Natural Resources
Conservation Service
Ecological site F156AY340FL
Subtropical Pine Flatwoods and Palmetto Prairie of Miami Ridge / Atlantic Coastal Strip
Last updated: 4/14/2025
Accessed: 04/16/2026
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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): 156A–Florida Everglades and Associated Areas
This area makes up about 7,749 square miles (20,071 square kilometers) and is entirely in Florida. It is located at the southern tip of the State and has shoreline on both the Atlantic Ocean and the Gulf of America. Lake Okeechobee borders the MLRA to the north. Aside from sugar cane plantations in the north, the Everglades National Park, Big Cypress National Preserve, and the Big Cypress Seminole Indian Reservation comprise this area. Historical ditching, berming, and canals prevent natural water flow through this delicate ecosystem. To mitigate this, extensive restoration efforts have been implemented. Urban sprawl from Miami and cities to its north on the Atlantic Ridge has encroached along the eastern boundary of this area. Most of the MLRA has resisted urbanization because of a water table that is at or near the surface, a considerable acreage of unstable organic soils, and its identity as a national treasure.
About one-third of this area is in Native American reservations, national parks, game refuges, or other large holdings. Cypress forests are extensive in the area, but mangrove forests are widespread along the eastern and southern coasts. A large part of the area is open marsh. Much of the area is used for hunting, fishing, and other recreational activities. The cropland in the area is used mainly for winter vegetables, but citrus fruits, avocado, and papaya are grown on the better drained soils. Sugarcane is an important crop on the organic soils south of Lake Okeechobee. The acreage of improved pasture is increasing. Beef cattle are the principal kind of livestock, but dairying is an important enterprise locally. Urbanization is extensive along the eastern coast.
The major soil resource concerns are wind erosion, maintenance of the content of organic matter and productivity of the soils, and management of soil moisture and soil subsidence. Conservation practices on cropland generally include conservation crop rotations, cover crops, nutrient management, pest management, water-control structures, surface drainage systems (field ditches, mains, and laterals), pumping plants, and irrigation water management (including micro irrigation systems and surface and subsurface irrigation systems). Conservation practices on pasture and rangeland generally include prescribed grazing, brush management, pest management, prescribed burning, and watering facilities. Conservation practices on forestland generally include forest stand improvement, firebreaks, pest management, prescribed burning, and management of upland and wetland wildlife habitat.LRU notes
There is not an official LRU for the MLRA 156A area. For the time being the technical team recommended to add the four terrestrial physiographic provinces ecoregions (Big Cypress, Everglades, Southern Coast and Islands, and Miami Ridge / Atlantic Coastal Strip) and one subaqueous ecoregion (Coastal Marine and Estuarine) on this section. This PES occurs within the Miami Ridge / Atlantic Coastal Strip ecoregion.
The Miami Ridge/Atlantic Coastal Strip Ecoregion, sea level to 20 m (0 to 66 ft) in elevation, is a heavily urbanized region, with coastal ridges on the east and flatter terrain to the west that grades into the Everglades. The western side originally had wet and dry prairie marshes on marl and rockland and sawgrass marshes, but much of it is now covered by cropland, pasture, and suburbs. To the south, the Miami Ridge extends from near Hollywood south to Homestead and west into Long Pine Key of Everglades National Park. It is a gently rolling rock ridge of oolitic limestone that once supported more extensive southern slash pine forests and islands of tropical hardwood hammocks. The northern part of the region is a plain of pine flatwoods and wet prairie, and coastal sand ridges with scrub vegetation and sand pine. There are very few natural lakes in the region, but three types of ponded surface waters occur: 1) Pits dug deep into underlying "rock" containing water that is clear, high pH and alkaline, with moderate nutrients; 2) Shallow, surficial dug drains that are darker water; and 3) flow-through lakes (e.g., Lake Osborne) that are colored and nutrient rich.Classification relationships
All portions of the geographical range of this site falls under the following ecological / land classifications including:
-Environmental Protection Agency's Level 3 and 4 Ecoregions of Florida: 76 Southern Florida Coastal Plain; 76C Miami Ridge/ Atlantic Coastal Strip (Griffith, G. E., Omernik, J. M., & Pierson, S. M., 2013)
-Florida Natural Area Inventory, 2010 Edition: Pine Flatwoods and Dry Prairie (FNAI ,2010)
-Soil Conservation Service, 26 Ecological Communities of Florida: 6- South Florida Flatwoods (Florida Chapter Soil and Water Conservation Society, 1989)Ecological site concept
The Subtropical Pine Flatwoods and Palmetto Prairie of Miami Ridge/ Atlantic Coastal Strip ecological community are characterized by low, flat lands with poorly drained, sandy soils and an open overstory of pines with a dense grassy and / or shrubby understory. Frequent periodic disturbances are the biggest stressors of these communities. These sites have been highly altered due to the high demand for urbanization within the Miami Ridge/ Atlantic Coast Strip ecoregion.
Associated sites
R156AY320FL Subtropical Freshwater Non-Forested Wetlands of Miami Ridge/ Atlantic Coastal Strip
The Subtropical Freshwater Non-Forested Wetlands of Miami Ridge / Atlantic Coastal Strip occurs on lower landscape positions with greater hydroperiods and more hydrophytic herbaceous species composition. This community may gently grade into a flatwoods community, often with the presence of stunted pines as indication.
F156AY330FL Subtropical Freshwater Cypress Swamps of Miami Ridge / Atlantic Coastal Strip
The Subtropical Freshwater Cypress Swamps of Miami Ridge / Atlantic Coastal Strip occurs on lower landscape positions with greater hydroperiods and more hydrophytic woody coniferous species composition. This community may gently grade into a flatwoods community, often with the replacement of hydrophytic trees by slash pine.
F156AY360FL Subtropical Moist Hammocks of Miami Ridge / Atlantic Coastal Strip
The Subtropical Moist Hammocks of Miami Ridge / Atlantic Coastal Strip occurs on lower landscape positions with greater hydroperiods and more hydrophytic woody deciduous species composition. This community may gently grade into a flatwoods community, often with the replacement of hydrophytic trees by slash pine.
F156AY380FL Subtropical Hardwood Hammocks of Miami Ridge / Atlantic Coastal Strip
The Subtropical Hardwood Hammocks of Miami Ridge / Atlantic Coastal Strip occurs on higher landscape positions with greater mesic and xeric species composition. Soil drainage is more somewhat poorly to moderately well sandy soils.
F156AY390FL Subtropical Scrub of Miami Ridge / Atlantic Coastal Strip
The Subtropical Scrub of Miami Ridge / Atlantic Coastal Strip occurs on higher landscape positions with greater mesic and xeric species composition. Soil drainage is more moderately well to excessively drained sandy soils.
Similar sites
F156AY350FL Subtropical Forested Rocklands of Miami Ridge / Atlantic Coastal Strip
The Subtropical Forested Rocklands of Miami Ridge / Atlantic Coastal Strip has similar community structure but consists of shallow soils with the presence of limestone at or near the surface. This community has a more diverse species composition consisting of more tropical species.
F156AY010FL Subtropical Pine Flatwoods and Palmetto Prairie of Big Cypress
The Subtropical Pine Flatwoods and Palmetto Prairie of Big Cypress occurs in a separate ecoregion which have lower amounts of urbanization and slightly lower amounts of rainfall and lower elevation. Species composition and vegetative structure are similar. Resource concerns are reflected differently and require different management needs.
F156AY020FL Subtropical Forested Rocklands of Big Cypress
The Subtropical Forested Rocklands of Big Cypress occurs in a separate ecoregion which have lower amounts of urbanization and slightly lower amounts of rainfall and lower elevation. It also has more shallow depths to bedrock, exposed limestone rock, and the presence of rare plant species characteristic to this site.
F156AY130FL Subtropical Forested Rocklands of Southern Coast and Islands
The Subtropical Forested Rocklands of Southern Coast and Islands occur in a separate ecoregion which have lower amounts of urbanization and slightly lower amounts of rainfall and lower elevation. It also has more shallow depths to bedrock, exposed limestone rock, and the presence of rare plant species characteristic to this site.
Table 1. Dominant plant species
Tree (1) Pinus elliottii var. densa
(2) Sabal palmettoShrub (1) Serenoa repens
(2) Ilex glabraHerbaceous (1) Aristida stricta
(2) Ctenium aromaticumPhysiographic features
These areas are dominated by linear flatwoods that form in marine deposits. Slight changes in microtopography will often dictate species composition and hydroperiod. Micro-lows, or areas with slope shapes of linear – concave will reflect a seasonal high-water table of 0 to 6 inches and may hold standing water very long if endo- and epi-saturation are exhausted after periods of heavy rain. Micro-highs, or areas with slope shapes of convex – linear will reflect a seasonal high-water table of 6 to 18 inches and may hold standing water briefly if endo- and epi-saturation are exhausted after periods of extreme rain. Species composition may vary slightly based off the microtopography but will often reflect similar community structure and maintenance. These communities are often intermixed with one another and form a matrix of linear-concave, linear-linear, and convex-linear topography mapped within one soil component.
