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Chicxulub Impact: Mass Extinction

66 Million years ago · Prehistoric
GeologyBiologyEvolution

Approximately 66 million years ago, an asteroid roughly 10 kilometers in diameter struck the Yucatan Peninsula, creating the 200-kilometer-wide Chicxulub crater. The impact released energy equivalent to 100 teratonnes of TNT, generating shockwaves, tsunamis, and ejecting debris that blocked sunlight globally. The resulting prolonged cooling, darkness, and ocean acidification triggered the Cretaceous-Paleogene extinction event, eliminating approximately 75 percent of all plant and animal species, including all non-avian dinosaurs.

Key Figures

Luis Walter AlvarezWalter AlvarezGlen PenfieldAntonio Camargo-ZanogueraAlan Hildebrand

Locations

Chicxulub CraterGubbio

Topics

dinosaursmesozoicperiodslife

Connected Events — 3 Connections

Post-extinction warming event following the K-Pg boundary Paleocene-Eocene Thermal Maximum
c. 56 MYA · Climate · Prehistoric
Established biodiversity later disrupted by Cambrian Explosion
538.8 million years ago · Geology · Prehistoric
The Cretaceous hothouse conditions persisted for roughly 28 million years until the Chicxulub impact abruptly terminated the Mesozoic greenhouse and plunged Earth into a transient impact winter Oceanic Anoxic Event 2 Triggers the Cretaceous Thermal Maximum
c. 93.9 Million years ago · Climate · Prehistoric
The Time Detectives® · Cadet Mission
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