Articles | Volume 10, issue 6
https://doi.org/10.5194/cp-10-2215-2014
© Author(s) 2014. 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-10-2215-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
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
CORRESPONDING AUTHOR
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
MARUM Zentrum für Marine Umweltwissenschaften, Bremen, Germany
L. Lembke-Jene
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
R. Gersonde
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
MARUM Zentrum für Marine Umweltwissenschaften, Bremen, Germany
O. Esper
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
MARUM Zentrum für Marine Umweltwissenschaften, Bremen, Germany
F. Lamy
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
MARUM Zentrum für Marine Umweltwissenschaften, Bremen, Germany
H. Arz
IOW – Leibniz Institut für Ostseeforschung, Warnemünde, Germany
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
R. Tiedemann
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Viewed
Total article views: 6,792 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 06 Jun 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 3,254 | 2,669 | 869 | 6,792 | 270 | 276 |
- HTML: 3,254
- PDF: 2,669
- XML: 869
- Total: 6,792
- BibTeX: 270
- EndNote: 276
Total article views: 5,212 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 16 Dec 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 2,543 | 1,832 | 837 | 5,212 | 259 | 270 |
- HTML: 2,543
- PDF: 1,832
- XML: 837
- Total: 5,212
- BibTeX: 259
- EndNote: 270
Total article views: 1,580 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 06 Jun 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 711 | 837 | 32 | 1,580 | 11 | 6 |
- HTML: 711
- PDF: 837
- XML: 32
- Total: 1,580
- BibTeX: 11
- EndNote: 6
Cited
26 citations as recorded by crossref.
- Causes and timing of recurring subarctic Pacific hypoxia K. Knudson et al. https://doi.org/10.1126/sciadv.abg2906
- 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
- Reviews and syntheses: Review of proxies for low-oxygen paleoceanographic reconstructions B. Hoogakker et al. https://doi.org/10.5194/bg-22-863-2025
- Widespread tephra layers in the Bering Sea sediments: distal clues to large explosive eruptions from the Aleutian volcanic arc A. Derkachev et al. https://doi.org/10.1007/s00445-018-1254-9
- Deglacial Land-Ocean Linkages at the Alaskan Continental Margin in the Bering Sea R. Wang et al. https://doi.org/10.3389/feart.2021.712415
- Glacial-to-Holocene evolution of sea surface temperature and surface circulation in the subarctic northwest Pacific and the Western Bering Sea V. Meyer et al. https://doi.org/10.1002/2015PA002877
- Cyclicity related to solar activity in lacustrine organic-rich shales and their significance to shale-oil reservoir formation M. Lin et al. https://doi.org/10.1016/j.gsf.2023.101586
- Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming V. Meyer et al. https://doi.org/10.1088/1748-9326/ab2653
- Diatom responses to long‐term climate and sea‐level rise at a low‐elevation lake in coastal British Columbia, Canada K. Neil & T. Lacourse https://doi.org/10.1002/ecs2.2868
- The Northeast Pacific Ocean and Northwest Coast of North America within the global climate system, 29,000 to 11,700 years ago D. Mann & B. Gaglioti https://doi.org/10.1016/j.earscirev.2024.104782
- Intermediate- and Deep-Water Oxygenation History in the Subarctic North Pacific During the Last Deglacial Period E. Ovsepyan et al. https://doi.org/10.3389/feart.2021.638069
- Sea surface temperature across the Subarctic North Pacific and marginal seas through the past 20,000 years: A paleoceanographic synthesis C. Davis et al. https://doi.org/10.1016/j.quascirev.2020.106519
- Enhanced ocean deoxygenation in the Bering Sea during MIS 11c X. Feng et al. https://doi.org/10.1016/j.palaeo.2023.111982
- Late quaternary sea-ice and sedimentary redox conditions in the eastern Bering Sea – Implications for ventilation of the mid-depth North Pacific and an Atlantic-Pacific seesaw mechanism H. Detlef et al. https://doi.org/10.1016/j.quascirev.2020.106549
- Changes in sediment provenance and ocean circulation on the northern slope of the Bering Sea since the last deglaciation Y. Sun et al. https://doi.org/10.1016/j.margeo.2021.106492
- Varves in marine sediments: A review A. Schimmelmann et al. https://doi.org/10.1016/j.earscirev.2016.04.009
- Alternating Influence of Northern Versus Southern‐Sourced Water Masses on the Equatorial Pacific Subthermocline During the Past 240 ka N. Rippert et al. https://doi.org/10.1002/2017PA003133
- Evidence of meltwater pulses into the North Pacific over the last 20 ka due to the decay of Kamchatka Glaciers and Cordilleran Ice Sheet S. Gorbarenko et al. https://doi.org/10.1016/j.gloplacha.2018.09.014
- Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20 000 years V. Meyer et al. https://doi.org/10.5194/cp-13-359-2017
- Enhanced North Pacific deep-ocean stratification by stronger intermediate water formation during Heinrich Stadial 1 X. Gong et al. https://doi.org/10.1038/s41467-019-08606-2
- 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
- North Pacific deglacial hypoxic events linked to abrupt ocean warming S. Praetorius et al. https://doi.org/10.1038/nature15753
- Sea-ice variability in the subarctic North Pacific and adjacent Bering Sea during the past 25 ka: new insights from IP25 and Uk′37 proxy records M. Méheust et al. https://doi.org/10.1007/s41063-018-0043-1
- Deglacial records of terrigenous organic matter accumulation off the Yukon and Amur rivers based on lignin phenols and long-chain n-alkanes M. Cao et al. https://doi.org/10.5194/cp-19-159-2023
- Lacustrine leaf wax hydrogen isotopes indicate strong regional climate feedbacks in Beringia since the last ice age W. Daniels et al. https://doi.org/10.1016/j.quascirev.2021.107130
- Deglacial variability in Okhotsk Sea Intermediate Water ventilation and biogeochemistry: Implications for North Pacific nutrient supply and productivity L. Lembke-Jene et al. https://doi.org/10.1016/j.quascirev.2017.01.016
26 citations as recorded by crossref.
