HARVARD UNIVERSITY LIBRARY \ OF THE Museum of Comparative Zoology The Library Museuin of Comparative Zoology Harvard University 'K)A'L(auy UNIVERSITY OF KANSAS Mi^CELi^NEous MUSEUM OF NATURAi^ RlST0R¥- ^^ ^ publication LIBRARY No. 53 I Evolutionary Relationships, Osteology, and Zoogeography of Leptodactyloid Frogs By John D. Lynch UNIVERSITY OF KANSAS LAWRENCE 1971 June 30, 1971 UNIVERSITY OF KANSAS PUBLICATIONS MUSEUM OF NATURAL HISTORY The University of Kansas Publications, Museum of Natural History, beginning with volume 1 in 1946, was discontinued with volume 20 in 1971. Shorter research papers formerly published in the above series are now published as Occasional Papers, Mu- seum of Natural History. The Miscellaneous Publications, Museum of Natural History, began with number 1 in 1946. Longer research papers are published in that series. Monographs of the Museum of Natural History were initiated in 1970. Institutional libraries interested in exchanging publications may obtain the Occa- sional Papers and Miscellaneous Publications by addressing the Exchange Librarian, University of Kansas Library, Lawrence, Kansas 66044. Individuals may purchase separate numbers of all series. Prices may be obtained upon request addressed to Publications Secretary, Museum of Natural History, University of Kansas, Lawrence, Kansas 66044. University of Kansas Museum of Natural History Miscellaneous Publication No. 53 June 30, 1971 Evolutionary Relationships, Osteology, and Zoogeography o£ Leptodactyloid Frogs By John D. Lynch Department of Zoology University of Nebraska Lincoln, Nebraska 68508 University of Kansas Lawrence 1971 1 University of Kansas Publications, Museum of Natural History Editors: Craig C. Black, William E. Duellman, Philip S. Humphrey Miscellaneous Publication No. 53 pp. 1-238; 131 figures Pubhshed June 30, 1971 Museum of Natural History University of Kansas Lawrence, Kansas 66044 U.S.A. Printed by University of Kansas Printing Service Lawrence, Kansas CONTENTS INTRODUCTION .. 7 Acknowledgments 8 Nomenclatoiial Resume 8 Materials and Methods 17 Generic Concept 18 ANALYSIS OF CHARACTERS 19 Non-Osteological Characters 21 Amplectic Position 22 Breeding Behavior and Development 24 Tadpole Morphology 25 Secondary Sex CJiaracters 28 Pupil Shape 29 Hands and Feet 30 Body Glands 32 Myology 33 Hyolaryngeal Apparatus 34 Chromosome Numbers 36 Osteological Characters 37 Maxillary Arch 38 Lower ]aw 42 Roof of the Skull 43 Temporal Architecture 47 Palate 48 Otoccipital and Columella 52 Vertebral Column 53 Pectoral Girdle 58 Pelvic Girdle 60 Limb Elements 64 SYSTEMATIC ACCOUNTS 67 Genera Excluded from the Leptodactylidae 68 Geobatrachus Ruthven, 1915 69 Hylopsis Werner, 1896 69 3 Rhinoderma Dumeril and Bibron, 1841 69 Keys to the Genera of Leptodactylid Frogs 71 Key to Africa7i and Australo-Papiian Genera 71 Key to African and Neotropical Genera 72 LEPTODACTYLIDAE Berg, 1896 ( 1838) 75 CYCLORANINAE Parker, 1940 75 Cycloranini Parker, 1940 76 Cyclorana Steindachner, 1867 76 Heleioporus Gray, 1841 78 Mixophyes Giinther, 1864 79 Neobatrachiis Peters, 1863 81 Notaden Giinther, 1873 82 Limnodynastini New Tribe 83 Adelotus Ogilby, 1907 84 Lechriodns Boulenger, 1882 85 Limnodytuistes Fitzinger, 1843 86 Kyarranus Moore, 1958 -— 88 Philoria Spencer, 1901 89 MYOBATRACHINAE Schlegel, 1850 90 Crinia Tschudi, 1838 91 Pseudophryne Fitzinger, 1843 94 Taudactylus Straughan and Lee, 1966 95 Glauertia Loveridge, 1933 97 Uperoleia Gray, 1841 99 Metacrinia Parker, 1940 100 Myohatrachus Schlegel, 1850 101 ilndohatrachus Noble, 1930 103 HELEOPHRYNINAE Noble, 1931 103 Heleophryne Sclater, 1898 104 CERATOPHRYINAE Tschudi, 1838 105 Ceratophrys Wied, 1824 107 Lepidobatrachus Budgett, 1899 110 fWawelia Casamiquela, 1963 112 TELMATOBIINAE Fitzinger, 1843 112 4 Telmatobiini Fitzinger, 1843 113 Caudiverbera Laurenti, 1768 114 Telmatohufo Schmidt, 1952 116 Telmatohius Wiegmann, 1835 118 ■\Neoprocoela Schaeffer, 1949 120 Batrachophrynus Peters, 1873 122 Alsodini Mivart, 1869 : 123 Eupsophus Fitzinger, 1843 124 Hylorina Bell, 1843 126 Batrachyla Bell, 1843 128 Thoropa Cope, 1865 129 Odontophrynini New Tribe 130 Odontophrynus Reinhardt and Liitken, 1862 131 Proceratophrys Miranda-Ribeiro, 1920 133 Grypiscini Mivart, 1869 135 Crossodactylodes Cochran, 1938 136 Cycloramphus Tschudi, 1838 137 Zachaenus Cope, 1866 139 Eleutherodactylini Lutz, 1954 142 Amblyphrynus Cochran and Coin, 1961 143 Eleutherodactylus Dumeril and Bibron, 1841 144 Euparkerella Griffiths, 1959 150 Holoaden Miranda-Ribeiro, 1920 152 Hylactophryiie Lynch, 1968 153 Ischnocnerna Reinhardt and Liitken, 1862 155 Niceforonia Coin and Cochran, 1963 156 Sminthillus Barbour and Noble, 1920 158 SyrrJwphtis Cope, 1878 159 Tomodactylus Giinther, 1900 160 Tribe incertae sedis 162 Scythrophrys new genus 162 ELOSIINAE Miranda-Ribeiro, 1926 163 Crossodactylus Dumeril and Bibron, 1841 164 Hylodes Fitzinger, 1826 166 5 Megaelosia Miranda-Ribeiro, 1923 168 LEPTODACTYLINAE Berg, 1896 (1838) 169 Pleurodeniui Tschudi, 1838 172 Limnomedusa Fitzinger, 1843 175 Hydrolaetare Gallardo, 1963 176 Edalorhina Jimenez de la Espada, 1870 177 Litlxodijtes Fiizingex, 1843 179 Phijsalaemus Fitzinger, 1826 180 Paratelmatohius Lutz and Carvalho, 1958 182 Pseudopahidicola Miranda-Ribeiro, 1926 184 Leptodactijhis Fitzinger, 1826 186 Banjcholos Heyer, 1969 190 PHYLOGENY AND RELATIONSHIPS 192 The Fossil Record 192 Pelobatid-Leptodactylid Relationships 198 Intrafamilial Relationships of the Leptodactylidae 204 Extrafamilial Relationships of the Leptodactylidae 209 ZOOGEOGRAPHY 211 SUMMARY AND CONCLUSIONS 221 APPENDIX 225 LITERATURE CITED 229 6 INTRODUCTION Frogs of the family Leptodactylidae (auctomm) are distributed throughout the Neotropics north to Texas and Flor- ida, in southern Africa, and over most of the Australo-Papuan region (Fig. 1). The family is one of the largest amphib- ian families and was known to the early describers of the world's fauna. Linne (1758) knew two species of the family, Rana ocellata (^=Leptodactylus ocella- tus) and Rana cormita (^Ceratophnjs cornuta), and the tadpole of a third, La- certa caudiverhera (=Caudwerbera cau- diverbera), all from South America. The first representative of the Australian fauna was not described until Shaw's (1795) work naming Rana australiaca (=:Heleioporus australiacus). The fam- ily, as presently conceived, contains ap- proximately 650 species in 57 living gen- era arranged in seven subfamilies. Two of these subfamilies are restricted to Australia, New Guinea, and Tasmania, one to the Cape region of southern Africa, and the other four to the Neo- tropics. Seventeen genera are restricted to the Australo-Papuan realm, one to south Africa, and 39 to the Neotropics. Three factors have contributed to our current deplorable lack of general knowl- edge concerning this large family: 1) the most recent synopsis of a revisionary na- ture is that of Boulenger, 1882; 2) the bewildering number of generic names and the indiscriminant application of family and subfamily names of numer- ous authors; and 3) the problem of dealing with Eleutlierodactyliis, one of the largest vertebrate genera known. No part of this genus (either systematic or geographic) has been monographed. Initially, this study was restricted to a survey of the skeletal morphology of frogs of the genus EletitJierodactylus; however, this proved impractical, be- cause of the lack of understanding of Figure 1. Distributions of the family Leptodactylidae (stipple) and the pelobatid subfamily Mego- phryinae ( hatching ) . 8 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY intrageneric relationships. Therefore, I decided to re-evaluate the genera of the family and to attempt to point out supra- generic relationships. Detailed study and analysis of infrageneric relationships have, of necessity, been postponed, pend- ing a more complete and realistic under- standing of the genera involved. ACKNOWLEDGMENTS This study could not have been com- pleted were it not for the generosity of curators of numerous institutional and private collections. For loans and/ or gifts of specimens I am grateful to Wer- ner C. A. Bokermann, Sao Paulo; the late Doris M. Cochran and James A. Peters, United States National Museum; Alan Leviton, California Academy of Sciences ( CAS ) ; Alice G. Grandison, British Mu- seum ( Natural History ) ; Robert F. Inger and Karel Liem, Field Museum of Nat- ural Histoiy; Celia Limeses and Maria Tia, Laboratorio de Investigaciones Herpetologicas, Buenos Aires; A. R. Main, Department of Zoology, Univer- sity of Western Australia, Nedlands; Albert Schwartz, Miami; Hobart M. Smith, University of Illinois Museum of Natural History; Glen M. Storr, West- ern Australian Museum, Perth; I. R. Straughan, Department of Zoology, Uni- versity College of Townsville, Australia; Paulo Vanzolini, Museu de Zoologia, Universidade de Sao Paulo; C. F. Walk- er, University of Michigan Museum of Zoology; E. E. Williams, Museum of Comparative Zoology; and R. G. Zweifel, American Museum of Natural History. The majority of the material used in the study is deposited in the University of Kansas Museum of Natural History col- lection or in my own skeleton collection. Special thanks are extended to Werner C. A. Bokermann for always responding to requests for yet another specimen of an uncommon Brasilian frog and to James A. Peters and Richard G. Zweifel for pennitting preparation of skeletons of paratypes of Crossodactylodes pintoi and Noblella peruviana, respectively. Werner C. A. Bokermann, Jose Cei, M. J. Littlejolm, and J. A. Moore were especially helpful in providing informa- tion concerning reproduction. William E. Duellman, Arthur C. Echternacht, Jay M. Sa\age, Hobart M. Smith, Gerald R. Smith, Linda Trueb, Edward H. Taylor, and Charles F. Walker offered construc- tive critcism during the evolution of my concept of the evolution of leptodac- tyloid frogs. Special thanks are given to William E. Duellman, under those guid- ance this study was made; Theodore H. Eaton, George W. Byers, and Gerald R. Smith, read and criticized the manu- script. Field support was provided by grants from the Committee on Systematics and Evolutionary Biology, University of Kan- sas; a University of Kansas Graduate School Honors Fellowship; The Society of the Sigma Xi; and the Watkins Mu- seum of Natural History Grant in Aid of Research, University of Kansas. For as- sistance in the field I am grateful to Carlos Arroyo, William E. Duellman, Jerry James, Federico Medem, Juan Leon, Marsha Lynch, and Jesus Perez. NOMENCLATORIAL RESUME More genera are contained in the Leptodactylidae than in any other am- phibian family. The most recent author to monograph the Leptodactylidae was Boulenger ( 1882 ) , whose analysis suf- fered from a misunderstanding of what characters were of use in assessing fami- lies (Noble 1922, 1931). Boulenger ( 1882 ) recognized 179 species of lepto- dactylids and placed them in 34 genera in 7 famihes. No author subsequent to Boulenger has treated any major section of the Neotropical leptodactylid fauna, other than Parker (1927), who treated the frogs then placed in Paludicola [^=PhysaIaenms, Pleiirodema, and Pseu- dopaludicoki], although several works of major importance have appeared treat- ing faunal units and therefore parts of leptodactylid genera (Cei, 1962a; Coch- ran, 1955; and Cocliian and Coin, 1970). LYNCH: LEPTODACTYLOID FROGS 9 Gallardo ( 1965 ) presented a "synopsis of leptodactylids in South America" but this work in my opinion falls far short of its intended goal. Parker ( 1940 ) and Moore ( 1961 ) pro\'ided a good under- standing, albeit incomplete, of the Aus- tralo-Papuan leptodactylids. The status of the species of Heleophnjne in South Africa is now relatively well known. Twenty-three family group names have been proposed for frogs based on type-genera which are here included in the Leptodactylidae (Table 1). A num- ber of other family group names have been applied to leptodactylid frogs but do not have nomenclatural significance in a classification of the leptodactylids. Tschudi ( 1838 ) proposed two family group names, Cystignathi and Cerato- phrydes, based on Cystignathus Wagler, 1830, and Cemtophrys Wied, 1824, re- spectively. Although the Cystignathi was widely used ( Cystignathidae of Boulenger, 1882; Nieden, 1923), few authors (Cope, 1866 and Miranda-Ri- beiro, 1926) used the Ceratophrydes (or an emendation of it). The concept of the group changed whenever it was used. Parker (1935) pointed out that Noble's ( 1931 ) Pseudinae was probably an artificial assemblage and regardless should take the oldest available name, Ceratophryinae. Recently, several au- thors have proposed using Ceratophryi- dae (or an emendation of this name) as a family containing three genera of Neo- tropical frogs. With the discovery that Cystignathtis was an obligate synonym TABLE 1. Family group names proposed in the Leptodactylidae and the subfamilial or tribal name used herein. Name proposed Name used herein Cystignathi Tschudi, 1838 Leptodactylinae Ceratophrydes Tschudi, 1838 Ceratophryinae Telmatobii Fitzinger, 1843 Telmatobiinae, Telmatobiini Myobatrachidae Schlegel, 1850 Myobatrachinae Uperoliidae Giinther, 1859 Myobatrachinae Hylodidae Giinther, 1859 Eleutherodactylini Criniae Cope, 1866 Myobatrachinae Pleurodemae Cope, 1866 Leptodachtylinae Alsodina Mivart, 1869 Alsodini Cacotina Mivart, 1869 Alsodini Paludicolina Mivart, 1869 Leptodactylinae Plectromantidae Mivart, 1869 Leptodactylinae Giypiscina Mivart, 1869 Grypiscini Leptodactylidae Berg, 1896 (1838)^' Leptodactyhnae Elosiidae Miranda-Ribeiro, 1926 Elosiinae Heleophryninae Noble, 1931 Heleophryninae Cycloraninae Parker, 1940 Cycloraninae, Cycloranini Telmatobiinae Vellard, 1951 [Homonym] Cyclorhamphinae Lutz, 1954 Grypiscini Eleutherodactylinae Lutz, 1954 Eleutherodactylini Calyptocephalellinae Reig, 1960 Telmatobiini Batrachylinae Gallardo, 1965 Alsodini Pseudopaludicolinae Gallardo, 1965 Leptodactylinae Limnodynastini Proposed herein Odontophrynini Proposed herein " The family name Leptodactyhdae is a conserved name in the sense of Article 40 (International Code of Zoological Nomenclature, 1961) and hence dates from 1838, not 1896, for purposes of priority. 10 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY of Leptodactyhis Fitzinger, 1843, the family gioup name Cystignathidae be- came unavailable according to the rules then in effect, and Leptodactylidae was proposed as a family replacement name — this name has gained nearly universal acceptance and is thus a conserved name in the sense of the provisions of Article 40 of the International Code of Zoologi- cal Nomenclature ( 1961 ) and takes pri- ority over any other names proposed between 1838 and 1896. Therefore the oldest valid family group name for these frogs is Berg's ( 1896 ) Leptodactylidae. Tschudi ( 1838 ) knew eleven genera and twelve species of frogs that are now placed in the Leptodactylidae. He ar- ranged them in five families — Bombina- tores (Pletirodema and Telmatobius), Ceratophiydes (Ceratophnjs and Phryn- oceros), Cystignathi (Cystignotlnis and Crinia), Hylae (Cornufer, Elosia, and two species of Hylodes), and Ranae (Cy- doramphus and Peltoceplialus). Fitzinger, an active and often erratic classifier, proposed ( 1843 ) placing the 25 genera known to him in 7 families — Alytae (Calyptocephalus, Ceratophrys, Crinia, Hammatodactyhis, Leiuperus, Phrynoceros, Stomljiis, and Tomopterna), Gastrophrynae (Pcdiidicola), Limnodytae (Euhyas, Hylodes, and Lithodytes), Pe- lobii (Enydrohius), Phyllobatae [an older family name for Dendrobatidae (Crosso- dactylus and Scinacodes)], Ranae (Cys- tignatJnis, Cycloramphtis, Eupsophus, Gnathophysa, Leptodactyhis, Limnody- nastes, Limnomedusa, Physalaemus, and Sihilatrix). Burger (1954) correctly pointed out that the terminal endings of family group names such as these pro- posed by Fitzinger do not affect their priority and that Vellard's (1951) Tel- matobiinae is a homonym of Fitzinger's Telmatobii. Giinther ( 1859a ) attempted a world- wide catalogue of the amphibians, and, although less successful than Boulen- ger's (1882) second edition of this im- portant project of the British Museum, it did present a synthesis of most of the genera of frogs as then known. Giin- ther's family concepts were very differ- ent from those used during the following century, which explains in part why he placed the 23 leptodactylid genera known to him in elcxen families — Alyti- dae (Heleioporus), Brachycephalidae (Pseudophryne), Bombinatoridae (Al- sodes and Tehnatohiiis), Cystignathidae (Cystignathus, Leiuperus, Limnodynas- tes, and Pleurodema), Discoglossidae (Chiroleptes), Engystomatidae (Chelydo- batracJms), Hylodidae (Crossodactylus and Hylodes), Myobatrachidae (Myo- hatrachus), Polypedatidae (Cornufer and Elosia), Ranidae (Calyptocephalus, Cera- tophrys, Cyclorhamphus, Hylorhina, Limnocharis, Pithecopsis, and Pyxiceph- alus), and Uperoliidae (Uperoleia). Of these eleven families, the Hylodidae and Uperoliidae represented new groups based on leptodactylid genera. The Hylodidae was based on Hylodes of Fitzinger (1843, not 1826), and thus ap- plies to the group I designate as Eleu- therodactylini; in addition, the type genus, Hylodes Fitzinger (1843), is a homonym. Myobatrachidae was first used by Schlegel (1850). It perhaps re- flects the difficulties of communication that Giinther recognized both Chelydo- hatrachus and Myobatrachus, which are synonymous, and included them in dif- ferent families, Engystomatidae and Myobatrachidae. Cope (1866) considerably altered the previous classifications, and relied so heavily on osteological characters that most subsequent authors have over- reacted (in my opinion) in arguing that the osteocranium cannot reasonably serve in anuran classification. Cope rec- ognized 37 genera of leptodactylid frogs and placed all but two of these in the Cystignathidae. Cryptotis (^Adelotus) was placed in the Asterophrydidae and Thoropa in the Hyhdae. Cope placed the other 35 genera in six subfamilies, two of which (Criniae and Pleurodemae) were new. Cope recognized the Cera- tophrydes (Ceratophrys, Chiroleptes, LYNCH: LEPTODACTYLOID FROGS 11 Limnomedusa, Stombus, Tomopterna, and Zachaenus), Criniae (Abodes, Bor- horocaetes, Crinia, Cycloramplms, Etiso- plnis, Helioporus, Hyperoleio, Isleohatra- chus, and Plotyplectnim), Cystignathi (Cys-ti'lid pattern of thigh muscula- ture based on the patterns in Bufo and Leptodactylus respectively. She demon- stiated a continuum of muscle patterns within the Neotropical leptodactylids from the bufonid condition (Cerato- phrys, Lepidobatrachus, Odontophrynus, and Froceraiophrys cristiceps) to an "in- termediate" condition ( Macro genioglot- tiis and Froceraiophrys, except P. cristi- ceps) to the leptodactylid condition. She regarded the leptodactylid condition as grading from a cycloramphine pattern (most like the bufonid type) through a telmatobiine pattern to the leptodactylid pattern. Limeses' study demonstrated the inadvisability of using the thigh musculature in classifications above the generic level; she felt that the data sup- ported the contention of Reig and his students that the ceratophryines are fa- milially distinct and more closely allied to bufonids. Limeses (1964) concluded that the thigh muscle complexes of Noble were "progressive" characters and therefore should not be given much weight in de- fining families or suborders. Griffiths ( 1959, 1963 ) pointed out variability in the distal tendons in the dendrobatids ( a variability which overlaps the spectrum seen in myobatrachines ) , but he still at- tached considerable importance to the character complex because the muscula- ture supported his unique contention that dendrobatids are a subfamily of ranids. The conclusion of Tihen (1965) and Inger (1967) that in the course of evo- lution an increase in the complexity of the musculature is to be expected car- ries much weight in support of the argu- ment that the diplasiocoelan condition is labile as evidenced by its appearance in the Myobatrachinae, Dendrobatidae, and in Crossodactyhis. I am not of the opinion, in view of the other data avail- able, that the diplasiocoelan condition in the Myobatrachinae suggests ranoid af- finities, although it is not inconceivable 34 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY that the origin of the arthroleptine raiiids might be the Australo-Papuan Myobatra- chinae. At present, the arrangements of the thigh muscles in the cycloranine and myobatrachine leptodactyhds are re- garded as only one additional character in support of Parker's ( 1940 ) subfamilial classification. Griffiths (1959, 1963) used the mus- culature of the temporal arch as one of the two characters separating leptodac- tylids and hylids from bufonids. In the former group the m. depressor mandihu- lae is divided into two slips (pars tym- panicus and pars scapularis), whereas in the bufonids the pars scapidaris is ab- sent. Limeses ( 1965 ) investigated the m. depressor mandibiilae in several of the "ceratophrydids" and compared her data with that for a number of "normal" leptodactylids. I dissected at least one specimen for each leptodactylid genus except Amhlijphnjnus and Hijlorina in order to examine the state of the m. de- pressor mandihidae. The only taxa with the bufonid type [pars tympanicus only) are Crinia, Eupsophus juninensis, Lepi- dobatrachiis, Philoria, and Pseudo- phryne. A massive pars tympanicus and minute pars scapularis are exhibited in several Eleiitherodactylus (biporcatus, bufoniformis, cornutus, galdi, stdcatus), Proceratophrys (except in P. cristiceps), and Tebnatobufo; the condition seen in Ceratophrys and Macrogenioglottus is slightly more leptodactylid, but the pars scapularis is still small. In Odonto- phrynus and Proceratophrys cristiceps both slips are large. In the remaining leptodactylids both muscle slips are pres- ent, and the pars scapularis is usually larger. Starrett (1968) studied the jaw mus- culature in many anurans and distin- guished several insertional patterns of the m. depressor mandibulae. She con- sidered the condition of this muscle too variable to be used in defining families but useful at lower taxonomic levels when used in combination with the ad- ductor muscles. Based on my study of most of the leptodactylid genera, I con- sider the m. depressor mandibulae to be of questionable value in leptodactylid frog classification. I did not investigate the condition of the adductor muscles in leptodactylids. The reader is referred to Starrett (1968) for a detailed review of anuran jaw musculature. An associated character is the path- way of the mandibular ramus of the tri- geminal nerve through the muscle blocks. Limeses (1965) investigated this character for several of the broad- headed South American leptodactylids and considered it useful in defining her "Ceratophrydidae" — which included only parts of some genera (for example, Pro- ceratophrys). The musculature of the hyolarynx has been successfully used by several authors in systematic studies of frogs. The mus- culature is discussed with the hyoid ( see below). Hyolaryngeal Apparatus Trewavas ( 1933 ) investigated the hyolarynx in a wide variety of frogs. Among the sixty species he treated were nine leptodactylids. Parker (1940) used the shape of the hyoid plate, condition of the cricoid cartilage ventrally, and the patterns of insertion of the deeper throat muscles on the hyoid plate in separating the two subfamilies of the Australo-Papuan leptodactylids. Grif- fiths (1959) described the hyolarynx of Sminthillus. Among the potentially use- ful characters in the hyolarynx of lepto- dactylids are 1) the extent and shape of the alary process of the hyoid plate, 2) branching of the hyale, 3) variation in the postero-lateral process of the hyoid plate, 4) division (ventrally) of the cricoid cartilage, and 5) attachment of the m. petrohyoideus anterior and m. sternohyoideus on the hyoid plate. The cricoid is divided ventrally in all genera of the Myobatrachinae but is complete in all other genera of the fam- ily. Griffiths (1963) reported the cri- coid to be divided ventrally in Lepto- LYNCH: LEPTODACTYLOID FROGS 35 dachjlus prognathus, but I have been unable to verify this observation in my specimens. The esophageal process of the cricoid has been used as a systematic tool, but it is apparently of such vari- ability (poorly to well developed) that its use at the generic level is not wise. In ranoids the esophageal process is elongate, as it is in Heleophryne, but in most leptodactylids the process is either reduced in size or only of moderate size. In the Myobatrachinae, the alary processes of the hyoid are broad and wing-like, and the m. petrolnjoideus an- terior inserts on the alary process. The elongate insertion of the m. sternoJujoid- eus begins anteriorly on the hyoid plate medial to the alaiy process and pos- teriorly moves nearer the midline of the hyoid plate (Fig. 8). In contrast to the condition seen in the myobatrachines, the cycloranines have a narrow stalked alary process and the m. petrohijoideus anterior inserts on the posterolateral edge of the hyoid plate. The m. sterno- Injoideus inserts medially on, but at the edge of, the hyoid plate. Anteriorly, its insertion is like that seen in the myo- batrachines, but posteriorly the muscles are disposed more laterad. The muscle disposition in Heleophryne is exactly like that seen in the Cycloraninae; the only differences in the hyolarynx be- tween the Cycloraninae and Heleo- phryne are the presence of an anterior process on the cornu and the elongate esophageal process in Heleophryne. Among Neotropical leptodactyhds, only the Leptodactylus marmoratus group, Physahemus (including Engy- stomops and Eupemphix), and Pseudo- paludicola have the myobatrachine pat- tern of muscle insertions on the hyoid plate. These genera also have the ex- panded and wing-like alary processes of the hyoid plate as does Hydrolaetare. The alary processes are absent in Cera- tophrys, Euparkerella, Holoaden, Lepi- dobatrachus, Limnomedusa, and Smin- thillus. Holoaden and Pseudopaludicola lack the posterolateral processes of the hyoid plate. The posterolateral proc- esses of the hyoid plate are large in the Ceratophryinae and Limnomedusa (Fig. 9). This enlargement may be a struc- tural compensation for the loss of the alary processes in these genera. An- terior processes of the cornua are lacking in the Australo-Papuan genera and in about one-half of the Neotropical gen- era. I found anterior processes of the cornua in Edalorhina, Eleutlierodacty- lus, Euparkerella, Eupsophus, Holoaden, Heleophryne, Hylactophryne, Ischno- cnema, Lithodytes, Megaelosia, Nice- foronia, Odontophrynus, Proceratophrys, Physalaemus, Sminthillus, Syrrhophus, and Tomodactylus. Specimens were not available of Amhlyphrymis, Batrachyla, Caudiverbera, Crossodactylodes, Hylo- FiGURE 8. Hyoid plates of Heleophryne natalen- sis (A, KU 105925, X 5) and Physalaemus pusiulatus (B, UIMNH 80710, X 10) illus- trating the two muscle insertional patterns. The insertion site for the m. sternohyoideus is stip- pled; the other muscle is the ni. petrohijoideus anterior. 36 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY rina, and Telmatohufo. The cerato- phiyines have broad cornua in compari- son to other leptodactylids. The entire hyoid plate is elongate in EuparhereUa, Holoaden, and Smintliilhis in contrast to all other leptodactylids (Fig. 9). Figure 9. Hyoid plates of (A) Limnomediisa macwglossa (female, KU 74327, X 2.5), (B) Lepidohatrachus asper (male, KU 86782, x 4.5), (C) Holoden hradei (female, KU 107086, X 4.5 ) and ( D ) Stninthilhis limbatiis ( after Griffiths, 1959). Variations in the hyolarynx appear useful in comparing and contrasting lep- todactylid genera. In some cases, the hyolaryngeal data support the classifica- tion at the tribe or subfamily level — the Australo-Papuan groups and the Cerato- phiyinae. The variation in the shape of the hyoid plate among the Neotropical leptodactylids is impressive in view of the uniformity of the structure within the two Australo-Papuan subfamilies. Chiomosome Numbers'* In recent years, increasing attention has been given chromosome numbers in ' The chromosome number account presented here includes only 15 species of leptodactylids. The efforts in this area have greatly increased the number of species (78) for which counts are available. The pertinent literature includes Barrio (1970), Barrio and Rinaldi de Chieri (1970a, 1970b), Be(,ak (1968), Be(,ak, Denaro, and Begak (1970), Bogart (1970), Brum- Zorrilla and Saez (1968), Morescalchi and Gargiulo (1968), and Morescalchi, Gargiulo, and Olmo (1968). Rabello (1970) summarized much of the data but was unaware of other observations; she published counts contrary to those reported in some of the original work. The somatic counts range from 18 to 104, although Becak, Denaro, and Becak (1970) stated that a \'alue of 16 is the lowest known. The highest counts are for polyploid populations. Values of 2N =8X^104 are known for Ceratophnjs dor- sata and C. ornata ( Barrio and Rinaldi de Chieri, 1970b). Tetraploid counts (2N=4X= 44) are known for Odontophnjnus americanus (Bogart, 1967) and Pleurodema bibronii and P. kricgi ( Barrio and Rinaldi de Chieri, 1970a). The published counts for 67 other Neotropical and six Australian leptodactylids range from 18 to 36. The six Australian leptodactylids (Crinia, Limnodijnastes, Pseudophryne, and Uperoleia) have 2N=24 (Morescalchi, Gargiulo, and Olmo, 1968). The diploid counts for all leptodactylid gen- era are siimmerized below. The data are pre- sented as follows: genus (number of species for which counts are known), 2N value(s), and where germane, citations of intrageneric (and intraspecific ) variations. Polyploid counts are not repeated here. The names used in the orig- inal accounts have been brought into line with the generic classification employed in this work. Batrachyla (2), 2N=26; Caudiverbera (1), 2N= 26; Ccmtophnjs (3), 2N=:26; Crmia (2), 2N= 24; Cro.ssodactyhis (2), 2N=26, however, Brum-Zorrilla and Saez ( 1968) reported 2N=22 for C. gaudichaudii, whereas Bogart (1970) obtained 2N=26 for the same species; Cyclo- ramphus (3), 2N=26, however, Brum-Zorrilla and Saez ( 1968) reported 2N=:22 for C. /t///g/- nosiis (sic), whereas Bogart (1970) obtained 2N=26 for the same species; Eleuthewdactyhis (11), 2N=18(2), 20(2), 22(4), 34(2), and 36(1), see Bogart (1970); Eupsophus (4), 2N=22(1), 26(1), 28(1), and 30(1), see Bo- gart (1970) for a detailed account; Hylacto- phryne (1), 2N=22; Hylodes (2), 2N=26; Insuctoi)luynus (1), 2N=26; Lcpidobat radius (3), 2N=26; Leptodactylus (8), 2N=22; Limnodynastcs (2), 2N=i 24; Lithodytcs (1), 2Niizl8; OdontopJirymis (4), 2N=22; Physa- lacnnis (6), 2N=22; Pleurodema (6), 2N=22; Proccratophrys (2), 2N=22; Pseudopahidicola (2), 2N = 18, 20, and 22, P. ameghini is 2N=20 and P. falcipes has 2N values of 18, 20, and 22 (Brum-Zorrilla and Saez, 1968, and Batistic, Beyak, and Vizotto, 1969, discussed the situ- ation in this genus); Pseudophryne (1), 2N=24; Syrrhophus (1), 2N=30; Tehnatobius (2), 2N=22 and 26, see Barbieri (1954) and Brum- Zorrilla (1968); Thoropa (1), 2N=26; Tomo- dactylus (1), 2N=22; Uperoleia (1), 2N=24; and Zachacnus ( 1 ), 2N=26. James P. Bogart has a considerable amount LYNCH: LEPTODACTYLOID FROGS 37 systematic studies. Data are only now being accumulated for the leptodacty- lids, and to date no counts are available for the Australo-Papuan or African gen- era. Likewise, no data have accumlated for the Neotropical subfamily Elosiinae Bogart (1967), Moreschalchi (1967), and Saez and Brum ( 1959 ) reported counts for the ceratophryine genera; Ceratophn/s calcarata, Chacophnjs pier- otti, and Lepidohatrachus Uanensis have 2n of 26, whereas Ceratophrys ornata has been reported to have 2n of 88, 92, 98, 104, and 108. Bogart (1967) pre- sented convincing arguments that this species is octaploid (n = 13). Of the subfamily Leptodactylinae, counts of 2n of 22 are available for five species of Leptodactylus and Pseudopal- udicola falcipes (Barbieri, 1950, Bogart, 1967, and Saez and Brum, 1960). Counts for the Telmatobiinae range from 2n of 22 to 50. The major variation occurs in the genus Odontophrynus — O. americanus is tetraploid (2n of 44) [Becak, et al., 1966, Bogart, 1967]. Saez and Brum (1966) reported 2n = 42, 44, and 50 for various populations of this of unpublished observations on leptodactylid chromosome numbers. He has counts for three genera not included abo\'e — Edalorhina (1), 2N=22; Hcleophnjnc (1), 2N=26; and Isch- nocncma (1), 2N=22 — and counts for addi- tional species in eight genera. The additions are Cycloratuphus (three more species, 2N=26), Eleuthewdactijlus ( 19 more species, 2N=22 in five, 26 in nine, 30 in three, and 34 in two); Hylodes (one more species, 2N=26); Lepto- dacttjlus (eight more with 2N=22, and two species of the mannoratus group, subgenus Adenomcra, with 2N=26); Physalaemus (six more species, 2N=22); Syrrhophus (one more species, 2N=26); Telmatobius (three more spe- cies, 2N=26; one of these is T. montanus which Gallardo, 1970, placed in Abodes); and Thowpa (one more species, 2N=26). These 47 species increase the total known to 126 representing 29 genera and all seven subfamilies. The sub- families have counts of: Cycloraninae, 2N=24, Myobatrachinae, 2N=24, Heleophryninae, 2N= 26, Ceratophryinae, 2N=26 (and 8X=104), Elosiinae, 2N=26, Leptodactylinae, 2N=18, 20, 22, and 26 (and 4X=44), and Telmatobiinae, 2N = 18, 20, 22, 26, 28, 30, 34, and 36 (and 4X=44). species. The other two species of the genus for which counts are available have 2n of 22 (Saez and Brum, 1966). Tehnatohius schreiteri has a 2n =: 26 (Barbieri, 1954), whereas the other spe- cies of the subfamily (except the tetra- ploid Odontophrynus americanus) have 2n =r 22 (HylactopJiryne aufi^iisti, Tomo- dactylus nitidus; Duellman, 1967). It is generally conceded that the more primitive members of a group have higher chromosome numbers than do the more advanced members of a given group. Although this generalization is supported by too few data to be clearly stated, it is significant that except for i^he cases of tetraploidy and octaploidy in the leptodactylids, the more primitive Neo- tropical groups ( Ceratophryinae and the Telmatobiini ) have diploid numbers of 26, as opposed to 22 in the advanced lines (as detennined on other grounds). I anticipate the Cycloraninae and Heleo- phryninae also to have diploid numbers of 26, as do the pelobatids (Duellman, 1967, Moreschalchi, 1967). The Myo- batrachinae might have fewer than 26 since they are morphologically diver- gent from the Cycloraninae. OSTEOLOGICAL CHARACTERS With the notable exceptions of the vertebral centra, sacral diapophyses, terminal phalanges, and the gross pec- toral structure, few osteological charac- ters have been used in generic and su- prageneric classifications of bufonoid frogs. Cope (1865, 1866, 1889) placed undue weight on minor variations of the skull bones. Subsequent authors, in not- ing the obvious errors in Cope's scheme, tended to regard most osteological varia- tion as trivial and therefore of no value in a classification at or above the generic level. The most recent author to ex- pound this point was Griffiths (1963). The major efforts in anuran phylogeny have been based on the pectoral archi- tecture ( Cope, Boulenger, and Griffiths ) and on the vertebral column and thigh musculature (Nicholls and Noble). 38 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY I am convinced that at least within the Bufonoidea, the osteocranium can serve as a primary source of characters for classification. I have completed a generic-level analysis of the skeletons of the frog family Leptodactylidae and have briefly checked certain points among the genera of the Bufonidae, Centrolenidae, Dendrobatidae, Hylidae, and Pseudidae. Additional data are available in the pectoral and pelvic girdles and in the vertebral column. I consider the appendicular skeleton of relatively little use, although the shape of the terminal phalanges and the fusion of the tarsal bones are useful sources of characters. Maxillary Arch The premaxillae, maxillae, septomax- illae, and quadratojugals make up the maxillary arch. The quadratojugals are the only bones that are variable in occur- rence. In no case are the premaxillae fused. Loss of the quadratojugals occurs sporadically throughout frog families from the most primitive (Leiopelma, Pipa) to the advanced (some Hyla). The quadratojugals have been lost in six lep- todactylid genera — Batrachyla, Crosso- dactylus, Hylorina, Notaden, Pleurode- ma, and Pseud opaludicoh. The maxil- lary arch is incomplete (Fig. 10) but the quadratojugal is present in several leptodactylids. The degree of separation of the maxilla and quadratojugal is vari- able. Most leptodactylids have the quad- ratojugals in articular contact with the maxillae, although the contact is tenuous in some genera (Hylodes). Fusion of the elements of the maxil- lary arch (maxilla and quadratojugal) is seen only in the genera of the subfamily Ceratophryinae (Ceratophrys and Lepi- dohatrachus). These frogs and the Chilean Caudiverhera caudiverhera have bony, stegocephalian-like skulls with a complete and small orbit. In contrast to the latter genus, the ceratophryines are characterized by the fusion of all of the skull bones (except the columellae, sep- tomaxillae, and premaxillae) into an akinetic unit. Loss of the maxillary and premaxil- lary teeth was once considered a family character in frogs, and very often its use resulted in the erroneous association of several leptodactylids with the Bufoni- dae. In his later works, George A. Boulenger laid an ever decreasing em- phasis on the lack of teeth in the maxil- lary arch. Noble (1922) completely dis- missed the character and combined the Bufonidae and Leptodactylidae. Sub- sequent authors have usually considered loss of the teeth of the maxillary arch of at least generic value; even Noble ( 1925 ) later decided that the presence or absence of maxillaiy teeth was a ge- neric character. If Moore (1961) is correct in recog- nizing a single species of Uperoleia, then at least one species of frog has intra- specific variation in the presence of teeth on the maxillary arch. Most leptodacty- lids have teeth on the maxillary arch; Figure 10. Lateral views of the skulls of (A) Baimrhyh Irptopiis ( UMMZ S-2246, X 6.5), (B) Etii)soi)]iiis lusciis (AMNH 22104, X 4.2) and (C) Cyclommphus eleutherodactyhis (KU 92785, X 3.3) illustratinjf variation in the extent of the quadratojugal bone. LYNCH: LEPTODACTYLOID FROGS 39 Batrachophnjmis, Glauertia, Metacrinia, Myohatrachus, Notaden, some species of PJiysolaenuis (maculwentris, nanus, nat- tereri, ohtectus, petersi, pnstulosus, and signifenis), Pseudophnjne, Sminthillus, some species of Telmafobius, and some Uperoleia lack teeth. Fhnjnanodus na- nus Ahl was long thought to be tooth- less, but examination of the unique holo- type revealed a full complement of teeth and satisfied me that the monotypic genus was identical to Eleutherodactylus parvus (Lynch, 1968c). Loss of teeth is either uniform or \'ariable in ten leptodactylid genera; these genera belong to four clearly de- finable subfamilies, none of which is de- fined by tooth loss. Notaden is the only cycloranine which has no teeth; it is closely related to Neobatrachus, a toothed genus. Of the five toothless myobatrachine genera, Fseudophryne is most closely related to Crinia, a toothed genus; the other four edentate genera form a group but are not closely related to one another. Tooth loss occurs in the subfamily Leptodactylinae only in Thysa- laemus. Not all species of the genus lack teeth; this variation has contributed to unnatural classifications, in which some species of the genus were placed in the Bufonidae and others in the Cystignathi- dae. Most of the species of the nattereri and petersi groups of Fhysalaemus lack teeth — one species in each group has teeth. All species of the Fhysalaemus cuvieri group have teeth. Batraclwphry- nus and its Oligocene relative, Neopro- coela, are toothless but closely allied to the toothed genera, Caudiverbera, Tel- matobufo, and Telmatobius. A few spe- cies of Tehnatobius are toothless and have been erroneously associated with Batrachophrynus. As Vellard (1951) and Cei and Roig ( 1968 ) pointed out, the toothless species of Telmatobius are closely related to toothed species. Smin- thillus is an edentate derivative of the West Indian complex of Eleutherodac- tylus. Noble (1931) contended that the Criniinae ( =zCycloraninae -\- Myoba- trachinae) had deeper maxillae than did the Neotropical leptodactylids. His ob- servations apparently were very limited because among the Australo-Papuan lep- todactylids, the Myobatrachinae have shallow maxillae (little or no facial lobe of the maxilla) whereas deep maxillae are found in the Cycloraninae. The maxillae of the cycloranines are no deep- er than those seen in many Telmato- biinae (e.g., some Eleutherodactylus, Odontophrynus, Froceratophrys) or Lep- todactylinae (Fleurodema). The depth of the maxilla appears to be correlated with the degree of reduction of ossifica- tion. Uperoleia and Myohatrachus have deeper maxillae than the other myo- batrachines, and Uperoleia is the only myobatrachine lacking an extensive fron- toparietal fontanelle. The alary processes of the premaxil- lae are well developed in all leptodac- tylid genera, except Myohatrachus, in which they are essentially obsolete ( Fig. 11). The extensive reduction of the an- terior portion of the skull of Myohatra- chus has resulted in minute premaxillae. The palatal shelf is still well developed and similar to those of the other Myo- bati-achinae. The reduction of the an- terior cranial elements in Myohatrachus is compensated for by the development of massive palatines. The alary processes are directed an- terodorsally, dorsally, or posterodorsally (Fig. 10), and the slope is apparently correlated with the development of bur- rowing habits; the more posterior the slope, the greater the burrowing ten- dencies. In several genera, most notably members of the Elosiinae, the alary processes have a lateral vector as well. In general, the alary processes are rela- tively narrow near their base in the Af- rican and Neotropical genera (Fig. 11), whereas the processes are very broad at the base in the majority of the Australo- Papuan genera (Fig. 11). The range of variation of this character in the sub- 40 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 11. Variation in the premaxillae of lep- todactylids. (A) median view of left premaxilla of Ceratophnjs calcarata, JDL S-237, X 2.5; (B ) frontal view of same; ( C ) median view of left premaxilla of Eleiithewdactt/Ius curtipes, JDL S-351, X 10; (D) frontal view of same; (E) frontal view of left premaxilla of Batracho- phnjmis macrostomus, KU 98127, X 2; (F) frontal view of left premaxilla of Mixophijes fasciolattts, KU 56627, X 2.5; (G) ventral view of right premaxilla of Batrachophrynus macro- stomus, KU 98127, X 2; (H) ventral view of right premaxilla of Eleutherodactylus ctniipes, JDL S-351, X 10; (I) ventral view of right premaxilla of Batmchyla leptopus, UMMZ S- 2246, X 9; (J-K) frontal and ventral views of bones of snout of Myohatrachus gouldi, KU 110333, X 5. Following abbreviations are used: m — maxilla, n — nasal, s — septomaxilla, ap — alary process, and ps — palatal shelf. family Telmatobiinae is as great as the variation throughout the family. The palatal shelf of the premaxilla is functionally absent in the Ceratophryi- nae but present in all other leptodactylid genera. The variation in this structure in the non-ceratophryines involves depth of the shelf, degree of medial dissection, and the development of the palatal process (Fig. 11). Deep palatal shelves characterize Batrachophrynus and Neo- procoela and may reflect loss of teeth, although the shelf is relatively deep in HoJoaclen, a toothed genus. Batraclitjh, Crossodactijhis, and Hijlodes have very shallow palatal shelves and long palatal processes. Telmafobius and Thoropa, and to a lesser extent, PhijsaJaemus, have shallow palatal shelves, which extend laterally to meet the maxillae. In each case, the palatal process is either elon- gate or large, or both. Deeply dissected palatal shelves occur in Eleutlierodactij- his, Hylactopliryne, Ischnocne?na, Lith- odytes, Niceforonia, Paratehnatohius, some Physalaemus, Proceraiophrys, Smintliilhis, SyrrJwphus, and Tomodac- tyhis. The shelf is most deeply dissected in some Eleiitherodactyhis, Hylacto- phryne, Niceforonia, and Tomodactyhis. The depth of the palatal shelf may re- flect stress on the anterior end of the skull during burrowing. The Australo-Papuan genera exhibit almost no variation in the shape and extent of the palatal shelf. The maxillae show only minor varia- tion in the depth of the facial lobe, the degree of Haring of the maxilla, and the development of exostosis. Megaelosia is unique among leptodactylids in its posterior expansion of the maxilla (Fig. 12), which is characteristically a taper- ing bone. Exostosis is seen in Caiidiver- hera, Cyclorana australis, the cerato- phryine genera, some Eleutherodactylus {cornutus and unistrigatus groups), and some species of Proceraiophrys. The range of variation in the palatal shelf of the maxilla is less than that in the premaxilla. In most genera, the pos- terior end of the maxillary palatal shelf is expanded (pterygoidal process) and abuts or overlaps the anterior ramus of the pterygoid. In some genera (e.g., Caudiverbera), there is a definite suture between the pterygoidal process and the pteiygoid (Fig. 12). This character is apparently correlated with a more solid skull architecture. LYNCH: LEPTODACTYLOID FROGS 41 Figure 12. Expansion of the posterior portion of the maxilla in (A) Megaelosia gocldi ( KU 92966, X 4). Maxilla-pterygoid articulation in (B) Leptodachtijhis pentadactyhis (KU 68159, X 1) and (C) Caiidiverbera caudiverbera (FMNH9703, X 1). Teeth, when absent on the premaxil- la, are also absent on the maxilla. In all toothed genera except Adelotiis, the teeth form a continuous row from the suture between the premaxillae to a point near the end of the maxilla, pos- terior to the maxilla-pterygoid junction. In Adelotiis (Fig. 13) there is a distinct diastema between the maxillary and pre- maxillary teeth. Leptodactylid teeth are of two types, exemplified by Ceratophnjs and Odon- tophrijnus. In Ceratophnjs and four other genera, the teeth are fang-like, some (e.g., Megaelosia) more so than others, whereas in Odontophnjniis and most other genera, the teeth are blunt with some indications of bulbing and cusp formation (like that described for several hylids — Duellman and Trueb, 1966, Trueb, 1966). The teeth in Megae- losia are six to seven times as long ( pro- portionately) as those in most other lep- todactylids. Parsons and Williams (1962, 1963) characterized the Lissamphia by numer- ous features, one of which was jointed or hinged teeth — a basal pedicel and a distal crown. Reig and Limeses (1963) pointed out that the ceratophryine gen- era do not have hinged teeth, whereas the genera often wrongly combined with Ceratophnjs [Odontophrynus and Pro- ceratophnjs (=zStomhus auctorum)] pos- sess hinged teeth. The ceratophryines have comparatively long teeth (here termed "fang-like" for purposes of dis- cussion). Among the American genera, elongate fang-like teeth are found in Ceratophnjs (including Chacophrys) , Lepidohatrachus, Megaelosia, and Tel- matohius. The teeth of Crossodactijlus, Hylodes, and Telmatobufo tend to be pointed and elongate but are not com- parable to those of members of the "fang-like teeth" group. Distinct pedi- cel-crown development is seen in the "fanged" Megaelosia and Telmatobitis but not in the Ceratophryinae (Fig. 13). Among the toothed Australo-Papuan leptodactylids, fang-like teeth are found only in the cycloranine Adehtus; it and all other toothed Australo-Papuan gen- era and Heleophryne have pedicelate teeth. Goin (1959) published a note on the number of teeth per maxilla in approxi- FiGURE 13. (A,B) Anterior portion of the skull of Adelotiis brevis ( KU 56242) illustrating the diastema. (C) Maxillary teeth of Pwceratophnjs appendiculata ( KU 93070) and (D) same of Ceratophrys cakamta (JDL S-237). Teeth of Pioceratophrys are pedicellate; those of Cerat- ophrys are non-pedicellate. A and B, X 3; C and D, X 12.5. 42 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY mately 65 species of EJeutherodactijlus and 12 species of Leptodactyhis; the range in the former was 33 to 111 per maxilla and in the latter 43 to 79. Goin asserted that, within the species groups with which he was familiar, the species groups could be characterized on the basis of average number of teeth. I con- sider the number of teeth, in most cases, to more accurately reflect the average size of the species studied than relation- ships. Most species of Eleutlwrodactyliis have between 50 and 80 teeth on each maxilla. Reig and Limeses (1963) noted the low tooth counts of the cerato- phryines ( about 25 per maxilla ) as com- pared with 50 or more per maxilla in most other leptodactylids. They reported the following data for the cerato- phryines: Chacophnjs, 22 ± 2 per max- illa; Ceratophnjs, 27 ± 3, and Lepido- hatrachus, 28 ± 5. In Megaelosia there are 29 to 34 teeth per maxilla (based on four individuals); these data compare favorably with those for the cerato- phryines and for Adelotus (26 to 28 teeth per maxilla). The septomaxillae are small, incon- spicuous elements of the maxillary arch and are intricately associated with the nasal cava. The shape of the bones re- flects the connecting pathways of the cava. The septomaxillae are proportion- ately minute in Ceratoplinjs when com- pared with those of most leptodactylids. The smallest species of the family have simple U-shaped septomaxillae ( Baldauf and Tanzer, 1965 ) . I have examined few leptodactylids for the detail of the septo- maxillae, but have determined that the bones are invariably present. The septo- maxillae of several genera of leptodacty- lids are illustrated in Figure 14. Serious study of the septomaxillae will probably require study of serially sectioned ma- terials. Lower Jaw The anuran mandible contains two bones, the dentary and angular, and the mentomeckelian cartilage (Fig. 15). No leptodactylid has true teeth on the lower jaw, although odontoids are developed to varying degrees by several species. Grypiscus was once thought to have mandibular teeth, but Noble (1922) re- ported these "teeth" to be a serrate ridge. 1 have not found a serrate ridge on the mandible of any Cydoramphus (^Gry- piscus) or any other leptodactylid frog except large Ceratophrys. Many indi- viduals of Ceratophrys have a sharp odontoid on the mentomeckelian carti- lage near the mandibular symphasis. The only leptodactylid with large odon- toids is Adelotus hrevis (Fig. 15). These tusk-like odontoids are better developed in the male than in the female. The maxillary diastema of Adelotus is ap- parently a spacing adaptation for the oc- FiGURE 14. Septomaxillae of several Neotropical leptodactylid frogs. (A-D) dorsal, ventral, lat- eral and median views of right septomaxilla of Leptodactyhis pentadactijlus (KU 84982, x 9.5), (E) ventral view of right septomaxilla of Eleutherodacttjhis flcischmanni ( KU 68158, X 9.5), (F) posteroventral view of right septo- maxilla of Ceratophrys calcarata ( JDL S-237, X 16), (G) lateral view of left septomaxilla of Hylodes lateristri^ata ( KU 92878, X 9.5), (II-I) lateral and dorsal views, respectively, of left septomaxilla of Tchnatohius liaittholi (KU 72879, X 9.5). LYNCH: LEPTODACTYLOID FROGS 43 Figure 15. Left mandibles of (A-B) Cerato- phrt/s aurita ( EHT 1415, X 1), and (C-D) Addotiis brevis (AMNH 59490, X 2.5). Lateral and dorsal views, respectively. elusion of the teeth of the maxillary arch and the odontoid of the dentary. Roof of the Skull The following bones are included in this category: nasals, sphenethmoid (en- dochondral), frontoparietals, prootics, and exoccipitals. Unlike some of the casque-headed hylids, the casque- headed leptodactylids always lack a der- mal sphenethmoid. Trueb (1966, 1970) reported a dermal sphenethmoid in some casque-headed, co-ossified hylids (Apor^ asphenodon, Conjthomantis, some Hyla, Osteocephalus, Tmchycephalus, and Tri- prion petasatus). The frontoparietals and nasals are co-ossified in Caudiver- bera and the Ceratophryinae, and are extensively exostosed in Ctjclorana aus- tralis and several EleitthewdactyJus. Functionally, the prootic and exoccipital form a single bone (otoccipital), al- though they are not always fused (per- haps paedomorphic). The nasals exhibit considerable varia- tion in size and position relative to the premaxillae, sphenethmoid, and fronto- parietals. Large nasals are present in some members of those genera with the nasals in medial contact (e.g., Eleuthero- dactyhis), and small nasals are usually correlated with medial separation (e.g., Hylodes). In general, widely separated nasals are correlated with a proportion- ately large sphenethmoid; however, large sphenethmoids may also be found in genera with closely juxtaposed nasal bones. Separation of the nasals does not always correlate with the presence of a large frontoparietal fontanelle (Fig. 16). A large sphenethmoid usually is corre- lated with an anterior rotation of the alary processes of the premaxillae, pre- sumably reflecting the forward shift of the nasal capsule. At present, I am un- willing to state that nasal and fronto- parietal separation always correlates with a reduction in the amount of bone in the skull or that the enlargement of the sphenethmoid correlates with the abo\'e. I consider the variations in the bones of the roof of the skull as dis- cordant. A frontoparietal fontanelle is present in juveniles of all leptodactylids [even Ceratophnjs just before metamor- phosis (Fig. 74)] but is retained in rela- tively few genera ( 21 ) in the adult. The South African Heleophryne has a large frontoparietal fontanelle, and large fon- tanelles are seen in the myobatrachine genera Crinki, Glauertia, Metacrinia, Myohotrachus, and Pseudophryne but not in Taudactyhis or Uperoleia. The skull roof is solid in the cycloranines Adelotus, CycJorarm, Lechriodm, and Mixophyes, whereas in Heleioporus, Ki/arranm, Limnodynastes, Neobatrach- us, Notaden, and PhUoria moderately well-developed frontoparietal fontanelles are present. Frontoparietal fontanelles are lacking in the Ceratophryinae, Elo- siinae, and all but two genera of the Leptodactylinae (Paratehnatobius and Pleuwdema), although the leptodactyline PseudopaJudicola could be described as having a long, narrow fontanelle (Fig. 17). Among the Telmatobiinae, only two genera (BatrachyJa and Thoropa) have moderate-sized fontanelles; small fontanelles are found in Batmchophry- niis, Eupsophus, Holooden, Neoprocoeh, Tehnatobius, and Tehnatobtifo. The skull is completely roofed in the other 44 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 16. (A) Skull diastema, KU 68263) ; of a leptodactylid lacking a frontoparietal fontanelle {Eleutherodachjlus uid (B) one with a relatively large fontanelle (Thoropa hitzi, KU 92850). Both X 6.8. Fif;uRE 17. Separation of nasal bone.s. ceiatoplinjs hoiei ( KU 93076, X 2.3); (A) Pscudopahidicola salfica ( KU 93068, X 6.8); (B) Pro- and (C) Elcutlicwdactijlus richmondi (AS 12623, X 4.5). LYNCH: LEPTODACTYLOID FROGS 45 17 Neotropical leptodactylid genera. Few species of Eleutlierodactyhis char- acteristically have a frontoparietal fon- tanelle as an adult. Boulenger ( 1882 ) reported this condition in E. cuiiipes, but I think he confused the skeletons of E. curtipes and E. ichijmperi. The nasals are in median contact in Amhhjphnjmis, Barycholos, Batracho- phnjmis, Caiidwerbera, Crossodacty- lodes, Cycloramphus, Eleutlierodactylus, Hylocfophnjne, Ischnocnema, Mixo- phyes, Fhiloria, Scythrophrys, Syrrho- phus, Tomodactyhis, Zachaenus, in all but two genera (Paratehnatohius and Pseudop(dudicoJa) of the Leptodactyli- nae, the Ceratophryinae, and are in con- tact or very narrowly separated in all but one genus (Taiidactylus) of the Myo- batrachinae. The nasals are slightly to moderately separated in Adelotus, Cy- clorana, Eiiparkerelh, Eiipsophns, He- leioporus, Holoaden, HyJorina, Limno- dynastes, Megaelosia, Neohatrachus, Niceforonia, Notaden, Odontophrynus, Paratehnatohius, Proceratophrys, Smin- thUhis, Tehiiatohim, Telmatohtifo, and Thoropa. The nasals are widely sep- arated in Batraclnjla, Crossodactylus, Hekophryne, Hylodes, Kyarranus, Pseti- dopahidicola and Taiidactyhis. In those genera with slight separation of the nasals, the separation may be due to a general reduction of bone or to an an- terior extension of the sphenethmoid, as in Proceratophrys (Fig. 17). Without developmental studies, separation of the latter two groups is not feasible. Contact between the nasals and fron- toparietals is uncommon in the Lepto- dactylidae. When these bones are in contact, the sphenethmoid is not visible dorsally unless there is a partial separa- tion of the frontoparietals anteriorly (as in Cycloramphus) or a posteromedial separation of the nasals (as in Ambhj- phrynus, Eleutlwrodactyhis, and Procera- tophrys). Relatively broad nasal and frontoparietal contact occurs in the gen- era Caiidiverhera, Ceratophrys, Cyclo- ramphus, Hydrolaetare, Lepidohatrach- us, and Phdoria; tenuous contact occurs in Glauertia, Mixophyes, and Myo- hatrachus. The nasals and frontoparietals of all specimens of Leptodactyhis I have examined are separated, although Gal- lardo ( 1964 ) reported contact in the Leptodactyhis ocellatus group. Ornamentation of the frontoparietals, as expressed externally in cranial ridges or crests, has been noted by many authors dealing with the Leptodactyli- dae. Development of crests has often influenced generic recogniton (e.g., Eleutherodactylus hiporcatns, cornutus, and galdi groups). Much of the early systematic study of the Bufonidae in- volved minor variations in the develop- ment of such crests, and it is in Bufo that the greatest development of crests occurs (e.g., Bufo typhomus) . The fron- toparietal ornamentation in leptodactyl- ids varies from slight ridges above the orbits (Niceforonia) to the heavy crest development and exostosis seen in Cy- clorana australis, Eleutlwrodactylus hi- porcatus, E. cornutus, E. devillei, E. galdi, E. sulcatus, and Proceratophrys cristiceps, to the dermostosis of the skull bones seen in the ceratophiyines and Caudiverbera. The ornamentation be- gins at the lateral edges of the fronto- parietals near the posterior edge of the orbit and proceeds posteriorly, then medially, and finally anteriorly. Concur- rent with the development of ornamen- tation on the nasals, ornamentation be- gins on the otic plate of the squamosal. The thickening of the frontoparietal posteriorly and/ or the involvement of the dermis of the head in co-ossification results in the enclosure of the carotid artery in a bony canal. Posteriorly, this results in a carotid foramen (Figs. 18- 19 ) . Distinct carotid foramina are found in the ceratophryines and Caudiverbera, but not in other Neotropical genera. The carotid artery usually passes above the otic region of the skull between the epi- otic eminences and the edge of the fron- toparietal shelf. This is true of Heleo- phryne and all Australo-Papuan genera 46 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 18. Occipital canal and foramen devel- opment in non-casque-headed leptodactylids. (A) open canal, Notaden nichoUsi, KU 93582, X L2, (B) short enclosed canal, Heleioponis eijeri, UMMZ 124504, x 1.4, (C) long enclosed canal, Mixophyes fasciolatiis, KU 56627, x 1-2, and (D) Lechriodiis fletcheri, AMNH 59488, X 1.4. except Cylorana, Heleioponis, Kyarran- us, Lechriodiis, Mixophyes, Neobatrach- us, Notaden, and Philoria. In Cyclo- rana and Notaden the carotid artery lies in a shallow or deep, exposed channel (Fig. 18), whereas in the other genera the passage is overlain by bone to form a short (Heleioponis, Kyananiis, Neo- hatraclnis, and Philoria) to long (Lechri- odiis and Mixophyes) canal (Fig. 18). The crista parotica is, for purposes of my discussion, more a region than a B,, ->. "--^lP^ ^s^^ S5^~x ^^g — ^^ Figure 19. Squamosal-maxillary angles in lep- todactylid frogs. (A) Neohatrachus picttis, /_ =55° (FMNH 97281, X 1.2, (B) Myobatrachtis goiddi, angle not subject to measurement ( KU 110333, X 2.4, (C) Eleuthewdactyhis bufoni- formis, /=53° (KU 80621, X 0.6), and (D) Leptodacfyhis insidarum, / =36° ( KU 41026, XO.6). structure. It is the otoccipital (fused ' prootic and exoccipital) lateral to the epiotic eminences. In leptodactylids the cristae paroticae are either short and stocky or long and narrow. In Eleuthero- dactyhis these two groups tend to grade into one another. Fusion of the otoccipital to the fron- toparietal is known in several bufonid groups (Tihen, 1960a, 1962a) as well as in SyrrJwplms (Baldauf and Tanzer, 1965). Among the 57 genera of lepto- dactylids this fusion occurs only in EleutJierodactyhis and some of its allies (EuparkereUa, SmintliiUus, Syrrhophus, and Tomodactyhis). All but one species group of West Indian EleiitJierodactyhis {inoptatiis group) have the otoccipital and frontoparietal fused, as do some of the species of Eleiitlierodactyhis living in the higher parts of the Andes in Colom- bia, Ecuador, and Venezuela. Schaeffer (1949) regarded the pres- ence of a temporal arcade (articulation between the squamosal and frontopari- etal over the cristae paroticae) to be unique to Caudiverbera, among lepto- dactylids. The distribution of the char- acter in other frog families is sporadic. In several genera, lateral growth of the frontoparietal is such that the fronto- parietal almost meets the squamosal, but fails to do so because the squamosal is not expanded medially (Anotheca, Eopelobates, and Pelobates, except P. ciiltripes, where contact occurs). Sev- eral bufonids have a suture between the otic plate of the squamosal and the frontoparietal, as do the following hylid genera: AparaspJwnodon, Corijthoman- tis, Heniipliractiis, Pternohyla (fodiens, but not dentata), Trachycephalus, and Triprion. The suture is present in only three leptodactylid genera — Caudiver- bera (including Eopliractus and Gigan- tobatrachus) , Ceratophrys (including Chacophrys), and Lepidobatrachus; these genera include only a dozen spe- cies, slightly fewer than the number of species of hylids exhibiting sutural con- tact between the squamosal and fronto- LYNCH: LEPTODACTYLOID FROGS 47 parietal. The intrageneric variation in this character in Pelobates and Pterno- Jnjla serves as adequate warning as to the amount of weight that can be given this character; fortuitously, there is no intrageneric variation in this character in the leptodactylid genera, so they can be diagnosed by the presence of the suture. Expression of the sutural contact always accompanies casque develop- ment. Temporal Architecture Griffiths (1954) pointed out the pos- sible use of the squamosal-maxillary angle in ascertaining the relationships of higher frogs. The squamosal-maxillary angle is the angle formed by the body of the ventral ramus of the squamosal and the maxillary arch. The muscula- ture of the region (principally the m. depressor 7nancUbnlae) has been used to separate the Pelobatidae from the higher frogs and to separate the Bufonidae (and Atelopodidae) from the Hylidae and Leptodactylidae (see page 34). The discussion here is concerned with the squamosal bone and the associated an- gle. Griffiths (1954, 1959, 1963) reported that all leptodactylids have squamosal- maxillary angles between 45° and 50° and that the bufonid-atelopodid com- plex has an angle greater than 55°. My investigation of this character complex does not support Griffiths' statements. Leptodactylids have an observed range of from 15° to nearly 90°. The curva- ture of the posterior portion of the max- illary arch and the inner edge of the ventral ramus of the squamosal often renders measurements of angles difficult or impossible. In addition to a dorso- ventral curvature of the maxillary arch, there is a lateral curvature of the quad- ratojugal in many genera. Loss of the quadratojugal precludes measurements of the squamosal-maxillary angle. The peculiar rotation of the cranial elements of Myobatrachiis has resulted in a tenu- ous contact between the strongly curved (dorso-ventral) quadratojugal and max- illa (Fig. 19). Use of the squamosal- maxillary angle in any suprageneric clas- sification of frogs is hazardous at best. StaiTctt (1968) came to this same con- clusion. The presence of an otic plate of the squamosal in casque-headed frogs was noted above. In general, the otic ele- ment of the squamosal is not well de- veloped and does not overlie the otoccip- ital. In Caudwerhera, Ceratophnjs, and Lepidohatrachus, the otic plate is large. In Ceratophnjs a posttemporal fenestra (Fig. 20) is formed by the contact of the squamosal and frontoparietal. The otic plate of the squamosal and laterally expanded frontoparietal rest flush on the otoccipital in Caudiverbera and Lepi- dobatrachus. Figure 20. Posterior views of skulls of (A) Ceratophnjs calcarata (JDL S-237) and ( B) Caudwerhera caudiverbera (FMNH 9703) il- lustrating presence and absence, respectively, of temporal fenestrae. The lower figure is also a type II occipital condyle arrangement; compare with figure 29B. X 0.5. In lateral profile, several variations on the "typical" squamosal are apparent in the lengths and sizes of the zygomatic and otic rami (Fig. 21). The myobatrach- ine genera have short, knob-like zygo- matic rami and elongate otic rami of the squamosals. The otic plate, if present, is a narrow structure and not clearly de- fined. This pattern also occurs in the West Indian Eleutherodacttjlus, Smin- 48 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 21. Variation in length of rami of squamosals. (A) Procciatophrys boiei ( KU 9.3076, X 4), (B) Cijcloramphus eleuthewdactijlus ( KU 92785, X 3.5), (C) Zachaenus steinegeri (KU 92747, dorsal view X 9), (D) Eleutliewdactyhis fitzingeri (KU 117.358, X 3.5), (F) Telmatohius marmoratus (UMMZ 68179, X 3), and (F) Eleutherodacttjlus diastema (KU 68263, X 6.8). t- thillus, Syrrhophiis, Tomodactyhis, and a few mainland Eleutlierodactylus. The otic ramus is very short in Batraclw- phnjnus, Neoprocoela, Telmatohius, and TeJmatohufo; in these genera, the zygo- matic ramus is moderate in length. The zygomatic and otic rami of all other lep- todactylids (except Caudiverhera, Cera- tophnjs, Cyclorana amtralis, EJeutJiero- dactyhis ruthae, Lepidohatrachus, Me- gaelosia, and Proceratoplirys) are equally developed. An otic plate is developed in many groups. Caudwerhera, Cerato- plirys, and Lepidohatrachus have a broad maxillary-squamosal articulation which completes the ventroposterior margin of the orbit. Cyclorami australis and Proceratoplirys have broad articula- tions between the squamosal and maxil- la, but in these species there is no pos- terodorsal growth of a squamosal process of the maxilla. In Megaelosia, there is a strong, ligamentous contact between the bones, but a suture is not apparent. The zygomatic ramus of Eleutherodactyhis rutljae is very long and in tenuous con- tact with the maxilla. A similar develop- ment of the squamosal was noted in Cyclorana alhoguttata by Parker (1940). Determination of the extent of the maxilla and squamosal in the maxillary- scjuamosal bridge of the ceratophryines is impossible without the aid of a de- velopmental series. Some authors have figured what I consider to be fictitious suture lines. In Ceratoplirys ornata froglets (stage 46), development of the bridge is clearly evident. The ventral portion of the arch is provided by a pos- terodorsal growth of the maxilla and the dorsal portion is made up of the zygo- matic ramus of the squamosal ( Fig. 74 ) . Palate Parker (1940) presented a complete survey of the anterior palate in the Aus- tralo-Papuan leptodactylids as then LYNCH: LEPTODACTYLOID FROGS 49 Figure 22. Variation in the size of the prevomerine bones of Neotropical leptodactyhds. (A) Batra- chophnjmi.s macwstomiis (KU 98127, X 1.2), (B ) Euparkerella brasiUetms {KU 93192, X 13.4), (C) Synliophus pipilam nchtiJosus ( KU 59950, X 6.8), (D) Eleutherodactijlus Cochrane (AS\'8014, X 9), (D) E. atkinsi (AS V6263, x9), and (F) £. hufoniformh (KU 80621, X 2.4). understood (Neobatraclnis, PJiiloria, and Taudactylus were not available or not recognized by Parker). Almost no data have been presented on the palate of African or Neotropical leptodactyhds except for the papers of Mehely (1904) and Parker ( 1927 ) concerning the palu- dicoline leptodactyhds (Physalaeimis, Pleurodema, and Pseiidopaludicola). Primitively, the prevomers are large and toothed; their reduction or loss is a derived condition. The prevomers are minute or absent in all members of the Australo-Papuan Myobatrachinae and the Neotropical genera Batrachophnjnus and Euparkerella as well as in some spe- cies of Eiipsophus, Niceforonia, and Syr- rhophus. An almost complete, graded series in the size of the prevomers ( from large to minute) can be demonstrated within the subfamily Telmatobiinae ( Fig. 22 ) . The prevomers are minute in Batrachophrymis and are progressively larger in Euparkerella, Syrrhophus pipi- lans, SrninthiUus Ihnhatus, Syrrhophus longipes (often toothed), Eleutherodac- tylus cochranae, E. atkinsi, and E. bu- foniformis. Reduction in the size of the prevomer does not necessarily mean that the pre- vomerine teeth are lost. Although loss of the prevomer appears to be the trend in Crinia and Syrrhophus, some members of each genus have prevomerine teeth. The prevomerine teeth have been lost in the following leptodactylid genera: Ba- trachophrymis, Crinia (part), Crosso- dactylus, Crossodactylodes, Eleuthero- dactylus (part), Euparkerella, Eupso- phus (part), Glauertia, Metacrinia, Myo- hatrachus, Niceforonia (part), Physalae- mus (occasionally present in one spe- cies), Pseiidopaludicola, Pseudophryne, Sminthilhis, Syrrhophus (part), Taudac- tylus, Telmatobius (part, intraspecifical- ly variable), and Uperoleia. Only nine leptodactylid genera are completely edentulous (Batrachophrynus, Glauertia, 50 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Metacrinia, Myohotroclms, seven species of Thijsalaemus, PseudopJinjne, Smin- tliillus, Taudactylus, and one species of Vperoleia). Loss of the prevomerine teeth has occurred in all members of three other bufonoid families ( Bufonidae, Dendro- batidae, and Rhinodennatidae) and oc- curs sporadically in the Hylidae. In the Dendrobatidae, the prevomerine bones are reduced in size and may be lost in some groups (Fig. 23). Figure 23. Anterior palatal region of Co- lostethus panamensis (KU 77681, X 10). The telmatobiine genera (Eleuthero- dactylini ) Eleutherodactijlus, Euparker- ella, SmintJiiUiis, Syrrlioplnis, and Tomo- dactylus show interesting geographic variation in the size and median separa- tion of the prevomers. The prevomers are relatively small and widely separated in the West Indian Eleutherodactylus, Etiporkerella, SmintliiUus, Syrrlioplnis, and Tomodactylus, whereas the bones are relatively larger and only slightly separated or in median contact in the Middle and South American species of Eleutherodactylus. Large prevomers (in median contact) are found in the South American genera Amhlyphrynus and Ischnocnema; these genera are probably derivatives of Eleutherodactijlus. The prevomers of the Cycloraninae and Heleophryninae are large and toothed. The median separation of the bones varies from moderate (Notaden) to none (Mixophyes). I recognize two tribes of the Cycloraninae — Cycloranini and Limnodynastini. They differ in breeding biology and in the relative positions of the prevomerine dentigerous processes to the choanae. The dentiger- ous processes in the Cycloranini lie be- tween the choanae, anterior to the pos- terior edge of the choanae, whereas in the Limnodynastini, the dentigerous processes lie posterior to the choanae. The dentigerous processes lie anterior to the choanae in Heleophryne — the prevo- mers of this genus are unique ( Fig. 73 ) . Contrary to older reports in the lit- erature, the anuran palatine does not bear teeth. The "palatine teeth" are either odontoids on the palatal bones or are the prevomerine teeth. The palatine bones are present in all leptodactylids, but they are very small in Crinia, Eu- parkerella, and Pseudophryne. In Myo- hatrachus the palatines form the major supportive elements of the anterior part of the skull. Palatal ridges occur in sev- eral of the larger Eleutherodactylus, in Batrachophrynus, Caudiverhera, Cerato- phrys, Proceratophrys, and in Cyclorana australis. Discrete odontoids occur on the palatal ridges in large specimens of Caudiverhera and Ceratophrys. The palatines are absent in several bufonid genera (Tihen, 1960a) and in all den- drobatids and rhinodermatids. In the dendrobatids, loss of the palatines is compensated for by the development of a large palatal shelf from the postero- ventrolateral edge of the sphenethmoid. The dendrobatids are clearly derived from the Elosiinae; in the Elosiinae the palatine bones are present, and a pos- teroventrolateral palatal shelf develops in Hylodes but is not especially evident in the other genera. The parasphenoid is an unpaired bone covering much of the ventral sur- face of the skull. It is tri-radiate, with an anterior ramus and two lateral alae. The anterior ramus rests anteriorly on the sphenethmoid, and the alae rest on the otic capsules. In Batrachophrynus, the anterior ramus extends well anterior to the palatines — the parasphenoid does not extend farther anterior in any other leptodactylid genus. In the Elosiinae, LYNCH: LEPTODACTYLOID FROGS 51 the anterior ramus is very short (as it is in dendrobatids ) . A median keel is found on the parasphenoid in a few lep- todactyHds — the significance of a median keel is not apparent. The lateral alae are short or long, oriented at right angles to the anterior ramus or deflected posterior, and over- lapped or not by the median rami of the pterygoids ( Fig. 24 ) . The alae are over- lapped by the median rami of the ptery- goids in the Ceratophryinae, Cyclo- raninae, Heleophryninae, in Megaelosia, in Hydrolaetare, Leptodactyhis {ftisciis, melanonotus, ocellatus, and pentadacty- hi.s groups), Limnomedusa, and Pletiro- dema (Leptodactylinae), in Amhlyphry- nus, Batrachophrynus, Caudiverbera, Crossodactylodes, Cyclora7npJius, Eupso- phus, Hylactophryne, Hylorina, Ischno- cnema, Odontophrynus, Proceratophrys, Thoropa, and Zachaenus (Telmatobii- nae). In many species of Eleutherodac- tylus, the pterygoid and parasphenoid overlap. The bones are in tenuous con- tact in Edalorhina, Hylodes, Physahe- mus, and Pseudopaludicola, as well as in some Eleutlierodactyhis. The bones are widely separated in the Myobatrachinae, Barycholos, Batrachyla, Crossodactylus, some EleutherodactyJus, Euparkerella, Holoaden, some Leptodactylus (marmo- ratiis group), Lithodytes, Niceforonia, Paratelmatobitis, Smintliillus, Syrrho- phus, Tehnatobius, Telnmtobufo, and Tomodactylus. Non-overlap of the pterygoid and parasphenoid seems to have been ac- complished in two ways — by simple shortening of both elements, or by bend- ing of the median ramus of the ptery- goid. The latter means is apparently the most common in the Leptodactylinae, in which an almost complete graded series can be demonstrated. The tri-radiate, paired pterygoids articulate laterally at two points on the maxillary arch and medially they may (or may not) rest on the otic capsule. The anterior ramus is always longer than the median or posterolateral rami and is either in ligamentous or sutural con- tact with the maxilla (Fig. 12). Tihen ( 1962b ) used the long anterior ramus of Neoprocoela (reaching the palatines) as one character to synonymize the genus with the Bufo calamita group. Palatal- pterygoid contact occurs in five telmato- biine genera (Batrachophrynus, Odonto- phrymis, Proceratophrys, Tehnatobius, and Tehnatobufo), one elosiine genus (Hylodes), and two leptodactyline gen- era (Pleurodema and Pseudopaludicola). The palatines and pterygoids are nar- rowly separated in the telmatobiine gen- era Batracliyla, Eupsophus, and Hylo- rina, the elosiine genus Crossodactylus, and the leptodactyHne genera Limno- FiGURE 24. Ventral views of the skulls of leptodactylids with a pterygoid-parasphenoid overlap (A) Eleuthewdachihis fleischmanni, KU 68157, X 2, and one without an overlap (B) E. inop- tatus; AS X2356, X 2.4. 52 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY medusa and Pliysalaetnus; these bones are moderately separated in the lepto- dactyhne genera Edalorhina and Litho- dytes. The palatines and ptciygoids are narrowly separated in all cycloranines except Philoria (wide separation). Ac- tual contact of the bones occurs as a variation in Adelotiis, Cyclorana aus- fralis, Heleioponis, and Neohatrachus. They are widely separated in all other leptodactylid genera. A ventral flange occurs on the body of the pterygoid ( Fig. 25 ) in a few Neo- tropical genera — Cycloromphus, Hydro- laetare, and Zachaenus. Principally be- cause of the absence of this character, Zachaenus roseus Cope was removed from the genus Zachaenus. The holo- type of Z. roseus is a macerated heap of fragments, and its systematic status is uncertain. The flange may have devel- oped for the attachment of muscles used in burrowing in the genera Cycloram- phus and Zachaenus; Hydrolaetare is ap- FiGtTRE 25. Occipital view of the skull of Cijclo- ramphtis dnhiiis ( KU 92780, X 7.5) illustrating the enlarged pterygoidal flange. parently aquatic, and the flange may re- flect the habit of burrowing in mud. Otoccipital and Columella The otoccipital bone is the fused prootic and exoccipital. These bones are occasionally separate — usually in juve- niles and in species with many paedo- morphic features. Dorsomedially, the otoccipitals are bordered by the fronto- parietals. The frontoparietals and otoc- cipitals are fused in a few genera of the Eleutherodactylini. Ventrally, the otoc- cipitals rest on the parasphenoid. The columella is associated with the otoccipi- tal and rests on the cartilaginous oper- culum. The shape, size, and direction of the columella show some variation; I have not investigated these variations. The columellae are lacking in Crosso- dactylodes pintoi, Euparkerella hrasili- ensis, Eupsophus juninensis, E. monti- coki, Holoaden, Paratehnatobius, all species of Pseudophryne, Tehnatohius niger, Tehnatol)ufo hidlocki, and proba- bly in Niceforonia simonsii. I am not willing, at present, to recognize loss of the columella (or entire middle ear) as being of taxonomic value at the generic level. Gallardo (1965) regarded the degree of median separation of the occipital condyles of considerable importance in discerning intrafamilial relationships of the Leptodactylidae. This character is also reflected in the positions of the atlantal cotyles. Tihen ( 1962a ) cited the form of the occipital condyles as evi- dence of a close relationship between bufonids and the ceratophryine genera. An essentially heterocoelus condition ob- tains in Ceratophrys, Caudiverhera, and LepidohatracJnis — the condyles are not discrete elements. In the Cycloraninae, Batrachophrynus, Eupsophus, Hylorina, Heleophryne, Limnomedusa, Megaelo- sia, Pleurodema, Proceratophnjs, Tehna- tohius, and Tehnaiohufo, the occipital condyles are closely juxtaposed but dis- crete elements (Fig. 26). In the other 34 Recent leptodactylid genera, the con- dyles are widely separated. The distinc- tion between "closely juxtaposed" and "widely separated" occipital condyles may be partially size-dependent. The small species of Leptodactyhis have widely separated condyles whereas the larger species (pentadactyhis group) have the condyles less widely separated ( Fig. 27 ) . The occipital condyles are widely separated in the largest species of Eleutlierodactyhis and in the large- headed And)]yphrynus. These observa- tions suggest that some taxonomic LYNCH: LEPTODACTYLOID FROGS 53 Figure 26. Occipital views of skulls of (A) Ceratophrtjs calcarata (JDL S-237, X 2) and (B) Cychrana atistralis ( KU 93550, X 4) show- ing confluent occipital condyles as opposed to the cond\lar arrangement typical of a type II cenical cotylar arrangement. weight may be accorded this character. In small leptodactylid frogs, both condi- tions are found; I regard this observation as additional evidence in support of the use of this character as a primary tool in systematics of leptodactylids and other bufonid frogs. The condyles are closely juxtaposed in the primitive frog families, several Figure 27. Posterior views of skulls of a small Leptodactylus (A) L. qiiadrivittatus, KU 41030, X 4, with widely separated occipital condyles and, a large species, (B) L. pentadactyhts, KU 68159, X 1, with comparatively narrowly sepa- rated occipital condyles. leptodactylid genera, Rhinoderma, and all bufonids. The condyles are widely separated in all other frogs. Vertebral Column All leptodactylids have eight pre- sacral vertebrae, although the first (cer- vical ) and second vertebrae are fused in several genera. In no case is there verte- bral deletion of presacral vertebrae ( tlirough incoi-poration into the sacrum ) as is known in several bufonids (Noble, 1926b, Tihen, 1960a, 1965). The verte- brae are procoelus in most leptodacty- lids, but the majority of the Australo- Papuan and African genera have free intervertebral discs (ectochordy) or an unconsolidated intervertebral tissue (a paedomorphic trait). The anuran cen- trum has been the focus of several lengthy discussions (see Griffiths, 1963, for a summaiy, and Inger, 1967) and was one of the primary characters that Noble ( 1922 ) used in constructing his anuran phylogeny. Cervical vertebra. — The cervical and first thoracic vertebrae are fused in Ade- lotus, Heleioporus, Heleophryne, Kijar- raniis, Limnodynastes, NeobatracJuis, Notaden, and Fhiloria. The vertebrae are sometimes fused in large specimens of Ceratophrys and Lepidohatraclms, but in these genera the fusion is variable and most often reflects senility. As noted above, the occipital con- dyles are either widely separated or closely juxtaposed. The articular sur- faces are either separated or confluent. In those frogs with closely juxtaposed occipital condyles, it is difficult to de- termine whether the articular surfaces are narrowly separated or confluent; this distinction can be made by examining the cotylar arrangement of the cervical vertebra. The variation in cervical cotylar ar- rangements permits the definition of three classes (Fig. 28). Type I: the cervical cotyles are widely spaced (this class is the concave atlas pattern of Gallardo, 1961, 1965). 54 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 28. Three patterns of atlantal cotylar arrangements. (A-C) Dorsal, lateral, and anterior views of cervical vertebra of Ceratophnjs calcarata (JDL S-237), (D-F) Livwodynastes dorsalis (UMMZ S-165), and (G-I) Eleiitherodactijlus ntgidostts (JDL S-1238); Types III, II, and I, respectively. All X 5. This pattern is the most widespread in leptodactylids and advanced frogs. In this class, the cotyles are sometimes stalked; when they are stalked, there is a prominent gap between the cervical vertebra and exoccipital bridge (Fig. 29). Type II: the cervical cotyles are nar- rowly separated and there are two dis- tinct articular surfaces. In many species, there is a deep notch between the cotyles ( Fig. 28D ) . In most of the frogs with a type II cervical, the occipital condyles are clearly discrete articular surfaces. Type III: the cervical cotyles' are confluent and represent a single articular surface. The occipital condyles are con- fluent and the occipital-cervical articular pattern is hererocoelus. Only two lepto- dactylid genera (Ceratophnjs and Lepi- dohatrachus) have a type III cervical vertebra. Consistent fusion of the cervi- cal and second vertebrae is found in eight Australo-Papuan and African gen- era with type II cervicals. Type II cervical vertebrae occur in AdeJotus, Batrachophninus, Caudiver- hera, Cijclorana, Eupsophus, Heleiopor- us, HeJeophnjne, Kijarranus, Limnody- nastes, Me<^aelosia, Mixopliyes, Neobat- rachus, Notaden, Philoria, Procerato- phrys, Tehnatobius, and Tehnatobtifo. The Oligocene Neoprocoeki has a type II cervical. The occipital condyles are very large in Limnomediisa, Odonto- plirynu.s; and Pleurodema; the cervical LYNCH: LEPTODACTYLOID FROGS 55 Figure 29. The two occipital-cervical articula- tion types in the Leptodactylidae. (A) Eleu- therodacttjhis sulcatus, KU 100355, X 2; and (B) Cyclorana australis, KU 93550, X 2. pattern is intermediate between type I and type II cervical patterns. In all other leptodactylid genera, the type I cervical is uniformly present. The Australo-Papuan Cycloraninae all have type II cervical vertebrae, and the Myobatrachinae all have type I cer- vical vertebrae. One genus of the Elo- siinae has a type II cervical (Megaelosia), and the other two genera have type I cervical vertebrae. The Leptodactylinae have only type I cervical vertebrae, al- though two genera (Limnomedusa and Pleurodema) have an intermediate type cervical. In the largest leptodactylid subfamily, the Telmatobiinae, type II cervicals are found in all of the genera of the Telmatobiini, in two of the four genera of the Alsodini, and in one of the genera of the Odontophrynini. Only type I cervicals are found in the Grypis- cini and Eleutherodactylini. The cer- vical vertebral type seems to be very useful in ascertaining the relationships of leptodactylids. The type II cervical is probably primitive, as evidenced by the uniform occurrence of this type in the archaic frog families and Pelobati- dae. Type II cervical vertebrae are also characteristic of the Bufonidae and Rhinodermatidae. Presacral vertebrae. — Hecht (1960) pointed out that the primitive frogs have very short transverse processes on the posterior presacral vertebrae, and prin- cipally for this reason he associated Eorubeta (Eocene) with the advanced frog families. Zweifel (1956a) demon- strated that some of the pelobatids of the subfamily Megophryinae have long transverse processes of the posterior pre- sacral vertebrae (as long as the sacral diapophyses) and very long (here termed expanded) transverse processes of the anterior presacral vertebrae. Some Megophryinae have short posterior pre- sacral vertebral transverse processes {LeptobracJuiim, Boulenger, 1908). As noted by Hecht (1960) the transverse processes of the posterior presacral vertebrae of most leptodactylids are as long as or only slightly shorter than the sacral diapophyses. However, in sev- eral of the more primitive leptodactylid genera, the transverse processes of the posterior presacral vertebrae are short- ened to varying degrees (Fig. 30). The transverse processes of the anterior pre- sacral vertebrae seem to vary in length independently of the variation in the length of the transverse processes of the posterior presacral vertebrae. The short- ening of the transverse processes of the anterior presacral vertebrae and the concurrent lengthening of the transverse processes of the posterior presacral verte- brae represent an evolutionary trend in frogs. The transverse processes of the anterior (second, third, and fourth) pre- sacral vertebrae are widely expanded (much wider than the width of the 56 MISCELLANEOUS PUBLICATIOX MUSEUM OF NATURAL HISTORY sacral diapophyses ) in Ceratophnjs and Lepidohatrachus. The transverse proc- esses of the anterior presacral vertebrae are slightly expanded in Cydorana, Odontophnjmis, Proceratophnjs, and Telmatobiifo. The transverse processes of the anterior presacral vertebrae are not wider than the width of the sacral vertebrae in all other leptodactylids and are shortened (their greatest width is less than the width of the sacral dia- pophyses) in Crinia and Pseudoplnyne (Fig. 31). The transverse processes of the pos- terior presacral vertebrae are greatly shortened (knob-like) in Neobatraclms and Notaden (Fig. 30), very short (less than one-half the width of the sacral Figure 30. Posterior vertebral columns of four genera of cycloranine leptodactylids illustrating reduction in transverse processes in advanced Cycloranini, and presence of lateral flanges on urostyle in primitive genera of subfamily. (A) Limnodtjnastes tasmaniensis, AMNH 60589, X 5; (B) Cydorana australis, KU 93550, X 2.5; (C) Hek'iopows eijeri, UMMZ 124504, X 2.5; and (D) Neobatraclms centralis, KU 93578, X2.5. diapophyses) in Crinia, Heleioporus, LepidobatracJnts, and Pseudophryne, and moderately to slightly shortened in Caudiverhera, Ceratophrys, Cydorana, Cydoramphus, Eiipsophus, Glauertia, Heleophryne, Myobatradnis, Odonto- pJirynus, Proceratophrys, and Uperoleia. In all the other 39 leptodactylid genera, the transverse processes of the posterior presacral vertebrae are as wide as the sacral diapophyses. CeratopJirys and Lepidobatradnis have a bony shield overlaying the sec- ond, third, and fourth vertebrae (Fig. 31). In Ceratophrys, the shield is at- tached to the neural spines by ligaments. Among the species of Ceratophrys, there is little variation in the size and shape of the shield; some species of the genus have been reported to lack a dorsal shield, but I have not seen any adult Ceratophrys that lack the shield, al- though most juveniles of Ceratophrys lack a vertebral shield. In Ceratophrys, the shield is a loosely consolidated plate of osteoderms. Based on limited obser- vations, the number of elements in the plate is reduced by fusion of adjacent plates with increasing age. I have not seen any specimens with only one or two elements in the shield. Dermostosis of the shield occurs in both genera. In Lepidobatradnis laevis, the shield is small and fused to the neural spines; the shield is larger in L. asper and L. llanen- sis and is connected to the vertebrae by ligaments (Reig, 1960b, Reig and Cei, 1963). Sacral vertebrae. — The sacro-coccy- geal articulation is bicondylar in all lep- todactylids including the African and Australo-Papuan genera with ectochor- dal vertebral columns. Several authors (Noble, 1930, 1931, Schaeffer, 1949) noted the differences in the dilation of the sacral vertebral diapophyses. Schaef- fer (1949) implied that all Australo- Papuan leptodactylid genera had dilated sacral diapophyses and all Neotropical genera had narrow (rounded) sacral diapophyses. Noble (1931) and Reig LYNCH: LEPTODACTYLOID FROGS 57 (1960a) pointed out that at least some of the Neotropical genera characteris- tically have dilated sacral diapophyses. The sacral diapophyses are broadly dilated in all pelobatids, bufonids, and most hylids. The fossil Oligocene lepto- dactylid, Neoprocoela, has broadly di- lated sacral diapophyses, as does the enigmatic Chilean Rlunodenna. No ex- tant leptodactylid genus has broadly dilated sacral diapophyses, although it is impossible to place lower limits on Figure 31. Vertebral columns of (A-B) Ccratophnjs aiiiita, A has the bony shield removed ( KU 98129, X 0.9; FMNH 51704, X .9), (C) Lepidohatmchiis asper ( KU 80783, X 2.2), (D) Crinio slgniferaiKU 56243, X 6.4) and (E) Leptodactyliis pentadactijlus (KU 68159, X 0.9). 58 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY the character of "dilated sacral dia- pophyses." The sacral diapophyses are moderately dilated in all of the Australo- Papuan genera and in eight Neotropical genera (Batrochylo, Caudiverhera, Cros- sodactylocJes, Edalorhina, Eupsophus, Odontophnjnus, PhijsaJaemus, and Fleu- rodema). Any distinction between the degree of dilation exhibited by some of the abox'e-mentioned genera and such leptodactylids as Ceratophnjs and Fara- telmatobius is a very fine one and prob- ably is not defensible. The majority of the African and Neotropical leptodacty- lid genera have rounded, undilated sacral diapophyses which are either per- pendicular to the sagittal plane or slanted posteriorly (Fig. 32). Figure 32. Sacral vertebrae of leptodactylids and a bufonid illustrating the degree of expan- sion of the sacral diapophyses. ( A ) Eletithero- dactylus nigulosus (JDL S-I238, X 4), ( B) Odontophnjnus cultripes ( KU 92975, X 2.5), (C) Cijclomna dalili (UMMZ 65250, X 3), and (D ) Bufo marmoreus ( KU 84894, X 2 ) . Coccyx. — I have not observed zyga- pophyseal processes on the anterior por- tion of the coccyx of any leptodactylid, although S. B. McDowell (in litt.) has observed prezygapophyseal processes on the coccyx of Metacrinia. The coccyx is short and stocky in several genera; nerve foramina are evident on the anterolateral surface of the coccyx in several leptodac- tylids. Neither of these characters shows a clear trend but appears sporadically among the species I have examined. Batrachoplirynus has large transverse processes at the anterior end of the coc- In the Elosiinae, the neural arches cyx (Fig. 79). are distinctly non-imbricate and poorly ossified. The roof of the neural canal of the coccyx is likewise poorly ossified. Pectoral Girdle The primary basis for the divisions of the advanced frogs by Cope and Boulen- ger was the variation in the architecture of the pectoral girdle. The two divisions, the Arcifera and Firmisterna, differ in the overlapping epicoracoidal cartilages in the former and the median fusion of the epicoracoidal cartilages in the latter. Noble (1921, 1922, 1931) severely criti- cized the Cope-Boulenger system after he found several South American frogs with intermediate types of pectoral girdles. Griffiths (1959, 1963) redefined the terms arciferal and firmisternal on the basis of the presence (arciferal) or absence (firmisternal) of free epicora- coidal horns. Griffiths also pointed out that the two types of pectoral girdles have different developmental patterns. When the primary basis of frog clas- sification changed from the pectoral girdle to the vertebral column and tliigh musculature, relatively few groups shifted between the Arcifera ( ^Procoe- la and Bufonoidea) and the Firmisterna (=Diplasiocoela and Ranoidea). The Dendrobatidae, GeohatracJws, Rhino- derma, and Sminthillus (Euparkerella, Noblella, and SmintliiUus) were alter- nately associated with the Bufonoidea and the Ranoidea. Noble (1926b and 1931) considered all of these genera to be bufonid derivatives, whereas Griffiths ( 1959 ) considered the dendrobatids to be a Neotropical subfamily of the Rani- dae, Geobatrachtis and Rhinoderma to be the only members of a Neotropical leptodactylid subfamily, and Sminthillus to be a polyphyletic assemblage of EleutJwrodactyliis derivatives. Most leptodactylid frogs are clearly arciferal (in either Cope's sense or Grif- fiths' sense). Prior to the refinement of the distinction between arcifery and firmisterny, the leptodactylid frogs of the genera SmintliiUus and Noblella were LYNCH: LEPTODACTYLOID FROGS 59 characterized by their arcifero-firmister- nal pectoral girdles. Noble ( 1921, 1922, 1926b, 1931 ) considered the epicoracoid- al cartilages of SiuinthiUus to be fused from a point at the base of the omoster- num to the anterior edge of the coracoid, whereas Griffiths (1959) found that the epicoracoidal bridge was restricted to the anterior-most portion of the carti- lages and always restricted to a narrow zone anterior to or between clavicles. I have found epicoracoidal bridges in both small and large species, but the fusion is most often found in the smaller speci- mens, because one tends to be less me- ticulous in the dissection of larger speci- mens. All leptodactyhds have discrete epicoracoidal horns which are usually partially concealed by the sternum. Hoffman (1930) reported Heleophnjne to pass from arcifery in juveniles and subadults to firmisterny in adults. Poyn- ton ( 1964 ) pointed out that Heleophnjne is always arciferal and that Hoffman's "old adult Hehophnjne" was a specimen of a ranid (either Hijhimhates or Lepto- pelis). All other leptodactyHd genera are, and have always been, regarded as arciferal in the sense of Cope and Boulenger.^ The relative bulk of the clavicle and coracoid, the presence of an omoster- num, and the presence of an osseous sternal ( post-zonal ) element are variable characters in the pectoral girdles of lep- todactylid frogs. Piatt (1934) distin- guished three types of omosterna and three types of sterna in 35 species of lep- todactylids (Eleittherodoctyhis, Lepto- cloctylus, and LitJiodytes) based on the character states uniformly cartilaginous, partly calcified, and containing an os- seous element. I am unwilling to place much taxonomic weight on small varia- tions in the size of the omosternum and sternum, or on the distinction between uniformly cartilaginous and partly cal- cified. Calcification of the sternum oc- curs in large females of several species in which the sternum of the smaller male is uniformly cartilaginous. The larger specimens of a given species are more likely to have some calcification of the sternal plate than are the smaller specimens of the species. In several lep- todactyHd genera, the differences in the average adult size of the various species of that genus are reflected in the pres- ence and absence of calcification of the sternum and often of the omosternum and epicoracoidal cartilages. Although fully cognizant of the limitations of both, I consider the following characters to be useful in distinguishing the genera of leptodactylids: 1) presence of a carti- laginous or calcified sternal plate versus the presence of a discrete osseous ster- nal element (usually a style) and 2) presence of an omosternum. The sternum in most leptodactylids is a cartilaginous plate (Fig. 33); in the Neotropical Leptodactylinae (Barycho- los, EckilorJiina, Hydrolaetare, Leptodac- tylus, Limnomedtisa, Litljodytes, Fara- telmatohiiis, Physahemus, Fleurodema, and Fseudopaludicola) the sternum con- tains an osseous (or calcified) style or an osseous plate (Paratelmatobiiis). Litli- odytes also has an osseous style in the omosternum; the omosternum is carti- laginous in all of the other genera. Parker ( 1940 ) reported that the omo- sternum was reduced in size or absent in all Australo-Papuan leptodactylids. In the Australo-Papuan genera Adelotus, Cyclorana, Lechriodus, Limnodynastes, and Mixophyes, the omosternum is large to moderately large ( Fig. 33 ) . The omo- ' Barrio ( 1970 ) named a new Chilean genus (Instietophrynus) with a pseudofimiisternal pec- toral girdle similar to that seen in some Ateloptis, but having a well-developed prezonal element. Figure 33. Pectoral girdles of ( A ) Heleophnjne natalcnsis (KU 105925, X 1.5), (B) Limno- dynastes peronii ( KU 93562, x 1.2), and (C) Crinia signifera ( KU 56317, X 4). 60 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY sternum is absent in Mijohatrachus and reduced in size in the other Australo- Papuan genera of the Myobatrachinae and the cycloranine genera Heleioporus, Kyorranus, Neohatraclnis, Notaden, and Philoria. The omosternum in Crinia is usually elongate and not separable from the anterior extent of the epicoracoidal cartilages (Fig. 33). The omosternum is present in all other leptodactylids that I have examined except Lepidobotm- dnis, OdontopJirynus, Froceratophnjs, and EhutherodactyJus ruihae, although the omosternum is small in several spe- cies of the West Indian Eleutherodac- tyhis. The omosternum is unusually large — often larger than the sternum — Fk;ure 34. Pectoral girdles of leptodactyline leptodactylid (A) Pseudopaludicola ameghini (KU 93050, X 5.5 ) and two telmatohiines ( B) Tclmatohiiis hautholi ( KU 72879, X 2) and (C) Eleiitherodacti/lus hogotcnsis ( KU 110409, X4). in a few Neotropical leptodactylids (Ceratophrys and Telmatobufo). The clavicles are large and strongly arched in the Ncoti-opical genera Caudi- verhera, Tehnatobiiis, and Tebnatobufo, and are very slender and fragile in many of the smaller species of leptodactylids ( Fig. 34 ) . In most species of the fam- ily, the clavicles are neither massive nor fragile. The clavicles are relatively straight in most Neotropical leptodac- tylids (except the Ceratophryinae and Telmatobiini) and many Cycloraninae. In most myobatrachines the clavicles are slender and strongly arched (Fig. 33) but in Myobatrachus the clavicles are massive and only slightly arched. The following generalizations con- cerning the architecture of the leptodac- tylid pectoral girdle are suggested: 1) arcifery is the primitive character state — pseudofirmisterny is derived and of little taxonomic significance; 2) an osse- ous element in either the pre-zonal or post-zonal element is secondary to uni- formly cartilaginous elements; calcifica- tion of the sternal plate is a labile fea- ture; and 3) primitively, the omosternum is large — reduction in size or loss of the omosternum is derived. The osseous post-zonal elements of leptodactylines are primitively broad and become more style-like in the ad- vanced genera (Fig. 35). Posterior bi- furcation of the style is derived. Pelvic Girdle The pectoral girdle has long been recognized as an important complex for systematic studies of anurans whereas few authors sought to find characters in the simpler pelvic girdle, which is more closely associated with the primary adaptive shift of frogs — jumping. The anuran pelvis is composed of three ele- ments (ilium, ischium, and pubis) of which only the ilium exhibits familial or consistent generic variation. Some pale- ontologists (e.g., Auffenberg, Chantell, Estes, Holman, and Tihen) considered the ilium of paramount importance in LYNCH: LEPTODACTYLOID FROGS 61 Figure 35. Pectoral girdles of four leptodacty- line leptodactylids. (A) Phtj.salaeiniis ])ustuIosiis (KU 68272, X 5.5), (B) Leptodactyliis mcla- nonotus ( KU 68276, X 3), (C) Physalaemus signifcnis (KU 93033, X 5.5), and (D) Para- telmatohiiis hitzi ( KU 107089, X 5.5). the identification of disarticulated frog fossils at the familial, generic, and, in some cases, specific level. Brief refer- ences were made by some of these authors to the range of variation ex- hibited by the leptodactylid genera. Holman (1965) noted the variation in development of the ilial crest and in the size and shape of the ilial promi- nence (termed by him, vastus promi- nence). The nomenclature for the ilial morphology adopted here follows that of Chantell (1964) and is illustrated for lep- todactylid frogs in Figure 36. The only additional term employed here is the "preacetabular zone" — that area of the ventral acetabular expansion lying anter- ior to the lip of the acetabulum and dor- sad to the ventral lip of the acetabulum. Owing to the diverse forms of the ilium in leptodactylids, no familial diag- nosis can be made at this time. The rela- tively few genera available support this conclusion. Skeletons of the following genera were available: Adelotus, Barij- chohs, BatracJwpJinjmis, Caudiverbera, Ceratophrys, Crossodactylus, Cyclorain- phus, Cyclorana, Edalorhina, Eleuthero- dactylus, Eupsophus, Heleioporus, Hy- lactophryne, Hylodes, Isclinocnema, Kyarramis, Lechroidus, Lepidobatra- chus, Leptodactyliis, Limnodynastes, Limnomedusa, Megaelosia, Neobatra- cJiiis, Notaden, Odontophrynus, PJujsa- laemiis, Pleiirodema, Proceratophrys, Pseiidophryne, Syrrliophus, Tebnutobius, Thoropa, Tomodactyhis, and Zachaenus. The two ilial types are briefly de- scribed below. Ceratopliryine type: ilial shaft rela- tively short; dorsal crest not developed, if present, in form of ilial shaft ridge; dorsal protuberance not, or but slightly, differentiated from spike-like dorsal prominence; dorsal acetabular expansion well developed, distinct dorsal vector; preacetabular zone present, broad; ven- tral acetabular expansion relatively Figure 36. Nomenclature of the leptodactylid ilium. Top is ilium of Cerafophnjs ornata (genus lacking dorsal crest); middle is that of Lepto- dactijlus pentadactyhis (genus with dorsal crest). (A ) dorsal acetabular expansion; ( B ) dorsal pro- tuberance (vastus prominence of Holman); (C) dorsal prominence; ( D ) acetabular fossa; (E) ventral acetabular expansion; (F) shaft; (G) dorsal crest. The preacetabular zone is hatched in the lower figure. 62 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY small; angle of ventral acetabular ex- pansion greater than 90°; acetabular fossa relatively small (Fig. 37). Leptodactyline type: ilial shaft rela- tively long; dorsal crest well developed, usually higher anteriorly and in the re- gion of dorsal protuberance; dorsal pro- tuberance relatively large [vastus prom- inence of Holman ( 1965 ) ] , ovoid, or tear-drop-shaped, situated on a large dorsal prominence which is confluent with dorsal crest; posterior border of dorsal prominence gently sloping; dorsal acetabular expansion not well developed, little or no dorsal vector; preacetabular zone present, broad; ventral acetabular expansion relatively large; angle of ven- tral acetabular expansion much less than 90°; acetabular fossa relatively large (Fig. 37). Figure 37. Right ilia of (A) Pseudophryne hihroni, AMNH 64511, X 5.4; (B) Adelotiis hrevis, AMNH 59489, xL6; (C) Cydorana (lustralis, AMNH 62228, X 1.2; (D) Liiuno- dynastes dorsalis, KU 93553, X 1.6; (E) left ilium of Neohatmchus centralis, KU 93578, X 1.6; and (F) right ilium of Notaden hennetti, FMNH 97858, X 1.2. The ilia of the two genera of the Ceratophryinae are nearly impossible to separate. Lepidohatrachus has a more distinct ilial shaft ridge than does Cera- tophnjs and a slightly less pronounced dorsal prominence (spike); too few specimens are available to make a gen- eralization. Odontophnjmis and Procera- tophrys ( Telmatobiinae, Odontophryn- ini) are the only other Neotropical gen- era examined which have the cerato- phryine pattern. Both genera differ from the Ceratophryinae in having a more distinct dorsal protuberance, larger ventral acetabular expansion, and less obtuse angle of ventral acetabular ex- pansion (Fig. 38). Several cycloranine genera have ilia which differ only slightly from the cera- tophryine pattern. All Australo-Papuan genera examined have a relatively large angle of ventral acetabular expansion (90-110°) and relatively small acetabu- lar fossa. The dorsal prominence is never spike-like and most genera have a distinguishable dorsal protuberance (e.g., Adelotiis, HeJeioponis, Lecliriodus, and 'Neohatrachus) . The dorsal protu- berances of Kijarranus and Limnody- nastes are only slightly less differen- tiated, but those of Cydorana, Notaden and the myobatrachines are not distin- guishable from the dorsal prominence. Dorsal crests are lacking in the myo- batrachines, and all cycloranines exam- ined except Adelotiis, Kyarranus, and Lecliriodus (Fig. 38). The angle of ventral acetabular ex- pansion is slightly greater than 90° in Caiidiverhera, Edalorliina, Eleutliero- dactylus, Engystomops, Eupsoplnis, Hy- lactophryne, Limnomedtisa, Pleiirodenia, Syrrhoplnis, Tomodactylus, and Zachae- nus, whereas it is markedly acute in Crossodactylus, Cycloramphus, Hylodes, Leptodactylus, Megaelosia, and Tlioropa. In Batrachophryniis, Ischnocnema, and Telinatobhis it is about 90°. The dorsal crest is absent in Edalo- rliina, Eupsophus, Physalaemus, and Pleurodema. In some Eletitlierodactyltis and the Mexican Syrrhoplnis and Tomo- dactylus, the dorsal crest is reduced to a small area immediately anterior to the dorsal prominence. This latter condition is also seen in Limnomedusa. The dor- sal crest is well developed in Caiidiver- hera, Crossodactylus, Cycloramphus, most Eleiitherodactylus, Hyhctophryne, Hylodes, Ischnocnema, Leptodactylus, Megaelosia, and Zachaenns; in Batra- chophrynus, Telmatobius, and Thoropa LYNCH: LEPTODACTYLOID FROGS 63 Figure 38. Right ilia of (A) Hijlodes nasus, KU 92894, X 2.1; (B) Thoropa miliaris, KU 92856, X 1.6; (C) Eupsophus wseus, AMNH 22104, X 1.6; and (D) Odontophnjnus cultripes, KU 92975, X 1.6. it is low and almost ridge-like (Figs. 37-40). The dorsal protuberance is well de- veloped in all elosiine, leptodactyline, and telmatobiine frogs examined except Megaelosia and Pleuwdema. In these J latter two genera, the muscle scar for the vastus externus head of the m. triceps jemoris is broad and covers the whole of the dorsal prominence. The protuber- ance is ovoid, round, or elongate, and no characterization of genera can be made owing to the variability of the protuber- ance in Eleutherodactylus. The degree of dorsal vector in the dorsal acetabular expansion shows some variation in the Neotropical leptodacty- lids. Almost no dorsal vector is seen in Batrachophrymis, Edalorliina, Leptodac- tylus, Pleuwdema, Telmatobius, and Thoropa, whereas the other genera ex- hibit a considerable dorsal vector. Eleu- FiGURE 39. Right iha of ( A ) Eleutherodactylus diastema, JDL S-244, X 6.6; (B) £. inoptatus, AS X2356, X 1.2; (C) E. nigulosus fleisch- manni, KU 68157, X 1.2; (D) E. palmed, JDL S-242, X 3.3; and (E) Ctjcloratiiphus fulginosus, KU 92790, X 1.2. therodactylus palmeri (Fig. 39), in con- trast to the other species of the genus examined, has no dorsal vector and the dorsal crest appears to be lacking but is present and curved over the body of the ilial shaft. The ilium seems to have some merit in suggesting relationships among the leptodactylid genera, but at this time inadequate data are available in order to incorporate the variation of the ilium into my generic classification. In some cases ( Ceratophryinae and Elosiinae), the ilial variation is consistent with the \'ariations of other character complexes, but in other cases (Leptodactylinae), Figure 40. Right ilia of (A) Phijsalaemus pustulosus, KU 41031, X 5.4; (B) Pleuwdema cinerea, KU 80836, X 1.6; (C) Leptodactylus wagneri, KU 104390, X 1.2; (D) Caudiverhera caudiverbera, A.M.N.H. No. 51510, X 0.6; and (E) Batrachophrymis macrostomus, KU 98127, XO.6. the variation is not consistent with my other data. Owing to these discordan- cies, use of the ilium in a leptodactylid classification is deferred pending a broader survey of the variation in the ilia of other leptodactyhd frogs. The data now available are adequate to permit a reassessment of the status of a Lower Miocene Leptodactylus recently described from Florida. Holman (1965) named L. abavus based on five ilia from the Arikareean horizon of Thomas Farm, Gilchrist County, Florida. The frog he described and figured has almost no pre- acetabular zone, a moderately large angle of ventral acetabular expansion, and a small ventral acetabular expan- 64 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY sion. These characteristics are not t>'pi- cal of Leptodoctylus but are typical of Rana — especially the species of the R. pipiens group. There is a marked simi- larity between his figures of the ilia of Leptodactyhis abaviis, Rana miocenica, and Rana cf. R. pipiens. Leptodactyhis ahaviis Holman, 1965, is accordingly here removed from the family Leptodactyli- dae and placed in the Ranidae. The specific status of Rana abavus (Hol- man), new combination, is beyond the scope of this paper, but at present, there are no apparent differences between it and Rana miocenica, a sympatrant. Limb Elements To a certain extent, the mode of life of a frog is reflected in the proportions of the long bones (humerus, radioulna, femur, tibiofibula, and astragulus and calcaneum). Species living in paramos and those with burrowing habits tend to have heavier, stockier long bones than do the arboreal or active terrestrial frogs, in which the limb bones are relatively slender. Those differences that do exist are subtle and offer little in the way of taxonomic utility. Because the charac- ters seem more reasonably associated with ecological adaptation, they are not regarded as useful in a phylogenetic classification. The intrageneric variation in EJeutherodactyhis precludes the use of relative proportions of the limb elements for generic or suprageneric classifica- tions. The greatly enlarged arms of males of some species of Leptodactyhis have been noted by several authors. The skeletal base for the sexual dimorphism is considerably more striking. Large flanges are present on the humeri of the male, whereas the female has humeri more typical of frogs (Fig. 41). Devel- opment of humeral flanges is uncommon in the Leptodactylidae, and is most pro- nounced in the genus Leptodactyhis. The development of humeral flanges in LeptodactyJus appears to be species- group variable and therefore may prove useful in subgeneric classifications. Mod- erate flanges are seen in the Eupsophus nodosus group, again restricted to the male (Grandison, 1961), in Crossodac- tylodes, Paratehnatobius, some PJiysa- laemus, and Telmatobius (Fig. 41). Figure 41. Humeri of (A) female Leptodactyhis pentadactijhis ( lateral view of right humerus, KU 68159, X 0.8) and (B) male L. pentadacty- lus (lateral view of left humerus, KU 84981, X 0.8); medial views of left humeri of male (C) Physalacmiis signiferiis ( KU 93033, X 4.8), (D) P. awieri (KU 92999, X 4.8), and (E) Paratehnatobius httzi (KU 107089, X 4.8). Thalan<:,eal formulae. — The primitive phalangeal formulae of the Leptodactyli- dae are 2-2-3-3 for the hand and 2-2-3-4-3 for the foot. Phalangeal reduction is often regarded as a character sui generis in amphibian classifications, because it is a relatively uncommon phenomenon. The only variations on the above for- mulae in the Leptodactylidae are seen in Etiparkerella which has a 2-2-3-2 formula for the hands and a normal foot formula (Figs. 42-43) and in Limnodynastes peronii which has a 1-2-3-3 hand for- LYNCH: LEPTODACTYLOID FROGS 65 inula (all other Limnodipiastes have a 2-2-3-3). Parker (1940) and Moore (1961) briefly mentioned that the digits were reduced in some of the myobatra- chine leptodactylids (Crinia and Psetido- phrijne). In external appearance, the digits are short and stubby, but the phalangeal formulae are typical for bu- fonoid frogs (2-2-3-3, 2-2-3-4-3). Terminal PJialanges. — The nature of the terminal phalanges has been one of the major character complexes in lepto- dactylid classification. Generic diag- noses invariably contain reference to "simple, pointed, knobbed or T-shaped" terminal phalanges. Based on a literature study, there seems to be a wide range of terminal phalangeal types within the Leptodactyl- idae. The phalangeal types are termed pointed, simple, knobbed, bifurcate, Y- shaped, and T-shaped. In the past, the technique for observing the terminal phalanges was to dissect the digital tip and observe the shape of the bone. Since the terminal phalanges are often very small and delicate, dissection tends to break any lateral expansions. Observa- tions of the bones with the naked eye often fails to discern small lateral proc- esses. In my opinion, the only technique acceptable for the observation of the terminal phalanges is examination of macerated or cleared and stained speci- mens. My studies, presented below, are based almost exclusively on examination of cleared and stained material. No leptodactylid normally has pointed terminal phalanges. The most simple phalanges are very slightly knobbed (e.g., Limnodynastes and the Pseudopaludicola falcipes complex). A graded series can be demonstrated rang- ing from P. falcipes to some of the ar- boreal Eleutherodactylus with widely expanded, delicate, T-shaped terminal phalanges (Figs. 42-44). The following genera exhibit definite T-shaped terminal phalanges in all spe- cies: Batrachyla, Crossodactylodes (see Fig, 44, Y-shaped), Crossodactylus, Hel- FiGURE 42. Palmer views of the skeletons of the hands of (A) Eletitherodactylus brevicrus, KU 108982, X 10.5; (B) Euparkerella brasiliensis, KU 93192, X 21); and (C) Eleittherodactijlus binotatus, KU 92813, X 7. eophryne, Hylodes, Lithodytes, Megae- losia, Sininthillus, Syrrhoplnis, Taudac- fyhts, Thoropa, and Tomodactijlus. Mod- ified T-shaped terminal phalanges are seen in Euparkerella (Figs. 42-43). Barycholos and the Leptodactylus mar- moratiis group have terminal phalanges with moderately long lateral processes. In the genus Eleutherodactylus there is a continuum of variation in the terminal phalanges from those of E. binotatus and E. nigrovittatus (knob-like) to that ex- emplified by E. brevicrus (broadly T- shaped). The phalangeal type of all other leptodactylids, except the Pseudo- paludicola falcipes group and Limnody- nastes (Fig. 45), is included in the bot- tom of the Eleutherodactylus series [for example, Holoaden, Leptodactylus (ex- cept marmoratus group), Niceforonia, 66 MISCELLANEOUS PUBLICATIOxX MUSEUM OF NATURAL HISTORY Figure 43. Plantar views of skeletons of feet of (A) Eleutherodactyhis hogotensis, KU 110409, X 7; and ( B ) Euparkerella brasiliensis, KU 93192, X 21. Paratelmatohius, PseudopJiryne, Telma- tohius, and Zachaenus (Fig. 44)]. Use of the nature of the terminal phalanges is not invalidated by the above data. Even when the lateral processes of the terminal phalanges are reduced (as in E. hinotatus and E. nigrovittatus) , the eleutherodactyline digital groove is evi- dent externally. The lateral expansions of the terminal phalanges of the hands in £. nigrovittatus, Holoaden bradei, and Niceforonia festae are comparable, but there are true T-shaped terminal pha- langes in Eleutlierodactylus nigrovittatus but merely the lateral expansion of knobbed terminal phalanges in Holoa- den and Niceforonia (Fig. 45). Further- more, in Eleutherodactylus nigrovittatus, at the tip of each digit (except the thumb and inner toe) there is a trans- verse terminal groove. The degree of development of lateral expansions varies on the different digits of the hand and foot as well as between the hand and foot. When reduction of lateral expan- sions occurs, it is most readily observed on the hand; the toes retain relatively well developed lateral expansions. The lateral expansions of the inner digits show greater reduction than do those of the outer digits. PrepoUex and inner metacarpal. — The presence of nuptial excrescences, asperi- ties, or spines serves as an external in- dicator of some modification of the first metacarpal and /or expansion or modifi- cation of the prepollex. These changes F Si a H Figure 44. Third fingers of representative lep- todactylids (A) Eleutherodactylus nigrovittatus (USNM GOV 8108, x 17), (B) £. parvus ( KU 92834, x 17), (C) Holoaden bradei (KU 107088, X 8.5), (D) Niceforonia festae (KU 118137, X 17), (E) Tehnatohius hautholi ( KU 72879, X 4.2), (F) Leptodacttjlus melanonotus ( KU 68275, X 5.6), (G) Pseudophryne hibroni (KU 93588, X 8.5), (H) Liiiinodyiiastes peronii (KU 93566, X 8.5), (I) Pseudopaludicola pusilla (UMMZ 54589, X 17), (J) P. ameghini (KU 93050, X 17), (K) Zachaenus parvulus ( KU 107090, X 8.5), (L) Paratelmatohius lutzi ( KU 107089, X 8.5), and (M) Crossodactylodes pintoi (USNM 102611, X 17). LYNCH: LEPTODACTYLOID FROGS 67 Figure 45. Skeletons of hand of (A) Eleuthero- dactijhis niprovittatits (USNM GOV 8108) and feet of (B) Niceforonia fcstae ( KU 118137) and (G) Eleutherodactiilus iiifiwvittattis (USNM GOV 8108). All X 10.5. are not manifest in the female and while perhaps of some phylogenetic importance are not employed here. Pre- pollices are absent or greatly reduced in size in those genera and species which lack nuptial asperities or swelling of the thumb. In some genera (e.g., Telmato- hius), the prepollex is greatly enlarged (Fig. 46), whereas in others with simi- lar nuptial excrescences (e.g., Physalae- mus), the inner metacarpal is modified for support. In those genera with large, isolated nuptial spines ( e.g., Heleioporus and Leptodactylus) , the inner spine is prepollical and the outer metacarpal (Fig. 46). Figure 46. Skeletons of first finger (thumb) and prepollices of male leptodactylids. (A) Lepto- dactylus pentadactyhis (KU 84981, X 1.2), (B) L. melanonotiis (KU 68275, X 4.8), (G) Telma- tohitis hatitholi (KU 72879, X 3.6), (D) Paratel- matohius hitzi (KU 107089, x 15), and (E) Physalaemus signifems (KU 93033, X 7). SYSTEMATIC ACCOUNTS In the following accounts those char- acters which are only diagnostic at the subfamily level are listed in the subfam- ily accounts but not in the generic ac- counts. I consider it desirable to use the same sequence of character statements in all of the generic accounts, and have numbered all character or character com- plexes consecutively throughout the fol- lowing accounts. In some cases, where the state of a character is not known for a genus, the number is retained in the diagnosis, but no statement follows it. The following characters and character complexes were used to diagnose the subfamilies, tribes, and genera recog- nized herein: 1) sternum cartilaginous, or bearing an osseous plate or style; 2) a dermostosed vertebral shield is present or absent; 3) the transverse processes of 68 MISCELLANEOUS PUBLICATION' MUSEUM OF NATURAL HISTORY the anterior presacral vertebrae are ex- panded or not; 4) the arrangement of the cervical cotyles; 5) cervical and sec- ond vertebrae free or fused; 6) cranial bones involved in dermostosis or not; 7) omosternum present or absent, large or small; 8) degree of dilation of sacral diapophyses; 9) maxillary arch toothed or not, teeth pointed or blunt, pedicel- late or not; 10) direction of and width at the base of the alary processes of the premaxillae; 11) shape of the palatal shelf of the premaxilla; 12) size of facial lobe of maxilla; 13) shape of the palatal shelf of the maxilla, development of pterygoid process of maxilla; 14) maxil- lary arch complete or not, if not, quad- ratojugal present or absent; 15) size of nasals and degree of median contact be- tween nasals; 16) contact of nasals and maxillae, nasals and pterygoids; 17) con- tact of nasals and frontoparietals; 18) frontoparietal fontanelle — present or ab- sent; 19) ornamentation of frontopari- etals; 20) fusion of frontoparietal and prootic; 21) temporal arcade present or not; if present, temporal fenestra present or not and temporal notch present or not; 22) development of epiotic emi- nences; 2.3) shape of cristae paroticae; 24) size of zygomatic ramus of squa- mosal; 25) size of otic ramus of squamo- sal, development of otic plate; 26) size of squamosal-maxillary angle; 27) colu- mella present or absent; 28) prevomers toothed or not, in median contact or not, and position of dentigerous processes relative to choanae; 29) median and lateral extent of palatines, development of odontoids; 30) sphenethmoid divided or entire, shape and extent anteriorly; 31) shape of anterior ramus of para- sphenoid, keeled medially or not; 32) degree of overlap of alae of parasphe- noid and median rami of pterygoids, and posterior deflection of parasphenoid alae; 33) relative bulk of pterygoid, length of anterior ramus and median ramus; 34) size, shape, and arrangement of occipital condyles; 35) development of mandibular odontoids; 36) shape of terminal phalanges; 37) size and shape of alary processes of hyoid plate; 38) cri- coid cartilage divided venti-ally or not; 39) patterns of insertion of m. petro- liyokleiis anterior and r?j. sternolujoideiis on hyoid plate; 40) single or double slip of m. depressor mandibulae; 41) pupil shape — horizontal or vertical; 42) nup- tial asperities on thumb and /or chest or not; type of vocal sac; 43) development of major body glands — parotoid, flank, lumbar, and inguinal; 44) tongue shape; 45) webbing of toes, shape of digital tips, development of tarsal folds, and presence of an outer metatarsal tubercle; 46) larval morphology — vent median or dextral, tooth rows, and development of labial papillae; 47) amplectic position; 48) egg deposition — foam nest, in water, or terrestrial situation; 49) snout- vent lengths of adults — abbreviated SVL; 50) tympanum visible, concealed, or absent; 51) any unique characters that are es- pecially diagnostic of the genus. Characters 1), 2), and 3) do not oc- cur in any generic account and charac- ters 5), 6), 14), 21), and 39) occur in only some generic accounts. Character 51) is used only when appropriate. GENERA EXCLUDED FROM THE LEPTODACTYLIDAE As a result of my reassessment of the variation of many characters used in the classification of the Leptodactylidae, tliree genera were found to belong to other families. Geobatraclius is removed from the Leptodactylidae primarily on the basis of discussions with Charles F. Walker concerning the systematic posi- tion of the genus; Hylopsis, long an enig- matic Neotropical frog genus, is a hylid and probably inseparable from Hijh; and Wiinoderma is excluded from the Leptodactylidae because it exhibits no close similarity to any of the 57 lepto- dactylid genera, but does exhibit some similarity to the endemic South Ameri- can bufonid genera. LYNCH: LEPTODACTYLOID FROGS 69 Geobatrachus Ruthven, 1915 Ruthven (1915) named Geobatrachus walkeri as a new genus and species of the Dendrobatidae. The species remains rare and is apparently endemic to the Santa Marta Mountains of Colombia. Noble (1931) considered Geobatrachus most closely allied to Rhinoderma and SminthiUiis. Griffiths (1959) demon- strated that the species of SminthiUus are leptodactylids. He placed Geoba- trachus and Rhinoderma in the Rhino- dermatinae, a subfamily of the Lepto- dactylidae; the two genera were asso- ciated together because of their common pseudofirmisterny and edentulousness. Dr. Charles F. Walker is currently engaged in a study of the relationships of Geobatrachus and does not consider it to be a leptodactylid genus. Teeth are present, the pectoral girdle is firmister- nal, the sacral diapophyses rounded, the tarsal bones fused, and the anterior zonal elements of the pectoral girdle are greatly reduced or possibly absent. Geo- batrachus is apparently a microhylid genus. Hylopsis Werner, 1894 Werner (1894) named Hylopsis phtycephalus as a new genus and spe- cies of the Cystignathidae. The type- locality is "South America." Werner's meager description of the holotype does not provide many clues as to its relation- ships but the following data are of sig- nificance in determining the status of Hylopsis platyceplmlus: pectoral girdle arciferal (inferred from the family as- signment; Werner must have examined the pectoral girdle because he com- ments on the omosternum ) , omosternum cartilaginous (therefore present), pupil horizontal, large digital pads on hands and feet, fingers one-half webbed, and toes fully webbed. The webbing pattern described by Werner is unique if Hylopsis is a lepto- dactylid; no leptodactylid now known has webbing between the fingers, and very few species have fully webbed feet. The webbing pattern is not unique in the Centrolenidae, Hylidae, or Pseudi- dae. Pseudids do not have digital pads whereas most centrolenids and hylids do. Centrolene, Centrolenelh, Hyla (part), Osteocephalus, PJirynohyas, Smilisca, and Sphaenorhynchus have webbing pat- terns that are like that described for Hylopsis. All have horizontal pupils, but Centrolene and Centrolenella lack an omosternum. Werner reported the pre- vomerine teeth to be absent but did not give the size or sex of the unique holo- type. If prevomerine tooth patches were absent and the specimen was half grown or an adult, then it is unlikely that Hy- lopsis could be associated with Osteo- cephalus, Phrynohyas, or Smilisca. Wer- ner's description of the holotype suggests that the frog had a very different snout shape from that of Sphaenorhynchus. Hylopsis cannot be distinguished from Hyla, although this could be an artifact of Werner's description. If the genus is a bufonoid genus, then it must be close to or identical with Hyla (assuming Werner correctly presented the charac- ters of the holotype). Rhinoderma Dumeril and Bibron, 1841 Rhinoderma was often placed in its own family or subfamily by pre-Noble systematists. Mivart (1869) and Bou- lenger (1882) placed it in the Engys- tomatidae. Noble ( 1931 ) argued that it was a brachycephalid — a heterogeneous Neotropical family group of derived bu- fonids. Davis (1935) and Griffiths (1954) argued that if the three brachy- cephalid subfamilies recognized by Noble were independently evolved from bufonids, then the Atelopodinae, Den- drobatinae, and Rhinodermatinae were families of frogs, not subfamilies. Griffiths (1959) studied the Brachy- cephaHdae and placed the included gen- era in four famihes: Atelopodidae (Ate- lopus and Brachycephalus), Bufonidae (Cacophryne, Demlrophryniscus, Didy- namipus, and Oreophrynellu), Leptodac- 70 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY tylidae (Geohatrachus, Nohlellu, Rhino- derma, and Sminthilhis), and Ranidae (Dendrohates, PhijUohates, and Prosther- apis). The three ranid genera were placed in the subfamily Dendrobatinae. The leptodactylid genera were placed in the Rhinodermatinae (Geohatrachus and Rhinoderma) and Sminthillus divided into three genera — Euparkerella, No- blella, and Sminthilhis, which were all considered very closely related to Eleti- therodactyhis. The breeding behavior of Rhinoder- ma darwini is unique among amphib- ians. Amplexus is axillary. Like many other frogs, the eggs are large (3-6 mm. in diameter), few in number (20-40), and pigmented. The eggs are laid in a sheltered terrestrial situation and are guarded by the male. After hatching, the larvae complete their development in the hypertrophied vocal sacs of the Figure 47. Dorsal and lateral views of the skull of Rhinoderma danoini ( KU 68685, X 5.5). The anterior outline of the head is indicated by the dashed lines. male. The mouthparts are modified; the tooth rows are 1/2 and a beak is present; the labial papillae are interrupted an- teriorly, and the vent is median. The skull of Rhinoderma is not heavily ossified (Fig. 47) except pos- teriorly. The occipital condyles are broad and close together and the cer- vical cotylar arrangement is type II. Teeth are lacking, the palatines and pre- \'omers are lacking, the maxillary arch is incomplete, but the quadratojugal is present. The columella is present, the squamosal-maxillary angle is about 55°, and no otic plate is developed on the squamosal. The m. depressor mandilm- lae consists of the pars tympanicus only. There are eight presacral vertebrae, all procoelus, and the cervical and sec- ond vertebrae are fused. The sacral dia- pophyses are broadly dilated, and the sacrum articulates with the coccyx by a bicondylar articulation. The pectoral girdle is pseudofirmisternal with free epicoracoidal horns and an omosternum and sternum are present and cartilagi- nous. The organ of Bidder is lacking. The terminal phalanges are knobbed. Rhinoderma lacks outer metatarsal tu- bercles. Rhinoderma is clearly not related to the Dendrobatidae, as claimed by Cei ( 1962a ) , nor is it closely related to any other Neotropical gioup. It differs least from the endemic South American Bu- fonidae (several genera referred to the Atelopodidae or Bufonidae by various authors), but is clearly not a bufonid, because it lacks an otic plate on the squamosal, organ of Bidder, outer meta- tarsal tubercle, and has a well developed omosternum. The family Leptodactyli- dae is sufficiently loosely defined that the inclusion of Rhinoderma would not appreciably expand the family definition. If Rhinoderma is included in the Lepto- dactylidae, I would recognize it as the sole member of a subfamily. However, I anticipate that when a more thorough study of the Neotropical bufonids is made, the differences between Rhino- LYNCH: LEPTODACTYLOID FROGS 71 derma and the Bufonidae will be in part demonstrated to be corollaries of the reduction in ossification in Rhinoderma. I prefer to recognize the Rhinodermati- dae for this enigmatic Chilean genus and define the family as follows: bufonoid frogs with a pseudofirmisternal pectoral girdle, cartilaginous pre-zonal and post- zonal elements, lacking an organ of Bid- der, palatines, prevomers, teeth, an otic plate on the squamosal, having broadly dilated sacral diapophyses, and a unique life history among frogs — tadpoles de- velop in the male vocal sacs. KEYS TO THE GENERA OF LEPTODACTYLID FROGS The purpose of a key should ulti- mately be for rapid and accurate iden- tification of a specimen, regardless of what information accompanies it. Keys are especially useful in the identification by non-herpetologists of a specimen with no hint of its provenance. It is very dif- ficult to prepare an effective key to a group of organisms when one places as a primary limitation that the characters used in that key will be characters that are readily accessible and/or superficial. In the family Leptodactylidae, as in most other groups, the members on different continents have undergone parallel mod- ifications in adapting to their environ- ment or to a particular mode of life. Therefore it is almost impossible to write a key, based on external (or super- ficially available internal) characters, to the Leptodactylidae on a world-wide level. Thus the following keys are 1) a key to the African and Australian genera and 2) a key to the African and Ameri- can genera. Heleophrijne, the sole Afri- can genus, has been included in both keys in an attempt to make the keys more cosmopolitan. As superficial characters I include several characters readily visible once the skin in the tympanic region has been reflected; the presence or absence of a tympanic membrane can be observed as can the nature of the musculus depressor mamlibulae. Most of the other charac- ters used are those that traditionally have been used in keys. Key to African and Australo- Papuan Leptodactylids Two subfamilies of leptodactylids oc- cur in Australia and are not readily sep- arated by any "key" external character. Osteologically, they separate readily, but since my intent in preparing the keys was for utility in identifying preserved specimens, I have avoided using all but easily accessible osteological characters. All cycloranines possess prevomerine dentigerous processes and these proc- esses are absent in all myobatrachines except for some of the species of Crinia. Outer metatarsal tubercles are absent in almost all cycloranines and present in all myobatrachines except some Crinia and Taudactyhis. With the exception of the microcephalic Mijohatrachus, all myobati-achines are very much smaller than any of the cycloranine leptodacty- lids. Alosolute size however is a very poor key character. 1. M. depressor mandihidae in a single slip (par tympanicus) 2 M. depressor mandihulae in two slips 4 2. Tympanic annulus absent Pseudophryne Tympanic annulus present 3 3. Large parotoid glands present Philoria Parotoid glands absent Crinia 4. Prevomerine teeth absent 5 Prevomerine teeth present 9 5. Outer metatarsal tubercle present .— 6 Outer metatarsal tubercle absent _.- Taiidactylus 6. Anal flap present; parotoid and flank glands present; pupil vertical in life Uperoleia 72 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Anal flap absent; parotoid glands absent or poorly defined; flank glands absent; pupil horizontal 7 7. Toes webbed Glauertia Toes devoid of webbing 8 8. Head minute compared to body Myobatrachus Head of normal proportions Metacrinia 9. Maxillary teeth absent Notaden Maxillary teeth present 10 10. Prevomerine dentigerous processes between choanae 11 Prevomerine dentigerous processes posterior to choanae 14 11. First finger opposable to others Cyclorana First fiinger not opposable to others 12 12. Outer metatarsal separated by web Mixophyes Outer metatarsals united 13 13. Males with diffuse nuptial pads; toes one-third to fully webbed Neohatrachus Males with or without nuptial spines, no nuptial pads; toes one-fourth or less webbed Heleioporus 14. Toes more than two-thirds webbed Heleophryne Toes less than one-third webbed - 15 15. Tympanum clearly visible externally Lechriodus Tympanum partially or completely concealed 16 16. Prominent odontoids on lower jaw; diastema in tooth row on maxilla Aclelotus No odontoids on mandible or dia- stema in maxillary tooth row 17 17. Fingers short, first shorter than second Kyarranus Fingers longer, first as long as or longer than second __ Limnodynasies Key to African and Neotropical Leptodactylids"^ The following key is much less defin- itive than the former because several leptodactylid genera cannot be separated solely upon the basis of external char- acters. For example, the genera Eupso- phus and Niceforonia cannot be sepa- rated on external characters but are readily separated once the nature of the occipital condylar-cervical articulation is known. I consider these two genera to belong to different tribes of the Telma- tobiinae. In the later couplets in the key I have resorted to more and more osteo- logical features — for the most part these are discernible with the aid of a thin probing needle and the figures of the skulls for reference. The genera Paratelmatohitis and Pseud opahidicola will key out in two sections of the key since the nature of the sternal style in Pseudopaludicolu is difficult to assess from the examination of preserved material and because the osseous plate in Paratelmatohius is not a style. As will be apparent, the genera Eiip- soplnis and Niceforonia key out together three times in the following key (coup- lets 32, 34, and 42) and are never sepa- rated. Separation of these two genera on external characters is effectively impos- sible unless one has a breeding male ( Eiipsophus has nuptial asperities on the •''' Insuetophnjnus can be readily separated from all Neotropical leptodactylids as Barrio ( 1970) pointed out on the basis of the pectoral archi- tecture. Presumably, the quadratojugal bone is present, and Insuetophnjnus would key out at couplet 32 as "Eupsophus (part) and Nicefo- ronia (part)." Inspection of the pectoral girdle will provide evidence for separating Insueto- l)hnjnus, because the former two genera have arciferal girdles in contrast to the pseudofirmi- sternal girdle of Insuetophnjnus. LYNCH: LEPTODACTYLOID FROGS 73 thumb whereas Niceforonia does not). Eleutlwrodactylus and Syrrliophiis key out together (couplet 22). Most species may be separated by the presence of numerous supernumerary plantar tuber- cles in Sijrrhophus and the absence of such tubercles in Eleutlwrodactylus. Some species of the Beta division of Eleutlwrodactylus have as many super- numerary tubercles as do Syrrhophus or more. 1. Cranial bones involved in dermo- stosis 2 Cranial bones not involved in der- mostosis 4 2. Toes fully webbed Caudiverhera Toes less than two-thirds webbed _. 