0.687 230 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 54. Radula of T. protea, USNM 857954, Hot Creek: a, Centrals (bar = 12 um); b, c, Laterals and inner marginals (bars = 8.6 um); d, Outer marginals (bar = 7.5 wm). VOLUME 102, NUMBER 1 231 Fig. 55. (1.92 mm); b-d, Paratypes, USNM 853557. northern Death Valley and Ash Meadows, apart from enigmatic T. robusta, apparently comprise a single local radiation. T. protea from west of Death Valley (Long and [fossil; Taylor 1985:317] Panamint Valleys) is quite similar (in shell) to at least one represen- SEM micrographs of 7. robusta from Nevares Springs, upper spring: a, Holotype, USNM 860411 tative from the east, 7. variegata (contrary to Taylor 1985:317) and may not represent a separate lineage (as implied by Taylor 1985:317). Pluvial waters of the Death Valley System provided aquatic continuity (and thus the Table 5.—Results of discriminant function analysis on small-sized Tryonia (T. elata, T. ericae, T. margae, T. rowlandsi, T. salina). Also given are canonical correlations, number of specimens used (by species, ordered as above), and percent correct classification (overall). Standardized coefficients Variable Function 1 WH —0.044 SH P92 SW 0.393 LBW 0.423 WBW = |\-)5)// AL ieols AW 0.003 W —0.031 D 0.286 Tp —0.071 SA 0.736 C. correlation 0.994 N 30: 19: 6, 16, 15 % correct classification 97 Correlations Function 2 Function 1 Function 2 0.672 0.109 0.487 0.600 —OaWs 0.699 O735 —0.580 0.432 02227 —0.402 O:535 —0.908 —0:521 0.493 —0.341 —O:510 0.580 0.634 —0:622 0.405 0.081 =U. a a=) eel 0.191 0.032 —0.030 0.429 0.131 0.427 0.828 0.073 0.353 0.975 232 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 56. SEM micrographs of T. robusta, Nevares Springs, upper spring, USNM 853557: a-c, Views of apex (bars = 75, 43, 100 um); d, Dorsal operculum (bar = 200 um). VOLUME 102, NUMBER 1 233 Fig. 57. Radula of 7. robusta, Nevares Springs, upper spring, USNM 857999: a, Centrals (bar = 6.0 um); b, c, Laterals and inner marginals (bars = 3.8, 5.0 um); d, Outer marginals (bar = 3.8 wm). 234 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 58. SEM micrographs of penes of T. robusta, USNM 857999, Nevares Springs, upper spring: a, Dorso- right lateral aspect, with attachment to head on lower left (bar = 136 um); b, Distal tip of papilla (bar = 23.1 um); c, d, Distal tips of penis, showing ciliation (bars = 30, 20 um). VOLUME 102, NUMBER 1 235 Fig. 59. SEM micrographs of 7. rowlandsi from Grapevine Springs, upper warm spring: a, Holotype, USNM 860409 (2.18 mm); b-e, Paratypes, USNM 857953 (bar = 100 um). PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 60. Radula of 7. rowlandsi, USNM 857953, Grapevine Springs, upper warm spring: a, Centrals (bar = 15 um); b, Laterals (bar = 13.6 wm); c, Inner marginal (bar = 6.0 um); d, Outer marginals (bar = 5.0 um). means for potential exchange ofaquatic fau- ern springsnail zoogeography indicates that na) across current drainage dividesimposed the above did not facilitate much mixing by the region’s predominant north-south between pluvial Owens and Amargosa Riv- trending basin and range topography. Mod- er faunas. These results support earlier con- VOLUME 102, NUMBER 1 Fig. 61. clusions of Taylor (in Miller 1981:58, 1985: 317-318), although his observation that “Spillover from Lake Panamint into Death Valley ... had no recognizable effect on mollusc distribution” (Taylor 1985:318) is contradicted by distribution of P. micro- coccus (and possible close affinities between T. protea and congeners to the east). Taylor (1985:317) suggested that faunal exchange between Amargosa and Owens River drainages might have been precluded by a saline dispersal barrier consisting of an arm of Bouse embayment (from former Gulf of California) extending into Death Valley. Although this hypothesis appears plausible, it may not need to be invoked to explain patterns described above. Apart from ad- ditional influences on snail distribution im- posed by far older lacustrine episodes than considered above (Smith 1984) and other aspects of complex regional geologic/hydro- logic history (Minckley et al. 1986), fun- damental questions relating to types of hab- itat occupied by Pleistocene springsnails and plausibility of dispersal of such (frequently stenotopic) organisms along chains of plu- 23ST SEM micrographs of T. salina from Cottonball Marsh: a, Holotype, USNM 860410 (3.27 mm); b, c, Paratypes, USNM 853556 (bar = 120 um). vial lakes have not been thoroughly inves- tigated (see Hershler and Minckley 1986). Details such as size, number, and salinity of inter-connected lakes; and length and gra- dient of lake outlets obviously would affect probability of snail dispersal. Further, other modes of dispersal undoubtedly occurred and could have produced distributions comparable to or conflicting with those pre- dicted by pluvial drainage models. The presence of fauna in isolated basins recently created or devastated by volcanic activity (Long, Adobe Valleys, respectively), or those that either lacked pluvial connections (Sa- line Valley, Frenchman Flat [Cane Spring]; Hubbs and Miller 1948) or connected with snailless areas (Deep Springs Valley, whose pluvial lake spilled into Eureka Valley; Mil- ler 1928) attests to importance of factors other than late Pleistocene pluvial drainage systems in effecting modern snail distribu- tions in the region. A detailed zoogeograph- ic analysis encompassing the above consid- erations will be provided following completion of springsnail survey of remain- ing portions of the Death Valley System. 238 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 62. Radula of T. salina, USNM 857998, Cottonball Marsh: a, Centrals (bar = 10 um); b, Laterals and inner marginal (bar = 7.5 wm); c, Inner and outer marginals (bar = 8.6 wm); d, Outer marginal (bar = 5.0 um). VOLUME 102, NUMBER 1 239 Fig. 63. SEM micrographs of 7. variegata: a (2.8 mm), b, USNM 853554, Saratoga Spring; c (2.86 mm), d, USNM 853550, Shoshone Spring (bar = 86 um). | | | passin Fig. 64. Radula of 7. variegata: a,b, USNM 857995, Saratoga Spring (a, centrals, bar = 10.0 um; b, laterals, bar = 7.5 wm); c, d, USNM 857993, Shoshone Spring (c, laterals and inner marginals, bar = 6.0 wm; d, outer marginal, bar = 4.3 wm). — Fig. 65. Map of Pleistocene Death Valley System showing drainage relations (not necessarily contempora- neous). Stippled areas encircled by dashed lines may not have contained lakes for significant portions of the pluvial period. In the northeast, Lake Russell (Mono Valley) spilled into Lake Adobe (Adobe Valley), which in turn overflowed (through a gap in Benton Range) to enter the (now mostly dry) north fork of ancestral Owens River (Putnam 1949; Hubbs and Miller 1948; Gilbert et al. 1968). Lake Long Valley filled shortly after Long Valley caldera was created by explosive eruption of Bishop tuff 700,000 BP (Bailey et al. 1976), and spilled into south fork of Owens River. Outflow from Owens Lake, possibly initiated as a result of increased flow due to 240 C5 5 fe) 25 50 75 L. Long Valley | | | | Kilometers L. Searles L. Mojave to Colorado R. Base map from Snyder et al. 1964 118° capture of upper San Joaquin River drainage in Long Valley (Huber 1981, Smith et al. 1983), passed between Sierra Nevada and Coso Range to enter and fill China and Searles Lakes. Searles Lake overflowed into Panamint Valley, which held a large lake in its southern portion that spilled into Death Valley during several periods between 120,000 and 20,000 BP (Gale 1914, Hooke 1972, Smith 1976, Hale 1984). To the west, the lush wetland of Ash Meadows (that did not have a large pluvial lake; Mifflin and Wheat 1979, Hay et al. 1986) drained at least intermittently to Amargosa River during Pliocene-Pleistocene. Further downflow the river was ponded in mid- to late-Pleistocene by alluvial fans above Amargosa Gorge to form Lake Teopa (Sheppard and Gude 1968, Starkey and Blackmon 1979), which spilled into southern Death Valley. Mojave River filled a series of three pluvial lakes, with Lake Mojave overflowing toward southern Death Valley during several intervals of late Pleistocene from > 14,500—9000 BP (Ore and Warren 1971). Overflow from Death Valley System to Colorado River during an extreme pluvial period is conjectural, and has often been hypothesized based on distribution of aquatic biota (Miller 1981, Taylor 1986). Hale (1984) described an old (pre-Pleistocene) fluvial channel at Ash Hill near Ludlow, CA, that could be a product of such outflow. The channel is at 594 m elevation, which would require a vast pluvial lake (> 300 km long and >650 m maximum depth) extending to northern Death Valley: additional geological evidence is needed to confirm this remarkable possibility. 241 242 Acknowledgments Fieldwork in the Death Valley area was supported by Smithsonian Institution Re- search Opportunity Fund (ROF), Wildlife Conservation International of the New York Zoological Society, and contracts awarded by U.S. Fish and Wildlife Service, Great Basin Complex (Order No. 14320-0182); Bureau of Land Management, California Desert District (CA-060-CT5); and Califor- nia Fish and Game (C-1922). Collecting permits were provided by National Park Service (Death Valley National Monument) and State of California, and access to sites on Nevada Test Site, China Lakes Naval Weapons Center, and Fort Irwin is also gratefully acknowledged. Bureau of Land Management (District offices in Ridgecrest and Bishop), California Fish and Game (Bishop office), and National Park Service (Death Valley National Monument) loaned field vehicles and provided other forms of logistic support. Field assistance was pro- vided by numerous individuals, especially J. Aardahl, R. Brown, W. Cassidy, T. Ford, D. Giuliani, D. Herbst, B. Kohfield, P. Rowlands, and D. Wong. Heidi Wolf sorted material and produced excellent SEM mi- crographs. Paul Greenhall digitized shell material. Molly Ryan drew shells and draft- ed maps (with assistance from C. Flamer). Literature Cited Bailey, R. A., G. B. Dalrymple, & M. A. Lanphere. 1976. Volcanism, structure, and geochronology of Long Valley Caldera, Mono County, Califor- nia.— Journal of Geophysical Research 81:725- 744. Blackwelder, E. 1933. Lake Manley: An extinct lake of Death Valley.— Geographical Review 24:464— 471. Blake, W. P. 1857. Geological Report.— United States War Department Pacific Railroad Surveys 5:1- 310. Chapman, R. E., M. G. Harasewych, & R. Hershler. [In Preparation.] CONCH: An interactive com- puter program for the analysis of shell coiling parameters. Conrad, T. A. 1855. Description of a new species of PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Melania. — Proceedings of the Academy of Nat- ural Sciences of Philadelphia 7:269. Gale, H. S. 1914. Salines in the Owens, Searles, and Panamin Basins, southeastern California. — United States Geological Survey Contributions to Economic Geology (1913):251-323. Gilbert, C. M., M. N. Christensen, Y. Al-Rawi, & K. R. Lajoie. 1968. Structural and volcanic his- tory of Mono Basin, California-Nevada. —Geo- logical Society of America Memoir 116:275- 329. Gould, A. A. 1855. New species of land and fresh- water shells from western America.—Proceed- ings of the Boston Society of Natural History 5: 127-130. Gregg, W. O., & D. W. Taylor. 1965. Fontelicella (Prosobranchia: Hydrobiidae), a new genus of West American freshwater snails. — Malacologia 3:103-110. Hale, G. R. 1984. Reassessment of the Death Valley- Colorado River overflow hypothesis in light of new evidence. Ph.D. dissertation (unpublished), University of California, Berkeley, 291 pp. Hay, R. L., R. E. Pexton, T. T. Teague, & T. K. Kyser. 1986. Spring-related carbonate rocks, Mg clays, and associated minerals in Pliocene deposits of the Amargosa Desert, Nevada and California. — Geological Society of America 97:1488-1503. Hershler, R., & W. L. Minckley. 1986. Microgeo- graphic variation in the banded spring snail (Hy- drobiidae: Mexipyrgus) from the Cuatro Cie- negas Basin, Coahuila, Mexico.—Malacologia 27:357-374. ——., & D. W. Sada. 1987. Springsnails (Gastro- poda: Hydrobiidae) of Ash Meadows, Amar- gosa Basin, California-Nevada.— Proceedings of the Biological Society of Washington 100:776— 843. —, & F.G. Thompson. 1987. North American Hydrobiidae (Gastropoda: Rissoacea): Rede- scription and systematic relationships of Tryon- ia Stimpson, 1865 and Pyrgulopsis Call and Pils- bry, 1886.—Nautilus 10:25-32. Hewett, D. F. 1954. Geology of the Natural Prov- inces. Pp. 5—20 in R. H. Jahns, ed., Geology of Southern California, California Division of Mines Bulletin 170, Chapter II. Hooke, R. L. 1972. Geomorphic evidence for Late- Wisconsin and Holocene tectonic deformation, Death Valley, California.— Geological Society of America Bulletin 83:2073-2098. Hubbs, C. L., & R. R. Miller. 1948. Correlation be- tween fish distribution and hydrographic history in the desert basins of western United States. Pp. 17-166 in The Great Basin, with emphasis on Glacial and Postglacial times. Bulletin of the University of Utah 38, Biological Series 10. VOLUME 102, NUMBER 1 Huber, N. K. 1981. Amount and timing of Late Ce- nozoic uplift and tilt of the Central Sierra Ne- vada, California—evidence from the Upper San Joaquin River Basin. — United States Geological Survey Professional Paper 1197:1-28. Kohn, A. J., & A. C. Riggs. 1975. Morphometry of the Conus shell.—Systematic Zoology 24:346- B59: LaBounty, J. F., & J. E. Deacon. 1972. Cyprinodon milleri, a new species of pupfish (Family Cy- prinodontidae) from Death Valley, Califor- nia.—Copeia 1972:769-780. Mifflin, M. D., & M. M. Wheat. 1979. Pluvial lakes and estimated pluvial climates of Nevada. — Ne- vada Bureau of Mines and Geology 94:1-57. Miller, R.R. 1943. Cyprinodon salinus, a new species of fish from Death Valley, California.—Copeia 1943:69-78. 1946. Correlation between fish distribution and Pleistocene hydrography in eastern Cali- fornia and southwestern Nevada, with a map of the Pleistocene waters. — Journal of Geology 54: 43-53. 1948. The cyprinodont fishes of the Death Valley System of eastern California and south- western Nevada.— Miscellaneous Publications of the Museum of Zoology, University of Mich- igan 68:1-155. 1981. Coevolution of desert and pupfishes (genus Cyprinodon) in the American Southwest. Pp. 39-94 inR. J. Naiman and D. L. Soltz, eds., Fishes in North American deserts. John Wiley and Sons, New York. —, & E. P. Pister. 1971. Management of the Owens Pupfish, Cyprinodon radiosus, in Mono County, California. — Transactions of the Amer- ican Fisheries Society 100:502-509. Miller, W. J. 1928. Geology of Deep Spring Valley, California.— Journal of Geology 36:510-525. Minckley, W. L., D. A. Hendrickson, and C. E. Bond. 1986. Geography of western North American freshwater fishes: Description and relationships to intracontinental tectonism. Pp. 519-613 in C. H. Hocutt and E. O. Wiley, eds., Zoogeog- raphy of North American freshwater fishes. John Wiley and Sons, New York. Ore, H. T., & C. N. Warren. 1971. Late Pleistocene- Early Holocene geomorphic history of Lake Mo- jave, California.— Geological Society of Amer- ica Bulletin 82:2553-2562. Pilsbry, H. A. 1899. Catalogue of the Amnicolidae of the Western United States. — Nautilus 12:121- 127. Putnam, W.C. 1949. Quaternary geology of the June Lake District, California.— Bulletin of the Geo- logical Society of America 60:1281-1302. Sheppard, R. A., & A. J. Gude. 1968. Distribution 243 and genesis of authigenetic silicate minerals in tuffs of Pleistocene Lake Tecopa, Inyo County, California.— United States Geological Survey Professional Paper 597:1-38. Smith, G. I. 1984. Paleohydrologic regimes in the southwestern Great Basin, 0-3.2 my Ago, com- pared with other long records of “global’’ cli- mate.— Quaternary Research 22:1-17. , V. J. Barczak, G. F. Moulton, & J. C. Liddicoat. 1983. Core KM-3, a surface-to-bedrock record of Late Cenozoic sedimentation in Searles Val- ley, California.— United States Geological Sur- vey Professional Paper 1256:1-24. —., & F. A. Street-Perrott. 1983. Pluvial lakes of the United States. Pp. 190-212 in H. E. Wright, ed., Late-quaternary environments of the United States, Volume 1, The Late Pleistocene (S. C. Porter, ed.). University of Minnesota Press, Minneapolis. Smith, G. R. 1978. Biogeography of intermountain fishes. Pp. 17-42 in K. T. Harper and J. L. Re- veal, eds., Intermountain biogeography, a sym- posium. Great Basin Naturalist Memoir 2. Smith, R. S. 1976. Late-Quaternary pluvial and tec- tonic history of Panamint Valley, Inyo and San Bernardino Counties, California. Ph.D. disser- tation (unpublished), California Institute of Technology, 295 p. Snyder, C. T., G. Hardman, & F. F. Sdenek. 1964. Pleistocene lakes in the Great Basin.— United States Geological Survey Miscellaneous Geo- logical Investigations Map I-416. Soltz, D. L., & R. J. Naiman. 1978. The natural history of native fishes in the Death Valley Sys- tem.— Natural History Museum of Los Angeles County, Science Series 30:1-76. Starkey, H. C. & P. D. Blackmon. 1979. Clay min- eralogy of Pleistocene Lake Tecopa, Inyo Coun- ty, California.— United States Geological Sur- vey Professional Paper 1061:1-34. Stearns, R.E.C. 1893. Report on land and freshwater shells collected in California and Nevada by the Death Valley Expedition, including a few ad- ditional species obtained by Dr. C. Hart Mer- riam and assistants in parts of the southwestern United States. —North American Fauna 7:269- 283. Taylor, D. W. 1950. Three new Pyrgulopsis from the Colorado Desert, California.— Leaflets in Mal- acology 1:27-33. . 1966. Summary of North American Blancan nonmarine mollusks. — Malacologia 4:1-172. 1981. Freshwater mollusks of California: A distributional checklist.—California Fish and Game 67:140-163. 1985. Evolution of freshwater drainages and molluscs in western North America. Pp. 265- 244 321 inC. J. Hocutt and A. B. Leviton, eds., Late Cenozoic History of the Pacific Northwest. American Association for the Advancement of Science, San Francisco, California. Wilkinson, L. 1986. SYSTAT: The system for sta- tistics. SYSTAT, Inc., Evanston, IL. Department of Invertebrate Zoology, NHB STOP 118, National Museum of Nat- ural History, Smithsonian Institution, Washington, D.C. 20560. Appendix Collection localities, numbered as in Figs. 2-7. Data include name of site, state, county, topographic sheet, township and range coordinates, site elevation, and date of visitation (for negative sites only). 1. Stream in Sage Canyon. CA: Kern; Horse Canyon, CA (7.5), 7.0 km SW of NE corner of quadrangle, 1342 m. 2. Boulder Spring. CA: Kern; Horse Canyon, CA, 5.6 km S-SW of NE corner of quadrangle, 1251 m, 3-26-87. 3. Stream in Indian Wells Canyon. CA: Kern; Inyokern, CA, NW '4 sec. 17, T 26S, R 38E, 1068 m, 3-26-87. 4. Spring in SW corner of Short Canyon. CA: Kern; Inyokern, CA, NW 4 sec. 5, T 26S, R 38E, 1129 m, 3-26-87. 5. Stream in Grapevine Canyon. CA: Kem; Inyokern, CA, center of sec. 29, T 25S, R 38E, 946 m, 3-26-87. 6. Stream in Sand Canyon. CA: Kern; Little Lake, CA, center of sec. 7, T 25S, R 38E, 1068 m. 7. Stream in Noname Canyon. CA: Kern; Little Lake, CA, 10.0 km NE of SW corner of quadrangle, 976 m, 3-26-87. 8. Stream in Ninemile Canyon. CA: Inyo; Little Lake, CA, 12.2 km NE of SW corner of quad- rangle, 976 m, 3-26-87. 9. Spring 0.8 km §S of Little Lake, W of HW 395. CA: Inyo; Little Lake, CA, SE sec. 18, T 23S, R 38E, 946 m, 4-1-87. 10. Spring at Little Lake, E of HW 395. CA: Inyo; Little Lake, CA, NW 4 sec. 17, T 23S, R 38E, 946 m. 11. Stream in Little Lake Canyon. CA: Inyo; Little Lake, CA, NE % sec. 12, T 23S, R 37E, 1129 m, 4-1-87. 12. Springs ca. 1.0 km N of Little Lake Canyon. CA: Inyo; Little Lake, CA, SW sec. 1, T 23S, R 37E, 1159 m, 4-30-87. 13. Stream in canyon ca. 3.0 km N of Little Lake Canyon. CA: Inyo; Little Lake, CA, 4.4 km SE of NW corner of quadrangle, 1220 m, 4-30-87. 14. Stream in Por- tugese Canyon. CA: Inyo; Haiwee Reservoir, CA, 2.19 km NE of SW corner of quadrangle, 1342 m, 4-1-87. 15. Springs on Portugese Bench. CA: Inyo; Haiwee Reservoir, SW corners of secs. 3, 10, T 22S, R 37E, 1160-1220 m, 4-30-87. 16. Lower spring in Tunawee Canyon. CA: Inyo; Haiwee Reservoir, CA, SW ' sec. 33, T 21S, R 37E, 1373 m, 4-25-87. 17. Upper spring in Tunawee Canyon. CA: Inyo; Monache Mtn., CA, 7.0 km N-NW of SE corner of quadrangle, 1525 m, 4-30-87. 18. Haiwee Creek. CA: Inyo; Monache Min.., PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON CA, 12.6 km S-SW of NE corner of quadrangle, 1586 m, 4-30-87. 19. Springs in (2) unnamed canyons N of Haiwee Canyon. CA: Inyo; Monache Mtn., CA, NW corners secs. 30, 31, T 20S, R 37E, 1556 m, 4-30-87. 20. Hogback Creek. CA: Inyo; Monache Mtn., CA, 7.3 km SW of NE corner of quadrangle, 1586 m. 21. Sum- mit Creek. CA: Inyo; Monache Mtn., CA, NE 4 sec. 7, T 20S, R 37E, 1373 m. 22. Spring ca. 3.0 km N of Summit Creek. CA: Inyo; Monache Mtn, CA, center of sec. 6, T 20S, R 37E, 1281 m. 23. Walker Creek. CA: Inyo; Monache Mtn., CA, NE 4% sec. 34, T 19S, R 37E, 1769 m, 4-16-87. 24. Cartago Creek. CA: Inyo; Olancha, CA, NE ‘4 sec. 11, T 19S, R 37E, 1159 m, 4-16-87. 25. Spring at Cabin Bar Ranch, ca. 2.5 km N of Olancha. CA: Inyo; Olancha, CA, SW 4 sec. 6, T 19S, R 37E, 1098 m. 26. Braley Creek and springs just to S. CA: Inyo; Olancha, CA, 10.0 km NW of SEcorner of quadrangle, 1190 m, 4-16-87. 27. Springs on edge of Owens Lake at Permanente. CA: Inyo; Olancha, CA, 13.8 km N of SE corner of quadrangle, 1068 m, 2-9- 85. 28. Ash Creek. CA: Inyo; Olancha, CA, 15.6 km NW of SE corner of quadrangle, 1068 m, 4-16-87. 29. Cottonwood Creek. CA: Inyo; Olancha, CA, 9.6 km SW of NE corner of quadrangle, 1037 m, 4-16-87. 30. Lower Centennial Spring. CA: Inyo; Keeler, CA, 2.3 km W of SE corner of quadrangle, 1769 m, 3-31-87. 31. Dirty Socks (Hot Spring). CA: Inyo; Keeler, CA, NE 4 sec. 34, T 18S, R 37E, 1098 m, 2-9-85. 32. Springs at S end of Owens Lake, ca. 3.5 km NW of Dirty Socks. CA: Inyo; Keeler, CA, NW 4 sec. 17, T 18S, R 38E, 1098 m, 2-9-85. 33. Springs on edge of Owens Lake, ca. 3.0 km S of Keeler. CA: Inyo; Keeler, CA, NW 4 sec. 22, T 17S, R 38E, 1098 m, 4-25-87. 34. Lubkin Creek and spring feeding creek from south. CA: Inyo; Lone Pine, CA, SE 4 sec. 16, T 16S, R 36E, 1220 m. 35. Spring along E side of Tuttle Creek. CA: Inyo; Lone Pine, CA, NE 4 sec. 6, T 16S, R 36E, 1281 m. 36. Hogback Creek. CA: Inyo; Lone Pine, CA, NW %, sec. 2, T 15S, R 35E, 1159 m. 37. Spring at NE end of Alabama Hills, ca. 4.2 km N-NW of Lone Pine. CA: Inyo; Lone Pine, CA, NE 4 sec. 31, T 14S, R 36E, 1159 m, 4-25-87. 38. George Creek. CA: Inyo; Lone Pine, CA, NE 4 sec. 27, T 14S, R 35E, 1251 m, 4-25- 87. 39. Independence Creek. CA: Inyo; Independence, CA, SE 4 sec. 23, T 13S, R 34E, 1342 m, 4-17-87. 40. Boron Springs. CA: Inyo; Mt. Pinchot, CA, NW '% sec. 22, T 13S, R 34E, 1556 m. 41. Oak Creek, south fork. CA: Inyo; Mt. Pinchot, CA, SW 4 sec. 10, T 13S, R 34E, 1525 m, 4-17-87. 42. Springs ca. 1.0 km W of Mt. Whitney Fish Hatchery. CA: Inyo; Mt. Pinchot, CA, SE 4 sec. 3, T 13S, R 34E, 1342 m, 4-18-87. 43. Stream in Charlie Canyon. CA: Inyo; Mt. Pinchot, CA, SW sec. 3, T 13S, R 34E, 1617 m. 44. Springs feeding N fork Oak Creek. CA: Inyo; Mt. Pinchot, CA, SW sec. 3, T 13S, R 34E, 1586 m, 4-25-87. 45. Oak Creek, north fork. CA: Inyo; Mt. Pinchot, CA, center of sec. 3, T 13S, R 34E, 1525 m, 4-17-87. 46. Grover Anton Spring. CA: Inyo; Mt. Pinchot, CA, SW 4 sec. 20, T VOLUME 102, NUMBER 1 12S, R 34E, 1586 m, 4-18-87. 47. Harry Birch Springs. CA: Inyo; Mt. Pinchot, CA, NW '%4 sec. 17, T 12S, R 34E, 1464 m, 4-18-87. 48. Sawmill Creek. CA: Inyo; Mt. Pinchot, CA, SW '% sec. 9, T 12S, R 34E, 1251 m, 4-17-87. 49. Division Creek and Scotty Springs just to N. CA: Inyo; Mt. Pinchot, CA, SW % sec. 1, T 12S, R 33E, 1739 m, 4-17-87. 50. Goodale Creek. CA: Inyo: Mt. Pinchot, CA, SE 4 sec. 17, T 11S, R 34E, 1251 m, 4-18-87. 51. Taboose Creek. CA: Inyo; Big Pine, CA, SE % sec. 8, T 11S, R 34E, 1281 m, 4-18-87. 52. Tinnemaha Creek. CA: Inyo; Big Pine, CA, NW 's sec. 28. T 10s, R 34E, 1281 m, 4-18-87. 53. Springs N of Tinnemaha Creek and W of Poverty Hills. CA: Inyo; Big Pine. CA, NE '% sec. 30, T 10S, R 34E, 1403 m, 4-18-87. 54. Big Pine Creek. CA: Inyo: Big Pine, CA, SE % sec. 24, T 9S, R 33E, 1373 m, 4-18-87. 55. Baker Creek. CA: Inyo; Big Pine, CA, NE % sec. 13, T 9S, R 33E, 1312 m, 4-18-87. 56. Big Pine Spring. CA: Inyo: Big Pine, CA, NE 4 sec. 16, T 9S, R 33E, 1891 m, 4-18-87. 57. Spring on hill S of Warren Lake. CA: Inyo: Big Pine, CA NE 4 sec. 16, T 9S, R 33E, 1220 m. 58. Springs in canyon W of Warren Lake. CA: Inyo; Big Pine, CA, SW 4 sec. 2. T 9S, R 33E, 1251 m, 4-18- 87. 59. Springs in canyon S of Shannon Canyon. CA: Inyo; Big Pine, CA, SW 4 sec. 33, T 8S, R 33E, 1373 m. 60. Springs N of Klondike Lake. CA: Inyo: Big Pine, CA, SW ¥s sec. 23, T 8S, R 34E, 1208 m. 5-1-87. 61. Freeman Creek. CA: Inyo: Big Pine, CA, NE 4 sec. 20. T 8S, R 33E, 1434 m, 4-18-87. 62. Spring S of Rawson Creek. CA: Inyo; Bishop. CA, center of sec. 6, T 8S, R 33E, 1434 m, 4-18-87. 63. Spring in Chip- munk Canyon. CA: Inyo; Bishop, CA, SW 's sec. 28. T 7S, R 32E, 1708 m, 4-20-87. 64. Stream in Butter- milk Country. CA: Inyo; Mt. Tom, CA, NE 4 sec. 31, T 7S, R 31E, 2349 m, 5-1-87. 65. Stream in McGee Meadow. CA: Inyo: Mt. Tom, CA, NE 4 sec. 22, T 7S, R 31E, 1800 m, 4-24-87. 66. Spring in Deep Can- yon. Mt. Tom, CA, center of sec. 12, T 7S, R 31E, 1555 m, 4-29-87. 67. Horton Creek. CA: Inyo; Mt. Tom, CA, center of sec. 33, T 6S, R 31E, 1495 m, 4-28-87. 68. Springs N of Horton Creek. CA: Inyo; Mt. Tom, CA, SW ‘4 sec. 32, T 6S, R 31E, 1586 m, 4-28- 87. 69. Spring along N side of upper Pine Creek. CA: Inyo; Mt. Tom, CA, NE % sec. 26, T 6S, R 30E, 1830 m. 70. Springs entering Pine Creek in Birchim Canyon. CA: Inyo: Mt. Tom, CA, SE '% sec. 9, T 6S, R 31E, 1373 m. 71. Spring in Wells Meadow. CA: Inyo; Mt. Tom, CA, NW % sec. 2, T6S, R 31E, 1617 m, 4-24- 87. 72. Spring W of Sierra Paradise. CA: Mono; Mt. Tom, CA, NW '% sec. 25, T 5S, R 30E, 1769 m, 4-24- 87. 73. Stream in Swall Meadow. CA: Mono: Casa Diablo Mtn., CA, NW 1s sec. 14, T 5S, R 30E, 2196 m, 4-24-87. 74. Spring in Owens Gorge. CA: Inyo; Casa Diablo Mtn., CA, SW % sec. 31, T 4S, R 31E, 1830 m. 75. Fish Slough, “BLM Spring.” CA: Mono: Bishop, CA, SW \% sec. 30, T 5S, R 33E, 1251 m. 76. Fish Slough, ““Northwest Springs.*”* CA: Mono: White Mtn. Peak, CA, SE % sec. 13, T 5S, R 32E, 1281 m. 77. Fish 245 Slough, ““NE Spring.” CA: Mono; White Mtn. Peak, CA, NW '4 sec. 18, T 5S, R 33E, 1281 m. 78. Antelope Spring. CA: Mono; Casa Diablo Mtn., CA, SW 's sec. 9, T 4S, R 31E, 1830 m, 5-1-87. 79. Moran Spring. CA: Mono; Casa Diablo Mtn., CA, SW '%4 sec. 29, T 3S, R 31E, 2104 m, 5-1-87. 80. Banner Springs. CA: Mono: Casa Diablo Mtn., CA, SE % sec. 18, T 3S, R 31E, 2196 m, 5-1-87. 81. Spring by Tower Mine. CA: Mono: Casa Diablo Mtn., CA, SE % sec. 3, T 3S, R 31E, 1952 m, 4-21-87. 82. Springs entering Marble Creek. CA: Mono: White Mtn. Peak, CA, SE ' sec 28, T 2S, R 32E, 1525 m. 83. Marble Creek at HW 6. CA: Mono; White Mtn. Peak, CA, NE 4 sec. 28, T 2S, R 32E, 1525 m, 4-21-87. 84. Springs ca. 3.0 km S of Benton, W of HW 6. CA: Mono: Benton, NV-CA, SE Vy sec. 8, T 2S, R 32E, 1617 m, 4-21-87. 85. Benton Hot Springs. CA: Mono: Glass Mountain, CA-NV, SW Ys sec. 2, T 2S, R 31E, 1708 m, 4-21-87. 86. Springs at N end of Blind Spring Valley. CA: Mono; Glass Mountain, CA-NV, SW 14 sec. 36, T 1S, R 31E, 1708 m. 87. Springs at Bramlette Ranch. CA: Mono; Benton, NV-CA, SW ‘4 sec. 6 (springsnail positive), SE 4 sec. 6 (negative), T 1S, R 32E, 1678 m, 4-21-87. 88. Stream in Long John Canyon. CA: Inyo: New York Butte, CA, 14.4 km N-NE of SW corner of quadrangle, 1769 m, 5-4-87. 89. French Spring. CA: Inyo, New York Butte, CA, 8.8 km S of NW corner of quadrangle, 1617 m. 90. Spring in Willow Springs Canyon. CA: Inyo: In- dependence, CA, 6.5 km NW of SE comer of quad- rangle, 1861 m, 8-18-87. 91. Barrel Springs. CA: Inyo, Independence. CA, 13.6 km SW of NE corner of quad- rangle, 1952 m. 92. Spring ca. 1.6 km SE of Mule Spring. CA: Inyo; Waucoba Mtn., CA, 11.7 km N-NE of SW corner of quadrangle. 1586 m. 93. Mule Spring. CA: Inyo, Waucoba Mtn., CA, SE 4 sec. 1. T 10S, R 34E, 1312 m. 94. Spring at Graham Ranch. CA: Inyo, Waucoba Mtn., CA, NE % sec. 12. T9S, R 34E, 1373 m. 95. Ulymeyer Spring. CA: Inyo; Waucoba Min., CA, NE ' sec. 10, T 9S, R 34E, 1235 m, 4-19-87. 96. Wilkerson Springs. CA: Inyo, Waucoba Mtn., CA, NW Ys sec. 10. T 9S, R 34E, 1220 m. 97. Spring at Toll House. CA: Inyo, Waucoba Mtn., CA, NE 4 sec. 24, T 8S, R 34E, 1861 m. 98. Warm Springs. CA: Inyo, Bishop, CA, SW ‘4 sec. 8, T 8S, R 34E, 1220 m. 99. Spring S of Poleta Canyon. CA: Inyo; Bishop, CA, SE Vs sec. 18, T 7S, R 34E, 1373 m, 5-4-87. 100. Spring S of Silver Canyon. CA: Inyo; Bishop, CA, SE % sec. 26, T6S, R 33E, 1281 m, 4-26-87. 101. Stream in Silver Canyon. CA: Inyo; Bishop, CA, SE 4 sec. 24, T 6S, R 33E, 1434 m, 4-26-87. 102. Stream in Coldwater Can- yon. CA: Mono; Bishop, CA, SE "% sec. 26, T 5S, R 33E, 1494 m, 5-3-87. 103. Springs on bench S of Piute Creek. CA: Mono, Bishop, CA, SE % sec. 22, T 5S, R 33E, 1342 m. 104. Stream in canyon S of Piute Creek. CA: Mono, Bishop, CA, NE ¥% sec. 23, T 5S, R 33E, 1617 m. 105. Spring S of Millner Creek at Copper Queen Mine. CA: Mono; White Mtn. Peak, CA, NE Ys sec. 21, T 4S, R 33E, 1586 m, 4-28-87. 106. Spring 246 S of Lone Tree Creek at Hill Ranch. CA: Mono; White Mtn. Peak, CA, NE % sec. 5, T 4S, R 33E, 1617 m, 4-22-87. 107. Birch Creek. CA: Mono; White Mtn. Peak, CA, SE % sec. 7, T 3S, R 33E, 1617 m, 4-22- 87. 108. Orchard Spring. NV: Mineral; Benton, NV- CA, SW % sec. 35, T IN, R 32E, 2135 m, 5-10-87. 109. Spring in Queen Canyon. NV: Mineral; Benton, NV-CA, SE % sec. 25, T 1N, R 32E, 2166 m, 5-10- 87. 110. Stream in Queen Canyon (above spring). NV: Mineral; Benton, NV-CA, NE 4 sec. 36, T 1N, R 32E, 2288 m, 5-10-87. 111. Springs just downslope from Long Valley Dam. CA: Mono; Casa Diablo Mtn., CA, NW 4 sec. 20, T 4S, R 30E, 1922 m, 5-3-87. 112. Stream on W side of Little Round Valley. CA: Mono; Casa Diablo Mtn., CA, SE %4 sec. 36, T 4S, R 29E, 2105 m, 4-23-87. 113. McGee Creek. CA: Mono; Mt. Morrison, CA, 7.9 km NW of SE corner of quadrangle, 2501 m, 4-23-87. 114. Stream (W of Convict Creek) feeding Convict Lake. CA: Mono; Mt. Morrison, CA, SW \% sec. 22, T 4S, R 28E, 2562 m, 4-27-87. 115. Springs on S side of HW 395 W of Crowley Lake. CA: Mono; Mt. Morrison, CA, SW 4 secs. 1 (4-23-87) and 2 (4-29-87), T 4S, R 28E, 2172 m. 116. Spring E of Laurel Creek. CA: Mono; Mt. Morrison, CA, NE %4 sec. 9, T 4S, R 28E, 2196 m, 4-29-87. 117. Whitmore Hot Springs. CA: Mono; Mt. Morrison, CA, NE % sec. 6, T 4S, R 29E, 2105 m, 4-29-87. 118. Springs at Hot Creek Hatchery. CA: Mono; Mt. Morrison, CA, SW 4 sec. 35, T 3S, R 28E, 2166 m, 4-23-87. 119. Springs at Hot Creek Ranch. CA: Mono; Mt. Morrison, CA, SE %4 sec. 35, T 3S, R 28E, 2166 m, 4-23-87. 120. Casa Diablo Hot Springs (cool seeps). CA: Mono; Mt. Mor- rison, CA, NW % sec. 32, T 3S, R 28E, 2257 m, 4-23- 87. 121. Hot Creek. CA: Mono, Mt. Morrison, CA, NE % sec. 25, T 3S, R 28E, 2196 m. 122. Layton Springs (unnamed on topographic sheet). CA: Mono, Casa Diablo Mtn., CA, SE % sec. 36, T 3S, R 29E, 2074 m. 123. Springs feeding Little Alkali Lake. CA: Mono; Mt. Morrison, CA, SW 4 sec. 20, T 2S, R 29E, 2104 m, 4-29-87. 124. Little Hot Creek (source). CA: Mono; Mt. Morrison, CA, NW 4 sec. 13, T 3S, R 28E, 2074 m, 5-6-87. 125. Deadman Creek. CA: Mono; Mt. Morrison, CA, NE 4 sec. 27, T2S, R 27E, 2257 m, 4-29-87. 126. Big Springs. CA: Mono; Cowtrack Mtn.., CA, NE 4 sec. 25, T 2S, R 27E, 2166 m, 4-23-87. 127. Spring ca. 0.5 km E-NE of Arcularius Ranch. CA: Mono; Cowtrack Mtn., CA, SE %4 sec. 20, T 2S, R 28E, 2135 m, 5-6-87. 128. Springs along lower section of Mc- Laughlin Creek. CA: Mono; Cowtrack Mtn., CA, NE % sec. 15, T 2S, R 28E, 2318 m, 5-6-87. 129. Mc- Laughlin Spring. CA: Mono; Cowtrack Mtn., CA, NE Y, sec. 12, T 2S, R 28E, 2654 m, 5-6-87. 130. Springs at S end of Black Lake. CA: Mono; Glass Mountain, CA-NV, SW %4 sec. 4, T 2S, R 31E, 1922 m, 4-21-87. 131. Springs at N end of Black Lake. CA: Mono; Glass Mountain, CA-NV, SE %4 sec. 29, T 1S, R 31E, 1952 m, 4-21-87. 132. River Spring. CA: Mono, Glass Mountain, CA-NV, NE 4 sec. 24, T 1N, R 30E, 1983 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON m. 133. Stream in Crooked Meadows. CA: Mono; Cowtrack Mtn., CA, NW 4 sec. 36, T 1S, R 28E, 2654 m, 5-6-87. 134. Pilot Spring. CA: Mono; Cowtrack Mtn., CA, SE % sec. 27, T 1S, R 28E, 2623 m, 5-6- 87. 135. Baxter Spring. CA: Mono; Cowtrack Mtn., CA, SE % sec. 1, T 1S, R 28E, 2623 m, 5-6-87. 136. Gaspipe Spring. CA: Mono; Cowtrack Mtn., CA, NW ¥% sec. 1, T 1S, R 28E, 2440 m, 5-6-87. 137. Indian Spring. CA: Mono; Cowtrack Mtn., CA, 13.4 km SE of NW corner of quadrangle, 2288 m, 5-6-87. 138. Simons Spring (and others in large marshy area). CA: Mono; Cowtrack Mtn., CA, 6.9 km SE of NW corner of quadrangle, 1968 m, 5-5-87. 139. Willow Spring (not shown on topographic sheet). CA: Mono; Cow- track Mtn., CA, NE % sec. 15, T IN, R 27E, 1952 m, 5-5-87. 140. Spring along Lee Vining Creek. CA: Mono; Mono Craters, CA, NW 4 sec. 19, T IN, R 26E, 2227 m, 5-5-87. 141. Springs feeding lower section of Lee Vining Creek. CA: Mono; Mono Craters, CA, NW 4 sec. 9, T IN, R 26E, 2000 m, 5-5-87. 142. Springs along HW 395 ca. 5.0 km NW of Lee Vining. CA: Mono; Mono Craters, CA, NE 4 sec. 31, T 2N, R 26E, 1950-2075 m, 5-6-87. 143. Lower Dechambeau Creek and associated springs. CA: Mono; Bodie, CA, SE %4 sec. 19, T 2N, R 26E, 1922 m, 5-6-87. 144. Spring ca. 2.0 km S of Dechambeau Creek along HW 395. CA: Mono; Bodie, CA, SE % sec. 30, T 2N, R 26E, 1922 m, 5-6-87. 145. Mill Creek. CA: Mono; Bodie, CA, NW 4% sec. 15, T 2N, R 25E, 2379 m, 5-6-87. 146. Stream N of Mill Creek. CA: Mono; Bodie, CA, SE sec. 1, T 2N, R 25E, 2105 m, 5-6-87. 147. Stream in Rattlesnake Canyon. CA: Mono; Bodie, CA, NW 4 sec. 30, T 3N, R 26E, 2288 m, 5-6-87. 148. Murphy Spring. CA: Mono; Bodie, CA, SE % sec. 24, T 4N, R 26E, 2501 m, 5-6-87. 149. Stream S of Murphy Spring. CA: Mono; Bodie, CA, NE 4 sec. 25, T 4N, R 26E, 2410 m, 5-6-87. 150. Stream in Cottonwood Canyon. CA: Mono; Bodie, CA, SE % sec. 32, T 4N, R 27E, 2227 m, 5-6-87. 151. Sulphur Pond and pool to E. CA: Mono; Trench Canyon, CA-NV, SE 4 sec. 26, T 3N, R 27E, 1952 m, 5-6-87. 152. Saline Marsh. CA: Inyo; New York Butte, CA, center of sec. 27, T 14S, R 28E, 335 m. 153. Stream in Hunter Canyon. CA: Inyo; New York Butte, CA, 14.5 km SE of NW corner of quad- rangle, 549 m, 3-28-87. 154. Stream in Beveridge Can- yon. CA: Inyo; New York Butte, CA, 12.3 km E-SE of NW corner of quadrangle, 580 m, 3-28-87. 155. Bad- water Spring. CA: Inyo; Waucoba Wash, CA, 10.0 km NE of SW corner of quadrangle, 488 m, 3-28-87. 156. Springs S of Lower Warm Springs. CA: Inyo; Waucoba Wash, CA, NE % sec. 30, T 13S, R 39E, 381 m, 3-29- 87. 157. Springs NW of Upper Warm Springs. CA: Inyo; Waucoba Wash, CA, SE 4 sec. 5, T 13S, R 39E, 549 m, 3-29-87. 158. Upper Warm Spring. CA: Inyo; Dry Mountain, CA, NE 4 sec. 9, T 13S, R 39E, 488 m, 2-11-85. 159. Willow Creek. CA: Inyo; Waucoba Wash, CA, 12.3 km N-NE of SW corner of quadrangle, 915 m, 3-28-87. 160. Corral Springs. CA: Inyo; Blanco VOLUME 102, NUMBER 1 Mtn., CA, SW % sec. 3, T 8S, R 36E, 1525 m. 161. Bog Mounds Springs. CA: Inyo; Blanco Mtn., CA, SW Ys sec. 32, T 7S, R 36E, 1508 m, 4-26-87. 162. Antelope Spring. CA: Inyo; Blanco Mountain, CA, NW % sec. 24, T 7S, R 35E, 1708 m. 163. Samms Spring. CA: Inyo; Blanco Mountain, CA, SW 4 sec. 13, T 78, R 35E, 1739 m, 3-29-87. 164. Willow Spring. CA: Inyo; Magruder Mtn., NV-CA, 10.0 km N-NE of SW corner of quadrangle, 1739 m, 3-30-87. 165. Wheelbarrow Spring (not shown on topographic sheet). CA: Inyo; Soldier Pass, CA-NV, NE '4 sec. 5, T 7S, R 37E, 1708 m, 3-30-87. 166. Wyman Creek. CA: Inyo; Soldier Pass, CA-NV, SW 4 sec. 23, T 6S, R 36E, 1769 m, 3-29-87. 167. Stream in Indian Joe Canyon. CA: Inyo; Trona, CA, NW 4 sec. 24, T 24S, R 42E, 732 m, 4-13- 87. 168. Allen Spring (not shown on topographic sheet). CA: Inyo; Trona, CA, NE 4 sec. 24, T 24S, R 42E, 854 m, 4-13-87. 169. Stream in Great Falls Basin. CA: Inyo; Trona, CA, SW 4 sec. 12, T 24S, R 42E, 854 m, 4-13-87. 170. Stream in Canyon N of Great Falls Basin. CA: Inyo; Trona, CA, NW 4 sec 7, T 24S, R 43E, 915 m, 3-25-87. 171. Stream in S fork Home- wood Canyon. CA: Inyo; Trona, CA, NW 4 sec 2, T 24S, R 42E, 1159 m, 3-25-87. 172. Benko Spring. CA: Inyo; Trona, CA, NE 4 sec. 34, T 23S, R 42E, 1037 m, 3-25-87. 173. Stream in N fork Homewood Can- yon. CA: Inyo; Trona, CA, SW \4 sec. 25, T 23S, R 42E, 1098 m, 3-25-87. 174. Bircham Springs. CA: Inyo; Trona, CA, NE 4 sec. 20, T 23S, R 42E, 1708 m, 3- 4-85. 175. Wild Rose Spring. CA: Inyo; Mountain Springs Canyon, CA, SW 4 sec. 11, T 23S, R 41E, 1525 m, 3-4-85. 176. LaMotte Spring. CA: Inyo; Trona, CA, NE % sec. 31, T 22S, R 42E, 1525 m, 3-4-85. 177. Stream in N fork Water Canyon. CA: Inyo; Trona, CA, NE 4 sec. 36, T 22S, R 42E, 1098 m, 4-11-87. 178. Tennessee Spring. CA: Inyo; Coso Peak, CA, SW 4 sec. 13, T 21S, R 41E, 1830 m. 179. Haiwee Spring. CA: Inyo; Haiwee Reservoir, CA, SW 4 sec. 10, T 21S, R 39E, 1403 m, 3-5-85. 180. Stream in Knight Canyon. CA: Inyo; Maturango Peak, CA, SE 4 sec. 14, T 21S, R 42E, 1037 m. 181. Stream in Revenue Canyon. CA: Inyo; Maturango Peak, CA, NW '% sec. 3, T 21S, R 42E, 976 m, 4-14-87. 182. Stream in Snow Canyon. CA: Inyo; Maturango Peak, CA, 5.1 km S-SE of NW corner of quadrangle, 1342 m. 183. Black Spring. CA: Inyo; Coso Peak, CA, 1.6 km E of NW corner of quad- rangle, 1769 m, 3-31-87. 184. Darwin Wash. CA: Inyo; Darwin, CA, China Garden Spring, NE % sec. 4, T 19S, R 41E, 1037 m; spring above Darwin Falls, NW % sec. 3, T 19S, R 41E, 854 m; stream below falls, SW Ys sec. 34, T 18S, R 41E, 732 m. 185. Stream in Grape- vine Canyon. CA: Inyo; Ubehebe Peak, CA, 8.4 km NW of SE corner of quadrangle, 1525 m, 3-28-87. 186. Big Dodd Spring. CA: Inyo; Ubehebe Peak, CA, 11.5 km NW of SE corner of quadrangle, 1159 m, 3-12-87. 187. Stream in Goler Canyon. CA: Inyo; Manley Peak, CA, 15.3 km NE of SW corner of quadrangle, 549 m, 3-31-87. 188. Anvil Spring. CA: Inyo; Manley Peak, 247 CA, 11.3 km SW of NE corner of quadrangle, 1373 m, 2-18-85. 189. Seepage on SW side of Panamint Lake bed. CA: Inyo; Manley Peak, CA, E sides of secs. 28 and 34, T 22S, R 44E, 317 m, 3-31-87. 190. Stream in Pleasant Canyon. CA: Inyo; Telescope Peak, CA, 6.9 km NE of SW corner of quadrangle, 793 m. 191. Post Office Spring. CA: Inyo; Telescope Peak, CA, NE 4 sec. 9, T 22S, R 44E, 317 m, 2-14-85. 192. Stream in Happy Canyon. CA: Inyo; Telescope Peak, CA, 11.3 km NE of SW corner of quadrangle, 1098 m, 4-11-87. 193. Spring mounds on Panamint Lake bed NW of Ballarat. CA: Inyo; Maturango Peak, CA, NW ' sec. 20, T 21S, R 44E, 323 m, 4-14-87. 194. Stream in Surprise Canyon. CA: Inyo; Telescope Peak, CA, 15.3 km NE of SW corner of quadrangle, 1098 m. 195. Warm Sulphur Springs. CA: Inyo; Telescope Peak, CA, SE 4 sec. 10, T 21S, R 44E, 305 m, 2-13-85. 196. Stream in Jail Canyon. CA: Inyo; Telescope Peak, CA, 10.0 km SE of NW corner of quadrangle, 1220 m. 197. Stream in Tuber Canyon. CA: Inyo; Telescope Peak, CA, 5.6 km SE of NW corner of quadrangle, 1098 m, 4-11-87. 198. Wildrose Spring. CA: Inyo; Emigrant Canyon, CA, 3.8 km NE of SW corner of quadrangle, 1080 m, 2-15-85. 199. Springs in upper Wildrose Can- yon. CA: Inyo; Emigrant Canyon, CA, 5.3 km NE of SW corner of quadrangle, 1220 m, 2-15-85. 200. Cave Spring. CA: San Bernardino; Avawatz Pass, CA, 7.7 km NE of SW corner of quadrangle, 1129 m, 4-9-87. 201. Sheep Creek Spring. CA: San Bernardino; Ava- watz Pass, CA, 3.8 km NW of SE corner of quadrangle, 427 m, 4-10-87. 202. Salt Creek E of HW 127. CA: San Bernardino; Avawatz Pass, CA, 14.1 km S-SW of NE corner of quadrangle, 92 m, 3-15-87. 203. Owl Hole Springs. CA: San Bernardino; Leach Lake, CA, NW 1% sec. 22, T 19N, R 3E, 641 m, 3-16-85. 204. Saratoga Spring. CA: San Bernardino; Avawatz Pass, CA, NW 4sec. 2, T 18N, R 5E, 61 m. 205. Ibex Spring. CA: San Bernardino; Shoshone, CA, 8.5 km E-NE of SW corner of quadrangle, 366 m, 3-22-87. 206. Horse Thief Springs. CA: San Bernardino; Horse Thief Springs, CA-NV, 10.4 km E-NE of SW corner of quadrangle, 1403 m, 4-10-87. 207. Willow Spring. CA: Inyo; Te- copa, CA, SW 4 sec. 25, T 20N, R 7E, 427 m, 3-22- 87. 208. Springs in Amargosa Gorge, S of Tecopa. CA: Inyo; Tecopa, CA, NW '% sec. 15, T 20N, R 7E, 397 m. 209. Spring in marsh E of Grimshaw Lake. CA: Inyo; Tecopa, CA, NE 4 sec. 9, T 20N, R 7E, 427 m. 210. Northernmost of Tecopa Hot Springs. CA: Inyo; Tecopa, CA, NW 4 sec. 33, T 21N, R 7E, 397 m. 211. Shoshone Spring. CA: Inyo; Shoshone, CA, NW 4 sec. 30, T 22 N, R 7E, 519 m. 212. Resting Spring. CA: Inyo; Tecopa, CA, SE % sec. 31, T 21N, R 8E, 549 m. 213. Lost Spring (unnamed on quadrangle). CA: Inyo; Wingate Wash, CA, 12.8 km SE of NW corner of quad- rangle, 702 m, 3-10-87. 214. Salsberry Spring. CA: Inyo; Shoshone, CA, 10.6 km SW of NE corner of quadrangle, 366 m, 3-14-85. 215. Warm Spring. CA: Inyo; Wingate Wash, CA, 7.2 km SE of NW corner of 248 quadrangle, 732 m, 2-18-85. 216. Lower Talc Mine Spring. CA: Inyo; Bennetts Well, CA, 6.4 km E-NE of SW corner of quadrangle, 915 m, 3-10-87. 217. Willow Spring. CA: Inyo; Funeral Peak, CA, 7.8 km NE of SW corner of quadrangle, 732 m, 3-20-87. 218. Hidden Spring. CA: Inyo; Funeral Peak, CA, 15.3 km NE of SW corner of quadrangle, 1342 m, 3-17-87. 219. Springs at Mormon Point. CA: Inyo; Bennetts Well, CA, 6.7 km N-NW of SE corner of quadrangle, —64 m, 3-9- 85. 220. Spring (lower) in Johnson Canyon. CA: Inyo; Telescope Peak, CA, SW 4 sec. 22, T 21S, R 46E, 1190 m. 221. Eagle Borax Spring. CA: Inyo; Bennetts Well, CA, 13.3 km SE of NW corner of quadrangle, —79 m, 2-16-85. 222. Hanaupah Spring. CA: Inyo; Telescope Peak, CA, 7.6 km S-SW of NE corner of quadrangle, 1281 m. 223. Badwater Spring. CA: Inyo; Bennetts Well, CA, 2.7 km SW on NE corner of quadrangle, —79 m, 2-16-85. 224. Tule Spring. CA: Inyo; Bennetts Well, CA, 10.8 km E-SE of NW corner of quadrangle, —79 m, 2-28-85. 225. Grapevine Springs. NV: Nye; Ash Meadows, NV-CA, NE 4 sec. 2, T 19S, R SOE, 732 m, 3-14-85. 226. Blackwater Spring. CA: Inyo; Emigrant Canyon, CA, 12.9 km S-SW of NE corner of quadrangle, 946 m, 3-10-87. 227. Navel Spring. CA: Inyo; Ryan, CA-NV, NW 4 sec. 13, T 26N, R 2E, 640 m, 3-17-87. 228. Travertine Springs. CA: Inyo; Fur- nace Creek, CA, NW ‘4 sec. 25, T 27N, R 1E, 122 m. 229. Salt Springs, NW of Cow Creek. CA: Inyo; Chlo- ride Cliff, CA-NV, SW % sec. 21, T 28N, R 1E, —79 m, 2-3-85. 230. Nevares Springs. CA: Inyo; Chloride Cliff CA-NV, NE 4 sec. 36, T 28N, R 1E, 275 m. 231. Cottonball Marsh. CA: Inyo; Chloride Cliff, CA-NV, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 2.8 km NE of SW corner of quadrangle, —79 m. 232. Salt Springs, W of Cottonball Marsh. CA: Inyo; Chlo- ride Cliff, CA-NV, 1.0 km NE of SW corner cf quad- rangle, —73 m, 2-22-85. 233. Salt Springs S of Cow Creek. CA: Inyo; Furnace Creek, CA, SE % sec. 3, T 27N, R 1E, 31 m, 2-5-85. 234. Stream in Cottonwood Canyon. CA: Inyo; Marble Canyon, CA, stream 10.0 km NW of SE corner of quadrangle, 732 m, 2-15-85, stream 11.2 km E-NE of SW corner of quadrangle, 1037 m, 3-12-87. 235. McLean Spring (Salt Creek). CA: Inyo; Stovepipe Wells, CA, SW 4 sec. 31, T 15S, R 46E, 37 m, 3-8-85. 236. Springs NW of Keane Won- der Mine. CA: Inyo; Chloride Cliff, CA-NV, SE % sec. 1,T 15S, R 46E, 366 m, 2-13-85. 237. Monarch Spring. CA: Inyo; Chloride Cliff, CA-NV, SE 4 sec. 24, T 14S, R 46E, 915 m, 2-4-85. 238. Keane Spring. CA: Inyo; Chloride Cliff, CA-NV, NW ‘4 sec. 8, T 30W, R 1E, 1159 m, 2-4-85. 239. Cane Spring. NV: Nye; Cane Spring, NV, 6.0 km N-NE of SW corner of quadrangle, 1238 m. 240. Spring in Oasis Valley, 13.2 km N of Beatty. NV: Nye County; Thirsty Canyon, NV, SE 4 sec. 32, T 10S, R 47E, 1128 m. 241. Grapevine Springs. CA: Inyo; Ubehebe Crater, CA-NV, NE % sec. 3, T 11S, R 42E, 824 m. 242. Spring 1.6 km E of Scotty’s Castle. CA: Inyo; Ubehebe Crater, CA-NV, NW 4 sec 5, T 11S, R 42E, 946 m. 243. Little Sand Spring. CA: Inyo; Last Chance Range, CA-NV, SE % sec. 17, T 9S, R 41E, 915 m, 387. 244. Sand Spring. CA: Inyo; Last Chance Range, CA-NV, SE 4 sec. 7, T 9S, R 41E, 946 m, 3-30-87. 245. Last Chance Spring. CA: Inyo; Ma- gruder Mtn., NV-CA, SE % sec. 2, T 8S, R 39E, 1739 m, 3-30-87. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 249-263 FOUR NEW SPECIES OF FREE-LIVING MARINE NEMATODES IN THE GENUS PAREURYSTOMINA (NEMATODA: ENOPLIDA) WITH OBSERVATIONS ON OTHER MEMBERS OF THE GENUS Edwin J. Keppner Abstract.—Four new species of Pareurystomina and the male of P. flagelli- caudata are described for the first time from sediments in St. Andrew Bay and the Gulf of Mexico, Bay County, Florida, U.S.A. Additional information is provided for P. bissonettei, P. floridensis, and P. acuminata. P. americana n. sp. and P. vaughtae n. sp. differ from one another in the shape of the spicules and gubernaculum, and from P. atypica in the location of the excretory pore and shape of the spicules and gubernaculum. P. parafloridensis n. sp. differs from P. floridensis in the number of circles of denticles in the stoma and in the size and arrangement of the denticles. P. alima n. sp. differs from P. parafloridensis n. sp. in the number of circles of denticles in the stoma, in the absence of a gubernaculum, and in the shape of the spicules. It differs from P. agubernacula in the number of circles of denticles in the stoma and the length and shape of the spicules. The genus Megeurystomina is placed in synonymy with Pareurystomina, and M. combesi becomes P. combesi n. comb. A key to the species of the genus Pareurystomina is given. The genus Pareurystomina Micoletzky & Kreis, 1930, was erected for those species of free-living marine nematodes of the subfamily Eurystomininae Filipjev, 1921, in which the spinneret and caudal glands are absent, and the terminus of the tail is acute. Wieser (1959) described Pareurys- tomina pugetensis, described the cervical setae as flattened in this species, and re- viewed the known species in the genus. He recognized as valid only those species for which males had been described. He ex- pressed doubt as to the inclusion of Pareu- rystomina tenuicauda Stekhoven, 1950, in the genus because circles of denticles are absent from the stoma in this species where- as they are present in all other species in the genus. Luc & De Coninck (1959) described Pareurystomina armorica and provided a key to six species of the genus. Chitwood (1960) described Pareurystom- ina atypica and provided a key to the nine species then in the genus and included P. tenuicauda. The key used a number of char- acters to differentiate the species including the number of circles of denticles in the sto- ma, tail length, length of spicules, and pres- ence or absence of flattened cervical setae. He also recognized the problem of the ab- sence of male descriptions for some species. Hopper (1963) discussed the presence of large hypodermal gland cells in Pareurys- tomina. Hopper (1970) described Pareurys- tomina bissonettei, discussed the presence of flattened cervical setae, the arrangement of the denticles in the stoma in Pareurys- tomina, and emended the description of P. atypica to include flattened cervical setae. Lambshead & Platt (1979) described a new genus Batheurystomina, provided a tabular key to the genera of the Eurystomininae, and discussed each genus in the subfamily. They considered male specimens to be crit- ical to an understanding of the Eurystomi- 250 ninae. They considered Eurystomina re- panda Wieser, 1959, to be a synonym of P. pugetensis based on the presence of flat- tened cervical setae and similarity of the male genital apparatus. They considered all species of Pareurystomina for which males are unknown as species dubiae, and P. ten- uicauda was considered species dubia due to the absence of information pertaining to the stoma. Collections of free-living marine nema- todes from various habitats in St. Andrew Bay, and the Gulf of Mexico, Bay County, Florida, U.S.A. from 1981-1987 yielded 174 specimens of nine species in the genus Par- eurystomina. The purpose of this paper is to describe the species collected, provide some additional information for known species and present a key to the species of the genus Pareurystomina. Specimens were recovered from sediment from a number of subtidal sites in the above- mentioned waterbodies with core samplers of variable diameters. Nematodes were ex- tracted from the samples by repeated wash- ing of the sediment in water from the site. Nematodes were removed alive from the settled material of the final washing, fixed in hot alcohol-formalin-acetic acid or hot 4% formalin in sea water for 24 h and de- hydrated and mounted in anhydrous glyc- erine on Cobb slides. All measurements are given in um unless otherwise stated, and the mean is followed by the range in parentheses. The spicular lengths are given as the chord of the arc unless otherwise indicated. The taxonomic hierarchy is from Gerlach & Riemann (1974). Type specimens and specimens of known species have been deposited in the U.S. National Museum of Natural History (USNM) and the Florida Nematode Col- lection, University of Florida, Gainesville (FNC). Taxonomic Account The specimens of Pareurystomina col- lected during this study presented a variety PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON of spicular and gubernacular shapes and sizes, a variable number of circles of den- ticles in the stoma, and a variety of denticu- lar shapes and arrangements. Particular em- phasis was given to placing males collected during this study with previously described species in which the males are unknown. The characters used to place males with fe- males were the number of circles of stomatal denticles, shape and size of the denticles in each circle, tail length, size of amphid, and location of the excretory pore. Comparison of males with males of recognized species included the above characters as well as the shape of the male genital apparatus. All specimens examined during this study have the following features in common (Figs. 1-3). Body size and shape is variable within a species as evidenced by the wide range of lengths and wide range of the demanian “a” values in some species. The cuticle is thin and smooth, and the terminus of the tail is acute. Caudal glands and spinneret were not observed. Hypodermal gland cells are pres- ent and arranged as described by Hopper (1963, 1970). The gland cells are more prominent and abundant in some species than in others. The head is retracted in some specimens which gives the appearance of an anterior displacement of the amphid and cephalic setae. The head has six small lips each with a papilla, and a single circle of 10 (6 + 4) cephalic setae. Four of the subme- dian cephalic setae are shorter than the oth- er six cephalic setae. The lip region is de- lineated from the remainder of the head by a cephalic groove. The amphid is large, wid- er than long, and located over the stoma. Stoma is large with heavily cuticularized walls and is divided into an anterior and posterior chamber by a stomatal suture at about midlevel. The stoma has a single, large, right subventral tooth and a variable number of circles of denticles. The circles of denticles can be complete or interrupted on the right subventral wall of the stoma as described by Hopper (1970). The excretory pore is anterior to the level of the cephalic VOLUME 102, NUMBER 1 setae. Cervical setae are compressed and ap- pear flattened with a broad base and ter- minus. The width and length of these setae vary somewhat among species. The female reproductive system is amphidelphic and the ovaries are antidromous. Males have two spicules, and two cuticularized, cup- shaped, pre-anal supplements. Two excep- tions to these statements were observed during this study; a single male of P. flori- densis with only one pre-anal supplement and a male of P. floridensis in which the gubernaculum was absent. Gerlach (1952) described a male of Pareurystomina acu- minata (De Man, 1889) with a single pre- anal supplement. A gubernaculum is absent or reduced in some species of Pareurysto- mina. The characters of most value in differ- entiating the species of Pareurystomina are the shape and size of the spicules and the presence or absence and shape of the gu- bernaculum. The number of circles of den- ticles in the stoma, the shape of the denticles in each circle, tail length and position of the excretory pore were also of value in differ- entiating both males and females of the var- ious species. The use of the number of cir- cles of denticles in the stoma can be a problem because the posterior circles are often incomplete. Hopper (1970), in the de- scription of P. bissonettei, noted that the fewest rows of denticles occur on the wall of the stoma from which the large subven- tral tooth originates, and the largest number of rows of denticles occurs on the stomatal wall opposite the origin of the subventral tooth. The presence of partial circles of den- ticles and the location of the interruption requires examination from lateral aspects in order to determine accurately the maxi- mum number of denticular circles in the stoma. Some descriptions of Pareurysto- mina species are not clear as to whether the maximum or minimum number of denticu- lar circles is stated. It is assumed, for pur- poses of this paper, that the stated or figured number of circles of denticles for each pre- 251 Figs. 1-3. Pareurystomina floridensis: 1, Male, head, lateral view; 2, Entire male, lateral view; 3, Male, an- terior pre-anal supplement, lateral view. Scale bars in um. Legend: a = amphid. aa = anterior apophysis. cg = cervical groove. cs = cephalic setae. d = denticles. ep = excretory pore. es = esophagus. fs = flat cervical setae. ga = gubernacular apophysis. hg = hypodermal gland cell. in = intestine. lp = labial papilla. nr = nerve ring. p = papilla. pa = posterior apophysis. ps = pre- anal supplement. r = mm of cup. s = spicule. ss = stomatal suture. st = subventral tooth. t = testis. viously described species is the maximum number. Wieser (1959) recognized that the size and shape of the denticles can vary between cir- cles in Pareurystomina and used these dif- ferences with other characters to distinguish the species. In the specimens examined dur- ing this study, the size and shape of the denticles varied between circles in some species but were of the same size and shape within a given circle in the same species. Pareurystomina americana, new species Figs. 4-12 Diagnosis. —(Ten males, 3 females and 5 juveniles from St. Andrew Bay.) Body long, slender. Four submedian cephalic setae 252 Figs. 4-12. Pareurystomina americana: 4, Male paratype, head, lateral view; 5, Male holotype, head, lateral view; 6, Male paratype, head, lateral view; 7, Male holotype, posterior end, lateral view; 8, Male holotype, pre-anal supplements, lateral view (anterior, left; posterior, right); 9, Male holotype, right spicule and gubernaculum, lateral view; 10, Male paratype, right spicule and gubernaculum, lateral view; 11, Male paratype, pre-anal supplements, lateral view (anterior, left; posterior, right); 12, Female, posterior end, lateral view. Scale bars in um. about 4 length of other 6. Flat cervical setae with narrow base present from base of sto- ma to about 2 distance to nerve ring; one male with additional setae for about '2 dis- tance from nerve ring to base of esophagus. Somatic setae not observed; caudal setae sparse in male, not observed in female. Am- phids over midlevel of stoma. Single com- plete circle triangular denticles and one in- complete circle small, round denticles anterior to stomatal suture; single incom- plete circle large, triangular denticles pos- terior to suture. Excretory pore anterior to cephalic setae. Tail conical with acute ter- minus. Males (n = 6): Length 4.52 mm (4.24— PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 4.94), width at midbody 35.8 (30-43). Head diameter 27 (25-29) at level of cephalic se- tae; cephalic setae 15 (14-17) and 5.3 (5-6) long. Amphid 13.7 (13-16) wide. Stoma 24.2 (23-26) long, 17.5 (16-19) wide. Esophagus 0.964 mm (0.730-1.10) long; nerve ring 188.2 (179-195) from anterior end. Tail 140.2 (138-163) long, 34.2 (32-37) wide at anus. Two midventral, cuticularized, cup- shaped, pre-anal supplements present 119 (107-136) and 228 (208-248) anterior to anus. Posterior apophysis of each supple- ment larger than anterior; rim of cup striat- ed. Two pairs subventral papillae between anus and first pre-anal supplement; two pairs subventral papillae between first and second pre-anal supplements. Two pairs subventral setae immediately anterior to anus; subven- tral, lateral, subdorsal setae present poste- rior to anus. Spicules gently curved 41.8 (37-45) long; tips blunt, barb absent. Gu- bernaculum with narrow corpus surround- ing spicules; gubernacular apophysis 14.7 (14-16) long, bent dorsally at midpoint. a = 125.9 (114.9-147.8); b = 4.77 (3.96-6.03); c = 30.8 (27.0-33.6). Females (n = 3): Length 4.19 mm (3.36- 4.65), width at midbody 42.3 (42-45). Head diameter 28.7 (28-30) at level of cephalic setae; cephalic setae 15 (14-17) and 5.3 (5- 6) long. Amphid 12.3 (11-13) wide. Stoma 24 (22-26) long and 18.7 (18-19) wide. Esophagus 848 (789-896) long, nerve ring 182.3 (171-200) from anterior end. Tail 186.7 (165-203) long, 33.7 (32-35) wide at anus. Vulva 2.76 mm (2.15-—3.11) from an- terior end. a = 98.7 (84.0-110.7); b = 4.92 (4.26—-5.31); c = 23.7 (17.5—31.2); V = 65.7% (64-68). Type specimens. — Holotype male, USNM 77137; paratype males, USNM 77138- 77140; allotype female, USNM 77141; paratype female, USNM 77142. Paratype males, FNC A-144 and A-146. Type locality. —Holotype male from non- vegetated sediment from the north shore of St. Andrew Bay, Bay County, Florida 0.3 km west of the inlet to Lake Caroline VOLUME 102, NUMBER 1 (85°41'10”W, 30°09’45’”N). Also in vegetat- ed and nonvegetated sediment from Fresh- water Bayou, St. Andrew Bay, Bay County, Florida, (85°39'00”W, 30°07'30’N). Etymology. —Named for the place of col- lection, America. Remarks. —Pareurystomina americana 1s most similar to Pareurystomina atypica Chitwood, 1960, from which it differs in the location of the excretory pore (anterior to cephalic setae vs. 104 from anterior end), in the width of the amphid (11-16 vs. 7), in the shape of the spicules (blunt tip vs. narrow, pointed tip) and in the shape of the gubernacular apophysis (bent dorsally vs. bent ventrally). P. americana is also similar to P. vaughtae described next but differs from P. vaughtae in the shape of the spicules (absent of barb at tip), the corpus of the gubernaculum is not conical and the gu- bernacular apophysis is bent dorsally rather than straight. Pareurystomina vaughtae, new species Figs. 13-20 Diagnosis. —(Five males, 3 females, and 3 juveniles from mouth of Freshwater Bay- ou and Grand Lagoon, St. Andrew Bay.) Body long, slender. Four submedian ce- phalic setae about 28% length of other 6. Flat cervical setae narrow; present from base of stoma almost to nerve ring. Somatic setae sparse; caudal setae abundant in males, sparse in females. Amphids over midlevel of stoma. Single complete circle large tri- angular denticles anterior to stomatal su- ture, single incomplete circle large, trian- gular denticles posterior to suture. Excretory pore anterior to cephalic setae. Tail conical with acute terminus. Males (n = 5): Length 3.24 mm (2.63- 4.70), width at midbody 33.8 (30-37). Head diameter 26.6 (26-29) at level of cephalic setae; cephalic setae 18.1 (16-20) and 4.8 (4—5) long. Amphid 11.4 (11-12) wide. Sto- ma 24.6 (24-27) long, 17.2 (16-18) wide. Esophagus 713.2 (606—936) long; nerve ring 179 (168-200) from anterior end. Tail 138 253 Figs. 13-20. Pareurystomina vaughtae: 13, Male holotype, head, ventral view; 14, Male paratype, head, lateral view; 15, Male holotype, posterior end, lateral view; 16, Male, anterior pre-anal supplement, lateral view; 17, Male holotype, left spicule and gubernacu- lum, lateral view; 18, Male holotype, anterior pre-anal supplement, lateral view; 19, Male paratype, left spic- ule and gubernaculum, lateral view; 20, Female, tail, lateral view. Scale bars in um. (126-144) long, 31.6 (29-35) wide at anus. Two cuticularized, cup-shaped, midventral, pre-anal supplements present 118.8 (114—- 136) and 200.4 (184-216) anterior to anus. Posterior apophysis of each supplement larger than the anterior; rim of cup not striated. Two pairs subventral papillae be- tween anus and first pre-anal supplement. Two pairs subventral setae immediately an- terior to anus. Spicules 41.8 (38-45) long, gently curved, tip with small barb. Corpus of gubernaculum 7.2 (6-8) long, conical, surrounds distal end of spicules; gubernacu- lar apophysis straight, 11 (8-13) long, di- rected dorsally. Post-anal setae abundant. a = 95.0 (80.0—127.0); b = 4.50 (3.95-5.02); c = 23.4 (18.7-32.6). 254 Females (n = 3): Length 3.32 mm (3.07— 3.54), width at midbody 45.3 (43-48). Head diameter 28.3 (27-29) at level of cephalic setae; cephalic setae 19.3 (18-21), 4.7 (4-5) long. Amphid 11.7 (1 1-13) wide. Stoma 23.3 (22-24) long, 19 (18-20) wide. Tail 166.3 (163-168) long, 34.7 (32-37) wide at anus. Vulva 2.05 mm (1.91—2.16) from anterior end. a = 73.4 (63.9-78.7); b = 3.83 (3.69- 4.02); c = 19.9 (18.8-21.1); V = 61.7% (61- 62). Type specimens. — Holotype male, USNM 77143; paratype males, USNM 77144—- 77145; allotype female, USNM 77146. Paratype male, FNC A-155; paratype fe- male, FNC A-156. Locality. —Holotype from sediments in a bed of Shoalgrass (Halodule wrightii) at the mouth of Freshwater Bayou, St. Andrew Bay, Bay County, Florida (85°39'00’W, 30°07'30’”N). Other site, Grand Lagoon off St. Andrew Bay, Bay County, Florida (85°43'15”W, 30°07'50’N). Etymology. —Named for Ms. Rosalie Vaught, librarian. This and other studies could not have been completed without her voluntary dedication to obtaining the re- quired literature. Remarks.—Pareurystomina vaughtae is most similar to P. americana but differs from it in the presence of the large cone-shaped corpus of the gubernaculum, straight rather than bent gubernacular apophysis, and the presence of two rather than three circles of denticles in the stoma. P. vaughtae is also similar to P. armorica in the presence of two circles of denticles in the stoma. It dif- fers from that species in that the excretory pore is anterior to the cephalic setae rather than at the cephalic groove, the amphid is larger (50% of head diameter vs. 31% of head diameter), and the tail is shorter (4.8 anal diameters vs. 6 anal diameters). Pareurystomina parafloridensis, new species Figs. 21-28 Diagnosis. —(Eleven males, 4 females and 6 juveniles from various sites in St. Andrew PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Bay). Body long, broad. Four submedian cephalic setae about '4 length of other 6. Flat cervical setae broad; present from base of stoma almost to nerve ring. Somatic setae and caudal setae sparse. Amphids over mid- level of stoma. Stoma with 4 circles of den- ticles anterior to stomatal suture, one circle posterior to suture. Last circle anterior to suture and circle posterior to suture incom- plete. Small triangular denticles in anterior- most 4 circles uniform in size within each circle and between circles. Posterior-most circle with larger triangular denticles. Ex- cretory pore anterior to cephalic setae. Male tail, short, conical with acute terminus. Fe- male tail longer, conical then narrow to acute terminus. Males (n = 6): Length 4.59 mm (3.95— 5.10), width at midbody 70 (61-75). Head diameter 37.3 (37-38) at level of cephalic setae; cephalic setae 16.3 (15-18) and 5 (4— 6) long. Amphid 20.3 (19-21) wide. Stoma 30.2 (29-32) long, 24.6 (24-26) wide. Esophagus 1.02 mm (0.971-1.08) long; nerve ring 230.7 (224-242) from anterior end. Tail 188.8 (157-222) long, 57.5 (56—- 61) wide at anus. Two cuticularized, cup- shaped, midventral, pre-anal supplements present 179.5 (152-208) and 295 (240-360) anterior to anus. Posterior apophysis of each supplement about twice size of anterior apophysis; rim of cup striated. Two pairs small subventral papillae immediately an- terior to anus and another more lateral pair posterior to anus. Spicules 78.3 (75-82) long, gently curved then recurved at tip; tip broad with large barb. Gubernaculum with small corpus and narrow apophysis 34.3 (32-38) long; lateral parts of apophysis more heavily cuticularized; apophysis directed almost dorsally. a = 65.3 (60.3-70.8); b = 4.51 (3.91-4.95); c = 24.5 (20.6—27.7). Females (n = 4): Length 4.39 mm (3.63-— 4.96), width at midbody 104.8 (99-109). Head diameter 37.5 (34—40) at level of ce- phalic setae; cephalic setae 17 (16-18) and 5.5 (5-6) long. Amphid 18.8 (18-19) wide. Stoma 32 (30-34) long, 27.3 (26-29) wide. VOLUME 102, NUMBER 1 Esophagus 1.06 mm (0.846-1.12) long; nerve ring 240.8 (213-254) from anterior end. Tail 283.5 (258-323) long, 52 (48-54) wide at anus. Caudal setae restricted to anal region. Vulva 2.68 mm (2.03-3.12) from anterior end. a = 43.7 (36.7-51.7); b = 4.15 (3.94—4.31); c = 15.5 (14.0-17.1); V = 62% (60-64). Type-specimens. — Male holotype, USNM 77147; male paratypes, USNM 77148- 77149; female allotype, USNM 77150; fe- male paratype, USNM 77151. Paratype males, FNC A-152, A-153; female para- type, FNC A-154. Locality. —Holotype male from sedi- ments in a bed of shoalgrass (Halodule wrightii) in Grand Lagoon, St. Andrew Bay, Bay County, Florida (85°43'15’W, 30°07'50”N). Other locality, sediments in a bed of manatee grass (Syringodium fili- forme) at mouth of Freshwater Bayou, Bay County, Florida (85°39’00” W, 30°07'30’N). Etymology. —From the Greek para meaning beside and floridensis referring to Pareurystomina floridensis. Remarks.—Pareurystomina paraflori- densis 1s similar to P. floridensis in the length and shape of the spicules and gubernaculum in males and most characters in females. P. parafloridensis differs from P. floridensis primarily in the number of circles of den- ticles in the stoma and the shape and size of the denticles in each circle. P. paraflori- densis has five circles of stomatal denticles and the anterior four circles are of equal size and shape; each denticle is a small triangular structure. The posterior-most circle has larger triangular denticles. In P. floridensis there are three to four circles of denticles of variable size and shape; the denticles of the anterior-most circle are large elongate trian- gules, the following two circles are small and rounded and the posterior circle is large and rounded. P. parafloridensis is also similar to Pareurystomina combesi (Luc & De Con- inck, 1959) n. comb. in the number of rows of denticles in the stoma. It differs from P. combesi in that the excretory pore is ante- 255 Figs. 21-28. Pareurystomina parafloridensis: 21, Male holotype, head, lateral view; 22, Male holotype, head, lateral view; 23, Male holotype, posterior end, lateral view; 24, Male holotype, left spicule and gu- bernaculum, lateral view; 25, Male holotype, pre-anal supplements, lateral view (posterior, top right; anterior, bottom left); 26, Female, posterior end, lateral view; 27, Male paratype, left spicule and gubernaculum, lat- eral view; 28, Female, head, lateral view. Scale bars in yum. rior to the cephalic setae rather than pos- terior to the cephalic groove and the female tail is longer (c = 14—-17.1 vs. c = 47.8). Pareurystomina alima, new species Figs. 29-36 Diagnosis. —(Four males, 3 females, and 5 juveniles from mouth of Freshwater Bay- ou and Grand Lagoon, St. Andrew Bay). Body short, broad. Four submedian ce- phalic setae about %4 length of other 6. Flat cervical setae broad; extend from base of stoma to nerve ring; somatic setae not ob- served; caudal setae present. Amphids over level of stomatal suture when relaxed, an- terior to stomatal suture when contracted. Denticles in 2 broad bands of 3 circles each; Ol Figs. 29-36. Pareurystomina alima: 29, Male ho- lotype, head, right lateral view (contracted); 30, Male holotype, posterior end, lateral view; 31, Male holotype pre-anal supplements, lateral view (anterior, top; pos- terior, bottom); 32, Male paratype, right spicule, lateral view; 33, Female, tail, lateral view; 34, Male holotype, right spicule, lateral view; 35, Female, head, lateral view; 36, Male paratype, head, lateral view. Scale bars in um. first 4 circles anterior to suture complete with small, triangular denticles; next 2 cir- cles posterior to suture incomplete; first with small, round denticles; second with large, triangular denticles. Excretory pore anterior to cephalic setae. Tail conical, terminus acute. Males (n = 4): Length 3.22 mm (3.05-— 3.57), width at midbody 75.5 (53-86). Head diameter 38 (32-40) at level of cephalic se- tae; cephalic setae 13.5 (13-14), 3.7 (3-4) long. Amphid 16.5 (14-19) wide. Stoma 26 (24-27) long, 23.8 (21-25) wide. Esophagus 709.8 (598-792) long; nerve ring 210.5 (194— PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 219) from anterior end. Tail 168.5 (128- 184) long, 46 (38-50) wide at anus. Two midventral, cuticularized, cup-shaped, pre- anal supplements present 130.5 (70-160) and 211.8 (101-272) anterior to anus. Pos- terior apophysis of each supplement about twice size of anterior apophysis; rim of cup not striated. Two pairs circular, subventral, plaque-like papillae between anus and first pre-anal supplement. Two pairs small, sub- ventral setae immediately anterior to anus. Spicules straight, broad, 50 (45-54) long. Gubernaculum absent. a = 44.0 (36.6—57.4); b = 4.57 (4.36-5.10); c = 19.5 (17.1—23.8). Females (n = 3): Length 4.19 mm (3.24— 4.90), width at midbody 90 (80-104). Head diameter 42.3 (40-45) at level of cephalic setae; cephalic setae 14.7 (14-16), 3.7 (3-4) long. Amphid 17.3 (16-19) wide. Stoma 30.3 (27-32), 27.7 (26-30) wide. Esophagus 1.03 mm (0.843-1.15) long; nerve ring 236.7 (213-259) from anterior end. Tail 282.6 (248-328) long, 50 (48-51) wide at anus. Caudal setae sparse. Vulva 2.46 mm (1.83- 2.94) from anterior end. a = 47.8 (31.2- 57.0); b = 4.04 (3.84-4.26); c = 14.8 (13.1- 16.3); V = 58.3% (56-60). Type-specimens.— Holotype male, USNM 77152; paratype males, USNM 77153- 77154; allotype female, USNM 77155; paratype female, USNM 77156. Paratype male, FNC A-143; paratype female, FNC A-145. Locality.—Holotype male nonvegetated sediments from the mouth of Freshwater Bayou, St. Andrew Bay, Bay County, Flor- ida (85°39'00”W, 30°07'30’N). Other site, nonvegetated sediments in Grand Lagoon off St. Andrew Bay, Bay County, Florida (85°43'15”W, 30°07'50’N). Etymology.—From the Greek halimos meaning pertaining to the sea. Remarks.— Pareurystomina alima is most similar to P. parafloridensis in the stomatal characters. It differs in the greater number of circles of denticles (6 vs. 5), in the shape and size of the denticles in the posterior- most two circles, and the denticles in each VOLUME 102, NUMBER 1 circle are smaller. P. alima males differ from P. parafloridensis in the absence of a gu- bernaculum and in the short straight spic- ule. P. alima is similar to P. agubernacula Keppner, 1986, in the absence of a guber- naculum and the presence ofa short straight spicule. It differs from P. agubernacula in the greater number of circles of denticles (6 vs. 2) and shape and length of the spicules (45-54 vs. 25-27). Pareurystomina flagellicaudata Stekhoven, 1946 Figs. 37-41 Diagnosis. —(One male from site in Gulf of Mexico, Bay County, Florida.) Body very long, slender. Four submedian cephalic se- tae about '4 length of other 6. Flat cervical setae short, broad; present from base of sto- ma to about *3 distance to nerve ring. So- matic setae and caudal setae sparse. Am- phid just posterior to midlevel of stoma. Denticles in 2 circles, one complete circle large, triangular denticles anterior to suture, one incomplete circle large, triangular den- ticles posterior to suture. Excretory pore an- terior to cephalic setae. Tail conical then flagellate with acute terminus. Male (n = 1): Length 7.83 mm, width at midbody 48. Head diameter 30 at level of cephalic setae; cephalic setae 22 and 7 long. Amphid 14 wide. Stoma 29 long, 18 wide. Esophagus 782 long; nerve ring 248 from anterior end. Tail 600 long and 45 wide at anus. Two cuticularized, cup-shaped, mid- ventral supplements present 139 and 304 anterior to anus. Anterior and posterior apophyses of each supplement about equal; rim of cup not striated. Two pairs subven- tral setae immediately anterior to anus; sub- ventral and dorsolateral setae present from anus to just anterior to anterior supplement. Conical portion of tail with numerous small setae. Spicules almost straight, 48 long with blunt tip. Gubernaculum with short, weakly cuticularized apophysis 6 long, corpus a thin distal extension. a = 163; b = 10.0; c = 13.5 Figs. 37-41. Pareurystomina flagellicaudata: 37, Male, anterior end, lateral view; 38, Male, posterior end, lateral view; 39, Male, pre-anal supplements, lat- eral view (posterior, top; anterior, bottom); 40, Male, head, lateral view; 41, Male, right spicule and guber- naculum, lateral view. Scale bars in wm. Specimen. —One male, USNM 77157. Locality.—Coarse sand and shell near ledge in water 24 m deep in the Gulf of Mexico, Bay County, Florida (85°49'30’"W, 30°01'30’N). Remarks.—Pareurystomina flagellicau- data was described from a single female specimen. Hopper (1963) observed a spec- imen of P. flagellicaudata from Woods Hole, Massachusetts U.S.A., but did not mention the sex or provide figures of the specimen. To the writer’s knowledge, the male of this species has not been described. The speci- men described above is considered to be P. flagellicaudata based upon the number of rows of denticles in the stoma and the length of the tail. It differs from the original de- scription in the length of the cephalic setae and in having distinctly flattened cervical setae. However, the original description did not figure or state that the cervical setae 258 Figs. 42-46. Pareurystomina acuminata: 42, Male, head, right lateral view; 43, Male, head, left lateral view; 44, Male, posterior end, lateral view; 45, Male, pre-anal supplements, lateral view (posterior, left; an- terior, right); 46, Male, right spicule and gubernaculum, lateral view. Scale bars in pm. were flat or not, and the position of the ex- cretory pore was not mentioned. Pareurystomina acuminata (De Man, 1889) Figs. 42—46 Diagnosis. —(one male from sediment in St. Andrew Bay.) Body long, slender. Four submedian cephalic setae about '3 length of other 6. Fiat cervical setae broad, restricted to region just posterior to stoma. Somatic and caudal setae sparse. Amphid wide, an- terior to stomatal suture. Two circles tri- angular denticles present anterior to sto- matal suture, posterior circle incomplete with slightly smaller denticles; denticles ab- sent posterior to suture. Excretory pore an- terior to cephalic setae. Tail conical, tapers rapidly to acute terminus. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Male (n = 1): Length 3.50 mm, width at midbody 37. Head diameter at level of ce- phalic setae 24; cephalic setae 15 and 5 long. Amphid 13 wide. Stoma 28 long, 14 wide. Esophagus 651 long; nerve ring 194 from anterior end. Tail 235 long, 37 wide at anus. Two midventral, cuticularized, cup-shaped, pre-anal supplements present 165 and 309 anterior to anus. Anterior and posterior apophyses of each supplement about equal. Two pairs subventral papillae between anus and first pre-anal supplement. Single pair subventral setae immediately anterior to anus. Spicules 55 (chord), 72 (arc) long, strongly arcuate, tip with narrow velum and small lateral barb. Corpus of gubernaculum 14 long, does not surround spicules; gu- bernacular apophysis 16 long, straight, broad, heavily cuticularized, directed pos- tero-dorsally. a = 94.4; b = 5.38; c = 14.9. Specimen. —Male, USNM 77158. Locality.—Coarse sand and shell from water about 9 m deep in St. Andrew Bay off the mouth of Freshwater Bayou, Bay Coun- ty, Florida (85°39'17”W, 30°07'45’N). Remarks. —Gerlach (1952) described a male of P. acuminata and figured the am- phid as spiral in shape. Blome (1974) de- scribed two males of P. acuminata and fig- ured the amphid as a loose spiral. Neither author mentioned or figured the position of the excretory pore, and both figured the cer- vical setae as not flattened. The specimen described herein as P. acuminata 1s similar in all important characters to those de- scribed above with the exception of the shape of the amphid and the presence of flat cer- vical setae. Hopper (1963) described a female nema- tode collected at Gulf Shores, Alabama, U.S.A. as P. acuminata. However, this specimen has three circles of denticles in the stoma, a long tail, an oblong amphid, and the cephalic setae are shorter than those de- scribed for P. acuminata. The description and figures given by Hopper (1963) appear to be that of P. americana n. sp. with the exception of the absence of flat cervical se- VOLUME 102, NUMBER 1 tae. The cervical setae in P. americana are narrow and could be overlooked. Therefore, P. acuminata sensu Hopper (1963) is con- sidered to be a synonym of P. americana. Pareurystomina bissonettei Hopper, 1970 Figs. 47-50 This species was the second most abun- dant Pareurystomina collected (20 males, 14 females, and 9 juveniles). It was present in nonvegetated and vegetated, shallow water, estuarine sediments and one male was obtained from nonvegetated sediments in the Gulf of Mexico. Specimens agree with the description given by Hopper (1970). The notable exception is the male collected in the Gulf of Mexico. This male is appreciably larger but morphologically similar to the males from shallow, estuarine sediments. The body measurements are about equally proportional to the smaller estuarine males. A description of this male follows. Diagnosis.—Body long, slender. Large, vacuolated, subcuticular cells present in ad- dition to the hypodermal gland cells. Four submedian cephalic setae about 4 length of other 6. Flat cervical setae short, narrow, extend about '2 distance to nerve ring. So- matic setae short, sparse; caudal setae nar- row, flattened in males. Amphid wide, at midlevel of stoma. Denticles in 5 circles; those in 2 posterior circles slightly larger than those in anterior circles. Tail short, with narrow terminal spike with minute spines. Male (n = 1): Length 7.56 mm, width at midbody 107. Head diameter 85 at level of cephalic setae; cephalic setae 40 and 11 long. Stoma 66 long, 56 wide. Amphid 35 wide. Esophagus 1.70 mm long; nerve ring 320 from anterior end. Tail 145 long, 88 wide at anus; caudal setae numerous. Two cuti- cularized, cup-shaped, midventral, pre-anal supplements present 221 and 422 anterior to anus. Cup of each supplement with 4 arms each with striated distal terminus; arms directed anteriorly, posteriorly, and later- ally. Posterior apophysis of each supple- 259 Za Figs. 47-54. Pareurystomina bissonettei: 47, Male, head, sublateral view; 48, Male, pre-anal supplements, lateral view (anterior, left; posterior, right); 49, Male, posterior end, lateral view; 50, Female, tail, lateral view. Pareurystomina floridensis: 51, Male, head, lateral view; 52, Male, left spicule and gubernaculum, lateral view. Pareurystomina agubernacula: 53, Male, head, lateral view; 54, Male, left spicule, lateral view. Scale bars in um for all figs. ment very large, anterior apophysis small. Two pairs subventral papillae between anus and first pre-anal supplement. Single pair subventral setae immediately anterior to anus. Spicules 128 long, arcuate with small barb at tip. Corpus of gubernaculum does not surround spicules; gubernacular apoph- ysis 26 long, directed dorsally. a = 70.7; b = 4.45: c = 52.1 Specimen.—One male, USNM 77165; other males, 77159-77163; females, 77164 and 77166. Two males, FNC, A-147, A-148, A-149: female, A-150. Locality.—Coarse sand and shell near ledge in water about 24 m deep, Gulf of Mexico, Bay County, Florida (85°49'30’W, 30°01'30”N). Other specimens from various sites in St. Andrew Bay, Florida. 260 Pareurystomina floridensis Keppner, 1986 Figs. 51-52 This species was the most abundant en- countered during this study (33 males, 16 females, and 6 juveniles). It was recovered only from shallow water, nonvegetated sed- iments at a variety of sites in St. Andrew Bay and Lake Powell, Bay County, Florida. Examination of specimens recovered after the original description reveals that in some of the specimens there is an additional, par- tial circle of very small, round denticles present just anterior to the stomatal suture in addition to the three circles originally described. The apophysis of the gubernac- ulum in the specimens examine curves slightly ventrally at the tip. Figures are in- cluded for comparative purposes. Pareurystomina agubernacula Keppner, 1986 Figs. 53-54 This species has not been recovered since the original description, and the figures are included for comparative purposes. Megeurystomina combesi Luc & De Coninck, 1959 Luc & De Coninck (1959) described a new genus and species of Eurystomininae, Megeurystomina combesi. They differen- tiated the genus Megeurystomina from Par- eurystomina on the basis of the short length of the tail, the structure of the head partic- ularly its ability to retract and protract, and body size (10 mm and greater) in Megeu- rystomina. Lambshead & Platt (1979) con- sidered Megeurystomina to be a dubious genus due to the absence of a description of the male. The tail length (2 anal diameters), as a generic character for Megeurystomina, is contradicted by P. bissonettei that also has a short tail (1.5—2.5 anal diameters). The large male of P. bissonettei collected during this study from the Gulf of Mexico is about 1.6 times larger than the average P. bisso- nettei male collected from inshore waters. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON This reduces the importance of body size as a generic character for Megeurystomina. The retracted head observed in some of the spec- imens examined during this study reduces the importance of this as a generic character. M. combesi, therefore, may be a large form of a species of Pareurystomina. The struc- ture of the head is similar to that of the species of Pareurystomina with five or six circles of stomatal denticles. For these rea- sons, Megeurystomina is considered to be a synonym of Pareurystomina and the species Pareurystomina combesi (Luc & De Coninck, 1959) n. comb. is included in the key. It can be differentiated from the other species on the basis of the number of circles of denticles in the stoma, the position of the excretory pore, and the tail length. Key to Species of Adult Pareurystomina The taxonomic history of the genus Par- eurystomina 1s similar to that of the genus Eurystomina Filipjev, 1921, with regard to the characters of importance in differen- tiating species. Wieser (1953) stressed the importance of the characters of the head in distinguishing the species of Eurystomina. Inglis (1962) stressed the importance of the male genital apparatus, particularly the shape of the gubernaculum, in distinguish- ing the species of Eurystomina, and Yeates (1967) agreed with this approach. Wieser & Hopper (1967) recognized the value of using a combination of characters involving the head and male genital apparatus. As in the Eurystomina, the identification of the species of Pareurystomina is best achieved when males are available for study. In the following key, the maximum num- ber of circles of denticles in the stoma, po- sition of the excretory pore, and tail length are used to differentiate those species for which only females are known. The use of these characters allowed all species previ- ously described to be placed in the key with the exception of P. parapugetensis Vitiello, 1970, described from one juvenile and P. VOLUME 102, NUMBER 1 tenuissima (Filipjev, 1927) Filipjev 1946 described from one female. Both species could not be placed in the key because the position of the excretory pore is unknown. Therefore, these two species remain species dubiae in accordance with Lambshead & Platt (1979). The presence or absence of flat cevical setae was not used in the key because their presence on the species described prior to Hopper (1970) is uncertain. 1. Circles of denticles present in StORDE) eee D SiC RE eee _..P. tenuicauda Stekhoven, 1950 2(1). One to two circles of denticles HUAMSPOMNAS oie c. cas wyoue epee oe at 3 — Three or more circles of den- GIGIES IM SCOMA ...5.....4. 6. 11 3(2). One circle of denticles in sto- I ee a cP atts Oe 4 rk: 4 — Twocircles or denticles in sto- eee ht Oe, GUA), 5 4(3). Tail 18 anal diameters long . eee P. filicaudata Allgen, 1934 — Tail 4.5 anal diameters long ...P. typica Micoletzky & Kreis, 1930 5(3). Excretory pore posterior to ASE OF StOMA. 42. ean: s me ne 6 — Excretory pore anterior to base Ommstomiauxts! |. corey le aor! i 6(5). Stoma twice as long as wide; tail 10-11 anal diameters long (male unknown) ........... ... P. biserialis Stekhoven, 1946 — Stoma about 1.5 times as long as wide; tail less than 10 anal diameters long; spicules slen- der with recurved tip ....... Se « P. atypica Chitwood, 1960 7(5). Excretory pore at cephalic groove; amphid 31% of head diameter; tail 6 anal diameters long (male unknown) ....... ..P. armorica Luc & De Coninck, 1959 10(9). 11(2). 12(11). Excretory pore anterior to ce- phalic groove and setae; am- phid greater than 40% of head diameter; tail less than 6 anal diameters long .2:j/om05.:..- 8 Gubernaculum absent; spic- miesSiraight evn. dikekrn 2. .. P. agubernacula Keppner, 1986 Gubernaculum present; spic- ules straight to curved ...... 9 Gubernacular apophysis re- duced; spicules straight; tail 15 anal diameters long ........ _.. P. flagellicaudata Stekhoven, 1946 Gubernacular apophysis dis- tinct, elongate; spicules curved; tail less than 6 anal diameters lomo Sethe SERIA BOR: 10 Spicules thin, strongly arcuate, tip not recurved, with small lateral barb; corpus of guber- naculum elongate, does not surround spicules; gubernac- ular apophysis straight, direct- ed postero-dorsally ......... .. P. acuminata (De Man, 1889) Spicules broad, gently curved, tip recurved, small lateral barb absent; corpus of gubernacu- lum cone-shaped, surrounds spicules; gubernacular apoph- ysis straight, directed dorsally CHO ers Te: P. vaughtae, n. sp. Tail short, cylindrical, abrupt- ly narrows to terminal spike with minute spines in male, terminal spines absent in fe- male P. bissonettei Hopper, 1970 Tail conical, tip without mi- nute spines in males and fe- males Siew Saline. Ls i? Stoma with 5-6 circles of den- ticles, denticles in circles an- terior to stomatal suture small andiof equalisized 5 &. iil. «.: 13 Stoma with 3-4 circles of den- ticles, denticles in circles an- 262 1312): 14(13). 15(12). 16(15). 17(16). 18(17). PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON terior to stomatal suture equal orunequaloinsizes Gijon... ES Excretory pore posterior to ce- phalic groove; tail short (2 anal diameters) .. P. combesi, n. comb. Excretory pore anterior to ce- phalic groove and setae; tail longer (4 anal diameters or MOLO}e st. HU AGR ee 14 Stoma with 5 circles of denti- cles; spicules curved, tip re- curved with terminal barb; gu- bernaculum present; female cephalic setae 45% and amphid 50% of head diameter ...... Baths) etic P. parafloridensis, n. sp. Stoma with 6 circles of denti- cles; spicules straight, tip with- out terminal barb; gubernac- ulum absent; female cephalic setae 35% and amphid 40% of head diameter ...P. alima, n. sp. Tail 14 anal diameters long .. .... P. micoletzkyii Filipjev, 1946 Tail less than 10 anal diame- ters ONS IE O=rri a0 Fee. 16 Spicules without terminal barb; gubernacular apophysis bent dorsally at midpoint; male post-anal papillae absent ae 2 eee P. americana, Nn. sp. Spicules with terminal barb; gubernacular apophysis not bent dorsally at midpoint; male post-anal papillae present or absentrio).2) Serie hes 4 by/ Male post-anal papillae ab- sent; spicules with broad, cup- shaped tip with large barb ....P. floridensis Keppner, 1986 Male post-anal papillae pres- ent; spicules with narrow tip and:small bathtins 2no.%. .44 18 Male post-anal papillae about 4 distance from anus to tail tip; gubernacular apophysis short, directed dorsally ..... .. P. scillionensis Warwick, 1977 — Male post-anal papillae im- mediately post-anal; guber- nacular apophysis long, di- rected postero-dorsally ..... Gitar P. pugetensis Wieser, 1959 Acknowledgments Sincere appreciation is expressed to Dr. W. Duane Hope, National Museum of Nat- ural History, for his review of the manu- script, examination of the specimens, and continued encouragement. Appreciation is also expressed to Dr. Armen C. Tarjan, University of Florida, for his review of the manuscript and his encouragement. Mr. and Mrs. William Fable, National Marine Fish- eries Service, collected the sediment sam- ples from the Gulf of Mexico. Literature Cited Blome, D. 1974. Zur Systematik von Nematoden aus dem Sandstrand der Nordseeinsel Sylt.—Mik- rofauna Meeresboden 33:1-25. Chitwood, B. G. 1960. A preliminary contribution on the marine nemas (Adenophorea) of North- ern California.— Transactions of the American Microscopical Society 79:347-384. Gerlach, S. A. 1952. Nematoden aus dem Kiusten- grundwasser. — Abhandlungen der Akademie der Wissenschaften und der Literature, Mainz 6:315— S72: Hopper, B. E. 1963. Marine nematodes from the coast line of the Gulf of Mexico III. Additional species from Gulf Shores, Alabama.—Canadian Jour- nal of Zoology 4:841-863. 1970. Free-living marine nematodes from Biscayne Bay, Florida, III. Eurystominidae: Pareurystomina bissonettei sp. n. from Biscayne Bay and other locations.— Proceedings of the Helminthological Society of Washington 37:175— 178. Inglis, W.G. 1962. Marine nematodes from Banyuls- sur-Mer: With a review of the genus Eurysto- mina. — Bulletin of the British Museum (Natural History) Zoology 10:531-552. Lambshead, P. J. D., & H. M. Platt. 1979. Batheu- rystomina, a new genus of free-living marine nematodes (Enchelidiidae) from the Rockall Trough.—Cahiers de Biologie Marine 20:371- 380. Luc, M., & L. A. P. De Coninck. 1959. Nematodes libres marins de la region de Roscoff. — Archives VOLUME 102, NUMBER 1 de Zoologie Expérimentale et Générale 98:103- 165. Wieser. W. 1953. Free-living marine nematodes. I. Enoploidea.—Acta Universitatis Lundensis, Medica, Mathematica, Scientiae Rerum Natur- alium (N. F. 2) 49:1-155. . 1959. Free-living nematodes and other small invertebrates of Puget Sound beaches. Univer- sity of Washington Press, Seattle, Wash. 179 pp. , & B. E. Hopper. 1967. Marine nematodes of the east coast of North America. I. Florida.— 263 Bulletin of the Museum of Comparative Zool- ogy, Harvard University 135:239-344. Yeates,G. W. 1967. Studies on nematodes from dune sands 3. Oncholaimidae, Ironidae, Alaimi- dae.— New Zealand Journal of Science 10:299- Va 306 Hibiscus Avenue, Panama City Beach, Florida 32407. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 264-271 NEOTROPICAL MONOGENEA. 14. REVISION OF CALLORHYNCHOCOTYLE SURIANO AND INCORVAIA, 1982 (HEXABOTHRIIDAE) WITH THE DESCRIPTION OF C. AMATOI Walter A. Boeger, Delane C. Kritsky, and Joaber Pereira, Jr. Abstract. —The generic diagnosis of Callorhynchocotyle Suriano & Incorvaia, 1982, is emended based on new information obtained from specimens of the type species, C. marplatensis, collected from Callorhinchus callorynchus from the coasts of Uruguay and Argentina. Callorhynchocotyle marplatensis is re- described; Squalonchocotyle callorhynchi is redescribed and transferred to Cal- lorhynchocotyle; and C. amatoi is proposed for hexabothriids reported previ- ously from Callorhinchus milii by Manter (1955) and Dillon & Hargis (1968). All known Hexabothriidae are parasitic on gills of elasmobranch or holocephalan fishes (Class Chondrichthyes). Approxi- mately 60 species are described from elas- mobranchs; two are known from holo- cephalans. Manter (1955) described Squalonchocotyle callorhynchi from the holocephalans, Callorhinchus capensis Du- meril and C. milii Bory, from marine waters off South Africa and New Zealand, respec- tively. Dillon & Hargis (1968) redescribed this species as Erpocotyle callorhynchi (Manter, 1955) Yamaguti, 1963, based on specimens from C. milii in New Zealand waters. Lebedev & Parukhin (1969) report- ed the parasite under the latter name from C. capensis in Wallfish Bay (southwestern Africa); and in 1970, Kuznetsova recorded S. callorhynchi from Callorhinchus antarc- ticus Fleming (=C. callorynchus) from the Patagonian Shelf off South America. Suri- ano and Incorvaia (1982) proposed Callo- rhynchocotyle (Hexabothriidae) for their new species, C. marplatensis, from Callorhin- chus callorynchus (Linnaeus) off Argentina (38°S, 57°W). In the present study, Callo- rhynchocotyle Suriano & Incorvaia, 1982, is revised; C. marplatensis is redescribed; S. callorhynchi is redescribed and trans- ferred to Callorhynchocotyle; and C. ama- tol, N. sp., is proposed for hexabothriids re- ported from Callorhinchus milli by Manter (1955) and Dillon & Hargis (1968). Materials and Methods Hosts (Callorhinchus callorynchus) were collected by trawl off the coasts of Uruguay and Argentina during May 1985 and June 1986. Methods of parasite collection, prep- aration, measurement, and illustration are as described by Kritsky et al. (1986). Mea- surements are in micrometers; averages are followed by ranges in parentheses. Mea- surements of curved structures represent straight-line distances between extreme points; see Fig. 4 for those obtained from each sclerite. Vouchers (specimens collected during the present study) are deposited in helminthological collections of the National Museum of Natural History (USNM), which is housed at the USDA in Beltsville, Mary- land; the University of Nebraska State Mu- seum (HWML), Lincoln, Nebraska; the Fundacao Instituto Oswaldo Cruz (FIOQ), Rio de Janeiro, Brazil; and the Museo de La Plata (MP), La Plata, Argentina. Callorhynchocotyle Suriano & Incorvaia, 1982 Emended diagnosis. —Hexabothriidae. Body elongate. Tegument thin, smooth. VOLUME 102, NUMBER 1 Caeca confluent in peduncle posterior to testes. Testes numerous, irregular; vas def- erens sinuous, surrounded by small gland cells along most of its length, with small loop proximal to entrance into cirrus. Cirrus comprising two parts: distal part ovate, bul- bous; proximal part a thick-walled nonex- panded tube. Genital pore at level of gut bifurcation. Ovary lobate anteriorly, coiled posteriorly; oviduct originating from pos- terior end of ovary; seminal receptacle sac- like, reduced; ootype smooth; uterus dorsal to ovary, ventral to vas deferens. Vagina parallel, comprising two portions; distal portion glandular, proximal portion deli- cate. Vaginal pores on ventral surface about midway between body midline and lateral margin on each side of cirrus. Vitellaria comprising 2 bilateral bands extending from level of vaginal pores into peduncle; vitel- line commissure, genitointestinal canal dor- sal to ovary. Eggs with two polar filaments, forming continuous chain by united fila- ments. Excretory pores marginai at level of genital pore. Haptor asymmetrical; with 2 small, 4 large sucker-sclerite complexes; small complexes lying on same side of lon- gitudinal axis of haptor; appendix originat- ing from dorsal haptoral surface lateral to body midline, armed with 2 anchors, 2 ter- minal suckers. Parasites of Callorhinchidae. Type species.