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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>Gretchen J. Swarr</dc:contributor>
  <dc:contributor>Konrad A. Hughen</dc:contributor>
  <dc:contributor>Ross J. Jones</dc:contributor>
  <dc:contributor>Scott Birdwhistell</dc:contributor>
  <dc:contributor>Kathryn Furby</dc:contributor>
  <dc:contributor>Sujata A. Murty</dc:contributor>
  <dc:contributor>Nancy G. Prouty</dc:contributor>
  <dc:contributor>Chun-Mao Tseng</dc:contributor>
  <dc:creator>Carl H. Lamborg</dc:creator>
  <dc:date>2013</dc:date>
  <dc:description>&lt;p id="sp0005"&gt;We have developed a technique that combines a high temperature quartz furnace with inductively coupled plasma-mass spectrometry for the determination of Hg stored in the annual CaCO&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;bands found in coral skeletons. Substantial matrix effects, presumably due to the discontinuous introduction of CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;to the gas stream, were corrected for by simultaneously supplying a stream of argon containing highly enriched elemental&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;202&lt;/sup&gt;Hg&lt;sup&gt;o&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;and observing peaks in the&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;200&lt;/sup&gt;Hg/&lt;sup&gt;202&lt;/sup&gt;Hg signal as the sample was decomposed. Primary signal calibration for Hg was achieved using gas injections from a saturated vapor standard. The absolute instrument detection limit was low (about 0.2&amp;nbsp;fmol), with a practical limit of detection (3&lt;i&gt;σ&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;of blanks) of 2&amp;nbsp;fmol. Reproducibility of samples was (RSD) 15–27%.&lt;/p&gt;&lt;p id="sp0010"&gt;We applied this method to the determination of Hg concentrations in two colonies of&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Diploria labyrinthiformis&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;collected from Castle Harbour, Bermuda, at a site about to be buried under the municipal waste landfill. The temporal reconstructions of Castle Harbour seawater Hg concentrations implied by the coral record show a decline throughout the period of record (1949–2008). The coral archived no apparent signal associated with waste disposal practices in the Harbour (bulk waste land-filling or, since 1994, disposal of waste incinerator ash), and mercury concentrations in the coral did not correlate to growth rate as assessed by linear extension. There was, however, a large and nearly exponential decrease in apparent Hg concentration in the Harbour which circumstantially implicates the dredging and/or landfilling operations associated with the construction of the airport on St. David’s Island.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.gca.2013.01.026</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Determination of low-level mercury in coralline aragonite by calcination-isotope dilution-inductively coupled plasma-mass spectrometry and its application to Diploria specimens from Castle Harbour, Bermuda</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>