Hyun Joo Lee, Yves Moussallam, Estelle Rose-Koga, Laurette Piani, Johan Villeneuve, Nordine Bouden, Andrey Gurenko, Brian Monteleone, Glenn Gaetani

Secondary ion mass spectrometry (SIMS) has been used for isotope analysis of volatile components dissolved in silicate melts for decades. However, carbon in situ stable isotope analysis in natural silicate glasses has remained particularly challenging, with the few published attempts yielding high uncertainties. In this context, we characterized 31 reference silicate glasses of basaltic and basanitic compositions, which we then used as standards to calibrate δ13C-value analyses in silicate glasses by SIMS. This set of standards covers a wide range of CO2 concentrations (380 ppm − 12000 ppm) and δ13C values (−28.1±0.2 to −1.1±0.2 ‰, ±1). The standard sets were analyzed using large−geometry SIMS at two ion microprobe facilities to test reproducibility across different instrumental setups. The instrumental mass fractionation (IMF) varied widely with two different large−geometry SIMS instruments as well as with different analytical parameters such as field aperture size and primary beam intensity. We found that a precision better than ±1.1 ‰ (both average internal and external precision, ±1σ) could be achieved using a primary beam intensity of less than 5 nA, resulting in a final spot size of 10–20 µm, allowing precise analysis of δ13C in mineral−hosted melt inclusions. This level of precision was achieved at CO2 concentrations as low as 1800 ppm. This advance opens a wide range of new possibilities for the study of δ13C-value in mafic melts and their mantle sources. The reference glasses are now available at the CNRS–CRPG ion microprobe facility in Nancy, France and will be deposited at the Smithsonian National Museum of Natural History, Washington, USA where they will be freely available on loan to any researcher (catalogue numbers will be available for the final version of this manuscript).