Wetlands cover a small portion of the world, but have disproportionate influence on global
carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes …

The global budget of atmospheric CH4, which is on the order of 500–600 Tg CH4 per year,
is mainly the result of environmental microbial processes, such as archaeal methanogenesis …

Maximizing carbon sequestration in mangroves is part of the global effort to combat the
climate crisis. However, methane (CH4) emissions can partially offset carbon sequestration …

Methane (CH4) emissions from aquatic systems should be coupled to CH4 production, and
thus a temperature‐dependent process, yet recent evidence suggests that modeling CH4 …

Lacustrine methane emissions are strongly mitigated by aerobic methane-oxidizing bacteria
(MOB) that are typically most active at the oxic-anoxic interface. Although oxygen is required …

Freshwater reservoirs are a known source of greenhouse gas (GHG) to the atmosphere, but
their quantitative significance is still only loosely constrained. Although part of this …

Lake sediments are “hot spots” of methane production in the landscape. However, regional
and global lake methane emissions, contributing to the greenhouse effect, are poorly known …

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 …

Methanogenesis has traditionally been assumed to occur only in anoxic environments, yet
there is mounting, albeit indirect, evidence of methane (CH4) production in oxic marine and …

Methane (CH4) represents a major product of organic matter decomposition in lakes. Once
produced in the sediments, CH4 can be either oxidized or emitted as a greenhouse gas to …