{"title":"Multi-proxy evidence for woodland clearance in northeast Northumberland (England) during the Iron Age","authors":"Eline N. van Asperen, Jason R. Kirby, Helen Shaw","doi":"10.1007/s00334-023-00979-1","DOIUrl":null,"url":null,"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.","PeriodicalId":23527,"journal":{"name":"Vegetation History and Archaeobotany","volume":"33 4","pages":"559-575"},"PeriodicalIF":2.5000,"publicationDate":"2023-12-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s00334-023-00979-1.pdf","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Vegetation History and Archaeobotany","FirstCategoryId":"0","ListUrlMain":"https://doi.org/10.1007/s00334-023-00979-1","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
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.
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.