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Project, and Lake Belt Storage Projects. The Coastal
Wetlands Project has the objective of restoring the historic water supply patterns through wetlands to the
southern Biscayne Bay. Wastewater reuse has the potential to affect bay water quality. The remaining projects listed all directly affect the amount of fresh water
available to Biscayne Bay.
To guide a science-based, adaptive-management approach to water-management planning, a conceptual
ecological model of Biscayne Bay was developed
based upon a series of open workshops involving researchers familiar with Biscayne Bay. Since the adaptive management process for CERP is the context in
which this conceptual model was developed and will
be used, the emphasis of the Biscayne Bay CEM is on
the relationship between the bay ecology and the mainland shoreline and freshwater sources.
EXTERNAL DRIVERS AND ECOLOGICAL
STRESSORS
In the Biscayne Bay Conceptual Ecological Model
(Figure 2), the two principal drivers applicable to the
Comprehensive Everglades Restoration Plan (CERP)
are watershed development and water management.
They exert their effects through four principal stressEXHIBIT 7
Browder et al., Biscayne Bay CEM 857
ors: toxicant and pathogen inputs, altered solids and
nutrient inputs, altered freshwater inflow, and operation of physical structures, particularly water-control
structures and maintenance of infrastructure. Altered
freshwater flow is the stressor that CERP will most
directly affect and includes flow volume, velocity, timing and spatial distribution. CERP may indirectly affect the input of solids, nutrients, toxicants, and pathogens.
Construction of the major canals through the Everglades and dredging of natural tributaries and transverse glades that carried fresh water to Biscayne Bay
resulted in lowered regional and coastal water tables
(Parker et al. 1955), reduced water storage in the watershed, decreased ground-water flow to the bay, and
the elimination of many tributaries. Drainage of the
watershed greatly affected the natural salinity gradients and ecotones from the Everglades through coastal
wetlands and tidal creeks into the bay, and reduced or
eliminated critical estuarine habitat for bay species requiring low-to-moderate salinity waters. In addition,
constructed drainage systems result in pulsed, pointsource discharge degrading estuarine habitat near canal
mouths by creating biologically damaging zones of
bottom scouring and rapid salinity fluctuations. Departures from natural salinity patterns are ecologically
damaging to many species because salt concentration
affects growth, survival, reproduction, and other critical physiological processes in both plants and animals
(see, for example, Kinne [1971]). The general lowering of the water table on the east-coast ridge and diversion of both surface and ground water into canals
has degraded not only estuarine habitats within the
bay, but also adjacent coastal wetland communities,
including herbaceous freshwater marshes and coastal
mangrove wetlands that were once functionally connected to the estuarine habitats. The few coastal tropical hammocks that remain have also been detrimentally affected by the lowered water table (M. Roessler,
pers. comm.).
The bay has also been significantly affected by the
watershed development made possible by water management (Alleman et al. 1995). Before drainage of the
watershed, urban and agricultural development was restricted to the highest ground along the Atlantic Coastal Ridge, consisting of hammocks and pinelands (University of Miami and SFWMD 1995). As land was
drained, development encroached into lower lands and
former wetlands. Today, most new development is occurring in former wetlands.
Development has had many detrimental consequences. The continued loss of open, pervious land
increases stormwater runoff velocity and pollutant
loads and reduces the quantity of water storage in the
watershed. Other dramatic changes occurred in northern Biscayne Bay as a result of dredging and filling.
Bottom dredging resulted in the loss of seagrass beds
in northern Biscayne Bay and has affected the stability
of bay sediments and the capacity to assimilate nutrients and trap particulates. Stormwater runoff from urban development has increased the bay’s exposure to
contaminants and excessive nutrients. At the same
time, the filling and destruction of coastal wetlands has
eliminated natural filtering capacity. The dredging of
inlets at Haulover and Government Cuts significantly
increased salinity in northern Biscayne Bay (Wanless
1969, Wanless et al. 1984), changing much of it from
an estuarine to a more marine system.
Biscayne Bay’s water quality has improved substantially in the past 30 years because of the elimination
of direct discharge of sewage into the bay and other
pollutant-control measures (McNulty 1970, Alleman et
al. 1995, DERM 2005a). Parts of North Biscayne Bay
now support substantial seagrass beds. Extensive seagrass beds have always been characteristic of South
Biscayne Bay. In recognition of its exceptional values,
the State of Florida has designated the bay and its
natural tributaries as Outstanding Florida Waters, and
as such, they receive the highest level of state protection from degradation. Present water quality generally
meets or exceeds federal, state, and local standards for
recreational use and propagation of fish and wildlife.
Nonetheless, the bay still receives dissolved nutrients,
trace metals, organic chemicals, and suspended sediments via stormwater runoff, sewage overflows, discharges from industrial facilities or vessels, and canal
discharges. Canal water typically has lower dissolved
oxygen and clarity and higher concentrations of contaminants than receiving waters of the bay.
ECOLOGICAL ATTRIBUTES
Ecological attributes of the overall health of the Biscayne Bay ecosystem include four types of habitat:
seagrass meadows, mangrove forests, herbaceous wetlands, and benthic faunal communities (both soft bottom and hard bottom). Ecological attributes that have
been defined because of their special relevance and
utility for monitoring and reporting the state of the bay
include pink shrimp (Farfantepenaeus duorarum Burkenroad), blue crabs (Callinectes sapidus Rathbun),
stone crabs (Menippe mercenaria Say), oysters, estuarine fish communities, fish and bottlenose dolphin
(Tursiops truncatus Montagu) health, crocodiles (Crocodylus acutus Cuvier), West Indian manatees (Trichechus manatus latirostris Linnaeus), and wading
birds.
EXHIBIT 7
858 WETLANDS, Volume 25, No. 4, 2005
Seagrass Habitat
Large areas of the bay bottom support seagrass communities because sediment depth and nutrients are sufficient, water depths are shallow, and water clarity is
high. Seagrass has been documented to cover up to
64% of the bay bottom (DERM 1985). There is very
little area of bare bottom with sufficient sediment to
support seagrass except where there has been a physical disturbance such as dredging. Seagrass beds function as vital habitat to support critical life stages of a
variety of ecologically important and commercially or
recreationally valuable species. At least seven species
of seagrasses occur in Biscayne Bay: turtle grass
(Thalassia testudinum Banks & Soland. ex Koenig),
shoal grass (Halodule wrightii Aschers.), manatee
grass (Syringodium filiforme Kuetz.), three species of
Halophila, including H. johnsonii (Eiseman), which is
a federally-listed protected species, and Ruppia maritime (Linnaeus). Distribution of seagrass species is