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Wetlands have the capacity to improve water quality by filtering pollutants and sediments from
flowing waters. As water flows through wetlands it undergoes certain changes, primarily as a result
of: 1) a reduction in the velocity of flowing water as it enters or passes through a wetland, 2)
decomposition of organic substances, 3) metabolic activities of plants and animals, 4) photosynthesis,
and 5) sediment binding of ions and particles. Because of this capacity to improve the quality of
water, natural and artificial wetlands have been used for the treatment of waste waters (Sather and
Smith, 1984).
The ability of wetland systems to bind nitrogen and phosphorus is reviewed by Adamus (1983).
This function depends upon several attributes, including the capacity of the vegetation, on a net
annual basis, to assimilate and transfer to deep sediments more nutrients than are released through
leaching and decay. The substrate of the wetland system accumulates organic matter on a net annual
basis. Generally, sediments accrete faster than they are removed, and the rate of denitrification in
wetland soils consistently exceeds the rate of nitrogen fixation.
In an attempt to counter achievement of economic gains through development of wetlands,
several studies have been performed to place a defensible monetary value on wetlands based upon
the tangible and intangible benefits which wetlands provide to society. However, no standard
method for estimating the value of wetlands has been established. Also, it is difficult to place a
monetary value on many wetland functions. As a result, available estimates vary greatly.
Several studies have been conducted to quantify the role of wetlands in fisheries production.
Turner (1977) hypothesized that the abundance and type of commercially valuable quantities of
penaeid shrimp are directly related to the area and type of estuarine intertidal vegetation. Numerous
factors influence the distribution and abundance of shrimp, including the nature of the substrate,
area of estuarine lagoons or wetlands, and other physical and biological factors (Kutkuhn, 1966).
Turner demonstrated that there is a direct relationship between the volume of commercial penaeid
shrimp landings and the area of intertidal land over a wide geographical area. He also presented a
discussion of the limitations of such a study, which include the fact that:
1. Fishermen are taxed based on pounds of shrimp landed; therefore, actual landing amounts
may be under reported.
2. Species other than commercial penaeid shrimp may be included.
3. In some instances, shrimp are "de-headed" at sea, which is not always easily determined.
4. Shrimp landed in one area may have been caught in another.
5. Estimates of intertidal area are not uniformly accurate. However, the author believes that
if a statistically, significant relationship between land and yield for a variety of locations
32
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were demonstrated, the relationship probably would be real even with these sampling
inaccuracies.
In addition, poundage landed is based on both effort and the size of the population. In Turner's
study, the data from more than 27 locations, representing a stabilized and developed fishing effort,
were averaged for several years. Several efforts were made to assure the data quality, and data were
normalized when necessary. Intertidal areas were defined as coastal areas vegetated by the salt
marsh macrophytes, Spartina spp., Juncus spp., or mangroves.
The annual shrimp yields per area of intertidal land ranged from 8.9 to 178 lb/ac (10 to 200
kg/ha), and a highly significant (P = 0.02) relationship was found between yield and degree latitude
(Turner, 1977). Also, there was a good relationship (r = 0.69) between the area of intertidal land and
yields of shrimp caught in inshore Louisiana waters. No statistically significant relationship was
found between the average landings (inshore) and estimates of estuarine water surface, average of
estuarine water surface, or average depth or volume. Of the total amount of shrimp caught (inshore),
the percentage of brown shrimp was highly correlated with the percentage of saline marsh vegetation
(r = 0.92).
These analyses lacked data on the amount of submerged macrophytes in the estuarine waters.
Inclusion of such data could improve the regression equation relating the weight of shrimp to
vegetated estuarine habitats. Also, there are insufficient data to determine the impact of mangrove
litter production with changes in latitude. Given these restrictions, a positive relationship was
demonstrated between commercial yields of penaeid shrimp with area, intertidal vegetation, and
latitude for 27 locations. Thus, on a regional basis, the inshore yields of shrimp are directly related
to areas of estuarine vegetation (Turner, 1979).
The association between shrimp life cycles and estuarine and wetland acreage is discussed by
Turner and Boesch (1988). The complex stock-recruitment relationships for penaeid shrimp are
presented. Adult stock is dependent upon juvenile and postlarvae abundance. Causal relationships
exist, given reasonable assumptions, between wetland acreage and juvenile abundances, which affect
subsequent adult densities. Recruitment is dependent upon acceptable climatic factors and habitat
quality; conversely, adverse changes in habitat quality and quantity can be detrimental to shrimp
production.
Long-term yields of shrimp are linearly related to both the quantity and quality of intertidal
habitats. Positive relationships were found between penaeid stock sizes (reflected in annual harvests)
and coastal wetland areas within specific regions around the world and in the Gulf of Mexico
(Turner and Boesch, 1988). Correlation coefficients between amounts of shrimp harvested and
33
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amounts of wetlands (total length of mangrove-lined rivers) were: 0.76 for Australia, 0.74 for
Malaysia, and 0.62 for the Philippines. A correlation of 0.97 was reported between shrimp landing
and intertidal vegetation in the Gulf of Mexico. Turner and Boesch (1988) also documented changes
in penaeid shrimp stock following changes in intertidal wetland habitats. Changes in quantity of
vegetation resulted in changes in quantity of shrimp stock in Louisiana, Kuwait, Saudi Arabia, El
Salvador, and Vietnam. Decline of shrimp yields in Japan were related to the cumulative losses of
intertidal lands (r - 0.85).
Several experimental studies have demonstrated a gain in shrimp stocks following gains in
wetland acreage or quality. A marsh rehabilitated by planting with Spartina alterniflora (smooth
cordgrass) accumulated higher densities of juvenile and postlarvae penaeid shrimp than control sites
which were not planted (Turner and Boesch, 1988). Thus, vegetative structure positively affected
habitat selection. However, the presence of vegetation, in itself, does not define a healthy productive
marsh for fisheries organisms. Evidence suggests that a large amount of edge is beneficial and that
creeks and channels which connect the, interior of the marsh with the open bay provide Hushing
necessary to maintain moderate soil salinities required for plant health and access to more of the
marsh surface (Minello et al. 1986). Edge has also been increased with creation of "brush-parks"-
which are areas of brush strategically placed in estuaries. Brush-parks accumulated higher densities
of fish or stimulated growth/production in West Africa and other countries (Turner and Boesch,
1988).
Data presented by Turner and Boesch (1988) support the hypothesis that habitat quality and
quantity control adult stocks of penaeid shrimp, and they conclude that conservation of habitat
quality is of high significance to success of sustained recruitment. Because other aquatic animals
inhabit these ecosystems and have life histories similar to shrimp, it is probable that the quality of
wetland habitats can directly limit the productivity of other fisheries as well.
Turner (1982) suggests that where there are large areas of wetlands and estuaries, there are
likely to be substantial fishing industries nearby. This relationship has been quantified in Louisiana,
where coastal wetlands area is positively correlated with commercial landings of shrimp caught in
inshore waters (Turner, 1977). The relationship between landings and area of open water is not
statistically significant and appears to be negative. Data also suggest that species of shrimp landed
are directly related to the kind of vegetation present (Zimmerman, Minello, and Zamora, Jr., 1984;
Minello and Zimmerman, 1985).
34
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Total animal production in various ecosystems is ranked in Table 12. In areas where plant
production is high, animal production is high. Animal production in swamps and marshes (9.0
gC/m2/yr) and estuaries (17.8 gC/m2/yr) is higher than production in terrestrial ecosystems (2-3
gC/m2/yr). Total animal production in estuaries is among the highest measured (17.8 gC/m2/yr).
Turner (1982) concludes that although the exact mechanism coupling fisheries productivity and
coastal habitat is not always clear, a strong correlation is clearly indicated. He further states that if
the reported figures of a 1% loss of wetlands per year is equivalent to a 1% decline in the potential
fishing yield, then the impact of wetland loss on cumulative loss in dockside dollar value over a 20-
year period (1982-2002) would be $380 million (1982 dollars). The actual economic value could be
three times higher than the dockside value as a result of value added during processing and delivery
(Jones et al., 1974). Harris (1983) supports that conclusion. Harris compared the landings of spotted
seatrout (Cynoscion regalis) and red drum (Sciaenops ocellatd) from two geographically separate but
similar bays (Tampa Bay and Charlotte Harbor, Florida). Because these two species spend so much
time in estuaries, their catch and landings are an indication of the health of the estuaries in which
they live. Tampa Bay yielded a much lower amount of these species than Charlotte Harbor,
presumably because of greater cumulative habitat losses, changes in circulation, and pollution due
to human sources.
Deegan et al. (1986) evaluated the relationship of physical factors and vegetation to fishery
harvest for 64 estuaries in the Gulf of Mexico. Many estuaries along the coast were formed by
combinations of tectonics, coastal processes, and riverine deposition. These three factors, acting
together but on different time scales, have formed the present intertidal and inshore open water areas
bordering the Gulf of Mexico. A listing of major estuaries in the five U.S. Gulf coastal states is
given in Table 13. Gulf estuaries are generally shallow systems, averaging from 3.9 to 19.3 ft (1.2
to 5.9 m) in depth, and contain relatively large acreages of submerged and emergent vegetation.
Except for estuaries associated with the Mississippi River, most Gulf coast estuaries have small
volumes of riverine discharges compared to estuaries along the Atlantic coast.
The areal development of different vegetation types is related to the water budget of the
estuary. The two principal sources of fresh water to most estuaries are rivers and streams and local
rainfall. The percentage of the total fresh water input into estuaries from rivers and streams averages
42% over the Gulf and ranges from 0 to 99% in different locations. The area of emergent vegetation,
including marsh or mangrove, was directly dependent upon intertidal area and rainfall. The area of
emergent vegetation was not significantly related to river discharge through stepwise linear
regression. However, all areas with high river discharge also have high rainfall amounts, which
complicates the statistical analyses. An analysis of fishery catch statistics in estuaries from three
35
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Table 12. Preliminary Estimates of Animal Secondary Production, Consumption, Standing Stock
and Turnover for Different Ecosystems (Adapted from Whittaker and Likens (1973) and Turner
(1982))
Ecosystem Type
Rock, ice, and sand
Desert scrub
Tundra and alpine
meadow
Cultivated land
Boreal forest
Woodland and shrubland
Temperate evergreen
forest
Temperate deciduous
forest
Temperate grassland
Open ocean
Tropical seasonal
forest
Lake and stream
Tropical rain forest
Savanna
Continental shelf
Swamp and marsh
Upwelling zones
Estuaries
Algal bed and reef
gC/m2
Animal
Biomass
0.01
0.02
0.02
0.02
2.2
2.2
4.5
7
3.1
1.1
5.4
2.2
9.0
6.8
9.0
4.5
4.5
6.8
9.0
% Animal
Consumption
Plant Production
2
3
3
1
4
5
4
5
10
40
6
20
7
15
30
8
35
15
15
gC/m2/yr
Animal
Production
0.0004
0.15
0.2
0.3
1.4
1.4
2.4
2.7
3.3
3.4
4.0
5.5
6.5
7.0
7.3
9.0
12.5
17.8
18.3
Days Turnover
of Animal
Biomass
9,125
486
365
243
573
573
684
946
343
118
493
146
505
354
450
183
131
139
180
TOTAL CONTINENTAL 3.1
2.5
452
36
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Table 13. Characteristics of Some Gulf of Mexico Estuaries (Adapted from Deegan et al.,
1986)1
Estuary
Florida Bay
Ten Thousand Is.
Charlotte Harbor
Sarasota Bay
Tampa Bay
Apalachicola Bay
Pensacola Bay
Perdido Bay
Mobile Bay
Mississippi Sound
Deltaic Plain
Calcasieu Lake
Sabine Lake
Galveston Bay
Corpus Christi Bay
Submerged
Vegetation
Areas (acres)
259,712
4,831
53,270
7,611
29,615
9,380
7,912
0
5,001
29,652
247
0
0
18,105
12,753
Emergent
Vegetation
Areas (acres)
213,675
178,147
64,693
4,070
21,046
21,307
10,418
1,070
21,480
66,932
1,905,618
252,222
42,499
231,493
45,017
Open
Waters
(acres)
606,675
103,782
277,896
34,760
306,046
170,039
151,472
17,270
284,795
434,454
3,720,866
231,817
55,857
353,872
109,839
Mean
Depth
(m)
1.3
1.4
2.3
1.7
3.3
2.9
5.9
2.6
2.5
3.0
2.0
1.5
1.4
2.3
1.2
Mean Annual
River Discharge
(CMS)
283.1
9.5
86.0
2.3
43.8
763.6
268.0
26.5
1,664.0
715.0
22,897.7
157.8
474.0
73.1
24.5
1 Acreage originally reported in hectares
37
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states in Mexico demonstrated that the numbers of fish captured per unit area are positively related
to river discharge. Deegan et al. (1986) state that while the mechanisms remain uncertain, there is
little doubt that both estuarine area and fresh water input are related to fishery harvest.
Other studies have attempted to place a market value on wetland acreage based on the ecological
links between wetlands and fishery landings or value. For example, Batie and Wilson (1978)
attempted to correlate economic values from oyster production with acreage of adjacent wetlands and
developed a bioeconomic model to define the contribution of wetlands to oyster production. Using
this model, they calculated the marginal value products and capitalized values from oyster harvesting
accruing to wetlands in seven Virginia counties. The values reflected in that study do not compare
favorably with development values. For example, the discounted marginal value associated with
residential development of Virginia Beach wetlands is approximately $17,650 per acre (1978 value).
The model suggests a wetlands marginal value product of $47.11 (±$1,402.33) per acre if the wetlands
are preserved for oyster production. When other possible values of the wetlands such as erosion
control, wildfowl habitat, or fishery nursery are added, the amount may or may not exceed the
average $17,650 per acre estimated marginal value of development. The important conclusions to
be reached from this study are not the estimated values per se, but rather that refined estimates of
value are possible if appropriate data are collected over a period of time on all parameters including
wetlands acreage, property rights, fishing effort variables, biological variables, and prices.
Bell (1989) recently studied the importance of estuarine wetlands to commercial and recreational
marine fisheries in Florida. Wetlands were found to be linked to approximately 80% of the total
weight of fish landed by recreational fishermen, and nearly 92% of Florida's commercial landings
(Bell, 1984). These data are probably applicable to the Gulf coast in general. According to Bell
(1989), one approach to determining the tangible value of wetlands is to assign a monetary value to
harvestable products and divide the market value of products by total wetland acreage to establish
a dollar value per acre. Some disagree with dollar per acre values when used as the only evaluation,
because this approach does not include true values of ecological and intangible products (e.g.,
aesthetics). The method also assumes that reduction in wetlands acreage directly affects the amount
of a product that is harvested; however, harvest can be affected by other factors. The cost of
harvesting the product is added to the value assigned when the total monetary value of the product
is allocated to wetland value. Other methods assume that the actual dollar value of harvestable
products includes the increasing dollar value generated as the product is processed, wholesaled, and
retailed (Gosselink et al., 1974).
Bell (1989) employed marginal productivity theory in estimating the value of estuarine wetlands.
This approach utilizes population dynamics, as employed by ecologists and fishery biologists, and
38
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marginal analysis, as used by economists. The theory is based upon a direct linkage between
wetlands and marine fishery catch. The marginal product of an acre of estuarine wetland, holding
all other factors constant, is valued at how much the public is willing to pay for the fishery product.
Bell estimates 84% of the value of commercial fishery landings (by weight) on Florida's east coast
and 95% of the value on Florida's Gulf coast are estuarine dependent. The degree to which they are
dependent is established by estimation of a marine fisheries product function that includes fishing
effort and salt marsh or estuarine acreage. A production function was estimated for eight estuarine-
dependent species: blue crab, stone crab, grouper, red drum, oyster, spiny lobster, shrimp, and black
mullet. The results indicated a strong statistical correlation between catch, fishing effort, and salt
marsh acreage. The marginal product model calculates the retail value of an acre of salt marsh to
the commercial fisheries of Florida at $1,355 on the west coast and $8,811 on the east coast. The
recreational estuarine-dependent species generated a value of $1,222 on the west coast and $8,073
on the east coast. Bell believes that the marginal productivity approach is a possible method to
integrate and summarize economic and biologic principles toward a common goal of wetland
valuation. Nontangible wetland products were not included in this analysis.
Gosselink et al. (1974) estimated the value of unaltered wetlands to be as high as $82,000 per
acre. (1974 dollars) using a "life-support" valuation. These scientists calculated the economic value
of the products of wetlands including the market value of estuarine-dependent species as well as sales
of fur-bearing animals. Criticisms of this technique include: 1) the methodology assumes that
marketable fish harvest is directly linked to wetland acreage, whereas fish catch also depends on
biomass and fishing effort; 2) the methodology implies that all wetland acreage is equally productive;
3) value gained or lost cannot be approximately measured by comparison to total market; and 4) the
whole market value of the fisheries is attributed to the wetlands. This method also assumed that
value of capital and effort of the fishing industry was zero.
Odum (1977) proposed that the value of wetlands can be determined by establishing energy
units as the common denominators of economic and environmental exchanges. The general formula
is as follows:
$/acre/year = kcal/acre/year x
Gross National Product
Consumption
Critics maintain that this method assumes that all goods and services, as well as inputs such as labor,
machinery, and raw materials, are transformed energy. In addition, this method does not consider
consumer demand and energy use.
39
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Foster (1978) observed that the environmental benefits of wetland areas are largely in the public
domain while alternative uses for wetlands are primarily for private benefit only. This fact has led
to widespread destruction of wetlands. While society has exerted some governmental control to
maintain the public benefits of wetland resources, many difficulties are encountered in calculating
the social value of wetland benefits due to the nonmarket, intangible nature of many benefits. All
benefits derived from wetlands cannot be measured in the same way. Decisions affecting public
benefit are made daily by private and governmental bodies. These decisions result in giving up some
benefits to secure others. The private decision-maker, in general, has little difficulty making the
decisions, as intangible wetland benefits are perceived to have little value, while development may
be of considerable value. On the other hand, the public decision-maker must weigh the social values
of wetland benefits against their loss (Foster, 1978).
If more information were available, it would be easier to make these decisions. However, in
most circumstances regulatory decisions must be made in a timely manner regardless of information
gaps; decisions of this nature are made daily. In measuring the social value of wetlands, several of
their characteristics must be considered (Foster, 1978):
1. The benefits of wetlands vary from place to place.
2. The level of benefits also vary.
3. The intangibility of some wetland benefits cannot be measured by market demand.
4. The value of wetlands vary from place to place and time to time.
Given these assumptions, Foster suggests that it is possible for the loss of wetlands to be more
beneficial than their preservation. If the policy is to preserve all wetlands, valuations of productivity
become unnecessary. Foster (1978) concluded that the public condones the draining and filling of
wetlands for real estate and agricultural uses and construction of canals for navigation purposes
because the value of wetlands to commercial and recreational fisheries has not been fully appreciated.
Not all of the proposed evaluations of wetlands are based on their value to commercial and
recreational fisheries. Farber (1987) estimated the value of coastal wetlands for protection of coastal
communities from hurricane winds. The basis for this protection is that wetlands help to weaken
storms and provide a vegetated buffer between the storm and populated areas. As a hurricane makes
landfall, the central core weakens as it passes over flat coastal terrain because the core no longer is
fueled by the ocean heat source. Also, it is possible for wetlands to diminish the inland tidal surge
that results from a hurricane impacting the coastline because of the effects of marshlands on wave
energy and the reservoir capacity of the intervening area. A simple model of damages suggests a
40
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structural equation in which wind velocity is a function of the distance of location inland, the
distance from the path of the storm, the intensity of the storm at landfall, and the nature of the
intervening terrain. The terrain variable would reflect topographical features such as wetland areas.
Farber used this model to estimate effects of wind damage of coastal Louisiana. The value of
the loss of a one mile (1.6 km) depth of coastal wetlands along the Louisiana Gulf coast was
estimated for each Louisiana parish. The total incremental annual damages from the loss of one mile
(1.6 km) of wetlands along the 250 mi (403 km) coast was $63,676 per year based on 1988 costs.
When the annual incremental damage is capitalized, the present value (in 1980 dollars) of increased
wind damage is between $1.1 and $3.7 million. On a per-acre basis, this amounts to between $7 and
$23 per acre. The current market value (1987) of Louisiana wetlands is approximately $200 per acre;
this value is derived primarily from mineral and hunting rights.
Farber suggests that hurricane protection is only one of several functions that wetlands produce
as "public goods." To achieve an estimate of the full value of wetlands, their value for wind
protection must be added to other values such as flood protection, recreation, and fishery values.
All these goods and services provided by wetlands must be examined and considered when decisions
are made on costly projects to revegetate or otherwise protect wetlands. Also, the same concept
applies when decisions are made to destroy wetlands through canal construction and other
developments. Flood damage is probably more damaging to low-lying coastal areas than wind, and
wetland areas may be more useful for flood protection than wind protection. That relationship
remains to be quantified.
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Quality of Coastal Habitats
By virtue of their location in the coastal zone, coastal habitats are extremely vulnerable to
natural and man-induced destructive forces. The effects of the destructive force can be categorized
into reversible and irreversible impacts. Obviously, impacts which irreversibly alter the character
or quality of a habitat are most destructive. The severity of an adverse impact is directly
proportional to the length of time that it takes for the system to recover from the impact.
It is important to understand that ecosystems change in time, and attempts by man to stabilize
inherently unstable systems are very expensive and ultimately may be doomed to failure. For
example, the westward drift of barrier islands along the central portion of the Gulf Coast is
inevitable, given prevailing currents and sediment transport systems. Man's activities can hasten or
exacerbate loss of barrier island habitat by upsetting the equilibria which maintain those systems or
control their patterned development. Thus, dredging a channel on the western margin of a barrier
island may result in loss of island habitat by precluding island accretion. Likewise, dredging of
channels through seagrass meadows or creating channels by propeller scouring can result in increased
seagrass losses due to changes in hydrological patterns and increased erosion.
Naturally occurring physical and biological processes can adversely affect the quality of coastal
wetland habitats, including subsidence, erosion, and rising sea level, phytoplankton blooms, and plant
diseases. Common human activities which adversely impact wetlands, include construction of canals
and channels, dredging, spoil disposal, impounding, draining, and filling.
The impacts of natural and man-induced activities on habitats of Mobile Bay, Alabama, were
summarized in conceptual models by Watzin et al. (in preparation). Those models consist of a
problem statement, a list of causes, and an evaluation of effects. This approach is useful since it
produces a summary and evaluation of habitat issues. Sources of habitat degradation and effects for
Gulf of Mexico habitats, including vegetated habitats, are summarized in this manner in Figures 3,
4, and 5. Although there are not enough quantitative data to rank the causes of habitat loss, changes
in sedimentation patterns, water movement, subsidence, and dredging and filling activities are the
causes of the majority of losses of all Gulf habitats. Structure and function of habitats are
inextricably related. Forces which impact structure always detrimentally impact the ecological
functions provided by that habitat (e.g., filling of wetlands eliminates fish foraging sites).
