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Vertebral Morphology, Dentition, Age, Growth, and Ecology of the Large Lamniform Shark Cardabiodon Ricki
Vertebral morphology, dentition, age, growth, and ecology of the large lamniform shark Cardabiodon ricki MICHAEL G. NEWBREY, MIKAEL SIVERSSON, TODD D. COOK, ALLISON M. FOTHERINGHAM, and REBECCA L. SANCHEZ Newbrey, M.G., Siversson, M., Cook, T.D., Fotheringham, A.M., and Sanchez, R.L. 2015. Vertebral morphology, denti- tion, age, growth, and ecology of the large lamniform shark Cardabiodon ricki. Acta Palaeontologica Polonica 60 (4): 877–897. Cardabiodon ricki and Cardabiodon venator were large lamniform sharks with a patchy but global distribution in the Cenomanian and Turonian. Their teeth are generally rare and skeletal elements are less common. The centra of Cardabiodon ricki can be distinguished from those of other lamniforms by their unique combination of characteristics: medium length, round articulating outline with a very thick corpus calcareum, a corpus calcareum with a laterally flat rim, robust radial lamellae, thick radial lamellae that occur in low density, concentric lamellae absent, small circular or subovate pores concentrated next to each corpus calcareum, and papillose circular ridges on the surface of the corpus calcareum. The large diameter and robustness of the centra of two examined specimens suggest that Cardabiodon was large, had a rigid vertebral column, and was a fast swimmer. The sectioned corpora calcarea show both individuals deposited 13 bands (assumed to represent annual increments) after the birth ring. The identification of the birth ring is supported in the holotype of Cardabiodon ricki as the back-calculated tooth size at age 0 is nearly equal to the size of the smallest known isolated tooth of this species. The birth ring size (5–6.6 mm radial distance [RD]) overlaps with that of Archaeolamna kopingensis (5.4 mm RD) and the range of variation of Cretoxyrhina mantelli (6–11.6 mm RD) from the Smoky Hill Chalk, Niobrara Formation. -
Bolletí De La Societat D'història Natural De Les Balears Està Integrat Pels Següents Membres, a Tots Els Quals La Junta De Publicacions Agraeix La Seva Col·Laboració
Bolletí de la Societat d’Història Natural de les Balears ISSN 0212-260X Volum 53 (2010) Palma de Mallorca BSHN (Scopoli, 1772), fotografia d’Aurora M. de Castilla Argiope bruennichi 53 Bolletí de la Societat d’Història Natural de les Balears Revista editada per la Societat d’Història Natural de les Balears amb l’esperit de contribuir a l’increment del coneixement de la naturalesa preferentment dins de l’àmbit de les Illes Balears i la Mediterrània, encara que també publica treballs originals de qualsevol àrea del món. Se publica en la modalitat d’un volum anual. Junta de Publicacions Editor: Guillem X. Pons i Buades Miquel A. Conesa i Muñoz Joan J. Fornós i Astó Lluís Gómez-Pujol Amàlia Grau i Jofre Natàlia Llorente Nosti Junta Directiva President: Antoni M. Grau i Jofre Vice-President: Francesc Gràcia i Lladó Secretari: Damià Vicens Xamena Tresorera: Maria Vidal Rigo Bibliotecari: Martí Llobera O’Brien Editor: Guillem X. Pons i Buades Vocal 1er: Antelm Ginard Fullana Vocal 2on: Francesca Mir Socies Vocal 3er: Damià Ramis i Bernad Direcció Postal i Administració del Bolletí Societat d’Història Natural de les Balears Carrer Margalida Xirgu, 16 baixos 07011 Palma de Mallorca http: //www.shnb.org E-mail: [email protected] BOLLETÍ de la SOCIETAT D’HISTÒRIA NATURAL DE LES BALEARS 53 (2010) El present bolletí ha estat editat per la Societat d’Història Natural de les Balears no ha comptat amb cap subvenció. Vol. 53 (2010) SOCIETAT D’HISTÒRIA NATURAL DE LES BALEARS Bolletí de la Societat d’Història Natural de les Balears Data de publicació: desembre 2010 Palma de Mallorca ISSN 0212-260X Depòsit legal, PM 56-1959 ISSN 0212 – 260 X Impressió: GBR produccions Gràfiques c/ Porto 4 07014 Palma Telf. -
Bibliography Database of Living/Fossil Sharks, Rays and Chimaeras (Chondrichthyes: Elasmobranchii, Holocephali) Papers of the Year 2016
