Early Berriasian Ammonites from the Štramberk Limestone in the Kotouč Quarry (Outer Western Carpathians, Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F13%3A86088280" target="_blank" >RIV/61989100:27350/13:86088280 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68145535:_____/13:00425944

Výsledek na webu

<a href="http://www.asgp.pl/sites/default/files/volumes/83_4_329_342.pdf" target="_blank" >http://www.asgp.pl/sites/default/files/volumes/83_4_329_342.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Early Berriasian Ammonites from the Štramberk Limestone in the Kotouč Quarry (Outer Western Carpathians, Czech Republic)

Popis výsledku v původním jazyce

Over 100 ammonites were collected from a block of bedded shallow-water Štramberk Limestone at a new location at the Kotouč Quarry, near Štramberk (Silesian Unit, Czech Republic). Berriaselline neocomitids, including Berriasella jacobi, B. oppeli, Tirnovella allobrogensis, T. cf. allobrogensis, Delpinella consanguinea, Pseudosubplanites cf. grandis and Malbosiceras cf. asper, are the most abdundant species in this ammonite association. The olcostephanitid, Spiticeras blancheti, is rare. The index speciesin this ammonite jacobi, occurs in large numbers. On the basis of the present study, the upper boundary of the stratigraphic range of the Štramberk Limestone in the type area is dated as early Berriasian (ammonite Berriasella jacobi Zone). Ammonites with ages younger than early Berriasian have never been found in the Štramberk area. The deposition of the Štramberk Limestone in the Štramberk area came to an end during that period.

Název v anglickém jazyce

Early Berriasian Ammonites from the Štramberk Limestone in the Kotouč Quarry (Outer Western Carpathians, Czech Republic)

Popis výsledku anglicky

Over 100 ammonites were collected from a block of bedded shallow-water Štramberk Limestone at a new location at the Kotouč Quarry, near Štramberk (Silesian Unit, Czech Republic). Berriaselline neocomitids, including Berriasella jacobi, B. oppeli, Tirnovella allobrogensis, T. cf. allobrogensis, Delpinella consanguinea, Pseudosubplanites cf. grandis and Malbosiceras cf. asper, are the most abdundant species in this ammonite association. The olcostephanitid, Spiticeras blancheti, is rare. The index speciesin this ammonite jacobi, occurs in large numbers. On the basis of the present study, the upper boundary of the stratigraphic range of the Štramberk Limestone in the type area is dated as early Berriasian (ammonite Berriasella jacobi Zone). Ammonites with ages younger than early Berriasian have never been found in the Štramberk area. The deposition of the Štramberk Limestone in the Štramberk area came to an end during that period.

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

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Annales Societatis Geologorum Poloniae

ISSN

0208-9068

e-ISSN

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Svazek periodika

83

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

14

Strana od-do

329-342

Kód UT WoS článku

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EID výsledku v databázi Scopus

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