High-Resolution Geochemical Records in the Inner Shelf Mud Wedge of the East China Sea and Their Indication to the Holocene Monsoon Climatic Changes and Events
Wang Longsheng1,3,7; Zhou Bin2; Zheng Bang2; Wang Ke4; Mei Xi5; Wang Qing1; Wang Xiaohui1; Zheng Hongbo6
通讯作者Wang Longsheng(52wls@163.com) ; Zhou Bin(zhoubinok@163.com)
2021-12-01
发表期刊JOURNAL OF OCEAN UNIVERSITY OF CHINA
ISSN1672-5182
卷号20期号:6页码:1409-1418
摘要The inner shelf mud wedge (ISMW) located in the East China Sea (ECS) is the fine-grained sedimentary area with high sedimentation rate and has provided an ideal study area for understanding the East Asian Summer Monsoon (EASM) evolution during the Holocene. In this paper, we presented the high-resolution geochemical data of the sediments from the core MD06-3040 in the ISMW of the ECS determined by X-ray fluorescence core scanning (XRF-CS) analysis, a high-resolution, continuous, and multi-element method. Geochemical and factor analysis results reveal that the variations of elemental compositions (Al, Si, K, Ti, Fe), the elemental ratios of Al/Zr, Ca/Ti and Rb/Sr, and the factor scores (F1) are correlated with the changes of the EASM during the period of 6000-1300 cal yrBP. The higher values of geochemical compositions indicating the terrigenous inputs implied the intensification of anthropogenic activities after 1300 cal yrBP. Meanwhile, the significant decrease of most geochemical compositions and the F1 factor scores during 4500-3500 cal yrBP and 1700-1500 cal yrBP, within the dating errors, coincided with the weak EASM events (presumably drought and cold events). The spectral analysis results of K concentrations, Al/Zr ratios and F1 factor scores show the millennial and centennial climatic fluctuations, which are consistent with other marine sedimentary records in the adjacent areas. All the findings show that the geochemical compositions of sediments from core MD06-3040 are influenced by the EASM evolution, the variable El Nino/Southern Oscillation (ENSO) and the local oceanic thermohaline circulation (e.g., Kuroshio Current). These results are greatly helpful in uncovering the forcing mechanism of the monsoonal climate in the east China over the Holocene and also contribute to the understanding of EASM variability.
关键词Holocene climatic event East Asian Summer Monsoon XRF core scanning inner shelf mud wedge
DOI10.1007/s11802-021-4651-1
关键词[WOS]CHANGJIANG YANGTZE-RIVER ; NORTH-ATLANTIC CLIMATE ; ASIAN SUMMER MONSOON ; LATITUDE CLIMATE ; SURFACE-WATER ; ICE-SHEET ; VARIABILITY ; SEDIMENTS ; DELTA ; SOUTH
收录类别SCI ; SCI
语种英语
WOS研究方向Oceanography
WOS类目Oceanography
WOS记录号WOS:000720813700010
出版者OCEAN UNIV CHINA
引用统计
被引频次:3[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/361006/17261
专题黄土与第四纪地质国家重点实验室(2010~)
通讯作者Wang Longsheng; Zhou Bin
作者单位1.Ludong Univ, Coast Inst, Yantai 264025, Peoples R China
2.Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210023, Peoples R China
3.Chinese Acad Sci, Yantai Inst Coastal Zone Res YIC, Key Lab Coastal Environm Proc & Ecol Remediat, Yantai 264003, Peoples R China
4.Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, Tokyo 1130033, Japan
5.Minist Nat Resources, Key Lab Gas Hydrate, Qingdao Inst Marine Geol, Qingdao 266071, Peoples R China
6.Yunnan Univ, Res Ctr Earth Syst Sci, Kunming 650091, Yunnan, Peoples R China
7.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
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Wang Longsheng,Zhou Bin,Zheng Bang,et al. High-Resolution Geochemical Records in the Inner Shelf Mud Wedge of the East China Sea and Their Indication to the Holocene Monsoon Climatic Changes and Events[J]. JOURNAL OF OCEAN UNIVERSITY OF CHINA,2021,20(6):1409-1418.
APA Wang Longsheng.,Zhou Bin.,Zheng Bang.,Wang Ke.,Mei Xi.,...&Zheng Hongbo.(2021).High-Resolution Geochemical Records in the Inner Shelf Mud Wedge of the East China Sea and Their Indication to the Holocene Monsoon Climatic Changes and Events.JOURNAL OF OCEAN UNIVERSITY OF CHINA,20(6),1409-1418.
MLA Wang Longsheng,et al."High-Resolution Geochemical Records in the Inner Shelf Mud Wedge of the East China Sea and Their Indication to the Holocene Monsoon Climatic Changes and Events".JOURNAL OF OCEAN UNIVERSITY OF CHINA 20.6(2021):1409-1418.
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