The Miami Ridge/ Atlantic Coastal Strip falls under the Pleistocene series Miami Limestone geologic formation, also known as Miami Oolite. It forms the Atlantic Coastal Ridge and extends beneath the Everglades where it is commonly covered by thin organic and freshwater sediments, as well as extending down into the Florida Keys. To the north the Miami Limestone formation grades laterally northward into the Anastasia Formation. The Miami Limestone consists of two facies, an oolitic facies and a bryozoan facies. The oolitic facies consists of white to orangish gray, poorly to moderately indurated, sandy, oolitic limestone (grainstone) with scattered concentrations of fossils. The bryozoan facies consist of white to orangish gray, poorly to well indurated, sandy, fossiliferous limestone grainstone and packstone). Beds of quartz sand are also present as unindicated sediments and indurated limey sandstones. Fossils present include mollusks, bryozoans, and corals. Molds and casts of fossils are common. The highly porous and permeable Miami Limestone forms much of the Biscayne Aquifer of the surficial aquifer system.Table 2. Representative physiographic features
Geomorphic position, flats (1) Talf
(2) Dip
(3) Rise
Geomorphic position, terraces (1) Tread
Slope shape across (1) Convex
Slope shape up-down (1) Linear
(2) Linear
(3) Concave
Landforms (1) Coastal plain
(2) Marine terrace > Flat
(3) Marine terrace > Flatwoods
Runoff class Very low to low Flooding frequency None Ponding duration Brief (2 to 7 days) to long (7 to 30 days) Ponding frequency Occasional to frequent Elevation 3 – 66 ft Slope 0 – 2 % Ponding depth 0 – 10 in Water table depth 6 – 18 in Aspect Aspect is not a significant factor Climatic features
The climate of MLRA 156A is subtropical, with mild winters and hot wet summers. The average annual precipitation of this MLRA is 37 to 62 inches (950 to 1,565 millimeters). About 60 percent of the precipitation occurs from June through September. Most of the rainfall occurs during moderate intensity, tropical storms that produce large amounts of rain from late spring through early autumn. Late autumn and winter are relatively dry. The average annual temperature of the MLRA is 74 to 78 degrees F (23 to 26 degrees C). The freeze-free period of the MLRA averages 355 days and ranges from 345 to 365 days.
The following tables and graphs consist of specific climate stations found within the range of this ecological site within this MLRA.Table 3 Representative climatic features
Frost-free period (characteristic range) 370 days Freeze-free period (characteristic range) 370 days Precipitation total (characteristic range) 60-60 in Frost-free period (actual range) 370 days Freeze-free period (actual range) 370 days Precipitation total (actual range) 50-70 in Frost-free period (average) 370 days Freeze-free period (average) 370 days Precipitation total (average) 60 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) ROYAL PALM RS [USC00087760], Homestead, FL
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(2) HOMESTEAD GEN AVIATION [USC00084095], Homestead, FL
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(3) PERRINE 4W [USC00087020], Miami, FL
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(4) MIAMI KENDALL TAMIAMI EXEC AP [USW00012888], Miami, FL
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(5) MIAMI WSO CITY [USW00012859], Miami, FL
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(6) MIAMI NWSFO [USC00085667], Miami, FL
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(7) CAPE FLORIDA [USC00081306], Key Biscayne, FL
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(8) MIAMI BEACH [USW00092811], Miami Beach, FL
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(9) MIAMI OPA LOCKA AP [USW00012882], Opa Locka, FL
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(10) NORTH MIAMI BEACH #2 [USC00086315], Miami, FL
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(11) HOLLYWOOD NORTH PERRY AP [USW00092809], Hollywood, FL
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(12) WESTON [USC00089511], Fort Lauderdale, FL
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(13) FT LAUDERDALE [USC00083163], Fort Lauderdale, FL
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(14) LOXAHATCHEE NWR [USC00085184], Boynton Beach, FL
">Influencing water features
The flat topography creates minimal gradients, resulting in sufficient time for percolation, soil saturation and slow runoff that occasionally creates very poorly defined first-order ephemeral streams and typically results in sheet flow patterns if water becomes high. Where a soil hardpan is present, water moves slowly vertically relative to horizontal movement, through horizons above and below the hardpan layer. With standing water, wet flatwood soils may become waterlogged and poorly aerated during the rainy season. Mesic pine flatwoods soils can also become waterlogged and poorly aerated during the extreme rain events. This results in the saturated soils typical of unaltered, undrained mesic flatwoods. During the dry season, high evapotranspiration draws most of the water out of the upper soil horizons, drying them out. Soil moisture becomes depleted in the upper soil layers, above the hardpan, and a persistent drought condition frequently prevails through the dry season. As a result, during the dry season, groundwater is inaccessible for plants that cannot penetrate the hardpan. The most frequent and widespread hydrologic alterations typically result in reduced depth and duration of inundation, which tends to shift affected wetland plant communities towards shallower wetland types, or with sufficient drainage to upland types.<br />
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Water depths in flatwoods vary throughout the seasonal hydrologic cycle. With the onset of the rainy season, flatwoods may become quickly saturated. As the rate of precipitation exceeds the rate of runoff and percolation, standing water may begin to appear in the microlows in June. By July, flatwoods are uniformly wet. Deepest water levels are attained by the late rainy season in September. As the dry season begins in November the pattern reverses, with a shift to runoff and percolation exceeding precipitation. This results in the formation of isolated pools, as sheet flow recedes below the ground surface. The recession of the surface water is quick to reside after periods of rain as water drains to lower landscape positions. In the Miami Ridge/ Atlantic Coastal Strip, extensive urbanization has highly fragmented these habitats, altering hydroperiods which may not exhibit ponding or flooding periods due to drainage and sewer systems.Wetland description
Surface water ponding and soil saturation levels may vary from year to year based on local environmental conditions. According to the USDA-NRCS in Florida and the National Wetland Inventory (NWI), mesic and wet flatwoods are not considered wetland habitats but may have the potential to support wetland habitats. Location specific investigations are required to determine site specific conditions for wetland delineation.
Figure 7. Historical development of South Florida canal systems from 1900 to 1920 before the urbanization of the Miami Ridge. Image modified from Duever et al. 1979.
Figure 8. Historical development of South Florida canal systems from 1930 to 1950 during the early urbanization of the Miami Ridge. Image modified from Duever et al. 1979.
Figure 9. Historical development of South Florida canal systems from 1960 to 1970 during the heavy urbanization efforts of the Miami Ridge. Image modified from Duever et al. 1979.
Figure 10. Conceptual hydrologic system model of South Florida. Image modified from Swain et al. 2019.
Soil features
Soils associate with this ecological site occur in the isohyperthermic soil temperature regime of MLRA 156A. The isohyperthermic soil temperature regime has mean annual soil temperatures of 22 °C (72⁰F) or more and a difference between mean summer and mean winter soil temperatures of less than 5 °C (41⁰F) at 50 cm (20 inches) below the surface.
These are deep to very deep soils occurring on poorly to very poorly drained upland sites where permeability is rapid to very rapid in the A and E horizon, but very slow to moderate in the organic hardpan, usually seen as a Bw or Btg horizon within several feet of the soil surface. They are formed in sandy and loamy marine sediments overlying loamy materials and are nutrient-poor and acidic. This area has undergone extreme urbanization efforts and much of the historic representative soils in this area have been replaced with an "Urban Complex" phase or have been completely altered to the extent of being "Urban Land", and the representative soil destroyed. Common soil orders that could have be found in this ecological site are entisols or alfisols with a subsurface clay layer to impede drainage. Present soils include: udorthents and urban land. Representative soil series may include Margate, Sunny Isles, and Grande Oaks.Table 4. Representative soil features
Parent material (1) Marine deposits
(2) Residuum – limestone
Surface texture (1) Fine sand
Drainage class Very poorly drained to poorly drained Permeability class Rapid to very rapid Depth to restrictive layer 30 – 80 in Soil depth 40 – 80 in Surface fragment cover <=3" Not specified Surface fragment cover >3" Not specified Available water capacity
(0-80in)0.5 – 1.1 in Calcium carbonate equivalent
(0-80in)Not specified Electrical conductivity
(0-80in)0 – 1 mmhos/cm Sodium adsorption ratio
(0-80in)1 Soil reaction (1:1 water)
(0-80in)5.6 – 7.3 Subsurface fragment volume <=3"
(0-80in)Not specified Subsurface fragment volume >3"
(0-80in)Not specified 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 dynamic 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.
The natural vegetation is mainly dominated by a scattered slash pine (Pinus elliottii) or South Florida slash pine (Pinus elliottii var. densa) overstory with a grass and shrub dominated understory. In a mature stand, pine canopy covers 10 to 20 % with low intensity fires suppressing herbaceous and invasive species. Small outcrops of weathered limestone may be present in this community due to high acidity of pine needles contributing to the karst topography of South Florida. Slash pines are self-pruning conifers that form open canopies allowing for a well vegetated understory. It is tolerant of a wide array of conditions, and can form large surface roots that create micro-highs. This often makes distinguishing between these ecological sites' vegetative communities difficult as it appears to form a matrix of different communities described below. Small variations in hydroperiods and fire frequency will drive the distribution of two reference communities (1.1 and 1.2) in this provisional ecological site (PES). Thus, we included both wet flatwoods (1.1) and mesic flatwoods (1.2) as the two reference site conditions, with the caveat that mesic flatwoods are not the successional stage of wet flatwoods, but rather reflect a variation in hydroperiod and fire frequency. Although these slight changes in hydroperiod and fire frequency affect different plant compositions, these differences are not captured in the soil map units.
All flatwoods require relatively short fire intervals all its constituent plant species recover rapidly from fire and several species require fire to reproduce. Wet Flatwoods require 1 to 3 year intervals between fires to maintain a grassy understory, while mesic flatwoods require 2 to 4 year fire intervals to inhibit invasion of undesirable species into the understory such as shrubs. Drainage, either directly by ditching or indirectly by drawdown of the water table can allow for shrubs to invade giving the area the appearance of scrubby flatwoods. However, scrubby flatwoods are not a natural community found within this MLRA due to their formation on naturally moderately well drained soils, which is not naturally seen within this ecoregion unless anthropogenically altered. This is less seen due to consistent fire intervals via anthropogenic or natural ignitions, as well as natural events such as rare frost events and hurricane winds that weed out hardwood trees with shallow root systems, slowing succession. Soil that have been drained and underwent disturbance render flatwoods in South Florida vulnerable to community transitions and to invasion by the exotic melaleuca (Melaleuca quinquenervia) which may be difficult to control once established since fire and herbicide treatments stimulate its seed release. Other invasive species in flatwoods include cogon grass (Imperata cylindrica) and Brazilian pepper (Schinus terebinthifolius), which are difficult to remove once established and are fire adapted species.
