THE STALAGMITE MICROBANDING IN RESEARCH OF HIGH RESOLUTION CLIMATIC-ENVIRONMENTAL CHANGES
Received date: 2001-07-12
Revised date: 2001-10-23
Online published: 2002-06-01
It’s one of the most important task to reconstruct high resolution climatic-environmental changes in the last 2 ka of global change. The same as other natural materials (loess、ice-core、tree rings、sea deposits), spleothems are important repositories of palaeoclimatic and palaeoenvironmental information. On the basis of sedimentary characteristics and bedding-structure, stalagmite microbanding are ideal data in research of high resolution climatic-environmental changes, able to provide climate information with an annual resolutions and much longer time span compared to tree rings. Two aspects of annual banding of stalagmite have been reported, the luminescent microbanding observed under a fluoromicroscope and the lamina which is visible to the naked eye. It involves same climatic-environmental information, such as precipitation, temperature, soil and vegetation. In this paper, the authors analyze the causation、category and influencing factor of microbanding grey and microbanding thickness in detail, review and synthesize the recent advances in stalagmite microbanding research of high resolution climatic-environmental changes, and also point out the existing problems and forecast the trends.
LIU Qi-ming, WANG Shi-jie, OUYANG Zi-yuan . THE STALAGMITE MICROBANDING IN RESEARCH OF HIGH RESOLUTION CLIMATIC-ENVIRONMENTAL CHANGES[J]. Advances in Earth Science, 2002 , 17(3) : 396 -401 . DOI: 10.11867/j.issn.1001-8166.2002.03.0396
[1]Tan Ming , Liu Dongsheng , Zhong Hua , et al. Preliminary study on the climatic data from stable isotopes of speleothems under monsoon[J].Chinese Science Bulletin , 1997, 42(12): 1 302-1 306.[谭明, 刘东生, 钟华,等. 季风条件下全新世洞穴碳酸盐稳定同位素气候信息初步研究[J]. 科学通报,1997,42(12):1 302-1 306.]
[2]Li Hongchun , Gu Delong , Stott L D. Applications of interannual-resolution stable-isotope records of speleothem—climatic changes in Beijing and Tianjin, China during the past 500 years —the δ18O Record[J]. Science in China (Ser D) , 1998, 28(2):181-186.[李红春, 顾德隆, Lowell D Stott,等. 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.]
[3]Li Bin , Yuan Daoxian , Lin Yushi , et al . Oxygen and carbon isotopic characteristics of rainwater, drip water and present speleothems in a cave in Guilin area and their environmental meanings[J]. Science in China (Ser D) , 2000,30(1): 81-87. [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(D辑),2000,30(1):81-87.]
[4]Shopov Y Y. Laser luminescent microzonal analysis:A new method for investigation of the alterations of climate and solar activity during the Quaternary[A]. In: Kiknadze T, eds. Problems of Karst study in Mountainous Countries[C]. Tbilisi: Georgia , Metsniereba, 1987.228-232.
[5]Roberts M S, Smart P L, Hawkesworth C J, et al.Trace element variations in coeval Holocene speleothems from GB. cave, southwest England[J]. The Holocene, 1999, 9: 707-713.
[6]Goede A, Vogel J C.Trace element variation and dating of a Late Pleistocene Tasmanian speleothem[J]. Palaeogeography Palaeoclimatology Palaeoecology, 1991,88:121-131.
[7]Gascoyne M. Trace-element partition coefficients in the calcite - water system and their paleoclimatic significance in cave studies[J]. Journal of Hydrology, 1983, 61:213-222.
[8]Baker A, Smart P L, Edwards R L, et al.Annual growth banding in a cave stalagmite[J]. Nature, 1993, 364: 518-520.
[9]Baker A, Caseldine C J, Gilmour M A, et al. Stalagmite luminescence and peat humification records of palaeomoisture for the last 2 500 years[J]. Earth and Planetary Science Letters, 1999, 165(1):157-162.
[10] Fairchild I J, Borsato A, Tooth A, et al. Controls on Trace-element (Sr-Mg) compositions of carbonate cave waters Implications for speleothem climatic records[J]. Chemical Geology, 2000, 166: 255-269.
[11]Tan Ming, Liu Dongsheng. Study on paleoclimatic records from cave calcite deposits [J]. Advance 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. ]
[12]Zhang Cheng, Yuan Daoxian. Study on continental paleoenvironmental proxy based on speleothems (drop stones) [J]. Advance in Earth Sciences, 2001, 16(3): 374-381. [章程, 袁道先. 洞穴滴石石笋与陆地古环境记录研究进展[J]. 地球科学进展,2001, 16(3): 374-381.]
