The Dimetrodon Dilemma: Reassessing Posture in Sphenacodontians and Related Non-Mammalian Synapsids
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Distributions of Extinction Times from Fossil Ages and Tree Topologies: the Example of Some Mid-Permian Synapsid Extinctions Gilles Didier, Michel Laurin
Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions Gilles Didier, Michel Laurin To cite this version: Gilles Didier, Michel Laurin. Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions. 2021. hal-03258099v2 HAL Id: hal-03258099 https://hal.archives-ouvertes.fr/hal-03258099v2 Preprint submitted on 20 Sep 2021 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. Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions Gilles Didier1 and Michel Laurin2 1 IMAG, Univ Montpellier, CNRS, Montpellier, France 2 CR2P (\Centre de Pal´eontologie { Paris"; UMR 7207), CNRS/MNHN/SU, Mus´eumNational d'Histoire Naturelle, Paris, France September 16, 2021 Abstract Given a phylogenetic tree that includes only extinct, or a mix of extinct and extant taxa, where at least some fossil data are available, we present a method to compute the distribution of the extinction time of a given set of taxa under the Fossilized-Birth-Death model. Our approach differs from the previous ones in that it takes into account (i) the possibility that the taxa or the clade considered may diversify before going extinct and (ii) the whole phylogenetic tree to estimate extinction times, whilst previous methods do not consider the diversification process and deal with each branch independently. -
Biodiversity of the Southern Rupununi Savannah World Wildlife Fund and Global Wildlife Conservation
THIS REPORT HAS BEEN PRODUCED IN GUIANAS COLLABORATION VERZICHT APERWITH: Ç 2016 Biodiversity of the Southern Rupununi Savannah World Wildlife Fund and Global Wildlife Conservation 2016 WWF-Guianas Global Wildlife Conservation Guyana Office PO Box 129 285 Irving Street, Queenstown Austin, TX 78767 USA Georgetown, Guyana [email protected] www.wwfguianas.org [email protected] Text: Juliana Persaud, WWF-Guianas, Guyana Office Concept: Francesca Masoero, WWF-Guianas, Guyana Office Design: Sita Sugrim for Kriti Review: Brian O’Shea, Deirdre Jaferally and Indranee Roopsind Map: Oronde Drakes Front cover photos (left to right): Rupununi Savannah © Zach Montes, Giant Ant Eater © Gerard Perreira, Red Siskin © Meshach Pierre, Jaguar © Evi Paemelaere. Inside cover photo: Gallery Forest © Andrew Snyder. OF BIODIVERSITYTHE SOUTHERN RUPUNUNI SAVANNAH. Guyana-South America. World Wildlife Fund and Global Wildlife Conservation 2016 This booklet has been produced and published thanks to: 1 WWF Biodiversity Assessment Team Expedition Southern Rupununi - Guyana. The Southern Rupununi Biodiversity Survey Team / © WWF - GWC. Biodiversity Assessment Team (BAT) Survey. This programme was created by WWF-Guianas in 2013 to contribute to sound land- use planning by filling biodiversity data gaps in critical areas in the Guianas. As far as possible, it also attempts to understand the local context of biodiversity use and the potential threats in order to recommend holistic conservation strategies. The programme brings together local knowledge experts and international scientists to assess priority areas. With each BAT Survey, species new to science or new country records are being discovered. This booklet acknowledges the findings of a BAT Survey carried out during October-November 2013 in the southern Rupununi savannah, at two locations: Kusad Mountain and Parabara. -
Continental Invertebrate and Plant Trace Fossils in Space and Time: State of the Art and Prospects
