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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BGD</journal-id>
<journal-title-group>
<journal-title>Biogeosciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">BGD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1810-6285</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bgd-10-17275-2013</article-id>
<title-group>
<article-title>Plankton community response to Saharan dust fertilization in subtropical waters off the Canary Islands</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Franchy</surname>
<given-names>G.</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>Ojeda</surname>
<given-names>A.</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>López-Cancio</surname>
<given-names>J.</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>Hernández-León</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Instituto de Oceanografía y Cambio Global, Universidad de Las Palmas de Gran Canaria, Canary Islands, Spain</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Instituto Canario de Ciencias Marinas, Telde, Canary Islands, Spain</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Grupo de Estudios Atmosféricos, Departamento de Ingenierí a de Procesos, Universidad de Las Palmas de Gran Canaria, Canary Islands, Spain</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>11</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>11</issue>
<fpage>17275</fpage>
<lpage>17307</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 G. Franchy et al.</copyright-statement>
<copyright-year>2013</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/preprints/10/17275/2013/bgd-10-17275-2013.html">This article is available from https://bg.copernicus.org/preprints/10/17275/2013/bgd-10-17275-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/preprints/10/17275/2013/bgd-10-17275-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/preprints/10/17275/2013/bgd-10-17275-2013.pdf</self-uri>
<abstract>
<p>The plankton community response to natural fertilization caused by the Saharan dust was studied in
  the Canary Islands waters during winter–spring 2010. For this, a weekly sampling was carried out
  to characterize the pico-, nano- and microplankton communities. During this period several dust
  events were identified from atmospheric suspended matter and metal composition.  Temperatures
  above 19 °C in the mixed layer, high stratification and a very low concentration
  of chlorophyll &lt;i&gt;a&lt;/i&gt;, indicated the absence of the characteristic late winter bloom during this
  year. However, relatively high primary production rates were measured, probably fuelled by
  nutrient release from the deposited atmospheric dust. In fact, this winter–spring was one of the
  most intense dust periods during the last years and Saharan dust events were identified in every
  month. The effect of the Saharan dust over the plankton community mainly consisted in the
  enhancement of primary producers, mostly diatoms, and the increase of the mesozooplankton stock,
  whereas cyanobacteria and autotrophic picoeukaryotes were negatively affected. These results
  suggest that the Saharan dust deposition would be partly fuelling the primary production in these
  oligotrophic waters of the northeast Atlantic, and could be especially significant during
  stratified periods, when the atmospheric dust would be the most important nutrient source.</p>
</abstract>
<counts><page-count count="33"/></counts>
</article-meta>
</front>
<body/>
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