Reconstruction of an Extraordinary Extinct Primate from Madagascar
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EAZA Best Practice Guidelines Bonobo (Pan Paniscus)
EAZA Best Practice Guidelines Bonobo (Pan paniscus) Editors: Dr Jeroen Stevens Contact information: Royal Zoological Society of Antwerp – K. Astridplein 26 – B 2018 Antwerp, Belgium Email: [email protected] Name of TAG: Great Ape TAG TAG Chair: Dr. María Teresa Abelló Poveda – Barcelona Zoo [email protected] Edition: First edition - 2020 1 2 EAZA Best Practice Guidelines disclaimer Copyright (February 2020) by EAZA Executive Office, Amsterdam. All rights reserved. No part of this publication may be reproduced in hard copy, machine-readable or other forms without advance written permission from the European Association of Zoos and Aquaria (EAZA). Members of the European Association of Zoos and Aquaria (EAZA) may copy this information for their own use as needed. The information contained in these EAZA Best Practice Guidelines has been obtained from numerous sources believed to be reliable. EAZA and the EAZA APE TAG make a diligent effort to provide a complete and accurate representation of the data in its reports, publications, and services. However, EAZA does not guarantee the accuracy, adequacy, or completeness of any information. EAZA disclaims all liability for errors or omissions that may exist and shall not be liable for any incidental, consequential, or other damages (whether resulting from negligence or otherwise) including, without limitation, exemplary damages or lost profits arising out of or in connection with the use of this publication. Because the technical information provided in the EAZA Best Practice Guidelines can easily be misread or misinterpreted unless properly analysed, EAZA strongly recommends that users of this information consult with the editors in all matters related to data analysis and interpretation. -
An Introduction to Lemurs for Teachers and Educators
AN INTRODUCTION TO LEMURS FOR TEACHERS AND EDUCATORS WELCOME TO THE WORLD OF AKO THE AYE-AYE The Ako the Aye-Aye Educator’s Guide introduces you to the remarkable world of lemurs. This guide provides background information about the biological concepts conveyed through the 21 Ako lessons. These lessons were created to accompany the Ako books. The Ako book series were developed by renowned primatologist Alison Jolly for students in Madagascar to inspire understanding and appreciation for the unique primates that share their island home. In addition to the books there is also a set of posters which showcase the habitat of each lemur species and their forest “neighbors.” GOALS OF THE AKO LESSONS: • Inspire students to make a positive difference for lemurs and other wildlife. • Promote environmental awareness, understanding and appreciation. • Provide activities that connect students to nature and motivate conservation action. HOW TO USE THIS GUIDE Each lesson aligns with a specific grade level (Kindergarten-1st, 2nd-3rd and 4th-5th) and one of the seven environmental themes below. Before carrying out an activity, we recommend reading the corresponding section in this guide that matches the theme of the lesson. The themes are: • LOOKING AT LEMURS—CLASSIFICATION AND BIODIVERSITY (PAGE 4) • EXPLORING LEMUR HABITATS (PAGE 10) • INVESTIGATING LEMUR ADAPTATIONS (PAGE 18) • DISCOVERING LEMUR COMMUNITIES—INTER-DEPENDENCE (PAGE 23) • LEARNING ABOUT LEMUR LIFE—LIFE CYCLES AND BEHAVIOR (PAGE 26) • DISCOVERING MADAGASCAR’S PEOPLE AND PLACES (PAGE 33) • MAKING A DIFFERENCE FOR LEMURS (PAGE 40) Lessons can be completed chronologically or independently. Each activity incorporates multiple learning styles and subject areas. -
