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==Lichens==
==Lichens==
===Overview===
Lichens are unique organisms that consists of a symbiotic relationship between fungal filaments and algae or cyanobacteria. Algae and cyanobacteria are known as photobionts, while the fungal component of lichen is called a mycobiont. Algae are photosynthetic and provide the fungus with carbohydrates which can be used to produce energy. Cyanobacteria on the other hand, fix nitrogen or carbon which the fungal can use to synthesize amino acids and carbohydrates respectively. The fungus can also be considered a parasite because it provides no dehydration protection or nutrients for the photobionts.


===Environment===
===Environment===
Lichens can inhabit a diverse environment ranging from deserts and tundras all over the world covering an estimated 8% of all land. Lichens can be found in deserts such as Saudi Arabia, Australia and North America. In these environments lichens are situated on tree barks, leaves, ground, and rocks.
As stated earlier lichens come in many form, each with different roles and adaptations that suit their environment. Many of these lichens can occupy the same niche but over time the lichen that has the best adaptations for the environment will have a higher growth rate and a lower death rate, and out live the poorly suited lichen. Lichens can even overgrow and kill mosses that are in their niche by excreting toxins. Lichens are also known to produce useful antibodies and dyes that have been harnessed by humans.
Lichens can survive in extreme desert heat. In the desert Lichens can survive up to -60 º to 55 º Celsius which is -76 to 131º Fahrenheit. The water content for lichens can vary from 2%-300% dry weight. The low water content lichens are ideal for desert rock lichens because deserts are known for their miniscule or non-existent precipitation. Due to the lack of precipitation, lichens obtain most of their water from the atmosphere and morning dews. When not enough water is obtained from the atmosphere the lichen turns off metabolic processes and go dormant, which can last several years. However when a small amount of water is obtained from morning dews the lichen comes out of its dormant stage and resumes physiological activities. Compared to cyanobacteria, algae are more adaptive at low water levels and can occupy desert niches better.
===Symbiotic Relationship===
Since Lichens are composed of a symbiotic relationship between fungus and photosynthetic algae there can be many combinations of lichens. It is estimated that 85 percent of the photobiont are eukaryotic algae while 10 percent are cyanobacteria and 5 percent are a combination of cyanobacteria and eukaryotic algae.  Some examples of alga are trebouxia, Pseudotrebouxia, and Trentepohlia while some examples of cyanobactera are Nostoc and Scytonema. The fungi that are in the symbiotic relationship can be Ascomycota, Basidiomycota, or Conidial fungi.
The relationship between the fungal and the alga or cyanobacteria can be considered to be parasitic because the fungal benefits from the photobionts but the photobionts do not benefit from the fungal. Studies using radioactively labeled carbon have shown that photobionts retain only 20% of the carbon they fix, while they transport 80% of the fixed carbon the fungus. Algae release the carbon they fix in the form of glucose, while cyanobacteria release carbons in the form of polyhydric alcohols. These forms of carbon can then move on to provide energy for the photobionts and the mycobionts.
Cyanobacteria, particularly Nostoc, are unique from alga because along with fixing carbon they also fix nitrogen into ammonia. Most of the ammonia is actually used by the fungus to synthesis necessary amino acids
===Changes to Environment===
Most lichens change the diverse environment they live in. They can form fruticose which looks like shrubs, foliose which are like leaves, crustose which are like a crust on the surfaces they are in contact with. Lichens are also known to weather rocks through chemical and physical methods. Chemical weathering of rocks is due to the secretion of oxalic acid converted from insoluble carbonates and silicates. Physical weathering of rocks is done by contracting and swelling of the body of the lichen. Swelling of the body of the lichen happens during wet periods, while contracting happens during the dry periods of the lichen. The changes in size of the lichen help those that are embedded in cracks of rocks to break the rock apart.





Revision as of 06:56, 27 August 2008

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Description of Niche

Lichens

Overview

Lichens are unique organisms that consists of a symbiotic relationship between fungal filaments and algae or cyanobacteria. Algae and cyanobacteria are known as photobionts, while the fungal component of lichen is called a mycobiont. Algae are photosynthetic and provide the fungus with carbohydrates which can be used to produce energy. Cyanobacteria on the other hand, fix nitrogen or carbon which the fungal can use to synthesize amino acids and carbohydrates respectively. The fungus can also be considered a parasite because it provides no dehydration protection or nutrients for the photobionts.

