The numerous dystrophic (humic) lakes are a very important feature of Wigry National Park, NE Poland. As the most recent palaeoecological data indicate, at the beginning of its development (in the Late Glacial and Early and Middle Holocene) these water bodies functioned as harmonious lakes, and their transformation into dystrophic lakes and the stabilization of the trophic state took place at the beginning of the Subboreal. Palynological analysis of sediments from two such lakes (Lake Ślepe and Lake Suchar II), with special emphasis on non-pollen palynomorphs (NPPs), was aimed at a detailed biological characterization of dystrophic lakes during their long-lasting existence. The obtained results allowed for the designation of organisms chara...
A sediment core, 350 cm long recovered from Młynek Lake, northern of Poland (Warmia and Masuria Regi...
The stages of development of small Solontsovskie (Shanduyskie) Lakes located in the middle mountains...
The Lubuskie Lake District played an important part in recolonisation of the Polish Plain due to its...
The nu mer ous dystrophic (humic) lakes are a very im por tant fea ture of Wigry Na tional Park, NE ...
The main phases of the Late Glacial and Holocene development of vegetation in the Wigry National Par...
The main phases of the Late Gla cial and Ho lo cene de vel op ment of veg e ta tion in the Wigry Na ...
Soft water lakes are mostly acid, poor in minerals and have a lot of free CO2 in their water and bot...
This article is the first approach analyzing the non-pollen palynomorphs types (NPP) occurring in pa...
Samples collected from Late Pleistocene varved clays of the Vistulian (Weichselian) glaciation expos...
Late glacial and Holocene environmental history of Lake Łukie and its catchment is reconstructed fro...
m thick, are developed as lacustrine chalk intercalated with sand, mud and locally overlayed by peat...
Cladocera are a group of water animals, which are strongly dependent on environmental conditions. Th...
Lacustrine sediments of the lakes Wigry and Białe Wigierskie (Wigry National Park), up to ca. 2.5 mt...
This study aimed to reconstruct environmental changes in the Wkra River Valley near Bielawy Gołuskie...
Our research confirmed the value of kettle-hole mires for reconstructing Holocene environmental chan...
A sediment core, 350 cm long recovered from Młynek Lake, northern of Poland (Warmia and Masuria Regi...
The stages of development of small Solontsovskie (Shanduyskie) Lakes located in the middle mountains...
The Lubuskie Lake District played an important part in recolonisation of the Polish Plain due to its...
The nu mer ous dystrophic (humic) lakes are a very im por tant fea ture of Wigry Na tional Park, NE ...
The main phases of the Late Glacial and Holocene development of vegetation in the Wigry National Par...
The main phases of the Late Gla cial and Ho lo cene de vel op ment of veg e ta tion in the Wigry Na ...
Soft water lakes are mostly acid, poor in minerals and have a lot of free CO2 in their water and bot...
This article is the first approach analyzing the non-pollen palynomorphs types (NPP) occurring in pa...
Samples collected from Late Pleistocene varved clays of the Vistulian (Weichselian) glaciation expos...
Late glacial and Holocene environmental history of Lake Łukie and its catchment is reconstructed fro...
m thick, are developed as lacustrine chalk intercalated with sand, mud and locally overlayed by peat...
Cladocera are a group of water animals, which are strongly dependent on environmental conditions. Th...
Lacustrine sediments of the lakes Wigry and Białe Wigierskie (Wigry National Park), up to ca. 2.5 mt...
This study aimed to reconstruct environmental changes in the Wkra River Valley near Bielawy Gołuskie...
Our research confirmed the value of kettle-hole mires for reconstructing Holocene environmental chan...
A sediment core, 350 cm long recovered from Młynek Lake, northern of Poland (Warmia and Masuria Regi...
The stages of development of small Solontsovskie (Shanduyskie) Lakes located in the middle mountains...
The Lubuskie Lake District played an important part in recolonisation of the Polish Plain due to its...