A novel procedure for pollen-based quantitative paleoclimate reconstructions and its application in China | |
Chen JianHui1; Lv FeiYa1; Huang XiaoZhong1; Birks, H. John B.2,3; Telford, Richard J.2,3; Zhang ShengRui4; Xu QingHai4; Zhao Yan5,6; Wang HaiPeng1; Zhou AiFeng1 | |
刊名 | SCIENCE CHINA-EARTH SCIENCES |
2017-11-01 | |
卷号 | 60期号:11页码:2059-2066 |
关键词 | Pollen Quantitative reconstructions Statistical significance Marginal areas of the Asian summer monsoon |
ISSN号 | 1674-7313 |
DOI | 10.1007/s11430-017-9095-1 |
通讯作者 | Chen JianHui(jhchen@lzu.edu.cn) |
英文摘要 | Traditionally, the evaluation of pollen-based quantitative paleoclimate reconstructions focuses on the ability of calibration sets to infer present climatic conditions and/or the similarity between fossil and modern assemblages. Objective criteria for choosing the most appropriate climate parameter(s) to be reconstructed at a specific site are thus lacking. Using a novel approach for testing the statistical significance of a quantitative reconstruction using random environmental data, in combination with the advantageous large environmental gradients, abundant vegetation types and comprehensive modern pollen databases in China, we describe a new procedure for pollen-based quantitative paleoclimatic reconstructions. First, the most significant environmental variable controlling the fossil pollen assemblage changes is identified. Second, a calibration set to infer changes in this targeted variable is built up, by limiting the modern ranges of other environmental variables. Finally, the pollen-based quantitative reconstruction is obtained and its statistical significance assessed. This novel procedure was used to reconstruct the mean annual precipitation (P-ann) from Gonghai Lake in the Lvliang Mountains, and Tianchi Lake in the Liupan Mountains, on the eastern and western fringe of the Chinese Loess Plateau, respectively. Both P-ann reconstructions are statistically significant (p<0.001), and a sound and stable correlation relationship exists in their common period, showing a rapid precipitation decrease since 3300 cal yr BP. Thus, we propose that this procedure has great potential for reducing the uncertainties associated with pollen-based quantitative paleoclimatic reconstructions in China. |
资助项目 | National Natural Science Foundation of China[41471162] ; National Natural Science Foundation of China[41571182] ; National Key R&D Program of China[2017YFA0603402] |
WOS关键词 | ASIAN SUMMER MONSOON ; LAST GLACIAL MAXIMUM ; CLIMATE-CHANGE ; LOESS PLATEAU ; PRECIPITATION CHANGES ; HOLOCENE VEGETATION ; TIBETAN PLATEAU ; NORTHERN CHINA ; LAKE ; MIDHOLOCENE |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000413691300012 |
资助机构 | National Natural Science Foundation of China ; National Key R&D Program of China |
内容类型 | 期刊论文 |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/61247] |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Chen JianHui |
作者单位 | 1.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab West Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China 2.Univ Bergen, Dept Biol, N-5020 Bergen, Norway 3.Univ Bergen, Bjerknes Ctr Climate Res, N-5020 Bergen, Norway 4.Hebei Normal Univ, Inst Nihewan Archaeol Res, Shijiazhuang 050024, Hebei, Peoples R China 5.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China 6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Chen JianHui,Lv FeiYa,Huang XiaoZhong,et al. A novel procedure for pollen-based quantitative paleoclimate reconstructions and its application in China[J]. SCIENCE CHINA-EARTH SCIENCES,2017,60(11):2059-2066. |
APA | Chen JianHui.,Lv FeiYa.,Huang XiaoZhong.,Birks, H. John B..,Telford, Richard J..,...&Wei GuoYing.(2017).A novel procedure for pollen-based quantitative paleoclimate reconstructions and its application in China.SCIENCE CHINA-EARTH SCIENCES,60(11),2059-2066. |
MLA | Chen JianHui,et al."A novel procedure for pollen-based quantitative paleoclimate reconstructions and its application in China".SCIENCE CHINA-EARTH SCIENCES 60.11(2017):2059-2066. |
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