L. Marynowski et al., Phenylnaphthalenes and polyphenyls in Palaeozoic source rocks of the Holy Cross Mountains, Poland, ORG GEOCHEM, 32(1), 2001, pp. 69-85
Source rocks from a marine depositional setting from Palaeozoic formations
in the Holy Cross Mountains region (Midlands, Poland) were analysed for aro
matics using capillary gas chromatography-mass spectrometry (GC-MS). The oc
currence of two novel series of aromatic hydrocarbons in these sediments, n
amely phenyl derivatives of fused ring polycyclic aromatic hydrocarbons (Ph
PAH) and polyphenyls (PPh), was established. Furthermore, the methyl deriva
tives of these compounds were also present. The chromatographic behaviour o
f the triaromatic members of the series, i.e. two isomers of phenylnaphthal
ene (1-PhN and 2-PhN) and three isomers of terphenyl (o-TrP, m-TrP and p-Tr
P) was evaluated using authentic standards. The isomeric composition of the
phenylnaphthalenes (PhNs) and terphenyls (TrPs) was found to depend on the
rmal maturity. In the lower maturity samples abundances of 1-PhN and o-TrP
are higher. Increase in sample maturity is indicated by an increase in the
relative abundance of 2-PhN as well as m-TrP and p-TrP. Three thermal matur
ity parameters of the organic matter based on the relative abundances of th
e PhN and TrP isomers are proposed: PhNR = 2-PhN/1PhN, TrP1 = p-TrP/o-TrP,
and TrP2 = (m-TrP + p-TrP)/o-TrP. In general their values positively correl
ate with the vitrinite reflectance (R-o) and MDR, while correlation of the
other biomarker maturity parameters such as the Ts/Tm ratio are less appare
nt. The compounds above are believed to be geochemical products from unknow
n precursors. A potential geochemical process of formation for the o-TrP is
proposed, and involves initial preservation of carbohydrates in sediments
through sulfur incorporation, further dehydration, cyclisation and aromatis
ation to respective furan and/or thiophene derivatives, and finally reducti
ve elimination of oxygen and sulfur in the furan and thiophene products, re
spectively. (C) 2001 Elsevier Science Ltd. All rights reserved.