The Y. D. and climate abrupt events in the early and middle Holocene: Stalagmite oxygen isotope record from Maolan, Guizhou, China
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- 作者：Jiaming Qin (1)
Daoxian Yuan (1)
Hai Cheng (2)
Yushi Lin (1)
Meiliang Zhang (1)
Fuxing Wang (1)
R. L. Edwards (2)
Hua Wang (1)
Jingcheng Ran (3) - 关键词：sotope record ; climate event ; stalagmite ; Libo ; Guizhou
- 刊名：Science China Earth Sciences
- 出版年：2005
- 出版时间：April 2005
- 年：2005
- 卷：48
- 期：4
- 页码：530-537
- 全文大小：161KB
- 参考文献：1. Petter, D., Global Younger Dryas? Quaternary International, 1995, 28: 93-04. CrossRef
2. Fairbanks, R. G., The age and origin of the “Younger Dryas climate event-in Greenland ice cores, Paleoceanography, 1990, 5(6): 937-48. CrossRef
3. Yang Zhihong, Yao Tandong, Huang Cuilan et al., The record of Y.D. event in Guliya ice core, Chinese Science Bulletin (in Chinese), 1997, 42(18): 1975-978.
4. Yao Tandong, Abrupt climate change on the Tibetan Plateau during the last glacial, Science in China, Ser. D, 1999, 42(4): 358-68.
5. Tarlor, K. C., Lamorey, G. W., Doyle, G. A. et al., The flickering switch of late Pleistocene climate change, Nature, 1993, 361: 432-36. CrossRef
6. Johnsen, S. J., Clausen, H. B., Dansgaard, W. et al., Irregular glacial interstadials recorded in a new Greenland ice core, Nature, 1992, 359: 311-13. CrossRef
7. Wang, Y. J., Cheng, H., Edwards, R. L. et al., A high-resolution absolute-dated late Pleistocene monsoon record from Hulu cave China, Science, 2001, 294: 2345-348 CrossRef
8. Bond, G., Showers, W., Cheseby, M. et al., A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates, Science, 1997, 278: 1257-266. CrossRef
9. McDermott, F., Mattey, D. P., Hawkesworth, Chris, Centennial-scale Holocene climate variability revealed by a high-resolution speleothem δ 18O record from SW Ireland, Science, 2001, 294: 1328-331. CrossRef
10. Baldini,James, U. L., McDermott, F., Fairchild, Ian, J., Structure of the 8200-year cold event revealed by a speleothem trace element record, Science, 2002, 296: 2203-206. CrossRef
11. Qin Jiaming, Yuan Daoxian, Lin Yushi et al., Isotopic records of stalagmites from Guilin since 44 ka BP and their environmental interpretation, Acta Geoscientia Sinica (in Chinese), 2000, 21(4): 407-16.
12. Zhang Meiliang, Yuan Daoxian, Lin Yushi et al., The records of climatic change from stalagmite in Xiashuilong cave of Xuanwei city since 46 ka, Acta Sedimentologica Sinica (in Chinese), 2002, 20(1): 124-28.
13. Qin Jiaming, Yuan Daoxian, Lin Yushi et al., Records of high- resolution climate events from stalagmites since 160000 aBP in Guangxi and Guizhou, China, Earth Science Frontiers (in Chinese), 2001, 18(1): 99-05.
14. Wu Jiangying, Wang Yongjin, Cheng Hai et al., A high-resolution stalagmite O-C isotope record from Nanjing and its rapid response to climatic events, Chinese Science Bulletin, 2002, 47(2): 139-43.
15. Huang Junhua, Hu Chaoyong, Zhou Qunfeng, High resolution carbon and oxygen isotope records from stalagmite and palaeo-climatein Heishangdong cave, Qingjiang, Hubei Province, Earth Science-Journal of China University of Geosciences (in Chinese), 2000, 25(5): 505-09.
16. Stuiver, M., Braziunas, T. F., Grootes, P. M. et al., Is there evidence for solar forcing of climate in the GISP2 oxygen isotope record?, Quaternary Research, 1997, 48: 259-66. CrossRef
17. Stuiver, M., Grootes, P. M., Braziunas, T. F., The GISP2 18O climate record of the past 16,500 years and the role of the sun, ocean and volcanoes, Quaternary Research, 1995, 44: 341-54. CrossRef
18. Dansgaard, W., Johnsen, S. J., Clausen, H. B. et al., Evidence for general instability of past climate from a 250-ka ice-cores record, Nature, 1993, 364: 218-20. CrossRef
19. 19 Klitgaard-Kristensen, D., Sejrup, H. P., Haflidason, H. et al., A regional 8200 cal. a BP cooling event in northwest Europe, induced by final stages of the Laurentide ice-sheel deglaciation?, J. Quat. Sci., 1998, 13: 165-69. CrossRef - 作者单位：Jiaming Qin (1)
Daoxian Yuan (1)
Hai Cheng (2)
Yushi Lin (1)
Meiliang Zhang (1)
Fuxing Wang (1)
R. L. Edwards (2)
Hua Wang (1)
Jingcheng Ran (3)
1. The Karst Dynamic Laboratory, 541004, IKG, CAGS, Guilin, China
2. Geology and Geophysics Department, Minnesota University, 55455, MN, USA
3. The Management of Maolan National Nature Reserve, 558400, Libo, China - ISSN：1869-1897
文摘
The isotope records which range from 3.9 kaBP to 15.7 kaBP with an average resolution of 90 a have been obtained from 45 cm to 193.6 cm of the upper part of D4 stalagmite from Dongguo Cave in Libo, Guizhou, by using system TIMS U-series dating and carbon and oxygen stable isotope analyses.The study indicates that the last cold event, the YD (Younger Dryas) event, of the last glacial period was apparently shown in D4 record, which started from 12.80 kaBP and ended in 11.58 kaBP, with a great range of drop in temperature. The end of the last glacial period was consistent with the termination I in oceanic isotope records and was with time limit of 11.3 kaBP. The three most distinct cold events in the early and middle Holocene occurred respectively in 10.91 kaBP, 8.27 kaBP and 4.75 kaBP, with a range of drop in temperature reaching 2-°C. The climate abrupt events in thousand and hundred years scale recorded in stalagmite δ 18O can be compared to those in GISP2 ice cores from Greenland in their happening time and the range of their lasting time. The cold events in 8.27 kaBP and 4.75 kaBP can also be compared to CC3 stalagmite records in Ireland, which indicate that climate changes of short range in China monsoon areas, western Europe and polar regions, have the same driving factor. This has a global significance. In addition, the trend of record curves in some time- stages is apparently different, which reflects probably the difference between environment in monsoon climate areas and in polar regions.