Plectronoceratoidea: Difference between revisions
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| taxon = Plectronoceratoidea |
| taxon = Plectronoceratoidea |
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| authority = Wade, 1988 |
| authority = Wade, 1988 |
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| subdivision_ranks = Orders |
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| subdivision = |
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*†[[Plectronocerida]] |
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*†[[Yanhecerida]] |
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*†[[Protactinocerida]] |
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*†[[Ellesmerocerida]] ([[paraphyletic]]) |
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}} |
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'''Plectronoceratoidea''' is a superorder or subclass containing primitive [[Nautiloidea|nautiloids]] from the Late [[Cambrian]] and Early [[Ordovician]]. This group is best considered a [[Paraphyly|paraphyletic]] [[Evolutionary grade|grade]] of early [[Cephalopod|cephalopods]], as it contains the ancestors of subsequent post-Cambrian cephalopod orders.<ref>{{Cite journal |last=Mutvei |first=Harry |date=2020-04-02 |title=Restudy of some plectronocerid nautiloids (Cephalopoda) from the late Cambrian of China; discussion on nautiloid evolution and origin of the siphuncle |url=https://www.diva-portal.org/smash/get/diva2:1515645/FULLTEXT01.pdf |journal=GFF |volume=142 |issue=2 |pages=115–124 |doi=10.1080/11035897.2020.1739742 |issn=1103-5897}}</ref><ref name=":0">{{Cite journal |vauthors=King AH, Evans DH |date=2019 |title=High-level classification of the nautiloid cephalopods: a proposal for the revision of the Treatise Part K |url=https://sjpp.springeropen.com/articles/10.1007/s13358-019-00186-4 |journal=Swiss Journal of Palaeontology |language=en |volume=138 |issue=1 |pages=65–85 |doi=10.1007/s13358-019-00186-4 |issn=1664-2384}}</ref> |
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'''Plectronoceratoidea''' is a superorder of primitive [[Nautiloidea|nautiloids]] from the Late [[Cambrian]] and Early [[Ordovician]] that include the ancestors of subsequent [[Cephalopoda|cephalopod]] orders. Included within are the exclusively Cambrian [[Plectronocerida]], [[Protactinocerida]], and [[Yanhecentida]], and the Cambro-Ordovician [[Ellesmerocerida]]. |
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Plectronoceratoidea contains several exclusively Cambrian cephalopod orders: [[Plectronocerida]], [[Protactinocerida]], and [[Yanhecerida]].<ref name=":0" /> Under some classification schemes, the plectronoceratoid grade may also contain the paraphyletic Cambro-Ordovician [[Ellesmerocerida]].<ref name=":1">{{cite journal |display-authors=6 |vauthors=Pohle A, Kröger B, Warnock RC, King AH, Evans DH, Aubrechtová M, Cichowolski M, Fang X, Klug C |date=April 2022 |title=Early cephalopod evolution clarified through Bayesian phylogenetic inference |journal=BMC Biology |volume=20 |issue=1 |pages=88 |doi=10.1186/s12915-022-01284-5 |pmc=9008929 |pmid=35421982}}</ref> A few older studies consider Plectronocerida to be descended from Ellesmerocerida (rather than ancestral),<ref>{{Cite journal |last=Flower |first=Rousseau H. |date=1964 |title=The nautiloid order Ellesmeroceratida (Cephalopoda) |url=https://geoinfo.nmt.edu/publications/monographs/memoirs/downloads/12/Memoir-12.pdf |journal=New Mexico Bureau of Mines and Mineral Resources Memoir |volume=12 |pages=1-164}}</ref> but this is no longer believed to be the case.<ref name=":0" /> |
