Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11
Oxygen-18 analyses of pelagic and benthic foraminifera from core K 11 indicate that during the last glaciation Norwegian Sea bottom waters were warmer than in modern times and had the same physical parameters (temperature, oxygen isotope ratio, and salinity) as the North Atlantic deep water. This re...
Published in: | Science |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
1975
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1126/science.188.4194.1208 https://www.science.org/doi/pdf/10.1126/science.188.4194.1208 |
id |
craaas:10.1126/science.188.4194.1208 |
---|---|
record_format |
openpolar |
spelling |
craaas:10.1126/science.188.4194.1208 2024-06-09T07:47:56+00:00 Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 Duplessy, Jean Claude Chenouard, Lydie Vila, Françoise 1975 http://dx.doi.org/10.1126/science.188.4194.1208 https://www.science.org/doi/pdf/10.1126/science.188.4194.1208 en eng American Association for the Advancement of Science (AAAS) Science volume 188, issue 4194, page 1208-1209 ISSN 0036-8075 1095-9203 journal-article 1975 craaas https://doi.org/10.1126/science.188.4194.1208 2024-05-16T12:54:46Z Oxygen-18 analyses of pelagic and benthic foraminifera from core K 11 indicate that during the last glaciation Norwegian Sea bottom waters were warmer than in modern times and had the same physical parameters (temperature, oxygen isotope ratio, and salinity) as the North Atlantic deep water. This result indicates that the glacial Norwegian Sea was not a sink for dense surface water, as it is now, and that during glacial times North Atlantic deep water invaded the deep Norwegian basin. Article in Journal/Newspaper North Atlantic Deep Water North Atlantic Norwegian Sea AAAS Resource Center (American Association for the Advancement of Science) Norwegian Sea Science 188 4194 1208 1209 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Oxygen-18 analyses of pelagic and benthic foraminifera from core K 11 indicate that during the last glaciation Norwegian Sea bottom waters were warmer than in modern times and had the same physical parameters (temperature, oxygen isotope ratio, and salinity) as the North Atlantic deep water. This result indicates that the glacial Norwegian Sea was not a sink for dense surface water, as it is now, and that during glacial times North Atlantic deep water invaded the deep Norwegian basin. |
format |
Article in Journal/Newspaper |
author |
Duplessy, Jean Claude Chenouard, Lydie Vila, Françoise |
spellingShingle |
Duplessy, Jean Claude Chenouard, Lydie Vila, Françoise Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 |
author_facet |
Duplessy, Jean Claude Chenouard, Lydie Vila, Françoise |
author_sort |
Duplessy, Jean Claude |
title |
Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 |
title_short |
Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 |
title_full |
Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 |
title_fullStr |
Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 |
title_full_unstemmed |
Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11 |
title_sort |
weyl's theory of glaciation supported by isotopic study of norwegian core k 11 |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1975 |
url |
http://dx.doi.org/10.1126/science.188.4194.1208 https://www.science.org/doi/pdf/10.1126/science.188.4194.1208 |
geographic |
Norwegian Sea |
geographic_facet |
Norwegian Sea |
genre |
North Atlantic Deep Water North Atlantic Norwegian Sea |
genre_facet |
North Atlantic Deep Water North Atlantic Norwegian Sea |
op_source |
Science volume 188, issue 4194, page 1208-1209 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.188.4194.1208 |
container_title |
Science |
container_volume |
188 |
container_issue |
4194 |
container_start_page |
1208 |
op_container_end_page |
1209 |
_version_ |
1801379415775510528 |