Study on Laminae or Lamella Groups and Types of Stalagmite in Caves

ZHANG Mei-liang; LIN Yu-shi; QIN Jia-ming

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ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

Citation:

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

Study on Laminae or Lamella Groups and Types of Stalagmite in Caves

Institute of Karst Geology,CAGS,Guilin Guangxi,541004

Received Date: 2001-05-28
Rev Recd Date: 2001-08-30

Abstract

Stalagmite is a typical dripstone shape of CaC0₃ in caves and the most comprehensive and systematical paleoclimate environment in for mation carrier too. With advances of dating techniCues and analytic methods with high resolution，it is of great significance in the paleoclimate environment reconstruction. The combi nation，thickness，grain size and bedding plane structure of depositional laminae in stalagmite are the material base to resume droping water trends of for ming stalagmite and the related paleo- hydrological conditions. 0n the basis of the analysis and study of many stalagmite vertical profiles and systematic isotopic compositions,trace elements and specific laminae，it has been demonstrated that stalagime sedimentary laminae have obvious rhythmic combination,sedimentary cycles and indication of paleoclimatic environments. It is firstly put for ward that stalagmite is of lamina groups of cone in cone,cone and pillar,cone i n cone and pillar combined types and with the sediment ary structures,such as continuity,cycle,disconnected and compound lamina types. The paper discusses their indivitual charatersitics，trends of dropping and flow water and evolutionary characteristics of climatic environments.
- cave stalagmite,
- sediment laminae,
- lamina types,
- paleoclimatic environment

References

[1]	张美良,林玉石,覃嘉铭等.桂林水南洞石笋的沉积学特征[J]. 沉积学报,1999,17(2):233～239 [Zhang Meiliang, Lin Yushi, Qin jiaming,Sedimentological characteristics of a stalagmite from Shuinan cave, Guilin[J]. Acta Sedimentologica Sinica, 1999,17(2):233～239]
[2]	谭明, 潘根兴, 王先锋等.石笋与环境-石笋纹层形成的环境机理初探[J]. 中国岩溶,1999,18 (3):197～206 [Tan Ming, Pan Genxing, Wang Xianfeng et al,Stalagmites and Environment-Preliminary study on the formation of laminated stalagmites[J]. Carsologica Sinica,1999,18(3):197～206]
[3]	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,1995,18(3): 1 210～1 213[Yuan Daoxian. Sensitivity of karst process to environmental change and its record[J].Chinese Science Bulletin, 1995, 40(13):1 210～1 213]
[4]	杨明德, 谭明, 梁虹. 喀斯特流域水文地貌系统[M]. 北京:地质出版社,1998.24～34[ Yang Mingde,Tan Ming,Liang Hong.Hydrogeomorphologicial system of karst drainage basin[M]. Beijing: Geological publishing house,1998.24～34]
