Comparison of regional tree-ring cutting-date distributions from the southern Colorado Plateau and the Rio Grande region with tree-ring-based reconstructions of the Palmer Drought Severity Index (PDSI) and with the timing of archaeological stage transitions indicates that Southwestern Native American cultures were periodically impacted by major climatic oscillations between A.D. 860 and 1600. Sitespecifi c information indicates that aggregation, abandonment, and out-migration from many archaeological regions occurred during several widespread megadroughts, including the well-documented middle-twelfth-and late-thirteenthcentury droughts. We suggest that the demographic response of southwestern Native Americans to climate variability primarily refl ects their dependence on an inordinately maize-based subsistence regimen within a region in which agriculture was highly sensitive to climate change.
RESUMEN
La comparación entre las distribuciones de anillos de árboles con fecha de corte de la zona sur de la Colorado Plateau y la región del Río Grande con reconstrucciones basadas en anillos de árboles del Índice Severo de Defi ciencia Palmer (PDSI, por sus siglas en Inglés) y con el momento del período de transición arqueológica, indica que las culturas Nativas