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- W2023007775 abstract "Monthly samples were collected by a sediment trap deployed for one year at 473 m above the sea floor in water 2123 m deep at a station located at 75°N, 11°E, southwest of Spitsbergen. This station was positioned at the northernmost extension of the Norwegian Current and was not covered by sea ice throughout the year of the experiment. The annual particle flux was 28.3 g m−2, of which 49% was biogenic and 51% was lithogenic particles. The annual fluxes of organic carbon, calcium carbonate, and biogenic opal were 2.9, 6.6 and 2.0 g m−2, respectively. Biogenic particles settling in the northern Norwegian Sea are dominated by carbonate, not opal. There were three distinct seasonality phases in sedimentation: phase 1, May to July was a period of relatively small flux, reflecting the spring bloom material in the surface layer; phase 2, August to November, showed the largest flux of carbon and other biogenic particles; and phase 3, December to May, was a period of outburst of lithogenic particle sedimentation which peaked during mid-January to mid-February. We assume that this outburst is related to cold deep water generated on the Barents Sea shelf and flowing southwestward through the Storfjord Trough into the Norwegian Sea." @default.
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- W2023007775 date "1988-08-01" @default.
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- W2023007775 title "Annual particle flux and a winter outburst of sedimentation in the northern Norwegian Sea" @default.
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- W2023007775 doi "https://doi.org/10.1016/0198-0149(88)90078-7" @default.
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