Articles | Volume 10, issue 6
Clim. Past, 10, 2215–2236, 2014
https://doi.org/10.5194/cp-10-2215-2014
Clim. Past, 10, 2215–2236, 2014
https://doi.org/10.5194/cp-10-2215-2014

Research article 16 Dec 2014

Research article | 16 Dec 2014

Laminated sediments in the Bering Sea reveal atmospheric teleconnections to Greenland climate on millennial to decadal timescales during the last deglaciation

H. Kuehn et al.

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Short summary
Annually laminated sediments from the NE Bering Sea reveal a decadal-scale correlation to Greenland ice core records during termination I, suggesting an atmospheric teleconnection. Lamination occurrence is tightly coupled to Bølling-Allerød and Preboreal warm phases. Increases in export production, closely coupled to SST and sea ice changes, are hypothesized to be a main cause of deglacial anoxia, rather than changes in overturning/ventilation rates of mid-depth waters entering the Bering Sea.