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Introductory

SPECIES: Distichlis spicata | Saltgrass
ABBREVIATION : DISSPI SYNONYMS : saltgrass seashore saltgrass inland saltgrass alkali-grass SCS PLANT CODE : DIST COMMON NAMES : saltgrass inland saltgrass seashore saltgrass alkali-grass TAXONOMY : The currently accepted scientific name for saltgrass is Distichlis spicata (L.) E. Greene [85,89]. Recent literature does not recognize intrataxa within this species [85,89]. LIFE FORM : Graminoid FEDERAL LEGAL STATUS : No special status OTHER STATUS : NO-ENTRY COMPILED BY AND DATE : Ronald Uchytil/July 1990 LAST REVISED BY AND DATE : NO-ENTRY AUTHORSHIP AND CITATION : Uchytil, Ronald J. 1990. Distichlis spicata. In: Remainder of Citation

DISTRIBUTION AND OCCURRENCE

SPECIES: Distichlis spicata | Saltgrass
GENERAL DISTRIBUTION : Saltgrass is widely distributed across the western United States and Canada from Saskatchewan to eastern Washington, south to California, Texas, and Mexico [37]. ECOSYSTEMS : FRES17 Elm - ash - cottonwood FRES21 Ponderosa pine FRES28 Western hardwoods FRES29 Sagebrush FRES30 Desert shrub FRES34 Chaparral - mountain shrub FRES35 Pinyon - juniper FRES36 Mountain grasslands FRES38 Plains grasslands FRES39 Prairie FRES41 Wet grasslands STATES : AZ CA CO ID IA KS MN MO MT NE NV NM ND OK OR SD TX UT WA WY AB MB SK MEXICO ADMINISTRATIVE UNITS : AGFO ARCH BADL BICA CACH CANY COLM DETO DEVA DINO GLAC GLCA GRCA GRTE JODA JOTR MEVE ORPI PEFO THRO WHIS WICA WUPA YELL ZION BLM PHYSIOGRAPHIC REGIONS : 3 Southern Pacific Border 5 Columbia Plateau 6 Upper Basin and Range 7 Lower Basin and Range 8 Northern Rocky Mountains 9 Middle Rocky Mountains 10 Wyoming Basin 11 Southern Rocky Mountains 12 Colorado Plateau 13 Rocky Mountain Piedmont 14 Great Plains 15 Black Hills Uplift 16 Upper Missouri Basin and Broken Lands KUCHLER PLANT ASSOCIATIONS : K011 Western ponderosa forest K016 Eastern ponderosa forest K017 Black Hills pine forest K023 Juniper - pinyon woodland K027 Mesquite bosque K037 Mountain mahogany - oak scrub K038 Great Basin sagebrush K039 Blackbrush K040 Saltbush - greasewood K041 Creosote bush K049 Tule marshes K050 Fescue - wheatgrass K051 Wheatgrass - bluegrass K055 Sagebrush steppe K056 Wheatgrass - needlegrass shrubsteppe K057 Galleta - three awn shrubsteppe K063 Foothills prairie K064 Grama - needlegrass - wheatgrass K065 Grama - buffalograss K066 Wheatgrass - needlegrass K067 Wheatgrass - bluestem - needlegrass K068 