Podrobnosti záznamu

Název
    Late glacial climatic and environmental changes in eastern-central Europe: Correlation of multiple biotic and abiotic proxies from the Lake Švarcenberk, Czech Republic
Autor
    Bučkuliaková, S.
    Horáček, I.
    Hošek, J.
    Kadlec, Jaroslav
    Kubovčík, V.
    Lisá, Lenka
    Pokorný, P.
    Rojik, C.
    Žáčková, P.
Jazyk
    anglicky
Typ dokumentu
    článek v odborném periodiku
Zdrojový dokument - seriál
    Palaeogeography, Palaeoclimatology, Palaeoecology
Svazek/č.
    Roč. 396, 15 February
Strany
    s. 155-172
Rok
    2014
Poznámky
    Rozsah: 18 s. : E
Předmětová kategorie
    biotic/abiotic responses
    climate changes
    Eastern-Central Europe
    lacustrine sediments
    Last Glacial Termination
Klíčové slovo
    Abiotic
    Biotic
    Changes
    Climatic
    Correlation
    Czech
    Eastern-central
    Environmental
    Europe
    Glacial
    Lake
    Late
    Multiple
    Proxies
    Republic
    Švarcenberk
Abstrakt (anglicky)
   Thick lake sediments discovered in the southern part of the Czech Republic provide a high-resolution archive for detailed study of paleoenvironmental changes during the Late Pleistocene to Holocene in eastern-central Europe. Until recently, no similar records were available for this important region in the transition from oceanic to continental macro-climatic settings. Using a multi-proxy approach that combines sedimentological, pollen-analytical, paleozoological (Chironomids), geochemical and mineral-magnetic methods we demonstrate that major climatic events of the Late Glacial can be correlated with Atlantic rather than continental regimes as reported in paleoclimatic literature for the area of the interest. The sensitivity of applied biological and abiological techniques to climatically-driven processes allows trans-regional comparisons and enables us to discuss the pattern of geographic variation in these processes.
   We are able to establish a clear relationship between vegetation cover, soil development and erosional processes. A short-term intra-Alleröd cool event has been correlated with the Gerzensee oscillation. Proxy evidence suggests that the early half of the Younger Dryas was rather humid, whereas the latter half was dry and had significant impact on vegetation, sedimentary dynamics and lake level status during the YD/Preboreal transition.
Přispěvatel
    AV ČR Brno, Geologický ústav
Kód přispěvatele
    AV ČR, GLÚ
Zdrojový formát
    U
Datum importu
    23. 10. 2014