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Introductory

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
ABBREVIATION : CLASPP SYNONYMS : Cladonia alpestris = C. stellaris Cladonia arbuscula = C. sylvatica SCS PLANT CODE : NO-ENTRY COMMON NAMES : reindeer lichen lichen reindeer moss lichen caribou lichen TAXONOMY : The most widely accepted genus name for reindeer lichens is Cladonia Wigg. (subgenus Cladina (Nyl.) Vain) [13,35,40]. The characters derived from the mycobiont (the fungal member of a lichen) have been given most weight in the recognition of orders, families, and genera of lichen. The characters used to separate these categories are now almost exclusively mycological, but genera largely based on such features have not found general acceptance [13]. Some authorities separate the reindeer lichens into the genus Cladina, while others refer to it as subgenus Cladina of the genus Cladonia [40]. In this report taxonomy will follow the latter, with emphasis on the four species of reindeer lichens listed below: Cladonia alpestris (L.) Rabenh. Cladonia arbuscula (Wallr.) Rabenh. Cladonia rangiferina (L.) Nyl Cladonia mitis Sandst. LIFE FORM : Lichen FEDERAL LEGAL STATUS : See OTHER STATUS OTHER STATUS : Cladonia perforata is federally listed as endangered [45]. COMPILED BY AND DATE : Julie L. Tesky, August 1992. LAST REVISED BY AND DATE : NO-ENTRY AUTHORSHIP AND CITATION : Tesky, Julie L. 1992. Cladonia spp. In: Remainder of Citation

