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Integrated stratigraphical study of the candidate Oxfordian Global Stratotype Section and Point (GSSP) at Redcliff Point, Weymouth, Dorset, UK

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EN
Ham Cliff near Redcliff Point, Weymouth, Dorset (SW England) exposes one of Europe's most complete Callovian-Oxfordian boundary sequences and has consequently been identified as a potential candidate GSSP for the base of the Oxfordian Stage. The boundary sequence lies within the thick mudrock facies of the Oxford Clay Formation and is abundantly fossiliferous, cardioceratid ammonites in particular being conspicuous. By convention, the stage boundary is drawn at the first occurrence of the genus Cardioceras here represented by C. redcliffense Page, Melendez and Wright at the base of the Scarburgense Subchronozone of the Mariae Chronozone. Associated Perisphinctoidea (including Peltoceras, Alligaticeras and Euaspidoceras) provide additional biostratigraphical information. Other macrofossil groups show less discernible changes, although frequent belemnites (Hibolithes) provide new highresolution carbon and strontium isotope data which are consistent with global curves and continuous sedimentation across the boundary interval. Magnetostratigraphic information is also available. Foraminiferal assemblages are dominated by epistominids but include a flood of early planktonic forms, including ?Globuligerina oxfordiana (Grigelis) immediately above the boundary. Well-preserved nannofloras are dominated by Watznaueria with conspicuous Zeugrhabdotus, podorhabdids and Stephanolithion indicating the NJ14 Biozone. Ostracoda and holothurian spicules are also recorded. These results are synthesised to provide a multidisciplinary, integrated review of the suitability of Redcliff Point for the definition of an Oxfordian GSSP. Correlations with the French candidate site in Haute-Provence are discussed and proposals made for formally establishing a GSSP for the base of the Oxfordian Stage in Europe.
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101--111
Opis fizyczny
Bibliogr. 37 poz.
Twórcy
autor
autor
autor
autor
autor
autor
autor
  • School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK, kpage@plymouth.ac.uk
Bibliografia
  • 1. Arkell W. J. 1947. The geology of the country around Weymouth, Swanage, Corfe and Lulworth. Memoir of the Geological Survey (England and Wales), 386 pp. London.
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  • 5. Callomon J. H. 1990. On the definition of the basal boundary stratotype of the Jurassic Oxfordian stage. In: G. Melendez (Ed.), 1st Oxfordian Meeting, Zaragoza 1988, Publicaciones Sepaz Paleontología, Zaragoza, 2: 119-127.
  • 6. Callomon J. H. 1993. Oxford Clay. In: J. H. Callomon, J. C. W. Cope. The Jurassic geology of Dorset, guide to excursions. Arkell International Symposium, September 1993, University College London: 41-48, London.
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  • 9. Cox B. M. and Sumbler M. G. 2002. British Middle Jurassic Stratigraphy. Geological Conservation Review Series, 26: 508 pp. Joint Nature Conservation Committee, Peterborough
  • 10. Doyle P. and Page K. N. 1991. Belemnites. In: D. M. Martill and J. D. Hudson (Eds), Fossils of the Oxford Clay. Palaeontological Association Field Guides to Fossils, 4: 144-150.
  • 11. Duff K. D. 1991. Bivalves. In: D. M. Martill and J. D. Hudson (Eds), Fossils of the Oxford Clay. Palaeontological Association Field Guides to Fossils, 4: 35-77.
  • 12. Fortwengler D. and Marchand D. 1994 a. The Thoux section: Callovian-Oxfordian boundary (Lamberti to Mariae Zone) under 'Terres Noires' facies. In: F. Atrops (Ed.), Guide book and abstracts, 4th Oxfordian and Kimmeridgian Working Groups Meeting, Lyon, France, June 1994: 103-106, Lyon.
  • 13. Fortwengler D. and Marchand D. 1994 b. Nouvelles unites biochronologiques de la zone ariae (Oxfordien inferieur). Geobios Mémoire Special, 17: 203-209.
  • 14. Fortwengler D. and Marchand D. 1997. Les coupes de Thuoux et de Savournon (SE de la France et la limite Callovien-Oxfordien). Geobios, 30: 519-540, Lyon.
  • 15. Henderson A. S., Talwar A. D. and Hart M. B. 1992. Some holothurian sclerites from the Corallian Group of North Dorset. Proceedings of the Ussher Society, 8: 11-14.
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  • 17. Hudson W., Hart M. B., Sidorczuk M. and Wierzbowski A. 2005. Jurassic planktonic foraminifera from Pieniny Klippen Belt and their taxonomic and phylogenetic importance (Carpathians, southern Poland). Tomy Jurajskie, 3: 1-10.
