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Ecological site PX138X00Y110
Sandy Over Loamy Lowland Flats
Last updated: 6/09/2025
Accessed: 09/15/2026
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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.
MLRA notes
Major Land Resource Area (MLRA): 138X–North-Central Florida Ridge
The MLRA notes section provides a brief description of the entire MLRA. This description is intended to provide some context about the MLRA within which this ecological site is associated. A more complete description of the MLRA can be found in Ag Handbook 296 (USDA-NRCS, 2022).
This MLRA is on a limestone upland that is mantled with sandy marine deposits and has an irregular, gently rolling topography. Because of the underlying karst topography, there are a moderate number of limestone sinkholes, some filled with water. Production of cash crops, hay, and pasture is the primary land use. This area comprises about 2,196 square miles (5,688 square kilometers) and is entirely within Florida.
This area is underlain by sediments of the Quaternary Period (present to 2.58 million years ago) that overlie the Neogene (2.53 to 23.03 million years ago) and Paleogene (23.03 to 66 million years ago) formations of the Hawthorn Group (Green et al., 2006). The rocks are progressively older to the south. The Quaternary sediments are largely undifferentiated marine deposits consisting of fine to coarse sands that are poorly to moderately sorted with variable mixtures of clay and organic material. The formations of the Hawthorn Group are, from youngest to oldest, the Statesville Formation, Coosawhatchie Formation, Suwannee Limestone, and Ocala Limestone. The Statesville Formation consists of thinly interbedded, and commonly cross-bedded, dolostone and clay alternating with beds of sand. Phosphate grains are common to abundant. The Coosawhatchie Formation is made up of poorly to moderately sorted sandy clay or clayey sand with phosphate grains, limestone, and dolostone. The Suwannee Limestone is a cream colored to tan, crystalline, vuggy and muddy, fossiliferous, variably dolomitic carbonate. It has chert nodules in some areas. The Ocala Limestone was deposited in the Eocene (33.9 to 56 million years ago) and is the oldest rock formation exposed in Florida. It is a white to cream-colored, fossiliferous limestone and has chert nodules in some areas.
This area borders MLRA 133A to the north, which has only slight differences in use and management due to the underlying karst topography. Its boundaries with MLRA 152A to the west and MLRA 153A to the east are distinguishable by an abrupt scarp on a lower, younger marine terrace. Its boundary with MLRA 154 is a gradual transition to slightly younger marine sediments to the south.
Elevation of the MLRA ranges from 26 to 197 feet (8 to 60 meters). Local relief is generally 10 to 20 feet (3 to 6 meters) but can be as much as 35 feet (10 meters).
The dominant soil orders are Ultisols, Entisols, and Alfisols. The soils in the area dominantly have a thermic temperature regime, a udic moisture regime, and siliceous mineralogy.
This area supports open pine and oak vegetation. Major wildlife species include white-tailed deer, raccoon, skunk, opossum, rabbit, gray squirrel, fox squirrel, turkey, bobwhite quail, and mourning dove.
The abundant rainfall and the Floridan aquifer are the principal sources of water in the area. The many lakes and ponds are used for recreation. Most of the river water is suitable for almost all uses. Shallow and deep wells in the Floridan aquifer provide water for public supply, domestic use, industry, mining, livestock, and irrigation. This aquifer is one of the most productive sources of ground water in the United States. Its water is hard but of good quality. Wells yield large quantities of the calciumbicarbonate type of water. The Floridan aquifer is a thick sequence of Tertiary limestone and dolomite. The Eocene Avon Park Formation and Ocala Limestone are the thickest and most productive units in the aquifer system.
A significant portion of this MLRA along riparian areas remains wooded with some larger holdings used exclusively for forestry. Pulpwood and lumber are the principal forest products. Hay and pasture are of great extent throughout this MLRA. The cropland in the area is used mainly for corn, peanuts, tobacco, soybeans, vegetables, and melons.
The major resource concerns are maintenance of organic matter and productivity of the soils, management of soil moisture, and management of animal waste. Conservation practices on cropland generally include crop rotations, cover crops, nutrient management, pest management, and irrigation water management.
(USDA, NRCS, 2022)Classification relationships
Most of this area is in the East Gulf Coastal Plain section of the Coastal Plain province of the Atlantic Plain. The southern one-quarter is in the Floridian section of the same province and division. (McNab et al., 2007; USDA, NRCS, 2022)
MLRA 138 is relatively small and comprises the eastern half of EPA level IV ecoregion 65o, Tallahassee Hills and Valdosta Limesink, which is part of level III ecoregion 65, Southeastern Plains. (U.S. EPA, 2013)
The reference community of this site corresponds approximately with the Mesic and Wet Flatwood communities (FNAI, 2010).
