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Introductory

SPECIES: Phragmites australis | Common Reed
ABBREVIATION : PHRAUS SYNONYMS : Phragmites communis Trin. SCS PLANT CODE : PHAU7 COMMON NAMES : common reed giant reed giant reedgrass roseau roseau cane yellow cane cane TAXONOMY : The currently accepted scientific name of common reed is Phragmites australis (Cav.) Trin. ex Steudel [14,50]. There are no recognized subspecies, varieties, or forms. LIFE FORM : Graminoid FEDERAL LEGAL STATUS : No special status OTHER STATUS : NO-ENTRY COMPILED BY AND DATE : Ronald Uchytil, June 1992 LAST REVISED BY AND DATE : NO-ENTRY AUTHORSHIP AND CITATION : Uchytil, Ronald J. 1992. Phragmites australis. In: Remainder of Citation

DISTRIBUTION AND OCCURRENCE

SPECIES: Phragmites australis | Common Reed
GENERAL DISTRIBUTION : Common reed has a nearly worldwide distribution. It grows in North America, South America, Europe, Africa, and Australia. In North America, its range extends from Nova Scotia to British Columbia southward throughout most of the United States and Mexico. It is absent from some inland areas of the South Atlantic States [22,28,50]. ECOSYSTEMS : FRES11 Spruce - fir FRES15 Oak - hickory FRES16 Oak - gum - cypress FRES17 Elm - ash - cottonwood FRES18 Maple - beech - birch FRES21 Ponderosa pine FRES28 Western hardwoods FRES29 Sagebrush FRES35 Pinyon - juniper FRES36 Mountain grasslands FRES38 Plains grasslands FRES39 Prairie FRES41 Wet grasslands STATES : AL AZ AR CA CO CT DE FL GA ID IL IN IA KS LA ME MD MA MI MN MS MO MT NE NV NH NJ NM NY NC ND OH OK OR PA RI SC SD TN TX UT VT VA WV WA WI WY AB BC MB NB NF NS ON PQ SK MEXICO ADMINISTRATIVE UNITS : AMIS APIS ARCH ASIS BADL BIBE BICY BICA CACH CANY CACO CAHA CARE CHCU COLM CUVA DEVA DEWA DINO EVER FIIS GATE GLCA GRTE GUIS INDU ISRO JELA JOTR LAME LAMR MEVE NABR NERI OLYM ORPI PEFO RICH SAMO SLBE VAFO WUPA ZION 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 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 K037 Mountain-mahogany - oak scrub K038 Great Basin sagebrush K039 Blackbrush K040 Saltbush - greasewood K041 Creosotebush K049 Tule marshes 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 K070 Sandsage - bluestem prairie K074 Bluestem prairie K078 Southern cordgrass prairie K080 Marl - everglades K081 Oak savanna K092 Evergaldes K094 Conifer bog K096 Northeastern spruce - fir forest K098 Northern floodplain forest K099 Maple - basswood forest K100 Oak - hickory forest K106 Northern hordwoods K113 Southern floodplain forest SAF COVER TYPES : 5 Balsam fir 13 Black spruce - tamarack 25 Sugar maple - beech - yellow birch 26 Sugar maple - basswood 33 Red spruce - balsam fir 38 Tamarack 42 Bur oak 97 Atlantic white-cedar 101 Baldcypress 102 Baldcypress - tupelo 235 Cottonwood - willow 237 Interior ponderosa pine 239 Pinyon - juniper SRM (RANGELAND) COVER TYPES : NO-ENTRY HABITAT TYPES AND PLANT COMMUNITIES : Thoughout most of its range, common reed typically forms closed, monodominant stands along marsh and slough edges [3,16,31]. These stands are often dense, with up to 19 stems (live and dead) per square foot (200/sq m) [5]. In coastal marshes of the southeastern United States, common reed often codominates with big cordgrass (Spartina cynosuroides) along the upland edge of the marsh [28,34]. Publications describing common reed dominated communities are listed below: Plant ecology of spring-fed salt marshes in western Utah [3]. Riparian dominance types of Montana [16]. Plant associations of Region Two [23]. A preliminary classification of the natural vegetation of Colorado [1]. Plant communities in the marshlands of southeastern Louisiana [34]. Vegetation of a prairie marsh [31]. The vegetation of the Canadian prairie provinces III. Aquatic and semiaquatic vegetation [29]. The vegetation of the Canadian prairie provinces III. Aquatic and semiaquatic vegetation, Part 2. Freshwater marshes and bogs [30].

