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- W2554775744 abstract "During the Late Pleistocene, modern Homo sapiens began dispersing out of Africa and into the rest of the world. The timing of the arrival of humans on each continent parallels the disappearance of many megafaunal genera. The Late Pleistocene also saw climate-caused changes in plant communities and moisture regimes, which would have affected megafaunal genera in most regions; yet, the animals had survived numerous earlier changes and recovered each time. Only the presence of modern humans clearly sets the late Pleistocene changes apart from the earlier climatic fluctuations. Climate changes probably fragmented megafaunal populations, cumulatively shrank optimal ranges, and increased competition among native predators, but the addition of human impacts such as killing—even at low levels—and disruptions of access to scattered resources such as water and migratory routes was the decisive factor leading to extinction for many megafaunal genera." @default.
- W2554775744 created "2016-11-30" @default.
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- W2554775744 date "2018-01-01" @default.
- W2554775744 modified "2023-09-23" @default.
- W2554775744 title "OBSOLETE: The Evidence for Human Agency in the Late Pleistocene Megafaunal Extinctions" @default.
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- W2554775744 doi "https://doi.org/10.1016/b978-0-12-409548-9.10012-0" @default.
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