Natural Resources
Conservation Service
Ecological site R150BY550TX
Northern Salt Marsh
Last updated: 9/22/2023
Accessed: 11/21/2024
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): 150B–Gulf Coast Saline Prairies
MLRA 150B is in the West Gulf Coastal Plain Section of the Coastal Plain Province of the Atlantic Plain and entirely in Texas. It makes up about 3,420 square miles. It is characterized by nearly level to gently sloping coastal lowland plains dissected by rivers and streams that flow toward the Gulf of Mexico. Barrier islands and coastal beaches are included. The lowest parts of the area are covered by high tides, and the rest are periodically covered by storm tides. Parts of the area have been worked by wind, and the sandy areas have gently undulating to irregular topography because of low mounds or dunes. Broad, shallow flood plains are along streams flowing into the bays. Elevation generally ranges from sea level to about 10 feet, but it is as much as 25 feet on some of the dunes. Local relief is mainly less than 3 feet. The towns of Groves, Texas City, Galveston, Lake Jackson, and Freeport are in the northern half of this area. The towns of South Padre Island, Loyola Beach, Corpus Christi, and Port Lavaca are in the southern half. Interstate 37 terminates in Corpus Christi, and Interstate 45 terminates in Galveston.
Classification relationships
USDA-Natural Resources Conservation Service, 2006.
-Major Land Resource Area (MLRA) 150B
Ecological site concept
Salt Marshes are closed depressions of the inland Coastal Plains exhibiting salt-tolerant vegetation.
Associated sites
| R150BY551TX |
Salty Prairie This site is on a higher landform and not as wet. |
|---|---|
| R150BY552TX |
Tidal Flat This site is on a lower landform and is subject to daily tides. |
| R150BY530TX |
Northern Coastal Sand This site is in a higher site and are sandy throughout. |
Similar sites
| R150BY652TX |
Southern Salt Marsh This site is in a drier precipitation regime. |
|---|
Table 1. Dominant plant species
| Tree |
Not specified |
|---|---|
| Shrub |
Not specified |
| Herbaceous |
(1) Spartina patens |
Physiographic features
The Salt Marsh formed in flood plains and flats on the barrier islands and coastal plains adjacent to the Gulf of Mexico. They are on broad tidal areas in coastal marshes. The landscape is typically very flat and interspersed with small drainages, small depressional areas, and variable sized open water bays. Streams or rivers that flow may cross towards the ocean. The marshlands may extend a few hundred yards or up to several miles from the coast depending on the slope gradient. Due to their location between the ocean and inland, the marshes are influenced by tides, saline substrates, and freshwater inflows. This site was formed in saline clayey coastal sediments. The slope is nearly level with elevation ranging from 0 to 10 feet.
Table 2. Representative physiographic features
| Landforms |
(1)
Delta plain
> Flood plain
(2) Coastal plain > Marsh |
|---|---|
| Runoff class | Negligible to high |
| Flooding duration | Long (7 to 30 days) |
| Flooding frequency | Occasional to frequent |
| Ponding duration | Very brief (4 to 48 hours) to very long (more than 30 days) |
| Ponding frequency | None to occasional |
| Elevation | 0 – 3 m |
| Slope | 0 – 1% |
| Water table depth | 0 – 76 cm |
| Aspect | Aspect is not a significant factor |
Climatic features
The climate is predominately maritime, controlled by the warm and very moist air masses from the Gulf of Mexico. The climate along the upper coast of the barrier islands is subtropical subhumid and the climate on the lower coast of Padre Island is subtropical semiarid (due to high evaporation rates that exceed precipitation). Almost constant sea breezes moderate the summer heat along the coast. Winters are generally warm and are occasionally interrupted by incursions of cool air from the north. Spring is mild and damaging wind and rain may occur during spring and summer months. Tropical cyclones or hurricanes can occur with wind speeds of greater than 74 mph and have the potential to cause flooding from torrential rainstorms. Despite the threat of tropical storms, the storms are rare. Throughout the year, the prevailing winds are from the southeast to south-southeast.
