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Vita Scientia Revista De Ciências Biológicas Do CCBS
Volume III - Encarte especial - 2020 Vita Scientia Revista de Ciências Biológicas do CCBS © 2020 Universidade Presbiteriana Mackenzie Os direitos de publicação desta revista são da Universidade Presbiteriana Mackenzie. Os textos publicados na revista são de inteira responsabilidade de seus autores. Permite-se a reprodução desde que citada a fonte. A revista Vita Scientia está disponível em: http://vitascientiaweb.wordpress.com Dados Internacionais de Catalogação na Publicação (CIP) Vita Scientia: Revista Mackenzista de Ciências Biológi- cas/Universidade Presbiteriana Mackenzie. Semestral ISSN:2595-7325 UNIVERSIDADE PRESBITERIANA MACKENZIE Reitor: Marco Túllio de Castro Vasconcelos Chanceler: Robinson Granjeiro Pro-Reitoria de Graduação: Janette Brunstein Pro-Reitoria de Extensão e Cultura: Marcelo Martins Bueno Pro-Reitoria de Pesquisa e Pós-Graduação: Felipe Chiarello de Souza Pinto Diretora do Centro de Ciências Biológicas e da Saúde: Berenice Carpigiani Coordenador do Curso de Ciências Biológicas: Adriano Monteiro de Castro Endereço para correspondência Revista Vita Scientia Centro de Ciências Biológicas e da Saúde Universidade Presbiteriana Mackenzie Rua da Consolação 930, São Paulo (SP) CEP 01302907 E-mail: [email protected] Revista Vita Scientia CONSELHO EDITORIAL Adriano Monteiro de Castro Camila Sachelli Ramos Fabiano Fonseca da Silva Leandro Tavares Azevedo Vieira Patrícia Fiorino Roberta Monterazzo Cysneiros Vera de Moura Azevedo Farah Carlos Eduardo Martins EDITORES Magno Botelho Castelo Branco Waldir Stefano CAPA Bruna Araujo PERIDIOCIDADE Publicação semestral IDIOMAS Artigos publicados em português ou inglês Universidade Presbiteriana Mackenzie, Revista Vita Scientia Rua da Consolaçãoo 930, Edíficio João Calvino, Mezanino Higienópolis, São Paulo (SP) CEP 01302-907 (11)2766-7364 Apresentação A revista Vita Scientia publica semestralmente textos das diferentes áreas da Biologia, escritos em por- tuguês ou inglês: Artigo resultados científicos originais. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
New Chondrichthyans from Bartonian-Priabonian Levels of Río De Las Minas and Sierra Dorotea, Magallanes Basin, Chilean Patagonia
Andean Geology 42 (2): 268-283. May, 2015 Andean Geology doi: 10.5027/andgeoV42n2-a06 www.andeangeology.cl PALEONTOLOGICAL NOTE New chondrichthyans from Bartonian-Priabonian levels of Río de Las Minas and Sierra Dorotea, Magallanes Basin, Chilean Patagonia *Rodrigo A. Otero1, Sergio Soto-Acuña1, 2 1 Red Paleontológica Universidad de Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Santiago, Chile. [email protected] 2 Área de Paleontología, Museo Nacional de Historia Natural, Casilla 787, Santiago, Chile. [email protected] * Corresponding author: [email protected] ABSTRACT. Here we studied new fossil chondrichthyans from two localities, Río de Las Minas, and Sierra Dorotea, both in the Magallanes Region, southernmost Chile. In Río de Las Minas, the upper section of the Priabonian Loreto Formation have yielded material referable to the taxa Megascyliorhinus sp., Pristiophorus sp., Rhinoptera sp., and Callorhinchus sp. In Sierra Dorotea, middle-to-late Eocene levels of the Río Turbio Formation have provided teeth referable to the taxa Striatolamia macrota (Agassiz), Palaeohypotodus rutoti (Winkler), Squalus aff. weltoni Long, Carcharias sp., Paraorthacodus sp., Rhinoptera sp., and indeterminate Myliobatids. These new records show the presence of common chondrichtyan diversity along most of the Magallanes Basin. The new record of Paraorthacodus sp. and P. rutoti, support the extension of their respective biochrons in the Magallanes Basin and likely in the southeastern Pacific. Keywords: Cartilaginous fishes, Weddellian Province, Southernmost Chile. RESUMEN. Nuevos condrictios de niveles Bartoniano-priabonianos de Río de Las Minas y Sierra Dorotea, Cuenca de Magallanes, Patagonia Chilena. Se estudiaron nuevos condrictios fósiles provenientes de dos localidades, Río de Las Minas y Sierra Dorotea, ambas en la Región de Magallanes, sur de Chile. -
