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Introductory

SPECIES: Clintonia uniflora | Queencup Beadlily
ABBREVIATION : CLIUNI SYNONYMS : NO-ENTRY SCS PLANT CODE : CLUN2 COMMON NAMES : queencup beadlily beadlily bride's bonnet blue bead bluebead lily clintonia one-flowered clintonia queen's cup TAXONOMY : The currently accepted scientific name of queencup beadlily is Clintonia uniflora (Schult.) Kunth [17]. There are no recognized subspecies, varieties, or forms. LIFE FORM : Forb FEDERAL LEGAL STATUS : No special status OTHER STATUS : NO-ENTRY COMPILED BY AND DATE : R. J. Habeck, December 1991 LAST REVISED BY AND DATE : NO-ENTRY AUTHORSHIP AND CITATION : Habeck, R. J. 1991. Clintonia uniflora. In: Remainder of Citation

DISTRIBUTION AND OCCURRENCE

SPECIES: Clintonia uniflora | Queencup Beadlily
GENERAL DISTRIBUTION : This forb inhabits the West Coast from Alaska south into California. Inland populations occur from southern Alberta and British Columbia south through Montana, Idaho, and into eastern Oregon [16,17,23]. ECOSYSTEMS : FRES23 Fir - spruce FRES24 Hemlock - Sitka spruce STATES : AL CA ID MT OR WA AB BC ADMINISTRATIVE UNITS : CRLA GLAC MORA NOCA OLYM YOSE BLM PHYSIOGRAPHIC REGIONS : 1 Northern Pacific Border 2 Cascade Mountains 3 Southern Pacific Border 4 Sierra Mountains 8 Northern Rocky Mountains KUCHLER PLANT ASSOCIATIONS : K001 Spruce - cedar - hemlock forest K003 Silver fir - Douglas-fir forest K004 Fir - hemlock forest K015 Western spruce - fir forest SAF COVER TYPES : 206 Engelmann spruce - subalpine fir 213 Grand fir 226 Coastal true fir - hemlock SRM (RANGELAND) COVER TYPES : NO-ENTRY HABITAT TYPES AND PLANT COMMUNITIES : Queencup beadlily occurs within many habitat type series. In Montana and Idaho, these include the spruce (Picea), grand fir (Abies grandis), subalpine fir (A. lasiocarpa), mountain hemlock (Tsuga mertensiana), and western red cedar (Thuja plicata) series. Typical phases associated with queencup beadlily habitat types include menziesia (Menziesia ferruginea), beargrass (Xerophyllum tenax), and queencup beadlily. In Montana, queencup beadlily is an indicator of more maritime microsites. In northern and central Idaho, however, it is an indicator of more mesic microsites [5,24,29]. Publications listing queencup beadlily as an indicator or dominant species in habitat types (hts), community types (cts), or plant associations (pas) are listed below: Area Classification Authority MT forest hts Pfister & others 1977 MT forest pas Hansen & others 1991 sw MT forest hts Hansen & others 1989 n ID forest hts Cooper & others 1991 c ID forest hts Steele & others 1981 w WA forest cts Franklin & Dyrness 1984 s WA, n OR forest cts Franklin & Dyrness 1984 e WA, n ID forest cts Daubenmire & Daubenmire 1968 WA: Gifford Pinchot forest pas Topik 1989 National Forest

