| The Soil Biology Primer  Chapter 5:  SOIL PROTOZOABy Elaine R. Ingham THE LIVING SOIL:  PROTOZOAProtozoa are single-celled animals that feed primarily on bacteria, but 
      also eat other protozoa, soluble organic matter, and sometimes fungi. They 
      are several times larger than bacteria – ranging from 1/5000 to 1/50 of an 
      inch (5 to 500 µm) in diameter. As they eat bacteria, protozoa release 
      excess nitrogen that can then be used by plants and other members of the 
      food web. Protozoa are classified into three groups based on their shape:  
      Ciliates are the largest and move by means of hair-like cilia. 
      They eat the other two types of protozoa, as well as bacteria. 
      Amoebae also can be quite large and move by means of a temporary 
      foot or “pseudopod.”  Amoebae are further divided into testate 
      amoebae (which make a shell-like covering) and naked amoebae 
      (without a covering). Flagellates are the smallest of the 
      protozoa and use a few whip-like flagella to move. 
        
        
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          | Figure 1: Protozoa play an important role 
            in nutrient cycling by feeding intensively on bacteria. Notice the 
            size of the speck-like bacteria next to the oval protozoa and large, 
            angular sand particle. Credit: 
            Elaine R. Ingham
 | Figure 2: Bacteria ingested by an 
            amoeba. Credit:  No. 35 from 
            Soil Microbiology and Biochemistry Slide Set. 1976. J.P. 
            Martin, et al., eds. SSSA, Madison, WI
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          | Figure 3: Flagellates have one or two 
            flagella which they use to propel or pull their way through soil. A 
            flagellum can be seen extending from the protozoan on the left. The 
            tiny specks are bacteria. Credit: 
            Elaine R. Ingham
 | Figure 6: Ciliates are the largest of the 
            protozoa and the least numerous. They consume up to ten thousand 
            bacteria per day, and release plant available nitrogen. Ciliates use 
            the fine cilia along their bodies like oars to move rapidly through 
            soil. Credit: Elaine R. 
            Ingham
 |  WHAT DO PROTOZOA DO? Protozoa play an important role in mineralizing nutrients, 
      making them available for use by plants and other soil organisms. Protozoa 
      (and nematodes) have a lower concentration of nitrogen in their cells than 
      the bacteria they eat. (The ratio of carbon to nitrogen for protozoa is 
      10:1 or much more and 3:1 to 10:1 for bacteria.)  Bacteria eaten by 
      protozoa contain too much nitrogen for the amount of carbon protozoa need. 
      They release the excess nitrogen in the form of ammonium (NH4+). This 
      usually occurs near the root system of a plant. Bacteria and other 
      organisms rapidly take up most of the ammonium, but some is used by the 
      plant. (See figure for explanation of mineralization and 
      immobilzation.)
 Another role that protozoa play is in regulating bacteria populations. 
      When they graze on bacteria, protozoa stimulate growth of the bacterial 
      population (and, in turn, decomposition rates and soil aggregation.)  
      Exactly why this happens is under some debate, but grazing can be thought 
      of like pruning a tree – a small amount enhances growth, too much reduces 
      growth or will modify the mix of species in the bacterial community. Protozoa are also an important food source for other soil organisms and 
      help to suppress disease by competing with or feeding on pathogens. WHERE ARE PROTOZOA?Protozoa need bacteria to eat and water in which to move, so moisture 
      plays a big role in determining which types of protozoa will be present 
      and active. Like bacteria, protozoa are particularly active in the 
      rhizosphere next to roots. Typical numbers of protozoa in soil vary widely – from a thousand per 
      teaspoon in low fertility soils to a million per teaspoon in some highly 
      fertile soils. Fungal-dominated soils (e.g. forests) tend to have more 
      testate amoebae and ciliates than other types. In bacterial-dominated 
      soils, flagellates and naked amoebae predominate. In general, high 
      clay-content soils contain a higher number of smaller protozoa 
      (flagellates and naked amoebae), while coarser textured soils contain more 
      large flagellates, amoebae of both varieties, and ciliates. NEMATODES AND PROTOZOAProtozoa and bacterial-feeding nematodes compete for their common food 
      resource: bacteria. Some soils have high numbers of either nematodes or 
      protozoa, but not both. The significance of this difference to plants is 
      not known. Both groups consume bacteria and release NH4+.   
      BUG BIOGRAPHY:  Soil Dwelling Vampires  Most protozoa eat bacteria, but one group of 
      amoebae, the vampyrellids, eat fungi. The perfectly round holes drilled 
      through the fungal cell wall, much like the purported puncture marks on 
      the neck of a vampire’s victim, are evidence of the presence of 
      vampyrellid amoebae. The amoebae attach to the surface of fungal hyphae 
      and generate enzymes that eat through the fungal cell wall. The amoeba 
      then sucks dry or engulfs the cytoplasm inside the fungal cell before 
      moving on to its next victim.
 Vampyrellids attack many fungi including root pathogens, such as 
      Gaeumannomyces graminis, shown in the photo. This fungus attacks wheat 
      roots and causes take-all disease. >Go 
      to next chapter: Soil Nematodes <Return 
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