The diversity of organic and organo-mineral substances in soil account
s for its individual and unique character. Trends in terrestrial organ
ic residue transformations underwent considerable changes over the geo
logical time scale: coal formation was replaced by mineralization and
humus formation in accordance with the sequence of geological periods.
The state and composition of soil organic matter as a function of fiv
e soil-forming factors may be followed both in historical and geograph
ical aspects. Soil organic matter is a sensitive indicator of undue in
teractions between human beings and nature.