The Record of Paleoclimatic Change and the Termination of the Last Interglacial Period From A Stalagmite of Qingxin Cave in South Guizhou

ZHANG Mei-liang; LIN Yu-shi; QIN Jia-ming; ZHANG Cheng; TU Lin-lin; CHENG Hai

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(3): 473-481

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming, ZHANG Cheng, TU Lin-lin, CHENG Hai. The Record of Paleoclimatic Change and the Termination of the Last Interglacial Period From A Stalagmite of Qingxin Cave in South Guizhou[J]. Acta Sedimentologica Sinica, 2003, 21(3): 473-481.

Citation:

The Record of Paleoclimatic Change and the Termination of the Last Interglacial Period From A Stalagmite of Qingxin Cave in South Guizhou

1.
Karst Dynamics Laboratory,Institute of Karst Geology,CAGS, Guilin Guangxi 5 41004;
2.
Geography Department, Minnesota University, MN55455,USA

Received Date: 2002-06-25
Rev Recd Date: 2002-08-27
Publish Date: 2003-09-10

Abstract

Under the predictive study of the global climate change at present, the dating ages of the high-resolution and the change law revealed by the carbon and oxy ge n isotopic composition from cave stalagmites have made a great contribution for the breakthrough and filling gaps in this field. The high-resolution cl im ate records from 109.00 ka B.P. to 65.90 ka B.P. have been obtained through TIMS -U series dating of 11 samples and carbon and oxygen isotopic analysis of 79 sampl es from No.1 stalagmites in the south part of Guizhou. The No.1 stalagmite began to grow before 109.00 ka B.P. and stopped to grow after 65.90 ka B.P.,its ave rag e growth rate is 4.58mm/100a and is the sediment of the late Pleistocene. The st udy of No.1 stalagmite section in the Qingxin cave reveals that its age and isot ope records can be compared with the oxygen isotopic records of deep-sea cores or sediments at 5a, 5b and 5c phase of Ⅴstage and Ⅳ stage and Lishi Loess beds(L2) in the north of China. The carbon and oxygen isotopic records of stalagmite reveal that these tw o stages between 109.0～102.5 ka B.P. and 86.6～82.0 ka B.P. represented the war m-humid climatic environment and indicated the strong influence of the Asian (Southeast) summer monsoon, the rainfall increased more,the δ ¹⁸ O trende d to lowre or negative and the air temperature rose.The stage from 102.5 ka B.P. to 86.6 ka B.P. represented the cold-cool semi-arid and warm-cool humid cli matic envi ronment and indicated that the Asian (Southeast) summer monsoon was gradually weak, the meteoric water was decreased gradually, the δ ¹⁸ O was much h e avier, and the air temperature gradually decreased. And the stage from 78.92 ka B.P. t o 65.90 ka B.P. represented the dry-cold climatic environment and indicated tha t t he Asian (Southeast) winter monsoon and the Northwest cold air mass were streng thened, the meteoric water was decreased gradually, the δ ¹⁸ O was much hea vier, a nd the air temperature went down quickly,and is the cold beginning period of the last glacial period. In addition, we have determined that the termination point of the last intergla c ial period is 78.92±0.7 ka B.P.,and this age is the beginning point of the las t glacial period at the same time and can be taken as the boundary age of MIS4/5 according to the precise dating age of TIMS-U series and the records of carbo n and oxygen isotopes from No.1 stalagmite of Qixin cave in Guizhou. The determina tion of the record chronological is not only of stratigraphic significance, but also is chronological significance.
- stalagmites,
- TIMS-U series ages,
- paleoclimate,
- termination point of the last interglacial peri- od,
- Qingxin cave of the south Guizhou

