Protomelission Temporal range:
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Microfossil of Protomelission from Wirrealpa. Reproduced from Zhang et al. 2021[2] | |
Scientific classification | |
Clade: | Viridiplantae |
Division: | Chlorophyta |
Class: | UTC clade |
Order: | Dasycladales (?) |
Genus: | †Protomelission Brock, G. A. & Cooper, B. J. 1993[1] |
Protomelission is a Cambrian fossil taxon of contested affinity. It comprises cataphract arrays of box-like chambers, forming a club-shaped thallus surrounding a hollow central cavity. It was first described from phosphatized microfossils whose individual chambers were interpreted as housing the zooids of a non-mineralized bryozoan, which would make it the only affinity representative of that phylum – implying that all animal phyla originated in the Cambrian period.[3] The subsequent discovery of articulated macrofossils from the Xiaoshiba[4] biota called into question the biological nature of the distal apertures, showing that the surface was instead covered with leaf-like triangular flanges. This has led to the reinterpretation of the fossil material as a "seaweed", strictly as a dasycladalean green alga.[5]