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A3180 Atriplex obovata - Atriplex cuneata Scrub Alliance

Type Concept Sentence: This alliance occurs in the northern Chihuahuan Desert and Colorado Plateau from western Texas, south-central and northwestern New Mexico, and northeastern Arizona and is dominated or codominated by Atriplex obovata.


Common (Translated Scientific) Name: Mound Saltbush - Valley Saltbush Scrub Alliance

Colloquial Name: Mound Saltbush - Valley Saltbush Scrub

Hierarchy Level:  Alliance

Type Concept: This alliance occurs in the northern Chihuahuan Desert and Colorado Plateau from western Texas, south-central and northwestern New Mexico, and northeastern Arizona. The vegetation is characterized by a sparse to moderately dense dwarf-shrub layer that is dominated or codominated by Atriplex obovata. Some occurrences may have a dense understory of perennial grasses. Shrub associates may include scattered Atriplex confertifolia, Ericameria nauseosa, Isocoma drummondii, Gutierrezia sarothrae, Prosopis glandulosa var. torreyana, Opuntia spp., or Suaeda spp. The herbaceous layer ranges from moderately dense to absent, and is usually dominated by perennial grasses such as Sporobolus airoides and Pleuraphis jamesii. Other associated species may include Achnatherum hymenoides, Bouteloua gracilis, Elymus elymoides, and Sporobolus cryptandrus. Stands are known from mesas, plains, floodplains, valley bottoms, alluvial flats, lower to upper hillslopes, often in a "badlands" landscape. Soils are generally shallow, poorly developed, and alkaline.

Diagnostic Characteristics: Shrub and shrub-herbaceous scrub vegetation where Atriplex obovata is the principal shrub with cover of 10-60%. Pleuraphis jamesii and Sporobolus airoides typically form an open to dense herbaceous layer.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This alliance includes associations which are considered shrub-dominated, as well as one that is considered shrub-herbaceous which was previous attributed to former Sporobolus airoides - (Pleuraphis jamesii) Shrub Herbaceous Alliance (A.1532).

This alliance often occurs in "badlands" landscapes adjacent to barren and sparsely vegetated areas and may include vegetation that may be too sparse to be classified as a dwarf-shrubland. Further study is needed throughout its range, especially to assess the effects of livestock grazing on vegetation structure.

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

Physiognomy and Structure: Vegetation in this alliance is dominated by sparse to moderate cover of facultatively deciduous dwarf-shrubs with a sparse to dense perennial graminoid layer.

Floristics: The vegetation is characterized by a sparse to locally moderately dense dwarf-shrub layer (10-60% cover) that is dominated or codominated by Atriplex obovata (3-40% cover). Shrub associates may include scattered Atriplex confertifolia, Atriplex canescens, Artemisia bigelovii, Ericameria nauseosa, Gutierrezia sarothrae, Isocoma drummondii, Opuntia spp., Prosopis glandulosa var. torreyana, or Suaeda spp. The herbaceous layer ranges from moderately dense to absent (0-50% cover) and is usually dominated by perennial grasses such as Sporobolus airoides and Pleuraphis jamesii. Other associated species may include Achnatherum hymenoides, Bouteloua gracilis, Elymus elymoides, and Muhlenbergia torreyi. Forb cover is sparse and typically includes Astragalus spp. and Sphaeralcea coccinea.

Dynamics:  Grazing has significantly impacted much of the vegetation in the Rio Puerco basin of northwestern New Mexico, which has had a long history of settlement and heavy livestock use. With proper livestock management and time, palatable species such as Sporobolus airoides may increase and Opuntia spp. may decline (Francis 1986).

Environmental Description:  Elevation ranges from 1500-1850 m. Stands are known from mesas, plains, floodplains, valley bottoms, alluvial flats, lower to upper hillslopes, often in a "badlands" landscape. Soils are generally shallow, poorly developed, and alkaline. Textures range from fine sandy loam to silty clay loam and clay (Henrickson 1974, Francis 1986, TNC 1997b) which are often saline or gypseous. Parent materials include alluvium and colluvium derived from igneous or sedimentary materials such as basalt, shale, and clay. There is high cover of bare soil. Typically, areas have been severely degraded by erosion.

Geographic Range: Communities in this alliance are described from the southeastern part of the Colorado Plateau in the upper Rio Puerco watershed in northwestern New Mexico and Arizona; the Trans-Pecos region in Brewster County, western Texas; and in south-central New Mexico. The alliance probably also occurs in Utah and Chihuahua and Coahuila, Mexico.

Nations: MX?,US

States/Provinces:  AZ, MXCHH?, MXCOA, NM, TX, UT




Confidence Level: Moderate

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: No Data Available

Concept Author(s): M. Hall, in Faber-Langendoen et al. (2013)

Author of Description: M.E. Hall

Acknowledgements: No Data Available

Version Date: 01-08-14

  • Faber-Langendoen, D., J. Drake, M. Hall, G. Kittel, S. Menard, C. Nordman, M. Pyne, M. Reid, M. Russo, K. Schulz, L. Sneddon, K. Snow, and J. Teague. 2013-2019b. Screening alliances for induction into the U.S. National Vegetation Classification: Part 1 - Alliance concept review. NatureServe, Arlington, VA.
  • Francis, R. E. 1986. Phyto-edaphic communities of the Upper Rio Puerco Watershed, New Mexico. Research Paper RM-272. USDA Forest Service, Rocky Mountain Forest and Range Experiment Station, Fort Collins, CO. 73 pp.
  • Henrickson, J. 1974. Saline habitats and halophytic vegetation of the Chihuahuan Desert region. Pages 249-272 in: R. H. Wauer and D. H. Riskind, editors. Transactions of the symposium on the biological resources of the Chihuahuan Desert region, United States and Mexico. USDI National Park Service. Transactions of Proceedings Series No. 3. Washington, DC.
  • Reid, M. S., L. S. Engelking, and P. S. Bourgeron. 1994. Rare plant communities of the conterminous United States, Western Region. Pages 305-620 in: D. H. Grossman, K. L. Goodin, and C. L. Reuss, editors. Rare plant communities of the conterminous United States, an initial survey. The Nature Conservancy, Arlington, VA.
  • TNC [The Nature Conservancy]. 1997b. An alliance level classification of the vegetation of the southeastern United States. Unpublished report. The Nature Conservancy, Southeast Conservation Science Department, Southeast Regional Office, Chapel Hill, NC.
  • Thomas, K., M. Hansen and C. Seger. 2003b. Vegetation of Petrified Forest National Park, Part I: Vegetation of Petrified Forest National Park. Southwest Biological Science Center, U.S. Geological Survey unpublished report to Petrified Forest National Park.
  • Welsh, S. L., N. D. Atwood, S. Goodrich, and L. C. Higgins, editors. 1987. A Utah flora. Great Basin Naturalist Memoirs 9. Provo, UT. 894 pp.
  • West, N. E., R. T. Moore, K. A. Valentine, L. W. Law, P. R. Ogden, F. C. Pinkney, P. T. Tueller, and A. A. Beetle. 1972. Galleta: Taxonomy, ecology and management of Hilaria jamesii on western rangelands. Utah Agricultural Experiment Station. Bulletin 487. Logan, UT. 38 pp.