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2008 Annual Monitoring Report (pdf 10.9MB) - Bolsa Chica ...

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<strong>Bolsa</strong> <strong>Chica</strong> Lowlands Restoration <strong>Monitoring</strong><br />

<strong>2008</strong> <strong>Annual</strong> <strong>Report</strong><br />

Salt Panne<br />

Salt panne in the Seasonal Ponds.<br />

The habitat covering the third largest area within the study area<br />

was unvegetated salt panne, primarily in the Seasonal Pond and<br />

Future Full Tidal Basin areas. These areas were historically<br />

subsided marsh plain inundated by seawater, but are currently<br />

inundated intermittently by primarily freshwater. These low<br />

permeability areas collect water during rainy months, and later<br />

dry by evaporation as conditions warm in spring and summer<br />

months. This leaves hypersaline conditions that are<br />

inhospitable to most marsh plants. Although pickleweed has<br />

colonized much of the salt panne areas or its margins, the areas<br />

lowest in elevation that pool water for extended periods remain<br />

unvegetated.<br />

Disturbed Salt Panne<br />

Due to the use of the salt panne habitat by various migratory birds,<br />

including western snowy plovers for nesting, it is relevant to call<br />

out large areas of salt panne that are disturbed. Generally, these<br />

areas are previously flat expanses that have been traversed by<br />

various trucks and equipment, primarily for contaminated sediment<br />

removal work. When disturbed during wet periods, this activity<br />

leaves the ground deeply rutted, less desirable to foraging and<br />

nesting birds, and of some concern in relation to harboring pests<br />

such as mosquitoes longer into the summer season. Disturbed salt<br />

panned made up only 3% of the total salt panne area.<br />

Disturbed salt panne in the Seasonal Ponds.<br />

Intertidal Sand Shoal<br />

This category refers to the depositional flood shoals present in the FTB inlet. The shoals were<br />

composed of unvegetated and unconsolidated sand that can be highly transitory in nature as they are<br />

chronically accreted and reworked by the tides and waves. Their mapped extent was fully dependent<br />

on the tidal elevation at the time of the aerial imagery collection. A more comprehensive assessment<br />

of the shoal is included in the bathymetric monitoring section of this report (see Section 2.2).<br />

Intertidal Mudflat<br />

This habitat included the unvegetated intertidal mudflats occurring below elevations at which vascular<br />

plant communities occur. This habitat occurred primarily on the borders of FTB, in portions of the<br />

Muted Pocket Marsh, and at the lower elevations of Rabbit Island where inundated salt marsh<br />

transitioned to mudflat after the opening of the inlet. Although the cordgrass bench on the east shore<br />

of the FTB is above the typical intertidal mudflat zone, it will also be mapped as intertidal mudflat<br />

until such time as marsh vegetation develops.<br />

Open Water<br />

Open water habitat included all tidal waters, all permanently inundated areas in the FTB, Muted Pocket<br />

Marsh, and Freeman Creek. Standing water in the Seasonal Ponds and FFTB areas were mapped as<br />

salt panne in consideration of their underlying, persistent substrate. This habitat covered the greatest<br />

acreage in <strong>2008</strong>, due to the large expanses of open water in the FTB. As with mudflat and sand shoal,<br />

its mapped extent was dependent on the tidal elevation at the time of the aerial imagery collection. In<br />

Merkel & Associates, Inc. 28

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