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  2. 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 ...

  3. 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 ...

  4. Soil respiration - Wikipedia

    en.wikipedia.org/wiki/Soil_respiration

    Soil animals graze on populations of bacteria and fungi as well as ingest and break up litter to increase soil respiration. Microfauna are made up of the smallest soil animals. These include nematodes and mites. This group specializes on soil bacteria and fungi.

  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. 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 ]

  7. Azotobacter - Wikipedia

    en.wikipedia.org/wiki/Azotobacter

    Bacteria of the genus Azotobacter are also known to form intracellular inclusions of polyhydroxyalkanoates under certain environmental conditions (e.g. lack of elements such as phosphorus, nitrogen, or oxygen combined with an excessive supply of carbon sources).

  8. Rhizobacteria - Wikipedia

    en.wikipedia.org/wiki/Rhizobacteria

    The rhizobacteria require oxygen to metabolize, so oxygen is provided by a hemoglobin protein called leghemoglobin which is produced within the nodules. [4] Legumes are well-known nitrogen-fixing crops and have been used for centuries in crop rotation to maintain the health of the soil.

  9. Obligate aerobe - Wikipedia

    en.wikipedia.org/wiki/Obligate_aerobe

    A unique obligate aerobe is Streptomyces coelicolor which is gram-positive, soil-dwelling, and belongs to the phylum Actinomycetota. [7] It is unique because the genome of this obligate aerobe encodes numerous enzymes with functions that are usually attributed to anaerobic metabolism in facultatively and strictly anaerobic bacteria .