The improved pasture community of the managed grassland state corresponds well with Forage Suitability Group G138XA241FL. (USDA, NRCS, 2013)Ecological site concept
This site is on poorly drained soils in lowland flats where the dominant hydrology is a fluctuating water table. The land is flat with slopes mostly from 0 to 2 percent.
Soils are mostly sandy over loamy, and have an argillic horizon between 20 and 40 inches. Some soils may have a mollic or umbric horizon.
This site often supports Mesic and Wet Flatwoods, Coniferous Plantations, Improved Pasture, and Rural communities.Associated sites
PX138X00Y100 Sandy Lowland Flats
These soils are in a similar landscape position but have different physical properties and productivity.
PX138X00Y120 Loamy and Clayey Lowland Flats
These soils are in a similar landscape position but have different physical properties and productivity.
Similar sites
PX138X00Y100 Sandy Lowland Flats
These sites support similar native vegetation communities, but production is somewhat different, especially regarding grazing forage production.
Table 1. Dominant plant species
Tree (1) Pinus palustris
(2) Pinus elliottiiShrub Not specified
Herbaceous Not specified
Legacy ID
F138XY110AL
Physiographic features
This site occurs in landscape positions that are not along major rivers and stream, or if it does occur near major rivers and streams it is not influenced by regular flooding events, even in the absence of water control structures. This site occurs on mesic or hydric lowlands. Dominant hydrology on this site is typically a fluctuating water table. Slope is typically 0 to 2 percent.
Table 2. Representative physiographic features
Landforms (1) Marine terrace > Flatwoods
(2) Marine terrace > Flat
Runoff class Very low Flooding frequency None Ponding duration Not specified
Ponding frequency None Elevation 25 – 200 ft Slope 0 – 2 % Water table depth 6 – 18 in Aspect Aspect is not a significant factor Table 3. Representative physiographic features (actual ranges)
Runoff class Very low Flooding frequency None Ponding duration Brief (2 to 7 days) Ponding frequency None to frequent Elevation 25 – 200 ft Slope 0 – 2 % Water table depth 0 – 18 in Climatic features
The maximum precipitation occurs in summer, and the minimum occurs in winter and late autumn. Rainfall occurs during high-intensity, convective thunderstorms in summer. The average annual temperature is 68 to 69 degrees F (20 to 21 degrees C).
An additional hazard of concern during late summer through early fall are tropical cyclones. While most impacts from hurricanes and tropical storms are confined along the coastal zone, heavy rainfall, severe flooding, and high winds can occur well into Florida when such systems pass through the area. To the extreme, the region is susceptible to the effects of a strong Bermuda High during the summer, which can cause devastating drought conditions for weeks and even months in some years.
(USDA, NRCS, 2022)Table 4 Representative climatic features
Frost-free period (characteristic range) 220-230 days Freeze-free period (characteristic range) 250-260 days Precipitation total (characteristic range) 50-50 in Frost-free period (actual range) 210-230 days Freeze-free period (actual range) 240-270 days Precipitation total (actual range) 50-50 in Frost-free period (average) 220 days Freeze-free period (average) 260 days Precipitation total (average) 50 in Characteristic rangeActual rangeBarLineFigure 1. Monthly precipitation range
Characteristic rangeActual rangeBarLineFigure 2. Monthly minimum temperature range
Characteristic rangeActual rangeBarLineFigure 3. Monthly maximum temperature range
BarLineFigure 4. Monthly average minimum and maximum temperature
Figure 5. Annual precipitation pattern
Figure 6 Annual average temperature pattern
Climate stations used
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(1) JASPER [USC00084394], Jasper, FL
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(2) LIVE OAK [USC00085099], Live Oak, FL
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(3) MAYO [USC00085539], Live Oak, FL
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(4) LAKE CITY 2 E [USC00084731], Lake City, FL
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(5) HIGH SPRINGS [USC00083956], High Springs, FL
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(6) BELL 4NW [USC00080598], Old Town, FL
">Influencing water features
The Suwannee River, which originates in the Okefenokee Swamp to the northeast and is spring-fed, flows through this MLRA. The Alapaha and Withlacoochee Rivers join the Suwannee River in the area. Another Suwannee River tributary, the Santa Fe River, crosses the southern part of the area. (USDA, NRCS, 2022)
Wetland description
Dominant hydrology on this site is a fluctuating water table. This site is poorly drained. It represents locations where the soils may or may not meet hydric field criteria, and the variation between the two may be exceptionally subtle. In situations where the soil is hydric, this site represents locations that are seasonally saturated and/or ponded, are not typically flooded, and are not exposed to tidal influences, so any wetlands that occur on this site are palustrine in nature.
