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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. -
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). -
Phylogenetic Analysis of the Allometry of Metabolic Rate and Mitochondrial Basal Proton Leak
Author’s Accepted Manuscript Phylogenetic analysis of the allometry of metabolic rate and mitochondrial basal proton leak Elias T. Polymeropoulos, R. Oelkrug, C.R. White, M. Jastroch www.elsevier.com/locate/jtherbio PII: S0306-4565(16)30294-7 DOI: http://dx.doi.org/10.1016/j.jtherbio.2017.01.013 Reference: TB1878 To appear in: Journal of Thermal Biology Received date: 28 September 2016 Revised date: 24 January 2017 Accepted date: 25 January 2017 Cite this article as: Elias T. Polymeropoulos, R. Oelkrug, C.R. White and M. Jastroch, Phylogenetic analysis of the allometry of metabolic rate and mitochondrial basal proton leak, Journal of Thermal Biology, http://dx.doi.org/10.1016/j.jtherbio.2017.01.013 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting galley proof before it is published in its final citable form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Phylogenetic analysis of the allometry of metabolic rate and mitochondrial basal proton leak 1 2 3 4,5 Polymeropoulos Elias T. , Oelkrug R. , White C.R. , Jastroch M. 1Menzies Institute for Medical Research, University of Tasmania, 7001 Hobart, Australia, 2Center of Brain, Behaviour and Metabolism, University of Lübeck, 23562 Lübeck, Germany, 3Centre for Geometric Biology, School of Biological Sciences, Monash University, 3800 Melbourne, Australia 4Institute for Diabetes and Obesity, Helmholtz Zentrum, 85764 Munich, Germany, 5 Department of Animal Physiology, Faculty of Biology, Philipps University of Marburg, D-35032 Marburg, Germany Abstract The mitochondrial basal proton leak (MBPL) significantly contributes to high body temperatures (Tb) and basal metabolic rates (BMR) in endotherms. -
Short Communication a Remarkable Case of a Shark
Journal of Vertebrate Paleontology 30(2):592–597, March 2010 © 2010 by the Society of Vertebrate Paleontology SHORT COMMUNICATION A REMARKABLE CASE OF A SHARK-BITTEN ELASMOSAURID PLESIOSAUR ∗ KENSHU SHIMADA, ,1,2 TAKANOBU TSUIHIJI,3 TAMAKI SATO,4 and YOSHIKAZU HASEGAWA5; 1Environmental Science Program and Department of Biological Sciences, DePaul University, 2325 North Clifton Avenue, Chicago, Illinois 60614, U.S.A., [email protected]; 2Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601, U.S.A.; 3National Museum of Nature and Science, 3-23-1 Hyakuhin-cho, Shinjuku-ku, Tokyo 169-0073, Japan, [email protected]; 4Department of Astronomy and Earth Sciences, Tokyo Gakugei University, 4-1-1 Nukui-Kita-Machi, Koganei City, Tokyo 184-8501, Japan, [email protected]; 5Gunma Museum of Natural History, 1674-1 Kamikuroiwa, Tomimoka, Gunma 370-2345, Japan, [email protected] Futabasaurus suzukii Sato, Hasegawa, and Manabe, 2006, is an is embedded near the anterodorsal corner of the right humerus elasmosaurid plesiosaur from the Upper Cretaceous in central immediately distal to its tuberosity (Fig. 3A). The labial face of Japan. The holotype and the only known specimen of this taxon Tooth 85 faces the posterior side of the right humerus, suggest- is a partial skeleton (Fig. 1), which co-occurred with “several tens ing that the shark bit the forelimb from its anterior side. Two of shark teeth” (Sato et al., 2006:468). The shark teeth were pre- teeth, Teeth 83 and 84, are embedded in the posterodorsal cor- viously identified as those of ‘Odontaspis sp.’ (e.g., Obata et al., ner of the neural spine of “Vertebra #34,” a posterior cervical 1970), but we re-identified them as an extinct lamniform shark, vertebra (Fig. -
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. -
Upper Cretaceous Chondrichthyes Teeth Record in Phosphorites of the Loma Gorda Formation•
