001     57134
005     20161225222921.0
024 7 _ |2 DOI
|a 10.1016/j.palaeo.2006.03.053
024 7 _ |2 WOS
|a WOS:000241313800015
037 _ _ |a PreJuSER-57134
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 Wollenweber, J.
|b 0
|0 P:(DE-HGF)0
245 _ _ |a Characterisation of non-extractable macromolecular organic matter in Palaeozoic coals
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
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|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 Comprehensive organic-geochemical investigations were applied to Permian, Carboniferous and Devonian coals. The major goal of the investigation was to quantify differences in organic matter composition of the coals on a molecular level and to associate these differences with either i) primary composition of the precursor plant material, or ii) diagenetic processes related to burial and temperature increase or iii) evolutionary time trends.The pre-extracted samples were analysed by means of pyrolytic and chemical degradation techniques as well as FTIR spectroscopy. Additionally, Rock-Eval pyrolysis and organic petrography were used to obtain information on the bulk of the coal samples.The degradation analysis revealed a wide variety of individual compounds including n-alkanes, isoprenoids, polycylic aromatic compounds, fatty acids, alkylbenzenes, aromatic carboxylic acids and phenols. Relative concentrations of substances or compound groups were correlated with bulk parameters and age of the samples.Significant correlations of the chemical data were found out mainly for maturity parameters and maceral composition. Time depending changes in chemical composition were observed only to a minor extent. Thus, the rapid morphologic evolution of higher land plants in the Late Palaeozoic is not reflected in a significant way by the chemical composition of the non-extractable matter in the coal samples investigated. (c) 2006 Elsevier B.V. All rights reserved.
536 _ _ |a Geosysteme - Erde im Wandel
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588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a macromolecular organic matter
653 2 0 |2 Author
|a infrared spectra
653 2 0 |2 Author
|a Palaeozoic
653 2 0 |2 Author
|a plant evolution
653 2 0 |2 Author
|a thermal maturity
653 2 0 |2 Author
|a pyrolysis
653 2 0 |2 Author
|a chemical degradation
700 1 _ |a Schwarzbauer, J.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Littke, R.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Wilkes, H.
|b 3
|0 P:(DE-HGF)0
700 1 _ |a Armstroff, A.
|b 4
|u FZJ
|0 P:(DE-Juel1)VDB3401
700 1 _ |a Horsfield, B.
|b 5
|0 P:(DE-HGF)0
773 _ _ |a 10.1016/j.palaeo.2006.03.053
|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.2006.03.053
909 C O |o oai:juser.fz-juelich.de:57134
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913 1 _ |k P21
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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
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980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)ICG-5-20090406


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