厄瓜多尔亚马逊地区Ridgetop森林景观变化的证据

IF 1.1 3区 地球科学 Q2 ANTHROPOLOGY
W. Balée, Tod D. Swanson, M. G. Zurita-Benavides, J. R. Ruiz Macedo
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引用次数: 1

摘要

纳波河流域位于上亚马逊考古区内,是大亚马逊地区物种最多的森林之一。学术界和科学界的标准思维认为,这些森林基本上是原始的,因为过去对土著人的任何影响都很小,种子库就在附近,自然森林在人类离开、灭绝或分散后会重新出现。2019年对库拉雷流域内Waorani地区的三个脊顶森林(排入纳波河右岸)的清查研究,以及对努希尼奥河沿岸一个控制点森林(也在库拉雷流域)的可比清查显示,大约从19世纪末到1960年,人类受到了影响;它们发生在战争时期,在瓦奥拉尼人之间,在瓦奥人与外来者之间。人类的影响导致了两种具有重要瓦奥拉尼文化用途的长寿物种的高基底区存在:可可(Theobroma cacao L.)和无爪棕榈(Oenocarpus bataua Mart.)。这些物种具有较高的频率和优势值,并且没有出现在控制区,就样本中河流泛滥区以上的海拔而言,这是可比的。这些发现意味着,Napo河流域右岸(或南部)的阿尔法多样性不能通过参考传统的生物公认的生态演替模式来先验解释,但可能需要了解土著土地利用的历史模式和由于过去人类(特别是Waorani)的影响而导致的二次景观变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evidence for Landscape Transformation of Ridgetop Forests in Amazonian Ecuador
The Napo River basin, which is situated within the Upper Amazon archaeological region, is one of the most speciose forests in Greater Amazonia. Standard thinking in scholarship and science holds that these forests are essentially pristine because any Indigenous impacts in the past would have been minimal, seedbanks would have been nearby, and natural forests would have reappeared after the humans left, died out, or dispersed. Inventory research in 2019 on three ridgetop forests in Waorani territory inside the Curaray basin (which drains to the right margin of the Napo River) and a comparable inventory on one control site forest along the Nushiño River (also in the Curaray basin) show human impacts from about the late nineteenth century to about 1960; they occurred during the period of wartime among Waorani themselves and between Wao people and outsiders. The human impacts resulted in the high basal-area presence of two long-lived species with important Waorani cultural uses: cacao (Theobroma cacao L.) and ungurahua palm (Oenocarpus bataua Mart.). These species have high frequency and dominance values and do not occur in the control site, which is comparable in terms of elevation above the flood zone of the rivers in the sample. These findings mean that alpha diversity in the right margin sector (or south) of the Napo River basin cannot a priori be explained by reference to traditionally, biologically accepted patterns of ecological succession but may require knowledge of historical patterns of Indigenous land use and secondary landscape transformation over time due to human (specifically Waorani) impacts of the past.
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