Fire is an important driver for maintaining Florida flatwoods community structure. Both Florida slash pines and slash pines have thick bark to protect them from fire and their seeds need the mineral soil and open sunlight that fire provides to germinate; and both form a grass stage for several years after germination that is resistant to fire. Wiregrass requires fire to flower, along with several other characteristic herbs, including, but not limited to, whitetop aster (Oclemena reticulata), many-flowered grass pink, crowpoison (Stenanthium densum), and grassleaf goldenaster (Pityopsis oligantha). The greater the understory development due to absence of regular fire there is a greater chance for a catastrophic fire due to accumulated needle beds and the height of flammable understory shrubs. A crown fire can spread from tree to tree independent of fire movement on the ground, causing mass tree mortality. Pine trees that undergo mass mortality will open the canopy and can transition the flatwoods into a palmetto prairie, with standing dead or burned-out stumps present. If fires are very frequent, along the scale of every 1 to 2 years, seedling regeneration cannot occur, and the flatwoods can become dominated by a herbaceous understory with cabbage palms becoming emergent as a cabbage palm flatwoods.
Palmetto prairies consist of low shrubs and grasses occupying vast, level expanses in the Florida landscape. They are similar to the mesic version of pine flatwoods but lack the overhead pine component. The stress of fire at the beginning of the rainy season followed immediately by the stress of a seasonal high water table with the start of the summer rainy season, both of which would have been more frequent events in palmetto prairie compared to the surrounding flatwoods, may be sufficient to prevent pine seedlings from becoming established . Thus, a suite of conditions including soil impermeability and timing of fire and rain events in Florida may intersect to produce palmetto prairie landscapes. Natural fire intervals are very short, within the order of every 1 to 2 years to maintain community structure. Mechanical removal such as roller chopping can also be used to replace fires in highly urban or controversial areas, but treatment can damage non-target species as well as leading to woody invasion.
The extent of palmetto prairies is limited to south central Florida, with few small patches entering the Miami Ridge/ Atlantic Coastal Strip eco region in the southeast corner of the MLRA. Much of the historical extent for palmetto prairie has been converted to natural resource or urban land. Palmetto prairies differ from pine flatwoods by the lack of overstory species such as pine, and different understory species in wet flatwoods. While fragmented in size, remaining natural palmetto prairies completely lack pine species, extreme fire events in mesic pine flatwoods can create an altered palmetto prairie looking state where burned pine stumps may be present, but lack any living trees. Palmetto prairies differ from wet prairies from the lack of shrubs, presence of drier grass species such as wire grass or blue maidencane, and the presence of wetland herbs.
In highly urban areas where prescribed fire is not the preferred management of pine flatwoods and palmetto prairies due to the smoke nuisance, mechanical removal is often used. This includes roller chopping and other similar range practices, but commonly leads to more grasses and less shrubs in the understory,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
States 1, 5 and 6 (additional transitions)
States 2, 5 and 6 (additional transitions)
T1A - Overstory Mortality T1B - Absence of Fire T1C - Invasion of Non-Native / Exotic Species T1D - Modified for Desired Land Use T1E - Human Alteration / Transportation of Materials T2A - Pine Regeneration / Fire T2B - Change in Fire Frequency/ Logging T2C - Invasion of Non-Native / Exotic Species T2C - Modify for Desired Land Use T2D - Human Alteration / Transportation of Materials T3A - Logging of Oaks/ Return Fire Frequency T3B - Mechanical/ Chemical Removal / Fire Reintroduction T3C - Invasion of Non-Native / Exotic Species T3D - Modify for Desired Land Use T3E - Human Alteration / Transportation of Materials R4A - Mechanical / Biological / Chemical Removal of Undesirable Species R4B - Mechanical / Biological / Chemical Removal R4C - Mechanical / Biological / Chemical Removal R4D - Mechanical / Biological / Chemical Removal T4A - Human Alteration / Transportation of Materials R5A - Landscape and Habitat Restoration R5B - Landscape and Habitat Restoration R5C - Landscape and Habitat Restoration T5A - Invasion of Non-Native / Exotic Species T5B - Human Alteration / Transportation of Materials State 1 submodel, plant communities
1.1A - Decreases in Long Term Hydroperiod and Fire Frequency 1.1B - Fire Suppression / Decrease in Natural Hydroperiod 1.2A - Increases in Long Term Hydroperiod and Fire Frequency 1.2B - Fire Suppression / Decrease in Natural Hydroperiod 1.3A - Reduction or Removal of Undesirable Species / Reintroduce Natural Fire Frequency 1.3B - Reduction or Removal of Undesirable Species / Reintroduce Natural Fire Frequency State 2 submodel, plant communities
2.1A - Fire Suppression / Decrease in Natural Hydroperiod 2.2A - Reduction or Removal of Undesirable Species / Reintroduce Natural Fire Frequency State 3 submodel, plant communities
3.1A - Absence of Fire 3.2A - Reintroduction of Fire State 5 submodel, plant communities
Communities 2 and 5 (additional pathways)
5.1A - Land Clearing Practices 5.2A - Habitat Restoration 5.2B - Pasture Preparation 5.2C - Agriculture Preparation 5.2D - Silviculture Preparation 5.3A - Land Clearing Practices 5.3B - Agriculture Preparation 5.3C - Silviculture Preparation 5.4A - Land Clearing Practices 5.4B - Silviculture Preparation 5.5A - Land Clearing Practices State 6 submodel, plant communities
6.1A - Urban Development 6.1B - Waste Accumulation 6.2A - Land Reclamation 6.2B - Industrial / Urban Development 6.2C - Waste Accumulation 6.3A - Land Reclamation State 1
Pine FlatwoodsPine Flatwoods are the reference state on these soils throughout the Florida peninsula. These are open canopy pine woodlands on flats and flatwoods landscape positions derived from marine deposits. The reference communities are dependent on microtopography, slight differences in hydroperiods and fire return intervals. These will often succeed or transition into different communities dependent on management or lack of management of the reference community, but is highly unlikely that the reference communities will succeed or transition into one another.
Characteristics and indicators. Pine flatwoods are characterized by an open overstory of pine trees with a dense understory of grasses and / or shrubs dependent on microtopography.
Resilience management. The main threats to these habitats include fire suppression and alteration of the natural hydroperiod. Fire is used in these communities to prevent woody species encroachment and buildup of fuels. Alteration of the natural hydroperiod of these areas may intensify the effects of species encroachment and fire intensity.
Dominant resource concerns
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Wind erosion
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Compaction
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Organic matter depletion
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Seasonal high water table
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Wildfire hazard from biomass accumulation
Community 1.1
Wet Flatwoods
Figure 11. Example of Wet Flatwoods grading into mesic flatwoods in the background. Microsite in the left middleground shows root mat support mesic composition of saw palmetto.
These are pine flatwoods found on micro-low positions, with depth to seasonal high-water tables range from 0 to 6 inches below the surface. The overstory is often identified as open, widely spaced pines, often slash pine (Pinus elliottii) or Florida slash pine (P. elliottii var densa). The understory is often identified as a dense cover of grasses and forbs. During the wet season, periphyton or other algal species may be present as a thin layer of ground cover between existing plants.
Resilience management. Maintenance of these communities is dependent on frequent fire intervals estimated at every 1 to 3 years. This frequent interval is enough to maintain the grassy understory and inhibit invasion by shrubs. The overstory pines are tolerant of light surface fires due to its thick bark and their seeds need the mineral soil and open sunlight that fires provides to germinate. Fires typically occur in the growing seasons (April to mid-August), and will often reduce the resilience of hardwood species, decrease shrub invasion, and promote flowing of desired herbaceous groundcover. Many factors including fire frequency, season of fire, soil moisture, groundwater levels, etc. will often influence the outcome of vegetative response to fire. Specific management plans should be made based off individual assessment of an area. A seasonal high-water table often seen at 0 to 6 inches often limits growth of shrubby and subcanopy species. Fires at too long of an interval (5 to 10 years) can lead to an increase in woody species cover and decline in grasses and forb cover, shifting this community to a fire suppressed flatwood. In these cases physical removal or mowing of woody vegetation as well as reintroducing a natural fire interval of every 1 to 3 years may be necessary to restore a suppressed area back, but may cause damage to soil structure and desired vegetation. Alteration of natural hydroperiods, whether directly or indirectly, may make these areas more vulnerable to undesirable woody species encroachment as well as invasive species.
Dominant plant species
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Florida slash pine (Pinus elliottii var. densa), tree
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slash pine (Pinus elliottii), tree
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cabbage palmetto (Sabal palmetto), tree
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pond cypress (Taxodium ascendens), tree
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wax myrtle (Morella cerifera), shrub
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saw palmetto (Serenoa repens), shrub
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blue maidencane (Amphicarpum purshii), grass
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toothache grass (Ctenium aromaticum), grass
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yelloweyed grass (Xyris), grass
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beaksedge (Rhynchospora), grass
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whitetop (Doellingeria), grass
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longleaf threeawn (Aristida palustris), grass
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bladderwort (Utricularia), other herbaceous
Community 1.2
Mesic FlatwoodsThese are pine flatwoods found on micro-high positions, with depth to seasonal high-water tables range from 6 to 18 inches below the surface. The overstory is often identified as open, widely spaced pines, often slash pine (Pinus elliottii) or Florida slash pine (P. elliottii var densa). The understory is often identified as a dense cover of shrubs, grasses, and forbs.
