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You are here >1Up Info > Wildlife, Animals, and Plants > Plant Species > Shrub > SPECIES: Acer glabrum | Rocky Mountain Maple
 

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BOTANICAL AND ECOLOGICAL CHARACTERISTICS

SPECIES: Acer glabrum | Rocky Mountain Maple

GENERAL BOTANICAL CHARACTERISTICS:


Rocky Mountain maple is a native, deciduous tall shrub or small tree [56,66,74,123,141,159,169,172,203,256,310,325,328,333]. It often grows 20 to 30 feet ( 6.1-9.1 m) tall, with crown widths from 10 to 20 feet (3-6 m) wide and a stem diameter up to 12 inches (30.5 cm) [74,123,150,156,172,175,203,234,243,310,325,328], though it can reach 40 feet (12.2 m) tall [169,259] and 2 feet (0.6 m) in diameter [169]. Rocky Mountain maple is usually tall and spindly in closed stands, with a more dense and brushy growth form in open stands [233,234]. Though it may have a single dominant stem [80], Rocky Mountain maple most often occurs as a multi-stemmed shrub 5 to 6.5 feet (1.5-2 m) tall [74,80,123,169,172,325].

Rocky Mountain maple has opposite, ascending to erect branches, rounded twigs, and a narrow crown [123,150,325]. The bark of Rocky mountain maple is smooth until maturity, when fissures develop [150,156,159,310,325]. Rocky mountain maple has a wide, spreading root system with a combination of deep and lateral woody roots [123,310,325].

Rocky Mountain maple may be monoecious [74,123,150,172,203,256,310] or dioecious [74,123,141,172,203,310,325,328]. Flowers are borne in loose terminal cymes arising from lateral buds [74] and grow in drooping clusters [123]. The paired seeds are winged samaras [74,123,141,150,325,328]. Seeds are 0.16 to 0.2 inch (4-5 mm) long [256] and samaras are 0.08 to 0.12 inch (20-30 mm) long [203].

RAUNKIAER [262] LIFE FORM:


Phanerophyte

REGENERATION PROCESSES:


Seed production:
The mating system of Rocky Mountain maple is dioecious or staminate plants with some bisexual flowers [136]. Rocky Mountain maple likely begins to produce seed before 10 years of age [243]. The large seeds [128] are dispersed by wind [123,176,256,284,294,295], and Rocky Mountain maple often seeds into disturbed areas [62]. Seeds are both animal and wind pollinated [256]. Existing literature is conflicting regarding on-site seed storage; Stathers and others [289] report that Rocky Mountain maple regenerates from seed stored on-site, while Steele and Geier-Hayes [291,294,295] state that seed is not stored. Large seed crops occur every 1 to 3 years [123,243]. Seeds remain viable for short periods of time, losing their viability during dry, frosty periods [123]. Rocky Mountain maple seeds germinate in partial shade on mineral soil [86,123,294,295] or shallow organic layers [123]. Due to embryo dormancy, Rocky Mountain maple seeds require approximately 6 months of chilling to germinate [279].

Vegetative regeneration:
Following stem damage or top-kill, Rocky Mountain maple readily resprouts from the root crown [33,62,72,123,176,186,193,295]. Resprouts may not set seed for 3 years after disturbance [72].

Development:
Rocky Mountain maple experiences a rapid increase in height following disturbance, which tapers off around 20 years post-disturbance. Growth modeling estimates that Rocky Mountain maple may reach 4.2 feet (1.3 m) 2 years after disturbance and 10 feet (3 m) by 10 years after disturbance [178], and may overtop even rapidly growing tree seedlings [215]. Maximum heights are reached approximately 30 to 40 years after disturbance [233], on sites with 40 to 50% of full sunlight [144]. Even in closed canopies, Rocky Mountain maple grows above the dominant shrub layer [56].

SITE CHARACTERISTICS:


Temperature:
Rocky Mountain maple occurs in subalpine boreal, boreal, temperate, semiarid, and mesothermal climates [164,167]. Approximate temperatures on Rocky Mountain maple sites range from 14 to 75 degrees Fahrenheit (-10-24 oC) [188,257,265,313]. Annual precipitation may by as low as 9 inches (229 mm) and as high as 60 inches (1,542 mm) [100,127,177,188,257,313,316].

Location:
Rocky Mountain maple occurs on wetlands, streambanks, canyons, and upland mountain slopes [2,71,72,74,158,172,239,263,265,307,325]. Though it occurs on both moist and dry sites [4,21,30,31,61,74,123,151,190,203,310,312], Rocky Mountain maple is more closely tied to drainages in arid zones of its distribution [79,97,177,310,311,324,325], but occurs on drier exposures northward and at higher elevations [325]. On upland sites, Rocky Mountain maple grows on lower, mid, and upper slopes [82,177,228,236,271], alluvial terraces [123,259], summits, ridgetops [4,177], snow chutes [122,123,204], and talus slopes [166,174,204,208]. Rocky Mountain maple is found on gentle, moderate, and steep slopes [82,177,188,189,205,228,233,290,336], with slopes ranging from 15 to 67% [3,99].

Elevation:
In southern California, Rocky Mountain maple is found from 5,980 to 10,000 feet (1,823-3,048 m) [222,316]. In Arizona and New Mexico, it is found between 5,000 and 12,000 feet (1,524-3,658 m) [7,47,79,82,153,203,221,228,261,307,324] on all aspects [4,81,177,192,228,311,324]. The lower elevation sites are often along streams or drainages [47,48,81,99,177,221,228]. In Colorado and Utah, Rocky Mountain maple grows at 5,000 to 12,700 feet (1,524-3,871 m) [40,93,130,159,174,175,205,242,290,310,336], with northern aspects being optimal for growth and establishment [310].