[5]	覃嘉铭. 古气候变化的石笋同位素记录-以桂林盘龙洞为例[J]. 地球学报,1997,18(3): 225～260 [Qin jiaming. Study on stalagmite isotope records of paleoclimatic changes[J].Acta Geoscientia Sinica.1997, 18(3): 255～260]
[6]	谭明, 秦小光, 刘东升.石笋记录的年际、十年、百年尺度气候变化[J].中国科学,1998,28(3):272～277 [Tan Ming, Qin Xiaoguang, Liu Dongsheng, et al. Interannual, decadal and century scale climatic changes revealed by stalagmite records[J]. Science in China, Series D, 1998, 41(4): 416～421 ]
[7]	李红春, 顾德隆, 陈文寄.利用洞穴石笋的δ^18O和δ¹³C重建3000年以来北京地区气候和古环境-石花洞研究系列之三[J]. 地震地质, 1997,19(1):71～85 [Li Hongchun, Ku The-lung, Chen Wenji, et al. Isotope studies of Shihua cave-Ⅲ:Reconstruction of paleoclimate and paleoenvironment of Beijing during the Last 3000 years from δ^18O and δ¹³C records in stalagmite[J]. Seismology And Geology,1997,19(1):77～86]
[8]	杨子赓, 牟昀智等. 北京猿人遗址综合研究[M]. 北京: 科学出版社,1985. 1～85 [Yang Zigeng, Mou Yunzhi. Synthetical study of Beijing-Man cave site[M]. Beijing:Scientific & Technical publishers,1985.1～85]
[9]	王丽娟. 桂林甑皮岩洞穴遗址第四纪孢粉分析[J].人类学报, 1989,8(1): 69～76 [Wang Lijuan.A Quaternary Sporo-pollen Analysis of Zengpiyan cave site,Guilin[J].Acta Anthropological Sinica,1989,8(1): 69～76]
[10]	黄万波.中国第四纪洞穴堆积[J].中国岩溶,1995,14(增刊):122～128 [Huang Wanbo. Quaternary cave accumulation in China[J]. Carsologica Sinica,1995,14(Supp.):122～128]
[11]	刘育燕.桂林甲宅太平岩洞穴石柱的古地磁年龄[J]. 中国岩溶, 1995,14(3) :247～250[Liu Yuyan. Paleogeomagnetic age of column from Taiping cave, Guilin[J]. Carsologica Sinica,1995,14(3):247～250]
[12]	赵树森, 刘明林, 乔广生. 中国东部喀斯特洞穴沉积物铀系年代[J]. 中国岩溶,1989,8(1): 53～61[ Zhao Shusen, Liu Minglin, Qiao Guangsheng. The U-series ages of speleothem of karst caves in east China[J]. Carsologica Sinica,1989,8(1):53～61]
[13]	汪训一.桂林茅茅头大岩洞穴沉积物的放射性年龄及氧、碳同位素特征[J]. 科学通报, 1985,30(2): 528～531[Wang Xunyi.Ages and characteristics of car bon and oxygen isotope of cave sediments from Maomaotoudayan cave in Guilin[J]. Chinese Science Bulletin,1985, 30(2): 528～531]
[14]	沈冠军.热电离质谱法测定贵州郑洞石笋的铀系年代及其古气候意义[J]. 中国岩溶, 1997,16(1):11～18[ Shen Guanjun, Bassem Gahleb, Jin Linhong. TIMS-U series dating of a stalagmate from Zhengjiadong cave in Guizhou and its paleoclimatic implications[J]. Carsologica Sinica,1997,16(1):11～18]
[15]	覃嘉铭, 袁道先, 林玉石等.桂林全新世石笋高分辨率δ¹³C记录及其古生态意义[J].第四纪研究,2000,20(4): 351～358[Qin jiaming,Yuan Daoxian, Lin Yushi, et al.High resolution records of δ¹³C and its paleoecology significance from stalagmite formed in Holocene in Guilin[J]. Quaternary Sciences, 2000,20(4):351～358]
[16]	林玉石, 张美良, 覃嘉铭.桂林盘龙洞石笋地质时代与环境[A]. 岩溶与人类生存、环境、资源和灾害[C]. 广西桂林:广西师范大学出版社,1996. 71～81[ Lin Yushi, Zhang Meiliang, Qin jiaming. Geological age and Paleo-environmental Records of a stslagmite from the Panlongdong cave, Guilin[A]. Karst and Human Survival, Environment, Resources, and Hazards[C]. Guilin, Guangxi: Teachers University Press, 1996. 71～81]

