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Famennian ostracods from the Istanbul Zone (Gebze, Kocaeli, NW Turkey) and their paleogeographical relations

机译:伊斯坦布尔地区(盖布泽,科贾埃利,西北土耳其)的法门鳄类成龙及其古地理关系

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摘要

Famennian (Late Devonian) ostracods of the Thuringian Mega-Assemblage were recovered for the first time from three incomplete sections of the Ayineburnu Member of the Büyükada Formation in the Denizlik?y area (Gebze, NW Turkey), which were sampled for conodonts. Conodont faunas define an interval extending from the Upper rhomboidea? or Lower marginifera Zone into the Middle expansa Zone of the standard Upper Devonian conodont zonation. The ostracod faunas found here consist of -species mainly with thin-walls, long spines and often smooth surfaces such as Rectonaria, Tricornina' Orthonaria, Triplacera, Beckerhealdia, Timorhealdia' Bohemina, Paraberounella (and Acratia. These taxa indicate faunal relationship with Thuringia and the Rhenish Massif in Germany, the Cantabrian Mountains and Pyrenees in Spain, Holy Cross Mountains in Poland, North Africa and China.
机译:图林根巨型组合的Famennian(晚泥盆世)原虫是首次从Denizlik?y地区(Gebze,NW土耳其)的Büyükada组的Ayineburnu成员Ayineburnu成员的三个不完整部分中回收的,用于牙形体采样。牙形动物定义了从上菱形延伸的间隔?或下边缘区带进入标准上泥盆统牙形带分区的中扩展区。在这里发现的成虫类动物群主要由薄壁,长刺和经常光滑的表面组成,例如雷克托尼亚,特里科利纳的Orthonaria,Triplacera,Beckerhealdia,Timorhealdia'Bohemina,Paraberounella(和Acratia)。这些类群表明与图林根和德国的Rhenish地块,西班牙的Cantabrian山和比利牛斯山,波兰,北非和中国的圣十字山。

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