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  3. Responses of vegetation and testate amoeba trait composition to fire disturbances in and around a bog in central European lowlands (northern Poland)
 

Responses of vegetation and testate amoeba trait composition to fire disturbances in and around a bog in central European lowlands (northern Poland)

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BORIS DOI
10.7892/boris.127683
Date of Publication
March 2019
Publication Type
Article
Division/Institute

Institut für Pflanzen...

Oeschger Centre for C...

Institute of Plant Sc...

Contributor
Marcisz, Katarzyna
Institut für Pflanzenwissenschaften (IPS)
Lamentowicz, Mariusz
Gałka, Mariusz
Colombaroli, Danieleorcid-logo
Institut für Pflanzenwissenschaften (IPS)
Adolf, Carole
Institut für Pflanzenwissenschaften (IPS)
Tinner, Willy
Institut für Pflanzenwissenschaften (IPS)
Subject(s)

500 - Science::580 - ...

Series
Quaternary science reviews
ISSN or ISBN (if monograph)
0277-3791
Publisher
Elsevier
Language
English
Publisher DOI
10.1016/j.quascirev.2019.02.003
Uncontrolled Keywords

Central Europe

Charcoal

Functional and morpho...

High-resolution

Macrofossils

Palaeoecology

Fire history

Peatland

Description
Compared to boreal or Mediterranean biomes, the influence of fire on peatlands in Central Europe is not well studied. We aim to provide first analysis of statistically significant charcoal-inferred fire events from a peatland from central European lowlands, spanning the period of the last 650 years, and define peatland vegetation and microbial trait-related responses to local fire events. Here, we reconstructed regional and local fire activity from Bagno Kusowo bog (Poland) using high-resolution microscopic charcoal and macroscopic charcoal and its morphotypes, inferring past fire regimes using numeric analyses. We compared fire data with extra-local (pollen) and local (plant macrofossils, testate amoebae (TA) and their trait composition) proxies. Our data show that within the chronological uncertainties, regional fires recorded in the peat core coincide with historically-documented fires. Macroscopic charcoal analysis suggests 3–8 local fire events, while fire frequency varied between 0 and 2 events/1000 years. Wood charcoal was dominant throughout the profile, pointing to forest fires in close proximity to the peatland. Local fire activity was the most intensive in the 17th century, when the water table was at its lowest. The abundance of Sphagnum spp. declined, whereas vascular plants, mixotrophs and TA with proteinaceous shells were significantly positively correlated to fire. Xenosomes were significantly negatively correlated to fires, and they responded to water table lowering. We show that the peatlands’ vegetation recovered from low-intensity and short-lasting disturbances and, to some extent, maintained “pristine” local vegetation cover with Sphagnum as the dominant taxon. TA traits common before disturbances, mainly mixotrophs and TA with proteinaceous shells, temporarily re-appeared after fire. We conclude that TA communities in peatlands are good bioindicators of disturbances.
Handle
https://boris-portal.unibe.ch/handle/20.500.12422/65007
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FileFile TypeFormatSizeLicensePublisher/Copright statementContent
2019_QuatSciRev_ 208_129.pdftextAdobe PDF2.18 MBpublisherpublished restricted
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