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	Mid-Pleistocene climate transition triggered by Antarctic Ice Sheet growth
通讯作者	An, Zhisheng(anzs@loess.llqg.ac.cn) ; Zhang, Xu(xuang@bas.ac.uk) ; Liu, Zhonghui(zhliu@hku.hk)
	An, Zhisheng1,2,3; Zhou, Weijian1,2,3; Zhang, Zeke1,2,4; Zhang, Xu5,6; Liu, Zhonghui1,7; Sun, Youbin1,2; Clemens, Steven C.8; Wu, Lixin9,10; Zhao, Jiaju1,2; Shi, Zhengguo1,2
	2024-08-02
发表期刊	SCIENCE (IF:41.058[JCR-2017],40.627[5-Year])
ISSN	0036-8075
卷号	385期号:6708页码:560-565
摘要	Despite extensive investigation, the nature and causes of the Mid-Pleistocene Transition remain enigmatic. In this work, we assess its linkage to asynchronous development of bipolar ice sheets by synthesizing Pleistocene mid- to high-latitude proxy records linked to hemispheric ice sheet evolution. Our results indicate substantial growth of the Antarctic Ice Sheets (AISs) at 2.0 to 1.25 million years ago, preceding the rapid expansion of Northern Hemisphere Ice Sheets after similar to 1.25 million years ago. Proxy-model comparisons suggest that AIS and associated Southern Ocean sea ice expansion can induce northern high-latitude cooling and enhanced moisture transport to the Northern Hemisphere, thus triggering the Mid-Pleistocene Transition. The dynamic processes involved are crucial for assessing modern global warming that is already inducing asynchronous bipolar melting of ice sheets.
DOI	10.1126/science.abn4861
收录类别	SCI
语种	英语
关键词[WOS]	CARBON-DIOXIDE CONCENTRATION ; SEA-SURFACE TEMPERATURES ; LAST GLACIAL MAXIMUM ; SOUTHERN-OCEAN ; NORTH-ATLANTIC ; CHINESE LOESS ; BORON ISOTOPE ; CIRCULATION CHANGES ; RECORD ; VARIABILITY
资助项目	Fund of Shandong Province[LSKJ202203300] ; Basic Science Center for Tibetan Plateau Earth System (BSCTPES, NSFC)[41988101] ; Chinese Academy of Sciences[XDB40000000] ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Alfred Wegener Institute (AWI) through the research program PACES-II of the Helmholtz Association ; Helmholtz Climate Initiative REKLIM ; National Key Scientific and Technological Infrastructure project Earth System Science Numerical Simulator Facility (Earth Lab)
WOS研究方向	Science & Technology - Other Topics
WOS类目	Multidisciplinary Sciences
WOS记录号	WOS:001285367900038
项目资助者	Fund of Shandong Province ; Basic Science Center for Tibetan Plateau Earth System (BSCTPES, NSFC) ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Alfred Wegener Institute (AWI) through the research program PACES-II of the Helmholtz Association ; Helmholtz Climate Initiative REKLIM ; National Key Scientific and Technological Infrastructure project Earth System Science Numerical Simulator Facility (Earth Lab)
出版者	AMER ASSOC ADVANCEMENT SCIENCE
文献类型	期刊论文
条目标识符	http://ir.nigpas.ac.cn/handle/332004/44157
专题	中国科学院南京地质古生物研究所
通讯作者	An, Zhisheng; Zhang, Xu; Liu, Zhonghui
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess Sci, Xian 710061, Peoples R China 2.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China 3.Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier, Beijing 100875, Peoples R China 4.Nanjing Univ, Dept Earth & Planetary Sci, Nanjing 210023, Peoples R China 5.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Resources, Beijing 100101, Peoples R China 6.British Antarctic Survey, Cambridge CB3 0ET, England 7.Univ Hong Kong, Dept Earth Sci, Hong Kong, Peoples R China 8.Brown Univ, Dept Earth Environm & Planetary Sci, Providence, RI 02912 USA 9.Laoshan Lab, Qingdao 266000, Peoples R China 10.Ocean Univ China, Inst Adv Ocean Studies, Key Lab Phys Oceanog, Qingdao 266100, Peoples R China
推荐引用方式 GB/T 7714	An, Zhisheng,Zhou, Weijian,Zhang, Zeke,et al. Mid-Pleistocene climate transition triggered by Antarctic Ice Sheet growth[J]. SCIENCE,2024,385(6708):560-565.
APA	An, Zhisheng.,Zhou, Weijian.,Zhang, Zeke.,Zhang, Xu.,Liu, Zhonghui.,...&Cai, Wenju.(2024).Mid-Pleistocene climate transition triggered by Antarctic Ice Sheet growth.SCIENCE,385(6708),560-565.
MLA	An, Zhisheng,et al."Mid-Pleistocene climate transition triggered by Antarctic Ice Sheet growth".SCIENCE 385.6708(2024):560-565.

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