3 3. Pupil horizontal; outer metatarsal tubercle absent Ceratophrys Pupil vertical; outer metatarsal tubercle present Lepidohatraclnis 4. Pupil vertical 5 Pupil horizontal 9 5. Sternum a broad cartilaginous (sometimes calcified) plate 6 Sternum bearing a distinct bony or calcified style 8 6. Toes fully webbed 7 Toes free of webbing Hylorina 7. Parotoid gland present; digital tips simple Telmatohufo Parotoid gland absent; digital tips pad-like Heleophryne 8. Toes fully webbed Hydrolaetare Toes free or basally webbed Limnomedusa 9. Sternum with a distinct bony or cal- cified style 10 Sternum a cartilaginous, calcified, or osseous plate 17 10. Quadratojugal bone absent 11 Quadratojugal bone present 12 11. Antebrachial tubercles present Pseudopaludicola Antebrachial tubercles absent Pleurodema 12. Prevomerine teeth absent Physalaemus Prevomerine teeth present, on well defined processes 13 13. Eyelid bearing fleshy tubercles Edalorhina Eyelid without fleshy tubercles — _ 14 14. Sternal element style shaped 15 Sternal element irregular in outline, plate-like Paratelmatobius 15. Sternal style bifurcate posteriorly ._ Barycholos Sternal style not bifurcate posteriorly 16 16. Terminal phalanges distinctly T- shaped; digital discs with circum- ferential groove Lithodytes Terminal phalanges knobbed or weakly T-shaped; no circumferential groove on digital discs Leptodactylus 17. Dorsal surface of each digital pad bearing a pair of scute-like glands 18 Dorsal surface of digital pad or tip without distinct glands 20 18. Quadratojugal absent or present only as a sliver-like bone; small frogs, adults less than 40 mm. SVL 19 Quadratojugal massive; adults 50 to 110 mm. SVL Megaelosia 19. Males with median subgular vocal sac; nuptial spines present; pre- vomerine teeth usually absent; quad- ratojugal bone absent Crossodactylus 74 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Males with paired lateral vocal sacs or none; nuptial spines absent; pre- vomerine teeth usually present; quadratojugal present Hylodes 20. Tips of at least outer digits bearing transverse, terminal groove along edge of digital pad 21 Tips of digits without terminal grooves 23 21. Maxillary arch toothless Smintliilhis Maxillary arch toothed 22 22. Lumbar gland present Tomodactijlus Lumbar gland absent __ Eleutlierodactylus and Syrrhophus 23. Terminal phalanges T-shaped or Y- shaped 24 Terminal phalanges knobbed 26 24. Digital pads large, tympanum absent Crossodactylodes Digital pads relatively narrow; tym- panum visible externally 25 25. Quadratojugal bone present Thoropa Quadratojugal bone absent Batrachyla 26. Quadratojugal bone absent Pseudopaludicola Quadratojugal bone present 27 27. Sternum an osseous plate Paratelmatohius Sternum cartilaginous 28 28. Supernumerary plantar tubercles large, numerous 29 Supernumerary plantar tubercles absent or small 30 29. Discoidal fold present Hyhctophryne Discoidal fold absent - Ischnocnenia 30. Tympanic annulus absent 31 ' Tympanic annulus visible externally or concealed beneath skin 33 31. Fingers short, especially fourth finger Euparkerella Fingers of normal proportions to long 32 32. Toes fully webbed Batrachophrynus Toes free to two-thirds webbed Eupsophus ( part ) and Niceforonia (part) 33. Tympanum visible externally 34 Tympanum concealed beneath skin 35 34. Large frontoparietal crests present ^ Amhlyphrynus No cranial crest Eupsophus (part) and Niceforonia (part) 35. Inner metatarsal tubercle spade-like elevated 36 Inner metatarsal tubercle not ele- vated or spade-like 37 36. Large cranial crests present; parotid glands absent Proceratophrys (part) Frontoparietal region flat or edge of frontoparietals slightly ridge-like; parotoid glands present or absent - Odontophrynus 37. Cranial crests present Proceratophrys (part) Cranial crests absent 38 38. Metatarsal tubercles flat, sub-equal in size Holoaden Inner metatarsal tubercle at least twice as large as outer 39 39. Outer metatarsal tubercle minute, less than one-fourth size of inner; toes webbed Tehnatobius LYNCH: LEPTODACTYLOID FROGS 75 Outer metatarsal tubercle larger, about one-third to one-half size of inner; toes free or webbed; if webb- ed, outer tubercle one-half size of inner 40 40. Skin or dorsum uniformly pustular, toes free or webbed; large inguinal gland present Cijcloramphus Skin or dorsum smooth or with scat- tered pustides; toes free of webbing; inguinal gland absent 41 41. Inner lingers and toes very short .„^ Scijthrophnjs Fingers and toes of normal length 42 42. Tongue free all around, anterior edge only slightly free; if appearing adherent anteriorly, axillary patag- ium present Zachaenus Tongue firmly adherent anteriorly; axillary patagium absent Etipsophus (part) and Niceforonia (part) Leptodactylidae Berg, 1896 (1838) Cystignathi Tschudi, 1838, Classification der Batrachier, p. 25, 37, 78. [Type-genus Cys- tignathus Wagler, 1830]. Leptodactylidae Berg, 1896, An. Mus. Buenos Aires, 5:161. [Type-genus Leptodactyhis Fitzinger, 1826]. The subfamilial, tribal, and generic accounts follow. In the generic accounts, I have provided generic synonymies in- cluding all synonyms and permutations thereof and the manner of designation of the type-species; the diagnostic defini- tion listing the states for the 50 charac- ters scored for each genus; a statement of composition, and where appropriate, the most recent revisionary works on the group; a statement of distribution; and a section of remarks. In the remarks section, I have justified any new generic synonymies or partitionings. Brief re- marks on the relationships of the genera are made in the remarks section. Drawings of the skulls of all genera of leptodactylids are included with the exception of those genera known from so few specimens that the only available data are taken from stereo-radiographs. In genera having sufficient intrageneric variation (for example, Cyclorana and Eletitherodactyhis) , drawings of more than one species are included. Cycloraninae Parker, 1940 Cycloraninae Parker, 1940:12. In his monogiaph of the Australo- Papuan leptodactylids, Parker (1940) amply demonstrated the desirability of recognizing two subfamiHes. My studies have further substantiated Parker's divi- sion of Noble's ( 1931 ) Criniinae into two subfamilies. Parker (1940) suggested that with additional study, it might be possible to demonstrate that there was a close relationship between some of the Cycloraninae and some Myobatrachinae. My studies have enhanced the differ- ences, not mitigated them, and I con- sider that the two subfamilies possibly represent independently derived groups. The following diagnostic statements are true for all members of the subfam- ily Cycloraninae: 1) sternum cartilagi- nous; 2) vertebral shield absent; 3) transverse processes of anterior presacral vertebrae not greatly expanded; 4) cer- vical cotylar arrangement type II; 6) cranial bones not dermostosed; 8) sacral diapophyses dilated; 14) maxillary arch complete; 20) frontoparietals not fused to prootics; 21 ) temporal arcade lacking; 27) columellae present; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate on narrow stalks; 38) cricoid cartilage not divided ventrally; 39) m. petrohyoideus anterior and m. sternohyoideus insert on the lateral edges of hyoid plate; and 47) amplexus in- guinal in known species. All species have dilated sacral diapophyses; Parker's ( 1940 ) statement to the contrary for Mixophyes is in error because his obser- vation was made on a juvenile. 76 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY The primitive members of the sub- family exhibit some or all of the follow- ing characteristics: omosternum rela- tively large; cervical and second verte- brae fused; intervertebral discs free; transverse processes of posterior pre- sacral vertebrae short and directed an- teriorly; frontoparietal fontanelle lack- ing; carotid artery enclosed in a bony canal; outer metatarsal tubercle lacking; pupil vertical; eggs not deposited in a foam nest; aquatic tadpoles present; tadpole with median vent and 3/3 to 4/3 tooth rows. Two tiibes of the Cycloraninae are recognized herein. In the Cycloranini, the eggs are deposited in water without a foam nest, on land in moist situations, or in dry burrows with a foam nest. All species have aquatic tadpoles. Females lack spatulate fringes on the inner fin- gers (Fig. 48). The prevomerine den- tigerous processes lie between, not pos- terior to, the choanae in all Cycloranini. In the Limnodynastini, the eggs are de- posited in a foam nest floating on water or in a foam nest in moist terrestrial situations. All species except Kyarranus and Philoria have aquatic, feeding tad- poles. Development is direct in the montane Kyarranus and Thihria. Fe- males of all Limnodynastini have spatu- late fringes on the fingers (Fig. 48), which are used in the construction of the foam nest (Parker, 1940, Martin, Figure 48. Palmar views of hands of adult females of ( A ) Cijdorana australis ( KU 93545) and (B) Limnodyiiastcs ))cionii (KU 93562). Both X 3.7. 1968). The prevomerine dentigerous processes are situated posterior to the choanae in all Limnodynastini. Cycloranini Parker, 1940 Five genera are included in this tribe: Cyclorana, Heleioporiis, Mixo- phyes, Neobatradnis, and Notaden. He- leioporiis lays its eggs in dry burrows in a foam nest (Lee, 1966, Martin, 1968), but the other genera lay their eggs in water or in moist terrestrial sites (Mar- tin, 1968). Cyclorana Steindachner, 1867 (Figs. 49-50) ChiioJcptes Giinther, 1859, Cat. Bat. Sal. British Mus., p. 34 [Type-species by monotypy, Chiwleptes australis (Gray), 1842; pre- occupied by Chiwleptes Kirby, 1837 ( In- secta : Hemiptera ) ] . Cyclorana Steindachner, 1867, Reise Novara, Amph., p. 29 [Type-species by monotypy, Ci/clorana tiovaehoUatidiae Steindachner, 1867]. Phractops Peters, 1867, Mtber. k. Preuss. Akad. Wiss., Berlin, 1867:30 [Type-species by monotypy, Phractops ahitaceus Peters, 1867.]. Mitrohjsis Cope, 1889, Bull. U.S. Natl. Mus., 34:312 [Type-species by monotypy, Chiro- leptes alhoguttatus Giinther, 1867]. Cheiroleptes Spencer, 1901, Proc. Roy. Soc. Victoria (2) 13:176 [Replacement name for Chiroleptes Giinther, 1859 (preoccupied); hence taking the same type-species]. Diagnostic definition. — 5 ) cervical and second vertebrae free; 7) omoster- num present, moderate in size; 9) maxil- lary arch toothed, teeth blunt, pedicel- late; 10) alary processes of premaxillae directed posterodorsally, relatively wide at base; 11) palatal shelf of premaxilla broad, deeply incised; 12) facial lobe of maxilla deep, weakly exostosed in alho- guttatus and more so in australis; 13) palatal shelf of maxilla moderate in width, expanded posteriorly into a ptery- goid process; 15) nasals separated me- dially, relatively small, exostosed in australis; 16) nasals in broad contact with maxillae, not in contact with ptery- goids; 17) nasals separated from fronto- parietals; 18) frontoparietal fontanelle LYNCH: LEPTODACTYLOID FROGS 77 Figure 49. Dorsal and ventral views of the skull of Cyclorana australis (KU 93550, X 2.5). lacking; 19) lateral edges of frontopari- etals exostosed in australis, not orna- mented in other species; 22) epiotic eminences prominent; 23) cristae paroti- cae long and relatively broad; carotid artery not enclosed in a bony canal; 24) zygomatic ramus of squamosal in broad articular contact with maxilla in australis and extensively sculptured; in tenuous contact with maxilla in albo- guttatus and not ornamented; elongate but widely separated from maxilla in other species; 25) otic ramus of squa- mosal long, developed into small otic plate; in australis, otic plate is propor- tionately larger than that in other spe- cies and otic ramus is large and sculp- tured; 26) squamosal-maxillary angle 26-35°; 28) prevomers large, entire, toothed, narrowly separately medially; 29) palatines large, deep, bearing odon- toid ridge in australis; 30) sphenethmoid entire, extending anterior beneath na- sals; 31 ) anterior ramus of parasphenoid narrow, not keeled medially; 32) para- sphenoid alae oriented at right angles to anterior ramus, broadly overlapped by median rami of pterygoids; 33) ptery- goids moderate in size, no ventral flange, anterior rami in long contact with max- illae, not reaching palatines; 34) occipi- tal condyles moderate sized, not stalked, narrowly separated medially; 35) man- dible lacking odontoids; 40) m. depres- sor mandibulae in two slips; 41) pupil horizontal; 42) males with median sub- gular vocal sac, nuptial asperities on thumb; 43) body lacking glands; 44) Figure 50. (Top) dorsal, (middle) lateral views of the skull of Cyclorana dahli (UMMZ 65250 ) ; and ( bottom ) lateral view of skull of C. australis ( KU 93550). All X 2.5. 78 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY tongue large, free posteriorly; 45) toes webbed at base to fully webbed; outer metatarsal tubercle absent except in in- ennis; digital tips narrow; first finger longer than second; 46) larvae with me- dian or dextral vent, 2/3 tooth rows, labial papillae interrupted anteriorly; 47) amplexus inguinal; 48) eggs laid in gelatinous masses in temporary ponds; 49) males 35-90, females 35-100 mm. SVL; 50) tympanum visible externally; 51) thumb opposable. Composition. — Parker (1940) recog- nized seven species (allwguttatus, aus- tralis, hrevipes, cultripes, dahU, inermis, and pJattjcepljahis). One other species (slevini) has been described since. Distribution. — Austialia except on the western coast and interior. The genus does not occur on New Guinea or Tas- mania. Remarks. — The generic synonymy of Cyclorana has been stable since 1940. The status of the nominal species of the genus is seriously in need of review. Cy- clorana is a generalized genus of Cyclo- raninae. Osteologically, it is least dif- ferent from Lechriochis and Mixophyes, but it has no close relationship with either of these genera. The variation in the skulls of this genus is striking. Cyclorana albogtittata is intermediate between the heavily exostosed australis and the other species of the genus. The only other leptodac- tylid genus with comparable variation in the skull bones is Eleutherodactylus. Heleioporus Gray, 1841 (Figs. 51-52) Heleioporus Gray, 1841, Ann. Mag. Nat. Hist., (1)7:91 [Type-species by monotypy, Helei- oporus alhopunctatus Gray, 1841]. Helioporus Gray, in Grey, 1841, J. Exped. Cent. Australia, 2:447 [Emendation of Heleio- porus Gray, 1841]. Perialia Gray, in Eyre, 1845, J. Exped. Cent. Australia, 1:406 [Type-species by monotypy, Perialia eijeri Gray, 1845]. Philocrijphus Fletcher, 1894, Proc. Linn. Soc. New South Wales, (2)8:233 [Type-species by monotypy, Philocrtjphus flavoguttattis Fletcher, 1894]. Diagnostic definition. — 5) cervical and second vertebrae fused; 7) omo- sternum present, small; 9) maxillary arch toothed, teeth blunt, pedicellate; 10) alary processes of premaxillae di- rected posterodorsally, broad at base; 11) palatal shelf of premaxilla relatively narrow, moderately long palatal process; 12) facial lobe of maxilla of moderate depth, not exostosed; 13) palatal shelf of maxilla relatively narrow, pterygoid process present; 15) nasals small, short, very wide, separated medially; 16) na- sals in broad contact with maxillae, sep- arated from pterygoids; 17) nasals not in contact with frontoparietals; 18) fron- toparietal fontanelle moderate in size; 19) frontoparietals not ornamented; 22) epiotic eminences prominent posteriorly; 23) cristae paroticae long and narrow; carotid artery enclosed in a bony canal, roofed over; 24) zygomatic ramus of Figure 5 1 . Dorsal and ventral views of the skull oi Heleioporus eyeri (UMMZ 124504, X 6). LYNCH: LEPTODACTYLOID FROGS 79 Figure 52. Lateral view of skull of Heleioponis eyed (UMMZ 124504, x 6). squamosal short, slightly longer than otic ramus; 25) otic ramus of squamosal de- veloped into small otic plate; 26) squa- mosal-maxillary angle about 50°; 28) prevomers large, entire, toothed, nar- rowly separated medially; 29) palatines large, narrowly separated medially; 30) sphenethmoid entire, extending anterior- ly beneath posterior half of nasals; 31) anterior ramus of parasphenoid narrow, not keeled; 32) parasphenoid alae ori- ented at right angles to anterior ramus, broadly overlapped by median rami of pterygoids; 33) pterygoids relatively slender, anterior rami in long contact with maxillae, reaching palatines; 34) occipital condyles large, not stalked, nar- rowly separated medially; 35) mandible lacking odontoids; 40) m. depressor mandihulae in two slips; 41) pupil ver- tical; 42) males with large nuptial spines on thumb or not, never pad-like asperi- ties; males with median, subgular vocal sac; 43) extensive parotoid glands pres- ent, small inguinal glands present; 44) tongue large, notched and free pos- teriorly; 45) feet basally webbed, outer metatarsal tubercle absent, inner meta- tarsal tubercle spade-like, tips of digits narrow, first finger longer than second; 46) larvae with median or dextral vent, 2/3 to 5/4 tooth rows, labial papillae broadly interrupted anteriorly; 47) am- plexus inguinal; 48) eggs laid in foam nest in dry burrow, tadpoles emerge when nest is flooded; 49) males 38-95, females 41-95 mm. SVL; smallest species is psammopliilus, largest is australiacus; 50) tympanum visible externally. Composition. — Lee (1966) recog- nized six species (albopunctatus, aus- traliacus, barycragus, eijeri, inornatus, and psammophilus). Distribution. — Southeastern and southwestern Australia. Rejnarks. —Farker (1940) did not differentiate the genera Heleioporus and Neobatrachus. Main, Lee, and Little- john (1958) considered the ethological and morphological differences between the groups ample for generic distinction. Moore (1961) and Lee (1966) con- curred in this opinion; I consider the differences in the sizes of the transverse processes of the presacral vertebrae addi- tional support for the continued separa- tion of these genera. The two genera are unquestionably related but are not so similar that their combination would re- sult in a clarification of relationships. Neobatraclnis is more closely allied to a third related genus, Notaden. Mixophyes Giinther, 1864 (Figs. 53-54) Mixophyes Giinther, 1864, Proc. Zool. Soc. Lon- don, p. 46 [Type-species by monotypy, Mixophtjes fasciolatus Giinther, 1864]. Diagnostic definition. — 5) cervical and second vertebrae free; 7) omoster- num present, relatively large; 9) maxil- lary arch toothed, teeth blunt, pedicel- late; 10) alary processes of premaxillae directed posterodorsally, broad at base; 11) palatal shelf of premaxilla narrow, palatal process elongate; 12) facial lobe of maxilla deep with a slight squamosal processes, not exostosed; 13) palatal shelf of maxilla very narrow, no ptery- goid process; 15) nasals large, in median contact anteriorly, separated posteriorly, exposing sphenethmoid; 16) nasals in contact with maxillae, not in contact with pterygoids; 17) nasals in tenuous contact with frontoparietals; 18) fron- toparietal fontanelle absent; 19) fronto- parietals not ornamented; 22) epiotic eminences prominent; 23) cristae paroti- cae long and narrow; carotid artery en- closed in a complete bony canal; 24) 80 MISCELLAxXEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 53. Dorsal and ventral views of skull of Mixophyes fasciolatiis ( KU 56627, X 3.5). zygomatic ramus of squamosal elongate, tendon contacting squamosal process of maxilla; 25) otic ramus of squamosal long, developed medially into otic plate; 26) squamosal-maxillary angle 45-50°; 28) prevomers small, entire, toothed, separated medially; 29) palatines thin, separated medially, bearing odontoid ridges; 30) sphenethmoid entire, extend- ing anteriorly to anterior edge of nasals; 31 ) anterior ramus of parasphenoid nar- row, not keeled; 32) parasphenoid alae deflected posteriorly, overlapped lateral- ly by median rami of pterygoids; 33) pterygoids large, anterior rami in long contact with maxillae, nearly reaching palatines and nasals; 34) occipital con- dyles moderate sized, not stalked, sep- arated medially; 35) mandible lacking odontoids; 40) m. depressor mandibulae in two slips; 41) pupil vertical; 42) males with median subgular vocal sac, nuptial asperities on thumb; 43) body lacking glands; 44) tongue large, rounded, only posterior edge free; 45) toes two-thirds webbed, outer metatar- sal tubercle absent, inner metatarsal tubercle not spade-like, tips of digits narrow; 46) larvae with dextral vent, 6/3 tooth rows, labial papillae not in- terrupted anteriorly; 47) amplexus in- guinal; 48) eggs laid in terrestrial situa- tions and hatch upon flooding; 49) males and females 50-100 mm. SVL; 50) tym- panum visible externally. Composition. — Only one species is now recognized, but it is apparently a composite of two (Moore, 1961, Little- john, 1968). Distribution. — Mountains and coastal areas of eastern Australia. Remarks. — Mixophyes has been rec- ognized as a distinctive genus since its discovery. This distinction was based in part on misconceptions. Boulenger (1882) reported the sacral diapophyses as rounded; Parker (1940) agreed. Hecht (1960) reported the sacral dia- pophyses were dilated. The specimens I have examined all have dilated sacral diapophyses. Fletcher (1889) stated that Mixophyes exhibits axillary amplex- us. Littlejohn (pers. comm.) informs me that the amplectic pattern is inguinal, as in all other Australo-Papuan leptodac- tylids. Figure 54. Lateral and occipital views of skull of Mixophyes fasciolatiis ( KU 56627, X 5.5). LYNCH: LEPTODACTYLOID FROGS 81 Neobatrachus Peters, 1863 (Figs. 55-56) Neobatrachus Peters, 1863, Mtber. k. Preuss. Akad. Wiss., Berlin, 1863:234 [Type-species by monotypy, Neobatrachus pictus Peters, 1863]. Diagnostic definition. — 5) cervical and second vertebrae fused; 7) omoster- num minute; 9) maxillary arch toothed, teeth blunt, pedicellate; 10) alary proc- esses of premaxillae long, directed pos- terodorsally, relatively wide at base; 11) palatal shelf of premaxilla narrow, pala- tal process long; 12) facial lobe of max- illa deep, not exostosed; 13) palatal shelf of maxilla narrow, no pterygoid process; 15) nasals small, separated medially; 16) nasals in contact with maxillae, not with pterygoids; 17) nasals not in contact with frontoparietals; 18) frontoparietal fontanelle moderate in size; 19) fronto- parietals not ornamented; 22) epiotic eminences prominent; 23) cristae paroti- FiGURE 55. Dorsal and ventral views of skull of Neobatrachus pictus (FMNH 97281, X 3). Figure 56. Lateral views of the skulls of Neo- batrachus pictus (FMNH 97281, top) and Notaden nichollsi ( KU 93582, bottom). Both X3. cae long and narrow; carotid artery lies in a deep groove, exposed dorsally; 24) zygomatic ramus of squamosal minute; 25) otic ramus of squamosal very small, developed medially into a small otic plate; 26) squamosal-maxillary angle 50- 55°; 28) prevomers of moderate size, entire, toothed, narrowly separated me- dially; 29) palatines thin, widely sep- arated medially; 30) sphenethmoid en- tire, extending anteriorly beneath nasals; 31 ) anterior ramus of parasphenoid nar- row, weakly keeled; 32) parasphenoid alae oriented at right angles to anterior ramus, narrowly overlapped laterally by median rami of pterygoids; 33) ptery- goids relatively large, anterior rami in long contact with maxillae, not reaching palatines; 34) occipital condyles rela- tively small, not stalked, narrowly sep- arated medially; 35) mandible lacking odontoids; 40) m. depressor mandibuhe in two slips; 41) pupil vertical; 42) males with median subgular vocal sac; nuptial pad (callosities) on thumb and second finger; 43) body lacking glands; 44) tongue large, round, free behind; 45) toes one-fourth to fully webbed, outer 82 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY metatarsal tubercle absent, inner meta- tarsal tubercle spade-like, tips of digits narrow, first finger longer than second; 46) larvae with dextral vent, 3/3 tooth rows, labial papillae interrupted an- teriorly; 47) amplexus inguinal; 48) eggs deposited in long strings in slow moving streams and temporary ponds; 49) adults not exceeding 50 mm. SVL; 50) tym- panum indistinct externally, concealed beneath skin. Composition. — Five species (centra- lis, pelohatoicJes, picttis, sutor, and tcih- morei) are presently recognized, al- though no one has reviewed the group since Parker (1940). Distrihtition. — Mainland Australia except in northern West Australia and along the northern coast, where Neo- hatrachiis is apparently replaced eco- logically by its close relative, Notaden. Remarks. — Main, Lee, and Littlejohn (1958) argued that the Heleioporus pictus group (Neohatrachiis) should be afi^orded generic status since it differs ethologically from typical Heleioporus. Typical Heleioporus lays the eggs in burrows in a foam nest and when the burrow is flooded, the tadpoles emerge to complete their development like typi- cal frogs. Neohatrachiis lays long egg strings ( like Biifo ) in still or slowly mov- ing water. The two groups also differ in the kind of nuptial excrescence (spines in Heleioporus, roughened pad in Neo- hatrachiis), adult size (Heleioporus are larger frogs), and the shape of the ster- num (bifurcate posteriorly in Heleio- porus). The transverse processes of the posterior presacral vertebrae of the two genera differ in size (Fig. 30), and there is a slight difference in the sizes of the zygomatic and otic rami of the squa- mosals. The separation of these two genera is based more on the so-called adaptive approach to genera than the morpho- logical approach. Without the ethologi- cal data, I doubt if I would have adopted a different approach from that taken by Parker (1940). Notaden Glinther, 1873 ( Figs. 56-57 ) Notaden Giinther, 1873, Ann. Mag. Nat. Hist., (4)11:349 [Type-species by monotypy, Notaden bennetti Giinther, 1873]. Diagnostic definition. — 5) cervical and second vertebrae fused; 7) omoster- num absent; 9) maxillary arch eden- tate; 10) alary processes of premaxillae elongate, directed dorsally, narrow at base; 11) palatal shelf of premaxilla nar- row, palatal process relatively short; 12) facial lobe of maxilla shallow; 13) pala- tal shelf of maxilla absent; 14 ) maxillary arch incomplete, maxilla not contacting quadratojugal or premaxilla, quadrato- jugal present; 15) nasals small and sep- arated medially; 16) nasals not in con- tact with maxillae or pterygoids; 17) na- sals in tenuous contact with frontopari- etals; 18) frontoparietal fontanelle large; 19) frontoparietals not ornamented; 22) epiotic eminences prominent; 23) cristae paroticae short, stocky; carotid artery lies in a shallow groove exposed dorsal- ly; 24-25) zygomatic and otic rami of squamosal lacking; 26) squamosal-maxil- FiGURE 57. Dorsal and ventral views of skull of Notaden nichollsi ( KU 93582, X 3 ) . LYNCH: LEPTODACTYLOID FROGS 83 lary angle about 80°; 28) prevomers moderately large, entire, toothed, sep- arated medially; 29) palatines reduced in size, not contacting maxillae and wide- ly separated medially; 30) sphenethmoid entire, small, not extending anteriorly to nasals; 31) anterior ramus of parasphe- noid broad, short, not keeled; 32) para- sphenoid alae oriented at right angles to anterior ramus, not overlapped laterally by median rami of pterygoids; 33 ) ptery- goids small, anterior rami in long contact with maxillae, usually contacting pala- tines; 34) occipital condyles large, not stalked, narrowly separated medially; 35) mandible lacking odontoids; 40) 7n. depressor 7nandihiilae in two slips; 41) pupil horizontal; 42) males with median subgular vocal sac; nuptial pad on thumb; 43) dorsum covered with at least two ill-defined glands, less discrete but more extensive than in Heleioporus; 44) tongue large, round, not free behind; 45) toes one-half to two-thirds webbed, outer metatarsal tubercle absent, inner metatarsal tubercle spade-like, tips of digits narrow, first finger about as long as second; 46) larvae with median vent, 3/3 tooth rows, labial papillae inter- rupted anteriorly; 47-48); 49) adults to 70 mm. SVL; 50) tympanum concealed. Composition. — Hosmer (1962) rec- ognized three species — hennetti, mela- noscaplnis, and nichollsi. Distribution. — Northwestern, north- central, and southeastern Australia west of the dividing range. Remarks. — Notaden has been recog- nized as distinct since its description chiefly because it lacks maxillary teeth. The loss of teeth reflects a general re- duction in the amount of bone; in Nota- den, the reduction is striking. The loss of the upper portions of the squamosals is unique in the family, as is the free floating maxilla. Because Notaden lives in an arid environment, Parker ( 1940 ) thought it might exhibit direct develop- ment. Slater and Main (1963) found tadpoles in ponds and suggested that de- velopment was rapid, but definitely was not abbreviated. Notaden is closely related to Heleio- porus and Neohatrachus. All have free intervertebral discs, fused cervical and second vertebrae, short transverse proc- esses of the posterior presacral vertebrae, moderate to large frontoparietal fonta- nelles, deep skulls, and large, spade-like inner metatarsal tubercles. Notaden has a horizontal pupil and lacks maxillary teeth, whereas the other two genera have vertical pupils and have maxillary teeth. Notaden and Heleioporus have extensive glandular areas on the dorsum; Neo- hatrachus lacks glands. Neohatrachus and Notaden have nuptial pads, and He- leioporus has large spines on the thumb. The tadpoles of the three genera are similar and cannot be separated generi- cally owing to the intrageneric variability in vent position and tooth rows in He- leioporus. Limnodvnastini New Tribe Limnodynastine leptodactylids build a foam nest in which the eggs are de- posited. The few observations that have been made indicate that the female uses the spatulate fringes on the inner fingers (Fig. 48) to build the nest. Develop- ment is direct in two of these genera (Kyarranus and Philoria). Martin (1968) proposed an evolu- tionary course of terrestrial foam nest development. He cited Australo-Papuan genera where germane, but used Neo- tropical genera for certain stages of de- velopment. The foam nest is deposited in open water by some Limnodijnastes, in water-filled burrows adjacent to open water in other Limnodijnastes, in pud- dles adjacent to open water in Leptodac- tylus pentad actijlns, in dry burrows which will later flood in Heleioporus, and in moist, terrestrial situations in Kyarranus and Philoria. 84 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Adelotus Ogilby, 1907 (Figs. 58-59) Cryptotis Giinther, 1863, Ann. Mag. Nat. Hist., (3)11:27 [Type-species by monotypy, Cryptotis brevis Giinther, 1863; preoccupied by Cryptotis Poniel, 1848 (Mammalia: In- sectivora ) ] . Adelotus Ogilby, 1907, Proc. Roy. Soc. Queens- land, 20:32 [Replacement name for Crypt- otis Giinther, 1863 (preoccupied); hence taking same type-species]. Diagnostic defi n itio n. — 5 ) cervical and second vertebrae fused; 7) omoster- num present, moderate sized; 9) maxil- lary arch toothed, teeth elongate, pedi- cellate; distinct diastema in tooth row; 10) alary processes of premaxillae di- rected posterodorsally, elongate, rela- tively broad at base; 11) palatal shelf of premaxilla narrow with a moderately large palatal process and long process lying along maxilla; 12) facial lobe of maxilla deep; maxilla deep for entire length, not exostosed; 13) palatal shelf of maxilla narrow, pterygoid process well developed; 14) quadratojugal expanded; 15) nasals wide and short, small, sep- FiGURE 58. Lateral and dorsal views of the skull of Adelotus brevis (KU 56242, X 2.5). Figure 59. Ventral view of the skull of Adelo- tus brevis (KU 56242, X 2.5). arated medially; 16) nasals in contact with maxillae, not with pterygoids; 17) nasals widely separated from frontopari- etals; 18) frontoparietal fontanelle lack- ing; 19) frontoparietals not exostosed but bearing large sagittal crest; 22) epi- otic eminences obsolete; 23) cristae paroticae short but relatively broad; carotid artery not enclosed in an open or closed canal; 24) zygomatic ramus of squamosal slender, of moderate length; 25) otic ramus of squamosal short, de- veloped medially into prominent otic plate; 26) squamosal-maxillary angle about 45°; 28) pre vomers toothed, en- tire, separated medially, dentigerous ramus greatly elongated; 29) palatines very broad, lacking odontoid ridge, sep- arated medially; 30) sphenethmoid en- tire, relatively small, rounded anteriorly, not reaching nasals; 31) anterior ramus of parasphenoid broad, not keeled, an- terior edge deeply serrated; 32) para- sphenoid alae deflected posteriorly, short, overlapped laterally by median rami of pterygoids; 33) pterygoids rela- tively large, anterior rami in long con- tact with maxillae, nearly reaching pala- tines; 34) occipital condyles large, close- ly approximated medially; 35) mandible bearing elongate tusk (Fig. 15), longer in male than in female; 40) m. depressor mandihulae in two slips; 41 ) pupil hori- LYNCH: LEPTODACTYLOID FROGS 85 zontal; 42) males with median subgular vocal sac; no nuptial asperities on thumb; 43) body lacking glands; 44) tongue large, posterior edge free; 45) toes with basal webbing, outer meta- tarsal tubercle present, digital tips nar- row, first finger as long as second; 46) larvae \\ith dextral vent, 2/3 tooth rows, labial papillae narrowly interrupted an- teriorly; 47) amplexus inguinal; 48) eggs laid in foam nest in ponds or running water (streams); 49) males to 50 mm., females to 40 mm. SVL; 50) tympanum usually completely concealed. Composition. — A single species, A. brevis. Distribution. — Coastal southeastern Australia. Remarks. — Since its discovery, the tusked frog has been recognized as ge- nerically distinct. The large mandibular tusks are characters sui generis. The species was originally named Cryptotis brevis but the generic name, Cryptotis Giinther, 1863, is a junior homonym of Cryptotis Pomel, 1848, the generic name of some American shrews. Adelotus is not closely related to any other genus of the Limnodynastini, but is least different from Limnodynastes. Lechriodus Boulenger, 1882 (Fig. 60) Batrachopsis Boulenger, 1882, Cat. Batr. Sal. British Mus., p. 439 [Type-species by mono- typy, Asterophrys melanoptjga Doria, 1875; preoccupied by Batrachopsis Fitzinger, 1843 (Amphibia: Caudata)]. Lechriodus Boulenger, 1882, Cat. Batr. Grad. British Mus., p. 116 [Replacement name for Batrachopsis Boulenger, 1882 ( preoccupied ) and hence taking same type-species]. Phanerotis Boulenger, 1890, Proc. Linn. Soc. New South Wales, (2)5:594 [Type-species by monotypy, Phanerotis ftetcheri Boulen- ger, 1890]. Diagnostic definition. — 5) cervical and second vertebrae free; 7) omoster- num present, moderate sized; 9) maxil- lary arch toothed, teeth blunt, pedicel- late; 10) alary processes of premaxillae directed posterodorsally, wide at base; 11) palatal shelf of premaxilla moderate Figure 60. Dorsal and ventral views of skull of Lechriodus fletcheri (AMNH 59488, X 3). in width, deeply incised; 12) facial lobe of maxilla deep, not exostosed; 13) pala- tal shelf of maxilla relatively narrow, small pterygoid process; 15) nasals mod- erate sized, apparently in median con- tact; 16) nasals in contact with maxil- lae, not with pterygoids; 17) nasals not in contact with frontoparietals; 18) fron- toparietal fontanelle lacking; 19) fronto- parietals not ornamented; 22) epiotic eminences poorly defined; 23) cristae paroticae long and relatively broad; carotid artery enclosed in long, roofed, bony canal; 24) zygomatic ramus of squamosal slightly shorter than otic ramus; 25) otic ramus of squamosal of moderate length, expanded medially into small otic plate; 26) squamosal-maxillary angle about 50°; 28) prevomers entire, toothed, large, dentigerous rami in tenu- ous median contact; 29) palatines large, narrowly separated medially; 30) sphen- ethmoid entire, extending anteriorly beneath posterior edge of nasals; 31) an- 86 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY terior ramus of parasphenoid narrow, not keeled; 32) parasphenoid alae oriented at right angles to anterior ramus, over- lapped laterally by median rami of pterygoids; 33) pterygoids relatively large, anterior rami in long contact with maxillae, nearly reaching palatines; 34) occipital condyles moderately large, not stalked, narrow separated medially; 35) mandible lacking odontoids; 40) m. depressor mancUhiiloe in two slips; 41) pupil horizontal; 42) males with median subgular vocal sac; nuptial as- perities of many small spines on thumb; 43) body lacking glands; 44) tongue round, posterior edge free; 45) toes lack webbing, outer metatarsal tubercle ab- sent, digital tips narrow, first finger as long as second; 46) larvae with dextral vent, 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 47) am- plexus inguinal; 48) eggs laids in foam nest in temporary ponds and puddles; 49) males 40-70, females 40-96 mm. SVL; 50) tympanum visible externally. Composition. — Parker (1940) recog- nized four species (fetcheri, melanopij- gus, papuanus, and platyceps). The spe- cies of this genus appear to be sorely in need of review. Distribution. — Eastern New Guinea, the Aru Islands, and the eastern edge of Australia southward to New South Wales. Remarks. — Lechriodus was long- thought to be the only Australo-Papuan pelobatid genus. Noble (1926a) demon- strated that Lechriodus was a leptodac- tylid (bufonid in his terminology). In many respects, Lecliriodus is the most primitive genus of Limnodynastini — the skull is completely roofed, and the maxil- lary dentition is similar to that seen in the Cycloranini. In terms of breeding biology, it is only slightly more advanced than the generalized Limnodynastes. The firmly ankylosed intervertebral discs and the non-fusion of the cervical and second vertebrae possibly are advanced characters. Limnodynastes Fitzinger, 1843 (Figs. 61-62) Limnodynastes Fitzinger, 1843, Syst. Rept., 31 [Type-species by original designation, Cys- ti^nathiis peronii Dumeril and Bibron, 1841]. Wa^leria Girard, 1853, Proc. Acad. Nat. Sci. Philadelphia, 6:421 [Type-species by mono- typy, Cystignathus peronii Dumeril and Bib- ron, 1841]. Platyplectntm Giinther, 1863, Ann. Mag. Nat. Hist., (3)11:27 [Type-species by monotypy, Phityplectrinn marmoratum Giinther, 1863]. PlatypJectwn Peters, 1863, Mtber. k. Preuss. Akad. Wiss., Berlin, 1863:235 [Emendation of Platyplectrum Giinther, 1863; hence tak- ing .same type-species]. Lymnodynastcs Cope, 1865, Rev. Nat. Hist., 5:113 [Emendation of Limnodynastes Fitz- inger, 1843; hence taking same type- species]. Opisthodon Steindachner, 1867, Reise Novara, Amph., p. 9 [Type-species by mono- typy, Opisthodon frauenfeJdti Steindachner, 1867]. Heliorana Steindachner, 1867, Ibid., p. 32 [Type-species by monotypy, Heliorana graiji Steindachner, 1867]. Ranaster MaCleay, 1878, Proc. Linn. Soc. New South Wales, 2:135 [Type-species by mono- typy, Ranaster convexiuscidus MaCleay, 1878]. Diagnostic definition. — 5) cervical and second vertebrae fused; 7) omoster- num present, moderately large; 9) maxil- lary arch toothed, teeth blunt, pedicel- late; 10) alary processes of premaxillae directed posterodorsally, wide at base; 11) palatal shelf of premaxilla relatively narrow, palatal process present; 12) fa- cial lobe of maxilla deep, not exostosed; 13) palatal shelf of maxilla narrow, pterygoid process small; 15) nasals rela- tively small and widely separated medi- ally; 16) nasals in broad contact with maxillae, not contacting pterygoids; 17) nasals separated from frontoparietals; 18) frontoparietal fontanelle present, moderate-sized; 19) frontoparietals not ornamented; 22) epiotic eminences prominent; 23) cristae paroticae rela- tively short, stocky; carotid artery not enclosed in bony canal or groove; 24) zygomatic ramus of squamosal as long as otic ramus, widely separated from maxilla; 25) otic ramus of squamosal LYNCH: LEPTODACTYLOID FROGS 87 Figure 61. Dorsal and ventral views of skull of Limnochjnastes dorsalis ( KU 93553, X 2.2). moderate length, developed medially in- to small otic plate; 26) squamosal-maxil- lary angle about 50°; 28) prevomers large, entire, toothed, narrowly separated medially; 29) palatines broad, narrowly separated medially; 30) sphenethmoid entire, extending anteriorly to center of nasals; 31) anterior ramus of parasphe- noid of moderate width, not keeled; 32) parasphenoid alae oriented at right an- gles to anterior ramus, broadly over- lapped laterally by median rami of pterygoids; 33) pterygoids slender and large, anterior rami in long contact with maxillae, not reaching palatines; 34) oc- cipital condyles large, not stalked, nar- rowly separated medially in dorsalis group, moderately separated medially in pewnii group; 35) mandible lacking odontoids; 40) m. depressor mandibulae in two slips; 41) pupil horizontal; 42) males with median subgular vocal sac; males of convexiusculus, dorsalis, orna- tiis, spenceri, and tasrnaniertsis have nup- tial pads on thumb, whereas males of fietcheri, peronii, salmini, and the Eids- vold tasmaniensls lack nuptial asperi- ties; 43) tibial glands in dorsalis, other species lacking glands; 44) tongue large, slightly notched, free posteriorly; 45) toes lacking web to one-half webbed, inner metatarsal tubercle spade-like in the dorsaUs group, normal in the peronii group, outer metatarsal tubercle absent in all species except tasmaniensis, digi- tal tips narrow, first finger shorter than to longer than second; 46) larvae with median vent, 3/3 to 4/3 tooth rows, la- bial papillae broadly interrupted an- teriorly; 47) amplexus inguinal; 48) eggs laid in foam nest floating in open water or in water-filled holes adjacent to the main body of water; 49) males 32-87, females 32-83 mm. SVL; 50) tympanum visible externally or indistinct. Composition. — Parker (1940) recog- nized eight species — convexiusculus, dor- salis, fietcheri, ornatus, peronii, salmini, spenceri, and tasmaniensis. Moore ( 1961 ) suggested that spenceri was a subspecies of ornatus; he discussed a population of tasmaniensis-Vike frogs and considered them subspecifically or spe- cifically distinct but did not name or otherwise treat them taxonomically. Littlejohn (1968) noted northern and southern call races of tasmaniensis. Parker (1940) recognized five subspecies of dorsalis, but Moore (1961) did not discuss their status; Littlejohn (1968) recognized the fom* that occur in south- eastern Australia and Tasmania but stated that they hybridize (not inter- grade ) wherever their ranges meet there- by suggesting that the five are species. The nominal forms are dorsalis, dumerili, grayi, insularis, and interior is. Distribution. — Australia and Tas- FiGURE 62. Lateral view of skull of Limno- dynastes dorsalis ( KU 93553, X 2 ) . 88 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY mania; the genus is apparently absent from most of the western Eyrean sub- region. Remarks. — The two species-groups of Limnodynastes are readily separated. The dor sails group (dor sails, ornatus, and spenceri) is composed of medium sized, stocky frogs with large, spade-like inner metatarsal tubercles. The peronii group is composed of smaller species with a Rana-\ike habitus and "normal" inner metatarsal tubercle. Frogs of the dorsalis group are burrowers, whereas those of the peronii group seldom bur- row. The data presently available are sufficient to assert that the genus Lim- nodynastes does not contain enough variability to justify recognition of sub- genera. Cope (1866) combined Limnody- nastes with Borhorocaetes (an emenda- tion of Borborocoetes Bell; principally refers to Eupsophus). In an earlier paper Cope ( 1865 ) had considered them closely related but separable on the basis of the lateral extension of the prevo- merine tooth rows. Limnodynastes and Eupsophus differ in many respects — principally characters with which Cope was not familiar. The breeding biology of the two is quite different, and the vertebral column of Limnodynastes does not resemble that of Eupsophus; both are relatively generalized leptodactylids. The superficial skull bones of the two are very similar. Among the most im- portant characters in Cope's system were the separation of the prefrontals ( =na- sals) and the presence of a frontopari- etal fontanelle — Eupsophus and Limno- dynastes agree in these two characters. Kyarranus Moore, 1958 (Fig. 63) Kyarranus Moore, 1958, Amer. Mus. Novitates, 1919:1 [Type-species by original designa- tion, Kyarranus sphagnicolus Moore, 1958 {=Kyarranus sphagnicola)]. Diag,nostic definition. — 5) cervical and second vertebrae fused; 7) omoster- num present, small; 9) maxillary arch Figure 63. Lateral ( X 2.6) and dorsal ( X 2.3) views of the skull of Kyarranus sphagnicola (KU 110331). toothed, teeth blunt, pedicellate; 10) alary processes of premaxillae directed dorsally, relatively wide at base; 11) palatal shelf of premaxilla relatively nar- row, palatal process large; 12) facial lobe of maxilla deep, not exostosed; 13) palatal shelf of maxilla of moderate width, pterygoid process small; 15) na- sals small, widely separated medially; 16) nasals in contact with maxillae, not with pterygoids; 17) nasals not in con- tact with frontoparietals; 18) frontopari- etal fontanelle large; 19) frontoparietals not ornamented; 22) epiotic eminences obsolete; 23) cristae paroticae short and stocky; carotid artery enclosed in short, roofed, bony canal; 24) zygomatic ramus of squamosal relatively long, widely sep- arated from maxilla; 25) otic ramus of squamosal slightly shorter than zygo- matic ramus, expanded medially into moderately large otic plate; 26) squa- mosal-maxillary angle about 65°; 28) prevomers entire, toothed, widely sep- arated; 29) palatines wide, narrowly separated medially; 30) sphenethmoid entire, extending anteriorly to anterior edge of nasals; 31) anterior ramus of parasphenoid broad, not keeled; 32) parasphenoid alae oriented at right angles to anterior ramus, overlapped laterally by median rami of pterygoids; LYNCH: LEPTODACTYLOID FROGS 89 33) pterygoids slender, anterior rami in long contact with maxillae, nearly reach- ing palatines; 34) occipital condyles large, not stalked, narrowly separated medially; 35) mandible lacking odon- toids; 40) m. depressor mandihuJae in two slips; 41) pupil horizontal; 42) males with nuptial callosities on thumb; median, subgular vocal sac; 43) body lacking glands; 44) tongue large, notched posteriorly, posterior edge free; 45) toes free of webbing, outer metatarsal tuber- cle lacking, digital tips narrow, first fin- ger shorter than second; 46) develop- ment direct; 47) amplexus inguinal; 48) eggs laid underground in sphagnum or loose earth in a foam nest; 49) males 21- 35, females 30-34 mm. SVL; 50) tym- panum concealed. Composition. — Two species (love- ridgei and sphagnicola). Distribution. — The New England Range of eastern Australia and a dubi- ous record from Warragul, Victoria ( lowlands ) . Remarks. — Parker (1940) named loveridgei as a species of FJnJoria; Moore (1958) reexamined the holotype of Vhi- loria frosti and concluded that loveridgei was generically different from frosti. He included loveridgei with a new species from the southern part of the New Eng- land Range in a new genus, Kijarranus. The principal differences between Ki/ar- ronus and Limnodijnastes, according to Moore ( 1958, 1961 ) , were in breeding biology — the former exhibits direct de- velopment and the latter has tadpoles. Littlejohn ( 1963 ) questioned the separa- tion of Kijarranus and Philoria after he found that Philoria also exliibits direct development. The two genera differ in the development of the parotoid glands and in the arrangement of several skull bones. Kijarranus has a large frontopari- etal fontanelle and widely separated na- sals; in Fhiloria, the fontanelle is small and the nasals large and broadly in con- tact. Philoria Spencer, 1901 (Fig. 64) Fhiloria Spencer, 1901, Proc. Roy. Soc. Victoria, 13(2) :176 [Type-species by monotypy, Fhiloria frosti Spencer, 1901]. Diagnostic definition. — 5) cervical and second vertebrae fused; 7) omoster- num present, small; 9) maxillary arch toothed, teeth blunt, pedicellate; 10) alary processes of premaxillae directed posterodorsally, wide at base; 11) pala- tal shelf of premaxilla of moderate width, palatal process small; 12) facial lobe of maxilla deep anteriorly, shallow posteri- orly; 13) palatal shelf of maxilla of mod- erate width, large pterygoid process pos- teriorly; 15) nasals large, in broad medi- an contact; 16) nasals not in contact with maxillae or pterygoids; 17) nasals in contact with frontoparietals; 18) fron- toparietal fontanelle present, relatively small; 19) frontoparietals not orna- mented; 22) epiotic eminences poorly defined; 23) cristae paroticae relatively short and stocky; carotid artery enclosed Figure 64. Dorsal and ventral views of skull of Philoria frosti (KU 50699, X 4). 90 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY in a short, complete, canal; 24) zygo- matic ramus of squamosal of moderate length, widely separated from maxilla; 25) otic ramus of squamosal long, large, expanded medially into very large otic plate; 26) squamosal-maxillary angle about 58°; 28) pre vomers moderate- sized, entire, toothed, widely separated medially; 29); palatines large, widely separated medially; 30) sphenethmoid entire, large, extending anteriorly to mid- dle of nasals; 31 ) anterior ramus of para- sphenoid broad, not keeled; 32) para- sphenoid alae oriented at right angles to anterior ramus, slightly overlapped lat- erally by median rami of pterygoids; 33) pterygoids relatively small, anterior rami in long contact with maxillae, not reach- ing palatines; 34) occipital condyles large, not stalked, separated medially; 35) mandible lacking odontoids; 40) m. depressor manclilmlae in one slip — pars tympanictis; 41) pupil horizontal; 42) males with median subgular vocal sac but lacking nuptial asperities; 43) very large parotoid gland present; 44) tongue large, oval, free posteriorly; 45) toes free of webbing, outer metatarsal tubercle absent, inner of normal shape and size, first finger shorter than second; 46) de- velopment probably direct in nature; in laboratory-raised clutch, the tadpoles hatched but did not feed; had median vent, and mouth parts greatly reduced (Littlejohn, 1963); 47) amplexus ingui- nal; 48) eggs laid in foam nests in bur- rows and in holes dug in sphagnum; 49) males 41-46, females 47-51 mm. SVL; 50) tympanum concealed. Composition. — Monotypic, P. frosti. Distribution. — Known only from Mount Baw Baw, Victoria, Austraha. Remarks. — Philoria is related to Kyarranus and Limnodynastes. The three genera are readily distinguished on the basis of body glands and skeletons. Kyarranus and Philoria are superficially very similar in that their breeding biolo- gies are identical, both are genera of stubby frogs with short fingers, and the tympani are concealed. The similarity. in part, is probably due to adaptation to montane environments because several Neotropical genera living in the Andes, bear superficial resemblance to these Australian frogs. Kyarranus and Pluloria probably represent independent diver- gences from a Limnodynastes-\ike an- cestor. Myobatrachinae Schlegel, 1850 Myobatiachidae Schlegel, 1850:10. Uperoliidae Giinther, 1859a: 39. Criniae Cope, 1866:89. Criniinae: Noble, 1931:496. Myobatrachinae: Parker, 1940:64. The Myobatrachinae, as presently conceived, are restricted in distribution to the Australo-Papuan Region. The fol- lowing diagnostic statements are true for all members of the subfamily Myobatra- chinae: 1) sternum cartilaginous; 2) vertebral shield absent; 3) transverse processes of anterior presacral vertebrae not greatly expanded; 4) cervical cotylar arrangement type I; 5) cervical and sec- ond vertebrae free; 6) cranial bones not dermostosed; 8) sacral diapophyses di- lated; 14) maxillary arch complete; 20) frontoparietals not fused to prootics; 21 ) temporal arcade lacking; 30) spheneth- moid usually divided; 35) mandible lacking odontoids; 37) alary processes of hyoid plate broad and wing-like; 38 ) cri- coid cartilage divided ventrally; 39) m. petroliyoideus anterior and m. sterno- lu/oideus insert on the body of the hyoid plate, near the midline; 45) first finger shorter than second; 47) amplexus in- guinal in known species. All Myobatra- chinae exhibit free intervertebral discs and non-imbricate neural arches. The transverse processes of all vertebrae are shortened in some genera. Metacrinia sometimes has prezygapophyses on the anterior end of the coccyx. The presence of free intervertebral discs and small prevomerine bones are the most diagnos- tic osteological characteristics of the sub- family. Within the subfamily, there is an evolutionary trend toward the reduc- tion of bone in the skull; this reduction LYNCH: LEPTODACTYLOID FROGS 91 is reflected in the frontoparietal fonta- nelle, size of the nasal bones, massive- ness of the maxillary arch, divided sphenethmoid, and reduction in the size of the bones of the anterior palate. Two groups of myobatrachine genera tend to be segregated on the bases of several characters. Uperoleia is the only genus with vertical pupils, and the only one lacking a frontoparietal fon- tanelle. Glauertia and Uperoleia have two large, compressed, metatarsal tuber- cles— in the other myobatrachine genera, both metatarsal tubercles are small and not compressed, or the outer absent (Crinia: darlingtoni, haswelli, laevisjeai, rosea, and victoriana; and Taiidactyliis acutirostris). The quadratojugal bones are deep (Figs. 65, 69, and 71) in Crinia, Glauertia, and Uperoleia, but more slen- der in the other genera. The nasal bones are comparatively large in Glauertia, Metacrinia, Myohatrachtis, and Upero- leia. In these genera, the occipital con- dyles are larger than those of Crinia, Pseudophryne, and Taudactylus. The zygomatic rami of the squamosals are relatively short in Glauertia, Metacrinia, Myohairachus, and Uperoleia; in Crinia, PseudopJiryne, and Taudactylus the zygo- matic rami are longer. Loss of the teeth of the maxillary arch is characteristic of all genera of the subfamily, except Crin- ia and Taudactylus. Uperoleia rugosa (two species are included under this name, see Littlejohn, 1968) and U. mjoe- bergi have teeth on the maxillary arch, but U. marmorata lacks maxillary teeth. All myobatrachines except some species of Crinia lack prevomerine teeth. Crinia and Pseudophryne differ from the other myobatrachines in having no pars scapu- laris (m. depressor mandibulae); all other myobatrachines have two slips in the m. depressor mandibulae. Myobatrachine tadpoles have labial papillae only lateral to the tooth rows and beak — unlike other leptodactylids, the myobatrachines have an anterior and a posterior interruption of the labial papillae. The tooth rows are 1/3 to 2/3 in the known taxa. About one-half of the species of Crinia {laevis complex) and Glauertia and Uperoleia lay their eggs in water and have normal tadpole develop- ment. In these species the eggs are small (Martin, 1968). In the Crinia signifera complex, Metacrinia, Myobatrachus, and Pseudophryne the eggs are large and laid on land, part or all of the larval de- velopment occurring in the absence of water ( Martin, 1968 ) . Data are unavail- able for Taudactylus, which probably also lays its eggs on land. At least some of the "terrestrial breeders" of the gen- era Crinia and Pseudophryne hatch as tadpoles when the nest is inundated and rapidly begin feeding and behaving like normally aquatic tadpoles. Some Crinia and probably Metacrinia nichoUsi and Myobatrachus gouldii have completely terrestrial development (Martin, 1968). Noble ( 19.30 ) named a new genus, Indobatrachus, for Rana pusillus Owen, a Lower Eocene frog from the Intertrap- pean beds of Bombay in peninsular In- dia. He considered the fossil closest to Crinia and therefore placed it in the group now designated as Myobatrachi- nae. Noble argued that the presence of a toothless bufonid in the early Cenozoic of the northern land masses indicated a northern origin for the group. Parker (1940) andHecht (1963) suggested that the remains of Indobatrachus were over- interpreted, but failed to say why or how they reached that conclusion. Noble's data are not incompatible with the osteo- logical data I have for the Recent Myo- batrachinae. However, Indobatrachus could also be interpreted as not being very distant from Nesomantis and Soo- glosstis, which may prove to be myo- batrachines as well; these subjects are discussed more fully in the generic ac- count of Indobatrachus. Crinia Tschudi, (Fig. 65) 1838 Crinia Tschudi, 1838, Mem. Soc. Sci. Nat. Neuchatel, 2:38 [Type-species by mono- typy, Crinia georgiana Tschudi, 1838]. 92 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Ranidella Girard, 1853, Proc. Acad. Nat. Sci. Philadelphia, 6:421 [Type-species by mono- typy, Crinia (Ranidella) sises, and slightly dilated sacral diapophyses. All four genera have free swimming tadpoles. The tadpoles of Batraclu/la differ from those of the other genera in ha\ ing an uninterrupted series of labial papillae. The tadpoles of Tlioropa are greatly flattened and atten- uate (Fig. 2) in an adaptation to tor- rential stream life. Amplexus is inguinal in Batracliyla, but is axillary in Eiipso- phus and Hijlorina; the amplectic posi- tion is not known for Thoropa. Eiipso- phus and Hylorina lay numerous small eggs in water, whereas Batraclujla lays fewer larger eggs in terrestrial sites. The eggs of Batraclujla hatch and the larvae live in the jelly mass until the mass is inundated. Tlioropa has large eggs which are deposited on wet stones in situations where water trickles over stone ledges (Myers, 1946). Werner C. A. Bokermann (pers. comm.) suggested that the eggs are laid on the banks of the torrential streams inhabited by Thoropa. The following diagnostic character- istics are uniform among the four gen- era of the group: 3) transverse processes of posterior presacral vertebrae long; 5) cervical and second vertebrae not fused; 6) cranial bones not involved in dermo- stosis; 7) omosternum present, mod- erately large; 8) sacral diapophyses somewhat dilated — see Fig. 79; 9) max- illary arch toothed, teeth blunt, pedicel- late; 12) facial lobe of maxilla deep, not exostosed; 17) nasals not in contact with frontoparietals; 18) frontoparietal fon- tanelle moderate-sized; 19) frontopari- etals not ornamented; 20) frontoparietal not fused with prootic; 21) temporal arcade lacking; 37) alary processes of hyoid plate on narrow stalks; 42) males with nuptial asperities on thumb and sometimes second finger; some species of Eiipsophus have cluster of asperities on chest; 45) outer .iietatarsal tubercle pres- ent, inner metatarsal tubercle not en- larged or spade-like; 46) larvae with median vent. The tribal name, Alsodini, is based on Abodes Bell, 1843, which was recent- ly shown to be a synonym of Eupsophus (Lynch, 1968b). The heterogeneity of the tribe and the mosaic of primitive characteristics exhibited by the four in- cluded genera suggest that the Alsodini might be best regarded as a suprageneric grade between the primitive Telmato- biini and the advanced Eleutherodacty- lini. Eupsophus Fitzinger, 1843 (Fig. 83) Eupsophus Fitzinger, 1843, Syst. Rept., p. 31 [Type-species by original designation, Cys- tignathus roseus Dumeiil and Bibron, 1841]. HammatodactijJus Fitzinger, 1843, Syst. Rept., p. 31 [Type-species by original designation, Cijstignuthus nodosus Dumeril and Bibron, 1841]. Borborocoetes Bell, 1843, Zool. Voy. Beagle, Reptiles, 5:34 [Type-species by present designation, Borborocoetes grayi Bell, 1843; preoccupied by Borborocoetes Sclioenherr, 1842 (Insecta: Coleoptera)]. Abodes Bell, 1843, Ibid., .5:34 [Type-species by monotypy. Abodes monticola Bell, 1843]. i^ '" Gallardo ( 1970) proposed recognizing Alsodes as distinct from Eupsophus and included seven Patagonian species in Abodes. The seven are Abodes gargoJa Gallardo, 1970, Eupsophus il- lotus (Barbour), 1922, £. monticola (Bell), 1843, E. nodosus (Dumeril and Bibron), 1841, Tehnatobius montanus Lataste, 1902, T. prae- basahicus Cei and Roig, 1968, and T. ivveiberii Cei, 1969. Gallardo (1970) defined the genus Alsodes as follows: atlas convex, sternum ex- panded and notched posteriorly, tympanum not visible externally, vocal sac absent in males, forelimbs of reproductively active males greatly enlarged, and nuptial spines present on fingers and chest of reproductixely active males. Barrio (1970) tentatively accepted Gallardo's arrange- ment but did not include Tehnatobius pracba- salticus and T. reverberii as species of Abodes. Further comment on this arrangement is post- poned pending completion of my studies of the skeletons of several Tehnatobius (sensu Into). The separation of Alsodes from all other lepto- dactylids rests on the presence of pectoral plates of nuptial spines. Some species of Tehnatobius ijelskii group) haxe pectoral plates, as does Insuetophrynus acat})icus (Barrio, 1970). If Fitzinger's ( 1843 ) paper antedates Bell's LYNCH: LEPTODACTYLOID FROCS 125 Figure 83. Lateral, dorsal, and \'entral \iews of .skull of Etipsophus roseus (AMNH 22104, X 4.3). Eusophus Cope, 1865, Rev. Nat. Hist., 5:113 [Emendation (?) of Eupsophus Fitzinger, 1843]. Borhorocactes Cope, 1866, J. Acad. Nat. Sci. Philadelphia, (2)6:94 [Emendation of Borborocoetes Bell, 1843, hence taking same type-species]. Cacotus Giinther, 1868, Proc. Zool. Soc. Lon- don, 1868:482 [Type-species by monotypy, Cacotus maciilatus Giinther, 1868]. Thnjnopus Peters, 1873, Mtber. k. Preuss. Akad. Wiss., Berlin, 1873:416 [Type-species by monotypy, Phrtjnopus peruanus Peters, 1873]. Borhorocoetea Strand, 1928, Ark. Naturgesch., 92A:55 [Replacement name for Borboro- coetes Bell, 1843 (preoccupied), hence taking same type-species]. Diagnostic definition. — 4) cervical cotylar arrangement type II; 10) alary processes of premaxillae directed pos- terodorsally, moderately wide at base; 11) palatal shelf of premaxilla relatively deep, palatal process elongate; 13) pala- (1843), as herpetologists have generally pre- sumed, Hammatodactylus Fitzinger, 1843 (type- species Cystignathiis nodosus Dumeril and Bibron, 1841) is the correct name for the generic group recognized by Gallardo (1970) and Barrio (1970) and called Alsodes. tal shelf of maxilla of moderate width, pterygoid process moderately large; 14) maxillary arch complete, quadratojugal present; 15) nasals small, widely sep- arated medially; 16) nasals in broad con- tact with maxillae, not in contact with pterygoids; 22) epiotic eminences promi- nent; 23) cristae paroticae relatively broad, elongate; carotid artery passes dorsal to skull bones; 24) zygomatic ra- mus of squamosal of moderate length, widely separated from maxilla; 25) otic ramus of squamosal as long as zygomatic ramus, expanded medially into small otic plate; 26) squamosal-maxillary angle 50- 55°; 27) columella present or absent; 28) prevomers moderate-sized, separated medially, entire, toothed except in jun- inensis; 29) palatines broad, widely sep- arated medially, bearing odontoid ridges; 30) sphenethmoid entire, extending an- teriorly to anterior edge of nasals; 31) anterior ramus of parasphenoid broad, short, keeled medially; 32) parasphenoid alae oriented at right angles to anterior ramus of parasphenoid, broadly over- lapped laterally by median rami of ptery- 126 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY golds; 33) pterygoids moderate-sized, anterior rami in long contact with maxil- lae, reaching palatines; 34) occipital condyles large, not stalked, narrowly separated medially; 36) terminal pha- langes knobbed; 40) m. depressor man- dihulae in two slips except in juninensis which has only the pars tympanicus; 41) pupil horizontal; 42) males with median subgular vocal sac or none; 43) body lacking glands or having extensive, dif- fuse glandular areas over dorsum; 44) tongue large, round, posterior edge free; 45) toes lacking webbing or fringing to two-thirds webbed; 46) larvae with 2/3 tooth rows, labial papillae interrupted anteriorly; 47) amplexus axillary; 48) eggs small and numerous, laid in gela- tinous masses in ponds; 49) males 32- 80, females 32-60 mm. SVL; 50) tym- panum visible externally, concealed, or absent. Composition. — Revisionary studies of the Argentine and Chilean species are available (Cei, 1962a, Grandison, 1961, and Gallardo, 1962 ) . As a result of these studies and my own (Lynch, 1971), seven species of the genus are presently recognized: illotus, juninensis, monti- cola, nodosus, peruanus, roseus, and ver- tehralis. The status of the genus in Peru is poorly known. Distribution.