<?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. H. Fletcher</dc:contributor>
  <dc:contributor>M. Field</dc:contributor>
  <dc:contributor>C.L. Conger</dc:contributor>
  <dc:contributor>C. Bochicchio</dc:contributor>
  <dc:creator>M.S. Engels</dc:creator>
  <dc:date>2008</dc:date>
  <dc:description>Twelve cores from the protected reef-flat of Molokai revealed that carbonate sediment accumulation, ranging from 3 mm year-1 to less than 1 mm year-1, ended on average 2,500 years ago. Modern sediment is present as a mobile surface veneer but is not trapped within the reef framework. This finding is consistent with the arrest of deposition at the end of the mid-Holocene highstand, known locally as the "Kapapa Stand of the Sea," ???2 m above the present datum ca. 3,500 years ago in the main Hawaiian Islands. Subsequent erosion, non-deposition, and/or a lack of rigid binding were probable factors leading to the lack of reef-flat accumulation during the late Holocene sea-level fall. Given anticipated climate changes, increased sedimentation of reef-flat environments is to be expected as a consequence of higher sea level. ?? 2008 Springer-Verlag.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s00338-008-0410-7</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Demise of reef-flat carbonate accumulation with late Holocene sea-level fall: Evidence from Molokai, Hawaii</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>