Microbial Recovery from Stress

FIGURE 2 Carbon respired over a 10-day incubation in the lab on litter samples that had been incubated under different treatments. Panel 

Another kind of stress that is important in trace gas dynamics is shifting aeration/anaerobiosis. In wetland systems the aeration history of the system is a significant controller of CFI4 efflux and 

J and Carballas T. (1996). Changes in physiological groups of microorganisms in soil following wildhre. FEMS Microbiol. Ecol. 20, 33-39. 

and Christensen, S. (1993). Denitriheation variability and control In a riparian fen irrigated with agricultural drainage water. Soil Biol. Biochem. 25, 915-923. 

Anderson, T. -H., and Joergensen, R. G. (1997). Relationship between SIR and FE estimates of microbial biomass C in deciduous forest soils at different pH. Soil Biol. Biochem. 29, 1033- 1042. 

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