Experimental fire increases soil carbon dioxide efflux in a grassland long-term multifactor global change experiment.

Numerous studies have demonstrated that soil respiration rates increase under experimental warming, although the long-term, multiyear dynamics of this feedback are not well constrained. Less is known about the effects of single, punctuated events in combination with other longer-duration anthropogenic influences on the dynamics of soil carbon (C) loss. In 2012 and 2013, we assessed the effects of decadal-scale anthropogenic global change - warming, increased nitrogen (N) deposition, elevated carbon dioxide (CO ), and increased precipitation - on soil respiration rates in an annual-dominated Mediterranean grassland.