Subsidence or "sinking" is the natural fate of delta marshes which undergo cyclic periods of
construction and deterioration. The construction period is initiated when a river changes course and
sediment deposition begins. Natural subsidence occurs as a result of dewatering, compaction of
42
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sediments, and sinking due to weight of sedimentary deposits. During the construction period,
deposition exceeds subsidence and the delta enlarges. As delta construction continues, the river
begins to favor a shorter pathway and deposition is reduced while subsidence continues. Land levels
may be maintained by an accumulation of organic materials and remobilization of mineral sediments.
However, subsidence rates eventually exceed organic accumulation, which initiates the destruction
phase which is characterized by the losses of large areas of wetlands (Leibowitz and Hill, in
preparation).
Disruption of hydrologic and sediment patterns by man's activities or natural processes can
accelerate this cycle. Swift currents and surges from hurricanes and storms can enhance the erosion
of sediment and other substrate and result in deterioration of wetland habitats. Sea level rise can
hasten the flooding of wetlands and result in more open water acreage.
River deltas along the Louisiana coast evolve through alternating periods of land building and
land loss. The frequency and duration of these, periods are determined by the balance between
sediment supply and variations in relative sea level. Ongoing subsidence resulting from compaction
and the sinking of Mississippi delta sediments is the major symptom of the relative sea-level rise.
The construction and maintenance of dams and canals, especially navigation canals, is a major cause
of changes in sedimentation patterns and wetland loss, especially in Louisiana (Johnson and
Gosselink, 1982; Turner, 1987; Turner et al., 1982; Chabreck, 1982; Lindall et al., 1979; Baumann
and Turner, 1990). Construction of canals contributes directly and indirectly to the disappearance
of Louisiana's coastal wetlands (Johnson and Gosselink, 1982). Dredging results in the conversion
of wetlands into open water. Also, as canals become older and are used by boats, the banks erode
and the canals becomes wider, resulting in additional wetland loss, increased open water from canal
construction can result in changes of water flow patterns and subsequent saltwater intrusion.
Saltwater intrusion related to canal construction is responsible for the loss of many acres of Louisiana
coastal marshes.
Oil and gas extraction activities can result in detrimental impacts to onshore, nearshore, and
offshore wetlands and other aquatic habitats. Onshore oil and gas activities which can affect habitats
include construction of pipelines and support facilities; nearshore activities include construction and
use of navigation channels. The detrimental effects of Outer Continental Shelf (OCS) activities on
Louisiana coastal habitats are discussed by Turner and Cahoon (1987). While it is difficult to
quantify a direct cause and effect relationship between OCS activities and habitat loss, it is
noteworthy that the rapid wetlands loss in the central area of the Gulf coast is confined to the most
concentrated development of onshore and offshore oil and gas recovery efforts. Over 40% of the
total OCS lease blocks sold in the United States are in the central Gulf region. Dredge and fill
activities have been responsible for the majority of conversions of wetland habitats to open water
46
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activities have been responsible for the majority of conversions of wetland habitats to open water
habitats in this region (Turner and Cahoon, 1987). Turner and Cahoon discuss the importance of
direct impact on wetland loss (habitat change), the significance of direct conversion of wetland
habitats to open water and spoil sites by oil and gas activities, and the relevance of construction of
navigation channels to continuing wetland losses. The extraction of oil and gas on the OCS has
contributed approximately 4-5 percent of wetlands losses from pipeline canals and navigation
channels crossing wetlands. Another 4-13 percent of wetlands loss was estimated to be due to
indirect impacts from these activities.
Johnson and Gosselink (1982) quantified the effects of canal construction on wetland habitats.
Their study areas included: oil field navigation channels on the Rockefeller Wildlife Refuge at
Grand Chenier, Louisiana; the Southwestern Louisiana Canal in southern Lafourche Parish; and the
Leeville oil fields near Leeville, Louisiana. Johnson and Gosselink (1982) observed that newly
dredged canals were constructed wider than the widths specified on permit applications and
concluded that few, if any, regulatory observations were made during canal construction. Also, boat
traffic greatly increased the permitted canal widths. Canals near navigation routes with increased
traffic widened from 4.8 to 5.3 ft (1.46 to 1.63 m) per year faster than those located some distance
from boat traffic. They demonstrated that once spoil banks eroded away, a dramatic increase in
canal widening occurred. •
Turner et al. (1982) also studied the effects of canals on south Louisiana wetlands. Historically,
some canals which were constructed for oil and gas exploration have been filled; but many more have
been abandoned after commercial use and are utilized recreationally. Canals are constructed in
straight lines, whereas natural creeks in the delta are serpentine. The linear structure of canals
results in major differences in water and sediment movement between canals and natural drainage
systems. The direct and indirect effects of canal development have greatly accelerated the rate and
geographic extent of wetland loss in Louisiana; wave attack and the deficit of sediment accretion
compared to subsidence and sea level rise result in localized land loss. Some have postulated that
canals probably caused at least a majority and perhaps as much as 90% of the present land loss in
coastal Louisiana (Penland and Boyd, 1982).
Hopkinson and Day (1979) also found that two canals, Bayou Segnette and Barataria Waterway,
have drastically modified the hydrology of the area. In the past, all water from the upper portion
of. Barataria Bay (mainly a fresh water area) passed through Lake Salvador. Now, only that portion
originating from the Des Allemands area passes through. Thus, the canals are causing saltwater
intrusion to occur farther north and stormwater runoff from the West Bank is flowing directly into
Barataria Bay.
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Lindall et al. (1979) concluded that construction and maintenance of navigation channels was
probably the largest form of estuarine alteration in the southeast. Increased rates of canal
construction are directly related to increases in human population. More than 4,400 mi (7,097 km)
of navigation channels existed, were under construction, or were planned at the time of the Lindall
study. Two years earlier (1977), Lindall and Solomon reported that an average of 151.5 million cubic
yards of sediment were removed each year from existing channels and the total yearly disposal from
Federal maintenance dredging was 200 million cubic yards. More recently, Mager (1990)
documented that marsh management projects are a major cause of habitat alteration in the southeast.
Typically, diked and managed marshes convert to open water.
Changes in habitat area in coastal Louisiana which occurred between 1955-1956 and 1978 are
summarized in Table 14. There has been a dramatic decrease in the area of marsh and swamp and
a concurrent increase in areas of open water, mudflats, canals, and spoil disposal sites.
Table 14. Changes in Area by Habitat in Louisiana's Coastal Zone from 1955/56-1978 (from
Bauman and Turner, 1990)1
Habitat Description
Marsh
Swamp
Forest/Upland
Aquatic Grass Bed/Mud Flat
Canal and Spoil
Open Water
Urban/Agriculture
Beaches and Dunes
Area (acres)
1955/56
3,125,825
518,436
119,890
16,173
84,189
4,881,211
455,400
11,757
Area (acres)
1978
2,494,030
437,560
142,206
66,193
198,733
5,344,219
523,476
7,613
Changes from
1955/56-78
-631,795
-80,876
+22,318
+50,020
+114,543
+462,910
+68,076
-4,144
1 Acreage originally reported in hectares
Although acreage of habitat loss caused by oil and gas activities is significant, these losses only
represent a small portion of total wetland losses experienced between 1955 and 1978 (Table 14). All
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sources of direct detrimental impacts to coastal wetlands accounted for an estimated 25.6% of the
total net wetland loss within the Louisiana portion of the study area from 1955/56 to 1978. Of the
total direct impacts of 182,619 ac (73,935 ha), OCS-related activities accounted for 28,636 to 33,682
ac (11,593 to 13,636 ha) of the wetland loss. Although this is a substantial areal loss, it represents
only 4.0 to 4.7% of the total Louisiana wetland loss from 1955/56 to 1978, and 15.7 to 18.4% of direct
impacts. " '
Direct impacts from OCS pipelines averaged 1.6 ac/mi (0.4 ha/km) and totalled 29,682 ac
(12,017 ha). Direct impacts are variable and are related to construction technique, geologic region,
habitat type, age and diameter of pipeline, and other factors that were not examined (Bauman and
Turner, 1990).. The current guidelines published by Minerals Management Service on the impacts
of pipelines on Gulf of Mexico coastal marshes estimate that construction of a single oil and gas
pipeline destroys approximately 25 ac of wetlands per mile of pipeline (6.28 ha/km).
The direct impacts per unit length of navigation channels were found on the average to be
approximately twenty times greater than pipelines. Navigation channels accounted for a minimum
of 41,765 ac (16,909 ha) of habitat change. Of the total change, 33,643 ac (13,620 ha) represented
the losses of wetland and beach habitats. The maximum amount of habitat change attributable to
OCS activities was 7,126 ac (2,885 ha; 17%) of which 5,666 ac (2,293 ha; 16.8%) was from the loss
of wetland and beach habitats. The impact of commercial traffic using navigational channels is due
mostly to activities other than those associated with OCS activities. Of the total direct wetland loss
resulting from navigation channels, 33,729 ac (13,655 ha; 81%) occurred in the Mississippi River
Gulf Outlet, Calcasieu Ship Channel, and Beaumont Channel/Sabine Pass. All of these areas have
very low OCS destination usage.
An example of the manner in which nature and human activities can adversely impact wetland
habitats is presented by Chabreck.(1982). He reported that there are four vegetative types that
typically occur in bands generally paralleling the coastline: saline, brackish, intermediate, and fresh.
Each band contains characteristic water salinity levels and plant communities. Human activities such
as construction of levees, canal dredging, and stream channelization along with natural processes
including subsidence and erosion have removed many natural tidewater barriers and reduced fresh
water flow through the marshes. As a result, saltwater intrusion from the Gulf of Mexico has greatly
increased and has resulted in alteration of vegetation types. Saline vegetation has increased while
brackish and intermediate types have retreated inland. This has caused a drastic reduction in the
acreage and diversity of freshwater vegetated communities.
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The definitions and acreages of plant communities which are discussed in Chabreck's Louisiana
study are:
Saline Vegetative Type. This type of vegetation borders the shoreline of the Gulf of Mexico
and is subjected to tidal fluctuations. It forms a narrow band in the Chenier Plain but is quite
extensive in the deltaic plain and occupies about 667,170 ac (270,000 ha). Water salinities average
18.0 ppt and soils have less organic content than those further inland. Species are salt-tolerant and
dominated by 5". alterniflora (cordgrass), Distichlis spicata (saltgrass), and Juncus roemerianus (black
needlerush).
Brackish Vegetative Type. Although this type is further removed from the shoreline, it is still
subject to tidal fluctuations. This is a major vegetative type and occupies about 1,284,400 ac
(520,000 ha) in coastal Louisiana. Water salinities average 8.2 ppt and the soils contain more organics
than more saline soils. The brackish vegetative type is dominated by S. patens (salt hay grass) and
D. spicata.
Intermediate Vegetative Type. This vegetative type is found inland of the brackish vegetation
and occupies an area of about 691,600 ac (280,000 ha). Some tidal influence is present and salinities
average 3.3 ppt. Plant diversity in this zone is high. S. patens dominates this zone; other common
plants include Phragmites communis (phragmites) and Sagittaria falcata (duck potato).
Fresh Vegetative Type. The fresh vegetative type occupies the zone inland from the
intermediate type and south of the Prairie formation and Mississippi River alluvial plain. It
encompasses an area of 1,309,100 ac (530,000 ha) and is normally free of tidal influence. This
community supports the greatest diversity of plants, and organic matter in the soil can exceed
Dominant plants include Panicurh hemitomon (maidencane) and Eleocharis spp.
Changes in the location of saline and brackish vegetative types over a period of approximately
25 years were determined by comparing maps of 1949 with those in 1968. Saline types in the deltaic
plain on the earlier map extended inland for an average of 5.8 mi (9.3 km) from the Gulf shoreline,
while the 1968 map shows an intrusion of 7.9 mi (12.7 km) inland (an encroachment averaging 2.1
mi (3.4 km) over the 25-year period). In the period from 1968 to 1978, the fresh vegetation type
was reduced by 6.8% while the saline type increased 8.9% (Chabreck, 1970).
Dredging and filling of wetland habitats has significantly altered the ecological balance of
coastal ecosystems throughout the Gulf Coast. For example, one study demonstrated that dredging
and filling for development in Florida resulted in the loss of an estimated 1,100 t (1,000 mt) of
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seagrass, 1,800 t (1,636 mt) of invertebrates, and 73 t (66 mt) of fishery products (Taylor and
Solomon, 1968). Even though our knowledge and appreciation of coastal wetlands has increased
substantially since the time of that study, the pressure to develop coastal habitats has not abated.
Indeed, the numbers of people moving to the Sun Belt to live on or near the water has continued to
increase (U.S. EPA, 1988c; Culliton et al., 1990). This has resulted in increased pressure to convert
natural coastal habitats into residential areas, marines, and other facilities. Creation of waterfront
development can adversely affect coastal habitats by directly obliterating (filling) coastal vegetated
communities, redistributing sediments, interrupting the normal access of tides and currents, and
replacing numerous natural zones of gradation (ecotones) with open water or developed upland
habitats.
Quantification of current losses through dredge and fill activities along the Gulf Coast are
summarized in a data base collected by the National Marine Fisheries Service's (NMFS) Habitat
Conservation Program (Mager and Thayer, 1986; Mager and Keppner, 1987; and Mager and
Ruebsamen, 1988, Mager, 1990). This data base summarizes the effectiveness of the U.S. Army COE
regulation program in controlling coastal wetland habitat loss. The COE has the responsibility and
authority to issue federal permits for dredging and filling activities in waters of the United States
including wetlands. Other federal and state resource agencies, such as the U.S. Fish and Wildlife
Service and U.S. Environmental Protection Agency, advise the COE on the potential environmental
impacts of proposed projects. The NMFS provides comments and recommendations to the COE
concerning the environmental impacts which could result with completion of a proposed action on
the management and development of marine fisheries resources. In the NMFS Southeast Region
(North Carolina to Texas including the Virgin Islands and Puerto Rico), most of commercial fishery
landings and most of the recreational fish caught consist of species that inhabit estuaries at some part
of their life cycle (Thayer and Astach, 1981; Lindall and Thayer, 1982; Mager and Thayer, 1986).
Yet, there is continuing competition for multiple use of estuaries and marshes that result in the loss
of the valuable habitat. Some modifications resulting in adverse effects on the habitat include
physical modification, addition of biological and chemical pollutants, and alteration of fresh water
inflow patterns (Lindall et al., 1979; Tiner, 1984).
A cooperative agreement between the NOAA and the U.S. Department of Army Corps of
• Engineers established pilot studies from 1985 to 1988 in the Southeast to evaluate the feasibility of
establishing a national program for creating and restoring fishery habitat. The results of the pilot
studies are summarized in Thayer et al. (1989) and Pullen and Thayer (1989) and a national
restoration program was established in 1991. As part of the pilot study, NOAA (NMFS) designed
and implemented a computerized system to track agency recommendations concerning permit
requests for proposed habitat alteration (dredging and filling) in the Southeast. Data from 1981-
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1987 were analyzed by Mager and Thayer (1986), Mager and Keppner (1987), and Mager and
Ruebasem (1988) and are summarized in Table 15.
The average values associated with permit actions reflect projected losses due to direct removal,
burial, impounding, and draining. However, the impact on habitats of point and non-point sources
of pollutants associated with development are not addressed by this program; thus, losses of certain
habitats, particularly submerged aquatic vegetation reported through the permit process, are
conservative. Of the sample of 5,122 permit applications evaluated, approximately 40% of the acres
proposed for dredging by applicants, 46% of the fill applications, and 2% of the drain applications
were "not objected to" by NMFS. During this time period, NMFS recommended against issuance of
Corps permits which would have resulted in the loss of 158,603 ac (64,212 ha) of coastal wetlands.
Dredging and filling activities not only result in creation of dry land from wetlands (U.S.
Department of the Interior, 1974), they can result in creation of canals which pose other
environmental threats to coastal ecosystems. Canal developments have been constructed throughout
the Gulf coast by excavating sediments from shallow estuarine bottoms adjacent to emergent
wetlands and pumping or placing this excavated material on marshlands or mangroves. Often,
bulkheads are built to contain the excavated materials. Canals which exist between filled fingers of
wetlands generally exhibit poor water quality due to poor circulation and nutrient loading from
adjacent development (U.S. EPA, 1973). As homesites on canals are developed, the sandy soil is
usually covered with grass that may be fertilized, watered, and treated with .pesticides and herbicides.
Runoff from lawns transports the nutrients and pesticides, as well as particulate material, to the
poorly flushed canals (U.S. EPA, 1973). Oil, gasoline, polychlorinated biphenyls from tire wear,
detergents, and other pollutants may reach the water in the canals. Water quality in canals and
adjacent waters can be further reduced due to failed septic tank systems located along canal
developments (U.S. EPA, 1982). .
Creation of finger-filled canal projects not only can destroy wetlands through filling and
creation of waters which may not conform to water quality standards, but it can also destroy
estuarine benthic organisms and vegetation. Suspended material from dredging activities can reduce
light penetration and retard the growth of submerged vegetation. Also, changes in the texture and
particle size of excavated materials may inhibit recolonization by invertebrates (Johnson, 1971).
Thus, this form of development can be disruptive to submerged and emergent habitats.
The indirect effects of urban development on habitats in Barataria Basin, Louisiana are
discussed by Hopkinson and Day (1979), who evaluated changes that occurred at the upper estuary
interface as a result of urban development. Their work suggests that processes occurring at the
52
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53
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uplands-estuary interface can have direct ecological effects, such as nutrient runoff and
eutrophication. In addition, these processes can cause indirect effects from a distance, such as
changes in hydrology. As previously discussed, hydrology changes may alter salinity distribution in
an estuary and in coastal waters.
Nutrient addition to coastal waters can severely disrupt ecological equilibria. Hopkinson and
Day (1979) studied three fresh to brackish water coastal lakes (Cataouatche, Salvador, and Little) for
one year. Measurements of community production and metabolism, chlorophyll, and water column
nitrogen and phosphorus were used to evaluate functional relationships between the uplands and the
estuary. Community heterotrophy decreased from upland to the lower estuary and chlorophyll,
nitrogen, and phosphorus concentrations were highest in the streams and lakes adjacent to upland
areas. This study concluded that Lake Cataouatche and Lake Salvador serve as efficient nutrient
processing traps. Lake Cataouatche is highly eutrophic and has experienced fish kills following storm
runoff from the West Bank area of New Orleans. These fish kills indicate that the lake is losing its
value as a prime nursery area for recreationally and commercially important fish species. Thus,
excess nutrients have reduced the quality of this lake and presumably the surrounding wetlands.
One critical indicator of the quality of estuarine habitats is the quality of indigenous shellfish
and the water in which they grow (Broutman and Leonard, 1988). Shellfish waters are classified for
the commercial harvest of oysters, clams, and mussels in relation to public health concerns. Shellfish
obtain nourishment by filtering large volumes of water and can accumulate (bioconcentrate)
pollutants contained in the water. Humans can acquire these pollutants, which include bacteria and
other pathogens, by eating poorly cooked or raw shellfish meats. Therefore, the harvest of shellfish
is strictly regulated and is not permitted in waters containing high levels of fecal coliform bacteria.
In 1985, Gulf of Mexico estuaries produced 60% of the weight (25,509,000 Ib; 11,571,000 kg) valued
at over 40% of the total U.S. shellfish catch. According to the NMFS (NOAA, 1987), over 30 million
Ib (13,600,000 kg) of oyster meats were landed in the Gulf of Mexico in 1986. The American oyster
(Crassostrea virginica) is the major species harvested, with some commercial clam harvest occurring
in south Florida.
Shellfish waters are classified by states and by the National Shellfish Sanitation Program (NSSP)
guidelines. These classifications reflect levels of pollutants, pollution sources, and fecal colif orm
bacteria levels in surface waters (Broutman and Leonard, 1988). Waters are classified by states into
four categories:
Approved Waters: Shellfish may be harvested for the direct marketing of shellfish at all times;
Conditionally Approved Waters: Waters do not meet the criteria for approved waters at all
times, but may be harvested when criteria are met;
54
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Restricted Waters: Shellfish may be harvested from restricted waters if subjected to a suitable
purification process; or,
Prohibited Water: Harvest cannot occur at any time.
The NSSP standard for approved waters is a total coliform bacteria concentration of less than
. 70 Most Probable Number (MPN) per 100 ml, with no more than 10% of the samples exceeding 230
MPN, per 100 ml. As the basis for closing waters to shellfish harvesting, most states, including all
the Gulf of Mexico states, use a fecal coliform standard of 14 MPN per 100 ml, with no more than
10% of the samples exceeding 43 MPN per 100 ml.
Most of the oyster reefs which are harvested in the Gulf of Mexico are classified as "approved",
"conditionally approved", or "conditional." The conditionally approved and conditional classification
is most used in waters that are affected by nonpoint sources. The classification requires the
development of a management plan that is explicit about the conditions for opening the waters for
harvest. Approximately 30% of coastal Gulf waters which are suitable for raising shellfish are closed
for harvest, and 58% are conditionally approved or prohibited (Table 16). A more recent analysis
of shellfish harvest classification in Alabama (Perkins, 1991) demonstrates a similar trend:
Approved- 73,919 ac (29,900 ha); Conditional- 193,774 ac (78,450 ha); Restricted- 84,313 ac (34,134
ha); Prohibited- 1,179 ac (477 ha); Unclassified- 17,452 ac (7,000 ha). An indication of the
occurrence of temporary closures of approved waters in the Gulf of Mexico is given in Table 17.
Table 16. Shellfish Harvest Classification by States in 1985 (Adapted from Broutman and Leonard,
1988)
State
Approved
Area (Acres)
Approved
Conditional Conditional
Prohibited Closures1
Florida
Alabama
Mississippi
Louisiana
Texas
Totals
Percentage of Total
95,092
0
76,888
1,620,458
727,941
2,520,379
42
153,595
0
120,083
0
570,045
843,723
14
138,622
175,487
189,958
283,242
0
787,309
13
199,212
84,860
96,749
1,042,157
328,500
1,751,478
29
17,452
0
0
0
0
17,452
1
1 For reasons other than a sanitary survey
55
-------
Table 17. Examples of Periods of Temporary Closures of Approved Waters in the Gulf of Mexico
(from NOAA, 1988c.)