Resilience management. Maintenance of these communities is dependent on frequent fire intervals estimated at every 2 to 4 years. This frequent interval is enough to maintain the shrubby and grassy understory while creating suitable conditions for reproduction of several species. The overstory pines are tolerant of light surface fires due to its thick bark and their seeds need the mineral soil and open sunlight that fires provides to germinate. Fires typically occur in the growing seasons (April to mid-August), and will often reduce the resilience of hardwood species, decrease shrub invasion, and promote flowing of desired herbaceous groundcover. Wiregrass requires fire to flower, along with a number of other characteristic herbs, including, but not limited to, whitetop aster (<a class="species-link" href="https://plants.usda.gov/core/profile?symbol=OCRE2" target="_blank" title="Open in plants.usda.gov"><i>Oclemena reticulata</i></a>), many-flowered grass-pink, crowpoison (Stenanthium densum), and grassleaf goldenaster (<a class="species-link" href="https://plants.usda.gov/core/profile?symbol=PIOL" target="_blank" title="Open in plants.usda.gov"><i>Pityopsis oligantha</i></a>). Many factors including fire frequency, season of fire, soil moisture, groundwater levels, etc. will often influence the outcome of vegetative response to fire. Specific management plans should be made based off individual assessment of an area. Fires at too long of an interval (5 to 10 years) can lead to an increase in woody species cover and decline in grasses and forb cover, shifting this community to a fire suppressed flatwood. In these cases physical removal or mowing of woody vegetation as well as reintroducing a natural fire interval of every 2 to 4 years may be necessary to restore a suppressed area back, but may cause damage to soil structure and desired vegetation. Alteration of natural hydroperiod, whether directly or indirectly, may make these areas more vulnerable to undesirable woody species encroachment as well as invasive species.
Dominant plant species
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Florida slash pine (Pinus elliottii var. densa), tree
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slash pine (Pinus elliottii), tree
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sand pine (Pinus clausa), tree
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saw palmetto (Serenoa repens), shrub
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large gallberry (Ilex coriacea), shrub
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inkberry (Ilex glabra), shrub
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fetterbush lyonia (Lyonia lucida), shrub
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dwarf live oak (Quercus minima), shrub
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blueberry (Vaccinium), shrub
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longleaf threeawn (Aristida palustris), grass
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dropseed (Sporobolus), grass
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witchgrass (Panicum capillare), grass
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bluestem (Andropogon), grass
Community 1.3
Fire Suppressed FlatwoodsThis community describes a reference flatwoods community that has had fire excluded from its system long enough for fire suppressed shrubs to grow into the subcanopy and into the canopy. These areas will typically have the reference overstory of widely spaced pines: slash pine (Pinus elliottii) or Florida slash pine (P. elliottii var densa). The unburned area will allow for shrubs such as gallberry (Ilex glabra), coastalplain staggerbush (Lyonia fruticosa), wax myrtle (Morella cerifera), and fetterbush (Lyonia lucida) to grow in height and density, often shading the understory. Increased shading will decrease the biodiversity of herbaceous species found in the reference communities. Absence of fire will also allow for the growth of oaks (Quercus virginiana, Q. laurifolia) into the midcanopy and if fire is absent long enough, create a closed canopy forest.
Resilience management. This community is often seen as a transitional community between a reference community and a closed canopy oak - palm dominated forest. This community will vary slight based on the reference community, but common features include unburned flatwoods which allow for shrub growth into the sub- and mid-canopy. Restoration of a natural reference community often is dependent on the removal of the overgrown shrubby species and reintroducing the natural fire return interval consistent to that of the reference community. If fire remains absent from this community for long periods of time the shrubs and shrubby trees may mature and form a closed canopy forest dominated by oaks and shrubs devoid of fire with sparse to absent groundcover. Due to the absence of fire these areas will begin to accumulate large amounts of woody and herbaceous debris, increasing the fuel load and making the area more susceptible to catastrophic fires. A catastrophic fire may cause mass mortality of the overstory pines, creating an open prairies or grassland habitat after species recovery.
Pathway 1.1A
Community 1.1 to 1.2Wet flatwoods occur on slightly lower landscape positions (along the scale of inches) than mesic flatwoods, which allows for the accumulation of water during the rainy season, creating habitat suitable for hydrophytic grasses and sparse trees. Large root mats may create micro highs that allow for the establishment of few shrubs and saw palmettos. With changes in long term hydroperiods, the seasonal high water table becomes lowered allowing the encroachment of shrubs from the micro high areas into the lower areas, shifting the community. Increased fire return intervals of every 1 to 3 years also maintains high densities of grasses and excluding shrubs. Longer fire return interval allows for the establishment of shrub species before fire may come through and kill any new growth. The transition from a wet to mesic pine flatwoods involves the shifting of species composition from hydrophytic grasses as the dominant understory composition to a more densely shrub populated understory. Decreases in long term hydroperiod are ways this community begins to transition to a mesic flatwoods. Decrease of the fire return interval also allows for the establishment of shrubs and saw palmettos that are characteristic of mesic flatwoods.
Context dependence.These are slight elevation differences that can exist within the natural range of variability within this site context.
Pathway 1.1B
Community 1.1 to 1.3Disturbances to the natural maintenance of these communities may allow for the growth of undesirable woody and shrubby species into the system. This transition is often seen through fire suppression when fire is estimated to be absent from the system for 5 to 10 years. This transition may also be seen via decrease in the natural hydroperiod of the area, whether directly (canal ditching) or indirectly (lowering of surrounding lands water table). The removal of these stressors may create an opportunity for undesirable woody and shrubby species and structure into the reference community.
Pathway 1.2A
Community 1.2 to 1.1Mesic flatwoods occur on slightly higher landscape positions (along the scale of inches) than wet flatwoods, which allows for the establishment of shrubs characterized by saw palmettos as well as an open canopy of tall pines. With increases in long term hydroperiods the seasonal high water table becomes higher allowing for water to be present in this community for a longer period of time each year (up to 60 days). This increase in long term hydroperiod over time will oversaturate the shrubs and kill them, allowing the establishment of hydrophytic grasses to become dominant. Shorter fire return intervals to every 1 to 3 years will shift the plant community to high densities of grasses and excluding shrub species that depend on longer fire return intervals of every 2 to 4 years to become established. The transition from a mesic to wet pine flatwoods involves the shifting of species composition from a dense, low ground layer of shrubs grasses and forbs to hydrophytic grasses as the dominant understory composition. Increases in long term hydroperiods are ways this community begins to transition to a wet flatwoods. Increase of the fire return interval also allows for the establishment of hydrophytic grasses that are characteristic of wet flatwoods.
Context dependence.These are slight elevation differences that can exist within the natural range of variability within this site context.
Pathway 1.2B
Community 1.2 to 1.3Disturbances to the natural maintenance of these communities may allow for the growth of undesirable woody and shrubby species into the system. This transition is often seen through fire suppression when fire is estimated to be absent from the system for 5 to 10 years. This transition may also be seen via decrease in the natural hydroperiod of the area, whether directly (canal ditching) or indirectly (lowering of water table). The removal of these stressors may create an opportunity for undesirable woody and shrubby species and structure into the reference community.
Pathway 1.3A
Community 1.3 to 1.1This restoration to the natural reference community may be achieved by the reduction and removal of the undesirable woody or shrubby species and reintroducing the natural fire return interval back into the reference community. Reduction and removal of undesirable species may include methods of mechanical (mowing, cutting), chemical (herbicides), or biological removal. Some methods of removal may create soil disturbances which makes the area more susceptible to invasion of exotic species into this system. Fire return intervals of every 1 to 3 years should be reintroduced after the reduction and removal of the undesired species to prevent excess fuel loads in the system to prevent catastrophic fires.
Pathway 1.3B
Community 1.3 to 1.2This restoration to the natural reference community may be achieved by the reduction and removal of the undesirable woody or shrubby species and reintroducing the natural fire return interval back into the reference community. Reduction and removal of undesirable species may include methods of mechanical (mowing, cutting), chemical (herbicides), or biological removal. Some methods of removal may create soil disturbances which makes the area more susceptible to invasion of exotic species into this system. Fire return intervals of every 2 to 4 years should be reintroduced after the reduction and removal of the undesired species to prevent excess fuel loads in the system to prevent catastrophic fires.
State 2
PrairiesPrairies are the altered state of pine flatwoods in areas of overstory mortality. Individual communities are dependent on the reference community and will reflect similar to the same microtopography, hydroperiods, and fire return intervals. These communities can often be identified as having similar characteristics to its reference flatwoods state, with the absence of the living overstory species. Standing dead pines or burned stump holes may be present and may be used to identify this state. Overstory mortality may be the result of a catastrophic fire which killed the overstory trees or by biological processes such as fusiform rust caused by fungi.
Characteristics and indicators. Indicators of these communities is dependent on the reference state it originates from but will both be generally treeless landscapes with dense groundcover of grasses and / or shrubs.
Resilience management. This state is maintained by stressors at the beginning of the rainy season, where natural fire return intervals of every 1 to 2 years as well as the maintenance of a high seasonal high water table.
Dominant resource concerns
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Wind erosion
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Compaction
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Organic matter depletion
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Seasonal high water table
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Wildfire hazard from biomass accumulation
Community 2.1
Palmetto PrairiesPalmetto prairies are the altered prairies community of the mesic flatwoods reference community. It is similar in species composition to its reference community with the absence of overstory pines. These habitats are often important for many animal species as habitat and forage including burrowing owls, gopher tortoises, and northern bobwhites.
