Feeding in Marine Mammals: an Integration of Evolution and Ecology Through Time
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6th European Workshop on Vertebrate Palaeontology - Florence and Montevarchi (Italy) - September 19-22, 2001 The organizing team welcomes the participants in the 6th European Workshop of Vertebrate Paleontology in Florence and expresses its deepest thanks to the many colleagues that enthusiastically answered to our call making this issue possible. The organizers hope the participants will find Florence not only that jewel-case of art celebrated all over the world, but also an appropriate place for discussing crumbled fossil bones. May the meeting come up to everybody’s best expectations! The 6th European Workshop on Vertebrate Paleontology has been made possible, thanks to the support and collaboration obtained from the Tethys Cultural Association, the Section of Geology and Paleontology of the Museum of Natural History of Florence, the Department of Earth Sciences of Florence and the Museum of Plaeontology of the Accademia Valdarnese del Poggio of Montevarchi. The organizers would like to thank the administration of the Section of Geology and Paleontology of the Museum of Natural History of Florence and the Accademia Valdarnese del Poggio for granting their facilities, and all the volunteers for their generous donation of time and talent. Without their dedication and tireless efforts, this issue would have been impossible. Special thanks are due to Maria Cristina Andreani, manager of the display department of the Section of Geology and Paleontology of the Museum of Natural History of Florence, for her assistance and for creating the logo and producing the panels of explanation of the evolution of the Upper Valdarno. The organizers are also grateful to the Comune of Montevarchi for offering the conference lunch and to Tiziana Vitali for arranging the tea party. -
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. -
1 Published in Journal of South American Earth Sciences, 31:414
Published in Journal of South American Earth Sciences, 31:414-425, 2011 (This is a prepublication version, with larger illustrations) A high resolution stratigraphic framework for the remarkable fossil cetacean assemblage of the Miocene/Pliocene Pisco Formation, Peru Leonard Brand a,*, Mario Urbina b, Arthur Chadwick c, Thomas J. DeVries d, Raul Esperante e, a Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, CA 92350 b Museo de Historia Natural, Lima 14, Peru c Southwestern Adventist University, Keene, TX 76059 d Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195 e Geoscience Research Institute, Loma Linda, CA 92350 Abstract The Miocene/Pliocene Pisco Formation of Peru contains a rich marine vertebrate fossil record, providing a unique opportunity for the study of paleoecology and evolution, along with the sedimentological context of the fossils. The lack of a high-resolution stratigraphic framework has hampered such study. In this paper we develop the needed stratigraphy for the areas in the Pisco Formation where most of the vertebrate paleontological research is occurring. In the Ica Valley and in the vicinity of Lomas, series of lithologically or paleontologically unique marker beds were identified. These were walked out and documented with GPS technology. Measured sections connecting these marker beds provide a stratigraphic framework for the areas studied. GPS locations, maps of the marker beds on aerial photographs, and outcrop photographs allow field determination of the stratigraphic positions of study areas. Keywords: Stratigraphy, Miocene, Pliocene, Pisco, Peru * Corresponding author. FAX 909-558-0259 E-mail address: [email protected] (Leonard Brand) 1. -
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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. -
A Monodontid Cetacean from the Early Pliocene of the North Sea
BULLETIN DE L’INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE, 77: 197-210,2007 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN, 77: 197-210,2007 A monodontid cetacean from the Early Pliocene of the North Sea by Olivier LAMBERT & Pierre GIGASE L a m b e r t O. & G ig a s e P., 2007 -A monodontid cetacean from fosse temporale est plus élevée que chez D. leucas et le rostre the Early Pliocene of the North Sea. Bulletin de I ’Institut royal des ne comporte pas la paire de dents maxillaires modifiées de M. Sciences naturelles de Belgique, Sciences de la Terre 77: 197-210, monoceros. Plusieurs sillons observés à la surface des os crâniens 9 figs, 2 tables, Brussels, October 15,2007 - ISSN 0374-6291. sont interprétés comme des marques de dents de requin, résultant soit d’un épisode de prédation, soit de l’action d’un charognard. Plusieurs os de l’oreille isolés du Néogène d’Anvers sont Abstract également attribués à un Monodontidae. Les nouveaux spécimens décrits ici indiquent que des membres de cette famille ont migré A partial skeleton from the Early Pliocene of Antwerp (north of vers des eaux plus froides avant ou durant le Pliocène précoce, Belgium), including a fragmentary skull, corresponds to the first bien avant les premières mentions pléistocènes de Delphinapterus record of a fossil member of the family Monodontidae in the North leucas dans la Mer du Nord. De plus, la paléobiogéographie des Sea. The vertex of the skull is lower than in the oldest known Delphinidae, Monodontidae et Phocoenidae fossiles suggère une Monodontidae, the latest Miocene Denebola brachycephala, and the origine pacifique pour les ‘crown-Delphinoidea’ de l’Atlantique orbit is more anteriorly shifted. -