VALUE AND USE

SPECIES: Phragmites australis | Common Reed
WOOD PRODUCTS VALUE : NO-ENTRY IMPORTANCE TO LIVESTOCK AND WILDLIFE : Common reed is a high quality livestock forage during early growth stages. At this time it is readily eaten by cattle and horses and may be cut for hay. After maturity, however, it becomes tough and unpalatable [16,28]. Common reed is not an important wildlife food. Occasionally, seeds are eaten by waterfowl, and rhizomes and stems by muskrats [33]. PALATABILITY : Common reed is highly palatable to livestock and wildlife when plants are young and growing vigorously [16]. This period of high palatability lasts for only a few weeks in Manitoba [48]. After maturity common reed becomes unpalatable [28]. NUTRITIONAL VALUE : Common reed's energy value is rated as fair and its protein value as poor [7]. In the Southeast, livestock should be fed a protein supplement when grazing this grass in the winter [28]. COVER VALUE : Nesting cover: Common reed often grows in vast, unbroken stands along marsh edges. These stands are typically dense and impenetrable, and except for the stand edge, are of little value to nesting waterfowl. Ward [48,49] reported that the interior of large common reed stands at the Delta Marsh, Manitoba, were practically void of nesting ducks. Stand edges, however, were frequently used; 31 percent of 147 duck nests were found there. The most common duck species nesting in common reed edges were the mallard, lesser scaup, canvasback, ruddy duck, and redhead. Conversely, Cross [4] found that both the interior and edges of common reed stands provided poor waterfowl nesting habitat. She cited studies at Fish Springs National Wildlife Refuge (NWR), Utah, and at the Delta Marsh in Manitoba, where only 4 to 6 percent of duck nests were found in common reed, all near the stand edge. At Fish Springs NWR, only snowy egrets, black-crowned night herons, and yellow-headed blackbirds nested in the interior of common reed stands. Hiding and thermal cover: Common reed provides good cover for flightless adult ducks during their molting period [42,48]. Common reed's height and density make it useful as hiding and escape cover for big game species like deer [16,49]. VALUE FOR REHABILITATION OF DISTURBED SITES : Common reed is an excellent soil stabilizer and spreads rapidly. It is used in many wetland rehabilitation and stabilization projects. It is used to revegetate disturbed riparian areas, control shore erosion, stabilize river and canal banks, and reduce wave action on watershed structures. It is best established by spring transplanting of sprigs or plugs collected from local stands. The cultivar 'Shoreline' is available for use in the southern part of the Central Great Plains [25,45]. OTHER USES AND VALUES : A cosmopolitan species, common reed has been cultivated and used for many purposes around the world. In Europe, it is used as thatching, to make mats, and as fodder and bedding for cattle. The aerial stems are sometimes used as a cellulose source in the paper and textile industries [19]. Native peoples of the American Southwest used the stems to make arrow shafts, prayer sticks, weaving rods, pipestems, mats, screens, nets, and thatching [24]. They also used the rootstocks and seeds as food. In the Southwest, it is also used for lattices and in the construction of adobe huts [22]. MANAGEMENT CONSIDERATIONS : Control: Because of its undesirable qualities [see Cover Value], control of common reed in marshes managed for waterfowl is sometimes necessary. However, because waterfowl may benefit from mixing common reed with other marsh plant species or open water, complete eradication is seldom warranted [5]. Aerial applications of systemic herbicides applied when plants are actively growing can control common reed. Amitrole, dalapon, and glyphosate are the most effective. Some researchers have found that split applications at one-half the dosage, with the second application 15 to 30 days after the first, are more effective than a single application [5]. Mechanical control includes discing or plowing, crushing, mowing, and dredging. Summer mowing greatly reduces common reed on sites that become dry during the summer but is ineffective on sites that remain moist [48]. At the Delta Marsh in Manitoba, common reed was replaced by a shortgrass-sedge-thistle meadow after 3 successive years of summer mowing [48]. In Britain, cutting during July resulted in a 40 percent reduction in aboveground biomass the following growing season [19]. Grazing is not recommended as a control measure in waterfowl management areas because the amount of grazing needed to reduce stands would be detrimental to desirable plant species as well [5]. Grazing: Common reed is moderately tolerant of grazing, but prolonged heavy grazing tends to reduce the extent and size of stands [15]. For maximum production in the Southeast, no more than 50 percent of the current year's growth by weight should be grazed during the growing season [28].

