Evidence for a Grooming Claw in a North American Adapiform Primate: Implications for Anthropoid Origins
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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. -
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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
A New Mammalian Fauna from the Earliest Eocene (Ilerdian) of the Corbie`Res (Southern France): Palaeobiogeographical Implications
Swiss J Geosci (2012) 105:417–434 DOI 10.1007/s00015-012-0113-5 A new mammalian fauna from the earliest Eocene (Ilerdian) of the Corbie`res (Southern France): palaeobiogeographical implications Bernard Marandat • Sylvain Adnet • Laurent Marivaux • Alain Martinez • Monique Vianey-Liaud • Rodolphe Tabuce Received: 27 April 2012 / Accepted: 19 September 2012 / Published online: 4 November 2012 Ó Swiss Geological Society 2012 Abstract A new mammal fauna from the earliest Eocene Keywords Ypresian Á Europe Á Mammals Á of Le Clot (Corbie`res, Southern France) is described. Some Multituberculates Á Palaeoclimate Á Palaeobiogeography taxa identified there, such as Corbarimys hottingeri and Paschatherium plaziati, allow a correlation with the pre- viously described Corbie`res fauna of Fordones. Moreover, 1 Introduction the presence at Le Clot of Lessnessina praecipuus, which is defined in Palette (Provence, Southern France) allows The beginning of the Eocene is characterized by two major correlating both localities. All three of these localities are phenomena: the warming event known as the Paleocene referred to the MP7 reference level, even if a direct cor- Eocene thermal maximum (PETM) (Stott et al. 1996), relation with the type locality of MP7 (Dormaal, Belgium) which likely triggered the second one: the mammalian is not ascertained. A Southern Europe biochronological dispersal event (MDE) (Beard and Dawson 1999; Hooker sequence is proposed for the beginning of the Eocene: 2000). This MDE is a critical event in the history of Silveirinha, Fordones/Palette/Le Clot, Rians/Fournes. The mammals as it corresponds to both the origin and dispersal diagnosis of a new species of a neoplagiaulacid multitu- of several modern mammalian orders (Perissodactyla, berculate (?Ectypodus riansensis nov. -
SMC 136 Gazin 1958 1 1-112.Pdf
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 136, NUMBER 1 Cftarlesi 3B, anb JKarp "^aux OTalcott 3^es(earcf) Jf unb A REVIEW OF THE MIDDLE AND UPPER EOCENE PRIMATES OF NORTH AMERICA (With 14 Plates) By C. LEWIS GAZIN Curator, Division of Vertebrate Paleontology United States National Museum Smithsonian Institution (Publication 4340) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JULY 7, 1958 THE LORD BALTIMORE PRESS, INC. BALTIMORE, MD., U. S. A. CONTENTS Page Introduction i Acknowledgments 2 History of investigation 4 Geographic and geologic occurrence 14 Environment I7 Revision of certain lower Eocene primates and description of three new upper Wasatchian genera 24 Classification of middle and upper Eocene forms 30 Systematic revision of middle and upper Eocene primates 31 Notharctidae 31 Comparison of the skulls of Notharctus and Smilodectcs z:^ Omomyidae 47 Anaptomorphidae 7Z Apatemyidae 86 Summary of relationships of North American fossil primates 91 Discussion of platyrrhine relationships 98 References 100 Explanation of plates 108 ILLUSTRATIONS Plates (All plates follow page 112) 1. Notharctus and Smilodectes from the Bridger middle Eocene. 2. Notharctus and Smilodectes from the Bridger middle Eocene. 3. Notharctus and Smilodectcs from the Bridger middle Eocene. 4. Notharctus and Hemiacodon from the Bridger middle Eocene. 5. Notharctus and Smilodectcs from the Bridger middle Eocene. 6. Omomys from the middle and lower Eocene. 7. Omomys from the middle and lower Eocene. 8. Hemiacodon from the Bridger middle Eocene. 9. Washakius from the Bridger middle Eocene. 10. Anaptomorphus and Uintanius from the Bridger middle Eocene. 11. Trogolemur, Uintasorex, and Apatcmys from the Bridger middle Eocene. 12. Apatemys from the Bridger middle Eocene. -
Proceedings of the United States National Museum
PALEOCENE PRIMATES OF THE FORT UNION, WITH DIS- CUSSION OF RELATIONSHIPS OF EOCENE PRIMATES. By James Williams Gidley, Assistant Curator, United States National Museum. INTRODUCTION. The first important contribution to the knowledge of Fort Union mammalian life was furnished by Dr. Earl Douglass and was based on a small lot of fragmentary material collected by him in the au- tumn of 1901 from a locality in Sweet Grass County, Montana, about 25 miles northeast of Bigtimber.* The fauna described by Douglass indicated a horizon about equivalent in age to the Torrejon of New Mexico, but the presence of unfamilar forms, suggesting a different faunal phase, was recognized. A few years later (1908 to 1911) this region was much more fully explored for fossil remains by parties of the United States Geological Survey and the United States National Museum. Working under the direction of Dr. T. W. Stanton, Mr. Albert C. Silberling, an ener- getic and successful collector, procured the first specimens in the winter and spring of 1908, continuing operations intermittently through the following years until the early spring of 1911. The present writer visited the field in 1908 and again in 1909, securing a considerable amount of good material. The net result of this com- bined field work is the splendid collection now in the National Museum, consisting of about 1,000 specimens, for the most part upper and lower jaw portions carrying teeth in varying numbers, but including also several characteristic foot and limb bones. Although nearly 10 years have passed since the last of this collec- tion was received, it was not until late in the summer of 1920 that the preparation of the material for study was completed. -
