Geography and ecology of the Everglades

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A color satellite image of the lower two-thirds of the Florida peninsula: large bodies of water are black, most chunk of land south of Lake Okeechobee is red, indicating the Everglades Agricultural Area; south of that is a solid swath of dark blue indicating where the Everglades flow in a southwesterly direction into the Gulf of Mexico
A satellite image of the lower Florida peninsula showing darkened portions south of Lake Okeechobee as the Everglades and Big Cypress Swamp. The reddish area bordering the large inland lake is the Everglades Agricultural Area.
Satellite image taken in March 2019 shows southeast of the Everglades, including Cape Sable and Florida Bay. Miami is on the right side.

Before drainage, the Everglades, a region of tropical wetlands in southern Florida, were an interwoven mesh of marshes and prairies covering 4,000 square miles (10,000 km2). The Everglades is both a vast watershed that has historically extended from Lake Okeechobee 100 miles (160 km) south to Florida Bay (around one-third of the southern Florida peninsula), and many interconnected ecosystems within a geographic boundary. It is such a unique meeting of water, land, and climate that the use of either singular or plural to refer to the Everglades is appropriate.[1] When Marjory Stoneman Douglas wrote her definitive description of the region in 1947, she used the metaphor "River of Grass" to explain the blending of water and plant life.

Although sawgrass and sloughs are the enduring geographical icons of the Everglades, other ecosystems are just as vital, and the borders marking them are subtle or nonexistent. Pinelands and tropical hardwood hammocks are located throughout the sloughs; the trees, rooted in soil inches above the peat, marl, or water, support a variety of wildlife. The oldest and tallest trees are cypresses, whose roots are specially adapted to grow underwater for months at a time. The Big Cypress Swamp is well known for its 500-year-old cypresses, though cypress domes can appear throughout the Everglades. As the freshwater from Lake Okeechobee makes its way to Florida Bay, it meets saltwater from the Gulf of Mexico; mangrove forests grow in this transitional zone, providing nursery and nesting conditions for many species of birds, fish, and invertebrates. The marine environment of Florida Bay is also considered part of the Everglades because its seagrasses and aquatic life are attracted to the constant discharge of freshwater.

These ecological systems are always changing due to environmental factors. Geographic features such as the Western Flatwoods, Eastern Flatwoods, and the Atlantic Coastal Ridge affect drainage patterns. Geologic elements, climate, and the frequency of storms and fire are formative processes for the Everglades. They help to sustain and transform the ecosystems in the Shark River Valley, Big Cypress Swamp, coastal areas, and mangrove forests. Ecosystems have been described as both fragile and resilient. Minor fluctuations in water levels have far-reaching consequences for many plant and animal species, and the system cycles and pulses with each change.

Shaping processes of ecosystems

At only 5,000 years of age, the Everglades is a young region in geological terms. Its ecosystems are in constant flux as a result of the interplay of three factors: the type and amount of water present, the geology of the region, and the frequency and severity of fires.[2][3]

Water

A storm over the Shark River in the Everglades, 1966
Photo:Charles Barron / State Library and Archives of Florida

Water is the dominant element in the Everglades, and it shapes the land, vegetation, and animal life of South Florida. The South Florida climate was once

springs and sinkholes. The abundance of fresh water allowed new vegetation to take root, and through evaporation formed thunderstorms. Limestone was dissolved by the slightly acidic rainwater. The limestone wore away, and groundwater came into contact with the surface, creating a massive wetland ecosystem.[4]
Although the region appears flat, the wearing away of the limestone in some areas created slight valleys and plateaus—a difference of inches in elevation—that affected not only the flow of water, but also types of vegetation present.

The Everglades are unique; no other wetland system in the world is nourished primarily from the atmosphere.[5] Before the first attempt at draining the Everglades in 1882, the entire watershed extended from Orlando to Florida Bay comprising the Kissimmee–Lake Okeechobee–Everglades (KLOE) watershed. Kissimmee River outlets flow into Lake Okeechobee, which sits 18 feet (5.5 m) above sea level.[6] Only two seasons exist in the Everglades: wet (May to November) and dry (December to April). Average annual rainfall in the Everglades is approximately 62 inches (160 cm), though fluctuations of precipitation are normal.[7] Droughts, floods, and tropical storms are normal occurrences in the area.[8] When Lake Okeechobee exceeds its water storage capacity during the wet season, it pours slowly over the southern rim and flows for 100 miles (160 km) to Florida Bay. The gradient change is so slight that the river moves only 2 feet (0.61 m) a minute.[9] Sawgrass thrives in this river, dominates freshwater marshes and sloughs, and is the main characteristic of the region.

