Iron oxide characteristics of the Chinese loess-red clay sequences and their implications for the evolution of the East Asian summer monsoon since the Late Oligocene

doi:10.1016/j.palaeo.2020.109604

IEECAS OpenIR > 古环境研究室

	Iron oxide characteristics of the Chinese loess-red clay sequences and their implications for the evolution of the East Asian summer monsoon since the Late Oligocene
	Zhao, Hui 1,2; Qiang, Xiaoke1,3 ; Xu, Xinwen 4; Sun, Youbin 1,3
通讯作者	Zhao, Hui(zhaohui@ieecas.cn)
	2020-04-01
发表期刊	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN	0031-0182
卷号	543 页码:9
摘要	The most significant climatic change in East Asia involved the formation and evolution of the coupled monsoon-arid environmental system during the Cenozoic, which was dynamically linked to global cooling and the growth of the Qinghai-Tibet Plateau. However, our understanding of monsoon evolution since the Late Oligocene remains controversial due to differences in the interpretation of various environmental proxies from loess archives. In this study, the composition and relative abundance of pedogenic iron oxides of two eolian sequences from the Lingtai section and the Zhuanglang drill core were investigated using rock magnetic, optical spectroscopy, and geochemical analyses. The results indicate that while the composition of iron oxides in the Mio-Pliocene red clay and Quaternary loess-paleosol sequences is similar, the concentrations of magnetite, maghemite, hematite and goethite are quite different between loess, paleosol and red clay. The combination of magnetic proxies (magnetic susceptibility, Fe-d/Pe(t), and color a(star) values) reveals that precipitation and temperature played varying roles in driving pedogenesis and chemical weathering since the Late Oligocene. During the Late Oligocene to Early Miocene, the occurrence of relatively strong pedogenesis and chemical weathering was likely the result of high temperatures rather than high precipitation. The East Asian summer monsoon intensified during the Middle Miocene Climate Optimum (16.5-14.5 Ma), in response to global climatic warming; subsequently, during the Middle to Late Miocene, the monsoon intensity gradually weakened due to global cooling. After similar to 8 Ma, the summer monsoon strengthened substantially and reached a maximum during 4.5-2.6 Ma, possibly as a result of the uplift of the northeastern margin of the Qinghai-Tibetan Plateau during the Late Miocene. The monsoon intensity then commenced a decreasing trend in the Early Pleistocene, but then strengthened again after similar to 1.0 Ma.
关键词	Chinese Loess Plateau Rock magnetism Fe-d/Fe-t Zhuanglang Lingtai Monsoon evolution
DOI	10.1016/j.palaeo.2020.109604
关键词[WOS]	TEMPERATURE-DEPENDENT SUSCEPTIBILITY ; NORTHERN TIBETAN PLATEAU ; MAGNETIC-SUSCEPTIBILITY ; SOUTH CHINA ; XINING BASIN ; XERALF CHRONOSEQUENCE ; SEDIMENTARY ARCHIVE ; MIOCENE CLIMATE ; HOLOCENE LOESS ; 20 MA
收录类别	SCI ; SCI
语种	英语
资助项目	Chinese Academy of Sciences[QYZDY-SSWDQC001] ; Chinese Academy of Sciences[QYZDY-SSW-DQC010] ; National Natural Science Foundation of China[41572164] ; Key Research and Development Program of Shaanxi Province[2017ZDCXL-SF-03-01-01] ; Shaanxi Postdoctoral Science Fund[2017BSHEDZZ16]
WOS研究方向	Physical Geography ; Geology ; Paleontology
项目资助者	Chinese Academy of Sciences ; National Natural Science Foundation of China ; Key Research and Development Program of Shaanxi Province ; Shaanxi Postdoctoral Science Fund
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS记录号	WOS:000518707600014
出版者	ELSEVIER
引用统计	被引频次：23[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/361006/12620
专题	古环境研究室第四纪科学与全球变化卓越创新中心
通讯作者	Zhao, Hui
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China 2.Xian Inst Innovat Earth Environm Res, Xian 710061, Peoples R China 3.Chinese Acad Sci, CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China 4.Northwest Univ, Coll Urban & Environm Sci, Xian 710127, Shaanxi, Peoples R China
推荐引用方式 GB/T 7714	Zhao, Hui,Qiang, Xiaoke,Xu, Xinwen,et al. Iron oxide characteristics of the Chinese loess-red clay sequences and their implications for the evolution of the East Asian summer monsoon since the Late Oligocene[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2020,543:9.
APA	Zhao, Hui,Qiang, Xiaoke,Xu, Xinwen,&Sun, Youbin.(2020).Iron oxide characteristics of the Chinese loess-red clay sequences and their implications for the evolution of the East Asian summer monsoon since the Late Oligocene.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,543,9.
MLA	Zhao, Hui,et al."Iron oxide characteristics of the Chinese loess-red clay sequences and their implications for the evolution of the East Asian summer monsoon since the Late Oligocene".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 543(2020):9.