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Reptile Family Tree
Reptile Family Tree - Peters 2015 Distribution of Scales, Scutes, Hair and Feathers Fish scales 100 Ichthyostega Eldeceeon 1990.7.1 Pederpes 91 Eldeceeon holotype Gephyrostegus watsoni Eryops 67 Solenodonsaurus 87 Proterogyrinus 85 100 Chroniosaurus Eoherpeton 94 72 Chroniosaurus PIN3585/124 98 Seymouria Chroniosuchus Kotlassia 58 94 Westlothiana Casineria Utegenia 84 Brouffia 95 78 Amphibamus 71 93 77 Coelostegus Cacops Paleothyris Adelospondylus 91 78 82 99 Hylonomus 100 Brachydectes Protorothyris MCZ1532 Eocaecilia 95 91 Protorothyris CM 8617 77 95 Doleserpeton 98 Gerobatrachus Protorothyris MCZ 2149 Rana 86 52 Microbrachis 92 Elliotsmithia Pantylus 93 Apsisaurus 83 92 Anthracodromeus 84 85 Aerosaurus 95 85 Utaherpeton 82 Varanodon 95 Tuditanus 91 98 61 90 Eoserpeton Varanops Diplocaulus Varanosaurus FMNH PR 1760 88 100 Sauropleura Varanosaurus BSPHM 1901 XV20 78 Ptyonius 98 89 Archaeothyris Scincosaurus 77 84 Ophiacodon 95 Micraroter 79 98 Batropetes Rhynchonkos Cutleria 59 Nikkasaurus 95 54 Biarmosuchus Silvanerpeton 72 Titanophoneus Gephyrostegeus bohemicus 96 Procynosuchus 68 100 Megazostrodon Mammal 88 Homo sapiens 100 66 Stenocybus hair 91 94 IVPP V18117 69 Galechirus 69 97 62 Suminia Niaftasuchus 65 Microurania 98 Urumqia 91 Bruktererpeton 65 IVPP V 18120 85 Venjukovia 98 100 Thuringothyris MNG 7729 Thuringothyris MNG 10183 100 Eodicynodon Dicynodon 91 Cephalerpeton 54 Reiszorhinus Haptodus 62 Concordia KUVP 8702a 95 59 Ianthasaurus 87 87 Concordia KUVP 96/95 85 Edaphosaurus Romeria primus 87 Glaucosaurus Romeria texana Secodontosaurus -
HOVASAURUS BOULEI, an AQUATIC EOSUCHIAN from the UPPER PERMIAN of MADAGASCAR by P.J
99 Palaeont. afr., 24 (1981) HOVASAURUS BOULEI, AN AQUATIC EOSUCHIAN FROM THE UPPER PERMIAN OF MADAGASCAR by P.J. Currie Provincial Museum ofAlberta, Edmonton, Alberta, T5N OM6, Canada ABSTRACT HovasauTUs is the most specialized of four known genera of tangasaurid eosuchians, and is the most common vertebrate recovered from the Lower Sakamena Formation (Upper Per mian, Dzulfia n Standard Stage) of Madagascar. The tail is more than double the snout-vent length, and would have been used as a powerful swimming appendage. Ribs are pachyostotic in large animals. The pectoral girdle is low, but massively developed ventrally. The front limb would have been used for swimming and for direction control when swimming. Copious amounts of pebbles were swallowed for ballast. The hind limbs would have been efficient for terrestrial locomotion at maturity. The presence of long growth series for Ho vasaurus and the more terrestrial tan~saurid ThadeosauTUs presents a unique opportunity to study differences in growth strategies in two closely related Permian genera. At birth, the limbs were relatively much shorter in Ho vasaurus, but because of differences in growth rates, the limbs of Thadeosau rus are relatively shorter at maturity. It is suggested that immature specimens of Ho vasauTUs spent most of their time in the water, whereas adults spent more time on land for mating, lay ing eggs and/or range dispersal. Specilizations in the vertebrae and carpus indicate close re lationship between Youngina and the tangasaurids, but eliminate tangasaurids from consider ation as ancestors of other aquatic eosuchians, archosaurs or sauropterygians. CONTENTS Page ABREVIATIONS . ..... ... ......... .......... ... ......... ..... ... ..... .. .... 101 INTRODUCTION . -
A Small Lepidosauromorph Reptile from the Early Triassic of Poland
