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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 closer examination of the fossil record and geological evidence suggests that volcanic activity, specifically the Deccan Traps eruptions in India, was the primary driver of this mass extinction. Three key lines of evidence support this volcanic hypothesis. First, the Deccan Traps eruptions began well before the asteroid impact, approximately 66.3 million years ago, and lasted for nearly a million years. This prolonged volcanic activity would have released enormous quantities of sulfur dioxide and carbon dioxide into the atmosphere, causing severe global cooling followed by long-term warming, ocean acidification, and disrupted photosynthesis. Such environmental stress would have gradually weakened dinosaur populations long before the impact. Second, the fossil record shows a gradual decline in dinosaur diversity in the few million years leading up to the extinction event, not a sudden die-off that would be expected from an instantaneous asteroid strike. For example, studies of dinosaur teeth and eggshells from the latest Cretaceous reveal signs of physiological stress, such as reduced thickness and abnormal morphology, indicating chronic environmental deterioration. Third, the timing of the main phase of Deccan volcanism coincides with the extinction horizon more precisely than the impact. Recent radiometric dating places the peak eruption phase at 66.0 million years ago, exactly at the Cretaceous-Paleogene boundary, whereas the Chicxulub impact occurred slightly earlier, possibly 66.04 million years ago, leaving a gap of several tens of thousands of years. This temporal mismatch suggests that volcanic eruptions, not the impact, delivered the final lethal blow.

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