PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
2015 | 60 | 2 |

Tytuł artykułu

A new bernissartiid crocodyliform from the Lower Cretaceous Wessex Formation (Wealden Group, Barremian) of the Isle of Wight, southern England

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
A substantially complete skull of a small crocodyliform recently found on the foreshore near Yaverland on the southeast coast of the Isle of Wight, southern England is described. The locality, mode of preservation and associated matrix indicate that it is derived from one of the plant debris beds of the Lower Cretaceous Wessex Formation (Barremian, Wealden Group). The dentition, unique among crocodyliforms, serves to confirm that the specimen is referable to the, until now, monotypic family Bernissartiidae. Apomorphies, including placement of the choana entirely within the pterygoids and disposition of cranial sutures demonstrate that the Isle of Wight skull cannot be referred to Bernissartia fagesii, known from contemporaneous strata. Furthermore, these characters indicate that the specimen should not be referred to a new species of Bernissartia. It is therefore placed in a new genus and species, Koumpiodontosuchus aprosdokiti. The systematic position of Bernissartiidae, and characters used to diagnose Eusuchia, including placement of the choana(e) within the prerygoids, are discussed. Until recently this condition was thought to be restricted to Eusuchia with all non-eusuchian neosuchian crorocdiliforms possessing choanae bounded posteriorly by the pterygoids and anteriorly by the palatines. While the choana of Koumpiodontosuchus aprosdokiti gen. et sp. nov. is entirely bounded by the pterygoids it differs from the choanae of eusuchians in lacking a median septum, being anteroposteriorly elongate and in its anterior placement.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

60

Numer

2

Opis fizyczny

p.257-268,fig.,ref.

