Regional variation in the response of vegetation to Lateglacial climatic events in Europe in Studies in the Lateglacial of North-West Europe.
There is great regional variation in the intensity of response of vegetation to Lateglacial climatic events in Europe. Between 11,000 and 10,000 radiocarbon years BP, a severe climatic deterioration brought about major changes in the species
to regional differences which have not been sufficiently appreciated in the literature. The deterioration from 11,000 to 10,000 BP is correlated with a readvance of polar water into the eastern North Atlantic. Evidently it affected coastal areas strongly
Europe is a natural geographical region for a common Quaternary stratigraphic nomenclature, and there does seem to be considerable agreement on the Lateglacial climate of this part of the world.
in altitude to the SW with a regional gradient of 0,13 m/km. It is suggested that the feature was formed by periglacial shore erosion during the Loch Lomond Stadial (Younger Dryas) and is of the same age as the Norwegian Main Line (P12). It is also proposed