The average annual precipitation is 45 to 57 inches in the northeastern half of this area, 26 inches at the extreme southern tip of the area, and 30 to 45 inches in the rest of the area. Precipitation is abundant in spring and fall in the southwestern part of the area and is evenly distributed throughout the year in the northeastern part. Rainfall typically occurs as moderate-intensity, tropical storms that produce large amounts of rain during the winter. The average annual temperature is 68 to 74 degrees F. The freeze-free period averages 340 days and ranges from 315 to 365 days.
Table 3. Representative climatic features
| Frost-free period (characteristic range) | 261-365 days |
|---|---|
| Freeze-free period (characteristic range) | 365 days |
| Precipitation total (characteristic range) | 1,041-1,245 mm |
| Frost-free period (actual range) | 247-365 days |
| Freeze-free period (actual range) | 365 days |
| Precipitation total (actual range) | 940-1,270 mm |
| Frost-free period (average) | 318 days |
| Freeze-free period (average) | 365 days |
| Precipitation total (average) | 1,118 mm |
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
-
(1) ARANSAS WR [USC00410305], Tivoli, TX
-
(2) PORT O'CONNOR [USC00417186], Port O Connor, TX
-
(3) PALACIOS MUNI AP [USW00012935], Palacios, TX
-
(4) MATAGORDA NO 2 [USC00415659], Matagorda, TX
-
(5) FREEPORT 2 NW [USC00413340], Freeport, TX
-
(6) GALVESTON SCHOLES FLD [USW00012923], Galveston, TX
-
(7) GALVESTON [USW00012944], Galveston, TX
Influencing water features
This site has an Aquic soil moisture regime. Gulf storms and high tides flood most areas occasionally or frequently for long periods. Ponding occurs on some areas for very long periods. A permanent water table can be found within 30 inches of the surface during most of the year. Runoff is negligible on depressed sites and high on others due to the high water table. These are hydric soils.
Wetland description
These areas have hydric soils. Onsite investigation needed to determine local conditions.
Soil features
The site consists of very deep, saline, very poorly drained, very slowly permeable soils. Tidal influence and salty substrates produce saline to brackish conditions. However, at any given location, the degree of salinity is a result of the local interaction of tidal influence, freshwater inflows, and substrate salt content. This site has an Aquic soil moisture regime with gleyed colors throughout the profile. Other features include moderate to strong sodicity and neutral to strong alkalinity. Soil correlated to this site include: Placedo, Swan, Velasco, and Veston.
Table 4. Representative soil features
| Parent material |
(1)
Alluvium
–
igneous, metamorphic and sedimentary rock
|
|---|---|
| Surface texture |
(1) Clay (2) Silty clay |
| Family particle size |
(1) Clayey (2) Fine-silty |
| Drainage class | Poorly drained to very poorly drained |
| Permeability class | Very slow |
| Soil depth | 203 cm |
| Surface fragment cover <=3" | 0% |
| Surface fragment cover >3" | 0% |
| Available water capacity (0-152.4cm) |
7.62 – 17.78 cm |
| Calcium carbonate equivalent (0-152.4cm) |
0 – 8% |
| Electrical conductivity (0-152.4cm) |
8 – 24 mmhos/cm |
| Sodium adsorption ratio (0-152.4cm) |
13 – 65 |
| Soil reaction (1:1 water) (0-152.4cm) |
7.9 – 9 |
| Subsurface fragment volume <=3" (63.5-152.4cm) |
0 – 1% |
Ecological dynamics
The environment is largely controlled by the Salt Marshes position between the ocean and inland upland sites. The generally flat, featureless plain is influenced by flooding of ocean tides, which vary seasonally and from year-to-year in their extent, duration, depth, and degree of salinity. In opposition to these ocean influences are freshwater inflows which move into the marsh as sheet flow from adjacent areas following precipitation events or result from flood overflow of streams that cross through the marsh from inland areas. Throughout the marsh, slight variations of a few inches in relief can produce noticeable changes in the plant community since minor variations in elevation can locally alter the salinity and water regime.
Within the marsh, many features add heterogeneity to the landscape and increase vegetation variability. Included are many small streams to large rivers that cross the marsh with their associated levees, oxbows, tidal guts, or drains that carry tidal waters inland. Depressional wetlands and small-to-large ridges that resulted from historic differential deposition and erosion within this geomorphologically recent and active surface are present. Interspersed within the vegetated marsh may be open water bays and mudflats that vary in size, depth, and duration of standing water. The interaction of the tidal influence and the freshwater inflows are temporally and spatially variable which contribute to vegetative variation. This results from the local internal variation in elevation, as well as the rise in elevation from the coast inland, which may be subtle and gradual over long distances or can be abrupt and rapid over short distances.
