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<front>
<journal-meta>
<journal-id journal-id-type="publisher">OS</journal-id>
<journal-title-group>
<journal-title>Ocean Science</journal-title>
<abbrev-journal-title abbrev-type="publisher">OS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ocean Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1812-0792</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/os-7-113-2011</article-id>
<title-group>
<article-title>Phytoplankton distribution and nitrogen dynamics in the southwest indian subtropical gyre and Southern Ocean waters</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Thomalla</surname>
<given-names>S. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Waldron</surname>
<given-names>H. N.</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>Lucas</surname>
<given-names>M. I.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Read</surname>
<given-names>J. F.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ansorge</surname>
<given-names>I. J.</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>Pakhomov</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Oceanography, University of Cape Town, Private Bag, Rondebosch, Cape Town 7701, South Africa</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Ocean Systems and Climate Group, CSIR, P.O. Box 320 Stellenbosch, 7599, South Africa</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Zoology, University of Cape Town, Private Bag, Rondebosch, Cape Town 7701, South Africa</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>National Oceanographic Centre (NOC), Southampton, SO143ZH, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Earth and Ocean Sciences, 6339 Stores Road, Univ. of British Columbia, Vancouver, BC, V6T 1Z4, Canada</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Department of Zoology, University of Fort Hare, Private Bag X1314, Alice 5700, South Africa</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>02</month>
<year>2011</year>
</pub-date>
<volume>7</volume>
<issue>1</issue>
<fpage>113</fpage>
<lpage>127</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 S. J. Thomalla et al.</copyright-statement>
<copyright-year>2011</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://os.copernicus.org/articles/7/113/2011/os-7-113-2011.html">This article is available from https://os.copernicus.org/articles/7/113/2011/os-7-113-2011.html</self-uri>
<self-uri xlink:href="https://os.copernicus.org/articles/7/113/2011/os-7-113-2011.pdf">The full text article is available as a PDF file from https://os.copernicus.org/articles/7/113/2011/os-7-113-2011.pdf</self-uri>
<abstract>
<p>During the 1999 Marion Island Oceanographic Survey (MIOS 4) in late austral
summer, a northbound and reciprocal southbound transect were taken along the
Southwest Indian and Madagascar Ridge, between the Prince Edward Islands and
31° S. The sections crossed a number of major fronts and smaller
mesoscale features and covered a wide productivity spectrum from subtropical
to subantarctic waters. Associated with the physical survey were measurements
of size fractionated chlorophyll, nutrients and nitrogen (NO&lt;sub&gt;3&lt;/sub&gt;, NH&lt;sub&gt;4&lt;/sub&gt;
and urea) uptake rates. Subtropical waters were characterised by low
chlorophyll concentrations (max = 0.27.3 mg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; dominated by
pico-phytoplankton cells (&gt; 81%) and very low f-ratios (&lt; 0.1), indicative
of productivity based almost entirely on recycled ammonium and urea.
Micro-phytoplankton growth was limited by the availability of NO&lt;sub&gt;3&lt;/sub&gt;
(&lt; 0.5 mmol m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; and Si(OH)&lt;sub&gt;4&lt;/sub&gt; (&lt; 1.5 mmol m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
 through strong vertical stratification preventing the upward
flux of nutrients into the euphotic zone. Biomass accumulation of small
cells was likely controlled by micro-zooplankton grazing. In subantarctic
waters, total chlorophyll concentrations increased (max = 0.74 mg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
relative to the subtropical waters and larger cells became more prevalent,
however smaller phytoplankton cells and low f-ratios (&lt; 0.14) still
dominated, despite sufficient NO&lt;sub&gt;3&lt;/sub&gt; availability. The results from this
study favour Si(OH)&lt;sub&gt;4&lt;/sub&gt; limitation, light-limited deep mixing and likely
Fe deficiency as the dominant mechanisms controlling significant new
production by micro-phytoplankton. The percentage of micro-phytoplankton
cells and rates of new production did however increase at oceanic frontal
regions (58.6% and 11.22%, respectively), and in the region of the
Prince Edward archipelago (61.4% and 14.16%, respectively). Here,
water column stabilization and local Fe-enrichment are thought to stimulate
phytoplankton growth rates. Open ocean regions such as these provide
important areas for local but significant particulate organic carbon export
and biological CO&lt;sub&gt;2&lt;/sub&gt; draw-down in an overall high nutrient low
chlorophyll Southern Ocean.</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
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