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The extinction of the woolly mammoth (Mammuthus primigenius) at the end of the Pleistocene has long puzzled scientists. While climate change and human hunting are often cited, a recent hypothesis proposes that a catastrophic extraterrestrial impact—a comet or asteroid strike—was the primary driver. This theory rests on three main arguments. First, proponents point to a thin layer of sediment found at many sites across North America and Europe, dating to roughly 12,800 years ago, that contains high concentrations of iridium, a rare element in Earth's crust but common in meteorites. This layer is interpreted as evidence of a large impact event. Second, the same sediment layer contains microscopic spherules and nanodiamonds, which are formed under extreme heat and pressure consistent with an impact. Third, the timing of this proposed impact coincides with the onset of the Younger Dryas, a sudden return to near-glacial conditions that would have drastically altered the mammoth's habitat, reducing its food supply and leading to population collapse. Thus, the impact hypothesis provides a unified explanation for both the mammoth's extinction and the abrupt climate shift.

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The theory that an extraterrestrial impact killed the woolly mammoth is intriguing, but it fails under scrutiny. First, the iridium layer is not unique to the proposed impact date. Similar enrichments have been found in sediments from other periods, often linked to volcanic activity or cosmic dust accumulation, not impacts. Moreover, the iridium concentrations at the 12,800-year-old layer are far lower than those associated with known impact events, such as the dinosaur-killing Chicxulub crater. Second, the spherules and nanodiamonds cited as impact markers are not conclusive. Recent studies show that these features can form through non-impact processes, such as forest fires or biological activity, and they have been found in layers of multiple ages, suggesting they are not unique to this event. Third, the timing argument is flawed. The onset of the Younger Dryas was not instantaneous but occurred over centuries, and many regions where mammoths thrived, like Siberia, did not experience as severe a cooling as North America. In fact, mammoth populations in some areas persisted for thousands of years after the proposed impact, indicating that climate change alone was not sufficient. Instead, a combination of human hunting and gradual climate change during the Holocene better explains their eventual extinction.