All the variables contribute influences on the degree and rate of change of water and salinity regime moving inland. This correspondingly controls change in plant composition, which may be gradual and continuous when there is a minor elevation gradient or more zonal where it is more abrupt. The variation in salinity fluctuates as the site is further away from the ocean. Typically, saline water (greater than 10 parts per thousand of salt) is found closest to the ocean. Located further inland, they become brackish (3.5 to 10 parts per thousand), then intermediate (0.5 to 3.5 parts per thousand). Eventually, they arrive on the inland border as fresh marsh with less than 0.5 parts per thousand of salt.
State and transition model
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View Interactive Models
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Ecosystem states
| T1A | - | Extreme disturbance event coupled with excessive grazing pressure |
|---|---|---|
| R2A | - | Absence of disturbance, reintroduction of native species and natural regeneration over time |
State 1 submodel, plant communities
State 2 submodel, plant communities
State 1
Reference
The Reference state is considered to be representative of pre-Euro settlement conditions. Historically the marsh was highly variable in both microtopography and vegetation. Community phase changes are primarily driven by flooding of ocean tides, which vary seasonally and from year-to-year in their extent, duration, depth, and degree of salinity. As well as freshwater inflows which move into the marsh as sheet flow from adjacent areas following precipitation events or result from flood overflow of streams that cross through the marsh from inland areas.
Dominant plant species
-
saltmeadow cordgrass (Spartina patens), grass
-
common reed (Phragmites australis), grass
Community 1.1
Salt Marsh Prairie
The reference community is a mixture of mid and tallgrasses making up greater than 80 percent of the biomass. Dominant grasses include marshhay cordgrass (Spartina patens), common reed (Phragmites australis), and seashore dropseed (Sporobolus virginicus). Interstitial graminoids include shoregrass (Monanthochloe littoralis), seashore paspalum (Paspalum vaginatum), and bulrushes (Scirpus spp.). Forbs include dwarf glasswort (Salicornia virginica), sea lavender (Limonium carolinianum), and seacoast sumpweed (Iva annua). Shrubs and half-shrubs are generally sparse in this community, but if present may include sea oxeye (Borrichia frutescens) and wolfberry (Lycium carolinianum). Smooth cordgrass (Spartina alterniflora), seashore saltgrass (Distichlis spicata), and saltmarsh bulrush (Bolboschoenus robustus) occur on the more saline areas. Fresher parts of the site are indicated by the presence of Common reed, big cordgrass (Spartina cynosuroides), and seashore paspalum. Shifts in composition may occur due to changes in the water and/or salinity regimes or in response to grazing impacts. Any of these sets of factors may produce similar vegetation responses and thus careful assessment must be made to determine the cause of observed changes. Many of the graminoids become coarse and unpalatable at maturity and fire can be used to stimulate new, more palatable growth and increase production. Improper grazing can cause a decrease in cordgrass, seashore dropseed, and common reed. When they are grazed frequently, they will be eliminated from the site because their root system is unable to recover. When the desirable plants have decreased, less desirable plants such as inland saltgrass and smooth cordgrass start to increase. Cordgrasses and other plants within this community primary reproduce vegetatively by rhizomes, which makes this site very resilient to disturbance. However, once they are eliminated they are hard to reestablish. Reseeding is not an option for this site because most of the seeds from these species are sterile. To reestablish these species transplanting or bringing in rhizomes are possible options for reestablishment. Unwanted species are limited due to the high salinity in the soil. Plants that are intolerant of salt are controlled with a tidal surge or hurricanes.
