We present soil organic carbon (SOC) inventories and carbon isotope compositions from over 900 samples collected in areas of minimally disturbed mature vegetation on freely drained soils (excluding peatlands) on a 1000 km transect along the Yennisey River, central Siberia. Carbon inventories over 0-30 cm depth range widely from 1.71 to 7.05 kg m-2. While an effect of changing climate or vegetation along the transect cannot be ruled out, the observed differences in SOC inventories are largely the result of variations in mineral soil texture, with inventories in fine-textured soils being approximately double those in coarse-textured soils. The δ13C values of SOC in the 0-5 cm interval ranged from -26.3 to -28.0‰, with δ13C values for the 5-30...
This study was conducted to evaluate the change in total soil carbon [TSC = litter carbon (LIC) + so...
Ice rich Yedoma-dominated landscapes store considerable amounts of organic carbon (C) and nitrogen (...
High latitude terrestrial ecosystems are considered key components in the global carbon (C) cycle an...
We present soil organic carbon (SOC) inventories and carbon isotope compositions from over 900 sampl...
Large amounts of carbon are stored in permafrost-affected soils of the Arctic tundra. The quantity, ...
Turnover rates of soil carbon for 20 soil types typical for a 3.7 million km2 area of European Russi...
In the past years considerable attention has been given to soil organic carbon (SOC) stored in perma...
An important portion of the large northern permafrost soil organic carbon (SOC) pool might be releas...
Soils of the high latitudes are expected to respond sensitively to climate change, but still little ...
The break-up of the Soviet Union in 1991 triggered cropland abandonment on a continental scale, whic...
Recent studies have shown that permafrost soils in the northern circumpolar region store almost twic...
The minor isotopes of carbon (C-13 and C-14) are widely used as tracers in studies of the global car...
The 50% variation in the estimates of carbon (C) content forest soils of Russia at present is caused...
High-latitude soils store a large amount of the global soil organic carbon (SOC). The SOC stocks in ...
The minor isotopes of carbon (C-13 and C-14) are widely used as tracers in studies of the global car...
This study was conducted to evaluate the change in total soil carbon [TSC = litter carbon (LIC) + so...
Ice rich Yedoma-dominated landscapes store considerable amounts of organic carbon (C) and nitrogen (...
High latitude terrestrial ecosystems are considered key components in the global carbon (C) cycle an...
We present soil organic carbon (SOC) inventories and carbon isotope compositions from over 900 sampl...
Large amounts of carbon are stored in permafrost-affected soils of the Arctic tundra. The quantity, ...
Turnover rates of soil carbon for 20 soil types typical for a 3.7 million km2 area of European Russi...
In the past years considerable attention has been given to soil organic carbon (SOC) stored in perma...
An important portion of the large northern permafrost soil organic carbon (SOC) pool might be releas...
Soils of the high latitudes are expected to respond sensitively to climate change, but still little ...
The break-up of the Soviet Union in 1991 triggered cropland abandonment on a continental scale, whic...
Recent studies have shown that permafrost soils in the northern circumpolar region store almost twic...
The minor isotopes of carbon (C-13 and C-14) are widely used as tracers in studies of the global car...
The 50% variation in the estimates of carbon (C) content forest soils of Russia at present is caused...
High-latitude soils store a large amount of the global soil organic carbon (SOC). The SOC stocks in ...
The minor isotopes of carbon (C-13 and C-14) are widely used as tracers in studies of the global car...
This study was conducted to evaluate the change in total soil carbon [TSC = litter carbon (LIC) + so...
Ice rich Yedoma-dominated landscapes store considerable amounts of organic carbon (C) and nitrogen (...
High latitude terrestrial ecosystems are considered key components in the global carbon (C) cycle an...