University of Birmingham the Last Erythrosuchid—A Revision Of
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8. Archosaur Phylogeny and the Relationships of the Crocodylia
8. Archosaur phylogeny and the relationships of the Crocodylia MICHAEL J. BENTON Department of Geology, The Queen's University of Belfast, Belfast, UK JAMES M. CLARK* Department of Anatomy, University of Chicago, Chicago, Illinois, USA Abstract The Archosauria include the living crocodilians and birds, as well as the fossil dinosaurs, pterosaurs, and basal 'thecodontians'. Cladograms of the basal archosaurs and of the crocodylomorphs are given in this paper. There are three primitive archosaur groups, the Proterosuchidae, the Erythrosuchidae, and the Proterochampsidae, which fall outside the crown-group (crocodilian line plus bird line), and these have been defined as plesions to a restricted Archosauria by Gauthier. The Early Triassic Euparkeria may also fall outside this crown-group, or it may lie on the bird line. The crown-group of archosaurs divides into the Ornithosuchia (the 'bird line': Orn- ithosuchidae, Lagosuchidae, Pterosauria, Dinosauria) and the Croco- dylotarsi nov. (the 'crocodilian line': Phytosauridae, Crocodylo- morpha, Stagonolepididae, Rauisuchidae, and Poposauridae). The latter three families may form a clade (Pseudosuchia s.str.), or the Poposauridae may pair off with Crocodylomorpha. The Crocodylomorpha includes all crocodilians, as well as crocodi- lian-like Triassic and Jurassic terrestrial forms. The Crocodyliformes include the traditional 'Protosuchia', 'Mesosuchia', and Eusuchia, and they are defined by a large number of synapomorphies, particularly of the braincase and occipital regions. The 'protosuchians' (mainly Early *Present address: Department of Zoology, Storer Hall, University of California, Davis, Cali- fornia, USA. The Phylogeny and Classification of the Tetrapods, Volume 1: Amphibians, Reptiles, Birds (ed. M.J. Benton), Systematics Association Special Volume 35A . pp. 295-338. Clarendon Press, Oxford, 1988. -
Heptasuchus Clarki, from the ?Mid-Upper Triassic, Southeastern Big Horn Mountains, Central Wyoming (USA)
The osteology and phylogenetic position of the loricatan (Archosauria: Pseudosuchia) Heptasuchus clarki, from the ?Mid-Upper Triassic, southeastern Big Horn Mountains, Central Wyoming (USA) † Sterling J. Nesbitt1, John M. Zawiskie2,3, Robert M. Dawley4 1 Department of Geosciences, Virginia Tech, Blacksburg, VA, USA 2 Cranbrook Institute of Science, Bloomfield Hills, MI, USA 3 Department of Geology, Wayne State University, Detroit, MI, USA 4 Department of Biology, Ursinus College, Collegeville, PA, USA † Deceased author. ABSTRACT Loricatan pseudosuchians (known as “rauisuchians”) typically consist of poorly understood fragmentary remains known worldwide from the Middle Triassic to the end of the Triassic Period. Renewed interest and the discovery of more complete specimens recently revolutionized our understanding of the relationships of archosaurs, the origin of Crocodylomorpha, and the paleobiology of these animals. However, there are still few loricatans known from the Middle to early portion of the Late Triassic and the forms that occur during this time are largely known from southern Pangea or Europe. Heptasuchus clarki was the first formally recognized North American “rauisuchian” and was collected from a poorly sampled and disparately fossiliferous sequence of Triassic strata in North America. Exposed along the trend of the Casper Arch flanking the southeastern Big Horn Mountains, the type locality of Heptasuchus clarki occurs within a sequence of red beds above the Alcova Limestone and Crow Mountain formations within the Chugwater Group. The age of the type locality is poorly constrained to the Middle—early Late Triassic and is Submitted 17 June 2020 Accepted 14 September 2020 likely similar to or just older than that of the Popo Agie Formation assemblage from Published 27 October 2020 the western portion of Wyoming. -
