Locomotion-Related Femoral Trabecular Architectures in Primates (Paidopithex Rhenanus, Pliopithecus Vindobonensis)
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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. -
ZOOLOGY Exploring the Biodiversity of Colorado and Theworld
CHAPTER 4 — ZOOLOGY Exploring the Biodiversity of Colorado and the World CHAPTER 4 ZOOLOGY Exploring the Biodiversity of Colorado and the World Jeffrey T. Stephenson, Before the Museum Paula E. Cushing, The first collections of specimens that make up what is now the Denver John R. Demboski, and Museum of Nature & Science were actually established well before the Frank-T. Krell founding of the institution in 1900, the selection of a board of trustees, or the construction of a building to house and exhibit the specimens. Edwin Carter (1830–1900) (Fig. 4.1) collected Colorado birds and mammals from the 1860s through the 1890s. Born in New York in 1830, Carter arrived in Colorado in 1859 hoping to make it rich in the goldfields, but he soon became interested in the region’s natural history. He learned hide tanning and, as his prospects for hitting the mother lode faded, he earned his living selling buckskin clothing that he handcrafted. Carter supplemented these earnings by mar- keting foodstuffs and other provisions to the growing population of successful and (mostly) unsuccessful prospectors flooding the region. His interest in nature turned to concern as he observed dwindling numbers of mammals and birds, owing largely to habitat destruction and overhunting. Period photographs of the area’s mining district show a landscape largely denuded of vegetation. By the 1870s, Carter noted that many animal species were becoming scarce. The state’s forests were being devastated, ranches and farms were replacing open prairie, and some species, including the last native bison in Colorado, were on the verge of extirpation or extinction. -
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. -
Cranial Remains of an Eocene Tarsier
Cranial remains of an Eocene tarsier James B. Rossie*†, Xijun Ni‡, and K. Christopher Beard§ *Department of Anthropology, Stony Brook University, Stony Brook, NY 11794; ‡Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, P.O. Box 643, Beijing 100044, China; §Section of Vertebrate Paleontology, Carnegie Museum of Natural History, 4400 Forbes Avenue, Pittsburgh, PA 15213 Edited by Alan Walker, Pennsylvania State University, University Park, PA, and approved January 30, 2006 (received for review October 28, 2005) The phylogenetic position of tarsiers relative to anthropoids and Paleogene omomyids remains a subject of lively debate that lies at the center of research into anthropoid origins. Omomyids have long been regarded as the nearest relatives of tarsiers, but a sister group relationship between anthropoids and tarsiers has also been proposed. These conflicting phylogenetic reconstructions rely heavily on comparisons of cranial anatomy, but until now, the fossil record of tarsiers has been limited to a single jaw and several isolated teeth. In this article, we describe cranial material of a fossil tarsiid from the middle-Eocene Shanghuang fissure-fillings in southern Jiangsu Province, China. This facial fragment, which is allocated to Tarsius eocaenus, is virtually identical to the corre- sponding anatomy in living tarsiers and differs substantially from that of early anthropoids such as Bahinia, Phenacopithecus, and Parapithecus. This new specimen indicates that tarsiers already possessed greatly enlarged orbits and a haplorhine oronasal con- figuration by the time they are first documented in the fossil record during the middle Eocene. China ͉ primate ͉ tarsiid ack of consensus regarding the interrelationships among Lanthropoids, tarsiids, and omomyids is largely due to con- tradictory similarities among the three groups in cranial anat- omy. -
08 Early Primate Evolution
