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The Devonian also saw the rise of the first labyrinthodonts, which was a transitional between fishes and amphibians.The colonisation of new niches resulted in diversification of body plans and sometimes an increase in size.It was from the lobe-finned fish that the tetrapods evolved, the four-limbed vertebrates, represented today by amphibians, mammals, reptiles and birds.

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The Devonian Period (395 to 345 Ma) brought in such giants as the placoderm Dunkleosteus, which could grow up to seven meters long, and early air-breathing fish that could remain on land for extended periods. The reptiles appeared from labyrinthodonts in the subsequent Carboniferous period.

The anapsid and synapsid reptiles were common during the late Paleozoic, while the diapsids became dominant during the Mesozoic. The later radiations, such as those of fish in the Silurian and Devonian periods, involved fewer taxa, mainly with very similar body plans.

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Unlike the other fauna that dominated the Cambrian, these groups had the basic vertebrate body plan: a notochord, rudimentary vertebrae, and a well-defined head and tail.

These were followed by indisputable fossil vertebrates in the form of heavily armoured fishes discovered in rocks from the Ordovician Period 500–430 Ma.

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Fish, like many other organisms, have been greatly affected by extinction events throughout natural history.

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