Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda

Seasonal variations in the oxygen-18/oxygen-16 ratio of calcite shells of living planktonic foraminifera in the Sargasso Sea off Bermuda are a direct function of surface water temperature. Seasonal occurrence as well as depth habitat are determining factors in the oxygen isotopic composition of plan...

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Published in:Science
Main Authors: Williams, Douglas F., Bé, Allan W. H., Fairbanks, Richard G.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1979
Subjects:
Online Access:http://dx.doi.org/10.1126/science.206.4417.447
https://www.science.org/doi/pdf/10.1126/science.206.4417.447
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spelling craaas:10.1126/science.206.4417.447 2024-06-09T07:49:04+00:00 Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda Williams, Douglas F. Bé, Allan W. H. Fairbanks, Richard G. 1979 http://dx.doi.org/10.1126/science.206.4417.447 https://www.science.org/doi/pdf/10.1126/science.206.4417.447 en eng American Association for the Advancement of Science (AAAS) Science volume 206, issue 4417, page 447-449 ISSN 0036-8075 1095-9203 journal-article 1979 craaas https://doi.org/10.1126/science.206.4417.447 2024-05-16T12:55:09Z Seasonal variations in the oxygen-18/oxygen-16 ratio of calcite shells of living planktonic foraminifera in the Sargasso Sea off Bermuda are a direct function of surface water temperature. Seasonal occurrence as well as depth habitat are determining factors in the oxygen isotopic composition of planktonic foraminifera. These relationships may be used to determine the seasonal temperature contrast of oceans in the past. Article in Journal/Newspaper Planktonic foraminifera AAAS Resource Center (American Association for the Advancement of Science) Science 206 4417 447 449
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Seasonal variations in the oxygen-18/oxygen-16 ratio of calcite shells of living planktonic foraminifera in the Sargasso Sea off Bermuda are a direct function of surface water temperature. Seasonal occurrence as well as depth habitat are determining factors in the oxygen isotopic composition of planktonic foraminifera. These relationships may be used to determine the seasonal temperature contrast of oceans in the past.
format Article in Journal/Newspaper
author Williams, Douglas F.
Bé, Allan W. H.
Fairbanks, Richard G.
spellingShingle Williams, Douglas F.
Bé, Allan W. H.
Fairbanks, Richard G.
Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda
author_facet Williams, Douglas F.
Bé, Allan W. H.
Fairbanks, Richard G.
author_sort Williams, Douglas F.
title Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda
title_short Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda
title_full Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda
title_fullStr Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda
title_full_unstemmed Seasonal Oxygen Isotopic Variations in Living Planktonic Foraminifera off Bermuda
title_sort seasonal oxygen isotopic variations in living planktonic foraminifera off bermuda
publisher American Association for the Advancement of Science (AAAS)
publishDate 1979
url http://dx.doi.org/10.1126/science.206.4417.447
https://www.science.org/doi/pdf/10.1126/science.206.4417.447
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Science
volume 206, issue 4417, page 447-449
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.206.4417.447
container_title Science
container_volume 206
container_issue 4417
container_start_page 447
op_container_end_page 449
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