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Tytuł artykułu

A new species of extinct bullhead sharks, Paracestracion viohli sp. nov. (Neoselachii, Heterodontiformes), from the Upper Jurassic of South Germany

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Konferencja
Evolution and Diversity of Chondrichthyans (2008 ; Warszawa)
Języki publikacji
EN
Abstrakty
EN
The early history of heterodontid sharks is documented mainly by isolated teeth. So far, three different heterodontid genera have been recorded from the Jurassic: Proheterodontus from the Middle Jurassic of England (and probably Upper Jurassic of France), Paracestracion from the Early to Late Jurassic of England, Belgium and S. Germany, and Heterodontus from the Upper Jurassic of South Germany. Paracestracion is known by isolated teeth in the Early and Middle Jurassic and by articulated skeletons in the Late Jurassic. Recently discovered skeletal remains from the upper Kimmeridgian locality of Schamhaupten, S. Germany, represent a new, hitherto unknown extinct species of Paracestracion, P. viohli sp. nov., which documents further taxonomic diversity of early heterodontids. This new taxon is represented by a subadult individual as indicated by the absence of molariform lateral teeth; it shares with other species of Paracestracion the characteristic holaulacorize cuspidate teeth. It differs from all other species in having ornamented lingual crown faces. Teeth of Proheterodontus differ in a different tooth root vascularisation. Proheterodontus and Paracestracion vanished before or at the Jurassic/Cretaceous boundary with Heterodontus becoming progressively more diverse in the Cretaceous and Cenozoic.
Rocznik
Strony
235--241
Opis fizyczny
Bibliogr. 23 poz.,
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autor
Bibliografia
  • BERG, L.S. 1940. Classification of fishes, both recent and fossil. Transactions of the Institute of Zoology, Academy of Sciences USSR, 5, 85-517.
  • BONAPARTE C.L.J.L. 1832-38. Selachorum tabula analytica. Nuovi Annali delle Scienze Naturali, 1, 195-214.
  • COMPAGNO L.J.V. 1977. Phyletic relationships of living sharks and rays. American Zoologist, 17, 303-322.
  • COMPAGNO L.J.V. 1999. Checklist of Living Elasmobranchs. In: HAMLETT, W.C. (Ed.), Sharks, Skates, and Rays – The Biology of Elasmobranch Fishes, pp. 471-498. Johns Hopkins University Press; Baltimore and London.
  • DAVIES, D.H., LAWSON, R., BURCH, S.J. & HANSON, J.E. 1987. Evolutionary relationships of a “primitive” shark (Heterodontus) assessed by micro-complement fixation of serum transferring. Journal of Molecular Evolution, 25, 74-80.
  • EASTMAN, C.R. 1914. Catalog of the fossil fishes in the Carnegie Museum, Part IV. Memoires of the Carnegie Museum, 6, 389-449.
  • GRAY J.E. 1851. List of specimens of fish in the collection of the British Museum, Part. I; pp. 1-160. British Museum (Natural History); London.
  • HAY, O.P. 1902. Bibliography and catalogue of the fossil Vertebrata of North America. United States Geological Survey, Bulletin, 179, 1-868.
  • HUXLEY J.T. 1880. On the application of the laws of evolution to the arrangement of Vertebrata and more particularly of the Mammalia. Proceedings of the Zoological Society of London, 1880, 649-662.
  • KOKEN, E. 1911. Pisces. In: ZITTEL, K.A. (Ed.), Grundzüge der Paläontologie. Zweite Abteilung, Vertebrata, pp. 1-142. Oldenbourg; München–Berlin.
  • KRIWET, J. & KLUG, S. 2004. Late Jurassic selachians (Chondrichthyes, Elasmobranchii) from southern Germany: Re-evaluation on taxonomy and diversity. Zitteliana, A 44, 67-95.
  • KRIWET, J. & KLUG, S. 2008. Diversity and biogeography pattern of Late Jurassic neoselachians (Chondrichthyes, Elasmobranchii). In: CALIN, L., LONGBOTTOM, A. & RICHTER, M. (Eds), Fishes and the break-up of Pangea. Geological Society of London, Special Publication, 295, 55-69.
  • MAISEY, J.G. 1982. Fossil Hornshark Finspines (Elasmobranchii; Heterodontidae) with Notes on a New Species (Heterodontus tuberculatus). Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, 164, 393-413.
  • MAISEY, J.G., NAYLOR, G.J.P. & WARD, D.J. 2004.Mesozoic elasmobranches, neoselachian phylogeny and the rise of modern elasmobranch diversity. In: ARRATIA, G. & TINTORI, (Eds), Mesozoic Fishes 3 – Systematics, Paleoenvironments and Biodiversity, pp. 17-56. Dr. Friedrich Pfeil; Munich.
  • MUSICK, J. A., HARBIN, M.M. & COMPAGNO, L.J.V. 2004. Historical zoogeography of the Selachii. In: CARRIER, J.C.,MUSICK, J.A. & HEITHAUS, M.R. (Eds), Biology of sharks and their relatives, pp. 33-78. CRC Press; Boca Raton, Florida.
  • SCHWEIZER, R. 1964. Elasmobranchier und Holocephalen aus den Nusplinger Plattenkalken. Palaeontographica, A123, 58-110.
  • SUMMERS, A.P., KETCHAM, R.A. & ROWE, T. 2004. Structure and Function of the Horn Shark (Heterodontus francisci) Cranium Through Ontogeny: Development of an Hard Prey Specialist. Journal of Morphology, 260, 1-12.
  • THIES, D. 1983. Jurazeitliche Neoselachier aus Deutschland und S-England (Jurassic Neoselachians from Germany and S-England). Courier Forschungsinstitut Senckenberg, 58, 1-116.
  • UNDERWOOD, C. J. 2002. Sharks, rays and a chimaeroid from the Kimmeridgian (Late Jurassic) of Ringstead, Southern England. Palaeontology, 45, 297-325.
  • UNDERWOOD, C. J. 2006. Diversification of the Neoselachii (Chondrichthyes) during the Jurassic and Cretaceous. Paleobiology, 32, 215-235.
  • UNDERWOOD, C.J. & WARD, D.J. 2004. Neoselachian Sharks and Rays from the British Bathonian (Middle Jurassic). Palaeontology, 47, 447-501.
  • WAGNER, J.A. 1857. Charakteristik neuer Arten von Knorpelfischen aus den lithographischen Schiefern der Umgegend von Solnhofen. Gelehrter Anzeiger der Bayerischen Akademie der Wissenschaften, 44, 288-293.
  • WOODWARD, A.S. 1889. Catalogue of the fossil Fishes in the British Museum. Part I; pp. 1-474. British Museum, (Natural History); London.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-2216-8656
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