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Introductory

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
ABBREVIATION : PINARI SYNONYMS : Pinus balfouriana var. aristata (Engelm.) Engelm. SCS PLANT CODE : PIAR COMMON NAMES : Rocky Mountain bristlecone pine Colorado bristlecone pine hickory pine TAXONOMY : Bailey designated the western populations of bristlecone pine as Pinus longaeva D. K. Bailey (Great Basin bristlecone pine) and reserved the older name of P. aristata Engelm. (Rocky Mountain bristlecone pine) for the eastern populations. Pinus balfouriana var. aristata (Engelm.) Engelm. is included in P. longaeva. Great Basin and Rocky Mountain bristlecone pines differ in several important characteristics: chemistry, needle structure, and cone morphology [2]. The Colorado-Green River drainage has separated them for millions of years, and crosses between the two species are relatively unsuccessful [5]. Today they are separated by 160 miles (260 km). LIFE FORM : Tree FEDERAL LEGAL STATUS : No special status OTHER STATUS : NO-ENTRY COMPILED BY AND DATE : Kathy Ahlenslager November 1986 LAST REVISED BY AND DATE : Kathy Ahlenslager December 1987 AUTHORSHIP AND CITATION : Ahlenslager, Kathleen E. 1986. Pinus aristata. In: Remainder of Citation

DISTRIBUTION AND OCCURRENCE

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
GENERAL DISTRIBUTION : The range of Rocky Mountain bristlecone pine extends from the eastern slope of the southern Rocky Mountains in the Laramie Range of southwestern Wyoming southward through the eastern San Juan Mountains of Colorado to the Sangre de Cristo Mountains east of Sante Fe, New Mexico. A disjunct population occurs 200 miles (500 km) west in north-central Arizona in the San Francisco Peaks [1,5,7,9,11,24,32]. ECOSYSTEMS : FRES20 Douglas-fir FRES21 Ponderosa pine FRES23 Fir - spruce FRES26 Lodgepole pine STATES : AZ CO NM WY ADMINISTRATIVE UNITS : FLFO BLM PHYSIOGRAPHIC REGIONS : 11 Southern Rocky Mountains 12 Colorado Plateau KUCHLER PLANT ASSOCIATIONS : K021 Southwestern spruce - fir forest SAF COVER TYPES : 206 Englemann spruce - subalpine fir 209 Bristlecone pine 219 Limber pine 237 Interior ponderosa pine SRM (RANGELAND) COVER TYPES : NO-ENTRY HABITAT TYPES AND PLANT COMMUNITIES : Stands of Rocky Mountain bristlecone pine are usually pure, even aged, and open. Trees associated with this species are limber pine (Pinus flexilis), white fir (Abies concolor), Engelmann spruce (Picea engelmannii), ponderosa pine (Pinus ponderosa), pinyon pine (P. edulis), subalpine fir (A. lasiocarpa), aspen (Populus tremuloides), and Rocky Mountain juniper (Juniperus osteosperma) [11]. The Rocky Mountain bristlecone pine series occurs on cold, dry sites at high elevations in pure stands or with limber pine. It grades into Engelmann spruce and subalpine fir at lower elevations. In southern Colorado and northern New Mexico, Rocky Mountain bristlecone pine and Engelmann spruce codominate in the Englemann spruce series. This series occurs on middle and upper slopes over 10,500 feet (3,200 m) and in the spruce-fir zone where tree growth is limited by drought. In the Douglas-fir (Pseudotsuga menziesii) series at higher elevations, Rocky Mountain bristlecone pine dominates or codominates. Publications using Rocky Mountain bristlecone pine in classification schemes are listed below. Forest vegetation of the Gunnison and parts of the Uncompahgre National Forests: a preliminary habitat type classification. [14] Major habitat types, community types and plant communities in the Rocky Mountains [1] Preliminary classification for the coniferous forest and woodland series of Arizona and New Mexico. [20] A preliminary classification of the natural vegetation of Colorado. [3] A series vegetation classification for Region 3. [26]

