First Morphological Evidence from the Paleocene of Morocco
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The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Inactivation of Thermogenic UCP1 As a Historical Contingency in Multiple Placental Mammal Clades
bioRxiv preprint doi: https://doi.org/10.1101/086819; this version posted November 9, 2016. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Title: Inactivation of thermogenic UCP1 as a historical contingency in multiple placental mammal clades Authors: Michael J. Gaudry1, Martin Jastroch2, Jason R. Treberg1,3, Michael Hofreiter4†, Johanna L.A. Paijmans4†, James Starrett5‡, Nathan Wales6, Anthony V. Signore1§, Mark S. Springer5 and Kevin L. Campbell1* Affiliations: 1Department of Biological Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada. 2Institute for Diabetes and Obesity, Helmholtz Zentrum München, German Research Center for Environmental Health, Parkring 13, 85748 Garching, Germany. 3Department of Human Nutritional Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada. 4Department of Biology, The University of York, Heslington, York, YO10 5DD, UK. 5Department of Biology, University of California, Riverside, CA 92521, USA. 6Centre for GeoGenetics, Natural History Museum of Denmark, Øster Voldgade 5-7, 1350 Copenhagen, Denmark. †Current address: Universität Potsdam, 14476 Potsdam, Germany. ǂCurrent address: San Diego State University, San Diego, California 92182, USA. §Current address: University of Nebraska, Lincoln, Nebraska 68588, USA. *Correspondence: [email protected] 1 bioRxiv preprint doi: https://doi.org/10.1101/086819; this version posted November 9, 2016. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. -
Perissodactyla, Mammalia) from the Middle Eocene of Myanmar Un Nouveau Tapiromorphe Basal (Perissodactyla, Mammalia) De L’Eocène Moyen Du Myanmar
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Geobios 39 (2006) 513–519 http://france.elsevier.com/direct/GEOBIO/ Original article A new basal tapiromorph (Perissodactyla, Mammalia) from the middle Eocene of Myanmar Un nouveau tapiromorphe basal (Perissodactyla, Mammalia) de l’Eocène moyen du Myanmar Grégoire Métais a, Aung Naing Soe b, Stéphane Ducrocq c,* a Carnegie Museum of Natural History, Section of Vertebrate Paleontology, 4400 Forbes Avenue, Pittsburgh, PA 15213, USA b Department of Geology, Yangon University, Yangon 11422, Myanmar c Laboratoire de Géobiologie, Biochronologie et Paléontologie Humaine, UMR 6046 CNRS, Faculté des Sciences de Poitiers, 40, avenue du recteur-Pineau, 86022 Poitiers cedex, France Received 29 September 2004; accepted 10 May 2005 Available online 20 March 2006 Abstract A new genus and species of tapiromorph, Skopaiolophus burmese nov. gen., nov. sp., is described from the middle Eocene Pondaung For- mation in central Myanmar. This small form displays a striking selenolophodont morphology associated with a mixture of primitive “condylar- thran” dental characters and derived tapiromorph features. Skopaiolophus is here tentatively referred to a group of Asian tapiromorphs unknown so far. The occurrence of such a form in Pondaung suggests that primitive tapiromorphs might have persisted in southeast Asia until the late middle Eocene while they became extinct elsewhere in both Eurasia and North America. © 2006 Elsevier SAS. All rights reserved. Résumé Un nouveau genre et une nouvelle espèce de tapiromorphe, Skopaiolophus burmese nov. gen. nov. sp., sont décrits dans la Formation de Pondaung d’âge fini-éocène moyen, au Myanmar. -
Evolution Des Caractères Crâniens Et Endocrâniens Chez Les Afrotheria (Mammalia) Et Phylogénie Du Groupe Julien Benoit