Severe weather, in the form of

orchids, bromeliads, and other epiphytes that once flourished in the mangroves; their reappearance may take a century or more. Donna also significantly spread buttonwood, saltwort, and glasswort, and epiphytes began to grow in new areas.[13] Although the lasting effects remain to be seen, Hurricane Andrew in 1992 also destroyed mangrove forests and snapped slash pines in half. However, regrowth occurred quickly, and sand deposited by the storm surge improved nesting conditions for crocodiles and sea turtles.[14]

Geology

Further information: Everglades § Geology

A vast marshland could only have been formed due to the underlying rock formations in southern Florida.[15] The floor of the Everglades formed between 25 million and 2 million years ago when the Florida peninsula was a shallow sea floor. The peninsula has been covered by sea water at least seven times since the earliest bedrock formation.[15] The rock that makes up the Everglades floor was created as layers of calcium carbonate were compressed by ocean water, making limestone. Fossilized bryozoans and tiny shells, or ooids, make the limestone porous. Water is stored in the rock, sometimes from one year to the next.[16] The length of time that a region in the Everglades remains flooded, called a hydroperiod,[4] determines what particular soils and vegetation are present.

Shorter hydroperiods of three or four months promote the growth of periphyton: algae and other microscopic organisms covered with calcium carbonate crystals.[15] Periphyton is the basic building block of marl, a calcitic mud. In areas with hydroperiods of longer than nine months, peat builds up over hundreds or thousands of years due to many generations of decaying plant matter. Peat and marl are considered nutrient-poor soils that foster the growth of specialized vegetation depending on the length of the regional hydroperiod.

Five types of peat appear in the Everglades system; each type supports a specific type of vegetation, such as sawgrass, tree islands, or custard apple trees.[17] Peat buildup is possible because water prevents oxygen from quickly decomposing plant matter. Once peat buildup reaches the surface, oxygen reacts with the microorganisms to decay the peat rapidly in a process called subsidence. Initial attempts at developing agriculture near Lake Okeechobee were successful, but the nutrients in the peat quickly deteriorated by drying, and were broken down by bacteria in the soil. The dried peat burned or was degraded into carbon dioxide and water by microorganisms. Some homes built near early farms had to restructure their foundations on stilts as the peat deteriorated; other areas lost approximately 8 feet (2.4 m) of soil depth.[18] Between the 1880s and 2005, an estimated 3.4 billion metric tons of soil has been lost in the Everglades due to oxidation. Most of that loss occurs in the Everglades Agricultural Area; the least amount of loss is found in Everglades National Park.[19]

Fire

Fire near a cypress dome in the Turner River area in the early 1920s

Fire is another important element in the maintenance of the Everglades. The majority are caused by lightning strikes from thunderstorms during the wet season. Their effects are largely superficial, and serve to foster further plant growth: sawgrass will burn above water, but the roots are preserved. Fire in the sawgrass marshes serves to keep out larger bushes and trees, and releases nutrients from decaying plant matter more efficiently than decomposition.[20] Large burned areas also affect waterflow, since wind and water are undeterred by the eradicated sawgrass; water may flow two to three times faster in recently burned areas.[21] During the wet season only dead plant matter and the tips of plants are burned; however, the effects of fire are much more significant in the dry season, as fire may be fed by organic peat and burn deeply, destroying root systems. The only impediment to the spread of fire in the Everglades is the presence of water. It takes around 225 years for one foot (0.3 m) of peat to develop, but the peat is not as dense as it should be for the 5,000 years of the Everglades' existence. Scientists point to fire as the reason.[3]

Researchers have noted that fires appear in cycles associated with those of the hydroperiods.