www.shark-references.com Version 13.01.2017 Bibliography database of living/fossil sharks, rays and chimaeras (Chondrichthyes: Elasmobranchii, Holocephali) Papers of the year 2016 published by Jürgen Pollerspöck, Benediktinerring 34, 94569 Stephansposching, Germany and Nicolas Straube, Munich, Germany ISSN: 2195-6499 copyright by the authors 1 please inform us about missing papers: [email protected] www.shark-references.com Version 13.01.2017 Abstract: This paper contains a collection of 803 citations (no conference abstracts) on topics related to extant and extinct Chondrichthyes (sharks, rays, and chimaeras) as well as a list of Chondrichthyan species and hosted parasites newly described in 2016. The list is the result of regular queries in numerous journals, books and online publications. It provides a complete list of publication citations as well as a database report containing rearranged subsets of the list sorted by the keyword statistics, extant and extinct genera and species descriptions from the years 2000 to 2016, list of descriptions of extinct and extant species from 2016, parasitology, reproduction, distribution, diet, conservation, and taxonomy. The paper is intended to be consulted for information. In addition, we provide information on the geographic and depth distribution of newly described species, i.e. the type specimens from the year 1990- 2016 in a hot spot analysis. Please note that the content of this paper has been compiled to the best of our abilities based on current knowledge and practice, however, -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR013 Features and paleoecological significance of the shark fauna from the Upper Cretaceous Hinoshima Formation, Himenoura Group, Southwest Japan Accepted Naoshi Kitamura 4-8-7 Motoyama, Chuo-ku Kumamoto, Kumamoto 860-0821, Japan (e-mail: [email protected]) Abstract. The shark fauna of the Upper Cretaceous Hinoshima Formation (Santonian: 86.3–83.6 Ma) of the manuscriptHimenoura Group (Kamiamakusa, Kumamoto Prefecture, Kyushu, Japan) was investigated based on fossil shark teeth found at five localities: Himedo Park, Kugushima, Wadanohana, Higashiura, and Kotorigoe. A detailed geological survey and taxonomic analysis was undertaken, and the habitat, depositional environment, and associated mollusks of each locality were considered in the context of previous studies. Twenty-one species, 15 genera, 11 families, and 6 orders of fossil sharks are recognized from the localities. This assemblage is more diverse than has previously been reported for Japan, and Lamniformes and Hexanchiformes were abundant. Three categories of shark fauna are recognized: a coastal region (Himedo Park; probably a breeding site), the coast to the open sea (Kugushima and Wadanohana), and bottom-dwelling or near-seafloor fauna (Kugushima, Wadanohana, Higashiura, and Kotorigoe). -
Evolution of White and Megatooth Sharks, and Evidence for Early Predation on Seals, Sirenians, and Whales
Vol.5, No.11, 1203-1218 (2013) Natural Science http://dx.doi.org/10.4236/ns.2013.511148 Evolution of white and megatooth sharks, and evidence for early predation on seals, sirenians, and whales Cajus G. Diedrich Paleologic, Petra Bezruce 96, Zdice, Czech Republic; [email protected], www.paleologic.eu Received 6 April 2013; revised 6 May 2013; accepted 13 May 2013 Copyright © 2013 Cajus G. Diedrich. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ABSTRACT ments were generally first attributed to “white shark Carcharodon carcharias (Linné, 1758) ancestors”. Con- The early white shark Carcharodon Smith, 1838 troversy has subsequently arisen whether they should be with the fossil Carcharodon auriculatus (Blain- ascribed to the megatooth shark (“Carcharocles”—he- ville, 1818) and the extinct megatooth shark Oto- rein Otodus), or to the white shark (Carcharodon) line- dus Agassiz, 1843 with species Otodus sokolovi age [1]. This controversy is partly a result of non-sys- (Jaeckel, 1895) were both present in the Euro- tematic excavation of single serrated similar looking pean proto North Sea Basin about 47.8 - 41.3 m.y. teeth from many localities around the world, and from ago (Lutetian, early Middle Eocene), as well as in horizons of different ages. DNA studies have at least the Tethys realm around the Afican-Eurasian resolved the general position of the extant form of Car- shallow marine habitats. Both top predators deve- charodon carcharias, placing it between the Isurus and loped to be polyphyletic, with possible two dif- Lamna genera [2,3], without taking into account a revi- ferent lamnid shark ancestors within the Early sion and including of extinct fossil species such as Oto- Paleocene to Early Eocene timespan with Car- dus. -
