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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 mammoth extinctions correlates with the end of the last Ice Age, when global temperatures rose rapidly. As the ice retreated, mammoth habitats—cold, dry grasslands known as steppe-tundra—shrank dramatically. Pollen records from Alaska and Siberia show that these grasslands were replaced by forests and wetlands, which provided unsuitable forage for mammoths. Second, genetic studies reveal a severe population bottleneck among mammoths long before human hunters arrived in their final refuges. DNA from mammoth remains on Wrangel Island indicates that the population there had already declined to fewer than 300 individuals by 7,000 years ago, likely due to shrinking food supplies. Third, human hunting pressure was minimal in the regions where mammoths survived longest. Archaeological sites from the Paleolithic period show that humans primarily hunted smaller game, such as reindeer, and mammoth bones found at these sites are often from natural carcasses, suggesting scavenging rather than active hunting. Therefore, climate-induced habitat loss, not human predation, drove mammoths to extinction.

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