首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >Meandropsinidae, an ophtalmidid family of Late Cretaceous K-strategist foraminifera endemic in the Pyrenean Gulf
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Meandropsinidae, an ophtalmidid family of Late Cretaceous K-strategist foraminifera endemic in the Pyrenean Gulf

机译:比目鱼Gulf科,一种在比利牛斯海湾流行的晚白垩纪K-战略家有孔虫科的甲虫科

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摘要

The Meandropsinids arc defined by their diaphanous umbo in their porcelaneous Shells that is always present at least in their microspheric generation. The extent of the development of their endoskeleton depends on the relative length of their apertural face of the spiral to annular chambers. The alar prolongations of the spiral chambers are Subdivided by ridges or complete septular walls arising from the basal layer of the chamber. These endoskeletal elements arc aligned in Subsequent chambers but interrupted by preseptal passages. All members of the family Meandropsinidae Occur within the Senonian and are restricted to the Late Cretaceous Pyrenean Gulf, except the most simple and small-sized members Nummofallotia and Eofallotia. In Spirapertolina and Larrazetia only microspheric specimens have been found. The large-sized members of the Meandropsinid family are interpreted as endemists in the Pyrenean Gulf in analogy to the larger sized representatives of the family Lacazinidae. The results of the structural analysis of the Meandropsinidae oblige to introduce the following new linnean names: Eofallotia simplex n. gen. n. sp., Fascispira schlumbergeri n. sp. and Alexina papyracea n. gen. n. sp.
机译:均滴类是由它们的透明壳中的透皮飞虫定义的,至少在它们的微球体世代中总是存在。它们的内骨骼发展的程度取决于它们的螺旋的小孔表面相对于环形腔的相对长度。螺旋形腔室的弧形延长部分由由腔室基底层形成的山脊或完整的隔壁分隔。这些骨骼内元素在随后的小室中对齐,但被前房间隔打断。除最简单和最小的成员Nummofallotia和Eofallotia之外,Meandropsinidae家族的所有成员都发生在Senonian内,并且仅限于白垩纪晚期的比利牛斯山脉海湾。在Spirapertolina和Larrazetia中,仅发现了微球标本。 Meandropsinid家族的大型成员被视为比利牛斯海湾的地方特有者,类似于Lacazinidae家族的大型代表。 Meandropsinidae的结构分析结果必须引入以下新的亚麻名称:Eofallotia simplex n。 gen。 。 sp。,Fascispira schlumbergeri。 sp。和Alexina papyracea。 gen。 。 sp。

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