Slow Loris Forest Protector Teacher's Pack
2 www.nocturama.org https://www.facebook.com/pages/Little-Fireface-Project/ littlefi[email protected] INTRODUCTION Welcome! Welcome to the Slow Loris—Forest Protector’s Teacher’s Pack and Learning Exercise Book. The purpose of this short booklet is to explain how to use the book and to help to reinforce its message through a series of fun and easy-to- We at the Little Fireface Project (LFP) our so glad you are using this teacher’s use exercises. pack. First we want to tell you about ourselves and our passion about one of the world’s most unique little primates. LFP is a UK Charity based out of Ox- ford Brookes University set up to help save the slow loris through studying In this pack, you will find the following materials to help you and your students them in the wild and through education projects. explore the story of two night-active (nocturnal) primates, slow lorises: a moth- er (Tereh—speedy) and her young son (Bunga—flower). Tereh lovingly teaches Why the slow loris and why a charity dedicated to one group of animals? Well, her son the life skills he needs to be a grown-up slow loris. At the same time, the eight species of slow lorises, found only in Asia, are facing a tough time. Bunga learns that by doing his job in the forest, he helps the forest to grow, They are threatened for many reasons beyond the habitat loss causing many of while helping protect the crops grown by people. Asia’s species to go extinct. -
Ecology and Behaviour of Tarsius Syrichta in the Wild
O',F Tarsius syrichta ECOLOGY AND BEHAVIOUR - IN BOHOL, PHILIPPINES: IMPLICATIONS FOR CONSERVATION By Irene Neri-Arboleda D.V.M. A thesis submitted in fulfillment of the requirements for the degree of Master of Applied Science Department of Applied and Molecular Ecology University of Adelaide, South Australia 2001 TABLE OF CONTENTS DAge Title Page I Table of Contents............ 2 List of Tables..... 6 List of Figures.... 8 Acknowledgements... 10 Dedication 11 I)eclaration............ t2 Abstract.. 13 Chapter I GENERAL INTRODUCTION... l5 1.1 Philippine Biodiversity ........... t6 1.2 Thesis Format.... l9 1.3 Project Aims....... 20 Chapter 2 REVIEIV OF TARSIER BIOLOGY...... 2t 2.1 History and Distribution..... 22 2.t.1 History of Discovery... .. 22 2.1.2 Distribution...... 24 2.1.3 Subspecies of T. syrichta...... 24 2.2 Behaviour and Ecology.......... 27 2.2.1 Home Ranges. 27 2.2.2 Social Structure... 30 2.2.3 Reproductive Behaviour... 3l 2.2.4 Diet and Feeding Behaviour 32 2.2.5 Locomotion and Activity Patterns. 34 2.2.6 Population Density. 36 2.2.7 Habitat Preferences... ... 37 2.3 Summary of Review. 40 Chapter 3 FßLD SITE AI\D GEIYERAL METHODS.-..-....... 42 3.1 Field Site........ 43 3. 1.1 Geological History of the Philippines 43 3.1.2 Research Area: Corella, Bohol. 44 3.1.3 Physical Setting. 47 3.t.4 Climate. 47 3.1.5 Flora.. 50 3.1.6 Fauna. 53 3.1.7 Human Population 54 t page 3.1.8 Tourism 55 3.2 Methods.. 55 3.2.1 Mapping. -
1 CURRICULUM VITAE E. Christopher Kirk Department of Anthropology Phone: (512) 471-0056 2201 Speedway Stop C3200 Fax: (512) 47
CURRICULUM VITAE E. Christopher Kirk Department of Anthropology Phone: (512) 471-0056 2201 Speedway Stop C3200 Fax: (512) 471-6535 University of Texas at Austin [email protected] Austin, Texas 78712 PROFESSIONAL APPOINTMENTS 2016-Present University Distinguished Teaching Professor, University of Texas at Austin 2015-Present Professor, Department of Anthropology, University of Texas at Austin 2014-Present Research Associate, Vertebrate Paleontology Laboratory, Jackson School Museum of Earth History, University of Texas at Austin 2009-2015 Associate Professor, Department of Anthropology, University of Texas at Austin 2005-2014 Assistant Research Professor, Texas Memorial Museum, University of Texas at Austin 2003-2009 Assistant Professor, Department of Anthropology, University of Texas at Austin 2000-2003 Instructor, Department of Biological Anthropology and Anatomy, Duke University EDUCATION Ph.D. 2003 Biological Anthropology and Anatomy: Duke University B.A. 1995 Anthropology: University of Texas at Austin PROFESSIONAL AND HONOR SOCIETY MEMBERSHIPS American Association of Physical Anthropology Society of Vertebrate Paleontology Phi Beta Kappa HONORS & AWARDS 2016 Member, Academy of Distinguished Teachers – Recognizes tenured faculty members who have made sustained and significant contributions to education, particularly at the undergraduate level; Nominated by the Department of Anthropology and the College of Liberal Arts 2016 Billy Carr Distinguished Teaching Fellowship – Awarded in recognition of my efforts to include students -
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. -
Do Saki Monkeys Possess a Grooming Claw?
