Hello Listers,

Here is an abstract and related articles I found tonight about Murchison 
meteorite and SiC, which are grains with highly unusual
isotopic compositions, and these presolar grains are rare grains which are 
naturally of great interest because they permit to get insights into specific 
aspects of stellar nucleosynthesis and evolution.


Title: 
 Unusual 29,30Si-rich SiCs of Massive Star Origin Found Within Graphites from 
the Murchison Meteorite 
Authors: 
 Croat, T. K.; Stadermann, F. J.; Bernatowicz, T. J. 
Affiliation: 
 AA(Department of Physics and Laboratory for Space Science, Washington 
University, Campus Box 1105, One Brookings Drive, St. Louis, MO 63130-4899, 
USA), AB(Department of Physics and Laboratory for Space Science, Washington 
University, Campus Box 1105, One Brookings Drive, St. Louis, MO 63130-4899, 
USA), AC(Department of Physics and Laboratory for Space Science, Washington 
University, Campus Box 1105, One Brookings Drive, St. Louis, MO 63130-4899, 
USA) 
Publication: 
 The Astronomical Journal, Volume 139, Issue 6, pp. 2159-2169 (2010). (AJ 
Homepage) 
Publication Date: 
 06/2010 
Origin: 
 IOP 
AJ Keywords: 
 dust, extinction, nuclear reactions, nucleosynthesis, abundances, stars: 
Wolf-Rayet, supernovae: general  
DOI: 
 10.1088/0004-6256/139/6/2159 
Bibliographic Code: 
 2010AJ....139.2159C 

Abstract

Correlated transmission electron microscopy and NanoSIMS isotopic studies have 
revealed two unusual SiCs with large 29,30Si enrichments within micron-sized 
graphites from the Murchison meteorite. Such anomalies are rare among the 
overall SiC population (in Lt0.01% of SiCs yet measured), whereas two of the 
three SiCs found within graphite show 29,30Si enrichments, in one case as large 
as 29Si/28Si = (2.28 ± 0.03) × solar and 30Si/28Si = (2.03 ± 0.03)× solar. 
C-burning and Ne-burning in massive stars (>8 M sun initial mass) during their 
post-main-sequence development are the only processes capable of producing 
sufficiently large 29,30Si enrichments. This material with heavy Si isotopic 
enrichments from the O/Ne and O/Si layers is later incorporated into 
carbonaceous stardust, either in ejecta from Type II supernovae or perhaps in 
the colliding winds of Wolf-Rayet binaries. Although often too small for Si 
isotopic measurements, four other SiC-containing
 graphites show other signatures of a massive star origin. Abundance estimates 
suggest that such unusual SiCs are present within ~1% of high-density 
graphites. This abundance can be reconciled with the much lower abundance in 
the overall SiC population if these unusual SiCs are naturally smaller (~200 nm 
or less) than SiCs from other isotopic subgroups and if differential 
destruction of small unusual SiCs occurs in massive star outflows unless these 
SiCs are encapsulated in graphite. 

Other related articles linking Murchison and SiCs

http://www.lpi.usra.edu/meetings/LPSC98/pdf/1765.pdf
http://www.lpi.usra.edu/meetings/lpsc2010/pdf/1082.pdf

Here are types and characteristics of presolar grains found in meteorites.

Type 

Size 

Concentration in Meteorites 

Sources 

Diamond
(C) 1-5 nanometers 1000 parts per million Supernovae 

Silicon carbide
(SiC) 0.1-10 micrometers 10 parts per million Carbon-rich giant stars, or 
supernovae 

Graphite
(C) 1-10 micrometers 2 parts per million Supernovae and carbon-rich giant stars 

Aluminum oxide
(Al2O3) 1-5 micrometers 0.1 parts per million oxygen-rich giant stars 

Spinel
(MgAl2O4) 1 micrometer 2 parts per billion oxygen-rich giant stars 

Silicon nitride
(Si3N4) 1 micrometer 2 parts per billion Supernovae 

Table adapted from a 1993 Meteoritics review by Edward Anders and Ernst Zinner, 
and Conel Alexander's Carnegie Institution Yearbook 95, report "Stardust in the 
Laboratory." 

http://www.psrd.hawaii.edu/July97/Stardust.html

Shawn Alan
eBayshop
http://shop.ebay.com/photophlow/m.html?_nkw=&_armrs=1&_from=&_ipg=&_trksid=p4340
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