The Cameca 1280-HR large geometry SIMS instrument is a highly versatile analytical tool which can support a broad range of geochemical applications.Research using the Potsdam 1280 instrument focuses primarily on isotope ratio determinations in geomaterials.Optimized measurement protocols have already been established forδ18O determinations in zircon,and we are also working towards routine oxygen isotope determinations for quartz,calcite,mica,apatite and titanite.The primary challenge in developing such measurement systems are the identification and characterization of suitable reference materials(RMs),and this is made particularly challenging due to the matrix dependent ion yields of the SIMS ion source.Here we wish to report our progress towards establishing new analytical protocols for the determination ofδ13C in both diamond and moissanite.In the case of diamond,our facility possesses three natural RMs with which we are able to produce data with a typical analytical repeatability of~0.15‰(1sd).An inter-comparison of our three diamond RMs demonstrates an overall data quality of better than 0.5‰in terms of systematic offset between the various materials characterized using gas source mass spectrometry(Palot et al.,2012).A single suchδ13C determination in diamond requires 80 s of data acquisition and involves a test portion mass of~400 pgof material.In-house diamond reference materials forδ15N calibration allow us to measure this isotopic system to a total analytical uncertainty of±1.6‰(1sd)at nitrogen concentrations reaching down to 250μg/g.Due to the relatively low abundance of nitrogen in diamonds,such isotope ratio determinations require around 9 minutes of data collection.With respect toδ13C determinations in moissanite,we use a kimberlitic Si C as calibrant(Mathez et al.,1995),on which we achieve a repeatability of~0.2‰(1sd)on a~350 pg test portion mass.Total data acquisition time for such measurements is 80 s.We are currently in the process of developing a second moissanite RM based on a synthetic,coarse-grained powder.We will also investigate this new material for itsδ30Si characteristics. The Cameca 1280-HR large geometry SIMS instrument is a highly versatile analytical tool which can support a broad range of geochemical applications. Research using the Potsdam 1280 instrument study on isotope ratio determinations in geomaterials. Optimized measurement protocols have already been established for δ18O determinations in zircon, and we are also working towards routine oxygen isotope determinations for quartz, calcite, mica, apatite and titanite. The primary challenge in developing such measurement systems are the identification and characterization of suitable reference materials (RMs), and this is made challenging due to the matrix dependent ion yields of the SIMS ion source. Here we wish to report our progress to establishing new analytical protocols for the determination of δ13C in both diamond and moissanite. In the case of diamond, our facility possesses three natural RMs with which we are able to produce data with a typical analytical repeatability of ~ 0.15 ‰ (1 sd). An inter-comparison of our three diamond RMs demonstrates an overall data quality of better than 0.5 ‰ in terms of systematic offset between the various materials proper using gas source mass spectrometry (Palot et al., 2012) . A single such δ13C determination in diamond requires 80 s of data acquisition and involves a test portion mass of ~ 400 pgof material.-House diamond reference materials for δ15N calibration allow us to measure this isotopic system to a total analytical uncertainty of ± 1.6 ‰ ( 1sd) at nitrogen concentrations reaching down to 250 μg / g. Due to the relatively low abundance of nitrogen in diamonds, such isotope ratio determinations require around 9 minutes of data collection. Wth respect to δ13C determinations in moissanite, we use a kimberlitic Si C calibrant (Mathez et al., 1995), on which we achieve a repeatability of ~ 0.2 ‰ (1sd) on a ~ 350 pg test portion mass. Total data acquisition time for such measurements is 80 s.We are currently in the process of developing a second moissanite RM based on a synthetic, coarse-grained powder. We will also investigate this new material for its δ30Si characteristics.