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天津云杉孢粉组合与披毛犀化石共存的发现及其意义
引用本文:罗宝信,王毓钊,黄秋圃,严富华,翟乾祥,柯曼红.天津云杉孢粉组合与披毛犀化石共存的发现及其意义[J].地质科学,1983,0(2):160-164.
作者姓名:罗宝信  王毓钊  黄秋圃  严富华  翟乾祥  柯曼红
作者单位:1. 天津地质矿产所;2. 天津地质局;3. 国家地震局地质所;4. 天津历史博物馆;5. 水文与工程地质所
摘    要:云杉孢粉组合与披毛犀,这两类晚更新世的重要化石,过去在天津还没发现和正式报道过。近年来,不但已在天津找到,而且还发现它们同层共存于一个钻孔之中,这种同孔同层共存的事例,在我国还是首次发现,对研究该化石本身及天津当时的地质地理具有重要意义。

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收稿时间:1981-11-12
修稿时间:1981-11-12;

THE DISCOVERY OF THE PICEA AND COELODONT A ANTIQUITALIS SYMBIONSIS IN TIANJIN AND ITS SIGNIFICANCES
Luo Bao-xin,Wang Yu-zhao,Huan Qiu-pu,Yan Fu-hua,Chai Chien-shing,Ke Man-hong.THE DISCOVERY OF THE PICEA AND COELODONT A ANTIQUITALIS SYMBIONSIS IN TIANJIN AND ITS SIGNIFICANCES[J].Chinese Journal of Geology,1983,0(2):160-164.
Authors:Luo Bao-xin  Wang Yu-zhao  Huan Qiu-pu  Yan Fu-hua  Chai Chien-shing  Ke Man-hong
Institution:1. Tianjin Institute of Geology and Mineral Resources;2. Tianjin Geology Bureau;3. Institute of Seismology;4. Tianjin Museum of History;5. Institute of Hydrogeology and Engineering Geology
Abstract: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℃ 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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