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Biogeosciences, 8, 2257-2267, 2011
www.biogeosciences.net/8/2257/2011/
doi:10.5194/bg-8-2257-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Planktonic dinitrogen fixation along a longitudinal gradient across the Mediterranean Sea during the stratified period (BOUM cruise)
S. Bonnet, O. Grosso, and T. Moutin
INSU-CNRS, Laboratoire d'Océanographie Physique et Biogéochimique (LOPB), UMR6535, CNRS-IRD-Université de la Méditerranée, Centre d'Océanologie de Marseille, Faculté des Sciences de Luminy, Case 901, 13288 Cedex 09 Marseille, France

Abstract. This study provides extensive data on planktonic N2 fixation rates across the whole Mediterranean Sea. They show that N2 fixation occurs in Mediterranean waters during the stratification period, with a clear decreasing trend from the oligotrophic western basin (10–76 μmol m−2 d−1) to the ultra oligotrophic eastern basin (0–0.4 μmol m−2 d−1). Highest rates are measured in the less oligotrophic western basin, between the surface and 75 m-depth, where 45 to 75 % of N2 fixation are found within the picoplanktonic fraction (<3 μm). While the biogeochemical impact of N2 fixation in the eastern basin seems negligible, N2 fixation is able to sustain up to 35 % of new primary production during the stratified period in the western basin. These data disagree with indirect estimates of N2 fixation based on geochemical tracers and nutrient budgets, which indicates that N2 fixation increases with increasing N:P ratios and decreasing stable N isotopic signature of particulate organic nitrogen and NO3 from west to east. These results finally point out the need to assess N2 fixation at a higher temporal resolution in order to better understand the diazotrophs' dynamic under contrasted biogeochemical conditions.

Citation: Bonnet, S., Grosso, O., and Moutin, T.: Planktonic dinitrogen fixation along a longitudinal gradient across the Mediterranean Sea during the stratified period (BOUM cruise), Biogeosciences, 8, 2257-2267, doi:10.5194/bg-8-2257-2011, 2011.
 
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