Picea glauca (white spruce) is the provincial tree of Manitoba and the state tree (as Black Hills spruce) of South Dakota.
PLANT COMMUNITIES:
White spruce communities are widespread throughout the North American boreal region [119,318]. White spruce becomes increasingly prominent in forests from the moist east to the drier west and northwest [356,358]. Many factors contribute to plant species composition in white spruce communities, including climate, topography, drainage, presence and thickness of permafrost, fire history, and forest age [64,102,425].
See Appendix B for scientific names of taxa mentioned in this review and for links to available FEIS reviews.
White spruce grows in pure and mixed stands [114,119,137,178,318,425]. Associated trees across much of its range include quaking aspen, paper birch, black spruce, and balsam poplar. Balsam fir commonly occurs with white spruce from Saskatchewan eastward [230]. Rocky Mountain lodgepole pine, hereafter lodgepole pine, is a common associate in the northwest Cordilleran region (Alberta foothills, northern British Columbia, and the Yukon) [358]. Other trees that commonly occur with white spruce include red spruce, yellow birch, jack pine, and sugar maple in the east; and subalpine fir and Rocky Mountain Douglas-fir (hereafter, Douglas-fir) in the west [118,119,230,318,358,433,467].
Tall shrubs and low trees associated with white spruce vary across its range. In the northwest, willows are most frequent; in the central region, mountain alder, pin cherry, and chokecherry are most frequent; in the east, mountain apple, northern mountain ash, and beaked hazelnut are common. American green alder occurs throughout much of white spruce's range. Medium and low shrubs associated with white spruce across much of its range include highbush cranberry, swamp red currant, prickly rose, and red raspberry. Other low shrubs that are regionally common include: russet buffaloberry from Alaska to central Alberta; common juniper from northern British Columbia to Lake Winnipeg; Saskatoon serviceberry from the Northwest Territories to northwestern Ontario; limber honeysuckle from Great Slave Lake to Lake Michigan; and bush-honeysuckle from Lake Winnipeg to western Quebec [230].
Herbaceous plants and dwarf shrubs associated with white spruce across much of its range include fireweed, sidebells wintergreen, single delight, twinflower, naked miterwort, bunchberry, and lesser rattlesnake plantain. Several herbaceous plants and dwarf shrubs that commonly occur in white spruce stands have more regional distributions [230].
White spruce codominates with quaking aspen [118], paper birch [467], and black spruce [433] over large areas. The white spruce-aspen forest cover type occurs in all the western provinces of Canada, the Northwest Territories, and Alaska on upland sites [118]. The white spruce-paper birch forest cover type has a similar distribution but may also occur along rivers [467]. Both the white spruce-aspen and white spruce-paper birch communities frequently precede late-successional white spruce forest [118,467]. Black spruce-white spruce woodland and forest types occur in northwestern Alaska and extend eastward to the Hudson Bay in Canada [433]. These communities frequently occur in open stands at alpine treeline throughout interior Alaska and northwestern Canada.
For a list of plant communities in which white spruce may occur and information on associated FIRE REGIMES, enter “white spruce” in the FEIS home page under "Find FIRE REGIMES". More detailed descriptions of white spruce communities follow by region.
Alaska: White spruce dominates or codominates many Alaskan boreal landscapes [263,303,434,435]. It is widespread in south-central and interior Alaska, extends to the limits of tree growth along the Brooks Range [152,425], and is less common in coastal regions [118]. At the landscape level, Alaskan white spruce communities form mosaics with quaking aspen, paper birch, balsam poplar, black spruce, and mixed forest stands [416,462]. The distribution of vegetation types is determined by past wildfires, altitude, soil drainage, topography, presence or absence of permafrost, and climate [428,430]. The sharp boundaries between stands of quaking aspen or paper birch and white spruce indicate edges of fires [263]. White spruce generally occupies upland, warm, well-drained, permafrost-free sites [263,425,428,457] (see Site Characteristics), whereas black spruce generally occupies cold, poorly drained sites with shallow permafrost [263,457].
Alaskan white spruce communities typically occur in riparian, upland, and treeline sites [83]. Extensive riparian white spruce stands are highly productive [303,356,425] and occur along valley floors and river terraces with permafrost deep underground or no permafrost at all [83,415,425]. Upland white spruce generally occurs on well-drained, south-facing slopes less than 1,300 feet (400 m) above sea level and may have a deep permafrost layer [136,413]. Upland forests are productive, but less so than riparian forests [83]. White spruce dominates treeline stands at the forest-tundra ecotone [152]. These forests have low productivity and have widely spaced, slow-growing tress [83,152].
In Alaska, white spruce may occur in pure or mixed stands, but pure stands typically occur only in areas where fire is infrequent [263] or at elevational treeline [303]. Mixed stands, including white spruce-quaking aspen, white spruce-paper birch, and balsam poplar-white spruce communities, often represent intermediate successional stages that are later replaced by white spruce types [118,136,263,467]. White spruce-quaking aspen communities establish after fire on warm, well-drained, upland sites and are generally replaced by white spruce types after 100 years or more [118,136,263]. White spruce-paper birch stands typically occur on upland sites but also occur along rivers [263,467]. Balsam poplar-white spruce stands occur on floodplains before succeeding to white spruce [425] (see Successional Status).
Black spruce-white spruce forests and woodlands are common in interior, south-central, southwest, and northwest Alaska, especially near treeline [136,310]. In interior Alaska, these forests occur wherever the white spruce type and black spruce type overlap. This occurs most frequently on lower, southerly slopes where white spruce forests meet black spruce muskegs on valley bottoms and near treeline [136]. Permafrost is often present at 20- to 24-inch (50-60 cm) depths, but it may be absent. Many of these communities may be climax or successionally stable. Other stands, especially those in floodplains, may transition from white spruce to black spruce in response to increasing organic layer thickness, rising permafrost, and decreasing soil temperature and drainage (see Successional Status) [425].
White spruce occurs as a minor component in many communities where it is not dominant or codominant. It may occur in unproductive or poorly drained black spruce forests, paper birch forests and woodlands, alder shrublands, birch-willow shrublands, and mesic birch-ericaceous shrublands [425].
NatureServe [300,301] identifies the following white spruce forest and woodland types in Alaska.
Montana: White spruce and western white spruce occur in northwestern Montana in the northern Rocky Mountains where they associate with Douglas-fir, western larch, and lodgepole pine [166,331]. In western and central Montana, white spruce, western white spruce, or Engelmann spruce communities often dominate coniferous riparian sites. White spruce tends to occur at lower elevation sites, while Engelmann spruce dominates higher elevation sites; western white spruce occurs where the 2 spruces overlap [166]. Western white spruce occurs in seral stands of subalpine fir/queencup beadlily stands [331].
NatureServe [300,301] does not identify any white spruce types or associations in Montana, but the following western white spruce associations occur in Montana:
Northwestern Great Plains: White spruce has limited distribution in the Black Hills of South Dakota and Wyoming. White spruce stands occur at high elevations of the subalpine zone and in cool canyon bottoms [184]. In some areas, it is an overstory dominant, but it is often codominant with or subordinate to interior ponderosa pine (hereafter, ponderosa pine) [399]. White spruce is considered the climax species in some ponderosa pine and quaking aspen stands [184,372]. White spruce occurs rarely in the subalpine forests of Bighorn National Forest, Wyoming [286].
Two white spruce habitat types are identified in the Black Hills: white spruce/twinflower and white spruce/grouse whortleberry [184]. White spruce/twinflower typically occurs on northwest- to northeast-facing slopes. Ponderosa pine and quaking aspen are frequent seral species. The white spruce/grouse whortleberry habitat type generally occurs on cool and moist sites at somewhat higher elevations than other local forest habitat types [184].
NatureServe [300,301] identifies the following white spruce woodland type in the northwestern Great Plains:
Great Lakes: White spruce occurs in mixedwoods, swamps, bogs, stream borders, and on wooded dunes and gravelly shores in the Great Lakes region [438]. It often codominates with balsam fir in mixed forests [77,87,277]. However, white spruce may not be abundant in some balsam fir-white spruce-paper birch stands [52,77]. White spruce is an associate in the jack pine [271], balsam fir [141], black spruce [92], tamarack [205], paper birch [362], red pine [30], and black ash-American elm-red maple [359] forest cover types.
Balsam fir-white spruce forests occur in northern Minnesota [144,229]. In the Boundary Waters Canoe Area, northeastern Minnesota, white spruce is often confined to lakeshore and wetland refuges from fire [143]. It also occurs in upland communities and in intermediate-aged stands [162,307,309]. White spruce often grows in the understory of jack pine, black spruce-jack pine, red maple-quaking aspen-paper birch, eastern white pine, red pine, and northern white-cedar communities [307,309].
In northern Wisconsin, old stands of white spruce-balsam fir are associated with eastern white pine, red pine, and northern white-cedar. On inland mesic sites, shade-tolerant hardwoods gradually replace white spruce and balsam fir. Young stands of dense balsam fir and white spruce also occur under aging quaking aspen or paper birch stands [87]. White spruce occurs in eastern white pine, eastern hemlock, and sugar maple-American beech habitat types, where it typically has low cover [224].
In Isle Royale National Park, Michigan, balsam fir-paper birch-white spruce dominates late-successional communities. Although white spruce is less common than balsam fir and paper birch, occurring only sparingly in most places, it is most conspicuous because it is usually taller [77].
NatureServe [300,301] identifies the following white spruce forest type in the Great Lakes region:
Northeast: In northern New England and New York, white spruce occurs in many community types where it does not dominate. In the northeastern United States, white spruce is associated with red spruce, northern white-cedar, and jack pine [300,301,318]. In northern New England, white spruce occurs in both late-successional and second-growth forests and may be associated with paper birch, quaking aspen, balsam fir, red spruce, yellow birch, and sugar maple [318]. It occurs as a minor type on abandoned agricultural lands in northern New England [95,318]. In New York, white spruce occurs in Adirondack spruce-fir swamps and spruce flats, calcareous pavement barrens, and limestone woodlands [342]. In coastal Maine, white spruce is associated with red spruce and balsam fir [95,318]; pure stands of white spruce occur along the shore [95].
NatureServe [300,301] identifies 2 white spruce associations in the northeastern United States:
Western Canada: In British Columbia and Alberta, white spruce is widespread and occurs with black spruce, lodgepole pine, subalpine fir, Douglas-fir, quaking aspen, Engelmann spruce, and balsam poplar [80,285]. White spruce is especially important in the Boreal and Montane Forest regions in western Canada [357]. It occurs from lower elevations in the boreal mixedwoods through the subalpine zone [80,285]. In northern British Columbia, the low and middle elevation boreal forest is dominated by white spruce, black spruce, and lodgepole pine; the subalpine forest is dominated by white spruce and subalpine fir [285]. In the boreal mixedwoods of west-central Alberta, white spruce is most abundant in older stands on wetter sites; quaking aspen tends to dominate the drier, well-drained sites and white spruce occurs in the understory [80]. On a landscape scale, white spruce communities form mosaics with early-seral stands dominated by lodgepole pine and quaking aspen [332].
For more information on white spruce communities of western Canada, see these sources [2,107,231].
Where white spruce and Engelmann spruce occur in the same area, white spruce predominates in lower elevations in valley bottoms, whereas Engelmann spruce dominates higher elevations. Hybrids occur where the 2 species overlap [2,193,305].
In boreal forests of south-central and eastern Yukon, white spruce and black spruce are climax species on moderate- to well-drained sites, and black spruce is climax on poorly drained sites. However, most communities are dominated by lodgepole pine due to fire setting back succession. In southwestern Yukon, black spruce or mixed black and white spruce form the climax community due to the presence of permafrost. White spruce is also common at arctic treeline and alpine treeline in the west and north [313].
In the forest-tundra ecotone in the Northwest Territories, white spruce grows in an open parkland. White spruce dominates the well-drained, drier sites, while black spruce dominates the more mesic areas [270]. On the Mackenzie River Delta, late successional white spruce woodlands occur on the most elevated sites. Four distinct white spruce communities are recognized based on differences in site characteristics, understory species composition, and tree age. Moisture regimes range from xeric in the white spruce/lichen-crowberry association to hygric to poorly-drained in the white spruce-tamarack/sphagnum bog-type woodland [321]. In poorly drained bogs, white spruce occurs with [249] or without black spruce [321].
Old-growth riparian white spruce forests in western Canada are often restricted to terraces of major river valleys where flooding rarely occurs because terraces are elevated and well-drained. Fire is limited because moist floodplains, wide channels, oxbows, and low fuel loadings act as natural firebreaks. On wet, poorly-drained riparian sites, white spruce/field horsetail forests generally develop from balsam poplar/red-osier dogwood stands after 100 to 300 years. On mesic sites associated with lakes and sloughs, floodplain terraces, and steep wooded draws, white spruce/highbush cranberry develops from quaking aspen/highbush cranberry or balsam poplar/red-osier dogwood stands after 100 to 300 years. Although this is a major type at low- to mid-elevations in the Boreal Forest Natural Region, old-growth stands are rare because stands often burn before they reach advanced maturity [403].
NatureServe [300,301] identifies several white spruce forest and woodland types in western Canada:
NatureServe [300,301] identifies the following white spruce woody wetlands and riparian types in western Canada:
Central and eastern Canada: White spruce typically occupies approximately 10% of the canopy in the southern boreal mixedwood forests of central and eastern Canada (reviewed in [100,101,102]). However, white spruce is locally dominant in some stands on the Atlantic coast [315,318,320]. White spruce stands are also found at the altitudinal treeline of the highest plateaus; the southernmost subalpine white spruce stands occur on an extensive high plateau of the Gaspé Peninsula [100,101]. The central and eastern portions of the Boreal Forest Region [357] are characterized by black and white spruce, balsam fir, and jack pine with varying amounts of eastern white and red pine, yellow birch, sugar maple, black ash, and northern white-cedar in the east. The Great Lakes-St. Lawrence Forest Region [357] is characterized by eastern white and red pines, eastern hemlock, and yellow birch. These mixed forests often include several hardwood species including sugar maple, red maple, northern red oak, basswood, and white elm as well as boreal species including white and black spruce, balsam fir, jack pine, quaking aspen, balsam poplar, and paper birch. In the Acadian Forest Region (New Brunswick, Nova Scotia, Prince Edward Island) [357] of the Maritime provinces, where red spruce and associated balsam fir, yellow birch, and sugar maple are dominant, white spruce has increased importance since the 1900s due to widespread invasion of abandoned farmland.
In the boreal lowlands of the Saskatchewan River delta in east-central Saskatchewan, white spruce-hardwood forests are confined to raised alluvium levees with relatively dry moisture regimes and no peat. Associated hardwoods include balsam poplar and American elm. Associated ground cover species depend on the site but often include meadow horsetail, wild sarsaparilla, and bluejoint reedgrass [106]. In subarctic northeastern Saskatchewan, black spruce dominates forest and woodland communities and white spruce is uncommon [16]. In the dry grassland region of southwestern Saskatchewan, white spruce forests occur on the Cypress Hills plateau, typically on cool, moist sites [47,402]. Balsam poplar and quaking aspen are frequent associates. At higher elevations, white spruce transitions to lodgepole pine. In closed stands on relatively dry, well-drained soil, there is little ground cover, whereas moist sites contain tall and low shrubs, herbaceous plants, and mosses [47].
The boreal forest in northern and central Manitoba is characterized by conifers including black spruce, jack pine, balsam fir, white spruce, and tamarack. Mixed conifer-hardwood stands may include quaking aspen, paper birch, and balsam poplar. White spruce mixedwood communities occur late in succession on well-drained, moist soils. Other white spruce communities include white spruce mixedwood/feather moss and white spruce/balsam fir shrub [477]. In northern Manitoba, white spruce is confined to alluvial deposits and eskers (areas lacking peat). On the Hudson Bay Lowlands, pure white spruce stands have a sparse shrub strata and either an herbaceous understory or a moss-dwarf shrub understory [344].
In the Maritime provinces, white spruce occurs in pure stands, mixedwoods, and predominantly hardwood stands. Pure stands occur on abandoned farmland and along the coastline, especially in cleared or disturbed areas. On many sites, white spruce occurs in mixed conifer stands in valley bottoms and on steep slopes of narrow valleys. On upland slopes, rolling hills, and flats, white spruce occurs in mixedwoods with red spruce, balsam fir, sugar maple, yellow birch, and red maple. In the New Brunswick Highlands Ecoregion, balsam fir, white spruce, black spruce, paper birch, and eastern white pine occur on the well-drained slopes. Along the Atlantic coast, white spruce, black spruce, and balsam fir dominate the mostly open, windswept stands. On some sites, white spruce dominates the immediate coast, whereas black spruce and balsam fir are more abundant farther inland. White spruce also occurs with eastern hemlock and red pine in the Maritime provinces [261].
In central Newfoundland, white spruce is most often associated with moist balsam fir-paper birch forests that have a splendid feather moss ground cover. These forests are comprised of a dense balsam fir overstory and scattered paper birch and white spruce and occasional black spruce. This forest type typically occurs on middle and lower seepage slopes on rugged terrain and moist soils. Scattered white spruce also occurs in balsam fir/woodfern-clubmoss forests and alder swamps [91]. White spruce is rare in southeastern Labrador where the cool maritime climate enables the development of a thick bryophyte layer and deep organic humus [140].
NatureServe [300,301] identifies several white spruce forest and woodland types in central and eastern Canada:
Botanical description: This description covers characteristics that may be relevant to fire ecology and is not meant for identification. Keys for identification are available (e.g., [110,151,197,268,369,438]).
Morphology: White spruce grows as a medium-sized tree or as a shrub. Trees typically average 80 feet (25 m) tall [194] but mature trees may exceed 100 feet (30 m) and 24 to 36 inches (60-90 cm) in diameter on favorable sites. The tallest individuals are more than 180 feet (55 m) tall [305]. In Alaska, white spruce is typically 40 to 70 feet (12-21 m) tall [435]. Prostrate and krummholz forms are common at or near treeline [18,93,152,272,369,396], where mature trees are often only 3 to 6 feet (1-2 m) tall [369,435], and sometimes only 4 to 8 inches (10-20 cm) tall [396].
The arrangement of vertically continuous branches may promote ignition and torching in white spruce [114,462,466]. White spruce trees typically have a straight bole with a broadly conical to narrow, almost linear crown and slightly drooping branches [135,194,197,435]. Trees in Alaska commonly have narrow, spire-like crowns [194,251], whereas in the northeastern United States, trees are narrow but not typically spire-like [151]. White spruce trees are typically much narrower than black spruce trees [406]. Crowns are usually densely foliated [129,356,394], and branches and needles are often retained low on the trunk [114,171,194,204,263] but sometimes are not [405]. Trees may shed their lower branches when growing in dense stands with low light [194]. The bole has thin smooth, scaly, or flaky bark, generally less than 8 mm thick [394]. Needles are short, ranging from 0.2 to 0.75 inch (5-18 mm) long [194,438]. The needles and bark are resinous [303], although less so than those of black spruce [405]. The pendulous cones are 1 to 2.4 inches (3-6 cm) long [197,435] and hang from the upper branches [314]. Seeds have a long, thin wing that is 2 to 3 times as long as the seed [435]. White spruce seeds are small (~0.001-0.003 gram) [82,471] but are larger and heavier than those of many associated boreal trees (e.g., paper birch, quaking aspen, black spruce, tamarack, alders, willows) [264,470].
Figure 6. White spruce tree, Itasca State Park, Minnesota. Figure 7. White spruce cones. Photo by Joseph O'Brien, USDA Forest Service, Bugwood.orgWhite spruce has lateral, vertical, layered, and adventitious roots [56,439]. The root system tends to be shallow [129,194,413]. Most roots grow in the upper 6 to 12 inches (15-30 cm) of soil, in the organic-mineral soil interface or almost entirely in the organic mat, but taproots and sinker roots may reach 10 feet (3 m) deep (reviewed in [56,413]). Multilayered, secondary, and adventitious root systems occur on floodplains as a response to alluvial deposits and increases in humus and feather moss [201,439]. Adventitious roots generally establish on young trees and seedlings and extend laterally in the organic-mineral soil interface. Adventitious root development in alluvial deposits results in mature white spruce with strong lateral and sinker roots [439].
Stand structure: White spruce stand structure varies tremendously [90,300,301,435], ranging from open woodlands at treeline [300,301], on dry sites, and on high benches [171], to closed forests in lowland mixed stands [300,301]. White spruce trees growing in open woodlands tend to have broad crowns, short stature, and branches that extend to the ground [171]. In Alaska, open white spruce types generally have a vigorous understory, whereas closed stands may have few vascular plants and a deep, continuous moss cover [303]. On the northern Alaskan forest-tundra treeline, tree density and mean tree height decrease with increasing elevation [152].
White spruce tree density tends to decline with increasing stand age [263,303,426] or peak before stands senesce [17,404]. In the white spruce forest type in interior Alaska, white spruce densities are often high in young (20- to 25-year-old) stands with 2,000 to 3,000 trees/acre (4,900-7,400 trees/ha); whereas, in older, 160- to 180-year-old stands, density may range from 300 to 500 trees/acre (740-1,200 trees/ha) [263]. On the Tanana River floodplain in interior Alaska, mature white spruce density is highest (up to 800 trees/acre (2,000 trees/ha)) in 100-year-old, even-aged stands, and it declines as stands age, with 210 trees/acre (520 trees/ha) in 250-year-old, uneven-aged stands [426]. However, in interior Alaska, early seral stages (i.e., quaking aspen and paper birch stages) of white spruce types have fewer mature white spruce than older white spruce stands. In young quaking aspen and paper birch stands, white spruce may average 8 trees/acre (19 trees/ha) and 46 trees/acre (113 trees/ha), respectively. In the mature white spruce stage, white spruce may average 200 trees/acre (496 trees/ha) [136]. In 35 mixedwood stands in Saskatchewan that ranged from <1 to 201 years since fire, density of white spruce peaked 172 years after fire at about 570 stems/acre (1,410 stems/ha) and was about 240 trees/acre (600 trees/ha) in the oldest stands [17].
