Abstract

The endemic radiodonts of the Cambrian Stage 4 Guanshan biota of South China

Highlights

  • Sitting temporally between the Stage 3 Chengjiang and Wuliuan Kaili Biotas, the Guanshan Biota contains numerous fossil organisms that are exclusive to this exceptional deposit

  • The Guanshan Konservat-Lagerstätte is unusual amongst Cambrian strata that preserve non-biomineralized material, as it was deposited in a relatively shallow water setting

  • In this contribution we double the diversity of radiodonts known from the Guanshan Biota from two to four, and describe the second species of Paranomalocaris

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Summary

Introduction

The Guanshan Biota (South China, Cambrian, Stage 4) contains a diverse assemblage of biomineralizing and non-biomineralizing animals. Sitting temporally between the Stage 3 Chengjiang and Wuliuan Kaili Biotas, the Guanshan Biota contains numerous fossil organisms that are exclusive to this exceptional deposit. The Guanshan Konservat-Lagerstätte is unusual amongst Cambrian strata that preserve non-biomineralized material, as it was deposited in a relatively shallow water setting.

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