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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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Cited articles  
Aizawa, C., Tanimoto, M., and Jordan, R. W.: Living diatom assemblages from North Pacific and Bering Sea surface waters during summer 1999, Deep-Sea Res. Pt. I, 52, 2186–2205, 2005.
Alexander, V. and Chapman, T.: The role of epontic algal communities in Bering Sea ice, in: The Eastern Bering Sea Shelf: Oceanography and Resources, edited by: Hood, D. W. and Calder, J. A., University of Washington Press, Seattle, Washington, 1981.
Asahi, H., Kender, S., Ikehara, M., Sakamoto, T., Takahashi, K., Ravelo, A. C., Alvarez Zarikian, C. A., Khim, B. K., and Leng, M. J.: Orbital-scale benthic foraminiferal oxygen isotope stratigraphy at the northern Bering Sea Slope Site U1343 (IODP Expedition 323) and its Pleistocene paleoceanographic significance, Deep-Sea Res. Pt. II, 125/126, 66–83, 2016.
Barr, I. D. and Clark, C. D.: Distribution and pattern of moraines in Far NE Russia reveal former glacial extent, Journal of Maps, 5, 186–193, 2009.
Barron, J. A., Bukry, D., Dean, W. E., Addison, J. A., and Finney, B.: Paleoceanography of the Gulf of Alaska during the past 15,000 years: results from diatoms, silicoflagellates, and geochemistry, Mar. Micropaleontol., 72, 176–195, 2009.
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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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