A shift in heavy and clay mineral provenance indicates a middle Miocene onset of a perennial sea ice cover in the Arctic Ocean

Author:

Krylov Alexey A.12,Andreeva Irina A.1,Vogt Christoph3,Backman Jan4,Krupskaya Viktoria V.5,Grikurov Garrik E.1,Moran Kathryn6,Shoji Hitoshi2

Affiliation:

1. VNIIOkeangeologia; St. Petersburg Russia

2. Kitami Institute of Technology; Kitami Japan

3. Department of Geosciences; University of Bremen; Bremen Germany

4. Department of Geology and Geochemistry; Stockholm University; Stockholm Sweden

5. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry; Russian Academy of Science; Moscow Russia

6. Graduate School of Oceanography; University of Rhode Island; Narragansett Rhode Island USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference51 articles.

1. Thermohaline circulation in the Arctic Mediterranean seas;Aagaard;J. Geophys. Res.,1985

2. Diatom assemblages in Arctic sea ice: Indicator for ice-drift pathways;Abelmann;Deep Sea Res.,1992

3. Is the central Arctic Ocean a sediment starved basin?;Backman;Quat. Sci. Rev.,2004

4. Arctic Coring Expedition (ACEX);Backman;Proc. Integr. Ocean Drill.,2006

5. Age model and core-seismic integration for the Cenozoic Arctic Coring Expedition sediments from the Lomonosov Ridge;Backman;Paleoceanography,2008

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