Asian monsoon and oceanic circulation paced sedimentary evolution over the past 1,500 years in the central mud area of the Bohai Sea, China

doi:10.1002/gj.3758

IEECAS OpenIR > 现代环境研究室

	Asian monsoon and oceanic circulation paced sedimentary evolution over the past 1,500 years in the central mud area of the Bohai Sea, China
	Lyu, Wenzhe 1,2; Yang, Jichao 3; Fu, Tengfei 2; Chen, Yanping 4; Hu, Zhangxi 5,6; Tang, Ying Zhong 5,6; Lan, Jianghu7 ; Chen, Guangquan 2; Su, Qiao 2; Xu, Xingyong 2; Chen, Shenliang 1
通讯作者	Lyu, Wenzhe(lvwenzhe1992@gmail.com) ; Yang, Jichao(yangjichao.1@163.com) ; Fu, Tengfei(futengfei@fio.org.cn)
	2020-02-05
发表期刊	GEOLOGICAL JOURNAL
ISSN	0072-1050
页码	13
摘要	Mud areas within China's marginal seas record critical information about historic environmental changes, which may have contributed to palaeoenvironmental processes and to understand their driving mechanisms. In this study, we investigated the sedimentary characteristics of a gravity core from the Bohai Sea central mud areas, to reveal the interactions between oceanic and climatic changes over the past 15 centuries. Sedimentary and mineral records indicated that the depositional environment and sediment sources were relatively stable, in which the East Asian Summer Monsoon (EASM) and Yellow Sea Warm Current (YSWC) variability can be derived. Based on these results, we found that the winter Arctic Oscillation (wAO) was negatively correlated with the coupled EASM and YSWC changes, namely, a negative (positive) relationship between EASM and YSWC during a positive (negative) wAO. We therefore suggest that over the past 15 centuries, Arctic winter climates may have modulated palaeoenvironmental changes over East Asia continental shelves, via teleconnections with the El Nino-Southern Oscillation (ENSO) and the Kuroshio Current.
关键词	Arctic Oscillation Bohai Sea continental mud area East Asian Summer Monsoon (EASM) sedimentary evolution Yellow Sea Warm Current
DOI	10.1002/gj.3758
关键词[WOS]	NORTH EQUATORIAL CURRENT ; LAST GLACIAL MAXIMUM ; ARCTIC-OSCILLATION ; WINTER MONSOON ; YELLOW SEA ; SUMMER MONSOON ; WARM CURRENT ; INNER SHELF ; HOLOCENE ; CLIMATE
收录类别	SCI ; SCI
语种	英语
资助项目	COMRA Project from China Ocean Mineral Resources RD Association[DY135-E2-1-01] ; National Key Research and Development Program of China[2017YFC0405503] ; National Natural Science Foundation of China[41602349] ; National Natural Science Foundation of China[41706068] ; National Natural Science Foundation of China[U1806212]
WOS研究方向	Geology
项目资助者	COMRA Project from China Ocean Mineral Resources RD Association ; National Key Research and Development Program of China ; National Natural Science Foundation of China
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:000510959400001
出版者	WILEY
引用统计	被引频次：7[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/12831
专题	现代环境研究室
通讯作者	Lyu, Wenzhe; Yang, Jichao; Fu, Tengfei
作者单位	1.East China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai, Peoples R China 2.Minist Nat Resources, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao, Peoples R China 3.Minist Nat Resources, Natl Deep Sea Ctr, Qingdao, Peoples R China 4.Minist Nat Resources, Inst Oceanog 2, Key Lab Engn Oceanog, Hangzhou, Peoples R China 5.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China 6.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China 7.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
推荐引用方式 GB/T 7714	Lyu, Wenzhe,Yang, Jichao,Fu, Tengfei,et al. Asian monsoon and oceanic circulation paced sedimentary evolution over the past 1,500 years in the central mud area of the Bohai Sea, China[J]. GEOLOGICAL JOURNAL,2020:13.
APA	Lyu, Wenzhe.,Yang, Jichao.,Fu, Tengfei.,Chen, Yanping.,Hu, Zhangxi.,...&Chen, Shenliang.(2020).Asian monsoon and oceanic circulation paced sedimentary evolution over the past 1,500 years in the central mud area of the Bohai Sea, China.GEOLOGICAL JOURNAL,13.
MLA	Lyu, Wenzhe,et al."Asian monsoon and oceanic circulation paced sedimentary evolution over the past 1,500 years in the central mud area of the Bohai Sea, China".GEOLOGICAL JOURNAL (2020):13.