Answers are grounded in this paper and cite their sources.
Ecdysozoans, animals characterized by a periodically moulted cuticle, became major components of Cambrian marine ecosystems, yet the structural organization of their earliest non-mineralized cuticles remains poorly documented. Here we report Spinosoma reticulatus gen. et sp. nov., a millimeter-scale ecdysozoan from Fortunian cherts on two paleogeographic blocks: the Liuchapo Formation, South China, and the Yurtus Formation, Tarim Block, dating to ca. 538 Ma. This occurrence represents one of the earliest Cambrian ecdysozoan body-fossil records and may predate the classic Kuanchuanpu scalidophoran assemblages. The material preserves a terminal mouth with large circumoral spines and abundant cuticular fragments. Its cuticle comprises a fibrous mesh, short upright plate-like structures, and hollow ridged spines. Morphological and Raman data support an ecdysozoan affinity, whereas scalidophoran placement remains tentative. Spinosoma reveals a previously undocumented cuticular architecture, suggesting that early ecdysozoan ecological breadth and integument diversity are underestimated in the earliest phase of the Cambrian Explosion.
No takes yet. Share an insight, caveat, or question.
Zhang et al. (2026) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: