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High resolution ammonite stratigraphy of the Charmouth Mudstone Formation (Lower Jurassic: Sinemurian-Lower Pliensbachian) in south-west England, UK

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The "Lower Lias" mudrocks of the Charmouth Mudstone Formation inWest Dorset coast are world famous for their ammonite faunas, which range from mid Lower Sinemurian (Semicostatum Chronozone) to Lower Pliensbachian (topmost Davoei Chronozone) in age. The succession includes significant non-sequences, however, and as certain other intervals yield only crushed and relatively poorly preserved material, much of the sequence of ammonite faunas of this interval in south-west England has remained poorly understood. Inland, however, although it has been realised for many years that some of the missing horizons reappear, the Formation is very poorly exposed and as a consequence little has been known about its detailed stratigraphy and palaeontology. The systematic recording over 40 years by Mr H.C. Prudden (Montacute) of temporary excavations in East Somerset (around 20 km north of the Dorset coast), combined with material collected by others from similar exposures has now, however, revealed a virtually complete sequence of ammonite faunas through the interval represented by the Formation including from many of the which are missing on the Dorset coast. In particular, only one subchronozone remains to be conclusively proven in the region, the terminal Sinemurian, Aplanatum Subchronozone (Raricostatum Chronozone). This faunal succession is correlated with that on the coast to provide a detailed synthesis of the sequence of ammonite biohorizons in the region, which is correlated with a contemporary Standard Zonation and high-resolution biohorizonal/ zonule scheme for interval in North-West Europe. The significance for regional and international correlations of the Lower Lias is also discussed.
Czasopismo
Rocznik
Strony
19--29
Opis fizyczny
Bibliogr. 35 poz.
Twórcy
autor
  • School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK, kpage@plymouth.ac.uk
Bibliografia
  • 1. Bristow C. R. and Westhead R. K. 1993. Geology of the Evercreech-Batcombe district (Somerset). British Geological Survey Technical Report, WA/93/89.
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  • 3. Callomon J. H. 1985. The evolution of the Jurassic ammonite family Cardioceratidae. Special Papers in Palaeontology, 33: 49-90.
  • 4. Callomon J. H. and Chandler R. B. 1990. A review of the ammonite horizons of the Aalenian-Lower Bajocian stages in the Middle Jurassic of southern England. Memoire Descitiva della Carta Geologica Italiana, 40: 85-112.
  • 5. Cox B. M., Sumbler M. G. and Ivimey-Cook H. C. 1998. A formational framework for the Lower Jurassic of England and Wales (onshore area). British Geological Survey Research Report, RR/99/01.
  • 6. Dean W. T., Donovan D. T. and Howarth M. K. 1961. The Liassic ammonite zones of the North-West European Province. Bulletin of the British Museum of Natural History, Geology Series, 4: 435-505.
  • 7. Dommergues J. -L., Meister C. and Mouterde R. 1997. Pliensbachien. In: E. Cariou, and P.
  • 8. Donovan D. T. 1989. Geology of a gas pipeline from Ilchester (Somerset) to Pucklechurch (Avon), 1985. Proceedings of the Somerset Archaeological and Natural History Society, 132: 297-317.
  • 9. Donovan D. T. and Kellaway G. A. 1984. Geology of the Bristol District: the Lower Jurassic rocks. Memoir of the British Geological Survey, Special Sheet.
  • 10. Getty T. A. 1980. Hettangian-Sinemurian correlation chart. In: Cope J. C. W., Getty T. A.,
  • 11. Hesselbo S. P. and Jenkyns H. C. 1995. A comparison of Hettangian to Bajocian successions of Dorset and Yorkshire. In: P. D. Taylor (Ed.): Field geology of the British Jurassic, 105-150. London: Geological Society.
  • 12. Hollingworth N. T. J., Ward D. J., Simms M. J. and Clothier P. 1990. A temporary exposure of Lower Lias, Late Sinemurian at Dimmer Camp, Castle Cary, Somerset, England. Mesozoic Research, 2: 163-180.
  • 13. Jenkyns H. C., Jones C. E., Grocke D. R., Hesselbo S. P. and Parkinson D. D. 2002. Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeooceanography. Journal of Geological Society of London, 159: 351-378.
  • 14. Kellaway G. A. and Wilson V. 1941. An outline of the geology of Yeovil, Sherborne and Sparkford Vale. Proceedings of the Geologists' Association, 52: 131-174.