Paper No. : 14 Human Origin and Evolution Module : 08 Early Primate Evolution Development Team Principal Investigator Prof. Anup Kumar Kapoor Department of Anthropology, University of Delhi Dr. Satwanti Kapoor (Retd Professor) Paper Coordinator Department of Anthropology, University of Delhi Mr. Vijit Deepani & Prof. A.K. Kapoor Content Writer Department of Anthropology, University of Delhi Prof. R.K. Pathak Content Reviewer Department of Anthropology, Panjab University, Chandigarh 1 Early Primate Evolution Anthropology Description of Module Subject Name Anthropology Paper Name Human Origin and Evolution Module Name/Title Early Primate Evolution Module Id 08 Contents: Fossil Primates: Introduction Theories of primate origin Primates: Pre- Pleistocene Period a. Palaeocene epoch b. Eocene epoch c. Oligocene epoch d. Miocene – Pliocene epoch Summary Learning outcomes: The learner will be able to develop: an understanding about fossil primates and theories of primate origin. an insight about the extinct primate types of Pre-Pleistocene Period. 2 Early Primate Evolution Anthropology Fossil Primates: Introduction In modern time, the living primates are graded in four principle domains – Prosimian, Monkey, Ape and man. On the basis of examination of fossil evidences, it has been established that all the living primates have evolved and ‘adaptively radiated’ from a common ancestor. Fossil primates exhibit a palaeontological record of evolutionary processes that occurred over the last 65 to 80 million years. Crucial evidence of intermediate forms, that bridge the gap between extinct and extant taxa, is yielded by the macroevolutionary study of the primate fossil evidences. The paleoanthropologists often utilize the comparative anatomical method to develop insight about morphological adaptations in fossil primates. -
ANTH 42: Primates in Nature Rules to a Story •What? •When? •Where
Rules to a story! … but today, not in that order:! •!What?! When? Dating methods and deep time! •!When?! Where? How do fossils form - ANTH 42: Primates in Nature! taphonomy! •!Where?! What? The primate fossil record! Lecture 2:! •!Why?! Why? Evolution and its Primate evolution! mechanisms (including natural selection) [later lecture!]! http://weber.ucsd.edu/~jmoore/courses/anth42web/! WHEN: Dating Bishop James Ussher: 1650 WHEN: Dating methods! Uniformitarianism methods! calculated from Bible that & the earth! Creation occurred 4004 BC! Strata laid down in layers, oldest are deepest.! Mary Ann Mantell: 1820 discovered “Iguanodon” tooth (Sussex, UK)*! Younger or older?! Richard Owen: 1842 coined Sometimes, word “Dinosaur”! geological 1854: Dinner in the Iguanodon! processes can Was hard to reconcile 6,000 years with creatures SO muddle that up.! different and so clearly extinct.! Uniformitarianism violated.! * Other giant bones known, but this specimen first to kick off ‘modern’ interest! But with more data, can usually figure it out.! WHEN: Dating methods! WHEN: Dating methods! 1566! " 100 years trying to date fossils. Absolute. ! Recognized fossil ‘stages’ - rocks with Dendrochronology! no crinoids or coral overlaid by rocks (tree rings)! Growth depends on with crinoids and coral, but no rainfall; annual rings.! dinosaurs, so could talk about “age of Count inward from crinoids” and “age of dinosaurs”. outermost ring, get age of tree.! Knew the order taxa showed up Bristlecone pine 5,000 yrs! (relative dating), but argue about when in years (absolute dating).! Buried log! WHEN: Dating methods! 1566! WHEN: Dating methods! Absolute. Dendrochronology! Absolute. ! River oaks, S. Radiometric! Dendrochronology! Germany: > (tree rings)! 10,000 yrs! Isotopic decay - Growth depends on measurable rainfall; annual rings.! Bristlecone rates! Pines, SW Count inward from USA: 8,500! outermost ring, get age of tree.! Bristlecone pine 5,000 yrs! Buried log! Buried log! WHEN: Dating methods! • total amount of WHEN: Dating methods! Absolute. -
Effects of Additional Postcranial Data on the Topologies of Early Eocene Primate
