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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>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1810-6285</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bg-2018-418</article-id>
<title-group>
<article-title>Surface transport of DOC acts as a trophic link among Mediterranean sub-basins</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Santinelli</surname>
<given-names>Chiara</given-names>
<ext-link>https://orcid.org/0000-0002-8921-275X</ext-link>
</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>Iacono</surname>
<given-names>Roberto</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>Napolitano</surname>
<given-names>Ernesto</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>Ribera d'Alcalá</surname>
<given-names>Maurizio</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CNR, Istituto di Biofisica, Pisa, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>ENEA, C. R. Casaccia, Rome, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Stazione Zoologica Anton Dohrn, Napoli, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>10</month>
<year>2018</year>
</pub-date>
<volume>2018</volume>
<fpage>1</fpage>
<lpage>18</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2018 Chiara Santinelli et al.</copyright-statement>
<copyright-year>2018</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/preprints/bg-2018-418/">This article is available from https://bg.copernicus.org/preprints/bg-2018-418/</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/preprints/bg-2018-418/bg-2018-418.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/preprints/bg-2018-418/bg-2018-418.pdf</self-uri>
<abstract>
<p>&lt;p&gt;Characterizing carbon cycling and redistribution in the ocean is an important issue for Mankind, because it may affect key ecosystem services, e.g., support to climate system and food provision. In this paper, using an integrated approach, we explore the impact of the surface circulation on carbon dynamics in the Western Mediterranean Sea, where strong inter-basin differences in primary production do exist. Detailed information on the surface circulation, derived from high-resolution model simulations, is combined with the analysis of accurate, repeated dissolved organic carbon (DOC) data. Our work indicates that the advection of the Atlantic Water acts as a trophic link between the Algerian Basin and the Tyrrhenian Sea, determining a flux of 8.8&amp;ndash;37.9&amp;thinsp;&amp;times;&amp;thinsp;10&lt;sup&gt;12&lt;/sup&gt;&amp;thinsp;g&amp;thinsp;DOC&amp;thinsp;yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt; into the basin. Thus, surface transport of DOC can redistribute chemical energy among regions with different trophic regimes. We hypothesize that this overlooked mechanism plays an important role also in the global ocean.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
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