Dragon Magazine #176
SPECIAL ATTRACTIONS Issue # 176 Vol. XVI, No. 7 9 The elves: a worId of difference December 1991 Two in-depth features on the elves and their beliefs. Servants of the Seldarine Chris Perry Publisher 10 Try elven clerics with real power! Specialty priests of the faerie folk. James M. Ward If You need Help Ask the Drow! Ed Greenwood and Steven E. 16 Schend Editor Roger E. Moore Good-aligned drow? Visit Undermountains temple of Eilistraee. Fiction editor Barbara G. Young O THER FEATURES Bruce A. Heard Associate editor The Voyage of the Princess Ark Dale A. Donovan 31 You got till noon to clear out of Smokestone City, said the sheriff to the admiral. Editorial assistant Propping Up Your Campaign Spike Y. Jones Wolfgang H. Baur 45 Some game-mastering tools you might never have thought ofthe Nerf ball, for instance. Art director Larry W. Smith The Role of Computers Hartley, Patricia, and Kirk Lesser 57 Lucky Jake Masters isnt very lucky these daysbut you will be with Production staff Heart of China. Gaye OKeefe Angelika Lokotz Time For an Experiment fiction by Michael G. Ryan Tracey Zamagne 64 He would rise from the depths to achieve everlasting fame. It was only a matter of time. Subscriptions Janet L. Winters Role-playing Reviews Doug Niles 74 The study of strategy: three board games with unusual tactics. U.S. advertising Roseann Schnering The MARVEL®-Phile Scott Davis and Steven E. Schend 77 Heroic castaways of the MARVEL UNIVERSE. U.K. correspondent Playing in the Paleozoic Gregory W. Detwiler and U.K. -
Extant Taxa Stem Frogs Stem Turtles Stem Lepidosaurs Stem Squamates
Stem Taxa - Peters 2016 851 taxa, 228 characters 100 Eldeceeon 1990.7.1 91 Eldeceeon holotype 100 Romeriscus Ichthyostega Gephyrostegus watsoni Pederpes 85 Eryops 67 Solenodonsaurus 87 Proterogyrinus 100 Chroniosaurus Eoherpeton 94 72 Chroniosaurus PIN3585/124 98 Seymouria Chroniosuchus Kotlassia Stem 58 94 Westlothiana Utegenia Casineria 84 81 Amphibamus Brouffia 95 72 Cacops 93 77 Coelostegus Paleothyris 98 Doleserpeton 84 91 78 100 Gerobatrachus Hylonomus Rana Archosauromorphs Protorothyris MCZ1532 95 66 98 Adelospondylus 85 Protorothyris CM 8617 89 Brachydectes Protorothyris MCZ 2149 Eocaecilia 87 86 Microbrachis Vaughnictis Pantylus 80 89 75 94 Anthracodromeus Elliotsmithia 90 Utaherpeton 51 Apsisaurus Kirktonecta 95 90 86 Aerosaurus 96 Tuditanus 67 90 Varanops Stem Frogs 59 94 Eoserpeton Varanodon Diplocaulus Varanosaurus FMNH PR 1760 100 Sauropleura 62 84 Varanosaurus BSPHM 1901 XV20 88 Ptyonius 89 Archaeothyris 70 Scincosaurus Euryodus primus Ophiacodon 74 82 84 Micraroter Haptodus 91 Rhynchonkos 97 82 Secodontosaurus Batropetes 85 76 100 Dimetrodon 97 Sphenacodon Silvanerpeton Ianthodon 85 Edaphosaurus Gephyrostegeus bohemicus 99 Stem100 Reptiles 80 82 Ianthasaurus Glaucosaurus 94 Cutleria 100 Urumqia Bruktererpeton Stenocybus Stem Mammals 63 97 Thuringothyris MNG 7729 62 IVPP V18117 82 Thuringothyris MNG 10183 87 62 71 Kenyasaurus 82 Galechirus 52 Suminia Saurorictus Venjukovia 99 99 97 83 70 Cephalerpeton Opisthodontosaurus 94 Eodicynodon 80 98 Reiszorhinus 100 Dicynodon 75 Concordia KUVP 8702a Hipposaurus 100 98 96 Concordia -
Early Triassic
