Vegetation Community
Forest woodland grassland scrubland desert scrubland marshland other
| Primary On-Site, Secondary On-Site, Surrounding Site | |
| a. Life Zone
Arctic-Alpine (A) Hudsonian (B) Canadian(C) Transitional (D) Upper Sonoran (E) Lower Sonoran (F) |
b. Community
Aspen (A) Spruce-Fir (B) Douglas Fir (C) Alpine Tundra (D) Ponderosa Pine (E) Lodgepole Pine (F) Other/Mixed Conifer (G) Piñon-Juniper Woodland (H) Wet Meadow (I) Dry Meadow (J) Oak-Maple Shrub (K) Riparian (L) Grassland/Steppe (M) Desert Lake Shore (N) Shadscale Community (O) Tall Sagebrush (P) Low Sagebrush (Q) Barren (R) March/Swamp (S) Lake/Reservoir (T) Agricultural (U) Blackbrush (V) Creosote Bush (Y) |
| Shrubland | |||||||
|
CES304.763 |
Colorado Plateau Blackbrush-Mormon-tea Shrubland |
|
|||||
|
CES304.762 |
Colorado Plateau Mixed Low Sagebrush Shrubland |
|
|||||
|
CES304.766 |
Colorado Plateau Pinyon-Juniper Shrubland |
|
|||||
|
CES304.783 |
Inter-Mountain Basins Mat Saltbush Shrubland |
|
|||||
|
CES304.784 |
Inter-Mountain Basins Mixed Salt Desert Scrub |
|
|||||
|
CES302.741 |
Mogollon Chaparral |
|
|||||
|
CES306.810 |
Rocky Mountain Alpine Dwarf-Shrubland |
|
|||||
|
CES306.818 |
Rocky Mountain Gambel Oak-Mixed Montane Shrubland |
|
|||||
|
CES306.822 |
Rocky Mountain Lower Montane-Foothill Shrubland |
|
|||||
|
CES304.793 |
Southern Colorado Plateau Sand Shrubland |
|
|||||
|
CES303.668 |
Western Great Plains Mesquite Woodland and Shrubland |
|
|||||
| Steppe/Savanna | |||||||
|
CES302.735 |
Apacherian-Chihuahuan Semi-Desert Grassland and Steppe |
|
|||||
|
CES302.732 |
Chihuahuan Gypsophilous Grassland and Steppe |
|
|||||
|
CES304.782 |
Inter-Mountain Basins Juniper Savanna |
|
|||||
|
CES304.785 |
Inter-Mountain Basins Montane Sagebrush Steppe |
|
|||||
|
CES304.788 |
Inter-Mountain Basins Semi-Desert Shrub-Steppe |
|
|||||
|
CES301.730 |
Madrean Juniper Savanna |
|
|||||
|
CES306.834 |
Southern Rocky Mountain Juniper Woodland and Savanna |
|
|||||
|
CES306.826 |
Southern Rocky Mountain Ponderosa Pine Savanna |
|
|||||
| Herbaceous | |||||||
|
CES302.736 |
Chihuahuan Sandy Plains Semi-Desert Grassland |
|
|||||
| Herbaceous | |||||||
|
CES304.787 |
Inter-Mountain Basins Semi-Desert Grassland |
|
|||||
|
CES306.811 |
Rocky Mountain Alpine Fell-Field |
|
|||||
|
CES306.816 |
Rocky Mountain Dry Tundra |
|
|||||
|
CES306.829 |
Rocky Mountain Subalpine-Montane Mesic Meadow |
|
|||||
|
CES306.824 |
Southern Rocky Mountain Montane-Subalpine Grassland |
|
|||||
|
CES303.817 |
Western Great Plains Foothill and Piedmont Grassland |
|
|||||
|
CES303.670 |
Western Great Plains Sand Prairie |
|
|||||
|
CES303.672 |
Western Great Plains Shortgrass Prairie |
|
|||||
| Woody Wetland | |||||||
|
CES302.748 |
North American Warm Desert Lower Montane Riparian Woodland and Shrubland |
|
|||||
|
CES302.752 |
North American Warm Desert Riparian Mesquite Bosque |
|
|||||
|
CES302.753 |
North American Warm Desert Riparian Woodland and Shrubland |
|
|||||
|
CES302.755 |
North American Warm Desert Wash |
|
|||||
|
CES306.821 |
Rocky Mountain Lower Montane Riparian Woodland and Shrubland |
|
|||||
|
CES306.832 |
Rocky Mountain Subalpine-Montane Riparian Shrubland |
|
|||||
|
CES306.833 |
Rocky Mountain Subalpine-Montane Riparian Woodland |
|
|||||
| Herbaceous Wetland | |||||||
|
CES300.729 |
North American Arid West Emergent Marsh |
|
|||||
|
CES302.747 |
North American Warm Desert Cienega |
|
|||||
|
CES302.039 |
North American Warm Desert Interdunal Swale Wetland |
|
|||||
|
CES306.812 |
Rocky Mountain Alpine-Montane Wet Meadow |
|
|||||
|
CES303.666 |
Western Great Plains Closed Depression Wetland |
|
|||||
| Herbaceous Wetland | |||||||
|
CES303.669 |
Western Great Plains Saline Depression Wetland |