BCE.[3]

Ecosystem characteristics

A color satellite image of the lower third of the Florida peninsula with labels superimposed over major landscapes before human alterations: directly to the south of Lake Okeechobee is a thin custard apple and cypress swamp, a much larger cypress swamp borders the lake to the east, and a major section of western pine flatwoods borders it to the west. Massive sawgrass plains are formed to the south of the custard apple swamps, which eventually merge into ridge and slough formations that narrow into the Shark River that flow into the Gulf of Mexico. Where the Shark River forms the area is lined with marl marshes, and the Big Cypress Swamp is located between the ridge and slough formations and the Gulf of Mexico. To the east the Atlantic Coastal Ridge rises slightly above the Everglades, which is where the major population centers are located
Major landscape types in the Everglades before human action. Source: U.S. Geological Survey

The Everglades are dominated by sawgrass in water; this is the titular "River of Grass" popularized by Marjory Stoneman Douglas in 1947. This river contains a wide variety of plant and animal life. Early American environmentalist Gifford Pinchot said of the Everglades, "It is a region so different that it hardly seems to belong to the United States. It is full of the most vivid and most interesting life on land, in the air, and in the water. It is a land of strangeness, separate and apart from the common things we all know so well."[22]

The sawgrass grows in prairies or strands, in between channels of water in a shallow river 100 miles (160 km) long and 60 miles (97 km) wide flowing from Lake Okeechobee to Florida Bay. Some authors refer to the sawgrass and water combination as the "true Everglades" or just "the Glades".[23][24] Prior to the first drainage attempts in 1905, the sheetflow, or the wide shallow river starting in Lake Okeechobee, occupied nearly a third of the lower Florida peninsula.[4] Though sawgrass remains the main feature of the Everglades, other ecosystems are scattered among the marshes and prairies, and their borders are sometimes imperceptible.

Sawgrass marsh

Most marshes in the Everglades are dominated by the sedge known as Cladium, or sawgrass in common terminology. The sedge is a three-dimensional v-shaped stalk with upward-pointing teeth. Sawgrass thrives in the slowly moving water, but may die if oxygen is unable to reach its roots and is particularly vulnerable to floods immediately after a fire.[25] Some of the sawgrass can grow up to 6 feet (1.8 m) tall, and directly south of Lake Okeechobee it has grown to 10 feet (3.0 m). Farther south, where the peat is not as rich, it typically grows 4 feet (1.2 m) tall in patches, as opposed to the prairies of the upper glades.[26] The hydroperiod for the marsh is usually nine months but can last longer. In shorter hydroperiods, marl may form instead of peat.[27]

Where sawgrass grows densely, few animals or other plants thrive, although

amphibians are supported by periphyton; these in turn provide food for birds, fish, and reptiles. Periphyton also absorbs calcium from the water, which creates marl where sawgrass takes root.[29]

Freshwater sloughs

Sloughs are channels of free-flowing water in between the sawgrass marshes. Sloughs are deeper than sawgrass marshes, about 3 feet (0.91 m), and may stay flooded for at least 11 months out of the year if not multiple years in a row.

apple snail.[31] Plants grow here, usually submerged or floating like bladderwort (Utricularia), waterlily (Nymphaeaceae), or spatterdock (Nuphar lutea). Major sloughs in the Everglades system include the Shark River Slough draining to Florida Bay, Lostmans Slough bordering The Big Cypress, and Taylor Slough
in the eastern Everglades.

A black and white illustration of a cross section of fresh water ecosystems: from the left is in the deepest water; pond sloughs merge into the slightly higher wet prairies, then the sawgrass marsh. Large cypress trees take over and the water deepens slightly and the land raises above the water completely indicating where hardwood hammocks are located relative to average water depths
A cross section of fresh water ecosystems in the Everglades, with relative average water depths

Wet prairie

A color photograph taken from above of a mid-sized alligator with its head above water resting on an outcropping of plants and the rest of its body submerged in clear water. The alligator is surrounded by strands of yellow and brown strands of periphyton underwater
An alligator amid strands of periphyton in the Everglades

Two kinds of wet prairies thrive in the Everglades: marl and water-marsh community. Wet prairies are slightly elevated like sawgrass marshes, but contain abundant plant diversity. Marl prairies are located where marl covers limestone that may protrude as pinnacles or erode into solution holes: depressions formed by the same processes that create sinkholes. Solution holes, however, do not meet the water table; they are filled with rain water.[32] The surface is covered only three to seven months of the year, but the water is usually just 4 inches (10 cm) deep.[33] Marl is created by layers of periphyton loosely attached to the limestone, and forms a grey or white crumbly mud when it dries. When flooded, the marl can support a variety of water plants, and dwarf cypresses may grow for hundreds of years though not exceed 10 feet (3.0 m) in height.[34] Solution holes may remain flooded even when the prairies are dry, and they support aquatic invertebrates such as crayfish and snails, as well as larval amphibians which feed young wading birds.[35] Where the predominant soil is peat, a water-marsh community exists. Its hydroperiod is longer than the marl prairie, although its plants are less diverse. These regions tend to be on the border between sloughs and sawgrass marshes.

