[1]  Winograd I J, Coplen T B, Landwehr J M,et al. Continuous 500,000 year climate record from vein calcite in Devils Hole,Nevada[J]. Science, 1992, 258: 255-260.
[2]  Baker A, Smart P L, Edwards R L,et al. Annual growth banding in a cave stalagmite[J]. Nature, 1993, 364:518-520.
[3]  Liu Dongsheng, Tan Ming, Qin Xiaoguang,et al. Discovery of microbanding in speleothems in China and its significance in study of global change[J].Quaternary Sciences. 1997,(1):41-51.[刘东生,谭明,秦小光,等.洞穴碳酸钙微层理在中国的首次发现及其对全球变化研究的意义[J].第四纪研究,1997,(1): 41-51.]
[4]  Lauritzen S E. High-resolution paleotemperature proxy record during the last interglaciation in Norway from speleothems[J], Quaternary Research, 1995, 43: 133-146.
[5]  Holmgren K, Karlen W, Lauritzen S E,et al. A 3000-year high-resolution stalagmite-based record of paleoclimate for northeastern South Africa[J]. The Holocene, 1999, 9(3):295-309.
[6]  Yuan Daoxian.Karst processes sensitivity to environmental change and its records[J]. Chinese Science Bulletin, 1995,40(13):1 210-1 213.[袁道先.岩溶作用对环境变化的敏感性及其记录[J].科学通报,1995,40(13):1 210-1 213.]
[7]  Lauritzen S E, Lundburg J. Calibration of the speleothem delta function: an absolute temperature record for the Holocene in north Norway[J]. The Holocene, 1999, 9(6):659-669.
[8]  Hendy C H. The isotope geochemistry of spleothems I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as paleoclimate indicators[J]. Geochimica et Cosmochimica Acta, 1971, 35:801-824.
[9]  William P W, Marshall A, Ford D C,et al. Palaeoclimatic interpretation of stable isotope data from Holocene speleothems of the Waitomo District, North Island, New Zealand[J]. The Holocene, 1999, 9(6): 649-657.
[10]  Gascoyne M. Palaeoclimate determination from cave calcite deposits[J]. Quaternary Science Reviews, 1992, 11: 609-632.
[11]  O' Neil J R, Adami L Hand Epstein S. Revised value for the ¹⁸O fractionation factor between H2O and CO2at 25℃[J]. United States Geological Survey Research, 1975,(3):623-624.
[12]  Zheng Shuhui,Hou Fagao, Ni Baoling. Study on hydrogen and oxygen stable isotope of precipitation in China[J].Chinese Science Bulletin, 1983,(13):801-806.[郑淑惠,侯发高,倪葆龄.我国大气降水的氢氧稳定同位素研究[J].科学通报,1983,(13):801-806.]
[13]  Tan Ming, Liu Dongsheng. Study on paleoclimatic records from cave calcite deposits[J]. Advancein in Earth Sciences,1996,11(4):388-395.[谭明,刘东生.洞穴碳酸钙沉积的古气候记录研究[J].地球科学进展,1996,11(4):388-395.]
[14]  Li Bin. Significance of δ¹³C,δ¹⁸O of speleothems for environmental changes[J].Carsologica Sinica, 1994,13(1):17-24.[李彬.洞穴化学沉积物中δ¹³C、δ¹⁸O对环境变迁的示踪意义[J].中国岩溶,1994,13(1):17-24.]
[15]  Hong A' shi, Peng Zicheng, Li Ping. Isotope geochemistry method for paleotemperature of stalagmites[J].Advance in Earth Sciences,1995,10(4):348-352.[洪阿实,彭子成,李平.洞穴石笋古温度的同位素地球化学方法[J].地球科学进展,1995,10(4):348-352.]
[16]  Qin J. Studies on oxygen isotope thermometry of cave sediment and paleoclimatic record[J]. Carsologica Sinica,1996,15(1-2):174-182.
[17]  Dorale J A, Gonzalez L A, Reagan M K,et al. A high-resolution record of Holocene climate change in speleothem calcite from cold water cave, northeast Iowa[J]. Science, 1992,258: 1 626-1 630.
