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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Janet K. Thompson</dc:contributor>
  <dc:contributor>James E. Cloern</dc:contributor>
  <dc:contributor>Gerard Thouzeau</dc:contributor>
  <dc:creator>Laurent Chauvaud</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>&lt;p&gt;Respiration and calcium carbonate production by the invasive Asian clam, &lt;i&gt;Potamocorbula amurensis&lt;/i&gt;, were calculated to assess their importance as CO&lt;sub&gt;2&lt;/sub&gt; sources in northern San Francisco Bay. Production, calculated using monthly population density and size structure measured at three sites over 7 yr and a shell length/CaCO&lt;sub&gt;3&lt;/sub&gt; conversion factor, averaged 221(±184)g CaCO&lt;sub&gt;3&lt;/sub&gt; m&lt;sup&gt;−2&lt;/sup&gt;yr&lt;sup&gt;−1&lt;/sup&gt;. Net calcium carbonate production by this exotic bivalve releases CO&lt;sub&gt;2&lt;/sub&gt; at a mean rate of 18(±17)g C m&lt;sup&gt;−2&lt;/sup&gt;yr&lt;sup&gt;−1&lt;/sup&gt;. Respiration by &lt;i&gt;P. amurensis&lt;/i&gt;, estimated from secondary production, releases additional CO&lt;sub&gt;2&lt;/sub&gt; at a mean rate of 37(±34)g C m&lt;sup&gt;−2&lt;/sup&gt;yr&lt;sup&gt;−1&lt;/sup&gt;. Therefore, total net CO&lt;sub&gt;2&lt;/sub&gt; production by &lt;i&gt;P. amurensis&lt;/i&gt; averages 55(±51)g C m&lt;sup&gt;−2&lt;/sup&gt;yr&lt;sup&gt;−1&lt;/sup&gt; in an estuarine domain where net primary production consumes only 20g inorganic C m&lt;sup&gt;−2&lt;/sup&gt;yr&lt;sup&gt;−1&lt;/sup&gt;. CO&lt;sub&gt;2&lt;/sub&gt; production by &lt;i&gt;P. amurensis&lt;/i&gt; in northern San Francisco Bay is an underestimate of the total CO&lt;sub&gt;2&lt;/sub&gt; supply from the calcified zoobenthic communities of San Francisco Bay, and results from other studies have suggested that this rate is not unusual for temperate estuaries. Global extrapolation yields a gross CO&lt;sub&gt;2&lt;/sub&gt; production rate in the world's estuaries of 1x10&lt;sup&gt;14&lt;/sup&gt;g C yr&lt;sup&gt;−1&lt;/sup&gt;, which suggests that calcified benthic organisms in estuaries generate CO&lt;sub&gt;2&lt;/sub&gt; equal in magnitude to the CO&lt;sub&gt;2&lt;/sub&gt; emissions from the world's lakes or from planetary volcanism (the net source is determined by the highly variable rate of CO&lt;sub&gt;2&lt;/sub&gt; consumption by carbonate dissolution). This biogenic CO&lt;sub&gt;2&lt;/sub&gt; source is increasing because of the continuing global translocation of mollusks and their successful colonization of new habitats.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.4319/lo.2003.48.6.2086</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Association for the Sciences of Limnology and Oceanography</dc:publisher>
  <dc:title>Clams as CO2 generators: The Potamocorbula amurensis example in San Francisco Bay</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>