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ABSTRACT SUPPLIED BY ORIGINATOR: The Atlantic meridional overturning circulation (AMOC) is a critical element of Earth’s climate system and it is currently weakening. While this weakening is frequently explained by freshwater-driven disruptions to ocean convection, uncertainties about the impacts of prolonged freshening limit our capacity to predict its future state. For example, during the warm and unusually long marine isotope stage (MIS) 11 interglacial, ~424 to 374 ka, several lines of evidence suggest that a strong AMOC persisted concomitant with fresher-than-present conditions in the Nordic Seas, challenging our current understanding of convection. Here, we present new foraminifer-bound nitrogen isotope data along with multiple additional geochemical reconstructions of upper-ocean hydrography in the Nordic Seas during this anomalous interval. Our data suggest that a weak summer stratification was driven by the prolonged upper-ocean accumulation of freshwater beginning at the onset of the climatic optimum, ~410 to 407 ka, which could have helped precondition the region for convection. A box model constrained by paleo-proxy data additionally suggests that the density gradient between the subpolar North Atlantic and Nordic Seas was favorable for the onset of convection in the Nordic Seas during the climatic optimum. It is thus likely that the Nordic Seas became a locus of convection around this time. Enhanced northern-hemisphere heating driven by convection in the Nordic Seas may have been important for delaying glacial conditions, thereby driving the extended warming characteristic of MIS 11. Such findings may also be relevant for near-future changes under a relatively fresher high-latitude North Atlantic.</gco:CharacterString>
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