Alligators have created an ecological niche in wet prairies; they dig at low spots with their claws and snouts and create ponds free of vegetation that remain submerged throughout the dry season. Alligator holes are integral to the survival of aquatic invertebrates, turtles, fish, small mammals, and birds during extended drought periods. Alligators feed upon animals that visit the hole.[36][37]

Tropical hardwood hammock

In a tropical hardwood hammock, plants are very dense and diverse.
Main article: Tropical hardwood hammock

Islands of trees featuring dense temperate or tropical trees are called tropical hardwood hammocks.[38] They may rise between 1 and 3 feet (0.30 and 0.91 m) above water level in freshwater sloughs, sawgrass prairies, or pineland. These islands illustrate the difficulty of characterizing the climate of the Everglades as tropical or subtropical. Hammocks in the northern portion of the Everglades consist of more temperate plant species, but closer to Florida Bay the trees are tropical and smaller shrubs are more prevalent. Tropical trees like the West Indian mahogany (Swietenia mahagoni) were probably spread by birds carrying seeds from the West Indies.[39]

These hammocks form on slightly elevated areas unharmed by deep peat fires or limestone plateaus rising several inches above the surrounding peat. Hardwood hammocks exhibit a mixture of subtropical and hardwood trees that grow in very dense clumps, such as southern live oak (

Serenoa repens) flourish, making the hammocks very difficult to penetrate. Water in sloughs flow around the islands creating moats. Though some ecosystems are maintained and promoted by fire, hammocks may take decades or centuries to recover; the moats are therefore essential for protection.[41] Islands vary in size, but most range between 1 and 10 acres (0.40 and 4.05 ha); the water slowly flowing around them limits their size and gives them a teardrop appearance from above.[42]
The height of the trees is limited by factors such as frost, lightning, and wind: the majority of trees in hammocks grow no higher than 55 feet (17 m).

Florida strangler figs (Ficus aurea) are common in hammocks, and find particular ease in rooting at the heads of cabbage palms (Sabal palmetto). After taking root into the ground, they build complex frameworks around the host tree, eventually squeezing out light and nutrients, and essentially taking its place.[43] A variety of invertebrates including beetles, ants, spiders, and tree snails support a food chain that includes frogs, owls and other birds of prey, snakes, rodents, bobcats, and raccoons. There are more than 50 varieties of tree snails in the Everglades; the color patterns and designs unique to single islands may be a result of the isolation of certain hammocks.[44]

Tropical hardwood hammocks in the Everglades have been harvested for lumber, particularly by shipbuilders seeking West Indian mahogany and black ironwood (

Krugiodendron ferreum). The largest and most mature of these trees had been removed by the late 18th century.[39] Seminoles made their villages in hammocks in the late 19th and early 20th centuries; they lived in groups of chickees numbering half a dozen, with one central chickee for cooking and another for eating. Dugout canoes, cookware, stills, and sewing machines may still be found in remote locations.[45]

Bayheads and willowheads

Some hammocks are dominated by types of vegetation that grow in relation to the amount of water or type of soil present. The majority of hardwood hammocks create a thin poor soil covering the limestone called

donut appearance from above.[47]

Flatwoods and the Atlantic Coastal Ridge

slash pines and shrubs like saw palmettos
.

The prairies and sloughs of the Everglades system are bordered by two areas of poorly drained sandy soil on both sides of Lake Okeechobee: the Eastern Flatwoods and the Western Flatwoods just north of Big Cypress Swamp. The predominant ecosystem in the Flatwoods is pine forest, but there are also cypress swamps and sloughs in the Eastern Flatwoods.

South Florida metropolitan area
is located on a portion of the Atlantic Coastal Ridge, and much of the landscape has changed drastically within the past 100 years as a result of urban growth.

