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Volume 4, issue 5
Biogeosciences, 4, 729–741, 2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

Special issue: Biogeochemistry and Optics South Pacific Experiment...

Biogeosciences, 4, 729–741, 2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  13 Sep 2007

13 Sep 2007

Nitrous oxide distribution and its origin in the central and eastern South Pacific Subtropical Gyre

J. Charpentier1,2, L. Farias2, N. Yoshida3,4, N. Boontanon4,5, and P. Raimbault6 J. Charpentier et al.
  • 1Programa de Postgrado, Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Chile
  • 2Departamento de Oceanografía & Centro Oceanográfico del Pacífico Sur (COPAS), Universidad de Concepción, Concepción, Chile
  • 3Frontier Collaborative Research Center, Tokyo Institute of Technology, Midori-ku, Yokohama, Japan
  • 4SORST project, JST, Kawaguchi, Saitama, Japan
  • 5Faculty of Environment and Resource Studies, Mahidol University 999 Phuttamonthon 4 Road, Phuttamonthon, Salaya, Nakhon Pathom 73170, Thailand
  • 6Laboratoire d'Océanographie et de Biogéochimie (CNRS UMR 6535), Centre d'Océanologie de Marseille, Campus de Luminy, Marseille Cedex, France

Abstract. The mechanisms of microbial nitrous oxide (N2O) production in the ocean have been the subject of many discussions in recent years. New isotopomeric tools can further refine our knowledge of N2O sources in natural environments. This study compares hydrographic, N2O concentration, and N2O isotopic and isotopomeric data from three stations along a coast-perpendicular transect in the South Pacific Ocean, extending from the center (Sts. GYR and EGY) of the subtropical oligotrophic gyre (~26° S; 114° W) to the upwelling zone (St. UPX) off the central Chilean coast (~34° S). Although AOU/N2O and NO3 trends support the idea that most of the N2O (mainly from intermediate water (200–600 m)) comes from nitrification, N2O isotopomeric composition (intramolecular distribution of 15N isotopes) expressed as SP (site preference of 15N) shows low values (10 to 12\permil) that could be attributed to the production through of microbial nitrifier denitrification (reduction of nitrite to N2O mediated by ammonium oxidizers). The coincidence of this SP signal with high – stability layer, where sinking organic particles can accumulate, suggests that N2O could be produced by nitrifier denitrification inside particles. It is postulated that deceleration of particles in the pycnocline can modify the advection - diffusion balance inside particles, allowing the accumulation of nitrite and O2 depletion suitable for nitrifier denitrication. As lateral advection seems to be relatively insignificant in the gyre, in situ nitrifier denitrification could account for 40–50% of the N2O produced in this layer. In contrast, coastal upwelling system is characterized by O2 deficient condition and some N deficit in a eutrophic system. Here, N2O accumulates up to 480% saturation, and isotopic and isotopomer signals show highly complex N2O production processes, which presumably reflect both the effect of nitrification and denitrification at low O2 levels on N2O production, but net N2O consumption by denitrification was not observed.

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