

Natural Resources
Conservation Service
Ecological site R054XY037ND
Wet Meadow
Last updated: 3/31/2025
Accessed: 04/14/2025
General information
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.

Figure 1. Mapped extent
Areas shown in blue indicate the maximum mapped extent of this ecological site. Other ecological sites likely occur within the highlighted areas. It is also possible for this ecological site to occur outside of highlighted areas if detailed soil survey has not been completed or recently updated.
MLRA notes
Major Land Resource Area (MLRA): 054X–Rolling Soft Shale Plain
MLRA 54 covers 29,280 square miles and encompasses approximately 18.7 million acres. MLRA 54 spans three states with 64 percent of it in North Dakota, 33 percent in South Dakota, and 3 percent in Montana. Most of MLRA 54 is underlain by soft, calcareous shale, siltstone, and sandstone of the Tertiary Fort Union Group and the Cretaceous Fox Hills and Hell Creek Formations. Most of the soils in MLRA 54 developed from residuum weathered in place including colluvial and alluvial deposits from residuum. Along the eastern and northern edges of the MLRA where MLRA 54 transitions into the glaciated Missouri plateau, remnants of glacial till parent materials remain on the high areas of the landscape. The MLRA 54 landscape is characterized by moderately dissected rolling plains with areas of local badlands, hills, and isolated buttes. Elevation is 1,650 feet (505 meters) on the eastern side of the MLRA with a gradual rise to 3,600 feet (1,100 meters) on the western side. The Missouri River runs along the north and east side of MLRA 54. Most of the Standing Rock Indian Reservation, the northwest third of the Cheyenne River Indian Reservation, and the Grand River National Grasslands are in the southern part of the MLRA.
Classification relationships
Level IV Ecoregions of the Conterminous United States: 43a – Missouri Plateau; 43c – River Breaks; 43j – Moreau Prairie.
Wetland Description: System Subsystem Class Sub-class Water Regime
Cowardin, et. al., 1979 Palustrine N/A Emergent Persistent Temporary/Saturated
Ecological site concept
The Wet Meadow ecological site is generally located in depressions and low-lying flats on uplands (till plains and sedimentary plains), in upland drainageways, and in swales on sand sheets. Also, a few sites occur in relict oxbows now isolated from frequent stream flooding. The soils are very deep and poorly drained; a seasonal high-water table is typically within a depth of 1.5 feet during the months of April through June; in depressions, it is frequently ponded (depth of ponding is typically <1.5 feet) in April and May. Generally, redox features are within a depth of 18 inches. Very slight or slight salinity (E.C. <8 dS/m) is allowable on this site. Effervescence ranges from none to violent. Hydrology (surface and sub-surface) is the primary factor used in identifying this site. All textures are included in the site. Slope is 0 to 2 percent. On the landscape, this site is below the Loamy, Loamy Overflow, Loamy Terrace, Sands, Sandy Terrace, and Thin Claypan ecological sites and above the Shallow Marsh site. The Closed Depression and Saline Lowland sites are on similar landscape positions. Closed Depression occurs in depressions and basins and has a dense, sodic claypan within a depth of 4 inches. The Saline Lowland typically occurs on flats; it has moderate or strong soil salinity (E.C. >8).
To see a full copy of the ecological site description with all tables and the full version 5 rangeland health worksheet. Please use the following hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/54_Wet_Meadow_Narrative_FINAL_Ref_FSG.pdf
Associated sites
R054XY033ND |
Thin Claypan This site occurs somewhat higher on the landscape on till plains and sedimentary plains. The soil has a dense, sodic, root-restrictive subsoil within a depth of 6 inches and accumulated salts within a depth of 16 inches. |
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R054XY022ND |
Closed Depression This site occurs in poorly drained depressions and basins. Commonly, the surface layer is grayish colored with platy structure. Where a dark-colored surface layer occurs, it is <6 inches thick. The subsoil is clayey (forms a ribbon >2 inches long). |
R054XY024ND |
Saline Lowland This site occurs on similar landscape positions as the Wet Meadow site. It has an accumulation of salts in the surface and subsoil layers (E.C. >8 dS/m). All textures are included in this site. |
R054XY042ND |
Sandy Terrace This site occurs on terraces with very rare to occasional flooding; the plant community is not significantly influenced by stream overflow. The soil forms a ribbon <1 inch long. |
R054XY025ND |
Sands This site occurs on higher slopes on sand sheets. Soil does not form a ribbon. It is >30 inches to redoximorphic features. |
R054XY031ND |
Loamy This site occurs on higher slopes on till plains and sedimentary plains. The surface layer and subsoil layers form a ribbon 1 to 2 inches long. It is >30 inches to redoximorphic features. |
R054XY041ND |
Loamy Terrace This site occurs on terraces with very rare to occasional flooding; the plant community is not significantly influenced by stream overflow. The soil forms a ribbon 1 to 2 inches long. |
R054XY036ND |
Shallow Marsh This site occurs in deep depressions (very poorly drained soils) which have frequent ponding through most of the growing season. All textures are included in this site. |
R054XY023ND |
Loamy Overflow This site occurs in upland swales. The surface and subsoil layers form a ribbon 1 to 2 inches long. It is deeper than 30 inches to redoximorphic features. |
Similar sites
R054XY022ND |
Closed Depression This site occurs in poorly drained depressions and basins. Commonly, the surface layer is grayish colored with platy structure. Where a dark-colored surface layer occurs, it is <6 inches thick. The subsoil is clayey (forms a ribbon >2 inches long). |
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R054XY032ND |
Subirrigated This site occurs on concave areas of flats and in shallow depressions with occasional, brief ponding. It has redoximorphic features at a depth of 18 to 30 inches. All textures are included in this site. |
R054XY036ND |
Shallow Marsh This site occurs in deep depressions (very poorly drained soils) which have frequent ponding through most of the growing season. All textures are included in this site. |
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
Not specified |
Herbaceous |
(1) Spartina pectinata |
Physiographic features
This site typically occurs in depressions and low-lying flats on uplands (till plains and sedimentary plains), in upland drainageways, and in swales on sand sheets. Also, a few sites occur in relict oxbows now isolated from frequent stream flooding. The parent materials vary widely. Slope is 2 percent or less.
Table 2. Representative physiographic features
Landforms |
(1)
Depression
(2) Swale (3) Flat (4) Drainageway (5) Oxbow |
---|---|
Runoff class | Negligible to low |
Flooding duration | Brief (2 to 7 days) |
Flooding frequency | None to occasional |
Ponding duration | Brief (2 to 7 days) to long (7 to 30 days) |
Ponding frequency | Rare to frequent |
Elevation | 1,650 – 3,600 ft |
Slope | 2% |
Ponding depth | 18 in |
Water table depth | 18 in |
Aspect | Aspect is not a significant factor |
Climatic features
MLRA 54 is considered to have a continental climate – cold winters and hot summers, low humidity, light rainfall, and much sunshine. Extremes in temperature are characteristic. The climate is the result of this MLRA’s location in the geographic center of North America. There are few natural barriers on the northern Great Plains. The air masses move unobstructed across the plains and account for rapid changes in temperature.
Annual precipitation ranges from 14 to 18 inches per year. The normal average annual temperature is about 42° F. January is the coldest month with average temperatures ranging from about 13° F (Beach, ND) to about 16° F (Bison, SD). July is the warmest month with temperatures averaging from about 69° F (Beach, ND) to about 72° F (Timber Lake, SD). The range of normal average monthly temperatures between the coldest and warmest months is about 57° F. This large annual range attests to the continental nature of this MLRA's climate. Hourly winds are estimated to average about 11 miles per hour annually, ranging from about 13 miles per hour during the spring to about 10 miles per hour during the summer. Daytime winds are generally stronger than nighttime and occasional strong storms may bring brief periods of high winds with gusts to more than 50 miles per hour.
Growth of native cool-season plants begins in late March and continues to early to mid July. Native warm-season plants begin growth in mid May and continue to the end of August. Green up of cool-season plants can occur in September and October when adequate soil moisture is present.
Table 3. Representative climatic features
Frost-free period (characteristic range) | 95-111 days |
---|---|
Freeze-free period (characteristic range) | 118-127 days |
Precipitation total (characteristic range) | 15-18 in |
Frost-free period (actual range) | 91-114 days |
Freeze-free period (actual range) | 116-129 days |
Precipitation total (actual range) | 15-18 in |
Frost-free period (average) | 101 days |
Freeze-free period (average) | 123 days |
Precipitation total (average) | 16 in |
Figure 2. Monthly precipitation range
Figure 3. Monthly minimum temperature range
Figure 4. Monthly maximum temperature range
Figure 5. Monthly average minimum and maximum temperature
Figure 6. Annual precipitation pattern
Figure 7. Annual average temperature pattern
Climate stations used
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(1) FT YATES 4 SW [USC00323207], Fort Yates, ND
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(2) DUPREE [USC00392429], Dupree, SD
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(3) HETTINGER [USC00324178], Hettinger, ND
-
(4) WATFORD CITY [USC00329233], Watford City, ND
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(5) MANDAN EXP STN [USC00325479], Mandan, ND
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(6) LUDLOW 3 SSE [USC00395048], Ludlow, SD
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(7) HEBRON [USC00324102], Hebron, ND
Influencing water features
This site is poorly drained. Many areas of this site receive additional water as surface runoff from adjacent uplands. Under average climatic conditions, the soils in depressions are frequently ponded in April and May and occasionally ponded in June. Depth of ponding typically is less than 1.5 feet during these months. In mid and late summer, ponded water commonly is not evident except after heavy rains. Ponding is rare on upland flats and occasional in swales on sand sheets.
When not ponded, a seasonal high-water table typically fluctuates with precipitation events between the surface and a depth of 1.5 feet during the months of April through June. In most soils, it is within a depth 3.5 feet through the remainder of the growing season. Some of the soils in this site have endosaturation (the soil is saturated with water in all layers) and some have episaturation (perched water table above a subsoil layer with slow or moderately slow permeability).
Surface infiltration ranges from slow to rapid. Permeability typically ranges from slow to rapid; some soils have a coarser-textured substratum with very rapid permeability. Water loss is primarily through evapotranspiration.
Wetlands receive water from different sources including ground water movement. Recharge wetlands (Wet Meadow) are epi-saturated, receiving water from the surface, and have groundwater flow predominantly away from the wetland moving toward or into a discharge (endo-saturated) wetland basin or drainageway.
Flowthrough wetlands have groundwater flowing away from the wetland basin but is balanced with water flowing into the basin.
Due to the potential high rate of surface evaporation along drainageways, these Wet Meadow drainageways are at risk of becoming saline if vegetative cover is reduced or removed.
Water loss is primarily through evapotranspiration and lateral movement into (and evaporation from) adjacent soils. During periods of drought or extreme wetness, water table fluctuations will also have an impact on depth of ponding, especially in sandy soils. During periods of drawdown (e.g., prolonged drought), soil and water chemistry may significantly impact the soil/water/vegetation dynamics of the site (see Site Development and Testing Plan).
Fluctuations in specific conductance are less pronounced during average or normal water conditions than during periods of excessive water depth or extreme drought. The approximate normal and extreme range in specific conductance (micromhos/cm3) of surface water in plant communities that are indicators of differences in average salinity are as follows:
Water Chemistry Normal Range (micromhos/cm3) Electroconductivity (dS/m)
Fresh <40 - 500
Wetland description
Wetland Description: System Subsystem Class Sub-class Water Regime
Cowardin, et. al., 1979 Palustrine N/A Emergent Persistent Temporary/Saturated
Soil features
Soils associated with Wet Meadow ES are in the Mollisol and Entisol orders. The Mollisols are classified further as Argiaquic Argialbolls, Typic Calciaquolls, and Typic Endoaquolls. The Entisols are classified further as Vertic Fluvaquents. These soils were developed under wetland vegetation. They formed in local alluvium from till and residuum, eolian deposits, or in stream alluvium (in relict oxbows).
The common feature of soils in this site are inundation or near-surface saturation in the early part of the growing season. The soils are very deep and poorly drained. Since hydrology (surface and sub-surface) is the primary factor used in identifying this site, all textures are included. Therefore, soil physical properties associated with texture vary widely.
Soil salinity is none to slight (E.C. <8 dS/m) to a depth of >20 inches. Sodicity is none or slight in the upper part of the soil (SAR <5); SAR values as high as 10 may occur below a depth of 20 inches. Soil reaction ranges from moderately acid to moderately alkaline (pH 5.6 to 8.4). The calcium carbonate content is none to high (0 to 45 percent).
The soil surface is stable and intact. In some soils, sub-surface layers are non-restrictive to water movement; in other soils a layer of clay accumulation slows water movement and prolongs surface ponding. The soil/water/plant relationship is strongly influenced by ponded/and or saturated conditions.
Major soil series correlated to the Wet Meadow site are Arveson, Lallie, Marysland, Regan, Tonka, Hamar, Vallers, Mckeen and Minnewaukan.
Access Web Soil Survey (https://websoilsurvey.nrcs.usda.gov/app/) for specific local soils information.
Table 4. Representative soil features
Parent material |
(1)
Till
(2) Alluvium (3) Eolian deposits (4) Residuum |
---|---|
Family particle size |
(1) Loamy (2) Clayey (3) Sandy |
Drainage class | Poorly drained |
Permeability class | Slow to rapid |
Depth to restrictive layer | 80 in |
Surface fragment cover <=3" | 5% |
Surface fragment cover >3" | 1% |
Available water capacity (0-40in) |
1.5 – 12 in |
Calcium carbonate equivalent (0-40in) |
35% |
Electrical conductivity (0-20in) |
8 mmhos/cm |
Sodium adsorption ratio (0-40in) |
10 |
Soil reaction (1:1 water) (0-40in) |
5.6 – 8.4 |
Subsurface fragment volume <=3" (Depth not specified) |
60% |
Subsurface fragment volume >3" (Depth not specified) |
2% |
Ecological dynamics
This ecological site description is based on nonequilibrium ecology and resilience theory and utilizes a State- and-Transition Model (STM) diagram to organize and communicate information about ecosystem change as a basis for management. The ecological dynamics characterized by the STM diagram reflect how changes in ecological drivers, feedback mechanisms, and controlling variables can maintain or induce changes in plant community composition (phases and/or states). The application of various management actions, combined with weather variables, impact the ecological processes which influence the competitive interactions, thereby maintaining or altering plant community structure.
