Bulletin of the British Museum (Natural History) The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences Gordon J. Howes Zoology series Vol 54 No 1 25 February 1988 The Bulletin of the British Museum (Natural History], instituted in 1949, is issued in four scientific scries. Botany, Entomology. Geology (incorporating Mineralogy) and Zoology, and an Historical series. Papers in the Bulletin are primarily the results of research carried out on the unique and ever-growing collections of the Museum, both by the scientific staff of the Museum and by specialists from elsewhere who make use of the Museum's resources. Many of the papers are works of reference that will remain indispensable for years to come. Parts are published at irregular intervals as they become ready, each is complete in itself, available separately, and individually priced. Volumes contain about 300 pages and several volumes may appear within a calendar year. Subscriptions may be placed for one or more of the series on either an Annual or Per Volume basis. Prices vary according to the contents of the individual parts. Orders and enquiries should be sent to: Publications Sales, British Museum (Natural History), Cromwell Road, London SW7 5BD, England. World List abbreviation: Bull Br. Mm. not. Hist. (Zool.) © Trustees of the British Museum (Natural History), 1988 The Zoology Series is edited in the Museum's Department of Zoology Keeper of Zoology : Mr J. F. Peake Editor of Bulletin : Dr C. R. Curds Assistant Editor : Mr C. G. Ogden ISSN 0 565050370 ISBN 0007 1498 Zoology series Vol 54 No. 1 pp 1-62 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 25 February 1988 The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phy logenetic inferences 2 5 F E B 1988 Gordon J. Howes Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD Contents Introduction List of specimens used Abbreviations used in the text figures Cranial ligaments Ligaments of the upper jaw and pterygoid bones Ligaments of the lower jaw and opercular bones Cranial muscles The adductor mandibulae and muscles of the suspensorium in macrouroids IBRITISH MUSEUI 3 (NATURAL HISTORY) 6 25FE8S938 6 8 PRESENTED 10T 10 Macrourinae 12 Macrouroidinae 15 Comparisons with gadoids 16 Summary and discussion of the muscles associated with the jaws and suspensorium 32 Muscles of the hyoid region 42 Ventral gill-arch muscles 46 Dorsal gill-arch muscles 48 Eye muscles 48 Functional and ecological inferences 49 Jaw protrusion mechanisms 49 Hyoid-opercular mechanisms 53 Pharyngeal mechanisms 54 Trophic strategies 55 Taxonomic and phylogenetic inferences 57 IntrarelationshipsoftheMacrouroidei 57 Conclusions 59 Acknowledgements 60 References 60 Introduction If overall oceanic diversity could be expressed in numbers of individuals and species, rat-tails would surely emerge as the most diverse family of benthopelagic fishes. So wrote Marshall ( 1 979) of the Macrouridae, a group assigned to that ill-defined assemblage of higher euteleostean fishes known as the Paracanthopterygii. Marshall (1965) had earlier noted the sparsity of knowledge of the morphology and biology of macro urid fishes. Since then, the studies by Okamura ( 1 91Qa & b) have contributed substantially to filling this gap. However, since Okamura studied only Japanese macrourid fishes, the work is taxonomically limited because morphologically more diverse taxa occur outside Japanese waters. The data Okamura has published, nevertheless are substantial enough to provide a foundation for further anatomical studies, particularly those aimed at producing cladistic analyses, which so far, have not been applied to macrourid taxa. Bull. Br. Mm. not. Hist. (Zool.) 54(1): 1-62 Issued 25 February 1988 2 G. J. HOWES Since Gilbert & Hubbs (1916) published their subfamilial arrangement of macrourid fishes, there have been few major taxonomic changes. Apart from the recognition of additional sub- families (Parr, 1946) and the elevation of the Macrouroidinae to family level (Okamura, 19700 & b), the most noticeable rearrangement was that of Marshall (1966) who recognised the non- monophyletic nature of the family. Marshall (op. cit.) found that three taxa, previously recognised as macrourids, viz: Steindachneria, Lyconus and Macruronus, shared more characters in common with the gadoid family, the Merlucciidae. Although not all of Marshall's chosen characters are synapomorphic for merlucciids, there is every reason to agree that these three genera do not belong with the macrourids (see Cohen, 1984; Howes, 1988). Most recent authors recognise four macrourid subfamilies (see Cohen, 1984), viz: the Bathygadinae, Trachyrincinae, Macrouroidinae and Macrourinae, the latter containing the majority (ca 30) of genera. Howes (1988), based largely on the data presented here, has challenged this concept of the Macrouridae (see below). Most macrourid taxonomy has been based on ecological-evolutionary premises. For example, Okamura (19706) viewed his hypothesised phylogenetic polarity of primitive to derived taxa as reflecting both ecological groups and an evolutionary sequence. McLellan (1977: 1034) devised an evolutionary scenario, based on her study of macrourid morphology and ecology, that reflected the invasion of continental slopes and deep ocean basins by taxa derived from pelagic ancestors; again, a sequence supposedly reflected in extant ecological groupings and ontogenetic development. As pointed out by Marshall (1965; 1979) most macrourids are found in tropical seas but some areas contain more speciose taxa than others, e.g. the Sulu Sea, Gulf of Mexico and Caribbean. Most species are confined to continental slopes and few are common to more than one ocean. Marshall (1973; 1979) has hypothesised that the amphi-Atlantic distribution of 33% of the total Atlantic species and subspecies, might be attributable to continental drift. Merrett et. al. (1983) also note that species common to the Atlantic and Indian Oceans are inhabitants of continental slope, abyssal and pelagic regions, a distribution seeming to indicate a more general underlying factor than simply one of random dispersal. In attempting to explain macrourid ecology and distribution, none of these authors has asked a fundamental taxonomic question; how closely related are the taxa under consideration? As yet, there exists no rigorously structured hypothesis of macrourid relationships. Since previous studies of macrourid morphology have, to a large extent, been concerned with feeding mechanisms and because phylogenetic interpretations have been based on comparisons of those mechanisms, it is the objective of this study to re-assess the morphological basis of those ideas. The jaw musculature of some macrourid taxa has been described by McLellan (1977) and Casinos (1978), these descriptions were, however, made more from a functional rather than a taxonomic and phylogenetic viewpoint, and a taxonomically restricted range of taxa were used. A comparative analysis of macrouroids and other paracanthopterygians would, it was hoped, reveal morphological patterns that might indicate both related groups within the suborder and the relationships of macrouroids with other gadiforms. The limitations of using a single character complex for this purpose are well realised by the author, but past experience with basal euteleosts (Howes, 1984; 1985) has indicated that cranial muscles can provide rewarding information on which to base phylogenetic interpretations. Where availability of material allowed, at least three specimens of each taxon were dissected to check the variability of the character described. Okamura (19706) has described other character complexes (osteology, scales, brain mor- phology, structure of light organs) and these have been used to a certain extent to test the con- gruency of relationships arrived at through the myological study. However, these other characters must themselves be evaluated by out-group comparisons, and it is evident in Okamura's analysis that many characters used to define sub-groups are plesiomorphic for Gadiformes. It remains, therefore, for future studies to make polarity assignments to osteological and other characters in order to produce a more refined hypothesis of macrourid interrelationships. Howes (1988) in an account based principally on the findings presented here has reviewed the relationships of macrouroids and gadoids, and shown that the Macrouroidei (sensu Cohen, 1984) and the Macrouridae are non-monophyletic groups. Although, in that previous study, clades were MACROUROID FISHES 3 identified they were not given formal taxonomic status. In this account two of those clades are recognised as families, namely, the Bathygadidae and the Trachyrincidae. More complete diag- noses and taxonomic reviews of both are in preparation. Since the Macrouroidei was restricted to containing a single family the Macrouridae (Howes, 1988), the terms macrouroid and macrourid are interchangeable. However, in this text the term macrouroid is used when making coordinate comparisons with Gadoidei (i.e. gadoids). Classification used in this text Suborder: MACROUROIDEI Family: Macrouridae Subfamilies: Macrourinae & Macrouroidinae Suborder: GADOIDEI Family: Trachyrincidae, Bathygadidae, Moridae, Melanonidae, Steindachneriidae, Euclichthyidae, Merlucciidae, Gadidae, Ranicepitidae, Lotidae, Phycidae, Muraenolepididae& Bregmacerotidae List of specimens used All the specimens used in this study are in the collections of the British Museum (Natural History). Type of preparation is indicated as CS = cleared and stained; D = dissected; SK = dry skeleton. MACROUROIDEI: Abyssicola macrochir, 1938.6.23: 12-13 (D); Cetonurus globiceps, 1986.4.22: 4-5 (D); Chalinura mediterranea, 1986.4.22: 3 (D); Chalinura profundicula, 1986.4.22: 9; Chalinura cf. Simula, 1967.12.11: 2 (D); Coelorinchus caribbaeus, 1963.2.25: 244-250 (D; CS, 185mmTL); Coelorinchus coelorincus, 1905.2.2: 18 (SK); Coryphaenoides rupestris, 1897.12.9: 82 (SK); Coryphaenoides anguilliceps, 1981.7.14: 1-4 (D); Coryphaenoides mexicanus, 1971.10.22: 24-25 (D); Cynomacrurus piriei, 1930.1.12: 952; Echniomacrurus mollis, 1967.12.11: 3^4 (D); Hymenocephalus italicus, 1973.3.5: 7-10 (D); Kumbadentoni, 1961.1.30: 6 (Holotype; superficial examination); Lionurus carapinus, 1934.12.19: 33-34 (D); Macrosmia phalacra, 1980.12.31: 2 (Paratype, D); Macrouroides inflaticeps, 1939.5.24: 684 (D); Macrourus berglax, 1965.6.22: 8-9 (D); Malacocephaluslaevis, 1960.12.20: 2-3 (D); 1904.1 1.30: 33 (SK); Mataeocephalus microstomus, 1939.5.24: 723-24 (D); Nematonurus armatus, 1986.4.22: 1-2 (D); Nezumia aequalis, 1973.3.5: 60-64 (CS, 130mm, tail broken); Nezumia hildebrandi, 1963.2.25: 138-153 (D); Odontomacrurus murrayi, 1967.12.11: 5 (D); Sphagemacrurus hirundo, 1934.12.19: 30 (D); 1986.4.22: 6-7 (D); Squalogadusmodificatus, 1963.2.1: 10 (D); Trachonurusvillosus, 1963.2.25: 226-228 (D); Ventr if ossa accident alls, 1965.2.25:61-71 (D; CS, 190mmTL). GADOIDEI: Antimorarostrata, 1903.9.29: 7 (D); 1986.4.22: 10-11 (CS); Austrophycis marginata, 1936.8.26: 424-431 (D; CS); Bathygadus favosus, 1963.2.25: 28-30 (D); Bathygadus macrops, 1973.3.5: 3-6 (D); Bathygadus melanobranchus, 1969.6.26: 3227-3231 (D, CS); Bathygadus vaillanti, 1963.2.2: 31-35 (D); Bregmaceros atlanticus, 1984. 1 1 . 14: 4 (D); Bregmaceros madellandi, 1939.5.24: 792, 799 (D); Brosme brosme, 1892.6.8: 9 (SK); Ciliata mustela, 1983.8.3: 13-26 (D); Enchelyopus cimbrius, 1980.12.18: 3-12 (D); Eudichthys polynemus, 1986.5.14: 1-3; 4-9 (D); Gadomus longifilis, 1963.2.25: 7-17 (D; CS, 190mmTL; 1890.6.16: 43 (SK); Gadus morhua morhua, 1971.2.16: 634-635 (D); 1971.2.16: 628-633 (CS, 81 mmSL); Gadus morhua callaris, 1985.9.6: 7-14 (D); Gaidrospsarus mediterraneus , 1971.10.7: 65-77 (D); uncat. (CS, 122, 54mmSL); Halargyreus affinis, 1973.10.29: 384-440 (D; CS, 117mmTL); Lepidion eques, 1981.3.16: 422-427 (D); 11981.3.16: 437^40 (CS, HOmmTL); 1902.10.30: 6 (SK); Lota lota, 1953.6.26: 15-18 (D); 168.6 (SK, skulls only); Lotilla marginata, 1974.9.28: 6-7 (CS, 1 18 mm TL); Lyconus brachycolus, 1907.6.20: 15 (Holotype, partly dissected); Macrur onus mage llanicus, 1936.8.26: 352-357 (D); Macruronusnovozealandi, 25, 120 (SK); Merlangius merlangus, 1971.2.16: 329-331 (D); Melanonus gracilis, 1930.1.12: 933 (D); Me lanonus zugmayeri, 1981.3.16: 377 (D); 1986.4.22: 8 (CS, HOmmTL); Merluccius merluccius, 1963.5.14: 94-109 (D); 1971.7.21: 44-57 (CS, 130mmTL); Merluccius productus, 1896.9.25: 6 (SK); Molva molva, 1976.6.29: 2-5 (D); Mora moro, 25.370 (SK); Muraenolepis microps, 1937.7.12: 24-29 (D); 1937.7.12: 11-17 (CS, 95mmTL); 1937.7.12: 24-29 (skull); Physiculus argyropastus , 1901.1.30: 22 (SK); Phycis blennoides, 1973.10.29: 4411-448 (D); 1976.7.30: 119 (CS); 1898.4.30: 14 (SK); Pseudophydsbrevisculus, 1873.12.13: 30 (SK); Phycis phycis, 25.400 (SK); Raniceps raninus 1967.1.1: 4 (D); 1893.7.6: 2 (D) 1971.2.16: 640 (CS, 40mmSL); 1864.8.26: 3 (SK); Salilota australis, 1936.8.26: 394-404 (CS, 58mmTL); Steindachneria argentea, 1963.2.25: 335-339 (D); 1963.2.25: 344-354 (CS, 130mmTL); Trachyrincus trachyrincus , 1904.11.30: 34-35 (D); 1976.7.30: 42-53 (D, CS, HOmmTL); 1888.6.15: 7 (SK); Urophycis regia, 1985.6.6: 109-11 9 (D). 4 G. J. HOWES OUT-GROUP SPECIES: Atherina presbyter, 1983.4.21: 28-37; Aulopus filamentosus , 1953.11.1: 10-13; Brotula jayakari, 1891.2.9: 30 (SK); Cataetyx messieri, 1936.8.26: 1060-61 (D); Centropomus ensiferus, 1984.8.8: 85-95 (D); Cynoscion jamaicensis, 1961.9.1: 107-113 (D); Dicrolene introniger, 1939.5.24: 1441-1444 (D); Diplacanthopoma brachysoma, 1972.10.24: 4 (D); Electrona antarctica, 1948.5.14: 128-138; Eleotris obscurus, 1903.5.14: 93-99 (D); Esox lucius, 1971.1 1.19: 45^*6 (D); Genypterus blacodes, 1936.8.26: 1052-57 (D); 1898.6.17: 73 (SK); Glyptophidiummacropus, 1939.5.24: 1456-1465; Gobiesoxnudus, 1985.3.18: 110-114 (D); Gobius guineensis, 1984.7.29: 1021-22 (D); Harpadon nehereus, uncat. (D); Hoplostethes melanopus, 1939.5.24: 817-8 (D); Lampanyctus crocodilus, 1976.7.30: 26-33 (D); Lamprogrammus niger, 1939.5.24: l4S3-S7(D);Lophiodesmutilus, 1939.5.24: 1 869-75 (D);Lycodesfrigidus, 1969.6.26:3145^9(0); Monomitopus metriostoma, 1964.8.6: 43-46 (D); Ophidian rochei, 1971.12.17: 6-8 (D); Percichthys trucha, 1981.10.14: 28 (D); Percopsis omiscomayus , 1973.3.20: 468 (D); Photichthys argenteus, 1930.1.12: 299-306; Plagioscion squamosissimum, 1970.4.2: 5-8 (D); Pogonias chromis, 1886.1.21: 1 1-13 (D); Polymixia nobilis, 1862.4.22: 17-18 (D); Porichthys porosissimum, 1948.8.6: 1460-72 (D); Senanus cabrilla, 1960.6.10: 6-8 (D); Siniperca knerii, 1981.2.3: 1-4 (D); Stephanoberyxmonae, 1972.10.24: 2-3; Tilapia mariae, uncat. (D). Abbreviations used in the text figures NB. Scale bars in all figures are in divisions of 1 mm. Al, Ala, Alp, Aly, A2, A2d, A2v, A3, Aa> Divisions of the adductor mandibulae musculature Aa Anguloarticular aap adductor arcus palatini muscle ad adductores muscle AH Anterohyal bf buccalis facialis of trigeminal nerve bpm bucco-pharyngeal membrane of 1 st gill-arch Bsr Branchiostegal membrane Cb Ceratobranchial ce chondroid element Cmb Coronomeckelian bone Cmc Coronomeckelian cartilage ct connective tissue De Dentary Dh Dorsohyal do dilatator operculi muscle Eb Epibranchial Ent Entopterygoid epx epaxialis muscle ey eyeball fA2 fascia of muscle A2 Hb Hypobranchial ht heart hyab hyohyoideus abductores muscle hyad hyohyoideus adductores muscle Hyo Hyomandibula H yop Opercular process of hyomandibula ica infracarinalis anterior muscle i A 1 P internal aponeurosis of muscle A 1 P 10 Interoperculum im intermandibularis muscle lap levator arcus palatini muscle le levator externus muscle Let Lateral ethmoid Icdh ceratobranchial-dorsohyal ligament lee lateral ethmoid-entopterygoid ligament lei entopterygoid-infraorbital ligament lep lateral ethmoid-palatine ligament les lateral ethmoid-suspensorial ligament 11 levator internus muscle lip interopercular-preopercular ligament MACROUROID FISHES lla labial ligament Imh mandibulo-hyoid ligament Imi mandibulo-interopercular ligament 1mm maxillo-mandibular ligament Imn maxillary-nasal ligament Imp maxillary-premaxillary ligament Imq mandibulo-quadrate ligament lo levator operculi muscle Ipl palatine-lachrymal ligament Ism supramaxillary ligament Isc semicircular ligament connecting 3rd hypobranchials ludh urohyal-dorsohyal ligament 1VII maxillary-rostral cartilage ligament 1IX maxillary-premaxillary ligament IX palatine-maxillary ligament 1X1 ethmoid-maxillary ligament 1XII palatine-premaxillary ligament Men Meniscus Met Metapterygoid Mmc Mentomeckelian cavity Mvp Maxillary ventromedial process MX Maxilla Mxh Maxillary head nm neuromast Nil Optic nerve NV Trigeminal nerve trunk NVII Facial (hyomandibularis) nerve NVllh Hyoid branch of facial nerve NVIIm Mandibular branch of facial nerve obd obliqui dorsales muscle obp obliquus posterior muscle obs obliquus superior muscle obv obliqui ventrales muscle oi obliquus inferior muscle Op Operculum Pal Palatine Pb Pharyngobranchial pee pharyngoclavicularis externus muscle pci pharyngoclavicularis internus muscle Ph Posterohyal phy protractor hyoideus muscle Pmx Premaxilla Po Preoperculum Pro Prootic Ps Parasphenoid Pte Pterotic Ptt Posttemporal Q Quadrate Re Rostral cartilage rd retractor dorsalis muscle Ra Retroarticular Rbv Buccal branch of trigeminal nerve re rectus communis muscle rd retractor dorsalis muscle re rectus externus muscle rei rectus inferior muscle ri rectus internus muscle RmV Mandibular branch of trigeminal nerve RmxV Maxillary branch of trigeminal nerve 6 G. J. HOWES rs rectus superior muscle rv recti ventrales muscle Scl Supracleithrum sh sternohyoideus muscle shl lateral segment of sternohyoideus So Suboperculum Tp Toothplate tv transversus muscle tvd transversi dorsalis muscle tA 1 a, 1 1 , t2 insertion tendons of adductor mandibulae A 1 muscles tA2 insertion tendon of adductor mandibulae A2 muscle Vo Vomer Cranial ligaments Ligaments of the upper jaw and pterygoid bones In the following account the terminology and numbering system for ligaments follows that of Stiassny(1986). Stiassny (1986) recognised two synapomorphic arthrological characters uniting the acanthomorph lineages 'Paracanthopterygii' and Acanthopterygii, namely: the absence of a median palato-maxillary ligament (ligament IV) and the subdivision of the palato-vomerine ligament (ligament VI). I would confirm Stiassny's findings that a median palato-maxillary ligament (IV) is absent in all paracanthopterygian taxa examined. In macrouroids there is a single, undivided palato-vomerine ligament, which, from its points of attachment to the centre of the palatine and the head of the vomer, corresponds with Stiassny's ligament V (the posterior palato-vomerine ligament). The ligament runs parallel to the medial face of the palatine and varies in size from a long slender strap to a broad band. In the latter case the palatine is deep and is closely applied to the ethmo-vomerine bloc (e.g. Coryphaenoides, Hymenocephalus) . In Gadoidei the palato-vomerine ligament is also single. The presence of a single rather than a double ligamentous connection in gadoids and macrouroids may indicate that there has either been a derived loss of the anterior palato-vomerine ligament (ligament VI) or that it represents the plesiomorphic condition found in non-acanthomorph fishes. A broad investigation of the condition among paracanthopterygians is necessary to support one or other of these hypotheses. The maxillo-rostroid ligament (ligament VII) is well-developed in all macrouroids. As in other acanthomorphs it runs from the medial portion of the folded maxillary head to the dorsolateral face of the rostral-cartilage. In all macrouroids ligament VII appears to be continuous across the dorsal surface of the cartilage. In gadoids, a similar situation obtains in Bathygadus and the Moridae where the ligament lies in a groove in the cartilage. In many other gadoids, however, ligament VII is broader and inserts on the lateral face of the rostral cartilage (Figs 13 & 17). In some macrouroids, ligament VII runs parallel to the palato-maxillary ligament (XII), e.g. Coryphaenoides (Fig. 1) whereas in others it runs at ca. 45° to that ligament (Fig. 3). Ligament VII passes medial to the tips of the premaxillary ascending processes and is not attached to them. According to Stiassny (1986) in acanthomorphs ligament VII inserts on the premaxillary ascend- ing processes. I have not found this attachment in any gadiform and the condition she reports is probably a derived one for acanthopterygians. Gosline (1981) has commented on the functional significance of ligament VII (Gosline's ligament re) believing it to be the primary cause of upper jaw protrusion in at least some acanthomorphs (see p. 50). Casinos (1978) although identifying ligament VII in macrouroids incorrectly states that it is absent in the Gadidae. In fact the ligament is present in all gadoid taxa (see comments on p. 5 1 concerning function). An anterior maxillo- premaxillary ligament (ligament IX of Stassny, 1986; ligament 'am' of Gosline, 1981) is present in all macrouroids and other gadiforms examined. In macrouroids MACROUROID FISHES 7 however, the ligaments of either side meet ventroposteriorly to the rostral-cartilage forming an X-shaped ligament connecting the maxillary heads (their menisci) and the premaxillary ascending processes (Figs 28B & C). In gadoids ligament IX is variously developed and attached. In Bathygadus and Trachyrincus, there is a complex attachment of the ligament to the maxillary head via a cylindrical chondroid or fibrous element whose posterior tip joins a thin ligament stretching caudally, which becomes incorporated with the connective tissue stretching between the maxilla and premaxilla (Figs 29 A & B). In melanonids and merlucciids, ligament IX attaches directly to the medial process of the maxillary head, although it may be associated with a thick wedge of fibrous connective tissue (Fig. 29C). In advanced gadoids, there is sometimes no discrete ligament but only tough connective tissue (e.g. Euclichthys) although in the majority there is a short ligament and a thin meniscus between the medial maxillary process and the premaxillary ascending process (Fig. 29D); see further comments on p. 39. An anterior palato-maxillary ligament (ligament X) is present in all macrouroids and gadoids examined. It generally connects the base of the palatine prong with the inner central portion of the maxillary head. However, in the macrouroids Coryphaenoides and Hymenocephalus, the ligament attaches to the medial aspect of the maxillary head then passes forward to attach to the anterior process of the premaxilla. An ethmo-maxillary ligament (ligament XI) is well-developed in all macrouroids and passes beneath the palato-premaxillary ligament (XII). Its attachments are to the lateral prong of the mesethmoid and the anterolateral face of the maxilla. In two macrourid genera, Cetonurus (Fig. 4) and Echinomacrurus, a ligament extends trans- versly from the ethmoid to the palatine. In this respect, the situation corresponds with that in the percomorph Morone illustrated by Stiassny (1986, fig. 10). According to Stiassny the additional ligament is a branch of a bifurcated ligament XI. Such may also be the case in the two macrourid taxa. It is noted that in both these genera the dorsal palatine process is higher than in others and that a lateral ethmo-palatine ligament is absent. Thus the 'additional' ligament may serve to brace the palatine against too great a lateral movement. In all Macrourinae there is a short ligament running from the head of the maxilla to the inner face of the extended nasal bone (Fig. 2). The ligament branches from the base of ligament XI; it is absent in Bathygadus, Gadomus, Trachyrincus and all other gadiform fishes. A maxillary-nasal ligament is apparently present in some acanthopterygians (Cichlidae, P. H. Greenwood, pers. comm.). I have not found the ligament in other paracanthopterygians examined, nor in berycoids or polymixiids. A palato-premaxillary ligament (ligament XII of Stiassny, 1986) is present in all macrouroids and runs from the base of the palatine prong to the contralateral premaxillary ascending process. Often, the ligament attaches to the antero-dorsal surface of the rostral cartilage prior to its insertion on the premaxillary process. Gosline (1963, fig. 5 A) shows a similar situation in the percopsiform Aphredoderus where ligament XII as well as attaching to the rostral cartilage is united with its antimere in the midline. In Percopsis, however, the ligament of each side attaches to its respective premaxillary ascending process, there being no contralateral attachment. The percopsiform situation may represent the plesiomorphic condition of ligament XII. A lateral ethmoid-palatine ligament is present in all macrouroids examined. This ligament, commonly present in nearly all teleosts, connects the posterior face of the lateral ethmoid wing with the dorsomedial surface of the palatine. In macrouroids, there are often two ligaments, the medial occupying the usual position, while the lateral ligament connects the outer margin of the lateral ethmoid to the lateral surface of the palatine. In the macrourines Nezumia and Ventrifossa the medial ligament extends posteriorly to the entopterygoid. Cynomacrurus and Odontomacrurus are exceptional among macrouroids in lacking a lateral ethmoid-palatine ligament. In the gadoid families Melanonidae, Merlucciidae and Steindachneriidae there is a single, stout lateral ligament connecting the lateral ethmoid with the palatine, which in Gadomus (Bathygadidae) extends medially to attach to the entopterygoid. In the Euclichthyidae there is a unique form of ligamentous connection between the lateral ethmoid and suspensorial elements. The lateral ethmoid ligament fans out to attach along the 8 G. J. HOWES dorsolateral surface of the palatine; it continues forward as a broad band along the dorsolateral border of the entopterygoid, enters to adductor arcus palatini muscle, curves ventrolaterally, leaves the muscle and attaches to the antero-medial face of the hyomandibula (Fig. 15). In the Moridae there are both separate lateral and medial lateral ethmoid-palatine ligaments, and a lateral ethmoid-entopterygoid ligament. In the Gadidae, however, there are no definite ligamentous connections between the posterior face of the lateral ethmoid and the palatine. In most gadids, the palatine's only ligamentous connection with the neurocranium is with the vomer (ligament V; see above). The lateral ethmoid wing of gadids is often reduced and the palatine articulates not with the wing but with the anterior part of the lateral ethmoid where it contacts the ethmovomerine bloc. In the Muraenolepididae, for example, the palatine bears a high dorsal process which contacts the dorsomedial face of the (considerably reduced) lateral ethmoid. The palatine process is tightly bound by connective tissue to the lateral ethmoid but is not connected to it by a discrete ligament. Among more 'advanced' gadoids there is a noticeable shift in the articulation of the palatine toward a more anteromedial position. Among macrouroids and plesiomorphic gadoids (Bathygadidae; Melanonidae), the palatine articulates with the ventral surface of the lateral ethmoid wing to which it is also ligamentously attached. In other gadoid taxa, however, the palatine articulates with the anterior, ethmoidal part of the lateral ethmoid and there is a correlated loss of ligamentous connection between the bones. In acanthopterygians, the lateral ethmoid- palatine connection may be via one or more ligaments (see for example, Stiassny, 1981: 74; Greenwood, 1985: 158). The widespread occurrence of discrete ligamentous connections between the lateral ethmoid and palatine in teleosts indicates that their absence, often coupled with that of an intimate articulation between the two bones (Howes, 1987) represents a derived condition. Ligaments of the lower jaw and opercular bones There is a single, strong mandibular-interopercular ligament present in all macrouroids. The ligament is variable in length and width, from long and strap-like to short and triangular. The mandibular attachment of the ligament is the retroarticular, which is usually dorso-ventrally elongate. Okamura (19706) has drawn attention to the varying types of retroarticular among macrouroids. Casinos (1978) refers to a 'circumbuccal' ligament in macrouroids and gadids which he describes as a '. . . tendon that contours all the mouth'. Casinos postulates that this ligament plays an important role in protrusion of the upper jaw (see p. 52). The 'circumbuccal' ligament of Casinos is present in some form or other in all gadiform fishes examined. It does not surround the perimeter of the jaw as is implied by Casinos, but is attached anteriorly to each dentary. I thus refer to it as the 'labial ligament'. The ligament varies in degree of thickness and complexity of anterior attachment, among gadoids being least in the Gadidae and most in the Bathygadidae, Moridae, Melanonidae and Merlucciidae. In macrouroids the ligament is also well-developed, but less so than in the four gadoid families. In Bathygadus (Fig. 9) where it is most highly developed, the labial ligament is a thick rope-like element having a bifurcate attachment on the anterior aspect of the dentary. At the rictus of the jaws, the ligament curves around to attach to the premaxilla, at the point of curvature sending off a posterior branch which anchors to the maxillary rim. A separate element, with the same gross consistency as the main ligament, forms a stump on the posteromedial surface of the maxilla, rising above the border of the bone. Rosen & Patterson (1969: 425) refer to this non-osseous structure in Melanonus (Melanonidae) as resembling a supramaxilla. I therefore refer to it as the 'supramaxillary ligament'. Histological sections of the labial and supramaxillary ligament, stained specifically for elastin, reveal the 'ligaments' to consist of a collagenous core surrounded by an elastin coat. This tissue is ligament-like in the nature of its attachments (it is free from the dentary, although closely adhering to it by a sheet of connective tissue, which is highly innervated by subranches of the ramus mandibularis facialis (VII) nerve. The distribution of the labial ligament among euteleosts is yet to be ascertained but is possibly a MACROUROID FISHES lee lo ao Fig. 1 Imq Coryphaenoides mexicanus; cranial muscles and ligaments. Above, in lateral view. Below, medial view of the lower jaw adductor musculature and ligamentous connections. eurypterygian character (Stiassny, pers. comm.). However, its complex posterior ramification in the gadoids listed above appears to be a derived specialization, whose functional significance is commented upon elsewhere (p. 52). The ligament which in euteleosts connects the posterior tip of the interoperculum to the anterior border of the suboperculum is, in Bathygadus and Gadomus reduced and supplemented by another ligament stretching from the dorsal midpoint of the interoperculum to the preoperculum and hyomandibula. In most gadoids the interoperculum and suboperculum are connected by thin connective tissue, the dorsally directed ligament spanning the two bones and attaching to the preoperculum and hyomandibula. In the Merlucciidae, the dorsal ligament is a broad band attach- ing the interoperculum to the preoperculum. The Trachyrincidae have a unique condition whereby the interoperculum is connected by dorsally directed ligaments to the preoperculum and opercu- 10 G. J. HOWES lee lep Imn Fig. 2 Coelorinchus caribbaeus; cranial muscles and ligaments. In lateral (above) and dorsal (below) views. lum (see Howes, 1988, figs 2 & 3). The ligamentous connection between the interoperculum and hyomandibula/preoperculum is considered to be a derived condition for gadoid fishes; its taxo- nomic and phylogenetic implications are discussed more fully in Howes (1988). The functional aspects of this linkage are discussed below, p. 54. Cranial muscles The adductor mandibulae and muscles of the suspensorium in macrouroids The muscles of the jaws and suspensorium in macrourids have been described for some taxa by Dietz, 1921, McLellan , 1977 and Casinos, 1978; 1981. Dietz gave a brief description of the muscles in Coleorinchus coelorinchus; McLellan referred to, and illustrated the adductor muscles of Bathygadus and Coelorinchus, and Casinos those of Coryphaenoides and Trachyrincus. The two MACROUROID FISHES 11 Fig. 3 Ventrifossa occidentalism cranial muscles and ligaments in lateral view. lo ao Hyop So Imm lo Fig. 4 Cetonurus globiceps; cranial muscles and ligaments in lateral view. 12 G.J.HOWES latter authors were concerned with describing the musculature in a functional context, although Casinos (1978) made some observations regarding the homology and evolution of certain adductor muscles. The taxonomic range of these authors' works is limited and the applicability of their functional conclusions to macrouroids in general requires a reappraisal in the light of morphological variations of which they were unaware. NB. In the following descriptions the dorsal muscle of the adductor element (levator maxillaris superioris of authors) is referred to as A 1 P; its homology is discussed later, p. 34. MACROURINAE Type 1 morphology: two subgroups are recognised, (a) Coryphaenoides , Abyssicola, Nezumia, Coelorinchus, Lionurus (synonymised with Coryphaenoides by Iwamoto & Stein, 1973); Nematonurus, Chalinura; (b) Macrourus, Trachonurus. The overall morphology of the adductor musculature is similar in the two subgroups, the only difference being the presence of an additional adductor element, Aly, in subgroup (a). In all the taxa included in the Type I group the mouth is inferior or subinferior and the jaws relatively short; the premaxillary ascending process is at least 80% the length of the dentigerous ramus; the maxilla is a deep, stout bone with a markedly convex dorsal border. The outer adductor muscle is thin but relatively deep and divisible into upper and lower parts which are either entirely separated (e.g. Coryphaenoides, Fig. 1), or partially so (e.g. Coelorinchus, Fig. 2). The lower part (Ala) originates from the preopercular limb, and in Coryphaenoides from a prominent lateral flange of that bone (Fig. 1). The muscle inserts tendinously along the lower part of the maxillo-mandibular ligament. The upper part of the adductor (A1P) originates from the preopercular limb and inserts via a stout tendon on to a ventromedial process of the maxilla; it is not joined to the maxillo-mandibular ligament. Running dorsomedially to Al P is a long spindle-shaped muscle here designated Aly (Fig. 3); see below. The fibrous part of the muscle originates from a long tendon which in turn stems from the fascia of Al p. Insertion is via a cord-like tendon on the same medial process of the maxilla as Al p. In Lionurus, there is a marked difference in the relative proportion of the fibrous part to the posterior tendinous part of the muscle between small and large-sized specimens. In a specimen of 150 mm TL, the muscle is 50% tendinous and 50% musculose, whereas in a specimen of 225 mm TL, 75% of the muscle is fibrous. In Abyssicola macrochir, muscle Aly is a larger and deeper element than in any other taxon examined. Also, unlike other taxa of this group the muscle originates from a broad tendinous sheet stemming from the rim of the hyomandibula. Muscle A2 is a deep, broad element whose medial fibres originate from the frontal, and those more lateral in position from the prootic and hyomandibula. A2 has a complex insertion in the lower jaw. Its posteromedial fibres insert into an aponeurosis which bifurcates into a vertical and a horizontal tendon. The vertical tendon inserts onto the coronomeckelian bone and continues to the dorsomedial surface of the narrow retroarticular, while the horizontal tendon runs forward into the mandibular cavity. The majority of fibres of A2 insert on the horizontal tendon, from which also originate those of the mandibularis section of the adductor Aco (Fig. 1). Muscle AGO lies mostly outside the mentomeckelian cavity, but with a small bundle of lateral fibres running forward into it. The levator arcus palatini (Figs 1 & 2) is a long, pyramidical muscle running between the sphenotic and the lateral face of the hyomandibula; its outermost fibres insert on the edge of the preopercular limb. The dilatator operculi (Figs 1 & 2) originates from the lateral hyomandibular fossa and inserts on the rim of the opercular facet. The adductor and levator opercularis muscles extend from the lateral border of the pterotic, the adductor inserting on the opercular process of the hyomandibula and the levator on the anteromedial face of the operculum (Figs 1 & 2). The adductor arcus palatini occupies the floor of the orbit, its anterior fibres inserting on the broad concave surface of the palatine (Figs 1 & 2). Posteriorly, the muscle runs between the parasphenoid and the lateral faces of the entopterygoid and metapterygoid and the medial face of the hyomandibula. MACROUROID FISHES 13 Type II morphology. Macrourinae (part): Ventrifossa, Cetonurus, Echinomacrurus , Malaco- cephalus, Hymenocephalus, Odontomacrurus, Sphagemacrurus , Cynomacrurus , Mataeocephalus. Taxa of this group have a terminal or subterminal mouth, with the exception of Echinomacrurus in which it is inferior. The ratio of premaxillary ascending process to dentigerous ramus length varies from 30-33% in Odontomacrurus and Chalinura to 50% in Ventrifossa. An opposite extreme is Mataeocephalus where the premaxillary ramus is 50% of the length of the ascending process (cf. Macrouroidinae, p. 1 5); in Echinomacrurus and Cetonurus, the ramus and ascending process are of almost equal length. The characteristic myological feature of this morphotype is that Al is a single, or incompletely divided, deep element. Ventrifossa occidentalis is taken to illustrate the morphotype, representative of the majority of taxa (Fig. 3). Echinomacrurus and Cetonurus which differ somewhat in detail from Ventrifossa are considered below. Ptt Fig. 5 Cynomacrurus piriei; levator arcus palatini and opercular muscles in lateral view. Muscle A 1 originates posterodorsally from the upper part of the preopercular limb and ventrally from the preoperculum and quadrate (Fig. 3). The dorsal border of the muscle is almost horizontal, there being a slight concavity and tendinous area below the orbit. Dorsal fibres of the muscle insert on the inner aspect of the maxilla, while the remainder of the muscle, separated from the upper part by an internal aponeurosis, inserts into the anterior third of the maxillo-mandibular ligament. Along the centre of the muscle is an aponeurosis which is marked laterally by a change in muscle fibre direction — from almost horizontal (dorsally) to oblique (ventrally). The position of the aponeurosis is marked in taxa belonging to morphotype I by a complete or partial division of the muscle. In this respect Cetonurus resembles the latter taxa (Fig. 4). Muscle A2 is a deep element originating from a cavity formed between the prootic and frontal, with fibres stemming from both bones. In Cynomacrurus and Odontomacrurus the anterior muscle fibres are vertically aligned or posteroventrally angled, in contrast to the more usual anteroventral angle present in Ventrifossa (Fig. 3). The insertion of muscle A2 in the lower jaw is via a cord-like tendon carrying outer fibres to the coronomeckelian bone and into a broad aponeurosis from which originates muscle AGO. The muscle is short, barely extending halfway along the mandible; only its dorsal fibres enter the mentomeckelian cavity. 14 G. J. HOWES lap do A2 Fig. 6 Macrouroidinae; above, Squalogadus modificatus, preoperculum and associated muscles; below, Macrour aides inflaticeps, anterior of adductor musculature. The levator arcus palatini is a large muscle in all Type II genera, extending from the sphenotic and pterotic to the lateral face of the hyomandibula, its anteroventral portion covering the postero- dorsal margin of Al . In Cynomacrurus the levator is angled forward to a greater degree than in the other included taxa (Fig. 5). The dilatator, adductor and levator operculares muscles are all well-developed. The dilatator operculi originates from a lateral hyomandibular fossa and the adductor from the ventral surface of the pterotic. Some fibres of the adductor operculi insert with those of the dilatator on the rim of the opercular condyle, but the majority insert on the opercular process of the hyomandibula. In Cetonurus the separate insertions of the muscle are further marked by the complete division of its body. The levator operculi is a long, deep muscle originating from the ventral surface of the pterotic and inserting along the anteromedial border of the operculum. In Cynomacrurus the adductor operculi inserts entirely on the opercular process of the hyomandibula and the levator operculi is divided. The anterior segment of the levator shares a common origin with the adductor operculi, but the posterior segment originates from the posttemporal (Fig. 5); both segments insert together on the anteromedial face of the operculum. With respect to its posttemporal origin, the levator of Cynomacrurus is similar to that of the gadoid Lota (see p. 32 and Howes, 1988). MACROUROID FISHES 15 The adductor arcus palatini extends the length of the parasphenoid and anteriorly inserts on the palatine; posteriorly it inserts on the ento- and metapterygoids and the medial face of the hyomandibula. In Cetonurus the muscle extends only halfway along the length of the parasphenoid (Fig. 4). MACROUROIDINAE Two monotypic genera are included in this subfamily, Macrouroides and Squalogadus. Of the former, only a single, poorly preserved specimen of Macrouroides inflaticeps was available for examination. The specimen has a damaged and partially disarticulated skull and it has been impossible to ascertain precisely the configuration and insertions of the adductor muscles. Likewise, only a single specimen of Squalogadus modificatus is available for examination and only a partial dissection of the posterior region of the cheek musculature has been possible (Fig. 6). Muscle Al is a single element originating from the preopercular limb and inserting on to the upper part of the maxilla via the maxillo-mandibular ligament. Muscle A2 is a thick, crescentic muscle stemming from the frontal and prootic; its insertions in the lower jaw and the extent of muscle Aco have not been ascertained in either taxon. Table 1 Grouping of Macrourinae based on jaw and ventral gill-arch muscle morphotypes (see text, p. 58), compared with Okamura's (19706) groupings Jaw muscles Gill-arch muscles Okamura's groups Type \a Abyssicola Coryphaenoides Nezumia (a) Abyssicola Coryphaenoides Coelorinchus Abyssicola Coelorinchus Macrourus Lionurus Lionurus Nematonurus Nematonurus Chalinura Chalinura Macrourus Type \b Macrourus Trachonurus Trachonurus Malacocephalus Mataeocephalus Cetonurus Echinomacrurus Type II Ventrifossa Malacocephalus Hymenocephalus Odon tomacrurus (b) Ventrifossa Hymenocephalus Nezumia Odontomacrurus* Ventrifossa Malacocephalus Odontomacrurus Cynomacrurus Mataeocephalus Macrosmia Cynomacrurus* Cynomacrurus Cetonurus Cetonurus Echinomacrurus Echinomacrurus Sphagemacrurus Sphagemacrurus NB. * these two genera lack a palatine-lateral ethmoid ligament. According to Iwamato & Stein (1973), Lionurus, Nematonurus and Chalinura should be treated as subgenera of Coryphaenoides. The following macrourine genera have not been examined, Astenomacrurus , Cetonurichthys , Haplomac- rourus, Lepidorynchus, Paracetonurus, Parakumba, Pseudocetonurus, Pseudonezumia. 16 lo So Imm Fig. 7 Trachyrincidae: Trachyrincus trachyrincus; cranial muscles in lateral view. The levator arcus palatini and operculi muscles are missing from the specimen of Macrouroides, but in the Squalogadus specimen there is a small levator arcus palatini, lying posterolaterally to the adductor mandibulae complex (Fig. 6). The adductor arcus palatini is a thick element flooring the orbital cavity, inserting anteriorly on the palatine and posteriorly on the lateral surface of the ento- and metapterygoids. Comparisons with gadoids The presence of a dorsal section of the adductor mandibulae originating from the palatoquadrate was considered by Rosen & Patterson (1969: 361 et seq.) to be a specialisation of paracanthoptery- gian fishes. Fraser (1972) commented that a muscle of this type had developed in several acanthop- terygian groups and could not be used as a character indicating phyletic relationships. He also pointed out that the number of taxa examined for this character by Rosen and Patterson was too few to make generalisations as to its occurrence and homology. Marshall & Cohen (1973) in referring to the so-called levator maxillaris superior is muscle note that '. . . character has received little comment; its distribution and taxonomic significance are at present in need of fuller survey'. There has been much confusion concerning the identity of the dorsal adductor muscle in para- canthopterygians. Rosen (1962) and Rosen & Patterson (1969: 341 et seq.} referred to the element as a levator maxillaris superioris (i.e. the homologue of that muscle in the halecomorph Amia; see Allis, 1897). Previous authors, viz. Holmquist (191 1) and Dietz (1921) had referred respectively to the muscle as A4 and Alp. Later, Rosen (1973: 417) reformulated his ideas and, following Dietz, referred to the muscle as A 10, a view supported by Winterbottom (19740) and most subsequent authors. Casinos ( 1 978: 443) continued to use the term levator maxillaris superioris '. . . because of functional reasons'. Because the muscle in question lies lateral to the mandibular branch of the trigeminal (V) nerve, I concur with Winterbottom (19740) in recognising it as part of muscle Al. Allis (1897: 581-2) comments that the '. . . course and position of the inferior maxillary nerve . . . seems to lie always between Al and A2 . . .'; see similar remarks of Freihofer (1978: 17) and Howes (1985: 275). MACROUROID FISHES 17 In all gadiform fishes I have examined, apart from some macrouroids noted above and the Trachyrincidae (see below), a dorsal division of muscle Al is present. The various conditions of this, and other cranial muscles are as follows: TRACHYRINCIDAE (Figs 7 & 8) The family (formerly recognised as a macrouroid subfamily) contains two genera Trachyrincus and Idiolophorynchus. Species are characterised by their unique adductor muscle arrangement (described below), interopercular-preopercular-opercular ligamentous arrangement, nasal mor- phology, caudal skeleton (see Howes, 1988) and other features such as dorsal scutes (given in diagnosis for subfamily by Marshall, 1973). In trachyrincids the jaws are long, the length of the premaxillary ascending process being 50% of the ramus. Muscle Al is a single, narrowly triangular element which extends from the anterolateral face of the preoperculum to insert via a double tendon on the maxilla. The upper tendon (t2, Fig. 7) passes medially to insert close to the maxillary head while the lower (tl, Fig. 7) joins the maxillo- mandibular ligament to insert on the lateral face of a maxillary dorsal process. Casinos (1978: 443) is incorrect in stating that a maxillo-mandibular ligament is absent in Trachyrincus. A ventral tendon runs from the aponeurosis to the coronomeckelian bone; muscle AGO extends from the anterior part of the aponeurosis, the majority of fibres lying medial (outside) the mentomeckelian cavity. The levator arcus palatini in contrast to that of macrouroid taxa, is extended posteriorly and its anteroventral part is covered by the adductor mandibulae. The muscle originates dorsally from the sphenotic and pterotic, and medially from the hyomandibula; insertion is across the extensive dorsal face of the preoperculum. The dilatator operculi originates from a common aponeurosis with the levator arcus palatini and has a strong tendinous insertion on the rim of the opercular condyle. The adductor operculi is a long muscle originating from the ventral surface of the pterotic and inserting for much of its length on the opercular process of the hyomandibula. Only the posterior fibres insert on the operculum, just medial to the insertion of the dilatator muscle. The levator operculi is a thin, narrow element running postero-laterally and inserting on the medial face of the small operculum. The adductor arcus palatini, although extending the length of the parasphenoid is weakly developed anteriorly (of single fibre thickness) and does not insert on the palatine. A2v Po Q Ra Aa Cmb Cmc Fig. 8 Trachyrincus trachyrincus; medial view of inner adductor muscle and lower jaw. 18 G. J. HOWES do Rt 'al Re lo De Imm Fig. 9 Bathygadidae: Bathygadus melanobranchus; cranial muscles and ligaments in lateral view. BATHYGADIDAE (Figs 9 & 10) Formerly recognised as a subfamily of macrouroids, Howes (1988) referred the 'bathygadine' genera Bathygadus and Gadomus to the Gadoidei as a clade, here recognised as a family. A complete taxonomic diagnosis is in preparation but it can be stated here that the family is dis- tinguished from other gadoid families by its lack of a caudal skeleton, derived RLA pectoral nerve pattern, reduced gill-filaments, reticulate scale pattern and myological synapomorphies detailed here. Bathygadus and Gadomus have a terminal mouth with a wide gape, the jaws are long and slender. The outer adductor muscle is a thin, shallow sheet of fibres originating from the preoperculum and posterior margin of the hyomandibula. In most Bathygadus species it is clearly divided into ventral (A 1 a) and dorsal (A 1 P) parts. However, in B.favosus, the two muscles can only be distinguished by their separate tendinous insertions on the maxilla. In the species where the Ala and Alp parts remain separated, Ala joins a broad aponeurosis with the maxillo-mandibular ligament halfway MACROUROID FISHES 19 along the length of the maxilla. Muscle Al(3 originates from the medial fascia of the levator arcus palatini muscle and is divided into anterior and posterior segments, the division being brought about by the muscle's tendinous constriction below the orbit. The anterior segment of A 1(3 inserts on the medial face of the maxillary process. In Gadomus muscle Ala has a definite insertion on the outer aspect of the anterior part of the maxilla, and the maxillo-mandibular ligament is longer and narrower than in Bathygadus. Muscle A2 is a large element originating from the hyomandibula, prootic and frontal and inserting on the lower jaw. Insertion is partly via a vertical tendon stretching down the medial face of the anguloarticular, and partly on a tendon inserting on the coronomeckelian bone and medial face of the anguloarticular. From these tendinous insertions stem the fibres of the mandibularis part of the adductor muscle (Aco). The anterior half of Aco enters a long mentomeckelian cavity. The levator arcus palatini is a large, deep element which inserts halfway down the preopercular limb and entirely covers the origin of muscle Al . The lateral posterodorsal fibres of the levator are inseparable from those of the dilatator operculi. The adductor arcus palatini extends nearly the entire length of the parasphenoid, but anteriorly it is feebly developed, with widely spaced, tendinous bands of fibres; posteriorly the muscle inserts on the lateral face of the metapterygoid and the medial face of the hyomandibula. As noted above, the anterior fibres of the dilatator operculi intermesh with the dorsoposterior fibres of the levator arcus palatini; those respective groups of fibres of both muscles originate from the hyomandibula, inserting together with the adductor operculi on the opercular condyle. The levator operculi is a well-developed element stemming from the pterotic and inserting along the posteromedial border of the operculum. ao lo A,P NVII Imm Fig. 10 Bathygadidae: Gadomus longifilis; cranial muscles and ligaments in lateral view. 20 G. J. HOWES MORIDAE (Fig. 11) In their overall morphology, the cranial muscles of morids are most similar to those of the Bathygadidae and Gadomus (Melanonidae). In Halargyreus (Fig. 1 1), Pseudophycis and Antimora, muscles A 1 a and A 1 P originate laterally to A2; A 1 P is tendinously constricted below the orbit, its anterior expansion joining the insertion tendon of A 1 a. The levator arcus palatini is large, its ventral tip extending to a point halfway down the pre- opercular limb (cf. Bathygadus). The adductor arcus palatini is divided into posterior and anterior parts, the latter inserting on the entopterygoid and not the palatine as in most other gadoids. In Lepidion (Fig. 1 0), muscles A 1 a and A 1 P are incompletely separated; both segments originate from a single body. The dorsal (A 1 P) and ventral (A 1 a) bundles insert on separate tendons beneath the orbit, which then join into a single muscle body lateral to the palatine before separating into their respective medial and lateral maxillary insertions. The levator arcus palatini covers the upper part of A2, dorsally it joins the dilatator operculi along an aponeurosis. The adductor arcus palatini is feebly developed in its central portion; the anterior fibres insert on the palatine. aap Fig. 1 1 Moridae: above, Halargyreus affinis; below, Lepidion eques; upper jaw and suspensorial muscles in lateral view. MACROUROID FISHES MELANONIDAE (Fig. 12) 21 In Melanonus muscles Ala and Alp are inseparable at their origins which is from the fascia of muscle A2. The individual elements only become apparent above the jaw articulation. A 1(3 is constricted into a tendon halfway along its length at the point where it is crossed transversely by a ligament running from the posterolateral edge of the palatine and the entopterygoid to the medial face of the second infraorbital. The anterior expansion of Alp inserts on the inner part of the maxillary head. The outer element, Ala, inserts via a separate tendon on to the outer face of the maxilla. do lip NVIlm Imm Fig. 12 Melanonidae: Melanonus zugmayeri; cranial muscles in lateral view (suboperculum removed). Muscle A2 is strongly developed, its anterior fibres being almost vertical. The muscle is partially divided by a hypertrophied ramus mandibularis interims facialis of the hyomandibularis VII nerve trunk (Fig. 12). The levator arcus palatini shares an aponeurotic origin with the dilatator operculi. The adductor arcuspalatiniis well-developed, flooring the orbital cavity, and inserting anteriorly on the palatine. The adductor and levator operculares muscles share a common origin from the ventral surface of the pterotic shelf. The adductor inserts both on the dorsomedial rim of the opercular condyle and the opercular process of the hyomandibula; the levator inserts along the dorsomedial border of the operculum: STEINDACHNERIIDAE (Fig. 13) In Steindachneria muscle Al is large, originating from the lower half of the preopercular limb. Its fibres are angled anterodorsally, and dorsally the muscle is divided. The posterodorsal group of fibres insert on an aponeurosis from which stems a sausage-shaped segment of fibres running 22 G. J. HOWES forward to meet, laterally, the maxillo-mandibular ligament. From this point, the muscle becomes separated from the ligament and almost immediately inserts on the medial aspect of the maxillary head. This part of the muscle is identified as A 1(3. The ventrolateral group of fibres inserts directly on the maxillo-mandibular ligament and is identified as Ala. Muscle A2 originates from the prootic, the sphenotic process and the upper part of the hyomandibula, its anterior fibres running almost vertically. Insertion in the lower jaw is via a strong vertical tendon to the coronomeckelian bone and a broad aponeurosis from which originates Aco. No fibres of A2 insert on the anguloarticular. Muscle Aco is lanceolate, the majority of its fibres filling the mentomeckelian cavity. The levator arcus palatini is moderately developed, originating from the sphenotic process and pterotic, and inserting in a lateral cavity of the hyomandibula. The muscle lies lateral to A2, but its lo ao do Fig. 13 Steindachneriidae: Steindachneria argentea: cranial muscles in lateral (above) and dorsolateral (below) views. NB. Not all the upper jaw ligaments are shown in the lower drawing. MACROUROID FISHES lap 23 lap Fig. 14 A,. Euclichthyidae: Euclichthys polynemus; above, cranial muscles in lateral view; below, posterior associations of muscle Atp; Ata reflected. ventral tip does not reach as far as the origin of muscle Al. The adductor arcus palatini is well- developed posteriorly and anteriorly, where it inserts on the palatine but its central portion is reduced to a few widely spaced fibres which are well-separated from the dorsal margin of the pterygoid series. Rosen & Patterson (1 969, fig. 44a) depict the adductor musculature of Steindachneria. However, my observations are not completely in accord with theirs, since they show muscles Ala and Al|3 separated for their entire lengths, and a fully developed adductor arcus palatini. The dilatator, adductor and levator operculares muscles are as described for Melanonus. EUCLICHTHYDIDAE (Figs 14 & 15) The adductor mandibulae muscle is a thick, deep element originating from the upright limb of the preoperculum; it comprises superficial, Ala, and medial, Al|3, elements which have complex associations posteriorly. Muscle Al p is, posteriorly, a shallow, band-like muscle, having its origins aponeurotically from, dorsally, the levator arcus palatini, and ventrally, the dorsomedial surface of Ala, thus partially dividing the latter. Anteriorly, muscle Alp becomes bulbous and transversely expanded, joining with Ala before separating from it to insert on the ventromedial surface of the maxillary head. 24 G. J. HOWES Muscle Ala is tendinous anteriorly and joins the maxillo-mandibular ligament together with A 1 0; its insertion is on the dorsolateral surface of the maxilla. Muscle A2 is well-developed, originating from the sphenotic and the dorsolateral surface of the hyomandibula. In the lower jaw, A2 joins a band-like aponeurosis, from which originates Aco; a strong vertical tendon runs from the aponeurosis to the coronomeckelian bone. Muscle Aco is long and shallow, lying within the mentomeckelian cavity for most of its length. The levator arcus palatini originates from the sphenotic and pterotic; it bifurcates ventrally, the anterior branch inserting on the hyomandibula and having an aponeurotic connection with muscle Alp (see above and Fig. 14); the posterior branch inserts on the preoperculum and overlaps the posterodorsal edge of Ala. The adductor arcus palatini is confined to the posterior part of the parasphenoid; it inserts on the lateral faces of the ento- and metapterygoids. A unique feature of this muscle is that it is divided by a strong ligament running from the lateral ethmoid and palatine to the medial face of the hyomandibula (see p. 7 and Fig. 1 5). The dilatator operculi is a spindle-shaped muscle extending from the pterotic to the opercular process. The adductor operculi runs almost laterally from the underside of a pterotic shelf to insert entirely on the opercular process of the hyomandibula; the levator operculi is an extensive muscle whose insertion extends along the entire dorsal border of the operculum. NSDh Met Fig. 15 Euclichthyidae: Euclichthys polynemus; adductor arcus palatini muscle and associated elements. MERLUCCIIDAE (Figs 16-18) The following descriptions are based on three genera, Merluccius, Macruronus and Lyconus; Lyconodes has not been examined. In Merluccius (Fig. 16) muscle Ala is a thin, shallow element, stretching from a tendinous origin on the preoperculum across the face of muscle A2 to insert via a cord-like tendon halfway along the maxilla where it joins the maxillo-mandibular ligament. Muscle Alp is a deep element having its origin from the meta- and entopterygoid and the palatine. It passes medial to the ramus mandibu- laris of the trigeminal nerve. The part of the muscle originating from the palatine is thick and bolster-like (Fig. 16). Insertion of Al p is across a wide area of the medial face of the maxilla. MACROUROID FISHES lap aaP 25 lo Fig. 16 Merlucciidae: Merluccius merluccius; cranial muscles in lateral view; above, entire; centre, palatine portion of muscle Atp (superficial); below, after removal of superficial muscle. The levator arcus palatini is well-developed and lies lateral to the adductor mandibulae A2, but does not cover the origin of A 1 . The adductor arcus palatini floors the orbital cavity and inserts on the palatine. An unusual feature is the presence of a separate, small muscle running from the medial face of the palatine to the lateral face of the ethmoid bloc (Fig. 16). The muscle stems from the fascia of the adductor arcus palatini; in some specimens there are no muscle fibres, but only a narrow sheet of connective tissue. The opercular muscles are well-differentiated, although the dilatator operculi shares an aponeurotic origin with the levator arcus palatini. In Macruronus (Fig. 1 7), muscle A 1 a is a thick, bulky element almost covering the lateral face of A2. In the pinnate arrangement of its fibres, the muscle differs from that in the taxa so far considered. Insertion is on the dorsal maxillary process via a thick tendon. Muscle A10 originates from the outer rim of the quadrate, the entopterygoid and a lateral cavity of the palatine; insertion is one the medial face of the maxillary head. The position of the ramus mandibularis of the trigeminal nerve lies posterior to the origin of Al (3. Muscle A2 originates from the dorsomedial face and anterior rim of the hyomandibula and from the prootic. Insertion is via a lateral tendon to the coronomeckelian bone and a medial aponeurosis from which stems Aco; the latter lies entirely within the mentomeckelian cavity. The levator arcus palatini is small, its ventral portion covered by Ala; insertion is into a small lateral hyomandibular cavity. The adductor arcus palatini is divided into anterior and posterior 26 G. J. HOWES lap aap Fig. 17 Merlucciidae: Macruronus magellanicus; cranial muscles in lateral view. portions, the former inserting into the medial cavity of the palatine. The adductor operculi inserts entirely on the opercular process of the hyomandibula. In Lyconus (Fig. 18), muscle Ala is a narrowly triangular element whose area of origin extends from the central to the upper part of the preopercular limb. Fibre direction in the anteroventral section of the muscle is at almost 45° to that of the dorsal part. Insertion is via a long tendon on to the dorsal aspect of the maxilla. Muscle Alp resembles that of Merluccius in that it originates medially to the ramus mandibularis of the trigeminal nerve. The muscle's origins and insertions are complex; a posterior segment originates from the metapterygoid, a narrow, medial segment from the rim of the entopterygoid, and a long anterior segment from the concave lateral face of the palatine. The posterior segment runs into a long tendon, separate from that of the single tendon shared by the medial and anterior segments. The two tendons run forward to share a common insertion on the dorso-medial part of the maxillary head. Muscle A2 is large, originating from the sphenotic and pterotic, its anterior fibres running almost vertically into the lower jaw. The levator arcus palatini is a small unipinnate muscle originating from the sphenotic and pterotic; its insertion on the preopercular limb is above the origin of Ala. The adductor arcus palatini is well-developed, flooring the orbital cavity and, anteriorly, inserting on the palatine. As only the type specimen of Lyconus brachycolus was available it has not been possible to make a sufficiently extensive dissection to ascertain the morphology of the other cranial muscles. GADIDAE (Fig. 18) The following descriptions are based on three genera, Gadus and Merlangius (Fig. 18). These taxa differ from all those previously described in that muscle Ala is merely a thin, flat sheet of fibres stemming from the lateral body of A2 (as reported for Microgadus by Rosen, 1 962). The separation of Ala from A2 is marked by the course of the ramus mandibularis of the trigeminal nerve, which MACROUROID FISHES 27 passes medial to the segment; the separated fibres insert on the dorsal aspect of the maxilla via the maxillo-mandibular ligament. Muscle A 1(3 is a noticeably stout muscle and also differs from the previously described con- ditions in that it originates tendinously from the lateral face of the hyomandibula, passing forward between muscles A2 and A3 and lateral to the ramus mandibularis nerve (cf. medial in Merluccius). The muscle is deep and parallel fibred, running against, but not attaching to, the palatine; insertion is on the ventral medial edge of the maxillary head. Holmquist (191 1: 12-17) has adequately described and illustrated the origins and insertions of the deeper adductor and the suspensorial and opercular muscles in Gadus; I find little variation from this condition in other gadid genera examined. It should be noted here, however, that the levator arcus palatini inserts on a lateral shelf or slope of the hyomandibula. Although in Gadus, the levator is, for the most part, covered laterally by muscle A2, in Merlangius, A2 originates from below the hyomandibular shelf, thus leaving the levator exposed laterally and its outermost fibres lying in the same lateral plane as those of A2. The adductor muscles A2 and A3 are further discussed below (p. 41). Fig. 18 Merlucciidae: above, Lyconus brachycolus, jaw and suspensorial muscles in dorsolateral view. Gadidae; below, Merlangius merlangus, jaw and suspensorial muscles in lateral view. 28 G. J. HOWES RANICEPITIDAE (Fig. 20) Howes (1987) recognised Raniceps as belonging to a distinct family on the basis of its sharing with certain phycids and the Muraenolepididae a tendinous attachment of the rectus communis muscle and the derived arrangement of the adductor musculature now described. Muscle Ala is a small, spindle-shaped element, originating from the anterolateral face of A2. It runs alongside A 1 p, to which it is closely applied, and inserts via a long tendon on the dorsolateral face of the maxilla. Muscle A 1 p is a broad, band-like element having its origin tendinously from the hyomandibula and passing between muscles A2 and A3; anteriorly, the muscle becomes bulbous and inserts on the ventral surface of the maxillary head. tA2 Fig. 19 Gadidae: Molva molva; jaw and suspensorial muscles in lateral view; above, entire; below, with outer adductor element removed to expose origin of AiP. Mandibularis branch of trigeminal nerve in solid black. MACROUROID FISHES 29 aap ao do lo epx Imm Fig. 20 Ranicepitidae: Raniceps raninus; cranial muscles in dorsolateral view. Muscles A2 and A3 are thick, bulbous elements, the former originating from the preoperculum and hyomandibula, and the latter from the pterosphenoid and prootic. Both muscles join a common aponeurosis in the lower jaw from which Aco originates. The levator arcus palatini is also a thick, bulbous element, stemming from the sphenotic and pterotic to insert on the hyomandibula and preoperculum. The lateral fibres of the levator meet those of adductor A2 along a near vertical raphe. The adductor arcus palatini is well-developed and floors the orbital cavity. The anterior fibres do not, however, insert on the palatine but remain within the confines of the entopterygoid. The dilatator operculi is a narrow, ribbon-like muscle sharing a common origin with the pos- terior fibres of the levator arcus palatini; it inserts tendiously on the rim of the opercular facet. The adductor and levator operculares muscles share a common origin from beneath the pterotic and are separable only because of their insertions. The adductor inserts entirely on the opercular process of the hyomandibula; the levator along the dorso-medial surface of the operculum. PHYCIDAE (Fig. 21) Urophycis is taken as the taxon representing this family but in at least one myological character both it and Phycis differ from other genera regarded as belonging to the family (see below). In Urophycis (Fig. 2 1 ), fibres of muscle A 1 share a common origin from the preopercular margin with those of A2. Al separates from the body of A2 above the jaw articulation, its fibre direction varying from horizontal to 45°, and inserts via a long tendon on the anterodorsal process of the maxilla. Ventromedially, the insertion of Ala joins the maxillo-mandibular ligament. Muscle Alp is a thick, cylindrical element originating, medially to A2, from the anterior rim of the hyomandibula. The muscle passes laterally to the ramus mandibularis of the trigeminal nerve, becoming slightly indented on its medial face below the orbit, and inserting musculously on to the ventral surface of the maxillary head. 30 G. J. HOWES Muscles A2 and A3 join a common aponeurosis medial to the anguloarticular (only a few fibres insert on the dorsal rim of the bone); the aponeurosis divides into medial and lateral tendons, the lateral one inserting on the coronomeckelian bone, while the medial branch forms the site of origin for muscle AGO. This muscle fills the mentomeckelian cavity with only a thin layer of fibres passing outside the cavity along the medial face of the dentary. The levator arcus palatini is extensive and lies between A2 and A3; its dorsoposterior part can only be distinguished as a dilatator operculi by the insertion of those fibres on the rim of the opercular facet. The adductor operculi runs from the pterotic to the opercular process of the hyomandibula; the levator operculi inserts on the medial rim of the operculum. Urophycis is unusual in that a segment of epaxial muscle runs anteroventrally from the supracleithrum to insert on the medial face of the operculum. The posteroventral border of the muscle meets a part of the epx lap hyad hyad Fig. 21 Phycidae: above Urophycis regia; cranial muscles in lateral view. Lotidae: below, Lota lota; cranial muscles in lateral view; extent of levator arcus palatini and pathway of ramus mandibularis are indicated by dashed lines. MACROUROID FISHES a Fig. 22 Bregmacerotidae (above): Bregtnaceros atlanticus. Muraenolepididae (below): Muraenolepis microps. Cranial muscle in lateral view (posterior extent of Atp indicated by dashed lines). hyohyoidei adductores which extends from the last branchiostegal ray almost to the dorsal margin of the operculum. The epaxialis segment is less well-developed in Phycis and such an arrangement is absent in other phycids (see Howes, 1988). LOTIDAE (Figs 19; 21) In Lota (Fig. 21) muscle Ala is only differentiable from A2 anteriorly by the separation of a bundle of lateral fibres which insert, via a long tendon, on the dorsal process of the maxillary bone. Muscle A 1 P originates from the anterior rim of the hyomandibula, medial to A2. A ventral tendon of A 1 (3 meets A 1 a at the anterior border of A2; the fibres of muscles A 1 a and A 1 P are indistinguishable for a short distance prior to separation. Alp inserts on the ventromedial face of the maxillary head. The ramus mandibularis of the trigeminal nerve passes medial to Al P, crosses above the lower jaw insertion of A2 + 3, and then passes medial to Ala. Muscle A3 is separated dorsally from A2 by Alp, the two former elements joining in a common aponeurosis from which Aco originates. The levator arcus palatini is not covered by A2 as in the Phycidae, its lateral fibres lying in the 32 G. J. HOWES same plane and meeting aponeurotically those of A2. The ventral surface of the levator is bevelled to accommodate the medial surface of A2. The opercular muscles are similar to those described for Urophycis and, as in that taxon, a segment of epaxial muscle inserts on the medial border of the operculum. Its site of origin, however, is the posttemporal rather than the supracleithrum as in Urophycis (but cf. Muraenolepis, below). In Molva (Fig. 19), muscle Alp occupies a position similar to that in Gadus and Merlangius but comprises a long tendon stemming from the point of origin on the hyomandibula and expanding anteriorly into a thick bundle of fibres which inserts on the maxillary head. Muscle A2 runs from the lateral face of the hyomandibula and preoperculum to insert with A3 on an aponeurosis from which muscle Aco also originates. MURAENOLEPIDIDAE (Fig. 22) In Muraenolepis (Fig. 22) muscle Al has its origins lateral and medial to A2. Its lateral origin is from a thin tendinous sheet covering the face of A2; its medial origin is from a tendinous fascia on the inner aspect of that muscle. The two bodies of the muscle join into a single element anterior to the border of A2. The lateral part of Al (Ala) inserts tendinously on the dorsal aspect of the maxilla; the ventral border of the insertion tendon joining the maxillo-mandibular ligament. The main portion of Al (A 10) inserts on the ventromedial aspects of the maxillary head. Muscle A2 is large, covering most of the levator arcus palatini laterally. It converges with muscle A3 into a thick tendon medial to the anguloarticular. A stout subbranch of the tendon inserts on the coronomeckelian bone. Muscle AGO extends from the principal part of the tendon; only its anterior tip enters the small mentomeckelian cavity. Muscle A3 is divided from A2 by the levator arcus palatini which is a large, laterally bulbous muscle, originating from the sphenotic and inserting into a shallow cavity on the lateral face of the hyomandibula. The adductor arcus palatini is well-developed, flooring the orbital cavity and inserting anteriorly on the palatine. The opercular muscles are well-differentiated from one-another; the dilatator is a narrow, spindle-shaped element inserting on the long anterior process of the operculum; the adductor and levator operculares originate from the underside of the pterotic and insert close together on the anteromedial face of the operculum (see Howes, 1988, fig. 5). As in Urophycis and Lota, a segment of epaxial musculature inserts on the medial face of the operculum, being narrowly separated from the hyohyoidei adductores. As in Lota, the site of origin of the epaxial segment is the posttemporal (see Howes, 1988, fig. 5). BREGMACEROTIDAE (Fig. 22) In Bregmaceros (Fig. 22) muscle A 1 is thin and shallow and incompletely divided. However, below the eye there is a strong, dorsal tendon and medial aponeurosis with a slight separation of the lateral fibres. The muscle insertion covers a long area of the maxilla, being tendinous anteriorly and musculose posteriorly. Muscle A2 is large with a deep concave anterior border. The levator arcus palatini is a small thin element lying posterodorsally to the adductor. The adductor arcus palatini is divided, the anterior part inserting on the palatine, the posterior on the medial rim of the hyomandibula. Summary and discussion of the muscles associated with the jaws and suspensorium Certain features of these muscles are common to all macrouroids, namely: 1 . Muscle Al is never separated by A2, as is the case in other gadiforms and divisions Ala and Al P lie in the same vertical plane. 2. Muscle A 1 P always lies lateral to the ramus mandibularis of the trigeminal nerve and, because of this relationship, is homologous with that muscle in other gadiforms. MACROUROID FISHES 33 Fig. 23 Muscle AtP and its associations in: A, Ophidian rochei (muscle Aj + A2 cut away, its borders indicated by dashed lines; B, Glyptophidium macropus; C, Ly codes frigidus. 3. Muscle Al p never originates from the palatine, in contrast to the condition in some gadoids. 4. Muscle Alp in the majority of macrouroids, is not constricted below the orbit, nor has it an anterior expansion. 5. The adductor arcus palatini is continuous and never divided as in some gadoids. 6. The levator arcus palatini lies lateral to muscle A 1 and A2, a feature shared with some gadoids but few other teleosts. 7. Muscle A3 is absent, in contrast to most other gadiforms and acanthopterygians. 34 G. J. HOWES Because of the often contrasting conditions in these features between macrouroids and other gadiforms, it is necessary to examine each in detail. 1. In macrouroids both muscles A Jo. and Alfi always lie lateral to muscle A 2 and the division between the Al element is in the vertical rather than the sagittal plane. In the Macrouroidinae (Macrouroides and Squalogadus) and some genera of Macrourinae (Type II morphotype, see p. 12), A 1 is undivided, or incompletely so. Incomplete separation of Ala and Al P occurs in some gadoids (i.e. Bregmaceros, Euclichthys, Lyconus, Steindachneria, Lepidion). In other paracanthopterygians (ophidioids, zoarcids and percopsids) there is no Ala, the single muscle inserting on the lower jaw. However, it is questionable whether this muscle is the homologue of A2 since the ramus mandibularis of the trigeminal nerve runs medial to it, and in some taxa the upper portion of the muscle has a close association with the maxillo-mandibular ligament. For example, in the ophidiiform Ophidian rochei (Fig. 23 A) the ramus mandibularis runs medial to the upper part of the muscle, which is attached to the maxillo-mandibular ligament, the nerve then piercing the element and running laterally into the lower jaw. In the zoarcid Lycodesfrigidus (Fig. 23C) the entire length of the nerve branch runs medial to the outer muscle bloc, but there is a distinct lateral myocomma which marks an abrupt change in fibre direction; the dorsal, parallel fibres insert directly onto the maxillo-mandibular ligament. In the percopsiform Percopsis (Fig. 24), although the nerve runs medial to the outer adductor muscle, there is no sign of any fibres running onto the maxillo-mandibular ligament or the upper jaw. Thus, on the basis of the position of the ramus mandibularis and on what has been said above (p. 1 6) concerning its topographical position, the outer muscle in the above mentioned ophidioids, zoarcids and percopsids must be construed as the homologue of the element identified as Al in macrouroids and gadoids (and various other teleosts) despite the fact that in some cases it does not insert on the upper jaw. Whether the lack of an upper jaw insertion is the plesiomorphic condition or whether attach- ment of the muscle to the upper jaw has been lost, may only be assessed through congruence with other synapomorphies. In the majority of acanthopterygians the ramus mandibularis of the trigeminal nerve consis- tently lies medial to muscle Al (and so by its position signifies the identity of that element) even though in some taxa it follows the anterior border of A2. 2. Muscle Al$ (andAlj). A brief account was given above (p. 16) of the nomenclatural history of muscle Al P and it is now treated in detail. Rosen (1973), realised, correctly, that the muscle in question is not the homologue of the levator maxillaris superioris of halecomorphs, which muscle comprises several sections having their origins from the infraorbitals and lateral ethmoid as well as from the palatine and hyomandibula. In macrouroids muscle Al P lies lateral to the ramus mandibularis and in some taxa it is incom- pletely separated from A 1 a posteriorly. It always inserts on to the medial face of the maxillary shaft and is never attached to an element of the suspensorium. In assumed primitive gadoids (Bathygadidae; see Howes, 1988), muscle Alp has a similar morphology to that in macrouroids and similarly lies in the same vertical plane as muscle Ala. However, in progressively more advanced gadoids Alp shifts medially; in Melanonus and Steindachneria the shift concerns only the anterior part of the muscle, but in the Euclichthyidae and other gadoids (apart from the Bregmacerotidae) the posterior part of Alp also shifts medially so that the entire muscle comes to lie mesiad not only to A 1 a, but also (in more advanced gadoids) to A2. In the Trachyrincidae although there is a single adductor muscle, it has a double insertion on the maxilla (p. 17) suggesting that Ala and Alp are fused. According to Casinos (1978) Trachyrincus has lost muscle Ala and it has been 'replaced' by a '. . . displacement outwards of the levator maxillae superioris' (i.e. A1P). There is, however, no evidence to suggest that such a loss and subsequent displacement has occurred. On the contrary, I would advocate that the opposite is the case and that muscle A 1 P has shifted medially in gadoids (see above). The situation in Trachyrincus is simply a derived specialisation of that taxon. Casinos (op. cit.) in studying a limited taxonomic range of macrouroids has failed to take into MACROUROID FISHES 35 Fig. 24 Percopsis omiscomayus. Upper jaw and suspensorial muscles in lateral view. Medial pathway of ramus mandibularis indicated by dashed lines. account the varying morphology of the adductor muscle. A single element also occurs in the Macrouroidinae and in a group of macrourines (see p. 13), and is probably also the result of fusion between A 1 a and A 1 p. Lauder & Liem (1983: 148) state that it is only in more advanced paracanthopterygians that muscle Al p alone inserts on the maxilla. These authors do not justify that statement by providing examples, nor do they include it as a synapomorphy in their cladogram of paracanthopterygians. Accepting their statement means that no gadiform can be considered 'advanced'. But, on the basis of this character ophidiiforms and percopsiforms must form a monophyletic assemblage. If lophiiforms are taken to be 'advanced paracanthopterygians' then Lauder & Liem's hypothesis is rejected because muscle A 1(3 is absent in these fishes (muscle Al is a single element inserting on a broad ribbon-like maxillary tendon and posteriorly is undifferentiated from A2). As noted above, in macrouroids and gadoids muscle Al p lies lateral to the ramus mandibularis of the trigeminal nerve. In other paracanthopterygians, however, the muscle lies medial to the nerve. A variation of this condition is illustrated in the ophidiiform Ophidian rochei where the nerve loops medially around the muscle's origin on the hyomandibula (Fig. 23 A). In another ophidioid, Glyptophidium macrops, the nerve also passes medially to Al p, but Ala is lacking (Fig. 23B). in the neobythitine ophidiiform Lamprogrammus niger the ramus mandibularis follows a convoluted path. In this taxon the outer muscle bloc comprises two elements, the dorsal of which inserts on the maxillo-mandibular ligament and the ventral on the mandible. There is a well-developed Alp which is divided posteriorly by the levator arcus palatini muscle. The mandibularis nerve passes between the divisions of Alp, then medially to the dorsal adductor element. The nerve then runs laterally across the upper part of the ventral adductor segment, after which it turns inward to course medially to the lower segment. Thus, using the nerve pathway as the criterion of muscle identification, not only is the upper segment Al a, but so is the ventral portion of the lower segment, 36 G. J. HOWES Imm Fig. 25 Lamprogrammus niger. Muscle A , P and its associations. In A the upper part of muscle A2 is cut away, and in B the superficial part is removed with AjCi reflected. despite its insertion on the lower jaw. Muscle A2 is that small dorsal portion of the lower segment inserting on the mandible (Fig. 25). Muscle A I P is reported to occur widely in neoteleosts; according to Lauder & Liem (1 983: 143) it occurs in stomiiforms, some acanthopterygians, some paracanthopterygians and some aulopi- forms but not in atheriniforms or neoscopelids. This statement appears, in part, to be based on the work of Rosen (1973). According to Rosen (op. cit.) there is, in stomiiform fishes, an Alp and sometimes an Ala. Fink & Weitzman (1984) maintained that Alp was a neomorphic feature independently derived in stomiiforms, myctophiforms and acanthomorphs (Fig. 26C). I agree that A 1 P in gadiforms is not homologous with the so-called A 1 P in stomiiforms or myctophiforms, nor indeed with that in lower groups in which it has been reported (e.g. halosauran elopomorphs; Greenwood, 1977). My reasoning for this assumption is that in those latter groups the muscle in question always lies medial to the ramus mandibularis of the trigeminal nerve (see for example Tchernavin, 1 953, fig. 29). In higher neoteleosts an A 1 P muscle is recorded by Rosen ( 1 973) in some beryciforms. He notes that stephanoberycids have entirely separate internal and external maxillary muscles similar to the gadiform condition. However, I find that in Stephanoberyx monae, an example illustrated by Rosen, muscles he labels as A2 and A 1 p are united at their origin (Fig. 26B). Rosen's A 1 p, which in his figure appears to have a double insertion on the maxilla, is equivalent to my Ala, and his Ala corresponds to the upper part of what I interpret as muscle A2 since this element inserts on the lower jaw; as shown in Rosen's figure. In the beryciform Hoplostethes, muscle A 1 lies laterally to A2 (Fig. 26A). MACROUROID FISHES 37 In the myctophiforms examined (Lampanyctus, Electrond) and that illustrated by Rosen (1973), (Protomyctophum), only an Alp is present and this also lies medial to the ramus mandibularis branch of the trigeminal nerve. Lauder & Liem's (1983: 143) statement that muscle Alp is absent in atheriniforms needs confirmation. In the small sample examined I find that in some taxa (e.g. Orestias) the man- dibularis nerve branch passes medially to a segment of adductor muscle which inserts on the lower jaw. This could be muscle A 1(3 having secondarily acquired a mandibular insertion. In Hemiramphus muscle A 1 appears to be entirely lacking. If the presence of A 1 P is an acanthomorph synapomorphy then its absence in various atheriniform lineages must be viewed as derived losses. In Polymixia the arrangement of adductor muscles is complex (Fig. 27B). Rosen (1973: 420) suggested that the polymixiid pattern was '. . . transitional between the Al and Al|3 systems'. My interpretation is somewhat different, however, since the specimen of Polymixia nobilis examined differs from that of P. japonica illustrated by Rosen. The principal lateral muscle of P. nobilis appears to be a combined Ala and A2 (Rosen's A2) since a group of fibres inserts via a narrow tendon on to the posterodorsal part of the maxillo-mandibular ligament and passes laterally to the ramus mandibularis nerve branch. A large anteromedial muscle, corresponding to Rosen's Al|3, inserts on to the dorsal surface of the maxilla. Although adhering to the maxillo-mandibular ligament by connective tissue along most of its length, its fibres remain separated from that ligament (Rosen's figure of P. japonica shows them inserting on to the maxillo-mandibular liga- ment). As shown by Rosen, there are two sections of muscle Al (3 which are separated by the course of the ramus mandibularis branch. The inner section is connected to the outer anteriorly along an internal aponeurosis which is evident laterally as a tendinous band (lalb, Fig. 27B). I am unable to locate in P. nobilis a muscle corresponding the Rosen's labelled A3 in P. japonica. Fig. 26 The superficial upper jaw adductor musculature of the beryciformes: A, Hoplostethes melanopus; B, Stephanoberyx monae; and the stomiiform, C, Photichthys argenteus. 