Manatee Brochure
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Contributions from the Museum of Paleontology the University of Michigan
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 29.. No. 3. PP. 69-87 November 30. 1994 PROTOSIREN SMITHAE, NEW SPECIES (MAMMALIA, SIRENIA), FROM THE LATE MIDDLE EOCENE OF WADI HITAN, EGYPT BY DARYL P. DOMNING AND PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals on request. A list of the separate issues may also be obtained by request. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48 109-1079. VOLS. 2-29. Parts of volumes may be obtained if available. Price lists are available upon inquiry. PROTOSIREN SMITHAE, NEW SPECIES (MAMMALIA, SIRENIA), FROM THE LATE MIDDLE EOCENE OF WADI KITAN, EGYPT Abstract-Protosiren smithae is a new protosirenid sirenian described on the basis of associated cranial and postcranial material from the late middle Eocene (latest Bartonian) Gehannam Formation of Wadi Hitan (Zeuglodon Valley), Fayum Province, Egypt. The new species is similar to Protosiren fraasi Abel, 1907, from the earlier middle Eocene (Lutetian) of Egypt, but it is younger geologically and more derived morphologically. P. smithae is probably a direct descendant of P. fraasi. The postcranial skeleton of P. imithae- includes well-developed hindlimbs, which suggest some lingering amphibious tendencies in this otherwise aquatically-adapted primitive sea cow. -
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A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases. -
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. -
The Giant Sea Mammal That Went Extinct in Less Than Three Decades
The Giant Sea Mammal That Went Extinct in Less Than Three Decades The quick disappearance of the 30-foot animal helped to usher in the modern science of human-caused extinctions. JACOB MIKANOWSKI, THE ATLANTIC 4/19/17 HTTPS://WWW.THEATLANTIC.COM/SCIENCE/ARCHIVE/2017/04/PLEIST OSEACOW/522831/ The Pleistocene, the geologic era immediately preceding our own, was an age of giants. North America was home to mastodons and saber-tooth cats; mammoths and wooly rhinos roamed Eurasia; giant lizards and bear-sized wombats strode across the Australian outback. Most of these giants died at the by the end of the last Ice Age, some 14,000 years ago. Whether this wave of extinctions was caused by climate change, overhunting by humans, or some combination of both remains a subject of intense debate among scientists. Complicating the picture, though, is the fact that a few Pleistocene giants survived the Quaternary extinction event and nearly made it intact to the present. Most of these survivor species found refuge on islands. Giant sloths were still living on Cuba 6,000 years ago, long after their relatives on the mainland had died out. The last wooly mammoths died out just 4,000 years ago. They lived in a small herd on Wrangel Island north of the Bering Strait between the Chukchi and East Siberian Seas. Two-thousand years ago, gorilla-sized lemurs were still living on Madagascar. A thousand years ago, 12-foot-tall moa birds were still foraging in the forests of New Zealand. Unlike the other long-lived megafauna, Steller’s sea cows, one of the last of the Pleistocene survivors to die out, found their refuge in a remote scrape of the ocean instead of on land. -
Zeezoogdieren
CRANIUM, nr. 2 -1998 De Nederlandse fossiele zeezoogdieren. Een overzicht Klaas Post Samenvatting Onder de worden in dit Cetacea de noemer zeezoogdieren artikel de (walvissen en dolfijnen), Pinnipedia de Sirenia Fossielen worden (zeehonden, zeeleeuwen en walrussen) en (zeekoeien) samengevat. van zeezoogdieren dan Naast het feit dat zeldzaam is hun veel minder aangetroffen fossielen van landzoogdieren. ze gewoon zijn voorkomen ook recente of fossiele zeebodems en stranden. nog beperkt tot specifieke gebieden: namelijk en is de evolutie bekend dus is de of Dientengevolge er nogweinig over van zeezoogdieren en genus- soortbepaling of Verder vooral oudere literatuur foutieve informatiete bevatten en vaak nog moeilijk geheel nietmogelijk. blijkt bovendien aantal verschillende dezelfde vermelden.Het is danook niet een enorm namen voor genera en soorten te verwonderlijk dat fossiele zeezoogdieren wetenschappelijk noch populair in de belangstelling staan. De de Noordzee behoren de wereld van fossielen van Nederlanden en aangrenzende tot rijkste vindplaatsen ter zeezoogdieren. Hoe kan het ook eigenlijk anders met zo’n waterrijke geologische geschiedenis. De