— The Andes of central Peru to Argentina and Chile; between about 10° and 50° S latitude in western South America. Remarks. — Boulenger (1882) com- bined a large number of genera and species into Borhorocoetes Bell {^Eup- sophus) in his synopsis of living am- phibians. While most of his generic groupings were a vast improvement over the previous classifications, Borhoro- coetes was a notable exception. He in- cluded a variety of unrelated groups in Borhorocoetes. The Borhorocoetes of Boulenger and Noble is best described as a grade (in the sense of Huxley, 1958). All of the species included are members of the Telmatobiinae, and ac- cording to the present classification be- long to the genera Batraclujia, Eleu- tJierodactyhis, Eupsophus, Ischnocnema, Niceforonia, TJioropa, and Zachaenus. The Chilean and Argentine species of Eupsophus were studied in detail by Cei (1960, 1962a, and 1962b) and Grandison ( 1961 ) , but they confused one species of BatracJu/la with Eupsophus (iaenia- tus). Cei (i962a) and Grandison (1961) divided Eupsophus into three species groups — nodosus group, peruanus group, and roseus group. These authors also recognized a monotypic taeniatus group, which is here included in Batraclujia. Two species of the genus (juninensis and monticola have lost the columella. These species also lack tympanic annuli. The tympanic annulus is very small in two other species of the genus, illotus and nodosus, and is concealed beneath the skin. In peruanus, roseus, and ver- tebralis, the columella is normal-sized and the tympanic annulus is visible ex- ternally. Schaeffer (1949) described, but did not name, a fossil frog from the Lower Oligocene of Chubut, Argentina, and re- ferred it to Eupsophus. ^^ The nasals of the fossil are apparently in median con- tact, unlike the condition seen in the living species of the genus. The fossil could equally well be a species of Tel- matohius, were it not for the fact that the frontoparietal fontanelle is moderate- ly large, not small. The middle ear was not preserved. Hylorina Bell, 1843 (Fig. 84) Hylorina Bell, 1843, Zool. Voy. Beagle, Rep- tiles, 5:44 [Type-species by monotypy, Hy- lorina sylvatica Bell, 1843]. Hylorliina Agassiz, 1846, Noniencl. Zool., in- dex: 190 [Emendation of Hylorina Bell, 1843, hence taking same type-species]. " Bogart ( 1970) implied that the Oligocene fos- sil of Eupsophus is not separable from living E. roseus. However, Schaeffer (1949) cited dis- tinguishing features of the fossil, chiefly in the arrangement of the nasal bones. The Oligocene fossil needs to be restudied to ascertain its dis- tinction from Tclmatohiits. LYNCH: LEPTODACTYLOID FROGS 127 Figure 84. Dorsal and ventral views of skull Diagnostic definition. — 4) cervical cotylar arrangement type II; 10) alary processes of premaxillae directed dorsal- ly, wide at base; 11) palatal shelf of pre- maxilla narrow, palatal process relatively small; 13) palatal shelf of maxilla nar- row, pterygoid process minute; 14) max- illary arch incomplete, quadratojugal ab- sent, replaced by ligamentous sheath; 15) nasals moderate sized, widely sep- arated medially; 16) nasals in tenuous contact with maxillae, not in contact with pterygoids; 22) epiotic eminences moderately well defined; 23) cristae paroticae short, stocky; carotid artery passes dorsal to skull bones; 24) zygo- matic ramus of squamosal of moderate length, widely separated from maxilla; 25) otic ramus of squamosal moderately long, shorter than zygomatic ramus, ex- panded medially into small otic plate; 26); 27) columella present; 28) prevo- mers moderately large, entire, narrowly separated medially, toothed; 29) pala- tines broad, widely separated medially, no odontoid ridges; 30) sphenethmoid entire, extending anteriorly to middle of nasals; 31) anterior ramus of parasphe- noid broad, short, not keeled medially; 32) parasphenoid alae oriented at right angles to anterior ramus, broadly over- lapped laterally by median rami of pterygoids; 33) pterygoids small, an- terior rami short, extending to middle of orbit; 34) occipital condyles moderately of Hijlorina stjlvatica (BMNH 91.29.17, X 3). large, not stalked, narrowly separated medially; 36) terminal phalanges knobbed, elongate; 40) m. depressor mandibtdue in two slips; 41) pupil ver- tical; 42) males with median subgular vocal sac; 43 ) body with glandular dorso- lateral folds; 44) tongue large, rounded, posterior edge free; 45 ) toes lacking web- bing or lateral fringes, digital tips narrow, first finger longer than second; 46) larvae with 2/2 tooth rows, labial papillae in- terrupted anteriorly; 47) amplexus axil- lary; 48) eggs small, numerous, laid in gelatinous masses at bases of plants in water; 49) males 50-60, females 60-68 mm. SVL; 50) tympanum visible exter- nally; 51) digits extremely long, phalan- geal formulae not increased. Composition. — Monotypic. Distribution. — Central Chile. Remarks. — Because Hylorina is un- common, the genus was studied with the aid of stereo-radiographs. Hylorina has been considered generically distinct since Bell's description of the type-species. In part the distinction stemmed from er- roneous data provided by Boulenger (1882), who reported the sternum as bony. The genus Hylorina is very dis- tinctive even though the sternum is a cartilaginous plate which tends to calcify in old adults. The combination of verti- cal pupil, free toes, greatly elongated digits, externally visible tympanum, and teeth on maxillary arch and prevomerine 128 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY dentigerous processes immediately dis- tinguishes Hylorina from all other frog genera. In spite of the distinctiveness of Hylorina, its skeletal morphology allies it with Eupsoplms. The data on breed- ing biology reported by Barrio (1967b) provide additional distinction for Hy- lorina, but also point out the similarity between Eupsophus and Hylorina. Batrachyla Bell, 1843 (Fig. 85) Batrachyla Bell, 1843, Zool. Voy. Beagle, Rep- tiles, 5:43 [Type-species by monotypy, Ba- traclujla leptoptis Bell, 1843]. Diagnostic definition. — 4) cervical cotylar arrangement type I; 10) alary processes of premaxillae directed dorsal- ly and somewhat laterally, moderately wide at base; 11) palatal shelf of pre- m axilla very narrow, palatal process rela- tively large; 13) palatal shelf of maxilla narrow, pterygoid process lacking; 14) maxillary arch incomplete, cjuadrato- jugal absent; 15 ) nasals widely separated medially, relatively small; 16) nasals separated from maxillae and pterygoids; 22) epiotic eminences obsolete; 23) cristae paroticae stocky, relatively long; carotid artery passes dorsal to skull bones; 24) zygomatic ramus of squa- mosal elongate, widely separated from maxilla; 25) otic ramus of squamosal moderately long, expanding medially in- to small otic plate; 26) squamosal-maxil- lary angle about 60°; 27) columella present; 28) prevomers relatively small, entire, separated medially, toothed; 29) palatines curved, narrow, widely sep- arated medially; 30) sphenethmoid en- tire, extending anteriorly to a point an- terior to nasals; 31) anterior ramus of parasphenoid broad, short, lacking medi- an keel; 32) parasphenoid alae oriented at right angles to anterior ramus of para- sphenoid, not overlapped by median rami of pterygoids; 33) pteiygoids small, thin, anterior rami short, not extending beyond middle of orbits; 34) occipital condyles small, not stalked, widely sep- arated medially; 36) terminal phalanges T-shaped; 40) 7n. depressor mandilmlae Figure 85. Lateral, dorsal, and ventral views of skull of Batrachyla leptopus (UMMZ S-2246, X 6). LYNCH: LEPTODACTYLOID FROGS 129 in two slips; 41) pupil horizontal; 42) males with median subgular vocal sac; 43) body lacking glands; 44) tongue moderately large, posterior one-third free; 45) toes lacking web or lateral fringes, digital tips bulbous, somewhat dilated, first finger shorter than second; 46) larvae with 2/3 tooth rows, labial papillae not interrupted about mouth; 47) amplexus inguinal; 48) eggs rela- tively few, large, laid in terrestrial situa- tions, tadpoles become aquatic after nest is inundated; 49) adults 27-40 mm. SVL; 50) tympanum visible externally. Composition. — Barrio (1967a) recog- nized two species (aniartandica and hp- toptis) of Batraclnjla. Lynch (1971) demonstrated that Eupsophiis taeniatus belongs to the genus Batrachyla. Distribution. — Chile and adjacent Argentina between 32° and 50° S lati- tude. Remarks. — Boulenger (1882) and Myers (1962) considered BatrachijJa synonymous with Eleutherodactijlus (Hylodes Fitzinger, 1843, in the case of Boulenger). Both authors were under the mistaken impression that the two genera did not differ in significant char- acters. The two differ as follows (the condition in EleutJierodactylus is en- closed in parentheses ) : quadratojugal absent (present), frontoparietal fonta- nelle present (absent), nasals small and widely separated medially (large and in median contact), sacral diapophyses di- lated (rounded), males with nuptial asperities on thumb (lacking nuptial asperities), aquatic tadpoles (develop- ment direct — no tadpole stage ) , and am- plexus inguinal ( axillary ) . The breeding biology of Batrachyla is decidedly more primitive than that of Eleutherodactylus but approaches the condition of the lat- ter in that the eggs are relatively large, few in number, and laid in moist ter- restrial situations (Barrio, 1967a, and Cei, 1962a). In contrast to the eleu- therodactyline pattern, tadpoles emerge when the egg hatches and development proceeds in the typical anuran manner. Thoropa Cope, 1865 (Fig. 86) Thoropa Cope, 1865, Rev. Nat. Hist., 5:110 [Type-species by monotypy, Cysiignathus tuissiessii Eydoux and Souleyet, 1842]. Ololygon Fitzinger (1843) is often cited as an older generic name for Tlioropa. The type-species of Ololygon is Hyla strigilata Spix, 1824 (by original designation of Fitzinger, 1843). There- fore, Ololygon Fitzinger is a synonym of Hyla Laurenti, 1768. Diagnostic definition. — 4) cervical cotylar arrangement type I; 10) alary processes of premaxillae directed dorsal- ly and slightly anteriorly, relatively nar- row at base; 11) palatal shelf of premax- illa very narrow with elongate palatal process; 13) palatal shelf of maxilla broad, pterygoid process present; 14) maxillary arch complete, quadratojugal present; 15) nasals relatively large with moderately long maxillary processes, sep- arated medially; 16) nasals not in con- tact with maxillae or pterygoids; 22) epiotic eminences relatively well defined; 23 ) cristae paroticae long and narrow in miliaris, short and relatively stocky in lutzi and petropolitanus; carotid artery passes dorsal to skull bones; 24) zygo- matic ramus of squamosal relatively short; 25) otic ramus of squamosal mod- erately long, no otic plate; 26) squa- mosal-maxillary angle 50-70°; 27) colu- mella present; 28) prevomers relative- ly small, entire, separated medially, toothed; 29) palatines long and narrow, expanded laterally, separated medially; 30) sphenethmoid entire, extending an- teriorly to posterior edge of nasals or not reaching nasals; 31) anterior ramus of parasphenoid broad, keeled medially, extending anteriorly to prevomers; 32) parasphenoid alae oriented at right angles to anterior ramus of parasphe- noid, relatively short, not overlapped laterally by median rami of pterygoids; 33) pterygoids large, anterior rami in long contact with maxillae, not reaching palatines; 34) occipital condyles large in miliaris, small in lutzi and petropoli- 130 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 86. Lateral, dorsal, and ventral views tanus, not stalked, moderately to widely separated medially; 36) terminal pha- langes T-shaped; 40) m. depressor man- dihulae in two sHps; 41) pupil horizon- tal; 42) males with median subgular vocal sac; 43) body lacking glands; 44) tongue large, oval, posterior edge free; 45) toes lacking webbing, bearing lateral fringes, digital tips bulbous, somewhat dilated, first finger shorter than second; 46) larvae with 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 47 ) ; 48 ) eggs large, few in number, laid in lotic situations; 49) males 19-78, fe- males 24-70 mm. SVL; 50) tympanum visible externally; 51) tadpoles with greatly flattened and attenuate bodies and tails. Composition. — Three species were recognized in the revision by Bokermann (1965): lutzi, miUaris, and petropoli- tanus. Distribution. — Mountains of south- eastern Brasil between 12° and 30° S latitude. Remarks. — Thoropa is least different from Batrachijla, although most authors have considered it inseparable from of skull of Thoropa Jutzi (KU 92850, X 4.5). Eupsophus. Gallardo (1965) and Lynch ( 1971 ) demonstrated the distinctiveness of these two genera. Lutz (1954) sug- gested that Thoropa was closely related to Cycloramplms. Tlwropa and Cyclo- ramphiis belong to different tribes; this distinction is supported by osteological, non-osteological, and behavioral and larvae data. Odontophrynini New Tribe Two genera are included in this tribe — Odontophnjnus and Proceratophnjs (the nominal genus Macrogenioglottus is inseparable from Odontoplinjmis) . Proceratophnjs is the generic name used herein for the group previously called Stomhiis. The members of this tribe bear considerable external resemblance to the Ceratophryinae, especially Cera- tophrys. The ilia of the Odontophrynini (Fig. 38) are nearly identical to those of the Ceratophryinae, but the two groups differ in many ways ( see subfamily char- acters for Ceratophryinae and Telmato- biinae). The Odontophrynini are dis- tributed in non-forested and some for- LYNCH: LEPTODACTYLOID FROGS 131 ested habitats in Argentina, Paraguay, Uruguay, and along the eastern edge of Brasil to Estado de Ceara. Like the other primitive Telmatobiinae, the Odontophrynini have an aquatic stage in the Hfe history, and amplexus is axillary. The following diagnostic characteristics are the same in both genera: 3) trans- verse processes of posterior presacral \'ertebrae short; 5) cervical and second xertebrae free; 6) cranial bones not in- x'olved in dermostosis; 7) omosternum lacking; 9) maxillary arch toothed, teeth blunt, pedicellate; 11) palatal shelf of premaxilla broad, weakly notched, pala- tal process large; 12) facial lobe of max- illa deep; 14) maxillary arch complete; 16) nasals in contact with maxillae and pterygoids; IS) frontoparietal fontanelle lacking; 20) frontoparietals not fused with prootics; 21 ) temporal arcade lack- ing; 22) epiotic eminences prominent; 23) cristae paroticae long and narrow; carotid artery passes dorsal to skull bones; 27) columella present; 28) pre- vomers relatively small, entire, toothed, narrowly separated medially; 29) pala- tines large, narrowly separated medially, bearing odontoid ridge, expanded lat- erally; 30) sphenethmoid large, entire, extending anteriorly to front edge of nasals; 31) anterior ramus of parasphe- noid narrow, pointed, not keeled; 32) parasphenoid alae oriented at right angles to anterior ramus, broadly over- lapped laterally by median rami of pterygoids; 33) pterygoids large, an- terior rami long, in broad sutural contact with maxillae, maxillary process of na- sals, and palatines; 36) terminal pha- langes knobbed; 37) alary processes of hyoid plate on narrow stalks; 40) m. de- pressor mandihulae in two slips; 41 ) pu- pil horizontal; 42) males with median, subgular vocal sac; 44) tongue large, round, posterior edge free; 46) larvae with median vent, 2/3 tooth rows, and labial papillae broadly interrupted an- teriorly; 47) amplexus axillary; 48) eggs small, numerous, laid in gelatinous masses in ponds; 50) tympanum con- cealed. The pectoral girdle is not as massive as in the Telmatobiini, and the omoster- num has been lost in the Odontophry- nini. The occipital condyles are more widely separated in Odontophnjnus than in Proceratophnjs (Figs. 87-88). The cervical cotylar pattern of both genera is type II, although the cotyles are more widely spaced in Odontophnjnus (Fig. 79). In several character complexes, the Odontophrynini are intermediate be- tween the Ceratophryinae and the Tel- matobiini, but they also bear some re- semblance to the EleutherodactyHni. Odontophrynus Reinhardt and Liitken, 1862 (Fig. 87) Odontophrynus Reinhardt and Liitken, 1862, Vid. Meddel. Naturh. Foren., 13:159 [Type- species by monotypy, Odontophrynus cul- tripes Reinhardt and Liitken, 1862]. Hyperoodon Philippi, 1902, Supl. Bat. Chilenas, p. 1 [Type-species by monotypy, Hyper- oodon asper PhiUppi, 1902; preoccupied by Hyperoodon Lacepede, 1804 (Mammalia: Cetacea)]. Macrogenioglottus Carvalho, 1946, Bol. Mus. Rio de Janeiro, (new ser. ) 73:1 [Type- species by original designation, Macrogenio- glottus alipioi Cai-valho, 1946]. Diagnosiic definition. — 4) cervical cotylar arrangement type II, but cotyles well separated medially; 8) sacral dia- pophyses slightly dilated; 10) alary processes of premaxillae directed pos- terodorsally, long, relatively narrow at base; 13) palatal shelf of maxilla broad, pterygoid process small or lacking; 14) maxillae not expanded posteriorly; 15) nasals relatively large, keeled, narrowly separated anteriorly; 17) nasals not in contact with frontoparietals; 19) fronto- parietals not ornamented except for ridge around posterior half of the brain- case roof; 24) zygomatic ramus of squa- mosal long, tapering, widely separated from maxilla; 25) otic ramus of squa- mosal long, expanded medially into nar- row otic plate; 26) squamosal-maxillary angle 50-55°; 34) occipital condyles 132 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 87. Lateral, dorsal, and ventral views of skull of Odontophrtinus carvalhoi (KU 100441, X 3.2). large, not stalked, median separation moderate; 42) males with nuptial as- perities on thumb; 43) parotoid and/ or temporal or tibial glands present; 45) toes about one-half webbed, outer meta- tarsal tubercle present, inner metatarsal tubercle enlarged and spade-like, digital tips narrow, relatively few supernu- merary tubercles on plantar surfaces, first finger longer than second; 49) males 30- 60, females 34-70 mm. SVL. Composition. — Savage and Cei (1965) recognized four species (americanus, carvalhoi, cultripes, and occidentalis). The type species of Macrogenioglottus, Odontophrijmis alipioi (Carvalho) [new combination] is here added to the genus. Distribution. — Semi-arid and arid non-forested habitats of northern Argen- tina, southern Bolivia and Paraguay, Uruguay, and along the coastal provinces of southeastern and eastern Brasil to Bahia. Remarks. — Carvalho (1946) named Macrogenioglottus alipioi on the basis of two specimens from Bahia, Brasil. The genus was distinguished from all others on the basis of the greatly enlarged m. genioglottus, slightly dilated sacral dia- pophyses, short coccyx, and slightly dif- ferent positions of the prevomerine den- tigerous processes. The myological dis- tinction between Macrogenioglottus and Odontophrynus remains valid, but with the description of O. carvalhoi (Savage and Cei, 1965 ) , the other differences be- tween the two genera were mitigated. The architecture of the temporal region of alipioi was figured by Limeses ( 1965) and is like that of other species of Odon- tophrynus. Savage and Cei (1965) rec- ognized two groups in Odontophrynus, one for cultripes and occidentalis, and another for americanus and carvalhoi. Odontophrynus alipioi belongs to the latter group and seems closely related to carvallioi. The two species share many characteristics but diff^er (insofar as is known at present ) in some body propor- tions, color pattern, and colors in life. Odontophrynus alipioi has been collected recently near Sao Paulo ( W. C. A. Boker- mann, pers. comm.). Boulenger (1882) confused Odonto- LYNCH: LEPTODACTYLOID FROGS 133 phnjnus with Ceratophnjs, Lepidobatra- chus, and Proceratophnjs. The cerato- phryine leptodactyHds are readily sep- arated from the two tehnatobiine genera in that the derm of the head is fused with the skull bones and a dermostosed vertebral shield is present in the Cerato- phryinae. In addition, the Ceratophryi- nae ha\'e non-pedicellate teeth whereas all other leptodactyHds (if dentate) have pedicellate teeth. Odontophnjnus and Proceratophnjs, especially those of the bigibbosa group, are somewhat difficult to separate on external characters alone. The thenar surfaces of Proceratoplirys are covered with numerous conical super- numeraiy tubercles, whereas the thenar surfaces of Odontoplirt/nus lack super- numerary tubercles or have relatively few, non-conical supernumerary tuber- cles. Some, but not all, species of Odon- tophnjnus have body glands (parotoid, temporal, or tibial), whereas no species of Proceratophnjs has glands. Osteo- logically, the two genera are readily sep- arated. Proceratophnjs has a complete post-orbital bridge (squamosal only), and Odontophnjnus has a "normal" squamosal. Proceratophnjs has extensive exostosis of the frontoparietal bones and Odontophnjnus has no exostosis of the frontoparietals but does have a ridge around the posterior half of the fronto- parietal shelf. Philippi (1902) named Hijperoodon asper on the basis of two specimens from Montevideo, Uruguay. Subsequent au- thors credited him with naming Hij- peroodon as a new genus although Philippi obviously credited the genus to Dumeril and Bibron. Hijperoodon Phil- ippi is probably a misspelling for Upero- don Dumeril and Bibron, a microhylid genus. Nieden (1923) tentatively re- ferred Hijperoodon asper to Pahidicola; the nominal species is currently consid- ered a possible synonym of Phijsalaemus gracilis (Gorham, 1966). Cei ( 1958 ) correctly pointed out that Hijperoodon asper is an Odonto- phnjnus and tentatively suggested that asper was identical with O. americanus. Inexplicably, Savage and Cei (1965) did not consider the nominal species in their review of Odontophnjnus. There is no question, in view of Philippi's descrip- tion and Cei's ( 1958 ) publication of Philippi's long-lost plates, that Hyper- oodon asper is an Odontophnjnus, except for Philippi's remarks that maxillaiy and premaxillary teeth are lacking in the types. Philippi further recorded the presence of prevomerine teeth, suggest- ing that his observation on the lack of maxillary and premaxillary teeth was er- roneous. Hyperoodon asper cannot be considered a synonym of any species of Physalaemus; it is here transferred to the synonymy of Odontophnjnus ameri- canus. Proceratophrys Miranda-Ribeiro, 1920 (Fig. 88) Proceratophrys Miranda-Ribeiro, 1920, Rev. Mus. Paulista 12:301 [Type-species by monotypy, Ceratophnjs bigibbosa Peters, 1872]. Diagnostic definition. — 4) cervical cotylar arrangement type II, cotyles closely approximated; 8) sacral dia- pophyses rounded; 10) alary processes of premaxillae long, strongly directed pos- terodorsally, except in bigibbosa group, relatively narrow at base; 13) palatal shelf of maxilla broad, pterygoid process prominent; 14) maxillae slightly ex- panded posteriorly; 15) nasals relatively narrow, keeled, separated medially (boiei group) or in contact (bigibbosa group) medially; 17) nasals in contact with frontoparietals; 19) frontoparietals bear lateral crests which meet posterior- ly; frontoparietal crests heavily exostosed posteriorly in cristiceps and probably in bigibbosa; 24) zygomatic ramus of squa- mosal broad and elongate, in sutural contact with maxilla, weakly exostosed; 25) otic ramus of squamosal large, exo- stosed, expanded medially into relatively large otic plate; 26) squamosal-maxillary angle 40-50°; 34) occipital condyles large, not stalked, closely juxtaposed; 134 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 88. (A-C) Dorsal, ventral and lateral views of skull of Proceratophnjs hoiei (KU 93076) and (13- E) dorsal and lateral views of skull of P. cristiceps ( KU 106273). All X 2.2. 42) males lacking nuptial asperities on thumb; 43) body lacking glands; 45) toes free of webbing, usually with lateral fringes, outer metatarsal tubercle pres- ent, inner metatarsal tubercle small or enlarged and spade-like, digital tips nar- row, numerous conical supernumerary thenar and plantar tubercles, first finger longer than second; 49) adults 30-95 mm. SVL. Composition. — Eight of the nominal species listed as Ceratoplirys by Gorham ( 1966) belong to this genus: appendicu- lata, Ingibbosa, boiei, cristiceps, fryi, goyanus, renalis, and schirchi. Gorham (1966) did not list Stombus melanopo- gon Miranda-Ribeiro, 1926. Bokermann (1966) considered boiei, melanopogon, renalis, and schirchi synonymous and used boiei, the oldest name. He also considered goyanus a synonym of cris- ticeps. Distribution. — The lowland zone east of the Brasilian Highlands from Forta- leza (Ceara) to Santa Catarina, Brasil, and adjacent Misiones Province, Argen- tina. Remarks. — Almost all of the litera- ture pertaining to species of this genus has accumulated under the generic name Stombus, a synonym of Ceratoplirys (see pp. 107-10). Reig and his students have consistently argued that Stotnbus (auc- torum) is generically distinct, but they have also repeatedly questioned the ge- neric position of cristiceps. I include cristiceps in the genus Proceratophrys and consider bigibbosa its closest rela- tive; this arrangement is similar to that used by Reig in that cristiceps is not con- sidered especially closely related to ap- pendiculata, boiei, and fryi. The differ- ences between bigibbosa and cristiceps on the one hand, and appemlicnlata, LYNCH: LEPTODACTYLOID FROGS 135 boiei, and fnji on the other, are not of the magnitude I would use at the ge- neric level. The five species form a group on the basis of the thenar and plantar tubercle arrangement, body shape, and the architecture of the tem- poral region. The two species groups differ in head shape and the correlated and underlying cranial architecture (snout is elongate and sloping in boiei group, blunt and short in higihhosa group) and in the development of cra- nial exostosis (Fig. 88). The differences in musculature that Limeses ( 1964, 1965) cited as suggestive of separate genera are trivial differences; greater ranges of variation occur within Odon- tophnjnus and several other frog gen- era. The species of the higihhosa group are less unlike Odontophnjnus in exter- nal features than are the species of the hoiei group. In the hoiei group, the eye- lids are provided with elongate "horns," whereas in the higihhosa group, the eye- lid has only a few large tubercles. Grypiscini Mivart, 1869 Grypiscina Mivart, 1869:295. Cyclorhaniphinae Lutz, 1954:175. Gycloramphiinae: Gallardo, 1965:84. Three genera are included in this tribe — Crossodactylodes, Cijcloramphus, and Zachaenus. The nominal genus Craspedoglossa is here considered to be a synonym of Zachaenus. The tribe name is based on Grypiscus Cope, a syn- onym of Cycloramphus Tschudi. At first glance, this group seems to be highly heterogeneous, especially when one con- "7siders the supposed relationships of the leptodactylid genera as recognized by herpetologists in the 1910-1930 period when the following genera (all of this group) were recognized: Craspedoglos- sa, Cycloramphus, Grypiscus, lliodlscus, Oocormus, and Zachaenus. Miranda- Ribeiro (1926), Lutz (1954), and Coch- ran (1955) considered Zachaenus to be closely related to Ceratophrys. Oocor- mus was often recognized even by Lutz after she pointed out that it was a syn- onym of Zachaenus (1944). Various authors including Noble ( 1931 ) sug- gested that Cycloramphus was closely related to Tehnatohius. Cycloramphus, Iliodiscus, and Grypiscus were usually considered valid until Bokermann ( 1951 ) pointed out that they were not generi- cally distinct. Lutz (1954) included only Cyclorhamphus (sic) and Thoropa in the subfamily, Lutz and Carvalho ( 1958) considered Paratelmatobius to be a generic link between Cycloraynphus and Batrachophrynus and Tehnatohius, and Gallardo ( 1965 ) placed Craspedo- glossus (sic), Cycloramphus, Holoaden, and Zachaenus in the subfamily Gyclo- ramphiinae. All of these authors used labile characters (head shape and toe webbing) to define their groupings. Most of the genera that have been con- sidered related to Cycloramphus are bur- rowing frogs and have long, flat snouts. The following diagnostic character- istics are the same in the included gen- era: 3) transverse processes of posterior presacral vertebrae not shortened; 4) cervical cotylar arrangement type I; 5) cervical and second vertebrae free; 6) cranial bones not involved in dermosto- sis; 9) maxillary arch toothed, teeth blunt, pedicellate; 12) facial lobe of maxilla deep, not exostosed; 14) maxil- lary arch complete, maxilla expanded posteriorly, quadratojugal deep; 15) na- sals relatively large, in broad median contact; 17) nasals in contact with fron- toparietals; 18) frontoparietal fontanelle lacking; 20) frontoparietal not fused to prootic; 21) temporal arcade lacking; 23) cristae paroticae very short, stocky; carotid artery passes dorsal to skull bones; 24) zygomatic ramus of squa- mosal attenuate, curved, widely sepa- rated from maxilla; 25) otic ramus of squamosal long, curved medially and expanded medially to form otic plate which rests on crista parotica; 34) occip- ital condyles relatively small, not stalked, widely separated medially; 37) alary processes of hyoid plate on narrow stalks; 40) m. depressor mandihulae in 136 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY two slips; 41) pupil horizontal; 47) am- plexus axillary. The developmental pattern of Cijclo- ramphus and Zacliaenus is intermediate between the typical pattern of an aquatic tadpole and the eleutherodactyline pat- tern of direct development ( Lutz, 1944 ) . The eggs are deposited in terrestrial situations (usually in very wet leaves on the forest floor) and the tadpole hatches and lives in the moist, decomposing gelatinous mass. The tadpoles can sur- vive in an aquatic medium but do not feed (Lutz, 1944). Crossodactylodes lays only a few large eggs in bromeliads and the tadpole develops in the moist axillae of the bromeliads (W. C. A. Bokermann, pers. comm.). Holoaden, Paratelmatohius, and Thoropa do not agree with the diagnos- tic characteristics listed above and are included in other groups; Holoaden is in the Eleutherodactylini, Paratelmatohius in the Leptodactylinae, and Tlwropa in the Alsodini. The three genera of the tribe occur in forested montane areas in southeast- ern Brasil and Uruguay. Two of the species presently placed in Zachaenus (roseus and sawayae) are not members of that genus. Their status is discussed in the account of Zachaenus. Crossodactylodes Cochran, 1938 (Fig. 89) Crossodactylodes Cochran, 1938, Proc. Biol. Soc. Washington, 51:41 [Type-species by original designation, Crossodactylodes pintoi Cochran, 1938]. Diagnosiic definition. — 7) omoster- num relatively small; 8) sacral dia- pophyses dilated; 10) alary processes of premaxillae directed posterodorsally, broad at base; 11) palatal shelf of pre- maxilla relatively broad, broadest lat- erally, with long palatal process; 13) palatal shelf of maxilla broad anteriorly, narrow over most of its length, pterygoid process lacking; 16) nasals in tenuous contact with maxillae, not in contact with pterygoids; 17) nasals in tenuous contact with frontoparietals, narrowly separated from frontoparietals; 19) fron- toparietals not ornamented, lacking sa- gittal crest; 22) epiotic eminences obso- lete; 26) squamosal-maxillary angle Figure 89. Lateral, dorsal, and ventral views of skull of Crossodactylodes pintoi (paratype, USNM 120611, X 8). LYNCH: LEPTODACTYLOID FROGS 137 about 45°; 27) columella absent; 28) prevomers small, edentate, dentigerous rami almost completely lost, widely sep- arated medially; 29) palatines narrow, widely separated medially, lacking odon- toid ridges; 30) sphenethmoid entire, ex- tending anteriorly beneath nasals; 31) anterior ramus of parasphenoid broad, not keeled; 32) parasphenoid alae ori- ented at right angles to anterior ramus, narrowly overlapped laterally by median rami of pterygoids; 33) pterygoids rela- tively small, anterior rami extending to middle of orbit, ventral pteiygoid flange small; 36) terminal phalanges Y-shaped, lateral processes long and slender; 37- 39); 42) males with median subgular vocal sac; males with cluster of spines on thumb; 43) body lacking glands; 44) tongue oval, posterior one-third free, non-boletoid; 45) toes not webbed, lack- ing lateral fringes, outer metatarsal tu- bercle present, inner metatarsal tubercle not enlarged and spade-like, digital tips enlarged into pads, first finger shorter than second; 46) tadpoles semi-aquatic; 48 ) eggs large, few in number, deposited in terrestrial bromeliads; 49) males 15- 17.5 mm. SVL; 50) tympanum absent ( not hidden, as stated by Cochran, 1938, 1955). Composition. — Monotypic. Distribution. — The Coastal Ranges of Guanabara and Espirito Santo, Brasil. Remarks.— Cochran (1938, 1955) considered Crossodactylodes to be re- lated to Crossodactyhis (Elosiinae). She based her opinion on the presence of a cluster of spines on the thumbs of the males of both genera and the erro- neous opinion that both genera have der- mal glands on the top of each digital pad. Cochran noted that when the digi- tal tips of Crossodactylodes were dried out, a weak furrow appeared in the cen- ter of the digital pad; she considered this condition a precursor of the condition seen in elosiines (distinct dermal glan- dular pads). The apparent glands ob- served by Cochran are an artifact result- ing from the presence of Y-shaped ter- minal phalanges. Cochran pointed out that the two genera shared the loss of pre vomerine teeth; the pre vomerine bones are much smaller in Crossodacty- lodes than in Crossodactyhis, which usually has larger prevomerine dentiger- ous processes and rarely prevomerine teeth. The architecture of the temporal re- gion and the size of the roofing bones of Crossodactylodes are like the condition seen in Cycloramphus and Zachaenits. The other cranial characters of Crosso- dactylodes are not contrary to the condi- tions which obtain in Cycloramphus and Zachaenus, although Crossodactylodes is separable from these two genera by many skull characters. The data on breeding biology were provided by Werner Bokermann (in litt.) and suggest that Crossodactylodes is more closely re- lated to Cycloramphus and Zachaenus than to the Eleutherodactylini, which it resembles in many osteological features. Cycloramphus Tschudi, 1838 (Fig. 90) Cycloramphus Tschudi, 1838, Classif. Batr., p. 81 [Type-species by monotypy, Cycloram- phus fulginosiis Tschudi, 1838]. Cyclorhamphus Agassiz, 1846, Nomencl. Zool., index, p. 110 [Emendation of Cycloramphus Tschudi, 1838, hence taking same type- species]. Pithecopsis Giinther, 1859, Cat. Bat. Sal. British Mus., p. 22 [Type-species by monotypy, Pithecopsis fulifiinosus (Tschudi, 1838)]. Grypiscus Cope, 1867, J. Acad. Nat. Sci. Phila- delphia, (2)6:206 [Type-species by mono- typy, Grypiscus ui>ihrinus Cope, 1867]. lliocliscus Miianda-Ribeiro, 1920, Rev. Mus. Paulista, 12:267 [Type-species by subse- quent designation (Bokermann, 1951), Telmatohius hrasiliensis Steindachner, 1864; his designation is hereby rejected (see "Re- marks" ) and the type-species is here desig- nated as lliocliscus cluhius Miranda-Ribeiro, 1920]. Niedenia Ahl, 1923, Zool. Anz., 58:107 [Type- species by monotypy, Niedenia spinulifer Alil, 1923]. Diagnostic definition. — 7 ) omoster- num moderate-sized; 8) sacral dia- pophyses rounded to very slightly di- lated; 10) alary processes of premaxillae 138 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 90. Lateral, dorsal, and ventral views of skull of Cycloramphus eletitherodactijlus (KU 92785, X 3.6). directed posterodorsally, relatively broad at base; 11) palatal shelf of premaxilla of moderate depth, not notched, palatal process short; 13) palatal shelf of maxil- la relatively narrow, pterygoid process large; 16 ) nasals in contact with maxillae, not with pterygoids; 19) frontoparietals not ornamented, bearing large sagittal crest; 22) epiotic eminences prominent posteriorly, obsolete anteriorly; 26 ) squa- mosal-maxillary angle less than 43°, measurement difficult because of curva- ture of both elements; 27) columella present; 28) prevomers present, entire, moderately large, toothed, separated medially; 29) palatines broad, widely separated medially, bearing small odon- toid ridges; 30) sphenethmoid entire, extending anteriorly beneath nasals, not visible dorsally or only a small area visi- ble between junctions of nasals and fron- toparietals; 31) anterior ramus of para- sphenoid broad, not keeled; 32) para- sphenoid alae oriented at right angles to anterior ramus, broadly overlapped by median rami of pterygoids; 33) ptery- goids relatively small, anterior rami ex- tending to middle of orbit, pterygoids bearing large ventral flange — cf. Fig. 25; 36) terminal phalanges knobbed; 42) males with median subgular vocal sac; males lacking nuptial asperities except for C. ohausi which has a cluster of spines on each thumb; 43) inguinal glands present; 44) tongue large, round, semi-boletoid; 45) toes free of webbing, bearing lateral fringes, or partly to fully webbed, outer metatarsal tubercle pres- ent, inner metatarsal tubercle not en- larged and spade-like, digital tips nar- row, first finger not longer than second; 46) larvae with very brief tadpole stage, semi-aquatic, vent median, 1/1 tooth rows, labial papillae broadly interrupted anteriorly; 48) eggs laid in moist ter- restrial situations, hatch near end of lar- val period, eggs large, few in number (Lutz, 1929); 49) adults 30-55 mm. SVL; 50) tympanum concealed. Composition. — Seven to nine species are recognized depending on the author. Gorham (1966) listed eight species — LYNCH: LEPTODACTYLOID FROGS 139 asper, cUringshoefensi, eleutherodactylus, ftilginosiis, gramdosus, neglectus, ohausi, and iimhrinus, whereas Bokerniann (1966) recognized houlengeri, diiJ)ius, and pinderi as valid (which Gorham considered synonyms of other names) and placed timhrinus in the synonymy of ftdginosus. The most recent revision of the genus is that of Bokerniann ( 1951 ) , although Cochran ( 1955 ) studied a large part of the genus. In view of the differ- ences of opinion as to how many, and which, species are valid, a thorough ge- neric review is desirable. Distribution. — Forested habitats in southeastern Brasil. Remarks. — Within comparatively re- cent times ( Miranda-Ribeiro, 1926, Noble, 1931), the genus Cycloramphus was divided into three genera (Cyclo- ramphus, Grypiscus, and Iliodisctis). Bokermann (1951) and Cochran (1955) combined the three into a single genus. Cochran (1955) suggested that the ge- nus is heterogeneous because C. ohausi mitigates some of the differences be- tween Ceratophrys, Cycloramphus, and Crossodactyhis. Her statements reflect a philosophy of single-character classifica- tion and do not accurately indicate the homogeneity of the genus Cycloram- phus. The generic partitioning of Cyclo- ramphus was based on the variation in webbing of the toes and Cope's argu- ment that the presence of pseudoteeth on the lower jaw of umbrinus justified generic distinction. I have not observed odontoids on the lower jaw of any spe- cies of the genus, although Noble (1922) figured a serrate lower jaw of a cotype of umbrinus. Six species of the genus (asper, diringshoefensi, dubius, eleu- therodactylus, granulosus, and pinderi) lack webbing or lateral fringes on the toes; three species (boidengeri, fidgino- sus, and neglectus) have one-half to fully webbed toes. The two gi'oups are bridged by ohausi which has basal webbing and lateral fringes on the toes. The basal webbing probably is best re- garded as the broadened junction of the fringes. I consider the lack of webbing to be primitive, because the allied Za- chaenus lacks webbing. Bokermann (1951) designated Telma- tobius hrasiliensis Steindachner (=zCy- cloramphus fulginosus) as the type-spe- cies of Iliodiscus Miranda-Ribeiro, 1920. This action rendered Iliodiscus a strict synonym of Cycloramphus. However, Miranda-Ribeiro (1920) placed the webless species of Cycloramphus in Iliodiscus; Telmatobius brasiliensis was included in Cycloramphus, not Iliodis- cus, and therefore cannot be considered for subsequent designation as the type- species of Iliodiscus. Accordingly, Bok- ermann's ( 1951 ) restriction is hereby rejected. Miranda-Ribeiro (1920) in- cluded four nominal species in Iliodiscus (dubius, eleutherodactylus, pinderi, and semipalmatus). Gorham (1966) listed dubius as the type-species. I designate /. dubius Miranda-Ribeiro, 1920, as the type-species of Iliodiscus Miranda-Ri- beiro, 1920. Zachaenus Cope, 1866 (Figs. 91-93) Zachaenus Cope, 1866, J. Acad. Nat. Sci. Phila- delphia, 6:94 [Type-species by original designation, Cystignathus parvulus Girard, 1854]. Oocormus Boulenger, 1905, Ann. Mag. Nat. Hist., (7)16:181 [Tyi^e-species by mono- typy, Oocormus microps Boulenger, 1905]. Craspedoglossa L. Miiller, 1922, Blatter Aquar. Terr., 33:167 [Type-species by monotypy, Craspedoglossa sanctaecatharinae L. Miiller, 1922]. Diagnostic definition. — 7) omoster- num relatively large; 8) sacral dia- pophyses rounded; 10) alaiy processes of premaxillae directed sharply posterodor- sally, relatively broad at base; 11) pala- tal shelf of maxilla relatively deep, not notched, palatal process moderate-sized; 13) palatal shelf of maxilla of moderate width, pterygoid process lacking; 16) nasals in contact with maxillae, not with pterygoids; 19) frontoparietals not orna- mented except for prominent sagittal crest and supraorbital processes; 22) 140 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 91. Dorsal, lateral, and \'entra] views of skuW oiZachaemisparvulusiKU 107090, X 7.5). epiotic eminences obsolete; 26) sqiia- mosal-maxillary angle about 45°; 27) columella present; 28) prevomers rela- tively large, entire, toothed, narrowly separated medially; 29) palatines slen- der, widely separated medially, no odon- toid ridges; 30) sphenethmoid entire, usually not visible dorsally; 31) anterior ramus of parasphenoid narrow, not keeled; 32) parasphenoid alae oriented at right angles to anterior ramus, broadly overlapped laterally by median rami of pterygoids; 33) pterygoids relatively small, anterior rami extending to middle of orbit, large ventral flange; 36) termi- nal phalanges knobbed; 42) males with median subgular vocal sac; males lack- ing nuptial asperities; 43) body lacking glands; 44) tongue round, semi-boletoid; 45) toes lacking webbing and lateral fringes, outer metatarsal tubercle pres- ent, inner metatarsal tubercle enlarged, not spade-like, digital tips narrow, first finger as long as second; 46) develop- ment abbreviated, tadpole semi-aquatic, vent median, 1/1 tooth rows, labial pa- pillae broadly interrupted anteriorly (Lutz, 1944); 48) eggs large, few in number, deposited in moist, terrestrial situation, larvae hatch and remain in Figure 92. Dorsal, lateral, and ventral xiews of skull of Zachaenus stejnegeri (KU 92742, X 7.5). LYNCH: LEPTODACTYLOID FROGS 141 Figure 93. Body outlines and sides of heads of (A-B) Zachaeniis stejnegeii (KU 92744) and (C-D) Z. parvtilus (KU 93078). All X 2. gelatinous mass until metamorphosis; 49) adults less than 30 mm. SVL; 50) tympanum concealed. Composition. — The nominal species of Craspedoglossa (holitoglossa, sanctae- cathorinae, and stejnegeri) and of Za- chaeniis (parvidus, roseus, and sawaijae). Bokermann (1966) considered sanctae- catharinae to be a synonym of bolitoglos- sus. I do not consider roseus or sawayae members of this genus ( see Remarks ) . Distribution. — Southern and south- eastern Brasil. Remarks. — Lutz (1944) demonstrated that Oocormus microps is a synonym of Zachaenus parvidus. Parker (1926) noted the striking similarities in color pattern and proportions between Oocor- mus microps (^Zachaenus parvulus) and SmintluUus hrasiUensis (=Eupark- erella), which occur sympatrically in southeastern Brasil. Boulenger ( 1905 ) confused them and included Euparker- ella in the syntypic series of Oocormus microps as juvenile specimens. The two genera belong to different ti-ibes and can be distinguished externally only by the shape and lengths of the fingers and toes (Fig. 94). Craspedoglossa is here placed in the synonymy of Zachaenus for the first time. Cochran (1955) pointed out that the two nominal genera might be best combined but separated them on the basis of the axillary patagium of Zachae- FiGURE 94. Hands of three frogs of the Telmato- biinae. (A) Zachaenus parvulus (KU 93078, X 4), (B) Euparkerella hrasiUensis ( KU 112370, X 6.6), and (C) Scydirophnjs sawayae (USNM 125530, X 6.6). 142 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY nus (see Fig. 93). Tehnatohufo is the only other leptodactyHd with an axillary patagium, although the loose, "baggy" skin of Batrachophnjmis and the sti-ictly aquatic Tehnotohius produces a poorly defined patagium. The snout is more sloping in Zachaenus parvitlus than in Craspedoglossa (sensu strictu). The axil- lary patagium is used as a species-group character in other groups of frogs (for example, the Hijla marmorata and H. godmani groups), and is best regarded as a species-group character here as well. In all other characters used in the generic diagnoses, Craspedoglossa and Zachaenus are identical. Cope (1890) named a second species of the genus (roseiis) based on a single specimen from Port Otway, Patagonia; the unifiue holotype is now a macerated heap of fragments (Cochran, 1955, 1961b). The original description in- cludes several points that clearly disasso- ciate roseiis from Zachaenus (tympanum visible, tongue not boletoid, prevomerine dentigerous processes small and round, outer metatarsal tubercle lacking, and toes fringed). The osteological data provided by Cope (nasals small, widely separated medially, and frontoparietals complete, i.e., no fontanelle) and those observed by me (pterygoid lacking ventral flange, zygomatic ramus of squa- mosal short and straight otic ramus of squamosal not curved medially but ex- panded medially into small otic plate) clearly disassociate roseus from Zachae- nus. Unfortunately, the present data are insufficient for generic assignment. Za- chaenus roseus Cope is tentatively con- sidered a species inquirenda in the fam- ily Leptodactylidae, probably in the Tel- matobiinae. Cochran (1953) named a single spec- imen of a frog from Parana, Brasil, as a third species of Zachaenus (saivayae). The species is clearly not a Zachaenus, although its relationships are not appar- ent; only the holotype is known, and no osteological observations can be made. Zachaenus sawayae is considered by me to be the type-species of a new genus of the Telmatobiinae; the tribal relation- ships are not apparent. The new genus is named at the end of the account of the Telmatobiinae. Eleutherodactylini Lutz, 1954 Eleutherodactylinae Lutz, 1954:175. Lutz (1954) proposed this subfamily for the inclusion of Eleutlierodactyhis alone; as was the case with the Cyclo- rhamphinae, she did not provide any diagnostic statements for the new group. Gallardo (1965) included Basanitia, Ctenocranius, Eleutherodactyhis, Micro- hairachyhis, and Syrrliophus in the Eleu- therodactylinae. I include the following genera in the tribe Eleutherodactylini: Amhhjphryniis, Eleutherodactyhis, Eu- parkereUa, Holoaden, Hylactophryne, Ischnocnema, Niceforonia, Sminthillus, Syrrhophus, and Tomoductylus. The nominal genera Basanitia, Nohlella, Phrynanodus, and Trachyphrynus are considered to be synonyms of Eleuthero- dactyhis (Lynch, 1968c, 1968d). The nominal genera Nohlella Barbour and Pseudohyla Andersson are considered to be synonyms of Eleutherodactyhis (see below ) . The following diagnostic characteris- tics are the same in all of the included genera: 3) tranverse processes of pos- terior presacral vertebrae not shortened; 4) cervical cotylar arrangement type I; 5) cervical and second vertebrae not fused; 8) sacral diapophyses rounded; 9) maxillary arch usually toothed, if toothed, teeth blunt, pedicellate; 14) maxillary arch complete, maxillae taper- ing posteriorly, quadratojugal shallow; 17 ) nasals not in contact with frontopari- etals; 18) frontoparietal fontanelle usual- ly absent; 21) temporal arcade lacking; 23) carotid artery passes dorsal to skull bones; 41) pupil horizontal; 42) males lacking nuptial asperities; 45) outer metatarsal tubercle present, inner meta- tarsal tubercle not spade-like; 46) de- velopment direct in known species; 47) amplexus axillary in known species; 48) LYNCH: LEPTODACTYLOID FROGS 143 eggs relatively large, few in number, de- posited in terrestrial situations, brome- liads, etc., in all known species. Except for the nature of the T- shaped terminal phalanges, the skeleton of the eleutherodactylines is relatively generalized. The sternum is cartilagi- nous, an omosternum is usually present and relatively large, the cervical cotyles are widely separated medially, the trans- verse processes of the presacral vertebrae are neither greatly expanded nor short- ened, the sacral diapophyses are rounded or only sHghtly dilated, the ilia are of the leptodactyline type, all cranial bones are present although a few species have lost the prevomerine bones or the colu- mellae. The cranial bones are not der- mostosed but exostosis is developed in several groups. The nasals are large and usually in median contact, and the fron- toparietal fontanelle is rarely developed. There is considerable variation in the size and shape of the zygomatic ramus of the squamosal among the genera and species of this tribe, and most of the variation is observed within Eleuthero- dactyhis. Morphologically, the tribe Eleuthero- dactylini is difficult to define. The rela- tionships of ten genera I include in this tribe are not entirely obvious. The defi- nition of the group rests solely on the mode of reproduction, and the included genera are judged to be related because the various sections of the tribe can be tied together through the use of several different character complexes. Species of the following genera are known to lay terrestrial eggs and to lack a free tadpole stage: Eleutherodactylus, Holoaden, Hy- lactophryne, Sminthillus, Syrrhophus, and Tomodactylus. Euparkerella and Niceforonia probably lay large terrestrial eggs, judging from the size of mature eggs and the oviducts. Reproductive data are not available for Amhlyphrynus and Ischnocnema. Females of the latter genus have moderately large, unpig- mented eggs, but the eggs are not so large as to be suggestive of direct devel- opment. However, the eggs of Ischno- cnema are no smaller than those of Eleu- therodactyJus maussi, which exhibits di- rect development (Heatwole, 1962). Eleutherodactylus, Sminthillus, Syrrho- phus, and Tomodactylus have broadly T-shaped terminal phalanges. The ter- minal phalanges of Euparkerella are broad and small, but could not be accu- rately described as T-shaped. The ter- minal phalanges of the other five genera (Amhlyphrynus, Holoaden, Hylacto- phryne, Ischnocnema, and Niceforonia) of the tribe are knobbed. Amhlyphrynus bears considerable resemblance to the Eleutherodactylus cornutus group and differs only in the nature of the terminal phalanges. Hylactophryne and Ischno- cnema bear considerable resemblance to one another and to the Eleutherodacty- lus hinotatus and guentheri groups; these genera also differ only in the nature of the terminal phalanges. Niceforonia is superficially similar to Eupsophus and to the Eleutherodactylus unistrigatus com- plex (several species groups are in- volved). Niceforonia differs from Eup- sophus in several osteological characters as well as in reproductive pattern, but differs from the Eleutherodactylus uni- strigatus complex only in the nature of the terminal phalanges. Holoaden is not obviously related to any group of Eleti- therodactylus, but is osteologically simi- lar to Niceforonia. Amhlyphrynus Cochran and Coin, 1961 Amhhjphnjnus Cochran and Coin, 1961, Fieldi- ana, Zool., 39:543 [Type-species by orig- inal designation, Amhhjphnjnus ingeri Coch- ran and Coin, 1961]. Diagnostic definition. — 7 ) omoster- num present; 9) maxillary arch toothed; 10) alary processes of premaxillae di- rected posterodorsally; 11); 12) facial lobe of maxilla deep, not exostosed; 13); 15) nasals large, in broad median con- tact; 16) nasals in tenuous contact with maxillae, not in contact with pterygoids; 19) frontoparietal bears large, well de- fined, exostosed, lateral crests; 20); 22) 144 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY epiotic eminences obsolete; 23) cristae paroticae long, narrow; 24) zygomatic ramus of squamosal of moderate length, widely separated from maxilla; 25) otic ramus of squamosal short, not expanded medially into otic plate; 26); 27) colu- mella present; 28) prevomers large, en- tire, toothed, in median contact; 29) palatines large, narrowly separated me- dially; 30) sphenethmoid entire, extend- ing anteriorly beneath nasals; 31) an- terior ramus of parasphenoid broad, not keeled, pointed anteriorly; 32) para- sphenoid alae oriented at right angles to anterior ramus, broadly overlapped lat- erally by median rami of pterygoids; 33 ) pterygoids of moderate size, lacking ven- tral flange, anterior rami not reaching palatines, median rami long; 34) occip- ital condyles large, not stalked, widely separated medially; 36) terminal pha- langes knobbed; 37-40); 42); 43) body lacking glands; 44) tongue large, round, posterior edge free; 45) toes free of webbing, digital tips narrow; 46-48); 49) the two known specimens are 51.5 and 83.0 mm. SVL; 50) tympanum visi- ble externally. Composition. — Monotypic. Distrihiition. — Known from two lo- calities in the Andes of central Colombia (850-2350 meters). Peracca's (1914) record of an Eleutlierodacti/ltis cornutiis from the highlands in Departamento Antioquia, Colombia, may refer to this species. Remarks. — Cochran and Coin ( 1961 ) suggested that AmhJijphnjnus is a mem- ber of the "broad-headed leptodactylid" group which includes the ceratophryine genera, Proceratophrys, and Zachaenus. They suggested that Amhiijphnjnus was probably most closely related to Zaclme- nus. The resemblance between these two genera is spurious. This association can only be made by comparison of de- scription of characters and will not bear up against specimen comparison or the additional osteological characteristics. The suggestion that this species is allied with the ceratophryine leptodactylids is contradicted by the lack of morphologi- cal agreement between the two groups. The ceratophryines have large, casqued skulls with extensive dermostosis and exostosis, a distinctly different type of cervical-occipital articulation, non-pedi- cellate teeth, expanded transverse proc- esses of the anterior presacral vertebrae and shortened transverse processes of the posterior presacral vertebrae, and a dermostosed vertebral shield. In many respects, Amblyplirynus re- sembles the large-headed frogs of the Eleiitlwrodactyhis cornutus group. The holotype of Amhlyphrynus ingeri was first reported by Dunn ( 1944 ) as an EleutJierodactylus cornutus. The only characteristic separating these two groups is the nature of the terminal pha- langes. When additional specimens of A. ingeri become available an effort must be made to determine if the terminal phalanges of the hind feet are knobbed or T-shaped. As pointed out previously, the terminal phalanges of the fingers may be knobbed and those of the toes T-shaped. This pattern is observed in several groups of Eleutherodactylus. The only specimens of this species available were studied through the use of stereo-radiographs. Eleutherodactylus Dumeril and Bibron, 1841 (Figs. 95-99) Cornufcr Tschudi, 1838, Classif. Batr., p. 28 [Type-species by monotypy, Cornufer uni- color Tschudi, 1838 {=Eleutherodactijlus inoptatus) . Suppression of Tschudi's names was requested by Zvveifel ( 1966)]. Elentherodactijlus Dumeril and Bibron, 1841, Erp. gen., 8:620 [Type-species by mono- typy, Hylodes rnaiiinicensis Tschudi, 1838. Myers ( 1962 ) Hsted the type-species desig- nation as l)y original designation. The name Elciitherodactyhis was included in the syn- onymy of Hylodes martinicensis by Dume- ril and Bibron (1841). Apparently they had planned to use the generic name in their £rpetoIogie generate until Tschudi (1838) named their martinicensis in the genus Hylodes]. Hylodes Fitzinger (non Hylodes Fitzinger, , 1826), 1843, Syst. Rep., p. 31 [Type-species i LYNCH: LEPTODACTYLOID FROGS 145 by original designation, Hijlodes martinicen- sis Tschudi, 1838]. Euhyas Fitzinger, 1843, Ibid., p. 31 [Type- species by original designation, Hylodes ricordii Dumeril and Bibron, 1841]. Crau'^astor Cope, 1862, Proc. Acad. Nat. Sci. Philadelphia, p. 153 [Type-species by sub- sequent designation ( Dunn and Dunn, 1940), Hijlodes fltzingeri O. Schmidt, 1858]. Strahomantis W. Peters, 1863, Mtber. k. Preuss. Akad. Wiss., Berlin, p. 405 [Type-species by monotypy, Strahomantis biporcatus W. Peters, 1863]. Leitjla Keferstein, 1868, Ark. Naturges., 34:296 [Type-species by monotypy, Leiyla guen- therii Keferstein, 1868]. Liijla Cope, 1870, Proc. Amer. Philos. Soc, 11: 160 [Emendation of Leiyla Keferstein, 1868]. himnophys Jimenez de la Espada, 1870, J. Sci. Math., Phys. Nat. Lisboa, 3:59 [Type- species by subsequent designation ( Myers, 1962), himnophys cornutus Jimenez de la Espada, 1870]. Pristimantis Jimenez de la Espada, 1870, Ibid., 3:61 [Type-species by monotypy, Pristi- mantis galdi Jimenez de la Espada, 1870]. Cyclocephalus Jimenez de la Espada, 1875, Vert. Viaje Pacif., Batr., pi. 3 [Type-species by monotypy, Cyclocephalus lacrimosus Ji- menez de la Espada, 1875]. Hypodictyon Cope, 1885, Proc. Amer. Philos. Soc, 22:383 [Type-species by original des- ignation, Phyllobates ridens Cope, 1866]. Liohyla Cope, 1894, Ibid., 31:335 [Emendation of Leiyla Keferstein, 1868]. Basanitia Miranda-Ribeiro, 1923, Rev. Mus. Paulista, 13:851 [Type-species by mono- typy, Basanitia lactea Miranda-Ribeiro, 1923]. Noblella Barbour, 1930, Zoologica, 11:81 [Type-species by original designation, Sminthillus peruvianus Noble, 1921]. Phrynanodus Ahl, 1933, Zool. Anz., 104:29 [Type-species by monotypy, Phrynanodus nanus Ahl, 1933]. Teletrema Miranda-Ribeiro, 1937, O Campo (Rio de Janeiro), 8 (89): 67 [Type-species by monotypy, Teletrema heterodactylum Miranda-Ribeiro, 1937]. Microbatrachylus Taylor, 1940, Univ. Kansas Sci. Bull., 26:499 [Type-species by original designation, Eleutherodactylus hobartsmithi Taylor, 1936]. Ctenocranius Melin, 1941, Medd. Goteborgs Mus. Zool. Avd., 88:49 [Type-species by subsequent designation (Myers, 1962), Lirmwphys cornutus Jimenez de la Espada, 1870]. Pseudohyla Andersson, 1945, Ark. Zool., 37A: 86 [Type-species by monotypy, Pseudohyla nigrogrisea Andersson, 1945]. Trachyphrynus Coin and Cochran, 1963, Proc. California Acad. Sci., 31:502 [Type-species by original designation, Trachyphrynus myersi Coin and Cochran, 1963]. Diagnostic definitioti. — 7) omoster- num usually present, small, medium- sized, or large, long and narrow or rela- FiGURE 95. Lateral and dorsal views of skull of Eleutherodactylus sulcatus (KU 100355, X 2.4). tively broad, absent in at least one spe- cies— E. ruthae; 9) maxillary arch toothed; 10) alary processes of premaxil- lae relatively broad at base, direction variable — dorsal, dorsolateral, or pos- terodorsal; 11) palatal shelf of premaxil- FiGURE 96. Lateral and dorsal views of skull of Eleutherodactylus diastema (KU 68263, X 6). 146 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY la deep, usually deeply dissected; 12) fa- cial lobe of maxilla deep, usually not exostosed; 13) palatal shelf of maxilla broad, usually with prominent pterygoid process; 15) nasals large, in broad me- dian contact, narrowly separated in some species; 16) nasals not in contact with pterygoids, sometimes in contact with maxillae; 18) frontoparietal fontanelle absent in adults except in E. pahneri and E. lohymperi; 19) frontoparietals not ornamented in most species groups, but bearing lateral crests in biporcattis, cor- mitus, galdi, and iinlstrigatus complexes; 20) frontoparietals fused with prootics or not. The bones are fused in most species in the West Indies and northern Andes, free in other groups; 22) epiotic eminences prominent to obsolete — group variable; 23) cristae paroticae short and stocky to long and narrow; 24) zygo- matic ramus of squamosal short to long, sometimes knobbed, in contact with maxilla in one species (rutliae); 25) otic ramus of squamosal short to long, usual- ly forming a small otic plate, orna- mented in a few species groups — notably the galdi group; 26) squamosal-maxil- lary angle 44-67°, most 50-60°; 27) colu- mella present; 28) prevomers nearly al- ways toothed, entire, narrowly separated medially to broadly separated medially; 29) palatines long, usually expanded lat- erally, relatively widely separated me- dially, no odontoid ridges; 30) spheneth- moid entire, extending anteriorly be- neath nasals variable distance; 31) an- terior ramus of parasphenoid narrow to broad, relatively long, nearly reaching prevomers, not keeled medially; 32) parasphenoid alae in two patterns: 1. alae deflected posteriorly, short, not overlapped laterally by median rami of pterygoids, and 2. alae oriented at right angles to anterior ramus, rarely deflected posteriorly, long, broadly overlapped by median rami of pterygoids. The first pat- tern is seen in West Indian species and some Andean species, whereas the sec- ond is seen in Central American and lowland South American species; 33) pterygoids slender to relatively massive, lacking ventral flange, anterior rami relatively short, not reaching palatines, median rami short to long, straight or bent; 34) occipital condyles relatively small, stalked or not, widely separated medially; 36) terminal phalanges nearly always clearly T-shaped, inner phalan- ges usually knobbed, terminal phalanges Figure 97. Dorsal views of the skulls of Eleutherodactylus conspicillattis (KU 108988, X 4.5) and E. planirostris (KU 92656, X 4.5). Arrows point to prevomerine teeth which are visible in dorsal view. LYNCH: LEPTODACTYLOID FROGS 147 Figure 98. Lateral views of skulls of Eletithew- dacitihis. (A) platuwstm (KU 92656, X 6), (B) ^aldi (USNM field GOV 8944, X 6), and (C) ruthae ( AS 4237, X 2). of toes more T-shaped than those of fingers; presence of T-shaped terminal phalanx is expressed externally by the presence of a terminal transverse groove across the tip of the digital pad; 37) alary processes of hyoid plate on narrow stalks; 40) m. depressor mandibukie in one slip in E. galdi, in one slip with sep- aration into two slips dorsally in species of hiporcatus and cornutus groups, or in two large slips in most species; 42) males with single subgular vocal sac or none, internal or external; 43) glands on body usually absent, those present are usually loosely organized inguinal glands; 44) tongue long and narrow to large and round, posterior edge usually free; 45) toes free of webbing to nearly fully webbed; when webbing is present, it is indicative of a close association with streams, webbing is greatest in anoma- lus, karhchmidti, punctariohis, and rani- formis, although several species of the rugulosiis group in Central America have the toes one-half webbed; digits usually bear large pads; 49) adults range from 12-100-|- mm. SVL; 50) tympanum ab- sent in anotis, concealed in many species, visible externally in most species. Composition. — Gorham (1966) listed nearly 300 species in the most recent compilation of names in the genus. Al- bert Schwartz informed me that there are 100 species in the West Indies (in- cluding Trinidad). My own estimate is that the genus contains about 400 spe- cies, many yet unnamed. Distribution. — Sinaloa and Tamau- lipas, Mexico (but not on the Mexican Plateau) southward and eastward throughout Middle America to northern Argentina and southern Brasil; all West Indian islands; introduced into Florida. Remarks. — Myers (1962) discussed the generic synonymy of this genus and included most of the generic synonyms listed above as well as Sijrrhophus and Lithodytes in the synonymy of Eleti- FiGURE 99. Dorsal views of skulls of (top) Eleiithewdactyhts btifoniformis ( KU 80621, X 2) and E. palmcri (KU 110923, X 3). 