Seasonal ecosystem variability in remote mountain lakes: implications for detecting climatic signals in sediment records.
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077387%3A_____%2F02%3A62023143" target="_blank" >RIV/60077387:_____/02:62023143 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Seasonal ecosystem variability in remote mountain lakes: implications for detecting climatic signals in sediment records.
Popis výsledku v původním jazyce
The main patterns of seasonal variability in the ecosystems of nine lakes in Europe are discussed with the implications for recording climatic features in their sediments. Despite the diversity in latitude and size, the lakes showed a number of common features. They were phosphorus limited, ice-covered between 5-9 months, and all but one were dimictic. Two types of lakes were distinguished according to the number of production peaks during the ice-free season. Lakes with longer summer stratification tended to have two productive periods: one at the onset of stratification, and the other during the autumn overturn. Lakes with shorter stratification had single peak during the ice-free period. All lakes presented deep chlorophyll maxima during summer stratification, and subsurface chlorophyll maxima beneath the ice. The major chemical components showed a short but extreme dilution during thawing. Certain lake features may favour the recording of particular climatic fluctuations.
Název v anglickém jazyce
Seasonal ecosystem variability in remote mountain lakes: implications for detecting climatic signals in sediment records.
Popis výsledku anglicky
The main patterns of seasonal variability in the ecosystems of nine lakes in Europe are discussed with the implications for recording climatic features in their sediments. Despite the diversity in latitude and size, the lakes showed a number of common features. They were phosphorus limited, ice-covered between 5-9 months, and all but one were dimictic. Two types of lakes were distinguished according to the number of production peaks during the ice-free season. Lakes with longer summer stratification tended to have two productive periods: one at the onset of stratification, and the other during the autumn overturn. Lakes with shorter stratification had single peak during the ice-free period. All lakes presented deep chlorophyll maxima during summer stratification, and subsurface chlorophyll maxima beneath the ice. The major chemical components showed a short but extreme dilution during thawing. Certain lake features may favour the recording of particular climatic fluctuations.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DA - Hydrologie a limnologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2002
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Paleolimnology
ISSN
0921-2728
e-ISSN
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Svazek periodika
28
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
22
Strana od-do
25-46
Kód UT WoS článku
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EID výsledku v databázi Scopus
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