中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Increased dust deposition in the Parece Vela Basin since the mid- Pleistocene inferred from radiogenic Sr and Nd isotopes

文献类型:期刊论文

作者Jiang, Fuqing1,2; Zhu, Xiao1,3; Li, Tiegang2,4; Zhou, Yu5; Xiong, Zhifang2,4; Feng, Xuguang1,3; Yin, Xuebo1; Li, Anchun1
刊名GLOBAL AND PLANETARY CHANGE
出版日期2019-02-01
卷号173页码:83-95
关键词Asian dust Sr and Nd isotopes Parece Vela Basin Mid-Pleistocene transition
ISSN号0921-8181
DOI10.1016/j.gloplacha.2018.12.011
通讯作者Jiang, Fuqing(fqjiang@qdio.ac.cn)
英文摘要Eolian dust deposition is crucial to paleoclimate reconstructions of dust source areas and may have played an important role in the climate during the mid-Pleistocene transition (MPT). Here, we present the radiogenic Sr and Nd isotopic composition and excess barium (Ba-xs) of a sediment core that was recovered from the Parece Vela Basin (PVB) in the northwestern Pacific. The new record indicates that these detrital sediments are primarily composed of dust from western and central Chinese deserts and volcanic materials from the islands in and around the PVB. A two end-member Sr isotope model was applied to distinguish Asian dust from volcanic materials and to reconstruct the mass accumulation rates (MARs) of dust over the last 2.1 Myr. Starting at similar to 1.2 Myr, the dust MARs doubled relative to those in the Early Pleistocene, which was coupled with the frequent congruence of minimum eccentricity and low obliquity. We argue that the congruent minimum eccentricity and low obliquity may have triggered the climate change before and during the MPT and resulted in the aridity of East Asia and increased dust input. The coupling of dust MAR, Ba-xs, MAR and atmospheric CO2 concentration and their rapid increase since the MPT strongly suggest that the internal positive feedback of dust input might be another mechanism behind dust input to the PVB since the MPT.
资助项目National Natural Science Foundation of China[41776065] ; National Natural Science Foundation of China[41576050] ; National Natural Science Foundation of China[41230959] ; National Natural Science Foundation of China[41576051] ; National Program on Global Change and Air-Sea Interaction[GASI-GEOGE-02] ; National Program on Global Change and Air-Sea Interaction[GASI-GEOGE-04] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11030302] ; Qingdao National Laboratory for Marine Science and Technology[QNLM2016ORP0205]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000457512400009
出版者ELSEVIER SCIENCE BV
源URL[http://ir.qdio.ac.cn/handle/337002/160894]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Jiang, Fuqing
作者单位1.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China
3.Univ Chinese Acad Sci, Beijing, Peoples R China
4.State Ocean Adm, Key Lab Marine Sedimentol & Environm Geol, Inst Oceanog 1, Qingdao 266061, Peoples R China
5.Sichuan Inst Geol Engn Invest, Chengdu 610072, Sichuan, Peoples R China
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Jiang, Fuqing,Zhu, Xiao,Li, Tiegang,et al. Increased dust deposition in the Parece Vela Basin since the mid- Pleistocene inferred from radiogenic Sr and Nd isotopes[J]. GLOBAL AND PLANETARY CHANGE,2019,173:83-95.
APA Jiang, Fuqing.,Zhu, Xiao.,Li, Tiegang.,Zhou, Yu.,Xiong, Zhifang.,...&Li, Anchun.(2019).Increased dust deposition in the Parece Vela Basin since the mid- Pleistocene inferred from radiogenic Sr and Nd isotopes.GLOBAL AND PLANETARY CHANGE,173,83-95.
MLA Jiang, Fuqing,et al."Increased dust deposition in the Parece Vela Basin since the mid- Pleistocene inferred from radiogenic Sr and Nd isotopes".GLOBAL AND PLANETARY CHANGE 173(2019):83-95.

入库方式: OAI收割

来源:海洋研究所

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