摘要：祁连山和河西走廊区石炭纪地层发育,动植物化石丰富,是研究我国海陆交互相石炭系的重要地区.臭牛沟组系袁复礼(1925)所建,标准地点在甘肃武威西南35 km的臭牛沟,据其中的腕足类和珊瑚化石的研究,确定其时代为早石炭世维宪期(Visean).研究材料来自甘肃景泰和靖远的早石炭世臭牛沟组,这里的臭牛沟组厚约120 m左右,由泥质页岩夹煤线、粉砂岩及薄层泥灰岩、灰岩组成,为潮间潟湖相至滨海沼泽相及泥炭沼泽相沉积.含丰富的植物化石,主要分子有:Sublepidodendron sp.,Lepidodendron ciyaoense sp.nov.,Lepjingyuanense sp.nov., Lepidodendron volkmannianum, Lep. gansuense sp. nov., Lep. shanyangense, Lep. cf. aolungpulukense,Lep. sp. 1, Lep. sp. 2, Cathaysiodendron jingyuanense, C. cf. incertum, Stigmaria ficoides, Lepidostrobophyllum cf. lanceolatum, L. rotundi folium sp. nov. , Lepidostrobus sp. 1, L. sp. 2, Bothrodendron ruchengense , Archaeocalamites scrobiculatus , Hamatoph yton verticillatum , Cardiopteridium spetsbergense , C. podozamioides,Triphyllopteris collombiana , Triphyllopteris sp. ( cf. T. lescuriana Lesquereux), Rhacopteris sp. , Adiantites gothanii, Sphenopteris sp. 1, Sphenopteris sp. 2, Rhodeopteridium hsianghsiangense, R. cf. hsianghsiangense,R. cf. chinghaiense, Rhodeopteridium sp. (cf. R. lipoldi) , Paripteris gigantea, P. cardiopteroides, Linopteris sp. , Codonospermum sp. , Trigonocarpus spp. , Cardiocarpus cordai, Cordaites sp. (cf. C. schenkii Halle) . 其下伏地层前黑山组中有菊石Kazakhstania sp.,为下石炭统底部Gattendor fia带分子,其余还有孢子化石、腕足类和植物,表明为杜内期沉积;而上覆地层靖远组底部有牙形石Gnathodus bilineatus bollandensis,G.bilineatus bilineatus,Paragnathodus commutatus及P.nodosus,是我国下石炭统顶部德坞阶的一个牙形石带化石;(竹蜓)化石:Mediocris breviscula,M. pilatus,M.cf.minima,Eostaf fella galinae,E. cf.mediocris是我国和州组常见分子,也产于贵州罗�

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