Increasing soil organic carbon (SOC) in croplands by switching from conventional to
conservation management may be hampered by stimulated microbial decomposition under …

The magnitude of the feedback between soil microbial respiration and increased mean
temperature may decrease (a process called thermal adaptation) or increase over time, and …

Microbes are responsible for cycling carbon (C) through soils, and predicted changes in soil
C stocks under climate change are highly sensitive to shifts in the mechanisms assumed to …

Ongoing global warming is expected to augment soil respiration by increasing the microbial
activity, driving self-reinforcing feedback to climate change. However, the compensatory …

Climate change factors alter soil microbial biomass and respiration, which represent two key
parameters of carbon (C) cycling in soils. While these interrelations are increasingly well …

Warming‐induced changes in precipitation regimes, coupled with anthropogenically
enhanced nitrogen (N) deposition, are likely to increase the prevalence, duration, and …

The commitment to energy efficiency in buildings has become more relevant as a measure
to mitigate the increase in temperature established by the Paris Climate Conference. This …

Adaptation of soil microbes due to warming from climate change has been observed, but it
remains unknown what microbial growth traits are adaptive to warming. We studied bacterial …

Understanding the temperature response of soil microbial respiration is essential for
predicting carbon (C) losses as the planet warms. As fresh, labile C inputs can further …

The factor Q 10 is used in neuroscience to adjust reaction rates of voltage-activated
membrane conductances to different temperatures and is widely assumed to be constant. By …