巴兰地地区(捷克共和国)泥盆纪拜伦龙和类似管状化石

Pub Date : 2022-12-01 DOI:10.1017/S1755691023000099
M. Mergl, P. Kraft
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引用次数: 0

摘要

摘要Byronids是一种可能与cnidarian亲缘关系有问题的化石,在泥盆纪很少有报道,但以前从未在捷克共和国的Barrandian地区进行过研究。两个新种Prestephanoscyphus branzovensis sp.nov.和Prestephanos cyphus robustus sp.nov..分别从Lochkovian和Eifelian建立。四个鲜为人知的物种被称为Byronia,以埃姆西亚和艾菲尔亚的开放命名法进行了描述。新属Parapyronia gen.nov.和模式种Parapyronnia elegans sp.nov.与其他蝶形体密切相关,但其特征是鞘上的横向脊和鞘开口端的短刺。罗奇科夫时代的新材料证明了磷酸环是拜伦子的附着结构。一个矮生圆锥虫Pidicocularia gen.nov.和模式种Pidicocleria tubulata sp.nov.以其微小的体积和非常精细的装饰而引人注目;其圆锥亲和性通过四个内部隆突和四个矩形下横截面得到证实。Prestephanoscyphus鞘的微观结构特征是排列的柱状微晶的致密层和磷灰石等轴晶的室状层交替。byronid鞘的增生生长和具有粘性踏板盘基底开口的固定器的结构支持了它们的cnidarian亲和力,尽管它们可能表现出双侧而不是四聚体对称性。提出了Prestephanoscyphus内质突两侧对称轮匝的保护作用,并对其在加强鞘壁或支持胃隔功能方面的作用存在争议。拜伦虫被认为是表生生物,而不是附着在岩石上。它们是具有磷壳的底栖生物群的代表,这些磷壳随着海洋中磷的可用性降低而减少。
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Byronids and similar tubular fossils from the Devonian of the Barrandian area (Czech Republic)
ABSTRACT Byronids are problematic fossils of possible cnidarian affinity, only rarely reported from the Devonian, but never previously studied in the Barrandian area, Czech Republic. Two new species Prestephanoscyphus branzovensis sp. nov. and Prestephanoscyphus robustus sp. nov. are erected from the Lochkovian and the Eifelian, respectively. Four poorly known species referred to Byronia are described in open nomenclature from the Emsian and Eifelian. The new genus Parabyronia gen. nov. with the type species Parabyronia elegans sp. nov. is closely related to other sphenothallids but is distinguished by transverse ridges on its theca and short spines at the apertural end of the theca. Definite identification of phosphatic rings as the attachment structure of byronids was proved by new material of the Lochkovian age. A dwarf conularia Pidiconularia gen. nov. with the type species Pidiconularia tubulata sp. nov. is remarkable by its minute size and very fine ornament; its conulariid affinity is proved by subrectangular cross-section and four internal carinae. Microstructure of theca of Prestephanoscyphus is characterised by alternation of compact laminae of aligned columnar microcrystallites and chambered laminae with isometric microcrystallites of apatite. Accretionary growth of byronid theca and structure of the holdfast with basal opening for the adhesive pedal disc support their cnidarian affinity although they likely display the bilateral instead of tetramerous symmetry. The protective function of bilaterally symmetrical whorls of internal apophyses in Prestephanoscyphus is suggested and their role in strengthening of thecal wall or supporting function of gastric septa are disputed. The byronids are regarded as epibionts rather than attached to the rocks. They are representatives of benthic groups with phosphatic shells that declined with decreasing availability of phosphorus in seas and oceans.
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