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The Ecology of Tijuana Estuary, California: An Estuarine Profile

The Ecology of Tijuana Estuary, California: An Estuarine Profile

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Table 4. Percent occurrence <strong>of</strong> the more abundant species in the transition from upland to<br />

wetland at the northernmost part <strong>of</strong> <strong>Tijuana</strong> <strong>Estuary</strong>. Data are from 0.25 rn2 circutar quadrats<br />

(numbers sampled in parentheses) taken per 40-cm elevation class (Zedler unpubl. data).<br />

Elevation classa<br />

1 2 3 4 5 6 7 8 9 10 11<br />

Species (29) (99) (52) (25) (33) (30) (31) (34) (22) (33) (8)<br />

Artemisia<br />

californica<br />

Eriogonum<br />

fascicula tum<br />

Haplopappus<br />

venetus<br />

Rhus<br />

laurina<br />

A triplex<br />

semibacca ta<br />

Cressa<br />

truxillensis<br />

Dis tichlis<br />

spicata<br />

Frankenia<br />

grandifolia<br />

Lycium<br />

californicum<br />

Monanthochloe<br />

littoralis<br />

Salicornia<br />

subterminalis<br />

Salicornia<br />

virginica<br />

Limonium<br />

californicum<br />

Atriplex<br />

watsonii<br />

aElevation classes each included a 40-crn (16-inch) elevat~on range, they are numbered from low to h~gh<br />

elevation<br />

at the uppermost elevations and the taller<br />

cordgrass (Sparl~na folrosa) at the lowest<br />

elevations helps to designate higher and lower<br />

marsh habitats. Unlike the drought-deciduous<br />

coastal scrub species, the plants <strong>of</strong> the salt marsh<br />

grow through the summer and early fall.<br />

Presumably, th~s is because the wetland plants<br />

have access to moisture from tidal waters<br />

throughout the dry summer and fail<br />

Figure 1 8. <strong>The</strong> wandering skipper. Body 14 mm long.<br />

Nlclntire collection, copyright 1986 by Zedler.<br />

<strong>The</strong> hlgher salt marsh (F~gure 20) is one <strong>of</strong> the<br />

most complex wetland communities, because it is<br />

subject to aiternating envi:onmental extremes <strong>of</strong><br />

drought and inundation, because d~sturbance is<br />

frequent, and because its topography is sometimes<br />

mounded. Eighty-six mounds that ranged from 9 to<br />

57 cm in helght and 5.6 to 18.6 m rn diameter were<br />

characterized in 1984 (Cox and Zedler, in press)

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