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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>
</journal-title-group>
<issn pub-type="epub">1810-6285</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bgd-9-4979-2012</article-id>
<title-group>
<article-title>Influence of CO&lt;sub&gt;2&lt;/sub&gt; and nitrogen limitation on the coccolith volume of &lt;i&gt;Emiliania huxleyi&lt;/i&gt; (Haptophyta)</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Müller</surname>
<given-names>M. 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>Beaufort</surname>
<given-names>L.</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>Bernard</surname>
<given-names>O.</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>Pedrotti</surname>
<given-names>M. L.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Talec</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sciandra</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute for Marine and Antarctic Studies (IMAS), Private Bag 129, Hobart, TAS 7001, Australia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CNRS/Université Aix-Marseille, CEREGE, 13545 Aix-en-Provence, Cedex 4, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>INRIA (French National Institute for Research in Computer Science and Automatic Control), BIOCORE, 2004 Route des Lucioles, 06902 Sophia-Antipolis, France</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>UPMC Univ. Paris 06, UMR7093, LOV, Observatoire océanologique, 06234 Villefranche/mer, France</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>CNRS, UMR7093, LOV, Observatoire océanologique, 06234 Villefranche/mer, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>9</volume>
<issue>4</issue>
<fpage>4979</fpage>
<lpage>5010</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<self-uri xlink:href="http://www.biogeosciences-discuss.net/9/4979/2012/bgd-9-4979-2012.pdf">The full text article is available as a PDF file from http://www.biogeosciences-discuss.net/9/4979/2012/bgd-9-4979-2012.pdf</self-uri>
<abstract>
<p>Coccolithophores, a key phytoplankton group, are one of the best studied
organisms with regard to the response to ocean acidification/carbonation. The
biogenic production of calcareous coccoliths has made coccolithophores a
promising group for paleoceanographic research aiming to reconstruct past
environmental conditions. Recently, geochemical and morphological analyses of
fossil coccoliths have gained increased interest in regard to changes in
seawater carbonate chemistry. The cosmopolitan coccolithophore
&lt;i&gt;Emiliania huxleyi&lt;/i&gt; (Lohm.) Hay and Mohler was cultured over a range
of &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; levels in controlled laboratory experiments under nutrient replete and
nitrogen limited conditions. Measurements of photosynthetic activity and
calcification revealed, as previously published, an increase in organic
carbon production and a moderate decrease in calcification from ambient to
elevated &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt;. The enhancement in particulate organic carbon production was
accompanied by an increase in cell diameter. Coccolith volume was best
correlated with the coccosphere/cell diameter and no significant correlation
was found between coccolith volume and particulate inorganic carbon
production rate. The conducted experiments revealed that the coccolith volume
of &lt;i&gt;E. huxleyi&lt;/i&gt; is variable with aquatic CO&lt;sub&gt;2&lt;/sub&gt; concentration within the tested
range but appears to be a primary function of the coccosphere/cell diameter
both under nitrogen limited and nutrient replete conditions. Comparing
coccolith morphological and geometrical parameters like volume, mass and size
to physiological parameters under controlled laboratory conditions is an
important step to understand variations in fossil coccolith geometry.</p>
</abstract>
<counts><page-count count="32"/></counts>
</article-meta>
</front>
<body/>
<back>
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