Articles | Volume 13, issue 13
https://doi.org/10.5194/bg-13-3945-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-3945-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Water level, vegetation composition, and plant productivity explain greenhouse gas fluxes in temperate cutover fens after inundation
Merten Minke
CORRESPONDING AUTHOR
Thünen Institute of Climate–Smart Agriculture,
Braunschweig, Germany
Institute of Botany and Landscape Ecology, Ernst-Moritz-Arndt University, Greifswald,
Germany
Jürgen Augustin
Institute for Landscape Biogeochemistry, ZALF e.V., Müncheberg,
Germany
Andrei Burlo
Scientific and Practical Centre of the National Academy of Sciences of
Belarus for Biological Resources, Minsk, Belarus
Tatsiana Yarmashuk
Institute for Nature Management of the National Academy of Sciences of
Belarus, Minsk, Belarus
Hanna Chuvashova
Scientific and Practical Centre of the National Academy of Sciences of
Belarus for Biological Resources, Minsk, Belarus
Annett Thiele
Institute of Botany and Landscape Ecology, Ernst-Moritz-Arndt University, Greifswald,
Germany
Michael Succow Foundation, Greifswald, Germany
Annette Freibauer
Thünen Institute of Climate–Smart Agriculture,
Braunschweig, Germany
Vitalij Tikhonov
Scientific and Practical Centre of the National Academy of Sciences of
Belarus for Biological Resources, Minsk, Belarus
Mathias Hoffmann
Institute of Soil Landscape Research, ZALF e.V., Müncheberg,
Germany
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40 citations as recorded by crossref.
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Latest update: 21 Nov 2024
Short summary
We studied GHG emissions along water-level gradients of two inundated cutover fens with closed chambers. N2O fluxes were negligible. CO2 and CH4 fluxes were controlled by vegetation composition and plant productivity, which in turn depended on water level and nutrient conditions. CH4 fluxes from mesotrophic sites were low and largely compensated for by CO2 uptake. Eutrophic sites were strong CH4 sources, and GHG balances depended on the plant's net C sink, which strongly differed between species.
We studied GHG emissions along water-level gradients of two inundated cutover fens with closed...
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