The ability of thionic and nitrifying bacteria to destroy some types o
f kimberlites from Southeast Belomor'e was studied. Oxidation of eleme
ntal sulfur by Thiobacillus thiooxidans at low pH values caused destru
ction of kimberlites of saponite and serpentine-saponite types: saponi
te, serpentine, chlorite, and calcite were dissolved and the granulome
tric composition of the rock was changed. Destruction of kimberlites b
y nitrifying bacteria was connected mainly with calcite dissolution; t
herefore, they caused a more profound degradation of carbonate type ki
mberlites, which contained up to 60% calcite.