La palafitta di Tombola di Cerea (Verona) (Scavo 1999)

L. Salzani, Claudio Balista, P. Butta, N. Martinelli, P. Torri, G. Bosi, M. Mazzanti, A. Mercuri, C. A. Accorsi, M. Bertolini, U. T. Hohenstein
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The structural elements of the palafitte find correspondents in others settlements in moist environment from the Middle Bronze Age. The paleogeographic reconstruction of the immediate hinterland confirm the location of the site at the center of the Menago River Paleovalley, an incision a few hundred meters wide and more than ten meters deep, at the base of a thick layer of peat. Previous studies, related to the origin of the deep incision generated by the homonymous spring-line river, mainly refer to geodynamic factors linked to buried tectonic lines, as main motives for the incisions caused by the diversion of Adige breach-channels captured towards the basin of Great Veronese Valleys, which occurred in the late Lateglacial-Holocene age. The analysis of new lithostratigraphies detected on exposures inside the paleovalley, has led to find the presence of a thick and almost continuous filling of organic-peaty sediments, which mark the accretions and the sedimentations verified starting from the basal levels of the pile-dwelling site, depositions that have lasted until fairly recent dates. A series of detailed comparisons made with the terms of the peat-debris-filling sequences of the basin that developed outside the embankments of the near and coeval Fondo Paviani site, led to verify a similar evolution in the growths that mark the upper reaches of these two important alluvio-organic successions. Ultimately, is claimed that the same incidence, of anthropogenic and climatic factors, is involved as the main contributors to the development of the upper fills of the Menago Paleovalley, in correspondence with the pile-dwelling station of the Tombola di Cerea and the embanked site of Fondo Paviani. A great number of ceramic fragments (ca 620 kg) and a smaller amount of bronze, terracotta and bone-horn artefacts had been found. This paper focus on chrono-typological analysis of the archaeological finds, in particular on ceramic of the medium-fine tipe. The goal is the overall classification artefacts, accompanied by a comparison made from materials found in geographically nearbysites. Dendrochronology and radiocarbon allow to date the wooden structures to the second half of the 15th Century cal BC, or in the first decades of the 14th Century cal BC at the latest; the vertical posts come from oak tree felled down once about every ten years. Archaeobotanical study includes pollen analysis carried out on 18 subsamples taken from a core collected in the pile-dwelling settlement and carpological and xilo-anthacological analysis, from 2 samples taken from layers (stratigraphic units) corresponding to the bottom of the core. 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Hunting was barely practiced on wild ungulates (red deer, roe deer, wild boar). Several anthropic marks were identified on the faunal remains emphasizing the use of lithic and metal tools. During the analysis 18 animal hard material artefacts were identified. 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引用次数: 1

