<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/10.1111/1758-2229.70168">
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    <dct:isReferencedBy>White Rose Research Online</dct:isReferencedBy>
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    <dct:isPartOf>Environmental Microbiology Reports</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2025-08-11</dct:created>
    <dc:description>ABSTRACT                   &lt;p&gt;                     We investigate the potential for the globally distributed marine ammonia oxidising archaeon (AOA)                     Nitrosopumilus maritimus                     to oxidise iodide (I                     &#65506;&#65416;&#65426;                     ), with the aim of identifying a key driver of seawater iodate (IO                     3                     &#65506;&#65416;&#65426;                     ) renewal. Batch cultures of                     N. maritimus                     grew well in concentrations of 0.1 to 1&#65506;&#65408;&#65417;mM NH                     4                     +                     and from 0.0001 to 1&#65506;&#65408;&#65417;mM I                     &#65506;&#65416;&#65426;                     . There was near 100% conversion of ammonium to nitrite over an 8&#65506;&#65408;&#65424;day growth period. No loss of I                     &#65506;&#65416;&#65426;                     or production of IO                     3                     &#65506;&#65416;&#65426;                     was detected in cultures where I                     &#65506;&#65416;&#65426;                     was added, indicating that                     N. maritimus                     is unable to drive I                     &#65506;&#65416;&#65426;                     oxidation under the tested conditions. This contrasts with previous observations of I                     &#65506;&#65416;&#65426;                     oxidation by ammonium oxidising bacteria (AOB). We explore whether differences between the metabolism of AOA and AOB could explain their differing actions on I                     &#65506;&#65416;&#65426;                     .                     N. maritimus                     cultures grown with the equivalent IO                     3                     &#65506;&#65416;&#65426;                     concentrations also showed no reduction in [IO                     3                     &#65506;&#65416;&#65426;                     ]. In addition, the growth of the                     N. maritimus                     culture was unaffected by inorganic iodine concentrations over 1000 times higher than in ambient seawater, suggesting a resilience to high iodine. These results suggest that AOA might have very little role in inorganic iodine turnover in the global ocean.                   &lt;/p</dc:description>
    <dc:subject>ammonium</dc:subject>
    <dc:subject>iodate</dc:subject>
    <dc:subject>archaea</dc:subject>
    <dc:subject>oxidation</dc:subject>
    <dc:subject>iodide</dc:subject>
    <dc:subject>Nitrosopumilus maritimus</dc:subject>
    <dc:subject>nitrification</dc:subject>
    <dc:subject>Research Article</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-5906-176x"/>
    <dc:creator>Alison L. Webb, Barbora Oudova&#8208;Rivera, Martyn Ward, Lucy J. Carpenter, Laura E. Lehtovirta&#8208;Morley, Rosie Chance, </dc:creator>
    <dc:date>2025-08-01</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>ABSTRACT                   &lt;p&gt;                     We investigate the potential for the globally distributed marine ammonia oxidising archaeon (AOA)                     Nitrosopumilus maritimus                     to oxidise iodide (I                     &#65506;&#65416;&#65426;                     ), with the aim of identifying a key driver of seawater iodate (IO                     3                     &#65506;&#65416;&#65426;                     ) renewal. Batch cultures of                     N. maritimus                     grew well in concentrations of 0.1 to 1&#65506;&#65408;&#65417;mM NH                     4                     +                     and from 0.0001 to 1&#65506;&#65408;&#65417;mM I                     &#65506;&#65416;&#65426;                     . There was near 100% conversion of ammonium to nitrite over an 8&#65506;&#65408;&#65424;day growth period. No loss of I                     &#65506;&#65416;&#65426;                     or production of IO                     3                     &#65506;&#65416;&#65426;                     was detected in cultures where I                     &#65506;&#65416;&#65426;                     was added, indicating that                     N. maritimus                     is unable to drive I                     &#65506;&#65416;&#65426;                     oxidation under the tested conditions. This contrasts with previous observations of I                     &#65506;&#65416;&#65426;                     oxidation by ammonium oxidising bacteria (AOB). We explore whether differences between the metabolism of AOA and AOB could explain their differing actions on I                     &#65506;&#65416;&#65426;                     .                     N. maritimus                     cultures grown with the equivalent IO                     3                     &#65506;&#65416;&#65426;                     concentrations also showed no reduction in [IO                     3                     &#65506;&#65416;&#65426;                     ]. In addition, the growth of the                     N. maritimus                     culture was unaffected by inorganic iodine concentrations over 1000 times higher than in ambient seawater, suggesting a resilience to high iodine. These results suggest that AOA might have very little role in inorganic iodine turnover in the global ocean.                   &lt;/p</dct:abstract>
    <dc:title>The Ammonia Oxidising Archaeon Nitrosopumilus maritimus Does Not Alter Iodine Oxidation State in Oxic Seawater</dc:title>
    <dc:identifier>10.1111/1758-2229.70168</dc:identifier>
    <dct:references>https://doi.org/10.1111/1758-2229.70168</dct:references>
    <dct:relation>852993</dct:relation>
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