The site developed under Northern Great Plains climatic conditions. The historical disturbance regime for the region includes frequent fires, both natural in origin and anthropogenic. Most fires, however, were anthropogenic fires set by Native Americans. Native Americans set fires in all months except perhaps January. These fires occurred in two peak periods, one from March-May with the peak in April and another from July-November with the peak occurring in October. Most of these fires were scattered and of small extent and duration. The grazing history would have involved grazing and browsing by large herbivores (such as American bison, elk, and whitetail deer). Herbivory by small mammals, insects, nematodes, and other invertebrates are also important factors influencing the production and composition of the communities.
A Note on Prairie Dogs: Prairie dogs prefer habitats composed predominantly of shortgrasses and avoid those dominated by tallgrasses. Historically, prairie dogs likely occupied a wide range of soils (at least occasionally) due to variations in environmental factors (such as drought severity and length, grazing pressure, etc.). Presently, the known occupation of this ecological site in this MLRA by prairie dogs is considered uncommon to rare. As a result, the presence of prairie dog towns for this ecological site in this MLRA is not included in this ecological description. However, prairie dog towns may be encountered on the site. If encountered impact would include increased bare ground, decreased production and plant vigor.
This ecological site generally has a more recent history of grazing by domestic livestock (particularly cattle) which, along with related activities (e.g., fencing, water development), has changed the disturbance regime of the site. Changes will occur in the plant communities due to weather fluctuations and/or management actions; under adverse impacts, a slow decline in vegetative vigor and composition will result. However, under favorable conditions the site has the potential to resemble the reference state.
Although grazing and fire are significant ecological drivers for this site, equally important drivers are hydrology and water chemistry. Hydrology is mainly a factor of landscape position including the size of the contributing watershed, connectivity to other basins, and whether the basin has an outlet. Water chemistry is influenced by soil chemistry and whether the site is a recharge, flow-through, or discharge site. Grazing and fire interaction, particularly when coupled with drought events, set up the dynamics discussed and displayed in the following state and transition diagram and descriptions.
When soils are saturated, particularly in the spring and early summer, Wet Meadow sites are susceptible to pugging damage, or hummocking of the soil by livestock walking on the site. Pugging is a form of soil compaction due to livestock which damages the soil structure. It can seal the soil surface which reduced infiltration and exacerbates waterlogging of the topsoil. The microtopography created by pugging generally supports plants of more well drained conditions and is often associated with an increase in weedy species. This can lead to a significant reduction in plant production and utilization.
Several years of above or below average precipitation can have a dramatic impact on this ecological site. During periods of above average precipitation the site has been observed to support vegetative communities associated with the Shallow Marsh ecological site. During drought periods the vegetation of the site may be similar to that of Subirrigated ecological site.
Seven vegetative states have been identified for the site (Reference, Native/Invaded, Wooded, Invaded/Saline, Invaded/Fresh Water, Invaded/Eutrophication, and Go-Back). Within each state, one or more community phases have been identified. These community phases are named based on the more dominant and visually conspicuous species; they have been determined by study of historical documents, relict areas, scientific studies, and ecological aspects of plant species and plant communities. Transitional pathways and thresholds have been determined through similar methods.
State 1: Reference State represents the natural range of variability that dominated the dynamics of this ecological site prior to European influence. Dynamics of the state were largely determined by variations in climate and weather (e.g., drought), as well as that of fire (e.g., timing, frequency) and grazing by native herbivores (e.g., frequency, intensity, selectivity). Due to those variations, the Reference State is thought to have shifted temporally and spatially between two plant community phases.
Currently the primary disturbances include widespread introduction of exotic species, concentrated livestock grazing, lack of fire, and perhaps long-term non-use and no fire. Because of these changes (particularly the widespread occurrence of exotic species), as well as other environmental changes, sites in the Reference State are declining. The presence of exotic species on the site precludes it from being placed in the Reference State. It must then be placed in one of the other states.
State 2: Native/Invaded State. Colonization of the site by exotic species results in a transition from State 1: Reference State to State 2: Native/Invaded State (T1A). This transition is probably inevitable; it often results from colonization by exotic cool-season grasses (such as redtop, creeping meadow foxtail, and/or exotic strains/hybrids of reed canarygrass). During dry period drawdown stages, cool-season exotics (such as Kentucky bluegrass, smooth brome, quackgrass, and barnyardgrass) are common under extended periods of no use and no fire. Other exotic plants (e.g., Canada thistle) are also known to invade the site.
Three community phases have been identified for this state and are similar to the community phases in the Reference State but have now been invaded by exotic cool-season grasses. These exotic cool-season grasses can be expected to increase. As that increase occurs, plants more desirable to wildlife and livestock may decline. A decline in forb diversity can also be expected. Under non-use or minimal use management, mulch increases and may become a physical barrier to plant growth. This also changes the micro-climate near the soil surface and may alter Infiltration, nutrient cycling, and biological activity near the soil surface. As a result, these factors combined with shading cause desirable native plants to have increasing difficulty remaining viable and recruitment declines.
To slow or limit the invasion of these exotic grasses or other exotic plants, it is imperative that managerial techniques (e.g., prescribed grazing, prescribed burning) be carefully constructed, monitored, and evaluated with respect to that objective.
Extended periods of no fire or infrequent fire of State 2: Native/Invaded State can lead to State 3: Wooded State which is typically dominated by willows (T2A). Heavy season-long grazing and below average precipitation can lead to a transition to State 4: Invaded/Saline State (T2B) or State 5: Invaded/Fresh Water State (T2C), both of which are dominated by exotic cool-season grasses. This transition may occur under a wide range of managerial conditions ranging from non-use and no fire to heavy season-long grazing (primarily Kentucky bluegrass). Eutrophication/sedimentation of the site will lead to a transition to State 6: Invaded/Eutrophication State, dominated by cattails or exotic strains/hybrids of reed canarygrass (T2D).
State 3: Wooded State. This state is typically dominated by willows, Plains cottonwood, and/or quaking aspen. Plains cottonwood or quaking aspen may occur as a ring on the periphery of wetlands. This community phase often results from extended periods of no fire or infrequent fire (T2A). A marked increase in non-use management and active fire suppression since European influence has enabled this state to expand and become more widespread. Brush control (e.g., herbicide, mechanical, long-term prescribed burning) may lead to State 2: Native/Invaded State (R3A). However, depending on the abundance of exotic cool-season grasses, brush control may need to be followed by a range planting to complete the restoration.
State 4: Invaded/Saline State. This state, dominated by exotic grasses, often forms with heavy season-long grazing of State 2: Native/Invaded State during periods of below average precipitation on discharge sites with saline conditions (T2B). It can also form under periods of no use and no fire, and no range planting following a hydrological restoration of State 7: Go-Back State under saline conditions (R7B).
State 5: Invaded/Fresh Water State. This state, dominated by exotic grasses, often forms with heavy season-long grazing of State 2: Native/Invaded State during periods of below average precipitation on recharge sites under non-saline conditions (T2C). It can also form under periods of no use and no fire with no range planting following a hydrological restoration of State 7: Go-Back State under fresh water (non-saline) conditions (R7C).
State 6: Invaded/Eutrophication State. This state, dominated by hybrid cattails or reed canarygrass, results from eutrophication and sedimentation of State 2: Native/Invaded State (T2D). It can also form under periods of no use and eutrophication/sedimentation following a hydrological restoration of State 7: Go-Back State (R7D).
State 7: Go-Back State often results from cropland abandonment and consists of one community phase. This weedy assemblage may include noxious weeds that need control. Over time, however, hybrid cattail or exotic strains/hybrids of reed canarygrass will likely dominate the vegetation of the site.
The following state and transition model diagram illustrates the common states, community phases, community pathways, and transition and restoration pathways that can occur on the site. These are the most common plant community phases and states based on current knowledge and experience; changes may be made as more data are collected. Pathway narratives describing the site’s ecological dynamics reference various management practices (e.g., prescribed grazing, prescribed burning, brush management, herbaceous weed treatment) which, if properly designed and implemented, will positively influence plant community competitive interactions. The design of these management practices will be site specific and should be developed by knowledgeable individuals; based upon management goals and a resource inventory; and supported by an ongoing monitoring protocol.
When the management goal is to maintain an existing plant community phase or restore to another phase within the same state, modification of existing management to ensure native species have the competitive advantage may be required. To restore a previous state, the application of two or more management practices in an ongoing manner will be required. Whether using prescribed grazing, prescribed burning, or a combination of both with or without additional practices (e.g., brush management), the timing and method of application needs to favor the native species over the exotic species. Adjustments to account for variations in annual growing conditions and implementing an ongoing monitoring protocol to track changes and adjust management inputs to ensure desired outcome will be necessary.
The plant community phase composition table(s) has been developed from the best available knowledge including research, historical records, clipping studies, and inventory records. As more data are collected, plant community species composition and production information may be revised.
State and transition model
More interactive model formats are also available.
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Click on state and transition labels to scroll to the respective text
Ecosystem states
States 2, 5, 6 and 7 (additional transitions)
States 4 and 7 (additional transitions)
T1A | - | Invasion by exotic grasses and forbs, no-use no fire, or heavy season-long grazing |
---|---|---|
T2A | - | Extended periods of no fire or infrequent fire |
T2B | - | Heavy season-long grazing, below average precipitation, salinity (discharge site) |
T2C | - | Heavy season-long grazing, below average precipitation, no salinity (recharge site) |
T2D | - | Eutrophication, sedimentation |
R3A | - | Mechanical treatment and long-term prescribed burning |
R4A | - | Extended periods above average precipitation |
R5A | - | Extended periods above average precipitation |
R6A | - | Extended periods above average precipitation |
R7A | - | Successful hydrological restoration and seeding |
R7B | - | No use, no fire, no range planting, salinity, successful hydrological restoration |
R7C | - | No use, no fire, no range planting, fresh water, successful hydrological restoration |
R7D | - | No use, eutrophication, sedimentation, successful hydrological restoration |
T8A | - | Cessation of annual cropping |
State 1 submodel, plant communities
1.1A | - | Below average precipitation, heavy season-long grazing |
---|---|---|
1.2A | - | Return to average precipitation and long-term prescribed grazing and prescribed burning |
State 2 submodel, plant communities
2.1A | - | Heavy season-long grazing, below average precipitation |
---|---|---|
2.2A | - | Heavy season-long grazing, above or below average precipitation (discharge site) |
2.3A | - | Return to average precipitation and long-term prescribed grazing and prescribed burning |
State 3 submodel, plant communities
State 4 submodel, plant communities
State 5 submodel, plant communities
State 6 submodel, plant communities
State 7 submodel, plant communities
State 1
Reference State
This site developed under Northern Great Plains climatic conditions which include frequent droughts and wide fluctuations in temperature and precipitation which can result in both short-term and long-term changes in water levels and water chemistry (e.g., alkalinity/salinity). Hydrology, water chemistry, grazing, and fire can all serve as important drivers of this site. Hydrology is mainly a factor of landscape position including the size of the contributing watershed, connectivity to other basins, and whether the basin has an outlet. Water chemistry is influenced by soil chemistry and whether the site is a recharge, flow-through, or discharge site. This state is typically co-dominated by a mixture of cool-season and warm-season graminoids (mainly woolly sedge, wheat sedge, and Sartwell’s sedge) along with prairie cordgrass and northern reedgrass. Prior to European influence the primary disturbance mechanisms for this site in the reference condition included water level fluctuations, periodic fire, and grazing by large herding ungulates. Spring snowmelt runoff and rainfall events, coupled with timing of fires and grazing events, dictated the dynamics that occurred within the natural range of variability. Along with water level fluctuations and water chemistry, present day primary disturbances are from concentrated livestock grazing and a lack of fire. Under these conditions, vegetation for livestock and wildlife can be expected to decline along with a corresponding increase in less desirable vegetation. Wet Meadow ecological sites are highly influenced by water levels (including saturated soil), water movement, and water chemistry (i.e., discharge and recharge hydrology). Water levels influence fire effectiveness and livestock use. Water levels also influence exotic species invasion. As Wet Meadow sites draw-down (drying and losing soil moisture), they transition to functioning as an upland ecological site and can increase in salinity/alkalinity. Exotic cool-season grasses and forbs begin to invade starting from the upland edge of the Wet Meadow ecological site moving toward the deeper portion of the wetland. Many factors will dictate the speed of exotic species invasion including duration of draw-down phase, management of the sites during the draw-down phase, changes in soil chemistry, and availability of exotic species seed or plants parts (e.g., propagules). During extended periods of draw-down, presence of exotic species adjacent to the site and lack of fire or heavy season-long livestock grazing can speed up the invasion of cool-season exotic grasses or forbs, such as Canada thistle or field sowthistle. Once the site is invaded, increased water depth can begin to reverse the invasion of exotic species. However, the increase in salt accumulation will be difficult to reverse back to levels prior to extended periods of draw- down. In addition, exotic cool-season grasses (such as quackgrass along with foxtail barley) can tolerate extended periods of inundation or saturation, never totally drowning out along the outer margins of the Wet Meadow site. The continued presence of exotic cool-season grasses prevents the site from transitioning back to State 1: Reference State.
Characteristics and indicators. Because of changes in disturbances and other environmental factors (particularly the widespread occurrence of exotic species), the Reference State is increasingly rare.
Resilience management. If intact, the reference state should be managed with current disturbance regimes which has permitted the site to remain in reference condition as well as maintaining the quality and integrity of associated upland ecological sites. Maintenance of the reference condition is contingent upon a monitoring protocol to guide management.
Community 1.1
Sedges/Prairie Cordgrass (Carex spp./Spartina pectinata)
This community phase evolved with grazing by large herbivores, occasional prairie fires, and relatively frequent shallow ponding or saturation events. It may be found on areas that are properly managed with grazing and/or prescribed burning, and sometimes on areas receiving occasional short periods of rest. Woolly sedge is typically the dominant graminoid while prairie cordgrass is the dominant warm-season grass and northern reedgrass the dominant cool-season species. A variety of sedges and rushes also occur throughout this community (e.g., wheat sedge, mountain rush, spikerushes). Switchgrass and fowl bluegrass are also common. Common forbs often include Canada germander, goldenrods, Flodman’s thistle, Indianhemp, white doll’s aster, and white panicle aster. Shrubs such as willows (e.g., Bebb willow), rose (e.g., prairie rose), and redosier dogwood are often minor components. Annual production can vary from roughly 4000-5000 pounds per acre, consisting of about 90 percent grasses and grass-likes, 5 percent forbs, and 5 percent shrubs. The community is further described in the “Plant Community Composition and Group Annual Production” portion of this ecological site description. This plant community phase is diverse, stable, productive, and well adapted to the Northern Great Plains. Temporary ponding or a high-water table supplies much of the moisture for plant growth; the plant composition and diversity will shift with these changes. This is a sustainable plant community in terms of soil stability, watershed function, and biologic integrity.