—Callorhynchocotyle mar- platensis Suriano and Incorvaia, 1982, from Callorhinchus callorynchus. Other species.—Callorhynchocotyle cal- lorhynchi (Manter, 1955), n. comb., from Callorhinchus capensis; Callorhynchocotyle amatoi, n. sp., from Callorhinchus milii. Callorhynchocotyle marplatensis Suriano & Incorvaia, 1982 Figs. 1-9, 10a, lla, 12a Synonyms.—Callorhynchocotyle callo- rhynchi Suriano & Incorvaia, 1982; C. cal- lorhynchy Suriano & Incorvaia, 1982. Host.—Callorhinchus callorynchus (Lin- naeus). 265 Distributions. —Coasts of Uruguay, Ar- gentina (holotype). Specimens studied.—Holotype, MP 12; 17 vouchers, USNM 80279, HWML 20705, 20706, FIOC 32.442, MP 1613 D. Description (measurements in Table 1).— Weak genital sucker, 94—110 testes. Papillae lacking on rim and inner wall of oral, hap- toral suckers. Sucker sclerite 2, 3 with elon- gate point, evenly curved shaft and point. Anchor with wide base, short roots, medi- ally curved shaft, short point. Remarks.—Suriano & Incorvaia (1982) treat this species under three names: C. marplatensis, C. callorhynchi, and C. cal- lorhynchy. The latter two apparently rep- resent typographic and/or editing errors. It iS apparent that these authors were not re- ferring to other species of Callorhynchoco- tyle since they consider the genus monotyp- ic. Clearly, the authors intended the name of their new species to be C. marplatensis which is considered herein as the valid name of the taxon. Based on the holotype and voucher spec- imens, it is evident that Suriano & Incorvaia (1982) confused polarity of the dorsoventral axis in their specimens. This is supported by their illustration of the holotype pre- sented as a dorsal rather than a ventral view as the specimen is mounted. Consequently, the sinistrodextral orientations of features of the parasite are reversed in the original description. Also contrary to the original description, the haptoral appendix origi- nates from the dorsal surface of the haptor, and the genitointestinal canal, uterus and vitelline commissure are dorsal to the ovary. The holotype is a damaged, excessively flattened, and contracted specimen. One of the haptoral suckers and its sclerite are torn away (not shown in fig. 1 of Suriano & In- corvaia 1982). Apparently, these original authors added the missing sucker to their drawing of the holotype based on the pres- ence of six suckers in other specimens of their collection. This, however, resulted in their apparent confusion of a damaged mus- 266 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Table 1.—Measurements (in micrometers) of Callorhynchocotyle species. Body length Body width Haptor Length Width Oral sucker Width Pharynx Length Width Genital sucker Diameter Egg Length Width Ovary Length Distal vagina Appendix Length Width Appendix sucker Length Width Anchor Length Base width Diameter of haptoral sucker Pair | Pair 2 Pair 3 Sclerite #1 Total Shaft Point Sclerite #2 Total Shaft Point Sclerite #3 Total Shaft Point C. callorhynchi (n = 2) 6052 (4995-7109) 845 (669-1021) 2007 284 (248-322) 102 64 (56-72) 152 (136-168) 58 (53-62) 639 (459-818) 276 2104 (1844-2363) 997 (972-1021) 289 109 194 (186-203) 274 (258-290) 362 319 283 (281-285) 31-32 42 (39-45) 362 88 106 35 84 (83-86) 123-124 C. marplatensis (n = 17) 9989 (7200-12,430) 939 (649-1217) 2719 (2051-3324) 1596 (1331-1918) 302 (231-362) 71 (58-83) 71 (60-78) 205 (153-262) 145 (125-193) 59 (52-66) 1147 (816-1505) 180 (136-203) 1397 (1275-1637) 256 (149-350) 181 (164-204) 195 (154-190) 190 (144-210) 87 (72-98) 305 (243-346) 365 (270-419) 345 (267-393) 353 (289-385) 33 (27-44) 50 (42-57) 460 (362-499) 76 (59-92) 117 (95-141) 454 (382-512) 80 (65-92) 129 (99-145) C. amatoi (n = 8) 7091 (5329-8474) 989 (706-1316) 1959 (1451-2482) 1201 (755-1639) 252 (191-356) 79 (69-91) 70 (62-89) 156 (144-169) 54 (48-60) 859 (651-971) 350 (269-432) 1108 (674-1429) 850 (541-1206) 272 (236-320) 144 (102-185) 182 (172-195) 85 (83-87) 267 (188-362) 332 (232-435) 310 (217-415) 297 (239-355) 20 (18-22) 37 (36-39) 412 (347-452) 54 (46-70) 83 (70-98) 408 (332-469) 56 (45-66) 92 (86-98) VOLUME 102, NUMBER 1 267 002 0002 5 = 6 Figs. 1-6. Callorhynchocotyle marplatensis: 1, Whole mount (ventral); 2, Sucker-sclerite complex; 3, Sclerite of complex 1; 4, Sclerite of complex 2; 5, Sclerite of complex 3; 6, Anchor. All figures are reproduced to respective scales except Figs. 3, 4, 5 are drawn to the 250-micrometer scale. Circled numbers identify sucker-sclerite pairs in the haptor. Fig. 4 shows measurements taken from each sclerite (Table 1): a = total length; b = shaft length; c = point length. cle as a haptoral extension of the gut. In the the esophagus has lateral diverticulae, the holotype the gut is not visible in the haptor, caeca are confluent posterior to the testes, although the structure depicted as gut (the and the intestine extends into the haptor muscle which apparently served the lost with branches, one of which occurs in the sucker) is evident. Our specimens show that haptoral appendix. 268 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Figs. 7-9. Callorhynchocotyle marplatensis: 7, Ventral view of anterior end; 8, Egg chain from uterus; 9, Female reproductive system (ventral). Figures are to respective 200-micrometer scales. Callorhynchocotyle amatoi, new species Figs. 10c, llc, 12c Synonyms.—Squalonchocotyle_ callo- rhynchi Manter, 1955 (part); Erpocotyle callorhynchi (Manter, 1955) Yamaguti, 1963 (part). Host.—Callorhinchus milii Bory. Type locality. —Coast of New Zealand. Specimens studied.—Holotype, USNM 37448; seven paratypes, USNM 71197, HWML 1442. Description (measurements in Table 1).— Genital sucker absent; 94-120 testes. Pa- pillae present on rim and inner wall of oral, haptoral suckers. Sucker sclerite 2, 3 with short point; indistinct angle formed at union of shaft and point of sclerite 3; sclerite 1 with delicate point, short shaft. Anchor with wide base, short roots, medially curved shaft, short point. Etymology. —This species is named for Dr. Jose Felipe R. Amato, Universidade Federal Rural do Rio de Janeiro, in recog- nition of his contributions in marine par- asitology. Remarks. —Our study of the type speci- mens of Squalonchocotyle callorhynchi Manter, 1955, and specimens identified as Erpocotyle callorhynchi (Manter, 1955) by Dillon & Hargis (1968) revealed that those from Callorhinchus milii from New Zea- land represent a species distinct from that occurring on C. capensis. Although Dillon & Hargis (1968) recognized the morpholog- ic differences between these specimens, they did not question their conspecificity. Since the holotype of Squalonchocotyle callorhynchi is a specimen collected from the gills of Callorhinchus capensis captured off South Africa, Callorhynchocotyle amatoi is proposed for those specimens from Cal- lorhinchus milii from New Zealand. Cal- lorhynchocotyle amatoi differs from C. cal- lorhynchi and C. marplatensis by having shorter shafts and points of all sucker scler- ites (Fig. 13) and an indistinct angle between the point and shaft of sclerite 3 (Fig. 12c). Callorhynchocotyle callorhynchi (Manter, 1955), new combination Figs. 10b, 11b, 12b Synonyms.—Squalonchocotyle callo- rhynchi Manter, 1955 (part); Erpocotyle cal- VOLUME 102, NUMBER 1 269 CA \ i, : \ | } 4 | \ WOE + : a. | | Soa / Se" | pny b | ( / b/ / shy Se / —e Ne i Se Se Figs. 10-12. Sclerites of Callorhynchocotyle spp.: 10, Sclerite of complex 1; 11, Sclerite of complex 2; 12, Sclerite of complex 3. a = C. marplatensis; b = C. callorhynchi; c = C. amatoi. All figures are drawn to the same scale. lorhynchi (Manter, 1955) Yamaguti, 1963 (part). Host.—Callorhinchus capensis Dumeril. Type locality. —Coast of South Africa. Specimens studied. —Holotype, paratype, USNM 37447. Description (measurements in Table 1).— Genital sucker absent, 96—98 testes. Pa- pillae present on rim and inner wall of oral, haptoral suckers. Sucker sclerite 1, 2, 3 with short point, moderate shaft, evenly curved shaft and point. Anchor with wide base, short roots, medially curved shaft, short point. Remarks.—Callorhynchocotyle callo- rhynchi is most similar to C. marplatensis, from which it differs by possessing papillae on the rim and inner walls of the oral and haptoral suckers, a comparatively long dis- tal portion of the vaginae, absence of a gen- ital sucker, and by the comparative mor- phology of the shaft and point of the sucker sclerites (Figs. 10-12). Discussion Callorhynchocotyle was proposed by Suriano & Incorvaia (1982) to accommo- date C. marplatensis. Among characters used to define the genus was the presence of marginal vaginal pores. Examination of the holotype (MP 12) of C. marplatensis and vouchers collected during the present study shows that the vaginae actually open sub- marginally as they do in members of all other hexabothriid genera. Apparently Suri- ano and Incorvaia (1982) confused the lat- eral excretory pores as the vaginal apertures. Other characters used by Suriano and In- corvaia (1982) for diagnosis of the genus include: 1) an asymmetric haptor with 6 suckers armed with sclerites of different sizes, 2) a sac-like seminal receptacle, 3) par- allel bilateral vaginae, 4) an unarmed cirrus, 5) a smooth ootype, and 6) the absence of a glandular region of the cirrus. Of these, only the absence of a glandular region of the cirrus is unique for the genus. In Callo- = 160 3 140 ~~" I= 120 ne © 100 QO, +4 80 O 1 ‘60 8 06 o e C. marplatensis =) 4 « C. amatoi a 40 ¢ © C. callorhynchi 4 20 , 15 30 45 60 45) 90 105 Length of shaft (um) 13 Fig. 13. Scatter diagram of length of point versus length of shaft of the sclerite for three species of Ca/lo- rhynchocotyle. The left column of symbols of the leg- end refers to sclerite 1 of respective species; the second column refers to sclerites 2, 3 of the respective species. 270 rhynchocotyle, the glandular region of the cirrus is apparently replaced by an extensive glandular segment of the vas deferens. These characters may represent an example of compensatory change (evolution) as defined by Brooks and Wiley (1986). Other hexabothriid genera with asym- metric haptors include Heteronchocotyle Brooks, 1934, Paraheteronchocotyle Mayes, Brooks and Thorson, 1981, Epicotyle Euzet & Maillard, 1974, Rhinobatonchocotyle Doran, 1953, and Neonchocotyle Ktari & Maillard, 1972. The haptor of Callorhyn- chocotyle most closely resembles that of Neonchocotyle in that the asymmetry re- sults from the apparent migration of one sucker-sclerite complex to the opposite side of the haptor. Further, the appendix does not originate from the midline which adds to haptoral asymmetry. In addition to the above, Callorhyncho- cotyle is distinguished from other hexa- bothriid genera by the combined presence of the following characters: presence of a bulbous distal cirrus, a dorsal instead of terminal haptoral appendix, and a terminal glandulomuscular portion of the vagina. Hargis (1955) reported that the genitoin- testinal canal of Heteronchocotyle leucas Hargis, 1955 (Hexabothriidae), apparently joined the left intestinal caecum and sug- gested that this condition was rare among the higher Monogenea. In individual spec- imens of Callorhynchocotyle, the genitoin- testinal canal was found to be united to the intestinal caecum which corresponded to the respective position of the ovary, 1.e., if the Ovary occurred to the right of the body mid- line (Fig. 9) the genitointestinal canal united with the right caecum and conversely with the left caecum if the ovary occurred to the left of the body midline (Fig. 1). Similarly, the haptoral appendix and the migrated sucker-sclerite complex occur either to the left or right of the longitudinal haptoral axis. However, there was no correlation between the asymmetry of the haptor and the loca- tion of the ovary. The sinistral or dextral PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON position of the ovary and genitointestinal canal and the position of the appendix and sucker-sclerite in the haptor are examples of intraspecific variation and do not con- stitute generic characteristics for the Hexa- bothrudae. Acknowledgments The authors wish to thank Drs. O. M. Blanco (MP), J. R. Lichtenfels (USDA), and M. Pritchard (HWML) for allowing us to examine specimens in their care. The Con- selho Nacional de Desenvolvimento Cien- tifico e Tecnologico provided a study grant (20.0115/84) to WAB. Literature Cited Brooks, D. R., & E. O. Wiley. 1986. Evolution as entropy. Toward a unified theory of biology. University of Chicago Press, Chicago, Illinois. 335 pp. Dillon, W. A., & W. J. Hargis. 1968. Monogenetic trematodes from the southern Pacific Ocean. Part IV. Polyopisthocotyleids from New Zealand fishes: The families Mazocraeidae, Diclidopho- ridae and Hexabothriidae. — Proceedings of the Biological Society of Washington 81:351-366. Hargis, W. J., Jr. 1955. Monogenetic trematodes of Gulf of Mexico fishes. Part VI. The superfam- ilies Polystomatoidea Price, 1936 and Dicli- dophoroidea Price, 1936.—Transactions of the American Microscopical Society 74:361-377. Kritsky, D. C., V. E. Thatcher & W. A. Boeger. 1986. Neotropical Monogenea.. 8. Revision of Uro- cleidoides (Dactylogyridae, Ancyrocephali- nae). — Proceedings of the Helminthological So- ciety of Washington 53:1-37. Kuznetsova, I. G. 1970. Parasitofauna of cartilagi- nous fishes of the Patagonian Shelf. Pp. 52-54 in Issues on marine parasitology, materials from the Ist annual All-Union Symposium on Par- asites and Diseases of Marine Life, Sevastopol. Publ. Naukova Dumka, Kiev. Lebedev, B. I., & A. M. Parukhin. 1969. Monogenea of some fish from Wallfish Bay (south-western Africa). —Gidrobiologicheskii Zhurnal 5:70-8 1. Manter, H. W. 1955. Two new monogenetic tre- matodes from elephant fishes (Callorhynchus) from South Africa and New Zealand. Pp. 211- 220 in Essays in the natural sciences in honor of Captain Allan Hancock. University of South- ern California Press, Los Angeles. Suriano, D. M., & I. S. Incorvaia. 1982. Sistematica VOLUME 102, NUMBER 1 y biologia de Callorhynchocotyle marplatensis gen. et sp. n. (Monogenea: Polyopisthocotylea) parasita de las branquias de Callorhynchus cal- lorhynchus (Linne, 1758) Garman, 1904 (Pisces: Holocephali) de la region costera de Mar del Plata. —Comunicaciones del Museo Argentino de Ciencias Naturales Bernardino Rivadavia e Instituto Nacional de Investigacion de las Cien- cias Naturales 2:19-32. (WAB) Department of Biological Sci- ences, Idaho State University, Pocatello, 271 Idaho 83209, and Instituto Nacional de Pesquisas da Amazonia, Manaus, Amazon- as, Brazil; (DCK) Department of Allied Health Professions and Idaho Museum of Natural History, Idaho State University, Pocatello, Idaho 83209; (JP) Departamento de Ciéncias Morfobidlogicas, Fundacao Universidade do Rio Grande, Rio Grande, Brazil. PROC. BIOL. SOC. WASH. 102(1), 1989, pp. 272-279 PHYTOPLANKTON COMPOSITION IN A BORROW PIT LAKE IN VIRGINIA Seba B. Sheavly and Harold G. Marshall Abstract.—The phytoplankton assemblages in Lake Trashmore, Virginia, a borrow pit, were dominated by centric diatoms and cyanobacteria, with sea- sonal pulses of cryptomonads, euglenoids, and chlorophyceans. Ninety species were identified and their abundance levels noted for a 12-month period. Borrow pit lakes are generally associated with highway construction and residential landscaping. In contrast, this borrow pit lake was formed as part of an above-ground landfill operation. Alternate layers of soil and refuse were laid down to eventually form a mound that was capped with soil, then landscaped. The pit formed in this process was gradually filled with water by 1971. The lake is located in Virginia Beach, Virginia, where it is now a part of a recreational park complex. The lake has a mean depth of 4 m, a maximum depth of 7.3 m, a surface area of 21 ha, and a volume of 8.4 x 10° m? (Virginia State Water Control Board 1982). The surrounding area is highly de- veloped. The lake is flanked to the north and south by major highways and is adja- cent to the disposal mound (Mount Trash- more) on the west, with residential devel- opment along the eastern section. The purpose of this study was to identify the seasonal phytoplankton composition and concentrations of this lake and to make comparisons with a phytoplankton survey of the lake made over a decade ago (Cocke 1973). Other phytoplankton studies in Virginia have concentrated on the two natural lakes in the state, Lake Drummond and Moun- tain Lake (Simmons & Neff 1974, Marshall 1979). In addition, the National Eutrophi- cation Survey (Anonymous 1972) included eight other Virginia lakes and reservoirs that were of greater size than Lake Trashmore, and all were found to be eutrophic. Phyto- plankton were included in a limited water quality study during the early formation of Lake Trashmore by Beck (1973). He indi- cated an abundance of diatoms, chlorophy- ceans, cyanobacteria and phytoflagellates. Later Cocke (1973) completed a one year study of the lake and reported 45 taxa, with chlorophyceans and diatoms dominant. In general, borrow pit lake studies are rare. In Nebraska, McCarraher et al. (1974) sur- veyed 41 borrow pit lakes in the Platte River Valley, with Adrian et al. (1970) conducting a primary productivity study on one lake. Seven Illinois borrow pit ponds were stud- ied by Lipsey (1980). In all of these studies, the formation of borrow pits was associated with a major highway development. Dia- toms, cyanobacteria and chlorophyceans were generally the dominant forms in these ponds or lakes. Methods. —One collection station was es- tablished at the center and deepest (7.3 m) portion of the lake. Samples were collected monthly from the upper and lower 0.5 m of the euphotic zone from Mar 1985 to Feb 1986. The lower sampling depth was deter- mined from transparency measurements with a Secchi disk (15 cm diam), according to Holmes (1970). A Kemmerer water bot- tle (2 liter) was used to obtain 500 ml water samples from both depths. These were pre- served immediately with Lugol’s solution VOLUME 102, NUMBER 1 and returned to the laboratory, where a set- tling and siphoning procedure was followed to obtain a 40 ml concentrate. Aliquots were taken from this concentrate and placed in settling chambers for examination with a Zeiss inverted plankton microscope. A ran- dom field and minimum count procedure was followed at magnifications of 312 x and 500 x for micro-, nano-, and picoplankton for a precision estimate of 85%. In addition, the net phytoplankton were counted by scanning the entire chamber at 125. Results. -—Mean water temperatures ranged from 4.0°C in January to 27.3°C in August, with only small differences gener- ally found with depth in the euphotic zone. The mean monthly pH value was 7.52, with a range from 6.5 (Dec) to 8.6 (Sep). Secchi disk readings ranged from 0.47 m (Mar) to 1.18 m (Aug), averaging 0.84 m. Ninety phytoplankton species were iden- tified in this study (Table 1), including 32 Chlorophyceae, 28 Bacillariophyceae, 16 Cyanobacteria, 8 Euglenophyceae, 5 Di- nophyceae, and 1 Cryptophyceae. Uniden- tified picoplankton and nanoplankton cells were counted by size groups <3, 3-5 and 5-10 wm. They were present throughout the year, with lowest concentrations in May (3.7 x 10° cells/liter), gradually increasing to a December high (61.5 x 10° cells/liter). The majority of these cells were <3 wm in size and under epifluorescence microscopy proved to be cyanobacteria. In contrast, larger and identifiable cyanobacteria had one major pulse in summer and early fall, reach- ing 37.0 x 10° cells/liter in September. Eu- glenoids and dinoflagellates also had high summer concentrations. In contrast, the cryptomonads were in lowest concentrations in summer and early fall and became more abundant during winter and spring. The diatoms had low concentrations in spring and summer, gradually increased into fall and early winter and peaked in December (9.4 x 10° cells/liter). The dominant species were Cyclotella spp. and Melosira spp., with representatives from these genera most 273 common in the unidentified category of cen- tric diatoms <20 um size. Discussion. —In comparison to early data on phytoplankton populations in Lake Trashmore (Beck 1973, Cocke 1973), there has been a shift in composition and domi- nant species. Cocke identified 45 species in a seven-month study (Aug—Feb), with the two dominant groups: pennate diatoms (e.g., Pleurosigma normanii, P. strigosum) and chlorophyceans (Pediastrum simplex) the major species. He found cyanobacteria (blue-green algae) to be common, but not abundant. Other dominant species included the desmids Closterium lunuae and Cos- marium circulare, the diatoms Fragilaria crotonensis, Melosira spp., Navicula spp.., and the dinoflagellate Gymnodinium sim- plex. Secchi disk readings at this time ranged between 24.0 and 54.0 cm, averaging 40.9 cm. The range of the surface pH values was 6.6 to 7.1, averaging 6.8. The present study indicated a more basic pH mean of 7.52, ranging between 6.5 and 8.6. However, the Secchi disk readings were higher, averaging 84 cm, with readings between 47 cm (Mar) and 118 cm (Aug). In addition to an increased diversity of species, there has been a change over the past decade in the phytoplankton popula- tions in Lake Trashmore. The transition has been from a dominance of pennate diatoms, chlorophyceans, and a filamentous-coccoid assemblage of cyanobacteria to the current status, where cyanobacteria, centric dia- toms (e.g., Cyclotella spp., Melosira spp.), plus a seasonal abundance of cryptomo- nads, euglenoids, and chlorophyceans are dominant. It is impossible to evaluate the significance of the high picoplankton and nanoplankton (<10 um) concentrations be- cause Cocke’s collection procedure by tow net would not have collected many of these cells. However, these changes in phyto- plankton composition and abundance are assumed to be in association with the chang- ing and advancing eutrophic state of the lake over the past decade. 274 Table 1.—Mean monthly abundance for each identified taxon (cells/liter). PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Mar Apr May Jun Bacillariophyceae Achnanthes sp. 47,268 639 5373 1S Amphora costata W. Smith 0 0 0 213 Amphora sp. 0 21 0 0 Biddulphia alternans (Bailey) Van Heurck 0 0 5 0 Cocconeis distans Gregory 21 0 0 0 Cyclotella meneghiniana Kitzing 0 77,867 29,373 18,131 Cyclotella sp. 273,843 27,084 28,213 4578 C. striata (Kiitzing) Grunow 0 0 18,056 0 Cylindrotheca closterium (Ehrenberg) Reimann & Lewin DTT 0 0 53 Cymbella sp. 9515 602 123 85 Diploneis sp. 0 0 16 12 Fragilaria sp. 0 0 0 10,579 Gomphonema sp. 0 0 16 53 Gyrosigma sp. 0 0 0 21 Melosira distans (Ehrenberg) Kiitzing 33,824 0 0 0 M. granulata (Ehrenberg) Ralfs 221,898 9649 299 1664 M. islandica Muller 5195 0 4557 85 M. moniliformis (Muller) Agardh 0 0 32 0 Melosira sp. 0 37 107 427 Navicula spp. 9813 37 32 117 Nitzschia clausii Hantzsch 0 0 0 64 N. pungens Grunow 43 0 0 75 N. seriata Cleve 43 0 0 0 Nitzschia sp. 14,411 16 0 32 Rhizosolenia eriensis H. L. Smith 0 0 0 0 Synedra acus Kaiitzing 0 0 0 0 Synedra spp. 0 21 85 587 Thalassionema nitzschioides (Grunow) Grunow & Hustedt 0 16 0 384 centrics (unid.) <20 wm diam. 285,376 293,413 178,303 81,607 centrics (unid.) 20-100 um diam. 109,243 0 0 14,374 pennates (unid.) >20 um in length 51,857 56,426 28,341 22,072 pennates (unid.) <20 um in length 26,076 112 101 21 subtotal 1,088,703 465,940 294,032 156,000 Dinophyceae Ceratium hirundinella (O. F. Muller) Dujardin 0 0 368 19,040 Glenodinium gymnodinium Penard 0 0 0 43 Glenodinium sp. 0 3 0 0 Gymnodinium sp. 0 0 0 36,113 Protoperidinium sp. 0 0 0 96 subtotal 0 3 368 55,292 Cyanobacteria Anabaena sp. IP) 23,138 0 576 Chroococcus limnecticus Lemmerman 0 0 0) 477,533 Dactylococcopsis raphidiodes Hansgirg 2,607,829 920,865 478,484 101,230 Gomphosphaeria aponina Kutzing 120,610 lay 2294 9028 Johannesbaptistia pellucida (Dickie) Taylor & Drouet 0 0 0 0 Lyngbya controta Lemmermann 0 0 0 0 VOLUME 102, NUMBER 1 275 Table 1.—Continued. Jul Aug Sep Oct Nov Dec Jan Feb 1984 0 0 0 0 256 0 0 469 64 107 0 0 0 0 64 0 0 0 0 0 247 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 18,057 18,078 36.113 0 36,455 180,907 J9,297, 483,016 9028 P5525 52 270,850 81,255 81,255 424,328 40,626 731,316 0 0 22.9571 0 0 0 0 40,628 0 32,154 46,187 0 128 213 208 725 43 64 207 128 128 640 52 139 43 0 0 0 0 0 0 0 533 853 36,849 0 341 768 0 0 0 64 0) 0 0 0 0 0 0 0 0 0 0 0 0 0 0) 0 0 36,415 1,363,278 3,403,654 ES7.677 153,780 28557 31,864 248,919 768,108 806,756 3,710,612 343,064 690,668 320 1472 427 198,623 0 0 0 0 0 0 0 0 0 0 0 0 9220 0 0 40 0 0 0 0 768 939 2965 1493 256 1963 64 18,099 9114 4557 0 0 0 256 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 128 0 Se) 0 0 0 0 0 0 117,432 63,198 0 0 0 0 0 43 875 532675 128 469 700 S17 789 597 51,789 124,323 49,878 3029 3212 171 299 299 18,505 2T2Z2NS 0 0 180,799 0 0 117,368 153,482 329,534 135,425 261,864 1,426,466 279,190 1;923;035 oA 21 18,227 0 213 640 38,369 31,599 22,571 9028 995312 54,170 939 232,435 58,682 90,282 85 40,734 341 85 768 1244 8028 533 219,248 617,507 1,626,645 1,325,748 2,555,879 9,569,435 961,930 4,164,983 5589 3392 23,467 13,227 1408 537 16 0 85 1835 1771 981 0 0 0 0 213 0 1600 18,185 0) 0 0 0 64 0 0 0 0 0 22,570 0 43 0 0 0 0 0 0 0 5994 3227 26,838 32,393 1408 ae We 22,586 0 1,173,683 9,619,689 6,238,578 157605525 2987 356,250 0 0 537,186 64,009 643,401 451,417 504,161 2,644,782 205,091 175,549 94,947 0 225,708 370,162 353,897 839,628 815,906 1,047,287 0 128 100,784 397,247 91,862 58,479 21,479 32,815 341 0 0 0 0 0 0 0 0 794,493 174,098 64,350 0 0 0 0 SSS 276 Table 1.—Continued. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Mar Apr May Jun Merismopedia glauca (Ehrenberg) Naegeli 0 0 0 0 Merismopedia punctata Meyen 0 0 8038 18,526 Merismopedia sp. 0 0 0 0 Merismopedia tenuissima Lemmermann 0 0 0 0) Microcystis aeruginosa Kiutzing 408,516 2,471,603 2,059,101 2,719,878 Nostoc commune Vaucher DAT 15,738 432 779 Oscillatoria limnetica Lemmermann 0 0 0 0 Oscillatoria sp. 0 32 208 4274 Spirulina laxa G. M. Smith 0 0 0 53 Spirulina subsalsa Oersted 0 0 0 52 blue green spheres (unid) 0) 0 54,168 0 blue green trichomes (unid) 64 1129 6782 23,010 subtotal 3,138,021 3,432,657 2,609,507 3,354,919 Euglenophyceae Euglena acus Ehrenberg 0 0 0 0 Euglena sp. 0 0 0 1821 Eutreptia lanowii Steuer py syl 52,529 D591 87,704 Eutreptia viridis Perty 85 0 5) 43 Phacus longicaudus (Ehrenberg) Dujardin 0 0 0 0 Phacus curvicaudus Swirenko 0 0 0 0 Trachelomonas hispida (Perty) Stein 0 0 0 0 Trachelomonas volvocina Ehrenberg 0 0 0 76,608 subtotal 2342 52,529 22,591 182,572 Chlorophyceae Ankistrodesmus falcatus Beijerinck 156,672 27,655 31,316 31,445 Ankistrodesmus fractus (West & West) Brunnthaler 0 0 0 0 Chlorella sp. 9028 0 0 0 Chlorella vulgaris Beijerinck 0 0 0 4104 Cosmarium botrytis Meneghini 0 0 0 0 Crucigenia apiculata (Lemmermann) Schmidle 0 0 0 0 Crucigenia fenestrata Schmidle 92,219 0 0 18,057 Crucigenia quadrata Morren 0 0 9113 744,539 Crucigenia sp. 0 0) 4514 0 Crucigenia tetrapedia (Kirchner) West & West 1,831,853 1435152 0 207,908 Dictyosphaerium pulcellum Wood 1365 309,316 143,839 2,013,046 Euastrum denticulatum (Kirchner) Gay 0 0 0 21 Franceia droescheri (Lemmermann) 0 0 0 0 Kirchneriella contorta (Schmidle) Bohlin STL WS) 293,977 302,438 283,177 Lagerheimia ciliata (Lagerheim) Chodat 0 0 0 0 Lagerheimia quadriseta Lemmermann (G. M. Smith) 0 0 0 0 Micractinium pusillum Frensenius 0 0 0 0 Oedogonium sp. 0 0 421 0 Oocystis borgei Snow 114,091 129,214 105,047 250,682 Pediastrum duplex Meyen 0 0 0 0 Pediastrum simplex (Meyen) Lemmermann 36,147 421 1259 5845 Scenedesmus armatus (Chodat) G. M. Smith 363 0 0 0 VOLUME 102, NUMBER 1 ZIT Table 1.—Continued. Jul Aug Sep Oct Nov Dec Jan Feb 0 S225 0 341 0 0 0 0 0 eA | ZAZS 1024 308,329 704 0 0 0 0 0 0 288,907 0 0 0 0 OF» 1559241935 5,673,395 870,724 928 18,056 0 £251,540 75031,505 8,564,855 9,331,530 6,593,405 4,709,592 82,145 251,908 2,902,609 6,414,631 4,441,940 5,254,490 3,891,212 2,146,677 928,350 853 0 993,117 672,611 3615133 0 0 0 0 22,912 132756 0 18,057 0 427 52 0 0 18,675 85 0 ii | 0 0 0 0 9071 0 0 0 0 0 0 0 0 0 0 0 0 0 0 4514 9028 90,283 18,057 43 0 48 213 14,987,732 25,083,530 37,079,401 23,701,728 1,290,568 10,757,467 2,071,107 150,862 0 192 299 0 0) 0 0 0 395953 12,634 186,958 55,493 768 341 0 0 1263397 54,234 288,907 180,567 63,284 208,333 80 4099 0 21 0 0 0 0 0 0 0 0 1664 0 128 0 0 0 0 256 e709 95,446 1323 0 2 0 448 832 832 46,282 118,307 2603 16,992 49,763 525218 0 0 27,085 TT, 54,170 16,928 63,433 198,568 67,785 355,751 404,873 256,037 265,447 34,032 154,186 66,646 9600 46,780 317,562 712,133 8021 437 405 0 0 0 0 0 112,487 6485 2112 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 $6,113 0 384 0 0 0 0 0 0 0 583,616 15295370 252,869 597 0 0 0 0 63,198 0 341 77,082 T2376 162,851 110,900 580,928 361,133 O15 07 DHT 1280 18,057 0 0 0 0 0 0 235 341 0 144,453 306,963 184,151 1,594,264 188,460 217;399 0 0 0 0 0 0 0 0 128 9178 135,425 S97 299 1024 0 0 18,057 0 0 0 384 0 0 0 18,057 0 0 4949 383,115 1,119,844 125,264 112,876 0 Joa 0 0 0 0 0 0 63,198 58,684 18,057 7d 0 341 0 0 0 0 0 4779 0 0 0 0 0 Nig 0 0 0 0 0 0 176,053 361,389 487,701 397,247 297,935 2,058,442 164,761 es er eS 0 0 0 0 0 0 0 0 10,197 10,603 G3, 95d 88,832 153,583 55,808 599 1792 0 0 0 0 0 0 0 0 278 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Table 1.—Continued. Mar Apr May Jun Scenedesmus bijugus Turpin Lager. 20,096 2343 0 37,685 Scenedesmus dimorphus (Turpin) Kutzing 0 0 0 85 Scenedesmus quadricaudus (Turpin) Brébisson 9625 40,405 27,276 196,406 Scenedesmus sp. 85 11,285 4530 18,398 Selenastrum gracile Reinsch 0 0 0 0 Staurastrum americanum (West & West) G. M. Smith 0 0 11 0 Staurastrum leptocladum var. insigne West & West 0 0 80 3008 Staurastrum paradoxum Meyen 0 0 11 341 Staurastrum sp. 0 a7 43 117 Tetraedron minimum (Braun) Hansgirg 64 580 21 102,122 Chlorophyceans (unid.) 171 16,928 136,549 650,038 subtotal 2,462,904 975,313 766,468 4,567,024 Cryptophyceae Cryptomonas sp. 825,700 1,816,905 1,271,836 554,242 subtotal 825,700 1,816,905 1,271,836 554,242 Other taxa micro-phytoflagellates <10 um 47,637 0 0 175,407 micro-phytoflagellates > 10 wm 0 0 8215 43,810 small green spheres (<3 um) 18,320,895 3,792,191 3,348,778 9,835,356 small green spheres (3—5 wm) 4,786,425 470,241 262,864 675,405 small green spheres (5—10 um) 997,156 131,192 84.883 115,001 subtotal 24,152,113 4,393,624 3,704,740 10,844,979 Total 31,669,783 11,136,971 869,542 19,715,028 Literature Cited Adrian, G. L., C. Throckmorton, & R. McDonald. 1970. A study of primary production in a Ne- braska Interstate 80 lake.— Transactions of the Kansas Academy of Science 73(2):227—236. Anonymous. 1972. Water quality criteria. A report of the Committee on Water Quality Criteria. — National Academy of Science and National Academy of Engineering. Washington, D.C., 219 pp. Beck, W. M., Jr. 1973. Building an amphitheater and costing ramp of municipal solid waste. U.S. En- vironmental Protection Agency. SW-52d.of. Of- fice of Solid Waste Programs Vol. I and II. Washington, D.C., 265 pp. Cocke, G. R. 1973. A comparative limnological sur- vey of a brackish water lake and freshwater lake at Mount Trashmore, Virginia Beach, Virginia. Masters Thesis. Old Dominion University, Norfolk, Virginia, 120 pp. Holmes, R. W. 1970. The secchi disk in turbid coastal waters. — Limnology and Oceanography 15:688- 694. Lipsey, L.L. 1980. Phytoplankton of selected borrow pit ponds in northern Illinois.— Ohio Journal of Science 80(3):108-113. Marshall, H.G. 1979. Lake Drummond: With a dis- cussion regarding its plankton composition. Pp. 169-182 in P. W. Kirk, ed., The Great Dismal Swamp. University Press, Charlottesville, Vir- ginia. McCarraher, D. B., R. McDonald, & G. Adrian. 1974. Some hydrobiological characteristics of Inter- state-80 highway lakes in Nebraska.—Trans- actions of the Kansas Academy of Science 77(2): 93-102. Simmons, G. M., & S. E. Neff. 1974. Observations on limnetic carbon assimilation rates in Moun- tain Lake, Virginia during its thermal stratifi- cation periods.— Virginia Journal of Science 24(4):206—-211. VOLUME 102, NUMBER 1 Table 1.—Continued. Jul Aug Sep Oct Nov Dec Jan Feb 388,218 173,006 439,333 507,080 257,401 15,104 299 1365 128 341 72,483 683 0 1024 0 0 193,623 55,109 218,088 361-133" ~ 352505202 326,042 84,234 198,623 49,656 0 0 153,482 35,455 270,847 0 0 0 0 21,662 128 0 0 0 0 0 0 0 0 0 981 0 64 555 2688 1536 1621 1579 512 16 0 128 1152 1314 724 384 256 0 64 13,628 85 0 0 0 0 32 0 (Peps | 148,968 2305223 252-193 99,696 622,950 ZIV SS ZAG? 1,060,829 S72 34" 3.954 410) 213975150. ~. 1,932,063). 3,186,975 354,349 442,388 Pee NO2 [887,651 5,982,435 . 24,376,822 4,752,529 11,915,805 1,232,874 1,315,247 306,963 446,903 979,574 451,417 486,558 1,733,426 822,677 1,584,473 306,963 446,903 979,574 451,417 486,558 1,733,426 822,677 1,584,473 81,255 279,878 419,818 343,077 379,190 442,385 144,448 18,057 1535 1535393 0 0 591,435 219,050 240,959 503,816 14,763,970 14,238,250 18,641,155 13,708,148 16,143,985 56,011,283 5,542,049 12,748,730 1,171,918 104,048 3,066,790 1,533,350 1,555,255 3,986,723 3933223 6Go75151 328,575 394,290 6,900,008 635,245 240,955 876,203 35,596 120,478 16,361,053 16,106,241 22,817,681 16,219,820 18,910,820 61,535,644 6,316,275 14,048,232 34,306,660 44,214,844 69,068,298 66,512,801 39,870,929 95,777,761 11,461,481 22,775,746 Virginia State Water Control Board. 1982. Classifi- Department of Biological Sciences, Old cation and Priority Listing of Virginia Lakes. U.S. Environmental Protection Agency. S- 003219-010. Richmond, Virginia, 727 pp. 29 Dominion University, Norfolk, Virginia 23529. 280 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON INTERNATIONAL COMMISSION ON ZOOLOGICAL NOMENCLATURE % British Museum (Natural History) Cromwell Road London, SW7 5BD 23 September 1988 The following applications were published on 23 September 1988 in Vol. 45, Part 3 of the Bulletin of Zoological Nomenclature. Comment or advice on these appli- cations is invited for publication in the Bulletin and should be sent to the Executive Secretary, ICZN, British Museum (Natural History), Cromwell Road, London SW7 SBD, U.K. Case No. 2449 Septotrochammina Zheng, 1979 (Foraminiferida): proposed designation of Remaneica gonzalezi Seiglie, 1964 as the type species. 2622 Pleuromma princeps Scott, 1894 (currently Gaussia princeps; Crustacea, Co- pepoda): proposed conservation of the specific name. 2568 ACRIDIDAE Karny, 1907, OEDIPODIDAE Walker, 1870 and LOCUSTIDAE La- treille, 1802 (Insecta, Orthoptera): proposed order of precedence. 2618 Bruchus Linnaeus, 1767, Ptinus Linnaeus, 1767 and Mylabris Fabricius, 1775 (Insecta, Coleoptera): proposed conservation. 2627 Coryphium angusticolle Stephens, 1834 (Insecta, Coleoptera): proposed con- servation of both the generic and specific names. 2632 Tachina orbata Wiedemann, 1830 (currently Peribaea orbata; Insecta, Dip- tera): proposed confirmation of neotype designation. 2628 Tenthredo zonula Klug, 1817 (Insecta, Hymenoptera): proposed conservation of the specific name. 2625 Saccopharynx Mitchill, 1824 (Osteichthyes, Saccopharyngiformes): proposed conservation. 2616 ICHTHYOPHIIDAE Taylor, 1968 (Amphibia, Gymnophiona): proposed con- servation. 2650 Thorius pennatulus Cope, 1869 (Amphibia, Caudata): proposed conservation of the specific name. 2441 Semioptera wallacii Gray, 1859 (Aves, Paradisaeidae): proposed confirma- tion as the correct spelling. 2640 Mus musculus domesticus Schwarz & Schwarz, 1943 (Mammalia, Rodentia): proposed conservation. J. D. D. SMITH Scientific Administrator VOLUME 102, NUMBER 1 281 INTERNATIONAL COMMISSION OF ZOOLOGICAL NOMENCLATURE % British Museum (Natural History) Cromwell Road London, SW7 5BD 23 September 1988 The following Opinions were published on 23 September 1988 in Vol. 45, Part 3 of the Bulletin of Zoological Nomenclature. Opinion No. 1501 Alveolina d@Orbigny, 1826 (Foraminiferida): Oryzaria boscii Defrance in Bronn, 1825 designated as the type species. 1502 Conus fergusoni G. B. Sowerby III, 1873 (Mollusca, Gastropoda): specific name conserved. 1503 PSEUDOCALANIDAE Sars, 1901 (Crustacea, Copepoda): not to be given pre- cedence over CLAUSOCALANIDAE Giesbrecht, 1892. 1504 BERYTIDAE Fieber, [1851] and Berytinus Kirkaldy, 1900 (Insecta, Heterop- tera): conserved. 1505 Sigara scholtzi Fieber, [1860] (currently Micronecta (Dichaetonecta) scholtzi; Insecta, Heteroptera): specific name conserved. 1506 Oncomera Stephens, 1829 (Insecta, Coleoptera): Dryops femorata Fabricius, 1792 designated as the type species. 1507 Musca marginalis Wiedemann, 1830 (currently Chrysomya marginalis; In- secta, Diptera): specific name conserved. 1508 Simulium austeni Edwards, 1915 (Insecta, Diptera): not to be given prece- dence over Simulium posticatum Meigen, 1838. 1509 Paraphytomyza Enderlein, 1936 (Insecta, Diptera): Phytagromyza luteo- scutellata de Meiere, 1924 designated as the type species. 1510 Microgaster Latreille, 1804 (Insects, Hymenoptera): Microgaster australis Thomson, 1895 deisgnated at the type species. 1511 Halictus costulatus Kriechbaumer, 1873 (currently Lasioglossum costulatum; Insecta, Hymenoptera): specific name conserved. 1512 Desorella Cotteau, 1855 (Echinodermata, Echinoidea): confirmation of Hy- boclypus elatus Desor, 1847 as the type species. 1513. Synapturanus Carvalho, 1954 (Amphibia, Anura): Synapturanus miranda- riberoi Nelson & Lescure, 1975 designated as the type species. 1514 Liasis Gray, 1842 (Reptilia, Serpentes): Liasis mackloti Duméril & Bibron, 1844 designated as the type species. 1515 LARIDAE Rafinesque Schmaltz, 1815 (Aves) and LARINI LeConte, 1861 (In- secta, Coleoptera): homonymy removed. 1516 Taeniolabis Cope, 1882 (Mammalia, Multituberculata): Polymastodon taoensis Cope, 1882 designated as the type species. 1517 Viverravus gracilis Marsh, 1872 (Mammalia, Carnivora): generic and specific names conserved. 282 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON REVIEWERS The following people reviewed manuscripts for the Proceedings in 1988. A. Alvarino, M. V. Angel, F. M. Bayer, B. Bieri, R. Birdsong, J. A. Blake, T. Bongers, J. Bouillon, T. E. Bowman, R. O. Brinkhurst, B. Brown, S. D. Cairns, D. R. Calder, R. Castro, F. L. Chace, Jr., L. L. Cole, B. B. Collette, P. F. S. Cornelius, R. F. Cressey, A. Crosnier, D. Davis, G. M. Davis, H. DeWitt, M. Dojiri, S. Edmonds, D. J. Eernisse, C. Ehrlich, K. Fauchald, K. Fitzhugh, V. A. Funk, A. L. Gardner, S. Gelder, I. M. Goodbody, T. M. Gosliner, G. R. Graves, K. Green, M. Harasewych, E. Harrison-Nelson, C. W. Hart, Jr., W. R. Heyer, H. H. Hobbs, Jr., W. D. Hope, J. Iverson, S. C. Jameson, B. F. Kensley, L. S. Kornicker, J. D. Kudenov, K. Kuroda, D. B. Lellinger, R. J. L. Lester, M. S. Loden, J. Lynch, W. G. Lyons, N. J. Maciolek, R. B. Manning, J. W. Martin, R. W. McDiarmid, J. H. McLean, M. Milligan, G. C. Mitchell, R. F. Modlin, R. J. Mooi, T. A. Munroe, A. T. Newberry, R. T. O’Grady, S. L. Olson, L. Parenti, K. Parks, D. L. Pawson, T. H. Perkins, M. H. Pettibone, W. L. Pratt, J. W. Reid, M. E. Rice, M. Robbins, C. R. Robins, W. Rudman, D. E. Russell, J. M. Savage, V. G. Springer, W. C. Starnes, M. Stiassny, F. G. Thompson, D. A. Thoney, R. P. Vari, M. Vecchione, T. C. Walter, L. Watling, S. H. Weitzman, M. J. Wetzel, A. B. Williams, S. Williams, R. Winterbottom, J. J. Wurdack, R. Zottoli, G. R. Zug, R. L. Zusi. B, Conint, #, ox » ) a4 WwW “ew iyvis/ O. he < «2 oS L.A. Maange pantcetapny At H, Proihe AO MeRaone, cheek. Yee De Raves INFORMATION FOR CONTRIBUTORS Content.—The Proceedings of the Biological Society of Washington contains papers bearing on systematics in the biological sciences (botany, zoology, and paleontology), and notices of business transacted at meetings of the Society. Except at the direction of the Council, only manuscripts by Society members will be accepted. Papers are published in English (except for Latin diagnoses/descriptions of plant taxa), with a summary in an alternate language when appropriate. Submission of manuscripts. —Submit manuscripts to the Editor, Proceedings of the Biological Society of Washington, National Museum of Natural History NHB-108, Smithsonian Insti- tution, Washington, D.C. 20560. 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Clarity of presentation, and requirements of taxonomic and nomenclatural procedures ne- cessitate reasonable consistency in the organization of papers. Telegraphic style is required for descriptions and diagnoses. Literature citations in the text should be in abbreviated style (author, date, page), except in botanical synonymies, with unabbreviated citations of journals and books in the Literature Cited sections. Direct quotations in the text must be accompanied by author, date, and pagination. The establishment of new taxa must conform with the requirements of the appropriate international codes of nomenclature. When appropriate, accounts of new taxa must cite a type specimen deposited in an institutional collection. Examples of journal and book citations: Eigenmann, C.H. 1915. The Cheirodontidae, a subfamily of minute characid fishes of South America.— Memoirs of the Carnegie Museum 7(1):1—-99. Ridgely, R. S. 1976. A guide to the birds of Panama. Princeton, New Jersey, Princeton University Press, 354 pp. Olson, S. L. 1973. The fossil record of birds. Pp. 79-238 in D. Farner, J. King, and K. Parkes, eds., Avian biology, volume 8. Academic Press, New York. Figures and tables with their legends and headings should be self-explanatory, not requiring reference to the text. Indicate figure and table placement in pencil in the margin of the manu- script. Plan illustrations in proportions that will efficiently use space on the type bed of the Proceedings. Original illustrations should not exceed 15 x 24 inches. Figures requiring solid black backgrounds should be indicated as such when the manuscript is submitted, but should not be masked. CONTENTS Paleontological type specimens in the Santa Barbara Museum of Natural History Scott E. Miller A new generic name for Tate’s (1933) Microtarsus group of South American mouse opossums (Marsupialia: Didelphidae) Alfred L. Gardner and G. Ken Creighton Description of a rock-dwelling cichlid (Teleostei: Cichlidae) from Lake Malawi, Africa J. R. Stauffer, Jr. and J. M. Boltz Ascidians collected around the Galapogos Islands using the Johnson-Sea-Link research sub- mersible Claude Monniot and Francoise Monniot Eukrohnia calliops, a new species of Chaetognatha from the northern Gulf of Mexico with notes on related species Jerry A. McLelland Smalleyus tricristatus, new genus, new species, and Pseudothelphusa parabelliana, new species (Brachyura: Pseudothelphusidae) from Los Tuxtlas, Veracruz, México Fernando Alvarez Two new genera and nine new species of geryonid crabs (Crustacea, Decapoda, Geryonidae) Raymond B. Manning and L. B. Holthuis Synalpheus arostris and Philocheras lapillus, two new species of caridean shrimp (Crustacea) from the tropical eastern Pacific Mary K. Wicksten The holotype of Heterocarpus alexandri A. Milne-Edwards (Crustacea: Decapoda: Pandalidae) Fenner A. Chace, Jr. Gammaropsis Ee a new species of marine Amphipoda (Crustacea) from Jamaica James Darwin Thomas and J. L. Barnard Natatolana pastorei (Giambiagi, 1925) (Crustacea, Isopoda, Cirolanidae) from the Straits of Magellan, South America: Redescription and notes on functional morphology Johann Wolfgang Wagele and Niel L. Bruce Neobrachiella anisotremi (Copepoda: Lernaeopodidae), a new species parasitic on an inshore fish, Anisotremus scapularis, off the Chilean coast Raul Castro Romero and Hernan Baeza Kuroki The First Annual Riser Lecture: Meiofauna and Microbes—the interactive relations of annelid hosts with their symbiotic bacteria Olav Giere Revision of the family Lysaretidae, and recognition of the family Oenonidae Kinberg, 1865 (Eunicida: Polychaeta) G. Kent Colbath Redescription of Nephtys squamosa Ehlers (Polychaeta: Nephtyidae) Takashi Ohwada Phallodrilus hessleri, new species (Oligochaeta: Tubificidae) from abyssal depths in the western Pacific Ocean Christer Erséus Phallodrilus vescus, new species (Oligochaeta, Tubificidae) from the Gulf of Mexico Christer Erséus New species of scale-worms (Polychaeta: Polynoidae) from ee hydrothermal rift-area of the Mariana Back-Arc Basin in the western central Pacific Marian H. Pettibone Polynoidae and Sigalionidae (Polychaeta) from the Guaymas Basin, with descriptions of two new species, and additional records from hydrothermal vents of the Galapagos Rift, 21°N, and seep-sites in the Gulf of Mexico (Florida and Louisiana) Marian H. Pettibone A new eulimid gastropod, Trochostilifer eucidaricola, parasitic on the pencil urchin Eucidaris tribuloides from the southern Caribbean Anders Warén and Robert Moolenbeek Springsnails (Gastropoda: Hydrobiidae) of Owens and Amargosa River (exclusive of Ash Meadows) drainages, Death Valley System, California-Nevada Robert Hershler Four new species of free-living marine nematodes in the genus Pareurystomina (Nematoda: Enoplida) with observations on other members of the genus Edwin J. Keppner Neotropical Monogenea. 14. Revision of Callorhynchocotyle Suriano and Incorvaia, 1982 (Hexabothriidae) with the description of C. amatoi Walter A. Boeger, Delane C. Kritsky, and Joaber Pereira, Jr. Phytoplankton composition in a borrow pit lake in Virginia Seba B. Sheavly and Harold G. Marshall International Commission on Zoological Nomenclature: Applications and Opinions Reviewers— 1988 1 106 109 116 124 131 134 137 154 169 176 249 264 272 / 280 282 THE BIOLOGICAL SOCIETY OF WASHINGTON 1988-1989 Officers President: Kristian Fauchald Secretary: G. David Johnson President-elect: Leslie W. Knapp Treasurer: Don E. Wilson Elected Council Gary R. Graves Meredith L. Jones W. Ronald Heyer Raymond B. Manning W. Duane Hope Wayne N. Mathis Custodian of Publications: David L. Pawson PROCEEDINGS Editor: C. Brian Robbins Associate Editors Classical Languages: George C. Steyskal Invertebrates: Stephen D. Cairns Frank D. Ferrari Plants: David B. Lellinger Raymond B. Manning Insects: Wayne N. Mathis Vertebrates: G. David Johnson Membership in the Society is open to anyone who wishes to join. There are no prerequisites. Annual dues of $15.00 ($20.00 to non-USA addresses) include subscription to the Proceedings of the Biological Society of Washington. Library subscriptions to the Proceedings are: $25.00 within the U.S.A., $30.00 elsewhere. The Proceedings of the Biological Society of Washington (USPS 404-750) is issued quarterly. Back issues of the Proceedings and the Bulletin of the Biological Society of Washington (issued sporadically) are available. Correspondence dealing with membership and subscriptions should be sent to The Treasurer, Biological Society of Washington, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560. Manuscripts, corrected proofs, editorial questions should be sent to the Editor, Biological Society of Washington, National Museum of Natural History, Smithsonian Institution, Wash- ington, D.C. 20560. Known office of publication: National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560. Printed for the Society by Allen Press, Inc., Lawrence, Kansas 66044 Second class postage paid at Washington, D.C., and additional mailing office. POSTMASTER: Send address changes to PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON, National Museum of Natural History, Washington, D.C. 20560. THIS PUBLICATION IS PRINTED ON ACID-FREE PAPER. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 283-299 A REVISION OF ARABELLA MUTANS (CHAMBERLIN, 1919) AND RELATED SPECIES (POLYCHAETA: ARABELLIDAE) G. Kent Colbath Abstract. — Arabella mutans (Chamberlin, 1919), previously considered cir- cumtropical in distribution, is revised using a combination of soft-part, setal, and maxillary characters. Emphasis is placed on adopting a population ap- proach to evaluating character states. Poorly preserved, isolated, or juvenile individuals may not be identifiable to species based on the criteria advocated here. Seven species with non-overlapping geographic ranges are recognized. Arabella mutans s. s. is restricted to tropical Polynesia. Arabella novecrinita Crossland, 1924 is recorded from the western Indian Ocean. Arabella logani Crossland, 1924 and A. atlantica Crossland, 1924 are recognized as distinct species, and recorded from the Red Sea and Cape Verde Islands, respectively. Arabella multidentata (Ehlers, 1887) is recognized to encompass western At- lantic and Carribean forms. Two new species are erected: Arabella panamensis for specimens from Pacific Panama, and A. monroi from the Galapagos. The genus Arabella is distributed throughout the world ocean, and includes 20 named species (Fauchald 1977b). Many of these species are relatively rare, and have not been satisfactorily circumscribed in terms of either morphology or distribution. Arabella mutans (Chamberlin, 1919) is one such species. Although A. mutans is re- ported to have a circumtropical distribution (Monro 1928, 1933a, b; Day 1967; Reish 1968; Gardiner 1976), this assertion has not been supported by detailed morphological comparisons of specimens (Fauchald 1970). The present study attempts to partially re- dress this situation by presenting informa- tion compiled from the detailed examina- tion of numerous specimens, including the holotypes of both A. mutans and the similar A. novecrinita Crossland, 1924. From a paleontological perspective, Ar- abella mutans is of interest because of the wide range of jaw morphologies which have been recorded for the species. Establishing constraints on the amount of variation in jaw morphology that can be expected within modern species should aid in the interpre- tation of fossil jaw assemblages. History of Study Chamberlin (1919:329-—332) described the new genus and species Cenothrix mutans based on a single specimen collected from Easter Island by the Albatross Expedition. He distinguished the genus Cenothrix from Arabella Grube, 1850 on the presence of a ventral, hooded seta in medial and posterior parapodia in the former, and the supposed absence of such setae in the latter. The new species was distinguished on the same taxo- nomic character. Crossland (1924:70) considered the pres- ence ofa single hooded seta per parapodium insufficient grounds for recognition of a new genus, and transferred C. mutans into Ar- abella. He described the new species Ara- bella novecrinita based on 16 specimens from the Atlantic and Indian Oceans, and noted that A. novecrinita “*... is like, and probably identical with A. (Cenothrix) mu- 284 tans,’ (Crossland 1924:71). Crossland ap- parently considered the jaws of the type specimen of A. mutans atypical, and justi- fied the erection of a new species on that basis. He recognized four varieties of A. no- vecrinita: the type material from Zanzibar and the Maldive Islands, A. novecrinita var. logani from the Red Sea, and A. n. var. atlantica and A. n. var. asymmetrica from the Cape Verde Islands. Monro (1928:91; 1933b:88) considered A. novecrinita a junior synonym of A. mu- tans, and considered the species circum- tropical in distribution. Monro essentially used Chamberlin’s specific name for spec- imens included within the range of variation described by Crossland. Subsequent work- ers prior to Orensanz (1974) followed Mon- ro, although Fauchald (1970:129) noted that Monro’s revision did not involve exami- nation of the type material of either species, and suggested that A. mutans, as considered by Monro, might actually include several species with more restricted distributions. Orensanz (1974:388) used Cenothrix as a subgenus of Arabella, and recognized three species within the subgenus, which he dis- tinguished based on their maxillary mor- phology. A. mutans was recognized for spec- imens with asymmetrical maxillae with falcate MI elements, A. asymmetrica for those with asymmetrical maxillae with a bi- fid left MI, and A. novecrinita for those with symmetrical maxillae. Perkins (1979:445—450) followed this ar- rangement and placed three species in Ar- abella (Cenothrix). He made the important observation that the type specimens of both Arabella multidentata (Ehlers, 1887) and A. maculosa Verrill, 1900 have ““hooded”’ ven- tral setae, and therefore should not be con- sidered junior synonyms of Arabella iricolor (Montagu, 1804) as proposed by Hartman (1944:173). Perkins distinguished A. mul- tidentata from A. mutans based on jaw sym- metry, and considered the two species sym- patric in the Florida region. He recognized PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON A. maculosa based on the extreme asym- metry of the “hoods” on the ventral setae on the type specimen from Bermuda. Materials and Methods The extensive collection of specimens catalogued as Arabella mutans in the U.S. National Museum of Natural History (USNM) was examined in its entirety, as were samples identified as Arabella novecri- nita. Additional material was obtained from the British Museum (Natural History) (=ZK), including Crossland’s type material for A. novecrinita. Selected specimens of Ar- abella iricolor from the National Museum collection and the Florida Department of Natural Resources (FSBC, EJ) were also ex- amined for comparative purposes. On each dissected specimen the lengths of the first maxillae (MIs), length and width of the prostomium, and length of the peri- stomium were measured. Measurements were made using an ocular micrometer on a Wild M5 wide-field microscope. Denticles were counted (where possible) for all max- illary jaws. Setae were prepared for scanning electron microscopy by allowing parapodia suspend- ed in alcohol to dry onto glass cover slips, which were in turn glued onto stubs. Jaws were mounted by leaving a flange of muscle tissue around the jaw margins which, when dried, fixed the jaws firmly onto glass cover slips. All specimens were coated with a thin film of carbon, then sputter coated with gold palladium. Observations were made on a Cambridge scanning electron microscope at the National Museum of Natural History, Smithsonian Institution. Taxonomic Characters Arabella mutans has been recognized by most authors based on the presence of a single morphologic character (the “hooded” ventral seta). Consideration of additional characters coupled with a closer examina- VOLUME 102, NUMBER 2 285 Table 1.— Distribution of taxonomic characters in species of Arabella under consideration. Nuchal Anal Postsetal Species papillae cirri lobe Ventral setae Maxillary symmetry Robust MI iricolor no 2 short ridged, gradual invariant bifid-falcate atlantica no 2 short ridged, abrupt invariant falcate logani no 0 short ridged, gradual ? absent monrol no 0 short ridged, abrupt invariant falcate multidentata no 4 short ridged, abrupt polymorphic bifid mutans no 4 short smooth, abrupt polymorphic dentate novecrinita no 4 short smooth, abrupt invariant absent panamensis no y, long ridged, abrupt polymorphic falcate sp. A yes @ short ridged, abrupt polymorphic bifid tion of the setae has allowed separation of discrete morphological subgroups, here rec- ognized as distinct species with discrete geo- graphic ranges. The taxonomic characters are discussed below, and the character states exhibited by each of the species are listed in Table 1. Soft-part morphology. —Soft-part mor- phology within the genus Arabella is noto- riously uniform and relatively simple, which accounts in part for the difficulty encoun- tered in treating these worms taxonomical- ly. The relative proportions of the prosto- mium are fairly uniform throughout the A. mutans species complex, and the ventral furrowing of the peristomium, although variable, does not seem to vary in a system- atic fashion. There are three features which are useful in differentiating these species, however. The postsetal lobe in parapodia from A. pana- mensis, N. sp. is markedly longer than that in the other species. Nuchal papillae are present in some large individuals from Guayanilla Bay, Puerto Rico, a unique feature in the arabellids. The specimens are from a population of other- wise identical worms which lack papillae, however, and the taxonomic significance of this character is unclear. The morphology of the pygidium is an extremely useful character, limited only by the difficulty of obtaining complete speci- mens. Species are characterized by having two anal cirri (Fig. 3b, f), four anal cirri (Fig. 3c, d), or two swollen pads lacking cirri (Fig. Base): Setae.—The most important point to emerge from SEM examination of the setae from the specimens studied here is that the “*hooded”’ ventral seta in medial and pos- terior parapodia used to define A. mutans is not hooded (in the sense of having a three dimensional structure enclosing the distal end of the seta). In all specimens examined, the distal end of the ventral seta consists of a relatively flat extension of the setal shaft. Although the diameter of the ventral seta is generally twice that of the other setae in these forms, it originates in the same mus- cular bundle, and is not an acicula as re- corded by some authors. The modification of the distal end of the ventral seta is dif- ferent only in degree, not in structure, from that observed in the ventral setae of Ara- bella iricolor. This observation strongly sup- ports Crossland’s (1924) contention that Cenothrix Chamberlin should be regarded as a junior synonym of Arabella. The terminology adopted here to describe the ventral setae is illustrated in Fig. 1. Three distinct morphologies are recognized. The shaft of the seta may be smooth with an abrupt taper from the shaft to the guard, ridged with an abrupt taper from the shaft to the guard, or ridged with a gradual taper 286 shaft Pee SE ridge Fig. 1. from the shaft to the guard. Arabella pan- amensis, n. sp. has ventral setae which are somewhat modified from the second type above in having an additional ridge near the tip of the shaft (Fig. 3h). SEM examination of the other setae re- veals that the distinction between smooth and “‘toothed”’ geniculate setae made by both Chamberlin (1919) and Crossland (1924) is indeed significant. The “‘toothed”’ setae are not actually toothed, however, but are in- stead ringed with loose rows of large fibrils, in contrast to the tight, irregular arrange- ment of fibrils in the smooth setae (Fig. 4k, 1). Jaws. — Maxillary jaws in eunicoid poly- chaetes are numbered, by convention, from posterior to anterior with roman numerals. Left and right jaws are indicated by a capital L or R respectively. Thus MIR refers to the posterior maxilla on the right side of the apparatus. Denticle formulas are indicated in sequence, with the left jaw in a given pair listed first. For populations, the low end of the range of denticles for a given jaw is listed first, with the high end of the range in pa- rentheses. Maxillae within some of the species are here considered polymorphic, but variation within single populations is limited to two or three morphs. The first and second max- illae (MI and MII) were found to be the most significant in differentiating species. The morphs recognized here are illustrated in Fig. 2. The MII jaws may be either “‘long,”’ PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ao ert guard Terminology used to describe morphology of the ventral seta in medial and posterior parapodia. extending posteriorly to the base of the MI, or “‘short,’’ extending posteriorly only half of the distance to the base of the MI (Fig. 2a, b). A long MII is invariably associated with a relatively slender MI (here termed “‘sracile’’) with a single falx (or hook) and a pronounced gap between the falx and the basal denticle row (Fig. 2e). MIs adjacent to short MIIs are wider and generally slight- ly longer than the gracile MIs, and are here termed “‘robust.’’ They may take one of three forms in adult worms. These jaws may have a single falx with pronounced gap (=“‘fal- cate,’ Fig. 2c), a bifid falx with pronounced gap (=“‘bifid,’’ Fig. 2d), or no distinct falx and no gap (=“‘dentate,”’ Fig. 2f). Dentate MIs are found in juvenile specimens of a number of different species, but in the ju- veniles with dentate MIs the anterior den- ticles project laterally rather than dorsally as in the adults (compare Fig. 4c, d). The statistical frequency of these jaw morphologies varies systematically among different populations of worms, and in most cases only one of the three morphologies of robust MIs is represented (if any). The pres- ence or absence of jaw symmetry polymor- phism within a population is also a useful taxonomic character. Within the species considered here, the lengths of MIs are highly correlated with the sizes of individual worms as measured by prostomial width (Fig. 7). A plot of MI length against prostomial width is similar for most of these species, with the exception of Ar- VOLUME 102, NUMBER 2 4 ial 287 e f Fig. 2. Schematic representation of morphologies observed in first and second maxillae. a, short MII; b, long MII; c, falcate robust MI; d, bifid robust MI; e, gracile falcate MI; f, dentate robust MI. abella panamensis. In A. panamensis indi- viduals have relatively large jaws for their size. The number of denticles on a given max- illa is variable, and has generally been dis- counted as a useful taxonomic character in eunicoid polychaetes (Kielan-Jaworowska 1966, Wolf 1980). With sufficient speci- mens, however, it may be possible to use the number of denticles on a statistical basis (see below under Arabella multidentata). The shape of the mandibles exhibits with- in-sample variation in these forms (Cross- land 1924), but proved of no value in dis- tinguishing species. A typical mandible is illustrated in Fig. 5b. Order Eunicida Fauchald, 1977 Family Arabellidae Hartman, 1944 Genus Arabella Grube, 1850 Arabella Grube, 1850:17. Notopsilus Ehlers, 1868:406. Maclovia Grube, 1871:58. Cenothrix Chamberlin, 1919:329. Type species. — Arabella iricolor (Monta- gu, 1804). Remarks. —Fauchald (1977b:110-11) noted that generic diagnoses within the Ar- abellidae are inconsistent. In forms with projecting acicular spines, the shape of the ML is used to separate the genus Drilonereis Claparede (falcate MIs) from WNotocirrus Schmarda (dentate MIs), while the genus Arabella (which lacks emergent acicular spines) includes forms with both maxillary morphologies. Fauchald suggested that either the genus Notopsilus Ehlers be rec- ognized to include species with dentate MIs which are presently placed in Arabella, or that Drilonereis and Notocirrus be consid- ered synonymous. The report here of species in which the jaws are polymorphic (including both den- tate and falcate MIs) strongly suggests that Notopsilus should be considered a junior synonym of Arabella. This does not imply, however, that Drilonereis and Notocirrus should also be considered synonymous. The basic arrangement of jaws is quite different in Drilonereis than it is in Notocirrus, and intermediate or hybrid maxillae have not been recorded. Arabella iricolor (Montagu, 1804) Figs. 3b, 4j, k, 5a, 6a Nereis iricolor Montagu, 1804. Arabella iricolor. — Pettibone, 1963:269, fig. 288 ee Big. 3. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON al h a, Arabella logani, holotype, ZK 1924.3.1.15, pygidium, left-lateral view; b, Arabella iricolor, USNM 61732, pygidium, right-lateral view; c, Arabella novecrinita, lectotype, ZK 1924.3.1.15, pygidium, dorsal view; d, Arabella mutans, USNM 57434, pygidium, oblique right-lateral view; e, Arabella monroi, holotype, ZK 1932.12.24.595, pygidium, right-lateral view; f-—h, Arabella panamensis, USNM 98237, holotype; f, pygidium, dorsal oblique right-lateral view; g, posterior parapodium, anterior view, note elongate post-setal lobe; h, ventral seta of parapodium in g, note 2 ridges, abrupt taper of shaft; i, Arabella sp. A, USNM 54915, anterior end with pharynx extended, lateral view, note nuchal papillae. Scale bars on a-f, i = 0.5 mm; g = 0.2 mm; h = 20 um. 7la—e; Gardiner, 1976:206-—207, figs. 27r—u, 28a; Uebelacker, 1984:42-5, fig. 42-2. Materials examined. —USNM 30058, FSBC I 24159, Seashore Key, Florida (6); FSBCI 13436, Terra Ceia Bay, Florida (1).— FSBC I 13102, Lower Tampa Bay, Florida (1).—EJ-72-66, EJ-73-414, Hutchinson Is- land, Florida (3).—USNM 61732, USNM 53026, Cape Lookout, North Carolina (11).—USNM 4676, Woods Hole, Massa- chusetts (7).—USNM 33787, Province- town, Massachusetts (8). Remarks.—The specimens of Arabella iricolor examined here are characterized by having ventral setae in medial and posterior parapodia which are ridged, with a gradu- ally tapering shaft (Fig. 4j). The pygidium has two cirri which arise dorsally (Fig. 3b). No variation in jaw symmetry was observed among adult specimens. In each individual the MIL is robust with a short MIIL, the MIR gracile with a long MIIR. The Florida specimens differ from those from North Carolina and Massachusetts in that all adult worms have falcate robust MIs VOLUME 102, NUMBER 2 289 Fig. 4. Setae, all in anterior view. a, b, Arabella monroi, ZK 1932.12.24.337-340, paratype, large anterior fragment, ventral seta, setiger 143, note ridge, abrupt taper of shaft. c, Arabella novecrinita, ZK 1924.3.1.15, lectotype, ventral seta, setiger 200, note smooth, abruptly tapered shaft. d, Arabella mutans, USNM 23933, ventral seta, posterior setiger, note smooth, abruptly tapered shaft. e, Arabella mutans, USNM 57434, ventral seta, posterior setiger, dorsal to bottom of page, note smooth, abruptly tapered shaft. f, Arabella atlantica, ZK 1923.11.5.1-2, large syntype, ventral seta, setiger 122, note ridge, abrupt taper. g, h, Arabella logani, ZK 1924.3.1.15, holotype, ventral seta, setiger 125, note ridge, gradually tapered shaft. i, Arabella multidentata, USNM 98154, ventral seta, posterior setiger, note ridge, abruptly tapered shaft. j, k, Arabella iricolor, USNM 30058 (Florida); j, ventral seta, posterior setiger, note ridge, gradually tapered shaft; k, ““smooth” seta, posterior setiger. 1, Arabella sp. A, USNM 54915, posterior setiger, smooth seta above, toothed seta below. All scale bars = 5 um. 290 (n = 8), in contrast to the bifid robust mor- phology (Fig. 5a) observed in the northern populations (25 of 26 adult specimens). Jaw morphology in these populations is quite stable, as the jaws are essentially iden- tical in specimens collected from Woods Hole in 1883 (USNM 4676), Provincetown in 1954 (USNM 33787), and North Caro- lina in 1974 (USNM 53026) and 1975 (USNM 61732). Thus although the differ- ence between the Florida and northern populations is small, the stability of the character suggests that the difference is he- reditary, and may be used to subdivide east coast populations of A. iricolor. As presently recognized, A. iricolor is probably a species complex. Two juvenile specimens of A. iricolor from Florida have dentate MILs which resemble those in several other species of Arabella, including A. mutans (Fig. 5d). Arabella atlantica Crossland, 1924, new rank Fig. 4f Arabella novecrinita var. atlantica Cross- land, 1924:78—80, text-figs. 99-101, 105. Arabella novecrinita var. asymmetrica Crossland, 1924:80-83, text-figs. 102- 104. Syntypes. —ZK 1923.11.5.1-2, Cape Verde Islands, two anterior fragments. Materials examined.—ZK 1923.11.5.1- 2, Cape Verde Islands (two anterior frag- ments).—jaw mounts from six specimens from the Cape Verde Islands as follows: ZK 1923.11.8.12-14, three unregistered slides labelled CV Isl. W9; three unregistered jaw mounts of Arabella novecrinita var. asym- metrica, Cape Verde Islands. Remarks. —Crossland (1924:78) record- ed 11 specimens from the Cape Verde Is- lands. Three small specimens which exhibit maxillae typical of juveniles in the genus Arabella were assigned to Arabella nove- crinita var. asymmetrica (Crossland, 1924, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON text-fig. 103). These specimens are here re- garded as juveniles of Arabella atlantica. Of the remaining eight specimens, two anterior fragments and six sets of jaws are represented in the collection of the British Museum (Natural History). At present it is impossible to determine which sets of jaws belong to the two preserved specimens, and thus no lectotype is designated. The soft-part morphology of this species is adequately described by Crossland (1924: 78-80, text-fig. 99). The ventral setae are ridged, with an abrupt taper from the guard to the shaft (Fig. 4f). In the specimens avail- able for examination, the MIL is robust fal- cate, the MIIL short, and the MIR gracile falcate with a long MIIR. No symmetry polymorphism observed (n = 6). This species is distinguished from Ara- bella novecrinita by its ridged ventral setae and robust MIL. It differs from A. multi- dentata in having falcate rather than bifid robust MIs, and in not exhibiting symmetry polymorphism. A. atlantica most closely re- sembles A. monroi n. sp. from the Gala- pagos, but because neither preserved spec- imen of A. atlantica has an intact pygidium, it cannot be compared based on this im- portant character. Arabella logani Crossland, 1924, new rank Figs. 3a, 4g, h Arabella novecrinita var. logani Crossland, 1924:75-78, text-figs. 96-98. Holotype. —ZK 1924.3.1.138, Red Sea. Materials examined. —ZK 1924.3.1.138, Red Sea (1). Remarks. —The soft-part morphology of the type and only specimen is accurately described by Crossland (1924:75-76). Noteworthy is the presence of two inflated pads on the pygidium (Fig. 3a) which lack anal cirri. No evidence for incomplete re- generation is apparent, and this may rep- resent the fully developed character state. The ventral setae in posterior parapodia VOLUME 102, NUMBER 2 291 Fig. 5. a, Arabella iricolor, USNM 33787, maxillae, dorsal view, note bifid MIL. b—-d, Arabella mutans, USNM 23933; b, mandibles, ventral view; c, maxillae of adult specimen, dorsal view, note dentate MIR, falcate tip of MIL broken during mounting; d, maxillae of juvenile specimen, note dentate MIL with anterior denticles which project laterally. e, Arabella sp. A, USNM 54915, maxillae, dorsal view, example of symmetrical apparatus with 2 long MIIs, 2 gracile falcate MIs. f, Arabella panamensis, USNM 66043, paratype, maxillae, dorsal view, note falcate MIL, falcate tip of MIR broken during mounting. Scale bars on a-c, e, f = 100 um; d = 50 um. 292 are ridged and gradually tapering (Fig. 4g, h), and are thus unlike those in other species within the Arabella mutans complex. The MIL is robust bifid, the MIIL short, and the MIR gracile falcate with a long MIIR (note that Crossland reversed the image in text-fig. 96, and incorrectly labeled the spec- imen as a “Cape Verde specimen’’). The bifid MIL serves to distinguish this species from Arabella iricolor, which in the eastern Mediterranean and Red Sea has a falcate robust MIL (Ben-Eliahu 1976:172). No statement concerning jaw variability can be made based on a single specimen, and full characterization of the species must await further collecting. Arabella monroi, new species Figs. 3e, 4a, b Arabella mutans. —Monro 1933b:88-89 (in part). Holotype.—ZK 1932.12.24.595, washed from peat, Isla Santa Cruz (Indefatigable), Galapagos Islands. Etymology. —In honor of C. C. A. Monro. Materials examined. —Holotype; ZK 1932.12.337—340 (paratypes), washed from peat, Isla Santa Cruz (Indefatigable), Ga- lapagos Islands (26).—ZK 1932.12.336, fine gravel in pools, Isla Isabela (Albermarle), Galapagos Islands (1).—ZK 1932.12.341, Post Office Bay, Isla Santa Maria (Charles), Galapagos Islands (3). Description. —Prostomium bullet-shaped, slightly longer than wide to slightly wider than long, V-shaped furrow on ventral sur- face, four eyes embedded in posterior dorsal margin. Peristomium divided into two rings, a shallow ventral median furrow in anterior ring only. Setigers numerous, exceeding 200 in large, adult specimens. Notopodia represented by small tubercle, neuropodia with blunt, sub- triangular postsetal lobe. Pygidium with two swollen pads (Fig. 3e), no anal cirri ob- served. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Notoacicula small, 2—3 per setiger. Neu- roacicula large, amber colored, 3—4 per se- tiger with tips protruding slightly through parapodial wall. Anterior setigers with 5-6 setae, 3 being smooth, 2—3 toothed. Medial and posterior setigers with 2 smooth, 1 toothed, and 1 ventral seta. Ventral setae ridged, shaft tapering abruptly to distal guard (Fig. 4a, b). Mandibles H-shaped, typical of Arabella. Maxillae with 2 long carriers and unpaired ventral ligament (=“‘third carrier” of some authors). Maxillary apparatus asymmetri- cal, no symmetry polymorphism observed. MIL robust falcate, MIIL short, MIR gracile falcate, MIIR long. Denticle formula: 6(9)- 6(8); 7(8)-12(16); 5(6)-5(6); 4(5)-4; 1-1. Holotype large, complete individual with 208 setigers, prostomium 0.68 mm long, 0.55 mm wide, peristomium 0.54 mm long, MIL 0.36 mm long, MIR 0.35 mm long, denticle formula 9-8; 8-16; 6-6; 4-4; 1-1. Remarks.—The collection from the Ga- lapagos includes 13 complete specimens. None have anal cirri, and it seems likely that the presence of two pygidial lobes with no cirri represents the fully developed adult character state. Arabella monroi is distinguished from A. mutans based on its asymmetrical maxillae which are not polymorphic, falcate rather than dentate robust MIs, ridged rather than smooth ventral setae, and by the absence of anal cirri. It differs from A. multidentata in having falcate rather than bifid robust MIs, in not exhibiting symmetry polymorphism of the maxillae, and in lacking anal cirri. The maxillary apparatus in A. monroi is identical to that in A. atlantica. The pygid- ium in the latter species is unknown, how- ever, and I consider it prudent to describe the Galapagos specimens as a separate species pending collection of additional ma- terial from the type locality of A. atlantica. The geographic range of A. monrolis pres- ently restricted to the islands of the Gala- pagos. VOLUME 102, NUMBER 2 Arabella multidentata (Ehlers, 1887) Figs. 41, 6b, 7 Aracoda multidentata Ehlers, 1887:112, pl. 34, figs. 8-10, pl. 35, figs. 1-4. Arabella multidentata. —Hartman, 1938:12; Perkins, 1979:447-449, fig. 13; Uebe- lacker, 1984:42-9, figs. 42-5, 6a-g. Arabella maculosa Verrill, 1900:651.— Treadwell, 1921:114, pl. 9, figs. 12-13, text-figs. 424-428; Perkins, 1979:450, fig. 14. Arabella mutans. —Gardiner, 1976:206, figs. 270—q; Fauchald, 1977a:45 (in part); Per- kins, 1979:445-447, fig. 12; ?Duenas, 1981:193. Arabella novecrinita. —Monro, 1933a:260- 261: ?Arabella asymmetrica.—Orensanz, 1974: 368-388, fig. III-6. Holotype. —MCZ 825, Florida. Materials examined. -USNM 55882, Gulf of Mexico (1).—USNM 54694-54696, Hutchinson Island, Florida (3).—USNM 59526, N Atlantic off Florida (2); USNM 59528, N Atlantic off N Carolina (1).— USNM 56844, N Atlantic off Virginia (1).— USNM 98142-98156, Bermuda (22).— USNM 53297, 54215, 54220, 54221, 54223, 54818, 54820, 98238, Guayanilla Bay, Puerto Rico (22).—USNM 54217, 54218, 54222, 54837-54840, Jobos Bay, Puerto Rico (8).—USNM 66044-66046, 73653, Galeta Reef, Panama (5).—?USNM 58273, Bay of Cartagena, Colombia (1). Remarks.—Perkins (1979:448-449) ac- curately described the soft-part morphology of A. multidentata. To his description of the setae I add that the ventral setae are ridged and abruptly tapered (Fig. 41). Perkins (1979:450) distinguished Arabel- la maculosa Verrill, 1900 from A. multi- dentata based on the “more obviously asymmetrical’’ ventral setae in the syntype of the former. I found the degree of asym- metry variable on a single specimen, and was unable to separate the species on this 293 Table 2.— Distribution of specimens of Arabella with particular MI morphologies in polymorphic species. 1 gracile, Species 2 robust 1 robust 2 gracile multidentata Bermuda 1 9 8 Others 5 15 12 mutans 4 4 2 panamensis 3 2, _ sp. A — 4 2 basis. The syntype of A. maculosa has a regenerated pygidium with two poorly de- veloped lobes and no cirri (Perkins 1979, fig. 14a). Eight complete specimens from Bermuda, with no indication of posterior regeneration, have four anal cirri as 1s typ- ical of A. multidentata. The jaws of the Ber- muda specimens are indistinguishable from those of other west Atlantic and Caribbean populations of A. multidentata (Table 2), and I therefore consider A. maculosa a ju- nior synonym of A. multidentata. Perkins (1979:447) distinguished sym- patric Florida populations of A. multiden- tata from A. mutans based on jaw sym- metry. Instead, I recognize a single species (A. multidentata) with polymorphic jaw symmetry which is distinct from A. mutans. A. multidentata has bifid (25 of 27 adult specimens with robust elements, remaining 2 falcate) rather than dentate robust MI ele- ments (where present), and further differs from A. mutans in having ridged rather than smooth ventral setae. A comparison between A. multidentata and A. iricolor sensu Pettibone (1963) is par- ticularly instructive, as the geographic ranges of the two species overlap along the east coast of the United States. A. multidentata has abruptly tapering shafts on the ventral setae (Fig. 41), rather than gradually tapering shafts as in A. iricolor (Fig. 4j), 1s further characterized by having four rather than two anal cirri, and by having polymorphic max- illary symmetry. The number of denticles 294 30:..= 7s 20 a US: = Number of Jaws @) — Saco aeecccenaeaaaeoe renee = Gn? BLL oulO LAL 11s 1 S16 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 6 1728 Number of Denticles Fig. 6. Histograms of denticle number in MII jaws in Arabella iricolor (a) and Arabella multidentata (b). Note that the distinction between short and long MII elements is evident from the diagram. Means are indicated for long MIIs. in long MII elements overlaps between the two species (Fig. 6a, b), but the difference in means is highly significant (P < 0.001, t = 6.14). Dentate jaws were observed in four ju- venile specimens of A. multidentata. The juvenile dentition is indistinguishable from that in other species of Arabella. As defined here, Arabella multidentata is a west Atlantic species recorded from the east coast of the United States as far north as Virginia, from Bermuda, Puerto Rico, the Gulf of Mexico, Atlantic Panama, and ques- tionably from the Bay of Cartagena, Colom- bia (single specimen with falcate rather than bifid robust MIL). The specimens described by Orensanz (1974) as A. asymmetrica have maxillae identical to the present material, and ventral setae with abruptly tapered shafts. It’s unclear whether or not the ven- tral setae are ridged, however, and the py- gidium was undescribed. This attribution must therefore be considered tentative. Arabella mutans (Chamberlin, 1919) Figs. 3d, 4d, e, 5b—-d Cenothrix mutans Chamberlin, 1919:330- 332, pl. 61, figs. 2-9, pl. 62, fig. 1. Arabella mutans. —Crossland, 1924:71; Hartman, 1954:624; Reish, 1968:220; Kohn and Lloyd, 1973:699. Arabella novecrinita. —Hartman, 1954:625. Holotype. —USNM 19740, Easter Island. Materials examined. —-USNM 19740, 57434, Easter Island (2).—USNM 23933- 23935, Bikini Island (14). Remarks. —Chamberlin’s (1919:330, pl. 61, fig. 4) description of the anterior end of the holotype is accurate. The pygidium is poorly developed, and represents incom- plete regeneration. A second specimen from Easter Island (USNM 57434) has four anal cirri (Fig. 3d), as do two specimens from Bikini, and this is considered the fully de- veloped character state. As noted above, the hooded acicula (or VOLUME 102, NUMBER 2 ‘““crochets”) which Chamberlin (1919:331) originally described for this species are neli- ther hooded nor acicula, but rather are setae typical of the genus Arabella which have an abruptly tapering shaft. The shaft is smooth on ventral setae in the holotype, and on the other specimens examined (Fig. 4d, e). Chamberlin (1919:61, fig. 2) inaccurately figured the MIs in the holotype. The MIL is robust dentate, with two upturned ante- rior denticles (as in MIR in Fig. 5c) which were not depicted by Chamberlin. The MIR is gracile falcate with the anterior tip broken off. Examination of additional specimens reveals that maxillary symmetry is poly- morphic (Table 2), and that if robust MIs are present they are dentate (Fig. 5c). Two juvenile specimens were observed with den- tate MIs of the type illustrated in Fig. 5d. Mandibles (Fig. 5b) are as described by Chamberlin (1919:332, pl. 61, fig. 3). Arabella mutans most closely resembles A. novecrinita as restricted here. In contrast to the symmetry polymorphism exhibited by A. mutans, A. novecrinita is characterized by symmetrical maxillae with gracile MIs and long MIIs. In view of the small number of A. novecrinita included here (n = 4), this distinction must be considered tentative. A. mutans has more denticles on long MIIs on average (13.3, n = 12) than does A. nove- crinita (10.6, n = 5), but again the small sample size makes use of this distinction tentative. As restricted here, A. mutans has been recorded from Easter Island and the Mar- shall Islands in the tropical Pacific. A spec- imen from Guam (USNM 54426), which had been identified as A. mutans, 1s now Missing its jaws, and the identification could not be confirmed. Day’s (1975:196-197) report of A. mu- tans from Western Australia was based on a single juvenile specimen, and must be con- sidered questionable on that basis. The jaws illustrated by Fauvel (1953:275, fig. 1401) from a small specimen collected from Cey- 295 lon are also those of a juvenile, and the record cannot be accepted. Tampi & Ran- garajan (1964:11, figs. 29-31) did not de- scribe the jaws in the anterior fragment they identified as A. mutans from Car Nicobar, Indian Ocean, and their record must also be considered questionable. Silva (1961:182) described but did not illustrate a specimen from Ceylon as A. mutans which has two “hooded acicula’” per parapodium, and asymmetrical maxillae with MIL robust fal- cate, MIIL short, MIR gracile falcate, and MIIR long. The presence of two “‘hooded”’ setae per parapodium is unusual, and the maxillae are unlike those in either A. mu- tans or A. novecrinita. Arabella novecrinita Crossland, 1924 Figs. 3c, 4c Arabella novecrinita Crossland, 1924:71-75, text-figs. 89-95. Lectotype.—ZK 1924.3.1.15, Zanzibar; designated herein. Materials examined.—ZK 1924.3.1.15, Zanzibar (1).—ZK 1924.3.1.292, Minikoi Island, Maldives, mounted jaws and para- podia (1?).—uncatalogued anterior frag- ment, Aldabra. Remarks. —Crossland (1924:71) record- ed two specimens (with maxillary formulas) from the Maldives. The British Museum (Natural History) collection includes only mounted jaws and parapodia from this lo- cation which may be from a single speci- men. In light of the fragmentary nature of the Maldive material, and the wide geo- graphic separation between Crossland’s original type localities, the Zanzibar speci- men is herein designated the lectotype. Crossland’s (1924:7 1-75, text-fig. 89) de- scription of the soft-part morphology in this species is accurate. Noteworthy is the pres- ence of four anal cirri (Fig. 3c) on the lec- totype (Crossland 1924:75). The ventral se- tae in medial and posterior parapodia have 296 a smooth shaft which tapers abruptly to the guard (Fig. 4c). The maxillae on the lecto- type are symmetrical, with gracile MIs and long MIIs (Crossland 1924:72), as are the jaws on the two specimens Crossland (1924: 73) recorded from the Maldives, and the anterior fragment recorded here from Al- dabra. The jaw formula for the lectotype is 7-7; 7+-10; 5-5; 5-4; 1-1. For the species it is 6(7)-7; 10(11)-10(1 1); 4(6)-4(5); 4(5)-3(4); 1-1. The mandibles are typical of Arabella, as illustrated by Crossland (1924, text-fig. 91). As noted above, the setae and soft-part characteristics of this species are similar to those in Arabella mutans, and the species are distinguished based on the maxillae. As restricted here, A. novecrinita is known only from islands in the Indian Ocean. Day (1967:446, fig. 17.18fh) recorded speci- mens (as A. mutans) from Mozambique and South Africa which may belong in A. no- vecrinita based on the illustrated maxillary apparatus. It’s not clear whether the ventral setae are ridged based on Day’s (1967, fig. 17.18f) illustration, and thus the report can- not be securely credited to A. novecrinita. A South African specimen identified as A. mutans in the British Museum collection (ZK 1932.11.24.38) proved to be a mis- identified specimen of Arabella iricolor sen- su lato, and thus this question remains un- resolved. Arabella panamensis, new species Figs. 3f—g, 5f, 7 Arabella mutans. —Fauchald, 1977a:45 (Gn part). Holotype. —USNM 98237, Paitilla Beach, Panama. Etymology. —From Panama, the type lo- cality. Materials examined. —Holotype; USNM 66042, 66043, 66365 (paratypes), Paitilla Beach, Panama (9).—?USNM 80225, Golfo de Nicoya, Costa Rica (1). Description. —Prostomium bullet-shaped, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON slightly wider than long, V-shaped mark on ventral surface, four eyes embedded in pos- terior dorsal margin. Peristomium divided into two rings, ventral median furrow in anterior ring only. Setigers numerous, up to 177 in complete adults. Notopodia not expressed on surface, neuropodia with elongate postsetal lobe (Fig. 3g) which is commonly pigmented. Pygid- ium with two ventral anal cirri (Fig. 3f). Notoacicula fine, from two to three per setiger. Neuroacicula large, amber colored, three per setiger, tips commonly protruding slightly through parapodial wall. Anterior setigers with three smooth and from two to three toothed setae, medial and posterior setigers with two smooth, from one to two toothed, and one ventral seta. Shafts on ventral setae taper abruptly to guard, two ridges present (Fig. 3h). Mandibles H-shaped. Maxillae with two long carriers and unpaired ventral ligament. Maxillae exhibit symmetry polymorphism. One or both MI elements robust falcate (Fig. 5f). Denticle formula: 5(8)-6(9); 6(7) or 9-5(7) or 11(12); 4(6)-4(5); 3(4)-3(4); 1-1. Holotype large, complete specimen with 177 setigers, prostomium 0.39 mm long, 0.70 mm wide, peristomium 0.39 mm long, MIL 0.41 mm long, MIR 0.41 mm long, denticle formula 7-9; 6-11; 6-5; 4-4; 1-1. Remarks. — This species differs from oth- ers in the A. mutans complex in having long- er postsetal lobes on medial and posterior parapodia, two anal cirri which arise ven- trally, and in having two ridges on the ven- tral setae. It further differs in having some- what longer MIs in individuals of a given size (Fig. 7). The post-setal lobe in Arabella semimaculata (Moore, 1911) resembles that in A. panamensis (compare Fig. 3g; Fau- chald 1970, pl. 20, fig. g), but the former species has smoothly bilimbate ventral se- tae (Fauchald 1970:133), unlike the ridged, abruptly tapering ventral setae in A. pana- menslis. A juvenile specimen from the Pacific side of Costa Rica (USNM 80225) with dentate VOLUME 102, NUMBER 2 Length of Robust MI (mm) 0 01 0-2 0-3 Width of Prostomium (mm) Da | 0-4 0-5 0-6 0-7 0:8 Fig. 7. Plot of robust MI length against width of prostomium for Arabella multidentata (@), Arabella pana- mensis (x), and Arabella sp. A (*). Prostomial width is less subject to distortion by fixation than is total length, and is used here as a more reliable measure of specimen size (and, by inference, maturity). The spread of points for A. multidentata is typical of that observed for the other species considered here with the exception of A. panamensis. The regression line for A. multidentata is of the form y = 0.55x — 0.44 (r = 0.94). Note that all of the points for A. panamensis plot above the regression line, suggesting that individuals of A. panamensis have larger jaws for their size than do individuals of A. multidentata. The slope of a linear regression for A. panamensis (not shown) is significantly different from the slope for A. multidentata (P = 0.005, t = 3.04, d.f. = 35). Note also that plots of points for papillate individuals (Arabella sp. A) fall within the large end of the range of variation for A. multidentata. MIR has setae comparable to A. panamen- sis, but lacks the elongate postsetal lobe in posterior parapodia. No data is available on ontogenetic changes to be expected in this character, and the specimen is only tenta- tively attributed to A. panamensis. The species 1s presently known only from the Pacific coast of Panama. Arabella sp. A Figs. 31, 41, S5e Materials examined. —USNM 54216, 54915, 98239, Guayanilla Bay, Puerto Rico (8). Remarks. —Three collections of Arabella multidentata from Guayanilla Bay included several relatively large individuals with two distinctive papillae arising from the nuchal fold (Fig. 31). The jaws (Figs. 5e, 7) and setae are comparable to those in A. multidentata. No papillate specimens were recorded from any other locality, and the significance of the papillae is presently unclear. The char- acter is sufficiently distinctive to warrant segregation of these forms (informally as sp. A) pending further investigation. Discussion The systematic treatment here afforded members of the Arabella mutans species complex should be regarded as a working hypothesis. The stability of the taxonomic characters employed can be evaluated by the collection of additional specimens, and data on additional characters (using electro- phoresis, for example) can be collected for 298 comparative purposes. Studies on the breeding interactions in living populations would, of course, provide the most powerful test of the systematics, but at the same time may be the most challenging to implement. Particular emphasis is placed here on characterizing species based on populations rather than single individuals. Thus, poly- morphism of jaw symmetry is considered a useful taxonomic character, even though it is Meaningless in regard to a single individ- ual. A single individual collected from a new location may thus not be identifiable to the species level. This restriction especially applies to ju- venile individuals. Similar maxillae have been recorded from juveniles in four (ques- tionably five) of the species of Arabella con- sidered here, although the adult maxillae in these forms exhibit significant differences. Studies of other species of Arabella should consider the maturity of specimens before maxillary form is included in the species diagnosis. In particular, the distinction commonly made between Arabella iricolor and A. geniculata (Claparede, 1868) might be worth re-evaluation in this light (Fauvel 1923:439-440, fig. 1751-1; Fauchald 1970: 226; Ben-Eliahu 1976:172). As restricted here, two of the species con- sidered are incompletely characterized (Ar- abella atlantica, A. logani). The remaining five species are separated geographically as well as morphologically. The concept of A. mutans as a single circumtropical species 1s clearly incorrect. This observation serves to underline the futility inherent in attempting to use the distribution of rare, poorly under- stood species for the study of biogeography. The chief lessons for paleontologists studying fossil polychaete jaws are as fol- lows: 1) jaw symmetry may vary within a single population, and should be used as a taxonomic character with caution, 2) the morphologies of the MI and MII maxillary elements may be useful for species level di- agnoses, 3) the denticles on jaws may be worth counting after all, but denticle num- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ber should only be used as a taxonomic character on a population basis. The second point has already been deduced from the study of fossil material (Kielan-Jaworowska 1966; Edgar 1984), suggesting that classifi- cation of recent and fossil material may be roughly comparable. The first point has been less fully appreciated, and some revision of generic and family level fossil taxa may be necessary on that basis. Acknowledgments I thank Kristian Fauchald and Marian H. Pettibone for informative discussions con- cerning polychaete systematics, and for crit- ically reading the manuscript. Alex I. Muir, British Museum (Natural History), and Thomas H. Perkins, Florida Department of Natural Resources, generously arranged the loan of type and comparative material. I also thank numerous members of the staff of the U.S. National Museum of Natural History, Smithsonian Institution, for their cooperation in the completion of this study. Joanne Simpson drafted Figs. 1, 2, 6, and 7. This research was supported by a post- doctoral fellowship, Smithsonian Institu- tion. Literature Cited Ben-Eliahu, M. N. 1976. Errant polychaete crypto- fauna (excluding Syllidae and Nereidae) from rims of similar intertidal vermetid reefs on the Mediterranean coast of Israel and the Gulf of Elat.