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and state-and-transition model (STM) were developed using archaeological and historical information, published and unpublished scientific reports, professional experience, consultation with technical experts, and NRCS inventories and studies.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 is represented of 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.
These are upland habitats that are above the coastal zone and are unaffected by daily and seasonal tides. Primarily driven by freshwater inputs from rain, these communities support large amounts of vegetation on thin organic/ marl soil over limestone bedrock and rely on a high-water table to maintain reservoirs. Weak acid from dissolving organic matter can create ongoing erosional processes that dissolves surface limestone forming solution holes, which helps maintain the seasonal high-water table. Small solution holes are frequent in this ecological site. These are highly diverse communities that are influenced by disturbance history, time since latest disturbance, community size, relative isolation from other similar sites, and physical environment (Olmsted 1980).
Pine rocklands are a unique habitat located in south Florida and limited in extent to this MLRA in each ecoregion sub-unit except the Everglades. It is characterized by an open canopy of pines and a patchy understory of tropical and temperate shrubs and palms. This site used to have a much larger extent than what is currently mapped today, but due to urbanization demands their range has reduced greatly. This habitat is maintained regularly by fire which burned on a 3 to 15 year interval, historically started by lightening strikes during summer months, now relied on prescribed fires. While this vegetative community is different from rockland hammock in structure, it is the primary community which succeeds to rockland hammocks after fire exclusion. These sites are usually excluded from flooding, but in areas near the ocean may experience flooding from storm surges. These pine rockland communities are different from the pine flatwood communities seen throughout peninsular Florida by the regular presence of exposed limestone rock throughout the community with very little soil development and the presence of rare plant species endemic to this community.
Rockland hammocks are the dominant forest type in the Florida Keys and often have greater than 120 native tree and shrub species, making up the diverse closed canopy and shrubs layers, in which many species reach their northern extent in Florida. Rockland hammock occurs on a thin layer of highly organic soil covering limestone on high ground that does not regularly flood, but it is often dependent upon a high-water table to maintain reservoirs in solution features of the limestone and to keep humidity levels high. These communities typically have large more mature trees in the interior where there is greater soil development and less disturbances, while the margins can be almost impenetrable in places with dense growth of smaller shrubs, trees, and vines. The tremendous development pressures in the rapidly urbanizing areas where rockland hammock occurs have greatly reduced the extent of this community. Exotic animals that have been introduced destroy and prey on native vegetation that is not adapted to their presence, leading to decline in native species. The dense canopy minimizes temperature fluctuations by reducing soil warming during the day and heat loss at night, creating mesic conditions. Mesic conditions are further maintained by the hammock’s rounded profile, which deflects winds, limiting desiccation during dry periods and reducing interior storm damage. Historically rockland hammocks in South Florida evolved with fire in the landscape, fire most often extinguishing near the edges when it encounters the hammock’s moist microclimate and litter layer. Rockland hammocks are susceptibly to damage from fire during extreme drought or when the water table is lowered from surrounding development. Extreme fires can cause root mortality and consume the humus layer, causing a succession back to a pine rockland community. Hurricanes and other disturbance events can have negative effects once fragmentation and exotic species become dominant, excessive damage from winds can be amplified due to roads and other development, opening space for exotic species. Severe storms can cause storm surges that can deposit overwash which can kill the understory. Thorn scrub is a community variant of rockland hammocks that occur along the ecotone of this community.
