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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Stratigraphic Paleobiology of an Evolutionary Radiation: Taphonomy and Facies Distribution of Cetaceans in the Last 23 Million Years
Fossilia, Volume 2018: 15-17 Stratigraphic paleobiology of an evolutionary radiation: taphonomy and facies distribution of cetaceans in the last 23 million years Stefano Dominici1, Simone Cau2 & Alessandro Freschi2 1 Museo di Storia Naturale, Università degli Studi di Firenze, Firenze, Italy; [email protected] 2 Dipartimento di Scienze Chimiche, della Vita e della Sostenibilità Ambientale, Università degli Studi di Parma, Parma, Italy; cau.simo- [email protected], [email protected] BULLET-POINTS ABSTRACT KEYWORDS: • The majority of cetacean fossils are in Zanclean and Piacenzian deposits. Neogene; • Cetacean fossils are preferentially found in offshore paleosettings. Pliocene; • Pleistocene findings drop to a minimum, notwithstanding offshore strata are Cetaceans; well represented in the record. Taphonomy. • A taphonomic imprinting on the cetacean fossil record is hypothesised, con- nected with a radiation of whale-bone consumers of modern type. offer a particularly rich cetacean fossil record and an INTRODUCTION area where available studies allow to explore this key The study of the stratigraphy and taphonomy of Neo- time of cetacean evolution at a stratigraphic resolution gene cetaceans is a fundamental step to properly frame finer than the stage. An increase in cetaceans diversity the evolutionary radiation of this megafauna, at the is recorded around 3.2 – 3.0 Ma, in coincidence of top of the pelagic marine ecosystem. Major evolutio- the mid-Piacenzian climatic optimum, and a drastic nary steps have been summarised in recent -
Diversity Partitioning During the Cambrian Radiation
Diversity partitioning during the Cambrian radiation Lin Naa,1 and Wolfgang Kiesslinga,b aGeoZentrum Nordbayern, Paleobiology and Paleoenvironments, Friedrich-Alexander-Universität Erlangen-Nürnberg, 91054 Erlangen, Germany; and bMuseum für Naturkunde, Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, 10115 Berlin, Germany Edited by Douglas H. Erwin, Smithsonian National Museum of Natural History, Washington, DC, and accepted by the Editorial Board March 10, 2015 (received for review January 2, 2015) The fossil record offers unique insights into the environmental and Results geographic partitioning of biodiversity during global diversifica- Raw gamma diversity exhibits a strong increase in the first three tions. We explored biodiversity patterns during the Cambrian Cambrian stages (informally referred to as early Cambrian in this radiation, the most dramatic radiation in Earth history. We as- work) (Fig. 1A). Gamma diversity dropped in Stage 4 and de- sessed how the overall increase in global diversity was partitioned clined further through the rest of the Cambrian. The pattern is between within-community (alpha) and between-community (beta) robust to sampling standardization (Fig. 1B) and insensitive to components and how beta diversity was partitioned among environ- including or excluding the archaeocyath sponges, which are po- ments and geographic regions. Changes in gamma diversity in the tentially oversplit (16). Alpha and beta diversity increased from Cambrian were chiefly driven by changes in beta diversity. The the Fortunian to Stage 3, and fluctuated erratically through the combined trajectories of alpha and beta diversity during the initial following stages (Fig. 2). Our estimate of alpha (and indirectly diversification suggest low competition and high predation within beta) diversity is based on the number of genera in published communities. -
Arktocara Yakataga, a New Fossil Odontocete (Mammalia, Cetacea) from the Oligocene of Alaska and the Antiquity of Platanistoidea
Arktocara yakataga, a new fossil odontocete (Mammalia, Cetacea) from the Oligocene of Alaska and the antiquity of Platanistoidea Alexandra T. Boersma1,2 and Nicholas D. Pyenson1,3 1 Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, D.C., United States of America 2 College of Extended Education, California State University, Monterey Bay, Seaside, CA, United States of America 3 Departments of Mammology and Paleontology, Burke Museum of Natural History and Culture, Seattle, WA, United States of America ABSTRACT The diversification of crown cetacean lineages (i.e., crown Odontoceti and crown Mysticeti) occurred throughout the Oligocene, but it remains an ongoing challenge to resolve the phylogenetic pattern of their origins, especially with respect to stem lineages. One extant monotypic lineage, Platanista gangetica (the Ganges and Indus river dolphin), is the sole surviving member of the broader group Platanistoidea, with many fossil relatives that range from Oligocene to Miocene in age. Curiously, the highly threatened Platanista is restricted today to freshwater river systems of South Asia, yet nearly all fossil platanistoids are known globally from marine rocks, suggesting a marine ancestry for this group. In recent years, studies on the phylogenetic relationships in Platanistoidea have reached a general consensus about the membership of different sub-clades and putative extinct groups, although the position of some platanistoid groups (e.g., Waipatiidae) has been contested. Here we describe a new genus and species of fossil platanistoid, Arktocara yakataga, gen. et sp. nov. from the Oligocene of Alaska, USA. The type and only known specimen was collected from the marine Poul Submitted 16 May 2016 Creek Formation, a unit known to include Oligocene strata, exposed in the Yakutat Accepted 13 July 2016 City and Borough of Southeast Alaska. -
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. -
A New Middle Eocene Protocetid Whale (Mammalia: Cetacea: Archaeoceti) and Associated Biota from Georgia Author(S): Richard C
