LARGE O-18 EXCESSES IN CIRCUMSTELLAR GRAPHITE GRAINS FROM THE MURCHISON METEORITE - INDICATION OF A MASSIVE-STAR ORIGIN

Forty-seven graphite round grains from the lowest density fraction ext racted from the Murchison carbonaceous chondrite were analyzed for the ir C and N isotopic ratios by ion microprobe mass spectrometry, and su bsets of the grains were analyzed for their O, Mg, Si, Ca, and Ti isot opic ratios. The C-12/C-13 ratios of the grains range from 6.3 to 3140 (solar ratio is 89). Most grains have N-15 excesses (up to 2.5 times solar), O-18 excesses (up to 100 times solar), and large inferred Al-2 6/Al-27 ratios (up to 0.15), and Si isotopic compositions range from S i-28 excesses (up to 30%) to Si-29 and Si-30 excesses (up to 50%). All seven grains analyzed for Ti show large Ti-49 excesses (up to 170%), and some show Ca-42 and Ca-43 excesses and Mg-25 excesses. The large O -18 excesses point to an origin in massive stars, either Wolf-Rayet st ars or Type II supernovae, where O-18 is produced from N-14 at the ons et of He burning. Most of the other isotopic signatures are consistent with such an origin: the Ti, Ca, and Mg anomalies can be explained by slow neutron capture during He burning, the large Al-26/Al-27 ratios by admixture of material that has experienced H burning. The large var iations in the Si isotopic compositions, including both Si-29 and Si-3 0 excesses and deficits, favor a supernova origin with Si-28 coming fr om oxygen burning in an inner layer of the star.