Some perisphinctoid ammonites of the Stramberk Limestone and their dating with associated microfossils (Tithonian to Lower Berriasian, Outer Western Carpathians, Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F17%3A10237221" target="_blank" >RIV/61989100:27350/17:10237221 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/68145535:_____/17:00482221
Výsledek na webu
<a href="http://www.geologicacarpathica.com/browse-journal/volumes/68-6/article-860/" target="_blank" >http://www.geologicacarpathica.com/browse-journal/volumes/68-6/article-860/</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1515/geoca-2017-0038" target="_blank" >10.1515/geoca-2017-0038</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Some perisphinctoid ammonites of the Stramberk Limestone and their dating with associated microfossils (Tithonian to Lower Berriasian, Outer Western Carpathians, Czech Republic)
Popis výsledku v původním jazyce
The present contribution deals with the taxonomy of seven species of perisphinctoid ammonite from the Stramberk Limestone (Outer Western Carpathians, Czech Republic) deposited in Moravian-Silesian museums. The age of these studied ammonites is compared with that of index microfossils contained in the matrix adhering to or infilling the studied specimens. The ammonites document a stratigraphic range from earliest Tithonian to early Berriasian. In addition to taxonomy and new ontogenetic data on some species, we also present data on their palaeogeographic distribution. The occurrence of Subboreal himalayitids in the Stramberk Limestone of an early Berriasian age is determined by both the microfauna and accompanying ammonites, which indicate connection of the Silesian-part of the Tethyan Carpathian area with the Subboreal Russian Platform Basin. These records also suggest an early Berriasian age (Jacobi Chron) for the lowermost part of the Ryazanian stage in its type area.
Název v anglickém jazyce
Some perisphinctoid ammonites of the Stramberk Limestone and their dating with associated microfossils (Tithonian to Lower Berriasian, Outer Western Carpathians, Czech Republic)
Popis výsledku anglicky
The present contribution deals with the taxonomy of seven species of perisphinctoid ammonite from the Stramberk Limestone (Outer Western Carpathians, Czech Republic) deposited in Moravian-Silesian museums. The age of these studied ammonites is compared with that of index microfossils contained in the matrix adhering to or infilling the studied specimens. The ammonites document a stratigraphic range from earliest Tithonian to early Berriasian. In addition to taxonomy and new ontogenetic data on some species, we also present data on their palaeogeographic distribution. The occurrence of Subboreal himalayitids in the Stramberk Limestone of an early Berriasian age is determined by both the microfauna and accompanying ammonites, which indicate connection of the Silesian-part of the Tethyan Carpathian area with the Subboreal Russian Platform Basin. These records also suggest an early Berriasian age (Jacobi Chron) for the lowermost part of the Ryazanian stage in its type area.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10506 - Paleontology
Návaznosti výsledku
Projekt
<a href="/cs/project/GA16-09979S" target="_blank" >GA16-09979S: Integrované multidisciplinární studium hranice jura-křída v mořských sekvencích: příspěvek pro globální definici hranice</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2017
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geologica Carpathica
ISSN
1335-0552
e-ISSN
—
Svazek periodika
68
Číslo periodika v rámci svazku
6
Stát vydavatele periodika
SK - Slovenská republika
Počet stran výsledku
23
Strana od-do
583-605
Kód UT WoS článku
000417560700006
EID výsledku v databázi Scopus
—