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  2. Atmospheric methane - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_methane

    Methane oxidation allows methanotrophic bacteria to use methane as a source of energy, reacting methane with oxygen and as a result producing carbon dioxide and water. CH 4 + 2O 2 → CO 2 + 2H 2 O Forest soils act as good sinks for atmospheric methane because soils are optimally moist for methanotroph activity, and the movement of gases ...

  3. Atmospheric carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_carbon_cycle

    Methane (CH 4) is one of the more potent greenhouse gases and is mainly produced by the digestion or decay of biological organisms. It is considered the second most important greenhouse gas, [10] yet the methane cycle in the atmosphere is currently only poorly understood. [11] The amount of methane produced and absorbed yearly varies widely. [10]

  4. Atmospheric methane removal - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_methane_removal

    Methane has a limited atmospheric lifetime, about 10 years, due to substantial methane sinks. The primary methane sink is atmospheric oxidation, from hydroxyl radicals (~90% of the total sink) and chlorine radicals (0-5% of the total sink). The rest is consumed by methanotrophs and other methane-oxidizing bacteria and archaea in soils (~5%). [5]

  5. Sulfate-methane transition zone - Wikipedia

    en.wikipedia.org/wiki/Sulfate-methane_transition...

    The SMTZ is a major sink for methane because AOM consumes mostly all of the methane produced by methanogens. [7] It has been shown that AOM takes up over 90 percent of all the methane produced in the ocean. [12] Since methane is a prominent greenhouse gas, AOM is especially vital to controlling the amount of greenhouse gases in the atmosphere. [13]

  6. Biological pump - Wikipedia

    en.wikipedia.org/wiki/Biological_pump

    Lakes are net emitters of methane, and organic and inorganic carbon (dissolved and particulate) flow into the ocean through freshwater systems. In the ocean, methane can be released from thawing subsea permafrost, and CO 2 is absorbed due to an undersaturation of CO 2 in the water compared with the atmosphere. In addition, multiple fluxes are ...

  7. The Summary. This was the Arctic’s second-hottest year on record, according to a new NOAA report. The tundra has become a source of emissions, rather than a carbon sink, the authors said.

  8. Cold seep - Wikipedia

    en.wikipedia.org/wiki/Cold_seep

    The benthic filter cannot affect methane that is not traveling through the sediment. Methane can bypass the benthic filter if it bubbles to the surface or travels through cracks and fissures in the sediment. [7] These organisms are the only biological sink of methane in the ocean. [8]

  9. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water is the medium of the oceans, the medium which carries all the substances and elements involved in the marine biogeochemical cycles. Water as found in nature almost always includes dissolved substances, so water has been described as the "universal solvent" for its ability to dissolve so many substances.