The hammocks on the Florida Keys tend to be drier than those on the mainland because of increased ocean breezes and lowered rainfall. They also have a higher percentage of tropical species in part because many temperate species, such as live oak, swamp bay (Persea palustris), sugarberry (Celtis laevigata), and coontie, reach their southern limits on the mainland or in the northern Keys. Many tropical tree species within Florida, such as rough strongbark (Bourreria radula) and lignum-vitae only occur in rockland hammocks of the Keys. Rockland hammock can be the advanced successional stage of mesic or xeric pine rocklands, especially in cases where rockland hammock is adjacent to flatwoods where hardwood seed rain is high. In such cases, when fire is excluded from adjacent flatwoods for 15 to 50 years it can succeed to rockland hammock vegetation that can retain a relict overstory of pine. Although rockland hammock can reestablish within 50 years after fire, maximum development of structure and diversity probably requires more than 100 fire-free years. Relative stability of hammock boundaries in relation to pine rocklands also suggests that the current vegetation mosaic is similar to the one which has existed during the past (Olmsted 1980). The ecotone between rockland hammock and pine rockland is abrupt when regular fire is present in the adjacent pine dominant community. However, when fire is removed, the ecotone becomes more gradual as hardwoods from the hammock push out into the pineland. Rockland hammock can be distinguished from pine rockland in having a closed, hardwood canopy rather than an open pine canopy. Rockland hammock can have almost the same structure and species composition as the tropical form of maritime hammock. It differs by being on a shallow rock substrate rather than the sand or shell substrate of barrier islands or high energy coasts.
Keys cactus barren is confined to the Florida Keys on limestone bedrock (Key Largo limestone) and is known from only six sites, four on the Upper Keys and two from the southern arm of Big Pine Key which is composed of Key Largo limestone (unlike the rest of Big Pine Key and the other Lower Keys, which are composed of Miami oolite). It occupies larger areas several acres in extent, or may occur as small, scattered patches within the thorn scrub variant of rockland hammock. The natural process giving rise to cactus barrens is not known, but since they occur on sites where the thin layer of organic soil over limestone bedrock is missing, they may have formed by soil erosion following destruction of the plant cover by fire, storm, or artificial clearing. This community is the most threatened by development and is unique only to this niche of Florida, totaling roughly 4.5 ha (11 acres).
Keys cactus barren is often surrounded by the thorn scrub variant of rockland hammock, consisting of low woody species such as buttonwood, blolly (Guapira discolor), catclaw blackbead, bayleaf capertree, poisonwood (Metopium toxiferum), and brittle thatch palm (Thrinax morrisii), forming a transition to the taller rockland hammock upland community. Prickly pear cacti in the genus Opuntia in this community are vulnerable to attack by the larvae of the cactus moth (Cactoblastis cactorum) which was inadvertently introduced from South America in the mid-1990s. Cactus barrens are vulnerable to development, even on public conservation lands, since their vegetation resembles weedy clearings and disturbed areas. Sites that have shown increasing encroachment of woody species over time may require efforts to maintain the open nature of the habitat, which favors the rare herbaceous species. Invasion by the exotic Brazilian pepper (Schinus terebinthifolius) is also a problem on some sites.
Sinkholes and exposed limestone bedrock can also be found as features within this community. Sinkholes can form in three ways. Dissolution sinkholes form when limestone is dissolved at or near the surface. Ongoing erosional processes result from the chemical and physical actions of underground water, which slowly dissolves the limestone and enlarges these cavities. Subsidence sinkholes, the most common type in Florida, form when the land subsides as limestone beneath is dissolved. These sinkholes develop into bowl-shaped depressions which can be shallow or deep. Collapse sinkholes can form when the water level in an underground cavern is lowered, either naturally (e.g., drought) or unnaturally (e.g., water table drawdown), creating a space between the water level and the roof of the cavern, which can cause a collapse of the roof. These sinkholes form rapidly when the weight of overlying sediments cause a collapse into the underground cavity. Sinkholes are found all throughout the state of Florida, but small dissolution sinkholes are frequent and most well represented in this ecosite, found within rockland hammocks, marl prairies, and pine flatwoods.
Sinkholes generally have higher relative humidity levels and lower light and temperature readings than the surrounding natural community. Whether they form a complete canopy or not, trees on the upper slopes or rim shelter the sinkhole from intense solar radiation. The depression itself also limits the effects of desiccating winds. Standing water in the bottom of the sinkhole, together with seepage from the surrounding uplands, helps to raise and maintain humidity levels. These conditions also buffer temperature extremes, providing frost-free habitats for cold sensitive species. This often allows for a unique mixture of tropical and temperate flora to exist in many Florida sinkholes. The sheltered habitat of sinkholes is also naturally protected from fires. Sinkholes that develop in fire-maintained communities often develop a hardwood canopy. Sinkholes may occur within most natural community types. In pyrogenic communities, sinkholes may form a natural barrier to fire that allows hardwood species to become established around the edge. Sinkholes drain readily and only contain standing water during, or for short periods following, heavy rains. The size of an individual sinkhole is variable and depends in large part on the local geology and hydrology.
