Algae occur in nearly all terrestrial environments on earth and are invariably encountered both on and beneath soil surfaces. The algal flora of the soil includes members of the Cyanochloronta, Chlorophycophyta, Euglenophycophyta, Chrysophycophyta, and Rhodophycophyta. Thirty-eight genera of prokaryotic and 147 genera of eukaryotic algae include terrestrial species, the majority of which are edaphic. Whereas systematic nomenclature of blue-green algae adheres to traditional classification based upon morphological features, proper taxonomic treatment of eukaryotic soil algae is predicated on standard methods of culture and interpretation of physiological attributes, plant mass characteristics, and morphological properties of axenic clones. While knowledge of the physiological ecology of soil algae is primarily based on laboratory evidence, it is well established that solar radiation, water, and temperature are the most important abiotic factors governing their distribution, metabolism, and life history strategies. Biotic interactions are often as important, whereas ionic factors (including pH), oxidation-reduction potential, and soil texture are less important, if only because their influences are less well understood. Algae play an important role in primary and secondary plant community succession by acting as an integral part of the colonial synusium. The principal functional attributes of algal communities in soil include primary production, dinitrogen fixation, and stabilization of aggregates. Although as many as 108 algae per gram have been documented, soils commonly support between 103 and 104 per gram. As an avenue for the incorporation of carbon and nitrogen and for minimizing erosion through stabilization of aggregates, algae are valuable in agriculture. Although manipulation of edaphic algal populations in temperate countries is of novel occurence, their successful use in India as a means for reclaiming saline soils and as a source of fertilizer nitrogen is well documented. Soil algae are affected by synthetic pesticides and pollutants. In general, most herbicides, fungicides, and soil fumigants are detrimental to soil algae while most insecticides are not. Algae have been utilized as biological assay organisms for anticipating crop response to both fertilizers and pesticides because of their biochemical similarity to higher plants and their quick generation time. As future research with soil algae leads to a greater awareness of their importance in soil, it might be anticipated that manipulation of populations in agricultural systems of temperate regions will become more widespread with consideration of the potential benefits of soil algae made by scientists in other disciplines.
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