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Natural Resources of the University
by the Sea:
Habitats and Ecosystems of Savannah State University
First published by the Savannah State College
Archives, Volume 1, number 2 winter 1994.
Revised 1/21/99
For more than 100 years the beauty of Savannah State University's campus
has provided an inspirational setting for intellectual and spiritual
growth at "The University by the Sea." The beauty is more than skin
deep. Containing elements of two biologically diverse and important
coastal ecosystems, the maritime live oak forest and the salt marsh
estuary, the 165-acre campus is ecologically unique among the 34
instructional units of the University System of Georgia. These natural
habitats and ecosystems provide natural laboratories for instruction and
research in the School of Science and Technology where they are closely
linked to abundant "hands-on" exposure and experiences, particularly in
the Bachelor of Science degree programs in Marine Biology and
Environmental Studies.
Savannah State University, formerly Georgia State Industrial College for
Colored Youth, was founded as a result of the Land Grant Act of 1890
which forced the Georgia General Assembly to establish a land grant
college for Blacks in Georgia or risk losing federal funds. Higher
education for Blacks at Atlanta University resulting from the 1862 Land
Grant Act became unsuccessful when legislators withdrew the funds from
the institution, arguing that since white students were being taught,
the laws of segregation of races in public education in Georgia were
being violated (Hall 1991). A community effort was begun on March 6,
1891, at the First African Baptist Church to secure the college for
Savannah. The group convinced a commission of five persons appointed by
the governor to locate the college in Savannah, and the first 76 acres
of land upon which the current 165-acre campus resides was deeded to the
Trustees of the University of in 1891 in two tracts: 10 acres donated by
George Parsons of New York City and 66 acres were purchased from Sara B.
Postell for $6,000. Bordering the predominantly white town of
Thunderbolt and Southeast coastal salt marsh, the land was, at one time,
part of the Placentia Plantation, later known as Warren Place and
contained two large homes which became Parson's Hall, located at the
site of the current swimming pool, and Boggs Hall, located in front of
Camilla-Hubert Hall (Hall 1991).
Construction of buildings on the campus began near these structures on
the sandy bluff overlooking the salt marsh in the area now known as
Felix J. Alexis Circle. This high ground represents barrier island beach
dunes that were formed during the Pleistocene epoch 35,000 to 40,000
years ago. At that time the coastline was adjacent to the current campus
because the sea level was higher as the result of globally warmer
temperatures and more water in the oceans from melted polar ice. Small
changes in sea level coupled to tidal and wave scouring can result in
significant landscape rearrangement along broad, gently-sloping, sandy,
barrier island coastlines. Even without sea level changes, the action of
wind, wave, and tides, especially during storms, annually re-configure
barrier island coastlines. Certain places on Wassaw Island, a favorite
field trip spot for SSC Marine Biology classes, have undergone changes
from dune, to beach, to tide pool, to salt marsh, back to dune over a
period as short as 14 years.
The campus is located in the low country, an area bordered by the
Atlantic Ocean to the east, sand hills to the west, and extending from
Georgetown, South Carolina, to St. Marys, Georgia. The diverse
ecological communities of the low country and campus result from the
considerable influence of fresh water, salty ocean water, and the tidal
mixing of them resulting in the biologically productive shallow aquatic
habitats called estuaries. The low country represents one of the most
extensive salt marsh estuary systems in the United States. The magnitude
of the system results from the broad gently sloping sandy coast and
continental shelf of the Southeast U.S. coupled with one of the highest
tide ranges along the east coast of North America. Each day, two high
and two low tides averaging 6 to 8 feet in range inundate a vast area of
the coastal zone, maintaining a system of creeks, channels, and rivers.
Since tides are principally the result of the gravitational pull of the
moon and the sun on the earth, the timing and range of the tides depend
upon their relative positions. Tidal range is greater than average when
the sun and moon are aligned with the earth during new and full moons
and are called spring tides. Tidal range is smaller than average when
they are not aligned during the other moon phases and are called neap
tides.
Besides an average annual rainfall of over 50 inches
per year, an enormous volume of freshwater enters the coastal zone from
rivers. The fresh water that drains into the tidal zone is mixed with
sea water and creating brackish conditions and one of the earth's most
productive ecosystem. Energy captured by plants from sunlight flows from
prey to predator throughout a complex estuarine food web in which
nutrients are absorbed, redistributed, and recycled. Due to the
abundance of early life stages of both coastal marine and oceanic
species in the system, estuaries are called the "nurseries of the sea."