- Causes and timing of recurring subarctic Pacific hypoxia K. Knudson et al. https://doi.org/10.1126/sciadv.abg2906
- 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
- Reviews and syntheses: Review of proxies for low-oxygen paleoceanographic reconstructions B. Hoogakker et al. https://doi.org/10.5194/bg-22-863-2025
- Widespread tephra layers in the Bering Sea sediments: distal clues to large explosive eruptions from the Aleutian volcanic arc A. Derkachev et al. https://doi.org/10.1007/s00445-018-1254-9
- Deglacial Land-Ocean Linkages at the Alaskan Continental Margin in the Bering Sea R. Wang et al. https://doi.org/10.3389/feart.2021.712415
- Glacial-to-Holocene evolution of sea surface temperature and surface circulation in the subarctic northwest Pacific and the Western Bering Sea V. Meyer et al. https://doi.org/10.1002/2015PA002877
- Cyclicity related to solar activity in lacustrine organic-rich shales and their significance to shale-oil reservoir formation M. Lin et al. https://doi.org/10.1016/j.gsf.2023.101586
- Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming V. Meyer et al. https://doi.org/10.1088/1748-9326/ab2653
- Diatom responses to long‐term climate and sea‐level rise at a low‐elevation lake in coastal British Columbia, Canada K. Neil & T. Lacourse https://doi.org/10.1002/ecs2.2868
- The Northeast Pacific Ocean and Northwest Coast of North America within the global climate system, 29,000 to 11,700 years ago D. Mann & B. Gaglioti https://doi.org/10.1016/j.earscirev.2024.104782
- Intermediate- and Deep-Water Oxygenation History in the Subarctic North Pacific During the Last Deglacial Period E. Ovsepyan et al. https://doi.org/10.3389/feart.2021.638069
- Sea surface temperature across the Subarctic North Pacific and marginal seas through the past 20,000 years: A paleoceanographic synthesis C. Davis et al. https://doi.org/10.1016/j.quascirev.2020.106519
- Enhanced ocean deoxygenation in the Bering Sea during MIS 11c X. Feng et al. https://doi.org/10.1016/j.palaeo.2023.111982
- Late quaternary sea-ice and sedimentary redox conditions in the eastern Bering Sea – Implications for ventilation of the mid-depth North Pacific and an Atlantic-Pacific seesaw mechanism H. Detlef et al. https://doi.org/10.1016/j.quascirev.2020.106549
- Changes in sediment provenance and ocean circulation on the northern slope of the Bering Sea since the last deglaciation Y. Sun et al. https://doi.org/10.1016/j.margeo.2021.106492
- Varves in marine sediments: A review A. Schimmelmann et al. https://doi.org/10.1016/j.earscirev.2016.04.009
- Alternating Influence of Northern Versus Southern‐Sourced Water Masses on the Equatorial Pacific Subthermocline During the Past 240 ka N. Rippert et al. https://doi.org/10.1002/2017PA003133
- Evidence of meltwater pulses into the North Pacific over the last 20 ka due to the decay of Kamchatka Glaciers and Cordilleran Ice Sheet S. Gorbarenko et al. https://doi.org/10.1016/j.gloplacha.2018.09.014
- Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20 000 years V. Meyer et al. https://doi.org/10.5194/cp-13-359-2017
- Enhanced North Pacific deep-ocean stratification by stronger intermediate water formation during Heinrich Stadial 1 X. Gong et al. https://doi.org/10.1038/s41467-019-08606-2
- 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
- North Pacific deglacial hypoxic events linked to abrupt ocean warming S. Praetorius et al. https://doi.org/10.1038/nature15753
- Sea-ice variability in the subarctic North Pacific and adjacent Bering Sea during the past 25 ka: new insights from IP25 and Uk′37 proxy records M. Méheust et al. https://doi.org/10.1007/s41063-018-0043-1
- Deglacial records of terrigenous organic matter accumulation off the Yukon and Amur rivers based on lignin phenols and long-chain n-alkanes M. Cao et al. https://doi.org/10.5194/cp-19-159-2023
- Lacustrine leaf wax hydrogen isotopes indicate strong regional climate feedbacks in Beringia since the last ice age W. Daniels et al. https://doi.org/10.1016/j.quascirev.2021.107130
- Deglacial variability in Okhotsk Sea Intermediate Water ventilation and biogeochemistry: Implications for North Pacific nutrient supply and productivity L. Lembke-Jene et al. https://doi.org/10.1016/j.quascirev.2017.01.016
Saved (final revised paper)
Latest update: 16 Jun 2026
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.
Annually laminated sediments from the NE Bering Sea reveal a decadal-scale correlation to...
