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Overview

Distribution

More info for the term: bog

Bog birch is native to North America. It is widely distributed from interior Alaska to Greenland and south through Canada to New York, Michigan, and Minnesota in the East and Colorado, New Mexico, and California in the West [51,60,66,75,76,159,168]. Flora of North America provides a distributional map of bog birch.
  • 60. Gleason, Henry A.; Cronquist, Arthur. 1991. Manual of vascular plants of northeastern United States and adjacent Canada. 2nd ed. New York: New York Botanical Garden. 910 p. [20329]
  • 168. Welsh, Stanley L.; Atwood, N. Duane; Goodrich, Sherel; Higgins, Larry C., eds. 1987. A Utah flora. The Great Basin Naturalist Memoir No. 9. Provo, UT: Brigham Young University. 894 p. [2944]
  • 51. Dugle, Janet R. 1966. A taxonomic study of western Canadian species in the genus Betula. Canadian Journal of Botany. 44(7): 929-1007. [66573]
  • 66. Harrington, H. D. 1964. Manual of the plants of Colorado. 2nd ed. Chicago, IL: The Swallow Press, Inc. 666 p. [6851]
  • 75. Hickman, James C., ed. 1993. The Jepson manual: Higher plants of California. Berkeley, CA: University of California Press. 1400 p. [21992]
  • 76. Hitchcock, C. Leo; Cronquist, Arthur. 1973. Flora of the Pacific Northwest. Seattle, WA: University of Washington Press. 730 p. [1168]
  • 159. Viereck, Leslie A.; Little, Elbert L., Jr. 1972. Alaska trees and shrubs. Agric. Handb. 410. Washington, DC: U.S. Department of Agriculture, Forest Service. 265 p. [6884]

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States or Provinces

(key to state/province abbreviations)
UNITED STATES
AK CA CO ID ME MI MN MT NH NM
NY ND OR SD UT WA WI WY    

CANADA
AB BC MB NF NT NS NU ON PQ SK
YK    

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Regional Distribution in the Western United States

More info on this topic.

This species can be found in the following regions of the western United States (according to the Bureau of Land Management classification of Physiographic Regions of the western United States):

BLM PHYSIOGRAPHIC REGIONS [21]:

2 Cascade Mountains

4 Sierra Mountains

8 Northern Rocky Mountains

9 Middle Rocky Mountains

10 Wyoming Basin

11 Southern Rocky Mountains

16 Upper Missouri Basin and Broken Lands
  • 21. Bernard, Stephen R.; Brown, Kenneth F. 1977. Distribution of mammals, reptiles, and amphibians by BLM physiographic regions and A.W. Kuchler's associations for the eleven western states. Tech. Note 301. Denver, CO: U.S. Department of the Interior, Bureau of Land Management. 169 p. [434]

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Greenland; Alta., B.C., Man., N.B., Nfld., N.W.T., N.S., Ont., P.E.I., Que., Sask., Yukon; Alaska, Calif., Colo., Idaho, Maine, Mont., N.H., N.Y., Oreg., S.Dak., Utah, Wash., Wyo.
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© Missouri Botanical Garden, 4344 Shaw Boulevard, St. Louis, MO, 63110 USA

Source: Missouri Botanical Garden

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Physical Description

Morphology

Description

More info for the terms: bog, shrub

This description provides characteristics that may be relevant to fire ecology, and is not meant for identification. Keys for identification are available (e.g., [31,48,60,75,76,77,159,162,168]).

Bog birch is a deciduous, long-lived shrub. Plants are low and spreading to erect with 1 to several main stems. Bog birch ranges from 8 inches (20 cm) tall on upland sites and in arctic environments to 10 feet (3 m) in drainages and in more southern areas [31,44,60,76,77,77,102,137,159,168]. The bark is thin, smooth, and does not peel readily [51,75,159,168]. Leaves are thick and leathery and range from 0.2 to 1.2 inches (0.5-3 cm) long and 0.2 to 0.8 inch (0.5-2 cm) wide [75,76,77,159]. The inflorescences are catkins. Male catkins are 0.4 to 1 inch (10-25 mm) long, and female catkins are 0.3 to 0.8 inch (7-20 mm) long [31,159,168]. Fruits are narrow-winged, single-seeded samaras 1 to 1.5 mm long and wide [31,41,104]. Rhizomes are 0.8 to 2.4 inches (2-6 cm) thick and are found in the top 2.4 inches (6 cm) of soil [44]. Bog birch has an extensive root system [24,42,104]. Roots are ectomycorrhizal, an adaptation to arctic and alpine soils that are generally low in inorganic nitrogen and phosphorus [37,145].

  • 60. Gleason, Henry A.; Cronquist, Arthur. 1991. Manual of vascular plants of northeastern United States and adjacent Canada. 2nd ed. New York: New York Botanical Garden. 910 p. [20329]
  • 48. Dorn, Robert D. 1984. Vascular plants of Montana. Cheyenne, WY: Mountain West Publishing. 276 p. [819]
  • 168. Welsh, Stanley L.; Atwood, N. Duane; Goodrich, Sherel; Higgins, Larry C., eds. 1987. A Utah flora. The Great Basin Naturalist Memoir No. 9. Provo, UT: Brigham Young University. 894 p. [2944]
  • 24. Blanken, Peter D.; Rouse, Wayne R. 1994. The role of willow-birch forest in the surface energy balance at arctic treeline. Arctic and Alpine Research. 26(4): 403-411. [24350]
  • 31. Brayshaw, T. Christopher. 1976. Catkin bearing plants of British Columbia. Occas. Pap. No. 18. Victoria, BC: The British Columbia Provincial Museum. 176 p. [6170]
  • 37. Cripps, Cathy L.; Eddington, Leslie H. 2005. Distribution of mycorrhizal types among alpine vascular plant families on the Beartooth Plateau, Rocky Mountains, U.S.A., in reference to large-scale pattern in arctic-alpine habitats. Arctic, Antarctic, and Alpine Research. 37(2): 177-188. [62243]
  • 41. de Groot, W. J.; Thomas, P. A.; Wein, Ross W. 1997. Biological flora of the British Isles: No. 194. Betula nana L. and Betula glandulosa Michx. Journal of Ecology. 85(2): 241-264. [65929]
  • 42. de Groot, W. J.; Wein, Ross W. 1999. Betula glandulosa Michx. response to burning and postfire growth temperature and implications of climate change. International Journal of Wildland Fire. 9(1): 51-64. [37477]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 51. Dugle, Janet R. 1966. A taxonomic study of western Canadian species in the genus Betula. Canadian Journal of Botany. 44(7): 929-1007. [66573]
  • 75. Hickman, James C., ed. 1993. The Jepson manual: Higher plants of California. Berkeley, CA: University of California Press. 1400 p. [21992]
  • 76. Hitchcock, C. Leo; Cronquist, Arthur. 1973. Flora of the Pacific Northwest. Seattle, WA: University of Washington Press. 730 p. [1168]
  • 77. Hulten, Eric. 1968. Flora of Alaska and neighboring territories. Stanford, CA: Stanford University Press. 1008 p. [13403]
  • 102. McLoughlin, Philip D.; Cluff, H. Dean; Messier, Francois. 2002. Denning ecology of barren-ground grizzly bears in the central Arctic. Journal of Mammalogy. 83(1): 188-198. [65939]
  • 104. Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L. 2004. Shrubs of other families. In: Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L., comps. Restoring western ranges and wildlands. Gen. Tech. Rep. RMRS-GTR-136-vol-2. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 598-698. [52846]
  • 137. Soper, James H.; Heimburger, Margaret L. 1982. Shrubs of Ontario. Life Sciences Miscellaneous Publications. Toronto, ON: Royal Ontario Museum. 495 p. [12907]
  • 145. Treseder, Kathleen K.; Mack, Michelle C.; Cross, Alison. 2004. Relationships among fires, fungi, and soil dynamics in Alaskan boreal forests. Ecological Applications. 14(6): 1826-1838. [55375]
  • 159. Viereck, Leslie A.; Little, Elbert L., Jr. 1972. Alaska trees and shrubs. Agric. Handb. 410. Washington, DC: U.S. Department of Agriculture, Forest Service. 265 p. [6884]
  • 162. Weber, William A. 1987. Colorado flora: western slope. Boulder, CO: Colorado Associated University Press. 530 p. [7706]

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Description

Shrubs , spreading or ascending, to 3 m. Bark dark brown, smooth, close; lenticels pale, inconspicuous, unexpanded. Twigs without taste or odor of wintergreen, essentially glabrous to sparsely pubescent, usually conspicuously covered with large, warty, resinous glands. Leaf blade mostly obovate to nearly orbiculate with 2--6 pairs of lateral veins, 0.5--3 × 1--2.5 cm, base cuneate to rounded, margins dentate-crenate, teeth obtuse to rounded, apex obtuse to rounded; surfaces abaxially glabrous to moderately pubescent, especially along major veins and in vein axils, often covered with resinous glands. Infructescences erect, cylindric, 1--2.5 × 0.5--1.2 cm, shattering with fruits in fall; scales glabrous, lobes diverging distal to middle, central lobe elongate, lateral lobes ascending, somewhat shorter and broader than central lobe. Samaras with wings narrower than body, broadest near summit, extended slightly beyond body apically. 2 n = 28.
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Ecology

Habitat

Habitat characteristics

More info for the terms: bog, organic soils, shrub, tundra

Bog birch occupies a wide variety of sites, ranging from rocky subarctic and alpine tundra to deep, organic, boreal soils [44]. It is typically a wetland species occurring most commonly on moist, acidic, and nutrient-poor organic sites including fens, swamps, bogs, muskegs, wet meadows, lake and stream margins, and seepage areas [22,31,48,60,75,76,77,159,168]. Bog birch is also found on upland sites including eskers, till ridges, rock outcrops covered with shallow soil, cliffs, sandy hillsides, and rocky ridges [5,31,51,82,137]. It dominates open valley bottoms in the Canadian Rocky Mountains [43] and is the most common shrub at treeline in interior Alaska, forming a nearly continuous zone between the treeline and alpine tundra in many areas [156].

Elevation: Bog birch occurs between 1,300 and 11,000 feet (400-3,400 m) across its range [66,75,79,80,123,125,168]. Elevational ranges are summarized below.

Elevational ranges for bog birch by state or province

State Elevation (feet)
California 6,500-7,500 [75,125]
   Sierra Nevada 6,500-8,500 [79]
Colorado 5,700-11,400 [46,66,80]
Montana 4,900-8,000 [46]
Utah 6,000-11,000 [46,168]
Wyoming 6,400-10,500 [46]
Nova Scotia 1,300 [123]

Temperature: Bog birch is tolerant of cold temperatures. It is common in black spruce forests in the Yukon where the mean annual temperature is 27 °F (-3 °C) [6]. Frost tolerance in bog birch is high, and bog birch grows abundantly over large areas of permafrost [87]. Bog birch tolerates severe winter temperatures by withdrawing water from the protoplast and freezing it in the cell walls [25].

Moisture: Although it is primarily a wetland plant, bog birch does not appear to tolerate continuous flooding. In bogs near Fairbanks, Alaska, bog birch abundance decreases as soil moisture increases. Bog birch is also more "vigorous" in communities that support taller tussocks [32]. In the Cariboo Forest Region of British Columbia, bog birch is common in wetlands that have no standing water late in the season [139]. In Montana, however, the water table is often within the rooting zone of bog birch throughout the summer, and bog birch grows in soils that remain flooded until midsummer or are saturated year-round [64]. In a willow (Salix spp.)-bog birch community near Churchill, Manitoba, the depth of the water table averaged 3 inches (6.5 cm) below the surface, and soil moisture in the organic layer was 63% [24]. Bog birch is an indicator of "substantial groundwater" in the North Thompson River valley, British Columbia [98].

