Anhang A: Körper- Und Spurenfossilien Von Dinosauriern

Total Page:16

File Type:pdf, Size:1020Kb

Anhang A: Körper- Und Spurenfossilien Von Dinosauriern Anhang A: Körper- und Spurenfossilien von Dinosauriern Bisher wurde nie richtig honoriert, wie lange und wie intensiv die Menschheit schon nach Dinosauriern sucht. Dinosaurierfossilien wurden bisher überall auf der Erde gefunden- allein schon in 31 der 50 US-Bundesstaaten. David Weishampel von der Johns Hopkins University hat alle Funde chronologisch und mit viel Akribie in dem von ihm herausgegebenen Werk The Dinosauria (siehe Anhang C: Empfehlenswerte Literatur) aufgelistet. Anband dieser Aufstellung wurden auf den folgenden Seiten alle Funde nach Ländern (bzw. Regionen) und Perioden geordnet und in die sich anschlie­ ßenden Karten eingetragen. Diese Daten wurden -mit Weishampels Genehmigung - auf den neuesten Stand gebracht. 278 DINOSAURIERFORSCHER Schlüssel T =Trias J=Jura K =Kreide Afrika Australien ÄgyptenK Neuseeland (Nordinsel) K Algerien 1, K Nordaustralien K Kenia K Queensland T, 1, K Lesotho T, J Südostaustralien K LibyenK Westaustralien K Madagaskar 1, K MalawiJ Europa MaliK Belgien T, K Marokko T, J, K Deutschland T, J, K NamibiaJ Frankreich T, J, K Niger J, K Italien T Simbabwe T, 1 Jugoslawien K Südafrika T, J, K Niederlande K Tansania 1 NorwegenK Tunesien K Österreich K Polen T Antarktis Portugal 1, K Antarktis J, K RumänienK Rußland K Asien SchwedenJ Afghanistan 1 Schweiz T, 1 China (Nordostchina) K Spanien J, K China (Nordwestchina) J, K Tschechische Republiken China (Südostchina) K (vordem: Tschechoslowakei) K China (Südwestchina) T, J, K UngamJ China (Zentralchina) J, K Vereinigtes Königreich T, J, K Indien (Nordostindien) J, K Indien (Südostindien) T, J, K Nordamerika Indien (Westindien) K AlabamaK Iran 1 AlaskaJ, K Israel K Arizona T, J, K Japan K Arkansas K Kasachstan K Colorado T, J, K LaosK Connecticut 1 Mongolei K Delaware K Sibirien K Georgia K SüdkoreaK Idaho K Syrien K Kalifomien K Thailand 1, K Kanada (Ostkanada) T, 1 Anhang A: Körper- und Spurenfossilien von Dinosauriern 279 Kanada (Westkanada) K OregonK Kanada (Yukon) K Pennsylvania T Kansas K South Dakota J, K MarylandK Texas T,J, K Massachusetts T, J Utah T,J,K MexikoK Virginia T Mississippi K WyomingJ,K Missouri K MontanaK Südamerika NebraskaK Argentinien T, J, K NevadaK Bolivien K New Jersey T, J, K Brasilien T, J, K New Mexico T, J, K ChileJ,K NewYorkT Kolumbien J, K North Carolina T, K PeruK North Dakota K UruguayK Oklahoma J, K c CJ T c c TJ TJ c AC T TC& c c c c A J JC JC TJ' c c TA CJc c AA c c ~c J AA JC C C C c A cc A c ATLANTIK c c JC PAZIFIK CJ c c cJ c Die heutige Weit A Spuren- und Körperfossilien von Dinosauriern T =Trias J = Jura C = Cretaceous (Kreide) & = Alle drei Perioden (Zeichnung von Deborah Perugi) c NORDPOLARMEER c J c T T :& c c CJ c c c T C c JC c cc J J JC c c c ... PAZIFIK c JC c c ... JC c J J c c TJ J INDISCHER J c ... .6. TJ OZEAN c c J Anhang B: Fundorte und Museen mit Dinosaurierfossilien Die folgenden Einrichtungen sind alphabetisch erst länderweise, dann nach Namen geordnet. Argentinien Museo Argentinode Ciencias Naturales, Buenos Aires Museode la Universidad de La Plata, La Plata Australien Australian Museum, Sydney Queensland