Some Notes on the Egg of Aepyornis Maximus (With Four Photos)
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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, -
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. -
Some Notes on the Egg of Aepyornis Maximus Author(S): Wm
Some Notes on the Egg of Aepyornis maximus Author(s): Wm. C. Bradbury Source: The Condor, Vol. 21, No. 3 (May - Jun., 1919), pp. 97-101 Published by: American Ornithological Society Stable URL: https://www.jstor.org/stable/1362458 Accessed: 14-09-2018 22:51 UTC JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms American Ornithological Society is collaborating with JSTOR to digitize, preserve and extend access to The Condor This content downloaded from 74.202.175.3 on Fri, 14 Sep 2018 22:51:53 UTC All use subject to https://about.jstor.org/terms THE CONDOR A Bi-Monthly Magazine of Western Ornithology Volume XXI May-June, 1919 Number 3 [Issued June 6, 1919] SOME NOTES ON THE EGG OF AEPYORNIS MAXIMUS By WM. C. BRADBURY WITH FOUR PHOTOS IT HAVING been suggested to me that probably many readers of THE CON DOR had never seen the egg of the extinct Aepyornis maximus, and that a description and photographs would be acceptable, I submit the following. Some three years ago, I first saw an egg of this species in the American Museum of Natural History, New York City, and immediately became imbued with a desire to possess one. -
The Cervantes Egg: an Early Malagasy Tourist to Australia
The Cervantes egg: an early Malagasy tourist to Australia l J J. A. Long , P. Vickers-Rich 2, K. Hirsch , E. Bray~ and C. Tuniz' [Department of Earth and Planetary Sciences, Western AustralIan Museum, Francis Street, Perth, Western AustralIa 6000, Australia 2 Earth Sciences Department, Monash University, Clayton, Victoria 3168, Australia , Universi ty of Colorado, Boulder, Colorado, USA. (deceased) 'Museum Geology section, University of Colorado, Boulder, Colorado, USA. '0 AustralIan Nuclear Science and Technology Organisation, Lucas Heights, Sydney, New South Wales 2234, AustralIa Abstract - A large fossil bird's egg discovered near Cervantes in Western Australia is identified as belonging to Acpyomis 11117:\II1I1IS by its size and eggshell structure. It is the second such egg found in Western Australian Holocene beach dune deposits. Radiocarbon dating of the specimen gives an age of about 2000 years. By comparison with other known rafting events, we suggest th"t this egg and the Scott River Acpyonlls egg both drifted .1cross on OCe.1nlC currents from M.1dagascar and were not brought to Austr.1II'l by human intervention. INTRODUCTION belonged to the Crown. An ex gratia payment of A large fossil bird's egg (Figure 1) was $25,000 was later made to the families involved as discovered by three primary school students about a goodwill payment. The legal wrangle 7 km north of the town of Cervantes, in Western surrounding the egg's ownership was thus Australia, in late 1992. It represents the second important in precipitating the first draft such discovery of a very large fossil bird egg from legislation pertaining to fossils and their the dune deposits of southern Western Australia, ownership for the State of Western Australia. -
Science Journals — AAAS
SCIENCE ADVANCES | RESEARCH ARTICLE ARCHAEOLOGY Copyright © 2018 The Authors, some rights reserved; Early Holocene human presence in Madagascar exclusive licensee American Association evidenced by exploitation of avian megafauna for the Advancement James Hansford1,2*, Patricia C. Wright3,4, Armand Rasoamiaramanana5, Ventura R. Pérez6, of Science. No claim to 6 7 7 1 original U.S. Government Laurie R. Godfrey , David Errickson , Tim Thompson , Samuel T. Turvey Works. Distributed under a Creative Previous research suggests that people first arrived on Madagascar by ~2500 years before present (years B.P.). This Commons Attribution hypothesis is consistent with butchery marks on extinct lemur bones from ~2400 years B.P. and perhaps with ar- NonCommercial chaeological evidence of human presence from ~4000 years B.P. We report >10,500-year-old human-modified bones License 4.0 (CC BY-NC). for the extinct elephant birds Aepyornis and Mullerornis, which show perimortem chop marks, cut marks, and de- pression fractures consistent with immobilization and dismemberment. Our evidence for anthropogenic perimortem modification of directly dated bones represents the earliest indication of humans in Madagascar, predating all other archaeological and genetic evidence by >6000 years and changing our understanding of the history of human colonization of Madagascar. This revision of Madagascar’s prehistory suggests prolonged human-faunal coexis- tence with limited biodiversity loss. INTRODUCTION Evidence for the timing of first human arrival in Madagascar Madagascar’s Holocene vertebrate megafauna included giant lemurs, during the late Holocene informs how researchers define pre-human hippopotami, giant tortoises, and the world’s largest birds—the ele- or “pristine” ecosystems, frameworks for understanding ecological phant birds [Aepyornithidae, ~500 kg (1)]. -
