Reassessing the Permian Saurian Fossil Record and the Timing of the Crocodile-Lizard Divergence Ezcurra, Martin; Scheyer, Torsten M.; Butler, Richard
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A Phylogenomic Analysis of Turtles ⇑ Nicholas G
Molecular Phylogenetics and Evolution 83 (2015) 250–257 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev A phylogenomic analysis of turtles ⇑ Nicholas G. Crawford a,b,1, James F. Parham c, ,1, Anna B. Sellas a, Brant C. Faircloth d, Travis C. Glenn e, Theodore J. Papenfuss f, James B. Henderson a, Madison H. Hansen a,g, W. Brian Simison a a Center for Comparative Genomics, California Academy of Sciences, 55 Music Concourse Drive, San Francisco, CA 94118, USA b Department of Genetics, University of Pennsylvania, Philadelphia, PA 19104, USA c John D. Cooper Archaeological and Paleontological Center, Department of Geological Sciences, California State University, Fullerton, CA 92834, USA d Department of Biological Sciences, Louisiana State University, Baton Rouge, LA 70803, USA e Department of Environmental Health Science, University of Georgia, Athens, GA 30602, USA f Museum of Vertebrate Zoology, University of California, Berkeley, CA 94720, USA g Mathematical and Computational Biology Department, Harvey Mudd College, 301 Platt Boulevard, Claremont, CA 9171, USA article info abstract Article history: Molecular analyses of turtle relationships have overturned prevailing morphological hypotheses and Received 11 July 2014 prompted the development of a new taxonomy. Here we provide the first genome-scale analysis of turtle Revised 16 October 2014 phylogeny. We sequenced 2381 ultraconserved element (UCE) loci representing a total of 1,718,154 bp of Accepted 28 October 2014 aligned sequence. Our sampling includes 32 turtle taxa representing all 14 recognized turtle families and Available online 4 November 2014 an additional six outgroups. Maximum likelihood, Bayesian, and species tree methods produce a single resolved phylogeny. -
PROGRAMME ABSTRACTS AGM Papers
The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important. -
Biomechanical Assessment of Evolutionary Changes in the Lepidosaurian Skull
Biomechanical assessment of evolutionary changes in the lepidosaurian skull Mehran Moazena,1, Neil Curtisa, Paul O’Higginsb, Susan E. Evansc, and Michael J. Fagana aDepartment of Engineering, University of Hull, Hull HU6 7RX, United Kingdom; bThe Hull York Medical School, University of York, York YO10 5DD, United Kingdom; and cResearch Department of Cell and Developmental Biology, University College London, Gower Street, London WC1E 6BT, United Kingdom Edited by R. McNeill Alexander, University of Leeds, Leeds, United Kingdom, and accepted by the Editorial Board March 24, 2009 (received for review December 23, 2008) The lepidosaurian skull has long been of interest to functional mor- a synovial joint with the pterygoid, the base resting in a pit (fossa phologists and evolutionary biologists. Patterns of bone loss and columellae) on the dorsolateral pterygoid surface. Thus, the gain, particularly in relation to bars and fenestrae, have led to a question at issue in relation to the lepidosaurian lower temporal variety of hypotheses concerning skull use and kinesis. Of these, one bar is not the functional advantage of its loss (13), but rather of of the most enduring relates to the absence of the lower temporal bar its gain in some rhynchocephalians and, very rarely, in lizards in squamates and the acquisition of streptostyly. We performed a (12, 14). This, in turn, raises questions as to the selective series of computer modeling studies on the skull of Uromastyx advantages of the different lepidosaurian skull morphologies. hardwickii, an akinetic herbivorous lizard. Multibody dynamic anal- Morphological changes in the lepidosaurian skull have been ysis (MDA) was conducted to predict the forces acting on the skull, the subject of theoretical and experimental studies (6, 8, 9, and the results were transferred to a finite element analysis (FEA) to 15–19) that aimed to understand the underlying selective crite- estimate the pattern of stress distribution. -