Tooth Size Proportions Useful in Early Diagnosis
#63 Ortho-Tain, Inc. 1-800-541-6612 Tooth Size Proportions Useful In Early Diagnosis As the permanent incisors begin to erupt starting with the lower central, it becomes helpful to predict the sizes of the other upper and lower adult incisors to determine the required space necessary for straightness. Although there are variations in the mesio-distal widths of the teeth in any individual when proportions are used, the sizes of the unerupted permanent teeth can at least be fairly accurately pre-determined from the mesio-distal measurements obtained from the measurements of already erupted permanent teeth. As the mandibular permanent central breaks tissue, a mesio-distal measurement of the tooth is taken. The size of the lower adult lateral is obtained by adding 0.5 mm.. to the lower central size (see a). (a) Width of lower lateral = m-d width of lower central + 0.5 mm. The sizes of the upper incisors then become important as well. The upper permanent central is 3.25 mm.. wider than the lower central (see b). (b) Size of upper central = m-d width of lower central + 3.25 mm. The size of the upper lateral is 2.0 mm. smaller mesio-distally than the maxillary central (see c), and 1.25 mm. larger than the lower central (see d). (c) Size of upper lateral = m-d width of upper central - 2.0 mm. (d) Size of upper lateral = m-d width of lower central + 1.25 mm. The combined mesio-distal widths of the lower four adult incisors are four times the width of the mandibular central plus 1.0 mm. -
A New Plesiosaur from the Lower Jurassic of Portugal and the Early Radiation of Plesiosauroidea
A new plesiosaur from the Lower Jurassic of Portugal and the early radiation of Plesiosauroidea EDUARDO PUÉRTOLAS-PASCUAL, MIGUEL MARX, OCTÁVIO MATEUS, ANDRÉ SALEIRO, ALEXANDRA E. FERNANDES, JOÃO MARINHEIRO, CARLA TOMÁS, and SIMÃO MATEUS Puértolas-Pascual, E., Marx, M., Mateus, O., Saleiro, A., Fernandes, A.E., Marinheiro, J., Tomás, C. and Mateus, S. 2021. A new plesiosaur from the Lower Jurassic of Portugal and the early radiation of Plesiosauroidea. Acta Palaeontologica Polonica 66 (2): 369–388. A new plesiosaur partial skeleton, comprising most of the trunk and including axial, limb, and girdle bones, was collected in the lower Sinemurian (Coimbra Formation) of Praia da Concha, near São Pedro de Moel in central west Portugal. The specimen represents a new genus and species, Plesiopharos moelensis gen. et sp. nov. Phylogenetic analysis places this taxon at the base of Plesiosauroidea. Its position is based on this exclusive combination of characters: presence of a straight preaxial margin of the radius; transverse processes of mid-dorsal vertebrae horizontally oriented; ilium with sub-circular cross section of the shaft and subequal anteroposterior expansion of the dorsal blade; straight proximal end of the humerus; and ventral surface of the humerus with an anteroposteriorly long shallow groove between the epipodial facets. In addition, the new taxon has the following autapomorphies: iliac blade with less expanded, rounded and convex anterior flank; highly developed ischial facet of the ilium; apex of the neural spine of the first pectoral vertebra inclined posterodorsally with a small rounded tip. This taxon represents the most complete and the oldest plesiosaur species in the Iberian Peninsula. -
First Description of a Tooth of the Extinct Giant Shark Carcharocles
