Paleontologic Technique for Defining Ancient Ocean Currents

Subtraction from the new data, of a quadratic surface fitted to the taxonomic diversity data of recent planktonic foraminifera yields a residual surface closely related to ocean current systems. This technique could be applied to fossil materials to develop knowledge of ocean circulation patterns du...

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Bibliographic Details
Published in:Science
Main Author: Stehli, F. G.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1965
Subjects:
Planktonic foraminifera
Online Access:http://dx.doi.org/10.1126/science.148.3672.943.b
https://www.science.org/doi/pdf/10.1126/science.148.3672.943.b
id craaas:10.1126/science.148.3672.943.b
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spelling craaas:10.1126/science.148.3672.943.b 2024-06-09T07:49:06+00:00 Paleontologic Technique for Defining Ancient Ocean Currents Stehli, F. G. 1965 http://dx.doi.org/10.1126/science.148.3672.943.b https://www.science.org/doi/pdf/10.1126/science.148.3672.943.b en eng American Association for the Advancement of Science (AAAS) Science volume 148, issue 3672, page 943-946 ISSN 0036-8075 1095-9203 journal-article 1965 craaas https://doi.org/10.1126/science.148.3672.943.b 2024-05-16T12:54:29Z Subtraction from the new data, of a quadratic surface fitted to the taxonomic diversity data of recent planktonic foraminifera yields a residual surface closely related to ocean current systems. This technique could be applied to fossil materials to develop knowledge of ocean circulation patterns during glacial and interglacial climatic episodes. Article in Journal/Newspaper Planktonic foraminifera AAAS Resource Center (American Association for the Advancement of Science) Science 148 3672 943 946
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Subtraction from the new data, of a quadratic surface fitted to the taxonomic diversity data of recent planktonic foraminifera yields a residual surface closely related to ocean current systems. This technique could be applied to fossil materials to develop knowledge of ocean circulation patterns during glacial and interglacial climatic episodes.
format Article in Journal/Newspaper
author Stehli, F. G.
spellingShingle Stehli, F. G.
Paleontologic Technique for Defining Ancient Ocean Currents
author_facet Stehli, F. G.
author_sort Stehli, F. G.
title Paleontologic Technique for Defining Ancient Ocean Currents
title_short Paleontologic Technique for Defining Ancient Ocean Currents
title_full Paleontologic Technique for Defining Ancient Ocean Currents
title_fullStr Paleontologic Technique for Defining Ancient Ocean Currents
title_full_unstemmed Paleontologic Technique for Defining Ancient Ocean Currents
title_sort paleontologic technique for defining ancient ocean currents
publisher American Association for the Advancement of Science (AAAS)
publishDate 1965
url http://dx.doi.org/10.1126/science.148.3672.943.b
https://www.science.org/doi/pdf/10.1126/science.148.3672.943.b
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Science
volume 148, issue 3672, page 943-946
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.148.3672.943.b
container_title Science
container_volume 148
container_issue 3672
container_start_page 943
op_container_end_page 946
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