geography and ecology of the everglades
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Geography and ecology of the Everglades 1
Geography and ecology of the Everglades
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.
The geography and ecology of the Everglades involve the
complex elements affecting the natural environment
throughout the southern region of the U.S. state of Florida.
Before drainage, the Everglades were an interwoven mesh of
marshes and prairies covering 4,000 square miles ( km2).
The Everglades is simultaneously a vast watershed that has
historically extended from Lake Okeechobee 100 miles ( 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 fresh water from Lake
Okeechobee makes its way to Florida Bay, it meets salt water 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 sea grasses and aquatic
life are attracted to the constant discharge of fresh water.
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.
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Geography and ecology of the Everglades 2
Shaping processes of ecosystems
Water
A storm over the Shark River in the Everglades,
1966
Photo:Charles Barron / State Library and
Archives of Florida
At only 5,000 years of age, the Everglades is a young region in
geological terms. Its ecosystems are in constant flux due to three
factors: the type and amount of water present, the geology of the
region, and the frequency and severity of fires.[2][3]
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 arid and semi-arid, interspersed with wet periods.
Between 10,000 and 20,000 years ago, sea levels rose, submerging
portions of the Florida peninsula and causing the water table to rise.
Fresh water saturated the limestone, eroding some of it and creating
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
plateausa difference of inches in elevationthat 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 KissimmeeLake OkeechobeeEverglades (KLOE) watershed. Kissimmee River outlets flow
into Lake Okeechobee, which sits 18 feet ( 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
( 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 ( km) to Florida Bay. The gradient change is so slight that the
river moves only 2 feet ( 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 tropical storms and hurricanes, also affects the structure of the Everglades. Between
1871 and 2003, 40 tropical cyclones struck the Everglades, usually every one to three years.[10][11]
These storms
alter the coastline, flush decaying vegetation from estuaries, strip weakened branches from trees, and disperse seeds,
pollen, and plant material.[12]
Hurricane Donna in 1960 affected 120 square miles ( km2) of mangrove forests by
depositing marl over the roots and depriving the trees of oxygen. It also eradicated 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]
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Geography and ecology of the Everglades 3
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 storedin 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 ( 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.[3]
The first cycle is the
annual wet-season fires that occur with rapid frequency during the summer, but are quickly extinguished. Dry-season
fires are rarer due to the lack of lightning, but their damage may be more pervasive.[20]
A longer fire cycle spanning
ten to fourteen years coincides with similar water cycles affected by global climate conditions. Fires in this cyclemay be numerous and have little effect, or rare and have catastrophic consequences. The third cycle appears in a
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Geography and ecology of the Everglades 4
550-year frequency associated with severe drought. Layers of charcoal have been detected inside peat in parts of the
Everglades, indicating the region endured severe fires for years at a time, although this trend seems to have abated
since the last occurrence around 940 BCE.[3]
Ecosystem characteristics
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. An early
American environmentalist named 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 ( km) long and 60 miles ( km) wideflowing 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 ( m) tall, and directly south of Lake Okeechobee it has grown to 10 feet ( m).
Farther south, where the peat is not as rich, it typically grows 4 feet ( 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 alligators often choose these locations
for nesting. Where there is more room, periphyton grows, appearing as mats or brown sausage-shaped chunks.
Periphyton is predominantly algae, although over 100 different microorganisms help create it.[28]
Larval insects and
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 ( m), and may stay flooded for at least 11 months out of the year if not multiple years in a
row.[30]
The peat beds that support sawgrass are slightly elevated and may begin abruptly creating ridges of grass.
The borders between these systems are called "ridge-and-slough" landscapes. Aquatic animals such as turtles, young
alligators, snakes, and fish live in sloughs and they usually feed on aquatic invertebrates, such as the Florida apple
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Geography and ecology of the Everglades 5
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 cross section of fresh water ecosystems in the Everglades, with relative average water depths
Wet prairie
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 limestonethat 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
( 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 ( 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]
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Geography and ecology of the Everglades 6
Tropical hardwood hammock
In a tropical hardwood hammock,
plants are very dense and diverse.
Islands of trees featuring dense temperate or tropical trees are called tropical
hardwood hammocks.[38]
They may rise between 1 and 3 feet (unknown
operator: u'[' and unknown operator: u'[' 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 (Quercus virginiana), gumbo limbo (Bursera simaruba), royal
palm (Roystonea), and willow bustic (Dipholis salicifolia).
