Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes
Changing weathering intensity, sediment transport, and provenance variations over the past 22.0 lea BP have been investigated by high -resolution clay mineralogy, grain-size and stable oxygen isotopes of planktonic foraminifera records along core CG2 recovered from the continental slope of the Sunda...
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Online Access: | http://ir.qdio.ac.cn/handle/337002/112460 https://doi.org/10.1016/j.jseaes.2015.12.019 |
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/112460 2023-05-15T18:01:02+02:00 Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes Huang, Jie Jiang, Fuqing Wan, Shiming Zhang, Jin Li, Anchun Li, Tiegang 2016-03-01 http://ir.qdio.ac.cn/handle/337002/112460 https://doi.org/10.1016/j.jseaes.2015.12.019 英语 eng JOURNAL OF ASIAN EARTH SCIENCES Huang, Jie,Jiang, Fuqing,Wan, Shiming,et al. Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes[J]. JOURNAL OF ASIAN EARTH SCIENCES,2016,117(2016):317-327. http://ir.qdio.ac.cn/handle/337002/112460 doi:10.1016/j.jseaes.2015.12.019 Grain Size Clay Minerals Sea Level Changes East Asian Summer Monsoon Southern South China Sea Article 期刊论文 2016 ftchinacasciocas https://doi.org/10.1016/j.jseaes.2015.12.019 2022-06-27T05:37:26Z Changing weathering intensity, sediment transport, and provenance variations over the past 22.0 lea BP have been investigated by high -resolution clay mineralogy, grain-size and stable oxygen isotopes of planktonic foraminifera records along core CG2 recovered from the continental slope of the Sunda Shelf (southern South China Sea). Our results indicated that the reworking of older sediments outcropping on the Sunda Shelf exerted a great influence on the sediment supply during the last glacial and most of the last deglacial, modulated by sea level and monsoon rainfall changes. During the last 9.01 a BP, relative increased kaolinite and heavier delta O-18(seawater) values might reflect the higher influence of the tropical Indonesian Islands sources due to the reopen of southern straits, implying the formation of modern oceanic circulation and depositional patterns. High sediment fluxes in core CG2 during Heinrich stadial 1 might be a synthetic result of the intensified monsoon rainfall originated from the southward shift of the Intertropical Convergence Zone and the proximal location of the study core before the flooding of the Sunda Shelf. Fluctuations in smectite/(illite + chlorite) ratios correlated well with monsoon intensity, and periods of strong monsoon rainfall (lighter delta O-18(seawater) values) were associated with an intensification of erosion of pre-existing, more weathered materials on the Sunda Shelf. Finally, we concluded that sediment composition and mineralogy in the southern South China Sea slope were controlled by varying degrees of reworking on the Sunda Shelf, as well as climatically modulated sediment supply from the Mekong River and southern tropical islands over the last 22.0 ka BP. (C) 2015 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Planktonic foraminifera Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Sunda ENVELOPE(-6.982,-6.982,62.205,62.205) Journal of Asian Earth Sciences 117 317 327 |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Grain Size Clay Minerals Sea Level Changes East Asian Summer Monsoon Southern South China Sea |
spellingShingle |
Grain Size Clay Minerals Sea Level Changes East Asian Summer Monsoon Southern South China Sea Huang, Jie Jiang, Fuqing Wan, Shiming Zhang, Jin Li, Anchun Li, Tiegang Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes |
topic_facet |
Grain Size Clay Minerals Sea Level Changes East Asian Summer Monsoon Southern South China Sea |
description |
Changing weathering intensity, sediment transport, and provenance variations over the past 22.0 lea BP have been investigated by high -resolution clay mineralogy, grain-size and stable oxygen isotopes of planktonic foraminifera records along core CG2 recovered from the continental slope of the Sunda Shelf (southern South China Sea). Our results indicated that the reworking of older sediments outcropping on the Sunda Shelf exerted a great influence on the sediment supply during the last glacial and most of the last deglacial, modulated by sea level and monsoon rainfall changes. During the last 9.01 a BP, relative increased kaolinite and heavier delta O-18(seawater) values might reflect the higher influence of the tropical Indonesian Islands sources due to the reopen of southern straits, implying the formation of modern oceanic circulation and depositional patterns. High sediment fluxes in core CG2 during Heinrich stadial 1 might be a synthetic result of the intensified monsoon rainfall originated from the southward shift of the Intertropical Convergence Zone and the proximal location of the study core before the flooding of the Sunda Shelf. Fluctuations in smectite/(illite + chlorite) ratios correlated well with monsoon intensity, and periods of strong monsoon rainfall (lighter delta O-18(seawater) values) were associated with an intensification of erosion of pre-existing, more weathered materials on the Sunda Shelf. Finally, we concluded that sediment composition and mineralogy in the southern South China Sea slope were controlled by varying degrees of reworking on the Sunda Shelf, as well as climatically modulated sediment supply from the Mekong River and southern tropical islands over the last 22.0 ka BP. (C) 2015 Elsevier Ltd. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Huang, Jie Jiang, Fuqing Wan, Shiming Zhang, Jin Li, Anchun Li, Tiegang |
author_facet |
Huang, Jie Jiang, Fuqing Wan, Shiming Zhang, Jin Li, Anchun Li, Tiegang |
author_sort |
Huang, Jie |
title |
Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes |
title_short |
Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes |
title_full |
Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes |
title_fullStr |
Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes |
title_full_unstemmed |
Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes |
title_sort |
terrigenous supplies variability over the past 22,000 yr in the southern south china sea slope: relation to sea level and monsoon rainfall changes |
publishDate |
2016 |
url |
http://ir.qdio.ac.cn/handle/337002/112460 https://doi.org/10.1016/j.jseaes.2015.12.019 |
long_lat |
ENVELOPE(-6.982,-6.982,62.205,62.205) |
geographic |
Sunda |
geographic_facet |
Sunda |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
JOURNAL OF ASIAN EARTH SCIENCES Huang, Jie,Jiang, Fuqing,Wan, Shiming,et al. Terrigenous supplies variability over the past 22,000 yr in the southern South China Sea slope: Relation to sea level and monsoon rainfall changes[J]. JOURNAL OF ASIAN EARTH SCIENCES,2016,117(2016):317-327. http://ir.qdio.ac.cn/handle/337002/112460 doi:10.1016/j.jseaes.2015.12.019 |
op_doi |
https://doi.org/10.1016/j.jseaes.2015.12.019 |
container_title |
Journal of Asian Earth Sciences |
container_volume |
117 |
container_start_page |
317 |
op_container_end_page |
327 |
_version_ |
1766170354274795520 |