Cold seeps and hydrothermal vents deliver large amounts of methane and other gaseous alkanes into marine surface sediments. Consortia of archaea and partner bacteria thrive on the oxidation of these alkanes and its coupling to sulfate reduction. The inherently slow growth of the involved organisms and the lack of pure cultures have impeded the understanding of the molecular mechanisms of archaeal alkane degradation. Here, using hydrothermal sediments of the Guaymas Basin (Gulf of California) and ethane as the substrate, we cultured microbial consortia of a novel anaerobic ethane oxidizer, "Candidatus Ethanoperedens thermophilum" (GoM-Arc1 Glade), and its partner bacterium "Candidatus Desulfofervidus auxilii," previously known from methane-o...
Methyl‐coenzyme M reductase (MCR) has been originally identified to catalyse the final step of the m...
The anaerobic formation and oxidation of methane involve unique enzymatic mechanisms and cofactors, ...
The deep ocean and its sediments are a continuous source of non-methane short-chain alkanes (SCAs) i...
Cold seeps and hydrothermal vents deliver large amounts of methane and other gaseous alkanes into ma...
Cold seeps and hydrothermal vents deliver large amounts of methane and other gaseous alkanes into ma...
Ethane is the second most abundant component of natural gas in addition to methane, and—similar to m...
In deep sediment layers, geothermal heat degrades organic matter into a complex mix of hydrocarbons....
Crude oil and gases in the seabed provide an important energy source for subsurface microorganisms. ...
ABSTRACT Crude oil and gases in the seabed provide an important energy source for subsurface microor...
Oil-rich sediments from the Gulf of Mexico were found to contain diverse alkane-degrading groups of ...
Crude oil and natural gas are formed due to the degradation of the organic matter in deep subsurface...
The anaerobic formation and oxidation of methane involve unique enzymatic mechanisms and cofactors, ...
Ethane, the second most abundant hydrocarbon gas in the seafloor, is efficiently oxidized by anaerob...
Alkanes are saturated apolar hydrocarbons that range from its simplest form, methane, to high-molecu...
Methyl-coenzyme M reductase (MCR) has been originally identified to catalyse the final step of the m...
Methyl‐coenzyme M reductase (MCR) has been originally identified to catalyse the final step of the m...
The anaerobic formation and oxidation of methane involve unique enzymatic mechanisms and cofactors, ...
The deep ocean and its sediments are a continuous source of non-methane short-chain alkanes (SCAs) i...
Cold seeps and hydrothermal vents deliver large amounts of methane and other gaseous alkanes into ma...
Cold seeps and hydrothermal vents deliver large amounts of methane and other gaseous alkanes into ma...
Ethane is the second most abundant component of natural gas in addition to methane, and—similar to m...
In deep sediment layers, geothermal heat degrades organic matter into a complex mix of hydrocarbons....
Crude oil and gases in the seabed provide an important energy source for subsurface microorganisms. ...
ABSTRACT Crude oil and gases in the seabed provide an important energy source for subsurface microor...
Oil-rich sediments from the Gulf of Mexico were found to contain diverse alkane-degrading groups of ...
Crude oil and natural gas are formed due to the degradation of the organic matter in deep subsurface...
The anaerobic formation and oxidation of methane involve unique enzymatic mechanisms and cofactors, ...
Ethane, the second most abundant hydrocarbon gas in the seafloor, is efficiently oxidized by anaerob...
Alkanes are saturated apolar hydrocarbons that range from its simplest form, methane, to high-molecu...
Methyl-coenzyme M reductase (MCR) has been originally identified to catalyse the final step of the m...
Methyl‐coenzyme M reductase (MCR) has been originally identified to catalyse the final step of the m...
The anaerobic formation and oxidation of methane involve unique enzymatic mechanisms and cofactors, ...
The deep ocean and its sediments are a continuous source of non-methane short-chain alkanes (SCAs) i...