Figure 8. Annual production by plant type (representative values) or group (midpoint values)
Table 5. Annual production by plant type
| Plant type | Low (kg/hectare) |
Representative value (kg/hectare) |
High (kg/hectare) |
|---|---|---|---|
| Grass/Grasslike | 7061 | 10088 | 13114 |
| Shrub/Vine | 392 | 560 | 729 |
| Forb | 392 | 560 | 729 |
| Tree | – | – | – |
| Total | 7845 | 11208 | 14572 |
Figure 9. Plant community growth curve (percent production by month). TX7751, Midgrass Prairie Community. Open grassland plain composed of mid-grasses with seacoast bluestem and gulfdune paspalum dominate the site..
| 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 | 5 | 15 | 20 | 15 | 10 | 10 | 15 | 6 | 4 | 0 |
Community 1.2
Degraded Salt Marsh Prairie
Changes in the plant community are characterized by a decrease in common reed, seashore dropseed, and marshhay cordgrass. Other plants such as inland saltgrass, smooth cordgrass, gulf cordgrass, sea ox-eye, devil weed (Leucosyris spinosa), and sesbania increase. Plants within this community have high salt tolerance. Plants found in this community can tolerate grazing because of their growth forms. Rhizomes are present on most of the species, which allow this community to withstand extended intense grazing because they are not dependent on producing seeds. Gulf cordgrass has leaves with a sharp point and high lignin content, both of which reduce desirability to cattle. Inland saltgrass is a course-growing plant, which makes it unpalatable to cattle. Ground surface changes occur within this community. Bare ground is increased because of improper grazing. Litter on this site is reduced because the plants are heavily grazed and above ground biomass is removed. Fire is used to maintain this community to make the gulf cordgrass more palatable. With proper grazing management and fire, restoring this community back to the Salt Marsh Prairie Community is possible. However, restoring this community will require time. If too much vegetation is lost, reseeding is not an option for this site because most of the native species found on this site produce sterile seeds. To reestablish these species transplanting or sprigging are options. If grazing pressure is not reduced or a hurricane occurs, this community will transition to a Mudflat Community (2.1).
Community 1.3
Hurricane Impacted
The Hurricane Impacted Community (1.3) is characterized by vegetation that has been burned due to high salinity content carried by storm-driven flooding and by high winds laden with coastal water. Vegetation may be buried under thick sediment deposits left by storm surges. Some areas are scoured and devoid of vegetation and may temporarily suffer complete vegetative loss. Vegetation production will vary greatly in this community depending on the amount of plant survival and depth of sediment burial. Bare ground is abundant within this community because of the sediment deposit caused by a hurricane. The amount of sediment deposited on this site will determine how long it takes the site to return to the reference community. However, it is estimated that it will take 1 to 5 years to recover, depending on which community was impacted. More than likely, the reference community will recover naturally, whereas the Degraded Salt Marsh (1.2) will more easily transition to the Mudflat State (2). Areas that have a higher number of plant species that can tolerate salinity will recover quicker than areas that have plants with a lower tolerance to salinity. Salt-tolerant species may have a noticeable die-off following a hurricane depending on the amount of soil removed from around the roots. If the roots are exposed to sunlight and air, it causes mortality in the plants. This delays the recovery rate back to the reference community. Hurricanes are a natural deterrent to invasive plants because they are not adapted to high levels of salinity that is often associated with a hurricane. Invasive plants are usually eliminated from the community after the passing of a hurricane and its associated storm surges. Grazing pressure should be reduced post-hurricane. Without rest, this community will take longer to reach the reference community. Plant revegetation can be slow, but to hasten restoration revegetating is an option to assist in recovery.
Pathway 1.1A
Community 1.1 to 1.2
Heavy grazing will impact the site negatively and cause a transition to Community 1.2.
Pathway 1.1B
Community 1.1 to 1.3
Hurricanes and storm surges denude vegetation and cause the transition to Community 1.3.
Pathway 1.2A
Community 1.2 to 1.1
Prescribed grazing, specifically deferment, will allow the vegetation to transition back to reference conditions.
Pathway 1.3A
Community 1.3 to 1.1
Natural or land manager-induced revegetation will restore the reference community.
State 2
Mudflat
This state is the result of severe disturbance and is characterized by sparse vegetation and extensive bare ground.
Community 2.1
Mudflat
The Mudflat Community (2.1) represents extreme disturbance for this site. This community is typified by sparse vegetation. The site may have large areas devoid of plants. However, some remnants of plants may exist depending on the extent of the damage from grazing or a hurricane. A hurricane or destructive grazing by snow geese and/or livestock are drivers for this community transition. Returning to the Salt Marsh Prairie (1) requires extensive restoration. Plants such as marshhay cordgrass, common reed, and seashore dropseed reproduce primarily vegetatively, which makes it hard for them to reestablish. If plants remain on site, it will take to self-propagate because the seeds they produce are not viable. However, to reestablish them on a site, vegetative stem propagation or transplanting are options. Grazing should not be allowed on this site due to the limited amount of forage.
