3D Computational Mechanics Elucidate the Evolutionary Implications of Orbit Position and Size Diversity of Early Amphibians
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Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
Marzola Et Al 2017 Cyclotosaurus Greenland
Journal of Vertebrate Paleontology e1303501 (14 pages) Ó by the Society of Vertebrate Paleontology DOI: 10.1080/02724634.2017.1303501 ARTICLE CYCLOTOSAURUS NARASERLUKI, SP. NOV., A NEW LATE TRIASSIC CYCLOTOSAURID (AMPHIBIA, TEMNOSPONDYLI) FROM THE FLEMING FJORD FORMATION OF THE JAMESON LAND BASIN (EAST GREENLAND) MARCO MARZOLA *,1,2,3,4 OCTAVIO MATEUS 1,3 NEIL H. SHUBIN5 and LARS B. CLEMMENSEN 2 1GeoBioTec, Departamento de Ciencias^ da Terra, Faculdade de Ciencias^ e Tecnologia, Universidade Nova de Lisboa, Quinta da Torre, 2829-516 Caparica, Portugal, [email protected]; [email protected]; 2Institut for Geovidenskab og Naturforvaltning (IGN), Det Natur-og Biovidenskabelige Fakultet, Københavns Universitet, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark, [email protected]; 3Museu da Lourinha,~ Rua Joao~ Luıs de Moura, 95, 2530-158 Lourinha,~ Portugal; 4Geocenter Møns Klint, Stengardsvej 8, DK-4751 Borre, Denmark; 5Department of Organismal Biology and Anatomy, University of Chicago, Chicago, Illinois 60637, U.S.A., [email protected] ABSTRACT—Cyclotosaurus naraserluki, sp. nov., is a new Late Triassic capitosaurid amphibian from lacustrine deposits in the Fleming Fjord Formation of the Jameson Land Basin in Greenland. It is based on a fairly complete and well-preserved skull associated with two vertebral intercentra. Previously reported as Cyclotosaurus cf. posthumus, C. naraserluki is unique among cyclotosaurs for having the postorbitals embaying the supratemporals posteromedially. The anterior palatal vacuity presents an autapomorphic complete subdivision by a wide medial premaxillary-vomerine bony connection. The parasphenoid projects between the pterygoids and the exoccipitals, preventing a suture between the two, a primitive condition shared with Rhinesuchidae, Eryosuchus, and Kupferzellia. -
A New Large Capitosaurid Temnospondyl Amphibian from the Early Triassic of Poland
A new large capitosaurid temnospondyl amphibian from the Early Triassic of Poland TOMASZ SULEJ and GRZEGORZ NIEDŹWIEDZKI Sulej, T. and Niedźwiedzki, G. 2013. A new large capitosaurid temnospondyl amphibian from the Early Triassic of Po− land. Acta Palaeontologica Polonica 58 (1): 65–75. The Early Triassic record of the large capitosaurid amphibian genus Parotosuchus is supplemented by new material from fluvial deposits of Wióry, southern Poland, corresponding in age to the Detfurth Formation (Spathian, Late Olenekian) of the Germanic Basin. The skull of the new capitosaurid shows an “intermediate” morphology between that of Paroto− suchus helgolandicus from the Volpriehausen−Detfurth Formation (Smithian, Early Olenekian) of Germany and the slightly younger Parotosuchus orenburgensis from European Russia. These three species may represent an evolutionary lineage that underwent a progressive shifting of the jaw articulation anteriorly. The morphology of the Polish form is dis− tinct enough from other species of Parotosuchus to warrant erection of a new species. The very large mandible of Parot− osuchus ptaszynskii sp. nov. indicates that this was one of the largest tetrapod of the Early Triassic. Its prominent anatomi− cal features include a triangular retroarticular process and an elongated base of the hamate process. Key words: Temnospondyli, Capitosauridae, Buntsandstein, Spathian, Olenekian, Triassic, Holy Cross Mountains, Poland. Tomasz Sulej [[email protected]], Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, PL−00−818 Warszawa, Poland; Grzegorz Niedźwiedzki [[email protected]], Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, PL−00−818 Warszawa, Poland; current addresses: Department of Organismal Biology, Uppsala Uni− versity, Norbyvägen 18A, 752 36 Uppsala, Sweden and Department of Paleobiology and Evolution, Faculty of Biology, University of Warsaw, ul. -