Wheatgrass - grama - buffalograss K069 Bluestem - grama prairie K070 Sandsage - bluestem prairie K074 Bluestem prairie K075 Nebraska sandhills prairie K098 Northern floodplain forest SAF COVER TYPES : 235 Cottonwood - willow 237 Interior ponderosa pine 239 Pinyon - juniper 241 Western live oak 242 Mesquite SRM (RANGELAND) COVER TYPES : NO-ENTRY HABITAT TYPES AND PLANT COMMUNITIES : Saltgrass occurs in varying densities in many plant communities, but it is only a dominant or codominant under certain conditions. Nearly pure stands of saltgrass are indicative of sites where soils are saline and fine textured and where the surface soils are wet at least part of the growing season [65,80]. Great Plains communities dominated by saltgrass occupy low, moist, saline areas [59,77,86]. The boundary between saltgrass meadows and upland communities is often sharp, as soil textures change along an elevational gradient [51]. In the sagebrush (Artemisia tridentata) steppe and bluebunch wheatgrass (Pseudoroegneria spicata)-Idaho fescue (Festuca idahoensis) vegetation types of eastern Washington, saltgrass habitat types either consist of pure stands of saltgrass or support a two-layered association consisting of a continuous stand of saltgrass with well-spaced bunches of basin wildrye (Leymus cinereus) or black greasewood (Sarcobatus vermiculatus) [14]. Saltgrass is a dominant grass in the low-elevation desert shrub vegetation of the Great Basin where it often forms a sod under black greasewood, rabbitbrush (Chrysothamnus spp.), or shadescale (Atriplex confertifolia) [18,65,82]. Cooccurrence of black greasewood and saltgrass is usually an indication of soils with high moisture content. If soil salinity becomes greater than about 1 percent, black greasewood gives way to pure stands of saltgrass [18]. Published classification schemes listing saltgrass as an indicator species or as a dominant part of the vegatation are listed below: Analysis of grassland vegetation on selected key areas in southwestern North Dakota. [86] Classification and management of riparian sites in southwestern Montana. [34] Classification and management of riparian and wetland sites in central and eastern Montana. [35] Plant associations of Region Two. [42] Range plant communities of the Central Grasslands Research Station in southwestern North Dakota. [47] Riparian dominance types of Montana. [33] Steppe vegetation of Washington. [14] Vegetation and soils of the Cow Creek Watershed. [3]