A Review of Tertiary Climate Changes in Southern South America and the Antarctic Peninsula. Part 1: Oceanic Conditions
Sedimentary Geology 247–248 (2012) 1–20 Contents lists available at SciVerse ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Review A review of Tertiary climate changes in southern South America and the Antarctic Peninsula. Part 1: Oceanic conditions J.P. Le Roux Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile/Centro de Excelencia en Geotérmia de los Andes, Casilla 13518, Correo 21, Santiago, Chile article info abstract Article history: Oceanic conditions around southern South America and the Antarctic Peninsula have a major influence on cli- Received 11 July 2011 mate patterns in these subcontinents. During the Tertiary, changes in ocean water temperatures and currents Received in revised form 23 December 2011 also strongly affected the continental climates and seem to have been controlled in turn by global tectonic Accepted 24 December 2011 events and sea-level changes. During periods of accelerated sea-floor spreading, an increase in the mid- Available online 3 January 2012 ocean ridge volumes and the outpouring of basaltic lavas caused a rise in sea-level and mean ocean temper- ature, accompanied by the large-scale release of CO . The precursor of the South Equatorial Current would Keywords: 2 fi Climate change have crossed the East Paci c Rise twice before reaching the coast of southern South America, thus heating Tertiary up considerably during periods of ridge activity. The absence of the Antarctic Circumpolar Current before South America the opening of the Drake Passage suggests that the current flowing north along the present western seaboard Antarctic Peninsula of southern South American could have been temperate even during periods of ridge inactivity, which might Continental drift explain the generally warm temperatures recorded in the Southeast Pacific from the early Oligocene to mid- Ocean circulation dle Miocene. -
Redalyc.A Late Eocene Age Proposal for the Loreto Formation (Brunswick
Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Otero, Rodrigo A; Torres, Teresa; Le Roux, Jacobus P.; Hervé, Francisco; Fanning, C. Mark; Yury- Yáñez, Roberto E.; Rubilar-Rogers, David A Late Eocene age proposal for the Loreto Formation (Brunswick Peninsula, southernmost Chile), based on fossil cartilaginous fishes, paleobotany and radiometric evidence Andean Geology, vol. 39, núm. 1, enero, 2012, pp. 180-200 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173922203009 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 39 (1): 180-200. January, 2012 Andean Geology formerly Revista Geológica de Chile www.andeangeology.cl A Late Eocene age proposal for the Loreto Formation (Brunswick Peninsula, southernmost Chile), based on fossil cartilaginous fishes, paleobotany and radiometric evidence Rodrigo A. Otero1, Teresa Torres2, Jacobus P. Le Roux3, Francisco Hervé4, C. Mark Fanning5, Roberto E. Yury-Yáñez6, David Rubilar-Rogers7 1 Consejo de Monumentos Nacionales, Av. Vicuña Mackenna 084, Providencia, Santiago, Chile. [email protected] 2 Facultad de Ciencias Agronómicas, Universidad de Chile, Av. Santa Rosa 11315, Santiago, Chile. [email protected] 3 Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile. [email protected] 4 Escuela de Ciencias de la Tierra, Facultad de Ingeniería, Universidad Nacional Andrés Bello, Sazie 2350, Santiago, Chile. -
Lamniformes, Odontaspididae) from the Eocene of Antarctica Provides New Information About the Paleobiogeography and Paleobiology of Paleogene Sand Tiger Sharks