38 G. J. HOWES It seems that, at least in P. nobilis, muscle Alp is present, although poorly differentiated, and muscle A 1 P corresponds in topographical position to the so-called A 1 P in myctophiforms and stomiiforms. This observation supports Stiassny's ( 1 986) phylogenetic positioning of Polymixia as the sister-group of the Paracanthopterygii plus Acanthopterygii. Rather surprisingly, the adductor muscle arrangement in the Sciaenidae (a family currently placed in Acanthopterygii) greatly resembles that of Polymixia and certain gadoids. In Cynoscion for example (Fig. 27 A) muscle A 1 P is divided as in Polymixia by the ramus mandibularis branch of the trigeminal nerve, the outer section running into the maxillo-mandibular ligament; the inner section, which originates from the quadrate and hyomandibula, also joins the maxillo-mandibular ligament for part of its length. The anterior, expanded part of the muscle originates from the palatine as in merlucciid gadoids (see above). Interestingly, Freihofer (1978: 45) draws attention to the resemblances between sciaenid and percopsiform musculature, including the innervation pattern. One group of macrouroids, designated as morphotype la possesses an additional adductor muscle, termed Aly (p. 12). This muscle is usually a weak spindle-shaped element originating via a thin tendon from the medial face of Alp and having a common insertion with that muscle on the maxilla. In Abyssicola, the tendon of origin stems from the anterior rim of the hyomandibula and in this respect resembles the condition of Alp in certain gadoids (see above). I have not found a muscle corresponding to Aly in any other acanthomorph taxon and regard it as synapomorphic for the macourine genera Coryphaenoides, Abyssicola, Nezumia, Coelorinchus, Lionurus, Nemato- nurus and Chalinura. 3. Origin of muscle A 1$ from the palatine. Among gadoids this feature occurs in the Merlucciidae (Merluccius, Macururonus and Lyconus). The anterior part of muscle Al P originates from a lateral palatine cavity (complexly so in Lyconus; see p. 26 above). The origin of part of Alp from the palatine also occurs in some sciaenids (see above) in which taxa it is considered to have arisen independently from that in merlucciids (see Howes, 1988 concerning the phylogenetic position of the Merluccidae). 4. Suborbital constriction of muscle Al$ and its insertion. There is no suborbital constriction of muscle A 1 P in macrouroids. In gadoids, however, a tendinous constriction of the muscle occurs in the Bathygadidae, Moridae, Melanonidae (sensu Howes, 1988) and Euclichthyidae. Constriction of the muscle below the orbit leads to an anterior expansion of the muscle. The occurrence of a suborbital constriction of the dorsal part of A 1 in such unrelated groups as Cichlidae (Otten, 1981) and Cyprinidae (Howes, 1984a) casts doubt on the feature having any phylogenetic significance; it seems to be a functional means of accommodating the eye. That this is so is indicated bythe long and obliquely angled jaws of the gadoid taxa possessing the constriction, which necessitates a sharp change in angle to pass around the eyeball. In contrast, the jaws of macrouroids are short, so that the fibres of muscle Al P are directed downward and their course is uninterrupted by the eye. The Trachyrincidae are exceptional in that although possessing long jaws they are horizontally aligned and the muscle remains unconstricted (Fig. 7), although the eye is not relatively smaller than that in macrouroids. Although in primitive gadoids such as Bathygadus and Gadomus (Figs 9 & 1 1 ) the anterior 'expansion' of muscle Alp follows as a consequence of suborbital constriction, in more advanced gadoids this expansion has apparently a functional nature in that it is bulbous and transversely expanded, and fills the palatine cavity; in merlucciids this section of the muscle is even attached to the palatine (see p. 12). Thus, I have considered the anterior development of muscle Alp to be a synapomorphy for gadoids including and above Bathygadus (Howes, 1988). The variability of the site of attachment of muscle Al P to the maxilla demands some comment. In macrouroids the anterior part of the maxilla bears a prominent ventromedial process which contacts the ascending process of the premaxilla (Mvp, Figs 2 & 3). On the inner side of the maxillary ventral process is a small depression into which inserts the tendon of Alp (Fig. 28 A). A similar ventromedial process occurs in the Bathygadidae and Moridae but is not so well-developed MACROUROID FISHES 39 Let Fig. 27 Jaw adductor muscles in A, a sciaenid Cynoscion jamaicensis and B, a polymixiid Polymixia nobilis. as that in macrouroids and the tendon of A1J3 inserts on the posterior rim of the ventromedial process (Fig. 29 A). In the Trachyrincidae, the inner insertion tendon (presumably representing A 1 P; see above, p. 1 7) inserts on the dorsal aspect of a medial maxillary shelf (Fig. 29B). This is similar to the situation in other gadoids where the muscle insertion is shifted forward to insert along the dorsomedial ledge of the maxilla (e.g. Euclichthyidae). In the Melanonidae and Merlucciidae Alp inserts on the medial aspect of the maxillary head (Fig. 29C) whereas in the more advanced gadoids (Gadidae, Lotidae, Phycidae, Ranicepitidae, Muraenolepididae; see Howes, 1 988) its insertion is on the ventral limb of the maxillary head (Fig. 29D). The anterior shift of A 1 p insertion appears to be correlated with the transverse expansion of that muscle and its shift from a lateral to medial position with respect to the outer adductor muscle (see above). It is supposed that the anterior placement of the muscle's insertion site is a derived condition for those families listed above. 5. The adductor arcus palatini is, in some gadoids divided into anterior and posterior parts. According to Winterbottom (19740: 238) the adductor arcus palatini in its plesiomorphic state is 40 G. J. HOWES Mxh Fig. 28 A, Nezumia hildebrandi, insertion of muscle AjP on maxilla (ventral view); B, Coelorinchus caribbaeus, ventral view of maxillary and premaxillary ligamentous connections; C, Ventrifossa occidentalis, lateral view of maxillary-premaxillary-rostral cartilage associations. confined to the posterior region of the orbit between the skull and hyomandibula; its derived condition is to floor the orbital cavity and extend posteriorly. Part of the adductor in gadoids usually originates from the parasphenoid, only a small portion stemming from the prootic; a separate adductor hyomandibulae is not recognisable. The division of the adductor arcus palatini in some gadoids (Bregmaceros , Macruronus} is, on the basis of in- and out-group distribution, a derived condition and a 'precursor' can be recognised in some morids (p. 20) and Steindachneria (p. 22) where the central portion of the muscle is thin and weakly developed. Apart from Bathygadus, Gadomus and Euclichthys an anterior insertion of the adductor arcus palatini on to the palatine is a feature of all gadiform fishes examined, and is also present in some ophidiiforms. Among acanthopterygians a palatine attachment of the adductor arcus palatini is present in Sciaenidae, Eleotridae and some Cichlidae (see, for example, Greenwood, 1985). Of other families checked for this feature, it is lacking in Pomacentridae, Labridae, Atherinidae, Nototheniidae, Stephanoberycidae, Polymixiidae, Scombridae, Sparidae and Lutjanidae. Admittedly this is not an exhaustive survey of acanthopterygian taxa but it does not indicate that a palatine attachment of the adductor arcus palatini is an unusual acanthopterygian condition; such an attachment has been treated as derived (Greenwood, 1985: 156; 165). To treat a palatine attachment of the adductor as a synapomorphy uniting the majority of gadiforms and some ophidiiforms, would conflict with the pattern of relationships arrived at through other synapo- morphies (see Howes, 1988). It is more parsimonious to assume an independent derivation of the feature in the various lineages in which it occurs. 6. In the Trachyrincidae, the levator arcus palatini is extensive posteriorly, covering the upper part of the plate-like preoperculum and lying medial to Al (Fig. 7). In the Melanonidae and Steindachneriidae the levator is small, its insertion being high on the preopercular limb (Figs 12 & 1 3). A similar situation occurs in the Bregmacerotidae, where the levator is much reduced and inserts on the dorsal margin of the preoperculum (Fig. 22), a feature also present in the percopsiform Percopsis (Fig. 24). MACROUROID FISHES 41 The Euclichthyidae has an autapomorphic arrangement of the levator arcus palatini. Although extensive, the muscle does not lie laterally to the superficial adductor musculature as in lower gadoids and macrouroids, but mostly posteromedial. Near its insertion the levator is bifurcate, the posterior segment inserting on the preoperculum and just overlapping the posterodorsal edge of Al, the anterior one inserting on the hyomandibula and joining an aponeurosis from which originates muscle Al P (Fig. 14). The morphology of the levator in Euclichthys could, in evolutionary terms, be construed as the 'precursor' of the situation found in other gadoids where the entire muscle lies medial to the outer part of the adductor mandibulae. If the acanthomorph condition of the levator arcus palatini occurring medially to the outer adductor muscle be regarded as the plesiomorphic condition, then the similarly placed muscle in higher gadoids is a phylogenetic reversal from the laterally placed levator which characterises the macrouroids and majority of gadoids. One may then interpret as 'intermediates' between these taxa and higher gadoids the posterior shifts of the levator found in the Melanonidae and Bregmacerotidae and partial lateral overlap of the adductor in the Euclichthyidae. 7. Muscle A3 is lacking in macrouroids. This muscle is usually defined as the most medial of the adductor complex, having its insertion in the lower jaw (according to Winterbottom 1 914a: 234) on the 'medial face of the dentary, in the Meckelian fossa, or both.' Allis (1897: 581) identifies the A3 as that muscle lying medial to the adductor ramus of the maxillaris inferioris nerve. In most acanthomorphs, the ventral fibres of A3 converge with those of A2 on to a common aponeurosis which attaches to the inner face of the anguloarticular. Dorsally, A2 and A3 are separated by the levator arcus palatini. In macrouroids and many gadoids, the levator lies outside the adductor complex (see above) and so the medial adductor bloc comprises a single element dorsally . Only in the more advanced gadoids (Gadus, Lota etc.) is it possible to distinguish an A3 on the grounds of its dorsal separation from A2 by a levator arcus palatini. In macrouroids and lower gadoids, the insertion of the medial adductor element (A2) on the lower jaw is a simple one; all fibres converge into an aponeurosis from which departs a ventrally directed tendon. The tendon inserts on the coronomeckelian bone; no fibres are associated with the tendon. In advanced gadoids the situation is more complex, with the inner fibres of A2 inserting on the coronomeckelian tendon, while those of A3 cross over to insert on the lateral tendinous sheet. According to Casinos (1978) muscle A3 in gadoids is homologous with the inner part of the macrouroid adductor complex. Furthermore, Casinos regards the gadoid ( = my higher gadoids, e.g. Gadus, Merluccius, Pollachius) condition of separate A2 and A3 muscles to be plesiomorphic ,Pmx Men Fig. 29 Maxillary insertion of muscle A l (3 and the ligamentous connection between the maxilla and premaxilla in: A, Bathygadidae, Bathygadus favosus; B, Trachyrincidae, Trachyrincus trachyrincus; C, Melanonidae; Melanonus zugmayeri; D, Gadidae, Gadus morhua. 42 G. J. HOWES a lo hyad Fig. 30 Hyoid musculature of A, Macrouroidinae: Squalogadus modiftcatus; B, Macrourinae: Coryphaenoides mexicanus. Ventral views. and to have given rise to derived states in macrouroids either by the amalgamation of A2 and A3 or the loss of A2. Casinos' assumptions are based on the recognition of the gadoids as being plesiomorphic but on the contrary they appear to be the derived sister-group of macrouroids (see Howes, 1988). I would suggest that the 'amalgamation' of A2 and A3 in macrouroids (and in out-groups) is the plesio- morphic state representing an undifferentiated muscle bloc. The differentiation of a medial muscle element (A3) is a derived condition that has undoubtedly occurred independently in several teleostean lineages. Muscles of the hyoid region Among macrouroids there is little variability of the hyoid muscles, such variation as does occur concerns the points of attachment of the protractor hyoidei and the degree of development of the hyohyoidei abductores. The protractor hyoidei originates from the anterohyal at the articulation of, and usually attach- ing to the 2nd, 3rd or 4th branchiostegal ray. Most frequently the muscle attaches to the proximal stem of the 3rd and 4th rays. Only in Lionurus is there a single attachment to the 2nd branchiostegal ray. The protractor hyoidei is usually well-developed. In most taxa the left and right parts of the muscle continue forward, narrowly separated from one another in the midline. Anteriorly the parts diverge slightly to insert on their respective dentary. Echinomacrurus is unusual among the Macrourinae in having a ribbon-like protractor hyoidei with the right and left parts separated in the midline. In this respect, Echinomacrurus resembles taxa of the Macrouroidinae. In both macrouroidine genera the protractor hyoidei is a rope-like element extending from the anterohyal MACROUROID FISHES 43 anterior to the articulation of the 4th branchiostegal ray; insertion is close to the symphysial tip of the dentary (Fig. 30). The left and right parts of the muscle are separated for their entire lengths. In Cetonurus the left and right parts of the protractor meet only beneath the ventral hyoids, remaining separated for the remainder of their lengths. An intermandibularis is present in all taxa examined with a single exception, namely the macrouroidine Squalogadus. The muscle is a thin, narrow band of fibres with the protractor hyoidei inserting below it. The hyohyoidei abductores run from the 1st branchiostegal ray to insert tendinously on the contralateral dorsohyal. The hyohyoidei adductores are weakly developed in all taxa and usually comprise a few widely spaced fibres arranged in narrow bands connecting the branchiostegal rays (Fig. 32). Posteriorly, those fibres connecting the last branchiostegal ray with the suboperculum and operculum are stronger and more numerous. In gadoids the hyoid musculature is generally more strongly developed than in macrouroids. For example, in the Muraenolepididae (Fig. 31), the protractor hyoidei is well-developed, attaching to the base of the 3rd and the upper part of the 2nd branchiostegal ray; an anterior segment of the muscle attaches tendinously to the ventromedial border of the dentary. The parts of either side meet in the midline and run forward as a single muscle inserting at the symphysis beneath a small intermandibularis. The hyohyoidei abductores and adductores are also well-developed. The morphology of the hyoid muscles in the Gadidae, Lotidae and Phycidae is similar to that in the Muraenolepididae except that the intermandibularis is more strongly developed in the former. Holmquist (1911) has described and figured the hyoid musculature ofGadus in which he identifies two sections of the intermandibularis. Winterbottom (19740: 245) concluded that the anterohyal section should properly be referred to as the protractor hyoidei. The morphology of the hyoid musculature is rather uniform and the often recognised taxonomic grouping of macrouroids based on the number of branchiostegal rays, viz. 6 or 7 is not reflected by different muscle morphotypes. The most noticeable differences are those between the Macro- uroidinae and Macrourinae where in the former the two parts of the protractor hyoidei are ribbon- like and separated in the midline and the intermandibularis is absent (at least in Squalogadus). A similar separation of the protractor also occurs in the macrourine, Echinomacrurus (see above). The osteology of Echinomacrurus is unknown, but its external morphology would indicate that it is a hyad Fig. 31 Hyoid musculature of Muraenolepis microps; ventrolateral view, position of intermandibularis indicated by dashed lines. 44 G. J. HOWES hyad Imh Fig. 32 Trachyrincus trachyrincus: above, hyoid musculature seen in oblique ventrolateral view; below, ligamentous connections of the lower jaw and hyoid bar seen in ventral view. member of the Macrourinae, although a highly derived one. The similarity in the morphology of its hyoid muscles with that of the macrouroidines has possibly been independently derived. The complete separation of the protractor hyoideiin the midline is an unusual feature amongst teleosts and is known elsewhere only in the otophysan Loricariidae (Howes, 1983) and the Gyrinocheilidae (pers. obs.). The sternohyoideus muscle, connecting the pectoral girdle with the hyoid bar occurs among gadiforms in two conditions — long and compressed or deep, broad and short. Usually, a long, compressed sternohyoideus attaches to a urohyal whose posterior margin is widely separated from the cleithrum, whereas a short, broad sternohyoideus is associated with a urohyal whose posterior border is in contact with, or narrowly separated from the cleithrum. The posterior limit of the sternohyoideus is usually well-defined ventrally by its attachment to the cleithra, but its lateral fibres are continuous with those of the body musculature (obliquus infer ioris). MACROUROID FISHES 45 In macrourids a long, compressed sternohyoideus occurs in Odontomacrurus, Hymenocephalus, Chalinura, Echinomacrurus , Cynomacrurus and Lionurus. A stout, broad muscle is present in Macruorus, tiezumia, Trachonurus, Malacocephalus and the macrouroidine, Squalogadus. The latter is unusual in possessing a stout sternohyoideus associated with a urohyal that is widely separated from the pectoral girdle, a feature also possessed by the Trachyrincidae. Among gadoids, the Bathygadidae and Moridae have a long compressed sternohyoideus. However, in bathygadids the tendons of the paired infracarinalis anterior stretch forward from the pelvic girdle to attach via connective tissue to the ventral tips of the cleithra, and continue forward into the ventral body of the sternohyoideus. The tendons of the infracarinalis finally insert on either side of the urohyal keel (Fig. 35). In other gadoids a long compressed sternohyoideus is present in the Merlucciidae where there is a well-defined ventral division of the muscle to which the infracarinalis anterior is tendinously linked. obv1-3 Dh shl rv4 Fig. 33 Ventral gill-arch musculature of: A, a macrourid, Macrourus berglax; B, a gadoid, Trachyrincus trachyrincus. Ventrolateral views. In A the anterior border of the cleithrum is indicated by a dashed line. 46 G. J. HOWES In all gadiforms and other paracanthopterygians examined a dorsolateral segment of the sternohyoideus inserts on a stout tendon which runs anterodorsally to insert on the 3rd hypo- branchial (see Figs 33-36). In acanthopterygians (?all) a similar tendon runs from the dorsomedial part of the muscle. Ventral gill-arch muscles Macrouroids, in common with almost all teleosts possess well-developed obliqus ventrales on the 1st through 3rd ventral gill-arches (Fig. 33 A; 34). In contrast, gadoids have reduced (or even lack) obliqus ventrales on either the 1st or the 1st and 2nd gill-arches (Fig. 35). The Bathygadidae, Steindachneriidae, Melanonidae, Moridae and Trachyrincidae have reduced (or in some bathygadids lack) the muscles from only the 1st arch (Figs 33B; 34); see Howes, 1988. Reduction takes the form of a tendon attaching to the proximal tip of the ceratobranchial and with only a minute muscular element being present. In the Bregmacerotidae, the muscles appear to be lacking entirely on the 1 st and 2nd gill-arches. Winterbottom (\914a: 263) notes that there are a variable number ofrecti ventrales in teleosts. The usual acanthomorph condition is for rectus ventrales IV to run between the semi-circular ligament connecting the 3rd hypobranchials across the midline, and the 4th ceratobranchial. This is also the condition present in the majority of macrouroids, with the exception of Hymenocephalus where the anteroventral part of the muscle inserts on the urohyal and in Macrourus, where the entire muscle inserts on the bone. Squalogadus is also exceptional in that the rectus ventrales IV joins posteriorly to the tendon of the rectus communis and so by-passes the 4th ceratobranchial, inserting instead on the 5th. Among gadoids, the rectus ventrales IV attaches to the urohyal in Lyconus (Merlucciidae), the Ranicepitidae, Phycidae and Muraenolepididae. In other merlucciids, Bathygadidae, Moridae, Steindachneriidae, Melanonidae and Lotidae, the muscle attaches together with the rectus communis to a dorsal aponeurosis of the sternohyoideus muscle (Fig. 35). In the merlucciid Macruronus, the rectus ventrales IV has a long tendon which inserts on the 5th ceratobranchial; the muscle itself is separated from the 4th arch, and anteriorly attaches to a complex aponeurosis of the sternohyoideus (Fig. 36). Table 2 Insertion sites of rectus communis and rectus ventralis IV muscles in macrouroids and gadoids. Uh = urohyal; Sh = sternohyoideus; 3Hy = third hypobranchial Rectus communis Ur Sh Rectus ventralis IV 3Hy Sh Uh Macrourinae (a, majority) (b, 5 genera) (see Table 1) Trachyrincidae Bathygadidae Moridae Euclichthyidae Merluccidae Melanonidae Steindachneriidae Gadidae Phycidae (part) Phycidae (part) Muraenolepididae Ranicepitidae Lotidae * and 3Hy *(Lyconus) MACROUROID FISHES 47 Uh sh Isc rv Fig. 34 Ventral gill-arch musculature of: A, a gadoid, Bathygadus melanobranchus; B, a macrourid, Nezumia hildebrandi. Ventral views. In other paracanthopterygians examined, rectus ventrales IV extends from the 3rd hypobranchial ligament to the 4th ceratobranchial, namely, the plesiomorphic acanthomorph condition. In nearly all macrouroids, as in the majority of acanthomorphs, the rectus communis runs from the urohyal to the 5th ceratobranchial. Exceptional taxa are Nezumia, Ventrifossa, Hymeno- cephalus, Odontomacrurus and Cynomacrurus , where the rectus communis runs from a dorsal tendon of the sternohyoideus to the 5th ceratobranchial. Among gadoids, the rectus communis almost always has a direct attachment to the sternohyoi- deus; in some taxa the rectus communis joins a tendinous aponeurosis (Merlucciidae, Fig. 36); in others, the fibres run into the body of the sternohyoideus and insert on an internal myocomma (Trachyrincidae, Fig. 33); and yet others, the rectus communis attaches directly to the urohyal (some Phycidae, Ranicepitidae, Muraenolepididae and Lotidae). However, unlike the condition in macrouroids and acanthomorphs it attaches to the anterior tip of the bone rather than to the lateral face of the keel. This different insertion site on the urohyal suggests that the attachment has been secondarily derived to that in acanthomorphs rather than representing a plesiomorphic condition (see Howes, 1988). The various conditions of ventral gill-arch muscles in macrouroids and gadoids are summarised in Table 2. Lauder (1983) considered a urohyal attachment of the rectus communis a synapomorphy for the ctenosquamates (Myctophiformes, Paracanthopterygii and Acanthopterygii). Because of its urohyal attachment, Lauder prefers the term 'pharyngohyoideus' for ctenosquamates rather than rectus communis. I have, however, continued the use of rectus communis for gadoids since here there is no, or at best, an indirect urohyal insertion. It could be argued that 'pharyngohyoideus' should be used for macrouroids, but here too there are exceptions to a urohyal insertion (see above and Table 2). 48 G. J. HOWES Following Lauder's assumption that a urohyal attachment for the rectus communis is a derived state it would appear that a direct linkage with the sternohyoideus represents a further derived condition. If it be assumed that this condition represented a less derived state, i.e. an evolutionary 'intermediate' position between a hypobranchial and urohyal attachment then it must also be assumed that the gadoids are less derived than myctophiforms, a conclusion unjustified on the basis of other synapomorphies (see Lauder & Liem, 1983). Howes (1987) considered the rectus communis-sternohyoideus linkage to be a synapomorphy uniting gadoids. It is now apparent that the feature also occurs in some macrouroids (see above). The possession by macrouroids of other synapomorphies lacking in gadoids makes it reasonable to assume, however, that the rectus communis-sternohyoideus linkage in the five macrouroid genera (see p. 47) is homoplastic. Lauder (1983: 26) notes that in euteleosts a rectus ventralis IV commonly originates from the urohyal, but that the muscle is mosaically distributed and has probably evolved independently in several lineages through the subdivision of the rectus communis. The lability of the rectus ventralis IV casts doubt upon its usefulness as a phylogenetic indicator and I have preferred to regard its association with the sternohyoideus in the Moridae, Merlucciidae and Lotidae as having been derived independently in those lineages; certainly there are no other synapomorphies that would suggest a close relationship of these taxa (see Howes, 1988). Further discussion of functional aspects of the ventral gill-arch musculature is given on pages 54-55. Dorsal gill-arch muscles Unlike the ventral gill-arch musculature, there is little variability in the dorsal gill-arch muscles among macrouroids apart from the angles at which the levatores are aligned between the gill-arches and the cranium, and in the size differences of some muscles. The basic pattern present in all macrouroid and gadoid taxa examined is: three levatores externi, two attaching to the 1 st and 2nd and the third to the 4th epibranchials (levator IV crosses the otic region of the cranium anteroventrally, medial to levatores I and II); two levatores interni, one attaching to the 2nd infraphayngobranchial, the other to the 3rd or 4th (Fig. 37); all these muscles originate from the intercalar and/or the upper part of the prootic. Transversi dorsales run from the 2nd, 3rd and 4th epibranchials to a midline raphe (that serving the 2nd and 3rd arches is a single element); an obliqus posterior connects the postero-medial surface of the 4th epibranchial with the 5th cerate-branchial (pharyngeal tooth-plate). In macrouroids the retractor dorsalis stems from the 3rd and 4th centra to insert tendinously on the medial rim of the 3rd pharyngobranchial. In some taxa, e.g. Nezumia (Fig. 38C), a ventral part of the retractor inserts on the rim of the 4th pharyngobranchial tooth-plate. Lauder (1983) noted that in the gadoid Pollachius, the retractor dorsalis inserts on both pharyngobranchials 3 and 4; I find similar sites of insertion in all 'advanced' gadoids, but in merlucciids, melanonids, morids and bathgadids the muscle inserts, as in most macrouroids on the medial rim of pharyngobranchial 3. In the Muraenolepididae, the retractor dorsalis inserts only on pharyngobranchial 4 (Howes, 1988). Lauder's (1983) and my own observations on acanthopterygians suggest that insertion on pharyngobranchial 3 is the plesiomorphic site of attachment and that one involving the 4th pharyngobranchial is the derived state. In this respect, the Muraenolepididae is the most derived group of gadoid taxa. Eye muscles Macrouroids and gadoids lack a posterior myodome, apparently a secondary loss (see Patterson, 1975: 544). The posterior eye muscles originate from a medial septum close to the floor of the parasphenoid and run almost lateral to their insertions on the eyeball. The accompanying figure of Gadomus (Fig. 39) exemplifies the condition in all macrouroids and gadoids examined (the eye muscles of Gadomus are narrower than in most other taxa). In some gadoids the posterior eye muscles originate from a small ossified protruberance of the parasphenoid. In Gaidropsarus , MACROUROID FISHES 49 Merluccius and Brosme the eye muscles pass medial to a vertical parasphenoid-pterosphenoid strut bordering the optic fenestra. The origin of the posterior eye muscles from the centre of the parasphenoid and their transverse orientation is considered a further synapomorphy uniting the Macrouroidei and Gadoidei (see Howes, 1988). rv4 Cb2 Hb1 Cb5 pci ica Fig. 35 Ventral gill-arch and hyoid muscles of a gadoid, Gadomus longifilis. Above, lateral; below, ventral view. Functional and ecological inferences Jaw protrusion mechanisms Recent recoveries of live macrouroids (Wilson & Smith, 1985) while encouraging, also indicate the difficulties of maintaining these fishes under laboratory conditions. Results so far discount the possibility of obtaining direct experimental data on jaw function. One is therefore obliged to derive hypotheses of functional mechanisms from morbid anatomical investigation. Those who have studied macrouroid anatomy are agreed that the jaws of most taxa are highly protrusible, the degree of protrusibility being a corollary of the length of the premaxillary ascending process (Okamura, 1970a,6; Marshall & Iwamoto, 1973: 479; Geistdorfer, 1975; McLellan, 1977; 50 G. J. HOWES Casinos, 1978; 1981). Several models of acanthomorph upper jaw protrusion mechanisms have been proposed, but most authors are in agreement that muscle A 1 plays a predominant part in this function (see Lauder, 1982: 280; Motta, 1984 for references to, and review of previous literature). Rosen ( 1 973) disagrees, however, believing that the development of an A 1 a or A 1 p division of the adductor mandibulae* . . . is not dependent on, or even correlated with, the existence of a protrusible jaw mechanism . . .'. According to Anker (1974) muscle Al serves not only to keep the mouth closed but possibly forces protrusion of the premaxilla. Gosline (1981: 15) thought the most likely cause of jaw protrusion in acanthomorph fishes is ligament IX, viz. that connecting the rostral cartilage with the maxilla. He hypothesised that as the maxilla twists around its articulation with the cranium, it pulls ligament IX anteroventrally, thus protruding the premaxilla which is attached to the rostral cartilage. This idea does not entirely explain protrusion, however, since the initial twisting of the maxilla must be explained in terms of muscular control. Is the maxilla pulled downward and inward passively by abduction of the lower jaw, or through direct action of muscles Ala and Al (3? McLellan (1977) accounted for upper jaw protrusion in macrouroids by the action of muscle A 1 , since she found that pulling on the maxillo-mandibular ligament along the line offeree exerted by Cb1 '9dh Vh rv4 re pci rv4 Fig. 36 Merlucciidae; ventral gill-arch and sternohyoid muscles of Merluccius merluccius in A, lateral and B, ventral views; the latter showing the partitions of the sternohyoideus. C, Macruronus magellanicus in lateral view. MACROUROID FISHES 51 tvd Eb1 obd Ie4 Fig. 37 Dorsal gill-arch muscles of a macrourid, Coelorinchus caribbaeus (dorsal view). the fibres of Al produced premaxillary protrusion. However, McLellan hypothesised that the macrouroid type of mechanism was '. . . a fundamentally different means of protruding the upper jaw from that of Bathygadus* , which she supposed to be produced by rotation of the maxillary head (i.e. as in Gosline's hypothesis). Geistdorfer (1975) gave a theoretical account of jaw movements in the macourine Ventrifossa occidentalis. For the most part, he considered jaw action to be similar to that in acanthopterygians and although stating that protrusion is limited by ligaments, he gave no account of arthrology. Casinos (1981) attempted an explanation of jaw protrusion in gadids (Gadidae) based on observation by high-speed cinematography, and in macrouroids by the extrapolation of these data. According to Casinos, there is no or little jaw protrusion in gadids, except Pollachius, whereas there is pronounced protrusion in macrouroids. Casinos devised a protrusion index (not to be confused with the protrusion index of Okamura, 1 9706; see below) which showed that although the gadid Pollachius has a high degree of protrusion, comparable with that of macrouroids, the 'macrouroid' Trachyrincus has a low protrusion index comparable with that of the gadids. Casinos' explanations of these apparent anomalies are confusing and rely on different sizes and moments of muscle Alp, and are also based on incorrect anatomical data. For example, Casinos explains the higher degree of protrusibility in macrouroids as due to an 'additional' rostro- maxillary ligament. However, a rostro-maxillary ligament (ligament VII, see p. 6) is present in all gadiforms and indeed all acanthomorphs (Stiassny, 1986). I would agree with Casinos (1981) that the restriction of muscle Al |3 to the same vertical plane as Ala gives the macrouroid upper jaw a degree of freedom greater than that of gadoids where the 52 G. J. HOWES vertical movement of the maxilla appears to be restricted by the obliquely and transversely angled A 1 P (particularly so in merlucciids where a short-fibred A 1 (3 runs from the palatine to the maxillary head thus affording the maxilla little downward movement). As noted above (p. 38) in some gadoids, seemingly those with restricted jaw protrusibility, the insertion of A 1 (3 is sited further anteriorly on the maxilla than in those with a greater degree of jaw freedom. In macrouroids the insertion of muscle A 1 P is on the ventromedial prominence posterior to the maxillary head. As noted above (p. 39) in gadoids the ventromedial process is less prominent and in more advanced taxa is reduced to a medial shelf, with the insertion of A 1 P shifted anteriorly to what is regarded as the most derived situation, namely to the symphysial border of the maxillary head. It was also noted above (p. 39) that the anterior insertion of A 1 P is correlated with the medial shift and enlargement of the entire muscle. What is possibly an important factor concerning differences in protrusion between macrouroids and gadoids is that in macrouroids muscle Ala is attached to the maxilla via the maxillo- mandibular ligament (Figs 1-4), whereas in gadoids Ala, although often associated with the maxillo-mandibular ligament is fastened to the jaw independently by its own tendon (Figs 9-20). Another factor which may affect the degree of protrusibility is the ligamentous connection between the maxillary head and the premaxillary ascending process. It was noted above (p. 7) that there are different forms of attachment between these bones in gadoids. The ligament (lig. XI) either attaches directly to the bone or via a cylindrical chondroid or fibrous element. The latter form of attachment (confined to the more plesiomorphic gadoids) suggests a greater degree of separation between the bones. In macrouroids the meniscus is a thick disc, loosely interposed between the maxillary head and the premaxilla, with ligament IX also attaching to the rostral cartilage (Fig. 28B & C). Thus, the only check on a total downward release of the premaxilla is ligament XI, which connects the maxilla to the ethmoid. If this ligament is cut in preserved specimens, there is a dramatic and passive jaw protrusion. Such is not the case in gadoids where muscle Al P runs obliquely from the suspensorium to the maxilla and acts as a brake, but there is a pronounced protrusion in those gadoids where A 1 P, like the macrouroids, lies in the same vertical plane as Ala (e.g. Bathygadus, Gadomus). Thus, it is suggested that muscle Alp plays an active role in both holding and rotating the maxilla and so effecting protrusion of the premaxilla as hypothesised by Alexander (1963) and Gosline (1981). A further point to be considered is that suggested by Casinos (1981) concerning the role of the labial 'ligament' (see p. 8). In Casinos' view in macrouroids the '. . . depression of the lower jaw transmits the force by means of the circumbuccal ligament' ( = labial ligament). Since a labial ligament is also highly developed in some gadoids (Bathygadus, Melanonus, Merluccius) presum- ably the same function applies in these taxa. Casinos' statement is somewhat ambiguous, however, particularly as he regards the ligament as extending around the mandibles whereas in fact, there is a separate ligament attached to each dentary (see Fig. 9). Nonetheless, the idea that the ligament plays a role in protruding the upper jaw appears valid when one considers the direct linkage of the ligament from the mandible to the premaxilla and maxilla and that it appears to be a contractile element (see p. 8). In this regard, some attention should be paid to the work of Otten (1983) who points out the importance of the maxillo-dentary, and the posterior premaxillary-maxillary ligaments in jaw protrusion. Otten (1983) recognised two groups of acanthopterygian fishes on the basis of jaw protrusion morphotypes: l.in which the maxilla rotates about its long axis and pushes the premaxilla anteriorly (exemplified by Percd). 2. in which the maxilla pushes, pulls and retains the premaxilla in protruded position (occurs in cichlids). He notes, however, that these two groups show some degree of overlap. Otten also makes the point that a shortening and steepening of the premaxillary ascending process coupled with a caudo-ventral shift in the insertion of muscle A 1 are factors responsible for increased biting force. Although Otten's hypotheses were directed toward cichlid jaw mechanisms, these principles also apply to macrouroids. Most macrouroids differ noticeably from gadoids in their long, steep premaxillary ascending processes and posterior insertion of Al P (see p. 38). MACROUROID FISHES 53 Motta ( 1 984) reviewed the history of ideas concerning the mechanics of teleost jaw protrusion and presented a classification of protrusion types but unfortunately disregarded paracanthopterygians in his account. Following Motta's classification the macrouroids and gadoids would seem to fall into three of his four categories, namely, type A: protrusion as a result of mandibular depression; type B: as a result of maxillary twist, and type C: as a result of neurocranial elevation (the degree of development ofepaxialis musculature in many gadoids suggest this). Motta also believes that the 'twisting maxilla model' has been overemphasised and that the 'mandible depression model' of jaw protrusion is probably the dominant type. Motta emphasised that the protruded mouth forms a circular orifice which is the most efficient configuration for employing suction feeding (see also Osse & Muller, 1980). A circular, protruded mouth profile is probably produced by all macrouroids and plesiomorphic gadoids (i.e. Bathygadus, Gadomus). Ie2 Fig. 38 Dorsal gill-arch muscles of: A, a gadoid, Gadomus longifilis; B, a macrourid, Nezumia hildebrandi (lateral views); C, Nezumia hildebrandi showing retractor dorsalis insertion (dorsal view). Hyoid-opercular mechanisms In discussing Bathygadus, McLellan (1977: 1026-7) states that '. . . the motion of the maxilla is mediated through a ligament of the interopercle . . .' and '. . . ligamentous connections between the interopercle, subopercle and opercle, and the contraction of the levator operculi muscle which runs from the cranium to the opercle.' Although the opercular series-jaw linkage serves to depress the mandible, its effect on moving the maxilla is doubtful. Furthermore, McLellan has overlooked the fact that Bathygadus, in 54 G. J. HOWES common with other gadoids, possesses a different jaw-opercular linkage system from that in other acanthomorphs (see p. 9). The interoperculum, instead of being the mediator between the mandible and suboperculum as in most acanthomorphs mediates between the mandible and preoperculum/hyomandibula. It should be noted that in most macrouroids and all gadoids the adductor operculi muscle inserts principally or entirely on the horizontal, opercular process of the hyomandibula; although the levator retains some attachment to the operculum, often its area of insertion is small and confined to the anterodorsal margin of the bone. The adductor operculi normally acts as an antagonist to the dilatator operculi and together they elevate the operculum. The consequences of the redirection of the adductor force to the hyomandibula are difficult to evaluate, but a rotational component directly coupled via the hyo- mandibular-interopercular ligament to the lower jaw is suggested. Another feature to note is that because of the anterior shift of the adductor operculi and the reduced insertion area of the levator operculi, there is a greater medial surface area available for the insertion of the hyohyoidei adduc- tores, and in the Phycidae, Lotidae and Muraenolepididae, for epaxial muscle as well (see p. 32). The presence in the Trachyrincidae of a mandibulohyoid ligament (Fig. 32) may be another indication of this taxon's closer relationships with gadoids than macrouroids (see Howes, 1987). However, as yet, too few comparative data exist on the distribution of a mandibulohyoid ligament to comment on its phylogenetic value. It is certainly present in most, if not all basal euteleosts and has been reported in clupeomorphs, stomiiforms and percomorphs (see Verraes, 1977; Otten, 1982 for specific examples). The ligament has also been reported by Holmquist (191 1) in the gadoid Gadus, a condition which I can confirm. Furthermore, the ligament is also present in other Gadidae examined and the Lotidae and Phycidae, but not in the Muraenolepididae. According to Verraes ( 1 977) a mandibulohyoid ligament is a feature of fishes having a long lower jaw and short interoperculum. In Trachyrincus the ligament attaches to the central part of the anterorhyal (Fig. 32) but in other gadoids it attaches to the posterior part of the anterohyal as in the percomorph Perca (see Verraes op. cit.). According to Lauder & Liem (1980: 389) in the salmonid Salvelinus the presence of the mandibulohyoid ligament possibly allows for another coupling to depress the lower jaw. Such may also be the case in Trachyrincus and other gadoids where it is present. Otten (1982: 47) believes that the occurrence of the mandibulohyoid ligament in various teleosts is homoplastic. 'Undoubtedly, ligaments are products of evolutionary pathways. Theoretically, redundancies may occur along these pathways, but it is more likely that ligaments evolve together with the whole apparatus in which they are functional . . .'. Finally, it should be noted that macrouroids and gadoids possess an elongate interhyal. Lauder & Liem (1980) drew attention to two functional roles of the inferhyal in feeding mechanics, namely: giving the hyoid an increased dorso ventral rotation and so providing greater orobranchial expansion giving the hyoid a posterodorsal movement. Although the above discussion has concentrated on the jaw mechanism in terms of feeding, the various modifications of the jaws and their couplings in gadoids possibly have a greater significance in respiratory function. After all, Smith & Hessler (1974) have pointed out that the respiratory rate for cod (Gadus) is over twenty times greater than that for a macrourid (Coryphaenoides). Experimental and functional analytic data are needed to assess the significance of the gadoid type of lower jaw coupling in which an interopercular-preopercular-hyomandibular ligament is introduced. Pharyngeal mechanisms Geistdorfer (1975) described and commented on the pharyngeal dentition of various macrouroid genera but paid no attention to the pharyngeal musculature. There is little variation in both the upper and lower pharyngeal muscles in the taxa examined (see p. 48). In general the posterior levatores are long, deep and angled at 45°, suggesting a high degree of forward movement of the upper pharyngeal apparatus. The functional significance of a sternohyoideus link with the rectus communis and recti ventrales MACROUROID FISHES 55 IV muscles is speculative. According to Lauder ( 1 983: 25) the shift of the anterior attachment of the rectus communis from hypobranchial 3 to the urohyal is a key specialisation in the evolution of euteleostean pharyngeal manipulation. A urohyal attachment of the muscle provides an axial rotation to the pharyngeal tooth plates. In gadoids the degree of axial rotation allowed by a direct sternohyoideus-rectus communis link would seem to be minimal but might facilitate asymmetrical activity of the lower pharyngeal tooth-plates. The reduction or absence oiobliqus ventrales muscles associated with the 1st and/or 2nd gill arch is probably correlated with a strong ligamentous attachment of the 1st gill-arch to the hyoid bar. n rei re ey Fig. 39 Eye muscles of a gadoid, Gadomus longifilis. Dorsal view of left eye. Trophic strategies The trophic ecology of macrouroids is poorly known, but it would seem that the majority of taxa feed on a broad spectrum of organisms (see Mauchline & Gordon, 1985). This trophic diversity is a consequence of the rather unspecialised organisation of the adductor and ventral gill-arch musculature described in this text. Okamura (1 9706) classified macrouroids into four groups according to their jaw and mouth type and devised a protrusion index (a percentage ratio of premaxillary ascending process length to that of the ramus), the application of which gives a higher figure to the smaller mouth. Okamura attempted to relate the index to ecological categories, those taxa with a low index being predomi- nantly nekton feeders, those with a high index being mostly benthic feeders. Okamura's groupings included Bathygadus and Gadomus, which are here considered to be gadoids and which according to his formula have a low protrusion index. Trachyrincus was not studied by Okamura, but application of his formula to this taxon gives it a protrusion index closer to Bathygadus and Gadomus than to any macrouroid. 56 G. J. HOWES McLellan (1977) also attempted to correlate head shape with trophic specialisations and believed she could match those taxa with long rostra (i.e. elongate nasals) to benthic habitats, whereas taxa with large, terminal mouths were associated with benthopelagic feeding. In McLellan's view Bathygadus and Coelorinchus represent two extremes of the Macrouridae with regard to ratio of mouth to head length, degree of jaw movement and expansion of orobranchial cavity. She considered Bathygadus to possess a prey-capture activity similar to that of 'other teleosts' with large, terminal mouths. However, as Lauder & Liem (1980: 387) point out, the feeding mechanisms of acanthopterygians (e.g. Percd) and basal euteleosts (e.g. Salvelinus) are quite different, involving different patterns of muscle activity. McLellan's reference to 'other teleosts' presumably refers to acanthopterygians, but the anatomical observations made in this text on the mode of jaw coupling in gadoids suggest that a somewhat different type of feeding pattern to that in other paracanthopterygians and in acanthopterygians might be operating. McLellan (1977: 1034) hypothesised that Coelorinchus and taxa with a protracted rostrum feed by using the rostrum as a sediment probe, as did Casinos (1978) for Trachyrincus. McLellan argues that this method of feeding prevents rapid forward swimming necessary for creating suction. As such she sees a high degree of muscular control in varying the protrusion angle of the upper jaw (elsewhere, however, she noted that Coelorinchus has 'weak musculature'). McLellan's assumption that rapid swimming is the only means of generating suction is not entirely correct, however, and she seems to be confusing inertial suction and ram feeding. For example, Lauder & Liem (1980) in their study of the salmonid Salvelinus note that although this fish is not primarily a suction feeder, inertial suction is created by varying the sequence of muscle activity, i.e. the activation of the levator arcus palatini prior to that of the levator operculi and the hyoid musculature. McLellan appears to be working from similar assumptions made by Weihs (1980) that higher swimming speeds extend the suction field further forward. However, this strategy would seem applicable only to predatory fish using strike tactics rather than hovering fish sucking food from the substrate whose principal feeding method would seem more likely to be inertial suction (see Liem, 1980). Both McLellan (1977) and Casinos (1978) have hypothesised that the rostrum of macrouroids and trachyrincids is used as a probe. Both authors have based their assumptions on the character- istic swimming mode of macrourids, shown in Marshall & Bourne (1964) to be head down and forming an angle of approximately 45° with the substrate. Isaacs & Schwartzlose (1975) have reported, from cinematographic evidence, macrouroids thrusting into the sediment and 'throwing a cloud of sediment through the gills'. Marshall (1979) believes this method of feeding enables macrourids to screen ooze-laden water by forcing it through the restricted first gill-slit. McLellan also supposed that the shorter snout of some species is probably more a sensory device than a mechanical probe. It should be emphasised that the rostrum is not part of the snout (i.e. ethmoid) but comprises the medially joined nasal bones which are trough-like, house many neuromasts and are fluid filled in life. Thus, a sensory function of the 'rostrum' seems a feasible idea. Casinos (1978) in his reconstruction of Trachyrincus probing and feeding from the substrate appears to overlook the fact that although the mouth may appear to be inferior in relation to the extended nasals, it is, in relation to the ethmoid, terminal. Furthermore, the lack of extended premaxillary ascending processes, the elongate jaws and the wide gape of the mouth (see p. 17) all point to Trachyrincus being benthopelagic rather than benthic in its feeding habits. Marshall & Merrett (1977: 489) point out that Trachyrincus '. . . has a marked preference for pelagic food'. As mentioned above, macrouroids display little morphological specialisation in their jaw musculature but from their trophic diversification (see Mauchine & Gordon, 1985) it would seem that they are capable of employing some specialised feeding habits. In this respect their feeding mechanisms resemble those of cichlids recognised by Liem (1980) as being suboptimilised. The hypothesis presented here and in Howes ( 1 988) that Bathygadus, Gadomus and Trachyrincus are not members of the Macrouroidei, but represent clades within the Gadoidei, negates to a certain degree the functional hypotheses advanced by McLellan (1977) and Casinos (1978; 1981). To those authors, the Macrouroidei was unquestionably a monophyletic group and so functional mechanisms identified among any of the included taxa would be considered homologous. The identification of a different jaw coupling in Bathygadus, Gadomus and Trachyrincus that is shared with gadoids necessitates a reappraisal of macrouroid trophic strategies. MACROUROID FISHES 57 Taxonomic and phylogenetic inferences The results of the character analyses in this study have already been utilised in another paper (Howes, 1988) to demonstrate the paraphyletic nature of the Macrouroidei. It has been established here and in Howes (1987) that four taxa formerly recognised as macrouroids, namely, Euclichthys, Bathygadus, Gadomus, and Trachyrincus share myological and arthrological synapomorphies with the Gadoidei, viz.: anterior expansion of the jaw adductor muscle Al reduction ofobliqui ventrales on the 1st and 2nd gill-arches rectus communis attaching aponeurotically to the sternohyoideus muscle possession of an interopercular-hyomandibular-preopercular ligament. As yet, there exists no comprehensive osteological account of Bathygadus and Gadomus, and their close affinities among gadoids are obscure. Howes (1988) tentatively recognised the Bathygadidae as the sister-group to the Moridae. The basis for this arrangement is the scale pattern shared between the two families. The scales are cycloid, with a reticulate pattern of sulci. According to Peabody (1931) the scale pattern of Bathygadus '. . . show no affinity for the Macrouridae and could easily be classified with either or both of the other families' (i.e. Gadidae and Bregmacerotidae). In Okamura's (19706) opinion, the 'bathygadine' scales are not secondarily derived from the ctenoid scales present in macrourids but are 'essentially primitive' and he draws attention to the '. . . striking resemblance to morids . . . which are characterised by the reticulate structure of ridges on the exposed area'. There are, regrettably, no derived myological features shared between the Bathygadidae and Moridae, the shared myomorphology being plesiomorphic for gadoids. The Bathygadidae was considered by Howes (1988) to represent a plesiomorphic lineage of gadoids. Work in progress has identified further synapomorphies that support the sister-group relationship of Bathygadus and Gadomus and the distinctiveness of the family (see also p. 18), but no further evidence has come to light which would suggest that the family is anything but plesiomorphic. Trachyrincus and Euclichthys each represent gadoid lineages, the former being recognised as the sister-group to all other gadoids, the latter as the sister-taxon of more advanced gadoid families (Howes, 1988). Intrarelationships of the Macrouroidei The attrition of the Macrouroidei by the removal of the Euclichthyidae leaves a single family in the suborder, the Macrouridae. In turn, this family has been reduced by the removal of the 'Bathygadinae' and Trachyrincinae' to two subfamilies, the Macrouroidinae and Macrourinae. The former contains two genera, Macrouroides and Squalogadus, the latter some 30 genera of diverse external morphology. The monophyly of the Macrouridae has been discussed by Howes (1988) and is supported by three derived characters; levator arcus palatini muscle enlarged and lying lateral to the jaw adductor musculature; trough-like nasal bones meeting in the midline; compressed, plate-like ethmoid. The laterally placed levator arcus palatini is a feature shared with the gadoids and is discussed in Howes (1988). The nasals of macrouroids are large, with a noticeable anteroventral curvature, the anterior border is often notched and the medial surface raised, contacting its partner along the midline. Enlarged, medially united nasals also occur in the gadoid family Trachyrincidae. Arguments for recognising the macrouroid and trachyrincid conditions as homoplastic are given in Howes (1988). The ethmoid region of macrouroid taxa comprises a deep, vertical, plate-like bone with an expanded base capping a cartilaginous bloc. The plate-like part of the ethmoid divides the posterior borders of the nasals and the anterior borders of the frontals. The dorsal margin of the ethmoid is confluent with the dorsomedial margin of the nasals, thus forming a long crest. The identity of the ossified crest-like cap of the ethmoid is doubtful, but it is easily detached from the ethmoid (mesethmoid) cartilage and, as there is no sign of perichondral ossification, it would appear to be a rostrodermosupraethmoid. 58 G. J. HOWES Apart from the derived nature of the levator arcus palatini, which is also shared with the Gadoidei, no myological synapomorphies have been identified which corroborate the monophyly of the Macrouridae. MACROUROIDINAE Three myological apomorphies have been identified in Squalogadus, one is also known to occur in Macrouroides but it has not been possible, with the nature of the material available (see p. 15), to observe the other two features. These characters are: protractor hyoidei entirely separated in the midline (present in Squalogadus and Macrouroides) intermandibularis lacking rectus ventralis IV joins rectus communis, by-passes and inserts on ceratobranchial 5. Okamura (19706) treated the group as a family on the basis of. . . notable differences from other macrouroids'. Indeed, from the characters he enumerates there is little doubt that the Macro- uroidinae possess a number of uniquely derived features, e.g. anterior and posterior ascending processes of the ethmoid (? rostrodermethmoid); division of the orbital fontanel; reduced, filamentous lateral ethmoid; deep 1st infraorbital; enlarged 5th infraorbital. Other features listed by Okamura (op. cit.} as defining the group, however, appear to be plesiomorphic, viz.: unmodified gill-rakers, unrestricted buccobranchial aperture, dorsal fin lacking spinous rays, flattened parietal, bar-like parasphenoid. It is more difficult to ascribe polarity to certain other characters, e.g. 'rostral' cartilage between ethmoid and parasphenoid (Okamura appears to confuse the rostral and mesethmoidal cartilages); lachrymal lacking ascending process (this could be a plesiomorphic condition or a reversal). MACROURINAE The characters given by Okamura (\91Qa,b) and Marshall (1973) as defining macrourines are, for the most part synapomorphic; they are: aperture between operculum and 1st gill-arch restricted by bucco-pharyngeal lining (Fig. 38B). olfactory bulbs lying close to nasal sac and within the nasal cavity spinule-bearing scales swimbladder (often) with drumming muscles and high number of retia mirabilia presence of light organs (in some taxa). The first three characters are common to all genera, but the other two only to some (see Fahay & Markle, 1984 for generic distribution of the light organs). No myological synapomorphies have been identified that support monophyly of the group. Within the Macrourinae three groups of genera can be distinguished on the basis of their jaw adductor muscle morphology; see pp. 12-13. These groups largely correspond with Okamura's (19706) scheme of generic relationships. Okamura's Coelorinchus group includes Coelorinchus , Coryphaenoides and Abyssicola and thus corresponds to my group la (p. 12). He also relates the genera Ventrifossa and Malacocephalus; Odontomacrurus and Cynomacrurus, and Echinomacrurus, Cetonurus and Sphagemacrurus; groupings which correspond with my group II (Table I). This group, however, is probably based on symplesiomorphies. Two groups of genera can be distinguished on the basis of their ventral gill-arch musculature, namely those where the rectus communis has an aponeurotic attachment to the sterno-hyoideus (as in gadoids) and where the muscle inserts on the urohyal. The latter group comprising the majority of macrourine taxa, the former includes Nezumia, Ventrifossa, Hymenocephalus, Odontomacrurus and Cynomacrurus. All these genera except for one (Nezumia) belong to the jaw muscle morphotype II. MACROUROID FISHES 59 Conclusions The salient points to emerge from this study of macrouroid and gadoid cranial muscles are: Anatomical The jaw adductor muscles of macrouroids are, in comparison with those of other 'paracanthoptery- gians', unspecialised. Muscle Alp is homologous with that so-called element in other acantho- morphs. M uscles A 1 a and A 1 p lie in the same vertical plane, an arrangement which seems to afford a large degree of jaw protrusion. The arrangement of macrouroid hyoid muscles are typically those of acanthopterygians, viz.: anterior attachment of the rectus communis to the urohyal (with the exception of five genera), rectus ventralis IV to the 3rd hypobranchial, and a well-developed complement of obliqui ventrales muscles. In gadoids, the rectus communis and rectus ventralis IV attach directly to the sternohyoideus and the obliqui ventrales are reduced on the 1 st or 1 st and 2nd gill-arches (in some bathygadids they are absent from the 1st arch). In common with acanthopterygians, macrouroids possess a mandibular-interopercular- subopercular ligamentous connection. In gadoids the linkage runs from the interoperculum to the hyomandibula, preoperculum or both. In both macrouroids and gadoids the adductor operculi muscle inserts wholly, or principally on the opercular process of the hyomandibula. Macrouroids, in common with 'lower' gadoids have the levator arcus palatini situated postero- lateral to the jaw adductor muscles. This is considered a derived condition and one allowing for a high degree of orobranchial expansion. Taxonomic and phylogenetic The Macrouroidei comprises a single family, the Macrouridae and two subfamilies, Macrourinae and Macrouroidinae. Although the monophyly of the Macrouridae is unsupported by myological characters, the presence of a maxillary-nasal ligament and a rostral cartilage attachment of ligament IX corroborates other synapomorphies. Monophyly of the Macrouroidinae is attested by ventral gill-arch and hyoid muscle synapo- morphies (pp. 43; 46). No myological characters have been identified as synapomorphic for the Macrourinae, although two jaw adductor muscle morphotypes are identified, one of which, pos- sessed by the genera Coelorinchus , Coryphaenoides, Abyssicola, Nezumia, Lionurus, Nematonurus and Chalinura is considered to be derived. Functional Previous functional hypothesis of macrouroid feeding mechanisms were based on the assumption that the group is monophyletic. The studies of McLellan ( 1 977) and Casinos ( 1 978; 1 98 1 ) included taxa which properly belong to the Gadoidei. Indications from jaw-opercular linkages and muscle insertions are that gadoids employ a different feeding mechanism from that of macrouroids. The extrapolation of data gleaned from functional studies of acanthopterygian fishes to 'paracanthopterygians' is a flawed approach. Ecological Hypotheses of trophic strategies have also suffered by the tacit assumption of macrouroid monophyly. The ecological and evolutionary scenarios of McLellan (1977) and Casinos (1978) must be reassessed in the light of the revised classification of macrouroids and gadoids (Howes, 1988; Howes & Crimmen, in prep.). That the monophyly of a group so seemingly highly characterised as the Macrouroidei should be questioned is a warning that functional and ecological hypotheses must be used guardedly and are valid only for groups whose monophyly is well corroborated. According to Lauder's (1981) 'decoupling hypothesis' there is a phylogenetic increase in the number of biomechanical components and their pathways. Thus the derived sister taxon of a group 60 G. J. HOWES displays greater diversity and 'constructional flexibility' than its plesiomorphic sister taxon. The Gadoidei are hypothesised to be the derived sister group of the Macrouroidei (see Howes, 1988), and as such Lauder's hypothesis is borne out (in part) since the macrouroids lack what might be the more manipulative functions of the upper jaws possessed by gadoids. There is also a more complex arrangement of the hyoid and ventral gill-arch musculature in gadoids, although it is arguable whether a greater range of function is achieved (see p. 54). Only a complete comparative functional analysis of feeding mechanisms of taxa in the two groups will support Lauder's claim. The intrarelationships of the morphologically diverse genera assigned to the Macrourinae have yet to be worked out cladistically. Myological characters have not been rewarding in this regard, and synapomorphies must be sought in other soft-anatomical (particularly in the structure of the light organs) and skeletal features. Acknowledgements I am most grateful to Humphry Greenwood, N. B. Marshall, Nigel Merrett and Alwyne Wheeler for their critical reading of the manuscript and their many helpful suggestions for its improvement. I am particularly indebted to Nigel Merrett of the Institute of Oceanographic Sciences, for supplying several macrouroid specimens for dissection and for much helpful discussion. Special thanks are due to my colleagues Mandy Holloway and Chris Sanford for preparing radiographs and cleared and stained specimens. References Alexander, R. McN. 1969. The functions and mechanisms of protrusible jaws of some acanthopterygian fishes. Journal of Zoology, London 151: 43-64. Allis, E. P. 1897. The cranial muscles and cranial and first spinal nerves in Amia calva. Journal of Morphology 12: 487-772. Anker, G. Ch. 1974. Morphology and kinetics of the head of the stickleback Gasterosteus aculeatus. Trans- actions of the Zoological Society of London 32: 311-416. Casinos, A. 1978. The comparative feeding mechanism of Gadidae and Macrouridae. 1. Functional morphology of the feeding apparatus. Gegenbaurs Morphologisches Jahrbuch, Leipzig, 124 (3): 434-449. - 1981. The comparative feeding mechanism of Gadidae and Macrouridae. II. Mechanics of the feeding action. Gegenbaurs Morphologisches Jahrbuch, Leipzig, 127 (2): 246-262. Cohen, D. M. 1984. Gadiformes: overview. In Ontogeny and systematics of fishes Special Publication No. 1 of the American Society of Ichthyologists and Herpetologists: 259-265. Dietz, P. A. 1921 . Uber die systematische Stellung der Gadidae. Zugleich Nr. 2 der 'Beitrage zur Kenntnis der Kiefer- und Kiemenbogenmuskulatur der Teleostier'. Anatomische Anzeiger 144: 56-64. Fahay, M. P. & Markle, D. F. 1984. Gadiformes: development and relationships. 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Report on the Japanese macrouroid fishes collected by the United States fisheries Steamer 'Albatross' in 1906, with a synopsis of the genera. Proceedings of the United States National Museum 51: 135-214. Gosline, W. A. 1963. Considerations regarding the relationships of the percopsiform, cyprinodontiform and gadiform fishes. Occasional Papers of the Museum of Zoology, University of Michigan No. 629: 1-38. - 1981. The evolution of the premaxillary protrusion system in some teleostean fish groups. Journal of Zoology, London 193: 1 1-23. Greenwood, P. H. 1977. Notes on the anatomy and classification of elopomorph fishes. Bulletin of the British Museum of Natural History (Zoology) 32: 65-102. MACROUROID FISHES 61 - 1985. Notes on the anatomy and phyletic relationships of Hemichromis Peters, 1858. Bulletin of the British Museum (Natural History) (Zoology) 48 (3): 131-171. Holmquist, O. 1911. Studien in der von den Nerven trigeminus und facialis innervierten Muskulatur der Knochen fische. 1. Die Trigemino-Facialis-Muskulatur bei Gadus callarias L. II. Zur vergleichende Morphologic der Mm. Intermandibularis, protractor hyoidei und hyohyoideus. Acta Universitatis Lundensisl (7): 1-79. Howes, G. J. 1984«. A review of the anatomy, taxonomy and biogeography of the African neoboline cyprinid fishes. Bulletin of the British Museum (Natural History) (Zoology) 47 (3): 151-185. — 19846. The cranial muscles of loricarioid catfishes, their homologies and value as taxonomic characters (Teleostei: Siluroidei). Bulletin of the British Museum (Natural History) (Zoology) 45 (6): 309-345. — 1985. Cranial muscles of gonorynchiform fishes, with comments on generic relationships. Bulletin of the British Museum (Natural History) (Zoology) 49 (2): 273-303. — 1987. The palatine bone and its associations in gadoid fishes. Journal of Fish Biology 31: 625—637. 1988. Phylogenetic relationships of macrouroid and gadoid fishes based on cranial myology and arthrology. WOGADS Symposium. Contributions in Science. Los Angeles County Museum. (In press). Inada, T. 1 98 1 . Studies on the merlucciid fishes. Bulletin of the Far Seas Fisheries Research Laboratory, no. 1 6: 1-172. Isaacs, J.D. & Schwartzlose, R. 1975. Active animals of the deep-sea floor. Scientific American 233 (4): 84-91 . lawmoto, T. & Stein, D. L. 1973. A systematic review of the rattail fishes (Macrouridae: Gadiformes) from Oregon and adjacent waters. Occasional Papers of the California Academy of Sciences 111: 1-79. Lauder, G. V. 1981. Intraspecific functional repertoires in the feeding mechanism of the characoid fishes Lebiasina, Hopliasand Chalceus. Copeia 1981: 154-168. — 1982. Patterns of evolution in the feeding mechanism of actinopterygian fishes. American Zoologist 22: 275-285. 1983. Functional design and evolution of the pharyngeal jaw apparatus in euteleostean fishes. Zoological Journal of the Linnean Society 77 (1): 1-38. Lauder, G. V. & Liem, K. F. 1 980. The feeding mechanism and cephalic myology of Salvelinusfontinalis; form, function and evolutionary significance. In: E. K. Balon (Ed.) Charrs: Salmonid fishes of the genus Salvelinus: 365-390. - 1983. The evolution and interrelationships of the Actinopterygian fishes. Bulletin of the Museum of Comparative Zoology, Harvard 150 (3): 95-197. Liem, K. F. 1980. Acquisition of energy by teleosts: Adaptive mechanisms and evolutionary patterns. In: M. A. Ali (Ed.) Environmental physiology of fishes: 299-334. McLellan, T. 1977. Feeding strategies of the macrourids. Deep Sea Research 24: 1019-1036. Marshall, N. B. 1965. Systematic and biological studies of the Macrourid fishes (Anacanthini-Teleostii) Deep Sea Research 12: 299-322. — 1966. The relationships of the anacanthine fishes Macruronus, Lyconus and Steindachneria. Copeia 1966: 275-280. — 1973. Genus Coryphaenoides. Family Macrouridae. Memoir, Sears Foundation for Marine Research 1. Fishes of the western North Atlantic (6): 565-580. — 1979. Developments in deep-sea biology. 566 pp. — & Bourne, D. W. 1964. A photographic survey of the benthic fishes of the Red Sea and Gulf of Aden. Bulletin of the Museum of Comparative Zoology, Harvard 132: 223-244. — & Cohen, D. M. 1973. Order Anacanthini (Gadiformes). Characters and synopsis of families. Memoir, Sears Foundation for Marine Research 1. Fishes of the western North Atlantic (6): 479-495. & Merrett, N. R. 1977. The existence of a benthopelagic fauna in the deep-sea. In: A voyage of Discovery (Ed. M. Angel): 483-497. Mauchline, J. & Gordon, J. D. M. 1 985. Trophic diversity in deep-sea fish. Journal of Fish Biology 26: 527-535. Merrett, N. R., Sazonov, Y. I. & Scherbachev, Y. N. 1983. A new genus and species of rattail fish (Macrouridae) from the eastern North Atlantic and eastern Indian Ocean, with notes on its ecology. Journal of Fish Biology 22:549-661. Motta, P. J. 1984. Mechanics and functions of jaw protrusion in teleost fishes: a review. Copeia 1984: 1-18. Okamura, O. 1970a. Macrourina. Fauna Japonica. Japanese Biogeographical Society, Tokyo, 216 pp. - 19706. Studies on the Macrouroid fishes of Japan— morphology, ecology and phylogeny. Reports of the Usa Marine Biological Station, Kochi University 17 (1-2): 1-179. Osse, J. W. M. & Muller, M. 1980. A model of suction feeding in teleostean fishes. In: M. A. Ali (Ed.) Environmental Physiology of fishes: 335-352. Otten, E. 1981. Vision during growth of a generalized Haplochromis species: H. elegans Trewavas 1933 (Pisces, Cichlidae). Netherlands Journal of 'Zoology 31 (4): 650-700. 62 G. J. HOWES - 1982. The development of a mouth-opening mechanism in a generalized Haplochromis species: H. elegans Trewavas 1933 (Pisces, Cichlidae). Netherlands Journal of Zoology 32 (1): 31-48. 1983. The jaw mechanism during growth of a generalized Haplochromis species: H. elegans Trewavas 1933 (Pisces, Cichlidae). Netherlands Journal of Zoology 33(1): 55-98. Parr, A. E. 1946. The Macrouridae of the western North Atlantic and central American seas. Bulletin of the Bingham Oceanographic Collection 10 article 1: 1-93. Patterson, C. 1975. The braincase of pholidophorid and leptolepid fishes, with a review of the actinopterygian braincase. Philosophical Transactions of the Royal Society of London B 269 (899): 275-579. Peabody, E. B. 193 1 . Scales of fishes of the order Anacanthini. University of Colorado Studies 18 (3): 1 33-1 50. Rosen, D. E. 1962. Comments on the relationships of the North American cave fishes of the family Amblyopsidae. American Museum Novitates 2109: 1-35. - 1973. Interrelationships of higher euteleostean fishes: In: Interrelationships of fishes. Eds Greenwood, P. H., Miles, R. S. & Patterson, C. Supplement No. 1 to the ZoologicalJournal of the Linnean Society 53: 397-513. & Patterson, C. 1969. The structure and relationships of the paracanthopterygian fishes. Bulletin of the American Museum of Natural History 141 (3): 357-474. Smith, K. L. & Messier, R. R. 1974. Respiration of benthopelagic fishes: In situ measurements at 1230 Metres. Stiassny, M. L. J. 1981 . Phylogenetic versus convergent relationship between piscivorous cichlid fishes from Lakes Malawi and Tanganyika. Bulletin of the British Museum (Natural History) (Zoology) 40 (3): 67-101 . - 1986. The limits and relationships of the acanthomorph teleosts. Journal of Zoology, London (B) 1: 411-460. Tchernavin, V. V. 1953. The feeding mechanism of a deep-sea fish Chauliodus sloani Schneider. British Museum (Natural History) 101 pp. Verraes, W. 1 977. Postembryonic ontogeny and functional anatomy of the ligamentum mandibulo-hyoideum and the ligamentum interoperculo-mandibulare, with notes on the opercular bones and some other cranial elements in Salmo gairdneri Richardson, 1836 (Teleostei: Salmonidae). Journal of Morphology 151 (1): 111-120. Weihs, D. 1980. Hydrodynamics of suction feeding offish in motion. Journal of Fish Biology 16: 425-433. Wilson, R. R. & Smith, K. L. 1985. Live capture, maintenance and partial decompression of a deep-sea genadier fish (Coryphaenoides acrolepis) in a hyperbaric trap-aquarium. Deep Sea Research 32 (12): 1571-1582. Winterbottom, R. 19740. A descriptive synonymy of the striated muscles of the Teleostei. Proceedings of the Academy of Natural Sciences, Philadelphia 125: 225-317. — 1974£. The familial phylogeny of the Tetraodontiformes (Acanthopterygii: Pisces) as evidenced by their comparative myology. Smithsonian Contributions to Zoology 155: 1-210. Manuscript accepted for publication 18 November 1986 British Museum (Natural History) The birds of Mount Nimba, Liberia Peter R. Colston & Kai Curry-Lindahl For evolution and speciation of animals Mount Nimba in Liberia, Guinea and the Ivory Coast is a key area in Africa representing for biologists what the Abu Simbel site in Egypt signified for archaeologists. No less than about 200 species of animals are endemic to Mount Nimba. Yet, this mountain massif, entirely located within the rain-forest biome, is rapidly being destroyed by human exploitation. This book is the first major work on the birds of Mount Nimba and surrounding lowland ram forests. During 20 years (1962-1982) of research at the Nimba Research Laboratory in Grassfield (Liberia), located at the foot of Mount Nimba, scientists from three continents have studied the birds. In this way Mount Nimba has become the ornithologically most thoroughly explored lowland rain-forest area of Africa. The book offers a comprehensive synthesis of information on the avifauna of Mount Nimba and its ecological setting. During the 20 years period of biological investigations at Nimba this in 1962 intact area was gradually opened up by man with far-reaching environmental consequences for the rain-forest habitats and profound effects on the birds. Therefore, the book provides not only a source of reference material on the systematics, physiology, ecology and biology of the birds of Mount Nimba and the African rain-forest, but also data on biogeography in the African context as well as conservation problems. Also behaviour and migration are discussed. At Nimba a number of migrants from Europe and/or Asia meet Afrotropical migratory and sedentary birds. Professor Kai Curry-Lindahl has served as Chairman of the Nimba Research Labc Committee since its inception in 1962. Peter Colston is from the Subdepartment of Ornithology, British Museum (Natural History), Tring, and Malcolm Coe is from the Animal Ecology Research Group, Department of Zoology, Oxford. 1986, 129pp. Hardback. 