MARINE MAMMALS, EXTINCTIONS of Glenn R

Total Page:16

File Type:pdf, Size:1020Kb

MARINE MAMMALS, EXTINCTIONS of Glenn R MARINE MAMMALS, EXTINCTIONS OF Glenn R. VanBlaricom,* Leah R. Gerber,† and Robert L. Brownell, Jr.‡ *U.S. Geological Survey and University of Washington, †University of California, Santa Barbara, and ‡National Marine Fisheries Service I. Introduction principal source for taxonomic nomenclature, includ- II. Patterns and Case Studies of Extinction in ing common names, is the recent review of Rice (1998). Marine Mammals The order Cetacea includes whales, dolphins, and III. Discussion porpoises (Table I). The ‘‘pinnipedia’’ is a group of species in three families in the mammalian order Carni- vora (Table I). The pinnipeds include the seals, fur seals, sea lions, and walrus. The term pinnipedia is no I. INTRODUCTION longer recognized formally by marine mammal taxono- mists, but it continues to appear in the systematic ver- A. Taxonomic Definition of nacular as a matter of tradition and convenience. The order Sirenia includes the extant manatees and dugong ‘‘Marine Mammals’’ and the extinct Steller’s sea cow (Table I). The order The marine mammals include one extinct order and Desmostylia is the only recognized order of marine three major extant taxa that were or are fully aquatic, mammals to become entirely extinct. in most cases occurring entirely in the marine habitats Two largely terrestrial families of the order Carnivora of the major ocean basins and associated coastal seas also include species recognized as marine mammals and estuaries. In addition, a few species of largely terres- (Table I). Sea otters and chungungos (family Mustel- trial taxa are currently regarded as marine mammals. idae) live entirely or primarily in marine habitats. Polar We consider 127 recent mammal species in total to bears (family Ursidae) also spend a significant propor- be marine mammals for purposes of this review. We tion of time at sea. acknowledge that species numbers within any taxon Many other species of mammal utilize aquatic or are subject to revision as new systematic methods and marine habitats, including monotremes, ursids, mustel- philosophies emerge. Our primary bases for defining ids, canids, primates, rodents, bats, and ungulates. Ulti- our list of marine mammal species are the protocols of mately, the distinction among aquatic, marine, and the U.S. federal government, determined largely by the terrestrial taxa is arbitrary. Thus, our reliance on defini- U.S. Marine Mammal Protection Act (MMPA) of 1972 tions and protocols of MMPA, NMFS, and FWS is sub- [16 U.S.C. §§1361-62, 1371-84, and 1401-07 (Supp. jective, although it is consistent with common practice IV 1974)] as amended (MMPA) and managed by two at least in the United States. U.S. federal agencies, the National Marine Fisheries We use the term ‘‘marine’’ to refer to large, contigu- Service (NMFS) and the Fish and Wildlife Service ous aqueous habitats with significant dissolved salt con- (FWS). Our choice of defining criteria is arbitrary. Our tent in ambient waters. Thus, we apply the term marine Encyclopedia of Biodiversity, Volume 4 Copyright 2001 by Academic Press. All rights of reproduction in any form reserved. 37 38 MARINE MAMMALS, EXTINCTIONS OF TABLE I TABLE II Major Taxa and Species Numbers of Marine Mammalsa Distinguishing Characteristics of the Major Marine Mammal Taxa Taxon No. of species Characteristic Cetacea Sirenia Pinnipedia Cetacea: Whales 83 Mysticeti: Baleen whales 12 Body streamlined x x x Balaenidae: Right whales 2 Limbs modified x x x Neobalaenidae: Pygmy right whale 1 Rear limbs modified as x Eschrichtidae: Gray whale 1 flippers Balaenopteridae: Rorquals 8 Rear limbs and pelvic girdle x x Odontoceti: Toothed whales 71 absent Physeteridae: Sperm whales 1 Propulsion by caudal spine x x Kogiidae: Pygmy sperm whales 2 and flukes Ziphiidae: Beaked whales 20 Loss of pelage x x Platanistidae: Indian river dolphin 1 Iniidae: Amazon river dolphin 1 Subcutaneous blubber layer x x x Lipotidae: Chinese river dolphin 1 Simplification of dentition x x x Pontoporiidae: