A lacustrine record of the early stage of the Miocene Climatic Optimum in Central Europe from the Most Basin, Ohre (Eger) Graben, Czech Republic
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F14%3A00437534" target="_blank" >RIV/67985831:_____/14:00437534 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985530:_____/14:00437534 RIV/61388980:_____/14:00437534
Výsledek na webu
<a href="http://dx.doi.org/10.1017/S0016756813001052" target="_blank" >http://dx.doi.org/10.1017/S0016756813001052</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1017/S0016756813001052" target="_blank" >10.1017/S0016756813001052</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
A lacustrine record of the early stage of the Miocene Climatic Optimum in Central Europe from the Most Basin, Ohre (Eger) Graben, Czech Republic
Popis výsledku v původním jazyce
This study reports on a similar to 150 mthick macrofossil-barren sequence of siliciclastic sediments from a Burdigalian age (Early Miocene) freshwater lake. The lake was located within an incipient rift system of the Most Basin in the Ohre (Eger) Graben,which was part of the European Cenozoic Rift System, and had an original area of approximate to 1000 km(2). Sediments from the HK591 core that cover the entire thickness of the lake deposits and some of the adjacent stratigraphic units were analysed byX-ray fluorescence spectroscopy (a proxy for element composition) and magnetic polarity measurement. The element proxies were subjected to frequency analysis, which provided estimated sedimentation rates, and allowed for sediment dating by magnetostratigraphy and orbital tuning of the age model. Based on the resulting age model and the known biostratigraphy, the lake was present between 17.4 and 16.6 Ma, which includes the onset of the Miocene Climatic Optimum in the latest Early Miocene
Název v anglickém jazyce
A lacustrine record of the early stage of the Miocene Climatic Optimum in Central Europe from the Most Basin, Ohre (Eger) Graben, Czech Republic
Popis výsledku anglicky
This study reports on a similar to 150 mthick macrofossil-barren sequence of siliciclastic sediments from a Burdigalian age (Early Miocene) freshwater lake. The lake was located within an incipient rift system of the Most Basin in the Ohre (Eger) Graben,which was part of the European Cenozoic Rift System, and had an original area of approximate to 1000 km(2). Sediments from the HK591 core that cover the entire thickness of the lake deposits and some of the adjacent stratigraphic units were analysed byX-ray fluorescence spectroscopy (a proxy for element composition) and magnetic polarity measurement. The element proxies were subjected to frequency analysis, which provided estimated sedimentation rates, and allowed for sediment dating by magnetostratigraphy and orbital tuning of the age model. Based on the resulting age model and the known biostratigraphy, the lake was present between 17.4 and 16.6 Ma, which includes the onset of the Miocene Climatic Optimum in the latest Early Miocene
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
—
Návaznosti výsledku
Projekt
<a href="/cs/project/GAP210%2F11%2F1357" target="_blank" >GAP210/11/1357: Libkovické vrstvy mosteckého souvrství: jezerní paleoenvironmentální archív burdigalu (spodní miocén)</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geological Magazine
ISSN
0016-7568
e-ISSN
—
Svazek periodika
151
Číslo periodika v rámci svazku
6
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
21
Strana od-do
1013-1033
Kód UT WoS článku
000343766600004
EID výsledku v databázi Scopus
—