Transition T1A
State 1 to 2
Heavy overgrazing or a hurricane can cause the transition to State 2. The Degraded Salt Marsh Community (1.2) is at risk to transition, as is the Hurricane Impacted Community (1.3) if the site is not allowed to revegetate.
Restoration pathway R2A
State 2 to 1
Revegetation of the natural plant system is necessary to restore the Salt Marsh Prairie State (1). Revegetating can be difficult because it requires sprigging as seed sources are usually not viable.
Additional community tables
Table 6. Community 1.1 plant community composition
| Group | Common name | Symbol | Scientific name | Annual production (kg/hectare) | Foliar cover (%) | |
|---|---|---|---|---|---|---|
|
Grass/Grasslike
|
||||||
| 1 | Tall/midgrasses | 6277–11657 | ||||
| common reed | PHAU7 | Phragmites australis | 6277–11208 | – | ||
| saltmeadow cordgrass | SPPA | Spartina patens | 6277–11208 | – | ||
| seashore dropseed | SPVI3 | Sporobolus virginicus | 6277–11208 | – | ||
| 2 | Tall/midgrasses | 392–729 | ||||
| smooth cordgrass | SPAL | Spartina alterniflora | 392–673 | – | ||
| saltgrass | DISP | Distichlis spicata | 224–448 | – | ||
| longtom | PADE24 | Paspalum denticulatum | 224–448 | – | ||
| seashore paspalum | PAVA | Paspalum vaginatum | 224–448 | – | ||
| switchgrass | PAVI2 | Panicum virgatum | 224–448 | – | ||
| marsh bristlegrass | SEPA10 | Setaria parviflora | 224–448 | – | ||
| gulf cordgrass | SPSP | Spartina spartinae | 0–224 | – | ||
| 3 | Rushes | 392–729 | ||||
| chairmaker's bulrush | SCAM6 | Schoenoplectus americanus | 392–729 | – | ||
|
Forb
|
||||||
| 4 | Forbs | 392–729 | ||||
| annual marsh elder | IVAN2 | Iva annua | 336–673 | – | ||
| bushy seaside tansy | BOFR | Borrichia frutescens | 336–673 | – | ||
| eastern annual saltmarsh aster | SYSU5 | Symphyotrichum subulatum | 336–673 | – | ||
| hairypod cowpea | VILU3 | Vigna luteola | 336–673 | – | ||
| salt heliotrope | HECU3 | Heliotropium curassavicum | 112–336 | – | ||
| sea lavender | LIMON | Limonium | 112–336 | – | ||
| dwarf saltwort | SABI | Salicornia bigelovii | 112–336 | – | ||
| Virginia glasswort | SADE10 | Salicornia depressa | 112–336 | – | ||
| turtleweed | BATIS | Batis | 112–336 | – | ||
|
Shrub/Vine
|
||||||
| 5 | Shrubs/Vines | 392–729 | ||||
| eastern baccharis | BAHA | Baccharis halimifolia | 112–673 | – | ||
| Carolina desert-thorn | LYCA2 | Lycium carolinianum | 112–673 | – | ||
| bigpod sesbania | SEHE8 | Sesbania herbacea | 112–673 | – | ||
Interpretations
Animal community
The animal communities of the Coastal Prairie communities are influenced by fresh and salt water inundations. Cattle and many species of wildlife make extensive use of the site. White-tailed deer may be found scattered across the prairie and are found in heavier concentrations where woody cover exists. Feral hogs are present and at times become abundant. Coyotes are abundant and fill the mammalian predator niche. Rodent populations rise during drier periods and fall during periods of inundation. Alligators are locally abundant and make frequent use of the marshes depending on salt concentrations in the marshes.
The region is a major flyway for waterfowl and migrating birds. Hundreds of thousands of ducks, geese, and sandhill cranes abound during winter. Whooping cranes are an important endangered species that occur in the area, especially near Aransas National Wildlife Refuge. Northern harriers are common predatory birds seen patrolling marshes. Curlews, plovers, sandpipers, and willets are shorebirds that make use of the tidal areas. Seagulls and terns are plentiful throughout the year trolling the shores as well. Further inland, rails, gallinules, and moorhens make use of the brackish marshes.
