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14,<br />

groups makes [2- C] -acetate metabolism a useful means of differentiating<br />

the importance of bacterial processes which ac<strong>com</strong>plish its oxidation<br />

to C0„ (sulfate reduction) or its conversion to CH, (methane<br />

production, see Fig. 1). [2- C]-acetate was metabolized only to C0„<br />

at all sites except in the surface layer of the oiled lie Grande site<br />

where small amounts of CH, were detected on one occasion (March,<br />

1979). This observation, however, was not repeated at later sampling<br />

dates. Rates of sulfate reduction were highest in the surface layer<br />

and decreased with depth in all sites (Fig. 8). Rates in the 0-3 cm<br />

intervals were higher in oiled <strong>com</strong>pared to control Aber mudflat sediments<br />

(p = .004). In the beach and salt marsh mudflat sediments , rates<br />

were higher in control sites than in oiled sites (p < .001). It is not<br />

possible, however, to attribute differences to the presence of AMOCO<br />

CADIZ oil since other differences between sites (e.g., amount of organic<br />

loading) could also explain differences in sulfate reduction.<br />

ABER ILDUT ILE GRANDE<br />

= 1<br />

'<br />

*<br />

SULFATE REDUCTION RATE (pmoles S04 mf'-day"<br />

Figure 8. Depth profiles for rates of sulfate reduction in oiled and<br />

control sediments. Bars indicate one standard deviation.<br />

To more directly observe the effect of oiling on microbial activities<br />

in sediments, AMOCO CADIZ mousse was added to lie Grande sediments,<br />

and activities <strong>com</strong>pared between mousse- treated and untreated<br />

sediments. Gas chromatograms of the saturate and aromatic fractions of<br />

this mousse are shown in Figures 9 and 10, respectively. These tracings<br />

can be <strong>com</strong>pared to fresh light Arabian Crude in Figures 9 and 10. In<br />

the saturate fraction of the mousse, no hydrocarbons below C-12 were<br />

detected. In the aromatic fraction all predominant <strong>com</strong>pounds were gone<br />

and only a UCM remained. Thus, extensive weathering of the low molecular<br />

weight <strong>com</strong>pounds in the mousse had occured before collection.<br />

Extensive biodegradation of aliphatic <strong>com</strong>pounds was not suggested as<br />

evidenced by the dominance of normal <strong>com</strong>pared to isoprenoid alkanes.<br />

177

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