Pollen evidence for a mid-Holocene East Asian summer monsoon maximum in northern China | |
Wen, Ruilin1; Xiao, Jule1,2; Fan, Jiawei1; Zhang, Shengrui1,2; Yamagata, Hideki3 | |
刊名 | QUATERNARY SCIENCE REVIEWS |
2017-11-15 | |
卷号 | 176页码:29-35 |
关键词 | East Asian Summer Monsoon Dali Lake Pollen Vegetation Precipitation Holocene Northern China |
ISSN号 | 0277-3791 |
DOI | 10.1016/j.quascirev.2017.10.008 |
文献子类 | Article |
英文摘要 | There is a controversy regarding whether the high precipitation delivered by an intensified East Asian summer monsoon occurred during the early Holocene, or during the middle Holocene, especially in the context of the monsoonal margin region. The conflicting views on the subject may be caused by chronological uncertainties and ambiguities in the interpretation of different climate proxies measured in different sedimentary sequences. Here, we present a detailed record of the Holocene evolution of vegetation in northern China based on a high-resolution pollen record from Dali Lake, located near the modern summer monsoon limit. From 12,000-8300. cal BP, the sandy land landscape changed from desert to open elm forest and shrubland, while dry steppe dominated the hilly lands and patches of birch forest developed in the mountains. Between 8300 and 6000 cal BP, elm forest was extensively distributed in the sandy lands, while typical steppe covered the hilly lands and mixed coniferous-broadleaved forests expanded in the mountains. Our pollen evidence contradicts the view that the monsoonal rainfall increased during the early Holocene; rather, it indicates that the East Asian summer monsoon did not become intensified until similar to 8000 cal BP in northern China. The low precipitation during the early Holocene can be attributed to the boundary conditions, i.e., to the remnant high-latitude Northern Hemisphere i.e sheets and the relatively low global sea level. (C) 2017 Elsevier Ltd. All rights reserved. |
WOS关键词 | HOLOCENE CLIMATE CHANGES ; LAST GLACIAL MAXIMUM ; INNER-MONGOLIA ; DAIHAI LAKE ; DALI LAKE ; VARIABILITY ; PRECIPITATION ; DEGLACIATION ; TRANSITION ; PLATEAU |
WOS研究方向 | Physical Geography ; Geology |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000416194300002 |
资助机构 | National Natural Science Foundation of China(41372188 ; National Natural Science Foundation of China(41372188 ; National Key R&D Program of China(2017YFA0603403) ; National Key R&D Program of China(2017YFA0603403) ; 41672166) ; 41672166) ; National Natural Science Foundation of China(41372188 ; National Natural Science Foundation of China(41372188 ; National Key R&D Program of China(2017YFA0603403) ; National Key R&D Program of China(2017YFA0603403) ; 41672166) ; 41672166) ; National Natural Science Foundation of China(41372188 ; National Natural Science Foundation of China(41372188 ; National Key R&D Program of China(2017YFA0603403) ; National Key R&D Program of China(2017YFA0603403) ; 41672166) ; 41672166) ; National Natural Science Foundation of China(41372188 ; National Natural Science Foundation of China(41372188 ; National Key R&D Program of China(2017YFA0603403) ; National Key R&D Program of China(2017YFA0603403) ; 41672166) ; 41672166) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/82104] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Wen, Ruilin |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China 3.Paleo Labo Co Ltd, Saitama 3350016, Japan |
推荐引用方式 GB/T 7714 | Wen, Ruilin,Xiao, Jule,Fan, Jiawei,et al. Pollen evidence for a mid-Holocene East Asian summer monsoon maximum in northern China[J]. QUATERNARY SCIENCE REVIEWS,2017,176:29-35. |
APA | Wen, Ruilin,Xiao, Jule,Fan, Jiawei,Zhang, Shengrui,&Yamagata, Hideki.(2017).Pollen evidence for a mid-Holocene East Asian summer monsoon maximum in northern China.QUATERNARY SCIENCE REVIEWS,176,29-35. |
MLA | Wen, Ruilin,et al."Pollen evidence for a mid-Holocene East Asian summer monsoon maximum in northern China".QUATERNARY SCIENCE REVIEWS 176(2017):29-35. |
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