148 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY thewdactijhis. Microhatmchijlus was synonymized by Lynch (1965), and he later (1968c, 1968d) considered Bamni- tia, Phnjnanodus; and Traclujphnjmis inseparable from Eleutlierodactijlus. Two generic synonyms are added at this time: NohJello Barbour and Pseu- dohyla Andersson. Noble (1921) named Smint]}iUiis penwiami.s on the basis of several specimens of a minute frog with an anterior epicoracoidal fusion (the distinguishing character of the genus). At the time of the description of peru- vianus, the genus SminthiUus was known only from Cuba, but with the description of a species from southeastern Brasil by Parker (1926), it began to appear that SminthiUus was a widespread, Neotropi- cal genus of small frogs. Noble ( 1926b, 1931) suggested that Sminthilhis was de- rived from Eleiitherodactyliis or Sijrrho- phus but placed it in another family ( Brachycephalidae ) . Griffiths ( 1959 ) placed each of the three species of Sminthilhis in a separate genus, utilizing Barbour's (1930) NohleUa ior peruviana. Barbour (1930) proposed Nohlella for peruviana because the Cuban species was geographically remote from the two South American species and because he believed SmintluUus to be a PJujUobates (Dendrobatidae). Griffiths offered a new generic name, Euparkerelh, for the Brasilian species. Etiparkerella, while here retained as an eleutherodactyline, is very distinct from all other genera of the tribe and subfamily. SminthiUus is retained as a genus of eleutherodacty- lines on less secure grounds — the maxil- lary teeth are absent. NohleUa peruvi- ana, on the other hand, has maxillary teeth, although it apparently has no pre- vomers. The single specimen of this species available to me cannot be gener- ically separated from EJeutherodactylus; an epicoracoidal bridge is not, in my opinion, sufficient basis for the mainte- nance of an otherwise undefinable ge- neric group ( see discussion on page 59 ) . NohleUa therefore is placed in the syn- onymy of Eleutherodactylus. This action creates one minor problem — Noble's peruvianus was proposed in 1921, but Melin ( 1941 ) proposed a Hylodes peru- vianus which becomes a secondary hom- onym of Noble's name. Rather than propose a replacement name for a prob- ably invalid species, I suggest that Me- lin's name be kept in mind by the person who eventually studies the conspicillatus group in the Amazon Basin of Peru. Andersson (1945) proposed Pseudo- hyla as a hylid genus, but having studied the holotype of P. nigrogrisea, I do not consider the genus separable from Eleu- therodactylus (Lynch, 1969a). Eleu- therodactylus nigrogriseus is a small spe- cies of the genus and has been found in the valley of the Rio Pastaza and on the slopes of the Cordillera Due in eastern Ecuador. The genus Eleutherodactylus is a large and unwieldy one, although Hyla and possibly Rana are more unwieldy at present. In contrast to the latter two genera (and perhaps to the opinions of several herpetologists) the genus Eleu- therodactylus is marked by considerable homogeneity. There is a large range of sizes among the species; most species lack webbing between the toes but some have it, including one species with fully webbed feet (E. karlschmidti). Exostosis of the cranial bones is developed in sev- eral species groups but in general the phenomenon is an uncommon trait in the genus. Some species have minute digi- tal pads and only small lateral projec- tions of the terminal phalanges on the hands, but all species have moderate to large T-shaped terminal phalanges on the toes (see pp. 65-66 for further dis- cussion ) . Three characters exhibit especially interesting variation in Eleutherodacty- lus— 1) fusion of the frontoparietal and otoccipital bones; 2) degree of overlap of the parasphenoid alae and median rami of the pterygoids; and 3) median separation of the prevomers. On the basis of the variation in these characters, the species of the West Indies and parts LYNCH: LEPTODACTYLOID FROGS 149 of the Andean system form one group and the species of Mexico, Central America, and lowland South America form a second group. These characters are discussed below. Baldauf and Tanzer ( 1965 ) im- proved our knowledge of leptodactylid skulls with the description of the cra- nium of SyrrJiopJms maniockii. In this work they pointed out the fusion of the frontoparietal and prootic in this species. These bones are fused in all species of Syrrlioplnis and Tomodactyltis, whereas they are not fused in the Eleutlwrodoc- tylus of Mexico and Middle America. Although fewer than one-third of the species of Eleutherodactylus have been studied for this character, I feel that I have checked a sufficiently representa- tive sample in that I have examined spe- cies from all parts of the range of the genus. Fusion of the frontoparietal and prootic ( otoccipital, since the prootic is usually fused with the exoccipital) oc- curs in the species of the genus found in the West Indies from Bermuda and the Bahamas (and Florida) to Trinidad. The species of the Hispaniolan inoptatiis group {inoptatiis and nifhae examined) as well as the Puerto Rican karhchmidti apparently have the two bones free. At least some (perhaps all) of the species of the Andean groups exhibit fusion of these bones. No species was examined from the Andes south of Ecuador, All species of the genera Syrrhophus and Tomodoctyhis as well as SmintJiiUiis ex- hibit the fusion. No species of Eleu- therodactylus in Mexico or Central America normally exhibits frontoparietal- prootic fusion (see below), nor do spe- cies of the genus found in Chocoan Co- lombia and Ecuador. Insofar as I am aware, no species found in the Amazon Basin exhibits the fusion nor do the rep- resentatives of the genus in southeastern Brasil. Some variability was noted. One specimen of E. fitzingeri (JDL S-407) exhibited fusion of the frontoparietal and otoccioital bones whereas the other nine specimens examined did not. One of three specimens of E. cldoronotus examined exhibited the fusion. Two of the 19 specimens of E. curtipes examined did not exhibit fusion of these bones; both were small specimens, suggesting that the fusion is an ontogenetic phenomenon. In the cases of the first two species, I regard the fusion as aberrant. In each instance, the frontoparietals, nasals, pre- vomers, and parasphenoid were bound to the sphenethmoid and otoccipitals with no apparent sutures. This suggests that the fusion in these cases resulted from extensive calcification rather than osteological fusion. The degree of overlap between the median rami of the pterygoids and para- sphenoid alae follows the same pattern as the frontoparietal-prootic fusion with some departure. The median pterygoid rami of the rhodopis group of Eleuthero- dactylus are short and bent so that there is no actual contact between the ptery- goid and parasphenoid, but the median ramus of the pterygoid abuts against the otic capsule just above the parasphenoid ala. In the majority of species of the genus, the median ramus is broadly in contact with the anterior edge of the parasphenoid ala or the median ramus is shortened and may or may not reach the otic capsule and does not reach the shortened parasphenoid ala. In those species with a pterygoid-parasphenoid overlap, the frontoparietals and prootic bones are free. The members of the rhodopis complex of Eleutherodactylus have the bent pterygoid and hence do not have a typical pterygoid-parasphe- noid overlap but because the median rami of the pterygoids are proportion- ately long, these species are included in the same complex as those species with a broad overlap of the parasphenoid alae and median pterygoid rami. In the rhodopis complex the frontoparietal and prootic bones are not fused. Those spe- cies with a very short median ramus on the pterygoid and no pterygoid-para- sphenoid overlap also exhibit the fused 150 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY frontoparietal-prootic. For purposes of further discussion, these two major groups are here termed the Alpha and Beta groups of Eleutherodactylus. Mem- bers of the Alpha group (fused fronto- parietal-prootic, non-overlap between pteiygoids and parasphenoid alae) usually have relatively widely separated prevomers, whereas the Beta group frogs (frontoparietal and prootic not fused, pterygoids overlap parasphenoid alae ) usually have the prevomers in con- tact or only narrowly separated. I submit that the two divisions, Alpha and Beta, are natural divisions within the genus Eleutherodactylus and not simply a chaotic array of species ex- hibiting two osteological patterns. I bor- rowed the terminology of Etheridge ( 1960 ) for the major divisions since at this time I am not willing to afford the two divisions nomenclatorial recognition and prefer the informal divisional names. This course is taken because only a rela- tively small part of the genus has been surveyed, and many species could not be assigned to subgenus were nomen- clatorial assignments made. If the two divisions were accorded nomenclatorial status, the Alpha group would be the subgenus Eleiithewdactyhis and the Beta group would take the name Cratigastor. Several osteological features seem to lend themselves well to the possible use of skeletal morphology in the assessment of species group relationships within the genus Eleutherodactylus. The degree of median separation of the prevomers has potential in that it varies concordantly with several other osteological traits ( the development of cranial crests, shape of the rami of the squamosal, and size and shape of the nasal bones). Among the West Indian species of the genus, the spe- cies groups have long been based at least in part on the length of the prevomerine dentigerous processes, and I would ex- pect this character complex to be of at least some value, although its use is greatly hampered by the occasional loss of dentigerous processes in several groups of the genus. I have not attempted to divide the species of the genus into spe- cies groups, because I have not studied all species of the genus and I cannot rely upon the literature for many characters that I regard as of potential importance. A study of the osteology of the genus Eleutherodactylus is envisioned, but prior to its initiation considerable re- search must be done in straightening out many nomenclatorial entanglements, the description of many more species, and synonymizing of many names. Euparkerella Griffiths, 1959 (Fig. 100) Euparkerella Griffiths, 1959, Proc. Zool. Sue. London, 132:477 [Type-species by original designation, Sminthillus brasiliensis Parker, 1926]. Diapiostic definition. — 7) omoster- num present, small; 9) maxillary arch toothed; 10) alary processes of premaxil- lae directed posterodorsally, broad at base; 11) palatal shelf of premaxilla very broad, not notched, palatal process mi- nute; 12) facial lobe of maxilla shallow; 13) palatal shelf of maxilla broad, taper- ing posteriorly, no pterygoid process; 15) nasals small, moderate median sep- aration; 16) nasals in contact with maxil- lae, separated from pterygoids; 19) fron- toparietals not ornamented; 20) fronto- i parietal fused to prootic; 22) epiotic I eminences small; 23) cristae paroticae very broad, stocky; 24) zygomatic ramus of squamosal of moderate length, widely separated from maxilla; 25) otic ramus of squamosal elongate, not expanded medially into otic plate; 26) squamosal- maxillary angle about 60°; 27) columel- la absent; 28) prevomers reduced to minute slivers, widely separated medial- ly, edentate, dentigerous rami lost; 29) palatines very slender, reduced in size, widely separated medially; 30) sphen- ethmoid divided, extending anteriorly under posterior edge of nasals; 31) an- terior ramus of parasphenoid very broad, not keeled medially; 32) parasphenoid alae oriented at right angles to anterior LYNCH: LEPTODACTYLOID FROGS 151 Figure 100. Lateral, dorsal, and ventral views of skull of Euparkeivlla brasiiieims (KU 93192, X5). ramus, short, not overlapped by median rami of pterygoids; 33) pterygoids rela- tively small, anterior rami long, not reaching palatines; 34) occipital con- dyles small, stalked, widely separated medially; 36) terminal phalanges short and broad, bearing small hook-like lat- eral processes; 37) alary processes lack- ing on hyoid plate; 40) in. depressor mandihtilae in two slips; 42) males with median subgular vocal sac; 43) body lacking glands; 44) tongue large, not notched, posterior edge free; 45) toes lacking webbing, digital tips pointed, not dilated, fingers and toes short; 46-48); 49) adults small, less than 20 mm. SVL; 50) tympanum absent. Composition. — Monotypic. Distribution. — Known only from the Serra dos Orgaos, state of Guanabara, Brasil. Remarks. — Parker (1926) named Sminthillus hrasiliensis on the basis of the "juvenile" cotypes of Boulenger's Oocormus microps (=zZachaenus parvu- lits). Noble examined Parker's drawings of the pectoral girdle of hrasiliensis and agreed with Parker that the species fit the characteristics of Sminthillus. At that time, SmintluUiis comprised tliree species — one Cuban, one Peruvian, and one Brasilian. Griffiths (1959) argued that if all three species were independent derivatives of Eleutherodactijlus, then each belongs to a separate genus. His solution was to place each in a mono- typic genus. Griffiths proposed Etipark- erelJa for the Brasilian species but did not provide diagnostic statements for the genus. Euparkerella is very distinctive in its osteology. In external morphology, Euparkerella is superficially very similar to Zachaenus parvulus. These two spe- cies live in the same habitat ( leaf litter ) in southeastern Brasil and are frequently collected syntopically. The coloration of 152 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY the two species is nearly identical. Eu- parkerella brasiliensis and Zachaenus parvuJus differ in adult size and the length of the fingers ( Fig. 94 ) . The skeleton of Eiiparkerelh does not bear any close resemblance to that of any other leptodactylid genus, al- though the squamosal architecture, lack of columellae, and shape of the hyoid plate of Euparkerella suggest a relation- ship to the genus Holoaden. The termi- nal phalanges of Euparkerella are unique in the shape of the lateral expansions (Figs. 43-44). The digits are not pad- like and lack the terminal transverse groove that is found on the digital tips of Eleiitherodactyhis, Sijrrhophus, Smin- thiUus, and Tomodactylus. The fronto- parietal and prootic fusion of Euparker- ella is suggestive of a relationship with the Alpha division of Eleutherodactylus. At present, I regard the relationships of Euparkerella as obscure but feel that the genus is probably more closely related to Holoaden than to either division of Eleu- therodactylus. Holoaden Miranda-Ribeiro, 1920 (Fig. 101) Holoaden Miranda-Ribeiro, 1920, Rev. Mus. Paulista, 12:319 [Type-species by mono- typy, Holoaden hiederwaldti Miranda- Ribeiro, 1920]. Diagnostic definition. — 7) omoster- num moderate-sized; 9) maxillary arch toothed; 10) alary processes of premaxil- lae directed dorsally, moderately wide at base; 11) palatal shelf of premaxilla broad, slightly indented; 12) facial lobe of maxilla relatively shallow, not ex- ostosed; 13) palatal shelf of maxilla of moderate width, no distinct pterygoid process; 15) nasals moderate-sized, nar- rowly separated medially; 16) nasals separated from maxillae and pterygoids; 18) frontoparietal fontanelle moderate- sized; 19) frontoparietals not orna- mented; 20) frontoparietals not fused with prootics; 22) epiotic eminences small; 23) cristae paroticae short, stocky; 24 ) zygomatic ramus of squamosal mod- erately long, widely separated from maxilla; 25) otic ramus of squamosal Figum: 101. Lateral (X 8), dorsal (X 4) and ventral (x 4) views of skull of Holoaden biadei (KU 107087). LYNCH: LEPTODACTYLOID FROGS 153 long, not expanded medially into otic plate; 26) squamosal-maxillary angle about 65°; 27) columella absent; 28) prevomers entire, toothed, separated me- dially; 29) palatines narrow, elongate, separated medially; 30) sphenethmoid entire, extending anteriorly beneath pos- terior edge of nasals; 31) anterior ramus of parasphenoid moderately broad, not keeled medially; 32) parasphenoid alae oriented at right angles to anterior ramus, widely separated from median rami of pterygoids; 33) pterygoids slen- der, anterior rami long, nearly reaching palatines; 34) occipital condyles small, not stalked, widely separated medially; 36) terminal phalanges knobbed; 37) hyoid plate lacking alary processes; 40) m. depressor mandihulae in two slips; 42) males lacking vocal sac; 43) entire skin glandular forming large, indefinite parotoid, Hank, and inguinal glands and a large glandular mass on the thighs; 44) tongue oval, not notched, posterior one-half free; 45) toes free of webbing, digital tips narrow; 49) adults small, 20- 48 mm. SVL; 50) tympanum absent. Composition. — Two species are pres- ently known (hradei and Itiederwoldti). Distribution. — The coastal Serras of southeastern Brasil. Remarks. — Miranda-Ribeiro ( 1920, 1926) included Holoaden in the Telma- tobiidae with Acris, Iliodlscus, and Tel- matohius. He considered the Telmato- biidae to be intermediate between the Hylidae and Leptodactylidae. Lutz (1958) considered Holoaden a member of a generic cline (Cijcloramphus-Cras- pedoglossa-HoIoaden) but did not place the genus in the Cycloramphinae. Holo- aden is superficially similar to Zachaenus stejnegeri (Craspedoglossa auctorum) but differs in several osteological characters. Holoaden and Eiiparkerella lack alary processes on the hyoid plate and differ from all other leptodactylids except Limnomedusa and Sminthillus in this character. Holoaden is osteologically similar to the Andean Niceforonia. This similarity may reflect a faunal relation- ship between the Brasilian highlands and the Andes or may reflect conver- gence in the arrangement of the skull bones resulting from adaptation to bur- rowing. In osteological and external characters, Holoaden does not seem especially closely related to any other genus included in the Eleutherodactylini except Eiiparkerella. Hylactopliryne Lynch, 1968 (Figs. 102-03) Hylactophrijne Lynch, 1968, Univ. Kansas Pubis. Mus. Nat. Hist., 17:511 [Type- species jjy original designation, HyJodes august i Duges, 1879]. Diagnostic definition. — 7) omoster- num large; 9) maxillary arch toothed; 10) alary processes of premaxillae di- rected posterodorsally, moderately wide at base; 11) palatal shelf of premaxilla broad, deeply dissected; 12) facial lobe of maxilla relatively deep, not exostosed; 13) palatal shelf of maxilla of moderate width, pterygoid process large; 15) na- sals very large, in broad median contact; 16) nasals in contact with maxillae, not with pterygoids; 19) frontoparietals not ornamented; 20) frontoparietals not fused to prootics; 22) epiotic eminences large; 23) cristae paroticae long, narrow; 24) zygomatic ramus of squamosal of moderate length, not reaching maxilla; 25) otic ramus of squamosal long, as long as zygomatic ramus, expanded me- dially into small otic plate; 26) squa- mosal-maxillary angle about 55°; 27) columella present; 28) prevomers large, entire, narrowly separated medially; 29) palatines large, broad, separated medial- ly; 30) sphenethmoid entire, large, ex- tending anteriorly beneath posterior edge of nasals; 31) anterior ramus of parasphenoid broad, not keeled; 32) parasphenoid alae oriented at right angles to anterior ramus, broadly over- lapped by median rami of pterygoids; 33) pterygoids moderate-sized, anterior rami long, reaching palatines; 34) oc- cipital condyles moderate-sized, not stalked, widely separated medially; 36) 154 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 102. Dorsal views of skulls of Ilylactophryue aiigiisti (KU 56187, X 2.3, left) and hchnocnema quixensis (KU 104,388, X 4.7, right). terminal phalanges knobbed; 37) alary processes of hyoid plate on narrow stalks; 40) ill. depressor matidibuhe in two slips; 42) males with median subgular vocal sac; 43) body free of glands; 44) tongue large, oval, posterior edge free; 45) toes free of webbing or lateral fringes, digital tips narrow, first finger longer than second; 49) males 37-77, fe- males 40-95 mm. SVL; 50) tympanum visible externally. Composition. — Two species are cur- rently recognized (augusti and torahti- maraeyisis). The fonuer is composed of four subspecies. The group was revised by Zweifel (1956b). Distribution. — Mexican Plateau from Arizona, New Mexico, and Texas to cen- FiGURE 103. Lateral and ventral views of skulls of Hylactophnjne augusti (KU 56187, X 3, left) and hchnocnema quixensis (KU 104388, X 3 and X 4.7, right). LYNCH: LEPTODACTYLOID FROGS 155 tral Mexico (Cordillera Volcanica and western Sierra Madre del Sur). An iso- lated population is known from the mountains in the Isthmus of Tehuan- tepec. Remarks. — Hylactopliryne is very dis- tinctive when compared with the Central American and Mexican leptodactylids but is less distinctive when compared with some of the South American eleu- therodactylines. When I named Hijlac- tophryne (Lynch, 1968a), I suggested that the genus was allied to Eupsoplms. At that time I was under the mistaken impression that Oreohaies qiiixensls was an Eupsophus. Subsequently, I have examined all of the species of frogs re- ferred to the genus Eupsophus by vari- ous authors and concluded that the genus Eupsophus in the broad sense (that of Noble, 1931, and Gorham, 1966) includes representatives of five genera. One of these genera is Ischnocnema (see following account), which contains two species in South America. Hyhcto- phryne and Ischnocnema are very simi- lar. The skulls of the two genera differ in proportions but are otherwise the same (Figs. 102-03). These genera are tentatively separated on the basis of the presence (HyJactophryne) or absence (Ischnocnema) of a discoidal fold. The two genera may prove to be independent derivatives of Eleutherodacfylus rather than primitive as I previously suggested (Lynch, 1968a). The Eleutherodactyhis guentheri group of frogs bear consider- able resemblance to Ischnocnema quix- ensis and /. verrucosa. Eleutherodacty- his carrioni of the southern Ecuadorian Andes is very similar to HyJactophryne augiisti. In both cases, the species of EleutJierodactyhis differ from the two genera in having T-shaped terminal pha- langes (rather than knobbed phalanges) and in having the terminal transverse groove on the digital pad (rather than no groove or pad ) . For the present, I do not advocate combining HyJactopliryne and Ischnocnema with one another or with Eleutlierodactylus. Ischnocnema Reinhardt and Liitken, 1862 (Figs. 102-03) Ischnocnema Reinhardt and Liitken, 1862, Vid. Meddel. Natnrh., Foren., 1861:239 [Type- species by monotypy, Leiupenis verrucosus Reinhardt and Liitken, 1862]. Oreohates Jimenez de la Espada, 1872, An. Soc. Espaiiola Hist. Nat., 1:87 [Type-species by monotypy, Oreohates cfuixcnsis Jimenez de la Espada, 1872]. Diagnostic definition. — 7 ) omoster- num moderate-sized; 9) maxillary arch toothed; 10) alary processes of premaxil- lae directed dorsally, moderately wide at base; 11) palatal shelf of premaxilla rela- tively deep, notched; 12) facial lobe of maxilla deep, not exostosed; 13) palatal shelf of maxilla relatively narrow, ptery- goid process large; 15) nasals very large, in broad median contact; 16) nasals separated from maxillae and pterygoids; 19) frontoparietals only sHghtly orna- mented; 20) frontoparietals not fused to prootics; 22) epiotic eminences poorly defined; 23) cristae paroticae relatively long and narrow; 24) zygomatic ramus of squamosal relatively long, widely sep- arated from maxilla; 25) otic ramus of squamosal slightly shorter than zygo- matic ramus, expanded medially into small otic plate; 26) squamosal-maxillary angle about 50°; 27) columella present; 28) prevomers large, entire, toothed, narrowly separated medially; 29) pala- tines large, broad, separated medially, bearing odontoid ridge in quixerisis; 30) sphenethmoid entire, extending anterior- ly beneath posterior edge of nasals; 31) anterior ramus of parasphenoid relative- ly narrow, not keeled medially; 32) para- sphenoid alae oriented at right angles to anterior ramus, slightly overlapped lat- erally by median rami of pterygoids; 33) pterygoids moderate-sized, anterior rami long, reaching palatines; 34) occipital condyles small, on small stalks, widely separated medially; 36) terminal pha- langes knobbed; 37) alary processes of hyoid plate on narrow stalks; 40) m. de- pressor mandiJ)ukie in two slips; 42) males with median subgular vocal sac; 156 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY 43) body lacking glands; 44) tongue large, oval, posterior edge free; 45) toes lacking webbing, digital tips narrow, first finger longer than second; 46-48); 49) adults to 55 mm. SVL; 50) tympanum visible externally. Composition.— Two species are pres- ently known (quixensis and verrucosa). Distribution. — Western edge of the Amazon basin in Ecuador, northeastern Peru, and adjacent Brasil (quixensis), and in the coastal Serras of southeastern Brasil (verruscosa). Both species are found in forested habitats. Remarks. — As mentioned before (Hy- lactophryne account), Ischnocnema is very similar to Hylactophryne; the two genera are here separated on the basis of trivial external characters, geography, and a lack of knowledge concerning breeding behavior and biology. The similarities in morphology between these two geographically isolated groups of eleutherodactylinc frogs is suggestive of an independent origin of each from an EleutherodactyJus stock through a de- parture from the arboreal adaptive zone. Typical Eleutherodactylus have toe pads (and are frequently mistaken for hylids by the uninitiated herpetologist ) and are usually semi-arboreal or arboreal in habits. Both Hylactophryne and Isch- nocnema are terrestrial frogs; the former lives in arid, non-forested regions and the latter lives in moist, forested en- vironments. Hylactophryne and Ischnocnema may represent relicts of a formerly wide- spread eleutherodactylinc stock from which more successful genera (Eleu- therodactylus) evolved. At present, too little is known of the osteology of Eleu- therodactylus to determine the evolu- tionary directions. Niceforonia Coin and Cochran, 1963 (Fig. 104) Niceforonia Coin and Cochran, 1963, Proc. California Acad. Sci., 31:499 [Type-species by original designation, Niceforonia nana Coin and Cochran, 1963]. Diagnostic definition. — 7) omoster- num moderate-sized; 9) maxillary arch toothed; 10) alary processes of premaxil- lae directed dorsally, relatively broad at base; 11) palatal shelf of premaxilla broad, deeply notched; 12) facial lobe of maxilla deep anteriorly, tapering pos- teriorly; 13) palatal shelf of maxilla broad, pterygoid process moderate-sized; 15 ) nasals small, narrowly separated me- dially; nasals in contact in fiavomacidata; 16) nasals in contact with maxillae, not with pterygoids; 19) frontoparietals not ornamented, except in flavomaculata; 20) frontoparietals not fused with prootics; 22) epiotic eminences obsolete; 23) cris- tae paroticae broad, stocky; 24) zygo- matic ramus of squamosal of moderate length, widely separated from maxilla; 25) otic ramus of squamosal long, ex- panded medially into small otic plate; 26) squamosal-maxillary angle about 55°; 27) columella present in most spe- cies, absent in montia, probably absent in simon.sii; 28) prevomers toothed or not, entire, relatively large, separated medially; 29) palatines slender, sep- arated medially; 30) sphenethmoid en- tire, extending anteriorly beyond an- terior edge of nasals; 31 ) anterior ramus of parasphenoid broad, long, not keeled medially; 32) parasphenoid alae oriented at right angles to anterior ramus, short, not overlapped laterally by median rami of pterygoids; 33) pterygoids small, me- dian rami short, anterior rami relatively long, not reaching palatines; 34) occipi- tal condyles relatively small, stalked, widely separated medially; 36) terminal phalanges knobbed; 37) alary processes on hyoid plate on narrow stalks; 40) m. depressor mamlihulue in two slips; 42) males with large median subgular vocal sac; 43) body lacking glands; 44) tongue large, round, free at posterior edge; 45) toes lacking webbing and lateral fringes, digital tips narrow; 46-48); 49) adults small, less than 30 mm. SVL; 50) tympa- num visible externally, concealed, absent (montia), or possibly absent (simonsii). Composition.— Lynch (1968d) in- LYNCH: LEPTODACTYLOID FROGS 157 Figure 104. Lateral, dorsal, and ventral views of skull of Niceforonia montia (MCZ 24352, X 5). eluded N. nana, N. festae, and N. montia as definite members of the genus and referred N. colinnbiana and N. simonsii to the genus. Based on examination of paratypes of Eupsophiis tvettsteini by stereo-radiographs, I now include that species in Niceforonia. EleutJierodacty- lus flavomaculattis Parker is a Nicefo- ronia (Lynch, 1969b) and Cei's (1968b) Syrrlwplnis hplacai is probably a mem- ber of Niceforonia as well. Distribution. — High elevations in the Andes of Colombia, Ecuador, Peru, and Bolivia. Remarks. — Coin and Cochran (1963) considered Niceforonia to be most closely allied to Eupsophus. In external characters, Eupsophus and Niceforonia cannot be separated. The cervical coty- lar arrangement and the median separa- tion of the occipital condyles suggests that Niceforonia is more closely related to the Eleutherodactylini than to the Alsodini. The breeding biology of Nice- foronia is unknown except that N. flavo- maculata lays large terrestrial eggs, but the large eggs are suggestive of direct development in all of the species of the genus. The very distinctive spheneth- moid of Niceforonia is duplicated by at least one species of Eleutlierodactijlus (bogotensis). Niceforonia is separated from Eleutlierodactyhis because the digital tips are narrow, there is no ter- minal transverse groove on the digital tips, and the terminal phalanges are knobbed. The slight median separation of the nasal bones in Niceforonia occurs in several groups of Eleutlierodactylus, although the trait is uncommon in Eleu- tlierodactylus. The other eleuthero- dactylines with knobbed terminal pha- langes (Amblyphrynus, Holoaden, Hy- lactop]}ryne, and Ischnocnema) are dis- tinctive when compared with Nicefo- ronia, although Holoaden resembles Niceforonia in the arrangement of the cranial bones. This osteological simi- larity possibly reflects convergence in view of the dissimilar morphology of the hyoid plates of these two genera. 158 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Sminthillus Barbour and Noble, 1920 (Fig. 105) SminthiUus Barbour and Noble, 1920, Bull. Mus. Conip. Zool., 63:402 [Type-species liy original designation, Plii/Uobates limhatus Cope, 1862]. Diagnostic dejinition. — 7) omoster- num small, elongate; 9) maxillary arch edentate; 10) alary processes of pre- maxillae directed dorsolaterally, short, broad at base; 11) palatal shelf broad, deeply dissected; 12) facial lobe of max- illa shallow; 13) palatal shelf of maxilla of moderate width, no pterygoid process; 15) nasals small, narrowly separated me- dially; 16) nasals in tenuous contact with maxillae, separated from pteiygoids; 19) frontoparietals not ornamented; 20) frontoparietals fused to prootics; 22) epiotic eminences present, small; 23) cristae paroticae very broad, stocky; 24) zygomatic ramus of squamosal very short, knobbed; 25) otic ramus of squa- mosal very long, no otic plate; 26) squa- mosal-maxillary angle about 60°; 27) columella present; 28) prevomers mi- nute, greatly reduced in size, entire, widely separated medially; 29) palatines slender, widely separated medially, lat- eral to prevomers; 30) sphenethmoid en- tire, extending anteriorly to middle of nasals; 31) anterior ramus of parasphe- noid narrow, not keeled medially; 32) parasphenoid alae slightly deflected pos- teriorly, very short, not overlapped lat- erally by median rami of pterygoids; 33) pterygoids very small, median and pos- terior rami short, anterior rami relatively long, extending to middle of orbit; 34) occipital condyles small, stalkc^d, widely separated medially; 36) terminal pha- langes T-shaped; 37 ) hyoid plate lacking alary processes; 40) m. depressor man- dihulae in two slips; 42) males with me- dian subgular vocal sac; 43) body lack- ing glands; 44) tongue narrow, posterior one-third free; 45) toes lacking webbing and lateral fringes, digital tips bear pads; Figure 105. Lateral (x 7.5), dorsal, and ventral views of skull of Sminthilhis limhatus ( KU 68684, X23). LYNCH: LEPTODACTYLOID FROGS 159 49) adults small, less than 15 mm. SVL; 50) tympanum visible externally. Composition. — Monotypic (S. limha- tusj with two subspecies. Distribution. — Cuba. Remarks. — SmintliiUus is closely re- lated to the West Indian species of Eleu- therodactylus and is most similar to the E. auriculatus group or to the E. dimi- diatus group (as defined by Shreve and Williams, 1963). SmintliiUus diiiers horn the Alpha division of EleutJierodactylus in two characters — the loss of teeth and the loss of the alary processes of the hyoid plate. Barbour and Noble ( 1920 ) considered SmintliiUus a dendrobatid or ranoid derivative, but Griffiths (1959) demonstrated that the genus was closely related to Eleutherodactyhis, an opinion often voiced by Noble (e.g., 1931). SfninthiUus was named by Barbour and Noble ( 1920 ) on the basis of a par- tial epicoracoidal fusion. However, the fusion is not as great as maintained by Noble ( 1926a, 1931 ) and occurs in many more frogs than he believed. I consider the presence of the fusion to reflect more accurately the care of a dissection than morphological divergence. The other two species named in SmintliiUus are now placed in other genera — the Peru- vian species (peruvianus) is placed in the Beta division of Eleutherodactyhis (see pp. 148-149) and the Brasilian species (hrasiliensis) is the only species of the genus Euparkerella. Syrrhophus Cope, 1878 (Fig. 106) Epirhexis Cope, 1866, J. Acad. Nat. Sci. Phila- delphia, 6:96 [Type-species by original designation, Batrachyla longipes Baird, 1859; suppression of the generic name re- quested by Lynch, 1967]. Syrrhophus Cope, 1878, Amer. Nat., 12:253 [Type-species by monotypy, Syrrhophus marnockii Cope, 1878]. Malachylodes Cope, 1879, Proc. Amer. Philos. Soc, 18:264 [Type-species by monotypy, Malachylodes guttilatus Cope, 1879]. Syrrhopus Boulenger, 1888, Proc. Zool. Soc. London, p. 206 [Emendation of Syrrhophus Cope, 1878]. Syirhaphus Giinther, 1901, Biol. Cent.-Amer., Kept, and Batr., p. 215 [Emendation of SyirhopJius Cope, 1878; hence taking same type-species (marnockii) and not verrucu- lattis as claimed by Gorham (1966)]. Diagnostic definition. — 7) omoster- num moderate-sized; 9) maxillary arch toothed; 10) alary processes of premaxil- lae directed dorsally, relatively narrow at base; 11) palatal shelf of premaxilla broad, deeply dissected; 12) facial lobe of maxilla shallow; 13) palatal shelf of maxilla broad anteriorly, narrowing pos- teriorly, no pterygoid process; 15) nasals large, in broad median contact; 16) na- sals not in contact with maxillae or pterygoids; 19) frontoparietal not orna- mented; 20) frontoparietal fused to prootic; 22) epiotic eminences obsolete; 23) cristae paroticae short, broad; 24) zygomatic ramus of squamosal very slender, relatively short; 25) otic ramus of squamosal elongated, not forming otic plate; 26) squamosal-maxillary angle about 65°; 27) columella present; 28) prevomers reduced in size, dentigerous ramus lost, widely separated medially, or dentigerous rami present, bearing a few teeth; 29) palatines narrow, separated medially, in contact with maxillae; 30) Figure 106. Lateral and dorsal views of skull of a male Syrrhophus pipilans (KU 59950, X 4). 160 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY sphenethmoid entire, extending anterior- ly beneath posterior edge of nasals; 31) anterior ramus of parasphenoid broad, not keeled medially; 32) parasphenoid alae deflected posteriorly, short, widely separated from median rami of ptery- goids; 33) pterygoids slender, all rami short; 34) occipital condyles small, not stalked, widely separated medially; 36) terminal phalanges T-shaped; 37) alary processes of hyoid plate on narrow stalks; 40) m. depressor mandibulae in two slips; 42) males with or without large median subgular vocal sac; 43) axillary and /or inguinal glands present; 44) tongue narrow to relatively broad and rounded, posterior edge free; 45) toes lacking webbing, bearing lateral fringes or not, digital tips very slightly to broad- ly dilated into pads; 49) adults 16-40 mm. SVL; 50) tympanum concealed or visible externally. Composition. — Lynch (1970a) recog- nized 12 species, two of which are poly- typic: cystignatlwides, dennisi, gtittila- tus, interorJ)itaUs, leprus, longipes, mar- nockii, modestus, nivocolimae, pipilans, nd)rimacidatus, and verrucipes. Distribution. — Discontinuous in the Pacific lowlands from Sinaloa, Mexico, to El Salvador, also in the eastern low- lands of Mexico from the Edwards Pla- teau of Texas to British Honduras. High- land species occur along the Sierra Madre Oriental up to 2000 meters. Remarks.— l^ynch (1968a, 1970a) discussed the generic separation of Eleu- tlierodactyhts, Sijrrhophus, and Tomo- dactylus. In external characters, Syr- rhophus is not separable from all Eleii- therodactylns. The osteological peculi- arities of Syrrlwphus are duplicated by Tomodactylus and the Alpha division of Eleutlierodactyhis. Syrrhophus and To- mod actyJus are distinguished in some external characters (lumbar gland, ar- rangement of the supernumerary plantar tubercles) and by one paedomorphic skeletal character — the sphenethmoid is usually divided in Tomodactylus and is entire in Syrrhophus. The division of the sphenethmoid is a paedomorphic feature and therefore should not be given undue weight in any classification. The separation of Syrrhophus and To- modactylus as distinct genera is a de- batable point, and I retain them as generically distinct only as a matter of convenience. The character of the glands used by Lynch ( 1968a ) to sep- arate the two genera tends to be less diagnostic when the species of the two genera from northwestern Mexico are compared (S. interorhitalis, S. modestus, T. saxatilis). Until a comprehensive revision of the genus Eleutlierodactyhis is completed and the skeletons of the majority of species studied, it will not be possible to argue definitively whether the genera Syrrhophus and Tomodactylus are deriv- atives of the Alpha or the Beta divisions of Eleutlierodactyhis. In an attempt to clarify this point, I studied representa- tives of all species groups of Central American Eleiitherodactylu^ and found no group which exhibits the osteological characteristics of the Alpha division. If Syrrhophus and Tomodactylus were de- rivatives of the South American groups of the Alpha division, one might expect some relict species to be distributed in parts of Lower Central America. How- ever, all Central American species of Eleutlierodactyhis examined by me are Beta division Eleutherodactylus, as are those species of the genus found in the Choco of Colombia and Ecuador. There- fore I suggest that the Mexican Syrrho- phus and Tomodactylus are more closely related to the West Indian Eleuthero- dactylus (Alpha division) than to any other groups of the genus. Within the Alpha division, the auriculatus group most closely approaches the morphology 1 of the endemic Mexican eleutherodacty- line genera Syrrhophus and Tomodac- tylus. Tomodactylus Giinther, 1901 (Fig. 107) Tomodactylus Giinther, 1901, Biol. Centr.- Amer., Rept. and Batr., p. 219 [Type- LYNCH: LEPTODACTYLOID FROGS 161 species by monotypy, Tomodactyhis amuJae Giinther, 1901]. Diagnostic definition. — 7) omoster- num moderate-sized; 9) maxillary arch toothed; 10) alary processes of premaxil- lae directed dorsally, broad at base; 11) palatal shelf of premaxilla narrow, pala- tal process elongate; 12) facial lobe of maxilla shallow; 13) palatal shelf of maxilla narrow, pterygoid process mod- erate-sized; 15) nasals large, in broad median contact; 16) nasals not in con- tact with maxillae or pterygoids; 18) frontoparietal fontanelle absent in adults, often present in young males; 19) fron- toparietals not ornamented; 20) fronto- parietal fused to prootic; 22) epiotic eminences obsolete; 23) cristae paroti- cae short and stocky; 24) zygomatic ramus of squamosal sliver-like, very short; 25) otic ramus of squamosal very long, no otic plate; 26) squamosal-maxil- lary angle 50-60°; 27) columella pres- ent; 28) prevomers reduced in size, edentate, widely separated medially; 29) palatines slender, widely separated me- dially; 30) sphenethmoid usually di- vided, not extending anteriorly to nasals; 31 ) anterior ramus of parasphenoid rela- tively broad, not keeled medially; 32) parasphenoid alae deflected posteriorly, short, not overlapped by median rami of pterygoids; 33) pterygoids slender, all rami short; 34) occipital condyles small, not or but slightly stalked, widely sep- arated medially; 36) terminal phalanges T-shaped; 37) alary processes of hyoid plate on narrow stalks; 40) m. depressor mandibulne in two slips; 42) males with large, median, subgular vocal sac; 43) lumbar gland usually well defined, axil- lary glands sometimes present; 44) tongue relatively small, narrow, posterior edge free; 45) toes lacking webbing, digital tips sHghtly to broadly dilated; 49) adults 21-31 mm. SVL; 50) tympa- num visible externally. Composition. — The genus was revised by Dixon ( 1957 ) and two species were subsequently named. Nine species are presently recognized: albolabris, angus- tidigitorum, dilatiis, ftiscus, grandis, niti- FiGURE 107. Lateral, dorsal, and ventral views of skull of a female Tomodactyhis nitidus (KU 102649, X 4.7). 162 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY dus (3 subspecies), rufescens, saxatilis, and syristes. Dixon and Webb (1966) briefly commented on an unnamed spe- cies from Nevado de Colima, Jalisco, Mexico. Distribution. — The Cordillera Vol- canica of Mexico from western Veracruz to Colima; the Oaxacan Plateau, the Sierra Madre del Sur of Oaxaca and Guerrero, and the Pacific lowlands from Sinaloa to Michoacan. The genus is largely allopatric to Sijrrhophus. Remarks. — Gallardo (1965) placed Tonwclactyliis in the Leptodactylinae and Syrrliophus and Eleutherodactylus in the Eleutherodactylinae. This asso- ciation was based on erroneous data concerning the breeding biology of Tomodactylus. Tomodactylus is primarily a lower montane genus, whereas the closely re- lated Syrrhophus is primarily a lowland genus ( Lynch, 1970a ) , but the two gen- era are sympatric in the lowlands of western Mexico. The differences between them are expressed to the greatest de- gree in eastern and southern Mexico and expressed to a lesser degree in western Mexico, suggesting that the generic di- chotomy occurred in western Mexico. Tribe incertae .sedis Scythrophrys new genus Type-species. — Zachaenus sawayae Cochran, 1953. The following characteristics of the diagnostic definition are observable: 1) sternum cartilaginous; 2) vertebral shield lacking; 6) cranial bones not der- mostosed; 7) omosternum small; 8) sacral diapophyses rounded; 9) maxillary arch toothed, teeth blunt, pedicellate; 14) maxillary arch complete; 18) fronto- parietal fontanelle lacking; 21) temporal arcade lacking; 24) zygomatic ramus of squamosal relatively long, widely sep- arated from maxilla; 28) prevomers toothed, dentigerous processes large, transversely elongate, situated posterior to choanae; 36) terminal phalanges ap- parently knobbed; 40) vi. depressor mandilndae in two slips, pars tympan- icus \e\y large, p. scapidaris minute; 41) pupil horizontal; 43) body lacking glands; 44) tongue relatively large, pos- terior edge free; 45) toes lacking web- bing but have lateral fringes, outer meta- tarsal tubercle present, inner metatarsal tubercle not enlarged or spade-like, digi- tal tips narrow on fingers, those of toes slightly dilated, thumb very short; 49) single adult female known is 16.9 mm. SVL; 50) tympanum concealed. Etymology. — G reek, scythros -{- phryne, meaning "sullen toad." Remarks. — A single specimen of this southeastern Brasilian frog is known; it was named as a member of Zachaenus by Cochran (1953). In external appear- ance, the frog resembles Pliysaluemus {maculiventris group) or Paratelmato- bius and, in some respects, Zachaenus. Cochran (1953) considered the small tubercles on the upper eyelid as indica- tive of some relationship with Zachaenus but noted the many points of disagree- ment between parvuhis and sawayae. The most striking difference between the two species is seen in the length and shape of the fingers ( Fig. 94 ) . The very short thumb of Scythrophrys is sugges- tive of a reduced phalangeal formula for the hand. The tympanum is recessed and smaller than indicated by Cochran (1953). Scythrophrys is placed with confi- dence in the Telmatobiinae but is not assigned to any tribe, because many characters are not known. Based on the available information, I consider the ge- nus to belong either to the Crypiscini or Eleutherodactylini, but until the osteol- ogy and breeding biology of Scyth- rophrys are known, definite assignment to a tribe would be presumptuous. Cochran's (1953) description of the holotype (USNM 125530) is relatively accurate. My measurements of the holo- type differ somewhat from hers, reflect- ing either differences in techniques or possibly shrinkage. I recorded the fol- LYNCH: LEPTODACTYLOID FROGS 163 lowing measurements (in millimeters): snout-vent length 16.9, shank length 8.4, head width 6.3, head length 5.6, eye length 1.9, eyelid width 1.7, and inter- orbital distance 2.6. A few cranial char- acters are visible through a small tear in the skin of the head. The frontoparietals are broad and a fontanelle is lacking. The nasals appear to be relatively large and in median contact. Two characters of the foot were not mentioned by Coch- ran. There is a small calcar on the heel and a narrow outer tarsal fold extending for the length of the tarsus onto the fifth toe. Elosiinae Miranda-Ribeiro, 1926 Elosiidae Miranda-Ribeiro, 1926:27. Elosiinae: Noble, 1931:504. Gallardo, 1965: 84. Miranda-Ribeiro (1926) proposed the Elosiidae for three genera; the concept and content of the group has remained unchanged since its proposal. Three genera are presently included in the sub- family: Crossodactijlus, Hijlodes (^EIo- sia aucfomm), and Megaelosia. Cochran (1938) named Crossodactijlodes, which she considered possibly related to the elosiines. She thought that the digital morphology of Crossodactijlodes indi- cated that the genus exhibited primitive elosiine characters. The apparent dorsal dermal glands on the digital pads of Crossodactijlodes are artifacts reflecting the Y-shaped terminal phalanges. Coin and Cochran ( 1963 ) suggested that Tracliijplirynus was related to Crosso- dactijlus. I previously discussed this point and placed Traclujphrijnus in the synonymy of Eleutherodactijlus (Lynch, 1968d). Noble (1922, 1931) considered the Elosiinae to be a bufonid group. The subfamily was associated with the Lep- todactylidae by Davis ( 1936 ) , who pointed out that the Bufonidae and Lep- todactylidae could be familially distin- guished. The type-genus of the subfam- ily, Elosia Tschudi, 1838, is a synonym of Hylodes Fitzinger, 1826 ( which is not to be confused with Hylodes Fitzinger, 1843, which is a synonym of Eleuthero- dactijlus Dumeril and Bibron, 1841). The family-group name need not be changed simply because the type-genus is a synonym (see Article 40, Interna- tional Code of Zoological Nomenclature, 1961). At any rate, the family-group name could not be changed so as to be based on Hylodes Fitzinger, 1826, be- cause Giinther ( 1859a ) proposed a Hy- lodidae based on Hylodes Fitzinger, 1843. Until recently, the subfamily was known only from southeastern Brasil and Misiones Province, Argentina, but it is now known to occur also in Venezuela (Cerro Duida, Guiana Massif). The sub- family is homogeneous morphologically and is readily distinguished from all other leptodactylid groups. The follow- ing diagnostic characters are common to the three genera of the Elosiinae: 1) sternum cartilaginous, tending to cal- cify in old adults; 2) vertebral shield lacking; 3) transverse processes of an- terior presacral vertebrae short, those of posterior presacral vertebrae also short- ened; 4) cervical cotylar arrangement type I; 5) cervical and second vertebrae not fused; 6) cranial bones not involved in dermostosis; 7) omosternum present, moderate-sized; 8) sacral diapophyses rounded; 9) maxillary arch toothed, teeth pointed, pedicellate; 12) facial lobe of maxilla shallow; 13) palatal shelf of maxilla narrow, no pterygoid process; 15) nasals small, widely separated me- dially; 17) nasals not in contact with frontoparietals; 18) frontoparietal fon- tanelle lacking; 19) frontoparietals not ornamented; 21) temporal arcade lack- ing; 23) carotid artery passes dorsal to skull bones; 27) columella present; 30) sphenethmoid very large, entire, extend- ing anteriorly to anterior edge of nasals; 36) terminal phalanges T-shaped; 37) alary processes of hyoid plate on narrow stalks; 38) cricoid cartilage not divided ventrally; 39) m. petrohyoidetis anterior and m. sternohyoideiis insert on lateral 164 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY edge of hyoid plate; 40) m. depressor mandibuhe in two slips; 41) pupil hori- zontal; 43) body lacking glands; 44) tongue large, not notched, posterior edge free; 45) toes bearing large lateral fringes, large flap-like tarsal fold present, outer metatarsal tubercle present, inner metatarsal tubercle not spade-like, digi- tal tips broad; 46) larvae with 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 47) amplexus axillaiy in known species; 48) eggs small, numer- ous, laid in moist terrestrial situations or in ponds or streams; 50) tympanum visible externally; 51) each digital pad has a pair of dermal, scute-like glandu- lar pads on dorsal surface. The verte- bral arches of all elosiines are very non- imbricate and the vertebrae and coccyx are poorly ossified. The Elosiinae are of particular in- terest in that the poison-arrow frogs ( Dendrobatidae ) are apparently derived from this leptodactylid subfamily. The two groups agree in cranial morphology, vertebral columns, the T-shaped termi- nal phalanges, the dermal glandular pads on top of the digital pads, and in the presence, in at least some species of each group, of toxic skin secretions (the secretions of the elosiines have not been chemically analyzed). The two groups differ in breeding biology and in the architecture of the pectoral girdle. Crossodactylus best fits my concept of the primitive elosiine but has diverged in at least one character — the loss of the quadratojugal. The genus is distinctive in its ranoid pattern of the attachment of the distal tendons of the thigh muscula- ture. The ranoid pattern of the thigh musculature of Crossodactylus is exactly like that seen in the dendrobatids and mitigates the importance of one of the criteria used by Griffiths ( 1963 ) to asso- ciate the dendrobatids as a Neotropical subfamily of the Ranidae. Crossodacty- lus has a median subgular vocal sac and nuptial asperities (cluster of spines) in the males. This condition is like that seen in most Telmatobiinae (excepting the Eleutherodactylini which lack nup- tial asperities); I regard the presence of vocal sac and nuptial asperities as primi- tive. The tadpoles of Crossodactylus have median vents in contrast to the dextral vents of the tadpoles of Hylodes and Megaelosia. Hylodes and Megae- losia have the bufonid pattern of the arrangement of the distal tendons of the thigh musculature, derived conditions of the vocal apparatus, and quadratojugal bones. I envision the dendrobatids as having diverged from the Crossodactylus stock prior to the loss of the quadrato- jugal, but after Hylodes and Megaelosia had evolved. Crossodactylus Dumeril and Bibron, 1841 (Fig. 108) Crossodactylus Dumeril and Bibron, 1841, Erpetologie generale, 8:635 [Type-species by monotypy, Crossodactylus gaudichaudii Dumeril and Bibron, 1841]. Limnocharis Bell, in Darwin, 1843, Zool. Voy- age Beagle, Reptiles, 5:33 [Type-species by monotypy, Limnocharis fuscus Bell, 1843]. Tarsopterus Reinhardt and Liitken, 1862, Vid. Meddel. Naturh., Foren., 1861:177 [Type- species by monotypy, Tarsopterus tracluj- stomus Reinhardt and Liitken, 1862]. Calamohates DeWitte, 1930, Miss. Biol. Beige Bresil, 2:219 [Type-species by monotypy, Calamohates boidengeri DeWitte, 1930]. Diagnostic definition. — 10) alary proc- esses of premaxillae directed anterodor- sally and laterally, broad at base; 11) palatal shelf of premaxilla narrow, pala- tal process elongate; 14) maxillary arch incomplete, maxilla tapering posteriorly, quadratojugal absent; 16) nasals sep- arated from both maxillae and ptery- goids; 20) frontoparietal fused to pro- otic; 22) epiotic eminences moderately distinct; 23) cristae paroticae short, stocky; 24) zygomatic ramus of squa- mosal of moderate length, pointed, widely separated from maxilla; 25) otic ramus of squamosal slightly shorter than zygomatic ramus, no otic plate; 26) squamosal-maxillary angle about 50°; 28) prevomers moderately small, sep- arated medially, dentigerous ramus lost LYNCH: LEPTODACTYLOID FROGS 165 or not, rarely toothed; 29) palatines small, narrow, widely separated medial- ly; 31) anterior ramus of parasphenoid short, broad, not keeled medially; 32) parasphenoid alae oriented at right angles to anterior ramus, short, widely separated from median rami of ptery- goids; 33) pterygoids with slender rami, anterior rami not reaching palatines; 34) occipital condyles small, stalked, widely separated medially; 35) mandible lack- ing odontoids; 42) males with median, subgular vocal sac, nuptial spines in a cluster in all species; 46) larvae with median vent; 49) adults relatively small, less than 40 mm. SVL. Composition. — Six species are pres- ently recognized (aeneus, dispar, gaudi- chaudii, grandis, schmidti, and tracluj- stoma), although some authors favor re- garding dispar and grandis as conspe- cific. The most recent revision of the genus (Cochran, 1955) did not treat C. grandis B. Lutz, 1951, or C. schmidti Gallardo, 1961. Distribution. — Southeastern Brasil in the lowlands from southern Minas Gerais to Misiones Province, Argentina. Remarks. — The generic synonymy of Crossodactylus has been stable for many years. Cochran (1955) and Gallardo ( 1961 ) presented studies of intrageneric variation and relationships. Crossodac- tylus is primitive to the other elosiines in tadpole morphology (median vent) and in the secondary sex characteristics (me- dian subgular vocal sac and nuptial as- perities ) , but is specialized in the loss of the quadratojugal. Hylodes is similar to Crossodactylus in having a poorly ossi- fied quadratojugal, but differs from Crossodactylus in the other characteris- tics mentioned. The ranoid pattern of the attachment of the distal tendons of the thigh muscu- latme of Crossodactylus distinguishes the genus from the other elosiines, as well as from all other Neotropical lepto- dactylids. The thigh musculature of Crossodactylus adds yet another charac- ter to the impressive list of characters shared by the dendrobatids and Crosso- FiGiTRE 108. Lateral, dorsal, and ventral views of skull of Crossodactylus gaudichaudii ( KU 92759, X 4.7). 166 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY dactijlus. Noble ( 1931 ) argued that the Dendrobatinae were derived from the bufonid genus Crossodactyhis, because he found the digital pad structure of the two groups to be identical and to exist in no other Neotropical bufonoid frogs. Noble argued that the condition of the epicoracoidal cartilages of Crossodacty- his is precursorial to the condition seen in developing PlnjUobates (:=Coloste- thus) sidjpunctatus. Noble considered his data adequate to demonstrate that the firmisternal dendrobatids passed through an arciferal condition in ontog- eny. Griffiths (1959, 1963) sought to ally the dendrobatids with ranids and argued that the dendrobatids do not pass through an arciferal stage in develop- ment. The developmental pattern of the pectoral girdle exhibited by Colostethus sidjpunctatiis is clearly ranoid. My own study of this subject completely supports that of Griffiths. Griffiths (1963) rejected Noble's argument that the thigh musculature was of primary importance in anuran classifi- cation, but cited the thigh musculature as additional evidence supporting his contention that dendrobatids are a ranid subfamily. Griffiths cited the similar de- velopment of the digital pads of the Petropedetinae (Ranidae) as supportive evidence for the close relationship be- tween the dendrobatids and ranids. His argument requires that we ignore the many similarities between elosiines and dendrobatids and regard several char- acter complexes as evolving in a parallel fashion in leptodactylids and ranids. Associating the dendrobatids with the bufonoids requires that we regard the firmisternal pectoral girdles of dendro- batids and ranids to have been inde- pendently evolved. This position is made less objectionable by the occurrence of a nearly complete transition from arcifery to firmisterny within the Neotropical Bufonidae. Noble's (1922) position that the firmisternal pectoral girdle has ap- peared more than once is regarded as correct. Griffiths ( 1963 ) cited several other characters as exclusively ranoid. The bursa angularis oris is not restricted to dendrobatids and ranids as Griffiths stated but occurs in most, if not all, groups of advanced frogs (Baldauf and Tanzer, 1965, Trueb, 1966, 1968, 1970, and Starrett, 1968). The dendrobatids are amply distinct from the elosiine leptodactylids. I do not intend to present an argument that the two families ought to be combined, because I think that there is value in recognizing the small, brightly colored, poisonous Neotropical dendrobatid frogs as familially distinct. The dendrobatids have lost the palatines, which are re- tained, although they are small, in elo- siine leptodactylids. The firmisternal architecture of the pectoral girdle of dendrobatids is markedly different from the arciferal architecture exhibited by all leptodactylids. The breeding behavior and biology of the dendrobatids is not unique among frogs but is very different from that of the elosiine leptodactylids. Dendrobatid tadpoles usually have 2/3 tooth rows, although several species have reduced numbers (Starrett, 1960). The tadpoles of all dendrobatids have a broad anterior interruption of the labial papil- lae as do most leptodactylids. Dendro- bates has either a median or dextral vent, whereas all known tadpoles of Colostethus and Plujlhbates have dex- tral vents. Hylodes Fitzinger, 1826 (Fig. 109) Hylodes Fitzinger, 1826, Neue Class. Kept., p. 38 [Type-species by monotypy, Hylodes ranoides (=HyIa ranoides Spix, 1824)]. Enydwbius Wagler, 1830, Nat. Syst. Ampli., p. 202 [Substitute name for Hylodes Fitzinger, 1826; hence taking same type-species]. Elosia Tschudi, 1838, Classif. Batr., p. 77 [Type-species by monotypy, Elosia nasiita Tschudi, 1838]. Scimicodes Fitzinger, 1843, Syst. Kept., p. 32 [Type-species by original designation, Hyla nastis Lichtenstein, 1823]. Diagnostic definition. — 10) alary proc- esses of premaxillae directed anterodor- LYNCH: LEPTODACTYLOID FROGS 167 sally and laterally, broad at base; 11) palatal shelf of premaxilla relatively narrow, palatal process relatively small; 14) maxillary arch complete, quadrato- jugal poorly ossified; 16) nasals not in contact with maxillae or pterygoids; 20) frontoparietals fused to prootics; 22) epiotic eminences moderately distinct; 23) cristae paroticae short, stocky; 24) zygomatic ramus of squamosal short, truncate, widely separated from maxilla; 25) otic ramus of squamosal about as long as zygomatic ramus, not expanded into otic plate; 26) squamosal-maxillary angle about 40°; 28) prevomers entire, toothed, separated medially; 29) pala- tines long, narrow, widely separated me- dially; 31) anterior ramus of parasphe- noid short, broad, keeled medially in at least some species; 32) parasphenoid alae oriented at right angles to anterior ramus, narrowly overlapped laterally by median rami of pterygoids; 33) ptery- goids relatively small, rami slender, an- terior rami elongate, reaching palatines; 34) occipital condyles small, not stalked, widely separated medially; 35) mandible lacking odontoids; 42) males with paired, lateral, membranous vocal sacs, absent in one species, and with nuptial asperities in a pad on thumb; 46) larvae with dextral vent; 49) adults 30-45 mm. SVL. Composition. — Bokermann ( 1966) listed nine species (aspera, glahrus, lat- eristrigatus, magalhaesi, mertensi, merid- ionaUs, nasus, perplicatus, and piilcher) in the genus, then known only from southeastern Brasil. Gorham (1966) listed gla])nis as a synonym of lateri- strigatiis and meridionalis as a subspecies of nasus. Bokermann ( 1967 ) named an additional species from Rio de Janeiro (ornata), and Rivero (1968) named dui- densis from Venezuela. All of these authors used the generic name Elosia, as did Cochran ( 1955 ) in her study of the species of southeastern Brasil. Distribution. — Coastal southern and southeastern Brasil from Rio Grande do Sul north to Minas Gerais. One species occurs on Cerro Duida in Amazonian Venezuela. Remarks. — Frogs of this genus ex- hibit relatively little intrageneric varia- tion and have been recognized as a dis- tinctive generic unit for many decades. Figure 109. Lateral, dorsal, and ventral views of skull of Hylodes asper ( KU 92870, X 4). 168 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY The nomenclatorial problems of the genus are by no means minor. Myers (1962) pointed out that the proper ge- neric name for these frogs is Hylodes Fitzinger, 1826, and not Elosia Tschudi, 1838, the name which had been appHed more or less universally for 60 years. The usage of one generic name in pref- erence to another in a significant work- must be taken into account when dealing with any question of priority and /or nomenclatorial stability. It is therefore significant that Cochran (1955) used Ehsia in her important study of the frogs of southeastern Brasil. However, the argument against usage of Hylodes as the proper generic name is based on the fact that Fitzinger proposed Hylodes twice, each time with a different type- species. Fitzinger (1826) proposed Hy- lodes for Hyla ranoides Spix, 1824, a member of the group later named Elosia by Tschudi (1838), and in 1843 pro- posed Hylodes for Hylodes martinicensis Tschudi, 1838, the type-species of Eleu- therodactyhis Dumeril and Bibron, 1841. I am in complete agreement with Myers ( 1962 ) , because there is no longer any confusion of what Hylodes is — the last author to use it in the sense of Fitzinger (1843) was Melin (1941). We have used Eleutherodactylus as the proper generic name since the early part of this centuiy when Stejneger (1904) pointed out the synonymies of Fitzinger's names. The genus Hylodes (or Ehsia) is a small one; even the least conservative author would not recognize a dozen species. The genus is restricted in distribution, and the species of the genus are rela- tively rare and therefore have not been frequently mentioned in the literature. A nomenclatorial change at the generic level creates relatively little instability even when the generic name used is one that has a junior homonym that is far better known. I do not regard the use of Elosia defensible while there are two older generic names (Hylodes and Eny- drobius) for the group. Megaelosia Miranda-Ribeiro, 1923 (Fig. 110) Megaelosia Miranda-Ribeiro, 1923, Rev. Mus. Paulista, 13:819 [Type-species by moiio- typy, Megaelosia bufonia Miranda-Ribeiro, 1923]. Diagnostic definition. — 9) maxillary teeth very long; 10) alary processes of premaxillae directed sharply posterodor- sally; 11) palatal shelf of premaxilla of moderate depth, palatal process elon- gate; 14) maxillary arch complete, pos- terior end of maxilla expanded, quad- ratojugal present, deep; 16) nasals in contact with maxillae, separated from pterygoids; 20) frontoparietals not fused to prootics; 22) epiotic eminences obso- lete; 23) cristae paroticae broad, stocky; 24) zygomatic ramus of squamosal long, expanded, in broad contact with maxilla; 25) otic ramus of squamosal relatively long, expanded medially into small otic plate; 26) squamosal-maxillary angle about 15°; 28) prevomers moderate- sized, entire, toothed; 29) palatines elon- gate, relatively broad, widely separated medially; 31) anterior ramus of para- sphenoid elongate, narrow, not keeled medially; 32) parasphenoid alae de- flected posteriorly, broadly overlapped laterally by median rami of pterygoids; 33) pterygoids large, anterior rami not reaching middle of orbits; 34) occipital condyles moderately large, not stalked, narrowly separated medially; 35) man- dible bearing a serrated odontoid ridge; 42) males lacking vocal sac and nuptial asperities; 46) larvae with dextral vent; 49) males reach 70 mm., females reach 120 mm. SVL. Composition. — M o n o ty p i c (goeldi); the type-species of the genus is a junior synonym. Disiribution.— The Coastal Ranges of southeastern Brasil (Estados Rio de Janeiro and adjacent Minas Gerais and Sao Paulo). Remarks. — Ever since its separation from Hylodes (Ehsia aiictorum), Megae- losia has been a poorly defined genus. Noble (1931) and Cochran (1955) re- LYNCH: LEPTODACTYLOID FROGS 169 marked that Megaelosia was merely a giant Elosia with somewhat enlarged maxillary teeth. Cochran ( 1955 ) recog- nized the genus because of its greater adult size. Megaelosia has diverged markedly from the other elosiines. The external morphology of M. goeldi compels me to retain it in the Elosiinae. The skull of this monotypic genus is strikingly dif- ferent from those of the other genera of the subfamily (see Figs. 108-10). In contrast to the rather delicate maxillary arch in the other genera of the subfam- ily, Megaelosia has a large, massive max- illa and quadratojugal. The teeth of Megaelosia are fang-like and much larger than those of the other genera of the subfamily. The squamosal architec- ture of Megaelosia is very different from that seen in the other elosiines; the zygo- matic ramus is enlarged and in broad contact with the maxilla, and the otic ramus of Megaelosia is more like that seen in the Grypiscini ( Telmatobiinae ) than that in Hylodes or Crossodactijlus. The very large (compared to those of the other elosiines) occipital condyles of Megaelosia are suggestive that the genus is primitive. In external morphology, Megaelosia goeldi is very similar to Hy- lodes. The tadpoles of the two genera are very difficult to separate. These data suggest that the two genera are indeed related although the skull morphology suggests that the external similarities are convergent or parallel. Leptodactylinae Berg, 1896 ( 1838 ) Cystignathi Tschudi, 1838:78. Cystignathidae: Giindier, 1859a: 26. Pleurodemae Cope, 1866:95. Paludicolina Mivart, 1869:290. Plectromantidae Mivart, 1869:291. Cystignathina: Mivart, 1869:293-94. Leptodactylidae Berg, 1896:161 [A replace- ment name for the Cystignathidae, the type- genus of which is a synonym of Leptodac- tylus]. Cystignathinae: Gadow, 1901:211. PaludicoHdae: Miranda-Ribeiro, 1926:153. LeptodactyHnae: Noble, 1931:504. Pseudopaludicolinae Gallardo, 1965:84. The unifying characteristic of this subfamily is the bony style or osseous plate in the sternum as compared with the cartilaginous sterna of the other lep- todactylids. The group is strictly Neo- FiGURE 110. Lateral, dorsal, and ventral views of skull of Megaelosia goeldi (KU 106271, X 2.3). 170 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY tropical and ranges south to southern Chile and north to the southern United States. For the most part, the group is a lowland component. The widespread genus Leptodactylus rarely reaches ele- \'ations abo\'e 1000 meters. The genus Pleurodema occurs in the Andean system in Chile, Bolivia and southern Peru, and therefore reaches elevations exceeding 4000 meters. Even at these elevations, the group breeds in ponds. The pond- breeding habits of the Leptodactylinae have restricted the dispersal of the group to lower elevations. Many of the species of the subfamily are the wide-spread, common, lowland frogs encountered in most tropical situations in the Americas. The following characteristics of the diagnostic definitions are common to all ten of the included genera : 1 ) sternum containing an osseous element; 2) ver- tebral shield lacking; 3) transverse proc- esses of anterior presacral vertebrae not expanded or shortened; 5) cervical and second vertebrae not fused; 6) cranial bones not involved in dermostosis; 7) omosternum present; manubrium ex- panded in all genera except Paratelma- tobius and PJu/salaemtis; 9) maxillary arch usually toothed, if present, teeth blunt, pedicellate; 11) palatal process of premaxilla long; 20) frontoparietal not fused to prootic; 21) temporal arcade lacking; 23) carotid artery passes dorsal to skull bones; 24) zygomatic ramus of squamosal widely separated from maxil- la; 30) sphenethmoid entire; 35) mandi- ble lacking odontoids; 38) cricoid carti- lage not divided ventrally; 40) m. de- pressor mandihuJae in two slips; 44) pos- terior edge of tongue free; 45) outer metatarsal tubercle present; 47) amplex- us axillary in all observed species. Most herpetologists familiar with the Neotropical fauna have recognized two informal groups of aquatic breeding lep- todactyline frogs — those associated with Leptodactylus (Hydrolaetare, Leptodac- tyhis, Limnomedusa, and Litlwdytes) and those long called "PahidicoUr (En- gystomops, Eupemphix, Paratelmato- hius, PhysaJaemus, Pleurodema, and Pseiidopaludicola). The rare genus Eda- lorhina is usually associated with the lat- ter group but bears considerable resem- blance to Lithodytes. Boulenger (1882) was familiar with most of the generic groups here included in the Leptodactylinae. Hydrolaetare and Paratelmaiohius were described subsequent to his studies. Boulenger in- cluded Enfi,ystomops and Eupempliix in the Bufonidae and incorrectly associated Hylorina with the Leptodactylinae, be- cause he believed that H. sylvatica had a bony sternum. One of the genera rec- ognized by Boulenger was Paludicola, which he considered to be wide-spread and generalized. Mehely (1904) and Parker ( 1927 ) pointed out the hetero- geneity of Boulenger's Paludicola and each proposed a partitioning based on osteological characters. Mehely divided Paludicola into two genera — Paludicola and Pleurodema. Parker (1927) divided it into three genera — Physalaemus, Pleu- rodema, and Pseudopaludicola. Mehely separated Boulenger's Paludicola into one group with prevomerine teeth and a simple (non-bifurcate) sternal style (Pleurodema) and into another group without prevomerine teeth and with a bifurcate sternal style (Paludicola). Nie- den (1923) uncritically followed Me- hely's system and included Edalorhina in Pleurodema. Parker (1927) criticized Mehely's arrangement because relatively few species had been studied; he pro- posed another classification of the palu- dicoline frogs based on loss of the pre- vomerine teeth, loss of the quadratojugal, shape of the sternal style, and the pres- ence of an antebrachial tubercle. Parker (1927) characterized Pseudopaludicola as having an elongate, cartilaginous, or calcified sternum. Virtually all subse- ciuent authors have repeated Parker's characterization of the sternum of Pseu- dopaludicola ( Barrio, 1954, Cochran, 1955, Rivero, 1961, and Gallardo, 1965). Principally on the basis of the cartilagi- nous sternum and breeding habits, Gal- LYNCH: LEPTODACTYLOID FROGS 171 lardo ( 1965 ) proposed a new subfamily for Pseudopahidicola. In the present study, at least one specimen of each of five currently recognized species of Pseu- dopahidicola was cleared and stained. The sternal style is narrow and elongate and is much more dense than the epi- coracoidal cartilages, but is not more dense than the coracoid bones. I con- sider the sternal style of Pseudopahidi- cola to be osseous. Parker (1927) re- ported simple and T-shaped terminal phalanges in frogs of the genus Pseudo- pahidicola. All specimens which I exam- ined have knobbed terminal phalanges. The foam-nesting habits of leptodac- tylines have been known for some time and have been used in the classification of the group ( Noble, 1927, Breder, 1946, Bokermann, 1962). Barrio (1954) first reported the ethological differences be- tween PJn/salaemus and Pseudopahidi- cola. P.seudopaludicola lays its eggs singly or in small clumps in water with- out the benefit of a foam-nest. The spe- cies of Physalaemus (including Engy- stomops and Eupemphix) lay their eggs in a foam-nest floating on water (Fig. 2). Frogs of the genus Leptodactyhis also make foam-nests but there is con- siderable variation within the genus. The species of the melanonotus and ocellatus groups lay their eggs in a foam-nest floating on water, as do Physalaemus and Pleurodema. The species of the pen- tadactylus group differ only slightly in that the foam-nest is deposited in pot holes filled with water along the edges of streams or ponds. The species in the fuscus or sibilatrix group deposit their eggs in a foam-nest in a burrow, and the tadpoles emerge after the nest is inun- dated. This recalls the situation seen in Heleioponis. The frogs of the nmnnora- tus group deposit their few, large eggs in a terrestrial underground incubating chamber in a foam-nest. There are no aquatic larvae. Edalorhina has aquatic larvae (R. Etheridge, in litt.). Repro- ductive data are unavailable for Bary- cholos, Hydrolaetare, Limnomedusa, Lithodytes, and Paratehnatobius. The subfamily Leptodactylinae was defined by Noble ( 1931 ) on the basis of the presence of an osseous style in the sternum. Other authors suggested that the foam-nest habits are characteristic of the subfamily, but these authors mis- takenly believed that Pseudopaludicola is not related to the Leptodactylinae. In view of the appearance and variability of sternal styles and osseous plates else- where among the Salientia, it can be argued that the subfamily Leptodactyli- nae is poorly defined and possibly poly- phyletic (see generic account for Para- telmatohiiis, pp. 182-4). Progressively graduated vicinal similarities of several characters within this group of genera were used to infer relationship through the whole set of genera. The sternum is an osseous plate in Paratelmatohius with a large cartilagi- nous xiphisternum. In the other nine genera of the subfamily, the sternum is a style. In Pleurodema the style is rela- tively broad, and in Limnomedusa, Bary- cholos, Edalorhina, and Physalaemus, the style is only slightly narrower than that of Pleurodema. The sternal style is elongate and narrow in Hydrolaetare, Leptodactyhis, Lithodytes, and Pseudo- paludicola. I consider the presence of a discrete style in the sternum as sound evidence of close relationship. The rela- tionships of Paratelmatohius are obscure — it does not have a bony style in the sternum. The transverse processes of the posterior presacral vertebrae are some- what shortened in Lithodytes, Paratel- matohius, Physalaemus, Pleurodema, and Pseudopaludicola, but are not shortened in Barycholos, Edalorhina, Hydrolaetare, Leptodactyhis, or Limnomedusa. The occipital condyles are relatively large and narrowly separated in Limnomedusa and Pleurodema. Limnomedusa has a type II cervical cotylar arrangement whereas, all other genera of the subfam- ily have a type I cervical cotylar ar- rangement. 