Bunchgrass

The Bunchgrass (BG) zone occupies the driest
and hottest regions of the southern interior of British Columbia (Lloyd
et. al. 1990) and lies in valley bottoms in the Fraser, Similkameen,
Nicola, Thompson, Chilcotin rivers and Okanagan valley. Upper elevations
range from 700-1000m. The climate consists of dry, hot summers with
a water deficit and cold winters. Mean annual precipitation ranges
from 242 - 328mm and mean annual temperatures range from 5.8 –
9.2 C (Lloyd et. al 1990).
Lloyd et. al. (1990) recognizes two subzones
that represent what is known as the lower and middle grasslands. The
very dry, hot subzone (BGxh) occurs in the driest valley bottoms up
to approximately 700 meters. The BGxh is also known as the lower grasslands.
The very dry, warm subzone (BGxw) occurs above the BGxh up to approximately
1000 meters. This area is commonly called the upper grasslands. The
Ponderosa Pine zone commonly occurs above the BG.
Soils are typically Chernozemic with thin
humus forms, which are found on morainal, glaciofluvial, glaciolacustrine,
colluvial and eolian parent materials.
Ecosystems
Due to an extensive water deficit in these
ecosystems, grasslands predominate and forest cover are generally
restricted to wet sites found near depressions and on lake and river
shores. Sparse canopy cover of Douglas-fir and Ponderosa Pine occur
on dry rocky outcrops and in open grasslands.
Grazing by cattle is common in this zone and has resulted in wide
range of weedy, invasive species (Steen and Coupe 1997). Ecological
knowledge of the climax vegetation on many grasslands is limited due
to a lack of reference ecosystems for investigation. Overgrazed grasslands
are commonly invaded by spotted and diffuse knapweed (Centaurea spp.)
and Cheatgrass (Bromus tectorum).
The following plant information is summarized
from the A Guide for Site Identification and Interpretation in the
Kamloops Forest Region (Lloyd et. al. 1990). Typical zonal site series
consist of several species including bluebunch wheatgrass (Pseudoroegneria
spicata), Sandberg’s bluegrass (Poa sandbergii) and Cladonia
spp. Lichens. Lower grasslands are represented by the occurrence of
big sagebrush (Artemesia tridentata) and upper grasslands are typified
by the occurrence of Junegrass (Koelaria macrantha) on zonal sites.
Dry sites generally have sites series consisting of Antelope brush
(Purshia tridentata), Needle-and-Thread grass (Hesperostipa comata),
Bluebunch wheatgrass, prickly-pear cactus (Opuntia fragilis) and compact
selaginella (Selaginella densa). Wetter grasslands are often found
within a mosaic of dry sites and include rough fescue (Festuca campestris)
and Giant wildrye (Leymus cinereus).
Forested sites in this zone generally occur
in wetter depressions. Lloyd et. al. (1990) classifies site series
in the lower grasslands as consisting of Ponderosa pine, Nootka rose
(Rosa nootkana), Poison Ivy (Toxicodendron rydbergii), black cottonwood
(Populus balsamifera), Snowberry (Symphoricarpos albus) and red-osier
dogwood (Cornus sericea). In addition, upper forested grasslands are
represented by site series consisting of Trembling aspen (Populus
tremuloides), Snowberry and Kentucky bluegrass (Poa pratensis).
The most northern extent of the BG occurs
in the Chilcotin region west of William’s Lake at the confluence
of the Chilcotin and Fraser Rivers (Steen and Coupe 1997). Vegetation
is similar in the Chilcotin with the exception that extensive invasion
of non-native species is not as common as in southern British Columbia.
Due to the narrow geographic range this
zone occupies and its unique climate, a large number of rare or endangered
plants and animals occur here such as the badger and the western rattlesnake.
Resources
Cattle grazing, agriculture, recreation
and human habitation are some of the most common uses of this zone.
Abundant, productive soils allow for a variety of agriculture uses
such as ranching, orchards, ginseng production and vineyards. Due
to proximity to large water bodies such as Okanagan Lake, recreational
water sports along with horseback riding, hunting, fishing, hiking
and mountain biking are common. Lack of continuous forest cover in
this zone limits forestry activities.
References
Lloyd, D., K. Angove, G. Hope, and C. Thompson.
1990. A guide to site identification and interpretation for the Kamloops
Forest Region. B.C. Min. For., Res. Br., Victoria, B.C., Land Manage.
Handb. No. 23. http://www.for.gov.bc.ca/hfd/pubs/docs/lmh/lmh23.htm
Meidinger, D. and Pojar, J. 1991. Ecosystems
of British Columbia. British Columbia Ministry of Forests. 330 pp.
http://www.for.gov.bc.ca/hfd/pubs/Docs/Srs/SRseries.htm
Steen, O.A., and R.A. Coupé. 1997.
A field guide to forest site identification and interpretation for
the Cariboo Forest Region. B.C. Min. For., Res. Br., Victoria, B.C.,
Land Manage. Handb. No. 39. http://www.for.gov.bc.ca/hfd/pubs/docs/lmh/lmh39.htm
Images © Ministry of Forests
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