Soils are sources of the potent greenhouse gas nitrous oxide (N2O) globally, but emissions
from permafrost-affected soils have been considered negligible owing to nitrogen (N) …

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 …

Soil carbon sequestration is seen as an effective means to draw down atmospheric CO2, but
at the same time warming may accelerate the loss of extant soil carbon, so an accurate …

Nitrogen (N) availability has been considered as a critical factor for the cycling and storage
of soil organic carbon (SOC), but effects of N enrichment on the SOC pool appear highly …

Understanding the effects of changing climate and long-term human activities on soil
organic carbon (SOC) and the mediating roles of microorganisms is critical to maintain soil C …

Microplastics, a growing environmental concern, impact soil inorganic nitrogen (N)
transformation, specifically affecting water-extractable nitrate N (NO 3−− N) and ammonium …

The ecosystem carbon (C) balance in permafrost regions, which has a global significance in
understanding the terrestrial C-climate feedback, is significantly regulated by nitrogen (N) …

Global greening, characterized by an increase in leaf area index (LAI), implies an increase
in foliar carbon (C). Whether this increase in foliar C under climate change is due to higher …

In contrast to the well-recognized permafrost carbon (C) feedback to climate change, the fate
of permafrost nitrogen (N) after thaw is poorly understood. According to mounting evidence …

Carbon allocated underground through belowground net primary production represents the
main input to soil organic carbon. This is of significant importance, because soil organic …