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Microbial ecology of the terrestrial subsurface
1Department of Microbiology, Cornell University, Ithaca, New York 14853.
Advances in Applied Microbiology
|January 1, 1988
Summary
Microbial life thrives in terrestrial subsurface aquifers, with abundance and activity dictated by sediment properties and nutrient availability. Bacteria dominate these environments, with their distribution influenced by depth and migration within aquifer sediments.
Area of Science:
- Terrestrial subsurface microbial ecology
- Aquifer microbiology
- Environmental microbiology
Background:
- Microorganisms are the predominant life forms in the terrestrial subsurface.
- Aquifer sediment and groundwater properties critically influence microbial abundance and activity.
- Environmental factors like pH and temperature are generally not limiting in shallow aquifers.
Purpose of the Study:
- To present a current view of microbial ecology in terrestrial subsurface environments, focusing on shallow aquifer sediments.
- To characterize the types, abundance, and metabolic activities of subsurface microorganisms.
- To understand the factors controlling microbial distribution and function in aquifers.
Main Methods:
- Employed aseptic sampling techniques for subsurface material.
- Utilized microbiological and biochemical methods for analysis.
- Conducted vertical profile studies of shallow aquifers and lateral distribution studies.
Main Results:
- Active microbial biomass generally declines with depth in shallow aquifers but can be variable in saturated zones.
- Bacteria are the dominant microorganisms, though eukaryotic microbes are also present.
- Microorganisms exhibit transport and migration within aquifer sediments over significant distances.
Conclusions:
- Aquifer properties such as pore size, nutrient, and electron acceptor availability are key determinants of microbial life.
- Microbial colonization of aquifers can occur during sediment deposition or via transport from surface areas.
- The nutritional ecology of pristine aquifers is typically oligotrophic, relying on organic compounds from overlying soil.