Oxygen isotope constraints on surface ocean temperatures
Published oxygen isotope results from benthic and planktonic foraminifera are used to constrain the extent to which surface ocean temperatures in the tropics changed between glacial and interglacial time. The possible impacts of bioturbation and of the redistribution of 18O16O ratios within the sea,...
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Elsevier
1986
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Online Access: | https://oceanrep.geomar.de/id/eprint/33105/ https://oceanrep.geomar.de/id/eprint/33105/1/broe.pdf https://doi.org/10.1016/0033-5894(86)90087-6 |
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ftoceanrep:oai:oceanrep.geomar.de:33105 2023-05-15T18:00:32+02:00 Oxygen isotope constraints on surface ocean temperatures Broecker, W. S. 1986 text https://oceanrep.geomar.de/id/eprint/33105/ https://oceanrep.geomar.de/id/eprint/33105/1/broe.pdf https://doi.org/10.1016/0033-5894(86)90087-6 en eng Elsevier https://oceanrep.geomar.de/id/eprint/33105/1/broe.pdf Broecker, W. S. (1986) Oxygen isotope constraints on surface ocean temperatures. Quaternary Research, 26 (1). pp. 121-134. DOI 10.1016/0033-5894(86)90087-6 <https://doi.org/10.1016/0033-5894%2886%2990087-6>. doi:10.1016/0033-5894(86)90087-6 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 1986 ftoceanrep https://doi.org/10.1016/0033-5894(86)90087-6 2023-04-07T15:26:04Z Published oxygen isotope results from benthic and planktonic foraminifera are used to constrain the extent to which surface ocean temperatures in the tropics changed between glacial and interglacial time. The possible impacts of bioturbation and of the redistribution of 18O16O ratios within the sea, putting aside the oxygen isotope results, are consistent with the CLIMAP project conclusion that tropical ocean temperatures remained within ±2°C of their present value. Article in Journal/Newspaper Planktonic foraminifera OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Quaternary Research 26 1 121 134 |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
Published oxygen isotope results from benthic and planktonic foraminifera are used to constrain the extent to which surface ocean temperatures in the tropics changed between glacial and interglacial time. The possible impacts of bioturbation and of the redistribution of 18O16O ratios within the sea, putting aside the oxygen isotope results, are consistent with the CLIMAP project conclusion that tropical ocean temperatures remained within ±2°C of their present value. |
format |
Article in Journal/Newspaper |
author |
Broecker, W. S. |
spellingShingle |
Broecker, W. S. Oxygen isotope constraints on surface ocean temperatures |
author_facet |
Broecker, W. S. |
author_sort |
Broecker, W. S. |
title |
Oxygen isotope constraints on surface ocean temperatures |
title_short |
Oxygen isotope constraints on surface ocean temperatures |
title_full |
Oxygen isotope constraints on surface ocean temperatures |
title_fullStr |
Oxygen isotope constraints on surface ocean temperatures |
title_full_unstemmed |
Oxygen isotope constraints on surface ocean temperatures |
title_sort |
oxygen isotope constraints on surface ocean temperatures |
publisher |
Elsevier |
publishDate |
1986 |
url |
https://oceanrep.geomar.de/id/eprint/33105/ https://oceanrep.geomar.de/id/eprint/33105/1/broe.pdf https://doi.org/10.1016/0033-5894(86)90087-6 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://oceanrep.geomar.de/id/eprint/33105/1/broe.pdf Broecker, W. S. (1986) Oxygen isotope constraints on surface ocean temperatures. Quaternary Research, 26 (1). pp. 121-134. DOI 10.1016/0033-5894(86)90087-6 <https://doi.org/10.1016/0033-5894%2886%2990087-6>. doi:10.1016/0033-5894(86)90087-6 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/0033-5894(86)90087-6 |
container_title |
Quaternary Research |
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26 |
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1 |
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121 |
op_container_end_page |
134 |
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1766169660167815168 |