Benthic Zone: Difference between revisions

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==Introduction==
==Introduction==
The benthic zone is the lowest level of a marine or freshwater system and includes the sediment surface, the water just above it, and some sub-surface layers.  Benthic zones exist all over the world in every appreciable water system, be it an ocean, lake, pond, river, or stream.  The benthic zone starts at the shore and extends down along the bottom of the lake or ocean.  This means that it could be as shallow as a few inches at its start, but may reach depths of 6,000 meters as it coincides with the abyssal plain at the bottom of the ocean.  Because of the depths it can reach, the benthic zone is often characterized by low sunlight and low temperatures.  This usually attributes to little life and biodiversity, so one would be inclined to assume that it is a vast waste.  However, the presence of sediment layers at the benthic zone provides many nutrients and adds greatly to species richness.  Because the benthic zone has such a range of depths, many kinds of organisms may live there.  Crustaceans, sponges, bivalves, snails, sea stars, polychaetes, fish, and many others can inhabit the zone. 
The nutrients at the sediment layer are usually the limiting source of energy for the organisms that inhabit the benthic zone.  These nutrients actually originate from dead or decaying organic matter from higher up in the water column.  This organic matter drifts down continuously from shallower depths and settles on the bottom, where it is consumed and is the main driver of the benthic zone food chain.  The organisms in the benthic zone are classified into those which dwell on the surface and those which burrow into the sea floor.  They are the epifauna and infauna, respectively.  Organisms inhabiting the benthic zone are collectively called the benthos.  The name benthos comes from the Greek noun βένθος, which means “depths of the sea”. 
[[Image:PHIL_1181_lores.jpg|thumb|300px|right|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.]]
[[Image:PHIL_1181_lores.jpg|thumb|300px|right|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.]]
<br>At right is a sample image insertion.  It works for any image uploaded anywhere to MicrobeWiki.  The insertion code consists of:
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Revision as of 08:19, 8 April 2013

This student page has not been curated.

Introduction

The benthic zone is the lowest level of a marine or freshwater system and includes the sediment surface, the water just above it, and some sub-surface layers. Benthic zones exist all over the world in every appreciable water system, be it an ocean, lake, pond, river, or stream. The benthic zone starts at the shore and extends down along the bottom of the lake or ocean. This means that it could be as shallow as a few inches at its start, but may reach depths of 6,000 meters as it coincides with the abyssal plain at the bottom of the ocean. Because of the depths it can reach, the benthic zone is often characterized by low sunlight and low temperatures. This usually attributes to little life and biodiversity, so one would be inclined to assume that it is a vast waste. However, the presence of sediment layers at the benthic zone provides many nutrients and adds greatly to species richness. Because the benthic zone has such a range of depths, many kinds of organisms may live there. Crustaceans, sponges, bivalves, snails, sea stars, polychaetes, fish, and many others can inhabit the zone.

The nutrients at the sediment layer are usually the limiting source of energy for the organisms that inhabit the benthic zone. These nutrients actually originate from dead or decaying organic matter from higher up in the water column. This organic matter drifts down continuously from shallower depths and settles on the bottom, where it is consumed and is the main driver of the benthic zone food chain. The organisms in the benthic zone are classified into those which dwell on the surface and those which burrow into the sea floor. They are the epifauna and infauna, respectively. Organisms inhabiting the benthic zone are collectively called the benthos. The name benthos comes from the Greek noun βένθος, which means “depths of the sea”.

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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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?)

Physical environment

Subsection 1

Subsection 1a

Subsection 1b

Subsection 2

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 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

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

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 <your name>, a student of Angela Kent at the University of Illinois at Urbana-Champaign.