The role of the Asian winter monsoon in the rapid propagation of abrupt climate changes during the last deglaciation
文献类型:期刊论文
作者 | Chu, Guoqiang1; Sun, Qing2; Zhu, Qingzeng1; Shan, Yabing2; Shang, Wenyu2; Ling, Yuan3; Su, Youliang4; Xie, Manman2; Wang, Xishen5; Liu, Jiaqi1 |
刊名 | QUATERNARY SCIENCE REVIEWS |
出版日期 | 2017-12-01 |
卷号 | 177页码:120-129 |
ISSN号 | 0277-3791 |
关键词 | Branched Gdgts Younger Dryas Tropic Maar Lake Winter Monsoon |
DOI | 10.1016/j.quascirev.2017.10.014 |
文献子类 | Article |
英文摘要 | High-resolution temperature records spanning the last deglaciation from low latitudes are scarce; however, they are important for understanding the rapid propagation of abrupt climate events throughout the Northern Hemisphere and the tropics. Here, we present a branched GDGTs-based temperature reconstruction from the sediments of Maar Lake Huguangyan in tropical China. The record reveals that the mean temperature during the Oldest Dryas was 17.8 degrees C, which was followed by a two-step increase of 2-3 degrees C to the Bolling-Allerod, a decrease to 19.8 degrees C during the Younger Dryas, and a rapid warming at the onset of the Holocene. The Oldest Dryas was about 2 degrees C warmer than the Younger Dryas. The reconstructed temperature was weighted towards the wintertime since the lake is monomictic and the mixing process in winter supplies nutrients from the lake bottom to the entire water column, greatly promoting biological productivity. In addition, the winter-biased temperature changes observed in the study are more distinctive than the summer-biased temperature records from extra-tropical regions of East Asia. This implies that the temperature decreases during abrupt climatic events were mainly a winter phenomenon. Within the limits of the dating uncertainties, the broadly similar pattern of winter-weighted temperature change observed in both tropical Lake Huguangyan and in Greenland ice cores indicates the occurrence of tightly-coupled interactions between high latitude ice sheets and land areas in the tropics. We suggest that the winter monsoon (especially cold surges) could play an important role in the rapid transmission of the temperature signal from the Arctic to the tropics. (C) 2017 Elsevier Ltd. All rights reserved. |
WOS关键词 | DIALKYL GLYCEROL TETRAETHERS ; INTERTROPICAL CONVERGENCE ZONE ; SOUTH CHINA SEA ; HUGUANGYAN MAAR LAKE ; GDGT-BASED PROXIES ; AFRICAN LAKE ; ENVIRONMENTAL CONTROLS ; SURFACE SEDIMENTS ; SUMMER MONSOON ; LIPIDS |
WOS研究方向 | Physical Geography ; Geology |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000418203900008 |
资助机构 | National Natural Science Foundation of China(41672174 ; National Natural Science Foundation of China(41672174 ; China Geological Survey(YYWF201618) ; China Geological Survey(YYWF201618) ; Joint NSFC-ISF Research Program ; Joint NSFC-ISF Research Program ; Israel Science Foundation(41561144010) ; Israel Science Foundation(41561144010) ; 41371219) ; 41371219) ; National Natural Science Foundation of China(41672174 ; National Natural Science Foundation of China(41672174 ; China Geological Survey(YYWF201618) ; China Geological Survey(YYWF201618) ; Joint NSFC-ISF Research Program ; Joint NSFC-ISF Research Program ; Israel Science Foundation(41561144010) ; Israel Science Foundation(41561144010) ; 41371219) ; 41371219) ; National Natural Science Foundation of China(41672174 ; National Natural Science Foundation of China(41672174 ; China Geological Survey(YYWF201618) ; China Geological Survey(YYWF201618) ; Joint NSFC-ISF Research Program ; Joint NSFC-ISF Research Program ; Israel Science Foundation(41561144010) ; Israel Science Foundation(41561144010) ; 41371219) ; 41371219) ; National Natural Science Foundation of China(41672174 ; National Natural Science Foundation of China(41672174 ; China Geological Survey(YYWF201618) ; China Geological Survey(YYWF201618) ; Joint NSFC-ISF Research Program ; Joint NSFC-ISF Research Program ; Israel Science Foundation(41561144010) ; Israel Science Foundation(41561144010) ; 41371219) ; 41371219) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/82384] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Chu, Guoqiang; Sun, Qing |
作者单位 | 1.Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Natl Res Ctr Geoanal, Beijing 100037, Peoples R China 3.Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China 4.China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China 5.Chinese Acad Geol Sci, MLR Key Lab Paleomagnetism & Paleotecton Reconstr, Inst Geomech, Beijing 100081, Peoples R China |
推荐引用方式 GB/T 7714 | Chu, Guoqiang,Sun, Qing,Zhu, Qingzeng,et al. The role of the Asian winter monsoon in the rapid propagation of abrupt climate changes during the last deglaciation[J]. QUATERNARY SCIENCE REVIEWS,2017,177:120-129. |
APA | Chu, Guoqiang.,Sun, Qing.,Zhu, Qingzeng.,Shan, Yabing.,Shang, Wenyu.,...&Liu, Jiaqi.(2017).The role of the Asian winter monsoon in the rapid propagation of abrupt climate changes during the last deglaciation.QUATERNARY SCIENCE REVIEWS,177,120-129. |
MLA | Chu, Guoqiang,et al."The role of the Asian winter monsoon in the rapid propagation of abrupt climate changes during the last deglaciation".QUATERNARY SCIENCE REVIEWS 177(2017):120-129. |
入库方式: OAI收割
来源:地质与地球物理研究所
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