Biomineralization of the Cambrian chancelloriids

As extinct animals that flourished during the Cambrian explosion, chancelloriids have a unique body plan lacking guts but with a flexible integument and a suite of star-shaped, hollow sclerites. Due to this body plan, along with the paucity of knowledge on sclerite biomineralization, the phylogenetic position of chancelloriids within the Metazoa is still controversial. Integration of analyses of diverse fossils from Cambrian stage 2 to the Wuliuan Stage of China and Australia indicates that chancelloriid sclerites possess an encasement-like organic layer and a fibrous aragonitic layer. The organic layer is inferred to be a specialized trait derived from the epidermal integument of the animal body. The sclerites were likely biomineralized by using the outer organic layer as a template to absorb cations and precipitate crystal nuclei, reflecting a strategy adopted by a range of eumetazoans with a developed epidermis. Therefore, the hypothesis that chancelloriids represent an epitheliozoan-grade animal and an early explorer of template-based biomineralization is supported.

Automated summary

Chancelloriids, extinct animals from the Cambrian explosion, have a unique body plan and sclerites, leading to controversy over their phylogenetic position within Metazoa. Research indicates that their sclerites possess an organic layer and aragonitic layer, likely mineralized through a template-based strategy. This supports the hypothesis that chancelloriids represent an epitheliozoan-grade animal exploring early biomineralization methods.