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EP116 Doug Erwin on the Cambrian Explosion

The Jim Rutt Show

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How Do We Tell Time in Paleontology?

Paleontologists look for fossilized volcanic ash layers in rocks. Ladders of ash, if they come from the right kind of volcano, will have a mineral called zircon. Zircon takes into its lattice uranium, that uranium decays, and then we take it back. They're actually two decay systems, so they cross check each other.

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