The abrupt ending of the Younger Dryas cooling episode marked the onset of the present interglacial and was the most prominent climate change in the Earth’s recent history. This study shows evidence for a sequence of events with a leading role of the ocean at the transition into the present day warm Holocene epoch.
- Christof Pearce
- Marit-Solveig Seidenkrantz
- Søren M. Kristiansen
