Soil organic carbon (SOC) plays a central role in ecosystem carbon sequestration and
climate change mitigation, and its stability and dynamics are related to sourcing from …

Forest ecosystems store~ 80% of the carbon in terrestrial ecosystems, but their long-term
carbon sequestration depends partly on how plant biomass and soil carbon stocks will …

Microbial communities in soils are generally considered to be limited by carbon (C), which
could be a crucial control for basic soil functions and responses of microbial heterotrophic …

Biochar plays an important role in reducing the harmful environmental effects of inorganic
nitrogen (N) fertilizers on agroecosystems, but the the impact mechanisms of biochar …

Forests provide invaluable economic, ecological, and social services. At the same time, they
are exposed to several threats, such as fragmentation, changing climatic conditions, or …

Soil microbes drive soil organic carbon (SOC) mineralization. Because microbial groups
differ in metabolic efficiency and respond differently to temperature variation, it is reasonable …

As a microbial-derived carbon (C) compound, the glomalin-related soil protein (GRSP) is not
only a considerable amount of soil active organic C, but also an effective aggregate binder …

Within a landscape, multiple habitats exist for soil microbial communities. But how these
habitats shape community composition requires an understanding of the way in which …

Soil carbon (C) sequestration plays a critical role in mitigating climate change. Nitrogen (N)
deposition greatly affects soil C dynamics by altering C input and output. However, how soil …

Nitrogen (N) deposition increases soil carbon (C) storage by reducing microbial activity.
These effects vary in soil beneath trees that associate with arbuscular (AM) and …