The aliphatic fraction of Shuicheng boghead is characterized by the mi
xed source inputs of microbes and higher plants. The products of micro
bial source inputs, i.e. C-21(-) n-alkanes, tricyclic terpanes, steran
es, single-methyl branched alkanes, isoprenoid alkanes except phytane
series, drimane series, tetracyclic terpanes and hopane type of triter
panes, amount to 52.4% of the aliphatic fraction, while hydrocarbons o
f higher plant source input, including C-22(+) alkanes and some sesqui
terpenoids, account for 32.2%. In addition, the phytane series of phot
oautotrophic chlorophyll source input just make up 7.0% of the fractio
n.