Ecosystem Profile Madagascar and Indian
ECOSYSTEM PROFILE MADAGASCAR AND INDIAN OCEAN ISLANDS FINAL VERSION DECEMBER 2014 This version of the Ecosystem Profile, based on the draft approved by the Donor Council of CEPF was finalized in December 2014 to include clearer maps and correct minor errors in Chapter 12 and Annexes Page i Prepared by: Conservation International - Madagascar Under the supervision of: Pierre Carret (CEPF) With technical support from: Moore Center for Science and Oceans - Conservation International Missouri Botanical Garden And support from the Regional Advisory Committee Léon Rajaobelina, Conservation International - Madagascar Richard Hughes, WWF – Western Indian Ocean Edmond Roger, Université d‘Antananarivo, Département de Biologie et Ecologie Végétales Christopher Holmes, WCS – Wildlife Conservation Society Steve Goodman, Vahatra Will Turner, Moore Center for Science and Oceans, Conservation International Ali Mohamed Soilihi, Point focal du FEM, Comores Xavier Luc Duval, Point focal du FEM, Maurice Maurice Loustau-Lalanne, Point focal du FEM, Seychelles Edmée Ralalaharisoa, Point focal du FEM, Madagascar Vikash Tatayah, Mauritian Wildlife Foundation Nirmal Jivan Shah, Nature Seychelles Andry Ralamboson Andriamanga, Alliance Voahary Gasy Idaroussi Hamadi, CNDD- Comores Luc Gigord - Conservatoire botanique du Mascarin, Réunion Claude-Anne Gauthier, Muséum National d‘Histoire Naturelle, Paris Jean-Paul Gaudechoux, Commission de l‘Océan Indien Drafted by the Ecosystem Profiling Team: Pierre Carret (CEPF) Harison Rabarison, Nirhy Rabibisoa, Setra Andriamanaitra, -
“Subfossil” Koala Lemur Megaladapis Edwardsi
Evolutionary and phylogenetic insights from a nuclear genome sequence of the extinct, giant, “subfossil” koala lemur Megaladapis edwardsi Stephanie Marciniaka, Mehreen R. Mughalb, Laurie R. Godfreyc, Richard J. Bankoffa, Heritiana Randrianatoandroa,d, Brooke E. Crowleye,f, Christina M. Bergeya,g,h, Kathleen M. Muldooni, Jeannot Randrianasyd, Brigitte M. Raharivololonad, Stephan C. Schusterj, Ripan S. Malhik,l, Anne D. Yoderm,n, Edward E. Louis Jro,1, Logan Kistlerp,1, and George H. Perrya,b,g,q,1 aDepartment of Anthropology, Pennsylvania State University, University Park, PA 16802; bBioinformatics and Genomics Intercollege Graduate Program, Pennsylvania State University, University Park, PA 16082; cDepartment of Anthropology, University of Massachusetts, Amherst, MA 01003; dMention Anthropobiologie et Développement Durable, Faculté des Sciences, Université d’Antananarivo, Antananarivo 101, Madagascar; eDepartment of Geology, University of Cincinnati, Cincinnati, OH 45220; fDepartment of Anthropology, University of Cincinnati, Cincinnati, OH 45220; gDepartment of Biology, Pennsylvania State University, University Park, PA 16802; hDepartment of Genetics, Rutgers University, New Brunswick, NJ 08854; iDepartment of Anatomy, Midwestern University, Glendale, AZ 85308; jSingapore Centre for Environmental Life Sciences Engineering, Nanyang Technological University, Singapore 639798; kDepartment of Anthropology, University of Illinois Urbana–Champaign, Urbana, IL 61801; lDepartment of Ecology, Evolution and Behavior, Carl R. Woese Institute for -
Fossil Lemur from Northern Madagascar (Palaeopropithecidae/Primate Evolution/Postcranium) WILLIAM L
