中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Alkenone-based temperature and climate reconstruction during the last deglaciation at Lake Dangxiong Co, southwestern Tibetan Plateau

文献类型:期刊论文

作者Ling, Yuan1,2; Sun, Qing3; Zheng, Mianping1; Wang, Hailei1; Luo, Yangbing1; Dai, Xinqin4; Xie, Manman3; Zhu, Qingzeng5
刊名QUATERNARY INTERNATIONAL
出版日期2017-07-10
卷号443页码:58-69
关键词Alkenone Alkane Temperature Last deglaciation Dangxiong Co Tibetan Plateau
ISSN号1040-6182
DOI10.1016/j.quaint.2016.07.036
文献子类Article
英文摘要The climate of the Tibetan Plateau is influenced by the monsoons and the Westerlies due to land-sea thermal contrasts. However, few quantitative temperature reconstructions have been made for the region, and this hinders our ability to validate climate models and to understand the coupling process between monsoon, ocean and ice sheets through time. Here we report a quantitative temperature reconstruction for the last deglaciation from a terrace of Lake Dangxiong Co in the southwestern Tibetan Plateau. Based on the unsaturation index of long-chain alkenones, the reconstructed mean annual air temperature during the late Last Glacial Maximum was about 0.2 degrees C, while the Bolling/Allerod (B/A) period was characterized by a rapid increase in temperature from 0.8 degrees C to 2.4 degrees C, (2.9) followed by an abrupt decrease in temperature to -0.9 degrees C in the early Younger Dryas (YD). The alkenones and n-alkanes record indicates that Dangxiong Co experienced a cold and wet climate in the early part of the last deglaciation after the Last Glacial Maximum, a warm-dry B/A, and a cold and dry YD. Our temperature reconstruction confirms that the thermal and dynamical effects of the Tibetan Plateau are one of the main elements contributing to abrupt changes in the Indian Summer Monsoon. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.
WOS关键词LONG-CHAIN-ALKENONES ; OCEAN SUMMER MONSOON ; HOLOCENE CLIMATE ; ASIAN MONSOON ; NAM-CO ; N-ALKANES ; ICE CORES ; ENVIRONMENTAL-CHANGES ; INDIAN MONSOON ; WESTERN TIBET
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000406753900006
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Science Foundation of China(U1407007) ; Geological Survey Project of China(12120114048501) ; National Science Foundation of China(U1407007) ; Geological Survey Project of China(12120114048501) ; National Science Foundation of China(U1407007) ; Geological Survey Project of China(12120114048501) ; National Science Foundation of China(U1407007) ; Geological Survey Project of China(12120114048501)
源URL[http://ir.iggcas.ac.cn/handle/132A11/61843]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Zheng, Mianping
作者单位1.Chinese Acad Geol Sci, Inst Mineral Resources, 26 Baiwanzhuang St, Beijing 100037, Peoples R China
2.China Univ Geosci, Fac Earth Resources, Wuhan 430074, Hubei, Peoples R China
3.Natl Res Ctr Geoanal, Beijing 100037, Peoples R China
4.China Univ Min & Technol, Coll Geosci & Surveying Engn, Beijing 100083, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
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Ling, Yuan,Sun, Qing,Zheng, Mianping,et al. Alkenone-based temperature and climate reconstruction during the last deglaciation at Lake Dangxiong Co, southwestern Tibetan Plateau[J]. QUATERNARY INTERNATIONAL,2017,443:58-69.
APA Ling, Yuan.,Sun, Qing.,Zheng, Mianping.,Wang, Hailei.,Luo, Yangbing.,...&Zhu, Qingzeng.(2017).Alkenone-based temperature and climate reconstruction during the last deglaciation at Lake Dangxiong Co, southwestern Tibetan Plateau.QUATERNARY INTERNATIONAL,443,58-69.
MLA Ling, Yuan,et al."Alkenone-based temperature and climate reconstruction during the last deglaciation at Lake Dangxiong Co, southwestern Tibetan Plateau".QUATERNARY INTERNATIONAL 443(2017):58-69.

入库方式: OAI收割

来源:地质与地球物理研究所

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