History of moisture change derived from slope sediments of the eastern Gonghe Basin (northeastern Qinghai-Tibetan Plateau) during the last 17ka
文献类型：期刊论文
| 作者 | Liu, Bing1,2; Jin, Heling1; Sun, Liangying1; Su, Zhizhu3; Zhang, Caixia1; Zhao, Shuang2 |
| 刊名 | GEOLOGICAL JOURNAL
 |
| 出版日期 | 2017-07-01 |
| 卷号 | 52期号:4页码:583-593 |
| ISSN号 | 0072-1050 |
| 关键词 | Aeolian deposits Gonghe Basin moisture change forcing mechanism |
| DOI | 10.1002/gj.2795 |
| 通讯作者 | Jin, Heling(jinhlster@gmail.com) |
| 英文摘要 | The palaeosol-loess-aeolian sand sequence in the eastern Gonghe Basin, which is located at the convergence of the Asian summer monsoon, winter monsoon and the westerlies, reveals detailed moisture changes in the northeastern Qinghai-Tibetan Plateau (NETP) during the last 17ka. Analysis of magnetic susceptibility (MS), total organic carbon, carbonate content, grain size and geochemical parameters indicate that the region was dominated by an extremely dry climate during similar to 17.0-15.82ka, accompanying large-scale desert expansion in the last glacial maximum (LGM). Subsequently, the climate became generally dry during 15.82-14.6ka, an interval in which loess rapidly accumulated. Enhanced humidity occurred at 14.6ka, probably associated with increased strength of the East Asian summer monsoon. The region experienced slightly decreased moisture at around 6.5 and 5.8ka. After 2.7ka, the climate became wetter. This interpretation correlates with climatic records from lacustrine and aeolian deposits in the NETP during the LGM, the last deglaciation and the early-middle Holocene. High climatic moisture in the Late Holocene facilitated the formation of a well-developed palaeosol in the NETP. The effective moisture change in the Gonghe Basin is not simply ascribed to the influences of Asian summer monsoons; instead, it was possibly influenced by the interaction of evaporation and monsoonal precipitation forced by solar insolation variation. The balance between these variables was very influential on the effective moisture change in the closed inland basin of the NETP. Copyright (c) 2016 John Wiley & Sons, Ltd. |
| 收录类别 | SCI |
| WOS关键词 | HOLOCENE CLIMATIC-CHANGE ; AEOLIAN DEPOSITS ; LAKE AREA ; CHINA ; DESERT ; RECORD ; VEGETATION ; EVOLUTION |
| WOS研究方向 | Geology |
| WOS类目 | Geosciences, Multidisciplinary |
| 语种 | 英语 |
| 出版者 | WILEY |
| WOS记录号 | WOS:000405249500004 |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2557721 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Jin, Heling |
| 作者单位 | 1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou, Peoples R China 2.Lanzhou Univ, MOE Key Lab Western Chinas Environm Syst, Lanzhou, Peoples R China 3.Shanxi Univ, Sch Hist & Culture, Taiyuan, Peoples R China |
| 推荐引用方式 GB/T 7714 | Liu, Bing,Jin, Heling,Sun, Liangying,et al. History of moisture change derived from slope sediments of the eastern Gonghe Basin (northeastern Qinghai-Tibetan Plateau) during the last 17ka[J]. GEOLOGICAL JOURNAL,2017,52(4):583-593. |
| APA | Liu, Bing,Jin, Heling,Sun, Liangying,Su, Zhizhu,Zhang, Caixia,&Zhao, Shuang.(2017).History of moisture change derived from slope sediments of the eastern Gonghe Basin (northeastern Qinghai-Tibetan Plateau) during the last 17ka.GEOLOGICAL JOURNAL,52(4),583-593. |
| MLA | Liu, Bing,et al."History of moisture change derived from slope sediments of the eastern Gonghe Basin (northeastern Qinghai-Tibetan Plateau) during the last 17ka".GEOLOGICAL JOURNAL 52.4(2017):583-593. |
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