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. -
I I 71-15,061 CAMERON, Christopher Paul, 1940- PALEOMAGNETISM of SHEMYA and ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA. University O
Paleomagnetism Of Shemya And Adak Islands, Aleutian Islands, Alaska Item Type Thesis Authors Cameron, Christopher Paul Download date 23/09/2021 14:56:00 Link to Item http://hdl.handle.net/11122/9194 I I 71-15,061 CAMERON, Christopher Paul, 1940- PALEOMAGNETISM OF SHEMYA AND ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA. University of Alaska, Ph.D., 1970 Geology University Microfilms, A XEROX Company, Ann Arbor, Michigan tutc nTCCTDTATTOM MAC HTTM MTPROFIT.MFD F.VAPTT.Y AS RF.OF.TVF.D Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PALE01IAGNETISM OF SHEMYA AMD ADAK ISLAUDS, ALEUTIAN ISLANDS, ALASKA A DISSERTATION Presented to the Faculty of the University of Alaska in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY by Christopher P/" Cameron B. S. College, Alaska May, 1970 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PALEOilAGNETISM OF SHEMYA AND ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA APPROVED: f t l ‘y l .V" ■i. n ■ ■< < ; N w 1 T *W -C ltc-JL It / _ _ ____ /vx... , ~ ~ 7 YdSV Chairman APPPvOVED: dai£ 3 / 3 0 / 7 0 Dean of the College of Earth Sciences and Mineral Industry Vice President for Research and Advanced Study Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT Paleomagnetic results are presented for Tertiary and Quaternary volcanic rocks from Shemya and Adak Islands, Aleutian Islands, Alaska. The specimens were collected and measured using standard paleomagnetic methods. Alternating field demagnetization techniques were applied to test the stability of the remanence and to remove unwanted secondary components of magnetization. -
Thomas Jefferson Meg Tooth
The ECPHORA The Newsletter of the Calvert Marine Museum Fossil Club Volume 30 Number 3 September 2015 Thomas Jefferson Meg Tooth Features Thomas Jefferson Meg The catalogue number Review; Walking is: ANSP 959 Whales Inside The tooth came from Ricehope Estate, Snaggletooth Shark Cooper River, Exhibit South Carolina. Tiktaalik Clavatulidae In 1806, it was Juvenile Bald Eagle originally collected or Sculpting Whale Shark owned by Dr. William Moroccan Fossils Reid. Prints in the Sahara Volunteer Outing to Miocene-Pliocene National Geographic coastal plain sediments. Dolphins in the Chesapeake Sloth Tooth Found SharkFest Shark Iconography in Pre-Columbian Panama Hippo Skulls CT- Scanned Squalus sp. Teeth Sperm Whale Teeth On a recent trip to the Academy of Natural Sciences of Drexel University (Philadelphia), Collections Manager Ned Gilmore gave John Nance and me a behind -the-scenes highlights tour. Among the fossils that belonged to Thomas☼ Jefferson (left; American Founding Father, principal author of the Declaration of Independence, and third President of the United States) was this Carcharocles megalodon tooth. Jefferson’s interests and knowledge were encyclopedic; a delight to know that they included paleontology. Hand by J. Nance. Photo by S. Godfrey. Jefferson portrait from: http://www.biography.com/people/thomas-jefferson-9353715 ☼ CALVERT MARINE MUSEUM www.calvertmarinemuseum.com 2 The Ecphora September 2015 Book Review: The Walking 41 million years ago and has worldwide distribution. It was fully aquatic, although it did have residual Whales hind limbs. In later chapters, Professor Thewissen George F. Klein discusses limb development and various genetic factors that make whales, whales. This is a The full title of this book is The Walking complicated topic, but I found these chapters very Whales — From Land to Water in Eight Million clear and readable. -
Letter to K. Baker, 1-29-07
Marine Mammal Commission 4340 East-West Highway, Room 905 Bethesda, MD 20814 29January 2007 Mr. Kyle Baker National Marine Fisheries Service 263 13th Avenue, South St. Petersburg, FL 33701 Dear Mr. Baker: The Marine Mammal Commission, in consultation with its Committee of Scientific Advisors on Marine Mammals, has reviewed the National Marine Fisheries Service’s 29 November 2006 Federal Register notice announcing its intent to conduct a review of the Caribbean monk seal, Monachus tropicalis, under the Endangered Species Act and requesting information on the species’ status. We have reviewed our files and, with great regret, we have concluded that the species is extinct and should be removed from the list of endangered and threatened species. Fossil and archeological evidence, along with sighting records, indicate that the species once occurred from the southeastern United States through the Bahamas and the Caribbean Sea. A review of those records by Rice (1973) concluded that the last authoritative sighting was of a small colony of animals at Seranilla Banks between Jamaica and the Yucatan Peninsula in 1952. A few other unconfirmed sightings were reported from the 1950s into the 1970s, but at least some of those were reported to involve escaped California sea lions (Gunter 1968 cited in Rice 1973). Although the species may have been extinct when the Endangered Species Act was passed in 1973, the Marine Mammal Commission wrote to the National Marine Fisheries Service on 26 January 1977 recommending that the Caribbean monk seal be listed as “endangered” under the Endangered Species Act and “depleted” under the Marine Mammal Protection Act. -
