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The new Upper Serpukhovian genus Zaphrufimia and homeomorphism in some rugose corals

机译:上古Serpukhovian属Zaphrufimia和一些同质珊瑚的同态

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A number of nondissepimented Visean and Serpukhovian rugose coral species are morphologically linked to Zaphrentites HUDSON, 1941 and Ufimia STUCKENBERG, 1895. Separate taxonomic positions for these groups of species are suggested by differences in the microstructure of their septa and isolation in time and space of their types (Early Carboniferous of Western Europe vs. Middle Artin-skian of the Ufa River area in Russia). The zaphrentoid early morphology, present in both lineages, is suggested to be the archetype for many Rugosa. Direct linking of the Early Carboniferous Ufimia-like corals to Zaphrentites suggests they evolved independently from Ufimia proper. Therefore they are assigned to the genus Zaphrufimia, newly introduced here. The probable derivation of this new genus suggests its relationship to the Stereolasmatina HILL, 1981, but not to the Plerophyllina SOKOLOV, 1960. Re-investigation of the lectotype of Zaphrentis' disjuncta CARRUTHERS, 1910, from the Arnsbergian (Upper Serpukhovian) of Scotland, allowed Tlerophyllum (Ufimia)' schwarzbachi SCHINDEWOLF, 1942, from both slightly older and equivalent strata of the Silesian Coal Basin to be placed in synonymy with that species. Three subspecies distinguished by SCHINDEWOLF (1952) are revised and re-described, using both the original collection and newly investigated specimens from the Lower Serpukhovian of the Czech Republic.
机译:形态上与Zaphrentites HUDSON(1941年)和Ufimia STUCKENBERG(1895年)在形态上相关联的是许多未散布的Visean和Serpukhovian皱纹珊瑚。这些种类的物种在微观结构上的差异以及在时间和空间上的隔离都表明了这些种类的分类位置类型(西欧早期石炭纪与俄罗斯乌法河地区的中阿丁斯基山脉)。在两个谱系中都存在的类phr蝶早期形态被认为是许多Rugosa的原型。早期石炭纪的类乌菲米亚珊瑚与Zaphrentites的直接联系表明它们独立于乌菲米亚自然而然演化。因此,它们被分配给Zaphrufimia属,在这里新引入。这个新属的可能起源表明它与1981年的Stereolasmatina HILL,而不是与1960年的杏鲍菇SOKOLOV。允许将来自西里西亚煤炭盆地稍老和同等地层的Tlerophyllum(Ufimia)的schwarzbachi SCHINDEWOLF,1942年作为该物种的代名词。对SCHINDEWOLF(1952)区分的三个亚种进行了修改和重新描述,使用了来自捷克共和国下塞尔普克霍维安(Serpukhovian)的原始样本和新近调查的样本。

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