A study of secondary anaerobes of microbial communities in athalassic
environments with pH 8-10, 1-20% salinity, and different hydrochemical
compositions (nine lakes in Tuva) revealed the predominance of methyl
otrophic methanogens and hydrogen- and lactate-utilizing sulfate reduc
ers under extreme conditions. Neither methanogenesis on hydrogen or ac
etate nor aceticlastic sulfidogenesis were observed. Lithotrophic acet
ogenesis was observed under various conditions with maximum activity a
t pH 8 and 5% salinity. A major sink of H-2 was shown to be provided b
y lithotrophic sulfate reducers able to grow at pH as high as 10 and 1
5% salinity; at higher salinity, sulfidogenesis was noted only on lact
ate. Some secondary anaerobes were found to develop under extreme cond
itions not previously known to allow their growth. The general distrib
ution of secondary anaerobes on the pH-salinity matrix is presented.