Evolution des caractères crâniens et endocrâniens chez les Afrotheria (Mammalia) et phylogénie du groupe Julien Benoit To cite this version: Julien Benoit. Evolution des caractères crâniens et endocrâniens chez les Afrotheria (Mammalia) et phylogénie du groupe. Biologie animale. Université Montpellier II - Sciences et Techniques du Languedoc, 2013. Français. NNT : 2013MON20073. tel-01001999 HAL Id: tel-01001999 https://tel.archives-ouvertes.fr/tel-01001999 Submitted on 5 Jun 2014 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. Thèse Pour l’obtention du grade de DOCTEUR DE L’UNIVERSITE MONTPELLIER II Discipline : Paléontologie Formation Doctorale : Paléontologie, Paléobiologie et Phylogénie Ecole Doctorale : Systèmes Intégrés en Biologie, Agronomie, Géosciences, Hydrosciences, Environnement Présentée et soutenue publiquement par Benoit Julien Le 6 Novembre 2013 Titre : Evolution des caractères crâniens et endocrâniens chez les Afrotheria (Mammalia) et phylogénie du groupe Thèse dirigée par Rodolphe Tabuce et Monique Vianey-Liaud Jury Lecturer and Curator, Dr. Asher Robert Rapporteur University Museum of Zoology, Cambridge Directeur de Recherche au CNRS, Dr. Gheerbrant Emmanuel Rapporteur Muséum d’Histoire Naturelle, Paris Professeur, Pr. Tassy Pascal Examinateur Muséum d’Histoire Naturelle, Paris Coordinateur du groupe de Recherche en Paléomammalogie, Dr. -
Early Eocene Fossils Suggest That the Mammalian Order Perissodactyla Originated in India
ARTICLE Received 7 Jul 2014 | Accepted 15 Oct 2014 | Published 20 Nov 2014 DOI: 10.1038/ncomms6570 Early Eocene fossils suggest that the mammalian order Perissodactyla originated in India Kenneth D. Rose1, Luke T. Holbrook2, Rajendra S. Rana3, Kishor Kumar4, Katrina E. Jones1, Heather E. Ahrens1, Pieter Missiaen5, Ashok Sahni6 & Thierry Smith7 Cambaytheres (Cambaytherium, Nakusia and Kalitherium) are recently discovered early Eocene placental mammals from the Indo–Pakistan region. They have been assigned to either Perissodactyla (the clade including horses, tapirs and rhinos, which is a member of the superorder Laurasiatheria) or Anthracobunidae, an obscure family that has been variously considered artiodactyls or perissodactyls, but most recently placed at the base of Proboscidea or of Tethytheria (Proboscidea þ Sirenia, superorder Afrotheria). Here we report new dental, cranial and postcranial fossils of Cambaytherium, from the Cambay Shale Formation, Gujarat, India (B54.5 Myr). These fossils demonstrate that cambaytheres occupy a pivotal position as the sister taxon of Perissodactyla, thereby providing insight on the phylogenetic and biogeographic origin of Perissodactyla. The presence of the sister group of perissodactyls in western India near or before the time of collision suggests that Perissodactyla may have originated on the Indian Plate during its final drift toward Asia. 1 Center for Functional Anatomy & Evolution, Johns Hopkins University School of Medicine, 1830 E. Monument Street, Baltimore, Maryland 21205, USA. 2 Department of Biological Sciences, Rowan University, Glassboro, New Jersey 08028, USA. 3 Department of Geology, H.N.B. Garhwal University, Srinagar 246175, Uttarakhand, India. 4 Wadia Institute of Himalayan Geology, Dehradun 248001, Uttarakhand, India. 5 Research Unit Palaeontology, Ghent University, Krijgslaan 281-S8, B-9000 Ghent, Belgium. -
Knowledge of the Evolution of African Paleogene Mammals
Knowledge of the évolution of African Paleogene mammals Contribution of the Bir El Ater locality (Eocène, Algeria) Rodolphe Tabuce Brigitte Coiffait Philippe-Emmanuel Coiffait Mohamed Mahboubi Jean-Jacques Jaeger 1 1 Introduction: The Early African Paleogene mammals The African fossil record of therians begins with the Early Cretaceous ofthe Middle Atlas (Morocco) (Sigogneau-Russell, 1991); however, the modem mammalian orders appear only during the early Tertiary in North Africa (figure 1A). The Paleocene and Ypresian localities from the Ouarzazate Basin (Morocco) hâve yielded mammalian faunas with possible creodonts, « insectivores » (paleoryctids, todralestids and adapisoriculids) (Gheerbrant, 1992, 1994, 1995), the oldest représentative ofeupri- mates (Sigé et al, 1990) and archaic ungulates (Sudre et al, 1993). Recently, the discovery of Phosphatherium (Proboscidea) in J\) .... Ypresian Early to Mlddla Mlddlalo Lata C> mlcldla BOCena eocena Ialaeocene eocena "III N'Tagourt2 ElKohol GllbZagdou GourLazib Chambl lnTaliclel M'Bodlone Bir el Ater DoralTalha Qaar (Moroc:co) (Algerla) (Algerla) (Algerla) (Tunlala) and (Sanagal) (Algarla) ·Evaporlt e1Sagha lamagullell Unit· (Fayum, (Mali) (LIbye) Egypt) Matatharla Kassarinolherium tunisiansa Creodonta Koholis gen. el sp. Aprarodon stlasansa indet Hyaanodon Carnlvora Glibzagdouis I8balbslsensis Condylarthra Condyfarthra Condylarthra Inda!. Inda!. Artlodaetyla cl.Bolhrio- ganys sp. Proboscldell KhSmsBcornJS Numidotherium Moerilharium Moenlherium Moarilherium 8srytherium 8srythenum buJbosus -