Limestone outcrops are common in areas of karst terrain where the limestone is near the surface. The often-sheltered position of limestone outcrops supports a moist microclimate that moderates temperature extremes, allowing for bryophytic species to grow in the crevices, which help form organic soil over time through decomposition, which can eventually transition into a forested community. These sites occur within geologic features such as solution holes and are terrestrial communities, whereas exposed rocky tidal areas are classified as consolidated substrate.
Human activities in the surrounding areas may affect the delicate microclimate of a sinkhole and induce deleterious responses. For example, logging of the surrounding canopy can increase both solar radiation and sedimentation levels. Major soil disturbances in the adjoining uplands could disrupt seepage water sources. Large withdrawals of groundwater could substantially lower water tables and reduce the hydroperiods of sinkholes. Sinkholes are sometimes used as dumpsites. Because sinkholes drain directly to underground aquifers, refuse dumping should be strongly discouraged. Chemical applications, waste treatments, and spills on the surrounding upland require active monitoring to determine their potential impacts and mitigation requirements. Invasive exotic species are sometimes problematic in sinkholes. Their establishment is often facilitated by the shaded, humid environmental conditions. Steep slopes and the presence of sensitive plant and animal species can complicate the treatment of exotic plants. Furthermore, the close connection of sinkholes to aquifers requires especially careful applications of herbicides to avoid groundwater contamination.
State 1
Pine Woodlands
This state depicts forested rocklands consisting of open canopied forests dominated by pine trees. Fire is used to maintain this habitat and will have an open to dense understory of diverse subtropical and temperate species. Exposed limestone rocks can be found throughout the entire area or close to the surface.
Characteristics and indicators. This site is characterized by shallow to exposed bedrock with an open pine woodland similar to pine flatwoods communities. Subtropical species will be present in the understory.
Resilience management. Fire is used to maintain community composition and structure and was historically introduced every 3 to 15 years. In areas of high density urbanization and fragmentation of this habitat, mechanical treatments such as roller chopping or hand removal can be utilized but are less effective than fire treatments.
Dominant resource concerns
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Sheet and rill erosion
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Subsidence
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Organic matter depletion
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Ponding and flooding
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Salts transported to surface water
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Salts transported to ground water
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Plant productivity and health
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Plant structure and composition
Community 1.1
Pine Rockland
Pine rocklands are open canopied forested dominated by pines with a patchy understory of tropical and temperate shrubs and palms and a rich herbaceous layer of mostly perennial species endemic to south Florida. These communities will exist on very shallow to bedrock soils that are dominantly marl textured. This community is globally impaired and limited in distribution to Big Cypress National Preserve (Monroe and Collier Counties), the Florida Keys, and the southern portion of the Miami Ridge. The pine rocklands in the Florida Keys area will be more xeric due to lower rainfall and has a well developed sub canopy of silver palm, brittle thatch palm, and a higher percentage of tropical shrub species since many temperate species reach their southern limit on the mainland.
Resilience management. Fire is used to maintain community structure and composition with return intervals every 3 to 15 years, and without fire would allow the development of hardwood species to close the canopy transitioning to a rockland hammock. Although hardwood species are a natural component of pine rocklands, an exclusion of fire greater than 50 years will result in a succession to rockland hammock.
