Mr. Roberts et Fs. Gilliam, DISTURBANCE EFFECTS ON HERBACEOUS LAYER VEGETATION AND SOIL NUTRIENTSIN POPULUS FORESTS OF NORTHERN LOWER MICHIGAN, Journal of vegetation science, 6(6), 1995, pp. 903-912
Recent disturbance models have identified changes in resource availabi
lity as factors that control plant community response. Soil nutrient r
esources typically are assumed to change following forest disturbance,
usually with nutrient availablity increasing initially and subsequent
ly decreasing through later stages of succession. We examined the effe
cts of disturbance (clearcut harvesting with a brief recovery period)
on soil organic matter, pH and extractable soil nutrients in successio
nal aspen forests of northern lower Michigan to determine relationship
s of these variables to changes in herbaceous layer vegetation. Two si
te types were identified: dry-mesic (glacial outwash sands, low in org
anic matter) and mesic (calcareous clay till, high in organic matter).
Extractable nutrient concentrations were 1.5 to 3 times higher in the
A(1) horizon of mesic sites than those of dry-mesic sites. Soil pH an
d cations increased after disturbance on mesic sites, but not on dry-m
esic sites. Patterns of change with disturbance were less pronounced i
n lower horizons on both site types. Herb-layer species diversity incr
eased after disturbance on mesic sites, but with decreases in the impo
rtance of shade-tolerant tree species and Maianthemum canadense. Speci
es characteristic of open habitats (e.g. Pteridium aquilinum, Rubus sp
p., Fragaria virginiana, and Diervilla lonicera), increased in importa
nce. Soil factors, species composition and diversity on dry-mesic site
s changed little after disturbance, with Pteridium aquilinum and erica
ceous species remaining dominant in both mature (55 - 82 yr) and distu
rbed (less than or equal to 15 yr) stands. These results suggest that
soil nutrient resources do not always change through secondary success
ion and that patterns of change can be distinctly site-dependent. Dist
urbance response patterns in the herbaceous layer of these aspen fores
ts are also site-dependent.