DISTRIBUTION AND OCCURRENCE

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
GENERAL DISTRIBUTION : Reindeer lichens have a circumpolar distribution. In North America, they occur throughout Alaska, Canada, and the northern United States southward to Florida and Alabama [11,19]. National Park occurrences are listed below by species. Cladonia alpestris ACAD APOS BELA CAKR DENA DETO DEWA GAAR GATE GLAC GRSO HOSP INDU ISRO KATM KOVA OLYM PIRO SACR SHEN SLBE THRO VOYA YELL Clandonia arbuscula ACAD APIS BELA CAKR DENA DEWA GAAR GLAC GRSM ILMI ISRO OLYM PIRO VOYA YELL YUCH Cladonia rangiferina ACAD APIS BELA CAKR CUVA DENA DEWA GAAR GRSM INDU ISRO KOVA MORA NOAT NOCA OLMY PIRO SACR SARA SHEN SLBE THRO VOYA YELL YUCH Cladonia mitis ACAD APIS CAKR GAAR GLAC GRSM INDU ISRO KATM OLYM PIRO SACR SLBE THRO VOYA YELL ECOSYSTEMS : FRES10 White - red - jack pine FRES11 Spruce - fir FRES18 Maple - beech - birch FRES19 Aspen - birch FRES20 Douglas-fir FRES22 Western white pine FRES23 Fir - spruce FRES24 Hemlock - Sitka spruce FRES25 Larch FRES26 Lodgepole pine FRES28 Western hardwoods FRES44 Alpine STATES : AL AK AR CA CO CT DE FL GA ID IL IA MD ME MI MN MT NH NJ NY NC ND OR PA RI SC SD UT VT VA WA WI WY AB BC MB NB NF NT NS ON PE PQ SK YT ADMINISTRATIVE UNITS : SEE GENERAL DISTRIBUTION BLM PHYSIOGRAPHIC REGIONS : 1 Northern Pacific Border 2 Cascade Mountains 3 Southern Pacific Border 4 Sierra Mountains 5 Columbia Plateau 6 Upper Basin and Range 8 Northern Rocky Mountains 9 Middle Rocky Mountains 10 Wyoming Basin 11 Southern Rocky Mountains 13 Rocky Mountain Piedmont 15 Black Hills Uplift 16 Upper Missouri Basin and Broken Lands KUCHLER PLANT ASSOCIATIONS : K001 Spruce - cedar - hemlock forest K002 Cedar - hemlock - Douglas-fir forest K003 Silver fir - Douglas-fir forest K004 Fir - hemlock forest K005 Mixed conifer forest K008 Lodgepole pine - subalpine forest K013 Cedar - hemlock - pine forest K014 Grand fir - Douglas-fir forest K015 Western spruce - fir forest K020 Spruce - fir - Douglas-fir forest K021 Southwestern spruce - fir forest K093 Great Lakes spruce - fir forest K094 Conifer bog K095 Great Lakes pine forest K096 Northeastern spruce - fir forest K097 Southeastern spruce - fir forest K106 Northern hardwoods K017 Black Hills pine forest K108 Northern hardwoods - spruce forest K109 Transition between K104 and K106 K110 Northeastern oak - pine forest K111 Oak - hickory - pine forest SAF COVER TYPES : 1 Jack pine 5 Balsam fir 12 Black spruce 13 Black spruce - tamarack 18 Paper birch 30 Red spruce - yellow birch 31 Red spruce - sugar maple - beech 32 Red spruce 33 Red spruce - balsam fir 34 Red spruce - Fraser fir 35 Paper birch - red spruce - balsam fir 37 Northern white-cedar 38 Tamarack 107 White spruce 201 White spruce 202 White spruce - paper birch 203 Balsam poplar 204 Black spruce 205 Mountain hemlock 206 Engelmann spruce - subalpine fir 251 White spruce - aspen 252 Paper birch 253 Black spruce - white spruce 254 Black spruce - paper birch SRM (RANGELAND) COVER TYPES : NO-ENTRY HABITAT TYPES AND PLANT COMMUNITIES : Reindeer lichens commonly occur as the dominant or codominant ground cover on open sites dominanted by white spruce (Picea glauca), black spruce (P. mariana), paper birch (Betula papyrifera), or jack pine (Pinus banksiana). The white spruce/Sphagnum spp.-Cladonia spp. community type described by Foote [12] is characterized by woodland or open forests often occurring on valley bottoms or on north-facing slopes where ice-rich permafrost is present. In this community type, Cladonia rangiferina and C. arbuscula grow intermixed with Sphagnum spp., Schreber's moss (Pleurozium schreberi), and Polytrichum spp. [12]. The black spruce/bog birch (Betula glandulosa)/Cladonia community type decribed by Viereck [39] is fairly common on well-drained sites and near treeline in interior, southwest, and northwest Alaska. Published classification schemes identifying Cladonia spp. as ground cover dominants or codominants are as follows: Classification, description and dynamics of plant communities following fire in the taiga of interior Alaska [12]. A preliminary classification system for vegetation of Alaska [39].

