s nanobacteria in travertines, carbonate sediments and hot springs of central Italy, which are very similar to those described as NB/CNP. The author contends that they are responsible for a great deal of mineral precipitation as well as conversion of igneous mineral to soils, and the corrosion of metals.
We found a strong correlation between renal stones and CNP in this study and these results open a new insight on this area to explore the etiology of stone formation. Whether NB/CNP are truly nanoorganisms or self-propagating mineral compounds is still controversial and its contribution, if any, in apatite nucleation and crystal growth remains uncertain. Future studies are necessary for understanding the mechanisms involved in kidney stone formation.
The authors wish to thank to CNPq and CAPES for financial support and to Drs Túlio Graziottin and André Bonfanti for calculi supply.
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