Figure 8. Annual production by plant type (representative values) or group (midpoint values)
Table 5. Annual production by plant type
Plant type | Low (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
---|---|---|---|
Grass/Grasslike | 2770 | 2970 | 3170 |
Shrub/Vine | 1100 | 1350 | 1600 |
Forb | 130 | 180 | 230 |
Total | 4000 | 4500 | 5000 |
Figure 9. Plant community growth curve (percent production by month). ND5410, Missouri Slope, Lowland, Warm Season Dominant. Lowland, warm-season dominant, cool-season subdominant..
Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
---|---|---|---|---|---|---|---|---|---|---|---|
J | F | M | A | M | J | J | A | S | O | N | D |
0 | 0 | 0 | 3 | 22 | 30 | 30 | 8 | 5 | 2 | 0 | 0 |
Community 1.2
Fowl Bluegrass/Spikerushes-Mountain Rush/Forbs (Poa palustris/Eleocharis spp.-Juncus arcticus/Forbs)
This community develops during periods of heavy season-long grazing, particularly during decreasing or low water conditions when grazing pressure on the site is disproportionately high. Compared to Community Phase 1.1, prairie cordgrass, northern reedgrass, and switchgrass have declined with noticeable increases in fowl bluegrass, spikerushes, mountain rush, and forbs. Common forbs include asters, goldenrods, and cinquefoils.
Pathway 1.1A
Community 1.1 to 1.2
Community Phase Pathway 1.1 to 1.2 occurs with below average precipitation and heavy season-long grazing. This is associated with a drop in water level and an increased frequency and intensity of grazing due to limited forage availability on the adjacent upland sites.
Pathway 1.2A
Community 1.2 to 1.1
Community Phase Pathway 1.2 to 1.1 results with the return to average precipitation resulting in higher water table and deeper ponding. If found the implementation of long-term prescribed grazing and prescribed burning may be needed to maintain in Community phase 1.1. This results in noticeable increases in prairie cordgrass, northern reedgrass, and switchgrass.
State 2
Native/Invaded State
This state may be characterized as consisting of similar community phases as found in the Reference State (i.e., Community Phase 1.1 and 1.2); but the site has now been colonized by exotic plants (such as redtop, creeping meadow foxtail, and/or exotic strains/hybrids of reed canarygrass). During dry period drawdown stages, cool-season exotics (such as Kentucky bluegrass, smooth brome, quackgrass, and barnyardgrass) are common under extended periods of no use and no fire. Canada thistle is also a frequent exotic on the state. Although the state is still dominated by native cool-season grasses and graminoids, an increase in the exotic cool-season grasses can be expected. These exotic cool-season grasses have been particularly and consistently invasive under extended periods of no use and no fire. To slow or limit the invasion of these exotic grasses, it is imperative that managerial techniques (e.g., prescribed grazing, prescribed burning, other) be carefully constructed, monitored, and evaluated with respect to that objective. If management does not include measures to control or reduce these exotic cool-season grasses, the transition to State 3: Invaded State should be expected. Production and diversity are typically much reduced compared to that of the Reference State. Production can vary widely due to variations in environmental factors and the extent of exotic grasses. However, annual production may be in the range of 3300-6000 pounds per acre. Willows (e.g., Bebb willow) may be present in this state. They may markedly increase, particularly during periods of infrequent fire (i.e., roughly 5-10 year intervals), leading to the transition to State 3: Wooded State (T2A). Restoration of State 2: Native/Invaded State back to State 1: Reference State is not considered to be achievable. However, it should be noted that, if the major invader is exotic strains/hybrids of reed canarygrass, prescribed grazing techniques that target reed canarygrass may be a good choice for restoration efforts because the species is not very tolerant of heavy grazing.
Characteristics and indicators. The presence of trace amounts of exotic cool-season grasses indicates a transition from State 1 to State 2. The presence of exotic biennial or perennial leguminous forbs (i.e., sweet clover, black medic) may not, on their own, indicate a transition from State 1 to State 2 but may facilitate that transition.
Resilience management. To slow or limit the invasion of these exotic grasses, it is imperative that managerial techniques (e.g., prescribed grazing, prescribed burning) be carefully constructed, monitored, and evaluated with respect to that objective. Grazing management should be applied that enhances the competitive advantage of native grass and forb species. This may include: (1) early spring grazing when exotic cool-season grasses are actively growing and native cool-season grasses are dormant; (2) applying proper deferment periods allowing native grasses to recover and maintain or improve vigor; (3) adjusting overall grazing intensity to reduce excessive plant litter (above that needed for rangeland health indicator #14 – see Rangeland Health Reference Worksheet); (4) incorporating early heavy spring utilization which focuses grazing pressure on exotic cool-season grasses and reduces plant litter provided that livestock are moved when grazing selection shifts from exotic cool-season grasses to native grasses. Prescribed burning should be applied in a manner that maintains or enhances the competitive advantage of native grass and forb species. Prescribed burns should be applied as needed to adequately reduce/remove excessive plant litter and maintain the competitive advantage for native species. Timing of prescribed burns (spring vs. summer vs. fall) should be adjusted to account for differences in annual growing conditions and applied during windows of opportunity to best shift the competitive advantage to the native species.
Community 2.1
Sedges/Prairie Cordgrass (Carex spp./Spartina pectinata)

Figure 10. Community Phase 2.1: Sedges/Prairie Cordgrass linear wet meadow, majority of hydrology provided by ground water movement. Prairie cordgrass and sedge dominated.
This plant community phase is similar in composition and production to that of Plant Community Phase 1.1 but has been colonized by exotic plants. It often develops under conditions of no use and no fire which can result in excessive litter accumulation which exacerbates the invasion by exotic strains/hybrids of reed canarygrass, Canada thistle, and perhaps red top. It can also develop under heavy season-long grazing.
Community 2.2
Fowl Bluegrass/ Spikerushes - Mountain Rush/Forbs (Poa palustris/ Eleocharis spp.-Juncus arcticus/ Forbs)
This plant community phase develops with heavy season-long grazing during periods of below average precipitation leading to a lower water table and a decrease in ponding levels. Sedge, mountain rush, spikerushes, and bulrushes will increase noticeably. Prairie cordgrass and sedges will decline, while grazing tolerant invasive plants (e.g., creeping meadow foxtail) may become prevalent if a seed source is present or nearby. This plant community is somewhat resistant to change. A combination of both prescribed grazing and prescribed burning is most effective in moving this plant community towards the Reference State. This community phase is often dispersed throughout a pasture in an overgrazed/ undergrazed pattern, typically referred to as patch grazing. Some overgrazed areas will exhibit the impacts of heavy use, while the ungrazed areas will have a build-up of litter and increased plant decadence. This is a typical pattern found in properly stocked pastures grazed season-long. As a result, Kentucky bluegrass tends to increase more in the undergrazed areas while the more grazing-tolerant, short statured species (such as blue grama and sedges) increase in the heavily grazed areas. If present, Kentucky bluegrass may increase under heavy grazing.
Community 2.3
Foxtail Barley/Mountain Rush-Spikerushes/Bare Ground
This plant community phase develops under prolonged conditions of disturbance (e.g., heavy season-long grazing) particularly during periods of below average precipitation when water tables are lower and ponding levels decrease and salinity increases (discharge site). The prolonged nature of this disturbance will tend to increase soil temperatures and evaporation, causing this site to become drier. Foxtail barley often becomes a prominent component of the community, largely resulting from an increase in soil salinity/sodicity and lack of utilization by livestock once awns begin to appear.
Pathway 2.1A
Community 2.1 to 2.2
Community Phase Pathway 2.1 to 2.2 occurs during times of heavy season-long grazing in conjunction with below average precipitation leading to a lower water table and a decrease in ponding levels.
Pathway 2.2A
Community 2.2 to 2.3
Community Phase Pathway 2.2 to 2.3 occurs with heavy season-long grazing along with a decrease in water depth and increased salinity (discharge site).
Pathway 2.3A
Community 2.3 to 2.2
Community Phase Pathway 2.3 to 2.2 occurs with long-term prescribed grazing in conjunction with increased precipitation leading to an increase in ponding depth above plant height leading to plant mortality.
State 3
Wooded State
This state occurs throughout the MLRA and often results from extended periods of no fire or infrequent fire. A threshold leading to this state appears to occur over roughly 5-10 years of no fire. Bebb willow and many other willows resprout following burns. A vigorous sprouting response, in combination with increased growth (e.g., size, canopy cover) and reduced fine fuel loads beneath the canopy, often enables the willows to increase with infrequent fires. Older, larger plants survive the fires while smaller and younger plants resprout following a burn. Over time, the willows may form rather extensive stands or thickets. A marked increase in non-use management and active fire suppression since European influence has enabled this state to expand and become more widespread.
Characteristics and indicators. The dominance of woody species (by cover and production) distinguishes this state from other herbaceously dominated states.
Resilience management. This state is resistant to change in the long-term absence of fire. Restoration efforts would require the use of prescribed fire, mechanical treatment, and prescribed grazing. Considerable time and effort will be required to restore to other states.
Community 3.1
Willows (Salix spp.)
This plant community phase is dominated by willows (e.g., Bebb willow). Associated shrubs may include redosier dogwood and perhaps white meadowsweet. Sedges and rushes generally dominate the herbaceous understory. Trees (such as Plains cottonwood and quaking aspen) may also occupy the site, particularly as a ring of trees at the margins of wetlands. Once established, this plant community is very resilient and resistant to change. The lack of fine fuels in the understory and high degree of shading makes the application of prescribed burning very difficult without a mechanical pretreatment a year to two prior to the burn.
State 4
Invaded/Saline State
Foxtail barley is a conspicuous component of the community; however, the exotic grasses make up the bulk of the vegetation. Plant composition and extent of bare ground can be quite variable due to climatic conditions and grazing intensity. Several exotic grasses may be present alone or in combination (e.g., redtop, creeping meadow foxtail, and/or exotic strains/hybrids of reed canarygrass). During dry period drawdown stages, cool- season exotics (such as Kentucky bluegrass, smooth brome, quackgrass, and barnyardgrass) are common under extended periods of no use and no fire. Common exotic forbs include Canada thistle, kochia, lambsquarters, and field sowthistle. Marsh fleabane (aka swamp ragwort) is also occasionally abundant on the site particularly during drawdown periods.
Characteristics and indicators. This site is characterized by exotic cool-season grasses constituting greater than 30 percent of the annual production and native grasses and grass-likes constituting less than 40 percent of the annual production.
Resilience management. Salinity levels need to be considered when developing management alternatives. Light or moderately stocked continuous, season-long grazing or a prescribed grazing system which incorporates adequate deferment periods between grazing events and proper stocking rate levels will maintain this State. Application of herbaceous weed treatment, occasional prescribed burning, and/or brush management may be needed to manage noxious weeds and increasing shrub (e.g., western snowberry) populations.
Community 4.1
Foxtail Barley/Exotic Grasses/Exotic Forbs (Hordeum jubatum/Exotic Grasses/Exotic Forbs)
This community phase is a saline phase of the invaded states; as such, it is predominantly composed of exotic grasses (e.g., barnyardgrass, quackgrass, and/or exotic strains/hybrids of reed canarygrass) alone or in combination. Foxtail barley, however, is generally a conspicuous component and is an indicator of the saline conditions. Other grasses are largely halophytic species and may include saltgrass, alkaligrass, and scratchgrass.
State 5
Invaded/Fresh Water State
This community is the freshwater phase of the Invaded State and appears similar to Community Phase 2.2. Exotic grasses dominate the site and may consist of Kentucky bluegrass, quackgrass, smooth brome, and barnyard grass (alone or in combination). Although foxtail barley may be present, it is much reduced compared to that of State 4: Invaded/Saline State. Canada thistle, field sowthistle, and lambsquarters are common forbs.
Characteristics and indicators. This site is characterized by exotic cool-season grasses constituting greater than 30 percent of the annual production and native grasses and grass-likes constituting less than 40 percent of the annual production.
Resilience management. Light or moderately stocked continuous, season-long grazing or a prescribed grazing system which incorporates adequate deferment periods between grazing events and proper stocking rate levels will maintain this State. Application of herbaceous weed treatment, occasional prescribed burning, and/or brush management may be needed to manage noxious weeds and increasing shrub (e.g., western snowberry) populations.
Community 5.1
Exotic Grasses/Exotic Forbs/Sedges/Rushes (Exotic Grasses/Exotic Forbs/Carex spp./Juncus spp.)
This community is the freshwater phase of the invaded states and appears similar to Community Phase 2.2. Exotic grasses (such as redtop, creeping meadow foxtail, and/or exotic strains/hybrids of reed canarygrass) dominate the site. During dry period drawdown stages, cool-season exotics (such as Kentucky bluegrass, smooth brome, quackgrass, and barnyardgrass) are common under extended periods of no use and no fire. Although foxtail barley may be present, it is much reduced compared to that of State 4: Invaded/Saline State. Canada thistle, field sowthistle, and lambsquarters are common forbs. Several species of sedges and rushes may still be present but compose a minor component of the community.
State 6
Invaded/Eutrophication State
This state results from eutrophication and sedimentation of the site, often due to tillage on or adjacent to the site. Depending upon what seeds, rhizomes, and propagules are present in the substrate, monotypic stands of hybrid cattails or exotic strains/hybrids of reed canarygrass often develop. A rise in water levels, particularly when in association with wetlands, may also lead to dominance by cattails.
Characteristics and indicators. This site is characterized by exotic cool-season grasses constituting greater than 30 percent of the annual production and native grasses and grass-likes constituting less than 40 percent of the annual production.
Resilience management. Light or moderately stocked continuous, season-long grazing or a prescribed grazing system which incorporates adequate deferment periods between grazing events and proper stocking rate levels will maintain this State. Application of herbaceous weed treatment, occasional prescribed burning, and/or brush management may be needed to manage noxious weeds and increasing shrub (e.g., western snowberry) populations.