Environment

Lichens can inhabit a diverse environment ranging from deserts and tundras all over the world covering an estimated 8% of all land. Lichens can be found in deserts such as Saudi Arabia, Australia and North America. In these environments lichens are situated on tree barks, leaves, ground, and rocks.

As stated earlier lichens come in many form, each with different roles and adaptations that suit their environment. Many of these lichens can occupy the same niche but over time the lichen that has the best adaptations for the environment will have a higher growth rate and a lower death rate, and out live the poorly suited lichen. Lichens can even overgrow and kill mosses that are in their niche by excreting toxins. Lichens are also known to produce useful antibodies and dyes that have been harnessed by humans.

Lichens can survive in extreme desert heat. In the desert Lichens can survive up to -60 º to 55 º Celsius which is -76 to 131º Fahrenheit. The water content for lichens can vary from 2%-300% dry weight. The low water content lichens are ideal for desert rock lichens because deserts are known for their miniscule or non-existent precipitation. Due to the lack of precipitation, lichens obtain most of their water from the atmosphere and morning dews. When not enough water is obtained from the atmosphere the lichen turns off metabolic processes and go dormant, which can last several years. However when a small amount of water is obtained from morning dews the lichen comes out of its dormant stage and resumes physiological activities. Compared to cyanobacteria, algae are more adaptive at low water levels and can occupy desert niches better.

Symbiotic Relationship

Since Lichens are composed of a symbiotic relationship between fungus and photosynthetic algae there can be many combinations of lichens. It is estimated that 85 percent of the photobiont are eukaryotic algae while 10 percent are cyanobacteria and 5 percent are a combination of cyanobacteria and eukaryotic algae. Some examples of alga are trebouxia, Pseudotrebouxia, and Trentepohlia while some examples of cyanobactera are Nostoc and Scytonema. The fungi that are in the symbiotic relationship can be Ascomycota, Basidiomycota, or Conidial fungi.

The relationship between the fungal and the alga or cyanobacteria can be considered to be parasitic because the fungal benefits from the photobionts but the photobionts do not benefit from the fungal. Studies using radioactively labeled carbon have shown that photobionts retain only 20% of the carbon they fix, while they transport 80% of the fixed carbon the fungus. Algae release the carbon they fix in the form of glucose, while cyanobacteria release carbons in the form of polyhydric alcohols. These forms of carbon can then move on to provide energy for the photobionts and the mycobionts.

Cyanobacteria, particularly Nostoc, are unique from alga because along with fixing carbon they also fix nitrogen into ammonia. Most of the ammonia is actually used by the fungus to synthesis necessary amino acids

Changes to Environment

Most lichens change the diverse environment they live in. They can form fruticose which looks like shrubs, foliose which are like leaves, crustose which are like a crust on the surfaces they are in contact with. Lichens are also known to weather rocks through chemical and physical methods. Chemical weathering of rocks is due to the secretion of oxalic acid converted from insoluble carbonates and silicates. Physical weathering of rocks is done by contracting and swelling of the body of the lichen. Swelling of the body of the lichen happens during wet periods, while contracting happens during the dry periods of the lichen. The changes in size of the lichen help those that are embedded in cracks of rocks to break the rock apart.


Influence by Adjacent Communities (if any)

Is your niche close to another niche or influenced by another community of organisms?

Conditions under which the environment changes

Do any of the physical conditions change? Are there chemicals, other organisms, nutrients, etc. that might change the community of your niche.

Desert Varnish

Environment

Physical and Chemical Conditions

Current Research

Who lives there?

Which microbes are present?

You may refer to organisms by genus or by genus and species, depending upon how detailed the your information might be. If there is already a microbewiki page describing that organism, make a link to it.

Are there any other non-microbes present?

Plants? Animals? Fungi? etc.

Do the microbes that are present interact with each other?

Describe any negative (competition) or positive (symbiosis) behavior

Do the microbes change their environment?

Do they alter pH, attach to surfaces, secrete anything, etc. etc.

Do the microbes carry out any metabolism that affects their environment?

Do they ferment sugars to produce acid, break down large molecules, fix nitrogen, etc. etc.



'Super' bacteria live on sheets, fingernails: study

On June 6, 2005, U.S reserachers

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.

Edited by [Priya Patel, Fatima Khan, Luanne Cabiling], students of Rachel Larsen