SCSIO OpenIR  > 中科院边缘海地质重点实验室
Influence of the Kuroshio Current intrusion on Holocene environmental transformation in the South China Sea
[Liu, Jianguo; Xiang, Rong; Chen, Muhong; Yan, Wen; Chen, Zhong; Liu, Fang] Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China; [Li, Tiegang] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Guangzhou 510301, Guangdong, Peoples R China; jgliu@scsio.ac.cn
2013
发表期刊HOLOCENE
ISSN0959-6836
卷号23期号:6页码:850-859
摘要Numerous studies have been conducted on the evolutionary history of the Kuroshio Current (KC) and other extensions. However, the history of the KC intrusion into the South China Sea (SCS) through the Luzon Strait has been little studied. Here we trace the Holocene developmental history of the KC intrusion and its impact on environmental transformation in the northern SCS. This study involved a comprehensive analysis of planktonic foraminifera, clay minerals and geochemical elements of core 05E306 sediments from the northeastern SCS. AMS C-14 dates indicated that the sedimentation rate at the core site was most rapid (>1000 cm/ka) before similar to 6.0 ka, relatively rapid (similar to 65 cm/ka) between 6.0 and 4.6 ka and slow (similar to 24 cm/ka) since 4.6 ka. The Pulleniatina minimum event (PME) occurred between 4.6 and 2.7 ka, together with high percentages of Neogloboquadrina dutertrei and Globorotalia menardii. Planktonic foraminifera indicated that the KC intrusion experienced three significant changes at 6.0, 4.6 and 2.7 ka in turn. Depositional environments, including input of terrigenous materials and development of biogenic materials, similarly underwent three important transformations at 6.0, 4.1 and 3.0 ka, respectively. Abrupt changes in sedimentary records at the study core are contemporary with records from the tropical Pacific during the Holocene. This indicates that development of the KC intrusion and its impact on depositional environments in the SCS can be correlated with tropical factors from the low-latitude oceans.
部门归属海洋地质
关键词Depositional Environment El Nino/southern Oscillation (Enso) Holocene Kuroshio Current Pulleniatina Minimum Event (Pme) South China Sea
学科领域Geography, Physical ; Geosciences, Multidisciplinary
资助者This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09). ; This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09). ; This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09). ; This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09).
URL查看原文
语种英语
资助者This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09). ; This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09). ; This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09). ; This study was jointly funded by the Basic Research Project of State Oceanic Administration People's Republic of China (2013CB956102), National Nature Science Foundation of China (40976028), the Knowledge Innovation Program of the Chinese Academy of Sciences (SQ201201), the State Key Program of National Natural Science of China (91128206, 91228207), the National Special Project on Basic Research of Science and Technology (2008FY110100) and the Open Fund of the Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences (MSGL12-09).
WOS记录号WOS:000319228000008
引用统计
被引频次:6[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/344004/11130
专题中科院边缘海地质重点实验室
通讯作者jgliu@scsio.ac.cn
推荐引用方式
GB/T 7714
[Liu, Jianguo,Xiang, Rong,Chen, Muhong,et al. Influence of the Kuroshio Current intrusion on Holocene environmental transformation in the South China Sea[J]. HOLOCENE,2013,23(6):850-859.
APA [Liu, Jianguo.,Xiang, Rong.,Chen, Muhong.,Yan, Wen.,Chen, Zhong.,...&jgliu@scsio.ac.cn.(2013).Influence of the Kuroshio Current intrusion on Holocene environmental transformation in the South China Sea.HOLOCENE,23(6),850-859.
MLA [Liu, Jianguo,et al."Influence of the Kuroshio Current intrusion on Holocene environmental transformation in the South China Sea".HOLOCENE 23.6(2013):850-859.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。