The Myth of the Hippo-Like Anthracothere: the Eternal Problem of Homology and Convergence
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11 Sualdea Et Al.Indd
SPANISH J OURNAL OF P ALAEONTOLOGY 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid) Lucía R. SUALDEA 1* , Adriana OLIVER 2, Fernando BLANCO 3, Iris MENÉNDEZ 1,4 , Manuel HERNÁNDEZ FERNÁNDEZ1,4, Laura DOMINGO 1,5 & Ana Rosa GÓMEZ CANO 6,7 1 Departamento de Geodinámica, Estratigrafía y Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, C/ José Antonio Novais 12, 28040, Madrid; [email protected], [email protected], [email protected], [email protected]. 2 Geosfera, C/ Madres de la Plaza de Mayo, 2, 28523, Rivas-Vaciamadrid, Madrid; [email protected] 3 Museum für Naturkunde, Leibniz-Institut für Evolutions und Biodiversitätsforschung, Invalidenstraße 43, 10115, Berlin, Germany; [email protected] 4 Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIC, UCM), C/ Dr. Severo Ochoa, 7, 28040, Madrid 5 Earth and Planetary Sciences Department. University of California Santa Cruz, 1156 High Street, 95064, Santa Cruz, USA 6 Transmitting Science, C/ Gardenia 2, Piera, 08784, Barcelona. 7 Institut Català de Paleontologia Miquel Crusafont, Edifi ci ICP, Campus de la UAB s/n, 08193, Cerdanyola del Vallès; [email protected] * Corresponding author Sualdea, L.R., Oliver, A., Blanco, F., Menéndez, I., Hernández Fernández, M., Domingo, L. & Gómez Cano, A.R. 2019. 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid). [20 años en el campus: actualización de la valoración -
JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
South Dakota to Nebraska
Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska. -
New Postcranial Specimens of the Anthracotheriidae (Mammalia; Artiodactyla) from the Paleogene of Fayum Depression, Egypt
International Journal of Scientific Engineering and Applied Science (IJSEAS) - Volume-1, Issue-8,November 2015 ISSN: 2395-3470 www.ijseas.com New postcranial specimens of the Anthracotheriidae (Mammalia; Artiodactyla) from the Paleogene of Fayum Depression, Egypt 1 2 Afifi H. Sileem , Abdel Galil A Hewaidy 1 Vertebrate paleontology section, Cairo Geological Museum, Cairo, Egypt, [email protected] 2Department of Geology, Faculty of Science, Al-Azhar University, Egypt, <[email protected]> Abstract: The fossiliferous deposits exposed north of Birket Qarun in the Fayum Depression, northeast Egypt, have produced a remarkable collection of fossil mammals from localities that range in age from earliest late Eocene (~37 Ma) to latest early Oligocene (~29 Ma). Anthracotheriidae are among the most common mammals that are preserved in these deposits. Here we describe a new fossil specimens of the Anthracotheriidae (Mammalia, Artiodactyla) discovered in the Jebel Qatrani Formation of Fayum. The specimens consist of a seven astragalus, which is referable to Bothriogenys sp. from the formation. The specimens Bothriogenys sp. show a higher degree of size variation and some feature suggest that the anthracothere are not closely related to Hippopotamus. Key word: anthracothere, Bothriogenys; astragalus; Fayum; Early Oligocene. 376 International Journal of Scientific Engineering and Applied Science (IJSEAS) - Volume-1, Issue-8,November 2015 ISSN: 2395-3470 www.ijseas.com Introduction: The fossiliferous sedimentary deposits exposed north of Birket (lake) Qarun in the Fayum Depression (Fig.1), northeast Egypt, have produced a remarkable collection of a wide variety of fish, amphibian, reptile, bird and mammal taxa (e.g. Andrews, 1906; Simons and Rasmussen, 1990; Murray et al. -
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. -
Hoganson, J.W., 2009. Corridor of Time Prehistoric Life of North
Corridor of Time Prehistoric Life of North Dakota Exhibit at the North Dakota Heritage Center Completed by John W. Hoganson Introduction In 1989, legislation was passed that directed the North Dakota and a laboratory specialist, a laboratory for preparation of Geological Survey to establish a public repository for North fossils, and a fossil storage area. The NDGS paleontology staff, Dakota fossils. Shortly thereafter, the Geological Survey signed now housed at the Heritage Center, consists of John Hoganson, a Memorandum of Agreement with the State Historical Society State Paleontologist, and paleontologists Jeff Person and Becky of North Dakota which provided space in the North Dakota Gould. This arrangement has allowed the Geological Survey, in Heritage Center for development of this North Dakota State collaboration with the State Historical Society of North Dakota, Fossil Collection, including offices for the curator of the collection to create