A high-resolution sediment record of East Asian summer monsoon from the northern South China Sea spanning the past 7500 years
Huang, Chao1,2,5; Li, Mingkun3; Liu, Zhifeng4; Wei, Gangjian2; Chen, Fajin5; Kong, Deming5; Huang, Xin1,5; Ye, Feng4
刊名HOLOCENE
2020-08-21
页码12
关键词East Asian summer monsoon grain size records Holocene magnetic parameters South China Sea
ISSN号0959-6836
DOI10.1177/0959683620950445
通讯作者Wei, Gangjian(gjwei@gig.ac.cn) ; Chen, Fajin(fjchen@gdou.edu.cn)
英文摘要High-resolution Holocene marine sediment records are limited, which hampers our understanding of paleomonsoon evolution. Continental shelf sediment records are derived mainly from terrestrial weathering products and are thus often sensitive to paleoclimate variations. In this study, the grain size and magnetic mineral composition of a well-dated sediment core (YJ Core) from the northern inner shelf of the South China Sea (SCS) were analyzed to provide a high-resolution record of the Holocene evolution of the East Asian summer monsoon (EASM). These magnetic and grain size records indicate that EASM intensity followed a general declining trend between approximately 6800 and 2000 cal yr BP. This general pattern is synchronous with other geologic archives from monsoon regions, and can be attributed to solar radiation forcing in the Northern Hemisphere. On centennial timescales, a weak EASM closely coincides with periods of weak solar activity. In addition, spectral analysis of clays reveals five prominent cycles, with periodicities of approximately 364, 202, 158, 119, and 104 years, which correspond to solar activity cycles. The similarities between the cyclicities of the Asian monsoon signal in sedimentary records and those of solar activity demonstrate that solar forcing has a relatively large influence on the centennial-scale variability of the EASM.
资助项目National Key Research and Development Project of China[2016YFA0601204] ; Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences[MGE2019KG04] ; Key Laboratory of Ocean and Marginal Sea Geology, Chinese Academy of Sciences[OMG2019-10] ; Guangdong Natural Science Foundation of China[2020A1515010500] ; Project of Enhancing School with Innovation of Guangdong Ocean University[GDOU230419097] ; program for scientific research startup funds of Guangdong Ocean University[R19007] ; South China Sea of Guangdong Ocean University[573118019]
WOS研究方向Physical Geography ; Geology
语种英语
出版者SAGE PUBLICATIONS LTD
WOS记录号WOS:000562078600001
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/168330]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Wei, Gangjian; Chen, Fajin
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
3.South China Normal Univ, Sch Geog, Guangzhou, Peoples R China
4.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Ocean & Marginal Sea Geol, Guangzhou, Peoples R China
5.Guangdong Ocean Univ, Guangdong Prov Key Lab Coastal Ocean Variat & Dis, Zhanjiang 524088, Peoples R China
推荐引用方式
GB/T 7714
Huang, Chao,Li, Mingkun,Liu, Zhifeng,et al. A high-resolution sediment record of East Asian summer monsoon from the northern South China Sea spanning the past 7500 years[J]. HOLOCENE,2020:12.
APA Huang, Chao.,Li, Mingkun.,Liu, Zhifeng.,Wei, Gangjian.,Chen, Fajin.,...&Ye, Feng.(2020).A high-resolution sediment record of East Asian summer monsoon from the northern South China Sea spanning the past 7500 years.HOLOCENE,12.
MLA Huang, Chao,et al."A high-resolution sediment record of East Asian summer monsoon from the northern South China Sea spanning the past 7500 years".HOLOCENE (2020):12.
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