Functional Morphology of Stereospondyl Amphibian Skulls
Functional Morphology of Stereospondyl Amphibian Skulls Samantha Clare Penrice Doctor of Philosophy School of Life Sciences College of Science July 2018 Functional morphology of stereospondyl amphibian skulls Stereospondyls were the most diverse clade of early tetrapods, spanning 190 million years, with over 250 species belonging to eight taxonomic groups. They had a range of morphotypes and have been found on every continent. Stereospondyl phylogeny is widely contested and repeatedly examined but despite these studies, we are still left with the question, why were they so successful and why did they die out? A group-wide analysis of functional morphology, informing us about their palaeobiology, was lacking for this group and was carried out in order to address the questions of their success and demise. Based on an original photograph collection, size independent skull morphometrics were used, in conjunction with analyses of the fossil record and comparative anatomy, to provide a synthesis of the functional morphology of stereospondyl amphibians. Stereospondyls originated in the Carboniferous and most taxonomic groups were extinct at the end of the Triassic. The early Triassic had exceptionally high numbers of short- lived genera, in habitats that were mostly arid but apparently experienced occasional monsoon rains. Genera turnover slowed and diversity was stable in the Middle Triassic, then declined with a series of extinctions of the Late Triassic. Stereospondyls showed the pattern of ‘disaster’ taxa: rapidly diversifying following a mass extinction, spreading to a global distribution, although this high diversity was relatively short-lived. Geometric morphometrics on characteristics of the skull and palate was carried out to assess general skull morphology and identified the orbital position and skull outline to be the largest sources of skull variation. -
A New Large Capitosaurid Temnospondyl Amphibian from the Early Triassic of Poland
A new large capitosaurid temnospondyl amphibian from the Early Triassic of Poland TOMASZ SULEJ and GRZEGORZ NIEDŹWIEDZKI Sulej, T. and Niedźwiedzki, G. 2013. A new large capitosaurid temnospondyl amphibian from the Early Triassic of Po− land. Acta Palaeontologica Polonica 58 (1): 65–75. The Early Triassic record of the large capitosaurid amphibian genus Parotosuchus is supplemented by new material from fluvial deposits of Wióry, southern Poland, corresponding in age to the Detfurth Formation (Spathian, Late Olenekian) of the Germanic Basin. The skull of the new capitosaurid shows an “intermediate” morphology between that of Paroto− suchus helgolandicus from the Volpriehausen−Detfurth Formation (Smithian, Early Olenekian) of Germany and the slightly younger Parotosuchus orenburgensis from European Russia. These three species may represent an evolutionary lineage that underwent a progressive shifting of the jaw articulation anteriorly. The morphology of the Polish form is dis− tinct enough from other species of Parotosuchus to warrant erection of a new species. The very large mandible of Parot− osuchus ptaszynskii sp. nov. indicates that this was one of the largest tetrapod of the Early Triassic. Its prominent anatomi− cal features include a triangular retroarticular process and an elongated base of the hamate process. Key words: Temnospondyli, Capitosauridae, Buntsandstein, Spathian, Olenekian, Triassic, Holy Cross Mountains, Poland. Tomasz Sulej [[email protected]], Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, PL−00−818 Warszawa, Poland; Grzegorz Niedźwiedzki [[email protected]], Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, PL−00−818 Warszawa, Poland; current addresses: Department of Organismal Biology, Uppsala Uni− versity, Norbyvägen 18A, 752 36 Uppsala, Sweden and Department of Paleobiology and Evolution, Faculty of Biology, University of Warsaw, ul. -
Morphological and Histological Description of Small Metoposaurids from Petrified Orf Est National Park, AZ, USA and the Taxonomy of Apachesaurus
