Theodoxus velox V. Anistratenko in O. Anistratenko et al., 1999
publication ID |
https://dx.doi.org/10.3897/zse.96.48312 |
publication LSID |
lsid:zoobank.org:pub:F2C8585A-1268-4436-9334-8B64AE20F6EE |
persistent identifier |
https://treatment.plazi.org/id/CFE8F3CD-A150-576C-94E3-DB2C5E9C9034 |
treatment provided by |
|
scientific name |
Theodoxus velox V. Anistratenko in O. Anistratenko et al., 1999 |
status |
|
Theodoxus velox V. Anistratenko in O. Anistratenko et al., 1999 Figure 22A-M View Figure 22
Theodoxus velox V. Anistratenko in O. Anistratenko et al. 1999: 17-18, fig. 4.7; Wesselingh et al. 2019: 66.
Type locality.
Dnieper Delta, Zburievkiy Liman, Kherson Region, Ukraine.
Type material.
Holotype and five paratypes are stored in IZAN (without coll. no.) .
Remarks.
This species was recently discussed by Wesselingh et al. (2019). While it was previously considered a junior synonym of T. fluviatilis ( Vinarski and Kantor 2016), molecular data shows strong monophyletic support for the independence of T. velox ( Sands et al. 2019a; Fig. 2 View Figure 2 ). Nevertheless, T. velox and T. fluviatilis still hold a sister relationship and likely diverged from one another during the early Pleistocene ( Sands et al. 2019a; Fig. 2 View Figure 2 ). Theodoxus velox is challenging to distinguish from T. fluviatilis given the overlap in geographic range and similarity of conchological features (Figs 3 View Figure 3 , 9 View Figure 9 , 10 View Figure 10 , 22 View Figure 22 ). Theodoxus velox has less phenotypic variability compared to T. fluviatilis (Figs 9 View Figure 9 , 10 View Figure 10 , 22 View Figure 22 ). Moreover, T. velox display more expansive spiral whorls and, in some instances, a more transparent operculum where the conchioline lamella extends deeper into the calcareous base and the callus is less pronounced (Figs 9 View Figure 9 , 10 View Figure 10 , 22 View Figure 22 ).
The geographic distribution range of T. velox overlaps with that of T. sarmaticus (Lindholm, 1901), which has been considered a junior synonym of T. fluviatilis (e.g. Vinarski and Kantor 2016). While T. sarmaticus and T. fluviatilis may on occasion share phenotypic similarity, the morphotypes of T. sarmaticus closely resemble T. velox (Fig. 22A-M View Figure 22 versus Fig. 22N-U View Figure 22 ). The similarity with T. velox could suggest T. sarmaticus is rather conspecific with that species as suggested by Glöer (2019). Unfortunately, no opercula or soft tissues were preserved among the syntypes of T. sarmaticus to corroborate this hypothesis. Molecular analyses of topotypic material is required to address this uncertainty. However, should this be confirmed at a later point, the name T. sarmaticus would have priority.
Distribution.
This species was indicated to be restricted to drainage systems of the northern Black Sea coast ( Anistratenko et al. 1999; Kantor and Sysoev 2006). Recent molecular data suggest it is distributed as far North as the eastern part of the Baltic Sea and as far South as Anatolia ( Sands et al. 2019a): the only record there derives from Lake Sapanca ( Sands et al. 2019a; Fig. 3C View Figure 3 ).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
Kingdom |
|
Phylum |
|
Class |
|
Order |
|
Family |
|
Genus |