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Study on Laminae or Lamella Groups and Types of Stalagmite in Caves

Institute of Karst Geology,CAGS,Guilin Guangxi,541004

Received Date: 2001-05-28

Rev Recd Date: 2001-08-30

Key words:

Abstract: Stalagmite is a typical dripstone shape of CaC0₃ in caves and the most comprehensive and systematical paleoclimate environment in for mation carrier too. With advances of dating techniCues and analytic methods with high resolution，it is of great significance in the paleoclimate environment reconstruction. The combi nation，thickness，grain size and bedding plane structure of depositional laminae in stalagmite are the material base to resume droping water trends of for ming stalagmite and the related paleo- hydrological conditions. 0n the basis of the analysis and study of many stalagmite vertical profiles and systematic isotopic compositions,trace elements and specific laminae，it has been demonstrated that stalagime sedimentary laminae have obvious rhythmic combination,sedimentary cycles and indication of paleoclimatic environments. It is firstly put for ward that stalagmite is of lamina groups of cone in cone,cone and pillar,cone i n cone and pillar combined types and with the sediment ary structures,such as continuity,cycle,disconnected and compound lamina types. The paper discusses their indivitual charatersitics，trends of dropping and flow water and evolutionary characteristics of climatic environments.

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Reference (16)

[1]	张美良,林玉石,覃嘉铭等.桂林水南洞石笋的沉积学特征[J]. 沉积学报,1999,17(2):233～239 [Zhang Meiliang, Lin Yushi, Qin jiaming,Sedimentological characteristics of a stalagmite from Shuinan cave, Guilin[J]. Acta Sedimentologica Sinica, 1999,17(2):233～239]
[2]	谭明, 潘根兴, 王先锋等.石笋与环境-石笋纹层形成的环境机理初探[J]. 中国岩溶,1999,18 (3):197～206 [Tan Ming, Pan Genxing, Wang Xianfeng et al,Stalagmites and Environment-Preliminary study on the formation of laminated stalagmites[J]. Carsologica Sinica,1999,18(3):197～206]
[3]	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,1995,18(3): 1 210～1 213[Yuan Daoxian. Sensitivity of karst process to environmental change and its record[J].Chinese Science Bulletin, 1995, 40(13):1 210～1 213]
[4]	杨明德, 谭明, 梁虹. 喀斯特流域水文地貌系统[M]. 北京:地质出版社,1998.24～34[ Yang Mingde,Tan Ming,Liang Hong.Hydrogeomorphologicial system of karst drainage basin[M]. Beijing: Geological publishing house,1998.24～34]
[5]	覃嘉铭. 古气候变化的石笋同位素记录-以桂林盘龙洞为例[J]. 地球学报,1997,18(3): 225～260 [Qin jiaming. Study on stalagmite isotope records of paleoclimatic changes[J].Acta Geoscientia Sinica.1997, 18(3): 255～260]
[6]	谭明, 秦小光, 刘东升.石笋记录的年际、十年、百年尺度气候变化[J].中国科学,1998,28(3):272～277 [Tan Ming, Qin Xiaoguang, Liu Dongsheng, et al. Interannual, decadal and century scale climatic changes revealed by stalagmite records[J]. Science in China, Series D, 1998, 41(4): 416～421 ]
[7]	李红春, 顾德隆, 陈文寄.利用洞穴石笋的δ^18O和δ¹³C重建3000年以来北京地区气候和古环境-石花洞研究系列之三[J]. 地震地质, 1997,19(1):71～85 [Li Hongchun, Ku The-lung, Chen Wenji, et al. Isotope studies of Shihua cave-Ⅲ:Reconstruction of paleoclimate and paleoenvironment of Beijing during the Last 3000 years from δ^18O and δ¹³C records in stalagmite[J]. Seismology And Geology,1997,19(1):77～86]
[8]	杨子赓, 牟昀智等. 北京猿人遗址综合研究[M]. 北京: 科学出版社,1985. 1～85 [Yang Zigeng, Mou Yunzhi. Synthetical study of Beijing-Man cave site[M]. Beijing:Scientific & Technical publishers,1985.1～85]
[9]	王丽娟. 桂林甑皮岩洞穴遗址第四纪孢粉分析[J].人类学报, 1989,8(1): 69～76 [Wang Lijuan.A Quaternary Sporo-pollen Analysis of Zengpiyan cave site,Guilin[J].Acta Anthropological Sinica,1989,8(1): 69～76]
[10]	黄万波.中国第四纪洞穴堆积[J].中国岩溶,1995,14(增刊):122～128 [Huang Wanbo. Quaternary cave accumulation in China[J]. Carsologica Sinica,1995,14(Supp.):122～128]
[11]	刘育燕.桂林甲宅太平岩洞穴石柱的古地磁年龄[J]. 中国岩溶, 1995,14(3) :247～250[Liu Yuyan. Paleogeomagnetic age of column from Taiping cave, Guilin[J]. Carsologica Sinica,1995,14(3):247～250]
[12]	赵树森, 刘明林, 乔广生. 中国东部喀斯特洞穴沉积物铀系年代[J]. 中国岩溶,1989,8(1): 53～61[ Zhao Shusen, Liu Minglin, Qiao Guangsheng. The U-series ages of speleothem of karst caves in east China[J]. Carsologica Sinica,1989,8(1):53～61]
[13]	汪训一.桂林茅茅头大岩洞穴沉积物的放射性年龄及氧、碳同位素特征[J]. 科学通报, 1985,30(2): 528～531[Wang Xunyi.Ages and characteristics of car bon and oxygen isotope of cave sediments from Maomaotoudayan cave in Guilin[J]. Chinese Science Bulletin,1985, 30(2): 528～531]
[14]	沈冠军.热电离质谱法测定贵州郑洞石笋的铀系年代及其古气候意义[J]. 中国岩溶, 1997,16(1):11～18[ Shen Guanjun, Bassem Gahleb, Jin Linhong. TIMS-U series dating of a stalagmate from Zhengjiadong cave in Guizhou and its paleoclimatic implications[J]. Carsologica Sinica,1997,16(1):11～18]
[15]	覃嘉铭, 袁道先, 林玉石等.桂林全新世石笋高分辨率δ¹³C记录及其古生态意义[J].第四纪研究,2000,20(4): 351～358[Qin jiaming,Yuan Daoxian, Lin Yushi, et al.High resolution records of δ¹³C and its paleoecology significance from stalagmite formed in Holocene in Guilin[J]. Quaternary Sciences, 2000,20(4):351～358]
[16]	林玉石, 张美良, 覃嘉铭.桂林盘龙洞石笋地质时代与环境[A]. 岩溶与人类生存、环境、资源和灾害[C]. 广西桂林:广西师范大学出版社,1996. 71～81[ Lin Yushi, Zhang Meiliang, Qin jiaming. Geological age and Paleo-environmental Records of a stslagmite from the Panlongdong cave, Guilin[A]. Karst and Human Survival, Environment, Resources, and Hazards[C]. Guilin, Guangxi: Teachers University Press, 1996. 71～81]

Study on Laminae or Lamella Groups and Types of Stalagmite in Caves

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