We studied the time-course of decomposition, at low temperatures (6-28
-degrees-C), of protein substrates (peptone, gelatin, casein, and fibr
in) by the microflora in the sediment from a piggery manure run-off, a
nd compared it with the self-fermentation of the sediment. The breakdo
wn of protein substrates at the low temperatures was not the limiting
factor in the anaerobic degradation of the manure. Ammonia fixation an
d acid generation proceeded rapidly and were only slightly temperature
-dependent. Acetoclastic methane generation rates fell perceptibly alr
eady at 20-degrees-C, while low temperatures affected lithotrophic met
hane generation to a lesser degree. The repression of lithotrophic met
hane generation in the course of protein substrate fermentation may ha
ve been due to the competition for available hydrogen between the lith
otrophic methane generation and the processes involving the Stickland
reaction. We obtained an enriched culture of apsychrotrophic homoaceta
te bacterium, and isolated two morphologically distinct strains of psy
chrotrophic methanosarcina.