Museum, Fortitude V alley Belgien Institut Royal des Seiences Naturelles, Brüssel Brasilien Museu Nacional, Rio de Janeiro China Beipei-Museum, Szetschuan Chengdu-Institut, Chengdu Institut für Wirbeltierpaläontologie und Paläoanthropologie, Peking Museum der Inneren Mongolei, Hohehot Museum für Naturgeschichte, Peking Naturhistorisches Museum Chungking (Qongqing), Szetschuan Dinosauriermuseum Zigong, Szetschuan Deutschland Bayerische Staatssammlung für Paläontologie und Geschichte der Geologie, München Geologisch-Paläontologisches Institut, Münster Humboldt-Museum für Naturalgeschichte, Berlin Institut und Museum für Geologie und Paläontologie, Tübingen Landesmuseum für Naturgeschichte, Stuttgart Landesmuseum für Naturgeschichte, Ludwigsburg Senckenberg-Museum der Naturgeschichte, Frankfurt (Main) 284 DINOSAURIERFORSCHER Frankreich Musee Nationale de l'Histoire Naturelle, Paris Großbritannien Birmingham Museum, Birmingham British Museum ofNatural History, London Crystal Palace Park, Sydenham, London The Dinosaur Museum, Dorchester, Darset Hunterian Museum, The University, Glasgow The Leicestershire Museums, Leicester Museum of Isle of Wight Geology, Sandown Royal Scottish Museum, Edinburgh Sedgwick Museum, Cambridge University Museum, Oxford Indien Geology Museum, Kalkutta Italien Museo Civico di Storia Naturale di Venezia, Venedig Museo G. Capinelli, Bologna Kanada Calgary Zoological Gardens, Alberta Dinosaur Provincial Park, Patricia, Alberta National Museum of Natural Sciences, Ottawa, Ontario Provincial Museum of Alberta, Edmonton, Alberta Royal Ontario Museum, Toronto, Ontario Tyrrell Museum ofPalaeontology, Drumheller, Alberta Marokko Museum für Geowissenschaften, Rabat Mongolische Republik Staatliches Zentralmuseum, Ulan Bator Niger Musee Nationale du Niger, Niamey Österreich Naturhistorisches Museum, Wien Polen Dinosaurierpark, Chorz6w, Schlesien Anhang B: Fundorte und Museen mit Dinosaurierfossilien 285 Institut für Paläobiologie, Warschau Rußland Zentralmuseum für Geologie und Bergbau, St. Petersburg Paläontologisches Institut, Moskau Simbabwe National Museum of Zimbabwe, Harare Südafrika (RSA) Bemard Price Institute ofPaleontology, Johannesburg South African Museum, Kapstadt Schweden Paläontologisches Museum, Uppsala Schweiz Musee d'Historie Naturelle, Genf Naturhistorisches Museum, Basel Naturhistorisches Museum, Bem Naturhistorisches Museum, St. Gallen Naturmuseum, Solothum Paläontologisches Institut und Museum, Zürich Taiwan Dinosaur Hall, National Zoo, Taipeh USA Academy of Natural Science, Philadelphia Alexander Ruthven Museums, University of Michigan, Ann Arbor American Museum ofNatural History, New York Amherst College, Amherst, Massachusetts Califomia Academy of Sciences, San Francisco Camegie Academy ofNatural History, Pittsburgh Cleveland Museum of Natural History Denver Museum ofNatural History Dinosaur National Monument, Jensen, Utah Dinosaur State Park, Rocky Hill, Connecticut (hier kann man selbst Gipsabdrücke von Dinosaurierspuren machen) Dinosaur Valley Museum, Grand Junction, Colorado Dinosaur Valley State Park, Glen Rose, Texas Earth Seiences Museum, Brigham Young University, Provo, Utah Field Museum of Natural History, Chicago Fort Worth Museum of Science, Texas