VALUE AND USE

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
WOOD PRODUCTS VALUE : NO-ENTRY IMPORTANCE TO LIVESTOCK AND WILDLIFE : Terrestrial lichens are important in the winter diet of caribou. In the forest zones of Ontario, the winter diet of caribou is made up almost exclusively of reindeer lichens [2]. In some places these lichens constitute over 50 percent of the caribou diet [2,21]. The winter diet of Newfoundland caribou is made up mostly of Cladonia mitis and C. rangiferina and to a lesser extent C. alpestris. Within the range of the Newfoundland caribou C. mitis seems to be the most important food-lichen. In Norway reindeer seem to prefer pastures with plenty of C. rangiferina to those with plenty of C. alpestris [41]. Reindeer lichens are also eaten by caribou throughout the summmer, although to a lesser extent [2]. PALATABILITY : Reindeer lichens are highly palatable to both barren ground and woodland caribou [2]. Cladonia rangiferina contains bitter fumarprotocetraric acid while C. alpestris and C. mitis do not contain this acid. It is questionable whether this difference in reindeer lichens affects their palatability to reindeer [41]. NUTRITIONAL VALUE : The nutritive value of reindeer lichens is rather poor. The protein content, calcium and phosphorous levels, and vitamin content are very low. The calcium/phosphorous ratio is rated as poor [2,34]. The crude fat in reindeer lichens is mainly lichen acids, which are largely indigestible. However, the nitrogen-free extract of these lichens is thought to be highly digestible. Crude fiber content is high. Reindeer lichens are high in digestible carbohydrates, mostly in the form of complex starches, and therefore are a good source of energy [17,34]. Ahti [2] listed the percent chemical composition of Cladonia species as follows: Carbohyrates= 93.4 to 94.4 percent minerals= 1.1 to 1.5 percent protein= 2.6 to 2.9 percent fat= 1.8 to 2.2 percent Although caribou can survive the winter on an exclusive reindeer lichen diet, the deficiency of protein usually results in a sharp decrease in body weight as the animal breaks down its own muscular tissue to compensate for the protein deficiency [30,34]. Caribou appear to be able to balance the low protein content of the reindeer lichens by including in their diet a portion of the nitrogen-fixing lichens of the genera Stereocaulon and Peltigera which have relatively high protein contents [18]. Additionally, caribou can digest reindeer lichens more efficently than other ruminants can [17]. The crude fiber is broken down by rumen bacteria and protozoa which liberate large amounts of energy [34]. COVER VALUE : NO-ENTRY VALUE FOR REHABILITATION OF DISTURBED SITES : NO-ENTRY OTHER USES AND VALUES : NO-ENTRY MANAGEMENT CONSIDERATIONS : Reindeer lichen growth is so slow that it should not be regrazed by caribou for 2 to 5 years if the grazing is moderate, or 10 to 15 years if the grazing is intense. Under intense grazing the ground may be almost totally depleted of reindeer lichens, with only the basal part of the podetia (upright growing branches) remaining [30]. At the Taltson River Region in the Northwest Territories, Cladonia alpestris had an average annual growth rate of 0.11 inch (3.4 mm) per year while C. rangiferina had an average annual growth rate of 0.14 inch (4.1 mm) per year [31]. C. alpestris has many lateral branches compared with C. rangiferina or C. mitis, and could produce more forage annually even though the annual linear growth rate may be less [25]. C. alpestris, however, can not withstand heavy grazing and trampling. Therefore, it can be the main reindeer lichen food only in areas with a comparatively small caribou population [41]. High relative humidity is especially important for reindeer lichens. Studies have shown that a 9-month fully dry period is lethal to Cladonia rangiferina, but under natural conditions much shorter periods are critical [2].

