Articles | Volume 12, issue 23
https://doi.org/10.5194/bg-12-7057-2015
© Author(s) 2015. 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-12-7057-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Carbon dynamics in boreal peatlands of the Yenisey region, western Siberia
E. D. Schulze
CORRESPONDING AUTHOR
Max Planck Institute for Biogeochemistry, P.O. Box 100164, 07701 Jena, Germany
E. Lapshina
Yugra State University, Khanty-Mansiysk, Khanty-Mansiysk Autonomous District, 628012 Russia
I. Filippov
Yugra State University, Khanty-Mansiysk, Khanty-Mansiysk Autonomous District, 628012 Russia
I. Kuhlmann
Max Planck Institute for Biogeochemistry, P.O. Box 100164, 07701 Jena, Germany
D. Mollicone
Max Planck Institute for Biogeochemistry, P.O. Box 100164, 07701 Jena, Germany
Dept. of Forestry, FAO, Viale delle Terme di Caracalla, 00153 Rome, Italy
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Cited
9 citations as recorded by crossref.
- Carbon and nutrients in the Yenisei River tributaries draining the Western Siberia Peatlands A. Prokushkin et al. https://doi.org/10.1088/1755-1315/232/1/012010
- Carbon Accumulation in Peatlands of the Mordovian Nature Reserve During the Holocene E. Novenko et al. https://doi.org/10.1134/S1028334X25606741
- Temperature Control of Spring CO2 Fluxes at a Coniferous Forest and a Peat Bog in Central Siberia S. Park et al. https://doi.org/10.3390/atmos12080984
- Macrocharcoal Signals in Histosols Reveal Wildfire History of Vast Western Siberian Forest-Peatland Complexes V. Startsev et al. https://doi.org/10.3390/plants11243478
- Carbon, nitrogen and their stable isotope (δ13C and δ15N) records in two peat deposits of Central Siberia: raised bog of middle taiga and palsa of forest-tundra ecotone A. Prokushkin et al. https://doi.org/10.1088/1755-1315/1093/1/012007
- Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers M. Behnke et al. https://doi.org/10.1073/pnas.2209883120
- Response to the letters by Kun et al. and Booth et al. E. Schulze et al. https://doi.org/10.1111/gcbb.12724
- Net ecosystem exchange and energy fluxes measured with the eddy covariance technique in a western Siberian bog P. Alekseychik et al. https://doi.org/10.5194/acp-17-9333-2017
- Carbon Accumulation and the Possibility of Carbon Losses by Vertical Movement of Dissolved Organic Carbon in Western Siberian Peatlands E. Zarov et al. https://doi.org/10.3390/f14122393
9 citations as recorded by crossref.
- Carbon and nutrients in the Yenisei River tributaries draining the Western Siberia Peatlands A. Prokushkin et al. https://doi.org/10.1088/1755-1315/232/1/012010
- Carbon Accumulation in Peatlands of the Mordovian Nature Reserve During the Holocene E. Novenko et al. https://doi.org/10.1134/S1028334X25606741
- Temperature Control of Spring CO2 Fluxes at a Coniferous Forest and a Peat Bog in Central Siberia S. Park et al. https://doi.org/10.3390/atmos12080984
- Macrocharcoal Signals in Histosols Reveal Wildfire History of Vast Western Siberian Forest-Peatland Complexes V. Startsev et al. https://doi.org/10.3390/plants11243478
- Carbon, nitrogen and their stable isotope (δ13C and δ15N) records in two peat deposits of Central Siberia: raised bog of middle taiga and palsa of forest-tundra ecotone A. Prokushkin et al. https://doi.org/10.1088/1755-1315/1093/1/012007
- Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers M. Behnke et al. https://doi.org/10.1073/pnas.2209883120
- Response to the letters by Kun et al. and Booth et al. E. Schulze et al. https://doi.org/10.1111/gcbb.12724
- Net ecosystem exchange and energy fluxes measured with the eddy covariance technique in a western Siberian bog P. Alekseychik et al. https://doi.org/10.5194/acp-17-9333-2017
- Carbon Accumulation and the Possibility of Carbon Losses by Vertical Movement of Dissolved Organic Carbon in Western Siberian Peatlands E. Zarov et al. https://doi.org/10.3390/f14122393
Saved (final revised paper)
Latest update: 02 Sep 2026
Short summary
At the eastern border of the West Siberian Plain, south of permafrost, peat started to accumulate 15000 years ago. Peat accumulated as fen peat at a constant rate of 0.2 mm yr-1 and 0.01 kgC m-2 yr-1. Over the last 2000 years, the bogs have changed into Sphagnum mires, accumulating about 0.1 kgC m-2 yr-1 until the present. The high accumulation rate of peat in unfrozen mires indicates that thawing of permafrost peat may change northern peatlands into long-lasting carbon sinks.
At the eastern border of the West Siberian Plain, south of permafrost, peat started to...
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