Ecological site group DX035X01CESG06
Mesas and Benches - Saline Uplands and Flats - loam to clay
Last updated: 10/05/2022
Accessed: 05/02/2024
Ecological site group description
Key Characteristics
- Mesa and Benches
- Saline Uplands and Flats
- Soils are loams to clays
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
The sites in this group occur on alluvial fans, drainageways, valley flats, structural benches, hills, and stream terraces. Runoff is low to very high and the soil is well drained. Slopes are typically 0-60%. Elevations are generally from 4000-6800 ft.
Climate
The climate is characterized by hot summers and cool to warm winters. Large fluctuations in daily temperatures are common. Mean annual high temperatures range from 51-70 degrees Fahrenheit and mean annual low temperatures range from 46-52 degrees Fahrenheit. Approximately 65–70% of moisture occurs as rain from March through October. On the average, April, May, and June are the driest months and August, September, and October are the wettest months. Precipitation is extremely variable from month to month and from year to year but averages between 6-12 inches. Much of the precipitation occurs as convection thunderstorms.
Soil features
The soils are shallow to very deep and well drained. The soil temperature and moisture regimes are mesic and typic aridic to ustic aridic respectively. Surface and subsurface textures are generally fine sandy loams, loams, clay loams, and silty clay loams. Rock fragments may occur on alluvial fan and hillslope positions and shale parachanners may occur in soils shallow to soft shale bedrock. Soils are slightly saline to strongly saline and may be sodic. Available water holding capacity is generally low.
Vegetation dynamics
This site developed under Colorado Plateau ecological conditions and the natural influences of herbivory and climate. This site’s plant species composition is generally dominated by James' galleta and shadscale. Torrey's tea, snakeweed, prickly pear and yellow rabbitbrush are common shrubs, and Indian ricegrass blue grama, mesa dropseed, and sand dropseed are common grasses.
There is no evidence that these sites historically burned on a regular basis due to very large and persistent gaps between plants. However, modern disturbances such as recreation and livestock grazing, may result in an opportunity for invasive annuals to enter the system. Cheatgrass, Russian thistle and halogeton have all been documented on these sites, but they are rarely dominant. Sharp and Sanders’ photo record indicates that insect herbivory coupled with climate fluctuations appear to drive some shadscale communities (Sharp and Sanders 2002). 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 lower under dry climatic conditions, and annual production decreases during drought.
This ecological site has been grazed by domestic livestock since they were first introduced into the area around 1860. It is highly resistant to winter grazing, which is the common season of use. The introduction of domestic livestock and the use of fencing and reliable water sources have influenced the disturbance regime historically associated with these ecological sites in some areas. Improperly managed livestock grazing (continuous season long grazing, heavy stocking rates, etc.) may cause the sites to depart from the reference plant community. Native perennial grasses will decrease while invasive forbs, annual grasses, rabbitbrush and broom snakeweed will increase. While shadscale, due to its spinescent nature, is resistant to moderate browsing pressures, improper grazing may stress this plant and allow nutrients to become available for invasive species to flourish. Timing of grazing also affects the ecological dynamics—spring grazing results in a decline of cool season grasses, while heavy summer/early fall grazing results in a decline of warm season grasses. Intense grazing of shadscale in the spring and early summer can damage shadscale (USU.edu, 2009). Shadscale is also susceptible to diseases such as root rot, water mold, and vascular wilt fungi (USU.edu, 2009).
Suitability for rangeland seeding is very poor because of low annual precipitation, and low available water capacity.
--References--
USU.edu, 2009. Range Plants of Utah. Available: http://extension.usu.edu/rangeplants/htm/shadscale.
Major Land Resource Area
MLRA 035X
Colorado Plateau
Subclasses
Correlated Map Unit Components
22960255, 22960267, 22960244, 22960248, 22934197, 22934208, 22934133, 22592421, 22592535, 22592653, 22592447, 22592553, 22592483, 22592503, 22963384
Stage
Provisional
Contributors
Vic Parslow
Keith Crossland
Jim Harrigan
Harry Hosler
Curtis Talbot
Click on box and path labels to scroll to the respective text.
Ecosystem states
T1A | - | E = Establishment of non-native plant species |
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State 1 submodel, plant communities
1.1a | - | CLd = Climate, dry I = Insect Herbivory |
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1.1b | - | CLw = Climate, wet |
State 2 submodel, plant communities
2.1a | - | CLd = Climate, dry G = Continuous, season-long grazing of perennial grasses I = Insect Herbivory |
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2.2a | - | CLw = Climate, wet |