High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea
High-resolution carbonate stratigraphy of the deep-sea core MD972151 from the southwestern South China Sea shows millennial-scale variability similar to oxygen isotopic fluctuations recorded in ice cores from Greenland. In a long term of glacial-interglacial scale, carbonate contents in the intergla...
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Chinese Geoscience Union
1999
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fttriple:oai:gotriple.eu:10670/1.ql0ool 2023-05-15T16:28:37+02:00 High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea Huang, Cy Wang, Cc Zhao, Mx 1999-01-01 https://archimer.ifremer.fr/doc/00239/35073/34557.pdf https://archimer.ifremer.fr/doc/00239/35073/ en eng Chinese Geoscience Union 10670/1.ql0ool https://archimer.ifremer.fr/doc/00239/35073/34557.pdf https://archimer.ifremer.fr/doc/00239/35073/ other Archimer, archive institutionnelle de l'Ifremer Terrestrial Atmospheric And Oceanic Sciences (1017-0839) (Chinese Geoscience Union), 1999-03 , Vol. 10 , N. 1 , P. 225-238 envir geo Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ 1999 fttriple 2023-01-22T17:19:32Z High-resolution carbonate stratigraphy of the deep-sea core MD972151 from the southwestern South China Sea shows millennial-scale variability similar to oxygen isotopic fluctuations recorded in ice cores from Greenland. In a long term of glacial-interglacial scale, carbonate contents in the interglacial time (up to 25 % by weight) were higher than that in the glacial periods (5-15 % by weight). Even for the last glacial, carbonate contents are relatively high in the interstadial events and low in the stadial horizons. This demonstrates clearly that carbonate content in the continental slope above the lysocline in the southwestern South China Sea is primarily controlled by dilution of terrigenous inputs, which in turn is due to sea-level fluctuations in response to changes of ice volume in high latitude regions. Text Greenland Unknown Greenland |
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envir geo Huang, Cy Wang, Cc Zhao, Mx High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea |
topic_facet |
envir geo |
description |
High-resolution carbonate stratigraphy of the deep-sea core MD972151 from the southwestern South China Sea shows millennial-scale variability similar to oxygen isotopic fluctuations recorded in ice cores from Greenland. In a long term of glacial-interglacial scale, carbonate contents in the interglacial time (up to 25 % by weight) were higher than that in the glacial periods (5-15 % by weight). Even for the last glacial, carbonate contents are relatively high in the interstadial events and low in the stadial horizons. This demonstrates clearly that carbonate content in the continental slope above the lysocline in the southwestern South China Sea is primarily controlled by dilution of terrigenous inputs, which in turn is due to sea-level fluctuations in response to changes of ice volume in high latitude regions. |
format |
Text |
author |
Huang, Cy Wang, Cc Zhao, Mx |
author_facet |
Huang, Cy Wang, Cc Zhao, Mx |
author_sort |
Huang, Cy |
title |
High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea |
title_short |
High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea |
title_full |
High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea |
title_fullStr |
High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea |
title_full_unstemmed |
High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea |
title_sort |
high-resolution carbonate stratigraphy of images core md972151 from south china sea |
publisher |
Chinese Geoscience Union |
publishDate |
1999 |
url |
https://archimer.ifremer.fr/doc/00239/35073/34557.pdf https://archimer.ifremer.fr/doc/00239/35073/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
Archimer, archive institutionnelle de l'Ifremer Terrestrial Atmospheric And Oceanic Sciences (1017-0839) (Chinese Geoscience Union), 1999-03 , Vol. 10 , N. 1 , P. 225-238 |
op_relation |
10670/1.ql0ool https://archimer.ifremer.fr/doc/00239/35073/34557.pdf https://archimer.ifremer.fr/doc/00239/35073/ |
op_rights |
other |
_version_ |
1766018286585118720 |