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Research Article

Silurian phyllocarid crustaceans (Phyllocarida, Archaeostraca) from South China

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Article: 2187718 | Received 19 Oct 2022, Accepted 01 Mar 2023, Published online: 04 Apr 2023
 

Abstract

In the Silurian, the suborder Caryocaridina of the phyllocarids was replaced by the suborder Ceratiocaridina as the dominant group. The latter did not achieve a global distribution until the late Silurian. In the early Silurian, ceratiocarids were a little-diversified group and palaeogeographically restricted mainly to Laurussia. Although previous studies have mentioned phyllocarid fossils from the Silurian of the South China plate, these have never been systematically described. This study describes three genera and four species (including one new genus, two new species, and two undetermined species), i.e. Cugocaris future gen. et sp. nov., Gonatocaris wuhanensis sp. nov., Gonatocaris sp. and Warneticaris sp., based on 38 phyllocarid specimens from the Fentou Formation in Wuhan. Cugocaris future gen. et sp. nov. is distinguished by an elliptic carapace ornamented by sinuous and anastomosing longitudinal striae, a styliform telson, and slender furcal rami. Gonatocaris wuhanensis sp. nov. is characterized by anastomosing longitudinal striae on the carapace, greatest carapace width in the centre of the carapace, and three different types of ornamentations on the surface of the abdominal segments. A phylogenetic analysis of 41 Palaeozoic phyllocarids reveals that Gonatocaris, Rolfecaris and Cugocaris gen. nov. form a monophyletic group. Thus, a new family, Gonatocarididae fam. nov., is proposed. This family is characterized by a carapace lacking median dorsal plate, rostral plate, a well-developed anterior carapace horn, and ornamented with prominent raised, wavy, anastomosing longitudinal striae. A palaeoecological analysis suggests that G. wuhanensis was a fairly active swimmer, while C. future was necto-benthic with relatively weak swimming abilities. This study not only extends the known morphological range of phyllocarids, but also has implications for the functional morphology, taxonomy, and evolution of archaeostracans as a whole.

http://zoobank.org/urn:lsid:zoobank.org:pub:4B6B60B6-19F1-4A58-AC65-3B1AEE5D0939

Acknowledgements

This work was supported by the National Natural Science Foundation of China (Nos. 42072041, 41902002, 41872034) and the Fundamental Research Founds for National University, China University of Geosciences (Wuhan) (Nos. CUGDCJJ202208). We would like to thank Guogang Zhang (Hubei University), Chao Guo, Jiayi Yin and Dan Tu (China University of Geosciences, Wuhan) and Yihui Ke (University of Chinese Academy of Sciences) for their help in the field work. We also thank Prof. Derek E. G. Briggs (New Haven, USA) and Dr Zhihong Wang (Wuhan, China) for providing literature. We also greatly appreciate the critical comments and detailed suggestions from reviewers Thomas A. Hegna and Joseph H. Collette, Editor-in-Chief Paul M. Barrett, and Associate Editor Greg Edgecombe, which helped to improve the manuscript.

Supplemental material

Supplemental material for this article can be accessed here: https://doi.org/10.1080/14772019.2023.2187718.

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