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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 driver. First, the timing of the Deccan Traps eruptions coincides with the extinction event. Geochemical dating shows that the main phase of volcanic activity occurred around 66 million years ago, exactly when the dinosaurs disappeared. This temporal correlation is too precise to be coincidental. Second, volcanic emissions would have caused severe climate change. The Deccan Traps released vast amounts of sulfur dioxide and carbon dioxide, leading to acid rain, global cooling followed by greenhouse warming, and disruption of photosynthesis. Such rapid environmental shifts could have destroyed food chains and habitats, making it impossible for large reptiles to survive. Third, the asteroid impact theory has weaknesses. The Chicxulub crater, often cited as evidence for the impact, is dated to about 300,000 years before the extinction, meaning the impact may have occurred too early to be the direct cause. Additionally, many species had already been declining for millions of years before the impact, suggesting a gradual environmental stress, which is more consistent with prolonged volcanic activity than with a sudden catastrophe.

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