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Updated: Nov 9, 2025

Sampling and Pretreatment of Tooth Enamel Carbonate for Stable Carbon and Oxygen Isotope Analysis
Published on: August 15, 2018
New Ag3 PO4 comparison material for stable oxygen isotope analysis
Andrea Watzinger1, Katharina Schott1, Rebecca Hood-Nowotny1
1Institute of Soil Research, Department of Forest and Soil Sciences, University of Natural Resources and Life Sciences Vienna, Konrad-Lorenz-Straße 24, Tulln, 3430, Austria.
Rationale:
A silver phosphate reference material (Ag3 PO4 ) for the measurement of stable oxygen isotope compositions is much needed; however, it is not available from the authorities distributing reference materials. This study aims to fill this gap by calibrating a new Ag3 PO4 stable isotope comparison material produced by the University of Natural Resources and Life Sciences (BOKU).
Methods:
Aliquots of Ag3 PO4 were distributed to four laboratories who frequently measure the δ18 O value in Ag3 PO4 ; the University of Natural Resources and Life Sciences (BOKU), the University of Western Australia (UWA), the University of Helsinki (UH), and the Helmholtz Centre for Environmental Research (UFZ). The instruments used to perform the measurements were high-temperature conversion elemental analysers coupled with continuous flow isotope ratio mass spectrometers. The working gas δ18 O value was set to 0‰ and the normalization was done by a three-point linear regression using the reference materials IAEA-601, IAEA-602, and NBS127.
Results:
The mean δ18 O value of the new BOKU Ag3 PO4 comparison material on the VSMOW-SLAP scale is 13.71‰ and the combined uncertainty is estimated as ±0.34‰. This estimated uncertainty is within the range typical for comparison materials of phosphates and sulphates. Consistent results from the different laboratories probably derived from similar instrumentation, and use of the same reference materials and normalization procedure. The matrix effect of the different reference materials used in this study was deemed negligible.
Conclusions:
The BOKU Ag3 PO4 can be used as an alternative comparison material for stable oxygen isotope analysis and is available for stable isotope research laboratories to facilitate calibration.
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