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Climate and environmental changes recognized by micromorphology in Paleolithic deposits at Arene Candide (Liguria, Italy)

机译:Arene Candide(意大利利古里亚)旧石器时代的微观形态识别的气候和环境变化

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摘要

The lowermost part of the stratigraphic sequence of the Arene Candide Cave, a key Upper Palaeolithic site in Italy, attests to significant climate and environmental change at the beginning of the Late Pleniglacial in coastal Liguria (Northwest Italy). These archaeological layers were studied using a suite of mineral-ogical and chemical technique including a contextual sedimentological analysis (micromorphology). This study shows that the lower layers are dominated by cryoclastic sediments covered by cyclically organized blackish and reddish layers, or lenses. The black layers mainly consist of bird and bat guano deposits, interfingered with thin brownish sandy-silt layers of aeolian origin, that contain large amount of Ca phosphate. In contrast, the bright red layers are rubified sediment due to Fe re-oxidizing in insoluble form. In these layers evidence of syngenetic freeze-thaw cycles, associated with gelifluction processes, indicates a cool episode in a (semi) arid periglacial environment coupled to an increase in humidity between ca. 31 and 27 ka cal BP. Subsequently, the occurrence of features associated with repeated runoff and debris flow processes that caused a significant accumulation of poorly layered and sorted materials in the overlying sediments indicates a further intensification of humid conditions and reflects a longer phase of more humid and temperate climate. This change from arid to semiarid/humid climates resulted in an increase in sediments resulting from the erosion of Pliocene marine terraces and soils located outside the cave. The identification in the studied sequence of guano layers and the scarcity of artefacts, in conjunction with an absence of clear cultural micromorphological evidence, support an interpretation of sporadic human occupation of this part of the cave during Middle Upper Palaeolithic (Gravettian). Therefore, the finding in such a context of the lavish ceremonial burial of the so called "Young Prince" may suggest that the cave was used as a special place for burials at that time.
机译:意大利主要的上古石器时代遗址Arene Candide Cave的地层序列的最低部分,证明了利古里亚沿海(意大利西北部)晚清冰期开始时的重大气候和环境变化。这些考古层是使用一套包括矿物沉积学分析(微观形态学)的矿物学和化学技术进行研究的。这项研究表明,较低的层主要是由周期性碎裂的微黑和微红层或晶状体覆盖的碎屑沉积物所致。黑色层主要由鸟类和蝙蝠鸟粪沉积物组成,中间有薄薄的褐色风沙源沙质粉砂层,其中含有大量的磷酸钙。相反,由于铁以不溶形式重新氧化,鲜红色层是磨碎的沉淀物。在这些层中,与胶凝作用过程相关的同质冻融循环的证据表明,在(半)干旱冰缘环境中出现了凉爽的天气,并伴随着大约两次之间的湿度增加。 31和27 ka cal BP。随后,与反复的径流和泥石流过程相关的特征的出现,导致上覆沉积物中大量分层和分类不良的物质大量堆积,这表明湿润条件进一步加剧,并反映出湿润和温带气候的长期发展。从干旱到半干旱/潮湿的气候变化导致了上新世海洋阶地和洞穴外部土壤的侵蚀导致沉积物增加。在研究的鸟粪层序列和人工制品稀缺性的识别中,加上缺乏清晰的文化微观形态学证据,支持对中上古石器时代(Gravettian)零星人类占领该部分洞穴的解释。因此,在所谓的“年轻王子”的豪华葬礼的这种背景下的发现可能表明该洞穴当时被用作特殊的葬礼场所。

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  • 来源
    《Quaternary International》 |2013年第27期|42-55|共14页
  • 作者单位

    Department of Earth, Environment and Life Science (DISTAV), University of Genoa, C.so Europa 26, 16132 Genoa, Italy;

    Department of Earth, Environment and Life Science (DISTAV), University of Genoa, C.so Europa 26, 16132 Genoa, Italy;

    Collaborator of the Soprintendenza per i beni archeologici della Liguria, Genoa, Italy;

    Department of Anthropology, University of Colorado, Denver, USA;

    Scuola di specializzazione in beni archeologici (DAFIST), University of Genoa, via Balbi 4, 16126 Genoa, Italy;

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