Yuan, Zineng; Xiao, Xiaotong; Wang, Fei; Xing, Lei; Wang, Zicheng; Zhang, Hailong; Xiang, Rong; Zhou, Liping; Zhao, Meixun
发表期刊QUATERNARY INTERNATIONAL
ISSN1040-6182
2018-07-20
卷号482页码:46-55
关键词HoloceneOcean circulationTemperature structureU-37(K ')TEX86East China Sea
研究领域Physical Geography; Geology
DOI10.1016/j.quaint.2018.04.025
产权排序[Yuan, Zineng; Xiao, Xiaotong; Wang, Fei; Xing, Lei; Wang, Zicheng; Zhang, Hailong; Zhao, Meixun] Ocean Univ China, Key Lab Marine Chem Theory & Technol, Minist Educ, Qingdao 266100, Peoples R China; [Xiao, Xiaotong; Xing, Lei; Wang, Zicheng; Zhang, Hailong; Zhou, Liping; Zhao, Meixun] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266061, Peoples R China; [Yuan, Zineng] Chinese Acad Sci, Shandong Prov Key Lab Coastal Zone Environm Proc, Key Lab Coastal Zone Environm Proc & Ecol Remedia, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China; [Xiang, Rong] Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China; [Zhou, Liping] Peking Univ, Lab Earth Surface Proc, Dept Geog, Beijing 100871, Peoples R China; [Zhou, Liping] Peking Univ, Ocean Res Inst, Beijing 100871, Peoples R China
作者部门海岸带环境过程实验室
英文摘要The Holocene environment evolution in the East China Sea (ECS) is characterized by the gradual establishment and strengthening of its shelf circulation system, but knowledge about temperature responses in temporal and spatial scales is limited due to the lack of continuous high-resolution records. Here, we compare U-37(K') and TEX86 temperature records for three cores from the ECS shelf, which provide the temporal and spatial patterns of Holocene temperature structure variations. These temperature records revealed broadly consistent temporal trends with three intervals characterized by two distinct shifts. During the early Holocene (10.0-6.0 ka), the modern-type circulation system was not established, which resulted in strong water column stratification; and the higher sea surface temperature (SST) might be associated with the Holocene Thermal Maximum (HTM). The interval of 6.0 to 1.0/2.0 ka displayed a weaker stratification caused by the intrusion of the Yellow Sea Warm Current (YSWC) and the initiation of the circulation system. A decreasing SST trend was related to the formation of the cold eddy generated by the circulation system in the ECS. During 1.0/2.0 to 0 ka, temperatures were characterized by much weaker stratification and an abrupt decrease of SST caused by the enhanced circulation system and stronger cold eddy, respectively. Thus, the temperature structure in the shelf of ECS was closely related with circulation system changes during the mid-late Holocene, which was most likely driven by the intrusion of Kuroshio Current (KC). The significant asynchrony of temperature decreases in the three locations during the late Holocene was likely caused by the gradual expansion of the ECS cold eddy area.
文章类型Article
资助机构National Key Research and Development Program of China [2016YFA0601403]; National Natural Science Foundation of China [41641048, 4130966]; "111" Project [B13030]
收录类别SCI
语种英语
关键词[WOS]SOUTHERN YELLOW SEA; ISOPRENOID TETRAETHER LIPIDS; LAST 15,000 YEARS; PALEOENVIRONMENTAL CHANGES; OKINAWA TROUGH; WINTER MONSOON; KUROSHIO CURRENT; HIGH-RESOLUTION; NORTH-ATLANTIC; CLIMATE-CHANGE
研究领域[WOS]Geography, Physical; Geosciences, Multidisciplinary
WOS记录号WOS:000434685000004
引用统计被引频次：15[WOS][WOS记录][WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cnhttp://ir.yic.ac.cn/handle/133337/24434
专题中科院海岸带环境过程与生态修复重点实验室_海岸带环境过程实验室
作者单位1.Ocean Univ China, Key Lab Marine Chem Theory & Technol, Minist Educ, Qingdao 266100, Peoples R China;
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266061, Peoples R China;
3.Chinese Acad Sci, Shandong Prov Key Lab Coastal Zone Environm Proc, Key Lab Coastal Zone Environm Proc & Ecol Remedia, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China;
4.Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China;
5.Peking Univ, Lab Earth Surface Proc, Dept Geog, Beijing 100871, Peoples R China;
6.Peking Univ, Ocean Res Inst, Beijing 100871, Peoples R China
推荐引用方式
GB/T 7714Yuan, Zineng,Xiao, Xiaotong,Wang, Fei,et al. Spatiotemporal temperature variations in the East China Sea shelf during the Holocene in response to surface circulation evolution[J]. QUATERNARY INTERNATIONAL,2018,482:46-55.
APAYuan, Zineng.,Xiao, Xiaotong.,Wang, Fei.,Xing, Lei.,Wang, Zicheng.,...&Zhao, Meixun.(2018).Spatiotemporal temperature variations in the East China Sea shelf during the Holocene in response to surface circulation evolution.QUATERNARY INTERNATIONAL,482,46-55.
MLAYuan, Zineng,et al."Spatiotemporal temperature variations in the East China Sea shelf during the Holocene in response to surface circulation evolution".QUATERNARY INTERNATIONAL 482(2018):46-55.
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