Twórcy

Bibliografia

  • Allen, P. and Wimbledon, W.A. 1991. Correlation of NW European Purbeck- Wealden (non-marine Lower Cretaceous) as seen from the Englishtype-areas. Cretaceous Research 12: 511–526.
  • Andrade, M.B. de, Bertini, R.J., and Pinheiro, A.E.P. 2006. Observations on the palate and choanae structures in Mesoeucrocodylia (Archosauria,Crocodylomorpha): phylogenetic implications. Revista Brasileirade Paleontologia 9: 323–332.
  • Andrade, M.B. de, Edmonds, R., Benton, M.J., and Schouten, R. 2011. A new Berriasian species of Goniopholis (Mesoeucrocodylia, Neosuchia) from England, and a review of the genus. Zoological Journal of the Linnean Society 163: S66–S108.
  • Batten, D.J. (ed.). 2011. English Wealden Fossils. Palaeontological Association Field Guide to Fossils, 14. 769 pp. The Palaeontological Association,London.
  • Benton, M.J. and Clark, J.M. 1988. Archosaur phylogeny and the relationships of the Crocodilia. In: M.J. Benton (ed.), The Phylogeny andClassification of Tetrapods. 1: Amphibians, Reptiles, Birds. Systematics Association, Special Volume 35A: 295–338.
  • Brazeau, M.D. 2011. Problematic character coding methods in morphology and their effects. Biological Journal of the Linnean Society 104:489–498.
  • Brochu, C.A. 1997 Morphology, fossils, divergence timing, and the phylogenetic relationships of Gavialis. Systematic Biology 46: 479–522.
  • Brochu, C.A. 1999. Phylogenetics, taxonomy, and historical biogeography of Alligatoroidea. Journal of Vertebrate Paleontology 19 (Supplement2): 9–100.
  • Buffetaut, E. 1975. Sur l’anatomie et la position systematique de Bernissartia fagesii Dollo, L., 1883, crocodilien Wealdien de Bernissart, Belque. Bulletin de l’Institute Royal des Sciences Naturelles de Belgique, Sciences de la Terre 51 (2): 1–20.
  • Buffetaut, E. and Ford, R.L.E. 1979. The crocodilian Bernissartia in the Wealden of the Isle of Wight. Palaeontology 22: 905–912.
  • Buscalioni, A.D. and Sanz, J.L. 1990 The small crocodile Bernissartia fagesii from the Lower Cretaceous of Galve (Teruel, Spain). Bulletin del’Institut Royal des Sciences Naturelles de Belgique, Sciences de laTerre 60: 129–150.
  • Buscalioni, A.D., Buffetaut, E., and Sanz, J.L. 1984. An immature specimen of the crocodilian Bernissartia from the Lower Cretaceous of Galve (Province of Teruel, Spain). Palaeontology 27: 809–813.
  • Clark, J.M. 1994. Patterns of evolution in Mesozoic Crocodyliformes. In: N.C. Fraser and H.-D. Sues (eds.), In the Shadow of the Dinosaurs, 84–97. Cambridge University Press, New York.
  • Clark, J.M. and Norell, M.A. 1992. The Early Cretaceous crocodylomorph Hylaeochampsa vectiana from the Wealden of the Isle of Wight. American Museum Novitates 3032: 1–19.
  • Dollo, L. 1883. Premiere note sur les crocodiliens de Bernissart. Bulletin de l’Institut Royal des Sciences Naturelles de Belgique 2: 309–338.
  • Gasparini, Z., Pol. D., and Spalletti, L.A. 2006. An unusual marine crocodyliform from the Jurassic–Cretaceous boundary of Patagonia. Science311: 70–73.
  • Goloboff, P.A., Farris, J.S. and Nixon, K.C. 2008. TNT, a free program for phylogenetic analysis. Cladistics 24: 774–786.
  • Hay, O.P. 1930. Second Bibliography and Catalogue of the Fossil Vertebrata of North America. xiv + 1074 pp. Carnegie Institute, Washington DC.
  • Hughes, N.F. and McDougall, A.B. 1990. New Wealden correlation for the Wessex Basin. Proceedings of the Geologists’ Association 100: 85–90.
  • Joffe, J. 1967. The “dwarf” crocodiles of the Purbeck Formation, Dorset: a reappraisal. Palaeontology 10: 629–639.
  • Kerth, M. and Hailwood, E.A. 1988. Magnetostratigraphy of the Lower Cretaceous Vectis Formation (Wealden Group) on the Isle of Wight, southernEngland. Journal of the Geological Society, London 145: 351–360.
  • Kitching, I.J., Forey, P.L., Humphries, C.J., and Williams, D.M. 1998. Cladistics: The Theory and Practice of Parsimony Analysis. Second edition.228 pp. Oxford University Press, Oxford.
  • Norell, M.A. 1988. Cladistic Approaches to Evolution and Paleobiology as Applied to the Phylogeny of Alligatorids. 544 pp. UnpublishedPh.D. Thesis, Yale University, New Haven.
  • Norell, M.A. and Clark, J.M. 1990. A reanalysis of Bernissartia fagesii, with comments on its phylogenetic position and its bearing on theorigin and diagnosis of the Eusuchia. Bulletin de l’Institut Royal desSciences Naturelles de Belgique, Sciences de la Terre 60: 115–128.
  • Ortega, F., Gasparina, Z., Buscalioni, A., and Calvo, J.O. 2000. A new species of Araripesuchus (Crocodylomorpha, Mesoeucrocodylia) from the Lower Cretaceous of Patagonia (Argentina). Journal of Vertebrate Paleontology 20: 57–76.
  • Owen, R. 1874. Monograph of the fossil Reptilia of the Wealden and Purbeck formations. Supplement No. IV (Hylaeochampsa). Monographof the Palaeontolographical Society 27 (No. 125 for 1873): 1–7.
  • Pol, D. and Powell, J.E. 2011. A new sebecid mesoeucrocodylian from the Rio Loro Formation (Palaeocene) of north-western Argentina. ZoologicalJournal of the Linnean Society 163: S7–S36.
  • Radley, J.D. 1994. Stratigraphy, palaeontology and palaeoenvironment of the Wessex Formation (Wealden Group, Lower Cretaceous) at Yaverland,Isle of Wight, southern England. Proceedings of the Geologists’Association 105: 199–208.
  • Robinson, S.A. and Hesselbo, S.P. 2004. Fossil-wood carbon-isotope strati graphy of the non-marine Wealden Group (Lower Cretaceous, southern England). Journal of the Geological Society of London 161:133–145.
  • Salisbury, S.W., Molnar, R.E., Frey, E., and Willis, P.M.A. 2006. The origin of modern crocodyliforms: new evidence from the Cretaceous of Australia. Proceedings of the Royal Society B 273: 2439–2448.
  • Salisbury, S.W. and Naish, D. 2011. Crocodilians. In: D.J. Batten (ed.), English Wealden Fossils. Palaeontological Association Field Guideto Fossils, 14, 305–369. The Palaeontological Association, London.
  • Schwarz-Wings, D., Rees, J., and Lindgren, J. 2009. Lower Cretaceous mesoeucrocodylians from Scandinavia (Denmark and Sweden). CretaceousResearch 30: 1345–1355.
  • Seeley, H.G. 1887. On Heterosuchus valdensis, Seeley, a procoelian crocodile from from the Hastings Sand of Hastings. Quarterly Journal ofthe Geological Society 43: 212–215.
  • Sereno, P.C., Larsson, H.C.E., Sidor, C.A., and Gado, B. 2001. The giant crocodyliform Sarcosuchus from the Cretaceous of Africa. Science 294: 1516–1519.
  • Sowerby, J. de C. 1826–29. The Mineral Conchology of Great Britain; or Coloured Figures and Descriptions of Those Remains of TestaceousAnimals or Shells, Which Have Been Preserved at Various Times and Depths in the Earth. Volume 6. 230 pp. Richard Taylor, London (seriesbegin by father, J. Sowerby).
  • Sweetman, S.C. 2011a. The Wealden of the Isle of Wight. In: D.J. Batten (ed.), English Wealden Fossils. Palaeontological AssociationField Guide to Fossils, 14, 52–77. The Palaeontological Association,London.
  • Sweetman, S.C. 2011b. Vertebrate microfossils. In: D.J. Batten (ed.), English Wealden Fossils. Palaeontological Association Field Guide to Fossils, 14, 192–204. The Palaeontological Association, London.
  • Sweetman, S.C. and Insole, A.H. 2010.The plant debris beds of the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southernEngland: their genesis and palaeontological significance. Palaeogeography,Palaeoclimatology, Palaeoecology 292: 409–424.
  • Turner, A.H. and Buckley, G.A. 2008. Mahajangasuchus insignis (Crocodyliformes: Mesoeucrocodylia) cranial anatomy and new data on the origin of the eusuchian-style palate. Journal of Vertebrate Paleontology 28: 382–408.
  • Whetstone, K.N. and Whybrow, P.J. 1983. A “cursorial” crocodilian from the Triassic of Lesotho (Basutoland), southern Africa. Occasional Papers ofthe Museum of Natural History, University of Kansas 106: 1–37.
  • Wu, X.C., Sues, H.D., and Dong, Z.M. 1997. Sichuanosuchus shuhanensis, a new? Early Cretaceous protosuchian (Archosauria: Crocodyliformes)from Sichuan (China), and the monophyly of Protosuchia. Journal of Vertebrate Paleontology 17: 89–103

Uwagi

Rekord w opracowaniu

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-63a09271-7c39-467c-a665-bffbf6e61237
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.