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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-7-289-2010</article-id>
<title-group>
<article-title>Response of the temperate coral &lt;i&gt;Cladocora caespitosa&lt;/i&gt; to mid- and long-term exposure to &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; and temperature levels projected for the year 2100 AD</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rodolfo-Metalpa</surname>
<given-names>R.</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>Martin</surname>
<given-names>S.</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>Ferrier-Pagès</surname>
<given-names>C.</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>Gattuso</surname>
<given-names>J.-P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>International Atomic Energy Agency-Marine Environment Laboratories, 4 Quai Antoine Ier, 98000, Principality of Monaco</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>INSU-CNRS, Laboratoire d&apos;Océanographie de Villefranche, B.P. 28, 06234 Villefranche-sur-mer Cedex, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre Scientifique de Monaco, Principality of Monaco</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>UPMC University of Paris 06, Observatoire Océanologique de Villefranche, 06230 Villefranche-sur-mer, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>01</month>
<year>2010</year>
</pub-date>
<volume>7</volume>
<issue>1</issue>
<fpage>289</fpage>
<lpage>300</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 R. Rodolfo-Metalpa et al.</copyright-statement>
<copyright-year>2010</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/7/289/2010/bg-7-289-2010.html">This article is available from https://bg.copernicus.org/articles/7/289/2010/bg-7-289-2010.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/7/289/2010/bg-7-289-2010.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/7/289/2010/bg-7-289-2010.pdf</self-uri>
<abstract>
<p>Atmospheric CO&lt;sub&gt;2&lt;/sub&gt; partial pressure (&lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt;) is expected to
increase to 700 &amp;mu;atm or more by the end of the present century.
Anthropogenic CO&lt;sub&gt;2&lt;/sub&gt; is absorbed by the oceans, leading to
decreases in pH and the CaCO&lt;sub&gt;3&lt;/sub&gt; saturation state (Ω) of
the seawater. Elevated &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; was shown to drastically decrease
calcification rates in tropical zooxanthellate corals. Here we show,
using the Mediterranean zooxanthellate coral &lt;i&gt;Cladocora
caespitosa&lt;/i&gt;, that an increase in &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt;, in the range predicted
for 2100, does not reduce its calcification rate. Therefore, the
conventional belief that calcification rates will be affected by
ocean acidification may not be widespread in temperate corals.
Seasonal change in temperature is the predominant factor controlling
photosynthesis, respiration, calcification and symbiont density. An
increase in &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt;, alone or in combination with elevated
temperature, had no significant effect on photosynthesis,
photosynthetic efficiency and calcification. The lack of sensitivity
&lt;i&gt;C. caespitosa&lt;/i&gt; to elevated &lt;i&gt;p&lt;/i&gt;CO&lt;sub&gt;2&lt;/sub&gt; might be due to its
slow growth rates, which seem to be more dependent on temperature
than on the saturation state of calcium carbonate in the range
projected for the end of the century.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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