[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δ18O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 δ18O 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]