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000057133 0247_ $$2DOI$$a10.1016/j.palaeo.2006.03.052
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000057133 084__ $$2WoS$$aGeography, Physical
000057133 084__ $$2WoS$$aGeosciences, Multidisciplinary
000057133 084__ $$2WoS$$aPaleontology
000057133 1001_ $$0P:(DE-Juel1)VDB3401$$aArmstroff, A.$$b0$$uFZJ
000057133 245__ $$aAromatic hydrocarbon biomarkers in terrestrial organic matter of Devonian to Permian age
000057133 260__ $$aAmsterdam [u.a.]$$bElsevier Science$$c2006
000057133 300__ $$a
000057133 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
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000057133 440_0 $$013362$$aPalaeogeography Palaeoclimatology Palaeoecology$$v240$$x0031-0182$$y1
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000057133 520__ $$aThis paper presents the results of a detailed study on the occurrence and distribution of alkylnaphthalenes and alkylphenanthrenes in 39 coal and sediment samples from the Late Palaeozoic containing predominantly terrestrial organic matter. Most of the samples represent the Euramerian flora realm and originate from locations beyond the Variscan front in Eastern, Northern and Central Europe, i.e. especially England and the Moscow Basin. The samples are of relatively low maturity (0.32 to 1.80% R-r) and consist mainly of mixtures of type III and II kerogen. Quantification of the C-0- to C-4-naphthalenes and the C-0- to C-4-phenanthrenes showed that these compound classes were highly abundant in all samples. Aromatic hydrocarbon maturity parameters in general are in good agreement with measured vitrinite reflectance values. 1,2,7-Trimethylnaphthalene, an assumed diagenetic product of oleanane type biomarkers was present in all investigated samples. This observation provides evidence that oleanane type lipids were biosynthesised by organisms predating the evolution of angiosperms or that assumed formation pathways for 1,2,7-trimethylnaphthalene are insecure. 1,2,8-Trimethylphenanthrene was significantly enriched in samples from the Permian and the one sample from the Devonian investigated in this study. The precursor(s) of 1,2,8-trimethylphenanthrene therefore may have been produced by organisms which were least abundant in the Carboniferous depositional environments represented by our samples. (c) 2006 Elsevier B.V. All rights reserved.
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000057133 65320 $$2Author$$aLate Palaeozoic
000057133 65320 $$2Author$$aterrestrial organic matter
000057133 65320 $$2Author$$aaromatic biomarkers
000057133 65320 $$2Author$$aalkylphenanthrenes
000057133 65320 $$2Author$$aalkylnaphthalenes
000057133 65320 $$2Author$$aage and source relationship
000057133 7001_ $$0P:(DE-HGF)0$$aWilkes, H.$$b1
000057133 7001_ $$0P:(DE-HGF)0$$aSchwarzbauer, J.$$b2
000057133 7001_ $$0P:(DE-HGF)0$$aLittke, R.$$b3
000057133 7001_ $$0P:(DE-HGF)0$$aHorsfield, B.$$b4
000057133 773__ $$0PERI:(DE-600)1497393-5$$a10.1016/j.palaeo.2006.03.052$$gVol. 240$$q240$$tPalaeogeography, palaeoclimatology, palaeoecology$$v240$$x0031-0182$$y2006
000057133 8567_ $$uhttp://dx.doi.org/10.1016/j.palaeo.2006.03.052
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