The response of above-ground plant and ecosystem processes to climate chang
e are likely to be influenced by both direct and indirect effects of elevat
ed temperature on soil biota and their activities. This study examined the
effects of elevated atmospheric temperature on the development of the soil
microbial community in a model terrestrial ecosystem facility. The model sy
stem was characterized by a soil of low nutrient availability, a condition
that simulates most native terrestrial plant communities. The experiment wa
s run over three plant generations, broadly mimicking the early stages of a
plant succession, and showed that microbial biomass, measured using phosph
olipid fatty acid (PLFA) analysis, increased significantly in response to e
levated temperature during the first generation only. This increase was unr
elated to changes in plant productivity or soil C-availability, and was lar
gely due to a direct effect of elevated temperature on fast-growing Gram-po
sitive bacteria. Slow growing soil micoorganisms such as fungi and actinomy
cetes were unaffected by elevated temperature throughout the experimental p
eriod. Measures of microbial biomass, microbial respiration and N-mineraliz
ation were also unaffected by elevated atmospheric temperature over the thr
ee generations. The lack of effects on the soil microbial community is thou
ght to be due to the fact that elevated temperature did not influence root
biomass or soil C-availability. We suggest that the observed reductions in
above-ground plant productivity, in response to elevated temperature, will
become apparent in the longer term when litter decomposition pathways are m
ore established. The temporal measures of PLFA and microbial biomass indica
ted that over the experimental period rapid initial changes occurred in mos
t soil biological characteristics, followed by periods of stabilization dur
ing later plant succession. These changes were associated with increases in
above ground plant productivity and amounts of available C in the soil. In
contrast, total microbial biomass declined during the last plant generatio
n. Reductions in the diversity of PLFAs in later plant generations appeared
to be associated with an increase in the proportion of fatty acids associa
ted with fungi, relative to those from bacteria. These changes are likely t
o be related to increased competition for resources within the soil, and an
associated reduction in N- and C-availability. These changes appear to be
broadly consistent with those reported for other studies on the successiona
l development of soil microbial and plant communities. Overall, our data su
ggest that elevated atmospheric temperature has little effect on the develo
pment of below-ground microbial communities and their activities in soils o
f low nutrient status.