Geological Museum, University of Wyoming, Laramie 286 DINOSAURIERFORSCHER Ghost Ranch, Ruth Hall Paleontology Room, Albuquerque, New Mexico Houston Museum of Natural Science, Houston Los Angeles County Museum of Natural History LSU Museum of Geoscience, Baton Rouge, Louisiana Museum of Comparative Zoology, Cambridge, Massachusetts Museum ofNatural History, University ofKansas, Kansas Museum ofNorthem Arizona, Flagstaff, Arizona Museum of Paleontology, University of Califomia, Berkeley, Kalifomien Museum ofthe Rockies, MontanaState University, Bozeman National Museum ofNatural History, Smithsonian Institution, Washington, D.C. Nebraska State Museum, University of Nebraska, Lincoln New Mexico Museum ofNatural History, Albuquerque Peabody Museum ofNatural History, Yale University, New Haven, Connecticut Petrified Forest National Park, Arizona Prehistoric Museum and Cleveland-Lloyd Dinosaur Quarry, Price, Utah Science Museum of St. Paul, St. Paul, Minnesota Teton Trail Village Museum, Choteau, Montana Texan Memorial Museum, University of Texas, Austin Trail Through Time, Grand Junction, Colorado Utah Field House of Natural History State Park and Dinosaur Gardens, Vemal Utah Museum ofNatural History, Salt Lake City Aktuelle Ausgrabungen Boston Museum of Science, Boston, Massachusetts The Dinosaur Society, New Bedford, Massachusetts Dinarnation International Corporation, San Juan Capistrano, Kalifomien Earthwatch, Watertown, Massachusetts Lawrence Hall of Science, University of Califomia, Berkeley, Kalifomien Milwaukee Public Museum, Milwaukee, Wisconsin Museum ofthe Rockies, MontanaState University, Bozeman, Montana Oregon Museum of Science and Industry, Portland, Oregon Southwest Paleontology Foundation, Albuquerque, New Mexico Anhang C: Empfehlenswerte Literatur Heute gibt es sehr viel aktuelle Literatur, die auch den absoluten Laien mit verschie­ denen Aspekten der Paläontologie, ihren Wissenschaftlern und natürlich auch mit den Dinosauriern bekannt macht. Viele der folgenden Werke sind in englischer Sprache verfaßt worden, viele von ihnen wurden allerdings mittlerweile auch ins Deutsche übertragen. Zusätzlich aufgenommene deutsche Titel wurden vom Übersetzer mit einem Sternchen versehen. Alexander, R. McNeill: Dynamics of Dinosaurs and Other Extinct Giants. Columbia University Press, New York 1989 (in Englisch). Ein sehr lebendig geschriebenes Buch, in dem die Fortbewegung der Dinosaurier wissenschaftlich untersucht wird. (Anmerkung für naturwissenschaftlich interessierte Leser: Vor einiger Zeit ist ein Artikel Alexanders zum gleichen Thema erschienen - Wie Dinosaurier sich fort­ bewegten. Spektrum der Wissenschaften, Heidelberg Juni 1991, Seite 82-89.) Bakker, Robert T.: The Dinosaur Heresies. William Morrow, New York 1986 (in Englisch). Auch als englische Taschenbuchausgabe bei Penguin Books, London 1986, erhältlich. Eine mit sehr viel Verve geschriebene Arbeit, in der Bakker seine sehr eigenwilligen Vorstellungen und Theorien darstellt. Das Buch enthält viele vom Autor selbst gezeichnete Illustrationen. Cox, Barry, Dougal Dixon, Brian Gardiner und R. J. Savage*: Dinosaurier und andere Tiere der Vorzeit. Umfangreiche, reich bebilderte Enzyklopädie zahlreicher Tiere, nicht nur des Mesozoikums.
