The global soil C reservoir, similar to 1500 Gt of C (1 Gt = 10(12) kg of C
), is dynamic on decadal time scales and is sensitive to climate and human
disturbance. At present, as a result of land use, soil C is a source of atm
ospheric CO2 in the tropics and possibly part of a sink in northern latitud
es. Here I review the processes responsible for maintaining the global soil
C reservoir and what is known about how it responds to direct and indirect
human perturbations.
"I am fire and air; my other elements I give to baser life"
-William Shakespeare, Antony and Cleopatra.