Number of the records: 1  

Palaeontology, sedimentary environments and climatic indices of the Kloubouky horizon (Líně formation, Upper Pennsylvanian, Kladno-Rakovník basin, Czech Republic)

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    SYSNO ASEP0326292
    Document TypeC - Proceedings Paper (int. conf.)
    R&D Document TypeThe record was not marked in the RIV
    TitlePalaeontology, sedimentary environments and climatic indices of the Kloubouky horizon (Líně formation, Upper Pennsylvanian, Kladno-Rakovník basin, Czech Republic)
    Author(s) Šimůnek, Z. (CZ)
    Martínek, K. (CZ)
    Zajíc, Jaroslav (GLU-S) RID, SAI
    Drábková, J. (CZ)
    Mikuláš, Radek (GLU-S) RID, SAI
    Valentová, D. (CZ)
    Source TitleXXXII sympozjum geologia formacji weglonosnych Polski : materialy. - Kraków : Akademia górniczo-hutnicza im. S. Staszica, 2009 - ISBN 978-83-919850-5-9
    Pagess. 69-78
    Number of pages10 s.
    ActionSympozjum geologia formacji weglonosnych Polski /32./
    Event date22.04.2009-23.04.2009
    VEvent locationKraków
    CountryPL - Poland
    Event typeEUR
    Languageeng - English
    CountryPL - Poland
    KeywordsUpper Pennsylvanian ; palaeontology ; Kladno-Rakovník Basin (Czech Republic)
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAA300130703 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    AnnotationThe Klobuky Horizon yielded 38 plant species to date. Ferns are dominant plant group. Sphenopsids and medullosan pteridosperms are locally common. Only one species of Callistophytales was found. Cordaitalean leaves are common in few places only. Both conifers and lycopsids are very rare. This floral assemblage belongs to the Sphenophyllum angustifolium Zone. Fauna is represented by at least 15 aquatic species. Trace fossils are very rare at Klobuky. Sedimentary facies and processes include progradation of lacustrine near-shore sand bodies over offshore mudstones, swamp/coal sedimentation, deposition of laminated offshore lacustrine mudstones with variable silty and sandy volcanogenic admixture. Fossiliferous, finely laminated muddy limestones are interpreted as lacustrine offshore deposits. The increasing seasonality and protraction of dry periods at the end of the Stephanian is deduced. However, the Klobuky Horizon with a coal seam represents a longer humid period.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2012
Number of the records: 1  

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