La Plata dolphin 1 Expansion of anterior skull x Monodontidae: Beluga and narwhal 2 Development of acoustic capa- xa xa Delphinidae: Dolphins 36 bility for communication Phocoenidae: Porpoises 6 and echolocation Carnivora, ‘‘Pinnipedia’’ 36 Amphibious capability x Otariidae: Sea lions and fur seals 16 Odobenidae: Walrus 1 a Echolocation capability is known only for the odontocete ceta- Phocidae: Seals 19 ceans. Carnivora, other marine taxa 3 Mustelidae: Marine otters 2 Ursidae: Polar bear 1 Sirenia: Manatees, dugongs, and sea cows 5 lated approximately with the duration of the evolution- Trichechidae: Manatees 3 ary history of the major marine mammal taxa. Dugongidae: Dugong and Steller’s sea cow 2 Although marine mammals are largely defined by marked departures from the terrestrial mammalian Total species 127 model, it is instructive to consider major features of a terrestrial mammals retained in marine mammals. In Following the conventions of Rice (1998). the context of extinction processes in general, and an- thropogenic extinctions in particular, two retained fea- to the world’s oceans, seas, and estuaries. We apply the tures are of particular importance. First, although most term ‘‘aquatic’’ to aqueous habitats without significant marine mammals spend most of their lives immersed measurable dissolved salt concentrations in ambient at sea, they retain largely terrestrial respiratory architec- waters, such as lakes and rivers above the elevation of ture and must surface and breathe in order to exchange significant mixing with marine waters, and to inland respiratory gasses. Second, marine mammals are ho- saline lakes that lack outlet streams connecting to ma- meothermic, with core body temperatures typically near rine habitats. ‘‘Terrestrial’’ habitats are those lacking 38ЊC, like their terrestrial relatives. The need to breathe standing water in normal circumstances. As indicated at the surface and the need for major anatomical adjust- in Table I, our list of ‘‘marine mammals’’ includes ma- ment to minimize rates of heat loss are constraints that rine and aquatic species. foster vulnerability to unsustainable rates of exploita- tion and to certain types of pollution. The significance 1. General Features and Habitat Boundaries of these constraints is developed in the case studies we Compared to terrestrial mammals, marine mammals are present later. characterized by many striking modifications in anat- The diving capabilities of marine mammals define omy, physiology, and ecology (Table II). In some cases, the three-dimensional nature of their habitats at sea. the modifications are sufficiently extreme that phyloge- Nearly all extant marine mammals dive to forage, al- netic linkages to terrestrial ancestry are obscured and though the ranges of diving capability and pattern difficult to resolve. The degree of modification is corre- are broad. Most marine mammals also spend signifi- MARINE MAMMALS, EXTINCTIONS OF 39 cant time submerged while traveling, socializing, or with small breathing holes, beluga whales and narwhals breeding. are also taken as food by polar bears. Thus, the extent Among cetaceans, sperm whales and beaked whales to which the at-sea habitat of marine mammals is truly likely dive the deepest and longest compared to other three-dimensional varies widely among the major taxa species. Sperm whales can dive to 1500 m, remaining and the individual species. Within species, there is also submerged for 20 min or more. The diving behavior of marked ontogenetic variation in diving capability and beaked whales is poorly known, but there is emerging pattern. evidence that beaked whales may also routinely make The marine mammals are geographically ubiquitous repetitive dives of long duration to great depth. Baleen in the world’s oceans, seas, and estuaries. Cetaceans whales may make long deep dives during breeding sea- occur in marine environments at all latitudes. For exam- son. Foraging dives of baleen whales normally are rela- ple, killer whales and minke whales may have the largest tively shallow and brief. Many of the smaller cetaceans