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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 5
Clim. Past, 13, 511–531, 2017
https://doi.org/10.5194/cp-13-511-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Climate–carbon–cryosphere interactions in the...

Clim. Past, 13, 511–531, 2017
https://doi.org/10.5194/cp-13-511-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 23 May 2017

Research article | 23 May 2017

Sedimentary record from the Canada Basin, Arctic Ocean: implications for late to middle Pleistocene glacial history

Linsen Dong et al.

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Cited articles

Adler, R. E., Polyak, L., Ortiz, J. D., Kaufman, D. S., Channell, J. E. T., Xuan, C., Grottoli, A. G., Sellén, E., and Crawford, K. A.: Sediment record from the western Arctic Ocean with an improved Late Quaternary age resolution: HOTRAX core HLY0503-8JPC, Mendeleev Ridge, Global Planet. Change, 68, 18–29, 2009.
Andrews, J. T.: Icebergs and iceberg rafted detritus (IRD) in the North Atlantic: Facts and assumptions, Oceanography, 13, 100–108, 2000.
Basilyan, A. E., Nikol'skyi, P. A., Maksimov, F. E., and Kuznetsov, V. Y.: Age of Cover Glaciation of the New Siberian Islands Based on 230Th/U-dating of Mollusk Shells, Structure and Development of the Lithosphere, Paulsen, Moscow, 506–514, 2010.
Bazhenova, E., Fagel, N., and Stein, R.: North American origin of “pink–white” layers at the Mendeleev Ridge (Arctic Ocean): New insights from lead and neodymium isotope composition of detrital sediment component, Mar. Geol., 386, 44–55, 2017.
Behrends, M.: Reconstruction of sea-ice drift and terrigenous sediment supply in the Late Quaternary: heavy-mineral associations in sediments of the Laptev-Sea continental margin and the central Arctic Ocean, Rep. Polar Res., 310, 1–167, 1999.
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In this manuscript, we present the results of our study conducted for a sediment core (ARC4-BN05) collected in the Arctic Ocean. Detailed examination of clay and bulk mineralogy along with grain size, content of Ca and Mn, and planktonic foraminiferal numbers in core ARC4–BN05 provides important new information about sedimentary environments and provenance. Based on these proxies, we try to reveal late to middle Pleistocene glacial history.
In this manuscript, we present the results of our study conducted for a sediment core...
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