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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, was the primary driver. First, the Deccan Traps eruptions began well before the asteroid impact and lasted for nearly a million years, releasing vast amounts of sulfur dioxide and carbon dioxide. These gases would have caused severe global cooling and acid rain, stressing ecosystems long before the impact. Second, the timing of the main phase of volcanic activity coincides with the mass extinction horizon, whereas the Chicxulub impact occurred slightly earlier but did not immediately cause extinction. Third, models of volcanic gas emissions show that the Deccan Traps could have produced enough atmospheric change to trigger a collapse in photosynthesis and marine food chains, independent of any impact effects. Thus, volcanic activity, not the asteroid, was the decisive factor.

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