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CEGL006866 Phragmites australis ssp. americanus Native Western Marsh

Type Concept Sentence: This marsh association is dominated by the native graminoid Phragmites australis ssp. americanus and is found in scattered locations in the Mojave Desert, southern Great Basin and likely Colorado Plateau within alkaline seep, stream, and lacustrine areas.


Common (Translated Scientific) Name: American Common Reed Native Western Marsh

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: The association forms an open to continuous herb layer that ranges from 20 to 90% cover with native graminoid Phragmites australis ssp. americanus characteristically dominant in the herbaceous layer. Other herbaceous species are present and commonly include Carex spp., Distichlis spicata, Schoenoplectus spp., and Typha spp. Shrubs may form a sparse layer (0-7% cover) that can include Suaeda moquinii and Ericameria nauseosa. Emergent trees are sometimes present with low cover (to 2%) and include Populus fremontii, Prosopis glandulosa, and non-native Tamarix spp. The association is known to occur commonly yet scattered in the Colorado Desert, Mojave Desert, and southern Great Basin within alkaline seep, stream, and lacustrine areas, including in Owens Valley, Saline Valley, Saratoga Spring, and other various seeps such as near Shoshone in Death Valley National Park, California and likely occurs in the Colorado Plateau. In the Mojave Desert, it is also found at the edge of Soda Lake and along spring-fed washes in the Granite Mountains in the Mojave National Preserve, California, and along Las Vegas Wash, near Salt Spring, and along channels at the west end of the lake near Northshore Road in Lake Mead National Recreation Area, in Arizona and Nevada. It occurs at low elevations, ranging from approximately 150 to 500 m, and averages 351 m. Slopes are typically very gentle (1 to 2°), allowing water to flow slowly or pool in areas. It is found primarily in alkaline seeps, streambeds/channels, and lake edges at various aspects. Soils range from clay, silt, to sandy loam, and are usually derived from alluvium.

Diagnostic Characteristics: Vegetation is dominated by Phragmites australis ssp. americanus usually with other native wetland species present.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: Across the western U.S., Phragmites australis has various genetic strains, including native (Phragmites australis ssp. americanus), introduced (Phragmites australis ssp. australis, Phragmites australis ssp. berlandieri) and hybrid (Phragmites australis ssp. americanus x australis) lineages. Introduced populations of Phragmites australis are invasive in or near major urban centers and associated with anthropogenic disturbance in wetlands and rivers. Within the NPS lands in the Mojave Desert, most stands are native and limited to naturally occurring, unmanaged freshwater and alkaline wetland sites; however, both hybrid and native stands occur along Las Vegas Wash (Lambert et al. 2016). Much of the community classification work with Phragmites australis did not identify the taxon to subspecies. Lambert et al. (2016) indicate that the Phragmites australis in the Colorado Plateau is native Phragmites australis ssp. americanus so vegetation classification work there needs to be reviewed and possibly changed to this association. For more information on native Phragmites australis ssp. americanus Saltonstall, P.M. Peterson & Soreng, including field key for identification, see Saltonstall et al. (2004), or see Saltonstall (2002) for information on invasion by non-native genotypes of Phragmites australis into North America.

Native North Americans have historically used Phragmites australis, and its distribution has been related to concentrations of tribes using this plant across an extensive area of the southwestern United States, including many remote locations such as desert springs. However, reduction or fragmentation of native stands in riparian and wetland areas with Phragmites are likely to occur due to droughts and drier climates in the southwestern U.S. (Kiviat and Hamilton 2001).

Similar NVC Types: No Data Available
note: No Data Available

Physiognomy and Structure: Tall perennial graminoid herbaceous vegetation that is <3 m in height.

Floristics: The vegetation is characterized by an open to continuous herb layer that ranges from 23 to 90%. The native perennial graminoid Phragmites australis ssp. americanus is dominant in the herbaceous layer but does not form monotypic stands (Saltonstall et al. 2004, Evens et al. 2014). Other herbaceous species are present and commonly include Ambrosia psilostachya, Anemopsis californica, Carex spp., Distichlis spicata, Glycyrrhiza lepidota, Iva axillaris, Juncus arcticus, Juncus cooperi, Juncus arcticus ssp. littoralis (= Juncus balticus), Mentha arvensis, Schoenoplectus americanus, Schoenoplectus acutus, Schoenoplectus californicus, Typha spp., and Xanthium strumarium. Shrubs may form a sparse layer (to 7% cover) that often includes Suaeda moquinii, Ericameria nauseosa, or Baccharis douglasii (Thomas et al. 2004, Evens et al. 2014). Emergent trees are sometimes present with low cover (to 2%) and include Populus fremontii, Prosopis glandulosa, and non-native Tamarix spp.