Pickford 2018 Namahyrax Corvus from Black Crow, Sperrgebiet
Additional material of Namahyrax corvus from the Ypresian/Lutetian of Black Crow, Namibia Martin PICKFORD Sorbonne Universités (CR2P, MNHN, CNRS, UPMC - Paris VI) 8, rue Buffon, 75005, Paris, France ([email protected]) Abstract : Three teeth of a small hyracoid were found during the 2017 campaign of acid digestion of blocks of limestone from Black Crow, Namibia. The specimens, a left D1/, half an upper premolar and a right p/1 can be attributed with confidence to Namahyrax corvus , up to now the only hyracoid known from the site. The D1/ is more complete than the broken P1/ in the holotype and yields additional information about the crown morphology of the anterior cheek teeth. The p/1 was not previously known for the species. The three teeth underscore the primitive brachyodont morphology of the teeth. The teeth are somewhat more primitive than the corresponding teeth in Dimaitherium patnaiki from the Fayum, Egypt. Direct comparisons cannot be made with Seggeurius amourensis and Bunohyrax matsumotoi because these tooth positions are unknown in these species, but the shape of the p/1 of Namahyrax corresponds with what would be expected from the p/2 morphology in them. Comparisons with Microhyrax lavocati are difficult to make because not even the p/2 is known in that species, but the simplicity of its p/3 (lack of crescentic cusps) suggests a ground plan for the p/1 that could correspond to that observed in the Black Crow specimen. The new specimens of Namahyrax resolve the uncertainty concerning its familial status, indicating that it belongs to the family Geniohyidae. -
Evolution of Horse
UNIT 11 EVOLUTION OF HORSE Structure____________________________________________________ 11.1 Introduction 11.3 Role of Climate in the Evolution of Horse Expected Learning Outcomes 11.4 Activity 11.2 Evolution of Horse 11.5 Summary Systematic Palaeontology 11.6 Terminal Questions Place and Time of Origin 11.7 References Major Evolutionary Transitions 11.8 Further/Suggested Readings Phylogeny of Horse 11.9 Answers 11.1 INTRODUCTION Vertebrates are a diverse group of organisms ranging from lampreys to human beings. The group includes animals with backbone, such as fishes, amphibians, reptiles, birds and mammals. The dinosaurs that have caught public attention by making their appearance in several films and books too are vertebrates. Vertebrates have a long geological history on the planet Earth beginning more than 500 million years (Myr) ago, starting from the Cambrian to the present. They first appeared in the fossil record during the Cambrian period of the Palaeozoic era. Fishes, amphibians and reptiles were the most dominant groups of vertebrates in the Palaeozoic and Mesozoic eras. In the Mesozoic era, dinosaurs- a group of reptiles, and mammals made their appearance. Dinosaurs had a wide geographic distribution, being reported from all continents and were the largest animals to roam the Earth during the Mesozoic era. The mammals began to diversify only after the demise of dinosaurs at the close of the Mesozoic era at around 66 Myr ago. In the Cenozoic era, mammals rapidly occupied every niche and corner of the globe and therefore, the Cenozoic era is also known as the “Age of Mammals”. Introduction to Palaeontology Block……………………………………………………………………………………………….….............….…........ 3 Mammals of the Cenozoic era belong to three groups: placentals (that give birth to young ones), marsupials (in which an offspring after birth continues to develop within the pouch of the mother) and monotremes (egg laying mammals). -
Reassessment of the Algerian Eocene Hyracoid Microhyrax : Consequences on the Early Diversity and Basal Phylogeny of the Order Hyracoidea (Mammalia)
Reassessment of the Algerian Eocene Hyracoid Microhyrax : consequences on the early diversity and basal phylogeny of the Order Hyracoidea (Mammalia) Autor(en): Tabuce, Rodolphe / Mahboubi, Mohamed / Sudre, Jean Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 94 (2001) Heft 3 PDF erstellt am: 11.10.2021 Persistenter Link: http://doi.org/10.5169/seals-168910 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch 0012-9402/O1/O30537-9 $1.50 + 0.20/0 Eclogae geol. Helv. 94 (2001) 537-545 Birkhäuser Verlag. Basel. 2001 Reassessment of the Algerian Eocene Hyracoid Microhyrax. Consequences on the early diversity and basal phylogeny of the Order Hyracoidea (Mammalia) Rodolphe Tabuce1, Mohamed Mahboubi2 & Jean Sudre3 Keywords: Hyracoidea. -