A SMALL LEPIDOSAUROMORPH REPTILE FROM THE EARLY TRIASSIC OF POLAND SUSAN E. EVANS and MAGDALENA BORSUK−BIAŁYNICKA Evans, S.E. and Borsuk−Białynicka, M. 2009. A small lepidosauromorph reptile from the Early Triassic of Poland. Palaeontologia Polonica 65, 179–202. The Early Triassic karst deposits of Czatkowice quarry near Kraków, southern Poland, has yielded a diversity of fish, amphibians and small reptiles. Two of these reptiles are lepido− sauromorphs, a group otherwise very poorly represented in the Triassic record. The smaller of them, Sophineta cracoviensis gen. et sp. n., is described here. In Sophineta the unspecial− ised vertebral column is associated with the fairly derived skull structure, including the tall facial process of the maxilla, reduced lacrimal, and pleurodonty, that all resemble those of early crown−group lepidosaurs rather then stem−taxa. Cladistic analysis places this new ge− nus as the sister group of Lepidosauria, displacing the relictual Middle Jurassic genus Marmoretta and bringing the origins of Lepidosauria closer to a realistic time frame. Key words: Reptilia, Lepidosauria, Triassic, phylogeny, Czatkowice, Poland. Susan E. Evans [[email protected]], Department of Cell and Developmental Biology, Uni− versity College London, Gower Street, London, WC1E 6BT, UK. Magdalena Borsuk−Białynicka [[email protected]], Institut Paleobiologii PAN, Twarda 51/55, PL−00−818 Warszawa, Poland. Received 8 March 2006, accepted 9 January 2007 180 SUSAN E. EVANS and MAGDALENA BORSUK−BIAŁYNICKA INTRODUCTION Amongst living reptiles, lepidosaurs (snakes, lizards, amphisbaenians, and tuatara) form the largest and most successful group with more than 7 000 widely distributed species. The two main lepidosaurian clades are Rhynchocephalia (the living Sphenodon and its extinct relatives) and Squamata (lizards, snakes and amphisbaenians). -
Elachistosuchus Huenei Janensch, 1949 (Reptilia: Diapsida) from the Upper Triassic of Germany and Its Relevance for the Origin of Sauria
RESEARCH ARTICLE Anatomy of the Enigmatic Reptile Elachistosuchus huenei Janensch, 1949 (Reptilia: Diapsida) from the Upper Triassic of Germany and Its Relevance for the Origin of Sauria Gabriela Sobral1☯*, Hans-Dieter Sues2☯, Johannes Müller1☯ 1 Museum für Naturkunde Berlin, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Berlin, Germany, 2 Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, Washington, DC, United States of America ☯ These authors contributed equally to this work. * [email protected] OPEN ACCESS Citation: Sobral G, Sues H-D, Müller J (2015) Abstract Anatomy of the Enigmatic Reptile Elachistosuchus huenei Janensch, 1949 (Reptilia: Diapsida) from the The holotype and only known specimen of the enigmatic small reptile Elachistosuchus hue- Upper Triassic of Germany and Its Relevance for the nei Janensch, 1949 from the Upper Triassic (Norian) Arnstadt Formation of Saxony-Anhalt Origin of Sauria. PLoS ONE 10(9): e0135114. μ doi:10.1371/journal.pone.0135114 (Germany) is redescribed using CT scans of the material. This re-examination revealed new information on the morphology of this taxon, including previously unknown parts of the Editor: Shree Ram Singh, National Cancer Institute, UNITED STATES skeleton such as the palate, braincase, and shoulder girdle. Elachistosuchus is diagnosed especially by the presence of the posterolateral process of the frontal, the extension of the Received: January 27, 2015 maxillary tooth row to the posterior margin of the orbit, the free posterior process of the Accepted: July 19, 2015 jugal, and the notched anterior margin of the interclavicle. Phylogenetic analyses using two Published: September 9, 2015 recently published character-taxon matrices recovered conflicting results for the phyloge- Copyright: This is an open access article, free of all netic position of Elachistosuchus–either as an archosauromorph, as a lepidosauromorph or copyright, and may be freely reproduced, distributed, as a more basal, non-saurian diapsid. -