Evolution of the Iguanine Lizards (Sauria, Iguanidae) As Determined by Osteological and Myological Characters David F
Brigham Young University Science Bulletin, Biological Series Volume 12 | Number 3 Article 1 1-1971 Evolution of the iguanine lizards (Sauria, Iguanidae) as determined by osteological and myological characters David F. Avery Department of Biology, Southern Connecticut State College, New Haven, Connecticut Wilmer W. Tanner Department of Zoology, Brigham Young University, Provo, Utah Follow this and additional works at: https://scholarsarchive.byu.edu/byuscib Part of the Anatomy Commons, Botany Commons, Physiology Commons, and the Zoology Commons Recommended Citation Avery, David F. and Tanner, Wilmer W. (1971) "Evolution of the iguanine lizards (Sauria, Iguanidae) as determined by osteological and myological characters," Brigham Young University Science Bulletin, Biological Series: Vol. 12 : No. 3 , Article 1. Available at: https://scholarsarchive.byu.edu/byuscib/vol12/iss3/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Brigham Young University Science Bulletin, Biological Series by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. S-^' Brigham Young University f?!AR12j97d Science Bulletin \ EVOLUTION OF THE IGUANINE LIZARDS (SAURIA, IGUANIDAE) AS DETERMINED BY OSTEOLOGICAL AND MYOLOGICAL CHARACTERS by David F. Avery and Wilmer W. Tanner BIOLOGICAL SERIES — VOLUME Xil, NUMBER 3 JANUARY 1971 Brigham Young University Science Bulletin -
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). -
Reinterpretation of the Holotype of Malerisaurus Langstoni, a Diapsid Reptile from the Upper Triassic Chinle Group of West Texas
Harris et al., eds., 2006, The Triassic-Jurassic Terrestrial Transition. New Mexico Museum of Natural History and Science Bulletin 37. 543 REINTERPRETATION OF THE HOLOTYPE OF MALERISAURUS LANGSTONI, A DIAPSID REPTILE FROM THE UPPER TRIASSIC CHINLE GROUP OF WEST TEXAS JUSTIN A. SPIELMANN1, SPENCER G. LUCAS1, ADRIAN P. HUNT1 AND ANDREW B. HECKERT2 1New Mexico Museum of Natural History and Science, 1801 Mountain Rd., Albuquerque, NM 87104-1375; 2Department of Geology, Appalachian State University, ASU Box 32067, Boone, NC 28608-2067 Abstract—The holotype of Malerisaurus langstoni from the Late Triassic (Otischalkian) Trilophosaurus quarry 2 of West Texas is a chimera. The holotype represents at least 6-7 individuals of four reptilian groups: Trilophosauridae, Rhynchosauridae, Parasuchidae and Aetosauria. The majority of the material, including all of the cranial fragments, are re-identified as Trilophosaurus buettneri. Based on the chimeric nature of the specimen, the holotype of M. langstoni is restricted to the skull fragments and considered a junior subjective synonym of T. buetterni. This reassessment of M. langstoni calls into question the validity of M. robinsonae from the Maleri Formation in India and suggests that at least some of the elements referred to this taxon may, in fact, be a record of Trilophosaurus. This would extend the paleogeographic range of Trilophosaurus from a taxon endemic to the American Southwest to a nearly Pangean distribution during the Late Triassic. INTRODUCTION Malerisaurus langstoni is a Late Triassic (Otischalkian) diapsid reptile known only from a single partial skeleton, the holotype, collected from Trilophosaurus quarry 2. Located in Howard County, West Texas, 25 km southeast of Big Spring, the Trilophosaurus quarries in the Colo- rado City Formation of the Chinle Group (Fig. -
Tiago Rodrigues Simões
