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They form on areas of the seafloor distant enough from land so that the slow but steady deposition of dead microorganisms from overlying waters is not obscured by sediments washed from the land.
Accumulation of atmospheric particles and dead microorganisms (algae) constitutes the major portion of humus.
Both living and dead microorganisms had been used in past to remove metal from liquid phase (Malik 2004; Liu et al. 2004; Wang and Chen 2009).
The TiO2/UV process does not only inactivate microorganisms, but also induces the mineralization of organic matter such as dead microorganisms [10,11].
The dead microorganisms might have increased the availability of carbon in the soil that caused an increased activity of both enzymes related to the C-cycle.
In biosorption, either live or dead microorganisms or their derivatives are used, which complex metal ions through the functioning of ligands or functional groups located on the outer surface of the cell [2].
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Usually, dead microorganism binds with the heavy metal ion through physiochemical mechanism.
These cellular entities provide negatively charged functional groups like carboxylate, hydroxyl, sulfate, phosphate and amino groups on the surface of dead microorganism.
Plants may favorably or adversely affect other plants through allelochemicals, which may be released directly or indirectly from live or dead plants (including microorganisms).
To get a better insight into the cenosis-forming role of microalgae, a mathematical model of the "autotroph heterotroph" aquatic biotic cycle has been constructed, taking into account the utilization of Chlorella photosynthates and dead cells by microorganisms and the contribution of the components to the nitrogen cycle.
First, the discrimination of dead or alive microorganisms represents a crucial problem in (environmental) bacteriology.
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