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dc.contributor.authorWeiner, Tomáš
dc.contributor.authorWeinerová, Hedvika
dc.contributor.authorMergl, Michal
dc.contributor.authorKalvoda, Jiří
dc.contributor.authorGregorová, Růžena
dc.date.accessioned2022-08-29T13:02:26Z-
dc.date.available2022-08-29T13:02:26Z-
dc.date.issued2022
dc.identifier.citationWEINER, T. WEINEROVÁ, H. MERGL, M. KALVODA, J. GREGOROVÁ, R. Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin. Bulletin of Geosciences, 2022, roč. 97, č. 2, s. 179-201. ISSN: 1214-1119cs
dc.identifier.issn1214-1119
dc.identifier.uri2-s2.0-85132176398
dc.identifier.urihttp://hdl.handle.net/11025/49409
dc.format23 s.cs
dc.format.mimetypeapplication/pdf
dc.language.isoenen
dc.publisherCzech Geological Surveyen
dc.relation.ispartofseriesBulletin of Geosciencesen
dc.rights© Czech Geological Surveyen
dc.titleCarboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basinen
dc.typečlánekcs
dc.typearticleen
dc.rights.accessopenAccessen
dc.type.versionpublishedVersionen
dc.description.abstract-translatedThe lower Badenian basal and marginal clastics of the Carpathian Foredeep represent a useful source of information on the Palaeozoic units of the Moravosilesian Basin (Bohemian Massif). This study addresses in detail a Tournaisian limestone boulder from a locality near Kučerov village. Foraminifers indicate a narrow interval within the Mississippian Foraminifer Zone 8, characterized by the co-occurence of Darjella monilis Malakhova, 1964 and Eoparastaffella ex. gr. vdovenkoae Devuyst & Kalvoda, 2007. Fourteen recorded brachiopod taxa include: markedly predominant chonetidines, represented by Megachonetes zimmermanni (Paeckelmann, 1930) and other rugosochonetids; less frequent strophomenides (Leptagonia M’Coy, 1844) and orthotetides (Pulsiidae, Schuchertellidae); and rather rare spiriferides, athyrides?, orthides and productidines. The brachiopod fauna is generally close to associations known from other European areas. Trilobites are represented by the genus Cummingella Reed, 1942. The specimens recorded do not match the species previously known from the Czech Republic and the morphological features preserved suggest similarity with taxa from other European areas (e.g. Belgium, Poland). The microfacies correspond to floatstone with a packstone/grainstone matrix and contain crinoids, peloids, foraminifers, intraclasts, cortoids, moravamminids, algae and other allochems. Based on microfacies and foraminifer data, the boulder might originate in the limestone succession of the Líšeň Formation in the vicinity of Mokrá or in the limestone olistoliths in the siliciclastic Culm facies. Accordingly, at least some of the dark grey limestone clasts at the studied locality correspond to the Carboniferous and not only to the Devonian as previously assumed.en
dc.subject.translatedBadenianen
dc.subject.translatedCarpathian Foredeepen
dc.subject.translatedTournaisianen
dc.subject.translatedMoravian Karsten
dc.subject.translatedbrachiopodsen
dc.subject.translatedtrilobitesen
dc.subject.translatedmicrofaciesen
dc.identifier.doi10.3140/bull.geosci.1851
dc.type.statusPeer-revieweden
dc.identifier.document-number809811300003
dc.identifier.obd43936188
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