www.nature.com/scientificreports OPEN A new specimen of Prolacerta broomi from the lower Fremouw Formation (Early Triassic) of Received: 12 June 2018 Accepted: 21 November 2018 Antarctica, its biogeographical Published: xx xx xxxx implications and a taxonomic revision Stephan N. F. Spiekman Prolacerta broomi is an Early Triassic archosauromorph of particular importance to the early evolution of archosaurs. It is well known from many specimens from South Africa and a few relatively small specimens from Antarctica. Here, a new articulated specimen from the Fremouw Formation of Antarctica is described in detail. It represents the largest specimen of Prolacerta described to date with a nearly fully articulated and complete postcranium in addition to four skull elements. The study of this specimen and the re-evaluation of other Prolacerta specimens from both Antarctica and South Africa reveal several important new insights into its morphology, most notably regarding the premaxilla, manus, and pelvic girdle. Although well-preserved skull material from Antarctica is still lacking for Prolacerta, a detailed comparison of Prolacerta specimens from Antarctica and South Africa corroborates previous fndings that there are no characters clearly distinguishing the specimens from these diferent regions and therefore the Antarctic material is assigned to Prolacerta broomi. The biogeographical implications of these new fndings are discussed. Finally, some osteological characters for Prolacerta are revised and an updated diagnosis and phylogenetic analysis are provided. Prolacerta broomi is a medium sized non-archosauriform archosauromorph with a generalized, “lizard-like” body type. Many specimens, mostly consisting of cranial remains, have been described and Prolacerta is considered one of the best represented early archosauromorphs1–3. -
Diversificação De Archosauromorpha Após a Extinção Permo-Triássica Survivors: Diversification of Archosauromorpha After Permo-Triassic Extinction
Terræ REVISÃO 10.20396/td.v16i0.8656060 Didatica Sobreviventes: Diversificação de Archosauromorpha após a Extinção Permo-Triássica SURVIVORS: DIVERSIFICATION OF ARCHOSAUROMORPHA AFTER PERMO-TRIASSIC EXTINCTION TIANE MACEDO DE-OLIVEIRA¹, FELIPE LIMA PINHEIRO², LEONARDO KERBER³ 1 - PROGR. PÓS-GRAD. BIODIVERSIDADE ANIMAL, UNIVERSIDADE FEDERAL DE SANTA MARIA (UFSM). SANTA MARIA, RS, BRASIL. 2 - LABORATÓRIO DE PALEOBIOLOGIA, UNIPAMPA, SÃO GABRIEL, RS, BRASIL. 3 - CENTRO DE APOIO À PESQUISA PALEONTOLÓGICA DA QUARTA COLÔNIA (CAPPA-UFSM), SÃO JOÃO DO POLÊSINE, RS, BRASIL. E-MAIL: [email protected], [email protected], [email protected] Abstract: The Archosauromorpha is defined as the clade that comprises all diapsids more closely related Citation/Citação: De-Oliveira, T. M., to the lineage of birds (Ornithodira or Avemetatarsalia) and crocodylians (Pseudosuchia or Crurotarsi) than Pinheiro, F. L., & Kerber, L. (2020). to Lepidosauria. In addition to their ‘basal’ taxa (e.g., Tanystropheidae, Rhynchosauria, and Allokotosau- Sobreviventes: Diversificação de Ar- ria), Archosauromorpha includes the clade Archosauriformes, which, by its turn, includes Archosauria. chosauromorpha após a Extinção During the Triassic, the archosauromorphs became the main group of diapsids to diversify in body size Permo-Triássica. Terræ Didatica, and morphological disparity. The Permo-Triassic mass extinction occurred 252 million years ago and 16, 1-23, e020009. doi: 10.20396/ produced a dramatic change in the composition of the floral and faunal communities at the beginning td.v16i0.8656060 of the Triassic period. The diversification of Archosauromorpha during the Triassic has been the focus of several recent studies, as this clade is a classic example of adaptive radiation. This paper synthesizes Keywords: Diapsida. -
