Methane (CH4) emissions from the boreal and arctic region are globally significant and
highly sensitive to climate change. There is currently a wide range in estimates of high …

Boreal peatlands represent a biogeochemically unique and diverse environment in high-
latitude landscape. They represent a long-term globally significant sink for carbon dioxide …

Tidal salt marshes produce and emit CH4. Therefore, it is critical to understand the
biogeochemical controls that regulate CH4 spatial and temporal dynamics in wetlands. The …

Permafrost peatlands are a significant source of methane (CH4) emissions to the
atmosphere and could emit more CH4 with continued permafrost thaw. Aerobic methane …

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

Permafrost thaw in northern peatlands often leads to increased methane (CH 4) emissions,
but gaps remain in our understanding of the underlying controls responsible for increased …

Arctic tundra exhibits large landscape heterogeneity in microtopography, hydrology, and
active layer depth. While many carbon flux measurements and experiments are done at or …

The sensitivity of peatland carbon (C) fluxes to changes in climate and hydrology are
uncertain due to the complex interactions between plants and peat properties. In this study …

Peatland biological, physical and chemical properties change over time in response to
alterations in long-term water table position. Such changes complicate our ability to predict …

Sphagnum mosses account for most accumulated dead organic matter in peatlands.
Therefore, understanding their responses to increasing atmospheric CO2 is needed for …