QUICK LINKS TO SECTIONS OF THIS DOCUMENT:
Introduction
Mississippi's CWCS Ecoregions
East Gulf Coastal Plain
Mississippi River Alluvial Plain
North Gulf of Mexico
Upper East Gulf Coastal Plain
Mississippi's Species of Greatest Conservation Need (SGCN)
Table of Mississippi's SGCN
Description of SGCN Table
INTRODUCTION
Mississippi's Comprehensive Wildlife Conservation Strategy (CWCS) is part of a national collaborative effort among natural
resource agencies, conservation organizations, corporations and private landowners to address habitat needs of declining
wildlife species. These strategies mark the first time in U.S. history that state wildlife agencies and the broader conservation
community have cooperated to design a conservation blueprint for all wildlife species.
Since the early 1990s, the 3,000-member nationwide Teaming with Wildlife Coalition has worked to secure funding for state fish
and wildlife agencies to take preventative actions, keeping rare species from becoming endangered and common species abundant.
In 2001, Congress responded to this need by creating the State Wildlife Grants (SWG) program and from 2001 - 2005, over $300
million has been allocated to state wildlife agencies.
In order to make the best use of the State Wildlife Grants (SWG) program, Congress charged each state and territory with
developing a CWCS. Over a three year period, the Mississippi Department of Wildlife, Fisheries and Parks (MDWFP) has
coordinated this effort on behalf of the state of Mississippi to meet congressional requirements and to provide a "conservation
blueprint" for agencies, organizations, industries, private landowners and academics across the state to advance sound management
of all of our fish and wildlife resources in the future. The overarching goal of this planning effort is to provide a guide to
effective and efficient long-term conservation of Mississippi's biological diversity.
MISSISSIPPI'S CWCS ECOREGIONS
What is an ecoregion?
Ecoregions are commonly considered to be large areas distinguished from surrounding regions by
differing biotic and environmental factors and/or ecological processes. Factors that are generally
used to distinguish these large regions from one another include differences in climate, physical
geography, soils, species or communities.

East Gulf Coastal Plain Ecoregion
The East Gulf Coastal Plain (EGCP) ecoregion includes portions of five states (Georgia, Florida,
Alabama, Mississippi and Louisiana) and over 42 million acres. It stretches from southwest Georgia
across the Florida panhandle and west to southeastern Louisiana. The ecoregion has a diversity of
ecological systems, ranging from sandhills and rolling longleaf pine-dominated uplands to pine
flatwoods and savannas, seepage bogs and bottomland hardwood forests. The meager topographic and
soil diversity of the EGCP suggests an area of low biodiversity and endemism, yet the ecoregion is one
of the biologically richest in North America. Many species, particularly vascular plants, reptiles,
amphibians and fishes occur only in this ecoregion and many of those are even more narrowly limited
within the ecoregion.
This ecoregion is physically characterized by subtle topography, a warm to hot, humid maritime climate,
and soils derived primarily from unconsolidated sands, silts and clays transported to the ecoregion by the
weathering of the Appalachian Mountains. Other features include a high percentage of land area in
wetlands, a dominant role of frequent fire over the majority of the landscape, a diversity of river and
stream systems, limited but important karst areas, and significant large scale disturbance events such as
hurricanes.
This ecoregion experiences high species richness, species endemism and community diversity in
terrestrial, freshwater and aquatic systems. Part of the reason for this is that the ecoregion has never
been glaciated, and has been continuously occupied by plants and animals since the Cretaceous period,
giving ample time for the evolution of narrow endemic species.
The dominant ecological drivers of the terrestrial systems are soils (texture and chemistry), fire
frequency and hydrology. While habitats in the EGCP include barrier island systems with annualdominated
beaches, maritime grasslands and scrub, maritime shrub hammocks, and evergreen forests
(both broadleaf and needleleaf) these habitats have been classified as part of the Northern Gulf of
Mexico Ecoregion (NGM) for the purpose of this CWCS. Inland, longleaf pine woodlands are dominant
over most of the landscape, on upland and wetland sites and a wide variety of soils. These pinelands
(sandhills, clayhills, flatwoods and savannas) support a tremendous diversity of plant and animal
species: most of them unique to these systems. Embedded in these pinelands, specialized patch
communities such as seepage bogs, treeless "savannas" and "prairies", and seasonally flooded depression
ponds provide rich habitat for plants, amphibians, and invertebrates. Imperiled plant species are
concentrated in fire-maintained pinelands (wetland and upland) and associated seepage bogs. While
many imperiled animal species also occur in these communities, there are also significant concentrations
in aquatic and bottomland systems.