White spruce usually forms multi-aged stands comprised of trees that establish episodically [17,34,67,145,330,429], although even-aged stands that date back to the last fire sometimes occur [137,430,431,460].
White spruce generally has a moderate lifespan, although individuals at stressed sites such as latitudinal or elevational treeline may be long-lived. White spruce commonly lives 100 to 250 years [137,442], with older trees (250->300 years) occurring in areas that are protected from fire such as islands and river channels [56,358,469]. Treeline sites across its range may support white spruce >350 years old [93,221,319]. The oldest reported white spruce (nearly 1,000 years old) occurs above the Arctic Circle [149].
White spruce is native to the United States and Canada [211,401]. It is primarily a boreal species occurring throughout much of Alaska and Canada, although it extends into the Great Lakes and the northeastern United States. Isolated populations occur in Montana, Wyoming, and South Dakota. White spruce becomes increasingly prominent in forest stands from the moist east to the drier west and northwest [356,358]. In the west, it is widespread in Alaska and all western Canadian provinces; white spruce is especially common in the interior of northern British Columbia [119].
States and provinces [409]:
United States: AK, CT, ID, MA, MD, ME, MI, MN, MT, NH, NY, PA, RI, SD, VT, WI, WY
Canada: AB, BC, LB, MB, NB, NF, NS, NT, NU, ON, PE, QC, SK, YT
Saint Pierre and Miquelon
Prescribed fire after logging: Prescribed fire is often used to consume logging slash, improve seedbed conditions, and promote regeneration after white spruce stands are logged (e.g., [19,163,220,284,325,407,465,476]). White spruce regeneration is variable and often inadequate after logging, in part because logging may not reduce thick organic layers or expose mineral soil [127,148,439,465]. Because white spruce typically establishes best on mineral or thin organic soils [61,71,103,124,206,336,385,439,468,472], prescribed fire may be used to expose mineral soil. In 2 white spruce floodplain forests in interior Alaska, prescribed broadcast burning following logging reduced small-diameter, downed woody fuels by 67% and 81%, and organic horizon depth by 43% and 55%. However, only 13% and 8% of the surface was exposed mineral soil after fire (desired exposed soil was 30%-40%). This was probably because of the high duff moisture content (130%-150%) at the time of burning. While seedbed conditions were somewhat improved by these experimental fires, the authors recommend mechanical site preparation or burning under drier duff conditions to increase mineral soil exposure [476].
Prescribed fire prior to planting white spruce may promote growth by reducing competition and warming the underlying soil [19,284]. In north-central interior British Columbia, white spruce seedlings grew best on severely burned sites. White spruce seedlings were planted on previously harvested sites where prescribed fire left a mosaic of severely burned, lightly burned, and unburned patches. On the severely burned patches, competing vegetation was greatly reduced and most of the organic horizon was removed, whereas on the unburned patches, competing vegetation was dense and averaged 32 inches (80 cm) tall. Competing vegetation and organic matter were barely affected on the lightly burned patches. Two years after planting, seedling growth was highest on severely burned patches (11 inches (28 cm)), followed by lightly burned patches (7.8 inches (20 cm)), then unburned sites (5.5 inches (14 cm)). Seedling survival was significantly higher on lightly burned (100%) and severely burned (83%) patches than on unburned (46%) patches [284].
While prescribed fires typically reduce logging slash fuels and improve seedbed conditions in small patches, regeneration of white spruce by seed is often inadequate because prescribed fires fail to consume sufficient organic material [127,407]). Additional seedbed treatments may be necessary to promote regeneration (reviewed in [472]).
For additional information about prescribed burning on sites that were clearcut in British Columbia see the following Research Papers:
For information about white spruce seedling establishment on experimental prescribed burns in red and eastern white pine forests see the following Research Project Summary:
Prescribed fire for habitat enhancement: Prescribed fire is used to enhance wildlife habitat on white spruce and Lutz spruce sites on the Kenai Peninsula [42,443,452]. Even though these forests probably had very long fire-return intervals historically (MFRI=~515 years) [31], managers were concerned because young birch-willow-quaking aspen habitat and hardwood stands were succeeding to white spruce and mountain hemlock, and moose numbers were declining. In an effort to restore winter range moose habitat and increase moose browse, the Chugach National Forest experimentally burned 12 sites. Sites were burned in May and June before greenup, with and without prior slashing. Burning increased browse production from an average of 9 pounds/acre to 37 pounds/acre by 3 years after fire, and moose used these areas "heavily" during the winter; however, browse quality increased for only 1 year after burning. On sites that were slashed prior to burning, fire intensity, tree top-kill, fuel consumption, hardwood sprouting, and hardwood seedling establishment were generally higher than on sites that were not slashed. Sites that were not slashed had patchier burns. Both burning treatments resulted in low duff reduction (13% on slashed sites, 6% on unslashed site). To generate higher fire intensities on sites that are not slashed, the author suggests burning during the fall [452].
Spruce beetle: There is concern that the extensive tree mortality and associated high fuel loads created by the massive spruce beetle outbreak of the 1990s in south-central Alaska will increase the risk of wildfire, especially in the wildland-urban interface areas around Anchorage and on the Kenai Peninsula [153,190,350,367]. While spruce beetles are within their native range, and outbreaks historically occurred relatively frequently (every ~50 years on average) [31,373], spruce beetle populations in the 1990s outbreak were "unprecedented" (reviewed in [350]). Since the outbreak, surface fuel loads increased as needles, branches, and snags fell to the forest floor. Between 1987 and 2000, fuel heights, fine fuels, and sound large fuels increased in beetle-killed white spruce stands (P=0.05). In unharvested white spruce stands, sound 1000-hour fuels increased by 3.02 tons/acre (P=0.05). In harvested beetle-killed white spruce stands, small fuels (10-hour and 100-hour) increased more than in unharvested stands (P=0.05) [367]. Fires that occur in beetle-killed areas are perceived to be intense and difficult to suppress, and result in "undesirable" conditions where spruce forests are replaced by grasses and shrubs due to a lack of seed source [350].
Dendrological and soil charcoal evidence indicated no association between fire activity and the relatively frequent spruce beetle outbreaks over the past ~2500 years [31]. However, Berg and Anderson [31] caution that the "trend of warmer summers coupled with an increasing human population and associated sources of ignitions may create a greater risk in all fuel types than was present during the time period covered by our study". The human-caused, 2014 Funny River Fire grew uncharacteristically large (195,858 acres (79,260 ha)) in beetle-killed forest on the Kenai Peninsula [7] (Figures 12, 13).
Because spruce beetles typically colonize stressed or dying spruce (e.g., windthrown, fire damaged, logged) (reviewed in [454]), a warmer, drier climate or increased fire frequency may result in increased susceptibility to spruce beetle outbreaks.
For additional information about the effects of spruce beetle outbreaks, see Insects.
Figure 12. Funny River Fire (2014) burning on the Kenai Peninsula. The brown-red area outside of the fire perimeter may be beetle-killed trees. Photo courtesy of Jesse Allen, NASA Earth Observatory. Figure 13. Immediately after the Funny River Fire (2014) on the Kenai Peninsula. Photo courtesy of the Office of the Governor.Eastern spruce budworm: Fire exclusion and climate change may affect eastern spruce budworm dynamics in central and eastern Canada and the northeastern United States. Since fire suppression began in eastern Canada (1920), eastern spruce budworm outbreaks have occurred at shorter intervals, are more widespread, and result in more mortality, especially of white spruce. Fire suppression coupled with logging of eastern white pine resulted in more continuous balsam fir-spruce stands and less of a mosaic comprised of early successional, non-susceptible species (reviewed in [280]). With climate change, wetter conditions are predicted to lengthen the fire-return interval of southeastern Canadian boreal forests [447]. Consequently, more extensive conifer forest may be available to support more extensive insect outbreaks (reviewed in [437]), including eastern spruce budworm.
Fuel loading and fire hazard following eastern spruce budworm attacks vary regionally over time. Eastern spruce budworm-killed trees create dead ladder fuels, which can support fast-moving crown fires [387]; however, live spruce and balsam fir are also highly flammable ladder fuels [392]. Conventional thought is that insect-caused tree mortality enhances fire potential (reviewed in [134,280]); however, this trend may only be supported at short time scales (i.e., <10 years) [134,387]. Over longer time scales, spruce budworm outbreaks may lessen fire risk [392]. In eastern spruce budworm-killed stands in central Ontario, experimental fires were conducted in the spring and summer up to 5 years after trees died. Stands were dominated by dead balsam fir; other trees included eastern white pine, jack pine, white spruce, and birches. Spring fires conducted before the understory vegetation flushed "exhibited spectacular behavior", with crown fire rates-of-spread as high as 269 feet/min (82 m/min). The fires "behaved explosively" regardless of whether the dead crowns were intact or on the ground. Summer fires that were ignited a few years after the trees died failed to spread, even under severe burning conditions. The open tree canopy resulted in a moist, green understory, which reduced fire spread. Fire potential was highest 5 to 8 years after trees died, when surface fuel loads peaked. By 4 to 5 years after the trees died, there were enough woody surface fuels to enable fires to spread in the summer [387].
Following the major eastern spruce budworm epidemic in the 1970s on the Cape Breton Highlands, Nova Scotia, there was little surface fuel accumulation. Balsam fir comprised 90% of the forest and white spruce and paper birch comprised the rest. Dead fuels decomposed rapidly due to the moist climate, and fires were not sustained in budworm-killed stands. Two late spring fires that occurred before understory plants leafed out originated in open fields and spread towards budworm-killed stands. Because there was little surface fuel in the budworm-killed stands, the fires stopped at the stand edge. Only live, young balsam fir trees growing along the edge of the stand were consumed [322]. In the Boundary Waters Canoe Area, simulation models of both presettlement era forests and contemporary forests indicated that area burned and fire severity during outbreak decades were similar to those of non-outbreak decades. Simulated eastern spruce budworm disturbance lengthened the fire-return intervals in both time periods (mean =229.1±6.3 (SE) years) relative to fire-only treatments (mean=199.2±3.1 (SE) years). The authors conclude that periodic eastern spruce budworm outbreaks reduce ladder fuels, which may partially mitigate future fire risk over the long term [392].
Very frequent fires: Repeated fires that occur in short intervals prevent white spruce from regenerating. In central Saskatchewan, agricultural clearance fires in the early 1900s escaped into southern boreal mixedwoods in and adjacent to Prince Albert National Park. Between 1883 and 1942, 81% of the forests burned in 2 or more escaped crown fires. Stands that experienced multiple short-interval fires shifted composition from mainly white spruce to mainly quaking aspen. Since 1883, sample points dominated by white spruce forest types have decreased from 41% to 19%, while sample points dominated by quaking aspen have increased from 29% to 49%. Sample points dominated by jack pine also increased from 8% to 21% at the expense of white spruce-paper birch. In stands that were logged and then burned in escaped fires, white spruce decreased even more than in unlogged stands. Since 1883, logged white spruce forest types decreased from 56% of the sample points to 9%, while quaking aspen-dominated forests increased from 25% to 75%. Because the fires burned in 15- to 20-year intervals, any white spruce that regenerated after the first fires would not have had sufficient time to produce seed before subsequent fires. Consequently white spruce regeneration was limited and populations were substantially reduced [450].
Climate change and fire: Climate change has the potential to affect white spruce distribution, abundance, and growth both directly and by altering FIRE REGIMES.
Increases in fire extent, frequency, and severity could facilitate a shift from coniferous forests to early successional hardwood forest [28,215,274,360]. In interior Alaska, the ALFRESCO model indicates that climate-driven changes in the fire regime are already occurring and will continue over the next 30 years. Hardwood stands have already replaced black and white spruce stands at many sites. By 2020, the replacement of spruce by hardwoods is predicted to slow because hardwood cover will be twice that of spruce. Additionally, once the fire-return interval drops below a threshold of 60 to 80 years, the model predicts that spruce will be increasingly excluded because they will not have enough time to replace faster growing hardwoods before subsequent fires. The future forest predicted by the ALFRSCO model may be similar to the poplar-dominated parkland of the early Holocene and the present-day boreal mixedwoods of south-central Canada, which grow under slightly warmer and drier conditions than forests in interior Alaska [274].
Logistic regression simulation models indicate that climate change (temperature and/or precipitation), fire frequency, and especially their interactions will affect the distribution of white spruce in interior Alaska in future years. With a warming climate and without increasing precipitation, white spruce distribution is predicted to decline; the drier the climate, the faster the decline. However, if precipitation increases as temperature increases (predicted increase 1.8-9 °F (1-5 °C)), white spruce distribution could expand to roughly twice its current distribution, peaking at 3.6 °F (2 °C) warming. With even greater increases in temperature and precipitation, the pattern is reversed: Under the Hadley CM2 model, which predicts increases in average growing season temperature of 5 °F (2.8 °C) and precipitation (+6 %) for interior Alaska by 2100, the landscape is predicted to consist mostly of black spruce, some hardwoods, and very little white spruce at intermediate elevations, and tundra at high elevations. Under this scenario, white spruce forest is predicted to decrease from 9% to 2% cover in interior Alaska [57].
With an unchanging climate, a lengthening or shortening of the fire-return interval by 30% is predicted to result in slight increases and decreases in white spruce distribution, respectively. However, increases or decreases in the fire-return interval accompanied by either a wetter or drier climate could lead to substantial declines in white spruce distribution. While these models are based on empirical data, they lack regional-scale (remotely sensed) validation data that distinguish black spruce from white spruce. In addition, it is unclear how processes such as seed dispersal, establishment, changes in soil conditions, and thawing permafrost are captured by the models [57].
See Climate change in Other Management Considerations and FIRE REGIMES of Alaskan white spruce communities for more information on this topic.Of all disturbances in boreal forests, "fire is the most widespread, frequent, and pervasive in its influence" [240]. Consequently, white spruce's distribution and occurrence are highly influenced by fire. Lightning-caused fires burn the most area across the boreal region [83,105,204,212,358,388,405], although human-caused fires have become more numerous in recent decades [8,24,83,213,299,405]. Most fires occur during late-spring and summer, although fires may occur from April through October [388,430]. White spruce trees are typically killed by all types of fire (crown, surface, and ground) [137,169,170,273,333,358,445], although soil burn severity is highly variable and typically patchy [120,206,347,445]. Most fires are small, but large fires account for most of the area burned [23,83,297,358]. Across white spruce's distribution, fires tend to be more frequent in the drier, western range than in the wetter eastern range (reviewed in [46,178]). White spruce communities tend to have less frequent fire than adjacent forest types throughout the species' range [113,238,298,315,461].
Because white spruce is widely distributed and is associated with many plant communities, it occurs on sites that exhibit a range of fire regime characteristics. The following is a summary of fire regime characteristics in white spruce communities throughout North America. For a detailed synthesis of fire regime characteristics in Alaskan white spruce communities, see FIRE REGIMES of Alaskan white spruce communities.
Ignition: Historically, lightning was the main source of ignition in North American boreal forests, including those dominated by white spruce [23,175,204,267]. Although human-ignited fires have outnumbered lightning-ignited fires throughout Alaska [8,24,83,213,405] and Canada [299,447] in recent decades, lightning-caused fires tend to be larger and account for most of the area burned in these boreal forests [83,105,204,212,358,388,405,447]. From 1956 to 1999, over 90% of the area burned in Alaska was ignited by lightning [175] and during the 1990s, 86% of the area burned in Canada was ignited by lightning [388].
Season: Most fires in white spruce ecosystems occur in late spring and summer. In boreal ecosystems of interior Alaska and Canada, the fire season begins in April and extends until September or October [388,430]. In Alaskan boreal forests, peak fire season occurs in June and July, coinciding with periods of high temperatures, frequent lightning, low humidity, and low precipitation [83,105,214,430]. However, fires may burn into August and September especially during "high fire years" (i.e., years where the area burned is >1.5 times the long-term average area burned) [214]. These late-running fire seasons are associated with higher severity fires (reviewed in [83]).
In the southern boreal forest, from central Alberta to northwestern Ontario, large areas burn in spring (April, May, and June) (reviewed in [202]). In boreal mixedwoods in Prince Albert National Park, central Saskatchewan, 97.7% of the fire scars, which spanned from 1831 to 1948, occurred in dormant or earlywood, indicating the dominance of a spring fire season. Between 1927 and 1945, about 90% of the area burned, burned in May. After 1945, about 55% of the area burned, burned in April, and about 95% of the area burned, burned in April through June [202].
Human-caused fires lengthen the fire season in Alaska and Canada [105,223,388]. Most early (April-May) and late season (September-October) fires are human-caused [105,388].
Type and severity: In the North American boreal forest, fires tend to be stand-replacing crown fires [172,178,204,451], although white spruce communities also experience stand-replacing surface and ground fires [147,298]. In general, white spruce stands experience less frequent crowning than black spruce stands because white spruce trees have fewer ladder fuels (higher canopy base height) and lower resin content than black spruce [137,298,405]. However, during extended dry periods, white spruce stands can burn with characteristics similar to those of black spruce [421], and closed white spruce forests often experience high intensity crown fires or severe, stand-replacing surface fires [179].
White spruce commonly occurs in mixedwood stands with varying proportions of hardwoods. Stands with a large component of hardwoods tend to be less flammable and have lower rates of fire spread than stands with few hardwoods, especially during the summer when hardwoods have leaves [204,298]. Similarly, stands with many hardwoods require higher rates of spread for crowning to occur than stands with few hardwoods [204]. Over a 36-year period in Alberta boreal mixedwood forests, hardwood stands had burn rates (i.e., burned area/total stand area/sample period (years)) less than one-third the rates of black spruce, white spruce, or pine [84].
Fires in white spruce stands tend to be stand-replacing [137,169,170,273,333,358,445] because of their thin bark, shallow roots, and exposed buds [194,204,263,394]. Low-intensity fires may kill white spruce [169,170], and they may have high severity. For example, in closed white spruce-balsam poplar stands in interior Alaska, the Bear Creek Fire killed all trees but left the canopy intact. "Many fine fuels (needles, leaves, small twigs) remain on shrubs and low tree branches, indicating this was not the result of an intense (hot) fire. Evidently the flame front passed through the area quickly, yet the fire continued to smolder in the dry duff, finally consuming it". In stands composed of approximately equal amounts of black and white spruce with 50% canopy closure, the same fire "burned both severely and intensely, crowning and killing all trees" [170].
Riparian white spruce stands may experience active crown fires during hot and dry weather. Fire behavior modeling of riparian, montane, >100-year-old white spruce stands in Banff National Park suggests that stands with high canopy bulk densities and/or low live crown base heights will support active crown fire under 90th percentile weather conditions. At 80th percentile weather conditions, stands were predicted to support surface or passive crown fire [311].
Some sites with white spruce experience mixed-severity FIRE REGIMES. In the Rocky Mountain foothills of west-central Alberta, mixed stands of lodgepole pine, white spruce, and black spruce were characterized by both high-severity fires and low-to-moderate-severity fires. Dendrochronological evidence indicated that high-severity fires (i.e., no surviving trees) initiated even-aged cohorts dominated by lodgepole pine. Subsequent, low-to-moderate-severity fires scarred, but did not kill, regenerating lodgepole pines. These fires gave rise to multiple cohorts of lodgepole pine, white spruce, black spruce, and subalpine fir [11]. A mixed-severity fire regime was also found in the North Fork of the Flathead Valley in Glacier National Park. Forests experienced both severe, stand-replacing fires and low-severity surface fires. Stands were dominated by western larch and lodgepole pine; western white spruce occurred within the study area and was considered a climax species [27].
In boreal forests, canopy mortality is often complete, while soil burn severity may be very patchy and highly variable [120,206,347,445]. Burn severity patterns are influenced by prefire organic layer depth and moisture content. Deeper and drier organic layers give rise to more intense surface fires and longer, deeper-burning ground fires, which result in more complete consumption of the organic layers [120]. Forest floor burn severity varied in white spruce stands after the Rosie Creek Fire (interior Alaska); stands lost between 5% and 76% of their prefire organic matter [417]. In mesic white spruce-quaking aspen stands in Alberta that burned during a single day of high-intensity fire that top-killed all of the sampled trees in the interior of the fire, the amount of forest floor combustion and exposed mineral soil (<0.8 inch (2 cm) humus) was highly variable. High variation in mineral soil exposure occurred both among and within stands; mineral soil exposure ranged from 0% to 100% among sample plots. Postfire organic layer depth averaged 40% less on burned sites compared to unburned sites, and exposed mineral soil occurred on approximately 35% of the burned area [158]. In the Gilles Creek Fire, interior Alaska, the depth of burn ranged from 0.3 to 11.9 inches (0.8-30.3 cm), with a mean burn depth of 7.6 inches (19.2 cm) in black spruce stands, and 4.5 inches (11.5 cm) in white spruce-quaking aspen stands. Prefire organic soil horizons were deeper in black spruce than white spruce-quaking aspen stands, but they were also wetter and less dense. This contributed to lower mean consumption of soil organic matter in black spruce stands (53%) than in white spruce-quaking aspen stands (66%) [347]. In southeastern Manitoba boreal mixedwood stands, the spring Black River Fire uniformly top-killed trees, but forest floor consumption was variable. Stands were codominated by quaking aspen, balsam fir, and white spruce. Severely burned plots had higher conifer basal area (38.2 m²/ha) and lower hardwood basal area (7.0 m²/ha) than scorched and lightly burned plots (P≤0.001). The author suggests that the difference may have occurred because the forest floor underneath the conifers was drier due to greater canopy interception, direct evaporation, and canopy transpiration [445].