Soil features
Please note that the soils listed in this section of the description may not be all inclusive. There may be additional soils that fit the site’s concepts. Additionally, the soils that provisionally form the concepts of this site may occur elsewhere, either within or outside of the MLRA and may or may not have the same geomorphic characteristics or support similar vegetation. Some soil map units and soil series included in this “provisional” ecological site were used as a “best fit” for a particular soil – landform catena during a specific era of soil mapping, regardless of the origin of parent material or the location of MLRA boundaries. Therefore, the listed soils may not be typical for MLRA 138 or a specific location, and the associated soil map units may warrant further investigation in a joint ecological site inventory – soil survey project. When utilizing this provisional description, the user is encouraged to verify that the area of interest meets the appropriate ecological site concepts by reviewing the soils, landform, vegetation, and physical location. If the site concepts do not match the attributes of the area of interest, please review the Similar or Associated Sites listed in the General Information section of this description to determine if another site may be a better fit for your area of interest.
This site is comprised of soils in the Goldhead, Mascotte, and Pelham series. These soils are poorly drained, sandy over loamy, and they have an argillic horizon between 20 and 40 inches. Some soils may have a mollic or umbric horizon.
.Table 5. Representative soil features
Parent material (1) Marine deposits
Surface texture (1) Fine sand
(2) Sand
Drainage class Poorly drained Permeability class Moderately rapid Soil depth 80 in Surface fragment cover <=3" Not specified Surface fragment cover >3" Not specified Available water capacity
(0-40in)2.1 – 4 in Soil reaction (1:1 water)
(0-10in)3.5 – 5.5 Subsurface fragment volume <=3"
(Depth not specified)Not specified Subsurface fragment volume >3"
(Depth not specified)Not specified Table 6. Representative soil features (actual values)
Drainage class Poorly drained Permeability class Moderately rapid Soil depth 80 in Surface fragment cover <=3" 0 % Surface fragment cover >3" 0 % Available water capacity
(0-40in)2.1 – 4 in Soil reaction (1:1 water)
(0-10in)3.5 – 5.5 Subsurface fragment volume <=3"
(Depth not specified)0 – 3 % Subsurface fragment volume >3"
(Depth not specified)0 % Ecological dynamics
The information presented in this ecological site description (ESD) and state-and-transition model (STM) were developed using archaeological and historical information, published and unpublished scientific reports, professional experience, consultation with technical experts, and NRCS inventories and studies. The information presented represents a complex set of plant community dynamics and environmental variables. Not all scenarios or plants are represented and included. Key indicator plants, animals, and ecological processes are described to help guide land management decisions and actions.
Unlike those of sandhill or scrub, plants of mesic flatwoods must be able to withstand the stress of soil saturation or inundation during the wet part of the year, as well as dry conditions at other times. Mesic flatwoods require frequent fire; all of its constituent plant species recover rapidly from fire and several species require fire to reproduce. Longleaf pines have thick bark to protect them from fire and their seeds need the mineral soil and open sunlight that fire provides to germinate; they form a grass stage for several years after germination that is resistant to fire. Wiregrass requires fire to flower, along with a number of other characteristic herbs, including, but not limited to, whitetop aster (Oclemena reticulata), many-flowered grass-pink, crowpoison (Stenanthium densum), and grassleaf goldenaster (Pityopsis oligantha). Red-cockaded woodpeckers, which nest in cavities in mature living pines, will abandon a nesting site if the midstory becomes too tall and dense, i.e. if fire is excluded for too long. The flatwoods salamander prefers a grassy border around its breeding ponds which is maintained against encroaching shrubs by frequent fire. Direct evidence for the natural fire return interval and season in mesic flatwoods comes from a study of fire scars on cross sections of old longleaf pine stumps in mesic flatwoods near the Gulf coast west of Apalachicola. Scars from 61 fires were recorded over a 189 year period (1679 to 1868). The average fire return interval was 3.2 years, and most fires occurred at two year intervals (42%) with three year intervals having the next highest number (22%). Seventy-two percent of all fires occurred within one to three year intervals and 23% occurred within four to six year intervals. The maximum interval recorded was ten years. Over 95% of all fires recorded before European settlement in the area (1830) occurred in the growing season. (FNAI, 2010)
The variations of vegetation structure and composition of wet flatwoods in Florida likely reflect variations in soil characteristics, hydrology and fire. The general historic fire frequency in pinelands across the southeastern U.S. coastal plain is estimated to be every 1-3 years. This interval is frequent enough to maintain grassy wet flatwoods and inhibit invasion by shrubs and is consistent with management of longleaf pine systems. Wet flatwoods that are naturally shrubbier and dominated by slash pine or pond pine may have had longer fire return intervals, or perhaps a few periods of longer intervals, on the order of 5-7 years, or up to 5-10 years, in order to allow the pines to establish and shrubs to proliferate. (FNAI, 2010)
Following this narrative, a “provisional” state and transition model is provided that includes the “perceived” reference state and several alternative (or altered) vegetation states that have been observed and/or projected for this ecological site. This model is based on limited inventories, literature, expert knowledge, and interpretations. Plant communities may differ from one location to the next depending on the severity of local land use activities and rates of deposition. Depending on objectives, the reference plant community may not necessarily be the management goal.
