Indian summer monsoon variability over last 2000 years inferred from sediment magnetic characteristics in Lugu Lake, southwest China

doi:10.1016/j.palaeo.2021.110581

CORC > 烟台海岸带研究所 > 中国科学院烟台海岸带研究所 > 中科院海岸带环境过程与生态修复重点实验室

	Indian summer monsoon variability over last 2000 years inferred from sediment magnetic characteristics in Lugu Lake, southwest China
	Wang, Xiaohui 1; Wang, Longsheng 1,2,3,4; Hu, Shouyun 2; Ma, Mingming 5; Wang, Qing 1; Cui, Buli 1; Zhan, Chao 1; Zeng, Lin 1; Liu, Xianbin 1; Shen, Ji 2
刊名	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
	2021-09-15
卷号	578 页码:12
关键词	Environmental magnetism Rock Magnetism Monsoon precipitation Catchment erosion Lake sediment
ISSN号	0031-0182
DOI	10.1016/j.palaeo.2021.110581
通讯作者	Wang, Longsheng(52wls@163.com) ; Hu, Shouyun(hu_shouyun@hotmail.com)
英文摘要	Knowledge of climatic change during the past 2000 years in southwestern China is important for understanding the evolution of the Indian summer monsoon (ISM). For this study, we conducted systematic analysis of magnetic minerals in sediments from Lugu Lake in northwestern Yunnan Province. Magnetic measurements suggest that magnetite dominated the studied magnetic mineral assemblages. Both natural origins and anthropogenic activities are considered to be the sources of the magnetic minerals based on the correlations of chi vs. chi(fd)% and chi(ARM)/chi. The magnetic minerals of natural origins can be attributed to terrestrial detrital input rather than biogenic sources. Combined with diatom and geochemical records, magnetic parameters including chi, chi(fd)%, and Sratio can be used as sensitive indicators of ISM change, and suggest that two significant dry periods occurred in the Medieval Warm Period (MWP, 800-1300 CE) and Roman Warm Period (RWP, 0-400 CE) and two relatively wet intervals in the Dark Ages Cold Period (DACP, 400-800 CE) and Little Ice Age (LIA, 1300-1850 CE). Significant shifts of magnetic parameters in Lugu Lake samples revealed sensitivity to precipitation-controlled catchment erosion. The climatic patterns shown by the magnetic characteristics were generally similar to those in extensive areas dominated by the ISM. We speculate that rainfall caused by the ISM during the last 2000 years may be related to the variations of El Nino/Southern Oscillation (ENSO) and the mean position migration of the ITCZ.
资助项目	National Natural Science Foundation of China[U1706220] ; National Natural Science Foundation of China[41702185] ; National Natural Science Foundation of China[41572152] ; National Natural Science Foundation of China[31800421] ; National Natural Science Foundation of China[41977039] ; Natural Science Foundation of Shandong Province[ZR2018PD005] ; Natural Science Foundation of Shandong Province[ZR2018PC004] ; Foundation of School and Land Integration Development in Yantai[2021XDRHXMQT18] ; Humanity and Social Science Foundation of Ministry of Education of China[19YJCZH171] ; Open Foundation of State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS[SKLLQG2024] ; Open Foundation of CAS Key Laboratory of Coastal Environmental Processes and Ecological Remediation, YICCAS[2020KGJJ10] ; Key Research and Development Plan of Shandong Province[2019GSF107018] ; Sino-German Center for Research Promotion[GZ675] ; Chinese Academy of Sciences Visiting Professorship for Senior International Scientists[2012T1Z0004]
WOS关键词	TIBETAN PLATEAU ; GUIZHOU PLATEAU ; EASTERN CHINA ; PRECIPITATION ; CLIMATE ; RECORD ; AGE ; TEMPERATURE ; SEA ; SUSCEPTIBILITY
WOS研究方向	Physical Geography ; Geology ; Paleontology
语种	英语
WOS记录号	WOS:000684182500015
资助机构	National Natural Science Foundation of China ; Natural Science Foundation of Shandong Province ; Foundation of School and Land Integration Development in Yantai ; Humanity and Social Science Foundation of Ministry of Education of China ; Open Foundation of State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS ; Open Foundation of CAS Key Laboratory of Coastal Environmental Processes and Ecological Remediation, YICCAS ; Key Research and Development Plan of Shandong Province ; Sino-German Center for Research Promotion ; Chinese Academy of Sciences Visiting Professorship for Senior International Scientists
内容类型	期刊论文
源URL	[http://ir.yic.ac.cn/handle/133337/29630]
专题	烟台海岸带研究所_中科院海岸带环境过程与生态修复重点实验室海岸带生物资源高效利用研究与发展中心
通讯作者	Wang, Longsheng; Hu, Shouyun
作者单位	1.Ludong Univ, Coast Inst, Yantai 264025, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Peoples R China 3.Chinese Acad Sci, Yantai Inst Coastal Zone Res, CAS Key Lab Coastal Environm Proc & Ecol Remediat, Yantai 264003, Peoples R China 4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China 5.Fujian Normal Univ, Inst Geog, Fuzhou 350007, Peoples R China
推荐引用方式 GB/T 7714	Wang, Xiaohui,Wang, Longsheng,Hu, Shouyun,et al. Indian summer monsoon variability over last 2000 years inferred from sediment magnetic characteristics in Lugu Lake, southwest China[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2021,578:12.
APA	Wang, Xiaohui.,Wang, Longsheng.,Hu, Shouyun.,Ma, Mingming.,Wang, Qing.,...&Shen, Ji.(2021).Indian summer monsoon variability over last 2000 years inferred from sediment magnetic characteristics in Lugu Lake, southwest China.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,578,12.
MLA	Wang, Xiaohui,et al."Indian summer monsoon variability over last 2000 years inferred from sediment magnetic characteristics in Lugu Lake, southwest China".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 578(2021):12.