Factors controlling the development of cold-climate dune fields within the central part of the European Sand Belt–Insights from morphometry

M Łopuch, RJ Sokołowski, Z Jary - Geomorphology, 2023 - Elsevier
The central part of the European Sand Belt is an area where intense aeolian processes led
to the development of large dune fields in the Lateglacial. They have been studied …

[PDF][PDF] Quaternary stratigraphy of Poland–current status

L Marks - Acta Geologica Polonica, 2023 - geojournals.pgi.gov.pl
A critical verification of the previous stratigraphic Quaternary subdivisions has updated the
setting of the stratigraphic units in Poland. Inconsequently applied classification and …

Common chironomids drive the biodiversity–temperature relationship during the Younger Dryas-Holocene transition in a southern Baltic coastal lake

G de Mendoza, B Kotrys, M Płóciennik, P Sydor… - Hydrobiologia, 2024 - Springer
Abstract The Younger Dryas-Holocene transition represents a period of significant thermal
change, comparable in magnitude to modern warming, yet in a colder context and without …

Preboreal oscillation in the light of multiproxy analyses—Early Holocene in Lake Jelonek (North Poland)

M Kramkowski, A Filbrand-Czaja, E Zawisza… - The …, 2023 - journals.sagepub.com
In this work, we studied the course of climatic fluctuations at the beginning of the Preboreal
period using multiproxy analyses (Chironomidae, pollen, diatoms, Cladocera, stable …

Late-Weichselian (Vistulian) environmental changes in NE Poland–Evidence from Lake Suchar Wielki

M Fiłoc, M Kupryjanowicz, M Suchora, TP Luoto… - Catena, 2024 - Elsevier
By applying pollen and subfossil Cladocera analyses to the Late-Weichselian section of the
sediment profile from Lake Suchar Wielki, we aimed to track paleoenvironmental changes in …

[PDF][PDF] Changes in habitat conditions in a Late Glacial fluviogenic lake in response to climatic fluctuations (Warta River valley, central Poland)

J Forysiak, D Okupny, M Obremska… - Geological …, 2023 - bibliotekanauki.pl
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 …

A Chironomidae-based reconstruction of the Saalian-Eemian transition (mis 6a–mis 5e) in a palaeolake from the “Parchliny 2016” profile, central Poland

M Płóciennik, S Łukawska, E Janowska… - Acta Geographica …, 2023 - ceeol.com
In the end of Saalian Glaciation (Wartanian Stadial, MIS 6a) there formed many glacial
depressions, melt-out kettleholes and subglacial channels in central Poland's ice-marginal …