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Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway

Published online by Cambridge University Press:  01 May 2009

A. R. Lord
A. R. Lord
Affiliation:
Postgraduate Unit of Micropalaeontology, Department of Geology, University College London, Gower Street, London WC1E 6BT
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Summary

Boreholes drilled at Sandnes, SW Norway penetrated Quaternary (Weichselian) marine interstadial sediments which contained ostracods. The ostracods, which are analysed and discussed, were found to be indicative of cool, probably sub-arctic, shallow-water conditions. Some evidence of faunal mixing is attributed to the effects of glacial meltwater input into a shallow marine environment.

Type
Articles
Information
Geological Magazine , Volume 117 , Issue 3 , May 1980 , pp. 227 - 242
Copyright
Copyright © Cambridge University Press 1980

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