Author: FAN YUXIN, LI ZHENJUN, YANG GUANGLIANG, YI SHUANGWEN, ZHANG QINGSONG, LIU WENHAO and MOU XUESONG
Abstract
The timing of high lake‐level stands during the Late Pleistocene in western China remains controversial. Here we report new results from Megalake Tengger based on a study of palaeo‐shorelines and a drill core from Baijian Lake in the northwestern Tengger Desert. Multiple dating methods, based on luminescence signals (quartz optically stimulated luminescence, K‐feldspar post infrared‐infrared stimulated luminescence) and electron spin resonance signals of quartz, were used to date beach sands from palaeo‐shoreline profiles at altitudes of ~1310m (+20m above lake level), ~1320m (+30 m) and ~1350m (+60 m), and from the top 20m of sandy sediments from the drill core obtained from the modern beach of Baijian Lake. The dating results show that high lake level stands associated with the previously reported Megalake Tengger (~1310–1320 m) occurred during the late Early to Middle Pleistocene, which is much earlier than previously reported. In addition, no geomorphological evidence of shorelines and sedimentary evidence from the drill core profile were found to support the previously reported Late Pleistocene lake levels. Our results indicate that the exact age of the previously reported ‘high lake level event’ in a large part of northwestern China during the Late Pleistocene needs to be re‐evaluated.
Keywords: ESR; feldspar; high lake level; OSL; quartz; Tengger