Mid-Holocene history of a central European lake: Lake Komořany, Czech Republic
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10295879" target="_blank" >RIV/00216208:11310/15:10295879 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985912:_____/15:00448975 RIV/67985939:_____/15:00448975 RIV/67985831:_____/15:00448975
Výsledek na webu
<a href="https://doi.org/10.1111/bor.12119" target="_blank" >https://doi.org/10.1111/bor.12119</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/bor.12119" target="_blank" >10.1111/bor.12119</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Mid-Holocene history of a central European lake: Lake Komořany, Czech Republic
Popis výsledku v původním jazyce
Palaeolimnological reconstruction of the aquatic environment in Lake Komoany, based on sedimentology, geochemistry, and diatom and macrofossil analyses in the littoral part of the basin, reflects the mid-Holocene history of the profile from its origin c.9100 cal. a BP to its final transformation into an alder carr c.4100 cal. a BP. The existence of the littoral zone can be best explained by increased precipitation during the studied interval. A stable diatom community, diatom-inferred total phosphorus (50-80gL(-1)) and pH (similar to 7.6), along with stable concentrations of elements associated with changes in its watershed indicate a long-lasting, balanced aquatic environment with no major shifts attributable to external factors, including climate change. From c.4700 cal. BP, there started a transition to terrestrial conditions, caused by either natural infilling processes or decreased precipitation. Alternation of remarkable dry/wet phases was not detected, in contrast to numerous analogous central European and supraregional records. Potential human impact was revealed through increases of Corylus and Populus pollen in the Neolithic. These anthropogenic changes in the lake surroundings had no detectable influence on the lacustrine environment. The gathered data suggest undramatic, balanced mid-Holocene environmental and climatic settings for this central European locality, in direct contrast to numerous analogous studies from the region emphasizing fluctuations and shifts found in the sediment record.
Název v anglickém jazyce
Mid-Holocene history of a central European lake: Lake Komořany, Czech Republic
Popis výsledku anglicky
Palaeolimnological reconstruction of the aquatic environment in Lake Komoany, based on sedimentology, geochemistry, and diatom and macrofossil analyses in the littoral part of the basin, reflects the mid-Holocene history of the profile from its origin c.9100 cal. a BP to its final transformation into an alder carr c.4100 cal. a BP. The existence of the littoral zone can be best explained by increased precipitation during the studied interval. A stable diatom community, diatom-inferred total phosphorus (50-80gL(-1)) and pH (similar to 7.6), along with stable concentrations of elements associated with changes in its watershed indicate a long-lasting, balanced aquatic environment with no major shifts attributable to external factors, including climate change. From c.4700 cal. BP, there started a transition to terrestrial conditions, caused by either natural infilling processes or decreased precipitation. Alternation of remarkable dry/wet phases was not detected, in contrast to numerous analogous central European and supraregional records. Potential human impact was revealed through increases of Corylus and Populus pollen in the Neolithic. These anthropogenic changes in the lake surroundings had no detectable influence on the lacustrine environment. The gathered data suggest undramatic, balanced mid-Holocene environmental and climatic settings for this central European locality, in direct contrast to numerous analogous studies from the region emphasizing fluctuations and shifts found in the sediment record.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Boreas
ISSN
0300-9483
e-ISSN
—
Svazek periodika
44
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
DK - Dánské království
Počet stran výsledku
12
Strana od-do
563-574
Kód UT WoS článku
000356626400008
EID výsledku v databázi Scopus
2-s2.0-84931955209