The field system of Gricignano d'Aversa (Southern Italy) and the agrarian impact in the Piana Campana, ca. 3900 cal BP
The field system of Gricignano d'Aversa (Southern Italy) and the agrarian impact in the Piana Campana, ca. 3900 cal BP
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Gricignano dAversa（意大利南部）的田地系统和对皮亚纳坎帕纳的农业影响，约。
DOI：
10.1016/j.quaint.2013.02.021
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发表时间：
2013
影响因子：
2.2
通讯作者：
A. Vanzetti
中科院分区：
文献类型：
--
作者：
F. Saccoccio;Amodio Marzocchella;A. Vanzetti
皮亚纳坎帕纳（南意大利）最近透露，其详细的考古和环境数据的恢复潜力，在晚全新世，由于索玛-维苏威火山和Campi Flegrei火山复合体的活动造成的存款增厚。定居点、墓葬、景观和农业基础设施（道路、田地、威尔斯等）这表明至少从新石器时代晚期（约2000年）以来，6.2 ka cal BP）。本研究来自考古研究支持的Soprintendenza per i贝尼Archeologici della Campania和Soprintendenza al Museo Nazionale Preistorico Etnografico“L. Pigorini”，Roma（1995-2005）.介绍了在Gricignano d 'Aversa/美国海军支援基地（Caserta）发现的史前（青铜时代早期）农业痕迹的综合模式。描述了一个60公顷的不间断的犁耕表面和田地系统，直接保存在Pomici di Avellino火山爆发（约200年）的下方。3900 cal BP）。在意大利，第一次重建了如此广泛的原始田野系统。农业特征（银行，冲沟，一个马车轨道）显示出显着的规律性，暗示在模式化的景观开发。通过在Piana Campana的背景下设置这些结果来扩大讨论。区域考古和花粉数据证实了这一时期对景观的显著农业影响。乔木花粉在Pomici di Avellino喷发下的值一般较低，但在此事件后平原上的值增加，可能是由于主要定居点迁移到更易迁移的地点。已确定的人类影响是由于从新石器时代晚期到青铜时代早期，人类社区采取的长期转变的农业战略。
The Piana Campana (Southern Italy) has recently revealed its potential for the recovery of detailed archaeological and environmental data, during the Late Holocene, due to the thickening of the deposits caused by the activity of the volcanic complexes of Somma-Vesuvius and Campi Flegrei. Settlements, burials, landscape and agrarian infrastructures (tracks, fields, wells, etc.) indicate an intense and continuous human presence since at least late Neolithic times (ca. 6.2 ka cal BP). This study derives from archaeological research supported by the Soprintendenza per i Beni Archeologici della Campania and the Soprintendenza al Museo Nazionale Preistorico Etnografico “L. Pigorini”, Roma (1995–2005). The comprehensive pattern of the protohistoric (Early Bronze Age) agrarian traces found at Gricignano d'Aversa/U.S. Navy support site (Caserta) is presented. An uninterrupted ploughed surface and field system of 60 ha is described, preserved directly below the Pomici di Avellino eruption (ca. 3900 cal BP). For the first time in Italy, such a wide protohistoric field system was reconstructed. The agrarian features (banks, gullies, one cart track) show a remarkable regularity, hinting at patterned landscape exploitation. The discussion is widened by setting these results in the context of the Piana Campana. Regional archaeological and pollen data confirm the marked agrarian impact over the landscape during this period. Arboreal pollen has generally low values under the Pomici di Avellino eruption, but it increases in the plain after this event, possibly due to the main settlement relocation in more defendable spots. The identified anthropic impact is due to the long-lasting shifting agricultural strategy adopted by human communities from the late Neolithic to the Early Bronze Age.