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.
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
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Cited
26 citations as recorded by crossref.
- 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. 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. 10.1016/j.margeo.2021.106492
- Causes and timing of recurring subarctic Pacific hypoxia K. Knudson et al. 10.1126/sciadv.abg2906
- Varves in marine sediments: A review A. Schimmelmann et al. 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. 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. 10.1016/j.gloplacha.2018.09.014
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- Enhanced North Pacific deep-ocean stratification by stronger intermediate water formation during Heinrich Stadial 1 X. Gong et al. 10.1038/s41467-019-08606-2
- Deglacial Land-Ocean Linkages at the Alaskan Continental Margin in the Bering Sea R. Wang et al. 10.3389/feart.2021.712415
- Origins and paleoclimatic and paleoceanographic significance of laminated sediments of middle Pleistocene age from the southern Bering Sea J. Onodera et al. 10.1016/j.marmicro.2023.102323
- 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. 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. 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. 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 10.1002/ecs2.2868
- North Pacific deglacial hypoxic events linked to abrupt ocean warming S. Praetorius et al. 10.1038/nature15753
- 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 10.1016/j.earscirev.2024.104782
- 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. 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. 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. 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. 10.1016/j.quascirev.2017.01.016
- Intermediate- and Deep-Water Oxygenation History in the Subarctic North Pacific During the Last Deglacial Period E. Ovsepyan et al. 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. 10.1016/j.quascirev.2020.106519
- Enhanced ocean deoxygenation in the Bering Sea during MIS 11c X. Feng et al. 10.1016/j.palaeo.2023.111982
- Modern modes of provenance and dispersal of terrigenous sediments in the North Pacific and Bering Sea: implications and perspectives for palaeoenvironmental reconstructions R. Wang et al. 10.1007/s00367-016-0445-7
- Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene B. Pelto et al. 10.1002/2017PA003265
24 citations as recorded by crossref.
- 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. 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. 10.1016/j.margeo.2021.106492
- Causes and timing of recurring subarctic Pacific hypoxia K. Knudson et al. 10.1126/sciadv.abg2906
- Varves in marine sediments: A review A. Schimmelmann et al. 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. 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. 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. 10.5194/cp-13-359-2017
- Widespread tephra layers in the Bering Sea sediments: distal clues to large explosive eruptions from the Aleutian volcanic arc A. Derkachev et al. 10.1007/s00445-018-1254-9
- Enhanced North Pacific deep-ocean stratification by stronger intermediate water formation during Heinrich Stadial 1 X. Gong et al. 10.1038/s41467-019-08606-2
- Deglacial Land-Ocean Linkages at the Alaskan Continental Margin in the Bering Sea R. Wang et al. 10.3389/feart.2021.712415
- Origins and paleoclimatic and paleoceanographic significance of laminated sediments of middle Pleistocene age from the southern Bering Sea J. Onodera et al. 10.1016/j.marmicro.2023.102323
- 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. 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. 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. 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 10.1002/ecs2.2868
- North Pacific deglacial hypoxic events linked to abrupt ocean warming S. Praetorius et al. 10.1038/nature15753
- 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 10.1016/j.earscirev.2024.104782
- 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. 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. 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. 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. 10.1016/j.quascirev.2017.01.016
- Intermediate- and Deep-Water Oxygenation History in the Subarctic North Pacific During the Last Deglacial Period E. Ovsepyan et al. 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. 10.1016/j.quascirev.2020.106519
- Enhanced ocean deoxygenation in the Bering Sea during MIS 11c X. Feng et al. 10.1016/j.palaeo.2023.111982
2 citations as recorded by crossref.
- Modern modes of provenance and dispersal of terrigenous sediments in the North Pacific and Bering Sea: implications and perspectives for palaeoenvironmental reconstructions R. Wang et al. 10.1007/s00367-016-0445-7
- Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene B. Pelto et al. 10.1002/2017PA003265
Saved (final revised paper)
Saved (final revised paper)
Latest update: 13 Dec 2024
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...