Paleontological Journal

, Volume 47, Issue 10, pp 1155–1162 | Cite as

Reflection of changes in sea surface circulation over the northeastern Iceland Basin in planktonic foraminiferal assemblages during the late Pleistocene-Holocene

  • L. D. BashirovaEmail author
  • N. P. Lukashina


Paleotemperature reconstructions based on foraminiferal analysis and estimates of the iceberg-rafted debris (IRD) obtained from sediment core AMK-4438 are provided. The sediments are dated 300 ka. It was shown that, during this period, sea surface conditions in the northeastern Iceland Basin varied considerably because of both glacial-interglacial alternation and short-term fluctuations of sea surface temperature due to ice melting during the Heinrich events.


planktonic foraminifers sea surface temperature Pleistocene Holocene Iceland Basin 


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Copyright information

© Pleiades Publishing, Ltd. 2013

Authors and Affiliations

  1. 1.Atlantic branch of the P.P., Shirshov Institute of OceanologyRussian Academy of SciencesKaliningradRussia
  2. 2.Immanuel Kant Baltic Federal UniversityKaliningradRussia

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