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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 their decline correlates with the warming of the Holocene, not with human expansion. Radiocarbon dating shows that mammoth populations on Wrangel Island survived until 2000 BCE, long after humans arrived on the mainland, yet they vanished shortly after a period of rapid climate warming. Second, their diet, based on dry, nutrient-poor grasses of the steppe-tundra, became scarce as warming led to the encroachment of shrubs and forests, reducing open grassland habitats. Isotopic analysis of mammoth bones reveals a shift to less nutritious plants in their final millennia, indicating dietary stress. Third, genetic studies of the last surviving mammoths show a loss of diversity and an increase in harmful mutations, which weakened their immune systems and fertility, making them more vulnerable to disease and environmental change. These factors, all tied to climate, explain their extinction more convincingly than human hunting, which was sporadic and localized.

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