BOTANICAL AND ECOLOGICAL CHARACTERISTICS

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
GENERAL BOTANICAL CHARACTERISTICS : Reindeer lichens are slow-growing, long-lived, densely branched ground lichens with short numerous outer branchelets [2]. These lichens often form clumps or mats composed of a large number of podetia [30]. The podetia are slender, elongated, and branched in whorls. They are often densely intertangled in large colonies [30]. The slender thalli of Cladonia rangiferina are hollow stems of very low density which are finely branched and not only have a high surface to volume ratio, but also have branches advantageously distributed to carry fire [28]. RAUNKIAER LIFE FORM : NO-ENTRY REGENERATION PROCESSES : The dispersal of reindeer lichens mainly occurs by means of thallus fragments and to a much smaller extent by ascopores. Wind is the most important dispersal agent. Reindeer lichens grow vegetatively by annually producing new growth at the top of the podetium, which lengthens the internode formed in previous years [2]. The podetium of Cladonia spp. passes through three growth stages. The first stage, called the growth-accumulation period, lasts an average of 10 years but can vary from 5 to 25 years. During this stage no part of the podetium dies off. During the second stage, called the growth-renewal period, the podetium grows at its highest rate but dies off at the base at a rate equal to the growth. This stage often exceeds 100 years. During the third stage, the podetium degeneration period, the podetium dies off at a greater rate than it grows. This stage may also exceed 100 years. Factors that probably contribute to variation in lichen growth include: the age of the podetium; prior disturbance by animals; and site conditions such as substrate, drainage, and exposure [25]. SITE CHARACTERISTICS : Reindeer lichens typically occur in submontane to alpine environments. They are scattered to plentiful in the open or in open-canopy forest and tundra on well-drained, water-shedding sites with shallow and/or coarse-skelatal soils. In these environments they often occur on soil and sometimes on rocks, stumps, and logs [19]. Cladonia arbuscula and C. mitis are the most competitive reindeer lichens on rock [2]. Northern boreal forests offer climatically optimal conditions for reindeer lichen growth largely because of slow plant succession and little competition from other plant forms. Dry reindeer lichen woodlands and lichen bogs are characteristic throughout the northern boreal forest belt [2]. On the Slate Islands of Lake Superior, Ontario, reindeer mosses grow best on dry open sites. Here, they occur more than twice as frequently in dry regime forest types than in moist regime forest types of the same composition and are more than ten times as abundant in the dry types [8]. Cladonia rangiferina has a wider ecological amplitude than other reindeer lichens and is thus more common than the others in less favorable habitats such as wet bogs and shaded woods. It is very common all over northern Ontario, being the most widely distributed ground lichen in the area. Even in the Cladonia alpestris stands of the northern boreal forest it is considerably more plentiful than C. mitis or C. arbuscula [2]. Cladonia arbuscula prefers a moister and more shaded habitat than most reindeer lichens but is frequently found mixed with C. mitis. C. mitis is commonly one of the dominants on rocks, in lichen woodlands, and on dry bog hummocks [2]. Soils and climate: Reindeer lichens commonly occur on moist to very dry, sandy, nitrogen-poor soils [19] on shallow humus layers or dry peat [2]. They are adapted to a cool, moist climate. Most reindeer lichens avoid calcareous soils and prefer the acid humus of podzolic soils during germination [32]. Reindeer lichens have been found on sites with pH values ranging between 4.5 and 5.5 [32]. Since reindeer lichens are able to take up moisture from the air, the underlying soil is not as important a source of moisture as it is to vascular plants. Reindeer lichens, therefore, can colonize and become a dominant floral element on soils too shallow or sterile to support higher plants, provided that humidity is sufficently high for lichen growth and temperature is sufficently low to inhibit competitors [2]. Plant associates: Reindeer lichens are commonly found associated with the following species: whortleberry (Vaccinium myrtillus), rock cranberry (V. vitris-idaea), bog blueberry (V. uliginosum), lowbush blueberry (V. angustifolium), bog birch, sheep laurel (Kalmia angustifolia), common bearberry (Arctostaphylos uva-ursi), black crowberry (Empetrum nigrum), Stereocaulon paschale, and Schreber's moss (Pleurozium schreberi) [6,7,29]. SUCCESSIONAL STATUS : Facultative Seral Species (C. mitis) Obligate Climax Species (C. alpestris, C. arbuscula, C. rangiferina) Reindeer lichens are shade intolerant [19]. Cladonia mitis is an early to mid-seral species, while C. alpestris, C. arbuscula, and C. rangiferina are late-seral to climax species [25]. C. mitis is generally the first reindeer lichen to become established in postfire succession of white spruce and black spruce stands. This lichen dominates for 30 to 40 years and is then replaced by other reindeer lichens such as C. alpestris and C. rangiferia. If the canopy becomes closed, reindeer lichens are generally replaced by the shade-tolerant mosses such as mountain fern moss (Hylocomium splendens) and Schreber's moss [2]. SEASONAL DEVELOPMENT : NO-ENTRY

FIRE ECOLOGY

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
FIRE ECOLOGY OR ADAPTATIONS : Reindeer lichens are not well adapted to fire. They are highly flammable and may take 30 to 100 years or more to recover to prefire densities [32]. POSTFIRE REGENERATION STRATEGY : NO-ENTRY

