... Although the organismic source is unknown, it has been speculated that these derivatives are formed via oxidation of the C-26 methyl group of the hopane skeleton followed by rearrangement and migration of the C-8ÀC-14 bond. In biodegraded oils from seeps in Pakistan, 8,14-seco-hopanes (191À196) were characterized as a homologous series of a diastereomeric ensemble of six isomers of configurations, 8βH,14αH,17α,21βH, 8βH,14αH,17β,21αH, 8αH,14βH,17α,21βH, 8αH,14αH,17α,21βH, 8αH,14αH,17β,21βH, and 8αH,14βH,17β,21βH [105] (Fig. 35). As these compounds seem to be highly bioresistant, and also occur in non-biodegraded Paleogene brown coal from the Zhoujing mine, Baise Basin, in 35 8,14-seco-Hopane diastereomers 8βH,14αH,17α,21βH-, 8βH,14αH,17β,21αH-, 8αH,14βH,17α,21βH-, 8αH,14αH,17α,21βH-, 8αH,14αH,17β,21βH-, 8αH,14βH,17β,21βH-191 to 8βH,14αH,17α,21βH-, 8βH,14αH,17β,21αH-, 8αH,14βH,17α,21βH-, 8αH,14αH,17α,21βH-, 8αH,14αH,17β,21βH-, 8αH,14βH,17β,21βH-196, and monoaromatic seco-hopane series 197-203 and 204-210 southern mainland China [106], these molecular fossils may either have a direct biological precursor or may have formed during early diagenesis. ...