Population Dynamics of Soil and Vegetation Protozoa

Many fresh-water protozoa can be found in litters and soils,but the ubiquitous species are those which are able to copewith fluctuating moisture conditions. Terrestrial protozoa aremore characteristic of bryophyte-soil habitats than aquaticecosystems. Nutritionally, two groups have evolved in responseto the plant community: naked, predominantly bacterial feeders,whose abundance is determined by the decomposability of thelitter in which they live; and the slow growing, humusassociatedtestacea, which are more abundant in the litters of slow decomposability.Ubiquitous species comprise about 90% of the protozoa in soils.More continuous moisture conditions enhance the appearance ofadditional species. Hence species diversity indicates highermoisture content of a soil. Protozoa may contribute to the functioningof the soil ecosystem by inducing fiocculation of bacterialpopulations and recycling of minerals through ingestion of bacteriaand excretion of soluble products. The surface of vegetationappears to represent the most terrestrial habitat a protozoancan exploit, because in contrast to the litter-soil ecosystem,only one species, Colpoda cucullus, dominates the population.     

Interstitial Protozoa and Algae of Louisiana Salt Marshes

SYNOPSIS. The majority of Louisiana salt marshes consists of stagnant pools among a vegetation of Spartina spp. and Distichlis spicata. The sediments constitute a "sulphide biome,'with Eh values reaching to –350 mV. The 200 interstitial ciliate species had definite stratification. Generally, algivores and omnivores occurred in the upper, and bactivores in the lower layers of the sediments. Compaction of particles prevented the flexible and large ciliates from inhabiting the lower layers, while Eh below –200 mV limited the distribution of some species but favored certain bactivores. The pH/Eh range and the abundance of nutrients in the sulfide biome provide habitable conditions for all the major groups of microflora. These, in turn, support nutritionally diverse predatory ciliate populations.     

The Numbers and Proportions of Testacea and Ciliates in Litters and Soils

SYNOPSIS. The numbers and kinds of testacea and ciliates were studied in the litters and soils of 23 sites, from temperate and subtropical coniferous and deciduous forests, and grasslands. In coniferous forests, testacea were 10 times or more abundant than ciliates, and numbered 10,000–24,000/g (wet weight) in litters and up to 8,000/g in soils. Ciliates numbered up to 1,500/g, but averaged less than 600/g in litters and less than 300/g in soils. Under deciduous vegetation, ciliates approached, equaled, or exceeded testacea, and numbered 1,000–5,000/g in litters, while remaining about the same in soils. Temperature and soil influence vegetation types, and their rates of litter decay affect the protozoa. Moisture favors numerical dominance of certain species. Among testacea, several species dominate in a particular habitat; among ciliates, the genus Colpoda dominates in almost all litter and soil habitats.     

Protist Biogeography1

Autecology (cellular organelles and secretions, encystment and dispersal abilities), environmental conditions (physiological tolerances and interaction with other organisms), and evolutionary history contribute to protist biogeography, which manifests ecological and historical aspects. Ecological biogeography is seen in the influence of geochemistry on the distribution of fresh-water phytoflagellates and algae, and of moisture and vegetation type on soil-litter protists. A temporal feature is often present because many protists encyst and respond only to certain ranges of temperature and organic content. Historical biogeography has occurred by radiative host evolution on symbiotic protozoa (e.g., termite flagellates and rumen ciliates), and by the isolating effects of water currents, temperature, and density gradients on oceanic protists (coccoliths, dinoflagellates, foraminifera, radiolaria, and tintinnines). These two aspects combine in protists living on animal surfaces. Humans affect protist biogeography by increasing parasite ranges through human migrations and by water pollution. They can diminish these situations by disease control and exploiting appropriate ciliates in sewage disposal. Many free-living protozoa appear to be cosmopolitan, but mating types and isoenzyme studies suggest that speciation with its geographic connotations may be more widespread than presently appreciated.     

Symposium on “Protozoan Ecology”: The Role of Protozoa in Litters and Soils1

Soil is the focus of organic matter turnover in terrestrial ecosystems and is an interstitial mosaic of microsites composed of particle aggregates and pore spaces, where transformation, decomposition, mineralization, and humification of organic matter takes place. Microorganisms and animals are scattered discontinuously in these microsites. Microarthropods and larger fauna increase the rate and amount of mineralization by comminution of organic matter and by redistribution of microsites through movements of earthworms and large arthropods; however, mineralization and return of nutrients to plants occurs in the community of bacteria, fungi, protozoa, and nematodes living in the water films covering aggregates and filling pore spaces. Protozoa, especially small amoebae, are important bacterial grazers because they can enter tiny spaces unavailable to nematodes. The latter graze bacteria, fungi, and protozoa. Protozoan and nematode predation increase the amounts of soluble nutrients and decrease the competitive abilities of bacteria, thus making these nutrients more available to plants. Protozoa enhance nutrient recycling out of proportion to their biomass.