In general, chondrules have highly variable Li isotope compositions, ranging from 未7Li of 鈭?#xA0;8.5 to + 10鈥? whereby the mean isotope composition of chondrules separated from a single chondrite is slightly lighter than its bulk. Remarkable, however, are the differences in Li concentrations between bulk chondrite and chondrules. Of the entire set studied here, 98%of the chondrules have significantly lower Li abundances (in the range of 0.2 to 0.75 渭g/g) than their hosts (typically around 1.5 渭g/g). Our results indicate that Li elemental and isotopic fractionation has not occurred extensively during chondrule formation. Low, but highly variable Li abundances as well as the relatively large range in Li isotopes point to small-scale heterogeneities in the chondrule-forming reservoir. With respect to Li, such a non-chondritic reservoir is unique to all chondrules. The compositional differences in Li isotopes between bulk carbonaceous and ordinary chondrites (Seitz et al., 2007) are likely to be the result of mixing chondrules, CAI and matrix in different proportions.