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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 9
Clim. Past, 12, 1739–1763, 2016
https://doi.org/10.5194/cp-12-1739-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 1739–1763, 2016
https://doi.org/10.5194/cp-12-1739-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

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 et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by Editor) (27 May 2016) by Luc Beaufort
AR by Beth Caissie on behalf of the Authors (04 Jul 2016)  Author's response    Manuscript
ED: Publish subject to technical corrections (31 Jul 2016) by Luc Beaufort
AR by Beth Caissie on behalf of the Authors (11 Aug 2016)  Author's response    Manuscript
Publications Copernicus
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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.
This paper presents the first millennial-scale reconstruction of Marine Isotope Stage (MIS) 11...
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