Pine rockland

Tetrazygia bicolor). The most diverse group of plants in the pine community are herbs, of which two dozen species exist. These plants contain tubers and other mechanisms allowing for quick sprouts after charring.[53]

Wildlife in pine rockland communities is diverse. In some forests, 15 species of birds can be found. Common among them are the

critically endangered Florida panther (Puma concolor coryi), Florida black bear (Ursus americanus floridanus), and several types of bats also live in the pine rocklands.[50]

Before urban development of the South Florida region, pine rocklands covered around 161,660 acres (654.2 km2) in

prescribed fires
occur in Everglades National Park in pine rocklands every three to seven years.

The Big Cypress

West of the sawgrass prairies and sloughs lies the Big Cypress Swamp, commonly called "The Big Cypress", referring to its size rather than the height or diameter of its trees. It takes up the majority of Collier County; at its most limited measurement, the swamp measures 1,200 square miles (3,100 km2), but its hydrological boundary is nearly twice as large.[55][56] The Big Cypress is slightly elevated at 22 feet (6.7 m) at its highest point and slopes gradually to the coastline for approximately 35 miles (56 km). Because the defining feature of The Big Cypress is the abundance of trees it is considered a swamp, rather than a marsh where grass is the main characteristic.

The basin for The Big Cypress receives on average 55 inches (140 cm) of water in the rainy season.[57] Most of The Big Cypress sits atop a bedrock covered by a thin layer of limestone that contains quartz, creating a sandy soil that hosts a variety of vegetation.[56] The majority of trees are bald cypress (Taxodium distichum) and pond cypresses (Taxodium ascendens). Cypresses are conifers that are uniquely adapted to thrive in flooded conditions, with buttressed trunks and root projections that protrude out of the water, called "knees".[58]

Cypress trees in the area can live for hundreds of years; some giants grow to 130 feet (40 m) and are 500 years old. Still, they may be only seventh- or eighth-generation cypresses. Few massive trees survived the logging operations that took place in the 1930s and 1940s. As a result, much of The Big Cypress is protected by various federal or state agencies that include

Fakahatchee Strand State Preserve and two Indian reservations.[59]

Cypress head

A color photograph of a pond surrounded by cypress trees in standing water, featuring their flared trunks at the bottom and some water plants bordering the pond in the foreground
A pond in The Big Cypress

Although The Big Cypress is the largest growth of cypress swamps in South Florida, such swamps—as well as portions of sawgrass marshes—can be found near the Atlantic Coastal Ridge and between Lake Okeechobee and the Eastern flatwoods. Hardwood hammocks and pineland are often interspersed with the cypress ecosystem. Much like tree islands that are colloquially referred to as "heads", cypress trees grow in formations that resemble domes, with the tallest and thickest trunks in the center, rooted in the deepest peat. As the peat thins out, cypresses continue to grow, but are smaller and thinner, giving the small forest the appearance of a dome.[60] They also grow in strands, slightly elevated on a plateau of limestone and surrounded on two sides by sloughs.[61] Other hardwood trees can be found in cypress domes, such as red maple (Acer rubrum), swamp bay (Persea palustris), and pop ash (Fraxinus caroliniana). If cypresses are removed, hardwoods take over, and the ecosystem is recategorized as a mixed swamp forest.

Because the cypress domes and strands retain moisture and block out much of the sunlight, plants such as

Mycteria americana) nest almost exclusively in cypress forests and in the past 100 years have seen a dramatic decline, probably due to lack of reproduction tied to controlled water. Wood storks' reproductive cycles coincide with the dry season, when small fish and amphibians are trapped in shallow pools and puddles. When water from canals or locks is released too soon or not at all, storks are unable to find enough food for themselves and their offspring. An estimated 20,000 wood storks nested in The Big Cypress in the 1930s, but by the 1990s less than 2,000 were counted.[63]

Mangroves and coastal prairie

Red mangrove trees bordering a canal in the Everglades near Flamingo

Water from Lake Okeechobee and The Big Cypress eventually flows to the ocean. At a transitional zone where fresh water meets salt water,

brackish mixture of water and mangrove systems, crisscrossed by hundreds of tidal creeks, harbors a very productive ecosystem. The depth of these zones is dependent on how much water flows from the Everglades. In the wet season, fresh water pours into Florida Bay and sawgrass appears near the coastline. In dryer years, salt water creeps inland to the coastal prairie, an ecosystem that buffers the freshwater marshes by absorbing sea water. Mangrove trees grow in fresh water ecosystems when the salt water flows far enough inland.[64] The Everglades have the most extensive contiguous system of mangroves in the world.[65] The mangrove forests of the Ten Thousand Islands cover almost 200,000 acres (810 km2).[66]

