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A multidisciplinary study of an exceptional prehistoric waste dump in the mountainous inland of Calabria (Italy): Implications for reconstructions of prehistoric land use and vegetation in Southern Italy

机译:卡拉布里亚山区内陆的特殊史前废物倾倒的多学科研究(意大利):史前土地利用与意大利南部植被的影响

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The mountainous inland of northern Calabria (Southern Italy) is known for its sparse prehistoric human occupation. Nevertheless, a thorough multidisciplinary approach of field walking, geophysical survey and invasive research led to the discovery of a major archaeological archive. This archive concerns a rich multi-phased dump, spanning about 3000 years (Late Neolithic to Late Imperial Roman Age) and holding two Somma-Vesuvius tephra. Of these, the younger is a distinct layer of juvenile tephra from the Pompeii eruption, while the older concerns reworked tephra from the Bronze Age AP2 eruption (ca. 1700 cal. yr BP). The large dump contains abundant ceramics, faunal remains and charcoal, and most probably originated through long-continued deposition of waste in a former gully like system of depressions. This resulted in an inversed, mound-like relief, whose anthropogenic origin had not been recognized in earlier research. The tephras were found to be important markers that support the reconstruction of the occupational history of the site. The sequence of occupational phases is very similar to that observed in a recent palaeoecological study from nearby situated former lakes (Lago Forano/Fontana Manca). This suggests that this sequence reflects the more regional occupational history of Calabria, which goes back to ca. 3000 BC. Attention is paid to the potential link between this history and Holocene climatic phases, for which no indication was found. The history deviates strongly from histories deduced from the few, but major palaeorecords elsewhere in the inlands of Southern Italy (Lago Grande di Monticchio and Lago Trifoglietti). We conclude that major regional variation occurred in prehistoric land use and its impacts on the vegetation cover of Southern Italy, and studies of additional palaeoarchives are needed to unravel this complex history. Finally, shortcomings of archaeological predictive models are discussed and the advantages of truly integrated multidisciplinary research.
机译:卡拉布里亚北部的山区内陆(意大利南部)以其稀疏的史前人类占领而闻名。尽管如此,彻底的多学科方法的实地步行,地球物理调查和侵入性研究导致了一个主要的考古档案的发现。这个档案涉及丰富的多相倾倒,跨越大约3000年(晚期到后期帝国罗马年龄)和举行两个索马 - 维苏威Tephra。其中,年轻人是庞培爆发中的少年Tephra的独特层,而老年人则从青铜年龄AP2喷发中重新改造Tephra(约1700克。YR BP)。大型垃圾箱含有丰富的陶瓷,动物遗骸和木炭,大部分可能是通过在前沟壑的萧条系统中长期沉积的废物沉积。这导致了逆转的土墩状的浮雕,其人为的起源在早期的研究中尚未认识到。发现Tephras是一个重要的标志,支持重建现场的职业历史。职业阶段的序列与附近的前湖泊(Lago Forano / Fontana Manca)的古生学研究中观察到的序列非常相似。这表明这一序列反映了卡拉布里亚的区域职业历史,返回加州。 3000公元前。关注这一历史和全仑气候阶段之间的潜在联系,没有发现任何指示。这些历史强烈地偏离了来自少数几个,但意大利南部内陆的主要古兰经(Lago Grande di Monticchio和Lago Trifoglietti)的主要古怪古怪的历史。我们得出结论,史前土地使用的主要区域变异及其对意大利南部植被覆盖的影响,并且需要研究额外的古代群体来解开这种复杂的历史。最后,讨论了考古预测模型的缺点以及真正集成的多学科研究的优势。

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