Decomposition of cellulose by the anaerobic alkaliphilic microbial communit
y at pH 9-10 and a mineralization of 10-20 g/l was studied. The main produc
ts of this process were found to be H-2, acetate, and H2S. The relatively r
apid decomposition of cellulose by alkaliphiles under anaerobic conditions
was accomplished by three groups of microorganisms acting successively: (1)
cellulolytic bacteria with associated primary anaerobes; (2) hydrogenotrop
hic and acetotrophic sulfidogens, and (3) anaerobic phototrophic oxidizers.
In the absence of sulfate, the last stage was implemented by acetogens. Me
thanogenesis was weak. Dominant bacteria, which were readily detectable mic
roscopically, could be accumulated by incubating the community with the res
pective substrates.