Recommended publications
  • The Dashanpu Dinosaur Fauna of Zigong Sichuan Short Report V - Labyrinthodont Amphibia
    The Dashanpu Dinosaur Fauna of Zigong Sichuan Short Report V - Labyrinthodont Amphibia Zhiming Dong (Institute of Vertebrate Paleontology, Paleoanthropology, Academia Sinica) Vertebrata PalAsiatica Volume XXIII, No. 4 October, 1985 pp. 301-305 Translated by Will Downs Department of Geology Bilby Research Center Northern Arizona University December, 1990 Abstract A brief discussion is presented on the morphological characteristics and phylogenetic position of Sinobrachyops placenticephalus (gen. et sp. nov.). The specimen is derived from the well-known Middle Jurassic Dashanpu dinosaur quarries of Zigong County, Sichaun Province. Sinobrachyops is the youngest geological occurrence of a labyrinthodont amphibian known to date. Its discovery extends the upper geochronological limit for the Labyrinthodontia into the Middle Jurassic. Introduction The first fossils collected from Dashanpu, Zigong, in 1979, were a pair of rhachitomous vertebrae. This discovery created a sense of perplexity among the workers, for the morphology of these pleurocentra and intercentra suggested an assignment to the Labyrinthodontia. This group of amphibians, however, was traditionally believed to have become extinct in the Late Triassic, a traditional concept that must be abandoned if scientific investigation is to be advanced and left unfettered. In 1983 the Institute of Vertebrate Paleontology, Paleoanthropology Academia Sinica launched a paleontological expedition in the Shishugou Formation (Middle-Late Jurassic) from the Kelameili region, northeast Jungar Basin, Xinjiang Autonomous Region, where several rhachitomous vertebrae were discovered. Later, a fragmentary skull of a labyrinthodont amphibian was collected, confirming that this group extended into the Middle Jurassic. The discovery from the Shishugou Formation convinced the workers that the rhachitomous vertebrae at Dashanpu belonged to the Labyrinthodontia.
    [Show full text]
  • Searchable PDF (No Class Notes) (9.906Mb)
    The paper used in this publication is manufactured from 100%-recycled fiber of which 50% is recovered from Post Consumer sources. This product is made exclusively for New Leaf Paper in San Francisco, California by Plainwell Paper Company and was offered to Kalamazoo College with their permis­ Jllege learning experience takes this young member of sion. New Leaf Paper is nationally known for their active role in the design and marketing of paper products that II which people and communities the power of that are entirely recycled and recyclable. Two members of the Kalamazoo College Jirectly, as she uses it to build her future. Class of 1963 had active roles in the manufacture of these items. rndations that support Kalamazoo College. The others 1e. All are vital. Your Annual Fund gift makes the ~e possible for young people like her. Most annual fund gifts are applied to student scholarships and program or facility improvements. Annual fund gifts are unrestricted, which confers upon the College the opportunity to use them in ways to best support the K-Plan. And the degree of Annual Fund participation unlocks additional gifts from corporations and foundations. Alumni participation is one of the first facts requested by grant officers when they consider major funding proposals from the College. So thank you again, alumni and friends. For the second consecutive year the Annual Fund reached and exceeded its goal. It will help enlighten futures. KALAMAZOO COLLEGE A~fiutd 1 9 9 8 - 1 9 9 9 Time will tell where her Kalamazoo College learning experience takes this young member of the Class of 1999; and time will tell which people and communities the power of that experience will touch, directly and indirectly, as she uses it to build her future.
    [Show full text]
  • D Inosaur Paleobiology
    Topics in Paleobiology The study of dinosaurs has been experiencing a remarkable renaissance over the past few decades. Scientifi c understanding of dinosaur anatomy, biology, and evolution has advanced to such a degree that paleontologists often know more about 100-million-year-old dinosaurs than many species of living organisms. This book provides a contemporary review of dinosaur science intended for students, researchers, and dinosaur enthusiasts. It reviews the latest knowledge on dinosaur anatomy and phylogeny, Brusatte how dinosaurs functioned as living animals, and the grand narrative of dinosaur evolution across the Mesozoic. A particular focus is on the fossil evidence and explicit methods that allow paleontologists to study dinosaurs in rigorous detail. Scientifi c knowledge of dinosaur biology and evolution is shifting fast, Dinosaur and this book aims to summarize current understanding of dinosaur science in a technical, but accessible, style, supplemented with vivid photographs and illustrations. Paleobiology Dinosaur The Topics in Paleobiology Series is published in collaboration with the Palaeontological Association, Paleobiology and is edited by Professor Mike Benton, University of Bristol. Stephen Brusatte is a vertebrate paleontologist and PhD student at Columbia University and the American Museum of Natural History. His research focuses on the anatomy, systematics, and evolution of fossil vertebrates, especially theropod dinosaurs. He is particularly interested in the origin of major groups such Stephen L. Brusatte as dinosaurs, birds, and mammals. Steve is the author of over 40 research papers and three books, and his work has been profi led in The New York Times, on BBC Television and NPR, and in many other press outlets.
