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埃迪卡拉纪后生动物揭示了冠轮动物亲缘关系并加深了寒武纪大爆发的根源。

Ediacaran metazoan reveals lophotrochozoan affinity and deepens root of Cambrian Explosion.

作者信息

Shore A J, Wood R A, Butler I B, Zhuravlev A Yu, McMahon S, Curtis A, Bowyer F T

机构信息

School of GeoSciences, University of Edinburgh, James Hutton Road, Edinburgh EH9 3FE, UK.

Department of Biological Evolution, Faculty of Biology, Lomonosov Moscow State University, Leninskie Gory, Moscow 119991, Russia.

出版信息

Sci Adv. 2021 Jan 1;7(1). doi: 10.1126/sciadv.abf2933. Print 2021 Jan.

Abstract

Through exceptional preservation, we establish a phylogenetic connection between Ediacaran and Cambrian metazoans. We describe the first three-dimensional, pyritized soft tissue in from the Ediacaran Nama Group, Namibia, which follows the underlying form of a stalked, cup-shaped, calcitic skeleton, with six radially arranged lobes projecting into an apical opening and lateral lumens. A thick body wall and probable J-shaped gut are present within the cup, and the middle layer of the often-spinose skeleton and skeletal pores are selectively pyritized, supporting an organic-rich composition and tripartite construction with possible sensory punctae. These features suggest a total group lophotrochozoan affinity. These morphological data support molecular phylogenies and demonstrates that the origin of modern lophotrochozoan phyla, and their ability to biomineralize, had deep roots in the Ediacaran.

摘要

通过特殊的保存方式,我们建立了埃迪卡拉纪和寒武纪后生动物之间的系统发育联系。我们描述了来自纳米比亚埃迪卡拉纪纳马群的首个三维黄铁矿化软组织,它遵循着有柄、杯状钙质骨架的基本形态,有六个呈放射状排列的叶状体,伸向顶端开口和侧向腔室。杯状结构内有一层厚厚的体壁和可能呈J形的肠道,通常具刺的骨架中层和骨骼孔隙被选择性地黄铁矿化,这支持了其富含有机物的成分和具有可能的感觉小孔的三方结构。这些特征表明其具有冠轮动物总门的亲缘关系。这些形态学数据支持分子系统发育,并表明现代冠轮动物门的起源及其生物矿化能力在埃迪卡拉纪就有深厚的根源。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3dbe/7775780/b9a93456decf/abf2933-F1.jpg

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