State and Estuary
Area
Dates of Closure
Florida
Tampa Bay
Apalachee Bay
St. Andrew Bay
Choctawhatchee
Pensacola Bay
Mississippi
Mississippi Sound
Galveston Bay
Cockroach Bay
Lower Tampa Bay
Wakulla Cty Waters
East Bay
West Bay
All
All
All
Escambia & East Bay
All Mississippi
Waters
W. Mississippi Snd.
All
Galveston and Trinity
Bays
East Bay
West Bay
Aug-84, Feb-83, Feb-80
Nov-83, Aug-83
Dec-85, Nov-85, Apr-84, Mar-83, Feb-
82, Jan-82, Feb-81, Nov-80, May-80,
Mar-80, Feb-80, Nov-79
Dec-85, Apr-84, Mar-84
Dec-85, Mar-84, Apr-83
Oct-85
Dec-85, Mar-84
Dec-85
Apr-84, Mar-84
Dec-87, Feb-83
Dec-82
Nov-86, Mar-85, Nov-84, Oct-84,
Jul-79, Apr-73, Mar-73
Feb-87, Nov-86, Jul-81, Jun-81,
Jun-76, Jan-74
Jan-87, Nov-86, Jul-81, Jun-76,
Jan-74
Jan-83, Jun-81
(Continued)
56
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Table 17. (Continued)
State and Estuary
Area
Dates of Closure
Matagorda Bay
San Antonio Bay
Aransas Bay
All
Lavaca, Cox, Keller
Bays
Lavaca Bay
East Matagorda Bay
Tres Palacios,
Carancahua Bay
Oyster and Powder-
horn Lakes
All
Portion
Copano Bay
Mission, Copano,
Port Bays
Mar-85, Nov-84
Dec-85, Nov-85, Nov-84, Mar-84,
Nov-83, Feb-83, Nov-82, Mar-82,
Nov-81
Feb-87, Jan-85
Feb-87, Jan-87, Nov-84
Feb-87, Apr-85, Nov-84, Feb-83
Mar-85, Mar-82
Dec-86, Dec-85, Apr-85,
Mar-85, Nov-81
Apr-85, Jan-79
Feb-87
Apr-85, Mar-85
57
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The NSSP standards are based upon concentration of pathogens in sewage; however, these
standards do not include biotoxins, Vibrio bacteria, or diseases that are not necessarily associated with
contaminated waters. Therefore, waters closed to shellfish harvest based on fecal coliform count do
not include waters closed to harvest due to biotoxins and Vibrio. In the Gulf of Mexico, the
dinoflagellate Ptychodiscus brevis produces toxins that cause fish kills and neurotoxic shellfish
poisoning from consumption of contaminated shellfish. Consumption of shellfish contaminated with
Vibrio causes gastroenteritis; this malady resulted in seven deaths in 1987 (Broutman and
Leonard, 1988). Studies indicate no apparent correlation between coliform-bacteria levels and Vibrio.
One function of wetlands is to filter pollutants and nutrients from flood or tidal waters. Thus,
the cumulative loss of wetlands may significantly impact the availability of approved shellfish waters.
Sources of water quality impacts in coastal waters have been summarized by Broutman and Leonard
(1988). They found that sources of fecal coliform pollution .that contribute to the permanent qr
temporary closure of shellfish areas include: sewage treatment plants (STP) that discharge
inadequately treated effluent or bypass raw sewage through an outfall pipe during overload periods;
straight pipes where sewage is discharged directly from units not connected to collection systems;
industrial discharges containing fecal coliform from seafood-processing plants, pulp and paper mills,
or human sewage; septic systems that leach improperly treated materials to surface waters; raw
sewage from boats; urban runoff from storm sewers, drainage ditches, or overland runoff from urban
areas containing fecal materials; agricultural and feedlot runoffs carrying fecal coliform; and wildlife
areas where runoff contains fecal coliform from waterfowl, rodents, rabbits, deer, etc.
The main sources of coliform contamination and pollution of Gulf estuarine waters were
summarized by Broutman and Leonard (1988). Gulf coast estuaries predominantly affected by STP's
and urban runoff include Caloosahatchee River, Tampa Bay, Pensacola Bay, Lakes Pontchartrain and
Borgne, Brazos River, and Corpus Christi Bay. Estuaries impacted by combined urban and nonurban
sources are St. Andrew Bay, Mississippi Sound, Galveston Bay, and Laguna Madre. Estuaries
impacted by upstream sources are Apalachicola Bay, Mobile Bay, Mississippi Sound, Mississippi
Delta, Atchafalaya and Vermilion Bays, and San Antonio Bay. Septic tank failure is the main source
of pollution in Aransas Bay; septic and straight pipes in Chandeleur/Breton Sounds, Terrebonne/
Timbalier Bays, and Caillou Lake; septics and boating activities in Ten Thousand Islands and
Charlotte Harbor; septics and wildlife in Apalachee and Choctawhatchee Bays; septics and
agricultural runoff in Matagorda Bay. Wildlife sources were listed as the main source of
contamination of the Suwannee River and agricultural runoff in Barataria Bay.
Coastal barrier islands and other natural structures are dynamic systems that provide a plethora
of ecological habitats. Shoreline changes and wetland losses of the Coastal Barrier Resource System
58
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were studied by Watzin and Baumann (1988). Data from selected barrier islands presented in that
study are summarized in Table 18. Under natural conditions, erosion along one shoreline of a barrier
structure is usually compensated by gains in habitat along the opposite shoreline. This process results
in a east to west drift of barrier islands along the northern Gulf coastline. However, the activities
of man have disrupted this delicate balance in many areas. Catastrophic natural forces can also
disrupt the balance that maintains barrier resources.
The general trend is recession of shoreline of all coastal barrier islands along the Gulf coast.
Many of the observed changes that have taken place are due to erosion of the shoreline. There are
many causes of increased rates of erosion and it is difficult to separate and quantify impacts from
the various sources. Erosion is generally accelerated through human activities such as construction
of coastal stabilization features, including jetties and groins, and results in an alteration of the
dynamic equilibrium of coastal processes. Dredging interrupts the littoral drift system and traps
sediment in areas where it is no longer available for beach nourishment. Nature can also have a
detrimental effect when hurricanes and storms erode beaches and wash over dunes and marshes.
Recession of barrier structures can also result from reduction in the amount of sediment
supplied to the coast due to damming of rivers and other factors. Also, sea level rise, due to melting
of polar glaciers, has resulted in flooding of barrier habitats. Reduction of onshore transport of
sediment from offshore sources is an additional cause of recession of barrier resources.
59
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Table 18. Areal Changes (in Acres) in Selected Coastal Barrier Resource Systems Units, ca. 1940's to
1982 (from Watzin and Baumann, 1983)
Unit Name
Florida
Cape San Bias
Moreno Point
(Destin)
Alabama
Mobile Point
Mississippi
Deer Island
Cat Island
Louisiana
Isles Dernieres
Texas
Bolivar Peninsula
Follets Island
Boca Chica
Land Area*
1982
3,002.43
3,147.90
3,769.79C
3,945.49
(1979)
505.18
549.04
2,381.55
6,667.19
3,005.59"
2,519.6
Land Areab
Pre-1982
2,915.70
(1943)
3,267.81
(1955)
3,945.49d
(1979)
3,969.65
(1956)
544.05
(1952)
804.77
(1956)
4,616.67
(1956)
6,759.65
(1956)
2,914.18
(1956)
2,580.97
(1948,1950)
I
Land Area
Change
+86.73
-119.91
-175.70
0
-38.86
-255.73
-2,235.12
-92.46
+91.41
-61.32
Percentage
Land Area
Change
+2.97
-3.66
-4.45
0
(within error
-7.14
-31.77
-48.41
-1.37
+3.13
-2.37
Annual Percentage
Land Area
Change
+0.08
-0.13
-1.48
0
margin)
-0.23
-1.22
-1.86
-0.05
+0.12
-0.07
* Land area includes the following habitats: fastlands, wetlands, and developed land. Excluded habitats
include: open water and inland open water. These numbers differ slightly from the total without water
reported in earlier tables because different computational procedures were used.
The numbers(s) in parentheses indicate the year of the earlier map base. Multiple dates indicate more
than one quadrangle map was required to cover the entire CBRS unit and these different maps had
different data dates.
c After Hurricane Frederick.
Before Hurricane Frederick.
* Does not' include extensive erosion caused by Hurricane Alicia (1983).
60
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Living Resources
Several publications give a broad overview of Gulf habitats. The living marine resources that
occupy Gulf coastal habitats have been described in a comprehensive atlas of the coastal and oceanic
resources (NOAA, 1985) which summarizes: 1) physical environments, 2) biotic environments, 3)
living marine resources, 4) economic activities, 5) marine environmental quality, and 6) jurisdictions.
Maps contained in the NOAA atlas are at a scale of 1:4,000,000. The distribution of forested and
nonforested wetland, seagrass, and benthic algal communities are summarized on maps; however,
acreages are not given in this large-scale, regional overview.
The occurrence and distribution of softTbottom communities of the northwest Gulf of Mexico
is contained in an atlas prepared by Minerals Management Service (1983b). Distribution patterns of
the biota are presented. Species are listed and numbers of individuals, percentage of the total catch,
and seasonal distributions of selected biota are presented.
The following is a summary of the acreages and functions of the major vegetated Gulf habitats.
This analysis is not intended to be a comprehensive literature review, but rather as a summary of
data pertinent to the status and trends of each habitat type. The major vegetated habitats, marshes,
seagrasses, and mangroves, have several common features and functions. Thayer and Ustach (1981)
found that regardless of community type, organic material exported from these systems is an
important energy source to adjoining estuarine and coastal systems. Some technical questions remain
concerning the relative importance of the various sources of organic matter in the nutrient and
energy dynamics of estuaries (Nixon, 1980). However, it is well documented that marshes,
mangroves, and seagrasses serve as feeding, reproductive, and nursery habitats for many species of
aquatic organisms and their existence is critical to important Gulf fishery and recreational resources
(Durako et al., 1985). A comparison of the relative importance of marsh and seagrass systems to
fauna has been conducted by Orth et al. (1984) and Orth and Montfrans (1990). The relative
importance of these habitats to selected species may vary regionally and latitudinally.
Marshes
The total area of tidal marsh along the Gulf coast was estimated by Lindall and Saloman (1977)
at 6 million ac (2.43 x 106ha), which represented 63% of the tidal marsh area in the United States.
At the time of that study, Louisiana contained most of the Gulf's tidal marsh (64%), followed by
Texas (19%), Florida (15%), Mississippi (1%), and Alabama (0.6%). The most recent estimate of Gulf
wetland acreage is given by NOAA (1991) to be 3.8 million acres (1.54 x 106 hectares) (Table 5).
The NOAA report summarizes the distribution of Gulf tidal marsh habitat as follows: Louisiana 69%;
Texas 17%; Florida 10%; Mississippi 2%; and Alabama 1%. The differences in acreage and
61
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percentages between these two studies probably represents a combination of delineation of habitat
types, sampling differences, and actual changes in acreage.
Spartina alterniflora is the predominant halophyte of Atlantic coast marshes. However, the
general environmental conditions of Gulf coast tidal marshes are quite different from tidal marshes
found along the Atlantic coast. Also, these conditions vary geographically along the Gulf coast. The
northeastern Gulf marshes are characterized by irregular flooding, low energy wave and tidal action,
and long periods of exposure (Stout, 1984). This area is also characterized by large discharges of
fresh water and raised marsh elevations (Crance, 1971; Eleuterius, 1973). These environmental
conditions are thought to be responsible for the predominance of J. roemerianus, in salt marshes of
the northeastern Gulf of Mexico. Kruczynski (1978) estimated that approximately 28% of intertidal
habitats along the entire Gulf coast of Florida are dominated by /. roemerianus, and that species was
the dominant herbaceous halophyte from Florida Bay to Pensacola, Florida. Eleuterius (1976)
observed that J. roemerianus was the dominant plant in 92% of the tidal marsh acreage in Mississippi
and 52% of tidal marsh acreage of Alabama. Approximately 8% of the U.S. tidal marsh area is found
in Florida, Alabama and Mississippi (627,249 acres; 253,947 hectares) and much of this acreage is
vegetated by J. roemerianus (Stout, 1984).
The zonation of Gulf tidal marsh plant species within a marsh is dependent Upon several
ecological factors including salinity, tidal range, and soils (Kurz and Wagner, 1957). thayer and
Ustach (1981) found that S. alterni flora occurs from mean sea level up to the level of the highest
predicted tide, and that J. roemerianus occurs landward from the zone occupied by Spartina.
Distichlis spicata and Spartina patens occur above the mean high tide line. : Spartina cynosuroides
is also found in low tide areas of many Gulf coast marshes (Eleuterius, 1976). Spartina patens and
S. alterni flora are the dominate species in tidal marshes of Louisiana, where marshes are dominated
by S. alterni flora at low elevations, and Salicornia spp. and Juncus at higher elevations. These
species are dominant in approximately 30% of the total Louisiana marsh area (Ferret et al., 1971).
The acreage and species composition of the four major plant communities as described by Chabreck
(1982) are discussed in Quality of Coastal Habitats.
Durako et al. (1985) reviewed the structure and function of tidal marshes of Florida.
Geologically, Florida marshes are a transitional community between mangroves and fresh water
communities. Grasses (Graminae), sedges (Cyperaceae), and rushes (Juncaceae) are the plant groups
most frequently found in Florida salt marshes. S. alterni flora is found in high salinities and S. patens
is more common at lower salinities. Cladium jamaicense (sawgrass) is also found in low-salinity
areas. /. roemerianus is found in association with mangroves south of Homestead and predominates
low energy tidal marshes from Tarpon Springs to Pensacola Bay (the Florida panhandle). There is
usually a fringe of S. alterni flora along tidal creeks and the waterward margin of Juncus marshes.
62
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Intertidal areas of Texas marshes present harsher conditions for development of tidal marsh
systems compared to other parts of the Gulf. Pulich (1990) reviewed the occurrence of marsh plant
species and the environmental regimes affecting their production in Texas estuaries. A gradient in
marsh types results from the decreasing precipitation gradient occurring from Sabine Lake southward
to Corpus Christi and Laguna Madre. The corresponding decrease in fresh water inflows, combined
with low tidal range, produces marsh vegetation adapted to moisture deficits, high groundwater
salinities, and low inputs of nutrients due to infrequent freshwater discharges. Along the northern
Texas coast, from Sabine Lake to Galveston Bay, extensive marshes are dominated by S. alterniflora
or S. patens-D. spicata. From Matagorda Bay south to Aransas Bay, limited amounts of S.
alternifiora occur in fringing bands near the water's edge, while extensive interior marshes of
Salicornia-Distichlis occur at slightly higher elevations. From Corpus Christi Bay south to lower
Laguna Madre and the Rio Grande Delta, both fringe and interior marshes are dominated by
succulent halophytes such as Batis maritime (saltwort), Salicornia yinginicus (glasswort), and
Borrichia frutescens (sea-oxeye). Changes in distribution and abundance of marsh indicator species
were attributed to moisture and nutrient requirements, rather than salinity tolerances.
Although tidal flats and sand flats are not vegetated, these intertidal areas constitute a distinct
habitat and major resource of the middle and lower Texas coastal zone. Because of low tidal range
and arid conditions, hypersaline flats develop instead of marsh wetlands. These areas are covered
by algae mats (diatom and cyanobacterial mats) and are very productive. Important functions of
these areas are the export of nutrients and organic matter to other estuarine habitats and feeding
habitats for foraging fish and decopods (Pulich and Rabalais, 1986; Pulich and Scalan, 1989).
Because of their superficial "wasteland" appearance, pressure to develop and destroy this habitat has
persisted.
"" Nationally, most of the research on the ecology of tidal marshlands has been confined to systems
dominated by Spartina spp. The biogeochemical cycling of Spartina marshes may not be applicable
to Juncus, Salicornia, or Batis marshes. The life cycle, metabolic pathways, and nutritive value of.
these halophytes are different (Pulich, 1990; Kruczynski et al., 1978a,b). The primary production
of Juncus marshes on the west coast of Florida is similar to the productivity of some east coast
marshes, but the standing crops and morphological features of Juncus differ within a marsh
depending, upon soils, tidal flooding, and elevation. Based upon these factors, Kruczynski et al.
(1978a) divided Juncus marshes into lower, middle, and upper marsh zones.
The primary ecological functions of salt marshes include primary productivity, detrital export,
nutrient export, sediment trapping, pollutant removal, and feeding grounds and protected habitat for
juvenile fish and shellfish. Durako et al. (1985) reported that over 90% of net primary productivity
63
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of a salt marsh may form plant detritus. The diverse microbial and algal communities of tidal
marshes contribute to the nutritive value of tidal marsh detritus, and the rate of detrital formation
is dependent upon flooding frequency within a marsh (Kruczynski et al., 1978; Stout, 1984). Animal
production is very high at the marsh-estuarine interface due to the abundant food sources found
there; plant detritus forms the base of the food chain for many marsh and estuarine species (Odum
and de la Cruz, 1967; Stout, 1984),
There is some scientific disagreement over the extent to which nutrients, including those
derived from salt marsh detritus, are exported from marsh areas and utilized by coastal fisheries
(Nixon, 1980). While the balance of energy sources driving these dynamic systems has not yet been
fully understood, the nursery role that marshes play for many species of commercial and recreational
importance is well known (Hackney, 1978). More than 1,100 species of vertebrates and invertebrates
depend upon salt marsh-estuarine habitats for at least one stage of their life cycle (Durako et al.,
1985). Production of commercial and sports fisheries depends upon the ecological viability of tidal
marsh habitats. Distribution and abundance of juvenile fishes in tidal marshes are dependent upon
salinity, food availability, water quality and depth, bottom type, and vegetative cover (Durako et al.,
1985; Subrahmanyam and Coultas, 1980).
Estimates of the numbers of commercial and recreational fish that spend at least a portion of
their history in estuarine habitats vary (McHugh, 1976; Lindall and Saloman, 1977, Thayer and
Ustach, 1981; and Comp and Seaman, 1985). However, most authors agree that species which make
up in excess of 90% of the Gulfs commercial or recreational catch spend a portion of their life cycle
in tidal creeks and marshes. Several species, such as penaeid shrimp and blue crab, may spend the
majority of their life cycle in wetlands and shallow estuarine habitats.
A diverse fauna has adapted to the unique environment of tidal marshes. Zooplankton is,
composed chiefly of the larvae of fiddler crabs and other decapods; meiofauna consist primarily of
nematodes and harpacticoid copepods; and macroinvertebrates include crustaceans (especially crabs),
molluscs, annelids, and insects. Several crustaceans such as grass shrimp, penaeid shrimp, blue crabs,
as well as resident and migratory fishes, are seasonally abundant in marsh creeks. Birds are one of
the larger carnivorous groups in this system and can bioconcentrate persistent pollutants which
accumulate through the food chain (Stout, 1984).
Subrahmanyam et al. (1976) observed 55 species of benthic invertebrates in Juncus marshes of
north Florida. Zonation of benthic fauna was correlated with soil type, flooding frequency, and
plant zonation. While the feeding strategies among this diverse group vary, detritivores were the
most common group. Detritivores in turn provide food for many commercially important species
which invade tidal creeks and marshes at high tide (Subrahmanyam and Coultas, 1980) Minello et
64
-------
al. (1986) demonstrated that waterways into vegetated marshlands are essential for their maximum
use by fisheries organisms.
Marshlands also provide habitat for many species of waterfowl and mammals. Of the five fur-
bearing species economically important in the south, the muskrat was the most abundant in three of
the four vegetative types studied by Palmisano (1973) (Table 19). The fur industry has changed
dramatically since the early 1970's, and these data may not be representative of the current
conditions.
Table 19. Estimated Fur Catch per 1,000 Acres of Coastal Marsh (from Palmisano, 1973)
Vegetative Type
Species
Muskrat
Nutria
Mink
Raccoon
Otter
Brackish
Mean Maximum
84.4
86.4
1.1
b
.2
6,477.7
191.1
12.8
15.6
.7
Intermediate Fresh
Mean Maximum Mean Maximum
97.5
284.9
.9
b
.4
513.9
499.6
11.9
6.3
1.3
78.5
512.7
2.1
b
.5
646.8
884.4
14.2
31.0
1.3
a Mean values are determined from recent records. Maximum values are an average of long-term
maximum-catch figures.
b Inadequate records.
Mississippi tidal marshes were sampled during 1968-1969 by Eleuterius (1972) to determine
species composition, area, zonation, production, and regulating factors. That study area covered
three of the four major estuarine systems in Mississippi: the Pascagoula River system, Biloxi Bay,
and Bay St. Louis. The total area of Mississippi tidal marshes was 66,931 ac (27,098 ha).
In addition to salinity-induced zonation along Mississippi estuaries, there was also a zonation
from low marsh to uplands. Of the total 66,931 ac (27,098 ha) of marshlands, 63,982 ac (25,904 ha)
were mainland salt marsh, 823 ac (333 ha) were freshwater marsh, and 2,126 ac (861 ha) of salt marsh
were found on offshore barrier islands. J. roemerianus dominated 96% (61,398 ac; 24,857 ha) of the
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mainland salt marsh. S. alterni'flora dominated approximately 30% (2,028 ac; 821 ha), S. patens 0.7%
(460 ac; 186 ha), and Scirpus olneyi 0.1% (96 ac; 39 ha) (Eieuterius, 1972).
Three hundred species of vascular plants were identified in Eieuterius' survey. Eieuterius
(1972) delineated two major divisions of tidal marshes: the lower region (saline and brackish) and
upper region (intermediate and freshwater). The lower region exhibited higher and more stable
salinities. The upper region exhibited lower salinities with greater fluctuations in salinity and greater
diversity of plant species. High plant diversity was the result of changes of freshwater input; Most
lower marshes were dominated by J. roemerianus with no definite sharp delineation between zones
within the marsh. S. alterni flora was predominant along creeks in saline marshes. There was a
reduction of S. alterni flora and increased density of /. roemerianus in the lower brackish marsh.
Seagrasses
Seagrass meadows cover approximately 7,440 mi2(19,275 km2) of the Gulf of Mexico, including
Mexico and Cuba. Seagrasses grow in shallow, clear waters in protected estuaries and nearshore
waters (e.g. Florida Big Bend Area). Iverson and Bittaker (1986) and Orth and Montfrans (1990)
estimated total seagrass coverage in Gulf states to.be 2.47 million ac (1 million ha). Florida has the
most acreage of seagrasses among the Gulf states-2.2 million ac (890,000 ha). Acreage in other Gulf
states is: Alabama-30,381 ac (12,300 ha); Mississippi-4,940 ac (2,000 ha); Louisiana-10,127 ac (4,100
ha); Texas-169,195 ac (68,500 ha).
Areal coverage of selected seagrass beds is given in Table 20. There are approximately 800,000
ac (323,887 ha) of sea grasses within Gulf estuaries. Approximately 95 percent estuarine acreage is
in Florida and Texas, where seagrasses occupy approximately 20 percent of bay bottoms (Thayer and
Ustuach, 1981). Although often considered continuous around the entire periphery of the Gulf, a
combination of low salinity and high turbidity results in only narrow bands or scattered patches of
seagrass communities, mostly in bays, from Louisiana to Copano-Aransas, Texas. Discontinuous
nearshore beds are found from Apalachicola, Florida, to Brownsville, Texas. Beds are particularly
well developed around the Chandeleur and Breton Islands, Louisiana, and in Laguna Madre, Texas.
