Soil carbon losses to the atmosphere through soil respiration are expected to rise with
ongoing temperature increases, but available evidence from mesic biomes suggests that …

A positive soil carbon (C)‐climate feedback is embedded into the climatic models of the
IPCC. However, recent global syntheses indicate that the temperature sensitivity of soil …

The respiratory release of carbon dioxide (CO2) from soil is a major yet poorly understood
flux in the global carbon cycle. Climatic warming is hypothesized to increase rates of soil …

Soil carbon losses to the atmosphere, via soil heterotrophic respiration, are expected to
increase in response to global warming, resulting in a positive carbon-climate feedback …

In the short‐term heterotrophic soil respiration is strongly and positively related to
temperature. In the long‐term, its response to temperature is uncertain. One reason for this is …

Despite decades of research, how climate warming alters the global flux of soil respiration is
still poorly characterized. Here, we use meta‐analysis to synthesize 202 soil respiration …

Climate change severely impacts the grassland carbon cycling by altering rates of litter
decomposition and soil respiration (R s), especially in arid areas. However, little is known …

Warming can affect soil microbial respiration by changing microbial biomass and community
composition. The responses of soil microbial respiration to warming under experimental …

The world's soils contain a large amount of carbon so that even a fractionally small loss or
gain could have a quantitatively important feedback effect on net CO2 emissions to the …

Respiratory effluxes of carbon (C) from the soil to the atmosphere are expected to rise with
temperature, potentially intensifying future climate warming. However, whether and how this …