The period following the Roman withdrawal from England in AD 410 has long been considered a time of ‘cultural decline’, owing to the relative paucity of archaeological evidence relating to this time and the dismal state of affairs described by the Dark Age historians Gildas (c AD 540) and Bede (AD 731). Traditionally this period has been viewed as a time of chaos in which farmland was abandoned and the population declined, leading to woodland regeneration in many areas. In Northwest England, archaeological remains for the early medieval period (c AD 410-1066) are sparse. Early palynological studies in Cumbria, for which radiocarbon dates were often lacking or imprecise, frequently assigned major ‘woodland clearances’ to the Romano-British p...
PhD ThesisThe vegetation history of the North Tyne basin, northern England, is presented for an e...
In a recent discussion of research priorities for palaeoecology, it was suggested that palaeoecologi...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
Multi-proxy palaeoecological analyses were conducted on late Holocene cores taken from six sites in ...
Pollen diagrams from nine mire sites in northern Britain have been constructed to assess the record ...
This is the author accepted manuscript. the final version is available from Brill via the DOI in thi...
This paper presents the results of palynological investigations on the limestone Tabular Hills of th...
The historic era, which in Cumbria begins with the Roman invasion of AD 71, is a frequently neglecte...
Pollen diagrams covering the Bronze Age to Roman period from northeast Northumberland are scarce. We...
Large areas of upland mire and moorland in Northwest Europe are regarded as degraded, not actively p...
The pollen spectra from four lakes and two peat bogs in lowland north Shropshire show that in the Ne...
Copyright © 2004 Elsevier. NOTICE: This is the author’s final version of a work accepted for publica...
The influence of anthropogenic activity on the natural environment is constantly changing. A series...
A number of analytical techniques have been applied to four peat profiles from three ombrotrophic mi...
This is the author accepted manuscript. The final version is available from Oxbow via the link in t...
PhD ThesisThe vegetation history of the North Tyne basin, northern England, is presented for an e...
In a recent discussion of research priorities for palaeoecology, it was suggested that palaeoecologi...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
Multi-proxy palaeoecological analyses were conducted on late Holocene cores taken from six sites in ...
Pollen diagrams from nine mire sites in northern Britain have been constructed to assess the record ...
This is the author accepted manuscript. the final version is available from Brill via the DOI in thi...
This paper presents the results of palynological investigations on the limestone Tabular Hills of th...
The historic era, which in Cumbria begins with the Roman invasion of AD 71, is a frequently neglecte...
Pollen diagrams covering the Bronze Age to Roman period from northeast Northumberland are scarce. We...
Large areas of upland mire and moorland in Northwest Europe are regarded as degraded, not actively p...
The pollen spectra from four lakes and two peat bogs in lowland north Shropshire show that in the Ne...
Copyright © 2004 Elsevier. NOTICE: This is the author’s final version of a work accepted for publica...
The influence of anthropogenic activity on the natural environment is constantly changing. A series...
A number of analytical techniques have been applied to four peat profiles from three ombrotrophic mi...
This is the author accepted manuscript. The final version is available from Oxbow via the link in t...
PhD ThesisThe vegetation history of the North Tyne basin, northern England, is presented for an e...
In a recent discussion of research priorities for palaeoecology, it was suggested that palaeoecologi...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...