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                <identifier>oai:data.mendeley.com/xfnfgb52wf.1</identifier>
                <datestamp>2021-06-30T15:03:30Z</datestamp>
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            <metadata><oai_dc:dc xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
    <dc:creator>maung thein, zin maung</dc:creator>
    <dc:title>Data for: Stable isotope analysis of the Gwebin mammalian fauna (late Pliocene, central Myanmar) and its implication to paleoenvironmental changes in late Neogene of central Myanmar</dc:title>
    <dc:publisher>Mendeley Data</dc:publisher>
    <dc:description>Isotopic composition of treated samples was measured on a Gasbench II coupled to a Finnigan Delta V Mass Spectrometer at the University of South Florida. The CO2 samples were run in continuous flow mode after reaction with 103% phosphoric acid (100% H3PO4 with excess P2O5) at 25 °C for 24 hours (McCrea, 1950). Seven replicate samples of Carrara Marble (an internal standard which has been assigned a value of δ13C=+2.01‰, δ18O=−1.79‰, based on analysis with respect to NBS-19, δ13C=+1.95‰, δ18O=−2.20‰) and NBS-18 carbonatite (13C=−5.04‰, δ18O=−23.05‰, NIST, 1992) were analyzed in each run of 60 samples. Standard deviation of replicate analyses for both isotope values was 0.15‰. Stable isotope data were reported in the conventional delta () notation for carbon (13C) and oxygen (18O) relative to V-PDB (Vienna-Pee Dee Belemnite, i.e., PDB expressed in terms of NBS-19): =[(R sample/R standard)−1]×1000‰, where R denotes 13C/12C or 18O/16O. The statistical analyses were carried out using PAST (version 3.20).</dc:description>
    <dc:subject>Statistics</dc:subject>
    <dc:subject>Stable Isotope</dc:subject>
    <dc:type>Dataset</dc:type>
    <dc:identifier>doi:10.17632/xfnfgb52wf.1</dc:identifier>
    <dc:identifier>oai:data.mendeley.com/xfnfgb52wf.1</dc:identifier>
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    <dc:date>2021-06-30T15:03:30Z</dc:date>
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