48 3RD INTERNATIONAL CONFERENCE OF CONTINENTAL ICHNOLOGY, ABSTRACT VOLUME & FIELD TRIP GUIDE Continental invertebrate and plant trace fossils in space and time: State of the art and prospects M. GABRIELA MANGANO1 *, LUIS A. BUATOIS1 1 Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon SK S7N 5E2, Canada * presenting author, [email protected] Continental invertebrate ichnology has experienced a substantial development during the last quarter of century. From being a field marginal to mainstream marine ichnology, represented by a handful of case studies, continental ichnology has grown to occupy a central position within the field of ani- mal-substrate interactions. This evolution is illustrated not only through the accumulation of ichnolog- ic information nurtured by neoichnologic observations and a detailed scrutiny of ancient continental successions, but also through the establishment of new concepts and methodologies. From an ichnofacies perspective, various recurrent associations were defined B( UATOIS & MÁNGANO 1995; GENISE et al. 2000, 2010, 2016; HUNT & LUCAS 2007; EKDALE et al. 2007; KRAPOVICKAS et al. 2016), a situation sharply contrasting with the sole recognition of the Scoyenia ichnofacies as the only valid one during the seventies and eighties (Table 1; Fig. 1). The ichnofacies model now includes not only freshwater ich- nofacies, but also terrestrial ones, most notably those reflecting the complex nature of paleosol trace fossils (GENISE 2017). Trace fossils are now being increasingly used to establish a chronology of the colonization of the land and to unravel the patterns and processes involved in the occupation of ecospace in continental set- tings (e.g. BUATOIS & MÁNGANO 1993; BUATOIS et al. -
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha)
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) by Richard Kissel A thesis submitted in conformity with the requirements for the degree of doctor of philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto © Copyright by Richard Kissel 2010 Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) Richard Kissel Doctor of Philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto 2010 Abstract Based on dental, cranial, and postcranial anatomy, members of the Permo-Carboniferous clade Diadectidae are generally regarded as the earliest tetrapods capable of processing high-fiber plant material; presented here is a review of diadectid morphology, phylogeny, taxonomy, and paleozoogeography. Phylogenetic analyses support the monophyly of Diadectidae within Diadectomorpha, the sister-group to Amniota, with Limnoscelis as the sister-taxon to Tseajaia + Diadectidae. Analysis of diadectid interrelationships of all known taxa for which adequate specimens and information are known—the first of its kind conducted—positions Ambedus pusillus as the sister-taxon to all other forms, with Diadectes sanmiguelensis, Orobates pabsti, Desmatodon hesperis, Diadectes absitus, and (Diadectes sideropelicus + Diadectes tenuitectes + Diasparactus zenos) representing progressively more derived taxa in a series of nested clades. In light of these results, it is recommended herein that the species Diadectes sanmiguelensis be referred to the new genus -
Distributions of Extinction Times from Fossil Ages and Tree Topologies: the Example of Some Mid-Permian Synapsid Extinctions
bioRxiv preprint doi: https://doi.org/10.1101/2021.06.11.448028; this version posted June 11, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions Gilles Didier1 and Michel Laurin2 1IMAG, Univ Montpellier, CNRS, Montpellier, France 2CR2P (“Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements”; UMR 7207), CNRS/MNHN/UPMC, Sorbonne Université, Muséum National d’Histoire Naturelle, Paris, France June 11, 2021 Abstract Given a phylogenetic tree of extinct and extant taxa with fossils where the only temporal infor- mation stands in the fossil ages, we devise a method to compute the distribution of the extinction time of a given set of taxa under the Fossilized-Birth-Death model. Our approach differs from the previous ones in that it takes into account the possibility that the taxa or the clade considered may diversify before going extinct, whilst previous methods just rely on the fossil recovery rate to estimate confidence intervals. We assess and compare our new approach with a standard previous one using simulated data. Results show that our method provides more accurate confidence intervals. This new approach is applied to the study of the extinction time of three Permo-Carboniferous synapsid taxa (Ophiacodontidae, Edaphosauridae, and Sphenacodontidae) that are thought to have disappeared toward the end of the Cisuralian, or possibly shortly thereafter. The timing of extinctions of these three taxa and of their component lineages supports the idea that a biological crisis occurred in the late Kungurian/early Roadian. -
