Plants of the modern ecosystem influence humous content mainly to a de
pth of 20 cm. Therefore any climate changes that lead to succession ch
anges of the ecosystem lead to a change in the humous content only in
that layer. In deeper horizons due to global climate change, either th
e former humous state will be preserved or the humous reserves will di
minish, which is related to mineralization of the humus or to gleying.
Global climate changes also lead to a change in the water regime, whi
ch will facilitate peat accumulation (in the case of submersion) and d
ecomposition with a more intensive water demand.