Proc. Natl. Acad. Sci. USA Vol. 88, pp. 9082-9086, October 1991 Evolution Phylogenetic and functional affinities of Babakotia (Primates), a fossil lemur from northern Madagascar (Palaeopropithecidae/primate evolution/postcranium) WILLIAM L. JUNGERSt, LAURIE R. GODFREYt, ELWYN L. SIMONS§, PRITHUJIT S. CHATRATH§, AND BERTHE RAKOTOSAMIMANANA$ tDepartment of Anatomical Sciences, State University of New York, Stony Brook, NY 117948081; tDepartment of Anthropology, University of Massachusetts, Amherst, MA 01003; §Department of Biological Anatomy and Anthropology and Primate Center, Duke University, Durham, NC 27705; and IService de Paldontologie, Universit6 d'Antananarivo, Antananarivo, Madagascar Contributed by Elwyn L. Simons, July 2, 1991 ABSTRACT Recent paleontological expeditions to the An- Craniodental Anatomy and Tooth Shape karana range of northern Madagascar have recovered the partial remains offour individuals ofa newly recognized extinct With an estimated body mass ofjust over 15 kg, Babakotia lemur, Babakoda radofia. Craniodental and postcranial ma- is a medium-sized indroid somewhat larger than the largest terial serve to identify Babakota as a member of the palae- living indrid (Indri) but similar in size to several of the opropithecids (also including the extinct genera Palaeopropith- smallest extinct lemurs, Mesopropithecus and Pachylemur ecus, Archaeoindris, and Mesopropithecus). Living indrids (4). A detailed description of the maxillary dentition of form the sister group to this fossil lade. The postcranial Babakotia exists -
Proposal for Inclusion of the Chimpanzee
CMS Distribution: General CONVENTION ON MIGRATORY UNEP/CMS/COP12/Doc.25.1.1 25 May 2017 SPECIES Original: English 12th MEETING OF THE CONFERENCE OF THE PARTIES Manila, Philippines, 23 - 28 October 2017 Agenda Item 25.1 PROPOSAL FOR THE INCLUSION OF THE CHIMPANZEE (Pan troglodytes) ON APPENDIX I AND II OF THE CONVENTION Summary: The Governments of Congo and the United Republic of Tanzania have jointly submitted the attached proposal* for the inclusion of the Chimpanzee (Pan troglodytes) on Appendix I and II of CMS. *The geographical designations employed in this document do not imply the expression of any opinion whatsoever on the part of the CMS Secretariat (or the United Nations Environment Programme) concerning the legal status of any country, territory, or area, or concerning the delimitation of its frontiers or boundaries. The responsibility for the contents of the document rests exclusively with its author. UNEP/CMS/COP12/Doc.25.1.1 PROPOSAL FOR THE INCLUSION OF CHIMPANZEE (Pan troglodytes) ON APPENDICES I AND II OF THE CONVENTION ON THE CONSERVATION OF MIGRATORY SPECIES OF WILD ANIMALS A: PROPOSAL Inclusion of Pan troglodytes in Appendix I and II of the Convention on the Conservation of Migratory Species of Wild Animals. B: PROPONENTS: Congo and the United Republic of Tanzania C: SUPPORTING STATEMENT 1. Taxonomy 1.1 Class: Mammalia 1.2 Order: Primates 1.3 Family: Hominidae 1.4 Genus, species or subspecies, including author and year: Pan troglodytes (Blumenbach 1775) (Wilson & Reeder 2005) [Note: Pan troglodytes is understood in the sense of Wilson and Reeder (2005), the current reference for terrestrial mammals used by CMS). -
Coexistence of Confamilial, Folivorous Indriids, Propithecus Diadema And
Washington University in St. Louis Washington University Open Scholarship Arts & Sciences Electronic Theses and Dissertations Arts & Sciences Spring 5-15-2017 Coexistence of Confamilial, Folivorous Indriids, Propithecus diadema and Indri indri, at Betampona Strict Nature Reserve, Madagascar Lana Kerker Oliver Washington University in St. Louis Follow this and additional works at: https://openscholarship.wustl.edu/art_sci_etds Part of the Biodiversity Commons, Biological and Physical Anthropology Commons, Natural Resources and Conservation Commons, and the Natural Resources Management and Policy Commons Recommended Citation Oliver, Lana Kerker, "Coexistence of Confamilial, Folivorous Indriids, Propithecus diadema and Indri indri, at Betampona Strict Nature Reserve, Madagascar" (2017). Arts & Sciences Electronic Theses and Dissertations. 