Conversion of tropical peat swamp forest to drainage-based agriculture alters greenhouse
gas (GHG) production, but the magnitude of these changes remains highly uncertain …

Peatlands accumulate organic matter (OM) under anaerobic conditions. After drainage for
forestry or agriculture, microbial respiration and peat oxidation induce OM losses and …

Net methane (CH 4) emission from lakes depends on two antagonistic processes: CH 4
production (methanogenesis) and CH 4 oxidation (methanotrophy). It is unclear how climate …

Tropical coastal systems play a vital role in sustaining biodiversity, performing ecological
functions, and providing ecosystem services. They are also home to 75% of people in the …

Root exudates represent a large and labile carbon input in tropical peatlands, but their
contribution to carbon dioxide (CO 2) and methane (CH 4) production remains poorly …

Anaerobic oxidation of methane (AOM) is a microbial process that consumes dissolved
methane (CH 4) in anoxic sediments and soils and mitigates CH 4 release to the …

Ebullition has been shown to be an important pathway for methane (CH 4) emissions from
inland waters. However, the CH 4 fluxes and their magnitudes in thermokarst lakes remain …

Tropical peatlands cycle and store large amounts of carbon in their soil and biomass,,,–.
Climate and land-use change alters greenhouse gas (GHG) fluxes of tropical peatlands, but …

As interfaces connecting terrestrial and ocean ecosystems, coastal wetlands develop
temporally and spatially complex redox conditions, which drive uncertainties in greenhouse …

The study of soil microbial communities and chemical properties of soil organic matter
(SOM) over altitudinal mountain gradients have been regarded as especially useful to better …