Abstract

The Cambrian Explosion by nature is a three-phased explosion of animal body plans alongside episodic biomineralization, pulsed change of generic diversity, body size variation, and progressive increase of ecosystem complexity. The Cambrian was a time of crown groups nested by numbers of stem groups with a high-rank taxonomy of Linnaean system (classes and above). Some stem groups temporarily succeeded while others were ephemeral and underrepresented by few taxa. The high number of stem groups in the early history of animals is a major reason for morphological gaps across phyla that we see today. Most phylum-level clades achieved their maximal disparity (or morphological breadth) during the time interval close to their first appearance in the fossil record during the early Cambrian, whereas others, principally arthropods and chordates, exhibit a progressive exploration of morphospace in subsequent Phanerozoic. The overall envelope of metazoan morphospace occupation was already broad in the early Cambrian though it did not reach maximal disparity nor has diminished significantly as a consequence of extinction since the Cambrian. Intrinsic and extrinsic causes were extensively discussed but they are merely prerequisites for the Cambrian Explosion. Without the molecular evolution, there could be no Cambrian Explosion. However, the developmental system is alone insufficient to explain Cambrian Explosion. Time-equivalent environmental changes were often considered as extrinsic causes, but the time coincidence is also insufficient to establish causality. Like any other evolutionary event, it is the ecology that make the Cambrian Explosion possible though ecological processes failed to cause a burst of new body plans in the subsequent evolutionary radiations. The Cambrian Explosion is a polythetic event in natural history and manifested in many aspects. No simple, single cause can explain the entire phenomenon.

Highlights

  • The Cambrian Explosion is by far the most dramatic chapter in the annals of animal evolutionary history, which laid foundations for animal evolution since the Phanerozoic

  • On the basis of currently update knowledge, here we address a current understanding on this unprecedented evolutionary event in the form of questions and answers in order to benefit a broader readership

  • Simple traces of bilateral animals were present by 560 Ma (Jensen et al 2005) or early (Pecoits et al 2012) and a possible trackway of a bilaterian with paired appendages was found in the latest Ediacaran (Chen et al 2018), the full suite of metazoan trace fossils that reflect a rapid diversification of body plans does not appear across a broad range of marine environments until close to the earliest Cambrian (Mángano and Buatois 2020)

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Summary

Introduction

The Cambrian Explosion is by far the most dramatic chapter in the annals of animal evolutionary history, which laid foundations for animal evolution since the Phanerozoic. Most living animal phyla made their first appearance in the fossil record during the first 20 million years of the Cambrian Period (Erwin et al 2011; Zhang and Shu 2014; Shu et al 2014).

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