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 124(2): 283-298. July 2018 THE SOUTHERNMOST OCCURRENCE OF BRACHYCARCHARIAS (LAMNIFORMES, ODONTASPIDIDAE) FROM THE EOCENE OF ANTARCTICA PROVIDES NEW INFORMATION ABOUT THE PALEOBIOGEOGRAPHY AND PALEOBIOLOGY OF PALEOGENE SAND TIGER SHARKS GIUSEPPE MARRAMÀ1*, ANDREA ENGELBRECHT1, THOMAS MÖRS2, MARCELO A. REGUERO3 & JÜRGEN KRIWET1 1*Corresponding author. Department of Paleontology, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria. E-mail: [email protected], [email protected], [email protected] 2 Department of Paleozoology, Swedish Museum of Natural History, P.O, Box 50007, SE-104 05 Stockholm, Sweden. E-mail: [email protected] 3 Division Paleontologia de Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 81900 FWA La Plata, Argentina, CONICET. E-mail: [email protected] ARKU To cite this article: Marramà G., Engelbrecht A., Mörs T., Reguero M.A. & Kriwet J. (2018) - The southernmost occurrence of Brachycarcharias (Lamniformes, Odontaspididae) from the Eocene of Antarctica provides new information about the paleobiogeography and paleobiology of Paleogene sand tiger sharks. Riv. It. Paleontol. Strat., 124(2): 283-298. Keywords: Chondrichthyes; Elasmobranchii; Ypresian; La Meseta Formation; biotic turnovers. Abstract. The first record of one of the most common and widespread Paleogene selachians, the sand tiger shark Brachycarcharias, in the Ypresian strata of the La Meseta Formation, Seymour Island, Antarctica, is pro- vided herein. Selachians from the early Eocene horizons of this deposit represent the southernmost Paleogene occurrences in the fossil record, and are represented by isolated teeth belonging to orectolobiforms, lamniforms, carcharhiniforms, squatiniforms and pristiophoriforms. -
Mary Anning: Princess of Palaeontology and Geological Lioness
The Compass: Earth Science Journal of Sigma Gamma Epsilon Volume 84 Issue 1 Article 8 1-6-2012 Mary Anning: Princess of Palaeontology and Geological Lioness Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/compass Part of the Paleontology Commons Recommended Citation Davis, Larry E. (2012) "Mary Anning: Princess of Palaeontology and Geological Lioness," The Compass: Earth Science Journal of Sigma Gamma Epsilon: Vol. 84: Iss. 1, Article 8. Available at: https://digitalcommons.csbsju.edu/compass/vol84/iss1/8 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in The Compass: Earth Science Journal of Sigma Gamma Epsilon by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. Figure. 1. Portrait of Mary Anning, in oils, probably painted by William Gray in February, 1842, for exhibition at the Royal Academy, but rejected. The portrait includes the fossil cliffs of Lyme Bay in the background. Mary is pointing at an ammonite, with her companion Tray dutifully curled beside the ammonite protecting the find. The portrait eventually became the property of Joseph, Mary‟s brother, and in 1935, was presented to the Geology Department, British Museum, by Mary‟s great-great niece Annette Anning (1876-1938). The portrait is now in the Earth Sciences Library, British Museum of Natural History. A similar portrait in pastels by B.J.M. Donne, hangs in the entry hall of the Geological Society of London. -
Smithsonian Contributions to Paleobiology • Number 90
SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER 90 Geology and Paleontology of the Lee Creek Mine, North Carolina, III Clayton E. Ray and David J. Bohaska EDITORS ISSUED MAY 112001 SMITHSONIAN INSTITUTION Smithsonian Institution Press Washington, D.C. 2001 ABSTRACT Ray, Clayton E., and David J. Bohaska, editors. Geology and Paleontology of the Lee Creek Mine, North Carolina, III. Smithsonian Contributions to Paleobiology, number 90, 365 pages, 127 figures, 45 plates, 32 tables, 2001.