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Geoarchaeological and Paleoenvironmental context of the human settlement in the Eastern Tandilia Range, Argentina

机译:阿根廷东坦迪利亚山脉人类住区的地球考古和古环境背景

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摘要

The Tandilia range is a discontinuous series of hills and valleys located at the central area of the Pampean region (Argentina). The process of human settlement reached in this zone the highest population densities and reoccupation levels of Southern South America, developing under the strongly changing climatic conditions that characterized the Pleistocene-Holocene transition. This paper analyzes the geoarchaeological and paleoenvironmental record of the Pleistocene—Holocene transition (c. 9400 —10,500 ~(14)C BP) recovered from cave and rockshelter sedimentary successions of the Tandilia range. The analysis of several lines of evidence (stratigraphic, geoarchaeological, archaeological, zooarchaeo-logical, and paleobotanical), suggests that a cold arid to semi-arid climate characterized the late Pleistocene (c. 10,500 BP), and changed abruptly to warmer conditions towards the beginning of the Post-Glacial Period. As a consequence of this climatic amelioration, the populations inhabiting the Tandilia range would have been benefited by a higher availability of resources, which could explain the higher levels of site density and reoccupation found in the area during this period.
机译:坦迪利亚山脉是一系列不连续的丘陵和山谷,位于潘潘区(阿根廷)的中部地区。在这个以更新世-全新世过渡为特征的剧烈变化的气候条件下,人类定居过程在该地区达到了南美南部最高的人口密度和重新居住水平。本文分析了从坦迪利亚山脉的洞穴和岩棚沉积序列中恢复的更新世-全新世过渡(约9400 —10,500〜(14)C BP)的地质考古和古环境记录。对几条证据线(地层,地质考古,考古,动物考古学和古植物学)的分析表明,晚更新世(约10,500 BP)的特征是寒冷干旱至半干旱气候,并突然转变为较暖的环境后冰河时期的开始。由于这种气候改善,居住在Tandilia山脉的人口将受益于更高的资源利用率,这可以解释该时期该地区发现的更高的站点密度和重新居住水平。

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  • 来源
    《Quaternary International》 |2013年第19期|23-37|共15页
  • 作者单位

    Institute de Ceologta de Costas y del Cuatemario, Facultad de Ciencias Exactas y Naturales, Universidad National de Mar del Plata, Funes 3350,7600 Mar del Plata, Argentina,Laboratorio de Arqueologia Regional Bonaerense, Universidad National de Mar del Plata, Argentina;

    Laboratorio de Arqueologia Regional Bonaerense, Universidad National de Mar del Plata, Argentina;

    Laboratorio de Arqueologia Regional Bonaerense, Universidad National de Mar del Plata, Argentina;

    Laboratorio de Paleobotanica, CICYTTP-Diamante C0N1CET, Materi y EspaHa s, Diamante 3105, Entre Rios, Argentina;

    Laboratorio de Paleobotanica, CICYTTP-Diamante C0N1CET, Materi y EspaHa s, Diamante 3105, Entre Rios, Argentina;

    Instituto de Investigationes Marinas y Costeras (IIMyC), FCEyN, CONICET-Universidad National de Mar del Plata, Argentina;

    Laboratorio de Paleobotanica, CICYTTP-Diamante C0N1CET, Materi y EspaHa s, Diamante 3105, Entre Rios, Argentina;

    Laboratorio de Paleobotanica, CICYTTP-Diamante C0N1CET, Materi y EspaHa s, Diamante 3105, Entre Rios, Argentina;

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