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The microstratigraphic record of human activities and formation processes at the Mesolithic shell midden of Pocas de Sao Bento (Sado Valley, Portugal)

机译:Pocas de Sao Bento(Sado Valley,Portugal)的人类活动和形成过程的微观信息记录

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Shell midden formation is largely controlled by anthropogenic processes, resulting from human exploitation of aquatic resources. This makes shell middens archives of both human behaviour and palaeoenvironmental records. However, their often complex stratigraphy hampers the isolation of individual anthropogenic events. In the central/southern coast of Portugal, extensive inland estuaries were preferential settings for Mesolithic groups from c. 6200 cal BC. Here, we present a microstratigraphic approach to the shell midden of Pocas de Sao Bento, one of the largest and best-known sites in the Sado Valley. The microfacies approach was based on sedimentary components, their abundance and arrangement, and post-depositional processes. Anthropogenic processes identified as tossing events and anthropogenically reworked deposits allowed inferences on spatial organisation, preferential refuse areas, occupational surfaces, and temporality of the occupations. The presence of calcareous pebbles in the anthropogenic, shell-rich sediments, together with foraminifera, presumably from the estuarine marshes, is compared with the regional geology, providing a hypothetical location of the shellfish gathering. The microstratigraphy described reveals a full internal dynamic in the formation of the apparently homogeneous shell midden layer. The human activities inferred at Pocas de Sao Bento have many similarities with those reported for Cabeco da Amoreira in the nearby Tagus palaeo-estuary. This evidence points to the need for further micromorphological approaches in similar deposits. The study of shell midden formation processes, through integrative microcontextual approaches, plays a major role in understanding Mesolithic societies in the large early Holocene estuary environments of Atlantic Iberia.
机译:壳体中间形成主要受到人为过程的控制,由人类利用水生水生成。这使得人类行为和古环境记录的壳体档案。然而,他们的经常复杂的地层困扰着单独的人为事件的分离。在葡萄牙的中央/南部海岸,广泛的内陆河口是来自C的亚伯里斯基团的优先设置。 6200 CAL BC。在这里,我们为萨达谷的最大和最着名的网站之一提供了一种微观图替方法。微电容方法基于沉积组分,其丰富和布置和沉积后的过程。鉴定为折腾事件和人为重新加工的存款的人为过程允许在空间组织,优先垃圾区,职业表面和职业的暂时性上推断。将钙质卵石在人为,富含脱壳的沉积物中存在与Foraminifera一起存在,这与雌缕属沼泽相比,与区域地质进行比较,提供贝类聚集的假设位置。所描述的微观数据描绘在形成明显均匀的壳体层的形成中揭示了全内部动态。 Pocas de Sao Bento推断的人类活动与附近的塔比帕拉诺 - 河口的Cabeco da Amoreira报道的人有许多相似之处。本证据点指出了类似沉积物中进一步的微观晶体方法。通过综合微观文密方法,壳中间形成过程的研究在理解大西洋伊比利亚大型全新诗河口环境中了解沉思社会的主要作用。

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