Community 6.1
Hybrid Cattail or Reed Canarygrass (Typha x glauca or Phalaris arundinacea)
Whether the site becomes dominated by hybrid cattail or exotic strains/hybrids of reed canarygrass is largely the result of which seeds, rhizomes, or propagules are present on the site. Either way, the community has little diversity, with the cattail or reed canarygrass forming virtual monocultures. Canada thistle, field sowthistle, and some asters may be present in the reed canarygrass stands
State 7
Go-Back State
This state is highly variable depending on the level and duration of disturbance related to the T8A pathway. In this MLRA, the most probable origin of this state is plant succession following crop abandonment. This plant community will initially include a variety of annual forbs and grasses, some of which maybe noxious weeds.
Characteristics and indicators. Tillage has destroyed the native plant community, altered soil structure and biology, reduced soil organic matter, and resulted in the formation of a tillage induced compacted layer which is restrictive to root growth. Removal of perennial grasses and forbs results in decreased infiltration and increased runoff.
Resilience management. Continued tillage will maintain the state. Control of noxious weeds will be required.
Community 7.1
Annual/Pioneer Perennial/Exotics
Plant composition of this state can be quite variable due to variations in hydrology, salinity, and other factors. In this MLRA, the most probable origin of this phase is plant succession following cropland abandonment. This plant community will initially include a variety of annual forbs and grasses, some of which may be noxious weeds needing control. However, plants commonly occurring in this state include quackgrass, foxtail barley, barnyardgrass, goosefoot, field sowthistle, knotweed, smartweed, burningbush, and beggartick. Restoration efforts to several states can be successful. It should be noted, however, that well-established stands of Canada thistle, field sowthistle, or quackgrass are particularly difficult to restore.
State 8
Any Plant Community
Transition T1A
State 1 to 2
This is the transition from the State 1: Reference State to State 2: Native/Invaded State over several years of no use and no fire or heavy season-long grazing. This transition is probably inevitable; it often results from colonization by exotic cool-season grasses (such as redtop, creeping meadow foxtail, and/or exotic strains/hybrids of reed canarygrass). During dry period drawdown stages, cool-season exotics (such as Kentucky bluegrass, smooth brome, quackgrass, and barnyardgrass) are common under extended periods of no use and no fire. Canada thistle is also a frequent exotic on the state.
Constraints to recovery. Current knowledge and technology will not facilitate a successful restoration to Reference State.
Transition T2A
State 2 to 3
This is the transition from State 2: Native/Invaded State to State 3: Wooded State. It often results from extended periods of no fire or infrequent fire. This transition appears to cross a threshold after roughly 5-10 years of no fire. Bebb willow and many other willows resprout following burns. A vigorous sprouting response, in combination with increased growth (e.g., size, canopy cover) and reduced fine fuel loads beneath the canopy, often enables the willows to survive subsequent fires and perhaps even expand coverage.
Constraints to recovery. Labor and financial cost of removal/control of woody species either through repeated prescribed burns, mechanical and/or chemical treatment.
Transition T2B
State 2 to 4
This is the transition from State 2: Native/Invaded State to State 4: Invaded/Saline State due to heavy season- long grazing during times of below average precipitation leading to a lower water table and a decrease in ponding levels and an increase brackish (alkalinity/salinity) condition (discharge site).
Constraints to recovery. Variations in growing conditions (e.g., cool, wet spring) will influence effects of various management activities on exotic cool-season grass populations.
Transition T2C
State 2 to 5
This is the transition from State 2: Native/Invaded State to State 5: Invaded/Fresh Water State during times of a lower water table and a decrease in ponding levels and freshwater conditions on conjunction with heavy season-long grazing.
Constraints to recovery. Variations in growing conditions (e.g., cool, wet spring) will influence effects of various management activities on exotic cool-season grass populations.
Transition T2D
State 2 to 6
This is the transition from State 2: Native/Invaded State to State 6: Invaded/Eutrophication State resulting from eutrophication and sedimentation of the site, often due to tillage on or adjacent to the site. Hybrid cattail or exotic strains/hybrids of reed canarygrass become dominant. A rise in water levels, particularly when in association with Shallow Marsh ecological sites, may also lead to dominance by cattails.
Constraints to recovery. Variations in growing conditions (e.g., cool, wet spring) will influence effects of various management activities on exotic cool-season grass populations.
Restoration pathway R3A
State 3 to 2
This is the restoration pathway from State 3: Wooded State to State 2: Native/Invaded State due to high willow mortality resulting from mechanical treatment followed by long-term prescribed burning. The prescribed burning will likely require repeated treatments because many of the willows will resprout following one burn.
Context dependence. Prescribed burning should be applied in a manner that enhances the competitive advantage of native grass and forb species over the exotic species. Prescribed burns should be applied at a frequency which mimics the natural disturbance regime or more frequently as is ecologically (e.g., available fuel load) and economically feasible. Burn prescriptions may need adjustment to: (1) account for change in fuel type (herbaceous vs. shrub vs. tree), fine fuel amount and orientation; (2) fire intensity and duration by adjusting ignition pattern (e.g., backing fires vs head fires); (3) account for plant phenological stages to maximize stress on woody and exotic species while favoring native species (both cool- and warm-season grasses). The method of brush management will be site specific but generally the goal would be to apply the pesticide, mechanical control or biological control (either singularly or in combination) in a manner that shifts the competitive advantage from the targeted species to the native grasses and forbs. The control method(s) should be as specific to the targeted species as possible to minimize impacts to non-target species.
Restoration pathway R4A
State 4 to 2
This is the restoration of State 4: Invaded/Saline State to State 2: Native/Invaded State resulting from extended periods of above average precipitation causing an increase in ponding level above the height of most exotic grasses. This results in considerable mortality of the exotic grasses and is sufficient to move the plant composition to more freshwater species.
Context dependence. Salinity levels need to be considered when developing management alternatives. Grazing management should be applied in a manner that enhances/maximizes the competitive advantage of native grass and forb species over the exotic species. This may include the use of prescribed grazing to reduce excessive plant litter accumulations above that needed for rangeland health indicator #14 (see Rangeland Health Reference Worksheet). Increasing livestock densities may facilitate the reduction in plant litter provided length and timing of grazing periods are adjusted to favor native species. Grazing prescriptions designed to address exotic grass invasion and favor native species may involve earlier, short, intense grazing periods with proper deferment to improve native species health and vigor. Fall (e.g., September, October) prescribed burning followed by an intensive, early spring graze period with adequate deferment for native grass recovery may shift the competitive advantage to the native species, facilitating the restoration to State 2: Native/Invaded. Prescribed burning should be applied in a manner that enhances the competitive advantage of native grass and forb species over the exotic species. Prescribed burns should be applied at a frequency which mimics the natural disturbance regime, or more frequently as is ecologically (e.g., available fuel load) and economically feasible. Burn prescriptions may need adjustment to: (1) account for change in fine fuel orientation; (2) fire intensity and duration by adjusting ignition pattern (e.g., backing fires vs head fires); (3) account for plant phenological stages to maximize stress on exotic species while favoring native species (both cool- and warm- season grasses). The longer this community phase exists, the more resilient it becomes. Natural or management disturbances that reduce the cover of cool-season exotic grasses are typically short-lived.
Restoration pathway R5A
State 5 to 2
This is the restoration of State 5: Invaded/Fresh Water State to State 2: Native/Invaded State during extended periods of above average precipitation leading to an increase in ponding level above the height of most exotic grasses. This results in considerable mortality and is sufficient to move the plant composition to more freshwater species.
Context dependence. Grazing management should be applied in a manner that enhances/maximizes the competitive advantage of native grass and forb species over the exotic species. This may include the use of prescribed grazing to reduce excessive plant litter accumulations above that needed for rangeland health indicator #14 (see Rangeland Health Reference Worksheet). Increasing livestock densities may facilitate the reduction in plant litter provided length and timing of grazing periods are adjusted to favor native species. Grazing prescriptions designed to address exotic grass invasion and favor native species may involve earlier, short, intense grazing periods with proper deferment to improve native species health and vigor. Fall (e.g., September, October) prescribed burning followed by an intensive, early spring graze period with adequate deferment for native grass recovery may shift the competitive advantage to the native species, facilitating the restoration to State 2: Native/Invaded. Prescribed burning should be applied in a manner that enhances the competitive advantage of native grass and forb species over the exotic species. Prescribed burns should be applied at a frequency which mimics the natural disturbance regime, or more frequently as is ecologically (e.g., available fuel load) and economically feasible. Burn prescriptions may need adjustment to: (1) account for change in fine fuel orientation; (2) fire intensity and duration by adjusting ignition pattern (e.g., backing fires vs head fires); (3) account for plant phenological stages to maximize stress on exotic species while favoring native species (both cool- and warm- season grasses). The longer this community phase exists, the more resilient it becomes. Natural or management disturbances that reduce the cover of cool-season exotic grasses are typically short-lived.
Restoration pathway R6A
State 6 to 2
This is the restoration pathway from State 6: Invaded/Eutrophication State to State 2: Native/Invaded State resulting from extended periods of above average precipitation leading to increased water level and chemical treatment, mechanical treatment, sediment removal, prescribed burning, and range planting. The aquatic version of glyphosate herbicide has been shown to be an effective method in restoration efforts. A range planting and, perhaps, the planting of plugs of plants (e.g., prairie cordgrass) have also been effective. Physically removing the sediment and associated rhizomes, seeds, etc., which are above the historical surface soil (A horizon), coupled with reseeding and replanting adapted plants as a range planting, is the most effective method of restoration.
Context dependence. Grazing management should be applied in a manner that enhances/maximizes the competitive advantage of native grass and forb species over the exotic species. This may include the use of prescribed grazing to reduce excessive plant litter accumulations above that needed for rangeland health indicator #14 (see Rangeland Health Reference Worksheet). Increasing livestock densities may facilitate the reduction in plant litter provided length and timing of grazing periods are adjusted to favor native species. Grazing prescriptions designed to address exotic grass invasion and favor native species may involve earlier, short, intense grazing periods with proper deferment to improve native species health and vigor. Fall (e.g., September, October) prescribed burning followed by an intensive, early spring graze period with adequate deferment for native grass recovery may shift the competitive advantage to the native species, facilitating the restoration to State 2: Native/Invaded. Prescribed burning should be applied in a manner that enhances the competitive advantage of native grass and forb species over the exotic species. Prescribed burns should be applied at a frequency which mimics the natural disturbance regime, or more frequently as is ecologically (e.g., available fuel load) and economically feasible. Burn prescriptions may need adjustment to: (1) account for change in fine fuel orientation; (2) fire intensity and duration by adjusting ignition pattern (e.g., backing fires vs head fires); (3) account for plant phenological stages to maximize stress on exotic species while favoring native species (both cool- and warm- season grasses). The longer this community phase exists, the more resilient it becomes. Natural or management disturbances that reduce the cover of cool-season exotic grasses are typically short-lived.
Restoration pathway R7A
State 7 to 2
This restoration pathway from State 7: Go-Back State to State 2: Native/Invaded State may be accomplished through a hydrological restoration (e.g., breaking tile or plugging a drain) and a range planting.
Context dependence. Reed canarygrass and hybrid cattail are difficult to control, largely due to vigorously spreading rhizomes, high seed production, and a large seed bank. Various control techniques may show signs of success but are often short-term with vegetation reverting within a few years. Adjacent upland ecological sites will need to remain intact or reseeded to native species to prevent sedimentation and nutrient loading to the Shallow Marsh ecological site. Prescribed grazing (e.g., heavy seasonal), high-intensity burns, and herbicides have shown some success in reducing the dominance by reed canarygrass. However, within several years the vegetation often reverts. Herbicides can be effective in reducing or eliminating hybrid cattail and can be followed by reseeding (or plugging) desirable species. Prescribed burning has also been effective during dry periods where fire temperatures may kill rhizomes and seeds. Although expensive, mechanical removal of the substrate has also been an effective technique.
Restoration pathway R7B
State 7 to 4
This restoration pathway from State 7: Go-Back State to State 4: Invaded/Saline State may be accomplished through no use, no fire, and no range planting with saline conditions and a hydrological restoration.
Context dependence. Reed canarygrass and hybrid cattail are difficult to control, largely due to vigorously spreading rhizomes, high seed production, and a large seed bank. Various control techniques may show signs of success but are often short-term with vegetation reverting within a few years. Prescribed grazing (e.g., heavy seasonal), high-intensity burns, and herbicides have shown some success in reducing the dominance by reed canarygrass. However, within several years the vegetation often reverts. Herbicides can be effective in reducing or eliminating hybrid cattail and can be followed by reseeding (or plugging) desirable species. Prescribed burning has also been effective during dry periods where fire temperatures may kill rhizomes and seeds. Although expensive, mechanical removal of the substrate has also been an effective technique.
Restoration pathway R7C
State 7 to 5
This restoration pathway from State 7: Go-Back State to State 5: Invaded/Fresh Water State may be accomplished through no use, no fire, and no range planting with freshwater conditions and a hydrological restoration.
Context dependence. Reed canarygrass and hybrid cattail are difficult to control, largely due to vigorously spreading rhizomes, high seed production, and a large seed bank. Various control techniques may show signs of success but are often short-term with vegetation reverting within a few years. Prescribed grazing (e.g., heavy seasonal), high-intensity burns, and herbicides have shown some success in reducing the dominance by reed canarygrass. However, within several years the vegetation often reverts. Herbicides can be effective in reducing or eliminating hybrid cattail and can be followed by reseeding (or plugging) desirable species. Prescribed burning has also been effective during dry periods where fire temperatures may kill rhizomes and seeds. Although expensive, mechanical removal of the substrate has also been an effective technique.
Restoration pathway R7D
State 7 to 6
This restoration pathway from State 7: Go-Back State to State 6: Invaded/Eutrophication State may be accomplished through no use and no fire under conditions of eutrophication and sedimentation with a hydrological restoration.
