This contribution (i) chemically distinguishes the two carbonatites: sovite
and alvikite, and (ii) presents new 'average' (median) compositions for th
em. The best and most used average chemical composition for calciocarbonati
te is that calculated by Woolley and Kempe in 1989, and it is shown here th
at this composition comprises two distinctively different compositions corr
esponding to those of sovite and alvikite. Sovite and alvikite are the coar
se-grained and the medium- to fine-grained varieties, respectively, of calc
ite-carbonatite. It is proposed that the corresponding calciocarbonatites s
hould be termed C1 calciocarbonatites and C2 calciocarbonatites, based on t
heir chemical compositions. The distinction of the two lies, not in the maj
or elements, but in the minor, trace- and rare-earth-element contents. Usin
g a comprehensive database of post-1970 analytical data, the 'average' comp
ositions for C1 and C2 calciocarbonatites have been calculated. Instead of
the arithmetical average, the arithmetical median has been calculated for e
ach, since this gives truer estimates of the two compositions. It is believ
ed that the two median compositions will enable C1 End C2 calciocarbonatite
s to be recognized.