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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 India, was the primary cause. First, the timing of the Deccan Traps eruptions aligns closely 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. Second, volcanic eruptions released enormous quantities of sulfur dioxide and carbon dioxide, leading to severe climate change. Sulfur aerosols caused rapid global cooling, while CO2 triggered long-term warming, creating a highly unstable environment that stressed ecosystems worldwide. Third, the fossil record indicates a gradual decline in dinosaur diversity millions of years before the impact, which is more consistent with the prolonged, episodic stress of volcanism rather than a sudden catastrophe. Therefore, while an asteroid may have contributed, the Deccan Traps volcanism was the dominant driver of the end-Cretaceous mass extinction.

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