Heterogeneity of the soil medium is considered as a factor determining
taxonomic and ecological variations of the soil fauna in the course o
f evolution. Differences between spatial niches occupied by groups of
invertebrates of different size are analyzed in terms of their respira
tion characteristics. The formation of three mechanisms of gas exchang
e is discussed, with soil animals taken as an example. Ethological and
ecological adaptation of large soil animals for formation and mainten
ance of aerated space in the mineral soil mass is considered. Air-fill
ed macropores are the main factor allowing population of deep horizons
of the soil profile by aerobiotic animals. A hypothesis on the coloni
zation of the soil stratum by terrestrial animals from the soil surfac
e is substantiated.