  • 15. Lang W. D. 1914. The geology of the Charmouth cliffs, beach and foreshore. Proceedings of the Geologists' Association (London), 25: 293-360.
  • 16. Lang W. D. 1928. The Belemnite Marls of Charmouth, a series in the Lias of the Dorset Coast. Quarterly Journal of the Geological Society of London, 84: 179-257.
  • 17. Lang W. D. 1932. The Lower Lias of the Vale of Marshwood. Proceedings of the Geologists' Association, 43: 97-126.
  • 18. Lang W. D. and Spath L. F. 1926. The Black Marl of Black Ven and Stonebarrow, in the Lias of the Dorset coast. Quarterly Journal of the Geological Society of London, 82: 144-187.
  • 19. Lang W. D., Spath L. F. and Richardson W. A. 1923. Shales with "Beef", a sequence in the Lower Lias of the Dorset coast. Quarterly Journal of the Geological Society of London, 79: 47-99.
  • 20. Page K. N. 1992. The sequence of ammonite correlated horizons in the British Sinemurian (Lower Jurassic). Newsletters on Stratigraphy, 27: 129-156.
  • 21. Page K. N. 1994. On the sequence of ammonite correlated chronostratigraphical horizons in the British Sinemurian (Lower Jurassic). In: Proceedings of the 3rd International Symposiumon Jurassic Stratigraphy, Poitiers 1991. Geobios, Mém. Spécial, 17, 1: 369-379.
  • 22. Page K. N. 1995. Biohorizons and zonules: intrasubzonal units in Jurassic ammonite stratigraphy. Palaeontology, 38: 801-811.
  • 23. Page K. N. 2002. A review of the ammonite faunas and Standard Zonation of the Hettangian and Lower Sinemurian succession (Lower Jurassic) of the East Devon Coast (South West England Geoscience in south-west England, 10: 293-303.
  • 24. Page K. N. 2003. The Lower Jurassic of Europe - its subdivision and correlation. In: K. Dybkjaer, J. Ineson and F. Surlyk (Eds). The Jurassic of Denmark and Greenland. Geological Survey of Denmark and Greenland Bulletin, 1: 23-60.
  • 25. Palmer C. P. 1972. The Lower Lias (Lower Jurassic) between Watchet and Lilstock in North Somerset, United Kingdom. Newsletters on Stratigraphy, 2: 1-30.
  • 26. Phelps M. C. 1985. A refined ammonite biostratigraphy for the Middle and Upper Carixian (Ibex and Davoei zones, Lower Jurassic) in north west Europe and stratigraphical details of the Carixian-Domerian boundary. Geobios, 18: 321-367.
  • 27. Simms M. J., Chidlaw J., Morton N. and Page K. N. 2004. British Lower Jurassic Stratigraphy Geological Conservation Review Volume, 30: 458 pp.
  • 28. Sowerby J. 1812-1922. The Mineral Conchology of Great Britain, 1-3. London.
  • 29. Sowerby J. de C. 1823-1946. The Mineral Conchology of Great Britain, 4-7. London.
  • 30. Spath L. F. 1938. A catalogue of the ammonites of the Liassic family Liparoceratidae in the British Museum (Natural History), 191 pp. London: Trustees of the British Museum.
  • 31. Ussher W. A. E. 1906. The geology of the country between Wellington and Chard. Memoir of the Geological Survey of England and Wales, Explanation of Sheet 311.
  • 32. Whittaker A. and Green G. W. 1984. Geology of the country around Weston-Super-Mare. Memoirs of the Geological Survey of Great Britain, 147 pp.
  • 33. Wilson V., Welch F. B. A., Robbie J. A. and Green G. W. 1958. Geology of the country between Bridport and Yeovil. Memoir of the Geological Survey of Great Britain, Sheet 312 and 327 (England and Wales), 239 pp.
  • 34. Woodward H. B. 1893. The Jurassic rocks of Britain. 3. The Lias of England and Wales (Yorkshire excepted). Memoir of the Geological Survey, 399 pp.
  • 35. Woodward H. B. 1905. Notes on the railway cuttings between Castle Cary and Langport in Somerset. Summary of the progress of the Geological Survey of the United Kingdom and Museum of Practical Geology for 1904: HMSO., London, 163-171.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0064-0003
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