Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 9, issue 8
Biogeosciences, 9, 3205–3212, 2012
https://doi.org/10.5194/bg-9-3205-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Nitrogen and global change

Biogeosciences, 9, 3205–3212, 2012
https://doi.org/10.5194/bg-9-3205-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Aug 2012

Research article | 21 Aug 2012

Following the N2O consumption in the oxygen minimum zone of the eastern South Pacific

M. Cornejo1 and L. Farías1,2 M. Cornejo and L. Farías
  • 1Laboratorio de Procesos Oceanográficos y Clima (PROFC), Departamento de Oceanografía, Universidad de Concepción, Casilla 160-C, Concepción, Chile
  • 2Centro de Investigación Oceanográfica en el Pacífico Suroriental (COPAS), Universidad de Concepción, Casilla 160-C, Concepción, Chile

Abstract. Oxygen minimum zones (OMZs), such as those found in the eastern South Pacific (ESP), are the most important N2O sources in the global ocean relative to their volume. N2O production is related to low O2 concentrations and high primary productivity. However, when O2 is sufficiently low, canonical denitrification takes place and N2O consumption can be expected. N2O distribution in the ESP was analyzed over a wide latitudinal and longitudinal range (from 5° to 30° S and from 71–76° to ~ 84° W) based on ~ 890 N2O measurements. Intense N2O consumption, driving undersaturations as low as 40%, was always associated with secondary NO2 accumulation (SNM), a good indicator of suboxic/anoxic O2 levels. First, we explore relationships between ΔN2O and O2 based on existing data of denitrifying bacteria cultures and field observations. Given the uncertainties in the O2 measurements, a second relationship between ΔN2O and NO2 (> 0.75 μM) was established for suboxic waters (O2 < 8 μM). We reproduced the apparent N2O production (ΔN2O) along the OMZ in ESP with high reliability (r2 = 0.73 p = 0.01). Our results will contribute to the quantification of the N2O that is recycled in O2 deficient waters, and improve the prediction of N2O behavior under future scenarios of OMZ expansion and intensification.

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