Dj. Hou et al., Distribution and characterization of C-31 sterane from cretaceous sediments and oils, Songliao Basin, China, CHIN SCI B, 44(6), 1999, pp. 560-563
Relatively high abundance of C-31 steranes has been identified from cretace
ous source rocks and crude oils in the Songliao Basin, China. C-31 steranes
which occur as ten isomers were tentatively identified as 4, 22, 23, 23-te
trametyhlcholestane based on their retention time and mass spectrum. They b
ear a lower thermal stability and occur as important components in the imma
ture oils of Chaochang region because they have three-methyl groups in thei
r side chain. The relatively high abundance of C-31 steranes in the samples
can indicate the source input of some special algae in the brackish and sa
line environment. Therefore they can be used as very useful biomarkers for
organic facies analysis and oil correlation. Their biological source perhap
s related to the dinoflagellate such as G. foliaceum and P. foliaceum. The
gorgostanol are considered as possible precursors for the putative C-31 4-m
ethyl sterane which formed in the stage of diagenesis.