172 MISCELLANEOUS PUBLICATIOiX MUSEUM OF NATURAL HISTORY I consider Pleurodema most like the primitive leptodactyline stock because it has a generahzed body form, pectoral architecture, skeleton, and tadpole. Pleurodema is specialized in one inter- esting character — the loss of the quad- ratojugal. Pleurodema is externally sim- ilar to Eupsophus, and the external simi- larity reflects the similarity in the osteol- ogy of these two genera. The two gen- era are readily distinguished by the loss of the quadratojugal in Pleurodema and the presence of a bony style in the ster- num of Pleurodema. The tadpole of Pleurodema has a median vent, 2/3 tooth rows, and a broad anterior interruption of the labial papillae, as do the tadpoles of Eupsophus and Leptodactylus. The tadpoles of Phijsalaemus and Pseudo- paludicola have a dextral vent, 2/3 tooth rows, and a broad anterior interruption of the labial papillae. Noble ( 1931 ) sug- gested that Physalaemiis was the stem genus of the Leptodactylinae, but my study suggests that Pleurodema more ac- curately fills this role. Physalaemus has departed from other leptodactylines in several morphological features, the most striking of which is the hyolaryngeal ap- paratus. Pleurodema Tschudi, (Fig. Ill) 1838 Pleurodema Tschudi, 1838, Class. Batr., p. 47 [Type-species by monotypy, Pleurodenm hibroni Tschudi, 1838]. Leiiipenis Dumeiil and Bibron, 1841, Erpetol- ogie generale, 8:420 [Type-species by monotypy, Leiii penis marmorattis Dumeril and Bibron, 1841]. Fhijsalaemus Fitzinger {non Fhijsalaemus Fitz- inger, 1826), 1843, Syst. Rept., p. 31 [Type-species by original designation, Cijs- tignathus bihroni of Dumeril and Bibron, 1841 { =:Pleurodema bibroni Tschudi, 1838)]. Lystiis Cope, 1868, Proc. Acad. Nat. Sci. Phila- delphia, 20:312 [Type-species by monotypy, Lystiis biachyops Cope, 1868]. Diagnostic definition. — 1 ) sternum bearing a broad, osseous style which tends to bifurcate in large adult females; 3) transverse processes of posterior pre- sacral vertebrae somewhat shortened; 4) cervical cotylar arrangement type I; 7) omosternum cartilaginous, usually not Figure 111. Lateral, dorsal, and ventral views of skull of Pleurodema cinerea (KU 80836, X 4). LYNCH: LEPTODACTYLOID FROGS 173 elongated, manubrium large; 8) sacral diapophyses slightly dilated; 9) maxil- lary arch toothed; 10) alary processes of premaxillae directed posterodorsally, broad at base; 11) palatal shelf of pre- maxilla broad; 12) facial lobe of maxilla deep; 13) palatal shelf of maxilla nar- row, pterygoid process lacking; 14) max- illary arch incomplete, quadratojugal lacking; 15) nasals in median contact, relatively small; 16) nasals not in contact with maxillae or pterygoids; 17) nasals not in contact with frontoparietals; 18) frontoparietal fontanelle large; 19) fron- toparietals not ornamented; 22) epiotic eminences small; 23) cristae paroticae relatively short, narrow; 24) zygomatic ramus of squamosal relatively short; 25) otic ramus of squamosal slightly longer than zygomatic ramus, no otic plate; 26) squamosal-maxillary angle 40-45°; 27) columellae present; 28) prevomers rela- tively large, toothed, narrowly separated medially; 29) palatines relatively nar- row, arched, narrowly separated medial- ly; 30) sphenethmoid large, extending anteriorly to posterior edge of nasals; 31 ) anterior ramus of parasphenoid long, narrow, not keeled medially; 32) para- sphenoid alae oriented at right angles to anterior ramus, broadly separated from median rami of pterygoids; 33) ptery- goids relatively slender, anterior rami long, reaching palatines; 34) occipital condyles large, not stalked, widely sep- arated medially; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate on narrow stalks; 39) m. petro- htjoideiis anterior and m. sternohijoideus insert on lateral edge of hyoid plate; 41) pupil horizontal; 42) males with median subgular vocal sac, nuptial asperities on thumb; 43) lumbar glands present or not; 44) tongue large, round; 45) toes lacking webbing, with lateral fringes or not, metatarsal tubercles spade-like or not, digital tips narrow; 46) larvae with median vent, 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 48) eggs laid in foam-nest in water, small and numerous; 49) adults 35-65 mm. SVL; 50) tympanum visible exter- nally or concealed. Composition. — Ten species are pres- ently recognized: hihroni, brachyops, hufonina, cinerea, darwinii, diplolistris, guayapae, marmorata, nebulosa, and tu- cumanay- The widespread P. hihroni is probably a composite superspecies. Distrihution. — Central Andean Peru south to southern Chile and Argentina and northeastward to Uruguay, along the coastal lowlands of extreme eastern Brasil in non-forested habitats; the arid and semiarid coastal belt from the Guay- anas through Venezuela to the Maricaibo Basin, the islands north of Venezuela, and in the savanas of central Panama. Remarks. — With the exception of P. hrachyops and P. diplolistris, frogs of the genus Pleiirodema are restricted to southern South America and temperate climates; P. diplolisiris occurs in the sub- tropical areas of eastern Brasil, and P. marmorata ranges northward in the high Andes to centi'al Peru. Leiupertis ver- rucosus Reinhardt and Liitken was placed in Pleiirodema by Parker (1927), who was uncritically followed by all subsequent authors. The species is a member of the genus Ischnocnema (Tel- matobiinae, Eleutherodactylini) . Parker (1927) included 18 nominal species in Pleurodema. Since his revi- sion of the genus one new species (guay- apae) has been named; Pleurodema illota is now placed in Eupsophus, and P. mex- icanus is an Eleutlierodactylus. Parker recognized P. pseudopliryne Philippi and P. montevidense Philippi, which are now considered synonyms of P. hihroni and P. dartvinii, respectively. Parker in- cluded Pleurodema coquimhensis in ^^ Donoso-Barros (1969) pointed out that Pleu- rodema bibrotiii Tschudi, 1838, is the same as Pleurodema darwinii Bell, 1843, and that the taxon Dumeril and Bibron ( 1841 ) called Pleu- rodema bihronii is Bufo tliatil Lesson, 1826. Thus Pleurodema bibronii Tschudi applies to the Uruguayan species called P. darwinii, and the correct name for the Chilean frogs called P. bibronii by most authors is P. thaul (Lesson), 1826. 174 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Physalaemus, but Cei (1962a) pointed out that it is a synonym of Pleurodema hibroni. At present, the most pressing sys- tematic problem in the genus Pleuro- dema is the status of the species pres- ently called P. hibroni and P. cinerea. Schmidt (1954b) recognized P. plebeya Philippi for the southern populations now called P. bihroni. Cei (1962a) com- bined the two nominal species but rea- lized that the complex is seriously in need of further study. Pleurodema cin- erea is closely related to P. hibroni; the two species are distinguished only by the external expression of the tympanum (concealed in bihroni, evident in cin- erea). The hibroni-cinerea complex is much in need of a detailed review. Of the ten species of Pleurodema recognized here, five (bihroni, hrachij- ops, hufonina, cinerea, and dancinii) have lumbar or lumbo-inguinal glands. These glands are well-defined, often brightly patterned, and present in both sexes. At least some of these species use the glands in a defense posture. The frog arches its back and tucks its head down thus presenting the large, pat- terned glands to a predator or aggressor. In this position, the glands appear to be large eyes (Cei, 1962a). The lumbar glands are moderate-sized in hibroni, hrachyops, cinerea, and darwinii, and very large in hufonina. Parker ( 1927 ) suggested that the spe- cies of Pleurodema with prevomerine teeth were more primitive than those lacking prevomerine teeth. Like so many other herpetologists of the 19th and early 20th centuries, Parker (1927) regarded the presence or absence of prevomerine teeth as a major character in leptodactylid classification. His pri- mary "key character" in subdividing the genus was the presence or absence of prevomerine (vomerine) teeth. As has been repeatedly pointed out in recent years, the prevomerine teeth are readily lost in many groups of frogs. The teeth may be present but concealed beneath the tissue of the palate ( as in Eleuthero- dactylus myersi) or they may be lost entirely. In most of the cases where the presence of prevomerine teeth has been reported to be variable within a species, I have found that the teeth are present but concealed beneath the tissue of the palate. Main (1957) criticized the use of the presence of prevomerine teeth as the primary character in the division of the species of Crinia into two groups. In four species of Pleurodema (hi- broni, hufonina, cinerea, and marmo- rata), the metatarsal tubercles are not enlarged. In these species, the outer metatarsal tubercle is small and conical and the inner metatarsal tubercle is an elongate oval. In the other six species of the genus, the inner metatarsal tubercle is enlarged, laterally compressed, and spade-like. In these six species, the outer metatarsal tubercle is enlarged and either compressed (hrachyops, diplolis- tris, '^uayapae, and nebulosa) or not (dancinii and tucumana). Pleurodema hibroni and cinerea have a short inner tarsal fold, and hufonina has a long inner tarsal fold; all other species of the genus lack tarsal folds. Pleurodema diplolistris has a prominent tarsal tubercle, much like that seen in many species of Physalaemus. Pleuro- dema nebulosa has a fimbriated anal flap, whereas no other species of the genus has more than a low transverse ridge above the anal opening. The sig- nificance of these characters is not ap- parent at this time, although the pres- ence of a tarsal fold in bihroni, cinerea, and hufonina is suggestive that they are closely related. These three species also agree in having lumbar glands and in having small, non-compressed metatar- sal tubercles. Of the eleven species listed in the genus Pleurodema by Gorham (1966), two are not included in this genus by me: sa<^ittifer O. Schmidt, 1857, is here treated as a species inquierenda, and verrucosus Reinhardt and Liitken, 1862, LYNCH: LEPTODACTYLOID FROGS 175 is placed in the genus Ischnocnema (Tel- matobiinae, Eleutherodactylini ) . Limnomedusa Fitzinger, 1843 (Fig. 112) Limnomedusa Fitzinger, 1843, Syst. Rept., p. 31 [Type-species by original designation, Ciistifinatliu.s inacwglossits Dumeril and Bibron, 1841]. Litopleiira Jimenez de la Espada, 1875, Vert. Viaje Pacif., Batr., p. 82 [Type-species by monotypy, Litopleiira maritimum Jimenez de la Espada, 1875]. Diagnostic definition. — 1 ) sternum bearing a broad osseous style; 3) trans- verse processes of posterior presacral vertebrae not shortened; 4) cervical co- tylar arrangement type II; 7) omoster- num cartilaginous, somewhat elongated, manubrium large; 8) sacral diapophyses round; 9) maxillary arch toothed; 10) alary processes of premaxillae directed dorsally, broad at base; 11) palatal shelf of premaxilla relatively narrow; 12) fa- cial lobe of maxilla moderately deep; 13) palatal shelf of maxilla narrow, pterygoid process small; 14) maxillary arch complete; 15) nasals relatively small, narrowly separated medially; 16) nasals not in contact with maxillae or pterygoids; 17) nasals not in contact with frontoparietals; 18) frontoparietal fontanelle large; 19) frontoparietals not ornamented; 22) epiotic eminences mod- erately large; 23) cristae paroticae short, stocky; 24) zygomatic ramus of squa- mosal short; 25) otic ramus of squamosal long, no otic plate; 26) squamosal-maxil- lary angle about 40°; 27) columellae present; 28) prevomers small, entire, toothed, widely separated medially; 29) palatines slender, widely separated me- dially; 30) sphenethmoid not reaching nasals; 31) anterior ramus of parasphe- noid narrow, not keeled; 32) parasphe- noid alae oriented at right angles to anterior ramus, narrowly overlapped lat- erally by median rami of pterygoids; 33) pterygoids small, all rami slender, an- terior rami long, reaching palatines; 34) occipital condyles large, not stalked, nar- rowly separated medially; 36) terminal phalanges knobbed; 37) hyoid plate Figure 112. Skull of Limnomedusa macroglossa. Dorsal, ventral, and lateral views. (KU 92960, X 3.5). 176 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY lacking alary processes; 39) m. petro- hyoideus anterior and m. sternohijoideus insert on lateral edge of hyoid plate; 41 ) pupil vertical; 42) males with median subgular vocal sac, nuptial asperities on thumb; 43) body free of glands; 44) tongue large, round; 45) toes fringed, basally webbed, metatarsal tubercles not enlarged, digital tips narrow; 46-48); 49) adults less than 60 mm. SVL; 50) tympanum visible externally. Composition. — Two species are rec- ognized: macroglossa and misiones. Distrihution. — Coastal lowlands of southern Brasil, Uruguay, and adjacent Misiones Province, Argentina. In Brasil, the genus is found in Parana, Santa Cata- rina, and Rio Grande do Sul. Remarks. — Frogs of this genus bear considerable external resemblance to Leptodactylus but differ from it in hav- ing vertical pupils, a nuptial pad on the thumb of the male, and a broad sternal style. Limnomedusa differs from all other leptodactylines in having a type II cervical cotylar arrangement. Nothing is known of the breeding biology of the frogs of this genus. The presence of a nuptial pad on the thumb suggests that clasping takes place in water. Hydrolaetare Gallardo, 1963 (Figs. 113-14) Hydrolaetare Gallardo, 1963, Neotropica, 9:42 [Type-species by original designation, Lim- nomedusa schmidti Cochran and Coin, 1959]. Diagnostic definition. — 1 ) sternum bearing an elongate osseous style; 3) transverse processes of posterior pre- sacral vertebrae not shortened; 4) cer- vical cotylar arrangement type I: 7) omosternum large, elongate, cartilagi- nous; 8) sacral diapophyses rounded; 9) maxillary arch toothed; 10) alary proc- esses of premaxillae directed posterodor- sally, broad at base; 11) palatal shelf of premaxilla broad; 12) facial lobe of max- illa deep; 13) palatal shelf of maxilla moderately wide, no pterygoid process; Figure 113. Dorsal and lateral views of skull of Hydrolaetare schmidti (KU 110613, X 3). 14) maxillary arch complete; 15) nasals relatively large, in broad median contact; 16) nasals in broad contact with maxil- lae, separated from pterygoids; 17) na- sals in broad contact with frontopari- etals; 18) frontoparietal fontanelle lack- ing; 19) frontoparietal bearing sagittal crest, slight exostosis; 22) epiotic emi- nences large posteriorly; 23) cristae Figure 114. Ventral view of skull of Hydro- laetare schmidti (KU 110613, X 3). LYNCH: LEPTODACTYLOID FROGS 177 paioticae narrow, relatively short; 24) zygomatic ramus of squamosal elongate; 25) otic ramus of squamosal relatively short, expanded medially into small otic plate; 26) squamosal-maxillary angle about 30°; 27) columella present; 28) prevomers large, toothed, in median con- tact; 29) palatines broad, separated me- dially by anterior ramus of parasphe- noid, bearing odontoid ridge; 30) sphen- ethmoid extending anteriorly to middle of nasals; 31) anterior ramus of para- sphenoid narrow anteriorly, extending to between palatines, not keeled medially; 32) parasphenoid alae deflected pos- teriorly, broadly overlapped by median rami of pterygoids; 33) pterygoids large, anterior rami extending to middle of orbit, prominent ventral flange present; 34) occipital condyles of moderate size, not stalked, widely separated medially; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate wing-like; 39) m. petrolujoicleiis anterior and m. sternohijoideus insert on lateral edge of hyoid plate; 41) pupil vertical; 42) males with median subgular vocal sac, no nup- tial asperities; 43) body lacking glands; 44) tongue large, deeply notched pos- teriorly; 45) toes fully webbed, metatar- sal tubercles not enlarged, digital tips narrow; 46-48); 49) adults large, known specimens 80-105 mm. SVL; 50) tympa- num visible externally. Composition. — Monotypic. Distribution. — A m a z o n i a n South America. Remarks. — Cochran and Coin (1959) named Limnomedusa schmidti on the basis of a single specimen collected near Leticia, Colombia. They pointed out that the new species was strikingly dif- ferent from the other two species of Limnomedusa. Gallardo (1963) reported additional specimens of the species and named a new genus for it (Hydrolaetare). Hydrolaetare and Liimiotnedusa share only two significant characters — vertical pupils and an osseous element in the sternum. Several osteological characters of Hydrolaetare suggest that the genus is allied to the Grypiscini ( Telmatobiinae ) . As in CyclorampJnis and Zachaenus, Hy- drolaetare has a relatively deep maxilla and quadratojugal, the nasals are rela- tively large, in broad median contact, and in broad contact with the maxillae, the nasals are in broad contact with the frontoparietals, the skull lacks a fonta- nelle and has a sagittal crest, the zygo- matic ramus of the squamosal is elon- gate, and the pterygoid bears a ventral flange. Unfortunately, reproductive data are lacking for Hydrolaetare, but the species lacks nuptial pads on the thumb, suggesting that amplexus occurs in ter- restrial situations (as in the Grypiscini). The three genera now included in the Grypiscini have large, cartilaginous ster- na, in contrast to the leptodactyline ster- num of Hydrolaetare. On the basis of the skull alone, I would place Hydro- laetare in the Grypiscini, but the sternal apparatus and striking similarity be- tween Hydrolaetare and Leptodactylus {ocellattis and pentadactylus groups) suggest that the genus is a leptodacty- line. Hydrolaetare lacks one important character of the Grypiscini; the otic ramus of the squamosal of Hydrolaetare is not medially curved to form a broad otic plate. The otic plate of Hydrolae- tare is small and like that seen in the melanonotiis, ocellattis, and pentadacty- lus groups of Leptodactylus. Edalorhina Jimenez de la Espada, 1870 (Fig. 115) Edalorhina Jimenez de la Espada, 1870, J. Sci. Math. Phys. Nat., Lisboa, 3:58 [Type- species by monotypy, Edalorhina perezi Jimenez de la Espada, 1870]. Btihonias Cope, 1874, Proc. Acad. Nat. Sci. Philadelphia, 26:124 [Type-species by monotypy, Btibonias plicifrons Cope, 1874]. Diagnostic definition. — 1 ) sternum bearing broad osseous style; 3) trans- verse processes of posterior presacral vertebrae not shortened; 4) cervical co- tylar arrangement type I; 7) omoster- num elongate, cartilaginous, manubrium large; 8) sacral diapophyses rounded; 178 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 115. Dorsal and lateral views of skull of Edalorhina perezi (KU 124225, X 6.4). 9) maxillary arch toothed; 10) alary processes of premaxillae directed dorsal- ly, moderately wide at base; 11) palatal shelf of premaxilla of moderate width; 12) facial lobe of maxilla deep; 13) pala- tal shelf of maxilla relatively narrow, pterygoid process small; 14) maxillary arch complete; 15) nasals large, in broad median contact; 16) nasals not in con- tact with maxillae or pterygoids; 17) nasals not in contact with frontopari- etals; 18) frontoparietal fontanelle lack- ing; 19) frontoparietals bear large, ex- ostosed, lateral crests; 22) epiotic emi- nences obsolete; 23) cristae paroticae short, stocky; 24) zygomatic ramus of squamosal of moderate length; 25) otic ramus of squamosal as long as zygomatic ramus, no otic plate; 26) squamosal- maxillary angle about 50°; 27) columella present; 28) prevomers relatively small, entire, toothed, separated medially, den- tigerous processes lie posterior to choa- nae; 29) palatines slender, separated me- dially; 30) sphenethmoid short, extend- ing anteriorly to posterior edge of na- sals; 31) anterior ramus of parasphenoid broad, relatively short, not keeled me- dially; 32) parasphenoid alae oriented at right angles to anterior ramus, narrowly overlapped laterally by median rami of pterygoids; 33) pterygoids slender, an- terior rami long, nearly reaching pala- tines; 34) occipital condyles small, not stalked, widely separated medially; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate on narrow stalks; 39) in. petrolnjoideus anterior and 7n. sternohijoideus insert on lateral edge of hyoid plate; 41) pupil horizon- tal; 42) males with median subgular vocal sac, nuptial asperities on thumb; 43) inguinal glands present; 44) tongue large; 45) toes lacking webbing, meta- tarsal tubercles not enlarged, digital tips narrow; 46-48) larvae aquatic; 49) adults small, less than 45 mm. SVL; 50) tym- panum visible externally. Composition. — Two species are cur- rently recognized: nasuta and perezi. Distribution. — Amazonian lowlands of Ecuador and northern and central Peru, and in extreme western Brasil. Remarks. — The genus was reviewed by Dunn (1949), who combined the nominal species huckleiji, perezi, and plicifrons, but noted that the Peruvian population of perezi usually lacks a snout projection, whereas the Ecuadorian pop- ulation has one. Dunn also pointed out that Shreve's (1941) Edalorhina piistu- lata (Pacific lowlands of Ecuador) was not an Edalorhina but is closely related to the Middle American Engijstomops pustulosus. I concur with Dunn but in- clude Engijstomops in Physalaemiis. Parker (1927) and Noble (1931) considered Edalorliina to be merely a Plnjsalaemiis with cranial crests and elongate papillae on the eyelids. Dunn (1949) disagreed and suggested that Edalorhina was more closely related to Pletirodema. I consider the genus to be intermediate between Litlwdytes and Physalaemus. The breeding biology of Edalorliina is unknown and could pro- vide useful clues to the relationships of the genus to the paludicoline leptodac- tylids. LYNCH: LEPTODACTYLOID FROGS 179 Lithodytes Fitzinger, 1843 (Figs. 116-17) Lithodytes Fitzinger, 1843, Syst. Kept., p. 31 [Type-species by original designation, Rana lineata Schneider, 1799]. Diagnostic definition. — 1 ) sternum bearing an elongate osseous style; 3) transverse processes of posterior pre- sacral vertebrae somewhat shortened; 4) cervical cotylar arrangement type I; 7) omosternum bearing an elongate osseous style and large cartilaginous manubrium; 8) sacral diapophyses rounded; 9) max- illary arch toothed; 10) alary processes of premaxillae directed dorsally, broad at base; 11) palatal shelf of premaxilla relatively broad; 12) facial lobe of max- illa relatively deep, not exostosed; 13) palatal shelf of maxilla relatively broad, no pterygoid process; 14) maxillary arch complete; 15) nasals large, in tenuous median contact; 16) nasals not in contact with maxillae or pterygoids; 17) nasals not in contact with frontoparietals; 18) frontoparietal fontanelle lacking; 19) frontoparietals not ornamented; 22) epi- otic eminences small; 23) cristae paroti- cae broad, stocky; 24) zygomatic ramus of squamosal relatively long; 25) otic ramus of squamosal short, expanded me- FiGURE 116. Dorsal and lateral views of skull of Lithodytes lineatus (KU 104340, X 2.6). Figure 117. Ventral view of skull of Lithodytes lineatus (KU 104.340, x 2.6). dially into small otic plate; 26) squa- mosal-maxillary angle about 50°; 27) columella present; 28) prevomers large, entire, toothed, narrowly separated me- dially; 29) palatines relatively narrow, widely separated medially; 30) sphen- ethmoid extending anteriorly to middle of nasals; 31) anterior ramus of para- sphenoid broad, relatively short, not keeled medially; 32) parasphenoid alae deflected posteriorly, short, not over- lapped laterally by median rami of pterygoids; 33) pterygoids slender, an- terior rami long, not reaching palatines; 34) occipital condyles small, not stalked, widely separated medially; 36) terminal phalanges T-shaped; 37) alary processes of hyoid plate on narrow stalks; 39) m. petroJujoideus anterior and m. sterno- hyoideus insert on lateral edge of hyoid plate; 41 ) pupil horizontal; 42) male with median subgular vocal sac, no nuptial asperities; 43) body lacking glands; 44) tongue large, rounded; 45) toes lacking webbing, metatarsal tubercles not en- larged, digital tips dilated, each pad bearing terminal transverse groove; 46- 48); 49) adults medium-sized, to 50 mm. SVL; 50) tympanum visible externally. Composition. — Monotypic. Distrihution. — Edge of the Amazon Basin from Guayana to Bolivia. Remarks. — S e v e r a 1 authors have placed Lithodytes lineatus in Eleuthero- dactijlus. Some did so following Noble (1917), who ignored the presence of 180 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY osseous styles in the oniostenuim and sternum and placed extra weight on the presence of T-shaped terminal phalan- ges. Ruthven (1919) effectively rejected Noble's arguments. Rana lineata Schneider has been fre- quently confused with Hylodes lineatus Brocchi. The latter is a Guatemalan spe- cies of Eleiitherodactylus and bears no resemblance to the Amazonian Litho- chjtes lineatus. Litlwdytes lineatus bears considerable superficial resemblance to some species of the Eleutlierodactylus jitzingeri group. Dunn ( 1931 ) named Litlwdytes gaigeae (erroneously spelled gaigei), a species found in Costa Rica and Panama, and Piatt (1934) correctly pointed out that gaigeae was a species of Eleutherodactylus. The two species are strikingly similar in color pattern. The skull of Lithodytes bears con- siderable resemblance to those of the paludicoline genera, but the sternal style is elongate, like that of Leptodactylus. The hyolaryngeal apparatus of Litlw- dytes is like that seen in Edalorkina, Leptodactylus, and Pleurodema. Nothing is known of the breeding biology of Lithodytes, but the lack of nuptial asper- ities suggests that the genus clasps on land and may exhibit direct develop- ment like the species of the Leptodac- tylus marmoratus group. Physalaemus Fitzinger, 1826 (Figs. 118-19) Physalaemus Fitzinger, 1826, Neue Class. Rept., p. 39 [Type-species by monotypy, Physa- laemus cuvieri Fitzinger, 1826]. Paludicola Wagler, 1830, Syst. Amph., p. 206 [Type-species by monotypy, Bujo albifrons Spiz, 1824]. Gomphobates Reinhardt and Liitken, 1862, Vid. Meddel. Naturh. Foren., 1861:172 [Type- species by monotypy, Gomphobates notatus Reinhardt and Liit]TO (manuscript name) of Gomphobates fusco- maculatus Steindachner; this generic name is invahd and not available]. Engystomops Jimenez de la Espada, 1872, An. Soc. Espanola Hist. Nat., 1:86 [Type- species by monotypy, Engystomops petersi Jimenez de la Espada, 1872]. Microphryne W. Peters, 1873, Mtber. k. Preuss. Akad." Wiss. Berlin, 1873:616 [Type-species by monotypy, Paludicola (Microphryne) pustulosa Cope, 1864]. Peralaimos Jimenez de la Espada, 1875, Vert. Viaje Pacif. Batr., p. 163 [Type-species by monotypy, Bujo stentor Jimenez de la Es- pada, 1872]. Diagnostic definition. — 1 ) sternum bearing relatively broad osseous sternal style; 3) transverse processes of posterior presacral vertebrae somewhat shortened; 4) cervical cotylar arrangement type I; 7) omosternum elongate, cartilaginous, manubrium small to large; 8) sacral diapophyses slightly dilated; 9) maxil- lary arch toothed or not; 10) alary proc- esses of premaxillae directed dorsally or slightly anterodorsally, relatively narrow at base; 11) palatal shelf of premaxilla relatively broad; 12) facial lobe of maxil- la short, of moderate depth; 13) palatal shelf of maxilla narrow, no pterygoid process; 14) maxillary arch complete; 15) nasals relatively large, in broad median contact; 16) nasals not in contact with maxillae or pterygoids; 17) nasals not in contact with frontoparietals; 18) fronto- parietal fontanelle lacking; 19) fronto- parietals not ornamented; 22) epiotic eminences small; 23) cristae paroticae short, stocky; 24) zygomatic ramus of squamosal short; 25) otic ramus of squa- mosal short, no otic plate; 26) squa- mosal-maxillary angle about 60°; 27) columella present; 28) prevomers entire, small, usually toothless, widely separated medially; 29) palatines long, slender, widely separated medially; 30) sphen- ethmoid extending anteriorly beneath posterior part of nasals; 31) anterior ra- mus of parasphenoid narrow, not keeled medially; 32) parasphenoid alae oriented at right angles to anterior ramus, nar- rowly separated from or narrowly over- LYNCH: LEPTODACTYLOID FROGS 181 Figure 118. Lateral, dorsal, and ventral views of skull of Physalaemus pustulosus (KU 68271, X 4.7). Figure 119. Lateral, dorsal, and ventral views of skull of Physalaemus ephippifer (KU 93005, X 4.7). 182 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY lapped laterally by median rami of ptery- goids; 33) pterygoids slender, rami long, anterior rami reaching palatines; 34) oc- cipital condyles small, on short stalks, widely separated medially; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate broad and wing-like; 39) m. petrohyoideus anterior and m. sterno- hijoideus insert on hyoid plate near mid- line; 41) pupil horizontal; 42) males with large external subgular vocal sacs, tending to bilobe, males with nuptial pads on thumb; 43) parotoid glands present or absent, inguinal glands pres- ent or absent, flank glands present or absent; 44) tongue relatively narrow; 45) toes free of webbing and lateral fringes, tarsus bearing tubercle on inner edge or not, metatarsal tubercles en- larged and spade-like or not, digital tips narrow; 46) larvae with dextral vent, 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 48) eggs small, numerous, laid in foam nest floating on water; 49) adults range in size from 17- 60 mm. SVL; 50) tympanum usually concealed, visible externally in pustu- lattis. Composition. — With the combination of the nominal genera Engystomops, Eu- pemplux, and Physahemiis into a single genus, Physahemiis is one of the larger genera of leptodactylids. I recognize 34 nominal species (aguirrei, albifrons, albo- notatiis, harrioi, biligonigerus, centralis, cicada, cuvieri, enesefae, ephippifer, evangelistai, fernandezae, ftiscomacula- tus, gracilis, henseli, kroeyeri, jordanen- sis, macidiventris, moreirae, nanus, nat- tereri, ohtectus, olfersi, paraenHs, peter- si, pustulattis, pustulosus, riograndemis, santafecinus, schereri, signiferus, soaresi, stentor, and ternetzi). Distribution. — Southern Mexico to Argentina in lowland non-forested re- gions (and through second growth and occasionally primary forest) except for the very arid Pacific lowlands south of Ecuador and over most of central and southern Argentina and Chile. Remarks. — In a separate paper, I (Lynch, 1970b) justified the combination of Engystomops, Eupemphix, and PJiy- salaemus. In that paper I suggested the recognition of at least four species groups — the petersi group, the maculi- ventris group, the curvieri group, and the fuscomaculatus group. Physalaemus has the criniine pattern of insertion of the hyoid musculature on the hyoid plate. The only other Neo- tropical leptodactyhds with this pattern are the species of the Leptodactylus marmoratus group and the genus Pseu- dopaludicola, although the hyoid plate of Hydrolaetare is like that seen in Phy- salaemus and Pseudopaludicola. For the present I consider Physalaemus and Pseudopaludicola to be relatively closely related but realize that the two genera differ in many respects. In some char- acteristics Physalaemus is closest to Lep- todactylus and Pleurodema, but in others it is closer to Edalorhina, Lithodytes, and Paratelmatobius. Paratelmatobius B. Lutz and Carvalho, 1958 (Fig. 120) Paratelmatobius B. Lutz and Carvalho, 1958, Mem. Inst. Oswaldo Cmz, .56:241 [Type- species by original designation, Paratclrnato- hius lutzi B. Lutz and Car\'alho, 1958]. Diagnostic definition. — 1 ) sternum bearing a broad osseous plate; 3) trans- verse processes of posterior presacral vertebrae shortened; 4) cervical cotylar arrangement type I; 7) omosternum present, small, cartilaginous, manubrium minute; 8) sacral diapophyses dilated; 9) maxillary arch toothed; 10) alary processes of premaxillae directed dorsal- ly, narrow at base; 11) palatal shelf of premaxilla broad; 12) facial lobe of max- illa shallow, expanded in snout region; 13) palatal shelf of maxilla broad, ptery- goid process moderate-sized; 14) maxil- lary arch complete; 15) nasals small, narrow, separated medially; 16) nasals not contacting maxillae or pterygoids, nasal with elongate maxillary process which nearly reaches maxilla; 17) nasals LYNCH: LEPTODACTYLOID FROGS 183 not in contact with frontoparietals; 18) frontoparietal fontanelle moderate-sized; 19) frontoparietals not ornamented; 22) epiotic eminences well defined; 2-3) cris- tae paroticae short, stocky; 24) zygo- matic ramus of squamosal relatively long, slender; 25) otic ramus of squa- mosal short, curved medially to form small otic plate; 26) squamosal-maxil- lary angle about 55°; 27) columella absent; 28) prevomers small, entire, toothed, widely separated medially; 29) palatines thin, elongate, broadly sep- arated medially; 30) sphenethmoid ex- tending anteriorly to middle of nasals; 31) anterior ramus of parasphenoid broad, short, lacking median keel; 32) parasphenoid alae short, narrow, de- flected posteriorly, not overlapped later- ally by median rami of pterygoids; 33) pterygoids small, median rami short, anterior rami not reaching palatines; 34 ) occipital condyles large, not stalked, widely separated medially; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate on narrow stalks; 39) m. petrohyoideus anterior and m. sterno- hyoideiis insert on lateral edge of hyoid plate; 41) pupil horizontal; 42) males lacking vocal sac, nuptial pads on first two fingers; 43) body lacking glands; 44) tongue large, round; 45) toes fully webbed, metatarsal tubercles not en- larged, digital tips narrow; 46-48); 49) adults small, less than 30 mm. SVL; 50) tympanum concealed. Composition. — Two species are pres- ently known (Ititzi and gaigeae). The latter was named P. pictiventris A. Lutz in B. Lutz and Carvalho (1958) but is a nomen nudum and an obligate synonym of Leptodactylus gaigeae Cochran, 1938. Distribution. — The coastal ranges in Estado Rio de Janeiro, Brasil. Remarks. — Aldopho Lutz collected the first specimens of this genus in De- cember 1931. He made water color sketches of the two specimens and noted that they represented a new species of Faludicola or Eupemphix. However, he never described the specimens or other- wise published on them. Cochran (1938) who received these two speci- mens, named and described them as Figure 120. Lateral and dorsal (KU 107089) and ventral (KU 92981) views of skulls of Paratelma- obius littzi. All X 8. 184 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Leptodactylus gaigeae. She suggested that the species was related to L. mar- moratus and served as a generic link between Leptodactylus and Zachaenus. Lutz and Carvalho ( 1958 ) discovered a new species allied to the frogs collected by A. Lutz nearly 30 years before and named it as a new genus and new spe- cies, Paratehnatohius lutzi; at the same time they published A. Lutz's figures of the other species and used his manu- script name, P. pictiventris, for them. They suggested that Paratehnatohius was intermediate between the endemic southeastern Brasilian genus Cycloram- phus and the Andean Tehnatohius. The architecture of the otic ramus of the squamosal of Paratehnatohius is identical to that seen in the Grypiscini, and the four genera bear considerable external resemblance to one another. The sternal plate in Paratehnatohius is not like the sternal style seen in the lep- todactylines but appears to be an ossifi- cation of the sternal plate — an advance- ment over the calcification of the same element seen in old individuals of a variety of leptodactylid genera and spe- cies. Nevertheless, Paratelmatohius dif- fers in several osteological characters from the Grypiscini — the presence of a frontoparietal fontanelle, the wide me- dian separation of the nasals, the absence of a ventral flange on the pterygoid. In summary, Paratehnatohius is os- teologically intermediate between the Leptodactylinae and the Grypiscini (Telniatobiinae). This might be re- garded as some evidence for polyphyly of the Telmatobiinae since one group of Telmatobiinae (i.e., Alsodini) undoubt- edly gave rise to the Leptodactylinae and I am here pointing out the possibil- ity of genetic relationship between Para- tehnatohius and the Grypiscini. The squamosal architecture of Paratehnato- hius and the Grypiscini may be a parallel (or convergent) development rather than a result of relationship. The ap- pearance of a very similar otic plate in Megaelosia (Elosiinae) is very sugges- tive that the appearance of this sort of otic ramus is a labile feature and should not be used in primary inferences of relationships. In the Grypiscini, several other osteological characters combine to render this character confirmatory and therefore it is used in the diagnosis of that group (p. 135). I am tentatively assigning Paratehnatohius to the Lepto- dactylinae. In several respects the genus bears some similarity to Physalaemus, although I do not regard the relationship (if any) to be close. The presence of nuptial asperities and a frontoparietal fontanelle, although small, in Paratehnatohius suggest that the genus is not allied with the Eleu- therodactylini. The nature of the oc- cipital condylar-cervical articulation as well as a variety of other osteological and external characters does not permit its association with the Ceratophryinae, Alsodini, Odontophrynini or Telmato- biini. The Elosiinae is a compact group, and the external and many internal fea- tures serve to illustrate the lack of cor- respondence between Paratehnatohius and the Elosiinae. If a new family group is not proposed for this small genus, then the genus must belong to the Giypiscini or the Leptodactylinae. I have fewer difficulties associating it with the latter, perhaps because the latter is a more heterogeneous group. The presence of an osseous plate in the sternum, al- though it is rather unlike the sternal style seen in the other genera of the subfamily, is not contrary to the diag- nostic feature of the subfamily. No other leptodactylid known to me normally pos- sesses an osseous post-zonal element. Although the presence of an osseous post-zonal sternal element is the only uniform character in the subfamily, I consider the subfamily to be monophy- letic (see the generic account of Hydro- laetare for further comment). Pseudopaludicola Miranda-Ribeiro, 1926 (Fig. 121) Pseudopahidicola Miranda-Ribeiro, 1926, Arch. Mus. Nac. Rio de Janeiro, 27:152 [Type- LYNCH: LEPTODACTYLOID FROGS 185 Figure 121. Lateral, dorsal, and ventral views of skull of Pseudopahidicola falcipes (KU 93068, X 8). species by monotypy, Liuperus (sic) falcipes Hensel, 1867]. Diagnostic definition. — 1) sternum bearing an elongate, osseous or calcified style; 3) transverse processes of posterior presacral vertebrae shortened; 4) cervi- cal cotylar arrangement type I; 7) omo- sternum elongate, cartilaginous, manu- brium small; 8) sacral diapophyses rounded; 9) maxillary arch toothed; 10) alary processes of premaxillae directed dorsally, broad at base; 11) palatal shelf of premaxilla broad; 12) facial lobe of maxilla shallow; 13) palatal shelf of maxilla narrow, no pterygoid process; 14) maxillary arch incomplete, quadrato- jugal absent; 15) nasals small, widely separated medially; 16) nasals not in contact with maxillae or pterygoids; 17) nasals not in contact with frontoparietals; 18) frontoparietal fontanelle absent, frontoparietals usually narrowly sepa- rated for entire length; 19) frontopari- etals not ornamented; 22) epiotic emi- nences obsolete; 23) cristae paroticae very short, broad; 24) zygomatic ramus of squamosal relatively short; 25) otic ramus of squamosal long, expanded me- dially into narrow otic plate; 26) squa- mosal-maxillary angle 50-60°; 27) colu- mella present; 28) prevomers small, re- duced to sliver-like elements, dentiger- ous rami lost, widely separated medially; 29) palatines narrow, sliver-like, in con- tact with maxillae, widely separated me- dially; 30) sphenethmoid very short, ex- tending anteriorly to posterior edge of nasals; 31) anterior ramus of parasphe- noid narrow, not reaching palatines, not keeled medially; 32) parasphenoid alae long, oriented at right angles to anterior ramus of parasphenoid, narrowly sepa- rated from median rami of pterygoids; 33) pterygoids small, median and pos- terior rami minute, anterior rami long, reaching to palatines; 34) occipital condyles small, stalked, widely sep- arated medially; 36) terminal phalanges knobbed; 37) alary processes of hyoid plate wing-like; 39) m. petwhyoideus 186 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY anterior and m. sternohyoideus insert on hyoid plate near midline; 41 ) pupil hori- zontal; 42) males with bilobed subgular vocal sac, nuptial asperities lacking; 43) body lacking glands; 44) tongue large, oval; 45) toes lacking webbing and lat- eral fringes, metatarsal tubercles not en- larged, digital tips narrow; 46) larvae with dextral vent, 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 48) eggs small, numerous, laid singly or in small clumps attached to submerged vegetation; 49) males reach 16 mm., fe- males reach 19 mm. SVL; 50) tympanum concealed; 51 ) the antebrachial tubercles are generically unique. Composition. — Parker (1927) recog- nized five species of the genus (ameg- hini, boliviana, falcipes, pusilh, and sal- tica). Bokermann ( 1966 ) recognized five species in the coastal lowlands of eastern and southern Brasil (ameghini, falcipes, mystacalis, saltica, and ternetzi), which Milstead (1963) had pronounced identical. I consider boliviana and pusil- la to be conspecific ( see "Remarks" ) and recognize six species (ameghini, falcipes, mystacalis, pusilh, saltica, and ternetzi). Distribution. — The coastal lowlands of Brasil from Bahia to northeastern Argentina; Amazonian Bolivia, Paraguay, and Venezuela, and in the coastal ranges of Venezuela and the Santa Marta moun- tains of Colombia. Remarks. — The genus Pseudopaludi- cola gained wide acceptance through the work of Parker (1927) and Barrio (1954). Parker included five species in the genus and considered two of these (boliviana and pusilla) to have T-shaped terminal phalanges. All species of the genus have elongate, knobbed terminal phalanges and agree in all details of skull ossification. Parker incorrectly characterized the genus as having a cartilaginous sternum (see account of pectoral girdles, pp. 58-60) and has been followed by all subsequent authors. I include the genus in the Leptodacty- linae and consider it closely related to the paludicoline genera in spite of the ethological differences pointed out by Barrio ( 1954 ) . The structure of the hyolarynx of Pseudopahidicola is not greatly different from that of Physalae- mus but very different from that of all other Neotropical leptodactylids except Ilydrolaetare and the Leptodactylus mar- moratus group. The species of this genus are readily distinguished from all other small lepto- dactylid frogs by their slender habitus, lack of digital webbing, unexpanded digital tips, concealed tympanum, and the presence of an antebrachial tubercle. The skeletons of the five nominal spe- cies available to me are indistinguish- able. Parker separated boliviana and pu- silla on slight differences in leg length and coloration. I tentatively consider the two nominal species identical because I am unable to separate paratypes and topotypic material of each from one another. Rivero ( 1961 ) reported "pusil- la" from Amazonian Venezuela and Parker (1935) reported "Z?o/iu/ana" from British Guiana and Paraguay. In view of the ethological differences recently discovered between the Brasilian species (W. C. A. Bokermann, pers. comm.), it might prove premature to combine the cis-Andean populations of Pseudopaludi- cola as a single species. The specimens examined by me represent a single mor- phological species. The Brasilian species were pronounced conspecific by Mil- stead ( 1963 ) . Bokermann has since examined most of the types of this genus and is familiar with all of the Brasilian species in the field; he informs me that most of the previously named kinds rep- resent valid species, and there are yet undescribed species living in the coastal lowlands of southeastern Brasil. All of the Brasilian species can be separated on the basis of call, leg length, and color pattern. Leptodactylus Fitzinger, 1826 (Figs. 122-24) Leptodactylus Fitzinger, 1826, Neue Class. Rept., p. 38 [Type-species by subsequent LYNCH: LEPTODACTYLOID FROGS 187 designation, (Fitzinger, 1843), Leptodac- tijlus typhonia ( ^Rana typhonia Daudin, 1803, non Rana typhonia Linno, 1758). Rami typhonia Daudin is R. sihilatrix Wied, 1824, which Heyer (1968) considered iden- tical witli Rana fusca Schneider, 1799, for which lie designated a neotype. However, at least some of tlie syntypes of Rana fusca are extant (W. C. A. Bokerniann, pers. conim.), and study of these must be made before Heyer's action can be accepted]. Cystignathiis Wagler, 1830, Syst. Amph., p. 202 [Type-species by present designation, Rana mystacea Spix, 1824]. Gnathophysa Fitzinger, 1843, Syst. Rept., p. 31 [Type-species by original designation, Rana hihyrinthica Spix, 1824]. Sihilatiix Fitzinger, 1843, Ibid., p. 31 [Type- species by original designation, Cystigna- thus gracilis Dumeril and Bibron, 1841]. Plectromantis W. Peters, 1862, Mtber. k. Preuss. Akad. Wiss. Berlin, 1862:232 [Type-species by monotypy, Plectromantis wagneri W. Peters, 1862]. Adenomera Steindachner, 1867, Reise Novara, Zool. Amph., p. 37 [Type-species by mono- typy, Adenomera marmorata Steindachner, 1867]. Entomoglossus W. Peters, 1870, Mtber. k. Preuss. Akad. Wiss. Berlin, 1870:647 [Type- species by monotypy, Entomoglossus pustii- latus W. Peters, 1870]. Pachypiis A. Lutz, 1930, Mem. Inst. Oswaldo Cruz, 23:22 [Proposed as a subgeneric name of Leptodactylus; no type-species was designated. Preoccupied by Pachypus Bill- berg, 1820 (Insecta: Coleoptera), Pachy- pus d' Alton, 1840 (Mammalia), and Pachy- pus Cambridge, 1873 ( Arachnida)]. Cavicola A. Lutz, 19.30, Ibid., 23:22 [Proposed as a subgeneric name of Leptodactylus; no type-species was designated. Preoccupied by Cavicola Ancey, 1887 (Mollusca)]. Parvulus A. Lutz, 1930, Ibid., 23:22 [Proposed as a subgeneric name in Leptodactylus; type-species by subsequent designation (Parker, 1932:342), Leptodactylus nanus L. Muller, 1922]. Diagnostic definition. — 1) sternum bearing an elongate osseous style; 3) transverse processes of posterior presa- cral vertebrae not shortened; 4) cervical cotylar arrangement type I; 7) omo- sternum large, elongate, cartilaginous, manubrium large; 8) sacral diapophyses rounded; 9) maxillary arch toothed, teeth frequently pointed; 10) alary proc- FiGURE 122. Lateral, dorsal, and ventral \iews of skull of Leptodactijlus quadriiittatus (KU 41030, X 4), a member of the fuscus group. 188 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY esses of premaxillac directed dorsally or posterodorsally. broad at base; 11) pala- tal shelf of premaxilla moderately broad; 12) facial lobe of maxilla relatively shal- low, entire maxilla same depth anterior to end of tooth row; 13) palatal shelf of maxilla relatively narrow, no pterygoid process; 14) maxillary arch complete; 15) nasals large, narrowly separated medially; 16) nasals usually not in con- tact with maxillae, never in contact with pterygoids, nasals have elongate maxil- lary processes in most species; 17) na- sals not in contact with frontoparietals; 18) frontoparietal fontanelle lacking; 19) frontoparietals bearing some orna- mentation posteriorly in old adults of the larger species; 22) epiotic eminences well defined posteriorly; 23) cristae paroticae moderately long, somewhat stocky; 24) zygomatic ramus of squa- mosal somewhat expanded, relatively short; 25) otic ramus of squamosal slight- ly longer than zygomatic ramus, ex- panded into narrow otic plate which usually rests tenuously on crista paro- tica; 26) squamosal-maxillary angle less than 45°; 27) columella present; 28) prevomers large, entire, toothed, nar- FiGURE 123. Dorsal views of skull of (top) Leptodactyltis pentadactyliis ( KU 68159, X D and L. wagncri (KU 104389, X 1). rowly separated medially; 29) palatines broad, narrowly separated medially, sometimes bearing odontoid ridge; 30) sphenethmoid extending anteriorly to middle of nasals in marmoraius, mela- nonotus, oceUatiis, and pentadactyliis groups, extending anteriorly to a point anterior to nasals and usually anterior to premaxillac in fuscus group; 31) anterior ramus of parasphenoid narrow, not keeled medially, reaching to palatines; 32) parasphenoid alae deflected pos- teriorly, narrowly overlapped laterally by median rami of pterygoids in fuscus, melanonotus, oceUatus, and pentadac- tyliis groups, separated in the marmora- tiis group; 33) pterygoids slender, an- terior rami reaching to middle of orbit; 34) occipital condyles moderate-sized, not stalked, moderate to wide median separation; 36) terminal phalanges knobbed; 37) alary processes of hyoid on narrow stalks in fuscus, melanonotus, oceUatus, and pentadactyliis groups, wing-like in mannoratiis group; 39) m. petrohyoideus anterior and m. sterno- hyoideus insert on lateral edges of hyoid plate in fuscus, melanonotus, oceUatus, and pentadactyliis groups, insert on hyoid plate near midline in marmoratus group; 41) pupil horizontal; 42) males with median subgular or paired lateral vocal sacs or none, males of fuscus and marmoratus groups lack nuptial asperi- ties, males of 7nelanonotus, oceUatus, and pentadactyliis groups have spines on the thumb, males of the pentadactyliis group have spines on the chest and thumb; 43) body with diffuse venti'al and flank glands or not, many species have glan- dular folds on the dorsum, species of the pentadactyliis group have inguinal glands; 44) tongue large, with two long posterior horns; 45) toes not webbed, species of the melanonotus and oceUatus groups have lateral fringes on the toes, metatarsal tubercles not enlarged, digital tips narrow, first finger slightly longer than second in marmoratus group, much longer than second in other species groups except for a few species in the LYNCH: LEPTODACTYLOID FROCS 189 melanonotus group; 46) frogs of mar- moratus group do not have tadpoles, in other groups larvae with median vent, 2/3 tooth rows, labial papillae broadly interrupted anteriorly; 48) eggs laid in foam nest floating on water in mela- nonotus, oceUatus, and pentadactijJtis groups, in these groups the eggs are small and numerous; in the fiisciis group eggs are deposited in a foam nest in an underground burrow and hatch when the nest is inundated; in the marmoratus group the eggs are large, few in number, and are deposited in an underground nest in foam; development is direct in the marmoratus group but the other groups have aquatic larvae; 49) adults range in size from 20-200 mm. SVL; 50) tympanum visible externally or concealed. Composition. — Gorham (1966) listed 60 species in the genus. Of these, three belong to other genera (L. gaigeae^= Paratelmatobius gaigeae; L. pulcherz= Barycholos pulcher; L. tubercluosus:= Ischnocnema quixensis). Heyer (1969a) recognized only 32 species. His system is admittedly conservative, but is a con- siderable improvement over that pre- sented by Gorham. Distribution. — Middle American low- lands from Sonora, Mexico, and southern Texas to the Argentine Chaco and Gua- yas region of Ecuador in South America, and on the Lesser Antilles and Hispani- ola. All localities for the species of the genus are lowland (usually below 1200 meters ) . Remarks. — No new generic synonyms are added here. The generic synonymy of Leptoclactylus has been stable for many decades, because the genus is rather morphologically uniform in ex- ternal characteristics. Heyer ( 1969a ) solved many systematic problems of the genus, among which was the discovery of the identity of Plectromantis wagneri. This species is a widespread species of the Amazon Basin and has accumulated nearly a dozen synonyms. I studied the skeletons of 18 species of the genus in formulating my concepts Figure 124. Lateral, dorsal, and ventral views of skull of Leptodactylus hijlaedactyhis (KU 119387, X5). 190 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY of the genus. This study illustrated the remarkable osteological homogeneity of the frogs of this genus. Accordingly, I do not advocate the use of subgenera such as those proposed by A. Lutz ( 1930 ) . Lutz placed the species of the genus in six subgenera; of these, two are generic homonyms, one is a valid generic name of Asiatic ranids (Phityniantis), and one (Plectromantis) was based on erroneous data. A major advancement in the system- atics of this genus was provided by Heyer, who divided the genus into five species groups based on external mor- phology, thigh musculature, jaw muscu- lature, developmental patterns and tad- pole morphology, some osteological characters, and vocalization. Heyer util- ized secondary sex characters in his classification; his classification appears to be a realistic one. I contend that his meJononotus group is a composite with part of the species (those with arched prevomerine dentigerous processes of the prevomerine bones) being members of the oceUatus group. Heyer advocated placing the mar- moratus group in a separate subgenus, Adenomera; this action is one of prefer- ence, but in keeping with the criteria followed throughout this review of the family, I choose not to recognize the subgenus. The frogs of the subgenus Adenomera differ from those of the sub- genus Leptodactijhis in that the former exhibit direct development whereas the latter have aquatic tadpoles. Heyer cited additional characteristics to distin- guish the marmoratus group from other Leptodactyhis but these additional char- acters are shared by some other species groups. The musculature of the hyo- larynx of the frogs of the marmoratus group is like that seen in FhysaJaemus and Pseudopahidicola (the criniine pat- tern). The frogs of the marmoratus group resemble Barycliolos pidclier (see following account) in some but not all morphological characters. When the breeding biology of all of the genera of the Leptodactylinae becomes known, the generic status of Adenomera and Bary- cholos should become more apparent. Barycholos Heyer, 1969 (Fig. 125) Banjcholos Heyer, 1969, Cont. Sci. Los Angeles Co. Mus., 155:6 [Type-species by original designation, Leptoclactijhis ptilcher Boulen- ger, 1898]. Diagnostic definition. — 1) sternum containing a calcified style, bifurcate posteriorly; .3) transverse processes of posterior presacral vertebrae slightly shortened; 4) cervical cotylar arrange- ment type I; 7) omosternum moderate- sized, manubrium elongate, partly calci- fied; 8) sacral diapophyses slightly di- lated; 9) maxillary arch toothed; 10) alary processes of premaxillae directed dorsally, broad at base; 11) palatal shelf of premaxilla relatively deep, deeply in- cised; 12) facial lobe of maxillae rela- tively shallow; 13) palatal shelf of maxil- la broad anteriorly, narrowing posterior- ly, no pterygoid process; 14) maxillary arch complete; 15) nasals large, in broad median contact; 16) nasals narrowly sep- arated from maxillae, widely separated from pterygoids; 17) nasals in tenuous contact with frontoparietals; 18) fronto- parietal fontanelle lacking; 19) fronto- parietals not ornamented; 22) epiotic eminences moderately well defined; 23) cristae paroticae relatively short, stocky; 24) zygomatic ramus of squamosal rela- tively short, broadly separated from maxilla; 25) otic ramus of squamosal relatively long, expanded medially to form small otic plate; 26) squamosal- maxillary angle 55°; 27) columella pres- ent; 28) prevomers small, irregular in outline, widely separated medially, bear- ing large, arched, transverse, toothed, dentigerous processes; 29) palatines slender, lacking odontoid ridge; 30) sphenethmoid entire, extending anterior- ly beneath nasals; 31) anterior ramus of parasphenoid narrow, not keeled, reach- ing prevomerine dentigerous processes; 32) parasphenoid alae oriented at right LYNCH: LEPTODACTYLOID FROGS 191 angles to anterior ramus, not overlapped laterally by median rami of pterygoids; 33) pterygoids small, all rami slender, anterior rami not reaching middle of orbit; ;34) occipital condyles small, not stalked, widely separated medially; 36) terminal phalanges T-shaped; 37) alary processes of hyoid plate small, on nar- row stalks; 38-39); 41) pupil horizontal; 42) males lacking nuptial asperities, vocal sac large, external, median, sub- gular; 43) body lacking glands; 44) tongue round, posterior edge free; 45) toes lacking webs and lateral fringes, outer metatarsal tubercle present, inner metatarsal tubercle not enlarged, digital tips dilated, no circumferential groove on discs, first finger much longer than second; 46-48); 49) adults small, about 25 mm. SVL; 50) tympanum visible externally. Composition. — Monotypic, B. ptil- cher. Distribution. — Pacific lowlands of Ecuador (Heyer, 1969b). Remarks. — In external appearance, Barijcholos pulcher is simply a small Leptodactijlus of the marmoratus group. Heyer ( 1969b ) concluded that Barij- cholos is not closely allied to Leptodac- tylus or Lithodijtes, but is most closely related to Eletitlierodactyhis. He did not consider the relationship between Barij- cholos and Eleutlierodactijlus to be close. Barijcholos pulcher exhibits the fol- lowing characteristics which are more Eleutherodactijlus-\ike than Leptodacty- lus-Mke: 11)," 15), 22), 32), and 36). Barycholos more closely resembles Lep- fodactylus in the following characteris- tics: 1), 13), and 45). Heyer (1969b) suggested that the life history of Bara- chijlos is more like that of Eleutherodac- tijlus than Leptodactyliis. Heyer exam- ined a single adult female of Barycholos pulcher which contained 43 ova about 2.8 mm. in diameter and concluded that the species probably exhibits direct de- velopment. I agree with Heyer on this point, but do not agree that this charac- ter, even in coincidence with T-shaped terminal phalanges, indicates a closer relationship to Eleutlierodactijlus than to Leptodactijlus. Heyer ( 1969a ) char- acterized the marmoratus group of Lep- todactijlus in having "4-25 eggs per nest; egg diameter 2.1-3.0 mm." In preserved L. hylaedactijlus, females usually con- tain about 20 eggs. The species of the marmoratus group were assigned to the subgenus Adenomera by Heyer ( 1969a, 1969b); the subgenus was in large part defined on the basis of direct develop- ment. As pointed out by Cochran ( 1955: 309), species of the marmoratus group Figure 125. Dorsal and ventral views of skuU of Barycholos pulcher (UMMZ S-2881, X 5.7). 192 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY have enlarged digital pads and some in- dication of T-shaped terminal phalanges. The phalanges are intermediate between the knobbed phalanges of the subgenus Leptodactyhis and the distinctly T- shaped phalanges of Eleiitlwrodactylus, Heleopliryne, Litliodytes, SmintliiUus, Syrrliopluis, Taudactyhis, and Tomodac- tyltis. BarycJiolos more closely resem- bles the subgenus Adenomera than Eleu- therodactyJus. Direct development has appeared several times in the course of leptodactylid evolution (for example, Crinia, the Eleutherodactylini, the sub- genus Adenomera of Leptodactyhis, and the cycloranine genera Kyarraniis and Pluloria). The leptodactyline genera LitJiodyfes and Paratelmatohius prob- ably exhibit direct development. The sternal style of Barycholos re- sembles those of the leptodactyline gen- era (except Paratelmatohius) and is very different from the sternal apparatus seen in non-leptodactyline leptodactylid gen- era. Heyer ( 1969b ) described the style as calcified in contrast to the osseous style seen in Leptodactylus. Histolog- ically, the calcified element is a precur- sor to an osseous one, and the distinction between a calcified and an osseous ele- ment cannot be considered of primary importance. The character of the sternal apparatus which can be considered of primary importance is its shape (style- like or plate-like) because this character is not age or size dependent. Because the sternal style of Barycholos pulclier is style-shaped, I consider Barycholos to be a genus of the Leptodactylinae and to not be closely related to Eleuthero- dactylus. The relationships of Barycholos with- in the Leptodactylinae are not entirely apparent, but I consider the genus most closely related to the subgenus Adeno- mera (Leptodactylus) and Lithodytes. Osteologically, Barycholos differs from the former in having larger nasals which are in broad median contact and in hav- ing smaller prevomers. Litljodytes has large nasals which look like those of Barycholos but the prevomers of Litho- dytes are like those of the Leptodactylus (Adenomera) marmoratus group. PHYLOGENY AND RELATIONSHIPS Ideally, a discussion of the phylogeny of a group of organisms should be based principally on their fossil record. In the absence of such a chronicle of the evolu- tion of the group, systematists turn to study of the living representatives and infer the phylogeny on the basis of primitive and advanced characters. Many fossils from Cretaceous through Pleistocene horizons have been assigned to the Leptodactylidae. Each of these is discussed below; I consider several of the fossils to represent frogs of families other than the Leptodactylidae. The leptodactylid fossils are too recent to be of any significance in determining phy- logeny within the family. My interpretation of the phylogeny of the Leptodactylidae is principally based on comparisons of the character- istics of pelobatid and leptodactylid frogs. The phylogeny is in large measure deduced from a study of evolutionary trends in many characters. Most of these evolutionary trends were noted by earlier authors; the principle difficulty was de- termination of the directions of the trends. THE FOSSIL RECORD Pleistocene: — Giinther (1859b) re- ported fossils of Ceratophrys aurita (as C. cormita), Leptodactylus ocellatus, L. pentadactylus, and Leptodactylus sp. (as Cystignathus) from Lagoa Santa, Minas Gerais, Brasil. Rusconi (1932) named Ceratophrys ensenadensis from a Pleistocene (Ensenadan) locality near Buenos Aires, Argentina. Mecham (1959) reported late Pleistocene cave deposits in central Texas containing Hy- lactophryne augusti (as Eleutherodacty- lus latrans). Tihen (1960b) and Lynch LYNCH: LEPTODACTYLOID FROGS 193 (1964) reported middle Pleistocene rec- ords for Syrrhophus marnockii from northern Texas. Auffenberg (1958) named some specimens from late Pleis- tocene cave deposits of Barbuda, British Leeward Islands, as Hyla barbiidemis, which Lynch (1966) placed in the genus EleutJierodactylus. Pliocene: — Ameghino (1899) named Ceratophrys prisca from the Upper Plio- cene of Monte Hermosa, Argentina. Miocene: — C a s a m i q u e 1 a ( 1963 ) named Wawelia ger]}oldi from the Up- per Miocene of Rio Negro, Argentina, and described additional skeletal re- mains of Caudiverbera catidiverbera (as Gigantobatrachus parodii) from the same locality and horizon. The type- specimens of Gigantobatrachus were col- lected from Miocene deposits in Santa Cruz, Argentina ( Casamiquela, 1959). Holman ( 1965 ) named Leptodactyhis abavus and reported (1967) Eleuthero- dactylus sp. from the Arikareean, Lower Miocene, of northern Florida. Oligocene: — Ameghino (1901) listed Teracophrys (a nomen nudum) from the Upper Oligocene of Patagonia. The specimens are now apparently lost (Schaeffer, 1949). Schaeffer (1949) re- corded Caudiverbera caudiverbera (as a new species, Calyptocephallela canque- li), Eupsophus sp., and Neoprocoela edentata from Lower Oligocene deposits in Chubut, Argentina. Eocene: — Schaeffer (1949) named Caudiverbera casamayorervsis (as a new genus, Eophractus) from the Lower Eo- cene of Chubut, Argentina. Hecht ( 1960 ) named Eorubeta nevadensis from the Lower Eocene of Nevada. Noble (1930) concluded that Rana pu- silla Owen, 1847, from the Eocene (In- tertrappean) of peninsular India was a myobatrachine leptodactylid and named a new genus for it (Indobatrachus). Cretaceous: — Estes (1964) reported several bones from the Lance Formation ( Upper Cretaceous ) of Wyoming as pos- sibly representing leptodactylid frogs; he named none of these. Hecht (1960) suggested that some of the frog fossils from the Trinity Sands (Cretaceous) of Texas were primitive leptodactyloids. The fossil record is summarized in Table 3. Some of these records require special comment, because they are not leptodactylid frogs. The following is a systematic summary (by subfamily) of the fossils I accept as members of the family Leptodactylidae. Ceratophryinae: — Upper Miocene to Recent of South America. Wawelia ger- holdi is not distinguishable from either Ceratophrys or Lepidobatrachus but is clearly a member of the subfamily (see generic account, p. 112. Three spe- cies of Ceratophrys are known as fos- sils; two of these are extinct (C. ensena- densis and C. prisca), the other species still lives in the same area from which the Pleistocene fossils were recovered. Teracophrys may be a ceratophryine, but its taxonomic status must await re- discovery of Ameghino's specimens. Cycloraninae: No fossil record. Elosiinae: No fossil record. Heleophryninae: No fossil record. Leptodactylinae : Pleistocene to Re- cent of South America. The three spe- cies of Leptodactylus {oceUatus, penta- dactylus and sp.) reported by Giinther ( 1859b ) are the only fossils known for the subfamily. Myobatrachinae: Eocene of penin- sular India. Indobatrachus pusillus is very similar to Crinia, and is probably a leptodactylid. However, before the sys- tematic position of Indobatraclms can be fully evaluated, an osteological study must be made of the Arthroleptinae (Ranidae). See the generic account of Imlobatrachus for further details (p. 103). Telmatobiinae : Fossils of three tribes are known. Telmatobiini: Lower Eocene to Up- per Miocene of Patagonia. Caudiverbera is represented in Lower Eocene, Lower Oligocene, and Upper Miocene deposits of south-central Argentina. The Miocene and Oligocene fossils are regarded as 194 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY TABLE 3. Geographic and temporal distribution of the fossil frogs currently considered members of the Leptodactylidae. NORTH AMERICA SOUTH AMERICA OLD WORLD PLEISTOCENE Eleutherodactyliis harhudensis" Hijlactophryne augiisti Syrrhophus marnockii Ceratophrys aurita C. ensenadensis Leptodactylus sp. Leptodactyhis ocellatus L. pentadactyhis PLIOCENE Ceratophrys prisca MIOCENE Leptodactylus ahavus Eleutherodactyliis sp. Wawelia gerholdi Caudiverhera caudiverbera OLIGOCENE C caudiverbera Eupsophus sp. Neoprocoela edentata ? Teracophrys EOCENE Eorubeta nevadensis Caudiverbera casamayorensis Indobatrachus pusillus PALEOCENE CRETACEOUS [Lance Formation] [Trinity Sands] ■■' West Indian: Barbuda, Leeward Islands. identical with the Recent species ( Hecht, 1963), but the Lower Eocene fossils are here recognized as specifically distinct. Neoprocoela edentata, an ancestral stock for Batrachophrynus, is known from the Lower Oligocene of Patagonia. Tihen ( 1962b ) placed it in Bufo, but his action is rejected here (see pp. 120-122). Alsodini: Lower Oligocene of Pata- gonia. Schaelfer's (1949) Eupsophus s]p. is the only fossil record for this tribe. Many specimens of the fossil are avail- able but all are incomplete. Further study of these fossils should be made to assess their specific status. The fossil species differs from all Recent species of the genus in apparently having the nasal bones in median contact. Eleutherodactylini: Pleistocene of Texas and Barbuda Island, Leeward Islands. Three species of this tribe are known as fossils. The West Indian Eleu- therodactyliis barbudetisis may be extinct or may be identical with E. martinicen- sis (Schwartz, 1967). The Pleistocene records of Syrrhophus marnockii occur 200 miles north of the present northern limit of the range of the species ( Lynch, 1970a). The fossil of Hylactophryne augusti is from a Late Pleistocene cave deposit within the present geographic range of the species. I do not consider the other species listed in Table 3 to be members of the Leptodactylidae. The fossils here re- moved from the family have been re- ported from deposits in North America (Lower Miocene to Upper Cretaceous). Eleutherodactylus sp. : H o 1 m a n ( 1967 ) referred one right ilium from the Thomas Farm Miocene beds of Gilchrest County, Florida, to the genus Eleuthero- LYNCH: LEPTODACTYLOID FROGS 195 dactijhis but because of limited compara- tive material, did not make a specific assignment. Many, if not most, mainland Central and South American Eleuthero- dactylus have distinct ilial crests in con- trast to most West Indian species which have the crest replaced by an ilial ridge. Holman's fossil is similar to the ilia of several West Indian Eleutherodactijlus but is equally similar to some small specimens of Acris which I have exam- ined. Referral of the fossil to the Lepto- dactylidae cannot be justified; it is equal- ly likely that the fossil represents a young individual of Acris, especially in light of Holman's fossil species, A. bar- houri, from the same locality. Leptodactylus abavus Holman, 1965: Leptodactylus abavus Holman (Lower Miocene of Florida) is a species of Rana and may not be separable from Rana miocenica Holman of the same horizon and locality. The reasons for placing the species in Rana are presented in the ac- count on pelvic girdles ( p. 63 ) . Eorubeta nevadensis Hecht, 1960. The fossils of this frog are preserved as organic imprints in an oil well core. In this condition, the fossils are badly crushed and must be studied under ultraviolet light. Hecht (1960) consid- ered the presence of maxillary teeth and long transverse processes of the posterior presacral vertebrae as characters ade- quate to associate the fossil with the advanced frogs (Hylidae, Leptodactyli- dae, and Ranidae ) . The Buf onidae were not considered because the fossil has a toothed maxilla. The sacral diapophyses of the fossil are dilated and oriented at right angles to the sagittal line; there- fore, Hecht reasoned that the fossil did not belong to the Ranidae. Hecht then looked for hylid and lep- todactylid frogs with long transverse processes of the posterior presacral ver- tebrae and dilated sacral diapophyses. He characterized hylids as having either somewhat shortened or very thin, needle- like transverse processes of the posterior presacral vertebrae. By process of elim- ination, Hecht assigned the fossil to the Leptodactylidae. Among the leptodac- tylids available to him, he concluded that the fossil was most similar to Mixo- plujes and Lechriodus, because both genera have dilated sacral diapophyses and long transverse processes of the pos- terior presacral vertebrae. Hecht stated that Eorubeta differed from both of these genera in having seven instead of eight presacral vertebrae; Eorubeta was further distinguished from Lechriodus, because the latter has transverse proc- esses on the atlas. The "atlas" (in the sense of Hecht) of Lechriodus is the fused cervical and second vertebrae. Hecht rightfully complained of a lack of skeletons of representative Re- cent genera in museums and the lack of comparative osteological studies of Re- cent frog families. With these restric- tions, Hecht's action in assigning the fossil to the Australian section of the Leptodactylidae seems capricious. My study of Eorubeta was limited to the description, remarks, and illustrations in Hecht's (1960) paper. Hecht's description is reasonably ac- curate. However, I consider the fossil to have eight presacral vertebrae (Hecht recorded seven). Seven presacral verte- brae are clearly evident and all of these bear long transverse processes which are as long as or only slightly shorter than the sacral diapophyses. In all Recent frog genera I have examined, the trans- verse processes of the second vertebra (first post-cervical) are invariably short- er than those of the third vertebra. The transverse processes of the third vertebra are as long as, or longer than, those of any other presacral vertebra, and are usually somewhat curved. The trans- verse processes of the right side of the anterior presacral vertebrae of Eorubeta are concealed beneath matrix except for the leading edge of the vertebra I con- sider to be the third (Hecht considered this vertebra to be the second). The remains of the skull overlie parts of the vertebral column in this region. It is 196 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY clearly e\ident from an examination of Hecht's figures, that the transverse proc- esses of vertebra 2 are very long (as long as the sacral diapophyses) and slightly curved. If this vertebra is the second as Hecht contends, then Eorubeta has a vertebral column like no other in the Anura. It is more reasonable to sug- gest that this vertebra is the third. Just anterior to the left transverse process of this vertebra and the scapula, is a small area of bone which Hecht tentatively suggested is the coracoid. This structure might be the left transverse process of the second vertebra. Another interpre- tation is possible for the bones Hecht called the squamosals, occipital con- dyles, and foramen magnum. If the "oc- cipital condyles and foramen magnum" are the centrum and neural arch of the second vertebra, then the "squamosals" are of the proper shape and length to be considered the transverse processes of the second vertebra. If this interpreta- tion is correct, then the cervical is not distinguishable from the bones of the posterior part of the skull. The structure designated "atlas" by Hecht is much too small to be this element and is probably not a complete bone. Pending the re- covery of additional specimens, I will not offer further interpretation of the osteology of Eorubeta nevadensis. I concur with Hecht that the fossil does not represent the Ascaphidae, Dis- coglossidae, Pipidae, or Rhinophrynidae, for his reason (the transverse processes of the posterior presacral vertebrae in the Recent genera of these families are very short and often knob-like). The fossil has dilated sacral diapophyses which are unlike those of any ranid known to me. The Dendrobatidae and leptodactylids of the subfamily Elosiinae have non-dilated sacral diapophyses and short transverse processes on all presa- cral vertebrae. The pelobatids of the subfamilies Pelobatinae and Pelodytinae have very short transverse processes on the posterior presacral vertebrae, as do some Australo-Papuan leptodactylids, and thus could not be closely related to the fossil frog. The other frog families have dilated sacral diapophyses in some or all of the included genera ( Bufonidae, Centrolenidae, Hylidae, Leptodactylidae, Megophryinae, Microhylidae and Pseu- didae). The only skeletal elements of Eorubeta nevadensis which are useful in comparisons are those of the vertebral column, ilium, and maxilla. Eorubeta does not closely resemble any genus in the seven families listed above. Eoru- beta has maxillary teeth and therefore is probably not a bufonid, although this character need not completely eliminate the Bufonidae from consideration. The ilium of Eorubeta has little indication of a dorsal protuberance, prominence, or ilial crest; this condition is seen in some leptodactylids, megophryine pelobatids, and microhylids. The ilium is not ex- posed in lateral aspect and therefore centrolenids and hylids cannot be elim- inated from consideration. EoruI)eta is not a bufonid, ceratophryine, telmato- biine, leptodactyline, or pseudid because the ilia of Eorubeta lack large ilial prom- inences and/or dorsal crests. The vertebral skeletons of the re- maining groups ( Centrolenidae, Hylidae, Cycloraninae, Heleophryninae, Myoba- trachinae, Microhylidae, and Megophryi- nae) are difficult to separate as units when the details of the cervical vertebra are unknown. The cervical cotyles are widely separated medially in the Centi'o- lenidae, Hylidae, Microhylidae, and Myobatrachinae, whereas the cotyles are narrowly separated in the Cycloraninae, Heleophryninae, and Megophryinae. The cervical vertebra is not distinguish- able in Eorubeta. The only genera of the seven family groups listed above with the transverse processes of the pos- terior presacral vertebrae as long as the sacral diapophyses are Heinipliractus and some Hyla (Hylidae), Batraclw- phrijnus, Lechriodus, Limnodynastes, and Mixophijes (Leptodactylidae, Tel- matobiinae and Cycloraninae), and Megophrys ( Pelobatidae, Megopliiyi- LYNCH: LEPTODACTYLOID FROGS 197 nae ) . The transverse processes of Batra- cJwphrynus (Fig. 79) are very similar in bulk to those of Eorubeta, but the sacral diapophyses of these two genera are very different from one another. Eorubeta is unique, insofar as I am aware, in having wide, dilated sacral diapophyses. The only comparable sa- cral diapophyses known to me are those of Atelopus and Rlunoderma. In summary, Eorubeta does not closely resemble the skeleton of any known modern frog genus and cannot be assigned to any presently recognized family on the basis of its known mor- phology. Hecht's (1960) assignment of Eorubeta to the Leptodactylidae is not defensible and probably in error. The only reasonable systematic assignment of the fossil is to "Family incertae sedis. Order Salientia." Estes ( 1964 ) described and figured several Upper Cretaceous frog fossils from the Lance Formation of Wyom- ing.