Cc. Mitchell et Wa. Niering, VEGETATION CHANGE IN A TOPOGENIC BOG FOLLOWING BEAVER FLOODING, Bulletin of the Torrey Botanical Club, 120(2), 1993, pp. 136-147
Vegetation change was documented along three permanent transects after
nearly three decades of beaver flooding. The anchored forested wetlan
d community was killed and replaced by a minerotrophic fen vegetation,
whereas minimal change occurred within the tall scrub-shrub, dwarf sh
rub and open meadow communities. Along all transects, tree cover was r
educed two- to five-fold, whereas low heath shrub cover, especially Ch
amaedaphne calyculata and Kalmia angustifolia, increased. Herbaceous c
over, primarily sedges, increased, especially in the newly created fen
. Within the floating mat communities the evergreen ericaceous shrubs
and scattered stunted Picea mariana and Larix laricina persisted as di
d the herbaceous bog flora. Species richness showed little change from
1960-1988 although there was a floristic shift toward more hydric spe
cies. Flooding differentially affected the vegetation pattern favoring
more minerotrophic species in some areas, but did not appear to threa
ten the typical bog flora. Historically, beaver and other environmenta
l influences have probably modified the vegetation development over mi
llenia, including prolonged quiescent periods interrupted by periodic
disturbances as documented in this study. For most peatlands this dyna
mic model appears more realistic than any orderly successional dogma.