Resilience management. Maintenance of these communities is dependent on frequent fire intervals estimated at every 1 to 2 years. This frequent interval is enough to maintain the shrubby and grassy understory while creating suitable conditions for reproduction of several species and prevent the reintroduction of pines into the overstory. Fires typically occur in the growing seasons (April to mid-August), and will often reduce the resilience of hardwood species, decrease shrub invasion, and promote flowing of desired herbaceous groundcover. Wiregrass requires fire to flower, along with a number of other characteristic herbs, including, but not limited to, whitetop aster (<a class="species-link" href="https://plants.usda.gov/core/profile?symbol=OCRE2" target="_blank" title="Open in plants.usda.gov"><i>Oclemena reticulata</i></a>), many-flowered grass-pink, crowpoison (Stenanthium densum), and grassleaf goldenaster (<a class="species-link" href="https://plants.usda.gov/core/profile?symbol=PIOL" target="_blank" title="Open in plants.usda.gov"><i>Pityopsis oligantha</i></a>). Many factors including fire frequency, season of fire, soil moisture, groundwater levels, etc. will often influence the outcome of vegetative response to fire. Specific management plans should be made based off individual assessment of an area. Fires at too long of an interval (5 to 10 years) can lead to an increase in woody species cover and decline in grasses and forb cover, shifting this community to a fire suppressed prairie. In these cases physical removal or mowing of woody vegetation as well as reintroducing a natural fire interval of every 1 to 2 years may be necessary to restore a suppressed area back, but may cause damage to soil structure and desired vegetation. Alteration of natural hydroperiods, whether directly or indirectly, may make these areas more vulnerable to undesirable woody species encroachment as well as invasive species. Absence of fire for a short period may allow for pines to become reestablished, and transition back to a mesic flatwoods over time if fire frequency is decreased.
Dominant plant species
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saw palmetto (Serenoa repens), shrub
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dwarf live oak (Quercus minima), shrub
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inkberry (Ilex glabra), shrub
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fetterbush lyonia (Lyonia lucida), shrub
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wax myrtle (Morella cerifera), shrub
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pineland threeawn (Aristida stricta), grass
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bottlebrush threeawn (Aristida spiciformis), grass
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rosette grass (Dichanthelium), grass
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broomsedge bluestem (Andropogon virginicus), grass
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lopsided Indiangrass (Sorghastrum secundum), grass
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narrowleaf silkgrass (Pityopsis graminifolia), other herbaceous
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polygala (Polygala), other herbaceous
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meadowbeauty (Rhexia), other herbaceous
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wild pennyroyal (Piloblephis rigida), other herbaceous
Community 2.2
Fire Suppressed PrairieThis community describes a prairie community that has had stressors excluded from its system long enough for suppressed shrubs to grow into the subcanopy and pines encroach into the canopy. These areas will typically be absent of overstory pine species common to the flatwoods state. These areas will allow for shrubs such as gallberry (Ilex glabra), coastalplain staggerbush (Lyonia fruticosa), saw palmetto (Serenoa repens), wax myrtle (Morella cerifera), and fetterbush (Lyonia lucida) to grow in height and density, often shading the understory. Increased shading will decrease the biodiversity of herbaceous species found in the reference communities. Stressors include fire suppression from a prairie system or drawdown of the seasonal high-water table. Drawdown of the water table is often seen indirectly through canal creations of adjacent habitats, lowering the water table for a whole area. Absence of fire will also allow for the growth of dwarf oaks, including live oak (Quercus virginiana) into the midcanopy and if fire is absent long enough, create a closed canopy forest.
Resilience management. This community is often seen as a transitional community between a reference prairie community and a closed canopy oak dominated forest. This community will vary slight based on the reference community, but common features include unburned or hydrologically suppressed prairies which allow for shrub growth into the sub- and mid-canopy. Restoration of a natural reference community often is dependent on the removal of the overgrown shrubby species and reintroducing the natural stressors consistent to that of the reference community. If fire remains absent from this community for long periods of time (greater than 20 years) the shrubs and dwarf oaks may mature and form a closed canopy forest dominated by oaks, palms, and shrubs devoid of fire with sparse to absent groundcover. Due to the absence of fire these areas will begin to accumulate large amounts of woody and herbaceous debris, increasing the fuel load and making the area more susceptible to catastrophic fires. Restoration of the hydroperiod of an area, if possible, may include filling in drainage ditches and canals to restore the seasonal high-water table.
Dominant plant species
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Florida slash pine (Pinus elliottii var. densa), shrub
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slash pine (Pinus elliottii), shrub
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saw palmetto (Serenoa repens), shrub
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inkberry (Ilex glabra), shrub
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fetterbush lyonia (Lyonia lucida), shrub
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wax myrtle (Morella cerifera), shrub
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live oak (Quercus virginiana), shrub
Pathway 2.1A
Community 2.1 to 2.2Disturbances to the natural maintenance of these communities may allow for the growth of undesirable woody and shrubby species into the system. This transition is often seen through fire suppression when fire is estimated to be absent from the system for 5 to 10 years. This transition may also be seen via decrease in the natural hydroperiod of the area, whether directly (canal ditching) or indirectly (lowering of water table). The removal of these stressors may create an opportunity for undesirable woody and shrubby species and structure into the reference community.
Pathway 2.2A
Community 2.2 to 2.1This restoration to the natural reference community may be achieved by the reduction and removal of the undesirable woody or shrubby species and reintroducing the natural fire return interval back into the reference community. Reduction and removal of undesirable species may include methods of mechanical (mowing, cutting), chemical (herbicides), or biological removal. Some methods of removal may create soil disturbances which makes the area more susceptible to invasion of exotic species into this system. Fire return intervals of every 1 to 2 years should be reintroduced after the reduction and removal of the undesired species to prevent excess fuel loads in the system to prevent catastrophic fires.
State 3
Pine - Oak - Cabbage Palm ForestsThis state describes a change in fire frequency that will change the community composition and structure. This includes two communities featuring cabbage palms and oak species becoming dominant in the subcanopy with pines. This will often shift the canopy from being open and sparse to closed and dense with hardwood and palms.
Characteristics and indicators. This is characterized by the presence of a low, closed, dense canopy dominated by hardwood and palm species on poorly drained sandy soils in flatwoods landscape positions. There will often be an emergent relict overstory of pine coming out of the oak canopy. Species which close the canopy in the absence of fire include oaks, cabbage palms, bays, and other subtropical species.
Resilience management. To return to a pine flatwoods, removal of the closed canopy must happen. This can occur by selective logging of oak species and other canopy species. Fire must also be reintroduced into the system, and will often remove the layer of leaf litter accumulated by the mesic conditions created by the closed canopy.
Dominant plant species
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cabbage palmetto (Sabal palmetto), tree
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Florida slash pine (Pinus elliottii var. densa), tree
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slash pine (Pinus elliottii), tree
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sand pine (Pinus clausa), tree
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saw palmetto (Serenoa repens), shrub
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longleaf threeawn (Aristida palustris), grass
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blue maidencane (Amphicarpum purshii), grass
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yelloweyed grass (Xyris), grass
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beaksedge (Rhynchospora), grass
Dominant resource concerns
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Wind erosion
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Compaction
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Organic matter depletion
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Seasonal high water table
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Plant productivity and health
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Plant structure and composition
Community 3.1
Cabbage Palm - Pine FlatwoodsThis state is characterized by cabbage palm species in the sub canopy or shrub layer, under an open layer of pine species. Natural fire return intervals are similar to wet flatwoods, along a shorter interval of every 1 to 2 years. Cabbage palms have a very slow growth cycle and can spend 10 to 15 years or more in a grass-like state before the trunk will grow. The grass-like state is dependent and tolerant on fire for growth and after the trunk becomes visible grows at slow rates up to 6 inches per year. This community is maintained by fire, and in the absence of fire will succeed to the final subclimax community within the pine flatwoods and palmetto prairie ecosite of mixed hardwood cabbage palm hammock.
Resilience management. This state can be maintained by regular fire intervals of every 1 to 2 years that prevents the establishment of shrubby species. Mechanical removal from hand removal or roller chopping may shift the community back towards a wet pine flatwood community, with an increased chance of encroachment of invasive species.
Community 3.2
Mixed Hardwood - Cabbage Palm HammockThis community is seen as the final subclimax community within the pine flatwoods and palmetto prairie eco site. It is created when fire has been excluded from the system for long periods of time. Time estimates of succession are believed to be 25 years or more without fire to have a fully formed hardwood-dominated hammock. Flatwoods that have hardwood shrubs growing in the midstory are close to this transition.
Resilience management. These are formed when fire has been excluded from the system for long periods of time. As shrubs grow in the midstory, the ground layer becomes more shaded and retains higher moisture conditions, helping exclude fire from the system. If fire is reintroduced to the system during periods of drought, large fuel loads in the understory may cause catastrophic fires which transition the community back to palmetto prairies or cabbage palm dominated flatwoods.
Pathway 3.1A
Community 3.1 to 3.2This is driven by the absence of fire from the system which allows for hardwood species growth over time. This shades the understory creating more moist conditions and helping further exclude fire from the system.
Context dependence.Estimates of fire exclusion is to be 25 years or more. Flatwoods dominated by shrubs in the midstory are close to this transition.
Pathway 3.2A
Community 3.2 to 3.1This is driven when fire is reintroduced into the system and kills the hardwood fire intolerant species. Depending on the amount of understory litter and hardwood growth, a catastrophic fire may transition the community into a palmetto prairie (if canopy fire).
State 4
Invasive Non-Native CommunityThis state consists of Florida Department of Agriculture and Consumer Services (FDACS) Non-Native Category 1 Species list . More information on these species list can be found:
https://www.fdacs.gov/content/download/63140/file/Florida%E2%80%99s_Pest_Plants.pdf
or by contacting the UF / IFAS Center for Aquatic and Invasive Plants (http://plants.ifas.ufl.edu/),
the UF / IFAS Assessment of Non-native Plants in Florida's Natural Areas (https://assessment.ifas.ufl.edu/),
or the FWC Invasive Plant Management Section (http://myfwc.com/wildlifehabitats/invasive-plants/).
This community will not represent every possibility of invasive species but rather the most common in these areas.
Characteristics and indicators. Non-native species include species that exist outside of Florida's natural range and introduced to the state by people, weather, or any other means.
Resilience management. This state can be found as a part of any other state and can completely destroy the native habitat if not properly managed. Restoration to natural communities after exotic invasion include practices such as mechanical, biological, and chemical removals.
Dominant resource concerns
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Subsidence
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Concentration of salts or other chemicals
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Nutrients transported to surface water
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Plant productivity and health
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Plant structure and composition
State 5
Managed Resource AreasThe following communities comprise the major land uses in the United States and the land uses receiving the majority of the conservation treatment that address soil, water, air, plant, and animal resources within the USDA.