VALUE AND USE

SPECIES: Distichlis spicata | Saltgrass
WOOD PRODUCTS VALUE : NO-ENTRY IMPORTANCE TO LIVESTOCK AND WILDLIFE : Llivestock generally avoid the harsh foliage of saltgrass. It usually remains green all summer long, even after other upland grasses become dry. If it is the only green vegetation in the area, livestock will eat it during the summer [63]. The seeds are eaten by numerous species of waterfowl and small mammals [54]. PALATABILITY : Saltgrass is harsh, wiry, and tough. It and is of low to fair palatability for livestock and wildlife [53,76,82]. The degree of use shown by livestock and wildlife species for saltgrass in several western states is rated as follows [16,63]: CO MT ND TX UT WY Cattle fair poor poor fair fair fair Sheep fair fair poor ---- poor fair Horses fair good fair fair fair good Pronghorn ---- poor poor ---- poor poor Elk ---- poor ---- ---- poor good Mule deer ---- poor poor ---- poor poor White-tailed deer ---- poor poor ---- ---- poor Small mammals ---- ---- ---- ---- fair fair Small nongame birds ---- ---- ---- ---- poor good Upland game birds ---- ---- ---- ---- poor fair Waterfowl ---- good fair ---- fair good NUTRITIONAL VALUE : Saltgrass is low in nutritive value. For cattle, diets of straight saltgrass should be avoided. Livestock that graze on this species only can develop severe rumen compaction [76]. Nutritional values of North Dakota plants, analyzed during full bloom in August, are given below [39]: % moisture % ash % crude protein % crude fiber % N fee extract 15 8.91 8.11 26.53 39.95 In Utah, the protein content of aerial plant parts dropped from 15 to 5 percent from April 1 to July 30, and remained at 5 percent through September [32]. COVER VALUE : Saltgrass provides cover for small wildlife species. It often forms a dense sod, which provides good concealment. Pure stands of saltgrass provide nesting sites for numerous species of ducks and shorebirds [5,87]. Nests can be subjected to flooding on some sites. VALUE FOR REHABILITATION OF DISTURBED SITES : Saltgrass is an outstanding plant for wind or water erosion control on saline or alkaline sites. Sites that have been stabilized with saltgrass include oil drilling sites contaminated from saltwater spills [31], red mud (bauxite residue) impoundments from mining activities [23], dry, saline lakebeds [19], the crowns and banks of irrigation ditches and levees [48], disturbed riparian sites [56], and roadside ditches [75]. Commercial seed is not available, but rhizomes collected in the field and planted onto problem areas quickly sprout and spread. Rhizomes can tolerate a wide range of osmotic potentials but are sensitive to desiccation [55]. Attempts to establish saltgrass from rhizome sections should be limited to wet, saline areas, unless irrigation is used during establishment. Planting rhizomes at depths of 1 to 2 inches (2.5-5 cm) has proven to be most successful [15]. Examination of rhizomes collected in the field showed that roughly 67 percent are capable of sprouting and forming shoots in any season. Rhizomes may be stored for up to 28 days at temperatures ranging from 35 to 50 degrees Fahrenheit (2-10 deg C) and at a relative humidity of 60 to 75 percent. Growth of rhizomes has been found to be best at temperatures between 77 and 86 degrees Fahrenheit (25-30 deg C) [55]. Although seed sources are limited, proper methods for seeding saltgrass have been discussed [10,11]. OTHER USES AND VALUES : NO-ENTRY MANAGEMENT CONSIDERATIONS : Saltgrass is highly resistant to grazing and is classified as an increaser. Because it normally occurs on moist sites, it is used to its best advantage during periods of drought. Cattle should not be allowed to graze it continually in late fall and winter when other more palatable grasses are scarce. If this cannot be avoided, cattle should be fed 5 pounds of alfalfa hay per head per day [76,82]. Saltgrass is highly resistant to trampling. It is therefore desirable in areas where livestock concentrate, such as watering sites, corrals, and trails [76]. It was found to be the most wear-resistant of several grasses subjected to various rates of compaction and wear from pick-up trucks [21]. Because saltgrass is a poor forage, attempts have been made to rehabilitate saltgrass meadows by killing the saltgrass and planting more palatable salt-tolerant grasses [6,46]. Plowing, discing, and other mechanical methods have proven ineffective in controlling it because it regrows profusely from rhizomes [49,50]. The herbicide ghyphosate has killed up to 98 percent of this grass in field and greenhouse experiments [49,50]. Soils of saltgrass-dominated sites are often high in clay content and are susceptible to compaction. Trails and roads should be located on adjacent uplands [34]. A sod formation of saltgrass around lakes often indicates alkaline conditions which are unfavorable for fish [33].

