Limb Ossification in the Paleozoic Branchiosaurid Apateon (Temnospondyli) and the Early Evolution of Preaxial Dominance in Tetrapod Limb Development
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Phylogeny and Evolution of the Dissorophoid Temnospondyls
Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses. -
Early Tetrapod Relationships Revisited
Biol. Rev. (2003), 78, pp. 251–345. f Cambridge Philosophical Society 251 DOI: 10.1017/S1464793102006103 Printed in the United Kingdom Early tetrapod relationships revisited MARCELLO RUTA1*, MICHAEL I. COATES1 and DONALD L. J. QUICKE2 1 The Department of Organismal Biology and Anatomy, The University of Chicago, 1027 East 57th Street, Chicago, IL 60637-1508, USA ([email protected]; [email protected]) 2 Department of Biology, Imperial College at Silwood Park, Ascot, Berkshire SL57PY, UK and Department of Entomology, The Natural History Museum, Cromwell Road, London SW75BD, UK ([email protected]) (Received 29 November 2001; revised 28 August 2002; accepted 2 September 2002) ABSTRACT In an attempt to investigate differences between the most widely discussed hypotheses of early tetrapod relation- ships, we assembled a new data matrix including 90 taxa coded for 319 cranial and postcranial characters. We have incorporated, where possible, original observations of numerous taxa spread throughout the major tetrapod clades. A stem-based (total-group) definition of Tetrapoda is preferred over apomorphy- and node-based (crown-group) definitions. This definition is operational, since it is based on a formal character analysis. A PAUP* search using a recently implemented version of the parsimony ratchet method yields 64 shortest trees. Differ- ences between these trees concern: (1) the internal relationships of aı¨stopods, the three selected species of which form a trichotomy; (2) the internal relationships of embolomeres, with Archeria -
Phylogeny and Evolution of the Dissorophoid Temnospondyls
Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses. -
Physical and Environmental Drivers of Paleozoic Tetrapod Dispersal Across Pangaea
ARTICLE https://doi.org/10.1038/s41467-018-07623-x OPEN Physical and environmental drivers of Paleozoic tetrapod dispersal across Pangaea Neil Brocklehurst1,2, Emma M. Dunne3, Daniel D. Cashmore3 &Jӧrg Frӧbisch2,4 The Carboniferous and Permian were crucial intervals in the establishment of terrestrial ecosystems, which occurred alongside substantial environmental and climate changes throughout the globe, as well as the final assembly of the supercontinent of Pangaea. The fl 1234567890():,; in uence of these changes on tetrapod biogeography is highly contentious, with some authors suggesting a cosmopolitan fauna resulting from a lack of barriers, and some iden- tifying provincialism. Here we carry out a detailed historical biogeographic analysis of late Paleozoic tetrapods to study the patterns of dispersal and vicariance. A likelihood-based approach to infer ancestral areas is combined with stochastic mapping to assess rates of vicariance and dispersal. Both the late Carboniferous and the end-Guadalupian are char- acterised by a decrease in dispersal and a vicariance peak in amniotes and amphibians. The first of these shifts is attributed to orogenic activity, the second to increasing climate heterogeneity. 1 Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. 2 Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany. 3 School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK. 4 Institut -
Apateon Dracyiensis Melanerpeton Sembachense Zone 99, 105
