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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-8593-2011</article-id>
<title-group>
<article-title>Quantification of the carbonaceous matter origin in submicron marine aerosol by &lt;sup&gt;13&lt;/sup&gt;C and &lt;sup&gt;14&lt;/sup&gt;C isotope analysis</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ceburnis</surname>
<given-names>D.</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>Garbaras</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>Szidat</surname>
<given-names>S.</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>Rinaldi</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fahrni</surname>
<given-names>S.</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>Perron</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wacker</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Leinert</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Remeikis</surname>
<given-names>V.</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>Facchini</surname>
<given-names>M. C.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Prevot</surname>
<given-names>A. S. H.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jennings</surname>
<given-names>S. 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>Ramonet</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>O&apos;Dowd</surname>
<given-names>C. D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Physics and Centre for Climate {&amp;} Air Pollution Studies, Ryan Institute, National University of Ireland, Galway, University Road, Galway, Ireland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Center for Physical Sciences and Technology, Institute of Physics, Vilnius, Lithuania</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Chemistry and Biochemistry &amp; Oeschger Centre for Climate Change Research, University of Berne, Switzerland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute of Atmospheric Sciences and Climate, National Research Council, Bologna, Italy</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Laboratory of Atmospheric Chemistry, Paul Scherrer Institut, Villigen, Switzerland</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Laboratory of Ion Beam Physics, Swiss Federal Institute of Technology â€“ ETH, Zurich, Switzerland</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Environmental Protection Agency of Ireland, Dublin, Ireland</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Laboratoire des Sciences du Climat et de l&apos;Environment (LSCE), Gif sur Yvette, France</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Department of Nuclear Physics, University of Lund, Sweden</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>08</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>16</issue>
<fpage>8593</fpage>
<lpage>8606</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/8593/2011/acp-11-8593-2011.html">This article is available from http://www.atmos-chem-phys.net/11/8593/2011/acp-11-8593-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/8593/2011/acp-11-8593-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/8593/2011/acp-11-8593-2011.pdf</self-uri>
<abstract>
<p>Dual carbon isotope analysis of marine aerosol samples has been performed
for the first time demonstrating a potential in organic matter apportionment
between three principal sources: marine, terrestrial (non-fossil) and fossil
fuel due to unique isotopic signatures. The results presented here,
utilising combinations of dual carbon isotope analysis, provides conclusive
evidence of a dominant biogenic organic fraction to organic aerosol over
biologically active oceans. In particular, the NE Atlantic, which is also
subjected to notable anthropogenic influences via pollution transport
processes, was found to contain 80 % organic aerosol matter of biogenic
origin directly linked to plankton emissions. The remaining carbonaceous
aerosol was of terrestrial origin. By contrast, for polluted air advected
out from Europe into the NE Atlantic, the source apportionment is 30 %
marine biogenic, 40 % fossil fuel, and 30 % continental non-fossil fuel.
The dominant marine organic aerosol source in the atmosphere has significant
implications for climate change feedback processes.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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