Abstract

The pile dwelling was discovered in 1955 in the valley of the river Menago, just a few hundred meters south of the settlement of Tombola di Cerea (VR). A first excavation was carried out that very year by Francesco Zorzi, director of the Museo Civico di Storia Naturale of Verona; the digging has been resumed in 1999 by the Soprintendenza Archeologica of Veneto. The results of these excavations have ascertained that the prehistoric dwelling site was built in a marshy environment. Only some vertical poles and some horizontal beams were preserved, which leads to the hypothesis that there existed a wooden platform on which the sheds were standing. The structural elements of the palafitte find correspondents in others settlements in moist environment from the Middle Bronze Age. The paleogeographic reconstruction of the immediate hinterland confirm the location of the site at the center of the Menago River Paleovalley, an incision a few hundred meters wide and more than ten meters deep, at the base of a thick layer of peat. Previous studies, related to the origin of the deep incision generated by the homonymous spring-line river, mainly refer to geodynamic factors linked to buried tectonic lines, as main motives for the incisions caused by the diversion of Adige breach-channels captured towards the basin of Great Veronese Valleys, which occurred in the late Lateglacial-Holocene age. The analysis of new lithostratigraphies detected on exposures inside the paleovalley, has led to find the presence of a thick and almost continuous filling of organic-peaty sediments, which mark the accretions and the sedimentations verified starting from the basal levels of the pile-dwelling site, depositions that have lasted until fairly recent dates. A series of detailed comparisons made with the terms of the peat-debris-filling sequences of the basin that developed outside the embankments of the near and coeval Fondo Paviani site, led to verify a similar evolution in the growths that mark the upper reaches of these two important alluvio-organic successions. Ultimately, is claimed that the same incidence, of anthropogenic and climatic factors, is involved as the main contributors to the development of the upper fills of the Menago Paleovalley, in correspondence with the pile-dwelling station of the Tombola di Cerea and the embanked site of Fondo Paviani. A great number of ceramic fragments (ca 620 kg) and a smaller amount of bronze, terracotta and bone-horn artefacts had been found. This paper focus on chrono-typological analysis of the archaeological finds, in particular on ceramic of the medium-fine tipe. The goal is the overall classification artefacts, accompanied by a comparison made from materials found in geographically nearbysites. Dendrochronology and radiocarbon allow to date the wooden structures to the second half of the 15th Century cal BC, or in the first decades of the 14th Century cal BC at the latest; the vertical posts come from oak tree felled down once about every ten years. Archaeobotanical study includes pollen analysis carried out on 18 subsamples taken from a core collected in the pile-dwelling settlement and carpological and xilo-anthacological analysis, from 2 samples taken from layers (stratigraphic units) corresponding to the bottom of the core. The results allows to draw the environmental framework of the settlement. The pollen diagram shows that the landscape was rich of wet environments: ponds, wet grassland and hygrophilous wood. The human activity was suggested by a number of anthropogenic indicators: cereal fields, ruderals and weeds. Seeds/fruits and pollen data testify to the presence in the area of edible fruits from plants such as blackthorn, hazelnut, currant, walnut and grapevine. The finds of Baldellia ranuncoloides – a threatened plants today - underline that the archaeobotanical research provide naturalistic information that allow us to better understand the history of plant species becoming rare today. The faunal assemblage is composed by 1995 bone remains. More than 80% of the faunal remains was identified at species level. Domestic animals are the most frequent. Age at death highlights different breeding strategies focused on meat consumption and secondary products. Hunting was barely practiced on wild ungulates (red deer, roe deer, wild boar). Several anthropic marks were identified on the faunal remains emphasizing the use of lithic and metal tools. During the analysis 18 animal hard material artefacts were identified. The good state of preservation allowed us to identify working traces linked to the reduction sequences of the tools.
Cerea宾果别墅(维罗纳)(Scavo 1999)
1955年,在Tombola di Cerea (VR)定居点以南几百米的Menago河山谷中发现了这个桩式住宅。就在那一年,维罗纳自然历史博物馆(Museo Civico di Storia Naturale)馆长弗朗西斯科·佐齐(Francesco Zorzi)进行了第一次发掘;1999年,威尼托的Soprintendenza考古学家恢复了挖掘工作。这些发掘的结果已经确定,史前居住地点是建在沼泽环境。只有一些垂直的杆子和一些水平的梁被保留下来,这导致了一个假设,即存在一个木平台,棚子就站在上面。古屋的结构元素在青铜时代中期潮湿环境中的其他定居点中也发现了相应的结构元素。直接腹地的古地理重建确认了遗址的位置,位于梅纳戈河古山谷的中心,这是一个几百米宽、十多米深的切口,位于一层厚厚的泥炭的底部。前人对同名泉线河流形成的深切口成因的研究,主要是将与隐伏构造线有关的地球动力学因素作为阿迪杰决口河道向大韦罗内塞河谷盆地转移的主要动机,这种情况发生在晚冰川期-全新世。对古山谷内部暴露物的新岩石地层学分析发现,存在着一层厚厚的、几乎连续不断的有机泥炭质沉积物,这标志着从桩居住地的基底层开始的增生和沉积,这些沉积一直持续到相当近的年代。与Fondo Paviani遗址附近和同时期河堤外的盆地泥炭-碎屑-充填序列进行的一系列详细比较,证实了标志着这两个重要冲积-有机序列上游的生长的类似演变。最后,有人声称,与Tombola di Cerea的桩屋站和Fondo Paviani的堤岸遗址相对应,Menago古山谷上部填埋物的发展主要是由于人为因素和气候因素的影响。发现了大量的陶瓷碎片(约620公斤)和少量的青铜、兵马俑和骨角人工制品。本文着重对考古发现的年代类型进行了分析,特别是对中细粒陶瓷进行了分析。目标是对人工制品进行总体分类,并与在地理上邻近的地点发现的材料进行比较。树木年代学和放射性碳测定可以将木结构的年代确定为公元前15世纪下半叶,或最迟公元前14世纪前几十年;垂直的柱子来自每十年被砍伐一次的橡树。考古植物学研究包括对从桩居聚落采集的岩心中采集的18个亚样本进行花粉分析,以及对从岩心底部对应的层(地层单位)中采集的2个样本进行人类学和西洛人类学分析。结果可以绘制出住区的环境框架。花粉图显示,该景观具有丰富的湿润环境:池塘、湿润草地和亲湿性木材。一些人为指标:谷物田、农田和杂草表明了人类活动的存在。种子/果实和花粉数据证明了该地区存在可食用的植物果实,如黑刺木、榛子、加仑子、核桃和葡萄藤。这一发现强调了考古植物学研究提供了自然主义的信息,使我们能够更好地了解当今稀有植物物种的历史。动物群由1995年的骨骸组成。超过80%的动物遗骸在物种水平上得到了鉴定。家畜是最常见的。死亡年龄突出了以肉类消费和次级产品为重点的不同育种策略。对野生有蹄类动物(马鹿、狍子、野猪)几乎不进行狩猎。在动物遗骸上发现了几个人类留下的痕迹,强调使用了石器和金属工具。在分析过程中,鉴定出18个动物硬材料人工制品。良好的保存状态使我们能够识别与工具还原序列相关的工作痕迹。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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