001     57133
005     20161225180128.0
024 7 _ |2 DOI
|a 10.1016/j.palaeo.2006.03.052
024 7 _ |2 WOS
|a WOS:000241313800014
037 _ _ |a PreJuSER-57133
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Geography, Physical
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Paleontology
100 1 _ |a Armstroff, A.
|b 0
|u FZJ
|0 P:(DE-Juel1)VDB3401
245 _ _ |a Aromatic hydrocarbon biomarkers in terrestrial organic matter of Devonian to Permian age
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2006
300 _ _ |a
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|0 0
|2 EndNote
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Palaeogeography Palaeoclimatology Palaeoecology
|x 0031-0182
|0 13362
|y 1
|v 240
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a This 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.
536 _ _ |a Geosysteme - Erde im Wandel
|c P21
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK405
|x 0
588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a Late Palaeozoic
653 2 0 |2 Author
|a terrestrial organic matter
653 2 0 |2 Author
|a aromatic biomarkers
653 2 0 |2 Author
|a alkylphenanthrenes
653 2 0 |2 Author
|a alkylnaphthalenes
653 2 0 |2 Author
|a age and source relationship
700 1 _ |a Wilkes, H.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Schwarzbauer, J.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Littke, R.
|b 3
|0 P:(DE-HGF)0
700 1 _ |a Horsfield, B.
|b 4
|0 P:(DE-HGF)0
773 _ _ |a 10.1016/j.palaeo.2006.03.052
|g Vol. 240
|q 240
|0 PERI:(DE-600)1497393-5
|t Palaeogeography, palaeoclimatology, palaeoecology
|v 240
|y 2006
|x 0031-0182
856 7 _ |u http://dx.doi.org/10.1016/j.palaeo.2006.03.052
909 C O |o oai:juser.fz-juelich.de:57133
|p VDB
913 1 _ |k P21
|v Geosysteme - Erde im Wandel
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914 1 _ |a Nachtrag
|y 2006
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-V
|l Sedimentäre Systeme
|d 31.12.2006
|g ICG
|0 I:(DE-Juel1)VDB51
|x 1
970 _ _ |a VDB:(DE-Juel1)89878
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)ICG-5-20090406
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)ICG-5-20090406


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