AMERICAN MUSEUM NOVITATES Published by

Similar documents
Williston, and as there are many fairly good specimens in the American

SOME LITTLE-KNOWN FOSSIL LIZARDS FROM THE

2. Skull, total length versus length of the presacral vertebral column: (0); extremely elongated neck (e.g. Tanystropheus longobardicus).

Fig. 5. (A) Scaling of brain vault size (width measured at the level of anterior squamosal/parietal suture) relative to skull size (measured at the

A new species of Hsisosuchus (Mesoeucrocodylia) from Dashanpu, Zigong Municipality, Sichuan Province

THE GORGONOPSIAN GENUS, HIPPOSAURUS, AND THE FAMILY ICTIDORHINIDAE * Dr. L.D. Boonstra. Paleontologist, South African Museum, Cape Town

ONLINE APPENDIX 1. Morphological phylogenetic characters scored in this paper. See Poe (2004) for

A skull without mandihle, from the Hunterian Collection (no.

A NEW GENUS AND SPECIES OF AMERICAN THEROMORPHA

Biology 3315 Comparative Vertebrate Morphology Skulls and Visceral Skeletons

SUPPLEMENTARY INFORMATION

OF THE TRIAS THE PHYTOSAURIA

Mammalogy Laboratory 1 - Mammalian Anatomy

[Accepted 8th October CONTENTS INTRODUCTION

Postilla PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY NEW HAVEN, CONNECTICUT, U.S.A.

List of characters used in the phylogenetic analysis. Capital letters T, R, and L, refer to

The cranial osteology of Belebey vegrandis (Parareptilia: Bolosauridae), from the Middle Permian of Russia, and its bearing on reptilian evolution

ON THE SCALOPOSAURID SKULL OF OLIVIERIA PARRINGTONI, BRINK WITH A NOTE ON THE ORIGIN OF HAIR

CRANIAL ANATOMY OF ENNATOSAURUS TECTON (SYNAPSIDA: CASEIDAE) FROM THE MIDDLE PERMIAN OF RUSSIA AND THE EVOLUTIONARY RELATIONSHIPS OF CASEIDAE

Cranial osteology of the African gerrhosaurid Angolosaurus skoogi (Squamata; Gerrhosauridae) HOLLY A. NANCE

HONR219D Due 3/29/16 Homework VI

v:ii-ixi, 'i':;iisimvi'\>!i-:: "^ A%'''''-'^-''S.''v.--..V^'E^'-'-^"-t''gi L I E) R.ARY OF THE VERSITY U N I or ILLINOIS REMO

ON TWO NEW SPECIMENS OF LYSTROSAURUS-ZONE CYNODONTS

Exceptional fossil preservation demonstrates a new mode of axial skeleton elongation in early ray-finned fishes

YANGCHUANOSAURUS HEPINGENSIS - A NEW SPECIES OF CARNOSAUR FROM ZIGONG, SICHUAN

Cranial morphology and taxonomy of South African Tapinocephalidae (Therapsida: Dinocephalia): the case of Avenantia and Riebeeckosaurus

Mammalogy Lab 1: Skull, Teeth, and Terms

complex in cusp pattern. (3) The bones of the coyote skull are thinner, crests sharper and the

A new sauropod from Dashanpu, Zigong Co. Sichuan Province (Abrosaurus dongpoensis gen. et sp. nov.)

