Difference between revisions of "Deep subsurface microbes"

From MicrobeWiki, the student-edited microbiology resource
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Deep subsurface microbes first came into question when the American geologist Edson S. Bastin questioned why samples of water extracted from oil fields contained hydrogen sulfide and bicarbonates.  Armed with the knowledge that certain species of bacteria can derive energy from reducing sulfur compounds in the absence of oxygen, he concluded that there must be populations of these bacteria living in the underground oil reserves, degrading the organic components of oil as a carbon source, and reducing sulfur compounds for energy.  By 1926, Bastin and his colleague, Frank E. Greer has cultured sulfur reducing bacteria from samples taken from the groundwater of an oil deposit several hundred meters below the surface.  Bastin and Greer's initial deduction was that the bacteria were the ancestors of those buried up to 300 million years ago when the organic materials constituting the oil deposit were buried.   
 
Deep subsurface microbes first came into question when the American geologist Edson S. Bastin questioned why samples of water extracted from oil fields contained hydrogen sulfide and bicarbonates.  Armed with the knowledge that certain species of bacteria can derive energy from reducing sulfur compounds in the absence of oxygen, he concluded that there must be populations of these bacteria living in the underground oil reserves, degrading the organic components of oil as a carbon source, and reducing sulfur compounds for energy.  By 1926, Bastin and his colleague, Frank E. Greer has cultured sulfur reducing bacteria from samples taken from the groundwater of an oil deposit several hundred meters below the surface.  Bastin and Greer's initial deduction was that the bacteria were the ancestors of those buried up to 300 million years ago when the organic materials constituting the oil deposit were buried.   
  
The deeps subsurface ecosystem begins at about 50m below the surface of earths crust, and extends variably downward, up to 2.8km (1.7mi)[1].  The organisms live within the flooded pore space within the rocks and live by reducing inorganic compounds found in the rock.
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The deeps subsurface ecosystem begins at about 50m below the surface of earths crust, and extends variably downward, up to 2.8km (1.7mi)[1].  The organisms live within the flooded pore space within the rocks and live by reducing inorganic compounds found in the rock.  These microbes have some very specific adaptations that allow them to proliferate in such a hostile environment.  Radiation resistant, thermophilic, anaerobic microorganisms with a large emphasis on DNA repair mechanisms survive for decades and centuries instead of hours or days.
With such a surprising diversity of organisms in such an extreme environment, the deep subsurface has been the subject of many studies in the recent years.  They carry out processes that alter the chemical makeup of minerals, degrade pollutants, and alter the mineral content of ground water.  Studies are being done to search for deep subsurface microbes that produce antibiotics and heat stable enzymes, and for those that assist in the degredation of toxic substances.
+
With such a surprising diversity of organisms in such an extreme environment, the deep subsurface has been the subject of many studies in the recent years.  They carry out processes that alter the chemical makeup of minerals, degrade pollutants, and alter the mineral content of ground water.  Studies are being done to search for deep subsurface microbes that produce antibiotics and heat stable enzymes, and for those that assist in the degradation of toxic substances.
  
 
Perhaps the most incredible thing about the microbes found in the deep subsurface, is that the majority of the populations can thrive indefinitely without any input from the earth's surface[1].  That being said, they are effectively 100% disconnected from the rest of life as we know it.
 
Perhaps the most incredible thing about the microbes found in the deep subsurface, is that the majority of the populations can thrive indefinitely without any input from the earth's surface[1].  That being said, they are effectively 100% disconnected from the rest of life as we know it.
  
 
==Physical environment==
 
==Physical environment==
 
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The deep subsurface biosphere is a very hostile environment. 
  
 
===Physical Factors===
 
===Physical Factors===
 +
Intense pressures, high temperatures, limited livable space, and limited nutrient availability are all factors that microbes living in this environment must adapt to.  It seems that the largest limitation to microbial life in this habitat is temperature, which increases with depth.  The highest temperature generally accepted as the livable range for microorganisms in this habitat is 110 degrees C [1]  In oceanic crusts, the temperature of the subsurface increases at a rate of about 15 degrees C per kilometer of depth, giving a maximum livable depth of about 7 kilometers.  In the continental crusts the rock warms at a significantly faster rate, about 25 degrees C per kilometer, resulting in a maximum livable depth of approximately 4 kilometers [1].
  
