Arctic Ocean meltwater outflow as a trigger for the Younger Dryas event – a review of available evidence from sediment cores

The Younger Dryas event at ca. 12.8-11.5 ka was a severe fall-back to quasi-glacial conditions during the last glacial termination in much of the northern hemisphere. For more than a decade since the late 1980s the widely accepted theory was that this event was triggered by a major meltwater ejectio...

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Bibliographic Details
Main Authors: Spielhagen, Robert F., Nørgaard-Pedersen, Niels, Telesinski, Maciej
Format: Conference Object
Language:unknown
Published: 2014
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/27631/