^'^ Among the fossils which are of significance to this discussion are the following: "Family PPelobatidae; Sub- order Neobatrachia, Family incertae sedis, near Hylidae?; and Family in- certae sedis, near Leptodactylidae?" (Estes, 1964: 57-61, figs. 30-32). The coccyx described and figured by Estes is unquestionably that of a megophryine pelobatid, although a generic assignment is not possible at present. The ilium de- scribed and figured by Estes is not sharply distinguishable from the ilia of some species of Pelobates and Scaphio- pus, but is different from the ilia of most Megophryinae and Pelodytinae. The in- complete left maxilla described and fig- ured by Estes resembles those of Pelo- bates, Scaphiopus, and, insofar as it is known, that of Eopelobates. Estes tentatively assigned an incom- plete right squamosal to the Leptodac- tylidae. The squamosal does not resem- ble that of any extant leptodactylid '■'' Estes (1970) associated a number of these Late Cretaceous elements with the genus Eopelobates (Pelobatidae, Megophryinae). genus but is similar to the squamosals of Scaphiopus (ScapJiiopus) and some Pelobates. Estes remarked that the fossil has an "opisthotic articulation surface [which] resembles that of leptodactyl- ids." This cryptic statement implies that there is (or are) a characteristic opis- thotic articulation of the squamosal in leptodactylids; the statement is not in agreement with my observations. A complete spectrum of opisthotic articula- tions can be demonstrated within the Leptodactylidae, ranging from species lacking the dorsal portion of the squa- mosal (Notaden) to those with the squa- mosal enclosing much of the crista paro- tica (Caudiverbera, Ceratophrijs). Estes (1969) subsequently assigned this squa- mosal as well as numerous other Late Cretaceous and Paleocene bones to Scotiophryne pustulosa ( Discoglossi- dae). Further comment on this action is deferred to a separate paper. The two bones (squamosal, figured; and na- sal) which Estes (1964) suggested might be from hylids or leptodactylids, could equally confidently be assigned to the Pelobatidae. The pelobatid centrum from the Middle Eocene of Wyoming figured by Hecht {in McGrew, 1959) is clearly that of a megophryine pelobatid, and as Hecht pointed out, is very similar to that of Eopelobates grandis from the Lower Oligocene of South Dakota. Hecht's fossil is probably generically identical with Eopelobates grandis and may not be specifically distinct. Estes' megophryine coccyx is possibly repre- sentative of the same complex. Hecht (1960:13) referred to some fossil frogs from the Trinity Sands of Texas (early Cretaceous) as "a primi- tive leptodactylid or some close relative." Until he publishes on them, no further comment will be made, although it should be born in mind that Hecht con- sidered Eorubeta a definite leptodac- tylid. Hecht and Estes (1960) named a Jurassic frog as Comobatraclius and placed it in Reig's (1958) Neobati-achia. 198 MISCELLANEOUS PUBLICATION MUSEUxM OF NATURAL HISTORY They further suggested that the fossil not be assigned to any recognized family but that "on the basis of probability [no confidence limits are given] a leptodac- tyloid affinity appears more likely [than a microhylid or hyperoliid affinity]." The fossil record for the Leptodac- tylidae can be summarized as follows: fossils of several stocks are known from the Tertiary of southern South America; an Eocene frog from peninsular India seems to be a myobatrachine leptodac- tylid; and leptodactylids are not known elsewhere in the world until the Pleisto- cene of the West Indies and Texas. With the exception of Neoprocoela and Indobatrachus, the fossil record of the Leptodactylidae is of little use in de- termining the phylogeny and is of limited value in discussing zoogeography. PELOBATID-LEPTODACTYLID RELATIONSHIPS Some Papuan leptodactylid frogs have been confused with pelobatid frogs. Lechriodus was erroneously believed to be a pelobatid until Noble ( 1924 ) dem- onstrated that the pectoral and thigh musculature were bufonoid, not pelo- batoid. In general, however, the two families have always been regarded as being very different from one another. This distinction hinged largely upon a distinction between the Pelobatinae (Pelohates and Scaphioptis) and the Neo- tropical leptodactylids. In the former, the coccyx is fused to the sacral verte- bra, whereas in leptodactylids the two bones are separate. The Pelobatidae may be separated from the Leptodactylidae by the greater dilation of the sacral diapophyses in the former, the sacral-coccygeal articulation (fused or with a single condyle in for- mer, double condyle in latter), mid- dorsal cricoid gap in former, single slip to m. depressor mandibulae (pars scapu- laris) in former, and m. semitendinosus and m. sartorius not separate in former. Two or three subfamilies are recognized depending on the author: Pelobatinae, Megophryinae, and sometimes Pelody- tinae. The Pelobatidae are unquestionably the more primitive group (Griffiths, 1963; Inger, 1967; Kluge and Karris, 1969; Noble, 1922, 1931; and Tihen, 1965), but the distinction between the two families is not so great as has been previously befieved, principally because previous authors have tended to ignore the similarities between the Megophryi- nae and the Austi-alo-Papuan leptodac- tylids and to stress those features which distinguish the two most abundant and best known groups of the two families (the Pelobatinae and Neotropical lepto- dactylids ) . The amplectic position of the male in the Pelobatidae, Cycloraninae and Myo- batrachinae is inguinal in contrast to the axillary amplexus in almost all advanced frogs. The Megophryinae, Myobatra- chinae and Cycloraninae (part) have free intervertebral discs, a character that has been regarded as paedomorphic or specialized by most authors but which is more likely primitive (Tihen, 1965). Several other characteristics, some here- tofore regarded as of little significance, occur in the primitive families and in some leptodactylids and sporadically, though rarely, in advanced frogs [e.g., absence of an outer metatarsal tubercle; vertical pupil; large, juxtaposed occipital condyles; small transverse processes on the posterior presacral vertebrae; imbri- cate neural arches; and tadpoles with complete row(s) of labial papillae and high number of anterior tooth rows (3-6)]. Griffiths ( 1963 ) contended that ecto- chordal and stegochordal centra were primitive to holochordal centra; Inger ( 1967 ) argued that holochordy is prob- ably primitive since it occurs in most extinct lepospondylous amphibians and that therefore ectochordy and stego- chordy are derived. Ectochordy has been termed paedomorphic; if so, then any distinction between frog families based on the nature of the coccygeal- LYNCH: LEPTODACTYLOID FROGS 199 sacral articulation cannot be seriously considered in interpreting the macro- systematic evolution of frogs. A full range of variation occurs in the Pelo- batidae — the ectochordal megophryines exhibit a monocondylar articulation, the stegochordal pelobatines exhibit a coc- cygeal-sacral fusion, and the presumably stegochordal pelodytines exhibit a bi- condylar articulation. Imbricate neural arches occur in all pelobatids and are found in cycloranines (but not myo- batrachines ) , in heleophrynines, in cera- tophryines, and in some telmatobiines ( Odontophrynini and Telmatobiini ) . The degree of dilation of the sacral dia- pophyses in pelobatids exceeds that seen in any leptodactylid except Neoprocoela (Lower Oligocene, Patagonia). Bufo- nids, which are generally conceded to be leptodactylid derivatives, have broad- ly dilated sacral diapophyses as well. If Neoprocoela is properly assigned famil- ially, then all primitive leptodactylids may have had sacral dilations of the pelobatid degree — those living leptodac- tylids with sacral dilations do not ap- proach the condition seen in bufonids or pelobatids. The sacral vertebra of Pelo- dtjtes is more like that of pipids than other pelobatids. Hecht (1960) mentioned the lack of moderate to long transverse processes on the presacral vertebrae in primitive frogs. My examination of skeletons of all ascaphid, discoglossid, pipid, and rhinophrynid genera confirms his obser- vation. Among the nine living and three extinct pelobatid genera some variation occurs. The transverse processes of the posterior presacral vertebrae are little more than bosses or are very short in Macropehhates, Pelobates and Scaphio- pus. Miopelodijtes and Felodytes have short processes strongly sloped anteriorly as in pipids. In the Megophnjs and Eopelobates (Megophryinae), the trans- verse processes of the posterior presacral vertebrae are of moderate length (Zwei- fel, 1956a; personal observation) but they are shortened and directed strongly anteriorly in at least one species of Lep- tobrachium (Boulenger, 1908), recalling the condition seen in Felodytes. The an- terior presacral vertebrae of all pelo- batids have elongate transverse proc- esses ( relative to the widths of the sacral diapophyses) as well as in some primi- tive leptodactylids ( Ceratophryinae ) . This same condition appears in some bufonids and is variable within Bufo. Several groups of leptodactylids have relatively short transverse processes on the posterior presacral vertebrae. This is most pronounced in Neobatrachus and Notaden (Fig. 30) but is also found in several Neotropical groups (e.g., Telma- tobiini, Odontophrynini, and Grypiscini) as well as in Heleophryne and most Myobatrachinae and Cycloraninae. The presence of postzygapophyses on the sacrum and prezygapophyses on the coccyx must be considered primitive. The zygapophyses are not present in Felodytes, and their presence is obliter- ated by sacral-coccygeal fusion in the Pelobatinae; they are found in the Mego- phryinae but not consistently in any leptodactylid. McDowell (in litt.) ob- served sacral postzygapophyses and coc- cygeal prezygapophyses in Metacrinia and in the enigmatic Sooglossus, but I have seen them only in Batrachophryntis and Megophnjs. Zweifel (1956a) de- scribed coccygeal zygapophyses in Eo- pelobates. The tadpoles of pelobatids and lepto- dactylids, as well as of all advanced frogs (except the microhylids whose relation- ships are obscure), are Type IV of Orton (1953). Admittedly, use of gross tad- pole morphology as a basis of macro- systematic ( interfamilial ) classification is hazardous (e.g., Inger, 1967), but an examination of intrafamilial variation can be useful in determining intrafamilial evolutionary trends. Inger (1967) char- acterized the Pelobatidae and Leptodac- tylidae as having tadpoles with median vents. Orton (1952) characterized the pelobatid tadpoles as follows: vent me- dian, beak present, tooth rows usually 200 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY divided with one complete short row anteriorly and two complete rows pos- teriorly, and labial papillae complete ex- cept for a narrow median interruption anteriorly. The data for pelobatids, in- sofar as is known, are summarized in Table 4. Only half of the pelobatid genera (and species) have median vents; the temperate Himalayan genera have dex- tral vents as does the subtropical and tropical Leptobrachitim. Inger's (1966: 25) statement that a complete row of papillae across the upper lip is charac- teristic of pelobatids is in error. Insofar as I am aware, it is true for only L. gracilis and L. pelodyfoides, although some Oreolalax have large, widely scat- tered papillae across the upper lip (Liu, 1950 ) . The uppermost tooth row is com- plete in all pelobatids (if teeth are present) and is very short in the Pelo- batinae and Megophryinae. In Pelodytes this row is almost as wide as the mouth, recalling the condition seen in most tad- poles. The Pelobatinae and Pelodytinae differ from the Megophryinae in having two complete tooth rows across the fully papillate lower lip; only a single com- plete row is found in megophryines. Most tooth rows are divided medially by the upper beak in pelobatids. This fea- ture in combination with the usually high tooth formula characterizes most pelobatids. This is not to say that this condition is not duplicated elsewhere; for example, Neohatrachtis has a dental formula of 1:2-2/1-1:11 to 1:3-3/1-1:11, Mixophijes has a 11:4-4/1-1:11 with three other very short lateral divided rows pos- teriorly and Heleophnjne has a IV/1-1: XII to IV/1-1: XVI formula; most bufo- noids exhibit a 1:1-1/111 tooth formula. The tadpoles of pelobatids suggest a closer relationship between the Euro- pean and North American genera than either group has to the Megophryinae. However, the variation within the Mego- phryinae suggests that the tadpole can be a hazardous source for definitive statements about relationships. Among bufonoid frogs the high tooth formulae in cycloranine and heleophrynine lepto- dactylids is suggestive of the pelobatid condition in distinction to the relatively dissimilar mouthparts seen in other bufo- noid frogs. Tadpole morphology repre- sents perhaps one of the most useful and most misused of the available char- acter complexes to be used in frog clas- sification. A major problem to be over- come is the descriptive formulae applied to the mouth parts. Many authors use the most simple, least informative system TABLE 4. Characteristics of Recent pelobatid genera— tadpoles" Labial papillae Tooth formula Vent complete Genus median anteriorly ( Low - High ) Scaphiopus" X O n:l-l/2-2:II-I:4-4/4-4:n Pelobates X O 1:3-3/3-3:11 Pelodytes X O 1:3-3/3-3:11 Nesobia ? ? ? Megophrys X A" 0 Leptobrachium O V 0 -1:7-7/5-5:1 Oreolalax O O 1:4-4/4-4:1-1:7-7/7-7:1 Scutiger O O 1:3-3/4-4:1-1:6-6/6-6:1 Vibrissaphora O O 1:5-5/4-4:1 "Data from Boulenger (1897), Inger (1966), Liu (1950), Orton (1952), Pope ( 1931), and Stebbins (1951). '' Including Spea. '' Absent. LYNCH: LEPTODACTYLOID FROGS 201 of arable numerals separated by a solidus (i.e., 2/3) for tadpoles with all of the rows complete or some of them divided. Using various systems, the dental for- mula for Vibrissaphora liui could be presented as: (A) 6/5 1 (C) 1:5-5/4-4:1 (D) IC, ID, 4L/1L, 3D, IC The formula with the greatest informa- tion content is the last ( D ) , in which the arable numeral preceding the letters C, D, and L refers to the number of complete, divided (but not lateral), and lateral (and divided) rows of teeth re- spectively. Lateral rows are separated by the beak. This system differs from that of Liu (1950) in distinguishing be- tween divided and lateral rows and does not require the use of Roman numerals. Liu's system is preferable to the 4- layered formula (B) in requiring less space on a printed page. The four- layered formula likewise does not dis- tinguish divided from strictly lateral rows although this distinction can be demonstrated to be two ends of a con- tinuum. There can be little argument against the statement that the Pelobatidae is the most primitive of the frog families, ex- cept the archaic Ascaphidae, Discoglos- sidae, Pipidae, and Rhinophrynidae (Ti- hen, 1965 ) . An appropriate test of which of the advanced families is most closely related to the Pelobatidae would be to compare them relative to the number of primitive characters shared. The selec- tion of characters and determination of evolutionary direction was made on the following bases: 1) characters shared between the Pelobatidae and some or all of the archaic frog families were re- garded as unquestionably ancestral; and 2) those characteristics which occur in these archaic families but also occm* in some of the bufonoid families were se- lected as being useful in measuring the relative primitiveness of each of the bu- fonoid families and subfamilies (and tribes of the leptodactylid subfamily Telmatobiinae ) . The familv or subfamilv with the lowest sum of values is judged to be most primitive, and the higher the sum of values, the greater is the divergence of that group from the ancestral stock. These primitive characters are ( I ) large, closely approximated occipital condyles — Types II or III; (II) imbricate neural arches; (III) anterior presacral vertebral transverse processes elongate and pos- terior presacral vertebral transverse proc- esses shortened; (IV) diapophyses of sacral vertebrae broadly dilated; (V) post-zygapophyses on sacral vertebra and prezygapophyses and /or transverse processes present on anterior end of coccyx; (VI) intervertebral discs free; (VII) ilium lacking dorsal crest, ilial prominence or protuberance; (VIII) all skull bones present; maxillaries, premax- illaries, and prevomers toothed; (IX) phalangeal formulae 2-2-3-3 and 2-2-3- 4-3; (X) pupil vertical; (XI) outer meta- tarsal tubercle absent; (XII) amplexus inguinal; (XIII) eggs small, laid in water, tadpole free-living; (XIV) tad- pole vent median; (XV) tadpole dental formula including at least three or four rows above and three rows below beak; and (XVI) pectoral girdle arciferal. Each of these 16 characters or character complexes was assigned a value from 0 to 2 for each of the 23 bufonoid and pelobatid taxa. The character states and values are summarized in Table 5 and the scores and sums for 35 family groups of "non-archaic" frogs in Table 6. A value of 0 indicates that the primitive condition is uniform within the group; a value of 1 indicates the group exhibits an intermediate condition or is variable with more than one-half of the included taxa exhibiting the primitive state; and a value of 2 indicates that a majority of or all of the included taxa share the (or a) 202 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY derived state for the character. The sum of the values for the 16 characters is an index of how far removed a given taxon is from the basal stock of the Bufonoidea — the Pelobatoidea. All three pelobatid subfamilies exhibit low values — the Megophryinae with 2, the Pelobatinae with 3, and the Pelodytinae with 4. The following leptodactylid groups exhibit values below 14 — Heleophryninae, Cy- cloraninae, Ceratophryinae, and Telma- tobiini ( Telmatobiinae ) . The Heleo- phryninae are only slightly removed from the pelobatid zone and are con- siderably more primitive than any other group of the "higher frogs." The Cyclo- raninae are well removed from the pelo- batid zone but less than one-half as far removed as are the Myobatrachinae. The leptodactylids of southern South America (Ceratophryinae and telmato- biine and alsodine Telmatobiinae) are more primitive than any other bufonoid groups (except the heleophrynine and cycloranine leptodactylids ) . Of the non- leptodactylid bufonoid families and sub- famihes, the Phyllomedusinae are least unlike the pelobatoid ancestor. The Bu- fonidae, which are usually regarded as only slightly advanced over the Lepto- dactylidae, are the next most primitive group. TABLE 5. Sixteen phylogenetically sig- nificant characters, their character states and values. I. Cervical type II =: 0 Cervical type I := 2 II. Neural arches imbricate == 0 Neural arches open = 2 III. Transverse processes of anterior presacral vertebrae expanded, those of posterior presacral verte- brae shortened = 0 All transverse processes as long as sacral diapophyses or all transverse processes shorter than sacral di- apophyses = 2 IV. Sacral diapophyses dilated = 0 Sacral diapophyses rounded = 2 V. Sacral vertebra bearing postzyg- apopyses and/ or coccyx bearing prezygapophyses = 0 Sacral vertebra lacking postzyg- apophyses and coccyx lacking pre- zygapophyses =: 2 VI. Intervertebral discs free = 0 Intervertebral disc fused to cen- trum ^ 2 VII. Ilium without dorsal crest or dorsal protuberance = 0 Ilium with dorsal crest and/ or dor- sal protuberance ^ 2 VIII. All skull bones present, premaxillae and maxillae bearing teeth ^= 0 IX. Phalangeal formulae normal = 0 Some skull bones lost and /or pre- maxillae and maxillae toothless = 2 Intercalary element present or pha- langes lost =z 2 X. Pupil vertical = 0 Pupil horizontal or round =^ 2 XI. No outer metatarsal tubercle = 0 Outer metatarsal tubercle present = 2 XII. Amplectic position inquinal = 0 Amplectic position axillary = 2 XIII. Eggs small, usually pigmented, lar- vae aquatic == 0 Eggs large, development abbrevi- ated or direct = 2 XIV. Tadpole vent median = 0 Tadpole vent dextral =^ 2 XV. Larval tooth formula at least 3/3 = 0 Larval tooth formula less than 3/3 = 2 XVI. Pectoral girdle arciferal = 0 Pectoral girdle firmisternal = 2 LYNCH: LEPTODACTYLOID FROGS 203 The Pelobatidac are intermediate be- and ranoid) frogs. The leptodactyhds tween the primitive ( discoglossoid and are the stem bufonoids and are difficult pipoid) and the advanced (bufonoid to separate from the pelobatids. TABLE 6. Vakies for each of the sixteen phylogenetically significant characters in non-archaic frog groups. Pelobatidae Megophryinae 0000001000000100 2 Pelobatinae 0000020100000000 3 Pelodytinae 0000220000000000 4 Leptodactylidae Heleophryninae 00122100000P0000 6 Cycloraninae 0011211001000110 9 Myobatrachinae 2211101102200220 17 Ceratophryinae 0002221001120010 12 Tehiiatobiini 0011221001120020 13 Alsodini 1111221002210020 16 Odontophrynini 1022221002220020 18 LeptodactyHnae 2122222002220120 22 Elosiinae 2222222102220220 25 Grypiscini 2222222002221220 25 Eleutherodactylini . 2222222002222220 26 Bufonidae 0121222202220121 22 Rhinodermatidae 0221222202222022 25 Centrolenidae 2221222122221020 25 Hyhdae Phyllomedusinae 2020222010221120 19 other HyHdae 2222222112222220 28 Dendrobatidae 2222222202221122 28 Pseudidae 2222222022222220 28 Sooglossidae 222200??020?2022 16+ Ranidae Raninae 2222222002220202 24 Rhacophorinae 2222222022121202 26 Petropedetinae 2222222002020202 22 Hemisinae ???222?220020202 16+ Hyperohidae Astylosterninae 2222222021020202 23 Hyperohinae 2222222020020202 22 Arthroleptinae 2222222022222022 28 Microhyhdae Dyscophinae ?0?0220001020022 11+ Brevicipinae ?0?022?202202022 16+ Asterophryinae 2020220202022022 20 MicrohyHnae 2000221102020022 16 CophyHnae 2220220002022022 20 Phrynomerinae 2220221222020022 23 204 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY INTRAFAMILIAL RELATIONSHIPS OF THE LEPTODACTYLIDAEi^ Figure 126 reveals that the Lepto- dactvHdae exhibit the greatest range of intrafamilial variabiUty or diversity among the Pelobatoidea, Bufonoidea, and Ranoidea. In part, this diversity represents a finer degree of knowledge about the Leptodaetylidae than about some other families, but the diversity is also real. The Leptodaetylidae have been the convenient "catch-all" for genera of bufonoid frogs with obscure relation- ships, and can be defined as "those bufo- noid frogs that are not members of the Bufonidae, Centrolenidae, Dendrobati- dae, Hylidae, Pseudidae, or Rhinoder- matidae." The intrafamilial relationships of the Leptodaetylidae are schematically summarized in Fig. 127. The Leptodaetylidae can be viewed as a series of increasingly more special- ized subfaiuilies and tribes which bridge the morphological and behavioral gaps between the Pelobatidae and the smaller families of the Bufonoidea and the Ra- " Elsewhere (Lynch, MS) I have proposed unit- ing the Old World leptodactyHd subfamilies as the family Myobatrachidae and using Lepto- dactyhdae for the four Neotropical subfamilies. As I noted in the paper to be published in "Evolutionary Biology of the Anura," the Neo- tropical subfamilies form a well-defined group which is approached by only one Old World subfamily, the Cycloraninae. The Myobatrachi- nae form a rather isolated group from all other leptodactyloids and could be placed in a family of their own (the Sooglossidae is probably not separable from Myobatrachinae ) . The cyclo- ranine-heleophrynine relationship is somewhat tenuous and apparently not very close, but these two groups seem to be somewhat more closely related to each other than either is to the myobatrachines or the Neotropical complex. Using the Leptodaetylidae as a single family for all seven subfamilies is only a slightly greater abstraction than to place the Old World sub- families in one family ( Myobatrachidae ) and the Neotropical subfamilies in a second (Lepto- daetylidae). Cladistically more sound would be to use three familes, one for the Myobatrachinae, a second for the Cycloraninae and Heleophry- ninae, and a third for the Neotropical families. If the latter fragmentation is employed, use of the term leptodactyloid becomes appropriate. noidea. The least specialized subfamilies and tribes of leptodactylids occur in southern Africa and the Australo-Papuan region. Other, only slightly more special- ized, groups occur in temperate South America, and the very specialized groups occur in the subtropical and tropical zones of South America and Middle America. The subfamily Heleophryninae con- tains one genus and is restricted in dis- tribution to southern Africa. HeJeophryne is the most primitive leptodactylid genus in terms of its degree of divergence from the pelobatids. In some characters, Heleophnjne resembles some of the gen- era of Australo-Papuan leptodactylids (Heleioporus, NeohatracJuis, Notoden, and Mixophyes) of the subfamily Cyclo- raninae, but the Australo-Papuan genera are closely interrelated, and none shows any evidence of a close relationship with Heleophnjne. The characteristics shared by HeleopJiryne, some of the Cyclo- raninae, the Ceratophryinae, and the Telmatobiini reflect those of the ancestral stock(s) of the Leptodaetylidae and may be used to demonstrate a close relation- ship among these eleven genera; how- ever, with the exception of Heleophryne and the ceratophryines, the other genera are the primitive members of larger groups. Heleophryne may represent an independent line of pelobatid derivatives which has achieved the leptodactylid or bufonoid grade. The Myobatrachinae are a relatively compact group of Australo-Papuan gen- era with one Eocene fossil genus from peninsular India. Although sympatric with the Cycloraninae, the Myobatra- chinae are not closely related to the Cycloraninae. Other than the character- istics of leptodactylid frogs, the two sub- families have one unifying character (inguinal amplexus), but this is shared with ascaphids, discoglossids, pipids, rhinophrynids, pelobatids, and Batra- chyla (Telmatobiinae, Leptodaetylidae). I consider it likely that two other genera of leptodactylids will be found to exhibit inguinal iV <1> UJ < Q m o (T Q 2 o o O c o 'c 'c o c >. l- "c Ui a c (U o 'c o x: o o < 2 >- q: UJ < 2 > l- k. X » c ■a o T3 O Q. o o E o C o o •♦- o o k- o o O c E Q. O o -Q O >» O O UJ m o _i III O LU LU O < _J ^ O O o -I X 2 2 Q. Figure 127. Dendrogram illustratinG; proposed relationships of the leptodactylid subfamilies and tribes and derived families. The hatched zone is Cretaceous time during which decreasing equability occurred. The vertical scale is not intended to indicate the duration or age of any group. Neotropical subfamilies than is the Lim- nodynastini which are more specialized than the Cycloranini. I consider each of the three subfam- ilies discussed above to have evolved independently from a megophryine an- cestor. One could therefore argue that the Leptodactylidae are polyphyletic. The Cycloraninae appear to be ancestral to the Neotropical leptodactylids, but the Heleophryninae and Myobatrachinae are apparently not involved in the phylogeny LYNCH: LEPTODACTYLOID FROGS 207 of the Neotropical leptodactylids. As stressed above, the Megophryinae and Aiistralo-Papuan leptodactyHds are simi- lar in most character complexes. Taken in combination, the Cycloraninae, Heleo- phryninae, and Myobatrachinae fomi an evolutionaiy grade between the Mego- phryinae and the Neotropical leptodacty- lids. However, I am reluctant to accord both the Heleophryninae and Myobatra- chinae familial status and consider equally unrealistic the idea of consider- ing either or both subfamilies of the Pelobatidae. The Myobatrachinae could be more reasonably distinguished famili- ally from the Pelobatidae than could the Heleophryninae. From an evolutionary standpoint, the Heleophryninae are a rel- ict of the Megophryine stock which gave rise to the Cycloraninae (see below, pp. 208-9). The Myobatrachinae probably evolved from a contemporaneous mego- phryine. Whether this megophryine was subfamilially distinct from the group which gave rise to the Cycloraninae can- not be known in the absence of fossils. I doubt that these two megophryines were subfamilially distinct and therefore con- sider the Leptodactylidae monophyletic following the reasoning of Simpson (1961:124). The subfamilies discussed below seem to have a common ancestry within the Leptodactylidae. This common ancestor was probably a cycloranine which was not unlike the modern Cycloranini. The subfamily Ceratophryinae con- tains only two extant genera and is a morphologically isolated group. This iso- lation has been described by several workers who consider the subfamily to be a family more closely allied to the Bufonidae than to the Leptodactylidae (Cei, Limeses, Reig). In spite of the morphological isolation of the Cerato- phryinae there are some striking simi- larities between the Ceratophryinae and the Odontophrynini. Boulenger (1882), Cochran ( 1955), Reig ( 1960b), Reig and Cei ( 1963), and Reig and Limeses (1963) suggested that Odontophrynus and Stom- bus auctorum ( =^Proceratophrys) are very closely related to the ceratophryines. The Odontophrynini may have been derived from a ceratophryine ancestor, but the ex- tant odontophrynine genera exhibit fewer primitive characters than do the genera of the Telmatobiini. The Odontophrynini represent either the first or second di- vergence from the original stock of the Telmatobiinae. The Ceratophryinae seem to represent the earliest divergence from the Neotropical leptodactylid stock. The remainder of the early Neotrop- ical leptodactylid stock (after the Cerato- phryinae diverged ) is represented by the Telmatobiinae and derived subfamilies (Elosiinae and Leptodactylinae). Some of the terrestrial genera of the Telmato- biini resemble the primitive Australo- Papuan Cycloranini (Cycloraninae) but more closely resemble the other tribes of Telmatobiinae. The Leptodactylinae are derived from the relatively primitive Alsodini (Eii- psophiis). The most primitive lepto- dactyline (Pleurodema) is very similar to Eupsophus. The two genera differ in the sternal apparatus, breeding biology, and loss of the quadratojugal. Pleurodema has an osseous sternal style (as do all other leptodactylines) and lays its eggs in a foam nest (like several other lepto- dactylines); these two characters clearly ally Pleurodema with the Leptodactyli- nae although its close relationship to Eupsophus is obvious and could be used to support the argument that the Lepto- dactylinae are only a tribe of the Tel- matobiinae. The Elosiinae are a small, morpho- logically homogeneous group except for the cranial adaptations of Megaelosia. The relationships of the subfamily to other leptodactylid groups are unclear and over-shadowed by the relationship between the Elosiinae and the Dendro- batidae. The Elosiinae exhibit many characters in common with the Alsodini, Grypiscini, and Eleutherodactylini, and I consider the elosiines to represent an early division from the alsodine stock which later gave rise to the Grypiscini and Eleutherodactylini. 208 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY I recognize two tribes in the Cy- cloraiiinae, the Cycloranini and tlie Lim- nodynastini. Of the two tribes, the Cycloranini are more primitive. The Limnodynastini are speciaHzed in their breeding biology. None of the five lim- nodynastine genera has vertical pupils and all have free intervertebral discs, the cervical fused to the second vertebrae, and relatively long transverse processes of the posterior presacral vertebrae. Adelotus brevis and one species of Lim- nodynastes have outer metatarsal tuber- cles, which are otherwise lacking in the tribe. The foam-nesting habits and the modifications of the fingers in females of the Limnodynastini are considered ade- quate reasons for separating these five genera from the Cycloranini which do not lay their eggs in foam nests (except Heleioporus) and do not have finger fringes in the females. The foam-nesting habit of Heleioporus is quite different from that of the Limnodynastini but sim- ilar to that exhibited by the frogs of the Leptodactylus fiisciis group. Heleio- porus, Neohatrachus, and Notaden are closely related. Although their skeletons are similar, the three genera differ in breeding biology and some external char- acters. Cyclorana and Mixophyes differ from Heleioporus, Neohatrachus, and Notaden in many features of the skull and vertebral column, but do not closely resemble each other. They are derived genera but probably have evolved several characters in a parallel fashion (ankylosis of intervertebral discs to centra, separa- tion of cervical and second vertebrae in adults, long transverse processes on the posterior presacral vertebrae, and lack of a frontoparietal fontanelle). The last character may be primitive to the pres- ence of a fontanelle, but in the lepto- dactylid groups the primitive genera fre- quently have a frontoparietal fontanelle. The Ceratophryinae and Heleophry- ninae do not exhibit a great amount of intrasu1)familial variability in that they are small groups. The Myobatrachinae are morphologically homogeneous in many characters but are heterogeneous in many others. With the possible ex- ception of bufonid and ranoid derivatives (see below), the myobatrachines do not figure prominently in bufonoid evolution. With respect to the Leptodactydae, the Myobatrachinae are an evolutionary dead-end. The Ceratophryinae and Telmato- biinae apparently evolved from cyclo- ranine ancestors. The Ceratophryinae represent an early divergence of the Neo- tropical stock and are a morphologically isolated and small group. The Telmato- biinae are a morphologically diverse and large group with one fossil and 24 Recent genera. I divide the Telmatobiinae into five tribes. The Telmatobiini (5 genera) and Odontophrynini (2 genera) are the most primitive tribes and the Alsodini are but slightly more advanced. The former two tribes have apparently not given rise to additional groups and have the bulk of their species in temperate or Andean South America. The Odonto- phrynini share several characteristics with the Ceratophryinae and may be early derivatives of that group which have paralleled the Telmatobiini. At present, I include the odontophrynines in the Telmatobiinae because they lack the distinctive vertebral column and vertebral shield of the ceratophryines. Cei ( 1965 ) demonstrated that the skin proteins of Ceratophrys and Lepidoha- trachus set these genera off from the other leptodactylids including Odonto- phrynus and Proceratophrys. The dis- tinctive ilia of the ceratophryines are identical with those of the odontophry- nines and unlike those of all other lepto- dactylids. The solution of the problem of whether the odontophrynines represent a proto-ceratophryine or a telmatobiine stock will probably require some fossil data. The Alsodini and their derivatives make up the majority of the Neotropical Leptodactylidae. The Alsodini occur in temperate and Andean South America, with one genus (Thoropa) endemic to southeastern Brasil. The tribe is some- what heterogeneous in that two of the LYNCH: LEPTODACTYLOID FROGS 209 genera (Eupsophus and Hylorina) have a type II cervical cotylar arrangement and lay relatively numerous small eggs in aquatic situations. Both of these gen- era engage in axillary amplexus and have outer metatarsal tubercles. One of them (Hylorimi) has vertical pupils. The other two alsodine genera (Batrachijla and Thoropa) have a type I cervical cotylar arrangement and lay relatively few large eggs in moist terrestrial situ- ations. The larvae of both genera be- come aquatic after the nest is inundated. Both genera have outer metatarsal tu- bercles and horizontal pupils. Batrachijla engages in inguinal amplexus (Barrio, 1967a), but amplectic behavior has not been observed for Thoropa. As men- tioned above, the Leptodactylinae seem to have been evolved from an ancestral stock with the characteristics of Eu- psophus. Batrachijla and Thoropa are probably representative of the alsodine stock which gave rise to the Eleuthero- dactylini, Grypiscini, and Elosiinae. I consider the Elosiinae to represent an early divergence from this stock because the Elosiinae have aquatic larvae. Os- teologically, the Elosiinae are isolated from the Grypiscini and Eleutherodacty- lini. I consider the Grypiscini more primitive than the Eleutherodactylini. The eggs of grypiscine genera are large and deposited in moist terrestrial situ- ations as is the case in the Alsodini, but in contrast to the Alsodini, the larvae are not aquatic ( Lutz, 1944 ) . The eleuthero- dactyline genera exhibit direct develop- ment. Unlike the grypiscine larvae, eleutherodactyline larvae never free themselves from the enclosing egg enve- lopes. The Grypiscini make up a small group which is restricted in distribution to the coastal ranges of southeastern and southern Brasil. The Eleutherodactylini range over the entire tropical and sub- tropical zones of the Americas except in the arid regions of Central America, Ecuador, Peru, and Venezuela. The ze- nith of the Leptodactylidae is Eleuthero- dactylus which contains probably 400 species and occurs over most of the range of the Eleutherodactylini. Direct devel- opment is probably the single adaptive change made by this tribe which per- mitted the tribe to evolve into such a large group. The success of the genus Eleutherodactijlus is measured by its di- versity and adaptability. The genus is rich in species throughout the West In- dies and occurs in semiarid as well as veiy moist habitats. Unlike many lepto- dactylid genera, it is not restricted to lowland situations where there are ponds (a requirement for species with aquatic larvae) but ranges altitudinally to at least 4200 meters in the Andes. EXTRAFAMILIAL RELATIONSHIPS OF THE LEPTODACTYLIDAE I have discussed the relationships be- tween the Pelobatidae and Leptodacty- lidae and the relationships within the Leptodactylidae above. In some cases, reference was made to the close relation- ship between a leptodactylid group and the frogs of other families. I consider the close relationship between the Pelobat- idae and Leptodactylidae to be estab- lished, and also consider the statement "the Leptodactylidae are the stem bufo- noid group" to be established. If the Leptodactylidae are the stem bufonoid group, then all other bufonoid families are leptodactylid derivatives or are inde- pendently derived from a pelobatid stock. The works of Griffiths (1963), Inger (1967), Kluge and Farris (1969), Noble (1922, 1931), and Tihen (1965) have clearly established that the archaic frog families (Ascaphidae, Discoglossi- dae, Pipidae, and Rhinophrynidae ) did not directly give rise to the "advanced frogs." These authors agree that these four families are clearly primitive and that the other frog families are advanced. Most consider the Pelobatidae to bridge the gap between "primitive" and "advanced" frogs. There is considerable debate as to whether the Microhylidae are primitive or advanced frogs. The proponents of the primitive position (Hecht, 1963, Inger, 210 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY 1967, Orton, 1957, and Starrett, 1968) based much of their argument on the tadpole moiphology, whereas the advo- cates of the advanced, ranoid position (Griffiths, 1963, Noble, 1922, 1931, and Parker, 1934) rely on the pectoral archi- tecture, thigh musculature, and the vari- able sacral-presacral central articulation. Further discussion of the relationships of the Microhylidae is withheld pending new data and perhaps another mono- graph of the family. I have plotted values for some of the microhylid subfamilies in the figure illustrating the degree of prim- itiveness in frog groups ( Fig. 126). The subfamily Microhylinae appears to be the most primitive subfamily of this group on the basis of the characters I used. Relatively little data of the breed- ing biologies of microhylids are available, and I have seen relatively few genera in computing my values of primitiveness for the family. In general the values are in agreement with the idea of the phylogeny of microhylids advanced by Parker ( 1934) —that the group represents an early ranid divergence. The data are not in accord with the position taken by Hecht (1963) and Starrett (1968)— that the family rep- resents one of the archaic families. The remaining frog families seem to have some relationship to the varied lepto- dactylid stocks. I consider the rhinodermatids to rep- resent a Neotropical bufonid derivative and therefore include that genus in a discussion of the relationships of the Bufonidae to the Leptodactylidae. As mentioned above, among the extant lep- todactylid groups the Myobatrachinae are most like the Bufonidae and are pre- sumably the modern representatives of the proto-bufonid stock. The two groups agree strikingly in the structure of the tadpole mouthparts. All bufonids (and Rhinoderrmi) lack teeth; few leptodactyl- ids are edentate, but this character-state is most pronounced in the Myobatra- chinae. All bufonids and myobatra- chines have dilated sacral diapophyses. Myobatrachines have a type I cervical cotylar arrangement (type II in bufo- nids), free intervertebral discs (pro- coelous vertebrae in bufonids), and lack Bidder's organ (present in bufonids). Most bufonids lack a prezonal element in the pectoral girdle ( omosternum pres- ent in Nectophnjnoides and at least one Btifo, B. haematiticus), whereas most lep- todactylids have a large omosternum and manubrium. The prezonal element in myobatrachines is small in most genera and absent in some. Although the Neo- tropical bufonids have radiated (7 en- demic genera ) , there is no close relation- ship between the Neotropical bufonids and leptodactylids. The relationships of the Centrolenidae are not apparent. Before the significance of the intercalary cartilage was accepted, they were often placed in the Hylidae or Leptodactylidae. Centrolenids are arbo- real, have aquatic tadpoles, intercalary cartilages, T-shaped tenninal phalanges, the astragulus and calcaneum fused, and lack a prezonal element in the pectoral girdle. Most authors consider them hylid derivatives (Eaton, 1958). Much of the argument that centrolenids are hylid de- rivatives rests on a conviction that all Neotropical taxa with intercalary carti- lages are related. The hyolarynx of Cen- troleneUa is distinctive (figured by Eaton, 1958) and quite different from that of most bufonoid genera. The variation in the hyolarynx of hylids has not been adequately investigated and until it has, the taxonomic value of the distinctive hyolaiynx of CentroleneUa remains un- known. The Dendrobatidae are an elosiine leptodactylid derivative and not ranoid as claimed by Griffiths ( 1959, 1963). This point was discussed in greater detail in the section of the Elosiinae (pp. 163-4). Griffiths ( 1963 ) , in arguing in support of his contention that the Dendrobatidae are a subfamily of the Ranidae, cited the apparent parallelisms in the Petro- pedetinae ( African ranids ) . My study of the group is limited to some dissection and examination of cleared and stained individuals but results in the conclusion that the two groups exhibit considerable LYNCH: LEPTODACTYLOID FROGS 211 similarity in myology and osteology. The similarities are quite striking and prob- ably reflect a community of ancestry rather than parallelism. However, it should be borne in mind that I have not studied the other ranid subfamilies and genera in detail and cannot therefore convincingly argue that the similarities are not due to parallelism. The relationships of the Hylidae are not apparent, but the family is usually tacitly considered a leptodactylid de- rivative. Inger's (1967: Fig. 6) phylogeny suggests that the Hylidae are the sister group ( sensii Hennig ) of the Ranidae + Rhacophoridae. The suggestion is unic(ue and mentally provocative but needs fur- ther investigation. Previous authors were committed to placing the Hylidae and Ranidae in different suborders because of convictions that the pectoral architecture or sacral centrum were characteristic of basic dichotomies. The same convictions required the Microhylidae to be closely related to ranids. The Pseudidae were considered lepto- dactylids until Parker (1935) suggested that they were hylids (because of the presence of an intercalary phalanx ) . The intercalary phalanx of pseudids is elon- gate and osseous instead of short, disc- like, and cartilaginous as in centrolenids, hylids, hyperoliids, rhacophorine ranids, and some microhylids (Phrynomerus). Savage and Carvalho ( 1953 ) named a new family for the Pseudidae (Lysapsus and Pseiidis) because they considered the accessory phalanx analogous to the in- tercalated cartilage. As pointed out by Burger (1954), Savage and Carvalho's "new family" was authored by Fitzinger (1S43). Savage and Carvalho (1953) considered Pseudis more primitive than Lysapsus and suggested that the family was derived from the Leptodactylidae. Burger ( 1954 ) considered Lysapsus more primitive than Pseudis and suggested that the group was a hylid subfamily. I have not studied pseudids in detail, and much information is lacking for Lysapsus, but I consider the group more closely allied to leptodactylids than to hylids. The pseudids are not closely related to any leptodactylid group. The ranoid families ( Hyperoliidae, Sooglossidae, Ranidae, and Rhacopho- ridae) are usually considered remote from leptodactylids. Sooglossus and 'Nesomantis were included in the Sooglos- sinae, a pelobatid subfamily with ranoid parallelisms by Noble (1931). The sub- family is restricted to the Seychelles. Darlington (1957) doubted on zoogeo- graphic grounds (with preconceived ac- ceptance of Matthew's conclusions ) that the Sooglossinae could be pelobatids, and Griffiths ( 1960), with similar zoogeo- graphic biases, demonstrated ranoid af- finities for the group and elevated the subfamily to family rank. The Sooglos- sidae have some pelobatid, myobatra- chine leptodactylid, and ranoid traits and are conceivably modern representatives of a leptodactylid derivative that gave rise to the Ranidae. Until further study is made of the numerous hyperoliid, ranid, and rhacophorid genera, aclditional comments on the relationships of these families to leptodactylids are held in abeyance. Vertical pupils are considered to be primitive by me and vertical pupils do not occur in the Ranidae or Sooglos- sidae. Vertical pupils are common in the genera of two of the subfamilies of Lau- rent's (1951) Hyperoliidae ( Astylosteri- nae and Hyperoliinae). Most of these genera also lack outer metatarsal tu- bercles. ZOOGEOGRAPHY Almost without exception, previous zoogeographic studies utilizing or in- volving anurans have been Matthewian in analysis and conclusion. Darlington (1957) voiced numerous suggestions con- cerning anuran zoogeography but lacked an understanding of the relationships of most groups. Noble ( 1924, 1926c, 1930) attacked many zoogeographic enigmas, but his approach was strictly Matthew- 212 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY ian. Many macrosystematic problems of frogs have been studied and solved in the past decade, and the major evolu- tionary patterns of the Anura are only now beginning to emerge. Many prob- lems, principally minor ones, remain to be solved; a major difficulty to be over- come is the relationships of the families assigned to the Ranoidea, especially the Microhylidae. Paleontological work has continued to force biologists to accept the antiquity of frogs; the order had diversified into several families by the Jurassic (Tihen, 1965). As the known antiquity of frogs increases, so must the consideration that continental drift may have played an important role in estab- lishing their present distributions. How- ever, simply because a group is an old one, continental drift need not be in- voked to explain distril)ution patterns (cf. Kluge, 1967). The present distribution of the Lepto- dactylidae ( Fig. 1 ) is suggestive of a southern origin and dispersal. No fossil evidence is available to establish the presence of the family in the northern hemisphere before the late Tertiary ex- cept for the Lower Eocene Indolxitra- chus from peninsular India. Noble (1930) and Darlington ( 1957 ) cited the fossil as evidence of a northern occurrence of the otherwise Australo-Papuan Myobatra- chinae. Both authors assumed that pe- ninsular India has always been part of the Asian continent or at least has been part of it for sufficiently long that, zoo- geographically, India is part of Asia. However, contrary evidence is impres- sive. Paleomagnetic studies place Bom- bay at 40 "" S in the Jurassic and record a steady northerly movement of the sub- continent throughout the later Mesozoic and Cenozoic. During the Eocene, Bom- bay was at lO'' S (Takeuchi, Uyeda, and Kanamori, 1967 ) , or at about the level of northern Australia, and the present Hi- malayan region was crossed by the Sea of Tethys. The frogs of the family Leptodactyl- idae presently occur in Australia (and New Guinea and Tasmania ) , in southern Africa, and in the Neotropics from south- ern Chile and Argentina (53-54° S) north to Arizona, Florida. New Mexico, and Texas (30-33° N). With the exceptions of a few leptodactyline and telmatobiine genera which range northward into Mid- dle America and the southern United States, no leptodactylid subfamily occurs on two continents. The Cycloraninae and Myobatrachinae occur only in the Australo-Papuan Region (two genera reach eastern New Guinea and three reach Tasmania), the Heleophryninae (monotypic) occur only in southern Af- rica, and the Ceratophryinae, Elosiinae, Leptodactylinae, and Telmatobiinae oc- cur only in South and Middle America. With the exception of Indohatnichus, the fossil record for each subfamily (insofar as it is known ) is included in the Recent distribution of the group (on the same continent). Five genera of the Telma- tobiinae range outside of South America; four of these (Hijlacfophryne, Sminthil- lus, Syrrhophiis, and Tomodactyhis) do not occur in South America, but the other (Eleiitherodactijlus) is wide-spread in tropical South America. Sminfhilhis is a Cuban endemic, and the other three non- South American genera are principally distributed on or around the Mexican Plateau. Three genera of the Lepto- dactylinae range outside of South Amer- ica. Fleurodema occurs in the savannas of central Panama but has its center of distribution in temperate South America. Physakiemus occurs in the Central Amer- ican lowlands as far northwest as Oaxaca and Veracruz, Mexico, but has its center of distribution in subtropical and tropical Argentina and Brasil. In the case of both genera, only a single species enters Cen- tral America. Leptodactylus ranges northwestward through Central America to Texas and Sinaloa but all Central American species are also found in north- ern South America. Leptodactylus also occurs on Hispaniola and Puerto Rico and on several islands in the Lesser An- tilles, but is not represented by extra- South American endemics. All of the Middle American leptodactylines arc LYNCH: LEPTODACTYLOID FROGS 213 Soiitli American species wliich have spread northward since the Late Phocene closmx' of the Panamanian portal (Lloyd, 1963). The Telmatobiine genera all be- long to the Eleutherodactylini. Three of the extra-South American genera (Smin- thillus, Syrrhophus, and Tomodactyhis) are derivatives of the alpha division of Eleuthewdactylus. The alpha division of EJentherodactyhis is centered in the West Indies ( about 100 species ) but also occurs in the Andean system in Colom- bia, Ecuador, Guyana, and Venezuela. The fourth extra- South American eleu- theroclactyline (Hylactophryne) is not ob- viously derived from Eleufherodactylus and shows a greater affinity with an Amazonian genus (Ischnocnema). The paleogeographic maps compiled bv Har- rington (1962), Jacobs et al (1963), and especially Lloyd ( 1963 ) strongly suggest that South America was not connected to North America during the Mesozoic and most of the Tertiary. Contact was estab- lished in the Pliocene (Lloyd, 1963). Animals could have moved northward across the volcanic island chain in the latter half of the Tertiary but the degree of isolation of animal groups suggests that the terrestrial South American faima was isolated in South America until the Pliocene. No leptodactylid group reached North America via a Panama-Costa Rica route until late in the Tertiary. Some leptodactylids may have reached North America earlier (perhaps Miocene) by way of the Antillean arc. Therefore, until the Middle Tertiary we may ignore North America insofar as leptodactylids are concerned. The history of the family lies in South America and the southern hemisphere. Vinson and Brineman (1963) suggested that Middle and South Amer- ica were connected by a Late Paleocene land bridge. These authors argued that this is true because of the lack of Danian- Paleocenc marine formations in the Isth- mian region of Panama. This land bridge was essential to Savage's ( 1966), analysis of the history of the Middle American heipetofauna. The Australo-Papuan and African leptodactylid groups share a few charac- ters but each of the three groups has more characters in common with the pelobatid subfamily Megophryinae. The Megophryinae seem to be ancestral to the Leptodactylidae, and the lack of ob- vious interrelationships between the Heleophryninae, Cycloraninae, and Myo- batrachinae suggests that each subfamily is an independent derivative of the mego- phryine stock. The Cycloraninae and Heleophryninae share one interesting character ( the fusion of the cervical and second vertebrae ) which does not appear elsewhere in the family. The fusion ap- pears in some African and South Amer- ican bufonid genera, rhinodermatids, palaeobatrachids, and pelodytids; the significance of this character distribution is not entirely apparent at present. The Recent distrijjution of the Mego- phryinae is much smaller than its early Tertiary distribution. Eopelobates is known from Europe in the early Miocene and western North America in the Eo- cene and Oligocene and is probably rep- resented in the late Cretaceous deposits of Wyoming. The Megophryinae are presently restricted to southeastern Asia and the Indo-Australian archipelago west of Wallace's Line but do not occur on Luzon and Masbate (Philippines). Both the Cycloraninae (Lechriodus) and Myobatrachinae (Crinia) occur in eastern New Guinea, and Lechriodus also occurs on the Aru Islands. Lechriodus has three endemic species in New Guinea and the Aru Islands, but one other spe- cies also occurs in eastern Australia. The single Crinia which occurs on New Guinea is also widespread on the Aus- tralian mainland. Each subfamily is dis- tributed over most suitable anuran habi- tat on the Australian mainland and both are absent over most of the western Eyrean desert. Among living leptodactylids, the Cy- cloranini are least unlike the primitive Neotropical leptodactylid genera. The morphological hiatus between the Neo- tropical leptodactylids and the several pelobatid stocks requires an intermediate 214 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY stage whose characteristics are Hke those exhibited by the Cycloranini. Darhngton (1957, 1965) considered the temperate South American frog fauna depauperate and thus of Httle zoogeographic impor- tance. Cei (1962a) and Vellard (1957) contended that the fauna is rehct. Vuil- leumier (1968) analyzed the amphil)ian fauna of the Nothofagus forests of tem- perate South America and noted that the present anuran distributional patterns are a result of Pleistocene events but ad- mitted that the high degree of endemism is a consequence of a long history in the Patagonian forests. Vuilleumier ( 1968) considered the frog fauna of the Notho- fagus forests to consist of four elements: 1) leptodactylid stocks which are au- tochthonous and have not subsequently diversified; 2) autochthonous lepto- dactylid elements which have subse- quently radiated into northern South America; 3 ) Nothofagus endemics which are derived from tropical South Amer- ican leptodactylids; and 4) bufonid and leptodactylid stocks which are wide- spread in South America and have more species outside of the Nothofagus forests than in it. He considered the available data as inadequate to permit determina- tion of whether these groups are secon- dary or primary inhabitants of southern South America. Vuilleumier's analysis must be rejected because his conclusions are in part based upon the erroneous conclusions of other authors. His second element [2), above] consisted of En- psophus. As I pointed out ( Lynch, 1971), Eupsophus (as used by Vuilleumier and many other authors) is a composite of seven genera. Eupsophus is restricted to western Argentina and Chile, except for two Andean species in southern and central Peru. Vuilleumier's third element has been altered taxonomically by Barrio (1967a) and Lynch (1971). Batrachyhi is valid and contains three species (all Nothofagus endemics); the genus is not an Eleutherodactylus de- rivative but an offshoot of a Eupsophus- Htjlorirm stock. The fourth element of Vuilleumier was misrepresented in part. Vuilleumier included the genera Bufo and Fleurodema. The former is wide- spread and species-rich in tropical and subtropical South America but Fleuro- dema is basically a temperate South American genus ( defined on the basis of cool or cold winters and cool summers). The distributions of eight of the ten species of the genus are contained in temperate South America; the other two species range northward into subtropical and tropical areas in Brasil, Colombia, Venezuela, and the Guianas (Fig. 128). Fleurodema is a temperate zone genus which has invaded the tropical zone, whereas Bufo is more a tropical zone genus which enters the temperate zone. Batrachophrymis, Batrachyla, Caudi- verhera, Eupsophus, Hylorina, Fleuro- dema, Telmatohufo, and Telmatohius are temperate South American leptodactylid genera either wholly or principally re- stricted to the temperate zone. This list of genera includes most of the primitive Telmatobiinae and the most primitive living Leptodactylinae. Ceratophrys, Lepidohatrachus, Limnomedusa, and Thoropa are also considered primitive, and with the exception of Ceratophrys do not range north of the southern sub- tropical zone. The primitive Cycloranini morpho- logically resemble the primitive Neo- tropical genera, which are the principally temperate South American genera. These coincidences require that we regard the similarities as convergent or that we con- sider them products of common ancestry. The latter conclusion further requires some land connection between Patagonia and Australia; the most plausible route is via Antarctica. To conclude that the route involved the Holarctic Region re- quires a massive extinction of the stocks which passed through the Holarctic and Neotropical regions, and further requires that these stocks survived only in tem- perate South America from which they gave rise to new groups which then in- vaded the tropical zone. A possible causative agent for such a mass extinction would be climatic zonation and decreas- LYNCH: LEPTODACTYLOID FROGS 215 Figure 128. Distribution of leptodactylids in South America. (A) Black areas encompass the range of the Alsodini. Thoropa is restricted to southeastern BrasiL The dotted Hne encloses the range of the genera Tehnatobius and Batrachophrynus. Two other genera of the tribe (Caiidiverbera and Tel- matobitfo) occur in the black area in Chile. ( B) Ranges of the genera Limnomedusa and Plevrodema, the most primitive genera of the Leptodactylinae. (C) Range of the Elosiinae. The area in southeast- em Brasil encompasses the distribution of Crossodactijlus and Megaelosia; the genus HijJodes also occurs on Cerro Duida, Amazonas, Venezuela. The range of the Elosiinae in southeastern Brasil approximates the range of the Grypiscini. ing climatic eqiial)ility of the northern hemisphere during Cretaceous time. However, this explanation results in two principle difficulties: 1) why did not leptodactylid stocks survive in areas in the northern hemisphere which retain high equabilities?, and 2) the mego- phryine pelobatids are probably equally sensitive to low equabilities yet they persisted in North America until the Oligocene and survive today in southeast Asia. Equability is a property of climate which expresses departures from 14.0° C and thus responds primarily to tempera- ture extremes (Axelrod and Bailey, 1968). High equabilities reflect little variation in temperatures about an annual mean of 14.0° C. Equability applies equally well to warm and cold regions. Bailey ( 1960, 1964 ) also noted a second aspect of tem- perature that affects biotic composition —effective temperature, which expresses warmth of the climate in terms of tem- perature and the duration of the summer (Axelrod and Bailey, 1968). Effective temperature is independent of the mean annual range of temperatures. Axelrod and Bailey ( 1968) noted that many areas in the southern hemisphere harbor relicts of the Cretaceous flora (cycads, tree ferns, podocarps, arau- carias). It is in some of these regions (south Africa, Australia, southern South America, southeastern Brasil) that prim- itive leptodactylids ( Cycloraninae, Myo- batrachinae, Heleophryninae, Telmato- biini, and Alsodini) occur. These areas are characterized bv high climatic equa- bility ( M = 60+). ' Mesozoic climates were characterized by high equabilities ( Axelrod and Bailey, 1968). Equability is increased if the locality is associated with large bodies of water (for example, the equability of localities along the Peruvian coast is higher than might be expected, as are the equabilities for localities in coastal Uruguay). The broad marine embay- ments and epeiric seas of Mesozoic land- masses probably contributed to the maintenance of high equabilities in con- tinental situations. Under a temperature regime of high equabilities, the dispersal routes of Mesozoic animals would not be temperature-limited. The southern hemi- 216 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Figure 129. (A) Distribution of the Odontophrynini. ( B) Distribution of the Ceratophryinae. (C) Distriliution of the LeptodactyHnae except for the primitive genera Limnomedusa and Fleurodema. sphere leptodactylid stocks could have invaded the northern hemisphere were land connections available because the northern hemisphere was also under a regime of high equabilities until the Cretaceous. During the Cretaceous many plant and animal groups became extinct or began to flourish. At the same time the earth began to experience a marked climatic zonation. With the development of climatic zonation, broad areas of the world experienced a decrease in equa- bility. Axelrod and Bailey suggested that the primitive faunas and floras presently living in areas of high equability survived in those regions because these groups are, and their ancestors were, adapted to climates of high equability. The part of South America (Figs. 129- 130) with high equabilities (58+) in- cludes the ranges of almost all of the primitive genera of Icptodactylids (Ba- trachophryrms, Batmchijla, Caudwer- bera, Etipsophus, Hylorimi, Lepidohatra- chus, Limnomedusa, Fleurodema, Telma- tobius, and Tehrmtobufo). A few of the species in these genera occur in areas of low equability ( for example, Fleurodema brachyops and P. diplolistris occur in areas with equabilities of 40-45). The Leptodactylinae probably evolved in re- sponse to the decreasing equability of the Late Cretaceous (see below). Before returning to the history of the Lepto- dactylidae in South America, it is con- venient to review briefly the history of the African and Australo-Papuan groups and the Megophryinae and to discuss the possible role of climatic equability in the establishment of the Recent distributions of these groups. The Megophryinae have survived in areas with relatively high equabilities. Even the temperate eastern Himalayas have equabilities of 60-[-. Regardless of which stance ( Wegenerian or fixed con- tinents) one wishes to take, the Mego- phryinae are probably a group which evolved in the northern hemisphere. The Cycloraninae, Heleophryninae, Myoba- trachinae, and Pelobatinae are the deriv- atives of the Megophryinae. Two of these derivatives are Australo-Papuan, one south African, and one Holarctic. The proximity of the present distributions of the Megophryinae, Cycloraninae, and LYNCH: LEPTODACTYLOID FROGS 217 Myobatrachinae tempts one to assume that megophryine stocks crossed the Inclo-AustraHan archipelago into Aiis- traha in the early Cretaceous with the Marsupalia and boid and elapid snakes. However, Inger ( 1954 ) considered the Megophryinae late invaders of the Phil- ippine Islands. Of further significance in this regard is the wider distribution of the Megophiyinae in the Late Cretaceous and early Tertiary of North America and Europe. Proponents of continental drift argue that the proximity of the Sundan shelf and Sahul shelf is a relatively recent phenomenon. The Indo-Australian archi- pelago is usually cited as the route whereby northern-evolved groups reached Australia in the Cretaceous (Clemens, 1968, Darlington, 1957, 1965). Biologists seeking support for this route have cited Audley-Charles (1966), who after studying the geology of Timor con- cluded that the relationship between Timor and the Sahul shelf has not changed since the Middle Triassic and that the relationship between Timor and 50.0 45.0 -55.0 Figure 130. Map of South America with isoequaphane h'nes (45, 50, 55, 60 and above) super- imposed. All dots on the map represent stations for which equability \ alues ( after Axelrod and Bailey, 1968) were computed. The hatched areas have equabilities of 50 or less. 218 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY tlie rest of the archipelago is apparently as ancient. As Hallani ( 1967 ) remarked, ". . . something more than island chain links is required to account for the pres- ence in Australia of the lungfish Neo- cerotochis and large Jurassic and Cre- taceous dinosaurs." A Jurassic dispersal of megophryinc stocks through eastern Africa onto penin- sular India, Antarctica, and Australia (Fig. 131) would explain the similarities of the Heleophryninae and some prim- itive Cycloranini, but would require that these continental masses be in close prox- imity instead of being widely separated as they are today. This route also re- quires that the megophryines not invade South America which was in close prox- imity with Africa until the Neocomian (Lower Cretaceous). The megophryine stock probably had the same reproduc- tive biology as do the living pelobatids and the Australo-Papuan leptodactylids. During the Jurassic and early Cretaceous, the Brasilian and Guiana shields must have been formidable barriers to pond- breeding frogs. On the slopes of these uplifted shields, ponds would be rare if they existed at all. In contrast, ponds would be available along the western edge of Africa in the vicinity of the East African Gulf of Tethys sea (Hallam, 1967). If the interior of Antarctica was as forbidding to amphibians as Darling- ton ( 1965 ) reasons it must have been, then the only southern route would have been across that part of Antarctica now called Enderby Land and the American Highland. Hallam (1967) suggested that a deep marine sea separated South Amer- ica and Africa from Antarctica, Australia, and Peninsular India in the Neocomian. Harrington ( 1962 ) noted the occurrence of marine facies over the southernmost tip of South America in the Neocomian but the extent of this marine sea was not as great: as suggested by Hallam. The leptodactylid stock that did reach south- ern South America probably entered the continent in Callovian (Upper Jurassic) or Neocomian (Lower Cretaceous) times. Whether dispersal was by a corridor or filter bridge (Darlington, 1957) route is non-consequential; dispersal could even have been via a sweepstakes route. The significant point to be made here is that contrary to Darlington's (1965:38) asser- tion, one group of terrestrial vertebrates (leptodactylid frogs) does show special relationships between the southern tem- perate fomis on different continents. Darlington stressed the absence of close- ly related cold-temperate vertebrates in Tierra del Fuego and Tasmania. How- ever, this absence is explained by in- creased cold and lowered equabilities in Tierra del Fuego. Once the Australo- Papuan groups reached Peninsular India and Australia, and the Australo-Papuan Cycloranini spread across Antarctica to Patagonia, continental connections were no longer necessary because each of the subfamilies occupied the appropriate continental masses. The probable time period was [or perhaps somewhat earlier than] the Neocomian (Lower Creta- ceous). After this time, Australia and South America appear to have been com- pletely isolated from all other land masses until the middle Tertiary in the case of Australia (connection via the Indo- Aus- tralian archipelago) and the late Tertiaiy in the case of South America ( connection via the Panamanian Isthmus). The early Cretaceous continental separations were followed by the impo- sition of a severe climatic regime on the distribution of the early Cretaceous fau- nas and floras. Insofar as the Mego- phryinae and their derivatives are con- cerned, the development of this new climatic regime had several important consequences: 1) evolution of a low- equability adapted group, the Peloba- tinae, in the northern hemisphere; 2) gradual extinction and range restriction of the Holarctic Megophiyinae; 3) isola- tion of the Heleophryninae into a high equability area in south Africa and/ or extinction of Heleophryninae or Mego- phryinae in east Africa; 4) extinction of Myobatrachinae in peninsular India; and 5) evolution of low-equability adapted groups in Australia and South America. LYNCH: LEPTODACTYLOID FROGS 219 The high-equability adapted groups were restricted in geographic distribution to areas of high equabiHty in southern South America and AustraHa. The de- velopment of climatic zonation probably resulted in physiological stresses on the Figure 131. Paleozoogeographic maps for three stages of the evolution and dispersal of leptodactyhd frogs and for related groups. (A) Jurassic (Callovian) — southerly dispersal of Megophryinae. ( B) Late Jurassic or eariiest Cretaceous — Africa is isolated from southern masses; climatic equability is beginning to influence dispersal routes. Leptodactylid invasion of South America. The dashed line is the route of free exchange of other vertebrate groups (e.g., characoid fishes and pipid frogs). ( C) Mid- dle Cretaceous — Africa-South American connection is tenuous, Neotropical leptodactylids are radi- ating from Patagonia into low-equability zones. Bufonidae spread into Africa. 