0 565 00982 6 £17.50. Titles to be published in Volume 54 The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences. By Gordon J. Howes A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles. By Keith H. Hyatt & Rowan M. Emberson A revision of Haplocaulus Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives. By Alan Warren Other titles to follow r. Dorset 28APJ Bulletin of the [,. British Museum (Natural History) A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles Keith H. Hyatt & Rowan M. Emberson Zoology series Vol 54 No 2 28 April 1988 The Bulletin of the British Museum (Natural History), instituted in 1949, is issued in four scientific series, Botany, Entomology, Geology (incorporating Mineralogy) and Zoology, and an Historical series. Papers in the Bulletin are primarily the results of research carried out on the unique and ever-growing collections of the Museum, both by the scientific staff of the Museum and by specialists from elsewhere who make use of the Museum's resources. Many of the papers are works of reference that will remain indispensable for years to come. Parts are published at irregular intervals as they become ready, each is complete in itself, available separately, and individually priced. Volumes contain about 300 pages and several volumes may appear within a calendar year. Subscriptions may be placed for one or more of the series on either an Annual or Per Volume basis. Prices vary according to the contents of the individual parts. Orders and enquiries should be sent to: Publications Sales, British Museum (Natural History), Cromwell Road, London SW7 5BD, England. World List abbreviation: Bull. Br. Mus. nat. Hist. (Zool.) © Trustees of the British Museum (Natural History), 1988 The Zoology Series is edited in the Museum's Department of Zoology Keeper of Zoology : Mr J. F. Peake Editor of Bulletin : Dr C. R. Curds Assistant Editor : Mr C. G. Ogden ISBN 0 565 05038 9 ISSN 0007 1 498 Zoology series Vol54 No. 2 pp 63-1 25 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 28 April 1988 A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles / 2 8 APS 1988 j Keith H. Hyatt k Department of Zoology, British Museum (Natural History), Cromwell Road, London, SW7 5BD Rowan M. Emberson Department of Entomology, Lincoln College, Canterbury, New Zealand* This paper is dedicated to Ernest Browning, M.B.E., who died on the 1st September 1987, aged 91 Contents Synopsis. Introduction ....... Material examined ...... Morphology Classification Genus Geholaspis Berlese s. lat. Genus Dissoloncha Falconer. Genus Macrocheles Latreille Genus Glyptholaspis Filipponi & Pegazzano . Genus Holostaspella Berlese .... Taxonomic Summary ..... Acknowledgements References BRITISH MUSED! (NATURAL HISTORY) 28 APR ^983 PRESENTED 63 63 64 64 68 69 76 78 114 118 122 123 123 Synopsis Thirty-two species of mites of the family Macrochelidae are now known to occur in the British Isles. Descriptions are given for the nine species, including one new to science, recorded for the first time, and for other selected species. Habitat and distributional data are given and keys to the genera and species for adults are provided. Two neotypes and four lectotypes are newly designated. The genus Dissoloncha Falconer, 1923 is resurrected and four specific names are newly synonymized. Introduction It is over thirty years since the publication by Evans & Browning (1956) of their work on the British Macrochelinae (now generally treated as the family Macrochelidae). This work was a turning point in the taxonomic study of the Macrochelidae. For the first time it was relatively easy to identify many of the common macrochelids, not only of the British Isles but also of northern Europe and to some extent further afield. It was also the first substantial revisionary work on European macrochelids since that of Berlese (1918). In the intervening time our knowledge of all aspects of macrochelids has increased rapidly. Their role as predators of the eggs and larvae of synanthropic flies has been fully realised, and steps taken to make practical use of this knowledge. In connection with this, detailed studies of the biology of "The first part of this work was done whilst on leave based at the British Museum (Natural History). Bull. Br. Mm. nat. Hist. (Zool.) 54 (2): 63-125 Issued 28 April 1988 63 64 K. H. HYATT & R. M. EMBERSON some species have been undertaken. Taxonomic work has proceeded at all levels within the family both in Europe and elsewhere. Generic concepts have changed, many new species have been described and the type specimens of old species re-examined. Groups of closely related species have been recognised and in some cases distinguished with the help of breeding experiments. It therefore seems appropriate to apply this new understanding of the group to the fauna of the British Isles, particularly as part of the acarine collection of the Rev. J. E. Hull, containing some of his type material of British macrochelids, has been found and is now housed in the Arachnida collections of the British Museum (Natural History). Evans & Browning (1956) recorded and gave descriptions of twenty-three species of Macrochelidae. It now seems likely that at least one and probably two of the species recorded by them are not members of the British fauna. The inclusion of these species was based on old records and no British material was seen by Evans & Browning or in the extensive collections examined in the present study. The names of seven previously recorded species must be changed. In all, nine species, one previously undescribed, are reported from the British Isles for the first time. Since the main purpose of this work is to bring our knowledge of the British Macrochelidae up to date, species described in detail by Evans & Browning are not redescribed here although amend- ments are made where necessary. However, species not previously recorded are described fully. All the species are figured; those previously recorded are illustrated, with some minor amendments, from the original figures of Evans & Browning, since that paper has been out of print for many years, whilst those recorded for the first time are newly illustrated. Notes on morphology and classification are included and keys to genera, species groups and species are provided. Material examined The primary source of material on which this study is based is the large collection of Macrochelidae preserved in the collections of the British Museum (Natural History). Over five and a half thousand specimens have been examined. All the 'locality information for the British Isles is based on this material, except where otherwise noted. In addition, macrochelid material in the Berlese Collection, Istituto Sperimentale per la Zoologia Agraria, Firenze, was examined. This was mainly for type material of species occurring in the British Isles, but much other material, particularly of European species, was also examined. Type material of species described by Bregetova & Koroleva (1960) was borrowed from the Institute of Zoology of the Academy of Sciences, in Leningrad and parts of the extensive collection of North American and tropical macrochelids in the Department of Entomology, Oregon State University, Corvallis, were also examined. The following abbreviations appear in the text: BMNH: British Museum (Natural History) ISZA: Berlese Collection, Istituto Sperimentale per la Zoologia Agraria, Firenze, Italy. ZINL: Institute of Zoology, Academy of Sciences, Leningrad, U.S.S.R. OSUC: Entomology Department, Oregon State University, Corvallis, U.S.A. Morphology A detailed study of the morphology of Glyptholaspis confusa (Foa) has been published by van der Hammen (1964), but not all of his interpretations would be accepted by all workers on Mesostigmata (Evans & Till, 1965). In general the terminology used here follows Evans & Till (1979). MACROCHELIDAE OF THE BRITISH ISLES 65 Idiosoma Dorsum The system of setal nomenclature used here was first developed by Lindquist & Evans (1965) for the Ascidae and has since been widely applied to other groups of gamasine Mesostigmata. The relationships between the setal nomenclature used by Evans & Browning ( 1 956) and that used here are shown in Figure 1A and further compared in Table 1 with those of Bregetova & Koroleva (1960) and Hirschmann (1957), both of which have been used by various authors. More recently Halliday ( 1 986) has compared in detail the various systems of dorsal setal nomenclature used in the Macrochelidae and has advocated that of Lindquist & Evans (1965) for general application in this family. The number of setae on the dorsal shield in British species is remarkably constant, varying from 56-60, but usually expressed as 28 regularly arranged pairs (Fig. 1 A). The major exception to this arrangement is in the opacus species group of Macrocheles (the former genus Macrholaspis Oudemans) which always have setae J3 present instead of J2 and, in addition have 1-4 setae, often asymmetrically arranged between j6 and J3. M. montanus (Willman) has both J2 and J3 present giving 29 pairs and Glyptholaspis confusa typically has one or two small asymmetric setae between j6 and J2. The situation in Geholaspis Berlese is more difficult to interpret. It has the usual 28 pairs of setae buty'5 andy'6 appear to have migrated posteriorly from their usual positions. Venter The form and ornamentation of the sternal shield have been used as one of the main characters to distinguish the genus Glyptholaspis Fillipponi & Pegazzano from Macrocheles, whilst the pattern of lines described by Berlese (1918) is very useful in distinguishing species and species groups of Macrocheles (Fig. 1 B). The setal nomenclature system of Lindquist & Evans (1965) is used for the opisthogaster. The setation of the ventrianal shield is now known to be more variable than previously realised. Holostaspella Berlese may have three or four pairs of setae, Zvl lying either on or off the ventrianal shield. In all British species it is on the shield (Fig. 22D). The opacus species group of Macrocheles, previously recognised as a separate genus, Macrholaspis, largely on the basis of only having Jv2 Table 1 Chaetotaxy of the dorsal shield. Dorsocentral series L&E E&B B&K H Mediolateral series L&E E&B B&K H Lateral series L&E E&B B&K H Marginal series L&E E&B B&K H J2 J3 J4 J5 J6 Dl D2 D3 D4 D5 D6 J2 D7 J3 — Fl F3 V Dl D2 D4 D6 D7 il si 12 i3 14 i5 Jl J2 zl z2 z4 z5 z6 Zl Z2 Anterior region (podonotum) Ml M2 L2 M3 M4 F2 rl Tl s2 Sc zl D3 z2 II z3 s2 LI SI Posterior region (opisthonotum) L4 L5 S4 S6 Zl Z2 J5 D8 S8 J5 Z4 L6 S7 Z3 Z5 MglO Mil S5 r3 s4 Mg3 S2 s5 s5 L3 S3 s6 s6 Mg5 M4 s7 51 Mg6 M6 SI 52 Mg7 M8 S2 54 Mg8 M9 S3 55 Mg9 M10 S4 r2 r3 r4 Mgl Ml r4 Mg2 M2 r5 Mg4 M3 r7 L & E = Lindquist & Evans ( 1 965) B & K = Bregetova & Koroleva ( 1 960) E & B = Evans & Browning (1956) H = Hirschmann (1957) 66 K. H. HYATT & R. M. EMBERSON Evens t Browning 1956 Prtstnt work, after Lindquist I Evans, 1965 Mg1 2 pore 1 linea Eingulata linea arcuata linea oblique anterior linea media transverse pore 2 linea oblique posterior areae punctatae B Fig. 1 A dorsal chaetotaxy of Macrocheles sp. comparing the systems of Evans & Browning (1956) and the present work, after Lindquist & Evans (1965); B structure and ornamentation of the sternal shield in the Macrochelidae, based on Berlese (1918). MACROCHELIDAE OF THE BRITISH ISLES 67 and Jv3 on the ventrianal shield, has been found to be much more variable. Species exist without any of the Jv series on the sclerotised part of the venter (Fig. 1 3B) and others with Jv3, or Jv2 and 3 or Jvl-3 on the ventrianal shield (Fig. 3B). The distribution and type of pore-like structures in the Gamasina has been studied by Athias- Henriot (1969). The inguinal pores occur in the anterolateral corners of the ventrianal shield in Geholaspis and Dissoloncha Falconer, but are free on the membrane in Macrocheles, Glyptholaspis and Holostaspella. In the genus Glyptholaspis all males have holoventral shields, whilst in Dissoloncha the males have separate sternogenital and ventrianal shields. In Macrocheles and Holostaspella the males have either separate sternogenital and ventrianal shields or holoventral shields. Gnathosoma The terminology used is that of Evans & Till (1979). The chaetotaxy of the pedipalps has been investigated by Evans (1964). The numbers and positions of setae in the Macrochelidae are quite typical for the free-living Gamasina having 2-5-6-15-15 setae on the trochanter, femur, genu, tibia and tarsus respectively. The form and length of the brush-like outgrowths of the cheliceral arthrodial membrane are important at the generic level, although they do not vary much in the British species. The form of the cheliceral dorsal seta is of use in distinguishing species groups in Macrocheles. The shape of the gnathotectum is of importance at the generic level and for species groups in Macrocheles (Figs 2B, 7B, 13B). Legs Leg I is without ambulacral apparatus in all British species although species with pulvilli in the adults and pulvilli and claws in the immature stages have been assigned to the macrochelid genus Neopodocinum Oudemans by Krantz (1965). The leg setation of the Gamasina has been studied by Evans (1963). Macrochelids have a remarkably constant pattern of leg setation (Table 2). The only variation known in species from the Table 2 Numbers of setae on leg segments in the Macrochelidae. legs I II III IV coxa 222 1 000 0 trochanter 1---1 1---1 1---1 1---1 333 3 or 1---1 550 3 femur 2—2 2---1 1---1 1---1 432 1 32 32 22 22 genu 2--, --2 2--, --2 1--, --1 1--, --0 11 11 10 10 2 2 or 1-- --1 1 0 32 22 12 12 tibia 2--, --2 2--, --2 1--, --1 1--, --1 21 11 11 11 tarsus 18 18 18 68 K. H. HYATT & R. M. EMBERSON British Isles is in genu IV which has seven setae in M. subbadius, seta/?/, being present, instead of the usual six setae. This condition is also found in a few other species of Macrocheles and in the mainly tropical genera Holocelaeno Berlese and Neopodocinum. The genus Neopodocinum also has only four setae on trochanter III instead of the usual five due to the absence of one of the ventral setae. The distribution of spurs on the legs of male macrochelids is useful at the generic level; Glyptholaspis having spurs on legs II, III and IV, Macrocheles on legs II and often on legs IV and Holostaspella only on femur II, if at all. The form and precise distribution of these spurs is also useful in distinguishing closely related species, as are the spurs on leg II of female Holostaspella. Spermathecal structures Recently there have been a number of studies on the method of insemination of gamasine mites and of the spermathecal structures. The information derived from this work has proved to be useful at all levels of classification in the Gamasina. There appear to be two basic types of insemination (Athias-Henriot, 1968), vaginal, or toco- spermic, in which insemination is via a median endogynal, cuticular sac and podospermic where it is via tubular cuticular invaginations associated with the bases of legs III or IV. In the British Gamasina, tocospermic insemination is found only in the families Parasitidae, Epicriidae and Zerconidae. Podospermic insemination is characteristic of other gamasine groups. Within the podospermic group two main variations of the spermathecal structures (Michael's organ) are found, the tubular cuticular invaginations may lead either to paired terminal organs (phytoseiid type) or to a single median organ (laelapid type). Paired spermathecal structures are found in the Phytoseiidae and some genera of the Ascidae (sensu Lindquist & Evans, 1965), median spermathecal structures are found in most other families of the Gamasina, including the Macrochelidae. The spermathecal complex has been described for a number of species of European Macro- chelidae (Petrova, 1960; Costa, 1966a, 1967; Athias-Henriot, 1968) and provides good taxonomic characters at the generic and species level. The opening, or solenostome, of the tubulus annulatus, is always on the posterior basal margin of coxa III. In Macrocheles the infundibulum is well developed, the rami are usually short and the sacculus generally consists of two, more or less, spherical lobes broadly joined by a tubular section which gives rise to the corniculum posteriorly (Fig. 14F). In a few species the sacculus is unlobed, spherical and merges into the corniculum to give an overall pear-shaped median organ (Costa, 1967). Dissoloncha superbus has a very different sacculus from all other species of Macrochelidae: it is large, more or less spherical and strongly convoluted. Classification Evans & Browning (1956) recognised two subfamilies of Macrochelidae, the Macrochelinae Tragardh, 1949 (sic) and the Areolaspinae Tragardh, 1952, based mainly on the patterns effusion of the ventral shields. Subsequently Evans (1956), in a radical reappraisal of the classification, taking into account the great variation shown in the ventral shields, proposed a new classification based on characters of the peritreme, gnathotectum, genital sclerotisation and gnathosoma. In this classification the family was split into the Macrochelinae Tragardh (sic) and the Parholaspinae Evans 1956 (Areolaspis having been shown to be closely allied to other macrocheline genera). Krantz ( 1 969) regarded the two groups as distinct families, as have most subsequent authors, but see Karg (1971) and Krauss ( 1 970). Evans' ( 1 956) definition of the group, however, remains almost unchanged. About sixteen genera of Macrochelidae are distinguished at present, of which only five occur in the British Isles. There has been some change in generic limits affecting these genera during the last thirty years. Macrholaspis is now generally regarded as a synonym of Macrocheles (Krantz, 1962) following MACROCHELIDAE OF THE BRITISH ISLES 69 recognition of species closely related to the type species, Gamasus opacus C. L. Koch, with three pairs of setae on the ventrianal shield and lacking denticulate margins to the dorsal shield. The genus Glyptholaspis has been split off from Macrocheles to contain several species, including two formerly confused under the name M. plumiventris Hull, in the British fauna. The main distinguishing features of the genus are the posterior extension of the sternal shields, the crenulate reticular pattern of the main shields and the presence of spurs on legs II, III and IV in the male. The genus Dissoloncha Falconer is here resurrected for M. superbus Hull, which is shown to share characters of the gnathosoma and other features with Geholaspis and to be isolated from Macrocheles s. str. The generic limits of Holastaspella have been widened to include species without seta Zvl on the ventrianal shield* and a greater range of variation in the form of the ventral sclerotisation. Geholaspis remains essentially unchanged although some authors give the subgenus Longicheles Valle full generic status (Athias-Henriot, 1968). A number of species groups have been distinguished in the genus Macrocheles following the work of Filipponi & Pegazzano (1962, 1963) on closely related species. This concept has been extended by Krantz (1972) and is also used here. Key to the genera of Macrochelidae occurring in the British Isles 1 Femur II armed with a sclerotised spur in the female, seta mv of tarsus II modified into a thick spine (Fig. 22B); vertical setae inserted on an anterior projection of the dorsal shield (Fig. 22A). British species with four pairs of preanal setae on the female ventrianal shield HOLOSTASPELLA Berlese (p. 1 18) Femur II unarmed in the female, seta mv of tarsus II unmodified; without anterior projection of the dorsal shield. British species never with four pairs of preanal setae 2 2 Ventrianal shield with inguinal pores on anterolateral corners; gnathotectum lacking lateral pro- cesses (Figs 2B, 4E); corniculi three or more time longer than broad (Fig. 3C) .... 3 Inguinal pores free on post-coxal membrane; gnathotectum with free or fused lateral processes (Fig. 7B, D); corniculi no more than twice as long as broad, or if gnathotectum without lateral processes and corniculi elongate then with anal shield only (Fig. 13B) 4 3 Ventrianal shield with five pairs of preanal setae; terrestrial litter species GEHOLASPIS Berlese (p. 69) Ventrianal shield with three pairs of preanal setae; seashore species DISSOLONCHA Falconer (p. 76) 4 Sternal shield with characteristic reticulate pattern (PI. 3C), extending posterolaterally to level of posterior margins of coxae III; legs II-IV of males armed with spurs GL YPTHOLASPIS Filipponi & Pegazzano (p. 1 14) Sternal shield variously ornamented but never similar to the above, not produced posterolaterally beyond the middle of coxae III; legs II and sometimes IV, but not III, armed with spurs and tubercles in the male MACROCHELES Lutreitte (p. 78) Genus GEHOLASPIS Berlese Geholaspis Berlese, 1918. Redia 13: 145. TYPE SPECIES. Gamasus longispinosus Kramer, 1876. The dorsal shield has 28 pairs of setae which are mostly pilose or plumose distally. The ventral setae are mostly simple except towards the posterior lateral margins. The sternal and genital shields are similar to those of Macrocheles, but the metasternal plates may be free or fused to the endopodal shields (subgenus Cyrtocheles Valle). The ventrianal shield has five pairs of preanal setae and bears the inguinal pores (Athias-Henriot, 1969) in the anterolateral corners. Males, where known, have *It should be noted that contrary to the statement and figures of Krantz (1967), H. sculpta Berlese, the type species of Holoxtaxpella, in fact lacks setae Zvl on the ventrianal shield (Filipponi & Pegazzano, 1967, and personal observation of R.M.E.). 70 K. H. HYATT & R. M. EMBERSON holoventral shields. The gnathotectum has an elongate median process that may be toothed or bifurcate distally and dentate laterally. The chelicerae may be either short (Geholaspis s. str. and Cyrtocheles) with basically tridentate fixed chelae and bidentate movable chelae, or very elongate (Longicheles Valle) and multidentate. The spermatodactyl is short and dorsally directed. The corniculi are elongate, more than three times as long as broad and the external hypostomal setae are anterior to the internals. The males have a small spur on femur II. The setation of the dorsum varies from the usual condition as seen in Macrocheles (Fig. 1 A) in that setaey'5 are displaced posteriorly, so as to lie mesad and only slightly anterior of/6 in subgenera Geholaspis s. str. (Figs 2A, 3A) and Cyrtocheles and considerably posterior to setaey'6 in subgenus Longicheles (Figs 4A, 5A). This latter position is associated with a posterior projection of the podonotal shield in the protonymphs and is no doubt a consequence of a posterior migration of the cheliceral retractor muscles, associated with the massive development of the chelicerae in this subgenus. Key to subgenera and species of Geholaspis s. lat. recorded from the British Isles 1 Cheliceral digits short, with not more than 5 teeth (Fig. 2C); gnathotectum more or less triangular, median process with prominent lateral projections (Fig. 2B) Subgenus GEHOLASPIS s. str. 2 Cheliceral digits prominently elongate, multidentate, movable digit with 10 or more teeth (Fig. 4F); gnathotectum with median process parallel sided, bifurcate distally (Fig. 4E) Subgenus LONGICHELES Valle 3 2 Dorsal setae less than 100 \xm in length; ventrianal shield only slightly wider than long (PI. 4A). Geholaspis (G.) longispinosus (Kramer) (p. 70) Dorsal setae generally exceeding 1 50 um in length; ventrianal shield conspicuously wider than long (Fig. 3B) Geholaspis (G.) aeneus Krauss (p. 71) 3 Setae z5 simple (Fig. 4A); median process of gnathotectum smooth or minutely denticulate behind terminal bifurcation (Fig. 4E); ventrianal shield almost as broad as or broader than long (Fig.4B-D) Geholaspis (L.) mandibularis (Berlese) (p. 74) Setae z5 plumosej'6 serrate or simple (Fig. 5 A); median process of tectum strongly toothed behind terminal bifurcation (Fig. 5C); ventrianal shield noticeably longer than broad (Fig. 5B) . Geholaspis (L.) hortorum (Berlese) (p. 74) Geholaspis (Geholaspis) longispinosus (Kramer) (Fig. 2A-C, PI. 4A) The description and synonymy given by Evans & Browning (1956) are unchanged. MATERIAL EXAMINED. 127 collections — 4 PNN, 16 DNN, numerous 99- ENGLAND: Isles of Scilly, Cornwall, Devon, Somerset, Dorset, Gloucestershire, Hampshire, Sussex, Surrey, London, Kent, Essex, Cambridgeshire (including Huntingdonshire), Norfolk, Suffolk, Hertfordshire, Berkshire, Buckinghamshire, Worcestershire, Warwickshire, Lincolnshire, Yorkshire, Cumbria (Cumberland and Westmorland), Northumberland. SCOTLAND: Strathclyde (Argyllshire), Dumfries & Galloway (Wigtownshire), Tayside (Perthshire), Highland (Inverness-shire, Wester Ross), Inner Hebrides (Mull, Ulva), Shetland. WALES: Glamorgan, Gwent, Gwynedd (Merionethshire and Caernarvonshire), Clwyd (Denbighshire). IRELAND: Clare, Westmeath, Galway, Mayo, Leitrim. CHANNEL ISLANDS: Jersey. HABITATS. Found in all sorts of forest leaf litter, among dead grass and other decaying vegetation, also in moss. Bregetova & Koroleva (1960) also have records from small mammal nests. DISTRIBUTION. One of the commonest European macrochelids, found throughout the British Isles and Europe generally (Valle, 1953; Balogh, 1958; Bregetova & Koroleva, 1960; Halaskova & Kunst, 1960; Johnston, 1970; Krantz, 1972). Emberson (\913a) has reported the species from New Zealand where it is presumably adventive. MACROCHELIDAE OF THE BRITISH ISLES 71 Fig. 2 Geholaspis (G.) longispinosus (Kramer): female — A dorsal shield; B gnathotectum; C chelicera. After Evans & Browning (1956). Geholaspis (Geholaspis) aeneus Krauss (Fig. 3A-C) Geholaspis (Geholaspis) aeneus Krauss, 1970. Acarologie 14: 38. FEMALE. The dorsal shield (Fig. 3 A) measures 11 30 (am long x 840 um wide (Krauss gives 1050 um x 750 um) and is finely granular. The posterior half is covered by a finely regular reticu- lated pattern, whilst anteriorly it is punctate-reticulate towards the lateral margins. There are 28 pairs of setae. With the exception of setae jl, zl and J5, all exceed 150 um in length. The majority are finely pilose, at least in their distal halves. The dorsal pores are conspicuous. The ventral ornamentation and chaetotaxy are shown in figure 3B. The sternal shield has a characteristic reticulate pattern. The metasternal plates are free. The genital and ventrianal shields have strong reticulate ornamentation. The ventrianal shield (460 um long x 630 um wide) is conspicuously wider than long and the preanal setae appear to be simple. The venter of the gnathosoma is shown in figure 3C. The corniculi measure c. 140 um in length, and the setae appear simple. The chelicerae and gnathotectum are not visible in the only specimen available for study. The leg setae are normal for the genus. The majority are pilose, whilst those on tarsus I and distally on the remaining tarsi are simple. 72 K. H. HYATT & R. M. EMBERSON Fig. 3 Geholaspis (G.) aeneus Krauss: female — A dorsal shield; B ventral sclerotisation; C venter of gnathosoma. MATERIAL EXAMINED. 1 collection — 19, in moss. IRELAND: Mayo. See below. This is the first British record. REMARKS. This species was described from protonymph, deutonymph and female stages collected at Valle de Lozera, Puento de Lozera (600 m), Lugo Province, in northwest Spain (Krauss, 1970). The habitat is given as the foot of an old sweet chestnut Castanea saliva tree and an oak Quercus toza tree in a dry river-bed. We have tried to obtain specimens, but have been informed by Dr W. Hirschmann that Dr Krauss (pers. comm.) has no specimens in his possession. The Halbert collection contains a single slide preparation labelled "Holostaspis longispinosus (Kram.), 19, Clare Island, in moss, HI/1910'. The idiosoma of this specimen has been damaged on the slide and it is felt at present inadvisable to dismount it. However, the dorsal and ventral chaetotaxy and the venter of the gnathosoma are clearly discernible. MACROCHELIDAE OF THE BRITISH ISLES 73 Fig. 4 Geholaspis ( Longicheles ) mandibularis (Berlese): female — A dorsal shield; B-D variation in the form of the ventrianal shield; E gnathotectum, F chelicera. After Evans & Browning (1956). 74 K. H. HYATT & R. M. EMBERSON Geholaspis (Longicheles) longulus (Berlese) The presence of this species in the British Isles is now doubtful. The discovery of a specimen in the Hull Collection with the data 'Macrocheles longulus dead fowl' is probably the one mentioned (Hull, 1 9 1 8) as being caught 'at one of my carrion traps'. This is a specimen of G. longispinosus. The specimens recorded by Halbert (1915) from Clare Island, Mulranny and Castlebar, all in Co. Mayo, have been examined and are G. mandibularis. Geholaspis (Longicheles) mandibularis (Berlese) (Fig. 4A-F) The description and synonymy given by Evans & Browning (1956) do not require amendment. TYPE MATERIAL. I lolotvpc 9, Cansiglio. Slide 2/34 [ISZA]. MATERIAL EXAMINED. 1 14 collections — 3 PNN, 29 DNN, many $9. ENGLAND: Isles of Scilly, Cornwall, Somerset, Dorset, Gloucestershire, Hampshire, Surrey, Sussex, London, Kent, Middlesex, Hertfordshire, Suffolk, Cambridgeshire (including Huntingdonshire), Berkshire, Lancashire, Cumbria (Westmorland), Northumberland. SCOTLAND: Strathclyde (Argyllshire), Dumfries & Galloway (Wigtownshire), Inner Hebrides (Mull, Ulva, lona), Highland (Ross & Cromarty), Shetland. WALES: Glamorgan, Gwent, Gwynedd (Merionethshire and Caernarvonshire). IRELAND: Clare, Sligo, Galway, Mayo, Leitrim, Westmeath. HABITATS. A wide variety of litter habitats, also turf, soil, moss, ants' nests and nests of small mammals. DISTRIBUTION. Found throughout the British Isles and widespread in Europe (Valle, 1953). The specimens recorded by Halbert (1915) from Co. Mayo, as Holostaspis longulus Berlese, have been examined and are G. mandibularis. Geholaspis (Longicheles) hortorum (Berlese) (Fig. 5A-D, PL 5A) Holostaspis longulus var. hortorum Berlese, 1904. Redia 1: 265. Macrocheles (Geholaspis) hortorum: Berlese, 1918. Redia 13: 145. Geholaspis (Longicheles) mandibularis hortorum: Valle, 1953. Redia 38: 349. FEMALE. Generally very similar to G. mandibularis but differing in numerous details. -The dorsal shield (Fig. 5A), which measures 770-880 um long x 440-500 um wide, is more tapered posteriorly than in G. mandibularis. The setae are arranged as in G. mandibularis, except that z5 is plumose and z6 is occasionally dentate; these setae are simple in G. mandibularis. Setae J5,j6, J2 and J5 are simple, all other dorsal setae are plumose. In the figured specimen there is, on the left side, an additional seta between and slightly below SI and Zl. The dorsal shield is ornamented with conspicuous, dense, small denticles which diminish towards the centre of the shield, becoming fine granulation. The lateral margins are crenate. With the exception of setae Zvl and Zv2 the setae of the ventral shields are simple. The sternal shield has a characteristic reticulate pattern with fine punctures (PI. 5A). The metasternal plate- lets are free and ovate. The genital and ventrianal shields have reticulate ornamentation. The ventrianal shield (Fig. 5B) is longer than broad (290-360 um long x 260-305 um wide) and has prominent pores at its anterolateral corners and on its posterolateral margin. The ventrianal setae are noticeably shorter than in G. mandibularis. Setae Zvl are pilose and Zv2 are plumose. The shield is ornamented with clear reticulation. Only the tubuli and rami of the spermathecal apparatus are normally visible. The gnathotectum (Fig. 5C) has the median process bifurcate and almost fimbriate distally; posterior to the bifurcation the process is distinctly toothed while basally there is a series of irregular lateral teeth. The cheliceral dorsal seta is simple. The chelae are elongate and multidentate (Fig. 5D). The fixed chela has a main row of about 10-15 teeth with the third or fourth tooth from MACROCHELIDAE OF THE BRITISH ISLES 75 Zv1 Fig. 5 Geholaspis (Longicheles) hortorum (Berlese): female — A dorsal shield; B ventrianal shield; C gnathotectum; D chelicera. 76 K. H. HYATT & R. M. EMBERSON the distal end noticeably larger than the others and a subsidiary row of 6 or 8 teeth on the exterior face extending posteriorly from the large tooth. The movable chela (c. 198 urn) has a main row of about nine teeth with the second noticeably larger, whilst there is a subsidiary outer row of about 5-6 teeth. Most leg setae are pilose, except for those on tarsus I, the distal part of tarsi II-IV, and the setae on coxae I and II, trochanters I and II and ventrally on femora I and II. MALE. Unknown. TYPE MATERIAL. Not seen, identification based on Valle's (1953) redescription of Berlese's type material. MATERIAL EXAMINED. 8 collections — 1 PN, 1 DN, 13 9$. ENGLAND: Yorkshire. HABITAT. The first British record. From semi-natural grasslands in the Yorkshire Wolds. DISTRIBUTION. Valle (1953) lists material from Italy, Switzerland, Austria, Belgium, Iceland and Germany, however it was not reported from Germany by Karg (1971) or Krauss (1970). REMARKS. This species is most clearly separated from G. mandibularis on the setation of the dorsal shield, the longer than broad ventrianal shield, details of the gnathotectum and the dentition of the chelicerae, which in British specimens of G. mandibularis are characterised by more numerous (fixed chela 1 8-20 teeth, movable chela 14-15 teeth) and smaller teeth, the fixed chela also lacks the clear subsidiary row of teeth found in G. hortorum. There seems to be considerable variation in the cheliceral dentition in continental specimens of both species and a complex of forms could be involved. Since G. hortorum and G. mandibularis occur together in Yorkshire, and appear to overlap in much of their continental ranges, they must be regarded as distinct species rather than subspecies as suggested by Valle (1953). Genus DISSOLONCHA Falconer Dissoloncha Falconer, 1923. Naturalist, Hull 1923: 151. TYPE SPECIES. Macrocheles super bus Hull, 1918. The dorsal shield has 28 pairs of setae which are mainly pilose distally; it has a distinct border and crenulate lateral margins. The ventral setae are all pilose distally with the exception of the paranals. The sternal and genital shields are similar to those of Macrocheles, but have distinctive patterns. The ventrianal shield has three pairs of preanal setae and bears the inguinal pores (Athias, 1969) in the anterolateral corners. There may be up to three pairs of muscle apodomes between the ven- trianal and genital shields, usually two pairs of these adjoin the ventrianal shield. Males have separate sternogenital and ventrianal shields. The gnathotectum tapers into an elongate median process, dentate laterally and bifurcate distally. The female chelae are elongate and basically bidentate; the male chelae are shorter, the fixed chela has four to five teeth and the movable chela is unidentate, the spermatodactyl is short, blunt and dorsally directed. The corniculi are elongate, more than three times as long as broad at the base and the external hypostomal setae are anterior to the internals. The males have major spurs on legs II and IV. The spermathecal sacculus is large, spherical and strongly convoluted, its diameter is greater than the distance between coxae IV. The most distinctive features of Dissoloncha are the shape of the gnathotectum, the elongate corniculi and the more distally placed external hypostomal setae, characters which are all shared with Geholaspis s. lat. The placement of the inguinal pores on the anterior lateral corners of the ventrianal shield, a feature also found in Geholaspis, is not simply a reflection of the lateral expansion of the ventrianal shield as species of Macrocheles in which the shield is strongly expanded still have the inguinal pores free on the membrane. The structure of the sacculus is unique within the Macrochelidae, as is the habitat of rotting seaweed and tidal wrack. MACROCHELIDAE OF THE BRITISH ISLES 77 Fig. 6 Dissoloncha superbus (Hull): female — A dorsal shield; B lateral margin of dorsal shield; C gnathotectum; D chelicera: male — E chelicera; F distal end of gnathotectum; G leg II; H leg IV. After Evans & Browning (1956). 78 K. H. HYATT & R. M. EMBERSON Dissoloncha super bus (Hull) (Fig. 6A-H, PI. 3D) Mac rochele s superbus Hull, 1918. Trans, nat. Hist. Soc. Nor thumb. 5, 1: 71. Dissoloncha superbus: Falconer, 1923. Naturalist, Hull 1923: 151. Macrocheles superbus: Evans & Browning, 1956. Bull. Br. Mus. nat. Hist. (Zool.) 4: 38. The description of this species given by Evans & Browning (1956) remains adequate. MATERIAL EXAMINED. 25 collections— 3 PNN, approximately 45 DNN, 28 <$<$ and 200 99. ENGLAND: Cornwall, Dorset, Kent, Essex, Yorkshire, Northumberland, Durham. SCOTLAND: Highland (Inverness-shire), Outer Hebrides (Lewis), Fife, Shetland, Fair Isle, Dumfries & Galloway (Wigtownshire). WALES: Menai Straits, Milford Haven. HABITATS. Common in rotting seaweed on beaches, also found in a salt marsh and in rotten grass on a beach. Bregetova & Koroleva (1960) reported it from gulls' nests. DISTRIBUTION. Probably around the entire coast of the British Isles; also northern Europe, Germany (Krantz, 1972), N. America (Krantz, 1972) and Kuril Islands (Bregetova & Koroleva, 1960). This is quite possibly a holarctic seashore species. Genus MACROCHELES Latreille Macrocheles Latreille, 1829. In Cuvier, Regne animalium 2nd ed. 4: 282. Type species: Acarus marginatus Hermann, 1804 = Acarus muscae domesticae Scopoli, 1772. Coprholaspis Berlese, 1918. Redia 13: 146. Type species: Holostaspis glabra Miiller, 1860. Nothrholaspis Berlese, 1918. Redia 13: 169. Type species: Holostaspis tridentinus G. & R. Canestrini, 1882. Monoplites Hull, 1925. Ann. Mag. nat. Hist. (9) 15: 215. Type species: Macrocheles (Monoplites) oudemansii Hull, 1925 = Macrocheles marginatus Oudemans, 1901 nee Hermann, 1804. Macrholaspis Oudemans, 1 93 1 . Ent. Ber. 8 No. 1 80: 272. Type species: Gamasus opacus C. L. Koch, 1 839. Andrholaspis Turk, 1948. Proc. zool. Soc. Lond. 118: 103. Type species: Andrholaspis trinitatus Turk, 1948. The dorsal shield has 28-30 pairs of setae and smooth or dentate lateral margins; the dorsum lacks an anterior extension bearing setae jl. The sternal shield does not extend posteriorly beyond the middle of coxae III. The metasternal platelets are free, usually small, rounded and bear the metasternal setae. The ventrianal shield has 0-3 pairs of preanal setae, depending on the extent to which it is reduced. If it is reduced there are 1-3 pairs of platelets (muscle apodemes) between it and the genital shield. The peritrematic shield is not fused to the expodal shields. The males either have holoventral shields or separate sternogenital and ventrianal shields. The gnathotectum is usually tripartite, the lateral processes may be free, fused basally or strongly reduced. The chelicerae are strong, the dentition is variable, the cheliceral brushes are shorter than the movable digit, the dorsal seta may be simple, spatulate or pectinate. The leg chaetotaxy is normal for the family (except M. subbadius Berlese which has seta plt present on genua IV). The legs of the females are without spurs, the males have spurs on leg II and often on leg IV. The main change to the definition of Evans & Browning (1956) has been its widening to include species formerly placed in Macrholaspis Oudemans (Krantz, 1962) following the realisation that there are species closely related to M. opacus (C. L. Koch), its type, with three pairs of preanal ventrianal setae. Ecological and morphological grouping of the species of Macrocheles The species of the genus Macrocheles fall into two broad categories on ecological grounds which correlate with certain morphological features. There are those species that are usually found in leaf litter, moss, nests of birds and small mammals and other habitats not predominantly associated with coprophilic insects, and there are those species that are usually coprophilic, but also found in compost heaps, rotting grass clippings, carrion and similar habitats, generally favoured as breeding grounds by synanthropic muscoid flies. MACROCHELIDAE OF THE BRITISH ISLES 79 Species of the latter grouping are often found phoretic, as females, on coprophilic and necro- philic insects, for instance dung beetles, burying beetles and synanthropic flies. Males of these species are rarely found, but when they are, they are usually strongly dimorphic in the shape of the dorsal shield and in the number of pilose dorsal setae, which tends to increase. Well developed spurs are usually found on legs IV of the males of this group as well as on legs II. In the European fauna species of this group tend to have a preponderance of simple setae that are only faintly pilose, but this feature is not constant, particularly in the tropical macrochelid fauna. Species of the former grouping are generally not phoretic on coprophilic insects, and in some, males are commonly found. The males are not strongly dimorphic, although smaller and with a more tapered dorsal shield. The number of pilose setae remains approximately the same in the males. Well developed spurs are usually only found on legs II although there may be minor tubercles and ridges on legs IV. There tends to be a greater number of strongly pilose setae than in the former grouping. A few species combine the characters of both these categories, M. penicilliger is found phoretic on insects, is not strongly dimorphic and has well-developed spurs on legs IV of the male. M. matrius is very often associated with chicken manure and compost heaps, but is not usually phoretic on coprophilic insects; it is not strongly dimorphic but has well developed spurs on legs IV of the male. Both these species have a preponderance of strongly pilose setae. The species of Macrocheles found in the British Isles may therefore be grouped as follows: Leaf-litter species Coprophilic species M. decoloratus M. muscaedomesticae M. punctoscutatus M. robustulus M. rotundiscutis glaber species group carinatus species group subbadius species group opacus species group Intermediate species M. matrius M. penicilliger It is interesting to note that Krantz (1981) has shown that the glaber species group, the subbadius species group, and M. robustulus, share characters of the ambulacra in the immature stages not found in other species of Macrocheles, and that M. penicilliger is intermediate between the two main types of ambulacral structures. Most of the coprophilic species have been shown to be specialised predators on eggs and young larvae of muscid flies and also on the nematodes and small enchytraeid worms found in their habitat. The leaf-litter group are more likely to be general predators on small anthropods and other animals in their habitat, although biological data are much more fragmentary for these species. The coprophilic way of life and the characters associated with it are probably derived from the more generalised leaf-litter species. This is supported by comparison with the genus Geholaspis which is all litter dwelling and is the most plesiomorphic group of macrochelids. However, males are very rare or unknown in most species of the genus Geholaspis and in the opacus species group which makes it difficult to draw positive conclusions about their relationships. Key to the females of the species of Macrocheles occurring in the British Isles 1 All setae on dorsal shield simple, needle-like, setae jl short, spine-like; sternal shield with lineae oblique anteriores joined by four or five transverse lines, the most posterior of which is the linea media transversa (PI. IF) ........ subbadius species group 2 Some dorsal setae, always including jl, pilose, at least distally; sternal shield variously ornamented, sometimes without regular lines and never as above 4 2 Sternal shield with lineae oblique anteriores connected by five lines (PI. 2A), linea media transversa straight or slightly curved posteriorly; genu IV with six or seven setae. ..... 3 Plate 1 Sternal, genital and ventrianal shields of the females of: A Macrocheles muscaedomesticae (Scopoli); B M. robustulus (Berlese); C M. glaber (Muller); D M. punctoscutatus Evans & Browning; E M. scutatus (Berlese); F M. insignitus Berlese. After Evans & Browning (1956). Plate 2 Sternal, genital and ventrianal shields of the females of: A Macrocheles merdarius (Berlese); B M. montanus (Willmann); C M. carinatus (C. L. Koch); D M. penicilliger (Berlese); E M. submotus Falconer; F M. tardus (C. L. Koch). After Evans & Browning (1956). 82 K. H. HYATT & R. M. EMBERSON Sternal shield with lineae oblique anteriores connected by four lines (PI. 1 F), linea media transversa arched forwards, all sternal shield lines with a strong edging of punctures; genu IV with six setae, pi, absent .......... M. insignitus Berlese (p. 1 1 3) 3 All lines of the sternal shield with a strong edging of punctures (PI. 6E); reticulations of dorsal shield densely covered with minute punctures (Fig. 19A); genu IV with seven setae, pi, present . . . . M.subbadius (Berlese) (p. 110) Transverse lines of sternal shield poorly marked and punctured (PI. 2A); dorsal shield reticu- lations more or less unmarked with punctures; genu IV with six setae, />/, absent M. merdarius (Berlese) (p. 113) 4 With 1-3 pairs of postgenital platelets or apodemes; ventrianal shield sometimes reduced in size, sometimes with less than three pairs of preanal setae (PI. 4B) 5 Without separate postgenital platelets, muscle attachments on ventrianal shield; ventrianal shield of normal size, always with three pairs of preanal setae . 12 5 All dorsal setae strongly pilose throughout their entire length, setae J3 always present, either with J2 also present or with unpaired setae betweeny'6 and J3\ ventrianal shield with two or three pairs of setae, or reduced to an anal shield (PI. 4B); lateral elements of gnathotectum free (Fig. 12D), reduced in size or absent (Fig. 1 3D) . . . . . opacus species group (partim) 6 Some dorsal setae, including j6, z5, z6, J2 and J5, simple, others only pilose in their distal half or two thirds, setae J3 absent (except M. montanus (Willmann)); ventrianal shield always with three pairs of preanal setae; lateral elements of gnathotectum fused basally (Fig. 1 1 B) carinatus species group 9 6 Opisthogastric sclerotisation reduced to an anal shield, without preanal setae (Fig. 13B); lateral elements of gnathotectum absent, with single median process bifurcate distally (Fig. 13D) M. emails sp. nov. (p. 96) Opisthogaster with a ventrianal shield with two or three pairs of preanal setae; gnathotectum with reduced lateral elements present (Fig. 12D) 7 7 Ventrianal shield with two pairs of preanal setae 8 Ventrianal shield with three pairs of preanal setae M. terreus (Canestrini & Fanzago) (p. 103) 8 Anterior portion of dorsal shield with a network of minute spicules (Fig. 12B), lateral margins with small rounded serrations (Fig. 12C), with a pair of setae in the J2 position (Fig. 12A) M. opacus (C. L. Koch) (p. 96) Anterior portion of dorsal shield without spicules (Fig. 14B), lateral margins with sharp pointed serrations (Fig. 14C), with three or four unpaired median setae between j6 and J3 (Fig. 14A) M. dentatus (Evans & Browning) (p. 101) 9 Dorsal setae zl smooth, nearly as long as or longer than setaey'7, and always extending beyond the bases of setaey'2 (Fig. 11 A, E) 10 Dorsal setae zl smooth or pilose, much shorter than setae jl and never reaching the bases of setae y2(Fig. 10A,E) . . 11 10 Dorsal shield never with more than six pairs of smooth setae (j6, zl, z5, z6, J2, J5), setae j5 as long as setae j4 and lightly pilose M. tardus (C. L. Koch) (p. 94) Dorsal shield with more than six pairs of smooth setae, setae j2,j5, s2, r3, r4 in addition also smooth (Fig. 11 A) M. submotus Falconer (p. 92) 11 Dorsal shield with 29 pairs of setae, J3 present (Fig. 10E) . M. montanus (Willmann) (p. 92) Dorsal shield with 28 pairs of setae, J3 absent, setae j5 shorter than setaey¥ M. carinatus (C. L. Koch) (p. 90) 12 Some dorsal setae, at least a group in the middle of the dorsal shield, including setaey'6, z5, z6 and J2, simple needle-like, not pilose (Fig. 9) 13 All dorsal setae pilose (Fig. 14A) 20 1 3 Most setae on the dorsal shield simple, setae s6, SI and S2 and usually others on the shield margin simple 14 All setae on the dorsal shield margins, including all the s-S series, pilose (Fig. 15C). 19 14 Dorsal setae generally long, curved or wavy, setae 7.4 reaching beyond bases of setae J5, setae j4, z2, z4, s2, r2, r3 pilose (Fig. 9); ventrianal shield subcircular, slightly truncate anteriorly, ornamented with lines and punctures . M. rotundiscutis Bregetova & Koroleva (p. 88) Dorsal setae generally short, straight or slightly curved; distal ends of setae 7.4 fall well short of bases of setae J5 (Fig. 16A); ventrianal shield usually pentagonal, truncate anteriorly (PI. IB), if strongly rounded then densely covered with minute punctations (PI. 1 D) and with only setaey'7 and r3 pilose on anterior part of dorsal shield (Fig. 8G) 1 5 1 5 Setaey'7 elongate, over twice as long as setaey'2 and noticeably longer than setaey'J, minutely pilose MACROCHELIDAE OF THE BRITISH ISLES 83 D Plate 3 Sternal, genital and ventrianal shields of the females of: A Macrocheles decoloratus (C. L. Koch); B M. matrius (Hull); C Glyptholaspis confusa (Foa); D Dissoloncha superbus (Hull). After Evans & Browning (1956). 84 K. H. HYATT & R. M. EMBERSON D Plate 4 Sternal, genital and ventrianal shields of the females of: A Geholaspis (G.) longispinosus (Kramer); B Macrocheles opacus (C. L. Koch); C M. dentatus Evans & Browning; D Holostaspella orngta (Berlese). After Evans & Browning (1956). MACROCHELIDAE OF THE BRITISH ISLES 85 distally (Fig. 1 6B), setae J5 simple, about half as long as setae Z5 (Fig. 1 6A); sternal shield without distinct lines but with a more or less symmetrical pattern of punctures some of which may be linearly arranged (PI. IB) M. robustulus (Berlese) (p. 106) Setae jl short and stout, little longer than setae j2 and/?, distinctly pilose in distal third to half, setae J5 simple or pilose, as long as or little shorter than setae Z5 (Fig. 8D); sternal shield with a distinct pattern of lines (PI. ID) 16 16 All sclerotised regions densely covered with minute punctations (Fig. 8D); ventrianal shield strongly rounded, almost subcircular in outline (PI. ID). M. punctoscutatus Evans & Browning (p. 88) Sclerotised regions not densely punctate as above; ventrianal shield pentagonal in outline (PI. 1C) glaber species group 1 7 17 Posterior series of dorsal setae with five pairs (J5, Z4, Z5, S4, 55) of setae on the dorsal shield pilose, at least distally (Fig. 1 7E); sternal shield with linea arcuata faintly impressed impunctate, all sternal shield punctures minute (PI. 6D) . . M. nataliae Bregetova & Koroleva (p. 109) Posterior series of dorsal setae with only one pair of pilose setae (/5) on the dorsal shield (Fig. 17A); sternal shield with several well developed punctures along linea arcuata (PI. 1C), sternal shield punctures of different sizes, some minute, some larger 18 1 8 Linea arcuata on sternal shield more or less straight but having its ends directed posteriorly, all lines on sternal shield well developed, not strongly punctured (PI. 1C) . . . M. glaber (Mutter) (p. 107) Linea arcuata strongly concave, having its ends directed anteriorly, lines on sternal shield not strongly impressed, punctures well developed (PI. IE). M. scutatus (Berlese) (p. 1 10) 19 Dorsal setae only pilose in their distal third; setae J5 pilose (Fig. 15C); lateral elements of gnatho- tectum free (Fig. 15D) M. muscaedomesticae (Scopoli) (p. 105) Dorsal setae pilose in their distal half to two thirds, setae J5 simple (Fig. 7C); lateral elements of gnathotectum fused basally (Fig. 7D) .... M . penicilliger (Berlese) (p. 86) 20 Dorsal setae pilose along their entire length, with an extra unpaired median seta present in the J2 position between j6 and J3 (Fig. 14E); sternal shield densely covered with punctures (PI. 6B) M. punctatissimus Berlese (opacus species group) (p. 101) Dorsal setae only pilose in their distal halves, setae J2 paired, setae J3 absent, i.e. with 28 pairs of setae (Fig. 8 A); sternal shield with a pattern of lines and small areas of punctures (PI. 3 A) . . 21 2 1 Setae J5 approximately equal in length to setae Z5 and little more than half as long as setae 55 (Fig. 8 A); outer margins of lateral elements of gnathotectum smooth (Fig. 8B) M. decoloratus (C. L. Koch) (p. 88) Setae J5 shorter than setae Z5, setae Z5 approximately equal in length to setae 55 (Fig. 7A); outer margins of lateral elements of gnathotectum serrated (Fig. 7B) . M. matrius (Hull) (p. 85) Macrocheles matrius (Hull) (Fig. 7A, B, PI. 3B) The description of Evans & Browning (1956) requires no amendment. TYPE MATERIAL. Lectotype 9 'n.v.' [? Ninebanks vicarage, Northumberland], poultry manure, Hull collection. Here designated. Paralectotypes 18 $$, same data as lectotype [BMNH]. MATERIAL EXAMINED. 1 1 collections — 4 <$<$, 194 ??. ENGLAND: Gloucestershire, Surrey, Cambridgeshire (Huntingdonshire), Worcestershire, Staffordshire, Derbyshire, Northumberland. SCOTLAND: Grampian (Aberdeenshire), Inner Hebrides (Pabay). HABITATS. Four collections associated with poultry, also with mink Mustela vison, water shrews Neomysfodiens, in a canary cage and from grass clippings and compost. DISTRIBUTION. Widespread in Europe; Germany (Krantz, 1972), Austria (Johnston, 1970), Bulgaria (Balogh, 1958), U.S.S.R. (Bregetova & Koroleva, 1960). Also known from the U.S.A. (Axtell, 1963), Israel (Costa, 19666) and New Zealand (Emberson, 1973a). 86 K. H. HYATT & R. M. EMBERSON Fig. 7 Macrocheles matrius (Hull): female — A dorsal shield; B gnathotectum. Macrocheles penicilliger (Berlese): female — C dorsal shield; D gnathotectum; E chelicera. After Evans & Browning (1956). Macrocheles penicilliger (Berlese) (Fig. 7C-E, PI. 2D) The description of Evans & Browning (1956) requires no amendment. TYPE MATERIAL. S\ nt\ pes 2 9? only, Italy, Cison di Valmarino, Treviso, sotto legni [under wood] slide 3/38 [ISZA]. MACROCHELIDAE OF THE BRITISH ISLES 87 Fig. 8 Macrocheles decoloratus (C. L. Koch): female — A dorsal shield; B gnathotectum; C chelicera. Macrocheles punctoscutatus Evans & Browning: female — D dorsal shield; E anterior margin of dorsal shield; F seta s2; G seta r3. After Evans & Browning (1956). 88 K. H. HYATT & R. M. EMBERSON MATERIAL EXAMINED. 13 collections — 3 DNN, 1 <$, 125 ??. ENGLAND: Cornwall, Surrey, Kent, London, Middlesex, Essex, Bucks, Oxfordshire, Cheshire. WALES: Gwynedd (Caernarvonshire). IRELAND: Clare. CHANNEL ISLANDS: Jersey. HABITATS. Three collections associated with Trox scaber (L.), also found in insect cultures, decay- ing leaves, compost and sewage culture. DISTRIBUTION. Apparently widespread in Europe; Germany (Karg, 1970), U.S.S.R. (Bregetova & Koroleva, 1960), also known from New Zealand (Emberson, 1973. Additions to the macrochelid mites in New Zealand (Acarina: Mesostigmata: Macrochelidae) N.Z. Ent. 5: 294-302. Evans, G. 0. 1 956. On the classification of the family Macrochelidae with particular reference to the subfamily Parholaspinae (Acarina: Mesostigmata). Proc. zool. Soc. Land. 127: 345-377. - 1963. Observations on the chaetotaxy of the legs in the free-living Gamasina (Acari: Mesostigmata). Bull. Br. Mus. not. Hist. (Zool.) 10: 277-303. - 1 964. Some observations on the chaetotaxy of the pedipalps in the Mesostigmata (Acari). Ann. Mag. nat. Hist. (13)6:513-527. - & Browning, E. 1956. British mites of the subfamily Macrochelinae Tragardh (Gamasina, Macro- chelidae). Bull. Br. Mus. nat. Hist. (Zool.) 4: 1-55. - & Till, W. M. 1965. Studies on the British Dermanyssidae (Acari: Mesostigmata). Part I. External morphology. Bull. Br. Mus. nat. Hist. (Zool.) 13: 247-294. & - - 1979. Mesostigmatic mites of Britain and Ireland (Chelicerata: Acari-Parasitiformes). An introduction to their external morphology and classification. Trans, zool. Soc. Lond. 35: 139-270. Falconer, W. 1923. Two British mites new to science and a new subgenus of Macrocheles Latr. Naturalist, Hull 1923: 151-153. Filipponi, A. & Ilardi, A. 1958. Sulla validita di tre specie del sottogenere Berlesiano Macrocheles (Acarina, Mesostigmata). Riv. Parassit. 19: 1 17-130. Filipponi, A. & Pegazzano, F. 1960. Acari del genere Glyptholaspis nom. nov. pro Macrocheles (Macrocheles) Berl. 1918 (Mesostigmata, Macrochelidae). Redia45: 133-171. — & 1962. Specie Italiane del gruppo-glaber (Acarina, Mesostigmata, Macrochelidae, Macrocheles). Redia 47: 211-23%. — & — — 1963. Specie Italiane del gruppo-subbadius (Acarina, Mesostigmata, Macrochelidae). Redia 48: 69-91. — & 1967. Contribute alia conoscenza del genere Holostaspella Berlese, 1903. (Acari: Mesostigmata: Macrochelidae). Redia 50: 219-259. Franz, H. 1954. Die Nordost-Alpen. 15. Ordnung Acarina, in Spiegel Land-Tierwelt, Innsbruck 1: 329^52. Halaskova, V. & Kunst, M. 1 960. Uber einige Bodenmilben-gruppen aus dem Moorgebeit "Soos" in Bohmen. (Acari: Gamasina, Zerconina, Oribatei). Ada Univ. Carol. Biol. Suppl. 1960:1 1-58. M albert. J. N. 1915. Clare Island Survey, Part 39 ii Acarinida: Section II — Terrestrial and marine Acarina. Proc. R. Ir. Acad. 31: 45-136. Halliday, R. B. 1986. On the systems of notation used for the dorsal setae in the family Macrochelidae (Acarina). Internal. J. Acarol. 12: 27-35. Hammen, L. van der. 1964. The morphology of Glyptholaspis confusa (Foa, 1900) (Acarida, Gamasina). Zool. Verh. Leiden No. 71: 1-56. Hirschmann, W. 1957. Gangsystematik der Parasitiformes. Teil 1. Rumpfbehaarung und Riickenflachen. Acarologie 1: 1-20. Hull, J. E. 1918. Terrestrial Acari of the Tyne Province. Trans, nat. Hist. Soc. Northumb. 5, 1: 13-88. Johnston, D. E. 1970. Notes on a collection of Austrian Macrochelidae with a description of Macrocheles beierin. sp. Annln. naturh. Mus. Wien 74: 145-150. Karg. W. 1971. Acari (Acarina), Milben Unterordnung Anactinochaeta (Parasitiformes). Die freilebenden Gamasina (Gamasides), Raubmilben. Tierwelt Dtl. 59: 475 pp. Krantz, G. W. 1960. A re-evaluation of the Parholaspinae Evans, 1965 (Mesostigmata: Macrochelidae). Acarologia 2: 293-433. — 1962. A review of the genera of the family Macrochelidae Vitzthum, 1930 (Acarina: Mesostigmata). Acarologia 4: 143-173. — 1965. A review of the genus Neopodocinum Oudemans, 1902 (Acarina: Macrochelidae). Acarologia 7: 139-226. - 1967. A review of the genus Holostaspella Berlese, 1904 (Acarina: Macrcochelidae). Acarologia 9, fasc. suppl.: 91-146. — 1972. Macrochelidae from Hamburg (Acari Mesostigmata), with descriptions of two new species. Ent. Mitt. zool. Mus. Hamburg 4: 263-275. MACROCHELIDAE OF THE BRITISH ISLES 1 25 — 1 981. Two new glaber group species of Macrocheles (Acari: Macrochelidae) from southern Africa. Int.J. Acarol.l:3-\6. & Filipponi, A. 1964. Acari della famiglia Macrochelidae (Mesostigmata) nella Collezione del South Australian Museum. Riv. Parassit. 25: 35-54. Krauss, W. 1970. Die europaischen Arten der Gattungen Macrocheles Latreille 1829 und Geholaspis Berlese 1918. (Eine systematische Studie aus dem Jahre 1960). Acarologie 14: 2-43. Leitner, E. 1946. Zur Kenntnis der Milbenfauna auf Diingerstatten. Zentbl. Gesamtgeb. Ent. 1: 75-156. Lindquist, E. E. & Evans, G. 0. 1965. Taxonomic concepts in the Ascidae, with a modified setal nomenclature for the idiosoma of the Gamasina (Acarina: Mesostigmata). Mem. ent. Soc. Can. 47: 1-64. Petrova, A. D. 1960. Materialien iiber den Bau des inneren Sackchens des Receptaculum seminis der gamasoiden Milben Macrochelidae Vitz. Zool. Anz. 165: 393-400. - & Taskaeva, E. Z. 1964. Gamasoid mites (Parasitiformes, Gamasoidea) from southern China (1st Communication). Byull. Mask. Obshch. Ispyt. Prir. (Biol.) 69, 5: 47-61. Sellnick, M. 1931. Acari. In Max Beier, Zoologische Forschungreise nach den Jonischen Inseln und dem Peloponnes. XVI Teil. Sher. Akad. Wiss. Wien 140: 693-776. Smith, K. G. V. 1975. The faunal succession of insects and other invertebrates on a dead fox. Entomologist's Gaz. 26: 277-287. Valle, A. 1953. Revisione di generi e sottogeneri Berlesiani di Acari (Primo contributo). Redia 38: 316-360. — 1955. Revisione dell' Acaroteca Canestrini. Atti Memorie Accad. patavina67: 67-101. Willmann, C. 1951. Untersuchungen iiber die terrestrische Milbenfauna in pannonischen Klimagebiet Osterreichs. Sber. Akad. Wiss. Wien 160: 91-176. Manuscript accepted for publication 8 April 1987 British Museum (Natural History) The birds of Mount Nimba, Liberia Peter R. Colston & Kai Curry-Lindahl For evolution and speciation of animals Mount Nimba in Liberia, Guinea and the Ivory Coast is a key area in Africa representing for biologists what the Abu Simbel site in Egypt signified for archaeologists. No less than about 200 species of animals are endemic to Mount Nimba. Yet, this mountain massif, entirely located within the rain-forest biome, is rapidly being destroyed by human exploitation. This book is the first major work on the birds of Mount Nimba and surrounding lowland rain- forests. During 20 years (1962-1982) of research at the Nimba Research Laboratory in Grassfield (Liberia), located at the foot of Mount Nimba, scientists from three continents have studied the birds. In this way Mount Nimba has become the ornithologically most thoroughly explored lowland rain-forest area of Africa. The book offers a comprehensive synthesis of information on the avifauna of Mount Nimba and its ecological setting. During the 20 years period of biological investigations at Nimba this in 1962 intact area was gradually opened up by man with far-reaching environmental consequences for the rain-forest habitats and profound effects on the birds. Therefore, the book provides not only a source of reference material on the systematics, physiology, ecology and biology of the birds of Mount Nimba and the African rain-forest, but also data on biogeography in the African context as well as conservation problems. Also behaviour and migration are discussed. At Nimba a number of migrants from Europe and/or Asia meet Afrotropical migratory and sedentary birds. Professor Kai Curry-Lindahl has served as Chairman of the Nimba Research Laboratory and Committee since its inception in 1962. Peter Colston is from the Subdepartment of Ornithology, British Museum (Natural History), Tring, and Malcolm Coe is from the Animal Ecology Research Group, Department of Zoology, Oxford. 1986, 129pp. Hardback. 0 565 00982 6 £17.50. Titles to be published in Volume 54 The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences. By Gordon J. Howes A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles. By Keith H. Hyatt & Rowan M. Emberson A revision of Haplocaulus Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives. By Alan Warren Echinoderms of the Rockall Trough and adjacent areas. 3. Additional records. By R. Harvey, J. D. Gage, D. S. M. Billet, A. M. Clark & G. L. J. Paterson Printed in Great Britain by Henry Ling Ltd., at the Dorset Press, Dorchester. Dorset - f J GEN Bulletin of the British Museum (Natural History) A revision of Haplocaulus Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives Alan Warren Zoology series Vol54 No 3 26 May 1988 The Bulletin of the British Museum (Natural History), instituted in 1949, is issued in four scientific series, Botany, Entomology, Geology (incorporating Mineralogy) and Zoology, and an Historical series. Papers in the Bulletin are primarily the results of research carried out on the unique and ever-growing collections of the Museum, both by the scientific staff of the Museum and by specialists from elsewhere who make use of the Museum's resources. Many of the papers are works of reference that will remain indispensable for years to come. Parts are published at irregular intervals as they become ready, each is complete in itself, available separately, and individually priced. Volumes contain about 300 pages and several volumes may appear within a calendar year. Subscriptions may be placed for one or more of the series on either an Annual or Per Volume basis. Prices vary according to the contents of the individual parts. Orders and enquiries should be sent to: Publications Sales, British Museum (Natural History), Cromwell Road, London SW7 5BD, England. World List abbreviation: Bull. Br. Mus. nat. Hist. (Zool.) ustees of the British Museum (Natural History), 1988 The Zoology Series is edited in the Museum's Department of Zoology Keeper of Zoology : MrJ. F. Peake Editor of Bulletin : Dr C. R. Curds Assistant Editor : Mr C. G. Ogden ISBN 0 565 05039 7 ISSN 0007-1 498 Zoology series Vol54 No. 3 pp 127-1 52 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 26 May 1 988 v ,f '.' 9 /» MAY 1OQ( A revision of Haplocaulus Precht, 1935 (Ciliophora: * Peritrichida) and its morphological relatives % • Alan Warren Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 ^JBD '•"Tirr"" * BRITISH MUSEUI Contents Q . I1T7- 1JUW988 Synopsis. .............. j^ 127 Introduction . Genus Haplocaulus . Genus Baikalonis . . . L143 Genus Cotensita ............. 145 Genus Parazoothamnium . ........... 145 Genus Piesika 147 Genus Pseudohaplocaulus 147 Incertae sedis 149 References . . . . . . . . . . . . . .150 Index to species 152 Synopsis The species of Haplocaulus and of five closely related genera have been revised. A diagnosis for each genus is given with a key to its constituent species. Two new genera, Piesika n. gen. and Pseudohaplocaulus n. gen. are described. All extant species are described and figured. These include Haplocaulus — of which 26 species are recognised; Baikaloms — 3 species; Cotensita — 1 species; Parazoothamnium — 2 species; Piesika — 1 species; Pseudohaplocaulus — 2 species. Two other genera, Monintranstylum and Tucolesca, are also considered. Introduction In two previous papers (Warren, 1986, 1987) the peritrich genera Vorticella and Pseudovorticella were revised. Both are solitary forms the stalks of which coil up in a helical fashion upon contrac- tion. The genera dealt with in this paper are also solitary and borne on unbranched contractile stalks but, upon contraction, the stalks do not coil helically. Two of the principal generic characters used here are the mode of stalk contraction and the presence of pellicular tubercles with their underlying reticulate silverline system. Nevertheless for some species, details concerning these characters are not available. For example, with the excep- tion of Haplocaulus terrenus, no species of the genera reviewed have been impregnated with silver — the possession of reticulate silverline systems has been assumed from the presence of pellicular tubercles. However, although pellicular tubercles are usually associated with reticulate silverline systems, this may not be true in every case (Foissner, pers. comm.). The major genus included here is Haplocaulus Precht, 1935 which is found in marine, fresh- water and terrestrial habitats attached to plant, animal and inanimate substrates. The only previous revision of Haplocaulus was that of Stiller (1971); seven new species have since been described and several species have been transferred from other genera. Baikalonis, Cotensita and Parazoothamnium, three genera closely related to Haplocaulus, are revised and two new genera, Piesika and Pseudohaplocaulus, are described. All extant species are described and figured and keys to their identification are provided. A brief account of the morphological structures important in the taxonomy of the Vorticellidae is given in Warren (1986). Bull. Br. Mus. nat. Hist. (Zool.) 54(3): 127-152 Issued 26 May 1988 127 128 A. WARREN Key to genera 1 Zooid with pellicular tubercles ............. 2 Zooid without pellicular tubercles 3 2 Stalk contracts in two stages, initially shortening in a concertina-like fashion and then bending in a zigzag manner PIESIKA Stalk contracts in zigzag manner only PSEUDOHAPLOCAULUS 3 Stalk sheath folded below zooid . COTENSITA Stalk sheath not folded below zooid 4 4 Upon contraction stalk shortens longitudinally and is enveloped by zooid . BAIKALONIS Contraction does not result in zooid enveloping stalk 5 5 Stalk contracts in two stages, initially shortening in a concertina-like fashion and then bending in a zigzag manner PARAZOOTHAMNWM Stalk contracts in zigzag manner only HAPLOCAULUS Genus HAPLOCA ULUS Precht, 1 935 The genus Haplocaulus was erected by Precht ( 1 935) to include solitary vorticellids whose stalks are circular in cross-section and which contract in a zigzag rather than helical fashion. Impregnation by silver reveals a pattern of equally spaced horizontal lines or striations which encircle the body. These striations may or may not be visible in the living zooid. Two species were originally described by Precht (1935), H. nicoleae and H. furcellariae, although he failed to designate either as the type. H. nicoleae is here transferred to the genus Pseudohaplocaulus. H. furcellariae is designated the type species. Stiller (1971) transferred ten species to Haplocaulus all of which had previously belonged to the genus Vorticella. Three more vorticellids are here assigned to Haplocaulus for the first time. DIAGNOSIS. Zooid borne upon an unbranched stalk which is circular in cross-section and contracts in a zigzag manner. Zooids usually oval, cylindrical or inverted bell-shaped. Impregnation by silver reveals a transverse silverline system. Spasmoneme lies either parallel to the walls of the stalk sheath or is slightly twisted in the form of a shallow helix. Key to the species of Haplocaulus \ Diameter of peristomial lip greater than or equal to maximum body width . Diameter of peristomial lip less than maximum body width 15 2 Pellicular striations visible on live zooid . Pellicular striations not visible on live zooid .10 3 Zooid elongate and cylindrical in shape 4 Zooid either cone- or inverted bell-shaped 8 4 Pellicle with knob-like projections H.eforianus Pellicle without knob-like projections 5 5 Zooid with two contractile vacuoles H. dipneumon Zooid with one contractile vacuole 6 6 Zooid with distinct, broadly spaced striations H.fluviatilis Zooid with fine, narrow-spaced striations 7 Macronucleus C-shaped and situated in anterior part of zooid .... H.procerus Macronucleus irregular and situated in centre of zooid .... H. furcellariae 8 Zooid inverted bell-shaped with constriction beneath peristome 9 Zooid cone-shaped, not constricted beneath peristome H. conosomus 9 Macronucleus lies horizontally in anterior part of zooid H.epizoicus Macronucleus lies longitudinally in centre of zooid H. distinguendus 10 Zooid elongate, length at least x 3 maximum body width .... Zooid length less than x 3 maximum body width .12 1 1 Upon contraction, zooid assumes characteristic nodding position . . H. crassicaulis Upon contraction, zooid remains vertical ........ H. extensa 12 Zooid with endosymbiotic zoochlorellae H. sertulariarum Zooid without endosymbiotic zoochlorellae .13 1 3 Zooid cone-shaped, not constricted beneath peristome H. pelagicus Zooid inverted bell-shaped, usually with constriction beneath peristome 14 HAPLOCAUL US MORPHOLOGICAL RELATIVES 129 14 Pellicular granules present Pellicular granules absent 1 5 Pellicular striations visible on live zooid Pellicular striations not visible on live zooid 16 Striations distinct and widely spaced Striations fine with narrow spacing 17 Pellicle with concave ribbing between striations Pellicle with convex ribbing between striations 18 Zooid elongate, length at least x 2 maximum body width .... Zooid rotund, length less than x 2 maximum body width .... 19 Macronucleus U-shaped; spasmoneme extends full length of stalk Macronucleus C-shaped; spasmoneme does not extend complete stalk length 20 Marine; epizoic on the echinoderm Amphiurae squamata .... Freshwater; epizoic on the amphibian Rana temporaria .... 21 Zooid elongate, length at least x 2 maximum body width .... Zooid length less than maximum body width 22 Macronucleus spirally twisted and lies longitudinally in zooid . Macronucleus C-shaped and lies horizontally in zooid .... 23 Zooid 1 34 — 155 um long; epizoic on the amphibian Rana temporaria . Zooid 60 um long; epizoic on the crustacean Gammarus pulex . 24 Macronucleus C-, S-, or irregular in shape; infundibulum reaches at least one- Macronucleus J-shaped; infundibulum less than one-third zooid length 25 Macronucleus S-shaped or irregular; stalk about equal to body length Macronucleus C-shaped or irregular; stalk up to x 2 body length //. leanderi H. elegans H. terrenus H. kahili H.fusiformis H. claudlcans H. amphlurae H. longinucleatus H. macronucleatus H. amphiblarum H. stlllerl third zooid length . H. walteri H. brehml H. carinogammarl 16 21 17 18 19 20 22 24 23 25 Species descriptions Haplocaulus furcellariae Precht, 1935 DESCRIPTION (Fig. 1). The zooid of this, the type species is elongate, almost cylindrical in shape, approxi- mately 98 urn long x 40 um wide. Peristomial lip 50-55 um in diameter. Disc convex. Contractile vacuole small and situated in the peristomial region. Macronucleus elongate and irregular in shape. Pellicle with distinct transverse striations. Stalk up to 400 um long. HABITAT. Marine, originally found as an epizoite of Furcellaria. Fig. 1 Haplocaulus furcellariae, after Precht, 1935. Bar = 50 um. 130 A. WARREN Haplocaulus amphibiarum Banina, 1 982 DESCRIPTION (Fig. 2). Zooid 134- 155 urn long x 52-65 um wide, tapering at both ends and widest in the central region. Diameter of peristomial lip less than maximum body width. Disc cone-shaped and prominent. Infundibulum reaches one-third body length. Contractile vacuole situated in upper half of zooid. Macronucleus C-shaped and lies horizontally across centre of body. Food vacuoles often numerous and spindle-shaped. Stalk less than body length. HABITAT. Freshwater, originally found near Leningrad, U.S.S.R. attached to the amphibian Rana temporaria. Fig. 2 Haplocaulus amphibiarum, after Banina, 1982. Fig. 3 Haplocaulus amphiurae, after Cuenot, 1891 Bar = 50 um. (called Vorticella amphiurae) . Bar = 25 urn. Fig. 4 Haplocaulus brehmi, after Liipkes, 1 975. Bar = 50 urn. HAPLOCAULUS MORPHOLOGICAL RELATIVES 131 NOTE. H. amphibiarum bears a strong rr^rphological similarity to H. fusiformis (Nenninger, 1948) Stiller, 1971 and to Carchesium amphibiarum Nenninger, 1948 which are also epibionts of amphibians. It is possible that these three species may be synonymous. Haplocaulus amphiurae (Cuenot, 1891) n. comb. Vorticella amphiurae Cuenot, 1891 DESCRIPTION (Fig. 3). Zooid 40 urn long x 25-30 um wide, oval in shape, rounded posteriorly and with a narrow peristome. Contractile vacuole situated in upper one-third of body. Macronucleus C-shaped or occasionally irregular. Pellicle with fine transverse striations. Stalk less than body length. HABITAT. Marine, originally isolated from the Bay of Naples as an epizoite of the echinoderm Amphiurae squamata. NOTE. H. amphiurae is morphologically similar to Baikalonis. The original description of H. amphiurae, however, was made from partially contracted specimens. In order to determine the correct taxonomic position of this species, a redescription based on observations of healthy living specimens is required. Haplocaulus brehmi Liipkes, 1975 DESCRIPTION (Fig. 4). Zooid oval in shape, 80 um long x 70 um wide. Peristomial lip well developed, 50 um in dhmeter. Disc slightly convex. Infundibulum broad and reaches two-thirds body length. Contractile vacuole situated just below the peristome. Macronucleus S-shaped or irregular, and lies longitudinally with respect to the major body axis. Pellicular striations not observed. Stalk about equal to body length. HABITAT. Freshwater, originally found attached to the gills of larvae of the caddis-fly Agapatus. Haplocaulus carinogammari Stiller ( 1 963), 1 97 1 Vorticella carinogammari Stiller, 1963 DESCRIPTION (Fig. 5). Zooid inverted bell-shaped, rounded, 45-75 um long. Peristomial lip well developed, diameter about equal to maximum body width. Disc convex. Infundibulum narrow and reaches centre of zooid. Contractile vacuole situated just beneath peristome. Macronucleus elongate and irregular in shape. Pellicular striations visible on fixed specimens. Stalk up to x 2 body length. HABITAT. Freshwater, originally found attached to the crustaceans Carinogammarus roeselii var triacanthus and Gammarus fossarum; also occurs on Rivulogammarus (Piesik, 1975) and Asellus aquaticus (Szczepanowski, 1978). Fig. 5 Haplocaulus carinogammari (a) contracted; (b) relaxed, after Stiller, 1963 (called Vorticella carinogammari); (c) & (d) showing variation of macronucleus, after Szczepanowski, 1978. Bar = 50um. 132 A. WARREN Fig. 6 Haplocaulus claudicans, (a) relaxed zooid; (b) contracted zooid; (c) detail of stalk, after Penard, 1922 (called Vorticella claudicans). Bar = 25 urn. Fig. 7 Haplocaulus conosomus, (a) after Stokes, 1 889 (called Vorticella conosoma) ; (b) relaxed zooid; (c) contracted zooid, after Gajewskaja, 1933 (called Vorticella conesoma). Bar = 50 urn. Haplocaulus claudicans (Penard, 1922) Stiller, 1971 Vorticella claudicans Penard, 1922 DESCRIPTION (Fig. 6). Zooid elongate, almost cylindrical in shape, 40-55 urn long x 30 urn wide. Diameter of peristomial lip less than or occasionally equal to maximum body width. Contractile vacuole situated in upper one-third of body. Macronucleus C-shaped and lies horizontally across centre of zooid. Pellicle with fine transverse striations. Stalk about equal to body length. Spasmoneme terminates about half-way down the stalk and is connected to the base of the stalk by a fibre. HAPLOCAULUS MORPHOLOGICAL RELATIVES 133 Fig. 8 Haplocaulus crassicaulis, (a) relaxed zooid; (b) contracted zooid, composite after Kent, 1881 (called Vorticella crassicaulis) and Nenninger, 1948. Bar = 25 um. HABITAT. Freshwater, originally found attached to mosses. NOTE. It is unclear whether the 'fibre' in the lower part of the stalk is an extension of the spasmoneme, or a separate structure. In the case of the latter, it may be necessary to transfer this species to the genus Monintranstylum. Haplocaulus conosomus (Stokes, 1889) n. comb. Vorticella conosoma Stokes, 1889 Vorticella conesoma Gajewskaja, 1933 DESCRIPTION (Fig. 7). Zooid conical and elongate, 75 um long x 30 um wide, and with a distinct ridge in the region of the telotroch band. Peristomial lip 35 urn in diameter. Contractile vacuole situated just beneath peristome. Macronucleus C-shaped or irregular, and situated either centrally or in the anterior part of the body. Pellicular striations visible on zooid. Stalk 150-200 um long. HABITAT. Freshwater. NOTE. In his original description, Stokes (1889) did not describe the spasmoneme. According to Gajewskaja (1933), however, the spasmoneme terminates in the upper part of the stalk. If spasmoneme length is accepted as a generic character, it may be necessary to transfer this species to the genus Monintranstylum. Haplocaulus crassicaulis (Kent, 1881) Stiller, 1971 Vorticella crassicaulis Kent, 1881 DESCRIPTION (Fig. 8). Zooid elongate, 45-50 um long x 25 um wide. Peristomial lip 20 um in diameter. Contractile vacuole situated in upper one-third of body. Macronucleus C-shaped and situated in centre of zooid. Stalk x 1 — x 2 body length. Stalk sheath has several transverse folds. HABITAT. Freshwater, originally isolated as an epizoite of the crustacean Asellus aquaticus. 134 A. WARREN Fig. 9 Haplocaulus dipneumon, after Penard, 1922 (called Vorticella dipneumon). Bar = 25 um. Fig. 10 Haplocaulus distinguendus , (a) after Sommer, 1951; (b) after Bierhof & Roos, 1976 (called Haplocaulus distinguendis ) ; (c) after Liipkes, 1976 (called Haplocaulus hengsti). Bar = 50 um. Haplocaulus dipneumon (Penard, 1922) Stiller, 1971 Vorticella dipneumon Penard, 1922 DESCRIPTION (Fig. 9). Zooid almost cylindrical in shape, 50-56 urn long x 25 urn wide. Peristomial lip well developed, 25-30 urn in diameter. Disc convex and raised centrally to a point. Infundibulum almost reaches centre of zooid. Two contractile vacuoles situated in upper one-third of body. Macronucleus elongate and lies HAPLOCA ULUS MORPHOLOGICAL RELATIVES 135 longitudinally with respect to the major body axis. Transverse striations visible on pellicle. Stalk less than body length. Spasmoneme flared at either end. HABITAT. Freshwater, originally found as an epizoite of the crustacean Gammarus pulex. NOTE. This species bears a strong morphological resemblance to Baikalonis. Until its mode of contraction has been described, however, H. dipneumon should remain in the genus Haplocaulus. Haplocaulm distinguendus Sommer, 1951 Haplocaulus distinguen dis (Sommer, 1951) Bierhof & Roos, 1976 H. hengsti Liipkes, 1976 DESCRIPTION (Fig. 10). Zooid ovoid, 60-79 um long x 34—49 um wide, and constricted beneath peristome. Peristomial lip well developed, 27-40 um in diameter. Disc convex. Infundibulum broad and reaches almost to centre of body. Contractile vacuole situated in upper half of zooid. Macronucleus irregular or C-shaped. Transverse pellicular striations visible on zooid. Stalk up to 190 um long x 7-0-9-0 um wide. HABITAT. Freshwater, attached to the river weed Enteromorpha intestinalis (Sommer 1951), to inanimate substrates (Liipkes, 1976), and to the crustaceans Asellus aquations (Sommer, 1951) and Gammarus spp. (Bierhof & Roos, 1976). NOTE. H. hengsti is synonymysed with H. distinguendus because of their morphological similarity. The main differences between the two are the size of the zooid, H. hengsti (79 jim) being slightly longer than H. distinguendus (60-75 um), and stalk length (H. distinguendus up to 190 um long: H. hengsti — less than body length). Neither of these characters are particularly reliable for separating species, and there are insufficient differences here to recognise the two as separate taxa. Haplocaulus eforianus (Tucolesco, 1962) n. comb Vorticella eforiana Tucolesco, 1 962 DESCRIPTION (Fig. 1 1). Zooid 55-60 um long x 20 um wide. Upper part of body cylindrical in shape, lower part conical. Peristomial lip 20-25 urn in diameter. Pellicle with transverse striations, and convex ribbing between the striations. Pellicle also ornamented with numerous knob-like projections. Stalk x 1-x 2 body length. HABITAT. Marine Fig. 11 Haplocaulus eforianus, (a) relaxed zooid; (b) contracted zooid; (c) pellicle, showing convex ribbing and knob-like projections, after Tucolesca, 1962 (called Vorticella eforiana). Bar = 25 um. 136 A. WARREN Fig. 12 Haplocaulus elegans (a) showing macronucleus; (b) relaxed zooid, after Nenninger, 1948 (called Vorticella elegans); (c) after Szczepanowski, 1978. Bar = 50 urn. Fig. 13 Haplocaulus epizoicus (a) after Sramek-Husek, 1948 (called Vorticella epizoica), bar = 25 urn; ) after Piesik, 1975, bar = 25 urn. Haplocaulus elegans (Wenninger, 1948) Stiller, 1971 Intranstylum elegans Nenninger, 1948 Haplocaulus elegans f. gammari Piesik, 1975 DESCRIPTION (Fig. 1 2). Zooid 42-84 um long, constricted beneath the peristome and tapering posteriorly towards the stalk. Diameter of peristomial lip less than maximum body width. Disc convex. Contractile vacuole situated in upper one-third of zooid. Macronucleus C-shaped and lies horizontally in the anterior part of the body. Pellicular striations not observed. Stalk x 1- x 2 body length. HABITAT. Freshwater, originally found attached to the crustaceans Asellus aquaticus and Cyclops sp. HAPLOCAULUS MORPHOLOGICAL RELATIVES 137 Fig. 14 Haplocaulus extensus (a) relaxed zooid; (b) contracted zooid, after Kahl, 1 935 (called Vorticella extensa) . Bar = 50 urn. Haplocaulus epizoicus (Sramek-Husek, 1948) Stiller, 1971 Vorticella epizoica Sramek-Husek, 1948 DESCRIPTION (Fig. 13). Zooid 25-46 um long x 18-37 um wide, inverted bell-shaped and rounded posteriorly. Diameter of peristomial lip about equal to maximum body width. Contractile vacuole situated just beneath peristome. Macronucleus C-shaped and lies either horizontally or obliquely in the anterior part of the zooid. Pellicle with fine transverse striations. Stalk x 1- x 2 body length. HABITAT. Freshwater, found as an epizoite of the crustaceans Megacyclopsis viridis (Sramek-Husek, 1948) and Gammamspulexfossarum (Piesik, 1975). Haplocaulus extensus (Kahl, 1935)Sommer, 1951 Vorticella extensa Kahl, 1935 DESCRIPTION (Fig. 14). Zooid elongate, 50-100 um long xl 5-27 urn wide (Kahl (1935) described two morphological forms of this species, one 90-100 urn the other 50-70 urn long). Peristomial lip 35 um in diameter. Contractile vacuole situated just beneath peristome. Macronucleus C-shaped and lies transversely in anterior part of zooid. Pellicle with fine transverse striations. Stalk up to 200 um long. HABITAT. Freshwater, found by Sommer (1951) attached to the river weed Enteromorpha intestinalis. Haplocaulus fluviatilis Shubernetskij & Chorik, 1977 DESCRIPTION (Fig. 15). Zooid barrel-shaped with broadened scopular region, 28-48 um (mean 38 um) long x 14-30 jim (mean 22 um) wide. Peristomial lip 17-25 um (mean 21 um) in diameter. Disc elevated at angle to peristome and raised centrally to a point. Infundibulum reaches one-third body length. Contractile vacuole situated just beneath peristome. Macronucleus C-shaped and lies horizontally across upper part of zooid. Pellicle with distinct transverse striations, and convex ribbing between the striations. Stalk up to 50 um long. HABITAT. Freshwater, originally found attached to the ostracod Heterocypris. 