Stable isotope record during the past 1 Myr of ODP Site 162-980 in the subpolar North Atlantic

During glacial intervals, significant increases in intermediate-to-deep delta13C gradients (commonly reaching >1.2 per mil ) are consistent with changes in deep water circulation and associated chemical stratification.

Bathymetric delta13C gradients covary with benthic foraminiferal delta18O and covary inversely with Vostok CO2, in agreement with chemical stratification as a driver of atmospheric CO2 changes. Three deep circulation indices based on delta13C show a phasing similar to North Atlantic sea surface temperatures, consistent with a Northern Hemisphere control of NADW/SOW variations. However, lags in the precession band indicate that factors other than deep water circulation control ice volume variations at least in this band.