natural geographic ranges of the earth’s mammals. Most commonly dive for less than 10 min at a time to depths of the mysticetes and some of the larger odontocetes no greater than a few hundred meters. have global ranges or are distributed antitropically. Among pinnipeds, elephant seals (Phocidae) have Smaller cetaceans are widely dispersed as well, although maximum diving capabilities comparable to the sperm individual populations typically concentrate in regions whales, and they are known to make remarkably long of predictably high local biological productivity. Several sequences of repetitive deep (to 1500 m), long (20 min species of small cetacean, including two delphinids, a or more) dives with surface intervals of only 2 or 3 phocoenid, and the four monotypic families of river min. These sequences may be maintained day and night dolphins, are found in major river systems in South for tens of days at a time. Many other phocid seals are America and Asia. Beluga whales also spend significant thought to have similar capabilities. The sea lions and time in river habitats. Pinnipeds occur in all the world’s fur seals (Otariidae), in contrast, usually dive for only major marine habitats, but most species are concen- a few minutes at a time, and usually to maximum depths trated in middle or high latitudes, in close association of a few hundred meters, although many otariids are with regions of high productivity. In addition, there known to be capable of continuous sequences of repeti- are several pinniped species or populations confined to tive shallow dives of 10–12 hr or more. Walruses are isolated large lakes in Europe, Asia, and North America. known to dive as deep as 80 m, with maximum dura- Most sirenians are limited to tropical or subtropical tions of 10 min. latitudes, in shallow seas that provide adequate macro- In contrast to cetaceans and pinnipeds, sirenians are phytic food and refuge from predation, and are ther- weak divers, normally remaining in shallow water (Ͻ20 mally tolerable. The sea otter is confined to the coastal m) and diving for only 2 or 3 min when active.
Recommended publications
  • Evolução, Hegemonia E Desaparecimento Dos Sirénios Dos Mares Europeus Ao Longo Do Cenozoico
    Universidade de Lisboa Faculdade de Ciências Departamento de Geologia Evolução, hegemonia e desaparecimento dos sirénios dos mares europeus ao longo do Cenozoico causas endógenas (alterações climáticas globais) ou exógenas (ambiente galáctico)? Gonçalo Abreu Prista Dissertação Mestrado em Ciências do Mar 2012 Universidade de Lisboa Faculdade de Ciências Departamento de Geologia Evolução, hegemonia e desaparecimento dos sirénios dos mares europeus ao longo do Cenozoico causas endógenas (alterações climáticas globais) ou exógenas (ambiente galáctico)? Gonçalo Abreu Prista Dissertação Mestrado em Ciências do Mar Orientadores: Professor Doutor Mário Albino Cachão Professor Doutor Rui Jorge Agostinho 2012 EVOLUÇÃO, HEGEMONIA E DESAPARECIMENTO DOS SIRÉNIOS DOS MARES EUROPEUS AO LONGO DO CENOZOICO causas endógenas (alterações climáticas globais) ou exógenas (ambiente galáctico)? GONÇALO ABREU PRISTA ORIENTAÇÃO CIENTÍFICA: PROF. DOUTOR MÁRIO ALBINO PIO CACHÃO Professor Auxiliar Agregado do Departamento de Geologia da Faculdade de Ciências da Universidade de Lisboa Membro do Centro de Geologia da Universidade de Lisboa PROF. DOUTOR RUI JORGE AGOSTINHO Professor Auxiliar Agregado do Departamento de Física da Faculdade de Ciências da Universidade de Lisboa Membro do Centro de Astronomia e Astrofísica da Universidade de Lisboa Director do Observatório Astronómico de Lisboa iii "Graças aos descobrimentos da Paleontologia, a História Natural é História, no sentido literal da palavra" Albert Gaudry (1827 - 1908). "O azoto no nosso DNA, o cálcio nos nossos dentes, o ferro no nosso sangue, o carbono nas nossas tartes de maçã foram feitos no interior de estrelas em colapso. Nós somos feitos de material estelar" Carl Sagan (1934 - 1996) iv AGRADECIMENTOS Primeiro aos meus pais, pois sem o seu apoio, a todos os níveis, este mestrado e esta dissertação não seriam possíveis.
