More info for the terms:
cover,
rhizomeSea oats is an excellent dune builder and sand binder. It thrives in
areas where dune building is active [
23] and contributes to maintenance
of the dune in its position. Sea oats traps windblown sand, forming
mounds of sand which increase as the plant responds with increased
growth [
15]. It possesses an extensive root and rhizome system which
produces new growth following sand burial [
4].
Sea oats is well adapted to and dominates the most exposed areas of the
dune where soil moisture is low. It tolerates drought, salt spray, and
rapid sand burial. Maximum leaf elongation occurs at 12.8 percent soil
moisture. Stomates close and leaf elongation slows when soil moisture
falls below 8.5 percent. Plants do not wilt until soil moisture falls
below 1.2 percent. Once drought is relieved, sea oats can recover from
very negative water potentials. Excessive soil moisture from a high
water table or inundation has a greater negative effect on sea oats
growth than does low soil moisture. With waterlogging stress due to a
high water table, stomates close and there is reduced biomass
production. Inundation of roots for just a few days results in death of
the plant [
12].
Erosion of dunes is accelerated by grazing. When sand on the windward
slope is not anchored by sea oats and other vegetation it is carried
over the top by the wind and deposited on the lee side, resulting in
migrating or "marching" dunes. When overgrazing results in the loss of
dune vegetation and the subsequent loss of the stable dune system, a
wide, flat beachfront may develop. Then extremely high storm induced
tides may inundate the entire beachfront and erode the older,
well-established dune systems protecting the interior, as occurred on
Cumberland Island, Georgia in 1971. Grazing has transformed several of
the banks in North Carolina into barren islands of shifting sand. Dune
damage from grazing has also been reported from South Carolina, Texas,
and several islands along the Georgia coast [
16]. Vegetation on North
Padre Island, Texas, is still recovering from cattle grazing from 1850
to 1971, when it was discontinued [
1].
Sea oats is adversely affected when the dunes on which it grows are
altered by urban development, by the impact of off-road vehicles on
vegetation cover and compaction of soil, and by pollution of adjacent
waters by treated and untreated sewage, fertilization, and contaminants
from marinas, fish processing plants, and highways [
23].
Sea oats was grown under greenhouse conditions in Louisiana dune sand.
Addition of the macronutrients nitrogen, phosphorus, and potassium
resulted in significantly greater leaf-elongation rates, number of
stems, and aboveground biomass than in controls with no additions.
However, additions of the micronutrients iron, manganese, copper, and
zinc in conjunction with the macronutrients led to reduced leaf
elongation and number of stems compared to controls. Micronutrients
alone had no positive or negative effects [
13].
Sea oats seedlings were outplanted to Miami Beach, Florida, beaches to
enhance beach stability. When seedlings were inoculated with
vesicular-arbuscular (VAM) fungi there were increases in seedling growth
over those that were not inoculated. Root colonization by VAM fungi was
higher when the inoculum was already-colonized roots rather than spores
alone [
28].