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The extinction of the dinosaurs at the end of the Cretaceous period has long been attributed to a massive asteroid impact. However, a growing body of evidence suggests that volcanic activity, specifically the Deccan Traps eruptions in India, was the primary driver of this mass extinction. First, the timing of the Deccan Traps eruptions coincides with the extinction event. Radiometric dating shows that the main phase of volcanic activity occurred around 66 million years ago, exactly when the dinosaurs disappeared. Second, volcanic emissions of sulfur dioxide and carbon dioxide would have caused severe climate change, including rapid global warming and ocean acidification, which could have disrupted ecosystems long before any asteroid impact. Third, the fossil record reveals a gradual decline in dinosaur diversity over the last few million years of the Cretaceous, which is more consistent with a slow, ongoing stressor like volcanism rather than a sudden catastrophic impact. Thus, while an asteroid may have delivered the final blow, the Deccan Traps eruptions were the fundamental cause of the dinosaurs' demise.

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