Paleoreconstruction of ecological changes in filled up lake using subfossil chironomids - preliminary results from the Vihorlat Mts, Slovakia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F13%3A00066181" target="_blank" >RIV/00216224:14310/13:00066181 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Paleoreconstruction of ecological changes in filled up lake using subfossil chironomids - preliminary results from the Vihorlat Mts, Slovakia

Popis výsledku v původním jazyce

This study brings the preliminary results of paleorecostruction of ecological changes in history of paleolake based on subfossil chironomid head capsules. The study site, small filled up lake (area of 2.3 ha) in altitude of 820 m a. s. l., is located inthe Vihorlat Mountains, 20 km westwards from Ukraine boundary in the East of Slovakia (48 g. 54' 46" N, 22 g. 09' 52" E). The catchment of palaeolake (45 ha) is placed on SE slope of the Motrogon hill and covered dominantly by broad-leaved forest. The uppermost 3.2 m thick layer of the lake is filled by peat and macroremnants at present, bud lower limnic layer, which goes to the total depth of 11,3 m, consisting of different types of gyttja. For the pilot analysis we use the lowermost 7.9 m of limnic sediment, which was separated into 5 cm thick layers.

Název v anglickém jazyce

Paleoreconstruction of ecological changes in filled up lake using subfossil chironomids - preliminary results from the Vihorlat Mts, Slovakia

Popis výsledku anglicky

This study brings the preliminary results of paleorecostruction of ecological changes in history of paleolake based on subfossil chironomid head capsules. The study site, small filled up lake (area of 2.3 ha) in altitude of 820 m a. s. l., is located inthe Vihorlat Mountains, 20 km westwards from Ukraine boundary in the East of Slovakia (48 g. 54' 46" N, 22 g. 09' 52" E). The catchment of palaeolake (45 ha) is placed on SE slope of the Motrogon hill and covered dominantly by broad-leaved forest. The uppermost 3.2 m thick layer of the lake is filled by peat and macroremnants at present, bud lower limnic layer, which goes to the total depth of 11,3 m, consisting of different types of gyttja. For the pilot analysis we use the lowermost 7.9 m of limnic sediment, which was separated into 5 cm thick layers.

Druh

O - Ostatní výsledky

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

—

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

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

Rok uplatnění

2013

Kód důvěrnosti údajů

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