CO2 efflux from soil depends on the availability of organic substances respired by roots and
microorganisms. Therefore, photosynthetic activity supplying carbohydrates from leaves to …

The terrestrial carbon (C) cycle has received increasing interest over the past few decades,
however, there is still a lack of understanding of the fate of newly assimilated C allocated …

Soil organic carbon harbors three times as much carbon as Earth's atmosphere, and its
decomposition is a potentially large climate change feedback and major source of …

Global mean temperature is predicted to increase by 2–7° C and precipitation to change
across the globe by the end of this century. To quantify climate effects on ecosystem …

Soil microbial respiration is an important source of uncertainty in projecting future climate
and carbon (C) cycle feedbacks. However, its feedbacks to climate warming and underlying …

Understanding the mechanisms of biospheric feedbacks to climate change is critical to
project future climate warming,,. Although microorganisms catalyse most biosphere …

Long-term observations have shown that many plants and aboveground animals have
changed their phenology patterns due to warmer temperatures over the past decades …

It has been well established by field experiments that warming stimulates either net
ecosystem carbon uptake or release, leading to negative or positive carbon cycle–climate …

Microbial decomposition of soil organic matter produces a major flux of CO2 from terrestrial
ecosystems and can act as a feedback to climate change. Although climate‐carbon models …

Among the largest uncertainties in current projections of future climate is the feedback
between the terrestrial carbon cycle and climate. Northern peatlands contain one-third of the …