[1] Baker A, Smart P L, Edwards R L, et al. Annual growth banding in a cave stalagmite[J]. Nature, 1993, (364): 518-520. [2] Shopov Y Y, Georgiev L, Tsankov L, et al. Methods for research of luminescence of cave minerals and speleothem records of the paleoclimate and solar activity in the past, in Geology, Climate, Hydrology and karst Formation: International Union of Geology and Speleology, Guilin, China[J]. Project, 1991, 299: 52-63. [3] Shopov Y Y, Ford D C, Schwarcz H P. Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate[J]. Geology, 1994, 22: 407-410. [4] Genty D, Quinif Y. Annually laminated sequences in the internal structure of some Belgian stalagmites-Importance for paleoclimatology[J]. Journal of Sedimentary Research, 1996, 60 (1): 275-288. [5] 刘东生, 谭明, 秦小光, 等. 洞穴碳酸盐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. [6] 谭 明, 刘东生, 秦小光, 等. 北京石花洞全新世石笋微生长层与稳定同位素气候意义初步研究[J]. 中国岩溶, 1997, 16 (1): 1~9. [7] 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——Ⅰ 微层显微特征[J]. 中国科学 (D辑), 1998, 28 (4): 91~96. [8] Xiaoguang Qin, Ming Tan, Tungsheng Liu, et al. Spectral analysis of a 1000—year stalagmite lamina-thickness record from Shihua Cavern, Beijing, China, and its climatic significance[J]. Holocene, 1999, 9 (6): 689-694. [9] Baker A, Proctor C, Lauritzen S R, et al. SPEP: High-resolution stalagmite records of NE Atlantic climate in the last millennium[J]. Pages, 2000, 8 (2):14. [10] 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. [11] Heine K, Geyh M A. Radiocarbon dating of speleothems from Rossing Cave, Namib Desert, and palaeoclimatic implications. in Vogel, J. C., ed., Late Cainozoic palaeoclimates of the Southern Hemisphere. Balkema: Rotterdam, 1984. 465-470. [12] Brook G A, Burney D A, Cowart J B. Desert paleoenvironmental data from cave speleothems with examples from the Chihuahuan, Somali-Chalbi, and Kalahari deserts[J]. Palaeo3, 1990, 76: 311-329. [13] Jian-xin Zhao, Qikai Xia, Collerson K D. Timing and duration of the Last Interglacial inferred from high resolution U-series chronology of stalagmite growth in Southern Hemisphere[J]. Earth and Planetary Science Letters, 2001, 184: 635-644. [14] Ayliffe L K, Marianelli P C, Moriarty K C, et al. 500 ka precipitation record from southeastern Australia: Evidence for interglacial relative aridity[J]. Geology, 1998, 26 (2): 147-150. [15] Gordon D, Smart P, Ford D C, et al. Dating of Late Pleistocene Interglacial and Intersradial Periods in the United Kingdom from Speleothem Growth Frequency[J]. Quaternary Research, 1989, 31: 14-26. [16] Baker A, Smart P L, Ford D C. Northwest European palaeoclimate as indicated by growth freqency variations of secondary calcite deposits[J]. Palaeo3, 1993, 100: 291-301. [17] Kashiwaya K, Atkinson T C, Smart P L. Periodic Variations in Late Pleistocene Speleothem Abundance in Britain[J]. Quaternary Research, 1991, 35: 190-196. [18] Wang Y J, Cheng H, Edwards R L, et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China[J]. Science, 2001, 294: 2345-2348. [19] Wang Y J, Wu J, Liu D et al. A quick cooling event of the East Asian monsoon responding to Heinrich Event 1: Evidence from stalagmite δ18O records. Science in China (series D), 2002, 45 (1): 88. [20] 李红春, 顾德隆, Lowel D Stott. 高分辨率洞穴石笋稳定同位素应用之一——京津地区500a来的气候变化——δ18O记录[J]. 中国科学(D辑), 1998, 28 (2): 181~186. [21] 汪永进,陈 琪,刘泽纯. 南京猿人洞石笋年代学研究及其古气候记录[J]. 地理科学, 1999, 19(1): 82~87. [22] 汪永进, 吴江滢, 吴金全, 等. 末次冰期南京石笋高分辨率气候记录与GRIP冰芯对比[J]. 中国科学(D辑), 2000, 30 (5): 533~539. [23] 吴江滢, 汪永进, 程 海, 等. 南京汤山石笋高分辨率氧—碳同位素记录对气候事件的快速响应[J]. 科学通报, 2001, 46 (15): 1307~1311. [24] Polyak V J, Asmerom Y. Late Holocene climate and cultural changes in the Southwestern United States[J]. Science, 2001, 294: 148-151. [25] Ford D C, Williams P. Karst Geomorphology and Hydrology[M]. London: Unwin-Hyman, 1989. 601-608. [26] Dorr H, Munnich K O. Annual variations of the 14C content of soil CO2[J]. Radiocarbon, 1986, 28: 338-345. [27] Poole D K, Miller P L. CO2 flux from three arctic tundra types in North-central Alaska[J]. Arct. Alp. Res., 1982, 14: 27-32. [28] Brook G A, Burney D A, Cowart J B. Desert paleoenvironmental data from cave speleothems with examples from the Chihuahuan, Somali-Chalbi, and Kalahari deserts[J]. Palaeo3, 1990, 76: 311-329. [29] Dreybrodt W. A possible mechanism for growth of calcite speleothems without participation of biogenic carbon dioxide[J]. Earth and Planetary Science Letters, 1982, 58: 293-299. |