Tetrapod Phylogeny
© J989 Elsevier Science Publishers B. V. (Biomédical Division) The Hierarchy of Life B. Fernholm, K. Bremer and H. Jörnvall, editors 337 CHAPTER 25 Tetrapod phylogeny JACQUES GAUTHIER', DAVID CANNATELLA^, KEVIN DE QUEIROZ^, ARNOLD G. KLUGE* and TIMOTHY ROWE^ ' Deparlmenl qf Herpelology, California Academy of Sciences, San Francisco, CA 94118, U.S.A., ^Museum of Natural Sciences and Department of Biology, Louisiana State University, Baton Rouge, LA 70803, U.S.A., ^Department of ^oology and Museum of Vertebrate ^oology. University of California, Berkeley, CA 94720, U.S.A., 'Museum of ^oology and Department of Biology, University of Michigan, Ann Arbor, MI 48109, U.S.A. and ^Department of Geological Sciences, University of Texas, Austin, TX 78713, U.S.A. Introduction Early sarcopterygians were aquatic, but from the latter part of the Carboniferous on- ward that group has been dominated by terrestrial forms commonly known as the tet- rapods. Fig. 1 illustrates relationships among extant Tetrápoda [1-4J. As the clado- grams in Figs. 2•20 demonstrate, however, extant groups represent only a small part of the taxonomic and morphologic diversity of Tetrápoda. We hope to convey some appreciation for the broad outlines of tetrapod evolution during its 300+ million year history from late Mississippian to Recent times. In doing so, we summarize trees de- rived from the distribution of over 972 characters among 83 terminal taxa of Tetrápo- da. More than 90% of the terminal taxa we discuss are extinct, but all of the subter- minal taxa are represented in the extant biota. This enables us to emphasize the origins of living tetrapod groups while giving due consideration to the diversity and antiquity of the clades of which they are a part. -
Download a PDF of This Web Page Here. Visit
Dinosaur Genera List Page 1 of 42 You are visitor number— Zales Jewelry —as of November 7, 2008 The Dinosaur Genera List became a standalone website on December 4, 2000 on America Online’s Hometown domain. AOL closed the domain down on Halloween, 2008, so the List was carried over to the www.polychora.com domain in early November, 2008. The final visitor count before AOL Hometown was closed down was 93661, on October 30, 2008. List last updated 12/15/17 Additions and corrections entered since the last update are in green. Genera counts (but not totals) changed since the last update appear in green cells. Download a PDF of this web page here. Visit my Go Fund Me web page here. Go ahead, contribute a few bucks to the cause! Visit my eBay Store here. Search for “paleontology.” Unfortunately, as of May 2011, Adobe changed its PDF-creation website and no longer supports making PDFs directly from HTML files. I finally figured out a way around this problem, but the PDF no longer preserves background colors, such as the green backgrounds in the genera counts. Win some, lose some. Return to Dinogeorge’s Home Page. Generic Name Counts Scientifically Valid Names Scientifically Invalid Names Non- Letter Well Junior Rejected/ dinosaurian Doubtful Preoccupied Vernacular Totals (click) established synonyms forgotten (valid or invalid) file://C:\Documents and Settings\George\Desktop\Paleo Papers\dinolist.html 12/15/2017 Dinosaur Genera List Page 2 of 42 A 117 20 8 2 1 8 15 171 B 56 5 1 0 0 11 5 78 C 70 15 5 6 0 10 9 115 D 55 12 7 2 0 5 6 87 E 48 4 3 -
