Natural History of the Okefenokee Swamp
The largest swamp in North America, the Okefenokee Swamp covers roughly 700 square miles and is located in the southeastern corner of Georgia, Charlton and Ware counties and parts of Brantley and Clinch counties. The swamp has a distinctive and fascinating natural history. Cypress swamps, winding waterways, and floating peat mats are a major part of the Okefenokee's habitat mosaic. Wet and dry prairies, swamps dominated by shrubs, and forests of black gum and bay trees intersperse the array of other habitats. A high ridge of sand known as Trail Ridge forms the eastern edge of the swamp. Wildlife abound; more than 400 species of vertebrates, including more than 200 varieties of birds and more than 60 kinds of reptiles, are known to inhabit the swamp.
A mix of geological events, environmental variables, and human impact has shaped the character of the Okefenokee Swamp. More than sixty-five million years ago, during the Cretaceous geological period, the region was beneath the sea. Marine sediments produced a deep layer of sandy, nutrient-poor soils. In more recent geologic times the depression forming the basin of the present-day Okefenokee Swamp was presumably created by wave action associated with an offshore sandbar. Today the depression is filled with fresh water and peat to create what Seminoles called the "land of trembling earth."
In logging operations beginning in 1910 and lasting for a quarter of a century, thousands of cypress, pine, and red bay trees were removed from the swamp. Some were among the largest and oldest individuals of their kind left in the country. In 1937 U.S. president Franklin D. Roosevelt provided official protection from logging and development by establishing the Okefenokee National Wildlife Refuge, which constitutes about 80 percent of the swamp. The absence of roads helps to maintain the integrity of the swamp ecosystem; canoe trails are the primary travel routes through the swamp.
In the subtropical climate, rainfall is approximately fifty inches a year and is the source of most of the water entering the swamp from the more than 1,400 square miles of upland watershed. The clear, tannin-stained, highly acidic waters of the Okefenokee generally are shallow, normally ranging up to depths of less than ten feet and averaging only two feet.
Most (about 85 percent) of the water leaving the Okefenokee is carried by the Suwannee River to the Gulf Coast of Florida. The St. Marys River, which flows into the Atlantic, drains the remainder of the swamp.
Because of its immensity and its physical and chemical attributes, the Okefenokee Swamp has a blend of habitats
The combination of physical and chemical features also has molded the swamp's natural history. The low-nutrient and acidic conditions have created ideal habitats for carnivorous plants, which attract, capture, and digest animals to compensate. Several species of large pitcher plants as well as smaller sundews and butterworts, which capture insects with a gluelike surface film on their leaves, are scattered throughout the swamp. Also present are bladderworts, aquatic carnivorous plants with tiny air-filled traps, called bladders, which snap shut when mosquito larvae or zooplankton trip the hair trigger.
The terrestrial and aquatic portions of the swamp support about thirty species of native mammals. Large terrestrial mammals include black bears, white-tailed deer, and bobcats. Smaller terrestrial carnivores are gray foxes, opossums, and raccoons. Aquatic species include otters, minks, and beavers. Two species of rabbits are associated with the Okefenokee Swamp, the cottontail, inhabiting higher ground, and the marsh rabbit, found in wetter habitats.
After birds, reptiles make up the most diverse group of vertebrates. American alligators and five species of venomous snakes are indigenous to the swamp, the most obvious and ecologically dominant being the alligator. The vocal communications of alligators during both day and night, coupled with protective maternal behavior,
The Okefenokee, with its continual array of wetland habitats, provides ideal situations for egg laying and larval development for three dozen kinds of amphibians. After nightfall, when most birds fall silent, swamp sounds begin anew from the more than twenty species of indigenous frogs and toads. As with birds, the call of each frog species is distinctive. Pig frogs and river frogs are similar in appearance to bullfrogs, which are absent from the swamp. Pig frogs, grunting both day and night, are the dominant vocalizers in most areas. The less common river frogs make a sound like deep snoring. The chuckles of leopard frogs are commonly heard in some areas. Warm rains bring forth southern toads with their trills and narrow-mouthed toads with their sheeplike bleating. Wailing choruses of eastern spadefoot toads can be heard over long distances after heavy rainfalls. A wide variety of tree frogs and their relatives inhabit the Okefenokee Swamp, including green tree frogs and barking tree frogs during the warm months and several species of chorus frogs that give their melodic calls during the winter months. Less obvious amphibians include the salamanders—two are giant salamanders, permanently aquatic creatures that reach lengths of more than three feet.
Although every species of plant or animal in the Okefenokee Swamp also can be found in other regions of the Southeast, the collective biodiversity creates a wildlife array of natural history that is unparalleled. All life forms in the swamp and its surrounding areas have adaptations that permit the existence of high biodiversity living under the singular environmental conditions of the Okefenokee Swamp.
Media Gallery: Natural History of the Okefenokee Swamp