Key points are not available for this paper at this time.
▪ Abstract The global soil C reservoir, ∼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 atmospheric CO 2 in the tropics and possibly part of a sink in northern latitudes. 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
Ronald Amundson (Tue,) studied this question.