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Mayan Depopulation

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The main argument of this article addresses how human-environment interactions played a part in the Maya depopulation of the central lowlands during the late classic period. They argue that climate change, especially the lack of sufficient rainfall played a major role in understanding the classic period collapse of the central Maya lowlands. The authors alluded to the evidences that indicated that the terminal classic period was wrecked by its severe droughts of 3-18 years in length in which precipitation dwindled by 36-52% below standard mean. These regional declines in precipitation and massive reduction in food production caused various places such as Palenque, Copan, Tikal, and Calakmul to experience tremendous stress on cultivation and

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