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Oceanology

, Volume 53, Issue 2, pp 211–222 | Cite as

Late quaternary oceanographic conditions in the Western Bering Sea

  • E. A. Ovsepyan
  • E. V. Ivanova
  • L. Max
  • J. -R. Riethdorf
  • D. Nürnberg
  • R. Tiedemann
Marine Geology

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.

Keywords

Holocene Bottom Water Last Glacial Maximum Marine Isotopic Stage Benthic Foraminifer 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Pleiades Publishing, Ltd. 2013

Authors and Affiliations

  • E. A. Ovsepyan
    • 1
  • E. V. Ivanova
    • 1
  • L. Max
    • 2
  • J. -R. Riethdorf
    • 3
  • D. Nürnberg
    • 3
  • R. Tiedemann
    • 2
  1. 1.Shirshov Institute of OceanologyRussian Academy of SciencesMoscowRussia
  2. 2.Alfred Wegener Institute for Polar and Marine ResearchBremerhavenGermany
  3. 3.GEOMAR Helmholtz Centre for Ocean Research (Kiel)KielGermany

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