Carbon stored in the terrestrial biosphere amounts to 3,170GTC.
Bio-molecules are complex carbon compounds and are produced by living things. They include proteins, carbohydrates, fats and oils.
The biosphere is the total sum of all living matter.
Soil carbon can contain inorganic carbon, such as calcite, dolomite or gypsum.
Peat is an accumulation of partially decayed vegetation or organic matter. It forms in wetland conditions.
In tropical rainforests, 50% of carbon is stored in the soil and 50% is stored in the biomass.
Peat is dead, un-decayed organic matter, which is found in boggy areas and contains 250GTC.
Soil organic matter contains 1,500GTC.
The biggest terrestrial store of carbon, which is 26%. The older trees store centuries of carbon and their heavy canopy blocks sunlight from reaching the forest floor.
Tropical rainforests store 20% of the terrestrial carbon.
In all forests, 31% of the carbon is stored in the biomass and 69% in the soil.
Soil humus is a thick brown or black substance that remains after most of the organic litter has been decomposed.
Peatlands from 3% of the land and store 250GTC.
The soil carbon pool is approximately 3.1 times larger than the atmospheric pool. Only the ocean has a large store.
Peat forms when permanent saturation obstructs flows of oxygen creating anaerobic conditions that slows decomposition.
Leaf accounts for 70% of litter in forests.
19% of carbon in the biosphere is stored in plants.