Diapsid Phylogeny and the Origin and Early Evolution of Squamates by Tiago Rodrigues Simões A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in SYSTEMATICS AND EVOLUTION Department of Biological Sciences University of Alberta © Tiago Rodrigues Simões, 2018 ABSTRACT Squamate reptiles comprise over 10,000 living species and hundreds of fossil species of lizards, snakes and amphisbaenians, with their origins dating back at least as far back as the Middle Jurassic. Despite this enormous diversity and a long evolutionary history, numerous fundamental questions remain to be answered regarding the early evolution and origin of this major clade of tetrapods. Such long-standing issues include identifying the oldest fossil squamate, when exactly did squamates originate, and why morphological and molecular analyses of squamate evolution have strong disagreements on fundamental aspects of the squamate tree of life. Additionally, despite much debate, there is no existing consensus over the composition of the Lepidosauromorpha (the clade that includes squamates and their sister taxon, the Rhynchocephalia), making the squamate origin problem part of a broader and more complex reptile phylogeny issue. In this thesis, I provide a series of taxonomic, phylogenetic, biogeographic and morpho-functional contributions to shed light on these problems. I describe a new taxon that overwhelms previous hypothesis of iguanian biogeography and evolution in Gondwana (Gueragama sulamericana). I re-describe and assess the functional morphology of some of the oldest known articulated lizards in the world (Eichstaettisaurus schroederi and Ardeosaurus digitatellus), providing clues to the ancestry of geckoes, and the early evolution of their scansorial behaviour. -
And Early Jurassic Sediments, and Patterns of the Triassic-Jurassic
and Early Jurassic sediments, and patterns of the Triassic-Jurassic PAUL E. OLSEN AND tetrapod transition HANS-DIETER SUES Introduction parent answer was that the supposed mass extinc- The Late Triassic-Early Jurassic boundary is fre- tions in the tetrapod record were largely an artifact quently cited as one of the thirteen or so episodes of incorrect or questionable biostratigraphic corre- of major extinctions that punctuate Phanerozoic his- lations. On reexamining the problem, we have come tory (Colbert 1958; Newell 1967; Hallam 1981; Raup to realize that the kinds of patterns revealed by look- and Sepkoski 1982, 1984). These times of apparent ing at the change in taxonomic composition through decimation stand out as one class of the great events time also profoundly depend on the taxonomic levels in the history of life. and the sampling intervals examined. We address Renewed interest in the pattern of mass ex- those problems in this chapter. We have now found tinctions through time has stimulated novel and com- that there does indeed appear to be some sort of prehensive attempts to relate these patterns to other extinction event, but it cannot be examined at the terrestrial and extraterrestrial phenomena (see usual coarse levels of resolution. It requires new fine- Chapter 24). The Triassic-Jurassic boundary takes scaled documentation of specific faunal and floral on special significance in this light. First, the faunal transitions. transitions have been cited as even greater in mag- Stratigraphic correlation of geographically dis- nitude than those of the Cretaceous or the Permian junct rocks and assemblages predetermines our per- (Colbert 1958; Hallam 1981; see also Chapter 24). -
Kirtlington Quarry: Its History and Geology and the Search for Early
Kirtlington Quarry: its history and geology and the search for early mammals Eric F Freeman Abstract: Kirtlington Quarry, a well-known former exposure of Middle Jurassic rocks north of Oxford, was worked for cement production from 1907 until 1929. Important but largely unpublished research undertaken there at the time by Charles J. Bayzand, a museum assistant and geological lecturer, is placed in the context of better known work by M. Odling and W.J. Arkell, his contemporaries at Oxford University. When integrated with the quarry’s industrial archaeology and growth, as reconstructed from old maps and cement production records, Bayzand’s work suggests that a sediment rich in mammal and other microvertebrate fossils, the Kirtlington Mammal Bed, was once extensively exposed, but went unrecognised, and had been largely quarried away prior to its eventual discovery in 1974. Augmented by more recent work, the old research by Bayzand, Odling and Arkell allows