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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 present-day India, was the primary cause. First, the timing of the Deccan Traps eruptions coincides with the extinction event. Geochemical dating shows that the main phase of eruptions began about 66 million years ago, just before the extinction, and continued for several hundred thousand years. This prolonged volcanic activity would have released vast amounts of sulfur dioxide and carbon dioxide, leading to severe climate disruption, including acid rain and global cooling, which could have devastated ecosystems. Second, the fossil record indicates a gradual decline in dinosaur diversity well before the asteroid impact. Paleontologists have found that dinosaur species were already decreasing in number and variety in the last few million years of the Cretaceous, suggesting that environmental stress from volcanic emissions was already taking a toll. Third, the asteroid impact, while dramatic, was a short-term event. The immediate effects, such as fires and tsunamis, would have been catastrophic locally, but the climate changes from an impact would have been brief, lasting only a few years to decades. In contrast, volcanic eruptions released gases over hundreds of thousands of years, creating a sustained and more deadly environmental crisis. Therefore, the Deccan Traps volcanism, not the asteroid, was the decisive factor in the dinosaur extinction.

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