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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, recent evidence suggests that volcanic activity, specifically the Deccan Traps in India, may have been the primary cause. First, the timing of the Deccan Traps eruptions coincides with the extinction event. Radiometric dating shows that the main phase of volcanic activity occurred around 66 million years ago, exactly when the dinosaurs disappeared. Second, volcanic eruptions release vast amounts of sulfur dioxide and carbon dioxide, which can cause severe climate change. Sulfur aerosols block sunlight, leading to a global cooling, while CO2 traps heat, causing long-term warming. Such rapid temperature fluctuations would have stressed ecosystems, making it difficult for large reptiles to survive. Third, the fossil record indicates a gradual decline in dinosaur diversity well before the asteroid impact. Studies of dinosaur fossils in North America show a decrease in species richness over the last few million years of the Cretaceous, suggesting that environmental stress from volcanism was already taking a toll. Therefore, the Deccan Traps volcanism, not the asteroid, is the more plausible driver of the mass extinction.

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