The distributions of alkylated fluoren-9-ones and carbazoles, includin
g their benzo-and dibenzo- and/or naphtho-annellated derivatives, have
been investigated in rock extracts from a maturity sequence of Posido
nia Shales from the Hils Syncline of northwest Germany. The fluoren-9-
one and carbazole derivatives are quantitatively the most important co
mpound types in the low polar heterocompound fraction obtained from th
e Posidonia Shale bitumens by liquid chromatography. This fraction com
prises 9.3-27.5% of the total bitumen depending on maturity. The conce
ntration of the fluoren-9-ones in the bitumens systematically increase
s with increasing maturity. Generally, a trend of decreasing degree of
alkylation is observed with increasing maturity. However, at the mole
cular level, less systematic maturity-dependent variations are observe
d for the fluoren-9-one distributions than for the carbazole distribut
ions. A remarkable exception is the 1-ethylfluoren-9-one/(1-ethylfluor
en-9-one + 1,8-dimethylfluoren-9-one) ratio which linearly decreases o
ver the entire maturity range (0.48-1.45% R-r). Among the carbazoles,
dibenzo-and/or naphtho-annellated derivatives become more abundant at
higher maturity. An oxidation of fluorenes may be ruled out as the maj
or process for the formation of fluoren-9-ones since Posidonia Shale w
as deposited under anoxic conditions and fluorenes are not present in
high amounts even in samples of low maturity. The fluoren-9-ones may r
ather be produced by cyclisation reactions of suitable precursors in t
he organic matter. Particularly, 2-carboxybiphenyls could be transform
ed to fluoren-9-ones either catalysed by Lewis acids, e.g, clay minera
ls, or solely under the influence of higher temperatures. The constant
ratio of fluoren-9-ones and benzofluoren-9-ones suggests that selecti
ve formation/degradation and interconversion during maturation plays a
minor role. This seems to be different for the carbazoles where a sig
nificant influence of maturity on the distribution of derivatives with
different numbers of aromatic rings was observed. (C) 1998 Elsevier S
cience Ltd. All rights reserved.