BOTANICAL AND ECOLOGICAL CHARACTERISTICS

SPECIES: Distichlis spicata | Saltgrass
GENERAL BOTANICAL CHARACTERISTICS : Saltgrass is a native, perennial, rhizomatous, warm-season grass 4 to 16 inches (10-40 cm) tall [83]. Under conditions of extreme salinity, plants are often dwarfed [80]. Plants are dioecious. The male panicle often extends above the leaves, but the female panicle is normally enclosed within the leaves [83]. Panicles of both sexes are 1.5 to 3 inches (4-8 cm) long with only a few spikelets [13]. The blue-green to gray-green leaves are stiff, sharp pointed, coarse, spread along the entire stem, and cure to a golden brown at the end of the growing season. Rhizomes are vigorous, scaly and up to 71 inches (180 cm) long [32]. In a Colorado study, saltgrass rhizomes were found growing 4.2 inches (10.7 cm) below the soil surface in a layer between the B2 and C soil horizons [51]. Saltgrass typically has a shallow root system. In a Nevada study, roots were never found deeper than 16 inches (40 cm) below the soil surface [10]. Saltgrass has many physiological adaptations which allow it to occupy saline environments. Plants contain salt glands that are active in the extrusion of salt. This helps retain sufficient ion concentrations in the leaf tissue to maintain adequate osmotic potentials [32]. The lacunae tissue of the roots is apparently continuous with the rhizome and leaf sheath which allows for gas exchange under partial inundation by water and in heavy soils [32]. Vesicular-abuscular mycorrhizal fungi have been observed on inland saltgrass roots and are thought to further enhance salt tolerance [38]. RAUNKIAER LIFE FORM : Geophyte REGENERATION PROCESSES : Saltgrass is a poor seed producer. Seed production is often restricted to favorable sites which support dense, healthy stands [10]. Reproduction is mainly vegetative; plants spread through a well-developed system of deep underground rhizomes. Rhizomes sprout even when buried under 12 inches (30 cm) of sediment [50]. Germination: Better than 80 percent germination of saltgrass seed from New Mexico was achieved with alternating temperatures above 81.5 degrees Fahrenheit (27.5 deg C) for 8 hours and 62 to 73 degrees Fahrenheit (16.5-23 deg C) for 16 hours [61]. For Nevada seed, alternating temperatures of 104 degrees Fahrenheit (40 deg C) for 8 hours and 50 degrees Fahrenheit (10 deg C) for 16 hours gave 58 percent germination [10]. In this study, temperature fluctuations of at least 36 degrees Fahrenheit (20 deg C) and an osmotic potential of -0.1 MPa were required for greater than 10 percent germination. Germination is inhibited by high levels of salinity. One study attained up to 72 percent germination of scarified seed placed in distilled water but only 21 percent germination of scarified seed in a 1.0 percent solution of sodium chloride [53]. These germination studies show that saltgrass seeds require relatively high temperatures, low salinities, and moist soils to germinate. In natural seedbeds, these conditions rarely occur [60]. Under natural conditions probably only a few seeds will germinate, unless precipitation or soil moisture is unusually high in the summer, a time when soil temperatures would be warm enough for large numbers of seeds to germinate [60]. Although plants can grow in soils with very low osmotic potentials and very high salt concentrations, seeds cannot germinate in such soils [10]. Germination only takes place in less saline soils. Seedbanking: Soil samples taken from a Utah marsh show that numerous marsh plants have viable seeds stored in the soil. When soil samples taken from an saltgrass-dominated community at this marsh were placed in a greenhouse under conditions favorable for germination, 340 saltgrass seedlings per square meter of surface soil were produced [68]. Saltgrass seeds were also present in soil samples from other vegetation types within the same marsh. Seeds can remain dormant for at least 4 years [63]. Seedbanking may allow plants to become established in large numbers when favorable conditions for germination are met. Seed dispersal: Seeds are dispersed by wind and water [71]. SITE CHARACTERISTICS : Saltgrass attains best development in depressed areas that receive seasonal runoff or have water tables near the soil surface. Typical sites supporting lush saltgrass growth include prairie and grassland swales, salt flats, desert playas and valley bottoms, intermittent ponds, saline meadows, and along the borders of springs, streams and lakes. Soil characteristics are the most important factors influencing distribution. Saltgrass tends to form a dense sod only on soils that have a high salt content, a fine texture, and a good supply of soil moisture throughout the year. Soil attributes are