Dominant plant species
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Florida slash pine (Pinus elliottii var. densa), tree
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Florida silver palm (Coccothrinax argentata), shrub
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Key thatch palm (Leucothrinax morrisii), shrub
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sweet acacia (Vachellia farnesiana), shrub
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smooth strongbark (Bourreria cassinifolia), shrub
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Long Key locustberry (Byrsonima lucida), shrub
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grannybush (Croton cascarilla), shrub
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buttonsage (Lantana involucrata), shrub
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mangroveberry (Psidium longipes), shrub
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white bully (Sideroxylon salicifolium), shrub
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coco plum (Chrysobalanus icaco), shrub
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Florida strangler fig (Ficus aurea), shrub
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wild banyantree (Ficus citrifolia), shrub
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wax myrtle (Morella cerifera), shrub
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Guianese colicwood (Myrsine cubana), shrub
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redbay (Persea borbonia), shrub
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white indigoberry (Randia aculeata), shrub
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winged sumac (Rhus copallinum), shrub
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cabbage palmetto (Sabal palmetto), shrub
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saw palmetto (Serenoa repens), shrub
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fewflower holdback (Caesalpinia pauciflora), shrub
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smallflower lilythorn (Catesbaea parviflora), shrub
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pride of Big Pine (Strumpfia maritima), shrub
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threeawn (Aristida), grass
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splitbeard bluestem (Andropogon ternarius), grass
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crimson bluestem (Schizachyrium sanguineum var. sanguineum), grass
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lopsided Indiangrass (Sorghastrum secundum), grass
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coontie (Zamia pumila), other herbaceous
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partridge pea (Chamaecrista fasciculata), other herbaceous
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pineland fern (Anemia adiantifolia), other herbaceous
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Bahama brake (Pteris bahamensis), other herbaceous
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brackenfern (Pteridium), other herbaceous
Community 1.2
Fire Excluded Pine Rockland
This community described a reference pine rockland in which fire has been excluded from the system for greater than 15 years but less than 50 years. This is longer than the naturally accepted fire return interval of 3 to 15 years but less than the 50 year exclusion limit where a rockland hammock gradually develops. Plant composition will be similar to the reference community, but community structure will be different. The shrubs will begin to shade out the understory and accumulate leaf litter, creating a moist environment.
Resilience management. Fire may still be carried through this community and can return to a reference pine rockland if introduced and maintained along a 3 to 15 year return interval.
Dominant plant species
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Florida slash pine (Pinus elliottii var. densa), tree
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Key thatch palm (Leucothrinax morrisii), shrub
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Florida thatch palm (Thrinax radiata), shrub
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seagrape (Coccoloba uvifera), shrub
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marlberry (Ardisia), shrub
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wild coffee (Psychotria), shrub
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blackbead (Pithecellobium), shrub
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cabbage palmetto (Sabal palmetto), shrub
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wax myrtle (Morella cerifera), shrub
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saw palmetto (Serenoa repens), shrub
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smallcane (Lasiacis divaricata), grass
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basketgrass (Oplismenus hirtellus), grass
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eastern poison ivy (Toxicodendron radicans), other herbaceous
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greenbrier (Smilax), other herbaceous
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medicine vine (Hippocratea volubilis), other herbaceous
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redgal (Morinda royoc), other herbaceous
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coontie (Zamia pumila), other herbaceous
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swordfern (Nephrolepis), other herbaceous
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maiden fern (Thelypteris), other herbaceous
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airplant (Tillandsia), other herbaceous
Pathway 1.1A
Community 1.1 to 1.2
This transition is driven by the exclusion of fire from the community for 15 to 50 years, which allows the establishment of shrubs to enter the midstory and begin a gradual transition to a hammock. This exclusion of fire can be due to high urbanization and fragmentation within the Florida Keys.
Pathway 1.2A
Community 1.2 to 1.1
This transition is driven by the reintroduction of fire into the system, which will assist in maintaining community structure of a reference pine rockland community. Once fire is reintroduced, to maintain a reference pine rockland community a fire return interval of every 3 to 15 years must be maintained to keep hardwoods excluded from growing into the midstory and preventing a possible hammock transition.
State 2
Rockland Forest
This state depicts forested rocklands consisting of closed canopied forests dominated by hardwood species. This is considered the successional stage of pine rocklands, characterized by long periods of time without fire in the system.