—Israel Journal of Zoology 25:156-177. Chamberlin, R. V. 1919. The Annelida Polychaeta. — Memoirs of the Museum of Comparative Zo- ology, Harvard 48:1-514. Crossland, C. 1924. Polychaeta of tropical East Af- rica, the Red Sea and Cape Verde Islands. The Lumbriconereidae and Staurocephalidae.— Proceedings of the Zoological Society of London 1924:1-106. Day. J. H. 1967. A monograph on the Polychaeta of southern Africa, part I. Errantia.— British Mu- seum (Natural History), London, 458 p. 1975. On a collection of Polychaeta from intertidal and shallow reefs near Perth, Western Australia.—Records of the Western Australia Museum (1975) 3:167—208. VOLUME 102, NUMBER 2 Duenas, P. R. 1981. Inventario preliminar de los poliquetos (Annelida) de aguas de la bahia de Cartagena y areas adyacentes.—Boletin Museo del Mar 10:82-138. Edgar, D.R. 1984. Polychaetes of the lower and mid- dle Paleozoic: a multi-element analysis and a phylogenetic outline. — Review of Palaeobotany and Palynology 43:255-—284. Ehlers, E. 1864-1868. Die Bornstenwurmer (Anneli- da, Chaetopoda). Leipzig, 748 p. 1887. Reports on the results of dredging in the U.S. Coast steamer ‘Blake.’ XX XI. Report on the annelids.—Memoirs of the Museum of Comparative Zoology, Harvard 15:1-335. Fauchald, K. 1970. Polychaetous annelids of the fam- ilies Eunicidae, Lumbrineridae, Iphitimidae, Arabellidae, Lysaretidae and Dorvilleidae from western Mexico.— Allan Hancock Monographs in Marine Biology 5:1-335. 1977a. Polychaetes from intertidal areas in Panama, with a review of previous shallow-water records.—Smithsonian Contributions in Zool- ogy 221:1-81. 1977b. The polychaete worms.— Natural History Museum of Los Angeles, Science Series 28:1-188. Fauvel, P. 1923. Faune de France 5, polychétes er- rantes. Office Central de Faunistique, Paris, 488 p. . 1953. The fauna of India including Pakistan, Ceylon, Burma and Malaya. Annelida Poly- chaeta. Allahabad, 507 p. Gardiner, S. L. 1976. Errant polychaete annelids from North Carolina. — Journal of the Elisha Mitchell Scientific Society 91:77—220. Grube, A.-E. 1850. Die Familien der Anneliden.— Archiv fur Naturgesch. Berlin 16.1:249-364. 1871. [untitled].—Jahresberichte der Schle- siche Gesellschaft ftir Vaterlandische Kultur, Breslau 49:56-58. Hartman, O. 1938. Annotated list of the types of polychaetous annelids in the Museum of Com- parative Zoology.—Bulletin of the Museum of Comparative Zoology, Harvard 85:1-31. 1944. Polychaetous annelids. Part V. Euni- cea.—Allan Hancock Pacific Expedition 10:1- 339. 1954. Marine annelids from the northern Marshall Islands.—U.S. Geological Survey Professional Paper 260Q:615-644. Kielan-Jaworowska, Z. 1966. Polychaete jaw appa- ratuses from the Ordovician and Silurian of Po- land and a comparison with modern forms.— Paleontologica Polonica 16:1—152. Kohn, A. J.,& M. C. Lloyd. 1973. Marine polychaete annelids of Easter Island.—Internationale Re- vue der Gestamten Hydrobiologie 58:69 1-712. 299 Monro, C. C. A. 1928. On the Polychaeta collected by Dr. Th. Mortensen off the coast of Panama. — Videnskabelige Meddelelser fra den Naturhis- toriske Forening 1 Kjobenhavn 85:75-103. 1933a. On a collection of Polychaeta from Dry Tortugas, Florida.—Annals and Magazine of Natural History, London, series 10, 12:244— 269. 1933b. The Polychaeta Errantia collected by Dr. C. Crossland at Colon, in the Panama Re- gion, and the Galapagos Islands during the ex- pedition of the S.Y. “‘St. George’’.— Proceedings of the Zoological Society of London 1933:1-96. Orensanz, J. M. 1974. Los anélidos poliquetos de la Provincia Biogeografica Argentina. VI. Arabel- lidae.—Physis, Seccion A 33:381-408. Perkins, T. H. 1979. Lumbrineridae, Arabellidae, and Dorvilleidae (Polychaeta), principally from Florida, with descriptions of six new species. — Proceedings of the Biological Society of Wash- ington. 92:415-465. Pettibone, M. H. 1963. Marine polychaete worms of the New England Region. 1. Aphroditidae through Trochochaetidae.— U.S. National Mu- seum Bulletin 227:1-356. Reish, D. J. 1968. The polychaetous annelids of the Marshall Islands. — Pacific Science 22:208-231. Silva, P. H. D. H. de. 1961. Contributions to the knowledge of the polychaete fauna of Ceylon. Part I. Five new species, two new varieties and several new records principally from the south- ern coast.—Spolia Zeylan 29:164-194. Tampi, P. R. S., & K. Rangarajan. 1964. Some poly- chaetous annelids from the Andaman waters. — Journal of the Marine Biological Association of India 6:98-121. Treadwell, A. L. 1921. Leodicidae of the West Indian region.— Publications of the Carnegie Institu- tion, Washington 15:1-131. Uebelacker, J. M. 1984. Family Arabellidae Hart- man, 1944. Pp. 42-1—42-29 in J. M. Uebelacker and P. G. Johnson, eds., Polychaetes of the Northern Gulf of Mexico, Volume 6, Barry A. Vittor & Associates, Mobile, Alabama. Verrill, A. E. 1900. Additions to the Turbellaria, Nemertina and Annelida of the Bermudas, with revisions of some New England genera and species.— Transactions of the Connecticut Academy of Arts and Sciences 10:595-671. Wolf, G. 1980. Morphologische Untersuchungen an den Kieferapparaten einiger rezenter und fos- siler Eunicoidea (Polychaeta). —Senckenber- giana Maritima 12:1-182. 2195 Deborah Way, Upland, California 91786. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 300-304 A NEW SPECIES OF BENHAMIPOLYNOE (POLYCHAETA: POLY NOIDAE: LEPIDASTHENIINAE) FROM AUSTRALIA, ASSOCIATED WITH THE UNATTACHED STYLASTERID CORAL CONOPORA ADETA Marian H. Pettibone Abstract. — Benhamipolynoe cairnsi, n. sp. from deep-water (398 m) off Queensland, Australia, was found in close symbiotic relationship with the unusual, unattached stylasterid coral Conopora adeta Cairns. The coral grows around the polynoid, enclosing it in a coiled tube. The species is compared with the type species of the genus, B. antipathicola (Benham), from off New Zealand, found in latticed tunnels formed by the antipatharian coral Paranti- pathes tenuispina (Silberfeld). Both polynoid species are referred to the new subfamily Lepidastheninae. While working on his description of the new species of stylasterid coral from Aus- tralia, the unique unattached Conopora ad- eta, Cairns (1987) noted the presence of a polychaete enclosed in each of his ten coral specimens. He brought them to my atten- tion and allowed me to extract the polynoids from two of the corals, which was no small task, since the coral paratypes had to be cut with the minimum of damage. On exami- nation, the commensal polynoids appeared to belong to an undescribed genus and species (Cairns 1987:143). After further study, they are described below as a new species of Benhamipolynoe Pettibone, 1970, with type species B. antipathicola, described by Benham (1927, under Lepidasthenia) and Pettibone (1970, under the new genus), from off New Zealand, associated with the anti- patharian coral Parantipathes tenuispina. The types are deposited in the Northern Territory Museum, Darwin, Australia (NTM) and the National Museum of Nat- ural History, Smithsonian Institution (USNM). Family Polynoidae Lepidastheniinae, new subfamily Types genus: Lepidasthenia Malmgren, 1867, with type species L. elegans (Grube, 1840), by monotypy. Diagnosis. —Prostomium bilobed, with 3 antennae and 2 palps; ceratophore of me- dian antenna in anterior notch, lateral an- tennae inserted terminally on anterior ex- tensions of prostomium, on same level as median antenna (or slightly subterminally); two pairs of eyes on posterior half of pro- stomium. First or tentacular segment not distinct dorsally; tentaculophores lateral to prostomium, each with aciculum and pair of dorsal and ventral tentacular cirri, with- out setae. Second or buccal segment with first pair of elytrophores and elytra, setig- erous parapodia and ventral or buccal cirri lateral to ventral mouth. Elytra smooth, without fringes of papillae, without tuber- cles, with or without scattered micropapil- lae. Parapodia subbiramous, with small no- topodium, notoaciculum, and without, or VOLUME 102, NUMBER 2 with very few, notosetae. Neuropodia with anterior and posterior lobes deeply cut dor- sally and ventrally, without projecting acic- ular lobes. Dorsal cirri on non-elytrigerous segments with basal cirrophores and distal styles; dorsal tubercles indistinct. Pharnyx with 9-13 pairs of border papillae and 2 pairs of chitinous jaws. Remarks. —Lepidasthenia has been in- cluded in the Subfamily Lepidonotinae Wil- ley, 1902, chiefly on the basis of the simi- larity of the prostomium to Lepidonotus Leach, 1816. It is separated herein based on the different types of parapodia and elytra. Also included in Lepidastheniinae are the following polynoid genera: Perolepis Ehlers, 1908; Parahalosydna Horst, 1915; Hyper- halosydna Augener, 1922; Alentiana Hart- man, 1942; Telolepidasthenia Augener & Pettibone, 1970; Benhamipolynoe Petti- bone, 1970. A new species is described be- low under the last named genus. Benhamipolynoe Pettibone, 1970 Type species: Lepidasthenia antipathicola Benham, 1927, by original designation. Diagnosis. —Body elongate, slender, flat- tened, segments numerous (more than 50, up to 200 or more). Elytra 10 or more pairs, on segments 2, 4, 5, 7, alternate segments to 15, then variable in arrangement, with either long posterior region without elytra or with elytra continuing posteriorly. Elytra without fringes of papillae, smooth except for scattered micropapillae. Prostomium lepidasthenoid, bilobed, with two palps and three antennae; ceratophore of median an- tenna in anterior notch of prostomium, lat- eral antennae inserted terminally on ante- rior extensions of prostomium, lateral to median antenna, with two pairs of eyes on posterior half of prostomium. Tentaculo- phores of tentacular segment lateral to pro- stomium, without setae, with two pairs of dorsal and ventral tentacular cirri. Second or buccal segment with first pair of elytra 301 and long ventral buccal cirri; without nuchal lobe. Parapodia subbiramous, with small conical notopodia on anterodorsal faces of neuropodia, without notosetae. Neuropo- dia deeply cut dorsally and ventrally, with anterior and posterior subequal rounded lobes, without projecting acicular lobes. Neurosetae relatively few in number (5-12), of single type, rather stout, smooth or with slight indication of spinous rows, with fal- cate entire tips. Dorsal cirri with short cy- lindrical cirrophores and long, smooth, ta- pering styles; dorsal tubercles indistinct. Ventral cirri short, subulate. Pygidium with paired long anal cirri. Nephiridial papillae short, cylindrical, beginning on segment 8. Remarks. — Benhamipolynoe differs from Lepidasthenia Malmgren in regard to the number and arrangement of the elytra and the types of neurosetae. In Lepidasthenia, the neurosetae have well-developed short and wide spinous regions and bifurcate tips; in Benhamipolynoe, the neurosetae have spinous regions scarcely developed or lack- ing and entire falcate tips. Benhamipolynoe antipathicola (Benham, 1927), originally described as Lepidasthen- ia, from off New Zealand in 128 meters, was associated with Parantipathes tenuispina (Silberfeld), where it was found in latticed tunnels formed by the serrated branchlets of the antipatharian. Additional specimens referred to B. antipathicola by Pettibone (1970) include one from the Gulf Stream off Key West, Florida, in 237 meters, associ- ated with Antipathes columnaris Duchas- saing, and one from Indonesia, in 520 me- ters, found in an empty tube of a eunicid polychaete. Benhamipolynoe cairnsi, new species Figs. 1, 2 Material. —Queensland, Australia, Mar- ion Plateau off MacKay, 20°46.2’S, 152°51.8'E, 398-399 m, F.R.V. Soela sta 25, 22 Nov 1985, A. Bruce, collector, re- moved from coiled galleries in stylasterid 302 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Po 1. Benhamipolynoe cairnsi, A, C-H, Holotype, NIM W4900; B, Paratype, USNM 118373: A, Dorsal view of anterior end, styles of median and might lateral antennae, left dorsal and ventral tentacular cirri all missing; right parapodium and dorsal cirrus of segment 3 not shown; B, Ventral view of anterior end, styles of median and left lateral antennae, left palp, and all tentacular cirri missing; C, Right elytrigerous parapodium of segment 2, posterior view, acicula and small notopodium dotted, elytrophore not shown; D, Right cirrigerous parapodium of segment 3, anterior view, acicula dotted; E, Neurosetae from same; F, Right Ist elytron from segment 2, with few micropapillae (not to scale); G, Right 2nd elytron from segment 4; H, Right 9th elytron from segment 19. Scales = 1.0 mm for A, B; 0.5 mm for C, D, F—H; 0.1 mm for E. coral Conopora adeta Cairns, holotype (NIM W4900) and paratype (USNM 118373). Description. —Holotype (in two pieces, incomplete posteriorly) with 38 segments, 16 mm long, 2 mm wide; paratype (in three pieces, complete) with 63 segments, 33 mm long, 3 mm wide; both specimens females, full of large yolky eggs. Body elongate, flattened ventrally, arched dorsally, widest in anterior half, tapering gradually posteriorly; without color except for black eyes. Prostomium oval, bilobed; ceratophore of median antenna large, oval, in anterior notch, style missing; lateral an- tennae inserted terminally on anterior con- tinuations of prostomium, lateral to median antenna, with long styles about equal to stout VOLUME 102, NUMBER 2 A B 303 Fig. 2. Benhamipolynoe cairnsi, Holotype, NIM W4900: A, Right cirrigerous parapodium from segment 12, posterior view, extension on anterior side of cirrophore dotted; B, Right cirrigerous parapodium from segment 21, posterior view; C, Upper and middle neurosetae from same, latter with tip worn; D, Right cirrigerous parapodium from segment 35, anterior view, acicula dotted; E, Upper and middle neurosetae from same. Scales = 0.5 mm for A, B, D; 0.1 mm for C, E. tapering palps; two pairs of subequal black eyes on posterior half of prostomium (Fig. 1A, B). First or tentacular segment not vis- ible dorsally; tentaculophores lateral to pro- stomium, without setae, each with pair of tentacular cirri, ventral one about as long as lateral antennae, dorsal one longer than palps; ventrally with bulbous facial tubercle (Fig. 1A, B). Second or buccal segment with slightly developed nuchal lobe, first pair of elytrophores, subbiramous parapodia with few neurosetae, and ventrally with long buc- cal cirri lateral to ventral mouth (Fig. 1A— C). Segment 3 with first pair of dorsal cirri; cirrophores longer than neuropodia, cylin- drical with distal bulbous extension and long style; ventral cirri almost as long as buccal cirri of segment 2 (Fig. 1A, B, D). Elytra and elytrophores 10 pairs on seg- ments 2-4, 5—7—9-1 1—13-15—19— 23, with dorsal cirri on all segments from 24 on. Ely- tra oval, attached eccentrically near lateral side, delicate, with “‘veins’’ and scattered round micropapillae on surface (Fig. 1 F—H). Parapodia subbiramous; notopodia in form of small conical acicular lobes on anterodorsal faces of larger neuropodia, without notosetae; neuropodia rather deep- ly cut dorsally and ventrally, forming rounded presetal and postsetal lobes, with row of 5—10 short neurosetae (Figs. 1C, 2A, B, D). Neurosetae stout, with faint spinous rows and slightly hooked entire tips, some- times slightly worn (Figs. 1E, 2C, E). Cir- rophores of dorsal cirri cylindrical, extend- ing beyond neuropodia, with triangular extension on lower side, with long, smooth styles tapering to slender tips and extending far beyond parapodia; ventral cirri wider basally, with long slender tips, extending slightly beyond tips of neuropodia (Fig. 2A, BaD): Nephridial papillae beginning on segment 8, small at first, becoming longer about seg- ment 15, cylindrical, directed dorsally be- tween parapodia. Pharynx not extended and not examined. Pygidium forming small lobe with dorsal anus between last pair of small parapodia and pair of long anal cirri, similar to dorsal cirri. Biology.—The two symbiont polynoids were removed from two paratypes of the 304 colonial stylasterid coral Conopora adeta, well figured by Cairns (1987, figs. 1-6). The coral is unusual in that it is unattached, formed of a massive globose solid base with several (3-6) stout, radiating, stabilizing branches and two main ascending porous branches. The polynoid occupied a coiled runway in the globose base connected to a U-shaped tube in the vertical branches. The close symbiotic relationship of the polynoid with the coral begins at an early stage in development and determines the morphol- ogy of the colony. One of the openings near the base of the colony was large enough for the polynoid to be able to protrude from the tube. All of the ten coral colonies examined by Cairns contained a polynoid symbiont. Both specimens of Benhamipolynoe cairnsi were females, full of large yolky eggs. Remarks. — Benhamipolynoe cairnsi dif- fers from B. antipathicola in having only 10 pairs of elytra and only dorsal cirri from segment 24 on, compared to numerous pairs of elytra continuing to the posterior end. In B. cairnsi, the cirrophores of the dorsal cirri have unique extra extensions: bulbous on segment 3 and triangular on the following cirrophores; this condition was not found on B. antipathicola and has not been noted previously on other polynoids. The two species differ in their positions with their respective coral hosts. As indicated above, the coiled runway of B. cairnsi is enclosed in the stylasterid coral Conopora adeta, al- lowing only limited movement to the ex- terior. For B. antipathicola, the antipathar- ian coral host, Parantipathes tenuispina, is a bottle-brush shaped colony where the in- terlacing branchlets form a complicated lat- tice-work tube that serves as an elongated PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON “‘worm-run,” described by Totton (1923: 106, fig. 9), thus allowing much greater ex- ternal movement for the polynoid com- mensal. Etymology.—The species is named for Stephen D. Cairns, who described and named the stylasterid coral host of the po- lynoid symbiont. Acknowledgments My thanks go to Stephen Cairns for bring- ing the polynoid commensal to my atten- tion and for allowing me to extract them from the stylasterid coral. The manuscript benefited from the reviews of Russel Hanley and Stephen Cairns. Literature Cited Benham, W.B. 1972. Polychaeta.— British Antarctic “Terra Nova” Expedition, 19106, Natural His- tory Reports, Zoology 7(2):47-182. Cairns,S.D. 1987. Conopora adeta, new species (Hy- drozoa: Stylasteridae) from Australia, the first known unattached stylasterid.— Proceedings of the Biological Society of Washington 100(1):141- 146. Pettibone, M. H. 1970. Polychaeta errantia of the Siboga-Expedition. Part 4: Some additional polychaetes of the Polynoidae, Hesionidae, Ne- reidae, Goniadidae, Eunicidae, and Onuphidae, selected as new species by the late Dr. Hermann Augener with remarks on other related species. — Siboga-Expedite 24,1d:199-270. Totton, A. K. 1923. Coelenterata. Part III. Antipa- tharia (and their Cirripede Commensals). — Brit- ish Antarctic (“Terra Nova’’) Expedition, 1910, Natural History Report. Zoology 5(3):97—120. Department of Invertebrate Zoology, Na- tional Museum of Natural History, Smith- sonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 305-310 TWO NEW SPECIES OF HARMOTHOINAE (POLYCHAETA: POLY NOIDAE) FROM THE EAST PACIFIC RISE, COLLECTED BY ALVIN DIVES 2000 AND 2003 Marian H. Pettibone Abstract.— Alvin dives in the East Pacific Rise in 2700 meters near 11°N collected two polynoid species of Harmothoinae: Harmothoe hollisi, n. sp. from dive 2000, associated with a “‘wood island,” and Eunoe alvinella n. sp. from dive 2003, collected from an inactive sulfide chimney. As a part of the dive series of the DSRV Alvin on the East Pacific Rise, during Dive 2000 in March 1988, near 11°51'N in 2750 meters, the pilot picked up a piece of wood that was densely covered with biota, in- cluding serpulid worms, gastropods, gala- theids, ophiuroids, and additional fauna (Van Dover 1988). Among the latter were two polynoid polychaetes sent to me for study by Cindy Lee Van Dover of the Woods Hole Oceanographic Institution. The col- lection site was in a field of lightly sedi- mented pillow basalt, within a few kilo- meters of known hydrothermal vent communities. The fauna of this ““wood is- land” is of particular interest in comparing it with the fauna associated with the hydro- thermal vents. The polynoid is described below as a new species of Harmothoe, H. hollisi, a widely distributed genus in Harmothoinae. A large polynoid, collected by Dive 2003 on an in- active sufide chimney, is described as a new species of Eunoe, E. alvinella, also a widely distributed genus is the same subfamily. Previously reported species of Harmothoe, associated with the “wood island” and panel experiments by Turner (1973, 1981) in the deep water of the North Atlantic, included two species described by Pettibone (1985a): H. ingolfiana Ditlevsen and H. vagabunda Pettibone. Harmothoe macnabi Pettibone was described by Pettibone (1985b) from Alvin dive 895 in the Galapagos Rift. The above three species of Harmothoe, as well as the new species, lack eyes, as character- istic of most deep sea polynoids. The new species of Eunoe differs from other species of Eunoe in having very large eyes, occu- pying the lateral borders of the prostomium. Subfamily Harmothoinae Horst, 1917 Genus Harmothoe Kinberg, 1856 Harmothoe hollisi, new species Pigs) 2 Material. —East Pacific Rise, Alvin dive 200022 Mar 1988) hS2"Ng .103°S 1 W, 2750 m, “wood island,” holotype (USNM 118867) and paratype (USNM 118868). Description. —Length of complete holo- type 24 mm, width with setae 15 mm, seg- ments 37, last one minute. Length of in- complete paratype 15 mm, width 7 mm, segments 21. Without color except for gold- en setae. Body flattened, subrectangular, tapered slightly anteriorly and posteriorly. Elytra 15 pairs, on large prominent elytrophores on segments 2, 4, 5, 7, alternate segments to 23, 26, 29, and 32 (Figs. 1A, 2A). Elytra large, overlapping, covering dorsum, oval to subreniform in shape, delicate (tear eas- ily), densely covered with conical micro- tubercles, smaller on anterior part, becom- ing gradually larger on posterior and lateral 306 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Pips: Harmothoe hollisi, A, B, D, holotype (USNM 118867); C, paratype (USNM 118868): A, Anterior end, dorsal view, palps missing; B, Same, ventral view; C, Anterior end, dorsal view, pharynx partially extended, right palp and right ventral tentacular cirrus shorter, regenerating, right dorsal tentacular cirrus missing; D, Right 5th elytron from segment 9, with detail of microtubercles and papillae (not to scale). Scales = 1.0 mm for A— C; 2.0 mm for D. borders; larger tubercles cylindrical or ovoid, with tips entire or with 2—8 nodular exten- sions; scattered filiform papillae on surface and lateral and posterior borders (Fig. 1D). Non-elytra-bearing segments with dorsal cirri and nodular to digitiform dorsal tu- bercles (Figs. 1A, 2B). Prostomium deeply bilobed, with distinct cephalic peaks, tending to curl inward, with- out eyes; median antenna with large bul- bous ceratophore in anterior notch and long papillate style; lateral antennae with short bulbous ceratophores inserted ventrally, with styles short, bulbous and papillate ba- sally, and long filamentous tips; palps (miss- ing on holotype) stout, tapered, smooth (Fig. 1A-C). Tentaculophores lateral to prosto- mium, each with small acicular process and 2-3 short notosetae on inner side, and dor- sal and ventral tentacular cirri similar to median antenna (Fig. 1A—C). Second or buccal segment with first pair of large elytro- phores, biramous parapodia, and long ven- tral buccal cirri inserted basally on neuro- podia lateral to ventral mouth, similar to tentacular cirri (Fig. 1A, B). Parapodia biramous, with golden setae. Notopodia rounded basally, with projecting acicular lobe on lower side, almost as long as neuropodia (Fig. 2A, B). Notosetae nu- merous, forming radiating bundle, slightly curved, about four different lengths, shorter VOLUME 102, NUMBER 2 307 Q Y B \ | \ \ | 4 \ I 4 ia willl (AI A v ? 1 WV | | a | 7 WW ra wth | { } wit | we { q \ | \ a | wey wh VA i ¥ A uted a | \ q io al | § ' { | wey wl | f t f ug a | \ | sf ' / au eee: i ie wl \ 4 | i y e | “ Ae a ve OT ue uy | Y y wey W if / 4 we 4 j i j wily wa y f j aug uy 4 ’ | q ay wl | 4 / way al } ; | wily me i y ! : 4 my ses ( wi { y 0) ] | | y lg } C D re Fig. 2. Harmothoe hollisi, holotype (USNM 118867): A, Right elytrigerous parapodium from segment 11, anterior view, acicula dotted; B, Right cirrigerous parapodium from segment 12, posterior view; C, Long and short notosetae; D, Subacicular neurosetae, with detail of tips; E, Supraacicular neuroseta, with detail of tip. Scales = 1.0 mm for A, B; 0.1 mm for C—E. than and much stouter than neurosetae; no- tosetae with numerous spinous rows and rather long, tapered bare tips (Fig. 2C). Cy- lindrical cirrophores of dorsal cirri on dor- soposterior sides of notopodia, with slender papillate styles extending beyond neurose- tae (Fig. 2B). Neuropodia with conical pre- setal lobe and projecting acicular process with small supraacicular extension, and shorter rounded postsetal lobe (Fig. 2A, B). Neurosetae numerous, forming fan-shaped bundle, with numerous spinous rows. Su- praacicular neurosetae more slender, with long spinous regions and bare split tips (Fig. 2E). Subacicular neurosetae stouter, with shorter spinous regions, and slightly hooked bare tips, all with rather long secondary tooth (Fig. 2D). Ventral cirri short, tapered, with abruptly narrowed distal tip (Fig. 2A, B). Pharynx not extended and not examined. Inflated ventral nephridial areas with small papilla on posterior side, beginning on seg- ment 6 (Fig. 2B). Pygidium forming small lobe between small parapodia of 2 posterior Table 1.—Comparison of Harmothoe ingolfiana and Harmothoe hollisi. H. ingolfiana H. hollisi Cephalic peaks of prostomium Elytral macrotubercles Neurosetae small present upper ones with bifid tips, middle and lower ones with entire tips prominent, tending to curl inward absent all with bifid tips 308 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 3. Eunoe alvinella, holotype (USNM 118866): A, Anterior end, dorsal view, pharynx partially extended, styles of median antenna, left lateral antenna, right and left dorsal and ventral tentacular cirri missing; B, Left 2nd elytron from segment 4, with detail of microtubercles and papillae (not to scale); C, Left middle elytron, with detail of microtubercles and papillae (not to scale). Scale = 1.0 mm for A-C. segments, with pair of anal cirri (styles miss- ing). Etymology.—The species is named for Ralph Hollis, the pilot of Alvin dive 2000, who collected the interesting ““wood island”’ with its associated biota. Comparison. —Harmothoe hollisi agrees in most respects with H. ingolfiana Ditlev- sen, reported from the North Atlantic south of Iceland to off New England in 1830-3506 meters and found in burrows of wood-bor- ing bivalves (Ditlevsen 1917:32, Pettibone 1985a:143). The two species are compared in Table 1. Genus Eunoe Malmgren, 1865 Eunoe alvinella, new species Figs. 3, 4 Material.—East Pacific Rise, Alvin dive 2003, 25 Mar 1988, 11°46’N, 104°47’'w, 2725 m, inactive sulfide chimney, sample no. 9, holotype (USNM 118866). Description. —Length of complete holo- type 41 mm, width with setae 14 mm, seg- ments 34, last one minute. Dorsum light brown, with colorless transverse bands. Body elongate-oval, slightly tapered an- teriorly and more so posteriorly, flattened ventrally, arched dorsally. Elytra 15 pairs, on large bulbous elytrophores on segments 2, 4, 5, 7, alternate segments to 23, 26, 29, and 32 (Figs. 3A, 4A, C). Elytra large, over- lapping, covering dorsum, oval to subreni- form in shape, thickly covered with rusty yellow and brown foreign material; elytral surface with microtubercles on most of sur- faces large globular macronodules on pos- terior third of elytra, variable in number and size, and filiform papillae on lateral bor- der and scattered on surface (Fig. 3B, C). Non-elytra-bearing segments with dorsal cirri and nodular dorsal tubercles (Fig. 4B, D). Prostomium deeply bilobed, wider than long, without distinct cephalic peaks, with two pairs of very large eyes occupying lateral sides of prostomium; median antenna with large bulbous ceratophore in anterior notch, style missing (probably long); lateral anten- VOLUME 102, NUMBER 2 309 Fig. 4. Eunoe alvinella, holotype (USNM 118868): A, Right elytrigerous parapodium from segment 2, anterior view, acicula dotted, style of ventral buccal cirrus missing; B, Right cirrigerous parapodium from segment 3, posterior view, style of dorsal cirrus missing; C, Right elytrigerous parapodium from segment 13, anterior view, acicula dotted, style of ventral cirrus hidden from view; D, Right cirrigerous parapodium from segment 14, posterior view; E, Short and long notosetae; F, Supraacicular neuroseta; G, Middle and lower subacicular neurosetae. Scales = 1.0 mm for A—D; 0.1 mm for E-G. nae with short bulbous ceratophores in- serted ventrally, styles short, tapered; palps stout, tapered, about one and a half times length of prostomium (Fig. 3A). Tentacu- lophores lateral to prostomium, each with projecting aciculum and one or two noto- setae on inner side, and dorsal and ventral tentacular cirri, styles missing (probably long); bulbous facial tubercle medial to cer- atophores of lateral antennae (Fig. 3A). Sec- ond or buccal segment with first pair of large elytrophores, biramous parapodia; cerato- phores of ventral buccal cirri inserted ba- sally on neuropodia lateral to ventral mouth, styles missing (probably longer than follow- ing ventral cirri) (Figs. 3A, 4A). Parapodia biramous, with golden setae. Notopodia smaller and shorter than neu- 310 ropodia (Fig. 4C, D). Notopodium wider basally, tapering to digitiform acicular lobe on lower side, tip of notoaciculum project- ing (Fig. 4C). Notosetae moderate in num- ber, much stouter than neurosetae, upper ones shorter, curved, lower ones longer, nearly straight, both with numerous spinous rows and rather short bare blunt tips (Fig. 4E). Cylindrical cirrophores of dorsal cirri on dorsoposterior sides of notopodia, with long papillate styles extending far beyond neurosetae (Fig. 4D). Neuropodium with conical presetal acicular lobe and projecting acicular process, tip of neuroaciculum pro- jecting; postsetal lobe shorter, rounded (Fig. 4A-D). Neurosetae numerous, with spinous rows. Supraacicular neurosetae slender, with long spinous regions, tapering to slender straight bare tips (Fig. 4F); middle and low- er subacicular neurosetae stouter, with shorter spinous regions and slightly hooked bare tips (Fig. 4G). Ventral cirri short, ta- pered (Fig. 4D). Pharynx not extended and not examined. Nephridial papillae small, beginning on seg- ment 4. Pygidium rectangular lobe between small parapodia of last segment, with pair of anal cirri (styles missing). Etymology.—The species is named for the collecting vessel, the DSRV Alvin. Comparisons. —E. alvinella differs from other species of Eunoe in having very large eyes occupying the lateral sides of the pro- stomium. The elytra, with their unique type of numerous globular macronodules, also differ from other species of the genus. Acknowledgments I wish to thank Cindy Lee Van Dover of the Woods Hole Oceanographic Institution, PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON as well as the pilot and observers of the submersible A/vin, on their celebration of dives 2000 and 2003, for the material on which this study is based. The manuscript benefited from the reviews of James A. Blake, J. Fred Grassle, and Cindy Lee Van Dover. Literature Cited Ditlevsen, Hj. 1917. Annelides I.—The Danish In- golf-Expedition, Copenhagen 4(4):1-71. Pettibone, M. H. 1985a. Polychaete worms from a cave in the Bahamas and from experimental wood panels in deep water of the North Atlantic (Polynoidae: Macellicephalinae, Harmothoi- nae).— Proceedings of the Biological Society of Washington 98(1):127-149. 1985b. New genera and species of deep-sea Macellicephalinae and Harmothoinae (Poly- chaeta: Polynoidae) from the hydrothermal rift areas off the Galapagos and western Mexico at 21°N and from the Santa Catalina Channel. — Proceedings of the Biological Society of Wash- ington 98(3):740-757. Turner, R. D. 1973. Wood-boring bivalves, oppor- tunistic species in the deep sea.—Science 180: 1377-1379. . 1981. “Wood islands” and “thermal vents” as centers of diverse communities in the deep sea. — The Soviet Journal of Marine Biology 7(1): 1-9. Van Dover, C. L. 1988. Alvin Dive 2000.—Sea Fron- tiers, 34(6):326-—331. Department of Invertebrate Zoology, Na- tional Museum of Natural History, Smith- sonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 311-312 VARICHAETADRILUS ANGUSTIPENIS (BRINKHURST AND COOK, 1966), NEW COMBINATION FOR LIMNODRILUS ANGUSTIPENIS (OLIGOCHAETA: TUBIFICIDAE) Ralph O. Brinkhurst Abstract. —Limnodrilus angustipenis Brinkhurst & Cook, 1966 is recognized as a member of the genus Varichaetadrilus Brinkhurst & Kathman, 1983. Re-examination of some of the type spec- imens of Limnodrilus angustipenis Brink- hurst & Cook, 1966 reveals that this taxon should be attributed to the genus Varichae- tadrilus Brinkhurst & Kathman, 1983. Five specimens of the original set collected from Saginaw Bay, Lake Huron in 1956 by the former United States Bureau of Commer- cial Fisheries Laboratory of Ann Arbor, Michigan, were examined. These were orig- inally donated to the author by J. K. Hil- tunen, now of Sugar Island, Michigan. As the species is usually identified by ref- erence to the shape of the somewhat elon- gate penis sheaths, very few if any dissec- tions or sections appear to have been prepared from this species. Furthermore, the male ducts have never been fully illustrated. The species was originally described in the third part of a series of publications on the North American aquatic Oligochaeta (Brinkhurst & Cook 1966) in which a few tubificid descriptions were added to a paper largely directed to the Family Lumbriculi- dae. No follow-up description has been published. The male ducts of one of the five speci- mens at hand are visible as a series of frag- ments from a dissection. The union of the vas deferens and atrium and the origin of the prostate gland close to this point is evident on both male ducts. The form of these could well be mistaken for those of Limnodrilus. Beyond this point, however, the atrium does not narrow to form an ejaculatory duct, but remains wide all the way to the base of the penis sheath on each side (Fig. 1). This unique construction of the male ducts is typical of Varichaeta- drilus. Neither of these male ducts is com- plete, and so the total length cannot be es- timated, but they would appear to be more like those of V. psammophilus (Loden, 1977) and V. minutus (Brinkhurst, 1965) than those of V. pacificus (Brinkhurst, 1981) or Pig. 1. Varichaetadrilus angustipenis drawn with the aid of a drawing tube from a paratype in the author’s collection. Scale in mm. a—atrium, p—prostate stalk, s—penis sheath, sp—spermatheca, sz—spermatozeugmata, v— vas deferens. Fragmented male ducts and spermatheca of 312 Fig. 2. Chaetae from segments II and VI of the dissected specimen, posterior chaetae from another whole mount. Scale in mm. dIJ—dorsal chaetae of II, dV1I—dorsal chaetae of VI, vVI— ventral chaetae of VI, pv—posterior ventral chaetae. V. fulleri Brinkhurst & Kathman, 1983, as illustrated by Brinkhurst (1986). In V. angustipenis the penis sac enclosing the long cuticular penis sheath lacks the spi- ral muscles diagnostic of the genus Lim- nodrilus s.s. (the positions of Limnodrilus grandisetosus Nomura, 1932 and Limnod- rilus silvani Eisen, 1879, might be chal- lenged in regard to this feature). The usual erectile penes of Varichaetadrilus appear to be reduced to the short conical structures in the bases of the penis sheaths in this species. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON In the original account, no mention was made of penial chaetae, and these do not seem to be modified on the specimens ex- amined here. The penial chaetae are mod- ified in V. pacificus and V. minutus (=V. nevadanus) but not in V. fulleri or V. psam- mophilus. Varichaetadrilus israelis Brink- hurst, 1971 appears to lack them, too, but this requires confirmation. The somatic chaetae have reduced upper teeth in anterior bundles (Fig. 2) but the upper teeth are longer than the lower in most bundles, though they may vary within a bundle. There are mostly five chaetae in an- terior bundles, but only one or two poste- riorly. The upper teeth are especially short in chaetae from II to V. The form of the penis sheath, and in par- ticular its length, is diagnostic for this species. Literature Cited Brinkhurst, R. O. 1986. Guide to the freshwater aquatic microdrile oligochaetes of North Amer- ica. — Canadian Special Publication of Fisheries and Aquatic Sciences 84:1—259. —, & D. G. Cook. 1966. Studies on the North American aquatic Oligochaeta. III: Lumbricu- lidae and additional notes and records of other families.— Proceedings of the Academy of Nat- ural Sciences of Philadelphia 118:1-33. Institute of Ocean Sciences, P.O. Box 6000, Sidney, British Columbia V8L 4B2, Canada. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 313-323 THE ADULT MALE OF THE TROGLOBITIC OSTRACODE SPELAEOECIA BERMUDENSIS ANGEL AND ILIFFE, 1987, FROM AN ANCHIALINE CAVE IN BERMUDA (CRUSTACEA: OSTRACODA: HALOCYPRIDOIDEA) Louis S. Kornicker Abstract.—The previously unknown adult male of Spelaeoecia bermudensis Angel & Iliffe, 1987, the type species of the monotypic genus Spelaeoecia Angel & Iliffe, 1987, is described and illustrated from a specimen collected in Won- derland Cave, Bermuda. The fifth limb bears a large sensory organ that is absent on the limbs of the adult female as well as the juvenile male, and has not been reported previously in the suborder Halocypridina. The rod-shaped posterior branch of the copulatory organ is not inside the canal of the broad anterior branch as in other genera of the superfamily Halocypridoidea. The separated anterior and posterior branches resemble those of the copulatory organ of adult males in the superfamily Thaumatocypridoidea, which together with the Halocypridoidea form the suborder Halocypridina. A brief supple- mentary description is given of the adult female. The species Spelaeoecia bermudensis was described by Angel & Iliffe (1987:545) from 56 specimens (22 adults, but 2 of the adults represented by carapaces only) collected in 8 anchialine caves in Bermuda. Angel & Iliffe (p. 552) stated, ““The absence of males in the collections could indicate that the species breeds by parthenogenesis, but it seems more likely that breeding occurs in parts of the cave inaccessible to divers.” Kornicker & Iliffe (1989) reported from 2 anchialine caves in Bermuda 10 additional specimens including 2 A-1 males, which they described briefly. They mentioned an adult male collected in Wonderland Cave, Ber- muda, which was encountered too late to conveniently include in their paper. That male is described herein. It was collected along with one juvenile and nine adult fe- males in a baited trap by Jan H. Stock in 1984. Angel & Iliffe (1987:tab. 2) reported three adults (two represented by carapaces only) from the same cave. Unless the ratio of adult females to males in the species is unusually high it seems likely, as suggested by Angel & Iliffe (1987), that adult females are more widespread than adult males. Per- haps the adult male described herein was attracted from some distance by the bait in the trap, and trapping rather than netting may be a more efficient method for collect- ing males. A brief supplementary descrip- tion is presented based on a study of the holotype. Superorder Myodocopa Sars, 1866 Composition. — This superorder compris- es the orders Myodocopida Sars, 1866, and Halocyprida Dana, 1853. Order Halocyprida Dana, 1853 Composition. —This order comprises the suborders Cladocopina Sars, 1866, and Hal- ocypridina Dana, 1853. Suborder Halocypridina Dana, 1853 Composition. —This suborder comprises the superfamilies Halocypridoidea Dana, 314 1853, and Thaumatocypridoidea Muller, 1906. Superfamily Halocypridoidea Dana, 1853 Composition. —This superfamily con- tains the family Halocyprididae Dana, 1853. Family Halocyprididae Dana, 1853 Composition. —This family comprises the subfamilies Halocypridinae Dana, 1853, Conchoecinae Claus, 1891, Archiconchoe- cinae Poulsen, 1969, Euconchoecinae Poul- sen, 1969, and Deeveyinae Kornicker & II- iffe, 1985. Subfamily Deeveyinae Kornicker & Iliffe, 1985 Composition. —The subfamily comprises the genera Deeveya Kornicker & Iliffe, 1985, and Spelaeoecia Angel & Iliffe, 1987. Spelaeoecia Angel & Iliffe, 1987 Type species.—Spelaeoecia bermudensis Angel & Iliffe, 1987. Composition. —The genus is monotypic. Terminology. — The lettering of bristles on the first and second antennae is the same as for the genus Deeveya explained in Kor- nicker and Palmer (1987:610). On the eighth joint of the first antenna of Deeveya the base of the d-bristle is slightly more lateral than on Spelaeoecia. Therefore, it is proposed that the anterior bristle regardless of wheth- er it is lateral or medial be designated the d-bristle; the definitely lateral bristle near Fig. 1. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON midwidth of the joint and posterior to the d-bristle and stouter than other bristles on the joint be designated the e-bristle; the def- initely medial bristle near midwidth of the joint and with proximal part slightly angled ventrally be designated the f-bristle, and the posterior bristle that is lateral to the f-bristle and either slightly medial to, or at same level, as the e-bristle be designated the g-bristle (Fig. 2a). The e-bristle is the “‘prin- cipal bristle.”’ The terminology of the sixth limb is that suggested by Angel & Iliffe (1987: 551) in which the joint previously inter- preted to be the first exopodial joint is now designated the basale, and a terminal dorsal process on that joint is now designated the endopodite. Spelaeoecia bermudensis Angel & Iliffe, 1987 Fig. 1-5 Spelaeoecia bermudensis Angel & Iliffe, 1987:545, figs. 2-6.—Kornicker & Iliffe, 1989, fig. 29. Holotype. —USNM 228468, adult female on five slides. Type locality.—Green Bay Cave, Ber- muda. Material. —Wonderland Cave, Bermuda: USNM 193483, one adult male on slide and in alcohol; USNM 193484A, one adult fe- male in alcohol; USNM 193484B, one ju- venile (length 1.27 mm, height 0.74 mm) plus nine adult females, all in alcohol; all collected 4 Oct 1984 in baited trap at 0-1 m depth by Dr. Jan H. Stock. Also exam- ined: holotype, and 2 A-1 males (USNM 193404A, 193405A) from Jane’s Cave, Ber- — Spelaeoecia bermudensis, adult male, USNM 193483: a, Lateral view of specimen from left side showing representative surface lineations and some internal characters, length 1.37 mm; b, Dorsal view of carapace with valves partly open (dashed lines indicate ventral edges of valves); c, Detail of posterodorsal corner of carapace, from “‘a’’; d, Detail of posterior of right valve; e, Specimen showing relationship of appendages (Bellonci Organ, furca, copulatory organ, and appendages of left side; not all bristles of appendages shown); f, Bellonci Organ and joints | and 2 of left 2nd antenna; g, Anterior of body and upper lip from right side, anterior to right; h, Upper lip from left side, anterior to left; i, }, Upper lip, anterior and posterior views, respectively; VOLUME 102, NUMBER 2 315 gland a, lig, i, k, Ventral view of lower lip, anterior towards bottom. Abbreviations as follows: a.m. = adductor muscle attachment area of shell; B.O. = Bellonci Organ; c.o. = copulatory organ; endop. = endopodite; epip. = epipodite; exop. = exopodite; i.m. = inner margin of infold; mnd. = mandible; mx. = maxilla; r.v. = right valve; v.e. = valve edge. Ist = First antenna, 2nd = second antenna, 5th = fifth limb, 6th = sixth limb, 7th = seventh limb. Arabic numerals without a prefix refer to joints of endopodite or exopodite with | indicating proximal joint. Roman numerals identify endites with I indicating proximal endite. 316 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON “ Fig.2. Spelaeoecia bermudensis, adult male, USNM 193483: a, Left 1st antenna, lateral view; b, c, Endopodite of right 2nd antenna, medial and lateral views, respectively; d, Endopodite of left 2nd antenna, lateral view; e, Exopodite of 2nd antenna; f, Right 6th limb (only proximal part of all except dorsal epipodial bristles shown), lateral view; g, Left 7th limb, lateral view, ventral to left; h, Left lamella of furca, apron, and bifurcate unpaired bristle; i, Copulatory organ, anterior to left. For abbreviations, see Fig. 1. — Fig. 3. Spelaeoecia bermudensis, adult male, USNM 193483: a-d, Left mandible: a, Dorsal view of coxale endite, anterior to right; b, Lateral view of mandible (not all bristles of basale and none of 3rd endopodial joint VOLUME 102, NUMBER 2 317 Moy [( yl KW wl NT ha wht f shown); c, Detail of proximal set of teeth of coxale endite, from “‘a’’; d, Joints 2 and 3 of endopodite, medial view. e-g, Right mandible: e, Ventral view of outer distal set of teeth and part of proximal teeth of coxale endite (inner distal set not shown), anterior to right; f, Ventral view of proximal set of teeth, anterior to right; g, Lateral view of basale and joint | of endopodite, lateral view. Adult female, holotype, USNM 228468: h, i, bristles between proximal and distal sets of teeth of coxale endite: h, Ventral view of endite of right limb, anterior to right; 1, Dorsal view of endite of left limb, anterior to right. For abbreviations, see Fig. 1. 318 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON baa Z Z<--., /coxale ; recoxal Tt ie Nae basale / | coxale / pasale | \ XX \ III | II \ precoxale, I a a ; I \) | : Fig. 4. Spelaeoecia bermudensis, adult male, USNM 193483, maxilla: a, Right limb (bristles of endites not shown); b, Left limb (not all endite bristles shown); c—-e, Endites I-III of left limb (only proximal part of dashed bristle of endite II shown). For abbreviations, see Fig. 1. —= Fig. 5. Spelaeoecia bermudensis, adult male, USNM 193483, 5th limb: a, Lateral view of right limb (only proximal part of epipodial bristles shown); b, Lateral view of sensory organ of protopodite of left limb, anterior to left (epipodial bristles not shown); c, Medial view of endopodite of right limb, anterior to left; d, Ventral VOLUME 102, NUMBER 2 319 oblique view of sensory organ of protopodite of right limb, distal end of limb to lower right. For abbreviations, see Fig. 1. 320 muda, both discussed in Kornicker & Iliffe (1989). Description of adult male (Figs. 1—3g, 4, 5).—Carapace uncalcified, elongate; dorsal margin straight, ventral margin broadly convex; anterior incisur just dorsal to mid- height (Fig. la); in dorsal view carapace broadest near middle and narrowing pos- teriorly (Fig. 1b). Anterior edge of valve sin- uate and posterior to anterior end of ros- trum. Ornamentation: Surface with thin linea- tions (representative lineations near poste- rior of left valve illustrated in Fig. la), and few single hairs. Infold: Broad infold except along hinge, narrower just posterior to inner end of in- cisur (Fig. la). Narrow list distal to mid- width of infold extending from anteroven- tral to posteroventral corners of valve (Fig. la); a second list forming narrow bar pos- terior to posterior juncture of hinge, then extending ventrally as narrow list intersect- ing posterior edge of valve at midheight (Fig. lc, d); at intersection second list joins la- mellar prolongation of selvage suggesting that second list represents edge of valve and that segment of shell posterior to list is outer valve surface and similar in nature to outer surface of valve forming inner side of ros- trum. Glands (Fig. la—d): Posteroventral corner of right valve with about 10 minute glan- dular pores along dorsal edge. In lateral view posterodorsal corner (part bearing glands) of right valve extending dorsally past more rounded corner of left valve (Fig. 1c). Outer edge of that part of infold extending from incisur to midheight of posterior end of valve with about 18 minute broad tube-like glan- dular openings, mostly along anteroventral margin and anterior three-fourths of ventral margin (last opening just ventral to inter- section of valve margin and second list); minute bristles along valve edge, generally one or two between adjacent tube-like glan- dular openings. Selvage: With narrow unfringed prolon- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON gation extending from inner corner of in- cisur to midheight of posterior end of each valve. Posterior end of prolongation ends at intersection between valve edge and ven- tral end of second list. Size: USNM 193483, length 1.37 mm, height 0.78 mm. First antenna (Figs. le, f, 2a): With eight distinct joints (Fig. 2a). First joint with ter- minal ventral extension with long spines. Second joint with distinct dorsal bristle with indistinct rings; medial surface of joint with distal spines. Third joint with ventral bristle with base on lateral surface. Fourth joint about half length of third, with dorsal bristle reaching past eighth joint, and very long ventral bristle. Fifth joint shorter than fourth, with long ventral bristle about three- times length of a-bristle of seventh joint. Sixth joint about same length as fifth joint, bare. Seventh joint longer than sixth, with short spinous a-bristle, long ventral b-bris- tle, and longer ventral c-bristle. Eighth joint with d-bristle anterior and slightly medial to e-bristle and about '4 longer than a-bristle of seventh joint; e-bristle about twice length of d-bristle with indistinct proximal rings, f-bristle medial, bent ventrally, slightly shorter and narrower than e-bristle, g-bris- tle about same length as f-bristle. Long bris- tles of fourth, fifth, seventh, and eighth joints with indistinct minute marginal spines and longer terminal spine. Second antenna (Figs. le, 2b—e): Proto- podite bare (Fig. le). Endopodite three- jointed (Fig. 2b—d): First joint elongate with two slender spinous a- and b-bristles (a- bristle about two-thirds length of b-bristle); second joint with short c- and d-bristles with distal spines, one short lateral e-bristle, one long f-bristle, and one long g-bristle (g-bris- tle longer, stouter, and medial to f-bristle); third joint with long equilength h-, i-, and j-bristles, and terminal club-like process (process of right limb longer and stouter than that of left limb); long bristles of second and third joints with terminal papilla. Exopod- ite with nine joints (Figs. le, 2e): First joint VOLUME 102, NUMBER 2 divided into long proximal and short distal segments (well developed separation of seg- ments in sclerotized dorsal (concave) edge but not in ventral (convex) edge), and with long terminal bristle (with minute ventral spines) reaching well past ninth joint; bris- tles of joints two to eight stouter than bristle of first joint and with natatory hairs; ninth joint with four bristles (1 minute bare, one short with slender ventral spines, two long with natatory hairs). Mandible (Figs. le, 3a—g): Coxale endite with proximal and distal sets of teeth sep- arated by space (Fig. 3a—c, e, f): proximal set comprising four stout cusps and with indistinct spinous bristle at each end; sur- face between cusps and proximal to cusps with slender spines; stout tooth and four spinous bristles between proximal and dis- tal sets of teeth. Distal set of teeth com- prising two flat teeth, each with seven cusps; one stout curved process and one small bris- tle proximal to flat teeth. Basale (Fig. 3b, g): distal edge with five terminal triangular cusps, one sharper triangular anterior cusp, and a smaller posterior cusp; lateral surface near distal edge with sharp tooth near mid- width; lateral surface at or distal to mid- length with one small bristle and five longer bristles; anterior margin with one long bris- tle distal to midlength; posterior margin hir- sute, with two distal ringed bristles (proxi- mal with slender tip, distal tubeformed); proximal medial surface with transparent plumose bristle on protuberance, and one short bristle near endopodite (Fig. 3g); two transparent plumose bristles present on or close to dorsal margin; lateral surface near insertion of endopodite with one long bare bristle. Endopodite (Figs. le, 3b, d, g): First joint with three bristles (one short, ventral, one long, medial, and one long, terminal, dorsal); second joint widening distally, with three terminal dorsal bristles (one claw-like, unringed, two ringed), one long unringed subterminal ventral bristle, and minute spines on dorsal margin and lateral surface near dorsal margin; third joint with two long 321 stout claw-like spinous terminal bristles, four short ringed bristles forming medial row along terminal edge, and one longer ringed bristle on terminal lateral edge; anterior margin and medial surface of third joint hir- sute. Maxilla (Figs. le, 4): Endite I with two proximal and nine terminal bristles (three tubeformed) (Fig. 4c); endite II with two proximal and eight terminal bristles (two tubeformed) (Fig. 4d); endite III with one long proximal bristle and six terminal bris- tles (two tubeformed) (Fig. 4e); some bris- tles on each endite stout pectinate. Basale with long stout dorsal bristle with long mar- ginal spines and one long ventral bristle with long marginal spines (Fig. 4a, b); division of basale and first endopodial joint indicat- ed only by separation at dorsal edge, else- where joints appearing fused. Endopodite (Fig. 4a, b): First joint with five anterior bristles (four proximal, one distal), two proximal bristles near posterior margin, and six distal bristles on or near posterior mar- gin (because of orientation of limb on slide, the six distal bristles of the illustrated left maxilla are not close to the posterior mar- gin); end joint with two stout claw-like bris- tles and five slender ringed bristles, and hairs along surface anterior to claws and bristles. Fifth limb (Figs. le, 5): Epipodite with bristles forming three groups, each with four (dorsal group), six, and five plumose bristles (Fig. 5a). Protopodite with long striate sen- sory organ with many minute papillae at tip, and two endites (Fig. 5a, b, d): endite I with three bristles with long spines; endite II with four bristles (two with spines, two tube- formed). Basale with medial hairs, one long anterior bristle with long spines, two prox- imal medial bristles with short spines, and six ventral bristles (two pectinate claw-like, three tubeformed and either bare or with short spines, one with long spines) (Fig. 5a). Endopodite with medial hairs, one proxi- mal medial bristle (with short spines) and eight additional bristles (one short tooth- like medial, two tubeformed, two claw-like, 322 two plumose, one long bare lateral) (Fig. 5a, c). First exopodial joint weakly divided into broad proximal and narrower distal parts (Fig. 5a): proximal part with eight bristles (three slender bare ventral bristles, one long plumose lateral bristle near ventral margin, one spinous medial distal bristle near ven- tral margin, one very long lateral plumose distal bristle at midheight of joint, one spi- nous lateral bristle near dorsal margin, and One spinous distal dorsal bristle); distal part with four bristles (one long subterminal bare dorsal bristle and three shorter bristles on or near ventral margin). Second exopodial joint: dorsal margin with one bare distal bristle; ventral margin with four slender bristles (bare or with short marginal spines) at midlength. Third exopodial joint with two stout claw-like unringed bristles (longer with indistinct minute ventral spines, other bare) and one slender bare ringed ventral bristle. Sixth limb (Figs. le, 2f): Epipodite with bristles forming three groups, each with six, six, and five plumose bristles (Fig. 2f). Pro- topodite separated from basale by distinct suture and separated into two shallow lobes by ventral indentation and suture not reach- ing dorsal margin: proximal part with four ventral bristles, all with long spines; distal part with five bristles (four with long spines, One with short spines). Basale with six plu- mose bristles on or near ventral margin, and one distal lateral bristle at about midwidth ofjoint. Endopodite single-jointed with four long bristles (three with long spines, one bare). Exopodite three-jointed: first joint with four bare ventral bristles; second joint with three bare bristles (two ventral, one dorsal); third joint with three bristles (mid- dle bristle claw-like with short ventral spines, dorsal bristle bare, tending to be claw-like, with oblique rings, ventral bristle bare). Protopodite and basale with long medial hairs. Seventh limb (Figs. le, 2g): Elongate with three long terminal bristles. Furca (Figs. le, 2h): Each lamella with PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON eight claws; claw 1 with two weak transverse sutures, claw 3 with three, claw 4 with two, claw 5 with one; claw 2 broken off near base; left lamella slightly anterior to right. Un- paired bristle bifurcate. Bellonci organ (Fig. le, f): Elongate with suture at proximal third, bifurcating at about two-thirds length; each branch with round- ed tip just reaching third joint of first an- tenna. Lips (Fig. 1g—-k): Anterior face with two small triangular processes (one on each side) and small glandular processes forming row on each side (four—six processes in each row) (Fig. 1g—i). Terminal posterior edge with a minute spine-like process and slender spines at each side of shallow median concavity (Fig. 1h, 1). Lower lip with triangular process on each side of mouth (Fig. 1k). Copulatory organ (Figs. le, 21): On left side of body and consisting of two parts: posterior rod-shaped organ with very long styliform process with hirsute tip; anterior part broad with slight knee-like bend at about distal two-thirds and terminating in foot-shaped process with rows of minute teeth in “‘heel”’ area. Apron (Fig. 2h): Reaching about three- fourths length of anterior margin of furcal lamellae. Supplementary description of adult fe- male (Fig. 3h, 1).—Size (mm): USNM 193484A, length 1.52, height 0.86; USNM 193484B, six specimens (length:height): 1.54:0.91, 1.49:0.85, 1.49:0.82, 1.43:0.83, 1.53:0.85, 1.46:0.83. Range: length 1.43- 1.52 mm, height 0.82—0.91 mm. Because some specimens were measured with valves slightly open, height measurement is less accurate than that of length. (Angel & Iliffe (1987:545) gave the dimensions of three fe- males: range of lengths 1.58—1.64 mm. They also presented (Fig. 7) a shell length-width graph with dimensions of 21 females having a length range of about 1.41—1.64 mm. Kor- nicker & Iliffe (1989) gave the dimensions of two females with lengths of 1.54 mm and VOLUME 102, NUMBER 2 1.57 mm. The lengths of the females in the present collection fall within the range of previous collections.) First antenna: Ventral bristle of fourth joint about same length as a-bristle of sev- enth joint; limb otherwise similar to that of adult male. Mandible (Fig. 3h, i): Similar to that of male. The exact number of bristles adjacent to the stout tooth between proximal and distal sets of teeth of the coxale endite is difficult to resolve; it is interpreted to be four herein (Fig. 3h, i), but could be only three. Angel & Iliffe (1987:547, fig. 4B) in describing the coxale stated, ““Between outer and middle list single long curved spine.” The spine is present on one limb of the ho- lotype but not on the other, and examina- tion of the “‘spine”’ under oil immersion re- vealed it to be debris. Sexual dimorphism. —The carapace of the single adult male (length 1.37 mm) is short- er than known females (range of length 1.41- 1.64 mm). The ventral bristle of the fourth joint of the first antenna is about the same length as the a-bristle of the seventh joint on the adult female and almost three-times the length on the adult male. The fifth limb of the adult male bears a well developed sensory organ not previously reported in the halocyprids. The fifth limbs of two adult females (Holotype and USNM 193484A) and 2 A-1l males (USNM_ 193404A, 193405A) were examined and found not to have a sensory organ; the A-1 males are from Jane’s Cave, Bermuda, and were dis- cussed in Kornicker & Iliffe (1989). Discussion. — Although classed in the Halocypridoidea, the Deeveyinae in many nonsexual characters appear to be a link be- tween the Thaumatocypridoidea and Hal- ocypridoidea. This relationship is also ev- ident when comparing the copulatory organs of adult males in the two superfamilies. The copulatory organ of the adult male S. ber- mudensis has the rod-shaped process sep- 323 arate from the broader anterior lobe, similar to the copulatory organ of thaumatocyprids. In halocyprids other than S. bermudensis the rod-shaped process of the adult male lies inside a canal within the anterior lobe. Ju- venile males of both thaumatocyprids and halocyprids have the rod-shaped process separate from the anterior lobe suggesting that having the rod-shaped process inside a canal within the anterior lobe is an apo- morphic character state. The endopodite of the adult male second antenna of S. bermudensis differs from those generally present in both thaumatocyprids and hal- ocyprids in having a straight rather than hook-shaped clasper. Not all halocyprids have a clasper. Acknowledgments I thank Dr. Jan H. Stock, Institut voor Taxonomische Zoology, Zodlogisch Mu- seum, Amsterdam, Nederland, for the os- tracodes from Wonderland Cave, Mr. Jack Schroeder for inking my camera lucida drawings, and Ms. Elizabeth Harrison-Nel- son for general assistance. Literature Cited Angel, M. V., & T. M. Iliffe. 1987. Spelaeoecia ber- mudensis, new genus, new species, a halocyprid ostracod from marine caves in Bermuda.— Journal of Crustacean Biology, 7(3):541-553. Kornicker, L. S., & T. M. Iliffe. 1989. Ostracoda (Myodocopina, Cladocopina, Halocypridina) mainly from Anchialine Caves in Bermuda.— Smithsonian Contributions to Zoology 470: 1-88. ,& R. J. Palmer. 1987. Deeveya bransoni, a new species of troglobitic halocyprid ostracode from anchialine caves on South Andros Island, Bahamas (Crustacea: Ostracoda). — Proceedings of the Biological Society of Washington, 100(3): 610-623. Department of Invertebrate Zoology, Na- tional Museum of Natural History, Smith- sonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 324-330 NEW RECORDS OF ENTOCYTHERID OSTRACODS INFESTING BURROWING CRAYFISHES, WITH THE DESCRIPTION OF A NEW SPECIES, ASCETOCYTHERE STOCKERI Horton H. Hobbs, Jr., and Daniel J. Peters Abstract.—New records of the occurrence of entocytherids on burrowing crayfishes are reported from Kentucky, North Carolina, Virginia, and West Virginia. These include members of the genera Ascetocythere (3), Dactylocythere (3), Donnaldsoncythere (1), Entocythere (2), and Uncinocythere (2). Ascetocyth- ere Stockeri, a close relative of A. cosmeta, is described from four localities in the Ohio Basin in Mason and Cabell counties, West Virginia, and a single locality in Carter County, Kentucky. In their study of burrowing crayfishes, Raymond F. Jezerinac and G. Whitney Stocker, of Ohio State University, Newark, saved the detritus from containers in which the crayfishes were preserved and have kindly permitted us to study the ostracods that were entrapped in it. Of the 20 samples received, 15 from the Ohio, Potomac, and Tennessee watersheds contained entocyth- erids among which were representatives of 11 species belonging to 5 genera. These were infesting six species of crayfishes (the iden- tities of which were furnished to us by Messrs. Jezerinac and Stocker), five of which are largely restricted to burrows. The as- sociations of the ostracods and their crayfish hosts in the 15 localities are recorded below. For each species of ostracod, the original description and the first use of the currently accepted orthography are cited. These are followed by a list of the new localities, cray- fish hosts, and remarks on the ecological and geographic distribution of the species. Except as noted otherwise, the ostracods are deposited in the National Museum of Natural History, Smithsonian Institution. Ascetocythere cosmeta Hobbs & Hart Ascetocythere cosmeta Hobbs & Hart, 1966: 46, figs. 24, 25. [Type locality: 4 mi N of jct of St. Rte. 89 and Blue Ridge Parkway, Grayson Co., Virginia. Host: Cambarus dubius Faxon.] New record.—North Carolina: Ashe County [New Basin], burrows near un- named trib of North Fork of New River on county road, 0.1 mi E of Crumpler, 8.8 mi NE of West Jefferson, 11 Aug 1984, G. W. Stocker, R. F. Jezerinac, and R. F. Thoma, host: Cambarus (Jugicambarus) dubius Faxon, associates: Dactylocythere daph- nioides (Hobbs, 1955), Entocythere harrisi Peters, 1975, and Uncinocythere simondsi (Hobbs and Walton, 1960). Habitat. —Crayfish burrows. Distribution. —The Catawba and New ba- sins in Alleghany, Ashe, and Avery coun- ties, North Carolina, and Grayson County, Virginia. Ascetocythere hyperoche Hobbs & Hart Ascetocythere hyperoche Hobbs & Hart, 1966:41, figs. 12, 13. [Type locality: trib. of Cherokee Reservoir, 0.5 mi W of ject of U.S. Hwys. 11E and 25E, Grainger Co., Tennessee. Host: Orconectes spinosus (Bundy), Cambarus (Hiaticambarus) lon- girostris Faxon, and Cambarus (C.) bar- tonii cavatus Hay.]| VOLUME 102, NUMBER 2 325 Pig. |. Ascetocythere stockeri, new sp.: a, Copulatory complex of holotypic male; b, Right valve of shell of holotype; c, Same of paratypic female (two irregular, overlapping masses in interior Ova). New records.— Virginia: Russell County [Holston Basin], floodplain of tributary to Big Moccasin Creek on County Rd 657, 0.9 air mi W of Hansonville, 15.9 air mi N of Bristol, 9 Aug 1986, G.W.S. and R.F.J., host: Cambarus (Jugicambarus) dubius Faxon, associate, Donnaldsoncythere donnaldson- ensis (Klie 1931). Habitat.—Probably largely confined to crayfish burrows. Distribution.—This ostracod was previ- ously known only from the type locality in the Holston River basin in Grainger Coun- ty, Tennessee, where Hobbs and Hart re- ported the hosts to be three stream-dwelling crayfishes. Ascetocythere stockeri, new species Figs Diagnosis. —Eye pigmented and located about one-sixth shell length from anterior margin. Shell (Fig. 1b) ovate with greatest height about one-third shell length from posterior end where about 1.5 times height at level of eye; margin entire, lacking emar- ginations and prominences. Submarginal setae present except dorsally. Copulatory complex (Fig. la) with peni- ferum expanded ventrally in bubiform en- largement following conspicuously slender constricted section about one-fourth of length of peniferum from distal extremity; anterior process lacking; ventral process digitiform extending ventrally much be- yond other processes; posterior process rep- resented by two acute teeth. Penis very prominent, spermatic and prostatic ele- ments not contiguous throughout their lengths, both C-shaped and emerging ven- trally at base of ventral process between it and small cephaloventrally directed lobe. Clasping apparatus broadly arched, obliter- ating junction of vertical and horizontal rami; postaxial border entire; preaxial bor- 326 Table 1—Measurements (in mm) of Ascetocythere stockeri, n. sp. Holotype Males (14) Females (5) Length (range) 0.39 0.35-0.43 0.39-0.42 Average 0.38 0.41 Height (range) 0:23 0.21-0.25 0.22-0.25 Average 0.23 0.24 der with three teeth grouped on thickened distal fifth. Dorsal finger moderately heavy and about one-half as long as curved, more slender ventral finger. Triunguis female.—Eye located about one-sixth shell length from anterior end. Shell (Fig. 1c) subovate, weakly concave in anterior three-fifths. Greatest height dis- tinctly posterior to midlength where about 1.4 times that at level of eye. Submarginal setae present except dorsally. Genital ap- paratus supported by pair of ribs extending dorsomesially from complex of supports at base of third leg. Apices of ribs in contact with small, subspherical, homogeneous, hyaline body embraced dorsally and pos- teriorly by larger, heterogeneous mass. For measurements, see Table 1. Type locality: Chief Cornstalk Hunting Grounds Campground, 2.1 miles southwest of Beech Hill, 10.1 mules southeast of Gallipolis, Mason County, West Virginia [Kanawha Basin], where it was found in a collection of crayfishes containing represen- tatives of three species: Cambarus (Jugi- cambarus) dubius Faxon, Cambarus (La- cunicambarus) diogenes Girard, and Cambarus (C.) bartonii cavatus Hay. These specimens were collected on 20 Apr 1986 by G. Whitney Stocker, Dave Chrisman, and R. F. Jezerinac. Disposition of types: The holotypic male is deposited in the National Museum of Natural History (Smithsonian Institution), USNM 240114. Paratypes are in the col- lections of H. H. Hobbs III and the Smith- sonian Institution. Hosts: Cambarus (C.) bartonii cavatus PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Hay, C. (Jugicambarus) dubius Faxon, and C. (Lacunicambarus) diogenes Girard. C. (J.) dubius was present in all of the collec- tions containing specimens of Ascetocythere stockeri, and we think it unlikely that this ostracod occurs on the first and last named crayfishes. Entocytherid associates: Dactylocythere macroholca Hobbs & Hobbs, 1970; Don- naldsoncythere donnaldsonensis (Klie, 1931); Entocythere elliptica Hoff, 1944; and Uncinocythere zancla Hobbs & Walton, 1963. Range and specimens examined: Nine- teen specimens from the following locali- ties. Kentucky: Carter County [Little Sandy Basin], (1) roadside ditch along Dry Fork 1.5 air mi S of Willard, 1 Sep 1986, Dave Hile, G.W.S., and R.F.J., host: C. (/.) du- bius, associates: Dactylocythere macroholca Hobbs & Hobbs, Entocythere elliptica Hoff, and Uncinocythere zancla Hobbs & Walton. West Virginia: Mason County [Kanawha Basin], (2) Type locality; (3) 3 mi S of type locality and 2.7 mi SE of Arlee, 2 May 1987, G. Lombardo, R. French, and G.W.S., host: C. J.) dubius, no ostracod associates. Cabell County [Ohio Basin], (4) Spurlock Creek on Union Ridge Rd, 1 mi S of St. Rte. 2, 1.8 mi N of Union Ridge, 3 May 1987, R.F., D. Chrisman, G.L., R.F.J., and G.W:S., host: Cambarus (J.) dubius, associate, Dn. don- naldsonensis; (5) along Brian Creek Rd, S of Union Ridge Rd, 4.4 mi S of Glenwood, 3.May 1987, G.L., R.F., D.G., Roe eae G.W.S., host: C. (J.) dubius, associate: Dn. donnaldsonensis. Relationships: Ascetocythere stockeri is a member of the Coryphodes Group (Hobbs & Hart 1966:44), characterized by the teeth on the preaxial margin of the clasping ap- paratus being grouped distally. Its closest relative is probably A. cosmeta Hobbs & Hart, 1966, from which it differs most con- spicuously in lacking an anterior process on the peniferum. It differs from the other members of the group, A. coryphodes Hobbs & Hart, 1966, and A. myxoides Hobbs & VOLUME 102, NUMBER 2 Hart, 1966, in lacking a snoutlike promi- nence on the anterior surface of the bulbous part of the peniferum. Etymology: This ostracod is named in honor of G. Whitney Stocker, who collected or participated in collecting most of the ma- terials on which this report is based. Dactylocythere crawfordi Hart Dactylocythere crawfordi Hart, 1965:255, figs. 1, 2. [Type locality: Macacheek Creek on St. Rte. 287, Logan Co., Ohio. Host: Cambarus (Lacunicambarus) diogenes Girard. ] New record. —West Virginia: Mason County [Ohio Basin], wet field along St. Rte. 2, 2.0 mi S of U.S. Hwy. 35, 1.5 air mi E of Gallipolis, 19 Apr 1986, D.C., R.F.J., G.W.S., host: Fallicambarus (Creaserinus) fodiens (Cottle). Habitat. —Crayfish burrows. Distribution.—Ohio River Basin: White and Wabash drainages in Indiana, Little Miami, Scioto, and Symmes Creek in Ohio, and in Mason County, West Virginia. Dactylocythere daphnioides (Hobbs) Entocythere daphnioides Hobbs 1955:325, figs. 1, 2, 5, 6-9. Dactylocythere daphnioides.—WHart, 1962: 130. New record.—North Carolina: Ashe County [New Basin], burrows near trib to North Fork of New River, 0.1 mi E of Crumpler; 8.8 mi NE of West Jefferson, 11 Aug 1984, R.F.J., G.W.D., R.F.T., host: C. (J.) dubius, associates: As. cosmeta, E. har- risi, and U. simondsi. Habitat.—Except for the record cited above, all known specimens have been found on crayfishes living in lotic habitats. Distribution. —“‘From headwaters of the Little Tennessee and Pee Dee drainage sys- tems in North Carolina northward to the New and Big Sandy systems in Virginia and West Virginia. The Kentucky and Missouri 327 localities cited by Hart and Hart (1974:56) should be confirmed’ (Hobbs & Peters, 1977:28). Dactylocythere macroholca Hobbs & Hobbs Dactylocythere macroholca Hobbs & Hobbs 1970:6, fig. 3a-d. New record.—Kentucky: Carter County [Little Sandy Basin], roadside ditch 1.5 air mi S of Willard, near Lawrence Co line, 1 Sep 1986, D.H., R.F.J., G.W.S., host: C. (/.) dubius, associates, As. stockeri, E. elliptica, and U. zancla. Habitat. — Burrows and streams. Distribution. —Ohio River Basin in Ken- tucky: Barren, Licking, and Little Sandy wa- tersheds. Donnaldsoncythere donnaldsonensis (Klie) Entocythere donnaldsonensis Klie, 1931: 334-341, figs. 1-9. [Type locality: Don- ald’s Cave, Lawrence County, Indiana. Host/s: uncertain; however, probably Or- conectes inermis inermis Cope and/or Cambarus (Erebicambarus) tenebrosus Hay. Donnaldsoncythere donnaldsonensis. — Hart, 1962:131. New record. — Kentucky: Lawrence Coun- ty [Big Sandy Basin], (1) roadside ditch 1.3 air mi NW of Webbyville, 1.4 air mi S of Willard, 1 Sep 1986, D.H., G.W.S., and R.F.J., host: C. (J.) dubius, associates: none. Lewis County [Licking Basin], (2) seep on St. Rte. 24, 3.8 mi E of county line, 2 air mi E of Foxport, 9 Jun 1984, G.W.S., Diane M. Williams, R.F.J., host: C. (J.) dubius, no associates. Virginia: Russell County [Hol- ston Basin], (3) floodplain along trib of Big Moccasin Creek on Co Rd 657, 0.9 air mi W of Hansonville, 15.8 air mi N of Bristol, 9 Aug 1986, G.W.S. and R.F.J., host: C. (J.) dubius, associate: As. hyperoche. West Vir- ginia: Barbour County [Tygart Basin], (4) roadside ditch 0.8 mi E of U.S. Hwy. 119 328 on Arden Rd, 1.3 air mi NE of Hopewell, R.F.J. and G.W:S., hosts: C. (J.) dubius, C. (J.) diogenes, no associates. Cabell County [Ohio Basin], (5) burrows along Brian Creek Rd, S of Union Ridge Rd, 4.4 mi S of Glen- wood, 3 May 1987, Greg Lombardo, Randy French, Dave Chrisman, R.F.J.,and G.W.S.., host: C. (J.) dubius, associate: As. stockert; (6) burrows on Union Ridge Rd, 1 mi S of St. Rte. 2, 1.75 mi N of Union Ridge, G.L., RF) D:.Ga RES and Giw'8:vhest €. Gs) dubius, associate: As. stockeri. Grant Coun- ty [Potomac Basin], (7) roadside ditch on Forest Rd 75, 10.2 air mi NW of Peters- burg, 28 Jun 1986, D.C. and G.W.S., host: C. (J.) monongalensis, no associates. Ma- son County [Kanawha Basin], (8) see type locality of As. stockeri, (9) burrows along dirt road 3 mi S of Chief Cornstalk Hunting Ground Campground, 2.7 mi SE of Arlee, 2 May 1987, G.L., R.F., and G.W:S. (8) See Locality “2” for As. stockeri. Pocahontas County [Greenbrier Basin], (10) seep in Falls of Hills Creek Scenic Area off St. Rte. 39, 1.6 mi E of Greenbrier Co line, 11.1 air mi ESE of Richwood, 7 Jul 1985, V.L. Stocker and G.W.S., host: C. (J.) monongalensis, no associates. Habitat. — All of the records cited above are based on specimens collected from bur- rowing crayfishes. This ostracod, however, inhabits a wide range of epigean and hy- pogean habitats. Distribution. —‘‘From northern Georgia to Indiana and Maine”? (Hobbs & Peters 1977:44). All of the localities cited since this summary statement appeared (Hobbs & Pe- ters, 1982:312; and Hobbs & McClure 1983: 772-778) lie within these limits. Entocythere elliptica Hoff Entocythere elliptica Hoff, 1944:328, figs. 15-21. [Type locality: north of Fargo, Clinch County, Georgia. Host: Procam- barus (Ortmannicus) seminolae Hobbs.] New record.—Kentucky: Carter County PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON [Little Sandy Basin], roadside ditch 1.5 air mi S of Willard near Lawrence County line, 1 Sep 1986, D.H., G.W.S., R.F.J., host: C. (J.) dubius, associates: As. stockeri, Dt. ma- croholca, and U. zancla. Habitat.— Burrows and lentic and lotic habitats. Distribution. —“‘Hart & Hart (1974:[87-— 88], 90) recorded the presence of E. elliptica and/or E. internotalus from Texas to North Carolina and from Kentucky to Florida, and Peters (1975:34) reported it from a number of localities in the James River watershed in Virginia’ (Andolshek & Hobbs, 1986: 31). The locality cited above extends the range diagonally across the entire state of Kentucky. Entocythere harrisi Peters Entocythere harrisi Peters, 1975:32, figs. 5-7. New record.—North Carolina: Ashe County [New Basin], burrows near trib of North Fork of New River, 0.1 mi E of Crumpler; 8.8 mi NE of West Jefferson, 11 Aug 1984, R.F.J., G.W.S., R.F.T., host: C. (J.) dubius, associates: As. cosmeta, Dt. daphnioides, and U. simondsi. Habitat. —Burrows and lotic habitats. Distribution. —On the Atlantic versant from the York River Basin in Virginia southward through the Catawba Basin in North Carolina, and the New River Basin in Ashe County, North Carolina. Uncinocythere simondsi (Hobbs & Walton) Entocythere simondsi Hobbs & Walton, 1960:17, figs. 1-10. Uncinocythere simondsi. — Hart, 1962:138. New record. —North Carolina: Ashe County [New Basin], burrows near trib of North Fork of New River, 0.1 mi E of Crumpler; 8.8 mi NE of West Jefferson, 11 Aug 1984, R.F.J., G.W.S., R.F.T., host: C. VOLUME 102, NUMBER 2 (J.) dubius, associates: As. cosmeta, Dt. daphnioides, and E. harrisi. Habitat. — Burrows and a broad range of epigean lotic and lentic habitats. Distribution. —From Illinois, Kentucky, and North Carolina southward to Missis- sippi and northern Florida (Hart & Hart 1974; Hobbs & Peters 1977, 1982; Andol- shek & Hobbs 1986). Uncinocythere zancla Hobbs & Walton Uncinocythere zancla Hobbs & Walton 1963:456, figs. 1-3. New record.—Kentucky: Adair County [Green Basin], burrows along St. Rte. 205, 0.8 mi NE of Neatsville, 10 mi N of Russell Springs, 15 Mar 1987, G.W.S. and R.F-.J., host: Cambarus (Jugicambarus) sp.?; no as- sociates; Carter County [Little Sandy Ba- sin], roadside ditch 1.5 air mi S of Willard near Lawrence County line, 1 Sep 1986, D.H., G.W.S., R.F.J., host: C. (J.) dubius, associates: As. stockeri, Dt. macroholca, and E. elliptica. Habitat.—This ostracod has been found most frequently infesting stream-dwelling crayfishes, but has also been found associ- ated with a troglobitic species in Hart Coun- ty, Kentucky, and with the burrower cited above. Distribution. —Known only from the Kentucky, Green, and Little Sandy wa- tersheds in Kentucky, and the Cumberland and Tennessee basins in Tennessee. Acknowledgments We are grateful to Raymond F. Jezerinac and G. Whitney Stocker for making possible our study of the material gleaned from their collections of burrowing crayfishes. Our thanks are also extended to C. W. Hart, Jr., of the Smithsonian Institution, and H. H. Hobbs III, of Wittenburg University for their criticisms of the manuscript. 329 Literature Cited Andolshek, Margaret D., & Horton H. Hobbs, Jr. 1986. The entocytherid ostracod faunas of southeast- ern Georgia.—Smithsonian Contributions to Zoology 424:1-—43. Hart, C. W., Jr. 1962. A revision of the ostracods of the family Entocytheridae.— Proceedings of the Academy of Natural Sciences of Philadelphia 114(3):121-147. 1965. New entocytherid ostracods and dis- tribution records for five midwestern states. — Transactions of the American Microscopical Society 84(2):255-259. Hart, Dabney G., & C. W. Hart, Jr. 1974. The os- tracod family Entocytheridae.—Academy of Natural Sciences of Philadelphia Monograph 18: ix + 239 pages. Hobbs, Horton H., Jr. 1955. Ostracods of the genus Entocythere from the New River system in North Carolina, Virginia, and West Virginia. — Trans- actions of the American Microscopical Society 74(4):325-333. , & C. W. Hart, Jr. 1966. On the entocytherid ostracod genera Ascetocythere, Plectocythere, Phymocythere (gen. nov.), and Cymocythere with descriptions of new species. — Proceedings of the Academy of Natural Sciences of Philadelphia 118(2):35-61. ——, & H. H. Hobbs, III. 1970. New entocytherid ostracods with a key to the genera of the subfam- ily Entocytherinae.— Smithsonian Contribu- tions to Zoology 47:1-19. —., & Auden C. McClure. 1983. Ona small col- lection of entocytherid ostracods with the de- scriptions of three new species. — Proceedings of the Biological Society of Washington 96(4):770— WIS). ——., & Daniel J. Peters. 1977. The entocytherid ostracods of North Carolina.—Smithsonian Contributions to Zoology 147:1-73. , and . 1982. The entocytherid ostracod fauna of northern Georgia. — Proceedings of the Biological Society of Washington 95(2):297-318. , & Margaret Walton. 1960. Three new ostra- cods of the genus Entocythere from the Hiwas- see drainage system in Georgia and Tennes- see.—Journal of the Tennessee Academy of Science 35(1):17—23. 1963. Three new ostracods (Ostracoda, En- tocytheridae) from the Duck River drainage in Tennessee.—American Midland Naturalist 69(2):456-461. Hoff, C. Clayton. 1944. New American species of the ostracod genus Entocythere.—American Mid- land Naturalist 32(2):327-357. 330 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Klie, W. 1931. Campagne spéologique de C. Bolivar et R. Jeannel dans l’Amérique du Nord (1928) 3: Crustacés Ostracodes.—Biospeologica: Ar- chives de Zoologie Expérimentale et Générale 71(3):333-344. Peters, Daniel J. 1975. The entocytherid ostracod fauna of the James and York River basins with a description of a new member of the genus Entocythere. — Virginia Polytechnic Institute and University, Research Division Bulletin 93:i11 + 50. (HHH) Department of Invertebrate Zo- ology, National Museum of Natural His- tory, Smithsonian Institution, Washington, D.C. 20560; (DJP) York High School, 9300 George Washington Highway, Yorktown, Virginia 23692. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 331-338 PSEUDOCYCLOPS LEPIDOTUS, A NEW SPECIES OF DEMERSAL COPEPOD (CALANOIDA: PSEUDOCYCLOPIDAE) FROM THE NORTHWESTERN PACIFIC Douglas J. Barr and Susumu Ohtsuka Abstract. —Pseudocyclops lepidotus, is described from Kuchinoerabu Island, off Kyushu, Japan. The main diagnostic characters are the lateral clefts in pediger 5, foliaceous urosomal scales, and structure of the fifth legs in both Sexes. Although most oceanic calanoid cope- pods are planktonic, many coastal species are demersal and occupy restricted habitats on or near the substrate. Such species may be overlooked or misidentified owing to their small size and resemblance to cyclopoid co- pepods. Several families of calanoids are comprised entirely of demersal species, the largest and most widely distributed of these being the family Pseudocyclopidae Gies- brecht, 1893. This family is monogeneric, containing only the genus Pseudocyclops Brady, 1872. Pseudocyclops at present contains 26 de- scribed species, 15 of which have been col- lected only from the North Atlantic. Only three species have been described from the Pacific: P. australis Nicholls, 1944, from southern Australia; P. pacificus Vervoort, 1964, from the Caroline Islands; and P. bi- lobatus Dawson, 1977, from southern Cal- ifornia. P. australis was subsequently re- ported by Tanaka (1966) from Kyushu, Japan, close to the type locality of the new species described below. Our specimens were obtained with a hand-held plankton net while using SCUBA over a coral sandy bot- tom at a depth of 9 m off Kuchinoerabu Island, Kyushu, Japan. Pseudocyclops lepidotus, new species Figs. 1-5 Material. —Dissected female holotype (USNM 229956), and dissected male allo- type (USNM 229957) collected 10 Sep 1986 from Nishino-Hama, Kuchinoerabu Island, Kagoshima Prefecture, Japan. Two female paratypes (USNM 229958), one dissected on slides and one whole, collected on same date from same locality. Description. — Female (Fig. 1A, B): length 0.90 mm, body compact, prosome oval in dorsal view; cephalosome partly fused with pediger 1, produced anteroventrally into acute rostrum (Fig. 1C); pediger 5 separate from pediger 4, with dorsolateral cleft bear- ing small seta (Figs. 1B, D; 5A). Urosome (Fig. 1E) 4-segmented, segments bearing transverse rows of subtriangular foliaceous scales, many of which have fallen off during dissection (Fig. 5B); genital segment longer than following segments combined, open- ings widely separate; segment 3 (Fig. 5C) with two dorsal processes reaching mid- length of caudal rami; anal segment re- duced, telescoped into segment 3; caudal ramus serrate posterodorsally, bearing one dorsal, one lateral and four apical setae. First antenna (Fig. 1F, G) 20-segmented, reaching posterior end of first pediger; seg- ment 1 with rows of anterior surface spi- nules, three large esthetascs; suture between segments 17 and 18 incomplete. Second antenna (Fig. 2A) with basipodal segments each bearing one seta on disto- medial margin; endopod three-segmented, segment | with two setae on medial margin and small spinules on outer distal margin, 332 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON yy i WH ° 9 0.2 mm Fig. 1. Pseudocyclops lepidotus, female: A, Habitus, dorsal; B, Habitus, lateral; C, Rostrum, ventral; D, Pedigers 4—5, lateral; E, Urosome, dorsal; F, First antenna; G, First antenna, segment 1. VOLUME 102, NUMBER 2 333 WAGE WY | AWM ANN ‘a Fig. 2. Pseudocyclops lepidotus, female: A, Second antenna; B, Mandible; C, First maxilla; D, Second maxilla; E, Maxilliped, posterior; F, First leg, anterior. 334 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 4 Vie vyy y ry ‘ , "tre Wry ayt yoy a y ve YANN SS E ayy yw - v awe Y. v Fig. 3. Pseudocyclops lepidotus, female: A, Second leg, anterior; B, Third leg, anterior; C, Fourth leg, anterior; D, Fifth leg, anterior. VOLUME 102, NUMBER 2 335 Se —) sy x & f Vt ae V7. S ee OG, op ni AIS \ : WAN) \ VAN I ZZNZW YN’ Fig. 4. Pseudocyclops lepidotus, male: A, Habitus, dorsal; B, Urosome, dorsal; C, Right first antenna; D, Left fifth leg, posterior; E, Right fifth leg, posterior. D 0.05 mm -————_+4 By, Dye PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 5. Pseudocyclops lepidotus, female: A, Pediger 5, lateral; B, Scales on urosome segment 2, dorsal; C, Urosome, posterodorsal. Male: D, Right first antenna, segments 14—18; E, Fifth legs, posterior; F, Right endopod, fifth leg, posterior. Scale bars = 10 microns. VOLUME 102, NUMBER 2 segment 2 with five medial and three ter- minal setae, segment 3 with seven terminal setae; exopod seven-segmented, segments 1—6 each with one terminal seta, segment 7 with one medial and four terminal setae. Mandible (Fig. 2B) with 8 heavily scler- otized teeth on gnathobase; basis with 3 medial setae; endopod with 2 segments, bearing 3 and 10 setae, respectively; exopod 4-segmented, bearing 1, 1, 1, and 3 setae, respectively. First maxilla (fig. 2C) with first inner lobe bearing 9 strong terminal spines, 4 setae on posterior surface, 1 seta on anterior surface; second and third inner lobes with 3 and 4 setae, respectively; outer lobes 1 and 2 with 8 and | setae, respectively; basis 2 bearing 4 distomedial setae; endopod 2 segmented, bearing 8 medial and 7 terminal setae; ex- opod one-segmented, with 10 setae. Second maxilla (Fig. 2D) with five inner lobes bearing five, three, three, three, and seven setae, respectively; endopod reduced, indistinctly segmented, bearing seven setae. Maxilliped (Fig. 2E) with coxa carrying four lobes bearing one, two, three, and three setae, respectively, lobes three and four with surface spinules; basis with two lobes bearing three and two setae, respectively; endopod five-segmented, bearing four, four, three, four, and four setae, respectively. Legs 1—4 (Figs. 2F; 3A—C) with three-seg- mented rami, all bearing anterior and pos- terior surface spinules; leg 1 (Fig. 2F) with acute medial process and inner seta on ba- sis, distolateral margins of endopod seg- ments 2 and 3 acutely produced, distolateral margins of exopod segments | and 2 pro- duced into blunt serrate processes; leg 2 (Fig. 3A) with serrate lateral margins of exopod segments 2 and 3; leg 4 (Fig. 3C) with short external seta on basis, endopod segment 3 bearing 7 setae. Fifth leg (Fig. 3D) smaller than fourth, basis with short outer posterior seta; en- dopod three-segmented, segments 1 and 2 produced distolaterally into bifurcate pro- 337 cess, segment 3 bearing six setae; exopod segment 3 with four inner setae and four flanged spines, innermost spine narrow, only flanged at base. Male (Fig. 4A): length 0.73 mm, prosome as in female. Urosome (Fig. 4B) 5-seg- mented, adorned with rows of foliaceous ““scales,’’ anal segment and caudal rami as in female. Left first antenna 20-segmented, seg- ments 4 and 5 partly fused, otherwise as in female. Other cephalic appendages, rostrum and legs 1—4 as in female. Right first antenna (Fig. 4C) 19-segment- ed, geniculate between segments 15 and 16 (Fig. 5D); segments 14 and 15 partly fused, bearing a sinuous process on anterior mar- gin; segment 16 with acute lateral process; segment 17 produced distally into sharp tri- angular process curving medially, almost reaching end of segment 18. Fifth legs (Figs. 4D—-E, 5E) asymmetrical, biramous, highly modified. Basipodal seg- ments of left leg (Fig. 4D) fused, those of right leg (Fig. 4E) separate, all with posterior surface spinules. Left endopod one-seg- mented, reaching tip of left exopod, bearing five plumose setae; left endopodal process slender, narrowing distally, confluent with basis, reaching end of endopod. Left exopod two-segmented, segment 1 with terminal spine flanged laterally, segment 2 complex, membranous, bearing four lobes: innermost lobe spatulate, medial margin serrate; sec- ond innermost lobe elongate, narrowed at tip; second outermost lobe half as wide as long, bearing proximal seta, distal margin with v-shaped cleft; outermost lobe longest, three times as long as wide, tip dissected into three acute processes, bearing small seta at base. Right endopod (Fig. 5F) one-seg- mented, narrow; small posterior sensory pit on lateral margin; distal margin blunt, with patch of small setae. Right exopod one-seg- mented, with flanged outer spine and two long equal spines curving medially, inner- most spine narrowed to acute apex, tip 338 curved laterally, with two setae and naked process at base. Etymology.—The specific name, /epido- tus (G.), meaning “‘with scales,” refers to the foliaceous scales on the urosome of both SEXES. Discussion.—Known species of Pseudo- cyclops are demersal, spending the greater part of the diel cycle on or near the sub- strate. The nearly spherical shape and short first antennae limit the ability of these co- pepods to remain in the water column. P. lepidotus, however, is unique among mem- bers of the genus in possessing relatively long first antennae. In previously known species, the first antennae have from 15 to 18 segments and scarcely extend beyond the cephalosome. In P. /epidotus the first an- tennae have 20 segments and extend be- yond the end of the first pediger. This fea- ture, combined with its comparatively large size and light purple coloration often as- sociated with planktonic species, suggests that P. lepidotus may spend more time in the water column than other species in the genus. The unique characteristics of urosomal scales, lateral clefts in pediger 5 and elongate first antennae, separate this species from all known species of the genus. At least one undescribed species of Pseudocyclops oc- curring in the western Pacific is closely re- lated to this new species (Barr, unpub- lished). This undescribed species, collected from coastal waters off Guam and the Phil- ippines, possesses all of the above-men- tioned characters. It differs from P. /epidotus in details of the fifth legs in both sexes and will be described in a forthcoming paper. Acknowledgments We thank Drs. Thomas E. Bowman (USNM), Taisoo Park (Texas A&M Uni- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON versity) and Merrill H. Sweet II (Texas A&M University) for their critical reviews of the manuscript. We also extend appreciation to Dr. Robert C. Burghardt (Texas A&M Uni- versity) for allowing access to the Electron Microscopy Center, and Dr. K. Gushima and Mr. M. Noda (Hiroshima University) for cooperation at sea. Literature Cited Brady, G. S. 1872. Contributions to the study of the Entomostraca, VII. A list of the non-parasitic marine Copepoda of the northeast coast of En- gland. — Natural History Transactions of North- umberland and Durham 4:423-445, pl. X VII- XX. Dawson, J. K. 1977. A new species of Pseudocyclops (Copepoda: Calanoida) from the southern Cal- ifornia coast.