Characteristics and indicators. These land uses consist of areas that are not completely naturalized (i.e. native habitat) but are not completely altered by anthropogenic means.
Dominant resource concerns
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Sheet and rill erosion
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Wind erosion
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Subsidence
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Organic matter depletion
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Concentration of salts or other chemicals
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Seasonal high water table
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Nutrients transported to surface water
Community 5.1
RangelandRangelands are described as lands on which the indigenous vegetation is predominately grasses, grass-like plants, forbs, and possibly shrubs or dispersed trees. Existing plant communities can include both native and introduced plants. Primary export from Florida ranges are cattle and have been present in the state since their first introduction by Spanish explorers in 1521. This is the reference community for this state because it requires very little alterations to the landscape for grazing species.
Rangelands provide a diversity of ecosystems and also provide a diverse and significant production of economic benefits and ecosystem goods and services. Livestock production along with sustainable wildlife populations provide for the major direct economic benefits, but also tourism, recreational uses, minerals/energy production, renewable energy, and other natural resource uses can be very significant. Vital ecosystem contributions include clean water, clean air, fish/wildlife habitat, as well as intangible considerations such as historical, cultural, aesthetic and spiritual values.
Resilience management. Grazing, by both domestic livestock and wildlife, is the most common ecological management process, with fire and weather extremes also being significant ecological factors. For information regarding specific cattle grazing techniques please contact your local NRCS office.
Community 5.2
Open Transitional Managed CommunitiesThis is an area that is managed to maintain open land before shifting to another community. These communities are often used as transitional periods from one practice to another and could lead to an abandoned / fallow field.
Community 5.3
Improved PasturePasture is a land use type having vegetation cover comprised primarily of introduced or enhanced native forage species that is used for livestock grazing. Pasture vegetation can consist of grasses, legumes, other forbs, shrubs or a mixture. The majority of these forages are introduced, having originally come from areas in other states or continents. Most are now naturalized and are vital components of pasture based grazing systems.
Pasture lands provide many benefits other than forage for livestock. Wildlife use pasture as shelter and for food sources. Well managed pasture captures rainwater that is slowly infiltrated into the soil which helps recharge groundwater. Many small pasture livestock operations are near urban areas providing vistas for everyone to enjoy. Pasture is the basis of any livestock operation that is truly sustainable. It is especially important as livestock grazers continues to experience extraordinarily high fuel and other input costs.
Resilience management. Pastures receive periodic renovation and cultural treatments such as tillage, fertilization, mowing, weed control, and may be irrigated. For more information regarding specific pasture management please contact your local NRCS office.
Community 5.4
AgricultureThe agriculture industry includes cultivated crops, aquaculture, and apiculture. Cultivated cropland includes areas used for the production of adapted crops for harvest. These areas comprises land in row crops or close-grown crops that are in a rotation with row or close-grown crops. Primary export from Florida consists of fruits, greenhouse and nursery products, sugar cane, and the signature export of citrus. Aquaculture includes the cultivation and maintenance of aquatic plants, aquatic reptiles, crustaceans, food/ ornamental fish, shellfish, and other miscellaneous species for harvesting. Apiculture includes the maintenance of honeybees and hives to provide beeswax, honey/ other edible bee products, crop pollination services, and sales of bees to other beekeepers. These areas have been modified resulting in land clearing practices and hydrologic management to fit the growers needs.
Resilience management. Major natural resource concerns facing agricultural lands include: (1) erosion by wind and water, (2) maintaining and enhancing soil quality, (3) water quality from nutrient and pesticides runoff and leaching, and (4) managing the quantity of water available for irrigation. For more specific information regarding cropland please contact your local NRCS office.
Community 5.5
SilvicultureSilviculture is land used in controlling the establishment, growth, composition, health, and quality of forests and woodlands to meet the diverse needs and values of landowners and society such as wildlife habitat, timber, water resources, restoration, and recreation on a sustainable basis. These are forestry practices that include thinning, harvesting, planting, pruning, prescribed burning and site preparation, for managed goals such as wildlife habitat creation or harvesting. Many managed silvicultural lands in Florida include tree plantations for growth of tropical ornamental species such as palms; and lumber, pulp, and paper species such as slash pine, longleaf pine, cypress, and eucalyptus.
This community also include management practices of agroforestry, the intentional mixing of trees and shrubs into crop and/or animal production systems to create environmental, economic and social benefits. This is included in this community and not any other state because the primary management is for tree species. This may include practices such as riparian forest buffers, windbreaks, forest farming, silvopasture, and alley cropping.
Resilience management. Management of silvicultural lands require specific prescriptions based on the management goals for the stand, and may include thinning, harvesting, planting, pruning, prescribed burning and site preparation. For more information regarding specific management for silviculture practices please contact your local NRCS office.
Pathway 5.1A
Community 5.1 to 5.2This pathway is driven by land clearing practices that consists of removing the existing vegetation from the habitat and altering the habitat to prepare for modified land use.
Pathway 5.2A
Community 5.2 to 5.1This pathway is driven by the restoration of the native habitat for the use of rangeland. This includes restoration of both the hydrology and landscape in advance of replanting native species. This is a time-consuming process and often results in second-hand community structure. Once restored to a natural capacity the introduction of grazing species to the system creates a managed rangeland.
Pathway 5.2B
Community 5.2 to 5.3This pathway is driven by preparing the land for pasteurization. This includes the planting of vegetation consisting of grasses, legumes, other forbs, shrubs or a mixture that will provide preferred forage for managed grazing species.
Pathway 5.2C
Community 5.2 to 5.4This pathway is driven by the preparation of land for agricultural uses. This change is dependent on the type of agricultural community is being created, but often depends on the growing, maintenance, and cultivation of an agricultural product for consumers. This community may require modification to the land to fit the hydrologic requirement of the growing crop.
Pathway 5.2D
Community 5.2 to 5.5This pathway is driven by the preparation of the land for silvicultural purposes. This change is dependent on the type of silvicultural product being cultivated, as many different practices require different growth requirement.
Pathway 5.3A
Community 5.3 to 5.2This pathway is driven by land clearing practices that consists of removing the existing vegetation from the habitat and altering the habitat to prepare for modified land use.
Pathway 5.3B
Community 5.3 to 5.4This pathway is driven by the preparation of land for agricultural uses. This change is dependent on the type of agricultural community is being created, but often depends on the growing, maintenance, and cultivation of an agricultural product for consumers. This community may require modification to the land to fit the hydrologic requirement of the growing crop.
Pathway 5.3C
Community 5.3 to 5.5This pathway is driven by the preparation of the land for silvicultural purposes. This change is dependent on the type of silvicultural product being cultivated, as many different practices require different growth requirements.
Pathway 5.4A
Community 5.4 to 5.2This pathway is driven by land clearing practices that consists of removing the existing vegetation from the habitat and altering the habitat to prepare for modified land use.
Pathway 5.4B
Community 5.4 to 5.5This pathway is driven by the preparation of the land for silvicultural purposes. This change is dependent on the type of silvicultural product being cultivated, as many different practices require different growth requirements.
Pathway 5.5A
Community 5.5 to 5.2This pathway is driven by land clearing practices that consists of removing the existing vegetation from the habitat and altering the habitat to prepare for modified land use.
State 6
Human Altered & Human Transported AreasThese areas include soils that were intentionally and substantially modified by humans for an intended purpose, commonly for terraced agriculture, building support, mining, transportation, and commerce. The alteration is of sufficient magnitude to result in the introduction of a new parent material (human-transported material) or a profound change in the previously existing parent material (human-altered material). They do not include soils modified through standard agricultural practices or formed soils with unintended wind and water erosion. When a soil is on or above an anthropogenic landform or microfeature, it can be definitely be associated with human activity and is assigned to a unique taxa, usually found as an "Urban land complex" within that communities natural soil properties (e.g., Grande Oaks fine sand- Urban land complex, 0-2% slopes).
Characteristics and indicators. Evidence of these areas include soils with manufactured items (e.g. artifacts) present in the profile, human altered-materials (e.g., deeply excavated or deeply plowed soil) or human-transported material (e.g., fill), and position on or above anthropogenic landforms (e.g., flood-control levees) and microfeatures (e.g., drainage ditches). Detailed criteria regarding the identification of anthropogenic (artificial) landforms, human-altered materials, and human-transported material are in the "Keys to Soil Taxonomy" (Soil Survey Staff, 2014).
Dominant resource concerns
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Compaction
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Ponding and flooding
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Seasonal high water table
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Emissions of greenhouse gases (GHGs)
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Objectionable odors
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Plant productivity and health
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Plant structure and composition
Community 6.1
Reclaimed AreasReclaimed areas are areas that have been modified through anthropogenic means that are restored to a natural or second-hand natural community. Areas that can be reclaimed are any intensely urbanized areas, and may be required to be reclaimed after urban use (e.g., active mines must be reclaimed). Examples of reclaimed lands may be shut down phosphate mining operations, superfund sites, or brownfields. These practices include the identification, removal, and stockpiling soil materials before altering the land, and revegetation and replacement of soil materials after altering the land. This also applies to nearby urban areas that have been adversely affected by the anthropogenic activities.
Community 6.2
UrbanThis urban community consists of development for human use. Urban areas include a variety of land uses, e.g., inner city or urban core, industrial and residential areas, cemeteries, parks, and other open spaces; the overall function which may benefit the quality of human life. These often form an urban soil mosaic, where the natural landscape has been fragmented into parcels with distinctive disturbance and management regimes and, as a result, distinctive characteristic soil properties.
