0345077 - ÚSMH 2011 RIV NL eng J - Článek v odborném periodiku
Matysová, Petra - Rössler, R. - Götze, J. - Leichmann, J. - Forbes, G. - Tailor, E. - Sakala, J. - Grygar, Tomáš
Alluvial and volcanic pathways to silicified plant stems (Upper Carboniferous–Triassic) and their taphonomic and palaeoenvironmental meaning.
Palaeogeography, Palaeoclimatology, Palaeoecology. Roč. 292, 1/2 (2010), s. 127-143. ISSN 0031-0182. E-ISSN 1872-616X
Grant CEP: GA AV ČR IAA300460804
Grant ostatní: AV ČR(CZ) KJB301110704
Výzkumný záměr: CEZ:AV0Z30460519; CEZ:AV0Z40320502
Klíčová slova: Quartz * Moganite * Environment
Kód oboru RIV: DB - Geologie a mineralogie
Impakt faktor: 2.390, rok: 2010
Web výsledku:
http://dx.doi.org/10.1016/j.palaeo.2010.03.036DOI: https://doi.org/10.1016/j.palaeo.2010.03.036

Various permineralized plant stems from Carboniferous, Permian, and Triassic test localities around the world have been studied by imaging and analytical tools. Microscopic techniques, hot cathodoluminescence spectroscopy, X-ray diffraction and electron microprobe analyses served to characterize miscellaneous mineral matter present. Two main permineralization pathways were distinguished: fluvial (alluvial) one and different one controlled by volcanism. The fluvial silicification of plant stems proceeded in seasonally variable climate, i.e. these fossils are significant palaeoenvironmental indicators independently on their palaeobotanic evaluation.
Trvalý link: http://hdl.handle.net/11104/0186430