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Repeated Pleistocene glaciation of the East Siberian continental margin

Nature Geoscience volume 6, pages 842–846 (2013)Cite this article

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Abstract

During the Pleistocene glaciations, Arctic ice sheets on western Eurasia, Greenland and North America terminated at their continental margins1,2,3,4. In contrast, the exposed continental shelves in the Beringian region of Siberia are thought to have been covered by a tundra landscape5,6,7. Evidence of grounded ice on seafloor ridges and plateaux off the coast of the Beringian margin, at depths of up to 1,000 m, have generally been attributed to ice shelves or giant icebergs that spread oceanwards during glacial maxima8,9,10,11,12. Here we identify marine glaciogenic landforms visible in seismic profiles and detailed bathymetric maps along the East Siberian continental margin. We interpret these features, which occur in present water depths of up to 1,200 m, as traces from grounding events of ice sheets and ice shelves. We conclude that the Siberian Shelf edge and parts of the Arctic Ocean were covered by ice sheets of about 1 km in thickness during several Pleistocene glaciations before the most recent glacial period, which must have had a significant influence on albedo and oceanic and atmospheric circulation.

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Figure 1: Proposed maximum extent of an ice sheet on the East Siberian continental margin (ESCM), Pleistocene ice sheets in the Arctic and area of investigation.
Figure 2: Evidence of grounded ice and glacial sedimentation on the Arlis Plateau (Fig. 1).
Figure 3: Glaciogenic fans and SGL on the East Siberian continental slope.
Figure 4: Glaciogenic facies and moraines on the East Siberian continental slope.

References

  1. Ehlers, J. & Gibbard, P. L. The extent and chronology of Cenozoicglobal glaciation. Quat. Internat. 164–165, 6–20 (2007).

    Article  Google Scholar 

  2. Svendsen, J. I. et al. Late Quaternary ice sheet history of Northern Eurasia. Quat. Sci. Rev. 23, 1229–1272 (2004).

    Article  Google Scholar 

  3. England, J. H., Furze, M. F. A. & Doupé, J. P. Revision of the NW Laurentide Ice Sheet: implications for paleoclimate, the northeast extremity of Beringia, and Arctic Ocean sedimentation. Quat. Sci. Rev. 28, 1573–1596 (2009).

    Article  Google Scholar 

  4. Batchelor, C. L., Dowdeswell, J. A. & Pietras, J. T. Variable history of Quaternary ice-sheet advance across the Beaufort Sea margin, Arctic Ocean. Geology 41, 131–134 (2013).

    Article  Google Scholar 

  5. Alekseev, M. N. Paleogeography and geochronology in the Russian Eastern Arctic during the second half of the Quaternary. Quat. Intern. 41/42, 11–15 (1997).

    Article  Google Scholar 

  6. Gualtieri, L., Vartanyan, S. L., Brigham-Grette, J. & Anderson, P. M. Evidence for an ice-free Wrangel Island, northeast Siberia during the Last Glacial Maximum. Boreas 34, 264–273 (2005).

    Article  Google Scholar 

  7. Brigham-Grette, J. & Gualtieri, L. Letter to the Editor. Quat. Sci. Rev. 62, 227–232 (2004).

    Google Scholar 

  8. Polyak, L., Edwards, M. H., Coakley, B. J. & Jakobsson, M. Ice shelves in the Pleistocene Arctic Ocean inferred from glaciogenic deep-sea bedforms. Nature 410, 453–459 (2001).

    Article  Google Scholar 

  9. Polyak, L. V., Darby, D. A., Bischoff, J. F. & Jakobsson, M. Stratigraphic constraints on late Pleistocene glacial erosion and deglaciation of the Chukchi margin, Arctic Ocean. Quat. Res. 67, 234–245 (2007).

    Article  Google Scholar 

  10. Jakobsson, M. et al. Glacial geomorphology of the Central Arctic Ocean: The Chukchi Borderland and the Lomonosov Ridge. Earth Surf. Proc. Landf. 33, 526–545 (2008).

    Article  Google Scholar 

  11. Jakobsson, M. et al. An Arctic Ocean ice shelf during MIS 6 constrained by new geophysical and geological data. Quat. Sci. Rev. 29, 3505–3517 (2010).

    Article  Google Scholar 

  12. Kristoffersen, Y. et al. Seabed erosion on the Lomonosov Ridge, central Arctic Ocean: A tale of deep draft icebergs in the Eurasia Basin and the influence of Atlantic water inflow on iceberg motion? Paleoceanography 19, PA3006 (2004).

    Article  Google Scholar 

  13. Stauch, G. & Gualtieri, L. Late Quaternary glaciations in northeastern Russia. J. Quat. Sci. 23, 545–558 (2008).

    Article  Google Scholar 

  14. Glushkova, O. Yu. Late Pleistocene Glaciations in North-East Asia. Dev. Quat. Sci. 15, 865–875 (2011).

    Google Scholar 

  15. Hu, A. et al. Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes. Nature Geosci. 3, 118–121 (2010).

    Article  Google Scholar 

  16. Rohling, E. J. et al. Antarctic temperature and global sea level closely coupled over the past five glacial cycles. Nature Geosci. 557, 500–504 (2009).

    Article  Google Scholar 

  17. Stein, R. et al. Towards a better (litho-) stratigraphy and reconstruction of quaternary paleoenvironment in the Amerasian Basin (Arctic Ocean). Polarforschung 79, 97–121 (2010).