Subfossil Lemurs of Madagascar
CHAPTER TWENTY-ONE Subfossil Lemurs of Madagascar LAURIE R. GODFREY, WILLIAM L. JUNGERS, AND DAVID A. BURNEY Madagascar’s living lemurs (order Primates) belong to a radia- on steady, gradual diversifi cation would suggest. We believe tion recently ravaged by extirpation and extinction. There that the latter scenario is more consistent with the fossil are three extinct and fi ve extant families (two with extinct record. members) of lemurs on an island of less than 600,000 km2. The question of how lemurs got to Madagascar is still far This level of familial diversity characterizes no other primate from resolved (Godinot, 2006; Masters et al., 2006; Stevens radiation. The remains of up to 17 species of recently extinct and Heesy, 2006; Tattersall, 2006a, 2006b). It is clear that (or subfossil lemurs) have been found alongside those of still Madagascar (with the Indian plate) separated from Africa extant lemurs at numerous Holocene and late Pleistocene long before primates evolved and that it arrived at its present sites in Madagascar (fi gure 21.1, table 21.1). The closest rela- position relative to Africa by 120–130 Ma (Krause et al., 1997; tives of the lemurs are the lorisiform primates of continental Roos et al., 2004; Masters et al., 2006; Rabinowitz and Woods, Africa and Asia; together with the lemurs, these comprise the 2006). Most scholars favor chance rafting of an ancestral suborder Strepsirrhini. lemur from continental Africa to Madagascar (Krause et al., Most researchers have defended an ancient Gondwanan 1997; Kappeler, 2000; Roos et al., 2004; Rabinowitz and (African or Indo-Madagascan) origin for lemurs. -
Sporormiella and the Late Holocene Extinctions in Madagascar
Sporormiella and the late Holocene extinctions in Madagascar David A. Burney*†, Guy S. Robinson*, and Lida Pigott Burney*‡ *Department of Biological Sciences, Fordham University, Bronx, NY 10458; and ‡The Louis Calder Center Biological Station, Fordham University, P.O. Box K, Armonk, NY 10504 Communicated by Henry T. Wright, University of Michigan, Ann Arbor, MI, July 24, 2003 (received for review January 25, 2003) Fossil spores of the dung fungus Sporormiella spp. in sediment cores from throughout Madagascar provide new information concerning megafaunal extinction and the introduction of livestock. Sporormiella percentages are very high in prehuman southwest Madagascar, but at the site with best stratigraphic resolution the spore declines sharply by Ϸ1,720 yr B.P. (radiocarbon years ago). Within a few centuries there is a concomitant rise in microscopic charcoal that probably represents human transformation of the local environment. Reduced megaherbivore biomass in wooded savannas may have resulted in increased plant biomass and more severe fires. Some now-extinct taxa persisted locally for a millennium or more after the inferred megafaunal decline. Sites in closed humid forests of northwest Madagascar and a montane ericoid formation of the central highlands show only low to moderate Sporormiella percentages before hu- mans. A subsequent rise in spore concentrations, thought to be evidence for livestock proliferation, occurs earliest at Amparihibe in the northwest at Ϸ1,130 yr B.P. ossil spores of the dung fungus Sporormiella spp. have been Fshown in western North America to serve as a reliable proxy for megafaunal biomass in late Pleistocene sediments. These spores decline rapidly at the end of the Pleistocene at the approximate time of megafaunal extinctions and increase again in sediments of recent centuries after livestock introduction (1, 2). -
Island Extinctions: Processes, Patterns, and Potential for Ecosystem Restoration
