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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Published in:Quaternary Research
Main Author: Broecker, W. S.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 1986
Subjects:
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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spelling 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
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id 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
container_volume 26
container_issue 1
container_start_page 121
op_container_end_page 134
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