138 A. WARREN Fig. 15 Haplocaulusfluviatilis, after Shubernetskij & Chorik, 1977. Bar = 25 urn. Fig. 16 Haplocaulus fusiformis, after Nenninger, 1948 (called Vorticellafusiforma). Bar = 75 um. Fig. 17 Haplocaulus kahlii (a) & (b) after Stiller, 1931 (called Vorticella kahlii) ; (c) after Bierhof & Roos, 1976. Bar = 25 urn. Haplocaulus fusiformis (Nenninger, 1948) Stiller, 1971 Vorticellafusiforma Nenninger, 1948 DESCRIPTION (Fig. 16). Zooid 140-162 um long x 60 um wide, spindle-shaped with prominent central bulge. Peristomial lip 45 um in diameter. Disc prominent and conical in shape. Infundibulum reaches one-quarter body length. Contractile vacuole situated in upper one-third of zooid. Macronucleus U-shaped and lies in anterior half of body. Food vacuoles large, dark and hexagonal in shape. Fine transverse striations visible on pellicle. Stalk less than body length. HABITAT. Freshwater, originally found attached to the tails of tadpoles. NOTE. Food vacuoles are not accepted as a taxonomic character among the Vorticellidae (Noland & Finley, 1931; Warren, 1986) or, indeed, the rest of the phylum Ciliophora. HAPLOCAULUS MORPHOLOGICAL RELATIVES Haplocauluskahlii (Stiller, 1931) Sommer, 1951 139 yorticellakahlii Stiller, 1931 DESCRIPTION (Fig. 1 7). Zooid pyriform with prominent bulge in anterior region, 32-44 um long x 24-36 um wide. Peristomial lip well developed, occasionally with central furrow giving the appearance of a double lip. Diameter of lip less than maximum body width. Macronucleus elongate, variable in shape. Pellicle distinctly striated with convex ribbing between striations. Stalk equal to or less than body length. HABITAT. Freshwater, found as an epizoite of the crustaceans Leptodora kindlii, Daphnia longispina var hyalina and Salpinia sp. (Stiller, 1931), Megacyclopsis viridis (Sramek-Husek, 1948), and Gammarus tigrinus (Bierhof & Roos, 1976). Haplocaulus leanderi Stiller, 1968 DESCRIPTION (Fig. 18). Zooid inverted bell-shaped, 30-32 um long x 22-24 um wide. Peristomial lip well developed, 26-28 um in diameter. Infundibulum reaches one-third body length. Macronucleus C-shaped and lies horizontally in anterior half of body. Pellicle furnished with numerous small granules. Stalk x 1- x 2 body length. HABITAT. Marine, originally isolated as an epizoite of the crustacean Leander sp. Haplocaulus longinuclei Banina, 1982 DESCRIPTION (Fig. 19). Zooid 43-61 um long x 41-49 um wide, somewhat variable in shape but usually oval or spherical and tapering sharply towards the stalk. Diameter of peristomial lip less than maximum body width. Infundibulum reaches centre of zooid. Macronucleus elongate and irregular in shape. Fine transverse striations visible on pellicle. Stalk less than body length. HABITAT. Freshwater, originally isolated as epizoites of tadpoles of the amphibian Rana temporaria. Haplocaulus macronucleatm (Nenninger, 1948) Stiller, 1971 Vorticella extensa var macronucleata Nenninger, 1948 DESCRIPTION (Fig. 20). Zooid elongate almost cylindrical in shape, 91-5 um long x 35 um wide. Diameter of peristomial lip about equal to maximum body width. Disc convex and raised centrally to a point. Contractile vacuole small and situated in upper one-third of body. Macronucleus broad, S-shaped and lies longitudinally with respect to major body axis. Pellicular striations not visible. Stalk about equal to body length. HABITAT. Freshwater, originally isolated as an epizoite of the hexapod Ephemera vulgata. Fig. 18 Haplocaulus leanderi, after Stiller, Bar = 25um. 1 968. Fig. 19 Haplocaulus longinuclei (a) relaxed zooid; (b) contracted zooid, after Banina, 1982. Bar = 25 um. 140 A. WARREN Fig. 20 Haplocaulus macronucleatus, after Nenninger, 1948 (called Vorticella extensa var. macronucleata) . Bar = 50 urn. Fig. 21 Haplocaulus pelagicus, after Gajewskaja, 1933 (called Vort icella pelagica) . Bar = 25 um. Fig. 22 Haplocaulus procerus , after Nenninger, 1948 (called Vorticella procera). Bar = 50 urn. Fig. 23 Haplocaulus sertulariarum, after Entz, 1884 (called Spastostyla sertulariarum). Bar = 50 urn. Haplocaulus pelagicus (Gajewskaja, 193 3) Stiller, 1971 Vorticella pelagica Gajewskaja, 1933 DESCRIPTION (Fig. 21). Zooid conical or inverted bell-shaped, 30-40 um long x 50 urn wide. Peristomial lip 70 um in diameter. Contractile vacuole situated just below peristome. Macronucleus elongate, irregular in shape and lies longitudinally with respect to major body axis. Pellicular striations not visible. Stalk usually less than body length. HABITAT. Marine HAPLOCA UL US MORPHOLOGICAL RELATIVES 1 4 1 Haplocaulm procerus (Nenninger, 1948) Stiller, 1971 Vorticella procera Nenninger, 1948 DESCRIPTION (Fig. 22). Zooid elongate, almost cylindrical in shape, 103 um long x 40 um wide. Peristomial lip 50 ^m in diameter. Disc flat. Contractile vacuole situated just beneath peristomial lip. Macronucleus C- shaped and lies either horizontally or obliquely in the anterior part of the zooid. Food vacuoles typically large. Fine transverse striations visible on pellicle. Stalk x 2- x 3 body length. HABITAT. Freshwater, originally found attached to the tails of tadpoles. Typically forms pseudocolonies. Haplocaulus sertulariarum (Entz, 1884)Banina, 1982 Spastostyla sertulariarum Entz, 1884 Vorticella sertulariarum (Entz, 1884)Kahl, 1935 DESCRIPTION (Fig. 23). Zooid inverted bell-shaped, 60-109 um long x 34-48 um wide. Diameter of peristomial lip greater than maximum body width. Disc flat. Infundibulum reaches centre of zooid. Contractile vacuole situated just beneath peristome. Macronucleus C-shaped and lies horizontally across centre of anterior part of zooid. Zoochlorellae may be present in cytoplasm. Stalk broad, and equal to or less than body length. Stalk sheath frequently with distinct transverse folds. HABITAT. Freshwater or marine, originally isolated from the Bay of Naples attached to polyps and sea urchins (Entz, 1884); also found as epizoites of tadpoles ofRana temporaria. NOTE. Entz (1884) considered this organism to be identicle to Rhabdostyla sertularium Kent, 1881. Rhabdostyla sertularium, however, does not possess a spasmoneme and the stalk is non-contractile whereas Entz's organism clearly has a spasmoneme. S. sertulariarum Entz, 1884 was transferred to Vorticella by Kahl (1935) and, more recently, to Haplocaulus by Banina (1982). Haplocaulus stilleri Piesik, 1975 DESCRIPTION (Fig. 24). Zooid spindle-shaped, 60 um long x 27 um wide, with prominent central bulge. Peristomial lip 20 um in diameter. Disc convex. Contractile vacuole situated just beneath peristome. Macro- nucleus C-shaped and lies horizontally across centre of zooid. Pellicular striations not observed. Stalk up to 60 um long and 12 um wide. HABITAT. Freshwater, originally described as an epibiont attached to the crustaceans Gammarus pulex pulex (L) and Gammarus pulex fossarum (Koch). Fig. 24 Haplocaulus stilleri, after Piesik, 1 975. Bar = 50 um. 142 A. WARREN Fig. 25 Haplocaulus terrenus, showing variability in relaxed and contracted zooids, (a) relaxed; (b) contracted, bar = 25 ^irn; (c) relaxed, bar = 25 ^im; (d) contracted, bar= 15 nm, after Foissner, 1981. Fig. 26 Haplocaulus walteri, (a) typical zooid; (b & c) variations in zooid shape under poor conditions; (d) telotroch, after Guhl, 1985. Bar = 25 urn. HAPLOCA ULUS MORPHOLOGICAL RELATIVES 1 43 Haplocaulus terrenm Foissner, 1 98 1 DESCRIPTION (Fig. 25). Zooid somewhat variable in shape, 40-60 um long x 20-26 nm wide. Peristomial lip 20 urn in diameter. Infundibulum reaches centre of zooid. Contractile vacuole large, situated in anterior part of zooid and empties into infundibulum via a short channel. Macronucleus C-shaped and lies either horizon- tally or obliquely across centre of body. Zooid has 30 transverse striations with concave ribbing between striations. Stalk 2-5-3-5 um wide, and one-half— x 3 body length. Upon contraction posterior end of zooid may become folded, overlapping the stalk. HABITAT. Terrestrial, originally isolated from Alpine soils. Haplocaulus vealteri Guhl, 1985 DESCRIPTION (Fig. 26). Zooid 55-75 um long x 40-60 um wide, cylindrical to inverted bell-shaped. Diameter of peristomial lip usually less than maximum body width. Infundibulum short. Contractile vacuole situated just below peristome. Macronucleus J- or 7-shaped. Pellicular striations not observed. Stalk up to 158 um long, and with rod-shaped bacteria attached to the stalk sheath. HABITAT. Freshwater, originally found in activated sludge. Genus BAIKALONIS Jankowski, 1982 The main distinguishing feature of this genus is the mode of contraction during which the stalk shortens longitudinally and is enveloped by the zooid. When Baikalonis was first described (Jankowski, 1982) just one species, B.foissneri, was known. B.foissneri thus became the type species by monotypy. Two more species, Vorticella undulata (Dons, 1918) Noland & Finley, 1931 and Haplocaulus sp. Bierhof & Roos, 1976 are here transferred to Baikalonis. Three other species of Haplocaulus, H. amphiurae, H. dipneumon and H.fusca, also bear a strong morphological resemb- lance to Baikalonis although their modes of contraction have yet to be described. DIAGNOSIS. Solitary, borne upon an unbranched stalk which is typically much shorter than the body. Spasmoneme straight and extends the entire length of the stalk. Upon contraction, the zooid envelopes the stalk which shortens longitudinally. Key to the species of Baikalonis 1 Freshwater; zooid with a contractile vacuole 2 Marine; zooid without a contractile vacuole B. undulata 2 Infundibulum broad and reaches centre of zooid. Contractile vacuole centrally located. Peristomial lip with central furrow B.foissneri Infundibulum lies diagonally and reaches one-third body length. Contractile vacuole situated just below peristome. Peristomial lip without a furrow B. gammari Species descriptions Baikalonis foissneri Jankowski, 1982 DESCRIPTION (Fig. 27). This the type species is cylindrical in shape, 56-60 um long x 20 um wide. Peristomial lip well developed with central furrow giving the appearance of a double lip. Disc prominently arched above peristome. Infundibulum broad and reaches centre of zooid. Contractile vacuole situated centrally in body. Macronucleus cylindrical in shape and slightly curved. Stalk 12-14 um long. Spasmoneme broad. HABITAT. Freshwater, originally found as an epizoite of the larvae of the caddis-fly Baicalina bellicosa in Lake Baikal, U.S.S.R. Baikalonis gammari n. sp. Haplocaulus sp. Bierhof & Roos, 1976 DESCRIPTION (Fig. 28). Zooid cylindrical in shape, narrowing slightly towards the stalk, 75 um long x 45 um wide. Peristomial lip well developed, diameter about equal to maximum body width. Infundibulum reaches one-third body length. Contractile vacuole situated just below peristome. Macronucleus C-shaped and lies longitudinally in centre of zooid. Fine transverse striations visible on pellicle. Stalk 10 um long x 8 um wide. HABITAT. Freshwater, originally isolated as an epizoite of the crustacean Gammarus pulex. 144 A. WARREN Fig. 27 Baikalonis foissneri, (a) relaxed; (b) contracted, after Jankowski, 1982. Bar = 25 um. Fig. 28 Baikalonis gammari, after Bierhof & Roos, 1976 (called Haplocaulus sp.). Bar = 50 um. Fig. 29 Baikalonis undulata, (a) relaxed; (b) contracted, after Dons, 1918 (called Vorticellopsis undulata) . Bar = 50 um. Baikalonis undulata (Dons, 1918) n. comb. Vorticellopsis undulata Dons, 1918 Vorticella undulata (Dons, 1918)Noland& Finley, 1931 DESCRIPTION (Fig. 29). Zooid pyriform, 1 10 um long x 72 um wide. Peristomial lip 57 um in diameter. Two distinct constrictions present on body, one beneath the peristomial lip and the other in the region of the telotroch band. Contractile vacuole not observed. Macronucleus C-shaped, 30 um long x 20 nm wide and lies longitudinally with respect to major body axis. Transverse striations clearly visible on pellicle. Stalk 1 15 um long x 19 um wide. Spasmoneme 12 um in diameter. HABITAT. Marine, originally found attached to the alga Desmaresita viridis. HAPLOCAULUS MORPHOLOGICAL RELATIVES 145 NOTE. Both Noland & Finley (1931) and Kahl (1935) considered that Vorticellopsis undulata Dons, 1918 should belong to the genus Vorticella. In a recent revision of Vorticella, Warren (1986) noted that the stalk of V. undulata does not contract spirally and should not, therefore, be included in the genus Vorticella. The mode of contraction and the morphology of the stalk both indicate that this species should belong to the genus Baikalonis. Genus COTENSITA Jankowski, 1982 The main distinguishing feature of the genus Cotensita is the stalk sheath which is folded in a characteristic fashion just beneath the zooid. Although some colonial peritrichs such as Craspedo- myoschiston have ornamentation of the stalk sheath, this feature has not previously been recorded among solitary vorticellids. The spasmoneme of Cotensita is straight and extends to about two- thirds of the stalk length. C. commensalis Jankowski, 1982 is the type species by monotypy. DIAGNOSIS. Spasmoneme straight, not extending the full length of the stalk. Stalk sheath twisted in the region just below the stalk. Upon contraction the zooid bends over to one side and assumes a characteristic 'nodding' position. Species description Cotensita commensalis Jankowski, 1982 DESCRIPTION (Fig. 30). This the type species is inverted bell-shaped, 46 um long x 36 um wide. Diameter of peristomial lip about equal to maximum body width. Contractile vacuole situated just beneath peristome. Macronucleus C-shaped. Stalk 85-90 um long. Stalk sheath twisted to form 1-2 helical coils just below zooid. Spasmoneme reaches two-thirds stalk length with the posterior end tapering to a point. HABITAT. Freshwater, originally isolated as an epizoite of the larvae of the caddis-fly Baicalina bellicosa from Lake Baikal, U.S.S.R. Genus PARAZOOTHAMNIUMPiesik, 1975 The main distinguishing feature of this genus is the mode of stalk contraction which takes place in two stages: initially the stalk shortens longitudinally in a concertina-like fashion but, if the stimulus is sufficiently strong, it loops and bends in the more usual manner. Fig. 30 Cotensita commensalis, (a) relaxed zooid, bar = 25 um. (b) partially contracted; (c) detail of stalk, after Jankowski, 1982. 146 A. WARREN Fig. 31 Parazoothamnium stenotica, after Piesik, 1975. Bar = 50 urn. Fig. 32 Parazoothamnium claparedei, (a) relaxed zooid; (b) contracted, after Andrussowa, 1886 (called Vorticella claparedei). Bar = 50 nm. Fig. 33 Piesika gammari, after Piesik, 1975 (called Parazoothamnium gammari) . Bar = 50 urn. Piesik (1975) originally described two species of Parazoothamnium, P. stenotica and P. gammari. The latter species, however, has rows of regularly arranged tubercles and, since this is recognised as a generic character among the Vorticellidae, P. gammari is transferred to the new genus Piesika. P. claparedeiis included in the genus Parazoothamnium for the first time. P. stenotica is designated the type species. DIAGNOSIS. Solitary, borne upon an unbranched stalk. Spasmoneme extends the complete length of the stalk. Stalk contraction takes place in two stages; initially it shortens longitudinally in a HAPLOCA ULUS MORPHOLOGICAL RELATIVES 1 47 concertina-like fashion but, if the stimulus is sufficiently strong, it loops and folds. Zooid has a transverse silverline system. Key to the species of Parazoothamnium 1 Macronucleus J-shaped; contractile vacuole situated in anterior half of body . P. stenotica Macronucleus C-shaped; contractile vacuole situated in posterior half of body . P. claparedei Species descriptions Parazoothamnium stenotica Piesik, 1975 DESCRIPTION (Fig. 31). This the type species is inverted bell-shaped, somewhat rotund, 70 um long x 50 um wide. Peristomial lip well developed, diameter about equal to maximum body width. Contractile vacuole situated just beneath peristome. Macronucleus J-shaped. Pellicle with fine transverse striations. Stalk up to 9-0 um wide. HABITAT. Freshwater, originally isolated as an epizoite of the crustacean Gammarus pulex. Parazoothamnium claparedei (Andrussowa, 1886) n. comb. Vorticella claparedei Andrussowa, 1 886 DESCRIPTION (Fig. 32). Zooid campanulate, 85 urn long x 60 um wide and with a distinct swelling just below the peristome. Peristomial lip 60 um in diameter and with a central furrow to give the appearance of a double lip. Disc raised obliquely above peristome. Infundibulum reaches centre of zooid. Single contractile vacuole situated in posterior half of zooid. Macronucleus C-shaped and lies longitudinally with respect to major body axis. Pellicular striations not observed. Upon contraction stalk sheath assumes a wrinkled appearance and stalk coils into two or three unevenly spaced loops. HABITAT. Marine, attached to filamentous algae. Genus PIESIKA n. gen. The possession of regularly arranged pellicular tubercles along with an underlying reticulate silverline system is regarded as a generic character among peritrichs (Foissner & SchifTmann, 1 974; Warren, 1986). The genus Piesika is erected to include solitary vorticellids which both possess pellicular tubercles, and exhibit the two stage stalk contraction process seen in Parazoothamnium. P. gammari is the type species by monotypy. DIAGNOSIS. Solitary zooids borne upon an unbranched stalk. Spasmoneme extends the complete length of the stalk. Contraction of the stalk takes place in two stages; initially the stalk shortens longitudinally in a concertina-like fashion but, if the stimulus is sufficiently strong, it loops and folds. Zooid with rows of regularly aligned pellicular tubercles. Species description Piesika gammari (Piesik, 1975) n. comb. Parazoothamnium gammari Piesik, 1 975 DESCRIPTION (Fig. 33). This the type species is inverted bell-shaped, 70 um long x 50 um wide. Diameter of peristomial lip about equal to maximum body width. Disc convex. Contractile vacuole situated just below peristome. Macronucleus elongate and irregular in shape. Stalk up to 240 um long x 10 um wide. Cysts nearly spherical in shape, 49 um x 43 um. HABITAT. Freshwater, originally found as an epizoite of the crustacean Gammarus pulex pulex. Genus PSEUDOHAPLOCA ULUS n. gen. Foissner & SchifTmann ( 1 974) reported that two types of silverline system are found among vorticellids; (i) transverse, in which the lines encircle the body in one direction only, and (ii) reticulate, which consists of a network of vertical and horizontal lines. Furthermore, it has been established that vorticellids with regularly arranged rows of pellicular tubercles also possess reticu- late silverline systems (Foissner, 1979, 1981; Carey & Warren, 1983; Warren, 1987). The genus Pseudohaplocaulus is erected to include Haplocaulus-\ike peritrichs which possess rows of regularly aligned pellicular tubercles and, therefore, reticulate silverline systems. There are two species of 148 A. WARREN Fig. 34 Pseudohaplocaulus nicoleae, after Precht, 1935 (called Haplocaulus nicoleae). Bar = 25 um. Fig. 35 Pseudohaplocaulus anabaenae, after Stiller, 1940 (called Vorticella anabaenae). Bar = 25 um. Pseudohaplocaulus, both formerly belonging to the genus Haplocaulus. Pseudohaplocaulus nicoleae (Precht, 1935) n. comb, is the type species. DIAGNOSIS. Solitary, borne upon an unbranched stalk that is circular in cross-section and contracts in a zigzag manner. Zooid with rows of regularly aligned pellicular tubercles and a reticulate silverline system. Key to species of Pseudohaplocaulus 1 Marine. Zooid with one contractile vacuole ....... P. nicoleae Freshwater. Zooid with two contractile vacuoles P. anabaenae Species descriptions Pseudohaplocaulus nicoleae (Precht, 1935) n. comb. Haplocaulus nicoleae Precht, 1935 DESCRIPTION (Fig. 34). This the type species is inverted bell-shaped, 35-40 urn long x 25 um wide. Peristomial lip 30 urn in diameter. Contractile vacuole situated just below the peristome. Macronucleus J-shaped. Stalk x 1- x 2 body length. Sites of previous zooid division may be visible as short lateral extensions of the stalk sheath (see Fig. 34). HABITAT. Marine, originally found as an epizoite of the polychaete, Nicolea zostericola. Pseudohaplocaulus anabaenae (Stiller, 1940) n. comb. Vorticella anabaenae Stiller, 1940 Haplocaulus anabaenae Stiller, (1940) 1971 DESCRIPTION (Fig. 35). Zooid inverted bell-shaped, 40-45 urn long x 40 um wide. Peristomial lip 45 urn in diameter. Disc flat. Infundibulum reaches one-third body length. Two contractile vacuoles, one situated near the base of the infundibulum, the other just below the peristome. Macronucleus J-shaped. Stalk x 1- x 2 body length. HABITAT. Freshwater, originally isolated as an epibiont attached to the Cyanobacterium Anabaena. HAPLOCA ULUS MORPHOLOGICAL RELATIVES 1 49 Incertae Sedis Genus MONINTRANSTYLUM Banina, 1977 Monintranstylum is a solitary peritrich the stalk of which contracts in a zigzag rather than helical fashion. The main distinguishing feature of Monintranstylum is the spasmoneme which is short and terminates above the base of the stalk, unlike that of Haplocaulus and other related genera where the spasmoneme is usually about the same length as the stalk. Spasmoneme length has long been recognised as a generic character among colonial peritrichs. Intranstylum Faure-Fremiet, 1904, for example, differs from Carchesium Ehrenberg, 1830 by the absence of the spasmoneme in the central trunk of the stalk. Myoschiston Precht, 1935 may similarly be recognised from Zoothamnium Bory, 1826. Among the solitary peritrichs, however, the situation is less clear and several species belonging to genera in which the whole stalk is normally contractile, have short or otherwise incomplete spasmonemes. The spasmoneme of Vorticella intermissa Nenninger, 1948, for example, begins a short distance below the scopula and is therefore absent in the uppermost part of the stalk; and in Haplocaulus claudicans a small 'fibre' connects the short spasmoneme to the stalk base (see p. 132). Furthermore, the author has fre- quently observed both solitary and colonial peritrichs in which the spasmoneme appears to have partially degenerated and lost its contractility (unpublished data). Clearly, further research is necessary before spasmoneme length can be accepted as a generic character among solitary peritrichs. NOTE. The name Monintranstylum was first mentioned in an abstract (Banina, 1976). A full description of Monintranstylum, however, did not appear until the following year (Banina, 1977a), the date from which the genus should properly be recognised. The first named species of Monintranstylum were described in a second article later in the same journal (Banina, 1977b). No type species was designated. DIAGNOSIS. Zooid borne upon a stalk which contracts in a zigzag manner. Solitary, never colonial, and carried upon an unbranched stalk. Spasmoneme present only in the upper part of the stalk. Species of Monintranstylum Three species of Monintranstylum were described by Banina (19776), M. rotundus, an epibiont of Daphnia longispina; M. stammeri, an epibiont of Polyphemus pediculus, Daphnia pulex, Ceriodaphina quadrangulata and Cyclops sp.; and M. sommeri on the abdomen of Eucydops serrulatus and the shell of Cypris sp. The original descriptions of these species were not available for this revision. Banina (1982) also transferred Intranstylum ranae Stiller, 1953 to the genus Monintranstylum on the basis that /. ranae is solitary rather than colonial, and that its spasmoneme terminates above the base of the stalk. However, for the reasons given above, M. ranae and the three other species of Monintranstylum may perhaps more properly belong to the genus Haplocaulus. Monintranstylum ranae (Stiller, 1953) Banina, 1982 Intranstylum ranae Stiller, 1953 DESCRIPTION (Fig. 36). Zooid 65-90 um long x 35-50 um wide. Diameter of peristomial lip usually less than the maximum body width. Contractile vacuole situated just below the peristome. Macronucleus variable, usually S-shaped. Pellicle with fine transverse striations. Stalk up to x 3 body length. Stalk base flattened to form a large attachment area, the diameter of which often exceeds that of the body. HABITAT. Freshwater, attached to the tail fins of frog tadpoles. Genus TVCOLESCA (Tucolesco, 1962) Lorn in Corliss, 1979 Leptodiscus Tucolesco, 1962. The main distinguishing features of this genus are (i) the reported absence of a peristomial lip, and (ii) upon contraction, the peristome remains open with the cilia extended while the stalk folds into several (usually three) loose coils. T. mirabilis is the type species by monotypy. The name originally assigned to this genus was Leptodiscus, a homonym of the dinoflagellate 150 A. WARREN Fig. 36 Monintranstylum ranae, (a) typical form; Fig. 37 Tucolesca mirabilis, after Tucolesco, 1962 showing variability of (b) zooid, and (c) macro- (called Leptodiscus mirabilis). Bar = 25 um. nucleus, after Stiller, 1953 (called Intranstylum ranae). Bar = 50 urn. Leptodiscus Hartwig, 1877 (Corliss, 1979). The genus was renamed Tucolesca by Lorn (unpub- lished— see Corliss, 1979). The taxonomic status of the genus and validity of the name are both considered doubtful. DIAGNOSIS. Zooid with long, prominent cilia and without a peristomial disc. Upon contraction, peristome remains open with the cilia extended while the stalk is folded into several loose coils. Species description Tucolesca mirabilis (Tucolesco, 1962) Lom Leptodiscus mirabilis Tucolesco, 1962 DESCRIPTION (Fig. 37). Zooid 27-30 urn long x 19 um wide. Peristomial lip 20 urn in diameter and obliquely orientated with respect to major body axis. Cilia 16-19 um long. Infundibulum reaches two-thirds of the body length. Contractile vacuole located near base of infundibulum. Macronucleus S-shaped and moniliform. Stalk up to 80 um long. HABITAT. Originally isolated from Lake Tekirghiol, a saline lake in Romania. References Banina, N. N. 1976. (Some consideration of the systematics of the families of the Aloricata (Peritricha Sessilina Kahl, 1935). Abstr.— in Russian). Mat. 11 All-Union Congress of Protozoology Pt. 1: 20-22. 1977a. (Morphological — systematical descriptions of Peritricha Sessila. — in Russian) Trudy Gosniorh 119:5-11. 19776. (New species of Peritricha on planktonic organisms of Ropsha ponds.- -in Russian) Trudy Gosniorh 119: 24-38. 1982. (Ciliates of Peritricha, Sessilina in amphibians from Leningrad environs. — in Russian). Parazitologiya 16: 1 44 - 1 5 1 . Bierhof, M. J. & Rons, P. J. 1976. Sedentary ciliates from two Dutch freshwater Gammarus species. Bijdragen tot de Dierkunde 46: 1 5 1-1 70. Bory de St. Vincent 1826. Essaid'une Classification des Animaux Microscopiques. Paris, 104 pp. HAPLOCA ULUS MORPHOLOGICAL RELATIVES 1 5 1 Carey, P. G. & Warren, A. 1983. The role of surface topography in the taxonomy of peritrich ciliates. Protistologica 19: 73-89. Corliss, J. O. 1979. The Ciliated Protozoa: Characterisation, Classification and Guide to the Literature, 2nd edition, Pergamon Press, Oxford, 455 pp. Cuenot, L. 1891. Protozoaires commensaux et parasites des echinodermes. Revue Biologique du Nordde la France 3: 292-293. Curds, C. R., Roberts, D. McL & Gates, M. A. 1983. British and other freshwater ciliated protozoa. Part 2. Ciliophora: Oligohymenophora and Polymenophora. Synopsis of the British Fauna (NS), 22: pp.387, London, Linnean Society. Dons, C. 1918. Neue marine Ciliaten und Suctorien. Tromso Museums Aarshefter 38-39 (yr 1915-1916)- 75-100. Ehrenberg, C. G. 1830(1832). Beitrage zur kenntnis der organisation der infusorien und ihrer geographischen verbeitung, besonders in Siberien. Abhandlungen der Akademie der Wissenschaften der DDR. Berlin Year 1832 1-88. Entz, G. 1 884. Uber infusorien des golfes von Neapel. Mittheilungen aus der Zoologischen Station zu NeapelS: 289-444. Faure-Fremiet, E. 1904. Sur la structure du pedoncle des Vorticellidae. Compte Rendu Hebdomadaire des Seances de I'Academie des Sciences. Paris 57: 506-508. Foissner, W. 1979. Peritriche ciliaten (Protozoa: Ciliophora) aus Alpinen kleingewassern. Zoologische Jahrbucher (Systematik) 106: 529-558. 1981 . Morphologic und taxonomie einiger heterotricher und peritricher ciliaten (Protozoa: Ciliophora) aus alpinen boden. Protistologica 17: 29-43. & Schiffmann, H. 1974. Vergleichende studien an argyrophilen strukturen von vierzehn peritrichen ciliaten. Protistologica 10: 489-508. Gajewskaja, N. 1933. Zur oekologie, morphologic und systematik der infusorien des Baikalsees. Zoologica. Stuttgart 32: 1-298. Guhl, W. 1985. Beitrag zur kenntnis der ciliatenfauna verschiedener belebtschlamme mit besonderer berucksichtigung der fruherkennung von blah- und schwimmschlammbildung an der variabilitat peri- tricher ciliaten. Archivfur Protistenkunde 129: 203-238. Jankowski, A. V. 1982. (New genera of protozoan symbionts for the fauna of Lake Baikal, Part 3. — in Russian). Izdalelistvo 'Nauka ' Sibirskoe otdelenie Novosibirsk p. 25-32. Kahl, A. 1935. Urtiere oder Protozoa. I: Wimpertiere oder ciliata (infusoria), eine bearbeitung der freileben- den und ectocommensalen infusorien der erde, unter ausschluss der marinen Tintinnidae. 4 Peritricha und Chonotricha. In: F. Dahl, ed., Die Tierwelt Deutschlands, Teil 30: 651-864. Kent, W. S. 1881. A Manual of the Infusoria vol II, Part V, pp. 577-720, London, David Brogue. Ltipkes, G. 1 975. Beitrag zur kenntnis der symphoriontenfauna auf trichopterenlarven: Haplocaulus brehmi n. sp. und Epistylis daxi n. sp., zwei neue peritrichen auf Agape tus fuscipes Larven. Symphoriontstudien 2. Protistologica 11: 295-296. 1976. Die vertikale verteilung von ciliaten im stygorhithral der fulda (beitrag zur kenntnis mesop- sammaler ciliaten in fliessgewassern). InternationalJournal of Speleology 8: 127-133. Nenninger, U. 1948. Die peritrichen der umgebung von erlangen mit besonderer berucksichtigung ihrer wirtsspezifitat. Zoologischer Jahrbucher (Systematik) 77: 169-266. Noland, L. E. & Finley, H. E. 1931. Studies on the taxonomy of the genus Vorticella. Transactions of the American Microscopical Society 50: 81-123. Penard, E. 1922. Etudes sur les Infusoires d'Eau Douce. George & Cie, Geneve, 331 pp. Piesik, Z. 1975. Orzeski epizoiczne kielzach w podrodzaju Rivulogammarus Karaman strumieni okolic Poznania. Badania Fizjogrqficzne nad Polska Zachodnia (Zoologica) 28: 41-77. Precht H. 1935. Epizoen der kieler bucht. Nova Acta Leopoldina Halle NF3: 405-474. Shubernetskij, I. V. & Chorik, F. P. 1977. (Epibiont peritricha infusoria (Ciliata: Peritricha) of the lower crustaceans. — in Russian). Izvestiya Akademii Nauk Moldavskoi SSR (Biologia) Year 1977: 61-66. Sommer, G. 1 95 1 . Die peritrichen ciliaten des grossen ploner sees. Archivfur Hydrobiologie 44: 349-440. Sramek-Husek, R. 1948. K Poznani planktonu a epizoonu stfedoceskych rybniku. Casopis Narodniho Musea 117: 67-81. Stiller J. 1940. Beitrag zur peritrichenfauna des grossen ploner sees in Holstein. Archivfur Hydrobiologie 36: 263-285. 1951. Die limnologischen verhaltnisse des naturschutzgebietes von batorliget in ungarn nebst beschrei- bung einiger neuer peritrichen-arten (Ciliata, Protozoa). Archivfur Hydrobiologie 56: 186-260. 1963. Zur limnologie der natrongewasser ungarns. I Der natronsee nagyszek und seine peritrichenfauna. Internationale Revue der Gesamten Hydrobiologie und Hydrographie 48: 603-612. 152 A. WARREN 1968. Peritriche ciliaten okologisch verschiedener biotope von rovinj und umgebung. Acta Zoologica Academiae Scientiarum Hungaricae 14: 185-21 1. 1971. Szajkoszorus Csillosok — Peritricha. Fauna Hungariae 105: 1-245. Stokes, A. C. 1 889. Notice on new peritrichous infusoria from the fresh waters of the United States. Journal of the Royal Microscopical Society 12: 477-482. Szczepanowski, P. 1978. (Epizoic Ciliata on Asellus aquaticus (L) of Poznah and surroundings.— in Polish). Prace Komisji Matematyczno- Przyrodniczej Poznanskie Towarszystwo Prvjacio Nank Poznan 47: 1-72. Tucolesco, J. 1962. 1. Especes nouvelles d'Infusoires de la Mer Noire et des bassins sales paramins. Archivfur Protistenkunde 106: 1-36. Warren, A. 1986. A revision of the genus Vorticella (Ciliophora: Peritrichida). Bulletin of the British Museum (Natural History). Zoology. London 50: 1-57. 1987. A revision of the genus Pseudovorticella Foissner & Schiffmann, 1974 (Ciliophora: Peritrichida). Bulletin of the British Museum (Natural History). Zoology. London 52(1); 1-12. Manuscript accepted for publication 14 July 1987 Index to species (Names given in roman refer to synonyms) Baikalonis foissneri 143 gammari 143 undulata 144 Cotensita commensalis 145 Haplocaulus amphibiarum 1 30 amphiurae 1 3 1 anabaenae 148 brehmi 1 3 1 carinogammari 131 claudicans 1 32 conosomus 133 crassicaulis 133 dipneumon 134 distinguendis 135 distinguendus 135 eforianus 135 elegans 1 36 elegans f. gammari 1 36 epizoicus 137 extensus 137 fluviatilis 137 fur cellar iae 129 fusiformis 138 hengsti 135 kahlii\39 leanderi 1 39 longinuclei 1 39 macronucleatus 139 nicoleae 148 pelagicus 140 procerus 141 sertulariarum 141 stiller i 141 terrenus 143 waiter i 143 Intranstylum elegans 136 ranae 149 Leptodiscus mirabilis 1 50 Monintranstylum ranae 149 rotundus 149 sommeri 149 stammeri 149 Parazoothamnium claparedei 147 gammari 147 stenotica 147 Piesika gammari 147 Pseudohaplocaulus anabaenae 148 nicoleae 148 Spastosty la sertulariarum 141 Tucolesca mirabilis 1 50 Vorticella amphiurae 131 anabaenae 148 carinogammari 131 claparedei 147 claudicans 132 conesoma 133 conosoma 133 crassicaulis 133 dipneumon 134 eforiana 135 epizoica 137 extensa 137 extensa var. macronucleata 139 fusiforma 138 kahlii 139 pelagica 140 procera 141 sertulariarum 141 undulata 144 Vorticellopsis undulata 144 British Museum (Natural History) The birds of Mount Nimba, Liberia Peter R. Colston & Kai Curry-Lindahl For evolution and speciation of animals Mount Nimba in Liberia, Guinea and the Ivory Coast is a key area in Africa representing for biologists what the Abu Simbel site in Egypt signified for archaeologists. No less than about 200 species of animals are endemic to Mount Nimba. Yet, this mountain massif, entirely located within the rain-forest biome, is rapidly being destroyed by human exploitation. This book is the first major work on the birds of Mount Nimba and surrounding lowland rain- forests. During 20 years (1962-1982) of research at the Nimba Research Laboratory in Grassfield (Liberia), located at the foot of Mount Nimba, scientists. from three continents have studied the birds. In this way Mount Nimba has become the ornithologically most thoroughly explored lowland rain-forest area of Africa. The book offers a comprehensive synthesis of information on the avifauna of Mount Nimba and its ecological setting. During the 20 years period of biological investigations at Nimba this in 1962 intact area was gradually opened up by man with far-reaching environmental consequences for the rain-forest habitats and profound effects on the birds. Therefore, the book provides not only a source of reference material on the systematics, physiology, ecology and biology of the birds of Mount Nimba and the African rain-forest, but also data on biogeography in the African context as well as conservation problems. Also behaviour and migration are discussed. At Nimba a number of migrants from Europe and/or Asia meet Afrotropical migratory and sedentary birds. Professor Kai Curry-Lindahl has served as Chairman of the Nimba Research Laboratory and Committee since its inception in 1962. Peter Colston is from the Subdepartment of Ornithology, British Museum (Natural History), Tring, and Malcolm Coe is from the Animal Ecology Research Group, Department of Zoology, Oxford. 1986, 129pp. Hardback. 0 565 00982 6 £17.50. Titles to be published in Volume 54 The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences. By Gordon J. Howes A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles. By Keith H. Hyatt & Rowan M. Emberson A revision of Haplocaulus Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives. By Alan Warren Echinoderms of the Rockall Trough and adjacent areas. 3. Additional records. By R. Harvey, J. D. Gage, D. S. M. Billet, A. M. Clark & G. L. J. Paterson Primed in Cireat Britain by Henry Ling Ltd., at the Dorset Press, Dorchester. Dorset (NATURA! - 1AI PRESENTED GEN; Bulletin of the British Museum (Natural History) Echinoderms of the Rockall Trough and adjacent areas 3. Additional records R. Harvey, J. D. Gage, D. S. M. Billett, Ailsa M. Clark & G. L J. Paterson Zoology series Vol 54 No 4 28 July 1988 The Bulletin of the British Museum (Natural History], instituted in 1949, is issued in four scientific series. Botany, Entomology, Geology (incorporating Mineralogy) and Zoology, and an Historical series. Papers in the Bulletin are primarily the results of research carried out on the unique and ever-growing collections of the Museum, both by the scientific staff of the Museum and by specialists from elsewhere who make use of the Museum's resources. Many of the papers are works of reference that will remain indispensable for years to come. Parts are published at irregular intervals as they become ready, each is complete in itself, available separately, and individually priced. Volumes contain about 300 pages and several volumes may appear within a calendar year. Subscriptions may be placed for one or more of the series on either an Annual or Per Volume basis. Prices vary according to the contents of the individual parts. Orders and enquiries should be sent to: Publications Sales, British Museum (Natural History), Cromwell Road, London SW7 5BD, England. World List abbreviation: Bull. Br. Mus. nat. Hist. (Zool.) © Trustees of the British Museum (Natural History), 1988 The Zoology Series is edited in the Museum's Department of Zoology Keeper of Zoology : MrJ. F. Peake Editor of Bulletin : Dr C. R. Curds Assistant Editor : Mr C. G. Ogden ISBN 0 565 05040 0 ISSN 0007-1498 Zoology series Vol54 No 4 pp 153- 198 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 28 July 1 988 Echinoderms of the Rockall Trough and adjacentT^ril^ 3. Additional records ., , 2 8 JUL )988 R. Harvey & J. D. Gage 1 Dunstaffnage Marine Research Laboratory, Scottish Marine Biological AW»ri*tirm rito. Jkv* -V.J Oban, Argyll PA34 4AD D. S. M. Billett Institute of Oceanographic Sciences, Brook Road, Wormley, Godalming, Surrey GU8 5UIT Ailsa M. Clark & G. L. J. Paterson Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD - 1AUGS98* Introduction This paper is the third part of a study primarily on the distribution of the echinoderm PRESENTED aunaofthe Rockall Trough. Part 1 dealt with the crinoids, asteroids and ophiuroids, while Part 2 covered the echinoids and holothurians (Gage et al. 1983, 19850). Taxonomic descriptions and discussion of new or problematic species in these collections are given separately in papers cited in the text. The present paper results from sampling undertaken from RRS Challenger by the Scottish Marine Biological Association (SMBA) since the publication of Parts 1 and 2. This has resulted in the recovery of four additional species of crinoids, ten asteroids, seven ophiuroids, one echinoid and eight holothurians. Of these, one asteroid, the goniasterid Mediaster bairdi, is a new record for the NE. Atlantic while another, a pterasterid, appears to be undescribed. Seven of the species mentioned in Parts 1 and 2 (one crinoid, one ophiuroid, one asteroid, one echinoid and three holothurians) are identified or re-identified as a result of further research. Additional records of species included in Parts 1 and 2 are given, together with a summary of the zoogeographic and bathymetric distribution with details of any range extension within the Trough provided by the new records. These data have mainly resulted from a greater intensity of sampling effort in the depth range 500-2000 m than in the period 1973 to 1982 covered by the previous papers. The majority of new records are from the Feni Ridge and Hebridean Slope, the latter having been obtained largely from fishing cruises by Dr J. D. M. Gordon of SMBA using a semi-balloon otter trawl (Gordon, 1986). In addition to records from new stations, an updated total is given for the number of specimens recovered from old stations where sorting of additional subsamples have provided more material. The depth range at the end of the list of stations for each species is the new range within the Rockall Trough area as indicated by our samples. The format of Part 3 broadly follows that of the two previous papers. Details of the gears employed in the sampling programme may be found in Part 1, while lists of sampling stations worked are distributed among all three parts. List of Species Only species additional to those included in Parts 1 and 2 are listed below. An asterisk denotes species included in Parts 1 and 2 under another name. Class Crinoidea Order Millericrinida Family Bathycrinidae Bathycrinus gracilis Wyville Thomson *Democrinus parfaiti Perrier Bull. Br. Mm. not. Hist. (Zool.) 54(4): 153-198 Issued 28 July 1988 153 1 54 HARVEY, GAGE, BILLETT, CLARK & PATERSON Order Comatulida Family Antedonidae Trichometra cubensis (Pourtales) Poliometra prolixa (Sladen) Family Atelecrinidae Atelecrinus balanoides (P. H. Carpenter) Class Asteroidea Order Paxillosida Family Astropectinidae * Persephonaster patagiatus (Sladen) Order Notomyotida Family Benthopectinidae Cheiraster sepitus (Verrill) Order Valvatida Family Asterinidae Anseropoda placenta (Pennant) Family Goniasteridae Ceramaster granularis (Retzius) Mediaster bairdi (Verrill) Family Poraniidae Chondt -aster grandis (Verrill) Poraniomorpha hispida rosea Danielssen & Keren Order Spinulosida Family Pterasteridae Pteraster ( Apterodon) sp. Diplopteraster multipes (M. Sars) Hymenaster regalis Verrill Order Brisingida Family Brisingidae Novodinia pandina Sladen Order Forcipulatida Family Asteriidae Neomorphaster talismani E. Perrier Class Ophiuroidea Order Phrynophiurida Family Ophiomyxidae Ophiomyxa serpentaria Lyman Ophioscolex glacialis Miiller & Troschel Ophiophrixus spinosus (Storm) Order Myophiurida Family Ophiacanthidae Subfamily Ophiacanthinae Ophiolebes bacata Koehler Subfamily Ophiotominae Ophiotoma coriacea Lyman Subfamily Ophioplinthacinae Ophiomitrella clavigera (Ljungman) Family Amphiuridae Amphiura tritonis Hoyle Family Ophiuridae Subfamily Ophiurinae *Ophiura scomba Paterson Class Echinoidea Order Spatangoida Family Spatangidae *Brissopsis ?lyrifera (Forbes) Brisaster fragilis (Diiben & Koren) ROCKALL TROUGH ECHINODERMS 3 1 55 Class Holothurioidea Order Dendrochirotida Family Paracucumidae Paracucumaria hyndmani (Thompson) Family Sclerodactylidae Pseudothyone raphanus (Duben & Koren) Family Cucumariidae Thyonefusus(O. F. Muller) Order Aspidochirotida Family Synallactidae Mesothuria intestinalis (Ascanius & Rathke) Mesothuria verrilli (Theel) Order Elasipodida Family Elpidiidae Ellipinion delagei (Herouard) Order Apodida Family Synaptidae Leptosynapta decaria (Ostergren) Family Myriotrochidae *Myriotrochus clarki Gage & Billett * Prototrochus zenkevitchi rockallensis Gage & Billett * Parvotrochus belyaevi Gage & Billett Order Molpadiida Family Caudinidae Hedingia albicans (Theel) Systematic Account A chart showing the localities of all records covered by the three papers is given in Fig. 1 . Classification of the Ophiuroidea follows Fell (1982). Treatment of the other four classes follows Parts 1 & 2 with the following exceptions: Asteriidae Blake ( 1 987), Brisingidae Downey ( 1 986), and Dendrochirotida Panning (1949) as amended by Pawson & Fell (1965). References to works describing species have only been given for those species which are listed here for the first time or where a new work has appeared since the publication of Parts 1 & 2, as in the case of the monograph of the deep North Atlantic Ophiuroidea (Paterson, 1985). Taxonomic responsibility is shared as follows: Crinoids, A.M.C.; Asteroids, A.M.C. & R.H.; Ophiuroids, G.L.J.P.; Echinoids, J.D.G.; Holothurians, D.S.M.B. & J.D.G. Class CRINOIDEA Order MILLERICRINIDA Family BATHYCRINIDAE Bat hycrinus gracilis Wyville Thomson, 1872 See: A. M. Clark, 1977: 164-167, fig. 1; A. M. Clark, 1980: 206-207, fig. 5. SAMPLE. ES 27 (1). [c. 2900m] DISTRIBUTION. Previously known from the West European and Iberian Basins in 4430-5275 m; the northernmost and also the least deep record was from the Porcupine Abyssal Plain, c. 50°N, 1 5°55'W (A. M. Clark, 1977). There is also an unpublished intermediate record in the collections of the Institute of Oceanographic Sciences (IOS), Wormley, from the Porcupine Seabight (Sta. 51 109 #2) in c. 3985 m depth. The new record, from the southern Rockall Trough, is somewhat shallower and farther north. REMARKS. The specimen consists of a crown including proximal parts of some arms to the sixth brachial. The total height is c. 6 mm. The appearance is similar to that of the specimen shown in Fig. 5 in A. M. Clark (1980), except that the knob-like fused basals and short uppermost columnals o°w Bathymetry 200 m 1000 m 2000 rn ••— 3000 IT AOOOrn ..... \ A V X y-^Tu'^^ k^rfi ...... , ^/V/^-X ^ 18°W 16 U Fig. 1 Bathymetric chart of the area sampled s 10 8 6 .howing location of all stations yielding echinoderms. ROCKALL TROUGH ECHINODERMS 3 1 57 are missing. The division series have sharp lateral flanges and a median keel, unlike the medially rounded ossicles of B. carpenteri (Danielssen & Keren), known from the deep basin of the Norwegian Sea in 1 360-28 1 5 m. In addition the collections include a very young specimen of Bathycrinus from SBC 21 1 on the Hebridean Slope in the anomalous depth of 402 m. This is at the same stage of development as the small B. gracilis figured by A. M. Clark (1977, fig. le) from the Porcupine Abyssal Plain, with rudimentary arms and an inverted conical calyx with all the sutures distinct and the basal ring 'integrated' with the radial ring, so that the suture between the two rings forms a zigzag. In larger specimens of Bathycrinus the articulation becomes almost a straight line. Only two division series remain attached to the calyx and these are too poorly developed to exhibit the specific characters. It is just possible that the specimen may be a juvenile Bathycrinus carpenteri that has been carried over the Wyville Thomson Ridge. Democrinus parfaiti Perrier, 1 883 See: Rom, 1977: 39^0, figs 4, 9, 10, 11, 16, pi. 2, figs 6-8, pi. 5, figs 1-6; A. M. Clark, 1977: 172-177, fig. 3a. Also Gage et al., 1983: 270 (as Rhizocrinus lofotensis). SAMPLES. SBC 66 (? frag.), SBC 67(2), SBC 2 1 6( 1 ), AT 230( 1 5), SBC 280 ( 1 ) [also ES 1 8(3), ES 20(8) in Part 1 as Rhizocrinus lofotensis}. [c. 1000-2200 m] DISTRIBUTION. The most northerly record hitherto is from SW. Ireland at c. 50°N. The discovery of these specimens since the completion of Part 1 suggests that the species represented in the Rockall Trough is not Rhizocrinus lofotensis, as thought by A.M.C. in 1983, but Democrinus parfaiti. The depths of more than 1000 m are also indicative of this species which ranges from 870-2500 m (and possibly 2959 m) off Western Europe and NW. Africa to the Azores. The specimen from Sta. 10 of the Ingolf, off SW. Iceland, that was figured by A.M.C. (1970, fig. 4e) as Rhizocrinus lofotensis, is likely to be referable to Democrinus parfaiti on the basis of the Rockall Trough records, thus extending the range even further. Records from Knight Errant, Lightning and Porcupine are also likely to be D. parfaiti. However the fragment described by Doderlein (1912) from the Wyville Thomson Ridge in 547 m under the name of/?, rawsoni may well have been R. lofotensis, the latter species occupying relatively shallow depths of 140-700 m in the southern part of the Norwegian Basin. It has however been recorded from down to 3475 m off Greenland. An unpublished recent IOS record of D. parfaiti in the Porcupine Seabight (Sta. 101 1 1 #8) in c. 1630 m helps to confirm the Helga record of A. H. Clark (1913), that specimen now being in a badly decalcified condition. The distinction between D. parfaiti and Rhinzocrinus lofotensis is discussed in Clark (1970: 21). REMARKS. The calyx of the largest of the present specimens, from SBC 67, is only 2.5 mm high, the same size as the smallest one given in the table of measurements of/), parfaiti in A. M. Clark ( 1 977). Study of the material indicates that the supposition made in 1977 that the calyx is consistently narrow, even in young specimens of this species, was incorrect. Judging from the smaller specimens from the Rockall Trough, the initial shape is inverted conical as in the other species of the genus for which ontogenic series have been observed. Order COMATULIDA Family ANTEDONIDAE Tnchometra cubensis (Pourtales, 1 869) See: A.M. Clark, 1970: 46-^8; 1980: 195-197. SAMPLES. AT 219(1), AT248(41), AT249(1), ES 250(3). [1 150-1991 m] DISTRIBUTION. North Atlantic from the Gulf of Mexico to the Davis Strait and from Morocco to Portugal and NW. Spain; 210-2380 m (72432 m). Also recorded from SW. of Iceland in 31 1 m. The present records from W. of the Anton Dohrn Seamount and from the North Feni Ridge represent an extension of range in the deeper NE. Atlantic. It is possible that the smaller specimens recorded from Helga stations in the Bay of Biscay and W. of Ireland under the name T. delicata A. H. Clark, 1911, will also prove to be conspecific with T. cubensis. 1 58 HARVEY, GAGE, BILLETT, CLARK & PATERSON REMARKS. The colour in life (AT 248) was brownish except for the very flared arm joints which were white. Poliometra prolixa (Sladen, 1881) See: A. M. Clark, 1970: 42-^5, figs 15, 16. SAMPLES. ES 87( 1 ), AT 226( 1 1 ). [c. 1 050- 1 1 1 8 m] DISTRIBUTION. Known only from the Arctic and Norwegian Sea, from Greenland to the seas off western Siberia. The present records from the Faeroe Bank Channel and Faeroe-Shetland Channel represent the southernmost limit of the range. The bathymetric range is 20-1960 m, but all of the more southern records exceed 500 m. Family ATELECRINIDAE Atelecrinus balanoides P. H. Carpenter, 1881 See: A. H. Clark, 1913: 45 (as A. helgae; A. M. Clark, 1970: 49-51, fig. 19 (as A. balanoides). SAMPLES. AT 223(1), AT 230(2), AT 248(3), AT 249(1), ES 250(1). 13/83/6 OTSB(l), 3/85/20 OTSB(2). [980-1 005m to 1270m] DISTRIBUTION. Known in the western tropical Atlantic from Florida to NW. Brazil, and in the NE. Atlantic from the southern Rockall Trough (Helgd) c. 54°N, 12°30'W and south west of the Faeroes (Thor). The present records are intermediate in position between these last two. The recorded bathymetric range is 532-1256 m. REMARKS. The very long straight delicate and easily lost cirri of this species contrast with the relatively short, curly ones of Trichometra cubensis which was often collected in the same haul, both in the Rockall Trough and in the western tropical Atlantic where both species extend. They are also distinguished by their habitats, T. cubensis being epizoic on other organisms such as the gorgonian Acanella, while A. balanoides is self-supporting on muddy substrates with its widely spread cirri. The colour in life (AT 249) was a yellowish-buff. Class ASTEROIDEA Order PAXILLOSIDA Family LUIDIIDAE Luidia ciliaris (Philippi, 1837) SAMPLES. AT 29 1(2), AT 292(4). 13/83/3 GT(ll), 13/83/4GT(7), 1 3/83/7 OTSB(6), 1 3/83/8 OTSB(23), 3/85/14 OTSB(IO), 3/85/38 OTSB(l), 3/85/43 OTSB(9), 3/85/44 OTSB(l). [220-270 m to 650-805 m] DISTRIBUTION. The new shallower records from the Hebridean Slope are more typical of the distribution of this common bathyal species than the single record from 650-805 m given in Part 1 . Family ASTROPECTINIDAE Astropecten irregularis (Pennant, 1 777) SAMPLES. RD 258(1), 13/83/7 OTSB(5). [135 m to 650-805 m] DISTRIBUTION. The new shallow records from Rockall Bank and the Hebridean Slope are not unexpected given the sublittoral and bathyal distribution of this species. Bathybiaster vexillifer (Thomson, 1873) SAMPLES. ES 34(?[juveniles] 4), ES 197(2), ES 200(3,?[juvenile] 1, AT 201(17), AT 218(1), AT 219(15), AT 228( 1 ), ES 232(2), AT 233( 1 4), ES 244( 1 ), AT 245(8), AT 247(juveniles 2), AT 248( 1 ), AT 267(juveniles 2), AT 271(10), AT 273(2), AT 288(22), 13/83/5 OTSB(l), 3/85/7 OTSB(3), 3/85/17 OTSB( 16). [992-2600 m] DISTRIBUTION. The record from AT 267 provides a slight increase in the lower bathymetric range within the Rockall Trough. ROCKALL TROUGH ECHINODERMS 3 1 59 Plutonaster bifrons (Thomson, 1873) SAMPLES. ES 184(2, ?[juvenile] 1), ES 190(?[juveniles] 2), AT 201(11), ES 202(5), ES 218(l;?[juvenile] 1), AT 2 1 9( 1 8), AT 22 1 ( 1 ), AT 223( 1 5), AT 228 (?[juveniles] 3), AT 229( 1 , juvenile 1 ), AT 230( 1 03, ?[juvenile] 1 ), ES 232(2), AT 233(1), AT 239(5), ES 244(2), AT 245(4), AT 247(5), AT 249(4), ES 250(6), AT 251(7), ES 252(juvenile 1), AT 254(2), ES 255Guvenile 1), AT 256(23), ES 264(juveniles 6), AT 267(7), AT 271(3), AT 273(1), ES 285(?[juvenile] 1), AT 286Guvenile 1), AT 287(?[juvenile] 1), AT 288(8), ES 289(1), 13/83/1 OTSB(?[juvenile] 1), 13/83/2 OTSB(38), 13/83/5 OTSB(71), 13/83/6 OTSB(13), 13/83/7 OTSB(l), 9/84/9 OTSB(22), 9/84/10 OTSB(l), 9/84/13 OTSB(12), 3/85/9 OTSB(l), 3/85/17 OTSB(77), 3/85/18 MBA(ll), 3/85/19 MBA(l), 3/85/20 OTSB(IO), 3/85/25 OTSB(2), 3/85/29 OTSB(IO), 3/85/30 OTSB(55). [580-630 m to 2965 m] DISTRIBUTION. The new records from the Hebridean Slope give an upward extension of bathymetric range by c. 400 m. Psilaster andromeda (Muller & Troschel, 1842) SAMPLES. ES 23(3), AT 223(12), AT 230(juvenile 1), AT 239(8), AT 291(20), GT 2(1), GT 7(1), GT 11(5), GT 14(2), GT 15(1), GT 16(4), AT 1(3), 13/83/6 OTSB(15), 13/83/7 OTSB(16), 9/84/1 OTSB(2), 9/84/13 OTSB(4), 3/85/9 OTSB(8), 3/85/10 OTSB(2), 3/85/13 OTSB(1 1 1), 3/85/1 4 OTSB(5), 3/85/18 MBA(27), 3/85/ 19 MBA(2), 3/85/25 OTSB(2), 3/85/28 OTSB(l). [640-780 m to 990-1075 m] DISTRIBUTION. Further studies on this and the related Persephonaster patagiatus (formerly Psilaster) (see remarks below and under that species) have shown that in the Rockall Trough on the Hebridean Slope Psilaster andromeda has a more restricted distribution than hitherto recorded, being common in the 700-1000 m zone. REMARKS. Following additional studies of the Astropectinidae by A.M.C., the distinction of Psilaster andromeda and Persephonaster patagiatus by the relative breadth of the superomarginal plates in dorsal view as shown by Mortensen (1927) was found to be fallacious. This character is variable in both species. A better distinction is the more convex contours of individual marginals in dorsal view in Persephonaster patagiatus compared with the flat surface but sharply-cut inter- marginal fascioles visible in Psilaster andromeda, when specimens are denuded with bleach. In section, the marginals of Psilaster andromeda tend to form continuously rounded arcs. In Persephonaster patagiatus however, the superomarginals in particular are more abruptly bent, making the sides of the arms flatter. Other differences are the more attenuated arms of P. patagiatus with somewhat longer and fewer marginal plates, usually 25-30 at R 60-90 mm as opposed to 35 + in P. andromeda at this size. The armament of the marginals is also different, the inferomarginal spines being more needle-like in P. patagiatus, and the armament at the apex of the jaw projecting horizontally below the mouth is very different. In Persephonaster patagiatus there is a pair of inset fascicles of blunt spines partly concealed above the apical spines, which are rounded in section, whereas in P. andromeda there is only a line of 3 or 4, very flat spade-like apical spines. Indeed this last character coupled with the absence of well-defined intermarginal fascioles in P. patagiatus justifies generic isolation of the species in the genus Persephonaster, which has previously been confused to some extent with Psilaster but can now be distinguished by these characters. The nomenclature is therefore restored to the combinations used by Mortensen (1927). Use of the above characters has resulted in the re-identification of some of the samples recorded in Part 1 . Persephonaster patagiatus (Sladen, 1889) SAMPLES. ES 15(2), ES 18(3), AT 68A(1), AT 107A(5), AT 186(3), AT 192(30,?[juveniles] 5), AT 221(4,? [juvenile] 1), AT 229(63), AT 254(1), AT 256(37), AT 287(27,?[juvenile] 1), SWT 18(8), SWT 27(4?), 13/83/1 OTSB(274), 13/83/2 OTSB(IO), 13/83/5 OTSB(15), 9/84/9 OTSB(3), 3/85/20 OTSB(?[juvenile] 1), 3/85/29 OTSB(13), 3/85/30 OTSB(66). [1265-1 130 m to 1809 m (?2965 m)] DISTRIBUTION. This species is widely distributed in the N. Atlantic (but see notes in Part 1. for possible complications). On the Hebridean Slope it occurs slightly deeper than Psilaster andromeda. 1 60 HARVEY, GAGE, BILLETT, CLARK & PATERSON Curiously there are no samples in which both species occurred. Following the reassignment of this species to the genus Persephonaster, as explained above, further clarification of the depth limits of the two species was sought by recourse to the collections from the Porcupine Seabight held at IOS, Wormley. These were found to include 21 samples of Psilaster andromeda identified by D.S.M.B. with positive depths ranging from 700 to 1490m, compared with 1 1 samples of Persephonaster patagiatus from 1360-2000 m. The deepest sample of/*, andromeda also included seven specimens of P. patagiatus. The SMBA record from SWT 27 (a fishing station) in 2965 m therefore seems doubtful, and may be a contaminant from an earlier haul. Family PORCELLANASTERIDAE Porcellanaster ceruleus Wyville Thomson, 1877 SAMPLES. ES 4(5, juveniles 2), ES 10(1 01, juveniles 7), ES 27(99), ES 57(1, juveniles 7), ES 1 1 1(75), ES 1 18(43), ES 129(75), ES 152(61 juvenile 1), SBC 174(juveniles 2), ES 184(5), ES 185(330), ES 190(165), ES 197(2, juveniles 3), ES 204(90), ES 207(344), ES 2 1 8(3), ES 23 1 (20 1 ), ES 266(7), AT 267(37), AT 282(4), ES 283(31 7), AT 284(6), ES 285(21), AT 286(3). [1993 m to 3425-3500 m] DISTRIBUTION. No change. Order NOTOMYOTIDA Family BENTHOPECTINIDAE Benthopecten simplex Perrier, 1 88 1 SAMPLES. ES 1 05(?[juvenile] 1 ), ES 1 84( 1 7, ?[juvenile] 1 ), ES 1 97(37), ES 200( 1 1 , ?[juveniles] 8), AT 20 1 (6 1 ), ES 202(3,?[juveniles] 8), AT 218(44), AT 219(103), AT 228(132), ES 232(12), AT 233(95), ES 244(12), AT 245(70), AT 247(4), ES 255(juvenile 1), AT 256(41), ES 257(1), ES 264(9), AT 271(82), AT 273(60), AT 288(102), ES 289(32), 13/83/5 OTSB(75), 13/83/6 OTSB(4), 9/84/9 OTSB(3), 3/85/7 OTSB(2), 3/85/17 OTSB(239), 3/85/29 OTSB(13). [1595 m to 3425-3500 m] DISTRIBUTION. The new records raise the upper bathymetric limit in the Rockall Trough from 1785-1 845m to 1595m. Pectinasterfilholi Perrier, 1885 SAMPLES. ES 34(8), ES 197(juveniles 20), AT 201(1), AT 219(4), AT 233(3), AT 267(3), AT 288(4), 3/85/7 OTSB(34). [1752-2909 m] DISTRIBUTION. No change. Cheiraster sepitus (Verrill, 1 885) See: Sladen, 1889: 52-55, pi. 8, figs 5 & 6, pi. 12, figs 5 & 6 (as Pontaster venustus); A. M. Clark, 198 1 : 1 1 7-1 1 8, figs 4i-r & 5c. SAMPLES. AT 229(7), AT287(9), 13/83/1 OTSB(45), 3/85/29 OTSB(4), 3/85/30 OTSB(23), 3/85/45 OTSB(2). [1383m to 1690- 1740m] DISTRIBUTION. Nova Scotia south to the Caribbean, Azores and Bay of Biscay south to Cape Verde; 485-3703 m, but mainly 1 000-2000 m. The present records from the Hebridean Slope extend the known distribution in the NE. Atlantic to c. 56° 30'N. confirming the prediction of Mortensen (1927) that Pontaster venustus Sladen, a synonym of Cheiraster sepitus according to A. M. Clark (1981), would probably be found in British waters. REMARKS. The 45 specimens measured from Sta. 1 3/83/1 OTSB range from R 45 mm to R 22 mm, R/r 4.8/1 to 3.0/1 (mean 3.7/1). Arm length varied within individuals and several specimens had regenerating arm tips. There was little tendency for the arm tips to curl dorsally in preserved specimens unlike those of Pontaster tenuispinus. The specimens are of a robust appearance due to the encroachment of the superomarginal plates on to the abactinal surface of the arms, and the tumidity of the inferomarginals. Sladen (1889) states that no pedicellariae of any kind are to be ROCKALL TROUGH ECHINODERMS 3 161 found in Cheiraster, whereas A. M. Clark (1981) found some to be present but only rarely. At least 8 of the Rockall specimens have small pectinate pedicellariae on the actinal interradii formed by the opposition of short spines on the plates. Their occurrence varies between interradii but where present they are distinctive. Pontaster tenuispinus (Diiben & Koren, 1 846) SAMPLES. AT 226( 1 ), AT 239(2), AT 27 1 (2), AT 273(2), AT 29 1 (22), 1 3/83/2 OTSB( 1 ), 1 3/83/7 OTSB( 1 59), 1 3/83/8 OTSB(6), 9/84/ 1 OTSB(9), 9/84/2 OTSB( 1 ), 9/84/ 1 0 OTSB( 1 ), 3/85/ 1 0 OTSB( 1 74), 3/85/ 1 1 OTSB(2), 3/85/14 OTSB(l), 3/85/43 OTSB(l), 3/85/44 OTSB(2). [500-560 m to 2255 m] DISTRIBUTION. The record from AT 271 extends the lower bathymetric limit to 2255 m. Order VALVATIDA Family ODONTASTERIDAE Hoplaster spinosus Perrier, 1 882 SAMPLES. ES 266(1), AT 267(1). [2300-29 10m] DISTRIBUTION. The new records from the Feni Ridge are intermediate in depth between those of the two specimens recorded in Part 1. R was 12 mm in the specimen from ES 266. Family RADIASTERIDAE Radiaster tizardi (Sladen, 1 882) SAMPLES. AT 223(22), 13/83/2 OTSB(2), 3/85/20 OTSB(l). [1075 m to 1 130-1265 m] DISTRIBUTION. The new records confirm the occurrence of this species in the Rockall Trough, the record in Part 1 being from a single juvenile. They are all within the previously known bathymetric range. REMARKS. The specimens from AT 223 and 3/85/20 OTSB have R 60-1 10 mm. Family ASTERINIDAE Anseropoda placenta (Pennant, 1777) See: Mortensen, 1927: 99-101, fig. 57. SAMPLES. 1 3/83/3 GT( 14), 1 3/83/4 GT(4), 1 3/83/8 OTSB(4). [220-270 m to 500-560 m] DISTRIBUTION. Known from the Shetlands to the Mediterranean around both the west and east coasts of Britain in 10-200 m, but previously down to 600 m only in the eastern Mediterranean. The present records from the Hebridean Shelf and Slope provide an extension of bathymetric range in northern waters. REMARKS. This species is thought to prefer sandy ground, which may explain its failure to penetrate far beyond the shelf edge. Family GONIASTERIDAE Ceramast er granularis (Retzius, 1783) See: Mortensen, 1927: 81-82, fig. 44. SAMPLES. AT 229(1), AT 248(1), AT 259(1), AT 273(1), AT 287(1). [1 150-2185 m] DISTRIBUTION. Widely distributed on both sides of the North Atlantic. Previously recorded from British waters from the Faeroe Channel, Lousy Bank, and on the Irish slope; 20-1400 m. The present records from the Feni Ridge and Hebridean Slope extend the lower bathymetric limit by nearly 800 m. Some of the specimens appear to intergrade morphologically with the more southern species C. grenadensis (recorded as C. balteatus by Mortensen, 1927). 1 62 HARVEY, GAGE, BILLETT, CLARK & PATERSON Pseudarchaster parelii (Diiben & Koren, 1846) SAMPLES. AT 20 1 ( 1 ), ES 202(juvenile 1 ), AT 223(1 ), AT 229( 1 ), AT 230(2), AT 248(3), AT 25 1 (juvenile 1 ;?3), AT 259(1), AT 267(74), AT 287(74), AT 288(4), AT 291(1), 13/83/8 OTSB(3), 3/85/10 OTSB(?1), 3/85/14 OTSB(7), 3/85/20 OTSB(2), 3/85/29 OTSB(l), 3/85/30 OTSB(4), 3/85/43 OTSB(2), 3/85/44 OTSB(2). [225-2965 m] DISTRIBUTION. No change. REMARKS. The distinction between P. parelii and P. gracilis is not clear in the Rockall samples. Halpern (1972) has separated the species on the basis of the armament of the actinal and infero- marginal plates, those of P. gracilis bearing cylindrical spines 3 to 5 times longer than wide, while in P. parelii the spines, if any, are short and flattened. Some of the specimens identified as P. parelii from the Rockall area have a few longer cylindrical spines. Mortensen (1927) states that P. parelii grows to nearly 200mm R, and Farran (1913) recovered specimens from the west of Ireland reaching R 192 mm, the majority of the Irish specimens measured being > 80 mm R. None of the Rockall specimens with R > 60 mm appear to be P. parelii, having very thorny actinal plates and a conspicuous pectinate pedicellaria-like arrangement of subambulacral spines said to be character- istic of P. gracilis (Halpern, 1972). It is possible therefore that the 'P. parelif specimens from the Rockall area are merely the young of 'P. gracilis'. Until more work can be done on the distinction of these two nominal species, the Rockall records of P. parelii refer to the small specimens with few spines on the actinal plates and less obvious 'pectinate pedicellariae'. Pseudarchaster gracilis (Sladen, 1889) SAMPLES. AT 219(1), AT 223(3), AT 229(2), AT 233(1, ?[juvenile] 1 ), AT 254(71), AT 287(1 , 71), AT 288(2), ES 289(1), 13/83/1 OTSB(6), 13/83/2 OTSB(l), 1 3/83/5 OTSB(21), 1 3/83/6 OTSB(5), 1 3/83/7 OTSB(7), 13/83/8 OTSB(l), 9/84/9 OTSB(l), 9/84/13 OTSB(l), 3/85/7 OTSB(5), 3/85/8 OTSB(l), 3/85/17 OTSB(14), 3/85/29 OTSB(l), 3/85/30 OTSB(2), 3/85/36 OTSB(l). [7500-560 m to 2190 m] DISTRIBUTION. The new records extend the known distribution northwards to just south of the Wyville Thomson Ridge and the North Feni Ridge c. 59° 40'N (but see remarks under P. parelii and below). REMARKS. The above records relate to the larger specimens of Pseudarchaster with more thorny actinal plates and prominent 'pectinate pedicellariae' along the subambulacrals. The colour in life was a bright brick red. The largest specimen measured R 165 mm. Paragonaster subtilis (Perrier, 1881) SAMPLES. ES 204(2), AT 267(18), AT 282(1), ES 283(1), AT 284(3), ES 285Guvenile 1), AT 286(18), 51301 OTSB(6), 3/85/5 OTSB(4), 3/85/7 OTSB(2). [1785-1845 m to 2970-2980 m] DISTRIBUTION. The new records slightly extend the maximum recorded depth for this species in the Rockall Trough. Plinthaster dentatm (Perrier, 1884) SAMPLES. ES 129(?[juvenile] 1), AT 223(1), AT 287(17), 13/83/1 OTSB(37), 13/83/5 OTSB(l), 3/85/17 OTSB(8), 3/85/29 OTSB(l), 3/85/30 OTSB(30), 3/85/37 OTSB(l), 3/85/45 OTSB(4). [945-985 m to 2910 m] DISTRIBUTION. The new records raised the upper bathymetric limit on the Hebridean Slope by almost 400 m. Mediaster bairdi (Verrill, 1 882) See: Gray, Downey & Cerame- Vivas, 1968: 150-151, fig. 24. SAMPLES. AT 229(14), ES 252(5), AT 287(49), 13/83/1 OTSB(22), 3/85/30 OTSB(72), 3/85/45 OTSB(2). [1383-1587 m] ROCKALL TROUGH ECHINODERMS 3 1 63 DISTRIBUTION. Previously known only in the W. Atlantic from Newfoundland to New Jersey, in the lesser Antilles and off Guyana; 642-1446 m. The Rockall records from the Hebridean Slope and North Feni Ridge are the first from the NE. Atlantic. Downey (pers. comm.) has found very little difference between N. American M. bairdi and M. capensis from S. Africa, and believes that any taxonomic distinction between them is infraspecific. REMARKS. The specimens from AT 287 ranged from R53 mm to R 21 mm, R/r = 2.4-3. 1/1. Gray et al. (1968) state that the specimen in their figure 24 has R/r 3.3/1, but measurements from this figure suggest a ratio nearer 2.5/1 . The specimens from AT 287 were a pale orange-ochre when collected fading to off-white in spirit. Family PORANIIDAE Porania pulvillus (O . F. Miiller, 1766) SAMPLES. ES 113(1, juveniles 2), AT 292(8), 13/83/3 GT(69), 13/83/4 GT(43), 13/83/8 OTSB(52), 3/85/38 OTSB(4), 3/85/43 OTSB(3). [148 m to 565-700 m] DISTRIBUTION. The new records are all from the Hebridean Slope and suggest that this species is more common below 300 m than was thought previously, four of the above samples having come from >400m. Poraniomorpha hispida rosea Danielssen & Koren, 1 88 1 See: Mortensen, 1927: 92-93, fig. 53; A. M. Clark, 1984: 34, fig. 1 1 B, C. SAMPLES. ES 112(?[juvenile] 1), AT 230(1), AT 287(1). [1210-1383(?1900)m] DISTRIBUTION. This subspecies was previously recorded from just south of the Wyville Thomson Ridge under the name Lasiaster villosus Sladen, 1889 (Porcupine Sta. 47A, 990 m). The synonymy of Poraniomorpha hispida and P. rosea is complicated but rosea has usually been treated as a stellate variety of the more nearly pentagonal P. hispida. However, in 1984 A.M.C. distinguished it subspecifically on account of the isolation of rosea for much of its range, both geographically and bathymetrically. Whereas P. hispida hispida is found all round the coast of Norway extending north to the southern Barents Sea, with positive depths of 100-350 m, P. hispida rosea seems to be essentially an upper bathyal taxon extending south from the Norwegian Basin along the Norwegian Trench to the Skaggerak in the east and down the Rockall Trough to the Bay of Biscay further west in 290m to c. 1400m. If the small specimen (R only 3-2 mm) from ES 1 12 is a young P. hispida rosea, as its already stellate form suggests, than the depth range extends further to 1900m. Chondraster grandis (Verrill, 1878) See: A. M. Clark, 1984: 27, figs 4A, B, 5A, 6, 7d. SAMPLES. AT 229 (1), AT 247(2), 3/85/9 OTSB(l). [945-1010 m to 2084 m] DISTRIBUTION. This species was recorded from the NE. Atlantic for the first time by A. M. Clark (1984) on the basis not only of the two deeper SMBA samples but also of six others ranging from the Lousy Bank south to the southern Bay of Biscay (BIOGAS), including Helga and more recent IOS material from the Porcupine Seabight. The small holotype of Marginasterfimbriatus Sladen, 1889 from Porcupine Sta. 31 (c. 56°N ll'W) in 2487m is almost certainly conspecific with C. grandis, though this depth exceeds by c. 300 m the positive maximum from AT 247. The type locality of C. grandis is in the vicinity of Cape Cod in c. 400 m but other records from N. America extend down to 1640 m, while E. Atlantic records range from 840 to 2070 (?2487)m. REMARKS. The colour in life of the specimens from AT 247 was light red midradially on the dorsal surface paling laterally to cream below. The specimen collected from 3/85/9 OTSB retained vermilion red colour in formalin on the upper side and around the ventral margin, the rest of the 1 64 HARVEY, GAGE, BILLETT, CLARK & PATERSON lower side being off-white. Distinct areas of white papulae were present along each arm of the latter specimen, with a central narrow naked zone and naked interradii. The madreporite was off-white in colour. Order SPINULOSIDA Family PTERASTERIDAE Pterastermilitaris(O. F. Muller, 1776) SAMPLES. 1 3/83/6 OTSB( 1 ), 3/85/ 1 3 OTSB( 1 ), 3/85/28 OTSB( 1 ). [934- 1 054 m to 990-1 075 m] DISTRIBUTION. The new records bring the total number of specimens recorded from the Rockall Trough to only 6, all from the Hebridean Slope at around 1000 m. Pteraster pulvillus M. Sars, 1861 SAMPLES. AT 230(1), 13/83/3 GT(1), 3/85/14 OTSB(l). [168-1210 m] DISTRIBUTION. The new records, all from the Hebridean Slope, supplement the two previous records to provide a more continuous bathymetric distribution. Pteraster reductus Koehler, 1907 SAMPLE. AT 251(1). [1530-1 900m] DISTRIBUTION. Only two other specimens of this species have been recorded from the NE. Atlantic, both from the Feni Ridge. The new record is almost 400 m shallower than the record in Part 1 . Pteraster (Apterodon) sp. aff. P. acicula (Downey, 1970) See: Downey, 1973: 79, pi. 34 C, D (for P. acicula). Also Gage et al, 1983: 282 (For P. sp. aff. P. acicula). SAMPLE. 3/85/13 OTSB(2). [958-995 m] DISTRIBUTION. The new specimens were recovered from almost the identical position and depth on the Hebridean Slope from which a specimen subsequently confirmed as P. acicula (M. Downey, pers. comm.) was recorded (see Part 1). These are the only records for the NE Atlantic, the type locality being in the Gulf of Mexico. REMARKS. The specimens are plump and pentagonal, both with R 16mm, rlOmm and in good condition with blunt arms curling dorsally at the tips. There is no webbing at all between the oral spines, an absence characteristic of the subgenus Apterodon. There are six spines on each oral plate, the apical spine being the largest and at least twice as long and thick as the distalmost spine. The single stout suboral spine is longer and slightly broader than the apical oral spine, glassy through- out its length and distincitively tricarinate, ending in an acute point. The grooves on the sides of these spines which give rise to their tricarinate form commence at about one third of the length from the spine base. The paxillae of the dorsal surface consist of a peripheral ring of c. 10 spinelets each around 0-06 mm thick with an imperforate portion immediately above the base which becomes regularly trabeculate distally without becoming broader, as in many echinoid spines. This structure continues to the spine tip. Within this ring are > 1 5 spinelets with more slender rod-like bases only 0-02 mm thick which become spatulate and trabeculate in their distal half and 0- 14 mm in width. The tips of both types of spinelet protrude through the dorsal membrane, those of the spatulate type having trifid tips. This feature, combined with the large number of spinelets, gives the dorsal surface a dense prickly appearance with only small inter-paxillar spaces. As this description is slightly at variance with that for P. acicula (Downey, 1 973), some doubt remains as to the specific identity of these new specimens. Pteraster (Apterodon) sp. See: Downey, 1973: 77, pi. 33, figs A, B (for P. caribbaeus). SAMPLES. AT 247(2), ES 264(10). [2084-2144 m] ROCKALL TROUGH ECHINODERMS 3 1 65 DISTRIBUTION. North Feni Ridge at the foot of Rosemary Bank and at the foot of Rockall Bank. REMARKS. This species is distinguished from P. acicula by having more attenuated arms and a distinctly hispid appearance as collected due to the protrusion through the dorsal membrane of the paxillar spinelets which end in a single point. There are c. 18-24 spinelets on each paxilla, all of uniform thickness for most of their length. The interpaxillar spaces are relatively large and the membrane is almost transparent. The unwebbed oral spines decrease evenly in size from the apical to the most distal sixth or occasionally seventh spine. Each oral plate bears one or sometimes two suboral spines which are larger than the apical oral spine and have a hyaline tip where the outer opaque sheath has worn away. They are trabeculate for most of their length with the exception of the slightly tricarinate distal portion. This species is superficially similar to P. caribbaeus Perrier, 1881, but the paxillae have almost twice as many spinelets and there are other small differences between the spines on the jaw plates and the musculature of the dorsal membrane. Seven of the specimens are in good condition. The records of this species and P. sp. aff. P. acicula suggest that there may be some separation on the basis of habitat, given the differences in depth and geographic distribution within the Trough. Diploptemster multipes (M. Sars, 1865) See: Fisher, 191 1: 371, pi. 107, figs 1,2. SAMPLES. 3/85/20 OTSB(l), 3/85/34 OTSB(l), 3/85/36 OTSB(l). [980-990 m to 1225-1245 m] DISTRIBUTION. This species is circumarctic extending south in the NE. Atlantic along the Norwegian coast to the Skagerrak, in the NW. Atlantic to the latitude of Chesapeake Bay, and in the Pacific to California in the east and Japan in the west. These are the first records from the Rockall Trough and they also provide an extension of the previous known bathymetric range of 91-1 170 m. A further sample has been taken by IOS in the Porcupine Seabight (Sta. 50602 #4) in 1080-1 120 m. The specimen from 3/85/34 OTSB has six arms. REMARKS. This is the largest pterasterid occurring in British waters, R max can reach c. 1 10 mm. In life the colour is pale mauve dotted with white dorsally continuing to the ventral interradii. The wide ambulacra are emphasised by red colouration along the subambulacral plates. Hymenaster membranaceus Wyville Thomson, 1 887 SAMPLES. ES 184(82), ES 185(?[juveniles] 5), ES 197(37, ?[juveniles] 4), AT 201(324), ES 202(12), ES 218(9), AT 219(277), ES 232(15), AT 233(324), ES 244(15), AT 245(421), AT 271(104), AT 273(? 1), AT 287(1), AT 288(367), ES 289(25), 3/85/5 OTSBGuvenile 1). [1383-2909 m] DISTRIBUTION. The record from AT 287 on the Hebridean Slope raises the upper bathymetric limit within the Trough by some 600 m, although this is still within the known distribution of this species (1000-3000 m). Hymenaster regalis Verrill, 1 895 See: Verrill, 1895: 203-204; H. L. Clark, 1941: 64. SAMPLE. AT 195(1) [in Part 1 as H. ?gennaeus], AT 288(1). [2190 m] DISTRIBUTION. Hymenaster regalis is a rare species known only from the holotype taken in the NW. Atlantic off N. Carolina at 36°34'N, 73°48'W; 2521 m, and from another single specimen taken off Cuba in 1847 m. REMARKS. The specimen from AT 195 measures 75mm R, 40mm r, while that from AT 288 measures c. 75 mm R, c. 55 mm r, the measurements being approximate due to the arched dorsal surface and recurved arm tips. Both of the previously known specimens were of a similar size. The dorsal surface is firm and opaque with distinct muscle fibres between the paxillae which consist of only a single stout spine raising the dorsal membrane into firm peaks. The membrane is perforated 1 66 HARVEY, GAGE, BILLETT, CLARK & PATERSON by small spiraculae numbering > 50 in the space within a ring of paxillae. In the life the specimen from AT 288 was a pale red dorsally. These are the first records of this species from the eastern Atlantic, and also represent a considerable extension of range northwards. Hymenaster gennaeus H. L. Clark, 1923 SAMPLE. AT 233(1). [2 180-29 10m] Family SOLASTERIDAE Crossaster squamatus (Doderlein, 1900) SAMPLE. AT 287(3). [1050-1383 m) DISTRIBUTION. Previously unknown south of the Faeroe Channel, this new record extends the range south to the Hebridean Slope at c. 56°N. Family ECHINASTERIDAE Henricia Gray Madsen is currently revising this genus (pers. comm.). The synonymy is complex and rather than confuse the literature further by publishing new records at this stage, it is felt that this should await the revision. Two species with slightly different depth distributions appear to be represented (see Gage et al. , 1 983: 284), that from the deeper stations being conspecific with Henricia abyssicola sensu Mortensen, 1 927 (non Cribrella sanguinolenta var. abyssicola Norman, 1 869) and distinguished by more attenuated arms and abactinal spinelets with a prolonged glassy point. The shallower species has less attenuated arms and abactinal spinelets ending in three points all at the same level. This taxon is conspecific with Norman's variety abyssicola. Order BRISINGIDA Family BRISINGIDAE Brisinga endecacnemos Asbjornsen, 1 856 SAMPLES. AT 201(5), AT 219(2), AT 233(1), AT 245(1), AT 254(1), ES 264(?[juvenile] 1), 13/83/5 OTSB(24), 9/84/9 OTSB(19), 3/85/17 OTSB(43), 3/85/29 OTSB(IO). [1690-1740 m to 2220 m] DISTRIBUTION. The new records raise the upper bathymetric limit on the Hebridean Slope although this is still much deeper than the shallowest known record of 286 m from Trondheim Fjord. REPRODUCTION. Tyler et al. (1984) have described the reproductive biology of this species. Up to 60 000 eggs may be produced by each individual and there was no clear evidence of any seasonality in breeding in the limited number of samples available. The oocytes reach a maximum diameter of c. 1250 um suggesting a direct form of demersal development. Brisingella coronata (G. O. Sars, 1871) SAMPLE. ES 289(1). [992-2450 m] REMARKS. This specimen is unusual in having only eight arms instead of the usual 9-13. DISTRIBUTION. No change. REPRODUCTION. This appears to follow a similar pattern to that in Brisinga endecacnemos (Tyler etal., 1984). Novo dinia pandina (Sladen, 1889) See: Sladen, 1889: 597-601, pi. 109, figs 1-5; Mortensen, 1927: 123-125, fig. 72 (as O dinia pandina); Downey, 1986: 27-29, fig. 13. SAMPLE. 3/85/28 OTSB(l). [990-1075 m] ROCKALL TROUGH ECHINODERMS 3 1 67 DISTRIBUTION. Known from the 'cold' area of the NE. Atlantic from the Faeroe Channel c. 790- 900 m (Lightning and Porcupine), to Iceland in 225 m (Einarsson, 1948). A single specimen was recently recovered from the western Atlantic off N. Carolina (Downey, 1986). The occurrence of this rarely found species at c. 56°N on the Hebridean Slope represents a southerly extension of range in the eastern Atlantic into the 'warm' area. Mortensen (1927) speculated however that O. pandina may be synonymous with O. semicoronata E. Perrier, 1885 recorded from the Denmark Strait and south of the Canaries in 1000-1435 m, and also O. robusta E. Perrier, 1885 known from the Bay of Biscay and south of the Canaries c. 880-1445 m. Following the discovery that the name Odinia is preoccupied, all these nominal species were referred to Novodinia by Dartnall et al., ( 1 969). In her revision of the Atlantic brisingids, Downey ( 1 986) synonymises N. semicoronata with N. robusta, while retaining N. pandina as a separate entity. She suggests that Novodinia is a genus of only moderately deep water c. 250-1 500 m. REMARKS. The specimen, in common with most brisingids recovered, is incomplete, consisting of a disc of radius 18mm with one partly detached arm and an arm fragment. There are sixteen ambulacral furrows. The attached arm measures 60 mm from the disc edge and 23 mm in height at the point of maximum gonadal swelling. The specific characters agree with Sladen's precise description and the presence of papulae on the disc and arms in particular distinguishes this specimen from all brisingids hitherto recorded from the Rockall Trough. This specimen is a male so no information can be given on the possible mode of development. Order FORCIPULATIDA Family ASTERIIDAE Stichastrella rosea (O. F. Miiller, 1776) SAMPLES. RD 258(1). [135m] DISTRIBUTION. Further study of the bathymetric limits of Stichastrella suggests that in the Rockall Trough area, S. rosea is confined to the shelf in depths of less than 200 m. The record from GT 1 4 in 713-788 m listed in Part 1 is therefore reassigned to the variety ambigua. Stichastrella rosea var. ambigua (Farran, 1913) SAMPLES. AT 259(2), AT 291(7), AT 292(21), GT 14(3) [listed as S. rosea in Part 1], 13/83/3 GT(44), 13/83/4 GT(45), 13/83/7 OTSB(IO), 13/83/8 OTSB(165), 3/85/38 OTSB(15), 3/85/43 OTSB(21), 3/85/44 OTSB(5). [220-270 m to 1632m] DISTRIBUTION. No change. Neomorphaster talismani Perrier, 1 894 See: Mortensen, 1927: 134-135, fig. 76. SAMPLES. AT 259(1), 3/85/30 OTSB(l). [1041m to 1420-1480 m] DISTRIBUTION. Known from SW. Ireland in 1350 m and south to Morocco mainly c. 400-2000 m but exceptionally found at 54 1 3 m. The above records from the Rockall Bank and Hebridean Slope extend the known geographic range of this species to the Rockall Trough. Family ZOROASTERIDAE Zoroaster fulgens Wyville Thomson, 1873 SAMPLES. AT 198(3), AT 201(1), AT 219(1), AT 223(8), AT 229(5), AT 230(2), ES 232(3), AT 233(3), AT 239(6; ?[juvenile] 1 ), AT 245( 1 ), AT 256( 1 3), AT 257( 1 ), AT 259( 1 4), ES 26 1 ( 1 ), ES 264(juvenile, 1 ), AT 267(3), AT 273(3), AT 287(190), AT 288(4), 13/83/1 OTSB(4), 13/83/2 OTSB(l), 13/83/5 OTSB(33), 13/83/6 OTSB(21), 9/84/9 OTSB( 14), 9/84/10 OTSB(3), 9/84/1 3 OTSB(30), 3/85/7 OTSB( 1 82), 3/85/8 OTSB(3), 3/85/ 9 OTSB(l), 3/85/17 OTSB(4), 3/85/18 MBA(IO), 3/85/20 OTSB(ll), 3/85/25 OTSB(43), 3/85/29 OTSB(49), 3/85/30 OTSB(lOl). [940-975(7580-630) m to 4810 m] 1 68 HARVEY, GAGE, BILLETT, CLARK & PATERSON DISTRIBUTION. The records from 9/84/10 OTSB approach the minimum depth known for this species, but it is possible that these specimens were contaminants from the previous samples in 1 750-1 770 m. This is supported by their small size, similar to the specimen figured as Z.fulgens var. ackleyiby Farran (1913 pi. 1, fig. 3). On the Hebridean Slope it is noticeable that individuals of Z. fulgens from depths greater than c. 1 500 m are nearly always of this smaller slender-armed form, whereas those from around 1000 m are larger and more robust. Class OPHIUROIDEA Order PHRYNOPHIURIDA Family ASTERONYCHIDAE Asteronyx loveni Miiller & Troschel, 1 842 See: Paterson, 1985: 13-15, fig. 9. SAMPLE. 3/85/32 OTSB(l). [1055 m to 1995-2020 m] DISTRIBUTION. All three specimens recovered in our samples have been from the Hebridean Slope. Family ASTEROSCHEMATIDAE Asteroschema inornatum Koehler, 1906 See: Paterson, 1985: 16, fig. 10. SAMPLE. ES 264(1). [1900-2144 m] DISTRIBUTION. This and the previous specimen are from the west side of the Trough and both were entwined in the branches of gorgonians. Family GORGONOCEPHALIDAE Gorgonocephalus caputmedusae (Linnaeus, 1 758) See: Paterson, 1985: 1 1-13, fig. 8. SAMPLES. AT 239(1), ES 250(?[juvenile] 1), GT 2(1), 13/83/2 OTSB(l), 13/83/6 OTSB(l), 9/84/13 OTSB(l), 3/85/13 OTSB(l), 3/85/19 MBA(4), 3/85/23 OTSB(l), 3/85/24 OTSB(2), 3/85/25 OTSB(4), 3/85/26 OTSB(6), 3/85/27 OTSB(4), 3/85/28 OTSB(2), 3/85/31 OTSB(3), 3/85/33 OTSB(l), 3/85/34 OTSB(2), 3/85/36 OTSB(6), 3/85/46 OTSB(l). [940-985 m to 1 130-1265(71270)] DISTRIBUTION. All specimens, with the exception of the queried one from the Feni Ridge are from the Hebridean Slope where this species is apparently common. The new records extend the bathymetric range in this area. Family OPHIOMYXIDAE Ophiomyxa serpentarla Lyman, 1883 See: Paterson, 1985: 18-20, fig. 1 1. SAMPLE. AT 259(1 5). [1041 m] DISTRIBUTION. Previously recorded in the eastern Atlantic from the Faeroe Channel and SW. Ireland to the Azores; 450-2440 m. Its occurrence on the Feni Ridge is therefore not unexpected. Ophioscolex glacialis Miiller & Troschel, 1842 See: Paterson, 1985: 20-21, fig. 11. SAMPLES. AT 248(1), AT 249(1), AT 251(1), AT 259(2), 9/84/2 OTSB(l), 3/85/28 OTSB(l). [91 0-960 m to 1530m] DISTRIBUTION. Previously recorded from both sides of the N. Atlantic and from Arctic seas; 50-2727 m. These specimens, mainly from the N. Feni Ridge but also from the Hebridean Slope, provide a link between a specimen recovered by IOS at the extreme SW. end of the Trough and the Arctic populations. ROCKALL TROUGH ECHINODERMS 3 1 69 Ophiophrixus spinosus (Storm, 1881) See: Paterson, 1985: 21-22, fig. 12. SAMPLES. AT 287(1), 3/85/9 OTSB(l), 3/85/10 OTSB(l), 3/85/14 OTSB(l), 3/85/28 OTSB(l), 3/85/46 OTSB(l). [720-775 m to 1383 m] DISTRIBUTION. Known from the Denmark Strait and SE. Iceland to the Azores; 40-1310 m. These specimens are all from the Hebridean Slope and provide a slight increase in bathymetric range. Order MYOPHIURIDA Family OPHIACANTHIDAE Subfamily OPHIACANTHINAE Ophiacantha abyssicola G. O. Sars, 1871 See: Paterson, 1985: 47-48, fig. 20. SAMPLES. AT 239(? 