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Barium isotope abundances in meteorites and their implications for early Solar System evolution
ISSN
1872-9533
0016-7037
Date Issued
2016
Author(s)
Bermingham, K. R.
Mezger, Klaus
Scherer, Erik E.
Horan, M. F.
Carlson, R. W.
Upadhyay, D.
Magna, T.
DOI
10.1016/j.gca.2015.11.006
Abstract
Several nucleosynthetic processes contributed material to the Solar System, but the relative contributions of each process, the timing of their input into the solar nebula, and how well these components were homogenized in the solar nebula remain only partially constrained. The Ba isotope system is particularly useful in addressing these issues because Ba isotopes are synthesized via three nucleosynthetic processes (s-, r-, p-process). In this study, high precision Ba isotope analyses of 22 different whole rock chondrites and achondrites (carbonaceous chondrites, ordinary chondrites, enstatite chondrites, Martian meteorites, and eucrites) were performed to constrain the distribution of Ba isotopes on the regional scale in the Solar System. A melting method using aerodynamic levitation and CO2-laser heating was used to oxidize SiC, a primary carrier of Ba among presolar grains in carbonaceous chondrites. Destruction of these grains during the fusion process enabled the complete digestion of these samples. The Ba isotope data presented here are thus the first for which complete dissolution of the bulk meteorite samples was certain. Enstatite chondrites, ordinary chondrites, and all achondrites measured here possess Ba isotope compositions that are not resolved from the terrestrial composition. Barium isotope anomalies are evident in most of the carbonaceous chondrites analyzed, but the Ba-135 anomalies are generally smaller than previously reported for similarly sized splits of CM2 meteorites. Variation in the size of the Ba-135 anomaly is also apparent in fused samples from the same parent body (e.g., CM2 meteorites) and in different pieces from the same meteorite (e.g., Orgueil, CI). Here, we investigate the potential causes of variability in Ba-135, including the contribution of radiogenic Ba-135 from the decay of Cs-135 and incomplete homogenization of the presolar components on the <0.8 g sample scale. (C) 2015 Elsevier Ltd. All rights reserved.