The environmental and biological characteristics of this site are complex and dynamic. As such, the following diagram suggests pathways that the vegetation on this site might take, given that the modal concepts of climate and soils are met within an area of interest. Specific locations with unique soils and disturbance histories may have alternate pathways that are not represented in the model. This information is intended to show the possibilities within a given set of circumstances and represents the initial steps toward developing a defensible description and model. The model and associated information are subject to change as knowledge increases and new information is garnered. This is an iterative process. Most importantly, local and/or state professional guidance should always be sought before pursuing a treatment scenario.State and transition model
More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective textEcosystem states
T1.2 - Land clearing, introduction of grasses, and applied grassland management T1.3 - Land clearing, site preparation, and tree planting T1.4 - Introduction of non-native species T2.4 - Introduction of non-native species T3.4 - Introduction of non-native species T4.1 - Mechanical, chemical or biological control T4.2 - Mechanical, chemical or biological control T4.3 - Mechanical, chemical or biological control State 1 submodel, plant communities
Communities 1, 5 and 2 (additional pathways)
P1.1.2 - Absence of fire P1.1.5 - Overstory removal P1.2.1 - Reintroduction of fire P1.2.3 - Absence of fire P1.2.5 - Overstory removal P1.3.1 - Reintroduction of fire P1.3.4 - Reintroduction of fire P1.3.5 - Overstory removal P1.3.6 - Absence of fire P1.4.1 - Reintroduction of fire P1.4.2 - Absence of fire P1.4.5 - Overstory removal P1.5.2 - Absence of fire P1.5.3 - Infrequent mixed severity fire regime P1.5.4 - Reintroduction of fire P1.6.5 - Overstory removal State 2 submodel, plant communities
P2.1.2 - Pasture abandonment P2.2.1 - Pasture restoration and applied grazing State 1
Naturalized Vegetation: Mesic and Wet FlatwoodsMesic flatwoods are flatland with sand substrate; mesic; frequent fire (2-4 years); open pine canopy with a layer of low shrubs and herbs; longleaf pine and/or slash pine, saw palmetto, gallberry, dwarf live oak, wiregrass. (FNAI, 2010).
Mesic flatwoods is characterized by an open canopy of tall pines and a dense, low ground layer of low shrubs, grasses, and forbs. Longleaf pine (Pinus palustris) is the principal canopy tree in northern and Central Florida. Although slash pine (Pinus elliottii) is currently more common than longleaf pine in mesic flatwoods in northern Florida, this a result of invasion by, or planting of, slash pine after logging of longleaf pine followed by a long period of fire exclusion in the early part of the twentieth century. (FNAI, 2010).
Wet flatwoods are flatland with sand substrate; seasonally inundated; frequent fire (2-4 years for grassy wet flatwoods, 5-10 years for shrubby wet flatwoods); closed to open pine canopy with grassy or shrubby understory; slash pine, pond pine, large gallberry, fetterbush, sweetbay, cabbage palm, wiregrass, toothache grass. (FNAI, 2010).
Wet flatwoods are pine forests with a sparse or absent midstory and a dense groundcover of hydrophytic grasses, herbs, and low shrubs. The pine canopy typically consists of one or a combination of longleaf pine (Pinus palustris), slash pine (P. elliottii), or pond pine (P. serotina). The subcanopy, if present, consists of scattered sweetbay (Magnolia virginiana), swamp bay (Persea palustris), loblolly bay (Gordonia lasianthus), pond cypress (Taxodium ascendens), dahoon (Ilex cassine), titi (Cyrilla racemiflora), and/or wax myrtle (Myrica cerifera). Shrubs include large gallberry (Ilex coriacea), fetterbush (Lyonia lucida), titi, black titi (Cliftonia monophylla), sweet pepperbush (Clethra alnifolia), red chokeberry (Photinia pyrifolia), and azaleas (Rhododendron canescens, R. viscosum). Saw palmetto (Serenoa repens) and gallberry (I. glabra), species also found in mesic flatwoods sites, may be present. (FNAI, 2010).Dominant plant species
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longleaf pine (Pinus palustris), tree
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slash pine (Pinus elliottii), tree
Community 1.1
Reference Community: Mature Even-Aged Pine Savanna10 to 20 percent tree canopy cover. 20 to 50 percent graminoid and shrub canopy cover.
