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Science 30 June 2006:
Vol. 312. no. 5782, pp. 1929 - 1932
DOI: 10.1126/science.1127213

Reports

Surface and Deep Ocean Interactions During the Cold Climate Event 8200 Years Ago

Christopher R. W. Ellison,1 Mark R. Chapman,1* Ian R. Hall2*

Evidence from a North Atlantic deep-sea sediment core reveals that the largest climatic perturbation in our present interglacial, the 8200-year event, is marked by two distinct cooling events in the subpolar North Atlantic at 8490 and 8290 years ago. An associated reduction in deep flow speed provides evidence of a significant change to a major downwelling limb of the Atlantic meridional overturning circulation. The existence of a distinct surface freshening signal during these events strongly suggests that the sequenced surface and deep ocean changes were forced by pulsed meltwater outbursts from a multistep final drainage of the proglacial lakes associated with the decaying Laurentide Ice Sheet margin.

1 School of Environmental Sciences, University of East Anglia (UEA), Norwich, NR4 7TJ, UK.
2 School of Earth, Ocean, and Planetary Sciences, Cardiff University, Main Building, Park Place, Cardiff, CF10 3YE, UK.

* To whom correspondence should be addressed. E-mail: Mark.Chapman{at}uea.ac.uk (M.R.C.); Hall{at}cardiff.ac.uk (I.R.H.)

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