Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1017/qua.2019.27 |
Late Quaternary lake-level and climate changes in arid central Asia inferred from sediments of Ebinur Lake, Xinjiang, northwestern China | |
Zhou, Jianchao1,3; Wu, Jinglu1,2; Ma, Long4; Qiang, Mingrui5 | |
通讯作者 | Wu, Jinglu |
来源期刊 | QUATERNARY RESEARCH
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ISSN | 0033-5894 |
EISSN | 1096-0287 |
出版年 | 2019 |
卷号 | 92期号:2页码:416-429 |
英文摘要 | Arid central Asia plays an important role in global climate dynamics, but large uncertainties remain in our understanding of the region's hydroclimate variability during the Late Quaternary. Here we present a new, high-resolution record of lacustrine sediment grain-size and element chemistry from Ebinur Lake, which was used to infer lake conditions and related climate changes in the study region between ca. 39.2 and 3.6 ka. End-member modeling analysis of grain-size data and PCA of elemental data show that lake level fluctuated dramatically from 39.2 to 34.0 ka. Subsequently, Ebinur Lake experienced a high stand from 34.0 to 28.0 ka, under humid climate conditions. The subsequent period, from 28.0 to 12.0 ka, was characterized by lake regression under dry climate conditions, whereas afterward (12.0-3.6 ka), considerably higher lake levels and humid conditions again prevailed. Millennial-scale abrupt climate changes, such as Heinrich events (H3 and H1) and the Younger Dryas, which are documented in the North Atlantic region, are also detected in the sediment record from Ebinur Lake. Comparisons with other sediment records from arid central Asia generally support the claim that climate change in this region was influenced mainly by variations in North Atlantic sea surface temperatures, through the westerlies. |
英文关键词 | Lake level Climate change Arid central Asia Grain size Elemental composition Ebinur Lake |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | SCI-E |
WOS记录号 | WOS:000487316500011 |
WOS关键词 | LACUSTRINE RECORD ; TIBETAN PLATEAU ; WESTERN CHINA ; GRAIN-SIZE ; NORTHERN XINJIANG ; EVENTS ; PLEISTOCENE ; MOUNTAINS ; EVOLUTION ; HISTORY |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
来源机构 | 中国科学院新疆生态与地理研究所 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/218260 |
作者单位 | 1.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China; 2.Chinese Acad Sci, Res Ctr Ecol & Environm Cent Asia, Urumqi 830011, Peoples R China; 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China; 4.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Peoples R China; 5.South China Normal Univ, Sch Geog, Guangzhou 510631, Guangdong, Peoples R China |
推荐引用方式 GB/T 7714 | Zhou, Jianchao,Wu, Jinglu,Ma, Long,et al. Late Quaternary lake-level and climate changes in arid central Asia inferred from sediments of Ebinur Lake, Xinjiang, northwestern China[J]. 中国科学院新疆生态与地理研究所,2019,92(2):416-429. |
APA | Zhou, Jianchao,Wu, Jinglu,Ma, Long,&Qiang, Mingrui.(2019).Late Quaternary lake-level and climate changes in arid central Asia inferred from sediments of Ebinur Lake, Xinjiang, northwestern China.QUATERNARY RESEARCH,92(2),416-429. |
MLA | Zhou, Jianchao,et al."Late Quaternary lake-level and climate changes in arid central Asia inferred from sediments of Ebinur Lake, Xinjiang, northwestern China".QUATERNARY RESEARCH 92.2(2019):416-429. |
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