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...
Main Authors: | , , |
---|---|
Format: | Conference Object |
Language: | unknown |
Published: |
2014
|
Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/27631/ |