Movile Cave, recently discovered in southern Romania, contains sulfide
-rich thermal waters in submerged passages, as well as isolated air po
ckets. The water surfaces within the air pockets are covered by substa
ntial microbial biofilms, while the air bells contain an abundant and
diverse community of terrestrial and aquatic animal species. Based on
the results of dehydrogenase activity, fecal streptococci counts, and
stable carbon isotope ratios, we propose that the cave community is bi
ologically isolated and receives little, if any, organic carbon inputs
from the surface environment. Several sulfide-oxidizing chemoautotrop
hic bacteria were isolated from the cave waters. One putative Thiospha
era sp. strain, LV-43, was further characterized. The presence and hig
h level activity of RuBisCO was clearly demonstrated in this strain.