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首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >Late Jurassic-Early Cretaceous stalked barnacles (Cirripedia, genus Eolepas WITHERS, 1928) from Stramberk, Moravia (Czech Republic)
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Late Jurassic-Early Cretaceous stalked barnacles (Cirripedia, genus Eolepas WITHERS, 1928) from Stramberk, Moravia (Czech Republic)

机译:摩拉维亚斯特拉伯克的晚侏罗纪-早白垩纪茎藤壶(Cirripedia,Eolepas WITHERS属,1928年)(捷克共和国)

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摘要

Newly collected material of stalked barnacles, here assigned to the scalpelliform Eolepas, is recorded from Upper Jurassic (middle-upper Tithonian) and Lower Cretaceous (lower Berriasian-lower Hauterivian) limestones exposed at Kotouc quarry near Stramberk, Moravia, Czech Republic. The latter records constitute the first definite note of the genus from post-Jurassic strata. Seven carinae in the collections of the Narodni Muzeum (Prague) are referred to the strambergensis morphotype, while three additional carinae and three terga show features typical of fimbriata. Because the original type of Brachylepas(?) fimbriatus has been lost, a neotype is designated here. We show that the holotype of Hamites(?) strambergensis BLASCHKE, 1911 refers to the same species that a later year was described by WITHERS (1912) as Brachylepas(?) tithonicus; it thus has priority. It is noted that differences between these two forms, as expressed in size and details of ornament, might turn out to be growth related, and that they could well be conspecific. On the basis of an XRD analysis, a carina is here shown to consist of francolite (calcium phosphate), a mineralogy typical of Eolepas. Relationships between the Moravian species and Late Jurassic congeners from England, Germany and France are briefly commented upon, as is the stratigraphy of cirripede occurrences at Kotouc Hill, with reference to the present material and previously recorded specimens.
机译:新收集的柄藤壶材料,这里被分配为扇形的Eolepas,是从捷克共和国摩拉维亚Stramberk附近的Kotouc采石场暴露的上侏罗统(中提通系中上层)和下白垩统(下Berriasian-下Hauterivian)下的石灰石记录的。后者的记录构成了侏罗纪后地层属的第一个明确记录。 Narodni Muzeum(Prague)的集合中有七个隆突被称为strambergensis形态型,另外三个隆突和三个terga表现出典型的菌毛特征。由于原来的Brachylepas(?)菌毛已经丢失,因此在此指定了新的类型。我们显示,Hamites(?)strambergensis BLASCHKE,1911的同种型指的是与WITHERS(1912)后来将其描述为Brachylepas(?)tithonicus相同的物种。因此,它具有优先权。值得注意的是,这两种形式之间的差异(以装饰物的大小和细节表示)可能与增长有关,并且很可能是特定的。根据X射线衍射分析,此处的隆起由方沸石(磷酸钙)组成,方沸石是Eolepas的典型矿物学。简要评论了摩拉维亚物种与来自英国,德国和法国的侏罗纪晚期同类动物之间的关系,并参考了目前的资料和先前记录的标本,对科托克山的卷柏成因地层进行了简要评论。

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