Skip to main content
Dryad

Data from: Humus forms and organic matter decomposition in the Swiss Alps

Data files

Oct 24, 2025 version files 48.84 KB

Click names to download individual files

Abstract

Organic matter decomposition is influenced by abiotic factors (i.e., climate) and biotic factors (i.e., plants and soil decomposers). To qualitatively assess the rate at which organic matter is degraded and integrated into the topsoil layers, a classification of humus forms has been developed. Yet, whether different humus forms could be experimentally linked to litter decomposition has still to be fully assessed.

To determine the relative influence of humus systems on organic matter decomposition, we worked in two regions of the Swiss Alps (Valais and Ticino) along elevational gradients by following a north/south exposure design. First, we quantified humus forms macrorests proportion types by the Ponge small-volume method (Ponge, 1984). Second, we measured the decomposition of green tea and rooibos teabags within the Parasystems and Terrosystems.

We found that Parasystems and Terrosystems differed in teabags decomposition rates, with a slower decomposition in Parasystems and a faster decomposition in Terrosystems. We also observed that elevation, and hence, vegetation type (i.e., forest versus grassland), drives humus forms distribution with Parasystem at the alpine and subalpine levels in Ticino. In contrast, in Valais, Parasystem were found only at the alpine level and Terrosystems at the subalpine level.

Our results thus indicate that organic matter decomposition is influenced by climate but also by different soil biota, for instance, highlighting more fungal activity in the subalpine level with wooden debris and the presence of earthworms in the less woody litters.

Further analyses are however needed to identify other variables that best correlate with variation in decomposition processes within humus systems, such as soil decomposer’s community composition.