Asaphiscus
Asaphiscus Temporal range: Middle Cambrian
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Asaphiscus wheeleri, Cambrian shale,Utah | |
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Genus: | Asaphiscus Meek, 1873
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Asaphiscus is a genus of trilobite that lived in the Cambrian. Its remains have been found in Australia and North America, especially in Utah.
Distribution
- A. wheeleri occurs in the Middle Cambrian of the United States (Delamaran, Lower Wheeler Shale, Millard County, Utah, 40.0°N, 113.0°W;[1] and Menevian, Wheeler Formation, House Range, Utah, 39.2° N, 113.3° W).[2]
Description
Asaphiscus are average size trilobites of (upto 8 centimetres or 3.1 inches) with a rather flat calcified dorsal exoskeleton of inverted egg-shaped outline, about 1½× longer than wide, with the widest point near the back of the headshield (or cephalon. The articulated middle part of the body (or thorax) has 9 segments (in A. wheeleri). The tailshield (or pygidium) has a wide flat border.
Reassigned species
Some species originally described as belonging to Asaphiscus have later been reassigned to other genera.[3]
- A. capella = Glyphaspis capella
- A. granulatus = Genevievella granulata
- A. gregarius = Blainia gregarius
- A. minor = Cedaria minor
- A. unispinus = Weeksina unispina
Sources
- A Pictorial Guide to Fossils by Gerard Ramon Case
References
- ^ Conway Morris, S.; Robison, R.A. (1986). "Middle Cambrian priapulids and other soft-bodied fossils from Utah and Spain". University of Kansas Paleontological Contributions. 117: 1–22. cited on Paul Hearn. "Lower Wheeler Shale". Fossilworks. Retrieved 2015-01-16.
- ^ Robison, R.A. (1971). "Additional Middle Cambrian trilobites from the Wheeler Shale of Utah". Journal of Paleontology. 45 (5): 796–804. cited on Shenan Peeters. "Wheeler Formation, House Range, Utah". Fossilworks. Retrieved 2015-01-16.
- ^ Peters, S.E. "2. Paleontology and taphonomy of the Upper Weeks Formation (Cambrian, Upper Marjuman, Cedaria Zone) of western Utah". http://www.geology.wisc.edu/~peters/pdfs/Weeks.pdf.
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External links
- Asaphiscus in the Paleobiology Database