Three humus forms that are widespread in the Inner Alps, a dysmull below Pi
nus sylvestris, an oligomull below Abies alba and a mor below Pinus cembra,
were studied by following mineral nitrogen production and uptake and by a
characterization of the pedofauna. Due to the production and uptake of nitr
ogen, mainly as nitrates and also due to the dominance of Lumbricids versus
Arthropods, the oligomull was the sole humus form that functioned as a mul
l. Nevertheless relatively weak mineral nitrogen production and the dominan
ce of endogeic soil-dwelling earthworms versus anecic earthworms demonstrat
ed the moderate activity of this mull, which is representative of humus for
ms of old growth forests and cold climates. There was a discrepancy between
the very low biological activity of the dysmull and its status of mull, wh
ile an observed bifunctioning between the different layers of this humus al
so differentiated it from the mor. (C) 2001 Academie des sciences/Editions
scientifiques et medicales Elsevier SAS.