The freshwater aquatic systems of the EGCP are among the most significant and at-risk aquatic
biodiversity resources in North America, particularly for fish and mussel species. Each of these groups
has unique biodiversity resources. Many aquatic animals are endemic to the ecoregion, and many are
restricted to a single river system and its tributaries. Thus, conservation of aquatic biodiversity in the
EGCP requires conservation of most of the river systems. In addition, the EGCP supports a range of
bottomland hardwood forests and cypress-gum swamps, as well as many lakes and natural ponds.
What is the current status of EGCP biodiversity? The pineland ecosystem (consisting of fire-maintained
longleaf pine and slash pine woodlands and their associated seepage bogs and depression wetlands) once
dominated a string of ecoregions from southeastern Virginia to eastern Texas. This system has now
been reduced to less than five percent of its former range, making it one of the most endangered
landscapes in North America. Not only have these pineland ecosystems been directly reduced in extent,
but remaining areas are also fragmented and many suffer from the exclusion of fire, a critical ecological
process for their maintenance and health. Aquatic systems have been severely affected by hydrologic
alterations, pollution and introduction of non-native species. Most of the hundreds of species endemic to
the ecoregion, many of which were never common, have been further imperiled by these changes.
The following habitat types described in Chapter IV of this CWCS can be found in the EGCP ecoregion:
- Dry- Mesic Upland Forests/Woodlands
- Agriculture Fields, Hay and Pasture Lands, Old Fields, Prairies, Cedar Glades and Pine Plantations
- Wet Pine Savannas/Flatwoods
- Mesic Upland Forests
- Bottomland Hardwood Forests
- Riverfront Forest/Herblands/Sandbars
- Spring Seeps
- Bogs
- Inland Freshwater Marshes
- Swamp Forests
- Lacustrine Communities
- Streams
- Urban and Suburban Lands
- Rock Outcrops and Caves
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Mississippi River Alluvial Plain Ecoregion
The Mississippi River Alluvial Plain (MSRAP) is a 23,968,700 acre ecoregion that includes several
uplands and most of the Atchafalaya Basin, but excludes the Red and Ouachita River Alluvial Plains and
coastal areas south of the forested portions of the Atchafalaya Basin. Its most defining feature is the
Mississippi River which flows south over the Mississippi Embayment, a structural trough in the earth's
crust that, over the past 100 to 200 million years, has thrust alternately upward and downward relative to
the sea. MSRAP is a geologically complex area, with Coastal Plain sediments having been deposited by
a retreating Gulf of Mexico during the Tertiary Period of the Cenozoic Era. The melting of the glaciers
during the Pleistocene forced the upper Midwest and the current Ohio River Basin to drain southward
and, over time, form the modern-day Mississippi River. Retreating glaciers left behind glacial outwash
that, through time, was reworked by the energy of the river and overlaid by deep alluvium deposited
through annual overbank flooding. Several distinct landforms in MSRAP represent an accumulation of
coarse, glacial sediments that have not been fully subjected to the erosional forces of big river systems,
and thus remain tens of feet above floodplain elevations. Crowley's Ridge in Arkansas is hundreds of
feet above the floodplain and is comprised of Tertiary deposits. Well-drained, highly-erodable, windblown
deposits (loess) originating from glacial outwash are characteristic of these landforms. Upland
pine hardwood plant communities and, in areas of clay-pan formation, prairie communities, characterize
these upland areas.
The bottomland hardwood forest is by far the dominant natural plant component of MSRAP. It is
maintained by regular back- and headwater flood events and localized ponding on poorly drained soils.
