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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, the timing of the mammoth’s decline correlates more closely with rapid warming at the end of the last Ice Age than with the arrival of human hunters. Fossil records show that mammoth populations peaked during cold periods and collapsed during warm interglacials, even in regions where humans were absent or scarce. Second, the warming climate drastically reduced the mammoth’s preferred habitat—the cold, dry steppe-tundra. Pollen and sediment data indicate that as temperatures rose, this habitat was replaced by forests and wetlands, which were unsuitable for mammoths. This habitat loss would have fragmented populations and reduced food availability, leading to a gradual decline. Third, the mammoth’s biology made it vulnerable to warming. Its thick fur, small ears, and specialized digestive system were adapted to cold, arid conditions. As the climate warmed, heat stress would have impaired reproduction and increased susceptibility to disease, further accelerating extinction. While human hunting may have contributed to the final demise of isolated populations on islands, it cannot explain the widespread extinction that occurred across continents well before humans reached those areas.

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