|
|||||
| Mixed Upland and Wetland | |||||||
|
CES302.746 |
Chihuahuan-Sonoran Desert Bottomland and Swale Grassland |
|
|||||
|
CES304.780 |
Inter-Mountain Basins Greasewood Flat |
|
|||||
|
CES303.956 |
Western Great Plains Riparian Woodland and Shrubland |
|
|||||
| Barren | |||||||
|
CES304.765 |
Colorado Plateau Mixed Bedrock Canyon and Tableland |
|
|||||
|
CES304.775 |
Inter-Mountain Basins Active and Stabilized Dune |
|
|||||
|
CES304.786 |
Inter-Mountain Basins Playa |
|
|||||
|
CES304.789 |
Inter-Mountain Basins Shale Badland |
|
|||||
|
CES304.791 |
Inter-Mountain Basins Volcanic Rock and Cinder Land |
|
|||||
|
CES302.744 |
North American Warm Desert Active and Stabilized Dune |
|
|||||
|
CES302.743 |
North American Warm Desert Badland |
|
|||||
|
CES302.745 |
North American Warm Desert Bedrock Cliff and Outcrop |
|
|||||
|
CES302.750 |
North American Warm Desert Pavement |
|
|||||
|
CES302.751 |
North American Warm Desert Playa |
|
|||||
|
CES302.754 |
North American Warm Desert Volcanic Rockland |
|
|||||
|
CES306.809 |
Rocky Mountain Alpine Bedrock and Scree |
|
|||||
|
CES306.815 |
Rocky Mountain Cliff, Canyon and Massive Bedrock |
|
|||||
|
CES303.665 |
Western Great Plains Cliff and Outcrop |
|
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|
Summary: This
ecological system occurs in dry mountains and foothills of the Colorado
Plateau region including the Western Slope of Colorado to the Wasatch
Range, south to the Mogollon Rim and east into the northwestern corner
of New Mexico. It is typically found at lower elevations ranging from
1500-2440 m. These woodlands occur on warm, dry sites on mountain
slopes, mesas, plateaus, and ridges. Severe climatic events occurring
during the growing season, such as frosts and drought, are thought to
limit the distribution of pinyon-juniper woodlands to relatively narrow
altitudinal belts on mountainsides. Soils supporting this system vary in
texture ranging from stony, cobbly, gravelly sandy loams to clay loam or
clay. Pinus edulis and/or Juniperus osteosperma dominate
the tree canopy. In the southern portion of the Colorado Plateau in
northern Arizona and northwestern New Mexico, Juniperus monosperma
and hybrids of Juniperus spp may dominate or codominate the tree
canopy. Juniperus scopulorum may codominate or replace Juniperus
osteosperma at higher elevations. Understory layers are variable and
may be dominated by shrubs, graminoids, or be absent. Associated species
include Arctostaphylos patula, Artemisia tridentata, Cercocarpus
intricatus, Cercocarpus montanus, Coleogyne ramosissima, Purshia
stansburiana, Purshia tridentata, Quercus gambelii, Bouteloua gracilis,
Pleuraphis jamesii, or Poa fendleriana. This system occurs at
higher elevations than Great Basin Pinyon-Juniper Woodland (CES304.773)
and Colorado Plateau shrubland systems where sympatric. Classification Approach: International Terrestrial Ecological Systems Classification (ITESC)
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Comprehensive Report Ecological System - Colorado Plateau Pinyon-Juniper Woodland

Figure 2.2 Provinces of Arizona and New Mexico; sections within provinces are delimited with solid lines; National Forests are indicated by solid fill pattern.province

Figure 2.3 Life zones of Arizona and New Mexico as characterized by biotic communities.biotic communities map
LIFE ZONES OF THE SOUTHWEST