—This volume on the geology and paleontology of the Lee Creek Mine is the third of four to be dedicated to the late Remington Kellogg. It includes a prodromus and six papers on nonmammalian vertebrate paleontology. The prodromus con tinues the historical theme of the introductions to volumes I and II, reviewing and resuscitat ing additional early reports of Atlantic Coastal Plain fossils. Harry L. Fierstine identifies five species of the billfish family Istiophoridae from some 500 bones collected in the Yorktown Formation. These include the only record of Makairapurdyi Fierstine, the first fossil record of the genus Tetrapturus, specifically T. albidus Poey, the second fossil record of Istiophorus platypterus (Shaw and Nodder) and Makaira indica (Cuvier), and the first fossil record of/. platypterus, M. indica, M. nigricans Lacepede, and T. albidus from fossil deposits bordering the Atlantic Ocean. Robert W. Purdy and five coauthors identify 104 taxa from 52 families of cartilaginous and bony fishes from the Pungo River and Yorktown formations. The 10 teleosts and 44 selachians from the Pungo River Formation indicate correlation with the Burdigalian and Langhian stages. The 37 cartilaginous and 40 bony fishes, mostly from the Sunken Meadow member of the Yorktown Formation, are compatible with assignment to the early Pliocene planktonic foraminiferal zones N18 or N19. -
A New Shark and Ray Fauna from the Middle Miocene of Mazan, Vaucluse
Swiss J Palaeontol (2011) 130:241–258 DOI 10.1007/s13358-011-0025-4 A new shark and ray fauna from the Middle Miocene of Mazan, Vaucluse (southern France) and its importance in interpreting the paleoenvironment of marine deposits in the southern Rhodanian Basin Nicolas Vialle • Sylvain Adnet • Henri Cappetta Received: 10 March 2011 / Accepted: 29 August 2011 / Published online: 16 September 2011 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2011 Abstract Recent paleontological excavations of the the last decades from several localities in the Natural Park Middle Miocene sandstones (top of the ‘‘Schlier’’ facies) of Lube´ron (South of Vaucluse). Selachian associations near Mazan, Vaucluse (southern France) uncovered a rich recovered in the Middle Miocene of Vaucluse are quite selachian teeth assemblage including 34 shark and ray particular because they indicate either neritic or deepwater species. This great diversity of selachian taxa provides new deposits. Such difference in faunal composition between information about the palaeoenvironmental settings of sites can be interpreted as a difference in age, a geo- some Middle Miocene deposits in the southern Rhodanian graphical heterogeneity of environmental deposits or a basin. For instance, the co-occurrence of some deepwater mixture of both. A new fossil locality, found in 2007 near Squaliformes and Rajidae with numerous Carcharhinifor- Mazan, was collected by one of the authors (H. Cappetta) mes and Myliobatiformes, usually inhabiting the conti- with the kind help of Eric Collier. A preliminary analysis nental shelf, suggests a deepwater deposit inshore, as indicates that the new rich selachian fauna comprises both adjacent to a submarine canyon area. types of the previous associations. -
Introduction and Bibliography
Downloaded from http://sp.lyellcollection.org/ by guest on October 3, 2021 Introduction and bibliography MIKE SMITH*, ZERINA JOHANSON, PAUL M. BARRETT & M. RICHTER Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK *Corresponding author (e-mail: [email protected]) Arthur Smith Woodward (1864–1944) was ac- Wegener was proposing his theory of continental knowledged as the world’s foremost authority on drift. It would be almost half a century before fossil fishes during his lifetime and made impor- his theory gained widespread acceptance. Hallam tant contributions to the entire field of vertebrate (1983, p. 135) wrote in Great Geological Contro- palaeontology. He was a dedicated public servant, versies that ‘The American palaeontologist G. G. spending his whole career at the British Museum Simpson noted in 1943 the near unanimity of (Natural History) (now the Natural History Museum, palaeontologists against Wegener’s ideas’. Smith NHM) in