The article presents the characteristics of the relief of the Rypienica channel (the Dobrzyń Lakeland, North Poland) and the postglacial development of vegetation in this area. The detailed analysis of the organic sediments of the peat-bog vegetation of the Rypienica channel documents the development of vegetation since the beginning of the Holocene until the younger part of the Subatlantic period. Holocene sediments record changes in the local vegetation of this peat-bog brought about by fluctuations in climate, changes in local hydrological conditions and the impact of human activity.
In the northern part of the Polish Outer Carpathians, the Beskid Makowski Mts., four landslides form...
A 11-m-long lake sediment core of a mountain lake situated at 1225 m a.s.l. in the Karkonosze Mounta...
The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four ...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gyt...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gytt...
During litho-stratigraphic studies of deposits in small mires in the upper basin of the Oder River, ...
Core drilling of a hole Bysławek-2 consisted of gyttja and peat, lying on the mineral deposits (fluv...
The sediments of Lake Kwiecko, located in the eastern part of the Bytowskie Lake District (part of t...
Bottom sediments of Lake Łańskie in NE Poland (Olsztyn Lake District) were studied by pollen analysi...
This study aimed to reconstruct environmental changes in the Wkra River Valley near Bielawy Gołuskie...
Artykuł poświęcony jest problematyce genezy równin torfowiskowych w strefie „staroglacjalnej” połudn...
Sediments from an oxbow lake located in the Prosna River valley (Poland) were analysed to investigat...
The Lubuskie Lake District played an important part in recolonisation of the Polish Plain due to its...
The environmental variability during the Mazovian/Holsteinian interglacial is better understood than...
Based on palaeobotanical analyses of organic deposits, as well as geomorphological and geological st...
In the northern part of the Polish Outer Carpathians, the Beskid Makowski Mts., four landslides form...
A 11-m-long lake sediment core of a mountain lake situated at 1225 m a.s.l. in the Karkonosze Mounta...
The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four ...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gyt...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gytt...
During litho-stratigraphic studies of deposits in small mires in the upper basin of the Oder River, ...
Core drilling of a hole Bysławek-2 consisted of gyttja and peat, lying on the mineral deposits (fluv...
The sediments of Lake Kwiecko, located in the eastern part of the Bytowskie Lake District (part of t...
Bottom sediments of Lake Łańskie in NE Poland (Olsztyn Lake District) were studied by pollen analysi...
This study aimed to reconstruct environmental changes in the Wkra River Valley near Bielawy Gołuskie...
Artykuł poświęcony jest problematyce genezy równin torfowiskowych w strefie „staroglacjalnej” połudn...
Sediments from an oxbow lake located in the Prosna River valley (Poland) were analysed to investigat...
The Lubuskie Lake District played an important part in recolonisation of the Polish Plain due to its...
The environmental variability during the Mazovian/Holsteinian interglacial is better understood than...
Based on palaeobotanical analyses of organic deposits, as well as geomorphological and geological st...
In the northern part of the Polish Outer Carpathians, the Beskid Makowski Mts., four landslides form...
A 11-m-long lake sediment core of a mountain lake situated at 1225 m a.s.l. in the Karkonosze Mounta...
The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four ...