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Paleozoic

From the Cambrian marine radiation to the end-Permian mass extinction.

Explore geological time

What changed during the Paleozoic Era?

The Paleozoic saw animal body plans diversify in the oceans, plants and vertebrates colonise land, forests transform climate and the largest known mass extinction close the era.

How did this history unfold?

Six periods run from the Cambrian radiation through Ordovician seas, Silurian–Devonian land colonisation, Carboniferous forests and Permian continental interiors.

What changed these ecosystems?

Five major crises affected Paleozoic ecosystems, culminating in the end-Permian extinction about 252 million years ago.

Three routes into this topic

Cambrian seas

Rapid diversification produced many durable animal body plans.

Life moves ashore

Plants, arthropods and vertebrates built terrestrial ecosystems.

End-Permian crisis

Warming, anoxia and volcanism transformed the biosphere.

How do scientists reconstruct this history?

Marine shells, reef limestones, fish skeletons, trackways, coal forests and volcanic ash beds create a highly varied record.

Frequently asked questions

What changed during the Paleozoic Era?

The Paleozoic saw animal body plans diversify in the oceans, plants and vertebrates colonise land, forests transform climate and the largest known mass extinction close the era.

How is the fossil record of this group preserved?

Marine shells, reef limestones, fish skeletons, trackways, coal forests and volcanic ash beds create a highly varied record.

Why did this group change or disappear?

Five major crises affected Paleozoic ecosystems, culminating in the end-Permian extinction about 252 million years ago.

Check the topic overview

Natural History Museum · Paleozoic Era Smithsonian · Deep Time
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