VALUE AND USE

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
WOOD PRODUCTS VALUE : The wood of Rocky Mountain bristlecone pine is moderately soft and is of low value in construction. It has been used for fuel and mine props [21,28]. IMPORTANCE TO LIVESTOCK AND WILDLIFE : The seeds of Rocky Mountain bristlecone pine are edible to some species of wildlife. Trees often occur in clumps, probably from the caches of seed eaters, such as Clark's nutcrackers. Small mammals and birds may benefit from these seed caches. Rocky Mountain bristlecone pine provides some cover for birds and small mammals. PALATABILITY : NO-ENTRY NUTRITIONAL VALUE : NO-ENTRY COVER VALUE : NO-ENTRY VALUE FOR REHABILITATION OF DISTURBED SITES : Rocky Mountain bristlecone pine has little to no value for rehabilitation due to the extremely slow rate of growth of seedlings and mature trees. Its growth on gentle to steep slopes is rated as good. Its potential for erosion control in Colorado is medium [8]. OTHER USES AND VALUES : With ages ranging to 1,500 years, Rocky Mountain bristlecone pines are among the oldest living trees. The dense, resinous wood of Rocky Mountain bristlecone pines contributes to the ability of dead trees to stand for hundreds of years and fallen wood to persist for thousands. This wood provides cross-reference for radiocarbon dating [2,6,15]. Living trees, standing snags, and fallen trees provide overlapping tree-ring chronologies. These ring-width chronologies are used as paleoclimatic indicators to determine past limits of tree growth. Variation in ring-widths of trees at upper treeline is an important indicator of past climatic variations, especially for temperature fluctuations. Data from these chronologies show that there has been a net retreat of upper bristlecone pine treeline in the United States over the last several thousand years [17,19]. The dates of major volcanic eruptions correlate with frost rings of bristlecones [18]. Rocky Mountain bristlecone pine is of value for its natural aesthetics and for watershed protection, as well as aiding in soil-building and stabilization in a harsh environment [12]. MANAGEMENT CONSIDERATIONS : NO-ENTRY