Island extinctions: processes, patterns, and potential for ecosystem restoration JAMIE R. WOOD1, JOSEP A. ALCOVER2, TIM M. BLACKBURN3,4, PERE BOVER2, RICHARD P. DUNCAN5, JULIAN P. HUME6, JULIEN LOUYS7, HANNEKE J. M. MEIJER8, JUAN C. RANDO9, JANET M. WILMSHURST1,10 1Landcare Research, Lincoln 7640, New Zealand; 2Institut Mediterrani d’Estudis Avançats (CSIC-UIB), Spain; 3Department of Genetics, Evolution & Environment, Centre for Biodiversity & Environment Research, University College London, Gower Street, London, WC1E 6BT, United Kingdom; 4Institute of Zoology, Zoological Society of London, Regent’s Park, London, NW1 4RY, United Kingdom; 5Institute for Applied Ecology, University of Canberra, ACT 2617, Australia; 6Department of Life Sciences, Natural History Museum, Akeman St, Tring, Herts HP23 6AP, United Kingdom; 7Department of Archaeology and Natural History, School of Culture, History and Languages, The Australian National University, Canberra, ACT, Australia; 8University Museum of Bergen, Department of Natural History, University of Bergen, Postboks 7800 5007 Bergen, Norway; 9Departamento de Biología Animal (UDI Zoología), Universidad de La Laguna, La Laguna, Tenerife, Canary Islands, Spain; 10 School of Environment, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand. SUMMARY Extinction has altered island ecosystems throughout the late Quaternary. Here, we review the main historic drivers of extinctions on islands, the patterns in extinction chronologies between islands, and the potential for restoring ecosystems through reintroducing extirpated species. While some extinctions have been caused by climatic and environmental change most have been caused by anthropogenic impacts. We propose a general model to describe patterns in these anthropogenic island extinctions. A general model describing patterns in anthropogenic island extinctions is proposed. -
Early Illustrations of Aepyornis Eggs (1851-1887): from Popular Science to Marco Polo’S Roc Bird
anthropozoologica 2019 ● 54 ● 12 Early illustrations of Aepyornis eggs (1851-1887): from popular science to Marco Polo’s roc bird Eric BUFFETAUT art. 54 (12) — Published on 6 September 2019 www.anthropozoologica.com DIRECTEUR DE LA PUBLICATION : Bruno David, Président du Muséum national d’Histoire naturelle RÉDACTRICE EN CHEF / EDITOR-IN-CHIEF: Joséphine Lesur RÉDACTRICE / EDITOR: Christine Lefèvre RESPONSABLE DES ACTUALITÉS SCIENTIFIQUES / RESPONSIBLE FOR SCIENTIFIC NEWS: Rémi Berthon ASSISTANTE DE RÉDACTION / ASSISTANT EDITOR: Emmanuelle Rocklin ([email protected]) MISE EN PAGE / PAGE LAYOUT: Emmanuelle Rocklin, Inist-CNRS COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD: Cornelia Becker (Freie Universität Berlin, Berlin, Allemagne) Liliane Bodson (Université de Liège, Liège, Belgique) Louis Chaix (Muséum d’Histoire naturelle, Genève, Suisse) Jean-Pierre Digard (CNRS, Ivry-sur-Seine, France) Allowen Evin (Muséum national d’Histoire naturelle, Paris, France) Bernard Faye (Cirad, Montpellier, France) Carole Ferret (Laboratoire d’Anthropologie Sociale, Paris, France) Giacomo Giacobini (Università di Torino, Turin, Italie) Véronique Laroulandie (CNRS, Université de Bordeaux 1, France) Marco Masseti (University of Florence, Italy) Georges Métailié (Muséum national d’Histoire naturelle, Paris, France) Diego Moreno (Università di Genova, Gènes, Italie) François Moutou (Boulogne-Billancourt, France) Marcel Otte (Université de Liège, Liège, Belgique) Joris Peters (Universität München, Munich, Allemagne) François Poplin (Muséum national d’Histoire naturelle, -
Holocene Extinctions and the Loss of Feature Diversity
CHAPTER 14 Holocene extinctions and the loss of feature diversity Arne Ø. Mooers, Simon J. Goring, Samuel T. Turvey, and Tyler S. Kuhn mouse 2}, because, on the tree, species {mouse 1} 14.1 Introduction preserves much of the feature diversity represented Species are hard to de/ ne, but under all de/ nitions by {beaver, mouse 2}. We can say that each of {bea- they are unique. Each species can be considered to ver, mouse 1, mouse 2} are redundant with respect possess a set of unique characters which comprise to the features represented by the rodent lineage its feature diversity, the diversity that would be lost that gave rise to them. when that species goes extinct. However, because The mouse/aardvark comparison and Fig. 14.1 species differentiate via evolution from other spe- allow us to consider a set of interesting observa- cies, they also share features as a function of degree tions about how feature diversity is distributed of relationship. So, within placental mammals, all across biodiversity, and