Phenylnaphthalenes and polyphenyls in Palaeozoic source rocks of the Holy Cross Mountains, Poland

Citation
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
Citations number
61
Categorie Soggetti
Earth Sciences
Journal title
ORGANIC GEOCHEMISTRY
ISSN journal
01466380 → ACNP
Volume
32
Issue
1
Year of publication
2001
Pages
69 - 85
Database
ISI
SICI code
0146-6380(2001)32:1<69:PAPIPS>2.0.ZU;2-S
Abstract
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.