Arid
DOI10.1016/j.gloplacha.2021.103707
Controls of precipitation and vegetation variability on the NE Tibetan Plateau during the late Pliocene warmth (similar to 3.5-3.0 Ma)
Schwarz, Florian; Salzmann, Ulrich; Koutsodendris, Andreas; Nie, Junsheng; Friedrich, Oliver; Ni, Jian; Garzione, Carmala; Fang, Xiaomin; Wu, Fuli; Woodward, John; Appel, Erwin; Pross, Joerg
通讯作者Salzmann, U (corresponding author),Northumbria Univ, Dept Geog & Environm Sci, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England.
来源期刊GLOBAL AND PLANETARY CHANGE
ISSN0921-8181
EISSN1872-6364
出版年2022
卷号208
英文摘要To better understand precipitation variability in a warmer-than-present world with elevated atmospheric CO2 concentrations, this study presents high-resolution palynological and element geochemical analyses of a late Pliocene drill core (3.5-3.0 Ma) from the today hyperarid Qaidam Basin on the north-eastern Tibetan Plateau. Quantitative rainfall estimates based on modern pollen-climate transfer functions indicate a 10-fold higher annual rainfall during the mid-Piacenzian Warm Period (mPWP; 3.264-3.025 Ma) than today, with values of 300-400 mm/a. Throughout the late Pliocene, the Qaidam Basin was covered with a temperate semi-desert shrubland. Varying percentages of the local lakeshore vegetation and long-distance arboreal pollen, as well as fluctuations in carbonate-silicate geochemistry, indicate a highly variable rainfall. Our study suggests that precipitation in the northern Qaidam Basin was primarily controlled by an East Asian Monsoon system (EAMS) that was located further north than today. Spectral analysis of the Artemisia/Chenopodiaceae (A/C) pollen ratio indicates an orbitally controlled cyclicity with a strong link between moisture availability and insolation forcing. A decline in precipitation before the end of the mPWP at ca. 3.15 Ma is likely to be linked to cooling in the North Atlantic and initial Northern Hemisphere ice-sheet build-up. Our study identifies NH insolation and ice-sheet advances as major controls of the late Pliocene variability and strength of the EAMS in semi-arid NW-China.
英文关键词Piacenzian Tibetan Plateau East Asian Monsoon Palynology XRF Qaidam Basin
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000740442500002
WOS关键词WESTERN QAIDAM BASIN ; COEXISTENCE APPROACH ; ASTRONOMICAL TIMESCALE ; BIOME DISTRIBUTION ; NORTHERN CHINA ; CLIMATE-CHANGE ; CENTRAL-ASIA ; TARIM BASIN ; ICE-SHEET ; POLLEN
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/2XILL650/376946
作者单位[Schwarz, Florian; Salzmann, Ulrich; Woodward, John] Northumbria Univ, Dept Geog & Environm Sci, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England; [Koutsodendris, Andreas; Friedrich, Oliver; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Nie, Junsheng] Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Lanzhou 73000, Peoples R China; [Ni, Jian] Zhejiang Normal Univ, Coll Chem & Life Sci, Jinhua 321004, Zhejiang, Peoples R China; [Garzione, Carmala] Univ Rochester, Dept Earth & Environm Sci, Rochester, NY 14627 USA; [Fang, Xiaomin; Wu, Fuli] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100085, Peoples R China; [Fang, Xiaomin; Wu, Fuli] CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100085, Peoples R China; [Appel, Erwin] Univ Tubingen, Ctr Appl Geosci, Dept Geosci, Holderlinstr 12, D-72074 Tubingen, Germany
推荐引用方式
GB/T 7714
Schwarz, Florian,Salzmann, Ulrich,Koutsodendris, Andreas,et al. Controls of precipitation and vegetation variability on the NE Tibetan Plateau during the late Pliocene warmth (similar to 3.5-3.0 Ma)[J],2022,208.
APA Schwarz, Florian.,Salzmann, Ulrich.,Koutsodendris, Andreas.,Nie, Junsheng.,Friedrich, Oliver.,...&Pross, Joerg.(2022).Controls of precipitation and vegetation variability on the NE Tibetan Plateau during the late Pliocene warmth (similar to 3.5-3.0 Ma).GLOBAL AND PLANETARY CHANGE,208.
MLA Schwarz, Florian,et al."Controls of precipitation and vegetation variability on the NE Tibetan Plateau during the late Pliocene warmth (similar to 3.5-3.0 Ma)".GLOBAL AND PLANETARY CHANGE 208(2022).
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