Annual precipitation ranges from 4 to 9 inches (109-230 mm) on 2 northern Canadian study sites where bog birch is abundant [6,24]. While some authors describe bog birch as drought intolerant [141], in a review of the literature de Groot and others [41] state that bog birch appears tolerant of periodic drought.

Soils: Bog birch grows in a variety of soils, ranging from sandy and gravelly loam on river terraces to poorly drained, organic soils in bogs, muskegs, and other wetland habitats [43,64,114,121,141]. It is tolerant of moderate salinity [24] and pH ranging from 3.1 to 6.5 [105,141].

  • 60. Gleason, Henry A.; Cronquist, Arthur. 1991. Manual of vascular plants of northeastern United States and adjacent Canada. 2nd ed. New York: New York Botanical Garden. 910 p. [20329]
  • 48. Dorn, Robert D. 1984. Vascular plants of Montana. Cheyenne, WY: Mountain West Publishing. 276 p. [819]
  • 168. Welsh, Stanley L.; Atwood, N. Duane; Goodrich, Sherel; Higgins, Larry C., eds. 1987. A Utah flora. The Great Basin Naturalist Memoir No. 9. Provo, UT: Brigham Young University. 894 p. [2944]
  • 5. Argus, George W. 1966. Botanical investigations in northeastern Saskatchewan: the subarctic Patterson-Hasbala Lakes region. Canadian Field-Naturalist. 80(3): 119-143. [8406]
  • 6. Arii, Ken; Turkington, Roy. 2002. Do nutrient availability and competition limit plant growth of herbaceous species in the boreal forest understory? Arctic, Antarctic, and Alpine Research. 34(3): 251-261. [42576]
  • 22. Bird, Ralph D. 1927. A preliminary ecological survey of the district surrounding the entomological station at Treesbank, Manitoba. Ecology. 8(2): 207-220. [63548]
  • 24. Blanken, Peter D.; Rouse, Wayne R. 1994. The role of willow-birch forest in the surface energy balance at arctic treeline. Arctic and Alpine Research. 26(4): 403-411. [24350]
  • 25. Blanken, Peter D.; Rouse, Wayne R. 1996. Evidence of water conservation mechanisms in several subarctic wetland species. Journal of Applied Ecology. 33(4): 842-850. [65926]
  • 31. Brayshaw, T. Christopher. 1976. Catkin bearing plants of British Columbia. Occas. Pap. No. 18. Victoria, BC: The British Columbia Provincial Museum. 176 p. [6170]
  • 32. Calmes, Mary A. 1976. Vegetation pattern of bottomland bogs in the Fairbanks area, Alaska. Fairbanks, AK: University of Alaska. 104 p. Thesis. [14785]
  • 41. de Groot, W. J.; Thomas, P. A.; Wein, Ross W. 1997. Biological flora of the British Isles: No. 194. Betula nana L. and Betula glandulosa Michx. Journal of Ecology. 85(2): 241-264. [65929]
  • 43. de Groot, William J. 1998. Fire ecology of Betula glandulosa Michx. Edmonton, AB: University of Alberta. 203 p. Dissertation. [66522]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 46. Dittberner, Phillip L.; Olson, Michael R. 1983. The Plant Information Network (PIN) data base: Colorado, Montana, North Dakota, Utah, and Wyoming. FWS/OBS-83/86. Washington, DC: U.S. Department of the Interior, Fish and Wildlife Service. 786 p. [806]
  • 51. Dugle, Janet R. 1966. A taxonomic study of western Canadian species in the genus Betula. Canadian Journal of Botany. 44(7): 929-1007. [66573]
  • 64. Hansen, Paul L.; Chadde, Steve W.; Pfister, Robert D. 1988. Riparian dominance types of Montana. Misc. Publ. No. 49. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station. 411 p. [5660]
  • 66. Harrington, H. D. 1964. Manual of the plants of Colorado. 2nd ed. Chicago, IL: The Swallow Press, Inc. 666 p. [6851]
  • 75. Hickman, James C., ed. 1993. The Jepson manual: Higher plants of California. Berkeley, CA: University of California Press. 1400 p. [21992]
  • 76. Hitchcock, C. Leo; Cronquist, Arthur. 1973. Flora of the Pacific Northwest. Seattle, WA: University of Washington Press. 730 p. [1168]
  • 77. Hulten, Eric. 1968. Flora of Alaska and neighboring territories. Stanford, CA: Stanford University Press. 1008 p. [13403]
  • 80. Kelly, George W. 1970. A guide to the woody plants of Colorado. Boulder, CO: Pruett Publishing Co. 180 p. [6379]
  • 82. Kelsall, John P.; Telfer, E. S.; Wright, Thomas D. 1977. The effects of fire on the ecology of the boreal forest, with particular reference to the Canadian north: a review and selected bibliography. Occasional Paper Number 32. Ottawa: Fisheries and Environment Canada, Canadian Wildlife Service. 58 p. [8403]
  • 87. Krajina, V. J.; Klinka, K.; Worrall, J. 1982. Distribution and ecological characteristics of trees and shrubs of British Columbia. Vancouver, BC: University of British Columbia, Department of Botany and Faculty of Forestry. 131 p. [6728]
  • 98. Majak, W.; Quinton, D. A.; Broersma, K. 1980. Cyanogenic glycoside levels in Saskatoon serviceberry. Journal of Range Management. 33(3): 197-199. [1510]
  • 105. Moore, T. R. 1980. The nutrient status of subarctic woodland soils. Arctic and Alpine Research. 12(2): 147-160. [51702]
  • 114. Peck, V. Ross; Peek, James M. 1991. Elk, Cervus elaphus, habitat use related to prescribed fire, Tuchodi River, British Columbia. Canadian Field-Naturalist. 105(3): 354-362. [18204]
  • 121. Robbins, W. W. 1918. Successions of vegetation in Boulder Park, Colorado. Botanical Gazette. 65(6): 493-525. [62933]
  • 123. Roland, A. E.; Smith, E. C. 1969. The flora of Nova Scotia. Halifax, NS: Nova Scotia Museum. 746 p. [13158]
  • 125. Sampson, Arthur W.; Jespersen, Beryl S. 1963. California range brushlands and browse plants. Berkeley, CA: University of California, Division of Agricultural Sciences; California Agricultural Experiment Station, Extension Service. 162 p. [3240]
  • 137. Soper, James H.; Heimburger, Margaret L. 1982. Shrubs of Ontario. Life Sciences Miscellaneous Publications. Toronto, ON: Royal Ontario Museum. 495 p. [12907]
  • 139. Steen, O. A.; Roberts, A. L. 1988. Guide to wetland ecosystems of the Very Dry Montane Interior Douglas-fir Subzone, Eastern Fraser Plateau Variant (IDFb2) in the Cariboo Forest Region, British Columbia. Williams Lake, BC: British Columbia Ministry of Forests and Lands. 101 p. [53384]
  • 141. Sutton, Richard F.; Johnson, Craig W. 1974. Landscape plants from Utah's mountains. EC-368. Logan, UT: Utah State University, Cooperative Extension Service. 135 p. [49]
  • 156. Viereck, Leslie A. 1979. Characteristics of treeline plant communities in Alaska. Holarctic Ecology. 2: 228-238. [8251]
  • 159. Viereck, Leslie A.; Little, Elbert L., Jr. 1972. Alaska trees and shrubs. Agric. Handb. 410. Washington, DC: U.S. Department of Agriculture, Forest Service. 265 p. [6884]
  • 79. Kartesz, John Thomas. 1988. A flora of Nevada. Reno, NV: University of Nevada. 1729 p. [In 2 volumes]. Dissertation. [42426]

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Key Plant Community Associations

More info for the terms: association, bog, lichen, marsh, shrub, shrubs, tundra, tussock

In the boreal forests of interior Alaska and Canada, bog birch is found in many
black spruce (Picea mariana) and white spruce (P. glauca)
communities and is especially common at the northern and altitudinal limit of
trees [3,6,117,152,154,159]. In these
northern environments, permafrost prevents the percolation of water, resulting
in the development of muskegs, bogs, and ponds that often impede the growth of
trees but support bog birch and other low-growing shrubs [55,159].
Bog birch is characteristic of many mixed shrub and tussock tundra
communities in Alaska and northern Canada [1,2,10,149]. In southwestern Canada and the contiguous United States,
bog birch often occurs on wetland sites including bogs, fens and carrs, within
lodgepole pine (Pinus contorta), Engelmann spruce (P. engelmannii),
or subalpine fir (Abies lasiocarpa) forest types and is often associated
with alders (Alnus spp.) and willows (Salix spp.) [15,22,84,86,110].
Bog birch is listed as a dominant species in the
following vegetation classifications:


United States


Alaska:



  • black spruce/bog birch/feather moss (Hylocomium spp.) vegetation type




  • black spruce/bog birch-marsh Labrador tea/sphagnum (Ledum palustre/Sphagnum spp.) vegetation type




  • black spruce-white spruce/bog birch vegetation type [152]




  • black spruce-white spruce/bog birch/feather moss community [157]




  • black spruce-white spruce/bog birch/reindeer lichen (Cladonia spp.) community [55]




  • black spruce-white spruce/thinleaf alder (Alnus incana ssp. tenuifolia)-bog birch/Schreber's big
    red stem moss (Pleurozium schreberi) vegetation type




  • bog birch vegetation type




  • bog birch-blueberry/rough fescue (Vaccinium spp./Festuca altaica)/feather moss-lichen vegetation type




  • bog birch-blueberry/Bigelow's sedge (Carex bigelowii) vegetation type




  • bog birch-bog blueberry-black crowberry (Vaccinium uliginosum-Empetrum nigrum)-
    marsh Labrador tea/lichen vegetation type




  • bog birch-bog blueberry/sedge (Carex spp.)/sphagnum vegetation type




  • bog birch-bog rosemary (Andromeda polifolia)/sphagnum vegetation type




  • bog birch-diamondleaf willow (Salix planifolia)-bog blueberry vegetation type


  • bog birch-Lapland rosebay (Rhododendron lapponicum)/sedge vegetation type



  • bog birch-mountain cranberry-cloudberry (Vaccinium vitis-idaea-Rubus chamaemorus)/sphagnum vegetation type




  • bog birch-marsh Labrador tea-blueberry vegetation type




  • bog birch-marsh Labrador tea/mountain cranberry/wideleaf polargrass (Arctagrostis latifolia) vegetation type




  • bog birch/Schreber's big red stem moss-mountain-fern moss (H. splendens) vegetation type




  • bog birch-sweet gale (Myrica gale)-bog rosemary/sphagnum vegetation type




  • bog birch-sweet gale/sedge/sphagnum vegetation type




  • bog birch-willow (Salix spp.)-marsh Labrador tea/Bigelow's sedge/feather moss-lichen vegetation type




  • bog birch-willow-thinleaf alder vegetation type




  • mountain alder (Alnus viridis subsp. crispa)-bog birch-marsh Labrador tea/sphagnum vegetation type




  • paper birch/bog birch/feather moss vegetation type




  • shrubby cinquefoil (Dasiphora fruticosa ssp. floribunda)-
    sweet gale-bog birch-black crowberry/sphagnum vegetation type




  • shrubby cinquefoil-sweet gale-bog birch-marsh Labrador tea/feather moss vegetation type




  • white spruce/bog birch/feather moss-reindeer lichen vegetation type




  • white spruce/bog birch/reindeer lichen vegetation type




  • white spruce/bog birch/sphagnum vegetation type




  • white spruce/bog birch/mountain-fern moss vegetation type [152]

Colorado:



  • diamondleaf willow-bog birch shrub association [13]




  • willow-bog birch type [100]




