The soil food web is the community of organisms that are 
interdependent for sources of carbon and energy.
Communities are variously defined but a common thread in the 
definitions is interaction for resources, including food and space:
  
    
    
      
        | "...(communities are) not mere assemblages of species 
        living together, but form closely-knit communities or societies similar 
        to our own." C. Elton (1927) 
 "an assemblage of populations of plants, animals, bacteria and fungi 
        that live in an environment and interact with one another, forming 
        together a distinctive living system with its own composition, 
        structure, environmental relations, development and function" R. 
        Whittaker (1975)
 
 "A collection of organisms in an environment" J. Emlen (1977)
 
 "Organisms that interact in a given area" P. Price (1984)
 
 "Associations of plants and animals that are spatially delimited and 
        that are dominated by one or more prominent species or by a physical 
        characterisitic" R. Ricklefs (1990)
 
 "Community: the species that occur together in space and time" Begon, 
        Harper, and Townsend (1996)
 
 | Background Music:The Nematodes' Picnic Lyrics: Kathy Merrifield Vocals: Pointless Sisters   | 
    
    
   
From Lewis Carroll:
  Big fleas have little fleas
  Upon their backs to bite'em
  And little fleas have smaller fleas
  And so ad infinitum
  Resources and Roles in Foodwebs
  - Organisms can be classified as
    autotrophs or heterotrophs.
-  Autotrophs obtain their
    carbon and energy by fixing atmospheric CO2 using light as an
    energy source (photosynthesis). Green plants are autotrophs. Some
    autotrophic bacteria use chemical reactions as the energy source, e.g.
    S-reducing bacteria use electrons from sulphur and reduce it to H2S.
    
- Heterotrophs obtain their
    carbon and energy from other organisms. They consume them while still alive
    (parasites), or kill them in the act of consumption (predators), or feed on
    their waste products, excretions, secretions, or remains (detritivores).
    Most organisms other than green plants are heterotrophs.
- The food supply to soil organisms
    originates through two main channels:
  - The photosynthetic activities of
    plants. Plant roots leak - root exudates; root tissues are sloughed during
    growth, when damaged, or when no longer useful to the plant. Herbivores
    graze on or parasitize plant roots. All the organisms exploiting the primary
    producer in this manner become food and energy sources for other organisms
    in the soil foodweb.
- Plant residues, manure and other
    organic material falling on or applied to the soil surface, or incorporated
    into the soil. All the organisms decomposing this material also become food
    and energy sources for other organisms in the soil foodweb.
 
  - Bacteria, fungi, plant-parasitic
    nematodes, root-grazing insects, gophers, etc. feed directly on plant roots
    as primary consumers. They are subject to parasitism and predation by other
    organisms; they die, defecate, excrete, etc. and provide food for other
    organisms.
- Bacteria and fungi assimilate plant
    secretions, and plant debris. They decompose dead organic matter of
    intrinsic or extrinsic origin. In general, more resistant substrates and
    substrates with higher C:N ratios are more likely to be exploited by fungi
    than by bacteria, while more labile substrates and those with lower C:N
    ratios may be predominated by bacteria.
- Nematodes (e.g. Tylenchida: Aphelenchina 
    andomnivorous Dorylaimida)
    and arthropods (Collembola and mites) feed on fungi.  Nematodes (e.g. Rhabditida), and Protozoa (flagellates and amoebae) feed on bacteria.
    
    Predaceous nematodes (e.g. Mononchus), omnivorous nematodes (e.g.  
  Labronema),
    
