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The effects of the Avellino Pumice eruption on the population of the Early Bronze age Campanian plain (Southern Italy)

机译:阿韦利诺浮石喷发对早期青铜时代的Campanian平原(意大利南部)人口的影响

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摘要

Palma Campania, the type-site of the Early Bronze Age Palma Campania culture, was covered by the products of the Avellino Pumice eruption, and was thus preserved in a similar way to the Roman sites in Campania covered by the AD 79 eruption. The devastating effects of this Plinian eruption led to the belief that it had killed a large part of the local population and/or caused large-scale emigration and landscape desertification. However, new sites have been found that were established shortly after the eruption and geoarchaeological studies of areas close to the Somma-Vesuvius volcano (Boscoreale, Boscotrecase, Torre Annunziata/Oplontis, Pompeii) and also further away (the Benevento area, Irpinia and the Salerno area) have shown continuity of occupation after the Avellino Pumice eruption and during the later, Middle Bronze Age, AP1 and AP2 eruptions. Palynological analysis also shows great similarly between the environments before and after the Avellino Pumice eruption. The pottery evidence is typologically very similar before and after the eruption, which suggests that the people who resettled the Campanian plain after the eruption were closely related to those living there previously, whose material culture is that of the Palma Campania culture. Radiocarbon dates also suggest a rapid recolonisation of some sites. In this paper we shall show that although the pyroclastic products of the Avellino Pumice eruption certainly had a major impact on the landscape (soils, flora, water resources) and may have killed off a percentage of the population in some areas, this eruption was not the main cause of the socio-economic and political transformations that occurred in this area during the Middle Bronze Age, which we believe to have been mainly caused by the cumulative effect of the later AP1 and AP2 eruptions.
机译:帕尔玛·坎帕尼亚(Palma Campania)是青铜时代早期的帕尔玛·坎帕尼亚(Palma Campania)文化的典型遗址,被阿韦利诺浮石(Avellino Pumice)喷发的产物覆盖,因此以类似于公元79年爆发的坎帕尼亚罗马遗址的方式保存。这次普林尼亚火山喷发的毁灭性影响使人们相信,它已经杀死了很大一部分当地人口和/或引起了大规模的移民和景观沙漠化。但是,已经发现在索马-维苏威火山附近的地区(Boscoreale,Boscotrecase,Torre Annunziata / Oplontis,庞贝城)以及附近(贝内文托地区,Irpinia和萨勒诺地区)在阿韦利诺浮石喷发后以及青铜器中期,AP1和AP2爆发之后显示出占领的连续性。孢粉学分析还显示,Avellino浮石喷发前后的环境非常相似。在喷发前后,陶器证据在类型上非常相似,这表明在喷发之后重新安置了坎帕尼亚平原的人们与先前居住在那里的人密切相关,他们的物质文化是帕尔马坎帕尼亚文化。放射性碳年代数据还表明某些地点迅速重新定殖。在本文中,我们将表明,尽管阿韦利诺浮石喷发的火山碎屑产物确实对景观(土壤,植物,水资源)产生了重大影响,并且可能杀死了某些地区的一部分人口,但这种喷发并未青铜时代中期在该地区发生的社会经济和政治转变的主要原因,我们认为这主要是由后来的AP1和AP2爆发的累积效应引起的。

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  • 来源
    《Quaternary International》 |2019年第ptab期|205-220|共16页
  • 作者单位

    CNRS, AMU, UMR 7299, Ctr Camille Jullian,MMSH, 5 Rue Chateau Horloge, F-13094 Aix En Provence, France;

    Univ Nottingham, Dept Class & Archaeol, Mediterranean Prehist, Nottingham NG7 2RD, England;

    Univ Naples L Orientale, Dept Asian African & Mediterranean Studies, Piazza S Domenico Maggiore 12, I-80134 Naples, Italy|ISMEO Int Assoc Mediterranean & Oriental Studies, Corso Vittorio Emanuele 2,244, I-00186 Rome, Italy;

    CNR, Ist Tecnol Appl Beni Culturali, Area Ric 1, Rome, Italy;

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