Soil microbiology

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Soil microbiology is the study of organisms in soil, their functions, and how they affect soil properties. It is believed that between two and four billion years ago, the first ancient bacteria and microorganisms came about in Earth's primitive seas. These bacteria could fix nitrogen, in time multiplied and as a result released oxygen into the atmosphere. This release of oxygen led to more advanced microorganisms. Microorganisms in soil are important because they affect the structure and fertility of different soils. Soil microorganisms can be classified as bacteria, actinomycetes, fungi, algae, and protozoa. Each of these groups has different characteristics that define the organisms and different functions in the soil it lives in.[1]

Bacteria[edit]

Bacteria and Archaea are the smallest organisms in soil apart from viruses. Bacteria and Archaea are prokaryotic. All of the other microorganisms are eukaryotic, which means they have a more advanced cell structure with internal organelles and the advanced ability to reproduce sexually. A prokaryote has a very simple cell structure with no internal organelles.[1] Bacteria and archaea are the most abundant microorganisms in the soil, and serve many important purposes, one of those being nitrogen fixation among other biochemical processes.[2]

Biochemical processes[edit]

One of the most distinguished features of bacteria as a whole is their biochemical versatility. A bacterial genera called Pseudomonas can metabolize a wide range of chemicals and fertilizers. In contrast, another genera known as Nitrobacter can only derive its energy by turning nitrite into nitrate, which results in a gain of oxygen and is known also as oxidation. Furthermore, the genera Clostridium is also an example of bacteria’s versatility because it, unlike most species, can actually grow in the absence of oxygen, respiring anaerobically. Several species of Pseudomonas, such as Pseudomonas aeruginosa are able to respire both aerobically and anaerobically, using nitrate, as the terminal electron acceptor..[2]

Nitrogen fixation[edit]

Bacteria are responsible for the process of nitrogen fixation, which is the conversion of atmospheric nitrogen into nitrogen-containing compounds (like ammonia) which can be used by plants to uptake. Autotrophic bacteria are bacteria that derive their energy by making their own food though oxidation, like the Nitrobacters species, rather than feeding on plants or other organisms. These bacteria are responsible for nitrogen fixation, and the amount of autotrophic bacteria is small compared to heterotrophic bacteria (the opposite of autotrophic bacteria, heterotrophic bacteria acquires energy by consuming plants or other microorganisms), but are very important because almost every plant and organism requires nitrogen in some way, and would have no way of obtaining it if not for nitrogen-fixing bacteria.[1]

Actinomycetes[edit]

Actinomycetes are soil microorganisms. They are a type of bacteria. They are similar to both bacteria and fungi, and have characteristics linking them to both groups. Actinomycetes are often believed to be the missing evolutionary link between bacteria and fungi, but they have many more characteristics in common with bacteria than they do fungi.[3]

Similar to bacteria[edit]

Actinomycetes are similar to bacteria because they, like bacteria, are prokaryotic, are sensitive to antibacterial and affected in the same way that bacteria is by them. Actinomycetes can hardly be distinguished from bacteria at its early stages because of how much they resemble bacteria in size, shape and gram-staining properties. Gram staining is a common technique used to classify organisms into two main groups: Gram-positive and Gram-negative, by staining organisms to distinguish its cell wall properties. Gram-positive means that the cell has a thick cell wall and gram-negative means the opposite, that the cell wall is thin. Cell wall properties can help distinguish different types of microorganisms from each other.[1]

Similar to fungi[edit]

Actinomycetes are most commonly linked to fungi, but they do share some characteristics with fungi. Actinomycetes are similar to fungi by their shape and branching properties, spore formation, which related to how fungi and actinomycetes reproduce by forming spores and duplicating.

Ability to produce antibiotics[edit]

One of the most notable characteristics of the actinomycetes is their ability to produce antibiotics. Streptomycin, neomycin, erythromycin and tetracyclin are only a few examples of the antibiotics derived from actinomycetes. Streptomycin is used to treat tuberculosis and infections caused by certain bacteria and neomycin is used to reduce the risk of bacterial infection during surgery. Erythromycin is a very important antibiotic that is used to treat certain infections caused by bacteria, such as bronchitis, pertussis whooping cough, pneumonia and ear, intestine, lung, urinary tract, and skin infections. This ability to produce these useful antibiotics is the basis of our entire pharmaceutical industry and has saved human lives.

