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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>D.M. Robbin</dc:contributor>
  <dc:contributor>E.A. Shinn</dc:contributor>
  <dc:creator>B. H. Lidz</dc:creator>
  <dc:date>1985</dc:date>
  <dc:description>Suggests a greater production of coralline sand (rather than slower Halimeda growth) results from a marked acceleration of bioerosion of abundant dead reefs in the area. -from Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:title>Holocene carbonate sedimentary petrology and facies accumulation, Looe Key National Marine Sanctuary, Florida.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>