Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments

Foraminferal dominance values above 50 percent and associated diversity minimums in surface sediments of the North Atlantic coincide with past extremes of temperature, productivity, or salinity in overlying surface waters. These parameters delimit a cold Polar-Subpolar water mass and an impoverished...

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Published in:Science
Main Author: Ruddiman, William F.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1969
Subjects:
Online Access:http://dx.doi.org/10.1126/science.164.3884.1164
https://www.science.org/doi/pdf/10.1126/science.164.3884.1164
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spelling craaas:10.1126/science.164.3884.1164 2024-06-09T07:47:57+00:00 Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments Ruddiman, William F. 1969 http://dx.doi.org/10.1126/science.164.3884.1164 https://www.science.org/doi/pdf/10.1126/science.164.3884.1164 en eng American Association for the Advancement of Science (AAAS) Science volume 164, issue 3884, page 1164-1167 ISSN 0036-8075 1095-9203 journal-article 1969 craaas https://doi.org/10.1126/science.164.3884.1164 2024-05-16T12:55:09Z Foraminferal dominance values above 50 percent and associated diversity minimums in surface sediments of the North Atlantic coincide with past extremes of temperature, productivity, or salinity in overlying surface waters. These parameters delimit a cold Polar-Subpolar water mass and an impoverished, saline Southern Sargasso Central water mass for the late Recent. Anticipated pole-to-equator diversity and dominance gradients in the open ocean are virtually eliminated by the stronger trends of the vigorous subtropical North Atlantic gyre. Article in Journal/Newspaper North Atlantic Planktonic foraminifera AAAS Resource Center (American Association for the Advancement of Science) Science 164 3884 1164 1167
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Foraminferal dominance values above 50 percent and associated diversity minimums in surface sediments of the North Atlantic coincide with past extremes of temperature, productivity, or salinity in overlying surface waters. These parameters delimit a cold Polar-Subpolar water mass and an impoverished, saline Southern Sargasso Central water mass for the late Recent. Anticipated pole-to-equator diversity and dominance gradients in the open ocean are virtually eliminated by the stronger trends of the vigorous subtropical North Atlantic gyre.
format Article in Journal/Newspaper
author Ruddiman, William F.
spellingShingle Ruddiman, William F.
Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments
author_facet Ruddiman, William F.
author_sort Ruddiman, William F.
title Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments
title_short Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments
title_full Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments
title_fullStr Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments
title_full_unstemmed Recent Planktonic Foraminifera: Dominance and Diversity in North Atlantic Surface Sediments
title_sort recent planktonic foraminifera: dominance and diversity in north atlantic surface sediments
publisher American Association for the Advancement of Science (AAAS)
publishDate 1969
url http://dx.doi.org/10.1126/science.164.3884.1164
https://www.science.org/doi/pdf/10.1126/science.164.3884.1164
genre North Atlantic
Planktonic foraminifera
genre_facet North Atlantic
Planktonic foraminifera
op_source Science
volume 164, issue 3884, page 1164-1167
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.164.3884.1164
container_title Science
container_volume 164
container_issue 3884
container_start_page 1164
op_container_end_page 1167
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