Characteristics and indicators. These rockland hammocks are characterized by closed canopy forests with a high diversity of species assemblage. These communities have shaded understories allowing for a dense assemblage of inflammable species and the creation of high moisture conditions creating a cool interior. Leaf litter accumulation will be present on the ground surface and will increase over time.
Dominant plant species
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gumbo limbo (Bursera simaruba), tree
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false tamarind (Lysiloma latisiliquum), tree
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tietongue (Coccoloba diversifolia), tree
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Florida strangler fig (Ficus aurea), tree
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live oak (Quercus virginiana), tree
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Florida slash pine (Pinus elliottii var. densa), tree
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stopper (Eugenia), shrub
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cabbage palmetto (Sabal palmetto), shrub
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greenbrier (Smilax), other herbaceous
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airplant (Tillandsia), other herbaceous
Dominant resource concerns
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Sheet and rill erosion
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Plant productivity and health
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Plant structure and composition
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Terrestrial habitat for wildlife and invertebrates
Community 2.1
Early Successional Rockland Hammock
This community describes an early successional rockland hammock in which fire has been excluded from a pine rockland for greater than 50 years, allowing for the shrubs to grow into the overstory and created shaded conditions that will no longer carry ground fires. Species composition will be similar to a rockland hammock but estimates require more than 100 fire free years to have maximum development of hammock structure and diversity. A relict overstory of slash pine may be present, representative of a transitioned pine rockland.
Resilience management. Gap succession is the main driver for this community and is often seen as windthrow during high energy storm events such as hurricanes. This community also requires time to transition to a rockland hammock and is estimated more than 100 fire free years to mature.
Dominant plant species
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Florida slash pine (Pinus elliottii var. densa), tree
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gumbo limbo (Bursera simaruba), tree
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false tamarind (Lysiloma), tree
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false mastic (Sideroxylon foetidissimum), tree
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Florida strangler fig (Ficus aurea), tree
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Florida fishpoison tree (Piscidia piscipula), tree
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paradisetree (Simarouba glauca), tree
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white bully (Sideroxylon salicifolium), tree
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live oak (Quercus virginiana), tree
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poisonwood (Metopium toxiferum), tree
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West Indian mahogany (Swietenia mahagoni), tree
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stopper (Eugenia), shrub
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thatch palm (Thrinax), shrub
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marlberry (Ardisia), shrub
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Seminole balsamo (Psychotria nervosa), shrub
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cabbage palmetto (Sabal palmetto), shrub
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seagrape (Coccoloba uvifera), shrub
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greenbrier (Smilax), shrub
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smallcane (Lasiacis divaricata), grass
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basketgrass (Oplismenus hirtellus), grass
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airplant (Tillandsia), other herbaceous
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swordfern (Nephrolepis), other herbaceous
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maiden fern (Thelypteris), other herbaceous
Community 2.2
Thorn Scrub
This community is a variant of a rockland hammock that is found only within the Florida Keys. It occurs along the ecotone of rockland hammocks or within openings of rockland hammocks. It is dominated by low-statured scrubby spiny species. It has also been referred to as "Keys hammock thicket", "transitional thorn woodland", or "cactus scrub". Much is still unknown about this community variant and requires further study on ecological stressors and successional patterns. This variant is more commonly seen in the southern Florida Keys in hammocks with lower, more scrubby, xeric species compositions.
Dominant resource concerns
Community 2.3
Rockland Hammock
Rockland hammocks are very diverse tropical hardwood forests and considered the successional stage to pine rocklands. Limestone bedrock is very near the surface and often exposed. These communities can have greater than 120 native tree and shrub species present, many of which are at the northern extent of their native range. Organic acids from the decomposition of leaf litter can cause dissolving in the limestone bedrock forming solution holes, which may hold water and help maintain high humidity within the hammock. These will occur in limited extent in the Florida Keys area and will be distinguished from the rockland hammocks in the Big Cypress and Miami Ridge ecoregions. The hammocks in the Florida Keys tend to be drier than those on the mainland because of increased ocean breezes and lowered rainfall. These will also have a higher percentage of tropical species due to many species reaching their northern extent on the the southern tip of Florida.
