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Late quaternary oceanographic conditions in the Western Bering Sea

  • Marine Geology
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Oceanology Aims and scope

Abstract

The benthic and planktonic foraminiferal assemblages and the distribution of coarse grain-size factions were studied in the upper 4.5 m of the Core SO201-2-85KL (57°30.30′ N, 170°24.79′ E, water depth 968 m) retrieved from the Shirshov Ridge. This part of the core covers 7.5 to 50 kyr BP. The glacial period is established to be characterized by low surface water productivity, the wide distribution of sea ice and/or icebergs in this area, and a high oxygen concentration in the bottom layer. Enhanced productivity is inferred from the maximum abundance of planktonic foraminifers at the very beginning of the deglaciation. The late Bølling-Allerød interstadial and the early Holocene were marked by the further two-phase increase in the surface productivity and the weakened ventilation of the bottom water.

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Authors and Affiliations

  1. Shirshov Institute of Oceanology, Russian Academy of Sciences, pr. Nakhimovskii 36, Moscow, 117997, Russia

    E. A. Ovsepyan & E. V. Ivanova

  2. Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany

    L. Max & R. Tiedemann

  3. GEOMAR Helmholtz Centre for Ocean Research (Kiel), Kiel, Germany

    J. -R. Riethdorf & D. Nürnberg

Authors
  1. E. A. Ovsepyan
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  2. E. V. Ivanova
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  3. L. Max
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  4. J. -R. Riethdorf
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  5. D. Nürnberg
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  6. R. Tiedemann
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Correspondence to E. A. Ovsepyan.

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Original Russian Text © E.A. Ovsepyan, E.V. Ivanova, L. Max, J.-R. Riethdorf, D. Nürnberg, R. Tiedemann, 2013, published in Okeanologiya, 2013, Vol. 53, No. 2, pp. 237–248.

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Ovsepyan, E.A., Ivanova, E.V., Max, L. et al. Late quaternary oceanographic conditions in the Western Bering Sea. Oceanology 53, 211–222 (2013). https://doi.org/10.1134/S0001437013020136

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  • DOI: https://doi.org/10.1134/S0001437013020136

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