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Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope
Huang, Jie1,2; Li, Anchun1; Wan, Shiming1; Huang, J (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2011-05-01
发表期刊QUATERNARY RESEARCH
ISSN0033-5894
卷号75期号:3页码:734-744
文章类型Article
摘要Changes in paleoenvironments over the last 17,500 yr have been documented by a high-resolution clay mineralogy and grain-size records of Core KNG5 from the northern slope of the South China Sea. Our results indicate that clay minerals are mainly from the Pearl River from 17,500 to 12,500 cal yr BP, and the South China Sea modern current system began to form since 12,500 cal yr BP, as a result, Taiwan turns to be the major contributor of clay minerals after 12,500 cal yr BP. Two grain-size populations with high variability through time were identified in the 13-28 mu m and 1-2.2 mu m grain-size intervals. The 1-2.2 mu m grain-size population are mainly controlled by provenance supply and current transport. The 13-28 mu m grain-size fraction could be controlled mainly by the sea-level change. The 1-2.2 mu m grain-size population record demonstrates that East Asian Summer Monsoon intensity generally follows changes in insolation and that the response is similar for a large area of China and other northern low-latitude records, implying the globality of the monsoon evolution since Holocene. The anomalous environmental conditions in the northern South China Sea may imply intensified ENSO activity during the late Holocene. (C) 2011 University of Washington. Published by Elsevier Inc. All rights reserved.; Changes in paleoenvironments over the last 17,500 yr have been documented by a high-resolution clay mineralogy and grain-size records of Core KNG5 from the northern slope of the South China Sea. Our results indicate that clay minerals are mainly from the Pearl River from 17,500 to 12,500 cal yr BP, and the South China Sea modern current system began to form since 12,500 cal yr BP, as a result, Taiwan turns to be the major contributor of clay minerals after 12,500 cal yr BP. Two grain-size populations with high variability through time were identified in the 13-28 mu m and 1-2.2 mu m grain-size intervals. The 1-2.2 mu m grain-size population are mainly controlled by provenance supply and current transport. The 13-28 mu m grain-size fraction could be controlled mainly by the sea-level change. The 1-2.2 mu m grain-size population record demonstrates that East Asian Summer Monsoon intensity generally follows changes in insolation and that the response is similar for a large area of China and other northern low-latitude records, implying the globality of the monsoon evolution since Holocene. The anomalous environmental conditions in the northern South China Sea may imply intensified ENSO activity during the late Holocene. (C) 2011 University of Washington. Published by Elsevier Inc. All rights reserved.
关键词Clay Mineral Grain Size South China Sea Sea Level Changes Current Transport East Asian Summer Monsoon
学科领域Physical Geography ; Geology
DOI10.1016/j.yqres.2011.03.002
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收录类别SCI
语种英语
WOS记录号WOS:000290831500034
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被引频次:55[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/11537
专题海洋地质与环境重点实验室
通讯作者Huang, J (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
第一作者单位中国科学院海洋研究所
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Huang, Jie,Li, Anchun,Wan, Shiming,et al. Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope[J]. QUATERNARY RESEARCH,2011,75(3):734-744.
APA Huang, Jie,Li, Anchun,Wan, Shiming,&Huang, J .(2011).Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope.QUATERNARY RESEARCH,75(3),734-744.
MLA Huang, Jie,et al."Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope".QUATERNARY RESEARCH 75.3(2011):734-744.
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