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First evidence of an underwater Final Pleistocene terrestrial extinct faunal bone assemblage from Central Chile (South America): Taxonomic and taphonomic analyses

机译:来自智利中部(南美)的水下最终更新世陆生灭绝动物骨组合的第一个证据:分类学和染色体分析

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摘要

Site GNL Quintero 1 (GNLQ1), located in Quintero Bay (32°S, Central Chile) constitutes the first evidence of a drowned terrestrial site on the continental West Coast of South America covered by sea-level rise after the Last Glacial Maximum. The site currently lies 650 m offshore and 13 m underwater, covers an area of ~ 64 m~2 and contains several discrete exposed and shallow-buried bone deposits. Through underwater archaeology survey and test excavations, a significant amount of animal bone assigned to the Late Pleistocene was successfully recovered and analyzed. After recovery and prior to the analyses, the bones were subjected to conservation and stabilization treatments, resulting in good preservation of the material. Taxonomic analyses (NISP 224) revealed high taxonomic diversity of extinct fauna (Camelidae, Cervidae, Artiodactyla, Equidae, Mylodontidae, Canidae, Rodentia and Xenarthra). The sample represents a continental faunal assemblage belonging to a drowned terrestrial context, probably related to an estuarine-lagoon environment. Taphonomic analysis allowed macroscopic identification of natural marks (punctures) associated with large and small size carnivores. The bones also show abrasion related to the action of marine sands along with colour alterations. By applying Scanning Electron Microscope (SEM) micrographs and Energy-Dispersive Spectroscopy (EDS) to fossil bones, marks and colour alterations were identified. Marks indicated rodent gnawing and trampling, while colour alterations were attributed to diagenesis processes, discarding thermal treatment. Site GNLQ1 is identified as having very high potential, for it provides the first evidence for a submerged palaeolandscape viable for human occupation and movement along the Pacific Coast of South America during the Late Pleistocene.
机译:位于Quento湾(智利中部32°S)的GNL Quintero 1站点(GNLQ1)首次显示了南美洲西海岸被淹死的陆地站点的证据,该站点在上次冰河期末之后被海平面上升所覆盖。该场所目前位于离岸650 m和水下13 m,占地面积约64 m〜2,并包含数个离散的裸露和浅埋骨沉积物。通过水下考古调查和测试挖掘,成功地回收和分析了分配给晚更新世的大量动物骨骼。恢复后和分析之前,对骨骼进行保护和稳定化处理,从而很好地保存了材料。分类学分析(NISP 224)显示,灭绝动物群(骆驼科,鹿科,偶蹄动物科,马科,Mylodontidae,Canidae,Rodentia和Xenarthra)具有较高的分类学多样性。该样本代表了一个被淹死的陆地环境的大陆动物群,可能与河口泻湖环境有关。音速分析可以宏观识别与大型和小型食肉动物相关的自然痕迹(穿刺)。骨头还表现出与海沙作用有关的磨损以及颜色变化。通过将扫描电子显微镜(SEM)显微照片和能量分散光谱(EDS)应用于化石骨骼,可以识别出痕迹和颜色变化。痕迹表明啮齿类动物啮齿和践踏,而颜色变化则归因于成岩过程,放弃了热处理。地点GNLQ1被认为具有很高的潜力,因为它为晚更新世期间南美洲太平洋沿岸的人类占领和迁徙提供了可能的水下古景观的第一个证据。

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  • 来源
    《Quaternary International》 |2013年第14期|45-55|共11页
  • 作者单位

    Departamento de Antropologia, Universidad de Chile, Ignacio Carrera Pinto 1045, Santiago, Chile;

    Universidad Catolica del Norte, IIAM, Gustavo Le Paige 380, San Pedro de Atacama, Luis Uribe 2320, Depto. 104, Santiago, Chile;

    ARKA Consultores S.A. Cochrane 401, Of. 1, Casilla 21, Correo Central Valparaiso, Chile;

    ARKA Consultores S.A. Cochrane 401, Of. 1, Casilla 21, Correo Central Valparaiso, Chile;

    Departamento de Geologia, Facultad de Ciencias Fisicas y Matemiticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile;

    Departamento de Geologia, Facultad de Ciencias Fisicas y Matemiticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile;

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