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旧石器时代中期晚期意大利南部的人类居住连续性:来自普利亚的古环境视角。

Human occupation continuity in southern Italy towards the end of the Middle Palaeolithic: a palaeoenvironmental perspective from Apulia.

作者信息

Boschin Francesco, Columbu Andrea, Spagnolo Vincenzo, Crezzini Jacopo, Bahain Jean-Jacques, FalguèRes Christophe, Benazzi Stefano, Boscato Paolo, Ronchitelli Annamaria, Moroni Adriana, Martini Ivan

机构信息

Dipartimento di Scienze Fisiche, della Terra, e dell'Ambiente Università Degli Studi di Siena Siena Italy.

Centro Studi sul Quaternario Sansepolcro Arezzo Italy.

出版信息

J Quat Sci. 2022 Feb;37(2):204-216. doi: 10.1002/jqs.3319. Epub 2021 May 25.

Abstract

After the last interglacial [Marine Isotope Stage (MIS) 5e] Europe was affected by several harsh climatic oscillations. In this context southern Italy acted, like the rest of peninsular Mediterranean Europe, as a 'glacial refugium', allowing the survival of various species, and was involved in the spread of 'cold taxa' (e.g. woolly mammoth and woolly rhino) only during the coldest phases (MIS 4 and MIS 2). Both late Mousterian and early Upper Palaeolithic sites testify to a human occupation continuity in southern Italy and especially in Apulia in this time span. Here we present a focus on three key Apulian Palaeolithic sequences (Grotta di Santa Croce, Riparo L'Oscurusciuto and Grotta del Cavallo - layers F-E) jointly spanning from the late MIS 4 to the demise of Neanderthals around 43 ka. Novel chronological, sedimentological and zooarchaeological data are discussed for the first time in the light of the palaeoenvironmental information provided by recent analyses carried out on a speleothem from Pozzo Cucù cave (Bari) and the results of the magnetic susceptibility analysis from Riparo L'Oscurusciuto. This integrated reading allows a better understanding of the role played by the Apulian region as both a refugium for late Neaderthals and a suitable habitat for the early settling of modern humans.

摘要

在上一个间冰期[海洋同位素阶段(MIS)5e]之后,欧洲受到了几次剧烈的气候振荡影响。在这种背景下,意大利南部与地中海欧洲半岛的其他地区一样,充当了“冰川避难所”,使各种物种得以存活,并且仅在最冷的阶段(MIS 4和MIS 2)参与了“耐寒类群”(如猛犸象和披毛犀)的扩散。莫斯特晚期和旧石器时代晚期早期的遗址都证明了这一时期意大利南部,尤其是普利亚地区人类居住的连续性。在此,我们重点关注普利亚地区三个关键的旧石器时代序列(圣十字洞穴、洛斯科鲁西托避难所和卡瓦洛洞穴 - F - E层),它们共同跨越了MIS 4晚期至约4.3万年前尼安德特人灭绝的时期。根据最近对巴里的波佐库库洞穴的一个洞穴堆积物进行分析所提供的古环境信息以及洛斯科鲁西托避难所的磁化率分析结果,首次讨论了新的年代学、沉积学和动物考古学数据。这种综合解读有助于更好地理解普利亚地区作为晚期尼安德特人的避难所和现代人类早期定居的适宜栖息地所发挥的作用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5487/9291488/aa6f182a18f2/JQS-37-204-g001.jpg

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