中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Long-term drying trends since the mid-Holocene in the Qaidam Basin

文献类型:期刊论文

作者Zhang, Ting2; Wang, Gen2,4; Wang, Yongli1; Wei, Zhifu2; He, Wei2; Ma, Xueyun2,3; Ma, He1,3; Yu, Xiaoli2,3; Zhang, Pengyuan1,3; Li, Shangkun2,3
刊名CATENA
出版日期2023-07-01
卷号228页码:14
ISSN号0341-8162
关键词GDGTs Climate change Landscape evolution Qaidam Basin Asian summer monsoon
DOI10.1016/j.catena.2023.107145
英文摘要This study was conducted to improve our understanding of climate changes and landscape evolution in the transitional area between the westerly-dominated regions and monsoonal regions, with the aim of contributing to solving the increasing debate over the "westerlies model" or "monsoon model" in the northeastern Tibetan Plateau. This research mainly focuses on glycerol dialkyl glycerol tetraethers (GDGTs) in a well-dated sediment core that covers the last similar to 14.1 ka from Hurleg Lake in the Qaidam Basin, combined with grain size and organic element characteristics, to explore the climate and landscape evolution under the influence of potential forcing. Based on the variations in core sedimentary facies and careful calibrations selection, this study reveals that Hurleg Lake experienced a warm-dry climate in the last deglaciation (14.1-11.2 cal ka BP), a cold-wet climate in the early Holocene (11.2-9.3 cal ka BP), a warm-wet climate in the mid-Holocene (9.3-3.5 cal ka BP), and a cool-dry climate in the late Holocene (after 3.5 cal ka BP). Our study suggests that the moisture evolution in the Hurleg Lake area was controlled by the Asian summer monsoon (ASM) and exhibits a typical "monsoon model", and the modern climate is drier than that in the mid-Holocene. The weakening of ASM since the mid-Holocene has caused the ASM boundary to retreat southeastward to the modern one. Therefore, long-term declines in temperature and precipitation may lead to vegetation deterioration, glacier advancement, and aeolian activity exacerbation, which in turn influence regional ecological landscape.
WOS关键词DIALKYL GLYCEROL TETRAETHERS ; ARID CENTRAL-ASIA ; TIBETAN PLATEAU IMPLICATIONS ; HOLOCENE MOISTURE EVOLUTION ; MEMBRANE-LIPIDS ; CLIMATIC-CHANGE ; LAKE QINGHAI ; PALEOENVIRONMENTAL CHANGES ; TEMPERATURE CALIBRATION ; ENVIRONMENTAL CONTROLS
资助项目National Natural Science Foundation of China[41831176] ; National Natural Science Foundation of China[42102195] ; National Natural Science Foundation of China[41902028] ; National Natural Science Foundation of China[41972030] ; National Natural Science Foundation of China[42072038] ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program[2019QZKK0707] ; China Postdoctoral Science Foundation ; National Key R&D Program of China[2021425] ; Youth Innovation Promotion Association CAS[2021 M703464] ; [2022YFF0800800]
WOS研究方向Geology ; Agriculture ; Water Resources
语种英语
出版者ELSEVIER
WOS记录号WOS:000986953700001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS
源URL[http://ir.iggcas.ac.cn/handle/132A11/110918]  
专题地质与地球物理研究所_兰州油气中心
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Wang, Gen; Wang, Yongli
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, CAS Ctr Excellence Life & Paleoenvironm, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Northwest Inst Eco Environm & Resources, Key Lab Petr Resources Res, Lanzhou 730000, Gansu, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Northwest Inst Eco Environm & Resources, 382 Donggang St, Lanzhou 730000, GS, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Ting,Wang, Gen,Wang, Yongli,et al. Long-term drying trends since the mid-Holocene in the Qaidam Basin[J]. CATENA,2023,228:14.
APA Zhang, Ting.,Wang, Gen.,Wang, Yongli.,Wei, Zhifu.,He, Wei.,...&Li, Lun.(2023).Long-term drying trends since the mid-Holocene in the Qaidam Basin.CATENA,228,14.
MLA Zhang, Ting,et al."Long-term drying trends since the mid-Holocene in the Qaidam Basin".CATENA 228(2023):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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