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Isotopic systematics of presolar silicon carbide from the Orgueil (CI) chondrite: Implications for Solar System formation and stellar nucleosynthesis

Huss, Gary R. and Hutcheon, Ian D. and Wasserburg, G. J. (1997) Isotopic systematics of presolar silicon carbide from the Orgueil (CI) chondrite: Implications for Solar System formation and stellar nucleosynthesis. Geochimica et Cosmochimica Acta, 61 (23). pp. 5117-5148. ISSN 0016-7037. doi:10.1016/S0016-7037(97)00299-8.

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One hundred and forty individual SiC grains (1-9.6 µm) and twenty-two grain aggregates (2.3-7.8 µm) from the Orgueil (CI) chondrite have been measured by ion microprobe. Silicon and carbon isotopic data were obtained for all individual grains and aggregates, and nitrogen, magnesium, and aluminum abundances and isotopic compositions were measured for most grains and aggregates. Abundances of lithium, beryllium, boron, and sodium were measured for some individual grains. Orgueil SiC is remarkably similar to Murchison K-series SiC in the ranges and distributions of silicon and carbon isotopic compositions, the initial abundances of ^(26)AI, the abundances of minor and trace elements, and the proportions of isotopically unusual grains. Higher ^(15)N/^(14)N ratios in 1-4/µm Murchison K-series SiC grains relative to similar-sized Orgueil grains are inferred to be due to higher amounts of terrestrial nitrogen in the Murchison samples. Higher ^(15)N/^(14)N ratios in 3-6 µm Murchison KJH SiC grains cannot be explained by terrestrial nitrogen and imply that larger SiC grains sampled a different population of parent stars. SiC aggregates have different average silicon and carbon compositions than individual grains, indicating different source stars for the 0.1-1 µm constituent grains. However, the aggregates probably formed by clumping of small grains during laboratory procedures, not at the stellar source. Differences between Murchison L-series SiC and SiC from Murchison K-series and Orgueil are due to the presence of terrestrial SiC among L-series grains and to the larger average grain size of L-series SiC. When terrestrial contamination, sample size, and grain size are taken into account, there is no evidence of an intrinsic difference between Orgueil and Murchison SiC. The Orgueil data provide new information about stellar nucleosynthesis and the SiC parent stars. Carbon and nitrogen isotopic compositions indicate that nuclear processing in addition to that described by most stellar models occurs below the convective stellar envelope during the Red Giant and AGB phases (Cool Bottom Processing). Grains with high ^(15)N/^(14)N but with other characteristics consistent with AGB source stars indicate that ^(15)N is produced in AGB stars, contrary to the predictions of the standard models. A significantly higher rate for the ^(18)O(ɑ,n)^(15)N reaction than is typically used might reconcile the models with the observations. No data currently rule out a higher reaction rate. Addition of ^(18)O produced via ^(14)N(ɑ, y)^(18)O below the hydrogen shell and burned to ^(15)N in the envelope may also play a role in producing the high ^(15)N/^(14)N ratios observed in some SiC grains. Following previous workers, we take the slope ~2.2 silicon isotope array defined by mainstream SiC grains to reflect the initial compositions of the parent stars due to galactic evolution. A general correlation between ^(12)C/^(13)C and ^(29'30)Si/^(28)Si and more scatter around the silicon array at low ^(29'30)Si/^(28)Si indicate that SiC grains with higher ^(29'30)Si/^(28)Si ratios come from higher-metallicity parent stars. A lack of resolved isotopic effects in ^(25)Mg/^(24)Mg suggests that variations in initial magnesium compositions of the parent stars are at least a factor of three smaller than those in silicon and that the ^(22)Ne neutron source was not significantly activated in the AGB stars that produced SiC grains, in accord with theory. These observations indicate that the parent stars of most mainstream SiC grains were ≤2.3 M_☉ and experienced enough Third Dredge-up thermal pulses to supply their envelopes with 2-3% material. A few grains have characteristics suggesting that they came from more-massive stars. Most parent stars of > 1 µm SiC grains apparently had metallicities higher than that of the sun.

Item Type:Article
Related URLs:
URLURL TypeDescription
Huss, Gary R.0000-0003-4281-7839
Wasserburg, G. J.0000-0002-7957-8029
Additional Information:© 1997 Elsevier Science Ltd. Received April 3, 1997; accepted in revised form August 11, 1997. We thank P. Pellas of the Musée d'Histoire Naturelle, Paris for providing the Orgueil sample used in this study, and our sincere thanks go to E. Zinner and P. Hoppe for access to their data files for Murchison SiC grains. E. Deloule helped identify and measure the SiC grains. The authors learned a tremendous amount about nucleosynthesis in Main Sequence and AGB stars from R. Gallino, M. Busso, A. Boothroyd, and I.-J. Sackmann. Detailed and helpful reviews were provided by D. Clayton, T. Bernatowicz, and an anonymous reviewer. Supported by NASA grants NAGW 3040 and NAGW 3297 to G.J. Wasserburg. Work performed under the auspices of the DOE by LLNL under Contract W-7405-Eng-48. Division contribution #5692 (947).
Funding AgencyGrant Number
Department of Energy (DOE) Lawrence Livermore National LaboratoryW-7405-Eng-48
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Caltech Division of Geological and Planetary Sciences5692
Lunatic Asylum Lab947
Issue or Number:23
Record Number:CaltechAUTHORS:20131119-120310106
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Official Citation:Gary R. Huss, Ian D. Hutcheon, G.J. Wasserburg, Isotopic systematics of presolar silicon carbide from the Orgueil (CI) chondrite: Implications for solar system formation and stellar nucleosynthesis, Geochimica et Cosmochimica Acta, Volume 61, Issue 23, December 1997, Pages 5117-5148, ISSN 0016-7037, (
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42571
Deposited By: Ruth Sustaita
Deposited On:19 Nov 2013 23:05
Last Modified:10 Nov 2021 16:25

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