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Table 20. Areal Coverage (Acres) of Selected Seagrass Beds.
Location
Size
Reference
Gulf of Mexico
Florida embayments
Big Bend area
Outer Florida Bay
Inner Florida Bay
Florida Keys Reef Tract
Alabama coast
Mississippi coast
Louisiana coast
Texas lagoons
157,403
741,300
716,590
624,000
197,680
30,393
4,942
10,131
169,264
McNulty et al. (1972)
Iverson and Bittaker (1986)
Iverson and Bittaker (1986)
Zieman et al. (1989)
Enos and Perkins (1977)
Minerals Management Service (1983a)
Eleuterius and Miller (1976)
Minerals Management Service (1983a)
Bureau of Economic Geology (1980)
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Five species of seagrasses occur in the Gulf: Thalassia testudinum (turtle grass), Halodule
wrightii (shoal grass), Syringodium fill forme (manatee grass), Halophila engelmannii, and Halophila
decipiens (Zieman and Zieman, 1989). In addition, Ruppia maritima (widgeon grass), which is
generally not considered as a true seagrass, is commonly reported in coastal zones of all Gulf coast
states.
Seagrasses display vertical zonation. Halodule can occur into the low intertidal zone. T.
testudinum, S. filiforme, and Halophila are found below the mean low tidal level. While T.
testudinum is the most abundant Gulf submergent, Halodule is dominant in Mississippi and Alabama,
and R. maritima is dominant in some areas of coastal Louisiana. Light, salinity, temperature,
substrate type, and currents are locally important factors that affect distributional patterns (Ferguson
et al., 1981).
In Texas, Halodule is the dominant species along the northern and middle coast, south to
Aransas Bay. Halodule and Syringodium are most abundant in lower Laguna Madre. Halodule
dominates in upper Laguna Madre. Annual changes between Halodule and Ruppia populations often
occur at northern and middle Texas coastal locations (Pulich and White, 1990).
Eleuterius (1977) reviewed four local species of seagrasses of Mississippi, including information
on productivity and local distribution. In that report, Eleuterius summarized most of the existing
literature on the following species: T. testudinum, H. wrightii, S. filiforme, and H. engelmannii. All
are found in estuarine beds north of the barrier islands off the Mississippi coast. These four species
are considered to be primarily tropical flora, and the Mississippi coast represents their northern limit.
The productivity for T. testudinum for Mississippi was determined to be at 1,848.5 gm dry
weight/m2/yr, and yearly production is about twice the standing crop.
The effects of a large-scale environmental perturbation, Hurricane Camille in 1969, on
seagrasses and macrophytic algae in. Mississippi waters were investigated by Eleuterius and Miller
(1976). They concluded that considerably smaller areas of coastal bottoms were vegetated with
seagrasses in the early 1970's compared to pre-1969 surveys. Physical disturbance of bay bottoms
due to heavy wave action was thought to have destroyed large areas of seagrass beds. Approximately
20,000 ac (8,097 ha) of submerged vegetation in Mississippi Sound were located and mapped in 1969.
Approximately 11,676 ac (4,727 ha) were lost as a result of Hurricane Camille. Losses due to low
salinity in the winters of 1971 through 1975 reduced the remaining acreage to 4,866 ac (1,970 ha).
Zieman and Zieman (1989) discussed the distribution, abundance, and productivity of dominant
species in seagrass systems on the west coast of Florida, from Florida Bay to Apalachicola Bay.
These seagrass beds were dominated by three species, T. testudinum, S. filiforme, and H. wrightii.
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Seagrasses occurred both on the shallow, zero-energy continental shelf and in inshore bays and
estuaries. The largest seagrass meadow is located within the boundaries of the Everglades National
Park in Florida Bay and is 1,359,050 ac (5,500 km2). The second largest is located between Tarpon
Springs and St. Marks and is 741,300 ac (3,000 km2). Tampa Bay once had 76,601 ac (31,000 ha) of
seagrass meadows, but as of 1982, the grassbeds have declined to approximately 20,000 ac (8,097 ha)
(Lewis et al., 1985; Lewis et al., 1991). Zieman and Zieman (1989) observed that grass meadows in
Florida estuaries were noticeably more stressed and impacted by human activities than the more
pristine nearshore beds. They observed that seagrasses within west Florida estuaries must rank
alongside the seagrasses of Chesapeake Bay as some of the most devastated and degraded in the entire
country. Urban development and dredging and filling are the major threats to seagrass beds in this
region. Motor boat propeller scouring is also a major threat to seagrass meadows in shallow waters.
Zieman and Zieman (1989) concluded that the importance of the loss of seagrasses to both the
ecology and economy of Florida are far out of proportion to the total acreage lost due to the critical
nature of estuarine seagrass meadows as nursing areas. While measures must be taken to ensure the
continued productivity of the nearshore beds, it is most critical that the water quality degradation
that has caused extensive losses of estuarine grass beds be arrested and reserved. Kenworthy and
Haunerdt (1991) summarized the dependency of seagrasses on adequate light and water quality
conditions and presented technically sound arguments for revising water quality standards and
initiating monitoring programs to protect and restore this dwindling resource'. The major man-
induced causes of seagrass declines worldwide are reviewed by Thayer et al. (1975) and Shepherd et
al. (1989). They list the main reasons for the "cultural" decline of seagrass meadows to be increases
in turbidity and sediment mobilization resulting in light reduction, increased epiphytism due to
nutrient enrichment, and increased grazing due to community imbalances. Once seagrass meadows
are totally destroyed, they are likely to remain lost forever, along with the myriad of organisms that
they feed and shelter.
The distribution of seagrasses on the broad, shallow Continental Shelf in the Florida Big Bend
area was also studied by the MMS (1985) which mapped and inventoried seagrass beds using a
combination of aerial photography (remote sensing) and shipboard/diver observations. The seaward
extent of major seagrass meadows was determined, and major benthic habitats were classified and
delineated. These mapping activities delineated 575,479 ac (232,987 ha) of dense seagrasses,
1,230,643 ac (498,236 ha) of sparse seagrasses, and 691,195 ac (279,836 ha) of patchy seagrasses
between Ochlockonee Bay and Tarpon Springs.
Three major species associations were found in the MMS (1985) study. An inner or nearshore
association consisted of T. testudinum, S. fHi forme, and H. wrightii that occurred in waters less than
29.5 ft (9 m). Seaward of that group, but still in waters less than 29.5 ft (9 m) was a community
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vegetated by five seagrass species: turtle grass, manatee grass, shoal grass, H. decipiens, and H.
engelmannii. Farther offshore, between the 32.8 and 65.6 ft (10- and 20-m) depth, a mixed
macroalgal/seagrass assemblage, in which the two Halophila species were the only seagrasses present;
was common. One of the unique aspects of the seagrass beds in the Big Bend area is the extended
nature of the deeper fringing zone of seagrasses dominated by H. decipiens and H. englemannii and
macroalgae. The macroalgae account for 21% of total blade density in this location. These
macroalgae communities have been relatively little studied, but are thought to provide habitat and
a food source for many species of the marine ecosystem.
Iverson and Bittaker (1986) investigated seagrass species composition, biomass, and areal
coverage on the seabottom along the West Florida Continental Shelf. They observed that T.
testudinum, S. filiforme, and H. wrightii form two large seagrass meadows along the northwest and
southern coasts of Florida. They found approximately 741,000 ac (3,000 km2) of seagrasses in the
Big Bend area and 1,358,500 ac (5,500 km2) in Florida Bay and concluded that the cross-shelf limits
of these two major seagrass beds are controlled nearshore by increased water turbidity and lower
salinity and offshore by light penetration to depths receiving 10% or more of sea surface
photosynthetically active radiation. Similar to the findings of the MMS study (1985), Iverson and
Bittaker observed that T. testudinum and S. filiforme were most abundant in shallow depths and H.
wrightii grew in shallow waters near the inner edges of the beds, while H. decipiens and H. wrightii
grew in deeper water outside the beds. Ruppia maritima grew chiefly in brackish water near the
mouths of rivers.
Many studies have enumerated the fauna inhabiting seagrass meadows (Zieman, 1982; Zieman
and Zieman, 1989; Lewis et al., 1985a; Sheridan and Livingston; 1983; and others). For example,
Sheridan and Livingston (1983) quantified the infauna and epifauna inhabiting a H. wrightii meadow
in Apalachicola Bay, Florida. Fifty-eight infaunal species were recorded, an average of 35 species
per monthly sample. Maximum faunal abundance was 104,338 organisms per m2 in April. Sixteen
species accounted for 84% of the total numbers and 80% of the total biomass over the study period.
Numerical dominants were Hargeria rapax, Heteromastus filiformis, Ampelisca vadorum, Aricidea
fragilis, and oligochaetes. Biomass dominants were Tagelus plebeius, Neritina reclivata, Ensis minor,
and Haploscoloplos fragilis. Epibenthic fishes and macroinvertebrates were sampled by monthly
trawling. Twenty-three species of fishes (mostly juveniles) were collected. Diversity and abundance
were greatest during the months May through September. Bairdiella chrysoura (silver perch),
Orthopristis chrysoptera (pigfish); and Lagodon rhombodies (pinfish) made up 76% of the total fish
numbers. Eleven species of macroinvertebrates were collected in trawls, most abundantly in June
and July. Callinectes sapidus (blue crab) made up 61% of the total invertebrate numbers. Sheridan
and Livingston postulated that the influx of juvenile fishes and crabs into the Halodule meadow in
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summer months caused a coincident decline of infaunal population densities (number per m2) through
predation. Infaunal biomasses were largely unaffected by these predators because the biomass
dominants were large or deep-burrowing species.
Mangroves
Wood et al. (1969) described the functional roles of mangroves. These include the following
factors:
1. Organic productivity is relatively high, and for some species it rivals or often exceeds that
of subsidized agricultural crops.
2. Standing crops are high but few organisms feed directly on the plant. As a result,
mangrove systems produce large quantities of detritus, which plays a major role in the
dynamics of the particular system and the estuary of which they are a part.
3. Leaves, stems, and prop roots present surfaces for epibiotic organisms. This increases both
the primary and secondary productivity of the habitat and the epibiota may be significant
food sources for fish and invertebrates.
4. Roots, stems, and leaves reduce current velocity, thus promoting sedimentation of both
inorganic and organic matter. Entrained allochthonous and autochthonous material
decomposes, thus recycling nutrients within the system.
5. The root system generally binds sediments and retards erosion.
6. The presence of above-substrate vegetation and lateral zonation presents a wide variety of
habitats for protection and growth of fish, birds, and invertebrates.
f
Four species of mangroves are native to the United States: red mangrove (Rhizophora mangle),
black mangrove (Avicennia germinans), white mangrove (Laguncularia racemosa), and buttonwood
(Conocarpus erectus). Only black mangroves occur more or less continuously from the Dry Tortugas
to the islands off the Mississippi Delta (Humm, 1973). Black and red mangroves also occur in Texas
(Duncan, 1974; Sherrod and McMillan, 1985). The distribution of mangrove wetlands is limited by
temperature, and permanent communities generally do not occur north of 25° north latitude or in
areas where temperatures routinely fall below'-4° degrees C (Thayer and Ustach, 1981).
Approximately 450,000 ac (182,186 ha) of mangroves occur along the Gulf coast, with the largest
proportion occurring in Florida. The Ten Thousand Islands area of Florida has the greatest aereal
extent of mangroves along the Gulf coast.
The different species of mangroves have different ecological requirements and exhibit zonation
along environmental gradients. Red mangroves are generally found in the deepest waters along
shorelines; landward are black mangroves, white mangroves, and buttonwoods (McNulty et al., 1972).
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Factors involved in zonation are disputed, but are generally considered to be the degree and duration
of inundation and soil and water salinity (Lugo and Snedaker, 1974).
Lewis et al. (1985b) described the three mangrove species to have the following requirements:
1. The red mangrove, R. mangle, is the most saline tolerant. Arching prop roots act as a tree
stabilizer and brace, as well as aid in gas exchange under anoxic conditions, as these trees
often grow in oxygen-depleted areas.
2. The black mangrove, A. germinans, is found landward of the red mangrove. It reaches
heights of 60 feet and is supported by a network of horizontal cable roots that give rise to
vertical aerating roots called pneumatophores, which appear as finger-like emergents in
the soil.
3. The white mangrove, L. racemosa, is the most landward species of the three. When its
habitat is flooded for extended periods of time it will produce adventitious roots.
Lewis et al. (1985b) state that mangrove forests thrive under strict environmental parameters.
Mangroves grow best in 10-20 ppt saltwater. These plants require a certain amount of fresh water
for adequate growth, and the salinity factor is important because it enables the mangroves to better
compete with other salt-tolerant plants. Fluctuating tides are necessary because they act to remove
toxic substances from the root system. Lewis et al. (1985b) described five types of mangrove
communities:
1. The basin forests, which are dominated by red mangroves, are located near terrestrial
runoff sites and associated with regular tidal flushing. In those areas where tidal flushing
rarely occurs, low salinities exist and white and black mangroves dominate.
2. The riverine forests are associated with rivers that are apt to flood. These forests
frequently are inhabited by the tallest red mangrove stands.
3. The fringe forests are found on the edge of the mainland or surrounding islands and act
as the buffer zone in high-energy situations.
4. The overwash forests are characterized by low organic accumulations that are frequently
washed away by tidal flushes.
5. The dwarf or scrub forests are stands of mangroves that are stunted in growth due to low
organic productivity, making few nutrients available to them.
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Distribution and productivity of mangroves may also be related to soil parameters. Odum et al.
(1982) found that:
1. Mangroves can grow on a wide variety of substrates including mud, sand, peat, and
limestone crevices.
2. Mangrove ecosystems appear to flourish on fine-grained sediments that are usually
anaerobic and may have a high organic content.
3. Mangrove ecosystems that persist for some time may modify the underlying substrate
through peat formation. This appears to occur only in the absence of strong physical
forces.
4. Mangrove peat is formed primarily by red mangroves and consists predominantly of root
material.
5. Red mangrove peats may reach thicknesses of several meters, have a relatively low pH, and
are capable of dissolving underlying layers of limestone.
6. When drained, dried, and aerated, mangrove soils usually experience dramatic increases in
acidity due to the oxidation of reduced sulfur compounds. This greatly complicates their
conversion to agriculture and other uses.
Several studies have described the occurrence and importance of mangrove communities in the
coastal system of Florida (Lewis et al., 1985b; Odum et al., 1982; Patterson, 1986; Thayer and Ustach,
1981; Thayer et al., 1987; and Yokel, 1975a and b). Ninety percent of the approximately 500,000
ac (202,429 ha) of mangrove forests located in Florida are found in four counties: Lee, Collier,
Monroe, and Dade. These mangrove forests serve as "land stabilizers," because the trees act as a
barrier, protecting the inland ecological systems from storm surges.
Areal estimates of mangrove communities in Florida vary from 430,000 to 650,000 ac (174,089
to 263,158 ha) due to: 1) the inclusion or exclusion of bays, ponds, and creeks, or 2) the incorrect
identification of mangroves and marshes from aerial photography (Lewis et al., 1985b). Clear
examples of differences in these estimates may be observed by comparing acreages given by the
Coastal Coordinating Council (CCC) with those given by the National Wetland Inventory (NWI)
(Lewis et al. 1985b). The CCC estimates 469,000 ac (190,000 ha) with a 15% error (400,000-540,000
ac; 162,000-219,000 ha). The NWI estimates 674,241 ac (272,973 ha) of mangroves (and 383,317 ac
(155,190 ha) of tidal marshes). Lewis et al. (1985b) theorize that the difference in acreages may be
the result of misidentification between marshes and mangroves on aerial photographs. A summary
of the acreages of emergent wetlands of coastal counties in Florida according to the NWI are given
in Table 21.
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Table 21. Estimates of Emergent Wetland Acreages (Acres) of Gulf Coast Counties in Florida
(Source: National Wetland Inventory, St. Petersburg, 1982, modified from Lewis et al., 1985b).
County
Bay
Charlotte
Citrus
Collier
Dixie
Escambia
Franklin
Gulf
Hernando
Hillsborough
Indian River
Jefferson
Lee
Levy
Manatee
Monroe
Okaloosa
Pasco
Pinellas
Santa Rosa
Sarasota
Taylor
Wakulla
Walton
TOTAL
Mangroves
(acres)
_
22,431
3,394
85,513
243
78
-
,
136
10,095
4,133
-
40,164
-
5,754
361,036
-
10,588
7,216
148
1,115
154
-
14
548,114
Tidal Marshes
(acres)
7,207
3,831
36,273
14,177
19,259
2,075
16,538
5,257
11,792
1,675
910
4,865
2,832
35,703
1,029
11,834
257
12,228
423
7,125
1,128
23,740
19,658
2,938
238,994
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Mangrove forests are composed of a "habitat mosaic," and there is much interaction between
the different habitats within this mosaic. Adverse impacts oil part of the mosaic can result in loss
of production within the entire forest (Lewis et al., 1985b). This complex community is particularly
important to maintenance of fish populations. There is a positive correlation between the acreage
of mangrove communities and the recruitment of juvenile fishes (Lewis et al., 1985b).
Mangrove forests are subject to degradation due to human activities. These activities include:
1) impounding or ditching for mosquito control, 2) reduction of fresh water input, 3) clearing, and
4) filling. Since 1972, 23,521 ac (9,523 ha) of wetlands (mostly mangroves) and open water have
been filled along the west coast of Florida and another 1,792 mi (2,890 km) of navigational channels
have been dredged. Of the approximately 650,000 ac (263,158 ha) of mangroves that existed before
1972, 23% have been lost and only approximately 500,000 ac (202,429 ha) remain. If the remaining
mangrove forests and marsh ecosystems are not protected, irreparable declines in fisheries production
will occur (Lewis et al., 1985b).
A number of studies have been conducted on the impact of pollutants on mangrove
communities. Mangroves do not actively take up organic pollutants but can concentrate heavy
metals. Concentrations of up to six times the background level of heavy metals have been found in
mangrove tissues. It is not certain whether heavy metal contamination is transferred to higher
organisms through the detrital food web. A mangrove tree may drop 217-1,082 gm dry weight/m2/yr
litter and this organic matter forms the base of the detritus food web in systems where mangroves
predominate (Lewis et al., 1985b).
The Rookery Bay Project (Yokel, 1975a and b) was initiated as a result of public concern over
the fate of coastal mangrove communities of Florida. In 1964, citizens of Naples, Florida became
alarmed at the loss of coastal wetlands and fisheries resources in Collier County. By 1966, the Collier
County Conservancy purchased 4,000 ac (1,619 ha) of bays, islands, and mangrove shorelines that
became the Rookery Bay Sanctuary. To date, over 5,000 ac (2,024 ha) of shoreline are included in
the Rookery Bay Sanctuary representing an investment of over $1 million of private capital. Located
5 mi (8 km) south of Naples, Florida, the Sanctuary consists of 5,038 ac (2,040 ha) of uplands,
marshes, mangrove forests, tidal creeks, and open water areas. Mangroves dominate this system with
2,368 ac (959 ha; 47%), while bays and tidal creeks account for 1,746 ac (707 ha; 35.1%), and tidal
marshes 688 ac (278 ha; 13.7%). These three submerged and intertidal habitats account for 95% of
the surface area. The results of the Rookery Bay study have provided some invaluable insights into
the requirements and vegetative characteristics of mangroves. Studies of preserved, pristine
mangrove systems, such as Rookery Bay, are critical to defining and quantifying the detrimental
impacts on these communities which have occurred due to coastal development.
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Odum et al. (1982) discussed the inhabitants of mangrove forests. Many animals utilize
mangrove forest habitats during various stages in their lives. However, very few species are
dependent directly upon growing mangrove tissue as a food source; these include the white-tailed
deer, the mangrove tree crab, a wood-boring isopod, and a variety of insects. Many species of
invertebrates and fishes depend upon mangrove detritus as a major source of energy.
The structurally diverse habitats provided by mangroves harbor a greater variety of bird life
than salt marshes, mud flats, and beaches. Wading birds, probing shore birds, floating and diving
water birds, aerially searching birds, birds of prey, arboreal birds, and migrating North American
land birds depend on the mangrove forests for food and shelter (Odum et al., 1982). Economically
important species associated with mangroves include the spiny lobster and grey snapper.
Endangered Species and Habitats
Coastal habitats are occupied by many plants and animals considered threatened or endangered
by extinction. According to the U.S. FWS (1979), "endangered" species are those that are in danger
of extinction throughout all or a significant portion of their range. A "threatened" species is defined
as one that is likely to become endangered in the foreseeable future. The U.S. FWS (1979, 1980,
1983, and 1987b), U.S. Department of the Interior, MMS (1986), heritage programs within the
various states (e.g., Texas Natural Heritage Program, 1989b,c), and various individuals (e.g. Eley,
1989) have summarized information on these species. The following discussion is not meant to be
a definitive summary of the ecology and life histories of endangered Gulf coast species, but rather
to emphasize their specific habitat requirements, where known.
The U.S. FWS (1980) published a series of species accounts to provide resource managers and
the public with information about Federally listed endangered and/or threatened vertebrate species
that occur along or within 62 mi (100 km) of the seacoast of the United States. Information on life
history, distribution,.requirements, and conservation is included for each species. This series is
intended to complement the computerized Sensitive Wildlife Information System (SWIS) developed
by the U.S. Army 'COE in coordination with the Offices of Endangered Species and Biological
Services of the U.S. FWS.
Figures 6 through 9 give the distribution of selected endangered and threatened vertebrates
which occur along the Gulf coasts as reported by FWS (1980). Although four species of sea turtles
are generally found along the entire Gulf coast (Figure 6), their numbers have severely declined in
recent years. The future of many of these species is threatened due to encroachment of development
on critical habitats.
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CO
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-fi-s
•43 o>
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Many states have programs which identify and list "sensitive" species and habitats. For
example, the Louisiana Natural Heritage Program (LNHP, 1988) is a comprehensive, computerized,
ecological inventory of the sensitive plants and animals and outstanding natural areas of Louisiana.
The program was initiated by the Nature Conservancy, a private conservation organization
specializing in the preservation of ecologically significant lands, including endangered species habitat,
outstanding examples of native natural communities, environmentally critical areas, and sites for
scientific research. The program is currently an interagency effort of the Louisiana Department of
Wildlife and Fisheries and the Louisiana Department of Natural Resources (LDNR). The data base
contains 545 elements in three classes: special plants, special animals (including water bird nesting
colonies), and natural communities. Forty-two percent of these elements have been recorded in the
Coastal Zone. Of 719 known occurrences of these elements in the Coastal Zone, 200 (28%) are
special animals, 222 (31%) are special plants, 131 (18%) are natural communities, and 166 (23%) are
unique features such as waterbird nesting colonies (162 occurrences), salt domes (3 occurrences), and
"champion" (i.e. large, old) trees (1 occurrence).
