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The extinction of the dinosaurs at the end of the Cretaceous period, about 66 million years ago, has long been attributed to a massive asteroid impact. However, a growing body of evidence suggests that intense volcanic activity, specifically the Deccan Traps in present-day India, may have been the primary driver. First, volcanic eruptions released enormous quantities of sulfur dioxide and carbon dioxide, leading to rapid climate swings—cooling from sulfate aerosols and subsequent warming from CO2—that would have stressed ecosystems over hundreds of thousands of years. Second, the timing of the Deccan Traps eruptions aligns closely with the extinction event, with the main phase of activity occurring just before the boundary layer where fossils disappear. Third, the fossil record shows a gradual decline in dinosaur diversity and other species in the millions of years preceding the impact, consistent with prolonged volcanic stress rather than a sudden catastrophe. Thus, while an asteroid may have delivered a final blow, volcanic activity likely weakened ecosystems to the point of collapse.

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