A. Behrens et al., Molecular characterization of organic matter in sediments from the Keg River formation (Elk Point group), western Canada sedimentary basin, ORG GEOCHEM, 29(8), 1998, pp. 1905-1920
Distributions of free and sulfur-bound biomarkers in organic-rich sediments
from the lower and upper Keg River formation (Elk Point group, western Can
ada) reveal deposition of these sediments under reducing conditions, in agr
eement with the geological data. The predominance of aryl isoprenoids of Ch
lorobiaceae origin indicates that photic zone anoxia occurred during time o
f deposition. A series of novel aryl isoprenoids with a carboxylic acid fun
ction was identified by GC-MS and the structure of the predominant 3-methyl
-5-(2',3',6'-trimethylphenyl)pentanoate was proven by synthesis of an authe
ntic standard. The occurrence of these acids gives evidence that oxidative
breakdown at least partially accounts for the diagenetic fate of aromatic c
arotenoids. Li/EtNH2 desulfurization of two kerogen concentrates yielded on
ly low amounts of sulfur-bound hydrocarbons, and suggests that either sulfu
r sequestration was not a predominant process or, more probably, that a maj
or part of the hydrocarbons, initially sulfurized, were released upon matur
ation, giving further evidence that (poly)sulfide bonds are cleaved at rela
tively low levels of thermal stress. (C) 1998 Elsevier Science Ltd. All rig
hts reserved.