<?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>In-depth characterization of diazotroph activity across the western tropical South Pacific hotspot of N-2 fixation (OUTPACE cruise)</dc:title>
  <dc:creator>/Bonnet, Sophie</dc:creator>
  <dc:creator>Caffin, M.</dc:creator>
  <dc:creator>Berthelot, H.</dc:creator>
  <dc:creator>Grosso, O.</dc:creator>
  <dc:creator>/Benavides, Mar</dc:creator>
  <dc:creator>Helias-Nunige, S.</dc:creator>
  <dc:creator>Guieu, C.</dc:creator>
  <dc:creator>Stenegren, M.</dc:creator>
  <dc:creator>Foster, R. A.</dc:creator>
  <dc:description>Here we report N-2 fixation rates from a similar to 4000 km transect in the western and central tropical South Pacific, a particularly undersampled region in the world ocean. Water samples were collected in the euphotic layer along a west to east transect from 160 degrees E to 160 degrees W that covered contrasting trophic regimes, from oligotrophy in the Melanesian archipelago (MA) waters to ultraoligotrophy in the South Pacific Gyre (GY) waters. N-2 fixation was detected at all 17 sampled stations with an average depth-integrated rate of 631 +/- 286 mu mol Nm(-2) d(-1) (range 196-1153 mu mol Nm(-2) d(-1)) in MA waters and of 85 +/- 79 mu mol Nm(-2) d(-1) (range 18-172 mu mol Nm(-2) d(-1)) in GY waters. Two cyanobacteria, the larger colonial filamentous Trichodesmium and the smaller UCYN-B, dominated the enumerated diazotroph community (&gt;80 %) and gene expression of the nifH gene (cDNA &gt; 10(5) nifH copies L-1) in MA waters. Single-cell isotopic analyses performed by nanoscale secondary ion mass spectrometry (nanoSIMS) at selected stations revealed that Trichodesmium was always the major contributor to N-2 fixation in MA waters, accounting for 47.1-83.8% of bulk N-2 fixation. The most plausible environmental factors explaining such exceptionally high rates of N-2 fixation in MA waters are discussed in detail, emphasizing the role of macro- and micro-nutrient (e.g., iron) availability, seawater temperature and currents.</dc:description>
  <dc:date>2018</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010073224</dc:identifier>
  <dc:identifier>fdi:010073224</dc:identifier>
  <dc:identifier>Bonnet Sophie, Caffin M., Berthelot H., Grosso O., Benavides Mar, Helias-Nunige S., Guieu C., Stenegren M., Foster R. A.. In-depth characterization of diazotroph activity across the western tropical South Pacific hotspot of N-2 fixation (OUTPACE cruise). 2018, 15 (13),  4215-4232</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>PACIFIQUE</dc:coverage>
  <dc:coverage>MELANESIE</dc:coverage>
  <dc:coverage>ZONE TROPICALE</dc:coverage>
</oai_dc:dc>