Index Page numbers in italic denote figures. Page numbers in bold denote tables. A7 Rhyolite, Provence 190, 283,284 Artinskian Actinopterygii, Carboniferous-Permian 217-30 Permian tracksite correlations 188 Lower Permian 224-6 SGCS 2, 2 Stephanian 221-4 Asselian Westphalian 218 21 Permian tracksite correlations 188 aeolian sediments SGCS 2, 2 Perm~Carboniferous climates 127 Asterochlaena laxa 55 ventifacts/dreikanters 287, 288 Australia, Sakmarian transgressive systems 119 Africa Autun Basin 99 101 Early Triassic correlation chart 330 1,330 magnetic polarity time scale across PTB 23-4 general succession 100 Karoo Group 23-4 sedimentological development 99-101 Inter-Tropical Convergence (ITC) 124 Autunian Karoo Basin 117, 119 flora 250, 309 Karoo Group, magnetic polarity time scale across PTB Permian composite section, Lodrve Basin 244 23-4 sedimentary cycles, Iberian Ranges 263-4 ocean currents, climate effects 126 as a series 5 recent precipitation 124 tetrapod ichnofacies and ichnocoenoses 147, 148, 191-2 Balearic Islands 249, 270, 270-2 Albania, Early Triassic 22 biostratigraphical data 271 2 algae, Chemnitz and Tocantins 49 Buntsandstein 292 Alleghanian orogenic system 120-1,298 Permian-Triassic 270 Alpine orogeny 261 Bas-Argens basin amniotes, traces (footprints) 158-63 A7 Rhyolite 190, 283,284 amphibian biostratigraphy correlations 201 15 tetrapod ichnofacies 189 90, 189, 193 biostratigraphical potential of other tetrapods 211 12 Batrachichnus delicatulus 181 France, Bourbon l'Archambault Basin, Massif Central Batrachichnus ichnofacies -
A Histological Study of a Femur of Plagiosuchus, a Middle Triassic Temnospondyl Amphibian from Southern Germany, Using Thin Sections and Micro-CT Scanning•
Netherlands Journal of Geosciences — Geologie en Mijnbouw | 92 – 2/3 | 97-108 | 2013 A histological study of a femur of Plagiosuchus, a Middle Triassic temnospondyl amphibian from southern Germany, using thin sections and micro-CT scanning• D. Konietzko-Meier1,2,* & A. Schmitt2 1 Uniwersytet Opolski, Katedra Biosystematyki, ul. Oleska 22, 45-052 Opole, Poland 2 Steinmann Institut, Universität Bonn, Nussallee 8, 53115 Bonn, Germany * Corresponding author. Email: [email protected] Manuscript received: August 2012, accepted: April 2013 Abstract The histology of a femur of Plagiosuchus, a Middle Triassic temnospondyl amphibian, is described on the basis of two supplementary methods: classic thin sectioning and micro-CT scanning. In addition, the effectiveness of high-resolution micro-CT scanning for histological analysis is assessed. A classic, mid-shaft thin section of the femur was prepared, but prior to slicing two micro-CT scans were made. One of these has an image stack of a total of 1,024 images in the horizontal plane and a slice thickness of 87.8 μm, so that the entire bone could be captured, while the second was at mid-shaft region only, yet with a higher resolution of 28.3 μm and an image stack of 787 images in the horizontal plane. The classic thin section shows a very small medullary region which is surrounded by a layer of endosteal bone. The thick cortex is highly porous with numerous large, mainly longitudinal, vascular canals arranged in layers. In the deepest cortex woven bone occurs and primary osteons had locally started to form (incipient fibro-lamellar bone), which gradually passes into parallel-fibred bone and more lamellar bone close to the outer surface. -
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. -
(Temnospondyli), and the Evolution of Modern
THE LOWER PERMIAN DISSOROPHOID DOLESERPETON (TEMNOSPONDYLI), AND THE EVOLUTION OF MODERN AMPHIBIANS Trond Sigurdsen Department of Biology McGill University, Montreal November 2009 A thesis submitted to McGill University in partial fulfillment of the requirements of the degree of Doctor of Philosophy © Trond Sigurdsen 2009 1 ACKNOWLEDGMENTS I am deeply grateful to my supervisors Robert L. Carroll and David M. Green for their support, and for revising and correcting the drafts of the individual chapters. Without their guidance, encouragement, and enthusiasm this project would not have been possible. Hans Larsson has also provided invaluable help, comments, and suggestions. Special thanks go to John R. Bolt, who provided specimens and contributed to Chapters 1 and 3. I thank Farish Jenkins, Jason Anderson, and Eric Lombard for making additional specimens available. Robert Holmes, Jean-Claude Rage, and Zbyněk Roček have all provided helpful comments and observations. Finally, I would like to thank present and past members of the Paleolab at the Redpath Museum, Montreal, for helping out in various ways. Specifically, Thomas Alexander Dececchi, Nadia Fröbisch, Luke Harrison, Audrey Heppleston and Erin Maxwell have contributed helpful comments and technical insight. Funding was provided by NSERC, the Max Stern Recruitment Fellowship (McGill), the Delise Allison and Alma Mater student travel grants (McGill), and the Society of Vertebrate Paleontology Student Travel Grant. 