26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1

Composite oxygen and carbon isotopic records of planktonic and benthic foraminifers and fine-fraction (<63 µm) carbonate were used to identify major paleoceanographic events in subantarctic surface and deep waters during the past 10 Ma. The late Neogene record of the subantarctic Southern Ocean i...

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Main Authors: David A. Hodell, Daniel W. Muller, Paul F. Ciesielski, Gregory A. Mead
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Southern Ocean
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4343
http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.547.4343 2023-05-15T18:25:08+02:00 26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1 David A. Hodell Daniel W. Muller Paul F. Ciesielski Gregory A. Mead The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4343 http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4343 http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf text ftciteseerx 2016-01-08T11:21:09Z Composite oxygen and carbon isotopic records of planktonic and benthic foraminifers and fine-fraction (<63 µm) carbonate were used to identify major paleoceanographic events in subantarctic surface and deep waters during the past 10 Ma. The late Neogene record of the subantarctic Southern Ocean is marked by progressive intensification of glacial-interglacial cycles, migrations of the Polar Front Zone, and changes in deep-water circulation. The two most important times of rapid paleoceanographic change occurred during the late Miocene (between 6.4 and 4.8 Ma) and late Pliocene (especially at —2.5 Ma). Text Southern Ocean Unknown Southern Ocean
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Composite oxygen and carbon isotopic records of planktonic and benthic foraminifers and fine-fraction (<63 µm) carbonate were used to identify major paleoceanographic events in subantarctic surface and deep waters during the past 10 Ma. The late Neogene record of the subantarctic Southern Ocean is marked by progressive intensification of glacial-interglacial cycles, migrations of the Polar Front Zone, and changes in deep-water circulation. The two most important times of rapid paleoceanographic change occurred during the late Miocene (between 6.4 and 4.8 Ma) and late Pliocene (especially at —2.5 Ma).
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author David A. Hodell
Daniel W. Muller
Paul F. Ciesielski
Gregory A. Mead
spellingShingle David A. Hodell
Daniel W. Muller
Paul F. Ciesielski
Gregory A. Mead
26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1
author_facet David A. Hodell
Daniel W. Muller
Paul F. Ciesielski
Gregory A. Mead
author_sort David A. Hodell
title 26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1
title_short 26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1
title_full 26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1
title_fullStr 26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1
title_full_unstemmed 26. SYNTHESIS OF OXYGEN AND CARBON ISOTOPIC RESULTS FROM SITE 704: IMPLICATIONS FOR MAJOR CLIMATIC-GEOCHEMICAL TRANSITIONS DURING THE LATE NEOGENE1
title_sort 26. synthesis of oxygen and carbon isotopic results from site 704: implications for major climatic-geochemical transitions during the late neogene1
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4343
http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4343
http://www-odp.tamu.edu/publications/114_SR/VOLUME/CHAPTERS/sr114_26.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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