The Tarsus of Erythrosuid Archosaurs, and Implications for Early Diapsid
Zoological Journal of the Linnean Society (1996), 116: 347–375. With 11 figures The tarsus of erythrosuchid archosaurs, and implications for early diapsid phylogeny DAVID J. GOWER Department of Geology, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, UK and Institut und Museum f¨ur Geologie und Pal¨aontologie, Universit¨at T¨ubingen, Sigwartstrasse 10, D-72076 T¨ubingen, Germany Received September 1994, accepted for publication February 1995 The morphology of the erythrosuchid ankle joint is reassessed. Two specimens, recently thought to have been incorrectly referred to Erythrosuchus africanus, are shown without doubt to belong to this taxon. Furthermore, the morphology is essentially similar to that of other early archosaurs. The tarsus of Erythrosuchus is poorly ossified and consists of a calcaneum, astragalus, and two distal tarsals. The calcanea of Erythrosuchus, Vjushkovia triplicostata, and Shansisuchus shansisuchus are all similar in being dorsoventrally compressed, possessing a lateral tuber, and lacking a perforating foramen. The astragalus of V. triplicostata is currently unknown. The astragalus of Shansisuchus is apparently unique in form. The erythrosuchid pes is therefore more derived than has been recently proposed. The tarsal morphology of several other archosauromorph taxa is reviewed and many details are found to be at variance with the literature. The plesiomorphic condition for the Archosauromorpha consists of four distal tarsals and a proximal row of three elements; two of which articulate with the tibia. These proximal elements are interpreted as the astragalus, calcaneum, and a centrale, and the same pattern is retained in the earliest archosaurs. This reassessed tarsal morphology has implications for the homology of the centrale and reconstruction of early diapsid phylogeny. -
The Last Erythrosuchid—A Revision of Chalishevia Cothurnata from the Late Middle Triassic of European Russia
The last erythrosuchid—a revision of Chalishevia cothurnata from the late Middle Triassic of European Russia RICHARD J. BUTLER, ANDREY G. SENNIKOV, MARTÍN D. EZCURRA, and DAVID J. GOWER Butler, R.J., Sennikov, A.G., Ezcurra, M.D., and Gower, D.J. 2019. The last erythrosuchid—a revision of Chalishevia cothurnata from the late Middle Triassic of European Russia. Acta Palaeontologica Polonica 64 (4): 757–774. Erythrosuchidae is a clade of early archosauriform reptiles that were large-bodied, hypercarnivorous, possibly apex pred- ators in late Early and Middle Triassic ecosystems following the Permo-Triassic mass extinction. Chalishevia cothurnata from the late Middle Triassic (Ladinian) of Russia, is the stratigraphically youngest known erythrosuchid species, but the holotype and referred material of this taxon has received little study. Here, we provide the first detailed anatomical description of C. cothurnata, including comparisons to other erythrosuchids. Although known from relatively fragmen- tary material, the anatomy of C. cothurnata is distinctive, including an autapomorphic strongly slanted ventral border of the antorbital fossa. The presence of a large accessory opening (the “accessory antorbital fenestra”) in the skull between the premaxilla, nasal and maxilla, together with the inferred presence of a narrow postnarial process of the premaxilla that articulated with a slot on the nasal, provides strong evidence for a sister taxon relationship between C. cothurnata and the erythrosuchid Shansisuchus shansisuchus from the early Middle Triassic (Anisian) of China. The inferred basal skull length of C. cothurnata was approximately 80 cm, making it one of the largest erythrosuchids known. Key words: Archosauriformes, Erythrosuchidae, anatomy, Triassic, Ladinian, Russia, Bukobay Gorizont. -
