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The significant features of the chemical changes that were observed<br />

included a marked decrease in the proportion of n-alkanes relative to<br />

isoprenoid hydrocarbons, the transient occurrence of an increase in<br />

unresolved hydrocarbons within the first year following the AMOCO CADIZ<br />

spillage, and the decreased importance of unsubstituted polynuclear<br />

aromatic hydrocarbons relative to dibenzothiophenes and the <strong>com</strong>parable<br />

or substituted forms of the polynuclear aromatic hydrocarbons (Figs. 2<br />

and 3).<br />

The In vitro hydrocarbon biodegradation experiments confirmed the<br />

fact that the indigenous microbial populations were capable of rapid and<br />

extensive degradation of Arabian crude oil. Much greater rates of<br />

biodegradation were observed in agitated <strong>com</strong>pared to flow through<br />

experiments (Figs. 4-9). Both the in vitro experiments and the analysis<br />

of field experiments support the hypothesis that mixing energy has a<br />

very significant effect on the rates of hydrocarbon biodegradation.<br />

Rates of biodegradation appear to be environmentally influenced by the<br />

turbulence of mixing which can ensure a continued supply of nutrients<br />

and oxygen as well as dispersing the oil so as to establish a favorable<br />

surface area to volume ratio for rapid microbial hydrocarbon<br />

biodegradation. The similarity of changes, observed in the <strong>com</strong>position<br />

of the hydrocarbon mixture i_n vitro <strong>com</strong>pared to the analysis of field<br />

samples also suggests that nutrients were not a limiting factor that<br />

determined the rates of hydrocarbon biodegradation.<br />

The analysis of the polar fractions from the iri vitro experiments<br />

showed some surprising results (Table 21). There was a lack of<br />

oxygenated aromatic <strong>com</strong>pounds. It had been predicted that there would<br />

be a greater accumulation of polar products from aromatic biodegradation<br />

since less CO was being produced than from aliphatic biodegradation<br />

where a significant proportion of the hydrocarbon that was biodegraded<br />

was released as CO . There were significant accumulations of polar<br />

<strong>com</strong>pounds that appear to be biodegradation products of aliphatic<br />

hydrocarbons, especially as C.,-C „ acids. Interestingly, the major<br />

polar products included unsaturated acids. As a rule, the predominant<br />

biochemical pathway for the biodegradation of straight chained<br />

hydrocarbons does not involve the formation of unsaturated <strong>com</strong>pounds,<br />

although a biochemical pathway has recently been elucidated for some<br />

bacteria that does introduce a double bond into the hydrocarbon. It<br />

appears that the microbial populations indigenous to the sediment of the<br />

Brittany Coast possess such a biochemical capability.<br />

18

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