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dc.contributor.authorMatrajt, G.
dc.contributor.authorIto, M.
dc.contributor.authorWirick, S.
dc.contributor.authorMessenger, S.
dc.contributor.authorBrownlee, D. E.
dc.contributor.authorJoswiak, D.
dc.contributor.authorFlynn, G.
dc.contributor.authorSandford, S.
dc.contributor.authorSnead, C.
dc.contributor.authorWestphal, A.
dc.date.accessioned2021-02-12T22:30:39Z
dc.date.available2021-02-12T22:30:39Z
dc.date.issued2008-01-01
dc.identifier.citationMatrajt, G., Ito, M., Wirick, S., Messenger, S., Brownlee, D. E., Joswiak, D., ... & Westphal, A. (2008). Carbon investigation of two Stardust particles: A TEM, NanoSIMS, and XANES study. Meteoritics & Planetary Science, 43(1‐2), 315-334.
dc.identifier.issn1945-5100
dc.identifier.doi10.1111/j.1945-5100.2008.tb00625.x
dc.identifier.urihttp://hdl.handle.net/10150/656397
dc.description.abstractIn this work we present the results of a systematic search for cometary organics in 14 Stardust particles (particles from comet 81P/Wild 2, captured by NASAs Stardust mission) by TEM and multidisciplinary studies (XANES and NanoSIMS) of Febo and Ada, two of the organic-bearing particles identified. The combination of the three analytical techniques has established the presence of organic, cometary degrees C in both particles. Using energy-filtered and high-resolution imaging it was shown that the degrees C is amorphous and rare, given that it is found in grains less than or equal to 200 nm in size that are not abundant throughout the particles. The XANES maps and spectra of the carbonaceous areas identified with the TEM have shown that the carbonaceous material is organic due to the presence of carbonyl (C=O) functional groups and the overlapping of degrees C and N on the same grains. In addition, several different C-XANES spectra were obtained from the same particle, suggesting that there is diversity in the types of carbonaceous phases present in these particles, as well as a heterogeneous distribution of the carbonaceous phases within these particles. The C-XANES spectra obtained are different from C-XANES spectra of carbonaceous chondrites and IDPs. In the particle Febo we found five spots showing a pronounced enrichment in the isotope 15N (delta-15N from 420 to 639 +/- 20 to 70 ppm, 1-sigma) that were clearly associated with the C-rich regions. The carbonaceous material has approximately solar C and D/H isotopic compositions, and the bulk O isotopic composition was found to be delta-17O = -18 +/- 13 ppm and delta-18O = -37 +/- 12 ppm (1-sigma). In the particle Ada we found a C-rich phase with enrichments in the isotope 15N (delta-15N = 550 +/- 70 ppm, 1-sigma) and the isotope D (delta-D = 610 +/- 254 ppm, 1-sigma). The C isotopic composition at this phase is solar (delta-13C = -4 +/-29 ppm, 1 sigma). The bulk O isotopic composition of Ada was found to be delta-17O = 9 +/- 14.6 ppm and delta-18O = -7.3 +/- 8.1 ppm (2-sigma).
dc.language.isoen
dc.publisherThe Meteoritical Society
dc.relation.urlhttps://meteoritical.org/
dc.rightsCopyright © The Meteoritical Society
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectNanoSIMS
dc.subjectTEM
dc.subjectcarbon
dc.subjectStardust Mission
dc.titleCarbon investigation of two Stardust particles: A TEM, NanoSIMS, and XANES study
dc.typeArticle
dc.typetext
dc.identifier.journalMeteoritics & Planetary Science
dc.description.collectioninformationThe Meteoritics & Planetary Science archives are made available by the Meteoritical Society and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume43
dc.source.issue1-2
dc.source.beginpage315
dc.source.endpage334
refterms.dateFOA2021-02-12T22:30:40Z


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