Abstract
AbstractA palaeotemperature record based on fossil coleopteran evidence and dated by accelerator mass spectroscopy (AMS) 14C determinations on plant macrofossils has been obtained for the last glacial‐interglacial transition from the site of Gransmoor in eastern England. Calibration of the radiocarbon measurements enabled a direct comparison to be made between this palaeotemperature curve and the snow accumulation record from the GISP‐2 Greenland ice‐core. The similarity between the two data sets suggests a degree of correspondence in the pattern and timing of climatic change in Greenland and the British Isles at the end of the last cold stage.
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