Abstract
Pollen records from two lake sites located in areas of modern heathland were used to reconstruct the local development of this vegetation type. A pollen record obtained from Loch of Knitchen on Rousay covered the last 6000 radiocarbon years. Betula-Corylus scrub was once locally present, although never a dominant community. Heath vegetation began to develop around 5700 BP. At about 5400 BP woodland taxa declined, possibly in response to Neolithic human activity, and heathland expanded. Calluna vulgaris increas ingly dominated the record thereafter, reflecting local blanket peat development. Data from Loch of Torness on Hoy cover the period from 7700 BP to around 4800 BP. Initial tall herb-type vegetation was replaced by a mixture of trees and heath taxa at around 7000 BP. Arboreal taxa declined at about 6000 BP, and the sub sequent record showed the development of maritime-type heath. The data show that heathland vegetation has been present in Orkney since at least 7000 BP, and that a range of causal processes have been important.