Context dependence. Reed canarygrass and hybrid cattail are difficult to control, largely due to vigorously spreading rhizomes, high seed production, and a large seed bank. Various control techniques may show signs of success but are often short-term with vegetation reverting within a few years. Prescribed grazing (e.g., heavy seasonal), high-intensity burns, and herbicides have shown some success in reducing the dominance by reed canarygrass. However, within several years the vegetation often reverts. Herbicides can be effective in reducing or eliminating hybrid cattail and can be followed by reseeding (or plugging) desirable species. Prescribed burning has also been effective during dry periods where fire temperatures may kill rhizomes and seeds. Although expensive, mechanical removal of the substrate has also been an effective technique.
Restoration pathway T8A
State 8 to 7
This transition from any plant community to State 4: Go-Back State. It is most commonly associated with the cessation of cropping without the benefit of range planting, resulting in a “go-back” situation. Soil conditions can be quite variable on the site, in part due to variations in the management/cropping history (e.g., development of a tillage induced compacted layer (plow pan), erosion, fertility, and/or herbicide/pesticide carryover). Thus, soil conditions should be assessed when considering restoration techniques.
Additional community tables
Table 6. Community 1.1 plant community composition
Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
---|---|---|---|---|---|---|
Grass/Grasslike
|
||||||
1 | Grass-Likes | 900–1575 | ||||
Sartwell's sedge | CASA8 | Carex sartwellii | 225–450 | – | ||
shortbeak sedge | CABR10 | Carex brevior | 225–450 | – | ||
woolly sedge | CAPE42 | Carex pellita | 180–360 | – | ||
clustered field sedge | CAPR5 | Carex praegracilis | 225–360 | – | ||
Grass-like (not a true grass) | 2GL | Grass-like (not a true grass) | 45–225 | – | ||
spikerush | ELEOC | Eleocharis | 135–225 | – | ||
flatsedge | CYPER | Cyperus | 45–90 | – | ||
mountain rush | JUARL | Juncus arcticus ssp. littoralis | 45–90 | – | ||
2 | Warm-Season Grasses | 900–1350 | ||||
prairie cordgrass | SPPE | Spartina pectinata | 900–1350 | – | ||
switchgrass | PAVI2 | Panicum virgatum | 135–225 | – | ||
mat muhly | MURI | Muhlenbergia richardsonis | 45–90 | – | ||
3 | Cool-Season Grasses | 675–1350 | ||||
northern reedgrass | CASTI3 | Calamagrostis stricta ssp. inexpansa | 450–675 | – | ||
American sloughgrass | BESY | Beckmannia syzigachne | 225–450 | – | ||
American mannagrass | GLGR | Glyceria grandis | 225–450 | – | ||
western wheatgrass | PASM | Pascopyrum smithii | 90–225 | – | ||
fowl bluegrass | POPA2 | Poa palustris | 45–90 | – | ||
tufted hairgrass | DECE | Deschampsia cespitosa | 45–90 | – | ||
4 | Other Native Grasses | 0–225 | ||||
rough bentgrass | AGSC5 | Agrostis scabra | 45–90 | – | ||
Grass, perennial | 2GP | Grass, perennial | 0–90 | – | ||
Forb
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5 | Forbs | 45–225 | ||||
dogbane | APOCY | Apocynum | 45–90 | – | ||
Maximilian sunflower | HEMA2 | Helianthus maximiliani | 45–90 | – | ||
Rydberg's sunflower | HENUR | Helianthus nuttallii ssp. rydbergii | 45–90 | – | ||
mint | MENTH | Mentha | 45–90 | – | ||
Canada goldenrod | SOCA6 | Solidago canadensis | 45–90 | – | ||
Flodman's thistle | CIFL | Cirsium flodmanii | 0–45 | – | ||
showy prairie gentian | EUEXR | Eustoma exaltatum ssp. russellianum | 0–45 | – | ||
cinquefoil | POTEN | Potentilla | 0–45 | – | ||
western dock | RUAQ | Rumex aquaticus | 0–45 | – | ||
blue-eyed grass | SISYR | Sisyrinchium | 0–45 | – | ||
Forb (herbaceous, not grass nor grass-like) | 2FORB | Forb (herbaceous, not grass nor grass-like) | 0–45 | – | ||
Shrub/Vine
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6 | Shrubs | 0–225 | ||||
willow | SALIX | Salix | 0–135 | – | ||
Shrub (>.5m) | 2SHRUB | Shrub (>.5m) | 0–135 | – |
Interpretations
Animal community
Animal Community – Wildlife Interpretations
Landscape
The MLRA 54 landscape is characterized by moderately dissected rolling plains with areas of local badlands, buttes, and isolated hills. MLRA 54 is considered to have a continental climate with cold winters and hot summers, low humidity, light rainfall, and much sunshine. Extremes in temperature are common and characteristic of the MLRA. This area supports natural mixed-grass prairie vegetation with prairie rose, leadplant, and patches of western snowberry interspersed throughout the area. Green ash, chokecherry, and buffaloberry occur in draws and narrow valleys creating woody riparian corridors. Complex intermingled ecological sites create diverse grass/shrub land habitats interspersed with varying densities linear, slope, depressional, and in-stream wetlands associated with headwater streams and tributaries to the Missouri River. These habitats provide critical life-cycle components for many wildlife species.
Historic Communities/Conditions within MLRA:
The northern mixed-grass prairie was a disturbance-driven ecosystem with fire, herbivory, and climate functioning as the primary ecological drivers (either singly or often in combination). Many species of grassland birds, small mammals, insects, reptiles, amphibians, and large herds of roaming American bison, elk, and pronghorn were historically among the inhabitants adapted to this semi-arid region. Roaming herbivores, as well as several small mammal and insect species, were the primary consumers linking the grassland resources to large predators (such as the wolf, mountain lion, and grizzly bear) and smaller carnivores (such as the coyote, bobcat, red fox, and raptors). The black-tailed prairie dog was once abundant and provided ecological services by manipulating the plant and soil community, thus providing habitat for the black-footed ferret, burrowing owl, ferruginous hawk, mountain plover, swift fox, small mammals, and amphibians and reptiles. Extirpated species include free-ranging American bison, grizzly bear, gray wolf, black- footed ferret, mountain plover, and peregrine falcon (breeding). Extinct from the region is the Rocky Mountain locust.
Present Communities/Conditions within MLRA:
Following European influence, domestic livestock grazing, elimination of fire, energy development, and other anthropogenic factors influenced plant community composition and abundance. Agriculture, transportation corridors, and energy development are the main factors contributing to habitat fragmentation, reducing habitat quality for area-sensitive species. These influences fragmented the landscape; reduced or eliminated ecological drivers (fire); and introduced exotic species including smooth brome, crested wheatgrass, Kentucky bluegrass, and leafy spurge. This further impacted plant and animal communities. The loss of the bison, black-tailed prairie dogs, and fire as primary ecological drivers greatly influenced the character of the remaining native plant communities and the associated wildlife, moving towards a less diverse and more homogeneous landscape. Included in this MLRA are the isolated Killdeer Mountains (limestone capped residual butte) containing bur oak, quaking aspen, green ash, paper birch, and American elm. Except for floodplain forests within the MLRA, the Killdeer Mountains contain the largest deciduous forest in southwestern North Dakota.
Some wildlife species in this area are mule deer, white-tailed deer, elk, pronghorn, moose, coyote, red fox, bobcat, prairie rattlesnake, American badger, raccoon, North American porcupine, beaver, striped skunk, American mink, white-tailed jackrabbit, black-tailed prairie dog, Eastern and Merriam’s turkey, golden eagle, ferruginous hawks, sharp-tailed grouse, black-billed magpie, and numerous species of grassland-nesting birds and pollinating insects.
Presence of wildlife species is often determined by ecological site characteristics including grass and forb species, hydrology, aspect, and other associated ecological sites. The home ranges of a majority species are larger than one ecological site or are dependent on more than one ecological site for annual life requisites. Ecological sites offer different habitat elements as the annual life requisites change. Habitat improvement and creation must be conducted within the mobility limits of a known population for the species.
Insects play an important role providing ecological services for plant community development. Insects that are scavengers or aid in decomposition provide the food chain baseline sustaining the carnivorous insects feeding upon them. Many insects provide the ecological services necessary for pollination, keeping plant communities healthy and productive. Insects provide a protein food source for numerous species including grassland-nesting birds and their young.
Species unique to MLRA:
Bald eagle: Bald Eagles prefer large rivers, lakes, reservoirs, or wetlands that are bordered by mature stands of trees or a single large tree. Bald eagles use the Missouri River system, including Lakes Sakakawea and Oahe, and associated tributaries. Mature trees, including cottonwoods, provide nesting sites adjacent to aquatic and upland foraging sites.
Dakota skipper: The extreme northern portion of this MLRA provides limited Dakota skipper habitat. Dakota skipper habitat within MLRA 54 is considered Type B habitat. Type B habitat is described as rolling native-prairie terrain over gravelly glacial moraine deposits dominated by bluestems and needlegrasses with the likely presence of bluebell bellflower, wood lily, purple coneflower, upright prairie coneflower, and blanket flower. The United States Fish and Wildlife Service lists two critical habitat units within the MLRA in McKenzie County, North Dakota.
Golden eagle: The Lake Sakakawea breaks, bluffs, and rock outcroppings within the northwest portion of the MLRA are key areas for golden eagle nesting. Grasslands, shrublands, and black-tailed prairie dog towns are used for foraging.
Black-footed ferret: Black-footed ferrets have been reintroduced as an experimental population in the southern portion of the MLRA located on the Cheyenne Sioux Indian Reservation. Since reintroduction between 1991 and 1996, black-footed ferrets have been documented on the Standing Rock Sioux Indian Reservation approximately 20 miles north of the reintroduction site. Black-footed ferrets rely exclusively on prairie dog towns for shelter, breeding, and food sources (prairie dogs and other species within the town).
Least tern (Interior): Least terns are found on the Missouri River system in MLRA 54. Sparsely vegetated sandbars within the free-flowing portions of the Missouri River or shorelines of Lake Oahe and Sakakawea are used for nesting and foraging.
Species of Concern within the MLRA:
The following is a list of species considered “species of conservation priority” in the North Dakota State Wildlife Action Plan (2015); “species of greatest conservation need” in the Montana State Wildlife Action Plan (2015) and the South Dakota State Wildlife Action Plan (2014); and “species listed as threatened, endangered, or petitioned” under the Endangered Species Act within MLRA 54 at the time this section was developed:
Invertebrates: Dakota skipper, little white tiger beetle, monarch butterfly, Ottoe skipper, regal fritillary, yellow-banded bumble bee, and western bumble bee.
Birds: American Kestrel, Baird’s sparrow, bald eagle, black-billed cuckoo, black tern, bobolink, Brewer’s sparrow, burrowing owl, chestnut-collared longspur, ferruginous hawk, golden eagle, grasshopper sparrow, greater sage-grouse, lark bunting, loggerhead shrike, least tern, long-billed curlew, marbled godwit, McCown’s longspur, mountain plover, northern goshawk, northern harrier, northern pintail, peregrine falcon (migration), piping plover, prairie falcon, red knot (migration), red- headed woodpecker, sharp-tailed grouse, short-eared owl, Sprague’s pipit, Swainson’s hawk, trumpeter swan, upland sandpiper, western meadowlark, willet, Wilson’s phalarope, and whooping crane (migration).
Mammals: Big and little brown bats, long-eared bat, long-legged bat, northern long-eared bat, Townsend’s big-eared bat, western small-footed bat, black-footed ferret, black-tailed prairie dog, dwarf shrew, gray wolf, hispid pocket mouse, Merriam’s shrew, northwestern moose, sagebrush vole, silver-haired bat, and swift fox.
Amphibians/Reptiles: Common snapping turtle, Great Plains toad, false map turtle, greater short- horned lizard, milk snake, northern leopard frog, plains hognose snake, plains spadefoot, smooth green snake, and smooth softshell and spiny softshell turtle.
Fish and Mussels: Blue sucker, burbot, flathead chub, fragile papershell, northern redbelly dace, paddlefish, pallid sturgeon, pearl dace, pink papershell, shortnose gar, sickle-fin chub, sturgeon chub, and sauger.
Grassland Management for Wildlife in the MLRA
Management activities within the community phase pathways impact wildlife. Community phase, transitional, and restoration pathways are keys to long-term management within each state and between states. Significant inputs must occur to cross the threshold between states (e.g., State 3.0 to 2.0) requiring substantial economic inputs and management (mechanical, reseeding, prescribed fire, woody vegetation removal, grazing intensity, etc.). Timing, intensity, and frequency of these inputs can have dramatic positive or negative effects on local wildlife species. Ranchers and other land managers must always consider the long-term beneficial effects of management on the habitat in comparison to potential short-term negative effects to individuals.
Ecological sites occur as intermingled complexes on the landscape with gradual or sometimes abrupt transitions. Rarely do ecological sites exist in large enough acreage to manage independently. Ecological sites that support a dominance of herbaceous vegetation (Loamy/Clayey) can be located adjacent to ecological sites that support medium to tall shrubs (Loamy Overflow). Conversely, ecological sites that are dominated by short- to mid-statured grasses (Claypan) can be adjacent to sites with bare soil only supporting minor amounts of short grasses and forbs (Thin Claypan).
Management of these complex ecological sites can provide a heterogeneous or a homogenous landscape. Grassland bird use declines as the plant community transitions to a homogenous state. Managers should recognize ecological sites and the complexes they occur in to properly manage the landscape. A management regime for one ecological site may negatively impact an adjacent site; for example, alteration of a grazing regime within a Loamy Overflow ecological site to encourage understory growth may encourage exotic cool-season grasses to increase or dominate an adjacent ecological site.
Life requisites and habitat deficiencies are determined for targeted species. Deficiencies must be addressed along community phase, transitional, and restoration pathways as presented in specific state-and-transition models. Ecological sites should be managed and restored within the site’s capabilities to provide sustainable habitat. Managers also should consider habitat provided by adjacent/intermingled ecological sites for species with home ranges or life requisites that cannot be provided by one ecological site.
With populations of many grassland-nesting birds in decline, it is important to maintain these ecological sites in a 1.0 Reference State (rarely found intact) or the 2.0 Native/Invaded. Plant communities optimal for a guild of grassland species serve as a population source where the birth rate exceeds mortality. Species may use marginal plant communities; however, these sites may function as a population sink where mortality exceeds the birth rate.
Understanding preferred vegetative stature and sensitivity to woody encroachment is necessary to manage for the specific grassland species. Various grass heights may be used for breeding, nesting, foraging, or winter habitat. While most species use varying heights, many have a preferred vegetative stature height. The following chart provides preferred vegetative stature heights and sensitivity to woody vegetation encroachment.