BOTANICAL AND ECOLOGICAL CHARACTERISTICS

SPECIES: Phragmites australis | Common Reed
GENERAL BOTANICAL CHARACTERISTICS : Common reed is a tall, native, warm-season, perennial, sod-forming grass. The culms are erect, rigid, smooth, and hollow. They may be nearly 1 inch (2.5 cm) in diameter and from 6 to 13 feet (2-4 m) tall, terminating in a 12-inch-long (30 cm) dense panicle. Leaves arise from the culm and are mostly 10 to 20 inches long (25-50 cm) and 0.4 to 2 inches (1-5 cm) wide [13,14]. Common reed has an extensive rhizome network and occasionally produces stolons as well. Rhizome depth has been variously reported: (1) 18 to 39 inches (40-100 cm) [19]; (2) mostly between 4 and 12 inches (10-30 cm), but up to 39 inches (100 cm) [11]; and (3) mostly between 8 and 39 inches (20-100 cm), but up to 78 inches (200 cm) [5]. Roots grow down to a depth of about 3.3 feet (1 m) [5]. RAUNKIAER LIFE FORM : Cryptophyte REGENERATION PROCESSES : Common reed's primary mode of reproduction is vegetative. Its extensive rhizome network is responsible for the maintenance and expansion of existing stands. Annual rhizome lateral spread averaged 16 inches (40 cm) in common reed stands in Wisconsin [6]. In Europe, lateral rhizome spread has been as great as 3.3 to 6.6 feet (1-2 m) per year [20]. Stolons, which may grow up to 4.25 inches (10.8 cm) per day, are produced in young stands or over open water and further aid in rapid stand expansion [5,39]. Common reed is a relatively good seed producer. The seeds are dispersed by wind and water and become a part of the marsh seed bank. Seed banking can be important in establishing new plants in vegetation-free areas following marsh drawdown. However, seeds of common reed are much less abundant in the marsh seed bank that are seeds of other marsh emergents such as cattails (Typha spp.) and bulrushes (Scirpus spp.). Natural germination of common reed is uncommon, and successful seedling establishment is rare [39,41]. SITE CHARACTERISTICS : Common reed grows on level ground in freshwater marshes, oxbow lakes, swales, and backwater areas of river and streams. It also grows around springs and along pond and lake margins, streambanks, and irrigation ditches [16,28,42]. It does not grow in permanently standing water but rather is found on sites with high water tables or sites that are seasonally flooded with not more than 20 inches (50 cm) of water [3,31,39]. Soil: Common reed grows on most soil textures from fine clays to sandy loams and is somewhat tolerant of saline or alkaline conditions [16]. In southern Manitoba, it grows on soils with a pH ranging from 6.4 to 8.1 [39]. Associated species: Common reed typically grows in closed, monodominant stands but is sometimes associated with cattail, bulrush, and arrowhead (Sagittaria spp.) in wetter habitats, and with white-top grass (Scholochloa festucacea), thistle (Circium spp.), sedge (Carex spp.), dock (Rumex spp.), northern reedgrass (Calamagrostis inexpansa), reed canarygrass (Phalaris arundinacea), and American mannagrass (Glyceria grandis) in drier habitats [16,31]. SUCCESSIONAL STATUS : Common reed is an aggressive competitor. Once established it tends to outcompete and eliminate marsh species with similar habitat requirements to form large, unbroken, climax stands [5,8,49]. Common reed has replaced brackish water species in some coastal wetlands where the installation of tidal gates has resulted in decreased water salinity [9]. SEASONAL DEVELOPMENT : Common reed is a warm-season grass that begins growth in the late spring usually after the last frost. Shoots emerge in late May in southern Manitoba [43], in April or May in Connecticut [18], in February in the Southeast [28], and from April to June in Utah [5]. The period of shoot emergence may last from 1 to 3 months [5]. Large buds formed the previous fall are the first to emerge, with smaller buds emerging later [5]. The shoots are sensitive to frost. If killed by frost, one to three side shoots develop from the side of the frosted shoot [18]. Spring-formed buds are small and remain dormant below the soil surface, ready to emerge as a replacement crop following disturbance [5]. Following emergence, stems grow rapidly (up to 1.6 inches (4 cm) per day). In southern Manitoba stems attain their maximum height by the end of July and maximum biomass by mid-August [43]. The foliage stays green until frost in the fall, and thereafter becomes brittle and turns a pale yellow. Stems remain standing throughout the winter [5]. Time of flowering has been reported as follows: Colorado - July through September [7] North Dakota - August and September [7] Utah - mid-July through August [5] Wyoming - July through September [7] Great Plains - June to October, mostly July to September [14] New England - mid-August to late September [38]

