Isotope stratigraphy, sedimentation rates, deep circulation, and carbonate events in the Labrador Sea during the last ~ 200 ka
High-resolution stable-isotope and accelerator mass spectrometry 14C measurements in 25 box and piston cores from the Labrador Sea allow the reconstruction of major paleoceanographical changes during the last ~ 200 ka in this basin and also document the links between the interior of the Laurentide Ice Sheet and the North Atlantic Ocean during this interval. Two deep circulation regimes are indicated by contrasting sedimentation rates on the slopes: (i) the modern situation is characterized by a gyre of the North Atlantic Deep Water (NADW) components into the basin, which is responsible for the high-energy Western Boundary Undercurrent; this regime also prevailed during the former "true" interglacials and possibly during shorter "warm" intervals (e.g., Bolling-Allerod); (ii) a more frequent NADW-free situation during glacial and interstadial intervals is marked by the presence of a vertically homogeneous water mass in the basin. Sedimentological records also indicate that carbonate events (i.e., pulses of ...