1), AT 259(2), AT 290(1), GT 1(?1), 13/83/5 OTSB(2), 13/83/13 OTSB(l), 3/85/17 OTSB(9), 3/85/28 OTSB(5). [7650-805 m to 1955-1995 m] DISTRIBUTION. The new records from the Rockall Bank and Hebridean Slope provide a consider- able extension of bathymetric range in the Trough from the maximum of c. 1000 m given in Part 1, although still well within the range known for this species. Ophiacantha bidentata (Retzius, 1 805) See: Paterson, 1985: 34-36, fig. 15. SAMPLES. ES 129(2,?[juvenile] 1),ES 184(61),ES 185(?[juvenile] 1),ES 1 97(1 60), ES 200(56), AT 20 1(265), ES 202(1 1), ES 207(?[juvenile] 1), AT 218(20), AT 219(308), AT 221(17), SBC 222(?[juvenile] 1), AT 228(6), AT 229(1), ES 232(23; ?[juvenile] 1), AT 233(95), ES 244(1, ?[juveniles] 3), AT 245(1 10), AT 247(32), AT 248(1), AT 251(4), ES 252(1), ES 255(3), AT 256(8), ES 257(1), ES 264(27), ES 266(2), AT 267(6), AT 271(93), AT 273(144), ES 283Guvenile 1), AT 288(1), ES 289(7), 13/83/6 OTSB(l), 3/85/7 OTSB(l), 3/85/17 OTSB(8). [980- 1005m to 2946m] DISTRIBUTION. The new records extend the upper bathymetric limit in the Trough from 1 330 m to c. 1000m. Ophiacantha crassidens Verrill, 1 885 See: Paterson, 1985: 40-41, fig. 17. SAMPLES. AT 223(4), AT 230(1). [1075 1862 m] DISTRIBUTION. The new records are from just south of the Wyville Thomson Ridge and Hebridean Slope and indicate a wider distribution within the Trough than the few previous samples suggested. Ophiolebes bacata Koehler, 1921 See: Paterson, 1985: 51, fig. 22. SAMPLE. AT 259(4). [1041m] DISTRIBUTION. Eastern Atlantic from the Bay of Biscay and off Madeira; 1 300-2034 m. This record from the North Feni Ridge is a considerable extension of range north to c. 57°N and to slightly shallower depths. Subfamily OPHIOTOMINAE Ophiotoma coriacea Lyman, 1883 See: Paterson, 1985: 57, fig. 23. SAMPLES. AT 22 1(1), AT 256(1). [160 5-1 705m] 170 HARVEY, GAGE, BILLETT, CLARK & PATERSON DISTRIBUTION. Recorded from both the western and eastern Atlantic; Cape Cod 1242m and the Azores to Iceland 1765-4106 m including a Helga record from SW. of Ireland. The present specimens from east of Rosemary Bank and the North Feni Ridge provide a small upward extension of bathymetric range in the eastern Atlantic and the first records from the Rockall Trough. Ophiolimna bairdi (Lyman, 1883) See: Paterson, 1985: 60, fig. 24. SAMPLE. ES 264(3). [2144-2910 m] DISTRIBUTION. This second record from the the foot of the Rockall Bank is shallower than the previous record by 750 m. The flow of cold water along the Feni Ridge and east side of the Rockall Bank may allow this circumpolar arctic species to extend into shallower depths on this side of the Trough. Subfamily OPHIOPLINTHACINAE Ophiomitrella clavigera (Ljungman, 1864) See: Paterson, 1985: 71, fig. 28. SAMPLE. AT 259(1). [104 1m] DISTRIBUTION. Known from both sides of the N. Atlantic: Davis Strait and W. Greenland; the Azores to the Faeroes; 1 66- 1 348 m. The single specimen was taken from the east side of Rockall Bank. Family OPHIACTIDAE Ophiactisabyssicola(M. Sars, 1861) See: Paterson, 1985: 76-78, fig. 32. SAMPLES. ES 990uvenile 1), ES 112(783; ?[juveniles 22), AT 153(2), ES 197(22), AT 201(2), ES 202(5), ES 218(1), AT 219(2), AT 223(18), AT 226(juvenile 1), AT 228(9), AT 229(33), AT 230(39), AT 233(1), AT 239(3), AT 247(19), AT 248(47), AT 249(1), ES 250(16), AT 251(6), ES 255(6), AT 256(2), AT 259(62), ES 261(1), ES 264(237), AT 271(32), AT 273(10), AT 287(21), AT 290(1), 13/83/1 OTSB(54), 3/85/28 OTSB(32), 3/85/29 OTSB(l), 3/85/30 OTSB(59). [168-3000 m] DISTRIBUTION. No change. Family AMPHIURIDAE Amphiura tritonis Hoyle, 1884 See: Mortensen, 1927: 213; Paterson, 1985: 85-86, fig. 33. SAMPLE. SBC 222(juvenile 1). [1 101 m] Fig. 2 Amphiura tritonis (a) ventral (b) dorsal view of disk; (c) ventral (d) dorsal view of the ends of the arms. Scale bars= 1 mm. ROCKALL TROUGH ECHINODERMS 3 171 DISTRIBUTION. A rare species having been recorded once from a position very near the current record just south of the Wyville Thomson Ridge and twice from the Bay of Biscay; 627-1290 m REMARKS. The undamaged specimen, which was recovered from a 0-25 m2 box core, is considerably smaller than the holotype from the same locality (disc diameters 2-5 and 12 mm respectively). The arm tips bear numerous newly added arm segments (Fig. 2c, d) which lack spines. This small specimen is characterised by the ventral interradial area being scaled; by large, broadly triangular oral papillae and by three arm spines, of which the middle one tends to be the largest (Fig. 2a). Of the three N. Atlantic species with similar characteristics, A. tritonis, A. richardi Koehler and A. abyssorum Norman, it appears to be closest to A. tritonis. The oral shield lacks the pronounced distal lobe seen in A. tritonis, but this might be due to the small size of the specimen. Both A. richardi and A. abyssorum lack scaling on the ventral interradial area and the oral papillae of A. abyssorum are spine-like. These features readily distinguish them from the Rockall specimens. Amphiura otteri Ljungman, 1871 See: Paterson, 1985: 86-87, fig. 33. SAMPLES. ES 1 12(1), SBC 205(1), ES 207(1), ES 231(3), ES 285(1). [1000-2906 m) DISTRIBUTION. The new records, while mainly from the SMBA Permanent Station in c. 2900m, include a record from 1 900 m on the South Feni Ridge. This, together with a 1 000 m record listed in Part 1 from the Hebridean Slope and its wide distribution in the N. Atlantic suggests that this species is tolerant of a variety of bottom conditions. The bathymetric range is 198-3200 m. Amphipholis squamata (Delle Chiaje, 1829) See: Paterson, 1985: 91, fig. 36. SAMPLES. ES 1 12(17), SBC 21 IGuvenile 1), ES 250(1). [402-1900 m] DISTRIBUTION. The record from ES 1 12 gives a further surprising extension of nearly 600 m to the known bathymetric range of this species; 0-1900 m. Amphilepis ingolfiana (Mortensen, 1933) See: Paterson, 1985: 93-94, fig. 37. SAMPLES. ES 27(2, ?[juveniles] 2), ES 118(2, juveniles 2), ES 129(1), ES 135(1, ?1), SBC 160(juvenile 1), ES 184(15, ?[juvenile] 1), ES 185(21), ES 197(76), ES 200(16), AT 201(1), ES 202(3), ES 204(5), ES 207(9), ES 218Guveniles 5), AT 219(5), SBC 220Guveniles 2), AT 221(1), ES 231(7), ES 232(6), AT 239(1), ES 244(juveniles 17), ES 255(1), AT 267(7), AT 271(1), SBC 272(3), AT 273(1), SBC 275(?[juvenile] 1), SBC 276Guvenile 1), AT 282(20), ES 283(9), ES 285(1), AT 286(4), ES 289Guveniles 31). [1047-2946 m] DISTRIBUTION. The record from AT 239 raises the upper limit of this species in the Rockall Trough to near the minimum of 957 m quoted by Mortensen (1933). Family OPHIOCHITONIDAE Ophiochiton ternispinus Lyman, 1883 See: Paterson, 1985: 96-97, fig. 39. SAMPLES. AT 221(5), AT 223(3), AT 228(4), AT 229(1), AT 230(1), AT 239(1), AT 251(1), ES 255(1), AT 256(2), AT 287(1), 13/83/1 OTSB(2), 1 3/83/2 OTSB(2), 13/83/5 OTSB(l), 9/84/9 OTSB(l), 3/85/17 OTSB(l), 3/85/29 OTSB(7), 3/85/30 OTSB(6). [1047-2200 m] DISTRIBUTION. The new records from the Hebridean Slope raise the known upper bathymetric limit within the Trough by 700 m. 1 72 HARVEY, GAGE, BILLETT, CLARK & PATERSON Family OPHIURIDAE Subfamily OPHIURINAE Ophiopleura inermis (Lyman, 1 878) See: Paterson, 1985: 128, fig. 48. SAMPLES. AT 223(6), AT 230(5), AT 239(3), AT 248(4), AT 249( 1 ), ES 250(4), AT 259(6), AT 290( 1 0), 1 3/83/2 OTSB(3), 13/83/6 OTSB(182), 9/84/13 OTSB(3), 3/85/8 OTSB(3), 3/85/9 OTSB(28), 3/85/13 OTSB(35), 3/85/20 OTSB(18), 3/85/23 OTSB(2), 3/85/24 OTSB(52), 3/85/25 OTSB(8), 3/85/26 OTSB(ll), 3/85/27 OTSB(3), 3/85/28 OTSB(119), 3/85/31 OTSB(l), 3/85/32 OTSB(2), 3/85/33 OTSB(21), 3/85/36 OTSB(6), 3/85/46 OTSB(3). [650-805 m to 1271 m] DISTRIBUTION. No change. Homophiura tesselata (Verrill, 1 894) See: Paterson, 1985: 135-138. SAMPLES. AT 181(4), AT 228(1). [1785-1 845m to 2264m] DISTRIBUTION. No change. Amphiophiura saurura (Verrill, 1894) See: Paterson, 1985: 134, fig. 50. SAMPLE. 3/85/20 OTSB(4). [1225-1245 m to 1900 m] DISTRIBUTION. This record extends the known distribution within the Trough to the Hebridean Slope and into shallower water. Ophioctengracilis(G. O. Sars, 1871) See: Paterson, 1985: 130, fig. 50. SAMPLES. ES 6(juveniles 1583), ES 14(juveniles 88), ES 15(juveniles 2908), ES 27(juveniles 5), ES 57(juveniles 76), ES 105(juveniles 3362), ES 129(juveniles 5, ?[juvenile] 1), SBC 150(juveniles 39), SBC 160Guveniles 3), SBC 163(juveniles 5), SBC 174(juvenile 1), ES 178(juveniles 789), ES 184(juveniles 654), SBC 188(]uvenile 1), ES 197(juveniles 2700), ES 200(juveniles 9), ES 202(juvenile 1), ES 204(juvenile 1), ES 2070uveniles 38), SBC 2 1 5(juveniles 2), SBC 2 1 6(?[juvenile] 1 ), ES 2 1 8(juveniles 1 768), SBC 220(juvenile 1 ), AT 226(3), AT 239( 1 62), ES 244Guveniles 285), ES 264(9), SBC 276(juveniles 4), SBC 278(juveniles 3), ES 283(juveniles 10), AT 290(11), 13/83/6 OTSB(118), 13/83/7 OTSB(95), 9/84/2 OTSB(27), 9/84/13 OTSB(54), 3/85/10 OTSB(68), 3/85/24 OTSB(IO), 3/85/26 OTSB(3), 3/85/28 OTSB(25), 3/85/36 OTSB(l). [704-2946 m] DISTRIBUTION. No change. Ophiocten hastatum Lyman, 1878 See: Paterson, 1985: 129, fig. 49. SAMPLES. SBC 64(1), ES 111(2), ES 129(2), ES 185(8), ES 204(1), ES 207(1, ?1), ES 266(1), AT 267(1), ES 283(2), 3/85/5 OTSB(9). [2000 m to 2970-2980 m] DISTRIBUTION. The new records slightly extend the bathymetric range within the Trough of this esentially abyssal species. Ophiura carnea Liitken, 1 858 See: Paterson, 1985: 117, fig. 42. SAMPLE. 3/85/9 OTSB(l). [630-2857 m] DISTRIBUTION. The new record extends the known distribution within the Trough to the Hebridean Slope. ROCKALL TROUGH ECHINODERMS 3 1 73 Ophiura scomba Paterson, 1985 See: Paterson, 1985: 125-127, figs 46 & 56; Gage et al., 1983: 297-298 (as O. irrorata). SAMPLES. AT 201(1), ES 218(1), AT 219(1), AT 245(1), AT 247(28), ES 252(5), AT 254(3), ES 255(1 1), AT 256(24), ES 257(7; ?[juvenile] 1), ES 261(17), ES 264(13), 3/85/17 OTSB(l). [1510-2220 m] DISTRIBUTION. O. scomba is known from Rockall south to Morocco; 1 595-4406 m. The new records are from the North Feni Ridge and also in the vicinity of a 2200 m repeat station (Sta. 'M') in the northern Rockall Trough and provide a new slightly shallower upper bathymetric limit. REMARKS. This species was recorded as O. irrorata in Part 1 . Subsequent studies have shown that the Rockall specimens should be referred to O. scomba. The swollen oral shields, rounded ventral arm plates and pointed oral papillae distinguish this species from its congener O. ljungmani, which has an overlapping bathymetric distribution in the Trough. Ophiura ljungmani (Lyman, 1878) See: Paterson, 1985: 1 18-120, fig. 44. SAMPLES. ES 27(172), ES 57(927), SBC 58(2), ES 105(juveniles 13), ES 111(623), ES 118(401), ES 129(951), SBC 159(juveniles 3), SBC 160(juvenile 1), SBC 163(juveniles 2), ES 180(305), ES 184(359), ES 185(634), ES 197(807), ES 200(juveniles 70), AT 201(8), ES 202(69), ES 204(106), SBC 205Guvenile 1), ES 207(232), ES 218(1 94), AT 2 1 9(8), SBC 220(2), AT 228(4 1 ), ES 23 1 (286), ES 232(26), AT 233( 1 6), ES 244( 1 70), AT 245( 1 7), AT 247(3), ES 264(67), ES 266(2 1 ), AT 267(22), AT 27 1 (6), AT 273( 1 4), SBC 278(juvenile 1 ), ES 283(4 1 4), ES 285(39), AT 288(4), ES 289Guveniles 111), 13/83/5 OTSB(2). [1050 m to 3425-3500 m] DISTRIBUTION. No change. Ophiura ophiura (Linnaeus, 1 758) See: Sussbach & Breckner, 191 1: 234-241 (as O. ciliaris); Mortensen, 1927: 236-238, fig. 128 (as O. texturata). SAMPLES. SBC 210(71), AT 292(2), 13/83/3 GT(8), 3/85/43 OTSB(2). [220-270 m to 704 m] DISTRIBUTION. These new records confirm the presence of this sublittoral to bathyal species at depths > 500 m on the Hebridean Slope as reported from a single record in Part 1 . Subfamily OPHIOLEPIDINAE Ophiomusium lymani Wyville Thomson, 1 873 See: Paterson, 1985: 147-148, fig. 58. SAMPLES. ES 105(juveniles2), ES 184(1 196), ES 185(juvenile 1), AT 186(1015), ES 197(451), ES 200(240), AT 20 1 (948), ES 202(3 1 ), ES 2 1 8(juveniles 1 2), AT 2 1 9( 1 458), SBC 220(juvenile 1 ), AT 22 1 (44), AT 228( 1 224), ES 232( 1 2 1 ), AT 233( 1 039), AT 239(3), ES 244(48), AT 245(392), AT 247(39 1 ), ES 250(2), AT 25 1 ( 1 7), ES 252(6), AT 254(12), AT 256(86), ES 257(12), ES 261(3), ES 264(10), AT 271(860), AT 273(572), ES 285(20), AT 287(3), AT 288(1787), ES 289(171), 13/83/5 OTSB(417), 3/85/7 OTSB(44), 3/85/17 OTSB(1800), 3/85/29 OTSB(1614), 3/85/30 OTSB(29). [810-2921 m] DISTRIBUTION. No change. Class ECHINOIDEA Order CIDAROIDA Family CIDARIDAE Cidaris cidaris (Linnaeus, 1 758) SAMPLES. AT 223(1), AT 292(3), 13/83/8 OTSB(l), 9/84/10 OTSB(l), 3/85/28 OTSB(4), 3/85/31 OTSB(l), 3/85/43 OTSB(155), 3/85/44 OTSB(52). [500-560 m to 1075 m] DISTRIBUTION. No change. 1 74 HARVEY, GAGE, BILLETT, CLARK & PATERSON Poriocidaris purpurat a (Wyville Thomson, 1872) SAMPLES. AT 223(3 1 ), AT 230(4), AT 239( 1 ), AT 248(3), AT 259( 1 ), 1 3/83/2 OTSB(3). [ 1 04 1 - 1 296 m] DISTRIBUTION. The record from AT 223 is near the type locality of this species. The new records raise the known upper bathymetric limit for the Rockall Trough by c. 1 50 m. Order ECHINOTHURIOIDA Family ECHINOTHURIIDAE Araeosomafenestratum (Wyville Thomson, 1869) SAMPLES. 1 3/83/2 OTSB(l), 1 3/83/7 OTSB(l). [631 m to 1265-1 130m] DISTRIBUTION. These new records from the Hebridean Slope provide an extension of the lower bathymetric range of this species in the NE. Atlantic. Calveriosoma hystrix (Wyville Thomson, 1869) SAMPLES. AT 223(19), AT 239(1), AT 248(2), AT 259(2), AT 291(11), AT 3(1), 13/83/2 OTSB(6), 13/83/6 OTSB(180), 13/83/7 OTSB(5), 9/84/1 OTSB(2), 9/84/2 OTSB(3), 9/84/10 OTSB(l), 9/84/1 3 OTSB(45), 3/85/8 OTSB(l), 3/85/9 OTSB(3), 3/85/10 OTSB(8), 3/85/13 OTSB(183), 3/85/14 OTSB(126), 3/85/18 MBA(109), 3/85/19 MBA(16), 3/85/25 OTSB(103), 3/85/28 OTSB(l). [580-630 m to 1265-1 130m] DISTRIBUTION. The new records extend both the upper and lower bathymetric limits of this species within the Trough. The numbers taken in fish trawls suggest that it is abundant on the Hebridean Slope at around 1000 m. REMARKS. The specimen from AT 239 was in excellent condition when recovered, with most of its long red spines intact and the body wall still supported by coelomic fluid. Trawled specimens are generally almost completely devoid of spines and give little impression of the magnificence of this species in life. The size-frequencies (Table 1) from semi-balloon trawls (OTSB) suggest that the largest individuals occur at the upper end of the depth range on the Hebridean Slope, whereas recruitment occurs towards the lower end of the depth range. The occurrence of juveniles at a greater depth than adults has been noted in a number of echinoderm taxa in the Rockall Trough (Gage et al., 1983, 1985<2). The smallest individual recovered measured 55mm, considerably larger than the smallest echinoids taken with this trawl, suggesting that recruitment may be sporadic in this non-seasonally reproducing species (Tyler & Gage, 19840). Hygrosomapetersii(A. Agassiz, 1880) SAMPLES. AT 230(2), AT 233(2), AT 239( 1 ), AT 282( 1 ), ES 283(2), AT 286(3), AT 287(2), SWT 27(2), 1 3/83/ 1 OTSB(l), 13/83/5 OTSB(l), 3/85/5 OTSB(IO), 3/85/21 OTSB(l), 3/85/30 OTSB(9), 3/85/45 OTSB(3). [11 60m to 2970-2980 m] DISTRIBUTION. The new records provide a small extension of the known lower bathymetric limit, the total range now being 730-2980 m. Sperosoma grimaldii Koehler, 1897 SAMPLES. AT 239(9), AT 248(2), AT 249(72), 13/83/2 OTSB(167), 13/83/5 OTSB(l), 13/83/6 OTSB(40), 9/84/13 OTSB(6), 3/85/8 OTSB(2), 3/85/9 OTSB(l), 3/85/1 1 OTSB(4), 3/85/13 OTSB(3), 3/85/18 MBA(88), 3/85/19 MBA(37), 3/85/20 OTSB(62), 3/85/23 OTSB(l), 3/85/24 OTSB(19), 3/85/25 OTSB(58), 3/85/28 OTSB(7), 3/85/33 OTSB(17), 3/85/43 OTSB(2). [565-700 m to 2910 m] DISTRIBUTION. Intensive trawlings on the Hebridean Slope suggest that this species is common at around 1000 m where it is frequently recovered with Calveriosoma hystrix. The upper bathymetric limit within the Trough is raised by around 500 m. REMARKS. Size-frequency data (Table 1) suggest that this species attains a smaller size on the Hebridean Slope than Calveriosoma hystrix. It appears also that as in C. hystrix the smallest ROCKALL TROUGH ECHINODERMS 3 175 0 O ON NO O O O — O OO — O O O oo m OOOfNO OOOO O O OOOrNO rN O — ' fN _ SO rn £ O O — OO O fN rN — f> a O O in rN 2 O O O n-> O n NO O fN — OOOOOOOO — rxi — _ _< rs] •o u u O O O fNNOooNom ON^>n— inoot^o — ^f — o — q3 O O O rN ON OO O ^^^SIC ^"^^ ^2^^^^^r^°S «J "o O O O — oo (^ U £-£^5 ?Q S^r^r^^^So^^ (M O T3 C O O O f*^ £ — NO NO^fN >n — ' TJ- ONfNin 0 o 0 0 O ON NO m c »n*nm inmino inm^n ooooo oomo oinooooo'nino oorj-NOfNO fioorso rot^ooinm^NOmrNO ON ON ON t — f*> •— ' ON O */^ St rn r*"i ro r*^ ^~ ^f l/") *O */~i v^ i: oooooooooo -2 oooooooo ^ op^op^oo^oo^oo^oo^oo^op^op^op^ N ~5 *s ' ^ S3 — R H U Q i g 1 •^ N^ O ..'. ^1 O U-. U-. (J-. t-~. ^ oooooooooo o oooooooo S oooooooooooooooooooo ^ ON ^— Tj* "^ ^f ^ ONON^Tt ^ ON ON ON ON — ^ ' — '^Tt^^f^f Q rN "^ oo oo m .^ — fN rN m ;? — -^ rN fN " . oo — rs c*i 50 mm in test diameter are 6-1 1 yr old. The estimated age of specimens of around 30 mm is 6 yr and agrees fairly well with results of Sime & Cranmer ( 1 985) from a study of populations at depths of 108-149 m in the northern North Sea. Echinus affinis Mortensen, 1903 SAMPLES. ES 1120uveniles 94 [not 1073 as stated in Part 2]), AT 154(116), ES 176(7, ?[juveniles] 73), AT 1 77(548), ES 1 84(58), AT 1 92(? 1 7), ES 1 97( 1 1 0, ?[juveniles] 8), ES 200(62, ?[juvenile] 1 ), ES 2 1 8(6, juveniles 2), ES 232(11), ES 244(10, ?0uveniles] 5), AT 245(92), AT 247(291), ES 264(130, ?[juveniles] 4), AT 267(7), AT 271(154), AT 273(708), AT 288(122), ES 289(14), 13/83/5 OTSB(191), 9/84/9 OTSB(78), 3/85/7 OTSBGuvenile 1 ), 3/85/1 7 OTSB(204), 3/85/29 OTSB(22), SWT 1 3(none [listed as 3 in Part 2]). [1 605-2605 m] ROCKALL TROUGH ECHINODERMS 3 1 77 DISTRIBUTION. The new records extend the known lower bathymetric limit of this species slightly. LIFE HISTORY. In the northern Rockall Trough at Sta 'M' in 2200 m where this species is abundant, E. affinis has a seasonal reproductive cycle and probably produces a planktotrophic larva. This seasonal reproduction is thought by Tyler & Gage ( 1 9846) possibly to be tuned to a pulsed annual fallout of phyto-detrital food to the sea floor in this area. Additional studies at this station have revealed skeletal banding which is thought to result from a seasonal growth pattern controlled by the same factor (Gage & Tyler, 1985). Adults were inferred to be up to c. 28 years old. These latter authors also indicate that postlarval survivorship is probably very low; a markedly uneven representation of ages in a large sample aged by means of growth rings was interpreted by them as probably reflecting multi-year cycles in recruitment success. Echinus alexandri Danielssen & Koren, 1883 SAMPLES. ES 112(12, ?[juveniles] 108), AT 248(7), AT 251Guvenile 1), AT 256(3), AT 259(4), AT 288(1), 13/83/1 OTSB(3), 3/85/30 OTSB(?[juvenile] 1). [1041-2300 m] DISTRIBUTION. The new records raise the upper bathymetric limit in the Trough by c. 230 m. Echinus elegans Diiben & Koren, 1 844 SAMPLES. AT 287(718), AT 291(63), 13/83/3 GT(3), 13/83/6 OTSB(7), 13/83/7 OTSB(l), 13/83/8 OTSB(l), 9/84/2 OTSB(15), 9/84/13 OTSB(3), 3/85/9 OTSB(241), 3/85/13 OTSB(77), 3/85/14 OTSB(5), 3/85/18 MBA(9), 3/85/20 OTSB(?10), 3/85/23 OTSB(l), 3/85/24 OTSB(21), 3/85/25 OTSB(l), 3/85/28 OTSB(205), 3/85/31 OTSB(2), 3/85/36 OTSB(l). [220-270 m to 1 210(71 383) m] DISTRIBUTION. The new records extend the known distribution within the Trough onto the shelf to considerably shallower depths than reported in Part 2, although still within the overall recorded range for this species. REMARKS. The maximum size of the specimens was 93 mm in test diameter, which is close to the maximum of 80 mm given by Mortensen (1927). Morphometric data from these large samples is given by Gage et al. (1986), these measurements showing good agreement with more limited data given by Mortensen (1943) from material collected from various other locations. The size frequencies of the Rockall samples are variable from haul to haul, with from one to three modes present; these appeared to show no relationship to either time of year or bathymetry. This species occurs at depths similar to those of trawlings yielding large numbers of its congener E. acutus var. norvegicus; yet, as pointed out above for the latter species, analysis of these hauls shows that in all of them either one or the other species is overwhelmingly dominant, while in many only one species occurs. Gage et al. (1986) suggest that this may result from differing habitat requirements. The muddy gut contents of E. acutus var. norvegicus indicate deposit feeding, while the varied particu- late remains found in E. elegans, that include both sediment and small prey, suggest a more omnivorous diet (Mortensen, 1943; Gage et al., 1986). LIFE HISTORY. The sexes are separate and equal in number. Females show a seasonal cycle in oogenesis, spawnout probably occurring in March. An egg size up to 60 um diameter is indicative of planktotrophic development as in other species of this genus (Gage et al., 1986). These authors interpret growth banding visible in the skeletal plates as reflecting a seasonal growth pattern. Counts of these growth zones and a fitted growth curve indicate that a size of 70 mm test diameter is reached at an age of 12-20 yr. Order SPATANGOIDA Family HEMIASTERIDAE Hemiaster expergitus Loven, 1874 SAMPLES. ES 15(juveniles 2), ES 18(juveniles 3), SBC 61 (juveniles 3), SBC 156(juveniles 3), SBC 160(juveniles 2), SBC 168(1), ES 172Guveniles 2), ES 176(juveniles 3), AT 177(?[juvenile] 1), ES 197(5), ES 204(juvenile 1), ES 207(1, juvenile 1), ES 218(juveniles 52), SBC 220(juveniles 2), SBC 222(juvenile 1), ES 232(2, juveniles 3), 1 78 HARVEY, GAGE, BILLETT, CLARK & PATERSON AT 239(juveniles 15), ES 244(juveniles 19), AT 245(9), ES 250(juvenile 1), AT 251(2), ES 252(40), ES 255(juveniles 4), ES 261(1), AT 271(1), AT 282(1), ES289(juvenilel). [1047-2910 m] DISTRIBUTION. These records raise the upper bathymetric limit slightly within the Trough. LIFE HISTORY. Counts of growth bands present in the test plates indicate a test length of 30 mm might be reached by c. 16 yr (Gage, 1987). Family SPATANGIDAE Spatangus raschi Loven, 1869 SAMPLES. SBC 210(?[juveniles] 4), AT 239(juvenile 1), AT 291(36), 13/83/7 OTSB(54), 13/83/8 OTSB(2), 9/84/1 OTSB(l), 3/85/10 OTSB(13), 3/85/13 OTSB(l), 3/85/14 OTSB(40), 3/85/18 OTSB(3), 3/85/26 OTSB(l), 3/85/43 OTSB(37). [225 m to 990-1020 m] DISTRIBUTION. The new records are all from the Hebridean Slope and extend the lower bathymetric limit within the Trough by some 200 m. This species appears to be most common in the 500-800 m depth zone in this area. Brissopsis llyrifera (Forbes, 1 84 1 ) See: Mortensen, 1907: 152-160, pi. 3, figs 2, 3, 7, 1 1, 12, 18, 20-23, pi. 4, figs 2, 3, 9, 14-17, pi. 18, figs 1, 6, 12, 18, 25-26, pi. 19, figs 3, 6, 10, 15, 18-21,29,34; 1927: 338-340, figs 200, 201; 1951: 380-390, pi. 30, figs 1-4, 7-13, pi. 32, figs 15, 20, 22, pi. 57, fig. 15; Gage et al., 1985a: 187, fig. 3 (as Brissopsis sp.). SAMPLES. ES 99(1), AT 239(31 + fragments). [1047-1 160 m] DISTRIBUTION. NE. Atlantic from Lofoten, S. and W. Iceland along the European coasts and the Mediterranean to S. of the Canaries; c. 5-1400 m; in soft mud. REMARKS. Except for the specimen from ES 99, the present material is all from a large haul (AT 239) of small, very fragile specimens, most of which were broken when examined. In this haul the cod-end of the trawl was full of a muddy deposit containing Brissopsis, specimens of Hemiaster expergitus (see above), and a single specimen of Brisaster fragilis (see below). The largest intact specimen measures 22-9 mm and the smallest 9 mm in test length. It is likely that smaller specimens had been lost through the 10 mm-wide meshes of the trawl. B. lyrifera is typically an inshore species, with only a few, somewhat doubtful records from deep water (Mortensen, 1927). For example, it seems very unlikely that it is this species that Thomson (1874) records from depths to 2090 fathoms (3873 m) from the Porcupine in 1869. However, the absence of any confluence in the posterior petals of the present material from deep water immedi- ately distinguishes it from the species Brissopsis atlantica and B. mediterranea which are known to occur to bathyal depths in the western Atlantic (Chesher, 1968). Furthermore, B. mediterranea, although known from the eastern Atlantic and Mediterranean, is thought there to be restricted to relatively shallow water. The present specimens are similar in size and appearance to two lots, each consisting of two partly broken specimens about 1 5 mm in length, labelled as Brissopsis lyrifera, in the collections of the British Museum (Natural History) (BMNH). These were dredged by the Triton (presumably on her voyage in 1882, see Deacon, 1977) from 942m and 1170m depth, respectively, from the Wyville Thomson Ridge and Faroe Bank Channel. A larger specimen at BMNH measuring 27-5 mm length was collected by the Helga in 1909 from the Porcupine Seabight at 956-1088 m depth (see Farran, 1913). The fragmented specimen recorded under 'Brissopsis sp.' in Part 2 that was taken from the same area and depth on the upper Hebridean Slope as the specimens from AT 239 is now identified as Brissopsis llyrifera. On the basis of the lengths and widths of the anterior and posterior petals it is estimated that this specimen was about 30 mm in test length. The pedicellaria in Fig. 3a, b of Part 2 from this specimen is a rostrate pedicellaria and not globiferous as labelled. Similar rostrate pedicellariae were found on inshore B. lyrifera. Examples of the double-pronged globiferous pedicellariae typical of B. lyrifera were not found on any of the deep- water specimens from BMNH. The tridentate pedicellaria in figure 3c of Part 2 that was also obtained from the large fragmented specimen from ES 99 agrees somewhat with Mortensen's ROCKALL TROUGH ECHINODERMS 3 179 0 o •o o. o o OH C ° 1^ "O lyj V3 O O S) 0 o\ "5 cd |1 fr| 0 03 s^ — 03 n » •_— M 'C "fi u i o> N S 01 » 1 s H2 .00 JS Jd 00 o ex fc « J _§" S rt Q ^ t/3 S II rrj •^ t. N *y^ .2 J. oo C fe • C ?3 ^3 6 ^•?5 2 o oo c — i r^ ON __ .00 cj ac: ^ -S -S 5 ^ oo oi oo v> C C C (L) (U (U O 2 .2-n J-H ±2 S.D. 1 80 HARVEY, GAGE, BILLETT, CLARK & PATERSON (1907) third form of tridentate of B. lyrifera, examples of the other two kinds, although described by Mortensen as richly developed, not being found on the present specimens. However, a typical form of the largest, narrow-bladed variety of tridentate pedicellaria, with the valves rather widely separated along their lower length, was found on one of the B. lyrifera from the Triton. Not surprisingly, no pedicellariae were found on the somewhat denuded specimens from AT 239. Measurements of 21 of the morphometric characters of the test, established by Chesher (1968), were made on the Triton and Helga specimens (although the accuracy of many of these is reduced as a result of not removing their spines) and on the present material from AT 239. In Table 2 these data are compared to similar measurements on inshore specimens dredged in 1968 from c. 165 m depth in the Arran Deep, Firth of Clyde, in the possession of J. D. G. The relatively small number and limited size range of the sample of inshore specimens is insufficient to adequately define the natural variation in this species, in which monstrosities in test form are known to occur (Brattstrom, 1946, Mortensen, 1951). However, measurements on specimens in BMNH trawled from stations in the Minch (c. 58°N, 06'W) by the Scottish Fisheries Board in 1927, nearly all lie within 2 S.D. of the mean of the measurements on those from the Arran Deep, only measurements of the span of the posterior petals on two specimens in one of the hauls falling slightly below this range. In contrast, values of 9 out of 21 characters measured on the small deep-water urchins fall outside 2 S.D. of the mean for the Arran Deep sample for some specimens while for 5 of these characters measurements on all specimens fall outside this range (Table 2). The present, and our previous, finds of this urchin in the SMBA samples concur with Thomson (1874) who noted that at great depths specimens of B. lyrifera decrease in size, having '. . . all the appearance of being very young . . .'. However, on the present material genital pores were present on specimens as small as 1 5 mm test length, which also possessed small gonads, indicating that sexual maturity is reached at a small size. Such differences might suggest that the deep water urchins constitute a distinct taxonomic entity. However, Brissopsis lyrifera is known to have a planktotrophic echinopluteus that may be dispersed over wide areas. Since such larvae are likely to stay in the plankton for some time, it seems likely that the deep-water populations off the W. of Scotland are in genetic continuity with inshore stocks. The small size of the deep-water individuals possibly then results from dwarfing as a result of resource limitation in the deep sea. The differences in test characters may possibly reflect other differences in bottom conditions as well as their smaller size. Until the range of variation amongst larger inshore samples, covering both a wider range in size and bottom environment, becomes better understood the possible separate identity of the deep-water urchins must remain uncertain. Brisaster fragilis (Diiben & Koren, 1844) See: Mortensen, 1907: 108-123,pl. I,figs6-7,pl. 13,pl. 14, fig. 3, 7, 11, 13, 16, 18,20,24-25,31,37,39,43,46, 50-51; 1927: 325-326, figs 187, 2-3, fig. 188, 2, fig. 189, 1-2. SAMPLES. SBC 224(1), AT 239Guvenile 1). [903-1047 m] DISTRIBUTION. NE. Atlantic from Finmark to Bergen, to north and west of the Shetlands, the Faroe-Shetland Channel, and from south and west of Iceland. In the western Atlantic from the Davis Strait to Florida; c. 65-1300 m on soft mud. REMARKS. The single specimen recovered in perfect condition from a box-core sample (SBC 224) measures 38 mm in overall test length. It was collected from 903 m depth in the Faroe Shetland Channel, where this species was previously taken by the Porcupine at about the same depth. The juvenile specimen from AT 239 measures 10-5 mm test length and was recovered from 1047 m on the upper continental slope west of Barra in a haul containing a mixed sample of small Brissopsis llyrifera and juvenile Hemiaster expergitus. As shown in the growth series figured and described by Mortensen (1907, pi. 13) the posterior petals at this size are relatively undeveloped. Genital pores, indicating sexual maturity, were not found, although Mortensen (1907) remarks that they appear at a size of 9-1 1 mm. ROCKALL TROUGH ECHINODERMS 3 181 The present records extend the recorded range of this species in the NE. Atlantic from the Faroe Shetland Channel to a latitude of 57°N in the Rockall Trough. REPRODUCTION. The large yolky eggs of Brisaster fragilis are thought to indicate direct development (Mortensen, 1907, 1927). Order POURTALESIOIDA Family POURTALESIIDAE Pourtalesia miranda A. Agassiz, 1869 SAMPLES. ES 59(8), ES 1 18(2), ES 120(2), ES 122(4), ES 143(3), ES 147(2), ES 152(3), ES 164(3), ES 204(9 [not 54 as stated in Part 2], ?[juvenile] 1), ES 207(6), ES 266(2), AT 282(1), ES 283(1). [2245-2946 m] DISTRIBUTION. The additional records extend the lower bathymetric limit slightly within the Trough. Echinosigra phiale (Wyville Thomson, 1874) SAMPLES. ES 27(24), ES 59(2), ES 111(2), ES 118(7), AT 121(14), ES 122(10), ES 129(9), AT 153(2), ES 172(23), ES 180(3), ES 184(1), ES 185(37), ES 197(5), ES 204(19), ES 207(15), ES 218(4), ES 231(6), AT 245(2), ES 257(1), AT 267(5), AT 282(6), ES 283(14), ES 285(3), AT 286(2), ES 289(2). [1993-2946 m] DISTRIBUTION. The lower bathymetric limit within the Trough is extended slightly and predictably, given the abyssal distribution of this species. LIFE HISTORY. Counts of growth zones present in the plates of the test indicate a size of 50 mm length may be reached by an age of 5-8 yr (Gage, 1987). Class HOLOTHURIOIDEA Order DENDROCHIROTIDA Family PSOLIDAE P solus pourtalesi Theel, 1886 SAMPLE. AT 247(233). [2084-2190 m] DISTRIBUTION. This sample, like the first described in Part 2 (Gage et al., 1985«) was taken from the west side of the Trough. The specimens were recovered from the base of Rosemary Bank close to areas where this species was found during the 7«go//"Expedition (Heding, 1942). Gage et al. (1985#) followed Mortensen (1927) in reporting P. pourtalesi from the West Indies. Mortensen (1927) cited specimens from the Blake Expedition (Theel, 18866), but these came from the eastern seaboard of North America, not the West Indies. P. pourtalesi has not been recorded south of 39°N in the western Atlantic. The lower bathymetric limit reported in Part 2 as 2271 m should be increased slightly to 2341 m to include the records of Deichmann (1940). The total range is therefore 1096-234 1m. REMARKS. Heding (1942) and Gage et al. (1985a) refer to this species as P. pourtalesii but it should be referred to as P. pourtalesi as in the original description (Theel, 18866). The present specimens were found attached to a collection of small, probably ice-rafted, cobbles. The specimens range from 12-33 mm in length. There is some suggestion of bimodality in the size distribution, with a small mode around 16 mm and a much larger mode around 25 mm (Table 3). Table 3 Psolus pourtalesi length frequencies from station AT 247 Lower bound of size class (mm) 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 Frequency 1 3 2 2 5 4 3 8 13 12 13 32 28 33 24 16 13 5 7 3 2 1 (n = 230) 1 82 HARVEY, GAGE, BILLETT, CLARK & PATERSON Family PARACUCUMIDAE Paracucumana hyndmani (Thompson, 1 840) See: Mortensen, 1927: 400-401, figs 237, 3; 239, 1 (as Cucumaria hyndmani); Madsen, 1942: 395-406, figs 1-6 (as Cucumaria hyndmani). SAMPLE. 13/83/8 OTSB(l). [500-560 m] DISTRIBUTION. The coasts of Europe from the Mediterranean north to the Shetland Isles and the coast of Norway including Rockall Bank. Mortensen (1927) notes that it is usually found in deep water, c. 20-1 150 m. The present specimen was taken at the top of the Hebridean Slope. REMARKS. Madsen (1942) recognised two forms of the species which he considered 'would prove to be of two geographical races of the same species': a more northern P. (Cucumaria) hyndmani f. typica and a more southern P. (Cucumaria) hyndmani f. robusta. Our single specimen agrees with the northern form and is close to the locality of a deep-water specimen examined by Madsen ( 1 942, p. 405). Family SCLERODACTYLIDAE Pseudothyone raphanus (Diiben & Koren, 1844) See: Mortensen, 1927: 407^*08, fig. 242: 2, 245: 1 (as Thyone raphanus); Panning, 1949: 456-457, fig. 52. SAMPLE. SBC 222(4, ?[juveniles] 2), AT 248(1 1). [1 101-1 150 m] DISTRIBUTION. P. raphanus occurs around the coasts of the British Isles and Norway as far north as c. 65°N. It is also known to occur in the Mediterranean. Bathymetric range c. 10-1050 m, the present records extending this slightly to 1 150 m. REMARKS. The two juvenile specimens from SBC 222, both 1 mm long, have only primary cross deposits which differ from the plate deposits normally found in adult P. raphanus. However, primary cross deposits are the precursors to plates, and in specimens intermediate in size, 3 to 4 mm long, both types of deposits occur. Family CUCUMARIIDAE Thyone fusus (O. F. Muller, 1776) See: Madsen, 1941: 17-26, Figs 3b, 4g-h, 7b, 12-16. SAMPLES. SBC 21 1 (juvenile, 1). [402 m] DISTRIBUTION. Northeast Atlantic from Trondheim Fjord to the Mediterranean, including the North Sea and adjacent Scandinavian Seas. There is some uncertainty in the bathymetric range of this species since T. fusus has been confused in the past with other species, such as T. gadeana Perrier and T. wahrbergi Madsen. From his analysis of Scandinavian holothurians, Hansen con- siders that T. fusus generally occurs between 10 and 200m (Hansen, pers. comm.). The present specimen from 402 m increases the lower bathymetric limit. However, since the specimen is a juvenile it is possible that as with several asteroids, ophiuroids and echinoids (Gage et al. 1983, 19850) the lower bathymetric limit is greater for juveniles than for adults. REMARKS. The specimen is only 2-5 mm long. The deposits of the body wall are irregular polyporous plates similar to those described for T. fusus f. subvillosa (Herouard, 1890; Madsen, 1941) with a spire made of two slender columns as in T. fusus and unlike those of T. wahrbergi and T. gadeana. The tubefeet are large in comparison to the size of the body and have terminal plates 100 to 125 um in diameter. These are smaller than the plates found in adult specimens but possess the concentric circles of large holes typical of T. fusus. The size of the specimen precluded an examination of the tentacle deposits. ROCK ALL TROUGH ECHINODERMS 3 183 Order DACTYLOCHIROTIDA Family YPSILOTHURIIDAE YpsilothuriatalismanitalismaniE. Perrier, 1886 SAMPLES. SBC 168(3), SBC 222(10, juvenile 1), AT 226(1), AT 230(2), AT 239(37), AT 248(8), ES 250(38). [c. 1000-1271 m] DISTRIBUTION. These additional records extend the distribution of this species to the North Feni Ridge and provide a geographical link between our previous records from the Rockall Trough and those of the Ingolffrom Iceland. Furthermore they confirm the essentially bathyal distribution of this species. Ypsilothuria bitentaculata attenuata R. Perrier, 1902 SAMPLES. ES 27(79, juvenile 1), ES 56(15), ES 111(23), ES 118(37), ES 129(30), ES 184(31, juvenile 15), ES 1 85(22 1 ), ES 1 90(48), ES 200( 1 1 3), ES 204(33 [not 78 as stated in Part 2]), ES 2 1 8(92), ES 23 1 (97), ES 232(1 8), AT 233(2), ES 244(20), AT 245(268), ES 26 1 ( 1 ), ES 266(4), AT 267(80), AT 27 1 (4), AT 273( 1 0), AT 282(5), ES 283(67), ES 285(5), AT 286(7), AT 288(6), ES 289(41). [1862-2951 m] DISTRIBUTION. No change. Echinocucumis hispida (Barrett, 1857) SAMPLES. SBC 222(juveniles, 3), AT 248(8), ES 250(13), 3/85/9 OTSB(l). [945-1270 m] DISTRIBUTION. These records from the Feni Ridge and Hebridean Slope broaden the known geographic and bathymetric range of this species within the Trough. Order ASPIDOCHIROTIDA Family SYNALLACTIDAE Bathyplotes natans (M. Sars, 1868) SAMPLES. AT 239(37), AT 248(3), AT 249(1), AT 259(1), 13/83/2 OTSB(25), 3/85/36 OTSB(2). [1000-1025 m to 11 30-1 265m] DISTRIBUTION. No change. REMARKS. These specimens were in better condition than those described in Part 2, and had spicules present in both the skin and papillae. A mid ventral groove was a distinctive feature of the better preserved specimens. The colour in spirit was off-white with the orange body organs showing faintly through the skin. Benthothuriafunebris R. Perrier, 1902 SAMPLES. ES 204(2), AT 284(1), ES 285(1), AT 286(9), 3/85/5 OTSB(9). [2890-2996 m] DISTRIBUTION. No change. Paelopatides grisea R. Perrier, 1902 SAMPLES. AT 219(1), AT 273(7), AT 288(1), 13/83/5 OTSB(35), 9/84/9 OTSB(18), 3/85/29 OTSB(3). [1690-1 740m to 2190m] DISTRIBUTION. These are the first records from the Rockall Trough, the single sample recorded in Part 2 having been taken in the Porcupine Seabight. They are all from the area between the lower Hebridean Slope and the Anton Dohrn Seamount and fall within the known bathymetric range. Mesothuria lactea (Theel, 1886) SAMPLES. AT 254(2), ES 255(7), 13/83/5 OTSB(l), 9/84/9 OTSB(13), 3/85/29 OTSB(86). [1595m to 1775-1 835m] 1 84 HARVEY, GAGE, BILLETT, CLARK & PATERSON DISTRIBUTION. These records from the North Feni Ridge and Hebridean Slope confirm the bathymetric distribution reported by Herouard (1923) for the NE. Atlantic. The Rockall records suggest a ribbon-like distribution along the margins of the Trough. Mesothuria intestinalis (Ascanius & Rathke, 1 767) See: Mortensen, 1927: 381, figs 225, 228: 3; Heding, 1942: 7, text-fig. 6. SAMPLES. AT 292(1), 3/85/38 OTSB(l). [41 0-490 m to 525 m] DISTRIBUTION. Widely distributed in the NE. Atlantic from off NW. Africa (Herouard, 1 923) to the coasts of Norway, although nowhere in the deep sea does it appear to be particularly common. A few specimens are known from the Mediterranean (see Perrier, 1902; Koehler, 1927; Sibuet, 1974) and the western Atlantic (Deichmann, 1930). The species has a wide bathymetric range c. 18-1445 m, but reports of this species occurring as deep as 2000 m , appear to be the result of confusion with Mesothuria verrilli. The shallowest records come only from cold waters off Norway. The present records are from the upper Hebridean Slope. Mesothuria verrilli (Theel, 1886) See: Mortensen, 1927: 381, 382, fig. 224: 4-5; Deichmann, 1930: 93-94, pi. 6, figs 1-8. SAMPLES. AT 287(2), 3/85/30 OTSB(l). [1383 m to 1420-1480 m] DISTRIBUTION. Widely distributed in the north Atlantic with some records from the Mediterranean. In the western Atlantic it is known from the Caribbean Sea, eastern Gulf of Mexico (Deichmann, 1954; Miller & Pawson, 1984) and off the Bahamas (Pawson, 1982). In the eastern Atlantic it is previously known from NW. Africa, the Canary Islands (Perrier, 1902), the Azores (Herouard, 1902, 1923; Perrier, 1902), the Bay of Biscay (Sibuet, 1977) and as far north as the Porcupine Seabight, southwest of Ireland (Mortensen, 1927). The present records extend the distribution northwards into the Rockall Trough on the Hebridean Slope. The bathymetric range is not known with certainty partly as a result of confusion with M. intestinalis. Hansen (1975) gives a wide bathymetric range of 6 18^1 65m for M. verrilli in the Atlantic and 280 to 1 103 m in the Mediterranean. With the aid of detailed bathymetric charts available today it is possible to see that all reliable records of this species deeper than 2000 m come from areas where the seabed is particularly steep e.g. on the continental slope off NW. Africa or in the area of the King's Trough (see Perrier (1902) for details of some stations). The accuracy of the depths from which some samples were taken must therefore be called into question. This also applies to a shallow sample of M. verrilli on the Magazan escarpment in 550m (Perrier, 1902). Mortensen (1927) gives a reduced range of c. 990-1765 m for M. verrilli sampled to the southwest of Ireland. Recent intensive sampling in the same area, the Porcupine Seabight, confirms this total range but indicates that M. verrilli is only common in a reduced range between 1250 and 1500 m (Billett, in preparation). The present samples from the Hebridean Slope fall within this narrower range, as do most of those taken off the Azores (Marenzeller, 1893; Herouard, 1902, 1923; Perrier, 1902). The samples from the eastern Atlantic fall within the total range proposed for M. verrilli in the western Atlantic of 699-3720 m (Deichmann, 1954; Miller & Pawson, 1984; Pawson, 1982; Suchanek et al., 1985). The study of Suchanek et al. (1985) increased the lower bathymetric limit from 2141 to 3720 m. The shallowest record, from 618m, quoted by Hansen (1975) for material from the Atlantic should be referred to specimens collected within the Mediterranean. REMARKS. In the western Atlantic M. verrilli is known to cover itself with detrital seagrass and shell material such as the seagrass Thalassia and brachiopod shells (Suchanek et at., 1985). Family STICHOPODIDAE Stichopus tremulus (Gunnerus, 1 767) SAMPLES. AT 292(4), 13/83/3 GT(14), 13/83/4 GT(29), 13/83/7 OTSB(l), 13/83/8 OTSB(91), 3/85/9 OTSB ROCKALL TROUGH ECHINODERMS 3 185 (juvenile 1), 3/85/14 OTSB(6), 3/85/18 OTSB(l), 3/85/38 OTSB(2), 3/85/43 OTSB(18), 3/85/44 OTSB(4). [168m to 990- 1020m] DISTRIBUTION. The new records from the Hebridean Slope extend the lower bathymetric limit within the Trough by some 300 m. Order ELASIPODIDA Family LAETMOGONIDAE Laetmogone violacea Theel, 1879 SAMPLES. AT 239(11), AT 248(9), AT 249(5), ES 250(1), AT 259(37), GT 8(6), 13/83/2 OTSB(5), 13/83/6 OTSB(157), 13/83/7 OTSB(9), 9/84/13 OTSB(54), 3/85/18 MBA(4), 3/85/19 MBA(7), 3/85/20 OTSB(112), 3/85/22 MBA(7), 3/85/23 OTSB(18), 3/85/24 OTSB(35), 3/85/25 OTSB(99), 3/85/28 OTSB(3), 3/85/33 OTSB(126). [940-975 m to 1400(3000) m] DISTRIBUTION. The new records from the North Feni Ridge and Hebridean Slope indicate the presence of large populations of this species in suitable localities. REPRODUCTION. A non-seasonal cycle with abbreviated development is indicated (Tyler et al., 1985/j). Benthogone rosea Koehler, 1 896 SAMPLES. AT 271(10), 1 3/83/5 OTSB(3). [1745-2255 m] DISTRIBUTION. No change. REPRODUCTION. Direct development is indicated by the large oocyte size and there is no evidence of seasonality in oogenesis (Tyler et al., 19856). Family PSYCHROPOTIDAE Psychropotes longicauda Theel, 1 882 SAMPLE. SWT 15(3) (incorrectly listed in Part 2 as SWT 5(3)). [2910-4810 m] REMARKS. P. longicauda has the largest known egg size for a holothurian at 4-4 mm diameter (Hansen, 1975). This size of egg probably leads to a prolonged form of early development within the deep-sea plankton, and juveniles of this species 13-23 mm in length have been recovered in pelagic nets fished at between 17 and 1500m above the seabed at abyssal depths (Billett et al., 1985). Family ELPIDIIDAE Peniagone azorica von Marenzeller, 1893 SAMPLES. AT 121(79), AT 271(23). [1991-3463 m] DISTRIBUTION. No change. REPRODUCTION. Additional information to that given for this species in Part 2 is provided by Tyler etal. (1985a). Kolga hyalina Danielssen & Koren, 1879 SAMPLES. ES 266(61). [2591-2910m] DISTRIBUTION. These records extend the geographic range within the Rockall Trough of this patchily distributed species to the north central part of the Trough and Feni Ridge. Ellipinion delagei (Herouard, 1 896) See: Herouard, 1902: 39^0, pi. 6 figs 1-3, pi. 8 figs 8-9; Hansen, 1975: 163, fig. 122. SAMPLE. AT 247(18). [2084 m] 186 HARVEY, GAGE, BILLETT, CLARK & PATERSON DISTRIBUTION. An extremely rare species found previously only around the Azores and Cape Verde Islands close to steep slopes (Herouard, 1902, 1923). The presence of specimens on the Rosemary Bank indicates a preference for steep topography by this species, particularly around seamounts and oceanic islands in the N. Atlantic. The total bathymetric range is 1 165-2478 m. REMARKS. Only one specimen is in good condition. It widens towards the posterior end and has 12 pairs of tubefeet bordering the entire ventral surface. Those tubefeet at the anterior end are spaced more widely than those at the posterior end. The posterior few pairs of tubefeet are slightly smaller than the rest. The deposits include large rods (up to 550 \im long), regular c-shaped deposits (about 1 30 urn long) and small irregularly curved rods (40-50 urn in size) which are usually c-shaped and are often developed into tripartite deposits (Herouard, 1902). Order APODIDA Family SYNAPTIDAE Labidoplax southwardorum Gage, 1985 SAMPLES. ES 1 0( 1 ), ES 34(?2), ES 53( 1 ), SBC 66(?3), ES 1 29(8, ?3), ES 1 37(3), ES 1 72(6), ES 1 76( 1 0 [not 22 as stated in Part 2]), ES 185(21), ES 190(7), ES 197(720), ES 200(1), ES 204(1), ES 218(16), SBC 220(2), ES 244(10), ES 283(37), ES 285(1), ES 289(6). [1000-2946 m] DISTRIBUTION. The new records provide a slight extension of the lower bathymetric limit. B Fig. 3 (A) Labidoplax similimedia from SBC 222: entire, uncontracted specimen showing pinnate tentacles and position of plates and anchors in body wall; (B) Prototrochus zenkevitchi rockallensis from SBC 220: entire specimen showing sac-like body distended with sediment. Scale bar = 1 mm. ROCKALL TROUGH ECHINODERMS 3 1 87 Labidoplax similimedia Gage, 1985 SAMPLES. ES 118(1), ES 129(2), ES 137(4), ES 143(71), ES 164(87), ES 169(4), ES 185(4), ES 218(72), SBC 222(8), ES 244(1), ES 283(6), ES 285(1), ES 289(2). [1 101-2946 m] DISTRIBUTION. The new records provide an upward extension of the bathymetric range by c. 1 100 m, and also an extension of the lower bathymetric limit. REMARKS. Several of the specimens from SBC 222 are complete (Fig. 3A), with the skin deposits scattered in the body wall rather than crowded together and overlapping as described by Gage (1985), and as found in the other material from epibenthic sled hauls. This is no doubt because the specimen is not severely contracted as material usually is when collected by the epibenthic sledge. The plates and anchors have a lateral orientation in the body wall (Fig. 3 A) similar to that of other synaptids. The tentacles are clearly pinnate with two pairs of rounded lateral, and a single terminal, digit (Fig. 3A). Leptosynapta decaria (Ostergren, 1905) See: Ostergren, 1905: 146-148, fig. IB; Clark, 1907: 93; Mortensen, 1927: 431, fig. 262, 3. SAMPLE. SBC 210(1 + frag.). [401 m] DISTRIBUTION. Hitherto known only from the Trondheim Fjord to the Kattegat, 40-70 m depth. REMARKS. The material consists of an anterior end with the oral ring measuring 1.41 mm in diameter along with a posterior end, quite possibly from the same specimen, around 0.6 mm wide. Both fragments were whitish in colour with no trace of pigmentation when examined from spirit. There are 10 tentacles, each with a short terminal digit and three pairs of short rounded digits, increasing in size distally. Deposits consist of plates and anchors, which are found in the skin of both fragments, and rods present only in the tentacles. The rods, which are slightly curved and possess enlarged, branched ends (Fig. 4), are numerous and present throughout the tentacles, increasing in size distally. Skin deposits (Fig. 4) consist of plates typical in form of Leptosynapta, with nine toothed holes, the outermost and central holes being the largest. In the anterior fragment the plates have a mean length of 124-8 urn, range 1 16-138 (« = 28) and mean width of 99-1 um, range 90-1 1 3 (n = 14). This agrees well with the values of 126-5 and 97-5 um, respectively, given by Ostergren (1905) for the deposits from the anterior of the animal. The anchors agree well with Ostergren's description; resembling those of Leptosynapta inhaerens but being smaller and possess- ing up to 5 (usually 3) teeth on each fluke. Anchors are slightly longer but narrower than the plates, mean length 144 um, range 127-160 um (« = 23), mean width 73-1 um, range 70-75 (« = 8). These values are also reasonably close to the values given by Ostergren (149 x 97 um). Besides the fully developed plates and anchors there are a number of developmental stages of both deposits present (Fig. 4). The deposits in the posterior end are similar to those in the anterior fragment, but slightly larger (plates, mean length 130 um, mean width 98 um; anchors, mean length 143, mean width 72 um n = 4). Assuming that the two fragments belong to the same animal, it is pertinent to note that in Leptosynapta, it is usual for the deposits to increase in size posteriorly (Ostergren, 1905; Cherbonnier, 1953, 1963). Both the whitish colour and diameter of the head-end fragment ( 1 -4 mm) is similar to that ( 1 -5-3 mm) described by Ostergren for L. decaria, and the three pairs of tentacle digits present is within the range of 2-4 pairs on each tentacle described by Ostergren (1905). Only two European species of Leptosynapta are known to possess 10 rather than the 12 tentacles typical of other species of the genus; L. minuta (Becher), a tiny viviparous species known from shallow water off NW Europe, and L. decaria. Both species are small and appear to lack pigmen- tation. The present specimen differs from L. minuta in possessing tentacle digits, in having anchors clearly longer than the plates (Fig. 4), and in having at the basal (articular) end of the plate small irregularly arranged holes, typical of most Leptosynapta species, rather than the regular slit-like holes of L. minuta. Ostergren (1905) found specimens of L. inhaerens with 10, 1 1 or 13 tentacles, this possibly influencing Clark (1907) to suggest that '. . . it is not impossible that this [L. decaria} is 188 HARVEY, GAGE, BILLETT, CLARK & PATERSON Fig. 4 Skin deposits from anterior fragment of Leptosynapta decaria from SBC 210. Fully developed (middle and lower right) and developing plates (upper left); fully developed (lower left) and developing (centre) anchor; rods from tentacles, lower left. Scale bar = 50 um. only the young of inhaerens. There is a striking similarity in the calcareous particles and in the tentacles, the differences in number of digits being simply a matter of age.' Dr Bent Hansen of the Zoological Museum, University of Copenhagen has confirmed (unpublished communication to J.D.G) that there appears to be no published record of L. decaria subsequent to Ostergren's (1905) paper. Dr Hansen very kindly re-examined Norwegian material from Tromso and Oslo, including ROCKALL TROUGH ECHINODERMS 3 189 A C u50 o> D CT O) CU Q_ 100 '2 Oocyte diameter pm 0 100 200 300 Oocyte diameter jum 400 Fig. 5 (A) Ovary dissected from a female Myriotrochus bathybius from ES 207 with a calcareous ring diameter of 4-5 mm; (B) oocyte diameter frequencies from this specimen (lower) and from a smaller M. bathybius from ES 207 (upper); (C) oocyte diameter frequencies from a female of Myriotrochus giganteus from ES 207. 1 90 HARVEY, GAGE, BILLETT, CLARK & PATERSON specimens examined by Ostergren, held in the Zoological Museum and also informs us that he considers that L. decaria is a valid species. He has also drawn our attention to a single record of L. decaria from 1 fathom depth in Port Erin Harbour in the Isle of Man dated 1933 that he was also able to re-examine and confirm as conforming to Ostergren's description of L. decaria. With the present record from 401 m depth we conclude that Leptosynapta decaria exists as a distinct species with a rather wide bathymetric distribution in muddy sediments of the continental shelf and adjacent upper slope of the more northerly areas of Europe. It is a small form that may well have been overlooked or lost when sieving benthic samples. Protankyra brychia (Verrill, 1885) SAMPLE. ES 1 18(1). [2871-2925 m] DISTRIBUTION. No change. Family MYRIOTROCHIDAE Myriotrochus bathybius H. L. Clark, 1920 See: Gage & Billett, 1986: 234-239, figs 1, 3-6, 7A, B, 9A, B, 18B. SAMPLES. ES 152(2), ES 185(3), ES 231(6), AT 267(1), AT 282(3), ES 283(2), ES 289(1). [1800-2946 m] DISTRIBUTION. The combined bathymetric data for samples of M. bathybius taken in the Rockall Trough and on the Porcupine Abyssal Plain gives a total bathymetric range of 1800 to 4310m (Gage & Billett, 1986). REPRODUCTION. The reference in Part 2 to Gage & Billett (in press) for details of the reproduction of this species was incorrect, and further information is therefore provided here. One of the pair of branched ovaries is shown in Fig. 5A from an incomplete female specimen with a calcareous ring diameter of 4- 5 mm. It contained previtellogenic oocytes measuring up to 160 urn in longest diameter (Fig. 5B). In a smaller specimen from the same sample (ES 207) the maximum oocyte size did not exceed 60 um (Fig. 5B). Myriotrochus giganteus H. L. Clark, 1920 See: Gage & Billett, 1986: 239-247, figs 1, 7C, 8, 9C, 10-12, 24B. SAMPLES. ES 169(1), ES 231(1), ES 283(1). [2898-2946 m] DISTRIBUTION. The new records provide a slight extension of the lower bathymetric limit within the Trough. The total known bathymetric range is 2898 to 3800 m. REPRODUCTION. The maximum dimension of the irregularly shaped, vitellogenic oocytes of the specimen from ES 207 referred to by Gage et al. (19850) is 320 um and not 211 x 169 um as given. However, the overall size distribution of the oocytes was, like those for M. bathybius, markedly skewed to the left, with the size frequencies peaking in the intervals between 20-60 um (Fig. 5C). Myriotrochus clarki Gage & Billett, 1986 See: Gage & Billett, 1986: 247-252, figs 1, 7D, 9D, 13-17, 18 A; also Gage et al. 1985a: 203 (as Myriotrochus sp.) SAMPLES. ES 90(1), ES 185(1), ES 218(1), SBC 222(71), ES 231(2, ?1), ES 232(1), ES 255(1). [c. 1040-2907 m] DISTRIBUTION. These new records increase the previously known bathymetric range of 1605- 2515m given in part 2. Prototrochus zenkevitchi rockallensis Gage & Billett, 1986 See: Gage & Billett, 1986: 252-259, figs 1,7E, F, 18C-E, 19-23,24A;Gagee/a/., \985a:2Q4(asP.zenkevitchi subsp.) ROCKALL TROUGH ECHINODERMS 3 191 SAMPLES. ES 56(1), ES 1 18(3), ES 129(7), ES 135(15), ES 147(2), SBC 156(2), SBC 159(1), SBC 160(1), SBC 163(1), SBC 168(3), ES 176(23), ES 184(1), ES 185(3), ES 197(36), ES 204(3), SBC 215(71), SBC 216(2), ES 218(8), SBC 220(3), SBC 222(2), ES 231(1), ES 232(3), SBC 275(1), SBC 276(1), ES 283(15), ES 285(2), ES 289(5). [c. 1 000-2946 m] DISTRIBUTION. The new records provide a slight increase in the lower bathymetric limit. Other subspecies of P. zenkevitchi, however, occur much deeper at between 7400 and 9735 m. A bathy- metric range of 1000-9735 m is unprecedented in deep-sea holothurians. Gage & Billett (1986) suggest that the wide geographic and bathymetric separation of such records of myriotrochid species results from the problems of sampling infauna in the deep sea. Possibly, characterisation of separate species will be possible given more material. REMARKS. Developing wheels, still lacking the rim, and with developing, spike-like spokes, have been found amongst the fully developed wheels on a specimen from SBC 220. The largest of the specimens from SBC 220 is complete, the sac-like body, length 2-36 mm, being distended with sediment (Fig. 3B); some of these being calcareous particles that are quite large compared to the size of the animal. REPRODUCTION. Gonads have not been found in any of the specimens examined by us, perhaps indicating that they are immature. Parvotrochm belyaevi Gage & Billett, 1986 See: Gage & Billett, 1986: 262-266, figs 1, 24C-F, 26, 27; Gage et al., 1985a: 204 (as Myriotrochidae gen. et sp.) SAMPLES. ES 99(2), ES 147(2), ES 152(3), ES 172(3), ES 204(2), SBC 220(1), ES 285(4). [1 160-2921 m] DISTRIBUTION. These new records are mainly from the type locality at c. 2900m depth in the southern Rockall Trough. The record from ES 99 in 1 160 m extends the known bathymetric range upwards by more than 500 m. Order MOLPADIIDA Family MOLPADIIDAE Cherbonniera utriculm Sibuet, 1974 SAMPLES. ES 27(242), ES 56(218), ES 111(183), ES 118(74), ES 129(151), SBC 174(1), ES 185(544), ES 190(161), ES 204(144), ES 23 1(667), £8283(1180), ES 285(1 16). [25 15-2946 m] DISTRIBUTION. The records from ES 283 provide a slight extension of the lower bathymetric range within the Trough. The total bathymetric range is 2039-4251 m. REPRODUCTION. The oocytes grow to a maximum diameter of 200 um, and Tyler et al. (1987) suggest that development may be planktotrophic. Too few specimens were examined to determine any possible periodicity in reproduction. Molpadia blakei (Theel, 1886) SAMPLES. ES 283(1), AT 288(2), 3/85/5 OTSB(l). [1991 m to 2970—2980 m] DISTRIBUTION. These records extend the lower bathymetric limit slightly within the Trough and also provide a slight extension northwards. Molpadia borealis M. Sars, 1858 SAMPLE. AT 107A(1 [No. of specimens omitted in Part 2]). [c. 2000m] Family CAUDINIDAE Hedingia albicans (Theel, 1886) See: Heding, 1935: 65-67, figs 18, 19, pi. 4, fig. 9, pi. 5, fig. 17, pi. 8, fig. 10 (as Haplodactyla albicans). SAMPLES. ES 252(1), ES 255(2), AT 256(1). [1510-1706 m] 1 92 HARVEY, GAGE, BILLETT, CLARK & PATERSON DISTRIBUTION. Eastern and western Atlantic from offNW. Africa (3200 m), southwest of Iceland ( 1 590- 1 628 m) and the eastern seaboard of N. America (1600-2423 m). Also known in the Mediterranean, off southern India and in the Bay of Bengal (484-8 14m). A variety, var. glabra Theel, 1886a is known from off New Zealand (1280 m). The present material increases the upper bathymetric limit in the Atlantic to 1510m, with the total worldwide range 494-3200 m. REMARKS. Only a few specimens are known from each of these widely separated localities. This may be the result of inefficient sampling of large infaunal animals by trawls and epibenthic sledges. The specimen from AT 256 measures c. 27 mm in length. Specimens measuring up to 45 mm in length were found by Heding ( 1 935) to have undeveloped gonads and were hence probably juveniles. The deposits in the body wall of our 27 mm specimen lacked both the trilobed appearance and the thorny spines on the column of some of those figured by Heding (1935, fig. XVIII), possibly because of the relatively small size of the present specimen. It is possible however, that distinct sub-species may be recognisable when more material becomes available. Discussion Gage et al. (1983, 19850) found a higher species richness amongst the relatively small number of samples taken on the western side of the Trough, despite the much higher sampling effort on the eastern side. This was thought to be related to stronger currents in the west (Jones et al., 1 970; Ellett & Roberts, 1973; Roberts, 1975; Lonsdale & Hollister, 1979) favouring microphagous suspension feeders. Many of the species found only in the west, particularly ophiuroids and asteroids, were inferred to feed on current-borne particles. In general these distributions have been confirmed by subsequent sampling but the following species have now been found to have a wider distribution: Hoplaster spinosus, Psilaster andromeda, Ophiacantha crassidens and Amphiophiura saurura. Bathymetric zonation for the most abundant echinoderm species in the samples covered by Parts 1 & 2 is summarised by Gage et al. 19856. These authors also employed the coincidence-of-range statistic of Backus et al. ( 1 965) to describe the rate of change in the joint bathymetric ranges of these species at 100-m depth intervals along a notional transect encompassing most of the sampling effort in the east of the Trough. Peaks in the value of this statistic occur at around 800-1200 and 1800 m depth and were thought to be related to discontinuities in hydrodynamic and water-mass properties. Despite the frequent sampling in the Rockall Trough since 1973, the echinoderm fauna is still imperfectly known, particularly on the southern Feni Ridge on the west side of the Trough from which only one sample has been taken. Interestingly, seven of the taxa recorded in this series of papers were only found at this station. From a total of 164 echinoderm taxa listed in Parts 1-3, 66 are recorded from less than 10 specimens and 22 of these are from single specimens. Some of these 'rarities' can be explained by the wide depth and geographic distribution of our samples, coupled with a low sampling effort at most stations. It is clear, however, from the more heavily sampled stations where the bottom is thought to be relatively homogeneous, that there are a number of relatively rare species which are widely distributed in the Atlantic z.g.Hymenaster gennaeus. The additional species recovered on the Hebridean Slope in 1985 with the semi-balloon otter trawl may reflect the greater catching power of this gear, with an estimated swept path width of 8-5 m compared with either the Agassiz Trawl (3 m) or the epibenthic sledge (1 m). Given the high diversity in the echinoderm fauna from the Feni Ridge revealed by the relatively low sampling effort so far, it is clear that further sampling is necessary. The clearer picture of echinoderm distribution resulting from this would help in evaluating the relative importance of sedimentary and hydrographic features in bringing about the contrasts in the echinoderm faunas of the eastern and western margins of the Trough. Until this can be accomplished, the echinoderm fauna, and its zonation on the relatively well sampled and comparatively gently sloping Hebridean Slope, should not be viewed as being typical of the margins of the Trough as a whole. Summary Five species of crinoids, eleven asteroids, eight ophiuroids, two echinoids and eight species of ROCKALL TROUGH ECHINODERMS 3 193 holothurian are identified, mainly from sampling carried out between 1983 and 1985 in the deep water areas to the west of the British Isles. The following echinoderm species have not been recorded previously from this area of the NE. Atlantic. Cheiraster sepitus Mediaster bairdi Pter aster (Apterodon) sp. Hymenaster regalis Ellipinion delagei Leptosynapta decaria Of these, Mediaster bairdi and Hymenaster regalis are new records for the eastern Atlantic, while the Pteraster (Apterodon) sp. is probably new to science. This study confirms the generally higher species richness along the western margin of the Trough noted in earlier papers in this series and the tendency for juveniles of many species to be distributed at the lower end of the bathymetric range of those species. Extensions to the bathymetric and geographic ranges of several species are provided by these records. Acknowledgements We again express our gratitude to the officers and crew of RRS Challenger, and to colleagues too numerous to name individually who participated in cruises and helped with the processing of samples. We are particularly indebted to Miss B. Rae of Dervaig, Isle of Mull, for her help in sorting sled and box-core samples; to Mr G. Davies and Mr A MacArthur for the sorting of other samples as summer students in the years 1983-85, and to Mrs Margaret Pearson for her valuable help in sorting and careful curation of the collections up to 1 983. Dr J. D. M. Gordon of SMBA kindly provided additional material from fishing cruises in which the authors did not participate. We also thank Dr J. M. Graham of SMBA for constructing a digitising caliper used to measure echinoids. The Scottish Marine Biological Association is grant-aided by the Natural Environment Research Council who have been generous in allocating cruise time on which the present records were made. Station List Only details of stations yielding records of echinoderms not listed by Gage et al. (1983, 19850) are given below. Station No. Date Position (at mid-point of track on bottom if applicable) Depth (m) Benthic stations SBC 156 SBC 159 SBC 160 SBC 168 ES231 ES232 AT 233 RMT 234 AT 239 ES244 AT 245 AT 247 AT 248 AT 249 ES250 5 Aug. 1979 8 Aug. 1979 8 Aug. 1979 13 Aug. 1979 17 May 1983 19 May 1983 19 May 1983 20 May 1983 24 July 1983 25 July 1983 26 July 1983 27 July 1983 27 July 1983 28 July 1983 28 July 1983 48°27'N, 10°21'W 1310 50°55'N, 12°21'W 2036 50°55'N, 12°20'W 2030 56°44'N,09°13'W 1206 54°42'N, 12°12'W 2898 57°17'N, 10°16'W 2195 57°17'N, 10°12'W 2180 57°12'N,09°54'W c. 2000 57°07'N, 09°23'W 1047 57°23'N, 10°20'W 2150 57°21'N, 10°21'W 2165 59°02'N, 10°55'W 2084 59°59'N, 10°33'W 1150 59°44'N, 12°36'W 1265 59°43'N, 12°33'W 1270 194 HARVEY, GAGE, BILLETT, CLARK & PATERSON Station No. Date Position (at mid-point of track on bottom if applicable) Depth (m) AT 251 30 July 1983 58°52'N, 12°56'W 1530 ES252 30 July 1983 58°52'N, 12°53'W 1510 AT 254 31 July 1983 58°26'N, 12°35'W 1595 ES255 31 July 1983 58°26'N, 12°42'W 1595 AT 256 31 July 1983 57°56'N, 12°21'W 1705 ES257 31 July 1983 57°55'N, 12°18'W 1700 RD258 1 Aug. 1983 57°56'N, 13°24'W 135 AT 259 1 Aug. 1983 57°27'N, 12°52'W 1041 ES261 lAug. 1983 57°24'N, 12°05'W 1824 ES264 2 Aug. 1983 56°26'N, 13°31'W 2144 ES266 3 Aug. 1983 56°24'N, 1 1°59'W 2591 AT 267 3 Aug. 1983 56°24'N, 1 1°58'W 2605 AT 271 4 Aug. 1983 56°39'N, 10°35'W 2255 SBC 272 5 Aug. 1983 56°40'N, 10°30'W 2250 AT 273 5 Aug. 1983 56°05'N, 10°28'W 2185 SBC 275 6 Aug. 1983 56°13'N, 10°06'W 1961 SBC 276 6 Aug. 1983 56°14'N,09°51'W 1792 SBC 278 6 Aug. 1983 56°15'N,09°46'W 1631 AT 282 14 April 1985 55°06'N, 11°22'W c. 2760 ES283 15 April 1985 54°39'N, 12°15'W 2946 AT 284 15 April 1985 54°40'N, 12°12'W 2906 ES285 15 April 1985 54°39'N, 12°14'W 2906 AT 286 16 April 1985 54°44'N, 12°17'W 2896 AT 287 18 April 1985 56°43'N,09°21'W 1383 AT 288 20 April 1985 57°18'N, 10°22'W 2190 ES289 21 April 1985 57°19'N, 10°25'W 2190 AT 290 26 April 1985 56°28'N,09°16'W 970 AT 291 27 April 1985 56°22'N,09°12'W 775 AT 292 27 April 1985 56°23'N, 09°08'W 525 Fishing stations Starting position Depth range 13/83/1OTSB 20 Sept. 1983 56°33'N, 09°40'W 1540-1550 1 3/83/2 OTSB 21 Sept. 1983 56°46'N,09°15'W 1130-1265 1 3/83/3 GT 21 Sept. 1983 56°36'N, 09°02'W 220-270 1 3/83/4 GT 21 Sept. 1983 56°32'N, 09°05'W 230-380 13/83/5 OTSB 21 Sept. 1983 56°41'N,09°47'W 1775-1835 13/83/6 OTSB 22 Sept. 1983 56°36'N,09°17'W 980-1005 13/83/7 OTSB 22 Sept. 1983 56°27'N,09°10'W 750-800 13/83/8 OTSB 22 Sept. 1983 56°20'N, 09°08'W 500-560 9/84/1 OTSB 2 Nov. 1984 56°32'N,09°13'W 760-815 9/84/2 OTSB 2 Nov. 1984 56°34'N,09°16'W 910-960 9/84/9 OTSB 4 Nov. 1984 56°47'N, 09°36'W 1750-1770 9/84/10 OTSB 4 Nov. 1984 56°16'N,09°13'W 580-630 9/84/1 3 OTSB 5 Nov. 1984 56°25'N,09°16'W 940-975 3/85/5 OTSB 15 April 1985 54°27'N, 12°25'W 2970-2980 3/85/7 OTSB 16 April 1985 55°47'N, 10°52'W 2500-2455 3/85/8 OTSB 17 April 1985 56°27'N,09°17'W 970-1010 3/85/9 OTSB 17 April 1985 56°43'N,09°11'W 945-1010 3/85/10 OTSB 17 April 1985 56°31'N,09°13'W 795-805 3/85/11 OTSB 18 April 1985 56°33'N, 09°26'W 1250-1270 3/85/13 OTSB 18 April 1985 56°28'N,09°17'W 960-995 ROCKALL TROUGH ECHINODERMS 3 195 Station No. Date Position (at mid-point of track on bottom if applicable) Depth (m) 3/85/14 OTSB 18 April 1985 56°30'N,09°12'W 720-775 3/85/17 OTSB 21 April 1985 56°54'N, 10°00'W 1955-1995 3/85/18 MBA 21 April 1985 56°27'N,09°17'W 990-1020 3/85/19 MBA 22 April 1985 56°34'N,09°18'W 1030-1035 3/85/20 OTSB 22 April 1985 56°34'N, 09°26'W 1225-1245 3/85/21 OTSB 22 April 1985 56°31'N,09°39'W 1480-1500 3/85/22 MBA 22 April 1985 56°25'N,09°17'W 995-1020 3/85/23 OTSB 23 April 1985 56°25'N,09°18'W 995-1000 3/85/24 OTSB 23 April 1985 56°26'N,09°17'W 980-990 3/85/25 OTSB 23 April 1985 56°25'N,09°18'W 1000-1005 3/85/26 OTSB 23 April 1985 56°25'N,09°16'W 940-985 3/85/27 OTSB 24 April 1985 56°24'N,09018'W 990-1000 3/85/28 OTSB 24 April 1985 56°35'N,09°18'W 990-1075 3/85/29 OTSB 24 April 1985 56°50'N,09°31'W 1690-1740 3/85/30 OTSB 24 April 1985 56°29'N, 09°38'W 1420-1480 3/85/31 OTSB 25 April 1985 56°24'N,09°17'W 995-1020 3/85/32 OTSB 25 April 1985 56°25'N,09°19'W 1055-1060 3/85/33 OTSB 25 April 1985 56°26'N,09°18'W 985-1000 3/85/34 OTSB 25 April 1985 56°24'N,09°18'W 980-990 3/85/36 OTSB 26 April 1985 56°24'N,09°19'W 1000-1025 3/85/37 OTSB 26 April 1985 56°25'N,09018'W 945-985 3/85/38 OTSB 26 April 1985 56°23'N, 09°08'W 410-490 3/85/43 OTSB 27 April 1985 56°17'N,09°12'W 565-700 3/85/44 OTSB 27 April 1985 56°18'N,09°11'W 545-600 3/85/45 OTSB 28 April 1985 56°30'N, 09°38'W 1470-1500 3/85/46 OTSB 28 April 1985 56°25'N,09°17'W 960-985 References Backus, R. H., Mead, G. L., Haedrich, R. L. & Ebeling, A. W. 1965. The mesopelagic fishes collected during cruise 1 7 of the R/V Chain, with a method for analysing faunal transects. Bulletin of the Museum of Comparative Zoology Harvard 134: 139-158. Billett, D. S. M., Hansen, B. & Huggett, Q. J. 1985. Pelagic Holothurioidea (Echinodermata) from the northeast Atlantic, pp. 399^1 1 1 In Keegan, B. F. & O'Connor, B. D. S. [Eds] Echinodermata. Proceedings of the 5th International Echinoderm Conference, Galway, 1984 Balkema, Rotterdam. Blake, D. B. 1987. A classification and phylogeny of post-Palaeozoic sea stars (Asteroidea: Echinodermata). Journal of Natural History 21: 48 1-528. Brattstrom, H. 1946. Obervations on Brissopsis lyrifera (Forbes) in the Gullmar Fjord. Arkivfor Zoologi 37a (18): 1-27. Cherbonnier, G. 1953. Recherches sur les synaptes (holothuries apodes) de Roscoff. Archives de Zoologie experimentale et generate 90: 163-1 86. 1963. 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Bulletin of the British Museum (Natural History) Zoology 38: 187-210. - 1981. Notes on Atlantic and other Asteroidea. 1. Family Benthopectinidae. Bulletin of the British Museum (Natural History) Zoology 41(3): 91-135. 1984. Notes on Atlantic and other Asteroidea. 4. Families Poraniidae and Asteropseidae. Bulletin of the British Museum (Natural History) Zoology 47(1): 19-51. Clark, H. L. 1907. The apodous holothurians. Smithsonian Contributions to Knowledge 35, No. 1732, 231 pp. Clark, H. L. 1941. Reports on the scientific results of the Atlantis expeditions to the West Indies, under the joint auspices of the University of Havana and Harvard University. The Echinoderms (other than Holothurians). Memoiras de la Sociedad Cubana de Historia Natural Felipe Poey 15( 1 ): 1 54 pp. Dartnall, A. J., Pawson, D. L., Pope, E. C. & Smith, D. J. 1 969. Replacement name for the preoccupied genus name Odinia Perrier, 1 885 (Echinodermata: Asteroidea). Proceedings of the Linnaean Society NSW 93: 2 1 1 . Deacon, M. 1977. Staff-Commander Tizard's journal and the voyages of H.M. Ships Knight Errant and Triton to the Wyville Thomson Ridge in 1880 and 1882. pp. 1-14. In Angel, M. [Ed.] A Voyage of Discovery. Pergamon, Oxford. Deichmann, E. 1930. The holothurians of the western part of the Atlantic Ocean. Bulletin of the Museum of Comparative Zoology Harvard 71(3): 43-226. 1940. Report on the holothurians, collected by the Harvard-Havana Expeditions 1938 and 1939, with a revision of the Molpadonia of the Atlantic Ocean. Memoiras de la Sociedad Cubana de Historia Natural 'Felipe Poey' 14: 183-240. 1954. The holothurians of the Gulf of Mexico. Fishery Bulletin of the United States Fish and Wildlife Service 55: 381-410. Doderlein, L. 1912. Die gesteilten Crinoiden der Deutschen Tiefsee-Expedition. Wissenschaftliche Ergebnisse derDeutschen Tiefsee— aufdem DampferValdivia 1898-1899, 17(1): 1-34. Downey, M. E. 1973. Starfishes from the Caribbean and the Gulf of Mexico. Smithsonian Contributions to Zoology 126: 1-158. 1986. Revision of the Atlantic Brisingida (Echinodermata: Asteroidea), with description of a new Genus and Family. Smithsonian Contributions to Zoology 435: 1-57. Duineveld, G. C. A. & Jenness, M. I. 1 984. Differences in growth rates of the sea urchin Echinocardium cordatum as estimated by the parameter of the von Bertalanffy equation applied to skeletal rings. Marine Ecology Progress Series, 19: 65-72. Einarsson, H. 1948. Echinoderma. The Zoology of Iceland 4(70): 1-67. Ellett, D. J. & Roberts, D. G. 1973. The overflow of Norwegian deep-sea water across the Wyville Thomson Ridge. Deep-Sea Research 20: 819-835. Farran, G. P. 1913. The deep-water Asteroidea, Ophiuroidea and Echinoidea of the west coast of Ireland. Scientific Investigations, 1912. Fisheries Branch, Department of Agriculture Ireland, Dublin 6: 1-66. Fell, F. J. 1982. Echinodermata. pp. 785-818 In Parker, S. P. [ed.] Synopsis and Classification of Living Organisms. McGraw-Hill, New York. Fisher, W. K. 1911. Asteroidea of the North Pacific and adjacent waters Part 1 . Phanerozonia and Spinulosa. Bulletin of the United States National Museum 76: 419 pp. Gage, J. D. (1987). Growth of the deep-sea irregular sea urchins Hemiaster expergitus and Echinosigra phiale in the Rockall Trough (N. E. Atlantic). Marine Biology 96: 19-30. & Billett, D. S. M. 1986. The family Myriotrochidae Theel (Echinodermata: Holothurioidea) in the deep northeast Atlantic Ocean. ZoologicalJournal of the Linnaean Society 88: 229-276. Jensen, M. & Tyler, P. A. 1985a. Echinoderms of the Rockall Trough and adjacent areas 2. Echinoidea and Holothurioidea. Bulletin of the British Museum (Natural History) Zoology 48(4): 1 73-2 13. — , Pearson, M., Billett, D. S. M., Clark, A. M., Jensen, M., Paterson, G. L. J. & Tyler, P. A. 19856. Echinoderm zonation in the Rockall Trough (NE Atlantic), pp. 31-36 In Keegan, B. F. & O'Connor, B. [eds] Echinodermata. Proceedings of the Fifth International Echinoderms Conference Galway, 1984. Balkema, Rotterdam. Clark, A M., Paterson, G. L. J. & Tyler, P. A. 1983. Echinoderms of the Rockall Trough 1. Crinoidea, Asteroidea and Ophiuroidea. Bulletin of the British Museum (Natural History) Zoology 45(5): 263-308. — & Tyler, P. A. 1985. Growth and recruitment of the deep-sea urchin Echinus affinis. Marine Biology 90: 41-53. & Nichols, D. ( 1 986). Reproduction and growth of Echinus acutus var. norvegicus and E. elegans on the continental slope off Scotland. Journal of experimental marine Biology and Ecology, 101: 61-83. Gordon, J. D. M. 1986. The fish populations of the Rockall Trough. Proceedings of the Royal Society of Edinburgh 88B: 191-204. ROCKALL TROUGH ECHINODERMS 3 1 97 Gray, I. E., Downey, M. E. & Cerame-Vivas, M. J. 1968. Sea stars of North Carolina. Fishery Bulletin of the United States Fish and Wildlife Service 67( 1 ): 1 27-1 63. Halpern, J. A. 1972. Pseudarchasterinae (Echinodermata: Asteroidea) of the Atlantic. Proceedings of the Biological Society of Washington #5(30): 359-384. Hansen, B. 1975. Systematics and biology of the deep-sea holothurians. Part 1 . Elasipoda. Galathea Report 13: 1-262. Harvey, R. & Gage, J. D. 1984. Observations on the reproduction and postlarval morphology of pourtalesiid sea urchins in the Rockall Trough area (N. E. Atlantic Ocean). Marine Biology 82: 181-190. Heding, S. G. 1935. Holothurioidea. Part 1. Apoda, Molpadioidea, Gephyrothurioidea. Danish Ingolf Expedition 4(9): 1-84. 1942. Holothurioidea. Part 2. Aspidochirota, Elasipoda, Dendrochirota. Danish Ingolf Expedition 4(13): 1 39. Herouard, E. 1902. Holothuries provenant des campagnes de la Princess Alice 1892-1897). Resultats des Campagnes Scientifique accomplies par le Prince Albert I Monaco 21: 1—61. 1923. Holothuries provenant des campagnes des yachts Princess Alice et Hirondelle II (1898-1915). Resultats des Campagnes Scientifiques accomplies par le Prince Albert I Monaco 66: 1-1 63. Jones, E. J. W., Ewing, M., Ewing, J. I. & Eittreim, S. 1970. Influences of Norwegian sea overflow water on sedimentation in the northern North Atlantic and Labrador Sea. Journal of Geophysical Research 7: 1655-1680. Koehler, R. 1927. Echinodermes des mers d 'Europe 2. 339 pp. Doin Paris. Lonsdale, P. & Hollister, C. D. 1979. A near bottom traverse of Rockall Trough: hydrographic and geologic inferences. Oceanologica Acta 2: 91-105. Madsen, F. J. 1941. On Thyone wahrbergi n. sp., a new holothurian from the Skagerrak with remarks on T. fusus (O. F. M.) and other related species. Goteborgs Kungl. Vetenskaps — och Vitterhets-Samhalles Handlingar F.6, Ser. B., 1(1), 1-31. 1942. Cucumaria hyndmani. The variation of its calcareous deposits. Videnskabelige Meddelelser fra Dansk Naturhistorisk Forening i Kjobenhavn 105: 395-406. Maranzeller, E. von 1893. Contribution a 1'etude des holothuries de 1'Atlantique Nord. Resultats des Campagnes Scientifiques accomplies par le Prince Albert I Monaco 6: 1-22. Miller, J. E. & Pawson, D. L. 1 984. Holothurians (Echinodermata: Holothuroidea). Memoirs of the Hourglass Cruises 7(1): 1-79. Mortensen, T. 1907. Echinoidea (Part 2). Danish Ingolf Expedition. 4(2): 1-200. 1927. Handbook of the Echinoderms of the British Isles. 471 pp. Oxford University Press, London. 1933. Ophiuroidea. Danish Ingolf Expedition 4(2): 1-121. 1943. A Monograph of the Echinoidea Vol. iii(3). Camarodonta. 2. Echinidae, Strongylocentrotidae, Paraseleniidae, Echinometridae. 446 pp. C.A. Reitzel, Copenhagen. 1951. A Monograph of the Echinoidea Vol. V(2). Spatangoida 2. Amphisternata. 2. Spatangidae, Loveniidae, Percosmidae, Schizasteridae, Brissidae. 593 pp. C. A. Reitzel, Copenhagen. Ostergren, H. 1905. Zur kenntnis der skandinavischen und arktischen Synaptiden. Archives de Zoologie Experimentale et Generate , Ser. 4, 3, Notes et revue, No. 17: 133-164. Panning, A. 1949. Versuch einer Neuordnung der familie Cucumariidae (Holothurioidea, Dendrochirota). Zoologische Jahrbucher Jena 78: 404-470. Paterson, G. L. J. 1985. The deep-sea Ophiuroidea of the North Atlantic Ocean. Bulletin of the British Museum (Natural History) Zoology 49(1): 1-162. Pawson, D. L. 1982. Deep-sea echinoderms in the Tongue of the Ocean, Bahama Islands: a survey, using the research submersible Alvin. Memoirs of the Australian Museum No. 16: 129-145. & Fell, H. B. 1965. A revised classification of the dendrochirote holothurians. Breviora No. 214: 1-7. Perrier, R. 1902. Holothuries. Expeditions Scientifiques du Travailleur et du Talisman 5: 273-554. Roberts, D. G. 1975. Marine geology of the Rockall Plateau and Trough. Philosophical Transactions of the Royal Society Series A 278: 447-509. Roux, M. 1 977. Les Bourguetcrinina du Golfe de Gascogne. Bulletin du Museum National d'Histoire Naturelle Paris y Serie. Zoologie No. 426. 296: 25-83. Sibuet, M. 1974. Echinodermes de la mer d'Alboran. Bulletin du Museum National d'Histoire Naturelle Paris 3e Serie. Zoologie No. 231. 155: 789-798. 1977. Repartition et diversite des Echinodermes (Holothurides-Asterides) en zone profunde dans le Golfe de Gascogne. Deep-Sea Research 24: 549-563. Sime, A. A. T. & Cranmer, G. J. 1985. Age and growth of North Sea echinoids. Journal of the Marine Biological Association of the United Kingdom 65: 583-588. 1 98 HARVEY, GAGE, BILLETT, CLARK & PATERSON Sladen, W. P. 1 889. Asteroidea. Report of the Scientific Results of the voyage of H. M.S. Challenger 1873-1876. Zoology 30: 1-935. Suchanek, T. H., Williams, S. L., Ogden, J. C, Hubbard, D. K. & Gill, I. P. 1985. Utilization of shallow- water seagrass detritus by Caribbean deep-sea macrofauna: 613C evidence. Deep-Sea Research 32: 201-214. Siissbach, S. & Breckner, A. 1911. Die Seeigel, Seesterne und Schlangensterne der Nord und Ostsee. Wissenschaftliche Meeresuntersuchungen (Kiel) N.S. 12: 167-300. Theel, H. 1882. Report on the Holothurioidea dredged by H.M.S. Challenger during the years 1873-1876. Part 1 . Report of the Scientific Results of the voyage of H.M.S. Challenger 1873-1876. Zoology 4( 1 3): 1-1 76. 1886a. Report on the Holothurioidea dredged by H.M.S. Challenger during the years 1873-1876. Part 2. Report of the Scientific Results of the voyage of H.M.S. Challenger 1873-1876. Zoology 14(39): 1-290. 