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EPA's Vessel General Permit and Small Vessel General

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Anthropogenic threats<br />

Although commercial harvests historically lead to black abalone depletion, current harvesting is<br />

a small fraction of those levels. However, small removals are still significant in small<br />

populations.<br />

Although toxicology of abalone is poorly known, red abalone have demonstrated metabolic<br />

breakdown when exposed to the pesticide 3-trifluoromethyl-4-nitrophenol (Viant et al. 2001).<br />

Silver, cadmium, <strong>and</strong> mercury are also known to bioaccumulate in abalone, likely from ingested<br />

algae (Huang et al. 2008). Update rates have been measured as 1.78 L g -1 d -1 for silver, 0.056 L<br />

g -1 d -1 for cadmium <strong>and</strong> 0.32 L g -1 d -1 for mercury, of which 58 to 83%, 33 to 59%, <strong>and</strong> 65 to<br />

78%, respectively, is assimilated. Abalone are known to bioaccumulate high levels of heavy<br />

metals in the presence of high environmental concentrations (Wang et al. 2009).<br />

Changes in sea surface temperatures have been suggested as a driving force in altering red<br />

abalone distribution in the past (Braje et al. 2009); it is unknown what affect, if any climate<br />

change may have on black abalone.<br />

Critical habitat<br />

On October 27, 2011, the NMFS designated critical habitat for black abalone This includes rocky<br />

areas from mean high water to six meters water depth in the Farallon, Channel, <strong>and</strong> Año Nuevo<br />

isl<strong>and</strong>s, as well as the California coastline from Del Mar Ecological Reserve south to<br />

Government Point (excluding some stretches, such as in Monterey Bay <strong>and</strong> between Cayucos<br />

<strong>and</strong> Montaña de Oros State Park) in northern <strong>and</strong> central California <strong>and</strong> between the Palos<br />

Verdes <strong>and</strong> Torrance border south to Los Angeles Harbor. These areas include primary<br />

constituent elements required by black abalone, such as rocky substrates to cling to, food<br />

resources (bacterial <strong>and</strong> diatom films, crustose coralline algae, <strong>and</strong> a source of detrital<br />

macroalgae), juvenile settlement habitat (rocky intertidal habitat containing crustose coralline<br />

algae <strong>and</strong> crevices or cryptic biogenic structures (e.g., urchins, mussels, chiton holes,<br />

conspecifics, anemones)), suitable water quality (temperature, salinity, pH, <strong>and</strong> other chemical<br />

characteristics necessary for normal settlement, growth, behavior, <strong>and</strong> viability of black<br />

abalone), <strong>and</strong> suitable nearshore circulation patterns (where sperm, eggs, <strong>and</strong> larvae are retained<br />

in the nearshore environment).<br />

Johnson’s seagrass<br />

Description of the species<br />

Johnson’s seagrass has only relatively recently been identified as a distinct species <strong>and</strong> therefore<br />

no historical distribution information is available (Eiseman <strong>and</strong> McMillan 1980).<br />

Distribution<br />

Current distribution includes lagoons along approximately 125 miles of southeastern Florida<br />

between Sebastian Inlet <strong>and</strong> north Biscayne Bay which means that Johnson’s seagrass has the<br />

most limited geographic distribution of any seagrass in the world (Kenworthy 1997). However,<br />

northern range extentions (likely temporary) have recently been observed (Virnstein <strong>and</strong> Hall<br />

199

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