Sur, a former late-glacial and Holocene lake at the westernmost margin of the Carpathians

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10140220" target="_blank" >RIV/00216208:11310/13:10140220 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61388980:_____/13:00397874 RIV/00216224:14310/13:00066341

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Sur, a former late-glacial and Holocene lake at the westernmost margin of the Carpathians

Popis výsledku v původním jazyce

There is a unique palaeolimnological record of the late-glacial and Holocene periods in the former lake Šúr near Bratislava in western Slovakia. The aim of this study was to reconstruct the development of the environment in the locality of the lake, including the gradual infilling of the lake. We reconstructed the development of the lake environment by combining results of a geochemical analysis with analyses of diatoms and plant macrofossils.We also carried out a pollen analysis to assess the changes in the surrounding terrestrial vegetation. The results reveal how the character of the lake has changed over time. At the peak of the glacial period, water flowed through the lake and deposited sand there. Later on the flowofwater through the lake ceasedand a vast oligotrophic lake developed. During the Holocene, the lake gradually became eutrophic. The pollen record contains evidence of the occurrence of woody species of broad-leaved forest in the late-glacial period in the Carpathians

Název v anglickém jazyce

Sur, a former late-glacial and Holocene lake at the westernmost margin of the Carpathians

Popis výsledku anglicky

There is a unique palaeolimnological record of the late-glacial and Holocene periods in the former lake Šúr near Bratislava in western Slovakia. The aim of this study was to reconstruct the development of the environment in the locality of the lake, including the gradual infilling of the lake. We reconstructed the development of the lake environment by combining results of a geochemical analysis with analyses of diatoms and plant macrofossils.We also carried out a pollen analysis to assess the changes in the surrounding terrestrial vegetation. The results reveal how the character of the lake has changed over time. At the peak of the glacial period, water flowed through the lake and deposited sand there. Later on the flowofwater through the lake ceasedand a vast oligotrophic lake developed. During the Holocene, the lake gradually became eutrophic. The pollen record contains evidence of the occurrence of woody species of broad-leaved forest in the late-glacial period in the Carpathians

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EF - Botanika

OECD FORD obor

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Projekt

<a href="/cs/project/GAP504%2F11%2F0429" target="_blank" >GAP504/11/0429: Gradienty prostředí, vegetační dynamika a krajinné změny v Západních Karpatech od pozdního glaciálu po současnost</a><br>

Návaznosti

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

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Preslia

ISSN

0032-7786

e-ISSN

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Svazek periodika

85

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

25

Strana od-do

239-263

Kód UT WoS článku

000325118300003

EID výsledku v databázi Scopus

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