Bacteria in post-glacial freshwater sediments.

Prokaryote communities in post-glacial profundal freshwater sediments of Windermere, representing 10-12,000 years of deposition, were examined for culturability, viability and community structure. The potential for active geochemical cycles was inferred from the presence of specific groups of bacteria. Direct count procedures revealed 10(12) cells (g dry wt sediment)-1 in the surface sediments, which declined to approximately 10(9) cells (g dry wt sediment)-1 at 6 m depth of core (Representing approximately 10,000 years of deposition).