The control of soil organic matter (SOM) stability by soil invertebrates is
evaluated in terms of their impact on the inherent recalcitrance, accessib
ility to microorganisms, and interaction with stabilizing substances of org
anic compounds. Present knowledge on internal (ingestion and associated tra
nsformations) and external (defecation, constructions) control mechanisms o
f soil invertebrates is also reviewed. Soil animals contribute to the stabi
lization and destabilization of SOM by simultaneously affecting chemical, p
hysical, and microbial processes over several orders of magnitude. A very i
mportant aspect of this is that invertebrates at higher trophic levels crea
te feedback mechanisms that modify the spatio-temporal framework in which t
he micro-food web affects SOM stability. Quantification of non-trophic and
indirect effects is thus essential in order to understand the long-term eff
ects of soil biota on SOM turnover. It is hypothesized that the activities
of invertebrates which lead to an increase in SOM stability partly evolved
as an adaptation to the need for increasing the suitability of their soil h
abitat. Several gaps in knowledge are identified: food selection and associ
ated changes in C pools, differential effects on SOM turnover, specific ass
ociations with microorganisms, effects on dissolution and desorption reacti
ons, humus-forming and humus-degrading processes in gut and faeces, and the
modification of invertebrate effects by environmental variables. Future st
udies must not be confined merely to a mechanistic analysis of invertebrate
control of SOM stability, but also pay considerable attention to the funct
ional and evolutionary aspects of animal diversity in soil. This alone will
allow an integration of biological expertise in order to develop new strat
egies of soil management which can be applied under a variety of environmen
tal conditions.