Overkill, glacial history, and the extinction of North America’s Ice Age megafauna

• Published in: Proceedings of the National Academy of Sciences - PNAS Vol. 117; no. 46; pp. 28555 - 28563
• Main Author: Meltzer, David J.
• Format: Journal Article
• Language: English
• Published: United States National Academy of Sciences 17-11-2020
• Subjects: Animals; Archaeology; Climate Change; Ecological effects; Endangered & extinct species; Extinction; Extinction, Biological; Fossils; Glacial periods; Glaciation; Holocene; Humans; Ice ages; Ice Cover; Mammals; Megafauna; North America; PERSPECTIVE; Pleistocene; Predation; Social Sciences; Species extinction; Survival; Tolerances; North America; glacial−interglacial climate change; human overkill; Pleistocene extinctions; North America; megafauna
• ISSN: 0027-8424; 1091-6490
• DOI: 10.1073/pnas.2015032117

The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial–interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that previous glacial–interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species’ histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene−Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial−interglacial transitions and the very last one was a human presence.