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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 massive volcanic eruptions in the Deccan Traps of India were the primary cause. First, the timing of the Deccan eruptions overlaps with the extinction event. Radiometric dating shows that the main phase of volcanic activity began about 66 million years ago, just before the mass extinction, and continued for roughly 750,000 years. This temporal correlation is too precise to be coincidental, whereas the asteroid impact, dated to 66 million years ago, occurred after the onset of the extinction, according to some sediment records. Second, volcanic emissions of sulfur dioxide and carbon dioxide would have caused severe global cooling and acid rain, followed by long-term warming. Such climate disruptions could have stressed ecosystems worldwide, leading to the gradual decline of dinosaur populations over hundreds of thousands of years, as seen in the fossil record. Finally, the Deccan eruptions released vast amounts of toxic gases, including mercury, which would have poisoned soils and water bodies. High mercury concentrations found in sediments near the extinction boundary align with peak volcanic activity, providing a direct toxicological mechanism for the extinction.

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