HIGHLIGHTS
SUMMARY
At the same time, soil formation occurs not only under the folic material of a forest floor located on the surface of mineral soil forming substrata but also in epiphytic organic and organo-mineral formations, typical for tropical wet forests. The first is a "classical" soil formed as result of interaction of the mineral part with incoming organic matter; these soils are not rich in organic matter due to the high mineralization rate. The main difference between suspended soils and classical mineral soils is that suspended soils have no direct connection with the mineral . . .
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