The eggs and larvae of both estuarine and marine species are carried
into a system where they find both resources and refuge. Estuarine
habitats are subdivided into salt marsh shrub zone, salt marsh flats,
needle rush marsh, smooth cord grass marsh, marsh edge zone, intertidal
creek banks, bars and flats, and tidal pools, creeks, and rivers.
The saline influence of the ocean in coastal environments is
significant. Sea water is salty because it contains 7 major ions
(elements forming salts when not separated by water in a solution), 5
minor elements, and 11 trace elements. The salinity or saltiness of
oceanic sea water is about 36 parts per thousand (3.6%) dissolved
inorganic ions and elements. The salinity of the brackish water in the
tidal creek and adjacent coastal waters can range from less than 5 to
over 30 parts per thousand during the year. The plants and animals that
inhabit this changing environment are generally well-adapted to it.
The major elements of the salt marsh ecosystem can be seen from the
University dock adjacent to the Marine Biology building. Smooth cord
grass is the dominant tall green grass found in the lower part of the
marsh where the ground stays wet and very muddy as a result of the tides
flooding the area twice daily. In late spring through late fall when
most of the salt marsh is lush green, darker dead-looking sections of
marsh grass can be seen. This dead-looking marsh grass has long, tubular
stems and sharp brown- pointed tips and is called the needle rush. These
two grasses are replaced toward higher ground by the sea oxeye, which
has a succulent leaf with a yellow aster flower in June and the similar,
but taller, marsh elder, a shrub that encroaches on part of the wooden
walkway leading to the dock. None of these salt tolerant plants, called
halophytes, is found beyond the influence of the brackish tidal water.
The tidal creek supports much more marine life during the summer than
during the winter. In summer, the warmer temperatures and greater
sunlight increases the overall productivity of the salt marsh while in
winter the colder temperatures and less sunlight decreases the
productivity. While the water in the tidal creek is never crystal clear
because the tides constantly stir up the mud, it is significantly
clearer in the winter because there are fewer microscopic organisms such
as algal cells suspended in it.
At low tide, the surface of the mud banks along the campus' tidal creek
is highlighted by the golden hue of millions of algal cells called
diatoms. Mud snails aggregate by the thousands on the mud zone. Mullet,
Atlantic menhaden, killifishes, blue crabs, mud crabs, white shrimp, and
brown shrimp are most responsible for activity at the surface of the
water in the creek. Because of the significant tidal flushing, pollution
does not accumulate in the creek; blue crabs and shrimp harvested here
are safe to eat.
Attached to the dock and its pilings are barnacles, oysters, seaweeds
and a variety of encrusting marine life known as hydrazoans, anthozoans,
and ascidians. Because they strain microscopic particles from the water,
including harmful microorganisms associated with animal waste, oysters
from the creek by the campus and many other tidal creeks and rivers near
human and animal habitation cannot safely be consumed. Attached and
clinging to the stalks of the salt marsh grasses are ribbed mussels and
periwinkle snails. In higher marsh sandy zones, fiddler crabs dig
burrows, feed, and interact. The one enlarged chela (claw) of the male
is useful for defense and communication but it is not effective for food
gathering. As a result, males must spend twice as much time feeding as
the females, which have two small chelae.
A non-natural, but common element of the salt marsh is marine debris:
plastic containers, Styrofoam, cans, and other material of human origin,
which ends up along coastal shorelines. These materials come from
commercial and recreational boats and ships, marinas and docks where
trash containers are absent or overflowing, construction sites and
vehicles on roadways near the water, and from deliberate littering.
Debris is constantly being redistributed on coastal shores by the action
of tides, winds, and waves. Based upon a 1992 study of the rates of
accumulation at four sites in Chatham County, over 40,800 kg or 40.8
metric tons of marine debris wash up on coastal shorelines in Chatham
County annually (Gilligan et al).
The maritime influence on the campus climate and vegetation is
significant. In the spring when it is somewhat hot and humid inland, the
campus has cool breezes from the still-cold tidal waters, a form of
natural air conditioning. In winter, the relatively warmer tidal waters
can prevent vegetation from freezing. For example, cabbage palms, a
distinctive tropical element of the low country, only grow naturally
close to salt marshes.