  • Wolf's willow (S. wolfii)-bog birch-shrubby cinquefoil shrub association [13]

Idaho:



  • bog birch/woollyfruit sedge (C. lasiocarpa) community type [33]

Montana:



  • bog birch dominance type [64]




  • bog birch/beaked sedge (C. rostrata) community type [28,116]




  • bog birch/tufted hairgrass (Deschampsia caespitosa) community type [116]




  • bog birch/woollyfruit sedge community type [33]

Canada

Alberta:



  • grayleaf willow (S. glauca)-bog birch-shrubby cinquefoil shrub type [63]

British Columbia:



  • bog birch-kinnikinnick (Arctostaphylos uva-ursi) shrub carr association [139]




  • white spruce/willow (Salix spp.)-bog birch zone [111]

Northwest Territories:



  • bog birch/star reindeer lichen (Cladonia alpestris)-moss community (Kershaw 1984, cited in [65])

Ontario:



  • birch (Betula spp.) vegetation association [83]

Yukon:





  • balsam poplar (Populus balsamifera)/bog birch/arctic lupine (Lupinus arcticus) vegetation type




  • black spruce/bog birch-marsh Labrador tea vegetation type [138]




  • bog birch/rough fescue community [49]




  • bog birch-bog blueberry-reindeer lichen vegetation type




  • cloudberry-bog birch-bog blueberry vegetation type




  • lichen-bog birch-marsh Labrador tea vegetation type [138]




  • white spruce/bog birch-crowberry community [49,69]




  • white spruce/bog birch/water sedge (Carex aquatilis) community [49]

  • 1. Abraham, Kenneth F.; Jefferies, Robert L.; Rockwell, Robert F. 2005. Goose-induced changes in vegetation and land cover between 1976 and 1997 in an arctic coastal marsh. Arctic, Antarctic, and Alpine Research. 37(3): 269-275. [60642]
  • 2. Ahlstrand, Gary M.; Racine, Charles H. 1993. Response of an Alaska, U.S.A., shrub-tussock community to selected all-terrain vehicle use. Arctic and Alpine Research. 25(2): 142-149. [21665]
  • 3. Alexander, M. E.; Stocks, B. J.; Lawson, B. D. 1991. Fire behavior in black spruce-lichen woodland: the Porter Lake project. NOR-X-310. Edmonton, AB: Forestry Canada, Northwest Region, Northern Forestry Centre. 44 p. [18823]
  • 6. Arii, Ken; Turkington, Roy. 2002. Do nutrient availability and competition limit plant growth of herbaceous species in the boreal forest understory? Arctic, Antarctic, and Alpine Research. 34(3): 251-261. [42576]
  • 10. Arseneault, Dominique; Payette, Serge. 1992. A postfire shift from lichen-spruce to lichen-tundra vegetation at tree line. Ecology. 73(3): 1067-1081. [18741]
  • 13. Baker, William L. 1984. A preliminary classification of the natural vegetation of Colorado. The Great Basin Naturalist. 44(4): 647-676. [380]
  • 15. Banci, Vivian; Harestad, Alton S. 1990. Home range and habitat use of wolverines Gulo gulo in Yukon, Canada. Holarctic Ecology. 13(3): 195-200. [13992]
  • 22. Bird, Ralph D. 1927. A preliminary ecological survey of the district surrounding the entomological station at Treesbank, Manitoba. Ecology. 8(2): 207-220. [63548]
  • 28. Boggs, Keith; Hansen, Paul; Pfister, Robert; Joy, John. 1990. Classification and management of riparian and wetland sites in northwestern Montana. Draft Version 1. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station, Montana Riparian Association. 217 p. [8447]
  • 33. Chadde, Steve W.; Shelly, J. Stephen; Bursik, Robert J.; Moseley, Robert K.; Evenden, Angela G.; Mantas, Maria; Rabe, Fred; Heidel, Bonnie. 1998. Peatlands on national forests of the Northern Rocky Mountains: ecology and conservation. Gen. Tech. Rep. RMRS-GTR-11. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 75 p. [29130]
  • 49. Douglas, George W. 1974. Montane zone vegetation of the Alsek River region, southwestern Yukon. Canadian Journal of Botany. 52: 2505-2532. [17283]
  • 55. Foote, M. Joan. 1983. Classification, description, and dynamics of plant communities after fire in the taiga of interior Alaska. Res. Pap. PNW-307. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 108 p. [18707]
  • 64. Hansen, Paul L.; Chadde, Steve W.; Pfister, Robert D. 1988. Riparian dominance types of Montana. Misc. Publ. No. 49. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station. 411 p. [5660]
  • 65. Harper, Karen A.; Kershaw, G. Peter. 1996. Natural revegetation on borrow pits and vehicle tracks in shrub tundra, 48 years following construction of the CANOL No. 1 Pipeline, N.W.T., Canada. Arctic and Alpine Research. 28(2): 163-171. [62701]
  • 69. Hawkes, Brad C. 1983. Fire history and management study of Kluane National Park. Winnipeg, MB: Parks Canada, Prairie Region. 85 p. [21211]
  • 83. Kershaw, K. A. 1974. Studies on lichen-dominated systems. X. The sedge meadows of the coastal raised beaches. Canadian Journal of Botany. 52: 1947-1972. [12966]
  • 84. Komarkova, Vera. 1986. Habitat types on selected parts of the Gunnison and Uncompahgre National Forests. Final report: Contract No. 28-K2-234. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 270 p. [1369]
  • 86. Kovalchik, Bernard L. 1987. Riparian zone associations: Deschutes, Ochoco, Fremont, and Winema National Forests. R6 ECOL TP-279-87. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Region. 171 p. [9632]
  • 100. Marr, John W. 1961. Ecosystems of the east slope of the Front Range in Colorado. University of Colorado Studies, Series in Biology. No. 8. Boulder, CO: University of Colorado Press. 134 p. [5724]
  • 110. Olson, R. A.; Gerhart, W. A. 1982. A physical and biological characterization of riparian habitat and its importance to wildlife in Wyoming. Cheyenne, WY: Wyoming Game and Fish Department. 188 p. [6755]
  • 111. Parminter, John. 1983. Fire history and fire ecology in the Prince Rupert Forest Region. In: Trowbridge, R. L.; Macadam, A., eds. Prescribed fire--forest soils: Symposium proceedings; 1982 March 2-3; Smithers, BC. Land Management Report Number 16. Victoria, BC: Province of British Columbia, Ministry of Forests: 1-35. [8849]
  • 116. Pierce, John; Johnson, Janet. 1986. Wetland community type classification for west-central Montana. Missoula, MT: U.S. Department of Agriculture, Forest Service, Northern Region, Ecosystem Management Program. 158 p. Review draft. On file with: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory, Missoula, MT; RWU 4403 files. [7436]
  • 117. Pojar, J.; Trowbridge, R.; Coates, D. 1984. Ecosystem classification and interpretation of the sub-boreal spruce zone, Prince Rupert Forest Region, British Columbia. Land Management Report No. 17. Victoria, BC: Province of British Columbia, Ministry of Forests. 319 p. [6929]
  • 138. Stanek, W.; Alexander, K.; Simmons, C. S. 1981. Reconnaissance of vegetation and soils along the Dempster Highway, Yukon Territory: I. Vegetation types. BC-X-217. Victoria, BC: Environment Canada, Canadian Forestry Service, Pacific Forest Research Centre. 32 p. [16526]
  • 139. Steen, O. A.; Roberts, A. L. 1988. Guide to wetland ecosystems of the Very Dry Montane Interior Douglas-fir Subzone, Eastern Fraser Plateau Variant (IDFb2) in the Cariboo Forest Region, British Columbia. Williams Lake, BC: British Columbia Ministry of Forests and Lands. 101 p. [53384]
  • 149. Van Cleve, Keith; Viereck, Leslie A. 1981. Forest succession in relation to nutrient cycling in the boreal forest of Alaska. In: Fire and succession in conifer forests of North America. New York: Springer-Verlag: 185-211. [50633]
  • 152. Viereck, L. A.; Dyrness, C. T.; Batten, A. R.; Wenzlick, K. J. 1992. The Alaska vegetation classification. Gen. Tech. Rep. PNW-GTR-286. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 278 p. [2431]
  • 154. Viereck, Leslie A. 1973. Wildfire in the taiga of Alaska. Quaternary Research. 3: 465-495. [7247]
  • 157. Viereck, Leslie A. 1980. Black spruce-white spruce. In: Eyre, F. H., ed. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters: 84-85. [50019]
  • 159. Viereck, Leslie A.; Little, Elbert L., Jr. 1972. Alaska trees and shrubs. Agric. Handb. 410. Washington, DC: U.S. Department of Agriculture, Forest Service. 265 p. [6884]
  • 63. Hamer, David. 1995. Buffaloberry (Shepherdia canadensis) fruit production in fire-successional bear feeding sites. Unpublished report [submitted to Parks Canada]. Banff, AB: Parks Canada, Banff National Park. 65 p. On file with: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory, Missoula, MT. [24885]

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Habitat: Rangeland Cover Types

More info on this topic.

This species is known to occur in association with the following Rangeland Cover Types (as classified by the Society for Range Management, SRM):

More info for the terms: cover, lichen, shrub, tundra, tussock

SRM (RANGELAND) COVER TYPES [131]:


216 Montane meadows

410 Alpine rangeland

901 Alder

904 Black spruce-lichen

911 Lichen tundra

912 Low scrub shrub birch-ericaceous

913 Low scrub swamp

916 Sedge-shrub tundra

917 Tall shrub swamp

918 Tussock tundra

919 Wet meadow tundra

920 White spruce-paper birch

921 Willow
  • 131. Shiflet, Thomas N., ed. 1994. Rangeland cover types of the United States. Denver, CO: Society for Range Management. 152 p. [23362]

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Habitat: Cover Types

More info on this topic.

This species is known to occur in association with the following cover types (as classified by the Society of American Foresters):

More info for the term: cover

SAF COVER TYPES [52]:

1 Jack pine

5 Balsam fir

12 Black spruce

13 Black spruce-tamarack

38 Tamarack

107 White spruce

201 White spruce

202 White spruce-paper birch

203 Balsam poplar

204 Black spruce

206 Engelmann spruce-subalpine fir

217 Aspen

218 Lodgepole pine

222 Black cottonwood-willow

251 White spruce-aspen

252 Paper birch

253 Black spruce-white spruce

254 Black spruce-paper birch
  • 52. Eyre, F. H., ed. 1980. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters. 148 p. [905]

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Habitat: Plant Associations

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This species is known to occur in association with the following plant community types (as classified by Küchler 1964):

KUCHLER [90] PLANT ASSOCIATIONS:

K008 Lodgepole pine-subalpine forest

K012 Douglas-fir forest

K015 Western spruce-fir forest

K052 Alpine meadows and barren

K093 Great Lakes spruce-fir forest

K094 Conifer bog
  • 90. Kuchler, A. W. 1964. Manual to accompany the map of potential vegetation of the conterminous United States. Special Publication No. 36. New York: American Geographical Society. 77 p. [1384]

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Habitat: Ecosystem

More info on this topic.

