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藏南古近系柳区砾岩孢粉化石的发现及初步研究

DISCOVERY AND PRELIMINARY STUDY ON PALYNOFOSSILS FROM THE PALEOGENE LIUQU CONGLOMERATES IN SOUTHERN XIZANG(TIBET)

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【作者】 韦利杰刘小汉严富华麦学舜周学君李广伟刘小兵

【Author】 WEI Li-jie1,2) , LIU Xiao-han1) , YAN Fu-hua3) , MAI Xue-shun3) , ZHOU Xue-jun1) ,LI Guang-wei1) and LIU Xiao-bing1) 1) Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 1000852) Graduate University of Chinese Academy of Sciences,Beijing 1000393) Institute of Geology,China Earthquake Administration,Beijing 100029

【机构】 中国科学院青藏高原研究所中国科学院研究生院中国地震局地质研究所

【摘要】 作者首次对柳区砾岩夹层中的泥岩和泥质粉砂岩进行了孢粉学研究,共鉴定出52个形态属。其孢粉组合特征是:以被子植物花粉占优势(62.77%—83.19%),其次是裸子植物花粉(11.95%—32.31%),蕨类植物孢子最少(4.80%—10.38%)。被子植物花粉以具孔类为主,三孔沟或三沟类花粉在组合中有一定含量。裸子植物花粉以具双气囊类居多。孢粉植物群的总体特征表明其时代可能为古近纪晚期。当时的古植被为落叶阔叶林或针阔混交林,气候较温暖湿润,主要为暖温带的环境。

【Abstract】 This paper reports the first palynological study of interlayers of mudstones and mud-sandstone in the Liuqu Conglomerates.Fifty-two genera were identified in this palynological assesmblage.The assemblage are characterzed by the predominant angiosperm pollen grains(62.77%—83.19%) .The second common group is gymnosperm pollens(11.95%—32.31%) ,and pteridophyte spores are relatively rare(4.80%—10.38%) .Among the angiosperm pollens the most abundant are porate pollens,followed by tricolporate and tricolpate pollens in a moderate percentage.Bisaccate pollens dominate the gymnosperm pollens.The palynological assemblage from the Liuqu Conglomerates suggests a age of the Late Paleogene and a broad-leaved deciduous forest or mixed with conifer-broad-leaved forest,showing a warm-temperate climatic condition.

【基金】 国家自然科学基金重点项目(40631004)
  • 【文献出处】 微体古生物学报 ,Acta Micropalaeontologica Sinica , 编辑部邮箱 ,2009年03期
  • 【分类号】Q914
  • 【被引频次】12
  • 【下载频次】166
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