    [Show full text]
  • Sirenian Feeding Apparatus: Functional Morphology of Feeding Involving Perioral Bristles and Associated Structures
    THE SIRENIAN FEEDING APPARATUS: FUNCTIONAL MORPHOLOGY OF FEEDING INVOLVING PERIORAL BRISTLES AND ASSOCIATED STRUCTURES By CHRISTOPHER DOUGLAS MARSHALL A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNrVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REOUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 1997 DEDICATION to us simply as I dedicate this work to the memory of J. Rooker (known "Rooker") and to sirenian conservation. Rooker was a subject involved in the study during the 1993 sampling year at Lowry Park Zoological Gardens. Rooker died during the red tide event in May of 1996; approximately 140 other manatees also died. During his rehabilitation at Lowry Park Zoo, Rooker provided much information regarding the mechanism of manatee feeding and use of the perioral bristles. The "mortality incident" involving the red tide event in southwest Florida during the summer of 1996 should serve as a reminder that the Florida manatee population and the status of all sirenians is precarious. Although some estimates suggest that the Florida manatee population may be stable, annual mortality numbers as well as habitat degradation continue to increase. Sirenian conservation and research efforts must continue. ii ACKNOWLEDGMENTS Research involving Florida manatees required that I work with several different government agencies and private parks. The staff of the Sirenia Project, U.S. Geological Service, Biological Resources Division - Florida Caribbean Science Center has been most helpful in conducting the behavioral aspect of this research and allowed this work to occur under their permit (U.S. Fish and Wildlife Permit number PRT-791721). Numerous conversations regarding manatee biology with Dr.
    [Show full text]
  • El Manatí Anmari Álvarez Alemán
    mamíferos en cuba 4.1 MAMÍFEROS ACUÁTICOS El manatí ANMAri ÁLVAREZ ALEMÁN Diversidad y evolución de los sirenios E l manatí es la única especie herbívora del grupo de los mamíferos marinos que forma parte de la fauna marina autóctona cubana (fig.1). Pertenece a Sirenia, orden que des cierra permanentemente esta conexión. está dividido en dos familias, Dugongidae y Trichechidae, Este fenómeno indujo un flujo de nu- y cuyos integrantes comparten muchas características con trientes y sedimentos a lo largo otros mamíferos marinos como los cetáceos: cuerpo hi- de la cuenca del Amazonas, que drodinámico, piel gruesa y reducción de las extremidades, conllevó a que las plantas acuá- entre otras; sin embargo, no están emparentados. Los sire- ticas tuvieran un alto contenido de nios pertenecen a un grupo de mamíferos referidos como sílice y por lo tanto fueran más abrasivas para subungulados, los cuales están evolutivamente relaciona- los dientes. De esta manera, la evolucion favo- dos. En este grupo también encontramos los órdenes Pro- reció una dentición con reemplazo horizontal de boscidea (elefantes), Hyracoidea (damanes) y Tubulidenta- los dientes para favorecer la alimentacion con este tipo de a ta (cerdo hormiguero). plantas abrasivas. El triquéquido Ribodon evolucionó en El linaje de los sirenios parece haber surgido en el viejo estas nuevas condiciones dando lugar a los manatíes 179 mundo durante el Eoceno, hace 50 millones de años. Los actuales, cuyas estructuras craneales tienen una estudios paleontológicos señalan la presencia de otras dos dentición capaz de alimentarse de las plantas mari- familias fósiles dentro del orden Sirenia: Prorastomidae y nas (fig.2).
