Scenella Temporal range: | |
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Dorsal view of the shell of Scenella tenuistriata | |
lateral view of the shell of Scenella tenuistriata | |
Scientific classification | |
Kingdom: | |
Phylum: | |
Superfamily: | |
Family: | † Scenellidae S. A. Miller, 1889 [2] |
Genus: | Scenella Billings, 1872 |
Synonyms [3] | |
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Scenella is an extinct genus of fossil invertebrate animal which is generally considered to be a mollusc; at various times it has been suggested that this genus belongs with the gastropods, the monoplacophorans, or the helcionellids, although no firm association with any of these classes has been established. [4] An affinity with the hydrozoa (as a flotation device) has been considered, [1] although some authors oppose this hypothesis. [5] A gastropod affinity is defended on the basis of six pairs of internal muscle scars, [6] whilst the serially-repeated nature of these scars suggests to other authors a monoplacophoran affinity. [1] However the specimens showing this scarring have not been convincingly shown to belong to the genus Scenella. [1] A similarity to the Ediacaran Ovatoscutum has also been drawn. [7]
The shell of Scenella is elongated along its anterior-posterior axis, and comprises concentric rings around a conical central peak. Radial and concentric corrugations exist in some species. [7] Some specimens are preserved as organic films, others appear to have been infilled with calcite. [1] They are usually preserved point-upwards, with their long axes consistently oriented; this probably represents their most stable position under their depositional current. [1] Soft parts have never been reported in association with Scenella, suggesting that the preserved fragments separated quickly from the associated tissue prior to burial. [1]
Scenella lived from the Cambrian to the Ordovician. Its remains have been found in Antarctica, Asia, Europe, and North America. Individual fossils are common throughout the Burgess shale, where they often occur in dense aggregations. [1] Where they overlap, specimens deform as by draping. [1] Specimens are sometimes cracked or torn, with margins often damaged by folding or "tattering". [1] 1206 specimens of Scenella are known from the Greater Phyllopod bed, where they comprise 2.29% of the community. [8]
Scenella is the only genus in the family Scenellidae. This family has no subfamilies and Scenella is the type genus of the family Scenellidae.
The taxonomy of the Gastropoda by Bouchet & Rocroi, 2005 [3] categorizes Scenellidae in the superfamilia Scenelloidea within the Paleozoic molluscs of uncertain systematic position.
Species in the genus Scenella include: [9]
Species | Authority | Range |
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Scenella affinis | Ulrich and Schfield, 1897 | |
Scenella amii | (Matthew, 1902) Babcock and Robinson 1988 | Burgess Shale (Mid Cambrian, 508 million years ago) [8] |
Scenella anomala | (Billings, 1865) Wagner 2008 | |
Scenella augusta | (Billings, 1865) Wagner 2008 | |
Scenella barrandei | (Linnarsson, 1879) (Bergerg-Madsen and Peel, 1986) [10] | |
Scenella beloitensis | Ulrich and Scofield (1897) | |
Scenella clotho | Walcott, 1936 | |
Scenella compressa | Ulrich and Scofield (1897) | |
Scenella conica | Whiteaves, 1884 | |
Scenella conula | (Walcott, 1884) | |
Scenella conicum | (Whitfield, 1886) Ulrich and Scofield (1897) | |
Scenella hujingtanensis | Yu, 1979 | |
Scenella magnifica | Ulrich and Scofield (1897) | |
S.? mira | Vasil’yeva, 1994 | |
Scenella montrealensis | Billings (1865) | |
Scenella obtusa | (Sardeson, 1892) Ulrich and Scofield (1897) | |
Scenella orithyia | (Billings, 1865) Ulrich and Scofield (1897) | |
Scenella pretensa | Raymond, 1905 | |
Scenella radialis | Ulrich and Scofield (1897) | |
Scenella radians | Babcock & Robinson | |
Scenella radiata | Yu, 1979 | |
Scenella reticulata | (Billings, 1872) (type) [11] | |
Scenella retusa | (Ford, 1873) [12] | |
Scenella unicarinata | (Kobayashi, 1934) Wagner 2008 | |
Scenella varians | Walcott 1908 | |
Scenella venillia | (Billings, 1865) Wagner 2008 | |
Scenella tenuistriata | Chapman, 1911 | Mid Cambrian [13] |
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Marrella is an extinct genus of marrellomorph arthropod known from the Middle Cambrian of North America and Asia. It is the most common animal represented in the Burgess Shale of British Columbia, Canada, with tens of thousands of specimens collected. Much rarer remains are also known from deposits in China.
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Elrathia is a genus of trilobite belonging to Ptychopariacea known from the mid-Cambrian of Laurentia. E. kingii is one of the most common trilobite fossils in the USA locally found in extremely high concentrations within the Wheeler Formation in the U.S. state of Utah. E. kingii has been considered the most recognizable trilobite. Commercial quarries extract E. kingii in prolific numbers, with just one commercial collector estimating 1.5 million specimens extracted in a 20-year career. 1950 specimens of Elrathia are known from the Greater Phyllopod bed, where they comprise 3.7% of the community.
"...trilobite occupied the exaerobic zone, at the boundary of anoxic and dysoxic bottom waters. E. kingii consistently occur in settings below the oxygen levels required by other contemporaneous epifaunal and infaunal benthic biota and may have derived energy from a food web that existed independently of phototrophic primary productivity. Although other fossil organisms are known to have preferred such environments, E. kingii is the earliest-known inhabitant of them, extending the documented range of the exaerobic ecological strategy into the Cambrian Period."
Helmetia is an extinct genus of arthropod from the middle Cambrian. Its fossils have been found in the Burgess Shale of Canada and the Jince Formation of the Czech Republic.
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