Anisus cf. spirorbis (Linnaeus, 1758)
publication ID |
https://doi.org/ 10.26879/936 |
persistent identifier |
https://treatment.plazi.org/id/03B287EF-FFF5-3205-DAD4-FC5A46DB819B |
treatment provided by |
Felipe |
scientific name |
Anisus cf. spirorbis (Linnaeus, 1758) |
status |
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Anisus cf. spirorbis (Linnaeus, 1758) View in CoL
Figure 8.3 View FIGURE 8
1758 Helix spirorbis, Linnaeus , p. 770.
1885 Planorbis spirorbis (Linnaeus) ; Westerlund, p. 73.
1952 Anisus spirorbis (Linnaeus) ; Zhadin, p.
185, fig. 90.
1955 Paraspira spirorbis (Linnaeus) ; Danilovskiy, p. 105, pl. 10, figs. 286-288.
1960 Paraspira spirorbis (Linnaeus) ; Kirillina, p.
151, pl. 8, figs. 97-98.
1964 Anisus spirorbis (Linnaeus) ; Ložek, p. 183, fig. 33.
1977 Anisus spirorbis (Linnaeus) ; Starobogatov, p. 170, fig. 405.
1998 Anisus spirorbis : Gittenberger, Janssen, Kuijper, Kuiper, Meijer, Velde and Vries, p.
147, figs. 297-299.
2002 Anisus (Anisus) spirorbis (Linnaeus) ; Glöer, p. 256, add. 278.
2007 Anisus spirorbis (Linnaeus) ; Sanko, p. 110, fig. 88.
Material. 3 specimens from layer 3.
Description. Planispiral shell (HS is 0.8 mm; WS
is 2.4 mm; WS/HS is 3), dented evenly from the upper and lower sides. There are 5-6 rounded whorls, slowly growing, convex, covered with longitudinal hatching. Suture is deep. The last whorl is
1.5 times wider than the penultimate one. Shell is flattened at the bottom, and a keel is observed along the periphery of the lower edge. Aperture is rounded, with a lip inside. The upper edge of aperture is extended forward.
Remarks. Preservation of shells is in a form of internal casts suggesting redeposition.
Region of distribution and age. Pleistocene – Present. European part of Russia, Asia, Europe (Glöer, 2002). Late Miocene of the the northeastern Azov Sea region.
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