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. National Park Service Publications and Papers National Park Service 5-22-2018 Morphological and histological description of small metoposaurids from Petrified orF est National Park, AZ, USA and the taxonomy of Apachesaurus Bryan M. Gee University of Toronto Mississauga & Petrified orF est National Park, [email protected] William G. Parker Petrified orF est National Park Follow this and additional works at: https://digitalcommons.unl.edu/natlpark Part of the Environmental Education Commons, Environmental Policy Commons, Environmental Studies Commons, Fire Science and Firefighting Commons, Leisure Studies Commons, Natural Resource Economics Commons, Natural Resources Management and Policy Commons, Nature and Society Relations Commons, Other Environmental Sciences Commons, Physical and Environmental Geography Commons, Public Administration Commons, and the Recreation, Parks and Tourism Administration Commons Gee, Bryan M. and Parker, William G., "Morphological and histological description of small metoposaurids from Petrified orF est National Park, AZ, USA and the taxonomy of Apachesaurus" (2018). U.S. National Park Service Publications and Papers. 198. https://digitalcommons.unl.edu/natlpark/198 This Article is brought to you for free and open access by the National Park Service at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in U.S. National Park Service Publications and Papers by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. HISTORICAL BIOLOGY 2020, VOL. 32, NO. 2, 203–233 https://doi.org/10.1080/08912963.2018.1480616 ARTICLE Morphological and histological description of small metoposaurids from Petrified Forest National Park, AZ, USA and the taxonomy of Apachesaurus Bryan M. -
Triassic Vertebrate Fossils in Arizona
Heckert, A.B., and Lucas, S.G., eds., 2005, Vertebrate Paleontology in Arizona. New Mexico Museum of Natural History and Science Bulletin No. 29. 16 TRIASSIC VERTEBRATE FOSSILS IN ARIZONA ANDREW B. HECKERT1, SPENCER G. LUCAS2 and ADRIAN P. HUNT2 1Department of Geology, Appalachian State University, ASU Box 32067, Boone, NC 28608-2607; [email protected]; 2New Mexico Museum of Natural History & Science, 1801 Mountain Road NW, Albuquerque, NM 87104-1375 Abstract—The Triassic System in Arizona has yielded numerous world-class fossil specimens, includ- ing numerous type specimens. The oldest Triassic vertebrates from Arizona are footprints and (largely) temnospondyl bones from the Nonesian (Early Triassic: Spathian) Wupatki Member of the Moenkopi Formation. The Perovkan (early Anisian) faunas of the Holbrook Member of the Moenkopi Formation are exceptional in that they yield both body- and trace fossils of Middle Triassic vertebrates and are almost certainly the best-known faunas of this age in the Americas. Vertebrate fossils of Late Triassic age in Arizona are overwhelmingly body fossils of temnospondyl amphibians and archosaurian reptiles, with trace fossils largely restricted to coprolites. Late Triassic faunas in Arizona include rich assemblages of Adamanian (Carnian) and Revueltian (early-mid Norian) age, with less noteworthy older (Otischalkian) assemblages. The Adamanian records of Arizona are spectacular, and include the “type” Adamanian assemblage in the Petrified Forest National Park, the world’s most diverse Late Triassic vertebrate fauna (that of the Placerias/Downs’ quarries), and other world-class records such as at Ward’s Terrace, the Blue Hills, and Stinking Springs Mountain. The late Adamanian (Lamyan) assemblage of the Sonsela Member promises to yield new and important information on the Adamanian-Revueltian transition. -
( Metoposaurus) Azerouali (Dutuit) Comb
