The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F21%3A00118753" target="_blank" >RIV/00216224:14310/21:00118753 - isvavai.cz</a>
Alternative codes found
RIV/60460709:41330/20:82253 RIV/61388980:_____/21:00522625 RIV/61989592:15310/21:73604795
Result on the web
<a href="https://doi.org/10.1007/s12549-019-00409-z" target="_blank" >https://doi.org/10.1007/s12549-019-00409-z</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s12549-019-00409-z" target="_blank" >10.1007/s12549-019-00409-z</a>
Alternative languages
Result language
angličtina
Original language name
The Devonian-Carboniferous boundary in the Moravian Karst (Czech Republic)
Original language description
The continuous and well-accessible Devonian-Carboniferous boundary successions of the Czech Republic are part of the Brunovistulian Unit, which belongs to the Variscan Rhenohercynian Zone of the Bohemian Massif. The well-studied sections, with almost continuous carbonate sedimentation, crop out in the Moravian Karst area and are characterised by carbonate turbidites (Lesní lom) and hemipelagic successions (Křtiny). In the Lesní lom quarry, a complete succession of conodont zones of the Devonian-Carboniferous boundary interval (Upper expansa, praesulcata, costatus-kockeli, kockeli, sulcata/kuehni, bransoni, duplicata zones) was documented in calciturbidites and can be correlated with coeval foraminiferal zones (Quasiendothyra kobeitusana, Quasiendothyra konensis and Tournayellina pseudobeata zones). The Hangenberg Crisis and its three phases can be well recognised both with lithological, biostratigraphical and geochemical approaches in the Lesní lom section. At Křtiny, the nodular limestones yielded conodonts of the Devonian-Carboniferous boundary interval, but missing protognathodid fauna hampered identification of the kockeli Zone. A stratigraphic gap covering the basal part of the sulcata/kuehni Zone or strong condensation can be inferred from the occurrence of the transitional morphotype Si. sulcata-bransoni at the base of this zone. The tested “Montpellier criterion” for the Devonian-Carboniferous boundary redefinition can be used only in the Lesní lom section, where the first Protognathodus kockeli occurs above the regressive Hangenberg Sandstone Event deposits.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10506 - Paleontology
Result continuities
Project
<a href="/en/project/GA19-17435S" target="_blank" >GA19-17435S: Palaeoclimatologic significance of Palaeozoic red pelagic carbonates: time specific facies or products of microbial activity?</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Palaeobiodiversity And Palaeoenvironments
ISSN
1867-1594
e-ISSN
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Volume of the periodical
101
Issue of the periodical within the volume
2
Country of publishing house
DE - GERMANY
Number of pages
13
Pages from-to
473-485
UT code for WoS article
000516244400001
EID of the result in the Scopus database
2-s2.0-85079706813