    [Show full text]
  • SUPPLEMENTARY INFORMATION: Tables, Figures and References
    Samuels et al. Evolution of the patellar sesamoid bone in mammals SUPPLEMENTARY INFORMATION: Tables, Figures and References Supplementary Table S1: Mammals$ Higher taxa Genus sp. Estimated. age of Patellar Comments# (partial) specimen, location state 0/1/2 (absent/ ‘patelloid’/ present) Sinoconodonta Sinoconodon Jurassic 0 Patellar groove absent, suggests no rigneyi (Kielan- patella Jaworowska, Cifelli & Luo, Sinoconodon is included on our 2004) phylogeny within tritylodontids. Morganucodonta Megazostrodon Late Triassic, southern 0 rudnerae (Jenkins Africa & Parrington, 1976) Morganucodonta Eozostrodon sp. Late Triassic, Wales 0 Asymmetric patellar groove, (Jenkins et al., specimens disarticulated so it is hard 1976) to assess the patella but appears absent Docodonta Castorocauda 164 Mya, mid-Jurassic, 0 Semi-aquatic adaptations lutrasimilis (Ji, China Luo, Yuan et al., 2006) Docodonta Agilodocodon 164 Mya, mid-Jurassic, 0 scansorius China (Meng, Ji, Zhang et al., 2015) Docodonta Docofossor 160 Mya 0 brachydactylus (Luo, Meng, Ji et al., 2015) Docodonta Haldanodon 150-155 Mya, Late 0 Shallow patellar groove exspectatus Jurassic, Portugal (Martin, 2005b) Australosphenida Asfaltomylos Mid-Jurassic, South ? Postcranial material absent patagonicus America (Martin, 2005a) Australosphenida Ornithorhynchus Extant 2 Platypus, genome sequenced Monotremata anatinus (Warren, Hillier, Marshall Graves et (Herzmark, 1938; al., 2008) Rowe, 1988) Samuels et al. Australosphenida Tachyglossus + Extant 2 Echidnas Monotremata Zaglossus spp. (Herzmark, 1938; Rowe, 1988) Mammaliaformes Fruitafossor 150 Mya, Late Jurassic, 0 Phylogenetic status uncertain indet. windscheffeli (Luo Colorado & Wible, 2005) Mammaliaformes Volaticotherium Late Jurassic/Early ? Hindlimb material incomplete indet. antiquus (Meng, Cretaceous Hu, Wang et al., 2006) Eutriconodonta Jeholodens 120-125 Mya, Early 0 Poorly developed patellar groove jenkinsi (Ji, Luo Cretaceous, China & Ji, 1999) Eutriconodonta Gobiconodon spp.
    [Show full text]
  • 25 Squires and Fritsche
    25 SQUIRES AND FRITSCHE Isurus sp. TRACE FOSSILS PI. 4, fig. 8 Unidentified burrows Isurus sp. (mako shark) teeth are the most " common shark teeth in the Sespe Creek area. Most The few unidentified burrows collected from the are moderately well preserved, nearly complete or Vaqueros Formation are about 9 cm long and about 1.5 complete, and not rounded by abrasion. Average cm in diameter. Burrows are more abundant in the length of complete specimens is about 1.5 cm; larger Santa Margarita Formation, where the most common type fragments are about 2.5 cm in length. is vertical, 1 to 3 cm in diameter, and straight to slightly curving. Some forms are branching, and at Genus Carcharodon Smith in Muller and Henle, 1838 locality 287, some resemble Ophiomorpha. Carcharodon angustidens L. Agassiz Kingdom PLANTAE PI. 4, fig. 3 Division RHODOPHYCOPHYTA Class RHODOPHYCEAE Carcharodon angustidens L. Agassiz, 1843, p. 255, Order CRYPTQNEMIALES pi. 28, figs. 20-25. Leriche, p. 13-14, pi. 11, figs. 8, 8a, 8b. Family Corallinaceae The figured specimen (PI. 4, fig. 3) of Carchar- Abundant whole and fragmented specimens of. an odon angustidens (great white shark) is a 6-cm-long unidentified coralline alga occur in a thin bed at tooth. Other specimens found include only a few locality 313. Small hemispherical colonies up to fragments. Remains of Carcharodon are previously 2.5 cm in height were collected, but most of the unreported from the Vaqueros Formation in the Sespe specimens are scattered fragments separated by Creek region (Loel and Corey, 1932). medium-grained sandstone.
