Print Report

CEGL002654 Betula occidentalis / Mesic Graminoids Wet Shrubland

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Water Birch / Mesic Graminoids Wet Shrubland

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: This shrubland association often occurs as dense bands up to 35 m wide along moderately wide to wide floodplains in mountain valleys of Colorado, Nevada and Utah. Stands also occur in small patches at higher elevations and around seeps and isolated springs on hillslopes away from the valley bottom. These shrublands are characterized by bands of vegetation dominated by Betula occidentalis (40-60% canopy cover) but often including Ribes inerme and Salix bebbiana. This vegetation may extend well way from the channel edge in deep pockets of sandy loam soils. Alnus incana may be codominant. Picea pungens and Juniperus scopulorum may also be present but usually with low cover. Stands with a dense shrub layer may have a limited (<10%) but diverse herbaceous cover. Graminoids typically dominate the herbaceous layer where the most abundant species usually include Carex pellita, Carex deweyana, or Carex nebrascensis. Deschampsia cespitosa and Carex utriculata are often present as well. Forb cover often includes Achillea millefolium, Cardamine cordifolia, Heracleum maximum, Maianthemum stellatum, and Vicia americana. Scouring rushes (Equisetum spp.) may also have significant cover. The introduced grasses Agrostis stolonifera and Poa pratensis may be present in disturbed stands. Diagnostic of this association is the dominance of Betula occidentalis in the shrub layer and the dominance of mesic graminoids in the herbaceous layer.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This plant association has been documented in Nevada, Colorado and Utah. It occurs at slightly lower elevations and on lower-gradient stream reaches than Alnus incana. Presence of coniferous trees in the canopy of some stands may indicate that the stand will become a tree-dominated type. It occupies wetter sites than ~Betula occidentalis / Maianthemum stellatum Wet Shrubland (CEGL001162)$$.

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

Physiognomy and Structure: No Data Available

Floristics: These shrublands are characterized by bands of vegetation along streams that are dominated by Betula occidentalis (40-60% canopy cover) with a lush mesic graminoid understory. Other shrubs present often include Acer glabrum, Ribes inerme, Rosa woodsii, Rhus trilobata, Salix bebbiana, Salix exigua, or Salix lutea. Alnus incana may be codominant. Picea pungens, Populus angustifolia, and Juniperus scopulorum may also be present but usually with low cover. Stands with a dense shrub layer may have a limited (<10%) but diverse herbaceous cover. Graminoids typically dominate the herbaceous layer where the most abundant species usually include Agrostis gigantea, Carex pellita (= Carex lanuginosa), Carex deweyana, or Carex nebrascensis. Calamagrostis canadensis, Carex utriculata, Deschampsia cespitosa, Eleocharis palustris, and Glyceria striata are often present as well. Forb cover is typically low. Achillea millefolium, Cardamine cordifolia, Heracleum maximum, Maianthemum stellatum, Mimulus guttatus, Rudbeckia laciniata, and Vicia americana are common associates (Manning and Padgett 1995, Kittel et al. 1999b, Carsey et al. 2003a, 2003b). Scouring rushes (Equisetum arvense, Equisetum laevigatum, Equisetum hyemale) may also have significant cover. The introduced grasses and forbs Agrostis stolonifera, Phleum pratense, Poa pratensis, and Taraxacum officinale are common in disturbed stands. Large, near-pristine stands are rare.

Dynamics:  This association requires a high water table throughout the growing season in order to persist. In stands where the water table has dropped or the stream has incised, the understory becomes less dense and shifts from wetland species-dominated to mesic species such as Maianthemum stellatum and Clematis ligusticifolia.

Environmental Description:  This lower montane riparian shrubland association is found in mountain valleys and canyons in Colorado, Nevada and probably Utah, from 1600-2530 m (5250-8300 feet) elevation. Streams were classified as wide, meandering, and cobble-bottomed (Rosgen''s Channel Type: C3) (Rosgen 1996, Kittel et al. 1999b). Stands often occur as dense bands up to 35 m wide along streams in moderately wide to wide floodplains. Sites are often floodplains, stream terraces and benches, but it may also occur in smaller patches around seeps and isolated springs on hillslopes to 35 m away from the valley bottom (Manning and Padgett 1995). Substrates are relatively deep, organic or more commonly moderately well-drained to poorly drained mineral soils. Soil textures range from sandy loam to clay loam with signs of mottling within the top 30 cm (12 inches), and soils are saturated all or most of the growing season (Manning and Padgett 1995, Kittel et al. 1999b, Carsey et al. 2003a, 2003b).

Geographic Range: This shrubland association often occurs as dense bands along moderately wide to wide floodplains in mountain valleys of Colorado, Nevada, and Utah.

Nations: US

States/Provinces:  CO, NV, UT




Confidence Level: Moderate

Confidence Level Comments: No Data Available

Grank: G3

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: >< Betula occidentalis / Poa pratensis Community Type (Padgett et al. 1989) [This type is considered to be a grazing-induced community and is dominated by non-native grasses in the understory.]
= Betula occidentalis / Mesic Graminoid Community Type (Manning and Padgett 1995)
= Betula occidentalis / Mesic Graminoid Plant Association (Kittel et al. 1999b)
= Betula occidentalis / Mesic Graminoid Shrubland (Carsey et al. 2003a)
= Betula occidentalis / Mesic Graminoid Shrubland (Carsey et al. 2003b)
>< Betula occidentalis Community Type (Hansen et al. 1995) [This type is considered to be a grazing-induced community and is dominated by non-native grasses in the understory.]
>< Betula occidentalis Community Type (Hall and Hansen 1997) [This type is considered to be a grazing-induced community and is dominated by non-native grasses in the understory.]

