Plejstoceński profil pyłkowy z okolic Koniecpola nad Pilicą
THE PLEISTOCENE POLLEN PROFILE FROM THE VlCINITY OF KONlECPOL ON THE PILICAThe pollen profile of a layer of brown silts containing a thin peat intercalation and separating two undrained series exposed in the Św. Piotr hill near Kaniecpol suggests a climatic oscillation of the magnitude of an interph...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Institute of Geology University of Warsaw
1966
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| Online Access: | https://gq.pgi.gov.pl/agp/article/view/10228 |
| Summary: | THE PLEISTOCENE POLLEN PROFILE FROM THE VlCINITY OF KONlECPOL ON THE PILICAThe pollen profile of a layer of brown silts containing a thin peat intercalation and separating two undrained series exposed in the Św. Piotr hill near Kaniecpol suggests a climatic oscillation of the magnitude of an interphase. This oscillation was probably responsible for a lowering of the water table in the basin and for an agglomeration of peat in the whole basin or at least a part of it. It also caused an intermittent invasion by a mixed pine and birch forest of an area which, before and after that time, was occupied by open plant assemblages of the tundra type. |
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