    [Show full text]
  • IDL-1426.Pdf
    The International Development Research Centre is a public corporation created by the Parliament of Canada in 1970 to support research designed to adapt science and technology to the needs of developing countries. The Centre's activity is concentrated in five sectors: agriculture, food and nutrition sciences; health sciences; information sciences; communications; and social sciences. IDRC is financed solely by the Government of Canada; its policies, however, are set by an international Board of Governors. The Centre's headquarters are in Ottawa, Canada. Regional offices are located in Africa, Asia, Latin America, and the Middle East. ©1978 International Development Research Centre Postal Address: Box 8500, Ottawa, Canada KlG 3H9 Head Office: 60 Queen Street, Ottawa Ronald, K. Selley, L.J. Amoroso, E.C. IDRC IDRC-TS13e Biological synopsis of the manatee. Ottawa, IDRC, 1978. 112 p. /IDRC publication/. Monograph on the manatee, an aquatic mammal (/animal species/) of the /tropical zone/s of I Africa south of Sahara/ and /Latin America/, with an extensive /bibliography/ - discusses the /classification/ of the species and subspecies of the genus Trichechus; /morphology/, /physiology/, /behaviour/, /reproduction/, /animal ecology/ (role in /aquatic plant/ /weed control/), and measures for /animal protection/ of the manatee. UDC: 599.55 ISBN: 0-88936-168-1 Microfiche edition available IDRC-TS13e Biological Synopsis of the Manatee K. Ronald, L.J. Selley, and E.C. Amoroso1 College ofBiological Science, University of Guelph, Guelph, Ontario 1 Present address: Agricultural Research Council, Institute of Animal Physiology, Babraham, Cambridge, England. This work was carried out with the aid of a grant from the International Development Research Centre.
    [Show full text]
  • Evolution of the Sirenia: an Outline
    Caryn Self-Sullivan, Daryl P. Domning, and Jorge Velez-Juarbe Last Updated: 8/1/14 Page 1 of 10 Evolution of the Sirenia: An Outline The order Sirenia is closely associated with a large group of hoofed mammals known as Tethytheria, which includes the extinct orders Desmostylia (hippopotamus-like marine mammals) and Embrithopoda (rhinoceros-like mammals). Sirenians probably split off from these relatives in the Palaeocene (65-54 mya) and quickly took to the water, dispersing to the New World. This outline attempts to order all the species described from the fossil record in chronological order within each of the recognized families of Prorastomidae, Protosirenidae, Dugongidae, and Trichechidae. This outline began as an exercise in preparation for my Ph. D. preliminary exams and is primarily based on decades of research and peer-reviewed literature by Dr. Daryl P. Domning, to whom I am eternally grateful. It has been recently updated with the help of Dr. Jorge Velez-Juarbe. However, this document continues to be a work-in-progress and not a peer reviewed publication! Ancestral line: Eritherium Order Proboscidea Elephantidae (elephants and mammoths) Mastodontidae Deinotheriidae Gomphotheriidae Ancestral line: Behemotops Order Desmostylia (only known extinct Order of marine mammal) Order Sirenia Illiger, 1811 Prorastomidae Protosirenidae Dr. Daryl Domning, Howard University, November 2007 Dugongidae with Metaxytherium skull. Photo © Caryn Self-Sullivan Trichechidae With only 5 species in 2 families known to modern man, you might be surprised to learn that the four extant species represent only a small fraction of the sirenians found in the fossil record. As of 2012, ~60 species have been described and placed in 4 families.
