Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology

Total Page:16

File Type:pdf, Size:1020Kb

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. gen. and comb. (Hyaenodontidae, Creodonta) and polyphyly of the Hyaenodontinae 102 Abstract 103 Introduction 103 Materials and Methods 104 Abbreviations 106 Systematic Paleontology 106 Description of new material 108 Skull and Dentition 108 v Axial Skeleton 112 Forelimb 113 Hindlimb 116 The Phylogenetic Position of Gazinocyon 121 Methods and Materials 125 Results 126 Discussion 131 Pterodontinae new subfamily 133 Hyaenodontinae Trouessart, 1885: revised description 135 Conclusion 136 Acknowledgments 138 Bibliography 139 Table 4.1: Measurements of the dentition of Gazinocyon vulpeculus 146 Table 4.2: List of species used in the determination of generic character states 148 Appendix 4.1: Characters Used in the phylogenetic analysis 151 Appendix 4.2: Data matrix 155 Figures 156 Chapter Five: The Basicranial Morphology of Hyaenodontidae (Creodonta, Mammalia) and its Phylogenetic Implications 166 Introduction 167 Abbreviations 169 Material and Methods 169 Development and General Morphology of the Basicranium 170 The Basicranium of Hyaenodon 171 The Basicranium of Tritemnodon 179 Morphological Variation in Hyaenodontid Ear Regions 182 vi Phylogenetic Analysis of Hyaenodontid Basicranial Characters 188 Conclusions 190 Acknowledgments 191 Bibliography 192 Table 5.1. Hyaenodontid species with preserved basicranial regions 199 Table 5.2: List of Basicranial Characters used in the phylogenetic analysis 201 Table 5.3: Data matrix used in the phylogenetic analysis 202 Figures 203 Chapter Six: Afterword: Some speculations on mammalian molar evolution in relation to development 212 Introduction 213 Sizing up the Situation 217 Mammalian Molar Crown Morphogenesis 219 Methods of Controlling Molar Morphogenesis 222 Complexity in Mammalian Molar Crown Patterns 226 Function and its Constraint in Mammalian Molar Evolution 230 An Example from Creodonta: The Evolution of Apterodon 231 Two Scenarios for Molar Evolution 242 Testing the Hypothesis 243 Conclusion 245 Acknowledgments 246 Bibliography 246 Figures 256 Appendix: Currently Recognized Species of Creodonta 268 Proviverrinae 269 Koholiinae 274 Hyaenodontinae 274 vii Pterodontinae 277 Other Hyaenodontine-like Creodonts 279 Limnocyoninae 280 Machaeroidinae 280 Oxyaeninae 281 Ambloctoninae 282 viii INTRODUCTION Systematics is a wide ranging field. It includes the naming of species, genera, and other taxonomic groups, the identification and interpretation of organisms and their remains, and analyses of the evolutionary relationships among groups. In all of these roles it touches many sub-disciplines of biology and geology. This dissertation is an exploration of all of these aspects of systematics. It is arranged as six separate papers, each of which deals with a different aspect. All of the papers are in some way connected with the systematics of the extinct Eutherian group Creodonta. The dissertation includes specific work on alpha-level systematics, legalistic nomenclature, phylogenetic systematics, and the history and philosophy of constructing classifications from an evolutionary or other "natural" framework. It also expands beyond the limits of pure systematics into other realms that systematics is only the necessary base upon which other work is based. These include biostratigraphy, functional morphology, and evolutionary theory. All of these aspects of systematics are explored through work on hyaenodontid creodonts. Creodonta is an extinct group of eutherian mammals. As currently delimited, the first creodonts appeared in the mid to late Paleocene and the last died in the latest Miocene. They lived in North America, Asia, Europe, and Africa and played the role of the dominant carnivore in terrestrial ecosystems on the continents for the first half of the Tertiary. They are a very diverse group with more than 200 species currently recognized (Appendix I). Unfortunately, they are very poorly studied. They were originally recognized as a distinct group by Edward Drinker Cope in 1874, and were studied intensively by him in the late 19th century and by W.D. Matthew in the early 20th. After Matthew, though, they have been given little treatment as phylogenetic interest shifted to earlier Mesozoic mammals. Creodonts are morphologically very primitive for eutherian ix mammals. They retain many primitive features of the dentition and skull of