Pattern and size: Fires typically do not burn uniformly in the boreal forest, which results in a mosaic of unburned, lightly burned, and severely burned areas (e.g., [10,120,337,417,449]). Topography, plant community composition, soil and fuel moisture, and weather influence burn patterns [10,84,358,449]. For instance, burn patterns may be more homogenous on flat landscapes than on hilly or mountainous landscapes [115], and differences in flammability among plant communities create different fire behavior [128,154]. Alaskan Monitoring Trends in Burn Severity data from 2004 (high fire year) and 2006 (low fire year) indicate that 20% and 66% of the area within fire perimeters did not burn, respectively, indicating the prevalence of mosaic fires in both high and low fire years [213].
Fire size varies greatly throughout white spruce's distribution. In Alaskan and Canadian boreal forests, most fires are small, but large fires account for most of the area burned [23,83,297,358,388]. In Alaska, approximately 60% to 80% of all fires are <12 acres (5 ha) [23], although large fires account for the most of the total area burned [23,105,130,213,214]. In Alberta and Saskatchewan, 98% of the fires account for less than l% of the area burned [297]. Large fires typically occur episodically because fire size is influenced by weather and climate patterns [1,26,83,116,131,213,297]. In severe fire years, individual fires in the Alaskan boreal forest tend to be large—often burning about 124,000 to >500,000 acres (50,000->200,000 ha); in contrast, in unusually wet years, the area burned may be negligible [121].
Frequency: White spruce is widely distributed and is associated with plant communities characterized FIRE REGIMES ranging from frequent, low-severity fires to infrequent, stand-replacing fires. White spruce communities do not occur where fire-return intervals are shorter than about 40 years because white spruce trees do not typically produce good cone crops until they are at least 45 years old (reviewed in [472]), and subsequent fires would kill regenerating trees before they reproduce. Fire history studies of white spruce stands are few, possibly because these stands occur within a broader mosaic of boreal forest types or because white spruce commonly occurs in mixed stands. White spruce communities typically have less frequent fire than other boreal forest types. Across the boreal region, fire-rotation intervals are generally shorter in the drier regions of western Canada and Alaska (50-100 years on average) than in the wetter areas of eastern Canada (average >200 years) (reviewed in [46,178]). The longest fire rotations in the western boreal region are likely in floodplain white spruce stands, where they may be ~300 years (reviewed in [178]). For a summary of reported fire-return intervals and fire-rotation intervals for white spruce communities in Alaska, see Table 2 in FEIS's FIRE REGIMES of Alaskan white spruce communities synthesis.
Boreal white spruce forests tend to have less frequent fire than adjacent forest types in interior Alaska [113,298,461] and Canada [238,315]. A large-scale analysis of 371 stand ages in the approximately 89,000,000-acre (36,000,000 ha) Porcupine and Upper Yukon river drainages of eastern Alaska, found hardwood stands had the shortest fire-rotation interval (26 years), followed by black spruce (36 years), then white spruce (113 years); and fire-return intervals were estimated to be 30, 43, and 105 years for hardwood, black spruce, and white spruce stands, respectively [461]. Another fire history study of 27 sites in the same area found that the mean fire-return interval (MFRI) in white spruce/quaking aspen stands (82 years) was not significantly different than that in black spruce stands (67 years) [113]. An analysis of 166 sites in the 11,087,600-acre (448,700 ha) Wood Buffalo National Park, northern Alberta, found that mean fire-rotation intervals in jack pine (39 years, 95% CI: 29-56) and quaking aspen (39 years, 95% CI: 26-68) forests were significantly shorter than those in black spruce forests (78 years, 95% CI: 65-109) and white spruce forests (96 years, 95% CI: 71-142) (P≤ 0.01). Sites with longer fire-rotation intervals were closer to waterbreaks than sites with shorter fire-rotation intervals (P≤ 0.05). The author suggested that variations in soil type and mean distance to a waterbreak influence forest type and fire frequency, respectively, and that white spruce's frequent occurrence near waterbreaks may be influenced by the longer fire rotations on those sites [238]. In the James Bay region of Quebec, white spruce occurs in pure stands along the shore. It is replaced by black spruce 0.3 mile (0.5 km) from the shore, and jack pine occurs 13.7 miles (22 km) from the shore. Along this shore to inland gradient, fires become more frequent. No evidence of fire was observed in the white spruce coastal forest in the 250 years since the land rose above sea-level, whereas fire-rotation intervals were calculated at 495 years in the black spruce forest (2,563,395 acres (1,037,369 ha)) and 115 years in black spruce-jack pine forest (7,985,146 acres (3,231,474 ha)). White spruce frequency was greatest in areas with less frequent fire, and black spruce and jack pine frequency was greatest in areas with more frequent fire. The authors suggest that the exclusion of white spruce farther inland may be related to the shorter fire-rotation intervals on those sites [315].
Several authors suggest that white spruce is limited to areas that burn infrequently [100,238,315,337,356,436]. On Alaskan floodplains, white spruce is often found on islands or terraces close to the river where fires rarely burn. On the uplands, white spruce stands often occur in isolated stands surrounded by less flammable hardwoods, making them relatively protected by fire [436]. Quirk and Sykes [337] reported that upland white spruce stringers were unburned while nearby black spruce stands had burned several times. These white spruce stands occurred in depressions along rills or swales with diffuse springs. The authors concluded that these stands were less susceptible to fire than the surrounding forests due to higher soil moisture and sheltered topography. In its northern range, particularly at treeline, white spruce often occurs on sparsely vegetated, dry sites where fire spread is unlikely [356]. Rowe [356] suggested that near its southern distributional limit in Saskatchewan and Manitoba, white spruce is commonly scattered on the upper slopes and crests of stabilized dunes that may have escaped fires that burned through the denser hardwood vegetation of adjacent sites. In the black spruce zone of central Quebec, white spruce and balsam fir dominate isolated subalpine sites that have escaped fire for prolonged periods. These isolated stands may be remnants of the historical balsam fir zone (currently to the south), which was replaced by fire-prone black spruce after recurrent fires [100].
Regional studies: Regional trends in fire ignition, season, type and severity, pattern, and size are discussed below. FIRE REGIMES in Canadian communities are not explicitly covered in this review except for when they inform adjacent communities in the United States. For instance, the fire regime in Kluane National Park, southwestern Yukon is discussed in the FIRE REGIMES of Alaskan white spruce communities synthesis, and studies in southeastern Canada are included in the discussion on FIRE REGIMES in the northeastern United States. Research from Canada was also included in the descriptions of fire regime characteristics in white spruce communities, above (i.e., Ignition, Season, Type and severity, Frequency, Pattern and size, Climate change).
Alaska: This section is summarized from FIRE REGIMES of Alaskan white spruce communities; see that synthesis for additional details and references. Historically, most fires in the Alaskan boreal forest were caused by lightning in June or July. Historical MFRIs in boreal white spruce communities typically range from about 80 to >250 years, and MFRIs in subboreal white spruce communities are longer. Floodplain, stringer, and treeline white spruce communities may have longer fire-return intervals than other boreal white spruce communities. Ground, surface, and crown fires can occur in white spruce communities, although crowning is generally less frequent than in Alaskan black spruce communities. Most fires are stand-replacing because white spruce is sensitive to fire. Most fires in the Alaskan boreal forest are small, but large fires account for most of the acreage burned.
Current FIRE REGIMES in white spruce communities may not differ much from historical regimes because most of the Alaskan boreal forest is sparsely populated and has little road access. Therefore, both human-caused ignitions and fire suppression efforts are limited. However, FIRE REGIMES in localized regions may have been influenced by human activity. Human-caused ignitions are increasingly common near settlements, but human-caused fires tend to be small because these areas are also where fires are actively suppressed. Climate change may lead to longer fire seasons, less effective moisture, and higher ignition rates and thus increase the area burned in Arctic and boreal regions. Climate change models predict varied effects on Alaskan white spruce communities; some communities may expand while others may decline. See the FIRE REGIMES of Alaskan white spruce communities synthesis for more detailed information and documentation.
Montana: White spruce and western white spruce occur in the Rocky Mountains in northwestern Montana, where they are associated with Douglas-fir, western larch, and lodgepole pine [331]. A fire history study of 3 sites west of the Continental Divide in Glacier National Park described 2 different 1) a mixed-severity regime with both surface and stand-replacing fires occurring at 25- to 75-year mean intervals, and 2) a stand-replacing fire regime with fires occurring at 140- to 340-year mean intervals. While western larch-lodgepole pine forest dominated the sites, western white spruce occurred as a minor component throughout the study areas. In the dry sites of the North Fork of the Flathead Valley, western white spruce is considered a climax species along with Douglas-fir. These sites experienced both frequent, surface fires (MFRI 36, range 28-52 years) and infrequent stand-replacing fires (MFRI 141, range 79-203 years) [27].
Northwestern Great Plains: White spruce is limited to relatively high-elevation, moist sites in the northern Black Hills. The "northwestern Great Plains highland white spruce woodland" Biophysical Setting (BpS 2910480) is generally limited to sideslopes and depressions, and sometimes riparian zones [232]. Because ponderosa pine is dominant in this community, it influences the fire regime characteristics. Little information was available to adequately characterize the fire regime in this community as of 2015. Brown [49] compiled chronologies from over 1,000 trees collected at over 50 locations throughout the Black Hills. He estimated that prior to European settlement, surface fires had MFRIs ranging from 30 to 33 years at higher elevations (where white spruce may occur), and 10 to 13 years at lower elevations. It is unclear what role stand-replacing and mixed-severity fires played in this community. While higher elevation forests and north-facing slopes dominated by white spruce are thought to be more prone to stand-replacing fires than lower elevation ponderosa pine forests in the Black Hills [232], Brown was unsure that the synchronous tree establishment that occurred at multiple spatial scales was due to stand-replacing fire. He suggested that widespread tree mortality caused by severe drought may have opened the forest canopy, and subsequent wet conditions may have promoted abundant tree regeneration. In many stands where even-aged cohorts occurred, older trees were also present. This suggests that seedlings established under partially open stands during optimal climatic conditions [49].
Great Lakes: In the Great Lakes region, white spruce is often a minor component in the southern boreal mixedwood mosaic, where it is most prominent in late-successional stands [144,177]. Recurrent fires limit the abundance and distribution of white spruce on fire-prone sites. Where fires have not occurred in a long time, white spruce may occur in the overstory [144].
In the Boundary Waters Canoe Area (BWCA), northeastern Minnesota, presuppression era forests were comprised of a mixture of fire-adapted species including jack pine, black spruce, quaking aspen, paper birch, and red pine. Advance regeneration of shade-tolerant species including white spruce, balsam fir, and northern white-cedar was sparse (reviewed in [142]). Before fire suppression began in the early 1900s, the fire-rotation interval was estimated to be ~100 years for the BWCA (including all forest types). Periodic "major fire years" (i.e., fires that burned >64,000 acres (25,900 ha) or 6% of undisturbed forest) accounted for most of the area burned and occurred every 26 years, on average. Because white spruces probably occurred in the understory of pines, quaking aspen, and paper birch, they would have been "caught up in the same fire rotations" of both surface and crown fires. After fire suppression began in 1911, the fire-rotation interval lengthened to ~2,000 years and ladder fuels accumulated, facilitating the spread of surface fires into the canopy [177]. Landscape models predict that white spruce and balsam fir will dominate these forests if fire is excluded for extended periods (e.g., 300 years) [363].
Before European settlement, fire was a dominant factor in the establishment and maintenance of forest communities in Itasca State Park, Minnesota. Varying fire frequencies and patterns, soil types, and regeneration success created a mosaic of forest types with different stand ages and compositions. "Major" fires occurred every 10.3 years. Shade-intolerant, fire-adapted species including red pine, eastern white pine, jack pine, quaking aspen, and paper birch dominated forest stands. After fires were excluded (~1920), stands began to succeed to either northern hardwoods or balsam fir-white spruce. This study, published in 1973, reported that balsam fir-white spruce communities were present in small stands and also common in the understory of aging jack pine, red pine, and eastern white pine forests. Historically, this successional trend was arrested by periodic fires [144].
In the Pictured Rocks National Lakeshore, Michigan, white spruce is a minor species in mixedwood forests. The historical MFRI for surface fires in the pine-dominated forests is 21.8 years [259], which is too frequent for white spruce stands to persist.
The Great Lakes-St. Lawrence-Acadian forests, where white spruce is often a minor component, had several distinct FIRE REGIMES. In the north, stand-replacing crown fires were typical. In western xeric sites, red and eastern white pine forests experienced both moderate-severity surface fires at 20- to 40-year intervals, and more severe fires that killed much of the stand at 15- to 200-year intervals. Farther east on mesic sites, eastern white pine forest experienced stand-replacing crown fires and severe surface fires at around 200- to 300-year intervals. Balsam fir, white spruce, and northern white-cedar often established during long intervals between fires, but these species rarely replaced eastern white pine before fire returned (reviewed in [178]).
Northeast: Little information was available on FIRE REGIMES of white spruce communities in the northeastern United States as of 2015. Along the northern New England and Canadian Maritime coast where white spruce is dominant or codominant, cool temperatures and frequent fogs create mesic conditions. Consequently, fires are likely infrequent. In northeastern Maine, land survey records from 1793 to 1827 and representative undisturbed stands indicate that 88% of the region was covered by late-successional forest and that shade-intolerant species were of minor importance. The author speculates that if crown fires occurred as frequently as every 100 years, at least half of the study area would have been dominated by pioneering birch-quaking aspen stands. He estimates that the fire-rotation interval is >806 years [260]. Elsewhere in the northeast, white spruce is a minor component in mixed forests. LANDFIRE models of the Acadian low-elevation spruce-fir-hardwood forest—where white spruce may occur—predict a MFRI of ~1,100 years for stand-replacing fires (e.g., BpS 6313730) [233].
The following paragraphs describe fire regime characteristics in southeastern Canada; similar patterns may exist in nearby northeastern states.
Fire is infrequent in mixedwoods and northern hardwood forests in the Timiskaming region, Quebec. White spruce is often subdominant in these forests. A study in western Quebec, north of western New York, found that more than 60% of the 443,100-acre (179,300 ha) study area remained unburned over the 413-year study period. For the entire study area, the presettlement fire-rotation interval was 909 years (95% CI: 489-1,690), the settlement period fire-rotation interval was 153 years (95% CI: 108-218), the post-settlement fire-rotation interval was 5,081 years (95% CI: 3,593-20,318), and the fire-rotation interval for the entire study period was 494 years (95% CI: 373-694) [112]. A 617,800-acre (250,000 ha) study in the same area also found relatively long fire-rotation intervals, which dipped during European settlement. For the entire study area, the presettlement fire-rotation interval was 262 years (95% CI: 163-422) and during the settlement period (1890-1948), the fire-rotation interval was 96 years (95% CI: 73-126). From 1950 to 1998, there were no large fires, and fewer than 12,400 acres (5,000 ha) burned in the entire study area. In parts of the study area where humans may have had less of an influence, fire-rotation intervals were estimated at 188 years for the entire study period and 314 years before 1890 [161].
In the lower St. Lawrence region of eastern Quebec, bordering Maine, historical survey data indicate that presettlement forests were dominated by fire-intolerant, late-successional species including balsam fir, white spruce, northern white-cedar, and sugar maple. Fire-adapted species such as quaking aspen and pines were infrequent throughout the study area. The dominance of late-successional species in presettlement forests suggests that fires were infrequent. Clearcutting and human-caused fires increased greatly after 1900, resulting in substantial shifts in species composition [117].
In the Gaspesian mixedwood forest, northeast of Maine, fires are generally very infrequent, but occasional large fires occur during dry periods. In a 1,601,000-acre (648,000 ha) study area, the fire-rotation interval increased from 89 to 176 years (P≤0.0001) since the end of the Little Ice Age (LIA) (~1850). This lengthening of the fire cycle may be due to the predominance of warmer, more humid air masses replacing the predominantly cold, dry air masses of the LIA. While fires are infrequent, dry conditions enable fires to occur. A dry, warm period in the early 1920s led to extensive fires in 1924. Since 1925, the mean and maximum fire weather index (a measure of fire risk) decreased, and the corresponding fire-rotation interval lengthened to 650 years. The authors suggest a fire-rotation interval between 170 and 250 years from 1850 to present, based on archival data (1920-2003) and survival analysis (1850-2003). This study did not find any significant differences in fire-rotation intervals between the 2 bioclimatic regions (eastern balsam fir-yellow birch and eastern balsam fir-white birch), or among different physiographic features (i.e., valleys, lowlands, or highlands) [241].
Climate change effects on In recent decades, fires have been burning over increasingly larger areas in the boreal region [150], and this trend is expected to continue throughout the century. Projected climate-change scenarios predict that North American boreal forests and their FIRE REGIMES will be dramatically altered (reviewed in [447]). Warmer temperatures, altered precipitation, and increasingly severe fire weather will directly and indirectly alter FIRE REGIMES [99,132,335,447]. Although the response of FIRE REGIMES to climate change is complex, across Arctic and boreal regions, the area burned, fire intensity, and fire severity will likely increase as fire seasons lengthen, effective moisture declines, and ignition rates increase [99,133,180,274,279,408] (reviewed in [132,335,447]). Across Canada, results from global climate models suggest that the number of fires will increase 75% to 140% from baseline (1975 to 1995) by 2100 [459] (reviewed in [335]). However, predictions of future fire occurrence vary spatially throughout the boreal forest [44,397]. Boulanger and others [44] predict heterogeneous responses of FIRE REGIMES to climate change across Canada. The largest increase in fire activity is predicted to occur in northwestern and central Canada. By 2071 to 2100, the predicted high fire occurrence and area burned in parts of this region may far exceed their historical range of variability. In sites where area burned, fire frequency, intensity, or severity is expected to increase, coniferous forests (including white spruce forests) may convert to early successional hardwood forests [28,98,215,360]. For instance, in quaking aspen-white spruce forests in Prince Albert National Park, shorter simulated fire-rotation intervals resulted in higher quaking aspen stem densities and lower white spruce stem densities than 1975 to 1990 densities [98]. As coniferous forest converts to hardwood, subsequent fire occurrence, frequency, and intensity could decrease due to the lower flammability of hardwoods, which could offset the increased likelihood of fire [28,98,215,397].
See FIRE REGIMES of Alaskan white spruce communities (separate synthesis) and Climate change and fire (below) for more information this topic.
Find additional fire regime information for plant communities in which white spruce may occur by entering ?white spruce? in the FEIS home page under "Find FIRE REGIMES", or see the Fire Regime Table for information on FIRE REGIMES of "potential natural" vegetation communities in which white spruce may occur.
Fire adaptations: White spruce is poorly adapted to survive fire compared to most associated trees [358], which makes its widespread distribution in fire-prone boreal forests perplexing. White spruce has many traits that favor its persistence under long fire-return intervals, such as requiring a long time to mature [263], variable seed production [138], short seed dispersal distance, thin bark, and non-serotinous cones (reviewed in [83]). Traits that enable white spruce to persist in boreal communities include the ability to establish on thin organic or mineral soil seedbeds after fire [61,329,336,356,468,472], years of high seed production, which sometimes coincide with fires [327,328,330,336,436], higher shade tolerance and longer lifespan than those of competing hardwoods [136], and the ability to establish in late-successional stands [17,34,67,145,330,429].
Rowe [358] compares the ability of boreal conifers to regenerate after fire based on life history traits (Table 4). White spruce ranks 4th out of 5 conifers.
Table 4. Relative ranking (1-5*, where 5 indicates best adaptation to fire) of characteristics of boreal conifers contributing to successful regeneration after fire. *Weighted up to twice the value of other characteristics, because it is the most important characteristic. Table modified from [358].
Jack pine Black spruce Tamarack White spruce Balsam fir Seed retention on tree* 10 6 2 3 1 Earliness of seed production 5 4 2 3 1 Seed mobility (relative size) 2 5 5 3 1 Seedling frost hardiness 5 3 4 2 1 Seedling palatability to animals 3 5 2 4 1 Seedling growth rate 5 2 4 3 1 Seedling response to full exposure (opposite of shade tolerance) 4 3 5 2 1 Totals 34 28 24 20 7Plant response to fire: White spruce abundance may be drastically reduced after fire because of high tree mortality and limited postfire recruitment [54,147,178,308,356], although white spruce may establish after fire when adequate seed sources and seedbeds are available [169,170,328,329,336]. White spruce establishment after fire depends on seed availability, fire characteristics, seedbed conditions, site and soil characteristics, and weather.
After fire, white spruce typically establishes from seed from trees along fire edges or from unburned trees within the burn [146,156,174,178,262,430]. Seedling establishment is typically highest close to the unburned seed source [145]. In northwestern Quebec boreal mixedwood forest, the average density of white spruce after fire decreased from 280 trees/acre (693 trees/ha) near the edge of the burn (0-200 feet (0-60 m) from edge), to 21 trees/acre (51 trees/ha) in the interior of the burn (3,940-6,560 feet (1,201-2,000 m) from edge) [145]. Because white spruce typically has a short dispersal distance (<330 feet (100 m)) [430,436,466], small burn areas may be colonized entirely from trees along the edges, and large burns may be colonized only around the perimeter. White spruce does not typically recruit into the interior of large fires unless unburned white spruce remain within the burned area [430]. Models of postfire recruitment indicate that adequate regeneration of white spruce would be limited to about 230 feet (70 m) from the fire's edge when the external seed source had a 5 m²/ha basal area. In the interior of a burn (>2,600 feet (800 m) from a fire edge), about half of the white spruce recruits would establish from small residual stands [156]. White spruce may occasionally establish far from unburned seed sources via long-distance seed dispersal [457] (e.g., secondary dispersal over snow, up-drafts) or crown-stored seed in fire-killed trees [288].
