Holocene lake level history of the Tangra Yumco lake system, southern-central Tibetan Plateau
文献类型：期刊论文
| 作者 | Furstenberg, S (Fuerstenberg, Sascha)4; Mausbacher, R (Maeusbacher, Roland)1; Wang, JB (Wang, Junbo)2; Haberzettl, T (Haberzettl, Torsten)1; Ahlborn, M (Ahlborn, Marieke)1; Mazzocco, J (Mazzocco, Jeaneth)3; Zhu, LP (Zhu, Liping)2; Pierson, J (Pierson, James)3; Frenzel, P (Frenzel, Peter)4; Ahlborn, M |
| 刊名 | HOLOCENE
 |
| 出版日期 | 2016 |
| 卷号 | 26期号:2页码:176-187 |
| 关键词 | Exposure Ages Qinghai Lake Donggi Cona Quartz Osl Nam Co China Luminescence Sediments Chronology Basin |
| DOI | 10.1177/0959683615596840 |
| 文献子类 | Article |
| 英文摘要 | Massive carbonate banks representing ancient lacustrine deposits are exposed in the catchment of the lake Tangra Yumco (southern-central Tibetan Plateau) and nearby lake Xuru Co. Nine sediment samples were taken below and above these lacustrine deposits to determine periods of changing lake level using optically stimulated luminescence (OSL) applying a multiple-aliquot regeneration (MAR) protocol. According to facies and stratigraphy, samples below the carbonate banks indicate a rising and samples from above a falling lake level. The results indicate that the rising lake level of Tangra Yumco passed the sampling location at 10.5 and 2.1 ka while a falling lake level passed the sampling location at 0.9 ka. The rising lake level of Xuru Co passed the sampling location at 7.9 and 1.7 ka and a falling lake level at 0.5 ka showing a similar trend as at Tangra Yumco. Combining these results with recalculated cosmogenic nuclide ages and previously published feldspar luminescence data allows the establishment of a Holocene lake level reconstruction for Tangra Yumco, which is unique for the southern-central Tibetan Plateau. The lake level of Tangra Yumco crested a lake level highstand of 181-183m above the recent lake level prior to 8.5 ka and has generally fallen after 8.5 ka, with a minor lake level rise at 2.1 ka. Lake level variations at Tangra Yumco occur simultaneously with other lakes on the Tibetan Plateau indicating that variations were controlled by monsoonal dynamics with a moist early Holocene and a successive reduction of available moisture thereafter. The average rate of the lake level rise between 10.5 and 8.5 ka is at least 0.05m a(-1) (compared with a modern value of 0.38m a(-1)), providing valuable insights in the monsoonal impact on lake level change on the southern-central Tibetan Plateau. |
| 学科主题 | 自然地理学 |
| 语种 | 英语 |
| WOS记录号 | WOS:000368332200002 |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/7773]  |
| 专题 | 青藏高原研究所_图书馆 |
| 通讯作者 | Ahlborn, M |
| 作者单位 | 1.Univ Jena, Phys Geog, Inst Geog, D-07743 Jena, Germany 2.Chinese Acad Sci, Key Lab Tibetan Environm Changes & Land Surface P, Inst Tibetan Plateau Res, Beijing 100864, Peoples R China 3.Univ Illinois, Luminescence Dating Res Lab, Dept Earth & Environm Sci, Chicago, IL USA 4.Univ Jena, Inst Geosci, D-07743 Jena, Germany |
| 推荐引用方式 GB/T 7714 | Furstenberg, S ,Mausbacher, R ,Wang, JB ,et al. Holocene lake level history of the Tangra Yumco lake system, southern-central Tibetan Plateau[J]. HOLOCENE,2016,26(2):176-187. |
| APA | Furstenberg, S .,Mausbacher, R .,Wang, JB .,Haberzettl, T .,Ahlborn, M .,...&Ahlborn, M.(2016).Holocene lake level history of the Tangra Yumco lake system, southern-central Tibetan Plateau.HOLOCENE,26(2),176-187. |
| MLA | Furstenberg, S ,et al."Holocene lake level history of the Tangra Yumco lake system, southern-central Tibetan Plateau".HOLOCENE 26.2(2016):176-187. |
入库方式： OAI收割
来源：青藏高原研究所
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。