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Vol. 53 - Alaska Resources Library and Information Services

Vol. 53 - Alaska Resources Library and Information Services

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Ecological Vulnerability. Armstrong, et al. (1983b) discussed in detail<br />

the types <strong>and</strong> magnitudes of stress that could affect larvae, <strong>and</strong> also<br />

the spatial <strong>and</strong> temporal vulnerability of this stage. They criticized<br />

some assumptions about larval biology used in previous models to predict<br />

oil impact (e.g., Sonntag, et al. 1980), <strong>and</strong> updated biological information<br />

obtained through 1983 in order to better portray possible oil<br />

stress. <strong>Information</strong> on larvae obtained during the present study helps<br />

to substantiate conclusions made by Armstrong, et al. (1983b) <strong>and</strong><br />

improves a sense of the relationship between larval settlement <strong>and</strong> young<br />

juvenile distribution nearshore. Yet, the relative importance of<br />

nearshore, coastal domain larvae is not so clear given the higher<br />

offshore densities found over Bristol Bay in June 1983.<br />

This life history stanza still seems particularly susceptible to oil<br />

pollution given physiological, ecological <strong>and</strong> spatial characteristics of<br />

larvae. Data through 1982 indicate that a major portion of the larval<br />

population occurs along the 50 m isobath <strong>and</strong> probably is transported by<br />

long-shore currents to the northeast as hypothesized by Hebard (1959),<br />

Haynes (1974) <strong>and</strong> Armstrong, et al. (1983b). Although the frontal<br />

system depicted by Kinder <strong>and</strong> Schumacher (1981a) is not as well studied<br />

along the NAS as in upper Bristol Bay, its integrity might be such as to<br />

entrain subsurface oil at the front with resultant transport concurrent<br />

with larval crab. Cline, et al. (1981) concluded from methane profiles<br />

originating from Port Moller that material rarely penetrated more than<br />

20 km offshore <strong>and</strong> was mostly entrained shoreward of the 50 m front<br />

while moving to the northeast, thus substantiating the notion of a<br />

strong front in this region. While movement of oil as a surface film by<br />

winds results in extensive coverage within brief time periods in the<br />

models of Leendertse <strong>and</strong> Liu (1981) <strong>and</strong> Pelto <strong>and</strong> Manen (1983), mixing<br />

of oil into the water column along the 50 m isobath might pose a more<br />

serious threat to red king crab larvae along the NAS for 10-20 days<br />

after a spill.<br />

Larval distribution <strong>and</strong> abundance in April <strong>and</strong> June 1983 furnish<br />

new information on three points: 1) there is probably considerable<br />

411

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