Carbon assimilation is the incorporation of carbon from an external source into an organism's cellular compounds and biomass. It involves chemical transformations, rather than merely transport across a membrane. Carbon can also be oxidized for energy or released in secreted products, so disappearance of a carbon source from the surroundings does not alone measure assimilation.
Methylotrophy provides an illuminating example. In the experimentally studied Methylobacterium pathway, methanol is converted to formaldehyde, with carbon then entering either oxidation toward carbon dioxide or assimilation into cellular compounds. The same incoming carbon pool can thus support different metabolic functions.[ref]
Suppose an invented closed carbon account records100millimoles of carbon atoms taken up,40released as carbon dioxide,10released in other products, and no change in an unmeasured internal store. The remaining50millimoles are retained in biomass: . This is a conservation calculation under explicit assumptions. A real experiment must also check unmeasured products, pre-existing carbon stores and losses before assigning the remainder to new biomass.
Carbon fixation is one route contributing to carbon assimilation when inorganic carbon is converted into organic compounds. Assimilation of an already organic substrate is a different starting point. Measuring metabolic flux or tracing labeled carbon can help distinguish the incoming material's transformations from an increase in total cell mass.
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