Low
Shrubs on Lava.
These communities occur on basalt ridges and other areas
where shallow soils overlay basalt (Figure 19).
Black sagebrush is often present, but usually not dominant.
Green rabbitbrush and broom snakeweed are common.
Wyoming big sagebrush and winterfat occur in some areas.
Native bunchgrasses and forbs typically are abundant.
Columbia goldenweed (Haplopappus acaulis, see
picture below), a suffrutescent shrub, is found on patches
of exposed lava.
Sagebrush-Rabbitbrush.
Communities in this class are characterized by an abundance
of green rabbitbrush, which may be the dominant shrub or a
co-dominant with Wyoming big sagebrush or, occasionally, black
sagebrush. Communities
in this class fall both on and off the basalt flows.
Many of these communities have a rich understory of
perennial grasses and forbs.
Cheatgrass is present and sometimes very abundant where
these communities occur on coarse-textured soils.
These communities variously intergrade with big sagebrush
steppe.
Green
rabbitbrush often is characterized in the literature as an
“early successional” species.
However, it is the only shrub that consistently increased
in abundance between 1950 and 1985 on the INEEL permanent
vegetation plots (Anderson and Inouye 1988).
That this occurred in the absence of any major disturbances
such as fire or livestock grazing indicates the “early seral”
characterization is inappropriate.
It may well be an opportunistic species that can take
advantage of disturbances, but the data from the INEEL does not
support the view that it will be displaced by other species in
later stages of vegetation development. Green rabbitbrush
can sprout vigorously following fire, so its abundance on some
sites may be a consequence of fire history.
Sagebrush-Winterfat.
Communities in this class typically are dominated by
Wyoming big sagebrush, but winterfat is typically abundant and may
be dominant or co-dominant. Green
rabbitbrush is common, as are members of the suite of perennial
grasses, especially Indian ricegrass.
This class occurs on soils derived primarily from
lacustrine deposits of ancient Lake Terreton.
Cheatgrass seldom is found in these communities.
Our vegetation data suggests that these communities are
intermediate between the Sagebrush/Green Rabbitbrush communities
and Salt Desert Shrub communities.
This may reflect a gradient from upland loess soils to the
more halomorphic lacustrine soil of the Lake Terreton basin.
Salt
Desert Shrub.
Salt desert shrub communities are found on the Big Lost
River and Birch Creek playas and on other playas within the Lake
Terreton basin. All
are dominated by members of the chenopod family, but their
composition varies considerably.
Our samples indicated the occurrence of three relatively
distinct community types. The
first is dominated by suffrutescent shrubs.
Nuttall saltbush is the dominant species.
Shrubby buckwheat is a co-dominant in some areas and
winterfat is often present. The
second type is dominated by shadscale.
Winterfat and green rabbitbrush are common in these
communities, and Nuttall saltbush may be present.
The third type is dominated by winterfat, but four-wing
saltbush (Atriplex canescens)
is abundant.
The
spectral complexity of the northern portions of the INEEL,
particularly within the area formerly occupied by Lake Terreton,
is apparent on the vegetation map.
This complexity is a consequence, at least in part, of
differential deposition of alluvial and lacustrine sediments and
wind-blown sands, which affects spectral properties of the soil
surface as well as vegetation development.
The salt desert shrub and other communities that occupy the
Lake Terreton basin often have a high percentage of bare ground,
which may dominate the spectral signature of a satellite image.
Thus, classification errors can be quite common because
there is not a close correlation between vegetation
characteristics and spectral properties of the area.
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