To view the chart, click on the hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/54_Wet_Meadow_Narrative_FINAL_Ref_FSG.pdf
Wet Meadow Wildlife Habitat Interpretation:
Wet Meadow ecological sites are poorly drained soils located primarily in depressions and on low- lying flats on upland (till plains and sedimentary plains). It also occurs in upland drainageways, in swales on sand sheets, and in relict oxbows now isolated from frequent stream flooding. Associated ecological sites include Closed Depression, Loamy, Loamy Overflow, Loamy Terrace, Sands, Sandy Terrace, Saline Lowland, Shallow Marsh, and Thin Claypan. This complex of ecological sites provides habitat for many edge-sensitive grassland bird species preferring short- to tall-statured vegetation.
Wet Meadow habitat features and components commonly support grassland-nesting birds, notably birds utilizing wetland vegetation habitats (such as Nelson’s and LeConte’s sparrow and sedge wren). Sharp-tailed grouse use this site for wintering and escape cover. Insects rely on associated forbs and grasses for survival and serve as food sources for birds and their young and as forage for small and large herbivores. When dominated by trees such as eastern cottonwood or aspen, these sites provide excellent food, thermal, protective, and escape cover for white-tailed deer and moose.
Wet Meadow ecological sites may be found in seven plant community states within a local landscape. Multiple plant community phases exist within this ecological site dependent upon water levels, saturation, water and soil chemistry, and management. Today, these states occur primarily in response to precipitation (extended periods of above normal precipitation or drought), water chemistry, fire, grazing, non-use (lack of management), and other anthropogenic disturbances.
Because there is no known restoration pathway from State 2.0 to State 1.0, it is important to intensively manage using tools in State 1.0 and State 2.0 Community Phase Pathways to prevent further plant community degradation along Transitional Pathways to invaded plant communities of other States. Native wildlife, dependent upon shallow wetlands as found in the Wet Meadow ecological site, generally benefit from the heterogeneous grasslands/graminoids found in Community Phases in States 1.0 and 2.0. Plant communities within State 2.0 are dependent upon long-term changes in precipitation (compounded by grazing intensity and frequency). The transition to wetter or drier conditions results in a plant community that is either taller in stature (such as Plant Community Phase 2.1 Sedges/Prairie Cordgrass) in wetter conditions, or shorter in stature (such as 2.3 Foxtail Barley/Mountain Rush-Spikerush/Bare Ground) in drier conditions.
Management along community phase, transition, or restoration pathways should focus upon attainable changes. Short- and long-term monetary costs must be evaluated against short- and long- term ecological services in creating and maintaining habitat of sufficient quality to support a sustainable population density.
Hydrological manipulation (surface or tile drainage, pumping, surface water diversion, etc.) modifies this ecological site’s functions, having a significant negative impact to wetland dependent wildlife such as invertebrates, amphibians, and water birds. Without restoring hydrologic function (which may include range seeding), managers need to reference state and transition models within those sites.
Hydrology will need to be fully restored in Wet Meadow and Shallow Marsh ecological sites for these sites to properly function. It is recommended that managers review the appropriate State and Transition Models prior to wetland restoration.
1.0 Reference State
Community Phase 1.1 Sedges/Prairie Cordgrass: This plant community offers quality vegetative cover for wetland wildlife; every effort should be made to maintain this ecological site within this community phase. This phase retains high functionality through continued maintenance including prescribed grazing with adequate recovery period as well as prescribed fire. Prescribed fire maintains a grass-dominated plant community providing habitat for wetland bird species sensitive to woody vegetation.
Invertebrates: Insects play a role in maintaining the forb community and provide a forage base for grassland birds, wetland birds, and rodents. This plant community contains a variety of forbs providing season-long pollen and nectar. However, due to wet soils, ground nesting pollinator species do not prefer this site. Dakota skippers, regal fritillaries, or monarch butterflies will use this site when swamp milkweed, New England aster, or goldenrods occupy this site.
Wet Meadow ecological sites provide habitat for a diverse suite of aquatic invertebrates, providing an important trophic link between macrophytes and vertebrates that depend upon them as food. Rapid warming during spring snowmelt allows the invertebrate population to flourish. The vegetative structure provided by shallow, vegetated wetlands increase the abundance of aquatic invertebrates compared to less vegetated sites.
Birds: This plant community provides quality nesting, foraging, and escape habitats favored by mid- to tallgrass-nesting birds especially those species preferring wetter (hydric) habitats (such as Nelson’s sparrow, black tern, northern harrier, sedge wren, American avocet, Wilson’s phalarope, etc.). This site can provide waterfowl pair bonding sites, early season invertebrate food sources, and early season shorebird habitat. The rapid warming during spring snowmelt provides water birds an abundant invertebrate protein source for egg laying. Prescribed fire maintains a grass-dominated plant community providing habitat for bird species sensitive to woody vegetation. This plant community does not provide suitable areas for sharp-tailed grouse lek sites or nesting habitat. However, it does provide winter cover and escape habitat, as well as brood-rearing habitat. This site provides good hunting opportunities for grassland raptors, especially northern harrier.
Mammals: The diversity of grasses and forbs provide high nutrition levels for small and large herbivores including arctic and pygmy shrew, rodents, jackrabbits, and deer (white-tailed and mule), elk, and moose. Tall- to mid-statured vegetation provides suitable food, thermal, protective, and escape cover for small and large herbivores. In addition, it provides foraging opportunities for raccoon, skunks, coyotes and other mammals that use wetlands and wetland edges for food resources.
Amphibians and Reptiles: This ecological site can provide habitat for the northern leopard frog and Canadian toad. Dependent upon the duration of surface water, this site may provide breeding habitat. Successful egg-laying and tadpole development habitat is dependent upon depth and duration of ponded water.
Fish and Mussels: This ecological site can be directly associated with streams, rivers, or water bodies. This site receives run-on hydrology from adjacent ecological sites and provides hydrology to shallow ground water and other surface waterbodies. Management on Wet Meadow sites, in conjunction with neighboring run-off sites, will have a direct effect on aquatic species in streams and/or tributaries receiving water from Wet Meadow sites. Optimum hydrological function and nutrient cycling limit potential for sediment yield and nutrient loading to the adjacent aquatic ecosystems from Community Phase 1.1.
Community Phase 1.2 Fowl Bluegrass/Spikerushes-Mountain Rush/Forbs: This plant community phase occurs during periods of below normal precipitation lowering the water table. The lower water table allows the plant community to shift fowl bluegrass and mid-statured grass-likes, mountain rush, and spikerushes. The forb community remains robust favoring pollinator insects. This plant community provides a quality food source for grassland nesting birds.
Invertebrates: Provides similar life requisites as Community Phase 1.1. However, drying of the soil during periods of prolonged, below normal precipitation allows for an increase in forbs; this provides increased pollen and nectar sources and increased bare ground for ground-nesting insects. The diverse suite of aquatic invertebrates found in Community Phase 1.1 is reduced and may only be found in spring during periods of snowmelt runoff.
Birds: Provides similar life requisites as Community Phase 1.1. However, decreased surface water reduces invertebrate production and use by waterfowl and shorebirds. The drying of the soil during periods of prolonged, below normal precipitation provides additional opportunities for grassland nesting birds that use mid-to tall-statured herbaceous vegetation found in a mesic (dry) vs. hydric habitats.
Mammals: A shorter statured mix of wetland vegetation reduces thermal, protective, escape, and winter habitat for a big game animals and other small herbivores.
Amphibians and Reptiles: Drying of the soil during periods of prolonged, below normal precipitation removes saturated soil and/or ponded water. Use by northern leopard frog and Canadian toad will decrease. This plant community may provide foraging but breeding habitat will be lost for egg-laying and tadpole development without ponded water.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1; however, decreased runoff from this site may reduce stream flows or water quantity in other aquatic sites.
2.0 Native Invaded State
Community Phase 2.1 Sedges/Prairie Cordgrass: This plant community develops through Transition Pathway T1 due to changes in management and the presence of non-native species (such as reed canarygrass, redtop, Kentucky bluegrass, field sowthistle, and Canada thistle). This plant community phase has a very similar appearance and function to the Plant Community 1.1 with a wide array of forbs providing nectar and pollen sources for pollinating species. Managers should consider management within the State 2.0 Community Phase Pathways to avoid transitioning to other states within this ecological site.
Invertebrates: Provides similar life requisites as Community Phase 1.1.
Birds: Provides similar life requisites as Community Phase 1.1.
Mammals: Provides similar life requisites as Community Phase 1.1.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1.
Community Phase 2.2 Fowl Bluegrass/Spikerushes-Mountain Rush/Forbs: This plant community phase occurs with heavy season-long grazing coupled with periods of below normal precipitation lowering the water table. Grazing tolerant rush and spikerush species increase while prairie cordgrass and sedges decline.
Invertebrates: Heavy season-long grazing does not allow flowering plants to recover, limiting pollen and nectar resources for bees and other pollinating insects. In addition, a shift from perennial to annual forbs reduces season-long pollen and nectar sources for pollinating insect species. Prolonged periods of reduced precipitation favor ground nesting pollinators; however, increased compaction from mechanical impacts or increased livestock presence negatively impacts ground nesting pollinator opportunities. This shift to drier soil conditions reduces or eliminates aquatic invertebrates.
Birds: Provides similar life requisites as Community Phase 1.2. In addition, the drying of the soil during periods of prolonged, below normal precipitation provides additional opportunities for grassland nesting birds that use mid-to short-statured herbaceous vegetation found in a mesic (dry) vs. hydric habitats.
Mammals: A shift to mid- to short-grass species and drier soil conditions reduces habitat for large mammals, such as white-tailed deer, while still providing vegetative cover for small mammals. Thermal, escape, and winter cover becomes limited for larger ungulates.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.2; however, heavy grazing coupled with below normal precipitation will reduce habitat for amphibians.
Fish and Mussels: Provides similar life requisites as Community Phase 1.2.
2.3 Foxtail Barley/Mountain Rush-Spikerushes/Bare Ground: This plant community phase occurs with heavy season-long grazing, coupled with periods of below normal precipitation, lowering the water table and increasing salinity. Grazing tolerant foxtail barley begins to dominate the site. Grazing tolerant rush and spikerushes increase along with bare ground.
Invertebrates: Pollinator friendly forbs decrease as salinity and foxtail barley increase, limiting pollen and nectar availability. Bare ground increases but few ground nesting species, if any within MLRA 54, use saline soils for nesting sites. This shift to drier soil conditions reduces or eliminates aquatic invertebrates.
Birds: Provides similar life requisites as Community Phase 1.1. In addition, the drying of the soil during periods of prolonged, below normal precipitation provides additional opportunities for grassland nesting birds that use short-statured herbaceous vegetation found in a mesic (dry) vs. hydric habitats.
Mammals: A shift to short-grass species and drier soil conditions reduces habitat for large mammals, such as white-tailed deer, while still providing vegetative cover for small mammals. Thermal, escape, and winter cover is no longer provided for larger ungulates.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.2.
Fish and Mussels: Provides similar life requisites as Community Phase 1.2; however, increased salinity may increase salinity into waters receiving runoff from this site.
3.0 Wooded State
Community Phase 3.1 Willows: The elimination of fire or mechanical disturbance, via Transitional Pathway T2A, allow for sandbar and Bebb willow species to dominate this site. Shade tolerant sedges and rushes dominate the shrub understory. Trees, such as Plains cottonwood, may also occur on the site - particularly as a ring of trees at the margins of wetlands. Restoration to State 2.0 via Restoration Pathway R3A requires a combination of mechanical and herbicide application coupled with repeated prescribed burns.
Invertebrates: The invasion of woody vegetation reduces habitat for pollinator insects within MLRA 54. Season-long pollen and nectar availability is limited on this site due to an understory of sedges and rushes. However, willow species provide an early season pollen source for native and honeybees. Overall, pollinator plant diversity is low, limiting season-long nectar and pollen production.
Birds: Dependent upon degree of invasion by willows and trees, grassland nesting birds which are sensitive to woody vegetation encroachment will discontinue use of this community phase. Shrub tolerant grassland birds may continue to use this site. Willows provide thermal and escape cover for year-long residents. Willow thickets provide habitat for brown-headed cowbirds, increasing nest parasitism on adjacent grassland nesting bird communities.
Mammals: Shrubs/trees will provide increased year-round cover for white-tailed deer, moose, and elk. Mammals, such as porcupines, that prefer woody habitat will use this site.
Amphibians and Reptiles: Willows should not impact use of this ecological site by the Canadian Toad.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1.
4.0 Invaded Saline State
Community Phase 4.1 Foxtail Barley/Exotic Grasses/Exotic Forbs: This change in states and plant community phase occurs during periods of long term below normal precipitation lowering the water table and increasing salinity. Coupled with increased animal impact, disturbance-tolerant non-native species (such as foxtail barley, quackgrass, Canada thistle, and field sowthistle) dominate this plant community phase. Foxtail barley will dominate with increased salinity. Extended periods of above normal precipitation along Restoration Pathway R4A can move this plant community back to State 2.0.
Invertebrates: Canada thistle and field sowthistle provide mid- to late-season pollen. This plant community has a low diversity with limited early- to mid-season forbs. Bare ground increases but few ground nesting species, if any within MLRA 54, use this plant community for nesting sites. This shift to drier soil conditions reduces or eliminates aquatic invertebrates.
Birds: Heavy season-long grazing coupled with a dominance of cool-season exotic grasses and foxtail barley provides limited nesting habitat for grassland birds. Foraging by water birds is limited, except during periods of inundation. Lack of forbs limits invertebrate production for grassland birds.
Mammals: Dominated by foxtail barley thermal, escape, and winter cover is no longer provided for small or large mammals.
Amphibians and Reptiles: During period of inundation, amphibians tolerant to salinity may use this site.
Fish and Mussels: Increased salinity may increase salinity into waters receiving runoff from this site.
5.0 Invaded/Fresh Water State
Community Phase 5.1 Exotic Grasses/Exotic Forbs/Sedges/Rushes: This plant community phase occurs during periods of below normal precipitation lowering the water table with water chemistry remaining fresh. Coupled with increased animal impact, disturbance-tolerant non-native species (such as quackgrass, Canada thistle, and field sowthistle) dominate this plant community phase. Foxtail barley will not dominate the site unless water chemistry increases in salinity. Extended periods of above normal precipitation along Restoration Pathway R5A can move this plant community back to State 2.0.
