Mid-Holocene history of a central European lake: Lake Komořany, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985939%3A_____%2F15%3A00448975" target="_blank" >RIV/67985939:_____/15:00448975 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985912:_____/15:00448975 RIV/67985831:_____/15:00448975 RIV/00216208:11310/15:10295879

Výsledek na webu

<a href="http://dx.doi.org/10.1111/bor.12119" target="_blank" >http://dx.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>

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 Komořany, 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 (50-80 ?g L-1) and pH (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 analogou

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 Komořany, 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 (50-80 ?g L-1) and pH (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 analogou

Druh

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

CEP obor

EF - Botanika

OECD FORD obor

—

Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Boreas

ISSN

0300-9483

e-ISSN

—

Svazek periodika

44

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

12

Strana od-do

563-574

Kód UT WoS článku

000356626400008

EID výsledku v databázi Scopus

2-s2.0-84931955209