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Late Pleistocene and Holocene evolution of the Durne Bagno peat bog (Lublin Polesie)



Late Pleistocene and Holocene evolution of the Durne Bagno peat bog (Lublin Polesie)



Przeglad Geologiczny 54(1): 68-72



The Durne Bagno peat bog is the eastern, peripheral part of a large marshland complex in the Lublin Polesie. Limnic biogenic deposits occurring directly on mineral deposits are up to 8.5 m thick. They exhibit great vertical facial variablility and small lateral differentiation. This indicates that the conditions of sedimentations/sedentation were similar in the whole basin in particular time intervals. The chronostratigraphically-correlated sequence of sediments allows reconstruction of the geosystem evolution in recent 13 Ka BP. In its entire Late Glacial and Holocene history two basis stages may be distinguished: lacustrine (OD-middle AT) and mire (middle AT-present time).

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