Globally, peatlands play an important role in the carbon (C) cycle. High water level is a key
factor in maintaining C storage in peatlands, but water levels are vulnerable to climate …

Drainage‐induced encroachment by trees may have major effects on the carbon balance of
northern peatlands, and responses of microbial communities are likely to play a central …

Peatlands store one‐third of Earth's soil carbon, the stability of which is uncertain due to
climate change‐driven shifts in hydrology and vegetation, and consequent impacts on …

Wetlands export large amounts of dissolved organic carbon (DOC) downstream, which is
sensitive to water-table fluctuations (WTFs). While numerous studies have shown that WTFs …

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 …

A small imbalance in plant productivity and decomposition accounts for the carbon (C)
accumulation capacity of peatlands. As climate changes, the continuity of peatland net C …

Dissolved organic matter (DOM) represents the most mobile and reactive pool of soil organic
matter (SOM). Climate changes, such as global warming and altered precipitation exert …

Globally, major efforts are being made to restore peatlands to maximise their resilience to
anthropogenic climate change, which puts continuous pressure on peatland ecosystems …

Wastewater discharge and salt marsh invasion are two main disturbances in global
mangrove wetland ecosystems, but their combined effects on greenhouse gas (GHG) …

Great Lakes coastlines are mosaics of wetland, stream, and lake habitats, characterized by a
high degree of spatial heterogeneity that may facilitate the co-occurrence of seemingly …