The Chicxulub Impact and the K-Pg Mass Extinction
Evidence from the global iridium layer, shocked quartz, and the Chicxulub crater demonstrating how an asteroid impact ended the Mesozoic Era.
Approximately 66.04 million years ago, a carbonaceous asteroid measuring an estimated 10 to 14 kilometers in diameter struck the carbonate-rich continental shelf of the Yucatan Peninsula in modern Mexico at an angle of roughly 45 to 60 degrees.
The Cascade of Global Cataclysms
- Kinetic Blast and Thermal Radiation: The impact released energy equivalent to approximately 100 million megatons of TNT, triggering regional thermal pulses that ignited global wildfires within hours.
- The Impact Winter: Billions of tons of vaporized sulfur-rich anhydrite, soot, and pulverized dust were propelled into the stratosphere, blocking sunlight and shutting down photosynthetic primary productivity in both terrestrial and marine ecosystems for multiple years.
- Selective Survival: Small ectothermic vertebrates with low metabolic requirements (such as crocodilians, turtles, and lizards), burrowing organisms, and toothless neornithine birds capable of feeding on seeds and detritus survived, while all non-avian dinosaurs succumbed.
Related Paleontological Discovery Hubs
Further Reading & Field Guides
Dinosaur Locomotion & Speed: Biomechanical Modeling, Trackways, and Skeletal Stress Constraints
A comprehensive scientific guide explaining how vertebrate paleontologists reconstruct dinosaur locomotion, evaluate trackway stride lengths, and calculate biomechanically constrained speed ranges.
Famous Dinosaur Fossil Formations: Global Lagerstätten, Bonebeds, and Key Paleontological Localities
An educational guide to the world's most scientifically vital fossil-bearing rock formations, detailing their taphonomy, geological age, and iconic dinosaur discoveries.