Community 1.2
High Stature Shrub / Mid-Story Encroachment, Fire Suppressed20 to 50 percent shrub canopy cover and decreasing grasses relative to the reference.
Community 1.3
Uneven-Aged Pine-Oak WoodlandGreater than 25 to 60 percent tree canopy cover with less than 50 percent cover by hardwoods.
Community 1.4
Immature Even-Aged Pine Savanna10 to 20 percent tree canopy cover, and 20 to greater than 50 percent graminoid and shrub canopy cover.
Community 1.5
Open Grassland Prairie / ShrublandLess than 10 percent tree canopy cover, and 20 to greater than 50 percent graminoid and shrub canopy cover.
Community 1.6
Mature Oak Closed Canopy ForestGreater than 60 to 100 percent tree canopy cover with greater than 50 percent cover of hardwood species and relict emergent super-dominant pine.
Pathway P1.1.2
Community 1.1 to 1.2Absence of fire for greater than 5 years
Pathway P1.1.5
Community 1.1 to 1.5Overstory removal: catastrophic fire, clearcut, disease, insect, and/or hurricane.
Pathway P1.2.1
Community 1.2 to 1.1Reintroduction of natural understory fire regime with a fire return interval of between 1 to 4 years. Burning should occur late spring to early summer.
Pathway P1.2.3
Community 1.2 to 1.3Absence of fire for great than 10 to 35 years
Pathway P1.2.5
Community 1.2 to 1.5Overstory removal: catastrophic fire, clearcut, disease, insect, and/or hurricane.
Pathway P1.3.1
Community 1.3 to 1.1Reintroduction of natural understory fire regime with a fire return interval of between 1 to 4 years. Burning should occur late spring to early summer. Treatments should include selective thinning and/or oak removal.
Pathway P1.3.4
Community 1.3 to 1.4Reintroduction of natural understory fire regime with a fire return interval of between 1 to 4 years. Burning should occur late spring to early summer. Treatments should include selective thinning and/or oak removal.
Pathway P1.3.5
Community 1.3 to 1.5Overstory removal: catastrophic fire, clearcut, disease, insect, and/or hurricane.
Pathway P1.3.6
Community 1.3 to 1.6Absence of fire for greater than 35 years to 100 years
Pathway P1.4.1
Community 1.4 to 1.1Reintroduction of natural understory fire regime with a fire return interval of between 1 to 4 years. Burning should occur late spring to early summer.
Pathway P1.4.2
Community 1.4 to 1.2Absence of fire for greater than 5 years
Pathway P1.4.5
Community 1.4 to 1.5Overstory removal: catastrophic fire, clearcut, disease, insect, and/or hurricane.
Pathway P1.5.2
Community 1.5 to 1.2Absence of fire for greater than 5 years
Pathway P1.5.3
Community 1.5 to 1.3Infrequent mixed severity fire regime
Pathway P1.5.4
Community 1.5 to 1.4Reintroduction of natural understory fire regime with a fire return interval of between 1 to 4 years. Burning should occur late spring to early summer.
Pathway P1.6.5
Community 1.6 to 1.5Overstory removal: catastrophic fire, selective logging of pine, disease, insect, and/or hurricane.
State 2
Managed GrasslandManaged grassland represents both improved and unimproved pasture including wooded pasture.
Community 2.1
Improved Pasture (FSG_G138XA241FL)Dominated by planted non-native or domesticated native forage species and evidence of current or recent pasture activity and/or cultural treatments (mowing, grazing, burning, fertilizing; Agro-Ecology Grazing Issues Working Group 2009). Improved pastures have been cleared of their native vegetation. Weedy native species are often common in improved pastures in Florida and include dogfennel (Eupatorium capillifolium), many species of flatsedge (Cyperus spp.), carpetgrasses (Axonopus spp.), crabgrasses (Digitaria spp.), and rustweed (Polypremum procumbens) among many others. (FNAI, 2010)
The native forage species listed are considered adapted to grow on the soils in this group at their natural pH levels. All introduced grass and legume species will need native pH raised to minimum 5.5 (unless noted) for best production. All forages listed are adapted to dryland conditions.
