Ts. Vinson et Tp. Kolchugina, POOLS AND FLUXES OF BIOGENIC CARBON IN THE FORMER SOVIET-UNION, Water, air and soil pollution, 70(1-4), 1993, pp. 223-237
The Former Soviet Union (FSU) was the largest country in the world. It
occupied one-sixth of the land surface of the Earth. An understanding
of the pools and fluxes of biogenic C in the FSU is essential to the
development of international strategies aimed at mitigation of the neg
ative impacts of global climate change. The territory of the FSU is re
presented by a variety of climate conditions. The major part of the FS
U territory is in the boreal and temperate climatic zones. The climate
in the FSU changes from arctic and subarctic in the North to subtropi
cal and desert in the South. From west to east, the climate makes a tr
ansition from maritime to continental to monsoon. The vegetation of th
e FSU includes the following principal types: forest, woodland, shrubl
and, grassland, tundra, desert, peatlands and cultivated land. Arctic
deserts and tundra formations are found in the northern part of the FS
U; deserts and semi-deserts are found in the southern part. A framewor
k was created to assess pools and fluxes of biogenic C in the FSU. Und
er the framework spatially distributed data were analyzed with a geogr
aphic information system to isolate ecoregions. The soil-vegetation co
mplexes for the ecoregions were linked to FSU data bases of soil and v
egetation C pools and fluxes. The C budget for an ecoregion was establ
ished by multiplying the area of the ecoregion by the unit area C cont
ent(s) or rate(s) associated with the soil-vegetation complex for the
ecoregion. The C pools and fluxes for all the ecoregions were summed t
o arrive at an initial estimate of the pools and fluxes of biogenic C
for 95% of the territory of the FSU. Based on the framework, net prima
ry productivity (NPP) for the FSU was estimated at 6.17 +/- 1.65 Gt C
yr-1, the vegetation C pool (live plant mass and coarse woody debris)
at 118.1 +/- 28.5 Gt C, the litter C pool at 18.9 +/- 4.4 Gt C, and to
tal soil C pool at 404.0 +/- 38.0 Gt C. The phytomass pool of the FSU
was 16% of the global biomass pool. The soil and litter pools of the F
SU were 20 and 23% of the global soil and detritus pools, respectively
. The NPP of the FSU was 10% of the global NPP. The phytomass, soil an
d litter densities of the FSU were greater than the world average. The
productivity of terrestrial ecosystems in the FSU was slightly lower
than the world average.