what the impacts of his- mice share all the characteristics that allow us to torically and prehistorically recent (i.e. Holocene) call something a mouse, whereas the sole living extinctions have been on this distribution. First, species of aardvark shares very few basic mam- it is now well known that biodiversity is very mal characteristics with anything: it must be true unevenly distributed across the tree of life: the fact that the Earth loses less diversity when any single that at the ordinal level the mammals are approxi- mouse species goes extinct than when the last liv- mately 50% rodents (Rodentia) and 0.02% aard- ing aardvark shuf7 es off its mortal coil. -
The Elephant Birds of Madagascar 17Th Century
NEWS & VIEWS offered for (illegal) sale as curios. A little- The Arabian Nights. The rokh, so the story known fact about the eggs is that until as goes, was an eagle-like bird so enormous recently as the mid-19th century they were that it preyed on elephants. There is good used by humans to transport liquids. There reason to suspect that this fanciful tale enormous, is something distinctly surreal about the originated from birds that occurred on notion of a gigantic egg, several centuries Madagascar, and elephant birds have long old, being used as a water container by a been seen as the obvious candidates. thirsty Malagasy traveller. But Steven Goodman and William enigmatic & extinct All the elephant birds were extinct by the Jungers have recently pointed out that The elephant birds of Madagascar 17th century. A French governor stationed another extinct Malagasy bird could in Madagascar during the mid-1600s men- have contributed to the origin of this n the mid-1800s three huge eggs Aepyornis and three Mullerornis species, mainly in forests, since the spiny vegeta- tioned ostrich-like birds that occurred in legend. Belonging to the same genus and were transported from Madagas- although the actual numbers remain un- tion typical of Madagascar’s arid regions remote regions, but he did not see them WIKIMEDIA COMMONS (2) approxi mately the same size as Africa’s car to France, and the Western clear. This uncertainty reflects the fact generally is characterised by other, iso- at first hand. There is no way of knowing Aepyornis skull on display in the National Crowned Eagle, Stephanoaetus mahery worldI came to learn that this island had that all these species were described topically distinct, photosynthetic path- whether the birds still existed at that time Museum of Natural History, Paris. -
Pleistocene-Holocene Extinctions: Distinguishing Between Anthropic and Climatic Causes
Universidade Federal do Rio de Janeiro Instituto de Biologia Programa de Pós-Graduação em Ecologia Pleistocene-Holocene extinctions: distinguishing between anthropic and climatic causes Bernardo Barros de Alvarenga Araujo Supervisor: Fernando A. dos Santos Fernandez Co-supervisor: José Alexandre F. Diniz-Filho Rio de Janeiro, RJ, Brazil - 2013 "The beauty and genius of a work of art may be reconceived, though its first material expression be destroyed; a vanished harmony may yet again inspire the composer; but when the last individual of a race of living beings breathes no more, another heaven and another earth must pass before such a one can be again." William Beebe, The Bird (1906). ACKNOWLEDGEMENTS Although this is one of the most enjoyable sections to write in a dissertation – mainly because it is a space to acknowledge the importance of many people I hold dear and because it is (hopefully) a red marker free zone – I will try to make it as quick as possible. First, I would like to thank my family for the infinite care offered throughout… well, through my whole life, but particularly in the years I’ve been in college. For eight years now I’ve had two homes filled with people who gave me nothing but love and incentive, and I couldn’t possibly begin to explain how much their support has meant (and will continue to mean) to me. In the respect of support, friends are also worth mentioning, especially the ones at the Laboratório de Ecologia e Conservação de Populações (Laboratory of Population Ecology and Conservation; LECP) of Universidade Federal do Rio de Janeiro (UFRJ), not only for the countless discussions and suggestions that were so valuable for the development of the present dissertation, but also for composing a working environment that is at the same time focused, greatly productive and so incredibly pleasant to inhabit.