Holocene climate controls on water isotopic variations on the northeastern Tibetan Plateau
文献类型：期刊论文
| 作者 | Liu, Weiguo1; Ito, Emi4; Zhao, Yan2,3; Yu, Zicheng8; Wang, Huanye1; Liu, Zhonghui6; Zhao, Cheng6,7,8; He, Yuxin5,6 |
| 刊名 | CHEMICAL GEOLOGY
 |
| 出版日期 | 2016-11-15 |
| 卷号 | 440期号:2016页码:239-247 |
| 关键词 | Hydrogen Isotopes Water Isotopes Leaf Wax Lake Sediments Tibetan Plateau Holocene |
| DOI | 10.1016/j.chemgeo.2016.07.024 |
| 文献子类 | Article |
| 英文摘要 | On the Tibetan Plateau, applications of delta D and delta O-18 values in paleoclimate studies tend to be complicated due to multiple processes influencing isotopic compositions in paleoclimatic archives. In this study, isotopic compositions of modern waters in the eastern Qaidam Basin on the northeastern Tibetan Plateau, and delta D values of n-fatty acids (n-FA delta D) from a sediment core at Hurleg Lake were systematically analyzed to infer hydroclimate controls during the Holocene. The modern water isotopic results show a major contribution of snowmelt water originating from high-elevation mountains to the north of the Qaidam Basin via river and groundwater discharge, and the importance of evaporation in affecting lake water budget in this region. n-C-26 FA delta D values tend to be more negative at millennial-scale warm-dry periods during the Holocene, and vice versa, opposite to what is commonly expected. Assisted with modern water isotopic results, we infer amplified contribution of snowmelt water to the soil water around this open lake system at warm-dry periods. Meanwhile, changes in n-C-16 FA delta D values at Hurleg Lake reflect the evolution of isotopic compositions of lake water, thus we use the isotopic difference between n-C-26 and n-C-16 FA (Delta DC16-C26) to infer hydroclimate and evaporation variations in this region. Based on our data, relatively low n-C-26 FA delta D and n-C-16 FA delta D values at 10-6 cal ka BP indicate large contribution of snowmelt water into the lake during the Holocene Climate Optimum. After 6 cal ka BP, changes in evaporation became the major control on lake hydrology and led to larger fluctuations of Delta DC16-C26. Our study highlights the importance of systematic analysis on modern processes before using stable isotopes for paleoclimate reconstructions, and demonstrates that delta D difference between long-chain and short-chain n-FA might be an effective way to better understand the controlling factor of hydrological variations in a climatic complex region like the Tibetan Plateau. (C) 2016 Elsevier B.V. All rights reserved. |
| WOS关键词 | INDIVIDUAL N-ALKANES ; ARID CENTRAL-ASIA ; PLANT LEAF WAXES ; DELTA-D VALUES ; D/H RATIOS ; LACUSTRINE SEDIMENTS ; LAKE QINGHAI ; ICE-CORE ; TERRESTRIAL PLANTS ; HIGH-RESOLUTION |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000383937500019 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5661]  |
| 专题 | 地球环境研究所_加速器质谱中心 |
| 作者单位 | 1.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian, Peoples R China 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China 4.Univ Minnesota, Dept Earth Sci, Limnol Res Ctr, Minneapolis, MN USA 5.Zhejiang Univ, Sch Earth Sci, Hangzhou, Zhejiang, Peoples R China 6.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China 7.Chinese Acad Sci, State Key Lab Lake Sci & Environm, Nanjing Inst Geog & Limnol, Nanjing 210008, Jiangsu, Peoples R China 8.Lehigh Univ, Dept Earth & Environm Sci, Bethlehem, PA 18015 USA |
| 推荐引用方式 GB/T 7714 | Liu, Weiguo,Ito, Emi,Zhao, Yan,et al. Holocene climate controls on water isotopic variations on the northeastern Tibetan Plateau[J]. CHEMICAL GEOLOGY,2016,440(2016):239-247. |
| APA | Liu, Weiguo.,Ito, Emi.,Zhao, Yan.,Yu, Zicheng.,Wang, Huanye.,...&He, Yuxin.(2016).Holocene climate controls on water isotopic variations on the northeastern Tibetan Plateau.CHEMICAL GEOLOGY,440(2016),239-247. |
| MLA | Liu, Weiguo,et al."Holocene climate controls on water isotopic variations on the northeastern Tibetan Plateau".CHEMICAL GEOLOGY 440.2016(2016):239-247. |
入库方式： OAI收割
来源：地球环境研究所
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