In the Keys, there will be slight structural changes to hammocks varying from north to south due to changes in geology, ground water salinity and rainfall. The northern Keys will have taller, more developed tree canopies (>35 ft in height) due to more permeable limestone and slightly higher rainfall. In the southern Keys the hammocks will have lower scrubby, xeric forms with species 20 ft tall or less, and will have higher abundance of the thorn scrub variant.
Dominant plant species
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live oak (Quercus virginiana), tree
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swamp bay (Persea palustris), tree
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rough strongbark (Bourreria radula), tree
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lignum-vitae (Guaiacum), tree
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gumbo limbo (Bursera simaruba), tree
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tietongue (Coccoloba diversifolia), tree
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false tamarind (Lysiloma), tree
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false mastic (Sideroxylon foetidissimum), tree
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Florida strangler fig (Ficus aurea), tree
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West Indian mahogany (Swietenia mahagoni), tree
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Florida poisontree (Metopium), tree
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Florida slash pine (Pinus elliottii var. densa), tree
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stopper (Eugenia), shrub
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Key thatch palm (Leucothrinax morrisii), shrub
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Florida thatch palm (Thrinax radiata), shrub
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sea torchwood (Amyris elemifera), shrub
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marlberry (Ardisia), shrub
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Seminole balsamo (Psychotria nervosa), shrub
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cabbage palmetto (Sabal palmetto), shrub
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coontie (Zamia pumila), shrub
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seagrape (Coccoloba uvifera), shrub
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sugarberry (Celtis laevigata), shrub
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greenbrier (Smilax), other herbaceous
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airplant (Tillandsia), other herbaceous
Dominant resource concerns
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Subsidence
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Ground water depletion
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Salts transported to surface water
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Plant productivity and health
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Plant structure and composition
Pathway 2.1A
Community 2.1 to 2.3
This transition is driven by time which causes the early succession community to mature into a rockland hammock. While the early successional community can form as soon as 50 years in the absence of fire, it is estimated to need an additional 50 years of a fire free system, for more than 100 years total of being fire free to have maximum development of structure and species diversity.
Context dependence. This often occurs when a rockland hammock is fragmented due to urbanization.
Pathway 2.3A
Community 2.3 to 2.1
This transition is driven by a disturbance event which may return a rockland hammock back to an early succession phase. Overstory mortality may create canopy gaps which would allow for the rapid growth of species as they compete for light availability. Many different factors may cause overstory mortality in a rockland hammock, including, but not limited to, windthrow, crown fires, selective logging, or tree fall by weathering limestone.
State 3
Bare Ground / Pioneer Habitat
This state depicts a community that lacks vegetation. This is most often associated with extreme fires that will cause high mortality rates within a vegetative community. This state will also describe the secondary succession pioneer habitat that will become established if left undisturbed.
Characteristics and indicators. It is characteristic of herbaceous and succulent species found on exposed bedrock with little to no soil development.
Dominant resource concerns
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Subsidence
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Salts transported to surface water
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Salts transported to ground water
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Plant productivity and health
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Plant structure and composition
Community 3.1
Bare Ground or Exposed Soil / Bedrock
This community describes an area in which a disturbance event has cleared or killed the existing vegetative community, leaving behind the bare ground or exposed soil or bedrock. Disturbance events may include wildfires which kill existing vegetation or windthrow from storm events such as hurricanes. In the Keys, habitats which are in close proximity to the ocean may become flooded by extreme storm events, leading to die off from high salinity levels.
Community 3.2
Secondary Succession Pioneer Habitat
This community described a secondary succession pioneer habitat where a disturbance has taken place and cleared the soil, but is still able to support plant growth due to an existing or introduced seedbed. Rapid colonization will begin from herbaceous species, shrubs, and climbing species as well as seedlings from pioneer tree species. Over time it will transition into either a pine rockland or rockland hammock depending on available seedbank and if managed properly for those habitats. If left unmanaged, this community will have large amounts of invasive species throughout the community.