Short communication Primate Biol., 7, 19–23, 2020 https://doi.org/10.5194/pb-7-19-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Do saki monkeys possess a grooming claw? Constanze Ohlendorf1,2,a and Eckhard W. Heymann2 1Soziobiologie/Anthropologie, Georg-August-Universität Göttingen, 37077 Göttingen, Germany 2Verhaltensökologie & Soziobiologie, Deutsches Primatenzentrum – Leibniz-Institut für Primatenforschung, 37077 Göttingen, Germany acurrent address: Planungsgemeinschaft LaReG, Helmstedter Straße 55A, 38126 Braunschweig, Germany Correspondence: Eckhard W. Heymann ([email protected]) Received: 19 February 2020 – Revised: 27 July 2020 – Accepted: 10 August 2020 – Published: 15 September 2020 Abstract. The presence of a grooming claw on the second toe is a characteristic of Strepsirrhini and tarsiers. There is also some evidence for the presence of a grooming claw in Platyrrhini. Here we report qualitative findings from different species of saki monkeys, genus Pithecia, on the presence of modified nails on the second toe. These observations suggest that a grooming claw or a grooming claw-like nail occurs in different Pithecia species, but that it does not consistently occur in all individuals. 1 Introduction Platyrrhini retain several plesiomorphic primate traits, e.g., the presence of three premolars and the fusion of the ec- totympanic ring with the side of the auditory bulla (Flea- Grooming claws are a well-known morphological charac- gle, 2013). Bluntschli (1929) was the first to suggest that teristic of Strepsirrhini and tarsiers. Strepsirrhini possess Platyrrhini may also retain a grooming claw. He reported grooming claws on the second toe, tarsiers also on the third modified nails on the second toe of wild individuals of the toe. -
8. Primate Evolution
8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America. -
A Study of the Pulp Cavities and Roots of the Lower Premolars and Molars of Prosimii, Ceboidea and Cercopithecoidea1
A STUDY OF THE PULP CAVITIES AND ROOTS OF THE LOWER PREMOLARS AND MOLARS OF PROSIMII, CEBOIDEA AND CERCOPITHECOIDEA1 MUZAFFER SÜLEYMAN SENYÜREK, Ph. D. Professor of Anthropology and Chairman of the Division of Palaeoanthropology University of Ankara In a study published in 1939, I had stated: "From the fact that the Eocene pri~nates and the living Cercopithecidae appear to be cynodont it is i~zferred that the South American monkeys have acquired taurodontism independently of the higher Anthropoids and fossil Hominids." 2 During a second visit to the United States in 1946-1947, I had X-rayed a number of additional fossil 3 and recent specimens. In view of this additional material I have decided to reconsider the problem of taurodontism in Prosimii, Ceboidea and Cercopithecoidea and the light it throws on the origin of taurodontism in the South American monkeys. THE MATERIAL Tl~e number of the individuals X-rayed is listed in Table t. Altogether I have so far had X-rayed the permanent teeth of 55 specimens belonging to Prosimii, Ceboidea and Cercopithecoidea. The The classificatory terms Prosimii, Ceboidea and Cercopithecoidea are after Simpson, 1950, pp. 61-66. 2 ~enyürek, 1939, p. 122. 3 In 1939 a specimen of Pelycodus frugivorus, one Adapis parisiensis and one Microchoerus (Necrolemur) edwardsi had been X-rayed at Harvard University. During 1946 - 1947 I have had X-rayed the following fossil prima tes at the American Museun~~ of Natural History of New York : Pelycodus trigonodus Notharctus osborni Notharctus crassus Adapis magnus Amphipithecus