    [Show full text]
  • A Huge Predatory Dinosaur, Built to Swim
    Science Now Discoveries from the world of science and medicine Spinosaurus: A huge predatory dinosaur, built to swim A digital skeletal reconstruction and transparent flesh outline of Spinosaurus aegyptiacus. The bones suggest this dinosaur was built to swim. Color codes show the origin of different parts of the digital skeletal model. (Model by Tyler Keillor, Lauren Conroy and Erin Fitzgerald, Ibrahim et al., Science/AAAS) By AMINA KHAN SEPTEMBER 11, 2014, 9:45 PM inosaurs ruled the land for millions of years. Now scientists have discovered a fearsome D species that could have wreaked havoc in its prehistoric waters. An unusual fossil whose parts were flung across two continents appears to be the first known semi-aquatic dinosaur, according to a report published Thursday by the journal Science. Measuring 9 feet longer than a Tyrannosaurus rex, the 95-million-year-old Spinosaurus aegyptiacus would have been the largest predatory dinosaur to walk the Earth. But it had several features that strongly suggest a life spent largely submerged in the water, including nostrils pushed toward the top of its skull and diagonally jutted teeth ideal for snapping up fish. “It was not a balancing, two-legged animal on land,” said study coauthor Paul Sereno, a paleontologist at the University of Chicago. “It would have been something very peculiar.” The differences between this Spinosaurus and other theropods are apparent from head to toe. Most theropods, like T. rex, ran on two powerful legs and had small, spindly arms. By contrast, the 50-foot-long Spinosaurus had muscular arms with blade-like claws that could have nabbed slippery prey, and shorter legs that were ill-equipped to walk on land.
    [Show full text]
  • From Fossils to Phylogenies Part 1: Mass Spectrometry
    From Fossils to Phylogenies Part 1: Mass Spectrometry Written by: Baylee Goodwin, Dane Besser, Stephen A. Ramsey Dinosaur Vocabulary Words Chemistry Vocabulary Words Biology Vocabulary Words Fossilization Mass spectrometry Central Dogma of biology T. rex Mass-to-charge ratio Proteins Mastodon Ion Peptide Hadrosaur Relative abundance Protein Spectrum Collagen Background: Imagine it is time for your lunch break. You take your sandwich outside and you sit down to enjoy your lunch with a beautiful view of Montana’s Rocky Mountains. As you look up, you see what appears to be a bone sticking out of the side of a rock wall. That bone just so happens to be part of one of the best-preserved Tyrannosaurus rex fossils ever found. If you are Bob Harmon, a field crew chief of the Museum of the Rockies, ​ that is exactly what happened. In the year 2000 Bob Harmon discovered a 68 million-year-old fossil, which is now named “B-Rex” after him. Tyrannosaurus rex lived 65 to 70 million years ago, in what ​ is now the western parts of the United States. They were among the last of the large dinosaurs that lived on Earth. In certain rare cases, dinosaur bones were trapped in the Earth and were preserved until the present day, through a process called fossilization. Much of what we know about dinosaurs ​ ​ comes from the scientific study of the shape, appearance, composition, and location of fossils. Dinosaurs' bodies were made up of the same general types of biological building blocks seen in all animals, such as tissues, cells, and proteins.
