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The extinction of the woolly mammoth, a giant herbivore that roamed the northern hemisphere during the Pleistocene, has long been attributed to overhunting by early humans. This 'Pleistocene overkill' hypothesis, first proposed by Paul Martin in the 1960s, posits that human hunters, migrating from Asia into North America and Eurasia, rapidly exterminated mammoth populations. Three main lines of evidence support this view. First, the timing of mammoth extinctions correlates with human arrival in different regions. For instance, in North America, mammoths disappeared around 13,000 years ago, shortly after the appearance of the Clovis culture, known for its distinctive stone spear points. Second, archaeological sites, such as the Murray Springs site in Arizona, contain mammoth remains with embedded projectile points, indicating direct human hunting. Third, the mammoth's life history traits—slow reproduction, long gestation, and late sexual maturity—made it particularly vulnerable to even modest hunting pressure, as population recovery rates were low. Thus, the combination of archaeological evidence and ecological reasoning strongly implicates human hunters as the primary cause of the mammoth's demise.

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While the overhunting hypothesis is compelling, it fails to account for several critical observations. First, the temporal correlation is not as clean as claimed. In Eurasia, mammoths survived until about 4,000 years ago on Wrangel Island, long after humans had settled there. If hunting were the primary driver, why did they persist for thousands of years in close proximity to human populations? Second, direct evidence of hunting is rare and ambiguous. The Murray Springs site, for example, shows mammoth bones with possible spear marks, but these could also be from scavenging, as the bones also show cut marks from butchering—but whether the animals were killed or found dead is unclear. In fact, many purported kill sites lack diagnostic projectile points in direct association with the skeletons. Third, the life-history argument is flawed because it ignores the role of climate change. At the end of the Pleistocene, rapid warming and shifts in vegetation drastically reduced the mammoth's preferred habitat—cold steppe grasslands. Paleobotanical evidence shows that these grasslands were replaced by forests and tundra, which could not support large herds. This habitat loss, not human hunting, likely drove populations to extinction, as seen in the case of other large mammals that also went extinct but were not hunted. Thus, while humans may have played a minor role, the primary cause was environmental change.