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Magnetic mineral dissolution recorded in a lacustrine sequence from the Heqing Basin, SW China, and its relationship with changes in the Indian monsoon
Xu, Xinwen1,2; Qiang, Xiaoke2; Zhao, Hui2; Fu, Chaofeng3
通讯作者Qiang, Xiaoke(qiangxk@loess.llqg.ac.cn)
2020-02-01
发表期刊JOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
卷号188页码:9
摘要The dissolution of magnetic oxides is an important process in many lake environments. Understanding this phenomenon is crucial for the paleoenvironmental interpretation of the magnetic properties of lake sediments. In order to reveal its effects on sedimentary magnetic properties, and to assess the possible associated paleoenvironmental implications, we carried out detailed rock magnetic analyses of the selected samples from a 920-kyr lacustrine sequence from the Heqing Basin, SW China. The results indicate that the sedimentary magnetic properties are controlled by the concentration and grain size of magnetite and maghemite. High magnetic susceptibility (chi) intervals contain more fine-grained magnetite and maghemite, while low chi intervals contain only minor amounts of residual magnetite. The decreased content of fine-grained maghemite from high chi to low chi intervals reflects the dissolution of magnetic oxides during deposition. Intervals affected by strong magnetic dissolution have a high TOC content and correspond to times of high Antarctic temperatures, suggesting that magnetic mineral dissolution intensity was associated with variations in the strength of the Indian Summer Monsoon (ISM). Notably, the ISM is sensitive to Southern Hemisphere warming. Weak magnetic dissolution indicates a dry climate occurred since similar to 320 kyr in the Heqing Basin. This dry/cool event was widespread across the Eastern Bay of Bengal, Equatorial Indian Ocean and Northern Australia, and was linked to a strengthened Indian Ocean Dipole (IOD). Since the moisture source of the Heqing Basin was mainly from the above regions, we infer that the influence of the IOD extended northwards to SW China.
关键词Lacustrine sediments The Heqing basin Rock magnetism Magnetic mineral dissolution Indian Summer Monsoon Indian Ocean Dipole
DOI10.1016/j.jseaes.2019.104081
关键词[WOS]CLIMATE VARIABILITY ; SUMMER-MONSOON ; LOESS PLATEAU ; LAKE BAIKAL ; MARINE-SEDIMENTS ; ARABIAN SEA ; IRON-OXIDES ; SUSCEPTIBILITY ; GREIGITE ; OXIDATION
收录类别SCI ; SCI
语种英语
资助项目National Science Fund of China[41402151] ; National Science Fund of China[41572164] ; National Science Fund of China[41272208] ; National Science Fund of China[41977379] ; National Natural Science Foundation of China[91855211] ; Open Fund of the State Key Laboratory of Loess and Quaternary Geology[SKLLQG1218] ; Shaanxi provincial education department special research project[14JK1738]
WOS研究方向Geology
项目资助者National Science Fund of China ; National Natural Science Foundation of China ; Open Fund of the State Key Laboratory of Loess and Quaternary Geology ; Shaanxi provincial education department special research project
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000509615200010
出版者PERGAMON-ELSEVIER SCIENCE LTD
引用统计
被引频次:6[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/361006/12789
专题古环境研究室
通讯作者Qiang, Xiaoke
作者单位1.Northwest Univ, Shaanxi Key Lab Earth Surface Syst & Environm Car, Xian 710127, Peoples R China
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
3.Changan Univ, Key Lab Western Mineral Resources & Geol Engn, Minist Educ China, Xian 710054, Peoples R China
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Xu, Xinwen,Qiang, Xiaoke,Zhao, Hui,et al. Magnetic mineral dissolution recorded in a lacustrine sequence from the Heqing Basin, SW China, and its relationship with changes in the Indian monsoon[J]. JOURNAL OF ASIAN EARTH SCIENCES,2020,188:9.
APA Xu, Xinwen,Qiang, Xiaoke,Zhao, Hui,&Fu, Chaofeng.(2020).Magnetic mineral dissolution recorded in a lacustrine sequence from the Heqing Basin, SW China, and its relationship with changes in the Indian monsoon.JOURNAL OF ASIAN EARTH SCIENCES,188,9.
MLA Xu, Xinwen,et al."Magnetic mineral dissolution recorded in a lacustrine sequence from the Heqing Basin, SW China, and its relationship with changes in the Indian monsoon".JOURNAL OF ASIAN EARTH SCIENCES 188(2020):9.
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