Nonmineralized triradial conulariids from the lowermost Cambrian Stage 2 of the Olenek Uplift, Siberian Platform

In the early Cambrian fossil record, triradial symmetry is typical for anabaritids and occurs among carinachitids. The former are an extinct group of minute benthic cnidarians covered with a calcareous tubular exoskeleton. The origin of the anabaritids is poorly understood, but previously reported t...

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Bibliographic Details
Published in:Journal of Paleontology
Main Authors: Zhiger A. Sarsembaev, Vasiliy V. Marusin
Format: Text
Language:English
Published: The Paleontological Society 2022
Subjects:
Online Access:https://doi.org/10.1017/jpa.2022.21