References

[1]	Hendy C H. The isotopic geochemistry of speleothems and its application to the study of past climates,Ph.D.C.Thesis,Victoria University,Wellington,New Zealand,1969.1～10
[2]	Hendy C H.The isotopic geochemistry of speleothems-Pt.I The calculation of the effects of different model of formation on the isotopic composition of speleothems and their applicability as pa1eoclimate indictors[J].Geochim.et Cosmochim. Acta,1971,35:801～824
[3]	Talma A S, Vogel J C.Late Quaternary paleotemperatures derived from a speleothem from Cango caves,Cape province,South Africa[J].Quaternary Research,1992,37:203～213
[4]	Winograd I J,Coplen T B,Landwehr J M, et al. Continuous 500000一year climate record from vein calcite in Devils Hole,Nevada[J]. Science,1992,258:255～260
[5]	Holmgren K, Karlen W. Paleoclimatic significance of the stable isotopic composition and petrology of a Late Pleistocene stalagmite from Botswana[J]. Quaternary Research,1995,43:320～328
[6]	Bar-Matthews M, Ayalon A.Late Quaternary paleoclimate in the Eastern Mediterranean region from stable isotope analysis of speleothems at Soreq cave,Israel[J].Quaternary Research,1997,47:155～168
[7]	Lauritzen S E, Onac B P. Isotopic stratigraphy of a last interglacial stalagmite from Northwestern Romania: Correlation with the deep-sea record and northern-latitude Speleothem[J]. Journal of Cave and Karst Studies,1999,61(1):22～30
[8]	McDermott F, Mattey D P, Hawkesworth C. Centenial-scale Holocene climate variability revealed by a high-resolution speleothem δ18O record from SW Ireland[J]. Science,2001,294:1 328～1 331
[9]	Baldini J U L, McDermott F, Fairchild I J. Structure of the 8200-year cold event revealed by a speleothem trace element record[J]. Science, 2002,296:2 203～2 206
[10]	赵树生,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,1990,9(3): 279～288[Zhou Shusen, Liu Mingli,Qiao Guangsheng. The U-series ages of speleothem of karst caves in the East of China[J]. Carsologica Sinica,1990,9(3):279～288]
[11]	张寿越. 中国大陆东部洞穴沉积物的230Th/ 234 U 年代及古环境研究[J]. 地球科学:武汉地质学院学报,1985,10(1):65～72[Zhang Shouyue, Zhao Shusen. The U-series ages of speleothem of karst caves in east China[J].Earth Science-Journal of Wuhan College of Geology 1985, 10(1): 65～72]
[12]	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 the carbon and oxygen isotope of cave sediments from Maomaotoudayan cave in Guilin[J]. Chinese Science Bulletin,1985, 30(2): 528～531]
[13]	朱学稳,汪王训一,朱德浩等. 桂林岩溶地貌与洞穴研究[M].北京:地质出版社,1988.96～117[Zhu Xuewen,Wang Xunyi, Zhu Dehao, et al. Study on karst geomorphology and caves in Guilin[M]. Beijing: Geological Publishing House,1988.96～117]
[14]	朱洪山, 张巽. 44万年以来北京地区石笋古温度记录[J]. 科学通报,1992,20: 1 880～1 884[Zhu Hongshan, Zhang Zhuan. Paleo-temperature record from stalagmites since 440 ka.B.P in the area of Beijing[J]. Chinese Science Bulletin,1992,20:1 880～1 884]
[15]	李红春,顾德隆,陈文寄等. 利用洞穴群的δ18O和δ¹³C重建3 000 a以来北京地区古气候和古环境-石花洞研究系列之三[J]. 地震地质,1997,19(1):77～85[ Li Hongchun, Ku The-lung, Chen Wenji, et al. Isotope studys 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):77～85]
[16]	李红春,顾德隆,陈文寄等. 高分辨率洞穴石笋中稳定同位素应用-北京元大都建立后对森林资源的破坏-δ¹³C记录[J].地质论评,1998,44(5):456～462[Li Hongchun, Ku Delung, Chen Wenji, et al. Application of high-resolution carbon isotope record of a stalagmite from the Shihua cave,Beijing-δ¹³C record of deforestation after the establishment of the Grand capital(Yuan Dadu) in 1271 A.D.[J]. Geological Review, 1998,44(5):456～462]
