<abstract xml:lang="en" xmlns="http://www.w3.org/1999/xhtml"><p>The paper presents the results of interdisciplinary (multiproxy) palaeoenvironmental studies of peat — calcareous tufa depositional sequences of spring mire from Radzików site (east Poland). Analyses of three biotic proxies (plant macrofossils, pollen, molluscs) were supplemented with sedimentological, geochemical, oxygen and carbon stable isotopes analyses and radiocarbon dating and used for reconstruction of environmental changes in Late Glacial and Holocene. The obtained results enable us to (1) reconstruct main phases of mire development and (2) determine environmental factors influencing changes of water supply.</p><p>The object started to develop in Allerød. The Late Glacial and Early Holocene deposit sequence is relatively thick (about 1.0 m), with good palaeoecological record. The boundary between Younger Dryas and Preboreal is especially well confirmed by palynological and malacological analyses as well as radiocarbon dating. The Mesoholocene deposits are considerably worse preserved. Mire development was evaluated in terms of general mire ecology.</p></abstract>

The paper presents the results of interdisciplinary (multiproxy) palaeoenvironmental studies of peat — calcareous tufa depositional sequences of spring mire from Radzików site (east Poland). Analyses of three biotic proxies (plant macrofossils, pollen, molluscs) were supplemented with sedimentological, geochemical, oxygen and carbon stable isotopes analyses and radiocarbon dating and used for reconstruction of environmental changes in Late Glacial and Holocene. The obtained results enable us to (1) reconstruct main phases of mire development and (2) determine environmental factors influencing changes of water supply.The object started to develop in Allerød. The Late Glacial and Early Holocene deposit sequence is relatively thick (about 1.0 m), with good palaeoecological record. The boundary between Younger Dryas and Preboreal is especially well confirmed by palynological and malacological analyses as well as radiocarbon dating. The Mesoholocene deposits are considerably worse preserved. Mire development was evaluated in terms of general mire ecology.

Interdisciplinary studies of spring mire deposits from Radzików (South Podlasie Lowland, East Poland) and their significance for palaeoenvironmental reconstructions

Institute of Earth Sciences, Maria Curie-Skłodowska University, Kraśnicka 2 cd, PL-20-718, Lublin, Poland

Faculty of Geology, Geophysics and Environment Protection, University of Science and Technology, Mickiewicza 30, PL-30-059, Kraków, Poland

Institute of Physics, Maria Curie-Skłodowska University, M.Curie-Skłodowska sq. 1, PL-20-031, Lublin, Poland

Institute of Physics, Silesian University of Technology, Krzywoustego 2, PL-44-100, Gliwice, Poland

Faculty of Horticulture, University of Life Sciences, Akademicka 13, PL-20-950, Lublin, Poland

Geochronometria

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

The paper presents the results of interdisciplinary (multiproxy) palaeoenvironmental studies of peat — calcareous tufa depositional sequences of spring mire...

Interdisciplinary studies of spring mire deposits from Radzików (South Podlasie Lowland, East Poland) and their significance for palaeoenvironmental reconstructions

Publicado en línea: 25 dic 2011

Páginas: 10 - 29

DOI: https://doi.org/10.2478/s13386-011-0052-3

Palabras clave
spring mire, peat, calcareous tufa, palaeoenvironmental reconstructions, Holocene, South Podlasie Lowland

© 2011 Silesian University of Technology, Gliwice, Poland

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Interdisciplinary studies of spring mire deposits from Radzików (South Podlasie Lowland, East Poland) and their significance for palaeoenvironmental reconstructions

Publicado en línea: 25 dic 2011

Páginas: 10 - 29

DOI: https://doi.org/10.2478/s13386-011-0052-3

Palabras clavespring mire, peat, calcareous tufa, palaeoenvironmental reconstructions, Holocene, South Podlasie Lowland

© 2011 Silesian University of Technology, Gliwice, Poland

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Palabras clave
spring mire, peat, calcareous tufa, palaeoenvironmental reconstructions, Holocene, South Podlasie Lowland