BOTANICAL AND ECOLOGICAL CHARACTERISTICS

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
GENERAL BOTANICAL CHARACTERISTICS : Rocky Mountain bristlecone pine is a long-lived, ectomycorrhizal, native species, which may be nitrogen fixing. Trees attain heights of 15 to 30 feet (5-9 m) with diameters between 12 and 18 inches (31-46 cm). Needles are retained in excess of 20 years. Trees often have a contorted and multistemmed appearance. The sparse crowns of twisted or contorted trees are supported by narrow strips of cambium. The effects of sand- and ice-blasting by wind are seen in older trees with a double "pick-a-back" growth form. Here the windward trunk is dead, but a narrow strip of cambium supports branches on the leeward side of the tree, the "piggy back" [10,28]. Rocky Mountain bristlecone pine exhibits slow growth rates and dense, highly resinous wood. Bristlecones are known for their longevity. Although trees of Rocky Mountain bristlecone pine may reach 1,500 years in age, some Great Basin bristlecones (Pinus longaeva) have been estimated to live 5,200 years. Rocky Mountain bristlecone pine and foxtail (Pinus balfouriana) grow more rapidly than the Great Basin bristlecone pine because of greater moisture availability. However, they also are more subject to heart rot and do not reach the longevity of Great Basin bristlecone [2,13]. Compared with other white pines, Rocky Mountain bristlecone pine is very resistant to white pine blister rust. Rocky Mountain bristlecone, Great Basin bristlecone, and foxtail pine share the following characteristics [10,24]: (1) occurrence at the upper limits of tree growth and a reduced rate of growth (2) a capacity for long life (3) continued growth after loss of large areas of tissue from drought, stress, wind injury, and soil erosion (4) heavy, dense, resin-impregnated wood with small, closely arranged water-conducting cells (tracheids) which provide resistance to moisture and decay (5) survival in an environment of drought, low temperatures, short growing seasons, daily temperature extremes, and poor soils (6) retention of needles for several years, which reduces the need for moisture and nutrients, as well as carrying a tree over several years of stress (7) relative safety from ground fire due to sparse ground cover and litter scarcity. RAUNKIAER LIFE FORM : Phanerophyte REGENERATION PROCESSES : The environmental and physiological factors contributing to the longevity of Rocky Mountain bristlecone pine also work to lower its regeneration potential. Trees are intolerant of shade, grow slowly, and are locally scattered in distribution. Reproduction is sparse. Bristlecones characteristically occur in old to moderately old, open stands, and form the vegetative climax. However, this species may also act like a pioneer in recently disturbed areas where under favorable conditions tree growth is vigorous and fast [5,28]. Recovery from logging, road construction, and other disturbances, though, is generally extremely slow, often taking hundreds of years [12]. With 75 percent seed germination within 8 days, researchers concluded that the seeds of bristlecone pines do not exhibit dormancy. In an effort to understand the limited occurrence of Rocky Mountain bristlecone pine, the germinability of seeds was studied in Clear Creek, Colorado. Rapid germination, scarification mortality, and lack of seedling cold hardiness were identified as contributing factors working against Rocky Mountain bristlecone pine reproduction. Seeds had a germination rate of 80 percent and germinated within 10 days (with or without light). Infected with fungus, 90 percent of the scarified seeds died. A gradual decrease in temperature to 14 degrees Fahrenheit (-10 deg C) killed 10- and 180-day-old seedlings [28]. SITE CHARACTERISTICS : Rocky Mountain bristlecone pine grows in subalpine areas. Stands are usually pure, even-aged, and open. They are found from 9,200 to 11,800 feet (2,800-3,600 m) in elevation in Colorado and New Mexico, usually on rocky outcrops of southern or southwestern slopes with limited soil, intense sunlight, and rapid runoff. In the San Francisco Peaks Research Natural Area in Arizona, bristlecone pines occur from 10,500 to 11,500 feet (3,200-3,500 m) on south-facing ridges and talus slopes [2,32]. Rocky Mountain bristlecone pines occur most often on igneous and volcanic substrates. Short growing seasons and little available moisture characterize their habitat. Trees are intolerant of shading and occur in areas of sparse ground cover. Precipitation ranges from 16 to 40 inches (400-1,000 mm) [2,31,32]. Above Sante Fe, New Mexico, limber pine dominates on xeric sites between 7,550 to 10,170 feet (2,300 and 3,100 m) but is replaced on the driest sites by Rocky Mountain bristlecone pine. To the north Rocky Mountain bristlecone pine increases in importance, and in the area of the Spanish Peaks of Colorado, it is found from treeline down to ponderosa pine-Gambel oak (Quercus gambelii) woodlands. North of this area Rocky Mountain bristlecone pine is replaced by limber pine. At Pikes Peak in Colorado, it is important on the south slopes from middle to high elevations; however, on north slopes it is restricted to high-elevation sites. On Mt. Evans in Colorado, bristlecone and limber pine occur at high elevations and are partitioned by substrates [2,25,30]. SUCCESSIONAL STATUS : Rocky Mountain bristlecone pine is a climax species and persists at treeline for hundreds to thousands of years in the absence of disturbance and competition. It is highly adapted to its habitat of very shallow soils, slow primary succession, short growing season, and avalanches. This tree is intolerant of shading and competition. Below its lower elevational limits, it is outcompeted and replaced by other conifers on moist sites. Although its upper limits of growth are temperature sensitive, its lower growth limits are precipitation sensitive [2,25,32]. There is no evidence for the expansion or recession of the range of Rocky Mountain bristlecone pine, so it is considered a senescent species [27]. SEASONAL DEVELOPMENT : Bristlecone pines flower from July to August, and cones start ripening about mid-September. The period of flowering and cone opening is uniform for Rocky Mountain and Great Basin bristlecone pines and foxtail pine [5,10]. Phenological data for Rocky Mountain bristlecone pine in the San Francisco Peaks area of Arizona are as follows: Plant Activity 1918-23 1969 ------------------------------------------------------------------------ Vegetative buds swelling June 1-20 June 1 Vegetative buds elongating or opening June 20-30 June 15 Shoots making rapid growth July 1-30 ---- Male buds appearing July 1-10 ---- Female and male buds mature ---- July 22 Pollen falling July 20-Aug. 20 July 22-27 Cones full grown Sept. 10-20 ---- Seeds mature Sept. 20-Oct. 10 Sept. 24-Oct. 2 Cones opening ---- Sept. 27-Oct. 10 Leaves falling Oct. 1-30 ---- Period of active growth June 20-Sept. 20 ----