Mangroves

Three species of mangrove trees exist in the region: red (

Laguncularia racemosa), although all are from different families.[67] All have the same characteristics: they are tolerant of salt, brackish, and fresh water; they grow in oxygen-poor soil; and they can survive drastic water-level changes.[68] Black and white mangroves excrete salt from under their leaves, and red mangroves filter the salinity of sea water. All species are integral to coastline protection during severe storms. Red mangroves, for example, have far-reaching roots that trap sediments. The trees not only stabilize coastlines, but add land as more sand and decaying vegetation is trapped in the root systems. All three mangroves also absorb the energy of waves and storm surges
.

The estuaries act as

fisheries for fry and nurseries for crustaceans. Shrimp, oysters, crabs, whelks, cockles, and snails thrive in these waters, as do primordial horseshoe crabs (Limulus polyphemus). The region supports a $59 million-a-year Tortugas pink shrimp (Farfantepenaeus duorarum) industry, and a $22 million-a-year stone crab (Menippe mercenaria) industry.[69] Between 80 and 90 percent of species that are harvested commercially in Florida are born or spend time in the shallow waters near the Everglades.[66][70] Oysters and mangroves work in tandem to build up the coastline. The sand around the coastline has minute white particles of quartz and fine shells. When currents are right, oysters grow in colonies or beds, and deposit their shells, reinforcing the bed. Mangrove seeds, called propagules, are full embryos and float in water until they reach a favorable location and take root, often on oyster beds. They shed skin and litter, ensuring other trees will not compete for space and nutrients.[71]

Mangroves also serve as excellent rookeries for birds. Wading birds, such as

birds of prey such as ospreys, hawks and vultures
are among the more than 100 species of birds that use Everglades mangrove trees to raise their young.

Florida Bay

Flamingo

Because much of the coast and inner estuaries are built by mangroves—and there is no border between the coastal marshes and the bay—the ecosystems in Florida Bay are considered part of the Everglades. More than 800 square miles (2,100 km2) of Florida Bay is protected by Everglades National Park, representing the largest body of water in the park boundaries.[73] There are approximately one hundred keys in Florida Bay, many of which are mangrove forests.[74] Larger islands may be taken over by hardwood hammocks. The outer rims of the Ten Thousand Islands and Cape Sable share characteristics of the intertwining saltwater bays and fresh water marshes.

The fresh water entering Florida Bay from the Everglades creates ideal conditions for vast beds of

Triplofusus papillosus), left-handed whelk (Sinistrofulgur), and the Florida crown conch (Melongena corona) as drinking vessels, picks, hammers, knives and awls.[76]

Sea grasses stabilize sea beds and protect shorelines from erosion by absorbing energy from waves. Shrimp,

Labor Day Hurricane of 1935 (only 146 were counted afterward).[79] After recovering to number more than 2,000, they were further endangered by Hurricane Donna in 1960, which decreased their numbers by 35 to 40 percent.[80]

Sea floor patterns of Florida Bay are formed by currents and winds. However, since 1932, sea levels have been rising at a rate of 1 foot (0.30 m) per 100 years.[81] Though mangroves serve to build and stabilize the coastline, seas may be rising more rapidly than the trees are able to build.[82]

Biodiversity

Ecosystems in the Everglades have been described as both fragile and resilient.[83] Author Michael Grunwald wrote about the observations of the Everglades' first American visitors: "If the Grand Canyon was a breathtaking painting, the Everglades was a complex drama, and everything in it had a role."[84] An estimated 11,000 species of seed-bearing plants and 400 species of land or water vertebrates live in the Everglades, but slight variations in water levels affect many organisms and reshape land formations. The health and productivity of any ecosystem relies on the number of species present: the loss of one species weakens the entire ecosystem.[85]

For example, Florida apple snails (

trophic dynamics, or food chains, the 174 species of invertebrates play a vital role in the Everglades.[88] Crayfish
, insects, scorpions, and other invertebrates also support a web of animals.