Fungi[edit]

Next to bacteria, fungi are abundant in soil population, but bacteria are more abundant than other microorganisms, including fungi. Fungi are important in the soil as food sources for other, larger organisms, pathogens, beneficial symbiotic relationships with plants or other organisms and help to reduce crop residues and biochemically process nutrients to improve the soil they inhabit. Fungi can be split into different species based on primarily on the size, shape and color of their spores, which are used to reproduce. Most of the environmental factors that influence the growth and distribution of bacteria and actinomycetes also influence fungi. The quality as well as quantity of organic matter in the soil has a direct correlation to the growth of fungi, because most fungi consume the organic matter for nutrition. Fungi thrive in acidic environments, while bacteria and actinomycetes cannot survive in acid, which results in an abundance of fungi in acidic areas. Fungi also grows well in dry, arid soils because fungi are aerobic, or dependent on oxygen, and the higher the moisture content in the soil, the less oxygen is present for fungi.

Algae[edit]

Algae can make its own nutrients through a process known as photosynthesis. Photosynthesis is when light energy is converted to chemical energy that can be stored as nutrients. For algae to grow, it must be exposed to areas of light because photosynthesis requires light, so algae is typically distributed evenly wherever sunlight and moderate moisture is available. Algae, however, do not have to be on the soil surface or directly exposed to sun rays, but it can live below the soil surface as long as the algae has uniform temperature and moisture conditions. Bacteria are not the only organism that can fix nitrogen, because algae are capable of performing nitrogen fixation as well.[1]

Types[edit]

Algae can be split up into three main groups: the Cyanophycease, the Chlorophycease, and the Bacillariacease. The Cyanophycease contain chlorophyll, which is the molecule that absorbs sunlight and uses that energy to make carbohydrates from carbon dioxide and water, and also pigments that make it blue-green to violet in color. The Chlorophycease usually only has chlorophyll in it which makes it green, and the Bacillariacease contains chlorophyll as well as pigments that make the algae brown in color.[1]

Blue-green algae and nitrogen fixation[edit]

Blue-green algae, or Cyanophycease, are the algae that are responsible for nitrogen fixation. The amount of nitrogen fixed by these algae depends more on physiological and environmental factors rather than the organism’s abilities. Some of these factors include intensity of sunlight, concentration of inorganic and organic nitrogen sources, and temperature and stability of the environment.[3]

Protozoa[edit]

Protozoa are eukaryotic organisms which are some of the first microorganisms to develop a means of sexual reproduction, which is a huge evolutionary step from duplication of spores, like many of the other soil microorganisms depend on. Protozoa can be split up into three categories: flagellates, amoebae, and ciliates.[3]

Flagellates[edit]

Flagellates are the smallest members of the protozoa group, and can be divided further based on whether they can participate in photosynthesis. Nonchlorophyll-containing flagellates are not capable of photosynthesis because chlorophyll is the green pigment that absorbs sunlight in the process. These flagellates are found mostly in soil and flagellates that contain chlorophyll typically occur in aquatic conditions. Flagellates can be distinguished by their flagella, which is their means of movement. Some have several flagella, and other species only have one, but it resembles a long branch or appendage that helps the flagella move.[3]

Amoebae[edit]

Amoebae are larger than flagellates and move in a different way. Amoebae can be distinguished from other protozoa by their slug-like properties and pseudopodia. A pseudopodia or “false foot” is a temporary obtrusion from the body of the Amoebae that helps pull it along surfaces for movement or helps to pull in food. The amoebae does not have permanent appendages and the pseudopodia is more of a slime-like consistency than a flagella.[3]

Ciliates[edit]

Ciliates are the largest of the protozoa group, and move by means of short, numerous cilia that produce beating movements. Cilia resembles small, short hairs, and they can move in different directions to propel the organism in different direction, giving it more mobility than flagellates or amoebae are capable of.[3]

It is important to understand the many different groups and species of microorganisms in different soils because they affect so much of the soil. Microorganisms contribute to nutrient availability in soil, manage soil stability by means of different biochemical processes such as nitrogen fixation, and they contribute to the growth and success of the plants and overall ecosystem of a soil environment.

Soil microbiologists[edit]

References[edit]

  1. ^ a b c d e f Rao, Subba. Soil Microbiology. Fourth ed. Enfield: Science Publishers, 1999. Print.
  2. ^ a b Wood, Martin. Soil Biology. New York: Chapman and Hall, 1989. Print
  3. ^ a b c d e f Sylvia, David M., Jeffry J. Fuhrmann, Peter G. Hartel, and David A. Zuberer. Principles and Applications of Soil Micobiology. Upper Saddle River: Prentice Hall, 1998. Print.