The developmental history, from the Oldest Dryas to the Late Holocene, of a paleolake and
mire located in a river valley in Central Poland was studied using high-resolution records of …

We reconstructed 3300 years (3500 BCE and 200 BCE) of the development history of the
Rąbień peatland located in central Poland, using pollen, macrofossil, testate amoebae …

The paleoecological evolution of a peat bog in the Campos region, Rio Grande do Sul State,
Brazil, was determined based on an integrated study of stratigraphy, palynology, and …

We use a range of environmental variables to explore the possible drivers influencing the
biota, especially the composition of aquatic invertebrates, during the Younger Dryas (YD) …

The chemical composition of lake and mire sediments can be used as proxies of past
changes in different accumula-tion environments. Here, I present these proxies that can be …

Fens have been forming in the river valleys of central Poland since the Bølling and went
through a transformation from fully aquatic to semiterrestrial habitats during the Younger …

Cladoceran-based paleotemperature estimates for the Younger Dryas for ten sections of
paleo-oxbow lakes, valley mires, and lacustrine sediments from central Poland are …

W pracy przeanalizowano wypełnienie niewielkiego paleokoryta Warty wyciętego z
początkiem holocenu w płaskiej i monotonnej powierzchni terasy niskiej. W rozwoju …

The Warta River valley was greatly influenced by the ice sheet of the Last Glacial Maximum
(LGM). A small peatland located in the Warta drainage system is here used as a …

Analizę geochemiczną przeprowadzono dla osadów organicznych z torfowiska Bęczkowice
w środkowym biegu doliny rzeki Luciąża. Z profilu B1, zlokalizowanego w południowej …