The paper analyzed the number of ecological-trophic groups of microorganisms and the elemental composition of the active, permafrost and thawed layers of a typical flat mount frozen peatlands (plateau palsa) in the Nadym-Pur interfluves, Western Siberia, with part of it affected by fire. The number of ecological-trophic groups was found to change after permafrost thaw. The study revealed a relationship between the number of microorganisms and the content of some chemical elements in the soil profile of the plateau palsa in the Nadym-Pur interfluve. A statistically significant relationship was found between the most probable number of microorganisms (CFU/g) in different peat layers and the pH, the ash content and the content of calcium, magn...
Investigation of organic carbon and nitrogen stock was conducted at depths greater than one meter in...
Geochemical conditions of the formation of various minerals were studied within the oligotrophic pin...
The fate of organic carbon (OC), nutrients and metals accumulated in thawing permafrost ice is at th...
The content and the profile distribution of the element composition of the 1 meter high peat deposit...
Of particular interest in the north of Western Siberia are frozen flat-mound bogs. Being formed in a...
Permafrost peatlands, containing a sizable amount of soil organic carbon (OC), play a pivotal role i...
The formation of significant amounts of low molecular weight (LMW) water-soluble organic compounds, ...
To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we ...
International audienceMobilization of dissolved organic carbon (DOC) and related trace elements (TEs...
The following primary variables were studied in order to understand which part microbial decomposers...
The microbial activity in the soils of the permafrost-affected zones is assumed to be one of the maj...
Permafrost soils differ significantly from other soils because they serve as a huge reservoir for or...
Soils are an important compartment of ecosystems and have the ability to buffer and immobilize subst...
International audienceWarming of the permafrost accompanied by the release of ancient soil organic c...
In this paper, we identify and describe the active and inert horizons of oligotrophic bogs. These of...
Investigation of organic carbon and nitrogen stock was conducted at depths greater than one meter in...
Geochemical conditions of the formation of various minerals were studied within the oligotrophic pin...
The fate of organic carbon (OC), nutrients and metals accumulated in thawing permafrost ice is at th...
The content and the profile distribution of the element composition of the 1 meter high peat deposit...
Of particular interest in the north of Western Siberia are frozen flat-mound bogs. Being formed in a...
Permafrost peatlands, containing a sizable amount of soil organic carbon (OC), play a pivotal role i...
The formation of significant amounts of low molecular weight (LMW) water-soluble organic compounds, ...
To better understand freezing - thawing cycles operating in peat soils of permafrost landscapes, we ...
International audienceMobilization of dissolved organic carbon (DOC) and related trace elements (TEs...
The following primary variables were studied in order to understand which part microbial decomposers...
The microbial activity in the soils of the permafrost-affected zones is assumed to be one of the maj...
Permafrost soils differ significantly from other soils because they serve as a huge reservoir for or...
Soils are an important compartment of ecosystems and have the ability to buffer and immobilize subst...
International audienceWarming of the permafrost accompanied by the release of ancient soil organic c...
In this paper, we identify and describe the active and inert horizons of oligotrophic bogs. These of...
Investigation of organic carbon and nitrogen stock was conducted at depths greater than one meter in...
Geochemical conditions of the formation of various minerals were studied within the oligotrophic pin...
The fate of organic carbon (OC), nutrients and metals accumulated in thawing permafrost ice is at th...