Climate of the Past
Climate of the Past
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Articles | Volume 12, issue 9
Articles | Volume 12, issue 9
https://doi.org/10.5194/cp-12-1739-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1739-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 12, issue 9
Research article
 | 
01 Sep 2016
Research article |  | 01 Sep 2016

Bering Sea surface water conditions during Marine Isotope Stages 12 to 10 at Navarin Canyon (IODP Site U1345)

Beth E. Caissie, Julie Brigham-Grette, Mea S. Cook, and Elena Colmenero-Hidalgo

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Short summary
This paper presents the first millennial-scale reconstruction of Marine Isotope Stage (MIS) 11 (~400 ka) from the subarctic Pacific Ocean. We use diatoms, calcareous nannofossils, grain size, and carbon and nitrogen isotopes to examine changing productivity and sea ice. These change in sync with other regional and global records. Initially, MIS 11 is highly productive, due to increased upwelling. Sea ice declines gradually during this warm period, but is present throughout.
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