18866. Report on the Holothurioidea of the Blake expedition. Bulletin of the Museum of Comparative Zoology Harvard 13( 1 ): 1-2 1 . Thomson, W. 1874. On the Echinoidea of the Porcupine deep-sea dredging expedition. Philosophical Transactions of the Royal Society 164: 719-756. Tyler, P. A., Billett, D. S. M. & Gage, J. D. (1987). The ecology and reproduction of Cherbonniera utriculus and Molpadia blakei from the N.E. Atlantic. Journal of the Marine Biological Association of the United Kingdom 67: 385-398. & Gage, J. D. 1 9840. The reproductive biology of echinothuriid and cidarid sea urchins from the deep sea (Rockall Trough, NE Atlantic). Marine Biology 80: 63-74. & 19846. Seasonal reproduction of Echinus affinis (Echinodermata: Echinoidea) in the Rockall Trough, NE Atlantic Ocean. Deep-Sea Research 31: 387-402. — , Gage, J. D. & Billett, D. S. M. 1985a. Life-history biology of Peniagone azorica and P. diaphana (Echinodermata: Holothurioidea) from the northeast Atlantic Ocean. Marine Biology 89: 71-81. , Muirhead, A., Billett, D. S. M. & Gage, J. D. 19856. Reproductive biology of the deep-sea holothurians Laetmogone violacea and Benthogone rosea (Elasipoda: Holothurioidea). Marine Ecology Progress Series 23: 269-277. -, Pain, S. L., Gage, J. D. & Billett, D. S. M. 1984. The reproductive biology of deep-sea forcipulate sea stars (Asteroidea: Echinodermata) from the N. E. Atlantic Ocean. Journal of the Marine Biological Association of the United Kingdom 64: 587-601. Verrill, A. E. 1 895. Distribution of the echinoderms of Northeastern America. American Journal of Science (3) 49: 127-141 & 199-212. Manuscript accepted for publication 3 June 1987 British Museum (Natural History) The birds of Mount Nimba, Liberia Peter R. Colston & Kai Curry-Lindahl For evolution and speciation of animals Mount Nimba in Liberia, Guinea and the Ivory Coast is a key area in Africa representing for biologists what the Abu Simbel site in Egypt signified for archaeologists. No less than about 200 species of animals are endemic to Mount Nimba. Yet, this mountain massif, entirely located within the rain-forest biome, is rapidly being destroyed by human exploitation. This book is the first major work on the birds of Mount Nimba and surrounding lowland rain- forests. During 20 years (1962-1982) of research at the Nimba Research Laboratory in Grassfield (Liberia), located at the foot of Mount Nimba, scientists from three continents have studied the birds. In this way Mount Nimba has become the ornithologically most thoroughly explored lowland rain-forest area of Africa. The book offers a comprehensive synthesis of information on the avifauna of Mount Nimba and its ecological setting. During the 20 years period of biological investigations at Nimba this in 1962 intact area was gradually opened up by man with far-reaching environmental consequences for the rain-forest habitats and profound effects on the birds. Therefore, the book provides not only a source of reference material on the systematics, physiology, ecology and biology of the birds of Mount Nimba and the African rain-forest, but also data on biogeography in the African context as well as conservation problems. Also behaviour and migration are discussed. At Nimba a number of migrants from Europe and/or Asia meet Afrotropical migratory and sedentary birds. Professor Kai Curry-Lindahl has served as Chairman of the Nimba Research Laboratory and Committee since its inception in 1962. Peter Colston is from the Subdepartment of Ornithology, British Museum (Natural History), Tring, and Malcolm Coe is from the Animal Ecology Research Group, Department of Zoology, Oxford. 1986, 129pp. Hardback. 0 565 00982 6 £17.50. Titles to be published in Volume 54 The crania] muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences. By Gordon J. Howes A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles. By Keith H. Hyatt & Rowan M. Emberson A revision of Haplocaulus Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives. By Alan Warren Echinoderms of the Rockall Trough and adjacent areas. 3. Additional records. By R. Harvey, J. D. Gage, D. S. M. Billett, A. M. Clark & G. L. J. Paterson A morphological atlas of the avian Uropygial gland. By David W. Johnston Primed in Great Britain by Henry Ling Ltd., at the Dorset Press, Dorchester, Dorset INAIUKAL PRESENTED GENERAL I Bulletin of the British Museum (Natural History) A morphological atlas of the avian uropygial gland David W. Johnston Zoology series Vol 54 No 5 24 November 1988 The Bulletin of the British Museum (Natural History), instituted in 1949, is issued in four scientific series. Botany, Entomology, Geology (incorporating Mineralogy) and Zoology, and an Historical series. Papers in the Bulletin are primarily the results of research carried out on the unique and ever-growing collections of the Museum, both by the scientific staff of the Museum and by specialists from elsewhere who make use of the Museum's resources. Many of the papers are works of reference that will remain indispensable for years to come. Parts are published at irregular intervals as they become ready, each is complete in itself, available separately, and individually priced. Volumes contain about 300 pages and several volumes may appear within a calendar year. Subscriptions may be placed for one or more of the series on'either an Annual or Per Volume basis. Prices vary according to the contents of the individual parts. Orders and enquiries should be sent to: Publications Sales, British Museum (Natural History), Cromwell Road, London SW7 5BD, England. World List abbreviation: Bull. Br. Mus. nat. Hist. (Zool.) © Trustees of the British Museum (Natural History), 1 988 The Zoology Series is edited in the Museum's Department of Zoology Keeper of Zoology : MrJ. F. Peake Editor of Bulletin : Dr C. R. Curds Assistant Editor : Mr C. G. Ogden ISBN 0565 05041 9 ISSN 0007- 1 498 Zoology series Vol54 No. 5 pp 199-259 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 24 November 1988 A morphological atlas of the avian uropygial gland David W. Johnston* Department of Zoology, University of Florida, Gainesville, Florida 3261 1 USA Dedicated to PIERCE BRODKORB, whose encouragement , friendship', and scholarship influenced the preparation of this monograph Contents Introduction Materials and methods Systematic accounts of gland morphology Weights and sizes of glands . . . . Feathers on glands Naked and tufted glands .... Gland absence Glands in flightless birds .... General taxonomic considerations of glands . Functions of glandular secretions . Future studies Acknowledgments Summary Literature Cited bKITISH M (NATURAL HI 25NOV PRESEN GENERAL L Introduction The uropygial gland (also known as the uropygium, preen-, oil-, rump-, tail-, and coccygeal gland; glandula uropygii; the 'eloeodochon' of Coues 1890) is the only compact gland in the avian - integument. Lying medially and dorsal to the levator muscles of the tail, this gland is usually bilobed and partly covered by skin and body feathers. It secretes a chemically complex oil through ducts in a papilla which often bears a feather tuft (circulus uropygialis of Baumel et al. 1979). Most reports and investigations on the gland for at least 1 50 years have concentrated on specific topics such as histology, morphology, function, chemical nature of secretions, and development. The earliest published references to the uropygial gland focused almost entirely on function. Emperor Frederick II of Hohenstaufen about 1260 (Wood & Fyfe 1943) in his treatise on falconry gave the view that birds of prey transfer oil from the gland to their talons via the mandibles, the oil presumably being noxious and capable of killing the prey more quickly. Willughby (1678) noted that the 'oyly pap . . . recomposes and places them [feathers] in due order.' The French anatomist Cuvier (1799-1805) provided the first description of the gland's internal anatomy. Burton (1822) considered size as well as function of the gland in Fregata aquila. Audubon (1829) discussed the use of the glandular secretion in lubricating the plumage of 'The Bird of Washington' (the Bald Eagle, Haliaeetus leucocephalus). From 1832-1836, F.O. Morris and Charles Waterton exchanged acrimonious and unscientific letters in which they debated the functions ('office') of the gland "Present address: 5219 Concordia St., Fairfax, Virginia 22032 USA. Bull. Br. Mm. nat. Hist. (Zool.) 54(5): 199-259 Issued 24 November 1988 200 DAVID W. JOHNSTON mostly in domestic birds, and they even questioned the ability of birds to preen with oil. Macgillivray's (1837) interest in the gland was also largely functional, although he reported an increase in gland size at the time of moulting. Crisp (I860) questioned this report, and found no experimental evidence for such seasonal size change. Hussey (1860), Waterton (1860), and Matthews (1861) continued to be concerned with preening and the use of oil in 'barn-door' fowls. Although these earlier authors were pre-occupied with the gland's functional attributes, some of their reports contained passing references to gland morphology in various birds (e.g., duck, fowl, dipper, robin). Nitzsch ( 1 840) published the first account to include morphological information for glands in many taxa. He discussed for many groups of birds the gland's presence or absence, tufted vs. naked condition, relative sizes, and shapes. This hallmark publication by Nitzsch was followed by subsequent authors who either copied Nitzsch or provided information on gland morphology in additional species: Crisp (1860, 1862), Owen (1866), Kossmann (1871), Garrod (1874a, 6), Coues (1890), and Newton (1893-1896). Beddard (1898) then published his renowned classification of birds in which he included some morphological notes on glands in many major taxa. Papers and books by Pycraft (1900, 1910), Lunghetti (e.g., 1906), Granvik (1913), and Paris (e.g., 1913) reported much new information about gland morphology in selected species. Thus, information about gland morphology in different groups and species was scattered among these and other publications through the first part of the 20th century. More recently, Elder (1954), Lucas & Stettenheim (1972), and Jacob & Ziswiler (1982) have provided information on gland morphology in additional taxa. These three publications and Stettenheim (1972) contain a wealth of references to various biological attributes of uropygial glands (histology, functions, and chemistry). The degree to which any gland attribute can be used in avian taxonomy remains controversial. Early classifications of birds (Nitzsch 1840, Beddard 1898, Paris 1913, Verheyen 195 5- 1960) often employed gland morphology as diagnostic properties of given taxa, but many more modern schemes (e.g., Hancock &Kushlan 1984) have not. Jacob (e.g., 1978), Jacob & Ziswiler (e.g., 1982), and von Jacob & Hoerschelmann (1985) provide a chemotaxonomic approach in which they relate the qualitative chemical composition of gland secretions to the systematic positions of avian taxa. Their results seem to show qualitative differences at some ordinal, family, and subfamily levels. Perhaps it is too soon to evaluate this approach, i.e. whether it is any more fundamental in avian taxonomy than a scheme employing only gland morphology, as a taxonomic characteristic. Despite a plethora of publications, to date no one has compiled a single, complete, comprehen- sive monograph on the gland's morphological variations in all major avian taxa. The present monograph covers, both generally and specifically, the morphology of the gland in all families and subfamilies, a review of the pertinent morphological literature, and corrections of erroneous and incomplete information about glands, much of this perpetuated from author to author over the years without questioning and adequate documentation. This comprehensive survey is deemed necessary prior to an accurate assessment of the function(s) of the gland's secretion and to the possible use of gland morphology as a character in avian systematics. Materials and methods Most birds examined in this study were preserved in alcohol or other fluids in museum collections. For a few species, where such specimens were unavailable, I examined museum study skins but only for rare species that were believed to have tufted glands. Supplementing the museum studies were ( 1 ) birds caught in mist-nets, or collected with a shotgun in Florida, (2) road kills in Virginia, England, Ireland, Belize, and Malawi and (3) some freshly-dead birds from zoos (e.g., parrots, toucans, and hornbills). I dissected a gland from one or more species in each family intact from the alcoholic specimen, and freed it from connective and other non-glandular tissues. That gland was then used for the artist's illustrations and studies of feathers. These gland examples currently remain in my collection. Anatomical nomenclature for the gland's major parts follows that of Baumel et al. (1979) as illustrated in Figure 1 . AVIAN UROPYGIAL GLAND 201 TUFT PAPILLA LOBES Fig. 1 External morphological nomenclature of the uropygial gland. Body and gland weights were taken, for the most part, from freshly killed birds, but some frozen birds (e.g., penguins, ducks, hawks) were thawed, weighed, and their glands dissected free for weighing. Linear dimensions of glands were usually not made. In only a few cases were zoo birds used for weights because I did not know whether the bird might have been emaciated at the time of its death. Glands from fresh birds were never compressed before weighing in order to preserve the gland's oil content at the time of death. The gland tuft, if present, was included in the gland weight, as was any oil in the tuft. For the microscopic study of gland feathers, two or three feathers were dissected from a gland, cleared in xylene, and mounted in Canada balsam on a microscope slide. Each feather preparation could then be studied under the microscope at magnifications up to SOX. I did not consider gland histology or development (see reviews in Lucas & Stettenheim 1972 and Jacob & Ziswiler 1982) or the number of orifices in the papilla's tip (see Jacob & Ziswiler 1982). This study resulted in the examination of representative glands from every family and all subfamilies (except one) as identified in Peters (1931-1986). In all, I examined 3011 individuals from 1433 species and 883 genera. The objectives of this examination were to determine for each individual the presence or absence of the gland, its shape, relative size, weight, presence or absence of the papilla and feather tuft. Any individual variations in these characteristics are noted in the systematic accounts to follow. Systematic accounts of gland morphology Classification here follows that of Peters (1931-1986). The terminology for gland morphology (see Fig. 1) has been adapted from Baumel et al. (1979). At the end of the Morphology section for each family is the gland feather type (see section on Feathers on glands for definitions). Unless otherwise indicated, all specimens were considered to be adults. Format for the Material examined: for each species, the number of individuals examined; in parentheses, when available, sex, body weight in grams followed by gland weight as a percent of body weight. Z = zoo bird; SK = study skin. Accompanying gland illustrations contain a linear scale that equals 1 cm. Order Struthioniformes General characteristics. Absent in adult Ostrich, Rhea, Cassowary, and Emu, but present (naked) in Rhea and Emu chicks. Present (naked or with minute feathers) in Apterygidae. 202 DAVID W. JOHNSTON Family Struthionidae (Ostriches) MORPHOLOGY. Absent in all age groups. Pycraft (1900) also found no glands in any age group of this species. MATERIAL EXAMINED. Struthio camelus 1 1 (9 chicks of various ages, 2 ad.). Family Rheidae (Rheas) MORPHOLOGY. Present (naked) and very small in all chicks examined; absent in adult. Pycraft (1900) found the gland in the 'embryo and nestling' but absent in the adult of Rhea americana. MATERIAL EXAMINED. Rhea americana 14(11 chicks up to 4 months, 3 ad.). Pterocnemia pennata, lad. Family Casuariidae (Cassowaries) MORPHOLOGY. Absent in all age groups (absent in adult fide Pycraft 1900). MATERIAL EXAMINED. Casuarius casuarius 4(1 chick, 1 immature, 2 ad.). Family Dromaiidae (Emus) MORPHOLOGY. Present (naked) in all chicks examined; probably absent in adults (first reported by Pycraft 1900). MATERIAL EXAMINED. Dromaius novaehollandiae 1 3 (chicks up to 2 weeks). Family Apterygidae (Kiwis) MORPHOLOGY. More terminally located than in any other family, apparently single-lobed, papilla conical, naked (or 1-2 minute 'bristle-like feathers' in A. australis mantellifide Beddard 1898, 1899). NOTE. Beddard ( 1 898, 1 899) was apparently the first to report a gland not only in Apteryx but also in any ratite bird. The kiwi gland is clearly different from every nonratite gland examined because of its single-lobed appearance and terminal location. Its presence only in adults distinguishes kiwis from other ratites. The presence of the gland in kiwis supports a suggested affinity between Apterygidae and Tinamidae (see Cracraft 1981). MATERIAL EXAMINED. Apteryx australis 5 (1 chick, 4 ad.); A. owenii 1. I 1 Rhea americana Dromaius novaehollandiae Apteryx australis (chick) (chick) Order Tinamiformes General characteristics. Tufted with long feathers. Family Tinamidae (Tinamous) MORPHOLOGY. Indistinctly bilobed, papilla small or lacking, tufted. Verheyen ( 1 960a) regarded the gland as always present in the family although 'sometimes vestigial.' In Crypturellus spp. the four AVIAN UROPYGIAL GLAND 203 feathers, 2 long and 2 short, are 4-5, 3-4 mm in length; in Eudromia spp. the four feathers are 13, 12 mm; shorter (1 -5 mm) in Rhynchotus rufescens (Jacob & Ziswiler 1982). Type II. MATERIAL EXAMINED. Crypturellus soui 1; C. undulatus 1; C. cinnamomeus 2; C. tataupa 1; Rhynchotus rufescens 1 ; Nothoproctaperdicaria 1 ; N. pentlandii 1 ; Eudromia elegans 3; E.formosa 1 ; Tinamotis pentlandii 1. Order Procellariiformes General characteristics. Densely tufted in all families. Family Diomedeidae (Albatrosses) MORPHOLOGY. Distinctly bilobed, papilla rounded and slightly raised, tufted (32 feathers in Diomedea exulans, Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Diomedea exulans 1; D. nigripes 2; D. immutabilis 1; D. melanophrys 1; Phoebe tria palpebrata 1 . Family Procellariidae (Fulmars, Petrels, Shearwaters) MORPHOLOGY. Distinctly bilobed, papilla small or lacking, tufted (24-36 feathers, Paris 1913; 36-42 feathers in 2 species, Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Macronectes giganteus 1 ; Fulmarus glacialoides 1 ; F. glacialis 2 (F im.: 642-4, 0-67); Thalassoicaantarctical', Daption capense 1; Pagodromanivea 1 (M: 245-0, 0-25); Pterodroma hasitata 5 (M: 481-3, 0-36; 364.9, 0-34. F: 459-0, 0-35); P. hypoleuca 1; Halobaena caerulea 1; Pachyptila desolata 1; Bulweria bulwerii 1; Calonectris diomedea 1 (F:410-0, 0-40); Puffinus gravis 7(M: 636-6, 0-44. F: 654-5, 0-39); P. griseus 3; P. puffinus l(unsexed: 450-0, 0-53); P. Iherminieri 2. Eudromia elegans Diomedea immutabilis Puffinus Iherminieri Family Hydrobatidae (Storm Petrels) MORPHOLOGY. Indistinctly (Oceanites) or distinctly (Oceanodroma) bilobed, papilla small, tufted (20 feathers in O. melania). Type I. 204 DAVID W. JOHNSTON MATERIAL EXAMINED. Oceanites oceanicus 5 (M: 35-6, 0-40; 31-1, 0-46. F: 35-0, 0-40; 33-6, 0-38); Oceanodroma leucorha 1 (M: 29-5, 0-23); O. melania 1 (unsexed: 53-8, 0-69); O. homochroa 1 (M: 34-0, 0-31); O.furcata \ (unsexed: 54-4; 0-39). Family Pelecanoididae (Diving Petrels) MORPHOLOGY. Distinctly bilobed, papilla small, tufted (20 feathers). Type I. MATERIAL EXAMINED. Pelecanoides magellani \ ; P. georgicus 1 ; P. urinator \ . Order Sphenisciformes General characteristics. Densely tufted. Family Spheniscidae (Penguins) MORPHOLOGY. Distinctly bilobed, flattened and raised papilla, tufted, ('about 50' feathers, Paris 1913; 44-48 feathers in 2 species, Jacob & Ziswiler 1982). Illustrations in Grasse (1950: 286) and Jacob & Ziswiler (1982, Fig. 4a, p. 216) of Spheniscus demersus, lacking a feather tuft, are inac- curate, copied from Paris (1913) who illustrated one gland from which the tuft had undoubtedly been removed. Type Ha. MATERIALS EXAMINED. Aptenodytes patagonica 1; A.forsteri 1; Pygoscelis papua 1; P. adeliae 2 (M: 4990, 0-06; 5348, 0-12); P. antarctica 1; Eudyptes crestatus 1; E. chrysolophus 1; Eudyptula minor 1 ; Spheniscus humboldti 1 . Oceanodroma melania I 1 Pelecanoides magellani Aptenodytes forsteri Order Gaviiformes General characteristics. Deeply bilobed, densely tufted. Family Gaviidae (Loons) MORPHOLOGY. Distinctly bilobed and elongated, small papilla, tufted (30^40 feathers, Paris 1913; 26-28 feathers in 2 species, Jacob & Ziswiler 1982). Type I. AVIAN UROPYGIAL GLAND 205 MATERIAL EXAMINED. Gavia stellata 5 (M: 1597, 0-19; 1638, 0-17. F: 1351, 0-21); G. arctica 2 (M: 1598, 0-30. 1 unsexed: 2082, 0-23); G. immer 15 (M: 2780, 0.09; 3180, 0-11; 3490, 0-11); G. adamsii 1 (unsexed: 41 15, 0-19). Order Podicipediformes General characteristics. Deeply bilobed, densely tufted. Family Podicipedidae (Grebes) MORPHOLOGY. Distinctly bilobed and somewhat flattened papilla raised nearly perpendicular to the two lobes, tufted (14-18 subterminal feathers in 2 species, Jacob & Ziswiler 1982). Verheyen (\959d) reported the gland as 'voluminous and crowned with long plumes.' Type I. MATERIAL EXAMINED. Rollandia rollandl; R. microptera 1 ; Tachybaptus ruficollis 1 ; T. rufolavatus 1 ; T. dominions 1; Podilymbus podiceps 8 (M: 358-0, 0-42; 380-2, 0-19. F: 312-0, 0-22; 301-2, 0-26); P. gigas 1 ; Podiceps major 1 ; P. auritus 3 (M : 410-0, 0-23; 342-7, 0-22); P. grisegena 1 ; P. nigricollis 2; P. occipitalis 2; P. taczanowskii \\Aechmophorus occidentalis 1 . Spheniscus humboldti Gavia immer Podiceps auritus Order Pelecaniformes General characteristics. Densely tufted. Family Phaethontidae (Tropicbirds) MORPHOLOGY. Distinctly bilobed, papilla tufted (40 feathers in P. lepturus}. Verheyen (19606) stated (p. 12) that the gland 'lacks a nipple except in Phaethon.' Type I. MATERIAL EXAMINED. Phaethon aethereus 1 (F: 496-0, 0-43); P. rubricauda 1; P. lepturus 3. 206 DAVID W. JOHNSTON Family Fregatidae (Frigatebirds) MORPHOLOGY. Indistinctly bilobed, papilla broad and flattened, tufted (ca 30 feathers in F. magnificens). Type I. MATERIAL EXAMINED. Fregata magnificens 4 (M: 1365-5, 0-07; 1336, 0-07. F: 1512, 0-06); F. aquila \ ; F. minor 1 ; F. ariel 1 . Family Phalacrocoracidae Subfamily Phalacrocoracinae (Cormorants) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, tufted (36-52 feathers in 2 species, Jacob & Ziswiler 1982). Papilla and feather tuft subterminal. Type I. MATERIAL EXAMINED. Phalacrocoraxharrisi\;P. auritus24(M: 1660,0-25; 1710, 0-25. xofSF: 1048, 0-25); P. aristotelis 1; P. magellanicus 1; P. bougainvillii 1; P. albiventer 1. Phaethon lepturus Fregata ariel Phalacrocorax auritus Subfamily Anhinginae (Darters) MORPHOLOGY. Bilobed and somewhat flattened, papilla absent, short tuft of 14 feathers. Type I. MATERIAL EXAMINED. Anhinga anhinga 11 (M: 1230, 0-16; 1352, 0-12; 1230, 0-16. F: 1307, 0-15; 1 1 78, 0- 1 7); A . melanogaster 2. Family Sulidae (Boobies, Gannets) MORPHOLOGY. Distinctly flattened and bilobed, papilla absent, tufted with 70 short feathers in S. bassana (Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Sula bassana 3 (M subad.: 2200, 0-38; S. dactylatra 2; 5. sula 1 . Family Pelecanidae (Pelicans) MORPHOLOGY. Large and bilobed, papilla very short and broad, tufted (70 feathers, Paris 1913; 66 feathers in P. onocrotalus, Jacob & Ziswiler 1982). Tuft and openings obviously subterminal, Type I. MATERIAL EXAMINED. Pelecanus onocrotalus 1; P. philippensis 1; P. erythrorhynchos 2 (M: 4700, 0-30; P. occidentalis 9 (M im.: 2730, 0-43; 3060, 0-32; unsexed ad.: 3320, 0-37). AVIAN UROPYGIAL GLAND 207 Anhinga anhinga Sula bassana Pelecanus onocrotalus Order Ciconiiformes General characteristics. Much inter- and some intrafamilial variation: naked, sparsely or densely tufted. NOTE. The large morphological differences among glands examined here lend support to Olson's (1979) view that the Ciconiiformes is not a natural order. Family Ardeidae (Herons, Bitterns) Subfamily Ardeinae (Day Herons) MORPHOLOGY. Although considerable variation occurs in the family, the gland is generally small (see also Paris 1913: 192), bilobed, lacks a papilla (or 'very short,' Paris 1913: 192), and is tufted (4-18 feathers) or naked. Although 'small' in many species, the gland cannot be regarded as 'rudimentary' as described by Jacob (1978: 168). Verheyen (19596) noted that in the Ardeae, the gland is naked or has a few vestigial feathers. Miller (1924) described variations in the tuft among 13 species, then reported the tuft as absent in Ardea goliath, A. herodias, A. cocoi, A. occidentalis, Notophoyx novaehollandiae , N. pacifica, Egretta candidissima, and Hydranassa tricolor. I found the tuft absent only in Pilherodias pileatus, Ardea pacifica, Egretta rufescens, E. tricolor, E. novaehollandiae, E. garzetta and E. sacra. In A. herodias (contra Miller 1924), all 10 specimens examined here had extremely small feathers, often as few as 4. Beddard (1898) and Gadow (1893) reported that all Ardeidae have feathered glands. Thus in the family, the tuft might be absent, represented by only 4-8 feathers (Ardea herodias, Agamia agami), or tufted with 16-18 feathers (Ixobrychus minutusfide Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Pilherodias pileatus 1*; Ardea cinerea 1; A. herodias 10 (M: 2695-0, 0-21; 1 28 1 -0, 0-05; 1 790, 0- 1 4. F: 1 250-0, 0. 1 7; 1 507, 0- 1 0); A . pacifica \*;A. melanocephala \\A. purpurea 1; A. alba 8 (M: 478-5, 0-15; 579-0, 0-12); Egretta rufescens 1*; E. tricolor *; E. ibis 1 1 (M: 342-6, 0-03. x of 5F: 286-8, 0-04); E. novaehollandiae 1*; E. caerulea 3 (F: 372-0, 0-07); E. garzetta 1*; E. sacra 1 *; Ardeola speciosa \;A. striata 1 (M: 220-3, 0-07; 220- 1 , 0-07; 1 95-4, 0-06); Agamia agami 2. NOTE. Ligon (1967: 1) believed 'that the storks and herons are dissimilar' in many features (osteology, myology, pterylography and others); the dissimilar uropygial glands of the two groups add another difference. *naked gland, present study. 208 DAVID W. JOHNSTON Subfamily Nycticoracinae (Night Herons) MORPHOLOGY. Indistinctly bilobed, no papilla, tufted (Nycticorax, Nyctanassa) or naked (Cochlearis). MATERIAL EXAMINED. Nyctanassa violacea 5 (M: 546-0, 0-04); Nycticorax nycticorax 2; Cochlearius cochlearius 2. NOTE. Peters regarded Cochlearis as comprising a separate family, the Cochlearidae (Peters 1931, Vol. I, 1st ed.). Mayr & Cottrell, (1974 in their 2nd ed. of Peters' Vol. I) and Hancock & Kushlan (1984), however, included Cochlearis in a subfamily (Nycticoracinae) of the family Ardeidae. The gland of Cochlearis differs markedly from that of all other ardeids because of its relatively large size, distinctive appearance (see figure), and absence of papilla and feather tuft. Beddard (1898) and Miller (1924) both noted this distinctiveness of the gland in Cochlearis. Subfamily Tigrisomatinae (Tiger Herons) MORPHOLOGY. Bilobed, short papilla, tufted. Type I. MATERIAL EXAMINED. Tigrisoma mexicanum 1 . Subfamily Botaurinae (Bitterns) MORPHOLOGY. Indistinctly bilobed, no papilla, small tuft. Type I. MATERIAL EXAMINED. Ixobrychus exilis 2 (M: 68-0, 0-05. F: 38-6, 0-03); Botaurus lentiginosus 5 (M: 564-0, 0-31; 789-0, 0-42; 720-0, 0-38. F: 599-3, 0-38). Family Scopidae (Hammerhead) MORPHOLOGY. Indistinctly bilobed, papilla short and somewhat flattened, and tufted (18 long feathers). The gland of this species is distinct from those of ardeids, more closely resembling that of Balaeniceps and the Ciconiidae (see figures). Type I. MATERIAL EXAMINED. Scopus umbretta 2. Family Ciconiidae (Storks) MORPHOLOGY. Distinctly bilobed and large, papilla small, tufted (36 feathers in C. ciconia, Jacob & Ziswiler 1982). Unlike the illustration of Mycteria here, in Anastomas, Ciconia nigra, and Ardea herodias Cochlearius cochlearius Scopus umbretta AVIAN UROPYGIAL GLAND 209 Leptoptilos the gland appears to be separated into right and left portions, each with a separate lobe, feather tufts and orifices, features implied by Nitzsch (1867: 131). Type I. MATERIAL EXAMINED. Mycteria americana 3 (F: 2490-0, 0-05); Anastomus oscitans 1; Ciconia nigra 1 ; C. abdimii 1 ; C. episcopus 1 ; C. ciconia 1 ; Ephippiorhynchus asiaticus 1 ; Leptoptilos crumeniferus 1 . Family Balaenicipitidae (Shoebill) MORPHOLOGY. Indistinctly bilobed and relatively small (see figure and Bartlett 1861), papilla small, tufted. With the exception of the large tuft in Scopus, I agree with Miller's (1924: 322) comment that 'in Balaeniceps the tuft is very much larger than in any heron,' although I did not count the feathers. Type II. MATERIAL EXAMINED. Balaeniceps rex 1Z. NOTE. Gland morphology sheds no light on the controversy over the affinities of Balaeniceps (Cottam 1957, Olson 1979, Cracraft 1981). Family Threskiornithidae (Ibises, Spoonbills) Subfamily Threskiornithinae (Ibises) MORPHOLOGY (family). Distinctly bilobed, papilla absent, tufted (26-28 feathers, Paris 1913; 30 feathers in E. ruber, Jacob & Ziswiler 1 982). Nitzsch ( 1 867) implied that ibises have glands 'divided in half.' In the present study one specimen each of Eudocimus albus and Platalea leucorodia had glands with nearly separate lobes, separate orifices, and separate feather tufts. Type I. MATERIAL EXAMINED. Eudocimus albus 2 (M, Z: 999, 0-12); E. ruber 2; Plegadis falcinellus 3 (M: 530-0, 0-18; F: 420.0, 0-19); Threskiornis aethiopicus 2. Subfamily Plataleinae (Spoonbills) MATERIAL EXAMINED. Platalea leucorodia 1; P. ajaja \ (M: 985-0, 0-11). Mycteria americana Balaeniceps rex Threskiornis aethiopicus 2 1 0 DAVID W. JOHNSTON Order Phoenicopteriformes General characteristics. Densely tufted. Family Phoenicopteridae (Flamingos) MORPHOLOGY. Bilobed, papilla absent, tufted (30 feathers, Paris 1913). Type Ha. NOTE. Paris (1913: 190) believed that the gland of Phoenicopterus roseus closely resembles that of the Anseriformes. In contrast, I found marked differences in the gland of Phoenicoparrus from both the Anseriformes and Ciconiiformes (see figures), relationships suggested by Sibley (1967), and Sibley et al. (1969). The gland resembles that of the Recurvirostridae, suggesting a charadriiform relationship as proposed by Olson & Feduccia (19806). MATERIAL EXAMINED. Phoenicopterus ruber 1; Phoeniconaias minor 2; Phoenicoparrus andinus 1; P.jamesi 1. Order Falconiformes General characteristics. Inter- and some intrafamilial variation: naked or sparsely to densely tufted. Family Cathartidae (American Vultures) MORPHOLOGY. Indistinctly bilobed, round papilla, naked; two separate, distinct orifices. Nitzsch's ( 1 867) report that 'vultures of the New World' have a short circlet of feathers at the gland apex appears to be in error. I did not confirm Fisher's (1943) statement that down is often present on the oil gland in Coragyps atratus. NOTE. My findings support Ligon's (1967: 1) view 'that the Cathartidae are not at all closely related to the remainder of the Falconiformes.' The naked glands of the Cathartidae, however, differ markedly from the heavily tufted glands of the Ciconiidae, to which cathartids might otherwise be related (Ligon 1967). MATERIAL EXAMINED. Coragyps atratus 5 (M: 2221-0, 0-04; 2245-0, 0-04. F: 2135-0, 0-05; 2238-0, 0-04); Cathartes aura 7 (M: 1939-0, 0-02. x of 5F: 2019-0, 0-02); Gymnogyps calif ornianus 2 (1 SK); Vultur gryphus 2; Sarcoramphus papa 2. Phoenicoparrus jamesi Cathartes aura Pandion haliaetus AVIAN UROPYGIAL GLAND 211 Family Accipitridae Subfamily Pandioninae (Osprey) MORPHOLOGY. Large and distinctly bilobed, indistinct papilla, tufted (18 feathers, Jacob & Ziswiler 1982). Type I. NOTE. Sometimes included in a separate family, Pandionidae (Cracraft 1981), the Osprey's gland differs from those of the Accipitrinae by being much heavier and having a longer, usually denser feather tuft. MATERIAL EXAMINED. Pandion haliaetus 5 (M: 1433-0, 0-28; 1363-0, 0-31. F: 1500-0, 0-32). Subfamily Accipitrinae (Hawks, Eagles) MORPHOLOGY. Bilobed, papilla moderately developed, sparsely (Ictinid) to densely (Haliaeetus) tufted (12-20 feathers in 7 species, Jacob & Ziswiler 1982). Type 1 . MATERIAL EXAMINED. Aviceda leuphotes 1; Elanoides forficatus 2 (M: 492-0, 0-13); Harpagus bidentatus 1; Ictinia plumbea 1; /. mississippiensis 1; Haliaeetus leucocephalus 3 (ad. sex?: 3625, 0-07); Neophron percnopterus 2; Gyps fulvus 1; Circus hudsonius 2 (F: 324-6, 0-03); Melierax canorus 1; Accipiter nisus 1; A. striatus 10 (subad. M: 84-2, 0-05; 98-0, 0-04; 88-9, 0-06. x of 4 ad. F: 157-3, 0-06); A. cooperii 4 (ad. F: 41 1 -7, 0-07; 390-0, 0-07)M. gentilis 4 (subad. M: 816-0, 0-06; 775-0, 0-05; 918-0, 0-07. Ad. F: 930-0, 0-03); Geranospiza caerulescens 1; Buteo lineatus 9 (ad. M: 612-3, 0-05; 595-7, 0-06. Ad. F: 601-0, 0-05; 566-7, 0-07); B. platypterus 2 (subad. M: 489-4, 0-04; 309-0, 0-05); B. swainsoni 1 (ad. M: 874-0, 0-04); B.jamaicensis 14 (ad. M: 1307-3, 0-04. Subad. M: 856-3, 0-06. Subad. F: 1210-0, 0-04; 1272-0, 0-08); B. lagopus 3 (ad. M: 860-0, 0-04); Pithecophagajefferyil; Aquila chrysaetos 1. Family Sagittariidae (Secretarybird) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, tufted (20 feathers). In most specimens the gland appears to be nearly separated into two distinct lobes, with separate papillae and feather tufts. Although writing about 'Les Cariamiformes,' Verheyen (1957c) stated erroneously that the gland is absent in Sagittarius. Type I. MATERIAL EXAMINED. Sagittarius serpentarius 6. Buteo jamaicemis Sagittarius serpentarius Falco columbarius 2 1 2 DAVID W. JOHNSTON Family Falconidae Subfamily Polyborinae (Caracaras) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, densely tufted. MATERIAL EXAMINED. Daptrius ater 1; Polyborus plancus 2 (unsexed im.: 900-5, 0-07). Subfamily Falconinae (Falcons) MORPHOLOGY. Distinctly bilobed, papilla moderately to well developed, tufted (17 feathers in Falco tinnunculus, Jacob & Ziswiler 1982), or rarely, naked. Both Miller (1924) and Verheyen (1959c) reported naked glands in Microhierax fringillarius and Nitzsch (1867) noted naked glands in two specimens of M. caerulescens. In my study all glands of 1 1 individuals of four species of Microhierax were naked, but all other genera and species in this subfamily had tufted glands. Type I. MATERIAL EXAMINED. Micros tur ruficollis 1 : Spiziapteryx circumcinctus 1 ; Polihierax semitorquatus 1 ; P. insignis 4; Microhierax (mostly SK) caerulescens 7; M. fringillarius 2; M. erythrogenys 1 ; M. melanoleucus 1; Falco sparverius 16 (x of 6 M: 100-3, 0-05. x of 6 F: 1 19-2, 0-08); F. tinnunculus 1; F. columbarius 2 (F: 191.0, 0-09); F. mexicanus 1; F. rufigularis 1; F. rusticolus 1; F. peregrinus 3 (M: 61 7-0, 0-08). Order Anseriformes Gland characteristics. Densely tufted. MORPHOLOGY (order). Large and distinctly bilobed, papilla moderately developed, tufted (22-90 feathers in 15 species, Jacob & Ziswiler 1982). The Anhimidae differ from the Anatidae only by having a gland that is less distinctly bilobed. Type I. Family Anatidae Subfamily Anseranatinae (Pied Geese) MATERIAL EXAMINED. Anseranas semipalmata, 1 . Subfamily Dendrocygninae (Whistling Ducks) MATERIAL EXAMINED. Dendrocygna bicolor 1 . Subfamily Anserinae (Swans, Geese) MATERIAL EXAMINED. Cygnusolor 1 (im. M: 10435,0-16); C. columbianus 1; Coscoroba coscoroba 1; Anser albifrons 1 (F: 2556, 0-11);^. caerulescens 2 (M: 2330, 0-13; 2154, 0-12); A. rossii 1 (M: 1616, 0-15); A. canagicus \ (M: 1855, 0-10); Branta canadensis 2 (M: 2435, 0-1 1. F: 3929, 0-15); Cereopsis novaehollandiae 1 . Subfamily Tadorninae (Shelducks) M ATERIAL EXAMINED. Alopochen aegyptica 1; Tachyeres pteneres 1; T.patachonicus 1. Subfamily Anatinae (Typical Ducks) MATERIAL EXAMINED. Rhodonessa caryophyllacea 1; Aix sponsa 3 (M: 642-0, 0-26; 573-1, 0-32. F: 595-2, 0-32); A. galericulata \\Anasstrepera 1 (M: 849-5, 0-20); A. crecca 3 (M: 251-0, 0-31; 295-5, 0-27. F: 262-0, 0-29); A. aucklandica 1; A. platyrhynchos 2 (M: 880-0, 0-23); A. acuta 1 (F: 708-5, 0-26); A. discors 8 (M: 341-5, 0-40; 368-2, 0-33. F: 365-5, 0-36; 384-0, 0-35; 430-0, 0-32); A. clypeata 2 (M: 672-0, 0-27); Aythya valisineria 3 (M: 893-3, 0-27. F: 792-0, 0-30; 884-2, 0-24); A. americana 2 (F: 1 172-0, 0-28); A. collaris 1 1 (x of 8 M: 749-6, 0-32. F: 697-5, 0-31; 745-0, 0-30); A. marila 2 (F: 843-0, 0-22; 991-6, 0-20); A. affinis 2 (M: 882-8, 0.22. F: 783-4, 0-22). Subfamily Merginae (Sea Ducks) MATERIAL EXAMINED. Somateria mollissima 1 (M: 2255, 0-18); S. spectabilis 1 (M: 1540, 0-26); Melanitta perspicillata 1 (F: 703-1, 0-20); Bucephala clangula 1; B. albeola 1; Mergus cucullatus 5 (M: 571-0, 0-34; 671-0, 0-37. F: 671-3, 0-30; 526-0, 0-28); M. senator 1 (F: 599-5, 0-36); M. merganser 2 (M: 1577, 0-21. F: 1027, 0-29); M. australis 1. AVIAN UROPYGIAL GLAND 2 1 3 Subfamily Oxyurinae (Stifftailed Ducks) MATERIAL EXAMINED. Oxyurajamaicensis 1 (M: 596-7, 0-27). Family Anhimidae (Screamers) MATERIAL EXAMINED. Anhima cornuta 1 (M, Z: 2600, 0-13); Chauna chavaria 1. Order Galliformes Gland characteristics. Inter- and intrafamilial variation: sparsely to densely tufted, or, rarely, naked. NOTE. Glands of most galliform families do not resemble those of the Anseriformes. These differ- ences do not support an anseriform-galliform relationship (see also Olson & Feduccia 1 980«). I did not confirm Pettingill's (1985) statement that 'certain species' of Galliformes lack a gland. Family Megapodiidae (Megapodes) MORPHOLOGY. Bilobed, papilla large, naked or tufted (6 feathers). The present study and the reports of Miller (1924) and Clark (1964) demonstrate naked glands in Leipoa, Alectura, Tallegalla jobiensis, and Aepypodius arfakianus, whereas tufted glands are known from five species of Megapodius and Macrocephalon maleo. Beddard (1898: 302) reported that megapodes have 'oil gland nude,' and both Sharpe and Ogilvie-Grant regarded the glands of these birds as nude (fide Miller 1924). Type I. MATERIAL EXAMINED. Megapodius nicobariensis 2; M.freycinet 3; M. pritchardii 6; Alectura lathami 1 ; Aepypodius arfakianus 1 . Anas discors Anhima cornuta Megapodius pritchardii Family Cracidae (Curassows, Guans, Chachalacas) MORPHOLOGY. Distinctly bilobed, papilla large, tuft usually short and sparsely feathered (6-12 feathers, 2-4 mm). Miller (1924: 322) reported an 'apparently bare' gland in one specimen of Ortalis vetula, and noted a 'virtually vestigial' tuft in all the Cracidae, this last conclusive statement confirmed in the present study. Type I. MATERIAL EXAMINED. Crax nigra 1 ; C. alberti 1 ; C. globulosa 1 ; Penelope jacu-caca 1 ; Ortalis guttata 2; O. vetula 1; Pipile pipile 1. 2 1 4 DAVID W. JOHNSTON Family Tetraonidae (Grouse, Ptarmigans) MORPHOLOGY. Distinctly bilobed, papilla large, tufted (10-12 feathers, Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Tetrao urogallus 2; Lyrurus tetrix 1; Lagopus lagopus 1 (M: 576-0, 0-18); Canachites canadensis 1 (M: 552-4, 0-02); Bonasa umbellus 3 (M: 552-2, 0-03. F: 591-5, 0-03); Pedioecetes phasianellus 1 (F: 664-0, 0-03); Tympanuchus cupido 1 (M: 863-5, 0-02); Centrocercus urophasianus 1 (M: 2221-7, 0-04). Family Phasianidae (Quails, Pheasants, Peacocks) MORPHOLOGY (family). Usually distinctly bilobed, papilla large, tuft variable (6-12 feathers, Paris 1913; 5-10 feathers in 6 species, Jacob & Ziswiler 1982; only 2 in Rollulus) or, rarely, absent (one specimen of Crossoptilon mantchuricum was naked as were five specimens of Argusianus). Earlier, Nitzsch (1840), Newton (1893-1896), Beddard (1898), Grasse (1950), and Verheyen (\956d) had reported the absence of a gland in Argusianus ( = Argus). Beddard (1898) found a tuft in one specimen of Callipepla squamata but a naked gland in another specimen. Type I. Subfamily Odontophorinae (American quail) MATERIAL EXAMINED. Callipepla squamata 2 (F: 209-4, 0-06); Lophortyx californica 3 (M: 133-2, 0-09. F: 169-4, 0-08); Colinus virginianus 9 (x of 4 M: 151-8, 0-15. x of 4 F: 156-5, 0-16); Cyrtonyx montezumae 1 . Subfamily Phasianinae (Partridges, Quails, Pheasants) MATERIAL EXAMINED. Francolinus adspersus 1; F. ahantensis 1; Perdix per dix 1 (F: 360-0, 0-09); Coturnix coturnix 1; Excalfactoria chinensis 3; Arbor ophila torqueola 1; A. brunneopectus 1; Rollulus roulroul 1; Tragopan temmincki 1; Lophophorus impejanus 1; Crossoptilon auritum 1; C. mantchuricum 1 ; Lobiophasis bulweri 1; Callus gallus 5 (M: 2270, 0-02); Callus gallus x Meleagris gallopavo 1; Catreus wallichii 1 (M, Z: 1340, 0-05); Phasianus colchicus 2 (M: 1374.7, 0-03; 1292, 0-02); Syrmaticus reevesii 1 ; Chrysolophus pictus 1 ; Argusianus argus 5; Pavo cristatus 3 (M, Z: 3350, 0-02); Afropavus congensis 3. Crax alberti Lyrurus tetrix Phasianus colchicus Family Numididae (Guinea fowl) MORPHOLOGY. Distinctly bilobed, papilla large, tufted (8 feathers in N. meleagris, Jacob & Ziswiler 1 982; only 2 in Phasidus). Type I. MATERIAL EXAMINED. Phasidus niger 1 ; Numida sp. 1 ; N. meleagris 1 ; Guttera pucherani 1 ; Acryllium vulturinum 1. AVIAN UROPYGIAL GLAND 215 Family Meleagrididae (Turkeys) MORPHOLOGY. Distinctly bilobed, papilla large, tufted (7, 9 feathers, Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Meleagris gallopavo 5 (ad. M: 7400, 0.02. Subad. M: 3740, 0-02. Subad. F: 1870,0-04). Family Opisthocomidae (Hoatzin) MORPHOLOGY. Bilobed, papilla small, tuft (up to 12 feathers) variable in size, or gland naked. Beddard (1898), Gadow (1893), and Verheyen (1956c) described the gland as feathered. I found that 9 nestlings, 'young,' or 'juveniles' had minute tufts, 2 'subadults' were naked, and 3 'adults' had tufted glands. Type I. MATERIAL EXAMINED. Opisthocomus hoazin 14. Numida sp. Meleagris gallopavo Opisthocomus hoazin Order Gruiformes Gland characteristics. Inter- and intrafamilial variation: gland absent, naked, or sparsely to densely tufted. Family Mesoenatidae (Mesites, Monias) MORPHOLOGY. Absent (also reported as such by Gadow 1893, Miller 1924, Verheyen 1958a, Van Tyne & Berger 1976). Beddard (1898: 381) erroneously reported the gland as present and nude. MATERIAL EXAMINED. Mesoenas variegata 1; M. unicolor 1; Monias benschil. Family Turnicidae (Bustard-Quails) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, tufted (also reported by Verheyen 1958«; ca 10 feathers). Type I. MATERIAL EXAMINED. Turnix sylvatica 2; T. tanki 1; T.suscitator 1; Ortyxelos meiffrenii 1. Family Pedionomidae (Collared Hemipodes) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, tufted (12 feathers). Type I. NOTE. Gadow ( 1 89 1 ) and Beddard ( 1 898) reported a tufted gland in this family. Olson & Steadman (1981) believe that Pedionomus is a charadriiform, but the tufted gland supports no specific relationship for this family. MATERIAL EXAMINED. Pedionomus torquatus 2. Family Gruidae (Cranes) MORPHOLOGY (family). Large and bilobed, papilla small with the end large and tufted (14-16 216 DAVID W. JOHNSTON feathers, Paris 1913; 32 feathers in G. grus, Jacob & Ziswiler 1982; 20 feathers in Grus, Nitzsch 1867). Gadow (1893) described the gland of Grus grus as naked, but that report was probably erroneous because of the tufted glands now known from all other species examined. Type I. Subfamily Gruinae MATERIAL EXAMINED. Grus canadensis 9 (ad. M: 3520, 0-05. Subad. M : 2360, 0-03. Ad. F: 3880, 0-05; 3560, 0-05); G. antigone 1; Anthropoides paradisea 2. Turnix suscitator Pedionomus torquatus Grus canadensis Subfamily Balearicinae MATERIAL EXAMINED. Balearica pavonina 2. Family Aramidae (Limpkin) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, tufted (14 feathers). Type I. MATERIAL EXAMINED. Aramus scolopaceus 9 (x of 6 M: 1 128-6, 0-28. F: 1300, 0-29). Family Psophiidae (Trumpeters) MORPHOLOGY. Indistinctly bilobed, papilla absent, sparse and short tuft (20 feathers). Nitzsch (1867) made the contradictory statement (p. 123), '. . . of the naked oil-gland, which is furnished with a circlet of feathers at the tip.' Type I. MATERIAL EXAMINED. Psophia crepitans 1; P. leucoptera 3. Family Rallidae (Rails, Coots, Gallinules) MORPHOLOGY (family). Distinctly bilobed, papilla usually large, tuft variable (Verheyen 19576) (1 1-17 feathers in 5 species, Jacob & Ziswiler 1982; 6 in Porphyrio) or gland naked. Miller (1924), Verheyen (1957Z>), and Ripley (1976) stated that Himantornis has a naked gland, a condition that I confirmed. Beddard (1898: 321) stated that Ralli 'have as a rule a tufted oil gland but Porzana Carolina is an exception.' Miller ( 1 924) and I each found that 5 different specimens of this species all had tufted glands. In Atlantisia rogersi 2 specimens at the British Museum had naked glands, but 2 specimens at the American Museum of Natural History and Museum of Comparative Zoology each had tufted glands. Type I. Subfamily Rallinae MATERIAL EXAMINED. Rallus longirostris 3 (F: 1 86-3, 0-23); R. elegans 3 (F: 298-0, 0-16; 372-7, 0-29); R. limicola 6 (M: 66-3, 0-34. F: 65-3, 0-09), R. owstoni 1; R. wakensis 1; Atlantisia rogersi 5; Tricholimnas sylvestris 1; Dryolimnas cuvieri 1; Rallina eurizonoides 1; Cyanolimnas cerverai 1; Gallirallus australis 2; Himantornis haematopus 1; Crecopsis egregia 1; Crex crex 1; Anurolimnas AVIAN UROPYGIAL GLAND 217 castaneiceps 2; Limmocorax flavirostra 2; Porzana Carolina 5 (M: 66-9, 0-15. F: 65-9, 0-22); P. albicollis 1; Porzanula palmeri 2; Later allus albigular is 1; Micropygia schomburgkii 1; Coturnicops noveboracensis 1; Sarothrura rufa 1; Poliolimnas cinerus 1; Tribonyx mortierii 1; Amaurornis phoenicurus 1 ; Gallicrex cinerea 1 ; Gallinula chloropus 8 (M: 364-2, 0- 1 1 ; 21 1 -5, 0-23. x of 4 F: 274-3, 0-18; Porphyriornis nesiotis 1; P. comeri 1; Porphyrula alleni 1; P. martinica 4 (F: 203-6, 0-16); Porphyrio porphyrio 1, P . poliocephalus 1; Notornis mantelli 1. Aramus scolopaceus Psophia leucoptera Porphyrio porphyrio Subfamily Fulicinae MATERIAL EXAMINED. Fw//ca americana 8 (M: 625-0, 0-1 1. F: 395-4, 0-16; 386-5, 0-17). Family Heliornithidae (Sun-Grebes) MORPHOLOGY. Broad and bilobed, papilla moderately developed, tufted (16 feathers). Type I. MATERIAL EXAMINED. Podica senegalensis 1; Heliopais per sonata 1; Heliornisfulica 1. Family Rhynochetidae (Kagu) MORPHOLOGY. Apparently single-lobed, indistinct papilla, naked. The gland is not 'rudimentary' as stated by Jacob (1978: 168). MATERIAL EXAMINED. Rhynochetos jubatus 1 . Family Eurypygidae (Sun-Bittern) MORPHOLOGY. Indistinctly bilobed, papilla moderately developed, tufted (10 1-2 mm feathers). Miller (1924: 322) concluded: 'Gadow gives the oil-gland ofEurypyga as bare; Beddard states that it is generally nude but occasionally tufted. In each of my two fresh examples, . . . there was a small tuft present.' Type I. MATERIAL EXAMINED. Eurypyga helias 3. Family Cariamidae (Cariamas) MORPHOLOGY. Apparently single-lobed, papilla large, naked. The unusual shape is described by Nitzsch (1867) as distinctly 'of a conical pyriform shape.' MATERIAL EXAMINED. Cariama cristata 1 . Family Otidae (Bustards) MORPHOLOGY. Gland absent in all species examined, a condition previously noted by Nitzsch (1840), Gadow (1893), Beddard (1898), Paris (1913), Grasse (1950), Verheyen (19576) and Van Tyne & Berger (1976). Paris (1913) reported 'well marked outlines of the gland' in embryos. 218 DAVID W. JOHNSTON Heliopais per sonata Rhinochetosjubatus Eurypyga helias MATERIAL EXAMINED. Choriotis kori 2; C. australis 1 ; Lophotis ruficrista 1 ; Eupodotis senegalensis 2; Lissotis melanogaster 1 . Order Charadriiformes Gland characteristics. Heavily tufted. NOTE. 1 0 families were described by Verheyen ( 1 9586) as being tufted. All individuals of 1 6 families in the present study had tufted glands. Type I. Family Jacanidae (Jacanas) MORPHOLOGY. Bilobed, papilla moderately developed (contra 'without a well-developed nipple' Verheyen \951d), tufted (12 feathers). MATERIAL EXAMINED. Jacana spinosa 2. Family Rostratulidae (Painted Snipe) MORPHOLOGY. Bilobed, papilla indistinct, tufted (12 feathers). MATERIAL EXAMINED. Rostratula benghalensis 1 . Cariama cristata Jacana spinosa Rostratula benghalensis AVIAN UROPYGIAL GLAND 219 Family Haematopodidae (Oyster-catchers) MORPHOLOGY. Bilobed, papilla small, tufted (28 feathers, Jacob & Ziswiler 1982). MATERIAL EXAMINED. Haematopus ostralegus 2. Family Charadriidae (Lapwings, Plovers) MORPHOLOGY (family). Distinctly bilobed, papilla moderately developed, tufted (12-24 feathers, Paris 1913; 1 2-1 4 feathers, Jacob & Ziswiler 1982). Subfamily Vanellinae MATERIAL EXAMINED. Vanellus vanellus 2; Hoplopterus spinosus 2; Hoploxypterus cay anus 1; Zonifer tricolor 1 . Subfamily Charadriinae MATERIAL EXAMINED. Squatarolasquatarola2(M: 205-3,0-22. F: 216-2,0-14); Charadrius hiaticula \ ; C. vociferus 4 (F: 92-0, 0-08; 94- 1 , 0-07); Eupoda montana 1 . Family Scolopacidae (Woodcock, Sandpipers) MORPHOLOGY (family). Distinctly bilobed, papilla small, tufted (12-24 feathers in 4 species, Jacob & Ziswiler 1982). Subfamily Tringinae MATERIAL EXAMINED. Bartramia longicauda 1; Numenius minutus 1; Tringa totanus 1; Actitis macularia 2 (F: 28-5, 0-12); Catoptrophorus semipalmatus 5 (M:297-8, 0-19). Haematopus ostralegus Charadrius vociferus Catoptrophorus semipalmatus Subfamily Arenariinae MATERIAL EXAMINED. Arenaria interpres 5. Subfamily Scolopacinae MATERIAL EXAMINED. Limnodromus scolopaceus 8 (x of 4M: 104-2, 0- 1 8. F: 121 • 1, 0-20); L. griseus 6 (F: m-9,Q-\2;S5-2,Q-\2y,Capellagallinago3(F: 101-5, 0-09); Philohela minor 5 (M: 106-0, 0-09.X of4F: 179-2,0-09). Subfamily Eroliinae MATERIAL EXAMINED. Calidris canutus 2 (M: 94-5, 0-08); Crocethia alba 2 (F; 49-9, 0-07); Ereunetes pusillus 2; Erolia minutilla 1; E.fuscicollis 1; E. alpina 2. 220 DAVID W. JOHNSTON Family Recurvirostridae (Avocets, Stilts) MORPHOLOGY. Bilobed, papilla small, tufted (ca 20 feathers). MATERIAL EXAMINED. Himantopus himantopus 3; Recurvirostra americana 1 (F: 289-4, 0-20). Family Phalaropodidae (Phalaropes) MORPHOLOGY. Distinctly bilobed, papilla small, tufted. MATERIAL EXAMINED. Phalaropusfulicarius 4 (unsexed: 40-5, 0-62; 40-4, 0-53. F: 42-0, 0-79); Lobipes Family Dromadidae (Crab-plovers) MORPHOLOGY. Distinctly bilobed, papilla apparently absent, tufted (16 feathers). MATERIAL EXAMINED. Dromas ardeola 1 . Himantopus himantopus Phalaropusfulicarius Dromas ardeola Family Burhinidae (Thick-knees) MORPHOLOGY. Indistinctly bilobed, broad papilla, tufted (14 feathers in B. oedicnemus, Jacob & Ziswiler 1982). MATERIAL EXAMINED. Burhinus oedicnemus 1; B. senegalensis 1; Esacus recurvirostris 1. Family Glareolidae (Pratincoles, Coursers) MORPHOLOGY (family). Indistinctly bilobed, large and round papilla, tufted (14 feathers). Subfamily Cursoriinae MATERIAL EXAMINED. Cursorius cursor 1 . Subfamily Glareolinae MATERIAL EXAMINED. Stiltia Isabella 1; Glareola pratincola 1. Family Thinocoridae (Seed-snipe) MORPHOLOGY. Indistinctly bilobed, papilla moderately developed, tufted (16 feathers). NOTE. Based upon comparisons of gland morphologies, the present study confirms the belief of Sibley et al. (1968: 243) that seed-snipe 'are more like ... the Charadriiforms than any other group.' MATERIAL EXAMINED. Thinocorus orbignyianus 1; T. rumicivorus 1. AVIAN UROPYGIAL GLAND 221 Burhinus oedicnemus H h Cursorius cursor Thinocorus rumicivorus Family Chionididae (Sheath-bills) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, tufted (16-18 feathers, Paris 1913). MATERIAL EXAMINED. Chionis alba \ . Family Stercorariidae (Skuas, Jaegers) MORPHOLOGY. Distinctly bilobed, papilla apparently absent, tufted. MATERIAL EXAMINED. Stercorarius pomarinus 2 (F: 616-0, 0-37); S. Iongicaudus4(ad M: 333-9, 0-23. Subad.F: 271-5, 0-28). Chionis alba Stercorarius pomarinus Larus atricilla 222 DAVID W. JOHNSTON Family Laridae Subfamily Larinae (gulls) MORPHOLOGY. Distinctly bilobed and broad (see also Verheyen 1954a), papilla moderately devel- oped, tufted (18-26 feathers in 4 species, Paris 1913; 22-29 feathers, Jacob & Ziswiler 1982). MATERIAL EXAMINED. Larus delawarensis 5 (ad. M: 330-0, 0- 1 5. Ad. F: 440-0, 0- 1 3); L. atricilla 8 (ad. M: 368-5, 0-29. Ad. F: 320-0, 0-20); L. Philadelphia 2 (ad. F: 179-8, 0-21); Rissa tridactyla 2. Subfamily Sterninae (Terns) MORPHOLOGY. Similar to Larinae except gland is more compact (see figures); 6-8 feathers in 4 species, Jacob & Ziswiler 1982. MATERIAL EXAMINED. Chlidonias nigra 2; Hydroprogne caspia (tschegrava of Peters) 4 (F: 686-0, 0'\%;69S-Q,Q-1S); Sterna hirundo 9 (M: 117-4,0-26. F: 137-7,0-33); S. paradisea 2 (M: 110-9,0-16); S.forsteri4(F: 147-0, 0-33); S. anaethetus 6 (M: 130-0, 0-43; 135-0, 0-31); S.fuscata 8 (M: 218-0, 0-29; 218-6, 0-25. F: 141-0,0-38; 156-0,0-35; 174-0, 0-38); S. albifrons 5 (M: 46-1, 0-46; 51-3, 0-57); Thalasseus maximus 1 (M: 385-9, 0-35. F: 353-2, 0-26); T. sandvicensis 3; Larosterna inca 2 (M, Z: 153-3, 0-21); Anous stolidus 4\ Gygis alba 2 (M: 117-9, 0-43; 113-3, 0-47). Family Rynchopidae (Skimmers) MORPHOLOGY. Bilobed, papilla broad and apparently double, densely tufted (24 feathers). MATERIAL EXAMINED. Rynchops niger 6 (M: 211-4, 0-20). Family Alcidae (Auks, Murres, Puffins) MORPHOLOGY. Elongated and bilobed, papilla moderately developed, tufted (Verheyen \958d; 30-50 feathers, Paris 1913; 2-8 (sic?) feathers, Jacob & Ziswiler 1982; 20-40, present study). MATERIAL EXAMINED. Plautus alle 2; Pinguinus impennis (mounted bird) 1 ; Uria lomvia 1 ; U. aalge 1 ; Cepphus grylle 1 (F: 363-0, 0-22); C. columba 3 (M: 380-0, 0-18. F: 371-5, 0-19); Synthliboramphus antiquus 2 (M: 180-5, 0-25); Ptychoramphus aleuticus 2 (F: 207-9, 0-47); Aethia cristatella 1; Cerorhinca monocerata 2 (M: 631-5, 0-31); Lunda cirrhata 2 (F: 673-5, 0-30; 792-4, 0-20). Sterna fuscata Rynchops niger Lunda cirrhata AVIAN UROPYGIAL GLAND 223 Order Columbiformes Gland characteristics. Naked or absent. Family Pteroclididae (Sand-grouse) MORPHOLOGY. Indistinctly bilobed, papilla broad and well developed, naked. MATERIAL EXAMINED. Syrrhaptes paradoxus 1; Pterocles namaqua 1; P. decoratus 1; P. lichtensteinii 1 . Family Columbidae (Pigeons and Doves) Subfamily Treroninae (Fruit pigeons) MORPHOLOGY. Absent or, when present, indistinctly bilobed, papilla large, naked. MATERIAL EXAMINED. Sphenurus apicauda 1 *; S1. oxyura 1 *; Treron curvirostra 2*; T. pompadora 2*; T. olax 1*; T. vernans 2*; T. bicincta 1*; T. s. thomae 1*; T. australis 1*; T. calva 1*; T. waalia 1*; Phapitreron leucotis 2; P. amethystina 1; Leucotreron occipitalis 1; Ptilinopus** dupetithouarsii 1; P. regina 1; P. insular is 1*; P. raratongensis 1; P. huttoni 1; P. porphyraceus 1; P. greyii 1; P. richardsii 1; P. perousii 1; P. superbus 3; P. pulchellus 2*; P. coronulatus 2*; P. monacha 1; P. iozonus 1 *; P. r/vo// 3*; P. eugeniae 1 *; P. hypogastra 1 *; P.jambu 1 ; P. aurantiifrons 1 ; P. ornatus 2; P. tannensis 1*; Chrysoena victor 1*; Alectroenas pulcherrima 1; ,4. madagascariensis 2; Megaloprepia magnified 1 *; Ducula oceanica 1 ; Z). pacifica 1 ; Z). #e«eo 1 ; Z). bicolor 1 ; Z). spilorrhoa 1; Z). fow//'0 1*; Z). rufigaster 1; Z). zoeae 1*. Subfamily Columbinae (Pigeons, Doves) MORPHOLOGY. Except for some individuals or varieties ofColumba livia, the gland is present in all genera and species of Columbinae thus far examined. Indistinctly bilobed, papilla large, naked. Reported by Beddard (1898) as absent in Ptilopaspuella( = Columbapuella of Peters), Starnoenas (also absent fide Garrod 1874#), and Turacoena, all genera and species unavailable for the present study. MATERIAL EXAMINED. Columba livia^ 2 (M: 268-0, 0-05. F: 312-8, 0-08); C. palumbus 1; C. leuco- cephala 3 (F: 205-2, 0-10; 264-0, 0-05); C. guinea 1; C. fasciata 1; Macropygia unchall 1; M. amboiensis 2; M. ruficeps 1 ; M. phasianella \ ; M. nigrirostris 2; Ectopistes migratoria 2; Zenaidura macroura 8 (M: 123-0, 0-01; 134-4, 0-03; 105-7, 0-02. F: 123-4, 0-01; 117-1, 0-03); Z. auriculata 1; Zenaida asiatica 1 (M : 1 73 -2, 0-02); Nesopeliagalapagoensis 1 ; Streptopelia orientalis 1 ; S. capicola 1 ; S. senegalensis 3; Geopelia humeralis 1; G. striata 2; G. cuneata 1; Metriopelia melanoptera 1; M. aymara 1; Scardafella inca 1; Columbigallina passer ina 1 (F: 41-5, 0-02); C. talpacoti 1; C. minuta 1; Claravispretiosa 3; Oena capensis 6; Turtur afer 1 ; T. chalcospilos 2; Chalcophaps indica!>; C. stephani 1; Henicophaps albifrons 1; Phaps chalcoptera 1; Ocyphaps lophotes 3; Lophophaps ferruginea 1; Geophaps smithii 2; Aplopelia larvata \; A. simplex 1; Leptotila verreauxi 1; L. ruf axilla 1; L. plumbeiceps 3; L. cassini 5;Oreopelia caniceps 1 ; Geotrygon versicolor 1 ; Gallicolumba luzonica 1 ; G. beccarii 1; G. rubescens 2; Otidiphaps nobilis 1; Caloenas nicobarica 2. Subfamily Gourinae (Crowned Pigeons) MORPHOLOGY. Absent MATERIAL EXAMINED. Gowra cristata 1; G. scheepmakeri 1; G. victoria 1. Subfamily Didunculinae (Tooth-billed Pigeons) MORPHOLOGY. Absent. Jacob & Ziswiler (1982) reported a gland in 2 specimens of Didunculus, an inexplicable difference from the present and all previous reports (Newton 1893-1896, Beddard 1898,Verheyenl957tf). MATERIAL EXAMINED. Didunculus strigirostris 3. *gland absent, present study; absent in Treron (Garrod 1 8740). Jacob & Ziswiler ( 1 982 and V. Ziswiler in litt.) found glands in adult Treron pompadora, T. vernans, T. waalia. **gland 'very small in Ptilinopus' fide Garrod 1874a. tabsent in some varieties such as Fantail, Oriental, Roller, Maltese, White Carneau (Darwin 1900, Johansson 1927, Levi 1941,Verheyenl957a). 224 DAVID W. JOHNSTON Order Psittaciformes* Gland characteristics. Tufted or absent. Family Psittacidae (Lories, Parrots, Macaws) Subfamily Strigopinae (Owl Parrots) MORPHOLOGY. Distinctly bilobed, papilla large, tufted. MATERIAL EXAMINED. Strigops habroptilus 1. Subfamily Nestorinae (Keas) MORPHOLOGY. Distinctly bilobed, papilla well developed, tufted (13 feathers, Jacob & Ziswiler 1982). MATERIAL EXAMINED. Nestor notabilis 3. Subfamily Loriinae (Lories) MORPHOLOGY. Distinctly bilobed, papilla large, tufted (5-8 feathers in 3 species, Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Chalcopsitta atra 1; Eos cyanogenia 1; E. squamata 1; E. bornea 3; Trichoglossus ornatus 1; T. haematodl; T. chlorolepidotus 1; Psitteuteles Johns toniae 1; Domicella garrula 3; Vini stepheni 1; Glossopsitta porphyrocephala 1; Charmosyna josefinae 1; C. papou 1; Oreopsittacus arfaki 1 ; Neopsittacus musschenbroekii 1 . Subfamily Micropsittinae (Pigmy Parrots) MORPHOLOGY. Distinctly bilobed, papilla large, tufted (3-4 feathers, Jacob & Ziswiler 1982). MATERIAL EXAMINED. Micropsitta pusio 1. Subfamily Kakatoeinae (Cockatoos) MORPHOLOGY. Absent or when present, distinctly bilobed, papilla large, tufted (4-8 feathers in 2 species, Jacob & Ziswiler 1982). NOTE. Newton (1893-1896: 653) stated that the gland 'exists, though hardly in a functional con- dition, in ... Cacatua cristata (Cockatoo) . . .' =Kakatoe sulphured citrino-cristata of Peters. Nitzsch (1867), Garrod 18746, Gadow (1893), and Grasse (1950), noted no gland in Cacatua sulfurea and its absence in C. roseicapella was reported by Paris (1913). I found that specimens of both of these species had tufted glands. P (erodes lichtensteinii Zenaidura macroura Ara chloroptera "many zoo and captive birds. AVIAN UROPYGIAL GLAND 225 MATERIAL EXAMINED. Probosciger aterrimus 4f; Calyptorhynchus baudinii 1; Callocephalon fimbriatum 2; Kakatoe galerita 7; K. sulphured 4; K. alba 3; K. moluccensis 1; K. haematuropygia 1; K. leadbeateri 1; K. sanguinea 1; K. tenuirostris 1; /T. roseicapella 3; Nymphicus hollandicus 4. Subfamily Psittacinae (Macaws, Parrots) MORPHOLOGY. Distinctly bilobed, papilla large, tufted (12 feathers, Paris 1913; 3-1 1 feathers in 33 species, Jacob & Ziswiler 1982) or gland absent. Type I. NOTE. Miller ( 1 924: 324) reported no gland in Orthopsittaca and Diopsittaca ( = Ara of Peters), but listed no species. Jacob (1978: 168) stated that the gland is absent in Ara but indicated on species. MATERIAL EXAMINED. Anodorhynchus hyacinthus 5*; A. leari 1 *; Ara** ararauna 2; A. militaris 2; A. macao 4 (F, Z: 996-5, 0-05); A. chloroptera 3; A. auricollis 1; A. severa 1; A. manilata 3*; Aratinga acuticaudata 1; A. guarouba 1; A. leucophthalmus 1; A. holochlora 1; A.jandaya 1; A. solstitialis 2; A. canicularis 1; A. aurea 2; Nandayus nanday 1; Conuropsis carolinensis 1; Rhynchopsitta pachyrhyncha 1; Cyanoliseus patagonus 1; Pyrrhura rhodogaster 1; P. molinae 1; P. hoffmanni 1; Myiopsitta monachus 1; Psilopsaigon aurifrons 1; Forpus conspicillatus 1; Brotogeris tirica I*; B. versicolurus 2*; 5. pyrrhyopterus 1*; B. jugularis 2*; 5. cyanoptera 2*; fi. chrysopterus 4*; 5. s/. thoma 1*; Pionites melanocephala 2; Graydidascalus brachyurus 2*; Pionus*** menstruus 2*; P. maximiliani 1*; P. senilis 1*; P. chalcopterus 1*; Amazona leucocephala \*\ A. ventralis \*\ A. xantholora 1*; ^4. albifrons 1*; .4. ag//w 1*; ^4. vittata 1*; /I. viridigenalis 1*; ,4. autumnalis 1*; ,4. barbadensis 1*; ,4. aestiva 1*; ^4. ochrocephala 3*; ^4. amazonica 1*; A.farinosa 1*; /I. vinacea 1*; y4. guildingii 1*; A imperialis 2*; Triclaria malachitacea 1; Poicephalus senegalus 2; P. meyeri 1; P. ruppellii 2; Psittacus erithacus 1; Coracopsis nigra 1; Psittrichas fulgidus 1; Lorius roratus 1; Prioniturus discurus 1; Psittacula krameri 5; P. alexandri 1; P. cyanocephala 1; Polytelis swainsonii 2; P. alexandrae 2; Aprosmictus erythropterus 3; Psittinus cyanurus 2; Agapornis roseicollis 2; ^4. fischeri \; A. lilianae 3; Loriculus vernalis 1; Platycercus elegans 1; P. eximius 3; P. icterotis 2; P. zonarius 2; Psephotus haematonotus 3; P. varms 3; Neophema elegans 3; TV. chrysostomus 1; TV. petrophila 1; TV. pulchella 7; TV. splendida 3; TV. bourkii 6; Cyanoramphus auriceps 2; Melopsittacus undulatus 1 . Order Cuculiformes Gland characteristics. Tufted or naked. Family Musophagidae (Plantain-eaters) MORPHOLOGY. Flattened and distinctly bilobed, papilla moderately developed, tufted (8 feathers). Verheyen (19566) was evidently in error when he noted (p. 2) that touracos have a naked gland. Type I. MATERIAL EXAMINED. Tauraco corythaix 1; J1. leucolophus 1; Gallirex porphyreolophus 1; Musophaga violacea 3; Crinifer leucogaster 1; C. africanus 2. Family Cuculidae (Cuckoos, Roadrunner, Anis) MORPHOLOGY (family). Flattened and more or less distinctly bilobed, papilla large and often appearing double, naked. Subfamily Cuculinae MATERIAL EXAMINED. Clamator glandarius 1; Cuculus canorus 1; Cacomantis merulinus 1; Chrysococcyx cupreus 1 ; C. fc/aas 1 ; C. caprius 9; Chalcites basalts 1 . tgland absent, this study and Beddard (1898). *gland absent, present study; Jacob & Ziswiler (1982, V. Ziswiler in litt.) found a gland in adult Pionus fuscus. **gland present in /I. ambigua and maracana (fide Garrod 18746). ''gland also absent in P. sordidus (fide Garrod 1 8746). *** 226 DAVID W. JOHNSTON Subfamily Phaenicophaeinae MATERIAL EXAMINED. Coccyzus americanus 4 (unsexed: 46-7, 0-09); Piaya cayana 2; Saurothera vetula 2; Ceuthmochares aereus 1; Rhopodytes diardi 1; R. tristis 2; Rhamphococcyx curvirostris 2; Dasylophus super ciliosus 1 . Subfamily Crotophaginae (Anis, Guiras) MATERIAL EXAMINED. Crotophaga ani 3 (M: 113-9, 0-03); C. sulcirostris 7; Guiraguira 1. Subfamily Neomorphinae (Roadrunners, Ground Cuckoos). MATERIAL EXAMINED. Taper a naevia 1 ; Morococcyx erythropygus 2; Geococcyx californiana 3. Subfamily Couinae (Couas) MATERIAL EXAMINED. Coua cristata \ . Subfamily Centropodinae (Coucals) MATERIAL EXAMINED. Centropus viridis 2; C. toulou 1; C. benegalensis 2. Order Strigiformes Gland characteristics. Naked or minutely tufted. NOTE. Glands of various strigiform species have usually been described as 'naked' or 'nude' (Gadow 1893, Beddard 1898, Jacob & Ziswiler 1982). Nitszch (1840), Miller (1924), and I used magnification and identified 1 to 12 'rudimentary,' 'vestigial,' or 'minute' feathers on the papilla's tip in some individual specimens. Family Tytonidae (Barn Owls) Subfamily Tytoninae MORPHOLOGY. Indistinctly bilobed, papilla moderately developed, tufted with minute feathers (1 or 2 5-mm feathers) or naked. Nitzsch (1867: 71) noted minute feathers on the papilla's apex in Strix flammea, S. perlata, and S.furcata (all = Tyto alba). Type I. MATERIAL EXAMINED. Tyto alba 7* (M: 502-0, 0-07; 490-0, 0-04. F: 530-0, 0-12; 488-4, 0-11). Subfamily Phodilinae MORPHOLOGY. Like Tytoninae. Nitzsch (1867: 71) reported minute feathers at the gland apex in Strix badia ( = Phodilus badius), but none were seen on 3 specimens in the present study. MATERIAL EXAMINED. Phodilus badius 3. Tauraco corythaix Saurothera vetula Tyto alba •minute feathers in 3 specimens. AVIAN UROPYGIAL GLAND 227 Family Strigidae (Typical Owls) MORPHOLOGY (family). More superficial than in any other avian family, appearing to lie on top of the skin ('almost standing up,' Paris 1913: 180), bilobed, papilla large, tufted (up to 10 1-mm minute feathers) or naked. Type I. Subfamily Buboninae MATERIAL EXAMINED (naked unless otherwise indicated). Otus spilocephalus It; O. scops 1; O. bakkamoena 1; O. asio 26ft, ttt (M: 103-2, 0-07; 107-7, 0-08. F: 149-3, 0-07; 108-4, 0-11); O. trichopsis It; O. guatemalae If; O. choliba If, ttt; O. watsonii 1; O. leucotis 1; Lophostrix cristata 2; Bubo virginianus 8ftt (M: 1207-0, 0-04; 1407-0, 0-04. F: 1887-0, 0-04; 1670-0, 0-03); B. bubo 1; B. africanus Ittt; B. lacetus Ittt; Ketupa^ketupu 1; Pulsatrix perspicillata Ittt; Nyctea scandiaca 2ftt; Surnia ulula 3 (M: 310-0, 0-07. F: 355-7, 0-04); Glaucidium brasilianum 2; G. brodiei 1; Micrathene whitneyi \\Ninoxnovaeseelandiae Ittt 5 N.philippensis 1; Athene noctual; A. brama 1; Speotyto cunicularia 4; Ciccaba virgata It; C. nigrolineata 1; C. woodfordii \. Subfamily Striginae MATERIAL EXAMINED (naked unless otherwise indicated): Strix aluco 1*; S. varia 20**, **** (M: 762-9, 0-09. x of 9 F: 775-4, 0-07); S. nebulosa 1*; Rhinoptynx clamator 1; Asio otus 5***, **** (F: 306-0, 0-09); A. madagascariensis 1*; A.flammeus 3*****; Pseudoscops grammicus 1; Aegolius acadicus5(M:91-l,Q-\Q). Order Caprimulgiformes Gland characteristics. Naked or rarely absent. Family Steatornithidae (Oil-bird) MORPHOLOGY. Indistinctly bilobed, papilla large, naked (first reported by Garrod 1873). Described by Paris (1913: 177) and Newton (1893-1896: 653) as 'large.' (See section on Weights and sizes of glands.) MATERIAL EXAMINED. Steatornis caripensis 1 . Family Podargidae (Frogmouths) MORPHOLOGY. Podargus — absent (see also Gadow 1893, Verheyen 19560, Grasse 1950, Miller 1924). Batmchostomus — indistinctly bilobed, papilla large, naked. The implication by Van Tyne & Berger (1976) that the gland is absent in (all) Podargidae is incorrect. MATERIAL EXAMINED. Podargus strigoides 2; P. papuensis 1; P. ocellatus 2; Batrachostomus auritus 1; B. septimus 2; B. stellatus 1; B.javensis 1. Family Nyctibiidae (Potoos) MORPHOLOGY. Very small, indistinctly bilobed, papilla large, naked. NOTE. Miller (1924: 324) reported 'the loss of the oil-gland' in Nyctibius. MATERIAL EXAMINED. Nyctibius griseus 3. tminute tuft, present study. ttminute tuft, up to 8 1-mm feathers in 8 specimens. ttfsome specimens with minute tuft fide Miller (1924: he also reported tufts in Ketupa zeylonensis, Bubo bubo, Gymnoglaux lawrencii). minute tuft, present study. *minute feathers in 6 specimens. **minute feathers in 3 specimens. ***some specimens with minute tuft (Nitszch 1840, Beddard 1898, Miller 1924, or Verheyen 1956a). ****'one or 2 very small white feathers,' Paris 1913: 182. 228 DAVID W. JOHNSTON Asioflammeus Steatornis caripensis Batrachostomus septimus Family Aegothelidae (Owlet-nightjars) MORPHOLOGY. Broad, flattened and bilobed, papilla large, naked. MATERIAL EXAMINED. Aegotheles insignis 1. Family Caprimulgidae (Nighthawks, Goatsuckers) MORPHOLOGY (family). Very small not apparently bilobed (see also Paris 1913: 173), papilla large, naked. I did not confirm the report by Arnall & Keymer (1975) that the gland is absent 'in nightjars.' Subfamily Chordeilinae (Nighthawks) MATERIAL EXAMINED. Lurocalis semitorquatus 1; Chordeiles minor 6 (M: 64-8, 0-01; 67-5, 0-01. F: 75-4, 0-01; 87-5, 0-01; 79-6, 0-01); Podager nacunda 2. Subfamily Caprimulginae (Goatsuckers) MATERIAL EXAMINED. Eurostopodus macrotis 1 ; Nyctidromus albicollis 4; Phalaenoptilus nuttallii 2; Otophones yucatanicus 1; Caprimulgus carolinensis 10 (M: 113-0, 0-01; 80-7, 0-01; 124-8, 0.01. x of 4 F: 1 14-2, 0-01); C. vociferus 2 (M: 55-5, 0-02. F: 52-5, 0-02); Scotornis climacurus 1; Semeiophorus vexillarius 1 ; Hydropsalis brasiliana 1 . Nyctibius griseus Aegotheles insignis Podager nacunda AVIAN UROPYGIAL GLAND 229 Order Apodiformes Gland characteristics. Naked. NOTE. The reference by Elder (1954) and Pettingill (1985) to gland absence in 'certain species' of Apodiformes was unsubstantiated by me. Family Apodidae (Swifts) MORPHOLOGY (family). Indistinctly bilobed, papilla moderately developed, naked. Subfamily Chaeturinae (Spine-tailed Swifts) MATERIAL EXAMINED. Collocalia inexpectata 1; C. vanikorensis 1; Hirund-apus giganteus 2; Streptoprocne zonaris 1; Chaetura pelagica 3; C. rutilus 1 . Subfamily Apodinae (Typical Swifts) MATERIAL EXAMINED. Apus apus 1 ; Aeronautes saxatalis 1 ; Reinarda squamata 1 ; Cypsiurus parva 1 . Family Hemiprocnidae (Crested Swifts) MORPHOLOGY. Indistinctly bilobed, papilla absent, naked. MATERIAL EXAMINED. Hemiprocne mystacea 1 ; H. comata 1 . Family Trochilidae (Hummingbirds) MORPHOLOGY. Distinctly bilobed with lobes greatly separated, papilla large, naked. MATERIAL EXAMINED. Glaucis hirsuta 1 ; Phaethornis superciliosus 2; P. eurynome 1 ; P. longuemareus 2; Eutoxeres condamini 2; Phaeochroa cuvierii 2; Campylopterus curvipennis 8; C. hemileurcurus 1 ; C. ensipennis 1 ; Eupetomena macroura 1 ; Florisuga mellivora 1 ; Colibriserrirostris 1 ; Anthracothorax nigricollis 1 ; Chrysolampis mosquitus 1 ; Stephanoxis lalandi 1 ; Chlorestes notatus 1 ; Thalurania furcata 1; Hylocharis chrysura 1; Chrysuronia oenone 1; Leucochloris albicollis 1; Amazilia Candida \\A. versicolor \;A. cyanocephala \;A. rutila \;A. tzacatl 1 3; Patagona gigas 1 ; Ensifera ensifera 1 ; Archilochus colubris 3; Selasphorus rufus 1 . Hirund-apus (Chaetura) Hemiprocne comata Glaucis hirsuta giganteus Order Coliiformes Gland characteristics. Tufted. Family Coliidae (Colics) MORPHOLOGY. Distinctly bilobed, papilla large, tufted. Verheyen (19566') makes the unsubstan- tiated comment that the gland of Urocolius ( = Colitis indicus and C. macrourus of Peters) is naked. Both Nitzsch (1867) and Garrod (1876) reported that the gland of Colius is tufted. Type I. MATERIAL EXAMINED. Colius striatus 4; C. colius 1 ; C. indicus 2; C. macrourus 1 . 230 DAVID W. JOHNSTON Order Trogoniformes Gland characteristics. Naked. Family Trogonidae (Trogons) MORPHOLOGY. Indistinctly bilobed, papilla large, naked. MATERIAL EXAMINED. Pharomachrus mocino 2; Priotelis temnurus 1; Temnotrogon roseigaster 1; Trogon strigilatus 1 ; T. citreola 1 ; Apaloderma marina 1 ; Harpactes erythrocephalus 1 . Patagona gigas Colius macrourus Pharomachrus mocino Order Coraciiformes* Gland characteristics. Much inter- and intrafamilial variation: naked, or sparsely to densely tufted. Family Alcedinidae (Kingfishers) Subfamily Cerylinae MORPHOLOGY. Indistinctly bilobed, papilla absent or small, tufted (16 feathers in C. alcyori). MATERIAL EXAMINED. Ceryle torquata 1; C. alcyon 6 (M: 102-5, 0-25. F: 104-5, 0-22); C. rudis 7; Chloroceryle americana 6; C. aena 4. Subfamily Alcedininae MORPHOLOGY. Like Cerylinae (12 feathers, Paris 1913, Jacob & Ziswiler 1982). MATERIAL EXAMINED. Alcedo atthis \;A. meninting \;A. euryzona 1; A. leucogaster 1; Ispidina picta 1; /. madagascariensis 1; Ceyx argentatus 1; C. azureus 1; C. erithacus 1 . Subfamily Daceloninae MORPHOLOGY. Indistinctly or distinctly bilobed, papilla absent (Pelargopsis) to large (Tanysiptera}, tufted (small in Lacedo, large in Halcyon) or gland naked (Tanysipterd) (12 feathers in Dacelo}. Tanysiptera species apparently have no distinctive ecological or behavioral traits that might be correlated with the unusual naked gland condition (Fry 1980). Type I. MATERIAL EXAMINED. Pelargopsis capensis 1; Lacedo pulchella 2; Dacelo novaeguineae 3; D. leachii 1; Clytoceyx rex 1; Melidora macrorrhina 1; Halcyon coromanda 1; H. smyrnensis 1; H. pileata 1; H. senegalensis 1; H. malimbica 1; H. albiventris 1; H. macleayii 1; H. cinnamomina 1; H. chloris 1; Tanysiptera galatea 2; T. sylvia 1 . Family Todidae (Todies) MORPHOLOGY. Indistinctly bilobed, papilla large, tufted (6 feathers in T. subulatus). Nitzsch (1867: 88) erroneously stated that Todus has a naked oil-gland, a point corrected by Forbes (1 882). Type I. MATERIAL EXAMINED. Todus angustirostris 1; T. subulatus 2. "morphology reported here is, with exceptions noted below, consistent with the descriptions in Verheyen (1955, a, b, c). AVIAN UROPYGIAL GLAND 231 Family Momotidae (Motmots) MORPHOLOGY. Flattened and distinctly bilobed with lobes widely divergent, papilla moderately to well developed, minutely tufted or naked. Much difference of opinion is found in the literature concerning the feathered condition of glands in this family probably because some investigators failed to use magnification in their examinations of glands. By combining here the comments of Garrod ( 1 878), Forbes ( 1 882), Newton ( 1 893-1 896), Beddard ( 1 898), Miller ( 1 9 1 5), and Verheyen ( 1 955fl) plus microscopic examinations in the present study, it is apparent that any specimen of any species might have a gland that is naked or one that is tufted with 1-8 'vestigial,' 'rudimentary,' or very small feathers (ca. 1 mm). Type I. MATERIAL EXAMINED. Hylomanes momotula 1 ; Electron platyrhynchum 1 ; Eumomota super ciliosa 5; Baryphthengus ruficapillus 3; Momotus momota 5. Dacelo novaeguineae Todus subulatus Momotus momota Family Meropidae (Bee-eaters) MORPHOLOGY. Indistinctly bilobed, papilla large, naked (also reported by Paris 1913: 175). MATERIAL EXAMINED. Melittophagus pusillus 1 ; Merops apiaster 2; M. viridis 1 ; Nyctyornis amicta 1 . Family Leptosomatidae (Cuckoo-rollers) MORPHOLOGY. Indistinctly bilobed, papilla large, naked. The gland, about 10 mm in length, does not conform to Nitzsch's description of 'atrophy and almost total disappearance . . .' (1867:161). MATERIAL EXAMINED. Leptosomus discolor 2. Family Coraciidae (Rollers) MORPHOLOGY (family). Flattened and indistinctly bilobed, papilla large, naked. Subfamily Brachypteraciinae MATERIAL EXAMINED. Brachypteracias leptosomus 1; Uratelornis chimaera 1. Subfamily Coraciinae MATERIAL EXAMINED. Coracias garrulus \\Eurystomusorientalis 1. Merops apiaster Leptosomus discolor Coracias garrulus 232 DAVID W. JOHNSTON Family Upupidae (Hoopoes) MORPHOLOGY. Distinctly bilobed with widely diverging lobes, papilla large, tufted (10 feathers, Paris 1913, Grasse 1950; 14 feathers, Jacob & Ziswiler 1982). Type I. MATERIAL EXAMINED. Upupa epops 2. Family Phoeniculidae (Wood-hoopoes) MORPHOLOGY. Small and not apparently bilobed, papilla large, tufted (10 feathers). Type Ha. MATERIAL EXAMINED. Phoeniculus purpureus 1 ; P. bollei \ ; Rhinopomastus minor 1 ; R. cyanomelas 1 . Family Bucerotidae (Hornbills) MORPHOLOGY. Distinctly bilobed (lobes completely separated), papilla small, tufted (50 feathers, Paris 1913; 32-48 feathers in T. erythrorhynchus, Jacob & Ziswiler 1982). In Tockus hartlaubi the gland and its feather tuft are 'vestigial' (Verheyen \955a). Type II. MATERIAL EXAMINED. Tockus alboterminatus 1; T. erythrorhynchus 1; T.flavirostris 1; T. deckeni 1; Aceros undulatus 1 ; A.plicatus 1 ; Anthracoceros malabaricus \;A. coronatus 1 ; Ceratogymna atrata 1; Buceros bicornis 1; B. hydrocorax 1; Bucorvus abyssinicus 2. Upupa epops Phoeniculus purpureus Tockus erythrorhynchus Order Piciformes Gland characteristics. Much inter- and intrafamilial variation: absent (rarely), naked, or sparsely to densely tufted. NOTE. Differences (see figures) in gland morphology among the six families lend evidence to a polyphyletic origin of the Piciformes as suggested by Olson (1983). Family Galbulidae (Jacamars) MORPHOLOGY. Indistinctly bilobed, papilla moderately developed, naked. MATERIAL EXAMINED. Galbalcyrhynchus leucotis 1; Brachygalba lugubris 1; Galbula albirostris 5; G. galbula 1; G. ruficauda 3; Jacamerops aurea 1 . Family Bucconidae (Puff-birds) MORPHOLOGY. Distinctly bilobed, papilla large, naked. Gadow (1893), Nitzsch (1867: 94), and Beddard (1898) each refer to some bucconids (e.g., Malacoptilafusca, Bucco, Monasa) as having glands with 'a few fine hairs at the apex' or 'feathered.' However, Miller (1915) and I found that all species and individuals in the Bucconidae that we examined had naked glands. AVIAN UROPYGIAL GLAND 233 MATERIAL EXAMINED. Notharchus macrorhynchos 3; Nystalus maculatus 1; Hypnelus bicinctus 1; Malacoptila striata 1 ; M.fusca 1 ; M. panamensis 6; Monasa nigrifrons 1 ; M. atra 1 ; M. morphoeus 1 ; Chelidoptera tenebrosa 2. Family Capitonidae (Barbels) MORPHOLOGY. Distinctly bilobed, papilla moderately developed, naked or sparsely tufted (8-12 feathers in 2 species, Jacob & Ziswiler 1982). In addition to the species marked * below, the following species were reported by Miller (1924: 323) as having naked glands: Stactolaema, Pogoniulus duchaillui, Trachyphonus cafer, and T. margaritatus. Individual differences (naked vs. tufted) have been found in Trachyphonus vaillantii, T. darnaudii, and Lybius torquatus. A feathered gland was reported for Pogonias (Lybius) by Nitzsch (1867: 93). Beddard (1898: 168) noted that (all) capitonids have feathered glands. I did not confirm the statement by Verheyen (\955b) that different species in the Capitonidae lack a gland. Type I. MATERIAL EXAMINED (tufted unless otherwise indicated). Semnornis frantzii 1; S. ramphastinus 1; Psilopogonpyrolophus 2; Megalaima rafflesii 2; M. mystacophanos 1 ; M.flavifrons 1 ; M. asiastica 1 ; M. henricii 1; M. haemacephala 1; Gymnobucco bonapartei 2*; Smilorhis leucotis 1*; Pogoniulus simplex I; P. bilineatus \;P. subsulphureus 1; Tricholaema leucomelan \*;T. diadematum 1*; Lybius guifsobalito 1*; L. leucocephalus 1*; L. dubius 2*; Trachyphonus purpuratus 1; T. vaillantii 2*; T. darnaudii 1*. Galbula ruficauda Notharchus macrorhnychos Megalaima rafflesii Family Indicatoridae (Honey-guides) MORPHOLOGY. Indistinctly bilobed, papilla moderately developed, tufted (2 feathers). Miller (1924: 323) correctly noted that the Indicatoridae are invariably tufted 'but the tuft is vestigial in Prodotiscus.' I did not confirm the statement by Verheyen (1955Z?) that different species in the Indicatoridae lack a gland. Type I. MATERIAL EXAMINED. Prodotiscus insignis 2; Indicator exilis 1; /. minor 1; /. maculatus 2; Melichneutes robustus 1 . Family Ramphastidae (Toucans) MORPHOLOGY. Distinctly bilobed, papilla poorly developed, tufted (8 feathers). Type I. MATERIAL EXAMINED. Aulacorhynchus prasinus 1 ; Pteroglossus torquatus 2 (M, Z: 1 83-3, 0- 14; 1 86-3, 0-12); Andigena hypoglauca 1; Ramphastos vitellinus 1; R. discolorus 1; R. sulfur atos \;R. swainsoni 1; R. tucanus 1; R. cuvieri 1; R. inca 1; R. toco 2. Family Picidae (Wryneck, Piculets, Woodpeckers) MORPHOLOGY (family). Absent or distinctly bilobed with widely separated lobes, papilla usually moderately developed, naked or tufted (8-12 feathers in 3 species, Jacob & Ziswiler 1982). In some *naked, present study. 234 DAVID W. JOHNSTON North American species (e.g., Dryocopus, Colaptes) each lobe narrows down to an extremely small 'band' before joining at the papilla, making dissection and removal of an intact gland difficult. Miller ( 1 924) noted the gland's absence in Campethera maculosa, permista, caroli, and nivosa, these in addition to C. cailliartii in the present study. The gland is naked in Dinopium and Gecinulus and naked or tufted in specimens of Chrysocolaptes validusfide Miller (1924). Subfamily Jynginae (Wrynecks) MORPHOLOGY. 'Well developed and clearly bilobed' (Paris 1913: 168), tufted (8 feathers, Paris 191 3). Type II. MATERIAL EXAMINED. Jynx torquilla 1 . Subfamily Picumninae (Piculets) MORPHOLOGY. Tufted. MATERIAL EXAMINED. Picumnus cirratus 1 ; Nesoctitesmicr omegas 1 ; Sasia ochracea 2; 5". abnormis 1 . Subfamily Picinae (Woodpeckers) MORPHOLOGY. Tufted, naked, or absent. Type I. MATERIAL EXAMINED (tufted unless otherwise indicated). Colaptes auratus 1 (M: 100-9, 0-12. F: 131-9, 0-12; 137-7, 0.11; 98-5, 0-12); Piculus simplex 1; Campethera punctuligera 2; C. nubica 4; C. bennettii 1; C. cailliautii 2*; C. abingoni 2; C. permista 1*; C. caroli 2**; C. nivosa 7*; Celeus flavescens 2; Micropternus brachyurus 1; Picus viridis 1; Dinopium beneghalense 2***; D.javanense 1 ***; Dryocopus pileatus 5 (M: 240-8, 0- 1 5. F: 220-8, 0- 1 2); Asyndesmus lewis 1 ; Melanerpes erythro- cephalus 2; M. carolinus 1 (M: 76-0, 0-09; 72-2, 0-14. F: 54-9, 0-12); M. aurifrons 3; M.flavifrons 1; Leuconerpes candidus 1; Sphyrapicus varius 4 (M: 43-4, 0-12; 50-3, 0-08. F: 45-5, 0-14); Trichopicus cactorum 2; Veniliornis fumigatus 2; V. passerinus 1 ; V. affinis 1 ; Dendrocopos hyperythrus 1 ; D. villosus 1 (F: 54-3, 0-11); D.pubescens 2; Picoides arcticus 1; Xiphidiopicus percussus 1; Thripias pyrrhogaster 1; Hemicircus canete 1; Blythipicus pyrrhotis 1; B. rubiginosus 1; Chrysocolaptes validus 2***; C. lucidus 8; Phloeoceastes guatemalensis 1; P. melanoleucus 1; P. leucopogon 1; P. haematogaster 1 ; Campephilus principalis 1 ; C. magellanicus 1 . NOTE. In his comprehensive study of woodpeckers of the world, Short ( 1 982) presents no ecological, structural, or behavioral information that might correlate with gland presence/absence, tufted/ naked condition in different species of Campethera, Dinopium, or Chrysocolaptes. Indicator maculatus Ramphastos toco Colaptes auratus *gland absent, this study; also absent in C. maculosa (Miller 1924). **gland present (tufted) or absent in some specimens, this study. ***gland naked, this study. Tuft is individually variable in specimens of Chrysocolaptes (Miller 1924: 324). AVIAN UROPYGIAL GLAND 235 Order Passeriformes Gland characteristics. Naked. MORPHOLOGY (order). Indistinctly or distinctly bilobed, papilla moderately or well developed, naked. Although varying slightly in shape ('kidney-vs heart-shaped'), weight, and relative length of papilla (Jacob & Ziswiler 1982), glands of all passerines have been uniformly described by all authors as being present and naked. In the present comprehensive study, representatives of all passerine families (68, Peters 1931-1986) and subfamilies were examined: 1 187 individuals of 349 genera and 482 species. Except for relative size (see Weights and sizes of glands section), I found no consistent, major morphological differences between or among any taxa. Paris (1913: 67) in his extensive study reported only slight variations in shape among at least 1 1 passerine families. Suborder Eurylaimi Family Eurylaimidae (Broadbills) Subfamily Eurylaiminae MATERIAL EXAMINED. Smithornis capensis 1 ; Eurylaimus javanicus 1 ; Psarisomus dalhousiae 1 . Subfamily Calyptomeninae MATERIAL EXAMINED. Calyptomena whiteheadi 1 . Suborder Tyranni Superfamily Furnarioidea Family Dendrocolaptidae (Wood-hewers) MATERIAL EXAMINED. Dendrocincla anabatina 8; D. homochroa 4; Sittasomus griseicapillus 4; Glyphorhynchus spirurus 10; Drymornis bridgesii 1; Dendrocolaptes certhia 7; Xiphorhynchus ocellatus 1; X. guttatus 2; X. flavigaster 3; Lepidocolaptes souleyetii 3; Campy lor hamphus trochilirostris 1 ; Family Furnariidae (Ovenbirds) MATERIAL EXAMINED. Geositta cunicularia 1; Upucerthiavalidirostris 1; Cinclodesfuscus \\Furnarius leucopus 1 ; Aphrastura spinacauda 2; Phleocryptes melanops 2; Schizoeacafuliginosa 1 ; Synallaxis albescens 1 ; S. erythrothorax 2; Poecilurus candei 1 ; P. scutatus 1 ; Asthenes hudsoni 1 ; Phacellodomus striaticollis 1; Coryphistera alaudina 2; Anumbius annumbi 2; Margarornis squamiger 1; Pseudosei- sura lophotes 2; Ancistrops strigilatus 1; Syndactyla rufosuperciliata 2; Philydor erythrocercus 1; Automolus infuscatus 1; A. albigularis I; A. ochrolaemus 7; Heliobletus contaminatus 1; Xenops minuta 1 1 ; Sclerurus guatemalensis 4. Family Formicariidae (Ant-thrushes) MATERIAL EXAMINED. Taraba major 1; Thamnophilus doliatus 5; T. aethiops 1; Myrmotherula surinamensis 1 ; Microrhopias quixensis 2; Formicivora grisea 1 ; Drymophila caudata 1 ; Cercomacra tyrannina 5; C. nigricans 1; Hypocnemis cantator 1; Myrmeciza longipes 1; Formicarius colma 1; F. analis 5; Chamaeza ruficauda 1; Pithy s albifrons 1; Gymnopithys leucaspis 1; Hylophylax naevioides 1 ; Grallaria guatimalensis 1 . Family Conopophagidae (Ant-pipits) MATERIAL EXAMINED. Conopophaga lineata 1; C. castaneiceps 1; Corythopis torquata 1. Family Rhinocryptidae (Tapaculos) MATERIAL EXAMINED. Pteroptochos tarnii 1; Scelorchilus rubecula 1; Rhinocrypta lanceolata 1 ; Teledromasfuscus 1 ; Melanopareia maximiliani 1 ; Scytalopus latebricola 1 . 