Difference between revisions of "DarwinsTheory"

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= Darwin's Theory =
 
= Darwin's Theory =
  
Darwin grouped coral reefs into three distinct types: barrier, fringing, and atolls. He believed that each reef type was really a separate stage of reef development around a slowly sinking volcanic island.<ref> Strykowski and Bonem, p. 18-19 </ref>
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In the late 1830's Charles Darwin spent several years in South America studying crustal movements, elevation, and subsidence. Along with Charles Lyell, he sought an answer to the question of South America's elevation. Ironically, his work on subsidence led to a now universally accepted theory of reef formation. <ref> Burkhardt, Frederick. "Darwin and Coral Reefs." ''Darwin Correspondence Project.'' University of Cambridge, 2012. http://www.darwinproject.ac.uk/darwin-coral-reefs 25 Feb 2013. </ref> In his 1842 report ''Coral Reefs,'' Darwin grouped coral reefs into three distinct types: barrier, fringing, and atolls. He then explained that each reef type was really a separate stage of reef development around a slowly sinking volcanic island. <ref name="palaces"> Strykowski, Joe and Rena M. Bonem. '''Palaces Under the Sea.''' Crystal River, FL: Star Thrower Foundation, 1993, p. 19-26. Print. </ref>  
[[File:reef types.png|thumb|]]
 
  
==Stage 1 - Fringing Reef==
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==The Theory==
A submarine volcano forms an island rising from the sea floor. Corals begin to grow in the shallow regions off the coast of the island. As the island gradually sinks, the reef grows upward in order to stay within a sunlit range. A fringing reef is a reef encircling this volcanic island while it first begins to sink.<ref> Strykowski and Bonem, p. 19 </ref>
 
  
==Stage 2 - Barrier Reef==
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[[File:reef types.png|left|150px|<ref name="p19"> Strykowski and Bonem, p. 19 </ref>]]
As the volcanic island continues to sink, a lagoon begins to form between the reef and the exposed island. In this phase, the reef is a barrier reef.<ref> Strykowski and Bonem, p. 19-20 </ref>
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[[File:Typesofreefscoral-reef-info.jpg|right|500px|thumb|aerial photos of the three types of reefs from left to right: atoll, fringing, barrier. image credit: coral-reef-info.com]]
  
==Stage 3 - Atoll==
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'''Stage 1 - Fringing Reef'''
Once the volcanic island is fully submerged, the reef is known as an atoll. The reef outline is circular with a central lagoon.<ref> Strykowski and Bonem, p. 20 </ref>
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A submarine volcano forms an island rising from the sea floor. [[ReefInhabitants#Coral|Corals]] begin to grow in the shallow regions off the coast of the island. As the island gradually sinks, the reef grows upward in order to stay within a sunlit range. A [[FringingReefs|fringing reef]] is a reef encircling this volcanic island while it first begins to sink.<ref name="palaces" />
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'''Stage 2 - Barrier Reef'''
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As the volcanic island continues to sink, a lagoon begins to form between the reef and the exposed island. In this phase, the reef is a [[BarrierReefs|barrier reef]].<ref name="palaces" />
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'''Stage 3 - Atoll'''
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Once the volcanic island is fully submerged, the reef is known as an [[Atolls|atoll]]. The reef outline is circular with a central lagoon.<ref name="palaces" />
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<br clear=all>
  
 
==Evidence==
 
==Evidence==
The Deep Sea Drilling Project sought evidence of volcanic cores beneath coral reefs and found it. First, in 1952 at the Einwetok Atoll in the Marshall islands, and again, in 1960 at the Midway Atoll, teams found volcanic rock strongly supporting Darwin's theory that coral reefs form around submerging islands. However, not all coral reefs have similar evidence, meaning Darwin outlined one way reefs form, not the only way.<ref> Strykowski and Bonem, p. 20 </ref>
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The Deep Sea Drilling Project sought evidence of volcanic cores beneath coral reefs and found it. First, in 1952 at the Einwetok Atoll in the Marshall islands, and again, in 1960 at the Midway Atoll, teams found volcanic rock strongly supporting Darwin's theory that coral reefs form around submerging islands. Today, Darwin's theory is universally accepted as a means of explaining these reef formations. <ref name="palaces" />  
  
  
==Notes==
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While many of the Pacific reefs form around islands as Darwin's theory describes, this is not the case in the Caribbean where there are few [[atolls]]. Here, other reef types like [[PatchReefs|patch]] and [[BankReefs|bank]] are also exhibited and form separately than Darwin's theory describes. <ref> Alevizon, William. "Types of Coral Reefs." http://coral-reef-info.com 2012. Web. 25 Feb 2013. </ref>
<references/>
 
  
 
==References==
 
==References==
*Strykowski, Joe and Rena M. Bonem. Palaces Under the Sea. Crystal River, FL: Star Thrower Foundation, 1993, p. 19-26. Print.
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<references/>

Latest revision as of 22:03, 16 February 2017

Darwin's Theory

In the late 1830's Charles Darwin spent several years in South America studying crustal movements, elevation, and subsidence. Along with Charles Lyell, he sought an answer to the question of South America's elevation. Ironically, his work on subsidence led to a now universally accepted theory of reef formation. [1] In his 1842 report Coral Reefs, Darwin grouped coral reefs into three distinct types: barrier, fringing, and atolls. He then explained that each reef type was really a separate stage of reef development around a slowly sinking volcanic island. [2]

The Theory

[3]
aerial photos of the three types of reefs from left to right: atoll, fringing, barrier. image credit: coral-reef-info.com

Stage 1 - Fringing Reef A submarine volcano forms an island rising from the sea floor. Corals begin to grow in the shallow regions off the coast of the island. As the island gradually sinks, the reef grows upward in order to stay within a sunlit range. A fringing reef is a reef encircling this volcanic island while it first begins to sink.[2]


Stage 2 - Barrier Reef As the volcanic island continues to sink, a lagoon begins to form between the reef and the exposed island. In this phase, the reef is a barrier reef.[2]


Stage 3 - Atoll Once the volcanic island is fully submerged, the reef is known as an atoll. The reef outline is circular with a central lagoon.[2]


Evidence

The Deep Sea Drilling Project sought evidence of volcanic cores beneath coral reefs and found it. First, in 1952 at the Einwetok Atoll in the Marshall islands, and again, in 1960 at the Midway Atoll, teams found volcanic rock strongly supporting Darwin's theory that coral reefs form around submerging islands. Today, Darwin's theory is universally accepted as a means of explaining these reef formations. [2]


While many of the Pacific reefs form around islands as Darwin's theory describes, this is not the case in the Caribbean where there are few atolls. Here, other reef types like patch and bank are also exhibited and form separately than Darwin's theory describes. [4]

References

  1. Burkhardt, Frederick. "Darwin and Coral Reefs." Darwin Correspondence Project. University of Cambridge, 2012. http://www.darwinproject.ac.uk/darwin-coral-reefs 25 Feb 2013.
  2. 2.0 2.1 2.2 2.3 2.4 Strykowski, Joe and Rena M. Bonem. Palaces Under the Sea. Crystal River, FL: Star Thrower Foundation, 1993, p. 19-26. Print.
  3. Strykowski and Bonem, p. 19
  4. Alevizon, William. "Types of Coral Reefs." http://coral-reef-info.com 2012. Web. 25 Feb 2013.