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A3419 Pinus ponderosa / Grass Understory Southern Rocky Mountain Open Woodland Alliance

Type Concept Sentence: These woodlands are characterized by widely spaced canopies dominated by Pinus ponderosa primarily occurring in the southern Rocky Mountains and extending into adjacent ecoregions.


Common (Translated Scientific) Name: Ponderosa Pine / Grass Understory Southern Rocky Mountain Open Woodland Alliance

Colloquial Name: Southern Rocky Mountain Ponderosa Pine / Grass Open Woodland

Hierarchy Level:  Alliance

Type Concept: These woodlands are characterized by widely spaced canopies primarily dominated by Pinus ponderosa in association with other conifers, including Juniperus spp., Pinus discolor, Pinus edulis, and Pseudotsuga menziesii. The typically moderately dense herbaceous layer has greater cover than the shrub layer and is dominated by graminoids. The most common dominant graminoids include Andropogon gerardii, Bouteloua gracilis, Festuca arizonica, Muhlenbergia montana, Muhlenbergia straminea, and Schizachyrium scoparium. These woodlands occur from the central and southern Rocky Mountains, extending south to the mountains of western Texas, escarpments of the Great Plains and west to the Mogollon Rim and Colorado Plateau. Stands occur on bottomlands, elevated plains, cinder cones, piedmont slopes, mesas, foothills, and mountains at elevations ranging from 1700-2900 m.

Diagnostic Characteristics: This alliance is dominated by well-spaced Pinus ponderosa. The diagnostic feature of this alliance is the depauperate shrub layer with cover typically <5% and dense herbaceous understory predominantly dominated by fire-resistant grasses.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: No Data Available

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

Physiognomy and Structure: These are widely spaced woodland stands of needle-leaved evergreen trees 10-30 m in height. Associated trees are primarily needle-leaved evergreen species. The understory may consist of a depauperate shrub layer with cover typically <5%. and a dense herbaceous understory predominantly dominated by graminoids.

Floristics: This alliance includes woodlands dominated by Pinus ponderosa. Structurally, these are savannas with large, open growth-form Pinus ponderosa trees (generally) as the only canopy dominant. Average tree canopy cover ranges from 10-50%. Other conifers, including Juniperus spp., Pinus discolor, Pinus edulis, and Pseudotsuga menziesii, may be present at low cover. The diagnostic feature of this alliance is the depauperate shrub layer with cover typically <5% and moderate to dense herbaceous understory predominantly dominated by fire-resistant grasses. Shrubs which may occur at low cover include Artemisia tridentata, Brickellia californica, Ceanothus fendleri, Ceanothus fendleri, Cercocarpus montanus, Chrysothamnus viscidiflorus, Ericameria nauseosa, Fallugia paradoxa, Mahonia spp., Purshia tridentata, Quercus gambelii, Quercus grisea, Rhus trilobata, Tetradymia canescens, and Yucca baccata. The herbaceous layer is dense and composed of fire-resistant graminoids. Dominant species may include Andropogon gerardii, Bouteloua gracilis, Festuca arizonica, Muhlenbergia montana, Muhlenbergia straminea (= Muhlenbergia virescens), and Schizachyrium scoparium. Other graminoid associates may include Achnatherum lobatum (= Stipa lobata), Andropogon gerardii, Aristida spp., Bothriochloa barbinodis (= var. barbinodis), Bouteloua curtipendula, Bouteloua hirsuta, Carex geophila, Carex rossii, Elymus elymoides, Hesperostipa comata, Koeleria macrantha, Piptochaetium fimbriatum, and Piptochaetium pringlei. An assortment of forbs may occur, but cover is low relative to graminoids. Common associates may include Ageratina rothrockii (= Eupatorium rothrockii), Allium cernuum, Antennaria spp., Artemisia ludoviciana, Campanula rotundifolia, Chaetopappa ericoides, Chaetopappa ericoides, Erigeron spp., Lotus wrightii, Oxytropis lambertii, Packera neomexicana, Penstemon spp., and Silene laciniata.

Dynamics:  Pinus ponderosa is a drought-resistant, shade-intolerant conifer which usually occurs at lower treeline in the major ranges of the western United States. Historically, surface fires and drought were influential in maintaining open-canopy conditions in these woodlands. With settlement and subsequent fire suppression, stands have become more dense. Presently, many stands contain understories of more shade-tolerant species, such as Pseudotsuga menziesii and/or Abies spp., as well as younger cohorts of Pinus ponderosa. These altered stand structures have affected fuel loads and altered fire regimes. Presettlement fires were frequent (5- to 15-year return intervals) with low-intensity surface fires triggered by lightning strikes or deliberately set by Native Americans. With fire suppression and increased fuel loads, fires are now less frequent and often become intense crown fires which can kill mature Pinus ponderosa. Establishment is erratic and believed to be linked to periods of adequate soil moisture and good seed crops, as well as fire frequencies which allow seedlings to reach sapling size. Longer fire-return intervals have resulted in many stands having dense subcanopies of overstocked and unhealthy young Pinus ponderosa.

Environmental Description:  These woodlands typically occur between grassland or shrubland and more mesic coniferous forests. The quantity and timing of precipitation vary greatly across the range of the alliance, ranging from 25-60 cm annually, with at least some seasonal drought. East of the Continental Divide and in the Southwest, summer precipitation predominates. Monsoonal summer rains can contribute a substantial proportion to the annual precipitation totals in the Southwest. Stands occur on bottomlands, elevated plains, cinder cones, piedmont slopes, mesas, foothills, and mountains at elevations ranging from 1700-2900 m. Fire is a key factor in maintaining the open canopies characteristic of these woodlands, but soil drought or infertility may be equally important in some areas. Soils are derived from igneous, metamorphic, and sedimentary materials and are characterized by good aeration and drainage, coarse textures, circumneutral to slightly acidic pH, an abundance of mineral material, and periods of drought during the growing season.

Geographic Range: This alliance is found predominantly in the central and southern Rocky Mountains, west into the Colorado Plateau and Mogollon Rim, east to Texas, the Great Plains and Black Hills.

Nations: MX,US

States/Provinces:  AZ, CO, MT, NE, NM, OK, SD, TX, UT, WY




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: A.530, A.1488, in parts

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: ? Pinus ponderosa woodland alliance (Hoagland 1998a)
>< Interior Ponderosa Pine: 237 (Eyre 1980)

Concept Author(s): M.S. Reid and D. Sarr, in Faber-Langendoen et al. (2013)

Author of Description: M.E. Hall

Acknowledgements: No Data Available

Version Date: 03-14-14

  • Diamond, D. D. 1993. Classification of the plant communities of Texas (series level). Unpublished document. Texas Natural Heritage Program, Austin. 25 pp.
  • Eyre, F. H., editor. 1980. Forest cover types of the United States and Canada. Society of American Foresters, Washington, DC. 148 pp.
  • 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.
  • Hoagland, B. W. 1998a. Classification of Oklahoma vegetation types. Working draft. University of Oklahoma, Oklahoma Natural Heritage Inventory, Norman. 43 pp.