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New chronology of the Chinese loess-paleosol sequence by leaf wax delta D records during the past 800 k.y.

文献类型：期刊论文

作者Wang, Zheng1,2; Liu, Weiguo1,2,3; Wang, Hong4; Cao, Yunning1,2; Hu, Jing1,2; Dong, Jibao1,2; Lu, Hongxuan1,2; Wang, Huangye1,2; Xing, Meng1,2; Liu, Hu1,2
刊名GEOLOGY
出版日期2021-07-01
卷号49期号:7页码:847-850
ISSN号0091-7613
DOI10.1130/G48833.1
通讯作者Liu, Weiguo(liuwg@loess.lgg.ac.cn) ; Wang, Hong()
英文摘要The Chinese loess-paleosol sequences provide important archives for studying paleoenvironmental changes. However, the lack of independent and accurate time scales hinders the study between loess and other records. Asian stalagmite delta O-18 records indicate synchronous patterns of paleoprecipitation delta O-18 over large geographic regions. The record of hydrogen isotopic composition of plant wax (delta D-wax) in Chinese loess is also controlled by rainwater delta D. Both share a common origin. The linear relationship between rainfall delta O-18 and delta D variance provides the basis to tie together chronologies of the same climate event in different records. Here, we show a new loess chronology by correlating chronologies of marker boundaries of the prominent climate chronozones in stalagmite delta O-18 and summer insolation to the equivalent climate stratigraphy in the loess delta D-wax sequence. We first developed and tested this novel methodology with data since the last interglacial on a millennial scale, and then applied this approach to the loess delta D-wax sequence for the past 800 k.y. to improve the traditional chronology based on magnetic susceptibility and grain size. The new delta D-wax time series provides not only an improved chronology for studying paleoclimate changes during interglacial intervals, it also represents a unique database with which to better understand the links between the Asian monsoon changes in the Chinese loess and other global climate events, especially for the periods prior to 640 ka, for which stalagmite records are not available.
WOS关键词EAST-ASIAN MONSOON ; PRECIPITATION ; VEGETATION ; VARIABILITY ; ISOTOPES ; CLIMATES ; PLATEAU ; SCALE
资助项目Strategic Priority Research Program of Chinese Academy of Sciences[XDB40000000] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDA2007020202] ; National Natural Science Foundation of China[41773010]
WOS研究方向Geology
语种英语
WOS记录号WOS:000675396700017
出版者GEOLOGICAL SOC AMER, INC
资助机构Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China
源URL[http://ir.ieecas.cn/handle/361006/16846]  
专题地球环境研究所_加速器质谱中心
第四纪科学与全球变化卓越创新中心
通讯作者Liu, Weiguo; Wang, Hong
作者单位1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
2.CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier, Beijing 100875, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Zheng,Liu, Weiguo,Wang, Hong,et al. New chronology of the Chinese loess-paleosol sequence by leaf wax delta D records during the past 800 k.y.[J]. GEOLOGY,2021,49(7):847-850.
APA Wang, Zheng.,Liu, Weiguo.,Wang, Hong.,Cao, Yunning.,Hu, Jing.,...&Liu, Hu.(2021).New chronology of the Chinese loess-paleosol sequence by leaf wax delta D records during the past 800 k.y..GEOLOGY,49(7),847-850.
MLA Wang, Zheng,et al."New chronology of the Chinese loess-paleosol sequence by leaf wax delta D records during the past 800 k.y.".GEOLOGY 49.7(2021):847-850.

入库方式： OAI收割

来源：地球环境研究所

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