Microbial residues contribute to the long‐term stabilization of carbon in the entire soil profile,
helping to regulate the climate of the planet; however, how sensitive these residues are to …

Soil carbon (C) stabilization has become an important topic in recent years in the context of
global climate change. Increasing evidence suggests that microbial residues represent a …

Warming is known to reduce soil carbon (C) stocks by promoting microbial respiration, which
is associated with the decomposition of microbial residue carbon (MRC). However, the …

Soil microorganisms are central to sustain soil functions and services, like carbon and
nutrient cycling. Currently, we only have a limited understanding of the spatial-temporal …

Microorganisms have a role as gatekeepers for terrestrial carbon fluxes, either causing its
release to the atmosphere through their decomposition activities or preventing its release by …

The impact of global warming on soil carbon pools has been extensively investigated,
however, there is still a lack of understanding regarding the specific response of microbial …

Soils represent the largest carbon (C) pool in terrestrial ecosystems. The preservation and
increase of soil C play a significant role in the fight against climate change, and can deliver …

Perturbations in soil microbial communities caused by climate warming are expected to
have a strong impact on biodiversity and future climate–carbon (C) feedback, especially in …

The paucity of investigations of carbon (C) dynamics through the soil profile with warming
makes it challenging to evaluate the terrestrial C feedback to climate change. Soil microbes …

Microbial communities play critical roles in soil carbon-warming feedback, but our
understanding of their linkages to soil carbon (C) pools in response to short-and long-term …