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

The result's identifiers

  • Result code in 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>

  • Alternative codes found

    RIV/67985912:_____/15:00448975 RIV/67985939:_____/15:00448975 RIV/67985831:_____/15:00448975

  • Result on the web

    <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>

Alternative languages

  • Result language

    angličtina

  • Original language name

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

  • Original language description

    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.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2015

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Boreas

  • ISSN

    0300-9483

  • e-ISSN

  • Volume of the periodical

    44

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    DK - DENMARK

  • Number of pages

    12

  • Pages from-to

    563-574

  • UT code for WoS article

    000356626400008

  • EID of the result in the Scopus database

    2-s2.0-84931955209