In Montana, this system occurs above upper treeline throughout the Montana Rocky Mountain ranges, and east
into the mountain island ranges. Elevation ranges from as low as 6,600 ft in
northwestern to 10,500 feet in
southwestern Montana. Turf communities form on gentle to moderate upper
slopes, flat ridges, valleys, basins, and gentle summit ridges where soil has
become relatively stabilized and the water supply persists until fall. At these
elevations, the growing season typically ranges from 60 to 90 days. During the
growing season, these areas are subjected to windy conditions and widely
variable diurnal temperatures. Freezing temperatures and snow can occur
throughout the summer months. Turf communities are composed of a diversity of
rhizomatous sedges, rushes, woodrushes, grasses and forbs that form a dense
turf that is rarely greater than 12 cm (5 inches) tall. Depending on slope
protection, soil development, snow depth, turf communities can range from dry
to mesic expressions.
Throughout
Montana,
alpine turf supports a high diversity of sedges, grasses and forbs. Common graminoid species include alpine bluegrass (Poa alpina),
alpine timothy (Phleum alpinum),
alpine fescue (Festuca brachyphylla),
and a highly diverse assemblage of sedges including northern singlespike sedge (Carex scirpoidea), curly sedge(C. rupestris),
blackroot sedge (Carex elynoides ), obtuse sedge (Carex obtusata), dunhead sedge (Carex phaeocephala),
Hayden’s sedge (Carex haydeniana), spiked woodrush (Luzula spicata), and Piper’s woodrush (Luzula piperi).
Alpine forbs can often form nearly half the cover in turf communities and can include
diverse leaf cinquefoil (Potentilla diversifolia),
alpine goldenrod (Solidago multiradiata),
moss campion (Silene acaulis), Parrot’s beak lousewort (Pedicularis contorta), arnica (Arnica species), alpine pussytoes (Antennariaspecies),
subalpine wandering daisy (Erigeron peregrinus), sibbaldia (Sibbaldia procumbens), glacier
lily (Erythronium grandiflorum),
and rhexi-leaf paintbrush (Castilleja rhexifolia),among many others. Woody, mat forming species such as arctic
willow (Salix arctica)
and bearberry (Arctostaphylos uva-ursi) can
contribute significant cover in many examples of turf communities. Due to the
very slow rate of community development, short growing season, and limited soil
development, alpine turf cannot support heavy levels of disturbance such as
repeated grazing, land disturbance and heavy foot traffic. Recovery of these
communities occurs over many decades. Climatic warming and decreasing snowpack
levels will alter the floristic composition and the distribution of peripheral
species, northern Rocky Mountain endemics and
rare species that occur within it.
This system occurs above upper treeline throughout the North American Rocky Mountain cordillera, including alpine areas of ranges in Idaho, Utah, Colorado, Wyoming and Nevada, and isolated alpine sites in the northeastern Cascades. In Montana, this system occurs above upper treeline throughout the Montana Rocky Mountain ranges, and east into the mountain island ranges. Snow pack is higher in alpine basins whereas ridges and summits can be blown free of snow due to high winds and sublimation.
Approximately 1,191 square kilometers are classified as Alpine Turf in the 2013 Montana Land Cover layers.
Grid on map is based on USGS 7.5 minute quadrangle map boundaries.
Carbon, Deer Lodge, Flathead, Gallatin, Glacier, Granite, Lewis and Clark, Missoula, Park, Powell, Ravalli, Stillwater, Sweet Grass
In Montana, alpine turf communities are well represented throughout the Northern Rocky Mountains and island mountain ranges. Elevation ranges from as low as 6,600 ft in northwestern Montana to 10,500 feet in southwestern Montana. Turf communities form on gentle to moderate upper slopes, flat ridges, valleys, basins, and gentle summit ridges where soil has become relatively stabilized and the water supply persists until fall. At these elevations, the growing season typically ranges from 60 to 90 days. During the growing season, these areas are subjected to windy conditions and widely variable diurnal temperatures. Freezing temperatures and snow can occur throughout the summer months. During winter months, turf communities are subjected to very cold temperatures, high winds, and heavy accumulations of snow. Snow pack accumulation is dependent on topography. Snow pack is higher in alpine basins whereas ridges and summits can be blown free of snow due to high winds and sublimation. In Montana, soils are derived a variety of parent materials, and can be acidic or calcareous. The A horizon is typically less than 10 cm deep. Soils are typically rocky or gravelly with good aeration and drainage.
Turf
communities are composed of a diversity of rhizomatous sedges, rushes,
woodrushes, grasses and forbs that form a dense turf that is rarely greater
than 12 cm (5 inches) tall. Depending on slope protection, soil development,
snow depth, turf communities can range from dry to mesic. In northwestern Montana, dry turf
communities are dominated by graminoids. Common species include alpine
bluegrass (Poa alpina), alpine
timothy (Phleum alpinum), alpine
fescue (Festuca brachyphylla),
dunhead sedge (Carex phaeocephala),
spiked woodrush (Luzula spicata),
Piper’s woodrush (Luzula piperi), and
Hayden’s sedge (Carex haydeniana).
