Malic acid derived from fossil resources is currently applied in the food and beverage
industries with a medium global production capacity. However, in the transition from a fossil …

Methylotrophy is a field of study dealing with microorganisms capable of utilization of
compounds devoid of carbon–carbon bonds (C1 compounds). In this review, we highlight …

Arctic lakes emit methane (CH 4) to the atmosphere. The magnitude of this flux could
increase with permafrost thaw but might also be mitigated by microbial CH 4 oxidation …

Anoxic and iron-rich (ferruginous) conditions prevailed in the ocean under the low-oxygen
atmosphere that occurred through most of the Archean Eon. While euxinic conditions (ie …

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 …

Understanding the drivers of aerobic methane (CH 4) oxidation (MOX) is paramount in
assessing the current and potential future CH 4 emissions from freshwater aquatic systems …

Most manganese (Mn) enrichments in the sedimentary rock record are hosted in carbonate
minerals, which are assumed to have formed by diagenetic reduction of precursor Mn …

In methane (CH4) generating sediments, methane oxidation coupled with iron reduction was
suggested to be catalyzed by archaea and bacterial methanotrophs of the order …

It is known that the physiology of Methanosarcina species can differ significantly, but the
ecological impact of these differences is unclear. We recovered two strains of …

Inland waters have a significant influence on atmospheric methane (CH4) levels. However,
processes determining the strength of CH4 emissions from these systems are not well …