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Uniform initial 10Be/9Be inferred from refractory inclusions in CV3, CO3, CR2, and CH/CB chondrites 1 1 Introduction 1 2 Methods 7 2.1 Samples and electron probe microanalysis (EPMA) 7 2.2 SIMS 10Be−10B Analyses 7 2.2.1 IMS-1290 (UCLA) measurements of 10Be–10B systematics 10 2.2.2 Comparing 10Be–10B analytical configurations and instruments 10 2.3 SIMS 26Al−26Mg Analyses 10 2.4 SIMS oxygen isotope analyses 11 2.5 Isotope ratio determination and isochron regression 13 3 Results 15 3.1 Twenty-five 10Be−10B CAI isochron regressions 15 3.2 Five 26Al−26Mg CAI isochron regressions 15 3.3 Oxygen Isotope Compositions in Five CAIs 15 4 Discussion 16 4.1 Uniform 10Be distribution recorded in CAIs? 16 4.1.1 Outlier FUN CAI CMS-1 17 4.2 Integration of 10Be–10B isotope systematics from this study with previous studies 18 4.3 Correlation of 10Be with 26Al, oxygen isotopes, 50Ti, and REEs 19 4.3.1 Importance of 26Al–26Mg, oxygen isotopes, 50Ti, and REEs 19 4.3.2 26Al–26Mg and oxygen isotope systematics in our CV3 and CR2 CAIs 20 4.3.3 Two distinct CAI groups 20 5 On the origin of 10Be and astrophysical implications 22 6 Conclusions 23 Declaration of Competing Interest 23 Acknowledgements 23 Appe

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