First description of a tooth of the extinct giant shark Carcharocles megalodon (Agassiz, 1835) found in the province of Seville (SW Iberian Peninsula) (Otodontidae) Primera descripción de un diente del extinto tiburón gigante Carcharocles megalodon (Agassiz, 1835) encontrado en la provincia de Sevilla (SO de la Península Ibérica) (Otodontidae) José Luis Medina-Gavilán 1, Antonio Toscano 2, Fernando Muñiz 3, Francisco Javier Delgado 4 1. Sociedad de Estudios Ambientales (SOCEAMB) − Perú 4, 41100 Coria del Río, Sevilla (Spain) − [email protected] 2. Departamento de Geodinámica y Paleontología, Facultad de Ciencias Experimentales, Universidad de Huelva − Campus El Carmen, 21071 Huelva (Spain) − [email protected] 3. Departamento de Geodinámica y Paleontología, Facultad de Ciencias Experimentales, Universidad de Huelva − Campus El Carmen, 21071 Huelva (Spain) − [email protected] 4. Usuario de BiodiversidadVirtual.org − Álvarez Quintero 13, 41220 Burguillos, Sevilla (Spain) − [email protected] ABSTRACT: Fossil remains of the extinct giant shark Carcharocles megalodon (Agassiz, 1835) are rare in interior Andalusia (Southern Spain). For the first time, a fossil tooth belonging to this paleospecies is described from material found in the province of Seville (Burguillos). KEY WORDS: Carcharocles megalodon (Agassiz, 1835), megalodon, Otodontidae, fossil, paleontology, Burguillos, Seville, Tortonian. RESUMEN: Los restos del extinto tiburón gigante Carcharocles megalodon (Agassiz, 1835) son raros en el interior de Andalucía (sur de España). Por primera vez, se describe un diente fósil de esta paleoespecie a partir de material hallado en Sevilla (Burguillos). PALABRAS CLAVE: Carcharocles megalodon (Agassiz, 1835), megalodón, Otodontidae, fósil, paleontología, Burguillos, Sevilla, Tortoniense. Introduction Carcharocles megalodon (Agassiz, 1835), the megalodon, is widely recognised as the largest shark that ever lived. -
Tulane Studies Tn Geology and Paleontology Pliocene
TULANE STUDIES TN GEOLOGY AND PALEONTOLOGY Volu me 22, Number 2 Sepl<'mber 20. l!J8~) PLIOCENE THREE-TOED HORSES FROM LOUISIANA. WITH COMMENTS ON THE CITRONELLE FORMATION EAHL M. MANNING MUSP.UM OF'GEOSCIF:NCE. LOUISJJ\NA STATE UNIVF:RSlTY. JJATO.\I ROI.JG/<. LOL'/S//\;\':1 and llRUCE J. MACFADDlrn DEJ>ARTM/<:NTOF NATUH/\LSCIENCES. F'LORJD/\ MUSf:UM Of<'NJ\TUIV\/, lllSTOUY UNIVERSITY OF FLOH!IJJ\. GJ\/NESVlU.E. Fl.OH/DA CONTENTS Page T. ABSTRACT 3.5 II INTRODUCTION :l5 Ill. ACKNOWLEDGMENTS :rn TV . ABBREVIATIONS :l7 V. SYSTEMATIC PALEONTOLOGY ;37 VI. AGE OF THE TUNICA HILLS HIPPARIONINES 38 VIL STRATIGRAPHIC PROVENIENCE 38 Vlll. PLIOCENE TERRESTRIAL VERTEBRATES OF THE GULF AND ATLANTIC COASTAL PLAIN .JO IX. COMMENTS ON THE CITRONELLE FORMATION .JI X. AGE OF THE CITRONELLE 42 XL TH E CITRONELLE FORMATION IN nm TUNICA HILLS .t:1 XII. LITERATURE CITED l.J January of 1985, the senior author was L ABSTRACT shown a large collection of late Pleistocene Teeth and metacarpals of early Pliocene (Rancholabrean land-mammal agel ver (latest Hemphillian land-mammal age) tebrate fossils from the Tunica Hills of three-toed (hipparionine) horses are de Louisiana (Fig. I) by Dr. A. Bradley scribed from the Tunica Hills of West McPherson of Centenary College, Feliciana Parish in east-central Louisiana. Shreveport. McPherson and Mr. Bill Lee An upper molar perta ins to Nannippus of Balon Rouge had collected fossils from minor, known from the Hcmphillian of that area since about 1981. Among the Central and North America, and two teeth standard assemblage of Rancholabrean and two distal metacarpals pertain to a re taxa (e.g. -
Geology of the Shepton Mallet Area (Somerset)