This species is known to occur in the following ecosystem types (as named by the U.S. Forest Service in their Forest and Range Ecosystem [FRES] Type classification):

ECOSYSTEMS [58]:

FRES10 White-red-jack pine

FRES11 Spruce-fir

FRES20 Douglas-fir

FRES23 Fir-spruce

FRES26 Lodgepole pine

FRES44 Alpine
  • 58. Garrison, George A.; Bjugstad, Ardell J.; Duncan, Don A.; Lewis, Mont E.; Smith, Dixie R. 1977. Vegetation and environmental features of forest and range ecosystems. Agric. Handb. 475. Washington, DC: U.S. Department of Agriculture, Forest Service. 68 p. [998]

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Arctic and alpine tundra, acidic rocky slopes and barrens, muskegs, peat bogs, stream banks, open subalpine summits; 0--3400m.
Creative Commons Attribution Non Commercial Share Alike 3.0 (CC BY-NC-SA 3.0)

© Missouri Botanical Garden, 4344 Shaw Boulevard, St. Louis, MO, 63110 USA

Source: Missouri Botanical Garden

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General Ecology

Fire Management Considerations

More info for the terms: bog, cover, fire exclusion, fire severity, fuel, natural, severity, shrub, shrubs, tundra

Prescribed burning can reduce bog birch cover. Naturally occurring fires controlled the spread of bog birch on Canadian Rocky Mountain rangelands prior to active fire exclusion. Today, prescribed fires are used to reduce the spread of bog birch and other shrubs and to restore and maintain native grasslands [45]. The effects of prescribed burning on bog birch vary depending on burning conditions, fire season, severity, and postfire growing conditions. Burning bog birch stands in spring, when carbohydrate reserves are lowest, apparently promotes postfire sprouting and growth. Increased fire severity and fall burning both increase mortality in bog birch [43].

Prescribed burning at 3- to 6-year intervals in the Rocky Mountain foothills of Alberta has decreased shrub cover and increased forage production [45]. Bog birch cover decreased by 35% following a moderate-severity, prescribed spring fire in wood bison habitat in Fort Providence, Northwest Territories. After 3 months, bog birch cover increased by 26% [59]. Due to bog birch's "vigorous" sprouting response, burning at regular intervals is necessary to minimize its regrowth [29].

Fuel potential of bog birch is low because leaf moisture content is high [143]. Moisture content of bog birch measured near Inuvik, Northwest Territories, is given in the table below [164].

Moisture content (%) of bog birch in dry and wet tundra [164]
  18 July 1 August 15 August
Dry tundra 44 47 47
Wet tundra 56 50 51

In very wet places bog birch stands act as natural fire breaks [64].
  • 29. Bork, Edward; Smith, Darrell; Willoughby, Michael. 1996. Prescribed burning of bog birch. Rangelands. 18(1): 4-7. [26709]
  • 43. de Groot, William J. 1998. Fire ecology of Betula glandulosa Michx. Edmonton, AB: University of Alberta. 203 p. Dissertation. [66522]
  • 45. DeBano, Leonard F.; Neary, Daniel G.; Ffolliott, Peter F. 1998. Preface. In: DeBano, Leonard F.; Neary, Daniel G.; Ffolliott, Peter F. Fire's effects on ecosystems. New York: John Wiley & Sons, Inc: xv-xvii. [29829]
  • 59. Gates, C. C.; Chowns, T.; Antoniak, R.; Ellsworth, T. 1998. Succession and prescribed fire in shrublands in northern Canada: shaping the landscape to enhance bison habitat. In: Close, Kelly; Bartlette, Roberta A., eds. Fire management under fire (adapting to change): Proceedings, 1994 Interior West Fire Council meeting and program; 1994 November 1-4; Coeur d'Alene, ID. Fairfield, WA: Interior West Fire Council: 125-132. [29068]
  • 64. Hansen, Paul L.; Chadde, Steve W.; Pfister, Robert D. 1988. Riparian dominance types of Montana. Misc. Publ. No. 49. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station. 411 p. [5660]
  • 143. Sylvester, T. W.; Wein, Ross W. 1981. Fuel characteristics of arctic plant species and simulated plant community flammability by Rothermel's model. Canadian Journal of Botany. 59: 898-907. [17685]
  • 164. Wein, R. W. 1974. Recovery of vegetation in arctic regions after burning. Rep. 74-6. Ottawa: Canadian Task Force on Northern Oil Development. 41 p. [13001]

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Plant Response to Fire

More info for the terms: bog, cover, density, fire severity, frequency, high-severity fire, lichen, low-severity fire, root crown, severity, top-kill, tundra, wildfire

Fire has a substantial influence on bog birch growth and population dynamics [43,44]. Bog birch survives most low- and moderate- severity fires by sprouting from the root crown and/or rhizomes after top-kill by fire [43,44,82,112,165]. It flowers "profusely" from young sprouts [11] and produces large leaves after burning. Bog birch leaves were up to 3 times larger 1 year after fire than leaves on unburned plants near Inuvik, Northwest Territories, a response that may be linked to the increase in available nutrients following the fire [164,165]. A large proportion of phosphorus released into the soil after fire is absorbed by the roots of bog birch and then incorporated into new stem and leaf tissue. Changes in bog birch root biomass, root phosphorus concentration, and root phosphorus mass with burning of a mature 140-year-old black spruce/star reindeer lichen woodland at Schefferville, Quebec, were as follows [11]:

Changes in root biomass and root phosphorus in bog birch before and after fire [11]
Root characteristics Mature (140-year-old) Burned (0-year-old) Change (%)
root biomass (kg/ha) 9,159 8,886 -4
concentration of P in roots (% dry weight) 0.047 0.133 +283
mass of P in roots (kg/ha) 4.30 11.80 +274

Bog birch increases after low- to moderate-severity fires [164]. Repeated fires near treeline and on some wet sites in Alaska and northern Canada result in thickets of bog birch, mountain alder, and willows (Salix spp.) [82,154]. On tundra sites near Inuvik, Northwest Territories, total vascular plant cover on a burned area was more than twice that on an adjacent unburned area. The increase was due in large part to bog birch, which increased 8.8% after the burn [92].

Because of its ability to sprout from the root crown and rhizomes, bog birch is among the first plants to regenerate after fire in many communities [26,43,44,69,105,149,150]. Bog birch also persists into middle and late successional stages [23,105,133,149,150]. It was present in all postfire successional stages observed in a black spruce/reindeer lichen woodland in northern Quebec, but was most abundant in the intermediate stages between approximately 20 and 50 years after fire [56]. Frequency of bog birch at each successional stage is summarized below.

Frequency (%) of bog birch at 4 postfire stages [56]
postfire year 5 postfire year 20 postfire year 50 postfire year 90
24 63 69 1

In subarctic black spruce forests of western Labrador, bog birch was most abundant 18 to 40 years after fire. Mean canopy volume of bog birch between 2 and 140 years after fire is summarized below [132].

Mean canopy volume (m³) of bog birch across 5 postfire successional stages [132]
postfire year 2 postfire year 18 postfire year 40 postfire year 80 postfire year 140
0.01 2.23 1.04 1.01 0.00

Low-severity fire and spring burning promote sprouting in bog birch. In a study conducted during the 1992 growing season in the Rocky Mountains of Alberta, bog birch plants were burned in low-, medium-, and high-severity treatments. Plants burned earlier in the growing season and in low-severity treatments produced more and taller sprouts by the end of the first year after burning than plants burned late in the growing season or in severe fire treatments. Bog birch in the high-severity treatments sprouted latest. Following high-severity fire, new sprouts originated from the bottoms of rhizomes, indicating mortality of buds closer to the soil surface. No sprouting occurred on plants burned after late June, which may be related to seasonal variation in plant hormones that release buds from dormancy and promote stem extension in bog birch. Fall burning resulted in greatest plant mortality than spring and summer burning. Some plants burned in the fall sprouted the following year [43,44].

Bog birch was more abundant in "lightly" burned areas than in "heavily" burned areas following a June 1971 wildfire in black spruce forest near Fairbanks, Alaska [151]. Density of bog birch for 4 years following the fire is provided below.

Bog birch density (stems/ha) after wildfire in heavily and lightly burned areas [151]
  postfire year 1 postfire year 2 postfire year 3 postfire year 4
heavy 125 1,625 750 1,625
light 1,125 4,500 1,750 3,375

The response of bog birch to fire in a valley-bottom floodplain in the Rocky Mountains of Alberta varied with fire severity. Bog birch stem density increased for 2 years after a spring prescribed, low-severity fire in 1984 due to abundant sprouting. Following high-severity burns in 1987 and 1993, however, both stem density and canopy cover sharply declined. Results of this study are given in the figure below [29].

Although survival of bog birch plants decreases when fire severity is high, seedlings establish more easily on the bare mineral soil that is exposed after a high-severity fire [23,42].

On some sites, including in Wisconsin fens, bog birch increases in the absence of fire [38]. In the Rocky Mountains of Alberta, bog birch forms extensive, closed-canopy stands where fire has been excluded [29].

  • 11. Auclair, A. N. D. 1983. The role of fire in lichen-dominated tundra and forest-tundra. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. Scope 18. New York: John Wiley & Sons: 235-256. [18510]
  • 23. Black, R. A.; Bliss, L. C. 1978. Recovery sequence of Picea mariana - Vaccinium uliginosum forests after burning near Inuvik, Northwest Territories, Canada. Canadian Journal of Botany. 56: 2020-2030. [7448]
  • 26. Bliss, L. C. 1988. Arctic tundra and polar desert biome. In: Barbour, Michael G.; Billings, William Dwight, eds. North American terrestrial vegetation. Cambridge; New York: Cambridge University Press: 1-32. [13877]
  • 29. Bork, Edward; Smith, Darrell; Willoughby, Michael. 1996. Prescribed burning of bog birch. Rangelands. 18(1): 4-7. [26709]
  • 38. Curtis, John T. 1959. Fen, meadow, and bog. In: Curtis, John T. The vegetation of Wisconsin. Madison, WI: The University of Wisconsin Press: 361-381. [60530]
  • 42. de Groot, W. J.; Wein, Ross W. 1999. Betula glandulosa Michx. response to burning and postfire growth temperature and implications of climate change. International Journal of Wildland Fire. 9(1): 51-64. [37477]
  • 43. de Groot, William J. 1998. Fire ecology of Betula glandulosa Michx. Edmonton, AB: University of Alberta. 203 p. Dissertation. [66522]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 56. Fortin, Marie-Josee; Payette, Serge; Marineau, Kim. 1999. Spatial vegetation diversity index along a postfire successional gradient in the northern boreal forest. Ecoscience. 6(2): 204-213. [36002]
  • 69. Hawkes, Brad C. 1983. Fire history and management study of Kluane National Park. Winnipeg, MB: Parks Canada, Prairie Region. 85 p. [21211]
  • 82. Kelsall, John P.; Telfer, E. S.; Wright, Thomas D. 1977. The effects of fire on the ecology of the boreal forest, with particular reference to the Canadian north: a review and selected bibliography. Occasional Paper Number 32. Ottawa: Fisheries and Environment Canada, Canadian Wildlife Service. 58 p. [8403]
  • 92. Landhausser, Simon M.; Wein, Ross W. 1993. Postfire vegetation recovery and tree establishment at the Arctic treeline: climate-change--vegetation response hypotheses. Journal of Ecology. 81: 665-672. [22741]
  • 105. Moore, T. R. 1980. The nutrient status of subarctic woodland soils. Arctic and Alpine Research. 12(2): 147-160. [51702]
  • 112. Parminter, John. 1984. Fire-ecological relationships for the biogeoclimatic zones of the northern portion of the Mackenzie Timber Supply Area: summary report. In: Northern Fire Ecology Project: Northern Mackenzie Timber Supply Area. Victoria, BC: Province of British Columbia, Ministry of Forests. 59 p. [9205]
  • 132. Simon, Neal P. P.; Schwab, Francis E. 2005. Plant community structure after wildfire in the subarctic forests of western Labrador. Northern Journal of Applied Forestry. 22(4): 229-235. [61221]
  • 133. Sirois, Luc; Payette, Serge. 1989. Postfire black spruce establishment in subarctic and boreal Quebec. Canadian Journal of Forestry Research. 19: 1571-1580. [10110]
  • 149. Van Cleve, Keith; Viereck, Leslie A. 1981. Forest succession in relation to nutrient cycling in the boreal forest of Alaska. In: Fire and succession in conifer forests of North America. New York: Springer-Verlag: 185-211. [50633]
  • 150. Viereck, L. A. 1983. The effects of fire in black spruce ecosystems of Alaska and northern Canada. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. New York: John Wiley and Sons Ltd.: 201-220. [7078]
  • 151. Viereck, L. A.; Dyrness, C. T. 1979. Ecological effects of the Wickersham Dome fire near Fairbanks, Alaska. Gen. Tech. Rep. PNW-90. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 71 p. [6392]
  • 154. Viereck, Leslie A. 1973. Wildfire in the taiga of Alaska. Quaternary Research. 3: 465-495. [7247]
  • 164. Wein, R. W. 1974. Recovery of vegetation in arctic regions after burning. Rep. 74-6. Ottawa: Canadian Task Force on Northern Oil Development. 41 p. [13001]
  • 165. Wein, Ross W.; Bliss, L. C. 1973. Changes in arctic Eriophorum tussock communities following fire. Ecology. 54(4): 845-852. [9827]

