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Rapid reductions in North Atlantic Deep Water during the peak of the last int...
Deep ocean circulation has been considered relatively stable during interglacial periods, yet little is known about its behavior on submillennial time scales. Using a... -
Sedimentological and geochemical records of the North Atlantic Glacial Easter...
The upper branch of the Atlantic Meridional Overturning Circulation (AMOC) plays a critical role in ocean circulation and climate change, yet its variability during the last... -
Interglacial instability of North Atlantic Deep Water ventilation
Disrupting North Atlantic Deep Water (NADW) ventilation is a key concern in climate projections. We use (sub)centennially resolved bottom water d13C records that span the...