FIRE ECOLOGY

SPECIES: Phragmites australis | Common Reed
FIRE ECOLOGY OR ADAPTATIONS : Common reed's rhizomes are deeply buried in soil and are often under water as well. The heat from most fires does not penetrate deep enough into the soil to injure these regenerative structures. For example, in drained common reed stands along the Great Salt Lake, Utah, soil temperatures at a depth of 1 inch (2.5 cm) did not exceed 118 degrees Fahrenheit (48 deg C) during an early September fire [40]. When fire consumes the aboveground foliage, new top-growth is initiated from the surviving rhizomes. POSTFIRE REGENERATION STRATEGY : Rhizomatous herb, rhizome in soil

FIRE EFFECTS

SPECIES: Phragmites australis | Common Reed
IMMEDIATE FIRE EFFECT ON PLANT : Flammability: Common reed stands are typically dense and contain much dead material. Standing dead canes and litter often constitute twice as much biomass as living shoots [39]. This abundant dead fuel carries fire well, allowing stands to burn during midsummer when the current year's shoots are green. At the Delta Marsh in Manitoba, spring, summer or fall burning removed more than 90 percent of living and dead plant material [43]. In a Nebraska common reed stand, a late February prescribed burn when the marsh was frozen removed all aboveground vegetation except for a 2- to 6-inch-tall (5-15 cm) stubble layer which apparently resulted from a vapor zone from accompanying steam [37]. Rhizome damage: Most fires cause little damage to common reed because the rhizomes are sufficiently protected by soil. Rhizomes can be damaged, however, by deep-burning fires which can occur when the soil is dry and the humidity of the litter and stembase is low. The effects of severe burning depend on the degree of damage inflicted upon the rhizomes. Following some severe fires, shoot emergence the following spring can be delayed for 1 to 2 months. The most damaging fires occur during drought years when entire peat layers can be consumed. This destroys the rhizomes and eliminates common reed from the area [21]. DISCUSSION AND QUALIFICATION OF FIRE EFFECT : NO-ENTRY PLANT RESPONSE TO FIRE : Most fires favor common reed. Fire removes the standing dead canes and accumulated litter, allowing the soil to warm up rapidly in the spring, which results in earlier shoot emergence [43]. Stands burned during the spring (before shoot emergence or during early growth stages), late summer or fall (plants green or dormant), or winter recover quickly; preburn stem density and biomass are attained within one growing season [44]. Although plants burned during the summer usually initiate new top-growth within a few days, stem density is greatly reduced, and stems regrow to only about half of normal height before killing frosts occur. Furthermore, early to midsummer burning during the peak of plant growth (when carbohydrate reserves are lowest) reduces stem density and aboveground biomass for two to four growing seasons [5,44,49]. DISCUSSION AND QUALIFICATION OF PLANT RESPONSE : At the Delta Marsh in Manitoba, common reed plots were burned on August 1, October 7, and May 11. The following spring, shoot emergence occurred on May 1 on fall- and summer-burned plots, on May 19 on spring-burned plots, and on May 26 on controls. At the end of the first full growing season following burning, total aboveground biomass increased on the spring-burned plots and remained unchanged on fall-burned plots. Biomass declined on the summer burn, but the decrease was short-lived. By the end of postfire year 2, aboveground biomass returned to preburn levels. In the stands burned on August 1, plants grew to 23 inches (58 cm) in height before they were killed by frost in late October [43,44]. Another study at the Delta Marsh used summer burning in conjunction with marsh drainage in an attempt to thin dense common reed stands [49]. Following a fire on July 21, stems grew to 4 inches (10 cm) in height within 10 days after burning, and reached 23 inches (60 cm) in height before being killed by frost. During the second growing season plants grew to 50 inches (126 cm) in height, but stem density was 80 percent below normal. Stem density remained lowered even after three growing seasons. When measured in June, stem density increased or remained stable in common reed stands burned the previous June 15, August 6, or August 24 in a Utah marsh. However, stem density was 25 to 50 percent less than unburned controls on sites burned June 29, July 13, or July 27. FIRE MANAGEMENT CONSIDERATIONS : The best way to reduce common reed with prescribed burning is to burn during the summer when carbohydrate reserves in the plant are low and when the soil is dry [21]. From a wildlife standpoint, this opens up the stands, making them more attractive to waterfowl [49]. Using summer burning to completely eliminate common reed is difficult. "Root burns", in which prescribed fires burn deeply into organic soils and consume the rhizomes, will probably only work on marshes where the water can be completely drained or on marshes experiencing severe drought [26]. In Utah, dalapon applied as an aerial spray 48 days after midsummer burning effectively controlled common reed [4].