Redescription of Arganasaurus ( Metoposaurus) azerouali (Dutuit) comb. nov. from the Upper Triassic of the Argana Basin (Morocco), and the first phylogenetic analysis of the Metoposauridae (Amphibia, Temnospondyli) Valentin Buffa, Nour-Eddine Jalil, J.-Sébastien Steyer To cite this version: Valentin Buffa, Nour-Eddine Jalil, J.-Sébastien Steyer. Redescription of Arganasaurus (Meto- posaurus) azerouali (Dutuit) comb. nov. from the Upper Triassic of the Argana Basin (Morocco), and the first phylogenetic analysis of the Metoposauridae (Amphibia, Temnospondyli). Special pa- pers in palaeontology, Wiley Blackwell Publishing, 2019, 5 (4), pp.699-717. 10.1002/spp2.1259. hal-02967815 HAL Id: hal-02967815 https://hal.sorbonne-universite.fr/hal-02967815 Submitted on 15 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. Page 1 of 60 Palaeontology 1 2 3 REDESCRIPTION OF ARGANASAURUS (METOPOSAURUS) AZEROUALI (DUTUIT) 4 5 6 COMB. NOV. FROM THE LATE TRIASSIC OF THE ARGANA BASIN (MOROCCO), 7 8 AND THE FIRST PHYLOGENETIC ANALYSIS OF THE METOPOSAURIDAE 9 10 -
A Giant Skull of the Temnospondyl Xenotosuchus Africanus from the Middle Triassic of South Africa and Its Ontogenetic Implications
A giant skull of the temnospondyl Xenotosuchus africanus from the Middle Triassic of South Africa and its ontogenetic implications ROSS DAMIANI Damiani, R. 2008. A giant skull of the temnospondyl Xenotosuchus africanus from the Middle Triassic of South Africa and its ontogenetic implications. Acta Palaeontologica Polonica 53 (1): 75–84. A previously unreported large skull of the mastodonsaurid temnospondyl Xenotosuchus africanus, from the Cynognathus Assemblage Zone (Early to Middle Triassic) of the Beaufort Group, Karoo Basin of South Africa, is described. The species is plesiomorphic in most aspects of its cranial anatomy, and only one autapomorphy is tentatively identified herein, namely contact between the left and right exoccipitals posterior to the parasphenoid. The new specimen permits recognition of a growth series for X. africanus from sub−adult (all previously known specimens) to fully adult (new specimen) stages. Ontogenetic changes associated with this include changes in skull proportions, and changes in the morphology of the lacri− mal flexure, frontal, postfrontal, cultriform process and body of the parasphenoid, and the transvomerine tooth row. Key words: Temnospondyli, Xenotosuchus africanus, ontogeny, variation, Triassic, South Africa. Ross Damiani [[email protected]], Staatliches Museum für Naturkunde Stuttgart, Rosenstein 1, D−70191 Stuttgart, Germany. Introduction canus as incertae sedis within the “Capitosauroidea”, noting its peculiar mixture of apomorphic and plesiomorphic char− Temnospondyls form an important part of the fauna of the acters. Damiani (2001a) referred Parotosuchus africanus to Permo−Triassic aged, non−marine deposits of the Beaufort the North American mastodonsaurid genus Wellesaurus Group (Karoo Basin) of South Africa (Damiani and Rubidge based largely on phenetic similarity, which had earlier been 2003). -
Bilaterally Symmetric Fourier Approximations of the Skull Outlines of Temnospondyl Amphibians and Their Bearing on Shape Comparison
Bilaterally symmetric Fourier approximations of the skull outlines of temnospondyl amphibians and their bearing on shape comparison † DHURJATI P SENGUPTA , DEBAPRIYA SENGUPTA* and PARTHASARATHI GHOSH Geological Studies Unit, Physics and Earth Science Division, *Statistics and Mathematics Division, Indian Statistical Institute, 203, BT Road, Kolkata 700 108, India †Corresponding author (Fax, 91-33-25776680; Email, [email protected]) Present work illustrates a scheme of quantitative description of the shape of the skull outlines of temnospondyl amphibians using bilaterally symmetric closed Fourier curves. Some special points have been identified on the Fourier fits of the skull outlines, which are the local maxima, or minima of the distances from the centroid of the points at the skull outline. These points denotes break in curvature of the outline and their positions can be compared to differentiate the skull shapes. The ratios of arc-lengths of the posterior and lateral outline of 58 temnospondyl skulls have been plotted to generate a triaguarity series of the skulls. This series grades different families, some of their genera and species as well as some individuals according to their posterior and lateral skull length ratios. This model while comparing different taxa, takes into account the entire arc-length of the outline of the temnospondyl skulls, and does not depend on few geometric or biological points used by earlier workers for comparing skull shapes. [Sengupta P D, Sengupta D and Ghosh P 2005 Bilaterally symmetric Fourier approximations of the skull outlines of temnospondyl amphibians and their bearing on shape comparison; J. Biosci. 30 377–390] 1. Introduction with extended height. -
