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Abstract

The Everglades is a freshwater wetland located in southern Florida. It originated 5500 years ago when rising waters of Lake Okeechobee and its vicinity fostered deposition of wetland soils through former uplands with widely exposed bedrock. Its development occurred in the presence of, and under the influence of Native Americans, their occupation having predated the Everglades by thousands of years. Prior to regional drainage, which began in the 1880s, the Everglades covered about 4000 square miles. It sloped southward at about 2.5 inches per mile from Lake Okeechobee to coastal tidal waters at the south end of Florida’s mainland. Just over half of the Everglades remains today, mostly broken into water-conservation impoundments controlled by levees and canals with only Everglades National Park at the south end still free-flowing. Pristine areas of the Everglades are oligotrophic, consisting mostly of marshes rich in periphyton. The marshes and periphyton are rapidly degraded by phosphorus enrichment over the maximum background of 10 ppb. Other enrichment of concern is sulfur and its association with elevated methylmercury, the latter biomagnified in Everglades fauna. Everglades marsh landscapes include long-hydroperiod sloughs (flooded 11+ months annually) and intermediate-hydroperiod sawgrass ridges (flooded 9–10 months), both underlain by peat soils, and smaller areas of short-hydroperiod, mixed-herb marshes (mostly flooded 3–7 months) underlain by marl. The latter occur around the edges of the southern Everglades. Unevenly distributed through these marshes are tree islands of several kinds based on their genesis and flora. One type was frequented through history by Native Americans, which influenced island development. Recent work has demonstrated the role of water flow in the evolution and maintenance of marsh and tree-island landscape features, all aligned with the pre-drainage direction of flow. Other Everglades features include small ponds called alligator holes that have various origins but are maintained by alligators and are ecologically important. Surrounding the Everglades are other plant communities, principally forests, and most outflows of water from the Everglades pass through extensive and highly productive tidal mangrove swamp forests before entering shallow marine waters at the south end of the system. Everglades wildlife responds to summer wet-season and winter-spring dry-season cycling, which characterizes southern Florida’s nearly tropical climate. Many introduced plants and animals have stressed the natural Everglades ecosystem, which supports 68 threatened and endangered species. Restoration efforts are in progress. Phosphorus reduction, initiated in the mid-1990s, has been successful but short of compliance targets. Overall ecosystem restoration is ongoing but slow. In combination with phosphorus reduction, it involves revision of South Florida’s water-control system to ensure the right quality, timing, and distribution of water.

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Notes

  1. 1.

    The name “Everglades” is used here a singular noun following most technical literature such as Loveless (1959), Davis and Ogden (1994), and McVoy et al. (2011). The plural form was used in an 1848 federal reconnaissance report (U.S. Senate 1911) and is common in popular literature such as Douglas (1947). The author discussed this issue with Ms. Douglas, who agreed, “Singular is appropriate but both are grammatically correct.”)

  2. 2.

    The name “red bay” is entrenched in Evergades literature as a bayhead species, referenced to the scientific name Persea borbonia. However, two varieties occur in the region and are now usually recognized as separate species: swamp bay (P. palustris), which tolerates shallow flooding for a month or more, is common in the Everglades; and red bay (P. borbonia), which is less tolerant of flooding and unusual or absent in the Everglades (Wunderlin et al. 2016; Nelson 2011). In lumping both together, a wide hydrologic tolerance is shown, as in Wetzel et al. 2017)

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Lodge, T.E. (2019). Overview of the Everglades. In: D. Pollman, C., Rumbold, D., Axelrad, D. (eds) Mercury and the Everglades. A Synthesis and Model for Complex Ecosystem Restoration . Springer, Cham. https://doi.org/10.1007/978-3-030-20070-1_1

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