A. Pearson et Ti. Eglinton, The origin of n-alkanes in Santa Monica Basin surface sediment: a model based on compound-specific Delta C-14 and delta C-13 data, ORG GEOCHEM, 31(11), 2000, pp. 1103-1116
Delta C-14 and delta C-13 values were measured for individual long-chain n-
alkanes (C24-33) from Santa Monica Basin sediments. The data were then simu
lated using a three-component mixing model designed to represent the contri
butions of different sources. The three selected end members were petroleum
, modern plant wax, and shale-derived alkanes. The model was optimized to f
it the data and to determine the fractional contribution of each component.
The results indicated that petroleum accounted for 12% of the alkanes in 0
-2.5 cm sediment and 5% in 2.5-7.5 cm sediment. Modern plant waxes contribu
ted 80% (0-2.5 cm) and 87% (2.5-7.5 cm), and the remaining 8% of each sampl
e was attributed to the shale source. The C-14 concentration of the modern
terrestrial end member was also determined from the model. Delta C-14 value
s of similar to +235 parts per thousand for the 0-2.5 cm (post-bomb) horizo
n and similar to 0 parts per thousand for the 2.5-7.5 cm (pre-bomb) horizon
indicate that plant leaf waxes have a continental residence time of decade
s in the southern California region. (C) 2000 Elsevier Science Ltd. All rig
hts reserved.