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What is the Cretaceous-Paleogene boundary iridium layer?

The Cretaceous-Paleogene boundary iridium layer is a thin band of sedimentary rock marking the major geological transition between the Mesozoic and Cenozoic eras 66 million years ago. This stratum contains unusually high levels of the rare platinum-group metal iridium compared to the Earth's crust. Discovered by Luis and Walter Alvarez in 1980, this iridium anomaly serves as crucial physical evidence that a massive extraterrestrial asteroid impact triggered the mass extinction event that wiped out the non-avian dinosaurs.

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