1134. https://openscholarship.wustl.edu/art_sci_etds/1134 This Dissertation is brought to you for free and open access by the Arts & Sciences at Washington University Open Scholarship. It has been accepted for inclusion in Arts & Sciences Electronic Theses and Dissertations by an authorized administrator of Washington University Open Scholarship. For more information, please contact [email protected]. WASHINGTON UNIVERSITY IN ST. LOUIS Department of Anthropology Dissertation Examination Committee Crickette Sanz, Chair Kari Allen Benjamin Z. Freed Jane Phillips-Conroy David Strait Mrinalini Watsa Coexistence of Confamilial, Folivorous Indriids, Propithecus diadema and Indri indri, at Betampona Strict -
The Biogeography of Large Islands, Or How Does the Size of the Ecological Theater Affect the Evolutionary Play
The biogeography of large islands, or how does the size of the ecological theater affect the evolutionary play Egbert Giles Leigh, Annette Hladik, Claude Marcel Hladik, Alison Jolly To cite this version: Egbert Giles Leigh, Annette Hladik, Claude Marcel Hladik, Alison Jolly. The biogeography of large islands, or how does the size of the ecological theater affect the evolutionary play. Revue d’Ecologie, Terre et Vie, Société nationale de protection de la nature, 2007, 62, pp.105-168. hal-00283373 HAL Id: hal-00283373 https://hal.archives-ouvertes.fr/hal-00283373 Submitted on 14 Dec 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. THE BIOGEOGRAPHY OF LARGE ISLANDS, OR HOW DOES THE SIZE OF THE ECOLOGICAL THEATER AFFECT THE EVOLUTIONARY PLAY? Egbert Giles LEIGH, Jr.1, Annette HLADIK2, Claude Marcel HLADIK2 & Alison JOLLY3 RÉSUMÉ. — La biogéographie des grandes îles, ou comment la taille de la scène écologique infl uence- t-elle le jeu de l’évolution ? — Nous présentons une approche comparative des particularités de l’évolution dans des milieux insulaires de différentes surfaces, allant de la taille de l’île de La Réunion à celle de l’Amé- rique du Sud au Pliocène. -
For Peer Review
View metadata, citation and similar papers at core.ac.uk brought to you by CORE Page 1 of 57 Journal of Morphology provided by Archivio della Ricerca - Università di Pisa 1 2 3 Title: The locomotion of Babakotia radofilai inferred from epiphyseal and diaphyseal 4 5 6 morphology of the humerus and femur. 7 8 9 Damiano Marchi1,2*, Christopher B. Ruff3, Alessio Capobianco, 1,4, Katherine L. Rafferty5, 10 11 Michael B. Habib6, Biren A. Patel2,6 12 13 14 1 15 Department of Biology, University of Pisa, Pisa, Italy, 56126 16 17 2 18 Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South 19 20 Africa, WITS 2050 For Peer Review 21 22 23 3 Center for Functional Anatomy and Evolution, Johns Hopkins University School of 24 25 26 Medicine, Baltimore, MD 21111 27 28 4 29 Scuola Normale Superiore, Pisa, Italy, 56126 30 31 5 32 Department of Orthodontics, School of Dentistry, University of Washington, Seattle, WA 33 34 35 98195 36 37 6 38 Department of Cell and Neurobiology, Keck School of Medicine, University of Southern 39 40 California, Los Angeles, CA 90033 41 42 43 Text pages: 28; Bibliography pages: 9; Figures: 6; Tables: 6 Appendices: 1 44 45 46 Running title: Babakotia radofilai postcranial suspensory adaptations 47 48 49 *Corresponding author: 50 51 52 Damiano Marchi 53 54 55 56 Address: Dipartimento di Biologia, Università di Pisa, Via Derna, 1 - ZIP 56126, Pisa - Italy 57 58 59 Ph: +39 050 2211350; Fax: +39 050 2211475 60 1 John Wiley & Sons Journal of Morphology Page 2 of 57 1 2 3 Email: [email protected] -