[40]
Near the bases of hammocks sharp saw palmettos(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 (unknown operator: u'[' and unknown operator: u'[' 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 ( 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 humus, made of
decaying plant matter and moisture trapped by the structure of the trees. When peat forms the layer atop the
limestone of a tree island, bayheads develop, dominated by bay trees such as sweetbay magnolia (Magnolia
virginiana) and others like swamp holly (Ilex decidua), wax myrtle (Myrica cerifera), and cocoplum (Chrysobalanus
icaco).[46]
Willowheads, dominated by willow trees (Salix caroliniana), take hold where the hydroperiod is long,
usually around solution or alligator holes, and may surround the holes, giving them a donut appearance from
above.[47]
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Geography and ecology of the Everglades 7
Flatwoods and the Atlantic Coastal Ridge
The Pine rockland ecosystem is dominated by
South Florida 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.[48]
Along the eastern border of the Everglades is the
Atlantic Coastal Ridge, rising 20 feet ( m) in elevation, and curving to
the southwest, gradually decreasing in elevation until it meets Taylor
Slough. The Coastal Ridge prevents Everglades water from flowing
into the Atlantic Ocean to the east, directing it southwesterly into
Florida Bay. The 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
Pine rocklands (also called pinelands) are found on uneven limestone substrates that contain pinnacles and solution
holes. There are three primary locations of pine rocklands: the Miami Ridge, which runs from Miami into Long Pine
Key near the main entrance of Everglades National Park; the lower Florida Keys; and the Big Cypress Swamp.[49]
The most significant feature of the pine rockland ecosystem is the South Florida slash pine (Pinus elliotti var densa;
also called Dade County pine) that reaches a height of 22 feet ( m). Pine rockland communities require fire for
maintenance; they have adapted to promote and resist fire at the same time.[50]
These communities are located in the
highest part of the Everglades with little to no hydroperiod, although some floors may have flooded solution holes or
puddles for a few months at a time. The sandy floor of the pine rocklands is covered with dry pine needles that are
highly flammable. South Florida slash pines are insulated by their bark to protect them from heat. Fire eliminatescompeting vegetation on the forest floor, and opens pine cones to germinate seeds.
[51]A period without significant
fire can turn pineland into hardwood hammock as larger trees overtake the slash pines.[52]
The understory shrubs in
pine rocklands include fire-resistant species like saw palmetto (Serenoa repens), cabbage palm (Sabal palmetto), and
West Indian lilac (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 pine warbler (Dendroica pinus), the red-bellied woodpecker (Melanerpes carolinus), and the eastern
meadowlark (Sturnella magna). More than 20 species of reptiles and amphibians have been noted, such as the green
anole (Anolis carolinensis), southern leopard frog (Rana sphenocephala), and southern black racer (Coluber
constrictor priapus). Mammals such as 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 ( km2) in
Miami-Dade County. Pine forests were extensively cleared by urban developers and the lumber industry in the 1930s
and 1940s.[50]
Within Everglades National Park, 19,840 acres ( km2) of pine rockland communities are protected, but
outside the park, 1,780 acres ( km2) of pine forests remain as of 1990, averaging 12.1 acres ( km
2) in size.
[50]Dade
County pine has a remarkable longevity and has proven to be termite-resistant, though dense enough to make driving
nails difficult.[54]
In 1984 they were protected by a county ordinance, after many pine areas had been depleted. A
misunderstanding of fire's role also played a part in the disappearance of pine forests, as natural fires were put out
and pine rocklands transitioned into hardwood hammocks.[50]
Today prescribed fires occur in Everglades National
Park in pine rocklands every three to seven years.
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Geography and ecology of the Everglades 8
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 ( km2), but its hydrological boundary is nearly
twice as large.[55][56]
The Big Cypress is slightly elevated at 22 feet ( m) at its highest point and slopes gradually to
the coastline for approximately 35 miles ( km). Because the defining feature of The Big Cypress is the abundance oftrees, it is considered a swamp rather than a marsh, in which grass is the main characteristic.
The basin for The Big Cypress receives on average 55 inches ( 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 not true cypresses
(Cupressaceae). 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 ( 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 Big Cypress National Preserve, Corkscrew Swamp Sanctuary, Fakahatchee Strand State
Preserve and two Indian reservations.[59]
Cypress head
A pond in The Big Cypress
Although The Big Cypress is the largest growth of cypress swamps in
South Florida, such swampsas well as portions of sawgrass
marshescan 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 orchids,bromeliads, and ferns thrive in cypress domes and strands. Orchids bloom throughout the year in cypress heads, and
bromeliads appear in many varieties; on Fakahatchee Strand alone, thirteen species have been documented.[62]
Bromeliads collect moisture from rain and humidity in the bases of their leaves, which also nurture frogs, lizards and
various insects. Wood storks (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]
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Geography and ecology of the Everglades 9
Mangrove 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,
mangrove trees thrive, adapted as they are to both kinds of water. This
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 ( km2).
