“…Heinrich events (Heinrich, 1988) are inferred from widespread and distinctive sediment layers that contain an iceberg rafted coarse component. However, in the Labrador Sea the layers are dominated by fine-grained detrital carbonate sediments (Chough, 1978;Kirby, 1996) that appear to record large meltwater or turbidite flows emanating from Hudson Strait (Hesse et al, 1997;Hesse and Khodabakhsh, 1998). Sudden iceberg and meltwater release could have accompanied either a surge or a breakup of the Hudson Strait Ice Stream (cf.…”