The stability of the ice margin in Baffin Bay led to active decentering of sediments in the deep basin and slopes 25,000−15,000 years ago, but as the ice sheet retreated 13,000-11,000 years ago, deposition moved largely toward the shelf, according to radiocarbon records from 79 sediment cores.
- Emmanuel Okuma
- Jürgen Titschack
- Dierk Hebbeln
