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The extinction of the dinosaurs at the end of the Cretaceous period, approximately 66 million years ago, has long fascinated scientists. While the asteroid impact theory is widely accepted, a competing hypothesis suggests that massive volcanic eruptions in the Deccan Traps of India played a more significant role. Proponents of the volcanic theory offer three main arguments. First, the Deccan Traps eruptions lasted for over a million years, releasing enormous amounts of sulfur dioxide and carbon dioxide. These gases would have caused severe global cooling and ocean acidification, creating a prolonged environmental stress that could have gradually wiped out dinosaur populations. Second, geological evidence shows that the most intense phase of volcanic activity occurred just before the Cretaceous-Paleogene boundary, coinciding with the dinosaur extinction. This timing suggests a causal link. Third, volcanic eruptions would have ejected large quantities of mercury, which has been found in sediments dating to the extinction layer, indicating that volcanic activity was a primary contributor to the environmental catastrophe. Thus, the volcanic hypothesis challenges the asteroid impact as the sole cause of the dinosaurs' demise.

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