Abstract. Soil erosion continues to be one of the most serious environmental problems
of our time and is exacerbated by progressive climate change. Until now,
forests have been considered an ideal erosion control. However, even minor
disturbances of the forest floor, for example, from heavy vehicles used for
timber harvesting, can cause substantial sediment transport. An important
countermeasure is the quick restoration of the uncovered soil surface by
vegetation. To date, very little attention has been paid to the development
of nonvascular plants, such as bryophytes, in disturbed areas of temperate
forests and their impact on soil erosion. This study examined the natural
succession of pioneer vegetation in skid trails on four soil substrates in a
central European temperate forest and investigated their influence on soil
erosion. For this purpose, rainfall simulations were conducted on
small-scale runoff plots, and vegetation was continuously surveyed during
the same period, primarily to map the development of bryophytes and the
occurrence of biological soil crusts (biocrusts). Biocrusts appeared immediately after disturbance, consisting primarily of
bryophyte protonemata and cyanobacteria as well as coccoid and filamentous
algae that lost their biocrust characteristics as succession progressed.
They were present from April to July 2019, with a particular expression in
the skid trail that was on shale clay (Psilonotenton Formation) and silty
clay loam substrate. In general, skid trails on clayey substrates showed
considerably higher bryophyte cover and species richness. Although
bryophytes were subsequently overtopped by vascular plants, they managed to
coexist until their growth was restricted due to leaf litter fall.
Brachythecium rutabulum and Oxyrrhynchium hians were the most important and persistent pioneer bryophyte species,
while Dicranella schreberiana and Pohlia lutescens were volatile and quickly disappeared after spreading in the
summer. Sediment discharge was 22 times higher on disturbed bare soil
compared with undisturbed forest soil and showed the largest sediment
removal in the wheel tracks. Counteracting this, soil erosion decreased with
the recovery of surface vegetation and was particularly reduced with growing
pioneer biocrusts in summer, but it again increased in winter, when vascular
vegetation became dominant. This leads to the conclusion that the role of
bryophyte-dominated biocrusts in forests has been underestimated so far, and
they can contribute more to soil conservation at specific times of
succession than vascular plants.