Abstract
Recent investigations at Camp Fauld in Buchan, Scotland have yielded two peat deposits of pre-late Devensian age. Percentage pollen diagrams are presented. One peat is radiocarbon-dated to 34-39 ka sp, which prompts correlation with the Hengelo-Denekamp sequence of NW continental Europe, but the pollen evidence, revealing the presence of a birch-pine woodland, suggests an earlier stage. The second peat deposit records 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 radiocarbon date, with the Glinde interstadial, identified in NW Germany, would be incorrect. Correlation with other Scottish pre-late Devensian sites has proved to be difficult.
| Original language | English |
|---|---|
| Pages (from-to) | 867-874 |
| Number of pages | 8 |
| Journal | New Phytologist |
| Volume | 125 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - Dec 1993 |
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