Perennial Species:
Grasses
Warm season (Introduced)
• Bahiagrass (Paspalum notatum, pH 5.0 – 6.5)
• Bermudagrass (Cynodon dactylon)
• Limpograss (Hemarthria altissima)
Warm season (Native)
• Big Bluestem (Andropogon gerardii)
• Purple Bluestem (Andropogon glomeratus var. glaucopsis)
• Yellow Indiangrass (Sorghastrum nutans)
• Lopsided Indiangrass (Sorghastrum secundum)
• Switchgrass (Panicum virgatum)
• Eastern Gamagrass (Tripsacum dactyloides)
Legumes
Warm season
• Rhizoma Perennial Peanut (Arachis glabrata, pH 5.8-7.0; additional management required for high water table)
Annual Species:
Grasses
Warm season
• Browntop Millet (Urochloa ramosa; =Panicum ramosum)
• Pearl Millet (Pennisetum glaucum)
• Sorghum (Sorghum bicolor; includes forage sorghums, sudangrass, and their hybrids)
Cool season
• Ryegrass, annual (Lolium perenne ssp. multi-florum; =L. multiflorum)
• Oat (Avena sativa)
• Rye (Secale cereale)
• Wheat (Triticum aestivum)
• Triticale (x Triticosecale)
Legumes
Warm season
• Aeschynomene (Aeschynomene americana)
• Hairy Indigo (Indigofera hirsuta)
Cool season
• White Clover (Trifolium repens, pH 6.0-7.5)
• Berseem Clover (Trifolium alexandrinum, pH 6.5-8.0)
• Ball Clover (Trifolium nigrescens, pH >6.5)
(USDA, NRCS, 2013m)Figure 7. Annual production by plant type (representative values) or group (midpoint values)
Figure 8. Plant community growth curve (percent production by month). FL0007 , Introduced Warm Season Annual Grasses. Growth Curves and Dry Matter Distribution for Introduced Warm Season Annual Grasses.
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 4 11 23 35 16 10 3 0 0 Figure 9. Plant community growth curve (percent production by month). FL0005 , Native Warm Season Perennial Grasses. Growth Curves and Dry Matter Distribution for Native Warm Season Perennial Grasses.
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec J F M A M J J A S O N D 1 2 3 5 10 20 27 19 7 3 2 1 Community 2.2
Unimproved Pasture with Woody EncroachmentThis community is characterized by a mixture of native and naturalized non-native species. Forage is usually grazed and/or harvested as stored forage, hay or haylage. Stands are generally productive, and forage and grazing management can maintain the community. Woody species grow quickly on this site and can be difficult and expensive to control. Maintenance of grass stands requires implementing pest management practices to control unwanted weedy and woody species.
Pathway P2.1.2
Community 2.1 to 2.2Pasture abandonment
Pathway P2.2.1
Community 2.2 to 2.1Pasture restoration and applied grazing
State 3
Pine PlantationPine plantations in Florida are often dominated by evenaged loblolly, sand, or slash pine (Pinus taeda, P. clausa, or P. elliottii, respectively). Dense pine plantations typically have sparse to absent herbaceous vegetation as a result of shading or a cover of deep pine needle duff. These plantations may be very shrubby or vine-dominated or open at ground level. The groundcover in most cases has been severely impacted by mechanical site preparation, such as roller chopping and bedding. However, while perennial grasses such as wiregrass (Aristida stricta var. beyrichiana) may be greatly reduced, many components of the native groundcover persist even though the relative abundance is altered. Groundcover can be partially restored by thinning and/or frequent burning, although some planting of perennial grasses such as wiregrass may be required. (FNAI, 2010)
Dominant plant species
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loblolly pine (Pinus taeda), tree
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slash pine (Pinus elliottii), tree
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sand pine (Pinus clausa), tree
State 4
DegradedThe degraded State represents vegetation conditions that have been degraded by the introduction and spread of non-native species.
Transition T1.2
State 1 to 2Land clearing, introduction of grasses, and applied grassland management
Transition T1.3
State 1 to 3Land clearing, site preparation, and tree planting
Transition T1.4
State 1 to 4Introduction of non-native species
Transition T2.4
State 2 to 4Introduction of non-native species
Transition T3.4
State 3 to 4Introduction of non-native species
Transition T4.1
State 4 to 1Mechanical, chemical or biological control
Transition T4.2
State 4 to 2Mechanical, chemical or biological control
Transition T4.3
State 4 to 3Mechanical, chemical or biological control
Additional community tables
Table 7. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 8. Community 1.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 9. Community 1.3 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 10. Community 1.4 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 11. Community 1.5 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 12. Community 1.6 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 13. Community 2.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Grass/Grasslike1 Graminoids 900–14000 Bermudagrass CYDA Cynodon dactylon 11000–14000 – limpograss HEAL5 Hemarthria altissima 8800–13000 – pearl millet PEGL2 Pennisetum glaucum 6600–12000 – eastern gamagrass TRDA3 Tripsacum dactyloides 4000–6750 – bahiagrass PANO2 Paspalum notatum 3300–6000 – big bluestem ANGE Andropogon gerardii 900–1800 – Forb2 Legumes 2200–3000 shyleaf AEAM Aeschynomene americana 2200–3000 – hairy indigo INHI Indigofera hirsuta 2200–3000 – Table 14. Community 2.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Supporting information
Inventory data references
Data collection and analysis of field data will be performed during the Verification Stage of ESD development. Production data for pasture communities taken from the USDA, NRCS Florida Field Office Technical Guide, forage suitability groups (USDA, NRCS, 2013).