Within this community there are three different levels of urbanization, based off population dynamics, residential density, and intensity of development. These are labeled as low-intensity, medium-intensity, and high-intensity urban areas, which can eventually be split apart into its own separate state. Low-intensity urban areas may consist of single dwelling homes with little impact on the surrounding community which still somewhat represents the natural community (e.g., represents natural landscape, hydrology, and vegetation) , other examples of this are urban parks, cemeteries, or campgrounds with little urban development. Medium-intensity urban areas consist of larger urban dwellings with some natural features, but have been modified to meet urban needs (e.g., towns). High-intensity urban areas are areas of heavily modified areas with complete alterations of the natural landscape, hydrology, and vegetation to support a very large population, which once constructed is permanently altered (e.g., metropolis areas).Community 6.3
Non-Reclaimed AreasNon-reclaimed areas are areas that have been modified through anthropogenic means that are unable to be restored to a natural or second-hand natural community. Areas that cannot be reclaimed are areas under active mining status or mined areas before the Phosphate Land Reclamation Act in 1975, which leaves shut down operations alone. These areas also include fallow mines that have been flooded and are now permanent bodies of water.
Community 6.4
LandfillsThis is an anthropogenic site for the disposal of waste material. It includes manufactured layers (artificial, root limiting layer below the soil surface) that are representative of human altered and human transported sites. These layers are often alternative between natural fill material and geotextile liners, asphalt, concrete, rubber or plastic that are built up and can rise above the surrounding landscape by 30 meters or more often impeding water, gas, or roots from moving through the profile.
Pathway 6.1A
Community 6.1 to 6.2This shift in communities is driven by clearing and developing the land for the desired community.
Pathway 6.1B
Community 6.1 to 6.4This transition is driven by the deposition of manufactured layers along with anthropogenic waste which is consistently built upon.
Pathway 6.2A
Community 6.2 to 6.1This transition is driven by the revegetation, reestablished hydrology, and replacement of displaced soil materials after altering the land.
Pathway 6.2B
Community 6.2 to 6.3This transition is driven from heavy industrial or urban development which causes the land to become non-reclaimable. This transition is rare due to the many environmental laws and regulations that must be followed when developing.
Pathway 6.2C
Community 6.2 to 6.4This transition is driven by the deposition of manufactured layers along with anthropogenic waste which is consistently built upon.
Pathway 6.3A
Community 6.3 to 6.1This transition is driven by the revegetation, reestablished hydrology, and replacement of displaced soil materials after altering the land.
Transition T1A
State 1 to 2Pine Flatwoods may transition to palmetto prairies under specific conditions, which once a transition occurs must be maintained to prevent the shift back to pine flatwoods. Unmaintained pine flatwoods may build high fuel loads that regular fire return intervals would normally prevent from establishing, which can allow the next fire to climb ladder fuels such as vines into the canopy. Canopy fires spread from tree to tree independent of the ground fire, which after consuming the live needles as its fuel, may kill the tree, leaving either the snag behind or burning down to the stump hole. Reestablishment of the natural fire return interval after this canopy fire may prevent native pines from becoming established, giving the appearance of palmetto prairies. Logging may also give the appearance by the removal of overstory pine species.
Constraints to recovery.Reestablished fire return intervals into the system (every 1 to 2 years) may prevent this new palmetto prairie habitat from shifting back into the pine flatwoods state by killing seedlings before they can become established.
Context dependence.Normal fire return intervals for pine flatwoods vary on the type of vegetation and hydroperiod of the system, but range from 3 to 15 years, with longer intervals allowing more shrubs and shorter intervals allowing more grasses. Catastrophic canopy fires may occur at any point, but usually happen when there is a high fuel load after multiple years of no burning. Palmetto prairies have normal fire return intervals every 1 to 2 years, which prevents the establishment of pine species.
Transition T1B
State 1 to 3This mechanism which drives the transition from pine flatwoods to an altered hardwood hammock is driven by a change in fire frequency. Removal of fire from the system, or its long term absence (>25 yrs) can allow the growth of understory species that were once limited by fire.
Constraints to recovery.Removal of midstory and newly entered canopy species would need to be removed, and desired shrub and tree density would need to be restored. Fire would need to be reintroduced into the system as well.
Transition T1C
State 1 to 4The invasion of non-native or exotic species can be driven by a multitude of different environmental factors such as changes in natural hydroperiods or in fire regimes. Typically once a change in one of the two factors mentioned above occurs, non-native or exotic invasive species become established and begin to compete with native species for habitat and nutrients.
Constraints to recovery.Recovery from non-native or exotic invasive species may be difficult due to many adaptations which allow them to outcompete and survive in altered conditions. Localized knowledge for each species must be known for best removal of it without harming the native environment, and often different treatments must be applied over one given area.
Context dependence.Growth of non-native and exotic invasive species can be rapid following a change in a natural stressor such as fire frequency or natural hydroperiods which might have once kept the invasive species at bay.
Transition T1D
State 1 to 5Modify the land for the desired land use. This may include the establishment of grazing species or the modification of land for the cultivation of crops of other desired products.
Transition T1E
State 1 to 6This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Transition T2A
State 2 to 1Increasing the time between fire return intervals from 1 to 2 years towards every 2 to 4 years, as seen in mesic pine flatwoods, can assist in the reestablishment of pine species. Similar understory species will be present in both palmetto prairies and mesic pine flatwoods. Decreasing the long term hydroperiod of the surrounding area through ditching or drainage might also allow the reestablishment of pine species in palmetto prairies, but makes the area more vulnerable to invasive species encroachment.
Context dependence.Palmetto prairies exclude pine species by high fire return intervals of every 1 to 2 years in at that start of the growing season as well as a relatively high seasonal high water table. The combination of both stress from water and fire exclude pine species, but allow for the establishment of understory species similar to a mesic pine flatwoods. Because these communities occur in similar landscapes and often form as intermixed communities, decreases in long term hydroperiods can allow for the encroachment of pine species from the surrounding habitats into the palmetto prairie. Increases in the time between fires may also allow for establishment of pine species into the area, shifting the community from a palmetto prairie to a mesic pine flatwood.
Transition T2B
State 2 to 3This mechanism which drives the transition from palmetto prairie to cabbage palm flatwoods depends on a change in fire frequency. Increases in fire return intervals to every 1 to 2 years may prevent pine seedlings from germinating while allowing fire loving cabbage palm to thrive. Whereas decreases in fire return intervals may allow for the encroachment of species such as cabbage palm and other hardwood species to become established. Logging of overstory pines may also cause this shift if a seedbank of cabbage palms are present, allowing them to become established.
Context dependence.Cabbage palms are very slow growing trees and spend the first 10 to 15 years or more within a grass-like state, making this transition towards a fully established state a long process (decadal scale).
Transition T2C
State 2 to 4The invasion of non-native or exotic species can be driven by a multitude of different environmental factors such as changes in natural hydroperiods or in fire regimes. Typically once a change in one of the two factors mentioned above occurs, non-native or exotic invasive species become established and begin to compete with native species for habitat and nutrients.
Constraints to recovery.Recovery from non-native or exotic invasive species may be difficult due to many adaptations which allow them to outcompete and survive in altered conditions. Localized knowledge for each species must be known for best removal of it without harming the native environment, and often different treatments must be applied over one given area.
Context dependence.Growth of non-native and exotic invasive species can be rapid following a change in a natural stressor such as fire frequency or natural hydroperiods which might have once kept the invasive species at bay.
Transition T2C
State 2 to 5Modify the land for the desired land use. This may include the establishment of grazing species or the modification of land for the cultivation of crops of other desired products.
Transition T2D
State 2 to 6This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Transition T3A
State 3 to 1To transition this state towards a more traditional pine flatwood community, mechanical or chemical removal is required to remove the cabbage palm trees. Because these sub canopy trees are fire dependent and fire tolerant, regular use of prescribed fire is ineffective. Increases in hydrology can also be seen as ineffective because they are tolerant of high water tables and can be seen in standing water, increasing hydrology can destroy the whole community. Mechanical removal such as roller chopping or cutting the trees is an effect way of removing them from the habitat and transitioning back to a pine flatwoods.
Constraints to recovery.Cabbage palm trees spend a long time in a grass-like state which can be difficult to effectively remove from the system unless dug out completely. This is a costly process, whereas waiting for the trunk to become present is also very time consuming.
Context dependence.Mechanical Removal
Transition T3B
State 3 to 2This is driven by either the mechanical/ chemical removal of species and / or the reintroduction of fire into the system. As time passes and the area is left unburned, hardwood species may begin to grow and create a build-up of leaf litter which if ignited can cause canopy fires killing the hardwood tree species. This would drive the vegetative community back to a palmetto prairie state.
Context dependence.Cabbage palm trees spend a long time in a grass-like state which can be difficult to effectively remove from the system unless dug out completely. This is a costly process, whereas waiting for the trunk to become present is also very time consuming.
Transition T3C
State 3 to 4The invasion of non-native or exotic species can be driven by a multitude of different environmental factors such as changes in natural hydroperiods or in fire regimes. Typically once a change in one of the two factors mentioned above occurs, non-native or exotic invasive species become established and begin to compete with native species for habitat and nutrients.
Constraints to recovery.Recovery from non-native or exotic invasive species may be difficult due to many adaptations which allow them to outcompete and survive in altered conditions. Localized knowledge for each species must be known for best removal of it without harming the native environment, and often different treatments must be applied over one given area.
Context dependence.Growth of non-native and exotic invasive species can be rapid following a change in a natural stressor such as fire frequency or natural hydroperiods which might have once kept the invasive species at bay.
Transition T3D
State 3 to 5Modify the land for the desired land use. This may include the establishment of grazing species or the modification of land for the cultivation of crops of other desired products.
Transition T3E
State 3 to 6This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Restoration pathway R4A
State 4 to 1Mechanical, biological, and chemical removal strategies include removing the non-native and exotic invasive species through various mechanisms. Localized knowledge for individual non-native or exotic invasive species is needed for specific management. Sometimes introduction of fire regimes may prevent or stop the growth of non-native or exotic invasive species, but many species are fire tolerant. Mechanical removal might include roller chopping, harvesting, or cutting and removal of invasive species. Chemical removal might include aerial dispersal from planes, or basal bark injection treatments.