summarized below: Salinity - Saltgrass tolerates a wide range of soil salinity. It occurs on highly saline and nonsaline soils. It has been found growing on soils ranging from .03 to 5.6 percent total salts [80]. Because many other grasses cannot survive in soils with high salinities, saltgrass is often a dominant, forming a sod with 2,000 to 3,000 stems per square meter, when the salt content of the soil becomes greater than about 0.33 to 0.5 percent [8,78,,80]. It can survive on sites where the soil surface is encrusted with a layer of salt. pH - Saltgrass is usually found on alkaline soils, with a pH between 7.5 and 8.5 [8,66,80,86]. Extremes in pH may range from 6.8 to 10.5 [40,83]. Texture - Soil textures vary from sand and gravel to clay, but saltgrass seems best adapted to medium- and fine-textured soils [63]. In the Great Plains, depressions and meadows dominated by saltgrass generally have soil textures ranging from fine clays to silt loams [35,36,86]. Moisture - Water tables are often near the surface. Some sites are periodically flooded and remain inundated in the spring. In Nebraska, saltgrass grew best in meadows where the water level was 16 to 36 inches (41-91 cm) below the soil surface [77]. Along the Rio Grande River in New Mexico, it was restricted to areas where the water table was within 4 feet (1.2 m) of the soil surface [9]. Soil-moisture gradient and associated communities: On an ancient lake bed in Ruby Valley, Nevada, plant distributions along a soil-moisture gradient were studied. In order of increasing depth to ground water, dominant species were baltic bulrush (Juncus balticus), saltgrass, shrubby cinquefoil (Potentilla fruiticosa), basin wildrye, black greasewood, and rubber rabbitbrush (Chrysothamnus nauseosus) [52]. In Montana, adjacent wetter communities tend to be dominated by hardstem bulrush (Scirpus acutus) and Nevada bulrush (S. nevadensis), while drier communities are often dominated by black greasewood or upland grasses [32,35]. In marshes along the Great Salt Lake in Utah, saltgrass is common in areas that periodically dry out. Adjacent wetter, less saline areas are dominated by cattails (Typha spp.), saltmarsh bulrush (Scirpus maritimus), hardstem bulrush, and reed (Phragmites australis) [73]. Associates: Associated grasses include alkaligrass (Puccinellia nuttalliana), foxtail barley (Hordeum jubatum), western wheatgrass (Pascopyrum smithii), alkali sacaton (Sporobolus airoides), plains bluegrass (Poa arida), Rocky Mountain glasswort (Salicornia rubra), and Pursh seepweed (Suada depressa) [32,47,80,86]. Flood tolerance: Saltgrass is very flood tolerant [56,63]. Plants grown in metal containers survived partial (plant crown covered) and total (entire plant underwater) inundation for 24 days. Although plants exhibited loss of vigor, they essentially recovered within 30 days after the water was drained [1]. Drought tolerance: Saltgrass has moderate to high drought tolerance [63]. It can remain dormant for long periods until rain or floodwaters replenish soil moisture [64]. Elevation: Elevational ranges for several western states are given below: below 6,000 feet (1,829 m) in AZ [40] from 3,500 to 9,000 feet (1,067-2,743 m) in CO [16] from 2,740 to 4,300 feet (835-1,311 m) in MT [16] below 6,500 feet (1,981 m) in NM [25] from 3,640 to 7,515 feet (1,010-2,290 m) in UT [85] from 4,000 to 7,500 feet ( 1,219-2,286 m) in WY [16] SUCCESSIONAL STATUS : Saltgrass is a pioneer species. It invades barren, saline soils that other grasses cannot tolerate. Its sharp-pointed rhizomes are well adapted to piercing heavy clays and shales [32]. Spreading by rhizomes allows saltgrass to colonize salt flats, inundated playas, lakeshores, shale cliffs, and other saline barren sites by extending from areas that are favorable for growth to areas that are less favorable [32,77,78]. Once established, it may aid in forming soils for the subsequent establishment of other plants. SEASONAL DEVELOPMENT : Saltgrass is a warm-season grass. It begins growth in the spring about 1 month later than cool-season grasses occurring in the same area. In eastern Washington, growth of new tillers begins in late April, and the shoots remain green all summer when upland grasses go into aestivation [14]. North Dakota plants were observed in full bloom in August [39]. Flowering in Montana occurs in June and July [16]. At Fish Springs National Wildlife Refuge in Utah, saltgrass phenology was observed on two areas of a saltmarsh. On portions of the marsh influenced by 80 degree Fahrenheit (27 deg C) spring water, saltgrass showed earlier phenological development [4]: date of initial growth date of anthesis warm spring salt marsh warm spring salt marsh water site site water site site April 2 April 14 May 30 June 10