Pinniped Evolution and Puijila Darwini
A pP pP eE nN dD iI xX AE Pinniped Evolution and Puijila darwini Pinnipeds are carnivorous marine mammals that fossils, evolution scientists have not found any defini- have “finned back feet,” similar to the fins used by a tive fossils showing a land mammal evolving into a scuba diver. The Latin-derived word “pinniped” seal, sea lion or walrus. literally means “finned-foot.” Pinnipeds include three Canadian paleobiologist and professor, Dr. Natalia groups of mammals living today; namely, sea lions, Rybczynski of the Canadian Museum of Nature, wrote seals, and walruses. this candid assessment in 2009: The “fossil evidence of By 2007, when the first edition of this book was the morphological steps leading from a terrestrial published, scientists had discovered 20,000 fossil ancestor to the modern marine forms has been weak or pinnipeds. (See Appendix A.) Despite this plethora of contentious.” 1 All three types of pinnipeds Sea lion living today, sea lions (left), walruses (bottom left), and seals (below), have finned back feet, the telltale sign of a pinniped. Seal Walrus Appendix E: Puijila Adarwini p p e n d i x 239 A P P E N D I X EA Enaliarctos—The Oldest Pinniped Enaliarctos, the oldest fossil pinniped, looks like a between a terrestrial ancestor and the appearance of sea lion, and not a missing link. 2 (See photos below.) flippered pinnipeds. Indeed, most studies of pinniped Dr. Natalia Rybczynski highlights this missing link relationships and evolution do not consider the critical problem—the absence of fossils from a land mammal -
Biology; of the Seal
7 PREFACE The first International Symposium on the Biology papers were read by title and are included either in of the Seal was held at the University of Guelph, On full or abstract form in this volume. The 139 particip tario, Canada from 13 to 17 August 1972. The sym ants represented 16 countries, permitting scientific posium developed from discussions originating in Dub interchange of a truly international nature. lin in 1969 at the meeting of the Marine Mammals In his opening address, V. B. Scheffer suggested that Committee of the International Council for the Ex a dream was becoming a reality with a meeting of ploration of the Sea (ICES). The culmination of such a large group of pinniped biologists. This he felt three years’ organization resulted in the first interna was very relevant at a time when the relationship of tional meeting, and this volume. The president of ICES marine mammals and man was being closely examined Professor W. Cieglewicz, offered admirable support as on biological, political and ethical grounds. well as honouring the participants by attending the The scientific session commenced with a seven paper symposium. section on evolution chaired by E. D. Mitchell which The programme committee was composed of experts showed the origins and subsequent development of representing the major international sponsors. W. N. this amphibious group of higher vertebrates. Many of Bonner, Head, Seals Research Division, Institute for the arguments for particular evolutionary trends are Marine Environmental Research (IMER), represented speculative in nature and different interpretations can ICES; A. W. Mansfield, Director, Arctic Biological be attached to the same fossil material. -
A NEW DWARF SEAL from the LATE NEOGENE of SOUTH AMERICA and the EVOLUTION of PINNIPEDS in the SOUTHERN HEMISPHERE by ANA M
[Papers in Palaeontology, Vol. 2, Part 1, 2016, pp. 101–115] A NEW DWARF SEAL FROM THE LATE NEOGENE OF SOUTH AMERICA AND THE EVOLUTION OF PINNIPEDS IN THE SOUTHERN HEMISPHERE by ANA M. VALENZUELA-TORO1,2,NICHOLASD.PYENSON2,3,CAROLINAS. GUTSTEIN1,2,4 and MARIO E. SUAREZ 1 1Red Paleontologica U.Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biologıa, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Nu~ noa,~ Santiago, Chile; e-mails: [email protected], [email protected], [email protected] 2Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, PO Box 37012, Washington, DC 20013-7012, USA; e-mail: [email protected] 3Departments of Mammalogy and Paleontology, Burke Museum of Natural History and Culture, Seattle, WA 98195, USA 4Current address: Area de Patrimonio Natural, Consejo de Monumentos Nacionales, Vicuna~ Mackenna, 84, Providencia, Santiago, Chile Typescript received 25 May 2015; accepted in revised form 15 September 2015 Abstract: Along the south-western coast of South America, foramen; a femur with a subtrochanteric fossa, among other three genera of fossil phocids (true seals) have been formally characters; in combination with a relatively small body size. described from the late Neogene: Acrophoca and Piscophoca All these features together distinguish A. changorum from all from Chile and Peru, and, more recently, Hadrokirus from other reported pinnipeds. This new taxon not only increases Peru, which all represent medium- to large-sized phocids. the taxonomic and morphological diversity of phocids of the Here, we report the discovery of Australophoca changorum late Neogene of the eastern South Pacific Ocean, but it also gen.