[17]	谭明,刘东升,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):1～10[Tan Ming,Liu Dongsheng, Qin Xiaoguang, et al. Preliminary study on the data from microbanding and stable isotopes of stalagmites of Beijing Shihua Cave[J]. Carsologica Sinica,1997,16(1):1～10]
[18]	秦小光,刘东升,谭明等. 北京石花洞石笋微层尺度变化特征及气候意义-1. 微层显微特征[J]. 中国科学(D辑),1998,28(2):91～96[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]
[19]	李平,彭子成,文启彬等. 福建宁化天鹅洞石笋年代和古温度[J]. 沉积学报,1996,14(1):149～154[Li Ping, Peng Zicheng, Wen Qibin. Study on stalagmite age and the paleotemperature of Tian'E cave in Ninghua, Fujian, China[J]. Acta Sedimentologica Sinica,1996,14(1):149～154]
[20]	林钧枢,张耀光等. 瑶琳洞形成与环境研究[M]. 北京: 中国科学技术出版社,1993. 74～100[Lin Junshu, Zhang Yaoguang, et al. Reseacrch on origin and environment of Yaolin cave in China[M]. Beijing: China Sciences & Techonology Press, 1993. 74～100]
[21]	汪永进,吴江莹,许汉奎等. 南京汤山洞穴石笋稳定同位素指示的气候与环境意义[J]. 地质学报,2000,74(4):333～338[ Wang Yongjin, Wu Jiangying, Xu Hankui, et al. Palaeoclimatic and environmental significance as indicated by the stable isotopic composition of cave stalagmite in Tangshan,Nanjing[J]. Acta Geologica Sinica,2000,74(4):333～338]
[22]	汪永进,吴江莹, 吴金全. 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[Wang Yongjin, Wu Jiangying, Wu Jinquan, et al. Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation[J].Science in China, Ser. D, 2001,40(1):14～21]
[23]	Wang Yunjing, Cheng Hai,Edwards R L, et al. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu cave,China[J]. Science, 2001, 294(14): 2 345～2 348
[24]	Yuan Daoxian. Sensitivity of karst process to environmental change along the PEP-ⅡTransect, Quternary International,Printed in Great Britain,1997,37:105～113
[25]	袁道先,覃嘉铭,林玉石等. 桂林20万年石笋高分辨率古环境重建[M]. 广西桂林:广西师范大学出版社,1999. 32～56[ Yuan Daoxian, Qin Jiaming,Lin Yushi, et al. High resolution paleoenvironmental reconstrction up to 200,000 years B.P. with speleothems from Guilin[M]. Guilin Guangxi: Teachers University Press, 1999. 32～56]
[26]	覃嘉铭等, 袁道先,林玉石等. 我国南方黔桂地区最近16万年高分辨率石笋记录的气候事件[J]. 地学前缘, 2001,8(1): 99～105[ Qin jiaming,Yuan Daoxian, Lin Yushi, et al. Records of high-resolution climate events from stalagmites since 160 000a B.P. in Guangxi and Guizhou provinces,China[J]. Earth Science Frontiers, 2001,8(1): 99～105]
[27]	李彬,袁道先, 覃嘉铭等. 桂林地区降水、洞穴滴水及现代洞穴碳酸盐碳氧同位素研究及其环境意义[J]. 中国科学,D辑,2000,30(1):81～87[Li Bin, Yuan Daoxian, Qin Jiaming, et al. Oxygen and carbon isotopic characteristics of rainwater,drip water and present speleothems in a cave in Guilinarea,and their environmental meanings[J]. Science in China(Series D),2000,43(3):276～285]
[28]	林玉石,张美良,覃嘉铭等. 云南宁蒗泸沽湖地区的古环境重建[J]. 中国岩溶,2001,20(3):174～182[Lin Yushi,Zhang Meiliang,Qin Jiaming, et al. The record of paleoclimatic environment in Lugu lake area of Linlan county,Yuannan[J]. Carsologica Sinica, 2001,20(3):174～182]
[29]	郑淑蕙,侯发高,倪葆龄. 我国大气降水的氢氧同位素研究[J]. 科学通报,1983,28(3):801～806[ Zheng Shuhui,Hou Fagao,Ni Baoling. Study on the stable hydrogen and oxygen isotope of the air precipitation in China[J]. Chinese Science Bulletin, 1983, 28(3):801～806]
[30]	Liu Enchun. Sequence of sediments at locality in Zhoukoudian and correlation with loess stratigraphy in Northern China and with the chronology of deep-sea cores[J]. Deep Sea Res., 1985, 23 :139～153
[31]	Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial pacific core V28～238: Oxygen isotope temperature and ice Volumes on a 10 year and 105 year scale [J]. Quaternary Research,1973,3:39～55
[32]	张美良,袁道先,林玉石. 贵州董哥洞3号石笋的年龄及其古气候信息[J].沉积学报,2001,19(3): 425～432[Zhang Meiliang,Yuan Daoxian, Lin Yushi, et al. Isotopic ages and paleocliamtic implications of No.3 stalagmite from Dongge cave in Libo[J]. Acta Sedimentologica Sinica, 2001, 19(3):425～432]