Resilience management. Once a seedbank is established this secondary succession pioneer community can transition to either a rockland hammock or pine rockland, dependent on what was the existing community. Maintenance of that habitat will be required to reflect natural conditions.
Community 3.3
Keys Cactus Barren
This is an open, herbaceous community with scattered shrubs on exposed limestone bedrock or areas with little soil or leaf litter in the Florida Keys. Primary vegetation are wide varieties of herb and succulent species which include cacti, agave, and several rare herbs. This is a very limited site and is only known from six sites which vary primarily in the degree of shrub and cacti cover.
Resilience management. The natural process giving rise to this community is not yet known, but it hypothesized that the thin layer of organic soil over limestone bedrock is missing, they may have formed via erosion following destruction of the plant cover by fire, storm, or artificial clearing. This is a highly endangered community and is most threatened by development.
Dominant plant species
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gumbo limbo (Bursera simaruba), tree
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button mangrove (Conocarpus erectus), tree
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boxleaf stopper (Eugenia foetida), shrub
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catclaw blackbead (Pithecellobium unguis-cati), shrub
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Spanish lady (Opuntia triacantha), shrub
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false sisal (Agave decipiens), shrub
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triangle cactus (Acanthocereus tetragonus), shrub
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bindweed dwarf morning-glory (Evolvulus convolvuloides), other herbaceous
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Yucatan flymallow (Cienfuegosia yucatanensis), other herbaceous
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skyblue clustervine (Jacquemontia pentanthos), other herbaceous
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indigo (Indigofera), other herbaceous
Pathway 3.1A
Community 3.1 to 3.2
This transition is driven by seedbank establishment, in where existing seeds are present in the remaining soil and begin to grow, creating an secondary succession pioneer habitat which represents the reference communities of State 1 or 2.
Context dependence. The seedbank must be preexisting in the remaining soil or must be deposited via natural or anthropogenic means.
Pathway 3.1B
Community 3.1 to 3.3
This transition is driven by seedbank establishment, in where existing cacti seeds are present in the remaining soil and begin to grow, creating a cactus barren. Maintenance of this community is still widely unknown.
Context dependence. The seedbank must be preexisting in the remaining soil or must be deposited via natural or anthropogenic means.
Pathway 3.2A
Community 3.2 to 3.1
This transition is driven by a disturbance event which destroys the secondary succession pioneer habitat back to exposed ground. This may be from abiotic factors such as hurricane events or by wildfires which will destroy the regrowth. In the Florida Keys, habitats in close proximity to the ocean may become flooded during extreme storm events, causing die off of species due to high salinities.
Pathway 3.3A
Community 3.3 to 3.1
This transition is driven by a disturbance event which destroys the secondary succession pioneer habitat back to exposed ground. This may be from abiotic factors such as hurricane events or by wildfires which will destroy the regrowth. In the Florida Keys, habitats in close proximity to the ocean may become flooded during extreme storm events, causing die off of species due to high salinities.
State 4
Invasive Non-Native Community
This 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 are introduced to the state via people, weather events, or any other means.
Resilience management. This state can be found as a part of any other state and can completely replace the native habitat if not properly managed. Restoration to natural communities after exotic non-native invasion includes practices such as mechanical and chemical removal.
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
Human Altered and Human Transported Areas
These 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., Pennekamp gravelly muck-Urban land complex, 0-2% slopes, extremely stony).
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 5.1
Reclaimed Areas
Reclaimed 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 intensity urban areas, and may be required to be reclaimed after urban use (e.g., active mines must be reclaimed). 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 5.2
Urban
This 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/ active mines).
Community 5.3
Non-Reclaimed Areas
Non-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 5.4
Landfills
This 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 5.1 to 5.2
This shift in communities is driven by clearing and developing the land for the desired community.
Pathway 6.1B
Community 5.1 to 5.4
This transition is driven by the deposition of manufactured layers along with anthropogenic waste which is consistently built upon.
