Characterization of hydrocarbons in a subsurface oil-rich layer in the Sargasso Sea

The hydrocarbon composition of seawater samples collected within a subsurface oil-rich layer in the southwest North Atlantic Ocean (Sargasso Sea) during February–March, 1978, has been examined in detail. Chromatograms generated through gas chromatographs/mass spectrometry (GC/MS) analyses of saturated and aromatic hydrocarbons are characterized by a narrow unresolved envelope (UCM or unresolved complex mixture) containing isoprenoids as major resolved peaks, suggesting a petroleum source which has undergone moderate biodegradative weathering. Distributions of terpanes, steranes and polycyclic aromatic hydrocarbons corroborate the inferred fossil origin. Stable carbon isotopic compositions ( δ 13 C) suggest that the source of these hydrocarbons is enriched in 13C in comparison with most petroleums. The results support the previous suggestions (Harvey et al., 1979) that this layer is part of a massive submarine oil seep originating somewhere on the Venezuelan shelf, although its origin cannot be attributed to seepage of a specific oil formation.