Geology of the Shepton Mallet area (Somerset) Integrated Geological Surveys (South) Internal Report IR/03/94 BRITISH GEOLOGICAL SURVEY INTERNAL REPORT IR/03/00 Geology of the Shepton Mallet area (Somerset) C R Bristow and D T Donovan Contributor H C Ivimey-Cook (Jurassic biostratigraphy) The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Somerset, Jurassic. Subject index Bibliographical reference BRISTOW, C R and DONOVAN, D T. 2003. Geology of the Shepton Mallet area (Somerset). British Geological Survey Internal Report, IR/03/00. 52pp. © NERC 2003 Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. 0131-667 1000 Fax 0131-668 2683 The British Geological Survey carries out the geological survey of e-mail: [email protected] Great Britain and Northern Ireland (the latter as an agency service for the government of Northern Ireland), and of the London Information Office at the Natural History Museum surrounding continental shelf, as well as its basic research (Earth Galleries), Exhibition Road, South Kensington, London projects. -
Crocodile Facts and Figures
Crocodile facts The saltwater crocodile is the largest living reptile species. It can grow up to six metres and is a serious threat to humans. Saltwater crocodiles have evolved special characteristics that make them excellent predators. • Large saltwater crocodiles can stay underwater for at least one hour because they can reduce their heart rate to 2-3 beats per minute. This means that crocodiles can wait underwater until they see prey, or if people are using the same spot regularly, the crocodile can wait underwater until someone approaches the water’s edge. • A crocodile can float with only eyes and nostrils exposed, enabling it to approach prey without being detected. • When under water, a special transparent eyelid protects the crocodile’s eye. This means that crocodiles can still see when they are completely submerged. • The tail of a crocodile is solid muscle and a major source of power, making it a strong swimmer and able to make sudden lunges out of the water to capture prey. These strong muscles also mean that for shorts bursts of time crocodiles can move faster than humans can on land. • Crocodiles have a thin layer of guanine crystals behind their retina. This intensifies images, allowing crocodiles to see better at low light levels. • Crocodiles have a ‘minimum exposure’ posture in the water, which means that only their sensory organs of eyes, cranial platform, ears and nostrils remain out of the water. This means that they often go unseen by prey, but if they are observed, the prey is often not able to tell how big the crocodile is. -
Abstractbook Vrcanscongress.Pdf
Two decades of Atlantic Neogene study V RCANS Congress Abstract Book M. Abad, T. Izquierdo, F. Ruiz (eds.) HUELVA; SEPTEMBER 24th TO 26th, 2013 ISBN: 978-84-695-8480-4 Depósito legal: H 153-2013 Cover design: Tatiana Izquierdo Cite this book: Abad, M., Izquierdo, T., Ruiz, F. (2013). Two decades of Atlantic Neogene study. V RCANS Congress abstract book. Universidad de Huelva, Huelva, Spain. 84 pp. Funding Institutions Instituto Geológico y Minero de España (IGME) Facultad de Ciencias Experimentales, Universidad de Huelva Departamento de Geodinámica y Paleontología, Universidad de Huelva Project CORE GL2010-15810. Spanish Government Two decades of Atlantic Neogene study V RCANS Congress Abstract Book ORGANIZING COMMITTEE President Francisco Ruiz Scientific Secretary Manuel Abad Technical Secretary Tatiana Izquierdo Advisors José Ángel González Delgado Ildefonso Armenteros Joaquín Rodríguez-Vidal Antonio Toscano María José Clemente-Pérez María Luz González-Regalado SCIENTIFIC COMMITTEE Manuel Abad (Spain) Paulo Legoinha (Portugal) Julio Aguirre (Spain) Pilar Mata (Spain) Sérgio P. Ávila (Portugal) Eduardo Mayoral (Spain) Abdelkhalak Ben Moussa (Morocco) Didier Merle (France) Anne-Marie Bodergat (France) João Pais (Portugal) Juan Carlos Braga (Spain) Driss Nachite (Morocco) Luis Miguel Cáceres (Spain) Fernando Pérez-Valera (Spain) Jorge Civis (Spain) Julio Rodríguez–Lázaro (Spain) Hugo Corbí (Spain) Carlos Ruiz Cánovas (Spain) Cristino Dabrio (Spain) Ana Santos (Spain) Ester Farinati (Argentina) Francisco Sierro (Spain) Clive Finlayson (Gibraltar, UK) Antonio Toscano (Spain) Edith Xio-Mara García (Mexico) Josep Tosquella (Spain) José Luis Goy (Spain) Cari Zazo (Spain) Tatiana Izquierdo (Spain) BIENVENIDA El Regional Committee on Atlantic Neogene Stratigraphy tiene como principal objetivo el estudio del Neógeno de los reinos marinos y terrestres a ambos lados del Atlántico, así como su relación con la historia de La Tierra.