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A Silurian armoured aplacophoran and implications for molluscan phylogeny

机译:Silurian装甲的Aplacophoran及其对软体动物系统发育的意义。

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摘要

The Mollusca is one of the most diverse, important and well-studied invertebrate phyla; however, relationships among major molluscan taxa have long been a subject of controversy. In particular, the position of the shell-less vermiform Aplacophora and its relationship to the better-known Polyplacophora (chitons) have been problematic: Aplacophora has been treated as a paraphyletic or monophyletic group at the base of the Mollusca, proximate to other derived clades such as Cephalopoda, or as sister group to the Polyplacophora, forming the clade Aculifera. Resolution of this debate is required to allow the evolutionary origins of Mollusca to be reconstructed with confidence. Recent fossil finds support the Aculifera hypothesis, demonstrating that the Palaeozoic-era palaeoloricate 'chitons' included taxa combining certain polyplacophoran and aplacophoran characteristics. However, fossils cqmbining an unambiguously aplacophoran-like body with chiton-like valves have remained elusive. Here we describe such a fossil, Kulindroplax perissokomos gen. et sp. nov., from the Herefordshire Lagerstatte (about 425 million years bp), a Silurian deposit preserving a marine biota in unusual three-dimensional detail. The specimen is reconstructed three-dimensionally through physical-optical tomography. Phylogenetic analysis indicates that this and many other palaeoloricate chitons are crown-group aplacophorans.
机译:软体动物是最多样化,重要和研究最充分的无脊椎动物门之一。但是,主要软体动物类群之间的关系长期以来一直是争议的主题。尤其是,无壳Ap形Aplacophora的位置及其与更知名的Polyplacophora(Chitons)的关系存在问题:Aplacophora被视为软体动物基部的近生或单生类,与其他衍生进化枝相似例如头足纲动物,或作为多角膜菌群的姐妹群,形成枝形针形虫。为了使软体动物的进化起源能够有把握地重建,需要解决这场辩论。最近的化石发现支持了Aculifera假说,表明古生代时代的古土壤“ Chitons”包括具有某些聚斑节和斑节状特征的类群。但是,化石仍然是难以捉摸的,将化石为无章石象牙色的尸体与类似chiton的瓣膜组合在一起。在这里,我们描述了这样的化石,Kulindroplax perissokomos gen。等。 11月,来自赫里福德郡(Herefordshire)Lagerstatte(约4.25亿年基点)的志留纪矿床,以不寻常的三维细节保存着海洋生物区系。标本通过物理光学层析成像三维重建。系统发育分析表明,这种和许多其他古隆起的Chitons是冠群apolophorans。

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  • 来源
    《Nature》 |2012年第7418期|p.94-97|共4页
  • 作者单位

    Department of Earth Sciences and Engineering, Imperial College London, London SW7 2BP, UK;

    Department of Geology & Geophysics, and Yale Peabody Museum of Natural History, Yale University, PO Box 208109, New Haven, Connecticut 06520-8109, USA;

    Department of Geology, University of Leicester, Leicester LEI 7RH, UK;

    Department of Earth Sciences, University of Oxford, South Parks Road,Oxford OX13AN, UK,Geological Collections, University Museum of Natural History, Oxford 0X1 3PW, UK;

    Queen's University Belfast, School of Biological Sciences, Marine Laboratory, Portaferry, Northern Ireland BT22 1PF,UK;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-18 02:54:20

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