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Index >> Fundamentals of Microbial Ecology >> Bio-Geochemical Cycle(BGC)

Bio-Geochemical Cycle(BGC)

Bio-geochemical Cycle (BGC)
Bio-geochemical cycling describes the movement and conversion of materials by biochemical activities throughout the atmosphere, hydrosphere and lithosphere. A cycle can be described in terms of pools of the substances concerned, so that there is perhaps a pool of soluble material (biotic), a pool of organically bound material and an abiotic atmospheric pool of the gaseous form.

BGC cycles include physical transformation (precipitation, fixation, etc.), chemical transformation (biosynthesis, biodegradation, etc.) and various combinations of physical and chemical changes.

All living organisms participate in the bio-geo chemical cycling but microbes play a major role in the process. In the BGC cycling, energy is absorbed, converted, temporarily stored and eventually dissipated (energy flows through the ecosystem). This flow of energy is fundamental to the functioning of ecosystem.
When energies flow through the ecosystem, materials undergo cyclic conversions that tend to retain materials within the ecosystem. The cyclic nature of material conversions leads to dynamic equilibrium between various forms of cycled materials.

The BGC cycles usually include negative feedback control mechanisms so that any abnormally high pool level corrects itself and the system returns to the equilibrium state.

Most elements are subjects to some degree of BGC cycling. The intensity or rate of BGC cycling for each element roughly correlates to the amount of the element in the chemical composition of the biomass.

The major elemental composition of living organisms (C, H, O, N, P and S) are cycled more intensely, and trace elements (B, Co, Cr, cu) and microelements (Mg, Na, K) which are required in small quantities are cycled less intensely.

Microorganisms also act as sources of particular compounds in the ecosphere and sinks for others. Transfer rate between pools vary and are generally enzyme- mediated.

Reservoirs The various chemical forms of a particular element constitute so called pools or reservoirs and the reservoir sizes can vary greatly from habitat to habitat. Reservoir size is an extremely important parameter to be considered in connection with possible distribution of a cycling system.

In BGC cycling, small, actively cycled reservoirs are the most prone to disturbances by either natural or human causes.

 

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