The group of animals most integral to the overall success of Everglades wildlife is freshwater fish. Few places in the Everglades stay submerged from one year to the next, so alligator holes and deep clefts in the limestone are vital to the survival of fish, and the animal community as a whole. Freshwater fish are the main diet of most wading birds, alligators, and otters, and require large areas of open water in order to repopulate. Young amphibians also play an important role in the food chain. Tadpoles spread quickly in isolated areas where fish do not have the time or access to reproduce in numbers necessary to support larger animals. Hundreds of species of amphibians are found in the Everglades, and their availability helps support wildlife during short hydroperiods or in remote locations.[89]

These smaller animals support communities of larger animals, including 70 species of land birds that breed within the Everglades, and 120 water birds, of which 43 breed in the area. Many of these birds go on to migrate through the West Indies and North America.

white tailed deer (Odocoileus virginianus), the Florida black bear, and the Florida panther.[91]

Although slight changes in water level affect many species, the system as a whole also cycles and pulses with each change. Some transformations to the diversity of plant and animal life are natural, caused by fire or storms, and some are induced by humans, such as urban encroachment, the

global warming. Environmental conditions in the Everglades favor no particular species. Some species, such as snail kites and apple snails, do well in wet conditions, but wood storks and Cape Sable seaside sparrows (Ammodramus maritimus mirabilis) do well in dryer circumstances.[83]

Human impact

Development

Main articles: Draining and development of the Everglades and Restoration of the Everglades

People have lived in the Everglades region for thousands of years. Within the past 100 years however, they have changed the natural landscape dramatically. Settlement of urban areas in South Florida was facilitated by large drainage projects intended to create more land. The drainage was often implemented without a full understanding of the intricacies of ecosystems and shaping processes of the Everglades.

South Florida metropolitan area grew exponentially, causing problems in ecosystems throughout the Everglades. By the 1990s, the diminishing quality of life in many of these urban areas was linked to the degraded local environment.[93] The State of Florida and the U.S. government devised and passed a plan in 2000 to restore as much of the Everglades to pre-drainage conditions as possible. It is the costliest and most comprehensive environmental restoration project in history.[94]

Invasive species

Main articles: List of invasive species in the Everglades and Burmese pythons in Florida

Humans have also adversely impacted the ecology of the Everglades by introducing numerous invasive species, which may prey on or compete with native species. A spectacular and particularly damaging example of this phenomenon is the recent proliferation of the Burmese python in the Everglades, as well as elsewhere in Florida. First observed in the wild in 1979 and not again until 1995,[95] they have increased alarmingly since 2000.[96] By 2011, decreases of 87.5%, 94.1%, 98.9% and 99.3% in sightings of bobcats, white-tailed deer, opossums and raccoons, respectively, were reported in park road surveys, while rabbits were no longer being seen at all.[96]

Climate change and sea level rise

Main article: Climate change in Florida

Mangroves are threatened in the Everglades, due to climate change resulting in sea level rise.[97]

See also

Notes and references

  1. ^ Lodge, p. 13.
  2. ^ U.S. Geological Survey (2004). "Environmental Setting – The Natural System: Watersheds and Coastal Waters (Big Cypress Watershed)". Circular 1134: The South Florida Environment – A Region Under Stress. U.S. Department of the Interior. Retrieved 2008-03-17.
  3. ^ a b c d McCally, p. 18–21.
  4. ^ a b c McCally, pp. 9–10.
  5. ^ Lodge, p.14.
  6. ^ Lodge, pp. 18–19.
  7. ^ U.S. Geological Survey (2004). "Environmental Setting – The Natural System: Climate". Circular 1134: The South Florida Environment – A Region Under Stress. U.S. Department of the Interior. Retrieved 2008-03-17.
  8. ^ Obeysekera, Jayantha; Browder, J.; Hornrung, L.; Harwell, M. (October 1999). "The natural South Florida system I: Climate, geology, and hydrology". Urban Ecosystems. 3 (3/4). Kluwer Academic Publishers: 223–244.
    S2CID 2526625
    .
  9. ^ Lodge, p. 21.
  10. ^ Hurricane Research Division (2008). "Atlantic hurricane best track". NOAA. Archived from the original on 2008-09-16. Retrieved 2008-05-03.
  11. ^ Lodge, p. 89.
  12. ^ Jewell, p. 35.
  13. ^ Lodge, pp. 89–93.
  14. ^ Toops, p. 95.
  15. ^
    ISBN 0-9634030-2-8
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  92. ISBN 0-9634030-2-8
  93. ^ "Chapter 1: Background and understanding". The Governor's Commission for a Sustainable South Florida. State of Florida. October 1, 1995. Archived from the original on May 18, 2011. Retrieved 2008-05-23.
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Bibliography

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