236 DAVID W. JOHNSTON Superfamily Tyrannoidea Family Tyrannidae (Tyrant Flycatchers) Subfamily Elaeniinae MATERIAL EXAMINED. Sublegatus modestus 1; Myiopagis viridicata 2; Elaenia flavogaster 3; E. pallatangae 1; Mionectes olivaceus 1; M. oleagineus 28; Leptopogon amaurocephalus 7; Oncostoma cinereigulare 8; Todirostrum sylvia 1; T. cinereum 2; Rhynchocyclus brevirostris 1; Tolmomyias sulphurescens 4; Platyrinchus cancrominus 4; P. mystaceus 4. Subfamily Fluvicolinae MATERIAL EXAMINED. Onychorhynchus coronatus 3; Terenotriccus erythrurus 1; Myiobius barbatus 2; Contopus virens 1; C. cinereus 1; Empidonax flaviventris 3; £". virescens 1; £. minimus 5; Sayornis phoebe 2; Ochthoecafumicola 1; Myiotheretes striaticollis 1; Xolmis irupero 1; Muscisaxicola sp. 1; Knipolegus aterrimus 1; Fluvicola pica 1. Subfamily Tyranninae MATERIAL EXAMINED. /J////0 spadiceus 7; Rhytipterna simplex 1; Myiarchus tuber culifer 2; Af. nuttingi 2; M. crinitus 2 (M: 42-4, 0-08); Pitangus sulphuratus 3; Megarhynchus pitangua 2; Myiodynastes bairdii 1 ; Tyrannus tyrannus 2 (F: 40-0, 0-10); T7. melancholicus \ . Subfamily Tityrinae MATERIAL EXAMINED. Pachyramphus cinnamomeus 1; Tityra semifasciata 2; r. inquistor 3. Family Pipridae (Manakins) MATERIAL EXAMINED. Schiffornis turdinus 3; Chloropipo uniformis 1; Xenopipo atronitens 1; Manacus manacus 10; Chiroxiphia lanceolata 1; Piprafilicauda 1; P. mentalis4Q; P. chloromeros 1. Family Cotingidae (Cotingas) MATERIAL EXAMINED. Ampelion rubrocristatus 1; Pipreola arcuata 1; P. chlorolepidota 1; Lipaugus vociferans 1 ; Gymnoderus foetidus 1 ; Querula purpurata 1 ; Pyroderus scutatus 1 ; Cephalopterus ornatus 1 ; Perissocephalus tricolor 1 ; Procnias nudicollis 1 ; Rupicola peruviana 1 . Family Oxyrunicidae (Sharpbills) MATERIAL EXAMINED. Oxyruncus cristatus 1 . Family Phytotomidae (Plantcutters) MATERIAL EXAMINED. Phytotoma rutila 1 . Family Pittidae (Pittas) MATERIAL EXAMINED. P/fte erythrogaster 1; P. granatina 1. Family Philepittidae (Asitys) Subfamily Philepittinae MATERIAL EXAMINED. Philepitta castanea 1 . Subfamily Neodrepanidinae MATERIAL EXAMINED. Neodrepanis coruscans 1. Family Acanthisittidae (New Zealand Wrens) MATERIAL EXAMINED. Acanthisitta chloris 2; Xenicus longipes 5; A', gilviventris 1 . NOTE. Most specimens available for examination were poorly preserved. I identified a gland in Acanthisitta, in only 1 of the 5 Xenicus longipes, and not in A', gilviventris. AVIAN UROPYGIAL GLAND 237 Suborder Menurae Family Menuridae (Lyrebirds) MATERIAL EXAMINED. Menura novaehollandiae 2. Family Atrichornithidae (Scrub-birds) MATERIAL EXAMINED. Atrichornis clamosus \ . NOTE. B. Gillies (in litt., 4 April 1985) reported that this specimen (Rl 1353) has a naked gland; another specimen (A 15926) is illustrated in Zusi (1985) as having a naked gland. Suborder Oscines Family Alaudidae (Larks) MATERIAL EXAMINED. Mirafrajavanica 1 ; M. assamica 1 ; Eremopterix signata 1 ; Alaemon alaudipes 1; Melanocorypha yeltoniensis 1; Calandrella cinerea 1; Galerida cristata 1; Lullula arborea 1; Eremophila alpestris 1 . Family Hirundinidae (Swallows) MATERIAL EXAMINED. Tachycineta bicolor 2; Progne subis 1 (F: 63-1, 0-03); Hirundo rustica 3; H. smithii 1 . Family Motacillidae (Wagtails, Pipits) MATERIAL EXAMINED. Dendronanthus indicus 1; Motacilla alba 2; M. aguimp 1; Macronyx croceus \\Anthusspinoletta 1 (M: 19-2, 0-13). Family Campephagidae (Cuckoo-shrikes) MATERIAL EXAMINED. Coracina novaehollandiae 1; C. striata 1; C. morio 1; C. panayensis 1; C. melaschistos 1; Lalage nigra 1; Campephaga phoenicea 1; Pericrocotus cinnamomeus 1; P.flammeus 1; Hemipus picatus 1. Family Pycnonotidae (Bulbuls) MATERIAL EXAMINED. Pycnonotus barbatus 8; P. goiavier 1 ; Chlorocichlaflaviventris 2; Bleda eximia 1; Criniger phaeocephalus 1; Setornis criniger 1; Hypsipetes everetti 1. Family Irenidae (Leaf Birds) MATERIAL EXAMINED. Irenapuella 1. Family Laniidae (Shrikes and Allies) Subfamily Prionopinae MATERIAL EXAMINED. Eurocephalus ruppelli 1; Prionops plumata 1. Subfamily Malaconotinae MATERIAL EXAMINED. Dryoscopus cubla 3; D. sabini 1; Tchagra senegala 1; T. australis 2; Laniarius ferrugineus 3; L. barbarus 1; Telophorus sulfureopectus 1; T. multicolor 1. Subfamily Laniinae MATERIAL EXAMINED. Corvinella corvina 1; Lanius collurio 1; L. ludovicianus 2. Subfamily Pityriasinae MATERIAL EXAMINED. Pityriasis gymnocephala 1. Family Vangidae (Vangas) MATERIAL EXAMINED. Calicalicus madagascariensis 1 ; Vanga curvirostris 1 . Family Bombycillidae (Waxwings) Subfamily Bombycillinae MATERIAL EXAMINED. Bombycilla garrulus 1; B. cedrorum 1 (F: 29-2, 0-10). 238 DAVID W. JOHNSTON Subfamily Ptilogonatinae MATERIAL EXAMINED. Ptilogonys cinereus 1 . Subfamily Hypocoliinae MATERIAL EXAMINED. Hypocolius ampelinus 1 . Family Dulidae (Palm Chat) MATERIAL EXAMINED. Dulus dominions 1 . Family Cinclidae (Dippers) MATERIAL EXAMINED. Cinclus cinclus 1 ; C. pallasii 1 ; C. mexicanus 4 (unsexed: 63-6, 0-48; 58-3, 0-65; 59-7,0-71). NOTE. Nitzsch (1867: 73) reported that the gland of Cinclus 'bears small down-feathers upon its surface,' but it is not clear that his 'surface' refers to the papilla's tip. All specimens examined in the present study had naked glands. Family Troglodytidae (Wrens) MATERIAL EXAMINED. Campylorhynchus rufinucha 1; Cistothorus platensis 2; C. palustris 2; Thryothorus pleurostictus 2; T. maculiectus 2; T. ludovicianus 1; T. rufalbus 1; Troglodytes aedon 2; Uropsila leucogastra 1; Henicorhina leucosticta 3. Family Mimidae (Mockingbirds and Allies) MATERIAL EXAMINED. Dumetella carolinensis 1 7 (F: 35-4, 0- 1 8); Mimuspolyglottos 5 (M: 47-6, 0- 1 6); Toxostoma rufum 5 (M: 55-3, 0-07. F: 69-1, 0-14). Family Prunellidae (Accentors) MATERIAL EXAMINED. Prunella collaris 1. Family Muscicapidae* Subfamily Turdinae (Thrushes) MATERIAL EXAMINED. Zeledonia coronata 4; Sialia currucoides 1; Catharus fusee scens 2 (F: 28-1, 0-09); C. minimus 2; C. ustulatus 3; C. guttatus 2; Hylocichla mustelina 28 (F: 47-4, 0-09; 59-7, 0-07); Turdus merula 1; T. iliacus 1; T.philomelos 1; T. viscivorus 1; T.grayi4; T. migratorius 4 (M: 85-3, 0-09. F: 72-4, 0-09; 85-7, 0-12). Subfamily Orthonychinae (Logrunners) MATERIAL EXAMINED. Cinclosoma cinnamomeum 1 . Subfamily Timaliinae (Babblers) MATERIAL EXAMINED. Trichastoma bicolor 1; Malacopteron magnum 1; Pomatorhinus schisticeps 1; Napothera brevicaudata 1; Chamaeafasciata 2; Turdoides squamiceps 1; Garrulax leucolophus 3; Actinodura ramsayi 1; Alcippe castaneceps 1. Subfamily Panurinae (Parrotbills) MATERIAL EXAMINED. Paradoxornis heudei 1 . Subfamily Picathartinae (Picathartes) MATERIAL EXAMINED. Picathartes oreas 1. Subfamily Polioptilinae (Gnatcatchers and allies) MATERIAL EXAMINED. Ramphocaenus melanurus 2; Polioptila caerulea 1 . "nomenclature and inclusive taxa according to Peters (Vol. X, 1964). AVIAN UROPYGIAL GLAND 239 Family Sylviidae (Old World Warblers) MATERIAL EXAMINED. Locus tella lanceolata 1; Acrocephalus scirpaceus 1; Cisticola erythrops 1; Sylvietta rufescens 1; Hylia prasina 1; Abroscopus schisticeps 1; Sylvia communis 1; S. hortensis 1; Regulus calendula 6; R. satrapa 1 . Family Muscicapidae (Old World Flycatchers)** MATERIAL EXAMINED. Muscicapa dauurica 1 . Family Platysteiridae (Puffback Flycatchers) MATERIAL EXAMINED. Batis molitor \ . Family Maluridae (Australo-Papuan Wrens) MATERIAL EXAMINED. Malurus lamberti 1 . Family Acanthizidae (Australasian Warblers) Subfamily Acanthizinae MATERIAL EXAMINED. Sericornis magnirostris 1 . Subfamily Mohouinae MATERIAL EXAMINED. Unavailable. Family Monarchidae (Monarch Flycatchers) Subfamily Monarchinae MATERIAL EXAMINED. Terpsiphone viridis 1; T. atrocaudata 1; Chasiempis sandwichensis 1. Subfamily Rhipidurinae MATERIAL EXAMINED. Ripidura albicollis \ . Family Eopsaltriidae (Australasian Robins) MATERIAL EXAMINED. Petroica phoenicea 1; P. vittata 1; Tregellasia leucops 1. Family Muscicapidae*** Subfamily Pachycephalinae (Whistlers) MATERIAL EXAMINED. Pachycephala lanioides 1 . Family Aegithalidae (Long-tailed Tits, Bush Tits) MATERIAL EXAMINED. Aegithalos caudatus 2. Family Remizidae (Penduline Tits) MATERIAL EXAMINED. Auriparusflaviceps 2. Family Paridae (Titmice) MATERIAL EXAMINED. Parus atricapillus 1; P. carolinensis 1; P. bicolor 1; Hypositta corallirostris 1. Family Sittidae Subfamily Sittinae (Nuthatches) MATERIAL EXAMINED. Sittapusilla 1; S. canadensis 1; S. carolinensis 1. Subfamily Daphoenosittinae (Treerunners) MATERIAL EXAMINED. Neositta chrysoptera 3; Daphoenositta miranda 2. * ""nomenclature and inclusive taxa according to Peters (Vol. XI, 1986). ***nomenclature and inclusive taxa according to Peters (Vol. XII, 1967). 240 DAVID W. JOHNSTON Subfamily Tichodromadinae ( Wallcreepers) MATERIAL EXAMINED. Tichodroma muraria \ . Family Certhiidae (Creepers) Subfamily Certhiinae (Treecreepers) MATERIAL EXAMINED. Certhiafamiliaris 2. Subfamily Salpornithinae (Spotted Creeper) MATERIAL EXAMINED. Salpornis spilonotus 1 . Family Rhabdornithidae (Philippine Creepers) MATERIAL EXAMINED. Rhabdornis mysticalis 1 . Family Climacteridae (Australian Treecreepers) MATERIAL EXAMINED. Climacteris melanura 1 . Family Dicaeidae (Flowerpeckers) MATERIAL EXAMINED. Rhamphocharis crassirostris 1 ; Prionochilus olivaceus 1 ; Dicaeum concolor 1 ; D. cruentatwn 1; Oreocharis arfaki 1; Pardalotus rubricates 1. Family Nectariniidae (Sunbirds) MATERIAL EXAMINED. Anthreptes malacensis 1; Hypogramma hypogrammicum 1; Nectarinia olivacea 1 ; N. senegalensis 7; N. sericea 1 ; N. jugularis 2; N. asiatica 1 ; N. venusta \ ; N. talatala 2; N. habessinica 1; Aethopyga boltoni 1; Arachnothera longirostra 1 . Family Zosteropidae (White-eyes) MATERIAL EXAMINED. Zosterops griseotincta 1 . Family Meliphagidae (Honeyeaters) MATERIAL EXAMINED. Oedistoma iliolophum 1; Myzomela sanguinolenta 1; M eliphaga fusca 1; M. pencillata 1; Melithreptus brevirostris 1; Philemon citreogularis 1; Melidectes fuscus 1; Acanthorhynchus tenuirostris 1; Anthochaera carunculata \. Family Emberizidae Subfamily Emberizinae (Buntings and American Sparrows) MATERIAL EXAMINED. Emberiza flaviventris 1; Calcarius lapponicus 1; Zonotrichia melodia 4 (M: 17-6, 0-12); Z. georgiana 3; Z. albicollis 7; Junco hyemalis 1; Ammodramus sandwichensis 3; A. savannarum 3; Spizella passerina 1; S. pusilla 1; Pooecetes gramineus 1; Aimophila aestivalis 2; Sicalis olivascens 1; Volatinia jacarina 2; Sporophila torqueola 6; S. telasco 1; Camarhynchus crassirostris 1; Pipilo erythrophthalmus 3 (M: 43-8, 0-26. F: 36-7, 0-22); Arremon aurantiirostris 3; Arremonops rufivirgatus 3; A. chloronotus 1. Subfamily Catamblyrhynchinae (Plush-capped Finch) MATERIAL EXAMINED. Catamblyrhynchusdiadema 1. Subfamily Cardinalinae (Cardinal-grosbeaks) MATERIAL EXAMINED. Pheucticus ludovicianus 1; P. melanocephalus 1 (F: 40-5, 0-09); Cardinalis cardinalis 5 (M: 40-3, 0-09; 33-0, 0-07. F: 40-0, 0-09); Saltator atriceps 1; S. maximus 2; S. aurantiirostris 1; Passerina cyanoides 8; P. caerulea 2; P. cyanea 6. Subfamily Thraupinae (Tanagers) MATERIAL EXAMINED. Eucometis pencillata 2; Lanio aurantius 3; Tachyphonus luctuosus 1; Habia rubica 3; H.fuscicauda \ 6; Piranga rubra 2; .P. olivacea 3 (F: 26-5, 0-06); Ramphocelus sanguinolentus 4; R. passer inii 4\ Thraupis episcopus 1 ; 7\ bonariensis 1 ; Euphonia affinis 2; Dacnis cyana 1 ; Cyanerpes cyaneus 4; Diglossa carbonaria 1 . AVIAN UROPYGIAL GLAND 241 Subfamily Tersininae (Swallow-tanager) MATERIAL EXAMINED. Tersina viridis 1 . Family Parulidae (Wood Warblers) MATERIAL EXAMINED. Mniotilta varia 3; Vermivora peregrina 2; Parula americana 1; Dendroica petechia 4; D. magnolia 1; D. coronata 3; D. cerulea 1; D.fusca 3; D. pensylvanica 2; D. castanea 2; D. striata 1 ; D.pinus 1 ; D.palmarum 1 ; Setophaga ruticilla4; Seiurus aurocapillus 6; S. noveboracensis 9 (M: 1 6-2, 0- 1 5); S. motacilla 2; Helmitheros vermivorus 6; Protonotaria citrea 1 ; Geothylpis trichas 4 (M: 11-5, 0-09); G. poliocephala 1; G.formosa 20; Wilsonia pusilla 4; Icteria virens 4; Coereba flaveola 2. Family Drepanididae (Hawaiian Honeycreepers) MATERIAL EXAMINED. Himatione sanguinea 1; Palmeria dolei 1; Vestiaria coccinea 1; Loxops virens 1. Family Vireonidae (Peppershrikes, Shrike- Vireos) Subfamily Cyclarhinae MATERIAL EXAMINED. Cyclarhis gujanensis 1 . Subfamily Vireolaniinae MATERIAL EXAMINED. Vireolanius pulchellus 1. Subfamily Vireoninae MATERIAL EXAMINED. Vireo griseus 3; V.flavifrons2\ V. solitarius 2; K. olivaceus 3; V.flavoviridis3; V. gilvus 1 ; Hylophilus ochraceiceps 4; //. decurtatus 1 . Family Icteridae (American Orioles and Blackbirds) Subfamily Icterinae MATERIAL EXAMINED. Psarocolius montezuma 2; Amblycerus holosericeus 1; Icterus galbula 1; /. spurius 2; /. dominicensis 1; Agelaius phoeniceus 26 (x of 16 M: 55-4, 0-17. x of 9 F: 42-8, 0-18); Sturnella magna 4 (M: 105-5, 0- 1 1 . F: 78-6, 0- 1 3): S1. neglecta 1 ; Quiscalus mexicanus 1 ; (2- ma/or 23 (x of 14M:192-9,0-17.xof9F:91-0, 0-21); Q.quiscula6(M: 113-4, 0-16; 117-4, 0-14; 119-1, 0-14.F: 84-2, 0-17); Euphagus carolinus 1 (M: 66-0, 0-13); Molothrus ater 15 (x of 6 M: 47-5, 0-13. x of 8 F: 37-3,0-14). Subfamily Dolichonychinae MATERIAL EXAMINED. Dolichonyx oryzivorus 12 (x of 10 M: 39-0, 0-09). Family Fringillidae Subfamily Fringillinae (Chaffinches and Brambling) MATERIAL EXAMINED. Fringilla coelebs 1; F. montifringilla 1 . Subfamily Carduelinae (Serins, Goldfinches, et al.) MATERIAL EXAMINED. Serinus mozambicus 14; Carduelis pinus 2 (M: 10-5, 0-10); C. tristis 1; Carpodacus purpureus 2 (M: 26-2, 0-03); C. mexicanus 2 (F: 23-2, 0-11); Pinicola enucleator 4 (F: 55-2, 0-06; 56-8, 0-05; 60-2, 0-03); Coccothraustes vespertinus 1 (M: 56-6, 0-05). Family Estrildidae (Waxbills, Grass Finches, and Mannikins) MATERIAL EXAMINED. Pytilia melba 2; Uraeginthus angolensis 8; Estrilda caerulescens 1; Poephila acuticauda 1; P. cincta 1; Chloebia gouldiae 1; Lonchura cucullata \\Amadinafasciata 1 . Family Ploiceidae Subfamily Viduinae (Indigo-birds and Whydahs) MATERIAL EXAMINED. Vidua paradisaea 1 . 242 DAVID W. JOHNSTON Subfamily Passerinae MATERIAL EXAMINED. Passer domesticus 14 (M: 24-5, 0-09; 24-8, 0-20. F: 22-3, 0-18; 25-1, 0-18); P. griseus 3. Subfamily Bubalornithinae MATERIAL EXAMINED. Dinemellia dinemelli 1 . Subfamily Ploceinae MATERIAL EXAMINED. Amblyospiza albifrons 1; Ploceus subaureus 3; P. xanthops 1; P. velatus 4; P. cucullatus 25; Euplectes hordeaceus 1 ; E. orix 1 1 . Family Sturnidae (Starlings) Subfamily Sturninae MATERIAL EXAMINED. Sturnus vulgaris 5 (M: 78-3, 0-11; 80-5, 0-13; 89-7, 0-11); Sarcops calvus 1; Gracula religiosa 1 . Subfamily Buphaginae MATERIAL EXAMINED. Buphagus erythrorhynchus 2; Buphagus sp. 1 . Family Oriolidae (Orioles) MATERIAL EXAMINED. Oriolus oriolus 1; O. chinensis 1; O. xanthornus 1. Family Dicruridae (Drongos) MATERIAL EXAMINED. Dicrurus remifer 1; D. hottentottus 1 ; D. paradiseus 1. Family Callaeidae (New Zealand Wattlebirds) MATERIAL EXAMINED. Callaeas cinerea 1 ; Creadion carunculatus 1 ; Heteralocha acutirostris 1 . Family Grallinidae (Australian Mud Nest Builders) Subfamily Grallininae MATERIAL EXAMINED. Grallina cyanoleuca 1 . Subfamily Corcoracinae MATERIAL EXAMINED. Corcorax melanorhamphos 1; Struthidea cinerea 2. Family Artamidae (Wood-swallows) MATERIAL EXAMINED. Artamus fuscus 1; A. leucorhynchus 1; A. super ciliosus 1; A. cinereus 1; A. minor 1. Family Cracticidae (Australian Butcherbirds) MATERIAL EXAMINED. Cracticus nigrogularis 1 ; Gymnorhina tibicen 1 ; Strepera graculina 1 . Family Ptilonorhynchidae (Bowerbirds) MATERIAL EXAMINED. Ailuroedus crassirostris 1; Amblyornis macgregoriae 2; Sericulus chrysocephalus 1; Ptilonorhynchus violaceus 1; Chlamydera nuchalis 2. Family Paradisaeidae (Birds of Paradise) MATERIAL EXAMINED. Manucodia comrii 1 ; Semioptera wallacei 1 ; Astrapia stephaniae 1 ; Lophorina superba 1 ; Cicinnurus regius 1 ; Diphyllodes respublica 1 ; Paradisaea apoda 1 . Family Corvidae (Crows, Magpies, Jays) MATERIAL EXAMINED. Cyanocitta cristata 14 (M: 77-7, 0-20; 78-4, 0-10. F: 59-4, 0-08); Aphelocoma coerulescens 2 (M: 70-3, 0-1 1; 72-0, 0-07); Garmlus glandarius 1; Pica pica 2; Corvus monedula 1; C.frugilegus 2; C. brachyrhynchos 39 (x of 14 M: 563- 1 , 0-05. x of 1 1 F: 495-7, 0-05); C. ossifragus 4 (M: 330-0, 0- 15. F: 232-0, 0- 1 3); C. corone 2. AVIAN UROPYGIAL GLAND 243 Dendrocolaptes certhia Cindus mexicanus Corvus brachyrhynchos Weights and sizes of glands Early accounts of uropygial glands included brief comments about relative size ('small,' 'large,' 'smaller than'; Willughby 1678; Burton 1822, Macgillivray 1837, Bartlett 1861). Such relative adjectives and phrases persist in the more contemporary literature (Austin 1961, Thomson 1964, Shortt 1977). Edwards Crisp (1860, 1862) was probably the first person to publish gland weights, and, by weighing birds and their glands separately, he presented the relative proportion of gland weight to the bird's body weight. He (1860: 258) presented data on 34 species of aquatic and terrestrial birds, showing relatively lightest glands in pigeons and heaviest ones in Cindus aquaticus (C. cinculus aquaticus of Peters) and six species of waterfowl. The frequent assertion that the preen gland of water-birds is relatively larger than that of land-birds (e.g., Kennedy 1971) is probably derived from Crisp's results (see also Coues 1890), even though Frederick II in 1260 reported large glands in aquatic species (Wood and Fyfe 1943). Subsequent authors have presented absolute or relative gland weights for many more species (Kossman 1871, Paris 1913, Kar 1947, Grasse 1950, Elder 1954, Kennedy 1971, Johnston 1979, Jacob & Ziswiler 1982). In these reports, differences in relative gland weights have variously been attributed to season (Kossman 1871, Kennedy 1971), habitat (Crisp 1860, Jacob & Ziswiler 1982), intergeneric body weight (Johnston 1 979), nutrition (Kossman 1871), individual variation (present study and others), and sex (Groebbels 1 932). Although Elder ( 1 954) suggested that glands of diving ducks (Aythyd) are relatively heavier than those of dabbling ducks (Anas), some of Jacob & Ziswiler's data (1982: 214) 'clearly refute this hypothesis.' Subsequently I compared relative gland weights from 7 species of dabbling ducks (N = 21, x = 0-30%, SD = 0-047) with weights from 5 species of diving ducks (N = 20, x = 0-29, SD = 0-065); the differences were not statistically significant (d.f. = 40, t = 0-7560, p > 0-05). Jacob & Ziswiler (1982) presented gland weights from 574 individuals in 183 species, and I obtained gland weights from 544 individuals in 200 species. All these weights are presented in Table 1 . A comparison of these two data sets shows reasonable agreement for the same taxon especially as regards mean values. Also apparent are variations in relative gland weights within and between species, variations that I attribute largely to individual body weight differences. The latter are probably due to sexual differences (see, for example, data for three species of Icterinae in the Systematic accounts) and variations in the amounts of subcutaneous fat. From their analysis of relative gland weights, Jacob & Ziswiler concluded that 'the only thing that can be said with certainty regarding the size of the uropygial gland is that birds that swim and dive have, without exception, a large uropygial gland' (1982: 214). This statement should be expanded to include the earlier demonstrated correlations with season, nutrition, and sex by the other authors mentioned above. I was able to examine the habitat-habit issue more thoroughly because of a much larger sample size, including birds living in most major habitat types. By grouping relative weights of birds at the family level and to broad habitat-habit categories (Fig. 2), I found that the largest (relative) glands 244 DAVID W. JOHNSTON Table 1 Summary of uropygial gland weights PRESENT STUDY JACOB & ZISWILER (1982) No. of species No. of glands Relative gland weight* No. of species No. of glands Relative gland weight* Tinamidae 1 12 0-18 Diomedeidae 1 1 0-30 Procellariidae 5 9 0-46 (0-30-0-67) 2 4 0-24-0-27 Hydrobatidae 4 6 0-16(0-07-0-37) Spheniscidae 1 2 0-08(0-06-0-12) 2 3 0-21-0-26 Gaviidae 4 9 0-18(0-09-0-30) 2 3 0-14-0-20 Podicipedidae 2 6 0-26(0-19-0-42) 2 7 0-48-0-61 Phaethontidae 1 1 0-43 Fregatidae 1 3 0-07 (0-06-0-07) Phalacrocoracinae 1 10 0-25(0-20-0-35) 3 12 0-21-0-31 Anhinginae 1 8 0-15(0-12-0-17) Sulidae 1 1 0-38 1 2 0-35 Pelecanidae 2 4 0-36(0-30-0-43) 1 1 0-19 Ardeidae 9 20 0-14(0-01-0-42) 3 7 0-05-0-07 Ciconiidae 1 1 0-05 1 2 0-08 Threskiornithidae 3 4 0-15(0-11-0-19) 3 4 0-03-0-11 Phoenicopteridae 2 4 0-18-0.21 Cathartidae 2 10 0-04(0-01-0-05) Pandioninae 1 2 0-25(0-18-0-31) 1 1 0-36 Accipitrinae 11 25 0-06(0-01-0-13) 7 17 0-04-0-22 Falconidae 4 15 0-07 (0-03-0-09) 1 4 0-08 Anatidae 25 55 0-26(0-10-0-42) 15 55 0-08-0-54 Anhimidae 1 1 0-13 Megapodiidae 1 1 0-18 Tetraonidae 6 7 0-05(0-02-0-18) 3 11 0-09-0-15 Phasianidae 8 17 0-07(0-02-0-16) 5 12 0-08-0-11 Meleagrididae 1 3 0-03 (0-02-0-04) 1 2 0-05 Numididae 2 3 0-05-0-18 Gruidae 1 4 0-05 (0-03-0-05) 1 1 0-05 Aramidae 1 7 0-28(0-17-0-42) Rallidae 6 27 0-19(0-11-0-34) 5 14 0-09-0-24 Haematopodidae 1 1 0-20 Charadriidae 2 4 0-18(0-07-0-22) 1 2 0-16 Scolopacidae 9 25 0-12(0-05-0-20) 4 5 0-11-0-18 Recurvirostridae 1 1 0-24 Phalaropodidae 2 4 0-59 (0-42-0-79) Burhinidae 1 1 0-09 Chionididae 1 1 0-17 Stercorariidae 2 3 0-29 (0-28-0-37) Larinae 3 5 0-20(0-13-0-29) 4 19 0-12-0-20 Sterninae 9 20 0-33(0-18-0-57) 4 5 0-19-0-44 Rynchopidae 1 1 0-20 Alcidae 5 7 0-27(0-18-0-47) 3 7 0-17-0-29 Pteroclididae 1 1 0-02 Columbidae 5 11 0-04(0-01-0-10) 4 5 0-02-0-04 Psittacidae 2 1 0-11(0-05-0-16) 41 125 0-04-0-19 Cuculidae 2 2 0-06 (0-03-0-09) 2 4 0-12-0-16 Tytonidae 1 4 0-09 (0-04-0- 12) 1 7 0-08 Strigidae 6 22 0-07(0-03-0-11) 4 9 0-04-0-09 Steatornithidae 1 0-22 Caprimulgidae 3 11 0-01 (0-01-0-02) 1 0-01 Apodidae 2 11 0.04-0-05 Alcedinidae 1 2 0-24(0-22-0-25) 2 0-18 Upupidae 2 0-14 Meropidae 1 0-11 Bucerotidae 2 4 0-08-0-11 AVIAN UROPYGIAL GLAND 245 Ramphastidae 1 2 0-1 3 (0-1 2-0- 14) 2 5 0-08-0-10 Picidae 5 13 0-1 2 (0-08^)- 14) 4 9 0-09-0-12 Tyrannidae 2 2 0.09(0-08-0-10) Alaudidae 1 1 0-28 Hirundinidae 1 1 0-03 1 6 0-21 Motacillidae 1 1 0-13 1 2 0-27 Bombycillidae 1 1 0-10 Cinclidae 1 3 0-61 (0-48-0-71) Troglodytidae 1 3 0-58 Mimidae 2 4 0-14(0-07-0-18) Prunellidae 1 1 0-28 Turdinae 3 6 0-09(0-07-0-12) 2 7 0-08-0-14 Aegithalidae 1 2 0-21 Paridae 2 23 0-14-0-15 Sittidae 1 1 0-12 Emberizinae 2 3 0-20(0-12-0-26) 2 6 0-26-0-31 Cardinalinae 2 4 0-09 (0-07-0-09) 1 2 0-18 Thraupinae 1 1 0-06 Parulidae 2 2 0-1 2 (0-09^)- 15) Icterinae 6 55 0-15(0-ll^)-24) Dolichonychinae 1 10 0-09(0-06-0-13) Fringillidae 5 7 0-06(0-03-0-11) 3 26 0-22-0-25 Estrildidae 6 24 0-17-0-23 Passerinae 1 4 0-16(0-09-0-20) Ploceidae 3 17 0-19-0-28 Sturnidae 1 3 0-12(0-11-0-13) 1 8 0-10 Corvidae 4 32 0-10(0-04-0-20) 7 40 0-08-0-12 *gland weight as percent of body weight; mean (extremes) are found in nonpasserines that swim, dive or rest on water (N= 18 families, x = 0-28%). The smallest glands occur in terrestrial (non-aquatic) birds: nonpasserines (N= 15, x = 0-07%) and passerines (N = 1 6, x = 0-04%). I found the largest relative gland weights in the Procellariidae (Oceanodroma melania, 0-69% Fulmarus glacialis, 0-67%) Phalaropodidae (Phalaropus fulicarius, 0-79%), Sterninae (Sterna albifrons, 0-57%), and Cinclidae (Cinclus mexicanus, 0-71 %). The largest glands reported by Jacob & Ziswiler (1982) were for Tachybaptus ruficollis (0-61%) and Troglodytes troglodytes (0-58%). Because of its habit of plunging into water for fish, the Osprey expectedly has a larger (0-25%) gland than any other of the Falconiformes (Accipitrinae, 0-06% and Falconidae 0-07%). The smallest glands, which could be accurately weighed in the present study, were found in Caprimulgidae (11 individuals averaging 0-01%), Meleagrididae (3 individuals, x = 0-03%) and Columbidae (1 1 individuals, x = 0-04%). Burton (1822: 4; and quoted by Murphy 1936) reported that the uropygial gland of Fregata aquila is a 'trifling size.' In my study, fresh weights of birds and glands of Fregatidae were available only for F. magnificens , so I could not compare relative gland weights among frigatebirds. How- ever, the length of glands (sans feathers) were as follows: F. magnificens, 1 5 mm; F. aquila, 13 mm; F. ariel, 1 3 mm. The gland of F. aquila is thus no smaller than that of F. ariel which is the smallest species of Fregata (Nelson 1975). Frigatebirds have smaller glands relative to body weight (0-07%) than other nonpasserine birds that live on or in water (e.g., Procellariidae, 0-44%; Phaethontidae, 0-30%; Pelecanidae, 0-28%; Anatidae, 0-27%) with the exception of Spheniscidae (0-08%). The putative relationship between a small, 'insufficient' gland and feathers becoming so wet that frigatebirds drown (first proposed by Burton in 1822 and paraphrased by Welty 1962) lacks scientific verification (see related discussion on spread-wing posture in Clark 1969). My findings enable me to correct several unverified statements in the literature on gland sizes. Gurney's (1913) assertion, paraphrasing Ticehurst, that the gland of Sula bassana 'is the largest proportionally' of all birds, now turns out to be incorrect. One relative gland weight for this species was only 0-38% (present study), compared with relatively much heavier glands in procellarids, 246 DAVID W. JOHNSTON CO E LJJ CO CO TERRESTRIAL - SWIM IN WATER - TERRESTRIAL - <0 FLY OVER WATER - LU 1 LU $ WALK IN WATER - Ma 1 SWIM, DIVE, OR REST ON WATER oooooo o O 000000*10 o oooo M 00 O OO. OO O o o = AVERAGE FOR A FAMILY M = MEAN oo o o ooo ooo o ooo o o 3000 M .00 .10 .20 .30 .40 .50 .60 -70 UROPYGIAL GLAND WEIGHT AS PERCENT OF BODY WEIGHT Fig. 2 Relationships between uropygial gland weights and avian habitat-habits. anatids, phalaropes, and others (above). Austin (1961) (see also Shortt 1977) wrote that dippers (Cinclidae) have a 'tremendous preen gland, ten times the size of that of any other passerine bird.' To be sure, the gland of Cinclus mexicanus (x = 0-61; 0-48-0-7 1%) is the largest yet reported for any passerine, but other passerine families (e.g., Emberizidae, Icteridae) have glands as large as 0-24-0-26% and Troglodytes troglodytes has a large gland (0-56-0-58%, Kennedy 1971; Jacob and Ziswiler 1982). My data show that large (i.e., heavy) birds have absolutely large uropygial glands. For 670 individuals, representing 61 families of passerine and nonpasserine birds, I found a significant correlation between body weight and gland weight (r = 0-694, P ^ 0-0 1 ). This correlation is import- ant especially because of the inverse relation of plumage weight (as a percent of body weight) with body weightier se (Kossman 1871, Turcek 1966). Kennedy (1971: 370) correctly cautioned that 'this parallel could result from a functional connection between the preen gland [size and] secretion and the area of feathers which require anointing with it. Additionally, it is possible that relative to body weight, water-birds have a larger area of feather surface requiring anointing with secretion than land-birds of similar size, which may partly explain their larger glands.' Conclusions drawn from size and weight relationships of glands must still be tentative. Despite the large numbers of weights and broad taxonomic coverage presented in this study and others (Kennedy 1971, Jacob & Ziswiler 1982), gland weights have never been reported from many birds — e.g., Apterygidae, wild Psittacidae, Trochilidae, Coliidae, most of the coraciiform and piciform families, and most of the passerines. Feathers on uropygial glands Feathers attached to the papilla at the end of the uropygial gland are collectively termed circulus uropygialis by Lucas & Stettenheim (1972) and Baumel et al. (1979). Through the years these feathers have been variously described in different birds as 'contour' (Nitzsch 1867), 'down' or 'downy' or 'modified down' (Nitzsch 1867, Newton 1893-1896, Beddard 1898, Verheyen 1956/, 1958c, d, Grasse 1950, Lucas & Stettenheim 1972, Baumel et al. 1979), 'semiplumes' (Nitzsch AVIAN UROPYGIAL GLAND 247 1840), 'plumules' or 'plumulets' (Paris 1913), 'plumes' (Beddard 1898), with or without a rachis and/or hyporachis (Paris 1913, Verheyen 1959c). Some of the earlier publications (e.g., Nitzsch 1867) even described 'fine hairs' at the tip of certain glands. Miller (1924) was apparently the first investigator to use magnification in determining the number and type of feathers on a gland. The number of feathers per gland ranges from 1 (minute) to 90 (Jacob & Ziswiler 1982, the present study). Jacob & Ziswiler provided a thorough discussion of the number, arrangement, density, and length of the feathers. Because of some individual variation in number of feathers and other considerations, Jacob & Ziswiler (correctly in my opinion) cautioned against the use of feather number for taxonomic or diagnostic criteria. Rather, from a functional standpoint, they noted a general tendency for waterbirds to have more and longer feather tufts than landbirds. They also believed that the proportional length of the papilla to that of the tuft is taxonomically specific (see also Schumacher 1919). Lucas and Stettenheim (1972) classified uropygial gland feathers as 'modified down,' defining down as feathers with a rachis shorter than the longest barbs and semiplumes having a rachis that exceeds the longest barbs. My microscopic study of gland feathers from 70 families containing tufted glands revealed the presence of three feather types (Fig. 3). Most of the family representa- tives (62) had feathers of type I which, by the definition of Lucas & Stettenheim (1972), are down. TYPE I -4-* T jTT-v- (TRUNCATE) BARB CALAMUS TYPE II TYPE lla Fig. 3 Diagrams of typical uropygial gland feathers. CALAMUS 248 DAVID W. JOHNSTON Three families each had feathers of Types II and Ha, both defined here as semiplumes. Nodal structures on barbules on these feathers differed from those on true down and contour feathers (Douglas Deedrick and Roxie Laybourne, pers. comm.). Therefore, the most appropriate terms for describing the circulus uropygialis are modified down or modified semiplumes. Contrary to the reports of some other investigators (e.g., Lucas & Stettenheim 1972), I found no afterfeathers on any gland feathers. Even in groups (e.g., Galliformes) renowned for having afterfeathers on body contour feathers, afterfeathers were not found. This difference might be attributable to the criterion for identifying an afterfeather. Lucas & Stettenheim (p. 252) regarded any group of outgrowths on the rim of the superior umbilicus as an afterfeather; outgrowths were not identified in the present study. Naked and tufted glands Most early investigators such as Nitzsch (1867), Beddard (1898), and Paris (1913) generally cate- gorized glands as either tufted or naked (nude, bare), that is, with or without feathers on the papilla. For the most part, the glands that they examined were 'obviously' (unmagnified) tufted or naked, although occasional references were made to a 'fine hair' at the tip of some glands (Nitzsch 1 867). This dichotomous difference apparently served well until some putative 'naked' glands were examined with magnification by Miller (1924) and were found to possess 1-2 mm feathers. It is now desirable to establish three categories of glands with respect to the degree of feathering on the papilla: naked (no feathers observable, even with magnification), minutely tufted (feathers detected only with magnification), and tufted (feathers observable without magnification). Glands previously considered to be naked by Paris (1913) and others but now known to be 'minutely tufted' include species in the families Apterygidae, Opisthocomidae, Tytonidae, Strigidae, and Momotidae. In each of these families, considerable individual variation has been found between the naked and minutely tufted conditions (see Systematic accounts). Naked glands are also morphologically variable, particularly as regards the length and width of the papilla. In all passerine birds, for example, the papilla is distinct and well defined. Most nonpasserine naked glands, on the other hand, either have no papilla (Rhinochetidae, Columbidae, Hemiprocnidae, Galbulidae) or the papilla is so ill-defined and broad that it appears to be continuous with the glandular lobes (e.g., Apterygidae, Cathartidae, Cuculidae). Although I believe the passerine gland shape is distinctive, some nonpasserine glands superficially resemble the passerine type — Cariamidae, Steatornithidae, Batrachostomus. Close examinations of figures in the Systematic accounts will show the distinctiveness of the naked passerine gland as opposed to the several naked nonpasserine ones. Jacob & Ziswiler (1982) recognized different shapes among many passerine glands (heart-shaped, kidney-shaped, etc.), but these designations were so variable between and within families that I could not use them. The majority of nonpasserines have obviously tufted glands, whereas passerine glands are uniformly naked. From an examination of all nonpasserine gland types, I conclude that the tufted gland is primitive. Derived types include those that are (1) minutely tufted, (2) naked (nonpasserine), and (3) naked (passerine). Gland absence The absence of uropygial glands in certain species of birds has been known at least since Nitzsch (1840). As more species were examined over the years, more were found to lack glands. For example, in the Columbidae, Garrod ( 1 8740) noted gland absence in only 4 genera, Beddard ( 1 898) and Grasse (1950) in 6 genera, and Verheyen (19570) added 'new' species in Treron and Goura. I made a special effort to examine as many species and individuals as available in the Columbidae, Psittacidae, and Picidae because of earlier discrepancies in reports for genera and species in these families. Nearly every published account containing any information on the absence of uropygial AVIAN UROPYGIAL GLAND 249 glands (Beddard, Paris, Grasse, Elder, VanTyne & Berger, and others) include at least one factual error on the subject, sometimes simply by omission and frequently by uncritically copying a statement from an earlier author. The glandless condition varies markedly at every taxonomic level: absent from entire orders, families, genera, species, and individuals. A gland might be present in some species of a genus, yet absent in others. At the individual level, for example in each of three species of Ptilinopus (coronulatus, pulchellus, rivoli), some individuals possess glands, whereas others do not. Darwin (1900) and Levi (1941) reported the gland's absence in certain varieties ofColumba livia. I found the gland to be absent in the following taxa (see Systematic accounts for details and pertinent comments): Struthionidae (all age groups), Rheidae (adults), Casuariidae (all age groups), Dromaiidae (adults), Mesoenatidae (all 3 species), Otidae (all 5 species examined), Columbidae (9 genera, 28 species), Psittacidae (6 genera, 31 species), Podargus (3 species examined), and Picidae (1 genus, 4 species). Some minor discrepancies exist between my findings and earlier reports. Although Garrod (1 874/?) reported no gland in Cacatua sulfur (Kakatoe sulphured), a live bird that I examined had a conspicuous, tufted gland. Nitzsch ( 1 840), Beddard ( 1 898), and others noted no gland in Argusianus (Argus); 5 specimens in the present study contained a gland. I suspect these discrepancies, as well as those in Ara and Cacatua roseicapella, can be attributed to individual variation among the specimens examined, most or all of them being captive birds. Because the glandless condition is found in such a wide diversity of species and other taxa, a quest for causal relationships is appropriate. Why, for example, do some parrots have glands whereas others do not? No single attribute (distribution, climate, ecology, flight, etc.) has been found to be consistent as an explanation, a conclusion also reached by Kossmann (1871) who stated that he could find no relationship between gland absence and 'way of life of the bird.' Some flightless birds lack glands; others do not. Some insular pigeons have glands; others do not. Some neotropical parrots lack glands; others have well-developed glands. In my opinion, uropygial glands have apparently been secondarily and independently lost in a variety of birds, but these losses remain unexplained. Although Beddard (1 898: 232) stated that 'presence or absence cannot be made use of as a fact of great systematic importance,' he (pp. 3 1 3-3 1 4 and elsewhere) nonetheless used the 'fact' as a family characteristic. Similarly, Garrod (1874&), Nitzsch (1840), Paris (1913) and many others have used presence or absence of glands (in addition to naked vs. tufted conditions) as distinctive family and generic characteristics. This is a valid use of uropygial gland data except in cases of known individual variation. Gland absence in all species of the Mesoenatidae is just as good a family characteristic as is their singular limited distribution. On the other hand, in the Picidae, and especially in only a few species of Campethera, gland absence is probably of little taxonomic importance at the family level. Glands in flightless birds Because some authors (e.g., Elder 1954) have suggested relationships among uropygial gland secretions, normal feather functions, and flight capabilities, an analysis of gland presence/ absence in flightless birds is desirable. Elder's experiments on ducks essentially showed that gland extirpation resulted in reduced feather waterproofing, thus rendering the birds flightless. The first consideration has been to determine if a relationship exists between a flightless con- dition and gland presence in nature. In Table 2, flightless species identified from several literature sources are listed along with the presence or absence of the gland. Except for most of the ratites (Struthionidae, Rheidae, Casuariidae, Dromaiidae), only one other taxon (all three species of Mesoenatidae) is known wherein flightless species lack a gland. Overall, this analysis reveals virtually no correlation between a flightless condition and gland absence: for 42 flightless species examined, only 8 lacked a gland in the adult. 250 DAVID W. JOHNSTON Table 2 The Relationship between the flightless condition* and presence of uropygial glands Struthionidae** Struthio camelus — absent in adult Rheidae** Rhe a americana — absent in adult Pterocnemia pennata — absent in adult Casuariidae** Casuarius bennetti — unavailable Casuarius casuarius — absent in adult Casuarius unappendiculatus — unavailable Dromaiidae** Dromaius novaehollandiae — absent in adult Apterygidae Apteryx australis — gland present, essentially naked (but see Beddard 1898, 1899) Apteryx owenii — gland present, naked Apteryx haastii — gland present, naked Spheniscidae 16 species — gland present and tufted in all 10 species examined Podicipedidae Rollandia microptera — gland present, tufted Podilymbus gigas — gland present, tufted Phalacrocoracidae Phalacrocorax harrisi — gland present, tufted Anatidae Tachyeres pteneres — gland present, tufted Tachyeres brachypterus — gland present, tufted Anas aucklandica — gland present, tufted Mergus australis — gland present, tufted (but perhaps capable of flight, see Weller 1980) Mesoenatidae Mesoenas variegata — gland absent Mesoenas unicolor — gland absent Manias benschi — gland absent Rallidae*** Rallus owstoni — gland present, tufted Rallus wakensis — gland present, tufted Cabalus modestus — unavailable Atlantisia rogersi — gland present, tufted or naked Tricholimnas lafresnayanus — unavailable Tricholimnas sylvestris — gland present, tufted Dryolimnas cuvieri aldabranus — gland present, tufted Cyanolimnas cerverai — gland present, tufted Nesoclopeus poeciloptera — unavailable Gallirallus australis — gland present, tufted Habropteryx insignis — unavailable Habroptila wallacii — unavailable Megacrex inepta — unavailable Porzanula palmeri — gland present, tufted Pennula san dwichensis — unavailable Aphanolimnas monasa — unavailable Tribonyx mortierii — gland present, tufted Porphyriornis nesiotis — gland present, tufted Porphyriornis comeri — gland present, tufted Notornis mantelli — gland present, tufted AVIAN UROPYGIAL GLAND 25 1 Rhynochetidae Rhynochetos jubatus — gland present, naked Alcidae Pinguinus impennis — gland present, tufted Psittacidae Strigops habroptilus — gland present, tufted Acanthisittidae Xenicus lyalli — unavailable (see Systematic accounts for other species). *Flightless species names taken from Thomson (1964), Greenway (1958), Austin (1961), Van Tyne & Berger (1976), Olson (1973fl, b\ Weller (1980), and Mlikovsky (1982). **Several authors (e.g., Beddard 1898, Jacob 1978) have reported the absence of a gland in all ratites except Apteryx, although the species examined were usually not identified by the author. ""•""Opinions differ on the flight capability of some of these species. Ripley and Beehler (1985: 7), for example, reported that Rallus owstoni 'can fly as high as one or two meters above the ground, but they seldom do so.' A second consideration concerns a possible relationship between gland size and a flightless condition. Although fresh gland weights from flightless species were unavailable to me, sizes (linear measurements) of glands of flightless species in the Podicipedidae, Phalacrocoracidae, Anatidae, and Rallidae were compared with glands from closely related (often congeners) species that fly. These comparisons revealed no major size differences in glands between flightless and flying birds. General taxonomic considerations of glands The use of the uropygial gland as a character in avian systematics has been both commonplace and controversial for many years. As early as 1840, Nitzsch identified general gland features (e.g., tufted vs. naked conditions) as characteristics of different avian taxa, and the gland was subse- quently much used in classification by ornithologists such as Coues (1890) and Beddard (1898). This use in taxonomy has continued to date by some investigators (e.g., Olson & Steadman's 1981 characterization of Pedionomus), but others have excluded gland morphology in taxonomic con- siderations (e.g., Cracraft, 1985). Thomson (1964) stated that the gland is 'unsatisfactory as a taxonomic character,' and Jacob & Ziswiler (1982) noted that the gland 'has little systematic importance ' From the systematic accounts of this monograph, it can be seen that the gland's presence or absence, tufted vs. naked condition (and variations thereof) might vary at any taxonomic level: intraspecific to interordinal. At the ordinal level, the gland is present and naked (with distinctive papilla) in all the Passeriformes, thus adding, as it were, another passerine characteristic. On the other hand, the several morphological variations in glands of the piciform families lend credence, I believe, to Olson's (1983) suggestion for a polyphyletic origin of the Piciforms (see also Burton 1984). The morphological gland characteristics that could be used in taxonomic analyses are: 1 . ontogeny — e.g., gland present in embryos and young of some ratites, but absent in all age groups of other ratites. 2. presence or absence of the gland — e.g., absent from families (Mesoenatidae in the Gruiformes) and genera (Amazona in the Psittacidae). 3. lobe shape — e.g., cf. Apodidae and Trochilidae in the Apodiformes. 4. tufted vs. naked condition — a. degree of feathering (cf. Momotidae and Meropidae) b. shape, size, and length of papilla (cf. Leptosomatidae and Coraciidae). 5. histology — little is known about histological variations, but features such as the number of gland openings are mentioned by Jacob & Ziswiler (1982). 252 DAVID W. JOHNSTON The value for a cladistic taxonomic scheme would depend on the number of variable features of the gland that could be analyzed and the incidence of multiple evolutions of those features. The recent chemo-taxonomic approach of Jacob & Ziswiler ( 1 982), based on chemical differences in uropygial secretions among different taxa, has as yet received little attention in avian taxonomic schemes. I believe that gland morphology is just as important a diagnostic taxonomic character as are muscle variations, osteological minutiae, incubation patterns, syringeal structures, and the like. The question is, of course, the degree of importance that one assigns to gland morphology in a large suite of taxonomic characters. Because of significant variations in gland morphology in different taxa, as identified in the present study, the least that could be said here is that gland morphology should be considered especially in cladistic taxonomic approaches. Functions of glandular secretions Uropygial gland functions (actually, the functions of glandular secretions) have been controversial ever since the gland was first described in the 13th century. Form and function of glands are biologically interrelated features, but, because the present report concentrates on gland mor- phology, only a brief summary of secretion functions is included here. (More detailed accounts can be found in Law (1929), Elder (1954), Thomson (1964), and Jacob & Ziswiler (1982)). At least 8 functions have been ascribed to the gland, and the interested reader is referred to the appropriate publications: 1. water-repellent action (Stubbs 1910, Elder 1954, Rijke 1970), 2. preserve physical structure of feathers (Rutschke 1960), 3. maintain horny sheath of bill (Thomson 1964), 4. as a scent organ (Giebel 1857, Jackson 1938, Mackworth-Praed and Grant 1970), 5. pheromone-producing (Balthazar! and Schoffeniels 1974), 6. antirhachitic action (Hou 1928), 7. prevent growth of skin microorganisms (King and McLelland 1984), 8. dislodge feather lice (Morris 1836#). Apparently any one or some combination of these functions could be ascribed to the secretions of an individual species but also the functions might not be identical for all birds. Most of the research on water-repellency ('waterproofing') has been appropriately conducted on aquatic birds, but virtually nothing is known about 'waterproofing' in landbirds. Indeed, Rutschke (1960) believed that the gland is only indirectly involved in 'waterproofing' of plumage in aquatic birds (see also Clark 1969), and Spearman (1971) made the unsupported comment that the glandular products are 'not essential for terrestrial birds.' Hou's studies (1928) on rickets and vitamin D were conducted only on chickens, pigeons, and, later, ducks. A scent-organ function for the gland has been reported for a variety of birds (e.g., Anas moschata, Phoeniculus bollei), but it is not clear how the 'foul-smelling' (to humans) secretions actually function. Contrary to the research reported by Elder (1954) on ducks, a number of reports have indicated that some birds from which glands had been surgically removed nonetheless had 'normal, bright plumages' (Arnall and Keymer 1975). As early as 1910, Pycraft expressed 'grave doubts' as to the function of the gland primarily because (1) he believed that some birds (e.g., Anastomus) presumably could not remove oil from the gland because of their peculiar bill structure and (2) birds lacking glands presumably keep their feathers in as good condition as those species possessing those glands. Throughout much of the literature on uropygial glands, one finds the recurring suggestion that powder down somehow fulfills the function of oil from glands in those species where the gland is small or absent (Bartlett 1861, Nitzsch 1867, Newton 1893-1896, Verheyen 1956/, Voitkevich 1966, Jacob 1978, Goodwin 1983). This presumed correlation arose, I believe, because observers were seeking functional replacements in those birds either lacking glands or possessing small glands. Goodwin (1983: 27), for example, reports for pigeons, The powder down . . . appears to AVIAN UROPYGIAL GLAND 253 function in lieu of preen oil to aid in waterproofing of the feathers.' Verheyen (1956/, 19570) variously describes the glands of Psittaciformes and Columbidae as being in a 'phase of regression' or 'deficient,' somehow compensated by 'a lot of powder.' This correlation argument contains a number of basic flaws, i.e., unproven assumptions (1) that a small gland produces insufficient oil and (2) that the oil and powder down are used more or less interchangeably for waterproofing feathers especially in land birds. It should be emphasized that virtually nothing is known about the quantity, rate of production, or rate of secretion of uropygial oils. Without experimental documentation, it cannot be assumed that small glands have any reduction in rate or quantity of secretion, whether the bird has powder down or not. It is true that birds known to produce a significant amount of powder down (Gadow 1891, Chandler 1916, Thomson 1964, Jacob 1978, Baumel et al. 1979) tend to have relatively small glands: (gland weights as a percent of body weight) Ardeidae (N = 20, x = 0-29%), Psittacidae (N = 41, x = 0- \Q%,fide Jacob &Ziswiler 1982 forzoo birds), Ramphastidae(N = 3,x = 0-12%), and Tinamidae (N= 1, 0-\8%fide Jacob & Ziswiler 1982). Relative gland weights are unavailable for other species that produce powder down: Podargidae, Cotingidae, Leptosomatidae, Artamidae, Ptilonorhynchidae, and others. The Mesoenatidae, which have five pairs of powder down patches (Olson 1 978), lack a gland. According to Schuz (1 927), 'powder downs are lacking, or nearly so, in ratite birds;' among the ratites, only Apteryx possesses a gland as an adult. Powder downs, produced in various amounts are known from a wide variety of other birds including Columbidae, Rhynochetidae, Eurypigidae, Podargidae, Otididae, and Accipitridae. This body of circumstantial evidence lends some support to the view that birds with well-developed powder down production have reduced (or no) uropygial glands. A cause-and-effect functional relationship remains unproven, however. Furthermore, the func- tion of powder remains conjectural probably because several types of powder (down) are known: as a waterproof dressing (Bartlett 1861), preserving feathers (Welty 1962), and cleaning feathers (Thomson 1964). Although the powder has a nonwettable property, it is composed largely of keratin, so its functional equivalence to uropygial oils must await experimental proof (see also Lucas & Stettenheim 1972). All this information strongly argues that more research on functions of glandular secretions is badly needed before physiological generalizations can be asserted. Particularly open to question is the function of secretions in terrestrial birds and in bird taxa containing some glandless members (e.g., doves, parrots). Future studies Several biological aspects of uropygial glands merit further investigations because results therefrom could help to explain some of the morphological variations identified in the present monograph. Johansson's studies (1927) indicated a strong genetic component in the inheritance of uropygial glands in Columba livia, as is also suggested from the fact that certain varieties of this pigeon lack glands (Darwin 1900, Levi, 1941, Goodwin 1983). Hutt (1949) reported that mutation of a dominant gene in chickens causes bifurcation of the gland's papilla and that most heterozygotes have no uropygial gland at maturity. The rumpless chickens of Waterton (1836a) presumably had no glands and might have been genetic mutants. Inheritance of double gland papillae were discussed by Kessel (1945) for domestic fowl. Apparently these are the only investigations pertaining to the inheritance of uropygial glands, and further genetic studies might reveal biological relationships to the absence of glands in taxa of wild birds. Another aspect in need of experimental studies is the physiology of gland production, secretion, and its relationship to preening. Nothing is known about either the quantity or rate of secretion of uropygial oils. Some information is available on histology, vascular supply and innervation (Kossman 1871, Paris 1913, Kanwar 1961). Many additional questions are unanswered, however: (1) do birds with large glands (e.g., waterbirds) produce more oil than birds with small glands (e.g., landbirds); (2) is gland oil production stimulated, and at what rate, by physical manipulation with the bird's bill; (3) is there either seasonal or daily variation in the quantity or rate of secretion? 254 DAVID W. JOHNSTON Despite some papers that address preening activities in birds (e.g., in penguins, Bekoftet al. 1979, and references therein), little is known about the relationship between gland secretion and types or rates of preening activities that involve this gland. A case in point was the radical statement by Gurney (1913) that Sula bassana does not use its gland in preening, a statement since disputed by Nelson (1978). As indicated in the previous account, attention should be given to functional attributes of glandular secretions, especially in terrestrial birds. Little is known about any relationship between gland shape and the underlying muscles and rectrices. Future research could focus on explaining the several different gland shapes identified in this study especially as those shapes might be related to muscle differences or to placement of the rectrices. A final research need is in embryology, especially post-hatching development as it might relate to function in certain species (a review of the gland's embryology is found in Jacob and Ziswiler 1982). Prior to the report by Pycraft in 1900, it was believed that ratites, with the exception of Apteryx, lack uropygial glands. He found, however, that in both Dromaius novaehollandiae and Rhea americana, a gland exists in both the embryo and nestling, but is absent in the adult. (Those conditions have been verified in the present study). Apparently no one has examined those embryonic glands histologically or functionally. Although no glands have been found in any age group ofStruthio or Casuarius, might some trace or anlage be found by an embryonic-histological study? In other adult birds lacking glands (e.g., Mesoenatidae, Otidae) is there any early embryological development of a gland? Acknowledgments Several organizations provided travel funds from 1970-1986 for this study — National Science Foundation (DEB-79-03687, BSR-82- 14603, suppl. to K. R. McKaye), American Museum of Natural History (Frank M. Chapman Memorial Fund), University of Florida Department of Zoology, and George Mason University Graduate School. Museums visited for examination of spirit collections were: National Museum of Natural History (R. L. Zusi), British Museum (Natural History) in Tring (P. J. K. Burton, G. Cowles, I. C. J. Galbraith), American Museum of Natural History (L. L. Short, A. V. Andors), Field Museum of Natural History (J. W. Fitzpatrick), Museum of Comparative Zoology (R. A. Paynter, Jr.), University of Michigan Museum of Zoology (R. W. Storer), Peabody Museum of Natural History (C. G. Sibley), Manomet Bird Observatory (K. S. Anderson, T. L. Lloyd-Evans), Charles R. Conner Zoology Museum (R. E. Johnson), North Carolina State Museum of Natural History (D. S. Lee), University of Georgia Museum of Zoology (J. E. Cadle), Stovall Museum of Science and Technology (G. D. Schnell, D. W. Mock), and California Academy of Sciences (L. F. Baptista). Some specimens were provided by D. G. Ainley, O. L. Austin, Jr., C. Dau, J. B. Faro, D. Forrester, M. S. Foster, M. J. Gilroy, R. Heath, H. W. Kale, II, B. Kessel, A. M. Lindahl, C. D. Marti, B. W. Miller, D. G. Matthiesen, S. A. Nesbitt, D. S. Peters, W. B. Robertson, Jr., R. W. Schreiber, R. Spenser, and G. E. Woolfenden. Additional specimens and data on glands came from the Tall Timbers Research Station (R. L. Crawford), Busch Gardens (Fla.), Sea World (Fla.), Louisiana State University Museum of Zoology (J. P. O'Neill), and Santa Fe Community College Teaching Zoo (Fla.). The microscopic study of feathers was enhanced by the labours of Ray Bienert and by discussions with Roxie Laybourne. Belinda Gillies supplied information on Atrichornis clamosus, and J. A. Bartle assisted in gathering information on the Acanthisittidae. Julian J. Baumel offered advice on several anatomical details. Caroline Carboni-Vetter kindly translated articles in French, and Elisabeth Egghart, articles in German. Through the years countless valuable specimens and much encouragement came from Pierce Brodkorb and Tony Gilyard. Anne Vale was generous with her time and expertise in locating references in the Rothschild Library at the British Museum of Natural History in Tring. Earlier drafts were read by Storrs Olson, Peter Stettenheim, Vincinz Ziswiler, and Richard Zusi; their suggestions helped to improve the manuscript. Anne O'Malley spent many hours typing and retyping several drafts of the entire manuscript. AVIAN UROPYGIAL GLAND 255 This investigation has also benefitted from numerous discussions with Storrs Olson especially on matters dealing with systematics and pertinent references. I am profoundly indebted to Richard L. Zusi who, over many years, freely offered his time, advice, and suggestions on virtually every aspect of the study. Finally, the study would have been incomplete without the superb illustrations meticulously executed by Esta L. Johnston. Summary The primary goal of this study has been to assemble a complete analysis of the uropygial gland's morphology in representatives of all bird families and subfamilies. Particular attention has been given to correcting erroneous information about glands in the existing literature. Morphological data are included from many avian taxa not previously reported. The largest glands, relative to body weight, are found in birds that swim, dive or rest on water. Progressively smaller glands occur in birds that walk in water, those that habitually only fly over water, and lastly, terrestrial species. Glands are now known to be absent in the Struthionidae (all age groups), Rheidae (adults only), Casuariidae (all age groups), Dromaiidae (adults only), Mesoenatidae, Otidae, Columbidae (9 genera, 28 species), Psittacidae (6 genera, 31 species), Podargus spp., and Picidae (1 genus, 4 species). The absence of glands in these taxa is believed to be a secondary and independent loss. Because only 17 percent of flightless species lack a gland, this study revealed no significant correlation between gland absence and a flightless condition. Many nonpasserine taxa possess tufted glands, whereas others have manifestly naked (non- tufted) glands. Apparently naked glands of others, e.g. Strigidae, actually might bear minute feathers. All species of the Passeriformes have naked glands. Feathers attached to the uropygial gland are more numerous in waterbirds than landbirds and are of two principal types, modified down or modified semiplumes. Only circumstantial evidence was found to support the oft-expressed hypothesis that power down is a substitute for gland secretions in glandless species. The present complete study provides sufficient morphological characteristics for their consideration in avian taxonomic schemes. Future investigations should focus on gland function, especially in terrestrial birds, the quantity and rate of secretion of uropygial oils, relationships between gland production and preening activities, details of feather structure, genetics, and embryological development. Literature cited Arnall, L. & I. F. Keymer. 1975. Bird diseases. Neptune City, New Jersey: T.F.H. Publications. Audubon, J. J. 1 829. Notes on the bird of Washington (Falco Washingtoniand) or Great American Sea Eagle. Magazine of Natural History 1: 1 15-120. Austin, O. L. Jr. 1961 . Birds of the world. New York: Golden Press. Balthazart, J. & E. Schoffeniels. 1979. Pheromones are involved in the control of sexual behaviour in birds. Naturwissenschaften 66: 55-56. Bartlett, A. D. 1861. On the affinities of Balaeniceps. Proceedings of the Zoological Society of London, pp. 131-134. Baumel, J. J., A. S. King, A. M. Lucas, J. E. Breazile, H. E. Evans (eds.). 1979. Nomina anatomica avium. New York: Academic Press. Beddard, F. E. 1898. The structure and classification of birds. London: Longmans, Green & Co. — 1899. Notes on the anatomy of the genus Apteryx. Novitates Zoologicae 6: 386—402. Bekoff, M., D. G. Ainley & A. Bekoff. 1979. The ontogeny and organization of comfort behavior in Adelie Penguins. Wilson Bulletin 91: 255-270. Burton, E. 1822. Observations on the natural history and anatomy of the Pelecanus Aquilus of Linnaeus. Transactions of the Linnaean Society of London, 13: 1-1 1. Burton, P. J. K. 1984. Anatomy and evolution of the feeding apparatus in the avian order Coraciiformes and Piciformes. Bulletin of the British Museum (Natural History) (Zoology) 47: 331^43. 256 DAVID W. JOHNSTON Chandler, A. C. 1916. A study of the structure of feathers, with reference to their taxonomic significance. University of California Publications in Zoology 13: 243-446. Clark, G. A., Jr. 1964. Ontogeny and evolution in the Megapodes (Aves: Galliformes). Postilla No. 78: 1-37. — 1969. Spread-wing postures in Pelecaniformes, Ciconiiformes, and Falconiformes. Auk 86: 136-139. Cottam, P. A. 1957. The pelecaniform characters of the skeleton of the Shoe-bill Stork, Balaeniceps rex. Bulletin of the British Museum (Natural History) (Zoology) 5(3): 49-72. Coues, E. 1890. Handbook of field and general ornithology. London: Macmillan & Co. Cracraft J. 1981. Toward a phylogenetic classification of the recent birds of the world (Aves). Auk 98: 681-714. - 1985. Monophyly and phylogenetic relationships of the Pelecaniforms: a numerical cladistic analysis. Auk 102: 834-853. Crisp, E. 1860. On the structure, relative size, and use of the tail-gland in birds. 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On plumage quantity in birds. Ekologia Polska Ser A 14: 1-7. Tyson, E. 1 863. Anatomy of the Mexico musk-hog. Philosophical Transactions of the Royal Society of London, Ser. A 13: 359-385. Van Tyne, J. & A. J. Berger. 1976. Fundamentals of ornithology. 2nd edition. New York: Wiley & Sons. Verheyen, R. 1955a. Analyse du Potential Morphologique et Considerations sur la Systematique des Coraciiformes (Wetmore 1934). Bulletin. Institut Royal des Sciences Naturellesde Belgique, Vol. 31, No. 31: 1-19. - 19556. Analyse du Potential Morphologique et Considerations sur la Systematique des Coraciiformes (Wetmore 1934). Bulletin. Institut Royal des Sciences Naturelles de Belgique, Vol. 31, No. 92: 1-16. - 1955c. Analyse du Potential Morphologique et Considerations sur la Systematique des Coraciiformes (Wetmore 1934). Bulletin. Institut Royal des Sciences Naturelles de Belgique, Vol. 31, No. 94: 1-16. — \955d. Contribution a la Systematique des Piciformes Basee sur 1' Anatomic Comparee. Bulletin. 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[Classification of flamingos (Phoenicopteriformes) by comparative analysis of their uropygial gland secretions.]. Zeitschrift fur Systematik Evolution 23: 49-58. Waterton, C. 1 832. On birds using oil from glands 'for the purpose of lubricating the surface of their plumage.' Magazine of Natural History 5: 412—415. - 1836tf. On the Robin and Dipper, and rumped, and rumpless birds. Magazine of Natural History 9: 158-159. 18366. The question of the office of the gland upon the rump of birds. Magazine of Natural History 9: 266-269. 1860. The oil-gland in birds. Zoologist 18: 7103-7104. Weller, M. W. 1980. The island waterfowl. Ames, Iowa: Iowa State University Press. Welty, J. C. 1962. The life of birds. Philadelphia, Pennsylvania: W. B. Saunders Co. Willughby, F. 1678. The ornithology of Francis Willughby. Translated by J. Ray. London: A.C. for John Martyn. Wood, C. A. & F. M. Fyfe. 1943. The art of falconry, being the De Arte Venandi Cum Avibus of Frederick II of Hohenstaufen. California: Stanford Unversity Press. Zusi, R. L. 1985. Muscles of the neck, trunk and tail in the Noisy Scrub-bird, Atrichornis clamosus, and Superb Lyrebird, Menura novaehollandiae (Passeriformes: Atrichornithidae and Menuridae). Records of the Australian Museum 37: 229-242. Manuscript accepted for publication 29 February 1988 British Museum (Natural History) The birds of Mount Nimba, Liberia Peter R. Colston & Kai Curry-Lindahl For evolution and speciation of animals Mount Nimba in Liberia, Guinea and the Ivory Coast is a key area in Africa representing for biologists what the Abu Simbel site in Egypt signified for archaeologists. No less than about 200 species of animals are endemic to Mount Nimba. Yet, this mountain massif, entirely located within the rain-forest biome, is rapidly being destroyed by human exploitation. This book is the first major work on the birds of Mount Nimba and surrounding lowland rain- forests. During 20 years (1962-1982) of research at the Nimba Research Laboratory in Grassfield (Liberia), located at the foot of Mount Nimba, scientists from three continents have studied the birds. In this way Mount Nimba has become the ornithologically most thoroughly explored lowland rain-forest area of Africa. The book offers a comprehensive synthesis of information on the avifauna of Mount Nimba and its ecological setting. During the 20 years period of biological investigations at Nimba this in 1962 intact area was gradually opened up by man with far-reaching environmental consequences for the rain-forest habitats and profound effects on the birds. Therefore, the book provides not only a source of reference material on the systematics, physiology, ecology and biology of the birds of Mount Nimba and the African rain-forest, but also data on biogeography in the African context as well as conservation problems. Also behaviour and migration are discussed. At Nimba a number of migrants from Europe and/or Asia meet Afro tropical migratory and sedentary birds. Professor Kai Curry-Lindahl has served as Chairman of the Nimba Research Laboratory and Committee since its inception in 1962. Peter Colston is from the Subdepartment of Ornithology, British Museum (Natural History), Tring, and Malcolm Coe is from the Animal Ecology Research Group, Department of Zoology, Oxford. 1986, 129pp. Hardback. 0565 00982 6 £17.50. Titles to be published in Volume 54 The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences. By Gordon J. Howes A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles. By Keith H. Hyatt & Rowan M. Emberson A revision of Haplocaulm Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives. By Alan Warren Echinoderms of the Rockall Trough and adjacent areas. 3. Additional records. By R. Harvey, J. D. Gage, D. S. M. Billett, A. M. Clark & G. L. J. Paterson A morphological atlas of the avian Uropygial gland. By David W. Johnston Miscellanea Printed in Great Britain by Henry Ling Ltd . at the Dorset Press. Dorchester. Dorset 25NOV1938 PRESENTED GENERAL LIBRAR Bulletin of the British Museum (Natural History) Miscellanea Zoology series Vol 54 No 6 24 November 1988 The Bulletin of the British Museum (Natural History), instituted in 1949, is issued in four scientific series. Botany, Entomology, Geology (incorporating Mineralogy) and Zoology, and an Historical series. V , Papers in the Bulletin are primarily the results of research carried out on the unique and ever-growing collections of the Museum, both by the scientific staff of the Museum and by specialists from elsewhere who make use of the Museum's resources. Many of the papers are works of reference that will remain indispensable for years to come. Parts are published at irregular intervals as they become ready, each is complete in itself, available separately, and individually priced. Volumes contain about 300 pages and several volumes may appear within a calendar year. Subscriptions may be placed for one or more of the series on either an Annual or Per Volume basis. Prices vary according to the contents of the individual parts. Orders and enquiries should be sent to: Publications Sales, British Museum (Natural History), Cromwell Road, London SW7 5BD, England. World List abbreviation: Bull. Br. Mus. nat. Hist. (Zool.) © Trustees of the British Museum (Natural History), 1988 The Zoology Series is edited in the Museum's Department of Zoology Keeper of Zoology : MrJ.F. Peake Editor of Bulletin : DrC.R. Curds Assistant Editor : Mr C. G. Ogden ISSN 0 565 05042 7 ISBN 0007 1498 Zoology series Vol54 No 6 pp 26 1-307 British Museum (Natural History) Cromwell Road London SW7 5BD Issued 24 November 1 988 Miscellanea Contents A review of the copepod endoparasites of brittle stars (Ophiuroida). By G. A. Boxshall . A new genus of tantulocaridan (Crustacea: Tantulocarida) parasitic on a harpacticoid copepod from Tasmania. By G. A. Boxshall Unusual ascothoracid nauplii from the Red Sea. By G. A. Boxshall & R. Bottger-Schnack New nicothoid copepods (Copepoda: Siphonostomatoida) from an amphipod and from deep-sea isopods. By G. A. Boxshall & K. Harrison A new genus of Lichomolgidae (Copepoda: Poecilostomatoida) associated with a phoronid in Hong Kong. By G. A. Boxshall & A. G. Humes Page 261 271 275 285 301 BRITISH MUSEU (NATURAL HISTORY) 25NOVJ988 PRESENTED GENERAL LIBRAI Geoffrey A. Boxshall Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD Summary A new family, the Chordeumiidae, is proposed for six genera of copepods that live as endoparasites of brittle stars. The status of these genera, Chordeumium, Arthrochordeumium, Lernaeosaccus , Ophioicodes, Ophioika and Parachordeumium is reviewed. The genera Ophioithys and Amphiurophilus are recognised as subjective synonyms of Parachordeumium. The sole species of Lernaeosaccus is reinterpreted and redescribed. Examination of the holotype of L. ophiacanthae revealed that it was originally described upside down. Codoba discoveryi is also redescribed from the types but cannot be placed in any of the existing families of the Siphonostomatoida at present. Introduction In his review of copepods associated with invertebrate hosts Gotto (1979) listed eight genera of endoparasites that utilise brittle stars as hosts. None of these has formally been placed in a family and even their ordinal placement is uncertain. There are obvious taxonomic problems concerning these genera which need to be resolved before their phylogenetic relationships with other copepods can be understood. Most of the species contained in these 8 genera have highly transformed females with bizarre body morphology in the adult and few, if any, recognisable limbs. How- ever, in some genera either males or developmental stages are known and these provide more taxonomically useful information. The monotypic genus Codoba Heegaard is much less modified, still retaining a more-or-less cyclopiform facies in the adult female (Heegaard, 1951). Codoba is redescribed, based on the type material, and the taxonomic status and phylogenetic relationships of the other genera endoparasitic in ophiuroids are reassessed. The morphology of the monotypic genus Lernaeosaccus Heegaard is reinterpreted and a new description and diagnosis of the genus is provided. Descriptions Genus CODOBA Heegaard, 1951 DIAGNOSIS. Adult female prosome 4-segmented, slightly swollen; urosome 5-segmented. Caudal rami distinct, bearing 6 setae. Antennule 20-segmented, lacking aesthetascs. Antenna reduced to unarmed process. Mouth tube well developed. Mandible stylet-like, without teeth; palp absent. Maxillule bilobed, inner lobe with 1, outer with 2 setae. Maxilla with distal recurved claw. Maxilliped 3-segmented. Legs 1-4 biramous, rami medially directed, intercoxal sclerites absent. Leg 5 lacking. Male unknown. TYPE SPECIES. Co doba discoveryi Heegaard, 1951 bymonotypy. Codoba discoveryi Heegaard, 1951 ADULT FEMALE. Body (Fig. 1 A) slightly transformed cyclopiform, but with distinct segmentation. Prosome swollen, comprising cephalothorax incorporating first pedigerous somite, and 3 free pedigerous somites. Total body length of figured syntype 1-97 mm. Each free pedigerous somite with a pair of posterolaterally directed epimeral processes. Urosome short (Fig. IB), comprising Bull. Br. Mus. not. Hist. (Zool.) 54(6): 261-270 Issued 24 November 1988 262 G. A. BOXSHALL COPEPOD ENDOPARASITES OF BRITTLE STARS 263 somite of leg 5 (95 x 398 urn), the genital complex (130xl30um), 2 postgenital somites (40x235(im, 25xl90um) and the anal somite (115xl50um). Genital apertures unarmed; located ventrolaterally on genital complex. Anal somite with row of spinules along posterior margin. Caudal rami (Fig. 1 B) about 1 -5 times longer than wide (80 x 53 um); armed with a lateral seta about at midlength, a naked dorsal seta and 4 distal margin setae, 3 of which are pinnate. Antennule (Fig. 1C) 20-segmented; lengths of segments measured along posterior margin 13, 9, 5, 10, 11, 10, 13, 12, 12,9,9,9, 18, 15, 14, 11, 15, 14, 11 and 61 um; armature elements as follows: 1—3, II— 1, III— 1, IV— 2, V— 2, VI— 1, VII— 1, VIII— 2, IX— 2, X— 2, XI— 1, XII— 1, XIII— 2, XIV— 1, XV— 1, XVI— 1, XVII— 1, XVIII— 1, XIX— 1, XX— 12. No aesthetascs present. The size and number of armature elements on the apical segment indicate that it is derived by fusion of 2 or more segments. Antenna vestigial; reduced to small unarmed process located between base of antennule and mouth tube (Fig. 2F). Mouth tube (Fig. ID) well developed, formed from labrum and labium. Mandible (Fig. IE) stylet-like, unarmed; palp lacking. Maxillule bilobed (Fig. 1 F); inner lobe represented by single hirsute seta; outer lobe short, armed with 2 hirsute setae. Maxilla (Fig. 1G) comprising unarmed syncoxa and distal basis. Basis drawn out into recurved claw, armed distally with patches of denticles as figured. Maxilliped (Fig. 2A) 3-segmented; basal segment armed with a row of spinules; second segment elongate, armed with a single seta and several rows of spinules; third segment bearing a tiny seta proximally on outer margin, a small inner seta and 2 unequal apical spines. Spines dentate, 51 um and 41 jim in length. Fine spinules present around apex. Swimming legs 1 to 4 biramous, positioned on ventral surface of somite with rami directed medially (Fig. IB); intercoxal bars (sclerites) absent. Leg 1 (Fig. 2B) with unarmed protopod; exopod unsegmented, bearing 4 pinnate setae along outer margin, 2 at apex and 2 distally on inner margin; endopod indistinctly 2-segmented, bearing 4 pinnate setae along inner margin, 2 at apex and 1 distally on outer margin. Leg 2 (Fig. 2C) with unarmed protopod. Exopod 2-segmented; first segment with outer pinnate seta, second with 4 naked setae on outer margin, 1 at apex and 2 on inner margin. Endopod unsegmented; with 5 pinnate setae along inner margin and 2 at apex. Leg 3 (Fig. 2D) with unarmed protopod; both rami indistinctly 2-segmented. Exopod with outer seta on first segment, second with 2 outer and 2 apical setae, and a row of spinules medially; endopod with 2 inner margin setae on first segment; second with 1 inner, 1 outer and 2 apical setae. Leg 4 (Fig. 2E) with unarmed protopod; exopod with single apical seta; endopod with 2 setae on inner margin and 3-branched spinous projection apically. Leg 5 lacking. Egg sacs lacking, eggs loose inside capsule with adult female. Capsule of specimen 1987.244 containing 44 eggs; eggs large, lecithotrophic, diameter approximately 190 um. MATERIAL EXAMINED. Syntypes: Dissected syntype (BM(NH) No. 1987.243) collected from Ophiura meridionalis (Lyman) at Discovery Stn 123, in 230-250 m off South Georgia, 15.12.1926. Intact syntype (BM(NH) No. 1987.244) from O. meridionalis at Discovery Stn 156, in 236m off South Georgia, 20.1.1927. Third syntype an empty capsule (BM(NH) No. 1987.245) collected from Amphiura belgicae Koehler at Discovery Stn 1 60, in 1 77 m off South Georgia, 7.2. 1 927. These are the data on the labels with the specimens and do not correspond in some details with those data published by Heegaard (1951). REMARKS. When Heegaard (1951) erected the genus Codoba he indicated that new families would probably have to be established to accommodate the copepods parasitic on echinoderms but felt that it would be premature to do so in view of the lack of knowledge of the group. The high number of antennulary segments in Codoba is a plesiomorphic character and is typical of the family Asterocheridae but the genus cannot be referred to the Asterocheridae as it lacks a mandibular palp and an aesthetasc on either the penultimate or antepenultimate segment of the antennule. Fig. 1 Codoba discoveryi Heegaard, 1951. Adult female syntype. A, dorsal; B, Fourth pedigerous somite and urosome, ventral; C, Antennule, ventral; D, mouth cone and maxillule, anteroventral; E, Mandible, anterior; F, Maxillule, lateral; G, Maxilla, posterior. Scale bars lOOum unless otherwise stated: A = 1 mm, B = 200 um, c = 50 um. 264 G. A. BOXSHALL B mnd mxl ant COPEPOD ENDOPARASITES OF BRITTLE STARS 265 These are regarded as diagnostic characters for the Asterocheridae by Stock (1987). The very reduced antenna is rare in siphonostomatoids, occurring mainly in species of the Nicothoidae. However, Codoba is not related to the Nicothoidae which primitively have reduced antennules and a well developed antenna. The typical subchelate antenna of siphonostomatoids is primarily an organ for grasping the host and its reduction is here interpreted as an adaptation to endoparasitism. Subject to a full review of the families of siphonostomes parasitic on invertebrates, which is in progress, the genus Codoba is left unassigned to any of the families recognised at present. Review of other endoparasitic genera and species AMPHIUROPHILUS Delamare Deboutteville, 1962 In his revision of the members of the family Philichthyidae parasitic on European fishes Delamare Deboutteville (1962) correctly removed Philichthys amphiurae Herouard, 1906 from the genus Philichthys Steenstrup, 1862 on the basis of differences in male morphology. He established a new genus, Amphiurophilus, to accommodate Philichthys amphiurae. Amphiurophilus is a junior objective synonym of Ophioithys which was established by Heegaard in 1951 with the same type species, Philichthys amphiurae of Herouard (1906). It is a subjective synonym of Parachordeumium Le Calvez, 1938 (see below). ARTHROCHORDEUMIUM Stephensen, 1918 DIAGNOSIS. Postmetamorphosis adult female highly transformed; body somewhat dorsoventrally compressed, indistinctly segmented and with short, paired lateral processes. Two pairs of limbs present; antennules and maxillae. Antennules unsegmented, bifid at tip. Maxillae 3-segmented, including terminal claw. Egg masses irregularly wrapped around body. Male and copepodid unknown. TYPE SPECIES. Arthrochordeumium appendiculosum Stephensen, 1918 (by subsequent designation, Stephensen, 1933). This is a valid genus established by Stephensen (1918) for A. appendiculosum. A second species, Arthrochordeumium asteromorphae, was described by Stephensen (1933). CHORDEUMIUM Stephensen, 1918 DIAGNOSIS. Postmetamorphosis adult female moderately transformed; body cylindrical with paired lateral swellings on genital complex only; segmentation distinct. Median process present posterodorsally on genital complex. Three pairs of cephalic appendages present. Antennules unsegmented, bifid at tip. Antennae reduced to papilliform processes. Maxillae 3-segmented, including terminal claw. Legs 1 to 4 represented by slender, laterally-directed processes. Egg mass extruded posteriorly into cyst surrounding parasite. Adult male similar to female in general fades but with better defined segments. Posterodorsal median process absent. Testes paired. Copepodid stage without discrete caudal rami, caudal setae located on margin of anal somite. TYPE SPECIES. Chordeumium obesum (Jungersen, 1912). This genus was proposed by Stephensen (1918) as a replacement name for Chordeuma of Jungersen (1912). Chordeuma was preoccupied for a genus of Myriapoda (Kock, 1847). The type species, Chordeuma obesum, described by Jungersen (1912,1914) becomes the type species of Chordeumium by monotypy. Fig. 2 Codoba discoveryi Heegaard, 1951. Adult female syntype. A, Maxilliped, posterior; B, Leg 1, ventral; C, leg 2, ventral; D, leg 3, ventral; E, leg 4, ventral; F. Area between mouth cone and antennule showing antenna (ant), mandible (mnd) and maxillule (mxl). All scale bars 100 urn. G. A. BOXSHALL B mx Fig. 3 Lernaeosaccus ophiacanthae Heegaard, 1951. Holotype female. A, lateral; B, ventral view showing antennules (atl), presumed maxillae (mx) and legs 1-4 (1-4); C, Posterior end of body, posterodorsal view showing median abdominal process and position of detached egg. Scale bars 1 mm unless otherwise stated: c = 0-25 mm. LERNAEOSACCUS Heegaard, 1951 DIAGNOSIS. Postmetamorphosis adult female sac-like, lacking external segmentation. Single pair of lateral processes present on trunk. Posterior end concave containing a median posterior lobe. Lobate antennules and vestigial maxillae present anteriorly. Swimming legs 1-4 reduced to tiny, posteriorly directed lobes. Eggs large, released into masses surrounding female. Male and copepodid stages unknown. TYPE SPECIES. Lernaeosaccus ophiacanthae Heegaard, 1951 (by monotypy). Lernaeosaccus ophiacanthae Heegaard, 1951 POSTMETAMORPHOSIS FEMALE. Body (Fig. 3A) highly transformed, lacking distinct segmentation COPEPOD ENDOPARASITES OF BRITTLE STARS 267 and tagmosis. Body swollen, rounded anteriorly and dorsally, flattened ventrally and concave posteriorly. Total body length of holotype 2-87 mm. Posterior part of body of holotype reflexed dorsally, probably due to fixation. Single pair of lateral lobes present posteriorly behind fourth legs (Figs 3 A-B). Concave posterior end containing genital openings, a median abdominal process and a median lobe. The median abdominal process originates close to the genital apertures (Fig. 3C). Eggs located at genital openings removed during examination. Eggs large; maximum diameter 173 um. Egg masses not contained within sacs; wrapped around body within capsule produced by host. Antennules represented by unarmed lobes (Fig. 3B, atl). Oral area obscured on holotype but apparently comprising a median structure and a pair of more posteriorly located limbs (probably maxillae, Fig. 3B, mx). Legs 1-4 present, reduced to unsegmented, unarmed and posteriorly directed lobes on ventral body surface (Fig. 3B, 1-4). MATERIAL EXAMINED. Holotype: Adult female (BM(NH) No. 1982.242) collected from Ophiacantha disjuncta (Koehler) at Discovery Stn 190, in 316m off the Palmer Archipelago on 24.03 . 1 926. The depth and date on the label differ from those given by Heegaard (1951), which were 278 m and 14.03.1926 respectively. REMARKS. This species was described by Heegaard (1951) upside down. The paired structures referred to by Heegaard as maxilliped 2 (Heegaard, 1951: Fig. 4b) are eggs. Dissected from the holotype, they were found to contain a nauplius at an early stage of development but with 3 recognisable pairs of appendages. The structure identified as a mouth cone containing mandibles is here reinterpreted as a median abdominal lobe. The thickening of the cuticle was misinterpreted by Heegaard as the paired mandibles. Close inspection of the trunk of the holotype revealed 4 pairs of posteriorly directed legs that were overlooked by Heegaard (1951). This parasite is closely related to Chordeumium obesum. The body morphology and appendage positioning are very similar. They are maintained as separate genera because of the differences in structure of the posterior part of the body. OPHIOICODES Heegaard, 1951 DIAGNOSIS. Postmetamorphosis adult female highly transformed; body asymmetrical, irregularly shaped and provided with numerous lateral and dorsal processes. No traces of segmentation visible. Female with midventral groove. Male highly transformed; body elongate, unsegmented and with a pair of long, slender lateral processes. Testes paired. Male lies in midventral groove of female. Copepodid stage unknown. TYPE SPECIES. Ophioicodes asymmetrica (Pyefinch, 1940). This is a valid genus. It was established by Heegaard (1951) on the basis of differences in male morphology between Ophioica asymmetrica Pyefinch, 1940 and the other 3 species of Ophioika Stephensen, 1933. He designated Ophioica asymmetrica Pyefinch, 1940 as type. OPHIOIKA Stephensen, 1933 DIAGNOSIS. Postmetamorphosis adult female highly transformed. Body unsegmented, apparently globular due to positioning of about 5 pairs of long lateral processes which curve ventrally. Four to six egg masses held within space enclosed by processes. Pair of small anterior processes possibly representing antennules. No other limbs recognisable. Median conical process may represent oral cone. Males degenerate body form with single well developed testis, male penetrating body of female. Copepodid unknown. TYPE SPECIES. Ophioika ophiacanthae Stephensen, 1933. This genus was established by Stephensen (1933) to accommodate Ophioika ophiacanthae 268 G. A. BOXSHALL Stephensen 1933. This becomes the type species by monotypy. Stephensen (1935) added a second species, Ophioica appendiculata, misspelling the generic name Ophioika. This is corrected here. OTHER SPECIES. Ophioikia appendiculata Stephensen, 1935; Ophioika tenuibranchia Heegaard, 1 95 1 . 