Warunki paleoekologiczne subkopalnego koryta Kolonia Bechcice na tle hydrologii środkowego odcinka doliny Neru
Journal Title: Acta Geographica Lodziensia - Year 2016, Vol 105, Issue
Abstract
The history of the Ner River valley is well documented in Kolonia Bechcice (NKB) palaeochannel sediments. It was cut-off from the riverbed in the Younger Dryas. Its history may be divided into five distinct phases. During the Younger Dryas, the NKB was a relatively deep, oligotrophic water body. From the onset of the Holocene, the lake became a eutrophic, overgrown pond which quickly palludified and transformed into a rich fen with ferns and birches. There is a hiatus in the middle of the Holocene fen stratigraphy. A peat sequence is covered by fluvial silt and sand deposits. The NKB sequence documents the Ner valley as a dynamic system during the Late Glacial and the Holocene. Local ecosystems of this oxbow have remained under a much stronger pressure of climate changes than palaeolakes and wetlands located on uplands in the Łódź region.
Authors and Affiliations
Mateusz Płóciennik, Piotr Kittel, Ryszard Borówka, Katarzyna Cywa, Daniel Okupny, Milena Obremska, Dominik Pawłowski, Renata Stachowicz-Rybka, Rafał Szperna, Andrzej Witkowski
Pojezierze eemskie: uwagi o genezie i zaniku jezior polodowcowych centralnej Polski
The ice sheet recession from the preEemian glaciation left a lakeland the traces of which we see in the sediments of lake basins forming at that time (Fig. 1). In Central Poland recognized are 58 sites of fossil lake and...
Geneza jezior i torfowisk dorzecza Prypeci w świetle polskich badań okresu międzywojennego
A study of mires and lakes (fossil and contemporary) was conducted in the whole Polesie area, within a framework of the Polish Governement Bureau for Land Reclamation in Polesie. The research lasted for five and a half y...
Wstęp: Klimat i bioklimat miast
-
Próba rekonstrukcji rozwoju zbiornika akumulacji biogenicznej w Bydlinie (Wyżyna Śląsko- -Krakowska)
The peat bog near the village of Bydlin in the Silesian-Cracovian Upland was subjected to geochemical, palaeobotanical and malacological analyses. The mire is located in a subsidence basin in a carbonate karst area. The...
Z badań czwartorzędu w Polsce. Pamięci Profesor Haliny Klatkowej
-