Sedimentology and Taphonomy of Late Permian Vertebrate Fossil Localities in Southwestern Madagascar
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Wits Institutional Repository on DSPACE Palaeont. afr., 36, 25-41 (2000) SEDIMENTOLOGY AND TAPHONOMY OF LATE PERMIAN VERTEBRATE FOSSIL LOCALITIES IN SOUTHWESTERN MADAGASCAR. by Roger M.H. Smith Divison of Earth Sciences, South African Museum, PO Box 61, Cape Town 8000 ABSTRACT This is the first report of a project that tests the accuracy of the currently accepted palaeoposition of southern Madagascar during the late Permian in juxtaposition to the coast of Tanzania. This is done by comparing the sediments and fossils that accumulated in a series of rift valleys, each around 25 km wide, that formed in this part of Gondwana at the beginning of pull-apart some 250 million years ago. The study reported here on the Madagascan side of the rift system will be followed by a similar study of the Tanzanian portion. Field data on the sedimentology and vertebrate taphonomy of three separate fossil localities in the Late Permian, Lower Sakamena Formation of southwestern Madagascar are used to reconstruct the subenvironments of the Sakamena axial rift valley lake. 1. Ranohira: dominated by microlaminated mudrocks with three horizons of fossil bearing micrite nodules. The fossils are mostly complete articulated skeletons of an ?aquatic procolophonid reptile, Barasaurus, which inhabited the offshore epilimnion of a deep, thermally-stratified closed lake. 2. Zavoloa River: alternating cross-bedded conglomeratic sandstone and laminated siltstone are interpreted as braided delta deposits entering the linear margin of the lake from the passive side of the half graben. -
1 Youngoides Romeri and the Origin of the Archosauriformes DAVID
Youngoides romeri and the origin of the Archosauriformes DAVID PETERS Independent researcher 311 Collinsville Avenue, Collinsville, IL U.S.A. [email protected] 1 ABSTRACT—Prior workers reported that all specimens attributed to Youngopsis and Youngoides could not be distinguished from the holotype of Youngina capensis. Others considered all specimens attributed to Proterosuchus, Chasmatosaurus, and Elaphrosuchus conspecific. In both cases distinct skull shapes were attributed to taphonomic variations due to distortion pressure or allometric growth. Here a large phylogenetic analysis of the Amniota (401 taxa) tests those hypotheses. The resulting tree recovers a den of small Youngina specimens preceding the Protorosauria. Another specimen nests at the base of the Protorosauria. Six others nest between the Protorosauria and the Archosauriformes. The most derived of these bears a nascent antorbital fenestra. Two other putative Youngina specimens nest at unrelated nodes. In like fashion, the various specimens assigned to Proterosuchus are recovered in distinct clades. One leads to the Proterochampsidae, Parasuchia and Choristodera. The latter lost the antorbital fenestra. Another clade leads to all higher archosauriforms. The present analysis reveals an evolutionary sequence shedding new light on the origin and radiation of early archosauriforms. Taphonomic distortion pressure and allometry during ontogeny were less of a factor than previously