the palaeoecology of the Mammal Bed to be modelled, including coastal dune-fields and mammal remains from the faecal debris of theropod dinosaurs. Since the days of Robert Plot (1640–1696), and his were found at the junction between two of the classic Natural History of Oxford-Shire, the area to the north Middle Jurassic rock units named by William Smith, of Oxford (Fig. 1), with its former profusion of quarries the Forest Marble and the Great Oolite. The bones were in highly fossiliferous Jurassic strata, and its proximity acquired by the Oxford University Museum, which had to the learned folk of Oxford University, has played an been opened in 1857, with William Smith’s nephew, important part in the development of geology. -
Reptile” Diversity and Evolution George A
“Reptile” Diversity and Evolution George A. Lozano Department of Biology University of Ottawa Summary Sauropsids Turtles Diapsids/Saurians Plesiosaurs † and ichthyosaurs † Lepidosaurs Tuatara Squamates (snakes, geckos, iguanas, monitors ) Archosaurs (crocodiles, dinosaurs, pterosaurs ) Dinosaurs 2 George A. Lozano Amniota Synapsida Sauropsida Diapsida Turtles Ancestral amniotes & Turtles Turtles - Testudina 250 species Carapace (vertebrae and ribs) Appendicular girdles INSIDE the shell Beak, no teeth (along with aves) Ear ossicle columella (ind?) 4 George A. Lozano Sauropsida Diapsida/Sauria Turtles 250 Archosaurs Ichthyosaurs† Lepidosaurs Plesiosaurs† 9.1K 7K Ear ossicle collumella, 3 rd ind. evol.) Lepidosaurs “scaly” reptiles 6700 species : 4000 lizards, 2700 snakes Tuatara: ancestral diapsid skull Squamata: derived diapsid skull, hemipenes Iguanas Geckos Snakes Skinks Gila monsters, monitor lizards, Komodo dragon 6 George A. Lozano Tuatara Turtles Squamates Modified Euryapsid: Aves diapsid Plesiosaur Ichthyosaur Snakes 8 George A. Lozano Sauropsida Diapsida Turtles Archosaurs Crocodiles Dinosaurs Pterosaurs† Dinosaurs Ornithischians† Saurischians •Ceratopsids •Duck-billed dino Sauropods† Theropods •Stegosaurus •Ankylosaurus Dinosaurs Ornithischians† Saurischians •-ceratops (uni, tri…) •Duck-billed dino Sauropods† Theropods •Stegosaurus •Diplodocus •Ankylosaurus •Brachiosaurus T. rex † Velociraptor † Birds 12 George A. Lozano Sauropod and ornithischian (ankylosaurus) 13 George A. Lozano 14 George A. Lozano Dinosaurs -
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. -
What Really Happened in the Late Triassic?
Historical Biology, 1991, Vol. 5, pp. 263-278 © 1991 Harwood Academic Publishers, GmbH Reprints available directly from the publisher Printed in the United Kingdom Photocopying permitted by license only WHAT REALLY HAPPENED IN THE LATE TRIASSIC? MICHAEL J. BENTON Department of Geology, University of Bristol, Bristol, BS8 1RJ, U.K. (Received January 7, 1991) Major extinctions occurred both in the sea and on land during the Late Triassic in two major phases, in the middle to late Carnian and, 12-17 Myr later, at the Triassic-Jurassic boundary. Many recent reports have discounted the role of the earlier event, suggesting that it is (1) an artefact of a subsequent gap in the record, (2) a complex turnover phenomenon, or (3) local to Europe. These three views are disputed, with evidence from both the marine and terrestrial realms. New data on terrestrial tetrapods suggests that the late Carnian event was more important than the end-Triassic event. For tetrapods, the end-Triassic extinction was a whimper that was followed by the radiation of five families of dinosaurs and mammal- like reptiles, while the late Carnian event saw the disappearance of nine diverse families, and subsequent radiation of 13 families of turtles, crocodilomorphs, pterosaurs, dinosaurs, lepidosaurs and mammals. Also, for many groups of marine animals, the Carnian event marked a more significant turning point in diversification than did the end-Triassic event. KEY WORDS: Triassic, mass extinction, tetrapod, dinosaur, macroevolution, fauna. INTRODUCTION Most studies of mass extinction identify a major event in the Late Triassic, usually placed at the Triassic-Jurassic boundary.