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Immediate Effect of Fire

More info for the terms: bog, high-severity fire, top-kill

Bog birch is easily top-killed by fire due to its thin bark, small stem diameter, and resinous, flammable twigs [44,77,159]. Both young and old bog birch plants are susceptible to top-kill by fire [44]. High-severity fire can kill bog birch plants by heating or consuming organic soil layers and scorching root crowns, rhizomes, and roots [93,169]. Seeds are easily killed by fire [44].
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 77. Hulten, Eric. 1968. Flora of Alaska and neighboring territories. Stanford, CA: Stanford University Press. 1008 p. [13403]
  • 93. Lotan, James E.; Alexander, Martin E.; Arno, Stephen F.; French, Richard E.; Langdon, O. Gordon; Loomis, Robert M.; Norum, Rodney A.; Rothermel, Richard C.; Schmidt, Wyman C.; Van Wagtendonk, Jan. 1981. Effects of fire on flora: A state-of-knowledge review: Proceedings of the national fire effects workshop; 1978 April 10-14; Denver, CO. Gen. Tech. Rep. WO-16. Washington, DC: U.S. Department of Agriculture, Forest Service. 71 p. [1475]
  • 159. Viereck, Leslie A.; Little, Elbert L., Jr. 1972. Alaska trees and shrubs. Agric. Handb. 410. Washington, DC: U.S. Department of Agriculture, Forest Service. 265 p. [6884]
  • 169. Zasada, J. 1986. Natural regeneration of trees and tall shrubs on forest sites in interior Alaska. In: Van Cleve, K.; Chapin, F. S., III; Flanagan, P. W.; Viereck, L. A.; Dyrness, C. T., eds. Forest ecosystems in the Alaska taiga: A synthesis of structure and function. New York: Springer-Verlag: 44-73. [2291]

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Post-fire Regeneration

More info for the terms: adventitious, initial off-site colonizer, rhizome, root crown, shrub

POSTFIRE REGENERATION STRATEGY [140]:
Small shrub, adventitious buds and/or a sprouting root crown
Rhizomatous shrub, rhizome in soil
Initial off-site colonizer (off site, initial community)
  • 140. Stickney, Peter F. 1989. Seral origin of species comprising secondary plant succession in Northern Rocky Mountain forests. FEIS workshop: Postfire regeneration. Unpublished draft on file at: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, Fire Sciences Laboratory, Missoula, MT. 10 p. [20090]

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Fire Ecology

More info for the terms: bog, cover, fire frequency, fire-return interval, frequency, fuel, lichen, lichens, root crown, shrubs, top-kill, tree

Fire adaptations: Bog birch can survive low- to moderate-severity fires. On many sites, bog birch has deep roots and rhizomes that are protected from all but high-severity fires [12,42]. Bog birch regenerates after fire by sprouting from the root crown and from dormant buds on the rhizomes [43,44,82,112,165]. In arctic and boreal ecosystems, bog birch increases sprout production, sprout height, and aboveground biomass production during the first 1 to 2 years after a fire. Bog birch responds to top-kill by sprouting from dormant buds on the root crown and rhizomes after top-kill release. Burned plants may produce large leaves that senesce later in the fall than leaves on undisturbed plants, thereby maximizing photosynthate production [43]. Bog birch samaras are dispersed by wind and can invade burned areas from off site [11]. Although bog birch can establish from seed after fire, seedlings are susceptible to both drought and shade [43,44].

FIRE REGIMES: Bog birch is adapted to a wide range of FIRE REGIMES, from subarctic and alpine areas that seldom burn to boreal environments that burn frequently [42,44]. Wetland areas where bog birch grows burn infrequently due to the high moisture content of the vegetation and soil. These sites sometimes act as firebreaks. Fires do occur, however, during dry summers or in the spring and fall when the vegetation is dry [35,43,44,86,104,143].

In interior Alaska, bog birch is found on poorly drained and permafrost underlain sites occupied primarily by black spruce stands, muskegs, and bogs. These types are widespread in Alaska and burn frequently [154,158]. Black spruce-birch (Betula spp.) is the most widespread forest type in interior Alaska and also the type with the highest frequency of fire [158]. Native Americans were an important cause of fires in the black spruce-birch ecosystem [96]. Fire frequency increased with the increase in mining activity in the 1800s [154]. Today, most fires are lightning caused [70,95]. Between 1940 and 1969, lightning was responsible for 78% of the area burned in interior Alaska [154].

Fires occur in interior Alaska between 1 April and 30 September. Most fires occur in May, June, and July, corresponding with the highest annual temperatures, longest day length, lowest humidity and precipitation, and high winds [55,154]. Fires can occur, however, whenever fuels are not covered with snow and are exposed to sufficiently warm temperatures and drying winds [154].

Fire years are sporadic in occurrence but tend to occur at least once every decade [71]. “Exceptional fire years” are characteristic of the black spruce-birch ecosystem. In Alaska, 6 years (1941, 1950, 1957, 1969, and 1977) accounted for 63% of the total area burned between 1940 and 1978 [160]. The average acreage burned each year in interior Alaska is approximately 1 million acres [96]. Fires tend to be large and may spread over thousands to hundreds of thousands of acres or more [71,94,150].

Estimated fire-return intervals in the black spruce-birch ecosystem vary from 50 to 200 years [71,160]. Fires occur every 50 to 70 years in black spruce-white spruce/bog birch/reindeer lichen communities in interior Alaska [55]. Heinselman [71] estimates a fire-return interval of 130 years for open black spruce/reindeer lichen forest and 100 years for closed-canopy black spruce forest. Mean fire-return intervals in lowland black spruce forests on the Kenai Peninsula, Alaska, range from 89 to 195 years [4,97].

Black spruce-birch communities experience high-severity, stand-replacing fires. These communities are highly flammable due to the abundance of ericaceous shrubs, the prevalence of dead, low-hanging branches on the black spruce trees, which are often covered with highly flammable epiphytic lichens, and the thick moss and lichen mats that cover the forest floor and become highly flammable after periods of low rainfall [94,95,155]. There is often nearly continuous fuel from the forest floor to the tree crowns [160]. Most fires in black spruce-birch communities are either crown fires or ground fires severe enough to damage or kill aboveground vegetation, including overstory trees. Fires may be severe enough to completely expose the mineral soil layer [50,71,150,160].

The following table provides fire return intervals for plant communities and ecosystems where bog birch is important. For further information, see the FEIS review of the dominant species listed below.