[13]Brecker W S. Radiocarbon measurement and annual rings in cave formations[J]. Nature, 1960,185:93-94.
[14]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.]
[15]Lauritzen S. Annually resolved stable isotope data from speleothem calcite by laster ablation/mass spectrometry[A]. In: Lauritzen S, ed. Climate Change: The Karst Record[C]. West Virginia: Karst Water Institute, Inc, 1996.31-38.
[16]Gilson J R, Macarthney E.Luminescence of speleothems from Devon UK. The presence of organic activators[J]. Ashford Speleological Society Journal, 1954, 6: 8-11.
[17]Gascoyne M. Trace elements in calcite: The only cause of speleothem color?[J]. National Speleological Society Bulletin, 1978,40: 90.
[18]White W B, Brennan E S. Luminescence of speleothems due to fulvic acid and other activators[A]. In: 10th Proceedings of the International Speleology Congress[C]. 1989,1:212-214.
[19]Shopov Y Y, Ford D C, Schwarcz H P. Luminescent microbanding in speleothems-high-resolution chronology and paleoclimate[J].Geology, 1994, 22(5): 407-410.
[20]Genty D, Baker A, Maire R. Comparison of annual luminescent and visible laminae in stalagmites[J].Comptes Rendus de l'Academie des Sciences, Ser Ⅱ.Fascicule A. Sciences Dela Terre et des Planetes, 1997,325:193-200.
[21]Li Bin, Yuan Daoxian, Lin Yushi, et al. Luminescence and palaeoenvironmental record in a stalagmite in Panlong Cave , Guilin [J]. Acta Geoscientia Sinica, 1997,18(4):400-406. [李彬, 袁道先, 林玉石,等. 桂林盘龙洞石笋发光特性及其古环境记录的初步研究[J]. 地球学报,1997,18(4):400-406.]
[22]Qin Xiaoguang, Liu Dongsheng, Tan Ming, et al. Grey characteristics of microbanding of stalagmite in Shihua cave , Beijing and its climatic signification (I)—The study of microstructure of microbanding [J]. Science in China (D), 1998,28(1):91-96. [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.微层显微结构[J]. 中国科学(D),1998,28(1):91-96.]
[23]Hill C, Forti P. Cave minerals of the world[Z]. National Speleological Society, 1997. 239-244.
[24]Baker A, Genty A. Environmental Pressures on conserving cave speleothems-effects of changing surface land-use and increased cave tourism[J].Journal of Environmental Management, 1998, 53(2):165-175.
[25]Martin J C, Mark B D. Temperature and moisture effects on the production of dissolved organic carbon in a spodosol[J]. Soil Biol Biochem, 1996,28(9):1 191-1 199.
[26]Baker A, Barnes W L, Smart P L. Speleothem luminescence intensity and spectral characteristics-signal calibration and a record of palaeovegetation change[J]. Chemical Geology, 1996, 130: 65-76.
[27]Liu Dongsheng , Tan Ming , Qin Xiaoguang , et al. Discovery of microbanding in speleothems in China and its significance in the study of global change[J]. Quaternary Sciences, 1997, 17 (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,1997,17(1),41-51.]
[28]White W B. Reflectance spectra and color in speleothems[J]. National Speleological Society Bulletin, 1981,43: 20-26.
[29]Perrette Y, Delannoy J J, Bolvin H. Comparative-study of a stalagmite sample by stratigraphy, laser-induced fluorescence spectroscopy, EPR spectrometry and reflectance imaging[J]. Chemical Geology, 2000, 162: 221-243.
[30]Dreybrodt W.Chemical-kinetics, speleothem growth and climate[J]. Boreas, 1999, 28(3):347-356.
[31]Tan Ming, Qin Xiaoguang, Liu Dongsheng.Interannual, decadal and century scale climatic changes revealed by stalagmite records[J]. Science in China (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),1998,28(3):272-277.]
[32]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): 646-648.]
[33]Qin Xiaoguang, Liu Dongsheng, Tan Ming, et al. Grey characteristics of microbanding of stalagmite in Shihua cave , Beijing and its climatic signification (II)—The interannual change of grey [J]. Science in China (D), 2000,30(3): 239-248. [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——II . 灰度的年际变化[J].中国科学(D), 2000,30(3): 239-248.]
[34]Baker B,William L B,Peter L S. Variations in the discharge and organic matter content of stalagmite drip waters in lower cave[J].Bristol Hydrological Processes,1997, 11:1 541-1 555.
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