Effects of Additional Postcranial Data on the Topologies of Early Eocene Primate Phylogenies Julia Stone ANT 679HB Special Honors in the Department of Anthropology The University of Texas at Austin May 2021 Liza J. Shapiro Department of Anthropology Supervising Professor E. Christopher Kirk Department of Anthropology Second Reader Acknowledgements This project would not have been completed without the help of my thesis supervisor Dr. Liza Shapiro. I was inspired to start the project after taking her courses in Primate Evolution and Primate Anatomy. She also met with me many times throughout this year to discuss the trajectory of the project as well as discuss papers that became the foundation of the thesis. She assisted me through technology issues, unresolved trees, and many drafts, and she provided invaluable guidance throughout this process. I also want to thank Dr. Christopher Kirk for being my second reader and providing extremely helpful insight into how to write about phylogenetic results. He also helped me to be more specific and accurate in all of the sections of the thesis. I learned a lot about writing theses in general due to his comments on my drafts. I also truly appreciate the help of Ben Rodwell, a graduate student at the University of Texas at Austin. He provided excellent help and support regarding the Mesquite and TNT software used in this project. ii Effects of Additional Postcranial Data on the Topologies of Early Eocene Primate Phylogenies by Julia Stone, BA The University of Texas at Austin SUPERVISOR: Liza J. Shapiro There are multiple hypotheses regarding the locomotor behaviors of the last common ancestor to primates and which fossil primates best represent that ancestor. -
Frontal Fusion: Collapse of Another Anthropoid Synapomorphy
THE ANATOMICAL RECORD 291:308–317 (2008) Frontal Fusion: Collapse of Another Anthropoid Synapomorphy 1,2,3 3 ALFRED L. ROSENBERGER AND ANTHONY S. PAGANO * 1Department of Anthropology and Archaeology, Brooklyn College, CUNY, Brooklyn, New York 2American Museum of Natural History, New York, New York 3Department of Anthropology, City University of New York Graduate Center, New York Consortium in Evolutionary Primatology (NYCEP), New York, New York ABSTRACT We test the hypothesis that the fused interfrontal suture of anthro- poids is a uniquely distinguishing feature and a derived characteristic indicative of their monophyletic origin. Our survey of nonanthropoid primates and several archontan families indicates frontal fusion is wide- spread. It is most variable (fused, open or partially fused) inter- and intra-specifically among strepsirhines. The frontal bone is more commonly fused in living lemuroids and indrioids than among lorisoids. It appears to be fused regularly among Eocene adapids. Among nonanthropoid haplorhines, the interfrontal is fused in Tarsius, even in neonates and invariably in adults, probably also in all fossil tarsiiforms preserving the frontal bone, and in the late Eocene protoanthropoid Rooneyia. The plesiadapiform pattern remains uncertain, but fusion is ubiquitous among living tree shrews, colugos and bats. Distributional evidence implies that interfrontal fusion was present in the last common ancestor (LCA) of haplorhine primates and possibly in the LCA of euprimates as well. Anthropoids, therefore, cannot be defined cladistically by interfrontal fusion, not out of concern for homoplasy but because it is probably a primitive feature inherited from other taxa related to anthropoids. Fusion of the large anthropoid frontal bone, which was extended anteriorly to roof the orbits and expanded laterally in connection with a wide forebrain in the LCA of anthropoids and protoanthropoids, may have been preadap- tive to the evolution of the postorbital septum. -
Geology* Paleontology, and Correlation of Eocene Volcaniclastic Rocks, Southeast Absaroka Range, Hot Springs County, Wyoming
Geology* Paleontology, and Correlation of Eocene Volcaniclastic Rocks, Southeast Absaroka Range, Hot Springs County, Wyoming GEOLOGICAL SURVEY PROFESSIONAL PAPER 1201-A Geology, Paleontology, and Correlation of Eocene Volcaniclastic Rocks, Southeast Absaroka Range, Hot Springs County, Wyoming By T. M. BOWN GEOLOGY OF THE ABSAROKA RANGE, NORTHWEST WYOMING GEOLOGICAL SURVEY PROFESSIONAL PAPER 1201-A Relations of Eocene volcaniclastic rocks and Eocene fossils date the sedimentary and structural evolution of the southeast Absaroka Range, clarify correlations with adjacent areas, and aid in timing large-scale events of gravity faulting UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Bown, Thomas M. Geology, paleontology, and correlation of Eocene volcaniclastic rocks, southeast Absaroka Range, Hot Springs County, Wyoming. (Geological Survey Professional Paper 1201-A) Bibliography: p.71 Supt.ofDocs.no.: II9.I6:1201-A 1. Geology, Stratigraphic Eocene. 2. Volcanic ash, tuff, etc. Wyoming Hot Springs Co. 3. Mammals, Fossil. 4. Stratigraphic correlation Wyoming Hot Springs Co. 5. Geology Wyoming Hot Springs Co. 1. Title. II. Series: United States. Geological Survey. Professional Paper 1201-A. QE692.2.B68 55I.7'84'0978743 80-607125 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract ------------------------------------------------- -
