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

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 mi...

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Bibliographic Details
Published in:Geological Magazine
Main Author: Lord, A. R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Geology
Arctic
Norway
Sandnes
Online Access:http://dx.doi.org/10.1017/s0016756800030454
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030454
id crcambridgeupr:10.1017/s0016756800030454
record_format openpolar
spelling crcambridgeupr:10.1017/s0016756800030454 2024-03-03T08:41:35+00:00 Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway Lord, A. R. 1980 http://dx.doi.org/10.1017/s0016756800030454 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030454 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 117, issue 3, page 227-242 ISSN 0016-7568 1469-5081 Geology journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0016756800030454 2024-02-08T08:46:17Z 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. Article in Journal/Newspaper Arctic Cambridge University Press Arctic Norway Sandnes ENVELOPE(15.092,15.092,67.235,67.235) Geological Magazine 117 3 227 242
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Lord, A. R.
Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
topic_facet Geology
description 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.
format Article in Journal/Newspaper
author Lord, A. R.
author_facet Lord, A. R.
author_sort Lord, A. R.
title Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
title_short Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
title_full Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
title_fullStr Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
title_full_unstemmed Weichselian (Late Quaternary) ostracods from the Sandnes Clay, Norway
title_sort weichselian (late quaternary) ostracods from the sandnes clay, norway
publisher Cambridge University Press (CUP)
publishDate 1980
url http://dx.doi.org/10.1017/s0016756800030454
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030454
long_lat ENVELOPE(15.092,15.092,67.235,67.235)
geographic Arctic
Norway
Sandnes
geographic_facet Arctic
Norway
Sandnes
genre Arctic
genre_facet Arctic
op_source Geological Magazine
volume 117, issue 3, page 227-242
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800030454
container_title Geological Magazine
container_volume 117
container_issue 3
container_start_page 227
op_container_end_page 242
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