(Table 1) Age determination in sediment core MD97-2142

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Auteurs principaux: Wei, Kuo-Yen, Chiu, Tzu-Chien, Chen, Yue-Gau
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2003
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author Wei, Kuo-Yen
Chiu, Tzu-Chien
Chen, Yue-Gau
author_facet Wei, Kuo-Yen
Chiu, Tzu-Chien
Chen, Yue-Gau
collection Datos científicos de ciencias marinas y ambientales
contents An astronomically tuned late Quaternary planktic foraminiferal delta18O record of Site MD972142 (12°41.33'N, 119°27.90'E; 1557 m water depth) in the southeastern South China Sea was established. The difference in delta18O between MD972142 and ODP792 of the Sulu Sea is regarded as a maritime proxy of the summer monsoon intensity over the South China Sea and Southeast Asia. The profile of this maritime proxy matches well with the summer monsoon index obtained from the terrestrial record of Louchuan, central Chinese Loess Plateau. The amplified planktic delta18O signals of the South China Sea relative to the Sulu Sea record are partly caused by the changing intensities of the East Asian Monsoons at the glacial-interglacial time-scale throughout the late Quaternary.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_740011
institution PANGAEA
language en
publishDate 2003
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Age determination in sediment core MD97-2142
Wei, Kuo-Yen
Chiu, Tzu-Chien
Chen, Yue-Gau
Age, comment; Age model; CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES; IMAGES III - IPHIS; International Marine Global Change Study; Marion Dufresne (1995); MD106; MD972142; MD97-2142
An astronomically tuned late Quaternary planktic foraminiferal delta18O record of Site MD972142 (12°41.33'N, 119°27.90'E; 1557 m water depth) in the southeastern South China Sea was established. The difference in delta18O between MD972142 and ODP792 of the Sulu Sea is regarded as a maritime proxy of the summer monsoon intensity over the South China Sea and Southeast Asia. The profile of this maritime proxy matches well with the summer monsoon index obtained from the terrestrial record of Louchuan, central Chinese Loess Plateau. The amplified planktic delta18O signals of the South China Sea relative to the Sulu Sea record are partly caused by the changing intensities of the East Asian Monsoons at the glacial-interglacial time-scale throughout the late Quaternary.
title (Table 1) Age determination in sediment core MD97-2142
topic Age, comment; Age model; CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES; IMAGES III - IPHIS; International Marine Global Change Study; Marion Dufresne (1995); MD106; MD972142; MD97-2142
url https://doi.org/10.1594/PANGAEA.740011