<?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>Cristiano Lana</dc:contributor>
  <dc:contributor>Ricardo Scholz</dc:contributor>
  <dc:contributor>Ian Buick</dc:contributor>
  <dc:contributor>Sandra K. Kamo</dc:contributor>
  <dc:contributor>Nick M.W. Roberts</dc:contributor>
  <dc:contributor>Axel Gerdes</dc:contributor>
  <dc:contributor>Michael Wiedenbeck</dc:contributor>
  <dc:contributor>Blair Schoene</dc:contributor>
  <dc:contributor>Francisco E. Apen</dc:contributor>
  <dc:contributor>Sean Patrick Gaynor</dc:contributor>
  <dc:creator>Marco Silva</dc:creator>
  <dc:date>2025</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Determining absolute ages of carbonate diagenesis, faulting, fossil formation, speleothem growth, carbonate-hosted hydrocarbon deposits, vein mineralisation and hydrothermal alteration has become increasingly accessible through LA-ICP-MS U-Pb dating of calcite, complementing traditional isotope dilution methods still applicable to certain materials (e.g., speleothems via micro-drilling). However, well-calibrated reference materials for LA-ICP-MS calcite geochronology remain scarce. Here, we characterise the Rio Maior calcite, designated ‘RioM-1’, as a potential reference material for U-Pb dating by LA-ICP-MS. Fragments (0.1 to 1 cm&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;) from a single scalenohedral crystal were analysed by ID-TIMS (U-Pb), LA-ICP-MS (U-Pb and&amp;nbsp;&lt;/span&gt;&lt;sup&gt;87&lt;/sup&gt;&lt;span&gt;Sr/&lt;/span&gt;&lt;sup&gt;86&lt;/sup&gt;&lt;span&gt;Sr), and SIMS (O isotopes). RioM-1 displays high U mass fraction and low, though variable, proportions of common Pb. Combined ID-TIMS analyses from two independent laboratories yielded a Tera-Wasserburg lower intercept date of 63.93 ± 0.11 Ma (2&lt;/span&gt;&lt;i&gt;s&lt;/i&gt;&lt;span&gt;, MSWD&amp;nbsp;=&amp;nbsp;1.3,&amp;nbsp;&lt;/span&gt;&lt;i&gt;n&lt;/i&gt;&lt;span&gt;&amp;nbsp;= 16). LA-ICP-MS U-Pb data from three independent laboratories are concordant with the TIMS age, producing a pooled date of 64.10 ± 0.12/1.2 Ma (2&lt;/span&gt;&lt;i&gt;s&lt;/i&gt;&lt;span&gt;, MSWD&amp;nbsp;=&amp;nbsp;7.7,&amp;nbsp;&lt;/span&gt;&lt;i&gt;n&lt;/i&gt;&lt;span&gt;&amp;nbsp;= 708) and an initial&amp;nbsp;&lt;/span&gt;&lt;sup&gt;207&lt;/sup&gt;&lt;span&gt;Pb/&lt;/span&gt;&lt;sup&gt;206&lt;/sup&gt;&lt;span&gt;Pb ratio of 0.85 ± 0.01. Other calcite reference materials, when normalised to RioM-1, yielded dates within uncertainty of their published values. SIMS measurements returned a mean&amp;nbsp;&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O/&lt;/span&gt;&lt;sup&gt;16&lt;/sup&gt;&lt;span&gt;O of 0.002044450 ± 181 (1&lt;/span&gt;&lt;i&gt;s&lt;/i&gt;&lt;span&gt;) and δ&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O&lt;/span&gt;&lt;sub&gt;SMOW&lt;/sub&gt;&lt;span&gt;&amp;nbsp;of 19.57 ± 0.92‰ (1&lt;/span&gt;&lt;i&gt;s&lt;/i&gt;&lt;span&gt;), while LA-ICP-MS strontium isotope measurement yielded a mean&amp;nbsp;&lt;/span&gt;&lt;sup&gt;87&lt;/sup&gt;&lt;span&gt;Sr/&lt;/span&gt;&lt;sup&gt;86&lt;/sup&gt;&lt;span&gt;Sr of 0.708177 ± 9 (2&lt;/span&gt;&lt;i&gt;s&lt;/i&gt;&lt;span&gt;).&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/ggr.70018</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>RioM-1: A new calcite reference material for U-Pb LA-ICP-MS geochronology</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>