中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet

文献类型:期刊论文

作者Liu,QS(Liu,Qingsong)2,3; Nie,JS(Nie,Junsheng)1,8; Garzione,C(Garzione,Carmala)8; Su,QD(Su,Qingda)1; Zhang,R(Zhang,Rui)1; Heslop, D(Heslop.David)5; Necula, C(Necula,Cristian)4; Zhang,SH(Zhang,Shihong)6; Song,YG(Song,Yougui)7; Luo,Z(Luo,Zeng)1
刊名Science Advances
出版日期2017-03-29
卷号3期号:3页码:e1600762
关键词Antarctica East Asian Monsoon Tibetan Plateau Eccentricity Ice Sheets Orbital Forcing
DOI10.1126/sciadv.1600762
文献子类期刊论文
英文摘要East Asian summer monsoon (EASM) precipitation received by northern China over the past 800 thousand years (ky) is characterized by dominant 100-ky periodicity, mainly attributed to CO2 and Northern Hemisphere insolation-driven ice sheet forcing. We established an EASM record in the Late Miocene from lacustrine sediments in the Qaidam Basin, northern China, which appears to exhibit a dominant 100-ky periodicity similar to the EASM records during the Late Quaternary. Because evidence suggests that partial or ephemeral ice existed in the Northern Hemisphere during the Late Miocene, we attribute the 100-ky cycles to CO2 and Southern Hemisphere insolation-driven Antarctic ice sheet forcing. This indicates a >6-million year earlier onset of the dominant 100-ky Asian monsoon and, likely, glacial and CO2 cycles and may indicate dominant forcing of Northern Hemisphere climate by CO2 and Southern Hemisphere ice sheets in a warm world.
项目编号2016YFE0109500 ; 2013CB956400 ; XDB03020400 ; 41422204 ; 41172329 ; 41290253 ; 1545859
语种英语
资助机构national key research and development program of China ; national key research and development program of China ; the (973) National Basic Research Program of China ; the (973) National Basic Research Program of China ; Strategic Priority Research Program of the Chinese Academy ofSciences ; Strategic Priority Research Program of the Chinese Academy ofSciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; U.S. NSF ; U.S. NSF
源URL[http://ir.ieecas.cn/handle/361006/5591]  
专题地球环境研究所_古环境研究室
通讯作者Nie,Junsheng
作者单位1.Key Laboratory of Western China’s Environmental System (Ministry of Education), Collegeof Earth and Environmental Sciences, Lanzhou University, Lanzhou, Gansu 730000, China
2.Department of Marine Science and Technology, South University of Scienceand Technology of China, Shenzhen 518055, China
3.Laboratory for Marine Geology, National Oceanography Laboratory, Qingdao 266061, China
4.Faculty of Physics, Paleomagnetic Laboratory,University ofBucharest, NicolaeBalcescu,Sector 1, 010041 Bucharest, Romania
5.Research School of EarthSciences, Australian National University, Canberra, Australian Capital Territory 0200, Australia
6.State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China
7.State KeyLaboratory of Loess and Quaternary Geology, Institute of Earth Environment, ChineseAcademy of Sciences, P.O. Box 17, Xi’an 710075, China
8.Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY14627, USA
推荐引用方式
GB/T 7714
Liu,QS,Nie,JS,Garzione,C,et al. Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet[J]. Science Advances,2017,3(3):e1600762.
APA Liu,QS.,Nie,JS.,Garzione,C.,Su,QD.,Zhang,R.,...&Nie,Junsheng.(2017).Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet.Science Advances,3(3),e1600762.
MLA Liu,QS,et al."Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet".Science Advances 3.3(2017):e1600762.

入库方式: OAI收割

来源:地球环境研究所

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