[33]	张美良,林玉石,覃嘉铭. 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 Jiamin. Sedimentological characteristics of a stalagmite from Shuinan cave,Guilin[J]. Acta Sedimentologica Sinica, 1999,17(2):233～239]
[34]	孙建中,赵景波.黄土高原第四纪[M]. 北京: 科学出版社,1991. 46～77[ Sun Jianzhong, Zhao Jingbo,et al. Quaternary of loss plateau in China[M]. Beijing: Science Press, 1991.46～77]
[35]	Martinson D G, Pisias N J, Hays J D, et al. Age dating and the orbital theory of ice ages: development of a high-resolution 1 to 300 000 years chronostratigraphy[J]. Quaternary Research,1987,27(1): 1～29.
[36]	Imbrie J, Hays J D, Martinson D G, et al. The Orbital theory of Pleistocene climate: support from a revised chronology of the marine δ18O record[A]. In: Berger A, Imbrie J, Hays J D, et al, eds. Milankovich and Climate (Part 1)[C]. Norwell MA: Reidel Press,1984. 269～305
[37]	冯文科,黎维峰. 南海北部深海平原晚更新世以来沉积环境和古气候变化[J]. 海洋地质与第四纪地质,1986,6(3): 9～24[ Feng Wenke, Li Weifeng. Sedimentary environment and paleoclimate in Northern south China sea since late Pleistocene[J]. Marine Geology & Quaternary, 1996, 6(3): 9～24]
[38]	姚檀栋, Thompson L G, 施雅风等. 古里雅冰芯中末次间冰期以来气候变化记录研究[J]. 中国科学(D),1997,27(5):447～452[Yao Tandong, Thompson L G, Shi Yafeng, et al. Study on the record of climatic change since the last interglacial period in the Guliya ice core of Qinghai-Tibetan plateau[J]. Science in China(Series D), 27(5):447～452]
[39]	李静,王玉海. 黄土沉积的地球化学记录与古气候演化[J]. 海洋地质与第四纪地质,1998,18(2):41～47[Li Jing, Wang Yuhai. The geochemical record of Loess deposit and paleoclimatic evolution[J]. Marine Geology & Quaternary,1998, 18(2):41～47]
[40]	余素华,朱照宇,李丙元等. 23万年以来青藏高原甜水海湖岩芯铁元素的气候记录刍义[J].海洋地质与第四纪地质,1998,18(3):63～70[ Yu Suhua, Zhu Zhaoyu, Li Bingyuan, et al. The climate records from variations of iron oxides since 230kaB.P. in the cores from Tianshuihai lake of Qinghai-Xizang plateau[J]. Marine Geology & Quaternary, 1998,18(3):63～70]
[41]	羊向东,王苏民,童国榜等. 云南鹤庆古湖晚更新世的孢粉记录及其古气候意义[J]. 第四纪研究,1998,(4): 335～343[ Yang Xiangdong,Wang Sumin,Tong Guobang, et al.The late Pleistocene pollen record in the lake sediments from ancient Heqing lake and its significance for palaeoclimate[J]. Quaternary Sciences, 1998, 4:335～343]
[42]	孙湘君,罗运利. 南海北部280ka以来深海花粉记录[J]. 中国科学(D辑),2001,31(10):846～853[ Sun Xiangjun, Lou Yunli. Pollen record of the last 280 ka from deep sea sediments of the northern South China Sea[J]. Science in China(Series D),2001,44(10):879～889]
[43]	薛滨,王苏民,吴敬禄等. 青藏高原东北部末次间冰期以来的古气候-以若尔盖盆地RM孔分析为例[J]. 海洋与湖沼,1999,30(3):327～332[ Xue Bin,Wang Sumin, Wu Jinglu, et al. Paleoclimate of Northeastern Qinghai-Xizang Plateau since last interglaciation- A case study from core RM of the Zoige basin[J]. Oceanologia et Limnologia Sinica, 1999,30(3):327～332]
[44]	李吉均,朱俊杰,康健成等. 末次冰期旋回兰州黄土剖面与南极东方站岩芯对比[J]. 中国科学(B辑),1990,(10):1 086～1 094[ Li Jijun, Zhu Junjie, Kang Jiancheng, et al. Comparison of Loess profile in Lanzhou and Vostok ice core during last interglaciation cycle[J]. Science in China(Series B, in Chinese), 1990,(10):1 086～1 094]
[45]	靳鹤龄,董光荣,李森等. 800ka B.P.来西藏"一江两河"中游地区的气候与西南季风变化[J]. 中国沙漠, 1996,16(1):9～12[ Jin Heling,Dong Guangrong, Li Sen, et al. The climate and Southwest monsoon change in the middle "one river two tributaries"basin,Tibet since 0.8Ma B.P.[J]. Journal of Desert Research, 1996,16(1):9～12]
[46]	黄阿实,彭子成,李平等. 福建宁化天鹅洞石笋晚第四纪同位素古温度研究[J]. 地球化学,1995,24(2):138～145[ Hong Ashi, Peng Zicheng, Li Ping, et al. A study on late Quaternary isotopic paleo-temperature of stalagmite from Tian'E Cave at Ninghua county, Fujian[J]. Geochemica, 1995,24(2):138～145]