Because of the large number of occurrences of sensitive plants and animals in the Louisiana
Coastal Zone and the high level of natural and human threats associated with this area, the LNHP
and LDNR have published information to aid field investigators in identifying sensitive species and
habitats (Louisiana National Heritage Program, 1988).
A special list on sensitive plant and animal species occurring in 13 coastal Texas counties was
prepared by the Texas Natural Heritage Program (1989a). Also, the Texas Colonial Waterbird Census
Summary (1988) contains information on rookery locations by county and latitude/longitude
coordinates.
Special interest has recently been given to the survival of endangered and threatened species
of sea turtles in the Gulf of Mexico. The literature on sea turtles is too voluminous to summarize
in this document and the interested reader should contact the National Marine Fisheries Service for
more detailed information. Eley (1989) suggests that due to rapidly diminishing populations, marine
turtles are receiving much attention at this time. All seven of the world's recognized species of
marine turtles are classified as either endangered, threatened, or rare. Very little ecological or
behavioral information has been recorded for the five species of marine turtles which exist in the
Gulf of Mexico.
Most turtle research has focused on the Caribbean, Pacific, and Indian Ocean populations; the
northern Gulf of Mexico has received relatively little attention. Eley (1989) censused nesting females
in order to develop a population index for the Gulf Islands National Seashore and adjacent areas in
Florida, Alabama, and Mississippi. Aerial surveillance, the primary assessment method, was
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supported by ground surveys to ascertain the correction factor (number of nests missed).
Approximately 58 hours of aerial surveys and about 300 hours of ground surveys yielded 133
loggerhead turtle nests and two green turtle nests along this portion of the Gulf coast (Table 22). It
is not known whether suitability of beach nesting sites limits the populations of these species.
Accidental killing of sea turtles in fishing nets is thought to be a major source of mortality of all
species of sea turtles in the Gulf of Mexico.
Collard (1987) hypothesized that Kemp's Ridley turtle undergoes an extended pelagic planktonic
developmental stage. The young hatchlings appear to vanish shortly after entering the ocean and
only reappear in the subadult stage. The hatchlings frequently take refuge in floating aggregations
of Sargassum (a macroalga often found floating in large mats throughout the Gulf of Mexico)
probably as a predator-avoidance or resting tactic. Collard cited evidence that between 200 to 1500
adult female Kemp's Ridley turtles nest each year on a 17 km stretch of beach in Tamaulipas State,
Mexico. It is estimated that the number of females nesting each year will decrease by 3%.
Collard states that even though survivorship rates of Kemp's Ridley turtles are unknown at this
time, the odds are against the survival of hatchlings. Hatchlings apparently live off their yolk sac
reserves until reaching the Sargassum mats. The mats may furnish habitat, food, and transportation,
as well as protection, but it is not known how long they remain on the mats. Encrusting organisms
indigenous to Sargassum mats have been found growing on young turtles, indicating extended
periods of time spent there. Carr (1986) suggests that the turtles rely on the mats more as a
concentration point for food than for transportation or other functions. DeSola and Abrams (1933)
suggest that the Kemp's Ridley gut seems to be characteristic of herbivores, and it is not known
whether gut morphology changes yvith age in this species. Forage preference changes when these
turtles arrive in the demersal and inshore environment and exhibit an increased efficiency in
searching for food. Their diet primarily consists of portunid crabs and other crustaceans, gastropods,
bivalves, echinoderms, jellyfish, and squids.
Carr and Meylan (1980) examined the stomach contents of 15 green turtle hatchlings that were
washed ashore during Hurricane David (1979) and found pieces of Sargassum, sargassum snails
(Litiopa melanostoma), pelagic snails (Diacria trispinosd), and the isopod, Idotea metallica. This
indicates that green turtle hatchlings feed on a variety of food organisms during their pelagic stage.
Rookeries are concentrations of colonial bird species and there are many bird rookeries along
the Gulf coast. Information on rookeries is maintained by the U.S. FWS, state agencies, and heritage
programs. Keller et al. (1984) summarized ground and air surveys of the coastal areas of Louisiana,
82
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Table 22. Number of Turtle Nests Observed Along Sections of Coast, Summer 1989 (from Eley, 1989).
Location1
Fort Walton Beach (D)
Eglin AFB (U)
Navarre (D)
Santa Rosa Area (U)
Pensacola Beach (D)
Fort Pickens (U)
Johnson Beach (U)
Perdido Key (D)
Gulf Shores-Ft. Morgan
Dauphin Island (D&U)
Petit Bois (U)
Horn Island (U)
East Ship (U)
West Ship (U)
Number of Nests
9
33
13
13
11
8
8
9
(D&U) 13
12
1
2
1
0
Length of Beach
(km)
28.8
55.4
7.5
43.2
8.6
12.2
15.0
12.6
46.7
23.0
10.6
20.1
6.1
6.1
Density
(nests/km)
0.31
0.60
1.73
0.30
1.28
0.66
0.53
0.71
0.28
0.52
0.09
0.10
0.16
0.00
TOTAL
133
295.9
0.45
\D)= Developed Coastline
(U)= Undeveloped Coastline
83
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Mississippi, and Alabama to locate active and abandoned nesting sites of wading birds and seabird
colonies. When these surveys were first conducted in 1976 (Portney, 1977), 847,000 birds
representing 26 species were reported nesting in the area's coastal swamps, marshes, and on barrier
islands. The census was carried out via ground and aerial surveys by teams who determined species
composition, nesting habitat, and colony sizes. The teams also plotted colonies on l:250,000-scale
maps and on l:24,000-scale USGS topographic or wetland habitat maps.
Two surveys were conducted one month apart for each census year. The first was performed
during the nesting period of wading birds (herons, egrets, ibises) and Forster's terns, and the second
during nesting periods of other birds of interest. Individual colonies were defined as groups of birds
nesting together and separated by at least 0.62 mi (1 km). If nesting birds were not found within
0.62 mi (1 km) of a historic site, that colony was recorded as deserted.
The manual contains an atlas section which consists of a series of photographically reduced
l:250,000-scale maps that locate individual colonies by a six-digit number. Also included in this
manual are 98 maps at 1:24,000 scale which depict active rookery sites, historic sites, and new
rookeries.
Numbers of wading birds and rookeries are directly correlated with wetland acreage. Nesbitt
et al. (1982) documented that wading birds are dependent upon wetland habitats for nesting and
feeding sites. Most waders nest between February and August in colonies that may contain several
species and anywhere from a few dozen to thousands of nests. Colony sites may be used in other
seasons as roosting sites. The birds fan out daily from the colonies, flying as far as 20 mi (32 km)
to feed in a variety of wetland habitats. Most species eat small fish, frogs, aquatic insects, crayfish,
or fresh water prawns, while the ubiquitous cattle egret eats insects captured in fields, pastures, and
along roadsides.
The location and size of nesting colonies depend directly on the presence of suitable nesting
habitat and adequate amounts of food. Most colonies in Florida are located in natural wetland
habitats characterized by woody vegetation over standing water or on islands. An increasing number
of colonies are now being found in artificial habitats such as dredged-material islands and fresh
water impoundments. This latter situation may suggest that sufficient undisturbed natural sites are
no longer available (Nesbit et al., 1982).
It is very difficult' to accurately determine the number of wading birds nesting in any locality.
Such an inventory requires a well organized effort, because wading birds move freely over large areas
and colony sites are frequently abandoned in one area in preference for another site the next year.
84
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Thus, long-term records of birds in a single colony may not accurately reflect statewide population
trends.
Although absolute numbers of the entire population of wading birds in Florida was never
measured, some historical information does exist on the trends in wading bird populations in south
Florida. A historical review of population trends of waders in southern Florida (Lake Okeechobee
south into Florida Bay) indicates that the estimated total number has changed drastically over the past
century due to human activities, primarily hunting and habitat alteration (Robertson and Kushlan,
1974). The estimated number of south Florida waders dropped from 2,500,000 birds in 1870 to
500,000 in 1910, primarily due to plume hunting, and then increased to 1,200,000 by 1953 after
plume hunting was made illegal. Increased rates of wetland destruction since 1935 have resulted
in a second acute decline to an estimated 150,000 waders in 1970 (Robertson and Kushlan, 1974) and
130,000 in 1975 (Kushlan and White, 1977). This recent decline is more pernicious since it may be
due primarily to habitat destruction and appears to be continuing. A review of regional wading bird
trends in the southeastern coastal plain shows that with the exception of cattle egrets and a few
estuarine species, wading birds have experienced greater declines in Florida than in most other
coastal states (Ogden, 1978). The most serious declines in Florida have occurred among those species
inhabiting primarily freshwater habitats and nesting in interior colonies. It has become increasingly
apparent that more quantitative information on wading birds and their nesting sites is needed to
understand their problems and how their habitats may be protected.
85
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Case Histories
The following is a summary of the status and trends of vegetated habitats in specific regions,
bays, and estuaries. These case histories provide more detailed accounts of specific wetland and
seagrass modifications that have taken place along the Gulf coast.
Texas
Matlock and Osborn (1982) provide a detailed summary of the shallow water habitats of
estuaries in Texas. Approximately 601,000 acres (243,000 ha) of Texas bays are 4 ft (< 1.2 m deep)
(6 ft; £ 1.8 m in Corpus Christi Bay system). Approximately 24% of this shallow water habitat is
found in lower Laguna Madre. The Galveston and Matagorda Bay systems each have about 99,000
acres (40,000 ha); the San Antonio Bay, Aransas Bay, and upper Laguna Madre systems have 57,000
ac (23,000 ha); East Matagorda has 37,000 ac (15,000 ha); and Corpus Christi Bay has 32,000 ac
(13,000 ha).
The length of shoreline in Texas is 2,351 mi (3,792 km), including 365 mi (588 km) of Gulf
beaches. The Galveston Bay system has the longest shoreline, 411 mi (662 km), followed by
Matagorda, 285 mi (458 km); Aransas, 264 mi (426 km); and the lower Laguna Madre, 252 mi (406
km). The San Antonio Bay and upper Laguna Madre systems each have approximately 224 mi (361
km) of shoreline and the Corpus Christi Bay system has 171 mi (276 km) of shoreline. The shorelines
of Sabine Lake, East Matagorda Bay, and Cedar Lake are less than 78 mi (126 km) each.
Texas estuaries support large commercial and sport fisheries. Dominant fishes found in Texas
estuaries are species able to tolerate a wide range of salinity (Armstrong, 1987). The dominant fish
species represent many different feeding strategies and include planktivores, detritivores, and
predators. Abundant planktivorous species include: Anchoa mitchilli (bay anchovy), Brevoortia
patronus (Gulf mendhaden), Menidia beryllina (tidewater silverside j, Mugil cephalus (striped mullet),
and Lagodon rhomboides (pinfish). Penaeid shrimp are common and are considered detritivores and
predators. Other common predators are the crustaceans, Callinectes spp. (crabs), and Squilla empusa
(mantis shrimp). Common vertebrate predators include Micropogonias undulatus (croaker),
Leiostomas xanthurus (spot), Paralichthys lethostigma (southern flounder), Pogonias cromis (black
drum), and Cynoscion arenarius (sand trout) (Armstrong, 1987). Many of these species are dependent
upon tidal creek and marsh habitats for feeding and shelter during their life histories.
Volume, depth, and acreage of wetlands for the mid 1970's in the major Texas river delta
estuaries is given in Table 23. In general, there has been a dramatic decrease in emergent wetland
habitats during recent years. However, there have been some localized increases in wetland acreage.
86
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White and Calnan (1990) analyzed the wetland losses in seven river deltas in Texas: Colorado,
Nueces, Guadalupe, Lavaca, Trinity, Neches, and San Jacinto. Distribution of emergent vegetation
was mapped from sequential aerial photographs, dating from the 1930's to the late 1970's and 1980's.
Field studies were conducted in the Colorado River delta and the Trinity River delta to document
changes in quantity and quality of marsh habitats.
Table 23. Water Volume, Average Depth, and Marsh Area of River Deltas (from Armstrong, 1987)
Estuary
Sabine Lake
Galveston Bay
Matagorda Bay
San Antonio Bay
Copano-Aransas Bays
Corpus Christi Bay
Laguna Madre
TOTAL
Volume (km3)
0.326
2.911
2.134
0.754
0.925
1.147
2.574
10.771
Average Depth (m)
1.8
2.1
2.3
1.4
2.0
2.4
1.2
Marsh (acres)
33,987
13,387
28,232
11,937
13,214
— -—
A total of 52,758 ac (21,359 ha) of wetlands occurred in all areas studied in the 1930's (Table
24). The acreage of vegetated wetlands in the Colorado River delta has increased since the mid
195.0's. However, there were marked declines in wetland habitat in all other Texas river estuaries.
White and Calnan (1990) concluded that hurricanes can result in major deposition of sediments which
can later result in marsh accretion which has occurred in the Colorado River delta. However, the
general trend in the deltaic wetlands along the Texas coast is replacement of vegetated areas by
shallow, open water habitat or barren intertidal flats.
Extensive losses of vegetated wetlands occurred from 1930-1980 along the San Jacinto and
Neches Rivers. Those losses accounted for greater than 70% of the total wetland losses of Texas river
deltas. Two factors were responsible for those losses: 1) rise of water level from human-induced
subsidence, natural compactional subsidence, and global sea-level rise, and 2) processes which impede
movement of sediment to marshes, such as reservoir development in river drainage basins and
channelization and disposal of spoil on natural levees.
87
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Table 24. Areal Extent (Acres) of Vegetated Wetlands by River System and Year (Adapted from
White and Calnan, 1990).
Fluvial-Deltaic Area and Year
Vegetated Area (Acres)
Colorado River
1937
1956
1974
1982
Guadalupe River
1930
1957
1974
1979
Lavaca River
1930
1958
1979
Nueces River
1930
1959
1975
1979
Neches River
1938
1956
1987
San Jacinto River
1930
1956
1986
Trinity River
1930
1956
1974
1988
799
5,117
5,061
5,222
8,667
7,903
7,526
7,428
7,690
7,313
6,252
5,582
5,449
5,126
5,262
9,027
8,182
4,958
9,404
7,948
4,839
11,589
13,061
9,495
9,276
88
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The dynamics of submerged lands and associated coastal wetlands in Texas were recently
studied during two projects, namely the Texas Barrier Island Project (Longely and Wright, 1989) and
the Submerged Lands of Texas Project (White et al., 1983, 1985, 1986, 1987, 1989).
Barrier Islands
The final report of the Texas Barrier Island Project presents a detailed description of each
Texas coastal basin with emphases on habitats and hydrology. Information is presented on the area,
physical appearance, flora and fauna, and human impacts on each region (Longley and Wright, 1989).
This Project was sponsored by the MMS and was a cooperative venture between the U.S. FWS and
Texas General Land Office. The Texas Barrier Island Region was examined through systems analysis
utilizing models to integrate diverse information about the region. A summary of information on
the ten coastal basins that make up the barrier region is presented in Table 25. Human activities
have adversely affected this region. Subsidence due to withdrawal of subsurface water, oil, and gas
has resulted in substantive increases in open water. Deposition of spoil and construction of roads,
railroads, dams, and drainage canals have resulted in changes in historic hydrologic patterns.
Disposal of sewage has resulted in restrictions on shellfish harvesting. Pesticides historically applied
to crops have reached coastal waters due to erosion processes and have resulted in mortality of
seafood and other estuarine organisms (Longley and Wright, 1989).
Estuaries
The Submerged Lands of Texas Project was an extensive sampling program which was initiated
in 1975. Surficial bottom sediments were collected at regularly spaced distances across the submerged
lands and the project resulted in detailed sedimentological, geochemical, and biological
characterization of shallow water habitats and tidal marshes. Samples were analyzed to characterize:
(1) sediment distribution; (2) selected trace metals and nutrient concentrations; and (3) benthic
macroinvertebrate populations.
Data from the Submerged Lands Project are presented in seven atlases and comprehensive texts
for the following areas of the Texas coast: Brownsville-Harlingen (White et al., 1986), Kingsville
(White et al., 1989), Corpus Christi (White et al., 1983), Port Lavaca (White et al., 1989), Bay City-
Freeport (White et al., 1988), Galveston-Houston (White et al., 1985), and Beaumont-Port Arthur
(White et al., 1987). General changes in the distribution of wetlands can be estimated by comparing
aerial photographs from the 1950's with photographs taken in 1979. The authors recommend caution
in making comparisons because: 1) wetland map units used in the two projects were similar but not
identical; (2) moisture and tidal conditions were at higher levels during 1979 than during the 1950's,
89
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91
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which was a period of drought; (3) more refined interpretations were possible due to the high quality,
color-infrared photographs taken in 1979; and (4) wetland mapping criteria varied between the two
projects. The information contained in these and other studies for specific Texas estuaries are
summarized below.
Matagorda Bav
McGowen and Brewton (1975) reported a net loss of marsh area between 1856 and 1957 of
about 5,000 ac (2,024 ha) in Matagorda Bay (Port Lavaca). These losses were due to natural processes
and human activities. Natural processes included shoreline erosion or accretion, land-surface
subsidence and burial beneath sediment, and burial loss during drought. Human activities included
burial of marshes by spoil disposal along bay margins, erosion of spoil creating conditions favorable
for marsh growth, and submergence of marshes by construction of dams across tidal creeks.
A visual comparison of wetlands on maps from the 1950's with those of 1979 show the
following changes in the Port Lavaca area: 1) conversion of intertidal and subtidal unvegetated
shallows to grassflats; 2) reduction of grassflats along some margins of the bay; 3) spread of saltwater
marshes over wind-tidal flats; 4).expansion of shallow subaqueous flats in areas of saltwater and
brackish water marshes; 5) landward expansion of existing marshes; 6) loss of marshes due to erosion
of bay shorelines; 7) erosion of spoil and encroachment of marsh vegetation along spoil island
margins; and 8) reduction of wetlands as a result of human activities.
Between 1956-57 and 1979, many vegetated areas occurring along the margins of the Bay were
replaced by subaqueous flats or wind-tidal flats. This change was particularly evident in the marsh
between Blackjack Peninsula and Sundown Bay, the interior of the marshes of St. Charles Bay, and
the southwest-projecting marsh on the eastern side of the mouth of Lavaca Bay.
Human activities which produced this habitat loss included: 1) dredging and spoil disposal
along the Intracoastal Waterway; 2) construction of holding ponds northeast of Mission Lake along
Victoria Channel, and 3) dam construction at the mouth of the small inlet along the northern shore
of Matagorda Bay east of Carancahua Bay. Local gains in marsh vegetation occurred as a result of
colonization of eroded spoil mounds and drainage of Burgentine Lake at the head of St. Charles Bay.
In 1979, the wetlands area had increased along the Pleistocene barrier strandplain, particularly
on Blackjack Peninsula, from the area shown in 1956-57. This was attributed to wetter climatic
conditions in 1979. The photographs in 1979 demonstrated obvious differences in the amount of
standing water and moisture levels in depressions on the Pleistocene barrier strandplain. The higher
92
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quality infrared photographs of 1979 also allowed a more detailed delineation of habitats. In
addition, two new map units were used in 1979, undifferentiated wetland/upland areas and
transitional areas, which allowed depiction of complex upland and wetland mosaics. The numerous
small marshes, water bodies, and transitional areas on the coastal plain, such as those west of the
San Antonio River, were within regions mapped as frequently flooded fluvial areas in the earlier
study. The increase in wetlands in these areas in 1979 was a result of mapping criteria and map unit
designations. Some of the additional wetlands noted in 1979 were also attributed to higher levels of
precipitation.
Brownsville
Near the Brownsville ship channel, obvious differences in the distribution of salt and brackish
water marshes were identified from comparison of 1960 photographs with those of 1979. In 1979,
marshes occurred in areas previously mapped as saline grasslands; this difference may have been due
to higher precipitation of the 1970's. Mangroves, salt marshes, and brackish water marshes along San
Martin Lake appeared to have spread into previously barren wind-tidal flats. Changes in municipal
and agricultural discharges into San Martin Lake may have contributed to the spread of marshes.
Little change was observed for inland fluvial-deltaic system wetlands. The resacas (former, often
marshy, stream channels) generally were mapped as fresh and saline water bodies and frequently
flooded fluvial areas.
Visual comparison of photographs from 1960 with those of 1979 and 1983 (White et al., 1986)
show that the following changes have occurred in the Brownsville-Harlingen area: 1) local increases
in marshes, including mangrove marshes along the margins of wind-tidal flats; 2) erosion of spoil
and encroachment of marsh vegetation along spoil-island margins and flats; 3) local expansion of
marine grassflats near the mainland shore of Laguna Madre; and 4) displacement of marine grassflats
along the lagoon ward margin of Padre Island by dredged channels and local storm-washover deposits.
Neches River
The most extensive changes in the Beaumont-Port Arthur area have occurred along the river
valleys. The Neches River is a dramatic example. Between Port Neches and Bridge City, extensive
marshes existing in 1956 were completely replaced by open water by 1978. Dredged canals, sediment
reduction, subsidence, and sea-level rise contributed to this habitat loss.
The dredging of the Neches River for deep-draft navigation and disposal of spoil on the banks
created an upland levee between the river and adjacent marsh areas. This levee deprived the
93
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adjacent marsh of sediment which was historically supplied by flooding events. In addition, natural
subsidence in the chenier plain of about 0.7 inches (1.7 cm) per year, coupled with the rise in sea
level, contributed to the drowning of these marshes.
West of State Highway 87, an increase in vegetated wetlands from 50 acres (20 ha) to 630 acres
(255 ha) was observed (Weirsema et al., 1973) between 1957 and 1971. This gain was attributed to
the intrusion of water from a dredged discharge canal created by the Sabine Power Station.
Human-induced subsidence was a major cause of marsh losses. Solution mining for sulfur in
salt dome cap rock, extraction of oil and gas, and extraction of ground water have resulted in
subsidence. White et al. (1987) presented evidence of subsidence occurring in the Nechesi River
Valley along a fault line. The fault is more easily identified in the 1978 photographs compared to
1956 photographs. Changes from marsh to open water from all causes in the Neches River basin are
summarized in Table 26.
Table 26. Net Changes in Area from Marsh to Open Water in the Neches River Basin, Texas (From
White et al., 1987)
Mao Unit
Water
Marsh
1956
Acres
2,560
15,740
1978
Acres
11,070
6,330
Net Change*
Acres
+8,510
-9,410
* Does not include loss of an additional 900 acres (365 hectares) of marsh due to spoil disposal.
