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Chapter 3 - Natural Resources - Marine Corps Base Camp Pendleton

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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

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