220 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY surviving fauna and flora; these stresses forced a concentration of the Cretaceous genera into the remaining areas of high equabihty and may well have been the principle factors causing a radiation of the Neotropical Icptodactylids. The de- velopment of foam-nesting habits in the breeding biologies of the Limnodynastini may have been stimulated by decreasing e(|uabilit)'. The foam-nesting habit en- ables the frogs of this group to survive in more xcric, and less equable, climates than are suitable for the Cycloranini and Myobatrachinae. The distribution of Icptodactylids in South America was greatly restricted during the later Cretaceous, when cli- matic zonation was developing and equa- bility was decreasing. The fauna prob- ably included only a half dozen genera (Batrachyla, Caud'werhera, Etipsophus, Lepidohatrachus, Telmatobiifo or Neo- procoela, and TJwropo). In response to decreasing equabilities the range of the Alsodini was contracted and probably resulted in the isolation of a relict popu- lation on the Brasilian shield. This popu- lation probably gave rise to the Elosiinae and Grypiscini. The decreasing equabil- ities also resulted in the evolution of a group of frogs utilizing foam-nests in their breeding biology. The ancestral stock of this group is Etipsophus which gave rise to Pleiirodema and possibly to Limnomedusa. The presence of a foam- nest enabled these frogs to breed in more xeric environments, but presumably the adults were adapted to high equabilities and were therefore unable to successfully invade the tropical zone. New genera evolved to occupy this region (Lepto- dactyhis and Physalaemus). Batrachyla and Thoropa lay their eggs in moist ter- restrial situations but require water for their aquatic tadpoles. The Elosiinae represents a derivative of this group which became isolated on the Brasilian and Guiana shields (high equability). The Eleutherodactylini also evolved from an ancestral stock not unlike the Alsodini and Grypiscini. The Grypiscini and Eleutherodactylini evolved direct devel- opment, which enabled these groups to invade regions lacking ponds. The evo- lution of these groups may have been prompted by avoidance of competition in the larval stage. The evolution of Eleutherodactyhis is probably partly cor- related with the Andean orogeny in the Mid-Tertiary. The Ceratophryinae and Odontophrynini represent groups that evolved in response to decreasing equa- bility but were adapted to xeric, non- forested habitats. The principle low- equability adaptations of these groups involve a heavier, drier skin. The Dendrobatidae are the low- equability adapted derivatives of the high-equability adapted Elosiinae. The similarities between the Dendrobatidae and Petropedetinae and the distributions of these two groups are suggestive of their evolution being synchronous with the last stage of separation of eastern Brasil and Africa. The Petropedetinae are low-equability adapted frogs. The radiation of the Dendrobatidae probably occurred during the Andean orogeny; the dispersal of the group into Central Amer- ica is a I^ate Tertiary phenomenon (Sav- age, 1966). The Bufonidae may represent a paedomorphic offshoot of the Telma- tobiinae rather than the Myobatrachinae. The heavy, frequently dermostosed skulls and thick, dry-adapted skin of bufonids suggest that this group evolved in re- sponse to decreasing equability. The antiquity of the group is not directly known, but the earliest fossils are Lower Miocene (North America and Europe). The most primitive genus is African (Tihen, 1960a), but the remainder of the genera are derived from the widespread Bufo. Among its derivatives are seven Neotropical, seven African, and five Ma- laysian and Philippine genera. Bufo ranges over all continents except Aus- tralia and Antarctica. The Bufonidae probably originated in Africa and South America when the two continents were connected. The early evolution and dis- persal of the Bufonidae is considered syntopic witli tliat of the Pipidae and characoid fishes. The Gymnophiona ex- LYNCH: LEPTODACTYLOID FROGS 221 hibit a distribution and radiation pattern which is similar to tliat of the Bufonidae except tliat there is no caecihan genus which ranges over the Holarctic. The evidence suggesting that the Bufonidae represent an offshoot of the Myobatra- chinae is meager. The mouthparts of the tadpoles of the two groups are similar. It is possible that the Bufonidae are a paedomorphic myobatrachine offshoot that invaded South America synchro- nously with the Telmatobiinae. If Ant- arctica was under a temperate regime of increasingly lower equability while Aus- tralia was under one of higher equability, it is conceivable that a low-equability adapted myobatrachine group evolved in Antarctica and dispersed into South America before the South America-Ant- arctica land bridge was obliterated in the Cretaceous. One serious objection to this hypothesis is the absence of any high-equability adapted bufonid genera in South America. Rhinoderma is a high- equability adapted genus and is related to the Bufonidae. Rhinodermatidae may represent this high-equability adapted proto-bufonid. The bufonid genus Mel- anophnjmsciis lives in areas of relatively high equability in northern Argentina and Uruguay but does not range south- ward into the zone of very high equa- bility (5S+). A further difficulty with the hypothesis is the requirement of a low-equability corridor through the high equability zone which presumably cov- ered all of Patagonia during the Late Cretaceous and subsequent Tertiary. A more thorough studv of Rhinoderma mav prove to be the key in ascertaining the relationships of the Bufonidae to the Australo-Papuan or southern South American leptodactylids. SUMMARY AND CONCLUSIONS Based on the variation of behavorial and morphological characters, 57 Recent and three fossil genera of the Lepto- dactylidae are recognized. These 60 gen- era are placed in seven subfamilies, two of which are further subdivided into tribes. Two of the subfamilies (Cyclo- raninae and Myobatrachinae) occur only in the Australo-Papuan region, one (Heleophryninae) in southern Africa, and four ( Ceratophryinae, Elosiinae, Lepto- dactylinae, and Telmatobiinae) in the Neotropical realm. ^■''' The fossil record of leptodactylid frogs is of little value in deducing macro- systematic phylogeny. Fossils are repre- '" The alternatives to a single family arrange- ment are cited elsewhere (footnote 14, p. 204). The alternatives are: 1) two families, an Old World Myobatrachidae and a Neotropical Lep- todactylidae; 2) two Old World families, an African-Australian group for the Cycloraninae and the Heleophryninae, an Australian group for the Myobatrachinae, and one Neotropical family; and 3) one Old World family and two Neo- tropical families, one for the two genera of the Ceratophryinae and a second for the other three Neotropical subfamilies. Other alternatives are simply permutations of the above. sented in the Pleistocene of North Amer- ica, the West Indies, and South America. Fossils of three phyletic lines are pre- served in Lower Eocene to Pliocene de- posits of Patagonia. All of the above- mentioned fossils are members of genera living in the same regions today or are closely related, extinct genera. The only zoogeographically important fossil is the Lower Eocene Indohatrachus, a myoba- trachine from peninsular India. The sub- family Myobatrachinae is presently re- stricted to the Australo-Papuan region. In order to determine the evolutionary direction ( primitive to advanced ) of sev- eral evolutionary trends, the following reasoning was used: character states shared by some or all archaic frog fam- ilies and the other lissamphibian orders are primitive in the Anura; character states shared by most archaic frogs and most pelobatids are primitive in the Anura; and character states which are rare in the archaic families but always evident in the Pelobatidae are primitive in the pelobatid-bufonoid superfamily complex and may be primitive in all 222 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY frogs. This analysis resulted in the con- clusion that the following character com- plexes are useful in ascertaining the rela- tive primitiveness of frog groups: 1) type of cervical cotylar arrangement and type of occipital condylar arrangement; 2) neural arches— imbricate or not; 3) rela- tive lengths of transverse processes of presacral vertebrae; 4) extent of dilation of sacral diapophyses; 5) presence of zygapophyses involved in sacral-coccyg- eal articulation; 6) separation of inter- vertebral discs from the centra; 7) com- plexity of the ilium; 8) loss of skull bones and teeth; 9) modifications of phalangeal formulae; 10) shape of pupil; 11) pres- ence of outer metatarsal tubercles; 12) amplectic position; 13) egg size, oviposi- tion site, larval development; 14 ) tadpole vent position; 15) tooth row formula of tadpole; and 16 ) architecture of pectoral girdle. The Megophryinae (Pelobatidae) gave rise to four principle groups: 1) the Pelobatinae, 2) the Heleophryinae, 3) the Cycloraninae, and 4) the Myobatra- chinae. Each of these groups appears to be an independent derivative. All of the Neotropical leptodactylids arc probably descendants of one invasion of a cyclo- ranine stock into South America. The Ceratophryinae and Telmatobiini are the most primitive Neotropical groups. The major leptodactylid radiation occurred within South America and radiated out of southern South America. One primi- tive tribe of the Telmatobiinae (Alsodini) gave rise to the advanced tribes of the subfamily (Grypiscini and Eleuthero- dactylini) as well as to two additional subfamilies (Elosiinae and Leptodactyl- inae). The Dendrobatidae are a deriv- ative of the Elosiinae. The Telmatobiini and Odontophrynini are two tribes of the Telmatobiinae which appear to be the most primitive. The evolution of leptodactylids is best explained on a superstructure involving continental drift. The following paleo- zoogeographic sequence is proposed: the basal stock, the Megophryinae, origi- nated on northern landmasses from an ascaphid-discoglossid ancestor and dis- persed southward in the Middle Meso- zoic. A single dispersal corridor was utilized, the area in east Africa to the west of the East African Gulf of Tethys Sea. The megophryine stock could not invade South America because of the lack of a lowland corridor between North and South America or between Africa and the Brasilian shield. The stock passed through south Africa onto the southern landmass composed of penin- sular India, Australia, and part of Ant- arctica. Progressive southerly extension of the East African Gulf isolated the derived group on India, Australia, and coastal Antarctica. During the Late Ju- rassic or early Cretaceous, a cycloranine stock dispersed along the coast of Ant- arctica into southern South America. Concurrently, climatic zonation and the ensuing decrease in climatic equability were bringing about the extinction of many groups of plants and animals. In the northern hemisphere, the Mego- phryinae gave rise to a low-equability adapted group, the Pelobatinae, and were restricted in distribution to a high- equability zone in southeast Asia. Lower- ing equability resulted in the isolation of the African megophryine derivative in the high-equability refugium in south Africa. This group is the Heleophryninae. The effect of decreasing equability in Australia was minor. The Cycloraninae evolved a low-equability tolerant group, the Limnodynastini. Decreasing equabil- ities with the northward movement of peninsular India during the Cretaceous and Tertiary resulted in the extinction of the myobatrachines living there. In South America, the more primitive lepto- dactylid genera survive in the area of high equability (often termed temperate South America). Decreasing equability resulted in the evolution of a low-equa- bility adapted group, the Leptodactyl- inae. The Ceratophryinae and Odonto- phrynini are arid-adapted frogs and were therefore able to invade the low-equabil- ity areas which were arid or semi-arid. LYNCH: LEPTODACTYLOID FROGS 223 Decreasing equabilities probably initially led to range restrictions which resulted in the isolation of the Elosiinae and Grypiscini in southeastern Brasil (a high- equability zone). The Dendrobatidae are low-equability adapted frogs which evolved from the high-equability adapted Elosiinae. The African ranids of the sub- family Petropedetinae are usually cited as ranids with adaptations paralleling the Neotropical dendrobatids. I have studied briefly the anatomy of Petropedetes and find the similarity to dendrobatids strik- ing. The two family groups may repre- sent remnants of a group once ranging across the South American-African isth- mus. However, before the relationship can be established, more study of the ranids needs to be made. In the course of this study, many taxonomic changes have been proposed. These are summarized below. 1. Geobatrachus Ruthven is removed from the Leptodactylidae and tentatively assigned to the Microhylidae, pending completion of a study of the systematic position of the genus by Dr. Charles F. Walker. 2. Htjlopsis pJattjcephalus Werner is a species of the Hylidae and perhaps not separable from Hyla. 3. Rhinodernia is placed in a mono- typic family, the Rhinodermatidae. 4. The subfamily Cycloraninae is rec- ognized for 10 genera. The subfamily is divided into two tribes: Cycloranini (Cyclorana, Heleioponis, Neohatrachus, and Notaden) and Limnodynastini new tribe (Adelotus, Kyarranus, Lechriodus, Limnodynastes, and Philoria). 5. The subfamily Myobatrachinae is recognized for one fossil and seven Re- cent genera (Crinia, Glatiertia, Indoha- trachus, Metacrinia, Myobatrachus, Pseu- dophryne, Taudactylus, and Uperoleia). 6. Glauertia mjoebergi is transferred to the genus Uperoleia. 7. Taudactylus diurnus is identical to Crinia acutirostris; the genus Taudactylus is worthy of recognition but the only species in the genus must now be called T. acutirostris.^^ 8. The subfamily Heleophryninae is recognized for the African leptodactylid, Heleophryne. The opinions of some earlier authors that Heleophryne is a ranid or the only genus of a monotypic ranoid family are rejected. The subfam- ily is similar to megophryine pelobatids but has achieved the leptodactylid grade. 9. The subfamily Ceratophryinae is recognized for two Recent genera (Cerat- ophrys and Lepidobatrachus). The group is not sufficiently different to be accorded family rank and is not more closely re- lated to the Bufonidae than to other leptodactylids. 10. Chacophrys is considered a syn- onym of Ceratophrys. 11. Stombus Gravenhorst, 1825, is a synonym of Ceratophrys Wied, 1824; Rana cornuta Linne is designated the type-species of Stombus. 12. The Miocene fossil Wawelia ger- holdi is a ceratophryine but is not sepa- rable from either Ceratophrys or Lepido- batrachus and is therefore tentatively recognized. 13. The subfamily Telmatobiinae is recognized for one fossil and 24 Recent genera of Neotropical leptodactylids. The following family group names are con- sidered synonymous with the Telmato- biinae: Hylodidae Giinther, 1859, Al- sodina Mivart, 1869, Cacotina Mivart, 1869, Grypiscina Mivart, 1869, Cyclo- rhamphinae Lutz, 1954, Eleutherodactyl- inae Lutz, 1954, Calyptocephalellinae Reig, 1960, and Batrachylinae Gallardo, 1965. The subfamily is divided into five tribes: Telmatobiini (Batrachophrynus, Caudiverbera, Neoprocoela, Tehnatobius, and Tebnatobufo), Alsodini (Batrachyla, Eupsophus, Hylorina, and Thoropa), Odontophrynini new tribe (Odonto- phrynus and Proceratophrys), Grypiscini (Crossodactylodes, Cycloramphus, and '" M. J. Tyler (in litt.) informed me that this statement is erroneous. The two species of Taudacttjhis are distinctive species. The mate- rials used in this work are T. acutirostris (Andersson). 224 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY JMchaeniis), and Eleiitherodactylini (Am- bh/phrynus, EleutJwrodactijhis, Eupark- erella, Holoaden, Hykictophryne, Isch- nocnema, Niceforonia, SmintluUus, Syr- rhophus, and Tomodactyhts). A new genus, ScythropJirys, is named for Zachaenus sawayae Cochran but cannot be confidently assigned to a tribe until osteological data are available. 14. The generic name Caudiverhera is used in preference to Calyptocepha- lella. Eophractiis Schaeffer is placed in the synonymy of Caudiverhera. Giganto- hatrachus parodii (Miocene of Patagonia) and CalyptocephaJeUa canqueli (Oligo- cene of Patagonia ) are placed in the syn- onymy of Caudiverhera caudiverhera. 15. Neoprocoela is not a synonym of Btifo and is recognized as a genus of leptodactylid frogs which is ancestral to BatracJwphrynus. 16. Tehiuitohufo is not a synonym of Aruncus; Aruncus is a synonym of Bufo. 17. Macrogenioglottus is placed in the synonymy of Odontophrynus. 18. Proceratophrys is the valid ge- neric name for the supraspecific group frequently called Stomhus. 19. Craspedoglossa is considered a synonym of Zachaenus. 20. Zachaenus roseus Cope is not a member of the genus Zachaenus and is considered a species inquirenda in the Leptodactylidae, probably in the Telma- tobiinae. 21. Nohlella is placed in the synonymy of Eleutherodactyhis. 22. Pseudohyla, previously considered a hylid genus or a synonym of Hyla, is a synonym of Eleutherodactyhis. 23. Eupsophus wettsteini is trans- ferred to the genus Niceforonia. 24. SyrrJiophus lapkicai is probably a member of the genus Niceforonia. 25. Syrrhophus is not a synonym of Eleutherodactyhis, but the separation of Syrrhoplms and Tomodactyhis is consid- ered tenuous. 26. The subfamily Elosiinae is recog- nized for three Recent genera (Crosso- dactylus, Hylodes, and Megaelosia). Hylodes Fitzinger is used in preference to EJosia Tschudi. 27. The subfamily Leptodactylinae is recognized for ten Neotropical genera (Barycholos, Edalorhina, Hydrolaetare, Leptodactylus, Lininomedusa, Litho- dytes, Paratehiuitobius, PJiysalaemus, Pleurodema, and Pseudopahidicola). 28. Paratehnatohius pictiventris A. Lutz, in Lutz and Carvalho, is a nomen nudum and an obliata.—KV 92878 (CS). Hijlodes magalhaesi. —KU 92887 ( CS ) . Hijlodes nasus.—KU 74209 (CS), 92893-94, JDL S-255-56, 258, 282. Htjlodes ptdcher. —KU 92899 (CS), 92900. Hijlorina .sy/uafica.— BMNH 91.29.17, FMNH7102 (SRC), 7107 (SRC). Ischnocnema quixensis. — KU 104388, UIMNH 59643 (CS). Kyarramis sphagnicola. — AMNH 64294, KU 1103.31 (CS). Lechriodiis fletcheri.— AMNH 59488, CAS 82221 (CS). Lepidohatrachus asper. — KU 80783. Leptodactylus albilabris. — UMMZ S-166. LeptodacttjJus bolivianus. — KU 41026. Leptodactylus bufonhis. — KU 92905. Leptodactylus chaquensis. — KU 80795. Leptodactylus gracilis. — KU 92913-14. Leptodactylus hylaedactylus. — KU 119387- 88 (CS). Leptodactylus labial is. — KU 41027, 68273- 74 (CS). Leptodactylus macrosternus. — KU 92919-20. Leptodactylus melanonotus. — KU 68275-76 (CS), JDL S- 1252-58, UMMZ S-858, 1045. Leptodacttjlus vnjstaceus. — KU 92932. Leptodactylus mystacinus. — KU 92925-26. Leptodactylus pentadactylus. — KU 41028- 29, 68159, 84981-82, 117366-68. Leptodactylus podicipinus. — KU 92938. Leptodacttjlus prognathus. — KU 80824 (CS), 92944. Leptodacttjlus piistidostis. — KU 92947. Leptodacttjlus quadrivittatus. — KU 41030. Leptodactylus syphax. — KU 92951. Leptodactyltis wagneri. — KU 104389-90. Limnodtjnastes dorsalis. — KU 93553, UMMZ S-165. Limnodtjnastes fletcheri. — KU 93559 ( CS ) . Limnodtjnastes peronii. — KU 93566 ( CS ) . Limnodynastes tasmanensis. — AMNH 60589, KU 93573-74 (CS). Limnomedusa macroglossa. — KU 92960 (CS), 92961. Lithodtjtes lineattis.—KU 104340 (CS). Megaelosia goeldi.—KU 92965-66, 106271. Metacrinia nichollsi.—KU 110332 (CS). Mixophtjes fasciolatus. — KU 56627. Mtjobatrachus gotddii.—KU 110333 (CS). Neobatrachus centralis. — KU 93578. Neobatrachus /;/cf(/.s.— FMNH 97281, KU 69278 (CS). Niceforonia festae.—KU 118137 (CS), USNM 160944 (CS), 160950 (CS). Niceforonia flacomaculata. — KU 119743 (CS). Niceforottia montia.— MCZ 24352 (CS). Niceforonia tvettsteini (paratypes of Etipso- plitts icettsteini).—NMW 15846:1-2 (SRC). Notaden bennetti.—FMNH 97658. Notaden nichollsi.—KU 93580 (CS), 93582 (CS). Odontophrijnus americanus. — KU 92968, 100437. Odontophrijnus carvalhoi. — KU 100441-42. Odontophrijnus cidtripes. — KU 92975. Odontophrijnus occidentalis. — LHUBA 1200, 1218. Paratelmatobius lutzi.—KU 92981 (CS), 107089 (CS). Philoria frosti.—KU 50699 (CS). Phijsalaemtis albonotatus. — KU 92987 (CS). Phtjsalaemus biligonigerus. — KU 84768-76. Phijsalaemus cetUralis.—KU 92993 (CS). Phtjsalaemus cuvieri. — KU 92999 (CS). Phtjsalaemus ephippifer.—KU 93005 (CS). Phtjsalaemus fiiscomaculatus. — KU 80811 (CS), 93010 (CS), UMMZ S-2357 (CS). Phtjsalaemus gracilis.— KU 93016 (CS). Physalaemus maculiventris. — KU 93022 (CS). Phtjsalaemus nanus.— KU 93025 (CS). Phtjsalaemus nattereri.—KU 92844 (CS), 92845. Phtjsalaemus petersi. — KU 120290 (CS). Phtjsalaemus pti.stulatus.—KU 118136 (CS). Phtjsalaemus pttsiulosus.—KU 41031, 68269- 72 (CS), JDL S-1204. Physalaemus signif ems. —KU 93033 ( CS ) . Pleurodema bihroni.-YMNYl 3746-47, 3758. Pleurodema brachtjops.— AMNH 69754, KU 96159, 104318 (CS), UIMNH WLB-725 (CS). Pleurodema cinerea.—KU 80836, 93038. Pleurodema diplolistris.—KU 93044 (CS), UMMZ 108521 (CS), 108895 (6) (CS). Proceratophrys appendiculata. — KU 93070. Proceratophrys boiei. — KU 93076. Proceratophrys cristiceps. — KU 106273, UMMZ 115658. Pseudopaludicola ameghini. — KU 93050 (CS). Pseudopaludicola falcipes.—KU 93056 (CS). Pseudopaludicola pusilla. — UMMZ 54589(2) (CS); boliviana topotypes, UMMZ (2), not cata- logued (CS). P.seudopaludicola saltica.—KU 93068 (CS). Fsetidophryne bibroni.—KU 93588 (CS). 228 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY PseiidopJinjne corrohoree. — AMNH 64510- 12. Scythmphrys- sawayae.—VISNM 125530 (ho- lotype), not a skeletal preparation; some skele- tal features were observed through slits in the skin. SDiintliillus limhatus.—KV 68684 (CS). Synhnphtis ^uttilatus. — JDL S-1215. Synhophus Icpnis— JDL S-992, UIMNH 27130 (CS). SynJwpJius marnockii. — JDL S-214. Synhophus poUidus.—KV 80320 (CS). SyirJwpJitts pipilans. — KU 59950 (CS). S y rrJiopJius nt J) r imacu hi t ii s. — U I M N H 55313-16 (CS). Taudactyhis aciitirostris.—K\] 124233 (CS). rdmatohms hauthaIi.—K\J 72879 (CS), UMMZ S-164. Tehnatohhia marmomtus. — UMMZ 68179 (2). Telmatobius puta^onicus.—K\J 80781 (CS). Telmatohufo huUocki.—FMNH 23842 (SRC). Thowpa hdzi.—KU 92850 (CS), 92908 (CS). Thowpa iuili(iris.—Kn 92855 (CS), 92856. Thowpa pet wpolitana. —K\J 92862 (CS). Tomodactyhis alholabris. —K\J 87780 (CS). Tomodactyhis ^landis. — UMMZ S-963. Tomodactyhis nitidtis.—Kn 102649 (CS), JDL S-1308, UIMNII 7830 (CS), 78.32-34 (CS), UMMZ S-2225. Upewleia riifiosa. — AMNH 109861 (CS). ZacJiaenus i)aiviihis. — KU 107090 (CS), 107091. Zacliacnus wseus. — USNM type). Zachaenus stejnc^rri. — KU 92747. 13336, KU 9,3082 (CS), 15126 (holo- 92742 (CS), LYNCH: LEPTODACTYLOID FROGS 229 LITERATURE CITED Ameghixo, F. 1899. Sinopsis geologico-palentologica. Sup- lemento ( Adiciones y conecciones ) . La Plata, Imprenta y Encuademacion "La Libertad," pp. 1-13. 1901. Lage des formations sedinientaires de Patagonie. An. Soc. Cient. Argentina, 51:65-91. Andersson, L. G. 1945. Batrachians from east Ecuador col- lected 1937, 1938 by Wm. Clarke- Macintyre and Rolf Blomberg. Arkiv for Zoologi, 37A (2):l-88. Audley-Charles, M. G. 1966. Mesozoic palaeogeography of Aus- tralasia. Palaeogeography, Palaeocli- matol., Palaeoecol., 2:1-25. AUFFENBERG, W. A. 1958. A small fossil herpetofauna from Bar- buda, Leeward Islands, with a de- scripticm of a new species of Hyla. Quart. J. Florida Acad. Sci., 21:248- 254. AXELROD, D. I. AXD BaILEY, H. P. 1968. Cretaceous dinosaur e.xtinction. Evo- lution, 22:595-611. Bailey, H. P. 1960. A method of determining the wannth and temperateness of climate. Geo- grafiska Ann., 42:1-16. 1964. Toward a unified concept of the tem- perate climate. The Geol. Rev., 54:516-545. Baldauf, R. J. AXD Taxzer, E. C. 1965. Contributions to the cranial morphol- ogy of the leptodactylid frog, Sijrrho- phus marnocki Cope. Texas ]. Sci., 17:71-100. Barbieri, F. D. 1950. Observaciones sobre los cromosomas y espermatozoids en algunos batracios del genero Leptodactylus. Acta Zool. Lilloana, 9:455-462. 1954. Observaciones preliminares sobre los cromosomas de Tebnatohius schreiteri. Sci. Genetica, 4:223-226. Barbour, T. 1930. A list of Antillean reptiles and am- phibians. Zoologica, 11:61-116. Barbour, T. and Noble, G. K. 1920. Some amphibians from northwestern Peru, with a revision of the genera Pliyllohates and Tebnatohius. Bull. Mus. Comp. Zool., 63:393-427. Barrio, A. 1954. Sistematica, morfologia y reproduccion de Physalaemus henselii (Peters) y Pseudopaludicola falcipes ( Hensel ) / (Anura, Leptodactylidae ) . Physis, 20:380-389. 1967a. Batmchyla antartandica n. sp. (Anura, Leptodactylidae) / descripcion y es- tudi(j comparativo con la especie geno- tipica, B. leptopus Bell. Ihid., 27:101- 109. 19671). Obser\aciones etoecologicas sobre Hylorina sylvatica Bell (Annra, Lepto- dactylidae). Ihid., 27:153-157. 1968. Revision del genero Lepidohatrachus Budgett ( Anura, Ceratophrynidae ) . Ihid., 28:95-106. 1970. Insuctophiynus acarpicus, un nuevo leptodactilido firmisternio sudameri- cano (Amphibia; Anura). Ihid., 30:331-341. Barrio, A. axd Rinaldi de Chieri, P. 1970a. Estudios citogeneticos sobre el genero Pleuiodema, y sus consecuencias evo- lutivas ( Amphibia, Anura, Lepto- dactylidae). Ibid., 30:309-319. 1970b. Relaciones cariosistematicas de los Ce- ratophryidae de la Argentina (Am- phibia, Anura). Ibid., 30:321-329. Batistic, R. F., BEgAK, M. L., and ViZOTTO, L. D. 1969. Variacao cromossomica no genero Pseudopahidicola (Anura). Ciencia e Cultura, 21:260. BEgAK, M. L. 1968. Chromosomal analysis of eighteen species of Anura. Caryologia, 21:191- 208. Becak, NL L., BEgAK, W., axd Rabello, M. N. 1966. Cytological evidence of constant tetra- ploidy in the bisexual South American frog Odontophrynus aniericantis. Chro- mosoma, 19:188-193. BEgAK, M. L., Denaro, L. and BEgAK, W. 1970. Polyploidy and mechanisms of karyo- typic diversification in Amphibia. Cytogenetics, 9:225-238. Bell, T. 1843. Reptiles. In C. Darwin, The zoology of the voyage of the HMS 'Beagle' . . ., vol. 5, 51 pp. Berg, C. 1896. Batracios argentinos. Anales Mus. Nac. Buenos Aires, (2) 5:147-226. BOGART, T- P. 1967. Chromosomes of the South American amphibian family Ceratophridae (sic) with a reconsideration of the taxo- nomic status of Odontophrynus amer- icanus. Canadian ]. Genetics and Cy- tology, 9:531-542." 1970. Systematic problems in the amphibian family Leptodactylidae (Anura) as indicated by karyotypic analysis. Cy- togenetics, 9:369-383. 230 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY BOKERMANN, W. C. A. 1951. Sinopse des especies brasileiras do genero Cyclorarnphus Tschudi, 1838. Arq. Mus. Nac, 42:77-106. 1962. Observances biologicas sobre "Physa- laemus cuvieri" Fitz., 1826. (Amphib- ia, Salientia). Rev. Brasil. Biol., 22:391-399. 1963. Girinos de anfibios brasileiros — 2. Ibid., 23:349-353. 1965. Notas sobre as especies de Thoropa Fitzinger ( Amphibia, Leptodactyli- dae). Anais Acad. Brasileira Ciencias, 37:525-537. 1966. Lista anotada das locahdades tipo de anfibios Brasileiros. Servico documen- tacao, Sao Paulo, Brasil, RUSP. 1967. Una nueva especie de Elosia de Itatiaia, Brasil ( Amphibia, Lepto- dactylidae). Neotropica, 13:1.35-137. BOULENGER, G. A. 1882. Catalogue of die Batrachia Salientia s. Ecaudata in the collections of the British Museum. 2nd Ed. .\\ i + 503 pp. 1897. The tailless batrachians of Europe. The Ray Society. Vol. 1, 210 pp. 1905. Descriptions of new tailless batra- chians in the collection of the British Museum. Ann. Mag. Nat. Hist., 7 (16):180-184. 1907. Description of a new frog of the genus Tehnatobius from Brazil. Ihid., 7 (19): 394. 1908. A revision of the oriental pelobatid batrachians (genus Me^alophrijs). Proc. Zool. Soc. London, 1908:407-430. 1912. Some remarks on the habits of British frogs and toads. Ibid., 1912 (1):19- 22. 1919. On the genus Lcpidobatrachti.s Bud- gett. Ann Mag. Nat. Hist., 9 (3):531- 533. Breder, C. M. Jr. 1946. Amphibians and reptiles of the Rio Chucunaque drainage, Darien, Pan- ama with notes on their life histories and habits. Bull. Amer. Mus., 86:375- 4,36. Bruch, C. 1863. Neue Beobachtungen zur Naturge- schichte der einheimischen Batrachier und Bericht iiber das Brutjahr. Wiirzb. Nat. Z., 4:92-151. Brum-Zorilla, N, and Saez, F. A. 1968. Chromosomes of Leptodactylidae (Am- phibia, Anura). Experimenta, 24:969. Burger, W. L. 1954. Two family-groups of neotropical frogs. Herpetologica, 10:194-196. Carvalho, a. L. 1946. Um novo genero de ceratophrydideo do sudeste bahiano. Bol. Mus. Nac, N. S. Zool., 73:1-18. Casamiquela, R. M. 1959. Un anuro gigante del Mioceno de Patagonia. Rev. Asoc. Geol. Argen- tina, 13:171-183. 1963. Sobre un par de anuros del Mioceno de Rio Negro ( Patagonia ) Wawelia gerholdi n. gen. et sp. ( Ceratophrydi- dae) y Gigantobatraclnis parodii (Lep- todactylidae). Ameghiniana (Rev. Asoc. Paleont. Argentina), 3:141-160. Cei, J. M. 1955. Chacoan batrachians in central Argen- tina. Copeia, (4):291-293. 1958. Las laminas originales del suplemento a los batraquios Chilenas de Philippi: primera impresion y comentario. Inv. Zool. Chilenas, 4:265-268, 10 pis. 1960. A survey of the leptodactylid frogs, genus Eupsophus, in Chile. Breviora, 118:1-13. 1962a. Batracios de Chile. Univ. Chile, Santi- ago, cviii + 128 pp. 1962b. El genero Eupsophus en Chile. Inv. Zool. Chilenas, 8:7-42. 1965. The relationships of some ceratophryid and leptodactylid genera as indicated by precipitin tests. Herpetologica, 20:217-224. 1968a. Notes on the tadpoles and breeding ecology of LepidobatracJiiis (Amphib- ia: Ceratophryidae ) . Ibid., 24:141- 146. 1968b. A new frog of the genus Syrrhophus from the Bolivian Plateau. J. Herpetol., 2:137-141. Cei, J. M., Erspamer, V., and Roseghini, M. 1968. Taxonomic ajid evolutionary signif- icance of biogenic amines and poly- peptides occurring in amphibian skin. I. Neotropical leptodactylid frogs. Syst. Zool., 16:328-342. Cei, J. M. and Roig, V. G. 1968. Telmatobiinos de las lagunas basalticas de Neuquen (Anura, Leptodactylidae). Physis, 27:265-284. Chaxtell, C. J. 1964. Some Mio-Pliocene hylids from the Valentine formation of Nebraska. Amer. Midi. Nat., 72:211-225. Clemens, W. A. 1968. Origin and early evolution of mar- supials. Evolution, 22:1-18. COGHRAN, D. M. 1938. Diagnoses of new frogs from Brazil. Proc. Biol. Soc. Washington, 51:41-42. 1953. Three new Brazilian frogs. Herpeto- logica, 8:111-15. 1955. Frogs of southeastern Brazil. Bull. U. S. Natl. Mus., 206. xvi + 423 pp. LYNCH: LEPTODACTYLOID FROGS 231 1961a. Living amphibians of the world. Doubleday & Co., Inc. 199 pp., nu- merous color plates. 1961b. Type specimens of reptiles and am- phibians in the U. S. National Mu- seum. Bull. U. S. Natl. Mus., 220. 291 pp. Cochran, D. M. and Coin, C. J. 1959. A new frog of the genus Limnomedusa from Colombia. Copeia (3):208-210. 1961. A new genus and species of frog (Leptodactylidae ) from Colombia. Fieldiana • Zool., 39:543-546. 1970. Frogs of Colombia. Bull. U. S. Natl. Mus., 288:xii + 655 pp. Cope, E. D. 1863. On Trachycephalus, Scaphiopus and other American Batrachia. Proc. Acad. Nat. Sci. Philadelphia, 1863:43-54. 1865. Sketch of the primary groups of Ba- trachia Salientia. Nat. Hist. Rev., 5:97-120. 1866. On the structure and distribution of the genera of arciferous Anura. J. Acad. Nat. Sci. Philadelphia, (2) 6:67-112. 1889. The Batrachia of North America. Bull. U. S. Natl. Mus., 34:7-525. 1890. Scientific results of the explorations by the U. S. Fish Commission steamer Albatross No. HI — Report on the ba- trachians and reptiles collected in 1887-'88. Proc. Natl. Mus., 12:141- 147. Darlington, P. J. 1957. Zoogeography: the geographical dis- tribution of animals. John Wiley & Sons, Inc. New York. 1965. Biogeography of the southern end of the world. Harvard Press, Cambridge. Davis, D. D. 1935. A new generic and family position for Bufo borbonica. Zool. Ser., Field Mus. Nat. Hist., 20:87-92. 1936. The distribution of Bidder's organ in the Bufonidae. Ibid., 20:115-125. Davis, D. D. and Gore, U. R. 1936. Clearing and staining skeletons of small vertebrates. Fieldiana • Tech- nique, 4:1-16. Dixon, J. R. 1957. Geographic variation and distribution of the genus Tomodactylus in Mexico. Texas J. Sci., 9:379-409. Dixon, J. R. and Webb, R. G. 1966. A new Syrrhophus from Mexico (Am- phibia: Leptodactylidae). Cont. Sci. Los Angeles Co. Mus., 102:1-5. DUELLMAN, W. E. 1967. Additional studies on chromosomes of anuran amphibians. Syst. Zool., 16:38- 43. DuELLMAN, W. E. AND TrUEB, L. 1966. Neotropical hylid frogs, genus Smi- lisca. Univ. Kansas Pubis. Mus. Nat. Hist., 17:281-375. DUMERIL, A. M. C. AND BiBRON, G. 1841. Erpetologie generale. Vol. 8 iv + 792 pp. Dunn, E. R. 1931. New frogs from Panama and Costa Rica. Occ. Papers Boston Soc. Nat. Hist., 5:385-401. 1944. Herpetology of the Bogota area. Rev. Acad. Colombiana Cien. Ex. Fis. Nat., 6:68-81. 1949. Notes on the South American frog genus Edalorhina. Amer. Mus. Novi- tates, 1416:1-10. Dunn, E. R. and Dunn, M. T. 1940. Generic names proposed in herpetol- ogv by E. D. Cope. Copeia (2):69- 76. du Toit, C. a. 1930. Die skedel morphologie van Heleo- phnjne regis. S. African J. Sci., 27:226-238. 1931. 'N korreksie van my verhandeling oor die skedelmorphologie van Heleo- phrtjne regis. Ibid., 27:408-410. Donoso-Barros, R. 1969. Posicion nomenclatural de un lepto- dactyido uruguayo (Amphibia-Anura). Bol. Soc. Biol. Concepcion, 41:161- 162. Eaton, T. H. 1958. An anatomical study of a neotropical tree frog, Centrolene prosoblepon ( Sa- lientia: Centrolenidae ) . Univ. Kansas Sci. Bull., 34:459-472. ESTES, R. 1964. Fossil vertebrates from the Late Cre- taceous Lance Formation/eastern Wy- oming. Univ. California Pubis. Geol. Sci., 49:1-180. 1969. A new fossil discoglossid frog from Montana and Wyoming. Breviora, 328:1-7. 1970. New fossil pelobatid frogs and a re- view of the genus Eopelobates. Bull. Mus. Comp. Zool., 139:293-340. EsTES, R. AND WaSSERSUG, R. 1963. A Miocene toad from Colombia, South America. Brevora, 193:1-13. Etheridge, R. 1960. The relationship of the anoles ( Rep- tilia: Sauria: Iguanidae): an interpre- tation based on skeletal morphology. Unpublished doctoral dissertation, Univ. Michigan. 236 pp. FiTZINGER, L. J. F. J. 1826. Neue Classification der Reptilien nach ihren natiirlichen Verwandtschaften. 66 pp. 1843. Systema Reptilium. Vienna. 106 pp. 232 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Fletcher, J. J. 1889. Observations on the oviposition and habits of certain Australian batra- chians. Proc. Linn. Soc. New South Wales, 4:357-387. Gadow, H. 190L Amphibia and Reptiles. Vol. 8. In S. F. Harnier and A. E. Shipley, eds. The Cambridge Natural History. Lon- don. Gallahdo. J. M. 1961. On the species of Pseudidae (Amphib- ia, Anura). Bull. Mus. Comp. Zool., 125:108-134. 1962. Los generos TeJmatohius y Batracho- phrynus (Amphibia, Leptodactylidae) en la Argentina. Neotropica, 8:45-58. 1963. Hijdrolactare, nuevo genero de Lepto- dactylidae (Amphibia) neotropical. Ibid., 9:42-48. 1964. "Leptodactylus prognathus" Boul. y "L. mystacinus" ( Burm. ) con sus re- spectivas especies aliadas ( "Amphibia, Leptodactylidae" del grupo "Cavi- cola"). Rev. Mus. Argentino Cien. Nat. "Bernardino Rivadavia," 6:89- 121. 1965. A proposito de los Leptodactylidae (Amphibia, Anura). Papeis Avulsos, 17:77-87. 1970. A proposito de los Telmatobiinae (Anura, Leptodactylidae) patagonicos. Neotropica, 16:73-85. Coin, C. J. 1946. Studies on the life history of Elcii- thewdactyltis ricordi planirostris. Univ. Florida Studies Biol. Sci., (4) 2:1-66. 1959. Notes on the maxillary dentition of some frogs of the genera Elettthew- dactyhis and Leptodactylus. Herpeto- logica, 15:134-136. Coin, C. J- and Cochran, D. M. 196.3. Two new genera of leptodactylid frogs from Colombia. Proc. California Acad. Sci., 31:499-505. GOHHANI, S. W. 1966. Liste der rezenten Amphibien und Reptilien. Ascaphidae, Leiopelmatidea (sic), Pipidae, Discoglossidae, Pelo- batidae, Leptodactylidae, Rhinophryn- idae. Das Tierreich, 85. x\'i + 222 pp. COSXER, K. L. 1960. A simplified table for staging anuran embryos and lai"vae with notes on identification. Herpetologica, 16:183- 190. Grandison, a. G. C. 1961. Chilean species of the genus Eupso- phus (Anura: Leptodactylidae). Bull. British Mus. (Nat. Hist.), 8:111-149. Gravenhorst, J. L. C. 1825. Stombus, eine neue Amphibien Gat- tung. Isis von Oken, 1825:920-922. 1829. Delicae Musei Zoologici Vratislavi- ensis. Reptilia Musei Zoologici Vrati- slaviensis recensita et descripta . . . continens Chelonias et Batrachia. 186 pp. Griffiths, I. 1954. On the otic element in Amphibia, Salientia. Proc. Zool. Soc. London, 124:35-50. 1959. The phylogeny of Sminthillus limbatus and the status of the Brachycephalidae (Amphibia, Salientia). Ibid., 132:457- 487. 1960. The phylogenetic status of the Sooglos- sinae. Ann. Mag. Nat. Hist., 13 (2): 626-640. 1963. The phylogeny of the Salientia. Bio- logical Reviews, 38:241-292. GiJNTHER, A. C. L. G. 1859a. Catalogue of the Batrachia Salientia in the collection of the British Museum, xvi -f 160 pp. 1859b. On sexual diflerences found in bones of some Recent and fossil species of frogs and fishes. Ann. Mag. Nat. Hist., 3 (3): 377-386. Halla.m, a. 1967. The bearing of certain palaeozoogeo- graphic data on continental drift. Palaeogeography, Palaeoclimatol., Pa- laeoecol., 3:201-241. Harrington, H. J. 1962. Paleogeographic development of South America. Bull. Amer. Assoc. Petro- leum Geol., 46:1773-1814. Harrison, L. 1927. Notes on some western Australian frogs, with descriptions of new species. Rec. Australian Mus., 15:277-287. Hfatwole, H. 1962. Contributions to the natural history of Eleutherodactylus cornutus maussi. Stahlia, Misc. Papers, 2:1-11. Hecht, M. K. 1959. Amphibia and reptiles, pp. 130-146. /;i P. O. McGrew, The geology and paleontology of the Elk Mountain and Tabernacle Butte area, Wyoming. Bull. Amer. Mus., 117:121-176. 1960. A new frog from an Eocene oil-well core in Nevada. Amer. Mus. Novi- tates, 2006:1-14. 1963. A reevaluation of the early history of the frogs. Part II. Syst. Zool., 12:20- 35. Hecht, M. K. and Estes, R. 1960. Fossil amphibians from Quarry Nine. Postilla, 46:1-19. LYNCH: LEPTODACTYLOID FROGS 233 Heyer, VV. R. 1968. The proper name for the type-species of the genus Lcptodactijhis. Copeia (1):160-162. 1969a. Biosysteniatic studies on the frog genus Leptodactylus. UnpubUshed doctoral dissertation, Univ. Southern California. 234 pp. 1969b. Studies on the genus Leptodacttjhis (Amphibia, Leptodactylidae ) III. A redefinition of the genus Leptodactylus and a description of a new genus of leptodactylid frogs. Cont. Sci. Los Angeles Co. Mus., 115:1-14. Hoffman, A. C. 1930. Description of the external characters and of the shoulder girdle of Helco- pJiryne; and a note on the systematic position of the genus. South African J. Sci., 27:414-425. 1935. Die sistematiese posisie van Heleo- phnjne. Sool. Navors, nas. Mus. Bloemfontein, 1:1-2. HOLMAN, J. A. 1965. Early Miocene anurans from Florida. Quart. J. Florida Acad. Sci. 28:68-82. 1967. Additional Miocene anurans from Florida. Ibid., 30:121-140. HOSMER, W. 1962. A new leptodactylid frog of the genus Notaden from northern Australia. Amer. Mus. Novitates, 2077:1-8. Huxley, J. S. 1958. Evolutionary processes and taxonomy with special reference to grades. Uppsala ITniv. Arssks., 1958:21-38. IXGER, R. F. 1954. Systematics and zoogeography of Phil- ippine Amphibia. Fieldiana • Zool., 33:181-531. 1958. Comments on the definition of genera, Evolution, 12:370-384. 1966. The systematics and zoogeography of the Amphibia of Borneo. Fieldiana • Zool., 52:1-402. 1967. The development of a phylogeny of frogs. Evolution, 21:369-384. Jacobs, C, Burgl, H., and Conley, D. L. 1963. Backbone of Colombia. Mem. Amer. Assoc. Petroleum Geol., 2:62-72. Jameson, D. L. 1955. Evolutionary trends in the courtship and mating behavior of Salientia. Svst. Zool., 4:105-119. Kluge, A. G. 1967. Higher taxonomic categories of gek- konid lizards and their evolution. Bull. Amer. Mus. Nat. Hist., 135:1-59. Kluge, A. G. and Farris, J. S. 1969. Quantitati\e phyletics and the evolu- tion of anurans. Syst. Zool., 18:1-32. KUHN, O. 1965. Die Amphibien / System und Stam- mesgeschichte. Verlag Oeben. 102 pp. Latsky, L. 1930. Die sistematiese posiesie van Heleo- phryne met betrekling tot die klassi- fikasie van Noble (1922). South Afri- can J. Sci., 27:442-445. Laurent, R. 1951. Sur la necessite de supprimer la famille des Rliacophoridae mais de creer celle des Hyperoliidae. Rev. Zool. Bot. African, 45:116-122. Lee, a. K. 1966. Studies in Australian Amphibia. II. Taxonomy, ecology, and evolution of the genus Heleiopoms Gray (Anura: Leptodactylidae). Australian T- Zool., 15:367-439. Limeses, C. E. 1963. La musculatura del muslo en las especies del genero Lepidobatmchus (Anura - Ceratophrynidae ) . Physis, 24:205-218. 1964. La musculatura del muslo en los ce- ratofrinidos y formas afines con un analisis critico sobre la significacion de los caracteres miologicos en la sis- tematica de los anuros superiores. Cont. Cientificas, Ser. Zool., Univ. Buenos Aires, 1:193-245. 1965. La musculatura mandibular en los ceratof rinidos y formas afines ( Anura, Ceratophrynidae). Physis, 25:41-58. LiNNE, C. 1758. Systema naturae. 10th ed., vol. 1. LiTTLEJOHN, M. J. 1963. The breeding biology of the baw baw frog Philoria frosti Spencer. Proc. Linn. Soc. New South Wales, 88:273- 276. 1968. Patterns of zoogeography and speci- ation in south-eastern Australian Am- phibia, pp. 150-174. In A. H. Weath- erley, ed., Australian Inland Waters and their Fauna. Australian National Univ. Press, Canberra. Liu, C. C. 1936. Secondary sex characters of Chinese frogs and toads. Zool. Ser., Field Mus. Nat. Hist., 22:113-156. 1950. Amphibians of western China. Fieldi- ana ■ Zool. Mem., 2:1-400. Lloyd, J. J. 1963. Tectonic history of the south Central- American orogen. Mem. Amer. Assoc. Petroleum Geol., 2:88-100. Loveridge, a. 1933. A new genus and three new species of crinine frogs from Australia. Occ. Pa- pers Boston Soc. Nat. Hist., 8:89-93. 234 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY 1935. LuTz, A. 1929. 1930. LuTz, B. 1944. 1954. 1958. LuTZ, B. 1958. Lynch, J 1964. 1965. 1966. 1967. 1968a. 1968b 1968c. 1968d. 1969a. Australian Amphibia in the Museum of Comparative Zoology, Cambridge, Massachusetts. Bull. Mus. Comp. Zool., 78:1-60. Taxonomia e biologia do genero Cy- cloramplius. Mem. Inst. Oswaldo Cruz, 22:5-25. Second paper on Brasilian and some closely related species of the genus Leptodactylus. Ibid., 23:21-34. Biologia e taxonomia de Zachaenus parvulus. Bol. Mus. Nac, Zool., 17:1- 66. Anfibios anuros do Distrito Federal. Mem. Inst. Oswaldo Cruz, 52:155-2.38. Anfibios novos e raros das Serras Costeiras do Brasil ( New or rare frogs from the Coastal Ranges of Brazil) Eleutherodactijhis venancioi n. sp., E. hoehnei n. sp. / Holoaden bradei n. sp. e H. liiderwaldti Mir.Rib., 1920. Ibid., 56:373-399. AND CaRVALHO, a. L. Novos anfibios anuros das Serras Cos- teiras do Brasil. Ibid., 56:239-249. .D. Additional hylid and leptodactylid re- mains from the Pleistocene of Texas and Florida. Herpetologica, 20:141- 142. A review of the eleutherodactylid frog genus Micwbatrachylus (Leptodactyl- idae). Nat. Hist. Miscellanea, 182:1- 12. The status of the tree frog, Hyla barbttdensis Auffenberg, from Bar- buda, British West Indies. Copeia (3):524-530. Epirhexis Cope, 1866 (Amphibia: Salientia ) : Request for suppression under the plenary powers. Bull. Zool. Nomencl., 24:313-315. Genera of leptodactylid frogs in Mex- ico. Univ. Kansas Pubis. Mus. Nat. Hist., 17:50.3-515. The identity of a Chilean frog, Alsodes nionticola Bell, and the status of the genus Alsodes (Amphibia: Lepto- dactylidae). Herpetologica, 24:255- 257. The status of the nominal genera Ba- sanitia and Phrynanodus from Brazil (Amphibia: Leptodactylidae ) . Copeia (4): 875-876. Systematic status of some Andean leptodactylid frogs with a description of a new species of Eleutherodactylus. Herpetologica, 24:289-300. The identity of the frog, Pseudohyla nigrogrisea of Ecuador. Bull. So. Cali- fornia Acad. Sci., 68:219-224. 1971. MS. 1969b. Taxonomic notes on Ecuadorian frogs (Leptodactylidae: Eleutherodactylus ) . Herpetologica, 25:262-274. 1970a. A taxonomic revision of the lepto- dactylid frog genus Syrrhophus Cope. Univ. Kansas Publ. Mus. Nat. Hist., 20:1-45. 1970b. Systematic status of the American leptodactylid frog genera Engysto- mops, Eupemphix, and Physalaemus. Copeia, (3): 488-496. Generic partitioning of the South American frog genus Eupsophus Fitz- inger, 1843 (Sensu lato). Bull. South. California Acad. Sci. (in press). The transition from archaic to ad- vanced frogs. In Vial, J. L., ed. Evo- lutionary biology of the anura. Univ. Missouri Press, ( in press ) . Lynn, W. G. 1942. Embryology of Eleutherodactylus 7iu- bicola, an anuran which has no tad- pole stage. Carnegie Inst. Washing- ton / Cont. Enibr., (190):27-62. Lynn, W. G. and Lutz, B. 1946a. The development of Eleutherodactylus guentheri. Bol. Mus. Nac, Zool., 71:1- 46. 1946b. The development of Eleutherodactylus nasutus. Ibid., 79:1-42. Main, A. R. 1957. Studies in Australian Amphibia. I. The genus Crinia Tschudi in south- western Australia and some species from south-eastern Australia. Aus- tralian J. Zool., 5:30-55. Main, A. R., Lee, A. K., and Littlejohn, M. J. 1958. Evolution in three genera of Aus- tralian frogs. Evolution, 12:224-233. Main, A. R. and Storr, G. M. 1966. Range extensions and notes on the bi- ology of frogs from the Pilbara region, Western Australia. Western Australian Nat., 10:53-61. Martin, A. A. 1965. Tadpoles of the Melbourne area. The Victorian Nat., 8:139-149. 1968. Australian anuran life histories; some evolutionary and ecological aspects, pp. 175-191. In A. H. Weatherley, ed., Australian Inland Waters and their Fauna. Australian National Univ. Press, Canberra. Mayr, E. 1963. Animal species and evolution. Belknap Press, Harvard. Mayr, E., Linsley, E. G., and Usinger, R. L. 1953. Methods and principles of systematic zoology. McGraw Hill Book Co., Inc. Mecham, J. S. 1959. Some Pleistocene amphibians and rep- tiles from F'riesenhahn Cave, Texas. Southwest. Nat., 3:17-27. LYNCH: LEPTODACTYLOID FROGS 235 Merely, L. von 1904. Investigations on Paraguayan batra- chians. Ann. Mus. Nat. Hungarici, 2:207-232. Melin, D. 1941. Contributions to the knowledge of the Amphibia of South America. Medd. Goteborgs Mus. Zooh Avdel., 88:1-71. MiLSTEAU, W. W. 1963. Notes on Brazilian frogs of the genus Phijsalaemus and Pseitdopahidicola. Copeia (3): 565-566. MlRANDA-RlBEIRO, A. 1920. O genero Telmatobius ja foi contatado no Brasil? Rev. Mus. Paulista, 12:261- 278. 1926. Notas para servirem ao estao dos Gymnobatrachios (Anura) brasileiros. Arq. Mus. Nac., 27:1-227. MivART, St. G. 1869. On the classification of the anurous batrachians. Proc. Zool. Soc. London, 1869:280-295. MoORE, J. A. 1958. A new genus and species of lepto- dactylid frog from Australia. Amer. Mus. Novitates, 1919:1-7. 1961. The frogs of eastern New South Wales. Bull. Amer. Mus. Nat. Hist., 121:149- 386. MORESCALCHI, A. 1967. The close karyological affinities be- tween a Ceratophrys and Pelobates (Amphibia Salientia). Experientia, 23:1071. MORESCALCHI, A. AND GaRGIULO, G. 1968. Su alcune relazioni cariologiche del genere Biifo ( Amphibia Salientia ) . Rend. Ace. Sc. Fis. Mat. Napoli (4) 35:117-120. MORESCALCHI, A., GaRGRTLO, G. AND OlMA, E. 1968. Note citotassonomiche sui Lepto- dactylidae (Amphibia Salientia). Bull. di Zool., 35:333-334. Myers, G. S. 1946. Lista provisoria dos anfibios do Dis- trito Federal, Brasil. Bol. Mus. Nac, Zool., 55:1-36. 1962. The American leptodactylid frog gen- era Eleutherodactylus, Hijlodes (— Elosia), and Caiidiverbera (= Cahjpto- cephalus). Copeia ( 1 ) : 195-202. NiEDEN, F. 1923. Anura I. Subordo Aglossa und Pha- neroglossa, Sectio 1 Arcifera. Das Tiereich, 46: xxxii + 584 pp. Noble, G. K. 1917. The systematic status of some batra- chians from South America. Bull. Amer. Mus., 37:793-814. 1921. Five new species of Salientia from South America. Amer. Mus. Novitates, 29:1-7. 1922. The phylogeny of the Salientia I. — The osteology and the thigh muscula- ture; their bearing on classification and phylogeny. Bull. Amer. Mus. Nat. Hist., 46:1-87. 1924. A new spadefoot toad from the Oligo- cene of Mongolia with a sunnnary of the evolution of the Pelobatidae. Amer. Mus. Novitates, 132:1-15. 1925. A new genus of Surinam toad ( Pipi- dae). Ibid., 164:1-3. 1926a. The hatching process in Ahjtes, Eleu- tJierodactijhis and other amphibians. Ibid., 229:1-7. 1926b. The pectoral girdle of the brachy- cephalid frogs. Ibid., 230:1-14. 1926c. An analysis of the remarkable cases of distribution among the Amphibia, with descriptions of new genera. Ibid., 212:1-24. 1927. The value of life-history data in the study of the evolution of the Amphib- ia. Ann. New York Acad. Sci., 30:31- 128. 1930. The fossil frogs of the Intertrappean beds of Bombay, India. Amer. Mus. Novitates, 401:1-13. 1931. The biology of the Amphibia. Mc- Graw-Hill Book Co., Inc. New York. 577 pp. Orton, G. L. 1952. Key to the genera of tadpoles in the United States and Canada. Amer. Midi. Nat., 47:382-395. 1953. The systematics of vertebrate larvae. Syst. Zool., 2:63-75. 1957. The bearing of larval evolution on some problems in frog classification. Ibid., 6:79-86. Parker, H. W. 1926. A new brachycephalid frog from Bra- zil. Ann. Mag. Nat. Hist., 9 (18):201- 203. 1927. A revision of the frogs of the genera Pseudopaludicola, Physalaemus, and Pleurodema. Ibid., 9 (20):450-478. 1931. Report of an expedition to Brazil and Paraguay in 1926-27. . . . Amphibia and Reptilia. J. Linn. Soc. London, 37:285-289. 1932. The systematic status of some frogs in the Vienna Museum. Ann. Mag. Nat. Hist., 10 (10):341-344. 1934. A monograph of the frogs of the fam- ily Microhylidae. British Museum, London. 1935. The frogs, lizards, and snakes of Brit- ish Guiana. Proc. Zool. Soc. London, 1935 (3): 505-530. 1940. The Australasian frogs of the family Leptodactylidae. Novitates Zoologicae, 42:1-106. 236 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY Parsons, T. S. and Williams, E. E. 1962. The teeth of Amphibia and their rela- tion to amphibian phylogeny. J. MorphoL, 110:375-389. 1963. The relationships of the modern Am- phibia / A re-examination. Quart. Rev. Biol., 38:26-53. Peracc.\, M. G. Conte de 1914. Reptiles et Batrachiens de Colombie. Mem. Soe. Neuchatel Nat. Hist., 5:96- 1902. Suplemento a los Batraquios Chilenas 111. Philippi, R. a. (deD. C. Gay). Santiago, Chile. 160 pp. Piatt, J. 1934. The systematic status of Eleuthero- dactylus latrans (Cope). Amer. Midi. Nat.. 15:89-91. Pope, C. H. 1931. Notes on amphibians from Fukien, Hainan, and other parts of China. Bull. Amer. Mus. Nat. Hist., 61:397- 611. POYXTOX, J. C. 1964. The Amphibia of southern Africa: a faunal study. Ann. Natal Mus., 17:1- oo4. Rabb, G. B. and Rabb, M. S. 1960. On the mating and egg-laying be- havior of the Surinam toad, P/;>fl ))ipa. Copeia (4):271-276. 1963a. On the behavior and breeding history of the African pipid frog, Uijmcno- cliinis hoettjicri. Zeitschrift fiir Tier- psychologie, 20:215-241. 1963b. Additional observations on breeding belia\ior of the Surinam toad, Pipa pi]>a. Copeia (4):636-642. Rahello, M. N. 1970. Chromosomal studies in Brazilian anurans. Caryologia, 23:45-59. Reig, O. a. 1958. Proposiciones para una nueva macro- sistematica de los anuros. Physis, 21:109-118. 1960a. Las relaciones genericas del anuro Chileno Cali/ptocephaleUa gayi (Dum. & Bibr. ). Actas y Trabajos Primer Congreso Sudamericano de Zoologica, 4:113-131. 1960b. La anatomia esqueletica del genero Lepidohairacliiis (Anura, Leptodactyl- idae), comparada con la de otros ceratofrinos. Ihid., 4:133-147. Reig, O. A. and Cei, J. M. 1963. Elucidacion morfologico-estadistica de las entidades del genero Lepicloba- tiacliiis Budgett (Anura, Ceratophryni- (lac), con consideraciones sobre la ex- tension del Distrito Chaqueiio del dominio zoogeografico subtropical. Physis, 24:181-204. Reig, O. A. and Llmeses, C. E. 1963. Un nuevo genero de anuros ceratofri- nidos del distrito Chaqueno. Ibid., 24:113-128. RiVEHO, J. A. 1961. Salientia of Venezuela. Bull. Mus. Comp. Zool., 126:1-207. 1968. A new species of Elosia ( Amphibia, Salientia) from Mt. Duida, \'enezuela. Amer. Mus. Novitates, 2334:1-9. RUSCONI, C. 1932. La presencia de anfibios ( "Ecuadata") y de aves fosiles en el piso ensenadense de Buenos Aires. An. Soc. Cient. Argentina, 113:145-149. RUTHVEN, A. G. 1915. Description of a new tailless amphib- ian of the family Dendrobatidae. Occ. Papers Mus. Zool. Univ. Mich- igan, 20:1-3. I9I9. The amphibians of the University of Michigan — Walker expedition to Brit- ish Guiana. //j;V/., 69:1-14. Saez, F. a. and Brum, N. 1959. Citogenetica de anfibios anuros de America del Sur. Los cromosomas de Odontophrtjnus americanus y Cerato- phnjs oniata. Anal. Fac. Med. Monte- video, 44:414-423. 1960. Chromosomes of some South Amer- ican amphibians. Nature, 185:945. Saez, F. A. and Brum-Zorilla, N. 1966. Karyotype variation in some species of the genus Odontophrynus (Amphibia — Anura). Caryologia, 19:55-63. Savage, J. M. 1966. The origins and history of the Central American herpetofauna. Copeia (4):719-766. Savage, J. M. and Carvalho, A. L. 1953. The family position of neotropical frogs currentlv referred to the genus Pseudis. Zoologica, 38:193-200. Savage, J. M. and Cei, J. M. 1965. A review of the leptodactylid frog genus, Odontophrymts. Herpetologica, 21:178-195. Schaeffer, B. 1949. Anurans from the early Tertiary of Patagonia. Bull. Amer. Nat. Hist., 93:47-68. Schlegel, H. 1850. Description of a new genus of batra- chians from Swann Ri\cr. Proc. Zool. Soc. London, (18): 9- 10. Schmidt, K. P. 1952. A new leptodactylid frog from Chile. Fieldiana • Zool., 34:11-15. 1954a. Notes on frogs of the genus Tehna- tobius with descriptions of two new Peruvian species. Ibid., 34:277-287. LYNCH: LEPTODACTYLOID FROGS 237 1954b. Reports of tlie Lund University Chile expedition 1948-1949. 13. An'iphibia Salientia con resumen en espaiiol. Lunds Univ. Arsskrift, N. F. Avd. 2, 49 (19):l-6. Schwartz, A. 1967. Frogs of the genus Eleutlierodactylus in the Lesser Antilles. Studies Fauna Curacao, Caribbean Is., 24:1-62. SnAW, G. 1795. (No title). Nat. Mis., 6:plate 200. Shreve, B. 1941. Notes on Ecuadorian and Peruvian reptiles and amphibians with descrip- tion of new forms. Proc. New England Zo5l. Club 18:71-83. Shrevk, B. and Williams, E. E. 1963. The frogs, pp. 302-42. In Williams, E. E., Shreve, B., and Humphrey, P. S., The herpetology of the Port-au- Prince region and Gonave Island, Haiti. Parts I-II. Bull. Mus. Comp. Zoo]., 129:291-342. SiMPSox, G. G. 1961. Principles of animal taxonomy. Co- lumbia Univ. Press, New York. Slater, P. and Main, A. R. 1963. Notes on the biology of Notaclen iiiclioUsi Parker (Anura; Leptodactyl- idae). Western Australian Nat., 8:163- 166. Smith, C. L. and Smith, G. R. 1967. A technique for making stereoscopic radiographs of animal skeletons. Copeia (4):848-850. Sporne, K. R. 1954. Statistics and the evolution of dicoty- ledons. Evolution, 8:55-64. Starrett, p. 1960. Descriptions of tadpoles of Middle American frogs. Misc. Pubis. Mus. Zool. Univ. Michigan, 110:1-37. 1967. Observations of the life history of frogs of the family Atelopodidae. Herpetologica, 23:195-204. 1968. The phylogenetic significance of the jaw musculature in anuran amphib- ians. Unpublished doctoral disserta- tion, Univ. Michigan. 179 pp. Stebbins, R. C. 1951. Amphibians of western North Amer- ica. Univ. California Press. Stejneger, L. 1904. The herpetology of Puerto Rico. Rep. U. S. Natl. Mus., 1902. pp. 549-724. Straughan, I. R. AND Main, a. R. 1966. Speciation and polymorphism in the genus Crinia Tschudi (Anura, Lepto- dactylidae) in Queensland. Proc. Royal Soc. Queensland, 78:11-28. Takeuchi, H., Uyeda, S., and Kanamori, H. 1967. Debate about the earth / approach to geophysics through analysis of conti- nental drift. Freeman, Cooper & Co., San Francisco. Thomas, A. 1854. Note sur la generation du Pelodyte ponctuc, avec quelques observations sur les batraciens anoures en general. Ann. Sci. Nat., pp. 290-293. Tihen, J. A. 1960a. Two new genera of African bufonids, with remarks on the phylogeny of re- lated genera. Copeia (3):225-233. 1960b. Notes on late Cenozoic hylid and leptodactylid frogs from Kansas, Okla- homa, and Texas. Southwestern Nat., 5:66-70. 1962a. Osteological observations on new world bufonids. Amer. Midi. Nat., 67:157-183. 1962b. A review of new world fossil bufonids. /fo/c/., 68:1-50. 1965. Evolutionary trends in frogs. Amer. Zool., 5:.309-318. Trewavas, E. 1933. The hyoid and larynx of the Anura. Philos. Trans., ( B)222:410-527. Trueb, L. 1966. Morphology and development of the skull in the frog Hijla septentrionalis. Copeia (3): 562-573. 1968. Cranial osteology of the hylid frog, Smilisca baudini. Univ. Kansas Publ. Mus. Nat. Hist., 18:11-35. 1970. Evolutionary relationships of casque- headed tree frogs with co-ossified skulls (family Hylidae). Ihid., 18:547- 716. Tschudi, J. J. 1838. Classification der Batrachier, mit Be- rucksichtigung der Fossilen Thiere disser Abtheilung der Reptilien. Neu- chatel. 102 pp. Valett, B. B. and Jameson, D. L. 1961. The embrology of Eleiithcrodactijliis augusti latiam. Copeia (1): 103-109. Vellard, J. 1948. Batracios del chaco argentino. Acta Zool. Lilloana, 5:1.37-174. 1951. Estudios sobre batracios andinos. L El grupo Telmatohitis y formas afines. Mem. Mus. Hist. Nat. "Javier Prado," (l):l-89. 1953. Estudios sobre batracios andinos II. — El grupo marmoratus y formas afines. Ibid., (2): 1-61. 1955. Estudios sobre batracios andinos III. — Los Telmatobius del grupo jelskii. z7w/., (4):l-28. 238 MISCELLANEOUS PUBLICATION MUSEUM OF NATURAL HISTORY 1957. Ill — Repartition des Batracien dans les Andes au sud de I'Equateur. Tra- vaux Inst. Frangais Estudes Andines, Lima, 5:141-161. 1960. Estudios sobre batracios andinos VI. - Notas complementarias sobre Telma- tobius. Mem. Mus. Hist. Nat. "Javier Prado," (10): 1-19. Vinson, G. L. and Brineman, J. H. 1963. Nuclear Central America, hub of the Antillean transverse belt. Mem. Amer. Assoc. Petroleum Geol., 2:101-112. VUILLEUMIER, F. 1968. Origin of frogs of Patagonian forests. Nature, 219 (5149):87-89. Werner, F. 1894. Uber einige Novitaten der herpetol- ogischen Sammlung des Wiener zoolog. vergl. anatom. Instituts. Zool. Anzeiger, 17:155-157. WiEGMANN, A. F. A. 1835. Beitrage zur Zoologie gesammelt auf einer Reise um die Erde, von Dr. F. T- F. Meyen, M. d. A. d. N. Siebente Abhandlung. Amphibien. Nova Acta Acad. Leop. Carol., 17:183-268, 268a- d. ZWEIFEL, R. G. 1956a. Two pelobatid frogs from the Tertiary of North America and their relation- ships to fossil and Recent forms. Amer. Mus. Novitates, 1762:1-45. 1956b. A survey of the frogs of the aufiusti group, genus Eleutherodacti/lus. Ibid., 1813:1-35. 1966. Cornufer unicolor Tschudi 1838 ( Am- phibia, Salientia); request for suppres- sion under the plenary po\\'ers Z. N. (S.) 1749. Bull. Zool. Nomenclat., 23:167-168. This manuscript was submitted as a disserta- tion in partial fulfillment for the requirements for the Ph.D. degree in the Department of Zoology, The University of Kansas, in March, 1969. ■Si^ 3 2044 093 361 616 Date Due BOUND 1972