This paper emphasizes some general aspects of soil protozoa as indicators o
f environmental quality-pros and cons, methods, and diversity. Protozoa are
at the base of the heterotrophic eukaryotic food web and an essential comp
onent in marine, freshwater, and soil ecosystems because they consume a sig
nificant portion (usually >50%) of the bacterial productivity. enhancing nu
trient cycles and energy flows to the benefit of microorganisms, plants and
animals. Accordingly, studies of their dynamics and community structures p
rovide a powerful means for assessing and monitoring changes in the biotic
and abiotic environment. This is exemplified by some representative studies
focusing on soil oxygen regime, differentiation of humus types, pesticides
, global warming, forest decline, movement of protozoan pathogens in soil,
and soil protozoan bioassays. Usually, protozoa are not replaceable by high
er animals (meso- and macrofauna) as indicator organisms because they have
unique physiological properties: they consume more food and have a higher r
espiration rate per mass unit, have shorter generation and life times, and
reproduce much faster. Direct counting methods should be given preference o
ver dilution culture techniques, which are beset with uncontrollable defici
encies. Thus, ciliates and, especially, testate amoebae, whose abundance an
d diversity can be reliably estimated in simple soil suspensions, should be
preferred in environmental studies. About 1600 protozoan species are known
to live in terrestrial habitats. However, data from studies of ciliates su
ggest that this is only a minor portion (20-30%) of the species actually pr
esent, most of which are still undescribed. Overcoming the methodological a
nd taxonomic problems are urgent needs which, at present, limit the use of
protozoa as bioindicators in terrestrial environments. Furthermore, species
monographs are required to compile the taxonomic, faunistic, and ecologica
l information available. (C)1999 Elsevier Science B.V. All rights reserved.