Fj. Singer et Mk. Harter, COMPARATIVE EFFECTS OF ELK HERBIVORY AND 1988 FIRES ON NORTHERN YELLOWSTONE-NATIONAL-PARK GRASSLANDS, Ecological applications, 6(1), 1996, pp. 185-199
The drought, frequent lightning strikes, and resultant large fires of
1988 in Yellowstone National Park were considered a several-century ev
ent for the area. They presented an unparalleled opportunity to docume
nt the effects of large fires on forage production, forage quality, an
d herbivory for the largest elk (Cervus elaphus) population in a natur
al area in North America. We documented elk-grassland dynamics on the
BIacktail Plateau on Yellowstone's northern elk winter range following
the burning of 25% of the study area in 1988. Contrary to predictions
of earlier scientists, grazing of the grasslands by elk prior to the
fires did not result in warmer, drier, or less productive bunchgrass c
ommunities. Soil moisture was equivalent, soil temperatures were coole
r, aboveground grass biomass was equivalent in two of three years, and
N, macronutrients (Ca, Mg, P, K), and digestibility concentrations we
re higher on grazed than ungrazed grasslands. Forb biomass, Poa sandbe
rgii biomass, and litter accumulations, however, were less on grazed s
ites, and more bare ground occurred on grazed (35%) than on ungrazed (
24%) grasslands (P < 0.05). Elk herbivory resulted in more documented
ecosystem effects for Blacktail Plateau elk than did burning. Two year
s postfire, burning had increased aboveground biomass of grasslands by
20%. However, digestibility of only one (Festuca idahoensis) of three
grass species (F. idahoensis, Pseudoroegneria spicata, and Koeleria m
acrantha) was enhanced. N, cellulose, and macronutrient concentrations
in grasses, and digestibility in P. spicata, K. macrantha were unaffe
cted by the fires. In grazed vs. ungrazed areas F. idahoensis, P, spic
ata, and K. macrantha averaged a 21% higher N concentration, and a 7%
higher digestibility. Aboveground herbaceous biomass was greater in gr
azed than ungrazed areas in one of three years, and total aboveground
N yield was greater in two of three years. Forage biomass did increase
postfire and could have benefited elk foraging efficiency. Elk use of
burned grasslands increased following the fires (P < 0.05). Elk avoid
ed burned forests during the first three winters postfire (P < 0.05),
but elk obtain few of their forages from forest communities on the nor
thern Yellowstone winter range (<10% of feeding observations prefire).
The possibility exists that shrub and herbaceous biomass in forest un
derstories will increase after greater than or equal to 3 yr postfire.
Other studies suggest slower recovery, or increases to preburn levels
in forests after approximate to 6-8 yr. Eventually, the elk might ben
efit from increased quality and biomass of forages in burned forests.
Grazing, by reducing fuels, can alter the extent of burning and create
a more patchy fire pattern than occurs on ungrazed areas, thus conser
ving N that would otherwise be volatilized by burning. We observed no
such interaction between elk herbivory and burning, in spite of a sixf
old reduction in litter on grazed sites. Burning did not affect N conc
entrations on either grazed or ungrazed study sites, apparently becaus
e accumulations of dead aboveground plant material were still very lig
ht on both treatments in comparison to, e.g., tallgrass or mixed-grass
prairies in the Great Plains. The relatively minor effects of the fir
es of 1988 on the grassland study sites were probably a result of the
relatively fast front fires, with little residual burning, and the rel
atively small dead plant accumulations in bunchgrass communities.