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article Metrics

Article views(716) PDF downloads(425) Cited by()

Proportional views

The Record of Paleoclimatic Change and the Termination of the Last Interglacial Period From A Stalagmite of Qingxin Cave in South Guizhou

1. Karst Dynamics Laboratory,Institute of Karst Geology,CAGS, Guilin Guangxi 5 41004;

2. Geography Department, Minnesota University, MN55455,USA

Received Date: 2002-06-25

Rev Recd Date: 2002-08-27

Publish Date: 2003-09-10

Key words:

stalagmites /
TIMS-U series ages /
paleoclimate /
termination point of the last interglacial peri- od /
Qingxin cave of the south Guizhou

Abstract: Under the predictive study of the global climate change at present, the dating ages of the high-resolution and the change law revealed by the carbon and oxy ge n isotopic composition from cave stalagmites have made a great contribution for the breakthrough and filling gaps in this field. The high-resolution cl im ate records from 109.00 ka B.P. to 65.90 ka B.P. have been obtained through TIMS -U series dating of 11 samples and carbon and oxygen isotopic analysis of 79 sampl es from No.1 stalagmites in the south part of Guizhou. The No.1 stalagmite began to grow before 109.00 ka B.P. and stopped to grow after 65.90 ka B.P.,its ave rag e growth rate is 4.58mm/100a and is the sediment of the late Pleistocene. The st udy of No.1 stalagmite section in the Qingxin cave reveals that its age and isot ope records can be compared with the oxygen isotopic records of deep-sea cores or sediments at 5a, 5b and 5c phase of Ⅴstage and Ⅳ stage and Lishi Loess beds(L2) in the north of China. The carbon and oxygen isotopic records of stalagmite reveal that these tw o stages between 109.0～102.5 ka B.P. and 86.6～82.0 ka B.P. represented the war m-humid climatic environment and indicated the strong influence of the Asian (Southeast) summer monsoon, the rainfall increased more,the δ ¹⁸ O trende d to lowre or negative and the air temperature rose.The stage from 102.5 ka B.P. to 86.6 ka B.P. represented the cold-cool semi-arid and warm-cool humid cli matic envi ronment and indicated that the Asian (Southeast) summer monsoon was gradually weak, the meteoric water was decreased gradually, the δ ¹⁸ O was much h e avier, and the air temperature gradually decreased. And the stage from 78.92 ka B.P. t o 65.90 ka B.P. represented the dry-cold climatic environment and indicated tha t t he Asian (Southeast) winter monsoon and the Northwest cold air mass were streng thened, the meteoric water was decreased gradually, the δ ¹⁸ O was much hea vier, a nd the air temperature went down quickly,and is the cold beginning period of the last glacial period. In addition, we have determined that the termination point of the last intergla c ial period is 78.92±0.7 ka B.P.,and this age is the beginning point of the las t glacial period at the same time and can be taken as the boundary age of MIS4/5 according to the precise dating age of TIMS-U series and the records of carbo n and oxygen isotopes from No.1 stalagmite of Qixin cave in Guizhou. The determina tion of the record chronological is not only of stratigraphic significance, but also is chronological significance.

HTML

Reference (46)

