Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
- 1 May 1980
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 117 (3), 227-242
- https://doi.org/10.1017/s0016756800030454
Abstract
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.Keywords
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