[18]  Cerling T E, Quade J. Stable carbon and oxygen isotope in soil carbonates[A]. In: Climate Change in Continental Isotope records [C]. Washington: American Geophysical Union, 1993.217-31.
[19]  Boutton T W. Stable carbon isotope ratios of natural materials. II. Atmospheric, terrestrial, marine, and fresh water environment[A]. In:Coleman D C, Fry B, eds. Carbon Isotope Technique[C]. San Diego: Academic Press, 1991.155-171.
[20]  Talma A S, Vogel J C. Late Quaternary paleotemperatures derived from a speleothem from Cango cave, Cape province,South Africa[J]. Quaternary Research,1992,(37):203-213.
[21]  Ehleringer J R, Brooks J R, Flanagan L B,et al. Carbon isotope composition of bored plants: functional grouping of life forms[J]. Oecologia,1997,(110):301-11.
[22]  Vogel J C, Fuls A, Ellis R P. The geolographical distribution of Kranz grasses in South Africa[J]. South Africa Journal of Science, 1978,(74):209-15.
[23]  Denniston R F, Gonzalez L A, Baker R G,et al. Speleothem evidence for Holocene fluctuations of the prairie-forest ecotone, north-central USA[J]. The Holocene, 1999, 9(6):671-676.
[24]  Schwarcz H P. Geochronology and isotopic geochemistry of speleothems[A]. In: Fritz P, Fontes J C, eds. Handbook of Environmental Isotope Geochemistry, Vol.2: the Terrestrial Environment[C]. Amsterdam: Elsevier,1986.271-300.                    
[25]  Frumkin A, Carmi I, Gopher A,et al. A Holocene milliennial-scale climate cycle from a speleothem in Nahal Qanah cave, Israel[J]. The Holocene, 1999, 9(6): 677-682.
[26]  Shopov Y Y, Ford D C, Schwarcz H. Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate[J]. Geology, 1994, 22:407-410.
[27]  Railsback L B, Brook G A, Chen J,et al. Environmental controls on the petrology of a late Holocene speleothem from Botswana with annual layers of aragonite and calcite[J].Journal of Sedimentary Research, 1994, 64:147-155.
[28]  Genty D, Quinif Y. Annually laminated sequences in the internal structure of some Belgian stalagmites: Importance of paleoclimatology [ J]. Journal of Sedimentary Research,1996, 66:275-288.
[29]  Tan Ming, Qin Xiaoguang, Liu Dongsheng, Interannual, decadal and century scale climatic changes revealed by stalagmite records[J]. Science in China(Ser D), 1998,28(3):272-277.[谭明,秦小光,刘东生.石笋记录的年际、十年、百年尺度气候变化[J].中国科学(D辑),1998,28(3):272-277.]
[30]  Tan Ming, Qin Xiaoguang, Shen Linmei,et al. Bioptical microcycles of laminated speleothems from China and their chronological significance [ J ]. Chinese Science Bulletin,1999,44(6):646-648.[谭明,秦小光,沈凛梅,等.中国洞穴碳酸盐双重光性显微旋回及其意义[J].科学通报,1999,44(6):646-468.]
[31]  Shopov Y Y. Laser luminescent microzonal analysis—A new method for investigation of alternations of climate and solar activity during the Quaternary [A]. In: Kiknadze T, ed.Problems of Karst Study in Mountainous Countries [C].Tbilisi Georgia, Metsniereba, 1987. 228-232.
[32]  Baker A, Barnes W, Smart P L. Speleothem luminescence intensity and spectral characteristics: Signal calibration and a record of paleovegetation change[J]. Chemical Geology,1996, 130: 65-76.
[33]  Qin Xiaoguang,Liu Dongsheng, Tan Ming,et al. Grey characteristics of microbanding of stalagmite in Shihua Cave, Beijing and itsclimatic signification ( 1 )—The study of microstructure of microbanding[J]. Science in China(Ser D),1998,28(2):151-157.[秦小光,刘东生,谭明,等.北京石花洞石笋微层灰度变化特征及其气候意义(1)——微层显微特征研究[J].中国科学(D辑),1998,28(2):151-157.]