[1]	Hendy C H. The isotopic geochemistry of speleothems and its application to the study of past climates,Ph.D.C.Thesis,Victoria University,Wellington,New Zealand,1969.1～10
[2]	Hendy C H.The isotopic geochemistry of speleothems-Pt.I The calculation of the effects of different model of formation on the isotopic composition of speleothems and their applicability as pa1eoclimate indictors[J].Geochim.et Cosmochim. Acta,1971,35:801～824
[3]	Talma A S, Vogel J C.Late Quaternary paleotemperatures derived from a speleothem from Cango caves,Cape province,South Africa[J].Quaternary Research,1992,37:203～213
[4]	Winograd I J,Coplen T B,Landwehr J M, et al. Continuous 500000一year climate record from vein calcite in Devils Hole,Nevada[J]. Science,1992,258:255～260
[5]	Holmgren K, Karlen W. Paleoclimatic significance of the stable isotopic composition and petrology of a Late Pleistocene stalagmite from Botswana[J]. Quaternary Research,1995,43:320～328
[6]	Bar-Matthews M, Ayalon A.Late Quaternary paleoclimate in the Eastern Mediterranean region from stable isotope analysis of speleothems at Soreq cave,Israel[J].Quaternary Research,1997,47:155～168
[7]	Lauritzen S E, Onac B P. Isotopic stratigraphy of a last interglacial stalagmite from Northwestern Romania: Correlation with the deep-sea record and northern-latitude Speleothem[J]. Journal of Cave and Karst Studies,1999,61(1):22～30
[8]	McDermott F, Mattey D P, Hawkesworth C. Centenial-scale Holocene climate variability revealed by a high-resolution speleothem δ18O record from SW Ireland[J]. Science,2001,294:1 328～1 331
[9]	Baldini J U L, McDermott F, Fairchild I J. Structure of the 8200-year cold event revealed by a speleothem trace element record[J]. Science, 2002,296:2 203～2 206
[10]	赵树生,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,1990,9(3): 279～288[Zhou Shusen, Liu Mingli,Qiao Guangsheng. The U-series ages of speleothem of karst caves in the East of China[J]. Carsologica Sinica,1990,9(3):279～288]
[11]	张寿越. 中国大陆东部洞穴沉积物的230Th/ 234 U 年代及古环境研究[J]. 地球科学:武汉地质学院学报,1985,10(1):65～72[Zhang Shouyue, Zhao Shusen. The U-series ages of speleothem of karst caves in east China[J].Earth Science-Journal of Wuhan College of Geology 1985, 10(1): 65～72]
[12]	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 the carbon and oxygen isotope of cave sediments from Maomaotoudayan cave in Guilin[J]. Chinese Science Bulletin,1985, 30(2): 528～531]
[13]	朱学稳,汪王训一,朱德浩等. 桂林岩溶地貌与洞穴研究[M].北京:地质出版社,1988.96～117[Zhu Xuewen,Wang Xunyi, Zhu Dehao, et al. Study on karst geomorphology and caves in Guilin[M]. Beijing: Geological Publishing House,1988.96～117]
[14]	朱洪山, 张巽. 44万年以来北京地区石笋古温度记录[J]. 科学通报,1992,20: 1 880～1 884[Zhu Hongshan, Zhang Zhuan. Paleo-temperature record from stalagmites since 440 ka.B.P in the area of Beijing[J]. Chinese Science Bulletin,1992,20:1 880～1 884]
[15]	李红春,顾德隆,陈文寄等. 利用洞穴群的δ18O和δ¹³C重建3 000 a以来北京地区古气候和古环境-石花洞研究系列之三[J]. 地震地质,1997,19(1):77～85[ Li Hongchun, Ku The-lung, Chen Wenji, et al. Isotope studys 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):77～85]
[16]	李红春,顾德隆,陈文寄等. 高分辨率洞穴石笋中稳定同位素应用-北京元大都建立后对森林资源的破坏-δ¹³C记录[J].地质论评,1998,44(5):456～462[Li Hongchun, Ku Delung, Chen Wenji, et al. Application of high-resolution carbon isotope record of a stalagmite from the Shihua cave,Beijing-δ¹³C record of deforestation after the establishment of the Grand capital(Yuan Dadu) in 1271 A.D.[J]. Geological Review, 1998,44(5):456～462]
[17]	谭明,刘东升,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):1～10[Tan Ming,Liu Dongsheng, Qin Xiaoguang, et al. Preliminary study on the data from microbanding and stable isotopes of stalagmites of Beijing Shihua Cave[J]. Carsologica Sinica,1997,16(1):1～10]
