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The study analyzes packrat middens from Canyon de Chelly, Arizona, to assess paleoecological and archaeological implications, revealing a significant turnover in flora from the late Pleistocene to the late Holocene. The findings challenge previous models of vegetation reconstruction based on pollen data from the Chuska Mountains, indicating a lower tree line depression and the presence of various conifer species at lower elevations than previously thought. Additionally, evidence of early agriculture, includ

Author

Leandro Valenzuela

Language

EN