methanogenesis

Most methane is the result of biological process called methanogenesis.

In order to produce energy, they use an anaerobic process called methanogenesis.

In other words, those methanogenesis improve the coefficient of utilization.

Naturally occurring methane is mainly produced by the process of methanogenesis.

Most methanogenesis, or methane production, occurs in oxygen poor environments.

Nickel-methyl intermediates have been proposed for the final step of methanogenesis.

During the low sulphate period, there was active methanogenesis and little production of sulphide.

Methanofuran converts to formylmethanofuran in an early stage of methanogenesis.

Methanogenesis occurs in the guts of humans and other animals, especially ruminants.

Several types of methanogenesis occur, differing in the starting compounds oxidized.

The terminal electron acceptor in methanogenesis is not oxygen, but carbon.

Sulphate availability may therefore be important in determining methanogenesis in man.

Most of these proteins are related to methanogenesis, and they could serve as potential molecular markers for the methanogens.

The coenzyme is the C1 donor in methanogenesis.

Methane is created near the Earth's surface, primarily by microorganisms by the process of methanogenesis.

Methylamine arises as a result of putrefaction and is a substrate for methanogenesis.

This hydrogen is then taken up by methanogens and converted to methane via methanogenesis.

Methanogenesis in microbes is a form of anaerobic respiration.

In man, the principal routes are via methanogenesis or dissimilatory sulphate reduction.

This enzyme is involved in methanogenesis from dimethylamine.

The terminal stage of anaerobic digestion is the biological process of methanogenesis.

Digestate is produced both by acidogenesis and methanogenesis and each has different characteristics.

The latter increased markedly, however, when sulphate was added to the diet, while methanogenesis became suppressed by approximately 60%.

Methanogenesis or biomethanation is the formation of methane by microbes known as methanogens.

Only methanogenesis and fermentation can occur in the absence of electron acceptors other than carbon.