Headwater or mainstem flooding results from rainstorms over the watersheds of the Mississippi's
tributaries, and produces the great spring floods characteristic of MSRAP. Backwater flooding is a
phenomenon in which high water stages on the Mississippi River create a damming effect, preventing
tributary drainage into the mainstem and at times reversing tributary flow upstream. As a result, longduration
flooding accompanied by sediment and nutrient deposition occurs throughout the associated
tributary watersheds.
Concomitant to these flooding mechanisms are the hydrogeomorphic processes associated with
meandering river systems. The high energy inherent in the Mississippi River and its tributaries once
sculpted the landscape, producing a surface geomorphology comprised of natural levees, meander scar
(oxbow) lakes, point bars and ridge and swale topography. Site conditions within MSRAP range from
permanently flooded areas supporting only emergent or floating aquatic vegetation to high elevation
sites that support climax hardwood forests. The distribution of bottomland hardwood communities
within the floodplains of the Mississippi River and its tributaries is determined by timing, frequency and
duration of flooding. Elevational differences of only a few inches result in great differences in soil
saturation characteristics and thus the species of plants that grow there. As a result, much variability
exists within a bottomland hardwood ecosystem, ranging from the bald cypress/tupelo swamp
community that develops on frequently inundated sites with permanently saturated soils, to the
cherrybark oak/pecan community found on the sites subjected to temporary flooding. Between these
rather distinct community types are the more transitional, less distinguishable overcup oak/water
hickory, elm/ash/hackberry and sweetgum/red oak communities.
In time, and in response to sediment texture, deposition rates and quantities, plant communities
characteristic of MSRAP undergo ecological succession from pioneer communities dominated by black
willow or cottonwood (depending on soil drainage characteristics) to red oak and finally white oak
dominated climax community. But other disturbances also influence plant community distribution.
Both human- and naturally-induced disturbances, such as ice storms, hurricanes, beaver activity,
hydrologic alteration and silvicultural practices, greatly influence the rate and direction of succession.
There is emerging thought that the dynamic nature of this water- and sediment-driven system, coupled
with frequent disturbance, historically precluded, in most cases, the development or long-term viability
of a closed canopy of senescent trees, or a community commonly thought of as old-growth. The presettlement
forests of MSRAP were likely a shifting mosaic of even-aged small patches of all-ages,
further defined by minute differences in elevation and tolerances among a large number of woody
plants.
The diversity of forests and other habitat characterizing the historic landscape provided an extraordinary
habitat for a range of species utilizing MSRAP. River floodplain systems are highly productive and
provide exceptional habitat for a variety of vertebrates including foraging and spawning fish,
amphibians and reptiles. Over 240 fish species, 45 species of reptiles and amphibians and 37 species of
mussels depend on the river and floodplain system of MSRAP. In addition, 50 species of mammals and
approximately 60 percent of all bird species in the contiguous United States currently utilize the Mississippi
River and its tributaries and/or their associated floodplains.
The following habitat types described in Chapter IV of this CWCS can be found in the MSRAP ecoregion:
- Agriculture Fields, Hay and Pasture Lands, Old Fields, Prairies, Cedar Glades and Pine Plantations
- Bottomland Hardwood Forests
- Riverfront Forests/Herblands/Sandbars
- Inland Freshwater Marshes
- Swamp Forests
- Lacustrine Communities
- Streams
- Urban and Suburban Lands
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Northern Gulf of Mexico Ecoregion
The Northern Gulf of Mexico (NGM) ecoregion extends from Anclote Keys, Florida to the southern extent
of the Laguna Madre de Temaulipas in Mexico. It is a rich and productive subtropical system that
supports some of the most extensive wetland and seagrass habitats in the world. Much of the nearshore
waters of the Gulf are divided into bay and estuarine systems behind barrier islands, which form a ring
of sites around the NGM. For the purposes of this CWCS habitats including barrier island systems with
annual-dominated beaches, maritime grasslands and scrub, maritime forests have been classified as part
of the NGM ecoregion. These grade through salt marshes to productive estuaries.
