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

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Cited articles

Addison, J. A., Finney, B. P., Dean, W. E., Davies, M. H., Mix, A. C., Stoner, J. S., and Jaeger, J. M.: Productivity and sedimentary δ15N variability for the last 17 000 years along the northern Gulf of Alaska continental slope, Paleoceanography, 27, PA1206, https://doi.org/10.1029/2011PA002161, 2012.
Ahagon, N., Ohkushi, K., Uchida, M., and Mishima, T.: Mid-depth circulation in the northwest Pacific during the last deglaciation: Evidence from foraminiferal radiocarbon ages, Geophys. Res. Lett., 30, 2097, https://doi.org/10.1029/2003GL018287, 2003.
Andersen, K. K., Svensson, A., Johnsen, S. J., Rasmussen, S. O., Bigler, M., Röthlisberger, R., Ruth, U., Siggaard-Andersen, M.-L., Steffensen, J. P., Dahl-Jensen, D., Vinther, B. M., and Clausen, H. B.: The Greenland Ice Core Chronology 2005, 15–42 ka – Part 1: constructing the time scale, Quaternary Sci. Rev., 25, 3246–3257, 2006.
Bauch, D., Erlenkeuser, H., Winckler, G., Pavlova, G., and Thiede, J.: Carbon isotopes and habitat of polar planktic foraminifera in the Okhotsk Sea: the "carbonate ion effect" under natural conditions, Mar. Micropaleontol., 45, 83–99, 2002.
Behl, R. J. and Kennett, J. P.: Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr, Nature, 379, 243–246, 1996.
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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.