The lake-level changes of Lop Nur over the past 2000 years and its linkage to the decline of the ancient Loulan Kingdom

Journal of Hydrology: Regional Studies

Huaze Gong¹  Jiaqi Liu¹  Tingting Zhang¹  Charles Elachi²  Yun Shao³  Chang-an Liu³  Brian Brisco³  Zhi Yang³  Xuncheng Xia⁴  Huadong Guo⁵  Yuyang Geng⁶  Shugang Kang⁷ 

[1] Laboratory of Target Microwave Properties, Deqing Academy of Satellite Applications, Zhejiang 313202, China;University of Chinese Academy of Sciences, Beijing 100049, China;Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China;California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA;Canada Centre for Remote Sensing, Natural Resources Canada, 560 Rochester Street, Ottawa, Ontario K1A 0E4, Canada;Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Xinjiang 830011, China;

关键词: Lop Nur;    Loulan Kingdom;    SAR remote sensing;    OSL dating;   

DOI  :  

来源: DOAJ

【 摘 要 】

Study region: Lop Nur, Xinjiang Province, China Study focus: Lop Nur has been a vast playa which was a historic lake in eastern Tarim Basin, northwest China. The lake's catchment played a significant role in the development of oasis states in the early Common Era, such as the ancient Loulan Kingdom. However, the history of lake dynamics remains unclear, and its potential linkage to the decline of Loulan Kingdom has been not well-examined. This paper aims to reconstruct the lake-level changes in Lop Nur over the last 2000 years using synthetic aperture radar (SAR) data, optically stimulated luminescence (OSL) dating of lacustrine and aeolian sediments, and radiocarbon (14C) dating of ancient bio-remains. Furthermore, the relationships between Lop Nur' fluctuation and the decline of ancient Loulan Kingdom were discussed New hydrological insights for the region: The results suggest that Lop Nur once covered an area more than 11, 602 km2 and that lake-level reduced gradually during 360–470 C.E. Subsequently, the lake experienced a few stages of lake-level fluctuation which never reached the upper-most shorelines. Also, the historical changes in the lake level were temporal coincided with the ancient Loulan Kingdom's collapse, showing that the dynamics of hydrological conditions in catchment may have a direct influence on the fall of human settlement in drylands.

【 授权许可】

Unknown