FIRE ECOLOGY

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
FIRE ECOLOGY OR ADAPTATIONS : Rocky Mountain bristlecone pine occurs for the most part in habitats where fuels to carry fires are essentially nonexistant. In the subalpine zone where bristlecones are found, low temperatures and a short growing season keep the production of organic matter low. Burns with enough intensity to result in crown fires rarely occur in the grass-dominated understory of bristlecone pine forests. Surface fires in these areas are infrequent, slow burning, and of low intensity [7]. POSTFIRE REGENERATION STRATEGY : Tree without adventitious-bud root crown Initial-offsite colonizer (off-site, initial community)

FIRE EFFECTS

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
IMMEDIATE FIRE EFFECT ON PLANT : Fire plays a minor role in bristlecone pine habitats due to sparse ground cover. Although scattered dead and living trees show evidence of fires, undergrowth is scarce with essentially no sign of past fires. In these areas undergrowth consists of small shrubs, cushion plants, and xerophytic bunchgrasses [7]. DISCUSSION AND QUALIFICATION OF FIRE EFFECT : NO-ENTRY PLANT RESPONSE TO FIRE : NO-ENTRY DISCUSSION AND QUALIFICATION OF PLANT RESPONSE : NO-ENTRY FIRE MANAGEMENT CONSIDERATIONS : NO-ENTRY