Invertebrates: Canada thistle and field sowthistle provide mid- to late-season pollen. This plant community has a low diversity with limited early- to mid-season forbs. Bare ground increases for ground nesting species. This shift to drier soil conditions reduces or eliminates aquatic invertebrates.
Birds: Decreased surface water reduces invertebrate production and use by waterfowl and shorebirds. The drying of the soil during periods of prolonged, below normal precipitation provides additional opportunities for grassland nesting birds that use mid-to tall-statured herbaceous vegetation found in a mesic (dry) vs. hydric habitats.
Mammals: Exotic grasses (such as reed canarygrass, smooth brome, quackgrass, etc.) may provide thermal, escape, or winter cover for mammals.
Amphibians and Reptiles: Below normal precipitation limits production of invertebrates used by water birds.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1.
6.0 Invaded/Eutrophication State
Community Phase 6.1 Hybrid Cattail or Reed Canarygrass: Community Phase: Eutrophication and sedimentation of the site, often due to tillage on or adjacent to the site, transitions this plant community to one dominated by hybrid cattails or exotic strains/hybrids of reed canarygrass. Hybrid cattail or reed canary grass generally develop into monotypic stands (outcompeting other grasses, graminoids or forbs). Extended periods of above normal precipitation along with mechanical treatment, sediment removal, prescribed burning, and reseeding via Restoration Pathway R6A can move this plant community back to State 2.0.
Invertebrates: Saturated or ponded soils favor aquatic invertebrates. Monotypic stands of hybrid cattail or reed canarygrass limit forb species, providing a decrease in pollen and nectar sources for insects. Restoration efforts, including prescribed grazing, can reduce hybrid cattail and reed canarygrass while increasing forb diversity. The initial flush of forbs may be Canada thistle and field sowthistle resulting from restoration efforts, especially prescribed grazing.
Birds: Monotypic stands of hybrid cattail or reed canarygrass reduce water bird use. LeConte’s and Nelson’s sparrow and yellow rail favor this plant community. American bittern may use this site. Restoration efforts, including prescribed grazing, can reduce hybrid cattail and reed canary grass; this increases open water providing foraging and breeding habitat for dabbling ducks and shore birds including an excellent food source of aquatic invertebrates.
Mammals: Monotypic stands of hybrid cattail or reed canarygrass provide winter cover for large herbivores including white-tailed deer and moose. Depending on degree of ponding or saturation, this plant community may provide season-long escape cover for white-tailed deer. This plant community provides foraging opportunities for raccoon, skunks, coyotes and other mammals that use wetlands and wetland edges for food resources. Tall- to mid-statured vegetation provides suitable food, thermal, protective, and escape cover for small and large herbivores.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1.
7.0 Go-Back State
Community Phase 7.1 Annual/Pioneer Perennial/Exotics: Following cropland abandonment, these plant communities are dominated by early pioneer annual and perennial plant species. Plant species composition and production are highly variable, but will consist of Canada thistle, field sowthistle, other annual weeds (dock, smartweed, barnyard grass, etc.), quackgrass, foxtail barley, slough grass, and pioneering spikerush species. Weedy plants can provide pollinator habitat along with spring and summer cover for many mammals and birds, and their young. Dense weed cover can keep soils moist, increasing insect presence. Tall stature provided by some weeds offers thermal cover and seeds throughout winter. The response by wildlife species will be dependent upon plant community composition, vegetative stature, patch size, and management activities (such as wetland restoration, sediment removal, prescribed grazing, burning, inter-seeding, haying, or noxious weed control).
Successful wetland restoration and seeding of native species along Transition Pathway R7A can result in a native grass and forb community in State 2.0. Management activities within State 2.0 are needed to avoid a transition out of State 2.0. Unsuccessful wetland restoration or unsuccessful native forb and grass seeding may lead to States 4.0, 5.0 or 6.0 dependent upon site hydrological modifications and restoration, salinity, and other site-related issues.
Animal Community – Grazing Interpretations
This site is well adapted to managed grazing by domestic livestock. The predominance of herbaceous plants across all plant community phases best lends these sites to grazing by cattle, but other domestic grazers with differing diet preferences may also be a consideration depending upon management objectives. Often, the current plant community does not match any particular plant community (as described in the ecological site description). Because of this, a resource inventory is necessary to document plant composition and production. Proper interpretation of this inventory data will permit the establishment of a safe, initial stocking rate for the type and class of animals and level of grazing management. More accurate stocking rate estimates should eventually be calculated using actual stocking rate information and monitoring data.
NRCS defines prescribed grazing as “managing the harvest of vegetation with grazing and/or browsing animals with the intent to achieve specific ecological, economic, and management objectives”. As used in this site description, the term ‘prescribed grazing’ is intended to include multiple grazing management systems (e.g., rotational grazing, twice-over grazing, conservation grazing, targeted grazing, etc.) provided that, whatever management system is implemented, it meets the intent of prescribed grazing definition.
The basic grazing prescription addresses balancing forage demand (quality and quantity) with available forage, varying grazing and deferment periods from year-to-year, matching recovery/deferment periods to growing conditions when pastures are grazed more than once in a growing season, implementation of a contingency (e.g., drought) plan, and a monitoring plan. When the management goal is to facilitate change from one plant community phase or state to another, then the prescription needs to be designed to shift the competitive advantage to favor the native grass and forb species.
Grazing levels are noted within the plant community narratives and pathways in reference to grazing management. “Degree of utilization” is defined as the proportion of the current years forage production that is consumed and/or destroyed by grazing animals (may refer to a single plant species or a portion or all the vegetation). “Grazing utilization” is classified as slight, moderate, full, close, and severe (see the following table for description of each grazing use category). The following utilization levels are also described in the Ranchers Guide to Grassland Management IV. Utilization levels are determined by using the landscape appearance method as outlined in the Interagency Technical Reference “Utilization Studies and Residual Measurements” 1734-3.
Utilization Level % Use Description
Slight (Light) 0-20 Appears practically undisturbed when viewed obliquely. Only choice areas and forage utilized.
Moderate 20-40 Almost all of accessible range shows grazing. Little or no use of poor forage. Little evidence of trailing to grazing.
Full 40-60 All fully accessible areas are grazed. The major sites have key forage species properly utilized (about half taken, half left). Points of concentration with overuse limited to 5 to 10 percent of accessible area.
Close (Heavy) 60-80 All accessible range plainly shows use and major sections closely cropped. Livestock forced to use less desirable forage, considering seasonal preference.
Severe > 80 Key forage species completely used. Low-value forages are dominant.
Hydrological functions
Under unaltered hydrologic conditions, the site is dominated by soils in hydrologic group D; where significantly impacted by drainage practices, these soils are in hydrologic group A/D, B/D, or C/D depending upon soil texture. Infiltration varies from slow to rapid; runoff potential varies from negligible to medium for this site depending on surface and subsoil texture, slope shape, and ground cover. In many cases, areas with greater than 75% ground cover have the greatest potential for high infiltration and lower runoff. An exception would be where shortgrasses form a dense sod and dominate the site. Areas where ground cover is less than 50% have the greatest potential to have reduced infiltration and higher runoff (refer to Section 4, NRCS National Engineering Handbook for runoff quantities and hydrologic curves).
Hydrological manipulation (surface or tile drainage, pumping, surface water diversion, etc.) modifies this ecological site. Under natural conditions, this ecological site includes a wide range of soil textures; after hydrologic manipulation, soil texture often becomes a more significant factor in vegetative response. If the degree of manipulation allows soil texture to influence the plant community or if altered soil properties (i.e., salinization or the addition of sediment or fill material) results in vegetation change, a transition to a completely different ecological site may have occurred. The transition to an altogether different ecological site will depend upon severity of altered hydrology, soil properties, and corresponding vegetation. Due to the many variables (e.g., hydrology, success and type of drainage, etc.), impacts to the ecological site will be site-specific. As a result, each situation will require field investigation to determine what, if any, change in ecological site designation is necessary and proceed accordingly.
Without restoring hydrologic function (which may include range seeding), managers need to reference state and transition models within those sites. Hydrology will need to be fully restored in Wet Meadow and Shallow Marsh ecological sites for these sites to properly function. It is recommended that managers review the appropriate State and Transition Models prior to wetland restoration.
Recreational uses
The largest acreage of public land available for recreation in the MLRA is owned and managed by the United States Forest Service (USFS) within the Little Missouri, Grand River, and Cedar River National Grasslands in South Dakota and the Little Missouri National Grasslands in North Dakota (687,398 acres). These areas are available for hunting, fishing, hiking, camping, horse and bike riding, nature viewing, etc. In addition, the Bureau of Land Management (BLM) manages (40,264 acres) in North and South Dakota with the same recreational opportunities as the USFS lands.
The United States Army Corps of Engineers (USAE) owns 496,162 acres of land and water located on and adjacent to Lake Sakakawea and Lake Oahe. The North Dakota and South Dakota Game and Fish Departments manage the fisheries resources. These two Missouri River reservoirs provide excellent fishing and water recreation opportunities. In addition, the United States Fish and Wildlife Service (USFWS) manages a national fish hatchery below Garrison Dam.
The USFWS manages 36,858 acres in the National Wildlife Refuge system while the North Dakota and South Dakota wildlife management agencies manage 72,218 acres as wildlife or game management areas. The North Dakota, South Dakota, and Montana Department of Trust Lands manage 486,482 acres. These areas provide hunting, bird watching, hiking, and other outdoor recreation opportunities. North Dakota Wildlife Management Areas along the shoreline of Lake Sakakawea and the Missouri River account for 60,000 acres of the approximately 72,218 acres of land managed by the states for wildlife habitat in MLRA 54. Located in the northern portion of the MLRA, the Killdeer Mountain WMA is the largest tract of state-owned land managed for wildlife habitat at approximately 7,000 acres.
The largest refuge managed by the United States Fish and Wildlife service is Lake Ilo National Wildlife Refuge totaling approximately 4,000 acres. United States Bureau of Reclamation manages approximately 11,000 acres at Lake Tschida and 8,460 acres at Bowman-Haley Lake for fish and wildlife habitat. The National Park Service manages the Knife River Indian Village National Historic Site; the North Dakota Historical Society manages the Double Ditch Indian Village site.
Bird watching: Public and private grasslands within MLRA 54 provide essential habitat for prairie-dependent bird species such as Sprague's pipits, western meadowlark, and Baird's sparrow along with some of the larger, showy members of the upland prairie include marbled godwits, upland sandpipers, willets, and sharp-tailed grouse. Publicly owned lands provide excellent birding opportunities. MLRA 54 is in the Central Flyway.
Hunting/Fishing: MLRA 54 is a fall destination for thousands of pheasant and upland game bird hunters. This MLRA also provides excellent deer (white-tailed and mule), pronghorn, and coyote hunting opportunities. Lake Sakakawea, Lake Oahe, Lake Tschida, and the Missouri River provide excellent year-round fishing opportunities. The North Dakota Game and Fish Department and South Dakota Game, Fish and Parks manage approximately 40 fishing lakes within the MLRA. Available species include yellow perch, walleye, northern pike, muskellunge, crappie, bluegill, rainbow trout, and smallmouth bass. Chinook salmon are stocked in Lake Sakakawea.
Camping: Numerous state operated campgrounds are located along the shores of Lake Sakakawea, Lake Oahe, Missouri River, and Shadehill Reservoir. Primitive camping is allowed on Grand River and Cedar River National Grasslands in South Dakota and the Little Missouri National Grasslands in North Dakota. Other numerous camping (primitive and improved) sites are available in numerous city and county parks.
Hiking/Biking/Horseback Riding: Hiking is permitted on most state and federally owned lands. Developed hiking and biking trails can be found on Harmon Lake (13.1 miles), Roughrider Trail (Morton County, 16.5 miles), Missouri River State Natural Area (5 miles), Ft. Abraham Lincoln State Park (8 miles), Cross Ranch State Park (14 miles), Grand River National Grasslands (7 miles), Lake Sakakawea State Park (5 miles), and Lewis & Clark State Park (5 miles). In addition, extensive biking and walking trails are found in local county and city parks. Ft. Abraham Lincoln State Park has 6 miles of horseback trails.
Wood products
No appreciable wood products are present on the site.
Other products
Seed harvest of native plant species can provide additional income on this site.
Other information
Site Development and Testing Plan
• Further investigation is needed on the wide range of landforms and soil textures (and associated properties) and their relationship to hydrology/plant dynamics.
• Further documentation may be needed for plant communities in all states. Plant data has been collected in previous range-site investigations, including clipping data. Vegetative data for calcareous soils in Wet Meadow needs review and more data likely needs to be collected. If geo-referenced sites meeting Tier 3 standards for either vegetative or soil data are not available, representative sites will be selected for further investigation.
• Further evaluation and refinement of the State-and-Transition model may be needed to identify disturbance driven dynamics. Additional states and/or phases may be required to address grazing response.
• The long-term goal is to complete an approved, correlated Ecological Site Description as defined by the National Ecological Site Handbook.
• NASIS revisions needed:
o One channeled, frequently flooded, poorly drained phase of Trembles should be relinked from Wet Meadow to Riparian Complex.
o Consider relinking Aveson, channeled component from Wet Meadow to Riparian Complex.
o Minnewaukan and McKeen soils series need to be evaluated for inclusion into the Riparian Complex ESD.
This ESD is the best available knowledge. The site concept and species composition table have been used in the field and tested for more than five years. It is expected that as additional information becomes available revisions may be required.
Supporting information
Inventory data references
Information presented here has been derived from NRCS and other federal/state agency clipping and inventory data. Also, field knowledge of range-trained personnel was used. All descriptions were peer reviewed and/or field-tested by various private, state and federal agency specialists.
Other references
Bakker, K.K. 2003. The effect of woody vegetation on grassland nesting birds: an annotated bibliography. The Proceedings of the South Dakota Academy of Science 82:119-141.
Barker, W.T. and W. C. Whitman. 1988. Vegetation of the Northern Great Plains. Rangelands 10(6): 266-272.
Bjugstad, A.J. 1965. Vegetation measurements in relation to range condition classification on the principal range sites of southwestern North Dakota. PhD Thesis. N D State University.
