Climate across Cretaceous–Paleogene boundary

The climate across the Cretaceous–Paleogene boundary (K–Pg or formerly the K–T boundary) is very important to geologic time as it marks a catastrophic global extinction event. Numerous theories have been proposed as to why this extinction event happened including an asteroid known as the Chicxulub asteroid, volcanism, or sea level changes.

Source: Wikipedia — Climate across Cretaceous–Paleogene boundary (CC BY-SA 4.0)

Climate across Cretaceous–Paleogene boundary

The climate across the Cretaceous–Paleogene boundary (K–Pg or formerly the K–T boundary) is very important to geologic time as it marks a catastrophic global extinction event. Numerous theories have been proposed as to why this extinction event happened including an asteroid known as the Chicxulub asteroid, volcanism, or sea level changes.

Source: Wikipedia "Climate across Cretaceous–Paleogene boundary" · CC BY-SA 4.0

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