Nitrogen Fixation and the Nitrogen Cycle
In
a symbiotic relationship with the soil bacteria known as 'rhizobia', legumes
form nodules on their roots (or stems, see figure below) to 'fix' nitrogen into
a form usable by plants (and animals). The process of biological nitrogen
fixation was discovered by the Dutch microbiologist Martinus Beijerinck.
Rhizobia (e.g., Rhizobium, Mesorhizobium, Sinorhizobium) fix atmospheric
nitrogen or dinitrogen, N2, into inorganic nitrogen compounds, such
as ammonium, NH4+, which is then incorporated into amino
acids, which can be utilized by the plant. Plants cannot fix nitrogen on their
own, but need it in one form or another to make amino acids and proteins.
Because legumes form nodules with rhizobia, they have high levels of nitrogen
available to them. Their abundance of nitrogen is beneficial not only to the
legumes themselves, but also to the plants around them. There are other sources
of nitrogen in the soil, but are not always provided at the levels required by
plants, making the symbiotic relationship between legumes and rhizobia highly
beneficial. In return for the fixed nitrogen that they provide, the rhizobia
are provided shelter inside of the plant's nodules and some of the carbon
substrates and micronutrients that they need to generate energy and key
metabolites for the cellular processes that sustain life (Sprent, 2001).
Nodulation and nitrogen fixation by rhizobia is not exclusive to legumes;
rhizobia form root nodules on Parasponis Miq., a genus of five species
in the Ulmaceae (see 'Rosales').
The picture on the left shows
typical root nodules, these from bur clover (Medicago). The picture on
the right shows "stem" nodules on Sesbania rostrata - stem
nodules are produced from lateral or adventitious roots and are typically found
in those few water-tolerant legume groups (Neptunia, Sesbania) that
prefer wet or water-logged soils (Goormachtig et al., 2004).
The nitrogen cycle (shown below)
describes the series of processes by which the element nitrogen, which makes up
about 78% of the Earth’s atmosphere, cycles between the atmosphere and the
biosphere. Plants, bacteria, animals, and manmade and natural phenomena all
play a role in the nitrogen cycle. The fixation of nitrogen, in which the
gaseous form dinitrogen, N2) is converted into forms usable by
living organisms, occurs as a consequence of atmospheric processes such as
lightning, but most fixation is carried out by free-living and symbiotic
bacteria. Plants and bacteria participate in symbiosis such as the one between
legumes and rhizobia or contribute through decomposition and other soil
reactions. Bacteria like Rhizobium, or the actinomycete Frankia
which nodulates members of the plant families Rosaceae and Betulaceae, utilize
atmospheric nitrogen and convert it to an inorganic form (usually ammonium, NH4+)
that plants can use. The plants then use the fixed nitrogen to produce vital
cellular products such as proteins. The plants are then eaten by animals, which
also need nitrogen to make amino acids and proteins. Decomposers acting on
plant and animal materials and waste return nitrogen back to the soil.
Human-produced fertilizers are another source of nitrogen in the soil along
with pollution and volcanic emissions, which release nitrogen into the air in
the form of ammonium and nitrate gases. The gases react with the water in the
atmosphere and are absorbed by the soil with rain water. Other bacteria in the
soil are key components in this cycle converting nitrogen containing compounds
to ammonia, NH3, nitrates, NO3-, and nitrites,
NO2-. Nitrogen is returned back to the atmosphere by
denitrifying bacteria, which convert nitrates to dinitrogen gas.
The Nitrogen Cycle. This image is a
work of an Environmental Protection Agency employee, taken or made during the
course of an employee's official duties. As works of the U.S.federal
government, all EPA images are in the public domain. The nitrogen cycle.
Goormachtig, S., W. Capoen, and M.
Holsters. 2004. Rhizobium infection: lessons from the versatile
nodulation behaviour of water-tolerant legumes. Trends in Plant Science 9:
518-522.
Sprent, J.I. 2001. Nodulation in
Legumes. Royal Botanic Gardens, Kew, UK.



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