1998•Unpublished venueRequires access

Study on the Paleoclimate and Sea Leave Change in Easthern China over 8×10 4 Years

Ustc Third

Abstract

The stable isotopes of carbon,hydrogen,oxygen in stalagmites of Zhoukoudian,Beijing and Lin An, Zhejiang were determined by the method of geochemistry for stable isotopes. The ages of the stalagmites were determined by U dating(Zhoukoudian) and by 14C dating(Ruijing cave). The records of paleoclimate evolution in Zhoukoudian (8—5×10 4a) and in Ruijing Cave (5—1×10 4a) are obtained, and compared with the curves of the sea level change of East China at the same period.

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Key concepts: Stalagmite, Paleoclimatology, Cave, Isotopes of oxygen, Geology, Beijing, Paleontology, China