Peatland restoration and rehabilitation action has become more widely acknowledged as a
necessary response to mitigating climate change risks and improving global carbon storage …

The positive Arctic–methane (CH4) feedback forms when more CH4 is released from the
Arctic tundra to warm the climate, further stimulating the Arctic to emit CH4. This study …

Soil microbes drive biogeochemical cycles of carbon (C) and nutrients, and land conversion
alters soil microbes and thus, affects C and nutrient cycling at the ecosystem level. To …

Tropical peatlands are one of the largest natural sources of atmospheric methane (CH 4)
and play a significant role in regional and global carbon budgets. However, large …

Mangroves forests may be important sinks of carbon in coastal areas but upon their death,
these forests may become net sources of carbon dioxide (CO 2) and methane (CH 4) to the …

The cultivation of flooding-tolerant grasses on wet or rewetted peatlands is a priority in
climate change mitigation, balancing the trade-off between atmospheric decarbonisation …

Northern peatlands are a terrestrial carbon store, with an annual sink of 0.1 Pg C yr− 1 and a
total storage estimate of 547 Pg C. Northern peatlands are also major contributors of …

In wetlands, hydrological conditions drive plant community distribution, forming vegetation
zones with plant species and material cycling. This mediates nitrogen migration and N 2 O …

Microbial processes are crucial in producing and oxidizing biological methane (CH4) in
natural wetlands. Therefore, modeling methanogenesis and methanotrophy is …

Wetlands account for up to 70% of the natural source of methane (CH4) in terrestrial
ecosystems on a global scale. Soil microbes are the ultimate producers and biological …