BOLETIN DE CIENCIAS DE LA TIERRA http://www.revistas.unal.edu.co/index.php/rbct Upper Cretaceous chondrichthyes teeth record in phosphorites of the • Loma Gorda formation Alejandro Niño-Garcia, Juan Diego Parra-Mosquera & Peter Anthony Macias-Villarraga Departamento de Geociencias, Facultad de Ciencias Naturales y Exactas, Universidad de Caldas, Manizales, Colombia. [email protected], [email protected], [email protected] Received: April 26th, 2019. Received in revised form: May 17th, 2019. Accepted: June 04th, 2019. Abstract In layers of phosphorites and gray calcareous mudstones of the Loma Gorda Formation, in the vicinity of the municipal seat of Yaguará in Huila department, Colombia, were found fossils teeth of chondrichthyes, these were extracted from the rocks by mechanical means, to be compared with the species in the bibliography in order to indentify them. The species were: Ptychodus mortoni (order Hybodontiformes), were found, Squalicorax falcatus and Cretodus crassidens (order Lamniformes). This finding constitutes the first record of these species in the Colombian territory; which allows to extend its paleogeographic distribution to the northern region of South America, which until now was limited to Africa, Europe, Asia and North America, except for the Ptychodus mortoni that has been described before in Venezuela. Keywords: first record; sharks; upper Cretaceous; fossil teeth; Colombia. Registro de dientes de condrictios del Cretácico Superior en fosforitas de la formación Loma Gorda Resumen En capas de fosforitas y lodolitas calcáreas grises de la Formación Loma Gorda, en cercanías de la cabecera municipal de Yaguará en el departamento del Huila, Colombia, se encontraron dientes fósiles de condrictios; estos fueron extraídos de la roca por medios mecánicos, para ser comparados con las especies encontradas en la bibliografía e identificarlos. -
Dinosaur Metabolism and the Allometry of Maximum Growth Rate
RESEARCH ARTICLE Dinosaur Metabolism and the Allometry of Maximum Growth Rate Nathan P. Myhrvold* Intellectual Ventures, Bellevue, Washington, United States of America * [email protected] Abstract a11111 The allometry of maximum somatic growth rate has been used in prior studies to classify the metabolic state of both extant vertebrates and dinosaurs. The most recent such studies are reviewed, and their data is reanalyzed. The results of allometric regressions on growth rate are shown to depend on the choice of independent variable; the typical choice used in prior studies introduces a geometric shear transformation that exaggerates the statistical OPEN ACCESS power of the regressions. The maximum growth rates of extant groups are found to have a Citation: Myhrvold NP (2016) Dinosaur great deal of overlap, including between groups with endothermic and ectothermic metabo- Metabolism and the Allometry of Maximum lism. Dinosaur growth rates show similar overlap, matching the rates found for mammals, Growth Rate. PLoS ONE 11(11): e0163205. reptiles and fish. The allometric scaling of growth rate with mass is found to have curvature doi:10.1371/journal.pone.0163205 (on a log-log scale) for many groups, contradicting the prevailing view that growth rate Editor: Anthony Fiorillo, Perot Museum of Nature allometry follows a simple power law. Reanalysis shows that no correlation between growth and Science, UNITED STATES rate and basal metabolic rate (BMR) has been demonstrated. These findings drive a con- Received: January 7, 2015 clusion that growth rate allometry studies to date cannot be used to determine dinosaur Accepted: September 6, 2016 metabolism as has been previously argued. -
Mosasaurs Continuing from Last Time…
Pliosaurs and Mosasaurs Continuing From Last Time… • Pliosauridae: the big marine predators of the Jurassic Pliosauridae • Some of the largest marine predators of all time, these middle Jurassic sauropterygians include such giants as Kronosaurus, Liopleurodon, Macroplata, Peloneustes, Pliosaurus, and Brachauchenius Pliosaur Mophology • While the number of cervical vertebrae is less than in plesiosaurs, there is still variation: Macroplata (29) vs. Kronosaurus (13) Pliosaur Morphology • Larger pliosaurs adopted a more streamlined body shape, like modern whales, with a large skull and compact neck, and generally the hind limbs were larger than the front, while plesiosaurs had larger forelimbs Pliosaur Morphology • Powerful limb girdles and large (banana sized) conical teeth helped pliosaurs eat larger, quicker prey than the piscivorous plesiosaurs Liopleurodon • NOT 25 m long in general (average of 40 