Faunistic assemblage of the Kroměříž Formation in Litenčice locality (Carpathian Foredeep, Central Moravia)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F46747885%3A24510%2F20%3A00009444" target="_blank" >RIV/46747885:24510/20:00009444 - isvavai.cz</a>

Výsledek na webu

<a href="https://journals.muni.cz/gvms/article/viewFile/13582/11701" target="_blank" >https://journals.muni.cz/gvms/article/viewFile/13582/11701</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5817/GVMS2020-13582" target="_blank" >10.5817/GVMS2020-13582</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Faunistic assemblage of the Kroměříž Formation in Litenčice locality (Carpathian Foredeep, Central Moravia)

Popis výsledku v původním jazyce

The fossil assemblages of the foraminifers, bryozoans, molluscs, corals, decapods, sharks and teleosteans were analysed from the Litenčice sand pit in the middle part of the Carpathian Foredeep. The section can be assigned to the Karpatian Stage of the Central Paratethys regional stratigraphy (uppermost Lower Miocene) on the basis of species Uvigerina graciliformis Papp et Turn., Lampanyctus carpaticus (Brz.) and Agapilia pachii (Hoern.). Rich and diversified assemblages indicate mainly shallow water marine environment. Foraminifers and molluscs indicate salinity perturbations. Bryozoans and also molluscs document environment with relatively high dynamics and depth of water about 100 m. Foraminifers, fishes and sharks represent deeper water taxa and indicate a possible reworking of shallow-water elements. The studied sands and gravels of the Holešov Member of the Kroměříž Formation are interpreted as sediments of gravitational currents, more precisely dense turbidity currents (high-density turbidity currents) in the sense of Lowe (1982). The deposition environment can probably be placed on the submarine slope of the coarse-grained delta of the Gilbert type (so-called foresets). This study provided evidence of a number of fossil groups that occur at the site.

Název v anglickém jazyce

Faunistic assemblage of the Kroměříž Formation in Litenčice locality (Carpathian Foredeep, Central Moravia)

Popis výsledku anglicky

The fossil assemblages of the foraminifers, bryozoans, molluscs, corals, decapods, sharks and teleosteans were analysed from the Litenčice sand pit in the middle part of the Carpathian Foredeep. The section can be assigned to the Karpatian Stage of the Central Paratethys regional stratigraphy (uppermost Lower Miocene) on the basis of species Uvigerina graciliformis Papp et Turn., Lampanyctus carpaticus (Brz.) and Agapilia pachii (Hoern.). Rich and diversified assemblages indicate mainly shallow water marine environment. Foraminifers and molluscs indicate salinity perturbations. Bryozoans and also molluscs document environment with relatively high dynamics and depth of water about 100 m. Foraminifers, fishes and sharks represent deeper water taxa and indicate a possible reworking of shallow-water elements. The studied sands and gravels of the Holešov Member of the Kroměříž Formation are interpreted as sediments of gravitational currents, more precisely dense turbidity currents (high-density turbidity currents) in the sense of Lowe (1982). The deposition environment can probably be placed on the submarine slope of the coarse-grained delta of the Gilbert type (so-called foresets). This study provided evidence of a number of fossil groups that occur at the site.

Druh

J_SC - Článek v periodiku v databázi SCOPUS

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2020

Kód důvěrnosti údajů

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

Název periodika

Geological Research in Moravia and Silesia

ISSN

1212-6209

e-ISSN

—

Svazek periodika

27

Číslo periodika v rámci svazku

44228

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

8

Strana od-do

45-53

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-85103312070