Historical increases in emissions and atmospheric deposition of oxidized and reduced
nitrogen (N) provided the impetus for extensive, global-scale research investigating the …

Soil organic nitrogen (N) is a critical resource for plants and microbes, but the processes that
govern its cycle are not well-described. To promote a holistic understanding of soil N …

Fungal decomposition of soil organic matter depends on soil nitrogen (N) availability. This
ecosystem process is being jeopardized by changes in N inputs that have resulted from a …

Irreversible climate change alters the decomposition and sequestration of soil carbon (C).
However, the stability of C components in soils with different initial organic matter contents …

Although nitrogen (N) enrichment enhances both soil N availability and soil acidification, it is
difficult to isolate their effects on microbial taxa that drive the soil carbon (C) dynamics under …

Nitrogen (N) addition can have substantial impacts on both aboveground and belowground
processes such as plant productivity, microbial activity, and soil properties, which in turn …

Nitrogen (N) deposition is known to increase carbon (C) sequestration in N‐limited boreal
forests. However, the long‐term effects of N deposition on ecosystem carbon fluxes have …

Trees associating with different mycorrhizas often differ in their effects on litter
decomposition, nutrient cycling, soil organic matter (SOM) dynamics, and plant-soil …

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 …

Increased nitrogen (N) inputs are widely recognised to reduce soil respiration (Rs), but how
N deposition affects the temporal dynamics of Rs remains unclear. Using a decade‐long …