The General Ecosystem Survey (Carleton et al. 1991) groups Southwestern ecosystems into life zones characterized by biotic community types including desert, grassland, chaparral, evergreen oak woodland, coniferous woodland, ponderosa pine, mixed conifer, spruce–fir, tundra, and riparian wetlands. Because this an assessment of forest, woodland, and associated riparian ecosystems, desert, grassland, chaparral, and tundra life zones are excluded from further discussion. The concept of a life zone is derived from a taxonomic classification system described first by Merriam (1898), revised by UNESCO (1973), and applied in the Southwest by the Terrestrial Ecosystem Survey. The General Ecosystem Survey life zones (Table 2.2) can be cross-referenced to the biotic communities described by Brown and Lowe (1977, 1980) and Brown (1994). Aspen is a component of the montane forest found mostly in the mixed conifer zone but also in the ponderosa pine and the spruce–fir zones. Riparian wetlands occupy little area but like aspen perform special and very important ecological and landscape functions within their life zone. Because of their uniqueness and value, aspen and riparian wetlands are treated here along with evergreen oak and coniferous woodlands, ponderosa pine, mixed conifer, and spruce–fir forests as forest biotic communities of the Southwest (Figure 2.3).
| Life Zone | Biotic Community |
|---|---|
| Evergreen oak woodland | Madrean evergreen woodland |
| Coniferous woodland | Great Basin conifer woodland |
| Ponderosa pine and mixed conifer | Rocky Mountain/Madrean montane coniferous forest |
| Spruce-fir | Rocky Mountain subalpine coniferous forest. |
| Life zones defined by Carleton et al. (1991); biotic communities described by Brown and Lowe (1977, 1980) and Brown (1994). | |
A specific ecosystem can be located with reference to a geographic province; and if it is defined by the dominant vegetation, it can also be associated with other ecosystems of similar biotic composition (life zone). Whereas the province scale is the correct perspective for examining landscape dynamics, the life zone is the appropriate scale for describing aspects of community development such as disturbance regime and successional pattern. Every ecosystem is a unique entity with its own particular history, composition, structure, and potential. Although ecosystems of a common life zone tend to respond in similar ways, each is different. Some of this difference can be explained by location within a landscape and province. Because most of the available information for past and current ecosystems is cataloged or identified by life zone, this assessment primarily describes Southwestern ecosystems by life zone and notes differences by province where they are known.
Evergreen Oak and Coniferous Woodlands
Woodlands generally include evergreen oak and conifer species that occupy certain areas along an elevational gradient from low-elevation desert shrub/grasslands and short-grass prairies to high-elevation montane coniferous forests of ponderosa pine and Gambel oak. Oak woodlands occur within the range of 4,000– to 9,000–feet elevation. Gambel oak occurs at higher elevations, and wavyleaf oak (Quercus undulata) occurs either below Gambel oak or intermingled with it in a transition zone. Woodlands were used extensively by prehistoric and historic populations for habitation and subsistence. Uses today include grazing, fuelwood harvest, and recreation.
Evergreen oak woodland, characterized by wet summers and mild winters, extends from the Sierra Madre of Mexico into southeastern Arizona and southwestern New Mexico. In the United States, a variety of oak species such as Emory oak (Quercus emoryi), Arizona white oak (Q. arizonica), Mexican blue oak (Q. oblongifolia), gray oak (Q. grisea), silverleaf oak (Q. hypoleucoides), and netleaf oak (Q. rugosa) are found in conjunction with the following Madrean pine species–Apache pine (Pinus engelmannii), Chihuahua pine (P. leiophylla var. chihuahuana), and Arizona pine (P. arizonica) (Brown 1994).
