中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Tectonic and climatic controls on long-term silicate weathering in Asia since 5 Ma

文献类型:期刊论文

作者Wan, Shiming1; Clift, Peter D.2; Li, Anchun1; Yu, Zhaojie1; Li, Tiegang1; Hu, Dengke3
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2012-08-15
卷号39页码:L15611
关键词SOUTH CHINA SEA SUMMER MONSOON EROSION RATES HISTORY RECORD EVOLUTION SEDIMENT FEEDBACK CYCLE
ISSN号0094-8276
通讯作者Wan, SM (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China.
英文摘要Determining the interplay between tectonic deformation, climate, atmospheric CO2 concentrations and continental weathering and erosion is key to understanding the mechanisms that forced Cenozoic global cooling. In contrast with studies of paleo-climate and pCO(2), the history of long-term silicate weathering in the Himalaya and Tibetan Plateau (HTP) during the late Cenozoic remains unclear. We reconstruct 5 m.y. of silicate sedimentary records at Ocean Drilling Program (ODP) Site 1143 in the South China Sea to explore the weathering history of the Mekong River basin that supplied the sediment. Coherent variation of weathering proxies from the South China Sea, Bay of Bengal, Loess Plateau, as well as the Yangtze and Yellow Rivers, indicates weakening chemical weathering intensity since the late Pliocene, as the climate cooled. This cooling, coupled with tectonic activity, shifted the dominant weathering regime from more transport-limited to more weathering-limited, causing less chemical depletion of silicate minerals. While silicate weathering rates became strongly correlated to erosion rates, they were decoupled from chemical weathering intensity. Physical denudation and associated silicate weathering rates in the HTP area increased in the Pliocene, driven by both rock uplift and stronger monsoon precipitation, decreasing atmospheric CO2 concentrations, and so contributing to Northern Hemisphere Glaciation (NHG). Citation: Wan, S., P. D. Clift, A. Li, Z. Yu, T. Li, and D. Hu (2012), Tectonic and climatic controls on long-term silicate weathering in Asia since 5 Ma, Geophys. Res. Lett., 39, L15611, doi:10.1029/2012GL052377.
学科主题Geosciences, Multidisciplinary
收录类别SCI
原文出处10.1029/2012GL052377
语种英语
WOS记录号WOS:000307742200003
公开日期2013-09-24
源URL[http://ir.qdio.ac.cn/handle/337002/12518]  
专题海洋研究所_海洋地质与环境重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA
3.Univ Aberdeen, Sch Geosci, Aberdeen, Scotland
推荐引用方式
GB/T 7714
Wan, Shiming,Clift, Peter D.,Li, Anchun,et al. Tectonic and climatic controls on long-term silicate weathering in Asia since 5 Ma[J]. GEOPHYSICAL RESEARCH LETTERS,2012,39:L15611.
APA Wan, Shiming,Clift, Peter D.,Li, Anchun,Yu, Zhaojie,Li, Tiegang,&Hu, Dengke.(2012).Tectonic and climatic controls on long-term silicate weathering in Asia since 5 Ma.GEOPHYSICAL RESEARCH LETTERS,39,L15611.
MLA Wan, Shiming,et al."Tectonic and climatic controls on long-term silicate weathering in Asia since 5 Ma".GEOPHYSICAL RESEARCH LETTERS 39(2012):L15611.

入库方式: OAI收割

来源:海洋研究所

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