Wang Sumin

TL;DR: In this article, multi-proxy analysis of a sediment core from Qinghai Lake, including pollen, carbonate, TOC, TN and δ 13 C of organic matter, was used to document regional climatic changes during the last 18,000 years.

TL;DR: Based on 11004 satellite images from CBERS CCD and Landsat TM/ETM, changes in the spatial characteristics of all lakes in China were determined following pre-established interpretation rules as discussed by the authors.

TL;DR: In this article, the authors focused mainly on the climatic and environmental variations 5 to 3 ka. B.P. with particular reference to one stable warmer and wetter millennium (7.2-6 ka B.p.).

TL;DR: In this paper, principal component analysis (PCA) was used to assess the degree of contamination and spatial distribution of heavy metals and nutrients in different areas of Taihu Lake, which is one of the largest freshwater lakes in China.

TL;DR: In this paper, the authors present a climate record for central Tibet spanning the time between 10500 and 1600 cal years BP from a 5.3m-long sediment core from Cuoe Lake, which shows that high Sr concentration, high TOC content, high C/N ratio and enriched δ13C of lake sediments correspond to stronger chemical weathering, high productivity, high lake level and warmer/wetter climate and vice versa.