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 …

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 …

While soil respiration is known to be controlled by a range of biotic and abiotic factors, its
temperature sensitivity in global models is largely related to climate parameters. Here, we …

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 …

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 …

The temperature response of soil microbial respiration (R h) is of significance, with the
optimum temperature of R h being the key parameter for accurately modeling how it …

The temperature dependence of soil respiration (RS) is widely used as a key characteristic
of soils or organic matter fractions within soils, and in the context of global climatic change is …

Understanding how climatic factors, soil properties, and vegetation characteristics influence
the inter-site and inter-annual variations in Q 10 of soil respiration across biomes may help …

Soil respiration represents a major carbon flux between terrestrial ecosystems and the
atmosphere, and is expected to accelerate under climate warming. Despite its importance in …

Soil respiration (Rs) is a major pathway by which fixed carbon in the biosphere is returned to
the atmosphere, yet there are limits to our ability to predict respiration rates using …