    [Show full text]
  • Novitates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET, NEW YORK, N.Y
    AMERICANt MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2870, pp. 1-8, figs. 1-3 April 6, 1987 Selected Features of the Desmostylian Skeleton and Their Phylogenetic Implications MICHAEL J. NOVACEK1 AND ANDRE R. WYSS2 ABSTRACT According to several standard descriptions, des- pertaining to these traits are either in error, or have mostylians lack certain specializations shared by alternative phylogenetic implications. Hence, proboscideans, sirenians, and hyracoids. These comparisons of these conditions do not exclude specializations are amastoidy and the serial ar- desmostylians from the superordinal group Teth- rangement ofthe carpals with the concomitant loss ytheria (proboscideans and sirenians) or the more of contact between the lunar and unciform. We inclusive Paenungulata (tethytheres and hyra- argue that original descriptions of desmostylians coids). INTRODUCTION The Desmostylia are an extinct order of be more conservative than sirenians (and, by mammals with specializations ofthe skeleton implication, proboscideans) with respect to suitable for an amphibious mode of life. Al- the reduction ofmastoid exposure (Hay, 1915; though this group was formerly associated Abel, 1922; VanderHoof, 1937) and the se- with the aquatic Sirenia (Simpson, 1945), and rial arrangement ofthe carpal elements (Shi- is now placed within a superordinal category kama, 1966). These differences have influ- Tethytheria, which also includes the Probos- enced more recent students of the problem cidea and Sirenia (McKenna, 1975), these (e.g., Tassy, 1981), who have opted for a close avowed relationships present some prob- association ofProboscidea (including the late lems. According to standard descriptions, Eocene-early Oligocene genus Moeritheri- desmostylians lack certain skeletal special- um) and Sirenia to the exclusion of Desmo- izations shared by Proboscidea and Sirenia.
    [Show full text]
  • First Record of the Family Protocetidae in the Lutetian of Senegal (West Africa)
    ARTICLE First record of the family Protocetidae in the Lutetian of Senegal (West Africa) LIONEL HAUTIERa, RAPHAËL SARRb, FABRICE LIHOREAUa, RODOLPHE TABUCEa & PIERRE MARWAN HAMEHc aInstitut des Sciences de l’Evolution de Montpellier, Université Montpellier 2, CNRS, IRD, Cc 064; place Eugène Bataillon, 34095 Montpellier Cedex 5, France bDépartement de Géologie, Faculté des Sciences et Techniques, Université Cheikh-Anta-Diop de Dakar, B. P. 5005 Dakar-Fann, Sénégal cCOGITECH, B.P. A362 Thiès, Senegal * corresponding author: [email protected] Abstract: The earliest cetaceans are found in the early Eocene of Indo-Pakistan. By the late middle to late Eocene, the group colonized most oceans of the planet. This late Eocene worldwide distribution clearly indicates that their dispersal took place during the middle Eocene (Lutetian). We report here the first discovery of a protocetid fossil from middle Eocene deposits of Senegal (West Africa). The Lutetian cetacean specimen from Senegal is a partial left innominate. Its overall form and proportions, particularly the well-formed lunate surface with a deep and narrow acetabular notch, and the complete absence of pachyostosis and osteosclerosis, mark it as a probable middle Eocene protocetid cetacean. Its size corresponds to the newly described Togocetus traversei from the Lutetian deposits of Togo. However, no innominate is known for the Togolese protocetid, which precludes any direct comparison between the two West African sites. The Senegalese innominate documents a new early occurrence of this marine group in West Africa and supports an early dispersal of these aquatic mammals by the middle Eocene. Keywords: innominate, Lutetian, Protocetid, Senegal Submitted 9 October 2014, Accepted 17 November 2014 © Copyright Lionel Hautier November 2014 INTRODUCTION cetacean found to date, seems to have been lost (pers.
    [Show full text]
  • Two New Oligocene Desmostylians and a Discussion of Tethytherian Systematics
    SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER 59 Two New Oligocene Desmostylians and a Discussion of Tethytherian Systematics Daryl P. Domning, Clayton E. Ray, and Malcolm C. McKenna SMITHSONIAN INSTITUTION PRESS City of Washington 1986 ABSTRACT Domning, Daryl P., Clayton E. Ray, and Malcolm C. McKenna. Two New Oligocene Desmostylians and a Discussion of Tethytherian Systematics. Smith­ sonian Contributions to Paleobiology, number 59, 56 pages, 23 figures, 1986.— A new genus, comprising two new species of desmostylians, is de­ scribed from marine Oligocene deposits of the Pacific Northwest. Behemotops proteus, new genus, new species, is based on an immature mandibular ramus and apparently associated skeletal fragments from the middle or (more likely) upper Oligocene lower part of the Pysht Formation of Clallam County, Washington. A related new species, Behemotops emlongi, is founded on a mandibular ramus of an old individual and a mandibular fragment with canine tusk from the uppermost Oligocene (early Arikareean equivalent) Yaquina Formation of Lincoln County, Oregon. The two new species are the most primitive known desmostylians and compare favorably with the primitive Eocene proboscideans Anthracobune and Moeritherium, and to the still more primitive tethythere Minchenella from the Paleocene of China. For many years the Desmostylia were widely regarded as members of the mammalian order Sirenia before being accepted as a taxon coordinate with the Sirenia and Proboscidea (Reinhart, 1953). On the basis of cladistic analysis we go a step further and regard the Desmostylia as more closely related to Proboscidea than to Sirenia because the Desmostylia and Proboscidea are interpreted herein to share a more recent common ancestor than either order does with the Sirenia.