    [Show full text]
  • GLACIERS and GLACIATION in GLACIER NATIONAL PARK by J Mines Ii
    Glaciers and Glacial ion in Glacier National Park Price 25 Cents PUBLISHED BY THE GLACIER NATURAL HISTORY ASSOCIATION IN COOPERATION WITH THE NATIONAL PARK SERVICE Cover Surveying Sperry Glacier — - Arthur Johnson of U. S. G. S. N. P. S. Photo by J. W. Corson REPRINTED 1962 7.5 M PRINTED IN U. S. A. THE O'NEIL PRINTERS ^i/TsffKpc, KALISPELL, MONTANA GLACIERS AND GLACIATTON In GLACIER NATIONAL PARK By James L. Dyson MT. OBERLIN CIRQUE AND BIRD WOMAN FALLS SPECIAL BULLETIN NO. 2 GLACIER NATURAL HISTORY ASSOCIATION. INC. GLACIERS AND GLACIATION IN GLACIER NATIONAL PARK By J Mines Ii. Dyson Head, Department of Geology and Geography Lafayette College Member, Research Committee on Glaciers American Geophysical Union* The glaciers of Glacier National Park are only a few of many thousands which occur in mountain ranges scattered throughout the world. Glaciers occur in all latitudes and on every continent except Australia. They are present along the Equator on high volcanic peaks of Africa and in the rugged Andes of South America. Even in New Guinea, which many think of as a steaming, tropical jungle island, a few small glaciers occur on the highest mountains. Almost everyone who has made a trip to a high mountain range has heard the term, "snowline," and many persons have used the word with­ out knowing its real meaning. The true snowline, or "regional snowline" as the geologists call it, is the level above which more snow falls in winter than can he melted or evaporated during the summer. On mountains which rise above the snowline glaciers usually occur.
    [Show full text]
  • Dec 2001 Entire
    P a l æ o n t o l o g i c a l S o c i e t y B u l l e t i n VOLUMEA 16 • NUMBER l 4 b e www.albertapaleo.org r t a DECEMBER 2001 ALBERTA PALÆONTOLOGICAL SOCIETY OFFICERS MEMBERSHIP: Any person with a sincere interest in President* Vaclav Marsovsky 547-0182 palaeontology is eligible to present their application for Vice-President* Dan Quinsey 247-3022 membership in the Society. (Please enclose membership Treasurer* (acting) Cindy Evans 285-0144 dues with your request for application.) Secretary* (acting)Dan Quinsey 247-3022 Single membership $15.00 annually Past-President* Wayne Braunberger 278-5154 Family or Institution $20.00 annually DIRECTORS Editor* Howard Allen 274-1858 THE BULLETIN WILL BE PUBLISHED Membership* Howard Allen 274-1858 QUARTERLY: March, June, September and Program Coordinator* Philip Benham 280-6283 December. Deadline for submitting material for Curator Ron Fortier 285-8041 publication is the 15th of the month prior to Librarian Mona Marsovsky 547-0182 publication. Events Coordinator* Keith Mychaluk 228-3211 Director at Large Dr. David Mundy 281-3668 Society Mailing Address: Social Director (position currently unfilled) Alberta Palaeontological Society APAC Representative† Vaclav Marsovsky 547-0182 P.O. Box 35111, Sarcee Postal Outlet * Officers and Directors marked with an asterisk are se- Calgary, Alberta, Canada T3E 7C7 nior board members for executive meeting quorum (Web: www.albertapaleo.org) purposes. † APAC is the Alberta Palaeontological Advisory Material for the Bulletin: Committee Howard Allen, Editor, APS 7828 Hunterslea Crescent, N.W. The Society was incorporated in 1986, as a non-profit Calgary, Alberta, Canada T2K 4M2 organization formed to: (E-mail: [email protected]) a.