Cranial osteology and phylogenetic relationships of Hamadasuchus rebouli (Crocodyliformes: Mesoeucrocodylia) from the Cretaceous of Morocco

THE SKULLS OF ARAEOSCELIS AND CASEA, PERMIAN REPTILES

Bulletin of Big Bend Paleo-Geo An Open Access Publication from Mosasaur Ranch Museum, Terlingua and Lajitas, Texas All rights reserved

4. Premaxilla: Foramen on the lateral surface of the premaxillary body (Yates 2007 ch. 4) 0 absent 1 present

Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at

SUPPLEMENTARY ONLINE MATERIAL FOR. Nirina O. Ratsimbaholison, Ryan N. Felice, and Patrick M. O connor

Muséum national d Histoire naturelle, F-75005, Paris, France c Karoo Palaeontology, Iziko South African Museum, PO Box 61, Cape Town, 8000, South

A NEW SPECIES OF EXTINCT TURTLE FROM THE UPPER PLIOCENE OF IDAHO

A M E G H I N I A N A. Revista de la Asociación Paleontológia Argentina. Volume XV September-December 1978 Nos. 3-4

VERTEBRATA PALASIATICA

Notes on Ceratopsians and Ankylosaurs at the Royal Ontario Museum

Supporting Online Material for

A New Ceratopsian Dinosaur from the Upper

On the cranial anatomy of the polycotylid plesiosaurs, including new material of Polycotylus latipinnis, Cope, from Alabama

The skull of Sphenacodon ferocior, and comparisons with other sphenacodontines (Reptilia: Pelycosauria)

CRANIAL OSTEOLOGY OF SCHIZOTHORAICHTHYS NIGER (MECKEL) MISRA (CYPRINIDAE: SCHIZOTHORACINAE). L NEUROCRANIUM

Anatomy. Name Section. The Vertebrate Skeleton

FURTHER STUDIES ON TWO SKELETONS OF THE BLACK RIGHT WHALE IN THE NORTH PACIFIC

CRANIAL ANATOMY AND PHYLOGENETIC AFFINITIES OF THE PERMIAN PARAREPTILE MACROLETER POEZICUS

AMERICAN MUSEUM. Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET


Osteology of the Clupeiform fish, genus Hyperlophus (II)

MACROCEPHALOSAURIDAE AND POLYGL YPHANODONTIDAE (SAURIA) FROM THE LATE CRETACEOUS OF MONGOLIA

A RELICT RHINESUCHID (AMPHIBIA: TEMNOSPONDYLI) FROM THE LOWER TRIASSIC OF SOUTH AFRICA

PALEONTOLOGICAL CONTRIBUTIONS

Chapter 2 Mammalian Origins. Fig. 2-2 Temporal Openings in the Amniotes

Marshall Digital Scholar. Marshall University. F. Robin O Keefe Marshall University,

Department of Biology, Faculty of Science, Razi University, Kermanshah, Iran 2

SUPPLEMENTARY OBSERVATIONS ON THE SKULL OF

PEABODY MUSEUM OF NATURAL HISTORY, YALE UNIVERSITY NEW HAVEN, CONNECTICUT, U.S.A. THE BRAINCASE OF THE ADVANCED MAMMAL-LIKE REPTILE BIENOTHERIUM

Temporal lines. More forwardfacing. tubular orbits than in the African forms 3. Orbits larger relative to skull size than in the other genera 2.

Brigham Young University Science Bulletin, Biological Series

( M amenchisaurus youngi Pi, Ouyang et Ye, 1996)

University of Iowa Iowa Research Online

FHSU Scholars Repository. Fort Hays State University. Joshua J. Fry Fort Hays State University, Summer 2015

SUPPLEMENTARY INFORMATION

New data on cranial anatomy of the ceratopsian dinosaur Psittacosaurus major

THE SKULL OF TELEOSAURUS CADOMENSIS (CROCODYLOMORPHA; THALATTOSUCHIA), AND PHYLOGENETIC ANALYSIS OF THALATTOSUCHIA

PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY NEW HAVEN, CONNECTICUT, U.S.A. GLYPTOLEPIS FROM THE MIDDLE DEVONIAN OF SCOTLAND

ABSTRACT. we define the taxa Alligatoroidae and Alligatoridae to be the descent community and crown group,

NEW INFORMATION ON THE CRANIUM OF BRACHYLOPHOSAURUS CANADENSIS (DINOSAURIA, HADROSAURIDAE), WITH A REVISION OF ITS PHYLOGENETIC POSITION