REFERENCES

SPECIES: Phragmites australis | Common Reed
REFERENCES : 1. Baker, William L. 1984. A preliminary classification of the natural vegetation of Colorado. Great Basin Naturalist. 44(4): 647-676. [380] 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. Bolen, Eric G. 1964. Plant ecology of spring-fed salt marshes in western Utah. Ecological Monographs. 34(2): 143-166. [11214] 4. Cross, Diana Harding. 1983. Wildlife habitat improvement by control of Phragmites communis with fire and herbicide. Fort Collins, CO: Colorado State University. 81 p. Thesis. [18403] 5. Cross, Diana H.; Fleming, Karen L. 1989. Control of phragmites or common reed. Fish and Wildlife Leaflet 13.4.12. Washington, DC: U.S. Department of the Interior, Fish and Wildlife Service. 5 p. [18396] 6. Curtis, John T. 1959. The vegetation of Wisconsin. Madison, WI: The University of Wisconsin Press. 657 p. [7116] 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. Dix, R. L.; Smeins, F. E. 1967. The prairie, meadow, and marsh vegetation of Nelson County, North Dakota. Canadian Journal of Botany. 45: 21-58. [5528] 9. Dobberteen, Ross A.; Jarman, Nancy M. 1991. Restoration underway in a common reed-dominated salt marsh. Restoration & Management Notes. 9(1): 41. [15703] 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. Fiala, Karel. 1976. Underground organs of Phragmites communis, their growth, biomass and net production. Folia Geobotanica & Phytotaxonomica. 11: 25-259. [18398] 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. Godfrey, Robert K.; Wooten, Jean W. 1979. Aquatic and wetland plants of southeastern United States: Monocotyledons. Athens, GA: The University of Georgia Press. 712 p. [16906] 14. Great Plains Flora Association. 1986. Flora of the Great Plains. Lawrence, KS: University Press of Kansas. 1392 p. [1603] 15. 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] 16. Hansen, Paul L.; Chadde, Steve W.; Pfister, Robert D. 1988. Riparian dominance types of Montana. Misc. Publ. No. 49. Missoula, MT: University of Montana, School of Forestry, Montana Forest and Conservation Experiment Station. 411 p. [5660] 17. Harris, Stanley W.; Marshall, William H. 1960. Experimental germination of seed and establishment of seedlings of Phragmites communis. Journal of Ecology. 41: 395. [16679] 18. Haslam, Sylvia M. 1969. The development and emergence of buds in Phragmites communis Trin. Annals of Botany. 33: 289-301. [16685] 19. Haslam, S. M. 1972. Biological flora of the British Isles: Phragmites communis Trin. Journal of Ecology. 60: 585-610. [16676] 20. Haslam, S. M. 1973. Some aspects of the life history and autecology of Phragmites communis Trin.: A review. Polish Archives of Hydrobiology. 