    [Show full text]
  • Notas Sobre Spinosauridae (Theropoda, Dinosauria) Notes on Spinosauridae (Theropoda, Dinosauria)
    Anuário do Instituto de Geociências - UFRJ ISSN 0101-9759 Vol. 28-1 / 2005 p. 158-173 Notas Sobre Spinosauridae (Theropoda, Dinosauria) Notes on Spinosauridae (Theropoda, Dinosauria) Elaine Batista Machado1 & Alexander Wilhelm Armin Kellner2 1Setor de Paleovertebrados, Museu Nacional/UFRJ Quinta da Boa Vista s/n., São Cristóvão, Rio de Janeiro - RJ, CEP: 20940-040 e-mail: [email protected] 2Setor de Paleovertebrados, Museu Nacional/UFRJ Quinta da Boa Vista s/n., São Cristóvão, Rio de Janeiro - RJ, CEP: 20940-040 email: [email protected] Recebido: 08/11/2005 Aprovado: 19/11/2005 Resumo Os espinossaurídeos são encontrados na África, Europa, Ásia e Brasil em depósitos com idade variando do Jurássico Superior até o Cretáceo Superior, tendo sido descritos até a presente data oito espécies. Apesar desta grande distribuição temporal e geográfica, pouco se sabe sobre este grupo de dinossauros uma vez que a maior parte dos espécimes são incompletos. O clado Spinosauridae é dividido em Baryonychinae (Suchomimus + Baryonyx + Cristatosaurus) e Spinosaurinae (Spinosaurus+ Angaturama + Irritator). Apenas na África representantes destes dois clados foram encontrados. Uma possível explicação para a distribuição dos espinossaurídeos seria a dispersão de formas relacionadas a Baryonyx (o mais primitivo membro do grupo) da Europa para a África, onde surgiram os Spinosaurinae que posteriormente se distribuíram para a América do Sul. Palavras-chave: Dinosauria, Theropoda, Spinosauridae Abstract Spinosaur remains were collected in Africa, Europa, Asia and Brazil, coming from deposits with ages ranging from the Late Jurassic to the Late Cretaceous. Although having a wide distribution - both geographically and temporally - little is actually known about the group since most specimens are incomplete.
    [Show full text]
  • FIELDREPORT Northern Rockies | Summer 2015
    FIELDREPORT Northern Rockies | Summer 2015 Sacred Ground A Lasting Legacy for Grand Teton Protecting the “Backbone of the World” By Sharon Mader Efforts to transfer ownership of state lands to Grand Teton Program Manager the Park Service are well underway, but are he Blackfeet Nation first encountered bound by an extremely ambitious timeline. Summer Celebration for Glacier’s North Fork the United States government in the resident Obama has an amazing The clock is ticking, and without immediate Tearly morning chill of July 27, 1806. opportunity, before the end of his action at the highest levels of government, Capt. Meriwether Lewis, returning with presidency, to create a profound his men from the Pacific, chanced upon P and lasting legacy for America’s national a band of eight young braves, camped in parks. As we look toward the Centennial spectacular buffalo country where unbroken of the National Park Service in August prairie crashes headlong into soaring 2016—NPCA is encouraging the peaks. What unfolded that morning was administration to prioritize protecting the only bloodshed recorded by Lewis lands in Grand Teton National Park that and Clark. are owned by the state of Wyoming. Before the summer sun had climbed high enough to warm the gravel banks of the More than 1,200 acres of state-owned Two Medicine River, two young Blackfeet lands fall within the boundary of the men—boys, really—were killed. park. These inholdings offer some of the most spectacular scenery and wildlife- Two centuries later, in 1982, the US viewing opportunities imaginable. Driving it’s possible this deal will not be completed in government returned to those very same by these lands, travelers assume these time.
    [Show full text]
  • 2013 NOV - I AM 19 REGIONS 8: R:·L L
    UNITED STATES ENVIRONMENTAL PROTECTION AGENCY 2013 NOV - I AM 19 REGIONS 8: r:·l L. ·1 . •- ..J Docket No. CWA-08-2014-0004 CPA HEGIOU VIII pr A~' l ~lc; CL FRI~ In the Matter of: ) ) Nelcon, Inc. ) ADMINISTRATIVE ORDER 304 Jellison Road ) FOR COMPLIANCE ON CONSENT Kalispell, Mt. 59903, ) ) Respondent. ) INTRODUCTION 1. This Administrative Order for Compliance on Consent (Consent Order) is entered into voluntarily by Nelcon, Inc. (Respondent) and the United States Environmental Protection Agency (EPA). The EPA has authority to issue this Consent Order pursuant to section 309(a) of the Clean Water Act (Act), 33 U.S.C. § 1319(a), which authorizes the Administrator of the EPA to issue an order requiring compliance by a person found to be in violation of, inter alia, section 301(a) of the Act. This authority has been properly delegated to the undersigned EPA official. 2. The Findings in paragraph numbers 7 through 44 below are made solely by the EPA. In signing this Consent Order, and for that limited purpose only, Respondent neither admits nor denies the Findings. 3. Without any admission of liability, Respondent consents to issuance of this Consent Order and agrees to abide by all of its conditions. Respondent waives any and all remedies, claims for relief, and otherwise available rights to judicial or administrative review that Respondent may have with respect to any issue of fact or law set forth in this Consent Order, including any right ofjudicial review of this Consent Order under the Administrative Procedure Page 1 of 12 Act, 5 U.S.C.
