Correlated Si isotope anomalies and large 13C enrichments in a family of exotic SiC grains.
A suite of morphologically distinctive silicon carbide (SiC) grains from the Orgueil and Murchison carbonaceous chondrite meteorites contains Si and C of highly anomalous isotopic composition.  All of the SiC grains in this suite are characterized by a distinctive platy morphology and roughly developed hexagonal crystal forms that allow them to be distinguished from other types of SiC found in the host meteorites.  The delta 29Si and delta 30Si values of individual SiC crystals deviate from those of normal solar material by more than 100%, while the delta 13C values range from 150 to 5200%.  Isotopically normal C and Si are not found in any of these SiC crystals.  The SiC grains belonging to this morphological suite are isotopically distinct from fine-grained SiC aggregates and other morphological types of SiC in unequilibrated meteorites.  The 29Si/28Si and 30Si/28Si ratios of these platy grains are well correlated and define a linear array that does not pass through the composition of normal, solar Si.  This behavior contrasts sharply with the diverse and poorly correlated Si isotopic compositions shown by the total SiC population.  We suggest that the distinctive morphological characteristics and comparatively simple Si isotope systematics identify the platy SiC crystals as a genetically related family, formed around a single, isotopically heterogeneous presolar star or an association of related stars.  The enrichments in 13C and the Si isotope systematics of the platy SiC are broadly consistent with theoretical models of nucleosynthesis in low-mass, carbon stars on the asymptotic giant branch.  The Si isotope array most plausibly reflects mixing between 28Si-rich material, inherited from a previous generation of stars, and material enriched in 29Si and 30Si, produced in intershell regions by neutron capture during He-burning.  13C is also produced in intershell regions by proton reactions on 12C seed nuclei and is carried with s-process nuclei to the stellar envelope by convection which penetrates down to the He shell.  The absence of a correlation between the Si and C isotopic compositions of the SiC suggests either episodic condensation of SiC, extending over several thermal pulses, in the atmosphere of a single star, or derivation of the SiC from several stars characterized by different rates of 13C production.  In the multiple star scenario, the linear correlation of the 29Si/28Si and 30Si/28Si ratios among the platy SiC indicates that these stars evolved from a common Si seed composition under similar conditions of neutron-capture nucleosynthesis.  The 29Si/30Si ratio of the SiC, inferred by us to be produced by neutron capture in the stellar interior, is distinct from values calculated from models of nucleosynthesis in AGB stars.
Stone
J
J
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena 91125, USA.
Hutcheon
I D
ID
Epstein
S
S
Wasserburg
G J
GJ
D055580:Astronomical Phenomena; D001256:Astronomy; D002244:Carbon / Q000032:analysis*; D017554:Carbon Compounds, Inorganic; D002247:Carbon Isotopes; D003460:Crystallization; D005118:Extraterrestrial Environment; D007554:Isotopes; D019110:Meteoroids; D012825:Silicon / Q000032:analysis*; D017655:Silicon Compounds / Q000032:analysis*; D016082:Solar System
D017554:Carbon Compounds, Inorganic; D002247:Carbon Isotopes; D007554:Isotopes; D017655:Silicon Compounds; D002244:Carbon; C022088:silicon carbide; D012825:Silicon