Furry Folk: Synapsids and Mammals
FURRY FOLK: SYNAPSIDS AND MAMMALS Of all the great transitions between major structural grades within vertebrates, the transition from basal amniotes to basal mammals is represented by the most complete and continuous fossil record, extending from the Middle Pennsylvanian to the Late Triassic and spanning some 75 to 100 million years. —James Hopson, “Synapsid evolution and the radiation of non-eutherian mammals,” 1994 At the very beginning of their history, amniotes split into two lineages, the synapsids and the reptiles. Traditionally, the earliest synapsids have been called the “mammal-like reptiles,” but this is a misnomer. The earliest synapsids had nothing to do with reptiles as the term is normally used (referring to the living reptiles and their extinct relatives). Early synapsids are “reptilian” only in the sense that they initially retained a lot of primitive amniote characters. Part of the reason for the persistence of this archaic usage is the precladistic view that the synapsids are descended from “anapsid” reptiles, so they are also reptiles. In fact, a lot of the “anapsids” of the Carboniferous, such as Hylonomus, which once had been postulated as ancestral to synapsids, are actually derived members of the diapsids (Gauthier, 1994). Furthermore, the earliest reptiles (Westlothiana from the Early Carboniferous) and the earliest synapsids (Protoclepsydrops from the Early Carboniferous and Archaeothyris from the Middle Carboniferous) are equally ancient, showing that their lineages diverged at the beginning of the Carboniferous, rather than synapsids evolving from the “anapsids.” For all these reasons, it is no longer appropriate to use the term “mammal-like reptiles.” If one must use a nontaxonomic term, “protomammals” is a alternative with no misleading phylogenetic implications. -
Evolution and Paleoenvironment of Early Modern Vertebrates During the Paleogene Program and Abstracts
September 10‐13, 2019 Royal Belgian Institute of natural Sciences, Brussels, Belgium International symposium Evolution and Paleoenvironment of Early Modern Vertebrates during the Paleogene Program and abstracts PalEurAfrica Meeting 2019 In the framework of the PalEurAfrica research project (see http://www.paleurafrica.be), we are happy to invite you to the Royal Belgian Institute of Natural Sciences (RBINS) for an international symposium related to the evolution and paleoenvironment of early modern vertebrates during the Paleogene. This allows us to gather specialists who work on macro‐ and micropaleontology, bio‐ and isotope stratigraphy, paleoenvironment, paleogeography, and geology of Paleogene vertebrate bearing sites. This international meeting also celebrates the memory of one of our PalEurAfrica partners, Gregg Gunnell (1954‐2017), who tragically died unexpectedly in the middle of his career, having made significant contributions to our understanding of research on Paleogene vertebrate evolutionary history. Host committee Thierry Smith (Chair) – Royal Belgian Institute of Natural Sciences, Brussels, Belgium Thierry De Putter – Royal Museum for Central Africa, Tervuren, Belgium Stephen Louwye – Universiteit Gent, Gent, Belgium Johan Yans – Université de Namur, Namur, Belgium Matthew Borths – Duke University Lemur center, Durham, NC, USA Nancy Stevens – Ohio University, Athens, OH, USA Scientific committee Massimo Delfino – Università di Torino, Torino, Italy Gilles Escarguel – Université de Lyon, Lyon, France Annelise Folie – Royal Belgian Institute of Natural Sciences, Brussels, Belgium Emmanuel Gheerbrant – Museum national d’Histoire Naturelle, Paris, France Jason Head – University of Cambridge, Cambridge, UK Gerald Mayr – Senckenberg Forschungsinstitut und Naturmuseum, Frankfurt, Germany Florias Mees – Royal Museum for Central Africa, Tervuren, Belgium Ellen R. Miller – Wake Forest University, Winston‐Salem, NC, USA Adán Pérez‐García – Universidad Nacional de Educación a Distancia, Madrid, Spain Rajendra Singh Rana – H.N.B.