Fire-return intervals for plant communities with bog birch
Community or Ecosystem Dominant Species Fire Return Interval Range (years)
birch Betula spp. 80-230 [142]
tamarack Larix laricina 35-200 [113]
Great Lakes spruce-fir Picea-Abies spp. 35 to >200
northeastern spruce-fir Picea-Abies spp. 35-200 [50]
Engelmann spruce-subalpine fir Picea engelmannii-Abies lasiocarpa 35 to >200 [7]
black spruce Picea mariana 35-200
conifer bog* Picea mariana-Larix laricina 35-200 [50]
jack pine Pinus banksiana <35 to 200 [34,50]
Rocky Mountain lodgepole pine* Pinus contorta var. latifolia 25-340 [16,17,144]
aspen-birch Populus tremuloides-Betula papyrifera 35-200 [50,161]
quaking aspen (west of the Great Plains) Populus tremuloides 7-120 [7,62,103]
Rocky Mountain Douglas-fir* Pseudotsuga menziesii var. glauca 25-100 [7,8,9]
*fire return interval varies widely; trends in variation are noted in the species review
  • 7. Arno, Stephen F. 2000. Fire in western forest ecosystems. In: Brown, James K.; Smith, Jane Kapler, eds. Wildland fire in ecosystems: Effects of fire on flora. Gen. Tech. Rep. RMRS-GTR-42-vol. 2. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 97-120. [36984]
  • 8. Arno, Stephen F.; Gruell, George E. 1983. Fire history at the forest-grassland ecotone in southwestern Montana. Journal of Range Management. 36(3): 332-336. [342]
  • 9. Arno, Stephen F.; Scott, Joe H.; Hartwell, Michael G. 1995. Age-class structure of old growth ponderosa pine/Douglas-fir stands and its relationship to fire history. Res. Pap. INT-RP-481. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 25 p. [25928]
  • 50. Duchesne, Luc C.; Hawkes, Brad C. 2000. Fire in northern ecosystems. In: Brown, James K.; Smith, Jane Kapler, eds. Wildland fire in ecosystems: Effects of fire on flora. Gen. Tech. Rep. RMRS-GTR-42-vol. 2. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 35-51. [36982]
  • 11. Auclair, A. N. D. 1983. The role of fire in lichen-dominated tundra and forest-tundra. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. Scope 18. New York: John Wiley & Sons: 235-256. [18510]
  • 12. Auclair, Allan N. D. 1985. Postfire regeneration of plant and soil organic pools in a Picea mariana-Cladonia stellaris ecosystem. Canadian Journal of Forest Research. 15(1): 279-291. [66004]
  • 35. Crane, Marilyn F. 1982. Fire ecology of Rocky Mountain Region forest habitat types. Final report: Contract No. 43-83X9-1-884. Missoula, MT: U.S. Department of Agriculture, Forest Service, Region 1. 272 p. On file with: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, Fire Sciences Laboratory, Missoula, MT. [5292]
  • 42. de Groot, W. J.; Wein, Ross W. 1999. Betula glandulosa Michx. response to burning and postfire growth temperature and implications of climate change. International Journal of Wildland Fire. 9(1): 51-64. [37477]
  • 43. de Groot, William J. 1998. Fire ecology of Betula glandulosa Michx. Edmonton, AB: University of Alberta. 203 p. Dissertation. [66522]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 55. Foote, M. Joan. 1983. Classification, description, and dynamics of plant communities after fire in the taiga of interior Alaska. Res. Pap. PNW-307. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 108 p. [18707]
  • 62. Gruell, G. E.; Loope, L. L. 1974. Relationships among aspen, fire, and ungulate browsing in Jackson Hole, Wyoming. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 33 p. In cooperation with: U.S. Department of the Interior, National Park Service, Rocky Mountain Region. [3862]
  • 70. Heinselman, Miron L. 1981. Fire and succession in the conifer forests of northern North America. In: West, Darrell C.; Shugart, Herman H.; Botkin, Daniel B., eds. Forest succession: concepts and applications. New York: Springer-Verlag: 374-405. [29237]
  • 82. Kelsall, John P.; Telfer, E. S.; Wright, Thomas D. 1977. The effects of fire on the ecology of the boreal forest, with particular reference to the Canadian north: a review and selected bibliography. Occasional Paper Number 32. Ottawa: Fisheries and Environment Canada, Canadian Wildlife Service. 58 p. [8403]
  • 86. Kovalchik, Bernard L. 1987. Riparian zone associations: Deschutes, Ochoco, Fremont, and Winema National Forests. R6 ECOL TP-279-87. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Region. 171 p. [9632]
  • 94. Lutz, H. J. 1956. Ecological effects of forest fires in the interior of Alaska. Tech. Bull. No. 1133. Washington, DC: U.S. Department of Agriculture, Forest Service. 121 p. [7653]
  • 95. Lutz, H. J. 1960. Fire as an ecological factor in the boreal forest of Alaska. Journal of Forestry. 58: 454-460. [16603]
  • 97. Lynch, Jason A.; Hollis, Jeremy L.; Hu, Feng Sheng. 2004. Climatic and landscape controls of the boreal forest fire regime: Holocene records from Alaska. Journal of Ecology. 92(3): 477-489. [48477]
  • 103. Meinecke, E. P. 1929. Quaking aspen: A study in applied forest pathology. Tech. Bull. No. 155. Washington, DC: U.S. Department of Agriculture. 34 p. [26669]
  • 104. Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L. 2004. Shrubs of other families. In: Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L., comps. Restoring western ranges and wildlands. Gen. Tech. Rep. RMRS-GTR-136-vol-2. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 598-698. [52846]
  • 112. Parminter, John. 1984. Fire-ecological relationships for the biogeoclimatic zones of the northern portion of the Mackenzie Timber Supply Area: summary report. In: Northern Fire Ecology Project: Northern Mackenzie Timber Supply Area. Victoria, BC: Province of British Columbia, Ministry of Forests. 59 p. [9205]
  • 113. Paysen, Timothy E.; Ansley, R. James; Brown, James K.; Gottfried, Gerald J.; Haase, Sally M.; Harrington, Michael G.; Narog, Marcia G.; Sackett, Stephen S.; Wilson, Ruth C. 2000. Fire in western shrubland, woodland, and grassland ecosystems. In: Brown, James K.; Smith, Jane Kapler, eds. Wildland fire in ecosystems: Effects of fire on flora. Gen. Tech. Rep. RMRS-GTR-42-vol. 2. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 121-159. [36978]
  • 142. Swain, Albert M. 1978. Environmental changes during the past 2000 years in north-central Wisconsin: analysis of pollen, charcoal, and seeds from varved lake sediments. Quaternary Research. 10: 55-68. [6968]
  • 143. Sylvester, T. W.; Wein, Ross W. 1981. Fuel characteristics of arctic plant species and simulated plant community flammability by Rothermel's model. Canadian Journal of Botany. 59: 898-907. [17685]
  • 144. Tande, Gerald F. 1979. Fire history and vegetation pattern of coniferous forests in Jasper National Park, Alberta. Canadian Journal of Botany. 57: 1912-1931. [18676]
  • 150. Viereck, L. A. 1983. The effects of fire in black spruce ecosystems of Alaska and northern Canada. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. New York: John Wiley and Sons Ltd.: 201-220. [7078]
  • 154. Viereck, Leslie A. 1973. Wildfire in the taiga of Alaska. Quaternary Research. 3: 465-495. [7247]
  • 155. Viereck, Leslie A. 1975. Forest ecology of the Alaska taiga. In: Proceedings of the circumpolar conference on northern ecology; 1975 September 15-18; Ottawa, ON. Washington, DC: U.S. Department of Agriculture, Forest Service: 1-22. [7315]
  • 158. Viereck, Leslie A.; Foote, Joan; Dyrness, C. T.; Van Cleve, Keith; Kane, Douglas; Seifert, Richard. 1979. Preliminary results of experimental fires in the black spruce type of interior Alaska. Res. Note PNW-332. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 27 p. [7077]
  • 160. Viereck, Leslie A.; Schandelmeier, Linda A. 1980. Effects of fire in Alaska and adjacent Canada--a literature review. BLM-Alaska Tech. Rep. 6; BLM/AK/TR-80/06. Anchorage, AK: U.S. Department of the Interior, Bureau of Land Management, Alaska State Office. 124 p. [28862]
  • 161. Wade, Dale D.; Brock, Brent L.; Brose, Patrick H.; Grace, James B.; Hoch, Greg A.; Patterson, William A., III. 2000. Fire in eastern ecosystems. In: Brown, James K.; Smith, Jane Kapler, eds. Wildland fire in ecosystems: Effects of fire on flora. Gen. Tech. Rep. RMRS-GTR-42-vol. 2. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 53-96. [36983]
  • 165. Wein, Ross W.; Bliss, L. C. 1973. Changes in arctic Eriophorum tussock communities following fire. Ecology. 54(4): 845-852. [9827]
  • 34. Cleland, David T.; Crow, Thomas R.; Saunders, Sari C.; Dickmann, Donald I.; Maclean, Ann L.; Jordan, James K.; Watson, Richard L.; Sloan, Alyssa M.; Brosofske, Kimberley D. 2004. Characterizing historical and modern FIRE REGIMES in Michigan (USA): a landscape ecosystem approach. Landscape Ecology. 19: 311-325. [54326]
  • 4. Anderson, R. S.; Hallett, D. J.; Berg, E.; Jass, R. B.; Toney, J. L.; de Fontaine, C. S.; DeVolder, A. 2006. Holocene development of boreal forests and FIRE REGIMES on the Kenai lowlands of Alaska. The Holocene. 16(6): 791-803. [66312]
  • 16. Barrett, Stephen W. 1993. FIRE REGIMES on the Clearwater and Nez Perce National Forests north-central Idaho. Final Report: Order No. 43-0276-3-0112. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, Fire Sciences Laboratory. Unpublished report on file with: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory, Missoula, MT. 21 p. [41883]
  • 17. Barrett, Stephen W.; Arno, Stephen F.; Key, Carl H. 1991. FIRE REGIMES of western larch - lodgepole pine forests in Glacier National Park, Montana. Canadian Journal of Forest Research. 21: 1711-1720. [17290]
  • 71. Heinselman, Miron L. 1981. Fire intensity and frequency as factors in the distribution and structure of northern ecosystems. In: Mooney, H. A.; Bonnicksen, T. M.; Christensen, N. L.; Lotan, J. E.; Reiners, W. A., technical coordinators. FIRE REGIMES and ecosystem properties: Proceedings of the conference; 1978 December 11-15; Honolulu, HI. Gen. Tech. Rep. WO-26. Washington, DC: U.S. Department of Agriculture, Forest Service: 7-57. [4390]
  • 96. Lutz, Harold J. 1950. Ecological effects of forest fires in the interior of Alaska. Natural Resources Council Bulletin. [Proceedings, Alaskan Science Conference]. 122: 120. [42128]

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Successional Status

More info on this topic.

More info for the terms: bog, climax, cover, frequency, shrub, tundra

Bog birch is shade intolerant [42,44,87]. It is characteristic of canopy openings in black spruce woodlands in boreal Canada [3]. It establishes from seed or, more commonly, by sprouting after fire and other disturbances [23,43,148,149] and in many communities persists through subsequent successional stages. In many black spruce communities in central Alaska and northern Canada, bog birch appears soon after low- to moderate-severity fires and is dominant in the vegetation 6 to 25 years after fire. Trees begin to dominate after 25 to 30 years, but the low shrub layer of bog birch and associated species continues to expand and increase in cover [149,150]. In black spruce woodlands in the Northwest Territories, bog birch is most common 15 to 20 years after fire but is also present in stands as old as 300 years [23].

The table below summarizes an analysis of 5 stands representing a vegetation chronosequence on gravel outwash of the Muldrow Glacier in Denali National Park, Alaska. Bog birch was not present in the earliest successional stage but was abundant in intermediate stages and persistent in the oldest stands [153].

Frequency (%) and cover (%) of bog birch at 5 successional stages [153]
Successional stage Frequency Cover
Pioneer stage (25-30 years) 0 0
Meadow stage (100 years) 80 <5
Early shrub stage (150-200 years) 100 50-75
Late shrub stage (200-300 years) 100 50-75
Climax tundra (5,000-9,000 years) 100 25-50
  • 3. Alexander, M. E.; Stocks, B. J.; Lawson, B. D. 1991. Fire behavior in black spruce-lichen woodland: the Porter Lake project. NOR-X-310. Edmonton, AB: Forestry Canada, Northwest Region, Northern Forestry Centre. 44 p. [18823]
  • 23. Black, R. A.; Bliss, L. C. 1978. Recovery sequence of Picea mariana - Vaccinium uliginosum forests after burning near Inuvik, Northwest Territories, Canada. Canadian Journal of Botany. 56: 2020-2030. [7448]
  • 42. de Groot, W. J.; Wein, Ross W. 1999. Betula glandulosa Michx. response to burning and postfire growth temperature and implications of climate change. International Journal of Wildland Fire. 9(1): 51-64. [37477]
  • 43. de Groot, William J. 1998. Fire ecology of Betula glandulosa Michx. Edmonton, AB: University of Alberta. 203 p. Dissertation. [66522]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 87. Krajina, V. J.; Klinka, K.; Worrall, J. 1982. Distribution and ecological characteristics of trees and shrubs of British Columbia. Vancouver, BC: University of British Columbia, Department of Botany and Faculty of Forestry. 131 p. [6728]
  • 148. U.S. Department of the Interior. 1982. Alaska Interagency Fire Management Plan: Tanana/Minchumian Planning Area. Environmental Assessment: Final. Anchorage, AK: U.S. Department of the Interior. 148 p. [21538]
  • 149. Van Cleve, Keith; Viereck, Leslie A. 1981. Forest succession in relation to nutrient cycling in the boreal forest of Alaska. In: Fire and succession in conifer forests of North America. New York: Springer-Verlag: 185-211. [50633]
  • 150. Viereck, L. A. 1983. The effects of fire in black spruce ecosystems of Alaska and northern Canada. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. New York: John Wiley and Sons Ltd.: 201-220. [7078]
  • 153. Viereck, Leslie A. 1966. Plant succession and soil development on gravel outwash of the Muldrow Glacier, Alaska. Ecological Monographs. 36(3): 181-199. [12484]

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Regeneration Processes

More info for the terms: bog, cover, density, layering, monoecious, root crown

Bog birch reproduces by seed and vegetatively by branch layering and sprouting [26,44]. Reproduction by seed is more common in southern populations, and vegetative reproduction is more common in northern populations [73,166,167].

Pollination: Bog birch is wind pollinated. In a bog birch population on Baffin Island, Northwest Territories, female catkins were smaller and contained 50% fewer flowers than were contained in female catkins from a more southern site in subarctic Quebec. There was an estimated 10-fold difference in pollen dispersed between the 2 sites. At the northern extent of its distribution, bog birch is clonal, and the distance between genetically distinct individuals is great. In these areas, female catkins are more likely to receive incompatible pollen, preventing fertilization from occurring [167].

Breeding system: Bog birch is monoecious [64,104]. Plants are not self fertile [167].

Seed production: Bog birch produces numerous catkins, each of which yields 30 to 50 samaras [166]. Seed production is generally high in more southern parts of its range [30,42,73]. In more northern areas, production of viable seed is limited by the shorter growing season, lower temperatures, and distance between genetically distinct individuals [166].

Seed dispersal: Bog birch seeds are dispersed in their samaras. Wind, water, and sometimes gravity disperse the samaras. Samaras may blow across crusted snow [11,44,104].

Seed banking: Bog birch produces numerous, tiny seeds and has a transient seed bank. In a review of the literature, Karrfalt [41] states that birch seeds may be abundant in the soil but the seeds are generally short lived. Rowe 1983 [124] states that viable bog birch seeds are "rare" in the soil seed bank. Bog birch seeds were present, however, in the first 1.2 inches (3 cm) of soil collected from alpine sites on the Gaspé Peninsula, Quebec [106]. Results of this study are provided in the table below.