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geodiversitas 2021 43 12 e of lif pal A eo – - e h g e r a p R e t e o d l o u g a l i s C - t – n a M e J e l m a i r o DIRECTEUR DE LA PUBLICATION / PUBLICATION DIRECTOR : Bruno David, Président du Muséum national d’Histoire naturelle RÉDACTEUR EN CHEF / EDITOR-IN-CHIEF : Didier Merle ASSISTANT DE RÉDACTION / ASSISTANT EDITOR : Emmanuel Côtez ([email protected]) MISE EN PAGE / PAGE LAYOUT : Emmanuel Côtez COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD : Christine Argot (Muséum national d’Histoire naturelle, Paris) Beatrix Azanza (Museo Nacional de Ciencias Naturales, Madrid) Raymond L. Bernor (Howard University, Washington DC) Alain Blieck (chercheur CNRS retraité, Haubourdin) Henning Blom (Uppsala University) Jean Broutin (Sorbonne Université, Paris, retraité) Gaël Clément (Muséum national d’Histoire naturelle, Paris) Ted Daeschler (Academy of Natural Sciences, Philadelphie) Bruno David (Muséum national d’Histoire naturelle, Paris) Gregory D. Edgecombe (The Natural History Museum, Londres) Ursula Göhlich (Natural History Museum Vienna) Jin Meng (American Museum of Natural History, New York) Brigitte Meyer-Berthaud (CIRAD, Montpellier) Zhu Min (Chinese Academy of Sciences, Pékin) Isabelle Rouget (Muséum national d’Histoire naturelle, Paris) Sevket Sen (Muséum national d’Histoire naturelle, Paris, retraité) Stanislav Štamberg (Museum of Eastern Bohemia, Hradec Králové) Paul Taylor (The Natural History Museum, Londres, retraité) COUVERTURE / COVER : Réalisée à partir des Figures de l’article/Made from the Figures of the article. Geodiversitas est -
DINOSAUR SUCCESS in the TRIASSIC: a NONCOMPETITIVE ECOLOGICAL MODEL This Content Downloaded from 137.222.248.217 on Sat, 17
VOLUME 58, No. 1 THE QUARTERLY REVIEW OF BIOLOGY MARCH 1983 DINOSAUR SUCCESS IN THE TRIASSIC: A NONCOMPETITIVE ECOLOGICAL MODEL MICHAEL J. BENTON University Museum, Parks Road, Oxford OX] 3PW, England, UK ABSTRACT The initial radiation of the dinosaurs in the Triassic period (about 200 million years ago) has been generally regarded as a result of successful competition with the previously dominant mammal- like reptiles. A detailed review of major terrestrial reptile faunas of the Permo- Triassic, including estimates of relative abundance, gives a different picture of the pattern of faunal replacements. Dinosaurs only appeared as dominant faunal elements in the latest Triassic after the disappear- ance of several groups qf mammal-like reptiles, thecondontians (ancestors of dinosaurs and other archosaurs), and rhynchosaurs (medium-sized herbivores). The concepts of differential survival ("competitive") and opportunistic ecological replacement of higher taxonomic categories are contrasted (the latter involves chance radiation to fill adaptive zones that are already empty), and they are applied to the fossil record. There is no evidence that either thecodontians or dinosaurs demonstrated their superiority over mammal-like reptiles in massive competitive take-overs. Thecodontians arose as medium-sized carnivores after the extinction of certain mammal-like reptiles (opportunism, latest Permian). Throughout most of the Triassic, the thecodontians shared carnivore adaptive zones with advanced mammal-like reptiles (cynodonts) until the latter became extinct (random processes, early to late Triassic). Among herbivores, the dicynodont mammal-like reptiles were largely replaced by diademodontoid mammal-like reptiles and rhynchosaurs (differential survival, middle to late Triassic). These groups then became extinct and dinosaurs replaced them and radiated rapidly (opportunism, latest Triassic).