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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-10-1143-2013</article-id>
<title-group>
<article-title>Effect of ocean acidification on the fatty acid composition of a natural plankton community</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Leu</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Daase</surname>
<given-names>M.</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>Schulz</surname>
<given-names>K. G.</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>Stuhr</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>Riebesell</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Norwegian Polar Institute, FRAM Centre, 9296 Tromsø, Norway</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Helmholtz Centre for Ocean Research Kiel (GEOMAR), 24105 Kiel, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: Alfred-Wegener-Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>02</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>2</issue>
<fpage>1143</fpage>
<lpage>1153</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 E. Leu 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/articles/10/1143/2013/bg-10-1143-2013.html">This article is available from https://bg.copernicus.org/articles/10/1143/2013/bg-10-1143-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/1143/2013/bg-10-1143-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/10/1143/2013/bg-10-1143-2013.pdf</self-uri>
<abstract>
<p>The effect of ocean acidification on the fatty acid composition of a natural
plankton community in the Arctic was studied in a large-scale mesocosm
experiment, carried out in Kongsfjorden (Svalbard, Norway) at 79&amp;deg; N. Nine mesocosms of ~50 m&lt;sup&gt;3&lt;/sup&gt; each were exposed to 8
different &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; levels (from natural background conditions to
~1420 μatm), yielding pH values (on the total scale)
from ~8.3 to 7.5. Inorganic nutrients were added on day 13.
The phytoplankton development during this 30-day experiment passed three
distinct phases: (1) prior to the addition of inorganic nutrients, (2) first
bloom after nutrient addition, and (3) second bloom after nutrient addition.
The fatty acid composition of the natural plankton community was analysed
and showed, in general, high percentages of polyunsaturated fatty acids
(PUFAs): 44–60% of total fatty acids. Positive correlations with
&lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; were found for most PUFAs during phases 2 and/or 3, with the
exception of 20:5n3 (eicosapentaenoic acid, EPA), an important diatom
marker. These correlations are probably linked to changes in taxonomic
composition in response to &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt;. While diatoms (together with
prasinophytes and haptophytes) increased during phase 3 mainly in the low
and intermediate &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; treatments, dinoflagellates were favoured by high
CO&lt;sub&gt;2&lt;/sub&gt; concentrations during the same time period. This is reflected in
the development of group-specific fatty acid trophic markers. No indications
were found for a generally detrimental effect of ocean acidification on the
planktonic food quality in terms of essential fatty acids.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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