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Gschwend%20thesis.pdf

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CHAPTER 6. SUMRY AND CONCLUDING REMARKS<br />

The major objectives of this thesis were to identify and quantify<br />

vola tile organic compounds in seawater, and to deduce their sources,<br />

transformations ,and transport mechanisms. Two approaches have been<br />

taken to accomplish these goals. First, samples from 3 open-ocean regions,<br />

the Sargasso Sea, the western Equatorial Atlantic, and the upwelling region<br />

off Peru, were analyzed for volatiles, and correlations with ancillary<br />

data were sought. In the second approach, temporal variations of the<br />

concentrations of volatile organic compounds in coastal seawater were<br />

investigated and interpreted by comparison with those of known coastal<br />

processes.<br />

Open-Ocean Seawater<br />

Total volatile concentrations found in oligotrophic surface Sargasso<br />

Sea samples were only 10-30 ng/kg, while<br />

total concentrations in samples<br />

from the biologically productive upwelling region off Peru were about<br />

100 ng/kg.<br />

Pentadecane was found in surface seawater samples from all 3 regions,<br />

typically at lO-40 ng/kg. This compound was not derived from fossil fuel<br />

inputs as other homologues (e.g. nCi4.and nCi6) were present at only<br />

trace levels. Based on a calculation, it appeared that a phytoplankton<br />

source was impronable, as the literature suggest that these organisms do<br />

not contain sufficient amounts of pentadecane. A transformtion of the<br />

abundant fatty acid, hexadecanoic acid, to pentadecane by zooplankton, in<br />

a manner analogous to the production of pristane from phytanic acid, may<br />

have been the source of open-ocean pentadecane.<br />

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