FIRE ECOLOGY

SPECIES: Distichlis spicata | Saltgrass
FIRE ECOLOGY OR ADAPTATIONS : Saltgrass rhizomes occur deep in the soil where they are insulated from the heat of most fires. Temperatures ranging from 118 to 156 degrees Fahrenheit (48-69 deg C) never penetrated deeper than 1.5 inches (3.8 cm) into the soil during a prescribed fire on September 2, 1981 at a drained marsh at Ogden Bay, Utah [70]. Following the fire, there was no decrease in living saltgrass roots or rhizomes. Viable seeds of saltgrass may be stored in meadow soils. Soil samples taken before and after the aforementioned fire contained comparable numbers of viable saltgrass seeds [71]. Fire did not kill the saltgrass seeds stored in the soil, and many germinated after the fire. POSTFIRE REGENERATION STRATEGY : Rhizomatous herb, rhizome in soil Ground residual colonizer (on-site, initial community) Initial-offsite colonizer (off-site, initial community)

FIRE EFFECTS

SPECIES: Distichlis spicata | Saltgrass
IMMEDIATE FIRE EFFECT ON PLANT : Most fires consume the aboveground foliage of saltgrass. DISCUSSION AND QUALIFICATION OF FIRE EFFECT : NO-ENTRY PLANT RESPONSE TO FIRE : Saltgrass survives fire by sending up new growth from rhizomes. Increases in biomass following fire are common. The aboveground standing crop of saltgrass increased following a prescribed burn on April 15, 1981, in a black greasewood/inland saltgrass habitat type in eastern Oregon. One year following this prescribed burn, the aboveground standing crop of saltgrass averaged 550 grams per square meter on burned plots, but only 398 grams per square meter on unburned plots [88]. In the true prairie of eastern North Dakota, saltgrass responded favorably to a prescribed burn on May 8. Before the fire, saltgrass frequency was 100 percent, and it remained at 100 percent during the growing season following the fire [28]. Three months after the fire on August 4, saltgrass aboveground biomass was greater on burned plots (115.2 grams oven dry weight/m2) than unburned plots (76.8 grams oven dry weight/m2) [28]. Daubenmire [14] reported that a basin wildrye-saltgrass stand in eastern Washington was burned annually for many years by "clean-up crews" and that the plants remained healthy and in high vigor. On a Utah marsh where a dense stand of saltgrass was killed by a combination of fire and flooding, some seedlings emerged from seed stored in the soil [81]. DISCUSSION AND QUALIFICATION OF PLANT RESPONSE : NO-ENTRY FIRE MANAGEMENT CONSIDERATIONS : In many wildlife refuges, marsh vegetation is controlled by regulating water levels of the marsh. Although saltgrass rhizomes survive burning, they will be killed if saltgrass sites are flooded following burning [70]. Flooding after burning apparently kills saltgrass rhizomes by preventing gas exchange. Saltgrass is an important cover plant for nesting waterfowl, and control is seldom warranted in waterfowl production areas. New growth following fire is higher in nutritive quality than unburned plants. Nutritional information concerning saltgrass plants sampled before and after a September prescribed fire in a Utah marsh is presented below [74]: protein ash cellulose hemicelulose lignin before burning, 4/81 11.68 9.19 30.13 32.99 11.14 after burning, 4/82 17.83 10.79 26.59 34.98 10.83

