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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>Heiko Moossen</dc:contributor>
  <dc:contributor>Harro A.J. Meijer</dc:contributor>
  <dc:contributor>Tyler B. Coplen</dc:contributor>
  <dc:contributor>Anita T Aerts-Bijma</dc:contributor>
  <dc:contributor>Lauren T Reid</dc:contributor>
  <dc:contributor>Heiko Geilmann</dc:contributor>
  <dc:contributor>Jurgen Richter</dc:contributor>
  <dc:contributor>Michael Rothe</dc:contributor>
  <dc:contributor>Willi A. Brand</dc:contributor>
  <dc:contributor>Blaza Toman</dc:contributor>
  <dc:contributor>Jacqueline Benefield</dc:contributor>
  <dc:contributor>Jean-Francois Helie</dc:contributor>
  <dc:creator>Haiping Qi</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;h3 id="rcm9006-sec-0001-title" class="article-section__sub-title section1"&gt;Rationale&lt;/h3&gt;&lt;p&gt;The stable carbon isotopic (&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C) reference material (RM) LSVEC Li&lt;sub&gt;2&lt;/sub&gt;CO&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;has been found to be unsuitable for&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C standardization work because its&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C value increases with exposure to atmospheric CO&lt;sub&gt;2&lt;/sub&gt;. A new CaCO&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;RM, USGS44, has been prepared to alleviate this situation.&lt;/p&gt;&lt;h3 id="rcm9006-sec-0002-title" class="article-section__sub-title section1"&gt;Methods&lt;/h3&gt;&lt;p&gt;USGS44 was prepared from 8 kg of Merck high-purity CaCO&lt;sub&gt;3&lt;/sub&gt;. Two sets of&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C values of USGS44 were determined. The first set of values was determined by online combustion, continuous-flow (CF) isotope-ratio mass spectrometry (IRMS) of NBS 19 CaCO&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;(&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt; = +1.95 milliurey (mUr) exactly, where mUr = 0.001 = 1‰), and LSVEC Li&lt;sub&gt;2&lt;/sub&gt;CO&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;(&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt; = −46.6 mUr exactly), and normalized to the two-anchor&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB-LSVEC&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;isotope-delta scale. The second set of values was obtained by dual-inlet (DI)-IRMS of CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;evolved by reaction of H&lt;sub&gt;3&lt;/sub&gt;PO&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;with carbonates, corrected for cross contamination, and normalized to the single-anchor&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;scale.&lt;/p&gt;&lt;h3 id="rcm9006-sec-0003-title" class="article-section__sub-title section1"&gt;Results&lt;/h3&gt;&lt;p&gt;USGS44 is stable and isotopically homogeneous to within 0.02 mUr in 100-μg amounts. It has a&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB-LSVEC&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;value of −42.21 ± 0.05 mUr. Single-anchor&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;values of −42.08 ± 0.01 and −41.99 ± 0.02 mUr were determined by DI-IRMS with corrections for cross contamination.&lt;/p&gt;&lt;h3 id="rcm9006-sec-0004-title" class="article-section__sub-title section1"&gt;Conclusions&lt;/h3&gt;&lt;p&gt;The new high-purity, well-homogenized calcium carbonate isotopic reference material USGS44 is stable and has a&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB-LSVEC&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;value of −42.21 ± 0.05 mUr for both EA/IRMS and DI-IRMS measurements. As a carbonate relatively depleted in&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;C, it is intended for daily use as a secondary isotopic reference material to normalize stable carbon isotope delta measurements to the&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB-LSVEC&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;scale. It is useful in quantifying drift with time, determining mass-dependent isotopic fractionation (linearity correction), and adjusting isotope-ratio-scale contraction. Due to its fine grain size (smaller than 63 μm), it is not suitable as a&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;O reference material. A&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;VPDB-LSVEC&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;value of −29.99 ± 0.05 mUr was determined for NBS 22 oil.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/rcm.9006</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>USGS44, a new high-purity calcium carbonate reference material for δ13C measurements</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>