Assessing charcoal and phytolith signals for pre-Columbian land-use based on modern indigenous activity areas in the Upper Xingu, Amazonia

IF 1.6 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Holocene Pub Date : 2023-07-10 DOI:10.1177/09596836231183066
J. Watling, Morgan Schmidt, M. Heckenberger, H. Lima, Bruno Moraes, K. Waura, H. Kuikuro, T. Kuikuro, Utu Kuikuro, Afukaka Kuikuro
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引用次数: 0

Abstract

The nature and extent of past indigenous transformations in the Amazon basin is an actively debated topic, and one that has important implications for both conservation policy and the cultural heritage of its indigenous and traditional populations. The use of charcoal and phytoliths to measure past human impacts in non-lacustrine settings has become especially influential in this debate but has also generated disagreement among scholars regarding the possible limits of these proxies for detecting ancient land-use. To contribute empirical data to this issue, our paper presents the first attempt to study charcoal and phytolith signals from areas of modern indigenous land-use, in the Xingu Indigenous Territory, southern Amazonia. Our findings show that, while charcoal and early successional herb phytoliths are good indicators of land-use intensity, certain types of land-use leave subtler traces in the phytolith record that can hinder their detection. We demonstrate how using finer sampling resolution and comparing local proxy data on their own terms are necessary steps in order to identify trends in human land-use across time and space.
基于亚马逊上新谷现代土著活动区评估前哥伦布时期土地利用的木炭和植硅体信号
亚马逊流域过去土著人转变的性质和程度是一个备受争议的话题,对保护政策及其土著和传统人口的文化遗产都有重要影响。在这场辩论中,使用木炭和植硅体来测量过去人类在非湖泊环境中的影响变得特别有影响力,但也引起了学者们对这些检测古代土地使用的指标的可能局限性的分歧。为了为这个问题提供经验数据,我们的论文首次尝试研究亚马逊南部新谷土著领地现代土著土地使用区域的木炭和植硅体信号。我们的研究结果表明,虽然木炭和早期演替草本植物植硅体是土地利用强度的良好指标,但某些类型的土地利用在植硅体记录中留下了更细微的痕迹,这可能会阻碍它们的检测。我们展示了如何使用更精细的采样分辨率并根据其自身条件比较当地代理数据是确定人类土地利用跨时间和空间趋势的必要步骤。
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来源期刊
Holocene
Holocene 地学-地球科学综合
CiteScore
4.70
自引率
8.30%
发文量
106
审稿时长
4 months
期刊介绍: The Holocene is a high impact, peer-reviewed journal dedicated to fundamental scientific research at the interface between the long Quaternary record and the natural and human-induced environmental processes operating at the Earth''s surface today. The Holocene emphasizes environmental change over the last ca 11 700 years.
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