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 -
Curriculum Vitae
CURRICULUM VITAE AMY C. HENRICI Collection Manager Section of Vertebrate Paleontology Carnegie Museum of Natural History 4400 Forbes Avenue Pittsburgh, Pennsylvania 15213-4080, USA Phone:(412)622-1915 Email: [email protected] BACKGROUND Birthdate: 24 September 1957. Birthplace: Pittsburgh. Citizenship: USA. EDUCATION B.A. 1979, Hiram College, Ohio (Biology) M.S. 1989, University of Pittsburgh, Pennsylvania (Geology) CAREER Carnegie Museum of Natural History (CMNH) Laboratory Technician, Section of Vertebrate Paleontology, 1979 Research Assistant, Section of Vertebrate Paleontology, 1980 Curatorial Assistant, Section of Vertebrate Paleontology, 1980-1984 Scientific Preparator, Section of Paleobotany, 1985-1986 Scientific Preparator, Section of Vertebrate Paleontology, 1985-2002 Acting Collection Manager/Scientific Preparator, 2003-2004 Collection Manager, 2005-present PALEONTOLOGICAL FIELD EXPERIENCE Late Pennsylvanian through Early Permian of Colorado, New Mexico and Utah (fish, amphibians and reptiles) Early Permian of Germany, Bromacker quarry (amphibians and reptiles) Triassic of New Mexico, Coelophysis quarry (Coelophysis and other reptiles) Upper Jurassic of Colorado (mammals and herps) Tertiary of Montana, Nevada, and Wyoming (mammals and herps) Pleistocene of West Virginia (mammals and herps) Lake sediment cores and lake sediment surface samples, Wyoming (pollen and seeds) PROFESSIONAL APPOINTMENTS Associate Editor, Society of Vertebrate Paleontology, 1998-2000. Research Associate in the Science Division, New Mexico Museum of Natural History and Science, 2007-present. PROFESSIONAL ASSOCIATIONS Society of Vertebrate Paleontology Paleontological Society LECTURES and TUTORIALS (Invited and public) 1994. Middle Eocene frogs from central Wyoming: ontogeny and taphonomy. California State University, San Bernardino 1994. Mechanical preparation of vertebrate fossils. California State University, San Bernardino 1994. Mechanical preparation of vertebrate fossils. University of Chicago 2001. -
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 -
Tracks and Evolution of Locomotion in the Sistergroup of Amniotes
A peer-reviewed version of this preprint was published in PeerJ on 31 January 2018. View the peer-reviewed version (peerj.com/articles/4346), which is the preferred citable publication unless you specifically need to cite this preprint. Buchwitz M, Voigt S. 2018. On the morphological variability of Ichniotherium tracks and evolution of locomotion in the sistergroup of amniotes. PeerJ 6:e4346 https://doi.org/10.7717/peerj.4346 On the morphological variability of Ichniotherium tracks and evolution of locomotion in the sistergroup of amniotes Michael Buchwitz Corresp., 1 , Sebastian Voigt Corresp. 2 1 Museum für Naturkunde Magdeburg, Magdeburg, Germany 2 Urweltmuseum Geoskop, Kusel, Germany Corresponding Authors: Michael Buchwitz, Sebastian Voigt Email address: [email protected], [email protected] Ichniotherium tracks with a relatively short pedal digit V (digit length ratio V/IV < 0.6) form the majority of yet described Late Carboniferous to Early Permian diadectomorph tracks and can be related to a certain diadectid clade with corresponding phalangeal reduction that includes Diadectes and its close relatives. Here we document the variation of digit proportions and trackway parameters in 25 trackways (69 step cycles) from nine localities and seven further specimens with incomplete step cycles from the type locality of Ichniotherium cottae (Gottlob quarry) in order to find out whether this type of Ichniotherium tracks represents a homogeneous group or an assemblage of distinct morphotypes and includes variability indicative for evolutionary change in trackmaker locomotion. According to our results, the largest sample of tracks from three Lower Permian sites of the Thuringian Forest, commonly referred to Ichniotherium cottae, is not homogeneous but shows a clear distinction in pace length, pace angulation, apparent trunk length and toe proportions between tracks from Bromacker quarry and those from the stratigraphically older sites Birkheide and Gottlob quarry. -
