Life 'explodes'

Trilobite fossils

Life became more diverse and abundant in the seas during the Cambrian time period, which started about 545 million years ago. Fossils in Pre-Cambrian rocks are of simple life forms such as bacteria, with more complex soft-bodied creatures appearing towards the beginning of the Cambrian. Cambrian rocks show large numbers of many different types animals, many with hard shells.

This important shift is often described as an "explosion", but new evidence suggests that it may have been a more gradual change. Part of the difficulty is that the fossil record is not complete - some life forms were more likely to be fossilised than others, and the conditions that allow fossilisation to occur were also not constant.

Image: Trilobite fossils. Trilobites appeared on Earth during the Cambrian period. (credit: Sinclair Stammers/SPL)

Introduction

Trilobite fossils Life 'explodes'

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Life 'explodes'

The Cambrian explosion, or Cambrian radiation, was the relatively rapid appearance, around 542 million years ago, of most major animal phyla, as demonstrated in the fossil record. This was accompanied by major diversification of other organisms.[note 1] Before about 580 million years ago,[note 2] most organisms were simple, composed of individual cells occasionally organized into colonies. Over the following 70 or 80 million years, the rate of evolution accelerated by an order of magnitude[note 3] and the diversity of life began to resemble that of today. Ancestors of many of the present phyla appeared during this period, with the exception of Bryozoa, which made its earliest known appearance in the Lower Ordovician.

The Cambrian explosion has generated extensive scientific debate. The seemingly rapid appearance of fossils in the “Primordial Strata” was noted as early as the 1840s, and in 1859 Charles Darwin discussed it as one of the main objections that could be made against his theory of evolution by natural selection. The long-running puzzlement about the appearance of the Cambrian fauna, seemingly abruptly and from nowhere, centers on three key points: whether there really was a mass diversification of complex organisms over a relatively short period of time during the early Cambrian; what might have caused such rapid change; and what it would imply about the origin and evolution of animals. Interpretation is difficult due to a limited supply of evidence, based mainly on an incomplete fossil record and chemical signatures remaining in Cambrian rocks.

Phylogenetic analysis has supported the view that during the Cambrian radiation metazoa evolved monophyletically from a single common ancestor: flagellated colonial protists similar to modern choanoflagellates.

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