Darwinius Masillae Is a Haplorhine D Reply to Williams Et Al
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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. -
Diagnosis and Differentiation of the Order Primates
YEARBOOK OF PHYSICAL ANTHROPOLOGY 30:75-105 (1987) Diagnosis and Differentiation of the Order Primates FREDERICK S. SZALAY, ALFRED L. ROSENBERGER, AND MARIAN DAGOSTO Department of Anthropolog* Hunter College, City University of New York, New York, New York 10021 (F.S.S.); University of Illinois, Urbanq Illinois 61801 (A.L. R.1; School of Medicine, Johns Hopkins University/ Baltimore, h4D 21218 (M.B.) KEY WORDS Semiorders Paromomyiformes and Euprimates, Suborders Strepsirhini and Haplorhini, Semisuborder Anthropoidea, Cranioskeletal morphology, Adapidae, Omomyidae, Grades vs. monophyletic (paraphyletic or holophyletic) taxa ABSTRACT We contrast our approach to a phylogenetic diagnosis of the order Primates, and its various supraspecific taxa, with definitional proce- dures. The order, which we divide into the semiorders Paromomyiformes and Euprimates, is clearly diagnosable on the basis of well-corroborated informa- tion from the fossil record. Lists of derived features which we hypothesize to have been fixed in the first representative species of the Primates, Eupri- mates, Strepsirhini, Haplorhini, and Anthropoidea, are presented. Our clas- sification of the order includes both holophyletic and paraphyletic groups, depending on the nature of the available evidence. We discuss in detail the problematic evidence of the basicranium in Paleo- gene primates and present new evidence for the resolution of previously controversial interpretations. We renew and expand our emphasis on postcra- nial analysis of fossil and living primates to show the importance of under- standing their evolutionary morphology and subsequent to this their use for understanding taxon phylogeny. We reject the much advocated %ladograms first, phylogeny next, and scenario third” approach which maintains that biologically founded character analysis, i.e., functional-adaptive analysis and paleontology, is irrelevant to genealogy hypotheses. -
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. -
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. -
From the Gulf Coastal Plain
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 355-361 355 EKGMOWECHASHALA (MAMMALIA, ?PRIMATES) FROM THE GULF COASTAL PLAIN L. Barry Albright III1 A single, small, water-worn tooth from the “middle” Arikareean Toledo Bend Local Fauna of the Gulf Coastal Plain closely resembles the lower fourth premolar of the questionable primate Ekgmowechashala. The only known species of the genus, Ekgmowechashala philotau Macdonald (1963), was originally recovered from the early Arikareean Sharps Formation of South Dakota, but is also known from similar aged strata of the John Day Formation, Oregon. Although the Toledo Bend specimen differs somewhat in morphology from the p4 of E. philotau, a new species is not named in this report because of such limited material and because the specimen is incomplete. Unfortunately, the specimen does not provide information that helps clarify current arguments regarding the affinities of Ekgmowechashala with primates or plagiomenids. It does, however, provide (1) a temporal range extension for the genus to the early late Arikareean, or about four million years younger than previously known, and (2) a geographic extension east and considerably south of its prior distribution. If Ekgmowechashala is ultimately deter- mined to belong to the Primates, then the Toledo Bend species would become the last known North American representative of the order. Key Words: Ekgmowechashala; Primates; Plagiomenidae; Texas Gulf Coastal Plain; Arikareean INTRODUCTION brate paleontology collections of the Louisiana State Uni- In 1990, while screen-washing matrix from the “middle” versity Museum of Geoscience (LSUMG V). Arikareean Toledo Bend site in the Fleming Formation of easternmost Texas (Albright 1994, 1996, 1998a, 1998b, BACKGROUND 1999), a small, unusual, water-worn tooth was recov- Ekgmowechashala philotau is a small “enigmatic late ered that differed considerably from the site’s more com- Oligocene mammal” (McKenna, 1990:226) heretofore mon and readily identifiable rodent teeth. -
Convergent Evolution of Olfactory and Thermoregulatory Capacities in Small Amphibious Mammals
Convergent evolution of olfactory and thermoregulatory capacities in small amphibious mammals Quentin Martineza,1, Julien Clavelb,c, Jacob A. Esselstynd,e, Anang S. Achmadif, Camille Grohég,h, Nelly Piroti,j, and Pierre-Henri Fabrea,k aInstitut des Sciences de l’Évolution de Montpellier (ISEM), CNRS, Institut de recherche pour le développement (IRD), Université de Montpellier (UM), UMR 5554, 34095 Montpellier, France; bDepartment of Life Sciences, The Natural History Museum, SW7 5DB London, United Kingdom; cUniv. Lyon Laboratoire d’Ecologie des Hydrosystèmes Naturels et Anthropisés, UMR CNRS 5023, Université Claude Bernard Lyon 1, École Nationale des Travaux Publics de l’État (ENTPE), F‐69622 Villeurbanne, Cedex, France; dMuseum of Natural Science, Louisiana State University, Baton Rouge, LA 70803; eDepartment of Biological Sciences, Louisiana State University, Baton Rouge, LA 70803; fMuseum Zoologicum Bogoriense, Research Center for Biology, Indonesian Institute of Sciences (LIPI), 16911 Cibinong, Indonesia; gDivision of Paleontology, American Museum of Natural History, New York, NY 10024; hLaboratoire Paléontologie Évolution Paléoécosystèmes Paléoprimatologie (PALEVOPRIM, UMR 7262, CNRS-Institut écologie et environnement [INEE]), Université de Poitiers, 86073 Poitiers, Cedex 9, France; iInstitut de Recherche en Cancérologie de Montpellier (IRCM), INSERM, U1194 UM, Institut du Cancer de Montpellier (ICM), F-34298 Montpellier, Cedex 5, France; jRéseau d’Histologie Expérimentale de Montpellier, UMS3426 CNRS-US009 INSERM-UM, 34298 Montpellier, France; and kMammal Section, Department of Life Sciences, The Natural History Museum, SW7 5DB London, United Kingdom Edited by David B. Wake, University of California, Berkeley, CA, and approved February 28, 2020 (received for review October 11, 2019) Olfaction and thermoregulation are key functions for mammals. The partitioning has been documented in histological, airflow dynamic, former is critical to feeding, mating, and predator avoidance behaviors, and performance test studies (9–13). -