[18]	秦小光,刘东升,谭明等. 北京石花洞石笋微层尺度变化特征及气候意义-1. 微层显微特征[J]. 中国科学(D辑),1998,28(2):91～96[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]
[19]	李平,彭子成,文启彬等. 福建宁化天鹅洞石笋年代和古温度[J]. 沉积学报,1996,14(1):149～154[Li Ping, Peng Zicheng, Wen Qibin. Study on stalagmite age and the paleotemperature of Tian'E cave in Ninghua, Fujian, China[J]. Acta Sedimentologica Sinica,1996,14(1):149～154]
[20]	林钧枢,张耀光等. 瑶琳洞形成与环境研究[M]. 北京: 中国科学技术出版社,1993. 74～100[Lin Junshu, Zhang Yaoguang, et al. Reseacrch on origin and environment of Yaolin cave in China[M]. Beijing: China Sciences & Techonology Press, 1993. 74～100]
[21]	汪永进,吴江莹,许汉奎等. 南京汤山洞穴石笋稳定同位素指示的气候与环境意义[J]. 地质学报,2000,74(4):333～338[ Wang Yongjin, Wu Jiangying, Xu Hankui, et al. Palaeoclimatic and environmental significance as indicated by the stable isotopic composition of cave stalagmite in Tangshan,Nanjing[J]. Acta Geologica Sinica,2000,74(4):333～338]
[22]	汪永进,吴江莹, 吴金全. 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[Wang Yongjin, Wu Jiangying, Wu Jinquan, et al. Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation[J].Science in China, Ser. D, 2001,40(1):14～21]
[23]	Wang Yunjing, Cheng Hai,Edwards R L, et al. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu cave,China[J]. Science, 2001, 294(14): 2 345～2 348
[24]	Yuan Daoxian. Sensitivity of karst process to environmental change along the PEP-ⅡTransect, Quternary International,Printed in Great Britain,1997,37:105～113
[25]	袁道先,覃嘉铭,林玉石等. 桂林20万年石笋高分辨率古环境重建[M]. 广西桂林:广西师范大学出版社,1999. 32～56[ Yuan Daoxian, Qin Jiaming,Lin Yushi, et al. High resolution paleoenvironmental reconstrction up to 200,000 years B.P. with speleothems from Guilin[M]. Guilin Guangxi: Teachers University Press, 1999. 32～56]
[26]	覃嘉铭等, 袁道先,林玉石等. 我国南方黔桂地区最近16万年高分辨率石笋记录的气候事件[J]. 地学前缘, 2001,8(1): 99～105[ Qin jiaming,Yuan Daoxian, Lin Yushi, et al. Records of high-resolution climate events from stalagmites since 160 000a B.P. in Guangxi and Guizhou provinces,China[J]. Earth Science Frontiers, 2001,8(1): 99～105]
[27]	李彬,袁道先, 覃嘉铭等. 桂林地区降水、洞穴滴水及现代洞穴碳酸盐碳氧同位素研究及其环境意义[J]. 中国科学,D辑,2000,30(1):81～87[Li Bin, Yuan Daoxian, Qin Jiaming, et al. Oxygen and carbon isotopic characteristics of rainwater,drip water and present speleothems in a cave in Guilinarea,and their environmental meanings[J]. Science in China(Series D),2000,43(3):276～285]
[28]	林玉石,张美良,覃嘉铭等. 云南宁蒗泸沽湖地区的古环境重建[J]. 中国岩溶,2001,20(3):174～182[Lin Yushi,Zhang Meiliang,Qin Jiaming, et al. The record of paleoclimatic environment in Lugu lake area of Linlan county,Yuannan[J]. Carsologica Sinica, 2001,20(3):174～182]
[29]	郑淑蕙,侯发高,倪葆龄. 我国大气降水的氢氧同位素研究[J]. 科学通报,1983,28(3):801～806[ Zheng Shuhui,Hou Fagao,Ni Baoling. Study on the stable hydrogen and oxygen isotope of the air precipitation in China[J]. Chinese Science Bulletin, 1983, 28(3):801～806]
[30]	Liu Enchun. Sequence of sediments at locality in Zhoukoudian and correlation with loess stratigraphy in Northern China and with the chronology of deep-sea cores[J]. Deep Sea Res., 1985, 23 :139～153
[31]	Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial pacific core V28～238: Oxygen isotope temperature and ice Volumes on a 10 year and 105 year scale [J]. Quaternary Research,1973,3:39～55
[32]	张美良,袁道先,林玉石. 贵州董哥洞3号石笋的年龄及其古气候信息[J].沉积学报,2001,19(3): 425～432[Zhang Meiliang,Yuan Daoxian, Lin Yushi, et al. Isotopic ages and paleocliamtic implications of No.3 stalagmite from Dongge cave in Libo[J]. Acta Sedimentologica Sinica, 2001, 19(3):425～432]
[33]	张美良,林玉石,覃嘉铭. 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 Jiamin. Sedimentological characteristics of a stalagmite from Shuinan cave,Guilin[J]. Acta Sedimentologica Sinica, 1999,17(2):233～239]
