Holocene climatic events linked to environmental changes at Lake Komořany Basin, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F17%3A43895481" target="_blank" >RIV/60076658:12310/17:43895481 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/17:10366429 RIV/00216208:11620/17:10366429

Výsledek na webu

<a href="http://journals.sagepub.com/doi/10.1177/0959683616683250" target="_blank" >http://journals.sagepub.com/doi/10.1177/0959683616683250</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1177/0959683616683250" target="_blank" >10.1177/0959683616683250</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Holocene climatic events linked to environmental changes at Lake Komořany Basin, Czech Republic

Popis výsledku v původním jazyce

Former Lake Komoany, located in Northwest Bohemia in Central Europe, provides multiple proxies (pollen, plant macrofossils, diatoms, chironomids and sediment chemistry) that allowed reconstruction of the development of its aquatic environment and catchment, throughout the Holocene. In order to reconstruct the climatic forcing of this development, we performed a pollen-based reconstruction of climate changes using the best modern analogue method. The climate reconstruction was successful for the interval of 10.0-3.2ka BP. We demonstrate that shifts in climate were coupled with biotic changes within the lacustrine environment. Both processes were interconnected mainly through changes in the water level status of the lake. The most significant climatic and environmental changes were recorded at 9.1, 6.3, 4.8/4.7, 3.8 and 3.5ka BP.

Název v anglickém jazyce

Holocene climatic events linked to environmental changes at Lake Komořany Basin, Czech Republic

Popis výsledku anglicky

Former Lake Komoany, located in Northwest Bohemia in Central Europe, provides multiple proxies (pollen, plant macrofossils, diatoms, chironomids and sediment chemistry) that allowed reconstruction of the development of its aquatic environment and catchment, throughout the Holocene. In order to reconstruct the climatic forcing of this development, we performed a pollen-based reconstruction of climate changes using the best modern analogue method. The climate reconstruction was successful for the interval of 10.0-3.2ka BP. We demonstrate that shifts in climate were coupled with biotic changes within the lacustrine environment. Both processes were interconnected mainly through changes in the water level status of the lake. The most significant climatic and environmental changes were recorded at 9.1, 6.3, 4.8/4.7, 3.8 and 3.5ka BP.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

10618 - Ecology

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

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

Rok uplatnění

2017

Kód důvěrnosti údajů

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

Název periodika

Holocene

ISSN

0959-6836

e-ISSN

—

Svazek periodika

27

Číslo periodika v rámci svazku

8

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

14

Strana od-do

1132-1145

Kód UT WoS článku

000407819800007

EID výsledku v databázi Scopus

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