Much research focuses on increasing carbon storage in mineral-associated organic matter
(MAOM), in which carbon may persist for centuries to millennia. However, MAOM-targeted …

Microbes are key biodiversity components of all ecosystems and control vital ecosystem
functions. Although we have just begun to unravel the scales and factors that regulate …

This research tests the casual link from political ideology to national greenhouse gas
emissions by utilizing multinational panel data covering 98 countries during the period 1990 …

Carbon and nitrogen losses from degraded wetlands and methane emissions from flooded
wetlands are both important sources of greenhouse gas emissions. However, the net …

High-latitude peatlands are changing rapidly in response to climate change, including
permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century …

Peatlands have acted as net CO2 sinks over millennia, exerting a global climate cooling
effect. Rapid warming at northern latitudes, where peatlands are abundant, can disturb their …

The water table and its dynamics are one of the key variables that control peatland
greenhouse gas exchange. Here, we tested the applicability of the Optical TRApezoid Model …

Peatland ecosystems are globally important carbon stores. Disturbances, such as drainage
and climate drying, act to lower peatland water table depths, consequently enhancing soil …

Wetlands are strategic areas for carbon uptake, but accurate assessments of their
sequestration ability are limited by the uncertainty and variability in their carbon balances …

Drainage poses a major threat to the tremendous soil organic carbon (SOC) reservoir in
wetlands. However, drainage-induced carbon loss may be mitigated by the accumulation of …