
End-Cretaceous Extinction Hinged on Ground Beneath Chicxulub
New modeling suggests the Chicxulub impact's global killing power hinged on striking hydrocarbon-rich, sulfur-bearing coastal rocks. The study estimates such geology could generate enough stratospheric soot to trigger 8–11°C global cooling, a major driver of the mass extinction, whereas rocks with lower hydrocarbon content would have caused milder effects. The claim is model-based and contingent on late-Cretaceous geology and the impact angle, and while it fits with related research, it remains not a settled consensus.













