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soil microbiology
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 oceans. These bacteria could fix nitrogen, in time multiplied and as a result released oxygen into the atmosphere. This led to more advanced microorganisms. Microorganisms in soil are important because they affect soil structure and fertility. Soil microorganisms can be classified as bacteria, actinomycetes, fungi, algae and protozoa. Each of these groups has characteristics that define them and their functions in soil.〔Rao, Subba. Soil Microbiology. Fourth ed. Enfield: Science Publishers, 1999. Print.〕
Up to 10 billion bacterial cells inhabit each gram of soil in and around plant roots, a region known as the rhizosphere. In 2011, a team detected more than 33,000 bacterial and archaeal species on sugar beet roots.
The composition of the rhizobiome can change rapidly in response to changes in the surrounding environment.
== Bacteria ==
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 ability to reproduce sexually. A prokaryote has a very simple cell structure with no internal organelles.〔 Bacteria and archaea are the most abundant microorganisms in the soil, and serve many important purposes, including nitrogen fixation.〔Wood, Martin. Soil Biology. New York: Chapman and Hall, 1989. Print〕
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