Publications des scientifiques de l'IRD

Dekaezemacker J., Bonnet Sophie, Grosso O., Moutin T., Bressac M., Capone D.G. (2013). Evidence of active dinitrogen fixation in surface waters of the eastern tropical South Pacific during El Niño and La Niña events and evaluation of its potential nutrient controls. Global Biogeochemical Cycles, 27 (3), 768-779. ISSN 0886-6236.

Titre du document
Evidence of active dinitrogen fixation in surface waters of the eastern tropical South Pacific during El Niño and La Niña events and evaluation of its potential nutrient controls
Année de publication
2013
Type de document
Article référencé dans le Web of Science WOS:000325488600014
Auteurs
Dekaezemacker J., Bonnet Sophie, Grosso O., Moutin T., Bressac M., Capone D.G.
Source
Global Biogeochemical Cycles, 2013, 27 (3), 768-779 ISSN 0886-6236
Biological N-2 fixation rates were quantified in the Eastern Tropical South Pacific (ETSP) during both El Nino (February 2010) and La Nina (March-April 2011) conditions, and from Low-Nutrient, Low-Chlorophyll (20 degrees S) to High-Nutrient, Low-Chlorophyll (HNLC) (10 degrees S) conditions. N-2 fixation was detected at all stations with rates ranging from 0.01 to 0.88nmolNL(-1) d(-1), with higher rates measured during El Nino conditions compared to La Nina. High N-2 fixations rates were reported at northern stations (HNLC conditions) at the oxycline and in the oxygen minimum zone (OMZ), despite nitrate concentrations up to 30 mu molL(-1), indicating that inputs of new N can occur in parallel with N loss processes in OMZs. Water-column integrated N-2 fixation rates ranged from 4 to 53 mu molNm(-2) d(-1) at northern stations, and from 0 to 148 mu molm(-2) d(-1) at southern stations, which are of the same order of magnitude as N-2 fixation rates measured in the oligotrophic ocean. N-2 fixation rates responded significantly to Fe and organic carbon additions in the surface HNLC waters, and surprisingly by concomitant Fe and N additions in surface waters at the edge of the subtropical gyre. Recent studies have highlighted the predominance of heterotrophic diazotrophs in this area, and we hypothesize that N-2 fixation could be directly limited by inorganic nutrient availability, or indirectly through the stimulation of primary production and the subsequent excretion of dissolved organic matter and/or the formation of micro-environments favorable for heterotrophic N-2 fixation.
Plan de classement
Milieux physico-chimique [032MILPHY]
Descripteurs
MILIEU MARIN ; EAU DE SURFACE ; EL NINO ; FIXATION BIOLOGIQUE DE L'AZOTE ; PRODUCTION PRIMAIRE ; FACTEUR LIMITANT ; CHLOROPHYLLE ; NUTRIMENT ; OXYGENE ; OLIGOTROPHIE ; LA NINA
Description Géographique
ZONE TROPICALE
Localisation
Fonds IRD [F B010061267]
Identifiant IRD
fdi:010061267
Contact