The coming 10–20 years will be most critical for making the transition to a global food
system in which mineral nutrients in agriculture must be managed in a more holistic manner …

Terrestrial ecosystem carbon (C) sequestration plays an important role in ameliorating
global climate change. While tropical forests exert a disproportionately large influence on …

Elevating levels of atmospheric carbon dioxide (CO 2), primarily driven by the burning of
fossil fuels, combustion of organic matter, and unsustainable land practices, have amplified …

Enhancing soil carbon (C) storage has the potential to offset human‐caused increases in
atmospheric CO2. Rising CO2 has occurred concurrently with increasing supply rates of …

Conservation tillage practices may stimulate soil organic carbon (SOC) storage in croplands
by reducing soil disturbance and increasing inputs of crop residue. Although the effect of …

Soil nitrogen (N) often limits productivity in agroecosystems, prompting fertilizer applications
that increase crop yields but can degrade the environment. Nitrogen's dual role in both …

Urban greenspaces continue to grow with global urbanization. The global distribution and
stock of soil organic carbon (SOC) in urban greenspaces remain largely undescribed and …

Formation of mineral‐associated organic matter (MAOM) supports the accumulation and
stabilization of carbon (C) in soil, and thus, is a key factor in the global C cycle. Little is …

Soil is the largest organic carbon pool in the terrestrial biosphere, and a small variation of
soil organic carbon (SOC) can substantially affect the global carbon cycle and climate …

Anthropogenic nitrogen (N) input has overtaken natural N fixation as the leading source of
reactive N, and can profoundly alter the structure and functions of terrestrial ecosystems. N …