feet), though perhaps certain individuals could reach that size, making Liopleurodon ferox the largest carnivore to ever live • Recent skull studies indicate that Liopleurodon could sample water in stereo through nostrils, locating scents much as we locate sound Cretaceous Seas • Breakup of Gondwana causes large undersea mountain chains to form, raising sea levels everywhere • Shallow seas encourage growth of corals, which increases calcium abundance and chalk formation • Warm seas and a gentle thermal gradient yield a hospitable environment to rays, sharks, teleosts, and the first radiation of siliceous diatoms Kronosaurus • Early Cretaceous -
Dr. Kenshu Shimada: Peer-Reviewed Published Articles [Last Updated 04/26/2019]
Dr. Kenshu Shimada: Peer-Reviewed Published Articles [last updated 04/26/2019] [* = undergraduate student; ** = graduate student] 2019 [105] Shimada, K. In press. A new species and biology of the Late Cretaceous 'blunt-snouted' bony fish, Thryptodus (Actinopterygii: Tselfatiiformes), from the United States. Cretaceous Research. [104] Cronin, T. J.*, and K. Shimada . In press. New anatomical information on the Late Cretaceous bony fish, Micropycnodon kansasensis (Actinopterygii: Pycnodontiformes), from the Niobrara Chalk of western Kansas, U.S.A. Transactions of Kansas Academy of Science. [103] Pimiento, C., J. L. Cantalapiedra, K. Shimada , D. J. Field, and J. B. Smaers. 2019. Evolutionary pathways towards shark gigantism. Evolution, 73(3):588–599. 2018 [102] Johnson-Ransom, E. D.*, E. V. Popov, T. A. Deméré, and K. Shimada. 2018. The Late Cretaceous chimaeroid fish, Ischyodus bifurcatus Case (Chondrichthyes: Holocephali), from California, USA, and its paleobiogeographical significance. Paleontological Research, 2(4):364-372. [101] Guinot, G., S. Adnet, K. Shimada , C. J. Underwood, M. Siversson, D. J. Ward, J. Kriwet, and H. Cappetta. 2018. On the need of providing tooth morphology in descriptions of extant elasmobranch species. Zootaxa, 4461(1):118–126. [100] Jacobs, P. K.*, and K. Shimada . 2018. Ontogenetic growth pattern of the extant smalltooth sandtiger shark, Odontaspis ferox (Lamniformes: Odontaspididae)— application from and to paleontology. Journal of Fossil Research, 51(1):23–29. [99] Guzzo, F.*, and K. Shimada . 2018. A new fossil vertebrate locality of the Jetmore Chalk Member of the Upper Cretaceous Greenhorn Limestone in north-central Kansas, U.S.A. Transactions of the Kansas Academy of Science, 121(1-2):59-68. -
Teacher Resource For: Evidence for Mesothermy in Dinosaurs
Teacher Resource for: Evidence for mesothermy in dinosaurs Table of Contents: I. Student Learning Goals II. Connect to Learning Standards III. Summary of the Article for the Teacher IV. Discussion Questions V. Related Multimedia Resources from HHMI|BioInteractive NOTE: To explore mass extinctions, including the end of the dinosaurs, we recommend HHMI's free eBook Mass Extinctions: Lessons from the Past. Student Learning Goals Connections to the nature of science from the article Were dinosaurs slow-metabolizing ectotherms like reptiles or fast-metabolizing endotherms like mammals and birds whose activities were unconstrained by temperature? How can the resting metabolic rate of extinct species be determined using fossils? The importance of this scientific research This research furthers the understanding of how dinosaurs regulated their body temperature in comparison to known ectotherms and endotherms. It determines the resting metabolic rate of dinosaurs using maximum growth rate as measured by bone growth rings. The actual science involved Thermodynamics Paleontology Connect to Learning Standards: The Next Generation Science Standards Science and Engineering Practice 2: Developing and using models Science and Engineering Practice 6: Constructing explanations (for science) and designing solutions (for engineering) The AP Biology Standards Essential knowledge 1.A.4: Biological evolution is supported by scientific evidence from many disciplines, including mathematics. Essential knowledge 2.A.1: All living systems require constant input of free energy. Essential knowledge 2.C.2: Organisms respond to changes in their external environments. Essential knowledge 2.D.2: Homeostatic mechanisms reflect both common ancestry and divergence due to adaptation in different environments. Common Core English Language Arts 11.12.8: Evaluate the hypotheses, data, analyses, and conclusions in a science or technical test, verifying the data when possible and corroborating or challenging conclusions with other sources of information. -
