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    <titleInfo>
      <title>Distributions and abundances of sublineages of the N-2-fixing cyanobacterium Candidatus Atelocyanobacterium thalassa (UCYN-A) in the New Caledonian coral lagoon</title>
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    <name type="personnal">
      <namePart type="family">Henke</namePart>
      <namePart type="given">B. A.</namePart>
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    <name type="personnal">
      <namePart type="family">Turk-Kubo</namePart>
      <namePart type="given">K. A.</namePart>
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    <name type="personnal">
      <namePart type="family">Bonnet</namePart>
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    <name type="personnal">
      <namePart type="family">Zehr</namePart>
      <namePart type="given">J. P.</namePart>
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    <abstract>Nitrogen (N-2) fixation is a major source of nitrogen that supports primary production in the vast oligotrophic areas of the world's oceans. The Western Tropical South Pacific has recently been identified as a hotspot for N-2 fixation. In the Noumea lagoon (New Caledonia), high abundances of the unicellular N-2-fixing cyanobacteria group A (UCYN-A), coupled with daytime N-2 fixation rates associated with the &lt;10 mu m size fraction, suggest UCYN-A may be an important diazotroph (N-2-fixer) in this region. However, little is known about the seasonal variability and diversity of UCYN-A there. To assess this, surface waters from a 12 km transect from the mouth of the Dumbea River to the Dumbea Pass were sampled monthly between July 2012 and March 2014. UCYN-A abundances for two of the defined sublineages, UCYN-A1 and UCYN-A2, were quantified using qPCR targeting the nifH gene, and the nifH-based diversity of UCYN-A was characterized by identifying oligotypes, alternative taxonomic units defined by nucleotide positions with high variability. UCYN-A abundances were dominated by the UCYN-A1 sublineage, peaked in September and October and could be predicted by a suite of nine environmental parameters. At the sublineage level, UCYN-A1 abundances could be predicted based on lower temperatures (&lt;23 degrees C), nitrate concentrations, precipitation, wind speed, while UCYN-A2 abundances could be predicted based on silica, and chlorophyll a concentrations, wind direction, precipitation, and wind speed. Using UCYN-A nifH oligotyping, similar environmental variables explained the relative abundances of sublineages and their associated oligotypes, with the notable exception of the UCYN-A2 oligotype (oligo43) which had relative abundance patterns distinct from the dominant UCYN-A2 oligotype (oligo3). The results support an emerging pattern that UCYN-A is comprised of a diverse group of strains, with sublineages that may have different ecological niches. By identifying environmental factors that influence the composition and abundance of UCYN-A sublineages, this study helps to explain global UCYN-A abundance patterns, and is important for understanding the significance of N2 fixation at local and global scales.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>Candidatus Atelocyanobacterium thalassa</topic>
      <topic>nitrogen fixation</topic>
      <topic>nitrogenase</topic>
      <topic>nifH</topic>
      <topic>oligotyping</topic>
      <topic>UCYN-A</topic>
      <topic>New Caledonia</topic>
      <topic>Western Tropical South Pacific</topic>
    </subject>
    <subject authority="local">
      <geographic>NOUVELLE CALEDONIE</geographic>
      <geographic>PACIFIQUE</geographic>
      <geographic>ZONE TROPICALE</geographic>
    </subject>
    <classification authority="local">034</classification>
    <classification authority="local">036</classification>
    <relatedItem type="host">
      <titleInfo>
        <title>Frontiers in Microbiology</title>
      </titleInfo>
      <part>
        <detail type="volume">
          <number>9</number>
        </detail>
        <extent unit="pages">
          <list>art. 554 [14 ]</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2018</dateIssued>
      </originInfo>
      <identifier type="issn">1664-302X</identifier>
    </relatedItem>
    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010072713</identifier>
    <identifier type="doi">10.3389/fmicb.2018.00554</identifier>
    <identifier type="issn">1664-302X</identifier>
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      <url usage="primary display" access="object in context">https://www.documentation.ird.fr/hor/fdi:010072713</url>
      <url access="row object">https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers18-04/010072713.pdf</url>
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      <recordCreationDate encoding="w3cdtf">2018-05-04</recordCreationDate>
      <recordChangeDate encoding="w3cdtf">2023-07-11</recordChangeDate>
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