Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index

Oscillations in the ratio of two principal types of secondary calcification of the test surface in Neogloboquadrina pachyderma populations closely parallel paleoclimatic oscillations over the last 6 million years in a deep-sea core drilled in the temperate South Pacific. The nature of secondary calc...

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Main Authors: Srinivasan, M. S., Kennett, J. P.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science 1974
Subjects:
Online Access:http://repository.ias.ac.in/51157/
http://www.sciencemag.org/content/186/4164/630.short
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record_format openpolar
spelling ftindianacasci:oai:repository.ias.ac.in:51157 2023-05-15T17:14:44+02:00 Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index Srinivasan, M. S. Kennett, J. P. 1974-11-15 http://repository.ias.ac.in/51157/ http://www.sciencemag.org/content/186/4164/630.short unknown American Association for the Advancement of Science Srinivasan, M. S. Kennett, J. P. (1974) Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index Science, 186 (4164). pp. 630-632. ISSN 0036-8075 QE Geology Article PeerReviewed 1974 ftindianacasci 2013-01-20T11:47:58Z Oscillations in the ratio of two principal types of secondary calcification of the test surface in Neogloboquadrina pachyderma populations closely parallel paleoclimatic oscillations over the last 6 million years in a deep-sea core drilled in the temperate South Pacific. The nature of secondary calcification in fossil planktonic foraminifera represents a useful index in interpreting Cenozoic climates. Article in Journal/Newspaper Neogloboquadrina pachyderma Planktonic foraminifera Indian Academy of Sciences: Publication of Fellows Pacific
institution Open Polar
collection Indian Academy of Sciences: Publication of Fellows
op_collection_id ftindianacasci
language unknown
topic QE Geology
spellingShingle QE Geology
Srinivasan, M. S.
Kennett, J. P.
Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index
topic_facet QE Geology
description Oscillations in the ratio of two principal types of secondary calcification of the test surface in Neogloboquadrina pachyderma populations closely parallel paleoclimatic oscillations over the last 6 million years in a deep-sea core drilled in the temperate South Pacific. The nature of secondary calcification in fossil planktonic foraminifera represents a useful index in interpreting Cenozoic climates.
format Article in Journal/Newspaper
author Srinivasan, M. S.
Kennett, J. P.
author_facet Srinivasan, M. S.
Kennett, J. P.
author_sort Srinivasan, M. S.
title Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index
title_short Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index
title_full Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index
title_fullStr Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index
title_full_unstemmed Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index
title_sort secondary calcification of the planktonic foraminifer neogloboquadrina pachyderma as a climatic index
publisher American Association for the Advancement of Science
publishDate 1974
url http://repository.ias.ac.in/51157/
http://www.sciencemag.org/content/186/4164/630.short
geographic Pacific
geographic_facet Pacific
genre Neogloboquadrina pachyderma
Planktonic foraminifera
genre_facet Neogloboquadrina pachyderma
Planktonic foraminifera
op_relation Srinivasan, M. S.
Kennett, J. P. (1974) Secondary calcification of the planktonic foraminifer Neogloboquadrina pachyderma as a climatic index Science, 186 (4164). pp. 630-632. ISSN 0036-8075
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