REVISION OF THE GENUS MARTINICHTHYS, MARINE FISH (TELESOSTEI, TSELFATIIFORMES) FROM THE LATE CRETACEOUS OF KANSAS (UNITED STATES)

PALEONTOLOGY AND BIOSTRATIGRAPHY OF MONGOLIA

Development of the Skull of the Hawksbill Seaturtle, Eretmochelys imbricata

SUPPLEMENTARY INFORMATION

A NEW SPECIES OF TROODONT DINOSAUR FROM THE

A New Dromaeosaurid Theropod from Ukhaa Tolgod (Ömnögov, Mongolia)

A Complete Late Cretaceous Iguanian (Squamata, Reptilia) from the Gobi and Identification of a New Iguanian Clade

AEROSAURUS WELLESI, NEW SPECIES, A VARANOPSEID MAMMAL-LIKE

ZOOLOGISCHE MEDEDELINGEN

A Late Jurassic Protosuchian Sichuanosuchus huidongensis from Zigong, Sichuan Province. Guangzhao Peng. Zigong Dinosaur Museum, Zigong, Sichuan

MIOCENE DIATOMACEOUS EARTH OF LOMPOC, CALI- FORNIA.i

Anatomy and Osteohistology of the basal hadrosaurid dinosaur Eotrachodon from the uppermost Santonian (Cretaceous) of southern appalachia

A Fossil Snake (Elaphe vulpina) From A Pliocene Ash Bed In Nebraska

DESCRIPTIONS OF NEW AND LITTLE-KNOWN FOSSIL LIZARDS FROM NORTH AMERICA

Description of Cranial Elements and Ontogenetic Change within Tropidolaemus wagleri (Serpentes: Crotalinae).

A NEW SPECIES OF THE SAUROPTERYGIAN GENUS NOTHOSAURUS FROM THE LOWER MUSCHELKALK OF WINTERSWIJK, THE NETHERLANDS

A Short Report on the Occurrence of Dilophosaurus from Jinning County, Yunnan Province

The Primitive Cynodont Procynosuchus: Functional Anatomy of the Skull and Relationships

THE SKULLS OF THE CATHARTID

CRANIAL OSTEOLOGY OF HYPSOGNATHUS FENNERI, A LATEST TRIASSIC PROCOLOPHONID REPTILE FROM THE NEWARK SUPERGROUP OF EASTERN NORTH AMERICA

AN INTERPRETATION OF THE SKULL OF BUETTNERIA, WITH SPECIAL REFERENCE TO THE CARTILAGES AND SOFT PARTS

Osteology and myology of Phrynosoma p. platyrhinos Girard and Phrynosoma d. hernandesi Girard

OSTEOLOGICAL NOTE OF AN ANTARCTIC SEI WHALE

A geometric morphometric analysis of Crocodylus Niloticus: evidence for a cryptic species complex

A New Dicynodont (Therapsida: Anomodontia) from the Permian of Southern Brazil and Its Implications for Bidentalian Origins

Cranial Osteology of the Andean Lizard Stenocercus guentheri (Squamata: Tropiduridae) and Its Postembryonic Development

AMERICAN MUSEUM NOVITATES

NOTES ON THE FIRST SKULL AND JAWS OF RIOJASAURUS INCERTUS (DINOSAURIA, PROSAUROPODA, MELANOROSAURIDAE) OF THE LATE TRIASSIC OF LA RIOJA, ARGENTINA

The cranial skeleton of the Early Permian aquatic reptile Mesosaurus tenuidens: implications for relationships and palaeobiology

ARTICLE. Midwestern University, N. 59th Ave., Glendale, Arizona 85308, U.S.A.

