Methane Emissions from Paludified Boreal Soils in European Russia as Measured and Modelled

Schneider, J.; Ťupek, Boris; Lukasheva, Maria; Gudyrev, Vasiliy; Miglovets, Mikhail; Jungkunst, Hermann F.

doi:10.1007/s10021-017-0188-y

Cited by 6 publications

(4 citation statements)

References 29 publications

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“…In comparison to few existing studies finding small CH4 emissions for forest -mire transects in Canada and Europe (Moosavi and Crill 1997, Ullah et al 2011, Schneider et al 2018, similarly in this study, the CH4 exchange of forestmire transitions was near zero during wetter periods and a small sink during drier periods. In landscape biogeochemistry, forest-mire transitions have the potential to become small sources of CH4 if their water level increases closer to the surface, but their CH4 emissions are expected to be smaller than in mires.…”

Section: Eqcontrasting

confidence: 51%

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Environmental controls of boreal forest soil CO2 and CH4 emissions and soil organic carbon accumulation

Ťupek¹

2020

Diss. For.

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Section: Eqcontrasting

confidence: 51%

“…Schneider J., Ťupek B., Lukasheva M. et al (2018). Methane Emissions from Paludified Boreal Soils in European Russia as Measured and Modelled.…”

Section: IVmentioning

confidence: 99%

Environmental controls of boreal forest soil CO2 and CH4 emissions and soil organic carbon accumulation

Ťupek¹

2020

Diss. For.

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“…On paludified soils Schneider et al [25] measured methane (CH 4 ) flux for forest and peatland areas. Open peatlands exhibited a methane emission rate of 21.9 ± 1.6 g m −2 yr. −1 in contrast with forested peatland transition zones (7.9 ± 0.5 g m −2 yr. −1 ).…”

Section: Research Studies Having a Focus On Carbon Loss As Greenhousementioning

confidence: 99%

Soil Genesis of Histosols and Gelisols with a Emphasis on Soil Processes Supporting Carbon Sequestration

Aide¹,

Aide²,

Braden³

2021

Environmental Issues and Sustainable Development

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Based on the U.S. Soil Taxonomy Histosols are soils that have a histic epipedon, which is a surface horizon that exhibits a sufficient abundance of soil organic matter to be distinctively different than other soil orders predominantly composed of clastic materials. Gelisols are soils that have permafrost, with histels being a suborder that is dominated by organic materials. Collectively, these soil orders are abundant in peatland ecosystems. The abundance of soil organic material is primarily a consequence of climate, topography, hydrology, vegetation. Peatland ecosystems have been a major research arena; however, added research attention is being directed to the potential release of carbon because of accelerated climate change. This review focuses of the structure and dynamics of organic soils and an understanding of their creation, evolution and ultimate fate. Attention is focused on degraded peatland net primary productivity because of potential forthcoming differences attributed to rainfall, temperature, vegetation, hydrology and permafrost disappearance.

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“…We found only a small number of studies providing data on soil consumption in small-leaved forests [9,10], broad-leaved forests [10][11][12], planted mixed forests [13], forest-tundra ecosystem [14], and light [15] and dark coniferous forests [16,17]. Several studies were focused on assessing methane emissions from Russian forests [18][19][20]. Thus, despite accounting for 80% of Russian forests [8], the taiga biome was mostly ignored.…”

Section: Introductionmentioning

confidence: 99%

Atmospheric Methane Consumption and Methanotroph Communities in West Siberian Boreal Upland Forest Ecosystems

Сабреков

Danilova

Terentieva

et al. 2021

Forests

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Upland forest ecosystems are recognized as net sinks for atmospheric methane (CH4), one of the most impactful greenhouse gases. Biological methane uptake in these ecosystems occurs due to the activity of aerobic methanotrophic bacteria. Russia hosts one-fifth of the global forest area, with the most extensive forest landscapes located in West Siberia. Here, we report seasonal CH4 flux measurements conducted in 2018 in three types of stands in West Siberian middle taiga–Siberian pine, Aspen, and mixed forests. High rates of methane uptake of up to −0.184 mg CH4 m−2 h−1 were measured by a static chamber method, with an estimated total growing season consumption of 4.5 ± 0.5 kg CH4 ha−1. Forest type had little to no effect on methane fluxes within each season. Soil methane oxidation rate ranged from 0 to 8.1 ng CH4 gDW−1 h−1 and was negatively related to water-filled pore space. The microbial soil communities were dominated by the Alpha- and Gammaproteobacteria, Acidobacteriota and Actinobacteriota. The major group of 16S rRNA gene reads from methanotrophs belonged to uncultivated Beijerinckiaceae bacteria. Molecular identification of methanotrophs based on retrieval of the pmoA gene confirmed that Upland Soil Cluster Alpha was the major bacterial group responsible for CH4 oxidation.

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Methane Emissions from Paludified Boreal Soils in European Russia as Measured and Modelled

Cited by 6 publications

References 29 publications

Environmental controls of boreal forest soil CO<sub>2</sub> and CH<sub>4</sub> emissions and soil organic carbon accumulation

Environmental controls of boreal forest soil CO<sub>2</sub> and CH<sub>4</sub> emissions and soil organic carbon accumulation

Soil Genesis of Histosols and Gelisols with a Emphasis on Soil Processes Supporting Carbon Sequestration

Atmospheric Methane Consumption and Methanotroph Communities in West Siberian Boreal Upland Forest Ecosystems

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