Fire timing, type, and severity affect white spruce seed source availability and recruitment after fire. Early- to mid-season, stand-replacing crown fires, which commonly occur in boreal forests, typically destroy white spruce seeds (e.g., [147]). However, crown-stored seed may occasionally be available on fire-killed trees depending on fire timing and intensity [157,169,170,287,288,468] (see Seed banking). When ground or surface fires occur after seed is ripe (i.e., mid-to late-season fires), viable seed may be available in fire-killed trees [169,170]. Large amounts of viable seed were found on fire-killed trees with intact crowns after an early-season fire that did not consume the canopy in interior Alaska. Trees with scorched or burned crowns did not produce seeds [468]. Crown-stored seed may result in high postfire recruitment [169,170], even in the interior of the burned area [288]. Even-aged white spruce stands may develop from this type of postfire establishment [137,430,431,460].
After fire, white spruce seedlings typically establish best on sites where most or all of the organic soil is consumed, leaving only a thin organic layer or exposed mineral soil [61,329,336,356,468,472]. Severe fires that consume the organic layer not only create a suitable seed bed for white spruce establishment, but also kill the perennating buds of competing hardwoods, shrubs, and herbs, which often occur in the organic horizon [356]. However, most fires do not consume the entire forest floor; mosaic fires result in patches of exposed mineral soil intermixed with areas where organic layers are intact or partially consumed [148,158,159,263,290]. Within individual burns, exposed mineral soil is highly variable, ranging from 0 to 100%, but averages about 35% in boreal mixedwoods in Alberta and in Alaska [158,263]. Even less mineral soil may be exposed around the fire perimeter, where most white spruce seed is dispersed. On a large fire in Alberta boreal mixedwoods, soil exposure on the fire's edge averaged only 5%, whereas in the interior, it averaged 35% [158]. Spring fires typically consume less organic material and expose less mineral soil than summer fires; consequently less white spruce regeneration occurs after spring fires than summer fires [329].
White spruce seedling establishment may occur within 20 years after fire [108,145,328,468]— generally within a few years [328]— when seedbeds are most receptive [148,328,336,471]. Initial postfire establishment may be highest when fires and mast years coincide [327,328,330,336], particularly if the fires create suitable seedbed conditions. Some studies report delays in postfire recruitment (e.g., [34]). This is probably due to low seed availability at the time of the fire and in subsequent years, and/or inadequate seedbed conditions following fire [34]. Some retrospective studies that use tree rings in mature stands to estimate tree regeneration after fire suggest substantial delays in white spruce regeneration, but their methods may not precisely estimate tree ages (and postfire establishment year); consequently, these studies may overestimate delays in regeneration [327]. White spruce is not limited to initial postfire regeneration; it commonly establishes later in succession [17,34,67,145,330,429,463].
Because white spruce trees are easily killed by fire, fire-adapted trees such as quaking aspen, paper birch, jack pine, or black spruce commonly dominate after fire on sites previously dominated by white spruce [65,147,262]. Regeneration density after fire is related to prefire basal area for many boreal tree species (e.g., jack pine, quaking aspen, paper birch, black spruce), but generally not for white spruce, because it often regenerates poorly after fire regardless of prefire abundance [65,147].
Site characteristics, such as soil type and topographic position, may influence white spruce's response to fire. Sites with coarse-textured soils and sites on south-facing slopes dry out more rapidly and tend to burn more frequently than sites with fine soils and sites on north-facing slopes. On fire-prone sites, white spruce is often eliminated and replaced by species that have shorter reproductive cycles and serotinous or semiserotinous cones, such as jack pine and black spruce. Consequently, white spruce rarely dominates fire-prone sites [356].
White spruce seed production is typically poor at the forest-tundra ecotone, so little or no seed is available for postfire regeneration. White spruce establishment was limited after a "severe" wildfire in the black spruce-white spruce forest-tundra ecotone northeast of Inuvik, Northwest Territories and none of the white spruce that established in the first 5 years after the fire in the 0.74 acre (0.3 ha) study area survived. In the 22 years after fire, limited establishment occurred in clumps close to surviving white spruce. Establishment peaked every 3 or 4 years. The authors suggest that establishment was restricted due to a lack of viable seeds and a short seed dispersal distance [236]; site characteristics may have played a part as well.
See Regeneration Processes for further information, including information on seed production, seed dispersal, germination, establishment, and growth. Successional Status discusses general patterns of postfire succession in white spruce communities. Examples of white spruce response to fire by region follow.
Alaska: In Alaska, white spruce may colonize recently burned sites, but regeneration often occurs later in succession. Severe fires typically set back white spruce forests to communities dominated by seral species including paper birch and quaking aspen, especially when fires are large and all white spruce are killed [262]. It generally takes about 150 years before white spruce regains dominance after fire [137]. Pure white spruce stands may establish immediately after fire, but this is not common [137,262].
In burned white spruce-reindeer lichen woodlands in the central Brooks Range, few white spruce established within the first 10 years after fire, although seedling establishment was generally continuous during the next ~90 years. Seedling establishment may have been delayed due to unfavorable seedbed conditions after the fire. On 1 of the 4 white spruce plots, 75% of the white spruce trees present ~100 years after fire established in the first 25 years; this is similar to black spruce establishment patterns. On the rest of the plots, it took 50 to 80 years for 75% of white spruce to establish [67].
In early June of the 1st growing season after the Wickersham Dome Fire in interior Alaska, white spruce was seeded onto a variety of seedbeds in burned black spruce stands on the north and south slope. Seedbeds included mineral soil, ash, and charred mosses. Germination was best on mineral soil; no white spruce germinated on charred mosses. On the north slope, germination peaked between June 27 and July 11. Subsequent mortality was initially caused by something eating the cotyledons, and additional mortality was caused by damping off, flooding, and smothering by other vegetation after rains in August. On the south slope, germination peaked between July 11 and August 8 and subsequent mortality peaked 3 weeks later when conditions were dry. Survival of germinants to September 10 was 72% on the north slope and 77% on the south slope. Most surviving seedlings ranged from 0.6 to 1 inch (1.5-2.5 cm) tall [71].
After the low-intensity Bear Creek Fire in interior Alaska, white spruce had high establishment rates. The fire burned closed white spruce-balsam poplar stands and killed all the trees but left the canopy intact. White spruce seedlings were abundant 1 growing season after the fire, probably because seeds were mature at the time of the fire (August), and canopies and seeds were unharmed. A thin layer of fallen needles may have created a mulching effect over mineral soil which may have helped stabilize seedbed moisture conditions. White spruce regeneration was estimated at 12,000 seedlings/acre (30,000 seedlings/ha) [169,170].
After stand-replacing fires (~1915) in conifer-hardwood stands on upland, south-facing sites in interior Alaska, white spruce establishment differed among plant communities (2 quaking aspen types, 2 paper birch-quaking aspen types, and 1 white spruce-paper birch type), and subsequent height growth and stand development followed 2 distinct patterns. A chronosequence study used tree rings to estimate tree ages and establishment dates 46 to 141 years after fire. In quaking aspen community types, quaking aspen established soon after fire, and white spruce established about 25 years after fire (Figure 10a). In paper birch-quaking aspen and white spruce-paper birch community types, white spruce established rapidly and concurrently with the hardwoods and no establishment occurred afterward (Figure 10b). When white spruce established at around the same time as the hardwoods, it grew rapidly (Figure 10b); when white spruce established after the hardwoods, it grew more slowly (Figure 10a) [463].
Figure 10. Tree growth and establishment patterns after stand-replacing fires (~1915) in (a) a quaking aspen community, and (b) a white spruce-paper birch community. Figure modified from Youngblood [463].Great Lakes: White spruce response to fire is not well documented in the Great Lakes region. However, white spruce is probably eliminated or severely reduced following stand-replacement fires in boreal mixedwoods. Studies from the region suggest that white spruce does not readily establish immediately after fire [78,308], with some exceptions (e.g., [176]). After the Little Sioux Fire in northeastern Minnesota, white spruce was eliminated from jack pine and quaking aspen stands where it had been locally common in the understory of 3 of the 7 studied stands. No white spruce regeneration was reported in the 5-year study period [176,308]. Five years after a stand-replacing fire in a balsam fir-white spruce-paper birch forest on Isle Royale, Michigan, white spruce seedlings were rare [78]. In contrast, after a stand-replacing fire in mixedwood stands in the Boundary Waters Canoe Area, Minnesota, white spruce established in abundance along with black spruce, paper birch, white pine, jack pine, balsam fir, and northern white-cedar. According to this retrospective study, most trees, including white spruce, established within 5 years after the fire. The seed source was likely an unburned mature mixed forest across the river from the burn [176]. In the Great Lakes region, white spruce dominance increases with stand age [77,198,199], and white spruce is most likely to occur on sites that burn infrequently [176].
Western Canada: After stand-replacing fire in white spruce forest, hardwood and pine seedlings often establish and white spruce establishment fails. Ten to 20 years after 5 stand-replacing wildfires on mesic, upland sites in central and northeastern Alberta boreal mixedwoods, few white spruce trees remained and white spruce regeneration was poor. Prefire stands were dominated by quaking aspen, white spruce, or a mixture of both, and 3 of the 5 fires occurred during mast years. Nonetheless, 79% of the <14-year-old plots and 91% of the 20-year-old plots had no white spruce seedlings. Lodgepole pine and jack pine seedlings established in many stands, including those that were pure white spruce before fire, even though pines were not present in prefire stands. The spring and early summer fires may not have consumed sufficient organic material to create suitable seedbeds for white spruce. Because there were few white spruce trees left after any of the fires, the authors suggested that most white spruce seedlings established from seed sources >1,600 feet (500 m) away, or from trees that fell before the study sites were visited [147].
After the 1,846-acre (747-ha), early-June Aishihik Fire in south-central Yukon, white spruce regeneration was variable. Most stands were located on high terraces of the Aishihik River Valley; prefire communities were dominated by white spruce and/or quaking aspen. Where white spruce dominated the prefire stand, white spruce establishment after fire varied from about 1,100 to 6,300 seedlings/acre (2,700-15,600 seedlings/ha) 5 years after the fire. Where quaking aspen dominated the prefire stand, white spruce regeneration was virtually absent. In general, quaking aspen was the most pronounced species in most postfire plots; 3 years after fire it occurred in 100% of the plots. White spruce seedlings occurred in 44% of the plots by postfire year 3, and in 77% of the plots by postfire year 5. Quaking aspen suckers averaged about 5 feet (1.5 m) tall 5 years after fire, whereas white spruce seedlings averaged about 0.8 inch (2 cm) tall. This suggests that quaking aspen will initially dominate much of the regenerating Aishihik Fire. Table 5 shows the variation in white spruce and quaking aspen regeneration after the Aishihik Fire [312].
Table 5. Tree regeneration 5 years after the Aishihik Fire, Yukon. Plots are 10 x 10 m. Table modified from Oswald and Brown [312]. Plot Prefire community White spruce (seedlings) Quaking aspen (suckers and seedlings) White spruce (seedlings/ha) Postfire exposed mineral soil (%) Moisture regime 1 White spruce 30 44 3,000 95 subxeric 2 White spruce/quaking aspen 44 141 4,400 95 subxeric 3 White spruce 156 37 15,600 100 subhygric 4 Quaking aspen 1 800 100 0 mesic 5 White spruce/quaking aspen 17 75 1,700 95 mesic 6 White spruce 27 1 2,700 95 subxeric 7 Quaking aspen 0 200 0 20 submesic 8 White spruce/quaking aspen 0 7 0 75 mesic 9 Quaking aspen 27 31 2,700 85 mesicIn northeastern Alberta, mixedwood boreal forests that are classified as "pure deciduous" often have a white spruce component. Emergent white spruce trees in these stands are much taller than the intermediate-age (≤70 years old) quaking aspen canopy (Figure 11). They are likely to be trees that survived previous fires because white spruce do not enter the canopy before 60 years and do not dominate the canopy until 100 to 120 years after fire. These white spruce are disproportionately large seed sources because of their size and position above the canopy. They have a strong influence on the distribution, abundance, and timing of white spruce recruitment immediately and for several decades after fire, when white spruce seedlings may establish under a mature aspen canopy [86].
Figure 11. Emergent white spruce within "pure" quaking aspen stands northwest of Peace River, Alberta. 86]Eastern Canada: White spruce is a common component of mixed stands in eastern Canada and is most important in mid- to late-successional stands. Like many other mixedwood sites in white spruce's distribution, early postfire succession in eastern Canada tends to be dominated by shade-intolerant species such as quaking aspen, paper birch, and jack pine, with few white spruce.
A study of 34 fires in 94 upland mixedwood stands in Ontario found that white spruce's relative composition in prefire stands was 14.9% greater than that in stands 5 to 18 years after fire (P<0.001). Stands that were dominated by white spruce before fire were dominated by quaking aspen after fire. White spruce seedling density was not related to its prefire basal area, while regenerating stem densities of quaking aspen, jack pine, balsam poplar, and black spruce were positively related to their prefire basal area [65].
A dendrochronological study of white spruce regeneration 69 years after a stand-replacing fire in boreal mixedwood forest, northwestern Quebec, found that initial regeneration was dominated by jack pine and quaking aspen. The fire left an 89-acre (36 ha) island of unburned forest within the interior of the fire. The basal area of the unburned island was dominated by white spruce, paper birch, and balsam fir, while the burned area was dominated by jack pine, quaking aspen, and paper birch. White spruce established in 2 waves after the fire. The first wave began in the first 5 postfire years and peaked in postfire year 20. The second, smaller wave began about 40 years after the fire and peaked about 10 years later. There was little white spruce recruitment between the 2 waves. The density of the initial white spruce cohort was negatively correlated with distance from unburned stands (R² = 0.37, P>0.0001). Average white spruce density decreased from 280 to 21 trees/acre (693-51 trees/ha) over a distance of 0 to 6,600 feet (0-2,000 m) from the unburned zone. The second cohort had slightly more seedlings closer to the unburned zone than farther away. The first cohort was probably a seed source for the second cohort [145].
One growing season after 4 prescribed fires in the Petawawa Research Forest, Ontario, white spruce had high rates of seedling establishment in stands that were dominated by red pine and eastern white pine, even though white spruce was a minor component of the stand. The "predominance" of white spruce seedlings 1 to 2 years after the fires was attributed to a "bumper crop" of white spruce seeds that year. About 280 to 24,700 white spruce seedlings/acre (690-61,000 seedlings/ha) established. Estimates of seedling abundance (white spruce and pines combined) were highest on severely burned sites [419]. For additional information about this study, see this Research Project Summary: Prescribed burning experiments in red and eastern white pine forests of eastern Ontario.
White spruce trees and forests are highly flammable, although less so than black spruce [83]. White spruce needles and bark are resinous [303], but less so than black spruce [405]. Compared to black spruce, white spruce-dominated stands may be less dense and have a less flammable understory [266]. Nonetheless, large amounts of fuels accumulate in white spruce forests including woody fuels, flaky bark, feather mosses, and shrubs, making these forests highly susceptible to fire [114]. Among white spruce sites, floodplain sites are less flammable than upland sites because the forest floor typically remains moist, and the understory often contains alders and willows, which are not flammable during the growing season [45,358,449].
The structure of white spruce trees contributes to their flammability. The arrangement of vertically continuous branches may promote ignition and torching [114,462,466], especially when branches are retained low on the trunk [114,171,194,263]. The forest floor surrounding white spruce boles may be especially flammable because white spruce trees often have dense, narrow crowns, which shelters the forest floor from precipitation and contributes to the accumulation of needles [356].
It is generally accepted that conifer forests are more flammable and more likely to burn than hardwood forests in the boreal region [84,179], and that stands with more hardwoods are less flammable than stands with fewer hardwoods [111]. Hardwoods and hardwood stands have structural and fuel attributes that contribute to lower flammability than conifers. These attributes include low canopy bulk density, leaves with high moisture content, low concentrations of flammable resins and oils, discontinuity of fuels between the forest floor and tree crowns, high rates of decomposition for coarse woody debris, and relatively fire-retardant fine fuels and litter. Consequently, hardwood stands may limit the intensity and spread of large fires (reviewed in [111]). In Alberta boreal mixedwoods, more lightning-caused fires occurred in white spruce-dominated forests than in quaking aspen-dominated forests. On a landscape scale, forest type explained more variation in annual fire initiation than did weather indices, even during years with extreme fire weather. The authors suggest that differences in fuel characteristics (e.g., flammability, ladder fuels, duff characteristics) may account for the greater number of lightning fires in white spruce stands [226]. Fire occurrence is lower in the hardwood-dominated Great Lakes-St. Lawrence region than in adjacent boreal landscapes despite having similar trends in fire weather. The proportion of "deciduousness" may account for the difference in fire hazard between the 2 landscapes [111]. Paleoecological studies from Alaska support the idea that the flammability of black spruce may override climatic factors in regulating fire frequency [50,180,181,196,215].
Seasonal trends in foliar moisture content influence white spruce flammability and crowning potential. In central Alberta, new and old white spruce foliage was periodically sampled between early March and mid-September during 2 consecutive years. The moisture content of old foliage ranged from 83% to 127%; the moisture content of new foliage ranged from 146% to 480%. The moisture content of new foliage peaked soon after flushing and declined rapidly through the summer. The moisture content of old foliage was relatively stable except for when it fell to its lowest level, during the "spring dip", just before the new foliage flushed. By late summer, moisture contents of old and new foliage were similar [68]. In a similar study at Petawawa Forest Experiment Station, Ontario, the moisture content of conifer foliage (including white spruce) followed similar patterns. The moisture content of old conifer foliage fell to its lowest level (84% for white spruce) in May and early June—just before new foliage flushed—then gradually rose to its maximum (~115% for white spruce) in late summer. The moisture content of new conifer foliage was very high at flushing, decreased sharply, and gradually levelled out by late summer [420]. Because seasonal trends in live foliar moisture content and associated foliar chemistry influence flammability and fire behavior in conifers [208,420], conifers (including white spruce) may be most flammable during the "spring dip" in foliar moisture content.
Spruce beetles affect fuels in white spruce and Lutz spruce forests by creating snags and fallen logs. In the Resurrection Creek drainage on the Kenai Peninsula, high mortality of large Lutz spruce resulted in a substantial number of fallen dead trees. Over a 16-year spruce beetle outbreak, approximately 71 Lutz spruce/acre (176 Lutz spruce/ha) fell; most of these had been killed by spruce beetles. While most of the trees were killed during the first 10 years of the outbreak, only 7 trees/acre (19 trees/ha) fell during the first 10 years, and most fell during the last 6 years (64 trees/acre (157 trees/ha)) [190]. This resulted in an increase of woody fuels from a median of 8.88 tons/acre during the outbreak to 35.4 tons/acre 20 years after the outbreak began. About 65% of this woody fuel (by weight) was comprised of sound wood >3 inches (7.6 cm) in diameter [366].
A few studies quantify forest floor depths and fuel loads for white spruce types in Alaska. In interior Alaska, 100- to 200-year-old white spruce/highbush cranberry/field horsetail/splendid feather moss stands had a 3- to 6-inch (8-15 cm) deep organic layer and 8- to 10-inch (20-25 cm) deep carpet of splendid feather moss, while 120- to 200-year-old floodplain white spruce types had a 2-inch (5 cm) deep organic layer on average [137]. In the Bonanza Creek Experimental Forest, mean litter + humus depth was 4.4 inches (11.2 cm) in 62-year-old white spruce stands [25]. In >100-year-old upland white spruce stands in interior Alaska, small-diameter woody fuels averaged 6.2 T/ha, and large-diameter woody fuels averaged 20.9 T/ha. The organic layer in these stands is about 3 to 5 inches (8-12 cm) deep and is comprised of about 2 to 3 inches (6-7 cm) of green moss and 3 to 4 inches (7-9 cm) of brown moss. Compared to black spruce stands in interior Alaska, white spruce stands may have thinner organic layers, but more large-diameter woody debris because white spruce trees typically have larger boles than black spruce [136].
For information about stand structural dynamics and fuel accumulation in fire-initiated stands throughout the boreal region, see Brassard and Chen [46].
White spruce seeds are conditionally dormant [305] — that is, seeds that are dispersed in fall and winter do not germinate until conditions become favorable during late spring and summer [305,354,356,474] (see Seasonal development). Field studies from Alaska [321] and Manitoba [354] suggest that white spruce seeds germinate at mean temperatures of 50 to 57 °F (10-69 °C), and reviews report that optimum germination temperature ranges from 46 to 90 °F (8-32 °C) [71].
White spruce seed may remain viable for about 1 year [157], although viability drops steadily after seeds ripen [352,470]. Clean, dried seed may remain viable for up to 10 years in storage (reviewed in [15]).
In general, most white spruce seeds fail to germinate [61], and viability varies among years, stands, dispersal periods, and regions. High viability generally occurs in years with high seed production [466,472]; however, germination tests of the highly productive 1970 seed crop from 29 stands throughout Alaska found germination rates ranged from 0% to 85% [471]. Seed viability is typically highest during the peak dispersal period. In Quebec, seed viability was highest during highest seed rain in September and October, and gradually decreased through winter, spring, and the following summer [352]. In interior Alaska, seeds dispersed in September were 72% viable, whereas those dispersed in March were 29% viable [468]. Seed viability ranged from 6% to 82% in interior Alaska [466,475], 3% to 33% in northwestern Canada [283], 83% to ~95% in Manitoba [216], and 80% to 96% in Saskatchewan [61]. Seed viability may often be low in the northernmost limits of white spruce's range [283,470]. Near treeline in the Tuktoyaktuk region of northwest Canada, seed germinability ranged from 3% in isolated tree islands to 33% in forest-tundra. Seed bank samples yielded no germinable white spruce seed and there were few seedlings across the region [283].
White spruce typically occurs in cold regions in riparian, upland, and treeline sites. It is the dominant tree species of the dry, usually upland North American boreal forest region [369]. It grows best on well-drained soils but occurs on a wide range of land forms and soil types, with many different associates, in various regional contexts [178,230].