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The Plectronocerida is the earliest group of the four and gave rise to the other three. Of these four orders, only the Ellesmerocerida crossed (barely) into the Ordovician, with two genera, ''[[Ectenolites]]'' and ''[[Clarkoceras]]''. The Ellesmerocerida in turn gave rise to the superorders [[Endocerida|Endoceratoidea]], [[Actinocerida|Actinoceratoidea]], [[Discosorida|Discosoratoidea]], [[Orthoceratoidea]], and [[Nautilitoidea]]. The Ellesmerocerida, Endoceratoidea, Actinoceratoidea, and Discosoratoidea are restricted to the Paleozoic. The Orthoceratoidea, which extend at least into the [[Triassic]], gave rise to the [[Ammonoidea]] which became extinct by the end of the [[Cretaceous]]. Nautilitoidea exist living today as the [[Nautilidae]], represented by ''[[Nautilus]]'' and ''[[Allonautilus]]''. |
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The Plectronocerida is the earliest group of the four, and may have given rise to the other three.<ref>{{Cite journal |last=Mutvei |first=Harry |last2=Zhang |first2=Yun-Bai |last3=Dunca |first3=Elena |date=2007 |title=LATE CAMBRIAN PLECTRONOCERID NAUTILOIDS AND THEIR ROLE IN CEPHALOPOD EVOLUTION |url=https://onlinelibrary.wiley.com/doi/10.1111/j.1475-4983.2007.00708.x |journal=Palaeontology |language=en |volume=50 |issue=6 |pages=1327–1333 |doi=10.1111/j.1475-4983.2007.00708.x |issn=0031-0239}}</ref> Of these four orders, only the Ellesmerocerida crossed (barely) into the Ordovician, with two genera, ''[[Ectenolites]]'' and ''[[Clarkoceras]]''.<ref>{{Cite journal |last=Jun-yuan |first=Chen |last2=Teichert |first2=Curt |date=1983-11-01 |title=Cambrian cephalopods |url=https://doi.org/10.1130/0091-7613(1983)112.0.CO;2 |journal=Geology |volume=11 |issue=11 |pages=647–650 |bibcode=1983Geo....11..647J |doi=10.1130/0091-7613(1983)11<647:CC>2.0.CO;2 |issn=0091-7613}}</ref> Ordovician ellesmerocerids in turn likely gave rise to several new nautiloid superorders: [[Endocerida|Endoceratoidea]], [[Multiceratoidea]], and [[Orthoceratoidea]]. The Ordovician-Triassic Orthoceratoids are ancestral to post-Paleozoic groups such as ammonoids (ammonites) and coeloids (modern cephalopods without external shells). The origin of modern nautilids is less certain, though they may be descended from coiled multiceratoids or orthoceratoids. Ellesmerocerida proper are restricted to the Paleozoic, though their indirect descendants survive to the present.<ref name=":1" /> |
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Plectronoceratoids are generally small to tiny forms with orthoconic or endogastric shells, a few being exogastric, with proportionally large ventral siphuncles that contain numerous diaphragms. Orders are determined principally by differences in siphuncle detail. |
Plectronoceratoids are generally small to tiny forms with orthoconic or endogastric shells, a few being exogastric, with proportionally large ventral siphuncles that contain numerous diaphragms. Orders are determined principally by differences in siphuncle detail. |
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==References== |
==References== |
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{{reflist}} |
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*{{Cite journal| doi = 10.1130/0091-7613(1983)11<647:CC>2.0.CO;2| issn = 0091-7613| year = 1983| volume = 11| issue = 11| pages = 647–650| title = Cambrian cephalopods | first1 = J. Y. | last1 = Chen| last2 = Teichert | first2 = C.| journal = Geology|bibcode = 1983Geo....11..647J }} |
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*Flower, R.H. 1964, The Nautiloid Order Ellesmeroceratida (Cephalopoda). Memoir 12; New Mexico Bureau of Mines and Mineral Resources, Socorro, NM. |
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*Wade, M. 1988. Nautiloids and their descendants: cephalopod classification in 1986. Memoir 44, pp 15–25; New Mexico Bureau of Mines and Mineral Resources, Socorro, NM. |
