Abstract
PROXY temperature records from Greenland ice cores1,2 and North Atlantic sediment cores3 have provided evidence for a high degree of climate instability during the last glacial period. Much of this variability seems to be linked with the dynamics of the Laurentide ice sheet that covered North America at this time3, which dis-charged iceberg flotillas into the North Atlantic that are now recorded in sediment cores as Heinrich events4. How (if at all) this variability was manifested on the other side of the Atlantic— in the Nordic seas and the ice sheets of northwest Europe and Scandinavia—has been unclear. Here we present sediment, micro-fossil and oxygen isotope data from a sediment core in the Norweg-ian sea, which reveal cooling events and iceberg discharges analogous to Heinrich events. We show that these climate fluctua-tions in the Norwegian Sea were in phase, or were phase-locked, with air temperatures over Greenland, suggesting that the rapid changes in heat fluxes in the North Atlantic recorded in previous records3 were felt in this high-latitude region. The iceberg dis-charges in our record seem to have come from the Fennoscandian ice sheet, implying that this and the Laurentide ice sheets fluctu-ated coherently on timescales shorter than those of Milankovitch orbital cycles.
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Fronval, T., Jansen, E., Bloemendal, J. et al. Oceanic evidence for coherent fluctuations in Fennoscandian and Laurentide ice sheets on millennium timescales. Nature 374, 443–446 (1995). https://doi.org/10.1038/374443a0
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DOI: https://doi.org/10.1038/374443a0
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