IOCAS-IR  > 海洋生态与环境科学重点实验室
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, Wenzhe1,2; Yang, Jichao3; Fu, Tengfei2; Chen, Yanping4; Hu, Zhangxi5,6; Tang, Ying Zhong5,6; Lan, Jianghu7; Chen, Guangquan2; Su, Qiao2; Xu, Xingyong2; Chen, Shenliang1
2020-02-05
Source PublicationGEOLOGICAL JOURNAL
ISSN0072-1050
Pages13
Corresponding AuthorLyu, Wenzhe(lvwenzhe1992@gmail.com) ; Yang, Jichao(yangjichao.1@163.com) ; Fu, Tengfei(futengfei@fio.org.cn)
AbstractMud 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.
KeywordArctic Oscillation Bohai Sea continental mud area East Asian Summer Monsoon (EASM) sedimentary evolution Yellow Sea Warm Current
DOI10.1002/gj.3758
Indexed BySCI
Language英语
Funding ProjectCOMRA 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 Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000510959400001
PublisherWILEY
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.qdio.ac.cn/handle/337002/165368
Collection海洋生态与环境科学重点实验室
Corresponding AuthorLyu, Wenzhe; Yang, Jichao; Fu, Tengfei
Affiliation1.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
Recommended Citation
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.
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