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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 5
Biogeosciences, 13, 1453-1468, 2016
https://doi.org/10.5194/bg-13-1453-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Biogeochemical processes, tropospheric chemistry and interactions...

Biogeosciences, 13, 1453-1468, 2016
https://doi.org/10.5194/bg-13-1453-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Mar 2016

Research article | 09 Mar 2016

Nitrogen cycling in shallow low-oxygen coastal waters off Peru from nitrite and nitrate nitrogen and oxygen isotopes

Happy Hu1,*, Annie Bourbonnais1,*, Jennifer Larkum1, Hermann W. Bange2, and Mark A. Altabet1 Happy Hu et al.
  • 1School for Marine Science and Technology, University of Massachusetts Dartmouth, 706 South Rodney French Blvd, New Bedford, MA 02744-1221, USA
  • 2GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker Weg 20, 24105 Kiel, Germany
  • *These authors contributed equally to this work.

Abstract. O2 deficient zones (ODZs) of the world's oceans are important locations for microbial dissimilatory nitrate (NO3) reduction and subsequent loss of combined nitrogen (N) to biogenic N2 gas. ODZs are generally coupled to regions of high productivity leading to high rates of N-loss as found in the coastal upwelling region off Peru. Stable N and O isotope ratios can be used as natural tracers of ODZ N-cycling because of distinct kinetic isotope effects associated with microbially mediated N-cycle transformations. Here we present NO3 and nitrite (NO2) stable isotope data from the nearshore upwelling region off Callao, Peru. Subsurface oxygen was generally depleted below about 30 m depth with concentrations less than 10 µM, while NO2 concentrations were high, ranging from 6 to 10 µM, and NO3 was in places strongly depleted to near 0µM. We observed for the first time a positive linear relationship between NO2δ15N and δ18O at our coastal stations, analogous to that of NO3 N and O isotopes during NO3 uptake and dissimilatory reduction. This relationship is likely the result of rapid NO2 turnover due to higher organic matter flux in these coastal upwelling waters. No such relationship was observed at offshore stations where slower turnover of NO2 facilitates dominance of isotope exchange with water. We also evaluate the overall isotope fractionation effect for N-loss in this system using several approaches that vary in their underlying assumptions. While there are differences in apparent fractionation factor (ε) for N-loss as calculated from the δ15N of NO3, dissolved inorganic N, or biogenic N2, values for ε are generally much lower than previously reported, reaching as low as 6.5 ‰. A possible explanation is the influence of sedimentary N-loss at our inshore stations which incurs highly suppressed isotope fractionation.

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