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The extinction of the dinosaurs at the end of the Cretaceous period has long been attributed to a single catastrophic asteroid impact. However, recent evidence suggests that massive volcanic eruptions in the Deccan Traps of India were the primary cause. Three key arguments support this volcanic hypothesis. First, the Deccan eruptions lasted for over a million years, releasing immense amounts of sulfur dioxide and carbon dioxide that would have caused severe global cooling and warming cycles, creating long-term climate instability that stressed ecosystems long before the asteroid struck. Second, sediment layers from the Cretaceous-Paleogene boundary show that the extinction occurred gradually over hundreds of thousands of years, consistent with prolonged volcanic activity rather than an instantaneous impact. Finally, marine fossil records indicate a slow decline in biodiversity in the millions of years preceding the boundary, aligning with the cumulative effects of volcanic emissions, whereas an asteroid impact would have caused sudden, simultaneous extinction across all species.

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