Li Ping, Peng Zicheng, Wen Qibin, Li Yucheng, Yang Hui, Hong Ashi, Xu Zifeng, Wang Mingliang, He Jie, Diao Shaobo, Ye Yuguang. Study on the Stalagmite Age and the Paleotemperature of the Tian E Cave in Ninghua, Fujian, China[J]. Acta Sedimentologica Sinica, 1996, 14(1): 149-155.
| Citation:
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Li Ping, Peng Zicheng, Wen Qibin, Li Yucheng, Yang Hui, Hong Ashi, Xu Zifeng, Wang Mingliang, He Jie, Diao Shaobo, Ye Yuguang. Study on the Stalagmite Age and the Paleotemperature of the Tian E Cave in Ninghua, Fujian, China[J]. Acta Sedimentologica Sinica, 1996, 14(1): 149-155.
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Study on the Stalagmite Age and the Paleotemperature of the Tian E Cave in Ninghua, Fujian, China
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Li Ping1
,
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Peng Zicheng1
,
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Wen Qibin2
,
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Li Yucheng2
,
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Yang Hui2
,
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Hong Ashi3
,
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Xu Zifeng3
,
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Wang Mingliang2
,
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He Jie4
,
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Diao Shaobo4
,
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Ye Yuguang4
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1 University of Science and Technology of China, Hefei 230026;
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2 State Key Laboratory of Gas Geochemistry, Lanzhou 730000;
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3 The Third Institute of National Marine Bureau. XiaMen 361005;
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4 Institute of Marine Geology, Qingdao 266071
- Received Date: 1994-12-02
- Publish Date:
1996-03-10
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Abstract
The δ18O change and the age of the stalagmite of the Tiane cave in Ninghua, Fujian Province, are corresponding to that of the V28-238 core of the deep sea. The growth period of the stalagmite began (1.8-25)×104 years ago and belonged to the Middle Pleistocene Epoch. The paleoclimate change in Ninghua area, Fujian, synchronizes with that in the globe and is the same as that in the Taiwan strait and the South China sea.
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References
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