    arthropods (e.g. mites, Collembola),  Protozoa (e.g. amoebae),
    Tardigrades,
    etc. feed on nematodes.  Arthropods (e.g. predaceous mites) feed on
    mites; Collembola and mites are parasitized by bacteria and fungi.
- At every trophic interaction, the
    debris and leakage become substrate for other organisms; the wastes and
    secretions of the new owners of the carbon molecules originally fixed by the
    autotroph are substrate for other organisms.
- Carbon, Nitrogen, and other
    molecules are mineralized during the metabolic processes of all organisms in
    the web through  
  respiration, 
  osmoregulation, etc. The mineralized molecules
    (CO2, NH4, NO3, etc) are available to
    plants, bacteria and fungi in the soil, or are returned to the atmosphere.
- Organisms in the soil tend to be
    aggregated in areas where carbon and energy originally enters the foodweb,
    e.g., in the plant rhizosphere, close to the soil surface, or in the tillage
    zone.
- The size of the foodweb is limited
    by the amount of carbon and energy entering it. As much as 90% of the
    remaining resources may be lost at each trophic interchange. That limits the
    length of chains or channels running through the web to four or five
    interchanges. In other words, a carbon molecule entering the web is unlikely
    to pass through more than five different organisms without being respired.
    In foodwebs limited in size by minimal carbon input the number of
    interchanges will be fewer as there are insufficient resources to support
    organisms at higher trophic levels. In that case, turnover of the microbial
    biomass may be small and minerals will be immobilized.
- Organisms at higher trophic levels
    in the soil foodweb are often more susceptible to disturbance than those
    smaller-bodied organisms at lower trophic levels. Further, the organisms at
    lower trophic levels are often opportunists, responding rapidly to
    availability of resources. Consequently, foodwebs in disturbed systems tend
    to be predominated by primary decomposers and direct herbivores since their
    predators are absent. That again leads to immobilization of minerals by the opportunists and to a lack of biological regulation of their abundance and
    dynamics.
 
  - Decomposition of organic matter
- Cycling of minerals and nutrients
- Redistribution of minerals and
    nutrients in space and time
- Reservoirs of minerals and nutrients
- Sequestration of carbon
- Detoxification of pollutants
- Modification of soil structure
- Community self-regulation
- Biological regulation 
  or suppression of pest
    species
- Etc.
 
Connectance:
proportion of the potential links in the foodweb that are actually realized.
Redundancy:
the number of links in the food web that perform the same "function";
complex foodwebs should have greater redundancy.
Resilience:
lack of change in the "function" of the food web when a link is broken
or a node removed; greater redundancy leads to greater functional resilience.
Suppressive: when there are sufficient 
predators of various kinds in the food web that populations of opportunistic 
species are actually reduced, i.e. the integral effect of the food web is 
suppressive to the opportunistic organisms.
Conducive: there are few higher trophic layers 
in the food web so that there is little predation on opportunists. The structure 
of the soil community is such that it will "allow", or at least not prevent, 
increase of opportunists.
Regulated: somewhere between conducive and 
suppressive. Opportunists may not decline in number but will also not increase 
exponentially. Their populations are regulated at relatively constant levels by 
the combined effect of various predators in the food web.
Remember, the predators of nematodes are not only other nematodes but also 
certain fungi, mites, collembola, protozoa, some bacteria, etc. The more 
abundant these various guilds of organisms, the more likely that opportunistic 
prey species will be regulated or suppressed.
 
Assessment and Monitoring of Soil
Foodwebs
  
  - Structural Analysis
    - Physical: Sample,
  extract, identify, enumerate each organism group - bacteria, fungi, protozoa,
  nematodes, arthropods, annelids, rodents…….., etc. (An enormous job!)
- Biochemical Analysis:PLFAs, DNA profiles, etc. indicate the presence of key organism groups or taxa.
  (Probably access relatively few taxa)
- Indicator Guilds:Monitor the presence and abundance of key taxa that are indicative of the
  presence of specific trophic guilds that perform critical or desired
  functions. (Soil nematode guilds occur at all trophic levels in food webs,
  they can be monitored by simple standardized techniques and are proving to be
  useful indicators of foodweb status).
Functional Analysis:
Confirm that key functions are occurring at desired rates; measure rates of
suppressiveness, decomposition, mineralization, respiration……etc. (Useful, but difficult to
interpret in terms of the key players in the system).
Bongers, T. and H. Ferris. 1999. Nematode community structure as a 
bioindicator in environmental monitoring. Trends in Evolution and Ecology 
14:224-228.
Ferris, H., T. Bongers, and R. G. M. de Goede. 2001. A framework for soil 
food web diagnostics: extension of the nematode faunal analysis concept. Applied 
Soil Ecology 18:13-29. 
 
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