IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2010~)
Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition
Li, Tao1; Liu, Fei2,3; Abels, Hemmo A.4; You, Chen-Fen5; Zhang, Zeke1,6; Chen, Jun1; Ji, Junfeng1; Li, Laifeng1; Li, Le1; Liu, Hou-Chun5; Ren, Chao1; Xia, Renyuan1; Zhao, Liang1; Zhang, Wenfang1; Li, Gaojun1
2017
Source PublicationEARTH AND PLANETARY SCIENCE LETTERS
Volume457Issue:2017Pages:181-190
SubtypeArticle
AbstractRecords from natural archives show that the strength of the East Asian summer monsoon (EASM) strongly depends on the orbital configuration of the Earth. However, the dominant orbital cycles driving EASM have been found to be spatially different. Speleothem stable oxygen isotopic records from southern China, which are believed to reflect large-scale changes in the Asian monsoon system, are dominated by climatic precession cycles. Further north, on the Chinese Loess Plateau (CLP), loess-and-paleosol sequences, which are argued to be controlled by monsoon intensity, are in pace with global ice volume changes dominated by obliquity, and after the mid-Pleistocene transition by 100-kyr cycles. To understand these critical discrepancies, here we apply a novel proxy based on the trace metal compositions of pedogenic carbonate in the eolian deposits on the CLP to reconstruct summer precipitation over the last 1.5 million years. Our reconstructions show that summer precipitation on the CLP is dominantly forced by obliquity not in pace with the ice-volume-imprinted loess-paleosol sequences before and after the mid-Pleistocene transition or with the precession-paced speleothem oxygen isotopic records. Coupled with climate model results, we suggest that the obliquity-driven variations of summer precipitation may originate from the gradient of boreal insolation that modulates the thermal contrast between the Asian continent and surrounding oceans. (C) 2016 Elsevier B.V. All rights reserved.
KeywordMicrocodium Monsoon Dynamics Milankovitch Cycles Climate Change Soil Carbonate
WOS HeadingsScience & Technology ; Physical Sciences
DOI10.1016/j.epsl.2016.09.045
WOS KeywordCHINESE LOESS PLATEAU ; ICE-AGE TERMINATIONS ; MONSOON PRECIPITATION ; PALEOSOL SEQUENCES ; PALEOCLIMATIC SIGNIFICANCE ; ISOTOPE FRACTIONATION ; INORGANIC CALCITE ; RECORDS ; CLIMATE ; TEMPERATURE
Indexed BySCI
Language英语
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics
WOS IDWOS:000389398000017
Citation statistics
Cited Times:9[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/5563
Collection黄土与第四纪地质国家重点实验室(2010~)
Affiliation1.Nanjing Univ, Dept Earth Sci, MOE Key Lab Surficial Geochem, 163 Xianlindadao, Nanjing 210023, Jiangsu, Peoples R China
2.Nanjing Univ Informat Sci & Technol, Earth Syst Modeling Ctr, 219 Ninglu Rd, Nanjing 210044, Jiangsu, Peoples R China
3.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, 219 Ninglu Rd, Nanjing 210044, Jiangsu, Peoples R China
4.Delft Univ Technol, Dept Geosci & Engn, Stevinweg 1, NL-2628 CN Delft, Netherlands
5.Natl Cheng Kung Univ, Earth Dynam Syst Res Ctr, Tainan 70101, Taiwan
6.Chinese Acad Sci, Inst Earth Environm, Xian 710075, Peoples R China
Recommended Citation
GB/T 7714
Li, Tao,Liu, Fei,Abels, Hemmo A.,et al. Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition[J]. EARTH AND PLANETARY SCIENCE LETTERS,2017,457(2017):181-190.
APA Li, Tao.,Liu, Fei.,Abels, Hemmo A..,You, Chen-Fen.,Zhang, Zeke.,...&Li, Gaojun.(2017).Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition.EARTH AND PLANETARY SCIENCE LETTERS,457(2017),181-190.
MLA Li, Tao,et al."Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition".EARTH AND PLANETARY SCIENCE LETTERS 457.2017(2017):181-190.
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