Articles | Volume 10, issue 6
https://doi.org/10.5194/cp-10-2215-2014
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, L. Lembke-Jene, R. Gersonde, O. Esper, F. Lamy, H. Arz, G. Kuhn, and R. Tiedemann

Viewed

Total article views: 5,794 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,612 2,361 821 5,794 183 175
  • HTML: 2,612
  • PDF: 2,361
  • XML: 821
  • Total: 5,794
  • BibTeX: 183
  • EndNote: 175
Views and downloads (calculated since 06 Jun 2014)
Cumulative views and downloads (calculated since 06 Jun 2014)

Cited

Saved (final revised paper)

Saved (final revised paper)

Latest update: 21 Nov 2024
Download
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.