Iron (Fe) minerals play an important role in stabilizing soil organic carbon (SOC). Fe-
mediated SOC protection is mainly achieved through adsorption, co-precipitation, or …

Nutrient enrichment is a major global change component that often disrupts the relationship
between aboveground biodiversity and ecosystem functions by promoting species …

Nitrogen (N) availability has been considered as a critical factor for the cycling and storage
of soil organic carbon (SOC), but effects of N enrichment on the SOC pool appear highly …

Soil microbes make up a significant portion of the genetic diversity and play a critical role in
belowground carbon (C) cycling in terrestrial ecosystems. Soil microbial diversity and …

The few percent of soil organic carbon (SOC) among mineral components form the interface
of climate, plant growth, soil biological processes, physical transport infrastructure, and …

Soil microbial diversity is one of the key factors affecting the structure and function of the
belowground ecosystem; yet, little is known about the response of microbial diversity to …

Permafrost thaw can stimulate microbial decomposition and induce soil carbon (C) loss,
potentially triggering a positive C-climate feedback. However, earlier observations have …

China is experiencing a high level of atmospheric nitrogen (N) deposition, which greatly
affects the soil carbon (C) dynamics in terrestrial ecosystems. Soil aggregation contributes to …

Direct quantification of terrestrial biosphere responses to global change is crucial for
projections of future climate change in Earth system models. Here, we synthesized …

Microbial growth and respiration are at the core of the soil carbon (C) cycle, as these
microbial physiological performances ultimately determine the fate of soil C. Microbial C use …