Article Skeletal Anatomy of Acaenasuchus Geoffreyi
Journal of Vertebrate Paleontology e1794885 (26 pages) This work was authored as part of Adam D. Marsh, Matthew E. Smith and William G. Parker’sofficial duties as Employees of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law. Randall B. Irmis and Ben T. Kligman hereby waive their right to assert copyright, but not their right to be named as co-authors in the article. DOI: 10.1080/02724634.2020.1794885 ARTICLE SKELETAL ANATOMY OF ACAENASUCHUS GEOFFREYI LONG AND MURRY, 1995 (ARCHOSAURIA: PSEUDOSUCHIA) AND ITS IMPLICATIONS FOR THE ORIGIN OF THE AETOSAURIAN CARAPACE ADAM D. MARSH, *,1 MATTHEW E. SMITH,1 WILLIAM G. PARKER, 1 RANDALL B. IRMIS,2 and BEN T. KLIGMAN 3 1Petrified Forest National Park, Division of Science and Resource Management, Arizona 86028, U.S.A., [email protected]; [email protected]; [email protected]; 2Natural History Museum of Utah and Department of Geology & Geophysics, University of Utah, Salt Lake City, Utah 84108-1214, U.S.A., [email protected]; 3Virginia Tech, Department of Geosciences, Blacksburg, Virginia 24061, U.S.A., [email protected] ABSTRACT—Acaenasuchus geoffreyi is a diminutive armored archosaur from the Upper Triassic Chinle Formation of northern Arizona, U.S.A., with uncertain evolutionary relationships and skeletal maturity. Known only from osteoderms, the taxon has been considered a valid taxon of aetosaur, juvenile specimens synonymous with the aetosaur Desmatosuchus spurensis, or a non-aetosaurian pseudosuchian archosaur. Here, we describe new fossils of Acaenasuchus geoffreyi that represent cranial, vertebral, and appendicular elements as well as previously unknown variations in the dorsal carapace and ventral shield. -
Two New Archosaur Reptiles from the Late Triassic Of
TWO NEW ARCHOSAUR REPTILES FROM THE LATE TRIASSIC OF TEXAS by MOMCHIL NIKOLAEV ATANASSOV, M.S. A DISSERTATION IN GEOSCIENCE Submitted to the Graduate Faculty of Texas Tech University in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY Approved Chairperson of the Qbmmittee Accepted Dean of the Graduate School August, 2002 Copyright 2002, Momchil Nikolaev Atanassov ACKNOWLEDGMENTS I would like to thank the members of my committee. Dr. James Barrick, Dr. Thomas Lehman, Dr. Richard Strauss, and the committee chairman. Dr. Sankar Chatterjee for their guidance, help, and support during the completion of this dissertation. In particular, I would like to express my gratitude to my dissertation advisor Sankar Chatterjee, who invited me to come to Texas Tech University, offered his generous hospitality, and provided valuable advice and guidance throughout this project. I also wish to thank my fellow students and colleagues Alan Coulson, Axel Hungerbiihler, Richard Kissel, Jeffrey Martz, Kyle McQuilkin, Bill Mueller, Eric Simpson, Jonathan Wagner, and Jonathan Weinbaum for many useful discussions and their help in the field and in the lab. A special thanks goes to Mariana Ivanova for her help in the field and especially for her skillful preparation of a significant amotmt of material from the Dockum Group, a tedious and time-consuming task. Bill Mueller from the Museum of Texas Tech University took most photographs with great skill and patience. I theink the Museum of Texas Tech University for allowing unlimited access to the fossil collections and the museum facilities, and the Department of Geosciences at Texas Tech University for the material support throughout my studies. -