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. -
Early Eocene Primates from Gujarat, India
ARTICLE IN PRESS Journal of Human Evolution xxx (2009) 1–39 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Early Eocene Primates from Gujarat, India Kenneth D. Rose a,*, Rajendra S. Rana b, Ashok Sahni c, Kishor Kumar d, Pieter Missiaen e, Lachham Singh b, Thierry Smith f a Johns Hopkins University School of Medicine, Baltimore, Maryland 21205, USA b H.N.B. Garhwal University, Srinagar 246175, Uttarakhand, India c Panjab University, Chandigarh 160014, India d Wadia Institute of Himalayan Geology, Dehradun 248001, Uttarakhand, India e University of Ghent, B-9000 Ghent, Belgium f Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium article info abstract Article history: The oldest euprimates known from India come from the Early Eocene Cambay Formation at Vastan Mine Received 24 June 2008 in Gujarat. An Ypresian (early Cuisian) age of w53 Ma (based on foraminifera) indicates that these Accepted 8 January 2009 primates were roughly contemporary with, or perhaps predated, the India-Asia collision. Here we present new euprimate fossils from Vastan Mine, including teeth, jaws, and referred postcrania of the Keywords: adapoids Marcgodinotius indicus and Asiadapis cambayensis. They are placed in the new subfamily Eocene Asiadapinae (family Notharctidae), which is most similar to primitive European Cercamoniinae such as India Donrussellia and Protoadapis. Asiadapines were small primates in the size range of extant smaller Notharctidae Adapoidea bushbabies. Despite their generally very plesiomorphic morphology, asiadapines also share a few derived Omomyidae dental traits with sivaladapids, suggesting a possible relationship to these endemic Asian adapoids. In Eosimiidae addition to the adapoids, a new species of the omomyid Vastanomys is described. -
Anthroquest the Newsletter of the Leakey Foundation
no. 35 Spring/Summer 2017 AnthroQuest The Newsletter of The Leakey Foundation Leakey Grantee Finds Oldest Primates of India THIERRY SMITH, LEAKEY FOUNDATION GRANTEE, ROYAL BELGIAN INSTITUTE OF NATURAL SCIENCES n 2004, Professor Kenneth D. Rose from John Hopkins I University invited me to lead a small team of paleontologists planning to explore lignite (brown coal) mines in India. The goal was to prospect for Paleocene-Eocene deposits (66-34 million years ago), which could yield ancient terrestrial mammals. Ken thought the screen-washing technique we used to find small fossil mammals in Wyoming would work well in India. I went to Mumbai with a student, Pieter Missiaen, and we travelled about 250 mile north to the Vastan mine in Thierry Smith screenwashing sediments for small remains of earliest Indian primates Gujarat to meet our Indian colleagues Photo: Annelise Folie for the first time. I remember well that on the second day in the mine, it was a mammal incisor the size of a human million years old). We published this hot, and I was nervous because we were incisor. It was the beginning of our jaw with four teeth under the new name six persons sharing only two hammers Indian adventure! Asiadapis cambayensis, and today this to look for fossils in a sticky clay layer. specimen is the reference of the family This deposit was so rich that we Asiadapidae. I suggested to my colleague, Professor collected all the matrix and screen- Rajendra Singh Rana, that he ask a washed it completely. Each sieve The Vastan mine was a paradise for miner to remove the lignite layer above contained small mammal teeth or paleontologists. -
Download HEB1330 Primate Diversity.Pdf
HEB 1330: Primate Social Behavior September 15th 2020 Primate Diversity Quiz 1 2 1. What is a spandrel (in an evolutionary context)? (1 point). Provide an example of a spandrel. (1 point) 2. Explain human lactation, using each of Tinbergen’s four questions. (4 points) 3. The table below has information about food distribution and feeding competition for two different groups of Chacma baboons, the Laikipia group and the Drakensberg group. How would you expect female-female relationships to differ between the two groups, and why? (2 points) 3 Overview 1) What is a Primate? 2) Basic Vocabulary 3) Brief Overview of Primate Groups Reading: Boyd R & Silk J. 2015. How Humans Evolved. Chapter 5, pg. 108-125. 4 What is a primate? What am I? 5 Primates are mammals 6 Primates have a Petrosal Bulla 7 Primates have an emphasis on vision rather than smell 8 Primates have a generalized dentition 9 Primates have opposable thumbs and mostly nails instead of claws 10 Primates have increased life spans 11 Primates have slow development 12 Primates have big brains 13 Primates are social 14 Where do primates live? • ~685 species and subspecies of primates • Primates are found in Africa, Asia, South / Central America in tropical regions (mostly forests) 15 Where do non-human primates live? • ~685 species and subspecies of primates • Primates are found in Africa, Asia, South / Central America in tropical regions (mostly forests) 16 Overview 1) What is a Primate? 2) Basic Vocabulary 3) Brief Overview of Primate Groups Reading: Boyd R & Silk J. 2015. How Humans Evolved.