<?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>Robert R. Seal, II</dc:contributor>
  <dc:contributor>Lauren T Reid</dc:contributor>
  <dc:contributor>James A Jordan</dc:contributor>
  <dc:contributor>Adam C. Mumford</dc:contributor>
  <dc:creator>Tyler B. Coplen</dc:creator>
  <dc:date>2024</dc:date>
  <dc:description>&lt;p&gt;Rationale&lt;/p&gt;&lt;p&gt;&lt;span&gt;Vein calcite in Devils Hole has been precipitating continuously in oxygen-isotope equilibrium at a constant temperature for over 500 000&amp;nbsp;years, providing an unmatched&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O paleoclimate time series. A substantial issue is that coeval calcite (based on matching&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O values) has uranium-series ages differing by 12 000&amp;nbsp;years.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;Methods&lt;/p&gt;&lt;p&gt;&lt;span&gt;An unparalleled high-accuracy&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O chronology series from continuously submerged calcite was used to correct the published uranium-series ages of non-continuously formed calcite in two cores, cyclically exposed by water-table decline during glacial–interglacial transitions. This method relies on the premise that the&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O values of coevally precipitated calcite are identical, allowing matching calcite&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O values to establish formation ages.&lt;/span&gt; &lt;/p&gt;&lt;p&gt;Results&lt;/p&gt;&lt;p&gt;&lt;span&gt;Exposed calcite can have apparent ages that are 12 000&amp;nbsp;years too young due to unrecognized uranium mobility and resulting mixed ages identified in over 50 mixed uranium-series ages from previous studies. Secondary uranium in fluids, sourced from the formation or dissolution of porous carbonate deposits (folia) with high uranium-238 (&lt;/span&gt;&lt;sup&gt;238&lt;/sup&gt;&lt;span&gt;U) concentrations, has migrated up to 10&amp;nbsp;mm into vein calcite.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;Conclusions &lt;/p&gt;&lt;p&gt;&lt;span&gt;The continuously submerged Devils Hole&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O chronology is not explained by orbital forcing. Rather, this chronology represents a regional climate record in the southern Great Basin of sea-surface-temperature (SST) variations off California, variations that preceded the last and penultimate deglaciations by 5000 to approximately 10 000&amp;nbsp;years. Temporal discrepancies between the continuously submerged Devils Hole chronology and other regional&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O records (e.g., the Leviathan chronology) can be explained by unrecognized cryptic, pernicious uranium mobility, leading to model estimations that may be thousands of years younger than actual ages. Consequently, paleo-moisture availability, water-table, and groundwater recharge models based on these mixed uranium-series ages are too young by as much as 12 000&amp;nbsp;years. The potential for post-formation uranium addition in subaerial cores and speleothems underscores the need for caution in uranium-series dating, highlighting&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O time-series comparisons as a method for identifying mixed ages.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/rcm.9926</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>Using stable oxygen isotope dual-inlet isotope-ratio mass spectrometry to elucidate uranium transport and mixed 230Th/U calcite formation ages at the seminal Devils Hole, Nevada, natural laboratory</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>