Methane-dependent nitrate and nitrite removal in anoxic environments is thought to rely on
syntrophy between ANME-2d archaea and bacteria in the genus 'Candidatus …

Wetlands are the largest and most uncertain biological source of atmospheric methane, with
hydrological fluctuations exacerbating this uncertainty. Here we critically explore the …

Methane (CH4) is an important greenhouse gas with a global warming potential 28–34
times that of CO2 over the 100-year horizon. Denitrifying anaerobic methane oxidation …

Rice paddy has been the main source of anthropogenic methane (CH 4) emissions, with
significant variations among rice varieties. 2-Acetyl-1-pyrroline (2-AP) is the key component …

Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is
performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related …

Methane (CH 4) is both generated and consumed in paddy soils, where anaerobic oxidation
of methane (AOM) serves as a crucial process for mitigating CH 4 emissions. Although the …

The greenhouse gas methane in soils has been considered to be consumed mainly by
aerobic methane-oxidizing bacteria for a long time. In the last decades, the discovery of …

Freshwater wetlands, paddy fields, inland aquatic ecosystems and coastal wetlands are
recognized as important sources of atmospheric methane (CH 4). Currently, increasing …

Paddy fields constitute a substantial anthropogenic reservoir of methane, with their
inundation management fostering an ideal habitat for anaerobic methane oxidation. Within …

The recent discovery of anaerobic oxidation of methane (AOM) in freshwater ecosystems
has caused a great interest in “cryptic methane cycle” in terrestrial ecosystems. Anaerobic …