Microbial loop

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Introduction

Electron micrograph of the Ebola Zaire virus. This was the first photo ever taken of the virus, on 10/13/1976. By Dr. F.A. Murphy, now at U.C. Davis, then at the CDC.

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Legend/credit: Electron micrograph of the Ebola Zaire virus. This was the first photo ever taken of the virus, on 10/13/1976. By Dr. F.A. Murphy, now at U.C. Davis, then at the CDC.
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The microbial loop is a depiction of the microbial food web. The pathway starts with dissolved organic matter (DOM) which makes its way through various trophic levels ultimately to the highest trophic levels. This is relevant in aquatic and soil systems. Organisms involved in the marine microbial loop include DOM, bacteria, micro flagellates and ciliates, phytoplankton and various other nutrient cycling bacteria [3]. The microbial loop is ecologically significant because it is directly involved in nutrient cycling and primary production of biomass ultimately effecting large-scale ecological functions.

Biological interaction

The microbial loop can best be explained starting with DOM. DOM, or dissolved organic carbon, are concentrations of free organic carbon below 0.45 micrometers. DOM consists of molecules which were once parts of living organisms such as proteins, carbohydrates lipids and nucleic acids. DOM is introduced into the system in many ways including sloppy feeding and excretion of waste products from aquatic organisms [3]. This DOM is then utilized as a food source for bacteria. Bacteria are the only organisms capable of recycling DOM making them an extremely vital component for the continuation ecosystem function. These bacteria are then consumed by protozoans, microbe consumers of bacteria and algae. Zooplankton, like copepods and other organisms then feed off these protozoans and the link to the traditonal food web is established. Zooplankton are eaten by bigger organisms (shrimp ) which are eaten by bigger organisms (fish) and so on down the line. All this organic matter is transferred from smaller levels to the largest levels of ecosystems [1]. The DOM is recycled back into the system as these various organisms from all trophic levels die off and are broken down smaller and smaller via decomposition and other methods mentioned earlier (sloppy feeding, excretion, etc.)

Niche

Describe the physical, chemical, or spatial characteristics of the niche where we might find this interaction, using as many sections/subsections as you require. Look at other topics available in MicrobeWiki. Create links where relevant.

Microbial processes

What microbial processes are important for this microbial interaction? Does this microbial interaction have some ecosystem-level effects? Does this interaction affect the environment in any way? Describe critical microbial processes or activities that are important in this interaction, adding sections/subsections as needed. Look at other topics in MicrobeWiki. Are some of these processes already described? Create links where relevant.

Key Microorganisms

What specific kinds of microbes are typically involved in this interaction? Or associated with important processes? Describe key groups (genera, species) of microbes that we find in this environment, and any special adaptations they may have evolved to survive in this environment. List examples of specific microbes that represent key groups or are associated with important processes found in this environment. Add sections/subsections as needed. Look at other microbe listings in MicrobeWiki. Are some of the groups of microbes from your environment already described? Create links to other MicrobeWiki pages where possible.

Current Research

Enter summaries of recent research here--at least three required

References

1. Azam F, Fenchel T, Field JG, Gray JS, Meyer-Reil LA, Thingstad F. (1983). “The ecological role of water-column microbes in the sea”. Marine Ecology Progress Series. 10: 257-263.

2. Bonkowski M. (2003). “Protozoa and plant growth: the microbial loop in soil revisited”. Tansley Review. 617-631.

3. Fenchel T. (2008). “The microbial loop – 25 years later”. Journal of Experimental Marine Biology and Ecology. 99-103.

4. Stone, Richard (June 18, 2010). "Marine Biogeochemistry: The Invisible Hand Behind A Vast Carbon Reservoir". Science Magazine. doi:10.1126/science.328.5985.1476.

Edited by Nathan Bohne, a student of Angela Kent at the University of Illinois at Urbana-Champaign.