利用创新技术解码索诺兰沙漠(墨西哥西北部)的早期人类活动

Georgina Ibarra-Arzave, Felipe García-Oliva, E. Solleiro‐Rebolledo, S. Sedov, Pamela Chávez-Ortiz, B. Chávez-Vergara, César Villalobos-Acosta, Y. Rivera-Uria
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引用次数: 0

摘要

美国西南部和墨西哥西北部的早期农业时期(EAP)开始于新热时期(公元前 7500-4500 年)之后。在早期农业时期,农业社会种植玉米并修建运河进行灌溉;然而,寻找这一时期的遗址并重建其周围的古代活动遇到了困难,需要开发地质考古学指标。本研究旨在利用物理、微观形态和生物地球化学特征,从墨西哥西北干旱地区的三种古溶胶中确定人类活动过程。此外,还通过冗余分析对物理和生物地球化学变量进行了分析。结果表明,物理、微形态-微形态计量学和生物地球化学的综合分析是早期农业时期(公元前 4500 年)农业的准确指标;此外,用盐酸提取的土壤有机磷(Po )组分(HCl-Po )也是人类火源管理引起土壤变化的良好指标。因此,这些方法的综合分析更有可能确定人类活动对全新世晚期古溶胶的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Use of Innovative Techniques to Decodify Early Anthropic Activity in the Sonoran Desert (NW Mexico)
The Early Agriculture Period (EAP) in the southwest of USA and northwest of Mexico began just after the Altithermal period (7500–4500 years BP). During the EAP, agricultural societies cultivated corn and constructed canals for irrigation; however, searching for the sites of this period and reconstruction of the ancient activities surrounding them meets difficulties and requires the development of geoarchaeological indicators. The present study aims to identify anthropic processes from three paleosols in the arid Northwest Mexico using physical, micromorphological and biogeochemistry characteristics. In addition, the physical and biogeochemical variables were analysed by redundancy analysis. Results show that the combination of physical, micromorphological-micromorphometric and biogeochemistry analyses are an accurate indicator of agriculture during the Early Agriculture Period (4500 years BP); additionally, the soil organic P (Po ) fraction extracted by HCl (HCl-Po ) is also a good indicator of soil changes induced by human fire management. The integrated analyses of these methods thus had a higher potential for determining the human activities effect on paleosols from the Late Holocene.
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