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地质论评  2006 

湖南衡东岭茶地区古近纪地层划分与中国早始新世哺乳动物群

Keywords: 下始新统岭茶组岭茶期哺乳动物群

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Abstract:

岭茶地区的古近纪地层常称为栗木坪组或岭茶组。根据哺乳动物化石、地层特征和新近的古地磁和碳同位素研究成果,本文将岭茶地区的古近纪地层分为上古新统栗木坪组和下始新统岭茶组。岭茶组典型剖面,可选在成家冲东北的岭茶―霞流公路旁。由于底部出现碳同位素负向漂移,是目前中国可确定的始新统/古新统界线。在中国早始新世哺乳动物中首次出现的哺乳动物有奇蹄类、偶蹄类、真正的灵长类和梳趾鼠类型的啮齿类,并有许多首现的属。根据哺乳动物群组成特征,将中国早始新世哺乳动物群分为两个组合带:以李官桥盆地大尖动物群为代表的岭茶晚期的犀貘一菱臼兽组合带(Heptodon--RhombomylusAssemblageZone)和以衡阳盆地岭茶动物群为代表的岭茶早期的始祖貘一软食中兽组合带(Homogalax--HapalodectesAssemblageZone)。

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