20(1): 79-100. [17261] 21. Higgins, Kenneth F.; Kruse, Arnold D.; Piehl, James L. 1989. Effects of fire in the Northern Great Plains. Ext. Circ. EC-761. Brookings, SD: South Dakota State University, Cooperative Extension Service, South Dakota Cooperative Fish and Wildlife Research Unit. 47 p. [14749] 22. Hitchcock, A. S. 1951. Manual of the grasses of the United States. Misc. Publ. No. 200. Washington, DC: U.S. Department of Agriculture, Agricultural Research Administration. 1051 p. [2nd edition revised by Agnes Chase in two volumes. New York: Dover Publications, Inc.]. [1165] 23. Johnston, Barry C. 1987. Plant associations of Region Two: Potential plant communities of Wyoming, South Dakota, Nebraska, Colorado, and Kansas. 4th ed. R2-ECOL-87-2. Lakewood, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Region. 429 p. [3519] 24. Kearney, Thomas H.; Peebles, Robert H.; Howell, John Thomas; McClintock, Elizabeth. 1960. Arizona flora. 2d ed. Berkeley, CA: University of California Press. 1085 p. [6563] 25. Knutson, P. L.; Woodhouse, W. W., Jr. 1983. Shore stabilization with salt marsh vegetation. Special Rep. 9. U.S. Department of Defence, Army Corps of Engineers. Microfiche. [18063] 26. Kruse, Arnold D.; Higgins, Kenneth F. 1990. Effects of prescribed fire upon wildlife habitat in northern mixed-grass prairie. In: Alexander, M. E.; Bisgrove, G. F., technical coordinators. The art and science of fire management: Proceedings, 1st Interior West Fire Council annual meeting and workshop; 1988 October 24-27; Kananaskis Village, AB. Inf. Rep. NOR-X-309. Edmonton, AB: Forestry Canada, Northwest Region, Northern Forestry Centre: 182-193. [14146] 27. 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] 28. Leithead, Horace L.; Yarlett, Lewis L.; Shiflet, Thomas N. 1971. 100 native forage grasses in 11 southern states. Agric. Handb. 389. Washington, DC: U.S. Department of Agriculture, Forest Service. 216 p. [17551] 29. Looman, J. 1981. The vegetation of the Canadian prairie provinces. III. Aquatic and semi-aquatic vegetation. Phytocoenologia. 9(4): 473-497. [18401] 30. Looman, J. 1982. The vegetation of the Canadian prairie provinces. III. Aquatic and semi-aquatic vegetation, Part 2. Freshwater marshes and bogs. Phytocoenologia. 10(4): 401-423. [18402] 31. Love, Askell; Love, Doris. 1954. Vegetation of a prairie marsh. Bulletin of the Torrey Botanical Club. 81(1): 16-34. [18103] 32. 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] 33. Martin, Alex C.; Erickson, Ray C.; Steenis, John H. 1957. Improving duck marshes by weed control. Circular 19 (Revised). Washington, DC: U.S. Department of the Interior, Bureau of Sport Fisheries and Wildlife. 60 p. [16324] 34. Penfound, W. T.; Hathaway, Edward S. 1938. Plant communities in the marshlands of southeastern Louisiana. Ecological Monographs. 