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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 15
Biogeosciences, 13, 4461-4479, 2016
https://doi.org/10.5194/bg-13-4461-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Biogeochemical and biological response to a diazotroph bloom...

Biogeosciences, 13, 4461-4479, 2016
https://doi.org/10.5194/bg-13-4461-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Reviews and syntheses 10 Aug 2016

Reviews and syntheses | 10 Aug 2016

Biogeochemical and biological impacts of diazotroph blooms in a low-nutrient, low-chlorophyll ecosystem: synthesis from the VAHINE mesocosm experiment (New Caledonia)

Sophie Bonnet1,2, Melika Baklouti1, Audrey Gimenez1, Hugo Berthelot1, and Ilana Berman-Frank3 Sophie Bonnet et al.
  • 1IRD, Aix Marseille Université, CNRS/INSU, Université de Toulon, Mediterranean Institute of Oceanography (MIO) UM110, 13288, Marseille-Noumea, France, New Caledonia
  • 2Institut de Recherche pour le Développement, AMU/ NRS/INSU, Université de Toulon, Mediterranean Institute of Oceanography (MIO) UM110, 98848, Noumea, New Caledonia
  • 3Mina and Everard Goodman Faculty of Life Sciences, Bar-Ilan University, Ramat Gan, Israel

Abstract. In marine ecosystems, biological N2 fixation provides the predominant external source of nitrogen (N; 140±50TgNyr−1), contributing more than atmospheric and riverine inputs to the N supply. Yet the fate and magnitude of the newly fixed N, or diazotroph-derived N (hereafter named DDN) in marine ecosystems is poorly understood. Moreover, whether the DDN is preferentially and directly exported out of the photic zone, recycled by the microbial loop and/or transferred into larger organisms remains unclear. These questions were investigated in the framework of the VAHINE (VAriability of vertical and tropHIc transfer of diazotroph derived N in the south wEst Pacific) project. Triplicate large volume ( ∼ 50m3) mesocosms were deployed in the tropical south-west Pacific coastal ocean (New Caledonia). The mesocosms were intentionally fertilized with  ∼ 0.8µM dissolved inorganic phosphorus (DIP) at the start of the experiment to stimulate diazotrophy. A total of 47 stocks, fluxes, enzymatic activities and diversity parameters were measured daily inside and outside the mesocosms by the 40 scientists involved in the project. The experiment lasted for 23 days and was characterized by two distinct and successive diazotroph blooms: a dominance of diatom-diazotroph associations (DDAs) during the first half of the experiment (days 2–14) followed by a bloom of unicellular cyanobacterial lineage C (UCYN-C during the second half of the experiment (days 15–23). These conditions provided a unique opportunity to compare the DDN transfer and export efficiency associated with different diazotrophs. Here we summarize the major experimental and modelling results obtained during the project and described in the VAHINE special issue, in particular those regarding the evolution of the main standing stocks, fluxes and biological characteristics over the 23-day experiment, the contribution of N2 fixation to export fluxes, the DDN released to dissolved pool and its transfer to the planktonic food web (bacteria, phytoplankton, zooplankton). We then apply our Eco3M modelling platform to further infer the fate of DDN in the ecosystem and the role of N2 fixation on productivity, food web structure and carbon export. Recommendations for future work are finally provided in the conclusion section.

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