RESPONSE OF PROTOZOAN AND MICROBIAL COMMUNITIES IN VARIOUS CONIFEROUSFOREST SOILS AFTER TRANSFER TO FORESTS WITH DIFFERENT LEVELS OF ATMOSPHERIC-POLLUTION
Mm. Couteaux et al., RESPONSE OF PROTOZOAN AND MICROBIAL COMMUNITIES IN VARIOUS CONIFEROUSFOREST SOILS AFTER TRANSFER TO FORESTS WITH DIFFERENT LEVELS OF ATMOSPHERIC-POLLUTION, Biology and fertility of soils, 27(2), 1998, pp. 179-188
During recent decades, forest ecosystems have been exposed to high lev
els of atmospheric pollution, and it has been argued that this affects
the composition and activity of decomposer communities and, subsequen
tly, ecosystem functioning. To investigate the effects of atmospheric
pollution on protozoa and microflora, a new experimental design was us
ed. Undisturbed soil columns, originating from six coniferous forests
across Europe and representing different stages of soil acidification,
were transferred to two Scots pine forests (Fontainebleau and Wekerom
) with different: levels of N and S deposition (NH4+-N=4.90 and 42.50
kg ha(-1) year(-1); SO4-S=10.90 and 30.40 kg ha(-1) year(-1), respecti
vely). The number of protozoa, microbial biomass C and microbial activ
ity were estimated in the organic layer (Of) of the transferred soils
at the two host sites after 21 months of incubation. The experiment ai
med at answering two questions: (1) Do changes in environmental condit
ions, studied by transferring soils from one site to another, affect p
rotozoa and microbial communities and, if so, (2) how important are ch
anges in both N and S deposition in explaining the effects of soil tra
nsfer on protozoa and microbial communities? The interaction between p
rotozoa and microbial communities was addressed with regard to these c
hanges in environmental conditions. No effect of enhanced N or S depos
ition on protozoan numbers and microbial biomass C, basal respiration
and caloric quotient was revealed. Reciprocal transfer of various soil
columns resulted in lower abundance and activity of protozoa and micr
obes. This reduction could not be explained by differences in N and S
deposition, but by differences in microclimate and adaptation. In some
cases, protozoa correlated with pH, CIN ratio, P and S content and le
ached mineral N.