VALUE AND USE

SPECIES: Clintonia uniflora | Queencup Beadlily
WOOD PRODUCTS VALUE : NO-ENTRY IMPORTANCE TO LIVESTOCK AND WILDLIFE : No information is available concerning the specific use of queencup beadlily by livestock or wildlife. The forage potential is basically fair in early seral habitat types which include queencup beadlily as an understory associate. As these sites mature, however, the forage potential becomes poor to nonexistent in late-seral to near-climax stands with closed canopies [5,14,24,29]. Low forage quality and abundance indicate that mature stands that include queencup beadlily are nonrange for livestock [32]. PALATABILITY : The fruit of queencup beadlily is often eaten by small mammals and birds. Birds in southeastern Washington chose it as food more than other species; this preference may be based on the amount of fresh pulp contained in the fruit [26]. Elk in central Idaho forage on queencup beadlily leaves, but the palatability is rated low [34]. NUTRITIONAL VALUE : Nutritional quality of queencup beadlily fruits from the Rainbow Creek Research Natural Area, southeastern Washington, was as follows [26]: Mean Standard Error ------ ---------------- % Protein 5.950 0.01 % Lipid 3.060 0.29 % Neutral Detergent Fiber 13.150 0.36 % Ash 12.400 0.06 % Calcium 0.768 NA % Magnesium 0.310 NA % Phosphorus 0.424 NA % Potassium 5.594 NA * Percentages based on dry pulp masses. COVER VALUE : NO-ENTRY VALUE FOR REHABILITATION OF DISTURBED SITES : Queencup beadlily is not transplanted for site recovery projects. It has low resistance to human trampling but also exhibits high short-term resilience to disturbance. Visitor-use disturbance to queencup beadlily, as well as its recovery rate, can be predicted [17]. OTHER USES AND VALUES : NO-ENTRY MANAGEMENT CONSIDERATIONS : Queencup beadlily is not specifically managed. The associated overstory, however, is usually highly productive [5,24,29]. Partial cutting on these sites generally leads to marked seral shrub and forb increase. Queencup beadlily has been observed to grow larger and possess more root biomass in open sun than in shade (35% open sun) [25]. Conversely, it has been reported to decrease in percent cover from uncut sites to cut sites [1,12,31]. This may indicate that queencup beadlily is prone to injury from logging, intolerant to excessive sunlight, or sensitive to change in soil moisture.

BOTANICAL AND ECOLOGICAL CHARACTERISTICS

SPECIES: Clintonia uniflora | Queencup Beadlily
GENERAL BOTANICAL CHARACTERISTICS : Queencup beadlily is a small, perennial, rhizomatus forb, with a single white flower about 1 inch (2 cm) long. Following pollination, a solitary, smooth, blue berry approximately 0.25 to 0.40 inch (6-10 mm) long forms on the stem. The plant has two or three shiny-green basal leaves which are broad and flat, and about 3 to 6 inches (7-15 cm) long. Both the stem and leaves are clothed with fine white epidermal hairs [16,17,23]. Means and ranges of queencup beadlily morphological characteristics are as follows [2]: Mean Range ------ ------- Number of Shoots 2.90 1-9 Number of Leaves 5.30 2-15 Total Rhizome Length (cm) 118.00 15-392 Max. Rhizome Depth (cm) 4.80 3-6 Number of Roots 18.00 8-48 Max. Root Depth (cm) 23.00 15-30 Total Plant Biomass (g) 1.13 0.47-3.69 Max. Age of Live Tissue (yr) 21.30 8-30 RAUNKIAER LIFE FORM : Geophyte REGENERATION PROCESSES : Queencup beadlily generally reproduces through rhizomes located 1.2 to 2.4 inches (3-6 cm) below the soil surface. In a laboratory study analyzing germination rates from seeds collected in the fall, queencup beadlily germinated approximately 250 days after sowing and continued to germinate steadily for 375 days. In early fall it germinated faster (approximately 100 days) and peaked quicker (approximately 140 days) [25]. Morphological characteristics of queencup beadlily fruit from the Rainbow Creek Research Natural Area, southeastern Washington, are as follows [26]: Mean Standard Error -------- ---------------- Fruit Diameter (mm) 9.94 0.15 Fruit Mass (mg) 435.66 18.92 Pulp Dry Mass (mg) 16.40 0.67 No. of Seeds per Fruit 6.76 0.36 Fresh Seed Mass per Fruit (mg) 82.23 5.10 Fresh Pulp Mass (mg) 6.85 0.69 * n=100 SITE CHARACTERISTICS : Queencup beadlily occupies moist, coniferous forest areas on high slopes, benches, and stream terraces. The elevational distribution of queencup beadlily ranges from 2,000 to 6,100 feet (555-1,860 m) [5,24,29]. It tends to occur on warm, moist sites, although it can be found on all aspects. Soils: Queencup beadlily occurs on a variety of soil types ranging from silty clay loams, loams, to gravelly loams. Parent materials generally include granite, quartz, and other noncalcareous substrates. Volcanic ash seems to be widely present in the upper soil horizons of most queencup beadlily habitat types [22]. Soil pH usually ranges from 5.5 to 6.5. SUCCESSIONAL STATUS : Obligate Climax Species Queencup beadlily is an understory indicator species primarily found in mature forests [5,24,29]. Its understory associates mostly include twinflower (Linnaea borealis), bunchberry dogwood (Cornus canadensis), and wintergreen (Pyrola spp.) [19]. Queencup beadlily is often a dominant understory species, making it a dependable habitat type indicator. SEASONAL DEVELOPMENT : Phenological observations for queencup beadlily in northern Idaho and west of the Continental Divide in Montana from 1928 to 1937 were as follows [28]: Average Earliest Latest Standard Number of Date Date Date Error Observations --------- -------- ------- --------- ------------- First Appearance May 10 Apr 25 May 20 2 13 Leaves Full Grown June 21 June 1 July 2 3 13 Flowers Start June 16 May 30 July 1 3 15 Flowers End July 1 June 15 July 25 3 15 Fruits Ripe Aug 11 July 22 Aug 26 3 14 Seed Fall Starts Aug 19 Aug 1 Aug 31 4 7 Leaves Wither Aug 23 Aug 1 Sept 1 2 14 Leaves Fallen Oct 1 Sept 14 Oct 7 2 13 First Frost Injury Sept 10 Aug 23 Sept 24 4 8

