Biology:Plectronoceratoidea
| Plectronoceratoidea | |
|---|---|
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Mollusca |
| Class: | Cephalopoda |
| Subclass: | Nautiloidea |
| Superorder: | †Plectronoceratoidea Wade, 1988 |
| Orders | |
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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". GFF 142 (2): 115–124. doi:10.1080/11035897.2020.1739742. ISSN 1103-5897. https://www.diva-portal.org/smash/get/diva2:1515645/FULLTEXT01.pdf.
- ↑ 2.0 2.1 2.2 "High-level classification of the nautiloid cephalopods: a proposal for the revision of the Treatise Part K" (in en). Swiss Journal of Palaeontology 138 (1): 65–85. 2019. doi:10.1007/s13358-019-00186-4. ISSN 1664-2384.
- ↑ 3.0 3.1 "Early cephalopod evolution clarified through Bayesian phylogenetic inference". BMC Biology 20 (1): 88. April 2022. doi:10.1186/s12915-022-01284-5. PMID 35421982.
- ↑ Flower, Rousseau H. (1964). "The nautiloid order Ellesmeroceratida (Cephalopoda)". New Mexico Bureau of Mines and Mineral Resources Memoir 12: 1–164. https://geoinfo.nmt.edu/publications/monographs/memoirs/downloads/12/Memoir-12.pdf.
- ↑ Mutvei, Harry; Zhang, Yun-Bai; Dunca, Elena (2007). "Late Cambrian Plectronocerid Nautiloids and Their Role in Cephalopod Evolution" (in en). Palaeontology 50 (6): 1327–1333. doi:10.1111/j.1475-4983.2007.00708.x. ISSN 0031-0239. https://onlinelibrary.wiley.com/doi/10.1111/j.1475-4983.2007.00708.x.
- ↑ Jun-yuan, Chen; Teichert, Curt (1983-11-01). "Cambrian cephalopods". Geology 11 (11): 647–650. doi:10.1130/0091-7613(1983)11<647:CC>2.0.CO;2. ISSN 0091-7613. Bibcode: 1983Geo....11..647J. https://doi.org/10.1130/0091-7613(1983)112.0.CO;2.
- 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.
Wikidata ☰ Q7204415 entry
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