In northern California, northwestern Nevada, and Oregon, Rocky Mountain maple is common between 2,800 and 9,000 feet (853-2,743 m) [64,175,244]. In Idaho, Montana, and Washington, Rocky Mountain maple occurs between 1,500 and 8,900 feet (457-2,712 m) [36,56,70,75,91,112,196,257,269,293,295,335] on all aspects [61,100,196,234,249]. On sites in Idaho, percent cover of Rocky Mountain maple increased with elevation, but frequency did not [339]. Though it occurs on all aspects, studies in northern Idaho found that Rocky Mountain maple had significantly greater (F=0.05) percent cover on southern aspects than on northern aspects [233]. In British Columbia, Rocky Mountain maple occurs from 1,148 to 4,760 feet (350-1,450 m) [188,189].

Soils:
Rocky Mountain maple occurs on silty, loamy, sandy, gravelly, and rocky soils [45,100,127,177,205,228,290,325,336], with a moderately acidic to slightly basic pH [290,310,325]. It grows on sandstone, limestone, basalt, gneiss, rhyolite, calcareous, and granitic parent materials [45,64,100,112,127,205,290,316]. Rocky Mountain maple grows on shallow [123,233] as well as relatively deep [100,150,228,233,236,310], well developed soils [3,4,156]. Rocky Mountain maple has high requirements of calcium, magnesium, nitrogen, potassium, and phosphorus [123,167,233]. In British Columbia, it is reported to be an indicator of nitrogen-rich soils [164].

Drought and Shade Tolerance:
Rocky Mountain maple occupies well-watered [164] and well-drained sites [45,100,123,177,228,310,325], though it will tolerate imperfectly drained soils, periodic flooding, and moderately high water tables [90,166,167,325]. Rocky Mountain maple occupies sites with a range of moisture levels, competing by adjusting total leaf area through stomatal control and shifting the water potential of its leaves [123]. Rocky Mountain maple has a weak to moderate drought tolerance [310,325] and is winter hardy [123,167,169,325]. It is also moderately shade tolerant [123,226,310,325], but experiences more vigorous growth and fruiting in full sun [325].

SUCCESSIONAL STATUS:


Rocky Mountain maple occurs in old-growth and second-growth forests [13,148,187,209,257]. It is found in early seral stages [12,15,23,30,71,72,109,126,145,176,193,199,201,208,257,266,294,318,338,339], growing within the first 10 years following fire [303] through mature and climax stages [12,15,23,56,67,72,108,115,120,128,148,201,225,226,257,266,294,302,333,338,339]. In British Columbia, Rocky Mountain maple is common in deciduous pioneer forest communities [69] and in late successional and climax floodplain vegetation [60]. On sites in northern Idaho, Rocky Mountain maple was present in unlogged stands as well as stands 7, 14, and 25 years following logging. However, the presence of Rocky Mountain maple was found to decrease in later successional stages [333]. Also in northern Idaho, Rocky Mountain maple was found in closed, non-disturbed stands as well as stands subjected to various harvest and burn treatments [233]. As a prolific resprouter, Rocky Mountain maple rapidly revegetates disturbed areas [56]. Rocky Mountain maple is one of the most common deciduous species occurring on mesic sites in avalanche paths due to its ability to survive avalanche impact pressures via resprouting, and is characteristic of avalanche paths in northern Montana [52,53].

Rocky Mountain maple is a major component or dominant in seral shrub-dominant vegetation, which develops rapidly following disturbance in the northern Rockies [36,55,57,58,70,105,113,114,125,133,184,245,299,329,338]. Seral shrubfields result from recurring disturbance including fire and downslope movement of snow, ice, water, and rocks [55,184]. These shrubfields may actually inhibit tree seedling establishment through direct competition and indirectly by providing habitat for browsing animals that damage seedlings [125]. The Rocky Mountain maple/mallow ninebark complex frequently becomes dominant on sites in the northern Rockies [65]. Similar seral shrubfields occur in the southern Rockies. Rocky Mountain maple may actually provide shade to Douglas-fir seedlings aiding in establishment and survival [63].

Rocky Mountain maple may have higher percent cover or occur with greater frequency on more open sites [145,173]. However, Antos [15] found that Rocky Mountain maple shows little response to successional development, maintaining >5% cover in both young and old stands. Rocky Mountain maple is described as shade intolerant to shade tolerant [128,164]; the ability to persist in heavy shade makes it an important species in closed canopy stands [234].

SEASONAL DEVELOPMENT:


Bud swell of Rocky Mountain maple occurs from late March through April [88,246], with bud burst occurring in early April to mid-May [88,123,275]. Leafing out occurs between mid-April and late May [88,135,246], with leaf growth occurring into late June [88,123,275]. Stem elongation begins in late April and continues to late August [88,246]. Rocky Mountain maple flowers from late April to late June [88,123,159,203,246,275]. Buds form in early to mid-July [88]. Fruit develops from June through August [246], and ripens from July into October [123,243,275]. Seed dispersal begins in September [123,243,275], but seeds may remain on stems as late as February [123,243]. Foliage coloration extends from early August to early September [88,123,275], and leaf fall lasts from early August to mid-November [88,123,246,275]. The timing of foliage coloration and leaf fall of Rocky Mountain maple may be related to moisture availability [88].

Related categories for SPECIES: Acer glabrum | Rocky Mountain Maple

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Information Courtesy: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory. Fire Effects Information System

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