Fossil Lemur from Northern Madagascar (Palaeopropithecidae/Primate Evolution/Postcranium) WILLIAM L
Proc. Natl. Acad. Sci. USA Vol. 88, pp. 9082-9086, October 1991 Evolution Phylogenetic and functional affinities of Babakotia (Primates), a fossil lemur from northern Madagascar (Palaeopropithecidae/primate evolution/postcranium) WILLIAM L. JUNGERSt, LAURIE R. GODFREYt, ELWYN L. SIMONS§, PRITHUJIT S. CHATRATH§, AND BERTHE RAKOTOSAMIMANANA$ tDepartment of Anatomical Sciences, State University of New York, Stony Brook, NY 117948081; tDepartment of Anthropology, University of Massachusetts, Amherst, MA 01003; §Department of Biological Anatomy and Anthropology and Primate Center, Duke University, Durham, NC 27705; and IService de Paldontologie, Universit6 d'Antananarivo, Antananarivo, Madagascar Contributed by Elwyn L. Simons, July 2, 1991 ABSTRACT Recent paleontological expeditions to the An- Craniodental Anatomy and Tooth Shape karana range of northern Madagascar have recovered the partial remains offour individuals ofa newly recognized extinct With an estimated body mass ofjust over 15 kg, Babakotia lemur, Babakoda radofia. Craniodental and postcranial ma- is a medium-sized indroid somewhat larger than the largest terial serve to identify Babakota as a member of the palae- living indrid (Indri) but similar in size to several of the opropithecids (also including the extinct genera Palaeopropith- smallest extinct lemurs, Mesopropithecus and Pachylemur ecus, Archaeoindris, and Mesopropithecus). Living indrids (4). A detailed description of the maxillary dentition of form the sister group to this fossil lade. The postcranial Babakotia exists -
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 Chronology for Late Prehistoric Madagascar
Journal of Human Evolution 47 (2004) 25e63 www.elsevier.com/locate/jhevol A chronology for late prehistoric Madagascar a,) a,b c David A. Burney , Lida Pigott Burney , Laurie R. Godfrey , William L. Jungersd, Steven M. Goodmane, Henry T. Wrightf, A.J. Timothy Jullg aDepartment of Biological Sciences, Fordham University, Bronx NY 10458, USA bLouis Calder Center Biological Field Station, Fordham University, P.O. Box 887, Armonk NY 10504, USA cDepartment of Anthropology, University of Massachusetts-Amherst, Amherst MA 01003, USA dDepartment of Anatomical Sciences, Stony Brook University, Stony Brook NY 11794, USA eField Museum of Natural History, 1400 S. Roosevelt Rd., Chicago, IL 60605, USA fMuseum of Anthropology, University of Michigan, Ann Arbor, MI 48109, USA gNSF Arizona AMS Facility, University of Arizona, Tucson AZ 85721, USA Received 12 December 2003; accepted 24 May 2004 Abstract A database has been assembled with 278 age determinations for Madagascar. Materials 14C dated include pretreated sediments and plant macrofossils from cores and excavations throughout the island, and bones, teeth, or eggshells of most of the extinct megafaunal taxa, including the giant lemurs, hippopotami, and ratites. Additional measurements come from uranium-series dates on speleothems and thermoluminescence dating of pottery. Changes documented include late Pleistocene climatic events and, in the late Holocene, the apparently human- caused transformation of the environment. Multiple lines of evidence point to the earliest human presence at ca. 2300 14C yr BP (350 cal yr BC). A decline in megafauna, inferred from a drastic decrease in spores of the coprophilous fungus Sporormiella spp. in sediments at 1720 G 40 14C yr BP (230e410 cal yr AD), is followed by large increases in charcoal particles in sediment cores, beginning in the SW part of the island, and spreading to other coasts and the interior over the next millennium.