assumed. The splitting of several specimens currently considered Youngina and Proterosuchus into distinct genera and species is supported here. INTRODUCTION The Archosauriformes is a widely recognized monophyletic clade that includes, by definition, the most recent common ancestor of Proterosuchidae, Erythrosuchidae, 2 Proterochampsidae, and Archosauria (Gauthier, 1986). Later studies (e.g., Sereno, 1991; Parrish, 1993; Juul, 1994; Ezcurra, 2010; Nesbitt, 2011) have universally rooted their archosauriform clades on Proterosuchidae or Proterosuchus. -
Reptile Family Tree Peters 2021 1909 Taxa, 235 Characters
Turinia Enoplus Chondrichtyes Jagorina Gemuendina Manta Chordata Loganellia Ginglymostoma Rhincodon Branchiostoma Tristychius Pikaia Tetronarce = Torpedo Palaeospondylus Craniata Aquilolamna Tamiobatis Myxine Sphyrna Metaspriggina Squalus Arandaspis Pristis Poraspis Rhinobatos Drepanaspis Cladoselache Pteromyzon adult Promissum Chlamydoselachus Pteromyzon hatchling Aetobatus Jamoytius Squatina Birkenia Heterodontus Euphanerops Iniopteryx Drepanolepis Helodus Callorhinchus Haikouichthys Scaporhynchus Belantsea Squaloraja Hemicyclaspis Chimaera Dunyu CMNH 9280 Mitsukurina Rhinochimaera Tanyrhinichthys Isurus Debeerius Thelodus GLAHM–V8304 Polyodon hatchling Cetorhinus Acipenser Yanosteus Oxynotus Bandringa PF8442 Pseudoscaphirhynchus Isistius Polyodon adult Daliatus Bandringa PF5686 Gnathostomata Megachasma Xenacanthus Dracopristis Akmonistion Ferromirum Strongylosteus Ozarcus Falcatus Reptile Family Tree Chondrosteus Hybodus fraasi Hybodus basanus Pucapampella Osteichthyes Orodus Peters 2021 1943 taxa, 235 characters Gregorius Harpagofututor Leptolepis Edestus Prohalecites Gymnothorax funebris Doliodus Gymnothorax afer Malacosteus Eurypharynx Amblyopsis Lepidogalaxias Typhlichthys Anableps Kryptoglanis Phractolaemus Homalacanthus Acanthodes Electrophorus Cromeria Triazeugacanthus Gymnotus Gorgasia Pholidophorus Calamopleurus Chauliodus Bonnerichthys Dactylopterus Chiasmodon Osteoglossum Sauropsis Synodus Ohmdenia Amia Trachinocephalus BRSLI M1332 Watsonulus Anoplogaster Pachycormus Parasemionotus Aenigmachanna Protosphyraena Channa Aspidorhynchus -
THE AERODYNAMICS of the BRITISH LATE TRIASSIC KUEHNEOSAURIDAE by KOEN STEIN* , COLIN PALMER , PAMELA G
[Palaeontology, Vol. 51, Part 4, 2008, pp. 967–981] THE AERODYNAMICS OF THE BRITISH LATE TRIASSIC KUEHNEOSAURIDAE by KOEN STEIN* , COLIN PALMER , PAMELA G. GILL and MICHAEL J. BENTON *Institut fu¨r Pala¨ontologie, Nußallee 8, 53115 Bonn, Germany; e-mail: [email protected] Department of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK; e-mail: [email protected] Typescript received 5 April 2007; accepted in revised form 17 September 2007 Abstract: The Kuehneosauridae (Late Triassic, Britain, probably present to enhance pitch control. Kuehneosuchus USA) had remarkable adaptations, most notably their elon- was capable of gliding at angles (h) between 13 and 16 gate mid-dorsal ribs that were presumably covered with a degrees, at speeds between 7 and 9 m ⁄ s, and was probably skin membrane in life. These lateral ‘wings’ have always been very manoeuvrable when airborne. Kuehneosaurus was capa- linked with some form of gliding adaptation, but quantita- ble of parachuting (h > 45 degrees) at speeds between 10 tive studies have been limited. Here, we provide a thorough and 12 m ⁄ s. It is unclear whether the British kuehneosaurid aerodynamic analysis of both genera of British kuehneosaur- material represents two genera, as assumed here, two species ids based on theory and on experiments with life-sized mod- of one genus, or sexual dimorphs of a single species, where els in a wind tunnel. Of the two genera, Kuehneosuchus, with the gliding Kuehneosuchus was the male, which used its glid- elongate ‘wings’, was a glider, and Kuehneosaurus, with much ing and perhaps highly coloured ‘wings’ to display to the shorter ‘wings’, was a parachutist. -
