Ceratitida: Difference between revisions
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{{Short description|Extinct order of molluscs}} |
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{{Automatic taxobox |
{{Automatic taxobox |
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| fossil_range = {{fossilrange| |
| fossil_range = {{fossilrange|Middle Permian|Late Triassic| Middle Permian - Late Triassic }} |
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| taxon = Ceratitida |
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|image = Ceratites nodosus MHNT.PAL.CEP.2001.105.jpg |
| image = Ceratites nodosus MHNT.PAL.CEP.2001.105.jpg |
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|image_caption = ''Ceratites nodosus'' Upper |
| image_caption = ''[[Ceratites nodosus]]'', Upper Muschelkalk - Germany |
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| authority = [[Karl Alfred von Zittel|Zittel]], (1884) |
| authority = [[Karl Alfred von Zittel|Zittel]], (1884) |
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| subdivision_ranks = Superfamilies |
| subdivision_ranks = Superfamilies |
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| subdivision = |
| subdivision = See text |
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}} |
}} |
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'''Ceratitida''' is an order that contains almost all [[Ammonoidea|ammonoid]] cephalopod genera from the [[Triassic]] as well as ancestral forms from the Upper [[Permian]], the exception being the [[Phylloceratina|phylloceratids]] which gave rise to the great diversity of post |
'''Ceratitida''' is an order that contains almost all [[Ammonoidea|ammonoid]] [[cephalopod]] genera from the [[Triassic]] as well as ancestral forms from the Upper [[Permian]], the exception being the [[Phylloceratina|phylloceratids]] which gave rise to the great diversity of post-Triassic [[Ammonitida|ammonites]]. |
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Ceratitids overwhelmingly produced planospirally coiled discoidal shells that may be evolute with inner whorls exposed or involute with only the outer whorl showing. In a few later forms the shell became subglobular, in others, trochoidal or uncoiled. Sutures are typically ceratitic, with smooth saddles and serrate or digitized lobes. In a few the sutures are goniatitic while in others they are ammonitic. |
Ceratitids overwhelmingly produced planospirally coiled discoidal shells that may be evolute with inner whorls exposed or involute with only the outer whorl showing. In a few later forms the shell became subglobular, in others, trochoidal or uncoiled. Sutures are typically ceratitic, with smooth saddles and serrate or digitized lobes. In a few the sutures are goniatitic while in others they are ammonitic. |
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== Taxonomy == |
== Taxonomy == |
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* Ceratitida |
* Ceratitida |
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**[[ |
**[[Ceratitoidea]] |
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**[[ |
**[[Choristoceratoidea]] |
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**[[ |
**[[Clydonitoidea]] |
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**[[ |
**[[Danubitoidea]] |
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**[[ |
**[[Dinaritoidea]] |
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**[[ |
**[[Lobitoidea]] |
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**[[ |
**[[Meekoceratoidea]] |
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**[[ |
**[[Megaphyllitoidea]] |
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**[[ |
**[[Nathorstitoidea]] |
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**[[ |
**[[Noritoidea]] |
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**[[ |
**[[Otoceratoidea]] |
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**[[ |
**[[Pinacoceratoidea]] |
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**[[ |
**[[Ptychitoidea]] |
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**[[ |
**[[Sageceratoidea]] |
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**[[ |
**[[Tropitoidea]] |
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**[[ |
**[[Xenodiscoidea]] |
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**[[Xenodiscaceae ]] |
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Only eight |
Only eight superfamilies are shown in the [[Treatise on Invertebrate Paleontology]], Part L,(1957), the Otocerataceae, Noritaceae, Ceratitaceae, Arcestaceae, Clydonitaceae, Lobitaceae, Ptychitaceae, and Tropitaceae, in text sequence. The other 10 have been added since, derived from within the original eight.{{citation needed|date=October 2014}} |
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==References== |
== References == |
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{{Reflist}} |
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* Arkell et al., 1962, Mesozoic Ammonoidea. [[Treatise on Invertebrate Paleontology]] part L, Mollusca 4, Ammonoidea. R.C. Moore (ed) |
* Arkell et al., 1962, Mesozoic Ammonoidea. [[Treatise on Invertebrate Paleontology]] part L, Mollusca 4, Ammonoidea. R.C. Moore (ed) |
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*[ |
*[https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=94126 Paleobiology Database] |
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{{fossil cephalopods}} |
{{fossil cephalopods}} |
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{{Taxonbar|from=Q1054661}} |
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[[Category:Ceratitida]] |
[[Category:Ceratitida| ]] |
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[[Category: |
[[Category:Guadalupian first appearances]] |
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[[Category:Triassic extinctions]] |
[[Category:Late Triassic extinctions]] |
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[[Category:Mollusc orders]] |
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{{ |
{{Ceratitida-stub}} |
Latest revision as of 19:42, 18 November 2024
Ceratitida Temporal range:
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Ceratites nodosus, Upper Muschelkalk - Germany | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Mollusca |
Class: | Cephalopoda |
Subclass: | †Ammonoidea |
Order: | †Ceratitida Zittel, (1884) |
Superfamilies | |
See text |
Ceratitida is an order that contains almost all ammonoid cephalopod genera from the Triassic as well as ancestral forms from the Upper Permian, the exception being the phylloceratids which gave rise to the great diversity of post-Triassic ammonites.
Ceratitids overwhelmingly produced planospirally coiled discoidal shells that may be evolute with inner whorls exposed or involute with only the outer whorl showing. In a few later forms the shell became subglobular, in others, trochoidal or uncoiled. Sutures are typically ceratitic, with smooth saddles and serrate or digitized lobes. In a few the sutures are goniatitic while in others they are ammonitic.
Taxonomy
[edit]- Ceratitida
Only eight superfamilies are shown in the Treatise on Invertebrate Paleontology, Part L,(1957), the Otocerataceae, Noritaceae, Ceratitaceae, Arcestaceae, Clydonitaceae, Lobitaceae, Ptychitaceae, and Tropitaceae, in text sequence. The other 10 have been added since, derived from within the original eight.[citation needed]
References
[edit]- Arkell et al., 1962, Mesozoic Ammonoidea. Treatise on Invertebrate Paleontology part L, Mollusca 4, Ammonoidea. R.C. Moore (ed)
- Paleobiology Database