A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F16%3A00088007" target="_blank" >RIV/00216224:14310/16:00088007 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.quascirev.2016.04.001" target="_blank" >http://dx.doi.org/10.1016/j.quascirev.2016.04.001</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quascirev.2016.04.001" target="_blank" >10.1016/j.quascirev.2016.04.001</a>

Jazyk výsledku

angličtina

Název v původním jazyce

A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development

Popis výsledku v původním jazyce

Temperature reconstructions based on biotic proxies are rare for inland Europe around 49 degrees N. We analysed lake deposits in the Vihorlat Mts in eastern Slovakia. Chironomid head capsules were used to reconstruct mean July temperature (T-July), other proxies (diatoms, green algae, pollen, geochemistry) were used to reconstruct local environmental changes, such as epilimnetic total phosphorus concentrations (TP), lake level changes and development of surrounding vegetation. During the Younger Dryas (YD), temperature fluctuated between 7 and 11 degrees C, that agree with other palaeoclimate records in Europe. The site was somewhat colder than expected from the general south-to-north YD temperature gradient within Europe, possibly because of north-facing exposition. The warmer phases of the YD were characterised by low water level or even complete lake desiccation. At the Late-Glacial/Holocene transition T-July steeply increased from from 11 to 15.5 degrees C - the highest T-July for entire sequence.

Název v anglickém jazyce

A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49 degrees N in inland Europe compared with local lake development

Popis výsledku anglicky

Temperature reconstructions based on biotic proxies are rare for inland Europe around 49 degrees N. We analysed lake deposits in the Vihorlat Mts in eastern Slovakia. Chironomid head capsules were used to reconstruct mean July temperature (T-July), other proxies (diatoms, green algae, pollen, geochemistry) were used to reconstruct local environmental changes, such as epilimnetic total phosphorus concentrations (TP), lake level changes and development of surrounding vegetation. During the Younger Dryas (YD), temperature fluctuated between 7 and 11 degrees C, that agree with other palaeoclimate records in Europe. The site was somewhat colder than expected from the general south-to-north YD temperature gradient within Europe, possibly because of north-facing exposition. The warmer phases of the YD were characterised by low water level or even complete lake desiccation. At the Late-Glacial/Holocene transition T-July steeply increased from from 11 to 15.5 degrees C - the highest T-July for entire sequence.

Druh

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

CEP obor

EH - Ekologie – společenstva

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

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

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název periodika

QUATERNARY SCIENCE REVIEWS

ISSN

0277-3791

e-ISSN

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Svazek periodika

141

Číslo periodika v rámci svazku

June

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

18

Strana od-do

94-111

Kód UT WoS článku

000376699800008

EID výsledku v databázi Scopus

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