Climate: White spruce grows in regions with long, cold winters and short, cool summers [3], but it can withstand large variations in temperature. In Alaska, Yukon, and Northwest Territories, the January temperature may average -20 °F (-29 °C), and throughout its range in Alaska and Canada the July temperature may average 55 °F (13 °C) [305]. At the northern extent of its distribution, climatic extremes may range from -54 °F (-65 °C) in January to 94 °F (34 °C) in July [305]. Precipitation generally increases from the northwest to the southeast of white spruce's distribution [179]. White spruce sites in Alaska and western Canada receive about 10 inches (250 mm) of precipitation annually, while sites in Nova Scotia and Newfoundland may average 50 inches (1,270 mm) [265,305].
Topography and elevation: White spruce typically grows on floodplains, upland slopes, and treeline sites [83,101,136,137,218], although it grows on a variety of landscape positions [349]. In Alaska and western Canada, lowland white spruce communities frequently occupy river terraces [137,188,303,356,403,415,418], while upland communities generally occupy warm, south-facing slopes [136,349,413,428,435]. In Alaska, white spruce commonly occurs on south-facing slopes within 5 miles (8 km) of major river valleys [137,435]. White spruce is often the dominant tree at altitudinal or arctic treeline [12,67,89,94,257,318,349,432]. In northeastern British Columbia, white spruce is associated with channels and concave slopes, which are generally richer and moister than ridges and convex slopes [9]. In Minnesota, at the southern end of its range, white spruce is often limited to lakeshore sites [143].
White spruce grows from sea level to nearly 7,000 feet (2,000 m) [184,305]. In Alaska, it reaches 3,000 feet (910 m) on the south slope of the Brooks Range [305]. In eastern forests, it grows from sea level to about 5,000 feet (1,520 m) [114]. In the Black Hills of South Dakota and Wyoming, white spruce occurs from about 5,700 to 6,700 feet (1,700 to 2,000 m) [184]. Although white spruce has a wide elevational range, it is often confined to stream bottoms and lower river benches [119].
Figure 3. Floodplain habitat, Yukon Flats National Wildlife Refuge, Alaska Figure 4. White spruce at treeline, Wolf Creek site, Yukon. Figure 5. White spruce forest in Denali National Park and Preserve. Photo © 2005 Barbara Logan, dlogan@alaska.netSoils and soil moisture regimes: White spruce typically grows best on warm, moderately to well drained, upland or floodplain soils [119,136,137,418,425,435,457]. Although white spruce may grow in a range of moisture conditions [2,22,80,119,240,332,394], it rarely occurs where permafrost is close to the surface [136,435,472], and grows poorly in sites with stagnant water [305] or high water tables [119]. Trees are often stunted and scrubby when growing in stagnant water or where soils are very dry [394]. White spruce seedlings are less tolerant of cold or flooded soils than black spruce, Rocky Mountain lodgepole pine, and tamarack seedlings [458]; and white spruce trees are less tolerant of long periods of flooding than balsam fir and black spruce trees [6].
White spruce tolerates a range of fertility levels [305], but moderate fertility is necessary for good growth [394]. The most productive white spruce stands occur on deep fertile soils on floodplains where periodic flooding enriches the soil [119,303,356]. White spruce also grows in nutrient-poor soils such as in the open spruce-lichen woodlands in northern Quebec [292]. White spruce growth is more sensitive to nutrient deficiencies than associated species including black spruce, red spruce, and pines [394]. In the Lake States, white spruce has higher nutrient requirements than associated conifers (jack pine, red pine, eastern white pine) [305].
White spruce grows on both acidic and alkaline soils. Optimum pH values are likely between 4.7 and 7.0 or higher [305]. In Alaska, white spruce typically occurs on sites with higher pH than that of black spruce [349]. In interior Alaska, soil pH values ranged from 5.0 to 8.2 on white spruce-dominated floodplains [474], and mean pH was 5.4 on upland white spruce sites [417]. In the Black Hills of South Dakota and Wyoming, pH ranged from 5.4 to 7.3 in white spruce communities [184]. In northern Quebec, white spruce often occurs on highly acidic soils with pH ranging from 3.1 to 4.6 [245,292].
Organic layer depth varies in white spruce communities depending on local site characteristics, associated species, and time since fire. In warm, relatively dry upland white spruce stands in interior Alaska, the moss-organic layer may be only 0 to 4 inches (0-10 cm) deep, [434] (reviewed in [40]), while mature white spruce stands on Alaskan floodplains may have a continuous carpet of feather mosses 4 to 8 inches (10-20 cm) deep [413]. Organic layer thickness increases with time since fire. On interior Alaskan white spruce sites, the organic layer gradually thickens from almost nothing immediately after fire to ~5 inches (12 cm) deep in 150- to 200-year-old stands, and splendid feather moss may form an 8 to 10 inch (20-25 cm) deep carpet [137]. In mature white spruce-quaking aspen stands in west-central Alberta, the mean forest floor thickness ranged from 2.3 to 2.4 inches (5.8-6.1 cm) [253]. In mixed white spruce and black spruce-lichen woodlands in northern Quebec, the lichen mat was 2 to 4 inches (5-10 cm) thick in sites that had not burned in >100 years [292]. In Alaska, forest floor temperatures are lower and soil moisture is higher in black spruce forests than in white spruce forests because black spruce forests typically have thicker organic mats [414].
White spruce grows in all soil textures [119], often dominating in sandy or gravelly alluvial soil [67,203,400]. On the southern shore of Walker Lake, northern Alaska, white spruce dominated on river deposits and soils with at least 85% sand, and black spruce dominated on soils with 49% to 69% sand [67]. Although white spruce may have "exceptionally good development" on clay soils [305], seedlings may die if clay soils become water saturated and have insufficient aeration [145].
Many wildlife species use white spruce communities. Mammals using white spruce communities as habitat include red squirrels [14,48,169,217], snowshoe hares [13,169], American marten [269,423], voles (northern red-backed voles, meadow voles, yellow-cheeked voles) [269,423], moose [289,324,412,443,452], American black bear [368], and caribou [237,370,380]. A variety of bird species use white spruce communities [76,182,295,364,398], including woodpeckers [195,295,398] and sharp-shinned hawks [70]. Many birds nest or forage in white spruce trees (reviewed in [364]).
Many wildlife species are adapted to particular successional stages in white spruce communities. For example, moose [246,410], black backed-woodpeckers [195,364], other woodpeckers [195,364], and northern hawk owls [165,364] use early postfire stages. Caribou use late-seral, open lichen woodlands dominated by white spruce as winter habitat in northeastern Alaska. In these woodlands, fires reduce available lichens in the short-term, which are the principal winter forage [237].
In interior Alaska, all white spruce postfire successional stages have important food sources for browse animals. In the earliest stages (1-5 years after fire), young trees (e.g., quaking aspen and paper birch) are most heavily browsed; in early-to midseral stages (6-50 years), willows are most heavily browsed; in late-successional white spruce stands (>50 years), non-willow shrubs are most heavily browsed [136]. In general, the greatest variety of wildlife occurs during the tall shrub-sapling stage (6-25 years), when plentiful forage, cover, and denning/nesting sites are available [410].
See Appendix C for links to FEIS reviews available for animal species mentioned in this section.
Wildlife population trends after fire: On white spruce sites on the Kenai Peninsula, moose populations are largest during early postfire succession [246,310,324,368,382,443,452,453]. After fire, willows, quaking aspen, and paper birch provide winter browse on white spruce sites. Browse production and density are generally high from about 7 to 30 years after fire and peak 15 years after fire [310,382,453]. Moose populations increase and are maintained from about 5 to 25 years after fire, sometimes much longer, as long as adequate forage is available; this is especially true in wintering areas [382,452]. Mature white spruce stands (>100 years old) lack enough willow to maintain moose herds, and paper birch browse is too tall (reviewed in [443]). Although mature white spruce stands provide less browse than early seral stands, mature stands comprised of paper birch, white spruce, and quaking aspen may provide year-round escape cover and winter refugia from deep snow. These stands may also provide alternate food sources such as mountain cranberry, which can be of considerable importance [246].
On the Kenai Peninsula, American black bears, hereafter 'bears', use mixed spruce (white and black)-hardwood sites in early- mid- and late-successional postfire stages. Bear density was similar in recent (13- to 18-year-old) and intermediate-aged (35- to 40-year-old) burns. However, bears in the recent burn had superior growth and reproduction, likely because they ate 4 times more moose calves than bears in the intermediate-aged burn. The recent burn was excellent moose habitat and had twice as many moose as the intermediate-aged burn. Bears living in both the recent and intermediate-aged burns migrated to old-growth stands each summer to eat devil's-club [368].
On the Bear Creek Fire, interior Alaska, American martens used burned (7-8 years after fire) and unburned white spruce habitat, because both provided food and winter cover. Most American marten observations were in unburned white spruce, a habitat that the author speculates has greater value for cover than for food. However, the burned white spruce forest had excellent cover and was used for resting and hunting. While northern red-backed voles (stable American marten food) were most abundant in unburned forest, tundra voles and meadow voles (preferred American marten foods) were most common in burned forest. The author concluded that fires may benefit American martens because fires create and maintain heterogeneous habitats [423].
Population dynamics of gray wolves were minimally affected after a 208,800-acre (84,500 ha) wildfire burned white spruce and black spruce forest and tundra communities in northwestern Alaska. Fire severity ranged from unburned to high severity. Gray wolves used the burned area more than expected during the summer of the fire and the following summer, but less than expected during the 2 subsequent winters. The authors suggest that lower use of the burned area during winter was due to shifts in caribou distribution, possibly caused by the fire. Gray wolf use of the burned area resembled prefire use 3 years after the fire [20].
Black-backed and three-toed woodpeckers occupy recently burned white spruce forests. Black-backed woodpeckers are extremely rare and three-toed woodpeckers have low population densities in interior Alaska; however, after the Rosie Creek Fire, both woodpeckers were common on the perimeter of burned mature white spruce stands. Black-backed woodpeckers were common in burned white spruce stands for 2 years after fire, rare 3 years after fire, and absent by the 4th postfire year. Black-backed woodpeckers fed almost exclusively on larval wood-boring beetles on moderately to heavily burned trees. These insects occurred on dying trees for only 2 to 3 years after the fire. Three-toed woodpeckers were common to abundant the 2nd winter after the fire and much less common to rare by the 3rd winter after fire. Three-toed woodpeckers primarily fed on bark beetle larvae on lightly to moderately burned trees. By the 3rd postfire year, bark beetle populations had declined [295]. In east-central Alberta, black-backed woodpeckers occurred in white spruce stands that burned 2 years prior; the nearest black-backed woodpeckers detected in unburned forest were in old white spruce stands 46 to 93 miles (75-150 km) from the fire. Three-toed woodpeckers were not detected in mature stands [195]. In mixedwood stands in north-central Alberta, bird communities were compared among stands that were either burned or logged 1 to 28 years prior. Black-backed and three-toed woodpeckers occurred only in stands that burned 1 year prior; they did not occur in older burned forests or forests that were logged [183].
Bird surveys in the Kluane Ranges, Yukon Territory, showed little difference in density, species richness, or species composition across 6 lowland (i.e., not subalpine or tundra) communities spanning several successional stages, although some species were more abundant in specific successional stages. A few species (darkeyed junco, Swainson's thrush, yellow-rumped warbler) were abundant in every seral stage. Wilson's warblers and American robins were less common in mature white spruce forests than in earlier stages of succession. In mature white spruce forests, 16 species were found. Darkeyed juncos were most abundant, followed by yellow-rumped warblers and boreal chickadees; these 3 species made up 55% of the total bird density in white spruce forests. The few differences in species composition along the successional sequence were mainly due to more aerial insect feeders (Bohemian waxwing, alder flycatcher, western wood pewee, and olive-sided flycatcher) on burned areas than elsewhere [398].
Literature reviews and meta-analyses of bird community composition after fire or harvest indicate differences among disturbance types, seral stages, and forest types in boreal forests of western North America. Bird communities present immediately after harvest differed from those present after fire, but these differences disappeared with stand age. After fire, communities are dominated by birds that nest in cavities of snags and/or forage on beetles that occur in snags. Both logged and burned sites were dominated by relatively few bird species 31 to 75 years after disturbance. Some birds that use old forests were present at this time, and then bird species richness increased 76 to 125 years after disturbance; however, bird community composition differed among quaking aspen, mixedwood, and white spruce forests. Most of the bird species common in white spruce forests >76 years old were also present in mixedwood forests, especially mixedwoods >125 years old. As mixedwood stands aged and became increasingly dominated by white spruce, many bird species that nest and forage in large quaking aspen trees became less common. Species reviewed are available in Schieck and Song [364].
Palatability and nutritional value: Wild ungulates and livestock rarely browse white spruce [167,209,228,317,453]. Moose occasionally eat white spruce [247,340,341], but it is generally avoided [340]. During the winter, caribou occasionally eat the needles and branches of small white spruce saplings [380]. Because white spruce is rarely browsed, tree species composition may shift in favor of white spruce under heavy browsing pressure [209,282,317,334]. An extreme example of this occurred in Isle Royale National Park, Michigan, where heavy moose browsing resulted in a "spruce moose savanna" [317].
White spruce is important browse for some birds and small mammals. Snowshoe hares browse white spruce throughout much of its range (reviewed in [168]). In some areas, white spruce is a preferred food, and in other areas, it is avoided (reviewed in [379]). In feeding trials on the Kluane research base, Yukon Territory, mature white spruce twigs were a consistently preferred food (ranked 2 of 10), while juvenile white spruce twigs were rarely eaten [379]. Snowshoe hares eat the resinous buds and new growth of seedlings and young trees, which may cause extensive damage and mortality [13,439]. In interior Alaska, white spruce needles are an important food source for spruce grouse in the late fall and winter [448], although white and black spruce needles are eaten less than needles of other conifers, and saplings <14 years old are avoided [51]. White spruce is more palatable to spruce grouse than black spruce (reviewed in [51]). In interior Alaska, red squirrels eat white spruce buds when the seeds are not available [48].
Numerous birds (reviewed in [148]) and mammals eat white spruce seed. It is a primary food for red squirrels, which harvest and cache white spruce cones and eat the seeds [48,90,326,381,390]. In some years, seed predation by red squirrels may substantially reduce regeneration [390] (see Cone and seed production). Deer mice, northern red-backed voles, meadow voles, and shrews eat white spruce seed after it is dispersed [439,470].
Cover value: White spruce provides good cover for moose, white-tailed deer, and ruffed grouse. In south-central Alaskan boreal floodplains, moose rest in shaded, mature white spruce forest during sunny, spring days even though forage may not be available [74]. On Isle Royale, moose used balsam fir-white spruce habitat during a period of deep snow, probably because snow was more shallow under the dense canopy than elsewhere on the Island [228]. In the Black Hills, where white spruce occurs at high elevations and on cool slopes and valley bottoms, white spruce habitat may provide important thermal and hiding cover for white-tailed deer in the summer and fall (reviewed in [376]). In southwestern Alberta, ruffed grouse preferentially select drumming sites with young white spruce cover [38]. Along the Tuchodi River, British Columbia, elk rarely use mature white spruce forest for forage or for resting [323].
In interior Alaska, sharp-shinned hawks nest in white spruce trees that occur within a matrix of hardwood trees [70].
White spruce is one of the most important commercial species in North American boreal forests [305] and is considered the most important commercial species in Alaska [291,444]. White spruce wood is light-weight, straight grained, and resilient. It is used primarily for pulpwood and as lumber [96,305,314]. The best timber often occurs on well-drained soils in river bottoms [291,428,444].
Historically, white spruce bark was used to cover dwellings and for smoking hides, roots were used for lashing in baskets and canoes, boughs were used for bedding, and pitch was used in medicines [189,305]. For additional information about Native American uses for white spruce, see the University of Michigan's database of Native American Enthnobotany.
White spruce typically grows in areas with a >60-day growing season, although the growing season ranges from about 180 days in parts of Maine to 20 days in parts of Canada (reviewed in [304]). New growth begins in the spring [305]. Pollination occurs over a 3- to 5-day period in May, June, or July depending on the location and climate. In general, trees at northern and treeline locations are pollinated later than trees at southern and lower elevation sites (reviewed in [305,472]). Seed dispersal typically begins in August, peaks late-August through October, and continues throughout the winter (Table 1).
Table 1. Regional phenology of white spruce State or province Event Period Alaska, interior pollination late May to early June [470] seed dispersal begins early Aug. [475] early Sept. [471] mid-Sept. [468] peak seed dispersal early to mid-Sept. [475] Sept. [471] British Columbia reproductive buds differentiate & shoot growth ceases mid- to late July male buds become dormant Oct. 1 female and vegetative buds become dormant mid-Oct. (reviewed in [305]) seed dispersal begins Aug. [109] peak seed dispersal Sept. to Oct. [109] Manitoba seeds disperse early Aug. to late Sept. [440]White spruce seeds disperse when cones dry out and open in late summer and early fall, when the moisture content of the cones is about 28% [82]. In interior Alaska, Zasada and others [471] found that cone moisture content ranged from 25% to 80% shortly after seed dispersal began. Most seed is dispersed during the early dispersal season (i.e., typically late summer and fall), although some seeds are dispersed in the winter, spring, and early summer [109,352,356,385,457,464,472]. In Quebec [352], British Columbia [109], and interior Alaska [464], >50%, 70%, and 75% of the seeds are dispersed by the end of October, respectively. In Alaska, 75% to 90% of the seeds are dispersed within 3 to 4.5 months after initial cone opening [466,475].
Seeds released during the peak dispersal period generally have higher quality than seeds released outside of the peak period [109,148,352,464,468]. In the Bonanza Creek Experimental Forest, interior Alaska, seed viability decreased from late September (>70% viable) through March (~30% viable) [468]. In Quebec, white spruce seed viability was highest during peak seed dispersal (September-October) and gradually decreased through winter and spring, with minimum viability occurring in July and August [352]. Along the Tanana River, interior Alaska, where most seeds were not filled, >75% of the filled seed was released before mid-October [464].
White spruce seeds typically germinate during early summer, although germination may occur from mid-May through early August [305,356,471]. Generally, germination is 75% to 100% complete by early July (reviewed in [305]). Following a high seed production year in the Bonanza Creek Experimental Forest, germination patterns reflected soil moisture content. Germination peaked between late May and early June (after snowmelt) and again between late July and early August (after heavy rainfall) [471]. See Germination for additional information about germination requirements.
Plant growth: Although white spruce is shade tolerant, seedlings require open conditions for optimal growth [124,225,305], and they grow fastest in sunny sites. In interior British Columbia, seedlings grown in 60% light were almost twice as tall as those grown in 20% light [124]. During their first growing season, seedlings typically grow 0.4 to 0.8 inches (1-2 cm), and roots may grow 0.8 to 4 inches (2-10 cm) deep [305]. In productive, upland sites in Alaska, the tallest seedlings were 1.2 to 1.6 inches (3-4 cm) tall and maximum root length was >4 inches (10 cm) by the end of the first growing season [470,471]. However, white spruce often grows very slowly in less favorable conditions. Seedlings (<5 feet (1.5 m) tall) in the understory of conifer and hardwood stands are often more than 40 years old [124,473]. Although initial white spruce growth is slow, growth often accelerates when the trees are mature [124,178].
White spruce seedling growth is typically slower than that of associated shrubs and hardwoods [59,356]. On the Tanana River floodplain in interior Alaska, seedlings of feltleaf willow, balsam poplar, and white spruce showed mean annual height growth of up 3.5, 4.7, and 0.8 inches/year (9, 12, and 2 cm/year), respectively (reviewed in [470]). Open grown white spruce seedlings may grow to 5 feet (1.5 m) in approximately 20 years, which is much slower than sprout growth of associated hardwoods [473].
White spruce seedlings that establish immediately after disturbance typically grow faster than those that establish later. In interior Alaska, "dominant" seedlings that germinated 1 year after seedbed clearing averaged 7.3 inches (18.5 cm) tall by the 5th growing season, whereas those that germinated 3 years after clearing were 2 inches (5 cm) tall; the same height as the regenerating mosses. While the later-germinating seedlings were younger, the authors suggested that the 1st seedling cohort would continue to dominate the site because the later cohort competed with mosses for moisture, light, and nutrients and thus grew more slowly [471]. After stand-replacing fires in interior Alaska, white spruce growth rates differed depending on when they established relative to hardwoods. When white spruce seedlings established at approximately the same time as quaking aspen and paper birch, they grew much faster than when they established ~25 years after the hardwoods (Figure 10) [463].
White spruce grows slowly when it occurs under poor site conditions. In Alaskan floodplain forests, white spruce growth is greatly reduced after 100 years. This reduction of growth may be due to cold soil temperatures caused by the insulating effect of the organic mat, which deepens in older stands (reviewed in [303]). In interior British Columbia, seedlings grew more slowly in litter than in mineral soil, although this effect was not significant until the seedling's 3rd growing season [124]. At treeline sites, where growing conditions are marginal, trees typically grow slowly and white spruce often forms shrub-like trees [40,305].
White spruce tree growth is influenced by climate. White spruce growth and temperature have positive relationships in many sites [12,18,393]; however, white spruce growth may be inhibited by moisture stress when warm temperatures are coupled with low precipitation [64]. For instance, in interior Alaska, white spruce trees often grow best in the coolest, wettest years [255]. See Climate change for more information on climate-growth relations and FIRE REGIMES of Alaskan white spruce communities for information about climate-growth relations in Alaska.
White spruce depends on annual seed production for regeneration [305,351]. White spruce does not have serotinous cones, and seeds do not persist in the soil. Because seed matures and falls within 1 year, there is no seed stored in trees [436].