FIRE EFFECTS

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
IMMEDIATE FIRE EFFECT ON PLANT : Reindeer lichens can survive cool fires but are almost always killed by severe fire [16,26,40]. In the black spruce zone, lichens generally burn poorly in early morning or near sunset, even on hot days, whereas at mid-day they flare up with almost incredible heat and flame. Humidity changes in the microclimate at ground level and dehydration of the lichens appear to be the most likely factors involved. Fifty percent or more of the lichens may survive if there is not much organic litter to retain the fire [16]. Following fire in a black spruce community, all the Cladonia spp. survived a light burn, whereas none survived a heavy burn [38]. DISCUSSION AND QUALIFICATION OF FIRE EFFECT : PLANT RESPONSE TO FIRE : Reindeer lichens recover very slowly after fire [22]. The length of time required for full recovery varies with species, the extent and intensity of the fires, and site and microclimatic condition, but an average of 40 to 50 years appears to be a conservative estimate [22,40]. Based on annual growth rates of 0.14 and 0.16 inch (4.1 and 4.9 mm) for C. alpestris and C. rangiferina, it has been estimated that these species would require nearly a century to reach prefire abundance [21]. After fire the first reindeer lichen to become established is Cladonia mitis. The second reindeer lichen phase is generally dominated by C. alpestris, C. rangiferina, or C. arbuscula [22,40]. DISCUSSION AND QUALIFICATION OF PLANT RESPONSE : One hundred forty years after a severe wildfire in Sweden, Cladonia alpestris still showed no recovery, but did show good recovery only 20 years after a light, controlled burn. Slow recovery rates were reported from the Seward Peninsula of Alaska, while rapid recovery rates have been reported from the open lichen woodlands of Newfoundland, where the climate is warmer than in Alaska [40]. In a black spruce and jack pine woodland in northwestern Manitoba and northeastern Saskatchewan, Cladonia mitis became established in less than 40 years after fire, while C. alpestris and C. rangiferina first appeared in stands greater than 40 years of age. A dense growth of reindeer lichens was found in stands that had not burned for at least 150 years. In south-central Alaska it took 30 to 40 years for C. rangiferina and C. arbuscula to recover after fire [25]. In a postfire black spruce-lichen vegetation type of interior Alaska, cover values for Cladonia species were 32 percent in 26- 50-year-old stands, and 41 percent in stands greater than 100 years [25]. In a lightly burned 75-year-old stand with a open canopy of spruce and occasional jack pine, C. alpestris made up 32.8 percent of the total ground cover and C. rangiferina made up 1.7 percent [16]. FIRE MANAGEMENT CONSIDERATIONS : Reindeer lichens are highly flammable. Cladonia rangiferina collected from Ely, Minnesota, and ovendried had a heat value of 4,360 cal/g [15]. They dry rapidly during periods of low atmospheric humidity because of the absence of roots, water storage tissues, and low resistance to water loss. Reindeer lichens resemble dead litter more than live tissue in their susceptibility to fire. Continuous mats of reindeer lichen present an uninterrupted surface along which a fire spreads. Lichen mats also typically accumulate tree and shrub litter which adds to the flammability [3]. In black spruce-Cladonia alpestris woodland, litter suspended in the lichen mat added 20.5 percent dry weight to the total combustible material present above the soil [3]. While the destruction of reindeer lichens may have an immediate effect on the winter range of caribou, some studies indicate that at least infrequent fire is necessary to maintain optimum lichen cover [40]. In the northern boreal lichen belt, lichen supplies could be increased by burning Sphagnum fuscum peatlands, treeless bogs, or wooded muskegs. The result of severe fire is an almost solid reindeer lichen stand in some 40 to 50 years. Because black spruce and mosses regenerate more slowly than lichen on these sites, good lichen growth persists for at least 100 years [2]. Light burning has been suggested as a method to improve reindeer range in Scandinavia [40].

