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Sphagnum Litter as the Most Important Genetic Horizon in the Profile of Peat Soils of Boreal Bogs
Abstract —Peat soils of the taiga zone of Western Siberia are historically relatively poorly studied. In the diagnostics of peat soils, the question...
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The Main Features of Hydrology and Hydrogeochemistry of Bogs: Case Study of the Ilasskii Bog Massif
AbstractThe study of the isotope hydrogeology of bogs in the Northwestern Russia included the analysis of the potential of the integrated use of...
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Specific Features of Soil-Vegetation Cover of Revegetated Oil-Polluted Oligotrophic Bogs Reclaimed by the Cutting Method in the Middle Ob Region
AbstractThe article provides data from a comparative analysis of vegetation restoration in areas of oligotrophic bogs with strong oil product...
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Topsoil removal for Sphagnum establishment on rewetted agricultural bogs
Rewetting drained agricultural peatlands aids in restoring their original ecosystem functions, including carbon storage and sustaining unique...
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Biogeochemical Features of Holocene Sediments in Oligotrophic Bogs of the Baraba Forest Steppe
Abstract—The paper presents data on the geochemical processes of postsedimentation transformations of boggy deposits at early diagenesis and the...
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Evolution of Organic Matter in Hummocky Bogs on the Barents Sea Coast in a Changing Climate
AbstractThe influence of macroparameters (botanical composition, degree of decomposition, and radiocarbon age of peat) on the molecular composition...
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Formation of the Composition of Polycyclic Aromatic Hydrocarbons in Hummocky Bogs in the Forest-Tundra–Northern Tundra Zonal Sequence
AbstractThe accumulation of polycyclic aromatic hydrocarbons (PAHs) in plants and peat of three natural subzones—forest-tundra, southern tundra, and...
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Geochemical Features of Peat Deposits at Oligotrophic Bogs in the Southern Taiga Subzone of West Siberia
Abstract—The paper presents original authors’ data on the geochemical aspects and peat deposits and conditions of their accumulation at the three...
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Impact of Forest Fires on the Microbiological Properties of Oligotrophic Peat Soils and Gleyed Peat Podzols of Bogs in the Northern Part of the Sym-Dubches Interfluve, Krasnoyarsk Region
AbstractKey plots of hydromorphic and semihydromorphic peat soils of oligotrophic bogs were studied in the area of the Middle Yenisei Station of the...
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Restoration of Raised Bogs in the Khanty-Mansiysk Ob Region after Reclamation of Oil- and Salt-Polluted Peat Soils in 2003–2005
AbstractThe process of natural remediation of oil- and soil-contaminated raised bogs reclaimed 14–16 years ago in Khanty-Mansiysk Autonomous...
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Identification of Hydrocarbons in the Waters of Raised Bogs in the Southern Taiga of Western Siberia
Abstract—The composition and content of hydrocarbons (HCs) in the waters three raised bogs of the south taiga subzone of Western Siberia: the Bolshoe...
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Taxonomic Structure of Bacterial Communities of Rhizospheric Soil under Bogs’ Plants
AbstractFor the first time, the ratio of large taxa and the genera spectrum of the prokaryotic community of the rhizosphere soil under typical plants...
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Greenhouse Gas Fluxes and Carbon Sequestration in the Oligotrophic Peat Soils of Southern Taiga in Western Siberia
AbstractThe carbon stock and the emission rates of greenhouse gases (CO 2 and CH 4 ) in the peat soils of southern taiga in Western Siberia were...
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Formation and decay of peat bogs in the vegetable belt of Switzerland
The rapidly collapsing glacial systems of the Alps produced a large number of melt-water lakes and mires after the Last Glacial Maximum (LGM) in the...
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Element stoichiometry and nutrient limitation in bog plant and lichen species
Ombrotrophic bogs receive new inputs of elements solely through atmospheric deposition, except for N where inputs are predominantly through N 2 -fixatio...
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Soils оf Oligomesotrophic аnd Mesotrophic Bogs in the Boreal Zone of West Siberia: Possibilities of Botanical Diagnostics within the Framework of the Type of Mesotrophic Peat Soils
AbstractDespite the widespread use of the taxon “mesotrophic (transitional) peat soils” in the present-day Russian and foreign pedology, including...
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Groundwater seeps are hot spots of denitrification and N2O emissions in a restored wetland
Restorations of former cranberry farms (“bogs”) aim to re-establish native wetland vegetation, promote cold water habitat, and attenuate nitrogen (N)...
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Sphagnoid spores as tracers of environmental and climatic changes in peatland habitats of the early Eocene
Peat mosses have been an important part of the lignite forming vegetation in the early Eocene of the Helmstedt Lignite Mining District. Three genera...
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Comparison of the transformation of organic matter flux through a raised bog and a blanket bog
This study has proposed that organic matter transfer and transformation into and through a peatland is dominated by preferential loss of...