8(1): 3-56. [15089] 35. Raunkiaer, C. 1934. The life forms of plants and statistical plant geography. Oxford: Clarendon Press. 632 p. [2843] 36. Riemer, Donald N. 1971. Effects of split applications of dalapon on phragmites. Proceedings of the Northeastern Weed Control Conference. 25: 65-70. [18399] 37. Schlichtemeier, Gary. 1967. Marsh burning for waterfowl. In: Proceedings, 6th annual Tall Timbers fire ecology conference; 1967 March 6-7; Tallahassee, FL. No. 6. Tallahassee, FL: Tall Timbers Research Station: 40-46. [16450] 38. Seymour, Frank Conkling. 1982. The flora of New England. 2d ed. Phytologia Memoirs 5. Plainfield, NJ: Harold N. Moldenke and Alma L. Moldenke. 611 p. [7604] 39. Shay, Jennifer M.; Shay, C. Thomas. 1986. Prairie marshes in western Canada, with specific reference to the ecology of five emergent macrophytes. Canadian Journal of Botany. 64: 443-454. [18397] 40. Smith, Loren Michael. 1983. Effects of prescribed burning on the ecology of a Utah marsh. Logan, UT: Utah State University. 159 p. Dissertation. [10218] 41. Smith, Loren M.; Kadlec, John A. 1983. Seed banks and their role during drawdown of a North American marsh. Journal of Applied Ecology. 20: 673-684. [11196] 42. Swanson, George A.; Duebbert, Harold F. 1989. Wetland habitats of waterfowl in the prairie pothole region. In: van der Valk, Arnold, ed. Northern prairie wetlands. Ames, IA: Iowa State University Press: 228-267. [15218] 43. Thompson, D. J.; Shay, J. M. 1985. The effects of fire on Phragmites australis in the Delta Marsh, Manitoba. Canadian Journal of Botany. 63: 1864-1869. [11481] 44. Thompson, D. J.; Shay, Jennifer M. 1989. First-year response of a Phragmites marsh community to seasonal burning. Canadian Journal of Botany. 67: 1448-1455. [7312] 45. Thornburg, Ashley A. 1982. Plant materials for use on surface-mined lands. SCS-TP-157. Washington, DC: U.S. Department of Agriculture, Soil Conservation Service. 88 p. [3769] 46. 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] 47. Toorn, J. van der; Mook, J. H. 1982. The infl. of environ. factors & mgt. on stands of Phragmites australis. 1. Eff. of burning, frost & insect damage on shoot density & shoot size. Journal of Applied Ecology. 19: 477-499. [16320] 48. Ward, Edward. 1942. Phragmites management. Transactions, 7th North American Wildlife Conference. 7: 294-298. [14959] 49. Johnsgard, Paul A. 1983. The grouse of the world. Lincoln, NE: University of Nebraska. 413 p. [18404] 50. Welsh, Stanley L.; Atwood, N. Duane; Goodrich, Sherel; Higgins, Larry C., eds. 1987. A Utah flora. Great Basin Naturalist Memoir No. 9. Provo, UT: Brigham Young University. 894 p. [2944] 51. 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. 7 p. [20090]

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