REFERENCES

SPECIES: Pinus aristata | Rocky Mountain Bristlecone Pine
REFERENCES : 1. Alexander, Robert R. 1985. Major habitat types, community types and plant communities in the Rocky Mountains. Gen. Tech. Rep. RM-123. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 105 p. [303] 2. Bailey, D. K. 1970. Phytogeography and taxonomy of Pinus subsection Balfourianae. Annals of the Missouri Botanical Garden. 57: 210-249. [375] 3. Baker, William L. 1984. A preliminary classification of the natural vegetation of Colorado. Great Basin Naturalist. 44(4): 647-676. [380] 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. Critchfield, William B. 1977. Hybridization of foxtail and bristlecone pines. Madrono. 24(4): 193-244. [713] 6. Currey, Donald R. 1965. An ancient bristlecone pine stand in eastern Nevada. Ecology. 46(4): 564-566. [725] 7. DeVelice, Robert L.; Ludwig, John A. 1983. Forest habitat types south of the Mogollon Rim, Arizona and New Mexico. Final Report. Cooperative Agreement No. 28-K2-240 between U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station and New Mexico State University. Las Cruces, NM: New Mexico State University. 47 p. [780] 8. 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] 9. Eyre, F. H., ed. 1980. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters. 148 p. [905] 10. Fritts, Harold C. 1969. Bristlecone pine in the White Mountains of California: growth and ring-width characteristics. Papers of the Laboratory of Tree-Ring Research. No. 4. Tucson, AZ: The University of Arizona Press. 44 p. [980] 11. Griffin, James R.; Critchfield, William B. 1972. The distribution of forest trees in California. Res. Pap. PSW-82. Berkeley, CA: U.S. Department of Agriculture, Forest Service, Pacific Southwest Forest and Range Experiment Station. 118 p. [1041] 12. Hess, Karl; Alexander, Robert R. 1986. Forest vegetation of the Arapaho and Roosevelt National Forests in central Colorado: a habitat type classification. Res. Pap. RM-266. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 48 p. [1141] 13. Hitch, Charles J. 1982. Dendrochronology and serendipity. American Scientist. 70(3): 300-305. [1164] 14. Komarkova, Vera; Alexander, Robert R.; Johnston, Barry C. 1988. Forest vegetation of the Gunnison and parts of the Uncompahgre National Forests: a preliminary habitat type classification. Gen. Tech. Rep. RM-163. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 65 p. [5798] 15. Krebs, Paula V. 1973. Dendrochronology of bristlecone pine (Pinus aristata Engelm.) in Colorado. Arctic and Alpine Research. 5(2): 149-150. [1376] 16. 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] 17. LaMarche, Valmore C., Jr. 1974. Paleoclomatic inferences from long tree-ring records. Science. 183(4129): 1043-1048. [1391] 18. LaMarche, Valmore C., Jr.; Hirschboeck, Katherine K. 1984. Frost rings in trees as records of major volcanic eruptions. Nature. 307(12): 121-126. [1392] 19. LaMarche, Valmore C., Jr.; Stockton, Charles W. 1974. Chronologies from temperature-sensitive bristlecone pines at upper treeline in western United States. Tree-ring Bulletin. 34: 21-45. [1395] 20. Layser, Earle F.; Schubert, Gilbert H. 1979. Preliminary classification for the coniferous forest and woodland series of Arizona and New Mexico. Res. Pap. RM-208. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 27 p. [1428] 21. Little, Elbert L., Jr. 1975. Rare and local conifers in the United States. Conservation Research Rep. No. 19. Washington, DC: U.S. Department of Agriculture, Forest Service. 25 p. [15691] 22. Little, Elbert L., Jr. 1978. Important forest trees of the United States. Agric. Handb. 519. Washington, DC: U.S. Department of Agriculture, Forest Service. 70 p. [1463] 23. Lyon, L. Jack; Stickney, Peter F. 1976. Early vegetal succession following large northern Rocky Mountain wildfires. In: Proceedings, Tall Timbers fire ecology conference and Intermountain Fire Research Council fire and land management symposium; 1974 October 8-10; Missoula, MT. No. 14. Tallahassee, FL: Tall Timbers Research Station: 355-373. [1496] 24. Mastroguiseppe, Ronald J. 1972. Geographic variation in foxtail pine, Pinus balifouriana Grev. & Balf. Humbolt, CA: California State University, Humboldt. 98 p. M.S. thesis. [1548] 25. Mirov, N. T. 1967. The genus Pinus. New York: Ronald Press. 602 p. [1663] 26. Moir, W. H. 1983. A series vegetation classification for Region 3. In: Moir, W. H.; Hendzel, Leonard, tech. coords. Proceedings of the workshop on Southwestern habitat types; 1983 April 6-8; Albuquerque, NM. Albuquerque, NM: U.S. Department of Agriculture, Forest Service, Southwestern Region: 91-95. [1672] 27. Peet, Robert K. 1978. Forest vegetation of the Colorado Front Range: patterns of species diversity. Vegetatio. 37(2): 65-78. [1866] 28. Preston, Richard J., Jr. 1948. North American trees. Ames, IA: The Iowa State College Press. 371 p. [1913] 29. Raunkiaer, C. 1934. The life forms of plants and statistical plant geography. Oxford: Clarendon Press. 632 p. [2843] 30. Reid, William H. 1972. Germination of Pinus aristata Engelm. Great Basin Naturalist. 32(4): 235-237. [1953] 31. Rominger, James M.; Paulik, Laurie A. 1983. A floristic inventory of the plant communities of the San Francisco Peaks Research Natural Area. Gen. Tech. Rep. RM-96. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 9 p. [2023] 32. Schaack, Clark G. 1989. Additions to Arizona flora-range extensions of noxious weeds, plant distribution records estab. by ADOT/USFS and the location for Arizona Lewisia rediviva Pursh. Journal of the Arizona-Nevada Academy of Science. 23: 35-37. [11414]

Index

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