Pathway 6.2A
Community 5.2 to 5.1
This transition is driven by the revegetation, reestablished hydroperiods, and replacement of displaced soil materials after altering the land.
Pathway 6.2B
Community 5.2 to 5.3
This 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 5.2 to 5.4
This transition is driven by the deposition of manufactured layers along with anthropogenic waste which is consistently built upon.
Pathway 6.3A
Community 5.3 to 5.1
This transition is driven by the revegetation, reestablished hydroperiods, and replacement of displaced soil materials after altering the land.
Transition T1A
State 1 to 2
This state transition is driven by an exclusion of fire from the system for greater than 50 years. The absence of fire for this amount of time will allow the understory shrub species to mature and grow in the overstory. This will shade out the understory, losing species diversity and accumulating organic matter over time, creating a cool, moist interior, which helps exclude fire from the area.
Constraints to recovery. As the shrubs grow into the overstory they will shade the understory creating more moist conditions in which fire is unable to pass through. If this state is surrounded by pine rocklands which have a regular fire return interval, there will be a sharp ecotone between these two states. If fire has been excluded from the reference state then there will be a gradual transition into the rockland hammock.
Context dependence. The absence of fire from these systems are largely due to the high levels of urbanization and fragmentation along the Florida Keys.
Transition T1B
State 1 to 3
This transition is driven by an extreme fire which removes all of the existing vegetation, leaving behind bare soil or exposed bedrock.
Constraints to recovery. An existing seedbank must be present in the soil and enough time must be allowed for the establishment of the native species to grow. During the growth of these species proper management must be taken to ensure there is no undesirable invasive or exotic species that become established.
Context dependence. An extreme fire can occur due to high buildup of organic matter (leaf litter) in the understory and presence of ladder fuels into the overstory.
Transition T1C
State 1 to 4
The 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 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.
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 5
This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Transition T2A
State 2 to 1
This transition is driven by the selective removal or hardwood and pine species to transition the community structure back to a pine rockland state. Once community structure and composition is to the desired criteria a regular fire return interval must be established every 3 to 15 years.
Constraints to recovery. This is a very costly and time consuming process.
Transition T2B
State 2 to 3
This transition is driven by an extreme fire which removes all of the existing vegetation, leaving behind bare soil or exposed bedrock.
Constraints to recovery. An existing seedbank must be present in the soil and enough time must be allowed for the establishment of the native species to grow. During the growth of these species proper management must be taken to ensure there is no undesirable invasive or exotic species that become established.
Context dependence. An extreme fire can occur due to high buildup of organic matter in the understory and presence of ladder fuels into the overstory.
Transition T2C
State 2 to 4
The 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 intolerable conditions. Localized knowledge for each species must be known for best management of it it without harming the natural habitat, 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 T2D
State 2 to 5
This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Restoration pathway R3A
State 3 to 1
This restoration strategy to reestablish a pine rockland community cannot be done without an established seedbank. This seedbank may be preexisting in the soil or may be planted via human restoration. Once the seedbank is established the area must continually undergo habitat management to ensure there is no presence of undesirable invasive or exotic species over time.
Context dependence. Maintenance of a pine rockland habitat includes regular fire return intervals every 3 to 15 years to prevent hardwood inclusion into the system, if fire is not present in the system this may gradually transition to a rockland hammock.
Restoration pathway R3B
State 3 to 2
This restoration strategy to reestablish a rockland hammock community cannot be done without an established seedbank. This seedbank may be preexisting in the soil or may be planted via human restoration. Once the seedbank is established the area must continually undergo habitat management to ensure there is no presence of undesirable invasive or exotic species over time.
Context dependence. Maintenance of a rockland hammock habitat includes the absence of fire from the system for greater than 50 years while the hammock undergoes development.
Transition T3A
State 3 to 4
The 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 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.
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 T3B
State 3 to 5
This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.
Restoration pathway R4A
State 4 to 1
Mechanical, 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 2
Mechanical, 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 3
Mechanical, 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 5
This transition is driven by the alteration and/ or transportation of materials via anthropogenic means.