A New Basal Sphenacodontid Synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany
A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany JÖRG FRÖBISCH, RAINER R. SCHOCH, JOHANNES MÜLLER, THOMAS SCHINDLER, and DIETER SCHWEISS Fröbisch, J., Schoch, R.R., Müller, J., Schindler, T., and Schweiss, D. 2011. A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany. Acta Palaeontologica Polonica 56 (1): 113–120. A new basal sphenacodontid synapsid, represented by an anterior portion of a mandible, demonstrates for the first time the presence of amniotes in the largest European Permo−Carboniferous basin, the Saar−Nahe Basin. The new taxon, Cryptovenator hirschbergeri gen. et sp. nov., is autapomorphic in the extreme shortness and robustness of the lower jaw, with moderate heterodonty, including the absence of a greatly reduced first tooth and only a slight caniniform develop− ment of the second and third teeth. Cryptovenator shares with Dimetrodon, Sphenacodon, and Ctenospondylus, but nota− bly not with Secodontosaurus, enlarged canines and a characteristic teardrop outline of the marginal teeth in lateral view, possession of a deep symphyseal region, and a strongly concave dorsal margin of the dentary. The new find shows that sphenacodontids were present in the Saar−Nahe Basin by the latest Carboniferous, predating the record of sphenacodontid tracks from slightly younger sediments in this region. Key words: Synapsida, Sphenacodontidae, Carboniferous, Saar−Nahe Basin, Germany. Jörg Fröbisch [[email protected]], Department of Geology, The Field Museum, 1400 South Lake Shore Drive, Chicago, Illinois 60605, USA and [joerg.froebisch@mfn−berlin.de], Museum für Naturkunde Leibniz−Institut für Evolu− tions− und Biodiversitätsforschung an der Humboldt−Universität zu Berlin, Invalidenstr. -
The Vertebrate Fauna of the New Mexico Permian Alfred S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/11 The vertebrate fauna of the New Mexico Permian Alfred S. Romer, 1960, pp. 48-54 in: Rio Chama Country, Beaumont, E. C.; Read, C. B.; [eds.], New Mexico Geological Society 11th Annual Fall Field Conference Guidebook, 129 p. This is one of many related papers that were included in the 1960 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Evolution and Homology of the Astragalus in Early Amniotes: New Fossils, New Perspectives
JOURNAL OF MORPHOLOGY 267:415–425 (2006) Evolution and Homology of the Astragalus in Early Amniotes: New Fossils, New Perspectives F. Robin O’Keefe,1* Christian A. Sidor,1 Hans C.E. Larsson,2 Abdoudaye Maga,3 and Oumarou Ide3 1Department of Anatomy, New York College of Osteopathic Medicine, Old Westbury, New York 11568 2Redpath Museum, McGill University, Montreal, Quebec H3A 2K6, Canada 3Institut de Recherches en Sciences Humaines, Niamey, Niger Republic ABSTRACT The reorganization of the ankle in basal tarsal elements are unclear, rendering the study of amniotes has long been considered a key innovation al- specific joint articulations difficult (Sumida, 1997, p. lowing the evolution of more terrestrial and cursorial be- 387). New data and new insights on the developmen- havior. Understanding how this key innovation arose is a complex problem that largely concerns the homologizing tal and evolutionary repatterning of the amniote of the amniote astragalus with the various ossifications in ankle are therefore of prime importance, for they the anamniote tarsus. Over the last century, several hy- bear on one of the key transitions in tetrapod his- potheses have been advanced homologizing the amniote tory: the attainment of full terrestriality after the astragalus with the many ossifications in the ankle of long transition from fin to limb (Clack, 2002). amphibian-grade tetrapods. There is an emerging consen- Perhaps the most important novelty within the sus that the amniote astragalus is a complex structure amniote tarsus is the astragalus, a large, complex emerging via the co-ossification of several originally sep- arate elements, but the identities of these elements re- bone comprising the primary area of articulation for main unclear.