Permafrost regions at high latitudes and altitudes store about half of the Earth's soil organic
carbon (SOC). These areas are also some of the most intensely affected by anthropogenic …

Early control of atmospheric methane is essential to achieving a 1.5° C warming pathway.
This paper considers a range of academic and gray literature reviews of methane control …

Carbon and nutrient inputs are required to stimulate the formation and mineralization of soil
organic carbon (SOC) through processes related to microbial growth and priming effects …

High-latitude and high-altitude regions contain vast stores of permafrost carbon. Climate
warming may result in the release of CO2 from both the thawing of permafrost and …

Permafrost thaw can stimulate microbial decomposition and induce soil carbon (C) loss,
potentially triggering a positive C-climate feedback. However, earlier observations have …

Microbial growth and respiration are at the core of the soil carbon (C) cycle, as these
microbial physiological performances ultimately determine the fate of soil C. Microbial C use …

Soil organic carbon (SOC) stored in permafrost across the high-latitude/altitude Northern
Hemisphere represents an important potential carbon source under future warming. Here …

The modification of soil organic matter (SOM) decomposition by plant carbon (C) input
(priming effect) represents a critical biogeochemical process that controls soil C dynamics …

Nitrogen (N) and phosphorus (P) availability plays a crucial role in carbon (C) cycling in
terrestrial ecosystems. However, the C: N: P stoichiometric regulation of microbial …

Soil microbes are directly involved in soil organic carbon (SOC) decomposition, yet the
importance of microbial biodiversity in regulating the temperature sensitivity of SOC …