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  2. Cable bacteria - Wikipedia

    en.wikipedia.org/wiki/Cable_bacteria

    Hydrogen sulfide (H 2 S) is oxidized in the sulfidic sediment layer, and the resulting electrons (e −) are conducted up through the cable bacteria filament to the oxic layer and used to reduce molecular oxygen (O 2). Cable bacteria are filamentous bacteria that conduct electricity across distances over 1 cm in sediment and groundwater aquifers.

  3. Soil microbiology - Wikipedia

    en.wikipedia.org/wiki/Soil_Microbiology

    These bacteria could fix nitrogen, in time multiplied, and as a result released oxygen into the atmosphere. [2] [3] This led to more advanced microorganisms, [4] [5] which are important because they affect soil structure and fertility. Soil microorganisms can be classified as bacteria, actinomycetes, fungi, algae and protozoa. Each of these ...

  4. Iron-oxidizing bacteria - Wikipedia

    en.wikipedia.org/wiki/Iron-oxidizing_bacteria

    The anoxygenic phototrophic iron oxidation was the first anaerobic metabolism to be described within the iron anaerobic oxidation metabolism. The photoferrotrophic bacteria use Fe 2+ as electron donor and the energy from light to assimilate CO 2 into biomass through the Calvin Benson-Bassam cycle (or rTCA cycle) in a neutrophilic environment (pH 5.5-7.2), producing Fe 3+ oxides as a waste ...

  5. Soil biology - Wikipedia

    en.wikipedia.org/wiki/Soil_biology

    Bacteria live in soil water, including the film of moisture surrounding soil particles, and some are able to swim by means of flagella. The majority of the beneficial soil-dwelling bacteria need oxygen (and are thus termed aerobic bacteria), whilst those that do not require air are referred to as anaerobic , and tend to cause putrefaction of ...

  6. Electric bacteria - Wikipedia

    en.wikipedia.org/wiki/Electric_bacteria

    Electric bacteria are forms of bacteria that directly consume and excrete electrons at different energy potentials without requiring the metabolization of any sugars or other nutrients. [1] This form of life appears to be especially adapted to low-oxygen environments. Most life forms require an oxygen environment in which to release the excess ...

  7. Biological carbon fixation - Wikipedia

    en.wikipedia.org/wiki/Biological_carbon_fixation

    Cyanobacteria such as these carry out photosynthesis.Their emergence foreshadowed the evolution of many photosynthetic plants and oxygenated Earth's atmosphere.. Biological carbon fixation, or сarbon assimilation, is the process by which living organisms convert inorganic carbon (particularly carbon dioxide, CO 2) to organic compounds.

  8. Methanogenesis - Wikipedia

    en.wikipedia.org/wiki/Methanogenesis

    Methanogens do not use oxygen to respire; in fact, oxygen inhibits the growth of methanogens. The terminal electron acceptor in methanogenesis is not oxygen, but carbon. The two best described pathways involve the use of acetic acid (acetoclastic) or inorganic carbon dioxide (hydrogenotrophic) as terminal electron acceptors:

  9. Microbiology of decomposition - Wikipedia

    en.wikipedia.org/wiki/Microbiology_of_decomposition

    As oxygen is present within a body at the beginning of decomposition, aerobic bacteria flourish during the first stages of the process. As the microbial population increases, an accumulation of gases changes the environment into anaerobic conditions which is consequently followed by a change to anaerobic bacteria . [ 4 ]

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