<?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:creator>Tyler B. Coplen</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Moseley &lt;/span&gt;&lt;i&gt;et al&lt;/i&gt;&lt;span&gt;.’s (Reports, 8 January 2016, p. 165) preferred-Termination-II age is subjective, as evidenced by variation in their Termination-II ages of 2500 years per meter. Termination-II-age bias decreases to zero at ~1.5 meters below the present-day water table, if one assumes linear variation with core-sample height. Maintaining the required gradient of thorium isotope &lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th over 3.6 meters for 1000 years, much less 10,000 years, seems exceedingly unlikely.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.aaf8074</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Science</dc:publisher>
  <dc:title>Comment on “Reconciliation of the Devils Hole climate record with orbital forcing”</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>