    [Show full text]
  • New Sirenian Findings from Crete Island
    Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 NEW SIRENIAN FINDINGS FROM CRETE ISLAND Svana K., Iliopoulos G. and Fassoulas C. Natural History Museum of Crete, University of Crete, PO Box 2208, 71409, Irakleio Crete, [email protected], [email protected], [email protected] Abstract In the last five years, the discovery of several new localities of fossil Sirenians found in the Neogene sediments of Crete has increased drastically the number of sirenian localities on the island. Some of the most important findings consist of almost complete post cranial skeletons (localities of Stilos, Panassos near Zaros and Tripitos in Agia Fotia near Siteia). Furthermore, the locality Kotsiana near Chania, where in 1973 Symeonidis and Schultz reported the first sirenian findings from Crete, was re- visited and several new sites were recorded. The most recent findings not thoroughly studied yet, are situated in three new fossiliferous sites near Panassos village (Ampelouzos, Panasos 2 and Kefala), and in Afrata at Rodopou peninsula. The preliminary morphological and metrical study of the remains from Panassos and Tripitos, and their comparison with other findings from Crete, as well as with Siren- ian material from European localities, has shown that all studied individuals belong to the species Metaxytherium cf. medium (Desmarest 1822). The age of the studied Cretan Sirenian material has been determined as Late Miocene (Tortonian) and the presence of Sirenia in Crete indicates the preva- lence of shallow and warm marine environments in coastal areas, rich in sea weeds.
    [Show full text]
  • India's Geodynamic Evolution During the Eocene
    Article 489 Sunil Bajpai1 and Vivesh V. Kapur2 India’s geodynamic evolution during the Eocene: perspectives on the origin and early evolution of modern mammal orders 1*Department of Earth Sciences, Indian Institute of Technology, Roorkee 247667, India 2 Birbal Sahni Institute of Palaeosciences, Lucknow 226007, India *Corresponding author; Email: [email protected] (Received : 30/01/2019; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020031 In recent years, explosion of research in the early and the resulting biotic endemism as well as dispersal during this Tertiary mammals of India has attracted widespread interval. The fossil biota from this interval encompasses the interval from India’s last phase of northward drift until its suturing with Asia. interest because of the importance of this fauna in In recent years it has been shown to represent three distinct understanding biogeographic origins, early evolution, biogeographic domains: Gondwanan, Laurasian, and the endemic and dispersal patterns of several modern mammal component. These components present major biogeographic puzzles orders as well for its paleogeographic implications. and have led to hypotheses that emphasize the fact that the distribution Although Paleocene mammals are yet to be discovered of terrestrial fossil biota provides compelling evidence for the reconstruction of paleogeographic relationships between the in the Indian subcontinent, Indian Early Eocene mammal landmasses (e.g., Ali and Aitchison, 2008; Chatterjee et al., 2017; faunas are now becoming increasingly important in Kapur and Khosla, 2018). debates concerning the origins of several modern The northern (Laurasian) land masses (North America/Europe/ terrestrial orders. In many cases, Eocene mammals China) have been historically considered to be the centre of placental from India represent primitive and stratigraphically evolution because of their rich fossil records from the Paleocene and Eocene.
    [Show full text]