Most of the natural and developed parts of the campus contain major
elements of the maritime live oak forests, which characterizes the low
country and its barrier islands. Well over 100 species of trees, shrubs,
vines, and grasses can be found on or near the campus. The most notable
and distinctive vegetative elements of the campus are the size and
number of canopy trees (live oak, cabbage palm, loblolly pine, southern
magnolia) and the large number of oak tree species.
Between the Marine Biology Building and dock are a weeping willow and
red mulberry. A larger red mulberry is located directly behind the
Kennedy Fine Arts Building. Adjacent to the Marine Biology Building
along the marsh is an eastern red cedar, which is characterized by its
dark, green, scaly leaves and light brown, fibrous bark and some very
tall and old cabbage palms. The smaller variety of palm found in
low-lying wooded areas is the saw palmetto because it has saw tooth
edges at the base of the frond stems. Near the entrance to the Marine
Biology Building are two sweet gum or gum-ball trees. Their star-shaped
leaves are fragrant when crushed, and their fruit are round and prickly.
Directly in front of the building are live oaks, so-called because they
do not lose their leaves and look "dead" in winter. Hanging from them is
Spanish moss which is neither Spanish nor a moss since it produces small
green flowers. It is a bromeliad (air plant) obtaining its nutrients
from debris on the branches. It does not harm the host tree but can
reduce nut production in pecan trees.
Along the marsh directly behind Camilla-Hubert Hall are several laurel
oaks between the parking lot and marsh. The leaves are elliptic, black
and deeply furrowed. Bordering the east entrance to the building is a
yucca or Spanish bayonet, a desert plant with succulent leaves with a
sharp point, wax myrtle, a shrub with small gray, aromatic leaves and
white berries, azaleas, and a hickory tree.
Across the street on Felix J. Alexis Circle is a
southern magnolia which has very thick, shiny, oval, evergreen 5 to 10
inch-long 2 to 3 inch-wide leaves. The fruit is reddish brown with a
fragrant smell. The circle is dominated by large live oaks, many of
which have resurrection fern growing on the limbs. Under dry conditions
the fronds curl up and turn brown but uncurl and turn green when wet.
Scattered on the north half of the circle are some near record size
loblolly pines which have pale blue needles bundled into threes and
reddish-brown bark.
There is a high diversity of both indigenous and planted tree species on
campus including pignut hickory (behind Herty Hall); tallow tree,
sugarberry (between Hubert and Kennedy Halls); pecan (next to Kennedy
Hall); slash pine (grove next to Griffith Drew Hall); long leaf pine,
swamp chestnut oak (grove next to Whiting Hall); water oak, willow oak,
Darlington oak, red oak (by Gardner Hall); black tupelo or black gum
sweet bay (between NROTC and the Orsot Apartments); Virginia pine
(behind Jordan Hall); Shumard oak, Carolina laurel (across from Plant
Operations); Bradford pear, red maple, silver maple, dogwoods,
lagustrum, mimosa, and many others.
Through the diversity and abundance of insects in the low country is
fascinating to a biologist, they are generally regarded as pests, and in
some cases, genuine nuisances. The prominent species in the later regard
is the small biting midge, affectionately known as sand gnats or "no-see
ums" which are occasionally abundant in early spring and late fall near
the salt marshes where they breed. Fortunately, their populations are
naturally regulated to unnoticeable levels during most of the year.
Mosquitoes, including a saltwater species, would be a significant
problem on campus if it were not for the diligent and efficient efforts
of the Chatham County Mosquito Control Commission which monitors
populations and employs a variety of control methods. In the mid 1980's,
the Asian tiger mosquito arrived in Savannah and has spread throughout
the county. It is a container breeder and need only a small amount of
standing water in which to lay its eggs, even water trapped in folded
magnolia leaves. It is not only difficult to reduce its breeding habitat
but also more difficult to control adult populations because it is
active during the day, and pesticide spraying is only effective during
the night.
The two major aquatic habitats on campus are the Placentia Canal, a
county-maintained, fresh water drainage system which runs through the
campus and drains into the Wilmington River, and the salt marsh estuary.
