Subfossil chironomid head capsules of filled up shallow lake Jurský Šůr near Bratislava, Slovakia - preliminary results

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F11%3A00059036" target="_blank" >RIV/00216224:14310/11:00059036 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Subfossil chironomid head capsules of filled up shallow lake Jurský Šůr near Bratislava, Slovakia - preliminary results

Popis výsledku v původním jazyce

This project is focused on vegetation and environmental changes in the Western Carpathians (Slovakia) during Late Glacial and Holocene period. The aim of this project is research of peats and lake sediment by using various analyses like palynology, macroremains, chironomids and geochemistry. The nature reserve Jurský Šůr is situated NE from Bratislava city (48o14'N,17o14'E). This former lake (2.8x4.3km) is situated in Danube lowlands (128-130 m a.s.l.) and bordering on NW the hillslope of the Small Carpathians.The site is covered by alder carr and particularly drained by artificial channels. The lake sediments, covering Pleistocene gravel-sands, are composed of organic material, fen and gyttja, which sediment in several periods of different sedimentation influx. The both, fluvial and lacustrine environments occur during the history of this shallow lake. Sediments were sampled to the depth of 245cm by the Russian peat sampler.

Název v anglickém jazyce

Subfossil chironomid head capsules of filled up shallow lake Jurský Šůr near Bratislava, Slovakia - preliminary results

Popis výsledku anglicky

This project is focused on vegetation and environmental changes in the Western Carpathians (Slovakia) during Late Glacial and Holocene period. The aim of this project is research of peats and lake sediment by using various analyses like palynology, macroremains, chironomids and geochemistry. The nature reserve Jurský Šůr is situated NE from Bratislava city (48o14'N,17o14'E). This former lake (2.8x4.3km) is situated in Danube lowlands (128-130 m a.s.l.) and bordering on NW the hillslope of the Small Carpathians.The site is covered by alder carr and particularly drained by artificial channels. The lake sediments, covering Pleistocene gravel-sands, are composed of organic material, fen and gyttja, which sediment in several periods of different sedimentation influx. The both, fluvial and lacustrine environments occur during the history of this shallow lake. Sediments were sampled to the depth of 245cm by the Russian peat sampler.

Druh

O - Ostatní výsledky

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

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