Ralf Conrad

Methane fluxes show consistent temperature dependence across microbial to ecosystem scales

The global methane cycle: recent advances in understanding the microbial processes involved

Soil microorganisms as controllers of atmospheric trace gases (H2, CO, CH4, OCS, N2O, and NO).

<i>Bacteria</i> rather than <i>Archaea</i> dominate microbial ammonia oxidation in an agricultural soil

Contribution of hydrogen to methane production and control of hydrogen concentrations in methanogenic soils and sediments

Microbial Ecology of Methanogens and Methanotrophs

Quantification of methanogenic pathways using stable carbon isotopic signatures: a review and a proposal

A 3‐year continuous record on the influence of daytime, season, and fertilizer treatment on methane emission rates from an Italian rice paddy

The capacity of hydrogenotrophic anaerobic bacteria to compete for traces of hydrogen depends on the redox potential of the terminal electron acceptor

Methanogenic archaea are globally ubiquitous in aerated soils and become active under wet anoxic conditions

Processes involved in formation and emission of methane in rice paddies

Competition for electron donors among nitrate reducers, ferric iron reducers, sulfate reducers, and methanogens in anoxic paddy soil