Transcription:

AMERICAN MUSEUM NOVITATES Published by Number 782 THE AmzRICAN MUSEUM OF NATURAL HISTORY Feb. 20, 1935 New York City 56.81, 7 G (68) A NOTE ON THE CYNODONT, GLOCHINODONTOIDES GRACILIS HAUGHTON BY LIEUWE D. BOONSTRA' The type in the Transvaal Museum was originally described by Haughton (Ann. Trans. Mus., XI, p. 85). Although it is not stated, Broom's figures (Mammal-like Reptiles of South Africa, p. 280) of the dorsal and ventral aspects of the skull were based, not on the type, but on a skull (A. M. 2223) now in the American Museum. This skull is nearly perfect-the lower jaw, the internasal bar and the quadrates being the only parts missing; furthermore, it has not suffered from post-mortem deformation as the type has. The following account incorporates and supplements the accounts by Haughton and Broom. In dorsal view (Fig. 1)2, the main features of interest can be enumerated as follows: the septomaxilla has practically no facial exposure, being a small bone lying nearly wholly within the nostril; the nasals are large and are constricted in their middle portion, but are wide anteriorly and posteriorly; the lacrymal is a fairly large bone with a flat outer surface showing no tubercle or foramen; the prefrontal is of medium size and forms a large part of the supraorbital border; the frontals are small and narrow and do not enter the orbital border; the postorbitals are large elements overlying the edges of the frontals and prefrontals; dorso-medially, they are raised above the frontal surface; their posterior extension along the lateral parietal face is not great; no postfrontal is visible in dorsal view; the parietals are small; the parietal crest is low and triangular in section and it forms the roof of the posterior part of the brain; a small pineal foramen pierces the parietal crest; the squamosal is a large element, extending very far anteriorly along the infratemporal bar, forming the mesial surface of a deep auditory groove and loosely supporting the posterior surface of the quadrates; the jugal forms nearly half of the postorbital bar and has a long posterior limb forming the ventral part of the infratemporal bar. 'Curator of the Palaeontological Collections, South African Museum, Cape Town. 2The drawings in this paper are by my wife, Esm6 E. Boonstra.

2 AMERICAN MUSEUM NOVITATES [No. 782 On the ventral surface (Fig. 2), some interesting features are revealed: the two halves of the secondary palate do not meet in the median line; between the two maxillary plates the ventral keel on the prevomer is visible; the secondary palate is formed by plates from the palatines, T a b. me_7 x. B.Oc. Fig. 1. Glochinodontoides gracilis. Dorsal view of the skull. Natural size. A. M. 2223. The right infratemporal and postorbital bars are drawn from the left side, where they are completely preserved. maxillaries and partly also from the premaxillaries; the anterior portion of the secondary palate is feebly developed, as here there are only beamlike processes of the premaxillaries between the prevomer and the anterior palatal vacuity; posterior to the palatal process of the right

1935] GLOCHINODONTOIDES GRACILIS 3 premaxilla, there lies a small piece of bone which may be part of the premaxilla, but a strip of matrix separates it from the premaxillary process proper; between the two premaxillary processes the widened anterior end of the prevomer is visible; the latter carries a median and a lateral a Pr.Mx. r F.Oc.7 B. p.b.0c. Fig. 2. Glochinodontoides gracilis. Ventral view of the skull. Natural size. A. M. 2223. The quadrates are not preserved. ridge as is typical in the therocephalians and gorgonopsians; the posterior end of the prevomer, which underlies the palatines, is broadly spatulate and carries a ventral keel, which dies out at the posterior end of the bone; the palatines are large and form part of the dorsal roof of the

