Data from ice 3590 meters below Vostok Station indicate that the ice was ac
creted from liquid water associated with Lake Vostok. Microbes were observe
d at concentrations ranging from 2.8 x 10(3) to 3.6 x 10(4) cells per milli
liter; no biological incorporation of selected organic substrates or bicarb
onate was detected. Bacterial 16S ribosomal DNA genes revealed Low diversit
y in the gene population. The phylotypes were closely related to extant mem
bers of the alpha- and beta-Proteobacteria and the Actinomycetes. Extrapola
tion of the data from accretion ice to Lake Vostok implies that Lake Vostok
may support a microbial population, despite more than 10(6) years of isola
tion from the atmosphere.