Carbon-nitrogen coupling is a fundamental principle in ecosystem ecology. However, how
the coupling responds to global change has not yet been examined. Through a …

Both atmospheric nitrogen (N) deposition and biochar application can markedly impact soil
heterotrophic respiration (RH), an important component of the global carbon cycle. However …

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 …

Anthropogenic activities have profoundly altered the global nitrogen (N) cycle. The
substantial changes in anthropogenic N inputs to various systems have resulted in …

The migration of trees induced by climatic warming has been observed at many alpine
treelines and boreal–tundra ecotones, but the migration of temperate trees into southern …

Soil represents the largest terrestrial carbon pool, and it liberates massive amounts of
carbon dioxide (CO2) to the atmosphere via respiration, which can influence global carbon …

Forests play a crucial role in global carbon cycling by absorbing and storing significant
amounts of atmospheric carbon dioxide. Although boreal forests contribute to approximately …

Understanding the spatial variability of ecosystem functions is an important step forward in
predicting changes in ecosystems under global transformations. Plant functional traits are …

Globally, boreal forests act as important carbon sinks, however, drought and forest
management could substantially alter the sink strength, though the controlling mechanisms …

Nitrogen (N) deposition is a significant threat to the functioning of forests and negatively
impacts the delivery of forest goods and services. Contemporary management approaches …