Abstract Concentrations of redox-sensitive elements (S, Mn, Mo, U, Cd, Re) were analyzed in a set of 27 sediment cores collected along the North American Arctic margin (NAAM) from the North Bering Sea to Davis Strait via the Canadian Archipelago. Sedimentary distributions and accumulation rates of the elements were used to evaluate early diagenesis in sediments along this section and to estimate the importance of this margin as a sink for key elements in the polar and global oceans. Distributions of Mn, total S and reduced inorganic S demonstrated that diagenetic conditions and thus sedimentary carbon turnover in the NAAM is organized regionally: undetectable or very thin layers (
Early diagenesis and trace element accumulation in North American Arctic margin sediments.
Z. Kuzyk,C. Gobeil,M. Goñi,R. Macdonald
Published 2014 in Geochimica et Cosmochimica Acta
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- Publication year
2014
- Venue
Geochimica et Cosmochimica Acta
- Publication date
2014-12-01
- Fields of study
Geology, Environmental Science
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