Context dependence.Mechanical, biological, and chemical removal of non-native and exotic invasive species is a time dependent process, with both removal types taking long times to be considered effective.
Restoration pathway R4B
State 4 to 2Mechanical, biological, and chemical removal strategies include removing the non-native and exotic invasive species through various mechanisms. Localized knowledge for individual non-native or exotic invasive species is needed for specific management. Sometimes introduction of fire regimes may prevent or stop the growth of non-native or exotic invasive species, but many species are fire tolerant. Mechanical removal might include roller chopping, harvesting, or cutting and removal of invasive species. Chemical removal might include aerial dispersal from planes, or basal bark injection treatments.
Context dependence.Mechanical, biological, and chemical removal of non-native and exotic invasive species is a time dependent process, with both removal types taking long times to be considered effective.
Restoration pathway R4C
State 4 to 3Mechanical, biological, and chemical removal strategies include removing the non-native and exotic invasive species through various mechanisms. Localized knowledge for individual non-native or exotic invasive species is needed for specific management. Sometimes introduction of fire regimes may prevent or stop the growth of non-native or exotic invasive species, but many species are fire tolerant. Mechanical removal might include roller chopping, harvesting, or cutting and removal of invasive species. Chemical removal might include aerial dispersal from planes, or basal bark injection treatments.
Context dependence.Mechanical, biological, and chemical removal of non-native and exotic invasive species is a time dependent process, with both removal types taking long times to be considered effective.
Restoration pathway R4D
State 4 to 5Mechanical, biological, and chemical removal strategies include removing the non-native and exotic invasive species through various mechanisms. Localized knowledge for individual non-native or exotic invasive species is needed for specific management. Sometimes introduction of fire regimes may prevent or stop the growth of non-native or exotic invasive species, but many species are fire tolerant. Mechanical removal might include roller chopping, harvesting, or cutting and removal of invasive species. Chemical removal might include aerial dispersal from planes, or basal bark injection treatments.
Context dependence.Mechanical, biological, and chemical removal of non-native and exotic invasive species is a time dependent process, with both removal types taking long times to be considered effective.
Transition T4A
State 4 to 6This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Restoration pathway R5A
State 5 to 1These practices include the restoration of both the natural hydroperiods and landscape in advance of revegetating the area (if needed).
Restoration pathway R5B
State 5 to 2These practices include the restoration of both the natural hydroperiods and landscape in advance of revegetating the area (if needed).
Restoration pathway R5C
State 5 to 3These practices include the restoration of both the natural hydroperiods and landscape in advance of revegetating the area (if needed).
Transition T5A
State 5 to 4The invasion of non-native or exotic species can be driven by a multitude of different environmental factors such as changes in natural hydroperiods or in fire regimes. Typically once a change in one of the two factors mentioned above occurs, non-native or exotic invasive species become established and begin to compete with native species for habitat and nutrients.
Context dependence.Recovery from non-native or exotic invasive species may be difficult due to many adaptations which allow them to survive and outcompete in intolerable conditions. Localized knowledge for each species must be known for best removal of it without harming the native environment, and often different treatments must be applied over one given area. Growth of non-native and exotic invasive species can be rapid following a change in a natural stressor such as fire frequency or natural hydroperiods which might have once kept the invasive species at bay.
Transition T5B
State 5 to 6This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Additional community tables
Table 5. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 6. Community 1.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 7. Community 1.3 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 8. Community 2.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 9. Community 2.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 10. Community 3.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 11. Community 3.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 12. Community 5.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 13. Community 5.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 14. Community 5.3 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 15. Community 5.4 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 16. Community 5.5 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 17. Community 6.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 18. Community 6.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 19. Community 6.3 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 20. Community 6.4 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Animal community
This community provides important habitat for many wildlife species, the understory shrubs and grasses are used for nesting, refuge, and forage, while overstory pines provide habitat for cavity nesting and tree nesting species. This community also provides refuge during the wet season for animals to move to drier ground. Due to intense fragmentation of this habitat, this species list is more representative of natural habitats such of those in the Big Cypress ecoregion. These species include:
Mammals: Florida black bear (Ursus americanus floridanus), Florida panther (Puma concolor coryi), gray fox (Urocyon cinereoargenteus), white-tailed deer (Odocoileus virginianus), fox squirrel (Sciurus niger), raccoon (Procyon lotor), cottontail rabbit (Sylvilagus floridanus), wild hogs (Sus scrofa), and armadillo (Dasypus novemcinctus). Several small rodents are also found in these habitats, including cotton rat (Sigmodon hispidus) and cotton mouse (Peromyscus gossypinus), least shrew (Cryptotis parva), short-tailed shrew (Blarina carolinensis), black rat (Rattus rattus), and house mouse (Podomys floridanus).
Birds: Among the most common resident species are pine warblers (Setophaga pinus), Florida scrub jay (Aphelocoma coerulescens) brown-headed nuthatch (Sitta pusilla), Bachman's sparrow (Peucaea aestivalis), great-horned owl (Bubo virginianus), American kestrel ( Falco sparverius), bald eagle (Haliaeetus leucocephalus) , wild turkey (Meleagris gallopavo silvestris), and bob-white quail (Colinus virginianus). Red-cockaded woodpeckers (Leuconotopicus borealis), an endangered species, use certain types of older, flatwoods pines for nesting.
Reptiles: Eastern diamondback (Crotalus adamanteus), Indigo snakes (Drymarchon couperi), pygmy rattlesnakes (Sistrurus miliarius), black racer (Coluber constrictor), Miami black-headed snake (Tantilla oolitca), mole snake (Pseudaspis cana), and pinewoods snake (Rhadinaea flavilata)
Amphibians: striped newt (Notophthlamus perstriatus), pinewoods tree frog (Hyla femoralis), oak toad (Anaxyrus quercicus), eastern box turtle (Terrapene carolina Carolina) and greenhouse frog (Eleutherodactylus planirostris).Hydrological functions
This area receives high amounts of rainfall, with topography and substrate keeping the rainwater from flowing quickly out of the watershed. Historically water flowed from Lake Okeechobee through the Everglades to shallow surface groundwater drainage pathways called transverse glades that connected the Everglades to the Atlantic Ocean. Currently this water moves faster from the northeast near Lake Okeechobee to the southeast through canals that pass through Miami and its surrounding cities along the Atlantic Coastal Strip. Man- made diversions such as canals, ditches, dams, and levees have locally changed the flow of water and lowered the water table. Largescale urban operations have changed the natural hydrology of the area, creating massive amounts of sheet flow from runoff into canal systems, moving water away from the little remaining natural communities into the ocean.
Due to flatwoods high evapotranspiration rates, land-to-water gradients as well as convective processes are reduced, helping control sea breeze intensity and the formation of convective thunderstorms. This effect is a natural feedback mechanism that results in a more even spatial distribution of seasonal rainfall (Bamberg 1980). Additionally, the wet flatwoods community becomes saturated and attains standing water in the middle to late wet season, corresponding with peak flowering periods for the understory components of the plant community, providing flowers and fruit for wildlife.Recreational uses
Remaining areas of this ecosite along the Miami Ridge / Atlantic Coastal Strip ecoregion are used as areas for hiking, birdwatching, and other outdoor activities.
Supporting information
Inventory data references
Information presented was derived from NRCS clipping data, current and historical literature, field observations, and personals contacts with local, state and federal partners. This is a provisional level ESD and is subject to change as more information becomes available, for any questions please contact your local NRCS office.
References
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1980. Fire Effects Information System. http://www.fs.fed.us/database/feis/.
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. 2021 (Date accessed). USDA PLANTS Database. http://plants.usda.gov.
Other references
Bamberg, M. 1980. Climate. Pages 32-46 in Water use and development plan, Volume III C, lower west coast. South Florida Water Management District. West Palm Beach, Florida.
Florida Chapter Soil and Water Conservation Society. 1989. 26 Ecological Communities of Florida
Florida Natural Areas Inventory (FNAI). 2010. Guide to the natural communities of Florida: 2010 edition. Florida Natural Areas Inventory, Tallahassee, FL
Harshberger, J. W. 1914. The Vegetation of South Florida South of 27 30 North, Exclusive of the Florida Keys. Philadelphia, Wagner Free Institute of Science, 1914.
Kambly, S., Moreland, T.R., 2009, Land cover trends in the Southern Florida Coastal Plain: U.S. Geological Survey Scientific Investigations Report 2009–5054, 16 p.
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
O'Brien, J. J., Mordecai, K. A., Wolcott, L., Snyder, J., & Outcalt, K. 2007. Fire managers field guide: hazardous fuels management in subtropical pine flatwoods and tropical pine rocklands. JFSP Research Projects Report. 101.
Scott, T. M. 2001. Text to accompany the geologic map of Florida. Florida Geologic Survey, Tallahassee, Florida.
Swain, E. D., Lohmann, M. A., & Goodwin, C. R. 2019. The hydrologic system of the south Florida peninsula—Development and application of the Biscayne and Southern Everglades Coastal Transport (BISECT) model (No. 2019-5045). US Geological Survey.
U.S. Fish & Wildlife Service Southeast Region (FWS). 1998. Dry Prairie. Multi-Species Recovery Plan for South Florida.
U.S. Fish & Wildlife Service Southeast Region (FWS). 1998. Hydric Pine Flatwoods. Multi-Species Recovery Plan for South Florida.
U.S. Fish & Wildlife Service Southeast Region (FWS). 1998. Mesic Pine Flatwoods. Multi-Species Recovery Plan for South Florida.
Yarlett, L. L. 1985. History of the Florida cattle industry. Rangeland Archives. 7(5), 205- 207.Contributors
Jack Ferrara
Craig Prink
Martin Figueroa
Jamie BeanApproval
Matthew Duvall, 4/14/2025
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 04/14/2025 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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