2 CONTRIBUTIONS OF AUTHORS Chapters 1 and 3 were written in collaboration with Dr. John R. Bolt from the Field Museum of Chicago. The present author decided the general direction of these chapters, studied specimens, conducted the analyses, and wrote the final drafts. -
Of Modern Amphibians: a Commentary
The origin(s) of modern amphibians: a commentary. D. Marjanovic, Michel Laurin To cite this version: D. Marjanovic, Michel Laurin. The origin(s) of modern amphibians: a commentary.. Journal of Evolutionary Biology, Wiley, 2009, 36, pp.336-338. 10.1007/s11692-009-9065-8. hal-00549002 HAL Id: hal-00549002 https://hal.archives-ouvertes.fr/hal-00549002 Submitted on 7 May 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. The origin(s) of modern amphibians: a commentary By David Marjanović1 and Michel Laurin1* 1Address: UMR CNRS 7207 “Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements”, Muséum National d’Histoire Naturelle, Département Histoire de la Terre, Bâtiment de Géologie, case postale 48, 57 rue Cuvier, F-75231 Paris cedex 05, France *Corresponding author tel/fax. (+33 1) 44 27 36 92 E-mail: [email protected] Number of words: 1884 Number of words in text section only: 1378 2 Anderson (2008) recently reviewed the controversial topic of extant amphibian origins, on which three (groups of) hypotheses exist at the moment. Anderson favors the “polyphyly hypothesis” (PH), which considers the extant amphibians to be polyphyletic with respect to many Paleozoic limbed vertebrates and was most recently supported by the analysis of Anderson et al. -
A Triassic Stem-Salamander from Kyrgyzstan and the Origin of Salamanders
A Triassic stem-salamander from Kyrgyzstan and the origin of salamanders Rainer R. Schocha,1, Ralf Werneburgb, and Sebastian Voigtc aStaatliches Museum für Naturkunde in Stuttgart, D-70191 Stuttgart, Germany; bNaturhistorisches Museum Schloss Bertholdsburg, D-98553 Schleusingen, Germany; and cUrweltmuseum GEOSKOP/Burg Lichtenberg (Pfalz), D-66871 Thallichtenberg, Germany Edited by Neil H. Shubin, University of Chicago, Chicago, IL, and approved April 3, 2020 (received for review January 24, 2020) The origin of extant amphibians remains largely obscure, with Cretaceous in northwestern China, providing much data on the only a few early Mesozoic stem taxa known, as opposed to a much early evolution and diversification of the clade. better fossil record from the mid-Jurassic on. In recent time, an- Recently, a German team excavating in the Kyrgyz Madygen urans have been traced back to Early Triassic forms and caecilians Formation (16) recovered a second find of Triassurus that is not have been traced back to the Late Jurassic Eocaecilia, both of only larger and better preserved, but also adds significantly more which exemplify the stepwise acquisition of apomorphies. Yet data on this taxon. Reexamination of the type has revealed the most ancient stem-salamanders, known from mid-Jurassic shared apomorphic features between the two Madygen speci- rocks, shed little light on the origin of the clade. The gap between mens, some of which turned out to be stem-salamander (uro- salamanders and other lissamphibians, as well as Paleozoic tetra- pods, remains considerable. Here we report a new specimen of dele) autapomorphies. The present findings demonstrate not Triassurus sixtelae, a hitherto enigmatic tetrapod from the Middle/ only that Triassurus is a valid tetrapod taxon, but also, and more Late Triassic of Kyrgyzstan, which we identify as the geologically oldest importantly, that it forms a very basal stem-salamander, com- stem-group salamander. -