Although white spruce does not have serotinous cones, crown-stored seed may occasionally be available after fire depending on fire timing, severity, and type [157,169,170,288,468]. Crown-stored seed is more likely to be available after fires in late summer—after seed is ripe, but before it is dispersed [288,466]. However, fires generally occur before white spruce seed is ripe; in Alaska, more than 86% of all fires occur before white spruce seed is mature [466]. One growing season after the August 1977 Bear Creek Fire in interior Alaska killed all the trees but left the canopy intact, white spruce seedlings were abundant (12,000 seedlings/acre (30,000 seedlings/ha)), which suggests that there were abundant crown-stored seeds even after the fire killed the trees [169,170]. In the Bonanza Creek Experimental Forest, fire-killed white spruce produced and dispersed viable seeds after an early season fire. The fire occurred at about the time of white spruce pollination, and female flowers were not affected by the severe ground fire. Trees that died by late summer due to severe burning of the roots and lower bole still produced large quantities of viable seeds (80% viable); trees with scorched or burned crowns did not produce seeds [468]. Simulation experiments suggest that white spruce seed contained in closed cones may survive heating by crown fire, and that approximately 12% of cones would contain viable seed after fire. However, the probability of a fire occurring when germinable seed is contained within cones (i.e., mid- to late-season fire) and coinciding with a mast year is low (perhaps 0.05) [288]. Crown-stored seed may explain why white spruce occasionally has high postfire recruitment [169,170], including in areas far from fire edges [288], and why even-aged white spruce stands occasionally develop after fire [137,430,431,460].
Soil seed banking does not appear important to white spruce, because seeds do not remain viable in the soil for long. Viability of seed in cones cached by red squirrels drops to nearly 0 after 1 to 2 years [305]. In quaking aspen mixedwood in Alberta — where white spruce comprised <20% of the basal area — no white spruce seed was found in the soil seed bank in unburned, lightly burned, or severely burned plots [242]. Seed bank samples near treeline in the Tuktoyaktuk region of northwest Canada yielded no germinable white spruce seed [283].
White spruce sometimes has "seedling banks" rather than soil seed banks [351,473], but seedlings would not survive fire. Seedling banks may establish after mast years when abundant seed germinates. Because mast years are episodic, seedling banks are replenished episodically and form a discontinuous age structure [351].
Wind disperses white spruce's winged seeds [109,356,464]. The seeds are small and lightweight [82,356,471]. Most seeds fall within 2 tree heights, or 150 to 200 feet (45-60 m) from parent trees [430,436,466]. Seed density declines rapidly with distance from source trees [468], although seeds have been reported at more than 1,300 feet (400 m) from their source [465]. Seeds may disperse up to 330 feet (100 m) from the stand edge, although most seeds fall within the stand [109,464]. Late-dispersed seeds may be blown over crusted snow and ice [145,157,457]; in clearings, these seeds may be found at greater distances from their source than in forested areas [109,157]. Although dispersal over snow generally contributes little to total seed dispersal, in central Quebec, 30% to 50% of the white spruce seed crop falls on snow, facilitating dispersal distances greater than a few hundred meters (personal communication in [157]).
Seed dispersal distance is influenced by release height, intercepting canopy, and windspeed. White spruce seed dispersal through quaking aspen forests was studied by releasing artificial "seed" from different heights of a meteorological tower. Mean dispersal distance increased with height of release. Windspeed is affected by the forest canopy, and dispersal distances were consequently affected by canopy characteristics. Before quaking aspen leaf fall, most "seed" landed close to and in all directions around the tower. After leaf fall, the mean dispersal distance increased, with peak densities occurring 50 feet (15 m) downwind of the tower. However, actual white spruce seedlings were found much farther away from isolated white spruce seed trees within quaking aspen stands than the seed dispersal distances observed during the experiments. This suggests that most white spruce seed is released at much higher windspeeds than those observed during the experiments [384].
In general, seeds that fall closer to the parent tree are more likely to be viable than seeds that are dispersed farther away. In a mature white spruce stand bordering a clearcut in central British Columbia, seeds were estimated to be 48% sound within the first 330 feet (100 m) of the stand and 31% sound in the next 330 feet (100 m). However, seed density 990 feet (300 m) into the clearcut still exceeded about 300,000 seeds/acre (740,000 seeds/ha), suggesting adequate quantities of seed were available to regenerate that far into the clearcut [109]. On a floodplain island of the Tanana River, interior Alaska, few seeds dispersed beyond 390 feet (120 m) [464].
White spruce seed dispersal and seedling establishment may be limited within large fires [436]. White spruce seed in burned areas is typically dispersed from unburned trees within or adjacent to the burned sites, because white spruce trees are usually killed by fire and cones are not serotinous [156,263,466]. White spruce regeneration densities are typically highest along old fire edges and near unburned patches [145,156,457], because seed dispersal is greatest close to unburned source trees and stand edges [109,464]. See Seedling establishment and Plant response to fire for more information about seedling establishment after fire.
Water may disperse white spruce seed along floodplains. Water-dispersed seed may be deposited in shrub and balsam poplar stands by late summer floods. Occasionally, white spruce establishes and forms dense stands early in the floodplain successional sequence [303]. See Floodplain succession for more information about succession on Alaskan floodplains.
White spruce often establishes after fire when seed and suitable seedbeds are available [72,328,329], although establishment later in succession is also common [17,34,67,83,145,148,329,463]. Establishment may be particularly high following episodic mast years [351], especially when masting and fire coincide [328]. Establishment rates are highly variable [148] and depend on several factors. Most importantly, adequate seed sources must be in close proximity to suitable seedbeds during favorable weather conditions. See Plant response to fire for additional information about regeneration of white spruce after fire.
Fire typically creates favorable seedbeds for white spruce, and white spruce seedlings often establish soon after fire [328]. Establishment also occurs episodically following mast years [328,351] and may be high when fires and masting coincide [327,328,330,336]. Studies in Alberta mixedwoods show mixed results. Over a 59-year period, white spruce densities were 2.5 times higher after mast-year fires than after fires in years of low cone production (P <0.001). In nonmast years, 53% of the stands had no postfire recruitment. Large cohorts did not occur when mast years occurred ≥4 years after fire, and very little regeneration occurred 7 to 20 years after fire [328]. After a mast-year fire where nearby seed sources were abundant, there was a complete lack of recruitment because a thick organic layer remained. White spruce seedling density 1 year after fire was negatively associated with organic layer depth and distance to seed source, and positively associated with seed source strength (P <0.01) [336]. A retrospective study of 5 fires in white spruce-dominated mixedwoods in central and northeastern Alberta, including 3 fires that occurred during mast years, found poor white spruce establishment. Fires occurred during the early summer before seed was ripe and likely resulted in poor organic matter consumption (not measured); very few seed trees remained on site or nearby [147].
While white spruce seedling establishment is often abundant after fire, many studies describe a more complex pattern of white spruce regeneration [17,34,67,145,330,429]. Out of 20 stands in Alberta boreal mixedwoods, 7 stands were dominated by initial postfire regeneration, 6 were dominated by delayed regeneration, and 7 had even mixtures of initial and delayed regeneration. Even when initial postfire regeneration is high following mast-year fires, delayed regeneration may constitute proportionally more of the total regeneration [329]. White spruce regularly established during the 75 years after fire in a Quebec southern boreal forest [34]. In boreal mixedwood forest, northwestern Quebec, white spruce established in 2 peaks after a stand replacement fire. The first peak occurred approximately 10 years after fire, and a second smaller peak occurred approximately 50 years after fire. The authors suggested that the first cohort was a likely seed source for the second cohort [145]. In black and white spruce woodlands of the central Brooks Range, Alaska, white spruce had a broad establishment period after fire without prominent peaks [67]. A chronosequence study of 35 stands in Saskatchewan southern boreal mixedwoods, which ranged from <1 to >200 years old found that white spruce seedlings established immediately after fire and recruitment continued at varying rates, peaking 50 years after fire at about 500 seedlings/acre (1,250 seedlings/ha). Seedling density was lowest between 110 and 125 years after fire. A second wave of recruitment began 127 years after fire and peaked 172 years after fire, at 622 seedlings/acre (1,537 seedlings/ha). The second peak in seedling recruitment may have resulted from the higher density of seed trees, increased light intensity due to gap formation, and increased availability of logs [17].
Most white spruce germinants die before they become established due to unfavorable seedbed and weather conditions, or smothering under leaf litter. Hot, dry summers tend to dry out the seedbed, especially on open sites (including recent burns) and sites with course-textured soil, feather mosses, and/or litter. Consequently, seedlings commonly die due to moisture stress or heat injury [123,148,178]. In interior Alaska, white spruce seedlings that germinated in May and June were most likely to die during their first summer, when conditions were hot and dry. Seedlings that germinated in July and August were most likely to die during their first winter. Most seedlings that survived the first summer and winter survived through the 5-year study period [471]. In 4 balsam fir-dominated stands in Quebec, white spruce seedling survival through their first winter ranged from 4% to 20% [351]. White spruce seedlings do not establish well in leaf litter, especially on hardwood sites, because the small seedlings get smothered and crushed under leaf litter and typically die [103,148,356,378,472]. It took 4 growing seasons before white spruce seedlings were large enough to avoid being smothered or crushed by leaves in an 80-year old paper birch stand in Alaska (reviewed in [472]). In spruce beetle-killed forests on the Kenai Peninsula, white and Lutz spruce seedling establishment was greater in plots that had <60% cover from litter of bluejoint reedgrass than in plots with greater cover (P = 0.04) [39]. Seedlings also die from frost, snowpress, flooding, browsing, and lack of resources due to competition (reviewed in [148]).
Interference from other species may reduce white spruce's rate of establishment, growth, and survival [58,73,75,122,139,147,148,356,374,441]. White spruce establishes more readily on recently disturbed sites if competition for light, moisture, and nutrients [58,356] is reduced [148,356,377]. After fire in Alaskan boreal forest, competition for nitrogen and carbon by early successional species inhibited white spruce establishment and growth (P ≤0.05). While bluejoint reedgrass appeared to be a stronger competitor than field horsetail, the authors suggested that apparent differences in competitive abilities were better explained by the temperature and moisture microenvironments that these species occupied [58]. In interior and south-central Alaska, growth of planted white spruce seedlings was greater in sites without interfering vegetation. White spruce seedlings were planted in untreated and "weed-free" (herbicide treatments that controlled interfering native vegetation) sites. Mean heights were 1.5 to 3.8 times greater and mean diameters were 2.0 to 3.8 times greater in the weed-free plots than those in untreated plots [73]. In Alaskan boreal forest, logging without disturbing the organic mat often leads to the establishment of bluejoint reedgrass, which may persist for 25 to 100 years, limiting the establishment of white spruce [75].
White spruce may establish on floodplains where deposited alluvium creates a suitable seedbed [62]. On floodplains in interior Alaska, white spruce often establishes in mid-succession under a canopy of balsam poplar; however, establishment may occur episodically after flooding during a good seed year [429].
Overview and trends: Fire initiates succession throughout white spruce's range but is more prevalent in western than in eastern North America. In its eastern distribution (and on relatively wet sites in the west), insect outbreaks and subsequent gap succession may be more important than fire in initiating succession. See Regional studies for more information.
Fires in white spruce communities are often stand-replacing, and postfire succession generally progresses through herb, shrub, and hardwood stages before succeeding to white spruce [136,137,263,415,418,428,430]. The postfire successional sequence depends on numerous factors including fire characteristics (e.g., severity, timing, type), seed availability, seedbed conditions, site characteristics, weather, and prefire plant community composition [147,329,336,356,436]. See Plant response to fire for more information about how these factors affect recruitment and succession after fire.
White spruce is generally considered a mid- to late-successional species [79,172,177,192,244,375], but it occurs in all stages of boreal forest succession. White spruce often colonizes recently disturbed sites [169,170,328,329,336] (see Seedling establishment) but it is also shade tolerant [178], and can establish years or decades after disturbance [17,34,67,145,330,429]. White spruce seedlings often persist in the understory for extended periods before emerging to the canopy [263,463]. White spruce typically becomes dominant when early-seral trees, such as quaking aspen, paper birch, and lodgepole pine die off [79,137,192,418]. White spruce forests may be more persistent than other boreal forest types (e.g., lodgepole pine, quaking aspen, paper birch) because white spruce is more shade tolerant and longer-lived than these species, and because it can regenerate in the shade of mature forests [136,355].
White spruce regeneration and succession following stand-replacing fire can follow two routes: delayed regeneration or self-replacement. When regeneration after fire is delayed, white spruce typically establishes and grows beneath a canopy of hardwoods (paper birch and quaking aspen in upland stands, balsam poplar in riparian stands) before eventually succeeding to dominate in mature stands (reviewed in [83]). Most studies indicate that delayed regeneration typifies white spruce stand development [17,34,67,145,330,429]. White spruce generally does not replace itself [65], due to limited seed sources after fire and inadequate seedbed conditions [328,336]. Occasionally, white spruce establishes prolifically after fire along with the hardwoods. When this occurs, white spruce forms part of an even-aged stand [137,430,431,460] and succession towards a white spruce-dominated community is accelerated [463].
Successional trends in the North American boreal forest depend, in part, on differences in fire frequency. When fire is frequent, the same species that colonized the stand after fire may dominate until the next stand-replacing fire. This leads to the persistence of shade intolerant species such as jack pine, quaking aspen, and paper birch. In contrast, when fire is infrequent, stands eventually become dominated by shade tolerant species such as white spruce, balsam fir, and northern white-cedar. Succession on mesic eastern, central, and west-central North American boreal forests is summarized and reviewed by Brassard and Chen [46]:
Floodplain succession in Alaska and western Canada follows similar sequences. Generally, forbs and willows colonize new alluvium, followed by alders, balsam poplar, and white spruce [418,439]. However, floodplain succession is not fully predictable due to differences in disturbances, seed dispersal, seedling establishment, weather, and site characteristics [188,404,442]. Old growth riparian white spruce forests may persist for 200 years or more because natural firebreaks inhibit fires in large river valleys. Consequently, floodplain white spruce forest tends to have more old growth than boreal uplands [404]. On some sites, white spruce floodplain forests may be replaced by black spruce as the organic layers thicken, soil cools, and permafrost forms [413,415,426,428,429]. See Regional studies for further discussion.
Insects: Insect outbreaks—especially those of eastern spruce budworm and spruce beetles—affect forest structure and successional patterns in portions of white spruce's distribution. Both insects preferentially attack large, overstory host trees leaving the understory intact and able to emerge into the canopy.
Figure 8. Eastern spruce budworm damage in white spruce. Figure 9. Spruce beetle kill of white spruce, Kenai Peninsula. Photo by William M. Ciesla, Forest Health Management International, Bugwood.orgEastern spruce budworm occurs in the eastern portion of white spruce's range; its distribution coincides with the range of balsam fir and spruce. Balsam fir is the preferred host species, but white spruce, black spruce, and red spruce are also attacked [46]. Unlike fire, which kills all or most conifers, eastern spruce budworm kills only some of the trees in a stand. Overstory hosts are killed or weakened, and smaller understory trees are spared [41,46,478]. Host trees die due to the chronic stress of intense defoliation, which often occurs over multiple years [365]. Between 1704 and 1950, eastern spruce budworm outbreaks occurred at 30- to 138-year intervals from western Ontario to eastern Quebec and Maine. In order for an outbreak to occur there must be extensive stands of mature balsam fir. Frequent fires limit balsam fir abundance, and, therefore, eastern spruce budworm epidemics. In drier regions where fire is more common, such as western Ontario, fewer old trees are available, and outbreaks are more limited in area. Consequently, outbreaks occur more frequently in the Atlantic region than in Ontario [37].
After an eastern spruce budworm outbreak kills overstory trees, understory trees typically emerge into the canopy [41,478]. Successional patterns depend on species composition before and after the outbreak [41]. While white spruce saplings may be available to grow into the canopy [41], balsam fir [41,478] or hardwoods [422] are more likely to replace the killed trees, and white spruce abundance may decrease after an outbreak [36,41]. In western Quebec mixed forests, an outbreak reduced white spruce from 44 trees/acre (108 trees/ha) to 24 trees/acre (36 trees/ha). There were only 30 saplings/acre (75 saplings/ha) of white spruce after the outbreak, while saplings of balsam fir were 80 times more abundant. White spruce was likely to be less common in the overstory after the outbreak than before [41].
Spruce beetle outbreaks occur in south-central and southwestern Alaska [32,39,190,373,454] and southwestern Yukon [32,185]. Spruce beetles do not normally kill all the trees in a stand, even during high-severity outbreaks [373]. Spruce beetles preferentially attack large-diameter mature spruce (white spruce, Lutz spruce, Sitka spruce, and rarely black spruce). Stands with high densities of mature white spruce are preferentially attacked, whereas stands with high densities of black spruce tend to be avoided (reviewed in [454]). Across south-central and southwestern Alaska, a 250-year record shows that the interval between outbreaks ranged from 10 to 165 years and averaged 48 years [373]. In white spruce and Lutz spruce forests on the Kenai Peninsula, spruce beetle outbreaks occurred every 50 years on average, whereas fires occurred approximately every 400 to 600 years [31]. This suggests that historically, spruce beetle outbreaks may have been a more important disturbance than fire in this region.
Vegetation change and succession following a spruce beetle outbreak vary by region due to differences in climate, soils, and competitive interactions among species [454]. On the Kenai Peninsula, vegetation change following recent spruce beetle outbreaks varied among geographic regions and forest type. On the southern Kenai Lowland, where white spruce was dominant, white spruce had high mortality (87% reduction in basal area of white spruce >5 inches (12.7 cm) DBH), and forests shifted toward early successional grasses and forbs. White spruce forests were converted to woodlands and herbaceous types due to expansion of bluejoint reedgrass populations and low densities of tree seedlings. In the Kenai Mountains, where stands were dominated by mountain hemlock and white spruce, white spruce had moderate mortality (46% reduction in basal area), and forests shifted towards a late-successional structure dominated by mountain hemlock. In another region of the Kenai Peninsula, where white spruce was a secondary species in mixed stands and had low mortality (28% reduction in basal area), no substantial shift in successional direction was detected. Over the entire study area, the authors speculated that 3% of the 115 plots had poor chance for forest regeneration due to abundant bluejoint reedgrass cover and lack of overstory trees. These areas are in the southern Kenai Lowlands [43]. On the Cook Inlet, a severe outbreak in the 1970s caused 65% mortality of white spruce >5 inches (12.7 cm) DBH. Paper birch became the dominant tree species in the residual stand (reviewed in [454]).
Gap succession: Insect outbreaks, mortality of individual trees, windthrow, and fungi can create gaps in communities where white spruce occurs. Gap dynamics are important in shaping forest structure, especially where fire-return intervals are long [46]; small-scale gap dynamics may shape succession in old growth stands in the east [278]. While succession throughout much of the boreal region is characterized by shade-tolerant species replacing shade-intolerant species, gaps allow early-successional species, such as hardwoods, to persist in late successional stands [422]. In northwestern Quebec mixedwoods, group tree mortality created small gaps in young (50-year-old) quaking aspen-dominated stands, and eastern spruce budworm created large gaps in old (234-year-old) balsam fir-dominated stands [222]. While understory white spruce may replace canopy trees [85,316,353] in small and large gaps, white spruce seedling abundance is generally insufficient for released seedlings and saplings to dominate mixedwood stands [85].
Regional studies: Examples of succession in white spruce communities follow by region.
Alaska: White spruce may be present in all stages of postfire succession in Alaska, although it generally does not regain dominance for over 100 years. White spruce often replaces hardwood (i.e., quaking aspen and paper birch) stands after approximately 100 to 150 years [137,262,264,415,418]; however, extensive fires may occur at about 100 to 150 year intervals in interior Alaska [136], precluding dominance by white spruce on many sites. Consequently, midseral communities dominated by quaking aspen or paper birch, or codominated by white spruce and hardwoods, are common and widespread throughout Alaska on relatively warm, upland sites [136,137,262]; and pure, old white spruce stands (i.e., stage 6, below) are less common than younger stands [136,137].
In the absence of subsequent fire, the most common postfire successional sequence on warm, well-drained white spruce sites in interior Alaska is characterized by white spruce gradually replacing herb, shrub, and hardwood stages [136,137,263,413,415,418,428,430,460]. Similar postfire successional patterns occur on the Kenai Peninsula in south-central Alaska [310]. Foote [137] describes 6 developmental stages in this postfire sequence:
White spruce may be absent or infrequent during the newly burned stage because seed may not be available during the first postfire year. Most white spruce seedlings establish during the first 30 years after fire (during the moss-herb and tall shrub-sapling stages) [137], although seedling establishment may peak again under older white spruce stands [136]. Although the dense tree phase is dominated by hardwoods, mature white spruce increases in density. White spruce gradually replaces hardwoods during the hardwood or mixed hardwood-spruce stage [137]. White spruce regains dominance by establishing and growing under the shade of other trees and living longer than earlier successional species [136].
A less common postfire successional sequence on white spruce sites may occur when white spruce seed is available after fire [137,169,170,262,418,430,431]. In this case, white spruce establishes with the hardwoods within the first few years after fire, and an even-aged white spruce stand may develop [137,430,431,460]. When white spruce establishes after hardwoods, its growth is suppressed by faster growing hardwood sprouts. However, when white spruce establishes along with hardwoods, its growth is less restricted and it reaches the canopy much faster (Figure 10) [463], which accelerates succession towards white spruce.
At arctic treeline, long fire-return intervals or absence of fire may lead to successional replacement of black spruce by white spruce. Following a fire in the early 1900s, black spruce had high recruitment for <30 years, while white spruce recruitment was consistently high after the fire and throughout the study period (about 100 years). By about 80 years after fire, black spruce established via layering, but white spruce establishment surpassed that of black spruce. After 100 years, white spruce seedling density was 14.6±16.9 seedlings/acre (90.3±41.7 seedlings/ha), and black spruce density was 8.7 ± 2.3 seedlings or clones/acre (21.6 ± 5.8 seedlings or clones/ha). This suggests that in the absence of fire, white spruce will become increasingly dominant in these stands [257].
