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Sources, transport and deposition of surface sediments from the South China Sea
[Liu, Jianguo; Xiang, Rong; Chen, Zhong; Chen, Muhong; Yan, Wen; Zhang, Lanlan; Chen, Han] Chinese Acad Sci, Key Lab Marginal Sea Geol, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China; jgliu@scsio.ac.cn
2013
发表期刊DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
ISSN0967-0637
卷号71页码:92-102
摘要Sediment sources, transport and deposition in the South China Sea (SCS) are addressed based on multiple proxies of 111 surface sediment samples, including clay minerals and rare earth elements. Results reveal that sediment sources in the SCS generally contain volcanic, biogenic and terrigenous materials. Volcanic material is typically distributed west of Luzon Island (including adjacent to Huangyan Island). Carbonate biogenic materials (e.g., coral and foraminifera) develop strongly around the Nansha and Xisha Islands. Terrigenous materials mainly derive from the continent via large rivers (e.g., the Pearl, Red and Mekong Rivers) and from islands via mountainous rivers (e.g. the Gaoping River in Southwest Taiwan and Rajang River in northern Kalimantan). According to clay mineral distributions of surface sediments from the SCS, the sediment transport route is traced. It extends to the central basin and even connects with the Sulu Sea through the Mindoro Strait. Further, based on rare earth element (REE) distribution patterns of the fine-grained fraction and clay mineral assemblage of surface sediments, contributions of various sediment sources are estimated at various locations on the SCS slope. (C) 2012 Elsevier Ltd. All rights reserved.
部门归属海洋地质
关键词Sediment Provenance Sediment Transport Quantitative Analysis Surface Sediments South China Sea Clay Minerals Rare Earth Elements
学科领域Oceanography
资助者We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2). ; We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2). ; We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2). ; We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2).
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资助者We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2). ; We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2). ; We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2). ; We thank John Milliman and another anonymous reviewer for their helpful comments on this paper. We also want to thank Prof. Lei Shao for helping to improve the writing of the manuscript. We are grateful to Yang Chen for improving the English text. This work was supported by the National Key Project for Basic Research of China (2013CB956102), the National Natural Science Foundation of China (41006026, 40976031, 40631007, 40906030), Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09), the National Special Project on Basic Research of Science and Technology (2008FY110100), the State Key Program of National Natural Science of China (91128206), and the Scientific and Technology Project of Ministry and Land Resources of the PRC (GZH201100311-2).
WOS记录号WOS:000314201100009
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被引频次:25[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.scsio.ac.cn/handle/344004/11143
专题中科院边缘海地质重点实验室
通讯作者jgliu@scsio.ac.cn
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[Liu, Jianguo,Xiang, Rong,Chen, Zhong,et al. Sources, transport and deposition of surface sediments from the South China Sea[J]. DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,2013,71:92-102.
APA [Liu, Jianguo.,Xiang, Rong.,Chen, Zhong.,Chen, Muhong.,Yan, Wen.,...&jgliu@scsio.ac.cn.(2013).Sources, transport and deposition of surface sediments from the South China Sea.DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,71,92-102.
MLA [Liu, Jianguo,et al."Sources, transport and deposition of surface sediments from the South China Sea".DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS 71(2013):92-102.
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