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《Chinese Journal of Geology》 1983-02
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THE DISCOVERY OF THE PICEA AND COELODONT A ANTIQUITALIS SYMBIONSIS IN TIANJIN AND ITS SIGNIFICANCES

Luo Bao-xin Wang Yu-zhao(Tianjin Institute of Geology and Mineral Resources)Huan Qiu-pu(Tianjin Geology Bureau)Yan Fu-hua(Institute of Seismology)Chai Chien-shing (Tianjin Museum of History)Ke Man-hong (Institute of Hydrogeology and Engineering Geology)  
The Picca spore-pollen complex of the late pleistocene was discovered and the Coelod.antiquitalis was detected in Tianjin city in 1978 (It was located in a bore hole at the depth of 42.5 meters and a Picea pollen complex at 42.4-40 meters).Their geological age is estimated to be about 40,000-10,000 or 22.800-22,000 Y.B.P..The Picea-Coelodonta fossil complex indicates that the air temperature at that time was about 11癈 lower than that of today and marine regression had occurred.But there were several reversed warm epochs during the regression period.For instance,an increase of Carpinus pollens of the broad leaf trees,24,400 and 22,900 Y.B.P.was identified.Perhaps the warm epoch implies a regional transgression of the sea.
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