voortdurend Pleistoceen het Holoceenincombinatie met wisselendeNoordzeekustlijnen gedurende Mioceen,Plioceen, en vroege de vele rivieren hebben Zo worden de mondingen van grote zeer gevarieerde zeezoogdierfauna’s nagelaten. de Pleistocene walrus wereld zoveel fossielen als in Nederland! Ondanks de bijvoorbeeld van nergens ter gevonden kwaliteit deze heeft de eind links laten De kwantiteit en van fossielen wetenschap ze sinds vorige eeuw liggen. helaas vaak verloren collecties verkeren veelal in slechte staat en de bijbehorende gegevens zijn gegaan. Summary lions and and the Sirenia In this article the Cetacea (wales and delphins), the Pinnipedia (seals, sea walrusses) (sea unitedunder the mammals.Fossils of mammals found lesser thanthose of land cows) are term sea sea are to a extent also: and fossil mammals. -
APPENDIX 4. Classification and Synonymy of the Sirenia and Desmostylia
revised 3/29/2010 APPENDIX 4. Classification and Synonymy of the Sirenia and Desmostylia The following compilation encapsulates the nomenclatural history of the Sirenia and Desmostylia as comprehensively as I have been able to trace it. Included are all known formal names of taxa and their synonyms and variant combinations, with abbreviated citations of the references where these first appeared and their dates of publication; statements of the designated or inferred types of these taxa and their provenances; and comments on the nomenclatural status of these names. Instances of the use of names or combinations subsequent to their original publication are, however, not listed. Of course, the choices of which taxa to recognize as valid and their proper arrangement reflect my own current views. This arrangement is outlined immediately hereafter to aid in finding taxa in this section. (Note that not all taxa in this summary list are necessarily valid; several are probable synonyms but have not been formally synonymized.) For a quick-reference summary of the names now in use for the Recent species of sirenians, see Appendix 5. – DPD Summary Classification and List of Taxa Recognized ORDER SIRENIA Illiger, 1811 Family Prorastomidae Cope, 1889 Pezosiren Domning, 2001 P. portelli Domning, 2001 Prorastomus Owen, 1855 P. sirenoides Owen, 1855 Family Protosirenidae Sickenberg, 1934 Ashokia Bajpai, Domning, Das, and Mishra, 2009 A. antiqua Bajpai, Domning, Das, and Mishra, 2009 Protosiren Abel, 1907 P. eothene Zalmout, Haq, and Gingerich, 2003 P. fraasi Abel, 1907 P. sattaensis Gingerich, Arif, Bhatti, Raza, and Raza, 1995 P. smithae Domning and Gingerich, 1994 ?P. minima (Desmarest, 1822) Hooijer, 1952 Family Trichechidae Gill, 1872 (1821) Subfamily Miosireninae Abel, 1919 Anomotherium Siegfried, 1965 1 Daryl P. -
Atypicat Molecular Evolution of Afrotherian and Xenarthran B-Globin
Atypicat molecular evolution of afrotherian and xenarthran B-globin cluster genes with insights into the B-globin cluster gene organization of stem eutherians. By ANGELA M. SLOAN A thesis submitted to the Faculty of Graduate Studies in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Department of Zoology University of Manitoba Winnipeg, Manitoba, Canada @ Angela M. Sloan, July 2005 TIIE I]MVERSITY OF' MANITOBA FACULTY OF GRADUATE STT]DIES ***** - COPYRIGHTPERMISSION ] . Atypical molecular evolution of afrotherian and xenarthran fslobin cluster genes with insights into thefglobin cluster gene organization òf stem eutherians. BY Angela M. Sloan A ThesislPracticum submitted to the Faculty of Graduate Studies of The University of Manitoba in partial fulfill¡nent of the requirement of the degree of Master of Science Angela M. Sloan @ 2005 Permission has been granted to the Library of the University of Manitoba to lend or sell copies of this thesis/practicum, to the National Library of Canada to microfilm this thesis and to lend or sell copies of the fiIm, and to University Microfïlms Inc. to publish an abstract of this thesis/practicum. This reproduction or copy of this thesis has been made available by authority of the copyright owner solely for the purpose of private study and research, and may only be reproduced and copied as permitted by copyright laws or with express written authorization from the copyright ownér. ABSTRACT Our understanding of p-globin gene cluster evolutionlwithin eutherian mammals .is based solely upon data collected from species in the two most derived eutherian superorders, Laurasiatheria and Euarchontoglires. Ifence, nothing is known regarding_the gene composition and evolution of this cluster within afrotherian (elephants, sea cows, hyraxes, aardvarks, elephant shrews, tenrecs and golden moles) and xenarthran (sloths, anteaters and armadillos) mammals. -