FIRE ECOLOGY

SPECIES: Clintonia uniflora | Queencup Beadlily
FIRE ECOLOGY OR ADAPTATIONS : Stickney [30] listed queencup beadlily as an on-site survivor following fire. It sprouts from rhizomes buried approximately 1.5 inches (4 cm) in the soil [1,9,16]. POSTFIRE REGENERATION STRATEGY : Rhizomatous herb, rhizome in soil Initial-offsite colonizer (off-site, initial community) Secondary colonizer - off-site seed

FIRE EFFECTS

SPECIES: Clintonia uniflora | Queencup Beadlily
IMMEDIATE FIRE EFFECT ON PLANT : Queencup beadlily is typically top-killed by fire. High-severity fires may lead to the total destruction of the plant. Miller and Miller [21] reported it to be absent from sample sites during 4 years of study following wildfires in North Cascades National Park, Washington. DISCUSSION AND QUALIFICATION OF FIRE EFFECT : NO-ENTRY PLANT RESPONSE TO FIRE : Although no information is available for queencup beadlily specifically, it usually decreases following fire. The postfire environment is not thought to be suitable for rapid recovery of queencup beadlily [9]. A queencup beadlily ecosystem in British Columbia steadily increased in percent cover following fire, leveling off about 9 years after the burn [13]. DISCUSSION AND QUALIFICATION OF PLANT RESPONSE : NO-ENTRY FIRE MANAGEMENT CONSIDERATIONS : NO-ENTRY

