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)