the earliest placentals. For this reason, they may prove very useful in solving the puzzle of deep branching within Eutheria. Before that, though, more must be known about variation and relationships within Creodonta. This dissertation goes a long way toward that end. The first chapter of the dissertation forms a backdrop for the successive chapters. It is an exploration of the historical relationship between classification and natural order. It concentrates on mammalian and creodont classification. The purpose of the second chapter is to update the identifications of the hyaenodontids from the Eocene Four Mile Fauna and to describe and illustrate material that is used in later chapters. The third chapter straightens out some confusion over the nomenclature of several Eocene Eurasian genera of hyaenodontids that are included in the phylogenetic analysis of the fourth chapter. The fourth chapter has the dual purpose of describing previously undescribed hyaenodontid postcranial material and using that information to form the basis of a phylogenetic analysis of the Hyaenodontidae. The fifth chapter is similar to the fourth, but deals with basicranial morphology of hyaenodontids. The final chapter is a synthesis of ideas from paleontology, systematics, embryology, and evolutionary theory to explain the multiple evolution of quadritubercular molars in mammalian history. Together these chapters represent many of the various manifestations of systematics mentioned above. x ACKNOWLEDGMENTS I would first like to thank my committee for reading and commenting on this dissertation. They spent many hours and their work improved it dramatically. I would also like to thank them for the many letters they have written for me and for being very supportive and easy to work with. I would like to thank Dr. C.B. Wood for first teaching me about mammalian molar function. I would like to thank Dr. Brigitte Lange-Badré for guidance in working with creodonts. Dr. Elmar Heizmann was kind enough to sponsor me for a Deutscher Akademischer Austauschdienst scholarship and as extremely helpful and hospitable to me during my stay in Germany. Dr. David Lindberg has also been very helpful and has provided many interesting discussions about much of the work presented in this dissertation. The late Dr. Allan Wilson inspired me to think about evolution and morphology in a new way. Dr. Tim Rowe has continually maintained an interest in my career and he and Dr. Chad Oliver receive credit for sparking my interest in this field. Wendy Olson, Michelle Koo, Francis Villablanca, Maria Orive, John Wakely, Jessica Theodor, Dan Garcia, Nancy Simmons, Anne Weil, Chris Bell, Mike Russell, Ken Warheit, Luo, Bob Dundas, and Chris Meyer have all been both helpful as fellow graduate students and made life more interesting. I would also like to especially thank Tina Rouse, Marlene Martinez, and Gayle Nelms for their love and support as founding members of the Dave Polly Fan Club. I would like to thank Jessica Theodor, editor of PaleoBios, and Brigitte Lange- Badré, my co-author on Chapter Three, for their permission to include the previously published and
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Artiodactyla and Perissodactyla (Mammalia) from the Early-Middle Eocene Kuldana Formation of Kohat (Pakistan)
    CO"uTK1BL 11015 FKOLI IHt \lC5tLL1 OF I' ALEO\ IOLOG1 THE UNIVERSITY OF IVICHIGAN VOI 77 Lo 10 p 717-37.1 October 33 1987 ARTIODACTYLA AND PERISSODACTYLA (MAMMALIA) FROM THE EARLY-MIDDLE EOCENE KULDANA FORMATION OF KOHAT (PAKISTAN) BY J. G. M. THEWISSEN. P. D. GINGERICH and D. E. RUSSELL MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Charles B. Beck, Director Jennifer A. Kitchell, Editor This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate issues may also be obtained by request. Correspond- ence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48109. VOLS. II-XXVII. Parts of volumes may be obtained if available. Price lists are available upon inquiry. I ARTIODACTI L .-I A\D PERISSODACTYL4 (kl.iihlhlAL1A) FROM THE EARLY-h1IDDLE EOCEUE KCLD..I\4 FORMATIO\ OF KOHAT (PAKISTAY) J. G. M. THEWISSEN. P. D. GINGERICH AND D. E. RUSSELL Ah.strcict.-Chorlakki. yielding approximately 400 specimens (mostly isolated teeth and bone fragments). is one of four major early-to-middle Eocene niammal localities on the Indo-Pakistan subcontinent. On the basis of ung~~latesclescribed in this paper we consider the Chorlakki fauna to be younger than that from Barbora Banda.