Galveston Bay
Galveston Bay is the seventh largest estuary in the United States and the largest in Texas (Sea
Grant College Program, 1989a), It is an irregularly shaped, shallow body of water, roughly 30 mi
(48 km) long and 17 mi (27 km) wide at its widest point. Water depth is generally between 7 and
9 ft (2 to 3 m). It is nearly separated into two parts by Red Fish Bar, a chain of small islets and
sho.als. The part of the bay north of Red Fish Bar is called the Upper Bay, and the area to the south
is known as Lower Bay. The northeastern section of Upper Bay is known as Trinity Bay. This bay
system is unique to Texas since it occurs in an area with high rainfall and humidity, as opposed to
the more arid climate found further south along the Texas coast. High rainfall aids in maintaining
94
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low overall salinity of Galveston Bay. Also, relatively low temperatures are especially important
during the summer fish and shellfish reproduction periods.
Galveston Bay provides the nursery and spawning grounds for approximately 30% of the total
fisheries harvest from the Texas coast. While turbid, water quality in the bay is typically described
as good, although it often has unacceptable levels of coliform bacteria. Large portions of the bay
are often closed to shellfishing, primarily as a result of bacteria introduced by runoff from
surrounding lands. The turbidity is a result of the bay's shallow nature and local wind patterns.
The greatest problem regarding maintenance of Galveston Bay habitats has been human
manipulation and utilization of estuarine resources, including coastal and freshwater wetlands and
other coastal habitats. The total area of marsh vegetation in Galveston .Bay declined by
approximately 16 % from 1956 to 1979 (Table 27). Remaining salt marshes are vegetated
predominantly by 5". alterniflora and cover approximately 34,580 ac (14,000 ha). Brackish marshes
occur in areas of moderate salinity and cover 56,810 ac (23,000 ha). There are 9,880 ac (4,000 ha)
of fresh marsh confined to the northern portions of Galveston Bay. A comparison of the 1956 and
1979 wetland surveys by the U.S. National Wetland Inventory indicates losses of 15,561 ac (6,300 ha)
of fresh marsh and 10,374 (4,200 ha) of salt and brackish marshes during that period (NOAA, 1989c).
The aerial extent of submerged vegetation in Galveston Bay declined from 5,187 ac (2,100 ha) in
1960 to less than 247 ac (100 ha) in 1979 (NOAA, 1989c).
Table 27. Galveston Bay Wetland Habitat Changes, 1956-1979 (Adapted from NOAA, 1989C)1
Wetland Habitat Type
Estuarine Marsh
Estuarine Open Water
Beach
1956
Acres
154,588
363,213
3,015
1979
Acres
130,139
388,397
1,413
. . Change
Acres %
-24,449
+25,184
-1,602
age
-15.8
+6.9
-53.1
1 Changes in acres calculated from U.S. FWS National Wetland Inventory Maps
Galveston Bay supports a large commercial and recreational fishery. Landings for 1986 are given
in Table 28. The percent of total Texas inshore fish landings, which were harvested by recreational
fishermen, has remained relatively constant between 1983-1986 (Table 29). However, there appears
to be an overall decline in landings from all Texas bays.
95
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Table 28. Landings of Commercial and Recreational Fisheries in Galveston Bay in 1986. (NOAA
1989c).
• Not available.
Commercial (x 1000)
Kg. £
Recreational (x 1000)
Atlantic Croaker
Flounder
Blue Crab
Shrimp (3 species)
Oyster
18
73
1,375
6,820
1,610
9
157
1,043
18,135
6,950
37
39
-1
-
™
11
52
-
-
"*
Table 29. Annual Weight of Finfish Landed by Recreational Boat Fishermen from Galveston Bay
during 1984, 1985, and 1986 (Osbourn and Fergason, 1987)
Year
Galveston Bav
All Texas Bavs
% of total from
Galveston Bav
1983-1984
1984-1985
1985-1986
1,391,100
940,700
1,121,400
4,316,900
2,922,000
3,205,400
32
32
35
A description of the biological components of Galveston Bay is given by NOAA (1989c).
Oyster reef assemblages occur primarily in central Galveston Bay and divide Galveston Bay into
upper and lower sections. Public oyster reefs within the estuary are densest in the mid- bay region
and across the mouth of East Bay. Settlement of oyster spat generally occurs from April to
November. Oysters reach market size in 13 to 18 months. Since 1975, the areal distribution of
oyster beds has been fairly stable.
*
NOAA (1989c) found that the following six species of fish accounted for 91% of the total
number of fish collected during a 2-year synoptic trawl study: Micropogonias undulatus (Atlantic
croaker, 51%), Anchoa mitchilli (bay anchovy, 22%), Stellifer lanceolatus (star drum, 8%), Leiostomus
xanthurus (spot, 4%), Cynoscion arenarius (sand seatrout, 3%), and Arius felis (hardhead catfish, 3%).
These six species, plus Mugil cephalus (striped mullet), were responsible for 74% of the biomass
collected (NOAA, 1989c).
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Approximately 139 species of birds associated with wetlands and bay habitats have been reported
to use the Galveston Bay area. The Galveston Bay system is important breeding habitat for three
species of waterfowl: Dendrocygna bicolor (fulvous whistling duck), Anas fulvigula (mottled duck),
and Aix sponsa (wood duck). Another 29 species of waterfowl use the bay as an overwintering site
or migration flyway. Large populations of migrating and overwintering shore birds make use of the
Galveston Bay area, especially during winter and spring months. Of the 35 species of shorebirds
reported to use the area, several are known to nest in the bay complex, including: Charadrius
wilsonia (Wilson's plover), Charadrius vociferus (killdeer), Catoptrophorus semipalmatus (willet),
Haematopus palliatus (American oystercatcher), and Himantopus mexicanus (black-necked stilt).
About 22 species of colonial waterbirds have been reported nesting during the 21 years of surveys.
The three most common species during the 1986 season were: Lams atricilla (laughing gull), Sterna
maxima (royal tern), and Bubulcus ibis (cattle egret). From 1973 to 1987, numbers of pairs of
colonial nesting waterbirds varied from lows of approximately 39,000 in 1978 and 1985 to a high of
71,700 in 1982, with a mean of 52,136. Active colony numbers have increased from 20 in 1973 to
42 in 1987 (NOAA, 1989c).
Pulich and White (1990) estimated acreage of seagrass beds in Galveston Bay system from 1987
NASA aerial photographs. Those measurements were corroborated with field surveys in 1988-1989.
Historic black and white photomosaics from 1956 Edgar Tobin aerial surveys, 1965 black and white
photographs from the U.S. Coast and Geodetic Survey, and 1975 color-infrared photographs from
NASA were compared with recent photographs to assess changes in acreage. Both upper and lower
Galveston Bay were studied. Since 1979, total acreage of seagrasses in Galveston Bay has declined
approximately 90%. The extent of seagrass decline was especially noticeable in the western half of
the Bay (West Bay) where there were 1,131 ac (458 ha) in 1956, 288 ac (117 ha) in 1965, 91 ac (37
ha) in 1975, and 0 ac in 1987. Several physical and hydrographic processes contributed to these
changes, including geomorphic impacts from Hurricane Carla, subsidence in the upper Bay, and
effects from industrial and urban shoreline development in the lower Bay.
Shew et al. (1981) listed rare and endangered vertebrates of the Galveston Bay area. These
include: Canis rufus (red wolf), which is considered extinct in Texas and Louisiana (other than for
a few isolated sightings); Lutra canadensis texensis (river otter) which is threatened; Ursus
americanus (black bear) which is endangered; Trichechus manatus latirostris (West Indian manatee)
which is endangered; and Lynx rufus texensis (bobcat) which is under consideration for an
endangered status. Endangered bird species found in Texas coastal areas include Haliaetus
leucocephalus leucocephalus (southern bald eagle), Grus americana (whooping crane), Pandion
haliaetus carolinensis (osprey), Falco peregrinus tundrius (Artie peregrine falcon), Pelecanus
occidentalis carolinensis (brown pelican), Tympanuchus cupido attwateri (Attwater's greater prairie
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chicken), Picoides borealis (red-cockaded woodpecker), Chen rossii (Ross's goose), Campephilus
principalis (ivory-billed woodpecker), and Numenius borealis (Eskimo curlew).
Alligator mississippiensis (American alligator) is listed as an endangered species in Galveston
Bay; however, recent reports indicate that populations of this species are increasing. Malaclemys
terrapin littoralis (Texas diamondback terrapin) and Opheodrys vernalis blanchardi (smooth green
snake) are both listed as threatened on the list prepared by the Texas Organization for Endangered
Species.
Florida
The Florida coastal zone has experienced significant historic losses of natural habitats.
Approximately 75% of Florida's population lives in coastal counties and the desire to live on or near
the coast has resulted in the loss of fringing wetland habitats through filling activities, loss of
seagrass communities through pollution, dredging for boat channels and marinas, increased use of
coastal waters, and a deterioration of water quality from point and nonpoint discharges. Coastal
development has exacerbated beach erosion and has resulted in loss of sand dune habitat.
Although the sensitivity of coastal habitats is becoming better understood, the demands on
Florida's coastal resources continue to increase. The movement of people to the Sun Belt is well
documented (Culliton et al., 1990). It is estimated that approximately one thousand people move to
Florida daily to establish permanent residence (Shoemyen et al., 1989). This rapidly growing
population places increasing demands on shipping, agriculture, transportation, and other industries.
Growth of these industries in response to population demands has resulted in increasing
encroachment on natural habitats and resources. Approximately 31% of Florida's Gulf coast estuaries
are severely affected by pollution. That amount is slightly less than the overall national average of
estuarine pollution (Comp and Seaman, 1985). More and more developments are appearing on
Florida's Gulf coast because the east coast of Florida is largely developed. Thus, the demands on
Gulf coast estuaries will continue to increase with increasing development.
The marine coastline of Florida is 1,300 mi long (2,097 km), and the tidal shoreline is 8,500 mi
(13,709 km) long. Approximately 22% of the U.S. Gulf coast acreage of estuaries and tidal wetlands
occur on the west coast of Florida (3 million ac; 1.2 million ha) (Comp and Seaman, 1985). Florida's
Gulf coast estuaries tend to be well mixed with broad salinity gradients caused by fresh water inflow.
The Gulf coast has low relief, and many rivers, creeks, and springs discharge into estuarine habitats.
The continental shelf along the Big Bend portion of Florida's Gulf coast (Tarpon Springs to
Apalachicola) is wide and shallow which results in a low-energy shoreline in that portion of the
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coast. In general, the remainder of the coast is characterized by high energy beaches on barrier
islands separated from the mainland by estuarine lagoons.
Tampa Bay
Tampa Bay is the largest estuary in Florida, covering an area of approximately 254,410 ac
(1,030 km2). It receives drainage from nine rivers and streams in a watershed that covers
approximately 1,407,900 ac (5,700 km2). Tampa Bay is subdivided into seven subunits: Old Tampa
Bay, Hillsborough Bay, Middle Tampa Bay, Lower Tampa Bay, Boca Ciega Bay, Terra Ceia Bay, and
the Manatee River. The origins of Tampa Bay are not clearly known; however, it is believed that
it is a large, drowned floodplain of a subtropical river flowing from the Florida peninsula to the Gulf
of Mexico. Tampa Bay is located in a transition zone between temperate and tropical climates. The
Peninsula Arch to the east and the broad continental shelf to the west tend to protect the bay from
oceanic influences (Lewis and Estevez, 1988).
Lewis and Estevez (1988) reviewed the physical and chemical properties of bay waters and
concluded: 1) Tampa Bay is not grossly polluted; 2) some parts of the bay are cleaner than others
for natural as well as cultural reasons; 3) the levels of some pollutants have declined over the past
decade while others have increased; and, 4) the overall quality of bay zones is the same whether
judged by ecological or human-use criteria. The significant environmental problems in Tampa Bay
include low dissolved oxygen which often results in fish kills, reduction of light to lower levels of
the water column, which decreases primary production from phytoplankton and seagrasses, and
excessive nutrients in runoff and discharges from sewage treatment plants, other point sources, and
nonpoint sources which can cause blooms of phytoplankton and algae.
According to Lewis et al. (1985a), four species of seagrass are found in Tampa Bay: T.
testudinwn, S. fHi forme, H. wrightii, and H. engelmannii. Ruppia maritima is also reported in Tampa
Bay. These species make up seagrass meadows covering 20,000 ac (8,097 ha) of the bay bottoms
(Lewis et al., 1985; Lewis et al., 1991). Estimations from comparing historical aerial photographs
and maps suggest seagrasses at one time covered 76,527 ac (30,980 ha) of Tampa Bay. It is probable
that this loss of 73% (56,527 ac; 22,885 ha) of seagrasses has adversely affected the fisheries resources
of Tampa Bay. There is recent evidence that seagrass systems are recovering in Tampa Bay.
However, it is still uncertain whether the observed expansion of seagrass meadows is short-term, due
to drought condition, or long-term, due to improved water quality.
Lewis et al. (1985) found that the seagrass meadows are generally monospecific stands.
Approximately 40% of the remaining beds are vegetated by T. testudinum, 35% by H. wrightii, 15%
by S. filiforme, and 10% by R. maritima. Five types of seagrass meadows occur in Tampa Bay: 1)
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mid-bay shoal perennial; 2) healthy fringe perennial; 3) stressed fringe perennial; 4) ephemeral; and
5) colonizing perennial. It is hypothesized that types 3 and 4 are stages that lead to the eventual
disappearance of a seagrass meadow due to human activities.
Approximately 17,791 ac (7,200 ha) of emergent wetlands border Tampa Bay and consist of five
major plant species: J. roemerianus, S. alterniflora, L. racemosa, R. mangle, and A. germinans (Lewis
and Whitman, 1985). Mangrove forests suffered significant losses during three recent freezes:
January 1977, December 1983, and December 1989. Because of these freezes, the total area of tidal
marsh may have increased as more temperature-tolerant marsh plants colonized the dead mangrove
forests.
An estimation of the annual production of primary producers in the Tampa Bay area is given
in Table 30. Phytoplankton are responsible for the majority of primary production in this system.
Table 30. Annual Production of Primary Producers in Tampa Bay (from Lewis and Estevez, 1988)1
Primary Producer
Seagrasses & Epiphytes
Macroalgae
Benthic Microalgae
Mangrove Forests
Tidal Marshes
Phytoplankton
Phytoplankton5
Production
(gC/m2/vr)
730
70
150
1.1322
300
340
50
Area
(Acres)
14,208
24,710
49,568
15,938s
2,595
213,494
23,722
Total Production
reC/vr X 106)
42.0
7.0
30.0
73.0
3.2
293.8
48.0
Percentage
of Total
8.5
1.4
6.0
14.7
0.6
59.1
9.7
1 Acreage originally recorded in km2
2 Estevez and Mosura, 1985.
8 Assumes 14% of the bay's emergent wetlands are tidal marsh.
4 For areas deeper than 2m.
5 For areas shallower than 2m.
Unvegetated bottoms are a major component of the Tampa Bay ecosystem. Approximately 74%
(228,067 ac; 92,335 ha) of the subtidal bottom of Tampa Bay is unvegetated (Haddad, 1989). This
habitat includes artificial reefs, natural rock reefs, sand, and mud bottoms.
Changes in the community structure of Tampa Bay between 1950 and 1982 were estimated
during a cooperative study between the U.S. FWS and the Florida Department of Natural Resources
(Table 31). A significant decline in vegetated habitats, particularly seagrasses, was documented.
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Increased urban and agricultural runoff probably led to this decline due to increased turbidity and
nutrient loading.
Table 31. Summary of Major Habitat Trends In Acres for the Tampa Bay Region (from Haddad,
1989)
Habitat
Mangrove
Salt marsh
Seagrasses
Mudflats
Agriculture
Urban
1950
21,314
5,096
63,728
16,825
62,607
80,843
1982
19,839
3,537
32,030
23,190
111,626
236,097
Percentage of Change
-7
-30
-50
+37
+78
+192
Lewis (1977) and Lewis et al. (1985a) estimated that 44% of the salt marsh and 81% of the
seagrass meadows in Tampa Bay have been lost since the 1800's. The recent calculations of Haddad
(1989; Table 31) are not readily comparable with those of Lewis et al. because of differences in time,
methods of calculation, vegetation classification, and other factors. However, the results of both
studies confirm that significant losses in habitat have occurred. Haddad suggests that the small
percentage of change in mangroves listed in Table 31 is an artifact of the classification system used
in his study which is currently being corrected.
Significant losses of habitats have occurred in the Tampa Bay area. Dredge and fill activities
have caused direct losses of mangroves, marshes, and seagrasses by uprooting or covering the habitat
and indirect losses in seagrasses by raising the turbidity and lowering the quality of the water.
Seagrass losses have occurred throughout the Tampa Bay, particularly in the upper portion where
shallow seagrass meadows were dredged and filled for residential and commercial development.
Although historic loss of seagrasses was partially due to direct mechanical destruction from dredging
and filling, most loss was due to deterioration of water quality. The causes of this deterioration
include: 1) loss of adjacent rangeland, forests, swamps, and marshes that normally filter runoff
water; 2) increases in agricultural area that may increase sedimentation and suspended particulates;
3) increase in urbanization and industrialization that introduces waste waters and storm water into the
bay; and 4) dredging that causes long-term release of fine sediments into the bay (Haddad, 1989).
Fisheries have historically been an important part of the Tampa Bay ecosystem (Lewis and
Estevez, 1988). The production of mullet, blue crabs, hard shell clams, tarpon, snook, and spotted
seatrout are an important contribution to the local economy. Declines in habitat such as seagrass
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meadows, mangrove forests, and tidal marshes that furnish food and protection for many of these
species have apparently resulted in declines in fishery production. Total emergent wetlands (tidal
marshes and mangrove forests) have declined from 24,831 ac (10,053 ha) (ca. 1876) to 13,906 ac
(5,630 ha) (ca 1976), a 44% loss (Lewis, 1977). This loss was mainly due to dredge and fill
operations. Commercial fishery landings of species that depend on wetland habitats have decreased
concurrently with wetland losses in Tampa Bay. Fishery landings in Tampa Bay are low compared
to those in Charlotte Harbor, a nearby estuary of similar size but with much less habitat loss.
U.S. FWS and Tampa Port Authority recently completed a three-year cooperative project to
establish a data base available for management of wildlife habitat and port development in Tampa
Bay (Fehring, 1986). This project identified management and mitigation options, developed an
information base, and defined long-range management scenarios for port development and
mitigation. The study produced a list of acreages of wetland habitats for 21 U.S. Geological Survey
quadrangles in the Tampa Bay region. Estuarine vascular aquatics (seagrasses) suffered the greatest
losses, but salt marshes and mangroves also declined significantly (Table 32).
Table 32. Area (Acres) of Various Wetland Habitats for 21 Quadrangles in the Tampa Bay Region
for Three Time Periods (Modified from Fehring, 1986)
Habitat Type
Salt marsh
Estuarine vascular
Mangroves
1950
Acres
4,672
aquatics 40,324
18,645
Estuarine open water 206,740
Beaches, bars and
flats 18,771
1972
Acres
3,610
25,576
18,656
214,043
16,369
1982
Acres
3,238
22,526
18,030
212,623
19,825
1948-1982
Change
-1,434
-17,798
-615
+5,883
+1,654
%
Change
-30.7
-44.1
-3.3
+2.8
+8.8
The impact of approximately 100 years of dredging activities on the Tampa Bay estuary is
discussed by Lewis (1977). Channel deepening, maintenance dredging, shell dredging, and dredging
for fill material for construction are the four major types of dredging activities which have impacted
the Bay. Over 12,355 ac (5,000 ha) of Tampa Bay have been converted to uplands for residential,
commercial, and dredged material disposal use. According to Lewis (1977), disposal of dredged
material resulted in most of the loss of 44 % of the original marine wetlands which bordered Tampa
Bay. Little research has been performed on the effects of channel dredging and construction of open
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water spoil disposal sites on the hydrological patterns in Tampa Bay. However, it is known that
recovery of disturbed seagrass meadows is extremely slow after dredging (Godcharles, 1971).
Open water spoil disposal can result in changes in hydrological patterns in enclosed water
bodies. The Federal Water Pollution Control Administration recognized this problem and
recommended in 1969 that a master plan be developed by pertinent Federal, state, and local operating
and regulating agencies for dredging and filling in Hillsborough Bay (a part of Tampa Bay).
However, there is no master plan for the entire Bay, and historic dredging arid filling in Hillsborough
Bay has occurred with little regard for the master plan. Studies undertaken by the U.S. Geological
Survey, funded by the Tampa Port Authority and the Corps of Engineers, evaluated a proposed
Harbor Deepening Project in 1970. Results of that modeling effort concluded that improved flushing
in Hillsborough Bay is probably not possible due to size and orientation of existing channels and spoil
disposal sites (Lewis, 1977).
In 1967, filled areas in Tampa Bay totaled 10,537 ac (4,266 ha). Filling created uplands where
there were once mangroves, tidal marshes, or seagrass communities (McNulty, Lindall, and Sykes,
1972). The filling of 3,458 ac (1,400 ha) of bay bottom in Boca Ciega Bay since 1950 has reduced
the total area of that bay by 20%. That study estimated a loss of 28,425 t (25,841 mt) of infauna and
an annual loss of $1.4 million (1972 dollars) in fisheries production due to filling.
Lewis (1977) suggested that a general increase in public environmental awareness and the
declining availability of marine resources make it unlikely that massive dredge and fill projects, such
as those which have historically despoiled Tampa Bay, will occur in the future. Unfortunately, loss
of wetland habitat and pollution in Tampa Bay have already decreased commercial harvest of fish
and shellfish and adversely affected populations of other organisms dependent upon the Bay for
survival.
Habitat losses, similar to those which have occurred in Tampa Bay, have been observed in
Sarasota Bay (Table 33). These losses are a symptom of the rapid development of coastal Florida.
Charlotte Harbor
Haddad (1986) compared the loss of habitat in Charlotte Harbor with .that observed in Tampa
Bay. Charlotte Harbor is on the southwest coast of Florida and is one of the State's least modified
and least polluted estuaries. Its dimensions are approximately 35 mi (56 km) from north to south,
encompassing 227,332 ac (92,000 ha) of water area, with an average depth of 10.5 ft (3.2 m). The
average tidal range is 5.9 ft (1.8 m). The harbor is used extensively by sport and commercial
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Table 33. Changes in Habitat Acreages in Sarasota Bay (Gail McGarry, Florida Department of
Natural Resources, Personal Communication)
Category
1948
1972
1987
% Change (1948-1987)
Seagrass (sparse-
med. density)
Seagrass (dense)
Seagrass (patchy)
TOTAL SEAGRASS
Mangrove swamp
Tidal marshes
Oyster beds
Bay waters
930
4,814
441
6,185
1,546
271
109
12,220
860
4,286
71
521
1,032
44
115
1,707
845
2,650
544
4,039
843
48
129
13,802
-9
-45
+23
-35
i.
