Stanford Paleoparadoxia Fossil Skeleton Mounting
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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. -
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 Paleontology Synthesis Project and Establishing a Framework for Managing National Park Service Paleontological Resource Archives and Data
Lucas, S.G. and Sullivan, R.M., eds., 2018, Fossil Record 6. New Mexico Museum of Natural History and Science Bulletin 79. 589 THE PALEONTOLOGY SYNTHESIS PROJECT AND ESTABLISHING A FRAMEWORK FOR MANAGING NATIONAL PARK SERVICE PALEONTOLOGICAL RESOURCE ARCHIVES AND DATA VINCENT L. SANTUCCI1, JUSTIN S. TWEET2 and TIMOTHY B. CONNORS3 1National Park Service, Geologic Resources Division, 1849 “C” Street, NW, Washington, D.C. 20240, [email protected]; 2National Park Service, 9149 79th Street S., Cottage Grove, MN 55016, [email protected]; 3National Park Service, Geologic Resources Division, 12795 W. Alameda Parkway, Lakewood, CO 80225, [email protected] Abstract—The National Park Service Paleontology Program maintains an extensive collection of digital and hard copy documents, publications, photographs and other archives associated with the paleontological resources documented in 268 parks. The organization and preservation of the NPS paleontology archives has been the focus of intensive data management activities by a small and dedicated team of NPS staff. The data preservation strategy complemented the NPS servicewide inventories for paleontological resources. The first phase of the data management, referred to as the NPS Paleontology Synthesis Project, compiled servicewide paleontological resource data pertaining to geologic time, taxonomy, museum repositories, holotype fossil specimens, and numerous other topics. In 2015, the second phase of data management was implemented with the creation and organization of a multi-faceted digital data system known as the NPS Paleontology Archives and NPS Paleontology Library. Two components of the NPS Paleontology Archives were designed for the preservation of both park specific and servicewide paleontological resource archives and data. A third component, the NPS Paleontology Library, is a repository for electronic copies of geology and paleontology publications, reports, and other media. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Pliocene and Early Pleistocene) Faunas from New Mexico
Chapter 12 Mammalian Biochronology of Blancan and Irvingtonian (Pliocene and Early Pleistocene) Faunas from New Mexico GARY S. MORGAN1 AND SPENCER G. LUCAS2 ABSTRACT Signi®cant mammalian faunas of Pliocene (Blancan) and early Pleistocene (early and medial Irvingtonian) age are known from the Rio Grande and Gila River valleys of New Mexico. Fossiliferous exposures of the Santa Fe Group in the Rio Grande Valley, extending from the EspanÄola basin in northern New Mexico to the Mesilla basin in southernmost New Mexico, have produced 21 Blancan and 6 Irvingtonian vertebrate assemblages; three Blancan faunas occur in the Gila River Valley in the Mangas and Duncan basins in southwestern New Mexico. More than half of these faunas contain ®ve or more species of mammals, and many have associated radioisotopic dates and/or magnetostratigraphy, allowing for correlation with the North American land-mammal biochronology. Two diverse early Blancan (4.5±3.6 Ma) faunas are known from New Mexico, the Truth or Consequences Local Fauna (LF) from the Palomas basin and the Buckhorn LF from the Mangas basin. The former contains ®ve species of mammals indicative of the early Blancan: Borophagus cf. B. hilli, Notolagus lepusculus, Neo- toma quadriplicata, Jacobsomys sp., and Odocoileus brachyodontus. Associated magnetostra- tigraphic data suggest correlation with either the Nunivak or Cochiti Subchrons of the Gilbert Chron (4.6±4.2 Ma), which is in accord with the early Blancan age indicated by the mam- malian biochronology. The Truth or Consequences LF is similar in age to the Verde LF from Arizona, and slightly older than the Rexroad 3 and Fox Canyon faunas from Kansas. -
Ore Bin / Oregon Geology Magazine / Journal
THE ORE.-BIN Volume XVI Vol. 16, No.1 THE ORE.-BIN 1 January 1954 Portland, Oregon STATE DEPARTKENT OF GEOLOGY AND KINERAL INDUSTRIES Head Ottice: 1069 State Ottioe Bldg., Portland 1, Oregon Telephone: Columbia 2161, Ext. 488 State Governing Board ~ Kason L. Bingham, Chairman, Portland R. E. Corooran Geologist Niel R. Allen Grants Pass Hollis K. Dole Geologist Austin Dunn Baker L. L. Hoagland Assayer & Chemist Ralph S. Kason Kining Engineer F. W. Libbey, Direotor T. C. Katthews Speotrosoopist Lenin Ramp Geologist K. L. Steere Geologist R. E. stewart Geologist F18ld Ottices 20" First Street, Baker 2'9 S.E. "H" street, Grants Pass N. S. Wagper, Field Geologist David J. White, Field Geologist ****************************** THE ASTORIA LANDSLIDES Erosion to most ot us means the slow, almost imperoeptible, wearing down ot the higher parts ot the earth's crust by running water, wind, or ice. Seemingly mountains remain the same height and stream valleys the same depth throughout the years. The only rapid changes in the landscape which are accepted as normal are the neat exoavations made when new roads, dams, or other man-made structures are constructed. It 1s not sur prising that special attention to the ohoioe of a toundation for an ordinary building is seldom given, tor our experience tells us that the durability ot the structure is infinitely less than that of the ground on whioh it is bull t. It oomes as a shock to us when exceptions to our everyday observations ocour. Suoh is the oase in the land sliding at Astoria, Oregon,at the mouth of the Columbia River. -
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. -
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. -
Pliocene Climates: Scenario for Global Warming
Department of the Interior U.S. Geological Survey Pliocene Climates: Scenario for Global Warming Abstracts from USGS Workshop, Denver, Colorado, October 23 - 25,1989 Edited by Linda B. Gosnell and Richard Z. Poore U.S. Geological Survey, Reston, VA 22092 Open-File Report 90-64 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Introduction: USGS Workshop on Pliocene Climates The US. Geological Survey (USGS) held a work tate quantitative estimates of environmental informa shop on Pliocene climates in Denver, Colorado on tion and the development of regional and global pat October 23-25,1989. The workshop brought together terns of climate data. members of the USGS who are working on a long- Better understanding of Pliocene climates, their ev term project to understand and map Pliocene cli olution, and rates and causes of change will provide mates and environments of the Northern Hemi important dues to future earth systems changes and sphere with interested collaborators from the USSR, impacts that will occur as a result of a greenhouse- The Geological Survey of Canada, the National Cen effect global warming. A major goal of the USGS Pli ter for Atmospheric Research, and the Institute for ocene Project is to produce a synoptic map or "snap Arctic and Alpine Research, University of Colorado. shot" of climate parameters during a time in the Plio Paleoclimate researchers from the USSR attended the cene representing conditions that are significantly workshop as part of an exchange and cooperative warmer than modern climates. The Pliocene "Scenar study of Pliocene climates that is organized under the io for Global Warming" will provide a means for test auspices of Working Group VIII of the US-USSR Bi ing and validating results of general circulation mod lateral Agreement on Protection of the Environment els (GCMs) which attempt to model global warming. -
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. -
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. -
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.