Foraminifera as environmental proxies of the Middle Miocene (Early Badenian) sediments of the Central Depression (Central Paratethys, Moravian part of the Carpathian Foredeep)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15410%2F12%3A33142256" target="_blank" >RIV/61989592:15410/12:33142256 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.3140/bull.geosci.1299" target="_blank" >http://dx.doi.org/10.3140/bull.geosci.1299</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3140/bull.geosci.1299" target="_blank" >10.3140/bull.geosci.1299</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Foraminifera as environmental proxies of the Middle Miocene (Early Badenian) sediments of the Central Depression (Central Paratethys, Moravian part of the Carpathian Foredeep)

Popis výsledku v původním jazyce

Middle Miocene sediments of the Central Depression have been studied based on foraminifera with a view to characterize palaeoenvironmental conditions. Rock material from HV-5 Rybnicek core were used. Foraminiferal evidence indicates biostratigraphic range of the lower part of the Upper Lagenid Zone (Early Badenian-Langhian, Middle Miocene). The sediments originate from a deeper marine basin at the level of outer shelf with potential extension deeper into the bathyal realm. Bottom waters were well-oxygenated with a redox boundary a few centimeters from the sea floor which was colonized by sub- and dysoxic foraminifers. Palaeotemperature of marine water corresponds to the Miocene climatic optimum with short-time climatic oscillations of cooler climate.

Název v anglickém jazyce

Foraminifera as environmental proxies of the Middle Miocene (Early Badenian) sediments of the Central Depression (Central Paratethys, Moravian part of the Carpathian Foredeep)

Popis výsledku anglicky

Middle Miocene sediments of the Central Depression have been studied based on foraminifera with a view to characterize palaeoenvironmental conditions. Rock material from HV-5 Rybnicek core were used. Foraminiferal evidence indicates biostratigraphic range of the lower part of the Upper Lagenid Zone (Early Badenian-Langhian, Middle Miocene). The sediments originate from a deeper marine basin at the level of outer shelf with potential extension deeper into the bathyal realm. Bottom waters were well-oxygenated with a redox boundary a few centimeters from the sea floor which was colonized by sub- and dysoxic foraminifers. Palaeotemperature of marine water corresponds to the Miocene climatic optimum with short-time climatic oscillations of cooler climate.

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

<a href="/cs/project/GA205%2F09%2F0103" target="_blank" >GA205/09/0103: Mělkovodní ekosystémy středního miocénu Centrální Paratethydy: Sukcese a interakce anorganické a organické složky ekosystémů</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Bulletin of Geosciences

ISSN

1214-1119

e-ISSN

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Svazek periodika

87

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

12

Strana od-do

431-442

Kód UT WoS článku

000309157700002

EID výsledku v databázi Scopus

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