Primate Evolution - Judith Masters
BIOLOGICAL SCIENCE FUNDAMENTALS AND SYSTEMATICS – Vol. IV - Primate Evolution - Judith Masters PRIMATE EVOLUTION Judith Masters Natal Museum, Pietermaritzburg, South Africa Keywords: Adapiformes, australopithecines, Catarrhini, Cercopithecoidea, dryopithecines, early simians, Euprimates, Haplorhini, hominins, Hominoidea, lemuriforms, lorisiforms, Omomyiformes, Oreopithecus, Platyrrhini, Pliopithecidae, Proconsulidae, sivapithecines, Strepsirrhini, tarsiers, Victoriapithecinae Contents 1. Introduction 2. Archaic Primates 3. Early Euprimates—“Primates of Modern Aspect” 3.1. Adapiforms and Omomyiforms 3.2. Early Simians 4. Later Simian Radiations 4.1. Early Monkeys 4.2. The Epoch of the Apes 5. The Origins of Modern Primate Groups 5.1. Nonhuman Primates 5.2. The Human Lineage 5.2.1. Early Hominins 5.2.2.The Genus “Homo” Acknowledgments Glossary Bibliography Biographical Sketch Summary Living primates include the Strepsirrhini (lemurs, lorises, and galagos) and the Haplorhini (tarsiers, monkeys, and apes). The order arose 80 MYBP (million years before present) to 90 MYBP, and the two major groups are likely to have diverged before 65 MYBP. The Plesiadapiformes, an extinct Paleocene group, may have been related toUNESCO true primates, but were not their– directEOLSS ancestors. The earliest true primate radiations occurred in the Paleocene and earliest Eocene, about 60 MYBP. These were the OmomyiformesSAMPLE (haplorhines, chiefly CHAPTERSin North America), the Adapiforms (strepsirrhines, mainly in Eurasia), and the simians (haplorhines, in North Africa). The origins of modern strepsirrhines are obscure, because of a scarcity of fossils. Between 45 MYBP and 37 MYBP the simians diverged into the two major groups recognized today: the Catarrhini (Old World monkeys) and the Platyrrhini (New World monkeys). The oldest fossil from the New World is only 29 MY old, suggesting the group probably emigrated from the Old World. -
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DENVER MUSEUM OF NATURE & SCIENCE ANNALS NUMBER 1, SEPTEMBER 1, 2009 Land Mammal Faunas of North America Rise and Fall During the Early Eocene Climatic Optimum Michael O. Woodburne, Gregg F. Gunnell, and Richard K. Stucky WWW.DMNS.ORG/MAIN/EN/GENERAL/SCIENCE/PUBLICATIONS The Denver Museum of Nature & Science Annals is an Frank Krell, PhD, Editor-in-Chief open-access, peer-reviewed scientific journal publishing original papers in the fields of anthropology, geology, EDITORIAL BOARD: paleontology, botany, zoology, space and planetary Kenneth Carpenter, PhD (subject editor, Paleontology and sciences, and health sciences. Papers are either authored Geology) by DMNS staff, associates, or volunteers, deal with DMNS Bridget Coughlin, PhD (subject editor, Health Sciences) specimens or holdings, or have a regional focus on the John Demboski, PhD (subject editor, Vertebrate Zoology) Rocky Mountains/Great Plains ecoregions. David Grinspoon, PhD (subject editor, Space Sciences) Frank Krell, PhD (subject editor, Invertebrate Zoology) The journal is available online at www.dmns.org/main/en/ Steve Nash, PhD (subject editor, Anthropology and General/Science/Publications free of charge. Paper copies Archaeology) are exchanged via the DMNS Library exchange program ([email protected]) or are available for purchase EDITORIAL AND PRODUCTION: from our print-on-demand publisher Lulu (www.lulu.com). Betsy R. Armstrong: project manager, production editor DMNS owns the copyright of the works published in the Ann W. Douden: design and production Annals, which are published under the Creative Commons Faith Marcovecchio: proofreader Attribution Non-Commercial license. For commercial use of published material contact Kris Haglund, Alfred M. Bailey Library & Archives ([email protected]).