• 责任者：Zeng Yan (State Key Laboratory of Environmental Geochemistry ; Institute of Geochemistry ; Chinese Academy of Sciences ; Guiyang 550002 ; China) ; Chen Jing’an
• 刊名：Geochimica
• 出版年：2011
• 卷期：40(3)
• 关键词：湖泊沉积物 ; lake sediments ; 古气候 ; paleoclimate ; 铷—锶计时 ; Rb-Sr dating ; 全新世 ; Holocene ; 广东 ; Guangdong Province
• 页码：p.249-257
• 图表：5 illus., 1 table, 49 refs.
• 分类号：1400
• issnNo：ISSN0379-1726
• isbnNo：CN44-1398/P

Through comparative analysis of Rb/Sr ratios in non-residual, residual and bulk samples, the authors found that the Rb/Sr ratios in non-residual samples were the closest to the chemical weathering in the catchment basin.  During AD740~860 and AD1400~1750, the non-residual Rb/Sr ratios were much lower, indicating that the chemical weathering of the two periods were relatively strong. The results showed that chemical weathering in the catchment was dominantly controlled by precipitation, while the effect of temperature was not obvious.