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{{Short description|Superfamily of molluscs (fossil)}}
{{Taxobox
{{Automatic taxobox
|name = ''Xenodiscaceae''
|fossil_range = Middle to late [[Permian]]
| fossil_range = {{Fossil range|Guadalupian|Early Triassic}}
| image = Xenodiscidae - Xenodiscus besairiei.JPG
|regnum = [[Animal]]ia
| image_caption = ''Xenodiscus besairiei'' on display at the [[Museo Civico di Storia Naturale di Milano]]
|phylum = [[Mollusc]]a
| taxon = Xenodiscoidea
|classis = [[Cephalopod]]a
⚫
| subdivision_ranks = Families
|subclassis = [[Ammonoidea]]
⚫
| subdivision =
|ordo = [[Ceratitida]]
|subordo = [[Paraceltitina]]
|superfamilia = Xenodiscaceae
⚫
|subdivision_ranks = Families
⚫
|subdivision =
* [[Dzhulfitidae]]
* [[Dzhulfitidae]]
* [[Huananoceratidae]]
* [[Huananoceratidae]]
Line 23: Line 19:
}}
}}


The '''Xenodiscaceae''' is a superfamily within the [[ammonoidea|ammonoid]] order [[Ceratitida]]. The Xenodiscaceae, named by Frech in 1902, presently contains ten families, only one of which was included in the original '''Otocerataceae''' of Hyatt, 1900, the remaining having been added.
'''Xenodiscoidea''', formerly '''Xenodiscaceae''', is a superfamily within the [[ammonoidea|ammonoid]] order [[Ceratitida]]. The superfamily was named by Frech in 1902, presently contains ten families, only one of which was included in the original '''Otocerataceae''' of Hyatt, 1900, the remaining having been added.


The Xenodiscaceae has its origin in the Middle [[Permian]] in the [[prolecanitida|prolecanitid]] Daraelitidae through the ancestral Xenodiscidae. According to Kummel (1952) and Arkell et al. (1957) the Xenodiscidae gave rise to the Otoceratidae and Ophiceratidae. The Ophiceratidae in turn gave rise to the Dieneroceratidae which is considered the source for all remaining ceratitid stocks. All four families made up the original Otocerataceae
The Xenodiscoidea has its origins in the Middle [[Permian]] in the [[prolecanitida|prolecanitid]] Daraelitidae through the ancestral Xenodiscidae. According to Kummel (1952) and Arkell et al. (1957) the Xenodiscidae gave rise to the [[Otoceratidae]] and [[Ophiceratidae]]. The Ophiceratidae in turn gave rise to the Dieneroceratidae which is considered the source for all remaining ceratitid stocks. All four families made up the original Otocerataceae


The Xenodiscidae is removed from the Otocerataceae as originally perceived (Arkell et al. 1957) to become the root of Xenodiscaceae, as emended. The Otoceratidae remains the type family of the Otocerataceae as revised. The Ophiceratidae is reassigned to the Noritaceae along with the Dieneroceratidae.
The Xenodiscidae is removed from the Otocerataceae as originally perceived (Arkell et al. 1957) to become the root of Xenodiscoidea, as emended. The Otoceratidae remains the type family of the Otocerataceae as revised. The Ophiceratidae is reassigned to the Noritaceae along with the Dieneroceratidae.


The Huananoceratidae, Liuchengoeratidae, Plueronodoceratidae, and Tapshanitidae, described by Zhao et al. 1978,{{Page needed|date=February 2010}} include Late Permian and Early Triassic genera from Asia. The Xenoceltitidae, established by Spath in 1930 are included in the Treatise in the superfamily Noritaceae
The Huananoceratidae, Liuchengoeratidae, Plueronodoceratidae, and Tapshanitidae, described by Zhao et al. 1978,{{full citation needed|date=February 2010}} include Late Permian and Early Triassic genera from Asia. The Xenoceltitidae, established by Spath in 1930 are included in the Treatise in the superfamily Noritaceae


The Xenodiscaceae gave rise through the Ophiceratidae to the Noritaceae. and through the Paraceltitidae to the revised Otocerataceae
The Xenodiscoidea gave rise through the Ophiceratidae to the Noritaceae. and through the Paraceltitidae to the revised Otocerataceae


