Problems associated with radiocarbon dating the close of the Lateglacial period in the Rannoch Moor area, Scotland in Studies in the Lateglacial of North-West Europe.
Radiocarbon dates spannning the Lateglacial-Flandrian transition are presented from seven sites in the Rannoch Moor area of the Grampian Highlands, Scotland. Problems associated with the interpretation of these dates are discussed, and possible
a climatostratigraphy recording climatic amelioration from the Late Devensian to the Flandrian, with a brief reversal corresponding to the Loch Lomond Stadial. Such complete sequences are rare onshore, but available offshore near the west coast of Scotland
. There are still problems when correlation is attempted from west to east coast sequences in Scotland, and correlation is sought with the published North Sea records. Such problems require fuller, more detailed study of continuous cores for ostracod data
Circulation atmosphérique ; Géographie physique ; Lake District ; Paléoclimatologie ; Précipitation ; Quaternaire zones moyennes ; Royaume-Uni ; Scotland ; Stade du Loch Lomond ; Tardiglaciaire
Equilibrium firn line altitudes and relative dimensions of Loch Lomond Advance glaciers in Scotland and the Lake District indicate that snowfall was associated mainly with S to SE air streams preceding warm and occluded fronts, although SW air
Environmental change during the Loch Lomond Stadial: evidence from a site in the upper Spey valley, Scotland in Studies in the Lateglacial of North-West Europe.
Enneigement ; Géographie de l'Europe ; Palynologie ; Paléo-environnement ; Paléoclimatologie ; Quaternaire zones moyennes ; Royaume-Uni ; Scotland ; Spey, valley ; Stade du Loch Lomond ; Tardiglaciaire