Other references
Carr, S. C., Robertson, K. M., & Peet, R. K. 2010. A vegetation classification of fire-dependent pinelands of Florida. Castanea, 75(2), 153-189.
Casey, W. P., & Ewel, K. C. 2006. Patterns of succession in forested depressional wetlands in north Florida, USA. Wetlands, 26(1), 147-160.
Dey, D. C., Brissette, J. C., Schweitzer, C. J., & Guldin, J. M. 2012. Silviculture of forests in the Eastern United States. Cumulative watershed effects of fuel management in the Eastern United States Gen Tech Rep SRS-161. Asheville, NC: US Department of Agriculture Forest Service, Southern Research Station, 7-40.
Florida Chapter Soil and Water Conservation Society. 1989. 26 Ecological Communities of Florida
Greenberg, C. H., & Simons, R. W. 1999. Age, composition, and stand structure of old-growth oak sites in the Florida high pine landscape: implications for ecosystem management and restoration. Natural Areas Journal. 19 (1): 30-40.
Grelen, H. E. 1962. Plant succession on cleared sandhills in northwest Florida. American Midland Naturalist, 36-44.
Haag, K. H., Lee, T. M., & Water, T. B. 2010. Hydrology and ecology of freshwater wetlands in central Florida: a primer. Reston, VA, USA: US Geological Survey.
Inventory, F. N. A. 2010. Guide to the natural communities of Florida: 2010 edition. Florida Natural Areas Inventory, Tallahassee, FL.
Kellison, R. C., & Young, M. J. 1997. The bottomland hardwood forest of the southern United States. Forest Ecology and Management, 90(2-3), 101-115.
Landers, J. L., & Boyer, W. D. 1999. An old-growth definition for upland longleaf and south Florida slash pine forests, woodlands, and savannas (Vol. 29). US Department of Agriculture, Forest Service, Southern Research Station.
LaPierre, G. D. J., Irizarry, N. M., & Andreu, M. G. 2022. Florida Soil Series and Natural Community Associations: FOR384/FR455, 5/2022. EDIS, 2022(3).
Light, H. M. 1993. Hydrology, vegetation, and soils of four North Florida river flood plains with an evaluation of state and federal wetland determinations (Vol. 93, No. 4033). US Department of the Interior, US Geological Survey.
Martin, T. A., & Jokela, E. J. 2004. Stand development and production dynamics of loblolly pine under a range of cultural treatments in north-central Florida USA. Forest Ecology and Management, 192(1), 39-58.
Martin, T. A., Adams, D. C., Cohen, M. J., Crandall, R. M., Gonzalez-Benecke, C. A., Smith, J. A., & Vogel, J. G. 2017. Managing Florida's plantation forests in a changing climate. Florida's Climate: Changes, Variations, & Impacts.
McNab, W.H.; Cleland, D.T.; Freeouf, J.A.; Keys, Jr., J.E.; Nowacki, G.J.; Carpenter, C.A., comps. 2007. Description of ecological subregions: sections of the conterminous United States [CD-ROM]. Gen. Tech. Report WO-76B. Washington, DC: U.S. Department of Agriculture, Forest Service. 80 p
Monk, C. D. 1968. Successional and environmental relationships of the forest vegetation of north central Florida. American Midland Naturalist, 441-457.
NatureServe. 2018. International Ecological Classification Standard: Terrestrial Ecological Classifications. NatureServe Central Databases. Arlington, VA. U.S.A. Data current as of 28 August 2018.
Schoeneberger, P.J., and Wysocki, D.A. 2017. Geomorphic Description System, Version 5.0. Natural Resources Conservation Service, National Soil Survey Center, Lincoln, NE.
Scott, T. M. 2001. Text to accompany the geologic map of Florida. Florida Geologic Survey, Tallahassee, Florida.
Tamang, B., Hedman, C., Haines, F., Stone, D., & Andreu, M. 2023. Upland forest community composition and structure by ecoregion in 73 Florida state parks–Insights for ongoing management. Forest Ecology and Management, 545, 121237.
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013. Forage Suitability Groups, MLRA 138XA. Retrieved from https://efotg.sc.egov.usda.gov/#/state/FL/documents/section=2&folder=52895.
