中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
HOLOCENE PRECIPITATION RECORDS FROM INNER MONGOLIA DERIVED FROM HYDROGEN ISOTOPE COMPOSITIONS OF SEDIMENT FATTY ACIDS

文献类型:期刊论文

作者Chen, Qingmin2; Zhou, Weijian1; Wang, Zhe2; Xian, Feng1; Burr, George S.1
刊名RADIOCARBON
出版日期2019-02-01
卷号61期号:1页码:51-65
关键词Duoerji East Asian monsoon hydrogen isotopes n-fatty acids precipitation records
ISSN号0033-8222
DOI10.1017/RDC.2018.75
通讯作者Zhou, Weijian(weijian@loess.llqg.ac.cn)
英文摘要The Inner Mongolian Plateau lies along the northern limit reached by the East Asian summer monsoon. This geographic setting makes it especially sensitive to environmental change and an excellent site for understanding Quaternary East Asian monsoon variability. In this study we present new results of hydrogen isotopic compositions of fatty acids extracted from sediments, which were used to construct Holocene paleoprecipitation (or moisture) changes in Northern China. The hydrogen isotopic composition (D/H ratio) of n-acids in the sedimentary sequence of the Duoerji peat. Inner Mongolia, was determined with gas chromatography and mass spectrometry. Changes in the precipitation from middle Inner Mongolia are recorded by the D/H ratio of n-C-20, n-C-22, n-C-24, n-C-26, n-C-28 acids (delta D). From 10-9 ka, the relatively high delta D values indicate reduced precipitation in the Early Holocene. Subsequently, increased precipitation is reflected by reduced delta D values from 9-5.5 ka. After 5.5 ka, gradually increasing delta D values record an overall decrease in precipitation. The precipitation trends established for the Duoerji sequence are consistent with other major paleoclimate proxies in the East Asian monsoon region, especially with a distinct Holocene optimum of increased monsoonal activity from 9-5.5 ka. The delta D resulting paleo-precipitation record clearly shows that the Holocene climate in Northern China is basically controlled by the insolation changes.
WOS关键词GRAIN-SIZE DISTRIBUTION ; ASIAN MONSOON ; N-ALKANES ; LEAF WAXES ; LACUSTRINE SEDIMENTS ; HIGH-RESOLUTION ; CLIMATIC-CHANGE ; NORTHERN IDAHO ; LAKE-SEDIMENTS ; D/H RATIOS
资助项目National Natural Science Foundation of China ; Ministry of Science and Technology of China ; Shaanxi Public Welfare Special Project of geological prospecting
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000458372300004
出版者UNIV ARIZONA DEPT GEOSCIENCES
资助机构National Natural Science Foundation of China ; Ministry of Science and Technology of China ; Shaanxi Public Welfare Special Project of geological prospecting
源URL[http://ir.ieecas.cn/handle/361006/14341]  
专题地球环境研究所_加速器质谱中心
通讯作者Zhou, Weijian
作者单位1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China
2.Shaanxi Inst Geol Survey, Shaanxi Ctr Geol Survey, Xian 710068, Shaanxi, Peoples R China
推荐引用方式
GB/T 7714
Chen, Qingmin,Zhou, Weijian,Wang, Zhe,et al. HOLOCENE PRECIPITATION RECORDS FROM INNER MONGOLIA DERIVED FROM HYDROGEN ISOTOPE COMPOSITIONS OF SEDIMENT FATTY ACIDS[J]. RADIOCARBON,2019,61(1):51-65.
APA Chen, Qingmin,Zhou, Weijian,Wang, Zhe,Xian, Feng,&Burr, George S..(2019).HOLOCENE PRECIPITATION RECORDS FROM INNER MONGOLIA DERIVED FROM HYDROGEN ISOTOPE COMPOSITIONS OF SEDIMENT FATTY ACIDS.RADIOCARBON,61(1),51-65.
MLA Chen, Qingmin,et al."HOLOCENE PRECIPITATION RECORDS FROM INNER MONGOLIA DERIVED FROM HYDROGEN ISOTOPE COMPOSITIONS OF SEDIMENT FATTY ACIDS".RADIOCARBON 61.1(2019):51-65.

入库方式: OAI收割

来源:地球环境研究所

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