Critics argue: “We’ve never found fused metals at the Cretaceous–Tertiary boundary, so they can’t be real evidence at the Younger Dryas.” But here’s the problem—just because it hasn’t been reported elsewhere doesn’t mean it doesn’t exist. Many sites haven’t even been analyzed for those markers. Science should ask: were we looking in the right places? | The Randall Carlson
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Boundary Problems in Indian Stratigraphy - Planet Geology
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Geologists have found that the boundary between the Cretaceous and Paleogene layers called the “K–Pg” boundary (previously known as the "K-T boundary"), in many regions is marked by high levels of the rare metal iridium. While it is true that nearly all dinosaur fossils are absent above this K-Pg boundary, the areas with high iridium levels are not restricted to the thin zone that defines this boundary. In fact, in the same regions where the K-PG boundary was discovered, recent studies have iden
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