Middle Pleniglacial pedogenesis on the northwestern edge of the Carpathian Basin: a multidisciplinary investigation of the Bíňa pedosedimentary section, SW Slovakia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F17%3A10364506" target="_blank" >RIV/00216208:11310/17:10364506 - isvavai.cz</a>

Výsledek na webu

<a href="http://www.bayceer.uni-bayreuth.de/geomorph2017/en/prog/bayconf/beitrag_detail.php?id_obj=15439" target="_blank" >http://www.bayceer.uni-bayreuth.de/geomorph2017/en/prog/bayconf/beitrag_detail.php?id_obj=15439</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Middle Pleniglacial pedogenesis on the northwestern edge of the Carpathian Basin: a multidisciplinary investigation of the Bíňa pedosedimentary section, SW Slovakia

Popis výsledku v původním jazyce

The Middle Pleniglacial on the northern hemisphere is characterized by millennial scale, frequent, and high amplitude environmental climatic shifts. In loess-paleosol sequences (LPSs) the transition from the Lower (MIS 4) to the Middle Pleniglacial (MIS 3) was accompanied by significant erosion events, as recorded in various terrestrial archives across Central Europe. As a result, potentially existing paleosol horizons of the particular period have been widely erased from the (LPSs) and only little is known about pedogenesis in this vast area. This study tries to fill this gap in our knowledge through studying a pedo-sedimentary record from Čata, a site situated in a relatively poorly investigated area on the north-western edge of the Carpathian Basin.

Název v anglickém jazyce

Middle Pleniglacial pedogenesis on the northwestern edge of the Carpathian Basin: a multidisciplinary investigation of the Bíňa pedosedimentary section, SW Slovakia

Popis výsledku anglicky

The Middle Pleniglacial on the northern hemisphere is characterized by millennial scale, frequent, and high amplitude environmental climatic shifts. In loess-paleosol sequences (LPSs) the transition from the Lower (MIS 4) to the Middle Pleniglacial (MIS 3) was accompanied by significant erosion events, as recorded in various terrestrial archives across Central Europe. As a result, potentially existing paleosol horizons of the particular period have been widely erased from the (LPSs) and only little is known about pedogenesis in this vast area. This study tries to fill this gap in our knowledge through studying a pedo-sedimentary record from Čata, a site situated in a relatively poorly investigated area on the north-western edge of the Carpathian Basin.

Druh

O - Ostatní výsledky

CEP obor

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OECD FORD obor

10508 - Physical geography

Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2017

Kód důvěrnosti údajů

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