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013a. Forage Suitability Group G138XA111, Sandy Soils on Ridges and Dunes of Xeric Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA111FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013b. Forage Suitability Group G138XA113, Sandy Soils on Strongly Sloping to Steep Side Slopes of Xeric Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA113FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013c. Forage Suitability Group G138XA114, Sandy Xeric Soils on Stream Terraces or Flood Plains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA114FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013d. Forage Suitability Group G138XA121, Sandy Soils on Rises, Knolls, and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA121FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013e. Forage Suitability Group G138XA123, Sandy Soils on Strongly Sloping to Steep Side Slopes of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA123FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013f. Forage Suitability Group G138XA124, Very Deep, Sandy Soils on Terraces and Floodplains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA124FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013g. Forage Suitability Group G138XA131, Sandy Soils on Rises and Knolls of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA131FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013h. Forage Suitability Group G138XA134, Sandy or Sandy Over Loamy Soils on Stream Terraces or Flood Plains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA134FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013i. Forage Suitability Group G138XA141, Sandy Soils, on Flats on Mesic and Hydric Lowlands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA141FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013j. Forage Suitability Group G138XA145, Sandy Soils on Stream Terraces, Flood Plains, or in Depressions. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA145FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013j’. Forage Suitability Group G138XA211, Sandy Over Loamy Soils on Knolls and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA211FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013k. Forage Suitability Group G138XA221, Sandy Over Loamy Soils on Rises, Knolls, and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA221FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013l. Forage Suitability Group G138XA231, Sandy Over Loamy Soils on Flats and Rises of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA231FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013m. Forage Suitability Group G138XA241, Sandy Over Loamy Soils on Flats of Hydric or Mesic Lowlands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA241FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013n. Forage Suitability Group G138XA245, Sandy Over Loamy Soils on Stream Terraces, Flood Plains or in Depressions. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA245FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013o. Forage Suitability Group G138XA311, Loamy and Clayey Soils on Knolls and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA311FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013p. Forage Suitability Group G138XA312, Loamy and Clayey Soils on Ridges and Side Slopes of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA312FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013p’. Forage Suitability Group G138XA321, Loamy and Clayey Soils on Rises and Knolls of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA321FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013p’’. Forage Suitability Group G138XA322, Loamy and Clayey Sols on Rises, Knolls, and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA322FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013q. Forage Suitability Group G138XA331, Loamy and Clayey Soils on Flats and Rises of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA331FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013r. Forage Suitability Group G138XA334, Loamy and Clayey Soils on Stream Terraces and Flood Plains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA334FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013s. Forage Suitability Group G138XA341, Loamy and Clayey Soils on Flats of Hydric or Mesic Lowlands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA341FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013t. Forage Suitability Group G138XA345, Loamy and Clayey Soils on Stream Terraces, Flood Plains or in Depressions. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA345FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2013u. Forage Suitability Group G138XA521, Shallow or Moderately Deep, Sandy or Loamy Soils on Rises and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA521FL.pdf
U.S. Department of Agriculture, Natural Resources Conservation Service. 2017. Geomorphic Description System, Version 5.0. Schoeneberger, P.J., and D.A. Wysocki (eds). USDA-NRCS, National Soil Survey Center, Lincoln, NE.
U.S. Department of Agriculture, Natural Resources Conservation Service. 2022. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. Agriculture Handbook 296.
U.S. Environmental Protection Agency. 2013. Level III and IV ecoregions of the continental United States: Corvallis, Oregon, U.S. EPA, National Health and Environmental Effects Research Laboratory, map scale 1:3,000,000, https://www.epa.gov/eco-research/level-iii-and-iv-ecoregions-continental-united-states.Contributors
Duvall, Matthew
Ferrara, Jack
Figueroa, MartinApproval
Charles Stemmans, 6/09/2025
Acknowledgments
Sincere appreciation goes to the MLRA 138X ecological sites technical team, especially NRCS Florida State Soil Scientist, Isabelle Giuliani, and NRCS Florida State Forester, Conrad Wysocki, for their persistent collaboration in the development of these Provisional ESDs.
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) Contact for lead author Date 09/15/2026 Approved by Approval date Composition (Indicators 10 and 12) based on Annual Production Indicators
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Number and extent of rills:
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Presence of water flow patterns:
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Number and height of erosional pedestals or terracettes:
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Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
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Number of gullies and erosion associated with gullies:
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Extent of wind scoured, blowouts and/or depositional areas:
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Amount of litter movement (describe size and distance expected to travel):
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Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
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Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
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Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
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Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
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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:
Sub-dominant:
Other:
Additional:
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Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
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Average percent litter cover (%) and depth ( in):
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Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
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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:
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Perennial plant reproductive capability:
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PrintThe 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.
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