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Gschwend%20thesis.pdf

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-139-<br />

This suggested an anthropogenic source related to summer recreational<br />

activities for these large inputs.<br />

An unknown ocmpound, probably an octatriene, was found in late<br />

February and March. This material<br />

may be related to the chemical<br />

attractant utilized by Fucus spp. (Phaeophyta) and may represent a<br />

biological signal.<br />

Naphthalenes were most abundant after an oil spill and in<br />

winter samples. Winter samples contained a greater abundance of naphtha-<br />

lene, relative to the methyl naphthalenes, than did summer samples; this<br />

suggests that more indirect sources are important in the winter and<br />

thereby allow fractionation during transport of these homologues.<br />

Pentadecane and heptadecane were the dominant n-alkanes observed.<br />

Separate large concentration increases for these compounds were found in<br />

the summer and the high "CPr" strongly suggests a biological source of<br />

these compounds. Benthic algae are abundant at this time of year, have<br />

been shown to contain these hydrocarbons (Youngblood et al., 1971;<br />

Youngblood and Blumer, 1973), and consequently have been identified as<br />

the probable sources.<br />

C6-CIO straight chain aldehydes were found in all samples year-<br />

round. These aldehydes, and longer chain homologs from Ci2-CI5' were<br />

greatly increased in abundance in the late winter. The coincidence with<br />

the Thalassiosira, nordenskioeldii bloom indicated that this phytoplankton,<br />

or oxidation of the organic matter produced by this diatom, was the source<br />

of these oxygenated volatiles.<br />

Dimethyl di-, tri-, and tetrasulfides were found in the coastal<br />

seawater. These polysulfides. may be formed by reaction of methyl<br />

mercaptan and elemental sulfur, or from polysulfide metabolites of marine<br />

organisms.

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