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.
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.
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)
Iowa State University, Ames, Iowa, USA
Julie Brigham-Grette
University of Massachusetts Amherst, Amherst,
Massachusetts, USA
Mea S. Cook
Williams College, Williamstown,
Massachusetts, USA
Elena Colmenero-Hidalgo
Universidad de León, León, Spain
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Cited
12 citations as recorded by crossref.
- Bering Sea surface water conditions during Marine Isotope Stages 12 to 10 at Navarin Canyon (IODP Site U1345) B. Caissie et al. https://doi.org/10.5194/cp-12-1739-2016
- Paleoceanography of the Bering Sea advanced by IODP Expedition 323: H. Asahi et al. https://doi.org/10.5575/geosoc.2017.0066
- Penultimate and last glacial oceanographic variations in the Bering Sea on millennial timescales: Links to North Atlantic climate E. Ovsepyan et al. https://doi.org/10.1016/j.quascirev.2017.03.012
- Authigenic greigite in late MIS 3 sediments: Implications for the Yellow Sea Cold Water Mass and Yellow Sea Warm Current evolution X. Zhang et al. https://doi.org/10.1016/j.margeo.2023.107057
- New evidence for a 179 ka age of the Old Crow tephra D. Yeo et al. https://doi.org/10.1016/j.quascirev.2026.109816
- Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene B. Pelto et al. https://doi.org/10.1002/2017PA003265
- Enhanced ocean deoxygenation in the Bering Sea during MIS 11c X. Feng et al. https://doi.org/10.1016/j.palaeo.2023.111982
- Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition S. Worne et al. https://doi.org/10.1016/j.quascirev.2021.106918
- Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum E. Cowan et al. https://doi.org/10.1038/s41467-020-15579-0
- Origins and paleoclimatic and paleoceanographic significance of laminated sediments of middle Pleistocene age from the southern Bering Sea J. Onodera et al. https://doi.org/10.1016/j.marmicro.2023.102323
- A diatom-based quantitative sea-ice proxy for the Bering and Chukchi seas A. Nesterovich & B. Caissie https://doi.org/10.1016/j.palaeo.2026.113686
- Effects of sea-level, sea-ice extent, and nutrient availability on primary production at the Umnak Plateau, Bering Sea (IODP Site U1339) during Marine Isotope Stage (MIS) 5 D. Vaughn & B. Caissie https://doi.org/10.1016/j.palaeo.2017.06.020
12 citations as recorded by crossref.
- Bering Sea surface water conditions during Marine Isotope Stages 12 to 10 at Navarin Canyon (IODP Site U1345) B. Caissie et al. https://doi.org/10.5194/cp-12-1739-2016
- Paleoceanography of the Bering Sea advanced by IODP Expedition 323: H. Asahi et al. https://doi.org/10.5575/geosoc.2017.0066
- Penultimate and last glacial oceanographic variations in the Bering Sea on millennial timescales: Links to North Atlantic climate E. Ovsepyan et al. https://doi.org/10.1016/j.quascirev.2017.03.012
- Authigenic greigite in late MIS 3 sediments: Implications for the Yellow Sea Cold Water Mass and Yellow Sea Warm Current evolution X. Zhang et al. https://doi.org/10.1016/j.margeo.2023.107057
- New evidence for a 179 ka age of the Old Crow tephra D. Yeo et al. https://doi.org/10.1016/j.quascirev.2026.109816
- Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene B. Pelto et al. https://doi.org/10.1002/2017PA003265
- Enhanced ocean deoxygenation in the Bering Sea during MIS 11c X. Feng et al. https://doi.org/10.1016/j.palaeo.2023.111982
- Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition S. Worne et al. https://doi.org/10.1016/j.quascirev.2021.106918
- Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum E. Cowan et al. https://doi.org/10.1038/s41467-020-15579-0
- Origins and paleoclimatic and paleoceanographic significance of laminated sediments of middle Pleistocene age from the southern Bering Sea J. Onodera et al. https://doi.org/10.1016/j.marmicro.2023.102323
- A diatom-based quantitative sea-ice proxy for the Bering and Chukchi seas A. Nesterovich & B. Caissie https://doi.org/10.1016/j.palaeo.2026.113686
- Effects of sea-level, sea-ice extent, and nutrient availability on primary production at the Umnak Plateau, Bering Sea (IODP Site U1339) during Marine Isotope Stage (MIS) 5 D. Vaughn & B. Caissie https://doi.org/10.1016/j.palaeo.2017.06.020
Saved (final revised paper)
Latest update: 09 Jun 2026
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...