 +
Microbes in these environments can only exist where water fills the pore spaces of rocks.  In the marine subsurface, this is rarely an issue, but in continental subsurface, there tends to be a bit more variability in groundwater dispersion.
 
===Chemical Factors====
 
===Chemical Factors====
  
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====Sedimentary Rock====
 
====Sedimentary Rock====
 
===Continental Subsurface===
 
===Continental Subsurface===
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Commonly found in deep aquifers, deep subsurface microbes provide a significant impact on the chemistry of the groundwater available in these aquifers.
 
====Granitic Rock====
 
====Granitic Rock====
  
  
 
==Microbial communities==
 
==Microbial communities==
What kind of microbes do we typically find in this environment? Or associated with important processes in this environment? Describe key groups 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. Link to other MicrobeWiki pages where possible.
 
 
Are there important biological interactions that are important in this environment? Do these interactions influence microbial populations and their activities? How do these interactions influence other organisms? Describe biological interactions that might take place in this environment, using as many sections/subsections as you require. Look at other topics available in MicrobeWiki. Create links where relevant.
 
  
 
===Subsection 1===
 
===Subsection 1===
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[2]Amend, J. P., & Teske, A. (2005). Expanding frontiers in deep subsurface microbiology. Palaeogeography, Palaeoclimatology, Palaeoecology, 219(1-2), 131-155. Elsevier. Retrieved from http://linkinghub.elsevier.com/retrieve/pii/S0031018204005954
 
[2]Amend, J. P., & Teske, A. (2005). Expanding frontiers in deep subsurface microbiology. Palaeogeography, Palaeoclimatology, Palaeoecology, 219(1-2), 131-155. Elsevier. Retrieved from http://linkinghub.elsevier.com/retrieve/pii/S0031018204005954
Edited by <your name>, a student of Angela Kent at the University of Illinois at Urbana-Champaign.
 
  
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Edited by <Craig Mack>, a student of Angela Kent at the University of Illinois at Urbana-Champaign.
  
 
<!-- Do not edit or remove this line -->[[Category:Pages edited by students of Angela Kent at the University of Illinois at Urbana-Champaign]]
 
<!-- Do not edit or remove this line -->[[Category:Pages edited by students of Angela Kent at the University of Illinois at Urbana-Champaign]]

Revision as of 02:59, 6 April 2011

This student page has not been curated.

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.


At right is a sample image insertion. It works for any image uploaded anywhere to MicrobeWiki. The insertion code consists of:
Double brackets: [[
Filename: PHIL_1181_lores.jpg
Thumbnail status: |thumb|
Pixel size: |300px|
Placement on page: |right|
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.
Closed double brackets: ]]

Other examples:
Bold
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Subscript: H2O
Superscript: Fe3+

This template gives you a general idea of the layout of your page. You are not completely restricted to this format, so feel free to try out different things. I'll give you feedback as you work on your pages. Make sure to copy the "code" of this page to your own page before editing. -Prof Kent

In the introduction, briefly describe the habitat that is the topic of this page. Introduce the habitat, its ecological significance, and the importance of microorganisms in this environment. (What processes do they carry out? What functions do they perform?)

Microbes have found a way to exist in every corner of the planet, and humans have found ways to utilize their incredible diversity for thousands of years. From fermenting cheese and wine, to the production of pharmaceuticals, microbes have been utilized for a myriad of reasons. It was not until the late 1920's however, that scientists thought to look deep within the body of our earth itself for a new source of potential biodiversity.