Bog birch seed production and density on sites in Quebec [106]

Site Total seeds/m² Viable seeds/m² % cover in aboveground vegetation
1 3 0 0
2 275 0 18
3 1,263 13 10
4 1,003 6 10
5 6 0 0

Germination: Prechilling improves germination of bog birch seeds. Optimum germination temperature for many arctic species is 59 to 86 °F (15-30 °C) [26]. The germination rate of bog birch seeds collected from alpine sites in the White Mountains, New Hampshire, was 25% for refrigerated seeds and 4% for unrefrigerated seeds. Days required for germination ranged from 14 to 28 for refrigerated seeds and from 27 to 299 for unrefrigerated seeds [108].

Seed viability varies with latitude. At the northern range limit of bog birch on Baffin Island, <0.5% of seeds were viable. Very few samaras contained seeds with fully developed embryos. At a southern site in subarctic Quebec, 70% of seeds were viable [166,167]. Seeds that overwinter on plants remain viable until they disperse the following spring [166].

Seed germination and samara weight may be correlated. In a germination study in Kuujjuaq, Quebec, no seeds from samaras weighing <0.09 mg germinated, few samaras weighing <0.12 mg had seed that germinated, and all samaras weighing >0.34 mg had seed that germinated [166]. Germination of wind-dispersed seeds may be highest on exposed mineral soils [104].

Seedling establishment/growth: Seedling recruitment rates in bog birch populations are usually very low. Site disturbance by fire increases the likelihood of seedling establishment [44]. Although recruitment from seed is almost nonexistent in northern bog birch populations, plants of all age classes were evident in a southern Quebec population [73,166]. Seedling growth is very slow, and seedling mortality is often high [41,44].

Vegetative regeneration: Bog birch reproduces vegetatively by branch layering and sprouting from dormant buds on the root crown and rhizomes [26,44]. Bog birch is clonal in the northern parts of its range [166].

  • 11. Auclair, A. N. D. 1983. The role of fire in lichen-dominated tundra and forest-tundra. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. Scope 18. New York: John Wiley & Sons: 235-256. [18510]
  • 26. Bliss, L. C. 1988. Arctic tundra and polar desert biome. In: Barbour, Michael G.; Billings, William Dwight, eds. North American terrestrial vegetation. Cambridge; New York: Cambridge University Press: 1-32. [13877]
  • 30. Boucher, Tina V. 2003. Vegetation response to prescribed fire in the Kenai Mountains, Alaska. Res. Pap. PNW-RP-554. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 59 p. [48392]
  • 41. de Groot, W. J.; Thomas, P. A.; Wein, Ross W. 1997. Biological flora of the British Isles: No. 194. Betula nana L. and Betula glandulosa Michx. Journal of Ecology. 85(2): 241-264. [65929]
  • 42. de Groot, W. J.; Wein, Ross W. 1999. Betula glandulosa Michx. response to burning and postfire growth temperature and implications of climate change. International Journal of Wildland Fire. 9(1): 51-64. [37477]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 64. Hansen, Paul L.; Chadde, Steve W.; Pfister, Robert D. 1988. Riparian dominance types of Montana. Misc. Publ. No. 49. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station. 411 p. [5660]
  • 73. Hermanutz, L. A.; Innes, D. J.; Weis, I. M. 1989. Clonal structure of arctic dwarf birch (Betula glandulosa) at its northern limit. American Journal of Botany. 76(5): 755-761. [7346]
  • 104. Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L. 2004. Shrubs of other families. In: Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L., comps. Restoring western ranges and wildlands. Gen. Tech. Rep. RMRS-GTR-136-vol-2. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 598-698. [52846]
  • 106. Morin, Hubert; Payette, Serge. 1988. Buried seed populations in the montane, subalpine, and alpine belts of Mont Jacques-Cartier, Quebec. Canadian Journal of Botany. 66: 101-107. [6376]
  • 108. Nichols, G. E. 1934. The influence of exposure to winter temperatures upon seed germination in various native American plants. Ecology. 15(4): 364-373. [55167]
  • 124. Rowe, J. S. 1983. Concepts of fire effects on plant individuals and species. In: Wein, Ross W.; MacLean, David A., eds. The role of fire in northern circumpolar ecosystems. SCOPE 18. New York: John Wiley & Sons: 135-154. [2038]
  • 166. Weis, I. M.; Hermanutz, L. A. 1988. The population biology of the arctic dwarf birch, Betula glandulosa: seed rain and the germinable seed bank. Canadian Journal of Botany. 66(10): 2055-2061. [7347]
  • 167. Weis, I. M.; Hermanutz, L. A. 1993. Pollination dynamics of arctic dwarf birch (Betula glandulosa; Betulaceae) and its role in the loss of seed production. American Journal of Botany. 80(9): 1021-1027. [66001]

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Growth Form (according to Raunkiær Life-form classification)

More info on this topic.

More info for the terms: chamaephyte, phanerophyte

RAUNKIAER [119] LIFE FORM:
Phanerophyte
Chamaephyte
  • 119. Raunkiaer, C. 1934. The life forms of plants and statistical plant geography. Oxford: Clarendon Press. 632 p. [2843]

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Life Form

More info for the term: shrub

Shrub

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Life History and Behavior

Cyclicity

Phenology

More info on this topic.

More info for the term: bog

In bog birch, leaf growth begins soon after snow melt, and growth continues throughout the growing season as shoots elongate [41]. Male catkins develop in late summer or fall and expand with or before leaf development the following spring. Female catkins appear with the leaves in the spring [78,104]. Flowering dates vary and are summarized below.

Flowering dates for bog birch by region
Alaska May-June [159]
Sierra Nevada, California April-June [79]
Gaspé Peninsula, Quebec June-August [106]

Fruits mature between July and October and can persist through the winter [104,106,159,166]. Samara dispersal occurs in the fall, just prior to snow fall, and in the following spring soon after snow melt [78,166]. Leaves begin to senesce in late summer, and leaf abscission is complete by late September [118].

Phenological stages for bog birch in a valley-bottom floodplain in west-central Alberta are summarized below.

Seasonal development of bog birch in west-central Alberta [44]
5 May most plants initiating leaf-break
10 June male catkins dropped; female catkins small and turning darker green
29 June female catkins at mature size
11 Aug. female catkins brown; terminal buds large
1 Sept. half of leaves on most plants yellow
  • 41. de Groot, W. J.; Thomas, P. A.; Wein, Ross W. 1997. Biological flora of the British Isles: No. 194. Betula nana L. and Betula glandulosa Michx. Journal of Ecology. 85(2): 241-264. [65929]
  • 44. de Groot, William J.; Wein, Ross W. 2004. Effects of fire severity and season of burn on Betula glandulosa growth dynamics. International Journal of Wildland Fire. 13: 287-295. [51228]
  • 104. Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L. 2004. Shrubs of other families. In: Monsen, Stephen B.; Stevens, Richard; Shaw, Nancy L., comps. Restoring western ranges and wildlands. Gen. Tech. Rep. RMRS-GTR-136-vol-2. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 598-698. [52846]
  • 106. Morin, Hubert; Payette, Serge. 1988. Buried seed populations in the montane, subalpine, and alpine belts of Mont Jacques-Cartier, Quebec. Canadian Journal of Botany. 66: 101-107. [6376]
  • 118. Prudhomme, Thomas I. 1983. Carbon allocation to antiherbivore compounds in a deciduous and an evergreen arctic shrub species. Oikos. 40(3): 344-356. [65946]
  • 159. Viereck, Leslie A.; Little, Elbert L., Jr. 1972. Alaska trees and shrubs. Agric. Handb. 410. Washington, DC: U.S. Department of Agriculture, Forest Service. 265 p. [6884]
  • 166. Weis, I. M.; Hermanutz, L. A. 1988. The population biology of the arctic dwarf birch, Betula glandulosa: seed rain and the germinable seed bank. Canadian Journal of Botany. 66(10): 2055-2061. [7347]
  • 79. Kartesz, John Thomas. 1988. A flora of Nevada. Reno, NV: University of Nevada. 1729 p. [In 2 volumes]. Dissertation. [42426]
  • 78. Karrfalt, Robert P. [In press]. Betula L.--birch, [Online]. In: Bonner, Franklin T.; Nisley, Rebecca G.; Karrfait, R. P., coords. Woody plant seed manual. Agric. Handbook 727. Washington, DC: U.S. Department of Agriculture, Forest Service (Producer). Available: http://www.nsl.fs.fed.us/wpsm/Betula.pdf [2007, August 22]. [67844]

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Flowering/Fruiting

Flowering late spring.
Creative Commons Attribution Non Commercial Share Alike 3.0 (CC BY-NC-SA 3.0)

© Missouri Botanical Garden, 4344 Shaw Boulevard, St. Louis, MO, 63110 USA

Source: Missouri Botanical Garden

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Molecular Biology and Genetics

Molecular Biology

Statistics of barcoding coverage: Betula glandulosa

Barcode of Life Data Systems (BOLDS) Stats
Public Records: 14
Specimens with Barcodes: 28
Species With Barcodes: 1
Creative Commons Attribution 3.0 (CC BY 3.0)

© Barcode of Life Data Systems

Source: Barcode of Life Data Systems (BOLD)

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Conservation

Conservation Status

Information on state-level protected status of plants in the United States is available at Plants Database.

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Management

Management considerations

More info for the terms: bog, cover

Bog birch decreases with grazing. Bog birch cover was significantly (P=0.01) greater on ungrazed
sites (88%) than on grazed sites (47%) within the summer range of the
Rivière George caribou herd in
northern Quebec and Labrador, Canada. Browsing and
trampling by caribou have opened the closed canopy of bog birch and reduced leaf
biomass by 60% [99]. Bog birch plants heavily browsed by snowshoe hares near Kluane, Yukon,
exhibited rapid growth of new twigs when hare numbers declined [136].

Expanding bog birch populations
on Canadian Rocky Mountain rangelands reduce forage for elk, bison, and
other grazing animals. Removal of bog
birch increases the production of forage grasses [43].
Information on the effects of herbicides on bog birch is available in Chapin and others [14].
  • 43. de Groot, William J. 1998. Fire ecology of Betula glandulosa Michx. Edmonton, AB: University of Alberta. 203 p. Dissertation. [66522]
  • 14. Balfour, Patty M. 1989. Effects of forest herbicides on some important wildlife forage species. Victoria, BC: British Columbia Ministry of Forests, Research Branch. 58 p. [12148]
  • 99. Manseau, M.; Huot, J.; Crete, M. 1996. Effects of summer grazing by caribou on composition and productivity of vegetation: community and landscape level. Journal of Ecology. 84: 503-513. [26980]
  • 136. Smith, J. N. M.; Krebs, C. J.; Sinclair, A. R. E.; Boonstra, R. 1988. Population biology of snowshoe hares. II. Interactions with winter food plants. Journal of Animal Ecology. 57: 269-286. [6713]

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Relevance to Humans and Ecosystems

Benefits

Value for rehabilitation of disturbed sites

More info for the terms: bog, shrubs

The erosion control potential for bog birch is high. In Montana, the dense underground network formed by bog birch and rhizomatous sedges help stabilize streambanks [28]. Because bog birch grows slowly, its short-term (1-3 years) revegetation potential is low. Bog birch is, however, suitable for long-term (>3 years) revegetation of exposed mineral soil [28,101].

Black spruce seedling survival after fire in the boreal forest may be facilitated by shading from bog birch and other shrubs that reproduce vegetatively and grow quickly [134].

