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DOI10.1016/j.quaint.2022.10.013
Late glacial and Holocene climate in the Kunlun Pass region (northern Tibetan Plateau) inferred from a multi-proxy lake record
Zhang, Wanyi; Mischke, Steffen; Hosner, Dominic; Zhang, Chengjun; Plessen, Birgit; Li, Huwei; Zhang, Xiaojing
发表日期2023
ISSN1040-6182
EISSN1873-4553
起始页码46
结束页码60
卷号643
英文摘要Holocene environmental and climate change on the Tibetan Plateau is intensively studied and discussed with the aim to better understand the factors controlling the hydrology of individual river catchments and especially the availability of water which is of utmost significance for the communities downstream in times of rapid climate change. Thus, a late glacial and Holocene sediment record from Lake Heihai in the Kunlun-Pass region was investigated using ostracod and geochemical analyses. Cold and dry conditions were inferred between ca. 12.9 and 12.3 cal ka BP and higher temperatures before and afterwards. The cold spell probably corresponds to the Younger Dryas (YD) event in the North Atlantic region. Warmer and wetter conditions with highest lake levels and decreased lake-water salinity were recorded from ca. 10.8 to 7.0 cal ka BP when the summer monsoon was strengthened. The cold 8.2 cal ka BP event is not significantly recorded in the region probably due to the pre-dominance of the summer monsoon over the westerlies. A declined lake level and increased lake-water salinity as the result of cold and dry conditions are inferred from ca. 7.0 to 4.5 cal ka BP when the strengthening of the mid -latitude westerly circulation probably triggered glacier advances in the catchment. An even lower lake level existed during cold conditions with glacier advances from ca. 4.5 to 1.2 cal ka BP. The level of Lake Heihai rose again after ca. 1.2 cal ka BP due to warmer conditions, causing the retreat of glaciers and higher runoff. Our record from the Kunlun Pass region provides further evidence for the catchment-specific response of hydro -graphical systems which are partly controlled by glaciers as major water sources.
关键词Central AsiaSummer monsoonGranulometryGeochemistryOstracoda
英文关键词MOUNTAINS NW CHINA; OXYGEN-ISOTOPE RECORD; BASIN WESTERN TIBET; OSTRACOD ASSEMBLAGES; ENVIRONMENTAL-CHANGES; QAIDAM BASIN; WATER-DEPTH; ICE-CORE; PALEOCLIMATIC CHANGES; SPATIAL-DISTRIBUTION
WOS研究方向Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000963127200001
来源期刊QUATERNARY INTERNATIONAL
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/283896
作者单位Lanzhou University; Lanzhou University; University of Iceland; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences
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GB/T 7714
Zhang, Wanyi,Mischke, Steffen,Hosner, Dominic,et al. Late glacial and Holocene climate in the Kunlun Pass region (northern Tibetan Plateau) inferred from a multi-proxy lake record[J],2023,643.
APA Zhang, Wanyi.,Mischke, Steffen.,Hosner, Dominic.,Zhang, Chengjun.,Plessen, Birgit.,...&Zhang, Xiaojing.(2023).Late glacial and Holocene climate in the Kunlun Pass region (northern Tibetan Plateau) inferred from a multi-proxy lake record.QUATERNARY INTERNATIONAL,643.
MLA Zhang, Wanyi,et al."Late glacial and Holocene climate in the Kunlun Pass region (northern Tibetan Plateau) inferred from a multi-proxy lake record".QUATERNARY INTERNATIONAL 643(2023).
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