Lm. Dowling et al., CARBON ISOTOPIC COMPOSITION OF HYDROCARBONS IN OCEAN-TRANSPORTED BITUMENS FROM THE COASTLINE OF AUSTRALIA, Organic geochemistry, 23(8), 1995, pp. 729-737
Bitumens stranding along the coastlines of the Northern Territory, Wes
tern Australia, South Australia, Victoria and Tasmania often have biom
arker signatures which closely match those of oils of S.E. Asian origi
n. A suite of these bitumens was studied to determine the isotopic sig
natures of their alkanes and to compare them to similar oils from the
Central Sumatra Basin. Saturated hydrocarbons were separated into a fr
action containing n-alkanes and isoalkanes and one containing the mult
ibranched/cyclic components using adduction into silicalite. Gas chrom
atography-isotope ratio mass spectrometry (GC-IRMS) of the n-alkanes r
evealed delta(13)C signatures covering a wide range of values from -25
.5 parts per thousand to -29 parts per thousand PDB but generally fall
ing between those of the botryococcane-containing Minas and Duri oils
from the Central Sumatra Basin. n-Alkanes of the Minas oil are 3-4 par
ts per thousand lighter than their Duri counterparts. The isotopic com
positions of pristane and phytane cover a similar range, delta(13)C =
-24 parts per thousand to -27 parts per thousand. Botryococcane is con
sistently heavy with delta(13)C values in the range -11 to -14 parts p
er thousand. One bitumen sample with no botryococcane but abundant bic
adinanes showed n-alkane delta(13)C values in the range -28 to -29 par
ts per thousand, at the light extreme for waxy bitumens in our sample
suite. Sample to sample differences in carbon isotopic signatures of n
-alkanes are attributed mainly to variations in primary source, with w
eathering and biodegradation as minor causes. Instances of low precisi
on for replicate analyses (+/- 2 parts per thousand) are caused by the
relative abundance of co-eluting isoalkanes. Overall, the isotopic pa
tterns of waxy bitumens from the Australian coastline provide independ
ent confirmation of their similarity to Central Sumatran lacustrine oi
ls. On the other hand, asphaltic bitumens from the southern Australian
coastline are isotopically light with n-alkane delta(13)C values in t
he range -31.5 to -33 parts per thousand. This distinctive feature may
assist identification of their source.