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- Conodont_Alteration_Index abstract "The Conodont Alteration Index (CAI) is used to estimate the maximum temperature reached by a sedimentary rock using thermal alteration of conodont fossils. Conodonts in fossiliferous carbonates are prepared by dissolving the matrix with acid, since the conodonts are composed of apatite and thus do not dissolve. The fossils are then compared to the index under a microscope.The CAI ranges from 1 to 6, as follows:The CAI is commonly used by paleontologists due to its ease of measurement and the abundance of Conodonta throughout marine carbonates of the Paleozoic. However, the organism disappears from the fossil record after the Triassic period, so the CAI is not available to analyze rocks younger than 200 million years. Additionally, the index can be positively skewed in regions of hydrothermal alteration.".
- Conodont_Alteration_Index wikiPageExternalLink cono-tafel.jpg.
- Conodont_Alteration_Index wikiPageID "8908470".
- Conodont_Alteration_Index wikiPageLength "2037".
- Conodont_Alteration_Index wikiPageOutDegree "13".
- Conodont_Alteration_Index wikiPageRevisionID "673468100".
- Conodont_Alteration_Index wikiPageWikiLink Apatite.
- Conodont_Alteration_Index wikiPageWikiLink Carbonate.
- Conodont_Alteration_Index wikiPageWikiLink Carbonates.
- Conodont_Alteration_Index wikiPageWikiLink Category:Conodonts.
- Conodont_Alteration_Index wikiPageWikiLink Category:Fossil_record_of_animals.
- Conodont_Alteration_Index wikiPageWikiLink Category:Sedimentology.
- Conodont_Alteration_Index wikiPageWikiLink Conodont.
- Conodont_Alteration_Index wikiPageWikiLink Foraminiferal_Colouration_Index.
- Conodont_Alteration_Index wikiPageWikiLink Metamorphism.
- Conodont_Alteration_Index wikiPageWikiLink Paleozoic.
- Conodont_Alteration_Index wikiPageWikiLink Sedimentary_rock.
- Conodont_Alteration_Index wikiPageWikiLink Senckenbergiana_Lethaea.
- Conodont_Alteration_Index wikiPageWikiLink Triassic.
- Conodont_Alteration_Index wikiPageWikiLinkText "Conodont Alteration Index".
- Conodont_Alteration_Index hasPhotoCollection Conodont_Alteration_Index.
- Conodont_Alteration_Index wikiPageUsesTemplate Template:Cite_journal.
- Conodont_Alteration_Index wikiPageUsesTemplate Template:Ma.
- Conodont_Alteration_Index subject Category:Conodonts.
- Conodont_Alteration_Index subject Category:Fossil_record_of_animals.
- Conodont_Alteration_Index subject Category:Sedimentology.
- Conodont_Alteration_Index type Subfield.
- Conodont_Alteration_Index comment "The Conodont Alteration Index (CAI) is used to estimate the maximum temperature reached by a sedimentary rock using thermal alteration of conodont fossils. Conodonts in fossiliferous carbonates are prepared by dissolving the matrix with acid, since the conodonts are composed of apatite and thus do not dissolve.".
- Conodont_Alteration_Index label "Conodont Alteration Index".
- Conodont_Alteration_Index sameAs m.027p66b.
- Conodont_Alteration_Index sameAs Q5162129.
- Conodont_Alteration_Index sameAs Q5162129.
- Conodont_Alteration_Index wasDerivedFrom Conodont_Alteration_Index?oldid=673468100.
- Conodont_Alteration_Index isPrimaryTopicOf Conodont_Alteration_Index.