REFERENCES

SPECIES: Cladonia (Cladina) spp. | Reindeer Lichen
REFERENCES : 1. Ahmadjian, V.; Hale, M. E. 1973. The lichens. New York: Academic Press. 697 p. [18880] 2. Ahti, T.; Hepburn, T. L. 1967. Preliminary studies on woodland caribou range, especially on lichen stands, in Ontario. Res. Rep. (Wildlife) No. 74. Toronto, ON: Ontario Department of Lands and Forests, Research Branch. 134 p. [13294] 3. 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] 4. 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] 5. 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] 6. Carroll, S. B.; Bliss, L. C. 1982. Jack pine - lichen woodland on sandy soils in northern Saskatchewan and northeastern Alberta. Canadian Journal of Botany. 60: 2270-2282. [7283] 7. Chrosciewicz, Z. 1978. Slash and duff reduction by burning on clear-cut jack pine sites in central Saskatchewan. Information Report NOR-X-200. Edmonton, AB: Forestry Service, Fisheries and Environment Canada, Northern Forest Research Centre. 12 p. [7288] 8. Cringan, Alexander Thom. 1957. History, food habits and range requirements of the woodland caribou of continental North America. Transactions, North American Wildlife Conference. 22: 485-501. [15651] 9. Duncan, U. K. 1959. A guide to the study of lichens. Arbroath: T. Buncle & Co. Ltd., Printers & Publishers. 164 p. [18878] 10. Eyre, F. H., ed. 1980. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters. 148 p. [905] 11. Fink, B. 1935. The lichen flora of the United States. Ann Arbor, MI: University of Michigan Press. 426 p. [18877] 12. 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. [7080] 13. Hawksworth, D. L. 1984. The lichen-forming fungi. New York: Chapman & Hall. [18881] 14. Heatwole, H. 1966. Moisture exchange between atmosphere and some lichens of the genus Cladonia. Mycologia. 58: 148-156. [18882] 15. Hough, Walter A. 1969. Caloric value of some forest fuels of the southern United States. Res. Note SE-120. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station. 6 p. [10517] 16. Kelsall, John P. 1957. Continued barren-ground caribou studies. Wildlife Management Bulletin Series 1: No. 12. Ottawa, Canada: Department of Northern Affairs and National Resources, National Parks Branch, Canadian Wildlife Service. 148 p. [16597] 17. Klein, David. 1979. Wildfire, lichens and caribou. In: Hoefs, M.; Russell, D., eds. Wildlife and wildfire: Proceedings of workshop; 1979 November 27-28; Whitehorse, YT. Whitehorse, YT: Yukon Wildlife Branch: 37-65. [14074] 18. Klein, David R. 1982. Fire, lichens, and caribou. Journal of Range Management. 35(3): 390-395. [10898] 19. Klinka, K.; Krajina, V. J.; Ceska, A.; Scagel, A. M. 1989. Indicator plants of coastal British Columbia. Vancouver, BC: University of British Columbia Press. 288 p. [10703] 20. 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] 21. Loughrey, A. G.; Kelsall, J. P. 1970. The ecology and population dynamics of the barren-ground caribou in Canada. In: Proceedings, Helsinki symposium; 1966; [Location unknown]. [Place of publication unknown]: UNESCO: 275-280. On file with: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, Fire Sciences Laboratory, Missoula, MT. [17029] 22. Lutz, H. J. 1953. The effects of forest fires on the vegetation of interior Alaska. Juneau, AK: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 36 p. [7076] 23. Maikawa, E.; Kershaw, K. A. 1976. Studies on lichen-dominated systems. XIX. The postfire recovery sequence of black spruce-lichen woodland in the Abitau Lake region, N.W.T. Canadian Journal of Botany. 54: 2679-2687. [7225] 24. Mayfield, Harold. 1960. The Kirtland's warbler. Bulletin No. 40. Bloomfield Hills, MI: Cranbrook Institute of Science. 33 p. [16778] 25. Miller, Donald R. 1976. Taiga winter range relationships and diet. Canadian Wildlife Service Rep. Series No. 36. Ottawa, ON: Environment Canada, Wildlife Service. 