Mechanisms of soil organic carbon (SOC) stabilization have been widely studied due to their
relevance in the global carbon cycle. No‐till (NT) has been frequently adopted to sequester …

Anthropogenic warming is expected to accelerate global soil organic carbon (SOC) losses
via microbial decomposition, yet, there is still no consensus on the loss magnitude. In this …

Soil respiration (Rs) plays a crucial role in regulating carbon (C) cycling in terrestrial
ecosystems and the atmospheric carbon dioxide (CO 2) concentration. However, the impact …

Research in global change ecology relies heavily on global climatic grids derived from
estimates of air temperature in open areas at around 2 m above the ground. These climatic …

Global soils store at least twice as much carbon as Earth's atmosphere,. The global soil-to-
atmosphere (or total soil respiration, RS) carbon dioxide (CO2) flux is increasing,, but the …

Soils harbor a substantial fraction of the world's biodiversity, contributing to many crucial
ecosystem functions. It is thus essential to identify general macroecological patterns related …

The sensitivity of soil microbial respiration to warming (Q 10) remains a major source of
uncertainty surrounding the projections of soil carbon emissions to the atmosphere as the …

Soil respiration (R s) represents the largest flux of CO2 from terrestrial ecosystems to the
atmosphere, but its spatial and temporal changes as well as the driving forces are not well …

The regional variability in tundra and boreal carbon dioxide (CO2) fluxes can be high,
complicating efforts to quantify sink‐source patterns across the entire region. Statistical …

Quantifying soil structural dynamics and aggregate turnover is important in understanding
soil organic carbon (SOC) stocks, particularly over decadal and larger time scales. Until now …