prehistoric life of North Dakota exhibits at the Heritage Center and displays of North Dakota fossils at over 20 other museums and interpretive centers around the state. The first of the Heritage Center prehistoric life exhibits was the restoration of the Highgate Mastodon skeleton in the First People exhibit area (fig. 1). Mastodons were huge, elephant- like mammals that roamed North America at the end of the last Ice Age about 11,000 years ago. This exhibit was completed in 1992 and was the first restored skeleton of a prehistoric animal ever displayed in North Dakota. The mastodon exhibit was, and still is, a major attraction in the Heritage Center. Because of its popularity, it was decided that additional prehistoric life displays should be included in the Heritage Center exhibit plans. -
Chapter 1 - Introduction
EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed. -
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology by Paul David Polly B.A. (University of Texas at Austin) 1987 A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Paleontology in the GRADUATE DIVISION of the UNIVERSITY of CALIFORNIA at BERKELEY Committee in charge: Professor William A. Clemens, Chair Professor Kevin Padian Professor James L. Patton Professor F. Clark Howell 1993 Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology © 1993 by Paul David Polly To P. Reid Hamilton, in memory. iii TABLE OF CONTENTS Introduction ix Acknowledgments xi Chapter One--Revolution and Evolution in Taxonomy: Mammalian Classification Before and After Darwin 1 Introduction 2 The Beginning of Modern Taxonomy: Linnaeus and his Predecessors 5 Cuvier's Classification 10 Owen's Classification 18 Post-Darwinian Taxonomy: Revolution and Evolution in Classification 24 Kovalevskii's Classification 25 Huxley's Classification 28 Cope's Classification 33 Early 20th Century Taxonomy 42 Simpson and the Evolutionary Synthesis 46 A Box Model of Classification 48 The Content of Simpson's 1945 Classification 50 Conclusion 52 Acknowledgments 56 Bibliography 56 Figures 69 Chapter Two: Hyaenodontidae (Creodonta, Mammalia) from the Early Eocene Four Mile Fauna and Their Biostratigraphic Implications 78 Abstract 79 Introduction 79 Materials and Methods 80 iv Systematic Paleontology 80 The Four Mile Fauna and Wasatchian Biostratigraphic Zonation 84 Conclusion 86 Acknowledgments 86 Bibliography 86 Figures 87 Chapter Three: A New Genus Eurotherium (Creodonta, Mammalia) in Reference to Taxonomic Problems with Some Eocene Hyaenodontids from Eurasia (With B. Lange-Badré) 89 Résumé 90 Abstract 90 Version française abrégéé 90 Introduction 93 Acknowledgments 96 Bibliography 96 Table 3.1: Original and Current Usages of Genera and Species 99 Table 3.2: Species Currently Included in Genera Discussed in Text 101 Chapter Four: The skeleton of Gazinocyon vulpeculus n. -
The Eternal Problem of Homology and Convergence
HYPOTHESES OF HIPPOPOTAMID ORIGINS 31 THE MYTH OF THE HIPPO-LIKE ANTHRACOTHERE: THE ETERNAL PROBLEM OF HOMOLOGY AND CONVERGENCE Martin PICKFORD Collège de France, and Département Histoire de la Terre, UMR 5143 du CNRS, Case postale 38, 57 rue Cuvier, 75005, Paris. e-mail: [email protected] Pickford, M. 2008. The myth of the hippo-like anthracothere: The eternal problem of homology and convergence. [El mito de la similitud entre antracoterios e hipopótamos: el eterno problema entre homología y convergencia.] Revista Española de Paleontología, 23 (1), 31-90. ISSN 0213-6937. ABSTRACT The notion that anthracotheres had hippo-like body proportions, locomotion and lifestyles has been in the lit- erature for so long, and has been repeated so many times, that it has taken on the aura of unquestionable truth. However, right from the beginning of studies into hippo-anthracothere relationships over a century and a half ago, observations were made that revealed the existence of fundamental differences in dental, cranial and post- cranial anatomy in the two groups. From 1836 to 1991 two skeletal characters (a descending plate at the angle of the mandible, and raised orbits) have overshadowed all others in suggesting close relationships between hippos and a single anthracothere genus (Merycopotamus) later to be joined by a second genus, Libycosaurus, in 1991 for the descending angle, and 2003 for the raised orbits (Lihoreau, 2003; Pickford, 1991). Close examination of these structures reveals that they are not homologous in the two groups, yet they have played an inordinately stubborn role in interpretations of the relationships between them, featuring in papers as recently as 2005. -
GEOL 204 the Fossil Record Spring 2020 Section 0109 Luke Buczynski, Eamon, Doolan, Emmy Hudak, and Shutian Wang