-45
-83
+16
+12
fishermen and provides over 50% of Florida's west coast commercial landings of red drum and
spotted seatrout. The Myakka, Peace, and Caloosahatchee Rivers, with a combined drainage basin
of approximately 2,668,680 ac (1.08 million ha), drain into Charlotte Harbor. These watersheds
include pasture, farmland, and citrus groves. Industrial effluents from phosphate mining areas, light
industry, and domestic wastes are discharged into these rivers.
i
Table 34 summarizes the cumulative effects of various perturbations on marine wetland habitats
in Charlotte Harbor. Except for an increase in mangrove habitat, there have been declines in all
natural habitat types. This trend is similar to the trends observed in Tampa Bay and Sarasota Bay.
Losses of salt marshes and mudflat habitats are particularly significant in Charlotte Harbor.
Table 34. Wetland Acreage Change in Charlotte Harbor from 1945-1982 (data from Harris et al.,
1983, as presented by Haddad, 1986)
Acreage
Wetland Habitat 1945 1982
Seagrasses 82,959 58,495
Mangroves 51,524 56,631
Salt marsh 7,251 3,547
Mudflats 11,206 2,723
Oyster reefs 806 488
% Change
-29
+10
-51
-76
-39
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The acreage of mangrove habitat increased by 10% during the study period. A portion of this
increase may be due to differences in photographic resolution and interpretation, but the majority
of this increase is probably due to management practices that began in the late 1960's. An important
part of this plan was the establishment of a wetland "buffer" zone around the harbor, and existing
mangroves were protected as part of the estuarine system. Thus, mangroves were allowed to grow
into mudflats and oyster reefs, and very few were lost due to direct removal for development. The
concept of establishing a preserved wetland fringe around the harbor was successful in maintaining
the mangrove community, but the concurrent loss of seagrass beds and salt marshes substantiates the
need for managing the entire ecosystem, including the drainage basin. Salt marshes decreased by
51%, probably due to dredge and fill activities, as well as from secondary impacts of extensive
upland development. This development included construction of canals that may have permitted
intrusion of saltwater, which resulted in increased growth of mangroves. Seagrasses declined almost
30%. Most of this decline was in an area where a coastal highway was constructed which required
extensive dredging and channelization of a river. Some of the decline was probably due to the
decrease in light penetration from turbidity produced by dredging and channelization. Loss of
seagrass habitat adversely affected fisheries resources, particularly bay scallops which historically
inhabited dense grass beds (Haddad, 1986).
During the period of this study (1945-1982), the urban area around Charlotte Harbor increased
by approximately 92,395 ac (37,400 ha). Approximately 50% of this increase was due to development
of large tracts of agriculture and rangeland.
In summary, although Charlotte Harbor is relatively unimpacted compared to other estuaries
of Florida, the area is undergoing rapid growth, and water and sediment quality are showing signs
of deterioration. Haddad (1986) listed the major lessons learned from monitoring the deterioration
of Charlotte Harbor:
1. Although dredging and filling can have a catastrophic direct effect, the long-term effects
from the release of fine sediment into the water column may be even more damaging.
2. The densities of phytoplankton may be significantly increased through the introduction of
nutrients in runoff and effluent discharges.
3. Alterations in natural drainage patterns can have an effect on ambient water quality and
the life cycle of biota in the estuary.
4. Altered circulation patterns resulting from the construction of roads, dikes, channels, etc.,
and the channelization of a contributing river also interact with water quality and cycles
of biota.
5. Alterations of drainage affect the habitat and survival of scallops within an estuary.
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Louisiana
Gosselink (1984) reviewed the ecological information on the extensive marshes of the Mississippi
River Deltaic Plain (MRDP). Over the last 6,000 years, the Mississippi River has built a delta onto
the continental shelf of the Gulf of Mexico which measures approximately 5,903,300 ac (23,900 km2).
The MRDP is the largest continuous wetland system in the United States with approximately
1,790,750 ac (725,000 ha) of wetlands, not including forested wetlands. These marshes represent
about 22% of the total coastal wetland area of the 48 continental United States. The Mississippi River
system is the largest in the United States, draining an area of over 826,440,776 ac (3,346,000 km2).
A community profile of the area was developed using the 1978 FWS habitat mapping data. At
that time, the MRDP consisted of 9,000,000 ac (3.6 x 106ha) in the following categories: 58% open
water, 5.6% urban and agricultural, 32% wetlands and 2.1% dredged canals and spoil banks.
Wetlands were categorized into salt marsh (15%), brackish marsh (47%), intermediate marsh (23%),
and seagrasses (1%).
The MRDP is composed of nine drainage basins, which are the result of shifts in the major
tributaries over time. The youngest basin is the Atchafalaya, which is actively prograding out
through the shallow Atchafalaya Bay. It receives approximately one-third of the flow of the
combined Mississippi and Red River systems; this interior basin is predominantly fresh all year long.
The next youngest basin in the active Mississippi River delta is the Balize Delta. It receives
almost two-thirds of the flow of the Mississippi River, emptying into deep water at the edge qf the
continental shelf. The majority of these areas are fresh water with some brackish marsh. In
succession, Barataria, Terrebonne, Vermilion-Cote Blanche, and the Pontchartrain-Lake. Borgne
basins are of increasing age. They all have extensive marshes with well-developed salt and brackish
zones.
Wetland losses in the Mississippi River Deltaic Plain have been studied by Turner (1990),
,
Gosselink (1984), Bahr et al., (1983), and Leibowitz and Hill (in preparation). Turner (1990) found
that Louisiana coastal zone habitats are converted to open waters and at an annual rate of 0.86%
Gosselink (1984) estimated the annual loss of delta marshes to be 1.5% Leibowitz and Hill (in
preparation) reported that annual land loss rates at Cameron, Terrebonn, and Lafourch study sites
were 0.77, 0.66, and 0.95%, respectively. Regardless of the discrepancies in rate, all authors agree
that the rate of marsh loss to open water has accelerated over the past 50 years and that human
activities have interfered with the cycle of delta formation and accretion. Duhbar et al. (1990) report
that the current land loss rate is approximately 31 square miles (80 km2) per year.
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Causes and mechanisms of changes in wetland acreage include: direct loss to dredging,
construction, filling, erosion and machinery (marsh buggies); subsidence from loss of accretion, oil
and gas withdrawal, and soil drying; changes in quantity and quality of vegetation from changes in
organic deposition and sediment trapping; and death of plants from pollutants. Turner (1990)
suggested that the majority of wetland losses are due to drowning of plants under increased water
depth.
The detrimental impacts of human activities on the MRDP have been cumulative. Evidence
of prehistoric Indian use of the area is indicated by the numerous elevated shell mounds that
currently harbor groves of trees. Permanent settlements in the delta appeared in the early 1700's.
The bases of the area's economy were agriculture, fishing, and trapping. Since the 1940's, man's
impact on the delta has greatly accelerated. For example, thousands of miles of canals have been
dredged throughout the delta to facilitate activities of the oil and gas industry.
Gosselink (1984) also listed reasons for the loss of marshes in the MRDP. The development of
the river delta is a dynamic process that involves both accretion and erosion of sediments.
Subsidence in marsh areas is usually not a significant concern because of continued deposition of new
sediments which result in a net landbuilding process. However, up-river dams selectively remove
the qoarser sediments resulting in less material available for the natural delta-building processes.
Gosselink argues that extensive navigation canals have allowed intrusion of saltwater deep into the
estuary, which often results in the death of salt-intolerant vegetation. Plant death results in erosion
of land before more tolerant plant species can be established. Dredged canals also act as a direct
route out of the marsh for finer sediments which historically were deposited and accreted in wetland
areas.
Many of the remaining marshes in the delta have been managed in an attempt to increase
fisheries production. Impoundments yield excellent crops of fish and shellfish. Juveniles are trapped
within an impounded marsh and grow within the sheltered waters (Davidson and Chabreck, 1983).
However, impoundments disrupt normal hydrological cycles and sediment deposition patterns and
can lead to conversion of emergent marsh to open water.
Leibowitz and Hill (in preparation) observed that marsh loss is not a spatially uniform process
that takes place at the shoreline and advances landward, Rather, losses are greatest within the
marshes proper, and areas of greatest loss are highly clustered. They concluded that the pattern and
causes of coastal marsh losses in Louisiana are both complex and heterogeneous.
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Bahr et al. (1983) described 20 habitat types in the MRDP and grouped them into three broad
categories: (1) highland or terrestrial habitats, (2) intertidal or periodically flooded habitats, and (3)
aquatic or continuously flooded habitats. Bahr et al. (1983) estimated the area of estuarine open-
water habitats in 1978 in the MRDP to be 4.7 x 106ac (1.9 X 106ha) or 56% of the region. The area
of estuarine open water has been increasing because sediments from the Mississippi River, through
the Atchafalaya River, are deposited into the Atchafalaya basin rather than on fringes of the marsh.
Thus, there is a net reduction of MRDP land. Brackish marsh is the second largest habitat in areal
extent in the MRDP, covering 997,880 ac (404,000 ha) or 11.7% of the entire area. Salt marsh makes
up a significant portion of the MRDP: 449,540 ac (182,000 ha), or more than 5% of the total area
in 1978. There are 17 other distinct habitat types in the MRDP that are discussed by Bahr et al. that
each cover less than 5% of the area.
Morgan and Morgan (1977) determined the rate of shoreline changes throughout coastal
Louisiana through a comparison of 1969 aerial photographs with those of two earlier periods (1954
and 1932). The comparison revealed that areas of land loss have far exceeded areas of new land
formation. They concluded that the dominant cause of land loss was the erosion by waves of soft,
unconsolidated sediments that compose the low-lying coastal zone, especially in the MRDP.
Linear shoreline retreat rates and areal land changes were evaluated to establish trends which
document continuing and accelerating rates of land loss along most of coastal Louisiana. For
example, Louisiana's shoreline has been retreating at an average linear rate of approximately 10 ft/yr
(3 m) for the past 37 years. However, that average reflects an increase from about 6.5 ft/yr (2 m)
in the interval between 1932 and 1954 to 17 ft/yr (5 m) during the period from 1954 to 1969.
Similarly, areal change measurements for 75% of the coast, where they could be made, show a loss
of about 374 ac (151 ha) per year (0.58 mi2/yr; 1.5 km2) during the 37-year period 1932-1969.
However, there has been an increase in rate of land loss from 348 ac (141 ha) per year during the
period 1932-1954 to 413 ac (167 ha) per year from 1954 to 1969.
Atchafalava Basin , •••,.., ; • •
The U.S. Army COE is evaluating the potential ecological impact of flood waters in the
_Atchafalaya Basin Floodway system that extends from the proximity of Old River, at the juncture
of the Red and Mississippi Rivers, to the Gulf of Mexico (Mathies, U.S. Army COE, personal
communication). The main purpose of the Atchafalaya Basin project is to safely convey one-half
of flood waters to the Gulf of Mexico. Operation of the Federal flood control project has induced
flooding in areas to the east and northeast of the end of the existing levee system due to backwater
flooding. Increased and prolonged flooding is destroying extensive areas of wetland habitats. Two
108
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alternative plans are being evaluated to provide protection against this increased flooding.
Potentially, the most environmentally damaging alternative is construction of a 5.5 mi (8.9 km)
extension of the existing Avoca Island levee. The levee extension would adversely impact the
Terrebone marsh complex, a 600,000 ac (242,915 ha) wetland area located to the east of the existing
levee, by restricting sediment-laden river flows from entering the area. By limiting river flows, the
vital nutrients and sediments carried by those flows and essential to nourish the marsh complex
would be limited.
To assess the ecological consequences of the levee extension alternative, the U.S. Army COE
recently provided funds to Louisiana State University, through the U.S. FWS, to develop a spatial
simulation model for the study area to predict ecological changes. The resulting Coastal Ecological
Landscape Spatial Simulation model (Costanza, et al., 1990) is comprised of nearly 2,500
interconnecting 1-square kilometer cells. Each cell is characterized by its own set of variables and
is connected to its four adjacent cells by the exchange of water and suspended materials. During the
model verification process, predicted conditions in 1978 and 1983 were evaluated against actual
conditions at those-time periods. Degree of fit was calculated relative to each of the simulations.
Numerous management scenarios, both with and without the levee extension, were evaluated and
future conditions predicted. The resulting 50-year predictions indicate that the levee extension
would induce the conversion of approximately 1,200 ac (486 ha) of existing marsh to open water
habitat. Several mitigation options have been evaluated to offset environmental impacts and provide
environmental compensation. However, selection of the flood control alternative has not been made
at this time. Information on historic acreage of various habitats in Atchafalaya Basin is shown in
Table 35.
Table 35. Acres (x 100) of Specific Habitats in the Atchafalaya Basin (After Costanzo, et ah,
1990)1.
Year
Swamp
Brackish Marsh Saline Marsh Open Water
1956
1978
1983
321.23
279.22
286.64
1561.67
1368.93
857.44
242.16
370.65
383.01
1833.48
2169.54
2466.06
1 Calculations from FWS Natural Wetland Inventory Maps and Photographs.
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Barataria Basin
The Barataria Basin is roughly triangular in shape, and is approximately 68 mi (110 km) long
and 31 mi (50 km) wide where it meets the Gulf of Mexico. The basin has been closed to river flow
since the leveeing of the Mississippi River in the 1930's and 1940's and the closing of Bayou
Lafourche, the Mississippi River connection, in 1902. Precipitation is the main source of fresh water
for the basin (Conner and Day, 1987).
Information on wetland losses in Barataria Bay is quantified in a computerized Geographical
Information System (GIS) (Johnston et al., 1986). They conclude that maintenance of marsh areas
continues to depend upon availability of nutrients and sediments from riverine inputs and that human
activities have greatly modified the input of both to Barataria Bay. Construction of flood control
levees along the Mississippi River and Bayou Lafourche has severely reduced fresh water inflow and
riverborne 'sediment into Barataria Bay. The GIS aided in identification of three problem areas:
Cut-off Golden Meadow Area, Lafitte oil field, and Adams Bay. Based on National Wetland
Inventory wetland maps digitized from 1956 and 1978 photographs, the loss rate of marsh and other
wetland habitat was different for each of the problem areas. However, for the entire Bay, from 1956
to 1978, wetland area decreased an average 12% and open water increased by 11% Marsh acreage
alone decreased from 548,356 ac (222,000 ha) in 1956 to 410,586 ac (166,229 ha) in 1978, a decrease
of 25%.
In another study, computer analysis was used to compare land and water areas of Barataria Bay
by comparing aerial photographs taken in 1945, 1956, 1969, and 1980. This study concluded that
the rate of marsh loss has increased from 0.36% per year in the 1945-56 period, to 1.03% per year
in 1956-69, and to 1.96% per year in 1969-80 (Sasser et al., 1986).
Patterns of marsh loss do not occur uniformly. Marsh loss rates have been highest where fresh
water marshes have been subjected to saltwater intrusion. The increase in wetland loss rates
corresponds to accelerated rates of subsidence and canal dredging and a cumulative increase in area
of canals and spoil deposits. The rate of change of marsh acreage from 1945 to 1980 is summarized
in Tables 36 and 37.
Conner and Day (1987) described the ecology and loss of wetlands in the Barataria Basin. This
area is noted for its network of interconnecting water bodies that allow transport of water and
migrating organisms throughout the basin. High ground within the wetlands is occupied by natural
and artificial levees that are surrounded by extensive swamp forests and fresh, brackish, and salt
marshes. These productive wetlands provide valuable nursery habitat for fish, shellfish, wintering
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Table 36. Net Areal Change (Acres) and Average Annual Rates of Change of Marsh to Nonmarsh in
Barataria Basin, Louisiana (from Sasser et al., 1986).
Type of Change
Marsh to nonmarsh (total change)
1945-1956a
1956-1969b
1969-1980°
1945-1980a
Marsh to canal/spoil
1945-1956"
1956-1969b
1969-1980°
1945-1980a
Marsh to developed"1
1945-1956a
1956-1969b
1969-1980°
1945-1980a
Area
(Acres)
6,175
20,299
28,315
54,083
2,335
8,784
1,520
9,600
378
4,599
7,976
12,953
Rate
(Acres/yr)
563
1,562
2,575
-
213
675
138
-
35
353
724
-
Change
(% marsh)
3.92
13.39
21.57
34.29
1.48
5.80
-1.16
6.09
0.24
3.03
6.08
8.21
Change Rate
(%/yr)
0.36
1.03
1.96
-
0.13
0.45
-0.11
-
0.02
0.23
0.55
—
Marsh to water (undetermined causes)
1945-19563
1956-1969b
1969-1980°
1945-1980°
area of change
0 ~ area of marsh 1945 (157,719
area of change
~ area of marsh 1956 (151,537
area of change
C Q/
3,462
6,281
21,537
31,530
acres)
acres)
314
484
1,957
—
2.20
4.14
16.41
19.99
0.20
0.32
1.49
~
*
~ area of marsh 1969 (131,255 acres)
d Developed includes agricultural, industrial, and residential areas
111
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112
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waterfowl, and fur-bearers. The basin is a dynamic system and is undergoing changes in the amount
of open water and wetland habitats due to subsidence, erosion, and human activities. The latter have
altered the natural hydrologic patterns in the basin, and this may cause long-term modifications of
wetland habitat.
Conner and Day (1987) divided the Barataria Basin into five environmental zones: levee and
developed lands, swamp forest, fresh marsh, brackish marsh, and salt marsh. The brackish marsh
is found between the lower swamp and upper marine environments and covers 338,390 ac (137,000
ha) (22% of the basin). This is the upper limit of the effects of tides and storm surges. Salinity
ranges from 2 to 10 ppt. It is the inland flow of saltwater that determines the kinds of vegetation
that grow, aids in nutrient recycling, and allows the inland migration of larval estuarine species.
Conner and Day (1987) found that S. patens is the dominant plant in the brackish marsh zone.
Chabreck (1972) observed the predominant composition of brackish marsh plants in the Basin was
S. patens (44%), Distichlis spicata (16%), Bacopa monnieri (12%), Pluchea camphorata (8.4%), and
S. alterniflora (4.5%). '
Barataria Bay has approximately 145,000 ac (58,704 ha) of salt marsh habitat. Salinity ranges
from 6 to 22 ppt. The major plant species is S. alterni flora, which covers 63% of the salt marsh area
(Conner and Day, 1987). Chabreck (1972) observed the salt marsh community to consist of the
following species: S. alterniflora (63%), /. roemerianus (15%), D. spicata (10.1%), S. patens (7.8%),
and Batis maritima (3.1%).
Several studies have demonstrated that alteration of normal hydrologic conditions can affect
structure and productivity of herbaceous and wooded wetlands. Mendelssohn et al. (1982) report that
hydrologic modifications of salt marshes cause increased waterlogging which may affect plant
productivity. For example, the Leeville oil field lies on the western boundary of the Barataria Basin
in a S. alterniflora marsh and consists of a dense network of canals dug for access to drilling sites.
Spoil disposal levees line many of the canals. Allen (1975) estimated that standing live Spartina
biomass was 50% lower in marshes surrounded by spoil banks than in a comparable control site.
Spoil banks along the canals also contain canal flow and restrict the natural lateral transport of water
necessary for the removal of wastes, the replenishment of marsh sediments, and the import of new
nutrients to the swamp forest. Obstruction of overbank flooding by levees can result in nutrient
starvation and blocking of swamp substrate accretion.
Northern Barataria Bay has experienced an annual increase in salinity of 0.108 ppt from 1961-
1974. Ultimately, the entire basin may become an open-water brackish bay or sound unless
Mississippi River flow is reintroduced to the area. Intrusion of saltwater as a result of diversion of
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fresh water has resulted in a decline of diverse swamp forests and an increase in monotypic marshes
and open water habitat (Van Sickle et al., 1976). The total number of plant species identified for
each wetland type is: swamp, 200+; fresh marsh, 154; brackish marsh, 23; and saline marsh, 25
(Conner et al., 1986). Loss of biodiversity has affected ecosystem functions of the area.
There are distinct differences between the primary aquatic production of the lower, more saline
part of the basin and the upper freshwater zone. Water bodies in the upper basin have high levels
of primary productivity that increase significantly in the summer and possess heterotrophic
characteristics. The aquatic community in the lower basin is less productive and lacks a consistent
seasonal trend (Conner and Day, 1987). The major categories of environmental impact within the
Barataria Basin are wetland loss, eutrophication, saltwater intrusion, reduction of nursery grounds
for fisheries, and introduction of toxic substances into wetlands.
There were 12,103 ac (4,900 ha) of natural oyster reefs in the basin in 1976 (Van Sickle et al.,
1976). These reefs experience high mortality in the summer months due to the protozoan Perkinsus
marinus, which is referred to colloquially as "Dermo." Increased salinity and temperature increase
the vulnerability of oysters to this disease.
The fish community in the Barataria Basin exhibits the most diversity of any water body in
Louisiana (186 species; 65 families). Because of the lack of freshwater input from river systems,
conditions in lower Barataria Bay closely resemble those of the nearshore Gulf of Mexico. Thus, the
fish community in that portion of the Basin is dominated by marine species. Studies of trawl-caught
fishes by Barrett et al. (1978) and Chambers (1980) revealed the following 10 most abundant species:
A. mitchilli (bay anchovy); M. undulatus (Atlantic croaker); Chloroscombrus chrysurus (Atlantic
bumper); B. patronus (Gulf menhaden); L. xanthurus (spot); Arius felis (hardhead catfish); C.
arenarius (sand seatrout); Polydactylus octonemus (Atlantic treadfin); Anchoa hepsetus (striped
anchovy); and Bagre marinus (gafftopsail catfish).
Several species of macroinvertebrates that inhabit Barataria Bay are commercially important.
Brown shrimp (Penaeus aztecus) and white shrimp (Penaeus setiferus) are harvested commercially
in the Bay. Pink shrimp (Penaeus duorarum), seabobs (Xiphopenaeus kroyeri), and two species of
Trachypenaeus can be significant components of the community during certain times of the year, but
generally are not taken in sufficient quantity to be of commercial importance. The blue crab
(Callinectes sapidus) is harvested commercially and recreationally. In many of the lower bay areas,
a related species, Callinectes similis, is found in greater abundance than C. sapidus; however, C.
Similis does not achieve a long enough size for commercial harvesting. The brief squid (Lolliguncula
brevis) is a nektonic mollusc that is abundant within the Barataria basin (Conner and Day, 1987).
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Craig and Day (1987) suggested that wetland losses in this system occur in three major ways:
1) wetlands become open water by erosion, subsidence, Or dredging, 2) wetlands are covered and
made into a terrestrial habitat, or 3) wetlands can be wholly or partly isolated by spoil banks.
