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Multi-proxy investigations at 2 Pier Road, North Woolwich, London, UK, have revealed deposits spanning the Middle-Late Holocene from the late Mesolithic (c. 4360 cal BC) onwards. Pollen data show an Elm Decline at c. 4210–3950 cal BC followed by landnám clearances at c. 4210–3910 cal BC and c. 3710–3030 cal BC and the first appearance of cereal at c. 3540–3030 cal BC. These events are potentially contemporary with the construction of nearby Neolithic trackways, providing indirect evidence for agriculture and settlement. REVEALS modelling shows the first significant reduction in woodland cover is coincident with the Neolithic Elm decline, but the main step-change to open conditions occurred in the Early Bronze Age, following a decline in lime at c. 2110–1630 cal BC. Palaeo-topographic modelling of the region shows that although the trend towards increasing openness coincides with gradual wetland expansion, the shift to open vegetation cover cannot be explained by this and is probably the result of human activity. This study highlights the value of combining deposit and vegetation cover modelling to contextualise wetland archaeology and shows that together these provide useful proxies for landscape-scale human activity that can identify ephemeral signals of prehistoric activity. [ABSTRACT FROM AUTHOR]

Iona is renowned for its early monastery, founded following the arrival of Columba in AD 563. This paper uses palaeoecological data to provide insight into the social and environmental transformations that influenced the landscape of Iona during the later prehistoric and historic periods. The identification of cereal pollen suggests that arable farming occurred during the Bronze Age and possibly continued through the Iron Age. Pastoral farming was also practiced. It remains unclear as to whether there were people living on the island at the time of the monastic community's arrival. Between AD 630 and 1100, woodland clearance and farming occurred. There were also two phases of woodland regeneration and agricultural decline. The first phase coincides with the period of Viking raids and may have witnessed a decline in population. The second phase occurred in conjunction with increased Scandinavian influence and political restructuring across the wider region; however, small-scale farming continued. After c. AD 1000 there was renewed intensification of landscape management prior to the arrival of Benedictine monks and Augustinian nuns (c. AD 1200). This may be linked to climatic amelioration during the Medieval Warm Period and economic growth in the Hebrides. [ABSTRACT FROM AUTHOR]

SUMMARY: Excavation at Liverpool Street, London, for Crossrail Limited, uncovered two large drains and a pit in an area of the city known since the medieval period as 'Moorfields'. Their fills can be closely dated to the mid 16th century and included artefacts such as personal possessions, domestic utensils and refuse, and material likely to be waste from leather and textile processing. The combination of excellent preservation, tight dating and an assemblage encompassing all facets of everyday life is seldom encountered for this period, making this a nationally significant assemblage, which is outlined here by broad functional category. [ABSTRACT FROM AUTHOR]

Two new multi-proxy records of environmental change are provided from Horton Kirby Paper Mill and Old Seager Distillery in the Lower Thames Valley. Each site has evidence for a decline in elm woodland, which at Horton Kirby Paper Mill is recorded earlier than any other published record from the British Isles: sometime between 7320 and 7240 cal BP. Scolytus scolytus/S. multistriatus (the vectors for Dutch elm disease) are recorded after the decline in both sequences, adding to the number of sites with such evidence in the British Isles. Evidence of paludification and human activity are also recorded at the time of the elm decline reinforcing the multi-causal hypothesis. Integration of these results with 21 palaeoenvironmental records has produced a large number of well-dated, multiproxy records of the elm decline in this part of the UK. On the basis of this dataset, a classification system for categorising the relationships between the causal factors of the elm decline is proposed and recommended for future studies. [ABSTRACT FROM AUTHOR]