Current knowledge of ammonite assemblages from the Stramberk Limestone (Tithonian-lower Berriasian) at Kotout Quarry, Outer Western Carpathians (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F18%3A00495101" target="_blank" >RIV/68145535:_____/18:00495101 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S0195667117305487?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0195667117305487?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.cretres.2018.04.016" target="_blank" >10.1016/j.cretres.2018.04.016</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Current knowledge of ammonite assemblages from the Stramberk Limestone (Tithonian-lower Berriasian) at Kotout Quarry, Outer Western Carpathians (Czech Republic)

Popis výsledku v původním jazyce

Forty-two species of perisphinctoid ammonites from the Stramberk Limestone at Kotouc Quarry near Stramberk (Moravia, Czech Republic) have been taxonomically assessed since 2013. Some of these species are contained in old collections at various Moravian-Silesian museums, while others are in the collections of two of us (ZV and PS), all are from Kotouc Quarry. In view of the fact that the Stramberk Limestone usually lacks distinct bedding, the stratigraphical position (ammonite zones) of the taxa identified is derived from literature data. Ammonite species identified document the entire Tithonian to the lower Berriasian. One taxon of early Berriasian age is described as new, Neocosmoceras eliasi. The Tithonian ammonite assemblage, with the exception of the uppermost portion of that stage, is close to those on record from the Mediterranean bioprovince in adjacent countries. In the uppermost Tithonian, a cosmopolitan species, Substeueroceras koeneni, appears. In the lower Berriasian, in addition to Mediterranean representatives, taxa that are known from the Crimean Peninsula and, exceptionally, those from the Subboreal Russian Platform Basin, are present.

Název v anglickém jazyce

Current knowledge of ammonite assemblages from the Stramberk Limestone (Tithonian-lower Berriasian) at Kotout Quarry, Outer Western Carpathians (Czech Republic)

Popis výsledku anglicky

Forty-two species of perisphinctoid ammonites from the Stramberk Limestone at Kotouc Quarry near Stramberk (Moravia, Czech Republic) have been taxonomically assessed since 2013. Some of these species are contained in old collections at various Moravian-Silesian museums, while others are in the collections of two of us (ZV and PS), all are from Kotouc Quarry. In view of the fact that the Stramberk Limestone usually lacks distinct bedding, the stratigraphical position (ammonite zones) of the taxa identified is derived from literature data. Ammonite species identified document the entire Tithonian to the lower Berriasian. One taxon of early Berriasian age is described as new, Neocosmoceras eliasi. The Tithonian ammonite assemblage, with the exception of the uppermost portion of that stage, is close to those on record from the Mediterranean bioprovince in adjacent countries. In the uppermost Tithonian, a cosmopolitan species, Substeueroceras koeneni, appears. In the lower Berriasian, in addition to Mediterranean representatives, taxa that are known from the Crimean Peninsula and, exceptionally, those from the Subboreal Russian Platform Basin, are present.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10700 - Other natural sciences

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2018

Kód důvěrnosti údajů

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

Název periodika

Cretaceous Research

ISSN

0195-6671

e-ISSN

—

Svazek periodika

90

Číslo periodika v rámci svazku

October 2018

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

9

Strana od-do

185-203

Kód UT WoS článku

000442334000019

EID výsledku v databázi Scopus

2-s2.0-85046689049