Caudal Fin Skeleton of the Late Cretaceous Lamniform Shark, Cretoxyrhina Mantelli, from the Niobrara Chalk of Kansas
Lucas, S. G. and Sullivan, R.M., eds., 2006, Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin 35. 185 CAUDAL FIN SKELETON OF THE LATE CRETACEOUS LAMNIFORM SHARK, CRETOXYRHINA MANTELLI, FROM THE NIOBRARA CHALK OF KANSAS KENSHU SHIMADA1, STEPHEN L. CUMBAA2, AND DEANNE VAN ROOYEN3 1Environmental Science Program and Department of Biological Sciences, DePaul University, 2325 North Clifton Avenue, Chicago, Illinois 60614; and Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601; 2Paleobiology, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada; 3Department of Earth Sciences, Carleton University, 2240 Herzberg Laboratories, 1125 Colonel By Drive, Ottawa, Ontario K1S 5B6, Canada. Abstract—The caudal fin morphology of the Late Cretaceous lamniform shark, Cretoxyrhina mantelli (Agassiz), was previously inferred from scale morphology, which suggested that it was capable of fast swimming. A specimen from the Niobrara Chalk of western Kansas is described here and offers new insights into the morphology of the caudal fin of the taxon. The specimen preserves the posterior half of the vertebral column and a series of hypochordal rays. These skeletal elements exhibit features suggesting that C. mantelli had a lunate tail and a caudal peduncle with a lateral fluke. The specimen also supports the idea that the body form of C. mantelli resembled that of the extant white shark, Carcharodon carcharias (Linneaus). Given a total vertebral count in Cretoxyrhina mantelli of about 230, this specimen suggests that the transition between precaudal and caudal vertebrae was somewhere between the 140th and 160th vertebrae. -
The Paleoenvironments of Azhdarchid Pterosaurs Localities in the Late Cretaceous of Kazakhstan
A peer-reviewed open-access journal ZooKeys 483:The 59–80 paleoenvironments (2015) of azhdarchid pterosaurs localities in the Late Cretaceous... 59 doi: 10.3897/zookeys.483.9058 RESEARCH ARTICLE http://zookeys.pensoft.net Launched to accelerate biodiversity research The paleoenvironments of azhdarchid pterosaurs localities in the Late Cretaceous of Kazakhstan Alexander Averianov1,2, Gareth Dyke3,4, Igor Danilov5, Pavel Skutschas6 1 Zoological Institute of the Russian Academy of Sciences, Universitetskaya nab. 1, 199034 Saint Petersburg, Russia 2 Department of Sedimentary Geology, Geological Faculty, Saint Petersburg State University, 16 liniya VO 29, 199178 Saint Petersburg, Russia 3 Ocean and Earth Science, National Oceanography Centre, Sou- thampton, University of Southampton, Southampton SO14 3ZH, UK 4 MTA-DE Lendület Behavioural Ecology Research Group, Department of Evolutionary Zoology and Human Biology, University of Debrecen, 4032 Debrecen, Egyetem tér 1, Hungary 5 Zoological Institute of the Russian Academy of Sciences, Universi- tetskaya nab. 1, 199034 Saint Petersburg, Russia 6 Department of Vertebrate Zoology, Biological Faculty, Saint Petersburg State University, Universitetskaya nab. 7/9, 199034 Saint Petersburg, Russia Corresponding author: Alexander Averianov ([email protected]) Academic editor: Hans-Dieter Sues | Received 3 December 2014 | Accepted 30 January 2015 | Published 20 February 2015 http://zoobank.org/C4AC8D70-1BC3-4928-8ABA-DD6B51DABA29 Citation: Averianov A, Dyke G, Danilov I, Skutschas P (2015) The paleoenvironments of azhdarchid pterosaurs localities in the Late Cretaceous of Kazakhstan. ZooKeys 483: 59–80. doi: 10.3897/zookeys.483.9058 Abstract Five pterosaur localities are currently known from the Late Cretaceous in the northeastern Aral Sea region of Kazakhstan. Of these, one is Turonian-Coniacian in age, the Zhirkindek Formation (Tyulkili), and four are Santonian in age, all from the early Campanian Bostobe Formation (Baibishe, Akkurgan, Buroinak, and Shakh Shakh).