Vegetation shifts in circum-Arctic permafrost peatlands drive feedbacks with important
consequences for peatland carbon budgets and the extent of permafrost thaw under …

It is important to investigate the responses of greenhouse gases to climate change
(temperature, precipitation) and anthropogenic factors in plateau wetland. Based on the …

Permafrost degradation in peatlands is altering vegetation and soil properties and impacting
net carbon storage. We studied four adjacent sites in Alaska with varied permafrost regimes …

While wetlands are major sources of biogenic methane (CH4), our understanding of resident
microbial metabolism is incomplete, which compromises the prediction of CH4 emissions …

Permafrost peatlands are vulnerable to rapid structural changes under climatic warming,
including vertical collapse. Peatland water budgets, and therefore peat hydraulic properties …

Interactions between microbiomes and metabolites play crucial roles in the environment, yet
how these interactions drive greenhouse gas emissions during ecosystem changes remains …

Soil microorganisms are pivotal in the global carbon cycle, but the viruses that affect them
and their impact on ecosystems are less understood. In this study, we explored the diversity …

Future permafrost thaw will likely lead to substantial release of greenhouse gases due to
thawing of previously unavailable organic carbon (OC). Accurate predictions of this release …

Quantifying the temperature sensitivity of methane (CH 4) production is crucial for predicting
how wetland ecosystems will respond to climate warming. Typically, the temperature …

The soil freeze-thaw (FT) state plays a significant role in cold ecosystems by influencing
hydrology, geomorphology, ecology, thermodynamics, and soil chemistry. As climate …