Sulfur four isotope NanoSIMS analysis of comet-81P/Wild 2 dust in impact craters on aluminum foil C2037N from NASA’s Stardust mission
Article first published online: 26 APR 2012
DOI: 10.1111/j.1945-5100.2012.01362.x
© The Meteoritical Society, 2012
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How to Cite
HECK, P. R., HOPPE, P. and HUTH, J. (2012), Sulfur four isotope NanoSIMS analysis of comet-81P/Wild 2 dust in impact craters on aluminum foil C2037N from NASA’s Stardust mission. Meteoritics & Planetary Science, 47: 649–659. doi: 10.1111/j.1945-5100.2012.01362.x
Publication History
- Issue published online: 26 APR 2012
- Article first published online: 26 APR 2012
- (Received 28 November 2011; revision accepted 27 March 2012)
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Abstract– We present NanoSIMS four-isotope S analyses of 24 comet Wild 2 dust impact residues in craters on aluminum foil C2037N returned by NASA’s Stardust mission. Except for one sample, all impact residues have normal S isotopic compositions within 2σ uncertainties of at least two S isotope ratios. This implies that most S-rich Wild 2 dust impactors formed in the solar system. Instrumental isotope fractionation due to sample topography is the main contribution to our analytical uncertainty. One impact crater residue shows small anomalies of δ33S = −57 ± 17‰, and δ34S = −41 ± 17‰ (1σ uncertainties). Although this could be simply a statistical outlier or the fingerprint of a chemical isotope fractionation it is also possible that the observed anomaly results from the mixture of a cometary FeS particle with a small (150 nm diam.) presolar FeS supernova grain. This would translate into a presolar sulfide abundance of approximately 200 ppm.

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