Number of the records: 1  

Early Middle Frasnian platform reef strata in the Moravian Karst interpreted as recording the atmospheric dust changes: the key to understanding perturbations in the punctata conodont zone

  1. 1.
    SYSNO ASEP0323037
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleEarly Middle Frasnian platform reef strata in the Moravian Karst interpreted as recording the atmospheric dust changes: the key to understanding perturbations in the punctata conodont zone
    TitleInterpretace časně středofrasnských vrstev útesových plošin v Moravském krasu ohledně záznamu změn v atmosférickém prachu: klíč k pochopení neobvyklých výkyvů uvnitř konodontové zóny punctata
    Author(s) Hladil, Jindřich (GLU-S) RID, SAI
    Koptíková, Leona (GLU-S) RID, SAI
    Galle, Arnošt (GLU-S) SAI
    Sedláček, Václav (GLU-S)
    Pruner, Petr (GLU-S) RID, SAI, ORCID
    Schnabl, Petr (GLU-S) RID, SAI, ORCID
    Langrová, Anna (GLU-S) RID, SAI
    Bábek, O. (CZ)
    Frána, Jaroslav (UJF-V)
    Hladíková, J. (CZ)
    Otava, J. (CZ)
    Geršl, M. (CZ)
    Source TitleBulletin of Geosciences. - : Česká geografická společnost - ISSN 1214-1119
    Roč. 84, č. 1 (2009), s. 75-106
    Number of pages32 s.
    Publication formwww - www
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsmineral dust ; platform reef ; stromatactis ; Devonian ; Alamo impact
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAAX00130702 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    IAA300130702 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    AV0Z10480505 - UJF-V (2005-2011)
    UT WOS000264709300009
    EID SCOPUS69349087815
    DOI10.3140/bull.geosci.1113
    AnnotationThe early Middle Frasnian stratigraphic interval was selected for this study in order to assess the contribution of atmospheric dust and to distinguish between the robust climatically driven anomalies and the potential distant effect of the Alamo impact. The methodology employed for undertaking this research was based on succession and combination of the following steps: biostratigraphy and facies analysis, magnetic susceptibility (MS), gamma-ray spectrometry (GRS), instrumental neutron activation analysis (INAA), and finally, separation and assessment of rare non-carbonate particles. The principal results are: refinement of the bow-shaped MS pattern for the E-MF, separation of climatically driven fluctuations from the catastrophic-event-triggered perturbations, defining the crisis and non-crisis duality in MS to eustasy relationships, estimates of Frasnian (Devonian) mineral dust burden, and correlation of stromatactis with reduced carbonate production.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2009
Number of the records: 1  

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