Marine Mammals from the Miocene of Panama
Journal of South American Earth Sciences 30 (2010) 167e175 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Marine mammals from the Miocene of Panama Mark D. Uhen a,*, Anthony G. Coates b, Carlos A. Jaramillo b, Camilo Montes b, Catalina Pimiento b,c, Aldo Rincon b, Nikki Strong b, Jorge Velez-Juarbe d a George Mason University, Fairfax, VA 22030, USA b Smithsonian Tropical Research Institute, Box 0843-03092, Balboa, Ancon, Panama c Department of Biology, University of Florida, Gainesville, FL, USA d Laboratory of Evolutionary Biology, Department of Anatomy, Howard University, WA 20059, USA article info abstract Article history: Panama has produced an abundance of Neogene marine fossils both invertebrate (mollusks, corals, Received 1 May 2009 microfossils etc.) and vertebrate (fish, land mammals etc.), but marine mammals have not been previ- Accepted 21 August 2010 ously reported. Here we describe a cetacean thoracic vertebra from the late Miocene Tobabe Formation, a partial cetacean rib from the late Miocene Gatun Formation, and a sirenian caudal vertebra and rib Keywords: fragments from the early Miocene Culebra Formation. These finds suggest that Central America may yet Panama provide additional fossil marine mammal specimens that will help us to understand the evolution, and Neogene particularly the biogeography of these groups. Miocene Ó Pliocene 2010 Elsevier Ltd. All rights reserved. Cetacea Sirenia 1. Introduction archipelago, Panama (Fig. 1A). The Tobabe Formation is the basal unit of the Late Miocene-Early Pliocene (w7.2ew3.5 Ma) Bocas del Central America includes an abundance of marine sedimentary Toro Group, an approximately 600 m thick succession of volcani- rock units that have produced many fossil marine invertebrates clastic marine sediments (Fig. -
Manatee-Math.Pdf
Name: _________________________ 890 NE Ocean Boulevard Stuart, Florida 34996 Manatee Facts (772) 225-0505 www.fosusa.org ¨ Manatees only have molars to grind their West Indian Manatee Trichechus manatus food. ¨ Manatees chew two times per second. Length: 12 plus feet ¨ Manatee teeth are constantly being replaced as Weight: over 3,500 pounds they wear down and fall out. Color: gray to gray-brown ¨ The intestine of an adult manatee can measure Food: 100 pounds of aquatic plants a day 130 feet long. Reproduction: One calf every ¨ Manatees only breath through their nostrils. 2 to 5 years ¨ Manatee can hold their breath for up to 24 Range in US: North Carolina minutes. to Texas, mainly ¨ Manatee lungs are 2/3 the length of its body. Florida ¨ A manatee cannot turn its head sideways, it Location: Rivers, canals, estuaries, saltwater must turn its whole body. bays, & occasionally ¨ It takes 13 months for a manatee to be born. the open ocean ¨ Calves spend two years with their mothers learning the migration routes. Gray to Small Wrinkled Thick Wrinkled Skin Gray-Brown Color Head & Face Manatees are Mammals Manatees breath air and have hair like all other mammals. They look like a relative of dolphins and whales but manatees are closer related to elephants. Little Mermaid? Whiskers on the Snout When the Spanish Explorers reached Florida they thought the Manatees were mermaids. Toenails Paddle Shaped Tail Two Front Flippers Name: _________________________ 890 NE Ocean Boulevard Stuart, Florida 34996 (772) 225-0505 www.fosusa.org 1) Manatees eat for up to 8 hours a day. -
Chapter 15 the Mammals of Angola
Chapter 15 The Mammals of Angola Pedro Beja, Pedro Vaz Pinto, Luís Veríssimo, Elena Bersacola, Ezequiel Fabiano, Jorge M. Palmeirim, Ara Monadjem, Pedro Monterroso, Magdalena S. Svensson, and Peter John Taylor Abstract Scientific investigations on the mammals of Angola started over 150 years ago, but information remains scarce and scattered, with only one recent published account. Here we provide a synthesis of the mammals of Angola based on a thorough survey of primary and grey literature, as well as recent unpublished records. We present a short history of mammal research, and provide brief information on each species known to occur in the country. Particular attention is given to endemic and near endemic species. We also provide a zoogeographic outline and information on the conservation of Angolan mammals. We found confirmed records for 291 native species, most