Alpine
forb cover is usually less than 40% in the drier expression of alpine turf
communities. Common species include forbs include diverse leaf cinquefoil (Potentilla diversifolia), alpine
goldenrod (Solidago multiradiata), moss
campion (Silene acaulis), Parrot’s
beak lousewort (Pedicularis contorta), arnica (Arnica species), Eschscholtz’s buttercup (Ranunculus eschscholtzii). Woody, mat forming arctic willow (Salix arctica) often forms high cover in
dry turf communities. In more well developed turf communities, forb diversity
increase and can reach greater than 40% percent cover. Additional species include
arnica (Arnica species), alpine
pussytoes (Antennaria species),
subalpine wandering daisy (Erigeron
peregrinus), one-stem fleabane (Erigeron
simplex), sibbaldia (Sibbaldia
procumbens), glacier lily (Erythronium
grandiflorum), rhexi-leaf paintbrush (Castilleja
rhexifolia), western anemone (Anemone
occidentalis), alpine Saint John’s wort (Hypericum formosum), elegant death camas (Zigadenus elegans), alpine bistort (Polygonum bistortoides), and viviparous bistort (Polygonum viviparum). Higher levels of
organic matter contribute to greater graminoid diversity including purple
mountain hairgrass (Deschampsia
atropurpurea) and beautiful sedge (Carex
spectabilis).
In
northwestern Montana,
the more mesic expressions of turf communities form on gentle slopes and basins
where subirrigation from permanent snow fields and higher levels of organic
matter accumulation occur in the soils. Although infrequent, they support additional
species including single spike sedge (Carex
scirpoidea), curly sedge (Carex
ruprestris), hair sedge (Carex
capillaris) and Payson’s sedge (Carex
paysonis).
In
southwestern Montana, the graminoid component of turf includes dunhead sedge,
Hayden’s sedge, showy sedge, single spike sedge, spiked woodrush, black and
white sedge(Carex albo-nigra), two-tipped sedge (Carex lachenalii), spike sedge (Carex
nardina), and Drummond’s rush (Juncus
drummondii). Grasses such as alpine blue grass, alpine timothy, alpine
fescue, and spike trisetum (Trisetum
spicatum) constitute the rest of the graminoid layer. Other common species
include blackroot sedge, curly sedge, Parry’s rush (Juncus parryi), Idaho
fescue (Festuca idahoenisis), spike
fescue (Festuca kingii), and purple
reedgrass (Calamagrostis purpurascens)
(Cooper et al., 1999).
Southwestern
Montana alpine turf communities include additional forb species more common in
the middle Rocky Mountain region. Species include alpine
forget-me-not (Eritrichium nanum), Ross
avens (Geum rossii), common
alp lily (Lloydia serotina), and sheep cinquefoil (Potentilla ovina).
Fern allies such as lesser spike moss (Selaginella densa) can be common. Moss and lichen
cover is typically very low within well developed turf, but is higher in areas
with the stoniest soils adjacent to fell fields and scree slopes with late
persisting snowfields. Mat forming, woody species such as arctic willow, arctic
dryad, snow willow (Salix nivalis),
and within the island mountain ranges, bearberry (Arctostaphylos uva-ursi) are usually present within the turf.
Throughout
its range in Montana,
this system intergrades with scree and talus and alpine fell field communities
in areas with decreasing levels of soil development. Turf development can still
be evident but is discontinuous due to high rock content and very shallow soil
development. In these areas, the turf community intergrades with fellfield
species and early colonizers such as arctic dryad (Dryas octopetala), yellow sweetvetch (Hedysarum sulphurescens), shrubby cinquefoil (Dasiphora fruticosa), silver lupine (Lupinus argenteus), crazyweed (Oxytropis
species) and milkvetch (Astragalus species).
These nitrogen-fixing species accumulate litter within the mats, thus facilitating
additional species colonization from the adjacent turf community. Species
within the stoniest soils typically include yarrow (Achillea millefolium), penstemon (Penstemon species), phacelia (Phacelia
species), alpine fireweed (Chamerion
latifolium), explorer’s gentian (Gentiana
calycosa), twinflower sandwort (Minuartia
obtusiloba), moss campion,alpine goldenrod and aster (Symphyotrichum species). Many of the cushion species
are very long lived, well adapted to limited available water during growth and
possess a deep, fleshy taproot. These species will persist for decades within
the turf as it develops. Early successional graminoids in these areas include
Dunhead sedge, Hayden’s sedge, Drummond’s rush, alpine bluegrass, slender
wheatgrass, Sandberg’s bluegrass, and spike trisetum. These same species
frequently colonize disturbed areas within the turf community such as grizzly
bear diggings and ground squirrel burrows.
Imbedded
within this system is a mosaic of alpine plant communities that vary in composition
depending on soil development, snow retention, subterranean hydrology and
localized topography. Snow bed communities dominated by ericaceous dwarf shrubs
and willows often occur in as well as alpine wet meadows dominated by tufted
hairgrass (Deschampisa cespitosa).
Alpine
turf communities are often bordered by subalpine forest krummolz mats and the
upper elevational limit of subalpine forests. The most common forest
association in Montana
is whitebark pine-subalpine fir (Pinus
albicaulis-Abies lasiocarpa).In
scattered locations on north and east facing aspects, turf communities are
bordered by alpine larch(Larix lyallii)forests.
Historically, stand-replacing fires occurred infrequently in adjacent associated subalpine woodlands (Arno 1980). Lightning strikes can cause fire within these systems, although severity and spread is usually limited and variable. Major disturbances in this system include high elevation mining, heavy recreational use, and grazing. Changing climatic patterns will impact this system and the distribution of peripheral species, northern Rocky Mountain endemics and rare species that occur within it.
Due to the very slow rate of community development, short growing season, and limited soil development, alpine turf cannot support heavy levels of disturbance such as repeated grazing, land disturbance and heavy foot traffic.
L. Vance, T. Luna