Journal
FRONTIERS IN MARINE SCIENCE
Volume 4, Issue -, Pages -Publisher
FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2017.00303
Keywords
N-2 fixation; nitrate diffusive flux; nifH; UCYN-A; Gammaproteobacteria; NW Iberian upwelling; Atlantic Ocean
Funding
- NICANOR project (Galician Government) [EM2013/021]
- FPU predoctoral fellowship from the Spanish Ministry of Education, Culture and Sports [FPU13/01674]
- RADIALES project of the Institute Espanol de Oceanogralin
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The classical paradigm about marine Nn fixation establishes that this process is mainly constrained to nitrogen-poor tropical and subtropical regions, and sustained by the colonial cyanobacterium Trichodesmiurn spp. and diatom-diazotroph symbiosis. However, the application of molecular techniques allowed determining a high phylogenic diversity and wide distribution of marine diazotrophs, which extends the range of ocean environments where biological N-2 fixation may be relevant. Between February 2014 and December 2015, we carried out 10 one-day samplings in the upwelling system off NW Iberia in order to: (1) investigate the seasonal variability in the magnitude of N-2 fixation, (2) determine its biogeochemical role as a mechanism of new nitrogen supply, and (3) quantify the main diazotrophs in the region under contrasting hydrographic regimes. Our results indicate that the magnitude of N-2 fixation in this region was relatively low (0.001 +/- 0.002-0.095 +/- 0.024 p.mol N m(-3) d(-1)), comparable to the lower-end of rates described for the subtropical NE Atlantic. Maximum rates were observed at the surface during both upwelling and relaxation conditions. The comparison with nitrate diffusive fluxes revealed the minor role of N-2 fixation (<2%) as a mechanism of new nitrogen supply into the euphotic layer. Small diazotrophs (<10 mu m) were responsible for all N-2 fixation activity detected in the region. Quantitative PCB targeting the nifH gene revealed the highest abundances of two sublineages of Candidatus Atelocyanobacterium thalassa or UCYN-A (UCYN-Al and UCYN-A2), mainly at surface waters during upwelling and relaxation conditions, and of Gammaproteobacteria gamma-24774A11 at deep waters during downwelling. Maximum abundance for the three groups were up to 6.7 x 10(2), 1.5 x 10(3), and 2.4 x 10(4) nifH copies L-1, respectively. Our findings demonstrate measurable Nr fixation activity and presence of diazotrophs throughout the year in a nitrogen-rich temperate region.
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