A New Middle Eocene Protocetid Whale (Mammalia: Cetacea: Archaeoceti) and Associated Biota from Georgia Author(s): Richard C. Hulbert, Jr., Richard M. Petkewich, Gale A. Bishop, David Bukry and David P. Aleshire Source: Journal of Paleontology , Sep., 1998, Vol. 72, No. 5 (Sep., 1998), pp. 907-927 Published by: Paleontological Society Stable URL: https://www.jstor.org/stable/1306667 REFERENCES Linked references are available on JSTOR for this article: https://www.jstor.org/stable/1306667?seq=1&cid=pdf- reference#references_tab_contents You may need to log in to JSTOR to access the linked references. JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms SEPM Society for Sedimentary Geology and are collaborating with JSTOR to digitize, preserve and extend access to Journal of Paleontology This content downloaded from 131.204.154.192 on Thu, 08 Apr 2021 18:43:05 UTC All use subject to https://about.jstor.org/terms J. Paleont., 72(5), 1998, pp. 907-927 Copyright ? 1998, The Paleontological Society 0022-3360/98/0072-0907$03.00 A NEW MIDDLE EOCENE PROTOCETID WHALE (MAMMALIA: CETACEA: ARCHAEOCETI) AND ASSOCIATED BIOTA FROM GEORGIA RICHARD C. HULBERT, JR.,1 RICHARD M. PETKEWICH,"4 GALE A. -
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. -
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. -
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes by Ryan Matthew Bebej A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ecology and Evolutionary Biology) in The University of Michigan 2011 Doctoral Committee: Professor Philip D. Gingerich, Co-Chair Professor Philip Myers, Co-Chair Professor Daniel C. Fisher Professor Paul W. Webb © Ryan Matthew Bebej 2011 To my wonderful wife Melissa, for her infinite love and support ii Acknowledgments First, I would like to thank each of my committee members. I will be forever grateful to my primary mentor, Philip D. Gingerich, for providing me the opportunity of a lifetime, studying the very organisms that sparked my interest in evolution and paleontology in the first place. His encouragement, patience, instruction, and advice have been instrumental in my development as a scholar, and his dedication to his craft has instilled in me the importance of doing careful and solid research. I am extremely grateful to Philip Myers, who graciously consented to be my co-advisor and co-chair early in my career and guided me through some of the most stressful aspects of life as a Ph.D. student (e.g., preliminary examinations). I also thank Paul W. Webb, for his novel thoughts about living in and moving through water, and Daniel C. Fisher, for his insights into functional morphology, 3D modeling, and mammalian paleobiology. My research was almost entirely predicated on cetacean fossils collected through a collaboration of the University of Michigan and the Geological Survey of Pakistan before my arrival in Ann Arbor. -
Thewissen Et Al. Reply Replying To: J
NATURE | Vol 458 | 19 March 2009 BRIEF COMMUNICATIONS ARISING Hippopotamus and whale phylogeny Arising from: J. G. M. Thewissen, L. N. Cooper, M. T. Clementz, S. Bajpai & B. N. Tiwari Nature 450, 1190–1194 (2007) Thewissen etal.1 describe new fossils from India that apparentlysupport fossils, Raoellidae or the raoellid Indohyus is more closely related to a phylogeny that places Cetacea (that is, whales, dolphins, porpoises) as Cetacea than is Hippopotamidae (Fig. 1). Hippopotamidae is the the sister group to the extinct family Raoellidae, and Hippopotamidae exclusive sister group to Cetacea plus Raoellidae in the analysis that as more closely related to pigs and peccaries (that is, Suina) than to down-weights homoplastic characters, althoughin the equallyweighted cetaceans. However, our reanalysis of a modified version of the data set analysis, another topology was equally parsimonious. In that topology, they used2 differs in retaining molecular characters and demonstrates Hippopotamidae moved one node out, being the sister group to an that Hippopotamidae is the closest extant family to Cetacea and that Andrewsarchus, Raoellidae and Cetacea clade. In neither analysis is raoellids are the closest extinct group, consistent with previous phylo- Hippopotamidae closer to the pigs and peccaries than to Cetacea, the genetic studies2,3. This topology supports the view that the aquatic result obtained by Thewissen et al.1. In all our analyses, pachyostosis adaptations in hippopotamids and cetaceans are inherited from their (thickening) of limb bones and bottom walking, which occur in hippo- common ancestor4. potamids9,10, are interpreted to have evolved before the pachyostosis of To conduct our analyses, we started with the same published matrix the auditory bulla, as seen in raoellids and cetaceans1. -
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. -
Chapter 26 Cenozoic Life
236 Chapter 26 Cenozoic Life GUIDED STUDY The text chapter should be studied one section at a time. Life on Land (pp. 552-560) Before you read, preview each section by skimming it, noting headings and boldface items. Then read the 5. Describe the adaptations of grasses and herbaceous appropriate section objectives from the following plants that caused their spectacular radiation in the outline. Keep these objectives in mind and, as you read Cenozoic. the chapter section, search for the information that will enable you to meet each objective. Once you have finished a section, write out answers for its objectives. Cenozoic Marine Life (pp. 550-552) 1. List examples of major invertebrate groups that were missing from Cenozoic seas. 6. Discuss the diversification of birds in the Cenozoic, and the dominant roles they played. 2. Describe the diversification of foraminifera during the early Cenozoic. 7. Marsupial mammals developed in both South America and Australia. Why did those in South America suffer greatly from extinction in the Pliocene Epoch, but those in Australia have survived untouched until modern times? 3. Which marine invertebrates seemed little affected by the Cretaceous-Tertiary extinction event? 8. Describe the different stages in the development of the modern horse. What features underwent the most change, and why? 4. Describe the various forms that led to the evolution of whales from original land-based predators. Copyright © Houghton Mifflin Company. All rights reserved. 237 Quaternary Extinctions (pp. 560-562) CHAPTER REVIEW 9. Describe the kinds of animals, both mammal and When you have finished reading the chapter, work bird, that were lost in the late Quaternary extinction through the material that follows to review it.