A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China
文献类型：期刊论文
| 作者 | Chen, FH; Wu, W; Holmes, JA; Madsen, DB; Zhu, Y; Jin, M; Oviatt, CG |
| 刊名 | CHINESE SCIENCE BULLETIN
 |
| 出版日期 | 2003-07-01 |
| 卷号 | 48期号:14页码:1401-1410 |
| 关键词 | western Inner Mongolian Plateau mid-Holocene lake desiccation dry climate |
| ISSN号 | 1001-6538 |
| DOI | 10.1360/03wd0245 |
| 通讯作者 | Chen, FH(fhchen@lzu.edu.cn) |
| 英文摘要 | The mid-Holocene in China is traditionally thought to be a warm and humid period with a strong summer monsoon, and is often termed the Holocene Climatic Optimum or Megathermal Period. Here we present lake geomorphologic and lithological evidence from the Alashan Plateau, part of the Mongolian Plateau, that indicates strong lake desiccation during the mid-Holocene. High resolution pollen data from Zhuyeze Lake, at the present summer monsoon margin, is also presented. These data show that present lakes and wetlands in the Juyanze Lake basin west of the Badain Jaran desert, in the Zhuyeze Lake basin between the Badain Jaran and Tengger deserts, and in lakes in the eastern Tengger desert, dried or experienced low lake levels in the mid-Holocene around 5000-7000 cal yr BP. Pollen data further indicate that the vegetation cover declined in both the local areas and in the Qilian Mountains, suggesting the climate was drier than that associated with the present Asian summer monsoon. This mid-Holocene drought interval was present throughout a quite large region of the south Inner Mongolian Plateau. The period was also probably colder, at least in the high Asian plateaus and mountains. |
| 收录类别 | SCI ; ISTP |
| WOS关键词 | NORTHWEST PACIFIC-OCEAN ; SHIYANG RIVER DRAINAGE ; BADAIN JARAN DESERT ; LATE PLEISTOCENE ; TENGGER DESERT ; ASIAN MONSOON ; ARID CHINA ; ICE CORE ; HOLOCENE ; EVOLUTION |
| WOS研究方向 | Science & Technology - Other Topics |
| WOS类目 | Multidisciplinary Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000184463300002 |
| 出版者 | SCIENCE PRESS |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2556925 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Chen, FH |
| 作者单位 | 1.Lanzhou Univ, Ctr Arid Environm & Paleoclimate Res, Natl Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China 2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China 3.UCL, Dept Geog, Environm Change Res Ctr, London WC1H 0AP, England 4.Desert Res Inst, Div Earth & Ecosyst Sci, Reno, NV 89512 USA 5.Kansas State Univ, Dept Geol, Manhattan, KS 66506 USA |
| 推荐引用方式 GB/T 7714 | Chen, FH,Wu, W,Holmes, JA,et al. A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China[J]. CHINESE SCIENCE BULLETIN,2003,48(14):1401-1410. |
| APA | Chen, FH.,Wu, W.,Holmes, JA.,Madsen, DB.,Zhu, Y.,...&Oviatt, CG.(2003).A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China.CHINESE SCIENCE BULLETIN,48(14),1401-1410. |
| MLA | Chen, FH,et al."A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China".CHINESE SCIENCE BULLETIN 48.14(2003):1401-1410. |
入库方式： iSwitch采集
来源：寒区旱区环境与工程研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。