Increased atmospheric CO2 concentration often stimulates plant photosynthes
is, enhances carbon (C) allocation belowground, increases plant nutrient up
take and improves the efficiency of plant water use. Recent studies suggest
that microbial responses to CO2-induced alterations in soil C, water and n
utrient availability play an important role in determining ecosystem feedba
ck to CO2 elevation. However, to date, most of the published results have b
een obtained from short-term experiments or from studies using high-nutrien
t or disturbed soils. Information on microbial responses to CO2-induced cha
nges in natural and/or mature ecosystems with nutrient limitations is criti
cal to predict changes in terrestrial ecosystem C storage under future CO2
scenarios.