寒武纪早期节肢动物茎系、五足动物、缓步动物和足类动物的衍生物及“东方”视角

A. Maas, D. Waloszek
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引用次数: 98

摘要

“Orsten”型保存是指角质层表面的磷化,没有任何进一步的变形,并产生了完整的三维化石,主要是节肢动物,尺度为100 μm-2 mm。这种特殊化石的记录现在在几个大陆和早寒武纪(大约在20世纪30年代)都有报道。公元前520万年)至早白垩纪(约为公元前530万年)。公元前100万年)。中、上寒武统的“Orsten”型konservat - Lagerstatten主要培育出甲壳类动物和真节肢动物的代表,但也有其早期茎系的衍生物。这些是上寒武纪五形虫的幼虫阶段,舌虫,今天是各种四足动物的寄生虫。一种中寒武纪微小缓步动物的代表目前正在描述中;它可能代表了现存缓步动物的光轴分类群。科学上的新发现是一种小管状、精细环状生物的碎片,具有类似环状的节段管状肢。目前正在研究的这个上寒武纪形式,可能代表了“奥斯滕”型保存的第一个足足动物,并将它们的记录扩展到晚寒武纪。它与下至中寒武统澄江页岩和布尔吉斯页岩的几个动物群一样,具有足形肢的设计,成对的节段背支,细环的管状体,在肢区光滑。这个“奥斯滕”化石提供的新信息涉及扁平化石上无法检测到的表皮细节。Pentastomids、缓步动物和onychophorans/lobopodians被称为“原”或“原节肢动物”,因为它们仍然缺乏或部分缺乏节肢动物进化谱系中后来的衍生物所具有的特征。在这三个分类群中,Pentastomida被认为是最新的分支,因为它们具有节肢,在物品之间有枢纽关节。在我们看来,现在所有“前节肢动物”甚至是古生代早期的真正的甲壳类动物的记录表明,节肢动物的祖先甚至可以追溯到更早的前寒武纪。
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Cambrian Derivatives of the Early Arthropod Stem Lineage, Pentastomids, Tardigrades and Lobopodians An ‘Orsten’ Perspective
Abstract ‘Orsten’-type preservation is the phosphatisation of cuticular surfaces without any further deformation and has yielded completely three-dimensional fossils, mainly arthropods at scale of 100 μm—2 mm. Records of such exceptional fossils are now reported from several continents and from the Early Cambrian (approx. 520 Mi. years BC) to the Early Cretaceous (approx. 100 Mi. years BC). ‘Orsten’-type konservat - Lagerstatten from the Middle and Upper Cambrian have brought up mainly crustaceans and representatives of the Euarthropoda, but also derivatives of their early stem lineage. These are larval stages of Upper Cambrian pentastomids, tongue worms, which today are parasites of various tetrapods. A Middle Cambrian representative of the minute tardigrades is currently under description; it possibly represents the adelphotaxon of extant Tardigrada. New to science are fragments of a small tubular, finely annulated organism with similarly annulated segmental tubular limbs. This Upper Cambrian form, currently under investigation, may represent the first lobopodian in an ‘Orsten’-type preservation and expands their record to the late Cambrian. It shares with several of the Lower to Middle Cambrian Chengjiang and Burgess Shale fauna lobopodians the lobopodian design of its limbs, paired segmental dorsal outgrowths, and the finely annulated tubular body, which is smooth in the limb regions. New information presented by this ‘Orsten’ fossil concerns cuticular details undetectable on flattened fossils. Pentastomids, tardigrades and the onychophorans/lobopodians have been called “pro-” or “prot-arthropods” because they still lack, or partly lack, characteristic features known from later derivatives of the evolutionary line of Arthropoda. Among the three taxa, the Pentastomida are assumed to be the latest offshoot because they possess segmented limbs with pivoted joints between the articles. The now established record of all of the “pro-arthropods” and even true crustaceans in the earliest Palaeozoic implies, in our view, that the ancestry of Arthropoda lies even further back well in the Pre-Cambrian.
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