Multi-proxy evidence for woodland clearance in northeast Northumberland (England) during the Iron Age

IF 2.5 2区 地球科学 Q1 PALEONTOLOGY
Eline N. van Asperen, Jason R. Kirby, Helen Shaw
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引用次数: 1

Abstract

Abstract Pollen diagrams covering the Bronze Age to Roman period from northeast Northumberland are scarce. We present a 14 C-dated pollen record from a peat-filled forest hollow in Chillingham Wild Cattle Park, northeast Northumberland, that spans the Iron Age. For the first time for this part of Northumberland, fungal spores are also analysed to investigate whether clearances took place in the context of crop cultivation or pastoralism. The pollen diagram shows significant woodland cover during the Late Bronze Age, with small-scale landscape openness potentially representing crop cultivation and animal grazing under a tree canopy. A local clearance event, with arboreal pollen falling to 13.2%, is radiocarbon dated to the late Early to Middle Iron Age, likely coinciding with the construction and occupancy of the nearby Ros Castle hillfort. A significant rise in dung fungal spores and the presence of Plantago and other open vegetation taxa indicate animal husbandry played an important role in this clearance phase. A subsequent large decrease in dung fungi and a small rise in arboreal pollen may reflect a degree of abandonment of the area after the climate cooled. Peat formation ceased in the late Middle to Late Iron Age as the hollow filled up. Limited renewed peat growth occurred in the last century or so, after peat shrinkage due to drying and consequent oxidation provided the possibility for renewed peat formation within the hollow.
铁器时代英格兰诺森伯兰郡东北部林地砍伐的多代理证据
诺森伯兰郡东北部覆盖青铜时代至罗马时期的花粉图十分稀少。我们在诺森伯兰郡东北部的奇灵厄姆野牛公园的一个充满泥炭的森林空洞中展示了一个14 c的花粉记录,它跨越了铁器时代。对于诺森伯兰郡的这一部分,真菌孢子也首次被分析,以调查是否在作物种植或畜牧业的背景下发生了清除。花粉图显示了青铜时代晚期大量的林地覆盖,小规模的景观开放可能代表了树冠下的作物种植和动物放牧。一个当地的清除事件,树木花粉下降到13.2%,放射性碳可以追溯到铁器时代早期晚期到中期,可能与附近的罗斯城堡山堡的建设和占用相吻合。粪便真菌孢子的显著增加以及车前草和其他开放植被分类群的存在表明畜牧业在这一清除阶段发挥了重要作用。随后粪便真菌的大量减少和树木花粉的少量增加可能反映了气候变冷后该地区在一定程度上被遗弃。泥炭的形成在中晚期到铁器时代晚期停止,因为洼地被填满了。有限的再生泥炭生长发生在上个世纪左右,在泥炭因干燥和随后的氧化而收缩后,在空心中提供了再生泥炭形成的可能性。
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来源期刊
CiteScore
5.30
自引率
8.00%
发文量
32
审稿时长
>12 weeks
期刊介绍: Vegetation History and Archaeobotany publishes research papers, review articles and short contributions of high quality from Europe, the Americas and other parts of the world. It covers the entire field of vegetation history – mainly the development of flora and vegetation during the Holocene (but also from the Pleistocene), and including related subjects such as palaeoecology. Of special interest is the human impact upon the natural environment in prehistoric and medieval times; this is reflected in pollen diagrams as well as in plant macroremains from archaeological contexts.
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