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

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posted on 2025-08-13, 12:43 authored by Y Wu, S Pates, M Zhang, W Lin, J Ma, C Liu, X Zhang, D Fu
The 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, but 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 generic level, Anomalocaris is the most cosmopolitan taxon, but most genera are endemic. Radiodonts show a high initial diversity that declines through the early Palaeozoic, allowing 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).

Funding

2022JC-DW5-01

2022M712570

41890844

41930319

42202011

42242201

China Postdoctoral Science Foundation

Chinese Academy of Sciences

D17013

Natural Science Basic Research Plan of Shaanxi Province

Natural Science Foundation of China

University of Cambridge

XDB26000000

History

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    URL - References http://osf.io/t6umg

Rights

© 2024 The Palaeontological Association

Rights Retention Status

  • No

Submission date

2024-01-09

Notes

This is the author accepted manuscript. The final version is available from Wiley via the DOI in this record Data archiving statement: All supplementary materials have been uploaded to the Open Science Framework (http://osf.io/t6umg).

Journal

Papers in Palaeontology

Publisher

Wiley / The Palaeontological Association

Version

  • Accepted Manuscript

Language

en

FCD date

2024-06-19T11:32:03Z

Citation

Vol. 10 (4), article e1583

Department

  • Ecology and Conservation

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