Cambrorhytium
Cambrorhytium Temporal range: Chengjiang–Burgess Shale | |
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Scientific classification | |
Kingdom: | Animalia |
Phylum: | Cnidaria |
Class: | Scyphozoa |
Clade: | †Conulariida |
Genus: | Cambrorhytium (Walcott 1908) Conway Morris and Robison, 1988[1] |
Species | |
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Cambrorhytium is an enigmatic fossil genus known from the Latham shale (California),[2] and the Chengjiang (China) and Burgess Shale (Canadian rockies) lagerstätte[3] 350 specimens of Cambrorhytium are known from the Greater Phyllopod bed, where they comprise 0.7% of the community.[4]
The fossil is conical, with iterated linear markings on its walls, parallel to its base. Its wall is thin, and it lacks the keel that is distinctive of hyoliths.[2]
It has been interpreted as a cnidarian polyp, with the interpretation suggesting that the animal lived in the tube and extended tentacles (of which no trace has been found) from the flat aperture.[5] The other possible, but probably unlikely, affinity is with the hyolith molluscs.[2]
Its name is from the Latin rhytium, drinking horn.[1]
C. elongatum has been described to contain an alimentary canal in a single Chinese specimen.[6]
C. major was originally described as a member of the hyolith genus Orthotheca.[7]
C. fragilis was originally included by Charles D. Walcott in the genus Selkirkia,[8][9] – a taxonomy that was retained by later workers[10][11] until finally questioned[12] and redescribed[1] as Cambrorhytium in the eighties.
Its similarity with the lower cambrian species Torellelloides giganteum may indicate a close relationship.[1]
See also
Cambrorhytium has been compared to the fossil Archotuba[5] and Sphenothallus[13]
References
- 1 2 3 4 Conway Morris, Simon; Robison, R.A. (1988). "More soft-bodied animals and algae from the Middle Cambrian of Utah and British Columbia." (PDF). University of Kansas Paleontological Contributions 122: 1–48.
- 1 2 3 Waggoner, Ben; Hagadorn, James W. (2005). "Conical fossils from the Lower Cambrian of Eastern California". Paleobios 25 (1).
- ↑ Zhang, X. L.; Hua, H. (2005). "Soft-bodied fossils from the Shipai Formation, Lower Cambrian of the Three Gorge area, South China". Geological Magazine 142 (6): 699. doi:10.1017/S0016756805000518.
- ↑ Caron, Jean-Bernard; Jackson, Donald A. (October 2006). "Taphonomy of the Greater Phyllopod Bed community, Burgess Shale". PALAIOS 21 (5): 451–65. doi:10.2110/palo.2003.P05-070R. JSTOR 20173022.
- 1 2 Han, J.; Zhang, Z.; Liu, J.; Shu, D. (2007). "EVIDENCE OF PRIAPULID SCAVENGING FROM THE EARLY CAMBRIAN CHENGJIANG DEPOSITS, SOUTHERN CHINA". PALAIOS (Society for Sedimentary Geology) 22 (6): 691–694. doi:10.2110/palo.2006.p06-117r. ISSN 0883-1351.
- ↑ Steiner, M.; Zhu, M.; Zhao, Y.; Erdtmann, B. (2005). "Lower Cambrian Burgess Shale-type fossil associations of South China". Palaeogeography, Palaeoclimatology, Palaeoecology 220: 129. doi:10.1016/j.palaeo.2003.06.001.
- ↑ Walcott, C. D. (1908). "Mount Stephen rocks and fossils". Canadian Alpine Journal 1: 232–248.
- ↑ Walcott, C.D. (1911). "Cambrian Geology and Paleontology II, no. 5. Middle Cambrian annelids". Smithsonian Miscellaneous Collections 57: 109–144.
- ↑ Walcott, C.D. (1912). "Cambrian of the Kicking Horse Valley, B.C.". Geological Survey of Canada Report 26: 188.
- ↑ Howell, B. F.; Stubblefield, C. J. (2009). "A Revision of the Fauna of the North Welsh Conocoryphe viola Beds implying a Lower Cambrian Age". Geological Magazine 87: 1. doi:10.1017/S0016756800075506.
- ↑ Conway Morris, S (1977). "Fossil priapulid worms". Special Papers in Palaeontology 20 (4): 1–95.
- ↑ Briggs, D.E.G.; S. Conway Morris (1986). Hoffman, A., M.H.; Nitecki, eds. "Problematic Fossil Taxa". New York: Oxford University Press.
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ignored (help) - ↑ Van Iten, H.; Zhu, M. Y.; Collins, D. (2002). "First Report of Sphenothallus Hall, 1847 in the Middle Cambrian". Journal of Paleontology 76 (5): 902–905. doi:10.1666/0022-3360(2002)076<0902:FROSHI>2.0.CO;2. ISSN 0022-3360. JSTOR 1307202.
External links
- "Cambrorhytium major". Burgess Shale Fossil Gallery. Virtual Museum of Canada. 2011.