Linguliformea: Difference between revisions
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| subdivision = {{Linked taxon list <!-- following the Treatise, 2000 --> |
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| name = Linguliformea |
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| Lingulata | |
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| regnum = [[Animal]]ia |
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| Paterinata | |
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| phylum = [[Brachiopod]]a |
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| subphylum = '''Linguliformea''' |
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| subdivision_ranks = Classes |
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| subdivision = [[Lingulata]]<br />[[Paterinata]] |
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'''Linguliformea''' is a subphylum of inarticulate [[brachiopod]]s.<ref>{{Cite journal|last=Torres-Martínez,M.A., Sour-Tovar,F.,|year=2016|title=Braquiópodos discínidos (Lingulida, Discinoidea) de la Formación Ixtaltepec, Carbonífero del área de Santiago Ixtaltepec, Oaxaca|url=http://boletinsgm.igeolcu.unam.mx/bsgm/vols/epoca04/6802/(9)Torres.pdf|journal=Boletín de la Sociedad Geológica Mexicana|volume=68|pages=313–321}}</ref> These were the earliest of brachiopods, ranging from the [[Cambrian]] into the [[Holocene]]. They rapidly diversified during the Cambrian into the [[Ordovician]], but most families became extinct by the end of the [[Devonian]]. |
'''Linguliformea''' is a subphylum of inarticulate [[brachiopod]]s.<ref>{{Cite journal|last=Torres-Martínez,M.A., Sour-Tovar,F.,|year=2016|title=Braquiópodos discínidos (Lingulida, Discinoidea) de la Formación Ixtaltepec, Carbonífero del área de Santiago Ixtaltepec, Oaxaca|url=http://boletinsgm.igeolcu.unam.mx/bsgm/vols/epoca04/6802/(9)Torres.pdf|journal=Boletín de la Sociedad Geológica Mexicana|volume=68|pages=313–321}}</ref> These were the earliest of brachiopods, ranging from the [[Cambrian]] into the [[Holocene]]. They rapidly diversified during the Cambrian into the [[Ordovician]], but most families became extinct by the end of the [[Devonian]]. |
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Revision as of 09:33, 12 October 2017
 | This article needs additional citations for verification. (November 2016) |
| Linguliformea | |
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Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Brachiopoda |
| Subphylum: | Linguliformea |
| Classes | |
Linguliformea is a subphylum of inarticulate brachiopods.[1] These were the earliest of brachiopods, ranging from the Cambrian into the Holocene. They rapidly diversified during the Cambrian into the Ordovician, but most families became extinct by the end of the Devonian.
The articulation in these brachiopods is lacking. These brachiopods have adductor and oblique muscles, but no diductor muscles. The anus is located at the side of the body. The pedicle is a hollow extension of the ventral body wall. Posterior body wall separates dorsal and ventral mantles.
The shells are usually made up of apatite (calcium phosphate), however rare cases have calcite or aragonite shells.
See also
References
- ^ Torres-Martínez,M.A., Sour-Tovar,F., (2016). "Braquiópodos discínidos (Lingulida, Discinoidea) de la Formación Ixtaltepec, Carbonífero del área de Santiago Ixtaltepec, Oaxaca" (PDF). Boletín de la Sociedad Geológica Mexicana. 68: 313–321.
{{cite journal}}: CS1 maint: extra punctuation (link) CS1 maint: multiple names: authors list (link)
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