Carboniferous limestone boulder from the Badenian clastics
(Carpathian Foredeep, Czech Republic): A useful data source on
the Palaeozoic of the Moravosilesian Basin

J 2022

Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin

WEINER, Tomáš; Hedvika WEINEROVÁ; Michal MERGL; Jiří KALVODA; Růžena GREGOROVÁ et. al.

Základní údaje

Originální název

Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin

Autoři

WEINER, Tomáš; Hedvika WEINEROVÁ; Michal MERGL; Jiří KALVODA (203 Česká republika, domácí) a Růžena GREGOROVÁ

Vydání

Bulletin of Geosciences, Praha, Czech Geological Survey, 2022, 1214-1119

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.900

Kód RIV

RIV/00216224:14310/22:00127360

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.3140/bull.geosci.1851

UT WoS

000809811300003

EID Scopus

2-s2.0-85132176398

Klíčová slova anglicky

Badenian; Carpathian Foredeep; Tournaisian; Moravian Karst; brachiopods; trilobites; microfacies

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 6. 12. 2022 15:20, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

The 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.

Citovat

WEINER, Tomáš; Hedvika WEINEROVÁ; Michal MERGL; Jiří KALVODA a Růžena GREGOROVÁ. 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. Praha: Czech Geological Survey, 2022, roč. 97, č. 2, s. 179-201. ISSN 1214-1119. Dostupné z: https://doi.org/10.3140/bull.geosci.1851.

@article{2237622,
   author = {Weiner, Tomáš and Weinerová, Hedvika and Mergl, Michal and Kalvoda, Jiří and Gregorová, Růžena},
   article_location = {Praha},
   article_number = {2},
   doi = {https://doi.org/10.3140/bull.geosci.1851},
   keywords = {Badenian; Carpathian Foredeep; Tournaisian; Moravian Karst; brachiopods; trilobites; microfacies},
   language = {eng},
   issn = {1214-1119},
   journal = {Bulletin of Geosciences},
   title = {Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin},
   url = {http://www.geology.cz/bulletin/contents/art1851#},
   volume = {97},
   year = {2022}
}

TY  - JOUR
ID  - 2237622
AU  - Weiner, Tomáš - Weinerová, Hedvika - Mergl, Michal - Kalvoda, Jiří - Gregorová, Růžena
PY  - 2022
TI  - Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin
JF  - Bulletin of Geosciences
VL  - 97
IS  - 2
SP  - 179-201
EP  - 179-201
PB  - Czech Geological Survey
SN  - 12141119
KW  - Badenian
KW  - Carpathian Foredeep
KW  - Tournaisian
KW  - Moravian Karst
KW  - brachiopods
KW  - trilobites
KW  - microfacies
UR  - http://www.geology.cz/bulletin/contents/art1851#
N2  - The 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.
ER  -

WEINER, Tomáš; Hedvika WEINEROVÁ; Michal MERGL; Jiří KALVODA a Růžena GREGOROVÁ. Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin. \textit{Bulletin of Geosciences}. Praha: Czech Geological Survey, 2022, roč.~97, č.~2, s.~179-201. ISSN~1214-1119. Dostupné z: https://doi.org/10.3140/bull.geosci.1851.

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