London. He served on the council and as Woodward certainly fell into this camp but was president of many of the important scientific socie- more inclined to note that no certainty could yet be ties and was elected a Fellow of the Royal Society attached to the palaeontological evidence (Wood- in 1901. He was knighted on retirement from the ward 1935). Scientific theories that we accept today Museum in 1924. were still controversial and intensely debated while Smith Woodward was born on 23 May 1864 in Smith Woodward was alive. Macclesfield, an industrial town in the north Mid- A book that celebrates the life and scientific lands of England. -
Aurora Fossil Museum Fossil Shark Tooth Frequency
North Carolina Shark Teeth Fossils Age Size and Frequency Checklist Name Scientific Name Size Frequency Cretaceous Paleocene Eocene Oligocene Miocene Pliocene Requiem Abdounia cnniskilleni ⅛˝ - ½˝ Singular • Requiem Abdounia lapierrei ⅛˝ - ¼˝ Very Rare • Requiem Abdounia recticona ¼˝ - ⅜˝ Occasional • Thresher Alopias superciliosus ¼˝ - ½˝ Rare • • Thresher Alopias vulpinus ½˝ - ¾˝ Very Rare • Ray Brachyrhizodus wichitaensis ½˝ - 1˝ Rare • Requiem Carcharhinus gibbesi ¼˝ - ⅜˝ Singular • Requiem Carcharhinus leucas ¼˝ - 1˝ Plentiful • • Sand Carcharias holmdelensis ¼˝ - ¾˝ † • Sand Tiger Carcharias koerti 1˝ - 2½˝ Very Rare • Sand Carcharias taurus ½˝ - 1½˝ Common • • Sand Tiger Carcharias vincenti ½˝ - 1 Very Rare • Giant White Carcharocles angustidens 1˝ - 4½˝ Rare • Giant White Carcharocles auriculatis 1˝ - 4½˝ Occasional • Giant White Carcharocles chubutensis 1˝ - 4½˝ Occasional • • Giant White Carcharocles megalodon 1˝ - 6¾˝ Occasional • • Giant White Carcharocles carcharias ½˝ - 2½˝ Rare • • Lamna Carcharoides catticus ½˝ - 1˝ Singular • Mackerel Cretodus arcuata ½˝ - 1˝ Rare • Mackerel Cretolamna appendiculata ½˝ - 1˝ Rare • Mackerel Cretolamna biauriculata ½˝ - 1˝ Occasional • String Ray Dasyatis jaekeli ⅛˝ - ¼˝ Singular • Bramble Echinorhinus blakei ¼˝ - ¾˝ Very Rare • • Tiger Galeocerdo contortus ½˝ - 1˝ Plentiful • • • • Tiger Galeocerdo cuvier ½˝ - 1½˝ Common • • Tiger Galeocerdo eaglesomei ½˝ - 1˝ Very Rare • Tiger Galeocerdo latidens ¼˝ - ½˝ Very Rare • Nurse Ginglymostoma africanum ⅛˝ - ¼˝ Singular • Snaggletooth Hemipristis -
Middle Eocene Vertebrate Fauna from the Aridal Formation, Sabkha of Gueran, Southwestern Morocco
geodiversitas 2021 43 5 e of lif pal A eo – - e h g e r a p R e t e o d l o u g a l i s C - t – n a M e J e l m a i r o DIRECTEUR DE LA PUBLICATION / PUBLICATION DIRECTOR : Bruno David, Président du Muséum national d’Histoire naturelle RÉDACTEUR EN CHEF / EDITOR-IN-CHIEF : Didier Merle ASSISTANT DE RÉDACTION / ASSISTANT EDITOR : Emmanuel Côtez ([email protected]) MISE EN PAGE / PAGE LAYOUT : Emmanuel Côtez COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD : Christine Argot (Muséum national d’Histoire naturelle, Paris) Beatrix Azanza (Museo Nacional de Ciencias Naturales, Madrid) Raymond L. Bernor (Howard University, Washington DC) Alain Blieck (chercheur CNRS retraité, Haubourdin) Henning Blom (Uppsala University) Jean Broutin (Sorbonne Université, Paris, retraité) Gaël Clément (Muséum national d’Histoire naturelle, Paris) Ted Daeschler (Academy of Natural Sciences, Philadelphie) Bruno David (Muséum national d’Histoire naturelle, Paris) Gregory D. Edgecombe (The Natural History Museum, Londres) Ursula Göhlich (Natural History Museum Vienna) Jin Meng (American Museum of Natural History, New York) Brigitte Meyer-Berthaud (CIRAD, Montpellier) Zhu Min (Chinese Academy of Sciences, Pékin) Isabelle Rouget (Muséum national d’Histoire naturelle, Paris) Sevket Sen (Muséum national d’Histoire naturelle, Paris, retraité) Stanislav Štamberg (Museum of Eastern Bohemia, Hradec Králové) Paul Taylor (The Natural History Museum, Londres, retraité) COUVERTURE / COVER : Réalisée à partir des Figures de l’article/Made from the Figures of the article. Geodiversitas est