A new method for identifying the origins of simple and complex hopanoids in sedimentary materials using stable isotope labelling with (CH4)-C-13 and compound specific stable isotope analyses
Zm. Crossman et al., A new method for identifying the origins of simple and complex hopanoids in sedimentary materials using stable isotope labelling with (CH4)-C-13 and compound specific stable isotope analyses, ORG GEOCHEM, 32(2), 2001, pp. 359-364
Forest soils were taken and incubated with C-13-labelled methane. The lipid
s from these soils were isolated using a Bligh Dyer extraction and fraction
ated. Simple hopanoids were present in the neutral fraction, while periodic
acid/sodium borohydride treatment of the total lipid extract released prim
ary alcohols from polyfunctionalised bacteriohopane derivatives. All hopano
ids were analysed by GC, GC/MS and GC/C/IRMS. Specific hopanoids, namely: d
iploptene, 17 beta (H), 21 beta (H)-homohopanol and 17 beta (H), 21 beta (H
)-bishomohopanol produced by methane oxidising bacteria were significantly
enriched in C-13 whilst others showed no enrichment. (C) 2001 Elsevier Scie
nce Ltd. All rights reserved.