ENTELODONT: The Hellacious Pigs of the Cenozoic GEOL 204 The Fossil Record Spring 2020 Section 0109 Luke Buczynski, Eamon, Doolan, Emmy Hudak, and Shutian Wang Entelodont Overview: From the family Entelodontidae, these omnivorous mammals had a wide geographic variety, as seen in image B. They first inhabited Mongolia then spread into Eurasia and North America, while in North America they preferred flood plains and woodlands. Entelodont were fairly aggressive and would fight with their own kind, using their strong jaws and large heads. They survived from the middle of Eocene to the middle of Miocene. Size and Diet: Skull Features: Figure D shows one of the largest Entelodont, Daedon, compared to an As seen on Figure C, the skull of the Entelodont is massive. They all 1.8 meter tall human, illustrating how immense they really were. contained large Neural Spines, most likely to hold up their huge head, Entelodont weighed from 150 kg on the small size, up to 900 kg (330 to which in turn created a hump. Entelodont contained a pretty small 2,000 pounds) and 1 to 2 meters in height. They had teeth that made them brain, but large olfactory lobes, giving them an acute sense of smell. capable of consuming meat, but the overall structure and wear on the the They held sturdy canines, long incisors, sharp serrated premolars, and suggest the consumption of plant matter as well. Although these large blunt square molars (a sign of omnivory), all of which were covered in a animals might not look it, their limbs were fully terrestrial and adept for very thick layer of enamel. -
Issn: 2250-0588 Fossil Mammals
IJREISS Volume 2, Issue 8 (August 2012) ISSN: 2250-0588 FOSSIL MAMMALS (RHINOCEROTIDS, GIRAFFIDS, BOVIDS) FROM THE MIOCENE ROCKS OF DHOK BUN AMEER KHATOON, DISTRICT CHAKWAL, PUNJAB, PAKISTAN 1Khizar Samiullah* 1Muhammad Akhtar, 2Muhammad A. Khan and 3Abdul Ghaffar 1Zoology department, Quaid-e-Azam campus, Punjab University, Lahore, Punjab, Pakistan 2Zoology Department, GC University, Faisalabad, Punjab, Pakistan 3Department of Meteorology, COMSATS Institute of Information Technology (CIIT), Islamabad ABSTRACT Fossil site Dhok Bun Ameer Khatoon (32o 47' 26.4" N, 72° 55' 35.7" E) yielded a significant amount of mammalian assemblage including two families of even-toed fossil mammal (Giraffidae, and Bovidae) and one family of odd-toed (Rhinocerotidae) of the Late Miocene (Samiullah, 2011). This newly discovered site has well exposed Chinji and Nagri formation and has dated approximately 14.2-9.5 Ma. This age agrees with the divergence of different mammalian genera. Sedimentological evidence of the site supports that this is deposited in locustrine or fluvial environment, as Chinji formation is composed primarily of mud-stone while the Nagri formation is sand dominated. Palaeoenvironmental data indicates that Miocene climate of Pakistan was probably be monsoonal as there is now a days. Mostly the genera recovered from this site resemble with the overlying younger Dhok Pathan formation of the Siwaliks while the size variation in dentition is taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct this study at this specific site to add additional information in the field of Palaeontology. A detailed study of fossils mammals found in Miocene rocks exposed at Dhok Bun Ameer Khatoon was carried out. -
Migration of Organisms Climate • Geography • Ecology Ashraf M
Ashraf M.T. Elewa Migration of Organisms Climate • Geography • Ecology Ashraf M. T. Elewa (Editor) Migration of Organisms Climate • Geography • Ecology With 67 Figures 123 Dr. Ashraf M. T. Elewa Professor Minia University Faculty of Science Geology Department Egypt E-mail: [email protected] Library of Congress Control Number: 2005927792 ISBN-10 3-540-26603-8 Springer Berlin Heidelberg New York ISBN-13 978-3-540-26603-7 Springer Berlin Heidelberg New York This work is subject to copyright. All rights are reserved, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitations, broadcasting, reproduction on microfilm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable to prosecution under the German Copyright Law. Springer is a part of Springer Science+Business Media springeronline.com © Springer-Verlag Berlin Heidelberg 2005 Printed in The Netherlands The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. Cover design: Erich Kirchner Production: Luisa Tonarelli Typesetting: Camera-ready by the editor Printed on acid-free paper 30/2132/LT – 5 4 3 2 1 0 Dedication This book is dedicated to all people who Believe in One God Believe in Peace Believe in Migration in the Way of God To my father who died on Sunday, the 10th of April, 2005 Foreword P.