Deep subsurface microbes first came into question when the American geologist Edson S. Bastin questioned why samples of water extracted from oil fields contained hydrogen sulfide and bicarbonates. Armed with the knowledge that certain species of bacteria can derive energy from reducing sulfur compounds in the absence of oxygen, he concluded that there must be populations of these bacteria living in the underground oil reserves, degrading the organic components of oil as a carbon source, and reducing sulfur compounds for energy. By 1926, Bastin and his colleague, Frank E. Greer has cultured sulfur reducing bacteria from samples taken from the groundwater of an oil deposit several hundred meters below the surface. Bastin and Greer's initial deduction was that the bacteria were the ancestors of those buried up to 300 million years ago when the organic materials constituting the oil deposit were buried.

The deeps subsurface ecosystem begins at about 50m below the surface of earths crust, and extends variably downward, up to 2.8km (1.7mi)[1]. The organisms live within the flooded pore space within the rocks and live by reducing inorganic compounds found in the rock. These microbes have some very specific adaptations that allow them to proliferate in such a hostile environment. Radiation resistant, thermophilic, anaerobic microorganisms with a large emphasis on DNA repair mechanisms survive for decades and centuries instead of hours or days. With such a surprising diversity of organisms in such an extreme environment, the deep subsurface has been the subject of many studies in the recent years. They carry out processes that alter the chemical makeup of minerals, degrade pollutants, and alter the mineral content of ground water. Studies are being done to search for deep subsurface microbes that produce antibiotics and heat stable enzymes, and for those that assist in the degradation of toxic substances.

Perhaps the most incredible thing about the microbes found in the deep subsurface, is that the majority of the populations can thrive indefinitely without any input from the earth's surface[1]. That being said, they are effectively 100% disconnected from the rest of life as we know it.

Physical environment

The deep subsurface biosphere is a very hostile environment.

Physical Factors

Intense pressures, high temperatures, limited livable space, and limited nutrient availability are all factors that microbes living in this environment must adapt to. It seems that the largest limitation to microbial life in this habitat is temperature, which increases with depth. The highest temperature generally accepted as the livable range for microorganisms in this habitat is 110 degrees C [1] In oceanic crusts, the temperature of the subsurface increases at a rate of about 15 degrees C per kilometer of depth, giving a maximum livable depth of about 7 kilometers. In the continental crusts the rock warms at a significantly faster rate, about 25 degrees C per kilometer, resulting in a maximum livable depth of approximately 4 kilometers [1].

Microbes in these environments can only exist where water fills the pore spaces of rocks. In the marine subsurface, this is rarely an issue, but in continental subsurface, there tends to be a bit more variability in groundwater dispersion.

Chemical Factors=

Marine Subsurface

Basaltic Rock

Sedimentary Rock

Continental Subsurface

Commonly found in deep aquifers, deep subsurface microbes provide a significant impact on the chemistry of the groundwater available in these aquifers.

Granitic Rock

Microbial communities

Subsection 1

Subsection 1a

Subsection 1b

Subsection 2

Microbial processes

What microbial processes define this environment? Describe microbial processes that are important in this habitat, adding sections/subsections as needed. Look at other topics in MicrobeWiki. Are some of these processes already described? Create links where relevant.

Subsection 1

Subsection 1a

Subsection 1b

Subsection 2

Current Research

References

[Sample reference] Takai, K., Sugai, A., Itoh, T., and Horikoshi, K. "Palaeococcus ferrophilus gen. nov., sp. nov., a barophilic, hyperthermophilic archaeon from a deep-sea hydrothermal vent chimney". International Journal of Systematic and Evolutionary Microbiology. 2000. Volume 50. p. 489-500.

[1]http://wvlc.uwaterloo.ca/biology447/modules/module6/Scientific_American_Article_Microbes.htm Fredrickson, J., Onstott, T. "Microbes Deep Inside the Earth." "Scientific American". 1996.

[2]Amend, J. P., & Teske, A. (2005). Expanding frontiers in deep subsurface microbiology. Palaeogeography, Palaeoclimatology, Palaeoecology, 219(1-2), 131-155. Elsevier. Retrieved from http://linkinghub.elsevier.com/retrieve/pii/S0031018204005954



Edited by <Craig Mack>, a student of Angela Kent at the University of Illinois at Urbana-Champaign.