REFERENCES

SPECIES: Distichlis spicata | Saltgrass
REFERENCES : 1. Aldon, Earl F. 1977. Survival of three grass species after inundation. Res. Note RM-344. Fort Collins CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Forest and Range Experiment Station. 2 p. [11218] 2. 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] 3. Blackburn, Wilbert H.; Eckert, Richard E., Jr.; Tueller, Paul T. 1969. Vegetation and soils of the Cow Creek Watershed. R-49. Reno, NV: University of Nevada, Agricultural Experiment Station. 77 p. In cooperation with: U.S. Department of the Interior, Bureau of Land Management. [458] 4. Bolen, Eric G. 1964. Plant ecology of spring-fed salt marshes in western Utah. Ecological Monographs. 34(2): 143-166. [11214] 5. Bomberger, Mary L. 1984. Quantitative assessment of the nesting habitat of Wilson's phalarope. Wilson Bulletin. 96(1): 126-128. [11426] 6. Bowman, R. A.; Mueller, D. M.; McGinnies, W. J. 1985. Soil and vegetation relationships in a Central Plains saltgrass meadow. Journal of Range Management. 38(4): 325-328. [11213] 7. Brotherson, Jack D. 1981. Aquatic and semiaquatic vegetation of Utah Lake and its bays. Great Basin Naturalist Memoirs. 5: 68-84. [11212] 8. Brotherson, Jack D. 1987. Plant community zonation in response to soil gradients in a saline meadow near Utah Lake, Utah County, Utah. Great Basin Naturalist. 47(2): 322-333. [10495] 9. Campbell, C. J.; Dick-Peddie, W. A. 1964. Comparison of phreatophyte communities on the Rio Grande in New Mexico. Ecology. 45(3): 492-502. [7003] 10. Cluff, Greg J.; Roundy, Bruce A. 1988. Germination responses of desert saltgrass to temperature and osmotic potential. Journal of Range Management. 41(2): 150-153. [11210] 11. Cluff, Greg J.; Roundy, Bruce A. 1988. Germination responses of desert saltgrass to temperature and osmotic potential. Journal of Range Management. 41(2): 150-153. [11210] 12. Costello, David F. 1944. Important species of the major forage types in Colorado and Wyoming. Ecological Monographs. 14: 107-134. [693] 13. Cronquist, Arthur; Holmgren, Arthur H.; Holmgren, Noel H.; [and others]. 1977. Intermountain flora: Vascular plants of the Intermountain West, U.S.A. Vol. 6. The Monocotyledons. New York: Columbia University Press. 584 p. [719] 14. Daubenmire, R. 1970. Steppe vegetation of Washington. Technical Bulletin 62. Pullman, WA: Washington State University, College of Agriculture, Washington Agricultural Experiment Station. 131 p. [733] 15. Delzell, Robert W. 1972. Desert saltgrass - a potential ground cover for intensive use areas. In: 25th Annual Meeting, Society for Range Management; [Date of conference unknown]; [Location of conference unknown]. [Place of publication unknown]. Society for Range Management: 26-27. [11421] 16. 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] 17. Eyre, F. H., ed. 1980. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters. 148 p. [905] 18. Fautin, Reed W. 1946. Biotic communities of the northern desert shrub biome in western Utah. Ecological Monographs. 16: 252-310. [913] 19. Fisher, Jack C., Jr. 1985. Use of native vegetation for dust control at Owens Dry Lake. In: Rieger, John P.; Steele, Bobbie A., eds. Proceedings of the native plant revegetation symposium; 1984 November 15; San Diego, CA. San Diego, CA: California Native Plant Society: 36-41. [3342] 20. 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] 21. Fraser, Joseph G.; Anderson, James E. 1980. Wear tolerance and regrowth between cuttings of some native grasses under two moisture levels. Res. Rep. 418. Las Cruces, NM: New Mexico State University, Agricultural Experiment Station. 5 p. [11425] 22. Frolik, A. L.; Shepherd, W. O. 1940. Vegetative composition and grazing capacity of a typical area of Nebraska sandhills rangeland. University of Nebraska Agricultural Experimental Station Research Bulletin. Number 117. 39 p. [5417] 23. Fuller, Robert D.; Nelson, Emily D. P.; Richardson, Curtis J. 1982. Reclamation of red mud (bauxite residues) using alkaline-tolerant grasses with organic amendments. Journal of Environmental Quality. 11(3): 533-539. [11424] 24. 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] 25. Gay, Charles W., Jr.; Dwyer, Don D. 1965. New Mexico range plants. Circular 374. Las Cruces, NM: New Mexico State University, Cooperative Extension Service. 85 p. [4039] 26. Gould, Frank W.; Shaw, Robert B. 1983. Grass systematics. 2d ed. College Station, TX: Texas A&M University Press. 397 p. [5667] 27. Great Plains Flora Association. 1986. Flora of the Great Plains. Lawrence, KS: University Press of Kansas. 1392 p. [1603] 28. Hadley, Elmer B. 1970. Net productivity and burning response of native eastern North Dakota prairie communities. American Midland Naturalist. 84(1): 121-135. [5434] 29. Hadley, E. B.; Buccos, R. P. 1967. Plant community composition and net primary production within a native eastern North Dakota prairie. American Midland Naturalist. 77: 116-127. [11422] 30. Hallsten, Gregory P.; Skinner, Quentin D.; Beetle, Alan A. 1987. Grasses of Wyoming. 3rd ed. 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Related categories for Species: Distichlis spicata | Saltgrass

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