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1 School of Geography, University of Leeds, Leeds LS2 9JT, UK
2 Department of Geography, University of Sussex, Brighton BN1 9QJ, UK
3 Department of Geography and Environment, University of Aberdeen, Aberdeen AB24 3UF, UK
4 Department of Zoology, University of Cambridge, Cambridge CB2 3EJ, UK
5 Grup de Recerca Consolidat (GRC) Geociències Marines, Universitat de Barcelona, 08028 Barcelona, Spain
6 Godwin Laboratory, Department of Earth Sciences, University of Cambridge, Cambridge CB2 3SA, UK
The regional expression of millennial-scale climate variability during the last glacial is examined with particular reference to the vegetation response in Greece. Inspection of three pollen records from contrasting bioclimatic areas suggests that differences in the magnitude of cold events as recognized in the North Atlantic and western Mediterranean are expressed in terms of tree population changes only in areas with a range of favorable habitats. By contrast, records from sites where populations approach their tolerance threshold do not appear to resolve differences in the amplitude of the climate oscillations. Understanding the importance of local factors in modulating the biological response to climate change is critical when attempting to establish the spatial pattern of millennial variability.
Key Words: paleoclimatology paleoecology last glacial North Atlantic Greece
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