42 p. (Biology of the Kaminuriak population of barren-ground caribou; pt 3). [13007] 26. Miller, Melanie; See, Marianne. 1981. Effects of fire on black spruce/lichen caribou range. Draft Research Proposal, Alaska BLM. On file at: U.S. Department of Agriculture, Forest Service, Intermountain Fire Sciences Laboratory, Missoula,.MT. 15 p. [15001] 27. Neiland, Bonita J. 1971. The forest-bog complex of southeast Alaska. Vegetatio. 22: 1-64. [8383] 28. Pech, Gyula. 1991. Dew on reindeer lichen. Canadian Journal of Forest Research. 21: 1415-1418. [16540] 29. Rencz, Andrew N.; Auclair, Allan N. D. 1978. Biomass distribution in a subarctic Picea mariana--Cladonia alpestris woodland. Canadian Journal of Forestry. 8: 168-176. [15867] 30. Richardson, D. H. S. 1974. The vanishing lichens. New York: Hafner Press (A division of MacMillan Publishing Co., Inc.). 231 p. [18876] 31. Scotter, G. W. 1963. Growth rates of Cladonia alpestris, C. mitis, and C. rangiferina in the Talston River region, N.W.T. Canadian Journal of Botany. 41: 1199-1202. [18879] 32. Scotter, George W. 1971. Fire, vegetation, soil, and barren-ground caribou relations in northern Canada. In: Slaughter, C. W.; Barney, Richard J.; Hansen, G. M., eds. Fire in the northern environment--a symposium: Proceedings of a symposium; 1971 April 13-14; Fairbanks, AK. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Range and Experiment Station: 209-230. [15730] 33. Scotter, George W. 1972. Fire as an ecological factor in boreal forest ecosystems of Canada. In: Fire in the environment: Symposium proceedings; 1972 May 1-5; Denver, CO. FS-276. [Ogden, UT]: U.S. Department of Agriculture, Forest Service, [Intermountain Forest and Range Experiment Station]: 15-25. [13404] 34. Scotter, George W. 1972. Chemical composition of forage plants from the Reindeer Preserve, Northwest Territories. Arctic. 25(1): 21-27. [16563] 35. Thomson, J. W. 1942. The lichen genus Cladonia in Wisconsin. American Midland Naturalist. 27: 696-709. [18883] 36. Viereck, Leslie A. 1979. Characteristics of treeline plant communities in Alaska. Holarctic Ecology. 2: 228-238. [8251] 37. 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] 38. 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] 39. 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] 40. Viereck, Leslie A.; Schandelmeier, Linda A. 1980. Effects of fire in Alaska and adjacent Canada--a literature review. BLM-Alaska Tech. Rep. 6. Anchorage, AK: U.S. Department of the Interior, Bureau of Land Mangement, Alaska State Office. 124 p. [7075] 41. Ahti, T. 1959. Studies on the caribou lichen stands of Newfoundland. Annals of the Botanical Society. Vanamo. 30(4): 1-44. [18901] 42. The Network of Natural Heritage Programs and Conservation Data Centers and The Nature Conservancy. 1994. Federally listed nonvascular plants. Arlington, VA: The Nature Conservancy, Central Conservation Databases. 1 p. [23108] 43. U.S. Department of the Interior, National Biological Survey. [n.d.]. NPLichen: A National Park Service lichen data base. Madison, WI: U.S. Department of the Interior, National Biological Survey, Wisconsin Cooperative Research Unit, Institute for Environmental Studies, University of Wisconsin-Madison. [23373] 44. Wood, Don A., compiler. 1994. Official lists of endangered & potentially endangered fauna and flora in Florida. Tallahassee, FL: Florida Game and Fresh Water Fish Commission. 22 p. [24196] 45. U.S. Department of the Interior, Fish and Wildlife Service. 1994. Endangered and threatened wildlife and plants. 50 CFR 17.11 & 17.12. Washington, DC: [Publisher unknown]. 42 p. [24413]

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

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