Almost half of the total organic carbon (C) in terrestrial ecosystems is stored in forest soils.
By altering rates of input or release of C from soils, forest management activities can …

Anthropogenic nitrogen (N) deposition is expected to increase substantially and
continuously in the future. Soil N availability regulates microbial communities and the …

Effective land-based solutions to climate change mitigation require actions that maximize
soil carbon storage without generating surplus nitrogen. Land management for carbon …

Terrestrial ecosystem carbon (C) sequestration plays an important role in ameliorating
global climate change. While tropical forests exert a disproportionately large influence on …

The crucial biogeochemical processes such as carbon and nutrient cycling are increasingly
altered at the ecosystem scale by global environmental changes. Although soil extracellular …

The availability of nitrogen (N) is a critical control on the cycling and storage of soil carbon
(C). Yet, there are conflicting conceptual models to explain how N availability influences the …

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 …

Agricultural and industrial activities have increased atmospheric nitrogen (N) deposition to
ecosystems worldwide. N deposition can stimulate plant growth and soil carbon (C) input …

Nitrogen (N) deposition is a component of global change that has considerable impact on
belowground carbon (C) dynamics. Plant growth stimulation and alterations of fungal …

Due to the profound impact of nitrogen (N) input on soil systems, linking the activity and
composition of soil microbial communities to soil organic carbon (SOC) is crucial to reveal …