Predictions of net wetland losses include 39.4 mi2 (102 km2) (25,212 acres) annually in coastal
Louisiana (Gagliano, 1981), with some estimates as high as 59.8 mi2 (155 km2) (38,265 ac) (Paul
Templet, LSU Environmental Studies, personal comrn., as cited by Craig and Day, 1987). Barrier
island retreat in Louisiana represents a serious problem indicated by a rate of loss estimated as high
as 160 ac (65 ha) per year. Shoreline retreat rates of 164 ft (50 m) per year have been reported by
Mendelssohn et al. (1982).
An example of wetland loss directly related to human activities occurred in the 12-year period
between 1962 and 1974, when 44,800 ac (18,138 ha) of wetlands in the Barataria basin were drained
or converted to water. Agricultural impoundments and oil access canals accounted for the largest
acreages (Adams et al., 1976). Craig and Day (1987) reported:
"...that between 40% and 90% of the total land loss in coastal Louisiana can be attributed
to canal construction, including canal-spoil area and cumulative losses (Craig et al., 1979b;
Scaife et al., 1983). In the deltaic plain of Louisiana, canals and spoil banks are currently
8% of the marsh area compared to 2% in 1955; there was an increase of 35,943 ac (14,552
ha) of canals between 1955 and 1978 (Scaife et al., 1983). Barataria Basin had a 0.93%/yr
direct loss of marsh due to canals for the period of 1955-78 (Scaife et al., 1983). Canals
indirectly influence land loss rates by changing the hydrologic pattern of a marsh, such
as blockage of sheet flow, which in turn lessens marsh productivity, quality, and the rate
of accretion. Canals widen with time because of wave action and altered hydrologic
patterns, and apparently the larger the canal, the faster it widens. Annual increases in
canal width of 2% to 14% in Barataria basin have been documented, indicating doubling
rates of 5 to 60 years (Craig et al., 1979b).H
Calcasieu Basin/Chenier Plain
Bahr et al. (1977) developed a conceptual model of the Chenier Plain coastal ecosystems in
southeastern Texas and southwestern Louisiana. The model took into account spatial heterogeneity,
ecological or functional complexities, time scale of events, and management needs. Use of this
model determined that annual primary production in the Calcasieu Basin is 2.5 x 106t (2.3 x 10 6mt).
This produces an estimated 1,100 t (1,000 mt) of shrimp, 8,470 t (7,700 mt) menhaden, 5 million
sport-fishing efforts, 222,000 dabbling ducks at peak density, and 49,000 fur pelts.
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According to Bahr et al. (1977), 18,038 ac (7,300 ha) of natural marsh have been lost since 1953,
70% of it to open water and the rest to impounded marshes, agriculture, and urban habitats. This
figure represents a loss of 26% of the total natural marsh area of the basin. The consequence in
natural resources is estimated to be a loss of 286,000 t (260,000 mt) of organic production, 77,000
birds per year, 19,000 fur pelts, and a significant impact on the shrimp and menhaden fisheries
(Table 38).
Table 38. Change in Area (Acres) of Habitats in the Calcasieu Basin, Louisiana between 1953 and
1975 (Adapted from Bahr et al., 1977)
Habitat
Open Water
Nearshore Gulf
Natural marsh
Area (Acres)
1953 1975
68,813 101,203
99,840 99,443
181,952 120,800
Net Area
Net % Change
+32.0
-0.4
-33.6
Other studies on the Chenier Plain were conducted by Gosselink et al. (1979), who observed
much of the impact is a result of canals that allow saltwater intrusion to change the habitat from
fresh swamp to brackish open water (Table 39).
Table 39. Wetland Losses (Acres) by Category in the Chenier Plain Between 1952 and 1974 (after
Gosselink et al., 1979)
Converted To
Acres
Area
Percentage
Urban
Agricultural
Spoil
Impounded marsh
Aquatic or open water
TOTAL
4,762
11,300
13,269
99,438
75,627
204,396
0.3
1.1
1.3
10.0
.7.6
20.3
The major nonrenewable resources of the Chenier Plain are oil and gas (value of $438
million/year). Major renewable resources (1977 dollars) are agricultural production of rice and cattle
($26 million/year); commercial fishing and trapping ($12 million/year), and recreational fishing and
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hunting ($21 million/year). The adverse effects of the direct pressure on the recovery of oil and gas
on renewable resources may have been too severe for the basins to recover naturally (Bahr et al.,
1977). . .
The Louisiana Geological Survey and U.S. EPA (1987) discussed the need for a long-term plan
to manage Louisiana's wetlands from losses due to the maintenance of shipping lanes, dredging of
canals, flood control levees, and withdrawal of oil and gas. Wetlands of coastal Louisiana are being
converted to open water at a rate of approximately 35 to 60 mi2/yr (91-155 km2/yr). If current
trends continue, an ecosystem that supports 33% of the nation's fishing industry and North America's
largest fur-producing area will become extinct. An acceleration of this trend (Table 40) is possible
if the predicted global warming from the greenhouse effect results in significant sea level rise.
Table 40. Change in Acreage (Acres x 100) in Louisiana Wetlands (from LGS and EPA, 1987)]
Habitat Tvoe
Marsh
Forested wetland
Upland
Dredge deposit
1956
Acreage
182,838
7,894
3,362
3,057
1978
Acreage
89,381
3,233
6,915
11,369
Acreage
Change
-93,457
-4,661
+3,553
+8,313
Percentage
Change
-51%
-59%
+106%
+272%
1 Calculations of acreage based in FWS National Wetlands Inventory documentation.
Alabama
Mobile-Tensaw River Delta
Stout et al. (1982) inventoried the extent and composition of wetlands and submerged aquatic
vegetation grassbeds in the Mobile-Tensaw River Delta. This delta, designated as a National Natural
Landmark in 1974, consists of approximately 115,103 ac (46,600 ha) of wetland habitats. The study
area was bordered to the north by the confluence of the Alabama and Tombigbee Rivers and
extended southward 45 miles (72.5 km) to the head of Mobile Bay.
Interpretation of color-infrared photography and field verification were used to delineate
wetland areas. Three general categories and nine wetland habitats were delineated, and acreage,
location, topography, and major plant species of each habitat were determined. The three general
categories of wetlands were forested wetlands, marshes, and submerged grassbeds. Of these three,
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forested wetlands were the most extensive, covering 100,014 ac (40,490 ha) (86.8%) of the total
wetland acreage. Marshes covered 10,589 ac (4,287 ha) (9.2%) and submerged grassbeds covered
3,696 ac (1,496 ha) (3.2%) (Table 41). Forested wetland types and corresponding acreages were: bay
forest, 3,291 ac (1,332 ha); alluvial swamp, 33,966 ac (13,751 ha); deep alluvial swamp, 35,301 ac
(14,292 ha); natural levees, 26,564 ac (10,755 ha); and moist pine savannah, 60 ac (24.3 ha). Many
rare and endangered plant species were found in the moist pine savannah community (Stout et al.,
1982). Freshwater marsh habitat was divided into low marsh, 4,354 ac (1,763 ha) and high marsh,
6,235 ac (2,524 ha). In addition to wetland habitats, 808 ac (327 ha) of upland pine-oak community
were delineated.
Table 41. Habitat Acreages in Alabama's Mobile-Tensaw River Delta (from Stout, 1982)
Wetland Category
Forested wetlands
Marshes
Submerged grassbeds
Acres
100,014
10,589
3,696
of Total
86.8
9.2
3.2
Summary of Wetland Habitats and Acreage from the Inventory:
Wetland Habitat Acres
Alluvial swamp
Deep alluvial swamp
Natural levee
Bay forest
Moist pine forest
Moist pine savannah
Freshwater marshes
High marsh
Low marsh
Submerged grassbeds
Upland pine-oak
33,966
35,301
26,564
3,291
832
60
6,235
4,354
3,696
808
There are no other detailed studies to which the results of this survey can be compared.
However, in recent years there has been increased oil and gas exploration in the area. Dredged
canals have the potential to modify the hydrology and community structure of the delta.
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Mobile Bay
Mobile Bay has received much attention during recent years because of declining natural
resources. The Alabama Sea Grant Extension Service (1987) summarized the knowledge of chemical,
physical, and biological oceanography of Mobile Bay. Stout (1979), Stout and Lelong (1981), and
Roach et al. (1987) surveyed the historic changes in wetlands, and Stout (1987b) summarized the
status of seagrass communities in coastal Alabama. Baldwin (1987) summarized waterfowl habitats
in Mobile Bay.
Watzin et al. (unpublished) are preparing a summary of the cumulative impacts on the Mobile
Bay ecosystem. This assessment proposes a strategy for effective environmental management of
Mobile Bay and includes: environmental problem analysis, status and trends analysis, goal setting
for bay resources, and implementation of goals. Information in that report is organized through the
use of cause and effect models. The first step in construction of the model is to state the problem.
Next, the causes of the problem are listed, and the effects of the problem defined. For example, one
problem discussed is the decline of natural emergent and submerged aquatic vegetation. Causes of
decline include filling activities that cover wetlands, dredging activities that remove vegetation, and
high concentrations of suspended particulate loads in bay waters that limit light penetration. Effects
include loss of primary production, cover for fish and wildlife, and benthic production. A total of
13 cause and effect models are being prepared which summarize the relationship between actions and
their effects on components of the Mobile Bay ecosystem.
Data from status and trends analyses in the Watzin et al. report were used to verify some of
the conceptual processes in the models and to quantify some impacts observed in the Mobile Bay
ecosystem. A decline of over 10,000 ac (4,049 ha) of emergent marsh and probable loss of 50% or
more of submerged aquatic vegetation occurred between the 1940's and 1979. In addition, the
hydrology of the Mobile Bay has been markedly altered through excavation of a deep channel
through the center of the Bay and the profusion of spoil areas in open water.
Watzin et al. report several animals which require large habitat ranges which once lived in this
area, but are no longer found, including red wolf (Canis n. niger), Florida panther (Felis concolor
coryi), and Florida black bear (Ursus americanus floridanus). Rare, but still occasionally found .are
swallowtail kite (Elanoides forficatus), sandhill crane (Cms canadensis), and gopher tortoise
(Gopherus polyphemus).
The most significant human impact noted in Mobile Bay by Stout (1979) was the direct and
indirect effects of dredging. Some of the effects of major dredging projects in Mobile Bay are given
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in Table 42. The impacts of small dredging projects are not included in Table 42 because they were
difficult to quantify. Approximately 6,000 ac (2,429 ha) of marshland have been destroyed and
approximately 2,200 ac (891 ha) created by spoil deposition. Assuming that a newly created marsh
is functionally equivalent to natural marshland (according to Stout, this is a dangerous assumption),
Mobile Bay has experienced a net loss of approximately 3,800 ac (1,538 ha) of marshland through
filling for spoil disposal. .
The distribution of the remaining marshes in Mobile Bay shows the influence of freshwater
inflow (Stout, 1979). Salt marshes dominated by S. alterniflora and /. roemerianus occur only in
lower Mobile Bay. The locations and marsh types in Mobile Bay are shown in Table 43..
Wetland losses due to erosion along the shoreline of Mississippi Sound in Alabama, including
adjace'nt islands, was approximately 21 ac (8.5 ha) per year, or a total of 630 ac (255 ha) from 1955-
1985. Much of this loss was marshland (Smith, 1989). This loss was not compensated by
accretionary gains which were negligible. Continued loss of coastal wetlands is expected under the
prevailing natural system and this progressive loss will be due, primarily, to action of natural forces
including wind-generated waves, tides, currents, and predicted drowning effect of sea level rise.
Smith presented a series of nine maps, representing the 1955 and 1988 shoreline positions of a
portion of this shoreline. Erosion rates as great as 12 ft (3.66 m) per year are reported (Smith, 1989).
Mississippi
Mississippi Sound is a large coastal body of water bounded seaward by a series of barrier
islands. The main estuaries of Mississippi Sound include the Pascagoula River, Biloxi Bay, Bay St.
Louis, and Pearl River. Approximately 70 mi (112.9 km) of coast occurs in Mississippi. The tidal
shoreline included in this distance is 369 mi (595 km). The total wet surface area at mean low water
(MLW) is 433,447 ac (175,485 ha) and at mean high water (MHW) is 500,379 ac (202,583 ha).
Approximately 21% of the area has a MHW depth of less than 3 ft (0.9 m), and about 6% has a depth
over 18 ft (5.5 m). The average depth at MLW is 11.7 ft (3.6 m) (Christmas, 1973).
Relatively little recent information is available on the status and trends of Mississippi's wetlands
and seagrass habitats. Mississippi marshes occur as an ecotone between saline and fresh water
habitats. Most of the coastal mainland marsh area (65,805 ac; 26,642 ha) is dominated by J.
roemerianus (61,398 ac; 24,857 ha). S. alterniflora (2,028 ac; 821 ha), S. patens (460 ac; 186 ha), and
Scirpus olneyi (96 ac; 39 ha) are the major plants that occur in the saline regions of the marsh. The
freshwater habitats are very diverse communities possessing more than 30 plant species (Christmas,
1973).
120
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Table 42. Impact of Dredging Activities on Mobile Bay Estuarine Marshes (from Stout, 1979).
Location
I. Loss to Spoil Deposition
Bon Secour River
Blakeley Island
East Fowl River
Little Dauphin Island
Dog River
I-10 Highway
I-10 Twin Tunnels
Alcoa-Blakeley Island
Scott Paper Company
3 Mile Creek
Private Projects
TOTAL
II. Loss to Canal Dredging
I-10
1-65
Theodore Industrial
Private Projects
TOTAL
III. Creation by Spoil Deposition
Blakeley Island
Polecat Bay
Pinto Island
Theodore Spoil Island
Acres
95
3,000
172
10
81
180
13
300
150
1,000
6,002
34
8
50
46
138
900
900
387
7
TOTAL 2,194
Total Loss 6,140 ha - Total Creation 2,194 ha = Net Loss 22% Total Marshlands
121
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Table 43. Estimates of Marsh Area by Type and Geographic Area for Mobile Bay and the Mobile
Delta (from Stout, 1979).
Geographic Area
Mobile Bay
1. Dog River
Salt/Brackisha
3,291C
Marsh Area (Acres)
Freshb
214
186
Total
3,505
2. Northwest Mobile Bay,
Dog River to Deer River 20
3. Deer River Complex 215
4. East Fowl River 358
5. Southwest Mobile Bay,
East Fowl River to
Cedar Point 300
6. East Dauphin Island 182
Little Dauphin Island
7. Weeks Bay 191
8. Oyster Bay/Bon Secour River 1,086
9. Fort Morgan Peninsula 939
Mobile Delta (Hwy, 90 North to
Mobile & Baldwin County Lines)
28
TOTALS 3,291
10,450
10,664
10,450
13,955
"From Stout, 1977
bFrom Vittor and Stout, 1975
122
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In 1968, there were 66,931 ac (27,098 ha) of coastal marsh in southern Mississippi. The 64,805
ac (26,237 ha) of coastal mainland marsh consisted of 823 ac (333 ha) of freshwater marsh and 63,982
ac (25,904 ha) of salt of brackish marsh. There were 2,126 ac (860 ha) of salt marsh found offshore
on the northern shores of the barrier islands. In addition, there were approximately 17,000 ac (6,883
ha) of submerged vegetation. The most abundant species were shoal grass, manatee grass, turtle
grass, and widgeon grass (Christmas, 1973).
Prior to 1930, approximately 1,000 ac (405 ha) of marsh were filled for road development.
Since 1930, another 8,170 ac (3,308 ha) have been filled for industrial or urban development, and
85 ac (34 ha) for landfills. As of 1973, 12% of Mississippi marshes had been filled for development
(Christmas, 1973).
The importance of Mississippi estuaries as a breeding and nursery ground for a multitude of
species has been well documented. The commercial catch of fish and shellfish in 1989 for all of the
Gulf states was 1.8 billion Ib (800,000 mt), with a dockside value of $649 million (NOAA, 1990a).
•?
These landings represented 21% of the total United States landing for that year. Mississippi's
contribution was 298,206,000 Ib (135,000 mt), which was 17% of the total from Gulf states. Of that
catch, most were menhaden, industrial bottom fish, shrimp, oysters, and crabs. The value of the
1989 Mississippi catch was $43,949,000. In 1989, the port of Pascagoula-Moss Point was third of all
U.S. ports in volume of landings with a catch of 282,100,000 Ib (128,000 mt). According to Power
(1963), 97% of the species caught by volume and 88% by value in the 1961 Mississippi landings were
estuarine dependent at one time or during all stages of their life histories.
Christmas (1973) listed 180 species of invertebrates found in trawl samples in Mississippi Sound.
Thirty species of crustaceans and molluscs made up 97% of the total number of species. White and
brown shrimp made up 29% and 14% of the catch, respectively. Crabs and oysters were collected
in amounts lower than expected because the sampling gear was not designed to capture them.
Bay anchovies were the predominant fish in samples taken in Mississippi Sound, and made up
70% of the catch by number. The small size of the bay anchovy adult has precluded commercial
exploitation of this fish. However, the anchovy was found to be very important as a forage fish, but
further study was needed to quantify its value to the commercial fishing industry. The next five
species in order of dominance were menhaden (10.7%), Atlantic croaker (6.6%), spot (2.3%),
butterfish (2.1%), and seatrout (1.6%). These species and the bay anchovy made up 93% of the total
number of fish collected (Christmas, 1973)..
123
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In 1880, 62,000 Ib (28 mt) of oysters were included in the first records of landings. This
amount represented 3% of the Gulf Coast harvest at that time. The maximum landings of oysters
occurred in 1937 with 12,894,000 Ib (5,860 mt) (53% of the Gulf harvest). The minimum harvest
of oysters in Mississippi (23,000 Ib; 10.4 mt) occurred in 1952 (0.2% of the Gulf harvest). More
efficient management resulted in increased landings. In 1964, 4,829,000 pounds (2,195 mt) (21%)
were harvested in Mississippi. Since that time, the State has produced approximately 13% to 17%
of the annual Gulf harvest.
Oyster reefs are located along the entire coast of Mississippi, with the largest reefs near the
western boundary. In 1962, approximately 100 oystermen were harvesting oysters from the reefs at
the mouth of the Pascagoula River, but that year heavy rains virtually wiped out the harvest. As of
1969, there were still very few oysters on the Pascagoula beds.
In 1966, according to a survey by WJ. Demoran (Gulf Coast Research Laboratory, Ocean
Springs, Mississippi), there were 9,934 ac (4,022 ha) of oysters; 582 ac (236 ha) were planted beds.
According to the National Register of Shellfish Production Areas (Houser and Silava, 1966), there
were 35,000 ac (14,170 ha) of approved shellfishing area. This is the highest classification available
to estuarine areas. A total of 87,300 ac (35,344 ha) of estuaries were closed to shellfishing. In 1961,
350 ac (142 ha) of a highly productive oyster reef in Back Biloxi Bay were closed. Also, 540 ac (219
ha) of oyster bottom at the Pascagoula oyster reef were closed due to pollution. The Escatawpa
River estuary is heavily contaminated for 7 mi2 (18 km2) and is "dead" in comparison with other local
rivers (Demoran, personal communication).
In a recent study, Eleuterius (in press) noted a decline of the area covered by seagrass and a
decline in occurrence of seagrass species in Mississippi Sound. 'Acreage of seagrasses in 1975 was
about 60% of that found in 1969, and losses are continuing. Hurricane damage and destruction by
fresh water discharged through a spillway accounted for approximately half of the observed loss.
The cause of the remaining loss is not known, but may be related to sediment quality (Eleuterius,
personal communication). The seagrass beds remaining in Mississippi Sound are composed almost
entirely of H. wrightii. However, even this relatively robust seagrass species exhibits sparse leaves.
124
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Conclusions .
The Gulf coastal zone is characterized by a great diversity of habitats, flora and fauna, natural
resources, industry, and recreational potential. The coast is richly endowed with productive wetland
habitats whose ecological functions enhance viable wildlife and fishery resources of the Gulf.
Coastal wetland systems are in natural biogeochemical balance with contiguous terrestrial, freshwater,
and marine systems. The natural balance can be adversely impacted by natural and human activities,
and these impacts can irreversibly change the character of the wetlands. For example, when
accretion of sediments by marshland is exceeded by subsidence, the result is a loss in marshland and
an increase in open water habitat.
• Although economic evaluation.of wetlands is still developmental, the value of some marshes,
based on sport and commercial fisheries landings alone, may be nearly equivalent to their real estate
value.
• In many instances, wetland habitats along the Gulf coast continue to be besieged by human
activities, such as dredging and filling for construction of canals, real estate development, and
conversion to other uses. Natural phenomena such as subsidence, sea level rise, impact of storms,
and erosion, also adversely impact wetlands. The primary causes of diminishing quality and acreage
of coastal emergent wetlands vary from state to state: subsidence due to extraction of oil, gas, and
fresh water in Texas; alterations of hydrodynamic flow due to construction of navigation channels,
as well as subsidence in Louisiana; dredge and fill operations in Mississippi and Alabama; and
conversion of wetlands to commercial and private developments in Florida.
• Although it is difficult, and sometimes impossible, to precisely compare acreages of
wetlands at different time intervals, reputable comparisons indicate a trend of major losses of
wetland habitats, particularly marsh, mangroves, and submerged aquatic vegetation. These losses are
summarized in Table 44. Some recent data suggest that the rate of loss may be declining in specific
areas (Table 45).
• Elevated levels of bacteria, which result in closure of waters to shellfish harvesting, is a
common problem in all Gulf states.
• Submerged aquatic vegetation in all Gulf coastal waters is especially susceptible to adverse
effects of dredging and filling activities, both from deposition of spoil directly on the plant
communities and from increased turbidity which reduces light penetration.
125
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• Excess nutrients from septic tank systems, sewage treatment plant discharges, and drainage
from agricultural fields contribute to seagrass loss by increasing turbidity and stimulating growth of
periphyton on the plants and phytoplankton (additional suspended particulates) in the waters over
the grass beds.
• The loss of quality and acreage of wetlands has slowed from the middle to late 1970's due to
passage and enforcement of Federal and state laws and regulations. Also, the ecological and
productive functions of wetlands are becoming better known to resource managers and to a more
interested and active public. Better informed managers and public awareness have made a positive
difference in management decisions concerning the disposition of wetland habitats.
• Interest in wetland management and research continues to grow, and many wetland-oriented
projects are underway. For example, the U.S. FWS is digitizing information on wetland acreages in
Gulf coastal states (some preliminary data are presented in this report), NOAA "continues to collect
data in their Status and Trends Program, MMS in cooperation with the state of Louisiana is
completing a study of marsh management practices, and the states of Florida and Texas will soon
publish updated data on wetland acreage. The U.S. Army Corps of Engineers is designing and testing
several freshwater diversion projects to improve the condition of wetland habitats along the lower
Mississippi River. Finally, the U.S. EPA Gulf of Mexico Program is developing a database on a GIS
system which will be instrumental in establishing a ecologically balanced management plan for
Mobile Bay.
129
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