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The extinction of the woolly mammoth has long been attributed to human overhunting, but recent evidence suggests that climate change was the primary driver. First, mammoth populations declined dramatically during periods of rapid warming, such as the Bølling-Allerød interstadial (14,700–12,900 years ago), when temperatures rose by several degrees within decades. These warming events shrank the mammoth’s preferred habitat—cold, dry steppe-tundra—by allowing shrubs and forests to expand, fragmenting the open grasslands on which mammoths depended. Second, genetic studies of ancient mammoth remains show a steady loss of genetic diversity and a rise in harmful mutations long before human populations reached high densities in the Arctic. This indicates that populations were already stressed by habitat loss, making them more vulnerable to extinction. Third, the final extinction occurred on isolated islands (e.g., Wrangel Island, St. Paul Island) where human hunting was minimal or absent, yet these populations disappeared around the time of sea-level rise and the arrival of novel vegetation, pointing to environmental causes rather than human predation. Therefore, climate-driven habitat change, not overhunting, was the decisive factor.

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