捷克共和国下泥盆世和中泥盆世Eurytholia的问题硬岩

M. Mergl
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引用次数: 2

摘要

摘要本文首次报道了中泥盆统Eurytholia中有问题的磷酸盐硬结岩。在捷克共和国中部波西米亚的巴兰地地区的六个地方,在Emsian至Eifelian晚期的石灰石中观察到明确的硬石。以前观察到的Eurytholia硬石的大小和形状变化阻止了对Emsian和Eifelian时代的少数标本的新物种的正式描述。因此,新的标本被鉴定为波西米亚Eurytholia。它们的存在表明Eurytholia动物存在的时间范围较长,不仅涵盖了已知的奥陶纪、志留纪和最早的泥盆纪,还包括下泥盆世晚期和中泥盆世。在形态和组织学上的相似特征表明其与一种牙形刺伪齿有关系,并支持了关于其硬骨的脊椎动物起源的观点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Problematic Sclerites Eurytholia from the Lower and Middle Devonian of the Czech Republic
Abstract Problematic phosphatic sclerites Eurytholia are reported for the first time from the Middle Devonian. Unequivocal sclerites were observed in limestones of Emsian to late Eifelian age in six localities of the Barrandian area of the Central Bohemia of the Czech Republic. Formerly observed size and shape variations of Eurytholia sclerites prevent formal description of a new species on few specimens of Emsian and Eifelian age. Therefore the new specimens are identified as Eurytholia aff. bohemica. Their presence indicates longer time range of the Eurytholia animal, covering not only the Ordovician, the Silurian and the earliest Devonian as known formerly, but also late Lower Devonian and the Middle Devonian. Similar features in morphology and histology of Eurytholia indicate relationship to a conodont Pseudooneotodus and a support suggestion about the vertebrate origin of Eurytholia sclerites.
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