Concept Author(s): A.E. Black

Author of Description: A.E. Black, K.A. Schulz and J. Coles

Acknowledgements: No Data Available

Version Date: 10-12-05

  • Bourgeron, P. S., and L. D. Engelking, editors. 1994. A preliminary vegetation classification of the western United States. Unpublished report. The Nature Conservancy, Western Heritage Task Force, Boulder, CO. 175 pp. plus appendix.
  • CNHP [Colorado Natural Heritage Program]. 2006-2017. Tracked natural plant communities. Colorado Natural Heritage Program, Colorado State University, Fort Collins. [https://cnhp.colostate.edu/ourdata/trackinglist/plant_communities/]
  • Carsey, K., D. Cooper, K. Decker, D. Culver, and G. Kittel. 2003b. Statewide wetlands classification and characterization: Wetland plant associations of Colorado. Prepared for Colorado Department of Natural Resources, Denver, by Colorado Natural Heritage Program, College of Natural Resources, Colorado State University, Fort Collins. 79 pp. [http://www.cnhp.colostate.edu/documents/2003/wetland_classification_final_report_2003.pdf]
  • Carsey, K., G. Kittel, K. Decker, D. J. Cooper, and D. Culver. 2003a. Field guide to the wetland and riparian plant associations of Colorado. Colorado Natural Heritage Program, Fort Collins, CO.
  • Cogan, D., J. E. Taylor, and K. Schulz. 2012. Vegetation inventory project: Great Basin National Park. Natural Resource Report NPS/MOJN/NRR--2012/568. National Park Service, Fort Collins, CO. 373 pp.
  • Coles, J., D. Cogan, D. Salas, A. Wight, G. Wakefield, J. Von Loh, and A. Evenden. 2008a. Vegetation classification and mapping project report, Dinosaur National Monument. Natural Resource Technical Report NPS/NCPN/NRTR-2008/112. National Park Service, Fort Collins, CO. 814 pp.
  • Hall, J. B., and P. L. Hansen. 1997. A preliminary riparian habitat type classification system for the Bureau of Land Management districts in southern and eastern Idaho. Riparian and Wetland Research Program, School of Forestry, University of Montana. Idaho Bureau of Land Management, Technical Bulletin No. 97-11. 381 pp.
  • Hansen, P. L., R. D. Pfister, K. Boggs, B. J. Cook, J. Joy, and D. K. Hinckley. 1995. Classification and management of Montana''s riparian and wetland sites. Miscellaneous Publication No. 54. Montana Forest and Conservation Experiment Station, School of Forestry, University of Montana. 646 pp. plus posters.
  • Kittel, G. M., and N. D. Lederer. 1993. A preliminary classification of the riparian vegetation of the Yampa and San Miguel/Dolores river basins. Unpublished report prepared for Colorado Department of Health and the Environmental Protection Agency by The Nature Conservancy, Colorado Field Office, Boulder.
  • Kittel, G., E. Van Wie, M. Damm, R. Rondeau, S. Kettler, A. McMullen, and J. Sanderson. 1999b. A classification of riparian and wetland plant associations of Colorado: A user''s guide to the classification project. Colorado Natural Heritage Program, Colorado State University, Fort Collins CO. 70 pp. plus appendices.
  • Kittel, G., E. Van Wie, M. Damm, R. Rondeau, S. Kettler, and J. Sanderson. 1999a. A classification of the riparian plant associations of the Rio Grande and Closed Basin watersheds, Colorado. Unpublished report prepared by the Colorado Natural Heritage Program, Colorado State University, Fort Collins.
  • Kittel, G., R. Rondeau, N. Lederer, and D. Randolph. 1994. A classification of the riparian vegetation of the White and Colorado River basins, Colorado. Final report submitted to Colorado Department of Natural Resources and the Environmental Protection Agency. Colorado Natural Heritage Program, Boulder. 166 pp.
  • Kittel, G., R. Rondeau, and S. Kettler. 1995. A classification of the riparian vegetation of the Gunnison River Basin, Colorado. Submitted to Colorado Department of Natural Resources and the Environmental Protection Agency. Prepared by Colorado Natural Heritage Program, Fort Collins. 114 pp.
  • Manning, M. E., and W. G. Padgett. 1995. Riparian community type classification for Humboldt and Toiyabe national forests, Nevada and eastern California. USDA Forest Service, Intermountain Region. 306 pp.
  • Padgett, W. G., A. P. Youngblood, and A. H. Winward. 1989. Riparian community type classification of Utah and southeastern Idaho. Research Paper R4-ECOL-89-0. USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT.
  • Richard, C., G. Kittel, and S. Kettler. 1996. A classification of the riparian vegetation of the San Juan National Forest. Draft 1 report. Colorado Natural Heritage Program, Colorado State University, Fort Collins.
  • Rosgen, D. 1996. Applied river morphology. Wildland Hydrology, Pagosa Springs, CO.
  • Salas, D., J. Stevens, and K. Schulz. 2005. USGS-NPS Vegetation Mapping Program: Rocky Mountain National Park, Colorado. Technical Memorandum No. 8260-05-02. USDI Bureau of Reclamation, Denver, CO. 161 pp. plus Appendices A-L (733 pp.).
  • Schulz, K. A., and M. E. Hall. 2011. Vegetation inventory project: Great Basin National Park. Unpublished report submitted to USDI National Park Service, Mojave Desert Inventory and Monitoring Network. NatureServe, Western Regional Office, Boulder, CO. 30 pp. plus Appendices A-H.
  • Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.