0P///0/77/FS Heegaard, 1951 Heegaard (1951) recognised the close relationship between Philichthys amphiurae and the genus Ophioika. He removed this species from Philichthys and proposed a new genus, Ophioithys, with P. amphiurae Herouard, 1906 as type, "i his name is a senior objective synonym of Amphiurophilus as both genera have the same designated type species. This genus is, however, recognised herein as a synonym of Parachordeumium Le Calvez, 1938 (see below). PARACHORDEUMIUM LeCtivez, 1938 DIAGNOSIS. Postmetamorphosis female highly transformed; body symmetrical, unsegmented, lacking limbs except for maxillae. Body with 4 pairs of major lateral processes, sometimes branched, forming enclosure containing egg masses; several paired and/or median papillae present dorsally; abdominal process well developed. Genital apertures paired. Maxillae 3-segmented, including terminal claw. Adult male small, highly transformed, living in permanent association with female; body unsegmented, drawn out into long abdominal process posteriorly, anteriorly with pair of long lateral processes. Maxillae 3-segmented, including terminal claw. Copepodid hatching with 3-pairs of developed biramous legs; lacking discrete caudal rami, caudal setae located on margin of anal somite. Antennules 5-segmented. Antenna 3-segmented, lacking exopod. Maxillae 3-segmented with terminal claw. Other cephalic appendages absent. This is a valid genus established to accommodate a single species, P. tetraceros Le Calvez 1938, which was the type species by monotypy. The dorsal and ventral figures of the adult postmetamor- phosis female P. tetraceros given by Le Calvez (1938) do not differ significantly from the figures in the detailed redescription of Amphiurophilus amphiurae by Goudey-Perriere (1979). Both these species inhabit the genital bursae of the Amphipholis squamata Delia Chiaje in European waters and it is here proposed that they be synonymised. The oldest available name for this species is Parachordeumium amphiurae (Herouard, 1906) and this is the type species of Parachordeumium. TYPE SPECIES. Parachordeumium amphiurae (Herouard, 1906) new combination, (syn. P. tetraceros Le Calvez, 1938). The three new species described by Goudey-Perriere (1979) and placed within the genus Amphiurophilus are here transferred to the genus Parachordeumium. These new combinations are: Parachordeumium bocqueti (Goudey-Perriere. 1 979); Parachordeumium humesi (Goudey-Perriere, 1979); Parachordeumium hendleri (Goudey-Perriere, 1979). REMARKS. The third appendage of the copepodid stage of P. amphiurae (as Amphiurophilus amphiurae was identified as the mandible by Goudey-Perriere (1979). This limb is retained in the adult of both sexes. Its morphology (the segmentation and possession of a terminal claw) is most atypical for a mandible and this limb is here reinterpreted as the maxilla. CHORDEUMIIDAE New Family DIAGNOSIS. Copepods endoparasitic in ophiuroids; adult females more-or-less highly transformed typically losing external segmentation and often with paired lateral and median dorsal or posterior processes. Lateral processes where fully developed forming 'cage' enclosing egg masses. Cephalic appendages reduced or absent; antennules and maxillae typically retained in adult. Antenna sometimes present as vestige in adult. Maxillipeds absent. Legs 1-4 reduced to uniramous pro- cesses or absent. Eggs or eggs masses retained within cyst of host origin enclosing female. Adult male typically transformed, with at most one pair of lateral processes. Maxillae typically retained COPEPOD ENDOPARASITES OF BRITTLE STARS 269 by adult male, sometimes antennules and antennae also. Copepodid larva lacking discrete caudal rami; caudal setae present on margin of anal somite. TYPE GENUS. Chordeumium Stephensen, 1918. OTHER INCLUDED GENERA. Arthrochordeumium, Lernaeosaccus , Ophioicodes, Ophioika and Parachordeumium. Discussion It is difficult to produce a meaningful diagnosis for the new family because so many of the species are extremely modified for their endoparasitic mode of life. Comparison between the better known species, Chordeumium obesum and Parachordeumium amphiurae, provides the best apomorphy for the family, based on the developmental stages. Both C. obesum and P. amphiurae lack discrete caudal rami in the copepodid stage (Jungersen, 1914; Goudey-Perriere, 1979). This character is rare in copepods and serves to link Chordeumium and Parachordeumium. This relationship is central to the definition of the family because the former genus shares several characters (the structure of the antennules and maxillae in the adult female, for example) with Arthrochordeumium and the latter, several characters of gross female morphology (the possession of paired lateral processes enclosing the egg masses, for example) with the genera Ophioicodes and Ophioika. The genus Lernaeosaccus, now reinterpreted, is apparently closely related to Chordeumium. Both genera have retained legs 1-4 as tiny lobes in the adult female, both have a pair of lateral processes posteriorly and both have a median abdominal process located just posterior to the gonopores. The new family is placed in the order Siphonostomatoida on the basis of the reports of a mouth cone in Ophioika by Stephensen (1935). The mouth cone described by Heegaard (1951) in Lernaeosaccus is an abdominal process. It is probable that the highly modified female body from has been derived independently within the family, from a siphonostomatoid precursor that moved freely over the surface of the brittle stars. The species of the family Cancerillidae are typically ectoparasites of brittle stars (Emson et al., 1985) and the family Asterocheridae contains species that live in the stomach of basket stars (Humes, 1986). A common ancestor shared with either of these families could have made the step towards a specialised endoparasitic existence. A relation- ship with the highly transformed families of fish parasites, such as the Chondracanthidae, Lernaeopodidae and Philichthyidae, is regarded as extremely improbable. The endoparasitic Cucumaricola notabilis Paterson, 1958 may be closely related to the Chordeumiidae. The highly transformed morphology of the adult female, with its paired lateral processes, resembles that of the chordeumiids. Also, this species retains only the antennules, antennae and maxillae in the adult female (Paterson, 1958), as in Chordeumium itself. It differs from the new family in having discrete caudal rami in the copepodid stage, although the presence of 5-segmented antennules at this stage is another similarity between Cucumaricola and Parachordeumium. Acknowledgement The author is grateful to Prof. Jan Stock (University of Amsterdam) for his valuable comments on the manuscript. References Delamare Deboutteville, C. 1962. Prodrome d'une faune d'Europe des Copepodes parasites de poissons. Les Copepodes Philichthyidae (Confrontation des donnees actuelles). Bulletin du Musee Oceanographique de Monaco 59: 3-44. Emson, R. H., Mladenov, P. V. & Wilkie, I. C. 1985. Studies of the biology of the West Indian copepod Ophiopsyllus reductus (Siphonostomatoida: Cancerillidae) parasitic upon the brittle star Ophiocomella ophiactoides. Journal of Natural History 19: 151-171. 270 G. A. BOXSHALL Gotto, R. V. 1979. The association of copepods with marine invertebrates. Advances in Marine Biology 16: 1-109. Goudey-Perriere, F. 1979. Amphiurophilus amphiurae (Herouard). Crustace Copepode parasite des bourses genitales de 1'Ophiure Amphipholis squamata Delia Chiaje, Echinoderme: morphologic des adultes et etude des stades juveniles. Cahiers de Biologic Marine 20: 201-230. Heegaard, P. 1951. Antarctic Parasitic Copepods and an Ascothoracid Cirriped from Brittle-stars. Videnskabelige Meddelelserfra Dansk Naturhistorisk Forening i Kjobenhavn 113: 171-190, pi. I-II. Herouard, E. 1906. Sur un nouveau Copepode parasite d'Amphiura squamata. Compte Rendu Hebdomadaire des Seances de V Academic des Sciences, Paris 142: 1287-1289. Humes, A. G. 1986. Two new species of Copepoda associated with the basket star Astroboa nuda (Ophiuroidea) in the Moluccas. Zoologica Scripta 15, 323-332. Jungersen, H. F. 1 9 1 2. Chordeuma obesum, a new parasitic copepod endoparasitic in Aster onyx loveni. Report. British Association for the Advancement of Science, 82nd Meeting (1912): 505-506. — 1914. Chordeuma obesum, a new parasitic copepod endoparasitic in Asteronyx loveniM. Tr. Mindeskrift for Japetus Steenstrup. 1 (16): 1-19, pi. I-II. Le Calvez, J. 1938. Parachordeumium tetraceros n. gen. n. sp., Copepode gallicole parasite d'une ophiure de Villefranche-sur-Mer. Compte Rendu du Congres des Societes savantes de Paris, Section des Sciences 71: 259-263. Paterson, N. F. 1958. External features and life cycle of Cucumaricola notabilis nov. gen. et sp., a copepod parasite of the holothurian Cucumaria. Parasitology 48: 269-290. Pyefinch, K. A. 1940. The anatomy oWphioica asymmetrica, sp. n., a Copepod endoparasitic in an Ophiuroid. Journal of the Linnean Society of London 41: 1-19. Stephensen, K. 1918. On a gall-producing parasitic Copepod infesting an Ophiurid. Videnskabelige Meddelelserfra Dansk Naturhistorisk Forening i Kjobenhavn 69: 263-275. - 1933. Some new Copepods, parasites of Ophiurids and Echinids. Videnskabelige Meddelelserfra Dansk Naturhistorisk Forening i Kjobenhavn 93: 197-213. 1935. Two Crustaceans (a Cirriped and a Copepod) endoparasitic in Ophiurids. Danish Ingolf- Expedition3(\2):\-\8. Stock, J. H. 1 987. Copepoda Siphonostomatoida associated with West Indian hermatypic corals 1 : associates of Scleractinia: Faviinae. Bulletin of Marine Science 40: 464-^83. Manuscript accepted for publication 3 May 1988 A new genus of tantulocaridan (Crustacea: Tantulocarida) parasitic on a harpacticoid copepod from Tasmania Geoffrey A. Boxshall Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD Introduction There are now eleven described species of Tantulocarida placed in five genera (Boxshall & Lincoln, 1987). One of these, Basipodella Becker, contains two species both of which are parasitic on copepods. The other four genera parasitise tanaid, isopod, cumacean and ostracod hosts. B. harpacticola Becker was described from unidentified harpacticoid hosts caught at depths of 2000 to 5000 m in the Peru Trench in the eastern Pacific (Becker, 1975). B. atlantica Boxshall & Lincoln was found at a depth of about 3000 m in the North Atlantic to the southwest of the Azores, on a copepod belonging to the harpacticoid family Tisbidae (Boxshall & Lincoln, 1983). Whilst examining a collection of harpacticoids from the Bass Strait, off Tasmania, a single specimen of a Stenhelia species was found bearing a tantulocaridan on the side of its urosome (Fig. 1). This specimen, a tantulus larva containing a developing male, is described below as a new genus. Description AUSTROTANTULUS gen. n. DIAGNOSIS. Class Tantulocarida. Tantulus larva with first thoracic tergite partly concealed beneath posterior margin of dorsal cephalic shield; cephalic shield ornamentation comprising longitudinal lamellae and pores; thoracopods 1-5 of tantulus larva biramous, with well developed endites, uniramous leg 6 with coupling spines on protopod; abdomen of tantulus 2-segmented; adult male formed within trunk sac originating posterior to sixth thoracic tergite of preceding stage. TYPE SPECIES. Austrotantulus lincolni gen. et sp. n. ETYMOLOGY. The generic name is derived from the Latin australis meaning South, and tantulus which forms part of the name of the class Tantulocarida. Austrotantulus lincolni gen. et sp. n. TANTULUS LARVA. The body (Fig. 2A) comprises the cephalic shield, 6 free thoracic somites and a 2-segmented abdomen. The body length is 125 um, measured from the tip of the cephalic shield to the posterior margin of the abdomen, excluding the caudal setae. This may be an overestimate because expansion of the trunk sac may have caused separation of the thoracic tergites. The cephalic shield (Fig. 2B) is longer than wide (47 x 32 um) and tapers anteriorly. The rostrum is absent. The oral disc has a diameter of about 1 5 um and is positioned anteriorly so that it is visible in dorsal view. The surface ornamentation of the head, as seen by light microscopy, consists of longitudinal lamellae dorsally and oblique lamella on the downturned ventrolateral margins. Associated with these lamellae are at least 5 pairs of pores, as marked on Figure 2B. Internally a pair of chitinous bars leads towards the central pore of the oral disc. The cephalic stylet is very slightly curved and is about 22 um long. Bull. Br. Mus. not. Hist. (Zool.) 54(6): 271-274 Issued 24 November 1988 272 G. A. BOXSHALL Fig. 1 Austrotantulus lincolni gen. et. sp. n. Holotype tantulus male undergoing metamorphosis attached to its harpacticoid host. Scale bar in um. The 6 free thoracic tergites are not conspicuously ornamented. The first tergite is partly concealed beneath the rear margin of the cephalic shield. Each thoracic somite bears a pair of well developed legs. The 2-segmented abdomen is 27 um in length (Fig. 2C) and is deflected ventrally by the expansion of the trunk sac posterior to the sixth tergite. The first abdominal somite is wider than long (5x13 um), the second longer than wide (21x13 um). The caudal rami are each represented by 1 short and 2 long setae arising from a common base. There are no cephalic appendages. Thoracopods 1 to 5 have a large unsegmented protopod bearing a single endite which originates at the proximal rim of the limb. The armature of the endites cannot be discerned by light microscopy, but probably resembles that of Deoterthron harrisoni (see Boxshall & Lincoln, 1987). Thoracopods 1 to 5 are biramous. The exopod is 2-segmented and carries 2 apical setae in leg 1 (Fig. 2D). It bears 4 setae apically in legs 2 (Fig. 2E) to 5. The endopod is more than twice as long as the exopod and is indistinctly 2-segmented. The endopod of leg 1 is armed with 2 apical spines only. The endopods of legs 2 to 5 each have the 2 apical spines and, in addition, the proximal segment bears 2 long setae distally on its lateral margin. Leg 6 (Fig. 2F) is uniramous and has a large protopod armed with 2 complex coupling spines on the medial margin. There is no endite. The ramus is 1 -segmented and armed with 2 long, curved setae. MALE. The trunk sac of the holotype contained a male at an intermediate stage of development. This developing male was still attached via the umbilical cord. The tagmosis of the adult male could be discerned only in part, through the wall of the trunk sac. The first 2 pedigerous thoracic somites were fused to the head to produce a cephalothorax of 7 somites and there were 4 free thoracopod- bearing somites. However, the segmentation of the folded abdomen was not visible. A cluster of aesthetascs was present anteriorly on the cephalothorax, as described for the adult male of D. harrisoni. The male was not in a sufficiently advanced state of development for it to be dissected out of the enclosing trunk sac. ETYMOLOGY. The species is named after Roger Lincoln in recognition of his work on the Tantulocarida. MATERIAL EXAMINED. Holotype: <$ tantulus, parasitic on the harpacticoid Stenhelia sp. from fine calcareous mud collected at about 22m depth in the Bass Strait (at approximately 41°00'S 146°00'E), off Round Hill Point, near Burnie on the north coast of Tasmania. BM(NH) Registration No. 1987.418. TANTULOCARIDA 273 Fig. 2 Austrotantulus lincolni gen. et sp. n. A, Holotype, lateral view; B, cephalic shield, dorsal; C, abdomen, dorsal; D, leg 1, posterior; E, leg 2, posterior; F, leg 6, posterior. All scale bars in \am. 274 G. A. BOXSHALL REMARKS. The new genus can be readily distinguished from Basipodella species, which are known to parasitise harpacticoids, by the segmentation of the abdomen. The abdomen is 2-segmented in the tantulus larva of the former and 6-segmented in the latter. Other differences include the general pattern of the surface ornamentation of the cephalic shield. In the new genus this basically consists of a system of longitudinal lamellae whereas in Basipodella species there are conspicuous transverse and longitudinal lamellae. The combination of 2-segmented abdomen in the tantulus, well developed endites and .ami on the tantulus thoracopods, and of longitudinal ornamentation on the cephalic shield is found only in the family Deoterthridae, in species of Deoterthron Bradford & Hewitt. However, the familial position of Austrotantulus is problematical because, whilst the larval characters agree with the familial diagnosis of the Deoterthridae (Boxshall & Lincoln, 1987) the position of the male trunk sac (posterior to the sixth tergite) is typical for the families Basipodel- lidae and Microdajidae. The families Deoterthridae and Microdajidae may have been established prematurely by Boxshall & Lincoln (1987), formalising morphological gaps between taxa which represented a lack of data more than a phylogenetic reality. The new genus is provisionally placed in the family Deoterthridae, although as more taxa are discovered it may become necessary to revise the farrilial arrangement of the tantulocaridans. The area around Tasmania and New Zealand is rich in tantulocaridans. Deoterthron aselloticola Boxshall & Lincoln was described from an isopod host, Hydroniscus lobocephalus Lincoln, caught at 3250-3340 m in the Tasman Sea (Boxshall & Lincoln, 1983) and D. megacephala Lincoln & Boxshall was also found on an isopod, Haploniscus tangaroae Lincoln, taken at 1386m in the Tasman Sea (Lincoln & Boxshall, 1983). The genotype, D. dentatum Bradford & Hewitt, was reported from the ostracod Metavargula mazeri Kornicker collected in 384 m to the east of New Zealand (Bradford & Hewitt, 1980). It is probable that this apparent species richness compared to other geographical regions can be attributed to sampling effort in this recently discovered taxon, rather than to any distinct zoogeographical pattern. Acknowledgement I would like to thank Dr Roger Lincoln for his comments on the manuscript. References Becker, K.-H. 1975. Basipodella harpacticola n. gen., n. sp. (Crustacea, Copepoda). Helgolander Wissens- chaftliche Meeresuntersuchungen 27: 96-100. Boxshall, G. A. & Lincoln, R. J. 1983. Tantulocarida, a new class of Crustacea ectoparasitic on other crustaceans. Journal of Crustacean Biology 3: 1-16. — & — - 1987. The life cycle of the Tantulocarida (Crustacea). Philosophical Transactions of the Royal Society, London, series B 315: 267-303. Bradford, J. M. & Hewitt, G. C. 1980. A new maxillopodan crustacean, parasitic on a myodocopid ostracod. Crustaceana 38: 67-72. Lincoln, R. J. & Boxshall, G. A. 1983. A new species of Deoterthron (Crustacea: Tantulocarida) ectoparasitic on a deep-sea asellote from New Zealand. Journal of Natural History 17: 881-889. Manuscript accepted for publication 11 May 1988 Unusual ascothoracid nauplii from the Red Sea Geoffrey A. Boxshall Department of Zoology, British Museum (Natural History) Cromwell Road, London SW7 5BD Ruth Bottger-Schnack Institut fur Meereskunde, Abtlg. Fischereibiologie, Diisternbrooker Weg 20, D-2300 Kiel, Federal Republic of Germany Introduction The study of larvae is important for elucidating the phylogenetic history of crustacean groups such as the maxillopodans where macroevolutionary events involving progenesis and neoteny may have occurred (Newman, 1983; Boxshall, 1983). It can also reveal homologies between apparently disparate structures such as the attachment disc on the antennule of a cirriped cyprid and the attachment claw on the same limb of an ascothoracid larva (Grygier, 1987a). One maxillopodan taxon, the Facetotecta, is still only known from larvae (see Grygier, 1985, 1987/>). It is therefore, of interest when larvae with clear maxillopodan affinities are discovered which cannot easily be placed in a known group. Grygier (19870) described a 'metanauplius incertae sedis' from the South China Sea which he tentatively identified as a postbrooding ascothoracid, possibly of a laurid (Ascothoracida: Lauridae). During recent plankton studies in the central Red Sea (Bottger, 1987) similar metanauplii were discovered in near surface waters, together with an earlier naupliar stage of what appears to be the same species. These and a similar metanauplius that clearly represents a related but distinct species are described in this paper. Description Nauplius type I Body discoid (Fig. 1 A), convex dorsally and concave ventrally; entirely covered with dorsal shield. Surface of shield (Fig. 1 B) punctuated with pores arranged in bilaterally symmetrical pattern around lateral margins and in irregular rows either side of dorsal midline. Nauplius eye present. Conspicuous dorsal pore present on swelling about in middle of shield. Margins of shield down- turned, provided with extensive ventral band of pores around entire circumference. Posteriorly shield drawn out into paired caudal processes each bearing a small ventral papilla. Papilla with apical pore. Caudal spine originating on ventral surface near posterior margin, 120 urn in length, armed with setules bilaterally. Body dimensions given in Table 1. Paired frontal filaments simple, setiform but with a blunt tip (Fig. 1 A, ff); positioned either side of midline just anterior to bases of antennules; median pore present between filaments. Antennule (Fig. 1 A, all; Fig. 1C) uniramous, 4-segmented. First segment unarmed; second with 1 naked seta; third with 1 plumose seta; fourth segment showing some signs of subdivision near its apex, armed with 5 plumose and 2 naked setae on and around apex. Labrum (Fig. 1A, la) an elongate muscular lobe extending posteriorly from between bases of antennae; bearing several rows of fine spinules around apex. Antenna (Fig. 1A, ant; Fig. 2A) biramous, comprising protopod, 3-segmented endopod and 9-segmented exopod. Protopod with 3 endites; proximal endite small, armed with a few spinules; middle endite strongly developed, produced into 2 spiniform processes with 3 slender setae; distal endite strongly developed, produced into 2 divergent spiniform processes, each armed with spinules, 1 naked seta present on anterior surface and a slender plumose seta distally on medial surface. First endopod segment with 3 naked seta, second with 3, third with 4 at tip. First exopod segment unarmed, second to eighth each armed with a long naked seta, ninth segment with 2 setae, that on apex with a swollen base possible representing a tenth segment. Bull. Br. Mus. not. Hist. (Zool.) 54(6): 275-283 Issued 24 November 1988 276 G. A. BOXSHALL & R. BOTTGER-SCHNACK ff Fig. 1 Red Sea nauplius type I. A, ventral view, showing frontal filaments (ff), antennule (atl), antenna (ant), mandible (mnd), labrum (la), maxillule (mxl) and caudal furca (cf); B, dorsal view; C, antennule, ventral. All scale bars 100 um. Mandible (Fig. 1 A, mnd; Fig. 2B) biramous, comprising protopod, 3-segmented endopod and 6-segmented exopod. Protopod with 2 endites; proximal endite armed with a large hirsute seta, a short spine and some spinules; distal endite armed with 4 stout setae, 3 of them plumose, and a row of long spinules. First endopod segment with 2 rows of long spinules, a naked seta and 2 stout setae ASCOTHORACID NAUPLII 277 bearing long setules, second with 3 naked setae, third with 4 naked setae. First to fifth exopod segments each with a single long seta, that on segment 4 being unusually robust and unilaterally spinulate; sixth segment with 3 naked apical setae. Paired lobes located on ventral body surface just posterior to mandibles; armed with rows of medially directed spinules. Maxillule (Fig. 1A, mxl) represented by a small lobe bearing a long, posteriorly directed, apical seta, a short incurved spine and rows of medially directed spinules. Caudal furca (Fig. 1 A, cf) comprising paired lobes each bearing an inner naked seta and a short outer spine. Table 1 Body dimensions and depth distributions of ascothoracid larvae type I in the central Red Sea. STAGE DEPTH (m) DATE (time) LENGTH (urn) WIDTH (^im) Nauplius 0-50 28.10.80(00:20) 443 350 0-50 05.11.80(15:20) 463 370 20-^0 04.11.80(15:20) 468 344 mean 458 355 Metanauplius 0-50 27.10.80(11:00) 732 591 0-50 05.11.80(00:13) 704 561 0-50 05.11.80(00:13) 728 564 50-100 27.10.80(11:00) 710 609 50-100 19.10.80(13:00) 774 589 50-100 05.11.80(00:13) 743 553 mean 732 578 Metanauplius type I Body discoid (Fig. 2C) convex dorsally, concave ventrally; entirely covered with dorsal shield. Surface of shield ornamented with fine lamellae anteriorly and posteriorly, and punctuated with numerous pores arranged more or less symmetrically in an irregular row either side of the midline and over entire dorsolateral area. Tripartite nauplius eye well developed. Middorsal pore present but less conspicuous than in early nauplius. Posteriorly shield bearing 3 pairs of sensory setules. Equatorial ring of marginal pores on ventral surface of downturned shield margins present. Caudal processes bearing marked papillae both dorsally and ventrally; ventral papilla with an apical pore. Caudal spine 278 um long. Body dimensions given in Table 1 . Frontal filaments as in early nauplius. Antennule (Fig. 3B) uniramous, 6-segmented. First segment unarmed; second and third each with 2 plumose setae, fourth with 3 plumose setae and a prominent angled spine passing obliquely across next segment; fifth segment with 4 long plumose setae, sixth with 4 long naked setae. Labrum as in early nauplius. Antenna (Fig. 4A) biramous, comprising 2-segmented protopod, 3-segmented endopod and 12- segmented exopod. First protopodal segment (coxa) with single well developed endite bearing 2 slender naked setae basally and 2 curved spines apically, one of which is armed with small denticles distally. Second segment (basis) produced into strong endite bearing 2 setulate spines apically, 2 plumose setae present on anterior surface at base of endite. First endopod segment with 3 naked setae and a row of spinules; second with 7 marginal setae and a patch of spinules; third with 4 apical setae. First exopod segment unarmed, second to eleventh each with a long seta, twelfth segment with 1 medial and 1 apical seta, the latter with a swollen base probably representing a thirteenth segment. 278 G. A. BOXSHALL & R. BOTTGER-SCHNACK Fig. 2 Red Sea nauplius type I. A, antenna, medial; B, mandible, medial. Red Sea metanauplius type I. C, dorsal view. Scale bars 100 jam unless otherwise stated. Mandible (Fig. 4B) biramous, comprising 2-segmented protopod, 3-segmented endopod and 7-segmented exopod. First protopod segment (coxa) armed with a large plumose seta, a short spine and some spinules; second armed with 5 stout setae, 4 of which are plumose, and some spinules. First endopod segment bearing 3 stout spinulate setae, second with 6 naked setae, third with 3 ASCOTHORACID NAUPLII 279 unilaterally plumose and 2 naked setae. First exopod segment unarmed; second to fourth each with a long seta; fifth with a robust, unilaterally spinulate seta; sixth with a plumose seta and seventh with 3 plumose setae. Maxillule (Fig. 3C) 2-segmented; first segment fused with body surface, armed with rows of Fig. 3 Red Sea metanauplius type I. A, ventral view, with setae omitted from anterior limbs on left side; B, antennule, medioventral; C, maxillule, ventral. Scale bars 100 ^m unless otherwise stated. 280 G. A. BOXSHALL & R. BOTTGER-SCHNACK Fig. 4 Red Sea metanauplius type I. A, antenna, medial; B, mandible, medial. All scale bars 100 \im. medially directed spinules that extend onto body; second segment bearing 2 short medial setae, 3 subapical setae on ventral surface and 3 distal margin setae. Seven pairs of limb buds visible through body wall, marked externally only by tiny sclerotised lobes at the tip of each bud. Limb buds presumably representing maxillae and first to sixth thoracopods of subsequent stage. Caudal furca comprising paired lobes, each bearing a long inner seta and a shorter outer seta. ASCOTHORACID NAUPLII 281 MATERIAL EXAMINED. 3 nauplii and 6 metanauplii collected at and around Valdivia Stn 1 77 (cruise 29) in the central Red Sea (21°25-96'N 38°04-22'E) between 0 and 100 m (see Table 1), in a multiple opening-closing net of mesh 0-1 mm. 1 nauplius and 2 metanauplii stored in the collections of the BM(NH), Reg. Nos 1988.100-102. REMARKS. The metanauplius type I from the Red Sea is very similar to that described from the South China Sea by Grygier (19870). There are small differences in the armature and segmentation of the antenna, mandible and maxillule, in the size of the caudal processes, and in the relative lengths of the caudal spine and setae on the lobes of the caudal furca. However, the basic organis- ation of these larvae is the same. As established by Grygier (19870), their possession of rudiments of 6 pairs of thoracopods implies a maxillopodan affinity. The flattened, bowl-shaped dorsal shield is typical of the Ascothoracida and the possession of an equatorial ring of pores around the shield margin which is found only in some families of Ascothoracida (Grygier, 19870) is here regarded as a derived character. These Red Sea larvae are referred to the Ascothoracida and, on the basis of similarities in the caudal region, possibly to the family Lauridae. Ascothoracid larvae of this type were distributed irregularly in small numbers in the upper 100 m (see Table 1) in the central Red Sea. None was found further north, above the Kebrit Deep. The free swimming nauplius does not contain an obvious store of yolk. This, combined with its highly setose antenna and mandible each bearing well developed gnathobases, suggests that it is a planktotrophic feeder. The metanauplius is about 1-6 times longer than the nauplius and shows a marked increase in the numbers of limb segments. It is inferred from this that there is at least one stage, intermediate in size and limb segmentation, between the two stages described above. The metanauplius is clearly equivalent to the sixth nauplius (NVI) of cirripedes. The primordia of the 6 pairs of thoracopods visible through the integument indicate that the next moult will be to the equivalent of the cyprid stage of development. The presence of a well developed, setose maxillulary rudiment tends to confirm that the metanauplius is equivalent to the cirripede NVI which may have a similar maxillulary rudiment (Moyse, 1987). The earlier nauplius is more difficult to equate precisely with a given nauplius stage of cirripedes. It appears to be a mid-development stage, most likely a NTV because it possesses 2 preaxial setae on the antennule. Whilst antennule segmentation varies within the cirripedes the sequence of appearance of preaxial setae on the antennule is remarkably constant. Typically the number of preaxial setae is 0 in NI-NII, 1 in NIII, 2 in NIV and 3 in NV-NVI. This pattern occurs repeatedly in both lepadomorph cirripedes, such as Capitulum mitella Linnaeus (Yasugi, 1937), and balanomorphs, such as Balanus eburneus Gould (Costlow & Bookhout, 1957) and Tetraclita serrata Darwin (Griffiths, 1979). Also the presence of 4 setae on the apical segment of the endopod of both the antenna and mandible is regarded as typical of the cirripede NIV, although this number does vary within the cirripedes. Thus, the free-living, postbrooding phase of ontogeny appears to comprise 3 or more stages. The length of any brooded phase, prior to release of the larvae, is unknown but may be relatively short. This presumed ontogenetic pattern is much less modified than that of any other ascothoracid (data from Grygier, 1984). The discovery of the nauplius stage, probably equivalent to the cirripede NIV, confirms Grygier's (19870) prediction that when ascothoracids release feeding naupliar stages these will resemble late instar cirripede larvae more closely than when nauplii are brooded. Metanauplius type II A single metanauplius (Fig. 5) was found which differed significantly from that described above. It is 808 um in length and has the same basic organisation. The primordia of the maxillae and 6 pairs of thoracopods are visible through the integument but are smaller and more anteriorly located than in the above metanauplius. Other differences include: the limbs are relatively smaller, the antennary exopod is only 8-segmented, the mandibular exopod is only 5-segmented, the nauplius eye is lacking, the labrum is broader and truncate, the maxillules have 5 setae, the caudal processes are very small, the caudal furca bears 2 subequal pairs of setae, and there is no trace of any median caudal spine. 282 G. A. BOXSHALL & R. BOTTGER-SCHNACK Fig. 5 Red Sea metanauplius type II, ventral view. Scale bar 200 \im. MATERIAL. A metanauplius collected on 23 February 1981 in the central Red Sea (21°23TN 38°04-7'E) during Valdivia cruise 29 between 0 and 50 m, in a multiple opening-closing net of mesh 0-1 mm. Stored in the collections of the BM(NH), Reg. No. 1988.198. REMARKS. This metanauplius is also identified as that of an ascothoracid probably of the family Lauridae, but there are sufficient differences to indicate that it represents a second species from the Red Sea. It differs from the Red Sea metanauplius type I and resembles the metanauplius described by Grygier (1987a) from the South China Sea in the following respects: the segmentation of the antennary and mandibular exopods, the maxillules have 5 setae, the caudal processes are small and the 2 pairs of setae on the caudal furca are subequal in length. It differs from the South China Sea specimen in the lack of a median caudal spine. Acknowledgements Cruise 29 of the RV Valdivia was funded by the Red Sea Joint Commission, Jeddah, and by the Bundesminis- terium fur Forschung und Technologic, Federal Republic of Germany. We are grateful to Dr Mark Grygier for his valuable comments on an earlier draft of the manuscript. References Bottger, R. 1987. The vertical distribution of micro- and small mesozooplankton in the central Red Sea. Biological Oceanography 4: 383-402. ASCOTHORACID NAUPLII 283 Boxshall, G. A. 1983. A comparative functional analysis of the major maxillopodan groups. In: F. R. Schram (Ed.), Crustacean Phylogeny, A. A. Balkema, Rotterdam. 121-143pp. Costlow, J. D. & Bookhout, C. G. 1957. Larval development ofBalanus eburneus in the laboratory. Biological Bulletin 112: 3\3-324. Griffiths, R. J. I. 1979. The reproductive season and larval development of the barnacle Tetraclita serrata Darwin. Transactions of the Royal Society of South Africa 44: 97-1 1 1 . Grygier, M. J. 1 984. Comparative morphology and ontogeny of the Ascothoracida, a step towards a phylogeny of the Maxillopoda. Ph.D. Thesis, University of California at San Diego, 417pp. — 1985. Comparative morphology and ontogeny of the Ascothoracida, a step towards a phylogeny of the Maxillopoda. Dissertation Abstracts International 45(8): 2466B-2467B. - 1987a. Nauplii, antennular ontogeny, and the position of the Ascothoracida within the Maxillopoda. Journal of Crustacean Biology 7: 87-104. 19876. New records, external and internal anatomy, and systematic position of Hansen's Y-larvae (Crustacea: Maxillopoda: Facetotecta). Sarsial2: 261-278. Moyse, J. 1987. Larvae of Lepadomorph barnacles. In: A. J. Southward (Ed.), Barnacle Biology, A. A. Balkema, Rotterdam. 329-362pp. Newman, W. A. 1983. Origin of the Maxillopoda: urmalacostracan ontogeny and progenesis. In: F. R. Schram (Ed.), Crustacean Phylogeny, A. A. Balkema, Rotterdam. 105-1 19pp. Yasugi, R. 1937. On the swimming larvae of Mitella mitella L. Botany and Zoology. Theoretical & Applied. Tokyo 5: 792-796. Manuscript accepted for publication 10 May 1988 New Nicothoid copepods (Copepoda: Siphonostomatoida) from an amphipod and from deep-sea isopods Geoffrey A. Boxshall & Keith Harrison Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD Summary One new genus, Cephalorhiza, and eight new species of parasitic copepods of the family Nicothoidae are described. One new species, Sphaeronella australis, is parasitic in the brood pouch of a lyssianasoid amphipod from southern Australia. All the other new taxa are parasites of deep-sea asellote isopods, from the North Atlantic and Indian Oceans. Two new species belong to the genus Rhizorhina, 4 belong to Diexanthema and one, Cephalorhiza flaccida, to the new genus. Introduction The family Nicothoidae contains eighteen genera of small, highly transformed copepods, all of which are parasitic on other crustaceans. Several of these genera are known either from amphi- pods (Stenothocheres Hansen) or from isopods (Diexanthema Ritchie, Choniorhiza Boxshall & Lincoln, Nicorhiza Lincoln & Boxshall), or from both amphipods and isopods (Rhizorhina Hansen, Sphaeronella Salensky). The present account describes a new species of Sphaeronella found in the marsupium of an amphipod from Australia and several new taxa from deep-sea asellote isopods collected in the North Atlantic and Indian Oceans. During an ecological study of the asellotes of the Rockall Trough, off the west coast of Scotland, about 15,500 asellote isopods were examined. Only four specimens harboured nicothoid parasites, which were found to represent four new species. Examination of additional material from the Porcupine Seabight and from the collections of the Centre National de Tri d'Oceanographie Biologique (CENTOB, Brest) made off the island of Reunion in the Indian Ocean, revealed another three new species, one belonging in a new genus. Descriptions Family NICOTHOIDAE Rhizorhina hystrix sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, simplified to a globular, almost spherical, trunk portion (Fig. IB) and an intricate branching holdfast (Fig. 1 A). Maximum width of globular trunk 859 urn, maximum length 788 um; trunk featureless except for raised gonopores located about 353 um apart on posterior surface. Small anterior swelling tapers towards branching holdfast. Holdfast 4-branched at origin, processes branching irregularly along length. Maximum extent of holdfast within host about 680 um from origin. Arrangement of holdfast branches more or less 2-dimensional within host. MATERIAL EXAMINED. Holotype ?, parasitic on a preparatory female of Eurycope complanata Bonnier (sensu Wilson, 1982). Locality: Discovery Stn 50602 # 2 in the Porcupine Seabight (51°1-0'N 13°7-2'W), depth 1955-1980 m, 07.vii.1979. Parasite located on arthrodial membrane between tergites of pereon segments 3 and 4. Holotype stored in BM(NH), Reg. No. 1987.435. Bull. Br. Mus. nat. Hist. (Zool.) 54(6): 285 299 Issued 24 November 1988 286 G. A. BOXSHALL & K. HARRISON B Fig. 1 Rhizorhina hystrix sp. n., Holotype female. A, Posterodorsal view of oral rootlet system; B, Trunk sac, showing point of attachment to rootlet system. Rhizorhina aesthetes sp. n., Holotype copepodid. C, Dorsal; D, Maxillule, lateral; E, Maxilla, posterior. Scale bars 200 urn, unless otherwise stated: C = 50 um, D = 10 urn, E = 20 urn. NICOTHOID COPEPODS 287 ETYMOLOGY. The species is named after the Porcupine seabight where it was collected. REMARKS. It is difficult to characterise parasites that have undergone such a metamorphic reduc- tion as Rhizorhina species. Four species of Rhizorhina have been described: R. ampeliscae Hansen from the amphipods Ampelisca diadema (Costa) and A. brevicornis (Costa), R. serolis Green from the isopod Serolis bromleyana Suhm, R. leptostracae Gotto from the leptostracan Nebaliella caboti Clark and R. tanaidaceae Gotto from the tanaid Leviapseudes hanseni (Lang). Small differences in size and shape of the trunk are given in Table 1 . The new species is much smaller than R. serolis and also differs from this species in shape (Green, 1959). It is considerably larger than both R. leptostracae and R. tanaidaceae, which also differ in shape, the former being somewhat flattened dorsoventrally and the latter subquadrate in dorsal aspect (Gotto, 1984) in comparison with the Table 1. Morphometrics of the adult females of Rhizorhina species. GONOPORES MAY WIDTH LENGTH SHAPE POSITION SEPARATION R. ampeliscae 1-05 mm 0-96 mm subspherical posterior 187 urn R. serolis 2-5 mm 2-0 mm subrectangular posterior 1-2 mm R. leptostracae 552 urn 521 urn discoid posterior 205 urn R. tanaidaceae 594 um 500 n.m subquadrate posterior 258 urn R. hystrix 859 urn 788 urn subspherical posterior 353 urn R. aesthetes 282 urn 304 urn subspherical ventral 132 urn almost spherical shape of R. hystrix. In size and shape the new species most closely resembles R. ampeliscae (Hansen, 1892). They can be distinguished on the basis of the much wider separation of the gonopores in R. hystrix. The branching holdfast system is probably not a good taxonomic character. It has rarely been described and may well vary according to position in the host, as has been described for the holdfasts of other mesoparasitic copepods (Fryer, 1961; Boxshall, 1989). It is noteworthy that the holdfast is basically 4-branched in both the new species and in R. serolis according to Green (1959). These branches are probably derived from the divided labrum and labium as found by Lincoln & Boxshall (1983) in the closely related Nicorhiza. Rhizorhina aesthetes sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, comprising globular trunk and branching holdfast. Trunk (Fig. 2A) subspherical, longer than wide; maximum width 282 urn, maximum length 304 um. Trunk lacking appendages, featureless except for gonopores located 132 urn apart on ventral surface, just posterior to midlevel. Holdfast broken off in host. COPEPODID STAGE. Body comprising 2-segmented prosome and 3-segmented urosome (Fig. 1C). Total body length 136 um, maximum width 75 um. First urosome somite bearing pair of setules dorsally and pair of setae posterolaterally representing the third swimming legs. Caudal rami about as long as wide; armed with a dorsal seta, lateral seta and 3 distal margin setae, all naked. Antennules 3-segmented (Fig. 2B); armature as follows: 1-1,11-1 + 1 aesthete, III-6+ 1 aesthete. Aesthete on second segment inflated proximally and distally, with mid-level constriction. All setae naked. Antenna absent. Mandible stylet-like, without apical teeth, palp absent. Maxillule (Fig. ID) reduced to simple lobe bearing 2 apical naked setae. Maxilla (Fig. IE) 2-segmented; basal segment unarmed, second segment bearing a terminal claw 19um long and seta 9 urn long. Maxilliped (Fig. 2C) 5-segmented, including terminal claw. Fourth segment bearing seta 7 um long and the terminal claw 24 um in length. 288 G. A. BOXSHALL & K. HARRISON Fig. 2 Rhizorhina aesthetes sp. n. A, Paratype female trunk, ventral; B, Holotype copepodid antennule, ventral; C, Maxilliped, posterior; D, leg 1, anterior; E, leg 2, anterior. Scale bars 20 um, unless otherwise stated: A = 100 um Swimming legs 1 and 2 biramous, with 1 -segmented rami. Leg 1 (Fig. 2D) exopod bearing 2 spines and 5 setae; endopod with 5 setae. Leg 2 (Fig. 2E) exopod bearing 2 spines and 4 setae, endopod with 4 setae. Leg 3 represented by posterolateral setae on surface of first urosomal somite. MATERIAL EXAMINED. Holotype copepodid, 1? paratype. Parasitic on an unidentified ischnomesid (a fragment only). Locality: the Scottish Marine Biological Association's (SMBA) 'Permanent NICOTHOID COPEPODS 289 Stn', sample ES172, in the southern Rockall Trough (54°39'N 12°17'W), depth about 2910m, 27. v. 1980. Adult female attached dorsolaterally to tergite of second pereon somite. Types stored in BM(NH), Reg. Nos 1987.436 (Holotype) and 1987.437 (paratype). ETYMOLOGY. The species name refers to the large aesthete present on the second antennulary segment. REMARKS. The new species is the only Rhizorhina described in which the adult female is longer than broad (see Table 1). This difference in shape, together with the small size of the trunk and the ventral position of the gonopores are sufficient to distinguish the female from other known species. The copepodid larva has 3-segmented antennules as in other species of Rhizorhina but, in addition to the usual apical aesthete, there is a conspicuous aesthete on the second segment. Diexanthema nudum sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, comprising a swollen, slightly dorsoven- trally flattened prosome and an unsegmented urosome (Figs 3A, B). Total body length in ventral view 302 urn, maximum width 267 um. Urosome length 75 urn, maximum width 86 um. Prosome bearing well developed mouth cone anteroventrally containing stylet-like mandibles. Paired irregular lobes just anterior to base of mouth cone may represent modified antennae. Other mouth- parts and legs 1-3 absent. Leg 4 represented by pair of minute papillae on ventral body surface. Urosome bearing leg 5 ventrolaterally. Leg 5 comprising a simple unsegmented lobe armed with 3 distal spines (Fig. 3B). Gonopores large and unarmed, opening on posterior surface of urosome. Postgenital abdominal segments reduced to small, median lobe on posterior surface of urosome. Caudal setae lacking. MATERIAL EXAMINED. Holotype 9, parasitic on a species of the desmosomatid Mirabilicoxa, probably M. acuminata Hessler. Locality: SMBA Stn ES10 in the central Rockall Trough (56°37'N 11°04'W), depth about 2540m, 04.vii.1973. Only one host specimen was infected out of a total of 61 examined from the Rockall Trough. Holotype stored in BM(NH), Reg. No. 1987.438. ETYMOLOGY. The species name refers to the absence of cuticular hairs from the surface of the prosome. REMARKS. The new species is closely related to D. bathydiaita Ritchie, a parasite of a species of Nannoniscus found in deep water off the western coast of Africa (Ritchie, 1975). The postmetamor- phosis female of both species have the same gross morphology and both possess a mouth cone containing mandibles, an irregular branching structure derived from the antennae and a lobate fifth leg armed with 3 spines. The species differ in the presence of caudal setae and of a covering of minute hairs over the cuticle of the prosome in D. bathydiaita (Ritchie, 1975). The tiny papillae representing the fourth legs of the new species are not figured for D. bathydiaita but they may have been overlooked. The host isopod is probably referable to M. acuminata described from the Gay Head-Bermuda transect off the eastern coast of the U.S.A. at depths of 3834 to 4800 m (Hessler, 1970). It differs only in having a lower pereopodal setal count in the preparatory female. Diexanthema corrugatum sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, comprising a swollen, globular prosome and a small unsegmented urosome (Fig. 3C). Total body length in ventral view 536 um, maximum width 507 um. Urosome length 107 um, maximum width 134 um. Oral area of holotype damaged, mouth cone not observed. Irregular branching structure present in a semicircle around oral area probably representing modified antennae. Other mouthparts absent. Leg 1 represented by pair of minute papillae on ventral surface of prosome posterior to oral region. Leg 3 represented by pair of naked setae located ventrolaterally. Leg 4 a free segment bearing 2 apical setae. Leg 5 absent. Gonopores unarmed, opening on posterolateral surface of urosome. Caudal setae lacking. 290 G. A. BOXSHALL & K. HARRISON MATERIAL EXAMINED. Holotype ?, parasitic on an as yet undescribed new species of the eurycopid Acanthocope. Locality; SMBA 'Permanent Stn' in the southern Rockall Trough (54°39'N12°17'W), depth about 2900m, 07.iv.1977. Only one host specimen was infected out of a total of 1 1 1 examined from the Rockall Trough (84 from the Permanent Stn). Holotype stored in BM(NH), Reg. No. 1987.439. B Fig. 3 Diexanthema nudum sp. n., Holotype female. A, Ventral view; B, Lateral view. Diexanthema corrugatum sp. n., Holotype female. C, Ventral view. Scale bars A, B= 100 urn, C = 200 jam. NICOTHOID COPEPODS 291 ft Fig. 4 Diexanthema ritchiei sp. n., Holotype female. A, Ventral view. Diexanthema apoda sp. n., Holotype female. B, Dorsal view of female attached to pereopod of host, showing 4 oral rootlets inside limb; C, Lateral view; D, Urosome, ventral. Scale bars A, D= 100 jim, B, C = 200 \im. ETYMOLOGY. The species name refers to the highly furrowed cuticle of the prosome. REMARKS. The new species is placed in Diexanthema because it possesses a globular prosome and an unsegmented urosome as in the preceding species. It differs from the three described species of Diexanthema in the structure of the third and fourth legs of the adult female. These legs are absent 292 G. A. BOXSHALL & K. HARRISON from D. desisloma Ritchie and D. bathydiaita (Ritchie, 1975) and absent (leg 3) or reduced to minute papillae (leg 4) in D. nudum. The third and fourth legs strongly resemble those ofNicorhiza species but the new species cannot be placed in this genus because of its truncated urosome. Nicorhiza species have a long, 4-segmented urosome (Lincoln & Boxshall, 1983). The host occurs widely in the southern Rockall Trough between 2076 and 2925 m. It is clearly distinguishable from other described species of Acanthocope. Diexanthema rltchiei sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, comprising a swollen, globular prosome and an unsegmented, slightly dorsoventrally flattened urosome (Fig. 4A). Total body length in ventral view 426 urn, maximum width 307 um. Urosome length 61 urn, maximum width 108 um. Prosome without recognisable mouthparts or legs. Irregular branching structure present anterior to oral area may represent antennae as in other species of Diexanthema. Conical structure present in oral region interpreted as broken base of oral rootlets. Urosome bearing leg 5 anteroventrally. Leg 5 a simple lobe bearing 3 spines distally. Gonopores on posterolateral surface, each armed with 2 tiny setules. Posterior margin of urosome slightly concave, without trace of postgenital segments or caudal setae. MATERIAL EXAMINED. Holotype 9, parasitic on juvenile female of the ischnomesid Haplomesus tenuispinus Vanhoffen. Locality: Discovery Stn 50604 # 1 in the Porcupine Seabight (50°6.2'N 13°52'W), depth 3490-3550 m, O4.vii. 1979. Holotype stored in BM(NH). Reg. No. 1987.440. ETYMOLOGY. The species is named after the late Larry Ritchie, who established the genus Diexanthema. REMARKS. The new species is placed in Diexanthema because of the gross body form, a swollen prosome and an unsegmented urosome. It possesses no obvious appendages on the prosome. The irregular branching structure anterior to the oral area is found in all other Diexanthema species except D. desistoma. D. ritchiei differs from other species in the structure of the feeding apparatus. D. desistoma, D. bathydiaita, and D. nudum all possess a typical nicothoid mouth cone containing stylet-like mandibles. The oral region of D. corrugatum was obscured (see above). The conical structure in the oral region of this species was not a typical oral cone. It appeared to be the broken stump of a rootlet system, as found in genera such as Rhizorhina, Choniorhiza and Nicorhiza. No rootlets were found in the host although this was in poor condition. The generic concept of Diexanthema is considerably broadened by the inclusion of this species as it now contains species with an oral cone and species with oral rootlets. The evolution of a rootlet system appears to have occurred independently several times within the Nicothoidae and, in our opinion, the presence of rootlets alone is insufficient to justify generic separation when the gross body morphology is the same. The host, H. tenuispinus, was first described from the Davis Strait and from off the south coast of Greenland (Hansen, 1916). In the present study 228 specimens were examined from depths of 1993 to 2925 m in the southern Rockall Trough. None was infected. Only the specimen taken in the Porcupine Seabight was infected. Diexanthema apoda sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, comprising a swollen prosome and a small unsegmented urosome (Fig. 4B). Total body length in lateral view (Fig. 4C) 529 urn, maximum width 495 um. Prosome extended anteriorly into a subrectangular 'hood'. Four oral rootlets originating on midventral surface of 'hood'. Rootlets unbranched, between 486 and 659 um in length and about 1 2 um in diameter. No other appendages or attachment structures present externally on prosome. Urosome (Fig. 4D) bearing unarmed gonopores ventrolaterally and small abdominal process posteromedially. Leg 5 absent. Caudal setae absent. MATERIAL EXAMINED. Holotype ?, parasitic on a preparatory male of the ilyarachnid Bathybadistes spinosissima (Hansen). Locality: SMBA 'Permanent Stn' in the southern Rockall Trough (54°39'N NICOTHOID COPEPODS 293 Fig. 5 Cephalorhiza flaccida gen. et sp. n., Holotype female. A, Lateral view; B, Tip of head process, dorsal; C, Tip of head process, ventrolateral; D, Urosome, ventral. Scale bars 100 urn, unless otherwise stated: A = 500 urn. 12°17'W), depth about 2910m, 27. v. 1980. A total of 839 specimens of B. spinosissima was examined from the entire Rockall Trough (783 from the 'Permanent Stn'), only 1 was infected. Holotype stored in BM(NH), Reg. No. 1987.441. ETYMOLOGY. The species name refers to the complete absence of any recognisable limbs. REMARKS. This species, like D. ritchiei, has rootlets instead of a typical siphonostomatoid mouth cone. It is even more reduced than D. ritchiei as it has lost the fifth legs but the general configuration of the urosome is the same as in other Diexanthema species. The fifth legs have also been lost in D. 294 G. A. BOXSHALL & K. HARRISON corrugatum. D. apoda differs from all of its congeners in the presence of an anterior 'hood' distinct from the prosome. The host, B. spinosissima, was first described from deep water (2702-3521 m) in and around the Davis Strait (Hansen, 1916). Chardy (1979) also recorded this species (as Ilyarachna spinosissimd) from the Bay of Biscay. It occurred widely in the southern Rockall Trough between 1993 and 2925 m and at the 'Permanent Stn' it was the commonest of the 79 species of asellotes recorded, accounting for 14-7% of the asellote population. Cephalorhiza gen. n. DIAGNOSIS. Nicothoidae. Postmetamorphosis female highly transformed, comprising swollen prosome and small, unsegmented urosome. Prosome bearing stout, somewhat twisted, head process. Head process ornamented with 2 transverse chitinous lamellae dorsally. Oral apparatus carried distally on head process, apparently consisting of rootlets. No recognisable limbs present on prosome or urosome. Urosome unsegmented, bearing gonopores posterolaterally. Median abdominal process present but lacking caudal setae. TYPE SPECIES: Cephalorhiza flaccida gen. et sp. n. REMARKS. The new genus is the nineteenth in the family. It differs from all other genera in the possession of the stout head process which is embedded in the host up to the level of its base. It can be placed in the Rhizorhina group of genera identified by Boxshall & Lincoln (1983). This group now comprises five genera. Rhizorhina, Choniorhiza, Nicorhiza, Diexanthema and Cephalorhiza, and 14 species including those taxa described in the present account. Members of this group have highly transformed adult females and they exhibit the tendency to lose all cephalic appendages and develop oral rootlets. The structure of the urosome of the new genus is similar to that of some Diexanthema species and this is probably its closest relative within the group. Cephalorhiza flaccida gen. et sp. n. POSTMETAMORPHOSIS FEMALE. Body highly transformed, comprising swollen prosome and small, unsegmented urosome (Fig. 5A). Body length 2-34 mm, measured in lateral view round curve from tip of head process to end of urosome. Prosome globular with maximum diameter of 1-01 mm, bearing at its anterior extremity a stout, somewhat twisted, head process. Head process ornamented with 2 transverse chitinous lamellae dorsally (Fig. 5B). Oral apparatus carried distally on head process, apparently consisting of rootlets (Fig. 5C), but broken off in holotype. No recognisable limbs present on prosome or urosome. Irregular branching structure present near oral rootlets similar to the modified antennae of Diexanthema species but located posteriorly to oral region and unlikely to be homologous. Urosome unsegmented; maximum length 129um, maximum width 260 (am. Gonopores unarmed, opening on posterolateral surface (Fig. 5D). Median abdominal process present but lacking caudal setae. MATERIAL EXAMINED. Holotype $, parasitic on preparatory female of Ilyarachna antarctica Vanhoffen; collected during the MD 32 cruise organised by the Terres Australes et Antarctiques Francaises (TAAF, Paris); chef de Mission Alain Guille and sorted by CENTOB, Brest. Locality: Marion-Dufresne Stn DS 106, off Reunion Island (20°47'5S 55°04'5E), depth 1710-1730 m. Holotype stored in Museum National d'Histoire Naturelle, Paris, No. MNHN Cp39. ETYMOLOGY. The genus name is derived from the Greek kephale, meaning a head, and rhiza, meaning root. The species name, derived from the Latin flaccidus meaning flaccid, refers to the posture of the head process. REMARKS. The host has the form of Ilyarachna bicornis as described by Hansen (1916). /. bicornis was synonymised with /. antarctica by Thistle (1980). Sphaeronella australis sp. n. ADULT FEMALE HOLOTYPE. Body subspherical (Fig. 6A) consisting of a small, somewhat dorsoven- trally flattened head and a swollen, almost spherical trunk. Total body length 831 jam, maximum NICOTHOID COPEPODS 295 Fig. 6 Sphaeronella australis sp. n., A, Holotype female, ventral view; B, Paratype male, lateral view. Scale bars A = 200 ^m, B = 100 ^m. width 623 (im. Size variable according to reproductive condition, trunk often much larger when fully gravid. Head dorsoventrally flattened, slightly concave ventrally. Anterior rim of head provided with fine marginal strip of hyaline membrane. Trunk covered with dense coat of tiny denticles. Antennules, mandibles, maxillules and maxillae as for male (see below). Isolated seta present anterior to mouth cone may represent the antenna, absent in male. Ornamentation on surface of 296 G. A. BOXSHALL & K. HARRISON maxilliped arranged into rows on female, rather than irregular as in male. Legs 1-2 comprising a single free segment bearing 2 unequal setae apically. Caudal rami slightly longer than wide, bearing 3 distal setae. ADULT MALE. Body highly transformed (Figs 6B, 7), dorsoventrally flattened, divided into head and small trunk. Body length 477 um, maximum width 311 um. Head naked dorsally and dorsolaterally, trunk covered with a dense coat of fine setules. Setules longer at junction between head and trunk, and at posterior extremity of trunk (Fig. 6B). Anterior margin of head (Fig. 7) complex, with deep indentations separating the median pseudorostrum from the lateral cephalic processes on either side. Margin of lateral cephalic processes armed with fine setules. Lateral margins of dorsal cephalic shield deflected ventrally, armed with row of submarginal setules. Antennule (Fig. 8 A) 3-segmented; first segment with 2 setae, second with 1, third segment with 9 simple setae and a double seta at the apex. Antenna absent. Mandible (Fig. 8B) a simple stylet armed with a marginal membrane distally; palp absent. Maxillule (Fig. 8C) comprising a simple Fig. 7 Sphaeronella australis sp. n., Paratype male, ventral view. Scale bar 100 u NICOTHOID COPEPODS 297 Fig. 8 Sphaeronella australis sp. n., Paratype male. A, Antennule, ventral; B, Mandible, posterior; C, Maxillule, ventral; D, Maxilla, posterior; E, Maxilliped, anterior; F, Maxilliped, posterior; G, Tip of maxillipedal claw, ventral; H, Leg 1, ventral; J, Leg 2, lateral; K, Leg 2, ventral; L, Caudal ramus, ventral. Scale bars 50 urn, unless otherwise stated: A-C = 25 urn. 298 G. A. BOXSHALL & K. HARRISON tapering process, bearing a naked seta proximally, and an isolated seta situated on ventral surface of head near base of maxillulary process. Maxilla (Fig. 8D) 2-segmented; syncoxa robust, armed with single row of stout spinules, basis claw-like, bearing 3 teeth distally and a row of fine setules. Maxilliped (Figs 8E, F) 4-segmented, including the terminal claw; first segment robust armed with many stout spinules on anterior and medial surfaces, and a row of slender setules distally on posterior surface. Second segment unarmed, third bearing the terminal claw and a subapical tricuspid spine. Terminal claw 33 um long, with complex quindentate tip. Two pairs of uniramous swimming legs present. Leg 1 (Fig. 8H) slender, comprising 2 incomple- tely fused segments with the indentation at midlevel marking the line effusion. Proximal segment bearing a naked seta, distal segment armed with 2 transverse rows of fine setules, a short (20 um) subapical spine and a long (70 um), sparsely pinnate, apical spine. Leg 2 (Fig. 8J, K) indistinctly 2-segmented, with deep indentation most apparent in lateral view (Fig. 8J). Proximal part bearing a single seta on a small ventral swelling; distal part with a patch of fine setules, a subapical seta (22 um) and a long (68 um), sparsely pinnate, apical spine. Caudal rami (Fig. 8L) bearing 3 naked setae and a few setules distally. A large female paratype (Museum of Victoria J 1 1 809) had produced 1 9 egg sacs with a mean size of 795 x 681 um (range 699 to 883 um x 589 to 810 um based on 19 measurements). Typical sac measuring 810 x 681 um contained 216 eggs. MATERIAL EXAMINED. Holotype 9, 399 and 1 $ paratypes all parasitic in brood chamber of a species of the lysianassoid genus Amaryllis. Locality: Holotype 9, Port Arthur, Tasmania (43°09'S 147°51E), 29 vii. 1909, Australian Museum (AM) No. P35852. Paratypes: I? (AM No. P35853) off end of South Mole, Arthur Head, Freemantle, Western Australia, depth 6m, 25.xii.1983, coll. J. K. Lowry; 1 9, 1 $ (Victoria Museum (VM) No. J 1 1 809), and 1 9 (J 1 1 8 1 0), FV 'Sarda', Bass Strait Stn 112 (40°22-2'S 145°17'E), depth 40 m, 3.xi.l980, coll. G. C. B. Poore. REMARKS. Sphaeronella contains 76 species, the majority (42 species) parasitic on amphipod hosts. The new species belongs to the S. leuckartii group which Hansen (1897) recognised for the following 9 species, S. antillensis Hansen, S. atyli Hansen, 5". chinensis Hansen, S. danica Hansen, S. leptocheiri Hansen, S. leuckartii Salensky, S. elegantula Hansen, S. messinensis Hansen, and S. vestita Hansen. This number was increased by the description of S. aorae by Scott (1905) and of S. devosae and S. ecaudata by Stock (in Stock & De Vos, 1960). Green (1958) regarded S. elegantula and S. aorae as synonymous with S. leuckartii. This group is characterised by the presence in the male of a conspicuous rectangular projection in the middle of the frontal margin of the head (here referred to as the pseudorostrum), by the rudimentary or absent antenna, and by the presence of a tuft of hairs at the base of the maxillule. Within the group the new species is most closely related to S. chinensis Hansen, which is known from the marsupium of Corophium bonelli Milne-Edwards from Hong Kong. The morphology of the males is very similar, especially in the configuration of the frontal margin of the head. However, the ventral sternal processes in the maxillipedal region of the male are better developed and more widely divergent in S. australis than in S. chinensis. Also the terminal seta on the apex of leg 2 is longer than the limb itself in S. chinensis but shorter than the limb in S. australis. The oral area of the male of the new species had collapsed inwards, thereby retracting the mouth cone so that it is less visible in ventral view. In life it would protrude more, as in the lateral view of S. chinensis given by Hansen (1897). Acknowledgements We would like to thank Dr J. D. Gage (SMBA) for making available material from the Rockall Trough investigations, the Insitute of Oceanographic Sciences for donating the material from the Porcupine Seabight, and Dr M. Segonzac for allowing us to examine CENTOB material. Joan Ellis sorted the parasitised isopods from the Porcupine Seabight material. Thanks are also due to J. K. Lowry (Australian Museum) and G. C. Poore (Victoria Museum) for the loan of S. australis. NICOTHOID COPEPODS 299 References Boxshall, G. A. 1989. Parasitic copepods of fishes: a new genus of Hatschekiidae from New Caledonia, and new records of Pennellidae, Sphyriidae, and Lernanthropidae from the South Pacific and South Atlantic. Systematic Parasitology 13: in press. Boxshall, G. A. & R. J. Lincoln, 1983. Some new parasitic copepods (Siphonostomatoida: Nicothoidae) from deep-sea asellote isopods. Journal of Natural History 17: 891-900. Chardy, P. 1979. Structure of deep sea asellota assemblages in the Bay of Biscay; relationships with the abyssal environment. Ambio Special Report 6: 79-82. Fryer, G. 1961 . Variation and systematic problems in a group of Lernaeid copepods. Crustaceana 2: 275-285. Gotto, R. V. 1984. Two new species of Rhizorhina (Copepoda: Siphonostomatoida) from leptostracan and tanaidacean hosts. Journal of Natural History 18: 81 1-817. Green, J. 1958. Copepoda parasitic on British Amphipoda (Crustacea), with a description of a new species of Sphaeronella. Proceedings of the Zoological Society of London 131: 310-313. - 1959. Sphaeronella serolis Monod, and a new species of Rhizorhina, copepods parasitic on the isopod Serolis bromleyana Suhm (Crustacea). Proceedings of the Zoological Society of London 132: 647-654. Hansen, H. J. 1892. Rhizorhina ampeliscae n. gen., n. sp. En ny til Herpyllobiidae, n. fam., horende Copepod, snyltende paa Amp. laevigata Lilljb. Entomologiske Meddelelser 3: 207-234. — 1897. The Choniostomatidae . A family of Copepoda, parasites on Crustacea Malacostraca. Copenhagen, 205pp, 13pl. 1916. Crustacea Malacostraca III.-V. The order Isopoda. The Danish Ingolf-Expedition, 3(5): 1-262. Hessler, R. R. 1970. The Desmosomatidae (Isopoda, Asellota) of the Gay Head-Bermuda Transect. Bulletin of the Scripps Institution of Oceanography 15: 1-185. Lincoln, R. J. & G. A. Boxshall, 1983. Deep-sea asellote isopods of the north-east Atlantic: the family Dendrotionidae and some new ectoparasitic copepods. Zoological Journal of the Linnean Society 79: 297-318. Ritchie, L. 1975. A new genus and two new species of Choniostomatidae (Copepoda) parasitic on two deep sea jsppods. Zoological Journal of the Linnean Society 57: 1 55-1 78. Stock, J- H. & De Vos, A. P. C. 1960. Einige wirbellose tiergruppen des Dollart-Ems-estuarium. Verhandel- ingen van het Koninklijk Nederlandsch Geologisch Mijnbouwkundig Genootschap (Geologische serie) 19: 203-220. Thistle, D. 1980. A revision ofllyarachna (Crustacea, Isopoda) in the Atlantic with four new species. Journal of Natural History 14: 1 1 1-143. Wilson, G. D. F. 1982. Systematics of a species complex in the deep-sea genus Eurycope, with a revision of six previously described species (Crustacea, Isopoda, Eurycopidae). Bulletin of the Scripps Institution of Oceanography 25: 1-64. Manuscript accepted for publication 3 May 1988 A new genus of Lichomolgidae (Copepoda: Poecilostomatoida) associated with a phoronid in Hong Kong Geoffrey A. Boxshall Department of Zoology, British Museum (Natural History), Cromwell Road, London SW7 5BD Arthur G. Humes Boston University Marine Program, c/o Marine Biological Laboratory, Woods Hole, Massachusetts 02543, U.S.A. Introduction Copepods are rarely reported as parasites or associates of the lophophorate phyla Bryozoa, Brachiopoda and Phoronida. Two new harpacticoids, Tegastes knoepffleri and Peltobradya bryozoophila, were described by Medioni & Soyer (1967) as associates of the bryozoans Schizobrachiella sanguined (Norman) and Schizomavella linearis (Hassall) respectively, at Banyuls-sur-Mer in southern France. Recently Humes & Boxshall (1988) described a new genus of the family Myicolidae which occurs on the intertidal brachiopod Lingula anatina Lamarck col- lected at Starfish Bay, New Territories, Hong Kong. This is the first known copepod associate of a brachiopod. Examination of other invertebrates collected at the same time in Starfish Bay has revealed a copepod associated with a phoronid, Phoronis australis Haswell, which is itself an associate of the burrowing anemone Cerianthusfiliformis Carlgren. The phoronid lives embedded in the mucilaginous tube of the Cerianthus (Morton & Morton, 1983). Three copepods were found in the lophophore of the phoronid and are described below as a new genus of the family Lichomolgidae. Material and Methods The phoronid was collected by a diver at a depth of 3 to 5 m in Hoi Sing Wan (Starfish Bay). The phoronid was placed in a plastic bag, transported to the laboratory and examined live. The copepods were picked off and fixed in 70% ethanol. All figures were drawn with the aid of a camera lucida. Descriptions Genus PHORONICOLA gen. nov. DIAGNOSIS. Body cyclopiform. Urosome in 9 4-segmented, in $ 5-segmented. Caudal ramus with 6 setae. Rostrum broad. First antenna 7-segmented. Second antenna 4-segmented, with the formula 1 , 1,4+1 articulated claw, and 4 + 3 articulated claws. Labrum incised medially. Mandible tapering smoothly into lash. Paragnath a small hairy lobe. First maxilla with 3 setae. Second maxilla with long slender lash, 2 setae near base of lash, and a short proximally directed seta. Maxilliped in ? 3-segmented with pointed tip, in £ 4-segmented. Legs 1-4 with 3-segmented rami, except for leg 4 endopod which is 1 -segmented. Leg 4 exopod armed 1-0; 1-1; I, I, 5: endopod armed with an apical serrate spine. Leg 5 with a free segment bearing 1 apical spine and 1 subapical seta. Leg 6 in $ represented by 2 setae situated on a small lobe at each genital aperture, in £ represented by single seta on genital flap. Associated with Phoronids. Bull. Br. Mus. nat. Hist. (Zool.) 54(6): 301-307 Issued 24 November 1988 302 G. A. BOXSHALL & A. G. HUMES TYPE SPECIES. Phoronicola spinulatus gen. et sp. n. ETYMOLOGY. The generic name is derived from Phoronis, the host genus, and the Latin -cola, meaning inhabiting. Phoronicola spinulatus gen. et sp. n. TYPE MATERIAL. 1 9 and 2^ from 1 Phoronis australis collected in 3-5 m in Hoi Sing Wan (Starfish Bay), on the southern shore of Tolo Harbour, New Territories, Hong Kong by Dr P. G. Oliver on 3 April 1986. Holotype $ (BM(NH) Reg. No. 1987.415), and 2^ paratypes (BM(NH) Reg. Nos 1987.416-417) deposited in the British Museum (Natural History), London. FEMALE. Body (Fig. 1 A) with stout prosome and slender urosome. Length (excluding caudal setae) 1-17 mm and greatest width 0-49 mm. Length to width ratio of prosome 1-41:1. First pedigerous segment fused with cephalosome. Ratio of length of prosome to that of urosome 1-47:1. Segment bearing leg 5 (Fig. IB) 62 x 139 um. Genital segment elongate, 189 um long, anterior half with convex lateral margins and broader (1 33 um) than posterior half (straight sides and width of 80 um). Genital areas located dorsolaterally about in middle of segment. Each area bearing a small process armed with 2 smooth setae (Fig. 1 B), an apical seta 23 um long and a subapical seta 29 um long. Postgenital segment 52 x 72 um, anal segment 82 x 65 urn. Caudal ramus (Fig. 1 A) 3-0 times longer than wide (84 x 28 um), bearing 6 setae. Outer lateral seta 63 um long, naked and positioned on mid-dorsal surface. Dorsal seta naked, 55 um long. Outermost terminal seta 84 um long, innermost terminal seta 106 um and 2 median terminal seta 377 um (outer) and 501 um (inner); all 4 of these setae plumose. Rostrum (Fig. 1C) broad based, moderately well defined. First antenna 7-segmented as in male (Fig. ID); formula for armature: 4, 12, 6, 3, 4+ 1 aesthete, 2+ 1 aesthete and 7+ 1 aesthete. Two setae on first segment, 3 on fourth segment, 1 on sixth segment and 5 on seventh segment plumose. Second antenna (Fig. IE) 4-segmented; armature 1, 1,4+1 articulated claw, and 4 + 3 articulated claws. Labrum (Fig. 1C) with 2 broad, tapering lobes. Mandible (Fig. IF) with a slender base carrying distally a bipectinate blade. Paragnath a small hairy lobe. First maxilla (Fig. 1G) conical, with 3 elements. Second maxilla (Fig. 2A) 2-segmented. First segment unarmed. Second segment drawn out into a slender apical lash with a comb of strong spinules along outer margin, and fine spinules along inner margin. Second segment armed with a stout barbed spine on medial margin, a naked spine near its base and a fine, proximally directed setule near the base of the outer margin. Maxilliped (Fig. 2B) 3-segmented. First segment unarmed; second segment bearing a naked seta and a stout spinose seta. Third segment armed with a naked spine, terminating in slightly curved spiniform process bearing 3 spinules. Ventral area between bases of maxillipeds (Fig. 2C) and first legs only slightly protuberant. Legs \~4 (Figs 2D-F, 3A) biramous with 3-segmented rami except for endopod of leg 4 being 1 -segmented. Spine and seta formula of legs as follows: PI coxa 0-1 basis 1-0 expl-0; 1-1; III , 1,4 enpO-l;0-l;I, 5 P2 coxa 0-1 basis 1-0 exp 1-0; 1-1 ; III, I, 5 enpO-l;0-2;I, II, 3 P3 coxa 0-1 basis 1-0 exp 1-0; 1-1 ; II, I, 5 enp 0-1; 0-2; I, II, 2 P4 coxa 0-0 basis 1-0 exp 1-0; 1-0; I, I, 5 enp I Outer distal angle of legs 1-2 coxae with patch of fine spinules. Inner margin of basis of legs 3-4 with rows of long hairs. Rows of hairs present on inner margins of all exopod segments and outer margins of all endopod segments. Leg 4 (Fig. 3 A) with 1 -segmented endopod 42 um in length, bearing a few spinules proximally on inner margin and a longer row of spinules on outer margin. Apical element spiniform, 62 urn long, armed with serrate membrane on both sides. LICHOMOLGIDAE B 303 Fig. 1 Phoronicola spinulatus gen. et sp. nov. A, Holotype female, dorsal; B, Fifth pedigerous and genital segments, dorsal; C, Rostrum and labrum, ventral; D, Male first antenna, anteroventral (with aesthetes absent in female marked with asterisks); E, Female second antenna, posterior; F, Mandible, posterior; G, First maxilla, anterior. All scales in um. 304 G. A. BOXSHALL & A. G. HUMES A B Fig. 2 Phoronicola spinulatus gen. et sp. nov. Female, A, Second maxilla, posterior; B, Maxilliped, posteromedial; C, Ventral body wall between maxillipeds and swimming legs; D, Leg 1 , posterior; E, Leg 2, posterior; F, Leg 3, posterior. All scales in urn. LICHOMOLGIDAE 305 Fig. 3 Phoronicola spinulatus gen. et sp. nov. A, Female leg 4, posterior; B, Paratype male, dorsal; C, Urosome, ventral; D, Maxilliped, posteromedial. All scales in jam. 306 G. A. BOXSHALL & A. G. HUMES Leg 5 (Fig. IB) free segment about 1-2 times longer than wide (21 x 18um), with a small spiniform projection at outer distal angle. Strong spiniform apical element 49 urn long, armed with serrate membrane both sides; subapical seta 56 um long, with tiny spinules along anterior margin. Dorsal seta 35 um. Leg 6 represented by process bearing 2 setae located in genital area (Fig. 1 B). Egg sacs not seen. Colour of live specimen white. MALE. Body (Fig. 3B) similar to that of female in general form. Length 1 -04 mm excluding caudal setae, greatest width 0-33 mm; length to width ratio of prosome 1 -73 : 1 . Ratio of length of prosome to length of urosome 1-25:1. Segment of leg 5 (Fig. 3C) 43 x 101 um. Genital segment 214 x 166 um. Three postgenital segments from anterior to posterior 49 x 51, 41 x 52 and 54 x 51 um. Caudal ramus similar to that of female but shorter, 56 x 20 um, ratio 2-8:1. First antenna (Fig. ID) 7-segmented; lengths of segments measured along posterior border 26, 61, 19, 34, 44, 29 and 18 um respectively. Armature formula as for female except for additional aesthetes on segments 2 and 4 (marked with asterisks on Figure ID). Rostrum, second antenna, labrum, mandible, paragnath, first and second maxilla like those of female. Maxilliped (Fig. 3D) slender, 4-segmented. First segment stout, unarmed. Second segment with 2 naked inner setae, a row of spinules along inner surface and a shorter row of fine spinules proximally. Third segment unarmed. Claw comprising short basal section representing the fourth segment, armed with 2 unequal setae. Claw curved, 146 um in length, bearing a row of fine spinules along concave margin. Legs 1-4 similar to those of female. Leg 5 (Fig. 3C) free segment more elongate than in female, 1 -7 times longer than wide (17 x 10 um). Apical serrate element 38 um long, subapical seta 40 um. Leg 6 (Fig. 3C) forming the posteroventral genital flap closing the genital aperture, armed with a single apical seta 34 um long. Spermatophores not seen. Colour of live specimens white. ETYMOLOGY. The specific name spinulatus refers to the spiniform nature of the single serrate element on the endopod of leg 4. REMARKS. The new genus belongs to the family Lichomolgidae. The lichomolgid genera Aspidomolgus Humes, Haplomolgus Humes & Ho, Kelleria Gurney, Lichomolgella Sars, Octopicola Humes, Paramacrochiron Sewell, Pseudomacrochiron Reddiah, Sewellochiron Humes and Telestacicola Humes & Stock share with the new genus the 1 -segmented endopod of leg 4 (Humes & Stock, 1973). Most species of Macrochiron Brady also exhibit this 1 -segmented con- dition. However, none of these genera has only a single apical element on the leg 4 endopod. Aspidomolgus (II, I), Kelleria (II, 1), Octopicola (2, 1) and Telestacicola (II, 1) all have 3 elements, Lichomolgella (II), Macrochiron (II), Paramacrochiron, Pseudomacrochiron (II) and Sewellochiron (II) have 2 apical elements and Haplomolgus has none. The presence of one articulated claw on segment 3 and 3 claws on segment 4 of the second antenna is recorded in only a single species of Acaenomolgus Humes & Stock, within the Lichomolgidae. Members of this genus, however, have a 2-segmented leg 4 endopod. Kelleria has 1 and 2 articulated claws on the third and fourth segments of the second antenna respectively and has a 1 -segmented endopod on leg 4 but differs from Phoronicola in possessing an additional urosome segment in both sexes and in the formula for the third exopod segment of leg 4 which is II, I, 5 compared with I, I, 5 in the latter. No phoronid has previously been recorded as host to a copepod. Cerianthus, with which the Phoronis is associated, is host to the copepod Boholia cerianthiphila Kossmann in the Philippine Islands (Kossmann, 1877). This lichomolgid has not been recorded since its original description and was regarded as insufficiently described or of uncertain position by Humes & Stock (1973) in their revision of the family. The original description of B. cerianthiphila shows that it possesses 2 strong claws at the apex of the second antenna whereas Phoronicola has 3 slender articulated setiform claws. The segmentation of the body is also different in these two genera. These differences are sufficient to distinguish between them. LICHOMOLGIDAE 307 Acknowledgements We would like to thank Professor Brian Morton (University of Hong Kong) for the opportunity to collect this material during the Second International Workshop on the Flora and Fauna of Hong Kong and Southern China held during April 1986. We are also grateful to Dr P. G. Oliver (National Museum of Wales) who collected the phoronid host. References Humes, A. G. & Boxshall, G. A. 1988. Poecilostome copepods associated with bivalve molluscs and a brachio- pod at Hong Kong. Journal of Natural History 22: 537-544. Humes, A. G. & Stock, J. H. 1973. A Revision of the Family Lichomolgidae Kossmann, 1877, Cyclopoid Copepods mainly associated with Marine Invertebrates. Smithsonian Contributions to Zoology, 127: 1-368. Kossmann, R. 1 877. Entomostraca (1 . Theil: Lichomolgidae). In: Zoologische Ergebnisse einer im Auftrage der Koniglichen Academic der Wissenschaften zu Berlin ausgefuhrten Reise in die Kustengebiete des Rot hen Meeres. IV: 1-24, pi. 1-6. Medioni, A. & Soyer, J. 1967. Copepodes Harpacticoides de Banyuls-sur-Mer: Quelques formes recoltees sur des Bryozoaires. Vie et Milieu, 18: 317-343. Morton, B. S. & Morton, J. E. 1 983. The sea shore ecology of Hong Kong. Hong Kong University Press: 350pp. Manuscript accepted for publication 6 May 1988 British Museum (Natural History) The birds of Mount Nimba, Liberia Peter R. Colston & Kai Curry-Lindahl For evolution and speciation of animals Mount Nimba in Liberia, Guinea and the Ivory Coast is a key area in Africa representing for biologists what the Abu Simbel site in Egypt signified for archaeologists. No less than about 200 species of animals are endemic to Mount Nimba. Yet, this mountain massif, entirely located within the rain-forest biome, is rapidly being destroyed by human exploitation. This book is the first major work on the birds of Mount Nimba and surrounding lowland rain- forests. During 20 years (1962-1982) of research at the Nimba Research Laboratory in Grassfield (Liberia), located at the foot of Mount Nimba, scientists from three continents have studied the birds. In this way Mount Nimba has become the ornithologically most thoroughly explored lowland rain-forest area of Africa. The book offers a comprehensive synthesis of information on the avifauna of Mount Nimba and its ecological setting. During the 20 years period of biological investigations at Nimba this in 1962 intact area was gradually opened up by man with far-reaching environmental consequences for the rain-forest habitats and profound effects on the birds. Therefore, the book provides not only a source of reference material on the systematics, physiology, ecology and biology of the birds of Mount Nimba and the African rain-forest, but also data on biogeography in the African context as well as conservation problems. Also behaviour and migration are discussed. At Nimba a number of migrants from Europe and/or Asia meet Afrotropical migratory and sedentary birds. Professor Kai Curry-Lindahl has served as Chairman of the Nimba Research Laboratory and Committee since its inception in 1962. Peter Colston is from the Subdepartment of Ornithology, British Museum (Natural History), Tring, and Malcolm Coe is from the Animal Ecology Research Group, Department of Zoology, Oxford. 1986, 129pp. Hardback. 0 565 00982 6 £17.50. Titles to be published in Volume 54 The cranial muscles and ligaments of macrouroid fishes (Teleostei: Gadiformes); functional, ecological and phylogenetic inferences. By Gordon J. Howes A review of the Macrochelidae (Acari: Mesostigmata) of the British Isles. By Keith H. Hyatt & Rowan M. Emberson A revision of Haplocaulus Precht, 1935 (Ciliophora: Peritrichida) and its morphological relatives. By Alan Warren Echinoderms of the Rockall Trough and adjacent areas. 3. Additional records. By R. Harvey, J. D. Gage, D. S. M. Billett, A. M. Clark & G. L. J. Paterson A morphological atlas of the avian Uropygial gland. By David W. Johnston Miscellanea Primed in Great Britain by Henry Ling Ltd., at the Dorset Press, Dorchester, Dorset