Difference between revisions of "Category:Coral"
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Imported from: [[imported from::core:Coral]] | Imported from: [[imported from::core:Coral]] | ||
| − | The geochemical tracers contain in the skeletons of [https://en.wikipedia.org/wiki/Coral corals] provide an unaltered record of the chemical and physical conditions that existed in the surrounding seawater at the time of accretion of its calcium carbonate skeleton < | + | <p>The geochemical tracers contain in the skeletons of [https://en.wikipedia.org/wiki/Coral corals] provide an unaltered record of the chemical and physical conditions that existed in the surrounding seawater at the time of accretion of its calcium carbonate skeleton <sup id="cite_ref-druffel1997_1-0" class="reference">[#cite_note-druffel1997-1 [1]]</sup> <sup id="cite_ref-2" class="reference"><a href="#cite_note-2">[2]</a></sup>. |
| − | + | </p><p>Corals are from the order Scleractinian, a group in the subclass Zoantharia. Scleractinians include solitary and colonial species of corals. may of which secrete external skeletons of [https://en.wikipedia.org/wiki/Aragonite aragonite] <sup id="cite_ref-druffel1997_1-2" class="reference">[#cite_note-3 [3]]</sup>. | |
| − | Corals are from the order Scleractinian, a group in the subclass Zoantharia. Scleractinians include solitary and colonial species of corals. may of which secrete external skeletons of [https://en.wikipedia.org/wiki/Aragonite aragonite] < | + | </p> |
| − | + | The polyp portion of the coral secretes calcium carbonate (CaCO<sub>3</sub>) as the mineral aragonite <sup id="cite_ref-druffel1997_1-3" class="reference">[https://en.wikipedia.org/wiki/Hermatypic_coral hermatypic corals] (i.e., reef-building corals) are more desirable than the branching varieties for paleoreconstructions. First, massive corals form round, wave-resistant structures that can include hundreds of years of uninterrupted growth. Second, the accretion rate of calcium carbonate is much higher for hermatypic corals that contain symbiotic [https://en.wikipedia.org/wiki/Zooxanthellae zooxanthellae] than for deep species <sup id="cite_ref-druffel1997_1-4" class="reference">[#cite_note-4 [4]]</sup><ol class="references"> | |
| − | The polyp portion of the coral secretes calcium carbonate (CaCO<sub>3</sub>) as the mineral aragonite [https://en.wikipedia.org/wiki/Hermatypic_coral hermatypic corals] (i.e., reef-building corals) are more desirable than the branching varieties for paleoreconstructions. First, massive corals form round, wave-resistant structures that can include hundreds of years of uninterrupted growth. Second, the accretion rate of calcium carbonate is much higher for hermatypic corals that contain symbiotic [https://en.wikipedia.org/wiki/Zooxanthellae zooxanthellae] than for deep species < | + | <li id="cite_note-druffel1997-1"><span class="mw-cite-backlink">? <sup>[#cite_ref-druffel1997_1-1 1.1]</sup> <sup>[#cite_ref-druffel1997_1-3 1.3]</sup> <sup><a href="#cite_ref-druffel1997_1-4">1.4</a></sup></span> <span class="reference-text">Druffel, E. R. M. (1997). Geochemistry of corals: Proxies of past ocean chemistry, ocean circulation, and climate. Proceeding of the National Academy of Sciences, 94, 8354-8361. </span> |
| − | + | </li> | |
| − | == | + | <li id="cite_note-2"><span class="mw-cite-backlink"><a href="#cite_ref-2">?</a></span> <span class="reference-text"> Gagan, M. K., Ayliffe, L. K., Beck, J. W., Cole, J. E., Druffel, E. R. M., Dunbar, R. B., & Schrag, D. P. (2000). New views of tropical paleoclimates from corals. Quaternary Science Reviews, 19(1-5), 45-64. doi:10.1016/S0277-3791(99)00054-2</span> |
| − | + | </li> | |
| − | + | <li id="cite_note-3"><span class="mw-cite-backlink"><a href="#cite_ref-3">?</a></span> <span class="reference-text"> Stanley, G. (1981). Early history of scleractinian corals and its geological consequences. Geology, 9, 507-511. </span> | |
| − | + | </li> | |
| − | + | <li id="cite_note-4"><span class="mw-cite-backlink"><a href="#cite_ref-4">?</a></span> <span class="reference-text">Knutson, D. W., Buddemeier, R. W., & Smith, S. V. (1972). Coal chronologies: seasonal growth bands in reef corals. Science, 177, 270-272. </span> | |
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<!-- Do not edit below this unless you know what you are doing --> | <!-- Do not edit below this unless you know what you are doing --> | ||
Revision as of 08:26, 12 November 2020
Category: Coral [1]
Imported from: core:Coral (core | Linked Earth Core)
The geochemical tracers contain in the skeletons of corals provide an unaltered record of the chemical and physical conditions that existed in the surrounding seawater at the time of accretion of its calcium carbonate skeleton [#cite_note-druffel1997-1 [1]] <a href="#cite_note-2">[2]</a>.
Corals are from the order Scleractinian, a group in the subclass Zoantharia. Scleractinians include solitary and colonial species of corals. may of which secrete external skeletons of aragonite [#cite_note-3 [3]].
The polyp portion of the coral secretes calcium carbonate (CaCO3) as the mineral aragonite hermatypic corals (i.e., reef-building corals) are more desirable than the branching varieties for paleoreconstructions. First, massive corals form round, wave-resistant structures that can include hundreds of years of uninterrupted growth. Second, the accretion rate of calcium carbonate is much higher for hermatypic corals that contain symbiotic zooxanthellae than for deep species [#cite_note-4 [4]]- ? [#cite_ref-druffel1997_1-1 1.1] [#cite_ref-druffel1997_1-3 1.3] <a href="#cite_ref-druffel1997_1-4">1.4</a> Druffel, E. R. M. (1997). Geochemistry of corals: Proxies of past ocean chemistry, ocean circulation, and climate. Proceeding of the National Academy of Sciences, 94, 8354-8361.
- <a href="#cite_ref-2">?</a> Gagan, M. K., Ayliffe, L. K., Beck, J. W., Cole, J. E., Druffel, E. R. M., Dunbar, R. B., & Schrag, D. P. (2000). New views of tropical paleoclimates from corals. Quaternary Science Reviews, 19(1-5), 45-64. doi:10.1016/S0277-3791(99)00054-2
- <a href="#cite_ref-3">?</a> Stanley, G. (1981). Early history of scleractinian corals and its geological consequences. Geology, 9, 507-511.
- <a href="#cite_ref-4">?</a> Knutson, D. W., Buddemeier, R. W., & Smith, S. V. (1972). Coal chronologies: seasonal growth bands in reef corals. Science, 177, 270-272.
Category Semantics
- Sub-Class of
Pages in category "Coral"
The following 70 pages are in this category, out of 70 total.
