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The extinction of the woolly mammoth at the end of the Pleistocene has long been attributed to human overhunting. However, a more recent hypothesis suggests that climate change, specifically the rapid warming and associated vegetation shifts, was the primary driver. Proponents of this climate-driven extinction theory point to three main lines of evidence. First, the timing of mammoth decline correlates closely with the Bølling-Allerød warming period, when temperatures rose dramatically and caused widespread habitat loss. Paleobotanical data show that the open steppe-tundra, which mammoths depended on for grazing, was replaced by forest and peatland, reducing their food supply. Second, genetic studies of ancient mammoth remains reveal a significant loss of genetic diversity prior to extinction, indicating population fragmentation and stress. This pattern is consistent with climate-induced habitat fragmentation, not the sudden, selective pressure of hunting. Third, archaeological evidence for human hunting of mammoths is scarce and geographically limited. Most known kill sites are in eastern Europe, while mammoths thrived across North America and Siberia, where such evidence is absent. If overhunting had been the main cause, one would expect more widespread and numerous hunting sites. Thus, while humans may have delivered a final blow, the underlying cause was likely environmental change that weakened mammoth populations long before they disappeared.

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