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The Impact of Experimental Temperature and Water Level Manipulation on Carbon Dioxide Release in a Poor Fen in Northern Poland

Authors :
Kamila M. Harenda
Mariusz Lamentowicz
Bjorn J. M. Robroek
Małgorzata Zielińska
Sandra Słowińska
Bogdan H. Chojnicki
Alexandre Buttler
Mateusz Samson
Michał Słowiński
Vincent E. J. Jassey
Jan Barabach
Department of Geoecology and Climatology, Institute of Geography and Spatial Organization
Polish Academy of Sciences
Institute of Physics [Toruń]
Faculty of Physics, Astronomy and Informatics [Toruń]
Nicolaus Copernicus University [Toruń]-Nicolaus Copernicus University [Toruń]
Laboratory of Wetland Ecology and Monitoring
Faculty of Geographical and Geological Sciences, Adam Mickiewicz University
University of Southampton
Laboratoire Chrono-environnement - CNRS - UBFC (UMR 6249) (LCE)
Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC)
Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC)
Laboratoire des systèmes écologiques (ECOS)
Ecole Polytechnique Fédérale de Lausanne (EPFL)
Faculty of Environment Engineering and Spatial Management, Department of Meteorology
Poznan University of Life Sciences
Polska Akademia Nauk = Polish Academy of Sciences (PAN)
Source :
Wetlands, Wetlands, Springer Verlag, 2018, 38 (3), pp.551-563. ⟨10.1007/s13157-018-0999-4⟩
Publication Year :
2018
Publisher :
HAL CCSD, 2018.

Abstract

Peatlands are ecosystems for which carbon budget relies strongly on the meteorological and hydrological conditions. Here, using a manipulative field experiment, we measured ecosystem respiration (RECO) over two years (2013–2014) in a poor fen in Poland to estimate the carbon emission in a changing climate. The experiment consisted of warming (open-top chambers - OTC) and water table manipulation. The application of OTC increased the mean values of daily maximum air temperature by approx. 1.1–1.8 °C. Warming or the increased water table depth separately resulted in an increase in ecosystem respiration by approx. 0.1 μmol CO2 m−2 s−1 and 0.3 μmol CO2 m−2 s−1, respectively. However, our results show also the additive nature of warming and water table drawdown impact on daily RECO during the studied years (2013–0.80 μmol CO2 m−2 s−1 and 2014–1.16 μmol CO2 m−2 s−1). With the natural dry period event which occurred in 2014, the seasonal RECO increased by approx. 0.2 μmol CO2 m−2 s−1 as compared to the previous year. Projected global warming will therefore significantly enhance C loss from poor fens in this region of Europe.

Details

Language :
English
ISSN :
02775212
Database :
OpenAIRE
Journal :
Wetlands, Wetlands, Springer Verlag, 2018, 38 (3), pp.551-563. ⟨10.1007/s13157-018-0999-4⟩
Accession number :
edsair.doi.dedup.....b204b98ec4c82910ba94404a616c8498
Full Text :
https://doi.org/10.1007/s13157-018-0999-4⟩