[1] O'Neil J R, Clayton R N, Mayeda T K. Oxygen isotope fractionation in divalent metal carbonates[J]. Journal of Chemical Physics,1969,51:5 547～5 558
[2] Hendy C H. The isotopic geochemistry of speleothems -Pt.I. The calculation of the effects of different model of formation on the isotopic compossition of speleothems and their applicability as paleoclimate indictors[J]. Geochim et Cosmochim Acta,1971,35:801～824
[3] Dorale J A, Gonzalez L A, Reagan M K, Pickett D A, Murrell M T, and Baker R G. A high resolution record of Holocene climate change in speleothem calcite from Cold Water cave, Northeast lowa[J]. Science, 1992, 258:1 626～1 630
[4] Talma A S, Vogel J C. Late Quaternary paleotemperatures derived from a speleothem from Cango caves, Cape province, South Africa[J]. Quaternary Research,1992,37:203～213
[5] Holmgren K, Karlen W. Paleoclimatic significance of the stable isotopic composition and petrology of a Late Pleistocene stalagmite from Botswana[J]. Quaternary Research,1995,43:320～328
[6] Bar-Matthems M, Ayalon A. Late Quternary paleoclimate in the Eastern Mediterranean region from stable isotope analysis of speleothems at Soreq cave, Israel[J]. Quternary Research,1997,47:155～168
[7] Yuan Daoxian, Qin Jiaoming, Lin Yushi, et al. High resolution paleoenvironmental reconstruction up to 200kaB.P. with speleothems from Guilin(in Chinese)[M].Guilin Guangxi: Guangxi Normal University Press, 1999. 1～2
[8] Tan Ming, Liu Dongsheng, Qin Xiaoguang, et al. Preliminary study on the data from microbanding and stable isotopes of stalagmites of Beijing Shihua cave[J]. Carsologica Sinica (in Chinese),1997,16(1):1～7
[9] Li Hongchun, Gu Delong, Chen Wenji, et al. Application of high-resolution carbon isotope record of a stalagmite from the Shihua cave, Beijing[J].Geologica Sinica,(in Chinese) 1998,44(5):457～459
[10] 蒋德隆.长江中下游气候[M]. 北京:气象出版社,1991.3～5 [Jiang Delong,Climate of the Yangtse Rive at middle of rive[M].Beijing:Meteorological Publishing House, 1991.3～5]
[11] Wang Junwei, Shen Jifang, Chao Nianying. The characteristics of Karst cave development and tourism resources in Banxia area of the Qingjiang river[J]. Carsologica Sinica(in Chinese),1997,16(3):268～269
[12] 李彬,袁道先,林玉石等. 桂林地区降水、洞穴滴水及现代洞穴碳酸盐氧碳同位素研究及其环境意义[J].中国科学,2000,30(1):82～86 [Li Bin,Yuan Daoxiao,Qin Jianing,et al.Oxygen and carbon isotopic characterisitics of rainwater,drip water and present spesent speleothems in a cave in Guilin area,and their environmental meanings[J].Science in China(Series D),2000,43(3):277～285]
[13] Cerling T E. The stable isotopic composition of soil carbonate and its relationship to climate[J]. Earth Parth. Sci. Lett.,1984,71:229～240
[14] Mucci A, Morse J W. Chemistry of low-temperature abiotic calcites: experimental studies on coprecipitation. Stability and Fractionation[J]. Rev. Aq.Sci. 1990,3:217～254
[15] Banner J L. Application of the trace element and isotope geochemistry of strontium to studies of carbonate diagenesis[J]. Sedimentol., 1995,42:805～824
[16] Johnsen S J, Clausen H B, Dansgaard W, et al. Irregular glacial interstadials recorded in a new Greenland ice[J]. Nature, 1992,356:311～313