Biomarker maturity indices have proven useful in petroleum exploration
to assess the thermal maturity of oils and sediments. However, their
application to deltaic petroleum systems is often hindered by source a
nd diagenetic interferences. Recently, we have described several new m
aturity indices based on the catagenetic products of the plant biopoly
mer polycadinene. These indices should be largely immune to biochemica
l effects during diagenesis, since little microbial activity will rema
in at temperatures sufficient to dissociate the polymer.Here we report
changes in five polycadinene-related maturity indices through a arine
-fluvio-deltaic depositional sequence in the South Sumatra Basin, Indo
nesia. The results are compared with the maturity required for oil gen
eration as estimated by kinetic modelling and with conventional maturi
ty indicators such as sterane epimerisation and the methyl phenanthren
e index. The data confirm that the polycadinene indices are less subje
ct to source and diagenetic interferences than those based on the ster
ane and aromatic hydrocarbon distributions. Values for several of the
indices have also been measured for 17 Tertiary oils from Southeast As
ia, Papua New Guinea, New Zealand and Australia. Contrary to an earlie
r report, the bicadinane maturity indicator (BMI-1) continues to chang
e into the oil window and hence may be useful in ranking the relative
maturity of oils as well as sediments. The BMI-1 values for two oils h
aving unusually low sterane maturities are normal, leading us to quest
ion whether the low sterane maturity of many Tertiary-age oils is due
to their source rocks having been heated more rapidly than those of ol
der oils. Copyright (C) 1996 Elsevier Science Ltd