    [Show full text]
  • First Nimravid Skull from Asia Alexander Averianov1,2, Ekaterina Obraztsova3, Igor Danilov1,2, Pavel Skutschas3 & Jianhua Jin1
    www.nature.com/scientificreports OPEN First nimravid skull from Asia Alexander Averianov1,2, Ekaterina Obraztsova3, Igor Danilov1,2, Pavel Skutschas3 & Jianhua Jin1 Maofelis cantonensis gen. and sp. nov. is described based on a complete cranium from the middle- upper Eocene Youganwo Formation of Maoming Basin, Guangdong Province, China. The new taxon Received: 08 September 2015 has characters diagnostic for Nimravidae such as a short cat-like skull, short palate, ventral surface of petrosal dorsal to that of basioccipital, serrations on the distal carina of canine, reduced anterior Accepted: 21 April 2016 premolars, and absence of posterior molars (M2-3). It is plesiomorphic nimravid taxon similar to Published: 10 May 2016 Nimravidae indet. from Quercy (France) in having the glenoid pedicle and mastoid process without ventral projections, a planar basicranium in which the lateral rim is not ventrally buttressed, and P1 present. The upper canine is less flattened than in other Nimravidae.Maofelis cantonensis gen. and sp. nov. exemplifies the earliest stage of development of sabertooth specialization characteristic of Nimravidae. This taxon, together with other middle-late Eocene nimravid records in South Asia, suggests origin and initial diversification of Nimravidae in Asia. We propose that this group dispersed to North America in the late Eocene and to Europe in the early Oligocene. The subsequent Oligocene diversification of Nimravidae took place in North America and Europe, while in Asia this group declined in the Oligocene, likely because of the earlier development of open habitats on that continent. Nimravids are cat-like hypercarnivores that developed saber-tooth morphology early in the Cenozoic and were top predators in the late Eocene – late Oligocene mammal communities of the Northern Hemisphere1–3.
    [Show full text]
  • Supplemental File 1: Addressing Claims of “Zombie” Lineages on Phillips’ (2016) Timetree
    Supplemental File 1: Addressing claims of “zombie” lineages on Phillips’ (2016) timetree The soft explosive model of placental mammal evolution Matthew J. Phillips*,1 and Carmelo Fruciano1 1School of Earth, Environmental and Biological Sciences, Queensland University of Technology, Brisbane, Australia *Corresponding author: E-mail: [email protected] Contents Addressing claims of “zombie” lineages on Phillips’ (2016) timetree ................................................... 1 Incorrect or poorly supported fossil placements ................................................................................. 1 Figure S1 ............................................................................................................................................ 4 Table S1 .............................................................................................................................................. 6 References .............................................................................................................................................. 7 Addressing claims of “zombie lineages” on Phillips’ (2016) timetree Phillips [1] found extreme divergence underestimation among large, long-lived taxa that were not calibrated, and argued that calibrating these taxa instead shifted the impact of the underlying rate model misspecification to inflating dates deeper in the tree. To avoid this “error-shift inflation”, Phillips [1] first inferred divergences with dos Reis et al.’s [2] calibrations, most of which are set among taxa
    [Show full text]
  • Origin and Beyond
    EVOLUTION ORIGIN ANDBEYOND Gould, who alerted him to the fact the Galapagos finches ORIGIN AND BEYOND were distinct but closely related species. Darwin investigated ALFRED RUSSEL WALLACE (1823–1913) the breeding and artificial selection of domesticated animals, and learned about species, time, and the fossil record from despite the inspiration and wealth of data he had gathered during his years aboard the Alfred Russel Wallace was a school teacher and naturalist who gave up teaching the anatomist Richard Owen, who had worked on many of to earn his living as a professional collector of exotic plants and animals from beagle, darwin took many years to formulate his theory and ready it for publication – Darwin’s vertebrate specimens and, in 1842, had “invented” the tropics. He collected extensively in South America, and from 1854 in the so long, in fact, that he was almost beaten to publication. nevertheless, when it dinosaurs as a separate category of reptiles. islands of the Malay archipelago. From these experiences, Wallace realized By 1842, Darwin’s evolutionary ideas were sufficiently emerged, darwin’s work had a profound effect. that species exist in variant advanced for him to produce a 35-page sketch and, by forms and that changes in 1844, a 250-page synthesis, a copy of which he sent in 1847 the environment could lead During a long life, Charles After his five-year round the world voyage, Darwin arrived Darwin saw himself largely as a geologist, and published to the botanist, Joseph Dalton Hooker. This trusted friend to the loss of any ill-adapted Darwin wrote numerous back at the family home in Shrewsbury on 5 October 1836.