*Wade, M. 1988. Nautiloids and their descendants: cephalopod classification in 1986. Memoir 44, pp 15–25; New Mexico Bureau of Mines and Mineral Resources, Socorro, NM. |
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Revision as of 15:40, 29 May 2022
| Plectronoceratoidea Temporal range:
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|---|---|
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Mollusca |
| Class: | Cephalopoda |
| Subclass: | Nautiloidea |
| Superorder: | †Plectronoceratoidea Wade, 1988 |
| Orders | |
Plectronoceratoidea is a superorder or subclass containing primitive nautiloids from the Late Cambrian and Early Ordovician. This group is best considered a paraphyletic grade of early cephalopods, as it contains the ancestors of subsequent post-Cambrian cephalopod orders.[1][2]
Plectronoceratoidea contains several exclusively Cambrian cephalopod orders: Plectronocerida, Protactinocerida, and Yanhecerida.[2] Under some classification schemes, the plectronoceratoid grade may also contain the paraphyletic Cambro-Ordovician Ellesmerocerida.[3] A few older studies consider Plectronocerida to be descended from Ellesmerocerida (rather than ancestral),[4] but this is no longer believed to be the case.[2]
The Plectronocerida is the earliest group of the four, and may have given rise to the other three.[5] Of these four orders, only the Ellesmerocerida crossed (barely) into the Ordovician, with two genera, Ectenolites and Clarkoceras.[6] Ordovician ellesmerocerids in turn likely gave rise to several new nautiloid superorders: Endoceratoidea, Multiceratoidea, and Orthoceratoidea. The Ordovician-Triassic Orthoceratoids are ancestral to post-Paleozoic groups such as ammonoids (ammonites) and coeloids (modern cephalopods without external shells). The origin of modern nautilids is less certain, though they may be descended from coiled multiceratoids or orthoceratoids. Ellesmerocerida proper are restricted to the Paleozoic, though their indirect descendants survive to the present.[3]
Plectronoceratoids are generally small to tiny forms with orthoconic or endogastric shells, a few being exogastric, with proportionally large ventral siphuncles that contain numerous diaphragms. Orders are determined principally by differences in siphuncle detail.
References
- ^ Mutvei, Harry (2020-04-02). "Restudy of some plectronocerid nautiloids (Cephalopoda) from the late Cambrian of China; discussion on nautiloid evolution and origin of the siphuncle" (PDF). GFF. 142 (2): 115–124. doi:10.1080/11035897.2020.1739742. ISSN 1103-5897.
- ^ a b c King AH, Evans DH (2019). "High-level classification of the nautiloid cephalopods: a proposal for the revision of the Treatise Part K". Swiss Journal of Palaeontology. 138 (1): 65–85. doi:10.1007/s13358-019-00186-4. ISSN 1664-2384.
- ^ a b Pohle A, Kröger B, Warnock RC, King AH, Evans DH, Aubrechtová M, et al. (April 2022). "Early cephalopod evolution clarified through Bayesian phylogenetic inference". BMC Biology. 20 (1): 88. doi:10.1186/s12915-022-01284-5. PMC 9008929. PMID 35421982.
{{cite journal}}: CS1 maint: unflagged free DOI (link) - ^ Flower, Rousseau H. (1964). "The nautiloid order Ellesmeroceratida (Cephalopoda)" (PDF). New Mexico Bureau of Mines and Mineral Resources Memoir. 12: 1–164.
- ^ Mutvei, Harry; Zhang, Yun-Bai; Dunca, Elena (2007). "LATE CAMBRIAN PLECTRONOCERID NAUTILOIDS AND THEIR ROLE IN CEPHALOPOD EVOLUTION". Palaeontology. 50 (6): 1327–1333. doi:10.1111/j.1475-4983.2007.00708.x. ISSN 0031-0239.
- ^ Jun-yuan, Chen; Teichert, Curt (1983-11-01). "Cambrian cephalopods". Geology. 11 (11): 647–650. Bibcode:1983Geo....11..647J. doi:10.1130/0091-7613(1983)11<647:CC>2.0.CO;2. ISSN 0091-7613.
- Wade, M. 1988. Nautiloids and their descendants: cephalopod classification in 1986. Memoir 44, pp 15–25; New Mexico Bureau of Mines and Mineral Resources, Socorro, NM.