Hydrological functions
In the Salt Marsh Prairie State (1) infiltration into marshy sandy soils is low because the water table is high. This site is a wetland and as such serves as a part of the wetland filtering system that is essential to the Gulf Coast. Because of landscape position, this site receives seepage water from adjacent sites and may be inundated following extensive rains from rainfall and seepage. Runoff and erosion from water are seldom a problem in the Cordgrass Plant State except for ship wake.
The hydrology of the Mudflat State (2) functions differently depending on the soil deposited following a hurricane. If it was a sandy textured soil infiltration will be high, however, if the soil had a clay type texture it is expected to have slower infiltration. As vegetation increases, infiltration will increase. The more slope on the site the high the runoff will be and the higher chance of erosion that is likely to occur because of the sand found in the soil.
Recreational uses
The beach area is a popular tourist designation throughout the year. Bird watching and saltwater fishing are other recreational uses.
Supporting information
Inventory data references
Information presented was derived from the Salty Marsh Range Site Description, NRCS clipping data, literature, field observations, and personal contacts with range-trained personnel.
Other references
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Contributors
Jack Alexander, Synergy Resource Solutions, Inc., Belgrade, MT
Dr. Fred Smeins, Professor, Texas A&M University, College Station, TX
Approval
Bryan Christensen, 9/22/2023
Acknowledgments
Reviewers and Technical Contributors:
Justin Clary, RMS, NRCS, Temple, TX
Shanna Dunn, RSS, NRCS, Corpus Christi, TX
Mark Moseley, RMS, NRCS, Boerne, TX
Tim Reinke, RMS, NRCS, Victoria, TX
Mike Stellbauer, RMS, NRCS, Bryan, TX
Site Development and Testing Plan:
Future work, as described in a Project Plan, to validate the information in this Provisional Ecological Site Description is needed. This will include field activities to collect low, medium and high-intensity sampling, soil correlations, and analysis of that data. Annual field reviews should be done by soil scientists and vegetation specialists. A final field review, peer review, quality control, and quality assurance reviews of the ESD will be needed to produce the final document. Annual reviews of the Project Plan are to be conducted by the Ecological Site Technical Team.
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) | Mike Stellbauer, Zone RMS, NRCS, Bryan, TX |
|---|---|
| Contact for lead author | |
| Date | 06/08/2004 |
| Approved by | Bryan Christensen |
| Approval date | |
| Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
None. -
Presence of water flow patterns:
At large scales, some drainage do occur. -
Number and height of erosional pedestals or terracettes:
None. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Less than 5 percent bare ground randomly distributed throughout. -
Number of gullies and erosion associated with gullies:
None. -
Extent of wind scoured, blowouts and/or depositional areas:
None. -
Amount of litter movement (describe size and distance expected to travel):
Small to medium-sized litter can be expected to move short to long distances depending on the degree and extent of flooding. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Soil surface is resistant to erosion. Stability class ranges from 4 to 5 on the surface. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Soil surface structure is 60 inches thick of dark gray to very dark gray clay or silty clay of moderate fine subangular blocky structure. SOM is 1 to 2 percent. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
This tallgrass marsh site along with adequate litter and little bare ground provides for maximum infiltration and little runoff under normal rainfall events. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
None. -
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:
Warm-season tallgrasses/grass-likesSub-dominant:
ForbsOther:
Warm-season midgrasses Shrubs Warm-season annual grasses Warm-season annual forbsAdditional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Grasses due to their growth habit will exhibit some mortality and decadence, though very slight. -
Average percent litter cover (%) and depth ( in):
Litter is primarily herbaceous. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
7,000 pounds per acre for below average moisture years to 13,000 pounds per acre for above average moisture years. -
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:
Chinese tallow and salt cedar. -
Perennial plant reproductive capability:
Perennial plants should be capable of reproduction, except for periods of prolonged drought conditions, heavy natural herbivory, hurricanes, and intense wildfires.
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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
| T1A | - | Extreme disturbance event coupled with excessive grazing pressure |
|---|---|---|
| R2A | - | Absence of disturbance, reintroduction of native species and natural regeneration over time |