[66]
Mangrove
Three species of mangrove trees exist in the region: red (Rhizophora mangle), black (Avicennia germinans), and
white (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 roseate spoonbills (Platalea ajaja),
egrets, and tricolored herons (Egretta tricolor) use the mangroves as a nursery, due to the proximity of food sources
and the protection offered from most prey. Thousands of birds can nest in the mangroves at once, making a noisy
and messy colony, but their droppings fertilize the mangrove trees.[72]
Shorebirds like rails, terns and gulls; diving
birds such as pelicans and grebes; and 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.
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Geography and ecology of the Everglades 10
Florida Bay
A clump of mangroves in the distance, Florida
Bay at Flamingo
Because much of the coast and inner estuaries are built by
mangrovesand there is no border between the coastal marshes and
the baythe ecosystems in Florida Bay are considered part of the
Everglades. More than 800 square miles ( 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 turtle grass and algae formations that foster animal life in the bay. Sea turtles and
manatees (Trichechus manatus latirostris) eat the grass, while invertebrates such as worms, clams, and other
mollusks consume algae formations and microscopic plankton.
[75]
Female sea turtles return annually to nest on theshore, and manatees spend the winter months in the warmer water of the bay. The Calusa Indians had various uses
for shells of marine invertebrates, due to the lack of dense rock with which to make tools. They used the horse conch
(Pleuroploca gigantea), left-handed whelk (Busycon contrarium), 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, spiny
lobsters, and sea urchins live in and among the grasses and feed on phytoplankton; they in turn feed larger predators
such as sharks, rays, barracuda, and king mackerel (Scomberomorus cavalla).[77]
Due to shallow water and abundant
sunlight, Florida Bay hosts communities of coral reefs and sponges, although the majority of the state's reefs are
closer to the Florida Keys.[78]
Everglades keys that foster mangroves also support nurseries for wading birds such as
the Great white heron (Ardea herodias), which was almost wiped out in the 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 ( 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 (Pomacea paludosa) are an amphibious fresh water mollusk.[86]
They have a
single gill and lung, and live on stalks of sawgrass in water depths no more than 20 inches ( cm). They are the
primary food of the endangered Everglades snail kite (Rostrhamus sociabilis) and limpkin (Aramus guarauna) as
well as the raccoon, otter, and young alligator. Apple snails lay their eggs on sawgrass stalks about 6 inches ( cm)
above the water line, and they are intolerant of being submerged for long periods of time. When the eggs hatch,
young snails must enter the water quickly or face death. When water levels are too low or rise too quickly while snail
eggs are developing, apple snails do not flourish, affecting the many reptiles, mammals, and birds that feed on
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Geography and ecology of the Everglades 11
them.[87]
With regard to the ecology of 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 wi ldlife 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 animportant 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.[90]
Several dozen species of mammals also thrive in the region, from tiny bats and
shrews to midsize raccoons (Procyon lotor), otters (Lontra canadensis), opossums (Didelphis virginiana), and foxes.
The largest include 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 introduction of exotic species, and rapid 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
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.[92]
Though the South Florida metropolitan
area grew exponentially, the result caused chaos 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]
Notes and references
[1][1] Lodge, p. 13.
[2] U.S. Geological Survey (2004). "Environmental Setting - The Natural System: Watersheds and Coastal Waters (Big Cypress Watershed)"(http://sofia.usgs.gov/publications/circular/1134/esns/bcw.html). Circular 1134: The South Florida Environment - A Region Under
Stress. U.S. Department of the Interior. . Retrieved 2008-03-17.
[3] McCally, p. 1821.
[4] McCally, pp. 910.
[5][5] Lodge, p.14.
[6] Lodge, pp. 1819.
[7] U.S. Geological Survey (2004). "Environmental Setting - The Natural System: Climate" (http://sofia.usgs.gov/publications/circular/1134/
esns/clim.html). 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 (Kluwer Academic Publishers) 3 (3/4): 223244. doi:10.1023/A:1009552500448.
[9][9] Lodge, p. 21.
[10] Hurricane Research Division (2008). "Atlantic hurricane best track" (http://www.aoml.noaa.gov/hrd/hurdat/tracks1851to2007-apr08.
txt). NOAA. . Retrieved 2008-05-03.
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Geography and ecology of the Everglades 12
[11][11] Lodge, p. 89.
[12][12] Jewell, p. 35.
[13] Lodge, pp. 8993.
[14][14] Toops, p. 95.
