Chapter 3 - Natural Resources - Marine Corps Base Camp Pendleton
Chapter 3 - Natural Resources - Marine Corps Base Camp Pendleton
Chapter 3 - Natural Resources - Marine Corps Base Camp Pendleton
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
Integrated <strong>Natural</strong> <strong>Resources</strong> Management Plan [March 2012 - Update]<br />
subject to wave action, and deposition and removal of sand and gravel. Foredunes are the<br />
first line of dunes subject to sand deposition, high winds, and salt deposition, but only<br />
rarely subject to wave action or overwash; backdunes may be stable (not subject to<br />
deposition or erosion by the wind) or moving (having sand deposited or removed). Where<br />
cliffs face the ocean, the exposure to high-winds and high salt deposition creates another<br />
distinctive habitat – coastal bluffs.<br />
On <strong>Camp</strong> <strong>Pendleton</strong>, the coastal strip is mostly a relatively narrow stretch of sandy beach<br />
lying below a typically steep bluff cut into poorly consolidated sediments of the coastal<br />
mesas.<br />
Foredunes on <strong>Camp</strong> <strong>Pendleton</strong>, consisting of shifting-sand substrate, are classified as<br />
southern foredune and are sparsely vegetated with plant cover ranging from 30% to 60%.<br />
On <strong>Base</strong>, this plant community is dominated primarily by Ambrosia chamissonis (beachbur,<br />
10% to 30% cover) and substantial populations of Abronia maritima (sand verbena),<br />
Carpobrotus chilensis (sea fig, nonnative), Cakile maritima (sea rocket, nonnative), and<br />
Camissonia cheiranthifolia suffruticosa (beach evening primrose) that cumulatively<br />
account for 5% to 15% of groundcover (Biosystems Analysis 1994). This community is<br />
estimated to occupy less than 25 ac on <strong>Base</strong>.<br />
The regularity and extent of tidal flushing, the magnitude and frequency of freshwater<br />
runoff, sedimentation rates, soil types, salinity, nutrient relations, and human uses all<br />
influence the structure of the coastal wetland systems of the <strong>Base</strong>’s estuaries and lagoons.<br />
Watershed flows and natural tidal prism are important factors in maintaining the viability<br />
of these wetlands. A strong<br />
correlation exists between the<br />
regularity of tidal flushing and<br />
the diversity and abundance of<br />
the flora and fauna present in<br />
coastal wetland habitats.<br />
Interruption of tidal flow has<br />
dynamic ecological effects and<br />
can greatly influence the<br />
distribution and abundance of<br />
organisms within these coastal<br />
wetlands; openings and closures<br />
of river and creek mouths are<br />
allowed to occur naturally on<br />
<strong>Base</strong> to maintain a sound<br />
balance of biodiversity within<br />
the ecosystems. Tidal<br />
circulation provides moisture<br />
during periods of low<br />
FIGURE 3-4.<br />
SANTA MARGARITA RIVER ESTUARY<br />
(PHOTO SOURCE: CAMP PENDLETON)<br />
precipitation typical of the southern California summer months. Nutrient concentrations,<br />
salinity, temperature, oxygen, strength of water currents, and light penetration all respond<br />
to the open or closed condition of river and creek mouths, allowing some species to<br />
flourish while others fade. For example, changes in these factors are stressful for many<br />
<strong>Chapter</strong> 3 – <strong>Natural</strong> <strong>Resources</strong> 3-13