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) …

The paradigm that permafrost-affected soils show restricted mineral nitrogen (N) cycling in
favor of organic N compounds is based on the observation that net N mineralization rates in …

Mineral-associated organic matter (MAOM) is considered a stable reservoir for soil nutrients
that influences long-term soil carbon (C) and nitrogen (N) dynamics. However, recent …

Input of labile carbon may accelerate the decomposition of existing soil organic matter
(priming effect), with the priming intensity depending on changes in soil nitrogen availability …

As global temperatures continue to rise, a key uncertainty of climate projections is the
microbial decomposition of vast organic carbon stocks in thawing permafrost soils …

In most terrestrial ecosystems, plant growth is limited by nitrogen and phosphorus. Adding
either nutrient to soil usually affects primary production, but their effects can be positive or …

Depolymerization of high‐molecular weight organic nitrogen (N) represents the major
bottleneck of soil N cycling and yet is poorly understood compared to the subsequent …

In the last few decades, temperatures in the Arctic have increased twice as much as the rest
of the globe. As permafrost thaws in response to this warming, large amounts of soil organic …

Permafrost regions, characterised by extensive belowground excess ice, are highly
vulnerable to rapid thaw, particularly in areas such as the Yedoma domain. This region is …

Soil resource heterogeneity can affect plant growth and competitive ability. However, little is
known about how soil resource heterogeneity affects competitive interactions between …