Adapting automated instrumentation for high-throughput calcium isotope measurements by multi-collector inductively coupled plasma mass spectrometry.

RATIONALE: Large, efficiently generated datasets of calcium isotope ratios offer tremendous utility in an increasing number of scientific disciplines. Modern analytical capabilities in mass spectrometry present unique challenges to previously established sample preparation techniques, the extent of which must be thoroughly examined before these data are interpreted and reported. This study addresses key methodological challenges in the determination of calcium isotopes using state-of-the-art, commercially available instruments. METHODS: Automated ion chromatography was used to isolate calcium from carbonate- and seawater-like samples prior to analysis by multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). A new, membrane-bearing desolvator (Apex-Ω) is implemented and achieves enhanced sensitivity, yet necessitates an update to established sample preparation techniques due to previously unobserved matrix effects. Performance of this method was assessed through analyses of multiple standard reference materials (SRM 915b, USGS EN-1, and seawater) and several in-house standards using a Neptune MC-ICP-MS instrument. RESULTS: The enhanced sensitivity afforded by the Apex-Ω also yields pronounced matrix effects during mass spectrometry, resulting specifically from heightened sample Na and Sr content and deviations in sample [Ca] from their bracketing standards. While the latter can be addressed by a concentration correction, the first two matrix effects are mitigated using a modified chromatography technique that implements unique rinsing protocols. CONCLUSIONS: This precise (0.14‰ 2σ), high-throughput method is very reproducible for small sample amounts and, at optimal efficiency, can generate approximately 140 sample δ44/40 Ca values per week with 5 h of in-person effort per day. Documented matrix effects are successfully mitigated through corrections and modified chromatographic techniques. Additionally, this method may be permuted to accommodate most major cations.

Sulfur isotope analysis of microcrystalline iron sulfides using secondary ion mass spectrometry imaging: Extracting local paleo-environmental information from modern and ancient sediments.

RATIONALE: Sulfur isotope ratio measurements of bulk sulfide from marine sediments have often been used to reconstruct environmental conditions associated with their formation. In situ microscale spot analyses by secondary ion mass spectrometry (SIMS) and laser ablation multiple-collector inductively coupled plasma mass spectrometry (LA-MC-ICP-MS) have been utilized for the same purpose. However, these techniques are often not suitable for studying small (≤10 µm) grains or for detecting intra-grain variability. METHODS: Here, we present a method for the physical extraction (using lithium polytungstate heavy liquid) and subsequent sulfur isotope analysis (using SIMS; CAMECA IMS 7f-GEO) of microcrystalline iron sulfides. SIMS sulfur isotope ratio measurements were made via Cs+ bombardment of raster squares with sides of 20-130 µm, using an electron multiplier (EM) detector to collect counts of 32 S- and 34 S- for each pixel (128 × 128 pixel grids) for between 20 and 960 cycles. RESULTS: The extraction procedure did not discernibly alter pyrite grain-size distributions. The apparent inter-grain variability in 34 S/32 S in 1-4 µm-sized pyrite and marcasite fragments from isotopically homogeneous hydrothermal crystals was ~ ±2‰ (1σ), comparable with the standard error of the mean for individual measurements (≤ ±2‰, 1σ). In contrast, grain-specific 34 S/32 S ratios in modern and ancient sedimentary pyrites and marcasites can have inter- and intra-grain variability >60‰. The distributions of intra-sample isotopic variability are consistent with bulk 34 S/32 S values. CONCLUSIONS: SIMS analyses of isolated iron sulfide grains yielded distributions that are isotopically representative of bulk 34 S/32 S values. Populations of iron sulfide grains from sedimentary samples record the evolution of the S-isotopic composition of pore water sulfide in their S-isotopic compositions. These data allow past local environmental conditions to be inferred.

Variability in the Raman Spectrum of Unpolished Growth and Fracture Surfaces of Pyrite Due to Laser Heating and Crystal Orientation.

Two probable causes of variability in the Raman spectrum of unpolished pyrite are well recognized, in principle, but not always in practice, namely: (1) downshifting of band positions due to laser heating; and (2) variations in the ratios of band intensities due to crystallographic orientation of the sample with respect to the laser's dominant polarization plane. The aims of this paper are to determine whether these variations can be used to acquire additional information about pyrites. Here, using laser Raman microprobe analysis of natural, unpolished pyrite samples, we investigate the magnitude of downshifting of band positions associated with laser heating of different sizes of pyrite grains. We demonstrate that the magnitude of this effect can be large (up to ∼10 cm-1), negatively proportional to grain size, of greater magnitude than the effect typically attributable to natural intersample differences in trace element (TE) solid solution, and of similar magnitude among bands. Through Raman analysis of naturally occurring faces on pyrite samples at various angles of rotation, we also demonstrate that the three most common faces on pyrite can be distinguished by the ratio of the intensities of the dominant bands. We conclude that for unpolished samples, laser Raman microprobe analysis is most effective as a means of identifying pyrite, and the presence of solid solution therein, when laser power is low enough to avoid substantial heating. Once pyrite has been identified, higher laser powers can be used to produce spectra whose ratios of band intensities indicate the face or crystallographic plane being irradiated.