First Palaeozoic Phyllocarid Crustaceans and Pterygotid Eurypterids in Serbia

M. Radonjić, V. Sachanski
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Abstract

Palaeozoic phyllocarid crustaceans and pterygotid eurypterids from the Gethicum Zone of Carpatho-Balkanides in Serbia are herein documented for the first time. The described and illustrated phyllocarid remains consisting of a coupled telson and furcal rami were collected from upper Silurian (?) shale. This specimen is fragmented and poorly preserved to allow identification to species level, and has thus been assigned to Ceratiocaris sp. indet. The eurypterids are represented by part of a fragment, showcasing the distinct scale-like ornamentation of the pterygotids, and a segment of a walking leg. The pterygotid remains were found together with a few graptolite taxa (Monograptus sudeticus Porębska, “M.” microdon microdon Reinh. Richter, Neomonograptus aequabilis (Přibyl), Uncinatograptus hercynicus (Perner), U. subhercynicus (Willefert)), which are characteristic for the lower part of the U. hercynicus graptolite zone (Lochkovian, Lower Devonian). There are at least two species in this stratigraphic interval that correspond to the pterygotid eurypterids remains from Serbia – Acutiramis perneri Chlupáč and Pterygotus cf. barrandei Semper, but without the chelicerae, it is impossible to make precise identification. These new finds from eastern Serbia, together with the Bulgarian ones, are a further confirmation of peri-Gondwanan origin of pre-Variscan Palaeozoic sediments in the West Srednogorie Unit in Bulgaria and in the Gethicum Unit in Serbia.
塞尔维亚第一古生代层状甲壳类和翼类全翅类
本文首次记录了塞尔维亚喀尔巴阡-巴尔干半岛Gethicum带的古生代层状甲壳类和翼状纲全翅类。所描述和说明的层状岩残体是在上志留统(2)页岩中收集到的,由一套耦合的层状岩和一套分叉岩组成。该标本支离破碎,保存较差,无法在物种水平上进行鉴定,因此被指定为角角兽属。泛翼龙由一块碎片和一段行走的腿来代表,这些碎片展示了翼龙独特的鳞状纹饰。这些翼龙化石与一些笔石分类群(Monograptus sudeticus Porębska,“M。" microdon microdon Reinh。Richter, Neomonograptus aequabilis (Přibyl), Uncinatograptus her愤世嫉俗(Perner), U. subher愤世嫉俗(Willefert)),这是U. her愤世嫉俗带下部(Lochkovian,下泥盆世)的特征。在这个地层层段中,至少有两种与塞尔维亚的翼足类全翅类遗骸相对应——Acutiramis perneri Chlupáč和Pterygotus cf. barrandei Semper,但没有chelicerae,就不可能进行精确的鉴定。这些来自塞尔维亚东部和保加利亚的新发现,进一步证实了保加利亚西斯雷诺戈里单元和塞尔维亚Gethicum单元的前variscan古生代沉积物起源于冈瓦纳时期。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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