B. Huseby et al., PORPHYRINS IN UPPER JURASSIC SOURCE ROCKS AND CORRELATIONS WITH OTHERSOURCE-ROCK DESCRIPTORS, Organic geochemistry, 25(5-7), 1996, pp. 273-294
The porphyrin content and composition in the extractable organic matte
r has been analysed in 13 Kimmeridge clay source rocks, spread from th
e north to the south of the Norwegian continental shelf. The samples a
re predominantly immature/early mature. The distribution of nickel and
vanadyl porphyrins within the samples is markedly different. Effects
of the thermal maturity on the composition of porphyrins is evaluated
and compared with biomarker parameters based on sterane and hopane rat
ios. Maturity is modelled using partial least-squares (PLS) multivaria
te analysis with T-max as a maturity indicator. Porphyrin parameters b
ased on the total carbon number distribution of DPEP and ETIO series f
rom the mass spectral data of the nickel and vanadyl porphyrin fractio
ns effectively describe the T-max of the samples with a better correla
tion than aliphatic biomarker ratios. Selected porphyrin and biomarker
ratios were used for principal component analysis (PCA) modelling, an
d found to describe two types of variation that may be indicative of t
he prevailing depositional redox conditions. (C) 1997 Elsevier Science
Ltd.