Ecological site group DX035X01CESG07
Mesas and Benches - Saline Uplands and Flats - sandy loams
Last updated: 10/05/2022
Accessed: 05/02/2024
Ecological site group description
Key Characteristics
- Mesa and Benches
- Saline Uplands and Flats
- Soils are sandy loams
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
Physiography
This site occurs on mesas, benches, hillslopes, mountain slopes, pediments, valleys, cuestas, and ridges. Run off is medium to high and is often influenced by micro-topography. Typically slopes range from 2-30% however sites have been mapped on slopes up to 70%.
Climate
The climate is characterized by hot summers and cool to warm winters, which can be slightly modified by local topographic conditions, such as aspect. Large fluctuations in daily temperatures are common. Mean annual high temperatures range from 67-75 degrees Fahrenheit and mean annual low temperatures range from 35-50 degrees Fahrenheit. Approximately 65-70% of moisture occurs as rain from July-November, mostly as convection thunderstorms and snow. Precipitation is variable from month to month and from year to year but averages between 5-10 inches. Snow packs when present are generally light and not persistent.
Soil features
The soils are very shallow to shallow, weakly to moderately developed, and well drained. Typically the dry surface is light reddish brown to dark reddish brown. Erosion potential of soils on reference state sites typically depends on surface rock fragments. Sites with greater than 30% rock fragments have lower wind and water erosion potentials than sites with less than 30% surface rock fragments. The soil temperature and moisture regimes are mesic and typic aridic or ustic aridic respectively. Surface and subsurface textures are generally loamy sands, channery loams, or gravelly sandy loams. Soils are nonsaline and the water holding capacity is low. Biological crust cover is characterized as a weak crust, with light cyanobacteria and/or isolated moss clumps with no continuity.
Vegetation dynamics
The ecological sites in this group developed under Colorado Plateau ecological conditions and the natural influences of climate and grazing. The dynamics described in this site description were determined through the study of rangeland relic areas, areas protected from excessive disturbance and influences such a improper livestock grazing and damaging recreational activities. Literature reviews, trends in plant community dynamics, and historical accounts have also been considered. Community phases, community pathways, states, transitions, thresholds, and restoration pathways have been determined through similar studies and experiences.
These ecological sites are found on very shallow to moderately deep, poorly developed soils in Major Land Resource Area (MLRA) 35. Vegetation on salt desert shrub lands is generally very sparse and thus fire did not carry well and therefore is not part of the historic natural disturbance regime (Simonin, 2001). Due to scarcity of local water sources this site was minimally influenced by large grazing ungulates before European settlement. The most prominent disturbance regime associated with this site is weather. During periods of drought perennial warm and cool season grasses decrease, while periods of normal and above average precipitation result in an increase in perennial warm and cool season grasses. Shrub cover is generally similar under both climatic conditions; however, annual production decreases during drought.
This site has been grazed by domestic livestock since they were introduced into the area. This introduction of livestock with it's use of fencing, and the development of reliable water sources have impacted the disturbance regime of this site. Improper livestock grazing (i.e., continuous season long grazing, heavy stocking rates, etc.) can cause this site to depart from it's reference plant communities and allow annual grasses, such as cheatgrass, to invade, and broom snakeweed to increase dramatically. These annual grasses can increase the sites fine fuel loads and make fire more prevalent, increasing the possibility that it will convert to an annual grassland community(Simonin, 2001).
As vegetative communities respond to changes in management or natural influences that move them to different ecological states, a return to previous states may not be possible. The amount of energy needed to affect vegetative shifts depends on present biotic and abiotic features and the desired results.
Major Land Resource Area
MLRA 035X
Colorado Plateau
Subclasses
Correlated Map Unit Components
22960105, 22960249, 22960260, 22934079, 22592523, 22592298, 22592542, 22592304, 22592309, 22592461, 22592567, 22592685, 22592687, 22592571, 22592584, 22592472, 22592590, 22592716, 22592603, 22592388, 22592394, 22592620, 22592508
Stage
Provisional
Contributors
Vic Parslow
Keith Crossland
Curtis Talbot
Click on box and path labels to scroll to the respective text.
Ecosystem states
T1A | - | D = Drought WS = Establishment of non-native invasive species ILG = Improper livestock grazing SD = Surface disturbances |
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T2A | - | D = Drought ILG = Improper livestock grazing F = Fire |
T2B | - | ILG = Improper livestock grazing SD = Surface disturbances |
R4A | - | BC = Biological Control PLG = Proper livestock grazing T = Time without disturbances W = Wet weather periods |
State 1 submodel, plant communities
1.1a | - | PLG = Proper livestock grazing T = Time without disturbances W = Wet weather periods |
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1.2a | - | D = Drought ILG = Improper livestock grazing SD = Surface disturbances |
State 2 submodel, plant communities
2.1a | - | W = Wet weather periods PLG = Proper livestock grazing T = Time without disturbances |
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2.2a | - | D = Drought ILG = Improper livestock grazing SD = Surface disturbances |
State 3 submodel, plant communities
3.1a | - | D = Drought ILG = Improper livestock grazing F = Fire |
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