Acidic bioflms present on cave walls in the sulfidic region of the Frasassi
Gorge, Italy, were investigated to determine their microbial composition a
nd their potential role in cave formation and ecosystem functioning. All bi
ofilm samples examined had pH values <1.0. Scanning electron microscopy of
the biofilms revealed the presence of various filaments and rods associated
in large clusters with mineral crystals. Qualitative energy-dispersive x-r
ay analysis was used to determine that the crystals present on the cave wal
ls, associated with the microbial biofilm, were composed of calcium and bar
ium sulfate. Ribosomal RNA-based methods to determine the microbial composi
tion of these biofilms revealed the presence of at least two strains of pot
ential acidophilic, sulfur-oxidizing bacteria, belonging to the genera Thio
bacillus and Sulfobacillus. An acid producing strain of Thiobacillus sp. al
so was obtained in pure culture. Stable isotope ratio analysis of carbon an
d nitrogen showed that the wall biofilms are isotopically light, suggesting
that in situ chemoautotrophic activity plays an important role in this sub
surface ecosystem.