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- W2007442025 abstract "A fine-mesh (0.5 km, 2.5 m) two-dimensional model of particle transport and decomposition in the aphotic zone (>150 m) is used to analyse time series (April–August) of element fluxes caught by sediment traps, moored in a transect from the upper slope (500 m) to the continental rise (2750 m) of the Mid-Atlantic Bight. Inclusion of a benthic boundary layer within generally quiescent offshore flows of t1 cm s−1 in the model allows replication of the time phasing and amount of organic carbon sampled by the traps at 50 m above bottom. Over the lower 75 m of the water column on the upper slope, the survival of shelf diatom chains (sinking at 10 m day−1), as well as slope picoplankton (1 m day−1) and zooplankton fecal pellets (100 m day−1), provides most of the model's fidelity after the demise of the spring bloom. On the lower slope, however, the slow setting classes of detritus (<10 m day−1) do not survive the descent, with fluxes of shelf macroaggregates (also sinking at 100 m day−1) and fecal pellets required instead to match observations of particle rain. Downslope resuspension, near-bottom transport, and particle disaggregation may introduce more organic matter to sediments of the continental margins than previously estimated with traps." @default.
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- W2007442025 date "1991-07-01" @default.
- W2007442025 modified "2023-09-27" @default.
- W2007442025 title "Organic debris on the continental margins: a simulation analysis of source and fate" @default.
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- W2007442025 doi "https://doi.org/10.1016/0198-0149(91)90020-g" @default.
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