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• W1940298059 endingPage "1972" @default.
• W1940298059 startingPage "1958" @default.
• W1940298059 abstract "Potential rates of sediment denitrification, anaerobic ammonium oxidation (anammox), and dissimilatory nitrate reduction to ammonium (DNRA) were mapped across the entire Niantic River Estuary, CT, USA, at 100–200 m scale resolution consisting of 60 stations. On the estuary scale, denitrification accounted for ~ 90% of the nitrogen reduction, followed by DNRA and anammox. However, the relative importance of these reactions to each other was not evenly distributed through the estuary. A Nitrogen Retention Index (NIRI) was calculated from the rate data (DNRA/(denitrification + anammox)) as a metric to assess the relative amounts of reactive nitrogen being recycled versus retained in the sediments following reduction. The distribution of rates and accompanying sediment geochemical analytes suggested variable controls on specific reactions, and on the NIRI, depending on position in the estuary and that these controls were linked to organic carbon abundance, organic carbon source, and pore water sulfide concentration. The relationship between NIRI and organic carbon abundance was dependent on organic carbon source. Sulfide proved the single best predictor of NIRI, accounting for 44% of its observed variance throughout the whole estuary. We suggest that as a single metric, sulfide may have utility as a proxy for gauging the distribution of denitrification, anammox, and DNRA." @default.
• W1940298059 created "2016-06-24" @default.
• W1940298059 creator A5008016103 @default.
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• W1940298059 date "2015-10-01" @default.
• W1940298059 modified "2023-10-10" @default.
• W1940298059 title "Nitrogen reduction pathways in estuarine sediments: Influences of organic carbon and sulfide" @default.
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• W1940298059 doi "https://doi.org/10.1002/2015jg003057" @default.
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