Floodplain succession: Primary succession on floodplains of interior Alaska typically begins with a bare surface adjacent to the river and passes through several developmental stages as river terraces rise and flood frequency decreases. Succession finally stabilizes as mature white spruce or black spruce stands [413,415,418,426,428,429,430]. Van Cleve and Viereck [418] describe 8 successional stages that occur on the Tanana River floodplain:
Although white spruce can germinate on mineral soil of newly established siltbars [442], seedlings cannot survive repeated flooding, yearly sediment deposition, high erosion, or periods of drought commonly associated with early succession[13,303,429,430]. Consequently, white spruce often establishes during the shrub and balsam poplar stages and becomes dominant after balsam poplar matures and dies [418,426,429,442]. White spruce may live to be about 400 years old in late-successional floodplain forests [442].
Although succession often follows the general pattern described above, multiple trajectories are possible depending on landscape features, initial establishment, climate, and disturbance agents [188]. Occasionally, white spruce seeds germinate on mineral soil soon after flooding, and a dense, even-aged white spruce stand develops following the shrub stage [303,430]. This tends to occur following major channel shifts rather than during the gradual buildup of floodplain terraces, because shifted channels experience less frequent flooding [303]. Many authors suggest that black spruce replaces white spruce in floodplain forests as the organic layer thickens, soil cools, and permafrost forms [413,415,426,428,429]. However, a chronosequence study on the Tanana River floodplain showed no evidence that black spruce replaces white spruce successionally [188]. White spruce sites had no black spruce seedling or sapling recruitment, permafrost, or shifts in species composition that made them more similar to black spruce sites. Other recent studies suggest that the occurrence of black spruce stands on floodplain sites may be a function of site drainage and fire history [187,188,273]. Black spruce may be restricted to poorly drained back swamps, while white spruce forests dominate the well-drained meander belts [273].
Succession after fire on Alaskan floodplains follows patterns similar to those on uplands, with herbs, shrubs, and hardwoods initially replacing white spruce or black spruce. However, riparian white spruce stands may burn less frequently than upland stands because they are often protected by natural firebreaks (reviewed by [430]). For additional information about FIRE REGIMES in Alaskan floodplain communities, see FIRE REGIMES of Alaskan white spruce communities.
Northwestern Great Plains: In the Black Hills of South Dakota and Wyoming, white spruce is considered the climax species in some ponderosa pine and quaking aspen stands [184,372].
Great Lakes: White spruce is often considered a climax species in the Great Lakes region, although fires typically occur before forests reach climax conditions [177,244]. White spruce increases dominance with stand age [77,198,199] and may codominate late-successional communities [77]. Mature balsam fir-white spruce stands often experience eastern spruce budworm outbreaks that alter successional patterns [176].
In many areas of the Great Lakes region, balsam fir, white spruce, northern white-cedar, and paper birch dominate late-successional forests. In the absence of fire, earlier seral stands of red pine, eastern white pine, or jack pine often succeed to stands codominated by white spruce [77,177,244]. In the Boundary Waters Canoe Area, Minnesota, jack pine can persist in the overstory for 210 to 250 years, but these communities will likely succeed to balsam fir-spruce-northern white-cedar-birch or black spruce-feathermoss communities without fire. In red pine and eastern white pine stands that have not burned in a long time, balsam fir, white spruce, northern white-cedar, and paper birch establish and grow in the understory [177], where they are poised to recruit into the overstory as the pines die out. In Isle Royale National Park, basal area and relative density of white spruce increase with stand age, while shade-intolerant species (e.g., paper birch, quaking aspen, and jack pine) decrease [198,199].
In northeastern Wisconsin, white spruce occurs in the sapling layer in stands that were logged and burned more than 100 years prior. For ~80 years following logging and fire, paper birch and quaking aspen dominated the site. By ~100 years, red pine and eastern white pine regained dominance and balsam fir, sugar maple, and white spruce saplings dominated the understory. The composition of the sapling layer suggests that the pines will eventually succeed to balsam fir, sugar maple, and white spruce in absence of disturbance [383].
On upland mixedwood forests in Algonquin Provincial Park, Ontario, succession after fire generally proceeds from paper birch-quaking aspen to either balsam fir-white spruce, or from eastern white pine to shade tolerant hardwoods (mostly sugar maple), and finally to eastern hemlock. After fire, white spruce may establish with the faster growing hardwoods, but it typically does not codominate stands until after the hardwoods decline [275].
Northeast: In northern New England, white spruce occurs in many stages of succession. It is a pioneer species following blow-downs and other disturbances that create extensive openings. Along the Acadian coastline, white spruce often colonizes abandoned agricultural land and forms a distinct border [95]. While considered a climax species [318], it is less shade tolerant than associated eastern species (i.e., red spruce and balsam fir) [55,95]. White spruce may die off in closed stands, which favor dominance by red spruce [95].
Fire histories and consequent patterns of succession were not well documented for red spruce-white spruce forests of New England (as of 2015). It is likely that successional patterns of white spruce in New England are similar to those in the Acadian Forest Region, which is discussed in the Eastern Canada section below.Western Canada: White spruce occurs in all successional stages in western Canada, although its basal area typically peaks in mid- to late-successional stands [69]. In British Columbia and Alberta, white spruce tends to replace lodgepole pine and quaking aspen in the absence of fire [69,79,97,192,254,293,296]. After fire, white spruce or western white spruce may establish along with lodgepole pine; however, lodgepole pine dominates early seral stands because it has much higher stem densities and faster initial growth rates [69,79,192]. Lodgepole pines dominates until it dies out, from 70 to 250 years after fire [69,97,192]. Spruce (white and Engelmann) and subalpine fir become increasingly important as lodgepole pine declines [192]. In west-central British Columbia, western white spruce basal area peaked 201 to 250 years after fire when lodgepole pines died [69]. While lodgepole pine stands theoretically succeed to spruce-subalpine fir communities, they are often maintained indefinitely by recurring fires [79,332], especially on dry, west-facing slopes [293]. If subalpine fir-white spruce stands reach a decadent, late-successional stage (>230 years in west-central Alberta), white spruce abundance may decline while subalpine fir increases [97,293].
The rate of succession from lodgepole pine to spruce-subalpine fir depends on initial postfire stand composition and moisture conditions. If spruce (white or Engelmann) does not establish with lodgepole pine after fire, succession is slower than when spruce establishes immediately after fire [79]. In the Alberta foothills, the rate of successional replacement of lodgepole pine by white spruce or Engelmann spruce was associated with moisture conditions. Lodgepole pine had greater persistence in drier conditions [192], possibly because of recurring fires [293].
White spruce replaced quaking aspen before succeeding to balsam fir in a postfire chronosequence in Saskatchewan southern boreal mixedwood forest. Thirty-five stands were studied; they ranged from <1 to 201 years after fire. Mean density of white spruce increased with stand age, peaked 172 years after fire, and declined in stands 175 years old and older. White spruce replaced quaking aspen between 50 and 165 years after fire and dominated the canopy between 93 and 172 years after fire [17].
A chronosequence study in the northern boreal-cordilleran region, central Yukon, describes a postfire successional sequence on well-drained, low-gradient sites. The youngest stands (8-11 years old) were dominated by quaking aspen and willows. Quaking aspen, shrub, and herb cover peaked 50 to 70 years after fire while white spruce cover gradually increased. White spruce began to replace quaking aspen in 50- to 60-year-old stands, and white spruce cover equaled or exceeded that of quaking aspen 90 to 100 years after fire. The author speculated that white spruce replaced quaking aspen faster than it typically does in the southern boreal region because it established early after fire. Rather than white spruce seedlings and saplings filling gaps created by dead quaking aspen, white spruce "forced" the replacement of healthy quaking aspen because it was already established within and directly below the quaking aspen canopy. These stands differ from southern boreal forests in western Canada on similar well-drained sites because lodgepole pine and balsam poplar are infrequent and firs are absent from the northern boreal forests [391].
A study of mid- to late-successional boreal mixedwood stands (120-175 years old) in Riding Mountain National Park, Manitoba, indicates long-term persistence of hardwoods rather than successional replacement by white spruce. The persistence of hardwoods was due to a second cohort of quaking aspen and balsam poplar that established via root suckers after the initial cohort broke up (about 80-140 years after stand establishment). Consequently, 175-year-old stands consisted of a mixture of white spruce and hardwoods. The author suggests that the ability of hardwoods to recruit into late-successional stands indicates that boreal mixedwood communities (i.e., white spruce-hardwood) are self-sustaining and not a transitional phase leading to a white spruce community [248].
A preliminary comparison of burned and unburned subarctic woodland stands in the lower Mackenzie River Valley, Northwest Territories, suggests that without periodic fires, white and black spruce may be eliminated and woodlands converted to a tundra-like moss/lichen association. In sites where fire had not occurred for 150 years or more, there was a dense growth of lichens, few or no tree seedlings, an open, unhealthy spruce stand, and permafrost close to the soil surface. Recently burned areas were initially colonized by liverworts, followed by herbs, mosses and low ericaceous shrubs, and then by a relatively dense and vigorous spruce stand. Fires may be necessary to reduce dense lichen mats and expose mineral soil to enable spruce recruitment [389].
Primary succession on floodplains in western Canada is similar to that of Alaska. Generally, willows colonize new alluvium, and as alluvial deposits raise the ground level above the floodplain, alder, balsam poplar, and finally white spruce forests develop [439]. This pattern is variable since it is subject to stochastic events such as flooding and seed dispersal [404,442]. Old-growth riparian white spruce forests are restricted to terraces of major river valleys where primary succession has continued undisturbed for 200 years or more. Fires are often inhibited in large river valleys because of natural firebreaks such as meanders, oxbow lakes, and seepage sites. There is generally more old growth in boreal riparian white spruce forests than in boreal uplands [404]. In the Peace River Lowlands, Wood Buffalo National Park, succession from old-growth white spruce to black spruce has not occurred [404]. On the most elevated sites of the Mackenzie Delta, white spruce forests are dying out and being replaced by tundra vegetation in xeric sites, and by white spruce/bog woodlands in poorly-drained sites. White spruce seedling establishment is limited to early seral stages and stands that are flooded periodically, have moderately-closed canopies, and have a ground cover of herbs rather than feathermosses and lichens. The authors suggest that a decrease in flood frequency—and consequent poor seedbed conditions—may be responsible, at least in part, for poor white spruce regeneration on elevated sites [321].
Eastern Canada: Although fire occurs throughout eastern Canada, it is more frequent in drier western regions, such as Ontario, than in the moist, eastern Maritime provinces. The general successional sequence after fire in eastern Canadian mixed forests is initial dominance by hardwoods (i.e., paper birch, quaking aspen), followed by successional replacement with white spruce and balsam fir. Without subsequent fire, balsam fir often replaces white spruce. On subalpine sites in central Quebec, it may take between 370 and 480 years before white spruce stands succeed to balsam fir [101]. On some sites, northern white-cedar may replace both balsam fir and white spruce [316]. Where jack pine occurs, it typically dominates the early postfire environment; without fire, these forests succeed to balsam fir and white spruce [172].
Several studies describe postfire successional dynamics in mixedwood stands near Lake Duparquet, northwestern Quebec, where white spruce is an important forest component. Early-seral stands are dominated by shade-intolerant hardwoods (paper birch and quaking aspen) or jack pine. As the initial canopy dies out, midsuccessional stands become codominated by balsam fir and white spruce [33,172,316] (reviewed in [35]). On some sites, the oldest stands may be dominated by monospecific patches of northern white-cedar [316]. Several studies indicate that white spruce importance and basal area peak in midsuccessional stands (approximately 150 years after fire) [33,316] (reviewed in [35]). While white spruce may establish within 10 years after fire, it is typically suppressed and does not reach the canopy until midsuccession because it grows more slowly than the hardwoods [33]. In early succession, white spruce gradually becomes dominant as small gaps are created by the deaths of individual trees or small groups of trees [222,316]. In late succession, large gaps are caused by eastern spruce budworm [222]. After eastern spruce budworm outbreaks, white spruce abundance often declines. Most xeric stands become dominated by northern white-cedar and black spruce, while mesic sites become dominated by balsam fir and northern white-cedar [36].
Although quantitative studies of forest cover and succession in the Acadian Forest Region are rare, early descriptions by explorers, surveyors, and settlers suggest that white spruce is more abundant today than it was historically. This region was characterized by shade tolerant hardwoods, spruce-fir forest, and mixed types. Human activities such as land clearing have resulted in a shift from late-successional species including sugar maple, red spruce, eastern hemlock, yellow birch, northern white-cedar, and beech to earlier successional species including white spruce. Abandoned farmland was colonized by pioneering white spruce throughout the Maritime provinces (reviewed in [258]). According to Fernow (1912) (cited in [258]), white spruce only accounted for about 1% of the presettlement forest in Nova Scotia and did not naturally occur in pure stands like it does today. While white spruce often occurs on abandoned farmland in the Acadian Forest Region, it also occurs in old-growth and senescent balsam fir stands in nearby Atlantic provinces, including stands on the Gaspé Peninsula, Quebec [104], and on the Great Northern Peninsula, Newfoundland, where succession is characterized by small-scale gap dynamics [278].The scientific name of white spruce is Picea glauca (Moench) Voss (Pinaceae) [110,135,197,211,268,369,438].
Hybrids: White spruce hybridizes with others of its genus [135]. Natural hybrids where distributions of white spruce and other spruces overlap are:
White spruce and Engelmann spruce occur together over large areas in British Columbia, Montana, and Wyoming. White spruce predominates at lower elevations (<5,000 feet (1520 m)), and Engelmann spruce predominates at higher elevations (>6,000 feet (1830 m)). Western white spruce occurs where the 2 species overlap [305].
Lutz spruce occurs in northwestern British Columbia and in parts of Alaska where Sitka spruce and white spruce distributions overlap [305].
Hybrids between black and white spruce, sometimes called Rosendahl spruce, have been reported in Minnesota [252], British Columbia [346] and the forest-tundra treeline in central Canada [239,305].
See Appendix B for scientific names of plant taxa mentioned in this review and for links to available FEIS reviews.
White spruce is useful for long-term revegetation of coal mine overburden. In Alberta, it is considered one of the best conifers for this purpose. Information about planted white spruce survival on reclaimed sites is available [446]. Western white spruce established on abandoned coal mine sites in the Rocky Mountain foothills, west-central Alberta [361]. White spruce has also established on coal mine overburden in south-central Alaska. This site was part of a reclamation project where the overburden (clay content 42-44%) was redeposited on the mined area and graded, scarified, seeded with graminoids and forbs, and fertilized; white spruce was not included in the seed mix [125]. White spruce has also colonized abandoned borrow pits (5-37 years after disturbance) in tundra regions of northwestern Canada, although white spruce cover was very low (0.01-1.04%) [219].
White spruce often colonizes abandoned agricultural fields in Maritime Canada and New England [95,305].
Picea glauca, the white spruce,[3] is a species of spruce native to the northern temperate and boreal forests in North America. Picea glauca is native from central Alaska all through the east, across western and southern/central Canada to the Avalon Peninsula in Newfoundland, and south to Montana, North Dakota, Minnesota, Wisconsin, Michigan, Upstate New York and Vermont, along with the mountainous and immediate coastal portions of New Hampshire and Maine, where temperatures are just barely cool and moist enough to support it. There is also an isolated population in the Black Hills of South Dakota and Wyoming.[4][5][1][6] It is also known as Canadian spruce, skunk spruce, cat spruce, Black Hills spruce, western white spruce, Alberta white spruce, and Porsild spruce.[7]
The white spruce is a large evergreen conifer which normally grows to 15 to 30 metres (50 to 100 ft) tall, but can grow up to 40 m (130 ft) tall with a trunk diameter of up to 1 m (3 ft 3 in). The bark is thin and scaly, flaking off in small circular plates 5 to 10 centimetres (2 to 4 in) across. The crown is narrow – conical in young trees, becoming cylindrical in older trees. The shoots are pale buff-brown, glabrous in the east of the range, but often pubescent in the west, and with prominent pulvini. The leaves are needle-like, 12 to 20 millimetres long, rhombic in cross-section, glaucous blue-green above (hence glauca) with several thin lines of stomata, and blue-white below with two broad bands of stomata.[4]
The cones are pendulous, slender, cylindrical, 3 to 7 cm long and 1.5 cm wide when closed, opening to 2.5 cm broad. They have thin, flexible scales 15 mm long with a smoothly rounded margin. They are green or reddish, maturing to pale brown 4 to 8 months after pollination. The seeds are black, 2 to 3 mm long, with a slender, 5 to 8 mm long pale brown wing.[4]
Young tree
_DDumais.jpg)
Mature tree
Mature tree that has lost its lower branches
The bark is thin and scaly, flaking off in small circular plates
Twig with striped, blue-green, four-sided needles
Mature female cone
Female cone
Young female cone
Male cone and pollen
Seeds are small, 2.5 to 5 mm long, oblong, and acute at the base. Determinations of the average number of sound seeds per white spruce cone have ranged from 32 to 130.[8][9]
Common causes of empty seed are lack of pollination, abortion of the ovule, and insect damage.
The average weight per individual seed varies from 1.1 mg to 3.2 mg.[10]
Each seed is clasped by a thin wing 2 to 4 times as long as the seed. Seed and wing are appressed to the cone scale. Embryo and megagametophyte are soft and translucent at first; later the endosperm becomes firm and milky white, while the embryo becomes cream-coloured or light yellow. At maturity, the testa darkens rapidly from light brown to dark brown or black.[11] Mature seeds “snaps in two” when cut by a sharp knife on a firm surface.[11]
White spruce cones reach their maximum size after 800 GDD. Cone moisture content decreases gradually after about 1000 GDD.[12]
Cone colour also can be used to help determine the degree of maturation, but cones may be red, pink or green.[13] Collection and storage dates and conditions influence germination requirements and early seedling growth.[14][15][16]
A bushel (35 L) of cones, which may contain 6500 to 8000 cones, yields 6 to 20 ounces (170 to 570 g) of clean seed.[17]
Seed dispersal begins after cone scales reflex with cone maturation in the late summer or early fall of the year of formation. Cones open at moisture contents of 45% to 70% and specific gravities of 0.6 to 0.8.[12][14][16] Weather affects both the initiation and pattern of seed dispersal, but cone opening and the pattern of seed dispersal can vary among trees in the same stand.[7] Even after dispersal has begun, cold, damp weather will cause cone scales to close; they will reopen during dry weather. Most seed falls early rather than late, but dispersal may continue through fall and winter and even into the next growing season.[18][19] Seed dispersal occurs mainly in late summer or early fall.[8]
White spruce seed is initially dispersed through the air by wind. Both the initiation and pattern of seed dispersal depend on the weather,[7] but these can vary among trees in the same stand.[18] Small amounts of white spruce seed are normally dispersed beyond 100 m from the seed source, but exceptionally seeds have been found more than 300–400 m from the nearest seed source.[18]
The root system of white spruce is highly variable and adaptable, responding to a variety of edaphic factors, especially soil moisture, soil fertility, and mechanical impedance.[20][21] On soils that limit rooting depth, the root system is plate-like, but it is a common misconception to assume that white spruce is genetically constrained to develop plate-like root systems irrespective of soil conditions.[22] In the nursery, or naturally in the forest, white spruce usually develops several long 'running' roots just below the ground surface.[23]
The structure of the tracheids in the long lateral roots of white spruce varies with soil nitrogen availability.[24]
White spruce can live for several hundred years, with an estimated average lifespan of 250 to 300 years.[25]
Slow-growing trees in rigorous climates are also capable of great longevity. White spruce 6 to 10 m (20 to 33 ft) high on the shore of Urquhart Lake, Northwest Territories, were found to be more than 300 years old.[26]
The bark of mature white spruce is scaly or flaky, grey-brown or ash-brown, but silvery when freshly exposed.[27][28] Resin blisters are normally lacking, but the Porsild spruce Picea glauca var. porsildii Raup has been credited with having smooth resin-blistered bark.[29]
White spruce bark is mostly less than 8 mm and not more than 9.5 mm thick.[30][31]
Isorhapontin can be found in spruce species such as the white spruce.[32]
White spruce has a transcontinental range in North America. In Canada, its contiguous distribution encompasses virtually the whole of the Boreal, Subalpine, Montane, Columbia, Great Lakes–St. Lawrence, and Acadian Forest Regions, extending into every province and territory.[33][34] On the west coast of Hudson Bay, it extends to Seal River, about 59°N, "from which the northward limit runs apparently almost directly north-west to near the mouth of the Mackenzie River, or about latitude 68°".[35] Collins and Sumner[36] reported finding white spruce within 13 km of the Arctic coast in the Firth Valley, Yukon, at about 69°30′ N, 139°30′ W. It reaches within 100 km of the Pacific Ocean in the Skeena Valley, overlapping with the range of Sitka spruce (Picea sitchensis), and almost reaching the Arctic Ocean at latitude 69° N in the District of Mackenzie, with white spruce up to 15 m high occurring on some of the islands in the Delta near Inuvik.[37] The wide variety of ecological conditions in which 4 Quebec conifers, including white spruce, are able to establish themselves, was noted by Lafond,[38] but white spruce was more exacting than black spruce. In the United States, the range of white spruce extends into Maine, Vermont, New Hampshire, New York, Michigan, Wisconsin, Minnesota, and Alaska,[28][39] where it reaches the Bering Strait in 66°44′ N" at Norton Bay and the Gulf of Alaska at Cook Inlet.[7]
Southern outliers have been reported in southern Saskatchewan and the Cypress Hills of southwestern Saskatchewan[7][40] and southeastern Alberta,[41] northwestern Montana,[28] south-central Montana, in the Black Hills on the Wyoming–South Dakota boundary, on the Manitoba–North Dakota boundary, and at Shushan, New York.[42][43][44]
White spruce is the northernmost tree species in North America, reaching just north of 69°N latitude in the Mackenzie River delta.[45] It grows between sea level and an elevation of 1,520 m (4,990 ft). Its northern distribution roughly correlates to the location of the tree line, which includes an isothermic value of 10 °C (50 °F) for mean temperature in July, as well as the position of the Arctic front; cumulative summer degree days, mean net radiation, and the amount of light intensities also figure. White spruce is generally found in regions where the growing season exceeds 60 days annually.[7]
The southern edge of the zone in which white spruce forms 60% or more of the total stand corresponds more or less to the July isotherm of 18 °C (64 °F) around the Great Lakes; in the Prairie Provinces its limit is north of this isotherm. During the summer solstice, day length values range from 17 hours at its southern limits to 24 hours above the Arctic Circle.[7]
One of the hardiest conifers, white spruce in parts of its range withstands mean daily January temperature of −6.7 °C (19.9 °F) and extreme minimum temperatures as low as −56.5 °C (−69.7 °F); minimum temperatures of −50 °C (−58 °F) are general throughout much of the range except the southernmost and southeasternmost parts.[46] By itself, or with black spruce and tamarack (Larix laricina), white spruce forms the northern boundary of tree-form growth.[47] White spruce up to 15 m in height occur at 69°N on islands in the Mackenzie Delta near Inuvik in the Northwest Territories. Hustich (1966)[48] depicted Picea spp. as forming the northernmost limit of tree growth in North America.
