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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BG</journal-id>
<journal-title-group>
<journal-title>Biogeosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">BG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1726-4189</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bg-9-4707-2012</article-id>
<title-group>
<article-title>Simulating the effects of phosphorus limitation in the Mississippi and Atchafalaya River plumes</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Laurent</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fennel</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hetland</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>School of Environmental Science and Engineering, Sun Yat-Sen University, Guangzhou, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Oceanography, Texas A&amp;M University, College Station, TX, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>11</month>
<year>2012</year>
</pub-date>
<volume>9</volume>
<issue>11</issue>
<fpage>4707</fpage>
<lpage>4723</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 A. Laurent et al.</copyright-statement>
<copyright-year>2012</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/articles/9/4707/2012/bg-9-4707-2012.html">This article is available from https://bg.copernicus.org/articles/9/4707/2012/bg-9-4707-2012.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/9/4707/2012/bg-9-4707-2012.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/9/4707/2012/bg-9-4707-2012.pdf</self-uri>
<abstract>
<p>The continental shelf of the northern Gulf of Mexico receives high dissolved inorganic nitrogen and phosphorus loads from the
      Mississippi and Atchafalaya rivers. The nutrient load results in high primary production in the river plumes and contributes to
      the development of hypoxia on the Louisiana shelf in summer. While phytoplankton growth is considered to be typically
      nitrogen-limited in marine waters, phosphorus limitation has been observed in this region during periods of peak
      river discharge in spring and early summer. Here we investigate the presence, spatio-temporal distribution and implications of
      phosphorus limitation in the plume region using a circulation model of the northern Gulf of Mexico coupled to a multi-nutrient
      ecosystem model. Results from a 7-yr simulation (2001–2007) compare well with several sources of observations and suggest that phosphorus
      limitation develops every year between the Mississippi and Atchafalaya deltas. Model simulations show that phosphorus limitation
      results in a delay and westward shift of a fraction of river-stimulated primary production. The consequence is a reduced flux of
      particulate organic matter to the sediment near the Mississippi delta, but slightly enhanced fluxes
      west of Atchafalaya Bay. Simulations with altered river phosphate concentrations (±50%) show that
      significant variation in the spatial extent of phosphorus limitation  (±40% in July) results from
      changes in phosphate load.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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