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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 intense volcanic activity in the Deccan Traps of India was the primary cause. First, the Deccan eruptions began approximately 66 million years ago, well before the asteroid impact, and lasted for nearly 30,000 years. This prolonged volcanic activity would have released vast amounts of sulfur dioxide and carbon dioxide, leading to severe global cooling followed by warming, which could have disrupted ecosystems long before any impact. Second, the fossil record shows a gradual decline in dinosaur diversity over the last few million years of the Cretaceous, consistent with the slow, cumulative stress of volcanic emissions rather than a sudden catastrophic event. Finally, recent high-precision dating of Deccan lava flows reveals that the most intense phase of eruptions occurred just before the mass extinction, and the associated environmental changes—such as ocean acidification and ozone depletion—were severe enough to cause a collapse in food chains. Thus, while the asteroid may have delivered the final blow, the volcanic activity was the fundamental driver of the extinction.

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