<?xml version='1.0' encoding='utf-8'?>
<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>C. Langdon</dc:contributor>
  <dc:contributor>B. Loose</dc:contributor>
  <dc:contributor>Kimberly K. Yates</dc:contributor>
  <dc:contributor>J. Corredor</dc:contributor>
  <dc:creator>W. R. McGillis</dc:creator>
  <dc:date>2011</dc:date>
  <dc:description>&lt;p&gt;&lt;span id="_mce_caret" data-mce-bogus="1" data-mce-type="format-caret"&gt;&lt;span class="paraNumber"&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span&gt;The metabolism of Cayo Enrique Reef, Puerto Rico, was studied using&amp;nbsp;&lt;/span&gt;&lt;i&gt;in situ&lt;/i&gt;&lt;span&gt;&amp;nbsp;methods during March 2009. Benthic O&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;fluxes were used to calculate net community production using both the boundary layer gradient and enclosure techniques. The boundary layer O&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;gradient and the drag coefficients were used to calculate productivity ranging from −12.3 to 13.7 mmol O&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;m&lt;/span&gt;&lt;sup&gt;−2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;h&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;. Productivity measurements from the enclosure method ranged from −11.0 to 12.9 mmol O&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;m&lt;/span&gt;&lt;sup&gt;−2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;h&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;. During the study, the mean hourly difference between the methods was 0.65 mmol O&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;m&lt;/span&gt;&lt;sup&gt;−2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;h&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(r&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;= 0.92), resulting in well‐reconciled estimates of net community production between the boundary layer (−33.1 mmol m&lt;/span&gt;&lt;sup&gt;−2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;d&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;) and enclosure (−46.3 mmol m&lt;/span&gt;&lt;sup&gt;−2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;d&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;) techniques. The results of these independent approaches corroborate quantified rates of metabolism at Cayo Enrique Reef. Close agreement between methods demonstrates that boundary layer measurements can provide near real‐time assessments of coral reef health.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2010GL046179</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Productivity of a coral reef using boundary layer and enclosure methods</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>