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秘鲁东北部中普图马约-阿尔戈松流域森林的 5000 年植被和火灾历史。

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

机构信息

Department of Anthropology, Smithsonian National Museum of Natural History, Washington, DC 20560;

Smithsonian Tropical Research Institute, Panama City 0843-03092, Panama.

出版信息

Proc Natl Acad Sci U S A. 2021 Oct 5;118(40). doi: 10.1073/pnas.2022213118. Epub 2021 Jun 7.

Abstract

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 (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 , , , and 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 C 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 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.

摘要

本文探讨了亚马孙地区研究中的一个重要争议,即史前人类对森林的改造规模、强度和性质。对秘鲁东北部偏远的中普图马约-阿尔戈顿流域(Medio Putumayo-Algodón watersheds)成熟(非泛滥、非河流)森林下的陆地土壤进行的植硅体和木炭分析,提供了至少过去 5000 年的植被和火灾历史记录。在该地区进行的树木清查使古代植硅体记录与现生植被得以校准,并能估算随时间推移景观上棕榈物种的密度。植硅体记录没有显示出森林开垦或主要一年生粮食作物和根作物种植的证据。重要经济棕榈的频率,如 、 、 和 种,其中一些在现代植物区系中含有超优势种,在史前时期并没有增加。这表明,如果未来的研究在该地区记录到前哥伦布时期的人类活动,这些物种的丰度也没有通过管理或种植而显著增加。其他木本和木本植物的植硅体同样反映了整个记录中稳定的森林结构和多样性。木炭 C 年代证据表明,大约在 2800 年至 1400 年前,当地发生了森林火灾。我们的数据支持了先前的研究,表明在史前时代,相当多的亚马孙 森林地区并没有受到人类活动的显著影响。相反,在过去的 5000 年里,该地区的土著人口与相对未受干扰的大片森林共存,并帮助维持了这些森林,就像他们今天仍在做的那样。

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