[15] Gleason, Patrick, Peter Stone, "Age, Origins, and Landscape Evolution of the Everglades Peatland" inEverglades: The Ecosystem and its
Restoration, Steven Davis and John Ogden, eds. (1994), St. Lucie Press. ISBN 0-9634030-2-8
[16] McCally, pp. 1214.
[17] McCally, pp. 15
17
[18][18] Lodge, p. 38.
[19][19] SFWMD (2010), p. 6-3.
[20] Lodge, pp. 3941.
[21] Schaffraneck, Raymond; Ami L. Riscassi, Nancy B. Rybicki, Alfonso V. Lombana (September 3, 2003). "Fire Effects on Flow in Vegetated
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[22][22] Grunwald, p. 12.
[23][23] George, p. 13.
[24][24] Douglas, p. 11.
[25][25] Whitney, p. 168.
[26] Lodge, pp. 2527.
[27][27] Jewell, p. 46.[28][28] Whitney, p.168.
[29][29] George, p. 42.
[30][30] Lodge, p. 31.
[31][31] George, p. 14.
[32] Whitney, p. 114115.
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[34][34] Whitney, p. 164.
[35][35] Whitney, p. 163.
[36] George, pp. 4546.
[37][37] Lodge, p. 35.
[38][38] George, p. 30.
[39][39] Lodge, p. 55.
[40] Douglas, pp. 4849.
[41][41] George, p. 31.
[42][42] Toops, p. 53.
[43][43] Lodge, p. 58.
[44][44] Toops, p. 57.
[45][45] Toops, p. 61.
[46][46] George, p. 39.
[47] Lodge, pp. 4546.
[48][48] McCally, p. 9.
[49][49] Jewell, p. 45.
[50] U.S. Fish & Wildlife Service. " South Florida Multi-Species Recovery Plan: Pine rockland (http://www.fws.gov/southeast/vbpdfs/
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[51] George, pp. 7
8.[52] "Land and Resource Management Projects" (http://sofia.usgs.gov/publications/reports/doi-science-plan/managefire.html).DOI science
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[55][55] Lodge, p. 67.
[56][56] George, p. 26.
[57][57] Ripple, p. 16.
[58][58] Jewell, p. 43.
[59] Ripple, pp. 1920.
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[65] Katherisen, K. (2001). "Biology of Mangroves and Mangrove Ecosystems",Advances in Marine Biology, Alan J. Southward (ed.) 40,
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[79][79] Toops, p. 88.[80][80] Williams, p. 26.
[81][81] Lodge, p. 100.
[82][82] Lodge, p. 104.
[83][83] Toops, p. 92.
[84][84] Grunwald, p. 14.
[85][85] Whitney, p. 383.
[86][86] Whitney, p. 241.
[87][87] Lodge, p. 136.
[88][88] Lodge, p. 140.
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[90] Lodge, pp. 183185.
[91] Lodge, pp. 175180.
[92] Light, Stephen, Dineed, J. Walter, "Water Control in the Everglades: A Historical Perspective", inEverglades: The Ecosystem and its
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Article Sources and Contributors 15
Article Sources and ContributorsGeography and ecology of the Everglades Source: http://en.wikipedia.org/w/index.php?oldid=520131769 Contributors: Acroterion, Bender235, Bibliomaniac15, Biruitorul, CapeVerdeWave,
Casliber, Climie.ca, Dank, Epbr123, Epipelagic, Eustress, Fairy gal123, Fiftytwo thirty, Glane23, Guettarda, Juliancolton, Kakofonous, Kevmin, LindsayH, Melchoir, Michael Devore, Miguel.v,
Miq, Moni3, Neutrality, Noles1984, Persephone's Lot, R'n'B, Rjwilmsi, Robert1947, SandyGeorgia, Scartol, Shyamal, Skizzik, Soundvisions1, StAnselm, Sun Creator, TDogg310, Theo F,
Tony1, Wadewitz, Wavelength, 7 anonymous edits
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Geological Survey
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CharlesNOTE: Attribution must be given when image is used. S uggested: Photo:Charles Barron / State Library and Archives of Florida (See Title XVIII, Chapter 257, section 35.6 (c) :Any use or
reproduction of material deposited with the Florida State P hotographic Collection shall be allowed pursuant to the provisions of paragraph (1)(b) and subsection (4) provided that appropriate
credit for its use is given.)
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1887-1971.
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File:Magnify-clip.png Source: http://en.wikipedia.org/w/index.php?title=File:Magnify-clip.png License: Public Domain Contributors: User:Erasoft24
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Image:Big cypress.jpg Source: http://en.wikipedia.org/w/index.php?title=File:Big_cypress.jpg License: Public Domain Contributors: U.S. Geological Survey
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