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首页> 外文期刊>Acta Palaeontologica Polonica >Phosphatised olenid trilobites and associated fauna from the Upper Cambrian of Vastergotland, Sweden
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Phosphatised olenid trilobites and associated fauna from the Upper Cambrian of Vastergotland, Sweden

机译:瑞典韦斯特格兰上寒武统的磷化油状三叶虫及相关动物群

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摘要

Secondarily phosphatised olenid trilobites from organic-rich limestones (orsten) in the Furongian (Upper Cambrian) of Vastergotland, south-central Sweden, are described and illustrated. All trilobites originate from the Peltura scarabaeoides Zone and were collected on the western slope of Kinnekulle. Only the dorsal exoskeletons have become secondarily phosphatised, and the ventral appendages are not preserved. Yet the material is otherwise remarkably well preserved and reveals the morphology of the olenid trilobites in greater detail than hitherto known. Species belonging to the genera Ctenopyge, Sphaerophthalmus, Parabolina, and Peltura are identified, and several juvenile specimens are present in the material. The material is disarticulated and fragmentary, and it has only been possible to identify a few specimens to species level. In addition to chaetognaths and conodonts, the trilobites are associated with pelmatozoan columnals, a possible camaroid, and fossils of uncertain affinities. These fossils, along with a probable conulariid fragment from the Peltura minor Zone, are also described and discussed. The presence of a benthic fauna of pelmatozoans, and possible conulariids and camaroids, indicates that at least parts of the Peltura zones were deposited during dysoxic rather than anoxic periods. Moreover, the sea floor must have been firm enough to allow colonisation by sessile organisms.
机译:其次,描述和说明了瑞典中南部的弗罗贡山脉(上寒武统)的富有机质石灰岩(磷灰石)中的磷酸化的油状三叶虫。所有三叶虫都起源于Peltura scarabaeoides地区,并收集在Kinnekulle西坡。仅背面外骨骼被二次磷酸化,腹附肢未保留。然而,该材料在其他方面显着地保存得很好,并且比迄今已知的更详细地揭示了油状三叶虫的形态。确定了属于Ctenopyge,Sphaerophthalmus,Parabolina和Peltura属的物种,并且该材料中存在一些少年标本。该材料是分离的和零碎的,只能确定一些标本到物种水平的标本。除了象牙鱼和牙形石之外,三叶虫还与Peltotozoan柱状体,可能的类Camaroid和不确定的亲和性化石有关。还描述和讨论了这些化石,以及可能来自Peltura小地带的卵石碎片。 pelmatozoans底栖动物群的存在,以及可能存在的虫卵和类Camaroids,表明至少部分Peltura区域是在缺氧时期而不是缺氧时期沉积的。此外,海床必须足够坚固,以允许无柄生物定殖。

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