Upper Famennian and Lower Tournaisian sections of the Moravian Karst (Moravo-Silesian Zone, Czech Republic): a proposed key area for correlation of the conodont and foraminiferal zonations

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F15%3A33157350" target="_blank" >RIV/61989592:15310/15:33157350 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/15:00080643

Výsledek na webu

<a href="http://onlinelibrary.wiley.com/doi/10.1002/gj.2523/epdf" target="_blank" >http://onlinelibrary.wiley.com/doi/10.1002/gj.2523/epdf</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1002/gj.2523" target="_blank" >10.1002/gj.2523</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Upper Famennian and Lower Tournaisian sections of the Moravian Karst (Moravo-Silesian Zone, Czech Republic): a proposed key area for correlation of the conodont and foraminiferal zonations

Popis výsledku v původním jazyce

Foraminiferal and conodont faunas at the Devonian-Carboniferous (D-C) boundary in the southern part of the Moravian Karst (Czech Republic) were studied in different facies of the basin slope. The joint presence of foraminifers and conodonts in calciturbidites along with a positive C-13 excursion of the Hangenberg anoxic event enabled the high-resolution calibration of the late Famennian-early Tournaisian interval (Upper expansa-crenulata conodont zones). The conodont stratigraphic and biofacies succession reveals a strong correlation with other European areas. The Siphonodella sulcata morphotype (close to Group 1 sensu Kaiser and Corradini and nov. gen. nov. sp. 1 sensu Tragelehn) enters prior to the Hangenberg Event, which resembles Upper and Uppermost Famennian conodont successions from Franconia, Bavaria and Morocco. The diversification of the early siphonodellids takes place after the Hangenberg Event and after the protognathodid radiation. In terms of foraminiferal biostratigraphy

Název v anglickém jazyce

Upper Famennian and Lower Tournaisian sections of the Moravian Karst (Moravo-Silesian Zone, Czech Republic): a proposed key area for correlation of the conodont and foraminiferal zonations

Popis výsledku anglicky

Foraminiferal and conodont faunas at the Devonian-Carboniferous (D-C) boundary in the southern part of the Moravian Karst (Czech Republic) were studied in different facies of the basin slope. The joint presence of foraminifers and conodonts in calciturbidites along with a positive C-13 excursion of the Hangenberg anoxic event enabled the high-resolution calibration of the late Famennian-early Tournaisian interval (Upper expansa-crenulata conodont zones). The conodont stratigraphic and biofacies succession reveals a strong correlation with other European areas. The Siphonodella sulcata morphotype (close to Group 1 sensu Kaiser and Corradini and nov. gen. nov. sp. 1 sensu Tragelehn) enters prior to the Hangenberg Event, which resembles Upper and Uppermost Famennian conodont successions from Franconia, Bavaria and Morocco. The diversification of the early siphonodellids takes place after the Hangenberg Event and after the protognathodid radiation. In terms of foraminiferal biostratigraphy

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP210%2F11%2F1891" target="_blank" >GAP210/11/1891: Hranice devonu a karbonu v Evropě - multidisciplinární přístup</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geological Journal

ISSN

0072-1050

e-ISSN

—

Svazek periodika

50

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

22

Strana od-do

17-38

Kód UT WoS článku

000348761800002

EID výsledku v databázi Scopus

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