Category:Coral - Revision history

Admin: Reverted edits by Admin (talk) to last revision by Khider

2020-11-12T15:58:16Z

Reverted edits by Admin (talk) to last revision by Khider

Admin: WTBootstrap: New Category Coral

2020-11-12T15:26:11Z

WTBootstrap: New Category Coral

Khider: /* Datasets based on Coral Archives */ Add number of datasets with the archive type

2017-05-16T14:54:19Z

‎Datasets based on Coral Archives: Add number of datasets with the archive type

New page

===Category: Coral [http://linked.earth/ontology#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 <ref name=druffel1997> 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. </ref> <ref> 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 </ref>

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] <ref>Stanley, G. (1981). Early history of scleractinian corals and its geological consequences. Geology, 9, 507-511.</ref>.

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 <ref> Knutson, D. W., Buddemeier, R. W., & Smith, S. V. (1972). Coal chronologies: seasonal growth bands in reef corals. Science, 177, 270-272. </ref>.

== Datasets based on Coral Archives==

Currently, the LinkedEarth wiki hosts {{#ask:
[[Category:Dataset_(L)]]
[[IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).HasProxySystem_(L).ProxyArchiveType_(L)::Coral]] OR [[Category:Location_(L)]] [[CoordinatesFor.ArchiveType::coral]]
| format = count
}} datasets based on coral archives.



{{#ask:
[[Category:Dataset_(L)]]
[[IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).HasProxySystem_(L).ProxyArchiveType_(L)::Coral]] OR [[Category:Location_(L)]] [[CoordinatesFor.ArchiveType::coral]]
| ?CollectedFrom_(L).Coordinates
| ?Name_(L)
| ?IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).ProxyObservationType_(L)
| showtitle=off
| maxzoom=14
| minzoom=1
| limit=500
| template=ByArchiveLocation
| format=leaflet
}}

==References ==

<references/>



Category Semantics
* Sub-Class of
** [[subcategory of::Category:ProxyArchive (L)]]

[[Category:ProxyArchive (L)]]

@@ Line 3: / Line 3: @@
 Imported from: [[imported from::core:Coral]]
-<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>.
+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 <ref name=druffel1997> 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. </ref> <ref> Gagan, M. K., Ayliffe, L. K., Beck, J. W., Cole, J. E., Druffel, E. R. M., Dunbar, R. B., &amp; 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 </ref>
-</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>.
-</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] <ref>Stanley, G. (1981). Early history of scleractinian corals and its geological consequences. Geology, 9, 507-511.</ref>.
-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">
-<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>
+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 <ref> Knutson, D. W., Buddemeier, R. W., &amp; Smith, S. V. (1972). Coal chronologies: seasonal growth bands in reef corals. Science, 177, 270-272.  </ref>.
-</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., &amp; 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>
+== Datasets based on Coral Archives==
-</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>
+Currently, the LinkedEarth wiki hosts {{#ask:
-</li>
+[[Category:Dataset_(L)]]
-<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., &amp; Smith, S. V. (1972). Coal chronologies: seasonal growth bands in reef corals. Science, 177, 270-272. </span>
+[[IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).HasProxySystem_(L).ProxyArchiveType_(L)::Coral]] OR [[Category:Location_(L)]] [[CoordinatesFor.ArchiveType::coral]]
-</li>
+| format = count
-</ol>
+}} datasets based on coral archives.
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