Pinyons and junipers, together or alone, dominate coniferous woodland communities. These woodlands occupy approximately 23 million acres in New Mexico, about 13 percent of which are on national forest lands, and 4.1 million acres in Arizona, 34 percent on national forest lands. The pinyons include Pinus edulis, the most common pinyon pine throughout the type, border pinyon (P. discolor), and Arizona singleleaf pinyon (P. californarium subsp. fallax). Junipers are frequently found at lower elevations than pinyons and typically occupy sites with deep soils. The most common junipers in the Southwest are one-seed juniper (Juniperus monosperma) found in central and southern New Mexico and much of Arizona below the Mogollon Rim, the Rocky Mountain juniper (J. scopulorum) in the higher and colder woodlands of northern New Mexico and Arizona, Utah juniper (J. osteosperma) in northwestern New Mexico and northern Arizona, and alligator juniper (J. deppeana) associated with the Madrean woodlands of southern Arizona and New Mexico (Brown 1994, Gottfried 1992).
Ponderosa Pine
Ponderosa pine (yellow pine or blackjack pine) is found from 6,500 to 8,000 feet elevation. At lower elevations, the ponderosa pine forest meets woodlands and at higher elevations transitions into the mixed conifer zone. Ponderosa pine forests of central and northern New Mexico and Arizona cover about 8.4 million acres. The predominant form throughout the Southwest is the three-needled, Rocky Mountain ponderosa pine (P. ponderosa var. scopulorum). In lower elevations of southern Arizona, however, the five-needled, Arizona pine is more common. Other species associated with ponderosa pine at low elevations are Gambel oak and New Mexico locust (Robina neomexicana); at high elevations associates are southwestern white pine (Pinus strobiformis), Rocky Mountain Douglas-fir (Pseudotsuga menziesii var. glauca), Rocky Mountain white fir (Abies concolor var. concolor), and quaking aspen (Populus tremuloides) (Brown 1994). Uses include timber harvest, grazing, camping, and other types of recreation offering cool relief from hot urban areas.
Mixed Conifer
Mixed conifer forests dominated by Douglas-fir, white fir, and blue spruce (Picea pungens) occur at elevations from 8,000 to 9,500 feet. There are about 1.5 million acres of mixed conifer forest in the Rocky Mountain and Madrean montane forests of southern Colorado, New Mexico, Arizona, and the Sierra Madre Occidental of Mexico (Brown 1994). Ponderosa pine, southwestern white pine, aspen, and a number of other tree species may occur in these forests. Uses are similar to the ponderosa pine community.
Spruce–Fir
Spruce–fir forests are found at high, subalpine, elevations in the Southwest from approximately 8,000 feet to over 12,000 feet. Spruce–fir forests are typically restricted to areas receiving more than 25 inches of precipitation from winter snows and summer thunderstorms. The predominant spruce is Engelmann spruce which is found as far south as the Pinaleno Mountains in Arizona and the Sacramentos in New Mexico. The co-dominant species is subalpine fir (Abies lasiocarpa). Some populations of subalpine fir possess a distinctive outer cortex and are called corkbark fir (A. lasiocarpa var. arizonica). Small stands of aspen or blue spruce are found within the spruce–fir forest (Brown 1994). Uses include wilderness recreation, skiing, and the enjoyment of high places. Mountain peaks have special cultural and religious significance for many Southwestern Indian tribes.
Aspen
Quaking aspen occurs at elevations above 6,000 feet as small, transient patches in ponderosa pine, mixed conifer, or spruce–fir forests. There are close to 500,000 acres of aspen in the Southwest, seventy-five percent in northern New Mexico and the remainder in the Mogollon Rim-White Mountains of Arizona (Brown 1994). Aspens can reproduce by cloning from an established root system and establish a new stand of trees quickly after a fire or other disturbance. Aspens, however, are intolerant of shade and eventually lose out to competition when they become overtopped by re-invading conifers. Aspen stands are especially valued for their scenic quality and use by traditional communities.
Riparian Wetlands
Riparian wetlands including cienegas make up less than 2 percent of the land of New Mexico and Arizona, but they are the most biologically diverse and productive ecosystems in the Southwest. Over 65 percent of Southwestern animals depend on riparian habitats during all or part of their life cycles. Millions of Southwestern residents use these areas for recreation and agriculture. The most important species of Southwestern riparian wetlands are the Fremont cottonwood (Populus fremontii) and the narrowleaf cottonwood (P. augustifolia) (Brown 1994).