==References==
== References ==
{{Reflist}}
*{{Citation |last=Arkell |first=W. J. |last2=Kummel |first2=B. |last3=Wright |first3=C. W. |year=1957 |chapter=Mesozoic Ammonoidea: Suborder Ceratitina |editor-first=Raymond Cecil |editor-last=Moore |title=Treatise on Invertebrate Paleontology |volume=Part L |pages=L130–147 |location=New York |publisher=Geological Society of America }}.
*{{Citation |last=Kummel |first=Bernhard |year=1952 |title=A Classification of the Triassic Ammonoids |journal=[[Journal of Paleontology]] |volume=26 |issue=5 |pages=847–853 |doi=10.2307/1299888 }}.
* {{Citation |last1=Arkell |first1=W. J. |last2=Kummel |first2=B. |last3=Wright |first3=C. W. |year=1957 |chapter=Mesozoic Ammonoidea: Suborder Ceratitina |editor-first=Raymond Cecil |editor-last=Moore |title=Treatise on Invertebrate Paleontology |volume=Part L |pages=L130–147 |location=New York |publisher=Geological Society of America }}.
* {{Citation |last=Kummel |first=Bernhard |year=1952 |title=A Classification of the Triassic Ammonoids |journal=[[Journal of Paleontology]] |volume=26 |issue=5 |pages=847–853 |jstor=1299888 }}.
*{{Citation |url=http://paleodb.org/cgi-bin/bridge.pl?action=checkTaxonInfo&taxon_no=86642&is_real_user=1 |title=The Paleobiology Database |month=November |year=2008 }}.
* {{Citation |url=http://paleodb.org/cgi-bin/bridge.pl?action=checkTaxonInfo&taxon_no=86642&is_real_user=1 |title=The Paleobiology Database |date=November 2008 }}.


{{Taxonbar|from1=Q21857369|from2=Q8043565}}
⚫
[[Category:Ceratitida]]


[[Category:Xenodiscoidea| ]]
⚫
[[Category:Ceratitida superfamilies]]
[[Category:Guadalupian first appearances]]
[[Category:Early Triassic extinctions]]



{{Ammonite-stub}}
{{Ceratitida-stub}}

Latest revision as of 13:32, 11 May 2024

Xenodiscoidea
Temporal range: Guadalupian–Early Triassic
Xenodiscus besairiei on display at the Museo Civico di Storia Naturale di Milano
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Mollusca
Class: Cephalopoda
Subclass: †Ammonoidea
Order: †Ceratitida
Suborder: †Paraceltitina
Superfamily: †Xenodiscoidea
Families

Xenodiscoidea, formerly Xenodiscaceae, is a superfamily within the ammonoid order Ceratitida. The superfamily was named by Frech in 1902, presently contains ten families, only one of which was included in the original Otocerataceae of Hyatt, 1900, the remaining having been added.

The Xenodiscoidea has its origins in the Middle Permian in the prolecanitid Daraelitidae through the ancestral Xenodiscidae. According to Kummel (1952) and Arkell et al. (1957) the Xenodiscidae gave rise to the Otoceratidae and Ophiceratidae. The Ophiceratidae in turn gave rise to the Dieneroceratidae which is considered the source for all remaining ceratitid stocks. All four families made up the original Otocerataceae

The Xenodiscidae is removed from the Otocerataceae as originally perceived (Arkell et al. 1957) to become the root of Xenodiscoidea, as emended. The Otoceratidae remains the type family of the Otocerataceae as revised. The Ophiceratidae is reassigned to the Noritaceae along with the Dieneroceratidae.

The Huananoceratidae, Liuchengoeratidae, Plueronodoceratidae, and Tapshanitidae, described by Zhao et al. 1978,[full citation needed] include Late Permian and Early Triassic genera from Asia. The Xenoceltitidae, established by Spath in 1930 are included in the Treatise in the superfamily Noritaceae

The Xenodiscoidea gave rise through the Ophiceratidae to the Noritaceae. and through the Paraceltitidae to the revised Otocerataceae

References

[edit]
  • Arkell, W. J.; Kummel, B.; Wright, C. W. (1957), "Mesozoic Ammonoidea: Suborder Ceratitina", in Moore, Raymond Cecil (ed.), Treatise on Invertebrate Paleontology, vol. Part L, New York: Geological Society of America, pp. L130–147.
  • Kummel, Bernhard (1952), "A Classification of the Triassic Ammonoids", Journal of Paleontology, 26 (5): 847–853, JSTOR 1299888.
  • The Paleobiology Database, November 2008.


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