IOCAS-IR  > 海洋地质与环境重点实验室
Global Cooling-Driven Summer Monsoon Weakening in South China Across the Eocene-Oligocene Transition
Jiao, Wenjun1; Wan, Shiming1,2; Li, Yong-Xiang3; Zhao, Debo1; Liu, Chang4; Jin, Hualong1; Li, Mengjun1; Yu, Zhaojie1; Zhang, Jin1; Pei, Wenqiang1; Li, Anchun1
2023-11-01
发表期刊JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
ISSN2169-9313
卷号128期号:11页码:20
通讯作者Wan, Shiming(wanshiming@ms.qdio.ac.cn)
摘要Recent research has suggested that East Asia has experienced a prevailing monsoon climate since the Eocene. However, there is little knowledge about the development of the East Asian monsoon system before the Miocene, particularly in southern China, due to a lack of well-dated continuous sediment records. Here, we present new magnetic proxy records from International Ocean Discovery Program Site U1501 in the northern South China Sea. We conducted rock magnetic experiments, made scanning electron microscopy observations and performed diffuse reflectance spectrum analysis on the late Eocene-early Oligocene core sediments. The magnetic signal of the sediments is dominated by detrital magnetite and titanomagnetite formed during the silicate weathering and erosion processes, which were used to infer the evolution of summer monsoon precipitation in southern China. Our results along with geochemical and clay mineral data from Site U1501 strongly indicate that the East Asian summer monsoon generally weakened across the Eocene-Oligocene transition. This change was linked to coeval global cooling rather than tectonic processes. Prior to the Eocene-Oligocene transition, the summer monsoon intensified, likely due to the latest Eocene warming event caused by the enhancement of the Atlantic Meridional Overturning Circulation, which may have preconditioned the Earth system for the greenhouse-to-icehouse transition.
关键词East Asian monsoon South China Sea environmental magnetism global cooling Eocene-Oligocene transition International Ocean Discovery Program (IODP) gSite U1501
DOI10.1029/2023JB027265
收录类别SCI
语种英语
资助项目We acknowledge the International Ocean Discovery Program and the scientific party and technicians of IODP Expedition 368 for recovering the samples. We are grateful to Dr. Qingsong Liu, Zhong Yi and Han Peng for their assistance in DRS measurements and dat ; International Ocean Discovery Program[42125602] ; International Ocean Discovery Program[42006050] ; International Ocean Discovery Program[42076052] ; International Ocean Discovery Program[4212500229] ; National Natural Science Foundation of China[XDB40010100] ; Strategic Priority Research Program of the Chinese Academy of Sciences[2022YFF0800503] ; National Key Research and Development Program of China[2017ASTCP-ES01] ; Taishan and Aoshan Talents Program
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:001099683800001
出版者AMER GEOPHYSICAL UNION
WOS关键词EAST-ASIAN MONSOON ; TIBETAN PLATEAU ; MAGNETIC-SUSCEPTIBILITY ; ENVIRONMENTAL-CHANGES ; SEA IMPLICATIONS ; CLIMATE ; EVOLUTION ; TEMPERATURE ; RECORDS ; UPLIFT
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文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/184074
专题海洋地质与环境重点实验室
通讯作者Wan, Shiming
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China
3.Nanjing Univ, Inst Geophys & Geodynam, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing, Peoples R China
4.Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA
第一作者单位中国科学院海洋研究所
通讯作者单位中国科学院海洋研究所
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GB/T 7714
Jiao, Wenjun,Wan, Shiming,Li, Yong-Xiang,et al. Global Cooling-Driven Summer Monsoon Weakening in South China Across the Eocene-Oligocene Transition[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2023,128(11):20.
APA Jiao, Wenjun.,Wan, Shiming.,Li, Yong-Xiang.,Zhao, Debo.,Liu, Chang.,...&Li, Anchun.(2023).Global Cooling-Driven Summer Monsoon Weakening in South China Across the Eocene-Oligocene Transition.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,128(11),20.
MLA Jiao, Wenjun,et al."Global Cooling-Driven Summer Monsoon Weakening in South China Across the Eocene-Oligocene Transition".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 128.11(2023):20.
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