Abstract
Anaerobic microcosms were established in which plant material was degraded by the co-operative interaction of various bacterial metabolic types, and the production of CH4 and sulfide was monitored. The introduction of the anaerobic ciliate Metopus palaeformis resulted in a reduction of bacterial abundance but an increase in the rate of CH4 and sulfide production. The enhanced bacterial activity (resulting in an increased rate of bacterial CH4 production) was positively correlated with the number of ciliates present. The endosymbiotic methanogens of M. palaeformis did not contribute significantly to the observed increase in CH4 production. It was concluded that protozoan excretions such as organic acids (acetate, propionate) were most likely responsible. Protozoa have previously been shown to enhance bacterial activity in aerobic systems, but this is the first report of the phenomenon in anaerobic systems. Bacterial stimulation by protozoan grazing signifies the importance of anaerobic protozoa in the natural environment, not just in controlling bacterial numbers but also in vitalising ecosystem function. Copyright (C) 1998 Federation of European Microbiological Societies.
| Original language | English |
|---|---|
| Pages (from-to) | 1-8 |
| Number of pages | 8 |
| Journal | FEMS Microbiology Ecology |
| Volume | 27 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 1 Sept 1998 |
| Externally published | Yes |
Keywords
- Anaerobic protozoon
- Decomposition
- Methane
- Metopus palaeformis
- Predation
- Sulfide