From a periglacial lake to an alkaline fen – Late Glacial/Early Holocene evolution of Lublin chalkland tracked in biogenic sediments of Bagno Staw (Western Polesie Lowland, E Poland)

Author:

Pietruczuk J.,Dobrowolski R.,Suchora M.,Apolinarska K.,Bieganowski A.,Trembaczowski A.,Polakowski C.,Bober A.

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference136 articles.

1. Multi-component stable isotope records from Late Weichselian and early Holocene lake sediments at Imiołki, Poland: palaeoclimatic and methodological implications;Apolinarska;J. Quat. Sci.,2009

2. Vegetational history of the lake Łukcze environment (Lublin, Polesie, E, Poland) during the Late Glacial and Holocene;Bałaga;Acta Paleobot.,1982

3. Hydrological changes in the Lublin Polesie during the Late Glacial and Holocene as reflected in the sequences of lacustrine and mire sediments;Bałaga;Stud. Quat.,2002

4. Changes of vegetation in Lake Perespilno environs (Lublin Polesie) in the Late Glacial and Holocene;Bałaga;Acta Palaeobot.,2004

5. Changes in the natural environment recorded in the sediments of the Karaśne lake-mire complex (Lublin Polesie, E Poland);Bałaga;Geochronometria,2007

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