Bone Histology of Azendohsaurus Laaroussii: Implications for the Evolution of Thermometabolism in Archosauromorpha Jorge Cubo, Nour-Eddine Jalil
Bone histology of Azendohsaurus laaroussii: Implications for the evolution of thermometabolism in Archosauromorpha Jorge Cubo, Nour-Eddine Jalil To cite this version: Jorge Cubo, Nour-Eddine Jalil. Bone histology of Azendohsaurus laaroussii: Implications for the evolution of thermometabolism in Archosauromorpha. Paleobiology, Paleontological Society, 2019, 45 (2), pp.317-330. 10.1017/pab.2019.13. hal-02969492 HAL Id: hal-02969492 https://hal.sorbonne-universite.fr/hal-02969492 Submitted on 16 Oct 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Bone histology of Azendohsaurus laaroussii. Implications for the evolution of 2 thermometabolism in Archosauromorpha 3 4 Jorge Cubo 1 * and Nour-Eddine Jalil 2, 3 5 6 1 Sorbonne Université, MNHN, CNRS, Centre de Recherche en Paléontologie – Paris (CR2P) 7 - 4 place Jussieu, BC 104, 75005 Paris, France. 8 E-mail: [email protected] 9 *Corresponding author 10 11 2Muséum national d’Histoire naturelle, Sorbonne Université, CNRS, Centre de Recherche en 12 Paléontologie – Paris (CR2P) - 75005 Paris, France. 13 E-mail: [email protected] 14 15 3Laboratory of Biodiversity and Dynamic of Ecosystems, Department of Geology, Fac. Sci. 16 Semlalia, UCA, Marrakesh, Morocco 17 18 1 19 Abstract.- This paper is aimed at constraining the phylogenetic frame of the acquisition of 20 endothermy by Archosauromorpha. -
Bibliography of the Amphibian and Reptile Research in Slovakia Between 1791 and 2017
Pavol Jozef Šafárik University in Košice Faculty of Science Bibliography of the amphibian and reptile research in Slovakia between 1791 and 2017 Marcel Uhrin, David Jandzik, Andrej Čerňanský, Michal Rindoš, Blanka Lehotská, Stanislav Danko, Ján Kautman, Peter Mikulíček, Peter Urban & Daniel Jablonski Pavol Jozef Šafárik University in Košice Faculty of Science Bibliography of the amphibian and reptile research in Slovakia between 1791 and 2017 Marcel Uhrin, David Jandzik, Andrej Čerňanský, Michal Rindoš, Blanka Lehotská, Stanislav Danko, Ján Kautman, Peter Mikulíček, Peter Urban & Daniel Jablonski Košice 2019 Bibliography of the amphibian and reptile research in Slovakia between 1791 and 2017 Electronic publication © 2019 Pavol Jozef Šafárik University in Košice, Faculty of Science © 2019 Authors © 2019 Uwe Fritz & Jiří Moravec Authors: Marcel Uhrin, David Jandzik, Andrej Čerňanský, Michal Rindoš, Blanka Lehotská, Stanislav Danko, Ján Kautman, Peter Mikulíček, Peter Urban & Daniel Jablonski Rewievers: Uwe Fritz, Senckenberg Natural History Collection of Dresden, Department Museum of Zoology, Dresden, Germany Jiří Moravec, National Museum, Natural History Museum, Praha, Czech Republic Cover photo: David Jandzik Typesetting and layout: Benjamín Jarčuška, Zvolen, Slovakia Available at: www.unibook.upjs.sk Publication date: 28.06.2019 ISBN 978-80-8152-737-1 (e-publication) Acknowledgments We would like to thank Peter Krišovský and Stanislav Levendovský (East Slovak Museum in Košice, Slovakia), Judita Samuelisová (P. J. Šafárik University in Košice, Slovakia), Petr Papežík (Comenius University in Bratislava, Slovakia), Zdeněk Mačát (NP Podyjí, Czech Republic), Edvárd Mizsei, Márton Szabolcs (both University of Debrecen, Hungary), Judit Vörös (Hungarian Natural History Museum, Budapest, Hungary) and Mario Schweiger (Obertrum, Austria) for their assistance in obtaining several references from the bibliography.