气候变化领域集成服务门户(CCPortal): Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial

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DOI	10.1007/s10933-017-9976-9
	Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial
	Hou, Juzhi; Tian, Qian; Liang, Jie; Wang, Mingda; He, Yue
通讯作者	Hou, JZ (通讯作者)
发表日期	2017
ISSN	0921-2728
EISSN	1573-0417
起始页码	257
结束页码	273
卷号	58 期号:2
英文摘要	The numerous and widespread lakes of the Tibetan Plateau (TP) constitute the largest group of alpine lakes on Earth. Some of the lakes are fed mainly by glacier meltwater and others by precipitation and groundwater. Past changes in the environments of these lakes differed because of differences in lake hydrological regimes and the complex pattern of climate change on the TP. Here we present records of scanning XRF, inorganic carbon (IC) concentration n-alkanoic acid average chain length (ACL) and percent aquatic inputs (Paq) in sediment cores from two non-glaciated lakes on the central TP (Dagze Co and Jiang Co), which span the past 19,000 years. We used these measures to investigate past changes in catchment hydrology, climate and environment. Variations in the concentration of Ti and other lithogenic elements at the two sites were influenced mainly by surface runoff, which is supported by the variation of IC, Ca/(Al, Ti, Fe) (reflecting authigenic carbonate precipitation), Rb/Sr (a chemical weathering proxy), and ACL and Paq. We attribute variations in surface runoff to changes in the precipitation/evaporation ratio, caused by the pattern of climate change on the central TP since the late Pleistocene. During the late Pleistocene, stronger runoff (indicated by higher Ti, higher Rb/Sr and Paq, lower IC, Ca/(Al, Ti, Fe) and ACL) likely resulted from lower temperatures. Lower runoff during the Holocene may reflect intensified evaporation caused by higher temperatures. Comparison with records from glaciated lakes in the region reveals opposite trends in catchment hydrology. Overall, our results suggest that since the late Pleistocene the central TP was influenced mainly by the Indian Summer Monsoon.
关键词	INTERTROPICAL CONVERGENCE ZONE NORTH-ATLANTIC CLIMATE N-ALKANE DISTRIBUTIONS ASIAN MONSOON LEAF WAX MOISTURE AVAILABILITY EARLY HOLOCENE CHINA QINGHAI RECORDS
英文关键词	Tibetan Plateau; Dagze Co; Jiang Co; XRF; Monsoon
语种	英语
WOS研究方向	Environmental Sciences & Ecology ; Geology ; Marine & Freshwater Biology
WOS类目	Environmental Sciences ; Geosciences, Multidisciplinary ; Limnology
WOS记录号	WOS:000404687500010
来源期刊	JOURNAL OF PALEOLIMNOLOGY
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/258954
推荐引用方式 GB/T 7714	Hou, Juzhi,Tian, Qian,Liang, Jie,et al. Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial[J]. 中国科学院青藏高原研究所,2017,58(2).
APA	Hou, Juzhi,Tian, Qian,Liang, Jie,Wang, Mingda,&He, Yue.(2017).Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial.JOURNAL OF PALEOLIMNOLOGY,58(2).
MLA	Hou, Juzhi,et al."Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial".JOURNAL OF PALEOLIMNOLOGY 58.2(2017).