References for species: Clintonia uniflora


1. Antos, Joseph Avery. 1977. Grand fir (Abies grandis (Dougl.) Forbes) forests of the Swan Valley, Montana. Missoula, MT: University of Montana. 220 p. Thesis. [6720]
2. Antos, Joseph A. 1988. Underground morphology and habitat relationships of three pairs of forest herbs. American Journal of Botany. 75(1): 106-113. [15052]
3. 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]
4. Cole, David N. 1988. Disturbance and recovery of trampled montane grassland and forests in Montana. Res. Pap. INT-389. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 37 p. [3622]
5. Cooper, Stephen V.; Neiman, Kenneth E.; Roberts, David W. 1991. (Rev.) Forest habitat types of northern Idaho: a second approximation. Gen. Tech. Rep. INT-236. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 143 p. [14792]
6. Daubenmire, Rexford F.; Daubenmire, Jean B. 1968. Forest vegetation of eastern Washington and northern Idaho. Technical Bulletin 60. Pullman, WA: Washington State University, Agricultural Experiment Station. 104 p. [749]
7. 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]
8. Eyre, F. H., ed. 1980. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters. 148 p. [905]
9. Fischer, William C.; Bradley, Anne F. 1987. Fire ecology of western Montana forest habitat types. Gen. Tech. Rep. INT-223. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 95 p. [633]
10. Franklin, Jerry F.; Dyrness, C. T. 1973. Natural vegetation of Oregon and Washington. Gen. Tech. Rep. PNW-8. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station. 417 p. [961]
11. Freedman, June D. 1983. The historical relationship between fire and plant succession within the Swan Valley white-tailed deer winter range, western Montana. Missoula, MT: University of Montana. 139 p. Dissertation. [6486]
12. Garrison, George A.; Bjugstad, Ardell J.; Duncan, Don A.; [and others]. 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]
13. Hamilton, Evelyn H.; Yearsley, H. Karen. 1988. Vegetation development after clearcutting and site preparation in the SBS zone. Economic and Regional Development Agreement: FRDA Report 018. Victoria, BC: Canadian Forestry Service, Pacific Forestry Centre; British Columbia Ministry of Forests and Lands. 66 p. [8760]
14. Hansen, Paul; Boggs, Keith; Pfister, Robert; Joy, John. 1990. Classification and management of riparian and wetland sites in central and eastern Montana. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station, Montana Riparian Association. 279 p. [12477]
15. Hansen, Paul; Pfister, Robert; Joy, John; [and others]. 1989. Classification and management of riparian sites in southwestern Montana. Missoula, MT: University of Montana, School of Forestry, Montana Riparian Association. 292 p. Draft Version 2. [8900]
16. Hitchcock, C. Leo; Cronquist, Arthur. 1973. Flora of the Pacific Northwest. Seattle, WA: University of Washington Press. 730 p. [1168]
17. Hitchcock, C. Leo; Cronquist, Arthur; Ownbey, Marion. 1969. Vascular plants of the Pacific Northwest. Part 1: Vascular cryptograms, gymnosperms, and monocotyledons. Seattle, WA: University of Washington Press. 914 p. [1169]
18. 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]
19. Lackschewitz, Klaus. 1991. Vascular plants of west-central Montana--identification guidebook. Gen. Tech. Rep. INT-227. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 648 p. [13798]
20. Stickney, Peter F. 1989. Seral origin of species originating in northern Rocky Mountain forests. Unpublished draft on file at: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, Fire Sciences Laboratory, Missoula, MT; RWU 4403 files. 10 p. [20090]
21. Miller, Margaret M.; Miller, Joseph W. 1976. Succession after wildfire in the North Cascades National Park complex. In: Proceedings, annual Tall Timbers fire ecology conference: Pacific Northwest; 1974 October 16-17; Portland, OR. No. 15. Tallahassee, FL: Tall Timbers Research Station: 71-83. [6574]
22. Nimlos, Thomas J. 1981. Volcanic ash soils in Montana. Bulletin 45. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station. 21 p. [8193]
23. Patterson, Patricia A.; Neiman, Kenneth E.; Tonn, Jonalea. 1985. Field guide to forest plants of northern Idaho. Gen. Tech. Rep. INT-180. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 246 p. [1839]
24. Pfister, Robert D.; Kovalchik, Bernard L.; Arno, Stephen F.; Presby, Richard C. 1977. Forest habitat types of Montana. Gen. Tech. Rep. INT-34. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Forest and Range Experiment Station. 174 p. [1878]
25. Piper, Jon K. 1986. Germination and growth of bird-dispersed plants: effects of seed size and light on seedling vigor and biomass allocation. American Journal of Botany. 73(7): 959-965. [5033]
26. Piper, Jon K. 1986. Seasonality of fruit characters and seed removal by birds. Oikos. 46: 303-310. [15348]
27. Raunkiaer, C. 1934. The life forms of plants and statistical plant geography. Oxford: Clarendon Press. 632 p. [2843]
28. Schmidt, Wyman C.; Lotan, James E. 1980. Phenology of common forest flora of the northern Rockies--1928 to 1937. Res. Pap. INT-259. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Forest and Range Experiment Station. 20 p. [2082]
29. Steele, Robert; Pfister, Robert D.; Ryker, Russell A.; Kittams, Jay A. 1981. Forest habitat types of central Idaho. Gen. Tech. Rep. INT-114. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Forest and Range Experiment Station. 138 p. [2231]
30. Stickney, Peter F. 1986. First decade plant succession following the Sundance Forest Fire, northern Idaho. Gen. Tech. Rep. INT-197. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 26 p. [2255]
31. Tobalske, Bret W.; Shearer, Raymond C.; Hutto, Richard L. 1991. Bird populations in logged and unlogged western larch/Douglas-fir forest in northwestern Montana. Res. Pap. INT-442. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station. 12 p. [15994]
32. Topik, Christopher. 1989. Plant association and management guide for the grand fir zone, Gifford Pinchot National Forest. R6-Ecol-TP-006-88. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Region. 110 p. [11361]
33. U.S. Department of Agriculture, Soil Conservation Service. 1982. National list of scientific plant names. Vol. 1. List of plant names. SCS-TP-159. Washington, DC. 416 p. [11573]
34. Young, Vernon A.; Robinette, W. Leslie. 1939. A study of the range habits of elk on the Selway Game Preserve. Bull. No. 9. Moscow, ID: University of Idaho, School of Forestry. 47 p. [6831]


[6831] Index

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