  • 28. Boggs, Keith; Hansen, Paul; Pfister, Robert; Joy, John. 1990. Classification and management of riparian and wetland sites in northwestern Montana. Draft Version 1. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station, Montana Riparian Association. 217 p. [8447]
  • 101. Maslen, Lynn; Kershaw, G. Peter. 1989. First year results of revegetation trials using selected native plant species on a simulated pipeline trench, Fort Norman, N.W.T., Canada. In: Walker, D. G.; Powter, C. B.; Pole, M. W., compilers. Reclamation, a global perspective: Proceedings of the conference; 1989 August 27-31; Calgary, AB. Rep. No. RRTAC 89-2. Vol. 1. Edmonton, AB: Alberta Land Conservation and Reclamation Council: 81-90. [14363]
  • 134. Sirois, Luc; Payette, Serge. 1991. Reduced postfire tree regeneration along a boreal forest - forest tundra transect in northern Quebec. Ecology. 72(2): 619-627. [13954]

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Importance to Livestock and Wildlife

More info for the terms: bog, cover

Bog birch is only lightly to moderately browsed by most classes of livestock [19,107]. It accounted for 2.7% of summer cattle forage, for example, on the Red Rock Lakes National Wildlife Refuge in Montana [47]. Browse production may be moderate to high in some bog birch communities. However, cattle tend to avoid the boggy soils associated with this species unless the soil becomes dry enough to walk on, usually in late summer [40,64,86,104]. Cattle eat bog birch in riparian wet meadows in the southern Blue Mountains, Oregon [120].

Numerous wildlife species eat bog birch, including moose, mule deer, white-tailed deer, Rocky Mountain elk, mountain goats, caribou, grizzly bears, American black bears, small mammals, birds, and insects [14,68,74,81,91,109,126,146,159]. Bog birch is a "preferred" browse species for game animals in Teton County, Wyoming [18]. It is dominant in tamarack swamps in southwestern Manitoba. These swamps provide habitat for moose, jumping mice, northern river otters, shrews, Canada jays, black-capped chickadees, white-throated sparrows, and Connecticut warblers [22].

Moose: Bog birch accounted for 11.8% of summer and 0.7% of winter moose forage on the Red Rock Lakes National Wildlife Refuge [47]. It is preferred browse in Banff and Jasper National Parks, Alberta [53], but is not preferred by moose in Alaska [30].

Caribou: Buds, leaves, and sprouts of bog birch are preferred foods for caribou in Alaska in the spring and early summer. The rumens of 6 caribou examined in mid-June contained almost exclusively bog birch. Caribou eat the leaves extensively into June and July, but by mid-September the leaves are less palatable than willow (Salix spp.) leaves [135,159]. Caribou also eat bog birch in summer and winter in northern Canada [20,36,72,128]. Heavy browsing by the Rivière George caribou herd in northern Quebec depleted winter carbohydrate reserves in bog birch, leading to decreased bog birch growth in spring [36].

Birds: Several species of ptarmigan and grouse eat bog birch in Alaska, Canada, and the contiguous northern United States [107,159]. Sharp-tailed grouse and greater prairie-chickens eat bog birch buds in Wisconsin in the winter [127], and spruce grouse eat bog birch seeds in central Alaska [163]. Bog birch and dwarf birch buds and catkins comprised 11% of the food in rock ptarmigan crops in Alaska in spring, 12% in summer, 45% in fall, and 79% in winter. For willow ptarmigan the 2 birches comprised 0% of food in crops in spring, 3% in summer, 4% in fall, and 12% in winter [163].

Small mammals: American beavers eat bog birch [109]. Bog birch is a preferred winter food of snowshoe hares in the southwestern Yukon [39,88,122,136]. Eastern heather voles eat bog birch bark in the winter in Canada [57]. White spruce/bog birch communities in the Kluane Region, Yukon, provide habitat for a number of small mammals including deer mice, northern red-backed voles, meadow voles, and heather voles [89].

Fish: Bog birch provides overhanging shade and cover for fish along low-gradient streams in western Montana [28].

Insects: Insect herbivores can cause "moderate" damage to bog birch. During the 1976 to 1980 growing seasons, bog birch plants in northern Quebec lost 20% to 50% of leaf biomass to insects [118]. In Alaska, the total number of herbivorous insects decreased with increases in latitude and altitude and distance from the white spruce forest zone. More detailed information on insects found on bog birch foliage is available [85].

Bog birch importance rankings for 9 ungulate species in British Columbia are provided below.

Importance of bog birch in the diets of ungulates in British Columbia [27]
Sitka black-tailed deer low
mule deer low
white-tailed deer low
mountain goat low
bighorn sheep low
Roosevelt elk low
Rocky Mountain elk moderate
moose high
caribou moderate

Palatability/nutritional value: The palatability of bog birch in several states is as follows

Palatability of bog birch for livestock and wildlife [28,38,46,67,125]:
  California Colorado Montana Wisconsin Wyoming
cattle poor fair poor ---* fair
domestic sheep fair-poor fair fair --- fair
horses poor poor poor --- fair
white-tailed deer --- --- poor --- ---
mule deer --- --- poor --- ---
moose --- --- -- --- high
elk --- --- poor --- ---
pronghorn --- --- poor --- ---
rabbits --- --- --- high ---
* No data available.

The energy and protein values of bog birch are low [28]. Sugar content in bog birch leaves declines in late summer. Nitrogen concentration in leaves peaks early in spring then declines throughout the growing season [118]. Nutritive values measured in bog birch plants near Inuvik, Northwest Territories, are given in the table below [129,130].

Nutritive values in bog birch twigs and leaves [129,130]
Plant part Month Cu Mo Fe Mn Zn K Mg Ca P crude fat crude fiber crude protein
    ppm %
twigs July 2.8 0.23 50 157 87 0.70 0.20 0.34 0.08 8.9 26.1 3.5
twigs Aug. 4.6 0.21 161 67 178 0.21 0.10 0.41 0.09 10.7 27.4 5.4
twigs Nov. 3.7 0.31 332 121 206 0.09 0.11 0.62 0.06 4.9 33.7 4.2
twigs Feb. 4.6 0.21 205 78 160 0.18 0.10 0.47 0.06 9.3 30.6 4.9
twigs May 4.7 0.23 102 92 152 0.23 0.10 0.47 0.09 9.8 28.5 6.0
leaves May 4.4 0.21 83 151 108 0.66 0.34 ---* --- --- --- ---
leaves July --- --- --- --- --- --- --- 0.44 0.13 7.3 12.7 10.4
leaves Aug. --- --- --- --- --- --- --- 0.63 0.15 7.9 15.8 12.1

* No data available.

Bog birch produces carbon and nitrogen-based antiherbivore compounds that deter browsing [41]. Sugar and nitrogen content is highest in the leaves in early spring. Bog birch allocates the greatest portion of its photosynthate to the production of antiherbivore phenolics at that time; otherwise, leaves would be susceptible to browsing insects [118].

Cover value: The table below summarizes thermal or feeding cover values of bog birch.

Cover values of bog birch for wildlife in 3 western states [28,46]
  Colorado Montana Wyoming
elk good poor poor
mule deer poor poor poor
white-tailed deer ---* poor poor
upland game birds good fair fair
waterfowl   good poor
small nongame birds good fair good
small mammals good fair good
* No data available.

Bog birch provides cover for willow, rock, and white-tailed ptarmigan in southwestern Yukon [115]. Grizzly bears in the central Canadian Arctic constructed their dens under bog birch cover more than any other plant species. Bog birch was present at 84% of 52 den sites, and it was the highest in percent cover around den entrances. Bog birch roots formed ceilings of several dens studied [102].

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Wikipedia

Betula glandulosa

Betula glandulosa, American Dwarf Birch, also known as Resin Birch or Shrub Birch, is a species of birch native to North America, occurring in arctic and cool temperate areas from Alaska east to Newfoundland and southern Greenland, and south at high altitudes to northern California and Colorado in the west, and locally south to northern New York in the east. In the Arctic it occurs down to sea level, while in the south of the range, it grows as high as 3400 m altitude.

American Dwarf Birch is a multi-stemmed shrub typically growing to 1-3 m tall, often forming dense thickets. The trunks are slender, rarely over 5-10 cm diameter, with smooth, dark brown bark. The leaves are nearly circular to oval, 0.5-3 cm long and 1.2.5 cm broad, with a toothed margin. The fruiting catkins are erect, 1-2.5 cm long and 5-12 mm broad.

It is closely related to the Dwarf Birch (Betula nana), and is sometimes treated as a subspecies of it, as B. nana subsp. glandulosa. It is distinguished from typical B. nana by the presence of glandular warts on the shoots and longer leaf petioles. Hybrids with several other birches occur.

References[edit]

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Comments

Betula glandulosa is the characteristic dwarf birch of upland habitats throughout much of the mountainous west, occurring as well in dry open areas across the north. Where their ranges meet, B . glandulosa intergrades with both B . pumila Linnaeus and B . nana Linnaeus subsp. exilis (Sukaczev) Hultén, creating a confusing complex of intermediate forms. In the east, it reaches its southernmost limit on the subalpine slopes of high Adirondack peaks, including Mt. Washington, where it forms low sprawling thickets and scrubs. 

 Specimens of Betula glandulosa have been reported from the St. Lawrence Valley, but I have not seen them.

Wherever Betula glandulosa comes in contact with B . pumila , it forms a bewildering swarm of plants, known as B . × sargentii Dugle, having intermediate states of most vegetative characters.

Plants intermediate between Betula glandulosa and B . nana subsp. exilis make up a continuum of forms linking the typical forms of Betula nana and B . glandulosa in parts of Alaska where the ranges of these species overlap. Wherever they occur in isolation, the species remain reasonably distinct and easy to identify. In southern Greenland, Betula glandulosa hybridizes with B . nana subsp. nana and with B . pubescens .

Betula × eastwoodiae Sargent (= B . glandulosa × occidentalis ) occurs in montane meadows and marshes in Alberta, British Columbia, Northwest Territories, Saskatchewan, Yukon, Alaska, Colorado, and Wyoming, where the range of the parents overlap.

Betula × dugleana Lepage (= Betula glandulosa Michaux × B . neoalaskana Sargent) is common throughout Alaska and the Yukon, where the parent species frequently come into contact (E. Hultén 1941--1950, vol. 4; E. Lepage 1976).

Betula × dutillyi Lepage [= Betula glandulosa Michaux × B . minor (Tuckerman) Fernald] is a putative hybrid that occupies the same general range as Betula minor . Like that species, however, it has not been studied experimentally. Careful examination of the entire complex to which this taxon belongs will be necessary before any of its parts can be truly understood. Betula × dutillyi exhibits many of the same characteristics as B . minor , but it is slightly smaller in habit, and its leaves are smaller with somewhat blunter tips and more cuneate bases (E. Lepage 1976).

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Names and Taxonomy

Taxonomy

More info for the term: bog

The scientific name of bog birch is Betula glandulosa
Michx. (Betulaceae) [31,54,60,61,75,76,77,137,159,168].

Bog birch hybridizes with dwarf birch (Betula nana subsp. exilis and
Betula nana subsp. nana) where
their ranges overlap [54,77,159]. Bog birch
also hybridizes with paper birch (Betula papyrifera) in interior Alaska [159].
Numerous other hybrids have been described including:



Betula × sargentii Dugle (B. nana × B. pumila)

Betula × eastwoodiae Sargent (B. nana × B. occidentalis) [31,51,54]

Betula × dugleana Lepage (B. nana × B. neoalaskana)

Betula × dutillyi Lepage (B. nana × B. minor, a
putative hybrid) [54]

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Common Names

bog birch

dwarf birch

glandular birch

resin birch

scrub birch

swamp birch

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