Abstract
We measured fluxes of NH +4 and NO −3 and δ15N of NH +4 , sediment, and porewater NH +4 from incubated sediment cores along a nitrate gradient and in different seasons from Childs River, MA. NH +4 flux was low at the downstream site with the lowest concentration of organic matter (high salinity) but otherwise did not differ along the estuary. The δ15N of regenerated NH +4 ranged from +6.1‰ to +15.3‰ but did not vary significantly with season or salinity; the mean for the entire estuary was +10.4 ± 0.5‰. Based on differences between the δ15N of regenerated NH +4 and sediment, and expected isotopic fractionation due to remineralization, we concluded that nitrification occurred after remineralization of NH +4 . Differences between the δ15N of regenerated NH +4 and the δ15N of porewater NH +4 provided further evidence of nitrification. We estimated that 11% to 48% of remineralized NH +4 underwent coupled nitrification–denitrification before release into the water column. In spite of losses to denitrification, NH +4 flux released 1.4 mol N m−2 year−1 to the water column and could provide 42% of phytoplankton nitrogen requirements.
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Acknowledgments
Funding to J.K.Y. was provided by a Palmer-McLeod Graduate Fellowship from the Boston University Marine Program, an Environmental Protection Agency (EPA)-STAR fellowship (U-91613501-0), and a National Oceanic and Atmospheric Administration (NOAA)-National Estuarine Research Reserve (NERR) Graduate Fellowship (NA17OR1198). G.T. was supported by a NOAA-NERR Graduate Fellowship (NA07OR0274) and a Woods Hole Oceanographic Institution (WHOI) Sea Grant (NA16RG2273). We thank J. McClelland for help with interpretation of isotopic signatures, J. Tucker for methodological suggestions, V. Starczak for help with statistics, and two anonymous reviewers for comments, which substantially improved the manuscript.
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York, J.K., Tomasky, G., Valiela, I. et al. Isotopic Approach to Determining the Fate of Ammonium Regenerated from Sediments in a Eutrophic Sub-estuary of Waquoit Bay, MA. Estuaries and Coasts 33, 1069–1079 (2010). https://doi.org/10.1007/s12237-010-9278-1
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DOI: https://doi.org/10.1007/s12237-010-9278-1