—Transactions of the American Microscopical Society 96:247-253. Giesbrecht, W. 1893. Mitteilungen uber Copepoden. 1-6.— Mitteilungen Zoologischen Station zu Neapel 11:56-106, pl. 5-7. Nicholls, A. G. 1944. Littoral Copepoda from South Australia (II). Calanoida, Cyclopoida, Notodel- phyoida, Monstrilloida and Caligoida.—Rec- ords of the South Australian Museum 8:1-62. Tanaka, O. 1966. Neritic Copepoda Calanoida from the north-west coast of Kyushu.— Proceedings of the Symposium on Crustacea, held at Erna- kulam from January 12 to 15, 1965, 1:38—50. Marine Biological Association of India, Man- dapam Camp. Vervoort, W. 1964. Free-living Copepoda from Ifa- luk Atoll in the Caroline Islands with notes on related species.— Bulletin of the United States National Museum 236:1-431. (DJB) Department of Biology, Texas A&M University, College Station, Texas 77843-3258; (SO) Hiroshima University, Faculty of Applied Biological Science, Si- tami, Saijo-cho, Higashi-Hiroshima 724, Japan. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 339-361 A REVISION OF THE GENUS MICROPROTUS RICHARDSON WITH DESCRIPTIONS OF TWO NEW SPECIES, M. ACUTISPINATUS AND M. LOBISPINATUS (ASELLOTA, ISOPODA, CRUSTACEA) George D. F. Wilson, Oleg G. Kussakin, and Galina S. Vasina Russian Abstract.— PE3IOME Pesu3ua poga Microprotus Richardson c ommcaHuem JIByX HOBbIX BUO0B (Asellota, Isopoda, Crustacea) Yuscou J[x.J1.®., Kycakuu O.T., Bacuna I.C. B pe3yjIbTaTe MpofesaHHOM peBu3uu poya Microprotus, paHee OTHOCHMOTrO K IIPHMUTUBHOMy cpegu Asellota cemelictTBy Janiridae, omMcaHbI 1Ba HOBbIX Bua u3 OaTHMasM pawona KypusibcKux OCTpoBos, Buy Storthyngura paradoxa Birstein TlepeHeceH B 3TOT Xe por. Iloka3aHo, 4TO, HECMOTPA Ha OTCYTCTBHE IlaBaTe- JIbHbIX TlepeonoyzoB, pox Microprotus ou2%KeH ObITb TepeHeceH B OHO 3 Hal- Oosee BbICOKO CllellMaJIM3HMPOBaHHbIX CeMencTB Asellota— Munnopsidae s.1., a1 IIpeqcTaBuTesIeh KOTOPOrO XapaKTepHbI IJlaBaTeJIbHble 3aHMe Mapbl MJICOMO OB. IIpusogzatca JIuarHo3bl cemeticTBa Munnopsidae s.]. B o6beMe, BKJIIOUaIOLIeM ceMenicTBa Eurycopidae, Ilyarachnidae 1 Munnopsidae s. s., poga Microprotus WM BCeX NATH M3BECTHbIX BHOB 3TOTO poga. ObcyxTaIoTCA POACTBeEHHbIe CBA3N Microprotus c qpyruMu pozamu Munnopsidae B uacTHOCTH c pogzoM Storthyn- gura, K KOTOpOMy OH HanOosiee O1u30K, xoTa Storthyngura—Tunuyunasa Eury- copidae c llaBaTesIbHbIMHM MepeonogqamMu, OTCyTCTBy1olWjuMU y Microprotus. OOcyxaeTCA BOMpPOC, ABJIA€TCA JIM OTCYTCTBMe IlaBaTeJIbHbIX HepeOMOOB y Microprotus nie3HOMOp@HbIM TpH3HaKOM WIM 3TO—pe3yJIbTaT BTOPHYHOTO yMpomeHus. Abstract.—The genus Microprotus Richardson, referred earlier to the rela- tively plesiomorphic family Janiridae, is revised. Two new species from the bathyal zone of the Kurile Islands, M. acutispinatus and M. lobispinatus, and Storthyngura paradoxa Birstein are also placed in this genus. Microprotus should be included in the Munnopsidae s.1., in spite of its lack of the highly specialized posterior natatory pereopods that characterize this family. Diagnoses are given for the family Munnopsidae s.l., for the genus Microprotus, and for all five species referred to this genus. The relationships between Microprotus and other munnopsid genera are discussed, and it is found to be most closely related to Storthyngura. Whether the absence of natatory pereopods in Microprotus is a plesiomorphic or an apomorphic reversion is discussed; the latter hypothesis is favored. 340 The status of the janiroidean genus Mi- croprotus has been suspect since its incep- tion. Richardson (1910) described two in- dividuals from the South Bering Sea which she put in the family Janiridae, where the genus remained until now. Her remarks on the genus include the statement (Richard- son 1910:116) “This genus has affinities with the Munnopsidae”’ (under Sars’ (1899) def- inition, this family also included Eurycope and I/yarachna), but later in the text she writes ““The absence of natatory legs, the general form of the body and the style of the uropods, however, are characters refer- able to the Janiridae.”’ The Munnopsidae Sars s.1. (Wilson 1989) is defined by unique natatory modifications, including paddle- shaped posterior legs with many fringing plumose setae. Richardson’s (1910) species, M. caecus, closely resembles some species in the munnopsid genus Storthyngura, ex- cept that its posterior legs are not in the least paddle-shaped and they have no plumose swimming setae. Vanhoffen (1914), the author of the genus Storthyngura, described a new species, Microprotus antarcticus from pleotelson fragments. Apparently Vanhoffen did not regard this species as a member of Stor- thyngura and included it in his currently unused and misspelled family Jolellidae. Storthyngura, however, has come to include a great variety of forms (see reviews by Bir- stein 1957, George & Menzies 1968a, b). Birstein (1970) included the species para- doxa in Storthyngura despite its lack of na- tatory posterior pereopods. His comments (translated) are revealing: ““This inexplica- ble trait [lack of swimming limbs] contra- dicts not only the diagnosis of the genus but even that of the family, although in all the other characteristics the new species can be regarded as a typical form of the genus Stor- thyngura.”’ Birstein (1970) undoubtedly overlooked the obscure genus Microprotus because all authors, including Wolff (1962), had put it in the Janiridae. In this paper, we remove the veil of ob- scurity from Microprotus by providing new PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON descriptions of the its members, and by dis- cussing the meaning of its lack of natatory limbs, at least from a phylogenetic point of view. M. caecus is redescribed, two new species are fully described, and diagnoses and a key to all species are provided. We argue that Microprotus is a derived member of the Munnopsidae related to the hetero- geneous genus Storthyngura, and that the absence of natatory limbs is a reversion to a primitive condition, rather than a plesio- morphy. The Systematic Position of Microprotus We present here a formal diagnosis of the Munnopsidae Sars, 1899 (sensu Wilson 1989), to aid the discussion of the system- atic position of Microprotus. Family Munnopsidae Sars, 1899 s.1. Diagnosis (derived from Wilson, 1989).— Janiroidea with a distinct natasome: pere- onites 5—7 enlarged, muscular, with artic- ulations often broadly joined or fused; pos- terior ventral nerve cord ganglia fused into a single mass in pereonite 5; pleotelson gen- erally tapering posteriorly. Pereopods V—VII natatory (in most genera) with many long, fully plumose setae on margins of broad, paddle-like carpi and propodi. Pereopodal dactylar claws with trough-like hollow be- tween superior and inferior claws enclosing distal sensillae. Antennular article 1 broad- ened and laterally flattened. Discussion. —The above definition of the Munnopsidae subsumes the smaller fami- lies Eurycopidae, Ilyarachnidae, and Mun- nopsidae s.s. The diagnosis includes fea- tures that are found in no other family of the Janiroidea in this combination. For a more detailed discussion, see Wilson 1989). The best corroborated phylogenetic trees of the Munnopsidae (Wilson 1989) suggest that the ancestral munnopsid had the following characters in addition to the diagnostic characters above: rostrum (a distinct frontal projection between the antennulae) present, natasomal pereonites and pleotelson freely VOLUME 102, NUMBER 2 articulated, pleopod III rami with many plumose setae. The diagnosis of the Munnopsidae is pre- sented here because Microprotus is a Ssig- nificant exception in its lack of natatory legs (Figs. 3D, 7, 10). This genus nevertheless has all other diagnostic characters including a completely fused natasome, an unusual feature for an ambulatory animal (Fig. 1A- B). Given this distribution of characters, two possible hypotheses emerge for the classi- fication of this genus: (1) the non-natatory legs are plesiomorphic within the Munnop- sidae, and Microprotus diverged early in the evolution of the family before swimming was acquired, i.e., it is the sister group of the remaining munnopsids; or (2) the non- natatory legs are a complete reversion, are a distinctive autapomorphy for the genus, and other characters must be used to estab- lish the affinities of the genus within the Munnopsidae. Using the non-natatory pe- reopod character alone, one would be forced to accept hypothesis 1 (H/) over hypothesis 2 (H2) because the former is more parsi- monious. Several other character com- plexes are examined here to establish which hypothesis is most likely. The parsimony values are counted globally for the Mun- nopsidae. Cephalon (Fig. 1E; Wilson 1989, fig. 38): The ancestral munnopsid probably had a distinct rostrum, while Microprotus does not. H/ predicts either that the presence of a rostrum in other munnopsids is a rever- sion or that Microprotus lost the rostrum independently of other munnopsids (two evolutionary steps), while H2 predicts that only the immediate ancestor of Microprotus (and taxa of its clade) lost the rostrum in its evolution (one evolutionary step). The cephalons of some munnopsids bear a synapomorphy called the frontal ridge, a supporting bridge between the mandibular articulations on both sides of the head. Be- cause Microprotus has a frontal ridge, H/ predicts that the frontal ridge is a synapo- morphy of all munnopsids and was subse- quently lost in several taxa (e.g., Euryco- 341 Table 1.—A parsimony analysis of two evolutionary hypotheses for the non-natatory pereopods V-VII in Microprotus. Hl = The ancestral munnopsid did not have natapods, and Microprotus diverged before na- tapods were evolved. H2 = The natapods in Micro- protus reverted to an ambulatory state. Values are the number of evolutionary steps required in the character for the phylogeny of the Munnopsidae (Wilson, 1989) given that a hypothesis is true. Character H1 H2 Pereopods V—VII not natatory Rostrum absent Frontal arch present Mandibular notch in cephalon Natasome completely fused ONNNN KS OK — — —& LO Total parsimony values pinae, Munnopsinae) or was developed at least twice (two steps). H2, on the other hand, only requires that the frontal ridge is a syn- apomorphy of the group to which Micro- protus belongs (one step). In the sister group Acanthaspidiidae and in some munnopsid genera, the mandible articulates with the head by a rounded pos- terolateral border, while other taxa, includ- ing Microprotus and Storthyngura, have a posterior projection of the mandible that articulates with the cephalon in a narrow posteriorly-directed slot. HJ suggests that this feature either evolved twice, or evolved once and then was lost in more derived taxa (two steps); H2 requires only that it is a apomorphy of some group of the munnop- sids (one step). Natasome (Fig. 1A—C): The posterior pe- reonites and the pleotelson of the ancestral munnopsid, although integrated into a unit, were probably fully articulated because both the Acanthaspidiidae, and several munnop- sid genera, such as Amuletta Wilson and Thistle, Munnopsurus Richardson, and Munnicope Menzies & George are fully ar- ticulated both ventrally and dorsally. The flexion of the segments, however, is restrict- ed and the integration of the natasome is obvious in these taxa. Because Microprotus has a fully fused natasome, H/ requires that this was achieved independently from the 342 remaining munnopsids (two steps), while H2 allows that complete fusion could be a syn- apomorphy ofa subset of the Munnopsidae. Table 1 shows parsimony values for mun- nopsid phylogenetic estimates using the characters discussed above under H/ or H72. Although these characters are only a subset of the possible features that are useful in munnopsid systematics (Wilson 1989), they are highly derived features that are unlikely to appear more than once in the evolution of this family. HJ adds nine steps to the munnopsid phylogenetic tree, while H2 only adds six steps and is therefore more prob- able. The ambulatory posterior pereopods of Microprotus are best explained as a re- version from a swimming form, and must be an autapomorphy of this genus alone. Furthermore, the natapod to pereopod re- version is not simply a reduction of features: no natatory landmark is present on pereo- pods V—VII of the adult (juveniles are un- known at present). There are no natatory setae, the carpi and propodi are much longer than in any other munnopsid, and these seg- ments are tubular rather than flattened. Other taxa, such as Syneurycope where the pereopodal swimming function may be greatly reduced, typically retain the rem- nants of these landmarks (e.g., Haugsness & Hessler 1979, fig. 31). The detailed similar- ity between the anterior and posterior legs (Fig. 3B, D) suggests that a genetic transfer in pereopodal developmental processes from anterior to posterior may underlie this re- version (first author’s opinion). In the cur- rent absence of information on munnopsid genetics, further evidence could be obtained by examining the pre- and postmarsupial development in Microprotus species, once juveniles and embryos are collected. Microprotus Richardson, 1910 Microprotus Richardson, 1910:116. Storthyngura (pars) Birstein, 1970:352. Type species. —Microprotus caecus Rich- ardson, 1910. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Species included. —Microprotus caecus Richardson, 1910; M. antarcticus Vanhof- fen, 1914; M. paradoxus (Birstein, 1970); M. lobispinatus, n. sp.; M. acutispinatus n. sp. Diagnosis. —Munnopsidae with ambula- tory pereopods V—VII: carpus and propodus elongate and tubular, not flattened, with op- posing margins with rows of unequally-bifid setae; all segments lacking plumose swim- ming setae. Cephalon with frontal ridge and without rostrum. Pereonites 5—7 and pleo- telson fully fused, with no free articulations either dorsally or ventrally; natasomal pere- onites collectively shorter than ambuloso- mal pereonites. Body dorsal surface, lateral margins of pereonites and pleotelson, coxae of pereonites 5—7, and basal articles of an- tenna with elongate spines; pleotelson ter- minating in pair of elongate spines. Pleo- telson with pronounced preanal ridge; ridge and anus not covered by opercular pleo- pods. Antennular article 1 elongate and sub- triangular. Mandible with cuticular projec- tion on posterolateral margin articulating with cephalon in elongate notch. Uropods elongate with tubular protopods and rami. Additional description. — Body with elon- gate, anteriorly curved spines in following pattern: dorsal midline with one spine on each pereonite and two on pleotelson; dor- solateral spines on pereonites 2-7; lateral spines on pereonites 5—7; two pairs of spines on lateral margins of pleotelson; one pair of spines on posterior tip of pleotelson; one or two spines on articles 1—3 of antenna; single spines on coxae of pereopods I; paired spines on coxae of pereopods II-IV. Cephalon without eyes or elongate spines, broader than long, with robust laterally pro- jecting cheeks at mandibular articulation point. Pleotelson broad, in most species broader than long; dorsally trilobed, with central section separated by troughs from dorsally projecting lateral lobes. Antennular flagellum elongate, with many articles, each article with one or several aesthetascs; articles 2, 3 and 5 near same VOLUME 102, NUMBER 2 length, distinctly longer than article 4; fla- gellar articles of male very short, wider than long, shorter than article 4. Antenna elon- gate, length more than two body lengths. Mandible normal but body abbreviated proximal to dorsal condyle and palp; molar process triturative but distally tapering; palp functional, longer than mandibular body; teeth on incisor process not distinct; lacinia mobilis normal with distinct teeth; spine row normal with many spines. Maxillipedal basis with many coupling hooks; epipod elongate, reaching to articulation between palp articles 2 and 3, with small rounded dorsolateral spine. Pereopod I much smaller than posterior pereopods, with thin carpus and propodus having only simple setae. Pereopods II-VII robust, elongate, with strong unequally-bi- fid setae on opposing margins of carpus and propodus. Male pleopod I elongate, much longer than wide, with distinct waist midlength, often with short thick spines or tubercles on ven- tral surface; distal tip with distinct medial and lateral lobes; lateral lobe more elongate, curving medially posterior to medial lobe. Male pleopod II protopod broad, laterally rounded, distally curving to short pointed tip; protopodal setae on lateral margin short, simple, not hemiplumose; endopodal stylet shorter than protopod length; exopod very short, rounded, with nonprojecting distal hook. Female pleopod II broader than long, without setae on keel. Pleopod III endopod broad and rounded; exopod long, thin, dis- tally rounded; exopod and endopod with numerous plumose setae. Remarks.—The inclusion of M. antarc- ticus Vanhoffen is rather dubious because the species is known only from fragments. Its pleotelson, however, is more similar to other species of Microprotus than to Stor- thyngura so it must remain in this genus until redescribed from new material. We (GSV & OGK) have examined the paratype of Storthyngura paradox Birstein (1970): this species has a strong resemblance to Micro- 343 protus and is transferred herein to this ge- nus. Two new species, M. lobispinatus and M. acutispinatus, extend the known mor- phological range of this genus. Microprotus has clear affinities with the heterogeneous genus Storthyngura, which does have well-developed natapods. The two genera share the following characters, often to small details: cephalon shape and man- dibular articulation; dorsal and lateral spi- nation; form and orientation of the anten- nula; uropod shape; fusion of natasomal segments (in some species); shape of venter of pleotelson; pleopod shape. Such a long list of similar features practically guarantees that these two genera form a monophyletic taxon within the Munnopsidae. Formal rec- ognition of this group as a subfamily, how- ever, must wait until the genus Storthyngura is revised, and its relationships to Acantho- cope are clarified. The subgeneric division of Storthyngura provided by George & Menzies (1968b) falls short of being useful because, although they say their analysis was based on 138 char- acters, only 3 or 4 characters were given in the descriptions of the subgroups; analysis of their groupings is therefore extremely dif- ficult. Furthermore, the subgroups may have dubious meaning because they separate species with truncate or forked pleotelson tips (as in Microprotus) into different groups, even though this may be an important char- acter at the generic level. Birstein (1970) also found the classification of George & Menzies (1968b) to be ineffective. Stor- thyngura should be subdivided because the type species S. elegans Vanhoffen is flat- bodied and broad while S. pul/chra Hansen (for example) is deep-bodied and has a mus- cular natasome. The strongly natatory at- tributes of the latter species are more like other Munnopsidae, indicating it may have diverged early in the evolution of the Stor- thyngura group. For the moment, Micro- protus 1s considered to be among a complex of genera represented by the polyphyletic or paraphyletic genus Storthyngura. 344 Geographic distribution of Micropro- tus.— This genus is an Indo-Pacific bathyal to upper-abyssal genus with 4 species in the northern Pacific: from 40°N to 52°14’N in the Japan and Kurile-Kamchatka Trenches, and off the South Aleutian Islands. A single Antarctic species has been found in the Da- vis Sea. This genus inhabits depths in the range of 550-3400 m. Key to the Species of Microprotus la. Posterior spines on pleotelson ex- tending to tip of uropods; uropodal exopod distinctly shorter than en- dopod ....... Microprotus antarcticus Vanhoffen, 1914 lb. Posterior spines on pleotelson not extending to tip of uropods; uro- podal exopod subequal to endo- pod 2a. Lateral spines on pleotelson broad, nearly as broad as long; male pleo- pod II stylet not tapering to thin hair-like tip 2b. Lateral spines on pleotelson thin, much longer than broad; male pleopod II stylet tapering to thin hair-like tip 3a. Dorsal and lateral spines on body distally thick and typically round- ed; pleotelson width (excluding spines) distinctly greater than length; male pleopod II stylet long, distinctly longer than half proto- pod length Microprotus lobispinatus, n. sp. (Figs. 5-7) 3b. Dorsal and lateral spines on body distally thin and pointed; pleotel- son width (excluding spines) sub- equal to length; male pleopod II stylet short, distinctly less than half protopod length .... Microprotus acutispinatus, n. sp. (Figs. 8-10) 4a. Dorsal and lateral spines on body strongly denticulate; posterior spines on pleotelson not recurved es © © © © © © © © © © © ee ee ee le e 8 © © © © © © © © ee ew 8 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON dorsally; pleotelson dorsal surface without pair of low bumps anterior to uropods; pleotelson width sub- equal to length vommde: Vhor: Microprotus paradoxus (Birstein, 1970) 4b. Dorsal and lateral spines on body finely denticulate; posterior spines on pleotelson strongly recurved dorsally; pleotelson dorsal surface with pair of low bumps anterior to uropods; pleotelson width greater than length tia ae Microprotus caecus Richardson, 1910 (Figs. 1-4) ee © © © © © © © ee ew ee ll oe 8 © © © © © © © ew ee 8 8 el tll ll The Species of Microprotus Microprotus caecus Richardson, 1910 Figs. 1—4 Types. — Holotype copulatory male, pleo- telson damaged, some legs missing, others loose in vial, body length 12.0 mm, USNM (United States National Museum no.) 39521. Paratype copulatory male, dam- aged, partly dissected, some limbs missing, estimated length 11.2 mm, USNM 39917. Type locality.—Albatross station 4781, 52°14.5’N, 174°13’E, off Cape Sabak, Agat- tu Island, Aleutian Archipelago, depth 544 m, bottom consisting of fine gray sand and pebbles. Diagnosis.—Cephalon width 1.1 times pereonite 1 width. Dorsal and lateral spines on body distinctly pointed distally, not rounded, finely denticulate. Pleotelson width 1.3 times length; dorsal surface with pair of low bumps anterior to uropods; lateral spines narrow, length 2.8 times basal width. Male pleopod II stylet short, length 0.45 of pro- topod length, with curved hair-like distal part. Uropods much longer than posterior spines of pleotelson; endopod length sub- equal to exopod length. Additional description of males. —Body (Fig. 1A—D): Cuticle heavily calcified. Pres- ervation color white. All margins and spines rugose, with many fine denticles. Body wid- est at pereonite 5, body length 2.7 times Fig. 1. Microprotus caecus, holotype male: A—B, Dorsal and lateral views of body; C, Ventral view of natasome; D, Ventral oblique view of cephalon and ambulosome, pereopods on right side omitted. Paratype male: E, Lateral oblique view of cephalon. Scale bars: 1.0 mm, all. 346 width. Articular margins of anterior per- eonites set in shallow transverse grooves. Dorsal-most parts of pereonites 1-4 also with shallow transverse groove. Pleotelson with pair of short broad spines or bumps posterior to last median spine; bumps not visible in lateral view; lateral spines on pleo- telson flattened dorsoventrally, postero- lateral spines anterior to uropods triangular in cross-section; posterior spines strongly curving dorsally. Antennula (Fig. 2H, I): Left antennula of holotype approximately 10 mm long; length 0.83 of body length. Surface of articles 1 and 2 denticulate. Article 1 length 1.9 times width; medial margin with dense group of denticles adjacent to insertion of article 2; dense patch of broom setae proximal to group of denticles on medial margin. Article 2 length 0.39 of article 1 length (including distal lobe). Article 3 subequal to article 2. Antenna (Fig. 2H): Length 2.8 times body length. Articles 2 and 3 with broad flattened spines projecting ventrally. Article 3 with spine in approximate position of scale. Ar- ticles 5 and 6 subequal, length of either 0.22 of total antennal length. Left mandible (Fig. 2A—D): Incisor pro- cess with one distinct cusp ventrally, with remaining incisive margin sinuous and lacking distinct cusps. Lacinia mobilis with four cusps, decreasing in length dorsally; ventral surface of lacinia mobilis with tuft of spinules or cuticular hairs. Spine row with 15 members, distal spines with spinules or cuticular hairs on basal ventral surface. Mo- lar process tapering distally, distal width roughly half proximal width; posterior mar- gin of triturative surface with 8 doubly set- ulose setae and row of basal denticles, ven- tral tooth present. Maxillula (Fig. 2E): Outer lobe with 12 large spine-like toothed setae. Inner lobe distal tip broadly rounded, not extending beyond medial end of outer lobe setal row. Maxilliped (Fig. 2G): Epipod length 0.93 of basis length; width 0.37 of length; distally rounded. Basal endite with 13 coupling PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON hooks and approximately 5 apical fan setae distally. Palp article 2 width subequal endite width. Pereopods (Fig. 3A—E): Total length in- creasing posteriorly with pereopod I dispro- portionately smaller than others: pereopod I approximately half body length while pe- reopods II-VI increasing from slightly less (approximately 5% shorter) to near body length. Pereopodal bases: II-IV length sub- equal; I length 0.71 length of II; V—VII long- er than IJ-IV, increasing in length poste- riorly, length ratios with H-IV 1.1, 1.3, 1.5. Ischia of all pereopods distinctly shorter than corresponding bases: ischia I and VI less than half bases length, ischium II length 0.69 of basis II length. Pereopod I propodus with many fine, blunt-tipped, aesthetasc-like se- tae; opposing margins of propodus and car- pus with only fine setae. Setae of pereopods II-VI: single row of unequally-bifid setae on opposing margins of propodus and carpus; propodus with numerous fine setae both dorsally and ventrally. Superior dactylar claws II-VI with triangular or blunt projec- tion on posterior margin. (Pereopod VII not known.) Male pleopod I (Fig. 4A—E): Sympod wid- est at proximal insertion, tapering to less than half proximal width at midlength, and expanding to 0.75 of proximal width dis- tally. Sympod with two broad irregular rows of low spines or bumps on ventral surface. Distal tip of in situ sympod resting exactly at tip of pleopod II protopod. Lateral lobes elongate, pointed, proximally broad, distal parts curving medially. Medial lobes short, rounded, approximately 0.25 of lateral lobe length, with numerous long curved simple setae reaching to tip of lateral lobe on distal margin. Male pleopod II (Fig. 4F, G): Protopod broad, laterally rounded, with fringe of sim- ple setae laterally and distally; length 1.4 times width; ventral surface with concavity lateral to internal musculature for exopod. Endopod inserting 0.65 of protopod length from pleopod insertion; exopod short, distal VOLUME 102, NUMBER 2 347 Fig. 2. Microprotus caecus, paratype male, mouthparts: A-D, Left mandible: A, Mandible, dorsal view; B, Incisor process and lacinia mobilis, anterior view; C, Molar process, anteromedial view; D, Distal part of mandible showing spine row; E, Right maxillula, ventral view; F, Right maxilla, ventral view; G, Right maxilliped, ventral view. Holotype male: H, Cephalon, dorsal view, showing antennula and antenna; I, Antennular basal articles, in situ. Scale bars: 0.2 mm, all except for H, 2.0 mm long. 348 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 3. Microprotus caecus, paratype male, pereopods: A, Pereopod I, lateral view; B, Pereopod II, lateral view; C, Enlargement of adjacent parts of carpus and propodus of pereopod VI; D, Pereopod VI, medial view; E, Pereopod VI, enlargement of dactylar claw, lateral view. Scale bars: 1.0 mm. VOLUME 102, NUMBER 2 hook not protruding, with small distal tuft of fine simple setae; exopodal extrinsic mus- culature small compared to size of proto- pod, extending only half way to lateral mar- gin of protopod. Pleopod III: Exopod distally rounded, with approximately 17 plumose setae. En- dopod distally broad, rounded, very thin, fringed with numerous setae. Uropod (Fig. 4H): Long, thin, with short setae, length 0.69 of pleotelson length. En- dopod and exopod subequal, length of either 0.87 of protopod length. Remarks. — Microprotus caecus is known only from two adult male specimens; fe- males or juveniles have not been collected. This species may be distinguished from oth- er species of the genus by the following char- acters: cephalon only slightly wider than pereonite 1; spines distinctly pointed, not rounded distally; pleotelson much wider than long; lateral pleotelson spines that are much longer than their basal width; and subequal uropodal rami. Overall, the other species are similar to M. caecus, perhaps with the exception of VM. antarcticus whose pleotelson shape differs rather more. Richardson (1910: fig. 38) illustrated the holotype of Microprotus caecus with distinct articulations between the natasomal seg- ments. Study of the type material reveals that the natasome ts fully fused with no free articulations. The dorsal surface of the na- tasome, however, does have slight ridges that are either remnants of the articulations or exterior expressions of apodemes. These ridges further corroborate the contention that pereonites 5—7 are natasomal in origin because each ridge extends well into the seg- ment anterior to it (Fig. 1A), as is typical with most munnopsids. Microprotus lobispinatus, new species Figs. 5-7 Types.—Holotype male, 12 mm long, (Zoologicheskogo Instituta Akademiya 349 NAUK (ZIN) No. 1/81502). Paratype male, 11 mm, (ZIN No. 2/81503). Type locality. —Pacific Ocean, near Itu- rup Island, 44°52’N, 149°27’E, depth 910- 920 m, habitat: muddy sand with stones, 25 Jul 1984, coll. B. Sirenko. Diagnosis. — Dorsal and lateral spines on body thick and rounded distally; spines fine- ly denticulate. Pleotelson width (excluding spines) 1.2 times length; lateral spines broad, length subequal to basal width. Male pleo- pod II stylet 0.66 of protopod length, with- out curved hair-like distal part. Uropods much longer than posterior spines of pleo- telson; endopod length subequal to exopod length. Additional description of adult male (Fig. 5). — Body somewhat robust, front half sub- equal in width to natasome. Body length approximately 2.2 times body width with- out lateral spines; body widest at pereonite 4. All dorsal spines distinctly flattened, often with concave front surface, usually curved forwards, sometimes widened in middle part. All dorsal spines with finely spinulous, rasp-like surface. Cephalon broad, approximately three times wider than long; frontal margin broadly concave. Pereonite 1 considerably narrower than cephalon, with single medial spine only. Pereonite 2 approximately 1.5 times wider than pereonite 1, slightly wider than pere- onite 4 and slightly narrower than pereonite 3. Dorsal surface of pereonites 2—7 with three spines. Medial spines gradually decreasing in length from pereonite 2 to 6, medial spine on pereonite 7 longer than that on pereonite 6. Dorsolateral spines nearly as long as me- dial spines; on natasomal pereonites, much nearer to medial spines than on pereonites 2-4. Lateral margins of pereonites 1 and 4 rounded, pereonites 2 and 3 nearly truncate, with produced posterolateral angles. Coxal plates of pereonites 2—4 long, strongly pro- duced, each plate with long spine-like lobes, anterior lobe longer than posterior. Coxal 350 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 4. Microprotus caecus, paratype male, pleopods: A—C, Pleopod I, ventral, dorsal, and lateral views respectively; D, E, Enlargements of pleopod I distal tip, ventral and dorsal views respectively; F, G, Right pleopod II, ventral and enlarged dorsal view respectively. Holotype male: H, Left uropod, in situ ventral view. Scale bars: 1.0 mm. plates of pereonite 1 with single anterior gles of pereonites 5-7 produced outwards spine-like lobe. into stout conical spine-like processes. Cox- Segments of natasome fused medially but al plates of pereonites 5—7 small, with distinct on lateral parts. Anterolateral an- rounded posterolateral angles. VOLUME 102, NUMBER 2 Pleon length not including posterior spines 0.3 of total body length. Anterodorsal mar- gin of first pleonite slightly marked by shal- low transverse depression, posterior margin somewhat more distinct. Dorsal surface of anterior pleonite convex, with median spine strongly curved forwards. Pleotelson broad, 1.3 times wider than long; lateral margins each with two long stout conical spines; an- terior spine thicker, located nearly at mid- length of pleotelson lateral margin. Dorsal surface of pleotelson with flattened spoon- like median spine curving forwards. Antennula (Figs. 5, 6F) when bent back- wards slightly exceeding middle of body; basal article more than two times longer than broad, its outer margin irregularly con- vex, inner margin roughly concave; second article inserting near midlength of first ar- ticle, approximately one third as long as first article, slightly increasing in width distally. Antennal second article with two curved spines, one spine directed outwards, and second inwards. Third article also with two spines, outer spine longer than inner one. Left mandible (Fig. 6C): Incisor process with one tooth. Lacinia mobilis with two teeth. Spine row with 12 spines, posterior spines longer than anterior ones. Molar pro- cess forming truncate cone, cut off distally, with small tooth on inner side and shallow apical excavation in middle. Third article of mandibular palp broad, oval, twisted, with numerous marginal setae, longer than palp article 1. Maxilliped (Fig. 6A, B): Endite with 10 coupling hooks. Epipod approximately three times longer than broad, distally rounded, with triangular lateral projection. Pereopods (Fig. 7A, E, F): Pereopod I simple, little differentiated; carpus approx- imately 2 times longer than propodus; both articles with numerous short setae. Carpus 1.3 times longer than ischium and merus together. Propodus of pereopod II slightly longer than carpus, ventral margin with dense row of bifid spine-like setae, dorsal margin with numerous fine setae; merus Fig. 5. Microprotus lobispinatus, male holotype, body in dorsal view. short, bearing setae on both margins. Car- pus and propodus of pereopods IIJ—VII ob- long, narrow, subequal in length, ventral margins with dense row of short spine-like bifid setae; on propodus all setae subequally long, on carpus small setae alternate with larger setae (not shown in Fig. 7E, F); pro- podus with one distal plumose seta. Per- eopod VI propodus slightly longer and near- ly twice as narrow as carpus. Male pleopod I (Fig. 7B): Pair complex narrowest at midlength, length 2.8 times proximal width. Lateral lobe longer than medial lobe, curving medially; medial lobe with distal tip rounded, lobe-like, bearing numerous setae. Male pleopod II (Fig. 7C): Somewhat broad; protopod suboval, length nearly 2 times width, inner distal tip triangular, pointed; distal part of outer margin and pos- terior margin with setae. As compared with M. acutispinatus, endopod relatively long. 352 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 6. Microprotus lobispinatus, male holotype, mouthparts and antennula: A, Maxilliped, dorsal view; B, Maxillipedal epipod, dorsal view; C, Right mandible, dorsal view; D, Maxillula, ventral view; E, Maxilla, ventral view; F, Antennula. Scale bars: 0.2 mm, all except F, 0.3 mm. = Fig. 7. Microprotus lobispinatus, male holotype, pereopods and uropod: A, Pereopod I; B, Pleopod I; C, Pleopod II; D, Uropod; E, Pereopod II; F, Pereopod VII. Scale bars: 0.2 mm—B—D; 0.3 mm—A; 0.5 mm— BSE: 354 Fig. 8. Microprotus acutispinatus, male holotype, body in dorsal view. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Stylet extending slightly beyond distal tip of protopod, length 0.7 of total protopod length. Exopod small, with dense group of fine simple setae on posterior curve. Uropod (Fig. 7D): Very long and slender, extending much beyond posterior spines of pleotelson. Endopod slightly shorter than exopod; latter ramus nearly as long as pro- topod. Remarks. — Microprotus lobispinatus is represented by only two adult males from one sample. This species can be distin- guished from all Pacific species by the wide, apically flattened and rounded dorsal spines. M. lobispinatus also differs distinctly from M. acutispinatus and M. paradoxus by its relatively wider pleotelson; the species is similar in this respect to M. caecus. M. lo- bispinatus is easily distinguished from the latter species by having thicker and shorter lateral spines, especially on the posterior pereonites and the pleotelson, by lacking dorsal lumps on the pleotelson anterior to the uropods, and by uropodal protopods that do not extend beyond the posterior spines of the pleotelson (as in M. caecus). This new species, like all other boreal species, dis- tinctly differs from M. antarcticus, a single species from the southern hemisphere con- ventionally assigned to this genus, by pos- terior spines on the pleotelson considerably shorter than the uropods, and by uropodal rami that are nearly equal in length. Etymology. —“‘Lobispinatus,”’ the adjec- tival form of two classical nouns, means ““provided with lobe-spines.”’ Microprotus acutispinatus, new species Figs. 8-11 Types. — Holotype, male 13 mm (ZIN No. 1/81500). Paratypes, 2 males, 2 females, all fragmented (ZIN No. 2/81501). Type locality. — Pacific Ocean, near Itu- rup Island, 44°48'N, 149°31’E, depth 1100- 1200 m; habitat: sand with pebbles; 25 Jul 1984, coll. B. Sirenko. VOLUME 102, NUMBER 2 Diagnosis. — Dorsal and lateral spines on body thin and pointed distally; spines finely denticulate. Pleotelson width (excluding spines) subequal to length; lateral spines broad, length subequal to basal width. Male pleopod II stylet 0.4 protopod length, with- out curved hair-like distal part. Uropods much longer than posterior spines of pleo- telson. Additional description of adult males (Figs. 8, 11B, E).— Body relatively slender, slight- ly widening posteriorly, so that natasome distinctly wider than pereonites 1-4 and ce- phalon; length slightly more than three times body width across pereonite 5 without lat- eral projections. All dorsal spines rather slender, narrow-conical, pointed, their sur- faces covered with minute spinules. Dorsal spines directed forwards and upwards on pereonites and backwards and upwards on pleon. Cephalon broad, width approximately three times length; frontal margin broadly concave. Pereonite 1 distinctly narrower than ce- phalon, with single median dorsal spine. Pereonites each with three spines; median spines subequal in length. Dorsolateral spines on natatory pereonites placed much nearer to medial spines than on pereonites 2—4. Lateral margins of pereonites 1 and 4 rounded, those of pereonites 2 and 3 nearly truncate, posterolateral angles produced outwards. Coxal plates of pereonites 2—4 with two produced, long, spine-like lobes (damaged on pereopod III in Figs. 8, 11A— C); anterior lobe longer than posterior one. Segments of natasome lacking dorsal artic- ulations; pereonites 5—7 and pleon not clear- ly delimited. Anterolateral corners of pere- onites 5—7 produced outwards into stout, conical spine-like projections. Coxal plates of pereonites 5-7 in dorsal view relatively short, suboval in form. Pleon length excluding posterior spines approximately one third total body length. First pleonite small, narrow, convex dor- 355 sally, with medial dorsal spine curved back- wards. Pleotelson (without projections) only slightly broader than long, somewhat pro- duced posterior part with pair of long spine- like pointed projections directed backwards and slightly outwards and two pairs of lat- eral long stout conical spines: anterior spine considerably thicker and slightly longer, lo- cated approximately at midlength of lateral margin of pleotelson, posterior spine smaller and placed near posterolateral angle of pleo- telson. Low broad dorsomedial keel with recurved spine-like process in middle part. Antennula (Fig. 8) when bent backwards, reaching midlength of body; basal article two times longer than broad, its outer mar- gin irregularly convex, inner margin con- cave; second article inserting at midlength of basal article, approximately one third length of basal article, slightly widening dis- tally. Antennal (Figs. 8, 11B) second article with two stout spines, one on inner and another on outer margin, third article also with two subequal spines. Left mandible (Fig. 9D): Incisor process with one tooth. Lacinia mobilis with three teeth. Spine row with eight setae, posterior spines longer than anterior ones. Molar pro- cess conical, obliquely cut off distally, with four setae on distal posterior edge; distal triturating surface with conical tooth. Third article of mandibular palp longer than first, broad, twisted, with setal row. Maxilliped (Fig. 9A): Endite with 11 cou- pling hook on inner margin. Epipod three times longer than broad; distally rounded, with triangular lateral projection. Pereopod I (Fig. 10C) simple, little dif- ferentiated; carpus slender and very long, length 1.4 times ischium and merus length together and 1.6 times propodus length. Ventral and dorsal margins of propodus and ventral margin of carpus with rows of short stout spine-like bifid setae. Pereopod II (Fig. 10D): Propodus some- what longer, slightly longer than carpus, with 356 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON \\ y Nh). Y LAs Z Wh, ee D Fig. 9. Microprotus acutispinatus, male holotype, mouthparts: A, Maxilliped and epipod, ventral view; B, Maxillula, ventral view; C, Maxilla, ventral view; D, Left mandible, dorsal view. Scale bars: 0.2 mm. VOLUME 102, NUMBER 2 setae only along ventral margin. Carpus with four bifid setae on ventral margin. Dorsal margin of merus serrate distally. Pereopods V—VII (Fig. 10E): Carpus and propodus long, slender, linear, subequal in length, without natatory setae, but ventral margins with row of short stout spine-like bifid setae. Dactylus short. Male pleopod I (Fig. 10A): Pair complex much narrower in middle part; length ap- proximately 2.5 times proximal width. Lat- eral lobe much longer than endopod; distal tip of medial lobe narrowly rounded, with short row of simple setae arranged in fan- like order. Male pleopod II (Fig. 10B): Protopod very broad, length approximately 1.5 times long- er than wide, semicircular, distomedial cor- ner slightly produced, pointed; posterior margin and distal part of outer margin with row of thin simple setae. Endopod and ex- opod small, reaching well short of distal tip of protopod. Stylet relatively short, extend- ing only slightly beyond distal margin of exopod and not reaching tip of protopod. Exopod with dense group of long, fine, sim- ple setae on posterolateral margin. Uropods (Fig. 8) long and slender, ex- tending beyond posterior spines of pleotel- son. Exopod slightly shorter than endopod; latter nearly as long as protopod. Description of female.—In general, out- line (Fig. 11A, C, D, F) similar to male; body length 12 mm. Dorsum somewhat wider than in male. Pleotelson bearing two tiny low lumps posterior to central dorsal median spine and anterior to uropods, sim- ilar to those in M. caecus (lumps not visible in lateral view, hidden by swelling of dorsal surface of pleotelson lateral to depressed medial part). Pleopod II (Fig. 10G) very broad, 1.3 times broader than long, ventro- medial keel without setae. Remarks.—Microprotus acutispinatus is represented by five specimens: three adult males and two females, of which only the holotype male is preserved in relatively good condition. The other individuals are badly 357 damaged, their bodies having broken in half. This species is easily distinguished from M. caecus and M. lobispinatus by its narrow pleotelson, which is nearly as wide as long and similar in this respect to M. paradoxus. It differs, however, from the latter species by the narrowly conical (not flattened) dor- sal spines on the pleotelson which are con- siderably shorter and stouter than those of M. paradoxus. Etymology. —“‘Acutispinatus,” contain- ing the adjectival form of “‘spinus” and modified by “acutus,’’ means “‘provided with pointed spines.” ~ > Microprotus paradoxus (Birstein, 1970) Storthyngura paradoxa Birstein, 1970, p. 334, Figs. 19-20. Syntypes. —Types were not found by Dr. Mezhov, who looked for them at our re- quest in the deep-sea isopod collection stud- ied by the late Professor Ya. Birstein. The collection was first deposited in the De- partment of Invertebrate Zoology of Mos- cow University, was later handed over to the Institute of Oceanology, and finally was deposited in the Zoological Museum of Moscow University. Type locality. —Kurile-Kamchatka Trench, Vityaz Station 5601, 46°26’N, 152°07'E, 2770-2820 m. Additional material. —Japan Trench, Vi- tyaz Station 6671, 40°15'N, 143°35’E, 2500 m. Three adult males (14.8, 14.6, and 12.9 mm long), one male fragment, one damaged female with oostegites (13.8 mm long), two fragments of females. This material was identified by B. Mezhov who kindly showed it to one of the authors (GSV). Diagnosis. — Dorsal and lateral spines on body thin and pointed distally; spines coarsely denticulate. Pleotelson width (ex- cluding spines) subequal to length; lateral spines narrow, length much greater than width. Male pleopod II stylet short, 0.44 of protopod length, with curved hair-like dis- tal part. Uropods much longer than poste- VOLUME 102, NUMBER 2 rior spines of pleotelson; endopod length subequal to exopod length. Remarks.—The specimens from the Ja- pan Trench in general correspond well to descriptions and drawings of syntypes given by Birstein. This species is clearly distin- guished by considerably thinner and longer acute spines on the posterior part of the body; these spines are not bent dorsally and extend far beyond the distal ends of the uro- podal protopodites. The dorsal surface of the pleotelson lacks lumps anterior to the uropods and the pleotelson is relatively nar- row. This species differs from M. Jobispi- natus and M. acutispinatus by considerably longer and thinner spines on the pleotelson, from M. lobispinatus by thin dorsal spines, and from M. acutispinatus by a flattened body. Microprotus antarcticus Vanhoffen, 1914 Microprotus antarcticus Vanhoffen, 1914: 545-546, Fig. 71la-d. Type. —Only a 2 mm long abdomen with a portion of the posterior pereonal segment and a pereopod basis are known. This ma- terial (not examined by the authors) is prob- ably at the Berlin State Museum, East Ger- many, where other Vanhoffen material has been found. Type locality.— Antarctic Indian Ocean, Davis Sea, Gauss station 30.11.1903, 65°27'S, 80°33’E, 3398 m. Diagnosis. —Lateral and posterolateral spines on pleotelson robust and elongate, posterior spines extending to distal tips of uropods. Uropodal exopod distinctly short- er than endopod. Remarks. —Microprotus antarcticus may actually belong in another genus of the Stor- thyngura complex, but until more speci- —— 359 mens are discovered, this species must be retained in Microprotus. With such scarce material at his disposal, Vanhoffen (1914) could not describe this Antarctic species adequately, and could only give comments, comparing the specimen with M. caecus, the only species of the genus Microprotus known at that time. According to Vanhoffen, Pacific (Arctic in Vanhoffen’s term) and Antarctic species differ mostly in that the latter has a low tubercle on the lon- gitudinal thickening of the caudal segment, while in the Antarctic species, the middle spine between both lateral spines looks abrupt. In addition, there are constrictions over the two posterolateral spines, and the uropods are equal in length to the distal spines, with the outer uropodal ramus being only one third of the inner ramus length. In M. caecus, all spines are considerably smaller in comparison with the abdomen, so that uropodal rami, which are subequal in length, extend beyond the distal spines. Judging from the rest of the posterior pe- reonal segment, the lateral spines in M. ant- arcticus are directed backwards, while in M. caecus, they are directed forwards and curved, and the dorsal surface of these seg- ments bears spines. The operculum and oth- er pleopods of the female, which are sche- matically drawn by Vanhoffen in his figure 71d, do not seem useful in his opinion and cannot be used in comparison because the male was known only for the northern species. Vanhoffen (1914) put the genus Micro- protus in his family Jolellidae (sic), where he also assigned the genera Jolella (sic, cor- rectly spelled Jolella Richardson), Janthop- sis (sic, correctly spelled Janthopsis Bed- dard), Acanthaspidia Stebbing, Jolanthe (sic, correctly spelled Jolanthe Beddard), Rhac- Fig. 10. Microprotus acutispinatus, male holotype: A, Pleopod I, ventral view; B, Pleopod II, dorsal view; C, Pereopod I; D, Pereopod II; E, Pereopod VII; F, Uropod. Female paratype: G, Pleopod II. Scale bars: 0.2 mm—A, B, F; 0.3 mm—C; 0.5 mm—D, E, G. 360 ee} PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. it. Microprotus acutispinatus, paratypes, body fragments: A, Female, cephalon and pereonites 1-3, dorsal view; B, Male, cephalon and pereonites 1-3, lateral view; C, Female, cephalon and pereonites 1-3, lateral view; D, Female, pleotelson and pereonites 6—7, lateral view; E, Male, pleotelson and pereonites 5-7, lateral view; F, Female, pleotelson and pereonites 6—7, dorsal view. VOLUME 102, NUMBER 2 ura Richardson, and Jaerella Richardson. These genera were earlier referred to the family Janiridae, owing to the presence of a more or less distinct rostrum, elongate lateral lobes on the body segments, and two or more lateral spines on the abdomen. In Vanhoffen’s opinion, the anterior body part of Microprotus is most similar to that of Tolanthe, but in the last case, the abdomen lacks distinct distal lobes. At the same time, Vanhoffen noted certain similarities be- tween Microprotus and the Munnopsidae, to which he also assigned the Eurycopidae: similar structure of long antennae, which he attributed to the deep-sea mode of life. Van- hoffen’s comments are important, because although Microprotus does not belong to his family “‘Jolellidae,’’ his family concept clearly indicates that certain of the deep-sea *‘Janiridae,”’ Jolella at least, may need to be recognized as belonging to a separate family with its name corrected to Iolellidae. Acknowledgments This paper had its inception when Kus- sakin asked Wilson to examine Microprotus caecus to clarify its relationships with the new species collected during Russian ex- peditions that are described in this paper. We would like to thank Dr. Thomas E. Bow- man, National Museum of Natural History, for loaning the type material of Microprotus caecus, carefully reading the manuscript, and offering suggestions for its improvement. We are also grateful to Dr. Boris Mezhov, Zoo- logical Museum of the University of Mos- cow, for giving us an opportunity to observe Storthyngura paradoxa specimens identi- fied by him. This research was partially sup- ported by National Science Foundation Sys- tematic Biology Grants BSR 82-15942 and BSR 86-04573 to Wilson. 361 Literature Cited Birstein, Ya. A. 1957. Certain peculiarities of the ultra-abyssal fauna with the example of the ge- nus Storthyngura. —Zoologicheskii Zhurnal, 36(7):961-985. 1970. Additions to the fauna of Isopods (Crustacea, Isopoda) of the Kurile-Kamchatka Trench. Part I. Jn Fauna of the Kurile-Kam- chatka Trench and its environment.—Akade- miya Nauk CCCP, Trudy Instituta Okeanologii Im. P. P. Schirshova 86:292-—340. (In Russian, English Translation: Israel Program for Scien- tific Translations, Jerusalem, 1972) Haugsness, J. A., & R. R. Hessler. 1979. A revision of the subfamily Syneurycopinae (Isopoda: Asellota: Eurycopidae) with a new genus and species (Bellibos buzwilsoni).—Transactions of the San Diego Society of Natural History 19(10): 121-151. George, R. Y., & R. J. Menzies. 1968a. Species of Storthyngura (Isopoda) from the antarctic with descriptions of six new species.—Crustaceana 14(3):275-301. ——-;, & . 1968b. Distribution and probable origin of the deep-sea isopod genus Storthyn- gura. —Crustaceana 15(2):171-187. Richardson, H. 1910. Isopods collected in the North- west Pacific by the U.S. Bureau of Fisheries steamer ‘Albatross’ in 1906.— Proceedings of the United States National Museum 37(1701):75— 129. Vanhoffen, E. 1914. Die Isopoden der Deutschen Sudpolar-Expedition 1901-1903.— Deutschen Sudpolar-Expedition 15 Zoology, 7:447-598. Wilson, G. 1989. Deep-sea Lipomerinae and the Munnopsidae (Crustacea: Isopoda: Asellota): a systematic revision. — Bulletin of the Scripps In- stitution of Oceanography 27:i—xiii, 1-138. Wolff, T. 1962. The systematics and biology of bathy- al and abyssal Isopoda Asellota.—Galathea Re- port 6:1-320. (GDFW) A-002, Scripps Institution of Oceanography, La Jolla, California 92093, USA; (OGK & GSV) Institute of Marine Biology, Far East Science Center, Academy of Sciences of the USSR, Vladivostok 690022, USSR. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 362-374 FOUR SPECIES OF SYNOPIIDAE FROM THE CARIBBEAN REGION (CRUSTACEA: AMPHIPODA) J. L. Barnard and James Darwin Thomas Abstract.— Synopia ultramarina is redescribed from the Gulf Stream and the Florida Keys and comments are made on the tangled taxonomy in Synopia. Tiron bellairsi, originally described from Barbados, is reported from Belize, at the opposite side of the Caribbean Basin. Garosyrrhoe bigarra, a Pacific species, is also reported from Belize, but no clear subspecific differences are detected as yet between Pacific and Atlantic populations. Specimens of Synopia ultramarina Dana (1853) are described and illustrated from the Gulf Stream and Synopia scheeleana Bovallius (1886) is also reported. A key to seven species of the genus Synopia was giv- en by J. L. Barnard (1972); Andres (1984) described 2 additional species. Four of the nine species remain poorly described: S. an- gustifrons Dana (1853, tropical Pacific), S. caraibica Bovallius (1886, Venezuela), S. gracilis Dana (1853, tropical Atlantic) and S. orientalis Kossmann (1880, Red Sea). Species of this genus are rarely reported in modern times, perhaps because they occur mainly in neritic waters or in epipelagic waters of the high seas. Collections made in neritic and epipelagic waters rarely are ex- amined by gammaridean taxonomists, who appear to concentrate on benthic samples. Two of the species come from the tropical Pacific where little neritic collecting has been accomplished this century. Individuals of Synopia may actually be mostly nighttime emergents into neritic waters though they appear to occur in daytime in epipelagic waters particularly in or near sargasso-like flotsam. We have searched for S. caraibica in neritic waters in the daytime in Florida, Belize and Trinidad, to no avail. Pereopods 5-7 of that species have ovate article 2 of pereopods 5-7 but otherwise the species is well enough described by Bovallius to sug- gest 1t is not a species of Jiron, a better known genus than Synopia. Synopiidae Synopia Dana Synopia Dana, 1852:315 (Synopia ultra- marina Dana, 1853, selected by J. L. Bar- nard, 1969b).—J. L. Barnard, 1972:50. Diagnosis. — Forehead protuberant (pos- sible exception, S. orientalis); lateral ce- phalic lobe not sharp. Eyes and accessory eyes present. Antenna | of female shorter than pereon, of male much longer than pere- on. Mandible with huge palp (mainly article 2), molar large, triturative or swollen, pil- lowlike in shape and poorly triturative (S. variabilis). Outer plate of maxilla 1 with eight or nine spines. Maxilliped inner plate lack- ing large smooth spines; outer plate fur- nished medially only with plumose setae (no inflexible spines). Coxae 1-2 small, similar, truncate dis- tally; coxae 3-4 pelagont, coxa 3 very large and enfolding small coxa 4. Gnathopods simple (propodus of gnathopod 1 often tumid), defining spines absent; gnathopod 2 very slender, dactyl tiny. Pereopods 3—4 slightly to strongly diversified, articles 4—5 stout; pereopods 5-7 elongate. Pleonites 1-6 neither denticulate nor toothed. Uropod 3 exceeding uropods 1-2, peduncle short. Telson relatively short for family. Relationship. — Differing from TJiron in the shorter peduncle of antenna 1, thick man- VOLUME 102, NUMBER 2 dibular palp, presence of only 8—9 spines on the outer plate of maxilla 1, the absence of large smooth apical spines on the inner plate of the maxilliped, the outer plate bearing only medial plumose setae, no smooth spines; the much enlarged coxa 3; inflated propodus of gnathopod 1; tiny dactyl of gnathopod 2; diversity and tumidity of pe- reopods 3-4; lack of dorsal body teeth; and relatively shorter telson. Remarks. —We believe that Barnard (1965) misrepresented the mandibular mo- lar of S. variabilis as being non-triturative; he apparently did not turn the molar far enough upward to see the triturative sur- face. Key to the Species of Synopia _. JES LS i 2 = 2117 00S ee 4 2. Apex of telson broad and armed with 3 widely spread spines ...... rotunda — Apex of telson narrow and armed with 2 or fewer appressed spines .. 3 3. Telson with 2 notches separated by subtruncate protrusion, bearing only setules variabilis — Telson with single apical notch armed with 2 spines ....... triangula 4. Forehead not protuberant .. orientalis —eenoneag protuberant ........... 5 5. Article 2 of pereopods 5-6 rectan- gular or with quadrate posteroven- i Sto SE ae 6 — Article 2 of pereopods 5-6 ovate or with rounded posteroventral cor- SES |. a 7 6. Article 2 of pereopod 5 narrowly rectangular, scarcely twice as broad as article 3 and with scarcely pro- truding posteroventral corner .... _ 2 fe angustifrons — Article 2 of pereopod 5 widely rect- angular, nearly twice as broad as ar- ticle 3 and with strongly protruding posteroveniral Corner ........ gracilis 363 7. Flagellar articles 2, 3,4...n ofan- tenna | with long “‘hairs’’* .. caraibica — Flagellar articles 2, 3,4...nofan- tenna | lacking long “‘hairs”’ 8. Telson scarcely longer than broad, apicolateral margins smooth, each apex with one stout spine .. scheeleana — Telson much longer than broad, apicolateral margins crenulate, each apex with one stout spine and one Femeiseed ys oes. 28002 ultramarina Synopia ultramarina Dana Fig. 1-4, part Synopia ultramarina Dana, 1853:995, pl. 68, fig. 6a—h.— Bovallius, 1886:613, pl. 1, figs. 1-21. Diagnosis.—Telson much longer than broad, deeply cleft, apicolateral margins scalloped-serrate, each apex with one long seta, one short setule, medial subapex with spine in notch. Forehead protuberant, with anterodorsal keel. Article 2 of pereopods 5— 6 broadly rounded posteroventrally, of pe- reopod 7 subrectangular and quadrate pos- teroventrally. Flagellar articles 1, 2, 3 on antenna 1 of both sexes with at least one stout spine, short in male, elongate in fe- male. Description of female “u’’ 4.53 mm.— Head with low anterior keel: rostrum ex- tending downward to shallow keel connect- ed to epistome, upper lip weakly bilobate from lateral view and bilobate from anterior view. Eyes purple in alcohol, pigment dif- fuse (omitted in drawings), accessory eye of 2 ommatidia each stained purple on inner apices. Accessory flagellum 2-articulate, basal ar- ticle elongate, armed with stiff spines; pri- mary flagellum short, 8-articulate, articles 1-5 and 7 each with stiff spine, spines longer on articles 1—3 than on 5 and 7. Each incisor * Structure unknown, possibly setae, aesthetascs, or straw-like scales. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 364 x ‘en rt ft 625 aaa VOLUME 102, NUMBER 2 and left lacinia mobilis with 4 teeth, mght lacinia mobilis bifid and weakly hook- shaped, larger rakers about 4 left, 7 right, first 2 or 3 when turned to plane view bifid; molar heavily triturative, armed basally with large brush of apically feathered setae. Inner plate of maxilla 1 with 5 large medial setae and 2 short apical setae, outer plate with 8 spines, apex of palp with 5 tooth-spines (one illustration showing 4 as aberrancy), medial oral face with groups of 3 and 4 apical setae. Two principal apical spines on inner plate of maxilliped plumose, with two other api- cal setae, one apicoventral seta, two medial setae and one ventral locking spine; medial margin of outer plate with marginal and ventral submarginal rows of plumose setae, lateral margin with two long setae, one ap- icad, the other strongly subapical, lateral base raggedly serrate; article 2 of palp evenly and densely setose medially; dactyl short, nail elongate. Many setae on gnathopod 2 apically forked; dactyl with shriveled appearance (but this appearance normal). Pereopods 3-4 with three unlocking setae each, pereopods 5-7 with two unlocking spines each, short and simple on pereopod 7, on pereopods 5-— 6 one spine elongate and with apical hooded hook. Gills large, unpleated, on coxae 2-7; oostegites, thin, strap-shaped, sparsely se- tose, on coxae 2-5. Epimera naked below, epimeron | sharp- ly quadrate, epimeron 2 with small tooth and epimeron 3 round-quadrate postero- ventrally. Each pleopod with two coupling hooks and one plumose accessory spine, pe- duncles with 1-3 setae only, rami with 12- 14 articles, inner rami with one fewer article —_ Fig. 1. 365 than outer rami and with forked basomedial spines, generally two. Urosomite 3 with posterodorsal spine. Outer rami of uropods 1-2 with dorsolateral comb, similar comb on inner rami ventro- lateral. Telson scarcely longer than pedun- cle of uropod 3, cleft about two-thirds, cu- ticle covered with notch-like lunes. Male “q’’ 5.84 mm.—Antenna 1 about 4.0 mm long, antenna 2 about 5.9 mm long. Eyes slightly larger than in female. Basal article of primary flagellum slightly longer than in female and callynophore denser; ar- ticles of primary flagellum with extra mid- ventral male sensory setules, large spines of female reduced in size. Dorsal margins of articles 4—5 of peduncle of antenna 2 plus articles of flagellum bearing dense male sen- sory setules. Epimera and pleopods larger than in female, epimeron 2 lacking tooth. Uropod 3 more setose than in female. Intermediate male “‘s’’ 4.33 mm.—Eyes scarcely enlarged. Antenna 1 elongate but basal spines of flagellum elongate as in fe- male. Posterior setules on flagellum of an- tenna 1 and anterior setules on antenna 2 poorly developed. Tooth of epimeron 2 in- termediate between male and female. Setae of uropod 3 moderately developed. Illustrations. —Maxilla 1 magnified more than maxilla 2; telson magnified more than uropod 3. Material. —MFP-1, in Gulf Stream, off Grand Bahama Island, 27°26'N, 78°57’'W, 219 m, 8 Jul 1986, coll. Jack Morton, at- tracted to night light, female “‘p” 4.35 mm, male “‘q’’ 5.84 mm (illustrated), female “‘r”’ 4.40 mm, male “s’’ 4.33 mm, male “‘t”’ 4.79 mm, female “‘u’’ 4.53 mm (illustrated) (and Synopia ultramarina, unattributed figures = female “‘u’’; q = male “‘q.”’ Capital letters as follows refer to parts; lower case letters to the left of capital letters refer to specimens noted in legends; lower case letters to right of capitals refer to adjectival modifications in list below: B, body; D, dactyl; G, gnathopod; H, head; I, inner plate or ramus; J, prebuccal; L, labium; M, mandible; O, outer plate or ramus; P, pereopod; R, uropod; S, maxilliped; T, telson; U, labrum; V, palp; W, pleon; X, maxilla; a, anterior; d, dorsal; 0, opposite; r, right; s, setae removed; t, left; x, apex. 366 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ee Fig. 2. Synopia ultramarina, unattributed figures = female “u”; q = male “q.” Letter codes, see Fig. 1. VOLUME 102, NUMBER 2 367 eee 99. u’’; q = male “q.”’ Letter codes, see Fig. 1. 368 6 other specimens). LKFR-5, Florida Keys, Looe Key Reef, 7 m, sand plain in front of fore reef zone, 9 Oct 1983, 2300 h, night light, full moon, coll. J. D. Thomas (35 spec- imens). Remarks. —Said by Dana (1853) to be “rich blue, to nearly colorless, with tinge of rich blue along the venter or about the ar- ticulations’’; our specimens and those of the first redescriber, Bovallius (1886), however were hyaline with yellowish cast when caught alive, mouthparts, especially maxillipeds with red cast under microscopy seen to be represented by tiny red granular inclusions below the chitinous exoskeleton. One may wonder if Dana might not also have col- lected S. scheeleana; he called the “‘male specimen”’ of S. u/tramarina ““ultramarine” but labeled it on his plate as S. gracilis and changed its identification in the published text; S. gracilis has since been recognized as a distinct species but has never been clari- fied adequately; unfortunately Dana’s ma- terial is presumed to have been lost in the great fire of Chicago, 1871; see other notes below. Despite the color, Bovallius chose this species to represent Dana’s u/tramarina on the basis of serrate telson and conformity in pereopods 5-7; we agree that this solution is correct on morphological grounds. Relationship. — Differing from the well defined S. scheeleana Bovallius (1886) in the longer telson bearing apicolateral ser- rations and at least one long apical seta on each lobe. Synopia caraibica Bovallius (1886) has article 2 of pereopod 7 ovate like that of pereopods 5-6. Synopia angustifrons Dana (1853) and S. gracilis Dana (1853) have ar- ticle 2 of pereopods 5-7 rectangular or with quadrate posteroventral corners. There is the possibility that Dana misinterpreted these legs as there is no indication he dis- sected them off the animal and pressed them flat. Synopia orientalis Kossmann (1880) does not have a protuberant forehead. The telson of S. variabilis Spandl (1923, see J. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON L. Barnard, 1965), S. triangula Andres (1984) and S. rotunda Andres (1984) is un- cleft. Distribution. —Tropical western Atlantic; specific localities include Cuba, Bahamas, Florida Keys and Dana’s 8-12°S, 11l- 144%4°W, 4-7°S, 21—25°W; neritic and pre- sumably epipelagic on the high seas; attract- ed to night lights. Synopia scheeleana Bovallius Synopia scheeleana Bovallius, 1886:16-18, pl. 2, figs. 22—-29.—Stebbing, 1888:799-— 804, pl. 52.—Chevreux, 1900:54.— Reid, 1951:233. Material.—Gulf Stream, 40 miles off Florida coast between Miami and Fort Pierce, 10 Dec 1987, R/S Sea Diver, male “a” 2.52 mm, specimen “‘b”’ 1.80 mm. Remarks. —Live color deep blue to s-blue, nos. 178 to 179, as matched to ISCC-NBS Centroid Color Chart 2106; we described this in the laboratory as cobalt blue; spec- imens courtesy of Dr. Mary E. Rice, Direc- tor, Smithsonian Research Station at Link- port. Distribution. — Atlantic Ocean, off Ft. Pierce, Florida to Barbados; tropical Pacific Ocean; assumed to be epipelagic. Tiron bellairsi Just Fig. 4, part Tiron bellairsi Just, 1981:259-263, figs. 14. Diagnosis. — Accessory eye composed of 2 and | separated ommatidia; accessory fla- gellum 2-articulate; labrum densely spi- nose; palp of mandible replaced by seta; in- ner plate of maxilla 1 long and thin, fully setose medially but setae small and widely spread, outer plate with 10 spines forming elongate multi-sigmoid cluster, palp re- duced, about half as long as outer plate; in- ner plate of maxilla 2 with row of submar- ginal setae; inner plate of maxilliped lacking thick simple spines; outer plate of maxil- VOLUME 102, NUMBER 2 369 ST OX1 Fig. 4. Left upper = Synopia ultramarina, male “‘q.”’ Right, Tiron bellairsi, male “‘o,”’ note 3 renderings of outer plate on maxilliped. Letter codes, see Fig. 1. 370 liped abnormal, lacking major spines, bear- ing plumose and tube-setae; dactyls of pe- reopods 3-7 stubby, nails scarcely curved; article 2 of pereopods 6—7 without special setal row, article 2 of pereopod 7 weakly crenulate and setulose posteriorly; pereon- ites 5—7 and pleonites 1-3 dorsally crenu- late, pleonite 4 with medium dorsal tooth, pleonite 5 with large dorsal tooth, pleonite 6 lacking tooth; outer ramus of uropod 1 as long as inner ramus but outer ramus of uro- pod 2 slightly shortened; rami of uropod 3 apically blunt; telson with one apical spine and 3 setae on each side, no dorsal or medial spines. Remarks. —We have redrawn minute de- tails of several mouthparts and the telsonic apex; we assume these are congruent with the Barbados population. The diagnostic format above is revised to include new char- acters not used by Barnard (1972). Material.—JDT Bel-53, Belize, Carrie Bow Key, 34 m, sand trough near fore reef drop-off, in coralgal mud, 11 Jun 1980, coll. J. D. Thomas, male “o” 2.49 mm (illus- trated), 2juvenile “‘p” 1.96 mm. Distribution. — Barbados, Holetown (type- locality), 5—? m (‘SCUBA”’ depths); Belize, Carrie Bow Cay, 34 m. Garosyrrhoe bigarra (J. L. Barnard), new synonymy Figs. 5-6 Syrrhoites bigarra J. L. Barnard, 1962:73- 1S USN Garosyrrhoe disjuncta J. L. Barnard, 1969a: 224-225, fig. 30. Taxonomy.—Syrrhoites bigarra and Ga- rosyrrhoe disjuncta are the male and female of the same species. The male is character- ized by the larger head with blunter ros- trum, elongate antenna 2 and more aes- thetascs and male setae on antennae 1-2. Barnard (1962) overlooked the complex na- ture of the dorsal teeth on pereonite 7 to pleonite 3. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON The Caribbean specimens are smaller than those from the eastern Pacific, where the species has been found between about 25° 32°N. As yet no specimens from the Pan- amanian isthmus region have been found and until comparisons between specimens from exactly similar latitudes and thermal regimes from Pacific and Atlantic waters can be compared, the small differences we find in the Atlantic specimens cannot be attrib- uted to speciation. Both sexes of material from Belize have fewer serrations on the epimera and the fe- male lacks serrations on article 6 of pereo- pod 4. Other differences between bigarra and disjuncta cited by Barnard (1969a) are inconsistencies lacking specific value as demonstrated in the present material and reexamination of the earlier materials. For example, the ventral spine on the inner plate of the maxilliped and the dorsally promi- nent pleonal teeth were overlooked in var- ious specimens; differences among pereo- pods are simply variables. Any of the differences, albeit minor, between individ- uals from different oceans, could be attrib- uted to the smaller adult size of Caribbean specimens. Small potential distinctions of specific value between Atlantic and Pacific populations may be present in articular pro- portions and armament patterns but con- firmation of these requires study of larger suites of Pacific material than are now avail- able. The following descriptions contain only new information and points we judge to be necessary to amplify and rectify the former depiction of this genus and species; illustra- tions are provided for characters which are difficult to visualize from descriptions. Description of male “‘x’’ 3.12 mm.—Pe- duncular articles 1—2 of antenna 1 with nu- merous dorsal aesthetascs, multiple aesth- etascs also present on articles 1-2 of accessory flagellum and article 1 of primary flagellum; on antenna 2 similar aesthetascs on article 4 of peduncle, aesthetascs on ar- ticle 5 apically curled, basal articles of fla- gellum also with multiple aesthetascs. VOLUME 102, NUMBER 2 a7 Fig. 5. Garosyrrhoe bigarra, unattributed figures = male “x”; w = female “‘w.” Letter codes, see Fig. 1. S72 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 6. Garosyrrhoe bigarra, male “*x.”” Letter codes, see Fig. 1. VOLUME 102, NUMBER 2 Right and left mandibular incisors with three large and one small teeth, each lacinia mobilis with five teeth, first raker on each side broadened, more so on left than on right mandible, right and left mandibles each with total of two and three rakers. Outer plate of maxilla 1 with 11 spines (versus 9 in Pacific material), inner plate with 6 me- dial setae, palpar apex with 4 spines, one apicolateral seta, 2 mediofacial setae. Inner plate of maxilliped with 5 subapical setae, 2 medial setae, one apicomedial spine, one ventral hooked locking spine; outer plate with 8 marginal spines and one apical spine- seta. Articles 4-5 of pereopod 5 more sparsely armed than in Pacific male (pereopods 6-7 in Pacific male unknown). Dactyl of pereo- pod 7 lacking comb present on pereopods 3-6. Serrations on epimera 1,2,3 = 2-4-9 (versus 4-7-12 on Pacific male). Details of one dorsal pleonite plus uropod 3 and telson are shown in illustrations. Female “w’” 3.40 mm (body slightly con- tracted). —Serrations on epimera 1,2,3 = 2-2-9 (versus 5-6-13 in Pacific female). Material.—JDT BEL-53, Belize, Carrie Bow Cay, 11 Jun 1980, forereef sand trough, 29 m, coralgal sand-mud, coll. J. D. Thom- as, female “w”’ 3.40 mm, male “x”? 3.12 mm and 4 other specimens. Also found in sim- ilar samples: JOT BEL-9B,C,D; JDT BEL- 14; -19; -53. Associated in amphipod com- munity on coralagal sediments at depths of 27 to 33 m with Netamelita and Hornellia. Distribution. —Southern California at border with Mexico and in Gulf of Califor- nia, 24-44 m; Caribbean Sea, Belize, 27- 33 m. Acknowledgments We thank Captain Jack Morton and stu- dents of the Marine Field Projects class of 1986, Florida Institute of Technology, Mel- bourne, Florida, for collecting amphipods while at sea. The second author was sup- ported by NSF grant BSR-8515186. 373 Literature Cited Andres, H. G. 1984. Zwei neue Synopiiden (Crus- tacea: Amphipoda: Gammaridea) aus dem war- men zentralen Nordatlantik. — Mittheilungen aus den Hamburg Zoologisch Museum und Institut 81:109-116. Barnard, J. L. 1962. Benthic marine Amphipoda of southern California: Families Tironidae to Gammaridae— Pacific Naturalist 3:70-115. 1965. Marine Amphipoda of atolls in Mi- cronesia. — Proceedings of the United States Na- tional Museum 117:459-552. 1969a. A biological survey of Bahia de los Angeles Gulf of California, Mexico, IV. Benthic Amphipoda (Crustacea).— Transactions of the San Diego Society of Natural History 15:175- 228. 1969b. The families and genera of marine gammaridean Amphipoda.— United States Na- tional Museum Bulletin 271:535 pp. 173 figs. 1972. A review of the family Synopiidae (=Tironidae), mainly distributed in the deep sea (Crustacea: Amphipoda).—Smithsonian Con- tributions to Zoology 124:1-94. Bovallius, C. 1886. Amphipoda Synopidea.— Nova Acta Regiae Societatis Scientiarum Upsaliensis 13:1-36. Chevreux, E. 1900. Amphipodes provenant des cam- pagnes de /’Hirondelle (1885-1888). — Résultats de Campagnes Scientifiques Accomplies par le Prince Albert I Monaco 16:iv and 195 pp., 18 pls. Dana, J. D. 1852. On the classification of the Crus- tacea Choristopoda or Tetradecapoda. — Amer- ican Journal of Science and Arts (2) 14 [Appen- dix]:297-316. . 1853. Crustacea. Part II.— United States Ex- ploring Expedition 14:689-1618, atlas of 94 pls. published in 1855. 1981. Tiron bellairsi sp. n. (Amphipoda, Sy- noplidae) from coral sand in Barbados, with notes on behaviour.— Zoologica Scripta 19:259- 263. Kossmann, R. 1880. Malacostraca. Zoologische Er- gebnisse einer im Auftrage KOniglichen Aca- demie der Wissenschaften zu Berlin ausgefuhr- ten Reise in die Kustengebiete des Rothen Meeres. Zweite Halfte, Erste Lieferung. III. Ma- lacostraca 67-140, pls. 4-15. Leipzig: Wilhelm Engelmann. Reid, D. M. 1951. Report on Amphipoda (Gam- maridea and Caprellidea) of the Coast of Trop- ical West Africa. — Atlantide Report 2:189-291, 58 figs. Spandl, H. 1923. Amphipoden der ‘Pola’-Expediti- onen in das Rote Meer.—Akademie der Wis- Just. Ff 374 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON senschaftlichen in Wien, Anzeiger, Jahrgang 60: 17-20, 87-89, 111-112. Stebbing, T. R. R. 1888. Report on the Amphipoda collected by H.M.S. Challenger during the years 1873-76. Report on the scientific results of the voyage of H.M.S. Challenger during the years 1873-1876, Zoology 29: xxiv and 1737 pp., 210 pls. (JLB) NHB-163, Division of Crustacea, Smithsonian Institution, Washington, D.C. 20560; (JDT) Newfound Harbor Marine In-. stitute, Rt. 3, Box 170, Big Pine Key, Flor- ida 33043. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 375-384 A NEW SPECIES, AMPELISCA BURKET, (CRUSTACEA, AMPHIPODA) FROM FLORIDA J. L. Barnard and James Darwin Thomas Abstract. — A new species Ampelisca burkei, from Florida, is described. This species appears to be very close to A. /obata Holmes, from the eastern Pacific Ocean, but differs in the shape and setation of article 4 on pereopod 7, and the presence of an anteroventral spine-seta on article 5 of pereopod 7. The new species, Ampelisca burkei de- scribed herein is a twin of A. Jobata Holmes from the eastern Pacific. The differences be- tween the two species are very small but recognition of both is justified by the trend for taxonomists to find and validate at the specific level small differences between Pa- cific and Atlantic amphipods. Small mor- phological characters are extremely consis- tent over wide geographic areas in the family Ampeliscidae. This consistency is not widely shared by amphipod groups, and care must be taken to document variation in particular characters before incorporating them into a taxonomic treatment. For example, Bar- nard (1980) separated the Pacific Methar- pinia oripacifica from the Atlantic M. flor- idana by the presence or absence of a single spine on the inner plate of the maxillipeds (2 spines in Pacific, one in Atlantic popu- lations). Dickinson (1982) separated the Pa- cific Ampelisca fageri from the Atlantic A. schellenbergi on subtle shapes and setation patterns of coxa 1, pereopod 7 and uropod 3. Ampelisca burkei, new species Figs. 1-5 ?Ampelisca lobata.—J. L. Barnard, 1954b: 2 (not Holmes, 1908, possible misidenti- fied specimens from Colombia and Aru- ba). Description of holotype, male, 4.92 mm.— Body smooth; urosomite | elevated, with thick keel, urosomites 2—3 coalesced, with strong dorsal saddle. Head as long as first three pereonites com- bined, slightly longer than tall, with short rostrum; head with lobe below attachment of antenna 1, then head sloping down and posteriorwards in two steps, no ventral tooth. One corneal lens present on each side strongly removed from anterior margin, second pair on ventral margin far below lat- eral lobe. Brown (unusual) pigmentary mass present for each lens, similar mass behind upper pair. Antenna | slender, much shorter than an- tenna 2, reaching 25 percent along flagellum of antenna 2; peduncle short, articles 1—2 equally long, article 3 short; base of flagel- lum forming callynophore; accessory fla- gellum absent; main flagellum 5 times as long as peduncle, first 2 articles with aes- thetascs attached ventrally. Antenna 2 about 2.4 times as long as antenna 1, about 1.4 times as long as body, peduncular article 5 almost as long as 4, anterior margins of ar- ticles 3—5 with male setular tufts, flagellum 3 times as long as peduncle. Epistome weakly and obtusely projecting anteriorly, labrum incised distally, broader than long (tall). Labium normal, with well- developed inner lobes. Mandible with well-developed strong tri- turative molar, incisor toothed; palp 3-ar- ticulate, article 1 short, article 2 longer than 3, setose, article 3 non-falciform, not dilated distally, with 3 D setae, 4 E setae. Maxilla 1: inner lobe with 2 short simple 376 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 7 et yn ee eal (A tins 2 Re x ee “ | \ 44th 7 | ee a iG eee f Gi EEE Yi SoS | iK 1 2 ; SN TA | Gim 4 HE aaa ate 5 Vice Ge fie hab rated, 7] ff com kE3 VOLUME 102, NUMBER 2 setae, outer lobe with 11 spines, three of these provided with 2-4 lateral teeth each; palp 2-articulate, symmetrical on both sides, second article barely dilated distally, pro- vided with 4 distal sharp cusps accom- panied by 4 spines, 4 subdistal setae and 2 apicomedial setae. Maxilla 2 with narrow lobes, inner lobe shorter than outer, without oblique facial row of setae, all medial setae marginal. Maxilliped: inner lobe of ordinary length, with 2 distal spines intermixed with several plumose setae; outer lobe reaching apex of palp article 2, bearing row of thick spines along medial margin and 2-3 apical setae; palp 4-articulate, article 3 not lobed, article 4 with main nail about as long as remaining part of article. Coxae 1—4 much longer than broad, coxa 1 dilated distally, with convex distal (=ven- tral) margin provided with one row of tiny setae, lacking posteroventral notch; coxae 2—4 with increasingly truncate distal mar- gins, coxae 2—4 with increasingly sparse set- ules, coxa 4 with small posteroproximal lobe produced bluntly in proximal part, other- wise apposite margins almost parallel. Gnathopods 1-2 linear, simple, gnatho- pod | shorter than gnathopod 2; gnathopod 1: article 5 scarcely longer than 6, densely setose along posterior margins, article 6 ta- pering distally with dactyl shorter than ar- ticle 6, bearing 5 setules along inferior mar- gin and | seta on outer margin. Gnathopod 2: article 5 linear, long, moderately setose; article 6 much shorter than 5, tapering dis- tally, dactyl like that of gnathopod 1. Pereopod 3 of medium stoutness, with articles 4-6 bearing long plumose setae along both margins, except posteriorly on article 6 and anteriorly on article 5; article 4 not inflated; dactyl slender, almost straight, , eel Fig. 1: 377 slightly longer than article 6. Pereopod 4 like that of pereopod 3, but much longer, article 4 setose on both sides to base. Pereopod 5: article 2 ovoid, with large posterior flangehump, anterior margin with one row of plumose setae, article 5 scarcely produced distoposteriorly, bearing row of spines on apex; article 6 with few long distal setae, dactyl short, unguiform, with 2 outer cusps. Pereopod 6: article 2 subquadrate, with strong posterior lobe and poorly setose anterior margin; articles 3-7 like those of pereopod 5. Pereopod 7: almost as long as pereopod 6 but article 2 large, scarcely ex- panding distalwards, lobe reaching middle of article 4, bearing sparse plumose setae along ventral margin in two disjunct groups; article 3 short; article 4 slightly longer than 3, weakly produced at posterodistal apex and bearing one short spine and posterior setae; article 5 narrow, with weak postero- distal spination and one anterior subdistal spine-seta, article 6 weakly tumid, scarcely longer than 5, dactyl tumid, tapering rapidly and apically pointed, much shorter than ar- ticle 6. Strongly plaited large gills on coxae 1-6, gills generally with 20+ pleats. Pleopods well developed, normal, with 2 retinacula and one simple accessory retinaculum each. Epimera 1-2 weakly convex behind, epimeron 1 with posteroventral setule at subsharp corner, epimeron | with 3 ventral setae; epimeron 3 not larger than 2, poste- rior margin almost straight, posteroventral corner sharply protuberant or obtuse (vari- able). Uropods 1-2 of ordinary length, uropod 1: peduncle slender, outer face of peduncle with 5 spines, dorsolateral margin with 3 spines, apex with cusp, medial corner with Ampelisca burkei, n. sp., unattributed figures, holotype male “h”’ 4.92 mm; k = male “k” 4.66 mm. Capital letters denote main parts in following list; lower case letters to left of capital letters or in body of figure indicate modifications as per following list; lower case letters to right of capital letters indicate specimens described in captions: A, antenna; C, coxa; D, dactyl; E, epimera; G, gnathopod; H, head; L, lower lip; M, mandible; P, pereopod; R, uropod; S, maxilliped; T, telson; U, upper lip; W, pleon; X, maxilla; m, medial. 378 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Ampelisca burkei, n. sp., holotype male “h” 4.92 mm. Letter codes, see Fig. 1. VOLUME 102, NUMBER 2 379 Fig. 3. Ampelisca burkei, n. sp. Upper, holotype male “‘h” 4.92 mm. Lower, female “‘o” 5.66 mm. Letter codes, see Fig. 1. 380 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 4. Ampelisca burkei, n. sp., unattributed figures = female ““m” 4.40 mm; h = holotype male “h” 4.92 mm. Arrows on hA2 and mH point to lines denoting undrawn lengths of antennae. Letter codes, see Fig. 1. Wie at Noyiratesar inurl) 6) > roy "Waray: 7 Fig. 5. Ampelisca burkei, n. sp. Upper, female ““m’ 4.40 mm. Lower, female “‘o” 5.66 mm. Letter codes, see Fig. 1. 382 2 spines, medial margin with 5 other spines, rami slender, as long as peduncle, curved and pointed distally, outer with 2 tiny lat- eral spines, medial margin with 4 spines, inner ramus lacking lateral spines, with 7 medial spines. Uropod 2: peduncle slender, slightly shorter than outer ramus, with 3 moderately spread dorsolateral and 3 tightly packed dorsomedial spines, with apicolat- eral cusp, outer ramus smaller than inner, of triangular cross-section, with 4—5 dorsal spines, 2 basomedial spines and one tiny lateral spine, inner ramus with 1 lateral spine, and 7—8 medial spines. Uropod 3 long, subfoliaceous, strongly exceeding apex of uropod 2: peduncle stout, short, with 2 me- dial spines; rami extending subequally, in- ner foliaceous, with sharp apices, outer much narrower than inner, setose laterally, and apicomedially, inner lined with stout me- dial spines paired with plumose setae, extra setae in gaps between spines. Telson reaching one third along rami of uropod 3, longer than broad, incised 90 per- cent of its length, each lobe expanding in middle and then tapering distally, notch narrowly beveled apically, each with apical spinule, 2 dorsal axial spines and subbasal pair plus satellite of penicillate setules (one spine occasionally substituted by pair of set- ules). Male “‘k.’’—Antenna 2 only 0.8 times as long as in holotype. Female ““m’’ 4.40 mm.—Oostegites on coxae 2—5 strap-shaped, narrow, weakly se- tose. Antenna | slightly exceeding peduncle of antenna 2, peduncle short, article 2 as long as 1, flagellum with few basal aesthe- tascs. Antenna 2 elongate, article 5 of pe- duncle slightly shorter than article 4. Gills much smaller than in male and with about 5—6 pleats. Hump on pleonite 4 lower than in male. Dorsolateral margin on peduncle of uropod 1 with 3 spines, inner apex with spine pair, medial margin with 3 other spines, outer ramus with 2 lateral and 3 me- dial spines, inner ramus with 3 medial spines; peduncle of uropod 2 with 2 dor- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON solateral spines, inner apex with triad of spines, medial margin with one other spine, outer ramus with 3 dorsal and one medial spines, inner ramus with 4 medial spines, other spine positions noted for male with- out spines. Outer ramus of uropod 3 slightly shorter than inner, with 5 lateral setal po- sitions bearing 1—2 setae each, apex notched and with 2 setae; inner ramus with 4 api- colateral setules, inner margin with 5 spine- notch positions. Telson with only one dorsal spine on each lobe besides one apical spine. Notes on the redescription of Ampelisca lobata by Dickinson, 1982.—Dickinson’s figure 5 of a female from North Bank Island, British Columbia, does not show details of pereopod 7 but in the small view presented lacks posterior setae on article 6 (a pre- sumed oversight) and lacks the anteroven- tral seta-spine on article 5 which is present in the Floridian material and was shown to be absent by Barnard on males (1954a). Dickinson does not show the basal aesthe- tascs on the flagellum of female antenna 1. Both inner rami of uropods 1—2 of Dick- inson’s specimen bear one lateral spine but none is present on Floridian female mate- rial; we assume this may have connection with size differences because the British Co- lumbian material also has many more pe- duncular and inner marginal rami spines than our females. Illustrations. —Left male uropod 3 drawn ventral side up. Etymology. —Named for the late William W. Burke, III, an original ““Son of Bennett” (honorary society of biologists at Louisiana State University), who first worked with Ampelisca in the marshes of Louisiana. Holotype. —USNM_ 195153, male ‘“h” 4.92 mm, illustrated. Type locality. —Florida Keys, Looe Key Reef, forereef, 8 m, Apr 1982, full moon 2200 hours, night diving, attracted to night light, coll. J. D. Thomas. Material.—Type locality, male “1” 4.72 mm, male “‘j” 4.84 mm, male “k” 4.66 mm and 29 other specimens. Females collected VOLUME 102, NUMBER 2 at same site, LKFR-1C, 18 Apr 1982, from algal turf community on Acropora cervicor- nis forereef, 8 m, coll. J. D. Thomas, female “1”? 4.69 mm, female ““m” 4.40 mm (illus- trated), female “‘o” 5.66 mm (illustrated) and 10 other specimens. Relationship. —Ampelisca burkei is easily distinguished from such sympatric species as A. abdita Mills (1964), A. vadorum Mills (1963) and A. declivititis Mills (1967) by the short article 3 of pereopod 7. The following species of Ampelisca bear similarities to A. burkei: A. agassizi Judd (see Dickinson 1982), A. holmesi Pearse (1908) (see Goeke & Gathof 1983), A. panamensis J. L. Bar- nard (1954a), A. parapanamensis J. L. Bar- nard (1954b), A. verrilli Mills (see Bousfield 1973), A. lobata Holmes (see Dickinson 1982), A. hancocki J. L. Barnard (1954a), A. milleri J. L. Barnard (1954a), A. cucullata J. L. Barnard (1954a), and A. romigi = is- ocornea J. L. Barnard (1954a). Ampelisca burkei differs: from eastern Pa- cific A. /Jobata in the weaker expansion and fewer setae on article 4 of pereopod 7, the presence of an anteroventral spine-seta on article 5 of pereopod 7 and the lack of a protrusion apically on article 5 of pereopod 5 in the female; from A. verri//iin the slender pereopod 7, short article 2 of antenna 1, lack of tooth on epimeron 3 and widely expand- ed head; from A. cucullata and A. agassizi in the slender articles 2-6 of pereopod 7, and short article 2 of antenna 1; from A. romigi in the smaller posteroventral lobe on article 4 of pereopod 7, less beveled article 2 of pereopod 7, short article 2 of antenna 1 and narrower posterior flange-lobe on ar- ticle 2 of pereopod 5; and from the male A. isocornea form by the large spines on female uropod 3, much larger process of pleonite 4 and lack of facial spines on article 6 of pereopod 7; from A. hancocki in the shape of pereopod 7, numerous spines of uropods 1-2, longer antenna | and shape of coxa 4; from A. milleri in the short article 3 and general shape of pereopod 7, dense spina- tion of uropods 1-2, and shape of coxa 4; 383 from A. panamensis and A. parapanamensis in the broad head and narrow articles 4—5 of pereopod 7; and from A. ho/lmesi in the short article 2 of antenna 1, narrower pereo- pod 7 and broader head. As far as we know, this species differs from all other American species of Ampe- lisca in the brown (versus red) pigment of the eyes; the species therefore looks super- ficially like a species of Bybiis. Distribution. —Florida Keys, Looe Key Reef, 0-8 m. Acknowledgments We thank Linda B. Lutz of Vicksburg, for inking our drawings; Janice B. Clark of Smithsonian for laboratory assistance; and the following referees who helped improve this study: Dr. James K. Lowry of the Aus- tralian Museum, and Dr. Thomas E. Bow- man of Smithsonian Institution; and anon- ymous referees. The junior author was supported by Grant BSR 8515186 from the National Science Foundation. Literature Cited Barnard, J. L. 1954a. Amphipoda of the family Am- peliscidae collected in the Eastern Pacific Ocean by the Velero III and Velero IV.—Allan Han- cock Pacific Expeditions 18:1—137, pls. 1-38. . 1954b. Marine amphipoda of Oregon.—Or- egon State Monographs, Studies on Zoology 8: 103. 1980. Revision of Metharpinia and Micro- phoxus (marine Phoxocephalidae Amphipoda from the Americas).— Proceedings of the Bio- logical Society of Washington 93:104—135. Bousfield, E. L. 1973. Shallow-water Gammaridean amphipoda of New England. Ithaca & London, Cornell University Press, vii—xii, 312 pp., 13 figs., 69 pls. Dickinson, J. J. 1982. The systematics and distri- butional ecology of the family Ampeliscidae (Amphipod: Gammaridea) in the Northeastern Pacific region I. The genus Ampelisca. —Publi- cations in Biological Oceanography, National Museum of Canada 10:1-39. Goeke, G. D., & J. M. Gathof. 1983. Amphipods of the family Ampeliscidae (Gammaridea). II. Notes on the occurrence of Ampelisca holmesi in the northern Gulf of Mexico. — Gulf Research Reports 7:289-291. 384 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Holmes, S. J. 1908. The amphipoda collected by the United States Bureau of Fisheries Steamer, “‘Al- batross,”’ off the west coast of North America, in 1903 and 1904, with descriptions of a new family and several new genera and species. — Proceedings of the United States National Mu- seum 35:489-543. Mills, E. L. 1963. A new species of Ampelisca (Crus- tacea: Amphipoda) from Eastern North Amer- ica, with notes on other species of the genus. — Canadian Journal of Zoology 41:971-989. ——. 1964. Ampelisca abdita, a new amphipod crustacean from Eastern North America.—Ca- nadian Journal of Zoology 42:559-575. 1967. The biology of an ampeliscid amphi- pod crustacean sibling species pair.— Journal of the Fisheries Research Board of Canada 24:305-— 355: Pearse, A. S. 1908. Descriptions of four new species of amphipodous Crustacea from the Gulf of Mexico. — Proceedings of the U.S. National Mu- seum 34 (1594):27-32. (JLB) NHB-163, Department of Inver- tebrate Zoology, Smithsonian Institution, Washington, D.C. 20560; (JDT) Newfound Harbor Marine Institute, Rt. 3, Box 170, Big Pine Key, Florida 33043. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 385-393 AEGLA DENTICULATA LACUSTRIS, NEW SUBSPECIES, FROM LAKE RUPANCO, CHILE (CRUSTACEA: DECAPODA: ANOMURA: AEGLIDAE) Carlos G. Jara Abstract.—A subspecies of Aegla denticulata Nicolet, 1849, is described as A. d. lacustris. The new subspecies is restricted to the preandean Lake Rupanco, in the River Bueno basin, Osorno Province, Chile, while the nominate sub- species is widespread in small, moderately fast running streams in the Central Valley of Valdivia, Osorno, and Llanquihue provinces. A. d. /acustris differs from A. d. denticulata in having markedly more prominent spinulation along the branchial margins of the carapace and upon the chelipeds. Aegla denticulata Nicolet, 1849, is one of the best known Chilean aeglids. Its mor- photype is easily distinguished from that of all other species of Aegla Leach (Schmitt 1942). Extensive collections made by the author in central southern Chile have shown that A. denticulata ranges between Cautin and Chiloé (Jara 1980 and unpublished data), living in small to medium-sized rivers along the Chilean Central Valley. A large population of A. denticulata was found occupying the sublittoral of Lake Ru- panco (Osorno Province). When I com- pared the specimens collected in the lake with those collected in rivers, it became ap- parent that the lake specimens differed markedly in the expression of the carapace ornamentation. The spininess of the lacus- trine specimens is remarkably more prom- inent than that of the riverine animals. Since this highly ornamented morpho- type was found to be restricted to Lake Ru- panco, this variant population was consid- ered to represent a geographic isolate of A. denticulata, thus deserving a description as a new subspecies (as defined by Mayr 1969). Aegla denticulata lacustris, new subspecies igs la;cje; ge, 1; komo Holotype.—Instituto de Zoologia, Uni- versidad Austral de Chile (IZUA), IZUA C-686, adult male, Huillin Cove on north- western shore of Lake Rupanco (40°49’S; 72°28'W), Chile, 25 m depth, baited crab trap, 30 Apr 1984, coll. C. G. Jara. Allotype.—Adult female, 8 Sep 1984, IZUA C-686, same locality, collecting de- vice and depth as for holotype. Paratypes. -IZUA C-687; eight adult males (P1 to P8), 30 Apr 1984; eight adult females (P10 to P16), 8 Sep 1984; one ovig- erous female (P9), 3 Apr 1984; same local- ity, collecting device and depth as for ho- lotype. Four juveniles (P17 to P20), 7 Sep 1984, 18 m depth, Scuba hand collection. Diagnosis. —External margin of antero- lateral lobe of carapace with row of tiny spinules; summit of middorsal carina with irregular narrow band of minute scales; dis- todorsal margin of merus of chelipeds with transverse row of small but well defined spines; posterior branchial margin of cara- pace definitely denticulate; summit of dor- solateral carina on second abdominal epi- meron with irregular row of. scales; laterodorsal area of tergum of second ab- dominal segment markedly protuberant, its apex scaly; dorsum of merus and carpus of second to fourth pereiopods clearly dentic- ulate; denticles on anterior branchial mar- gin conical; palmar crest of chelipeds deeply incised. Description. —Carapace ovoid, markedly 386 elevated along middorsal line forming well defined keel extending from rostrum to pos- terior margin of carapace. Dorsal surface of carapace and abdomen finely punctate; when dry, polished and glossy brilliant. Short stiff setae protrude from punctae, some together with minute lenslike scales. Rostrum prominent, straight, broad- based, extended in horizontal plane but sometimes slightly recurved at tip. Form varying, from strictly triangular to ligulate. Rostral margins well defined and slightly upturned, fringed with row of closely packed minute conical scales pointing towards ros- tral apex. Distal third flattened, merging with rostral carina into acute conical apex. Ros- tral carina narrow, sharp, with row of mi- nute scales not reaching rostral apex. Prox- imal end of rostral carina marked by two small pits just in front of protogastric lobes. Epigastric prominences blunt, slightly pro- tuberant. Protogastric lobes pronounced, their uppermost part with small field of lenslike scales. Orbits wide, deep, limited at external angle by acute conical orbital spine; short row of acute scales just posterior to orbital spine on orbital margin. Anterolat- eral angle of carapace produced as strong acute conical spine extending from broad flattened anterolateral lobe. Tip of spine reaching at least middle of cornea. Extraor- bital sinus a deep V-shaped notch. External margin of anterolateral lobe with row of small acute spines variable in number and size. Free angle of first hepatic lobe pro- duced as strong, acute, dorsally recurved spine bearing from two to five scales at base. Second and third hepatic lobes also well marked and bearing spiniform scale at fron- tal angle and row of minute scales along free margin. Gastric area quite elevated at mid- line, then sloping down both sides of cara- pace, reaching broad concavity at dorsum of hepatic lobes. Uppermost part of mid- dorsal carina rugose and scaly throughout. Cervical groove distinctly marked but not deeply incised. Anterior branchial area raised towards PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON midline but leveling into horizontal plane towards free margin. Frontal angle pro- duced as one or two coalescent, strong, sharply acute conical spines. Anterior bran- chial margin laterally expanded in row of from seven to nine single or multiple tipped prominent sharply acute denticles that scarcely decrease in size from anterior to posterior. Row of 9-11 tiny conical scales mounted atop small tubercles along external branchial suture. Posterior branchial area with complicat- ed topography; inner part raised and leveled with cardiac area, then sloping towards lat- eral margin, which rises again above mar- ginal zone leaving behind wide longitudinal trough. Margin markedly expanded in row of 9-11 clear-cut conical, single or multiple tipped, markedly recurved spinelike denti- cles. Anteriormost and posteriormost den- ticles smallest. At limit between anterior and posterior branchial margin, first posterior denticle overlaps last anterior denticle. Pos- terior margin of carapace thick, more pro- tuberant at middle section, which occasion- ally forms broad based tubercle. Abdominal terga deeply sculptured. Me- dian section markedly protuberant espe- cially at frontal edge, which forms moder- ately sharp transverse carina. On pleural area, near laterodorsal pit on second ab- dominal segment, dorsal surface raised frontally forming rotund broad-based prominence bearing at summit from two to five tiny scales. Anterolateral angle of sec- ond abdominal epimeron produced as strong spine tipped with sharp conical scale. It stands at frontal end of narrow oblique ca- rina extending over anterior two thirds of epimeral dorsum. Crest of carina with row of closely juxtaposed minute scales decreas- ing in size posteriorly. Lateroventral angle of epimeron acute; if rounded off, bearing two or three acute scales. Lateral angle of third and fourth epimera sharply acute. Tel- son plate dimerous, subpentagonal. Third thoracic sternum broad, its ventral surface protuberant, rugose, bearing tiny VOLUME 102, NUMBER 2 scales at frontal tip and sometimes one or two scales along median line. Fourth ster- num with long robust spinelike tubercle markedly compressed into sagittal plane, tipped with one major and two to three mi- nor scales. Fifth sternum slightly swollen but not forming tubercle. Frontal margin of sixth sternum bearing one or more tiny scales in transverse row. Chelae subtriangular to ovoid, dorsoven- trally depressed. Dorsal surface quite punc- tate and covered by numerous small scales atop minute tubercles. Scales on proximal external surface lenticular and flat, then be- coming more acute and prominent towards finger tips. Two low, relatively narrow ridges on dorsal surface of chelae, one starting from upper articulating condylus at carpus-prop- odus joint and ending at condylus of prop- odus-dactylus joint. Uppermost part of this ridge with irregular row of scales larger on proximal end. Second ridge along median line of chela extending from carpus-propo- dus joint to proximal end of cutting edge of fixed finger; it is marked by straight row of acute scales. Finger cutting edges closely fit- ted along distal two thirds but with small gap at proximal third. Dorsal edge of dac- tylus with sharply prominent conical tuber- cle at proximal end, followed distally by row of smaller acute tubercles or enlarged scales. Palmar crest semicircular in outline, deeply incised, formed by from two to three stout single or multiple tipped acute spines arising from thick bases. Smaller spines or spinules attached to basis of body of main spines. Frontal margin of propodus above propo- dus-dactylus joint with acuminate tubercle; spinules are found on both sides of it. Ven- tral surface of chela with low but well de- fined carina between lower condylus of car- pus-propodus joint and tip of fixed finger. Carpus strongly armed. Carpal crest with two or three sharp, long, robust spines; one or two small tubercles behind proximal spine. Carpal lobe spiniform, as long as sec- ond spine of carpal crest. Row of from five to seven spiniform tubercles external to and 387 parallel to carpal crest. Second row of small- er but acute tubercles external to above row. Distodorsal margin of carpus fringed by acute scales. Ventral surface with acute con- ical spine as long as second spine in carpal crest. Distoventral angle below carpus-pro- podus condylus with small spiniform tu- bercle. Dorsal margin of merus with from five to eight single or multiple tipped distinct spines decreasing in size proximally. Spinules oc- casionally present among bases of spines. External face roughened by scales, mostly on upper half. Distodorsal vertex with large, somewhat flattened procurved spine longer than the longest in row behind. Margin ex- ternal to it with row of sharp conical spi- nules. Inner ventral margin with from two to five spiniform tubercles in row behind single or double tipped spine at distal end. External ventral margin scabrous or tuber- culate. Distal end with spine as large as that on inner ventral margin. One to three small acute tubercles variable in size in front of latter. Articular lobe at distalmost end of same margin spiniform. Inner ventral mar- gin of ischium with low broad nodule on proximal end. Distal end with conical spine. Between both ends from one to four acu- minate tubercles variable in size. Distodor- sal angle with short but acute spine slightly displaced over outer surface. Distoventral margin of ischium of pe- reiopods fringed with minute scales; one of these scales occasionally larger just behind ischiomeral joint. Dorsal margin of merus with row of small but clear-cut acute den- ticles decreasing in size proximally; disto- dorsal angle noticeably spiniform:; ventral margin scabrous bearing minute scales in- termingled with short stiff setae. Dorsal margin of carpus also with small denticles; distodorsal angle spiniform. Dorsal and ventral margin of propodus with dense nar- row band of scales and setae. Dorsal surface of all pereiopodal articles except dactyl mi- cronodulose and squamous. Color (in life).—Dorsum of cephalotho- 388 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 1. male 25.7 mm CL from River Puquitre (IZUA C-686), b, d, f, h, j, 1, n, p. a, b, Dorsal view of carapace; c, d, Lateral view of carapace; e, f, Left margin of carapace (ventral); g, h, Second right pereiopod; i, j, Inner view of ischium and merus of left cheliped, carpus seen from above; k, 1, Ventral view of right cheliped; m, n, Chela and carpus (dorsal); 0, p, Lateral view of left second abdominal epimeron. rax and abdomen highly variable among in- dividuals, ranging from orange-yellow to al- most black. Though variation between both extremes is continuous, an attempt was made to quantify the frequency with which different patterns appear in the population. The following patterns were defined and their frequency recorded (Table 1): Pattern A: Dorsum of cephalothorax and abdomen uniformly orange-yellow to ter- racotta, occasionally scattered with small, irregular, dark brownish spots. Pattern B: Dorsum of cephalothorax and abdomen variegate; extensive reticulate dark green or dark brown design on a khaki or light brown background. Pattern C: Dorsum of cephalothorax and abdomen uniformly dark greenish brown or dark reddish brown. Aegla denticulata lacustris (holotype), a, c, e, g, i, k, m, 0; A. denticulata denticulata Nicolet, 1849, Pattern D: Dorsum of cephalothorax and abdomen variegate; small to extensive dark green patches on a lighter blue-green or brown-green background. Pattern E: Dorsum of cephalothorax and abdomen variegate; small but numerous yellowish or light greenish brown spots on a uniform dark brown background; in some specimens dorsal carina bluish tinged. Pattern F: Dorsum of cephalothorax and abdomen variegate; ample irregular blue- black or brown-green-black patches on a lighter blue-gray or gray-violet background. In all specimens, the dorsal surface of the pereiopods has the same color pattern as the dorsum of the carapace but with darker stripes across the carpus and merus. The distal half of the chelae is always white or yellowish-white, contrasting markedly with VOLUME 102, NUMBER 2 the darker proximal half. The ventral sur- face of the body and appendages is milky white or slightly yellowish. The articular membrane of the appendages is bright pur- ple-red. In formalin fixed specimens, the dorsum of the carapace is wine-red in color, whereas in alcohol preserved specimens the color changes to light brown or tan. Variation and measurements. —Making allowances for minor variation in the size and number of spines along the upper mar- gin of the merus and dorsum of the carpus of the chelipeds, adults in the type-series are quite similar. Juveniles (P17—20) have many features of the adult morphotype only slightly developed (spines, tubercles, etc.) but are still recognizable. The major differ- ence between adults and juveniles is that in the latter the tegumental scales are replaced by short fine setae, most notably on the dor- sum of the chelae and on the abdominal terga. Somatometric data of specimens in the type-series are give in Table 2. Measure- ments were made with calipers to the near- est 0.1 mm; symbols for the morphometric characters in the first column are given by Jara & Lopez (1981). Distribution. —Known only from the type locality. Attempts to collect A. denticulata lacustris in Lake Puyehue, 12 km to the north of Lake Rupanco, failed. In July 1984, dur- ing the winter high-water period of Lake Rupanco, two small specimens (LC about 10 mm) were collected in a protected site at the bank of River Rahue, 150 m from the outlet of the lake. These specimens were most probably washed out from the lake by the effluent current. Habitat and natural history.—Lake Ru- panco is the southernmost of three major preandean piedmont lakes included in the River Bueno basin, and is the fifth in size among Chilean lakes. It has a maximum depth of 274 m and an area of 233.4 km”. Limnologically, it is an oligotrophic, cold temperate monomictic lake that circulates at 9.6°C in midwinter and reaches 19°C at 389 Table 1.—Frequency of color patterns in 4. dentic- ulata lacustris, from Lake Rupanco. Color patterns de- fined in text. Sample size: 116 adult specimens col- lected at 25 m depth on 30 Apr 1984, with baited traps. Sex unrecorded. Frequency Pattern Absolute Relative (%) A 5 4.31 B 11 9.48 ee 3 2.59 D 39 33.62 E 29 25.00 EF 29 25.00 epilimnion in summer. Dissolved oxygen is high throughout the year (9.1 to 12.2 mg/ liter); conductivity is low (40.6 to 54.0 uS) and calcium is scarce (2.1 to 4.8 mg/liter) (Campos et al. 1985). Lake Rupanco lies at 118 m above sea level. Its eastern half is surrounded by massive mountains and vol- canoes (Puntiagudo and Casablanca) of the Andes Cordillera. Its affluents are small to medium-size rivers of pluvial or pluvio-gla- cial regime. Its effluent (River Rahue) dis- charges about 100 m?/sec on the average (Campos et al. 1985). Lake Rupanco is of glacial origin. The inferred chronology of the regional glacial events suggests that Lake Rupanco attained its present form about 11,000 years B.P. (Mercer 1972). Underwater observations, made by the author between 0 and 30 m depth at Huillin Cove, showed that A. d. lacustris occupies the sublittoral zone from 8 m depth down- ward. Its vertical distribution appears closely related to that of the soft substrate on which crabs alternatively walk and collect particles with their maxillipeds. Activity is markedly higher at night, while during the day a great proportion of the crabs rest buried in the substrate. No data are available on the diet of A. d. lacustris, but it can be presumed that they feed on fine-grained detrital mat- ter, though they were seen consuming a dead fish lying on the bottom of the lake. Berried females appear at the end of the summer period (March), and the release of newborn crabs from the brooding abdominal cham- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 390 ON Gaen) Cum (Cuma Guna San ae Samat icue mC Ole a OME gO. SSO SOre yi Soe 8c” sO BS OOS Com OL. 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Crs Cee ae Oe NGO Oe OLE =O Ee VLR 9 My Os OL 28 OL Te ‘Ta Clem AU onic SC 69C “6SC =I9C OGG TRIG "260 C8G SLO 6G 88G Cbc 266 960 Cle Tae 88¢ Se “TO A A A W | | A af A | fa * W W W W W W W W A W -X9§ (Ci ci ai ic Old sid eric eels ecldie Nido) sold 6d 8d Ld 9d Sd td €d 7d Id OY. OTOH :uouttoadg "yIsus] UOSTO} “TI ‘podorosod 19] YANOJ Jo yIsus] AejAjOVp “Tq py] :podotsiod jo] puooes Jo yysug] IeyAjoep “Tqz7] ‘podotsiod jo] puooses jo yZug] “Tq7T ‘yIsusy podipoyo yy si “JOY ‘yuo podipoyo yoy “JOT ‘yIprm soedeseo winuiixew “Ad ‘soqo] onedoy PIII SSOIOR DOURISIP ‘YIPIM [VOTAIOOOId WINUWITxeW ‘AAD ‘o0edeIKO JO so[sue [e191e[010]Uv JO SdI] UI9M19q DOURISIP “YIPIM [VIUOT “AAJ ‘9AOOIS [BOTAIOO JO JUTOdpru pue dij [eso1 us9Mj0qQ JOURISIP ‘YIBUD] [BVOTAIO.OId “JO _ ‘suIsIeW [e1IGIO JO JUIOd jsodoep 0} jUSSUR} OUT] [eSIOASUBI] JO JUTOdpIW pue dq} [e1]SsO1 UD9MJ9q 9OUL}SIP ‘yisug] jeso1 “Py ‘xe1oyo[eydoo jo ulsieW JO110}sod pue xode [e1jsO1 Ud9MI9q DOURISIP ‘YIBUD] DORdeILO “TD ‘sodAjered = QZ_ 01 [d :odAlO][e = OT[y ‘adA1ojoy = OJOP ‘a[Bulsy snNOJOSIAO = ,.f ‘o[eWay = 4 ‘oyeW = JY “WU UT SJUDWIOINSvOW [[Y ‘Sol1os-odA} ‘sorsodsqns MoU ‘S1JSNID] DIDINIIJUap “pv JO AaUI0JeWIOS —*Z 9[qQe L VOLUME 102, NUMBER 2 ber of the females occurs at the beginning of the subsequent spring (October). At Lake Rupanco, A. d. lacustris coexists with Aegla abtao Schmitt and the crayfish Samastacus spinifrons (Philippi). A. abtao occupies the littoral zone and the upper sub- littoral to 15 or 20 m depth. However, be- low 4 m only large adult males are found. The bulk of A. abtao’s population lives among and under big stones and boulders in the littoral. S. spinifrons is found in the sublittoral at least down to 80 m depth, only on soft substrate. Biological interactions among these three species of decapod crus- taceans are suspected but the only one ob- served so far is predation by large A. abtao males upon juveniles of A. d. /acustris. Oth- er faunal components of the benthic com- munity at Lake Rupanco are freshwater mussels of the genus Diplodon and Pisidi- um, aquatic snails of the genus Chilina, the minute janirid isopod Heterias exul (Bow- man et al. 1987), amphipods, acari, oligo- chaetes, chironomid larvae and caenid ephemeropteran nymphs. Etymology. —The trivial name /acustris, from Latin, alludes to the fact that this sub- species of A. denticulata is apparently re- stricted to a lentic environment. Comparison. —To compare lacustrine and riverine specimens of A. denticulata, four crabs (two males and two females) from the series from which the neotype of A. dentic- ulata was drawn, National Museum of Nat- ural History (USNM 169096 = USNM 80021) (Schmitt 1942) were examined. Ad- ditionally, 30 males (LC 18 to 26 mm) col- lected in rivers Puquitre and Remehue, 8 km north of Osorno city, and 50 males (LC 23 to 33 mm) from Rupanco were examined and measured. One male from the Puquitre (IZUA C-686) was employed for preparing Fig. 1b, d, f, h, j, 1 and p. A. denticulata lacustris is very similar to the nominate subspecies A. denticulata den- ticulata Nicolet, 1849, from which it de- parts by the morphological features already mentioned in the Diagnosis. Additionally, Rupanco —s n=50 Puquitre ch n=30 Valdivia es n=29 1.30 1.40 1.50 1.60 CW/ PCW Rupanco ch Puquitre ch Valdivia ch 1.30 1.40 1.50 1.60 CL/ PCL Fig. 2. Somatometric comparison of males of A. denticulata lacustris (Rupanco) and males of A. den- ticulata denticulata (Puquitre and Valdivia). Sample labeled Valdivia is a composite made of individuals collected all over the Valdivia River Basin (Jara 1980). Vertical line: mean value of somatometric proportion; open rectangle: confidence interval for the mean (P = 0.05). Above: proportion between maximum carapace width (CW) and maximum precervical width (PCW). Below: proportion between carapace length (CL) and precervical length (PCL). A. d. lacustris differs from A. d. denticulata in the following respects: ridge of dorsal ca- rina sharper; dorsal profile of carapace less inflated (cf. Fig. lc, d); external margin of anterolateral lobe of carapace minutely den- ticulate; denticles along ridge of merus of chelipeds longer and sharper; tubercles of middorsal row of carpus definitely spini- form; spine of carpal lobe longer and more slender (cf. Fig. 11, j); carpal ventral surface less hairy; denticles of palmar crest longer and slender; ventral angle of second abdom- inal epimeron often produced into short acute spine (cf. Fig. lo, p). Because of the slender and clear-cut ap- pearance of the main spines of its carapace, together with the cleanness of the carapace surface, A. d. lacustris is reminiscent of another lacustrine species, A. rostrata Jara, but differs from it in that A. rostrata lacks the dorsal carina and the median tubercle on the fourth thoracic sternum. On the other hand, A. d. l/acustris lacks the distinctive stylet-like rostrum of A. rostrata. In Fig. 2 the average and confidence in- 392 tervals (P = 0.05) of two somatometric pro- portions for riverine (Puquitre and Valdi- via) and lacustrine (Rupanco) samples are compared. Remarks. — Though at first sight the Lake Rupanco morphotype is clearly differentia- ble from the riverine morphotype found elsewhere in southern Chile, key characters that differentiate the two forms appear elu- sive. With the exception of the row of tiny spinules along the external margin of the anterolateral lobe of the carapace, the band of tiny scales on the ridge of the dorsal ca- rina, and some other minor details, every morphological attribute in_A. d. lacustris has its counterpart in A. d. denticulata. The dif- ference is a matter of degree of expression rather than of difference of attributes. The Rupanco’s morphotype appears to be an elaborate manifestation of the attributes found in riverine specimens. The decision to assign the Lake Rupanco population a subspecific status 1s supported by the fact that Lake Rupanco’s population is, on geo- graphical and ecological grounds, an outlier as compared to the remaining populations of the species. In fact, Lake Rupanco is the easternmost locality where A. denticulata has been reported in the River Bueno basin, and the only one in which the species inhabits a lentic environment. The possibility that Lake Rupanco’s population has already at- tained reproductive isolation with respect to the riverine populations, and therefore qualifies as a different species, remains an open question. As mentioned elsewhere (Jara 1986), the trend towards profuse spinulation in Aegla seems to be correlated with living in lentic environments. The prominent ornamenta- tion seen in A. d. lacustris lends support to this hypothesis. However, no explanation is available for this overgrown spinulation, neither from the ecological nor from the genetical point of view. Profuse spinulation in A. d. lacustris may well be an adaptive response to 1ts immediate biotic or abiotic environment. Otherwise, spinulation could PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON be a by-product of genetic changes related to presently unknown factors. Comparison of A. d. lacustris and A. d. denticulata life histories could be illuminating in these re- spects. If the geographical and chronological re- lationship between rivers and lakes in southern Chile is considered (see comments in Jara 1977, 1982, 1986), it appears evi- dent that lacustrine populations of aeglids descended from riverine stocks. These last would have withstood the Quaternary gla- cial events in non-glaciated areas, located along the western border of the Chilean Central Valley and in the Coastal Cordillera (Illies 1960). That scenario implies that ae- glids could have colonized the lakes rather recently (in geological time). Mercer (1972) estimates that lakes Llanquihue and Ru- panco became free of ice about 11,000 years B.P. Therefore, to colonize the Andean lakes, aeglids had to advance from west to east, along the rivers that drained the newly formed lakes. Most probably, the forerun- ners of A. d. lacustris were specimens of A. d. denticulata, which could have entered the young Lake Rupanco from rivers of the Central Valley of Osorno Province. If spi- nulation of A. d. lacustris is a derived con- dition related to modifications of the former riverine invader’s genome, one could expect to find evidence of these changes by com- paring population samples of both subspe- cies by suitable techniques (protein electro- phoresis, caryological analysis, etc.) (Wiley 1981). Acknowledgments The author thanks René Navarro and Gonzalo Aguilar for their assistance during the field work at Lake Rupanco; Dr. Ray- mond E. Manning of the National Museum of Natural History for the loan of four spec- imens of A. denticulata; Mrs. Patricia Araya and an anonymous reviewer for correcting the MS; Dr. Thomas E. Bowman for making available to the author his paper on Heterias VOLUME 102, NUMBER 2 exul; and Direccion de Investigacion y De- sarrollo, Universidad Austral de Chile, for funding field work through grant RS-83-39. Literature Cited Bowman, T. E., R. Prins, & J. Arenas. 1987. The occurrence of the freshwater isopod Heterias (Fritzianira) exul in the Lakes Region of Chile, with notes on the genus Heterias (Asellota: Jani- ridae).— Hydrobiologia 146:275-281. Campos, H., J. Arenas, W. Steffen, G. Agiiero, L. Vil- lalobos, & G. Gonzalez. 1985. Investigacion de la capacidad de cultivo de salmonidos de las principales hoyas hidrograficas del pais. III An- tecedentes limnologicos hoya Lago Rupanco. — Corporacion de Fomento de la Produccion (CORFO), Santiago, Chile, 404 pp. Illies, H. 1960. Geologie der Gegend von Valdivia (Chile). —Neues Jahrbuch fiir Geologie und Pa- laeontologie 111:30-110. (Translated into Spanish by J. Walper, in Publicacion Ocasional de la Universidad Austral de Chile, Valdivia, 1970.) Jara, C. 1977. Aegla rostrata n. sp., (Decapoda, Ae- glidae), nuevo crustaceo dulceafuicola del Sur de Chile.—Studies on Neotropical Fauna and Environment 12:165-176. 1980. Taxonomia y distribucion del género Aegla Leach (Crustacea, Decapoda, Anomura) ete le en el sistema hidrografico del rio Valdivia (Chile).— Universidad Austral de Chile, Facul- tad de Ciencias, Thesis, 126 pp. 1982. Aegla bahamondei, new species (Crus- tacea: Decapoda: Anomura) from the coastal mountain range of Nahuelbuta, Chile. — Journal of Crustacean Biology 2(2):232-238. 1986. Aegla spectabilis, a new species of freshwater crab from the eastern slope of the Nahuelbuta Cordillera, Chile.— Proceedings of the Biological Society of Washington 99(1):34—- 41. ,& M. T. Lopez. 1981. Anew species of fresh- water crab (Crustacea: Anomura: Aeglidae) from insular South Chile.— Proceedings of the Bio- logical Society of Washington 94(1):88-93. Mayr, E. 1969. Principles of systematic zoology. McGraw-Hill Book Co., New York, 428 pp. Mercer, J. H. 1972. Chilean glacial chronology 20,000 to 11,000 carbon-14 years ago: some global comparisons.—Science 176:1118-—1120. Schmitt, W. L. 1942. The species of Aegla, endemic South American freshwater crustaceans.— Pro- ceedings of the United States National Museum 91:431-520, pls. 25-28. Wiley, E. O. 1981. Phylogenetics. The theory and practice of phylogenetic systematics. John Wiley & Sons, New York, 439 pp. Instituto de Zoologia, Universidad Aus- tral de Chile, Casilla 567, Valdivia, Chile. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 394-400 FRESHWATER CRABS ASSOCIATED WITH CAVES IN SOUTHERN MEXICO AND BELIZE, WITH DESCRIPTIONS OF THREE NEW SPECIES (CRUSTACEA: DECAPODA) Gilberto Rodriguez and Horton H. Hobbs, Jr. Abstract. — Records of nine freshwater crabs frequenting subterranean hab- itats in Belize and Mexico are reported. Three of them are described as new: Potamocarcinus leptomelus, a troglophile from Veracruz; Odontothelphusa monodontis, also a troglophilic species, from Tabasco; and Typhlopseudo- thelphusa hyba, a troglobite, from Chiapas. The remaining crabs are troglo- philes, one of which occurs in Belize, and the others, two of which because of inadequate material cannot be fully identified, were found in caves in the states of Chiapas, Guerrero, Oaxaca, and Tabasco, Mexico. A study of several collections of cave- dwelling crabs, kindly donated to the Smithsonian Institution by James R. Red- dell, has prompted us to record additions to his list of Brachyura known to occur in subterranean habitats in Mexico, Guate- mala, and Belize (Reddell 1981). His list includes three troglobites and six others that are probable troglophiles. Subsequently, one troglobitic form, Typhlopseudothelphusa acanthochela Hobbs (1986), was described from Blind Crab Cave, 12 km SW Millio- nario, Cayo District, Belize, and a troglo- philic one, Pseudothelphusa mexicana A\- varez-Noguera (1987), from La Jolla [sic, Joya?] Cave in the State of Guerrero, Mex- ico. Records of the occurrence of eight ad- ditional species, two of which cannot be ful- ly identified because of inadequate material, are reported herein from spelean waters of Belize and Mexico. All of the ““Material’’ cited herein is de- posited in the National Museum of Natural History, Smithsonian Institution (USNM). Other abbreviations employed are: cl = car- apace length, and cb = carapace width. Pseudothelphusidae Ortmann, 1893 Potamocarcinus leptomelus, new species Fig. la—h Material. — Mexico: Cueva del Tuknel, Mahoilca, Porvenir Zongolica, Veracruz, 31 Dec 1986, Steve and Lori Robertson, male holotype, cl. 13.3 mm, cb. 21.1 mm (USNM 230080). Description. —Cervical groove narrow, almost straight, very shallow, reaching mar- gin of carapace. Postfrontal lobes obsolete, their position marked by slight depressions; median groove absent except for notch on upper margin of front. Surface of carapace between postfrontal lobes and front sloping gently ventromesially. Front low, of equal height throughout, bilobed in dorsal view, upper margin defined by series of irregularly placed papillae; lower margin V-shaped in median part, straight in lateral parts. Dorsal margin of orbits sinuous. Lateral orbital an- gle forming papillated tooth, followed by deep notch; rest of anterolateral margin cov- ered by small, irregularly placed, conical pa- pillae. Surface of carapace covered by very VOLUME 102, NUMBER 2 Fig. la-o. 4 (Gee jlet kag nse 395 } \ a-h, Potamocarcinus leptomelus, male holotype: a, Left gonopod, caudal view; b, Same, cephalic view; c, Same, lateral view; d, Right cheliped; e, Distal part of chela; f Opening of efferent channel; g, Left third maxilliped; h, Dorsal view of carapace. i-o, Pseudothelphusa mexicana, male, from Resumidor de la Joya: /, Left gonopod, mesial view; j, Same, cephalic view; k, Same, subapical view; /, Same, lateral view; m, Same, caudal view; n, Opening of efferent channel; 0, Left third maxilliped. small papillae, invisible to naked eye, par- ticularly in branchial region. Eyes small, with distinct faceted cornea and pigment, of usual shape, not filling or- bit. Third maxilliped with conspicuous notch on external margin of merus, near insertion of palp; external margin of is- chium convex; exognath 0.59 times length of ischium. As name suggests, all pereio- pods conspicuously slender. Chelae only slightly dissimilar in size and shape; palm of larger one very elongate with straight up- per and lower margins; fingers not gaping; carpus with strong internal spine preceded by four spinules; merus elongate with row of spinules on internodorsal and interno- ventral ridges and smaller spinules on outer ridge. Walking legs very long, length of third 396 pair 1.6 times breadth of carapace, and me- rus 6.3 times as long as broad; relations be- tween podomeres as follows: merus 1, car- pus 0.33, propodus 0.54, dactylus 0.54. Dactylus with seven spines in upper row and four in two lower ones. Gonopod subcylindrical, straight; apical part bearing triangular marginal process overreaching apex, spiniform mesial pro- cess directed distomesially, and bifid ce- phalic process with apices pointing mesial- ly. Field of spines very narrow, with few setae placed on distal surface of apex. Remarks.—The gonopod of this species resembles that of Potamocarcinus magnus (Rathbun 1896:377); the mesial process is similar but directed distomesially instead of mesially; the bifid process is present in both, although distinctly reduced in P. leptome- lus; and the marginal process of the latter is rudimentary rather than well developed and cup-shaped as in P. magnus. Potamocarcinus aspoekorum (Pretzmann) Pseudothelphusa (Zilchia) aspoekorum Pretzmann, 1968a:12. Potamocarcinus (Zilchia) mexicanus Pretz- mann, 1968a:12 [nomen nudum]. Potamocarcinus (Zilchia) aspoekorum. — Pretzmann, 1971:20; 1972:75, figs. 405- 407, 417-420. Potamocarcinus aspoekorum. — Rodriguez, 1982:115, figs. 69d; 70f, m; 71le, 1; 74a—c. Material. —Belize: Balam’s Cave (Uchen Balam), Cayo District, 22—26 Mar 1979, L. McNatt, 1 male cl. 18.6 mm, cb. 30.1 mm (USNM 230082). Remarks. — Troglobitic characters are not conspicuously developed in this species. The walking legs are moderately slender (third right pereiopod of largest male with total length 34.0 mm, merus 3.3 times as long as broad), but the dorsal surface of the cara- pace is not pale, and the eyes are normally developed. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Pseudothelphusa mexicana Alvarez-Noguera, 1987 Fig. li-o Pseudothelphusa mexicana Alvarez-No- guera,1987:1. Material.—Mexico: Resumidero de la Joya, San Gregorio, Guerrero, 23 Feb 1981, Steve Robertson, 2 males, cl. 18.6 and 16.5 mm, cb. 28.7 and 25.8 mm; 1 female, cl. 18.0 mm, cb. 28.2 mm (USNM 230084). Remarks.—Our specimens are from the type locality. Troglobitic characters are not obvious in this crab, although the walking legs are moderately slender (third right pe- reiopod of largest male with total length 29.5 mm, merus width/length = 0.35). The dor- sal surface of the carapace, however, is dark and the eyes are well developed. Odontothelphusa monodontis, new species Fig. 2a—f Material. —Mexico: Grutas del Cocona, Tabasco, 26 Aug 1972, R. W. Mitchell and W. H. Russell, 1 male holotype, cl. 17.0 mm, cb. 25.2 mm (USNM 230078). Description. —Cervical groove very shal- low and wide, not reaching margin of car- apace. Postfrontal lobes wide, flat, clearly delimited anteriorly, surface covered by flat papillae not visible to naked eye; median groove well marked between lobes, but not anterior to them. Surface of carapace be- tween frontal lobes and front flat. Upper border of front well marked by overhanging papillae and conspicuous notch in middle; lower margin slightly sinuous and lying slightly anterior to upper one; front high and excavate. Anterior margin of carapace with notch behind orbit, about 5 small papillae situated between notch and cervical groove, and approximately 15 papilliform teeth on rest of lateral margin. Third maxilliped con- spicuously wide; merus 1.43 times as wide as long; exognath 0.93 length of ischium of endognath. VOLUME 102, NUMBER 2 30 Fig. 2a-k. a-f, Odontothelphusa monodontis, male holotype: a, Right gonopod, caudal view; b, Same, mesial view; c, Same, cephalic view; d, Same, subapical view; e, Left third maxilliped; {, Opening of efferent channel. g—k, Typhlopseudothelphusa hyba, male holotype: g, Opening of efferent channel; 4, Left third maxilliped; 7, Left gonopod, caudal view; j, Same, lateral view; k, Same, cephalic view. Gonopod slender with apical part bent laterally at angle of 45 degrees; apex con- sisting of flat quadrangular lobe with long spur on proximomesial angle and papilli- form tubercle and small finger-like tubercle on cephalic surface; field of spines narrow, slitlike. Remarks. — This crab differs from its con- gener in possessing two tubercles on the ce- phalic surface of the gonopod and lacking a spiniform process on the distal angle of the mesial border. Some of the characteristics that have been associated with an obligate spelean existence are lacking in this species, but the dorsal surface of the carapace is pale, and the walking legs moderately slender (third right pereiopod with total length of 30.3 mm, merus 2.87 times as long as broad); the eyes, however, are well pigmented. ?Raddus sp. Material. —Mexico: Cueva El Chorrea- dero, Chiapas, 24 Dec 1973, R. Syme, | juvenile male, cl. 9.9 mm, cb. 13.8 mm (USNM 230090). The only specimen available is a distinct- ly juvenile male; however, the gonopod ex- 398 hibits the flat quadrangular form character- istic of Raddus, and the features of the carapace are those of other members of the genus. This cave is located 12 km E Tuxtla Gutiérrez (Reddell 1981:292), near the range of Raddus bocourti (A. Milne-Edwards, 1866). Typhlopseudothelphusa hyba, new species Fig. 2¢-k Potamocarcinus (Typhlopseudothelphusa) mocinoi. — Hobbs et al. 1977:145 [in part : localities 2 and 3]. Material. —Mexico: Cueva de Los Lla- nos, 15 km ESE San Cristobal de Las Casas, Chiapas, 29 Aug 1972, J. Cooke, W. Rus- sell, and R. Mitchell, male holotype, cl. 12.4 mm, cb. 18.1 mm (USNM 150633), 1 fe- male paratype, cl. 15.4 mm, cb. 22.8 mm (USNM 230081).—same locality, 5 Feb 1972, D. McKenzie and J. R. Reddell, 1 female, cl. 1.2 mm, cb. 24.6 mm (USNM 143613).—Cueva de los Murciélagos, 15 km ESE of San Cristobal de Las Casas, Chiapas, 29 Aug 1972, J. Cooke and R. Mitchell, 1 male, cl. 12.6 mm, cb. 19.9 mm, 2 females, cl. 14.7 and 11.6 mm, cb. 20.9 and 16.8 mm (USNM 150629). Description. —Carapace narrow (cb/cl = 1.46), strongly convex in anterior part. Cer- vical grooves forming paired, shallow depressions in holotype but absent in topo- typic female. Postfrontal lobes and median groove obsolete, but carapace with slight depression immediately posterior to front; latter, lacking upper margin, rounded and projecting forward, its lower margin bilobed in dorsal view. Lateral orbital angle forming well developed triangular tooth, followed by shallow notch. Margins of orbits and front with row of small granules. Lateral margin of carapace with larger, irregularly placed granules. Eyes reduced, lacking distinct fac- eted cornea and pigment. Third maxilliped with noticeable impression on external margin of merus, near insertion of palp; ex- ognath 0.61 times length of ischium. All PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON pereiopods extremely slender. Chelipeds subequal in size and shape; palm cylindri- cal; fingers also very slender, approximately twice as long as palm, and armed with mi- nute teeth; carpus with small, hooked spine on internal margin; merus very elongate, overreaching carapace by halfits length, and bearing rows of granules on its three ridges. Third pair of walking legs 1.6 times width of carapace; merus 5.87 times as long as broad, and relations of its podomeres as fol- lows: merus 1, carpus 0.35, propodus 0.66, dactyl 0.74; dactylus with six or seven spines in five rows. Gonopod wide in lateromesial plane, nar- row in cephalocaudal plane; distal part strongly bent; gonopore and field of spines directed cephalad; distal margin rounded and armed with prominent conical spines; marginal process cup-shaped and directed cephalad; and strong, triangular mesial pro- cess disposed in same plane as field of spines. Remarks. — Typhlopseudothelphusa hyba, like its congeners, exhibits a combination of advanced characters associated with its adaptations to a spelean environment. It may be distinguished from them by the tri- angular mesial process of the gonopod with a single apex. Pseudothelphusidae indet. species Material. — Mexico: Sumidero de Citla- lapa, Zongolica, Veracruz, 23 Mar 1981, Steve Robertson and Phillipe Ackamann, 1 fragmented female, cl. approx. 19.5 mm, cb. approx. 33.5 mm (USNM 240112). Description. —Cervical groove very shal- low and wide, not reaching margin of car- apace. Postfrontal lobes rounded, flat, not well delimited anteriorly; median groove well marked between lobes and narrowly linear anterior to them. Surface of carapace between frontal lobes and over front flat; upper border of latter well marked by over- hanging papillae and bearing conspicuous median notch; lower margin slightly sin- uous and lying slightly anterior to upper. VOLUME 102, NUMBER 2 Front high and excavate. Anterior margin of carapace with notch behind orbit, about 5 small papillae between notch and level of cervical groove, and approximately 15 pa- pilliform teeth on rest of lateral margin. Eyes normally developed, but unpigmented. Trichodactylidae Avotrichodactylus constrictus (Pearse, 1911) Trichodactylus constrictus Pearse, 1911:111, fig. 4.—Rodriguez & Manrique, 37:183. Trichodactylus (Trichodactylus) constric- tus. —Coifmann, 1939:111. Trichodactylus (Avotrichodactylus) constric- tus. —Pretzmann, 1968b:71. Trichodactylus (Rodriguezia) constrictus. — Bott, 1969:26.—Cottarelli & Argano, 19772210. Material. —Mexico: | km N of Palenque, Chiapas, 25 Jul 1973, J. Reddell, N. Ka- wakatsu, D. Denson, and S. R. Mitchell, 2 males, cl. 19.8 and 12.5 mm, cb. 17.9 and 12.9 mm (USNM 230085).— Cueva de Juan Sanchez, NW Acatlan, Oaxaca, 1 Jul 1976, T. Byrd, A. G. Grubbs, and M. Cossey, 1 female, cl. 16.5 mm, cb. 15.8 mm (USNM 230086). Remarks.—The female specimen from Cueva de Juan Sanchez is assigned to this species with doubt. It has five lateral teeth (not including the external orbital angle) on the right side and four on the left, whereas A. constrictus usually has two or three teeth. Avotrichodactylus bidens (Bott, 1969) Trichodactylus (Rodriguezia) bidens Bott, 1969:25, pl. 24: figs. 68, 69.—Cottarelli & Argano, 1977:207, figs. 3, 4. Material.— Mexico: Cuevita de la Cas- cada Azufre, 3 km N Tapiulapa, Tabasco, 15 Jun 1975, A. G. Grubbs, 1 juvenile male (USNM 230083). Remarks.—Bott (1969) designated the type locality ““Arroyo del Solpho’’ near 399 Tapiyulapa, which is almost certainly the same as, or perhaps an extension of, that from which our specimen was taken. This juvenile is very small, and the lateral teeth on the carapace are not well formed, but even at this size, the gonopod is clearly typ- ical of A. bidens. Acknowledgments Thanks are extended to James R. Reddell for donating the material cited herein to the Smithsonian Institution, thereby making it available to us. We are also grateful to Brian F. Kensley and Raymond B. Manning for their criticisms of the manuscript. Literature Cited Alvarez-Noguera, Fernando. 1987. Pseudothelphusa mexicana, a new freshwater crab from the state of Guerrero, Mexico (Brachyura: Pseudothel- phusidae).— Proceedings of the Biological So- ciety of Washington 100(1):1-3. Bott, Richard. 1969. Die Siisswasserkraben Siid- Amerikas und ihre Stammesgeschichte. — Ab- handlungen der Senckenbergischen Natur- forschenden Gesellschaft (Frankfurt am Main) 518:1-94. Coifmann, Isabel. 1939. Potamonidi della Guiana Inglesi.—Archivo Zoologico Italiano 27:93-1 16. Cottarelli, Vezio, & Roberto Argano. 1977. Tricho- dactylus (Rodriguezia) mensabaki n. sp. (Crus- tacea, Decapoda, Brachyura) granchio cieco delle acque sotterranee del Chiapas (Messico). — Quaderni Problemi Attuali di Scienza e di Cul- tura, Academia Nazionale dei Lincei 171(3):207- Die Hobbs, Horton H., Jr. 1986. A new troglobitic crab (Crustacea: Decapoda: Pseudothelphusidae) from Belize.—Texas Memorial Museum, Spe- leological Monographs 1:1-4. —., H. H. Hobbs II], & Margaret A. Daniel. 1977. A review of the troglobitic decapod crustaceans of the Americas.—Smithsonian Contributions to Zoology 244:v + 183 pages. Milne-Edwards, A. 1866. Description de trois nou- velles espéces du genre Bosica, Crustacés Brach- yures de la tribu des Telphusiens.— Annales de la Société Entomologique de France (4)6:203- 205. Pearse, A.S. 1911. Report on the Crustacea collected by the University of Michigan-Walker Expedi- tion in the State of Vera Cruz, Mexico. —Thir- 400 teenth Annual Report of the Michigan Academy of Science 13:108-113. Pretzmann, Gerhard. 1968a. Neue sudamerikanische Susswasserkraben (Vorlaufige Mitteilung).— Entomologisches Nachrichtenblatt (Wien) 15:1- 20. . 1968b. Die Familie Trichodactylidae (Milne Edwards 1835) Smth [sic] (Vorlaufige Mitteil- ung). —Entomologishce Nachrichtenblatt (Wien) 15:70-76. 1971. Fortschritte in der Klassifizierung der Pseudothelphusidae. —Sitzungsberichten der Osterreichische Akademie der Wissenschaften, Mathematisch-Naturwissenschaftliche Klasse (1)179(1-4):14-24. 1972. Die Pseudothelphusidae (Crustacea, Brachyura).— Zoologica 42(120), part 1:1-182. Rathbun, Mary J. 1896. Descriptions of two new species of fresh-water crabs from Costa Rica.— Proceedings of the United States National Mu- seum 18:(377-—389). Reddell, James R. 1981. A review of the cavernicole PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON fauna of Mexico, Guatemala, and Belize. — Bul- letin of the Texas Memorial Museum 27:1-327. Rodriguez, Gilberto. 1982. Les crabes d’eau douce d’Amérique. Famille des Pseudothelphusi- dae.—Office de la Recherche Scientifique et Technique Outre-Mer, Faune Tropicale 22:1- 223. , & Fernando Manrique. 1967. El género 7ri- chodactylus en México (Brachyura, Potamoni- dae).—Anales del Instituto de Biologia, Uni- versidad Nacional Autonoma de México 37:183- 186. (GR) Instituto Venezolano de Investiga- ciones Cientificas, Apartado 21827, Cara- cas 1010A, Venezuela; (HHH) Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institu- tion, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 401-404 A NEW DEEP-SEA CRAB OF THE GENUS CHACEON FROM CHILE (CRUSTACEA, DECAPODA, GERYONIDAE) Luis A. Chirino-Galvez and Raymond B. Manning Abstract.—Chaceon chilensis, a large species with five anterolateral teeth on the carapace and narrow, compressed dactyli on the walking legs, is described from localities off Chile, the Juan Fernandez Islands, and Isla San Félix. It is _ the only Recent East Pacific species of the genus. Until recently, carcinologists working with deep-sea crabs of the genus Chaceon from localities around the world often have iden- tified their material with the West Atlantic C. quinquedens (Smith, 1879), or the East Atlantic C. affinis (A. Milne Edwards & Bouvier, 1894); both of these species for- merly had been assigned to the genus Ger- yon (see Manning & Holthuis 1989). A species of Chaceon from off Chile has been identified erroneously in the past with both of these species. We describe the Chilean species as new herein. The holotype and several paratypes are in the Museo Nacional de Historia Natural, Santiago (MNHN). Other paratypes are in the collections of the Museo Instituto de Zoologia, Universidad Austral de Chile, Valdivia (MIZUA), the National Museum of Natural History, Smithsonian Institu- tion, Washington (USNM), the Instituto de Oceanologia, Universidad Catolica de Val- paraiso, Valparaiso (IOUV), the Museo de Zoologia, Universidad de Concepcion (MZUC), and the Museo de Historia Nat- ural, Valparaiso (MHNV). We use cl for carapace length, measured on the midline, and cb for carapace breadth, measured at and including the fifth antero- lateral spines, m for meter(s), and mm for millimeters. Chaceon chilensis, new species Figs. 1-2 Geryon affinis. —Dupré, 1975:34.—Baez & Andrade, 1977:215.—Andrade & Baez, 1980:263, 264.—Chirino-Galvez, 1985: R126.—Baez & Ruiz, 1985:103. [Not Geryon affinis A. Milne Edwards & Bou- vier, 1894.] Geryon quinquedens. —Retamal, 1977:249, 250, fig. 1; 1981:33, fig. 179. [Not Geryon quinquedens Smith, 1879.] Previous records. —Chile: Zapallar, 33°34'S, 71°38'W, 380-450 m (Baez & An- drade 1977).—Central Chile, taken in fish- ery for Heterocarpus reedi Bahamonde (An- drade & Baez 1980). Juan Fernandez Islands: Juan Fernandez Islands [33°00’S, 80°00’W] (Retamal 1977, Baez & Ruiz 1985).—Isla Alejandro Selkirk [33°45’S, 80°46’ W] (Chirino-Galvez 1985).—East of Isla Robinson Crusoe and near Isla Santa Clara [33°42’S, 79°00’W] (Dupré 1975). Isla San Félix (Baez & Ruiz 1985). Material. —Chile: Off Chile, 33°35'S, /TA2Z2W, 370m: 3 males (in 3° lots, MNHN D-10824, D-10825, D-10875).— Isla San Félix, 26°16’S, 80°00’W, 27 May 1969, in lobster traps: one male (cl 126.8 mm, cb 145.5 mm, holotype, MNHN D-10821).—Off Quintero [32°47’'S, 71°32’W], 400 m: one male IOUV C-005).— Off Zapa- lar [32°33’S, 71°29’W], 400 m: one female (LOUV C-003).— Off Zapallar, 360-400 m: one male (MHNYV).—Islas Juan Fernandez: Isla Robinson Crusoe [33°38’S, 78°52'W]: three males IOUV C-001, C-002, C-004). — Isla Robinson Crusoe, 270-300 m: one specimen (MZUC).—Off Caleta Sanchez, Isla Alejandro Selkirk, 150 m, in lobster 402 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 1. Chaceon chilensis, new species. Male holotype, cl 127 mm, Isla San Félix: a, dorsal view: b, ventral view. Male paratype, cl 120.5 mm, off Chile: c, front. Male paratype, cl 115 mm, off Caleta Sanchez: d, dorsal view; é, anterior part of carapace; f, cheliped. traps, 1985, associated with Jasus frontalis (H. Milne Edwards) and Paramola rathbuni Porter: one male, one female (USNM 205697), one male (MIZUA C-688). All specimens other than the holotype are paratypes. Description. —A large Chaceon, cl to 152 mm, cb to 175 mm in adults, with five an- terolateral teeth on the carapace and later- ally compressed dactyli on the walking legs. Carapace broader than long, breadth 1.0- 1.2 times length, inflated anteriorly, espe- cially at protogastric regions. Median pair of frontal teeth large, separated by broad, V-shaped sinus, overreaching similar lateral frontal teeth. Distance between submedian VOLUME 102, NUMBER 2 frontal teeth less than distance between them and lateral frontal teeth. Second and fourth anterolateral teeth more obtuse and lower than first, third, and fifth teeth. Distance between first and third teeth subequal to distance from third to fifth, distance be- tween first and second teeth much less than from second to third. Suborbital tooth vis- ible in dorsal view, not extending to apex of lateral frontal tooth. Carapace with curved ridge extending mesially from each fifth lat- eral tooth, surface, except for gastric, and branchial regions, especially granular. Che- liped rough dorsally, with blunt subdistal tooth dorsally on merus, carpus lacking out- er spine but with well-developed triangular inner spine, propodus lacking distal dorsal spine. Meri of walking legs lacking distal dorsal spine. Fifth leg: merus broad, length five times height, about two-thirds cb (0.61- 0.65); propodus broad, length about four times height; dactylus about four-fifths as long as propodus. Dactyli of walking legs compressed, narrow, height at midlength much greater than width. Size. —Males, cl 107 to 152 mm, cb 124 to 174.5 mm; females, cl 102 to 124.5 mm, cb 112 to 151 mm. Baez & Ruiz (1985) recorded males with cl ranging from 105.8 to 124 mm, cb from 120.8 to 144.3 mm. Baez & Andrade (1977) reported a specimen with cl 152.1 mm, cb 174.5 mm, and Re- tamal (1977) studied a specimen measuring cl 120 mm, cb 140 mm. Remarks.—This new species resembles C. fenneri (Manning & Holthuis, 1984) in general appearance, but differs in numerous features. It is a longer-legged species, with the merus of the fifth leg greater than 0.6 of the carapace breadth (less than 0.6 in C. fenneri), and, although the legs are longer, the dactylus is shorter. The dorsal ridge on the carpus of the walking legs is much smoother. The carapace is more inflated dorsally and more rounded posterolaterally, and is much more granular. The median frontal teeth extend further forward. The suborbital margin is shaped differently: it is 403 Fig. 2. Chaceon chilensis, new species. Male para- type, cl 115 mm, off Caleta Sanchez. a, orbit, ventral view; b, propodus of fifth leg, posterior view; c, same, dorsal view. evenly curved in C. chilensis, flattened for much of its length in C. fenneri. One of the specimens (MNHN D-10875) has but three frontal teeth; it is shown in Fig. bf: N. Bahamonde N., in a letter of 8 August 1973 to John S. Garth, commented that the fishermen called this species “‘jaiba blanca,” because of its light color in life. Retamal (1981) called this species “‘can- grejo de profundidad.”’ There are records in the literature from the following depths: 270-300 m (Dupré 1975, Retamal 1977); 380-450 m (Baez & Andrade 1977); 200- 2000 m, in fishery for Heterocarpus reedi Bahamonde (Andrade & Baez 1980). Etymology.—The specific name reflects the known geographic range of the species, from localities off central Chile. Distribution. —Known only from locali- ties off central Chile, including the Juan Fer- nandez Islands and Isla San Félix. 404 Acknowledgments We thank our colleagues who facilitated our study of material of this species in the collections under their care. Roy K. Kropp photographed the specimens from USNM 205697. Lilly King Manning prepared all of the figures for publication. Literature Cited Andrade V., H., & P. Baez R. 1980. Crustaceos de- capodos asociados a la pesqueria de Heterocar- pus reedi Bahamonde 1955 en la zona central de Chile.—Boletin de Museo Nacional de His- toria Natural (Chile) 37:261-267. Baez R., P., & H. Andrade V. 1977. Geryon affinis Milne Edwards y Bouvier 1894 frente a las cos- tas de Chile (Crustacea, Decapoda, Brachyura, Geryonidae).—Boletin de Museo de Historia Natural, Valparaiso 10:215-—219. , & R. Ruiz L. 1985. Crustaceos de las islas oceanicas de Chile depositados en el Museo Na- cional de Historia Natural de Santiago. Pp. 93- 108 in P. Arana, ed., Investigaciones Marinas en el Archipiélago de Juan Fernandez. Univer- sidad Catolica de Valparaiso. Chirino-Galvez, L. 1985. Stenotermia y biogeografia de gerionidos (Crustacea, Decapoda, Brachy- ura).—Archivos de Biologia y Medicina Exper- imentales 18(2):R126 (abstract). PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Dupré M., E. 1975. Lista de Crustaceos Decapodos citados para el Archipiélago de Juan Fernan- dez.—CIMAR Documentos Técnicos 8/75:1—46. Centro de Investigaciones del Mar, Universidad Catolica de Valparaiso. Manning, R. B., & L. B. Holthuis. 1984. Geryon fen- neri, anew deep-water crab from Florida (Crus- tacea: Decapoda: Geryonidae).— Proceedings of the Biological Society of Washington 97(3):666— 673. ——., & 1989. Two new genera and nine new species of geryonid crabs (Crustacea, De- capoda, Geryonidae).— Proceedings of the Bi- ological Society of Washington 102(1):50-77. Retamal R., M. A. 1977. Sobre Geryon quinquedens Smith, 1870, en el Archipiélago de Juan Fer- nandez.—Boletin de Sociedad de Biologia de Concepcion 51(1):249-251. 1981. Catalogo ilustrado de los crustaceos decapodos de Chile. —Gayana (Zoologia) 44:110 pp. (LAC-G) Museo Sociedad Fonck, 4 Norte, 784 Vina del Mar, Chile (Present address) Department of Geology, Kent State Uni- versity, Kent, Ohio 44242; (RBM) Depart- ment of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 405-410 UPOGEBIA CORALLIFORA, A NEW SPECIES OF CORAL-BORING SHRIMP FROM THE WEST INDIES (DECAPODA: UPOGEBIIDAE) Austin B. Williams and P. J. B. Scott Abstract. — Upogebia corallifora, a new species of shrimp from the West In- dies, lives in boreholes that it excavates in CaCO, substrates, dead coral and Pleistocene limestone. The species, here described and illustrated, is similar in morphology to U. noronhensis from Arquipélago de Fernando de Noronha off northeastern Brazil. The chelae of the new species differ in having a longer fixed finger and lacking a row of spines on the lower mesial surface of the palm. Recent ecological studies on thalassinid shrimps, Upogebia, in the West Indies have shown that an undescribed species of this genus constructs boreholes in “‘skeletons of dead coral or the dead bases of living corals”’ (Scott, Reiswig & Marcotte 1988), and that juveniles, here provisionally included with it, bore into limestone (Scott, Moser & Risk 1988). We describe the new species in this paper. Upogebia corallifora, new species Fig. 1 Material examined.—Jamaica: USNM 230075. Holotype 2; Port Royal, Drunken- mans Cay, 3—4 m, area of dead Siderastrea siderea (Ellis & Solander 1786), P. J. B. Scott, Oct 1986.—USNM 230076. Paratypes, 2 6, 22(1 ovig.); Port Royal, Drunkenmans Cay, approx. 2—4 m, P. J. B. Scott, 10 Oct 1986. One ¢ and one 2 from this lot of specimens are to be deposited in the National Museum of Canada. Upogebia corallifora new species ? USNM 230077. 2 2 Guv.), 2 juvs.; Discovery Bay, boring in Pleistocene CaCO, of an artificial reef, about 5 m depth, P. J. B. Scott, Oct 1986 (specimens softened in Aerosol OT solution after being dried). Diagnosis. — Projections to either side of rostrum ending in acute spine. Postocular spine present. First and second abdominal segment lacking ventral spines; sixth seg- ment lacking hooked anterolateral spine. Telson subrectangular. Carpus of cheliped with one small spine on mesiodistal margin. Leg 2 with proximal mesioventral spine on merus; merus of leg 4 spineless. Description. —Rostrum triangular, short, slightly downturned; tip exceeding eye- stalks; dorsal pair of strong subapical spines followed on each side by two spines suc- cessively shorter in length, and separated from first by wide interval; ornamented dor- sal two-thirds of carapace surface anterior to cervical groove bearing pilose tufts, changing from spiny anteriorly to tubercu- late posteriorly, and angling toward sides posteriorly; gastric surface posterior to this smooth; ornamented anterior part separat- ed from and flanked on each side by pos- teriorly divergent ridge bearing crest of about 12 spines, strongest on lateral rostral pro- cess and decreasing to obsolescence poste- riorly. Cervical groove deep and continu- ous, shoulder lateral to it bearing one obsolescent tubercle below intersection with thalassinidean line; latter continuing to pos- terior margin of carapace. Postocular spine present. Abdomen broadly and smoothly arched dorsally; pleura of segment 1 narrowly rounded posterolaterally, those of 2—5 broadly rounded, with dense fine plumose 406 TV A~ uC a A. 5 alee Fig. A. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Upogebia corallifora, 2 holotype: a, Cephalic region, lateral; b, Anterior carapace, dorsal; c, Right cheliped, lateral; d, Same, mesial; e, Leg 2; h, Leg 5; i, Parts of abdominal segment 6, telson and uropods. Paratypes: dissociated legs 3-4, f, g. Scales: 1, a—h; 2, 1; each 1 mm. setae on posterolateral corner of terga 3-4, and in tracts on pleura of segments 3-5; segment 6 subrectangular, wider than long, lateral margin sinuous, adapted for inter- locking with extended uropodal exopod, notch anterior to posterolateral lobe contin- uous with oblique groove and lunate dorsal impression. Telson subrectangular, a little wider than long, broadest proximally, angle on antero- lateral margin interlocking with groove on central rib of uropodal endopod; posterior margin shallowly biarcuate and densely fringed with setae; transverse proximal ridge fairly prominent and continuous with low lateral ridges at each side; median groove obsolescent. Eyestalk stout, deepest at about mid- VOLUME 102, NUMBER 2 length, convex ventrally; eye narrower than diameter of stalk and directed anterolater- ally. Antennular peduncle reaching to about proximal one-fourth of terminal article of antennal peduncle, its proximal two articles together slightly longer than terminal arti- cle; flagella unequal, lower thinner ramus somewhat longer than thicker upper one. Antennal peduncle with about one-half its length extending beyond tip of rostrum; article 2 bearing tiny subdistal ventral spine; scale moderate, oval, sometimes with mi- nute terminal spine. Mouthparts as figured for U. jonesi (Wil- liams 1986); maxilliped 3 with epipod. Epistomial projection rather broad in lat- eral view, bearing small apical spine. Chelipeds essentially equal. Ventral mar- gin of ischium bearing one tiny spine. Merus with single subdistal dorsal spine reaching level of postocular spine, row of five small to moderate spines on ventral margin. Car- pus trigonal, shallow longitudinal groove jaterally and slender spine at anterior ven- trolateral corner; mesiodorsal crest of al- most uniform small spines remote behind prominent spine on anterior margin and partly obscured by setae in proximal part of row, all directed distad, and three very small spines on anterodorsal margin mesial to articulation of carpus; one small spine near middle of distomesial margin, and an obsolescent spine dorsal to it. Palm oval in cross section, length including fixed finger about three times maximal height; bearing mixed prominent plumose and long setae in one sparse dorsal row, plus lateral oblique row of setae ending anteriorly in patch of long setae near base of fixed finger; mesio- dorsal row of small somewhat irregular spines ending distally in small acute spine above condyle of dactyl; lower mesial sur- face spineless but bearing low transversely arcuate ridge proximally. Fixed finger slightly shorter than dactyl and more slen- der, slightly downcurved in middle and ta- 407 pering to slender tip, four small teeth on proximal prehensile edge. Dactyl much stouter than fixed finger, its curved upper surface bearing about three small, proximal tubercles; tip preceded on prehensile edge by more or less straight edge growing more elevated proximally and capped by obscure small teeth, then a toothless notch basally. Leg 2 reaching about to distal one-fourth of palm; carpus with obsolescent distodor- sal spine and tiny, acute, subdistal ventral spine; merus with small subdistal dorsal spine and moderate proximal mesioventral spine; coxa with strong proximal and small- er distal spine mesially. Leg 3 with slender ventral spines on proximal half. Leg 4 with spineless merus and ischium. Subchelate leg 5 reaching beyond ischium of cheliped. Two arthrobranchs arranged in biserial rows of undivided (entire) lamellae on max- illiped 3 and legs 1-4. Uropod with obsolescent spine on pro- topod above base of endopod; nearly straight distal margin of endopod exceeded by curved margin of exopod, both rami with dense fringe of setae and minute scattered spines or granules on distal margin; endo- pod with low, median longitudinal rib, and less prominent lateral rib having shallowly concave margin except for rounded, prox- imal shoulder; exopod with three ribs, me- sial sturdiest one bearing obsolescent spine proximally, intermediate rib longer, lateral rib least evident of all, slightly curved out- ward but shallowly concave proximally. Measurements in mm.—Holotype 2, length anterior carapace 4.6, length cara- pace 7.3, length chela including fixed finger 4.5, greatest height chela 1.2. Paratype 4, length anterior carapace 2.4, length cara- pace 3.3, chelae missing. Known range. —Specimens examined are limited to Jamaican localities listed above, although one additional specimen of what appeared to be U. corallifora was collected from dead coral on the reef of Bellairs Re- search Institute, Barbados in 1981. The lat- 408 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig.2. a, Mud-lined borehole ofjuvenile U. corallifora? exposed ina slabbed section of Pleistocene limestone, with part of one individual intact; b, SEM micrograph x 560 of burrow lining composed of organic and inorganic constituents. VOLUME 102, NUMBER 2 ter specimen was lost and cannot now be verified. It is possible that the species is widely distributed, though rare, in other parts of the Caribbean. Known distribution of U. corallifora is patchy. No specimens were found in recent reef coral on the north coast of Jamaica, where 188 kg of coral rubble and 97 kg of living coral were surveyed quantitatively. All specimens boring in recent reef rock were found in much smaller, qualitative samples taken at Drunkenmans Cay on the south coast, near Kingston. Bioeroders are gen- erally much more abundant in that area than on the north coast, including a species of boring mussel Lithophaga aristata (Dillwyn 1817) which does not occur at all in Dis- covery Bay on the north coast of the island (Scott 1988). Juveniles questionably re- ferred to U. corallifora were, however, found in Pleistocene limestone placed in Discov- ery Bay during the building of an artificial reef (Fig. 2). This limestone is much harder and denser than natural, recent reef rock. These juveniles have more robust chelipeds than the adults described above, but resem- ble the adults in other respects. We ques- tionably refer them to the new species until more material is available for comparative study. Habitat.—The habitat of U. corallifora partly overlaps that of the much more abun- dant U. operculata Schmitt 1924. Both species inhabit dead coral skeletons in Ja- maica, but occurrence of the former is much restricted. It has not been found with bore- holes opening from living corals, which are a common habitat for U. operculata (Scott, Reiswig & Marcotte 1988); see Warme (1975) for distinction between boring in hard and burrowing in soft substrates. A coral- boring species, U. trypeta Sakai (1970, 1982), has also been reported from Japan. Boreholes of U. corallifora are similar in appearance to those of U. operculata (Klee- mann 1984; Scott, Reiswig & Marcotte 1988). Pairs of individuals (one 6, one 9) live in complex, multi-chambered excava- 409 tions which are just wide enough to allow the occupants to somersault and reverse di- rection. Excavations are lined with a mix- ture of mud, coral fragments and organic material. Energy dispersive X-ray analysis (EDAX) of borehole lining material re- vealed the presence of Ca, Si, Mg, Al, Cl, K & S. Openings to borings are difficult to detect on the irregular surface of dead coral; each opening lies a few millimeters below the surface in a smooth conical pit and is much narrower than the remainder of the hole to which it gives access. Adult shrimps are trapped in the borings by the restrictive openings. Remarks. — Upogebia corallifora is simi- lar to U. noronhensis Fausto-Filho 1969 (comparison made with paratype °°, No. 163, carcinological collection, LABOMAR, Universidade Federal do Ceara, Brazil, Fer- nando de Noronha, Baia de Sueste, Fausto- Filho, 7/8/68), which in turn has some sim- ilarity to U. spinigera (Smith 1871) of the eastern Pacific, but U. corallifora is appar- ently a smaller and less spinose species than either of the latter. Upogebia corallifora keys out to U. noronhensis in Williams (1986: 10), but the two can be separated by means of the following emendation to the con- cluding couplet of his key to Atlantic species of the genus. — Chelae with no spines proximal to fixed finger on ventral keel of palm 7. Chela with fixed finger about equal in length to dactyl; palm spineless on lower mesial surface eee eee U. corallifora, n. sp. — Chela with fixed finger about % length of dactyl; palm with row of more or less distinct spines on lower mesial surface lpg U. noronhensis Fausto-Filho Etymology.—The name, a noun form from the Latin “corallum,” coral, and ‘foro,’ bore or pierce, alludes to the coral- boring capabilities of the species. e, 0) lapresrette: tw) (oe) Gs) -el fe! 0) .a) ep 6 .e ce 410 Acknowledgments We thank Dr. Jeremy Woodley and staff of the Discovery Bay Marine Laboratory, University of the West Indies, and Dr. Dun- bar Steele, Chairman, Department of Zo- ology, University of the West Indies, Mona Campus, for facilities and assistance in the field. Many thanks also to dive buddy and cheerful coral basher Ian Sandeman. Con- tribution No. 437, Discovery Bay Marine Laboratory, University of the West Indies. Literature Cited Kleemann, K. 1984. Lebensspuren von Upogebia operculata (Crustacea, Decapoda) in karibisch- en Steinkorallen (Madreporaria, Anthozoa).— Beitrage zur Palaontologie von Osterreich, In- stitut flir Palaontologie der Universitat Wien 11: 35-49. Sakai, K. 1970. A new coral burrower, Upogebia try- peta sp. nov. (Crustacea, Thalassinidea) col- lected from Amami-Oshima, Japan.— Publica- tions of the Seto Marine Biological Laboratory 18(1):49-56. 1982. Revision of Upogebiidae (Decapoda, Thalasssinidea) in the Indo-West Pacific re- gion.— Researches on Crustacea, The Carcino- logical Society of Japan, Special Number 1:1- 106, plates A-C. Scott, P. J. B. 1988. Distribution, habitat and mor- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON phology of the Caribbean coral- and rock-boring bivalve, Lithophaga bisulcata (d’Orbigny) (My- tilidae: Lithophaginae).— Journal of Molluscan Studies 54:83-95. —., K.A. Moser, & M. J. Risk. 1988. Bioerosion of concrete and limestone by marine organisms: A 13 year experiment from Jamaica.— Marine Pollution Bulletin 19(5):219-222. —., H. M. Reiswig, & B. M. Marcotte. 1988. Ecol- ogy, functional morphology, behaviour, and feeding in coral- and sponge-boring species of Upogebia (Crustacea: Decapoda: Thalassini- dae).—Canadian Journal of Zoology 66:483- 495. Warme, J. E. 1975. Borings as trace fossils, and the processes of marine bioerosion. Pp. 181—227 in R. W. Frey, ed., The study of trace fossils, a synthesis of principles, problems, and proce- dures in ichnology. Springer-Verlag, New York. Williams, A. B. 1986. Mud shrimps Upogebia, from the eastern Pacific (Thalassinoidea: Upogebi- idae).—San Diego Society of Natural History, Memoir 14:1-60. (ABW) National Marine Fisheries Ser- vice Systematics Laboratory, U.S. National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560; (PJBS) Department of Geology, McMaster Uni- versity, Hamilton, Ontario L8S 4M1, Can- ada. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 411-417 ADDITIONAL RECORDS FOR AN ATLANTIC REEF LOBSTER, ENOPLOMETOPUS ANTILLENSIS LUTKEN, 1865 (CRUSTACEA, DECAPODA, ENOPLOMETOPIDAE) Raymond B. Manning and David K. Camp Abstract. — Additional records from the Gulf of Guinea, the Caribbean Sea, Bermuda, and Florida are provided for E. antillensis Litken, 1865. The syn- onymy of E. dentatus Miers, 1880, with E. antillensis is confirmed. The astacidean genus Enoplometopus A. Milne Edwards, 1862, now includes two subgenera and nine species (Holthuis 1983: 282; Kensley & Child 1986:520; de Saint Laurent 1988:61,62). Two representatives of the subgenus Hoplometopus Holthuis, 1983, occur in the Atlantic: E. callistus Intés & Le Loeuff (1970:1442), with its junior synonym E. biafri Burukovsky (1972:180) (see Holthuis 1983:281), from the East At- lantic, and E. antillensis Litken, 1865, from amphi-Atlantic localities. Another member of this subgenus, EF. holthuisi Gordon, 1968, is known from several localities in the Indo- West Pacific (Holthuis 1983:297), and de Saint Laurent (1988) recently described a fifth species, Hoplometopus gracilipes, from the Loyalty Islands. De Saint Laurent ele- vated the subgenus Hoplometopus to ge- neric status. All five representatives of the nominal subgenus occur only in the Indo- West Pacific (Holthuis 1983; Debelius 1984, 1986; Kensley & Child 1986). De Saint Laurent (1988) also established the family Enoplometopidae and _trans- ferred the family from the Thalassinidea to the Astacidea. Holthuis (1983:281-282) enumerated morphological differences between the two subgenera, and it appears that these are partly accompanied by differences in color pattern also. Members of the nominal sub- genus show color patterns dominated by scattered spots or lines of pigment on the abdomen and carapace, whereas two of the four members of Hoplometopus each have distinctive irregular circles of pigment, one white, one reddish, around a central white spot on each side of the red to reddish-or- ange carapace. Remnants of this pattern are visible in recently preserved specimens of E. antillensis reported here. The pattern is clearly shown for specimens of E. antillensis and E. holthuisi by the following authors: Cousteau (1958, color figure of E. antillensis on p. 393); Forest (1959, black and white print of E. antillensis; same figure as in Cousteau 1958); Debelius (1984, color fig- ure of E. holthuisi on p. 37); Debelius (1986, color figures of EF. antillensis and E. hol- thuisi on p. 13); Kosaki (1987, color figure of E. holthuisi on p. 14); Brady (1987, black and white figure of E. antillensis on p. 26); and Hunziker (1988, color figures of E. hol- thuisi on pp. 83 and 84). The pattern also was described by Holthuis (1983:297) based on color figures of E. holthuisi published by Daum (1982) and George & George (1979). In contrast, E. callistus lacks this distinctive color pattern (P. Le Loeuff, in litt.), as does H. gracilipes (M. de Saint Laurent, in litt.). Until recently, Enoplometopus antillensis had been recorded only once in the West Atlantic north of Brazil (1.e., ““West Indies,” Litken 1865). Another nominal species, EF. dentatus Miers, 1880, from St. Helena Is- land, had been questionably synonymized with E. antillensis by Holthuis (1946:79), 412 then more positively by Chace (1966:634) and Gordon (1968:80, footnote), although none of those authors had had an oppor- tunity to compare the types of the two species. Gordon (1968) published the first detailed description of the type of E. den- tatus, compared it with two unpublished drawings of the type of E. antillensis, and concluded that the two species were con- specific. Examination by one of us (D.K.C.) of material sent by Mr. John Brady for iden- tification after the discovery of a population of E. antillensis off Florida (Brady 1987) revealed some apparent discrepancies be- tween his material and Gordon’s descrip- tion of the type of E. dentatus. Our finding of the apparent discrepancies prompted us to compare the types of the two species, that of E. dentatus in the British Museum (Nat- ural History), London (BM), and that of E. antillensis in the Zoological Museum, Co- penhagen (ZMC), and to examine other At- lantic specimens of the genus in the collec- tions of the National Museum of Natural History, Smithsonian Institution (USNM), the Florida Department of Natural Re- sources (FSBC I), and the Indian River Coastal Zone Museum (IRCZM). The re- sults are presented here. Enoplometopus antillensis Liitken, 1865 Figs. 1-4 Enoplometopus antillensis Litken, 1865: 265.—De Man, 1916:96.—Holthuis, 1946:72, pl. 5, fig. h, pl. 7, fig. b.—Chace, 1966:634—Gordon, 1968:80 [foot- note].— Fausto Filho, 1970:55, figs. 1-2.- Burukovsky, 1972:188, fig. 2.—Fausto Filho, 1976:222, fig. 1.—Holthuis, 1983: 281, 282.—Debelius, 1986: lower right fig, on p.-1 3. Enoplometopus dentatus Miers, 1880:381, pl. 15, fig. 7.-—De Man, 1916:96.—Hol- thuis, 1946:72.—Gordon, 1968:80, figs. lL, 3-/3—Intes and ke Locult..19 70: 1442.—Holthuis, 1983:281. Enoplometopussp.—Gurney, 1938:296 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON [part; origin of figured specimens un- known].— Forest, 1959: pl. 3, fig. 4. nephropsid.— Cousteau, 1958: color fig. on p. 393. Enoplometopus Antillensis.—Brady, 1987: 26, unnumbered fig. Previous records. —East Atlantic: 1° 25'10’S, 5°36'10”E, Sao Tomé Island, Gulf of Guinea (Cousteau 1958, Forest 1959). Central Atlantic: St. Helena Island [15°58’S, 05°43'W] (Miers 1880, Chace 1966, Gordon 1968).—Off Brazil, 03°17’S, 29°57'W (late larva; Gurney 1938). West Atlantic: Off Rio Grande do Norte State, Brazil (Fausto Filho 1970).—Off northeast coast of Brazil (Fausto Filho 1976).— West Indies (Lutken 1865, Gordon 1968).—About | mile NE of Lake Worth Inlet, Florida (Brady 1987). Material. —East Atlantic: Gulf of Guinea, off Gabon, 3°30’S, 8°53’E, 110 fm (=201 m), Geronimo Sta. 227/2, 7 Sep 1963: 1 juvenile, cl 6.5 mm (USNM 136692). Central Atlantic: St. Helena Island: | fe- male, cl 19.5 mm (BM 68.57; holotype of E.. dentatus Miers). West Atlantic: Bermuda: Half way be- tween Kitcheners and N.E. marker, from gut of red hind caught in 10 fm (=18 m), W. Soares, 24 Feb 1985: 1 male, cl 38 mm (USNM). East coast of Florida: Spanish Anchor Reef, about 1 mile N of Lake Worth Inlet, 90 ft (=27 m), John Brady, 15 Dec 1985: exuvium of 1 male, cl 30 mm (USNM 231216).—Same locality, 27 Aug 1985: 1 damaged female, tl about 110 mm (FSBC I 31885).—Larsen’s Valley Reef, about 1 mile NE of Lake Worth Inlet, 65 ft (=20 m), John Brady, 15 Feb 1986: 1 female, cl 43 mm (IRCZM 89:6349). West Indies: 1 female, cl 20 mm (ZMC; holotype of E. antillensis Lutken). Bahama Islands: Grand Bahama Island, SE of Settlement Point, D. de Sylva et al., Sta..355, 27 Jul 1961: 1 female, cl 1525 mama (USNM 126226). Panama: Golfo de Mesquites, Bahia de VOLUME 102, NUMBER 2 413 Pip. 1. Holotype of Enoplometopus antillensis Liitken. a, Carapace, Lateral view; b, Carapace, dorsal view; c, Third maxilliped: d, Cheliped: e, Abdomen, lateral view; f, Posterior margin of sixth abdominal somite and tail fan. Almirante, 9°25'30”N, 82°20’W, lobster trap, 3-11 fm (=5-—20 m), Pelican Sta. 930, 23-25 May 1963: 1 male, cl 31 mm (USNM 170659). Netherlands West Indies: Bonaire, in caves, 30 ft (=9 m), R. V. Harrison, 21 Apr 1975: 1 ovigerous female, cl 31 mm (USNM 155655). Remarks. —In June 1986, one of us (R.B.M.) was able to compare the holotypes of E. dentatus Miers and D. antillensis Lit- ken at the British Museum (Natural His- tory), London. As a result of this compar- ison, we agree that these species are conspecific, as already suggested by others. Apparent discrepancies between Gordon’s account of the type of E. dentatus and ac- counts in the literature of E. antillensis are largely attributable to the poor condition of Miers’ type specimen, which apparently had dried out at one time. We provide here some sketches of the type of E. antillensis (Fig. 1). In her account of the type of FE. dentatus, Gordon noted that there was no inferodistal spine on the merus of the second pereopod. The spine is in fact present on all but one of the legs still loose with the holotype (Fig. 2a); on the second pereopod it appears to have been worn off. Gordon’s figure of the posterior margin of the sixth abdominal so- mite (see our Fig. 25) is a little misleading; the margin is not nearly so smooth as she shows it. Numbers of spines on the outer surface of the dactyli of the third and fourth pereopods could not be verified on the type of E. dentatus, as the ends of the dactyli were missing. The terminal spine of the an- tennal scale is not rounded anteriorly as de- scribed by Gordon; the tip appears to have been broken off, possibly since she exam- ined it. 414 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON a b ip i Fig. 2. Holotype of Enoplometopus dentatus Miers b, Telson. The color pattern of this species 1s quite distinctive. Overall, the body has an orange to orange red cast, and the long setae fring- ing the chelipeds are reddish; marginal spines on chelipeds are red proximally and have a white tip. Walking legs and third maxil- lipeds are banded with white, as are meri and fingers of the chelipeds; propodi of the chelipeds are red with darker red granules. In dorsal view, there is a darker red stripe . a, Distal part of merus and carpus of second pereopod; down the center of the body. On the cara- pace each dorsal spine bears a white spot, and on the abdomen there are white spots on the darker median stripe, as well as two prominent white spots laterally on each ab- dominal somite. Much of the lateral surface of the carapace is marked with wavy white lines, which, anteriorly, are replaced by a large, irregular, reddish circle surrounding a white spot (Fig. 3). Fig. 3. Enoplometopus antillensis Liitken. Color pattern of carapace of exuvium of male from Florida. VOLUME 102, NUMBER 2 415 Fig.4. Enoplometopus antillensis Litken. Juvenile from Gabon. a, Carapace, dorsal view; b, Carapace, lateral view; c, Cheliped: d, Abdomen, lateral view; e, Posterior margin of sixth abdominal somite and telson. Records for E. antillensis given here ex- tend the known range of the species in the West Atlantic northward to continental North America and Bermuda. Off Florida, specimens have been captured or observed (John Brady, in litt.) at the following local- ities between West Palm Beach and Fort Pierce: 26°41'22”N, 80°00'09”W, depth 60 ft (=18 m), four individuals seen at night only; 26°47'75"N, 79°59'28”W, depth 100 ft (=30 m), 18 individuals seen during day and night; 27°28'02”N, 80°09'23”W, depth 50 ft (=15 m), two specimens seen during daytime. All specimens were seen on lime- stone ridges that parallel the shoreline in those areas. The lobsters are very cryptic, usually hiding in crevices within the ledges during day and emerging at night, except in late March and early April in West Palm Beach. Numerous specimens, as many as five on one dive, were seen during the day. and they appeared to display aggressive ter- ritorial behavior. In contrast, few or none were observed during the day at the same location in May. The immature specimen from the Gulf of Guinea (Fig. 4) agrees well with other ma- terial of this species, in spite of its unusually deep occurrence in 201 m, and differs from E. callistus in the characters listed by Intés and Le Loeuff (1970). There are five rather than four median spines and three rather than two lateral spines on the carapace, and there are two rather than three posterior spines on the sixth abdominal segment. The anterior telson spines are close together and the claws are long and slender. Gurney (1938) reported a late larva of an Enoplometopus that may be identifiable with this species. According to M. de Saint Laurent (in litt.) there is a previously unreported specimen of this species from Madeira in the Muséum National d’Histoire Naturelle in Paris. Acknowledgments Torben Wolff, Zoological Museum, Co- penhagen, made possible the direct com- parison of the holotype of E. antillensis Lut- 416 ken with that of E. dentatus Miers by sending Liitken’s type to the British Museum (Nat- ural History), London, where one of us (R.B.M.) could examine both types togeth- er. Both Dr. Wolff and R. W. Ingle of the British Museum also provided working space and access to their collections. We thank Paula Mikkelsen for allowing us to work with material in the Indian River Coastal Zone Museum at the Harbor Branch Oceanographic Institution, Link Fort, Flor- ida. L. B. Holthuis made available a copy of the 1972 paper by Burukovsky, for which we thank him. John Brady of Sebastian, Florida, first brought the occurrence of E. antillensis off the east coast of Florida to our attention, and subsequently made spe- cial efforts to secure material for us; he also provided us with color photographs of this species. We thank M. de Saint Laurent, Mu- seum National d’ Histoire Naturelle, Paris, for telling us about the references to E. an- tillensis from the Gulf of Guinea and Gur- ney’s paper, which we otherwise would have overlooked, and for her comments on a draft of our manuscript. We thank Thomas H. Perkins and William G. Lyons, Florida Ma- rine Research Institute, for their comments on the manuscript. The figures were pre- pared by Lilly King Manning. This is contribution number 198 from the Smithsonian Marine Station at Link Port, Florida. Literature Cited Brady, J. 1987. Rare reef lobster identified. — Florida Scuba News, January 87:26. Burukovsky, R. N. 1972. Enoplometopus biafri— new lobster species of the family Nephropidae (Decapoda, Crustacea).— Trudy Atlantniro 42: 180-189 [in Russian]. Chace, F. A., Jr. 1966. Decapod crustaceans from St. Helena Island, South Atlantic.— Proceedings of the United States National Museum 118(3536): 623-661, pls. 1-2. Cousteau, J.-Y. 1958. Calypso explores an undersea canyon.—The National Geographic Magazine 113(3):373-396. Daum, W. 1982. Ueber die Gattung Enoplometopus. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Grossekrebse im Aquarium, 3.— Die Aquarien- und Terrarien-Zeitschrift, 35(7):265—269 [not seen]. Debelius, H. 1984. Armoured knights of the sea. 120 pp. Kernen Verlag, Essen. 1986. Reef lobsters: Genus Enoplometo- pus.—Freshwater and Marine Aquarium 9(3): 12-17. Fausto Filho, J. 1970. On the occurrence of Enoplo- metopus antillensis Litken, 1865 (Decapoda, Nephropidae) on the Brazilian coast.—Crusta- ceana 18(1):55-59. . 1976. Description of male of Enoplometopus antillensis Litken, 1865 (Decapoda, Nephro- pidae).—Crustaceana 30(2):222-224. Forest, J. 1959. Introduction, 1. Campagne de la Ca- lypso dans le golfe de Guinée et aux iles Principe, Sao Tomé, Annobon (1956), X. Résultats scien- tifiques des campagnes de la “Calypso,” 4.— Annales de |’Institut Océanographique 37:4—36, pls. 1-3. George, J. D., & J. J. George. 1979. Marine life. An illustrated encyclopedia of invertebrates of the sea. 288 pp, pls. 1-128 [not seen]. Gordon, I. 1968. Description of the holotype of En- oplometopus dentatus Miers, with notes on other species of the genus (Decapoda).—Crustaceana 15(1):79-97. Gurney, R. 1938. Nephropsidea and Thalassinidea. Larvae of Decapod Crustacea, part V.— Discov- ery Reports 17:291-344. Holthuis, L. B. 1946. The Decapoda Macrura of the Snellius Expedition, I.—Temminckia 7:1-178, pls. 1-11. 1983. Notes on the genus Enoplometopus, with descriptions of a new subgenus and two new species (Crustacea Decapoda, Axiidae).— Zoologische Mededelingen, Leiden 56(22):28 1- 298. Hunziker, R. 1988. Curious crustaceans—the reef lobsters.—-Tropical Fish Hobbyist 36(5):80-84. Intés, A., & P. Le Loeuff. 1970. Sur une nouvelle espéce du genre Enoplometopus A. Milne Ed- wards du Golfe de Guinée: Enoplometopus cal- listus nov. sp. (Crustacea, Decapoda, Homari- dea). — Bulletin du Muséum National d’ Histoire Naturelle, Paris (2)41(6):1442-1447, pl. 1. Kensley, B., & C. A. Child. 1986. A new species of Enoplometopus (Thalassinidea: Axiidae) from the northern Philippines.—Journal of Crusta- cean Biology 6(3):520-524. Kosaki, R. K. 1987. Hawaiian cave crustaceans. — Freshwater and Marine Aquarium 10(4):12-15. Liitken, Chr. 1865. Enoplometopus antillensis Ltk., en ny vestindisk Hummer-Art.— Videnskabe- lige Meddelelser fra Dansk Naturhistorisk For- ening, Copenhagen 6:265-268. VOLUME 102, NUMBER 2 de Man, J. G. 1916. Families Eryonidae, Palinuri- dae, Scyllaridae and Nephropsidae. The Deca- poda of the Siboga Expedition, Part III.—Si- boga-Expeditie 39a?:1—122, pls. 1—4. Miers, E. J. 1880. Crustacea Anomura and Macrura (except Penaeidea). On a collection of Crustacea from the Malaysian region, IJJ.—Annals and Magazine of Natural History (5)5:370-384, pls. 14-15. de Saint Laurent, M. 1988. Enoplometopoidea, nou- velle superfamille de Crustacés Décapodes As- 417 tacidea.—Compte Rendu Hebdomedaire des Seances de l’Académie des Sciences, Paris, Zoo- logie (3)307:59-62. (RBM) Department of Invertebrate Zo- ology, National Museum of Natural His- tory, Smithsonian Institution, Washington, D.C. 20560; (DKC) Florida Marine Re- search Institute, 100 Eighth Avenue, S.E., St. Petersburg, Florida 33701. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 418-433 STUDIES OF NEOTROPICAL CADDISFLIES, XL: NEW SPECIES OF SMICRIDEA (SMICRIDEA) FROM MIDDLE AMERICA AND THE WEST INDIES (TRICHOPTERA: HYDROPSYCHIDAE) Oliver S. Flint, Jr. and D. G. Denning Abstract. —Twelve species are described in the genus Smicridea, subgenus Smicridea: tobada (Tobago, Trinidad), anomala (Trinidad, Tobago), aurimac- ula (St. Vincent), cartiensis (Panama), multidens (Panama), corralita (Mexico), bulara (Trinidad), mirama (Panama), filicata (Costa Rica, Panama), circinata (Panama), holzenthali (Costa Rica), and /atipala (Panama). Abdominal pher- omone glands, found in segments 6 and 7 of the male, are described and illustrated for S. breviuncata Flint and S. cuna Flint. Variations in male genitalia are shown for these two species and S. turrialbana Flint. The nominal subgenus of Smicridea, con- taining over 60 species, is limited to the New World. Its closest relationships are with several similar genera from Tasmania and Australia (Flint 1989). The New World species are found from southwestern United States to southern South America, with species on all the larger Antillean islands. Flint revised the systematics of the species in North and Central America (1974a), in the Lesser Antilles (1968), in central, north- ern Venezuela (1981), and in Suriname (1974b). Although the majority of species from these regions are now namable, un- described species continue to be collected, and species descriptions and names are nec- essary for impending faunal studies. We have also obtained from the Univer- sity of California, Berkeley those unnamed specimens reported by McElravy et al. (1981). The genitalia were missing from the only example of “A,”’ so its identity remains unknown. Species “‘B” is described as S. filicata. All species described here belong to the subgenus Smicridea as defined by Flint (1974a). Males of species in this subgenus are easily distinguished form those in sub- genus Rhyacophylax by a spur count of 1, 4, 4 (rather than 1, 4, 2), and by two pairs of pheromone glands in the abdomen (lack- ing in Rhyacophylax). These glands open externally through the membranes between segments 7 and 8 and segments 6 and 7, but lie within segments 7 and 6 when not ex- truded. Within the subgenus Smicridea, the new species tobada is placed in the fasciatella group, and the remaining new species are placed in the nigripennis group (Flint 1974a). Smicridea anomala is quite unusual, be- cause its phallus is very long, open and membranous ventrally and contains a series of heavy spines. These characteristics are lacking in the fasciatella group. Species of the nigripennis group, however, have some- what similar phalli: generally open and membranous apicad and bearing a wide as- sortment of spines and processes. Therefore we place anomala in the latter group and recognize that when the Neotropical fauna is better known it may be transferred to a newly recognized species group. Acronyms used in the text indicate depos- itories of specimens as follows: CAS (Cali- fornia Academy of Sciences, San Francisco, California), DGD (D. G. Denning collec- tion, Moraga, California), NMNH (Nation- VOLUME 102, NUMBER 2 al Museum of Natural History, Smithson- ian Institution, Washington, D.C.), UCD (University of California, Davis, Califor- nia), UMSP (University of Minnesota, St. Paul, Minnesota), UPP (Fairchild Museo de Invertebrados, University of Panama, Pan- ama), WSU (Washington State University, Pullman, Washington). Smicridea (Smicridea) tobada, new species Figs. 1-5 This species is related to S. bulbosa Flint (Flint 1974b, figs. 191-193) on the basis of the general structure of the genitalia and the presence of apical sclerites in the phallus. Diagnostic differences are a less bulbous apex of the phallus, and especially, the basal angulation of the phallotheca, which is very prominent on the ventral margin, and the broader apex of the clasper. Adult.—Length of forewing, 4-5 mm. Color fuscous, legs and antennae paler; fore- wing fuscous with two white bands, apical fringe white. Male genitalia (Figs. 1-2): Ninth segment with anterior margin slightly expanded. Tenth tergite elongate, narrow- ing apicad in lateral aspect; in dorsal aspect elongate, apex obliquely truncate, with small apicomesal lobe. Clasper with basal seg- ment elongate, parallel-sided; apical seg- ment third length of basal segment, dorsal margin with apex acute, enlarged ventrad and nearly truncate, with cluster of small setae (Fig. 3). Phallus (Figs. 4—5) tubular, angled posteriad from base, with a distinct angle near base which is most pronounced on ventral margin; apex with a pair of dor- solateral sclerites with apices curved mesad; with a recurved internal sclerite in lateral aspect, dorsal aspect of this sclerite with me- sobasal section divided apically into two lateral, bandlike sclerites that curve ventrad and then basad. Type material. —Holotype, ¢, Tobago: St. John Province; Charlotteville, 14-21 Mar 1979, D. Hardy and W. Rowe (NMNHB). Paratypes: Same data, 1 6, 1 2 (NMNH). 419 Trinidad: Arima Valley, Spring Hill Estate, 1500’, 1 Feb 1983, W. G. Downs, 24 4 (DGD, NMNH). Smicridea (S.) breviuncata Flint Figs. 26-29 Smicridea (S.) breviuncata Flint 1974a:18. Minor differences are present between a specimen from southern Costa Rica (Figs. 26-29) and figures in Flint (1974a, figs. 60- 63) prepared from a specimen from central Costa Rica. Pheromone glands of abdominal segment 7 are shown in Figs. 28, 29. The reticulated capsule with glands extruded is translucent and covered with dense silver colored spi- nules (Fig. 28). The reticulated capsule with glands not extruded is shown in Fig. 29. Material examined.