Ecological site group DX035X01FESG12
Canyonlands - Sandy Grasslands and Shrublands - low elevation
Last updated: 10/12/2022
Accessed: 05/02/2024
Ecological site group description
Key Characteristics
- Canyonlands
- Sandy Grasslands and Shrublands
- Low Elevation MAST > 54 degrees F.
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 ecological sites in this group typically occur on dunes and sand sheets on structural benches, cuestas, hillslopes, mesas, fan piedmonts, and plateaus. Slopes typically range from 1 to 12 percent but may be as high as 30 percent. Run off is low and can be influenced by site micro-topography. Elevations range from 3,800 to 7,300 feet.
Climate
The climate is characterized by hot summers and cool winters which can be slightly modified by local topographic conditions, such as aspect. Average annual precipitation is 5 to 13 inches. Approximately 75 percent occurs as rain from March through October. On the average, February, May, and June are the driest months and April, August, September, and October are the wettest months. Precipitation is extremely variable from month to month and from year to year. Much of the summer precipitation occurs as convection thunder storms. Snow packs are generally light and not persistent.
Soil features
Characteristic soils in this site are 20 to 60 inches deep over sandstone and well drained to excessively well drained. They formed in eolian and alluvium deposits derived mainly from sandstone parent materials. Soils generally have high wind and water erosion potential. Coppice mounding is common. Soils are in the coarse-loamy textural family and typically have a calcic horizon occuring at less than 24 inches. The available water supplying capacity is 2 to 4.5 inches in the upper 40 inches of soil. The soil moisture regime is typic aridic or ustic aridic and the soil moisture regime is mesic.
Vegetation dynamics
The dominant visual aspect of the plant communities in this ecological site group is typically a near pure stand of blackbrush. A perennial grass and forb layer is variable is composition and production; the most common herbaceous plants are James’ galleta, Indian ricegrass, needle-and-thread, and dropseed species. Biological crust cover is also extremely variable ranging from very light cyanobacteria in the plant interspaces, with occasional moss and lichen pinnacles under shrub canopies, to sites with a dominance of lichen and moss pinnacles in the plant interspaces and cyanobacteria in the pinnacle interspaces
An important natural disturbance regime consisted of infrequent fires that were likely ignited by both natural causes and Native Americans. When fire starts in this blackbrush community, it can spread easily when the right conditions are present due to the dense, close spaced nature of blackbrush. There are typically few forbs or grasses to provide fine fuels needed to carry fire in these communities, but it is still able to burn during extreme conditions such as high temperature, high wind velocity, and low relative humidity. Fire is more common in moister years when annual production of grasses of forbs is highest. Blackbrush communities have the highest cover of any desert shrub community, and fires typically result in stand replacement. Blackbrush appears to act as a paleo-endemic species on some sites in this MLRA and may not be able to reestablish itself after significant disturbance. Though historical documentation of fire return intervals is lacking, the historical fire regime is estimated to be from 35-100+ years.
Another natural disturbance mechanism consists of fluctuating weather which can influence soil/water/vegetation relationships.
These ecological sites have been grazed by domestic livestock since they were first introduced into the area (~1860). They are highly resistant to grazing due to the unpalatable nature of blackbrush and lack of a significant grass component. Continuous season long grazing and/or heavy stocking rates may cause perennial grasses and mormon tea to decrease while yellow cryptantha, locoweed, desert trumpet, blackbrush, and snakeweed increase. This type of grazing may also increase the chance of invasion by cheatgrass and invasive annual forbs.
Major Land Resource Area
MLRA 035X
Colorado Plateau
Subclasses
Correlated Map Unit Components
22481050, 22592533, 22592290, 22592441, 22592560, 22592452, 22592453, 22592324, 22592331, 22592334, 22592400, 22594313, 22594980, 22594355, 22598343, 22597891, 22598344, 22964758, 22964743, 22964744, 22964733, 22963766, 22963804, 22963796, 22963747, 22963820, 22963753, 22963756, 22963662, 22963720, 22963688, 22963692, 22963679, 22963608, 22963616
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 E = Establishment of non-native invasive species ILG = Improper livestock grazing SD = Surface disturbances |
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T2A | - | D = Drought ILG = Improper livestock grazing SD = Surface disturbances |
State 1 submodel, plant communities
1.1a | - | D = Drought ILG = Improper livestock grazing SD = Surface disturbances |
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1.2a | - | PLG = Proper livestock grazing T = Time without disturbances W = Wet weather periods |
State 2 submodel, plant communities
2.1a | - | D = Drought ILG = Improper livestock grazing SD = Surface disturbances |
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2.2a | - | PLG = Proper livestock grazing T = Time without disturbances W = Wet weather periods |