Dynamics:  The remoteness of many Phragmites australis ssp. americanus stands has likely reduced the potential for invasion by introduced taxa (Phragmites australis ssp. australis, Phragmites australis ssp. berlandieri) and hybrid (Phragmites australis ssp. americanus x australis) lineages which are commonly associated with more developed areas.

Environmental Description:  This marsh association is known to occur commonly yet scattered in the Mojave Desert, southern Great Basin and likely in the Colorado Plateau within alkaline seep, stream, and lacustrine areas, including in Saline Valley, Saratoga Spring, and other various seeps such as near Shoshone in Death Valley National Park, California. It is also found at the edge of Soda Lake and along spring-fed washes in the Granite Mountains in Mojave National Preserve, California, and along Las Vegas Wash, near Salt Spring, and along a concrete channel at the west end of the lake near Northshore Road in Lake Mead National Recreation Area, in Arizona and Nevada (Evens et al. 2014, Lambert et al. 2016). It occurs at low elevations, ranging from approximately -45 to 500 m (Thomas et al. 2004, Evens et al. 2014). Slopes are typically very gentle (1-2°), allowing water to flow slowly or pool in areas. It is found primarily in alkaline seeps, streambeds/channels, and lake edges at various aspects. Soils range from clay, silt, to sandy loam, and are usually derived from alluvium.

Geographic Range: This marsh association commonly occurs scattered within alkaline seep, stream, and lacustrine areas in the Colorado, Sonoran, and Mojave Deserts, cismontane southern and central California, southern Great Basin and likely occurs in the Colorado Plateau. The distribution may be influenced by historic Native American use (Kiviat and Hamilton 2001).

Nations: US

States/Provinces:  AZ, CA, NV




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Phragmites australis - Scirpus spp. Association (Keeler-Wolf and Vaghti 2000)
= Phragmites australis Association (Hickson and Keeler-Wolf 2007)
= Phragmites australis Mojave Association (Evens et al. 2014)
>< Phragmites australis Semipermanently Flooded Herbaceous Alliance (Thomas et al. 2004)

Concept Author(s): Evens et al. (2014)

Author of Description: G. Kittel and K.A. Schulz

Acknowledgements: No Data Available

Version Date: 07-26-18

  • Evens, J. M., K. Sikes, D. Hastings, and J. Ratchford. 2014. Vegetation alliance descriptions for Lake Mead National Recreation Area, Death Valley National Park and Mojave National Preserve. Unpublished report submitted to USDI National Park Service, Mojave Desert Network Inventory and Monitoring Program. California Native Plant Society, Sacramento, CA.
  • Hickson, D., and T. Keeler-Wolf. 2007. Vegetation and land use classification and map of the Sacramento-San Joaquin River Delta. Prepared for the Bay Delta Region, California Department of Fish and Game by the Vegetation Classification and Mapping Program, California Department of Fish and Game, Sacramento. 152 pp. plus appendices.
  • Keeler-Wolf, T., and M. Vaghti. 2000. Vegetation mapping of Suisun Marsh, Solano County, California. A report to the California Department of Water Resources. California Department of Fish and Game, California Natural Diversity Database, Sacramento, CA.
  • Kiviat, E., and E. Hamilton. 2001. Phragmites use by Native North Americans. Aquatic Botany 69:341-357. [https://www.researchgate.net/publication/222005691_Phragmites_use_by_Native_North_Americans]
  • Lambert, A., K. Saltonstall, R. Long, and T. L. Dudley. 2016. Biogeography of Phragmites australis lineages in the southwestern United States. Biological Invasions 18:2597-2617.
  • Lambertini, C. 2016. Heteroplasmy due to chloroplast paternal leakage: Another insight into Phragmites haplotypic diversity in North America. Biological Invasions 18(9):2443-2455. [http://dx.doi.org/10.1007/s10530-016-1193-3]
  • Rocchio, Joe. Personal communication. Ecologist. Washington Natural Heritage Program, Department of Natural Resources, Olympia, WA.
  • Saltonstall, K. 2002. Cryptic invasion by a non-native genotype of the common reed, Phragmites australis, into North America. Proceedings of the National Academy of Science 99:2445-2449.
  • Saltonstall, K., P. M. Peterson, and R. J. Soreng. 2004. Recognition of Phragmites australis subsp. americanus (Poaceae: Arundinoideae) in North America: Evidence from morphological and genetic anlyses. Sida 21:683-692.
  • Smith, J. P., Jr., and K. W. Allred. 2016. Phragmites australis. In Jepson Flora Project, editors. Jepson eFlora. [http://ucjeps.berkeley.edu/cgi-bin/get_IJM.pl?tid=37931] (accessed on November 18, 2016).
  • Thomas, K. A., T. Keeler-Wolf, J. Franklin, and P. Stine. 2004. Mojave Desert Ecosystem Program: Central Mojave vegetation mapping database. U.S. Geological Survey, Western Regional Science Center. 251 pp.
  • Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.