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最古老的端足目甲壳动物揭示了十足目亲戚在晚泥盆世的淡水殖民化。

The oldest peracarid crustacean reveals a Late Devonian freshwater colonization by isopod relatives.

机构信息

School of Biological, Earth and Environmental Sciences, University College Cork, Distillery Fields, North Mall, Cork T23N73K, Ireland.

Institute of Earth Sciences, University of Lausanne, Géopolis, 1015 Lausanne, Switzerland.

出版信息

Biol Lett. 2021 Jun;17(6):20210226. doi: 10.1098/rsbl.2021.0226. Epub 2021 Jun 16.

Abstract

Peracarida (e.g. woodlice and side-swimmers) are, together with their sister-group Eucarida (e.g. krill and decapods), the most speciose group of modern crustaceans, suggested to have appeared as early as the Ordovician. While eucarids' incursion onto land consists of mainly freshwater and littoral grounds, some peracarids have evolved fully terrestrial ground-crawling ecologies, inhabiting even our gardens in temperate regions (e.g. pillbugs and sowbugs). Their fossil record extends back to the Carboniferous and consists mainly of marine occurrences. Here, we provide a complete re-analysis of a fossil arthropod-reported in 1908 from the Late Devonian floodplains of Ireland, and left with unresolved systematic affinities despite a century of attempts at identification. Known from a single specimen preserved in two dimensions, we analysed its anatomy using digital microscopy and multispectral macroimaging to enhance the contrast of morphological structures. The new anatomical characters and completeness of , together with a phylogenetic analysis with representatives of all major Eumalacostraca groups, indicate that is a crown peracarid, part of a clade including amphipods and isopods. As such, is the oldest known species Peracarida, and provides evidence that derived peracarids had an incursion into freshwater and terrestrial environments as early as the Famennian, more than 360 Ma.

摘要

等足目动物(例如潮虫和仰泳蝽)与它们的姐妹群真软甲亚目动物(例如磷虾和十足目动物)一起,是现代甲壳动物中种类最多的群体,据推测它们最早出现在奥陶纪。虽然真软甲亚目动物的登陆主要发生在淡水和滨海地区,但一些等足目动物已经进化出完全适应陆地地面爬行的生态,甚至在我们温带地区的花园中也有它们的身影(例如球潮虫和鼠妇)。它们的化石记录可以追溯到石炭纪,主要是海洋生物。在这里,我们对一个 1908 年从爱尔兰晚泥盆世洪泛平原报道的化石节肢动物进行了全面重新分析,尽管一个世纪以来一直试图确定其系统亲缘关系,但仍未解决其系统发育关系。该化石仅保存了二维标本,我们使用数字显微镜和多光谱宏观成像技术对其解剖结构进行了分析,以增强形态结构的对比度。新的解剖特征和 的完整性,以及对所有主要软甲亚目组代表的系统发育分析表明, 是冠等足目动物,是包括端足目动物和等足目动物的一个进化枝的一部分。因此, 是已知最古老的等足目动物,为衍生的等足目动物早在泥盆纪晚期(3.6 亿多年前)就已经进入淡水和陆地环境提供了证据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/555b/8205522/a304b6bf1d41/rsbl20210226f01.jpg

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