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首页> 外文期刊>Geosciences >Microstratigraphic Records as Tools for the Detection of Climatic Changes in Tana di Badalucco Cave (Liguria, NW Italy)
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Microstratigraphic Records as Tools for the Detection of Climatic Changes in Tana di Badalucco Cave (Liguria, NW Italy)

机译：显微地层记录作为探测塔纳迪巴达卢科洞穴（意大利西北利古里亚）气候变化的工具

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摘要

Tana di Badalucco cave is located in Imperia (Liguria, Italy), not far from the French border. This site is scarcely known and it has never been studied accurately, even though different archaeological excavations have returned really important elements, both in the archaeological and the paleoenvironmental aspects. Its stratigraphy ranges from Middle Paleolithic to Metal Ages, thus it has registered important climate and environmental variations specific to the Upper Pleistocene and Holocene. From 2012, the Soprintendenza Archeologia della Liguria, the Museo di Archeologia Ligure, and DiSTAV (University of Genova) have been collaborating in order to finally study this promising and complex stratigraphy, trying to reconstruct the paleoenvironmental context of the region. In this work, we present what we were able to assess thanks to the use of micromorphology, the study of undisturbed thin soil sections. This technique has proven useful in recognizing the alternating of cold and warmer conditions during the Quaternary, as well as in identifying primitive signs of human and animal occupation.
机译：Tana di Badalucco洞穴位于因佩里亚（意大利利古里亚），距法国边境不远。尽管在考古学和古环境方面，不同的考古发掘已返回了真正重要的元素，但该遗址鲜为人知，并且从未进行过准确的研究。其地层范围从旧石器时代中期到金属时代，因此它记录了上更新世和全新世特定的重要气候和环境变化。从2012年开始，Soprintendenza Archeologia della Liguria，利古雷博物馆（Museo di Archeologia Ligure）和DiSTAV（热那亚大学）开始合作，以期最终研究这一有前途且复杂的地层，试图重建该地区的古环境。在这项工作中，我们介绍了由于使用微观形态学，对未扰动的薄土层进行研究而能够进行的评估。事实证明，该技术在识别第四纪期间冷热条件的交替以及识别人类和动物占领的原始迹象方面很有用。

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