    [Show full text]
  • Title a Preliminary Report on Carnivorous Mammals From
    A preliminary report on carnivorous mammals from Pondaung Title fauna Author(s) Egi, Naoko; Tsubamoto, Takehisa Citation Asian paleoprimatology (2000), 1: 103-114 Issue Date 2000 URL http://hdl.handle.net/2433/199738 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University Asian Paleoprimatology, vol. 1:103-114 (2000) Kyoto University Primate Research Institute A preliminary rer r rt on canlivorous mammals from Pondaung fauna Naoko Egil and Takehisa Tsubamoto2 'Departmentof Geology, NationalScience Museum of Japan, Tokyo 169-0073, Japan 'Departmentof Geologyand Mineralogy , GraduateSchool of Science,Kyoto University, Kyoto606-8502, Japan Abstract Somecarnivore materials have been discovered from the PondaungFormation in cen- tralMyanmar recently. The materials are separableinto at leasttwo genera, both of which are hyaenodontidcreodonts. One of themis a medium-sizedproviverrine. Collected parts in- cludea maxilla,lower molar fragmen'ts, and some postcranial fragments. It showssome distinctivedental characters such as smallprotocone lobe on P4, anterolingually-placed proto- coneand posterolingually-placed metacone relative to paraconeon M' andM2, and relatively large 1\43 with a veryreduced metaconid. The otheris a muchlarger form. A maxillary fragmentwith a M' anda mandibularfraarneliL with P2 to M2have been found for this form. possessessome similarities to Pterodon,but observationson morecomplete specimens all!: comparisonswith other Pterodon-like hyaenodontids from Asia are necessaryto settlea sys- tematicassignment of thisform. The two hyaenodontidsare the onlyknown mammalian predatorsfrom Pondaung fauna (latest Middle Eocene) based on the currentknowledge. Since early in this century, many vertebrate fossils have been collected from the Pondaung Formation (latest Middle Eocene; central Myanmar). Mammals known from the Pondaung fauna belong to a variety of taxa: Artiodactyla, Creodonta, Perissodactyla, Primates, and Rodentia (Takai et al., 1999).
    [Show full text]
  • 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.
    [Show full text]
  • (Mammalia) from the French Locality of Aumelas (Hérault), with Possible New Representatives from the Late Ypresian
    geodiversitas 2020 42 13 né – Car ig ni e vo P r e e s n a o f h t p h é e t S C l e a n i r o o z o m i e c – M 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 : Made from the Figures of the article. Geodiversitas est indexé dans / Geodiversitas is indexed in: – Science
    [Show full text]
  • Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
    Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter­ ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran­ gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S.
    [Show full text]
  • Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field
    Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field June 12, 2007 ABSTRACT This is compilation of a technical analysis of existing paleontological data and a limited, selective paleontological field survey of the geologic bedrock formations that will be impacted on Federal lands by construction associated with energy development in the Jonah Field, Sublette County, Wyoming. The field survey was done on approximately 20% of the field, primarily where good bedrock was exposed or where there were existing, debris piles from recent construction. Some potentially rich areas were inaccessible due to biological restrictions. Heavily vegetated areas were not examined. All locality data are compiled in the separate confidential appendix D. Uinta Paleontological Associates Inc. was contracted to do this work through EnCana Oil & Gas Inc. In addition BP and Ultra Resources are partners in this project as they also have holdings in the Jonah Field. For this project, we reviewed a variety of geologic maps for the area (approximately 47 sections); none of maps have a scale better than 1:100,000. The Wyoming 1:500,000 geology map (Love and Christiansen, 1985) reveals two Eocene geologic formations with four members mapped within or near the Jonah Field (Wasatch – Alkali Creek and Main Body; Green River – Laney and Wilkins Peak members). In addition, Winterfeld’s 1997 paleontology report for the proposed Jonah Field II Project was reviewed carefully. After considerable review of the literature and museum data, it became obvious that the portion of the mapped Alkali Creek Member in the Jonah Field is probably misinterpreted.
    [Show full text]
  • Chiroptera: Vespertilionidae)
    Zoologischer Anzeiger 258 (2015) 92–98 Contents lists available at ScienceDirect Zoologischer Anzeiger jou rnal homepage: www.elsevier.com/locate/jcz Penile histomorphology of the neotropical bat Eptesicus furinalis (Chiroptera: Vespertilionidae) a a b a,∗ Manuela T. Comelis , Larissa M. Bueno , Rejane M. Góes , Eliana Morielle-Versute a Department of Zoology and Botany, São Paulo State University, UNESP, Campus São José do Rio Preto, São Paulo 15054-000, Brazil b Department of Biology, São Paulo State University, UNESP, Campus São José do Rio Preto, São Paulo 15054-000, Brazil a r a t i b s c t l e i n f o r a c t Article history: External and internal penile morphologies have evolved rapidly and divergently in many mammalian Received 19 January 2015 orders and are extremely useful for taxonomic studies, particularly in the recovery of phylogenetic rela- Received in revised form 3 August 2015 tionships. Eptesicus furinalis, a Vespertilionid bat, belongs to a taxon in which species recognition can be Accepted 6 August 2015 difficult when only traditional features are employed. Therefore, any feature that may contribute to the Available online 11 August 2015 more accurate characterization of this taxon is relevant. In this study, we describe the histomorphology Corresponding Editor: Alexander Kupfer. of the penis and baculum of this species after analyzing serial transverse sections and three-dimensional (3D) reconstructions. The glans penis was small with no epidermal projections and had an inverted Keywords: Y-shaped baculum for most of its length. Internally, the penis contained three erectile tissues: corpus cav- Glans penis Baculum ernosum, accessory cavernous tissue, and corpus spongiosum around the urethra.
    [Show full text]