Knightoconus
Knightoconus antarcticus is an extinct species of fossil monoplacophoran from the Cambrian Minaret Formation of Antarctica. It is thought to represent an ancestor to the cephalopods. It had a chambered conical shell, but lacked a siphuncle.
| Knightoconus Temporal range: Dresbachian
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| Artistic reconstruction of Knightoconus antarcticus | |
Scientific classification 
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| Kingdom: | Animalia |
| Phylum: | Mollusca |
| Class: | Monoplacophora |
| Order: | †Kirengellida |
| Family: | †Hypseloconidae |
| Genus: | †Knightoconus Yochelson et al., 1973[2] |
| Species: | †K. antarcticus
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| Binomial name | |
| †Knightoconus antarcticus Yochelson et al., 1973[2]
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Knightoconus antarcticus is an extinct species of fossil monoplacophoran from the Cambrian Minaret Formation of Antarctica.[2] It is thought to represent an ancestor to the cephalopods. It had a chambered conical shell, but lacked a siphuncle.[3]
Taxonomic debate
[edit]The absence of a siphuncle in K. antarcticus has been taken as evidence against its being an ancestor of cephalopods, as factors that would allow a siphuncle to penetrate preexisting septal chambers remain unknown. The prevailing argument suggests that a strand of tissue remained attached to the previous septum as the mollusc moved forwards and deposited its next septum, stopping that new septum from closing completely and becoming mineralised itself.[4]
Ten or more septa are found in mature individuals, occupying around a third of the shell – septa form very early and have been found in specimens as small as 2 mm in length.[5] Unlike monoplacophoran fossils, there is no evidence of muscle scarring in Knightoconus fossils.[5] Scars from the closely related Hypseloconus have been used to determine its orientation.[6] Knightoconus started life with an exogastric shell that became endogastric as the organism grew.[7]
An alternate taxonomy is: Tergomya: Kiringellida: Hypseloconidae.[1]
See also
[edit]References
[edit]- ^ a b "†Knightoconus Yochelson et al. 1973". Paleobiology Database. Retrieved 1 July 2025.
- ^ a b c Yochelson, E.L.; Flower, R.H. & Webers, G.F. (1973). "The bearing of the new Late Cambrian monoplacophoran genus Knightoconus upon the origin of the Cephalopoda". Lethaia. 6 (3): 275–309. Bibcode:1973Letha...6..275Y. doi:10.1111/j.1502-3931.1973.tb01199.x.
- ^ Boyle (2005). "Chapter 3: Origin and Evolution". Cephalopods – ecology and fisheries. p. 36. doi:10.1002/9780470995310.ch3. ISBN 9780632060481.
- ^ Holland, C.H. (1987) [1986]. "The nautiloid cephalopods: A strange success". Journal of the Geological Society. President's anniversary address. 144 (1): 1–15. Bibcode:1987JGSoc.144....1H. doi:10.1144/gsjgs.144.1.0001. S2CID 128629737.
- ^ a b Webers, G.F. & Yochelson, E.L. (1989). "Late Cambrian molluscan faunas and the origin of the Cephalopoda". In Crame, J.A. (ed.). Origins and Evolution of the Antarctic Biota. Special Publications. Vol. 47. London, UK: Geological Society. p. 29. doi:10.1144/GSL.SP.1989.047.01.04. S2CID 128682549.
- ^ Peel, J. S. (1991). "Functional Morphology of the Class Helcionelloida Nov., and the Early Evolution of the Mollusca". In Simonetta, A. M.; Conway Morris, S (eds.). The Early Evolution of Metazoa and the Significance of Problematic Taxa. Cambridge University Press. pp. 157–177. ISBN 978-0-521-40242-2.
- ^ Webers, G.F.; Pojeta, J. Jr. & Yochelson, E.L. (1992). "Cambrian Mollusca from the Minaret Formation, Ellsworth Mountains, West Antarctica". Geology and Paleontology of the Ellsworth Mountains, West Antarctica. Geological Society of America. pp. 181–248. ISBN 978-0-8137-1170-6.