Bluemle, J.P. 2017. North Dakota Notes No. 13, North Dakota’s mountainous areas: the Killdeer Mountains and the Turtle Mountains. Accessed on web, April 10, 2017, at https://www.dmr.nd.gov/ndgs/ndnotes/ndn15- h.htm.
Bluemle. J.P. 2016. North Dakota’s geologic legacy. North Dakota State University Press. 382 pages.
Brand, M. D. and H. Goetz. 1986. Vegetation of exclosures in southwestern North Dakota. Journal of Range Management 39: 434-437.
Briske, D.D. (editor). 2017. Rangeland systems – processes, management, and challenges. Springer Series on Environmental Management. 661 pages.
DeKeyser, E.S., G. Clambey, K. Krabbenhoft, and J. Ostendorf. 2009. Are changes in species composition on central North Dakota rangelands due to non-use management? Rangelands 31:16-19
Dodd, J.L. 1970. Distribution and community site relations of bluebunch wheatgrass in North Dakota. PhD Thesis. N D State University. Fargo, North Dakota.
Dornbusch, M.J., R.F. Limb, and C.K. Gasch. 2018. Facilitation of an exotic grass through nitrogen enrichment by an exotic legume. Rangeland Ecology & Management 71:691-694.
Dyke, S.R., S.K. Johnson, and P.T. Isakson. 2015. North Dakota state wildlife action plan. North Dakota Game and Fish Department, Bismarck, ND. 468 pages.
Ehrenfeld, Joan G. 2002. Effects of exotic plant invasions on soil nutrient cycling processes. Ecosystems 6:503-523.
Ereth, C., J. Hendrickson, D. Kirby, E. DeKeyser, K. Sedevic, and M. West. Controlling Kentucky bluegrass with herbicide and burning is influenced by invasion level. Invasive Plant Science and Management 10: 80-89.
Flesland, J.R. 1964. Composition and structure of the salt-desert shrub type in the badlands of western North Dakota. M.S. Thesis. ND State University.
Franzen, David. 2007. Managing saline soils in North Dakota. SF-1087. NDSU Extension Service. North Dakota State University.
Gilgert, W. and S. Zack. 2010. Integrating multiple ecosystem services into ecological site descriptions. Rangelands: 32:49-54.
Grant, T.A. and R.K. Murphy. 2005. Changes on woodland cover on prairie refuges in North Dakota, USA. Natural Areas Journal 25:359-368.
Hanson, H.C and W. Whitman. 1938. Characteristics of major grassland types in western North Dakota. Ecological Monographs. Vol. 8:57-114.
Heitschmidt, R. K., K. D. Klement, and M. R. Haferkamp. 2005. Interactive effects of drought and grazing on Northern Great Plains rangelands. Rangeland Ecology and Management 58:11-19.
Hendrickson, J.R., P. S. Johnson, M. A. Liebig, K. K. Sedivec, and G. A. Halvorson. 2016. Use of ecological sites in managing wildlife and livestock: an example with prairie dogs. Rangelands 38(1): 23-28.
Hendrickson, J.R., S.L. Kronberg, and E.J. Scholljegerdes. 2020. Can targeted grazing reduce abundance of invasive perennial grass (Kentucky bluegrass) on native mixed-grass prairie? Rangeland Ecology and Management, 73:547-551.
Higgins, K.F. 1984. Lightning fires in grasslands in North Dakota and in pine-savanna lands in nearby South Dakota and Montana. J. Range Manage. 37:100-103.
Higgins, K.F. 1986. Interpretation and compendium of historical fire accounts in the Northern Great Plains. United States Department of Interior, Fish and Wildlife Service. Resource Publication 161. 39 pages.
High Plains Regional Climate Center, University of Nebraska, 830728 Chase Hall, Lincoln, NE 68583-0728. (http://hprcc.unl.edu)
Hirch, K.L. 1985. Habitat type classification of grasslands and shrublands of southwestern North Dakota. Ph.D. Thesis. ND State University.
Hopkins, D.G., M.D Sweeny, D.R. Kirby, J. L. Richardson. 1991. Effects of revegetation of surficial soil salinity on panspot soils. Journal of Range Management 44(3): 215-219.
Hopkins, D.G., M.D Sweeny, J. L. Richardson. 1991. Dispersive erosion and entisol-panspot genesis in sodium-affected landscapes. Soil Science Society American Journal Volume. 55: 171-177.
Johnson, Sandra. 2015. Reptiles and amphibians of North Dakota. North Dakota Game and Fish Department. 64 pages.
Jordan, N. R., D.L. Larson, and S.C. Huerd. 2008. Soil modification by invasive plants: effects on native and invasive species of mixed-grass prairies. Biological Invasions 10:177-190.
Mader, E., M. Shepherd, M. Vaughan, and S.H. Black. 2011. Attracting native pollinators: protecting North America's bees and butterflies. Accessed at https://xerces.org, May 1, 2017.
Montana Fish, Wildlife and Parks. 2015. Montana state wildlife action plan. 2015. Viewed at https://xerces.org/ on May 1, 2017.
North Dakota Division of Tourism, Accessed on February 25, 2019. Available at https://www.ndtourism.com/sports-recreation
North Dakota Parks and Recreation Department, Accessed on February 25, 2019. Available at http://www.parkrec.nd.gov/recreationareas/recreationareas.html
Palit, R., G. and E.S. DeKeyser. 2022. Impacts and drivers of smooth brome (Bromus inermis Leyes.) invasion in native ecosystems. Plants: 10,3390. http://https://www.mdpi.com/2223-7747/11/10/1340
Palit, R., G. Gramig, and E.S. DeKeyser. 2021. Kentucky bluegrass invasion in the Northern Great Plains and prospective management approaches to mitigate its spread. Plants: 10,817. https://doi.org/10.3390/plants10040817
Printz, J.L. and J.R. Hendrickson. 2015. Impacts of Kentucky bluegrass invasion (Poa pratensis) on ecological processes in the Northern Great Plains. Rangelands 37(6):226-232.
Redmann, Robert E. 1975. Production ecology of grassland plant communities in western North Dakota. Ecological Monographs 45:83-106.
Reeves, J.L., J.D. Derner, M.A. Sanderson, J.R. Hendrickson, S.L. Kronberg, M.K. Petersen, and L.T. Vermeire. 2014. Seasonal weather influences on yearling beef steer production in C3-dominated Northern Great Plains rangeland. Agriculture, Ecosystems and Environment 183:110-117.
Royer, R. A., 2003. Butterflies of North Dakota: an atlas and guide. Minot State University, Minot, ND.
Sanford, R.C. 1970. Skunk bush in the North Dakota badlands: ecology, phytosociology, browse production, and utilization. Ph. D. Thesis. ND State University.
Seabloom, R. 2020. Mammals of North Dakota. North Dakota Institute for Regional Studies, Fargo, ND. 470 pages.
Sedivec, K.D., J.L. Printz. 2014. Ranchers guide to grassland management IV. NDSU Extension Service publication R1707.
South Dakota Dept. of Game, Fish and Parks. 2014. South Dakota wildlife action plan. Wildlife Division Report 2014-03.
Spaeth, K.E., Hayek, M.A., Toledo, D., and Hendrickson, J. 2019. Cool season grass impacts on native mixedgrass prairie species in the Northern Great Plains. America’s Grassland Conference: Working Across Boundaries. The Fifth Biennial Conference on the Conservation of America’s Grasslands. Bismarck, ND. 20-22 August.
Tidwell, D., D.T. Fogarty, and J.R. Weir. 2021. Woody encroachment in grasslands, a guide for understanding risk and vulnerability. Oklahoma State University, Oklahoma Cooperative Extension Service publication E- 1054. 32 pages.
Toledo, D., M. Sanderson, K. Spaeth, J. Hendrickson, and J. Printz. 2014. Extent of Kentucky bluegrass and its effect on native plant species diversity and ecosystem services in the Northern Great Plains of the United State. Invasive Plant Science and Management 7(4): 543-552.
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USDA, NRCS. 2006. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.
USDA, NRCS. National Soil Information System, 100 Centennial Mall North, Room 152, Lincoln, NE 68508- 3866. (https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/survey/tools/?cid=nrcs142p2_053552)
USDA, NRCS. National Water & Climate Center, 1201 NE Lloyd Blvd, Suite 802, Portland, OR 97232-1274. (https://www.wcc.nrcs.usda.gov/)
USDA, NRCS. 2001. The PLANTS database, Version 3.1 (http://plants.usda.gov). National Plant Data Center, Baton Rouge, LA 70874-4490 USA.
USDA, NRCS, Various published soil surveys.
USDI BLM.1999. Utilization studies and residual measurements. Interagency Technical Reference 1734-3.
U.S. Fish and Wildlife Service. 2015. Endangered and threatened wildlife and plants; designation of critical habitat for the Dakota skipper and Poweshiek skipperling; Vol. 79 No. Final Rule October 1, 2015, 50 CFR Part 17.
Vinton, M.A. and E.M. Goergen. 2006. Plant-soil feedbacks contribute to the persistence of Bromus inermis in tallgrass prairie. Ecosystems 9: 967-976.
Whitman, W.H., H. Hanson, and R. Peterson. 1943. Relation of drought and grazing to North Dakota range lands. North Dakota Agricultural Experimentation Bulletin 340.
Zaczkowski, N. K. 1972. Vascular flora of Billings, Bowman, Golden Valley, and Slope counties, North Dakota. Dissertation, ND State University.
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Contributors
ND NRCS: David Dewald, Jonathan Fettig, Jody Forman, Mike Gerbig, Alan Gulsvig, Mark Hayek, Jeanne Heilig, John Kempenich, Chuck Lura, Jeff Printz, Steve Sieler, and Hal Weiser.
Approval
Suzanne Mayne-Kinney, 3/31/2025
Acknowledgments
NRCS would like to acknowledge the United State Forest Service (USFS) and National Park Service (NPS) for access to USFS properties and technical assistance in ESD development. USFS: Jack Dahl, Nickole Dahl, and Chad Prosser.
Rangeland health reference sheet
Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.
Author(s)/participant(s) | M. Hayek, J. Printz, S. Boltz, R. Kilian, D. Froemke, M. Rasmusson |
---|---|
Contact for lead author | NRCS State Rangeland Management Specialist |
Date | 03/31/2025 |
Approved by | |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
Rills are not expected on this site. -
Presence of water flow patterns:
Water flow patterns are not visible. -
Number and height of erosional pedestals or terracettes:
Neither pedestals nor terracettes are expected. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground is less than 2%. If present, bare ground patches are very small (less than 2 inches in diameter) and disconnected. -
Number of gullies and erosion associated with gullies:
Active gullies are not expected on this site. -
Extent of wind scoured, blowouts and/or depositional areas:
No wind-scoured or depositional areas are expected on this site. -
Amount of litter movement (describe size and distance expected to travel):
Plant litter movement not expected on this site. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Soil surface resistance to erosion: Stability class averages 5 or greater. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Structure is granular within the upper A-horizon. A-horizons for this ecological site range from 4 to 14 inches thick. Hue 10YR with value of 3 or less moist or 3 to 5 dry, and chroma 2 or less moist. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Grass-likes and tall-statured rhizomatous grasses are dominant and well distributed across the site. Mid- and short-statured rhizomatous grasses, and mid- and short bunchgrasses are subdominant. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
No compaction layers occur naturally on this site. -
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):
Dominant:
Phase 1.1:
Grass-likes (7); Tall C4 rhizomatous grasses (2)Sub-dominant:
Phase 1.1:
Mid & short C3 rhizomatous grasses (2); Mid & short C3 bunch grasses (4); Tall C3 rhizomatous grasses (1)Other:
Minor - Phase 1.1:
Forbs; Mid & short C4 rhizomatous grassesAdditional:
Due to differences in phenology, root morphology, soil biology relationships, and nutrient cycling Kentucky bluegrass, smooth brome, and crested wheatgrass are included in a new Functional/structural group, mid- and short-statured early cool-season grasses (MSeC3), not expected for this site.
To see a full version 5 rangeland health worksheet with functional/structural group tables. Please use the following hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/54_Wet_Meadow_Narrative_FINAL_Ref_FSG.pdf -
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Rare to not occurring on this site. -
Average percent litter cover (%) and depth ( in):
Plant litter cover is 40 to 60% with a depth of 0.75 to 1.5 inches. Litter is in contact with the soil surface. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Annual production: Annual air-dry production is 4500 lbs./ac (reference value) with normal precipitation and temperatures. Low and high production years should yield 4000 lbs./ac to 5000 lbs./ac, respectively. -
Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
State and local noxious species, quackgrass, creeping foxtail, reed canarygrass, smooth bromegrass, and Kentucky bluegrass -
Perennial plant reproductive capability:
Noninvasive species in all functional/structural groups are vigorous and capable of reproducing annually under normal weather conditions.
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The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.
Click on box and path labels to scroll to the respective text.
Ecosystem states
States 2, 5, 6 and 7 (additional transitions)
States 4 and 7 (additional transitions)
T1A | - | Invasion by exotic grasses and forbs, no-use no fire, or heavy season-long grazing |
---|---|---|
T2A | - | Extended periods of no fire or infrequent fire |
T2B | - | Heavy season-long grazing, below average precipitation, salinity (discharge site) |
T2C | - | Heavy season-long grazing, below average precipitation, no salinity (recharge site) |
T2D | - | Eutrophication, sedimentation |
R3A | - | Mechanical treatment and long-term prescribed burning |
R4A | - | Extended periods above average precipitation |
R5A | - | Extended periods above average precipitation |
R6A | - | Extended periods above average precipitation |
R7A | - | Successful hydrological restoration and seeding |
R7B | - | No use, no fire, no range planting, salinity, successful hydrological restoration |
R7C | - | No use, no fire, no range planting, fresh water, successful hydrological restoration |
R7D | - | No use, eutrophication, sedimentation, successful hydrological restoration |
T8A | - | Cessation of annual cropping |
State 1 submodel, plant communities
1.1A | - | Below average precipitation, heavy season-long grazing |
---|---|---|
1.2A | - | Return to average precipitation and long-term prescribed grazing and prescribed burning |
State 2 submodel, plant communities
2.1A | - | Heavy season-long grazing, below average precipitation |
---|---|---|
2.2A | - | Heavy season-long grazing, above or below average precipitation (discharge site) |
2.3A | - | Return to average precipitation and long-term prescribed grazing and prescribed burning |