In Mississippi, the NGN borders the EGCP and is completely coincident with it. TNC has divided the
ecoregion into three broad subregions for planning purposes. Mississippi falls within the Central Gulf of
Mexico region which runs from Galveston Bay, Texas to Mobile Bay, Alabama. This region is characterized
by extremely high levels of riverine input. Freshwater and sediments from the Mississippi River
and to a lesser extent freshwater entering through Mobile Bay determine the characteristics of nearshore
waters in this region. Coastal waters are generally variable in salinity, and water clarity is low because of
the sediment load. Bottom sediments tend to be fine clays and muds. These conditions are ideal for the
growth of marshes and oyster reefs.
The drainage basin for the Gulf extends from the Appalachians to the Rockies. It contains nearly 60 percent
of the land area of the continental United States, including some the most fertile lands in the world.
This productive drainage makes the Gulf one of the primary producers of finfish and shellfish in the
United States. However, because much of this land is in agricultural use, fertilizers, herbicides and pesticides
threaten the productivity of the Gulf.
The NGM is a productive environment. In 1997, the estimated commercial value of the finfish and shellfish
harvest was $823 million.
The Gulf is ranked as the top region in the country for seafood harvest in both poundage and monetary
value. Much of the productivity of this region is believed to have its origins in the productivity of the
nearshore marshes and seagrasses, because these habitats serve as nurseries for juveniles, and/or simply
because they are the source of vast amounts of carbon and nutrients.
Estuarine, seagrass and marsh environments, which are in abundance in the NGM, are estimated to be
ten times more valuable to humans than any terrestrial habitat for ecosystem services like food production,
recreation and nutrient cycling.
The following habitat types described in Chapter IV of this CWCS can be found in the NGM ecoregion:
- Streams
- Upland Maritime and Estuarine Fringe Habitats
- Estuary and Mississippi Sound (Inside or Associated with the Barrier Islands)
- Marine Habitats
- Urban and Suburban Lands
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Upper East Gulf Plain Ecoregion
The Upper East Gulf Coastal Plain (UEGCP) ecoregion encompasses 33,861,051 acres. This large
ecoregion ranges from southern Illinois, western Kentucky and Tennessee, throughout much of
Mississippi, east to Alabama and a limited area of Georgia and southeastern Louisiana. The region is
bounded on the west by the MSRAP and on the north by the Ohio River, and Tennessee River. The
eastern margin occurs at the contact point with older rocks of the Piedmont and Southern Ridge and
Valley. This region has rugged terrain and hilly topography In addition, the southern boundary
approximates the range limits of major potential natural vegetation types oak-hickory-pine to the north,
and southern mixed hardwood forests to the south.
Coastal and fluvial processes have considerably reworked the land surface of the region. Approximately
70 million years ago, the area would have been around 4,000 foot elevation. However, the earth's crust
sagged forming the Mississippi Embayment. During the Tertiary and Cretaceous periods the Embayment
trough was repeatedly invaded by shallow seas leaving behind hundreds of meters of sediments that
occupy broad bands approximately paralleling the Gulf of Mexico. The result is a region of belted
character, in the form of inner lowlands and cuestas and other low-ridge landforms.
The upper Mississippi Embayment is underlain by an ancient, buried rift zone. This buried rift has acted
as a "zone of weakness" in the continental crust and serves to localize earthquake activity in the central
United States. There have been many large magnitude earthquakes and abundant seismic activity in the
region. The New Madrid earthquake (1811-1812) was among the strongest earthquakes in recorded
United States history, resulting in up to nine feet of land subsidence in the upper part of the region.
Further south, the geologic structure of the region has been affected by the presence of underground salt
in the form of salt plugs, domes, and basins. The Mississippi Interior Salt Basin, which extends into this
region, has extensive hydrocarbon reserves that are still largely undeveloped.
Throughout the region, soils are generally acidic with appreciable amounts of clay present. Ultisols,
deeply leached and low in nutrients, are the dominant soil order. Alfisols, less weathered and greater in
fertility, are present in more limited areas, especially associated with loess deposits (a unique type of
windblown silt). Large quantities of loess were probably carried by wind from exposed sediments of the
Mississippi River floodplain and deposited on adjacent uplands during the late Pleistocene and early
Holocene. Loess eventually covered much of the underlying topography under a thick blanket deepest
along the western edge and thinning abruptly eastward. Vertisols (soils with shrink-swell properties due,
in part, to especially high clay content) are uncommon in the southeastern coastal plain but are present in
limited areas of the Black Belt where they were derived from marl and chalk residues.