Indice Dei NOMI - VOLUME I
INDICE DEI NOMI - VOLUME I A Adanson M. 32 Alberti (von Alberti) F. Alberto Magno di Bollstädt 37 Aldrovandi U. 14, Allee W.C. 154 Allen J.A. 117 Alvarez L. 207 Amici G.B. 86 Aristotele 8, 9, 25, 26, 28, 37, 38 Arduino G. 14, 179, Argand E. 18, 215, 217 Armstrong H. A. Ashlock P.D. 36, 43 Ashurnasirpal II 86, Avcin M.J. Avery O. 21 Avicenna 9 B Bacone F. (Francis Bacon) 215 Bacone R. (Bacon R. o Doctor Mirabilis) 8 Bachmann A. (Rivinus) 31 Bada J. Bailey W. 20 Banks Harlan P. Barrande J. 33 Barrell Y.J. Bateson W. 20, 21 Bauer G. (Agricola) 9, 73 Bauhin K. 28, 29 Beccari J.B. 87 Becquerel A.H. 23 Belon P. 27, 28 Bengtson P. 34, Berg L.S. 71 Bergmann C.G.L.C. 46, 117 Berry E.W. 20, Boccaccio 9, Bock H. 27, Bosellini F. 135 Brillouin L. 57, Bromley R.G. 104, Brown R. 19 Brunfels O. 27 Brunhes B. 197, 208, Bruno G. 9 Busch, D.A. 176 C F Carey S.W. 216, Fischer G. 86 Cardano G. 9, Fisher O. 216 Castle W. 63 Fisher R.A. 21, 63 Cavalier-Smith T. Fleming W. 19 Cesalpino A. 25, 28, 29, 32 Fortis A. 17 Cesi F. 31, Fracastoro G. 9 Chamberlin R.T. 20, 215 Fuchs L. 27, 28, Chambers R. 17, Clausius R. 57, G Colonna F. 9, 11 Galton F. 19, 58 Colosi G. 62, Garbari F. 43 Conrad V. 2 Garstang W. 51 Cope E.D. -
An Early Kuehneosaurid Reptile (Reptilia: Diapsida) from the Early Trias− Sic of Poland
AN EARLY KUEHNEOSAURID REPTILE FROM THE EARLY TRIASSIC OF POLAND SUSAN E. EVANS Evans, S.E. 2009. An early kuehneosaurid reptile (Reptilia: Diapsida) from the Early Trias− sic of Poland. Palaeontologia Polonica 65, 145–178. The Early Triassic locality of Czatkowice, Poland has yielded fish, amphibians, and a series of small reptiles including procolophonians, lepidosauromorphs and archosauromorphs. The lepidosauromorphs are amongst the smallest and rarest components of the assemblage and constitute two new taxa, one of which is described and named here. Pamelina polonica shares skull and vertebral characters with the kuehneosaurs, a group of specialised long− ribbed gliders, previously known only from the Late Triassic of Britain and North America. The relationship is confirmed by cladistic analysis. Pamelina is the earliest known kuehneo− saur and provides new information about the history of this clade. It is less derived post− cranially than any of the Late Triassic taxa, but probably had at least rudimentary gliding or parachuting abilities. Key words: Reptilia, Kuehneosauridae, Triassic, Poland, gliding, Czatkowice. Susan E. Evans [[email protected]], Department of Cell and Developmental Biology, UCL, University College London, Gower Street, London, WC1E 6BT, UK. Received 1 May 2006, accepted 15 August 2007 146 SUSAN E. EVANS INTRODUCTION The Neodiapsida of Benton (1985) encompasses a wide range of diapsid lineages, most of which can be assigned to either Archosauromorpha or Lepidosauromorpha (Gauthier et al. 1988). Archosauromorpha encompasses a large and successful crown clade (Archosauria) and a series of distinctive stem lineages (e.g., protorosaurs, tanystropheiids, Prolacerta, Rhynchosauria, Trilophosauria, Evans 1988; Gauthier et al. 1988; Müller 2002, 2004; Modesto and Sues 2004).