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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, recent evidence suggests that volcanic activity, specifically the Deccan Traps eruptions in India, played a more significant role. First, the Deccan Traps eruptions lasted for over a million years, releasing enormous amounts of sulfur dioxide and carbon dioxide. These gases would have caused rapid climate fluctuations, including volcanic winters and greenhouse warming, which could have stressed dinosaur populations long before the impact. Second, the fossil record shows a gradual decline in dinosaur diversity in the million years preceding the impact, consistent with the prolonged environmental stress from volcanism rather than a sudden catastrophe. Finally, the timing of the impact (66 million years ago) coincides with the Chicxulub crater, but the most severe phase of Deccan volcanism occurred around 66.3 million years ago, predating the impact by 300,000 years—a timeline that better aligns with the gradual decline observed in sediments.

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