The UEGCP overlaps several distinctive aquatic ecoregions. The majority of this region has been
considered a priority for freshwater species conservation due to the richness of the fauna present. For
example, rivers in this region provide habitat for over 206 native fish species.
The region also supports relatively large numbers of crayfish and mussel species despite heavily
disturbed conditions in many areas that have likely reduced faunal diversity. The bulk of the regions'
rivers, especially the Mississippi tributaries, have been channelized and/or subjected to headcutting and
heavy sedimentation.
The region includes a diverse assemblage of streams that vary in size, origin, and geology. Particularly
noteworthy rivers of this region include the Hatchie, the longest free flowing tributary in the lower
Mississippi River valley and tributaries of the Pascagoula, America's longest unencumbered river.
The potential natural vegetation of the UEGCP may be characterized as broad bands of different
composition that roughly parallel the coast. From south to north these include southern mixed forests,
oak-hickory-pine forests, and oak-hickory forests, interrupted by occasional southern floodplain forests
and black belt prairies.
Southern mixed forests and oak-hickory-pine forests, the two predominant types in terms of area
occupied, are recognized by the presence of longleaf pine and shortleaf pine. Although longleaf forests
and woodlands were the dominant vegetation type of the southeastern United States coastal plain, they
occur in only limited areas of this region, extending landward into the UEGCP by only about 50 miles.
Northward, longleaf pine is replaced by shortleaf pine.
Bluffs along the eastern edge of the Mississippi River, such as those around Vicksburg, are covered with
up to 200 feet of loess. A number of factors account for the development and maintenance of precipitous
cliffs and ravines where loess is deepest. The vegetation of these loess bluffs is often richer than
surrounding areas due to the fertile topsoil and abundant moisture. In many cases, the bluffs provide
habitat for plant species that are rare or absent from other parts of the Coastal Plain. In addition, the
bluffs constituted a major refugium for mesophytic plant species, now generally more common to the
north, during the last glaciation.
Blackland Prairies occur in two discrete areas of the ecoregion: the Jackson Prairie and the Black Belt
(see Northeast Prairie subtype in this CWCS). These areas are among the distinct topographic regions in
the state of Mississippi. At their closest point, 65 miles separate the formations supporting the two
prairie types. The Black Belt is the larger of the two regions, stretching approximately 300 miles across
Mississippi and into adjacent parts of central Alabama. This region, generally 25-30 miles wide, derives
its name from the nearly black, rich topsoil that developed over Selma Chalk. Both areas have typically
calcareous soils and were formerly occupied by natural grasslands and associated vegetation.
The broad forest cover composition also differs between parts of the region. While the percentage of
total area occupied by deciduous forests is relatively evenly distributed across the region, mixed and
evergreen forests (each generally including a component of pine species) are much less common overall
in both the Black Belt and the North Unit (North of the Mississippi-Tennessee state line). The reasons
for this pattern are most obvious in the case of the North Unit, most of which lies outside the natural
range of the southern pine species (loblolly, shortleaf, longleaf) commonly encountered this ecoregion.
The lack of evergreen forests in the Black Belt is more complex, but is likely due to the poor suitability
of the predominantly calcareous soils for pine growth.
The composition of the ecoregion's forests is also changing. Vast acreages of the region are being
converted to pine plantations, in many cases at the expense of either existing deciduous or mixed forests,
constituting one of the most consequential forestry developments in the region in the last four decades.
The following habitat types described in Chapter IV of this CWCS can be found in the UEGCP ecoregion:
- Dry-Mesic Upland Forests/Woodlands
- Agriculture Fields, Hay and Pasture Lands, Old Fields, Prairies, Cedar Glades and Pine Plantations
- Mesic Upland Forests
- Bottomland Hardwood Forests
- Riverfront Forests/Herblands/Sandbars
- Inland Freshwater Marshes
- Swamp Forests
- Lacustrine Communities
- Streams
- Urban and Suburban Lands
- Rock Outcrops and Caves
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