    Google Scholar 

  18. Dowdeswell, J. A., Ottesen, D., Rise, L. & Craig, J. Identification and preservation of landforms diagnostic of past ice-sheet activity on continental shelves from three-dimensional seismic evidence. Geology 35, 359–362 (2007).

    Article  Google Scholar 

  19. Davies, T. A. et al. (eds) Glaciated Continental Margins. An Atlas of Acoustic Images (Chapman/Hall, 1997).

  20. Dowdeswell, J. A. et al. Submarine glacial landforms and rates of ice-stream collapse. Geology 36, 819–822 (2008).

    Article  Google Scholar 

  21. Hegewald, A. & Jokat, W. Relative sea level variations in the Chukchi region - Arctic Ocean - since the late Eocene. Geophys. Res. Lett. 40, 803–807 (2013).

    Article  Google Scholar 

  22. Tulaczyk, S., Kamp, W. B. & Engelhardt, H. F. Basal mechanics of Ice Stream B, West Antarctica. 1. Till mechanics. J. Geophis. Res. 105, 463–481 (2000).

    Article  Google Scholar 

  23. Lindén, M. & Möller, P. Marginal formation of De Geer moraines and their implications to the dynamics of grounding-line recession. J. Quat. Sci. 20, 113–133 (2005).

    Article  Google Scholar 

  24. O’Regan, M. et al. Constraints on the Pleistocene chronology of sediments from the Lomonosov Ridge. Paleoceanography 23, PA1S19 (2008).

    Google Scholar 

  25. Grosswald, M. G. & Hughes, T. J. The Russian component of an Arctic Ice Sheet during the Last Glacial Maximum. Quat. Sci. Rev. 21, 121–146 (2002).

    Article  Google Scholar 

  26. Greve, R., Wyrwoll, K-H. & Eisenhauer, A. Deglaciation of the Northern Hemisphere at the onset of the Eemian and Holocene. Ann. Glaciol. 28, 1–8 (1999).

    Article  Google Scholar 

  27. Basilian, A. C., Nikol’skyi, P. A. & Anisimov, M. A. Pleistocene glaciation of the New Siberian Islands - no more doubt. IPY News 12, 7–9 (2008) AARI.

    Google Scholar 

  28. Polyak, L. & Jakobsson, M. Quaternary sedimentation in the Arctic Ocean: Recent advances and further challenges. Oceanography 24, 52–64 (2011).

    Article  Google Scholar 

  29. Peltier, W. R. Rapid climate change and Arctic Ocean freshening. Geology 35, 1147–1148 (2007).

    Article  Google Scholar 

Download references

Acknowledgements

We are grateful for the support of the captains and crews of the RV Polarstern and RV Araon during the cruises ARK-XXIII/3 and ARA03B, respectively. We thank S. Hanisch, O. Thomas and J. Collins for improvement of text and figures. This publication is a contribution to the research programme PACES, topic 3 (Lessons from the Past) of the Alfred Wegener Institute, Helmholtz Centre for Polar und Marine Research (AWI) and the projects K-PORT (PM11080) and K-Polar (PP13030) of the Korea Polar Research Institute (KOPRI). This research was financially supported by AWI, KOPRI and MOF of Korea.

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Authors and Affiliations

  1. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI), Am Alten Hafen 26, 27568 Bremerhaven, Germany

    Frank Niessen, Anne Hegewald, Jens Matthiessen, Rüdiger Stein, Laura Jensen & Wilfried Jokat

  2. Korea Polar Research Institute (KOPRI), 26 Songdomirae-ro, Yeonsoo-gu, Incheon 406-840, Republic of Korea

    Jong Kuk Hong, Hyoungjun Kim, Sookwan Kim, Seung-Il Nam & Sung-Ho Kang

  3. University of Science and Technology, 217 Gajung-ro, Yuseong-gu, Daejeon, Republic of Korea

    Sookwan Kim

Authors
  1. Frank Niessen
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  2. Jong Kuk Hong
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  3. Anne Hegewald
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  4. Jens Matthiessen
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  8. Laura Jensen
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  9. Wilfried Jokat
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  10. Seung-Il Nam
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  11. Sung-Ho Kang
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Contributions

F.N. participated in both expeditions in 2008 and 2012, interpreted the hydro-acoustic data and wrote the first draft of the manuscript. J.K.H. led the bathymetric survey on RV Araon, A.H. processed and plotted the seismic multichannel data. H.K. acquired and processed multibeam data on RV Araon, S.K. compiled bathymetric data of KOPRI and conducted image processing. L.J. acquired and processed multibeam data on RV Polarstern and carried out image processing. J.M. contributed to Parasound data acquisition on RV Polarstern, R.S. and W.J. led the geological and geophysical data acquisition, respectively, on RV Polarstern and S-I.N. led the geological data acquisition on RV Araon. All authors contributed to writing the paper and analysing the results. S-H.K. led the K-PORT project and contributed to the geophysical survey on RV Araon.

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Correspondence to Frank Niessen or Jong Kuk Hong.

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Niessen, F., Hong, J., Hegewald, A. et al. Repeated Pleistocene glaciation of the East Siberian continental margin. Nature Geosci 6, 842–846 (2013). https://doi.org/10.1038/ngeo1904

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