Trilobite assemblage of Calceola-bearing beds in Acanthopyge Limestone (Middle Devonian,Eifelian, Prague Basin, the Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F19%3A00000120" target="_blank" >RIV/00025798:_____/19:00000120 - isvavai.cz</a>

Výsledek na webu

<a href="http://fi.nm.cz/wp-content/uploads/2019/08/10_Budil.pdf" target="_blank" >http://fi.nm.cz/wp-content/uploads/2019/08/10_Budil.pdf</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2478/if-2019-0007" target="_blank" >10.2478/if-2019-0007</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Trilobite assemblage of Calceola-bearing beds in Acanthopyge Limestone (Middle Devonian,Eifelian, Prague Basin, the Czech Republic)

Popis výsledku v původním jazyce

The trilobite assemblage of Calceola-bearing beds in the upper part of Acanthopyge Limestone (Choteč Formation,Eifelian) in the Koněprusy area, the Czech Republic, is described. Together with occurrence of Calceola, it indicates absenceof significant palaeogeographic barriers restricting the distribution of the Rhenish-Type faunas in the Middle Devonian. Thegeneric composition of the gathered trilobite assemblage somewhat differs from typical Acanthopyge-Phaetonellus assemblagecharacteristic for the Acanthopyge Limestone facies in possible absence and/or very rare occurrence of Phaetonellus, and onlyinfrequent occurrence of Acanthopyge. Phacopid Chotecops cf. hoseri (Hawle et Corda, 1847) distinctly dominates; all othertaxa are rather rare. Important is an occurrence of scutelluids of the Scutellum sensu lato group (preservation of remains does notenable more precise determination) and Longiproetus(?). Trilobite remnants are generally poorly preserved and very fragmented(only minute shields are not affected), which support a high-dynamic, shallow-water original environment.

Název v anglickém jazyce

Trilobite assemblage of Calceola-bearing beds in Acanthopyge Limestone (Middle Devonian,Eifelian, Prague Basin, the Czech Republic)

Popis výsledku anglicky

The trilobite assemblage of Calceola-bearing beds in the upper part of Acanthopyge Limestone (Choteč Formation,Eifelian) in the Koněprusy area, the Czech Republic, is described. Together with occurrence of Calceola, it indicates absenceof significant palaeogeographic barriers restricting the distribution of the Rhenish-Type faunas in the Middle Devonian. Thegeneric composition of the gathered trilobite assemblage somewhat differs from typical Acanthopyge-Phaetonellus assemblagecharacteristic for the Acanthopyge Limestone facies in possible absence and/or very rare occurrence of Phaetonellus, and onlyinfrequent occurrence of Acanthopyge. Phacopid Chotecops cf. hoseri (Hawle et Corda, 1847) distinctly dominates; all othertaxa are rather rare. Important is an occurrence of scutelluids of the Scutellum sensu lato group (preservation of remains does notenable more precise determination) and Longiproetus(?). Trilobite remnants are generally poorly preserved and very fragmented(only minute shields are not affected), which support a high-dynamic, shallow-water original environment.

Druh

J_SC - Článek v periodiku v databázi SCOPUS

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název periodika

Fossil Imprint

ISSN

2533-4050

e-ISSN

—

Svazek periodika

75

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

13

Strana od-do

79-91

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-85073787787