[34]  Ramseyer K, Miano T, D' Orazio V,et al. Nature and origin of organic matter in carbonates from speleothems, marine cements and coral skeletons[J]. Organic Geochemistry, 1997,26: 361-78.
[35]  Genty D, Baker A, Barnes W. Comparison entre les lamines luminescentes et les lamines visibles annuelles de stalagmites[J]. Comptes Rendus Acad Sci, Paris, Earth and Planetary Sciences, 1997, 325: 193-200.
[36]  Baker A, Barnes W L, Smart P L. Variations in the discharge and organic matter content of stalagmite drip waters in Lower Cave, Bristol[J]. Hydrological Processes, 1997,11(11): 1 541-1 555.
[37]  Wang Xianfeng, Liu Dongsheng, Liang Handong,et al.Preliminary analyses by SIMS on trace components of stalagmite microlayers and their climate significance[J].Quaternary Sciences, 1999,(1):59-66.[王先锋,刘东生,梁汉东,等.石笋微层物质组成的二次离子质谱初步分析及其气候意义[J].第四纪研究,1999,(1):59-66.]
[38]  Qin Xiaoguang, Liu Dongsheng, Tan Ming,et al. Thespectral analysis for a lamina thickness series of a stalagmite in Beijing and the climate variation in last lka[J]. Acta Geographica Sinica, 1999,54(6):543-549.[秦小光,刘东生,谭明,等.石笋微层的谱分析和北京地区1千年来的气候演变[J].地理学报,1999,54(6):543-549.]
[39]  Baker A, Proctor C J, Barnes W L. Variations in stalagmite luminescence laminae structure at Pool' s Cavern, England,AD 1910~1996; Calibration of a palaeoprecipitation proxy[J]. The Holocene, 1999, 9(6): 683-688.
[40]  Brook G A, Rafter M A, Railsback L B. A high-resolution proxy record of rainfall and ENSO since AD 1550 from layering in stalagmites from Anjohibe Cave, Madagascar[J]. The Holocene, 1999, 9(6): 695-705.
[41]  Ayalon A, Bar-Matthews M, Kaufman A. Petrography, strontium, barium, and uranium concentrations, and strontium and uranium isotope ratios in speleothems as palaeoclimatic proxies: Soreq Cave, Israel[J]. The Holocene, 1999. 9(6):715-722.
[42]  Burton E A, Walter L M. The effects of and temperature on magnesium incorporation in calcite on seawater and MgCl₂-CaCl₂solution[J]. Geochimica et Cosmochimica Acta, 1991,(55):777-85.
[43]  Goede J C, Vogel J C. Trace element variations and dating of a late Pleistocene Tasmanian speleothem[J]. Paleogeography, Paleoclimatology, Paleoecology, 1991,(88):121-31.
[44]  Roberts M S, Smart P C, Baker A. Annual trace element variations in a Holocene Speleothem[J]. Earth and Planetary Science Letters, 1998,154: 237-246.
[45]  Roberts M S, Smart P L, Chris J,et al. Trace element Variations in coeval Holocene speleothems from GB Cave, southwest England[J]. The Holocene, 1999, 9(6): 707-713.
[46]  Goede A, McCulloch M, McDermott F,et al. Aeolian contribution to strontium and strontium isotope variations in a Tasmanian speleothem[J]. Chemical Geology,1998,(149):37-50.
[47]  Bar-Matthews M, Ayalon A, Kaufman A,et al. The Eastern Mediterranean paleoclimate as a reflection of regional events: Soreq Cave, Israel[J]. Earth and Planetary Science Letters, 1999,(166):85-95.
[48]  Gonzalez L A, Carpenter S J, Lohman K C. Inorganic calcite morphology: roles of fluid chemistry and fluid flow[J]. Journal of Sedimentary Petrology, 1992,(62):382-99.