Hostname: page-component-78c5997874-lj6df Total loading time: 0 Render date: 2024-11-03T19:30:48.205Z Has data issue: false hasContentIssue false

Late Pleistocene deposits and Mollusca from Portland, Dorset

Published online by Cambridge University Press:  01 May 2009

D. H. Keen
Affiliation:
Department of Geography, Coventry (Lanchester) Polytechnic, Priory Street, Coventry CV1 5FB, U.K.

Abstract

The stratigraphy and fauna of terrestrial deposits at Portland Bill is described. The fauna is restricted to the head and is indicative of a cool climate rather than the temperate conditions suggested by earlier authors. An age in the Devensian Glacial Stage is tentatively suggested.

Type
Articles
Copyright
Copyright © Cambridge University Press 1985

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Arkell, W. J. 1947. The geology of the country around Weymouth, Swanage, Corfe and Lulworth. Memoir of the Geological Survey of Great Britain.Google Scholar
Bullen, R. A. 1900. Shells from the Portland Rubble Drift. Geological Magazine 7, 286–7.Google Scholar
Coope, G. R., Jones, R. L. & Keen, D. H. 1980. The palaeoecology and age of peat at Fliquet Bay, Jersey, Channel Islands. Journal of Biogeography 7, 187–95.CrossRefGoogle Scholar
Coope, G. R., Jones, R. L., Keen, D. H. & Waton, P. V. (in press). The flora and fauna of late Pleistocene deposits at St. Aubin, Jersey. Proceedings of the Geologists' Association.Google Scholar
Davies, K. H. & Keen, D. H. (in press), The age of Pleistocene marine deposits at Portland, Dorset. Proceedings of the Geologists' Association.Google Scholar
Ellis, A. E. 1962. British Freshwater Bivalve Molluscs. Linnean Society Synopses of the British Fauna, No. 13.Google Scholar
Holyoak, D. T. 1982. Non-marine Mollusca of the last glacial period (Devensian) in Britain. Malacologia 22, 727–30.Google Scholar
Kerney, M. P. 1963. Late-glacial deposits on the chalk of South-East England. Philosophical Transactions of the Royal Society B 246, 203–54.Google Scholar
Kerney, M. P. 1977. British Quaternary non-marine Mollusca: a brief review. In British Quarternary Studies – Recent advances (ed. Shotton, F. W.), pp. 3242. Oxford: Clarendon.Google Scholar
Kerney, M. P. & Cameron, R. A. D. 1979. A Field Guide to the Land Snails of Britain and North-west Europe. London: Collins.Google Scholar
Prestwich, J. 1875. Notes on the phenomena of the Quaternary period in the Isle of Portland and around Weymouth. Quarterly Journal of the Geological Society of London 31, 2954.CrossRefGoogle Scholar
Pugh, M. E. & Shearman, D. J. 1967. Cryoturbation structures at the south end of the Isle of Portland. Proceedings of the Geologists' Association 78, 463–71.CrossRefGoogle Scholar
Williams, R. B. G. 1975. The British climate during the last glaciation; an interpretation based on periglacial phenomena. In Ice Ages: Ancient and Modern (ed. Wright, A. E. and Moseley, F.), pp. 95120. Liverpool: Seel House.Google Scholar