<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Evidence of active dinitrogen fixation in surface waters of the eastern tropical South Pacific during El Ni&#xF1;o and La Ni&#xF1;a events and evaluation of its potential nutrient controls</dc:title>
  <dc:creator>Dekaezemacker, J.</dc:creator>
  <dc:creator>/Bonnet, Sophie</dc:creator>
  <dc:creator>Grosso, O.</dc:creator>
  <dc:creator>Moutin, T.</dc:creator>
  <dc:creator>Bressac, M.</dc:creator>
  <dc:creator>Capone, D.G.</dc:creator>
  <dc:subject>MILIEU MARIN</dc:subject>
  <dc:subject>EAU DE SURFACE</dc:subject>
  <dc:subject>EL NINO</dc:subject>
  <dc:subject>FIXATION BIOLOGIQUE DE L'AZOTE</dc:subject>
  <dc:subject>PRODUCTION PRIMAIRE</dc:subject>
  <dc:subject>FACTEUR LIMITANT</dc:subject>
  <dc:subject>CHLOROPHYLLE</dc:subject>
  <dc:subject>NUTRIMENT</dc:subject>
  <dc:subject>OXYGENE</dc:subject>
  <dc:subject>OLIGOTROPHIE</dc:subject>
  <dc:subject>LA NINA</dc:subject>
  <dc:subject>N2 fixation</dc:subject>
  <dc:subject>ETSP</dc:subject>
  <dc:subject>oligotrophic</dc:subject>
  <dc:subject>HNLC</dc:subject>
  <dc:subject>oxygen minimum zones</dc:subject>
  <dc:subject>nutrient</dc:subject>
  <dc:subject>limitation</dc:subject>
  <dc:description>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.</dc:description>
  <dc:date>2013</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010061267</dc:identifier>
  <dc:identifier>fdi:010061267</dc:identifier>
  <dc:identifier>Dekaezemacker J., Bonnet Sophie, Grosso O., Moutin T., Bressac M., Capone D.G.. Evidence of active dinitrogen fixation in surface waters of the eastern tropical South Pacific during El Ni&#xF1;o and La Ni&#xF1;a events and evaluation of its potential nutrient controls. 2013, 27 (3), 768-779</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>ZONE TROPICALE</dc:coverage>
</oai_dc:dc>