—Costa Rica: Las Cruces, 20 Jul 1977, Evan A. Sugden, 1 6 (UCD). Smicridea (S.) anomala, new species This peculiar species is placed in the m- gripennis group, although it differs radically from all other described species in the ge- nus. It alone has a phallus that is sclerotized and elongate dorsally. The similarity be- tween S. anomala and the nigripennis group is the membranous, ventral opening of the phallus which bears a series of large spines internally. Adult. —Length of forewing 4.5-5.0 mm. Wings uniformly black in alcohol, heavily setose; head, thorax black; antennae, legs ochraceous. Spurs small on first and third legs, large on second pair of legs. Male gen- italia (Figs. 6—7): Ninth segment with an- terior margin rounded, slightly produced. Tenth tergite in lateral and dorsal aspects wide, lightly sclerotized, tapering to a narrow, rounded apex. Clasper basal seg- ment expanded distally; apical segment short, apex acute and curved ventromesad. Phallus (Figs. 8, 9) semierect, sclerotized dorsally; apex and ventral area membra- ~ — — 420 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Figs. 1-9. Male genitalia of Smicridea. 1-5, tobada. 1, Lateral view. 2, Ninth and tenth terga and clasper, dorsal view. 3, Apical segment of clasper, posteroventral view. 4, Apex of phallus, dorsal view. 5, Phallus, lateral view. 6-9, anomala. 6, Lateral view. 7, Ninth and tenth terga and clasper, dorsal view. 8, Apical half of phallus, ventral view. 9, Phallus, lateral view. VOLUME 102, NUMBER 2 nous; 5—6 large, dark brown spines arise from mesal surface and project to or beyond ven- tral margin, a slightly darkened phallotre- mal sclerite near apex. Type material.—Holotype, 6, Trinidad Island: Simla Research Station, 2-15 Jun 1981, W. J. Hanson and C. L. Clemons (DGD, to be deposited in CAS). Paratypes: Same data, 1 6 (DGD). Tobago: St. John Province; Charlotteville, 14-21 Mar 1979, D. Hardy and W. Rowe, 1 6 (NMNH). Dr. W. H. Hanson informs us that the specimens were collected in a light trap, with “‘a few ponds and a stream about one-eighth mile away in the heavily forested area.”’ Smicridea (S.) aurimacula, new species Figs. 18-21 This species is a member of the nigripen- nis group of Smicridea and is in the cariba section where it is closely related to S. gren- adensis Flint (1968, figs. 61-63). Smicridea aurimacula shares with S. grenadensis the slightly upturned and truncate apex of the tenth tergum and six pairs of long internal phallic spines. However, it differs conspic- uously by the golden banding on the fore- wings and the presence of straight lateral spine and an apicolateral plate bearing sev- eral small teeth on the phallus. Adult. — Length of forewing, 4.5 mm. Col- or golden brown, head and thorax with gold- en hair; forewing with stripe of golden hair in costal cell widening at stigma and apicad, another broad golden stripe along posterior margin almost touching anterior stripe at chord, thus leaving a central, fuscus stripe in center of wing which is almost bisected at chord. Male genitalia (Figs. 18, 19): Ninth segment with anterior margin vertical, mak- ing a right angle posteriad subdorsally. Tenth tergite short, apex truncate and slightly up- turned in lateral aspect; in dorsal aspect short, apex truncate, broad. Clasper with basal segment long, extending beyond apex of segment 10, expanded distally; apical seg- 421 ment elongate, apex acute. Phallus (Figs. 20, 21) elongated basally, open apically; apex with ventral lobe entire, produced into a slightly flattened mesal lobe, with dorsal margin inrolled apically; with a large, paired, basolateral spine, endotheca with five to six pairs of large, apical spines and a paired, apicolateral, lightly sclerotized sclerite bear- ing several small spines, and a ventrobasal Y-shaped sclerite. Type material. — Holotype, 6, St. Vincent: Hermitage, 14 Nov 1975, C. L. de Freitas (NMNH). Paratypes: Same data, 16 6, 14 9 (NMNB). Smicridea (S.) cartiensis, new species Figs. 10-13 This species and S. multidens are the first discovered continental species of the cariba section of the nigripennis group. S. cartien- sis and multidens are closely related, differ- ing only in the armature of the endotheca. In cartiensis the endotheca bears a few scat- tered sclerotized small spines on its surface, but in multidens there is a large basolateral plate with many acute spines. Adult. — Length of forewing, 4 mm. Color fuscous, head with silvery hair mesally; forewing fuscous with scattered silvery hair basally, with two white bands, more distal band arcuate and not quite reaching pos- terior margin, apical fringe white. Male gen- italia (Figs. 10, 11): Ninth segment with small lateral lobe on anterior margin. Tenth tergite short, apex divided into lateral and mesal lobes, in lateral aspect apicodorsal angle acute, mesal lobe mostly hidden; in dorsal aspect short, lateral lobe truncate, broad, mesal lobe shorter and darker than lateral lobe. Clasper with basal segment long, inflated distally; apical segment elongate, apex acute. Phallus (Figs. 12, 13) elongated basally, open apically; apex with ventral lobe entire, produced into a tapered mesal pro- jection; endotheca with dorsal margin light- 422 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 16 Figs. 10-17. Male genitalia of Smicridea. 10-13, cartiensis. 10, Lateral view. 11, Ninth and tenth terga and clasper, dorsal view. 12, Phallus, ventral view. 13, Phallus, lateral view. 14-17, multidens. 14, Lateral view. 15, Ninth and tenth terga and clasper, dorsal view. 16, Phallus, ventral view. 17, Phallus, lateral view. ly sclerotized, with a large, paired, basolat- Type material.—Holotype, ¢, Panama: eral spine, a pair of large, internal spines Intendency of San Blas; Rio Carti Grande, apically and broad, short spines irregularly 2 km W. Nusagandi (9°20'N; 78°56’W), 5 located apicolaterally. Mar 1985, Flint and Louton (NMNH). VOLUME 102, NUMBER 2 Paratypes: Same data, 7 6, 3 2? (NMNH, UPP). Smicridea (S.) multidens, new species Figs. 14-17 This species is closely related to S. car- tiensis. Diagnostic differences are in the ar- mature of the membranous central lobe of the endotheca. In multidens this lobe bears a large basolateral plate armed with many spines; in cartiensis the plate is broken up and the spines are fewer and concentrated on the lateral surface of the endotheca. Adult. —Length of forewing, 4.5 mm. Col- or brown in alcohol, denuded; forewing membrane with pale band at level of stigma. Male genitalia (Figs. 14, 15): Ninth segment with small lateral lobe on anterior margin. Tenth tergite short, apex divided into lateral and mesal lobes, in lateral aspect, apico- dorsal angle acute, mesal lobe mostly hid- den; in dorsal aspect lateral lobe truncate, broad, mesal lobe shorter and darker than lateral. Clasper with basal segment long, in- flated distally; apical segment elongate, apex acute. Phallus (Figs. 16, 17) elongated ba- sally, open apically; apex with ventral lobe entire, produced into a mesal process; en- dotheca with large, paired, basolateral spine, a pair of large, internal spines apically, a basolateral plate with many short spines and an apicomesal membranous lobe bearing sclerotized projections. Type material.—Holotype, 6, Panama: Bocas del Toro Province; Miramar [9°N; 82°15’W], 21-27 Feb 1979, H. Wolda (DGD, to be deposited in UCD). Paratypes: Same data, but 15-21 Nov 1978, 1 4 (NMNH); 28 Feb-6 Mar 1979, 1 6 (UPP). Smicridea (S.) corralita, new species Figs. 22-25 The species is related to S. cholta Flint (1974a, figs. 90-93) and is distinguished by the male genitalia. In corralita the tenth ter- gite is shorter and broader in dorsal aspect than in cholta, and the apex is shaped dif- 423 ferently in lateral aspect. The base of the apicolateral lobe of the phallus is angled sharply ventrad in lateral aspect, and the dorsal arm is long and slender, as opposed to being nearly straight ventrally with the dorsal arm almost lost in cholta. Adult. — Length of forewing, 4.0—4.5 mm. Color fuscous, head with silvery hair mes- ally; forewing fuscous with scattered silvery hair basally, with two white bands, distal band arcuate and not quite reaching pos- terior margin, apical fringe white. Male gen- italia (Figs. 22, 23): Ninth segment with an- terior margin produced into a rounded lobe. Tenth tergite narrow, apex upturned in lat- eral aspect; in dorsal aspect lateral margin expanded basally, apex broadly rounded. Clasper with basal segment long, expanded distally; apical segment elongate, apex acute. Phallus (Figs. 24, 25) elongate basally, open apically, with small dorsomesal lobe; apical portion divided mesally into broad lateral plates that are sharply angled ventrad at base, apicodorsal arm long and slender bearing small ventral tooth, ventral arm very short and ending in 2 laterally directed teeth; in- ternally with a pair of long, slender spines. Type material.—Holotype, 6, Mexico: Chiapas State; Corralito, 7 km W. Aba- solo, 21 May 1981, C. M. and O. S. Flint, Jr. (NMNH). Paratype: Same data, 1 ° (NMNH). Smicridea (S.) bulara, new species Figs. 30-33 This species is a member of the S. nigri- pennis group and is similar to the Mexican S. nahuatl Flint (1974a, figs. 86-89). S. bu- lara is distinguished from nahuatl by the upturned apex of the tenth tergite, by the upturned apex of the ventral arm of each ventrolateral phallic lobe, and by the longer spines in the phallotheca. Adult.—Length of forewing, 4.5 mm. General color of body and wings fulvous in alcohol; forewings with an indication of faint pale band. Spurs of second and third pair of legs heavily setose. Fourth segment of 424 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Figs. 18-25. Male genitalia of Smicridea. 18-21, aurimacula. 18, Lateral view. 19, Ninth and tenth terga and clasper, dorsal view. 20, Phallus, ventral view. 21, Phallus, lateral view. 22-25, corralita. 22, Lateral view. 23, Ninth and tenth terga and clasper, dorsal view. 24, Phallus, ventral view. 25, Phallus, lateral view. maxillary palpus about twice length of sec- _tergite slender, apex curved dorsad; in dor- ond or third segment. Male genitalia (Figs. sal aspect (Fig. 31), posterior margin of ninth 30, 31): Ninth segment with anterior margin tergum dark brown and deeply incised; tenth expanded near base, sternum narrow. Tenth tergites rounded apically; a brown pig- VOLUME 102, NUMBER 2 425 Figs. 26-39. Male genitalia and pheromone glands of Smicridea. 26-29, breviuncata. 26, Lateral view, with ventral view of apex of phallus. 27, Ninth and tenth terga, dorsal view. 28, Pheromone capsule of segment 7, glands extruded. 29, Same, glands not extruded. 30-33, bulara. 30, Lateral view. 31, Ninth and tenth terga, dorsal view. 32, Phallus, ventral view. 33, Phallus, lateral view. 34-39, cuna. 34, Phallus, lateral view. 35, Phallus, lateral view with lateral portion of phallus detached to show translucent process (a), paired endothecal spines (sp), and large membranous mesal lobe. 36, Lateral plate of phallus (b) and mesal tubular process (c). 37, Segment 7 pheromone capsule, gland extruded, ventral view. 38, Segment 7 pheromone glands extruded, lateral view. 39, Segment 6 pheromone capsule, glands extruded, ventral view to left, dorsal view to right. mented line divides tergites into fulvous and translucent portions. Basal clasper segment expanded distally; apical segment slender, obtuse. Phallus (Figs. 32, 33) with dorsal margin expanded, giving rise to a short translucent ventrally curved lobe; ventral lobe divided mesally into broad lateral plates, dorsal arm produced into laterally directed point, ventral arm a large, apically acute lobe curved dorsad, in ventral aspect 426 apex of lobe acute and curved laterad; with pair of long, dark internal spines, each bear- ing a small mesal tooth near midlength. Type material.—Holotype, 6, Trinidad Island: Simla Research Station, 2-15 Jun 1981, W. J. dlansom’ and C."Yf.. Clemons (DGD, to be deposited in CAS). Smicridea (S.) mirama, new species Figs. 40-43 This species is distantly related to S. cuna Flint (1974a, figs. 106-109) and is easily distinguished from it by the male genitalia. The distinctive phallus has long, slender, ventrolateral plate with reflexed apices in both lateral and ventral aspects. Adult. — Length of forewing, 4.0—4.5 mm. Color brown in alcohol; forewing denuded, membrane with pale band from stigma. Male genitalia (Figs. 40, 41): Ninth segment with anterior margin produced into a rounded lobe. Tenth tergite narrow, apex slightly upturned in lateral aspect; in dorsal aspect base expanded laterally, apex broad- ly rounded with small mesal indentation. Clasper with basal segment long, expanded distally; apical segment elongate, apex acute. Phallus (Figs. 42, 43) elongate basally, open apically, with a dorsally sclerotized, dor- somesal appendage; ventrolateral process long and slender, with apex reflexed dor- solaterally; endotheca with 2 long and near- ly straight internal spines, and centrally an irregular sclerotized band, bifurcate apical- ly. Type material.—Holotype, 6, Panama: Bocas del Toro Province; Miramar [9°N; 82°15'W], 14-20 Feb 1979, H. Wolda (DGD, to be deposited in UCD). Paratypes: Same Locality: 3 6; 18-24 Oct 1978, 1 4; 15-21 Nov 1978, 3 6; 20-26 Dec 1978, 8 6; 10-16 Jan 1979, 3 6; 7-13 Feb 1979, 4 6; 21-27 Feb 1979, 12 6; 28 Feb 6—Mar 1979, 11 6; 7-13 Mar 1979, 19 6; 14—20 Mar 1979, 8 8; 9-15 May 1979, 13 4; 16—- 22 May 1979, 11 6; 23-29 May 1979, 7 6; PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 22-28 Aug 1979, 2 4; 10-16 Oct 1979, 16 (DGD, NMNH, UCD, UPP). Smicridea (S.) filicata, new species Figs. 44-47 Smicridea undescribed sp. ““B”’: McElravy, etal. LOST SS: Smicridea filicata, S. mirama and S. ulva Flint (1974a, figs. 102-105) are closely re- lated. Each has a phallus with an elongate dorsomesal structure, a pair of ventrolateral spines, and the ventrolateral margins pro- duced into one or two long processes. In both filicata and ulva the ventrolateral mar- gins of the phallus are produced into two pairs of processes; in mirama there is only one pair. In filicata the dorsalmost process of each pair is much longer than the ven- tralmost and its apex is sharply hooked lat- erad. In u/va the ventralmost process slight- ly surpasses the dorsalmost, and neither are sharply hooked apicad. Adult. — Length of forewing, 4 mm. Color fuscous, appendages paler, frons with white setae; forewing mostly denuded, a white band at stigma, possibly a pale band basally. Male genitalia (Figs. 44, 45): Ninth segment with anterior margin produced into a rounded lobe. Tenth tergite in lateral aspect narrow, apex angled dorsad; in dorsal aspect with apex rounded. Clasper with basal seg- ment long, expanded distally; apical seg- ment elongate, apex acute. Phallus (Figs. 46, 47) elongate basally, open apically, with a declivous, dorsomesal appendage; with two ventrolateral processes on each side, ven- tralmost short and acute, dorsalmost longer with apex sharply hooked laterad; endo- theca with two long, nearly straight internal spines, and centrally with long, lightly sclerotized lobe, weakly divided on the mid- line. Type material. — Holotype, 3, Costa Rica: Puntarenas Province; Rio Singri (9.057°N; 83.082°W), ca. 2 km (air) S. Finca Hele- chales, 720 m, 21 Feb 1986, Holzenthal, VOLUME 102, NUMBER 2 427 46 Figs. 40-47. Male genitalia of Smicridea. 40-43, mirama. 40, Lateral view. 41, Ninth and tenth terga and clasper, dorsal view. 42, Phallus, ventral view. 43, Phallus, lateral view. 4447, filicata. 44, Lateral view. 45, Ninth and tenth terga and clasper, dorsal view. 46, Phallus, ventral view. 47, Phallus, lateral view. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 428 “MOTA [RIJUDA “ATUO / JUSUISES JO soINjon.s sUIeS “Gh “MOTA [e191] “/ PUL 9 S]USWdas jo ‘spue]s popniixe puke sofnsdes suoWIOIOY ‘Bp “7 OOT = SUT] [eS ‘DUND VaplUgIWG Jo sydeIBOIOTUN UOI}99J9 SUTUULIS “6 p—-8p “SBI ~ 4 ~~ 3~. <* S “»*¥ a» we a VOLUME 102, NUMBER 2 Morse and Fasth (NMNBH). Paratype: Same data, 1 6 (UMSP). Panama: Chiriqui Prov- ince; Fortuna Dam Site [8°44’N, 82°16’ W], 23-29 Nov 1977 H. Wolda, 1 é(NMNH); same, but 28 Dec 1977-3 Jan 1978, 1 4 (OPP): Smicridea (S.) cuna Flint Figs. 34-39, 48, 49 Smicridea (S.) cuna Flint 1974a:23. This somewhat variable species is abun- dant in central Panama. Minor differences in the male genitalia, especially the phallus (Flint 1974a, figs. 108, 109), are figured here. The pheromone glands (Figs. 37-39, 48, 49) are referred to as “reticulated bodies” in the literature. The phallus (Figs. 34, 35) has an enlarged base and a dorsal margin that is produced into a ventral curved translucent process (a). Ventrad to this process is a small structure with only the acute apex discernable. Be- neath it are a pair of darkly pigmented, api- cally curved endothecal spines directed pos- terioly (sp). The ventral portion of the endotheca (Figs. 35, 36) consists of a large membranous lobe containing small, dark pigmented sclerites (possibly the phallotre- mal sclerites), which are hidden in lateral aspect by the brown pigmented lateral plate (b). The mesal surface of plate (b) gives rise to a slender, tubular, opaque lobe (c). Figs. 37-39, 48, 49 show the paired pher- omone glands of segment 6 and segment 7 extruded through inter-segmental mem- branes. Segment 7 pheromone glands (Figs. 37, 38, 49) are covered with minute silver- colored spinules. The glands originate from internal surface of a vase-like capsule with a lacelike and irregular external membrane. Segment 6 pheromone glands, extruded through intersegmental membrane 6-7, are smaller, but are also densely covered with silver spinules (Fig. 39). Material examined. —Panama: Canal Zone; Lion Hill Island, 27 Nov 1981, R. B. Kimsey, | 6; 27 Oct 1981, 1 6; Puma Island, 429 20 Nov 1981, R. B. Kimsey, 1 6; Juan Gal- legos Island, 27 Nov 1981, R. B. Kimsey, 11 6; Barro Colorado Island, Mar 1963, R. D. Akre, 16; 13 Mar 1963, Malaise Trap, R. D. Akre 2 6; Mar 1963, 7 4, 1 9; 21 May 1980, Henk Wolda, 1 ¢(DGD, UCD, WSU). Smicridea (S.) circinata, new species Figs. 50-53 The species is closely related to S. tur- rialbana Flint (1974a, figs. 94-97) with which it co-exists at the Miramar site. Di- agnostic characters are recognized only in the phallus. In circinata a pair of large dorsal processes arise from the phallus. The apex of the ventral process is not hooked laterad, and the basolateral spine is larger and more curved than in S. turrialbana. Adult. —Length of forewing, 3.5—-4.0 mm. Color brown in alcohol; forewing denuded, membrane with a pale transverse mark at stigma. Male genitalia (Figs. 50, 51): Ninth segment with anterior margin produced into a rounded lobe. Tenth tergite in lateral as- pect short, broad, with dorsal, subapical point; in dorsal aspect expanded laterally at base, narrowed apically with mesal inden- tation. Clasper with basal segment long, ex- panded distally; apical segment elongate, apex acute. Phallus (Figs. 52, 53) elongate basally, open apically; apex with a pair of large dorsal spines gradually curving later- ad, ventral lobe produced into a pair of pro- cesses curving dorsad, pair of curved baso- lateral spines ventrally, endotheca membranous with indistinct mesal sclero- tization. Type material.—Holotype, ¢, Panama: Bocas del Toro Province; Miramar [9°N; 82°15’'W], 14-20 Feb 1979, H. Wolda (DGD, to be deposited in UCD). Paratypes: Same data 18-24 Oct 1978, 1 6; 15-21 Oct 1978, 14 6; 29 Nov—5 Dec 1978, 3 6; 20- 26 Dec 1978, 1 6; 10-16 Jan 1979, 2 6; 7- 13 Feb 1979, 1 6; 21-27 Feb 1979, 11 6; 28 Feb—6 Mar 1979, 31 6; 7-13 Mar 1979, 4 6; 14-20 Mar 1979, 3 6; 16-22 May 1979, 430 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Figs. 50-56. Male genitalia of Smicridea. 50-53, circinata. 50, Lateral view. 51, Ninth and tenth terga and clasper, dorsal view. 52, Phallus, ventral view. 53, Phallus, lateral view. 54-56, turrialbana. 54, Phallus of holotype, lateral view. 55, Phallus of specimen from Miramar, Panama. 56, Phallus of specimen from Quebrada Grande, Costa Rica. VOLUME 102, NUMBER 2 5 6; 23-29 May 1979, 8 6; 4-10 Jul 1979, 3 4; 22-28 Aug 1979, 2 6; 10-16 Oct 1979, 3 6 (DGD, NMNH, UCD, UPP). Smicridea (S.) turrialbana Flint Figs. 54—56 Smicridea (S.) turrialbana Flint 1974a:22. We have seen material of this species from four widely separated localities in Costa Rica and Panama. There are three different forms of the dorsolateral point of the phallus. In the holotype from Turrialba, Costa Rica, the point is barely developed (Fig. 54). In the material from Miramar, Panama, the point is developed into a strong spine (Fig. 55), and in the examples from Quebrada Grande and Reserva Forestal San Ramon, Costa Rica, the point is produced into a hook-like process directed vertically (Fig. 56). The remainder of the genitalia do not appear to be significantly different. We be- lieve this to be variation in a single species and predict that examples from other lo- calites will also differ in the development of the dorsolateral point. Material examined. —Costa Rica: Carta- go Province; 3 mi W Turrialba, 18-21 Jun 1967, Flint and Ortiz, holotype 6 (NMNH); Guanacaste Province; Quebrada Garcia (10.862°N; 85.428°W), 10.6 km ENE Que- brada Grande, 470 m, 8 Mar 1986, Hol- zenthal and Fasth, 1 6 (NMNH); Alajuela Province; Rio San Lorenzo and tribs. (10.192°N; 84.510°W), Reserva Forestal San Ramon, 1090 m, 2-4 Jul 1986, Holzenthal, Heyn and Armitage, 6 6 (NMNH, UMSP). Panama: Bocas del Toro Province; Mira- mar [9°N; 82°15’W], 14-20 Feb 1979, H. Wolda, 2 6 (UCD, NMNH). Smicridea (S.) holzenthali, new species Figs. 57-64 This unusual species appears to be dis- tantly related to S. turrialbana. In holzen- thali the internal plate and spine of the phal- lus are greatly reduced to a small dorsal tooth 431 and a slightly curved ventral spine, neither extending beyond the margin of the phallus. The rodlike ventrolateral processes of the phallus are flat and broad in holzenthali. Adult. —Length of forewing, 4 mm. Color fuscous, appendages paler; frons white; forewing fuscous, with two white bands one at stigma, the other halfway between first band and wing base. Male genitalia (Figs. 57, 58): Ninth segment with anterior margin produced into a rounded lobe. Tenth tergite narrow, with upturned apex in lateral as- pect; in dorsal aspect, apex obliquely trun- cate. Clasper with basal segment long, ex- panded distally; apical segment elongate, apex acute. Phallus (Figs. 59, 60) elongate basally, open apically, with a small dorso- mesal appendage; ventrolateral plates long and broadened distally, each bearing a short hook apicodorsally; internal plate small, terminating in a slightly curved ventral spine and a short, erect, dorsal spine. Type material. —Holotype, 6, Costa Rica: Guanacaste Province; Rio Tizate (10.773°N; 85.449°W), 7.2 km NE Canas Dulces, 275 m, 28 Jun 1986, Holzenthal, Heyn and Ar- mitage (NMNH). Paratype: Same data, 1 4 (NMNH). Smicridea (S.) latipala, new species Figs. 61-64 This species is related to both S. campana Flint (1974a, Figs. 128-131) and S. sirena Bueno (1986, figs. 7-9) on the basis of the undivided, apicoventral lobe of the phallus. It is distinguished from both species in the details of the phallic structure. Only in /a- tipala does the phallus bear internally two pairs of long, slender spines, a mesal, un- paired structure, and a broadly rounded apex on the phallus, in ventral aspect. Adult. —Length of forewing, 5.5 mm. Col- or uniformly fuscous in alcohol. Male gen- italia (Figs. 61, 62): Ninth segment with an- terior margin produced into a narrowly rounded lobe. Tenth tergite narrow, apex upturned in lateral aspect; in dorsal aspect 432 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 64 Figs. 57-64. Male genitalia of Smicridea. 57-60, holzenthali. 57, Lateral view. 58, Ninth and tenth terga and clasper, dorsal view. 59, Phallus, ventral view. 60, Phallus, lateral view. 61-64, Jatipala. 61, Lateral view. 62, Ninth and tenth terga and clasper, dorsal view. 63, Phallus, lateral view. 64, Phallus, ventral view. VOLUME 102, NUMBER 2 apex broadly rounded. Clasper with basal segment long, expanded distally; apical seg- ment elongate, apex acute. Phallus (Figs. 63, 64) elongate basally, open apically; apex produced into single broadly rounded lobe beneath endotheca; internally bearing pair of long, dark spines dorsally, another pair of pale spines ventrally, and a single, shorter mesal process. Type material.—Holotype, ¢, Panama: Chirigqui Province; Guadalupe Arrriba (8°52'26"N; 82°33'13”W), 2200 m, 18-24 Apr 1984, H. Wolda, in light trap 20 m above ground (NMNH). Paratypes: Same data, 2 6, 1 2(NMNH); same, but 2-8 May 1984, 1 6, 1 2 (UPP); same, but 6-12 Feb 1985, 1 2 (NMNH); same, but 17-23 Apr 1985, 1 6 (NMNH); same, but 24-30 Apr 1985, 1 2 (NMNH); same, but 8-14 May 1985, 1 6, 1 2 (UPP); same, but 22—28 May 1985, 1 6 (NMNH); same, but 12-18 Jun 1985, 1 2 (NMNH); same, but 19-25 Jun 1985, 1 é (NMNH). Acknowledgments Thanks are given for loan of specimens by R. D. Akre, Washington State Univer- sity; E. H. Sugden, R. D. Schuster and R. B. Kimsey, University of California, Davis: W. J. Hanson, Utah State University; and R. W. Holzenthal, University of Minnesota. We also thank Eric P. McElravy, University of California, Berkeley for his work locating the material of Smicridea “A” and “‘B.” Henk Wolda, Smithsonian Tropical Re- search Institute, Panama made his light trap collections from Fortuna, Guadalupe Ar- riba, Miramar and Barro Colorado Island available to us for study. Discussions of the site and collecting methods at Fortuna are found in McElravy et al. (1981), at Miramar in Wolda & Flowers (1985) and Barro Col- orado Island in Wolda (1982). Thanks are extended to R. D. Schuster for the SEM photographs. 433 Literature Cited Bueno Soria, J. 1986. Estudios en insectos acuaticos VII: Cinco nuevas especies de Trichopteros de Mexico y Costa Rica (Trichoptera: Hydro- psychidae).— Folia Entomologica Mexicana 68: 53-65. Flint, O. S., Jr. 1968. Bredin-Archbold-Smithsonian Biological Survey of Dominica, 9. The trichop- tera of the Lesser Antilles.— Proceedings of the United States National Museum 125 (3665):1- 60. 1974a. Studies of neotropical caddisflies, XVII: The genus Smicridea from North and Central America (Trichoptera: Hydropsychi- dae).—Smithsonian Contributions to Zoology 167:1-65. . 1974b. The trichoptera of Surinam. — Studies on the Fauna of Suriname and other Guyanas 14 (55):1-151. 1981. Studies of neotropical caddisflies, XXVIII: The Trichoptera of the Rio Limon Ba- sin, Venezuela.—Smithsonian Contribution to Zoology 330:1-61. 1989. Studies of neotropical caddisflies, XXXIX: The genus Smicridea in the Chilean subregion (Trichoptera: Hydropsychidae).— Smithsonian Contributions to Zoology 472:1- 45. McElravy, E. P., V. H. Resh, H. Wolda, & O. S. Flint, Jr. 1981. Diversity of adult Trichoptera in a ““non-seasonal”” tropical environment.—Pro- ceedings of the 3rd International Symposium on Trichoptera: 149-156. Wolda, H. 1982. Seasonality of Homoptera at Barro Colorado Island. Pp. 319-330 in E. G. Leigh, Jr., A. S. Rand, & D. M. Windsor, ed., The ecology of a tropical forest: seasonal rhythms and long-term changes. Smithsonian Institution Press, Washington, D.C. —. & R. W. Flowers. 1985. Seasonality and di- versity of Mayfly adults (Ephemeroptera) in a ““nonseasonal” tropical environment.— Biotro- pica 17: 330-335. (OSF) Department of Entomology, NHB 105, Smithsonian Institution, Washington, D.C. 20560; (DGD) 2016 Donald Drive, Moraga, California 94556. Dr. Denning died on February 7, 1988 while this paper was in the final review stages. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 434-446 A REVIEW OF THE SHORE-FLY GENUS POLYTRICHOPHORA CRESSON FROM ASIA (DIPTERA: EPHYDRIDAE) Wayne N. Mathis and Jin Zuyin Abstract.— Asian shore flies of the genus Polytrichophora Cresson are re- viewed. Included are four previously described species (P. brunneifrons (Mei- jere), P. canora Cresson, P. duplosetosa (Becker), and P. pollinosa Miyagi). The tribe Discocerinini is characterized and a key to Asian discocerinine genera is provided; the monophyly of Polytrichophora is established, and a key to species occurring in the Palearctic and Oriental regions is presented, including P. or- bitalis (Loew), which was reported to occur in north Africa (we have not seen specimens of this species from the Old World, however, and doubt its occur- rence there). Polytrichophora luteicornis Cresson is determined to be a junior synonym of P. canora Cresson. All Asian species treated are redescribed, and characters of the male genitalia are illustrated. This is the second paper of a series on the Ephydridae or shore flies of Asia with em- phasis on species that occur in China. The first paper was on the genus Lamproscatella Hendel (Mathis & Zuyin 1988). The purposes of this paper are twofold: First, we present an overview of the tribe Discocerinini, including a key to genera that are found or are reported to occur in Asia. Second, we review the genus Polytricho- phora Cresson, one of the genera of Dis- cocerinini, from the same geographic area. As part of the latter study, we have exam- ined all primary types of species that have been reported to occur in Asia, and for each species, illustrations of the male genitalia are provided. With the exceptions to be not- ed below, these are the first illustrations of these species. Previous papers on Asian species of Poly- trichophora are mostly of limited scope, usually isolated descriptions as part of fau- nistic reviews. No comprehensive treat- ment exists for the Asian species, although Cresson (1945) did provide a list of species occurring in the Indoaustralian region. That list included a complete synonymy, and for some species, brief remarks, alluding to the generic placement of the species or a no- menclatural issue. More recently, Miyagi (1977) treated the Japanese fauna, which included two species of Polytrichophora, and the figures he produced were the first avail- able for these taxa. Two other important works are the fairly recent catalogs of the Oriental (Cogan & Wirth 1977) and the Palearctic (Cogan 1984) components of the Asian fauna. The catalogs provide a listing of species, primary references, and an out- line of their distributions. In this paper, we adhere generally to the methods and descriptive terminology that were used in the first paper of this series (Mathis & Jin 1988). For each species treat- ed in this study, we have noted, as appro- priate, its descriptive and nomenclatural history as part of the synonymy. Specimens for this study came primarily from the col- lections of the Academy of Natural Sciences of Philadelphia (ANSP), the Smithsonian Institution (USNM), Washington, D.C., and the Northwestern Teachers College (NTC), Lanzhou, Gansu Province, China. Sexes are similar, so descriptions are based on both VOLUME 102, NUMBER 2 sexes except for male genitalia. The termi- nology we have used for structures of the genitalia is as indicated on Figs. 6-9. Five cephalic and two venational ratios are used commonly in the descriptions; these are de- fined here for the convenience of the user. Head ratio: Head height/head width. Both measurements are the greatest dimensions of the head from an anterior view. Frontal ratio: Frons height/frons width. The width measurement is the straight line distance between the median margins of the compound eyes at the level of the anterior ocellus; the height measurement is the dis- tance from the anterior margin of the frons to a “‘line”’ through the posterior ocelli. Facial ratio: Face height/face width. The height measurement is the distance between the oral margin and the dorsum of the fron- tal suture; the width measurement is the narrowest distance between the compound eye across the face. Eye ratio: Eye height/eye width. Both measurements are the greatest dimensions as taken from a lateral view. Eye-to-cheek ratio: genal height/eye height. Both measurements are the greatest dimensions as taken from the head in lateral view. Costal vein ratio: The straight line dis- tance between the apices of R,,3; and R,,;/ distance between the apices of R, and R,, 3. M vein ratio: The straight line distance along vein M between crossveins (dm-cu and r-m)/distance apicad of dm-cu. Tribe Discocerinini Diagnosis.—Small to moderately small shore flies, length 1.25 to 3.5 mm; usually invested with considerable microtomen- tum, especially frons and mesonotum. Head: Ocellar setae inserted anterior to level of anterior ocellus, sometimes only slightly so; reclinate fronto-orbital seta in- serted anterior to proclinate fronto-orbital (if two proclinate fronto-orbitals present, inserted in front of the larger one); posto- cellar setae well developed, proclinate, and 435 slightly divergent, usually at least one-half length of ocellar setae; arista with from five to seven dorsally branching rays; face not conspicuously pitted or rugose; gena, in- cluding midportion, bearing setulae, its pos- terior (postgenal) margin rounded. Thorax: Mesonotum generally microto- mentose, usually densely so, although with some variation; supra-alar seta usually ev- ident although sometimes reduced; acros- tichal setae arranged in about 8 irregular rows; prescutellar acrostichal setae approx- imate and inserted behind level of poste- riormost dorsocentral setae; scutellum usu- ally densely setulose; both anterior and posterior notopleural setae inserted at about the same level. Abdomen: Male genitalia: surstyli not ev- ident, apparently lost or fused indistin- guishably with the ventral margin of the epandrium. Key to Asian Genera of the Tribe Discocerinini 1. Notopleuron with scattered setulae in addition to two larger setae .... 2 — Notopleuron setulae absent, with only the two larger setae ......... 3 2. Facial setae arranged in two dor- soventral series, secondary series of dorsolateroclinate setae laterad of inclinate primary series; eye densely invested with microscopic setulae eV aLIge TH OBIS Polytrichophora Cresson — Facial setae arranged in one series; eye at most with sparse, scattered microscopic setulae Ee RS POETS Discocerina Macquart 3. Supra-alar seta well developed, longer than posterior notopleural seta; face with an upcurved seta at lower lateral extremity AP OB F) he SEIS Diclasiopa Hendel — Supra-alar seta weak or absent, if present, distinctly shorter than pos- terior notopleural seta; face lacking upcurved seta at lower lateral ex- tremity 436 4. Hind tibia bearing spurlike, preapi- cal seta ventrally; facial series com- prised of from two to three large se- tae; dorsal seta inserted slightly medially and arising from distinct, shining papilla, with a small, slightly anaclinate seta laterad of dorsal seta; generally microtomentose, cinere- ous species, appearing dull side ee ra tah te Hecamedoides Hendel — Hind tibia lacking spurlike, preapi- cal seta; facial series comprised of two large setae, dorsal seta not aris- ing from a shining papilla and lack- ing a smaller seta laterad of dorsal seta; mostly sparsely microtomen- tose, shining to subshining species Ditrichophora Cresson ee © © ce © eo 8 © © © © © © © © © © © Polytrichophora Cresson Polytrichophora Cresson, 1924:161. Type species: Polytrichophora agens Cresson, 1924:161, orig. des. —Cogan and Wirth, 1977:327-—238 [Oriental catalog].—Co- gan, 1984:137-138 [Palearctic catalog]. Diagnosis. —Small to moderately small shore flies, length 1.25—3.0 mm; generally densely microtomentose, grayish species. Head: Eye conspicuously microsetulose; facial setae usually comprising eight setae, these generally decreasing in size from top to bottom, appearing as two series due to divergent orientation of setae in series; setae of primary series inclinate (setae 1, 2, 5, and 7), generally larger than setae of secondary series except for seta 2, which is much re- duced and inserted laterad and sometimes slightly ventrad of seta 1, seta 1 largest of all facials, inclinate (cruciate with opposite seta), but not arising from shining papilla; setae of secondary series oriented dorsolat- erally to laterally (setae 3, 4, 6, and 8), usu- ally smaller than setae of primary series; face lacking a distinctly anaclinate seta at ventral extremity; parafacial narrow to moderately wide, with or without setulae; gena generally low. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Thorax: Notopleuron bearing numerous setulae in addition to two larger setae; an- terior notopleural seta inserted conspicu- ously closer to posterior notopleural seta than to postpronotal seta; supra-alar seta reduced, about one-half length of postalar seta. Abdomen: Fourth tergum of male only slightly longer than third. Male genitalia with cerci fused ventrolaterally to median mar- gin of epandrium. Distribution. — This is one of the few gen- era of Ephydridae that occurs worldwide, and with approximately the same species diversity in each region, whether temperate or tropical. A dozen new species have been segregated from the neotropics (Mathis, in preparation), however, which, would make that region by far the richest in species. Natural history. —Specimens of Poly- trichophora are usually associated with mud- shore and sand-shore habitats (Deonier 1965) or rarely with a marsh-reed habitat (Scheiring & Foote 1973). We usually found the greatest diversity and abundance when collecting on mud and sandy shores that had a matlike covering of algae. Discussion. — Polytrichophora, along with Discocerina and Hydrochasma Hendel (New World), form a monophyletic lineage within the Discocerinini. An apomorphy to sub- stantiate the monophyly of this group is the setulose notopleuron. In other genera of the subfamily Psilopinae, the notopleuron is bare except for an anterior and a posterior seta, both of which are inserted near the ventral margin. In Polytrichophora, Hydro- chasma, and Discocerina, however, the notopleuron bears a few additional setulae that are usually inserted slightly dorsad and toward the anterior portion of the pleuron, usually around the anterior notopleural seta. Polytrichophora may be distinguished from Discocerina or Hydrochasma by the sec- ondary “‘series’”’ of facial setae (see generic description), a character that is unique to this genus and establishes its monophyly. Its relationship to Discocerina and Hydro- VOLUME 102, NUMBER 2 437 Figs. 1-5. lateral view. 3. Fifth sternum and hypandrium, ventral view. 4. Aedeagal apodeme and aedeagus, lateral view. 5. Aedeagus, dorsal view. chasma is not resolved, however; either or both of these genera could be paraphyletic and include Polytrichophora as a sublineage. In the following key, we have included all species that are reported to occur in the Palearctic and Oriental Regions. One species, P. orbitalis (Loew), which was de- scribed from specimens collected in North America, was reported to occur in North Africa (Cogan 1984). We have not con- firmed this, having studied no specimens that are conspecific with P. orbitalis from North Africa. In the event that this species Polytrichophora orbitalis. 1. Epandrium and cerci, posterior view. 2. Epandrium and left cercus, does occur there, we have included it in the key and have also provided figures of the male genitalia (Figs. 1-5) based on speci- mens from North America. Key to Palearctic and Oriental Species of Polytrichophora 1. Mesonotum mostly brown, but brown coloration extended laterally only to level of posterior dorsocen- tral setae, thereafter with gray-col- ored microtomentum in a broad lat- 438 eral stripe; membranous aedeagal flap closely appressed to aedeagus; ventral margin of epandrium short and broad in lateral view (Europe and’ ASia)i).2).4 - P. duplosetosa (Becker) — Mesonotum more extensively brown colored, brown coloration extended laterally to level of supra-alar setae, gray-colored areas restricted to ex- treme lateral and anterior margins; membranous aedeagal flap, if pres- ent, separated from aedeagus except at base; ventral margin of epan- drium long and narrow in lateral view 2. Face narrow, facial ratio averaging 0.75; fore femur with ventral flexor setulae longer than width of fore tib- ia at midlength; aedeagus lacking membranous flap at apex (North America, ? North Africa) (Figs. 1- 2D) he a) yer 2” dom P. orbitalis (Loew) — Face narrow, facial ratio averaging less than 0.60; fore femur with ven- tral flexor setulae shorter than width of fore tibia at midlength; aedeagus with apical, membranous flap .... 3 3. Fore coxa extensively invested with whitish gray to gray microtomen- tum, yellowish coloration faint; fore femur with a posteroventral row of 6—7 spine-like setae (Japan) kiione nea el ee P. pollinosa Miyagi — Fore coxa mostly yellow; fore femur with a posteroventral row of only 4— 5 spine-like setulae 4. Length of ventral process of epan- drium short, equal to one-fifth width of epandrium; aedeagus 3.5 x as long as wide; aedeagal apodeme sub- triangular ... P. brunneifrons (Meijere) — Length of ventral process of epan- drium long, narrow, digitiform, equal to 2 width of epandrium; ae- deagus 5 x as long as wide; aedeagal apodeme subrectangular P. canora Cresson PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Polytrichophora brunneifrons (Meijere) Figs. 6-10 Discocerina brunneifrons Meijere, 1916:270. Polytrichophora brunneifrons. —Cogan & Wirth, 1977:327-—328 [generic placement; Oriental catalog].—Cogan 1984:137 [Palearctic catalog]. Description.—Small shore flies, length 1.25 to 1.75 mm (holotype 1.72 mm). Head: Head ratio averaging 0.85. Frons rectangular, frontal ratio averaging 0.70, generally microtomentose, microtomentum tan; ocellar triangle more densely microto- mentose than remainder of frons; parafrons black, slightly orangish red along anterior margin; anterior fronto-orbital plate with very narrow white band immediately ad- jacent to eye; ocellar setae inserted slightly in front of anterior ocellus. Antennae most- ly orange, but dorsal surface of pedicel and lst flagellomere partially blackish; arista with 5 dorsally branching rays. Face densely invested with grayish to slightly bluish white microtomentum; parafacial setulae hair-like; parafacials lightly yellowish but becoming whitish; gena white and densely microto- mentose. Eye ratio averaging 0.70; eye-to- cheek ratio averaging 0.11. Palpus yellow. Thorax: Mesonotum densely microto- mentose, mostly light brown but postpro- notum, notopleuron, pleural sclerites whit- ish to silvery gray. Fore coxa yellow; femora yellow, invested with grayish microtomen- tum except for base and apex; tibiae and tarsi yellowish, apical tarsomere usually slightly darker, brownish; fore femur with a posteroventral row of 4 stout but acutely pointed setae. Wing hyaline; costal vein ra- tio averaging 0.80; M vein ratio averaging 0.52. Halter yellowish. Abdomen: Dorsum generally unicolor- ous, brown, darker than coloration of meso- notum and very slightly shining. Length of 5th tergum of male nearly 1.5 x that of 4th; 5th sternum (Fig. 8) with anterior margin rounded, lateral arms connected broadly at VOLUME 102, NUMBER 2 oe epandrium f\ é o ° aedeagal apodeme aedeagus on SS 9 membranous flap 439 5th sternum 0.045mm ee | 10 Figs. 6-10. Polytrichophora brunneifrons. 6. Epandrium and cerci, posterior view. 7. Epandrium and left cercus, lateral view. 8. Fifth sternum and hypandrium, ventral view. 9. Aedeagal apodeme and aedeagus, lateral view. 10. Aedeagus, dorsal view. base, base not interrupted medially. Male genitalia (Figs. 6—10) as follows: Epandrium (Figs. 6—7) more or less elliptical in posterior view, dorsal margin rounded, ventral mar- gin reduced as 2 short, sinuate (in posterior view), pointed processes, the length of which is Slightly less than greatest width of a cercus in posterior view; aedeagus (Figs. 9-10) about 5 x as long as width at middle, broad- er basally and with distinct taper at base and apex, apex pointed and bearing a nar- row, membranous flap that generally folds back under aedeagus, flap about *%4 length of aedeagus; aedeagal apodeme somewhat tri- angular, dorsal process short; posterior arms of hypandrium (Fig. 8) widely separated and nearly 74 total length of hypandrium, ante- rior margin with shallow but wide emargi- nation. Type material. —The holotype female of Discocerina brunneifrons is labeled “K. Ja- cobson Wonosobo Java [Indonesia] Mei 1909/9 29/927-929 op modderig grindban- ken langs stroomen[?] water. [handwritten and barely legible, = on mud and gravel banks along flowing water]/Clasiopa brunneifrons det. de Meijere. Type [black submargin; species name and “‘type”’ handwritten]/HO- LOTYPE [red with black border]/HOLO- TYPE 2 Discocerina brunneifrons de 440 M[eijere]. det. B. H. Cogan 1971 [all but “det. B. H. Cogan 197” handwritten]/Poly- trichophora brunneifrons meij[ere] det. B. H. Cogan 1973 [all but “det. B. H. Cogan 197° handwritten]/Polytrichophora brun- neifrons (Meij[ere].) WWirth 74 [black sub- margin; all but ““WWirth” handwritten].” The holotype is double mounted (minute nadel in rectangular block of foam plastic), is in good condition, and is deposited in the Instituut voor Taxonomische Zodlogie, Universiteit van Amsterdam, The Nether- lands. Distribution. —Oriental: India (Assam), Malaysia (Selangor), Pakistan (Dhamyal), and Thailand (Bangkok, Chiengmai, Chol- buri, Khon Kaen, Udon Thani). Several other records listed in Cogan and Wirth (1977), mostly from countries not listed above, have not been confirmed. Remarks. —The description above is based primarily on the holotype of P. brun- neifrons, which is a female. The illustrations of the male genitalia are from a specimen that was collected in Thailand (Khon Kaen Province, Meung District). Polytrichophora canora Cresson, revised status Figs. 11-15 Polytrichophora canora Cresson, 1929:165; 1945:62 [review of Indoaustralian species]|.—Cogan & Wirth, 1977:328 [Oriental catalog; as a synonym of P. brunneifrons}. Polytrichophora luteicornis Cresson, 1929: 166; 1945:62 [review of Indoaustralian species]|— Miyagi, 1977:20 [review, Ja- pan].—Cogan & Wirth, 1977:328 [Ori- ental catalog; as a synonym of P. brun- neifrons|. New Synonym Description. —Small shore flies, length of males averaging 1.15 mm (1.0-1.30 mm), females averaging 1.35 mm (1.15—1.55 mm); body mostly bronze colored but with some whitish gray microtomentum laterally; fore femur with 4—5 short, stout setae along api- cal half of posteroventral surface. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Head: Head ratio averaging 0.84. Frons rectangular, frontal ratio averaging 0.71 (males) or 0.73 (females), subshining with a sparse whitish gray microtomentum; parafrons black, partially golden to yellow- ish or slightly greenish dorsally; mesofrons, fronto-orbital plate, and ocellar triangle golden brown, sometimes slightly greenish; ocellar setae inserted slightly in front of or aligned immediately laterad of anterior ocellus. Antennae mostly yellow, dorsal sur- face of pedicel and 1st flagellomere black; arista with five dorsally branching rays. Face bearing three pairs of primary and four pairs of secondary facial setae; parafacial setulae hair-like; parafacials and gena ochraceous, with silvery microtomentum, microtomen- tum becoming denser on gena. Eye ratio averaging 0.74; eye-to-cheek ratio averag- ing 0.097. Palpus yellow. Thorax: Mesonotum mostly bronze col- ored, but with whitish gray microtomentum anteriorly and laterally; pleura brown, with densely whitish gray microtomentum. Fore coxa yellow, brownish basally; femora brown except base of fore femur yellow; tib- iae mostly yellow but brownish in median part; tarsomeres 1-4 yellow, Sth brownish; fore femur with 4—5 short, stout, black setae along apical half of posteroventral surface. Wing hyaline; costal vein ratio averaging 0.84; M vein ratio averaging 0.50. Halter yellowish. Abdomen: Dorsum generally concolor- ous with mesonotum but with whitish gray microtomentum laterally and posteriorly. Length of 5th tergum of male nearly 1.5 x that of 4th; 5th sternum (Fig. 13) with an- terior margin truncate. Male genitalia (Figs. 11-15) as follows: Epandrium (Figs. 11—12) in posterior view oval except for ventral processes; dorsal margin of epandrium rounded; ventral process of epandrium elongate, length greater than width of cer- cus, parallel sided; aedeagus (Figs. 14-15) 5x longer than wide, broader basally, ta- pered irregularly to apex; aedeagal flap ex- tended laterally from apex, length about two- thirds that of aedeagus; aedeagal apodeme VOLUME 102, NUMBER 2 441 Figs. 11-15. Polytrichophora canora. 11. Epandrium and cerci, posterior view. 12. Epandrium and left cercus, lateral view. 13. Fifth sternum and hypandrium, ventral view. 14. Aedeagal apodeme and aedeagus, lateral view. 15. Aedeagus, dorsal view. (Fig. 14) subrectangular, dorsal process short; posterior arms of hypandrium (Fig. 13) about one-half total hypandrial length, anterior margin mucronate. Type material.—The holotype female of Polytrichophora canora is labeled ‘‘Tai- nan[,] 909.II./Formosa Sauter/1115/TYPE No. 6330[,] Polytrichophora Canora 2 E. T. Cresson, Jr, [pink; number and species name handwritten].’> The holotype is double mounted (minute nadel in rectangular foam block), is in good condition, and is depos- ited in the ANSP (6330). The holotype female of Polytrichophora luteicornis is labeled ‘‘Singapore[,] BirOf[,] 1898/6 [sic]/Property of Hung [handwrit- ten] Loaned [pink]/Type No. Polytricho- phora Luteicornis E. T. Cresson, Jr, [dark pink; species name handwritten].’’ The ho- lotype is double mounted (minute nadel in rectangular form block), is in poor condition (pin obscures several structures), and is presently deposited in the ANSP. Distribution. —Oceania: Belau (Pelau); Federated States of Micronesia (Yap Is- lands, Caroline Islands); Solomon Islands (Rondova). Palearctic: China (Guang Xi); Japan (Honshu, Ryukyu Islands, Iriomote- jima, Okinawa). Oriental: Malaysia (Sara- wak, Selangor, Singapore); Taiwan (Tai- nan); Thailand (Bangkok). Remarks. —This species is similar to P. 442 brunneifrons, but the genitalia of the male, especially the long, slender processes at the ventral margin of the epandrium, are con- sistently different. We could not identify the holotype of either the senior or junior synonym with complete assurance and have primarily based our assignment of names to this species on its distribution. The holotype of P. canora was collected on Taiwan; that of P. luteicornis in Malaysia. We have exam- ined male specimens from Malaysia, and Taiwan is near the center of the known dis- tribution of this species. This also follows the precedent of Miyagi (1977), although he used the junior synonym as the name for the Japanese specimens he studied. The male specimen we illustrated is from China (Guang Xi). Polytrichophora duplosetosa (Becker) Figs. 16-20 Clasiopa duplosetosa Becker, 1896:162. Diclasiopa duplosetosa. — Becker, 1926:45. Polytrichophora duplosetosa. —Cresson, 1929:166 [generic placement].— Cogan, 1984:137 [Palearctic catalog]. Description.—Small shore flies, length 1.30 to 1.85 mm. Head: Head ratio averaging 0.80. Frons rectangular, frontal ratio averaging 0.68, generally brown microtomentose; ocellar triangle more densely microtomentose than remainder of frons, usually bearing from two to four setulae near anterior margin; para- frons black, slightly orange red along ante- rior margin; anterior fronto-orbital plate with narrow band of sparsely white micro- tomentum immediately adjacent to eye; ocellar setae inserted slightly in front of an- terior ocellus. Antennae mostly orange, but dorsal surface of pedicel and Ist flagello- mere partially blackish; arista with 5 dor- sally branching rays. Face densely invested with grayish to yellowish gray microtomen- tum; parafacial setulae hair-like; parafacials lightly yellowish, concolorous with face but becoming whitish; gena white and densely PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON microtomentose. Eye ratio averaging 0.67; eye-to-cheek ratio averaging 0.12. Palpus yellow. Thorax: Mesonotum distinctly two toned, with broad longitudinal brown vittae ex- tended laterally to level of posterior dor- socentral seta, thereafter lateral margin gray; pleural areas mostly gray to whitish gray, becoming lighter colored, more whitish, ventrally. Fore coxa mostly yellow, at most very lightly brownish basally but exten- sively invested with silvery gray microto- mentum; femora brownish gray to gray; fore and mid tibiae mostly gray, hind tibia most- ly yellow; tarsomeres 1-4 yellow, 5th, oc- casionally 4th, brownish; fore femur with four short, stout, black setae along apical half of posteroventral surface. Wing hya- line; costal vein ratio averaging 0.86; M vein ratio averaging 0.51. Halter yellowish. Abdomen: Dorsum generally concolor- ous with mesonotum but with whitish gray microtomentum laterally and posteriorly; posterior margin of 5th tergum of male with some gray microtomentum. Length of 5th tergum of male nearly 1.5 x that of 4th; 5th sternum (Fig. 18) with anterior margin near- ly straight and with posterior cleft extended to anterior margin, forming two triangular sternites. Male genitalia (Figs. 16-20) as fol- lows: Epandrium (Figs. 16-17) more or less elliptical in posterior view, dorsal margin rounded, ventral margin pointed in poste- rior view but lacking a process, ventral mar- gin blunt in lateral view; aedeagus (Figs. 19— 20) about 5 x as long as wide, an irregularly shaped tube, membranous flap weakly de- veloped, closely appressed to ventral sur- face, about 0.4 length of aedeagus; aedeagal apodeme (Fig. 19) subtriangular; posterior arms of hypandrium (Fig. 18) moderately close together and comparatively short, slightly more than one-half total length, an- terior margin rounded. Type material.—The lectotype male of Clasiopa duplosetosa, designated here, is la- beled ““Oderwald [Poland. Silesia] 19/5. 37059 [handwritten]/lecto Typus Mathis 1984 [red; “‘lecto,”’ ““Mathis,”’ “1984” hand- VOLUME 102, NUMBER 2 19 443 0.045mm —— oo Figs. 16-20. Polytrichophora duplosetosa. 16. Epandrium and cerci, posterior view. 17. Epandrium and left cercus, lateral view. 18. Fifth sternum and hypandrium, ventral view. 19. Aedeagal apodeme and aedeagus, lateral view. 20. Aedeagus, dorsal view. written]. There are three other specimens labeled ““Typus’’ from Oderwald; these are designated as paralectotypes. A fourth para- lectotype is labeled “‘duplosetosa Beck. [handwritten]/Orsova V.37681. [number handwritten; black submargins]/Typus [red].’’ The lectotype male is double mount- ed (minute nadel in rectangular block of pith), is in good condition, and is in the Humboldt Universitat. Distribution. — Widespread in Europe and extending into Asia as far east as Iran (Co- gan 1984). Remarks.—Except for records of P. or- bitalis in North Africa, specimens of which we have not studied, this is the only species of Polytrichophora in the western Palearctic Region. There is considerable variation in the col- oration of the face and parafacials in this species. The color varies from a silvery cream to a rusty gold. Moreover, the para- facials are not always concolorous with the face, although they usually are. Polytrichophora pollinosa Miyagi Figs. 21-25 Polytrichophora pollinosa Miyagi, 1977: 20.—Cogan, 1984:138 [Palearctic cata- log]. Description.—Small shore flies, length 1.83 mm (holotype, the only specimen with an intact abdomen). Head: Head ratio averaging 0.84. Frons rectangular, frontal ratio averaging 0.66, ttt PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Figs. 21-25. generally brown microtomentose; ocellar triangle more densely microtomentose than remainder of frons, usually bearing from two to four setulae near anterior margin; para- frons black, slightly orangish red along an- terior margin; anterior fronto-orbital plate with narrow band of sparsely white micro- tomentum immediately adjacent to eye; ocellar setae inserted slightly in front of an- terior ocellus. Antennae mostly orange, but dorsal surface of pedicel and Ist flagello- mere partially blackish; arista with 5 dor- sally branching rays. Face densely invested with grayish to yellowish gray microtomen- Polytrichophora pollinosa. 21. Epandrium and cerci, posterior view. 22. Epandrium and left cercus, lateral view. 23. Fifth sternum and hypandrium, ventral view. 24. Aedeagal apodeme and aedeagus, lateral view. 25. Aedeagus, dorsal view. tum; parafacial setulae hair-like; parafacials lightly yellowish, concolorous with face but becoming whitish; gena white and densely microtomentose. Eye ratio averaging 0.65; eye-to-cheek ratio averaging 0.17. Palpus yellow. Thorax: Mesonotum densely microto- mentose, mostly brown but postpronotum and notopleuron silvery gray to gray; pleural sclerites whitish to silvery gray, becoming more light colored ventrally. Fore coxa mostly yellow, at most very lightly brown- ish basally, but extensively invested with silvery gray microtomentum; femora VOLUME 102, NUMBER 2 brownish gray to gray; fore and mid tibiae mostly gray, hind tibia mostly with more yellow exposed on base and apex; tarso- meres 1-4 yellow, 5th, occasionally 4th, brownish; fore femur with 4 short, stout, black setae along apical half of posteroven- tral surface. Wing hyaline; costal vein ratio averaging 0.87; M vein ratio averaging 0.56. Halter yellowish. Abdomen: Dorsum generally concolor- ous with mesonotum but with whitish gray microtomentum laterally and posteriorly; posterior margin of 5th tergum of male with some gray microtomentum. Length of 5th tergum of male nearly 1.5 x that of 4th; Sth sternum (Fig. 23) divided into 2 diamond shaped sternites. Male genitalia (Figs. 21- 25) as follows: Dorsal margin of epandrium (Fig. 21) rounded in posterior view, pointed ventrally in lateral and posterior views (Figs. 21-22), median margin about one-third dis- tance from ventral margin, with small pointed spur in posterior view; aedeagus (Figs. 24-25) between 4—5x longer than wide, basal one-half parallel sided, apical one-half evenly tapered to apex; aedeagal flap attached subapically, elongate, about twice length of aedeagus; aedeagal apodeme (Fig. 24) subtriangular; posterior arms of hypandrium (Fig. 23) widely separated and over two-thirds total length of hypandrium, anterior margin with a distinct U-shaped emargination. Type material.—The holotype female is labeled “‘Hiraizumi [Iwate-ken, Honshu] Aug 25 1962/Japonia tohoku Prov. I. Mi- yagi/Discocerina-type (Polytrichophora) pollinosa I. Miyagi [except for “‘-type’’ the data on this label are handwritten; red].” The holotype is double mounted (minute nadel in cardbord rectangle), is in good con- dition, and is in the collection of I. Miyagi (University of the Ryukyus, Okinawa, Ja- pan). In the original publication, this spec- imen is stated to be a male, but it is a female. Distribution. —Palearctic. Japan: Hon- shu: Iwate-ken (Hiraizumi); Aomori-ken (Towada). Hokkaido: Horonobe; Barato. 445 Remarks. —This species is distinguished from Asian congeners by the following char- acters: fore femur with flexor row of from six to seven stout setulae along posteroven- tral margin; male genitalia as illustrated (Figs. 21-25) and described above. We found that separation of this species from P. canora is virtually impossible on external characters alone. The characters of the male genitalia, however, are very dis- tinctive and can be used to distinguish these species. Acknowledgments For reviewing a draft of this paper and offering constructive criticism, we thank T. Pape and R. V. Peterson. We also thank the following curators and their respective institutions for the loan of specimens, especially primary type mate- rial: Academy of Natural Sciences of Phila- delphia (Mr. Donald Azuma); Humboldt Universitat, Berlin, DDR (Dr. H. Schu- mann); Instituut voor Taxonomische Zoo- logie, Universiteit van Amsterdam, Am- sterdam, The Netherlands (Dr. Pjotr Oosterbroek and Mr. Ben Brugge); School of Health Science, University of the Ryu- kyus, Okinawa, Japan (Dr. Ichiro Miyagi). Literature Cited Becker, Th. 1896. Dipterologische Studien IV: Ephydridae.— Berliner Entomologische Zeit- schrift 41(2):91-276. . 1926. 56a, Ephydridae und 56b, Canaceidae. In. Lindner, ed., Die Fliegen der palaarktisch- en Region 6(1):1-115. Cogan, B.H. 1984. Family Ephydridae. Pp. 126-176 in A. Soos and L. Papp, eds., Catalogue of Pale- arctic Diptera. Volume 10. Clusiidae—Chloropi- dae. Akad. Kiado. Budapest, 402 pp. , & W. W. Wirth. 1977. Family Ephydridae. Pp. 321-339 in M. D. Delfinado and D. E. Hardy, eds., A catalogue of the Diptera of the Oriental Region, Vol. III: Suborder Cyclorrhapha (ex- cluding Division Aschiza). University Press of Hawaii, Honolulu. Cresson, E. T., Jr. 1924. Descriptions of new genera and species of the dipterous family Ephydridae. VI.—Entomological News 35:159-164. 446 . 1929. Studies in the dipterous family Ephyd- ridae. Paper IJ.— Transactions of the American Entomological Society 55:165-195. 1945. A systematic annotated arrangement of the genera and species of the Indoaustralian Ephydridae (Diptera). 1. The subfamily Psilo- pinae.—Transactions of the American Ento- mological Society 71:47-75. Deonier, D. L. 1965. Ecological observations on Iowa shore flies (Diptera, Ephydridae).—Iowa Acad- emy of Science 71:496-510. Mathis, W. N., & Jin Zuyin. 1988. A review of the Asian species of the genus Lamproscatella Hen- del (Diptera: Ephydridae).— Proceedings of the Biological Society of Washington 101:540—-548. Meijere, J. C. H. de. 1916. Studien iiber siidostasia- tische Dipteren. XII. Javanische Dolichopodi- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON den und Ephydriden.— Tijdschrift voor Ento- mologie 59:225-273. Miyagi, I. 1977. Ephydridae (Insecta: Diptera). Jn Fauna Japonica. Keigaku Publishing Company. Tokyo, 113 pp. Scheiring, J. F., & B. A. Foote. 1973. Habitat distri- bution of the shore flies of northeastern Ohio (Diptera: Ephydridae).—The Ohio Journal of Science 73(3):152-166. (WNM) Department of Entomology, NHB 169, Smithsonian Institution, Wash- ington, D.C. 20560; (JZ) Department of Bi- ology, Northwestern Teachers College, Lan- zhou, Gansu Province, China. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 447-457 ADELPHYDRAENA, NEW GENUS, AND TWO NEW SPECIES FROM VENEZUELA, AND REMARKS ON PHYLOGENETIC RELATIONSHIPS WITHIN THE SUBTRIBE HYDRAENINA (COLEOPTERA: HYDRAENIDAE) Philip D. Perkins Abstract.—A new genus of aquatic beetle, Adelphydraena (Coleoptera: Hy- draenidae) and two new species are described. The new species are from south- ern Venezuela: A. spangleri was collected from a stream at the base of the tepui Cerro de la Neblina; A. orchymonti was collected from a stream near Puerto Ayacucho. Synapotypic and plesiotypic character states of the genera Adelphy- draena and Hydraena are discussed. Phylogenetic relationships within the genus Hydraena, and evolution of the lineage leading to Hydraena s.s. are also dis- cussed. Taxonomically and phylogenetically significant structures of the two new species are illustrated. The sandstone mesas in northern South America, known locally as tepuis, have per- haps a greater concentration of floral and faunal endemics than any other area in the Americas. The tepuis are of great age, ap- parently having undergone relatively little of the massive geological and climatic changes which greatly modified South America after separation from Africa. Some of the endemic species found on or near the base of tepuis are thought to represent phy- logenetically relictual taxa. The new genus Adelphydraena described below appears to be such a phylogenetic relict. A biological survey of one of the tepui areas in Venezuela, Cerro de la Neblina Park, was conducted in 1985 by several institu- tions under the organization and direction of the Venezuelan Government (Spangler 1985). A team from the Smithsonian Insti- tution, comprised of Paul J. Spangler, Phyl- lis M. Spangler, Robin A. Faitoute, and Warren E. Steiner, surveyed the aquatic in- sects. Collecting on the tepui and in streams near the base, the team collected over 55,000 insects, including a total of 16,694 speci- mens of aquatic Coleoptera, representing many genera and families. Despite the re- markably high number of specimens, with collections from many habitat types, the material included only a single specimen of the new genus Adelphydraena. In 1986, Paul J. Spangler collected aquat- ic insects near Puerto Ayacucho, which is about 400 miles north of Cerro de la Neb- lina Park. Among 2419 specimens of aquat- ic Coleoptera collected by Spangler was a second specimen, representing a second species, of Adelphydraena. Members of the new genus Adelphy- draena are phylogenetically revealing in that they retain several ancestral characteristics which are found in the derived state in the putative sister-group, the widespread and successful genus Hydraena. The combina- tion of plesiotypic versus apotypic character states of members of Adelphydraena reveal part of the sequential development of de- rived characters in the lineage leading to Hydraena s.s. Based on the extreme rarity of the spec- imens, and remoteness of the habitat, it seems unlikely that new material will soon be forthcoming. Therefore, the new genus 448 and two new species are described at this time. Adelphydraena, new genus Type species.—Adelphydraena spangleri, new species. Description. —Form: Body oblong, elytra sometimes ovate. Size: Length 1.24—-1.72 mm, width 0.58—0.84 mm. Color: Brown; pronotum lighter than head and elytra. Head: Frons with a low carina at rear, ar- cuate to posterior. Fronto-clypeal suture well developed. Labrum long, projecting ante- riorly, with deep median emargination to form two lobes, each lobe approximately parallel sided; labrum not expanded on sides near base. Mentum long, sides slightly con- vergent from posterior to anterior; apico- median emargination well developed. Max- illary palpi elongate, combined lengths of articles longer than ventral surface of head; ratios of articles 2, 3, and 4 (last) about 3: 1:2. Antennomeres 10 (5+5) (Fig. 11). Mandibles with lateral surface visible in dorsal aspect; not interlocking with labrum. Pronotum: Sides produced, sometimes sub- cordiform, margin weakly denticulate. Disc with shallow transverse depression across base, lacking posterointernal foveolae; a weakly developed, incomplete transverse depression slightly anterior to midlength, depression slightly arcuate to posterior and interrupted in middle. Elytra: Nine com- plete rows of punctures, row ten reduced to a few punctures in anterior. Explanate mar- gin moderate to well developed. Proster- num: Intercoxal process broad, flat, ex- panded laterally behind coxae, coxal cavities closed; postcoxal process with a low carina on each side extended posteriorly from me- dian margins of procoxae. A median lon- gitudinal, low carina in front of coxae; ca- rina extended beyond anterior margin to form very small apicomedian process. An- terior margin on each side of apicomedian process with small acute process slightly larger than apicomedian process. Trochan- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON tin concealed. Proepisternum wide, not emarginate anteriorly, hence antennal cav- ities without ventral opening. Low carina separating hypomeron and proepisternum becoming effaced in anterior 0.33. Antennal cavities well developed. Mesosternum: Mesosternum with low median longitudinal carina and two carinae on each side, one carina at mesosternal-mesepisternal suture and one carina about midway between the latter and median carina. Sometimes with weakly developed carina extended ante- riorly from each side of mesosternal inter- coxal process. Mesosternal intercoxal pro- cess short, broad. Metasternum: Low median longitudinal carina in anterior 0.5. Plaque size and shape varying (Figs. 2, 3). Each side with two longitudinal low ridges or cuticular thickenings, visible when in fluid, one extended from middle of margin of mesocoxal cavity and one extended from near posterior limit of lateral carina of mesosternum. Abdomen: Intercoxal ster- nite slightly wider than mesosternal inter- coxal process, fused with first sternum to form plate, plate delimited on each side by a low ridge extended posteriorly from me- dian margin of metacoxal cavity. Suture be- tween intercoxal sternite and first sternum visible through cuticle, sometimes not ex- pressed externally. Legs: Tarsi with five ar- ticles. All femora moderately narrowed in basal 0.33. Ventral Vestiture: Vestiture ex- tremely short and dense. Etymology. —Greek adelphe (sister), plus Hydraena. Adelphydraena is the putative sister-group of Hydraena. Adelphydraena spangleri, new species Type data.— Venezuela, Territorio Fed- eral Amazonas, Cerro de la Neblina, 1 km SE. Basecamp, 0°50'N., 66°10’W., 140 m, 21 Feb 1985, P. J. and P. M. Spangler, R. A. Faitoute, W. E. Steiner. Holotype female deposited in the National Museum of Nat- ural History, Smithsonian Institution. Description.—Size: Body 1.72 x 0.84 VOLUME 102, NUMBER 2 mm; pronotum 0.40 x 0.68; elytra 0.96 x 0.84. Color: Brown-testaceous. Head: Frons finely punctate, punctures smaller than eye facets; shiny in middle, microreticulate and dull laterally; posterior line not extended forward at juncture of shiny and microre- ticulate areas. Clypeus strongly microreticu- late. Labrum slightly longer than clypeus; median emargination setose, length nearly 0.66 labrum length. Eyes small in dorsal aspect, width 0.3 interocular distance. Mentum elongate, narrowed anteriorly, lobe on each side of apicomedian emargination curved ventrally and toward midline; apical width 0.5X basal width. Genae without posterior ridge. Pronotum: Pronotum sub- cordiform. Posterior 0.5 of disc with raised, rounded relief on each side of midline, re- liefs separated anteriorly by two large punc- tures side-by-side, followed by a single puncture in midline; reliefs very shiny, very finely, sparsely punctate, punctures similar to those of frons. Punctures posterior to re- liefs very coarse and dense, forming two transverse rows, rows separated from one another by confluent interstices which form transverse line slightly less raised than dis- cal reliefs, transverse raised line connected to each discal relief by similarly raised, short longitudinal line on each side of midline. Punctures anterior to discal reliefs coarse, slightly smaller than posterior punctures, shallow, bottoms apparently flat with cen- tral seta, interstices shiny, 0.51—1.0 x punc- ture diameter. All interstices anterior and posterior to discal reliefs with extremely sparse, very fine punctures similar in size to those of discal reliefs. Lateral depressions with punctures less developed and interstic- es less shiny than punctate discal areas. Lat- eral margin denticulate, more distinctly so anterior to middle. Anterior margin weakly trisinuate. Posterior margin weakly bisin- uate. Elytra: Punctures on disc 1 x punc- tures on anterior area of pronotal disc. In- tervals raised slightly, shiny, 2—3 x puncture diameter. Punctures in anterior 0.5 of rows 1-5 larger and more widely spaced than on 449 ne ee ee Cais Gare ery G oe ee Wwe or @) eco co Ce 2 Gy ~ececee CGec Qf4 ——— a co} 9 9999} 0 oa 2 So Oyo). oS 29) OE Ae < 7799 \ c ie) 9 a*-. >: Ei ae 3 3% * a. > are eA Oy 28S). ale a 7? a5 aa). Ded B 9 A Pyare ae, ed OM cs weary eye } 4 9 Oe A98F 9. a a4 Cu Id OST a 29 tg 2 Ol Silken is ° eS lacy ee) ay Tn) 5 > ? Ge: ae) 9) 39) AO! ORO) GO pe PO > O0E 0 OREO E ED) ean oP ORS 9) (8 (4 to alan) nk ia: Foe nes 4. 4 neta SOe Onl bigsel. tus. Adelphydraena spangleri, new species, habi- remainder of elytron, interstices 2—4 x puncture diameter. Raised humeri con- nected with slightly produced anterior an- gles. Lateral margin strongly arcuate, ex- planate margin well developed, at midlength slightly wider than distal width of metatibia. Anterior margin with extremely small, pos- teriorly produced acute process at base of second interval. Prosternum: Prosternal in- tercoxal process as wide as mesosternal in- tercoxal process; prosternal midline length 2.75 X prosternal intercoxal process width. Prosternal postcoxal process flat between submedian carinae. Mesosternum: Meso- sternal intercoxal process length 1 x width, apex slightly arcuate. Submedian carinae at- taining thickened anterior border of meta- 450 sternum. Metasternum: Plaques well de- veloped (Fig. 2). When in fluid, a dark longitudinal line of strength visible, extend- ed posteriorly from each mesosternal suture to near posterior margin of metasternum. Abdomen: Distance separating coxal cavi- ties 2X mesosternal intercoxal process width. Submedian carinae of first sternum terminated slightly before posterior border of first sternum, distance separating carinae at posterior extreme slightly greater than midline length of first sternum plus fused intercoxal sternite. Sterna 1—5 with hydro- fuge, sterna 6 and 7 shiny, sparsely pubes- cent. Legs: All legs without apparent mod- ifications. Flight wings: Fully developed. Spermatheca: Fig. 13 (male unknown). Habitat. —The holotype was seined from rocks and leaf packs in the rapids of a white- water stream. The stream was 5 m wide and 30 cm deep, with sand/gravel margins and bottom; oxygen, 9 ppm; hardness, 0; pH, 5.0; water temperature 29°C The air tem- perature was a sweltering 42°C (Spangler, pers. comm.). Etymology.—It is with pleasure that I dedicate this new species to Paul J. Span- gler, whose dynamic fieldwork has provided a wealth of aquatic Coleoptera for system- atic studies. Adelphydraena orchymonti, new species Type data.—Venezuela, Territorio Fed- eral Amazonas, Puerto Ayacucho (40 km S.) at Tobogan, 24 Feb 1986, P. J. Spangler. Holotype female deposited in the National Museum of Natural History, Smithsonian Institution. Diagnosis.—Adelphydraena orchymonti and A. spangleri differ markedly in many characteristics. A. orchymonti lacks the sub- cordiform shape of the pronotum and broadly explanate elytra seen in A. spangleri (Figs. 1, 4), and is much smaller, 1.24 vs. 1.72 mm. The metasternal plaques are very small in A. orchymonti and very large in A. spangleri (Figs. 2, 3). The shape of the men- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON tum differs in the two species (Figs. 9, 10). Additional differences detailed in the species descriptions include sculpture of the prono- tum and head, relative widths of elytral punctures and intervals, and relative widths of the intercoxal processes. Description. —Size: Body 1.24 x 0.58; pronotum 0.32 x 0.54; elytra 0.76 x 0.58. Color: Brown, pronotum lighter than head and elytra. Head: Frons finely punctate, punctures smaller than eye facets; posterior arcuate line with lateral area extended for- ward. Clypeus finely punctate. Labrum as long as clypeus; median emargination se- tose, length slightly greater than 0.5 x la- brum length. Eyes small in dorsal aspect, width 0.2 interocular distance. Genae without posterior ridge. Pronotum: Disc with two slightly depressed, transverse areas with large, well impressed punctures 4-5 x eye facets, separated by thin walls: one area occupying basal 0.25 of disc, other area an ill-defined line, arcuate to posterior, across disc slightly anterior to middle; relief be- tween coarsely punctate areas very finely, sparsely punctate, punctures | x frons punc- tures, interstices shiny; area anterior to transverse line of coarse punctures with punctures becoming increasingly smaller toward anterior, those at margin | x frons punctures. Lateral depression finely sparse- ly punctate, moderately produced slightly anterior to midlength. Elytra: Punctures on disc 1x largest pronotal punctures. Inter- vals raised slightly, shiny, 1 x puncture di- ameter on disc, slightly narrower at inter- vals 4—6. Interstices slightly less than 1 Xx puncture diameter. Anterior margin with extremely small, posteriorly produced acute process at base of second interval. Proster- num: Prosternal intercoxal process as wide as mesosternal intercoxal process; proster- nal midline length 2.66 x prosternal inter- coxal process width. Prosternal postcoxal process slightly concave between subme- dian ridges (Fig. 5). Mesosternum: Meso- sternal intercoxal process length 0.66 width, apex slightly rounded. Submedian VOLUME 102, NUMBER 2 4 Figs. 2-5. 451 2, Adelphydraena spangleri, metasternum and anterior abdominal sterna; 3, A. orchymonti, same; 4, A. orchymonti, body outline; 5, A. orchymonti, prosternum. (Scale lines equal 0.1 mm.) Carinae not attaining thickened anterior border of mesosternum. Metasternum: Plaques extremely small, located at border of median, triangular, shallow depression. Apex of triangular depression joining low median carina to form inverted Y (Fig. 3). Abdomen: Distance separating coxal cavi- ties 1.25 mesosternal intercoxal process width. Submedian carinae of first sternum diverging posteriorly, distance separating carinae posteriorly equal to length of first sternum plus fused intercoxal sternite. Legs: Legs without apparent modifications. Flight wings: Fully developed. Spermatheca: Fig. 14 (male unknown). Habitat.—The holotype was collected among rootlets along the shallow, slightly sandy margin of the clear stream as it tum- bled over the polished granite bedrock. The stream was partially shaded, 3 m wide, with a maxinuney depth of ca.50.cm: pH, 5.0: oxygen, 12 ppm; hardness, 0; velocity, 46 cm/sec; water temperature, 25°C; and air temperature, 33°C at the time of collection. Etymology.—This new species is dedi- cated to Armand d’Orchymont in recogni- 452 tion of his contributions to the systematic literature of the family Hydraenidae. Phylogenetic Relationships of the Genus Adelphydraena Synapotypic Characters of the Subtribe Hydraenina All members of the subtribe Hydraenina share two distinctive derived characters: the prosternal intercoxal process is expanded laterally behind the procoxae, closing the procoxal cavities, and the second article of the maxillary palpus is elongate and slender (Perkins 1981: 415, Fig. 148 C; 431). Mem- bers of Adelphydraena also have these apo- typic characters (Figs. 5, 12), and are, there- fore, members of the Hydraenina. Synapotypic Characters of Hydraena s.1. In addition to possessing the apotypic characters of the subtribe Hydraenina, members of Hydraena s.|. have the follow- ing, previously undiscussed, synapotypic characters of the labrum, mandibles, and mentum. All members of Hydraena s.l. have the labrum abruptly widened, slightly de- pressed and thickened near the base. Each mandible has a dorsolateral process which, when the mandible is closed, fits tightly against and over the widened area of the labrum (fig. 7). The labral and mandibular structures function together to form an in- terlocking device. Interlocking may, in ad- dition to adding rigidity to the labrum, re- sult in better integration of movement of the labrum and mandibles during feeding and/or function to transfer to the labrum some of the opening and closing power of the strong mandibular muscles. In all members of Hydraena s.\. the men- tum has a prominent apicomedian process (Fig. 8). This process is generally lobate in profile and directed obliquely toward the dorsal surface of the head. When the head is seen in dorsal aspect the process is visible PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON because of the large median emargination between the lobes of the labrum. Synapotypic and Plesiotypic Characters of Adelphydraena The derived characters of the labrum, mandibles, and mentum present in Hy- draena s.\. are absent in members of Adel- phydraena. The labrum is straight sided, and the mandible lacks the anteriorly projecting dorsolateral process (Fig. 6). The mentum is emarginate apicomedially (Figs. 9, 10); this probably represents a derived condi- tion, but in a direction opposite that taken in the lineage leading to Hydraena. The api- comedian emargination of the mentum re- lates to other modifications in the labium; these labial structures will be described and compared with other genera in a separate paper. The ancestral number of antennal articles for the family Hydraenidae is almost cer- tainly eleven (by outgroup comparison with other Coleoptera). Members of Adelphy- draena have ten articles (Fig. 11), whereas members of Hydraena s.|. represent a fur- ther derived step in reduction, having nine articles. The ancestral number of elytral striae for the order Coleoptera is almost certainly ten (Crowson 1981:42), as is also true for the family Hydraenidae. Members of Adelphy- draena have the reduced condition of nine complete striae, with stria ten reduced to a few basal punctures (Fig. 1). The elytra of all members of Hydraena s.l. show at least some increase in the number of striae (see below). The reduced striae of Adelphy- draena members is a distinctive dorsal apo- typic character. The prosternal intercoxal process of Adel- phydraena is unique among Hydraenina in the possession of a longitudinal ridge on each side which extends posteriorly from the median margin of the procoxal cavity. The middle portion of the postcoxal pro- cess, between the ridges, is flat or slightly VOLUME 102, NUMBER 2 7 her 1 7 —_-+-- = -. 453 14 Figs. 6-14. 6, Adelphydraena orchymonti, labrum, mandible, and anterior region of head; 7, Hydraena riparia Kugelann, same. 8, H. riparia, mentum; 9, A. orchymonti, mentum; 10, A. spangleri, mentum; 11, A. spangleri, antenna; 12, A. orchymonti, maxillary palpus; 13, A. spangleri, spermatheca; 14, A. orchymonti, spermatheca. (Scale line equals 0.1 mm.) concave, and contiguous with the flat inter- coxal area (Fig. 5). In members of Hydraena the postcoxal process is raised in the middle, varying from slightly rounded to strongly, longitudinally carinate. In members of Hydraena the proepister- num is emarginate anteriorly, the emargi- nation providing a ventral opening to the pocket in which the antenna is held (cf. Per- kins 1981, figs. 63F, 148C). This emargi- nation is a synapotypic character for the ge- nus Hydraena; variation in degree of development of the episternal emargination will be discussed in a separate paper. Mem- 454 bers of Adelphydraena retain the plesiotypic condition, having the proepisternum non- emarginate anteriorly, hence the well de- veloped antennal pockets are not open ven- trally (Fig. 5). Nonpubescent, smooth and shiny sub- median areas of the metasternum, termed plaques, are characteristic for the genus Hy- draena, and frequently provide species-spe- cific characters. The presence of plaques in Adelphydraena spangleri (large) and A. or- chymonti (small) (Figs. 2, 3), suggests that plaques were present in the common ances- tor of Hydraena and Adelphydraena. In all other Hydraenidae, a portion of the true second sternum is visible between the metacoxae. This can be referred to as the intercoxal sternite (Perkins 1981:21). The intercoxal sternite takes many shapes in the family, but is always separated from the first complete sternum (true third) by a suture. In members of Adelphydraena the intercox- al sternite and the first complete sternum are fused, on the same plane, and together form a plate. This plate is delimited on each side by a raised line which originates near the lateral margin of the intercoxal area, and extends diagonally across the first sternum (Figs. 2, 3). In A. spangleri the suture be- tween the intercoxal sternite and the first sternum is visible through the cuticle (tem- porary slide mount), but no surface mani- festation of the suture was detected, whereas the suture is visible externally in A. orchy- monti. Additionally, in both species the first sternum is more tightly joined to the meta- sternum than is usually seen in members of Hydraena, adding to the rigidity of the area surrounding the metacoxae. The discal plate of the first sternum, which is similar to structures found in the family Elmidae, is a distinctive ventral apotypic character. Phylogenetic Relationships within the Genus Hydraena Hydraena is a large genus found on all continents. It is quite diverse, and has many PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON clusters of obviously closely related species. Various, apparently monophyletic, sub- groups of Hydraena were given formal, subgeneric status by Rey (1886) and Kuwert (1888). Of these subgenera, d’Orchymont (1936) recognized only Hydraena s.s., Haenydra Rey, and Kuwert’s Phothohy- draena, Holcohydraena, and Taenhy- draena. Perkins (1981:61) compared Amer- ican Hydraena with these subgenera and found that the characters upon which Ku- wert’s subgenera Holcohydraena and Taen- hydraena were based appeared in only some members of separate monophyletic clusters of species, and concluded that Holcohy- draena and Taenhydraena were not valid. Species with the strial configuration found in members of Haenydra and Phothohy- draena are not known from the New World (Perkins 1981). In contrast to the views of d’Orchymont (1936) and Perkins (1981), Ienistea (1968, 1978, 1982) considered the subgenera of Rey and Kuwert worthy of full generic status. In a revealing paper, Berthélemy (1986) compared the elytral striae of several species (principally Palearctic) representing the main groups of Hydraena s.l. Using ten striae as the ancestral condition (by outgroup com- parison), Berthelemy reasoned that all species with a duplication of striae resulting in the maximum configuration of 3a4b4c2d2e (a-e being nervures), are monophyletic and were derived after the divergence of species with less duplication. Since Hydraena riparia Kugelann has this strial configuration, and is the type-species of Hydraena, Berthélemy concludes, correctly I think, that all species with the derived condition of 3,4,4,2,2 are rightly members of Hydraena s.s. Perkins (1981:212) erected the genus Spanglerina for four species of Central American hydraenines. These four species share several unusual, derived characters, but also have the 3,4,4,2,2 strial configu- ration. If the nonduplicated condition is considered ancestral for Hydraena, and if one assumes that strial duplications have VOLUME 102, NUMBER 2 not been independently derived in different lineages, then one would conclude that the common ancestor of these four species must have arisen within Hydraena s.s. Spangler- ina, therefore, cannot be considered a taxon of equal rank with Hydraena, and perhaps for the time being can be treated as a sub- genus until the elytra and other structures of the diverse genus Hydraena are more completely known. The strial configurations illustrated by Berthelemy (1986) are summarized below, where the number of striae between the ner- vures are given for 16 species. Also included are six hypothetical intermediates, each in- dicated by a (?). Species having primarily two striae between nervures, but with some areas with three punctures, are assigned a value of 2+. Similarly, a value of 3— in- dicates that there are primarily three striae between the nervures, but with some areas having two punctures. 2 2 2+ 2 2. --gracilis, truncata, bicuspidata, polita 2 2 2+ 2— 2- -- minutissima eee et 2 = sharpi Pee ae bay 2 ==? Rap La Dae ie OY at, Dee oo lk 62) C-- pyemaea ieee l|6|6CD == Servilia Dae SVS 8) Rr a 4 3— 3-— 3-— 1 2. --pulchella Soo 2— 2 =- stussinerni Seow 4, lL) .2),.) =-stestacea SMe ot 2 2 aH? Semone ot 2. 2 --? Seen 4" 282) ==? 3 4 3 2 #2 -- rugosa (reversal) 3 4 4 2 2. --exarata, quadricollis 3 4 4 2. 2+ -- riparia, brachymera No species illustrated by Berthélemy has the ancestral condition of ten simple striae with no indication whatsoever of duplica- tion. Species traditionally placed in the sub- genus Haenydra (gracilis, etc.) have the least amount of strial duplication, with duplica- tion limited to a portion of stria six. Species sometimes placed in the subgenus Hadren- ya also have this configuration. Species in 455 Hydraena s.s. have the greatest amount of duplication. The clinical progression seen in the elytral data can be interpreted as reflecting many phylogenetic divergences from the line which eventually resulted in the maximum expression of strial duplication now known (3,4,4,2,2+). Although further study may reveal that some of the transitional config- urations are actually reversals from a more derived condition (Berthéelemy 1986), for the sake of discussion we can assume that transitional configurations did exist in some species (or are present in as yet undiscov- ered ones). This position would be consis- tent with the uncontested transformational nature of some extant configurations. Although Berthélemy concludes that striae 2 through 6 are duplicated in Hydraenas.s., it would seem that in any instance where there is a whole number increase without intermediate steps known (for example the increase from 3 to 4 striae between nervures a and b, and the similar increase between nervures b and c) we do not know for certain which of the striae became duplicated. But when transitional numbers exist, we can as- sume that they truly represent retention of the ancestral elytral condition for the mono- phyletic group of which they are a part, and from their configuration infer which stria was duplicated to form the next higher whole number configuration. For example, it is from the partial duplication of stria 6 pres- ent in gracilis (etc.), minutissima and sharpi that we infer that the extra stria between nervures b and c in testacea derives from stria 6 rather than stria 5. With respect to reversions, Berthélemy suggests that perhaps the pulchella-pyg- maea configuration (2+,2+,3—,1,2) isa re- version from the Hydraena s.s. configura- tion (3,4,4,2,2). However, this would skip the intermediate configuration of 3,3,3,1,2. H. testacea has this configuration and also shares with pulchella-pygmaea the derived state of only one stria between nervures c and d. According to the subgeneric divisions 456 recognized by Berthélemy, the strial reduc- tion from two to one between nervures c and d occurred independently in at least three separate lineages. Based on retention of the presumed an- cestral elytral configuration of Hydraena s.1., Berthélemy recognizes Haenydra as a valid subgenus. he also recognizes Hadrenya, al- though its members have the same config- uration as Haenydra. This decision is ap- parently based on the lack of known derived characters shared by all species in these two groups. Similarly, Berthélemy recognizes as valid the subgenus Phothohydraena, the members of which have a 3,3,3,2,2 config- uration (e.g. festacea). Therefore, formal subgeneric ranking is based upon two criteria: (1) elytra with less duplication than the maximum number (<3,4,4,2,2) and (2) absence of any synapo- typy with species which have the same ely- tral configuration. If these criteria are ac- cepted, then every species found to have a truly intermediate strial configuration (..e., not resulting from reversals) and no clear synapomorphy with members of the rec- ognized subgenera, would be treated as rep- resenting a new subgenus. Interestingly, the formal categories of subgenera as now recognized in Hydraena are therefore not simply monophyletic clus- ters of species which are easily recognized (the “sorting categories” of taxonomists), nor do they meet the criteria of sister-groups. Evolution of the Lineage Leading to Hydraena s.s. Based on the apotypic characters dis- cussed above, it can be said that in the sub- tribe Hydraenina, the following structural modifications were among those that evolved in the lineage leading to Hydraena S.S.: 1. Postcoxal process of prosternum de- velops lateral extensions, closing procoxal cavities PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON — Antenna becomes reduced from ten to nine articles — Labrum-mandible interlocking structure develops — Mental apicomedian process devel- ops — Proepisternal anterior emargination develops 6. Elytral strial duplications develop We can be fairly certain that modification of the postcoxal process was the first of these innovations in the Hydraenina because members of Adelphydraena have this struc- ture but retain the primitive condition for the antennae, labrum, mandibles, and pro- episterna. These four characters are thought to be truly plesiotypic in Adelphydraena and not a result of reversals from a derived con- dition. The following considerations seem to support this position: (A) Reduction in number of antennomeres has occurred in several lineages in the family, but no in- stance of increase in number of antenno- meres is known (Perkins, unpublished). (B) The labrum-mandible interlocking struc- ture 1s complex, involving corresponding modifications to each structure. The form of the labrum and mandibles in Adelphy- draena do not suggest reversal from the de- rived condition. The mentum of Adelphydraena, based upon comparison with other genera (Per- kins, unpublished), probably does not rep- resent the ancestral condition for the Hy- draenina. The form of the mentum 1s derived in both genera, but in opposite directions, the apical area being enlarged in Hydraena and emarginate in Adelphydraena. The primitive number of elytral striae for the Hydraenina is 10. In Adelphydraena none of the striae show any degree of du- plication, and stria 10 is reduced to an an- terior remnant consisting of a few punc- tures; consequently, there are only nine complete rows. In known Hydraena there is always some degree of strial duplication, and no species show a loss of stria 10. VOLUME 102, NUMBER 2 Of the six structural modifications, the duplication of elytral striae is almost cer- tainly the most recent development. All members of Hydraena have the first five derived characters but some members re- tain the ancestral condition for the striae (except stria six). Further, a transformation series of increasing strial duplication is seen in extant species of Hydraena. The sequence of appearance of the four other structural modifications, if indeed they developed sequentially and not concurrent- ly, is problematic. If they did develop se- quentially, their relative positions along the phylogenetic line leading to Hydraena s.s. can only be resolved with the discovery of as yet unknown taxa which have more of these derived states than Adelphydraena, and less than Hydraena. Acknowledgements I thank Paul J. Spangler for providing in- formation about the habitats of the new species, and for reviewing the manuscript. I also thank Young T. Sohn for drawing the habitus illustration. Literature Cited Berthelemy, C. 1986. Remarks on the genus Hy- draena and revision of the subgenus Phothohy- draena (Coleoptera: Hydraenidae).