  • 18. Jenkyns H. C. 1996. Relative sea-level change and carbon isotopes: data from the Upper Jurassic (Oxfordian) of Central and Southern Europe: Terra Nova, 8: 75-85.
  • 19. Jenkyns H. C., Jones C. E., Grocke D. R., Hesselbo S. P. and Parkinson D. N. 2002. Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography. Journal of the Geological Society, London, 159: 351-378.
  • 20. Jones C. E., Jenkyns H. C., Coe A. L. and Hesselbo S. P. 1994. Strontium isotopic variations in Jurassic and Cretaceous seawater. Geochemica et Cosmochimica Acta, 58: 3061-3074.
  • 21. Kilenyi T. 1978. The Jurassic Part lll: Callovian to Portlandian. In: H. Bate and E. Robinson (Eds), A Stratigraphical Index of British Ostraco a, Geological Journal, Special Issue, 8: 259-298.
  • 22. Melendez G., Atrops F. and Page K. N. 2007. The cardioceratid sucession and the recognition of the Callovian-Oxfordian boundary at Savournon (SE France). 23rd Jornadas de Paleontología. Socieded Espańola de Paleontología. Caravaca, Murcia, Spain. Abstract volume (in press).
  • 23. d'Orbigny A. 1842-1849. Paleontologie fran~aise; terrains jurassiques. 1, Cephalopodes, 119 pp, Paris.
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  • 25. Page K. N. 1994. A review of the suitability of key British Callovian-Oxfordian and Oxfordian Kimmeridgian sites as Global Stratotype sections and Points (GSSPs) for stage boundaries (Abstract). In: F. Atrops (Ed.), Guide book and abstracts, 4th Oxfordian and Kimmeridgian Working Groups Meeting, Lyon, France, June 1994: 15-16, Lyon.
  • 26. Page K. N. 1995. Horizons; Intra-subzonal units in Jurassic ammonite stratigraphy. Palaeontology, 38: 801-814.
  • 27. Page K. N. 2004. The Callovian-Oxfordian boundary in Britain: A review of key sections and their correlation with the proposed Global Stratotype Section and Point for the Oxfordian in Haute Provence, France. Rivista Italiana di Paleontologia e Stratigrafia, 110: 201-208.
  • 28. Page K. N., Hart M. B. and Oxford M. J. 2003. The search for a Global Stratotype Section and Point (GSSP) for the base of the Oxfordian Stage. Geoscience in south-west England, 10: 435-441.
  • 29. Page K. N., Melendez G. and Wright J. K. 2009. The ammonite faunas of the Callovian-Oxfordian boundary interval in Europe and their relevance to the establishment of an Oxfordian GSSP. Volumina Jurassica, 7: 89-99.
  • 30. Podlaha O. G., Mutterlose J. and Veizer J. 1998. Preservation of 18O and 13C in belemnite rostra from the Jurassic/Early Cretaceous successions. American Journal of Science, 298: 324-347.
  • 31. Price G. D. and Page K. N. 2008. A carbon and oxygen isotopic analysis of molluscan faunas from the Callovian-Oxfordian boundary at Redcliff Point, Weymouth, Dorset: implications for belemnite behavior. Proceedings of the Geologists' Association, 119: 153-160.
  • 32. Remane J., Bassett M. G., Cowie J. W., Gohrbrandt K. H., Lane R. H., Michelsen O. and Naiwen W. 1996. Revised guidelines for the establishment of global chronostratigraphic standards by the International Commision on Stratigraphy (ICS). Episodes, 19: 77-81.
  • 33. Wilkinson I. P. and Whateley R. C. 2009. Upper Jurassic (Callovian-Portlandian). In: J. E. Whittaker and M. B. Hart (Eds), the Micropalaeontological Society, Special Publications, 241-287. Geological Society, London.
  • 34. Wright J. K. 1968. The stratigraphy of the Callovian rocks between Newtondale and the Scarborough Coast, Yorkshire. Proceedings of the Geologists' Association, 84: 447-457.
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  • 36. Wright J. K. 1986. The Upper Oxford Clay at Furzy Cliff, Dorset: stratigraphy, palaeoenvironment and ammonite fauna. Proceedings of the Geologists' Association, 97: 221-228.
  • 37. Wright J. K. and Cox B. M. 2001. British Upper Jurassic Stratigraphy: Oxfordian to Kimmeridgian. Geological Conservation Review Series, 21: 266 pp. Joint Nature Conservation Committee, Peterborough.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0064-0011
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