New Specimen of Cacops Woehri Indicates Differences in the Ontogenetic Trajectories Among Cacopine Dissorophids
Foss. Rec., 18, 73–80, 2015 www.foss-rec.net/18/73/2015/ doi:10.5194/fr-18-73-2015 © Author(s) 2015. CC Attribution 3.0 License. New specimen of Cacops woehri indicates differences in the ontogenetic trajectories among cacopine dissorophids N. B. Fröbisch1, A. Brar2, and R. R. Reisz2 1Museum für Naturkunde, Leibniz Institut für Evolutions- und Biodiversitätsforschung, Invalidenstrasse 43, 10115 Berlin, Germany 2Department of Biology, University of Toronto at Mississauga, 3359 Mississauga Road N, Mississauga, ON L5L 1C6, Canada Correspondence to: N. B. Fröbisch ([email protected]) Received: 28 October 2014 – Revised: 22 December 2014 – Accepted: 7 January 2015 – Published: 27 January 2015 Abstract. The Lower Permian Dolese locality has produced 1 Introduction numerous exquisitely preserved tetrapod fossils represent- ing members of a lower Permian upland fauna. Therein, at least nine taxa of the clade Dissorophoidea, ranging in The Lower Permian Dolese Brothers Limestone Quarry lo- size from the large predaceous trematopid Acheloma to the cality near Richard Spur in Oklahoma is the most produc- miniaturized amphibamid Doleserpeton, highlight the great tive fossil site for Paleozoic terrestrial ecosystems, and has taxic and ecological diversity of this anamniote clade. Here yielded more than 40 fully terrestrial tetrapod taxa, many we describe a large specimen of the dissorophid Cacops of which are endemic to the locality (Anderson and Bolt, woehri, which was previously only known from the juvenile 2013; Anderson and Reisz, 2003; Bolt, 1969, 1977; Fröbisch or subadult holotype skull. Another member of the genus Ca- and Reisz, 2008; Fröbisch and Reisz, 2012; Maddin et al., cops present at the Dolese locality, Cacops morrisi, is also 2006; Reisz, 2005; Sullivan and Reisz, 1999; Sullivan et al., represented by specimens spanning juvenile, subadult, and 2000). -
A Supertree of Temnospondyli: Cladogenetic Patterns in the Most Species-Rich Group of Early Tetrapods Marcello Ruta1,*, Davide Pisani2, Graeme T
Proc. R. Soc. B (2007) 274, 3087–3095 doi:10.1098/rspb.2007.1250 Published online 10 October 2007 A supertree of Temnospondyli: cladogenetic patterns in the most species-rich group of early tetrapods Marcello Ruta1,*, Davide Pisani2, Graeme T. Lloyd1 and Michael J. Benton1 1Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK 2Laboratory of Evolutionary Biology, The National University of Ireland, Maynooth, Kildare, Ireland As the most diverse group of early tetrapods, temnospondyls provide a unique opportunity to investigate cladogenetic patterns among basal limbed vertebrates. We present five species-level supertrees for temnospondyls, built using a variety of methods. The standard MRP majority rule consensus including minority components shows slightly greater resolution than other supertrees, and its shape matches well several currently accepted hypotheses of higher-level phylogeny for temnospondyls as a whole. Also, its node support is higher than those of other supertrees (except the combined standard plus Purvis MRP supertree). We explore the distribution of significant as well as informative changes (shifts) in branch splitting employing the standard MRP supertree as a reference, and discuss the temporal distribution of changes in time-sliced, pruned trees derived from this supertree. Also, we analyse those shifts that are most relevant to the end-Permian mass extinction. For the Palaeozoic, shifts occur almost invariably along branches that connect major Palaeozoic groups. By contrast, shifts in the Mesozoic occur predominantly within major groups. Numerous shifts bracket narrowly the end-Permian extinction, indicating not only rapid recovery and extensive diversification of temnospondyls over a short time period after the extinction event (possibly less than half a million years), but also the role of intense cladogenesis in the late part of the Permian (although this was counteracted by numerous ‘background’ extinctions).