— Annales de Limnologie 22:181-193. 457 Crowson, R.A. 1981. The biology of the Coleoptera. Academic Press, London, 802 pp. Ienistea, M. A. 1968. Die Hydraeniden Rumaniens (Coleoptera, Hydraenidae).—Travaux du Mu- séum d’Histoire Naturelle ““Gr. Antipa.”’ Bucu- resti 8:759-795. 1978. Hydradephaga und Palpicornia, in J. Illies ed., Limnofauna Europaea, 2nd edit., G. Fischer, Stuttgart. XVII + 532 pp. . 1982. Hydraenoidea de la Suisse (Coleoptera) (Catalogue). — Archives des Sciences, Genéve 35: 303-316. Kuwert, A. 1888. Generalubersicht der Hydraenen de europaischen Fauna.— Deutsch Entomolo- gische Zeitschrift. Berlin 32:113-123. Orchymont, A.d’ 1936. Au sujet de la phylogenie du genre Hydraena (Col. Palpicornia Fam. Hy- draenidae).— Memoires du Musée Royal d’His- toire Naturelle de Belgique (2nd ser.) 3:61-67. Perkins, P. D. 1981. Aquatic beetles of the family Hydraenidae in the Western Hemisphere: clas- sification, biogeography and inferred phylogeny (Insecta: Coleoptera).—Quaestiones Entomo- logicae 16 (1980):3-554. Rey, C. 1886. Histoire naturelle des coléoptéres de France.—Annales de la Société Linnéenne de Lyon 32(1885):1-190. Spangler, P.J. 1985. A new genus and species of riffle beetle, Neblinagena prima, from the Venezuelan tepui, Cerro de la Neblina (Coleoptera, Elmidae, Larinae).— Proceedings of the Entomological Society of Washington 87:538-544. U.S. Dept. of Agriculture, APHIS, Suite 518, 10 Causeway Street, Boston, Massa- chusetts 02222. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 458-467 SYMPHURUS CALLOPTERUS (CYNOGLOSSIDAE, PLEURONECTIFORMES), A NEW DEEPWATER TONGUEFISH FROM THE EASTERN PACIFIC Thomas A. Munroe and Madhu N. Mahadeva Abstract.—A new species of eastern Pacific tonguefish, Symphurus callop- terus, is described from moderately deep continental shelf waters from Mexico south to northern Peru. The species is characterized by a unique interdigitation pattern (1-3-4) of dorsal pterygiophores and neural spines and the combination of a well-developed pupillary operculum, high counts (105-114 dorsal-fin rays, 91-98 anal-fin rays, 57-61 total vertebrae), and four hypurals. It is further characterized by a unique combination of pigmentation features including an unpigmented peritoneum, the presence of a dark brown or black blotch on the ventral portion of the ocular-side operculum, banding on the posterior head and along the body, and especially by the occurrence of an alternating series of distinct, black rectangular blotches and unpigmented areas on the posterior two-thirds of the dorsal fin and throughout the anal fin. Comments on overall size, size at sexual maturity, and co-occurrence with sympatric species of Sym- phurus are provided. Examination of radiographs revealed an interesting anom- aly in the number of neural and/or haemal spines occurring on preural centra. Of 180 specimens examined, 27 (15%) had double neural and/or haemal spines on the first and/or second preural centra. This anomaly is shown to result most likely from the fusion of two centra. Tonguefishes (family Cynoglossidae) are small to medium-sized, sinistral flatfishes. In the eastern Pacific, they range from southern Oregon (Eschmeyer et al. 1983) to northern Peru (Hildebrand 1946, Chiri- chigno 1974) and inhabit diverse sedimen- tary and bathymetric environments. Thir- teen nominal species of Symphurus have been described from the eastern Pacific and there are at least four additional species to be described. Knowledge of the eastern Pa- cific species of this genus is inadequate, al- though symphurine tonguefishes comprise significant components of the benthic ich- thyofauna in certain habitats (Bartels et al. 1983, 1984; Love et al. 1984). Bartels et al. (1984) found that tonguefishes, including several undescribed species (one of which was S. callopterus), were a numerically dominant component of the demersal fish fauna in the Gulf of Nicoya, Costa Rica. Since the earlier, mostly regional, studies by Jordan & Evermann (1898), Meek & Hil- debrand (1928) and Hildebrand (1946), there has been no published comprehensive revision of eastern Pacific Symphurus. The most recent, and only comprehensive, treat- ment of eastern Pacific tonguefishes is an unpublished dissertation by Mahadeva (1956) in which several new species were recognized. Mahadeva recognized the new species described herein based on ten spec- imens. Since Mahadeva’s study, trawling on the continental shelf off Mexico, Central America and South America has resulted in the collection of many additional tonguefish specimens, including 292 specimens of this species. Inclusion of this new material al- VOLUME 102, NUMBER 2 lows us to present a more complete and ex- panded description of the new species. A detailed systematic revision of eastern Pacific tonguefishes is in progress by the first author, but final results are not expected until a later date. Therefore, in order to make the name of this species available to other researchers conducting ecological and early life history studies on eastern Pacific tonguefishes, a formal description is pro- vided at this time. This paper is the first in a projected series of papers on symphurine tonguefishes. Re- visionary studies on eastern and western At- lantic tonguefishes, based largely on Mun- roe (1987) are forthcoming. Additionally, results ofa survey of interdigitation patterns of dorsal pterygiophores and neural spines in the genus Symphurus is in preparation. Completing this series will be a revision of eastern Pacific and Indo-Pacific Symphu- rus. A phylogenetic analysis of intrageneric relationships based on detailed osteological studies is also in progress and will comple- ment these revisionary studies. Type specimens of the new species are deposited in the following institutions: Cal- ifornia Academy of Sciences (CAS); Na- tional Museum of Natural History (USNM); Natural History Museum of Los Angeles County (LACM); Scripps Institution of Oceanography, Marine Vertebrate Collec- tion (SIO); University of Miami, Rosenstiel School of Marine and Atmospheric Sciences (UMML); Florida State Museum (UF); and the British Museum (Natural History) (BMNH). Methods. —Counts and measurements were modified from Ginsburg (1951), Ma- hadeva (1956), Menezes & Benvegnu (1976), and Munroe (1987). Counts and measure- ments are outlined briefly below. Meristic data, exclusive of scale counts, were taken from radiographs. Interdigitation pattern (ID). — Patterns of interdigitation of proximal dorsal pteryg- iophores and neural spines were counted and recorded for the first three, or in un- 459 usual cases, the first four interneural spaces. The number of dorsal pterygiophores in- serted into interneural spaces 1—3 was found to be diagnostic for species or groups of species of Symphurus (Munroe 1987). ID patterns are indicated by a pterygiophore formula such as 1-3-4. The 1-3-4 ID pattern indicates one pterygiophore inserts in inter- neural space one, three in interneural space two, and four in interneural space three. The first neural spine abuts directly against the cranium so there is no obvious space be- tween it and the cranium. Therefore, the first interneural space reflected in the for- mula is that between the first and second neural spines. Caudal-fin rays. —Previous authors (Ginsburg 1951, Mahadeva 1956, Menezes & Benvegnu 1976, Munroe 1987) have found that caudal-fin-ray count is extremely conservative within the genus. Previous studies have included the ultimate dorsal- and anal-fin rays in the caudal-ray counts. Because the ultimate rays of the median fins are supported by caudal elements and are aligned along the same vertical plane as the caudal-fin rays they are also included in cau- dal-ray counts reported here. Anal-fin rays.—Includes all rays and is exclusive of the thick, muscular gonadal duct preceding the first anal-fin ray. Vertebral counts. —There are consistently nine abdominal vertebrae, three without and six with haemopophyses; abdominal ver- tebrae counts are thus reported as (3+6). Counts of total vertebrae include the urosty- lar centrum (see Remarks section below). Specimens with obviously damaged verte- bral skeletons, underlying support bones, or caudal fins were excluded from summaries and analyses. Scale counts. — Accurate, repeatable scale counts are difficult to make in Symphurus, especially for species in which the scales are often abraded and lost during capture when specimens are trawled from any appreciable depths. Approximate counts were based on partial scale counts, counts of scale pockets, 460 or a combination of the two. Longitudinal scale row count includes the total number of complete diagonal rows of scales along a hypothetical line starting immediately above the opercular angle to the end of the hypural; the few rows of scales along the caudal-fin base are not included and the last scale must be at least halfin front of the hypural. Trans- verse scale count is the number of scales in a diagonal row from the base of the dorsal fin at a point directly above the posterior margin of the operculum to the base of the anal fin. Scales extending out onto the dor- sal- and anal-fin rays are not included. Head scale row count includes all the oblique rows of scales on the head counted posteriorly from the first complete row of scales passing the posterior border of the lower eye; it in- cludes the last complete row of scales im- mediately anterior to the mid-point emar- gination on the posterior border of the operculum, but the few small rows of scales present on either the dorsal or ventral fleshy lobes of the operculum are not included. All measurements were made on the ocu- lar surface except where noted. Measure- ments were taken to the nearest 0.1 mm with dial calipers (to 150 mm) or ocular micrometer. Measurements are expressed either as thousandths of standard length or thousandths of head length. Standard length: distance from tip of fleshy snout to posterior end of hypural plate. Body depth: distance across body at the anus, exclusive of fins; measured on blind side. Preanal length: tip of fleshy snout to origin of anal fin; mea- sured on blind side. Caudal-fin length: base of articulations of middle caudal-fin rays to tip of longest middle rays. Pelvic-fin length (only blind side pelvic fin present in adults): basal articulation to distal tip of the longest ray. Pelvic to anal length: shortest horizon- tal distance from base of most posterior pel- vic-fin ray to anal-fin origin. Head length: tip of fleshy snout to most posterior exten- sion of upper fleshy lobe of operculum. Head width: greatest distance across head at pos- terior portion of operculum. Postorbital PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON head length: posterior margin of lower eye to posterior extent of upper fleshy lobe of operculum. Upper head lobe width: dis- tance at operculum from dorsal margin of body to dorsal origin of operculum. Lower head lobe width: distance at operculum from dorsal origin of operculum to most ventral part of operculum. Snout length: anterior rim of lower eye to tip of snout. Upper jaw length: shortest horizontal distance from bony tip of premaxilla to angle of mouth. Eye diameter: greatest horizontal diameter of the cornea of the lower eye; does not include fleshy tissue surrounding eye. Chin depth: vertical distance from angle of the mouth to most ventral aspect of the head. Size at maturity was estimated by mac- roscopic examination of the extent of pos- terior elongation of the ovaries (ovaries of mature females are conspicuous through the body wall when light is transmitted from beneath the specimen; in immature females, developing ovaries are best observed by dis- section). Since no obvious differences in tes- ticular size were apparent in males, esti- mates of maturity were based entirely on females. Depth of capture (in feet or fathoms) was transformed to the nearest meter. If depth included a range of depths over which the nets were towed, an average depth for that particular trawl was calculated. Symphurus callopterus, new species Figs. 1-2 Holotype. —CAS 64023 (male, 116.9 mm SL); Peru; 05°59'S, 81°)2°W tomO0Se56 ss. 81°11’W, 65-70 m, 4 Jun 1966. Collected with 70 ft Gulf of Mexico semi-balloon trawl, R/V Anton Bruun Cruise 16, Station 631 B. Paratypes.—(Measured and counted 20 specimens; 93.2—-127.6 mm SL): Costa Rica.—USNM 164492, 2(93.2—96.1), 6 mi off Cabo Velas, Papagayos, 101 m, 01 Jul 1932.—UF 47590, (117.1), Puntarenas Province, Gulf of Nicoya, 317 m, 29 Jun VOLUME 102, NUMBER 2 461 Fig. 1. 1973. Panama Bay.—UMML 26069, 15(97.3-127.6), 8°00.4—00.7'N, 79°48.8- 41.5'W, 78 m, 4 May 1967.—UMML 34317, 2(104.1-121.7), 7°40.3'N, 79°50.9'W; 78 m, 2 May 1967. Counts were also taken from the following 46 paratypes (88.5-—145.7 mm SL): Mexico, Gulf of Tehuantepec. — SIO 63-518, 9(99.5-136.6), 15°57.5'N, 95°22.5'W, 65 m, 12 Jul 1963.—SIO 63- 521, 2(96.5—105.6), 15°41'N, 96°07.5’W, 55 m, 14 Jul 1963. Costa Rica. —BMNH 1956.3.1:3-4, 2(88.5-94.5), 6 mi off Cabo Velas, Papagayos (ca. 10°22’N, 85°53’W), 101 m, 1 Jul 1932.—LACM 33827-55, 4(96.6-119.9), Gulf of Nicoya (ca. 9.5°N, 85°W), 29 Jun 1973. Panama Bay.— UMML 26069, 18(92.4-128.3), 8°00.4—-00.7'N, 79°48 .8-41.5'W, 78 m, 4 May 1967. Peru. — CAS 24189, 11(109.7-145.7), (same as ho- lotype). Diagnosis.—A medium-sized Symphu- rus, reaching 162 mm SL (most specimens 90-140 mm SL), distinguished from all oth- er species in the genus by a unique 1-3-4 ID pattern and the following combination of characters: 105-114 dorsal-fin rays; 91-— 98 anal-fin rays; 57-61 (57 and 61 rare) ver- tebrae; 12 caudal-fin rays; 104-113 scales in a longitudinal series; head length equal to or nearly equal to head width in all but the largest specimens; a well-developed pupillary operculum; a distinct series of rectangular black blotches on the posterior three-fourths of the dorsal fin and along the entire length of the anal fin; an unpigmented peritoneum; a prominent black blotch across the lower half of the operculum; and 9-11 faint crossbars on the head and body begin- Symphurus callopterus, n.sp., holotype, CAS 64023, male 116.9 mm SL; Peru. ning from just behind the eyes and ending just anterior to the base of the caudal fin. Description. —Frequency distributions of meristic data are given in Table 1. ID pat- tern typically 1-3-4 (123 of 191 specimens), less frequently 1-4-3 (23/191), rarely 1-3- 3-3 or 1-4-4. Caudal-fin rays 12 (160 of 165), rarely 11 or 13. Dorsal-fin rays 105-114, usually 109-113, xX = 110.8. Anal-fin rays 91-98, usually 93-97, x = 94.7. Pelvic-fin rays 4. Total vertebrae 57-61, usually 58- 60, rarely 57 or 61, X = 58.9; abdominal vertebrae 9 (3+6). Hypurals 4. Longitudi- nal scale rows 97-114, usually 100-111. Scale rows on head posterior to lower orbit 20-26, usually 22-24. Transverse scales 35— 45, usually 37-41. Body relatively deep, proportionately deeper in larger specimens, 233-296 SL, x = 248; with greatest depth in anterior third of body; body width gradually tapering pos- teriorly giving body lanceolate shape. Preanal length 216-265 SL, x = 236; slightly less than body depth. Head relatively wide (216-278 SL, x = 237), nearly equal to body depth in specimens smaller than 150 mm SL, proportionately smaller than body depth in specimens larger than 150 mm SL. Head length nearly equal to head width (218-261 SL, x = 236). Postorbital length 146-189, X = 163. Lower head lobe (117-158 SL, x = 139) slightly larger than upper head lobe (101-136 SL, x = 118). Snout relatively short, 171-203 HL, xX = 185; covered with small ctenoid scales. Dermal papillae well- developed on blind side of snout. 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Mouth large, 222-271 HL, x = 245; posterior extension of maxilla reaches usu- ally to rear margin of lower eye, less fre- quently extending posteriorly only to rear margin of pupil of lower eye. Chin depth 179-272 HL, X = 207; slightly larger than snout length. Lower eye relatively small, 79- 118 HL, x = 103; eyes usually slightly sub- equal in position with upper slightly in ad- vance of lower eye. Anterior and medial surfaces of eyes partially covered with 3-5 rows of small ctenoid scales; 1—3 small cte- noid scales in narrow interorbital region. Pupillary operculum triangular and well-de- veloped. Length of dorsal-fin base 941-955 SL, x = 948. Dorsal-fin origin far forward; dorsal fin usually reaches anteriorly to a point directly above anterior margin of mi- grating eye, less frequently to anterior mar- gin of pupil and in a few specimens, only to middle of migrating eye; predorsal length 46-59 SL, x = 52. Length of anal-fin base 736-821 SL, X = 760. Blind sides of dorsal and anal fins without scales; 3-5 rows of small scales present on ocular-side bases of dorsal- and anal-fin rays. Pelvic fin with 4 rays; relatively short, 38-63 SL, x = 55; longest pelvic-fin ray reaches to first anal- fin ray. Caudal fin relatively short, 75-94 SL, x = 83. Teeth well-developed on blind side jaws. Teeth on ocular side of premaxilla slender, in single row, usually covering only anterior half or three-fourths of jaw; extending pos- teriorly to point directly below base of an- terior nostril. Teeth on ocular side dentary in single row, usually only extending along anterior three-fourths of dentary, some- times along entire dentary, or only anterior half. Pigmentation. —Specimens in alcohol with a chocolate brown ground color with series of 9-11 faint crossbars of variable width (usually 4—8 scale rows wide) from behind nape to base of caudal fin (holotype with 12 bars); and 10-19 well-defined, rect- angular, or sometimes slightly oval, black blotches alternating with very light areas on 463 median fins. Specimens from southern Mexico, Costa Rica and Panama generally darker than those from other locations. Blind side typically uniformly unpigmented, probably creamy white in life. Some indi- viduals of both sexes also have darkly pig- mented patches concentrated in caudal re- gion and sometimes scattered at various places along bases of dorsal- and anal-fins along posterior half of blind side of body. Head usually with two faint crossbars. Anterior bar about 3-4 scales in width, barely reaching ventral portion of head, and located posteriorly (about 4—5 scales width) to eyes. Well-defined posterior bar about 6- 8 scales wide, crossing opercular region, and extending ventrally slightly onto blind side of head; sometimes somewhat faint and dif- fuse dorsally. Inner lining of eyed-side oper- culum only lightly pigmented, most often only sprinkled with melanophores; blind- side opercular lining usually unpigmented. Isthmus mostly unpigmented except for small patch of melanophores on dorsal sur- face. Posterior two-thirds of dorsal fin and en- tire length of anal fin bear clearly-defined blotches, not extending to either tips or bas- es of rays. Blotches on both fins start ap- proximately equidistant from snout; ante- riormost blotches typically lighter than posterior ones; each blotch usually covers about 5-7 rays. Lighter areas between blotches cover about 3—5 rays and are stip- pled with tiny melanophores producing a faint duskiness barely discernible to naked eye. Median fins on blind side without me- lanophores. Number of black blotches on dorsal fin varies between 10-19. Anterior to point above anal-fin origin, dorsal fin without distinct blotches. Anal-fin blotches usually parallel in position to dorsal-fin blotches and with similar intensity of pig- mentation; usually between 12-15 (one specimen had 8, and another 19 blotches). Holotype with 14 blotches on dorsal and 11 on anal fin. Most posterior portions of me- dian fins heavily pigmented in melanistic 464 Fig. 2. Geographic distribution of Symphurus cal- lopterus based on available study material. Dots in- dicating collection localities may represent more than one occurrence and more than a single specimen from each locality. specimens, obscuring blotches to naked eye (but still perceptible under magnification). Caudal fin generally with two ill-defined blotches, one on the base and the other at distal tip, with lighter space between. Cau- dal-fin blotches may be faded and diffuse giving entire caudal uniformly dark color- ation. In some specimens of both sexes, blind side of caudal fin darkly pigmented. Size and sexual maturity. —Sexual ma- turity occurs at a large size relative to other Symphurus species. Of 53 females, 52, rang- ing in size from 90.8—162 mm SL, were ma- ture with elongate, gravid ovaries. The smallest of these measured 90.8, 93.0, 97.3 and 97.9 mm SL. The only immature fe- male examined was slightly smaller (87.3 mm SL) with ovaries just undergoing pos- terior elongation. The 66 males were only slightly smaller than the females (76.5-151 mm SL). Etymology. — Callopterus meaning ““pret- ty fin” (Greek kallos, beauty; and pterygion, fin, a diminutive form of pteron, wing); in reference to the striking black blotches on the median fins in an otherwise mundanely pigmented group of fishes. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Distribution.—Throughout the tropical eastern Pacific (Fig. 2) from Mazatlan and southern Baja California, Mexico, to north- ern Peru (10°36’S). Symphurus callopterus occurs primarily in moderate depths (18-317 m; SIO 63-522 and UF 47590, respectively) throughout its geographic range. The bathymetric center of abundance, based on both frequency of cap- ture and numerical abundance, occurs on the continental shelf between 60-110 m. Over 85% (244 of 285) of the specimens studied were collected at these depths. Cap- ture of this species at depths less than 60 m is unusual; only five specimens were col- lected between 40-60 m and only three specimens were taken shallower than 40 m (18 and 20 m). Symphurus callopterus has been collected rarely at depths greater than 110 m; only 10 of 285 specimens (4%) were collected deeper than 110 m with the deep- est occurrences reported for single speci- mens being 146, 196, 206 and 317 m. Geographical variation.—No latitudinal variation in meristic characters was ob- served in specimens collected between the northern and southern parts of the geo- graphic range. Remarks.—Two haemal and/or neural spines occurred on the first preural (PU 1) or the second preural centra (PU 2) in 27 of 180 (15%) specimens examined. Two hy- potheses may explain the high frequency of doubling of spines in these centra: 1) PU 1 or PU 2 frequently possess double neural and/or haemal spines, or 2) double spines result from fusion of two caudal vertebrae. The data support the latter hypothesis. In some specimens with two spines on PU 1, that centrum was slightly longer than nor- mal, suggesting that it might be the result of fusion of two centra. Additionally, when two-spined preural centra were counted as a single vertebra (Table 2), specimens with these centra had, as a group, one fewer ver- tebra than the normal specimens (x = 58.0 for double-spined specimens; x = 58.9 for VOLUME 102, NUMBER 2 465 Table 2.—Number of vertebrae in Symphurus callopterus. T-test comparing specimens possessing double neural and/or haemal spines on the PU 1 or PU 2 to those with single spines. Number of vertebrae PU 1/PU 2 spines 57 58 59 60 61 n x SD t jz Double (counted as one centrum) = 19 4 O7.3.0 Zi 53:0. 90:56 6.30 <0.000 Single (normal condition) SS Oe, Da 1 RSS) 758.910.7971 Double (counted as two centra) 0 rms TS 4 0 2h ODO, SOS6i F065 >0.90 Single (normal condition) ERIE S lies: 27 | 1 1532 S829 > 0.71 normal specimens; t = 6.30; P < Q.000). However, when two-spined centra were counted as two vertebrae, there were no sig- nificant differences in total vertebrae be- tween the two groups (x = 59.0 for double- spined group versus 58.9 for “normal” group; t = 0.63, P > 0.90). Because the data support the hypothesis that double spines are the result of vertebral fusion, vertebrae bearing them were counted as two. Co-occurring Symphurus species. —In the shallower portions of its bathymetric range along the coast of Mexico and Central America (at least as far south as Panama), S. callopterus has been collected with S. gor- gonae Chabanaud and S. atramentatus Jor- dan & Bollman; at greater depths in this region, S. callopterus is partially syntopic with an undescribed species. Comparisons.— Other tonguefishes with counts comparable to those of S. callopterus are S. maldivensis Chabanaud, S. marmor- atus Fowler and S. strictus Gilbert from the Indo-West Pacific including Hawaii, S. mi- crolepis Garman from the eastern Pacific, S. ligulatus (Cocco) from the eastern Atlan- tic, and S. jenynsi Evermann & Kendall and S. nebulosus (Goode & Bean) from the west- ern Atlantic. Symphurus callopterus differs from S. microlepis principally in ID pattern (1-3-4 versus 1-3-2) and pigmentation (peritoneum unpigmented and dorsal and anal fins with blotches in S. callopterus ver- sus dark black peritoneum and unpigment- ed fins in S. microlepis). Symphurus callop- terus differs from the other species in ID pattern and number of caudal-fin rays (1-3- 4, 12 versus 1-2-2 and 14, respectively, in S. strictus, S. marmoratus, S. ligulatus and S. nebulosus; 1-4-3 and 10 in S. jenynsi; 1-2-2 and unknown number of caudal-fin rays in S. maldivensis), as well as in features of its pigmentation (peritoneum unpig- mented in S. callopterus versus darkly pig- mented in all of the above species, except S. jenynsi; median fins highly ornate with alternating series of blotches and unpig- mented areas in S. callopterus versus uni- formly pigmented fins in the other species). Other species of Symphurus with similar pigmentation on the median fins are S. atra- mentatus Jordan & Bollman, and an un- described species from the eastern Pacific, as well as S. diomedeanus (Goode & Bean) from the western Atlantic. Symphurus cal- lopterus differs from them in its extremely high number of dorsal- and anal-fin rays and vertebrae and in the larger number of blotches on the fins. In addition, in S. cal- lopterus, head length is nearly equal to head width in all except the largest adults, where- as in the other species, head length is usually less than head width. Throughout its range, S. callopterus is occasionally collected with an undescribed species that has a similar body shape and pigmentation pattern. Sym- phurus callopterus differs from this unde- scribed species in several major features in- cluding ID pattern (1-3-4 versus 1-3-2), hypural number (4 versus 5), presence of a well-developed pupillary operculum versus its absence, pigmentation of the peritoneum 466 (unpigmented versus dark black showing through the abdominal wall), and modal dif- ferences in meristic characters. Material Examined Counts were taken from the following 138 non-type specimens (71.0-162 mm SL): Mexico.—UCLA W61-198, 2(116.0- 131.8), Sinaloa, 3—4 miles southwest of Ma- zatlan (ca. 23.5°N, TOGSSO0AW)2 29 ct 1961.—CAS 4785-4786, 2(93.0-101.9), Michoacan, South of Punta San Telmo off Michoacan coast (ca. 18.3°N, 103°40’W), 19 Jul 1932.—UCLA W56-80, (104.1), Oa- xaca, off Port Angeles Light (ca. 15.5°N, 96°40’W), 14 Jul 1932. Guatemala: —SIO 73-265, 14(71.0—90.0), 13°55.6-53.5'N, 92°02.5'W, 101 m, 13 Apr 1973. Nicara- gua.—SIO 73-279, 3(107.4—116.1), 12°09- 11.5’N, 87°32-35.5'W, 113 m, 17 Apr 1973. Costa Rica.—CAS 5304, (94.2), off Cabo Velas (ca. 10°22'"N, 85°53'W), FOL m. f Jul 1932.—CAS 11710, (119.3), 6 mi off Cabo Velas (ca. 10°22’N, $5°53'W), 1LOb met jul 1932.—LACM 33590-2, 3(105.0—130.0), 9 mi from Isla Herraderra, 17 May 1973.— LACM 33827-11, (124.4), Gulf of Nicoya, central Puntarenas (ca. 9.5°N, 85°W), 29 Jun 1973.—SIO 79-5, 42(76.6—-116.8), Gulf of Papagayo, 10°42.4’N, 85°55’W, 88 m, 02 Apr 1978. Panama Bay.—UMML 26003, 11(76.5-117.6), 7°49.3-49.8'’N, 80°00- 00.7'W, 46 m, 2 May 1967.—UMML 34318, 30(85.8-133.8), 7°40.3’N, 79° 50.9'W, 78 m, 2 May 1967. Colombia. — UMML 34319, (124.5), 4°00’N, 77°30'W, 92 m, 17 Sep 1961. Ecuador. —CAS 24195, 3(140.6—-162), 2°29’'S, 80°59'W, 93 m, 11 Sep 1966.—CAS 24198, (131.2), 3°35’S, 78°35'W, 79 m, 16 Sep 1966. Peru.—CAS 24188, 10(114.9-140.1), 5°59’S, 81°12’W, 100 m, 4 Jun 1966.—CAS 24190, (112.2), 6°20’S, 81°01’ W, 146 m, 4 Jun 1966.—CAS 2AITST SCiS1 35-1513). 62S. st 36 Ww. 100 m, 5 Jun 1966.—CAS 24957, (129.2), 6°21’S, 80°59’W, 140 m, 4 Jun 1966.—CAS 24192, 2(122.2—139.2), 6°24’S, 80°44’W, 20 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON m, 5 Jun 1966.—CAS 24194, 2(111.3- 132.6), 4°55’S, 81°19'W, 70 m, 8 Sep 1966.— UCLA W58-395, 3(106.5—123.5), 10°36’S, 77°54'W, 16 Oct 1958. Additional material examined but not counted or measured (97 specimens; 52.2— 143.1 mm SL): Mexico.—SIO 64-878, 2(55.9-58.7), Baja California, 24°18.9- 19.0'N, 111°47.6-48.6'W, 78 m, 13 Nov 1964.—SIO 62-75, (52.2), Sinaloa, 22°15’N, 106°03’W, 55 m, 25 Aug 1961.—SIO 62- 76, 23 (73.1-116.0), 22°13’N, 106°10’W, 79 m, 25 Aug 1961.—SIO 73-230, (89.9), 21°59'N, 106°20’W, 102 m, 30 Mar 1973.— SIO 73-232, 8(82.8-103.6), 21°57—-S6’N, 106°10-11'W, 52 m, 31 Mar 1973. Mexico, Gulf of Tehuantepec. —SIO 63-504, (113.0), 15°57.5'N, 95°00’W, 61 m; 8 Jul 1963.— SIO 65-165, (62.0), 15°55’N, 95°24’W, 102 m, 6-7 Jun 1965.—SIO 63-525, (104.2), 15°52’N, 95°43’W, 55 m, 15 Jul 1963.—SIO 63-522, (89.5), 15°44’N, 96°06.5’W, 18 m, 15 Jul 1963.—SIO 63-523, 2(70.5-89.1), 15°41'N, 96°07.5'W, 55 m, 15 Jul 1963.— SIO 63-513, (96.5), 15°07.5'N, 93°25’W, 102 m, 10 Jul 1963. Guatemala.—SIO 73-265, 4(81.0-92.0), 13°55.6-53.5'N, 92°02.5'W, 100 m, 13 Apr 1973. Costa Rica.—CAS 20965, (82.5), 6 mi off Cabo Velas (ca. 10°22'N, 85°53'W),; 101 m,; Igelies2 CAS 43880, (114.5), Cabo Blanco (ca. 9.5°N, 85°W), 206 m, 9 Mar 1974.—CAS 44140, (111.6), Gulf of Nicoya (ca. 9.5°N, 85°W), 83 m, 14 Mar 1974.—SIO 73-281, (103.1), 10°50.2—53.2'N, 86°20.0—24.3’W, 196 m, 18 Apr 1973.—SIO 73-296, 26(83-126.5), 9°37.4—37.7'N, 84°49.0-51.8'W, 87 m, 22 Apr 1973. Gulf of Panama.—CAS 24958, 2(115.5-117.2), 8°11'N, 79°36'W, 88 m, 23 Jul 1967.—CAS 24959, 3(127.5-143.1), 6°34'’N, 77°21'20”W, 60 m, 21 Apr 1967. Colombia.—CAS 24960, 6(121.5-132.0), 6°44'N, 77°33'30’W, 82 m, 10 Aug 1967. Acknowledgments We thank the following people who as- sisted with this study: R. Gibbons (photog- VOLUME 102, NUMBER 2 raphy and map preparation) and M. Nizin- ski (radiographs and technical support); the following curators and support staff who generously provided space and arranged for loan of specimens: S. Jewett (USNM); A. Wheeler (BMNH); R. Rosenblatt, D. Gib- bons, H. J. Walker (SIO); R. Lavenberg, J. Seigel, R. Feeney (LACM); C. Gilbert, G. Burgess (FSU); C. R. Robins (UMML); W. Eschmeyer, M. E. Anderson, D. Catania (CAS); and D. Buth (UCLA). The manu- script was much improved through critical reviews by B. B. Collette, G. D. Johnson, N. Menezes, R. Rosenblatt and R. P. Vari. Portions of this study were initiated while the senior author was a postdoctoral fellow in the Division of Fishes at the USNM. Travel funds enabling Munroe to work at UMML in 1982 were provided by the De- partment of Fisheries, Virginia Institute of Marine Science. A special thanks to W. Bussing, Univer- sity of Costa Rica, for allowing us to use information contained in his unpublished manuscript on the tonguefishes of Costa Rica. Literature Cited Bartels, C. E., K. S. Price, M. I. Lopez, & W. A. Bussing. 1983. Occurrence, distribution, abundance and diversity of fishes in the Gulf of Nicoya, Costa Rica.— Revista De Biologia Tropical 31(1):75- 101. —_. : , & 1984. Ecological assessment of finfish as indicators of habitats in the Gulf of Nicoya, Costa Rica.— Hydrobiologia 112:197-207. Chirichigno, F. N. 1974. Clave para identificar los peces marinos del Peru. —Informes Instituto del Mar del Pert: 44: 1-387. 467 Eschmeyer, W. N., E.S. Herald, & H. Hammann. 1983. A field guide to Pacific coast fishes from the Gulf of Alaska to Baja California. Boston, Massa- chusetts, Houghton Mifflin Company, 336 pp. Ginsburg, I. 1951. Western Atlantic tonguefishes with descriptions of six new species.— Zoologica, N.Y., 36(3):185-201. Hildebrand, S. F. 1946. A descriptive catalog of the shore fishes of Peru.— United States National Museum Bulletin 189:1-—530. Jordan, D. S., & B. W. Evermann. 1898. The fishes of North and Middle America.— United States National Museum Bulletin 47(3):2183-3136. Love, M.S., G. E. McGowen, W. Westphal, R. J. Lav- enberg, & L. Martin. 1984. Aspects of the life history and fishery of the white croaker, Geny- onemus lineatus (Sciaenidae), off California. — Fishery Bulletin, U.S. 82(1):179-198. Mahadeva, N. 1956. A review of the tonguefishes of the eastern Pacific, with descriptions of six new species. Unpublished dissertation, University of California at Los Angeles. 272 pp. Meek, S. E., & S. F. Hildebrand. 1928. The marine fishes of Panama.—Field Museum of Natural History, Publication 249, Zoological Series Vol- ume 15 (Part 3):709-1045. Menezes, N. A., & G. de Q. Benvegnu. 1976. On the species of the genus Symphurus from the Bra- zilian coast, with descriptions of two new species (Osteichthyes, Pleuronectiformes, Cynoglossi- dae).—Papeis Avulsos de Zoologia, Sao Paulo 30(11):137-170. Munroe, T. A. 1987. A systematic revision of Atlan- tic tonguefishes (Symphurus: Cynoglossidae: Pleuronectiformes) with a preliminary hypoth- esis of species group relationships. Unpublished dissertation, College of William and Mary, Wil- liamsburg, Virginia. 598 pp. (TAM) National Marine Fisheries Ser- vice, Systematics Laboratory, National Mu- seum of Natural History, Washington, D.C. 20560; (MNM) Department of Biology, Wisconsin State University, Oshkosh, Wis- consin 54901. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 468-482 SYSTEMATICS OF THE STEINDACHNERINA HYPOSTOMA COMPLEX (PISCES, OSTARIPHYSI, CURIMATIDAE), WITH THE DESCRIPTION OF THREE NEW SPECIES Richard P. Vari and Ann Williams Vari Abstract. — The Steindachnerina hyposoma complex is revised and four species are recognized: S. hypostoma (Boulenger) widely distributed through the Rio Amazonas system upstream of Manaus; S. planiventris, new species, from the Rio Negro and Rio Madeira basins, and various localities along the Rio Ama- zonas upstream of Manaus; S. gracilis, new species, apparently endemic to the Rio Tocantins system of eastern Brazil; and S. quasimodoi, new species, of the western portions of the Amazon basin in Brazil and Peru. The four species have in common derived expansions of the mesethmoid and frontals that result in a reduction in the size of the cranial fontanel, and unite them as a mono- phyletic assemblage. A key to the species of the complex is provided. Resumo.—O complexo Steindachnerina hypostoma € revisto e quatro es- pécies reconhecidas: S. hypostoma (Boulenger) amplamente distribuida no sis- tema do Rio Amazonas, acima de Manaus; S. planiventris, espécie nova, das bacias do Rio Negro e do Rio Madeira e varias localidades ao longo do Rio Solimoes acima de Manaus; S. gracilis, espécie nova, aparentemente endémica da bacia do Rio Tocantins no leste do Brasil; e S. guasimodoi, espécie nova, da parte oeste da Bacia AmazoOnica, no Brasil e Peru. As quatro espécies tém em commum expansoes derivadas do mesetmoide e frontais que causam a reducao em tamanho da fontanela craniana e unem estas quatro espécies em um grupo monofilético. Uma chave para as espécies do grupo é apresentada. Boulenger (1887:172) described Curi- matus hypostoma on the basis of four spec- imens collected by “Mr. W. Davis’ in the ‘““Ucayali River’? of Peru. At the end of his brief description, he noted the very shallow body depth characteristic of the species. That feature is indeed striking when one com- pares this species to other curimatids, most of which have moderately to very deep bod- les (see figures in Vari, 1982, 1984, in press a, b, c). Although this unusually shaped species was subsequently referred to by Ei- genmann & Eigenmann (1891), Eigenmann (1910), Fowler (1942, 1950, 1975), and Fer- nandez-Yépez (1948), among others, those citations were based on the original descrip- tion without examination of other speci- mens. The only subsequent locality record of Curimatus hypostoma based on addi- tional material was that of Eigenmann and Allen (1942:296) who reported on a series of specimens from various localities in the Amazon basin in Peru. Most recently Vari (1989) assigned Curimatus hypostoma to the speciose genus Steindachnerina Fowler. The limited number of references in the litera- ture to Steindachnerina hypostoma are rath- er surprising given that the species is rela- tively common in many of the major river systems of the Amazon basin, and has a geographic distribution much wider than re- ported in the literature. Collecting efforts in recent years through- out the Amazon basin have yielded large VOLUME 102, NUMBER 2 series of specimens typically identified as Curimatus hypostoma. The examination of these collections undertaken as part of more encompassing studies within the Curima- tidae has revealed that this material actually encompasses four distinct, albeit similar, species that form a monophyletic subunit of the Curimatidae. The known distribution of the species of the clade encompasses both the main Rio Amazonas basin and the as- sociated Rio Tocantins system of eastern Brazil. The shared derived features of these species are discussed, and a key to, and de- scriptions of the species are provided. Materials and methods. —Counts and measurements were taken using the meth- ods outlined in Vari (1982, 1984, in press a, b, c). In the case of new species the pre- sented ranges of counts and measurements include values of all type specimens. The ranges of these values for Steindachnerina hypostoma include all specimens cited for which standard lengths (SL) are given. Val- ues in square brackets in species descrip- tions are those of the holotype or lectotype. Information on localities and specimens ex- amined in detail is arranged as in Vari (1982, 1984, in press a, b, c). Measurements are presented as proportions of standard length (SL) or head length (HL). The following abbreviations for institu- tions are used: American Museum of Nat- ural History, New York (AMNH); British Museum (Natural History), London (BMNH); California Academy of Sciences, San Francisco (CAS); Stanford University, now deposited at CAS (CAS-SU); Jacques Gery, personal collection (GC); Indiana University, collections now at various re- positories (IU); Los Angeles County Mu- seum of Natural History (LACM); Museum of Comparative Zoology, Cambridge (MCZ); Museu de Zoologia da Universidade de Sao Paulo (MZUSP); Naturhistoriska Riksmu- seet, Stockholm (NRM); Naturhistorisches Museum, Vienna (NMW); Museo de His- toria Natural de la Universidad Nacional Mayor de San Marcos, Lima (MHN-USM); 469 and National Museum of Natural History, Smithsonian Institution, Washington, D.C. (USNM). Steindachnerina hypostoma complex Vari (1989) redefined Steindachnerina Fowler (1906) to include 32 nominal species or subspecies. Vari and Castro (1988) sub- sequently noted that Prochilodus stigma- turus Fowler is also a curimatid of the genus Steindachnerina rather than a prochilodon- tid. Steindachnerina has a wide distribution in lowland tropical South America on both sides of the Andean Cordilleras, but is by far most speciose in the Amazon basin, the region to which the Steindachnerina hypos- toma complex is endemic. The members of Steindachnerina share a series of synapo- morphous features of the first and second infraphyarnygobranchials, the mode of at- tachment of the ligament joining the second and third hypobranchials, and the form of the basihyal and its associated tooth-plate (see Vari [1989] synapomorphies 97 to 100). The four species of the Steindachnerina hy- postoma complex are, in turn, characterized by derived modifications of the meseth- moid and frontals of lesser universality that are reflected in the relative size and form of the cranial fontanel. Species of Steindachnerina outside of the hypostoma complex and curimatids in gen- eral have relatively extensive dorsomedian cranial fontanels extending from the supra- occipital to the mesethmoid (e.g., S. bi- maculata, Fig. 1A). In those outgroup taxa the anterior two-thirds of the relatively large opening is delimited laterally by widely sep- arated frontals. The medial margins of the frontals anterior to the epiphyseal bar are nearly parallel or converge very gradually anteriorly. Anteriorly the fontanel is bor- dered by a distinct notch situated in the middle of the posterior border of the mes- ethmoid. This arrangement of bones along an extensive fontanel is hypothesized as primitive within Steindachnerina given its 470 D Fig. 1. Dorsal view of anterior portion of cranial fontanel and proximate bones of A) Steindachnerina bimaculata, USNM 261450, 76.4 mm SL; B) Stein- dachnerina quasimodoi, USNM 293042, 76.0 mm SL; C) Steindachnerina planiventris, USNM 267987, 62.1 mm SL; D) Steindachnerina gracilis, USNM 293034, 63.4 mm SL; and E) Steindachnerina hypostoma, CAS 63192 (formerly IU 15825), 82.00 mm SL. Abbrevi- ations: EB—epiphyseal bar; FR—frontal; ME—mes- ethmoid; P—Parietals. Mesethmoid and parietals trun- cated, horizontal lines indicate cranial fontanel. general distribution in that genus and other curimatids. The species of the S. hypostoma complex demonstrate marked changes in the mor- phology of those portions of the meseth- moid and frontals bordering the cranial fon- tanel. All four species lack the extension of the fontanel into the posterior portion of the mesethmoid. The posteromedial region of the mesethmoid is instead developed posteriorly into a triangular process (Fig. 1B to E). More striking is the expansion in all four species of the anteromedial portions of the frontals and the associated pronounced reduction of the portion of the cranial fon- tanel anterior of the epiphyseal bar. As a consequence of this expansion the antero- medial margins of the frontals no longer extend roughly in parallel. The margins of the bones instead converge and are either separated by a small gap (Steindachnerina quasimodoi, Fig. 1B), or are in contact me- dially to varying degrees (S. planiventris, S. gracilis, S. hypostoma, Fig. 1C-E). PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Both the extension of the posteromedial portion of the mesethmoid and the medial expansion of the frontals in the four species of the Steindachnerina hypostoma complex are derived relative to the conditions of these bones in outgroups. These synapomorphies support a hypothesis that S. hypostoma, S. gracilis, S. quasimodoi, and S. planiventris are a monophyletic lineage within Stein- dachnerina. Key to the species of the Steindachnerina hypostoma complex 1. Dorsal fin plain, without dark spot at base of middle rays; snout length 0.28—0.31 of HL; lateral-line scales to hypural joint 46 to 50 ........ S. hypostoma (Boulenger) — Dorsal fin with dark spot at base of middle rays, spot sometimes faint; snout length 0.31—0.34 of HL; lat- eral line scales to hypural joint 40 to 46 or 50 to 54 2. Lateral-line scales to hypural joint SOHOmas . ae. S. gracilis, new species — Lateral line scales to hypural joint 40 to 46 3. Greatest body depth in specimens over 50 mm SL 0.30-0.34 of SL, body with distinctly humped dorsal profile (Figs. 6, 7); frontals separated by slight gap anteriorly (Fig. 1B) esheets S. quasimodoi, new species — Greatest body depth in specimens over 50 mm SL 0.27-0.34 of SL, dorsal profile of body without dis- tinct hump (Fig. 11); frontals in con- tact anteriorly (Fig. 1\C) eee a Gikas Pass S. planiventris, new species Steindachnerina hypostoma (Boulenger, 1887) Figs. 1-4, Table 1 Curimatus hypostoma Boulenger, 1887:172 [type locality: Ucayali River ].— Vari, 1989:tabs. 2, 3 [phylogenetic relation- ships]. VOLUME 102, NUMBER 2 7 > 7? a8 as a es ~~ = ~ s : +o>04 =a ss a 4 = . " E>. *Sess ~3RBar > a Pf = Li bee 53.3 DEVILS 471 a* 8480995 > %: — Fig. 2. Steindachnerina hypostoma, USNM 229190, 93.2 mm SL; Brazil, Amazonas, Rio Solimoes, Ilha Machantaria. Curimatus hypostomus, Eigenmann & Ei- genmann, 1889:426 [reference].—Eigen- mann & Eigenmann, 1891:47 [refer- ence].—Eigenmann, 1910:422 [reference]. Curimata hypostoma, Fowler, 1942:208 [reference].— Fowler, 1945:116 [refer- ence].—Eigenmann & Allen, 1942:296 [Peru: Rio Huallaga, Yurimaguas; Rio Morona; Rio Paranapura, Yurimaguas (in part)].— Fowler, 1945:116 [reference].— Géry, 1977:235 [reference].—Ortega & Vari, 1986:11 [Peru, Amazon basin; com- mon name]. Curimata hypostoma hypostoma, Fowler, 1950:285 [literature compilation]. Steindachnerina hypostomus, Fernandez- Yépez, 1948:58 [assignment to Stein- dachnerina]. Steindachnerina hypostoma, Fowler, 1975: 375 [reference]. Diagnosis. —The absence of a discrete patch of dark pigmentation at the base of the middle rays of the dorsal fin distinguish- es S. hypostoma from the other members of the complex, all of which have such pig- mentation developed to some degree. The 46 to 50 lateral line scales of S. hypostoma further differentiate the species from S. gra- cilis which has 50 to 54 scales in that series and from S. guasimodoi and S. planiventris which have 40 to 46. Differences in other meristic and morphometric features also discriminate S. hypostoma from the re- maining members of the complex (Table 1). Description.—Body elongate, relatively wide, particularly in ripe females. Dorsal profile of head straight or very slightly con- vex. Dorsal profile of body smoothly curved, slightly convex from rear of head to origin of dorsal fin; straighter and slightly postero- Fig. 3. Steindachnerina hypostoma, USNM 278579, 48.9 mm SL; Bolivia, Pando, Rio Madre de Dios, Laguna San Luis. 472 Fig. 4. Map of northern South America showing geographic distribution of Steindachnerina hypostoma (dots) and Steindachnerina gracilis (stars). Type local- ities: 1, Rio Aripuana, Aruana; 2, Rio Tocantins, Tu- curui; and 3, Rio Ucayali (exact collection site of syn- types of Curimatus hypostoma unknown). Some symbols represent more than one lot and/or collecting locality. ventrally slanted at base of dorsal fin, straight or very gently convex from base of last dor- sal-fin ray to caudal peduncle. Dorsal sur- face of body with distinct median keel an- terior to dorsal fin, keel more pronounced proximate to fin; body surface smoothly rounded transversely posterior to fin. Ven- tral profile of body very gently curved from tip of lower jaw to caudal peduncle. Pre- pelvic region wide, distinctly flattened, with five series of scales in transverse series across flattened surface. Pelvic fins distinctly sep- arated medially. Post-pelvic region some- what flattened proximate to pelvic fin, grad- ually becoming transversely rounded posteriorly. Greatest body depth at origin of dorsal fin, depth 0.24—0.27 [0.25]; snout tip to or- igin of dorsal fin 0.44—0.48 [0.45]; snout tip to origin of anal fin 0.80-0.85 [0.82]; snout tip to insertion of pelvic fin 0.48-0.53 [0.48]; snout tip to anus 0.70-0.75 [0.72]; origin of dorsal fin to hypural joint 0.56—0.60 [0.59]. Dorsal-fin margin pointed; anteriormost rays 2.8-3.5 times length of ultimate ray. Pectoral-fin margin pointed; length of pec- toral fin 0.17-0.20 [0.18], extends slightly PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON over three-quarters of distance to vertical through insertion of pelvic fin. Pelvic-fin margin obtusely pointed, length of pelvic fin 0.19-0.22 [0.20], reaches about three- fifths of distance to origin of anal fin. Caudal fin distinctly forked. Adipose dorsal fin well developed. Anal fin emarginate, anterior- most branched rays approximately two and one-half times length of ultimate ray. Cau- dal peduncle depth 0.11-—0.12 [0.11]. Head distinctly pointed in profile, more so in larger specimens, head length 0.24— 0.28 [0.27]; upper jaw distinctly longer than lower, mouth inferior; snout length 0.28- 0.31 [0.28]; nostrils very close, anterior cir- cular, posterior crescent-shaped with aper- ture closed by thin flap of skin separating nares; orbital diameter 0.28-0.34 [0.29]; adipose eyelid present, poorly developed, with rotund opening over center of eye; length of postorbital portion of head 0.39- 0.45 [0.43]; gape width 0.28—0.34; interor- bital width 0.38—-0.42 [0.39]. Pored lateral line scales from supraclei- thrum to hypural joint 46 to 50 [49]; all scales of lateral line pored, canals in scales straight; 4 to 6 series of scales extend beyond hypural joint onto caudal fin base; 8'2 to 914 [814] scales in transverse series from origin of dorsal fin to lateral line; 642 to 7% [7] scales in transverse series from lateral line to origin of anal fin. Dorsal-fin rays 11,9 or 111,9 (111,9 rare, when three unbranched rays present, first very short) [11,9]; anal-fin rays 1,7 or i11,7 (when three unbranched rays present, first very short) [11,7]; pectoral-fin rays 14 to 16 [14]; pelvic-fin rays 1,8 [1,8]. Total vertebrae 35 (8), 36 (86), 37 (2). Color in alcohol. —Overall coloration of specimens retaining guanine on scales sil- very to silvery-golden, darker on dorsal por- tions of head and body. Specimens fixed in formalin and lacking guanine on scales with overall ground coloration tan to light brown, darker on dorsal portions of head and body (Fig. 2). Pores of lateral line scales outlined by dark pigmentation in some specimens. VOLUME 102, NUMBER 2 473 Table 1.—Range of morphometrics and meristic features of species useful in discriminating species of Stein- dachnerina hypostoma complex. Measurements | to 4 are proportions of standard length; 5 to 7 are proportions of head length. hypostoma gracilis quasimodoi planiventris Morphometrics 1. Greatest body depth 0.24-0.27 0.25-0.27 0.27-0.34* 0.27-0.30 2. Snout to pelvic-fin origin 0.48-0.53 0.53-0.55 0.50-0.54 0.52-0.56 3. Snout to anus 0.70-0.75 0.73-0.75 0.75-0.76 0.72-0.76 4. Pelvic-fin length 0.19-0.22 0.19-0.21 0.23-0.26 0.19-0.23 5. Snout length 0.28-0.31 0.31-0.34 0.31-0.34 0.33-0.36 6. Orbital diameter 0.28-0.34 0.32-0.35 0.31-0.37 0.29-0.33 7. Postorbital length 0.39-0.45 0.39-0.42 0.36-0.40 0.36-0.41 Meristics Lateral line scales 45-50 50-54 40-46 40-46 Scale rows between dorsal-fin origin and lateral line 814-9 10-10% Th-9 614-8 Scale rows between anal-fin origin and lateral line 612-72 6'h-7'h Sh-6"2 Sh-6%/ * 0.30-0.34 in specimens of 50 mm SL or greater. Lateral line pigmentation more intense, when present, in smaller individuals, some- times forming distinct mid-lateral stripe (Fig. 3). Deeper lying dusky mid-lateral band extends from supracleithrum to caudal pe- duncle; typically more obvious in smaller individuals; masked in specimens retaining guanine on scales. Caudal-fin rays outlined by series of small chromatophores, lower lobe of caudal fin dusky. Anterior margin of dorsal fin sometimes dusky, but without spot of dark pigmentation at base of middle rays; other fins hyaline. Distribution.—Amazon basin upstream of Manaus, Brazil (Fig. 4). Common name.—Chio—chio (Ortega & Vari, 1986:11, Peru). Remarks. —Boulenger (1887a) described Curimatus hypostoma on the basis of four specimens from an unspecified location along the Rio Ucayali of Peru. An 87.5 mm SL syntype (BMNH 1881.5.13:105), which is in the best overall condition, is designated as the lectotype. The remaining specimens in the type series (BMNH 1881.5.13:106- 108) thus become paralectotypes. Allen Gn Eigenmann & Allen 1942:297) described a nominal subspecies Curimata hypostoma hastata on the basis of a single specimen from Puerto Bermudez, on the Rio Pichis, Peru. A re-examination of the ho- lotype (CAS 19881, formerly IU 17859) re- veals that although it is a member of the Steindachnerina clade, it is not conspecific with S. hypostoma, and indeed is not even a member of the S. hypostoma complex, but rather a specimen of S. dobula (Gunther). The specimens identified by Eigenmann & Allen (1942:296) as Curimatus hypostoma are an admixture of S. hypostoma and S. dobula (e.g., IU 17858 from Yurimaguas, Rio Paranapura). The complexity of that series of specimens may account, at least in part, for Allen’s assignment of hastata as a subspecies of hypostoma. Material examined. —286 specimens (70, 55.1—98.3). PERU: Ucayali River, BMNH 1881.5.13: 105, 1 (87.5, lectotype of Curimatus hypo- stoma); BMNH 1881.5.13:106-108, 3 (85.5—90.0, paralectotypes of Curimatus hy- postoma). Loreto; Shansho Cano, USNM 175867, 1. Beirut, near mouth of Rio Am- biyacu, USNM 261452, 2 (76.3-77.8). Rio Javari, near Petropolis, USNM 261438, 1 (78.3). Rio Amazonas, Ramon Castilla, 474 USNM 261512, 1 (79.6). Rio Javari system, Rio Galvez near mouth, NRM SOK/ 1984314.4058, 3. Rio Huallaga, Yurima- guas, USNM 293094, 1 (98.3); CAS 63191, 2 (84.0-86.8, formerly IU 17858); USNM 167802, 5 (83.0—-91.3); CAS 63192, 3 (83.8- 92.0; formerly IU 15825). Yurimaguas, Rio Paranapura, IU 17858, 2 (part of lot). Huanuco; Rio Pachitea, Tournavista, USNM 293092, 1. Ucayali; Rio Ucayali, Pucallpa, USNM 261513, 5 (80.1-91.2); USNM 261489, 5 (65.8—96.5); USNM 261465, 6 (3, 55.3-59.8); USNM 261477, 5 (3, 70.4-83.4); AMNH 35686, 1 (70.0); USNM 261493, 6; USNM 261496, 2; USNM 261488, 6; USNM 293087, 1. Rio Neshuyo where crossed by Pucallpa-Huan- uco Road, USNM 261401, 1. Rio Ucayali, Masisea, USNM 243237, 3 (60.4—63.4); USNM 293090, 5; USNM 293095, 10. Rio Ucayali, Nuevo San Juan near Masisea, USNM 293089, 3. Rio Ucayali, Utuquinia, USNM 293091, 1. BRAZIL: Amazonas; Ilha da Machantaria, USNM 293096, 1 (89.0); GC, 3 (86.3-—92.0); USNM 229190, 1 (94.1); USNM 229187, 1; USNM 229185, 2. Lago Janauaca and vicinity, MZUSP 21699, 2. Rio Solimoes, Fonte Boa, MZUSP 2094756) (7 TS=92/8) MZAUSPH 2095712 (81.5-84.9). Rio Jurua, BMNH 1897.12.1: 88-100, 8 (4, 55.1-60.7). Ilha Xibeco, Rio Solimoes above mouth of Rio Jutai, MZUSP 2VOLTSE1(94.4) = MZUSP) 2 10172683 7933= 83.7). Rio Solimoes, Ilha Sorubim above Coari, MZUSP 20926, 161 (6, 68.5-84.5). Rio Solim6ées, Tefé, mouth of Rio Japura, MZUSP 27360, 1. Rio Solimoes, Benjamin Constant, ‘Costa do*Capacétes MZUSP 27379, 1. Santo Antonio do Ica, mouth of Rio Ica, MZUSP 21000, 4 (75.0-82.8). Steindachnerina gracilis, new species Figs. 1, 4-5, Table 1 Diagnosis.—The 50 to 54 scales in the lateral line to the hypural joint and 10 or 104 scales above the lateral line to the or- igin of the dorsal fin distinguish S. gracilis PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON from S. planiventris and S. quasimodoi which have 40 to 46 lateral line scales and 7'2 to 8% and 7% to 9% scales above the lateral line respectively, and from S. hy- postoma which has 46 to 50 lateral line scales and 8'2 to 9% scales above the lateral line. Steindachnerina gracilis, which has a spot of dark pigmentation at the base of the mid- dle rays of the dorsal fin 1s readily separable from S. hypostoma which lacks such pig- mentation. A variety of meristic and mor- phometric features also distinguish S. graci- lis from the three other species within the complex (Table 1). Description. — Body elongate, moderately wide transversely. Dorsal profile of head straight or very slightly concave. Dorsal profile of body straight or very slightly con- vex from rear of head to origin of dorsal fin; Straight and very slightly posteroventrally slanted at base of dorsal fin, straight or gently convex from base of last dorsal-fin ray to caudal peduncle. Dorsal surface of body with distinct median keel anterior to dorsal fin, keel more pronounced proximate to dorsal fin; body surface smoothly rounded trans- versely posterior to fin. Ventral profile of body very slightly convex from tip of lower jaw to caudal peduncle. Pre-pelvic region wide, distinctly flattened transversely, with obtuse lateral angles in body wall, five series of scales transversely across flattened region. Pelvic fins distinctly separated medially. Post-pelvic region somewhat flattened proximate to pelvic fin, gradually becoming transversely rounded posteriorly. Greatest body depth at origin of dorsal fin, depth 0.25—0.27 [0.26]; snout tip to or- igin of dorsal fin 0.46—-0.49 [0.46]; snout tip to origin of anal fin 0.84—0.86 [0.83]; snout tip to insertion of pelvic fin 0.53-0.55 [0.53]; snout tip to anus 0.73-0.75 [0.73]; origin of dorsal fin to hypural joint 0.54—0.58 [0.56]. Dorsal-fin margin obtusely pointed, ante- riormost rays slightly less than three times length of ultimate ray. Pectoral-fin margin pointed; length of pectoral fin 0.17—0.21 [0.19], extends about three-quarters dis- VOLUME 102, NUMBER 2 ae e: B®, _ aids. geen od Fig. 5. Araguaia, Aruana. tance to vertical line through insertion of pelvic fin. Pelvic-fin margin obtusely point- ed, length of pelvic fin 0.19-0.21 [0.20], reaches about three-fifths distance to origin of anal fin. Caudal fin distinctly forked. Adi- pose dorsal fin well developed. Border of anal fin emarginate, anteriormost branched rays about two and one-half times length of ultimate ray. Caudal peduncle depth 0.11- O20. 11]. Head distinctly pointed in profile, head length 0.27—0.29 [0.27]; upper jaw distinctly longer than lower, mouth inferior; snout length 0.31-0.34 [0.32]; nostrils very close, anterior circular, posterior crescent-shaped with aperture closed by thin flap of skin separating nares; orbital diameter 0.32-0.35 [0.32]; adipose eyelid poorly developed, with rotund opening over center of eye; length of postorbital portion of head 0.39-0.42 [0.39]; gape width 0.32-0.35 [0.33]; interorbital width 0.39-—0.42 [0.41]. Pored lateral line scales from supraclei- thrum to hypural joint 50 to 54 [53]; all scales of lateral line pored, canals in scales straight; 3 to 5 series of scales extend beyond hypural joint onto caudal fin base; 10 to 10'4 [1014] scales in transverse series from origin of dorsal fin to lateral line; 612 to 7!2 [74] scales in transverse series from lateral line to origin of anal fin. Dorsal-fin rays 11,9 or 11,9 (when three unbranched rays present, first very short) [11,9]; anal-fin rays 11,7 or 111,7 (when three unbranched rays present, first very short) [11,7]; pectoral-fin rays 15 to 17 [16]; pelvic- fin rays 1,8 [1,8]. 475 Steindachnerina gracilis, new species, holotype, MZUSP 4857, 63.5 mm SL; Brazil, Goias, Rio Total vertebrae 35 (8), 36 (5). Color in alcohol. —Overall coloration of specimens retaining guanine on scales sil- very golden, darker on dorsal portions of head and body. Overall coloration of spec- imens fixed in formalin and lacking guanine on scales tan to light brown, darker on dor- sal portions of head and body. Pores of lat- eral line scales outlined by dark pigmenta- tion, spots forming irregular mid-lateral stripe. Deeper lying dusky stripe extending from supracleithrum to caudal peduncle, stripe masked in individuals retaining gua- nine on scales. Anterior margin and distal portions of dorsal fin dusky. Distinct dusky spot on middle rays of dorsal fin slightly above their insertion, spot faint in some in- dividuals. Rays of caudal fin outlined by series of small chromatophores; lower lobe of caudal fin dusky. Other fins hyaline. Distribution. —Rio Tocantins system (Fig. 4). Etymology. —The name gracilis, from the Latin for slender, refers to the relatively elongate body of the species. Type material. — 16 specimens, 56.7—73.4 mm SL. Holotype.—BRAZIL. Goids. Rio Ara- guaia, Aruana (approx. 14°54’S, 51°05’W), 63.5 mm SL; Excursion de Departamento de Zoologia (now MZUSP), MZUSP 4847, 15 to 19 Sep 1966. Paratypes.—BRAZIL: Goids; Rio Ara- guaia, Aruana, MZUSP 38591, 2 (56.7-63.5; taken with holotype); USNM 293035, 1 (67.2; taken with holotype); USNM 191632, 1 (approx. 73.4), H. A. Axelrod, 1960. Para: 476 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 6. Steindachnerina quasimodoi, new species, holotype, USNM 293041, 88.9 mm SL; Peru, Loreto, Rio Yavari, near Petropolis. Rio Tocantins, lagoons along margin of riv- er near Tucurui (approx. 3°42’S, 49°27'W), MZUSP 38592, 6 (61.5-64.9); USNM 293034, 6 (57.4-65.4, 2 specimens cleared and counterstained for cartilage and bone), Expedicao Permanente da Amazonas, 14 Sep 1970. Steindachnerina quasimodoi, new species Figs. 1, 6-10, Table 1 Diagnosis. — The 40 to 46 lateral line scales to the hypural joint distinguish S. quasi- modoi from S. gracilis which has 50 to 54 scales in that series and S. hypostoma which has 46 to SO. The presence of a discrete spot of dark pigmentation in the basal portions of the middle rays of the dorsal fin further separates S. guasimodoi from S. hypostoma which lacks that pigmentation. Other dif- ferences in meristic and morphometric fea- tures further differentiate S. quasimodoi Pigs: opposite Colonia Angamos, Peru. from S. hypostoma and S. gracilis (Table 1). Specimens of S. quasimodoi of greater than 50 mm SL are distinguished from com- parably sized individuals of S. planiventris in their greatest body depths (0.30-0.34 of SL versus 0.27—0.30, Fig. 8), by differences in the degree of convexity of the dorsal sur- face of the body (Figs. 6, 7, 11), length of the pelvic fins (0.23-0.26 of SL versus 0.19- 0.23, Fig. 9), and degree of contact of fron- tals anterior to cranial fontanel (Fig. 1B, C). The relative orbital width and length of the postorbital region of the head also discrim- inate the species to a degree (Table 1). Description. —Body elongate, deeper bodied in larger specimens, somewhat com- pressed laterally. Dorsal profile of head slightly convex anterior to vertical through nostrils, striaght from that line to rear of head. Dorsal profile of body slightly convex from rear of head to origin of dorsal fin, slope more pronounced with increasing size; Steindachnerina quasimodoi, new species, paratype, USNM 283040, 53.7 mm SL; Brazil, Rio Javari, VOLUME 102, NUMBER 2 GBD Fig. 8. Plot of greatest body depth (GBD) against standard length (SL), both in millimeters, and regres- sion lines for Steindachnerina quasimodoi (dots, Y = —4.052 + 0.380X) and Steindachnerina planiventris (stars, Y —4.089 + 0.351X) (some symbols represent more than one data point). straight and slightly posteroventrally slant- ed at base of dorsal fin in juveniles, adults with angle more pronounced; straight from base of last dorsal-fin ray to caudal pedun- cle. Dorsal surface of body transversely rounded anteriorly, with indistinct median keel immediately anterior to dorsal fin, smoothly rounded transversely posterior to PFL SL Fig. 9. Plot of length of pelvic fin (PFL) against standard length (SL), both in millimeters and regres- sion lines, for Steindachnerina planiventris (dots, Y = 0.851 + 0.185%) and Steindachnerina quasimodoi (stars, Y = 0.561 + 0.241X), (some symbols represent more than one data point). 477 ) Ue. “J Z { { ; 1 - at ee ag ye Fig. 10. Map of northern South America showing geographic distribution of Steindachnerina quasimodoi (stars) and Steindachnerina planiventris (dots). Type localities: 1, Rio Machado; and 2, Rio Yavari, Petro- polis. Some symbols represent more than one lot and/ or collecting locality. fin. Ventral profile of body very gently curved from tip of lower jaw to origin of anal fin, sigmoid from that point to caudal peduncle. Pre-pelvic region broadly flat- tened, with three irregular series of scales across flattened ventral surface. Scale series of pre-pelvic region flanked on each side by series of scales bent to conform to shape of lateral angles of body. Obtuse median keel posterior to pelvic fin insertion. Secondary obtuse keel on each side of post-pelvic por- tion of body two scales dorsal of ventral midline. Greatest body depth at origin of dorsal fin, depth 0.27-0.34 (0.30-0.34 in speci- mens above 50 mm SL) [0.33]; snout tip to origin of dorsal fin 0.47—0.50 [0.49]; snout tip to origin of anal fin 0.84—0.86 [0.86]; snout tip to insertion of pelvic fin 0.50—0.54 [0.50]; snout tip to anus 0.75-0.78 [0.76]; origin of dorsal fin to hypural joint 0.54— 0.59 [0.59]. Dorsal-fin margin poionted, less SO with increasing age; anteriormost rays about three to three and one-half times length of ultimate ray. Pectoral-fin margin pointed; length of pectoral fin 0.19-0.21 [0.21], extends posteriorly to point about two scales anterior of vertical through in- sertion of pelvic fin. Pelvic-fin margin 478 pointed, length of pelvic fin 0.23-0.26 [0.26], reaches two-thirds distance to origin of anal fin. Caudal fin forked. Adipose dorsal fin well developed. Anal fin emarginate, ante- riormost branched rays about three to three and one-half times length of ultimate ray. Caudal peduncle depth 0.11-—0.13 [0.13]. Head distinctly pointed, head length 0.27-— 0.33 [0.28]; upper jaw much longer than lower, mouth inferior; snout length 0.31- 0.34 [0.33]; nostrils very close, anterior cir- cular, posterior crescent shaped with aper- ture closed by thin flap of skin separating nares; orbital diameter 0.31-0.37 [0.32]; adipose eyelid present, more developed in larger specimens, particularly anteriorly, with broad vertically ovoid opening over center of eye; length of postorbital portion of head 0.36-0.40 [0.36]; gape width 0.30- 0.35 [0.33]; interorbital width 0.36-0.43 [0.42]. Pored lateral line scales from supraclei- thrum to hypural joint 40 to 46 [44]; all scales of lateral line pored, canals in scales straight; 4 to 6 series of scales extend beyond hypural joint onto caudal fin base; 72 to 9% [84] scales in transverse series from origin of dorsal fin to lateral line; 512 to 6% [614] scales in transverse series from lateral line to origin of anal fin. Dorsal-fin rays 11,9 or 111,9 (when three unbranched rays present, first very short) [111,9]; anal-fin rays 11,7 or ili,7 (when three unbranched rays present, first very short) [11,7]; pectoral-fin rays 15 to 17 [16]; pelvic- fin rays i,8 or rarely i,7,i [i,8]. Total vertebrae 35 (11), 36 (20). Color in life. —(The following description is based on a color transparency of a spec- imen captured in the Rio Javari by S. O. Kullander). Overall coloration bright silver, somewhat darker on dorsal portions of head and body. Iris silver. Fins yellowish with light margins. Dorsal fin with a small dark patch on basal portion of middle rays. Color in alcohol. —Ground coloration of specimens lacking guanine on scales tan, darker on dorsal portion of body. Dorsal portion of head dusky. Margins of scales on PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON lateral and dorsal portions of body outlined by series of small chromatophores in ju- veniles. Pigmentation field expanded in larger specimens to cover exposed surface of scales, particularly dorsally. Mid-dorsal line somewhat darker, particularly imme- diately anterior of dorsal fin. Pores in lateral line scales outlined dorsally and ventrally by chromatophores. Dorsal fin with diffuse patch of dark pigmentation on basal portion of membranes between third and fifth ray. Dorsal and caudal fins dusky. Adipose dor- sal fin margin dusky. Anal fin hyaline or with scattered chromatophores. Paired fins hyaline. Distribution. — Rio Javari (=Rio Yavari) system of Peru and Brazil, and proximate portions of Peruvian Amazon (Fig. 10). Etymology.—The specific name quasi- modoi is taken from Quasimodo, the mis- understood hunchback bell-ringer of the Cathedral in Victor Hugo’s novel Notre Dame de Paris, and refers to the pro- nounced humped dorsal profile of the body in larger specimens of the species. Type material. —39 specimens, 34.3-— 122.6 mm SL. Holotype.-PERU. Loreto. Rio Javari, near Petropolis; Hérnan Ortega, 2 Oct 1982, USNM 293041, 1 (88.9). Paratypes.-PERU. Loreto. 13 specimens taken with holotype, USNM 293042, 7 (49.7-122.6, two specimens cleared and counterstained for cartilage and bone); MHN-USM 1698, 4 (50.7—100.6); MZUSP 38593, 2 (58.4—-59.6). BRAZIL: Amazonas; Rio Javari system, immediately downstream of confluence of Rio Jaquirana and Rio Galvez; S. Kullan- der, et al., 31 July 1984. NRM SOK/ 1984312.4093, 9 (33.3-121.8); MZUSP 38594, 3 (50.1-53.6). Rio Javari system, opposite Colonia Angamos, Peru; S. Kul- lander, et al., 5 Aug 1984, NRM SOK/ 1984317.4091, 7 (40.0-69.2); MHN-USM 1699, 3 (49.8-57.0); USNM 293040, 3 (34.3-61.5). The following non-type specimens were also examined: VOLUME 102, NUMBER 2 479 Pip? 11. Rio Machado, near mouth. PERU: Loreto; Rio Ampiyacu, near the mouth, USNM 175868, 1 (48.4). Pebas, CAS-SU 36888, 1 (81.7). Steindachnerina planiventris, new species Figs. 1, 8-11, Table 1 Curimatus bimaculatus, Eigenmann and Ei- genmann, 1889:422 [in part, specimens from Ica, Brazil]. Diagnosis. — The 40 to 46 lateral in scales to the hypural joint distinguish S. planiven- tris from S. gracilis which has 50 to 54 scales in that series and S. hypostoma which has 46 to 50. The presence of a discrete spot of dark pigmentation in the basal portions of the middle rays of the dorsal fin further sep- arates S. planiventris from S. hypostoma which lacks that pigmentation. Other dif- ferences in meristic and morphometric fea- tures further differentiate S. planiventris from S. hypostoma and S. gracilis (Table 1). Specimens of S. planiventris of greater than 50 mm SL are distinguished from com- parably sized individuals of S. guasimodoi in their greatest body depths (0.27—0.30 of SL versus 0.30-0.34, Fig. 8), differences in the degree of convexity of the dorsal surface of the body (Figs. 7, 11), pelvic-fin length (0.19-0.23 of SL versus 0.23-0.26, Fig. 9), and degree of contact of the frontals anterior of the cranial fontanel (Fig. 1C, B). The rel- ative orbital width and length of the post- orbital region of the head also discriminate the species to a degree (Table 1). Description.—Body elongate, slightly com- pressed. Dorsal profile of head distinctly Steindachnerina planiventris, new species, holotype, MZUSP 35857, 65.7 mm SL; Brazil, Rondonia, convex anterior to vertical through nostrils, slightly convex or straight from that point to rear of head. Dorsal profile of body slight- ly convex from rear of head to origin of dorsal fin; straight and slightly posteroven- trally slanted at base of dorsal fin, straight from base of last dorsal-fin ray to caudal peduncle. Dorsal surface of body trans- versely rounded anteriorly, with indistinct median keel immediately anterior to dorsal fin, smoothly rounded transversely poste- rior to fin. Ventral profile of body gently curved from tip of lower jaw to caudal pe- duncle. Pre-pelvic region distinctly flat- tened, with three longitudinal series of scales on ventral flattened surface. Ventral scale series flanked on each side by series of scales bent to conform to shape of lateral angles of body. Barely discernable median keel posterior to pelvic-fin insertion. Secondary obtuse keel on each side of postventral por- tion of body about two scales dorsal of ven- tral midline. Greatest body depth at origin of dorsal fin, depth 0.27—0.30 [0.29]; snout tip to or- igin of dorsal fin 0.46—0.50 [0.49]; snout tip to origin of anal fin 0.83—0.87 [0.87]; snout tip to insertion of pelvic fin 0.52—0.56 [0.54]; snout tip to anus 0.72-0.76 [0.75]; origin of dorsal fin to hypural joint 0.54—0.59 [0.57]. Dorsal-fin margin pointed, less so with in- creasing age; anteriormost rays three to three and one-half times length of ultimate ray. Pectoral-fin margin pointed; length of pec- toral fin 0.18-0.23 [0.20], extends about three-quarters distance to vertical through insertion of pelvic fin. Pelvic-fin margin 480 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON pointed, length of pelvic fin 0.19—0.23 [0.21], reaches about two-thirds distance to origin of anal fin. Caudal fin forked. Adipose dor- sal fin well developed. Anal fin barely emar- ginate, anteriormost branched rays three to three and one-half times length of ultimate ray. Caudal peduncle depth 0.11-0.12 [0.12]. Head distinctly pointed, head length 0.26—- 0.31 [0.30]; upper jaw distinctly longer than lower, mouth inferior; snout length 0.33- 0.36 [0.33]; nostrils very close, anterior cir- cular, posterior crescent-shaped with aper- ture closed by thin flap of skin separating nares; orbital diameter 0.29-0.33 [0.30]; adipose eyelid present, moderately devel- oped, more so anteriorly, with broad ver- tically ovoid opening over center of eye; length of postorbital portion of head 0.36- 0.41 [0.38]; gape width 0.28-0.34 [0.32]; interorbital width 0.38-0.44 [0.40]. Pored lateral line scales from supraclei- thrum to hypural joint 40 to 46 [41]; all scales of lateral line pored, canals in scales straight; 4 to 6 series of scales extend beyond hypural joint onto caudal fin base; 612 to 812 [7'4] scales 1n transverse series from origin of dorsal fin to lateral line; 52 to 6% [54] scales in transverse series from lateral line to origin of anal fin. Dorsal-fin rays i1,9 or 11,9 (when three unbranched rays present, first very short) [11,9]; anal-fin rays 11,7 or i11,7 (when three unbranched rays present, first very short) [111,7]; pectoral-fin rays 15 to 17 [15]; pelvic- fin rays 1,8 [1,8]. Total vertebrae 34 (19), 35 (109), 36 (7). Color in alcohol.—Specimens retaining guanine on scales with overall coloration golden, somewhat purplish dorsally. Ground pigmentation in specimens lacking guanine on scales tan to light brown, darker on dor- sal portions of head and body. Scales on lateral and dorsal surfaces of body with margins outlined by series of small chro- matophores; chromatophore series most developed dorsally, increasingly less so ven- trally. Dorsal fin with patch of dark chro- matophores on basal portion of membranes between third and fifth rays. Median fins, particularly lower lobe of caudal fin in some individuals, dusky. Paired fins hyaline. Distribution. —Rio Madeira and Rio Ne- gro basins, main channel and tributaries of middle Rio Solimoes (Fig. 10). Etymology.—The specific name, plani- ventris, from the Latin planum, flat, and venter, belly, refers to the flattened ventral surface of the body in this species. Remarks. —In their revision of the then- known species of curimatids, Eigenmann and Eigenmann (1889:42) listed extensive series of specimens of Curimatus bimacu- latus Steindachner (=Steindachnerina bi- maculata) from various central and western Amazonian localities. At least some of the specimens from “‘I¢a”’ (the Rio I¢a of west- ern Amazonas State in Brazil) are Stein- dachnerina planiventris (USNM 120250). Type material. —80 specimens, 53.5—78.8 mm SL. Holotype. —BRAZIL: Rondonia; Rio Machado, near mouth (approx. 8°03’S, 62°53'W); M. Goulding, 4 Sep 1980, MZUSP 38587, 1 (65.7). Paratypes. —BRAZIL: Rondonia; 35 specimens taken with holotype: MZUSP 38588, 17 (55.5-74.1); USNM 267986, 18 (56.3-78.8). Rio Machado, Jauari, River Channel Beach; M. Goulding, 5 Sep 1980, USNM 267989, 18 (46.2-67.8), MZUSP 38590, 18 (53.5-65.2). Rio Machado, Santo Antonio; M. Goulding, 3 Sep 1980, USNM 267987, 6 (56.5-65.1, two specimens cleared and counterstained for cartilage and bone), MZUSP 38589, 5 (59.0-67.9). The 157 following non-type specimens were also examined: BRAZIL: Rio Jurua, BMNH 1897.12.1: 88-100, 13. Rondonia; Rio Machado, Cu- ruru, USNM 267988, 8. Roraima: Rio Branco, Boa Vista, NMW 68887, 9; 1 NMW 68888, 10; NMW 68889, 4; NMW 68890, 8; NMW 68892, 5; NMW 68897, 1. Rio Branco, 20 km below Boiagu, MZUSP 21164, 4 (49.3-53.7). Conceicao (? =Con- ceicao do Mau), NMW 68898, 6. Rio Bran- VOLUME 102, NUMBER 2 co, Serra Grande, 15 miles from Boa Vista, NMW 68885, 6 (53.1-87.0); NMW 68893, 3; NMW 68896, 2; NMW 697355, 4. Ama- zonas; Rio Negro, just below mouth of Rio Branco, USNM 293097, 22 (11, 52.5—80.6). Rio Negro, Anvilhanas, Municipio de Ay- rao, USNM 293098, 7. Rio Solimoes, Ilha Sorubim, above Coari, MZUSP uncat., 24 (62.3—71.3). Rio Solimoes, Coari, USNM 293099, 12. Rio Solimoes, near Ilha Ba- rurua, above mouth of Rio Jutai, MZUSP 20987, 3 (2, 63.2—71.7). Rio Solimoes, Ilha Xibeco, above mouth of Rio Jutai, MZUSP uncat., 1 (73.8). Iga, USNM 120250, 5 (for- merly MCZ 19571). BOLIVIA: Beni; Rio Mamoré, Puerto Siles, AMNH uncat., 2 (65.7—73.5). Acknowledgments We are indebted to the following individ- uals and institutions for the loan and ex- change of specimens, information, hospi- tality during visits, and other assistance: Dr. Gareth Nelson and Dr. C. Lavett Smith (AMNH); Mr. Gordon J. Howes, Dr. P. Humphry Greenwood and Mr. Alwyne Wheeler (BMNH); Dr. William Eschmeyer, Dr. Tomio Iwamoto and Mr. David Catan- ia (CAS); Dr. Jacques Geéry (GC); Dr. Camm Swift and Mr. Jeffrey Seigel (LACM); Dr. Naércio A. Menezes, Dr. Heraldo A. Brit- ski, and Dr. José Lima de Figueiredo (MZUSP); Prof. Hernan Ortega (MHN- USM); Dr. Sven O. Kullander and Mr. E. Ahlander (NRM); Dr. Barbara Herzig, Mr. Harald Ahnelt, and the late Dr. Rainer Hacker (NMW), and Dr. Gordon M. Reid (Horniman Museum, London). The type material of Steindachnerina planiventris was collected by Dr. Michael Goulding of the Museu Paraense “‘Emilio Goeldi,’” Belem, and that of Steindachner- ina quasimodoi by Prof. Hernan Ortega (MHN-USM) and Dr. Sven O. Kullander (NRM). Numerous specimens, including the majority of the paratypes of Steindachner- ina gracilis were made available through the 481 Expedicao Permanente de Amazonia (EPA), directed by Dr. Paulo E. Vanzolini (MZUSP). Collecting efforts in Peru were carried out as a joint project with the In- stituto Veterinario de Investigaciones Trop- icales y de Altura, and the Museo de His- toria Natural ““Javier Prado,’ Lima. The Consejo Nacional de Ciencia y Tecnologia of Peru, and in particular its director Dr. M. Vegas Velez greatly facilitated studies in that country. Dr. Naércio A. Menezes (MZUSP) provided the Portuguese trans- lation of the ““Abstract.’? Technical assis- tance at the Smithsonian was provided by Mr. Andrew G. Gerberich and Mr. Jeffrey Clayton. Photographs were prepared by Mr. Theophilus Britt Griswold. Research associated with this study in Peru and Brazil was partially supported by the Neotropical Lowland Research Pro- gram of the International Environmental Sciences Program of the Smithsonian In- stitution. This paper benefitted from the comments and suggestions of Dr. Wayne C. Starnes, Dr. Darrell Siebert, and Dr. Wil- liam L. Fink. Literature Cited Boulenger, G. A. 1887. Description of South Amer- ican characinoid fishes.— Annals and Magazine of Natural History 9:172-174. Eigenmann, C.H. 1910. Catalogue of the fresh-water fishes of tropical and south temperate Ameri- ca.—Report of the Princeton University Expe- dition to Patagonia, 1896-1899, 3 (Zoology, 4): 375-511. —,& W.R. Allen. 1942. Fishes of western South America. I. The intercordilleran and amazonian lowlands of Peru. II. The high pampas, Bolivia, and Northern Chile. With a revision of the pe- ruvian Gymnotidae, and of the genus Orestias. 494 p. Lexington: University of Kentucky. —, & R.S. Eigenmann. 1889. A revision of the edentulous genera of the Curimatinae. — Annals of the New York Academy of Sciences 4:409-— 440. ——., & 1891. A catalogue of the fresh- water fishes of South America.— Proceedings of the United States National Museum 14:1-81. Fernandez-Yeépez, A. 1948. Los curimatidos (peces fluviales de Sur America), catalogo descriptivo 482 con nuevas adiciones genericas y especificas. — Boletin Taxonomico del Laboratorio de Pes- queria de Caiquire 1:1—86. Fowler, H. W. 1906. Further knowledge of some het- erognathus fishes, Part I.—Proceedings of the Academy of Natural Sciences of Philadelphia, 58:293-351. 1942. Los peces del Peru.—Boletin Museo de Historia Natural “Javier Prado.” Lima 6: 206-222. 1945. Los peces del Peru.—Boletin Museo de Historia Natural “Javier Prado.” Lima 7:1- 298. 1950. Os peixes de aqua doce do Brasil (2a entrega).— Arquivos de Zoologia do Estado de Sao Paulo 6:205-404. 1975. Acatalogue of world fishes (XXIII). — Quarterly Journal of the Taiwan Museum 28(3): 277-402. Géry, J. 1977. Characoids ofthe world. Neptune City, New Jersey, TFH Publications. 672 pp. Ortega, H., & R. P. Vari. 1986. Annotated checklist of the freshwater fishes of Peru.—Smithsonian Contributions to Zoology 437:1-25. Vari, R. P. 1982. Systematics of the neotropical char- acoid genus Curimatopsis (Pisces: Characoid- ei). —Smithsonian Contributions to Zoology 373: 1-28. 1984. Systematics of the neotropical chara- ciform genus Potamorhina (Pisces: Characi- formes).—Smithsonian Contributions to Zool- ogy 400:1-36. PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON . 1989. A phylogenetic study of the neotropical characiform family Curimatidae (Pisces: Ostar- iophysi).—Smithsonian Contributions to Zool- ogy 471:1-71. in press a. Systematics of the neotropical characiform genus Curimata Bosc (Pisces: Characiformes).— Smithsonian Contributions to Zoology 474. in press b. Systematics of the neotropical characiform genus Psectrogaster Eigenmann and Eigenmann (Pisces: Characiformes).—Smith- sonian Contributions to Zoology 481. in press c. Systematics of the neotropical characiform genus Pseudocurimata Fernandez- Yeépez (Pisces, Characiformes).—Smithsonian Contributions to Zoology 490. , & R. M.C. Castro. 1988. Prochilodus stig- maturus Fowler, reassigned to the Curimatidae from the Prochilodontidae, with comments on other nominal curimatid and prochilodontid species treated by Fowler.—Copeia 1988(3):777— 780. (RPV) Department of Vertebrate Zoology (Fishes), National Museum of Natural His- tory, Smithsonian Institution, Washington, D.C. 20560; and (AWV) ADP, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 483-490 DESCRIPTION OF TWO NEW SPECIES OF THE ELEUTHERODACTYLUS MILESI GROUP (AMPHIBIA: ANURA: LEPTODACTYLIDAE) FROM NORTHERN HONDURAS James. R. McCranie, Jay M. Savage, and Larry David Wilson Abstract. —Two new species of the Eleutherodactylus milesi group (E. chry- sozetetes and E. cruzi) are described from the Cordillera de Nombre de Dios of northern Honduras. Eleutherodactylus milesi is shown to have a wide range in Honduras on scattered montane ridges and is reported from Guatemala for the first time. The systematics of Eleutherodactylus ma- tudai and E. milesi were reviewed by Savage (1975), who included them in the E. rugu- losus group. These species subsequently were removed from the rugulosus group (Miya- moto 1983, Savage 1987) and placed as a separate infrageneric lineage, the E. milesi group (Savage 1987). Members of this stock differ in karyology (2N = 22; NF = 44) and jaw musculature (DFSQAT + e) from those of the rugulosus group (2N = 20, 22; NF = 36; jaw muscle formula: dfsq; dfsqat + e). Externally, frogs of the mi/esi group are dis- tinct (features for the rugu/osus group in pa- rentheses) in: lacking tarsal folds (a well- developed inner tarsal fold), having a strongly tuberculate dorsum (dorsum smooth to rugose), and having a pair of para- anal light bars (never with such markings). In addition E. matudai has an indistinct tympanum in females and E. milesi has the tympanum indistinct or hidden (distinct, nearly transparent tympanum). Recent fieldwork in Guatemala and Hon- duras substantially increases the known range for Eleutherodactylus milesi and this information and data on variation are pre- sented here. Among other newly collected material from the Cordillera de Nombre de Dios of northern Honduras are two forms, clearly allied to E. matudai and E. milesi, but trenchantly different from them and from one another. These distinctive frogs are regarded as representing previously un- known species and are described below fol- lowing the style and terminology of Savage (1975); a few features not mentioned in that paper follow the definitions of Savage (1987). Eleutherodactylus chrysozetetes, new species Fig. 1 Holotype.—KU 209035, adult male, from Quebrada de Oro (15°38'N, 86°47'W), ele- vation 880 m, tributary of Rio Viejo, south slope of Cerro Bufalo, Cordillera de Nombre de Dios, Departamento de Atlantida, Hon- duras, 17 Aug 1984, James R. McCranie, Kenneth L. Williams, and Larry David Wil- son. Original number LDW 6529. Diagnosis. —Eleutherodactylus chrysoze- tetes is a moderately large frog and is distin- guished from the two previously described members of the milesi group, E. matudai and &. milesi (characteristics for these species in parentheses), in having extensive toe webbing with about three phalanges free of the web on toe IV (basal to moderate webbing, with four to four and one-half pha- langes free of web); strongly expanded finger and toe disks, about twice width of digit (finger disks definite, less than twice width of digit; toe disks weak, barely expanded); ey mh “= e~. Fig. 1. tympanum hidden in adult males and pre- sumably females (tympanum evident in adult males). Eleutherodactylus chrysoze- tetes is further distinguished from E. ma- tudai (states for matudai in parentheses) by having: paired vocal slits in adult males (no vocal slits); groin with a light spot on the dark uniform flank color (groin mottled). In addition, E. chrysozetetes can be distin- guished from E. milesi (states of milesi in parentheses) by having: a well-developed fleshy fringe along margins of toes (a very narrow ridge); adult males to 41.3 mm in standard length (20-34 mm). E. chrysoze- tetes 1s compared to the second new species described in this paper in the diagnosis for the latter form. Summary of characteristics. —Dorsum tuberculate; canthus rounded; tympanum hidden in adult males; first finger equal to or shorter than second; finger disks strongly PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Holotype, KU 209035. Eleutherodactylus chrysozetetes. expanded, at least twice width of digit just proximal to disks on fingers IIJ-IV; inner tarsal fold absent; toe disks strongly devel- oped, about twice width of digit; a well- developed fleshy fringe along margins of toes; toes extensively webbed, webbing for- mula: I 1+—2, II 1+-2 1/2, III 2-3 1/4, IV 3+—2 V; paired vocal slits in adult males; nuptial pads in adult males; throat and ven- ter heavily suffused with pale purple; dor- sum dark olive brown, blotched with pale Olive brown; groin light spotted on a uni- form dark flank; posterior surface of thigh uniform purplish-brown with a light para- anal bar; underside of tibial segment suf- fused with pale purple. Coloration. —In life the holotype was dark olive brown, blotched with pale olive brown; upper surfaces of limbs same as dorsum; posterior surface of thigh uniform purplish- brown with a light para-anal bar; venter and VOLUME 102, NUMBER 2 throat pale purple; soles of hands and feet purple; underside of tibial segment suffused with pale purple; iris steel gray with rust- red horizontal band. Measurements. —Standard length in mil- limeters, other measurements as percent- ages of standard length: standard length 41.3; head length 41.9; head width 42.1; orbit 13.3; snout length 17.2; loreal length 9.2; hindleg length 166.1; tibia length 53.0. Etymology. —The specific epithet is from the Greek chrysos (=gold) and zététés (=searcher), with reference to the occur- rence of this form along the Quebrada de Oro (stream of gold). Natural history notes. —The holotype and a juvenile specimen were collected during the morning in the forest alongside the Que- brada de Oro. The vegetation at the type locality is in the Subtropical Wet Forest for- mation (Holdridge 1967) and will be de- scribed in more detail in a subsequent pa- per. The known elevational range is 880- 1110 meters. Referred specimen.—KU 209036, a ju- venile from Quebrada de Oro, taken be- tween 920-1110 m. Eleutherodactylus cruzi, new species Fis. 2 Holotype.—KU 209037, adult male, from south slope of Cerro Bufalo (15°38'N, 86°47'W), elevation 1520 m, Cordillera de Nombre de Dios, Departamento de Atlan- tida, Honduras, 4 Jun 1980, Gustavo A. Cruz Diaz, James R. McCranie, and Larry David Wilson. Original number LDW 5606. Paratopotype.—KU 209038, adult male. Diagnosis.—A medium sized Eleuthero- dactylus (males to 32.6 mm in standard length, females presumably 8 to 10 mm longer) differing from all other members of the milesi group in having the following combination of characteristics: moderate toe webbing, with about four phalanges free of web on toe IV; definite finger disks, almost twice width of digit; toe disks weak, barely 485 expanded; a distinct ridge along toes, ba- sally; tympanum hidden in adult males (and presumably females); and a unique color- ation with a narrow, median dorsal light stripe, the venter cream and lightly punctate and the throat punctate. Eleutherodactylus cruzi most closely resembles the larger E. matudai (adult males to 50 mm in standard length) in disk size, toe webbing and fring- ing. The latter form has the tympanum dis- tinct in males and indistinct in females (hid- den in male and almost certainly in female E. cruzi), the venter uniform gray with sil- ver or white spots, throat heavily pigment- ed, dorsum without a median dorsal light stripe and groin mottled (venter cream and lightly punctate, throat punctate, a median dorsal light stripe and a distinct white spot in groin in cruzi). E. cruzi has more toe webbing, somewhat broader finger disks and somewhat better developed toe ridges than E. milesi but is most obviously distinct in having the tympanum hidden in males and in coloration (the latter species has the tym- panum evident but indistinct in males, the venter and throat heavily marked and/or suffused with dark pigment and the dorsum never with a narrow median light stripe). The newly described E. chrysozetetes can- not be confused with E. cruzi (features for the latter in parentheses) since the former has strongly expanded finger and toe disks, about twice as wide as digits (definite finger disks, less than twice as wide as digits; bare- ly expanded toe disks), extensive toe web- bing with only about three phalanges on toe IV free of web (about four phalanges free of web), distinct toe fringes (toes ridged) and a larger size to 41.3 mm in adult males (to 32.6 mm). Coloration also will separate these forms as E. chrysozetetes resembles E. ma- tudai and E. milesi in having the throat and venter heavily marked with dark pigment and lacks a mid-dorsal light stripe. Summary of characteristics. —Dorsum tuberculate; canthus rounded; tympanum hidden in adult males; first finger equal to or shorter than second; finger disks definite, 486 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Holotype, KU 209037. Eleutherodactylus cruzi. almost twice width of digit just proximal to disks on fingers IIJ-IV; inner tarsal fold ab- sent; toe disks weakly expanded; ridge along margins of toes basally; toes moderately webbed, modal webbing formula: I 2—2 1/2, II 2-3 1/2, II 3-4, IV 4-2 1/2 V; paired vocal slits in adult males; nuptial pads in adult males; venter cream, lightly punctate; throat punctate; dorsum uniform brown ex- cept for a narrow mid-dorsal light stripe; groin with a light spot; posterior surface of thigh uniform brown with a distinct light para-anal bar; underside of tibial segment banded; adult males 26.9—32.6 mm in stan- dard length. Coloration.—In preservative the holo- type (KU 209037) is uniform brown with a narrow mid-dorsal light stripe; dorsal sur- faces of limbs brown with dark brown bands; venter cream, lightly punctated with brown; throat cream, punctated with brown; groin brown with a cream colored light spot; pos- terior surface of thigh brown with light brown para-anal bar; underside of tibial sur- face cream, banded with brown. The para- topotype (KU 209038) is similar to the holotype except that the overall appearance of the dorsal surfaces is a slightly lighter shade of brown. Measurements. —Standard lengths in millimeters, other measurements as per- centages of standard length (holotype fol- lowed by paratopotype). Standard length in adult males 32.6, 26.9; head length 42.6, 45.0; head width 42.6, 44.2; orbit 16.3, 14.9; snout length 17.5, 18.6; loreal length 10.4, 11.2; hind leg length 184.0, 201.4; tibia length 58.0, 64.7. Etymology.—The species is named in honor of Gustavo A. Cruz Diaz, in recog- VOLUME 102, NUMBER 2 nition of the many years of friendship McCranie and Wilson have enjoyed with this exemplary Honduran biologist and the invaluable assistance he has proferred to them. Natural history notes.