Nutrient acquisition by plants occurs in an environment characterized by co
mplex interactions between roots, micro-organisms and animals, termed the r
hizosphere. Competition for mineral elements in this sphere is high. The rh
izosphere processes are driven by photosynthetically fixed carbon released
by roots either directly to myconhizal fungal symbionts or as exudates fuel
ling a wider spectrum of organisms, mainly bacteria. In particular, the rol
e of the soil fauna interacting with rhizosphere micro-organisms and plant
roots has so far found little attention. We present evidence that the inter
action between plant roots, root exudates and micro-organisms can only be u
nderstood in relation to soil faunal activity, indicating that the soil fau
na has an important function in regulating rhizosphere microbial processes
and therefore significantly affects plant growth. (C) 2000 Editions scienti
fiques et medicales Elsevier SAS.