<?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>Aphotic N-2 fixation in the Eastern Tropical South Pacific Ocean</dc:title>
  <dc:creator>/Bonnet, Sophie</dc:creator>
  <dc:creator>Dekaezemacker, J.</dc:creator>
  <dc:creator>Turk-Kubo, K. A.</dc:creator>
  <dc:creator>Moutin, T.</dc:creator>
  <dc:creator>Hamersley, R.M.</dc:creator>
  <dc:creator>Grosso, O.</dc:creator>
  <dc:creator>Zehr, J.P.</dc:creator>
  <dc:creator>Capone, D.G.</dc:creator>
  <dc:subject>MILIEU MARIN</dc:subject>
  <dc:subject>EL NINO</dc:subject>
  <dc:subject>COUCHE EUPHOTIQUE</dc:subject>
  <dc:subject>FIXATION BIOLOGIQUE DE L'AZOTE</dc:subject>
  <dc:subject>OXYGENE</dc:subject>
  <dc:subject>MICROORGANISME</dc:subject>
  <dc:subject>ANALYSE QUANTITATIVE</dc:subject>
  <dc:subject>PROFIL VERTICAL</dc:subject>
  <dc:subject>PROFONDEUR</dc:subject>
  <dc:subject>LA NINA</dc:subject>
  <dc:subject>COUCHE APHOTIQUE</dc:subject>
  <dc:subject>OMZ.OXYGENE MINIMUM ZONE</dc:subject>
  <dc:description>We examined rates of N-2 fixation from the surface to 2000 m depth in the Eastern Tropical South Pacific (ETSP) during El Ni&#xF1;o (2010) and La Ni&#xF1;a (2011). Replicated vertical profiles performed under oxygen-free conditions show that N-2 fixation takes place both in euphotic and aphotic waters, with rates reaching 155 to 509 mu mol N m(-2) d(-1) in 2010 and 24 +/- 14 to 118 +/- 87 mu mol N m(-2) d(-1) in 2011. In the aphotic layers, volumetric N-2 fixation rates were relatively low (&lt; 1.00 nmol N L-1 d(-1)), but when integrated over the whole aphotic layer, they accounted for 87-90% of total rates (euphotic+ aphotic) for the two cruises. Phylogenetic studies performed in microcosms experiments confirm the presence of diazotrophs in the deep waters of the Oxygen Minimum Zone (OMZ), which were comprised of non-cyanobacterial diazotrophs affiliated with nifH clusters 1K (predominantly comprised of alpha-proteobacteria), 1G (predominantly comprised of gamma-proteobacteria), and 3 (sulfate reducing genera of the delta-proteobacteria and Clostridium spp., Vibrio spp.). Organic and inorganic nutrient addition bioassays revealed that amino acids significantly stimulated N-2 fixation in the core of the OMZ at all stations tested and as did simple carbohydrates at stations located nearest the coast of Peru/Chile. The episodic supply of these substrates from upper layers are hypothesized to explain the observed variability of N-2 fixation in the ETSP.</dc:description>
  <dc:date>2013</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010061449</dc:identifier>
  <dc:identifier>fdi:010061449</dc:identifier>
  <dc:identifier>Bonnet Sophie, Dekaezemacker J., Turk-Kubo K. A., Moutin T., Hamersley R.M., Grosso O., Zehr J.P., Capone D.G.. Aphotic N-2 fixation in the Eastern Tropical South Pacific Ocean. 2013, 8 (12), e81265 [14 ]</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>ZONE TROPICALE</dc:coverage>
</oai_dc:dc>
