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    Wyświetlanie 1-3 z 3
    Tytuł:
    Early Vistulian climate oscillations in the light of pollen analysis of deposits from Dziadowa Kłoda (Silesian Lowland, Poland)
    Autorzy:
    Kuszell, T.
    Chmal, R.
    Słychan, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059521.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Silesian Lowland
    Eemian Interglacial
    Early Vistulian
    Brörup Interstadial
    climate oscillations
    palynology
    Opis:
    The stratigraphy and palaeogeography of Quaternary deposits under lying the Oleoenica Plain were investigated during mapping of the Syców sheet of the De tailed Geo logical Map of Poland on the scale of 1:50 000. The Oleoenica Plain is part of the southern foreland of the Trzebnica Ridge, the latter representing a frontal moraine of the South and Middle Polish Glaciations. Neopleistocene deposits found at the Dziadowa Kłoda site were analyzed for their pollen content. These lacus trine to swamp deposits represent a continuous and undisturbed sequence spanning the Eemian Interglacial to Brörup Interstadial interval. The Early Vistulian deposits have been the subject of detailed palynological investigations. The reconstructed pattern of vegetation changes has allowed a precise determination of the upper boundary of the last interglacial as well as the recognition of stadial-interstadial horizons. Three climatic oscillations have been noted, corresponding to the Herning and Rederstallstadials and the Brörup Interstadial. In the climatic optimum of the interstadial, dense boreal pine-birch forests accompanied by a minor admixture of alder and spruce were predominant. Cold stadials were dominated by open vegetation with tundra and steppe elements.The pollen sequence from Dziadowa Kłoda is the first site on the Silesian Lowland that shows the first fully developed Early Vistulian warm oscillation that correlates with the Brörup Interstadial. A distinctive feature of this site is a long, continuous pollen sequence of the Eemian passing into deposits of the Vistulian Glaciation in the same profile.
    Źródło:
    Geological Quarterly; 2007, 51, 3; 319-328
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    New investigations into Early Vistulian site at Białowice (Zielona Góra area, SW Poland)
    Autorzy:
    Kuszell, T.
    Klaczak, T.
    Bartczak, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/2058971.pdf
    Data publikacji:
    2012
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    late Quaternary deposits
    Western Poland
    Early Vistulian
    vegetation and climate changes
    palynology
    Opis:
    The Białowice site is situated in the north-west of the Nowa Sól Depression which is part of the Central Poland Lowlands. Palynological analysis shows that lake and swamp accumulations took place in the Early Vistulian. Two warm interstadial-rank oscillations (Brörup and Odderade) and a stadial (Rederstall) have been distinguished during the Early Vistulian. The sequence of changes at Białowice is similar to the sequences in profiles from other parts of Poland and Western Europe. Until now, in that region of Poland the vegetation succession of the Brörup and Odderade had remained unknown. The lithology of the profile at Białowice shows rapid changes of sedimentation which have been observed in the younger part of the Brörup and at the Brörup/Rederstall transition. Geological and palynological data suggests that the maximum limit of the Vistulian Glaciation to the south of the Żary Hills.
    Źródło:
    Geological Quarterly; 2012, 56, 1; 127-138
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Palynology and archaeology of Late Vistulian and Early Holocene sites in Lubuskie Lake District, western Poland
    Autorzy:
    Okuniewska-Nowaczyk, Iwona
    Sobkowiak-Tabaka, Iwona
    Powiązania:
    https://bibliotekanauki.pl/articles/2027267.pdf
    Data publikacji:
    2014
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Lubuskie Lake Dis trict
    Late Vistulian
    Early Ho lo cene
    palynology
    ar chae ol ogy
    Opis:
    The Lubuskie Lake Dis trict played an im por tant part in recolonisation of the Pol ish Plain due to its lo ca tion and the char ac ter of the ter rain. De spite that, it is and es pe cially its north ern part, poorly ex plored re gard ing both his tory of Late Gla cial and early Ho lo cene set tle ments, and the nat u ral en vi ron ment. The pa per pres ents re sults of multidisciplinary re search in this area. The most spec tac u lar dis cov er ies were con nected with re mains of set tle ments of the Hamburgian cul ture so ci et ies at Myszêcin – cur rently the rich est site of this cul ture over the en tire North Eu ro pean Plain. In the vi cin ity of this site sev eral Late Palaeo lithic and Mesolithic set tle ments of var ied func tions were re corded. First palynological re cords came from the Youn ger Dryas sed i ments in this area. In a log with a palynological spec trum com pris ing Youn ger Dryas and the be gin ning of the Ho lo cene, a char coal dust was found and it could in di cate hu man ac tiv ity as hu mans lived at a lake shore. An im por tant com ple ment to the im age of the Late Gla cial set tle ment at the Lubuskie Lake Dis trict was pro vided by the re search near Lubrza that re sulted in data re gard ing set tle ments of the Federmesser and OEwiderian cul ture so ci et ies. This re gion was not typ i cal in a palynological spec trum of de pos its dur -ing AllerÝd but also in di cated highly di ver si fied thick ness of basal peat in a small area.
    Źródło:
    Studia Quaternaria; 2014, 31; 39-50
    1641-5558
    2300-0384
    Pojawia się w:
    Studia Quaternaria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-3 z 3

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