    [Show full text]
  • Triassic, Carnian) and the Early Evolution of Sauropodomorpha
    A Basal Sauropodomorph (Dinosauria: Saurischia) from the Ischigualasto Formation (Triassic, Carnian) and the Early Evolution of Sauropodomorpha Ricardo N. Martinez*, Oscar A. Alcober Museo de Ciencias Naturales, San Juan, Argentina Abstract Background: The earliest dinosaurs are from the early Late Triassic (Carnian) of South America. By the Carnian the main clades Saurischia and Ornithischia were already established, and the presence of the most primitive known sauropodomorph Saturnalia suggests also that Saurischia had already diverged into Theropoda and Sauropodomorpha. Knowledge of Carnian sauropodomorphs has been restricted to this single species. Methodology/Principal Findings: We describe a new small sauropodomorph dinosaur from the Ischigualsto Formation (Carnian) in northwest Argentina, Panphagia protos gen. et sp. nov., on the basis of a partial skeleton. The genus and species are characterized by an anteroposteriorly elongated fossa on the base of the anteroventral process of the nasal; wide lateral flange on the quadrate with a large foramen; deep groove on the lateral surface of the lower jaw surrounded by prominent dorsal and ventral ridges; bifurcated posteroventral process of the dentary; long retroarticular process transversally wider than the articular area for the quadrate; oval scars on the lateral surface of the posterior border of the centra of cervical vertebrae; distinct prominences on the neural arc of the anterior cervical vertebra; distal end of the scapular blade nearly three times wider than the neck; scapular blade with an expanded posterodistal corner; and medial lamina of brevis fossa twice as wide as the iliac spine. Conclusions/Significance: We regard Panphagia as the most basal sauropodomorph, which shares the following apomorphies with Saturnalia and more derived sauropodomorphs: basally constricted crowns; lanceolate crowns; teeth of the anterior quarter of the dentary higher than the others; and short posterolateral flange of distal tibia.
    [Show full text]
  • Paleontological Contributions
    Paleontological Contributions Number 14 The first giant raptor (Theropoda: Dromaeosauridae) from the Hell Creek Formation Robert A. DePalma, David A. Burnham, Larry D. Martin, Peter L. Larson, and Robert T. Bakker October 30, 2015 Lawrence, Kansas, USA ISSN 1946-0279 (online) paleo.ku.edu/contributions Life restoration by Emily Willoughby of Dakotaraptor steini running with the sparrow-sized birds, Cimolopteryx petra while the mammal, Purgatorius, can be seen in the foreground. Paleontological Contributions October 30, 2015 Number 14 THE FIRST GIANT RAPTOR (THEROPODA: DROMAEOSAURIDAE) FROM THE HELL CREEK FORMATION Robert A. DePalma1,2, David A. Burnham2,*, Larry D. Martin2,†, Peter L. Larson3 and Robert T. Bakker4 1 Department of Vertebrate Paleontology, The Palm Beach Museum of Natural History, Fort Lauderdale, Florida; 2 University of Kansas Bio- diversity Institute, Lawrence, Kansas; 3Black Hills Institute of Geological Research, Hill City, South Dakota; 4Houston Museum of Nature and Science, Houston, Texas; e-mail: [email protected] ABSTRACT Most dromaeosaurids were small- to medium-sized cursorial, scansorial, and arboreal, sometimes volant predators, but a comparatively small percentage grew to gigantic proportions. Only two such giant “raptors” have been described from North America. Here, we describe a new giant dromaeosaurid, Dakotaraptor steini gen. et sp. nov., from the Hell Creek Formation of South Dakota. The discovery represents the first giant dromaeosaur from the Hell Creek Formation, and the most recent in the fossil record worldwide. A row of prominent ulnar papilli or “quill knobs” on the ulna is our first clear evidence for feather quills on a large dromaeosaurid forearm and impacts evolutionary reconstructions and functional morphology of such derived, typically flight-related features.
    [Show full text]