干旱区生态环境知识资源中心(Arid): Increased dust deposition in the Parece Vela Basin since the mid- Pleistocene inferred from radiogenic Sr and Nd isotopes

Arid

DOI	10.1016/j.gloplacha.2018.12.011
	Increased dust deposition in the Parece Vela Basin since the mid- Pleistocene inferred from radiogenic Sr and Nd isotopes
	Jiang, Fuqing 1,2; Zhu, Xiao 1,3; Li, Tiegang 2,4; Zhou, Yu 5; Xiong, Zhifang 2,4; Feng, Xuguang 1,3; Yin, Xuebo 1; Li, Anchun 1
通讯作者	Jiang, Fuqing
来源期刊	GLOBAL AND PLANETARY CHANGE
ISSN	0921-8181
EISSN	1872-6364
出版年	2019
卷号	173 页码:83-95
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.
英文关键词	Asian dust Sr and Nd isotopes Parece Vela Basin Mid-Pleistocene transition
类型	Article
语种	英语
国家	Peoples R China
收录类别	SCI-E
WOS记录号	WOS:000457512400009
WOS关键词	TIBETAN PLATEAU UPLIFT ; MARIANA TROUGH BASALTS ; WESTERN PHILIPPINE SEA ; CHINESE LOESS PLATEAU ; LAMINATED DIATOM MATS ; NORTH PACIFIC ; DEEP-SEA ; TRACE-ELEMENT ; GRAIN-SIZE ; SUBDUCTION COMPONENTS
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向	Physical Geography ; Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/216063
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
推荐引用方式 GB/T 7714	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],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.