Interactions between soil nitrogen (N) availability, fungal community composition, and soil
organic matter (SOM) regulate soil carbon (C) dynamics in many forest ecosystems, but …

The extent to which ectomycorrhizal (ECM) fungi decay soil organic matter (SOM) has
implications for accurately predicting forest ecosystem response to climate change …

Ectomycorrhizal fungi are essential for nitrogen (N) cycling in many temperate forests and
responsive to anthropogenic N addition, which generally decreases host carbon (C) …

Fungi dominate the microbial biomass of temperate forest soils and are a key driver of
ecosystem nutrient cycling. Chronic nitrogen (N) amendments frequently cause the …

As global change shifts the species composition of forests, we need to understand which
species characteristics affect soil organic matter (SOM) cycling to predict future soil carbon …

Plant–mycorrhizal interactions mediate plant nitrogen (N) limitation and can inform model
projections of the duration and strength of the effect of increasing CO2 on plant growth. We …

While the effect of nitrogen (N) deposition on belowground carbon (C) cycling varies,
emerging evidence shows that forest soils dominated by trees that associate with …

Forest soils store large amounts of carbon (C) and nitrogen (N), yet how predicted shifts in
forest composition will impact long‐term C and N persistence remains poorly understood. A …

The distribution of mycorrhizal associations across biomes parallels a distinct gradient of soil
carbon (C) and nitrogen (N) stocks, raising the question of how mycorrhizal traits relate to …

Atmospheric nitrogen (N) deposition has increased dramatically since preindustrial times
and continues to increase across many regions of the Earth. In temperate forests, this agent …