The arctic or northern timberline in North America forms a broad transition zone from Labrador to northern Alaska. In Labrador, white spruce is not abundant and constitutes less than 5% of the forest, with a range that coincides very closely with that of black spruce but extending slightly further north.[49]
The range of white spruce extends westwards from Newfoundland and Labrador, and along the northern limit of trees to Hudson Bay, Northwest Territories, Yukon, and into northwestern Alaska.[46] Across western Canada and Alaska, white spruce occurs further north than black spruce, and, while poplar (Populus), willow, and birch may occur along streams well into the tundra beyond the limits of spruce, the hardwoods are usually no more than scrub.[50] Spruce characteristically occurs in fingers of tree-form forest, extending far down the northern rivers and as scattered clumps of dwarfed “bush” spruce on intervening lands.[42][51] In Manitoba, Scoggan[40] noted that the northernmost collection of white spruce was at latitude 59°48’N, but Bryson et al.[52] found white spruce in the northern edge of continuous forest in central Canada at Ennadai Lake, about 60°45′ N, 101°’W, just north of the northwest corner of Manitoba. Bryson et al.[52] noted that the forest retained “the same general characteristics as when it was first described [by Tyrrell[53]] in 1896”. Collins and Sumner[36] reported finding white spruce within 13 km of the Arctic coast in the Firth valley, Yukon, at about 69°30′ N, 139°30′ W, and Sargent[39] noted that white spruce in Alaska “reached Behring Strait in 66°44′ N”.
_(14760113996).jpg)
Climate, especially temperature, is obviously a factor in determining distributions of northern flora. Halliday and Brown[51] suggested that white spruce's northern limit corresponds “very closely” with the July mean monthly isotherm of 10 °C in Ungava, but that the northern limit west of Hudson Bay was south of that isotherm. Other climatic factors that have been suggested as affecting the northern limit of white spruce include: cumulative summer degree days, position of the Arctic front in July, mean net radiation especially during the growing season, and low light intensities.[7] Topography, soil conditions, and glaciation may also be important in controlling northern limits of spruce.[54]
The southern limit of distribution of white spruce is more complex. From east of the main range of coastal mountains in British Columbia, the southern continuous limit of white spruce is the forest/prairie interface through Alberta, Saskatchewan, Manitoba, the northern parts of Minnesota and Wisconsin, central Michigan, northeastern New York, and Maine.[46] Sargent[39] and Harlow and Harrar[28] also included Vermont and New Hampshire; and, while Dame and Brooks[55] excluded New York and states further west, they included Massachusetts as far south as Amherst and Northampton, “probably the southern limit of the species” in that area. Nisbet[56] gave the range of white spruce as extending to “Carolina”, but he did not recognize red spruce as a species and presumably included it with white spruce.
Towards the southern parts of its range, white spruce encounters increasingly effective ecological competition from hardwoods, some of which may reinforce their growth-rate or sprouting competitiveness with allelopathic depredation of coniferous regeneration.[57] Further southward extension of the distribution is inhibited by white spruce's cold requirement.
As an exotic, white spruce is widespread but uncommon. It was introduced into England[58] and parts of continental Europe[56][59] in or soon after the year 1700, into Denmark about 1790,[60] and into Tasmania and Ceylon shortly before 1932.[61]
Nisbet[56] noted that firmly-rooted white spruce served very well to stabilize windswept edges of woods in Germany. In a narrow belt of mixed Norway and white spruces over an extremely exposed hilltop crest at high elevation in northern England, the Norway spruce were “completely dwarfed” whereas the white spruce had reached heights of between 3 and 4.3 m.[62] The age of the belt was not recorded, but adjoining 66-year-old stands may have been of the same vintage.
White spruce has also been used as a minor plantation species in England and Scotland.[63][64][65] In Scotland, at Corrour, Inverness-shire, Sir John Stirling Maxwell in 1907 began using white spruce in his pioneering plantations at high elevations on deep peat. However, plantations in Britain have generally been unsatisfactory,[66] mainly because of damage by spring frosts after mild weather had induced flushing earlier in the season. However, the species is held in high regard in the Belgian peat region, where it grows better than do the other spruces.[67]
White spruce is a climax canopy tree in the boreal forests of Canada and Alaska. It generally occurs on well-drained soils in alluvial and riparian zones, although it also occurs in soils of glacial and lacustrine origin.[7] The understory is dominated by feather mosses (Hylocomium splendens, Pleurozium schreberi, Ptilium crista-castrensis) and fork mosses, and occasionally peat moss.[68] In the far north, the total depth of the moss and underlying humus is normally between 25 and 46 cm (10 and 18 in), although it tends to be shallower when hardwoods are present in the stand.[7]
White spruce grows in soils with pH values of 4.7–7.0, although they have been found in soils as acidic as 4.0 in subalpine fir forests in the Northwest Territories. A presence of calcium in the soil is common to white spruce found in northern New York. White spruce most commonly grows in the soil orders of Alfisols and Inceptisols. Soil properties such as fertility, temperature, and structural stability are partial determinants of the ability of white spruce to grow in the extreme northern latitudes.[7] In the northern limits of its range, white spruce is the climax species along with black spruce; birch and aspen are the early succession species.[68] Wildfires typically occur every 60 to 200 years, although they have been known to occur as infrequently as every 300 years.[68]
White spruce will grow in USDA Growing Zones 3–7, but is not adapted to heat and humidity and will perform poorly in a hot climate. The tree attains its greatest longevity and growth potential in Zones 3–4.
White spruce occurs on a wide variety of soils, including soils of glacial, lacustrine, marine, and alluvial origins; overlying basic dolomites, limestones and acidic Precambrian and Devonian granites and gneisses; and Silurian sedimentary schists, shales, slates, and conglomerates.[69] The wide range of textures accommodated includes clays, even those that are massive when wet and columnar when dry, sand flats, and coarse soils.[33][70][71][72][73] Its occurrence on some organic soils is not characteristic, except perhaps on shallow mesic organic soils in Saskatchewan and in association with black spruce on organic soils in central Yukon.[7]
Podzolized, brunisolic, luvisolic, gleysolic, and regosolic (immature) soils are typical of those supporting white spruce throughout the range of the species.[72] Soils supporting white spruce are most commonly Alfisols or Inceptisols.[7] In the podzol region of Wisconsin, white spruce occurs on loam podzols, podzolized gley loams, strongly podzolized clays, gley-podzol clays, stream-bottom soils, and wood peat.[70] Moist sandy loams also support good growth.[28] On sandy podzols,[70] it is usually a minor species.[7] Good development occurs on moist alluvium on the banks of streams and borders of swamps.[72][74][75][76][77][33][78][79] White spruce makes good growth on well-drained lacustrine soils in Alberta Mixedwoods,[80] on moderately-well-drained clay loams in Saskatchewan,,[81] and on melanized loams and clays (with sparse litter and a dark-coloured organically-enriched mineral horizon) in the Algoma district of Ontario.[71]
White spruce becomes less accommodating of soil with increasing severity of climate. The distribution of white spruce in Labrador seems to depend almost entirely on the character of the soil,[78] and between the southwestern shores of Hudson Bay and the northeastern regions of Saskatchewan, white spruce is confined to very local physiographic features, characterized by well-drained or fertile soils.[82]
On dry, deep, outwash deposits in northern Ontario, both white spruce and aspen grow slowly.[83] But, broadly, white spruce is able to tolerate considerable droughtiness of sites that are fertile, and no fertile site is too moist unless soil moisture is stagnant.[84] Soil fertility holds the key not just to white spruce growth but to the distribution of the species. At least moderate fertility is needed for good growth, but white spruce occurs on many sites where nutrient deficiencies depress its growth more than that of black spruce, red spruce, Norway spruce, and the pines generally.[85] Minimum soil-fertility standards recommended for white spruce sufficient to produce 126 to 157 m3/ha of wood at 40 years are much higher than for pine species commonly planted in the Lake States (Wilde 1966):[86] 3.5% organic matter, 12.0 meq/100 g exchange capacity, 0.12% total N, 44.8 kg/ha available P, 145.7 kg/ha available K, 3.00 meq/100 g exchangeable Ca, and 0.70 meq/100 g exchangeable Mg.
Forest floors under stands dominated by white spruce respond in ways that vary with site conditions, including the disturbance history of the site.[7] Composition, biomass, and mineral soil physical and chemical properties are affected. In Alaska, the accumulation of organic layers (to greater thicknesses in mature stands of spruce than those in hardwood stands on similar sites) leads to decreased soil temperatures, in some cases leading to the development of permafrost.[87][88][89] Acidity of the mineral soil sampled at an average depth of 17 cm in 13 white spruce stands on abandoned farmland in Ontario increased by 1.2 pH units over a period of 46 years.[90]
A considerable range of soil pH is tolerated by white spruce.[72] Thrifty stands of white spruce in Manitoba have developed on soils of pH 7.6 at only 10 cm below the surface, and pH 8.4 at 43 cm below the surface;[91][92] rooting depth in those soils was at least 81 cm. An abundant calcium supply is common to most white spruce locations in New York state.[7] Chlorosis was observed in young white spruce in heavily limed nursery soils at about pH 8.3.[72] Wilde[86] gave 4.7 to 6.5 as the approximate optimum range of pH for white spruce in Wisconsin, but optimum growth seems possible at pH levels up to 7.0 and perhaps higher.[84] Alluvium on the floodplains of northern rivers shows pH levels from 5.0 to 8.2.[93] High-lime ecotypes may exist,[94] and in Canada Forest Section B8 the presence of balsam poplar and white spruce on some of the moulded moraines and clays seems to be correlated with the considerable lime content of these materials,[33][95] while calcareous soils are favourable sites for northern outliers of white spruce.[50]
Mature stands of white spruce in boreal regions often have well-developed moss layers dominated by feather mosses, e.g., Hylocomium splendens, Pleurozium schreberi, Ptlium crista-castrensis, and Dicranum, rather than Sphagnum.[96][97] The thickness of the moss–organic layer commonly exceeds 25 cm in the far north and may approach twice that figure. The mosses compete for nutrients and have a major influence on soil temperatures in the rooting zone. Permafrost development in parts of Alaska, Yukon, and the Northwest Territories is facilitated by the insulative organic layer (Viereck 1970a, b, Gill 1975, Van Cleve and Yarie 1986).[87][88][98][99]
White spruce is extremely hardy to low temperatures, provided the plant is in a state of winter dormancy. Throughout the greater part of its range, white spruce routinely survives and is undamaged by winter temperatures of −50 °C (−58 °F), and even lower temperatures occur in parts of the range.[7][46] Boreal Picea are among the few extremely hardy conifers in which the bud primordia are able to survive temperatures down to −70 °C, −94 °F.[100]
Especially important in determining the response of white spruce to low temperatures is the physiological state of the various tissues, notably the degree of "hardening" or dormancy. A natural progression of hardening and dehardening occurs in concert with the seasons.[101] While different tissues vary in ability to tolerate exposure to stressful temperatures, white spruce, as with woody plants in general, has necessarily developed sufficient winter hardiness in its various tissues to enable them to survive the minimum temperatures experienced in the distribution range.
White spruce is subject to severe damage from spring frosts. Newly flushed shoots of white spruce are very sensitive to spring frost.[102][103][104] This sensitivity is a major constraint affecting young trees planted without overstorey nurses in boreal climates.[105]
Forest succession in its traditional sense implies two important features that resist direct examination.[106] First, classical definitions generally connote directional changes in species composition and community structure through time, yet the time frame needed for documentation of change far exceeds an average lifespan.[106] The second feature that defies quantitative description is the end point or climax.
Floodplain deposits in the Northwest Territory, Canada, are important in relation to the development of productive forest types with a component of white spruce.[75] The most recently exposed surfaces are occupied by sandbar vegetation or riparian shrub willows and Alnus incana. With increasing elevation, the shrubs give way successively to balsam poplar and white spruce forest. In contrast, older floodplains, with predominantly brown wooded soils, typically carry white spruce–trembling aspen mixedwood forest.
Interrelationships among nutrient cycling, regeneration, and subsequent forest development on floodplains in interior Alaska were addressed by Van Cleve et al.,[107] who pointed out that the various stages in primary succession reflect physical, chemical, and biological controls of ecosystem structure and function. Thus, each successional stage has a species combination in harmony with site quality. Short-circuiting succession by planting a late successional species such as white spruce on an early successional surface may result in markedly reduced growth rates because of nitrogen insufficiency. Without application of substantial amounts of fertilizer, use would have to be made of early successional alder and its site-ameliorating additions of nitrogen.
Neiland and Viereck noted that “the slow establishment and growth of spruce under birch stands [in Alaska] may be partially due to effects of shading and general competition for water and nutrients, but may also be more directly related to the birch itself. Heikinheimo[108][109] found that birch ash inhibited white spruce seedlings, and Gregory[110] found that birch litter has a smothering effect on spruce seedlings.".[111]
On dry upland sites, especially south-facing slopes, the mature vegetation is white spruce, white birch, trembling aspen, or a combination of these species. Succession follows in one of two general patterns. In most cases, aspen and birch develop as a successional stage after fire before reaching the spruce stage. But, occasionally, with optimal site conditions and a source of seed, white spruce will invade with the hardwoods or within a few years thereafter, thereby producing even-aged white spruce stands without an intervening hardwood stage.
The White Spruce Cover Type may include other species in small numbers. In Alaska, associates include paper birch, trembling aspen, balsam poplar, and black spruce; in western Canada, additional associates are subalpine fir, balsam fir, Douglas-fir, jack pine, and lodgepole pine.[112] Seral species giving way to white spruce include paper birch, aspen, balsam poplar, jack pine, and lodgepole pine. On certain river bottom sites, however, black spruce may replace white spruce.[112] Earlier successional stages leading to the white spruce climax are the white spruce–paper birch, white spruce–aspen, balsam poplar, jack pine, and lodgepole pine types. The type shows little variation. The forest is generally closed and the trees well formed, other than those close to the timberline. Lesser vegetation in mature stands is dominated by mosses. Vascular plants are typically few, but shrubs and herbs that occur “with a degree of regularity” include: alder, willows, mountain cranberry, red-fruit bearberry, black crowberry, prickly rose, currant, buffaloberry, blueberry species, bunchberry, twinflower, tall lungwort, northern comandra, horsetail, bluejoint grass, sedge species, as well as ground-dwelling mosses and lichens. Several white spruce communities have been identified in interior Alaska: white spruce/feathermoss; white spruce/dwarf birch/feathermoss; white spruce/dwarf birch/sphagnum; white spruce/avens/moss; and white spruce/alder/bluejoint.[113][112]
Of the Eastern Forest Cover Types recognized by the Society of American Foresters,[114] only one, White Spruce, names that species in its title. The eastern White Spruce Cover Type, as defined, encompasses white spruce both in pure stands, and in mixed stands "in which white spruce is the major [undefined] component."[115]
In most of its range, white spruce occurs more typically in association with trees of other species than in pure stands.
White spruce is an associated species in the following Eastern Forest cover types, by the Society of American Foresters; in the Boreal Forest Region: (1) jack pine, (5) balsam fir, (12) black spruce, (16) aspen, (18) paper birch, and (38) tamarack; in the Northern Forest Region: (15) red pine, (21) eastern white pine, (24) hemlock-yellow birch, (25) sugar maple-beech-yellow birch, (27) sugar maple, (30) red spruce-yellow birch, (32) red spruce, (33) red spruce-balsam fir, (37) northern white-cedar, and (39) black ash-American elm-red maple.[7][114]
Outbreaks of spruce beetles have destroyed over 2,300,000 acres (9,300 km2) of forests in Alaska.[116]
Although sometimes described, e.g., by Switzer (1960),[117] as relatively resistant to attack by insects and disease, white spruce is far from immune to depredation. Important insect pests of white spruce include the spruce budworm (Choristoneura fumiferana), the yellow-headed spruce sawfly (Pikonema alaskensis), the European spruce sawfly (Gilpinia hercyniae), the spruce bud moth (Zeiraphera canadensis),[118] and spruce beetle (Dendroctonus rufipennis).[119][118][120] As well, other budworms, sawflies, and bark beetles, gall formers, bud midges, leaf miners, aphids, leaf eaters, leaf rollers, loopers, mites, scales, weevils, borers, pitch moths, and spittlebugs cause varying degrees of damage to white spruce.[120]
A number of sawflies feed on spruce trees. Among them European spruce sawfly, yellow-headed spruce sawfly, green-headed spruce sawfly and the spruce webspinning sawfly.[118]
More than a dozen kinds of looper feed on the spruces, fir, and hemlock in eastern Canada. The full-grown larvae of the larvae vary in length from 15 mm to 35 mm. Some feed briefly in the fall and complete their feeding in the spring; others feed mainly in the summer; still others feed mainly in the late summer and fall.
The fall and spring feeding group includes the dash-lined looper (Protoboarmia porcelaria indicataria), the diamond-backed looper (Hypagyrtis piniata), the fringed looper (Campaea perlata), and the false loopers (Syngrapha species). The summer feeding group includes the false hemlock looper (Nepytia canosaria Walker), occasionally occurring in large numbers and usually in conjunction with the hemlock looper (Lambdina fiscellaria), the Eupithecia species, the yellowlined conifer looper (Cladara limitaria), and the saddleback looper (Ectropis crepuscularia).
The late summer and fall group includes the common spruce-fir looper (Semiothisa signaria dispuncta) and the similar hemlock angle (moth) Macaria fissinotata on hemlock, the small spruce loopers Eupithecia species, the gray spruce looper Caripeta divisata, occasionally abundant, the black-dashed hydriomena moth (Hydriomena divisaria), and the whitelined looper (Eufidonia notataria).
Wildlife such as deer, rabbits, and grouse browse the foliage during the winter.[121]
The wood of white spruce is of a lower quality than that of Engelmann spruce, but is stronger. It was used to make shelters and as firewood by Native Americans and European settlers in Alaska, where lodgepole pine does not grow.[122] The wood is of major economic importance in Canada, being harvested for paper and construction. It is also used as a Christmas tree.
The wood is also exported to Japan where, known as "shin-kaya", it is used to make go boards as a substitute for the rare kaya wood.
Black Hills Spruce (Picea glauca var. densata) is used for bonsai.
White spruce is the provincial tree of Manitoba[123] and the state tree of South Dakota.
The new growth or tips of white spruce is used in beer making,[124] gin production,[125] flavouring pop,[126] candy making or in pickles and preserves. [127]
Several geographical varieties have been described, but are not accepted as distinct by all authors. These comprise, from east to west:[4]
The two western varieties are distinguished by pubescent shoots, and may be related to extensive hybridisation and intergradation with the closely related Engelmann spruce found further south in the Rocky Mountains. White spruce also hybridises readily with the closely related Sitka spruce where they meet in southern Alaska and northwestern British Columbia; this hybrid is known as Picea × lutzii.[4]
Numerous cultivars of various sizes, colours and shapes have been selected for use in parks and gardens. The following have gained the Royal Horticultural Society's Award of Garden Merit.[128]
'Conica' is a dwarf conifer with very slender leaves, like those normally found only on one-year-old seedlings, and very slow growth, typically only 2–10 cm (0.79–3.94 in) per year. Older specimens commonly 'revert', developing normal adult foliage and starting to grow much faster; this 'reverted' growth must be pruned if the plant is to be kept dwarf.
P. glauca has three different genomes; a nuclear genome,[132] a mitochondrial genome,[133] and a plastid (i.e. chloroplast) genome.[134] The large (20 Gbp) nuclear genome of P. glauca (genotype WS77111) was published in 2015,[135] and the organellar (plastid and mitochondrial) genomes (genotype PG29) were published in SD Jackman et al. 2015.[136] The plastid genome of P. glauca (genotype WS77111) has also been published.[137]
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{{cite journal}}: Cite journal requires |journal= (help) {{cite journal}}: Cite journal requires |journal= (help) {{cite journal}}: Cite journal requires |journal= (help) Picea glauca, the white spruce, is a species of spruce native to the northern temperate and boreal forests in North America. Picea glauca is native from central Alaska all through the east, across western and southern/central Canada to the Avalon Peninsula in Newfoundland, and south to Montana, North Dakota, Minnesota, Wisconsin, Michigan, Upstate New York and Vermont, along with the mountainous and immediate coastal portions of New Hampshire and Maine, where temperatures are just barely cool and moist enough to support it. There is also an isolated population in the Black Hills of South Dakota and Wyoming. It is also known as Canadian spruce, skunk spruce, cat spruce, Black Hills spruce, western white spruce, Alberta white spruce, and Porsild spruce.