—Both specimens of this species were collected during the morning at 1520 m alongside a trickle at the beginning of a small stream in the Lower Montane Wet Forest formation (Holdridge 1967). The Eleutherodactylus milesi Population System Recently collected material of frogs re- sembling Eleutherodactylus milesi from the Caribbean versant of Guatemala and Hon- duras provide significant extensions in the known geographic and elevational ranges for the species group and exhibit substantial variation in features previously used (Sav- age 1975) to diagnose the species. E. milesi was described from the mountains (Sierra de Omoa) west of San Pedro Sula, Depar- tamento de Cortés, Honduras. Additional localities for the species were the Montanas de Yoro, Departamento de Yoro and the Cordillera de Nombre de Dios, Departa- mento de Atlantida of north-central Hon- duras. These samples shared the following dis- tinctive features: 1) dorsum tuberculate; 2) canthus rounded; 3) tympanum indistinct in males, hidden in females; 4) finger disks definite; 5) no tarsal fold; 6) toe disks barely expanded, hardly wider than digit just prox- imal to disk; 7) a very narrow ridge along margins of toe; 8) toes with no or at most basal webbing; 9) paired vocal slits in adult males; 10) nuptial pads in adult males; 11) venter heavily suffused with light brown to chestnut pigment; 12) throat heavily pig- mented to almost uniform dark brown; 13) dorsum brown, spotted to occasionally blotched, rarely with a broad mid-dorsal light stripe; 14) groin with a single light spot 487 on dark uniform flank color; 15) posterior surface of thigh uniform reddish brown with a distinct light para-anal bar; 16) underside of tibial segment boldly marked with brown spotting or mottling, rarely suffused with chestnut pigment; 17) adult males 20-27 in standard length, females to 34 mm. The maximum size of adult males recorded as 22 mm in Savage (1975) was a typograph- ical error. The newly acquired specimens from east and west of previously known lo- calities for the species all agree with the above description in characteristics 1, 2, 4-6, 8-16. Variation in other features is briefly described below by general locality from east to west (populations numbered as on Fig. 3). Samples 1-6 are very similar to one another and to previously collected material except that adult males attain lengths (in mm) of 28 (sample 3) and 34 (sample 6) and a female reaches 39 (sample 3). Samples 7-10 have the tympanum indis- tinct in males and most females (no males present in sample 8, one female in sample 9 with the tympanum hidden on the right side); adult males reach to 28 (in mm) (sam- ple 7) and 30 (sample 9) and females 41 (sample 9). Samples 7 and 8 from the sierra along the border between Guatemala and Honduras and sample 9 from the Sierra de las Minas, Departamento de Baja Verapaz, Guatemala are slightly different from other series of the milesi complex in the condition of the tym- panum in females (usually indistinct, not hidden). However, we are reluctant to place undue emphasis on this feature or the slight variations in webbing, toe disk width and fringing and adult size among samples 1-9 and conclude that they represent a single morphospecies, Eleutherodactylus milesi. This species sseems to be comprised of iso- lated populations generally occurring on widely separated ridges between 500-1720 m elevation in Caribbean versant Guate- mala and Honduras. The single known fe- male (BM 1985/1452) from extreme eastern Honduras (sample 1) probably was taken Figs3: PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ELEUTHERODACTYLUS MILESI KILOMETERS Distribution of the Eleutherodactylus milesi group in Honduras and Guatemala. Numbers refer to samples discussed in text. E. milesi and both new species, E. chrysozetetes and E. cruzi described here occur at locality 5. below 500 m elevation and this population needs further study to establish its status conclusively. Sample 10, a single female (MVZ 159934), is from the somewhat isolated Sierra Xuc- aneb, Departamento de Alta Verapaz, Gua- temala. It differs from all other examples of the Eleutherodactylus milesi population system in having well-developed toe fringes, in this one feature it resembles E/leuthero- dactylus matudai of northwestern Pacific slope Guatemala and Eleutherodactylus chrysozetetes (described in this paper from northcentral Honduras). This specimen may represent a distinct species within the com- plex, but we are reluctant to recognize it as new without seeing adult males. Specimens examined.—Honduras: Co- lon; Sample 1, Rio Guaraska, north slope Montanas de Rio Platano, (BMNH 1985/ 1452). Olancho; Sample 2, Montana de Ma- lacate, 760 m (KU 209059). Sample 3, Sier- ra de Agalta, 1450 m (ROM 18099-107), 1060 m (ROM 18113), 1050 m (ROM 18109-111), 1000 m (ROM 18108, 18112). Yoro; Sample 4, Montanas de Yoro, Por- tillo Grande, 1460 m (MCZ 21290; FMNH 21862-64), Santa Marta, 1460 m (MCZ 21291). Atlantida; Sample 5, Cordillera de Nombre de Dios, above La Ceiba (MCZ 21293-294), Cerro Bufalo, Quebrada de Oro, 1110 m (KU 209058), 940 m (KU 209083-091), 880 m (KU 209080-082, 209096, 209098-104, 209142-143, LACM 137306-311), 810 m (KU 209105-—106), 780 m (KU 209092-095). Cortés; Sample 6, Sierra de Omoa, west of San Pedro Sula (FMNH 4699-4711, 142147, 21820, 21829), MCZ 21295-99, UMMZ 120388, USNM 118202), Cerro Cusuco, 1650-1720 m (LACM 137298-305), 1690 m (KU 209067-—070, 209107), 1580 m (KU VOLUME 102, NUMBER 2 209040-051), 1570 m (KU 209060), 1560- 1570 m (KU 209065-066), 1550 m (KU 209052-055, 209061-064), 1540-1550 m (KU 209071-075), 1530 m (KU 209056- 057, 209141). Copan; Sample 7, Sierra Es- piritu Santo, Montana Cerro Azul, 1050 m (KU 209077), 1100 m (KU 209076), 1300 m (KU 209078-079), 1350 m (KU 209097). Guatemala: Zacapa; Sample 8, Sierra Es- piritu Santo, La Union, 850 m (CM 57743- 44), Baja Verapaz; Sample 9, Sierra de las Minas, Aldea Vista Hermosa, 500-650 m (KU 189797-99, 189801-04). Alta Vera- paz; Sample 10, Sierra de Xucaneb, Finca Volcan, 875 m (MVZ 159934). Distribution. —Premontane and lower montane forests on the Atlantic versant of northern Honduras and adjacent eastern Guatemala (500-1720 m) (Fig. 3). Co-occurrence and Relationships The species Eleutherodactylus matudai (northwestern Guatemala), the various populations of Eleutherodactylus milesi (Caribbean slope Guatemala and Hondu- ras) and the montane form Eleutherodac- tylus cruzi from above 1500 m in north- central Honduras are allopatric, although the latter ultimately may prove to be sym- patric with E. milesi. Eleutherodactylus chrysozetetes is sympatric with E. milesi be- tween 880-1110 m elevation on Cerro Bu- falo. That three distinctive species of this group occur on Cerro Bufalo, and possibly elsewhere in the Cordillera Nombre de Dios, is almost inexplicible but perhaps reflects the stochastic influence of the orogenic fac- tor in tropical frog evolution. In terms of relationships the Caribbean versant species seem to form a derived clus- ter, as compared to Eleutherodactylus ma- tudai, and have the characteristic white groin spot and reduction in distinctiveness of the tympanum. E. matudai lacks vocal slits which are found in adult males of Caribbean versant populations. Other features (toe webbing, fringing, and finger disk devel- Opment) combine in a mosaic in the three 489 recognizable Caribbean slope forms. Of the three, Eleutherodactylus chrysozetetes is most similar to E. matudai in hand and foot structure but most different from it in the modification of the tympanum. Thus, while E. matudai seems to be the primitive sister- group (in which vocal slits have been lost) to the eastern forms, it is not possible on the basis of current data to explicate the relationships of the Caribbean versant species among themselves. Acknowledgments Gustavo A. Cruz Diaz, Mario Espinal, Kelly M. Hogan, and Kenneth L. Williams provided field assistance and companion- ship. Don Tomas Meraz and his family as- sisted McCranie and Wilson on all visits to the Cerro Bufalo-Quebrada de Oro area. Wilberto Aguilar N. and Gustavo A. Cruz Diaz were instrumental in the acquisition of collecting permits for Honduras. Brian I. Crother of the University of Miami drafted the map. We thank all of these individuals for their aid and the authorities at the fol- lowing institutions (abbreviations in paren- theses used to identify these collections throughout this paper) who arranged for us to examine pertinent materials: British Mu- seum (Natural History) (BMNH); Carnegie Museum (CM); Field Museum of Natural History (FMNH); Museum of Natural His- tory, University of Kansas (KU); Museum of Comparative Zoology, Harvard Univer- sity (MCZ); Museum of Vertebrate Zoology, University of California, Berkeley (MVZ); University of Michigan, Museum of Zool- ogy (UMMZ); National Museum of Natural History, Smithsonian Institution (USNM). The following abbreviations indicate col- lections where material reported here has been deposited: Natural History Museum of Los Angeles County (LACM) and Royal Ontario Museum (ROM). Literature Cited Holdridge, L. R. 1967. Life zone ecology. Tropical Science Center, San José, Costa Rica. 206 pp. 490 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Miyamoto, M. M. 1983. Frogs of the Eleutherodac- tylus rugulosus group: A cladistic study of al- lozyme, morphological, and karyological data. — Systematic Zoology 32(2):109-124. Savage, J. M. 1975. Systematics and distribution of the Mexican and Central American stream frogs related to Eleutherodactylus rugulosus. —Copeia 1975(2):254-306. —. 1987. Systematics and distribution of the Mexican and Central American rainfrogs of the Eleutherodactylus gollmeri group (Amphibia: Leptodactylidae). — Fieldiana: Zoology, N.S. 33: iv + 1-57. (JRM) 10770 S.W. 164th Street, Miami, Florida 33157; (JMS) Department of Biol- ogy, University of Miami, Coral Gables, Florida 33124; (LDW) Department of Bi- ology, Miami-Dade Community College, South Campus, Miami, Florida 33176. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 491-499 A NEW SPECIES OF DIMINUTIVE ELEUTHERODACTYLUS (LEPTODACTYLIDAE) FROM OAXACA, MEXICO Jonathan A. Campbell, William W. Lamar, and David M. Hillis Abstract. —Eleutherodactylus polymniae 1s described from the northern slopes of the Sierra Juarez, Oaxaca, México. It is a small species, with distinctively marked flanks and thighs, and has a vocal repertoire of at least four separate, distinct calls. This species is apparently a member of the a/fredi group, and may exist sympatrically with E. spatulatus. Resumen.-—Se describe una nueva especie de rana, Eleutherodactylus polym- niae, conocido del vertiente norteno de la Sierra Juarez, Oaxaca, México. Es una especie diminutiva, con manchas distintivas sobre la parte lateral del abdomen y sobre los muslos, y dispone de un repertorio vocal que consiste de por lo menos cuatro cantos separados y distintos. Aparentemente dicha expecie es miembro del grupo al/fredi, y posiblemente existe en simpatria con E. spat- ulatus. The vegetation covering the northern slopes of the Sierra Juarez in Oaxaca com- prises one of the most extensive tracts of cloud forest remaining in México. Within the last decade, however, agricultural clear- ings have steadily advanced up the hillsides so that most of the original forest below the 1200 m contour has been severely altered. Also the leeward (southern) side of the range is drier than the northern slopes, and is sub- ject to periodic man-induced forest fires that have damaged the higher portions of the cloud forest. Previously, owing to the cold, wet environment and poor soils, the portion of the forest between about 1500 and 3000 m was almost uninhabited by humans. However, with the recent advent of hard- wood logging, the entire forest is in danger of soon being irreversibly damaged with an associated loss of many species of animals. The cloud forest of the Sierra Juarez har- bors a remarkably diverse herpetofaunal as- semblage containing many endemic species. Only one road traverses the region (Mexican Highway 175), and it has been primarily along this road that biologists have made collections. Probably no other region of similar size in México has yielded more new species of amphibians and reptiles in the last few decades, nor remains so superfi- cially known. A few of the species, by no means a complete listing, of recently de- scribed species that, so far as is known, are endemic to the region include Pseudoeury- cea juarezi (Regal, 1966), Hyla cyvanomma and H. sabrina (Caldwell, 1974), H. echi- nata (Duellman, 1962), H. mixe(Duellman, 1965), Norops polyrhachis (Smith, 1968), Abronia mitchelli (Campbell, 1982), A. ka- laina (Good & Schwenk, 1985), Barisia Juarezi (Karges & Wright, 1987), Exiliboa placata (Bogert, 1968), Cryophis hallbergi (Bogert & Duellman, 1963), and Geophis duellmani (Smith & Holland, 1969). In the summer of 1983, we discovered yet another unknown anuran species in the Sierra Juarez. This frog inhabits steep slopes and is extremely difficult to collect. The re- markable voice of this species, in combi- nation with its habitat, where a misstep by 492 anyone pursuing it might have disastrous consequences, moves us to name this frog Eleutherodactylus polymniae, new species Figs. 1-3 Holotype.— University of Texas at Ar- lington (UTA) A-12976 (original number, JAC 9007), an adult male, collected 0.8 km N Vista Hermosa, northern slopes of the Sierra Juarez, Oaxaca, México, at an ele- vation of 1420 m, 25 Jul 1983, J. A. Camp- bell, W. W. Lamar, and D. M. Hillis. Paratype.—UTA A-23511, an adult to- potypic male, taken by the same collectors, 17 Aug 1983. Diagnosis. —A small species of Eleu- therodactylus (SVL of largest male, 19.7 mm); possessing expanded digital pads, es- pecially on the outer two fingers, which are between three and four times wider than the digits at their narrowest point; a relatively small tympanum, the horizontal distance across which is less than a third of the dis- tance across the eye; and distinctive white markings extending anterodorsally across the flanks from the inguinal region. The species differs from all Mexican congeners in having four separate, distinct calls. Description. —Dorsal outline of snout broadly rounded; snout profile in lateral view truncate; canthus rounded; choanae round except along the anterior edge which is straight owing to the shape of the lateral wings of the prevomers; vomerine teeth present, three or four teeth per fascicle; tongue ovoid, notched posteriorly; glottal disc large; vocal slits elongate, extending from a point about equal to midlength of tongue to the corner of the mouth; eyelids, dorsum, forearms, and shanks, with a few enlarged tubercles, otherwise skin of dor- sum smooth, that of venter corrugate; tym- panum small, dorsal margin of tympanic ring indistinct; no glands apparent in the axillary, lumbo-inguinal, or inguinal areas; second finger longer than first; finger and PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON toe discs expanded and truncate (emargin- ate in dorsal view), pads on outer fingers between three and four times wider than digit; a whitish nuptial thumb pad present; subarticular tubercles rounded and raised; supernumerary tubercles absent on digits; three rounded or oblong palmar tubercles; small calcar tubercles present; inner and outer tarsal folds absent, but several small tubercles along outer surface of tarsus, and a single tubercle along inner surface of tar- sus; inner and outer metatarsal tubercles present, inner larger; several small tubercles on distal plantar surface, not extending pos- teriorly to level between metatarsal tuber- cles; webbing on hands and feet vestigial. The dorsum is mostly greenish brown with some rust colored markings. Dark brown markings are present along the posterior margin of the nostrils and along the upper lip, with large spots below the eye and above the corner of the mouth. Dark brown mark- ings also extend along the upper border of the tympanum and the scapular region of the dorsum. The inguinal region is bright white with two irregular white bars extend- ing forward anterodorsally to about the midlength of the body (Fig. 1). The anterior and posterior surfaces of the thighs are pat- terned with sharply contrasting white and brown bars; the forearms, tibia, and dorsal surfaces of the thighs have moderately con- trasting pale brown and darker brown bars. The throat and venter are pale with scat- tered black melanophores; the ventral sur- faces of the thighs and the plantar surfaces are darker, with numerous melanophores. The snout-vent length (SVL) is 19.7 mm; the head length, 8.2 mm; the head width, 8.1 mm; the horizontal distance across the eye, 2.8 mm; the distance from the eye to the tip of the snout, 3.6 mm; the distance from the eye to the nostril, 2.5 mm; the horizontal distance across the tympanum, 0.9 mm; the tibia length, 11.3 mm; and the distance from the proximal edge of the inner metatarsal tubercle to the distal tip of the fourth toe, 9.7 mm. VOLUME 102, NUMBER 2 ; i aa Bip. 1. Variation.—The paratype (UTA A-23511) is similar to the holotype in most aspects of morphology, color, and pattern. Measurements for the paratype are as fol- lows: SVL, 19.0 mm; head length, 7.9 mm; head width, 7.3 mm: horizontal distance across eye, 2.5 mm; eye to tip of snout, 3.4 mm; eye to nostril, 2.3 mm; horizontal dis- tance across tympanum, 0.8 mm; tibia, 11.6 mm; and distance from proximal edge of inner metatarsal tubercle to distal tip of fourth toe, 9.5 mm. Etymology. —The name polymniae is de- rived from Polymnia, also known as “‘she of the many hymns,” one of the Greek si- rens that was believed to lure mariners to destruction by her singing. Remarks. —In many respects (size, color, morphology) FE. polymniae resembles cer- tain members of the genera Tomodactylus and Syrrhophus (for reviews of these genera, 493 Eleutherodactylus polymniae, new species, holotype, SVL 19.7 mm, UTA A-12976. see Dixon 1957, and Lynch 1970a, respec- tively). It may be distinguished from species contained in these genera by the absence of lumbo-inguinal or inguinal glands, and by the failure of the plantar supernumerary tu- bercles to extend posteriorly to a level be- tween the metatarsal tubercles. Most species of Syrrhophus and Tomodactylus also have supernumerary tubercles on the digits, and especially on the toes; in E. polymniae the digits lack supernumerary tubercles. Eleutherodactylus polymniae conforms to the diagnosis of the genus Eleutherodactylus provided by Lynch (1968). Mexican and Guatemalan members of the genus Eleutherodactylus having widely expand- ed digital pads have been placed in the a/- fredi group (Lynch 1965, 1966, 1967a, b, c, 494 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Pattern of posterior surface of thighs in Eleutherodactylus polymniae, paratype, UTA A-23511. 1970b). Other than sharing distinctive dig- ital pads, few characters have been reported to suggest that this group is monophyletic. Geographically, the group is relatively com- pact, with 11 species along the Atlantic coastal plain and versant from Tamaulipas, México, southward through much of the Yucatan Peninsula to the mountains of northern Guatemala. One species, E. guer- reroensis, 1S restricted to the Pacific versant, and another, FE. stuarti, occurs on both the Atlantic and Pacific side of the Continental Divide (Fig. 4). Most species have ex- tremely restricted montane distributions, and many are known from fewer than half a dozen specimens. Eleutherodactylus alfredi has a wide distribution, ranging from east- central Veracruz (Smith & Taylor 1948) to Tabasco (Lee 1980) and Piedras Negras, Guatemala (Duellman 1960, Stuart 1963). Eleutherodactylus decoratus occurs along the Atlantic slopes of the Sierra Madre Oriental from southern Tamaulipas to central Ve- racruz (Martin 1958, Lynch 1967c). Eleu- therodactylus stuarti ranges from western Chiapas (Johnson 1974, Johnson et al. 1976) into western Guatemala. Eleutherodactylus xucanebi occurs in the northern cloud for- ests of Guatemala and is the southernmost member of the group (Stuart 1941). With the possible exception of E. polymniae and E. spatulatus, no two members of the group are known to be sympatric with one another. Males in this group of frogs range in size from E. polymniae (19.7 mm) to E. guer- reroensis (39.6 mm). Considerable sexual dimorphism exists and females usually at- tain from 1.3 to 1.4 times the SVL of males. The relative size of the tympanum is also usually sex dependent, being larger in the males of most species. The tympanum to eye ratio of all species in which the males are known is 0.62 or greater, except for E. polymniae and E. spatulatus which have ra- tios of 0.25-0.30 and 0.32, respectively. Eleutherodactylus megalotympanum was VOLUME 102, NUMBER 2 495 Fig. 3. Ventral aspects of hand and foot of Eleutherodactylus polymniae, holotype, UTA A-12976. named in allusion to what was perceived to be the relatively large tympanum in fe- males. However, the tympanum is not larg- er than that known in females of several other species. Eleutherodactylus spatulatus differs from other species in the a/fredi group in that males have a slightly smaller tym- panum than females. A large series of E. decoratus was reported to have little sexual dimorphism in the size of the tympanum (Martin 1958). The tarsal fold in this group may be poorly to moderately developed or absent. The color pattern of the flank in most species is rather drab, being a pale yellow, cream, gray, or tan with irregular stippling or mottling. The specimens of E. decoratus that we have seen in life had a contrasting pattern of brown markings on a pale background, often with a narrow pale vertebral stripe. Eleutherodactylus polym- niae has the most distinctive markings in the al/fredi group, with a large irregular white 496 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON . decoratus . spatulatus - polymnius . megalotympanum . guerreroensts . stlvtcola . stuartt . taylort . glaucus . xuecanebt . yuecatanensts @ ez O fF ¥ EF VeE @ F£ AE OB ae E BeE AE Fig.4. Distributions of Mexican and Guatemalan species of Eleutherodactylus with greatly expanded, truncate digital pads on outer two fingers. In some instances, for multiple localities that are in close proximity, a single symbol is used. Localities for E. alfredi, ranging from east-central Veracruz to northwestern Guatemala, are not indicated. blotch in the inguinal region. The color pat- tern of the anterior, dorsal, and posterior surfaces of the thighs is unremarkable in most species. Generally, there are about four dark transverse bands on a somewhat paler background, but the bands are often ill-de- fined and, at best, only moderately contrast- ing with the adjacent color. Eleutherodac- tylus decoratus has relatively sharply contrasting thigh bands, and, in E. polym- niae, the bands are even more distinct (Fig. 2). Both the holotype and paratype of E. po- lymniae were taken from the side of an ex- tremely steep slope adjacent to a roadcut in virgin cloud forest. They were found be- tween 23:00 h and 03:00 h. They were call- ing from vegetation; the holotype was about 3 m up in a tree, and the paratype was about 1 m above the ground. In both instances, a low fog reduced visibility to only a few me- ters and rain had fallen within the preceding 24 hr. Had we not fortuitously selected the site to make camp for the night, we most probably would not have discovered these frogs. We became aware of their presence by their remarkably voluminous and varied calls. In fact, these tiny frogs are so loud that we at first mistakenly thought that their calls belonged to some large, night-calling bird, unknown to us. Field notes taken im- mediately after the capture of UTA A-23511 indicate calls include ‘“‘a low growl, a low chuckle, single clicks, and a multinote ‘laugh.’ First two are given [relatively infre- quently]; clicks (several) precede ‘laugh’.” Four other species of Mexican Eleuthero- dactylus with expanded toe pads are known to have vocal slits (Table 1), including E. spatulatus, with which E. polymniae may be sympatric; specimens of the former have been taken from the same hillside about 200 m above the type locality for E. polymniae. Some of the structures associated with vo- calization are relatively large in E. polym- niae. The vocal slits extend forward to a point about level with the midlength of the tongue in E. polymniae; in E. spatulatus, the slits extend only to about the posterior edge of the tongue. Perhaps more remark- able is the extent of development of the cir- cular disc surrounding the glottis, which is 497 ‘suoUoods oyeuloy A[UO poUTWIeX9 oY INQ ‘S}I[S [BOOA SHOR] so1oods sry Jey) poytodos (¢96]) YOUAT ‘sn Aq poinsevour (66vbZ-V V.LM) uourtoods ve woly st oInsy JOMO] OY “Ysty AT[ensnun susos pue (e/96]) YOUAT WO; Oye) SI UOTIeLIVA JO OBURI OY) UI oINBY JOYysIY OY] , ‘($S61) JoJo Puv UOUURYS UI (| “314) Ydersoj0Yd v WO vIep dso] POALIOp SARY OM PUP ‘UOI]CLIOSOp [VUIBIIO OY} UI UDATS JOU SVM SYSIY] pur syxULT oY} JO U1D}}ed 1O[OD oY], ‘so1oods sty} JO UstwUTOOds UMOUY A[UO pue odAJO[OY OY] POUTLULXd 1OU DARY IAA ¢ ‘Ploy B JO 9OUNSoId OY) WOIdOp oO} srvodde ‘poitsop 9q 0] YONW SOARS, YOTYM ‘UOTIRNSNII[I ue “IOADMOY “(SSG JO[OA\ PUL UOUUPLYS) UOTIdIIOSop [BUISIIO OY] UI UDATS SYM P[OJ [eSIe1 Be SUIPIedOI UONPULIOJUI ON ; "SOXOS UD9MI9q SIYdIOW Ip A[SULy{INS 10U SVM SoIoods ST} UI OZIS WINUedWA] Jey) potodol (QG6]) UNIe| , VOLUME 102, NUMBER 2 uMOIQ UMOIG YUP YIM polleg Jo Avid YUM poo yUSSqY’ jUussqy’ OO OS TS US OZ OSS Oi) Ore sace IQQUuvINxX “Y uIO} -jed Surjsesjuoo Ajdievys podoyjoaop SUTxOR] Inq ‘popurq ssdo7 SSUIYIVU SNOIAGO ON AJOVVINPOUL 0} A[IOOd s— 6b'0-Zr'0 — O'9€ — SISUIUDIDINA spueq yep m04 soyoied IoyIVp YA JUISOI juNsSqV _ ¢L'0 _ 0°97 MOJAD] “A Imoj Ajjensn ‘spueq UMOIQ JOYIep pouy soIOYdouROU pd19} “OP [IT YUIIM UMOIG o[ed “BOS YUM MOTIOA [eq juosqV Wesgqy +CL0-8t 0 YE [Ot T0) SOb SOE 1MDNIS “AT sutsei1juos Ajdieys UuMOIG yep jou ‘spueq yep Ino4 YIM popour Apepndoi1] JUNSIIg JUdSIIg €r'0-re'0 O€'0-SZ7'0 7p ZOE snjojnjods “3 ssul sulseijuos Ajdieys -yIVU Yep Moy & YIM jou ‘spueq yep Ino Po1O[OS UIedID ‘quid juNsSqY _ 6S'0 — ZOr — DJOIIAJIS “5 sieq UMOIG pue UOIdO1 UIOIS UT YD}OTq o11YM BuTselUOS A[dieys O11YM Ae[NSOLII ‘odIe] VW jussqYy JUDSIIg — ATO) — L'6l IDIUWUA]Od “i -suljseuos Ajdieys 10U Combined length of internasal and prefrontal medial sutures. > Where parietals meet supraoculars and frontal. + Measured to prefrontal-preocular junction. Description of holotype.—See Rossman (1969). Variation. — Dorsal scale rows are 17-15- 17 (1 specimen), 17-17-15 (2), 17-17-17 (6), and 19-17-17 (1). Where posterior reduc- tion occurs, it results from the loss of row four at about 60% of the distance from the first to the last ventral scute. Ventrals average 145.0 (142-150) in 8 99, 154.0 (152-156) in 2 46; subcaudals 53.4 (52-56) in 7 22, 64.0 (63-65) in 2 46; tail as a % of total length 19.4 (18.9-20.0) in 7 99, 22.0 (21.8—22.2) in 2 66. Total supralabials on both sides number 12 (1 specimen), 14 (7), and 15 (2); total infralabials 16 (8), 17 Ch): and? b9:(1): In the five snakes that lack a well-defined umbilical scar, head length as a percent of snout-vent length is 5.3 (237 mm SVL), 5.2 (274), 4.7 (330), 4.8 (347), and 4.6 (360), respectively. There appears to be some on- togenetic change in this character, the large specimens having a proportionately shorter head. Head scale measurements were made on the preceding five snakes and a series of ratios generated (Table 1). Noticeable sex- ual dimorphism appears to be present in several characters (prefrontal suture length/ internasal suture length, eye diameter/fron- tal length), but the sample size is so small that these distinctions may disappear when data from additional specimens become available. In the Nuevo Leon sample, there appears to be a marked ontogenetic change in dorsal color pattern. The juveniles (Fig. 2, lower) are prominently spotted in three or four al- ternating rows, the former condition re- sulting from the fusion of spots in the upper two rows. The anteriormost 0-7 spots may be vertically enlarged to extend to, or fuse across, the vertebral scale row. The verte- bral stripe is absent or faint and interrupted at intervals by the dorsal spotting. There is a prominent dark nuchal blotch that may or may not be very narrowly divided by the VOLUME 102, NUMBER 2 509 Fig. 1. Upper: Holotype of Thamnophis exsul from 17.7 km E, 5.6 km S San Antonio de las Alazanas, Coahuila, Mexico. Reprinted with permission from Rossman (1969). Lower: Adult Thamnophis exsul (EAL 4837) from 19.6 km NE San Antonio de Pea Nevada, Nuevo Leon, Mexico. 510 ye ee Se ee. A i | PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Fig. 2. Upper: Subadult Thamnophis exsul (LSUMZ 43836) from 19.6 km NE San Antonio de Pena Nevada, Nuevo Leon, Mexico. Lower: Three juvenile Thamnophis exsul (EAL 4971) from 17.9 km NE San Antonio de Pena Nevada, Nuevo Leon, Mexico. vertebral stripe. The nuchal blotch is either continuous with the dark dorsal coloration of the head or narrowly separated from it by a lighter zone (less than one scale long) immediately posterior to the parietals. The spotted pattern of the subadult (Fig. 2, up- per) is less distinct than that of the juveniles, and is barely, if at all, discernible in the larger adults (Fig. 1, lower). The lone example from Coahuila, an adult, differs from the Nuevo Leon animals in retaining the juvenile pattern, in having VOLUME 102, NUMBER 2 larger spots, and in having total suppression of the vertebral stripe (Fig. 1, upper). The everted hemipenis (Fig. 3) of EAL 4837 is single with the distal half greatly expanded. The sulcus spermaticus is simple and terminates apically between raised lips. The apical surface of the expanded portion is nude. The remainder of the organ is spi- nose, the spines being very small on the expanded portion, but becoming larger proximally. One enlarged basal hook les somewhat removed from the sulcus. Teeth average 20.3 (19-21) on six max- illae, 12.0 (12) on two palatines, 22.0 (21- 23) on two pterygoids, and 22.5 (22-23) on two dentaries. Relationships. —None of the data provid- ed by the new material contradicts Ross- man’s 1969 conclusion that Thamnophis exsul more nearly resembles J. sca/aris than it does any other garter snake. A detailed comparison of the two species awaits com- pletion of a variational study of the 7. sca- laris complex now in progress by Rossman. The lack of posterior dorsal scale row re- duction in most (8 to 10) 7. exsul is an unusual, but not unique, condition for a Thamnophis. Most of the 7. godmani ex- amined thus far from Oaxaca and Puebla have 17-17-17 rows, as do 20% of the T. scalaris from Veracruz. Ecological notes. — Both the Coahuila and Nuevo Leon localities are situated in mon- tane areas at elevations between 2650-2800 meters (Fig. 4). The adult specimens from Puerto de Pena Nevada were found in meadows with mixed oak, pine, madrone, and scrub brush, the meadows being used for grazing (Fig. 5, upper). The snakes were found in mid-morning after the cloud cover had lifted, but while the ground cover was still moist. When discovered in the open, the snakes crawled rapidly toward the scrub cover that was never far away. The young of the year were collected from a rotten log on an oak-madrone hillock with scattered logs, agave, and rocks (Fig. 5, lower). No Fig. 3. Drawing of everted hemipenis of adult male Thamnophis exsul (EAL 4837). All spines save the larger ones are diagrammatically approximated. standing water or streams were found in the area. The habitat at Rancho La Encantada was generally similar to that described for the Puerto de Pena Nevada area; but the holotype from Coahuila was found in a grassy “sump” above the head of a steep canyon (Rossman 1969). During Liner’s visits to the Puerto de Pena Nevada area, all in July, clouds would start to roll in around 1600 h; instead of the usual mist, a light drizzle (along with thunder and lightning) often would accompany the clouds and the temperature would then turn de- cidedly colder. In the morning, the sky would clear around 0900 h; during mid-day it was sunny and hot. The associated herpetofauna in the Puer- to de Pena Nevada area was: Chiropterotri- ton priscus, Pseudoeurycea galeanae, Cro- talus pricei, Storeria occipitomaculata, Thamnophis cyrtopsis, Barisia imbricata, Eumeces brevirostris, Sceloporus grammi- GUS. US. sealaris, S. torquatus (kimer, pers. obs.); at Rancho La Encantada, Crotalus lepidus, Storeria occipitomaculata, Barisia species, Sceloporus grammicus, and S. tor- quatus (Trevino, pers. obs.); and at the type 512 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON hes jig looe 98° 96° eS Ln maw ve \ / \ ii *S “> | a : im yh —\ ve Be N 5 L e a ees G a 3 Spies Ee we | se ea a Var TROPIC OF CANCER ---—-—~— fe Mee ( -y | \A ) Oe << ( 28 be i — 22° BX \ 5 sige ‘SS Pic coe ON 2 . sl 20° ? Hn Se ile eg c ¢ wae 1ge Statute 250 25 50 75 100 Se ae as ic ; niger dieses ee f A ae yy | Dy a 104° 102° 100° 98° 96° 94 Fig. 4. Map of northwestern Mexico showing known localities for Thamnophis exsul. Triangle represents type locality in Coahuila; circles represent the Nuevo Leon localities. VOLUME 102, NUMBER 2 oye) Fig. 5. Upper: Habitat 19.6 km NE San Antonio de Pefia Nevada, Nuevo Leon, Mexico, where adult specimens of Thamnophis exsul were collected. Lower: Habitat 17.9 km NE San Antonio de Pena Nevada, Nuevo Leon, Mexico, where juvenile specimens of Thamnophis exsul were collected. 514 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON locality in Coahuila, Crotalus pricei, Barisia imbricata, Eumeces dicei (=brevirostris), Sceloporus grammicus, and S. jarrovi (Ax- tell and Sabath, 1963; Liner, Rossman, and Johnson, 1974). Acknowledgments We wish to express our gratitude to the late Richard M. Johnson, who helped to collect some of the Nuevo Leon specimens; to Richard M. Blaney for serving as a cour- ier to bring the UANL specimens to Ross- man; and to the officials of the Direccion General de la Fauna Silvestre in Mexico City for issuing the necessary scientific col- lecting permits to Liner over the years. Literature Cited Axtell, R. W., & M. D. Sabath. 1963. Crotalus pricei miquihuanus from the Sierra Madre of Coa- huila, Mexico.—Copeia 1963(1):161-164. Liner, E. A., D. A. Rossman, & R. M. Johnson. 1973[1974]. Life history: Gerrhonotus (Bari- sia) imbricatus ciliaris. —HISS News-Journal 1(6):185. Rossman, D. A. 1969. A new natricine snake of the genus Thamnophis from northern Mexico.— Occasional Papers of the Museum of Zoology, Louisiana State University (39): 1-4. (DAR) Museum of Zoology, Louisiana State University, Baton Rouge, Louisiana 70803; (EAL) 310 Malibou Boulevard, Houma, Louisiana 70364; (CHT) Facultad de Ciencias Biologicas, Universidad Auton- oma de Nuevo Leon, San Nicolas de los Garza, Nuevo Leon, Mexico; (AHC) De- partment of Biology, Texas A&I University, Kingsville, Texas 78363. PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 515-519 THE TYPE SPECIMENS OF HEKSTRA’S OWLS M. Ralph Browning Abstract.—The erroneous holotype designations and errors in the type lo- calities in Hekstra’s descriptions of 24 new subspecies of New World owls are corrected. Several scientific names are emended and taxonomic comments are appended for a small number of Hekstra’s proposed taxa. Twenty-four new subspecies of New World owls of the genus Otus were named in a paper by Hekstra (1982b) issued 17 December 1982. These same new names also appeared in Hekstra’s (1982a) unpub- lished thesis. The holotypes of the new taxa are in 10 different collections, most of which are in the United States. Incorrect infor- mation was published with regard to mu- seum designation, museum number, and collecting locality of many of the holotypes. I here list the holotypes with their correct specimen label data. The species names are here presented in the sequence proposed by Marshall & King (1988). The subspecies are generally ar- ranged from north to south. The type lo- calities given are standardized, and the spellings are corrected where required. Ab- breviations for museum designations are given under acknowledgments. The num- bers following the names refer to the pages where the descriptions were given (Hekstra 1982b). Several of the scientific names pro- posed were spelled incorrectly and these have been emended in accord with Article 31c and Appendix D of the International Code (International Commission on Zoo- logical Nomenclature 1985). Taxonomic comments are appended for a small number of Hekstra’s proposed taxa. The remaining forms he named require further study. Otus flammeolus borealis, p. 56 Holotype. —MVZ 101700, adult female, Penticton, Okanagan Valley, British Co- lumbia, shore of Okanagan Lake, 22 Oct 1901, collected by Allan Brooks (original number 1818). Remarks. — The catalogue number of the holotype was given as “10,700.” The type locality, as published, did not include Oka- nagan Lake. Additional specimen label data are the collector’s original number and that the holotype was found dead, with the spec- imen label notation “‘probably killed two weeks before” (N. K. Johnson, in litt.). Otus flammeolus frontalis, p. 56 Holotype.—USNM 119650, female, Estes Park, Colorado, 20 Jun 1890, collected by W. G. Smith. Remarks. —Hekstra (1982b) stated that the holotype was a breeding individual but the specimen label does not so indicate. This form is a recognizable subspecies (J. T. Mar- shall, pers. comm.). Otus flammeolus meridionalis, p. 55 Holotype. —MVZ 109708, adult male, 25 Aug 1938, Cuapongo, Guerrero, Mexico, collected by W. W. Brown. Remarks.—The catalogue number was published as “10978.” The original label of the holotype indicates that the testes were minute (N. K. Johnson, in litt.). Otus seductus colimensis, p. 61 Holotype.—LSUMZ 39853, adult male, 7 miles south of Colima, Colima, [Mexico], 516 24 Dec 1958, collected by W. J. Schaldach, Jt Remarks.—This specimen was number 7001 in the Sheffler Collection, and on an additional label is recorded as “‘S. no. 4808,” which presumably is Schaldach’s personal catalogue number (J. V. Remsen, in litt.). Otus trichopsis inexpectus, p. 58 Holotype. —USNM 152828, adult fe- male, Porto Jimenz, Costa Rica, 30 May 1892, collected by Verrill. Remarks. —Hekstra (1982b) gave the museum designation as Chicago (=Field) Museum of Natural History and the cata- logue number as “52828.” The primaries of the holotype are clipped and no doubt the specimen was a Captive bird. The specimen is an example of Otus guatemalae in the red phase (J. T. Marshall, pers. comm.). Otus choliba caucae, p. 60 Holotype. —RMNHL 8091, [adult] male, El Tambo, 5100 ft., Rio Cauca, Colombia, 25 June 1938 [collected by Kjell von Schneidern]. Remarks. — There is no indication of the age or collector on the specimen label of the holotype but the published information (as above) is correct (G. F. Mees, in litt.). Otus choliba montanus, p. 61 Holotype. —BM(NH) 1914.11.22.219, adult male, Valle, Montana Sierra, 2000 m, Mérida, [Venezuela], 15 Apr 1909, collect- ed by S. Briceno Gabaldon. Otus choliba kelsoi, p. 61 Holotype. —AMNH 59483, adult male, Princes Town, Trinidad, 10 Mar 1893, col- lected by Frank M. Chapman. Remarks. —In naming this form Hekstra (1982b) stated that kelsoi “‘replaces Otus choliba portoricensis Kelso ... preoccu- pied.””’ However, Kelso (1942) clearly did not introduce a new name but only referred the population from Trinidad to the name PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Scops portoricensis Lesson, 1831. Hekstra (1982b) proposed ke/soi as the name of a new taxon (Greenway 1987). Hekstra (1982a) spelled the specific locality as “Princetown” which is the same as on the specimen label. Modern gazetteers spell the locality as Princes Town. Otus choliba guyanensis, p. 60 Holotype. —BM(NH) 1888.7.20.63, adult male, Mt. Roraima, 3500 ft., Guyana; 9 Jan 1884, collected by H. Whitely, Jr. (P. R. Colston, in litt.). Remarks.—The catalogue number was published as “*88.7.20.63.”? The type local- ity of guyanensis is the same as that for Scops roraimae Salvin, 1897 (=Otus gua- temalae roraimae, cf. Peters 1940), a name based on topotype 1888.7.20.62 that was collected by H. Whitley, Jr., on 1 Oct. 1883 (Warren 1966). Otus choliba caatingensis p. 59 Holotype. —FM 191645, adult male, Jan- auba, northern Minas Gerais, [Brazil], -- Jul 1949, collected by Ricardo Medeiros Berla. Otus choliba chapadensis, p. 59 Holotype. —AMNH 34595, adult female, Chapada, Mato Grosso, [Brazil], 9 Feb 1883, collected by H. H. Smith. Remarks.—The holotype of O. atricap- illus fulvescens Hekstra, AMNH 34597, was collected by Smith from the same locality as the holotype of chapadensis (see beyond). Otus choliba uruguaiensis, p. 59 Holotype. -AMNH 769736, adult fe- male, Arroyo, Urugua-i, km 10, Misiones, Argentina, 29 May 1958, collected by W. H. Partridge. Remarks. — Hekstra (1982b) proposed the trinomial as “urugaii” and under the head- ing of the derivation he spelled the name as “uruguail.’’> The AMNH catalogue number was given by Hekstra (1982b) as “76736” (see Greenway 1987). Hekstra (1982b) gave VOLUME 102, NUMBER 2 the collecting locality as “Argentina, Mi- siones, Arroyo, River Uruguai, km 10.” Otus choliba alilicuco, p. 59 Holotype. —BM(NH)_ 1899.1.27.236, adult male, Rosario, Province Salta, Argen- tina, 15 Sep 1896, collected by Gesling, for- merly R. P. Moreno collection (P. R. Col- ston, in litt.) Remarks. — Hekstra (1982b) published the catalogue number as “99.1.27.235, and year the of collection as “1895.” Otus choliba koepckeae, p. 60 Holotype. —-AMNH 802425, adult fe- male, near Yungai, 4000 m, Quebrada Yun- gay, Cordillera Blanca, Departamento An- cash, Peru, 3 Aug 1960, collected by Maria Koepcke. Remarks. —Hekstra (1982b) referred to the holotype as no. 1699 from the Koepcke collection “‘on loan at AMNH.”’ The name was originally spelled by Hekstra as “koepckei’’ and was properly emended to to koepckeae by Greenway (1987). This form is considered a distinct species by Marshall & King (1988). Otus atricapillus moreliensis, p. 62 Holotype. —AMNH 115738, male, Mo- relia (Rio Bodoquera), Caqueta, 600 ft., Co- lombia, 22 Jul 1912, collected by L. E. Mil- ler. Remarks. —The trinomial was originally spelled ‘‘morelius’’ and the locality as ‘“‘La Morelia” by Hekstra (1982b), who referred to the locality Caqueta as ““Rio Caqueta.”’ Otus atricapillus is known only from Par- aguay and adjacent Brazil, and the holotype may represent either O. sanctaecaternae or O. choliba (J. T. Marshall, pers. comm.). Otus atricapillus inambariensis, p. 62 Holotype. —FM 222284, female, Hua- jyumbe, near Quincemil on the Rio Inam- bari, 630 m Cuzco, Peru, 28 Jun 1953, col- lected by C. Kalinowski. 517 Remarks. —Hekstra (1982b) spelled the trinomial as “inambarii,” from the locality Rio Inambari. He gave the type locality as “Quince Mil. Huajyumba, at side of river of the Inambari, Cuzco, 630 m, Peru.” However, the Rio Inambari is 45 km SE of Quincemil (see Stephens & Traylor 1983). The holotype, an adult (D. Willard, in litt.), resembles examples of O. watsonii in the brown phase (D. Willard & J. Fitzpatrick, pers. comm.). Otus atricapillus ater, p. 61 Holotype.—USNM 513892, adult male, Belem, Para, [Brazil], 22 Jul 1964, collected by Phillip S. Humphrey. Remarks.—The ‘“SUSNM field nr. 196899,” given for the holotype by Hekstra (1982b), is the collector’s catalogue number. Additional information on the specimen la- bel include reproductive data and soft part colors. The holotype is an example of O. watsonil (pers. observ., J. T. Marshall, pers. comm.). Otus atricapillus fulvescens, p. 62 Holotype. —-AMNH 34597, adult female, Chapada, Mato Grosso, [Brazil], 20 Jul 1883, collected by H. H. Smith. Remarks.—The holotype of O. choliba chapadensis Hekstra, AMNH 34595, was collected by Smith from the same locality as the holotype of fulvescens. Otus guatemalae pettingilli, p. 56 Holotype. —DMNH 52892 (ex Cornell Univ. 10445), female, above Rio Savinas near Gomez Faria, Tamaulipas, Mexico, 11 Apr 1941, collected by O. S. Pettingill, Jr. (original no. 1046). Remarks. — Hekstra (1982b) did not name the repository or give a catalogue number for this holotype. Under the heading ““Type”’ and following the new name, Hekstra (1982b) wrote, in quotes: “G. M. Sutton, 1949 (manuscript name).’’ Under the head- ing “Derivation of name,” Hekstra stated 518 that the name pettingilli was “from a manu- script name on a label (by Griscom?).”” The holotype of pettingilli is the specimen of Otus guatemalae referred to by Sutton & Pettin- gill (1942) as being similar in size but grayer above than the holotype of O. g. cassini. Otus guatemalae petenensis, p. 57 Holotype. -UMMZ 137395, adult fe- male, Laguna Perdida, Peten, Guatemala, 18 Apr 1920, collected by P. W. Shufeldt (R. W. Storer, in litt.). Remarks. —Hekstra (1982b) spelled the trinominal as “‘peteni”’ from the locality Pe- ten. The name of the lake was incorrectly spelled as “‘Perida.”’ Otus guatemalae centralis, p. 57 Holotype. —USNM 484980, adult fe- male, Cerro Mali, 4100 feet, Darien, Pan- ama, 14 Feb 1964, collected by C. O. Han- dley, Jr. Remarks. — Additional information on the specimen label: “skull oss; ovary 15 x 10 [mm]; largest ova 3.” Otus guatemalae pallidus, p. 57 Holotype. —AMNH 476699, adult, sex unknown, Andes de Cumana, northern Venezuela, -- Mar 1897, collected by Eng. André, formerly Museo Delmas (no. B.11.3.C.-81) and Rothchild Collection. Remarks. —Hekstra (1982b) omitted the name of the collector and data on the mu- seums formerly holding the specimen (see Greenway 1987). Otus guatemalae rufus, p. 58 Holotype.—BM(NM) 1888.7.20.64, adult, sex unknown, Balzar Mtns., western Ecua- dor, -- Mar 1880, collected by Illingsworth. Remarks. —The museum designation was given by Hekstra (1982b) as “USNM”’ al- though the catalogue number was given as above. Derek Goodwin (in litt.) confirmed PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON that this specimen is in the British Museum (Natural History). Otus guatemalae pacificus, p. 58 Holotype. —BM(NH) 1902.3.13.1564, adult female, Morropon, 140 m, Piura, northwestern Peru, 27 Aug 1899, collected by P. O. Simons. Remarks. —The catalogue number of the holotype was given by Hekstra (1982b) as “BM 023.13.1564.’ Acknowledgments I thank the following who verified the in- formation on the specimen labels and the museum catalogue numbers of the holo- types: M. LeCroy, American Museum of Natural History (AMNH); D. Goodwin and P. R. Colston, British Museum (Natural History) (BM(NH)); D. Niles, Delaware Museum of Natural History (DMNH); D. Willard and S. Lanyon, Field Museum of Natural History (FM); J. V. Remsen, Jr., Louisiana State University Museum (LSUMZ); N. K. Johnson, Museum of Ver- tebrate Zoology (MVZ); G. F. Mees, Rijks- museum van Natuurlike Histoire (RMNH); and R. W. Storer, University of Michigan Museum of Zoology (UMMZ). The other holotypes are in the collection of the U.S. National Museum of Natural History (USNM). R. C. Banks, N. K. Johnson, M. LeCroy, and J. T. Marshall read the manuscript and offered helpful suggestions. Literature Cited Greenway, J. C., Jr. 1987. Type specimens of birds in the American Museum of Natural History. Pt. 4.—American Museum Novitates No. 2879, 63 pp. Hekstra, G. 1982a. “I don’t give a hoot...” A re- vision of the American Screech owls (Otus; Strigidae). Unpublished thesis, Universiteit te Amsterdam. The Netherlands. Hekstra,G. P. 1982b. Description of twenty-four new subspecies of American owls (Aves: Strigi- VOLUME 102, NUMBER 2 dae).— Bulletin Zoologisch Museum Universi- teit Amsterdam 9(7):49-63. International Commission on Zoological Nomencla- ture. 1985. International code of zoological nomenclature. 3rd ed. International Trust No- menclature, British Museum (Natural History), London, 338 pp. Kelso, L. 1942. The ear of Otus asio. Biological Leaf- let Number 14, 2 pp. Marshall, J. T., & B. F. King. 1988. Subfamily Strigi- nae typical owls genus Otus. Pp. 331-336 in D. Amadon and J. Bull, ed., Hawks and owls of the World: A distributional and taxonomic list. — Proceedings of the Western Foundation of Ver- tebrate Zoology 3(4):294-357. Peters, J. L. 1940. Check-list of birds of the world. Volume 4. Museum of Comparative Zoology, Harvard University, Cambridge. 291 pp. 519 Stephens, L., & M. A. Traylor, Jr. 1983. Ornitholog- ical gazetteer of Peru. Museum of Comparative Zoology, Harvard University, Cambridge. 271 pp. Sutton, G. M., & O. S. Pettingill. 1942. Birds of the Gomez Farias region, southwestern Tamauli- pas.— Auk 59(1):1-34. Warren, R. L. M. 1966. Type-specimens of birds in the British Museum (Natural History). Vol. 1. Non-passerines. Trustees British Museum (Nat- ural History), London. 320 pp. U.S. Fish and Wildlife Service, National Ecology Research Center, U.S. National Museum of Natural History, Washington, DG .20560: PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 520-531 CHROMOSOMES OF TEN SPECIES OF PHILIPPINE FRUIT BATS (CHIROPTERA: PTEROPODIDAE) Eric A. Rickart, Lawrence R. Heaney, and Mark. J. Rosenfeld Abstract.—Standard karyotypes and silver-stained nucleolar organizer re- gions (Ag-NORs) of ten species of Philippine pteropodids are described. Results are discussed in the context of an updated version of Andersen’s (1912) phy- logeny. Data for Cynopterus brachyotis (2N = 34), Eonycteris spelaea (2N = 36) and Macroglossus minimus (2N = 34) agree with previous reports. Pteropus hypomelanus (2N = 38) and Rousettus amplexicaudatus (2N = 36) have stan- dard karyotypes identical to those of congeners. The Philippine endemic species Haplonycteris fischeri (2N = 58), Ptenochirus jagori (2N = 44) and Ptenochirus minor (2N = 46) have distinctive karyotypes consisting primarily of acrocentric elements. Haplonycteris has the highest diploid number for the suborder. The karyotypes of Harpyionycteris whiteheadi (2N = 36) and Nyctimene rabori (2N = 38) are distinctive, but share some apparenntly derived features with cy- nopterine genera. In all taxa examined, the Ag-NORs corresponded to the secondary constrictions on the pair of ““marker’’ chromosomes. These results demonstrate that the cynopterine section is the most chromosomally variable clade in the Pteropodidae. The family Pteropodidae is a large and diverse assemblage of Old World bats that appears to constitute a natural group dis- tinct from other chiropterans (Smith 1980, Koopman 1984). In the only monographic study of the entire family, Andersen (1912) used morphological criteria to construct a detailed phylogeny. Andersen’s work re- mains the most complete statement of re- lationships within the family. However, it is important to test and, if necessary, modify his kinship hypotheses using independent evidence. Prior analysis of standard karyotypes of pteropodids had led to the early assumption that chromosomal variation within the family is relatively limited (Haiduk et al. 1980). However, differential staining tech- niques have shown that several genera with similar standard karyotypes substantially differ in banding patterns (Haiduk et al. 1981). Nevertheless, fewer than half of the recognized pteropodid genera have been karyotyped to date, and fewer have been examined for banding patterns (Haiduk et al. 1981). In this paper, we present standard karyo- types of ten species of Philippine pteropod- ids representing nine genera and two subfamilies. Chromosomal data for the gen- era Haplonycteris, Harpyionycteris, Nycti- mene, and Ptenochirus, and for eight of the species are reported for the first time. We also present results on silver-stained nu- cleolar organizer regions (Ag-NORs) for each species and discuss variation in pteropodid ““marker’” chromosomes. We have inter- preted our results in the context of Ander- sen’s (1912) phylogeny, as updated to in- clude genera described since 1912. Materials and methods.—Our animals were all freshly collected from wild popu- lations and killed with sodium pentabar- bitol (Nembutal) or with chloroform within 24 h of capture. Chromosome terminology and preparation methods followed those of Patton (1967) with the exception that 0.4% potassium chloride was used for the hypo- VOLUME 102, NUMBER 2 tonic treatment. Cells were processed and fixed in the field, and suspensions were stored at 0O-10°C within two weeks of fixa- tion. After three to seven months, air-dried slides were made at the University of Utah. Standard karyotypes were prepared for each specimen from photographs of slides stained with Giemsa. Silver-stained nucleolar or- ganizer regions (Ag-NORs) were examined using a procedure modified from that de- scribed by Howell & Black (1980). Deter- minations of diploid number were based on minimal counts of 10 mitotic spreads per individual. Fundamental numbers (FN) re- fer to numbers of autosomal arms. Due to variable specimen quality and the presence of minute chromosomes in some species, we consider some FN values to be provi- sional, as indicated by question marks. Specimens examined were prepared as skins with partial skeletons or preserved in fluid and are deposited in the National Museum of Natural History (USNM), Washington, DDG: Specimens Examined Cynopterus brachyotis (Muller, 1838).— Leyte Island, Leyte Province, 7 km N Bay- bay, cley. 10 m, 10°45'’N, 124°47’E (1 9); Negros Island, Negros Oriental Province, Mumacnete City, clev. 5 m,. 09°18’N, Pooks E (13, 2 29). Eonycteris spelaea (Dobson, 1871).— Leyte Island, Leyte Province, Cathedral Cave, 4 km S, 1 km E Inopacan, elev. 50 m, 10°28’N, 124°45’E (2 22); Negros Island, Negros Oriental Province, Caves at 4 km N Manjuyod, elev. 20 m, 09°43'N, 123°10’E (4 38). Haplonycteris fischeri Lawrence, 1939.— Biliran Island, Leyte Province, 5 km N, 10 km E Naval, elev. 850 m, 11°36’N, 124°29’E (ives 12); Leyte Island, Leyte Province, Mount Pangasugan, 10.5 km N, 4 km E Baybay, elev. 700 m, 10°47’'N, 124°50’E (1 6, 1 9). Harpyionycteris whiteheadi Thomas, 1896.—Leyte Island, Leyte Province, Mount 521 Pangasugan, 10.5 km N, 4 km E Baybay, elev. 700 m, 10°47’N, 124°50’E (3 3, 4 99); Negros Island, Negros Oriental Province, Mount Guinsayawan, 3 km N, 17 km W Dumaguete City, elev. 1280 m, 09°22’N, 123°09’E (1 &). Macroglossus minimus (E. Geoffroy, 1810).—Negros Island, Negros Oriental Province, Dumaguete City, elev. 5 m, 09°18'N, 123°18’E @G 6é, 1 9). Nyctimene rabori Heaney & Peterson, 1984.—Negros Island, Negros Oriental Province, Mount Guinsayawan, 3 km N, 17 km W Dumaguete City, elev. 1280 m, Q9°22'N, 123°O9EAGWS): Ptenochirus jagori (Peters, 1861).—Leyte Island, Leyte Province, 7 km N Baybay, elev. 10 m, 10°45'N, 124°47’E (1 6, 6 22), Mount Pangasugan, 10.2 km N, 2.2 km E Baybay, elev. 320 m, 10°46'N, 124°49’E (1 8). Ptenochirus minor Yoshiyuki, 1979.— Leyte Island, Leyte Province, Mount Pan- gasugan, 10.2 km N, 2.2 km E Baybay, elev. 320 m, 10°46’N, 124°49’E (2 64, 5 29). Pteropus hypomelanus Temminck, 1853.—Negros Island, Negros Oriental Province, 9 km N, 14 km W Dumaguete City, elev..600 m, 09223'N, 123°L17E (1 6, 2 99). Rousettus amplexicaudatus (E. Geoffroy, 1810).—Leyte Island, Leyte Province, 7 km N Baybay, elev. 10 m, 10°45'N, 124°47’'E (2 46, 4 22); Negros Island, Negros Oriental EFOvinee ~Oumacuete City, clev. 5 m, 09°18'N, 123°18’E (2 99). Results We present standard karyotypes and sil- ver-stained marker chromosomes for male specimens of eight pteropodid species in Figs. 1—4 and briefly discuss them below. Karyotypes for two additional species are discussed, but not illustrated. Subfamily Pteropodinae Cynopterus brachyotis. 2N = 34, FN = 58, Fig. 1A.—The karyotype is indistin- 522 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON Af SC AR RO BR RE BR * X Y Fig. 1. Standard karyotypes and silver-stained marker chromosomes showing nucleolar organizer regions (insets) of (A) Cynopterus brachyotis 6 (USNM 458083), 2N = 34, FN = 58; (B) Haplonycteris fischeri 6 (USNM 458196), 2N = 58, FN = 66(?). VOLUME 102, NUMBER 2 523 A le WX 6G AR ORR kK oa i Ab GA AR GS GK ne Ah AA 0H Of §b. mY B AY AR AR WR OBR ke RG Oe Ax 44 44 RA Bb ax “a6 a - ~*~ * ~ -£ = a » * Fig. 2. Standard karyotypes and Ag-NORs (insets) of (A) Harpyionycteris whiteheadi 6 (USNM 458213), 2N = 36, FN = 58; (B) Nyctimene rabori 6 (USNM 458906), 2N = 38; FN = 60. ‘teh = 3. XY Ak bp 4 * ea 20 88 @0 46 “* AA aoe se e8@ a@ 6 #*#* «ee B 44 Bh aK tk Aa a@ 80 @8 An ee a8 sz «? ya ; ae an esp 028 AH 47 2 oe « Ae XY Fig. 3. Standard karyotypes and Ag-NORs (insets) of (A) Ptenochirus jagori 6 (USNM 458322), 2N = 44, FN = 56(?); (B) Ptenochirus minor 6 (USNM 458424), 2N = 46, FN = 56(?). VOLUME 102, NUMBER 2 i Wo St UR xy ay ak aR 4S te ye La + " XY B SU AM ux KA XR OH B® 525 SA AA AA AA i - XY Fig.4. Standard karyotypes of (A) Pteropus hypomelanus 6(USNM 458447), 2N = 38, FN = 72; (B) Rousettus amplexicaudatus 6 (USNM 458486), 2N = 36, FN = 68. Asterisks indicate marker chromosomes. 526 guishable from those reported by previous workers (Yong et al. 1973, Ando et al. 1980, Harada & Kobayashi 1980). The autosomal complement consists of 11 pairs of meta- centrics or submetacentrics, 2 pairs of sub- telocentrics, and 3 pairs of acrocentric chro- mosomes. A_ pair of medium-sized metacentrics are marker chromosomes, that have a secondary constriction on the short arm near the centromere. In C. brachyotis, and in other species (see below), the sec- ondary constriction coincides with the Ag- NOR site. The X chromosome is a medi- um-sized submetacentric and the Y, a small acrocentric. Haplonycteris fischeri. 2N = 58, FN = 66(?), Fig. 1B.—The autosomal comple- ment consists of 3 pairs of small to medium- sized submetacentrics, 2 pairs of small to medium-sized subtelocentrics, and 23 pairs of small to medium-sized acrocentric (or possibly subtelocentric) chromosomes. The marker chromosome is a medium-sized ac- rocentric. The X is a medium-sized sub- metacentric and the Y, a small acrocentric. Harpyionycteris whiteheadi. 2N = 36, FN = 58, Fig. 2A.—The autosomal complement consists of six pairs of medium to large metacentric or submetacentric chromo- somes, six pairs of medium-sized subtelo- centrics, and five pairs of medium-sized ac- rocentrics. The marker chromosome is a large metacentric. The X chromosome is a medium-sized subtelocentric and the Y, a small acrocentric. Nyctimene rabori. 2N = 38, FN = 60(?), Fig. 2B.— The autosomal complement con- sists of eight pairs of medium to large meta- centrics and submetacentrics, four pairs of medium-sized subtelocentrics, and six pairs of small acrocentric (or subtelocentric) chromosomes. The marker chromosome is a medium-sized metacentric. The X chro- mosome is a medium-sized metacentric and the Y, a small submetacentric. Ptenochirus jagori. 2N = 44, FN = 56(?), Fig. 3A.—The autosomal complement has 4 pairs of small to large metacentric or sub- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON metacentric chromosomes, 3 pairs of me- dium-sized subtelocentrics, and 14 pairs of small to medium-sized acrocentrics (or sub- telocentrics). The marker chromosome is a medium-sized acrocentric. The X chro- mosome is a medium-sized submetacentric and the Y, a small acrocentric. Ptenochirus minor. 2N = 46, FN = 56(?), Fig. 3B.—The standard karyotype is similar to that of the P. jagori. However the auto- somal complement includes 2 subtelocen- tric pairs and 16 acrocentric pairs (as op- posed to 3 and 14, respectively, for P. jagori). Pteropus hypomelanus. 2N = 38, FN = 72, Fig. 4A.—A diploid number of 38 for this species was reported by Yong & Dhal- iwal (1976), but the karyotype was not il- lustrated. The autosomal complement con- sists of 10 pairs of small to large metacentrics or submetacentrics, and 8 pairs of small to medium-sized subtelocentrics. The marker chromosome is a medium-sized submeta- centric. The X chromosome is a medium- sized subtelocentric and the Y, a small ac- rocentric. Rousettus amplexicaudatus. 2N = 36, FN = 68, Fig. 4B.—The autosomal group con- sists of 13 pairs of small to large metacentric and submetacentric chromosomes, and 4 pairs of medium-sized subtelocentrics. The marker chromosome is a medium-sized metacentric. The X is a medium-sized sub- metacentric and the Y, a small acrocentric. Subfamily Macroglossinae Eonycteris spelaea. 2N = 36, FN = 66, not figured. — Our specimens yielded karyo- types similar to those reported previously (Yong & Dhaliwal 1976, Ando et al. 1980, Harada et al. 1982). The autosomes consist of 14 pairs of small to large metacentrics or submetacentrics, 2 pairs of medium-sized subteocentrics, and 1 pairs of small acro- centrics. The marker chromosome is a me- dium-sized metacentric. The X is a medi- um-sized metacentric and the Y, a small submetacentric. VOLUME 102, NUMBER 2 Macroglossus minimus. 2N = 34, FN = 62, not figured. — Our results agree with those of Ando et al. (1980) and Yong & Dhaliwal (1976). The autosomal complement in- cludes 12 pairs of small to large metacentric and submetacentric chromosomes, 3 pairs of medium-sized subtelocentrics, and 1 pair of minute acrocentrics. The marker chro- mosome is a medium-sized metacentric. The X chromosome is a medium-sized meta- centric and the Y, a small acrocentric. Discussion Karyotypic data represent a source of in- formation that may be used for studies of phylogenetic relationships. Because our data and those of previous reports are, with a single exception (Haiduk et al. 1981), re- stricted to unbanded standard karyotypes, we believe that there is not yet an adequate basis for an independent analysis of rela- tionships. Instead, we use Andersen’s (1912) morphologically-based phylogeny as a framework in which to examine chromo- somal data. Andersen (1912) did not use current ter- minology in his monograph of the Ptero- podidae. However, his general methodol- ogy is acceptable by today’s standards. He differentiated character polarities, prefer- entially used derived characters in con- structing the phylogeny, and recognized monophyly of groups. Andersen’s (1912: pp. lu, 1x1) graphic depiction of relationships within the portion of the subfamily Ptero- podinae relevant to this study is shown in Fig. 5, with several slight modifications. First, he considered Cynopterus to be near or part of the ancestral stock that gave rise to other members of the Cynopterus group, and so placed Cynopterus at the base of the group rather than on a terminal branch. The arrangement shown represents our inter- pretation of his conclusions based on his discussion of characters. Second, we have included six genera that have been named since 1912. The genera Aethalops, Latidens, S27 and Paranyctimene were described within the context of Andersen’s character system, and their cladistic positions are unambig- uous (Thomas 1932, Tate 1942, Thonglon- gya 1972). Unfortunately, the Philippine endemic genera Alionycteris, Haplonycteris, and Otopteropus were not described within Andersen’s framework, so their positions are harder to determine. The three genera are very similar and undoubtedly closely relat- ed (Lawrence 1939; Kock 1969a, b). They resemble several other small cynopterines (e.g., Aethalops and Balionycteris), but most similarities involve character losses. Pend- ing a thorough analysis of characters, we tenatively associate them with the Cynop- terus group. Several authors have differed with An- dersen’s interpretation of pteropodid phy- logeny: these differences indicate areas of uncertainty. Miller (1907) and Simpson (1945) listed Harpyionycteris as the sole member of a separate subfamily Harpyio- nycterinae. Anderson himself recognized the subfamily in his formal classification. How- ever, his discussion and diagrams indicate that he did so because of the many unique features of Harpyionycteris, and that he con- sidered Dobsonia, a member of the rouset- tine section, to be its sister-taxon (Fig. 5). Similarly, Miller (1907), Simpson (1945), and others have recognized the unique fea- tures of Nyctimene and Paranyctimene, and have placed them in a separate subfamily. However, Andersen noted that Nyctimene shared derived characters with members of the cynopterine section, and he placed it in that group. Andersen considered most char- acters of Myonycteris to be primitive for the family. However, on the basis of several derived features he united this genus with the cynopterines. Bergmans (1976) trans- ferred Myonycteris to the rousettine section based principally on characters that Ander- sen believed to be primitive for the family, but that Bergmans considered to be useful for defining the rousettines. Previous karyotypic work on megachi- 528 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON * - fe ” * = o = "” = . ae Ce een: ee ee ee = ww Op c 2 ow > ee te Sn a oma Mr Fa x 4“ wm 2D = te > Oar z2zo =F Oo Wok OCR rs) Om 2 Se SG So eon 22 oo 2 & 9. 0 4. - 0 2 4 Fz Oe 2 OU eee OO ‘a “Dn Of aE 2° Ore &- OVE aS Or aS o JS FatewWwr+reaewrtroadcr>+weatoryrodcdd ae q¢0O2ZzaAaf2 0 A 3 2 FO a2 << Of CO 8 2 ff ff Wea 7 ? CYNOPTERUS group CYNOPTERINE ROUSETTINE section section Fig. 5. Phylogeny of the cynopterine and rousettine sections of the subfamily Pteropodinae modified from Andersen (1912). Asterisks indicate genera described since 1912 (see text). ropterans suggested a rather narrow range of variation in chromosome number and shape, most taxa having diploid numbers ranging from 34 to 38 and a majority of biarmed elements (Summarized in Haiduk et al. 1980; 1981). Exceptions include Bal- ionycteris maculata (2N = 24) and Mega- erops ecaudatus (2N = 24, 26) with lower diploid numbers, and Penthetor lucasi (2N = 48) with a higher count (Yong & Dhaliwal 1976, Harada et al. 1982, Yong 1984). Our data on the Philippine endemic Haplonyc- teris (2N = 58; Fig. 1B) now place it at the upper extreme for the suborder Megachi- roptera. In contrast to all other pteropodids examined except Ptenochirus (see below), the karyotype of Haplonycteris consists pri- marily of acrocentric elements. In contrast to Cynopterus (2N = 34; Fig. 1A), the FN differences (66 vs. 58) indicates a series of changes including both whole arm translo- cations and non-Robertsonian events. The two species of Ptenochirus, another genus endemic to the Philippines, also have high diploid numbers (2N = 44 and 46). The difference in 2N supports the specific status of the recently described P. minor (Yoshiyuki 1979, Heaney & Rabor 1982). The species share an FN of 56 and appear to be separated by a single Robertsonian whole-arm translocation. As is the case with Haplonycteris, the karyotypes include a high proportion of acrocentrics (Fig. 3A, B). However, Ptenochirus also possess a num- ber of large biarmed elements not present in Haplonycteris. Andersen (1912) considered Nyctimene a specialized member of the cynopterine sec- tion. With FN = 60 and six pairs of small acrocentric elements, the standard karyo- type of Nyctimene rabori (Fig. 2B) does re- semble those of several cynopterines. How- ever, the small metacentric marker chromosome and the metacentric Y distin- guish it from other genera in this section. The relationship of Harpyionycteris to other pteropodids is uncertain. Andersen (1912) associated it with his rousettine sec- VOLUME 102, NUMBER 2 tion as the sister-taxon to Dobsonia, where- as Tate (1951) postulated a closer associa- tion with Nyctimene on the basis of certain shared characters (fusion of premaxillae and contact of lower canines). Although the dip- loid number of Harpyionycteris (2N = 38; Fig. 2A) is near the median value for the family (2N = 36), the standard karyotype is unique. Several pairs of relatively large acrocentric elements distinguish it from known karyotypes of epomophorine, rou- settine and macroglossine genera. This fea- ture allies it with the cynopterines, although the absence of small acrocentrics is distin- guishing. The rousettine section of the Pteropodi- nae seems relatively conservative karyotyp- ically. All members of the genus Pferopus examined to date, including P. hypomelan- us (Fig. 4A), exhibit similar standard karyo- types with 2N = 38, FN = 72 (Haiduk et al. 1980, Harada & Kobayashi 1980, Ka- sahara & Dutrilaux 1983). However, there are some interspecific differences in hetero- chromatin content (Kasahara & Dutrilaux 1983). Rousettus karyotypes resemble those of Pteropus in that they consist almost ex- clusively of biarmed elements. The stan- dard karyotype of Rousettus amplexicau- datus (2N = 36, FN = 68; Fig. 4B) is indistinguishable from that reported by Harada et al. (1982) and Ray-Chaudhuri et al. (1968) for R. leschenaulti. The only other member of the genus that has been exam- ined, Rousettus aegyptiacus (2N = 36, FN = 66), differs from R. amplexicaudatus and R. leschenaulti by a single rearrangement of the smallest autosomal element, which is acrocentric rather than biarmed (Dulic & Mutere 1973, Haiduk et al. 1981). Our data on the widespread macroglos- sine species Eonycteris spelaea and Mac- roglossus minimus agree with previous findings (Yong and Dhaliwal 1976). Little karyotypic variation has been detected among macroglossines, but few taxa have been examined (Haiduk et al. 1980). Extreme diploid numbers (24 to 58) for 529 the pteropodids are confined to the cynop- terine section of the subfamily Pteropodi- nae, whereas in the rousettine section and in the Macroglossinae, presumably out- groups to cynopterines, diploid numbers range only from 34 to 38 (Haiduk et al. 1980). This pattern suggests that both higher and lower diploid numbers represent de- rived states within the cynopterine section. The morphological specializations of both Haplonycteris and Megaerops relative to the presumed primitive genus Cynopterus (An- dersen 1912; Lawrence 1939) support this contention. The broad range in FN (44-66) indicates that karyotypic evolution within the cynopterine section has involved more than Robertsonian rearrangements. With the possible exception of Scotonyc- teris ophiodon, all pteropodids examined possess a pair of marker chromosomes with secondary constriction sites (Haiduk et al. 1980). Yong (1984) demonstrated that the secondary constriction corresponds to the silver-stained nucleolar organizer region in Megaerops. This same relationship, which also exists for several vespertilionids (Vol- leth 1987), was observed for all taxa in this study. In a few of our specimens, prepara- tions consistently revealed only one mark- er/NOR element (e.g., Fig. 1B). No speci- men had more than one pair. In Haplonycteris and Ptenochirus, the NOR sites are located on medium-sized acrocen- trics. In the other genera, they are on a pair of medium-sized or large metacentrics or submetacentrics. For all taxa, the NORs are located interstitially near the centromere. The general uniformity of the marker arms suggests that they are homologous through- out the family. However, variation in the size of biarmed marker chromosomes (e.g., between Harpyionycteris and Nyctimene) may indicate non-homologous Robertson- ian events or differences in heterochromatin content. Data currently available allow us to draw several general conclusions. First, the subfamily Macroglossinae and the rouset- 530 tine section of the subfamily Pteropodinae exhibit low variability in gross chromo- somal morphology. Second, our data rein- force earlier observations of the cynopterine section of the Pteropodinae as the most karyotypically variable clade in the family. Third, the karyotype of Harpyionycteris fur- ther highlights the uncertainty of its phy- logenetic placement. Although these con- clusions demonstrate the utility of karyotypes in investigating pteropodid phy- logenetic relationships, they also indicate the need for more extensive studies involving banding data. Acknowledgments We thank P. Heideman, J. Klompen, and R. Utzurrum for their valuable field assis- tance in the Philippines. M. Carleton and L. Wilburn provided helpful comments on the manuscript. We gratefully acknowledge the cooperation and assistance of the Phil- ippine Bureau of Forest Development, the Philippine National Museum, Silliman University, and the Institute of Philippine Culture at Ateneo de Manila University. This study was supported by National Sci- ence Foundation grant number BSR- 8514223 (awarded to L. R. Heaney). Literature Cited Andersen, K. 1912. Catalogue of the Chiroptera in the collection of the British Museum, Vol. 1: Megachiroptera. 2nd ed. British Museum (Nat- ural History), London. pp. ci + 854. Ando, K., T. Tagawa, & T. A. Uchida. 1980. A karyo- typic study on four species of the Indonesian fruit-eating bats belonging to Cynopterus, Eonyc- teris, and Macroglossus (Chiroptera: Pteropi- dae). —Caryologia 33:41-53. Bergmans, W. 1976. A revision of the African genus Myonycteris.—Beaufortia 24:189-216. Dulic, B. & F. A. Mutere. 1973. Les chromosomes de trois especes des Mégachiropteres (Mam- malia; Chiroptera) d’Afrique oriental.— Caryologia 26:389-396. Haiduk, M. W., R. J. Baker, L. W. Robbins, & D. A. Schlitter. 1981. Chromosomal evolution in African megachiroptera: G- and C-band assess- ment of the magnitude of change in similar stan- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON dard karyotypes.—Cytogenetics and Cell Ge- netics 29:221-—232. , L. W. Robbins, R. L. Robbins, & D. A. Schlit- ter. 1980. Karyotypic studies of seven species of African megachiropterans (Mammalia: Pteropodidae).—Annals of the Carnegie Mu- seum of Natural History 49:181-191. Harada, M., & T. Kobayashi. 1980. Studies on the small mammals of Sabah, east Malaysia II. Karyological analysis of some Sabahan mam- mals (Primates, Rodentia, Chiroptera).—Con- tributions from the Biological Laboratory, Kyo- to University 26:83-95. , M. Minezawa, S. Takada, S. Yenbutra, S. Nun- pakdee, & S. Ohtani. 1982. Karyological anal- ysis of 12 species of bats from Thailand. —Car- yologia 35:269-278. Heaney, L. R., & D. S. Rabor. 1982. Mammals of Dinagat and Siargao islands, Philippines. —Oc- casional Papers of the Museum of Zoology, Uni- versity of Michigan 699:1-—30. Howell, W. M., & D. A. Black. 1980. Controlled silver staining of neucleolus organizer regions with a protective colloidal developer: a 1-step method.— Experientia 36:1014—1015. Kasahara, S., & B. Dutrilaux. 1983. Chromosome banding patterns of four species of bats, with special reference to a case of X-autosome trans- location.— Annales de Génétique 26:197-201. Kock, D. 1969a. Eine neue Gattung und Art cynop- teriner Flughunde von Mindanao, Philippinen (Mammalia, Chiroptera).—Senckenbergiana Biologica 50:319-—327. 1969b. Eine bemerkenswerte neue Gattung und Art Flughunde von Luzon, Philippinen (Mammalia, Chiroptera).—Senckenbergiana Biologica 50:329-338. Koopman, K. F. 1984. Bats. Pp. 145-186 in S. An- derson and J. K. Jones, Jr., eds., Orders and families of Recent mammals of the world. John Wiley, New York, 686 pp. Lawrence, B. 1939. Collections from the Philippine Islands. Mammals. — Bulletin of the Museum of Comparative Zoology, Harvard University 86: 28-73. Miller, G. S., Jr. 1907. The families and genera of bats.— Bulletin of the United States National Museum 57:1-282. Patton, J. L. 1967. Chromosome studies of certain pocket mice, genus Perognathus (Rodentia: Het- eromyidae).— Journal of Mammalogy 48:27-37. Ray-Chaudhuri, S. P., S. Pathak, & T. Sharma. 1968. Chromosomes and affinities of Pteropidae (Megachiroptera) and Rhinopomatidae (Micro- chiroptera).—The Nucleus (Supplement):96— 101. Simpson, G. G. 1945. The principles of classification VOLUME 102, NUMBER 2 and a classification of mammals.—Bulletin of the American Museum of Natural History 85: 1-350. Smith, J.D. 1980. Chiropteran phylogenetics: intro- duction. Pp. 233-244, in D. E. Wilson and A. L. Gardner, eds., Proceedings fifth international bat research conference, Texas Tech Press, Lub- bock, 434 pp. Tate, G. H. H. 1942. Results of the Archbold expe- ditions. No. 46. A new genus and species of fruit bats, allied to Nyctimene.— American Museum Novitates 1204:1-2. 1951. Harpyionycteris, a genus of rare fruit bats.— American Museum Novitates 1522:1-9. Thomas, O. 1932. On some small mammals, chiefly bats, from the East Indian archipelago. — Annals and Magazine of Natural History, series 9, 11: 250-255. Thonglongya, K. 1972. A new genus and species of fruit bat from south India (Chiroptera; Ptero- podidae).—Journal, Bombay Natural History Society 69:151-158. Volleth, M. 1987. Differences in the location of nu- cleolus organizer regions in European vesper- tilionid bats.—Cytogenetics and Cell Genetics 44:180-197. Yong, H. S. 1984. Robertsonian translocation, peri- centric inversion and heterochromatin block in 531 the evolution of the tailless fruit bat.—Exper- ientia 40:875-876. , & §.S. Dhaliwal. 1976. Chromosomes of the fruit-bat subfamily Macroglossinae from pen- insular Malaysia. —Cytologia 41:85-89. abe Lam, Kook. Teh, & A; N. Start: 1973. Uniformity in the karyotype of the fruit bats Cynopterus (Mammalia: Chiroptera: Pter- opodidae).— Malaysian Journal of Science 2:19- 2. Yoshiyuki, M. 1979. Anewspecies of the genus Pren- ochirus (Chiroptera, Pteropodidae) from the Philippine Islands.—Bulletin of the National Science Museum (Tokyo), series A (Zoology) 5: 75-81. (EAR AND MJR) Utah Museum of Nat- ural History, University of Utah, Salt Lake City, Utah 84112; (LRH) Department of Vertebrate Zoology, Division of Mammals, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560; (Present address: Field Museum of Natural History, Roosevelt Road at Lake Shore Drive, Chicago, Illinois 60605). PROC. BIOL. SOC. WASH. 102(2), 1989, pp. 532-534 TAXONOMIC STATUS OF THE DELPHINID (MAMMALIA: CETACEA) TURSIO? PANOPE PHILIPPI, 1895 Robert L. Brownell, Jr. and James G. Mead Abstract.—Tursio? panope Philippi, 1895 is a junior synonym of Lageno- rhynchus obscurus (Gray, 1828) and not Cephalorhynchus eutropia (Gray, 1846) as noted by previous authors. Rodolpho Amando Philippi (1895) men- tioned a new species of dolphin as Tursio? panope based on a skull in the Museo Na- cional de Historia Natural, Santiago, Chile (MNHN-S). He described his specimen in more detail in 1896 (p. 14, pls. 4, 5, and 6). No locality was given for the holotype but Philippi (1896:14) implied that it was from Chile. The generic and specific identity of this delphinid have remained uncertain. True (1903:141) was unable to determine the generic affinity of 7.? panope with cer- tainty, but suggested that it probably rep- resented a new genus. He based this idea on Philippi’s drawing, which showed a bowed rostrum in lateral view (Fig. 1). Trouessart (1904:766) referred to the specimen as Lis- sodelphis? panope. Harmer (1922:631) be- lieved that 7.? panope might belong to the genus Cephalorhynchus. Miller (1928:171) was also uncertain about the generic affinity of the specimen but felt that it eventually would be placed in the genus Cephalorhyn- chus. He made this determination based on photographs of the type specimen taken by Waldo L. Schmitt in 1926. Unfortunately, these photographs were not published until now (Fig. 2). Cabrera (1961:615), Hersh- kovitz (1966:75), Donoso-Barros (1975:33) and Tamayo & Frassinetti (1980:364) listed T. panope as a junior synonym of Cepha- lorhynchus eutropia. Sielfeld (1980:277), in his list of marine mammal specimens in Chilean museums, included a _ skull MNHN-S 584, under C. eutropia. This specimen was later correctly identified as the holotype of Tursio? panope by Goodall et al. (1988:203). They noted that the known range of condylobasal length (CBL) in C. eutropia 1s 302 to 364 mm (mean 341.3 mm, n = 13), whereas the CBL of the type of 7. panope was slightly greater than 379 mm (the tip of the rostrum is damaged). They left 7. panope as incertae sedis. All previous authors have cited Philippi, 1896, as the type description of Tursio? pan- ope. We have used Philippi, 1895. Although Philippi (1895) provided only a synopsis of his 1896 account of Tursio? panope and sev- eral other new small cetaceans, the descrip- tion given is valid under the International Code of Zoological Nomenclature. We be- lieve that Philippi’s 1895 work was pub- lished before Philippi (1896) because a re- print of the 1895 paper in the Museo Nacional de Historia Natural, Montevideo has a separate cover that is also dated 1895. The year of publication, therefore, should be Philippi, 1895, not Philippi, 1896. Much confusion has exited regarding the specimens, numbers, and labels of the small cetaceans in the collection at the MNHN-S. In 1986 RLB examined the type specimen of Tursio? panope and confirmed its identity as the type. Cranial damage matches that shown in the photographs taken by Waldo L. Schmitt in 1926 (see Fig. 2) and the orig- inal drawings of the type specimen (see Fig. 1). The specimen bears the (old) number 937. The catalog entry for the specimen VOLUME 102, NUMBER 2 533 Pipe A: 5(2) and 6(2). states: ““Tursio? panope Ph. craneo San Vi- cente 1887 hallado en la playa.’ San Vicente is near Concepcion, Chile (36°44’S). This catalog number was probably assigned by Philippi. The new number 584 was assigned by the present Curator of Mammals, José Yanez, who started a new catalog and num- Original drawings of the holotype of Tursio? panope Philippi 1895, from Philippi 1896, Plates 4(2), bering system. The cards and catalog for the old system were retained (see discussion of this in Goodall et al. 1988:213). Very little has been published on the type of Tursio? panope. With no other descrip- tion available except for the drawings of the skull, all subsequent authors were puzzled Fig. 2. Dorsal, ventral and lateral views of the holotype of Tursio? panope Philippi, 1895. The condylobasal length is 380+ mm. Photography by Waldo L. Schmitt, 1926. 534 by the extraordinary downward curvature of the rostrum. The CBL (380+ mm as measured by Brownell; the rostrum is dam- aged) of 7.? panope exceeds that of the larg- est known physically mature specimens of Cephalorhynchus eutropia by more than 15 mm (see Goodall et al. 1988). The type of Tursio? panope is very similar in appear- ance and size to specimens of Lagenorhyn- cus obscurus (Gray, 1828). The CBL range for 16 specmens of L. obscurus is 333 to 421 mm with a mean of 373 mm (specimens in USNM). Although the age of the holotype is not apparent in Philippi’s drawings, examina- tion of the specimen revealed that it is im- mature. The basioccipital has not yet fused with the vomer, and the left zygomatic has not yet fused with the parietal and exoccip- ital. The upper tooth count of the holotype is 28 on the left and 29 or 30 on the right. This is a minimum count because of the damage to the tip of the rostrum. The man- dibular tooth count is 29 on each side. The CBL, skull shape and ventral topog- raphy of the type of Tursio? panope corre- spond closely to all specimens of Lageno- rhynchus obscurus examined by us. Based on CBL and immaturity alone, the skull is too large to be from a specimen of Cephalo- rhynchus eutropia. Therefore, Tursio? pan- ope Philippi, 1895 is reidentified here as a junior synonym of Lagenorhynchus obscu- rus (Gray, 1828). We thank José Yanez V., Museo Nacional de Historia Natural, Santiago, Chile, for al- lowing us access to various small cetacean specimens under his care, and Alvaro Mones, Museo Nacional de Historia Nat- ural, Montevideo, Uruguay, for his help with the Philippi literature. Ricardo Praderi, William F. Perrin and Clayton E. Ray pro- vided useful comments on this manuscript. Literature Cited Cabrera, A. 1961. Catalogo de los mamiferos de America del Sur.— Revista del Museo Argenti- PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON no de Ciencias Naturales ““Bernardino Riva- davia,”’ Buenos Aires, Ciencias Zoologicas 4(2): 309-732. Donoso-Barros, R. 1975. Contribucion al conoci- miento de los cetaceos vivientes y fosiles del territorio de Chile.—Gayana, Universidad de Concepcion, Zoologia 36:1—127. Goodall, R. N. P., K. S. Norris, A. R. Galeazzi, J. A. Oporto, & I.S. Cameron. 1988. On the Chil- ean dolphin, Cephalorhynchus eutropia (Gray, 1846).—Reports of the International Whaling Commission (Special Issue 9):197—257. Harmer, S. F. 1922. On Commerson’s dolphin and other species of Cephalorhynchus.—Proceed- ings of the Zoological Society of London 43: 627-638. Hershkovitz, P. 1966. Catalog of living whales.— United States National Museum, Bulletin 246: 1-259. Miller, G. S., Jr. 1928. The generic position of the porpoise described by Philippi as Tursio? pan- ope.— Proceedings of the Biological Society of Washington 41:171. Philippi, R. A. 1895. Los delfines Chilenos.—Anales de la Universidad de Chile, Santiago, 1895:281- 285. . 1896. Los craneos de los delfines Chilenos. — Anales del Museo Nacional de Chile, Santiago 1 (Zoologia) 12:1-18 + 6 pl. Sielfeld K., W. 1980. Mamiferos marinos en colec- ciones y museos de Chile. —Anales del Instituto de la Patagonia, Punta Arenas, Chile, 11:273- 280. Tamayo H., M., & D. Frassinetti C. 1980. Catalogo de los mamiferos fosiles y vivientes de Chile. — Boletin del Museo Nacional de Historia Natu- ral, Chile 37:323-405. Trouessart, E.-L. 1904. Catalogus mammalium tam viventium quam fossilium. R. Friedlande and Sohn, Quinquennale supplementum, 929 pp. True, F. W. 1903. On the species of the South Amer- ican Delphinidae described by Dr. R. A. Phi- lippi in 1893 and 1896.— Proceedings of the Bi- ological Society of Washington 16:133-143. (RLB) U.S. Fish and Wildlife Service, Post Office Box 70, San Simeon, California 93452; (JGM) Department of Vertebrate Zoology, National Museum of Natural His- tory, Smithsonian Institution, Washington, D.C. 20560. INTERNATIONAL COMMISSION ON ZOOLOGICAL NOMENCLATURE % British Museum (Natural History) Cromwell Road London SW7 5BD January 1989 The following applications were published on 16 December 1988 in Vol. 45, Part 4 of the Bulletin of Zoological Nomenclature. Comment or advice on these appli- cations is invited for publication in the Bulletin and should be sent to the Executive Secretary, ICZN, British Museum (Natural History), Cromwell Road, London SW7 SBD, U.K. Case No. 2663 Orbitolina dOrbigny, 1850 (Foraminiferida): proposed confirmation of Or- bulites concava Lamarck, 1816 as the type species. 2653 Hapalorhynchus beadlei Goodman, 1987 (Trematoda, Digenea): proposed replacement of the holotype by a lectotype. 2633 Phyllodoce (Carobia) rubiginosa Saint-Joseph, 1888 (currently also Nerei- phylla rubiginosa; Annelida, Polychaeta): proposed conservation of the specific name. 2636 Fizesereneia Takeda & Tamura, 1980 (Crustacea, Decapoda): proposed con- firmation of 7roglocarcinus heimi Fize & Seréne, 1956 as the type species. 2645 Bodotria Goodsir, 1843 (Crustacea, Cumacea): proposed conservation. 2644 Leucon Kr@yer, 1846 (Crustacea, Cumacea): proposed conservation. 2643 Iphinoe Bate, 1856 (Crustacea, Cumacea): proposed conservation. N.B. Would Editors of Molluscan journals note that this application involves the suppression of the gastropod name Iphinoe H. & A. Adams, 1854? Aleuropteryx Low, 1885 (Insecta, Neuroptera): proposed designation of Aleu- ropteryx loewii Klapalek, 1894 as the type species. Sialis Latreille, 1802 (Insecta, Megaloptera): proposed conservation by the confirmation of Phryganea phalaenoides Linnaeus, 1758 as the type species of Semblis Fabricius, 1775 (Insecta, Trichoptera). Ophonus Dejean, 1821 and Tachys Dejean, 1821 (Insecta, Coleoptera): pro- posed designation of type species. Papilio carthami Hubner, [1813] and Syrichthus serratulae major Staudinger, 1879 (currently both in Pyrgus; Insecta, Lepidoptera): proposed con- servation of the names carthami and major. Rapport sur les Myodaires du Docteur Robineau Desvoidy, (1826): proposed nomenclatural suppression. Physcus Howard, 1895 (Insecta, Hymenoptera): proposed conservation. J DD Smith Scientific Administrator INFORMATION FOR CONTRIBUTORS Content.—The Proceedings of the Biological! Society of Washington contains papers bearing on systematics in the biological sciences (botany, zoology, and paleontology), and notices of business transacted at meetings of the Society. Except at the direction of the Council, only manuscripts by Society members will be accepted. Papers are published in English (except for Latin diagnoses/descriptions of plant taxa), with a summary in an alternate language when appropriate. Submission of manuscripts. —Submit manuscripts to the Editor, Proceedings of the Biological Society of Washington, National Museum of Natural History NHB-108, Smithsonian Insti- tution, Washington, D.C. 20560. Review. —One of the Society’s aims is to give its members an opportunity for prompt pub- lication of their shorter contributions. Manuscripts are reviewed in order of receipt by a board of Associate Editors and appropriate referees. 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Literature citations in the text should be in abbreviated style (author, date, page), except in botanical synonymies, with unabbreviated citations of journals and books in the Literature Cited sections. Direct quotations in the text must be accompanied by author, date, and pagination. The establishment of new taxa must conform with the requirements of the appropriate international codes of nomenclature. When appropriate, accounts of new taxa must cite a type specimen deposited in an institutional collection. Examples of journal and book citations: Eigenmann, C.H. 1915. The Cheirodontidae, a subfamily of minute characid fishes of South America.— Memoirs of the Carnegie Museum 7(1):1-99. Ridgely, R. S. 1976. A guide to the birds of Panama. Princeton, New Jersey, Princeton University Press, 354 pp. Olson, S. L. 1973. The fossil record of birds. Pp. 79-238 in D. Farner, J. King, and K. Parkes, eds., Avian biology, volume 8. Academic Press, New York. Figures and tables with their legends and headings should be self-explanatory, not requiring reference to the text. Indicate figure and table placement in pencil in the margin of the manu- script. Plan illustrations in proportions that will efficiently use space on the type bed of the Proceedings. Original illustrations should not exceed 15 x 24 inches. Figures requiring solid black backgrounds should be indicated as such when the manuscript is submitted, but should not be masked. CONTENTS A revision of Arabella mutans (Chamberlin, 1919) and related species (Polychaeta: Arabellidae) G. Kent Colbath A new species of Benhamipolynoe (Polychaeta: Polynoidae: Lepidastheniinae) from Australia, associated with the unattached stylasterid coral Conopora adeta Marian H. Pettibone Two new species of Harmothoinae (Polychaeta: Polynoidae) from the East Pacific Rise, collected by Alvin dives 2000 and 2003 Marian H. Pettibone Varichaetadrilus angustipenis (Brinkhurst and Cook, 1966), new combination for Limnodrilus angustipenis (Oligochaeta: Tubificidae) Ralph O. Brinkhurst The adult male of the troglobitic ostracode Spelaeoecia bermudensis Angel and Iliffe, 1987, from an anchialine cave in Bermuda (Crustacea: Ostracoda: Halocypridoidea) Louis S. Kornicker New records of entocytherid ostracods infesting burrowing crayfishes, with the description of a new species, Ascetocythere stockeri Horton H. Hobbs, Jr. and Daniel J. Peters Pseudocyclops lepidotus, a new species of demersal copepod (Calanoida: Pseudocyclopidae) from the northwestern Pacific Douglas J. Barr and Susumu Ohtsuka A revision of the genus Microprotus Richardson with descriptions of two new species, M. acutispinatus and M. lobispinatus (Asellota, Isopoda, Crustacea) George D. F. Wilson, Oleg G. Kussakin, and Galina S. Vasina Four species of Synopiidae from the Caribbean region (Crustacea: Amphipoda) J. L. Barnard and James Darwin Thomas A new species, Ampelisca burkei, (Crustacea, Amphipoda) from Florida J. L. Barnard and James Darwin Thomas Aegla denticulata lacustris, new subspecies, from Lake Rupanco, Chile (Crustacea: Decapoda: Anomura: Aeglidae) Carlos G. Jara Freshwater crabs associated with caves in southern Mexico and Belize, with descriptions of three new species (Crustacea: Decapoda) Gilberto Rodriguez and Horton H. Hobbs, Jr. A new deep-sea crab of the genus Chaceon from Chile (Crustacea, Decapoda, Geryonidae) Luis A. Chirino-Galvez and Raymond B. Manning Upogebia corallifora, a new species of coral-boring shrimp from the West Indies (Decapoda: Upogebiidae) Austin B. Williams and P. J. B. Scott Additional records for an Atlantic reef lobster, Enoplometopus antillensis Liitken, 1865 (Crus- tacea, Decapoda, Enoplometopidae) Raymond B. Manning and David K. Camp Studies of neotropical caddisflies, XL: new species of Smicridea (Smicridea) from middle America and the West Indies (Trichoptera: Hydropsychidae) Oliver S. Flint, Jr. and D. G. Denning A review of the shore-fly genus Polytrichophora Cresson from Asia (Diptera: Ephydridae) Wayne N. Mathis and Jin Zuyin Adelphydraena, new genus, and two new species from Venezuela, and remarks on phylogenetic relationships within the subtribe Hydraenina (Coleoptera: Hydraenidae) Philip D. Perkins Symphurus callopterus (Cynoglossidae, Pleuronectiformes), a new deepwater tonguefish from the eastern Pacific Thomas A. Munroe and Madhu N. Mahadeva Systematics of the Steindachnerina hypostoma complex (Pisces, Ostariophysi, Curimatidae), with the description of three new species Richard P. Vari and Ann Williams Vari Description of two new species of the Eleutherodactylus milesi group (Amphibia: Anura: Lepucdeet eae) from northern Honduras James R. McCranie,.Jay M. Savage, and Larry David Wilson A new species of diminutive Eleutherodactylus (Leptodactylidae) from Oaxaca, Mexico Jonathan A. Campbell, William W. Lamar, and David M. Hillis Physalaemus crombiei (Amphibia: Leptodactylidae), a new frog species from Espirito Santo, Brazil with comments on the P. signifer group W. Ronald Heyer and Alan J. Wolf Redescription of the garter snake Thamnophis exsul Rossman, 1969 (Serpentes: Colubridae) Douglas A. Rossman, Ernest A. Liner, Carlos H. Trevifio, and Alan H. Chaney The type specimens of Hekstra’s owls M. Ralph Browning Chromosomes of ten species of Philippine fruit bats (Chiroptera: Pteropodidae) Eric A. Rickart, Lawrence R. Heaney, and Mark J. Rosenfeld Taxonomic status of the delphinid (Mammalia: Cetacea) Tursio? panope Philippi, 1895 Robert L. Brownell, Jr. and James G. Mead International Commission on Zoological Nomenclature: Applications hy, ls, ohh | ail if ia B's ¥ ‘ X vy +) 7 A ie bg he ef 27 ea Tem a ; ye i 4 J] a my ti " NS NS “fl WLAN. 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