We have known about the processes of methanogenesis and methanotrophy for over 100
years, since the days of Winogradsky, yet their contributions to the carbon cycle were …

Methane is estimated to have contributed 20% of postindustrial global warming.
Methanotrophs oxidize methane and curb methane emissions into the atmosphere …

Net emissions of the potent GHG methane from ecosystems represent the balance between
microbial methane production (methanogenesis) and oxidation (methanotrophy), each with …

In this chapter, the authors provide a comprehensive analysis and synthesis of the
interactions between important drivers and controls of hyporheic exchange and …

Methane emissions from organic-rich soils in the Arctic have been extensively studied due to
their potential to increase the atmospheric methane burden as permafrost thaws,–. However …

Anaerobic oxidation of methane (AOM) reduces methane emissions from marine
ecosystems but we know little about AOM in rivers, whose role in the global carbon cycle is …

In the Arctic, the spatiotemporal variation of net methane uptake in upland soils depends on
unresolved interactive controls between edaphic and microbial factors not yet included in …

Aquatic habitats beneath ice masses contain active microbial ecosystems capable of cycling
important greenhouse gases, such as methane (CH4). A large methane reservoir is thought …

The flux of terrestrial carbon across land‐water boundaries influences the overall carbon
balance of landscapes and the ecology and biogeochemistry of aquatic ecosystems. The …

Microbial methane (CH 4) oxidation is a major global sink of CH 4. Aerobic CH 4-oxidizing
bacteria (methanotrophs) represent a biological model system for CH 4 consumption and is …