代表性学术著作和论文: (1)Xue J.B., Zhong W., Cao J.Y. Changes in C3 and C4 plant abundances reflect climate changes from 41000 to 10000 years ago in northern Leizhou Peninsula, South China.Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 396: 173-182. (2)Zhong W., Xue J.B., Zheng Y.M., et al. Sediment geochemistry of Dahu Swamp in the Nanling Mountains, South China: implication for catchment weathering during the last 16,000 years. International Journal of Earth Sciences, 2012, 101(2):453-462. (3)Xue J.B., Zhong W. Holocene climate variations denoted by Barkol Lake sediments in northern Xinjiang and its possible linkage to the high and low latitude climates. Science China-Earth Science, 2011, 54(4): 603-614. (4)Zhong W., Xue J.B., Cao J.X., et al. Bulk organic carbon isotope record of lacustrine sediments in Dahu Swamp, eastern Nanling Mountains in South China: Implication for catchment environmental and climatic changes in the last 16,000 years. Journal of Asian Earth Sciences, 2010, 38: 162-169. (5)Zhong W., Xue J.B., Zheng Y.M., et al. Climatic changes since the last deglaciation inferred from a lacustrine sedimentary sequence in the eastern Nanling Mountains, south China. Journal of Quaternary Science, 2010, 25:975-984. (6)Xue J.B., Zhong W., Zheng Y.M., et al. A New High-resolution Late Glacial-Holocene Climatic Record from Eastern Nanling Mountains in South China. Chinese Geographical Science, 2009,19(3):274-282. (7)Xue J.B. , Zhong W., Zhao Y.J.,et al. Holocene abrupt climate shifts and Mid-Holocene drought intervals recorded in Barkol Lake, northern Xinjiang, NW China. Chinese Geographical Science, 2008,18(1):54-61. (8)薛积彬,钟巍,曹家元等. 末次冰期以来雷州半岛北部C3/C4植物相对丰度变化及其驱动因素. 湖泊科学,2014,26(3):464-472. (9)薛积彬,钟巍. 新疆巴里坤湖全新世气候环境变化与高低纬间气候变化的关联. 中国科学:地球科学, 2011,41(1):61-73. (10)薛积彬,钟巍. 新疆巴里坤湖全新世环境记录及区域对比研究. 第四纪研究,2008,28(4):610-620. |