[34]	孙建中,赵景波.黄土高原第四纪[M]. 北京: 科学出版社,1991. 46～77[ Sun Jianzhong, Zhao Jingbo,et al. Quaternary of loss plateau in China[M]. Beijing: Science Press, 1991.46～77]
[35]	Martinson D G, Pisias N J, Hays J D, et al. Age dating and the orbital theory of ice ages: development of a high-resolution 1 to 300 000 years chronostratigraphy[J]. Quaternary Research,1987,27(1): 1～29.
[36]	Imbrie J, Hays J D, Martinson D G, et al. The Orbital theory of Pleistocene climate: support from a revised chronology of the marine δ18O record[A]. In: Berger A, Imbrie J, Hays J D, et al, eds. Milankovich and Climate (Part 1)[C]. Norwell MA: Reidel Press,1984. 269～305
[37]	冯文科,黎维峰. 南海北部深海平原晚更新世以来沉积环境和古气候变化[J]. 海洋地质与第四纪地质,1986,6(3): 9～24[ Feng Wenke, Li Weifeng. Sedimentary environment and paleoclimate in Northern south China sea since late Pleistocene[J]. Marine Geology & Quaternary, 1996, 6(3): 9～24]
[38]	姚檀栋, Thompson L G, 施雅风等. 古里雅冰芯中末次间冰期以来气候变化记录研究[J]. 中国科学(D),1997,27(5):447～452[Yao Tandong, Thompson L G, Shi Yafeng, et al. Study on the record of climatic change since the last interglacial period in the Guliya ice core of Qinghai-Tibetan plateau[J]. Science in China(Series D), 27(5):447～452]
[39]	李静,王玉海. 黄土沉积的地球化学记录与古气候演化[J]. 海洋地质与第四纪地质,1998,18(2):41～47[Li Jing, Wang Yuhai. The geochemical record of Loess deposit and paleoclimatic evolution[J]. Marine Geology & Quaternary,1998, 18(2):41～47]
[40]	余素华,朱照宇,李丙元等. 23万年以来青藏高原甜水海湖岩芯铁元素的气候记录刍义[J].海洋地质与第四纪地质,1998,18(3):63～70[ Yu Suhua, Zhu Zhaoyu, Li Bingyuan, et al. The climate records from variations of iron oxides since 230kaB.P. in the cores from Tianshuihai lake of Qinghai-Xizang plateau[J]. Marine Geology & Quaternary, 1998,18(3):63～70]
[41]	羊向东,王苏民,童国榜等. 云南鹤庆古湖晚更新世的孢粉记录及其古气候意义[J]. 第四纪研究,1998,(4): 335～343[ Yang Xiangdong,Wang Sumin,Tong Guobang, et al.The late Pleistocene pollen record in the lake sediments from ancient Heqing lake and its significance for palaeoclimate[J]. Quaternary Sciences, 1998, 4:335～343]
[42]	孙湘君,罗运利. 南海北部280ka以来深海花粉记录[J]. 中国科学(D辑),2001,31(10):846～853[ Sun Xiangjun, Lou Yunli. Pollen record of the last 280 ka from deep sea sediments of the northern South China Sea[J]. Science in China(Series D),2001,44(10):879～889]
[43]	薛滨,王苏民,吴敬禄等. 青藏高原东北部末次间冰期以来的古气候-以若尔盖盆地RM孔分析为例[J]. 海洋与湖沼,1999,30(3):327～332[ Xue Bin,Wang Sumin, Wu Jinglu, et al. Paleoclimate of Northeastern Qinghai-Xizang Plateau since last interglaciation- A case study from core RM of the Zoige basin[J]. Oceanologia et Limnologia Sinica, 1999,30(3):327～332]
[44]	李吉均,朱俊杰,康健成等. 末次冰期旋回兰州黄土剖面与南极东方站岩芯对比[J]. 中国科学(B辑),1990,(10):1 086～1 094[ Li Jijun, Zhu Junjie, Kang Jiancheng, et al. Comparison of Loess profile in Lanzhou and Vostok ice core during last interglaciation cycle[J]. Science in China(Series B, in Chinese), 1990,(10):1 086～1 094]
[45]	靳鹤龄,董光荣,李森等. 800ka B.P.来西藏"一江两河"中游地区的气候与西南季风变化[J]. 中国沙漠, 1996,16(1):9～12[ Jin Heling,Dong Guangrong, Li Sen, et al. The climate and Southwest monsoon change in the middle "one river two tributaries"basin,Tibet since 0.8Ma B.P.[J]. Journal of Desert Research, 1996,16(1):9～12]
[46]	黄阿实,彭子成,李平等. 福建宁化天鹅洞石笋晚第四纪同位素古温度研究[J]. 地球化学,1995,24(2):138～145[ Hong Ashi, Peng Zicheng, Li Ping, et al. A study on late Quaternary isotopic paleo-temperature of stalagmite from Tian'E Cave at Ninghua county, Fujian[J]. Geochemica, 1995,24(2):138～145]

The Record of Paleoclimatic Change and the Termination of the Last Interglacial Period From A Stalagmite of Qingxin Cave in South Guizhou

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related