The rates of the processes of bacterial sulfate reduction (SR) and decomposition of organic matter (D(total)) were studied in the bottom sediments (BS) of 14 lakes in Lithuanian national and regional parks in the summers of 1998-2002. Anaerobic processes accounted for an average of 92% of D(total) in the depressions of deep-water lakes; for the sediments of shallow lakes, high rates of oxygen uptake were noted. The SR rate in different lakes varied from 0.09 to 2.60 mg S(2-)/(dm3 day). At low sulfate concentrations (13.3-70.6 mg S-SO4(2-) /dm3), characteristic of the BS of freshwater ecosystems, the main factor that affected the SR rate in the BS of the lakes studied was the content of readily available organic matter, only in special cases, was it affected by a change in the sulfate ion concentration. In shallow lakes, both temperature-dependent activation of sulfate-reducing bacteria and their inhibition by acidification of the environment were recorded. The contribution of SR to D(total) was 0.2 to 11.0%.
Anaerobiosis Biodegradation, Environmental