IEECAS OpenIR  > 加速器质谱中心
Grain size of Lake Qinghai sediments: Implications for riverine input and Holocene monsoon variability
Liu, Xingxing1,2; Vandenberghe, Jef3; An, Zhisheng1; Li, Ying1; Jin, Zhangdong1; Dong, Jibao1; Sun, Youbin1
2016-05-01
Source PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
Volume449Issue:2016Pages:41-51
SubtypeArticle
AbstractGrain-size compositions of lake sediments can provide direct information on changes in transporting mechanism and sedimentary environment. Various grain-size parameters have been employed to reconstruct hydrological conditions within the lake and dust influx from outside the lake. Here we present the grain-size results of a 5-m core retrieved from Lake Qinghai, northeastern Tibetan Plateau in order to address the links between Holocene depositional process and climatic change. Our results indicate that two parameters (skewness and grain-size ratio of 8-50/2-8 mu m) are sensitive to hydrodynamic changes in Lake Qinghai, which are further linked to the strength of the Asian summer monsoon. Variations of these two parameters reveal that summer monsoon intensity weakened gradually from early to late Holocene, superimposed by persistent centennial variability with dominant periods at 0.35, 0.23 and 0.12 kyr. Comparison of grain-size variations with solar activities and North Atlantic cooling events reveals that solar forcing likely plays an important role in driving centennial monsoon variability. (C) 2016 Elsevier B.V. All rights reserved.
KeywordLake Qinghai Grain Size Holocene Asian Summer Monsoon Solar Activities
WOS HeadingsScience & Technology ; Physical Sciences ; Life Sciences & Biomedicine
DOI10.1016/j.palaeo.2016.02.005
WOS KeywordNE TIBETAN PLATEAU ; NORTH-ATLANTIC CLIMATE ; OXYGEN-ISOTOPE RECORD ; ASIAN SUMMER MONSOON ; HIGH-RESOLUTION ; CENTRAL CHINA ; ATMOSPHERIC CIRCULATION ; LATEST PLEISTOCENE ; QUATERNARY CLIMATE ; CARBON ISOTOPES
Indexed BySCI
Language英语
WOS Research AreaPhysical Geography ; Geology ; Paleontology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS IDWOS:000374364400004
Citation statistics
Cited Times:29[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/5784
Collection加速器质谱中心
Affiliation1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
3.Vrije Univ Amsterdam, Inst Earth Sci, De Boelelaan 1085, NL-1081 HV Amsterdam, Netherlands
Recommended Citation
GB/T 7714
Liu, Xingxing,Vandenberghe, Jef,An, Zhisheng,et al. Grain size of Lake Qinghai sediments: Implications for riverine input and Holocene monsoon variability[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2016,449(2016):41-51.
APA Liu, Xingxing.,Vandenberghe, Jef.,An, Zhisheng.,Li, Ying.,Jin, Zhangdong.,...&Sun, Youbin.(2016).Grain size of Lake Qinghai sediments: Implications for riverine input and Holocene monsoon variability.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,449(2016),41-51.
MLA Liu, Xingxing,et al."Grain size of Lake Qinghai sediments: Implications for riverine input and Holocene monsoon variability".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 449.2016(2016):41-51.
Files in This Item:
File Name/Size DocType Version Access License
Grain size of Lake Q(2182KB)期刊论文出版稿开放获取CC BY-NC-SAApplication Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Liu, Xingxing]'s Articles
[Vandenberghe, Jef]'s Articles
[An, Zhisheng]'s Articles
Baidu academic
Similar articles in Baidu academic
[Liu, Xingxing]'s Articles
[Vandenberghe, Jef]'s Articles
[An, Zhisheng]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Liu, Xingxing]'s Articles
[Vandenberghe, Jef]'s Articles
[An, Zhisheng]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.