Abstract

Cambrian marine ecosystems were dominated by arthropods, and more specifically artiopods. Aglaspidids represent an atypical group amongst them, not the least because they evolved and rapidly diversified during the late Cambrian, a time interval between the two diversification events of the Early Palaeozoic. Recent phylogenetic analyses have retrieved aglaspidids within the Vicissicaudata, a potentially important, but difficult to define clade of artiopods. Here we describe a new aglaspidid from the Furongian Guole Konservat-Lagerstätte of South China. This taxon displays a pretelsonic segment bearing non-walking appendages, features as-yet known in all vicissicaudatans, but aglaspidids. A new comprehensive phylogenetic analysis provides strong support for the legitimacy of a monophyletic clade Vicissicaudata, and demonstrates the pertinence of new characters to define Aglaspidida. It also motivates important changes to the systematics of the phylum, including the elevation of Artiopoda to the rank of subphylum, and the establishment of a new superclass Vicissicaudata and a new aglaspidid family Tremaglaspididae. Two diversification pulses can be recognized in the early history of artiopods – one in the early Cambrian (trilobitomorphs) and the other in the late Cambrian (vicissicaudatans). The discrepancy between this pattern and that traditionally depicted for marine invertebrates in the Early Palaeozoic is discussed.

Highlights

  • The Aglaspidida is a group of early Palaeozoic marine arthropods that has attracted considerable attention by virtue of possessing a number of atypical features compared to other contemporaneous members of the phylum Arthropoda

  • In addition to revising the definition and applicability of Vicissicaudata, we describe a new aglaspidid arthropod from the Furongian Guole Konservat-Lagerstätte of South China, which provides new insights into the evolution of tagmosis in the Aglaspidida

  • The discovery of G. trispinicaudatus sp. nov. illuminates the early evolution of trunk tagmosis in aglaspidids

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Summary

Introduction

Recent phylogenetic analyses have resolved aglaspidids as part of a larger clade known as Vicissicaudata[22], which includes the Burgess Shale (Cambrian Age 5) arthropods Emeraldella and Sidneyia, and the Early Ordovician–Early Devonian cheloniellids[20, 22, 25] This group has been essentially recovered when using character weighting and identifying precise synapomorphic characters for it has proved challenging[2]. The case of chelicerates put aside, two main artiopodan groups have been recovered in several recent cladistic analyses: the Trilobitomorpha and the Vicissicaudata The former clade regroups concilitergans, nektaspidids, trilobites, xandarellids and various other taxa, and has gained wide acceptance over the last fifteen years[19, 21,22,23,24, 27, 28, 31, 32] Vicissicaudata – a clade essentially composed of aglaspidids, cheloniellids, and the Burgess Shale arthropods Emeraldella and Sidneyia – has proved more elusive and difficult to define

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