Benthic and planktonic foraminifera of sediment core GIK17957-2 ...
A detailed age model for core 17957-2 of the southern South China Sea was developed based on delta18O, coarse fraction, magnetostratigraphy, and biostratigraphy for the last 1500 kyr. The delta18O record has clear ~100-kyr cycles after the Mid-Pleistocene Revolution (MPR) at the entrance of marine i...
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ftdatacite:10.1594/pangaea.736629 2024-09-09T20:04:01+00:00 Benthic and planktonic foraminifera of sediment core GIK17957-2 ... Jian, Zhimin Wang, Pinxian Chen, Min-Te Li, Bill Zhao, Q H Bühring, Christian Laj, Carlo E Lin, Hui-Ling Pflaumann, Uwe Bian, Y Wang, Rujian Cheng, Xinrong 2000 application/zip https://dx.doi.org/10.1594/pangaea.736629 https://doi.pangaea.de/10.1594/PANGAEA.736629 en eng PANGAEA https://dx.doi.org/10.1029/1999pa000431 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type SO95 Sonne Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG article Collection Supplementary Publication Series of Datasets 2000 ftdatacite https://doi.org/10.1594/pangaea.73662910.1029/1999pa000431 2024-07-03T13:16:23Z A detailed age model for core 17957-2 of the southern South China Sea was developed based on delta18O, coarse fraction, magnetostratigraphy, and biostratigraphy for the last 1500 kyr. The delta18O record has clear ~100-kyr cycles after the Mid-Pleistocene Revolution (MPR) at the entrance of marine isotopic stage (MIS) 22. Planktonic foraminifera responded to the MPR immediately, showing the increased sea surface temperature (SST) and dissolution after the MPR. Benthic foraminifera did not respond to it until the Brunhes/Matuyama boundary. Since the MPR, the depth of thermocline gradually became shallower until MISs 6-5. This major change within MISs 6-5 was also reflected in the decreased SSTs and increased productivity and Deep Water Mass. Thus two major Pleistocene paleoceanographic changes were found: One was around the MPR; the other occurred within MISs 6-5, which speculatively might be ascribed to the reorganization of surface and deep circulation, possibly induced by tectonic forces. ... : Supplement to: Jian, Zhimin; Wang, Pinxian; Chen, Min-Te; Li, Bill; Zhao, Q H; Bühring, Christian; Laj, Carlo E; Lin, Hui-Ling; Pflaumann, Uwe; Bian, Y; Wang, Rujian; Cheng, Xinrong (2000): Foraminiferal responses to major Pleistocene paleoceanographic changes in the southern South China Sea. Paleoceanography, 15(2), 229-243 ... Article in Journal/Newspaper Planktonic foraminifera DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Gravity corer Kiel type SO95 Sonne Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG |
spellingShingle |
Gravity corer Kiel type SO95 Sonne Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG Jian, Zhimin Wang, Pinxian Chen, Min-Te Li, Bill Zhao, Q H Bühring, Christian Laj, Carlo E Lin, Hui-Ling Pflaumann, Uwe Bian, Y Wang, Rujian Cheng, Xinrong Benthic and planktonic foraminifera of sediment core GIK17957-2 ... |
topic_facet |
Gravity corer Kiel type SO95 Sonne Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG |
description |
A detailed age model for core 17957-2 of the southern South China Sea was developed based on delta18O, coarse fraction, magnetostratigraphy, and biostratigraphy for the last 1500 kyr. The delta18O record has clear ~100-kyr cycles after the Mid-Pleistocene Revolution (MPR) at the entrance of marine isotopic stage (MIS) 22. Planktonic foraminifera responded to the MPR immediately, showing the increased sea surface temperature (SST) and dissolution after the MPR. Benthic foraminifera did not respond to it until the Brunhes/Matuyama boundary. Since the MPR, the depth of thermocline gradually became shallower until MISs 6-5. This major change within MISs 6-5 was also reflected in the decreased SSTs and increased productivity and Deep Water Mass. Thus two major Pleistocene paleoceanographic changes were found: One was around the MPR; the other occurred within MISs 6-5, which speculatively might be ascribed to the reorganization of surface and deep circulation, possibly induced by tectonic forces. ... : Supplement to: Jian, Zhimin; Wang, Pinxian; Chen, Min-Te; Li, Bill; Zhao, Q H; Bühring, Christian; Laj, Carlo E; Lin, Hui-Ling; Pflaumann, Uwe; Bian, Y; Wang, Rujian; Cheng, Xinrong (2000): Foraminiferal responses to major Pleistocene paleoceanographic changes in the southern South China Sea. Paleoceanography, 15(2), 229-243 ... |
format |
Article in Journal/Newspaper |
author |
Jian, Zhimin Wang, Pinxian Chen, Min-Te Li, Bill Zhao, Q H Bühring, Christian Laj, Carlo E Lin, Hui-Ling Pflaumann, Uwe Bian, Y Wang, Rujian Cheng, Xinrong |
author_facet |
Jian, Zhimin Wang, Pinxian Chen, Min-Te Li, Bill Zhao, Q H Bühring, Christian Laj, Carlo E Lin, Hui-Ling Pflaumann, Uwe Bian, Y Wang, Rujian Cheng, Xinrong |
author_sort |
Jian, Zhimin |
title |
Benthic and planktonic foraminifera of sediment core GIK17957-2 ... |
title_short |
Benthic and planktonic foraminifera of sediment core GIK17957-2 ... |
title_full |
Benthic and planktonic foraminifera of sediment core GIK17957-2 ... |
title_fullStr |
Benthic and planktonic foraminifera of sediment core GIK17957-2 ... |
title_full_unstemmed |
Benthic and planktonic foraminifera of sediment core GIK17957-2 ... |
title_sort |
benthic and planktonic foraminifera of sediment core gik17957-2 ... |
publisher |
PANGAEA |
publishDate |
2000 |
url |
https://dx.doi.org/10.1594/pangaea.736629 https://doi.pangaea.de/10.1594/PANGAEA.736629 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1029/1999pa000431 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.73662910.1029/1999pa000431 |
_version_ |
1809936036856332288 |