of which from the orders Rodentia (85), Chiroptera (73), Carnivora (39), and Cetartiodactyla (33). There is a large number of endemic and near endemic species, most of which are rodents or bats. The large diversity of species is favoured by the wide P. Beja (*) CIBIO-InBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, Universidade do Porto, Vairão, Portugal CEABN-InBio, Centro de Ecologia Aplicada “Professor Baeta Neves”, Instituto Superior de Agronomia, Universidade de Lisboa, Lisboa, Portugal e-mail: [email protected] P. Vaz Pinto Fundação Kissama, Luanda, Angola CIBIO-InBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, Universidade do Porto, Campus de Vairão, Vairão, Portugal e-mail: [email protected] L. Veríssimo Fundação Kissama, Luanda, Angola e-mail: [email protected] E. -
Miocene Paleontology and Stratigraphy of the Suwannee River Basin of North Florida and South Georgia
MIOCENE PALEONTOLOGY AND STRATIGRAPHY OF THE SUWANNEE RIVER BASIN OF NORTH FLORIDA AND SOUTH GEORGIA SOUTHEASTERN GEOLOGICAL SOCIETY Guidebook Number 30 October 7, 1989 MIOCENE PALEONTOLOGY AND STRATIGRAPHY OF THE SUWANNEE RIVER BASIN OF NORTH FLORIDA AND SOUTH GEORGIA Compiled and edit e d by GARY S . MORGAN GUIDEBOOK NUMBER 30 A Guidebook for the Annual Field Trip of the Southeastern Geological Society October 7, 1989 Published by the Southeastern Geological Society P. 0 . Box 1634 Tallahassee, Florida 32303 TABLE OF CONTENTS Map of field trip area ...... ... ................................... 1 Road log . ....................................... ..... ..... ... .... 2 Preface . .................. ....................................... 4 The lithostratigraphy of the sediments exposed along the Suwannee River in the vicinity of White Springs by Thomas M. scott ........................................... 6 Fossil invertebrates from the banks of the Suwannee River at White Springs, Florida by Roger W. Portell ...... ......................... ......... 14 Miocene vertebrate faunas from the Suwannee River Basin of North Florida and South Georgia by Gary s. Morgan .................................. ........ 2 6 Fossil sirenians from the Suwannee River, Florida and Georgia by Daryl P. Damning . .................................... .... 54 1 HAMIL TON CO. MAP OF FIELD TRIP AREA 2 ROAD LOG Total Mileage from Reference Points Mileage Last Point 0.0 0.0 Begin at Holiday Inn, Lake City, intersection of I-75 and US 90. 7.3 7.3 Pass under I-10. 12 . 6 5.3 Turn right (east) on SR 136. 15.8 3 . 2 SR 136 Bridge over Suwannee River. 16.0 0.2 Turn left (west) on us 41. 19 . 5 3 . 5 Turn right (northeast) on CR 137. 23.1 3.6 On right-main office of Occidental Chemical Corporation. -
117 October 2013—PROGRAM and ABSTRACTS
Technical Session XV (Saturday, November 2, 2013, 9:45 AM) which is situated on the eastern Bolivian Altiplano (21° 52’ S, 66° 19’ W), several THE SIRENIAN GENUS METAXYTHERIUM: WHAT'S UP WITH THOSE kilometers southeast of the village of Cerdas (approx. 60 km southeast of Uyuni). Eight ANIMALS?? specimens were studied including several partial mandibles preserving posterior premolars and molars, a partial maxilla with P3-P4, two fragmentary dentaries preserving DOMNING, Daryl, Howard Univ., Washington, DC, United States, 20059; VELEZ- alveoli of the anterior dentition, several isolated cheek teeth, an upper incisor, and two JUARBE, Jorge, Florida Museum of Natural History, Gainesville, FL, United States calcanei. The specimens are referred to the Hegetotheriinae based on the absence of a Metaxytherium (Mammalia, Dugongidae) is one of the most widespread, long-lived, strongly trilobed m3 talonid, lack of conspicuous diastemata among i2-p2 alveoli, and a species-rich, commonly fossilized – and taxonomically troublesome – genera of Sirenia. relatively small I1. A Hegetotheriine affinity is supported by the two Cerdas calcanei, Its morphologically conservative nature had, until recently, made it difficult to properly which are more similar to Hegetotherium than Pachyrukhos in having a circular define this genus. In recent years, however, much has been done to clarify its contents, sustentacular facet, a large navicular facet, and an only moderately rugose tuber. The relationships, and eventful evolutionary history. Originally known only from the Miocene Cerdas species differs from Prohegetotherium in lacking a labial groove near the anterior and Pliocene, its presence in the New World late Oligocene is now established, along margin of the upper cheek teeth.