Though they contain the same ecological components (producers, consumers
and decomposers), fresh water and marine habitats are distinctly
different in terms of their component species. Many amphibians (frogs
and a large ell-like amphibian called the two-toed amphiuma) make their
home in the canal, but no amphibians are found in marine habitats. Over
100 coastal marine and estuarine fishes have been collected from the
salt marsh and nearly two dozen from the canal, but only a few species
are at home in both habitats.
The reptilian inhabitants and visitors to the campus include a variety
of non-poisonous snakes, lizards, geckos, and turtles. American
alligators, though fairly abundant in some parts of the low country, are
rare on or near the campus due to the lack of adequate fresh water
habitats that they prefer. Natural resource personnel remove small
alligators from the area to more suitable locations. The diamond back
terrapin, an attractive turtle, lay its eggs on high ground in the salt
marsh and several other turtle species are found on campus. Over 250
species of birds inhabit or visit the low country; however, fewer than
30 are seen daily on the campus. From the upland habitat of campus to
salt marsh to sounds and beaches, the most commonly observed birds here
are the common grackles, boat-tailed grackles, mockingbirds, common
crows, fish crows, turkey vultures (buzzards), mourning dove, ground
doves, swallows, red-winged blackbirds, cormorants, brown pelicans, five
species of herons, three species of egrets, laughing gulls, ospreys,
bald eagles, royal terns, least terns, and black skimmers. Winter
migratory residents of the campus tidal creek include hooded mergansers
and loons.
Fifty of nearly 100 species of coastal mammals recorded from the low
country sea islands have been reported in Chatham County. They include
both terrestrial species and marine species (whales, dolphins, and
porpoises). The largest mammal encountered near the campus is the
Atlantic bottlenose dolphin. Individuals and small pods have been
observed from the University dock swimming up the tidal creek to feed on
the abundant mullet. Pods exhibit a remarkable behavior here and in
other tidal creeks of the low country: they chase schools of mullet onto
the mud banks and emerge completely from the water onto the bank to feed
on them.
Large river otters and mink are occasionally seen swimming or running
along the mud banks and disappearing into the marsh grass along the
tidal creek. Raccoons would probably be more abundant on campus were it
not for the large populations of feral house cats that live and forage
near the marsh and dormitory trash bins. Several undeveloped areas
remain on the campus which contains natural understory vegetation of the
maritime forest. These acres are principally located along the north
margin of the campus bordered by the Placentia Canal, North Tompkins
Road and Drew-Griffith Hall. Another small, but diverse section remains
between the NROTC building and the Orsot Apartments.
No other instructional unit of the University System of Georgia can
boast such a rich endowment of coastal habitats and ecosystems. On a
calm cool evening in the early spring and late fall, the view through
the oaks, pines, palms, cedars, and magnolias to the salt marsh grasses
illuminated by the setting sun is a unique and enchanting experience of
singular beauty, inspiration, and wonder.
The natural environments of its campus have enhanced the rich
educational history and legacy of Savannah State University. This
spiritually uplifting place lives in the memories of all those who have
been touched by it and will continue to offer its unique qualities and
experiences in higher education to all.
The 165-acre campus of Savannah State University contains elements of
two biologically diverse coastal ecosystems: The maritime live oak
forest and the salt marsh estuary. The variety of plants and animals
found in these habitats provide a natural laboratory for instruction and
research.
Acknowledgements
We wish to thank the following individuals for sharing information about
the campus vegetation: Mr. Elias Golden, Head, Grounds and Maintenance,
Dr. Margaret C. Robinson, Dean, School of Sciences and Technology, Mr.
Risher Willard, Forester, Georgia Forestry Commission, for assistance
with tree identification, and Dr. Louise Golden, Associate Professor of
Humanities for editing. A 1993-1994 Title III Grant sponsored this
faculty and student research publication. Dr. Charles J. Elmore,
Director; Dr. John T. Wolfe, President
Authors
Matthew R. Gilligan, Ph.D., is a professor of Marine Sciences at
Savannah State University where he has served since 1980
Kelvin Austin who assisted with the project was a student in the Marine
Biology degree program at Savannah State University. His research
included library research, interviews, and field trips with University
and community experts.
Clara Aguero, M.F.A., was Director of Archives and Associate Professor
of Fine Arts at Savannah State University. She served as project
director for Archives publications and lectures.
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