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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-10-6639-2013</article-id>
<title-group>
<article-title>Calcification intensity in planktonic Foraminifera reflects ambient conditions irrespective of environmental stress</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Weinkauf</surname>
<given-names>M. F. G.</given-names>
<ext-link>https://orcid.org/0000-0002-4640-9659</ext-link>
</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>Moller</surname>
<given-names>T.</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>Koch</surname>
<given-names>M. 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>Kučera</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0002-7817-9018</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Eberhard Karls Universität,  Mathematisch–Naturwissenschaftliche Fakultät, Fachbereich  Geowissenschaften, Hölderlinstraße 12, 72074 Tübingen, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>MARUM, Leobener Straße, 28359 Bremen, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Johann  Wolfgang Goethe-Universität, Institut für Geowissenschaften,  Facheinheit Paläontologie, Altenhöferallee 1, 60438  Frankfurt am Main, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>10</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>10</issue>
<fpage>6639</fpage>
<lpage>6655</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 M. F. G. Weinkauf 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/10/6639/2013/bg-10-6639-2013.html">This article is available from https://bg.copernicus.org/articles/10/6639/2013/bg-10-6639-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/6639/2013/bg-10-6639-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/10/6639/2013/bg-10-6639-2013.pdf</self-uri>
<abstract>
<p>Planktonic Foraminifera are important marine calcifiers,  and the ongoing change in the oceanic
  carbon system makes it essential to understand the influence of environmental factors on the
  biomineralization of their shells. The amount of calcite deposited by planktonic Foraminifera
  during calcification has been hypothesized to reflect a range of environmental factors. However,
  it has never been assessed whether their calcification only passively responds to the conditions
  of the ambient seawater or whether it reflects changes in resource allocation due to physiological
  stress. To disentangle these two end-member scenarios, an experiment is required where the two
  processes are separated. A natural analogue to such an experiment occurred during the deposition
  of the Mediterranean sapropels, where large changes in surface water composition and
  stratification at the onset of the sapropel deposition were decoupled from local extinctions of
  planktonic Foraminifera species. We took advantage of this natural experiment and investigated the
  reaction of calcification intensity, expressed as mean area density (MAD), of four
  species of planktonic Foraminifera to changing conditions during the onset of Sapropel S5
  (126–121 ka) in a sediment core from the Levantine Basin. We observed a significant
  relationship between MAD and surface water properties, as reflected by stable isotopes
  in the calcite of Foraminifera shells, but we failed to observe any reaction of calcification
  intensity on ecological stress during times of decreasing abundance culminating in local
  extinction. The reaction of calcification intensity to surface water perturbation at the onset of
  the sapropel was observed only in surface-dwelling species, but all species calcified more
  strongly prior to the sapropel deposition and less strongly within the sapropel than at similar
  conditions during the present-day. These results indicate that the high-salinity environment of
  the glacial Mediterranean Sea prior to sapropel deposition induced a~more intense calcification,
  whereas the freshwater injection to the surface waters associated with sapropel deposition
  inhibited calcification. The results are robust to changes in carbonate preservation and
  collectively imply that changes in normalized shell weight in planktonic Foraminifera should
  reflect mainly abiotic forcing.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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