Soil organic carbon is a general term for the total of all the different
non-living organic compounds in the soil, it also excludes dead plants
and animals. The organic carbon in the soil is used by plants for
nourishment as they grow, and the plants themselves replenish the
resource when they decay after they die.
Although it would seem that high densities of soil carbon would
correspond to areas where vegetation thrives, this is not necessarily
the case. For example, the regions of the world categorized as tropical
rainforest typically have very low quality soils - not because the soils
are bad, rather because the highly active vegetation on the surface has
already extracted most of the nutrient from the soil. The regions of the
world where soil carbon accumulates, are therefore regions where
vegetation growth is generally slower - such as swamps, bogs, and wetlands.