Distribution of different types of
soil microorganisms
Soils
contain five major groups of microorganisms. They are bacteria, actinomycetes,
fungi, algae and protozoa. Among the soil microorganisms, bacteria are most
dominant group of organisms. All kinds of bacteria are found in the soil. This
is because all kinds of organic refuse are disposed off on the soil. Many of
the soil bacteria perform useful functions like decomposition of organic
matter, conver-sion of soil constituents into useful materials, production of
antibiotics in the soil, and biogeochemical cycling of elements like carbon,
nitro-gen, phosphorus, iron, sulfur and manganese.
The
bacterial population of the soil exceeds the population of all other groups of
microorganisms in both number and variety. Direct microscopic counts as high as
several billions bacteria per a gram of soil have been reported.
The
actinomycetes population as many as millions per gram of soil is present. The
most predominant genera present in the soil are Nocardia, Streptomyces and
Micromonospora. These organisms areresponsible for the characteristic musty
or earthy odour soon after the rainfall. This is due to sporulation of
actinomycetes. Actinomycetes are capable of degrading many complex organic substances
and con-sequently play an important role in building soil fertility. The
actino-mycetes have ability to synthesize and excrete antibiotics. Most of the
antibiotics are produced by actinomycetes. The presence of antibiotic
substances in soil can be detected with great difficulty.
The
fungal population ranging from thousands to hundred thou-sands per gram of soil
has been reported. They are aerobic in nature and found more numbers near the
earth surface. They exist in the atmosphere as mycelial and spore stage. Fungi
are active in decom-posing the major constituents of plant tissues, namely,
cellulose, hemi-cellulose, lignin and pectin.
The
population of algae in soil is very smaller than that of either bacteria or
fungi. The major types present in the soil are the greenalgae and diatoms.
Their photosynthetic nature accounts for their pre-dominance on the surface or
just below the surface layer of soil. In a fertile soil biochemical activities
of algae are masked by bacteria and fungi. In certain conditions, algae perform
prominent and beneficial changes. For example, on barren and eroded lands they
may initiate the accumulation of organic matter because of their ability to
carry out photosynthesis and other metabolic activities.
Many
soil protozoa are flagellates or amoebas; the population per gram soil ranges
from a few hundred to several thousand in moist soils rich in organic matter.
Protozoa are of significance since their dominant mode of nutrition involves
ingestion of bacteria.
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