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- W2037276563 abstract "Organic matter (OM) remineralization may be considered a key function of the benthic compartment of marine ecosystems and in this study we investigated if the input of labile organic carbon alters mineralization of indigenous sediment OM (OM priming). Using 13C-enriched diatoms as labile tracer carbon, we examined shallow-water sediments (surface and subsurface layers) containing organic carbon of different reactivity under oxic versus anoxic conditions. The background OM decomposition rates of the sediment used ranged from 0.08 to 0.44 μmol C mlws-1 day-1. Algal OM additions induced enhanced levels of background remineralization (priming) up to 31% and these measured excess fluxes were similar to mineralization of the added highly degradable tracer algal carbon. This suggests that OM priming may be important in marine sediments." @default.
- W2037276563 created "2016-06-24" @default.
- W2037276563 creator A5037846067 @default.
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- W2037276563 date "2009-07-18" @default.
- W2037276563 modified "2023-10-18" @default.
- W2037276563 title "Seafloor ecosystem functioning: the importance of organic matter priming" @default.
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- W2037276563 doi "https://doi.org/10.1007/s00227-009-1255-5" @default.
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