Exceptionally preserved radiodont arthropods from the lower Cambrian (Stage 3) Qingjiang Lagerstätte of Hubei, South China and the biogeographic and diversification patterns of radiodonts

Author:

Wu Yu12ORCID,Pates Stephen23ORCID,Zhang Mingjing1,Lin Weiliang1,Ma Jiaxin1,Liu Cong1ORCID,Wu Yuheng1ORCID,Zhang Xingliang14ORCID,Fu Dongjing1ORCID

Affiliation:

1. State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life & Environments, & Department of Geology Northwest University Xi'an 710069 China

2. Department of Zoology University of Cambridge Downing Street Cambridge CB2 3EJ UK

3. Centre for Ecology & Conservation University of Exeter Penryn Campus, Treliever Road Penryn Cornwall TR10 9FE UK

4. Nanjing Institute of Geology & Paleontology, Chinese Academy of Sciences Nanjing 210008 China

Abstract

AbstractThe Cambrian (Series 2, Stage 3) Qingjiang Lagerstätte of South China is one of the most diverse Burgess Shale‐type deposits around the world, yielding abundant non‐biomineralized fossils. Radiodonta, a taxonomically and ecologically diverse stem‐euarthropod group, has been generally thought to represent the largest consumers in early Palaeozoic marine ecosystems. Here we describe several new radiodont specimens from the Qingjiang Lagerstätte assigned to various groups, including Stanleycaris qingjiangensis sp. nov., a new type of hurdiid head carapace, one possible Hurdia carapace, and two partial appendages with uncertain affinities. These specimens not only extend the geographic and stratigraphic range of these taxa, they also illuminate the diversity of radiodonts (in particular hurdiids) in their early evolutionary history. Radiodont palaeobiogeographic patterns are visualized using network analysis. Laurentia and South China share many members at the genus level, Anomalocaris is the most cosmopolitan taxon, but most genera are endemic. Radiodonts show a high initial diversity that declines through the early Palaeozoic, enabling three diversification phases of radiodonts to be recognized: the thriving phase (Cambrian Series 2), declining phase (Cambrian Miaolingian) and terminal phase (Cambrian Furongian to Ordovician Floian).

Funder

Higher Education Discipline Innovation Project

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Publisher

Wiley

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