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Termites and Biogeochemical Cycling
Termites and Biogeochemical Cycling
In addition to being an economically important pest, termites are also important
ecologically to forest ecosystems. They are closely linked with biogeochemical
(nutrient) cycling. The major biogeochemical cycles are: hydrologic, carbon,
oxygen, nitrogen, sulfur, and phosphorus (Staley and Orians 1992). Components
of each conceptually belong to "reservoir pools". Depending on the scale,
reservoir pools may include all or part of the atmosphere, the ocean, the
sediments, and living organisms. In general, flux between reservoirs is dominated
by the biota and their activities. Elements are exchanged slowly between
some reservoirs over a long period of geological time (Rodhe 1992).
Termites are important in the carbon cycle through their roles as consumers
and detritivores (DeAngelis 1992). The termite gut is host to protozoan and
bacterial symbionts that are able to digest wood cellulose and thus release
the energy otherwise unavailable to the insects (Waller and La Fage 1987).
Termite foraging and tunnelling redistributes soil and increases the surface
area available to bacteria and fungi (Wood and Sands 1978). The breakdown
of lignin and cellulose found in wood is primarily facilitated by the enzymatic
secretions of fungi (Bold et al. 1980). Fungi are also able to liberate various
elements such as nitrogen, phosphorus, potassium, sulfur, iron, calcium,
magnesium, and zinc (Bold et al. 1980). The ability of termites to influence
the physical structure and chemical nature of their environment impacts
vegetation and other components of the ecosystem (Wood and Sands 1978). Their
effect on the nitrogen cycle has traditionally been recognized as returning
nutrients to the ecosystem. However, recent studies indicate that termites
may play a larger role in the cycling of nitrogen than was once thought.
The atmosphere is composed of 78% nitrogen as N2 gas. This represents
a reservoir pool for nitrogen in terrestrial ecosystems. Biota cannot use
this element until it is "fixed" into useable forms. Nitrogen fixation most
commonly occurs in two ways: lightning accounts for the fixation of 10% of
global available nitrogen and the other 90% of fixed nitrogen is generated
from the action of microbes. Free living bacteria, cyanobacteria, and symbiotic
bacteria in nodules in the low O2 environment within heterocysts
of leguminous plants are all involved in microbial nitrogen fixation (Jaffe
1992). However, there is another place where nitrogen fixation occurs.
The microbial gut flora of termites include nitrogen fixing bacteria (Benemann
1973, Breznak et al. 1973, French et al. 1976, Potrikus and Breznak 1977,
Prestwich and Bentley 1981). The rate at which nitrogen is fixed varies among
termite species (Prestwich et al. 1980, Breznak 1984, Bentley 1987, Waller
et al. 1989) and within species as a function of food quality (Breznak et
al. 1973), termite caste (Prestwich et al. 1980, Hewitt et al. 1987), and
termite size (Waller et al. 1989). Intraspecific variation may also exist
due to seasonal factors (Pandey et al. 1992, Waller et al. 1989). Newly fixed
nitrogen is incorporated into termite tissue, excretion products, and secretion
products (Bentley 1984).
References
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Bentley, B. L. 1984. Nitrogen fixation in termites:
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Bentley, B. L. 1987. Nitrogen fixation by Nasutitermes
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Bold, H. C., C. J. Alexopoulos and T. Delevoryas. 1980.
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French, J. R. J., G. L. Turner and J. F. Bradbury. 1976.
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Hewitt, P. H., M. C. Van der Westhuizen, T. C. De K. Van
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Copyright © Anthony Curtis, Ph.D.
1996-2007. All Rights Reserved. Do not duplicate without
permission.
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