4 AMERICAN MUSEUM NOVITA TES [No. 782 naso-pharangeal duct; antero-laterally, the palatine descends to form a ridge, whence it sends a sheet of bone mesially to form part of the floor of the naso-pharangeal passage; the lateral border of the palatine forms a slight ridge, lateral to which lies the ectopterygoid; the pterygoid has a fairly strong quadrate ramus, which does not, however, reach the quadrate; the lateral pterygoid ramus is weak and does not descend so far as in the more primitive therapsids; a ridge between the lateral and anterior pterygoid rami is continued forward on the palatine and served for the attachment of the soft palate; the basioccipital is practically excluded from the condyle, but, antero-ventrally, it has two fairly strong tubera to which the basisphenoid is applied; the basisphenoid has no tubera; anteriorly, it is clasped by the pterygoids; although here described as the Ven. Prot. Pa. fen.ov. P er. Fig. 3. Glochinodontoides gracilis. Lateral view of the posterior part of the right side of the brain-case. Nearly natural size. A. M. 2223. The occipital plate and the postero-lateral extremities of the epipterygoid are shown in section. basisphenoid, the bone visible in ventral view may really be a thin parasphenoid closely applied to an overlying basisphenoid; without a crosssection it is not possible to determine whether there are actually two bones; Parrington has described a parasphenoid in Thrinaxodon; when I was in Cambridge he very kindly showed me his specimens, and I was able to convince myself that in this genus at least, there is evidence of a thin shell of bone closely applied to the basisphenoid; it thus appears reasonable to assume the presence of a parasphenoid in all the cynodonts, but it would be valuable to have a series of cross-sections to confirm this assumption; the paroccipital is of medium size; laterally it abuts against the squamosal, where this bone forms the mesial surface of the auditory groove, and, mesially, it meets the basioccipital and exoccipital

19351 GLOCHINO.DONTOIDES GRA4CILIS 5 and contributes to the formation of the raised border of the foramen ovale; the double condyle is formed by the exoccipitals; the limits of the latter cannot be determined as they are very closely fused to the basioccipital. The outer surface of the brain-case has been exposed on the right side (Fig. 3). The occipital plate is shown in parasagittal section, and the outer surface of the brain-case as projected on the sagittal plane. The epipterygoid is widened, so that, dorsally, it has a long suture with the parietal and, ventrally, has a long base resting on the quadrate ramus of the pterygoid; the bone has a constricted waist, and its posterior edge is notched for the passage of branches of the fifth nerve; posterolaterally, the epipterygoid is prolonged beyond the termination of the quadrate ramus of the pterygoid; the anterior borders of the epipterygoids are situated widely apart (contrast "Lycaenodon"). The pro6tic lies at a greater distance from the median line than is the case in the more primitive gorgonopsians and therocephalians; it lies in the same plane as the epipterygoid, to which it is intimately applied; its dorsal edge meets the parietal and squamosal; its antero-ventral corner is notched for the passage of the two branches of the fifth nerve; a slit between the prootic and the parietal is a remnant of the large venous foramen usually found in therapsids. I have not been able to locate the foramen for the seventh cranial nerve. Postero-lateral to the prootic the small posttemporal fenestra pierces the occipital plate. SHORT DIscuSSION.-The wide spatulate posterior end of the prevomers appears to be a feature retained from the therocephalian ancestors. The widened epipterygoid, and the concomitant incorporation of the cavum epiptericum, are features whose development is foreshadowed in the primitive therocephalians and actually paralleled in some of the higher therocephalians. The narrow parietal crest and the loss of a distinct postfrontal are also therocephalian features. No therocephalian, however, has such a developed secondary palate; the approximation of the alveolar borders in the whaitsids is not homologous. In the bauriamorphs the development of the secondary palate has proceeded much further, but on a different path. In Bauria the false palate is formed by the premaxillaries and maxillaries, whereas in the cynodonts the premaxillary part is incomplete and the posterior part is formed by the palatine. If Bauria and the cynodonts are both derived from the therocephalians, then it is manifest that they diverged very early in their phylogenetic history.

6 AMERICAN MUSEUM NOVITATES [No. 782 Chief Measurements of the Skull Premaxilla to basioccipital... 106 mm. Premaxilla to pineal foramen... 76 mm. Premaxilla to front of orbit.... ;. 44 mm. Interorbital width... 23 mm. Intertemporal width... 11 mm. Width across the squamosals... 90 mm. Length of molar series (8 teeth)...... 22 mm.