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Geography and ecology of the Everglades

Natural environment in southern Florida, US

  • 28 min read
  • 8 chapters
Satellite image of the lower Florida peninsula. The darkened portion south of Lake Okeechobee is the Everglades.
US Geological Survey · Public domain

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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. 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 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.

Water

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. 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 the flow of water and types of vegetation present.

The Everglades are unique; no other wetland system in the world is nourished primarily from the atmosphere. 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. The Kissimmee River flows into Lake Okeechobee, which sits 18 feet (5.5 m) above sea level. 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. Droughts, floods, and tropical storms are normal occurrences in the area. 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. 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. These storms alter the coastline, flush decaying vegetation from estuaries, strip weakened branches from trees, and disperse seeds, pollen, and plant material. Hurricane Donna in 1960 affected 120 square miles (310 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. 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.

Geology

A vast marshland could only have been formed due to the underlying rock formations in southern Florida. 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. 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. The length of time that a region in the Everglades remains flooded, called a hydroperiod, 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. 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. 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. 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.

Fire

Fire is another important element in the maintenance of the Everglades. The majority of fires 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. Large burned areas also affect waterflow, since wind and water are unimpeded by the eradicated sawgrass; water may flow two to three times faster in recently burned areas. 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 might be, given the 5,000 years of the Everglades' existence. Scientists point to fire as the reason.

Researchers have noted that fires appear in cycles associated with those of the hydroperiods. 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. A longer fire cycle spanning ten to fourteen years coincides with similar water cycles affected by global climate conditions. Fires in this cycle may be numerous and have little effect, or rare and have catastrophic consequences. The third cycle appears in a 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.

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