Recent investigations at Camp Fauld in Buchan, Scotland have yielded t
wo peat deposits of pre-late Devensian age. Percentage pollen diagrams
are presented. One peat is radiocarbon-dated to 34-39 ka sp, which pr
ompts correlation with the Hengelo-Denekamp sequence of NW continental
Europe, but the pollen evidence, revealing the presence of a birch-pi
ne woodland, suggests an earlier stage. The second peat deposit record
s an open shrub-tundra in which Bruckenthalia spiculifolia is present.
The peat yielded a radiocarbon date of 40-51 ka sp, but is suspected
of having been contaminated by younger carbon. That suspicion and the
presence of Bruckenthalia suggest that a correlation, based on the rad
iocarbon date, with the Glinde interstadial, identified in NW Germany,
would be incorrect. Correlation with other Scottish pre-late Devensia
n sites has proved to be difficult.