A 5,000-year vegetation and fire history for tierra firme forests in the Medio Putumayo-Algodón watersheds, northeastern Peru

• Published in: Proceedings of the National Academy of Sciences - PNAS Vol. 118; no. 40; pp. 1 - 7
• Main Authors: Piperno, Dolores R., McMichael, Crystal H., Pitman, Nigel C. A., Andino, Juan Ernesto Guevara, Paredes, Marcos Ríos, Heijink, Britte M., Torres-Montenegro, Luis A.
• Format: Journal Article
• Language: English
• Published: United States National Academy of Sciences 05-10-2021
• Series: Tropical Forests as Key Sites of the Anthropocene Special Feature
• Subjects: Anthropogenic Effects; Biological Sciences; Burning; Calibration; Charcoal; Fires; Flora; Forest fires; Forests; Peru; Plant fossils; Prehistoric era; Terrestrial environments; Vegetation; Watersheds; Peru; vegetation history; Amazonia; charcoal; phytoliths
• ISSN: 0027-8424; 1091-6490
• DOI: 10.1073/pnas.2022213118

This paper addresses an important debate in Amazonian studies; namely, the scale, intensity, and nature of human modification of the forests in prehistory. Phytolith and charcoal analysis of terrestrial soils underneath mature tierra firme (nonflooded, nonriverine) forests in the remote Medio Putumayo-Algodón watersheds, northeastern Peru, provide a vegetation and fire history spanning at least the past 5,000 y. A tree inventory carried out in the region enables calibration of ancient phytolith records with standing vegetation and estimates of palm species densities on the landscape through time. Phytolith records show no evidence for forest clearing or agriculture with major annual seed and root crops. Frequencies of important economic palms such as Oenocarpus, Euterpe, Bactris, and Astrocaryum spp., some of which contain hyperdominant species in the modern flora, do not increase through prehistoric time. This indicates pre-Columbian occupations, if documented in the region with future research, did not significantly increase the abundance of those species through management or cultivation. Phytoliths from other arboreal and woody species similarly reflect a stable forest structure and diversity throughout the records. Charcoal 14C dates evidence local forest burning between ca. 2,800 and 1,400 y ago. Our data support previous research indicating that considerable areas of some Amazonian tierra firme forests were not significantly impacted by human activities during the prehistoric era. Rather, it appears that over the last 5,000 y, indigenous populations in this region coexisted with, and helped maintain, large expanses of relatively unmodified forest, as they continue to do today.