MolluscaBase name details

Cleopatra bifidicincta L. R. Cox, 1926 †

1066607  (urn:lsid:marinespecies.org:taxname:1066607)

 unaccepted > superseded combination
Species
marine, brackish, fresh, terrestrial
fossil only
Cox, L.R. (1926). Fossil Mollusca. In: Wayland, E.J. (Ed.) The Geology and Palaeontology of the Kaiso Bone-beds. <em>Geological Survey of Uganda Occasional Paper.</em> 2: 53-71.
page(s): 65-67, pl. 8, figs 12-14 [details] 
Note The type material was collected by J. Coates...  
Type locality The type material was collected by J. Coates in 1909 and described by Cox (1926) who gives ’Kazinga’ as the type locality and states in his introduction: ‘the probable locality of the Kazinga specimens is the bank of the Kazinga Channel, on the S. side, near Kazinga itself’. But the original reference on the label of Coates’ specimens is ’north-east of Lake Edward’. Since P. bifidicincta was never found in the Kazinga area during the detailed investigations by subsequent expeditions it is most likely that the real type locality is Bushabwanyama (Lake Edward, Uganda), ca 8 km south of Kazinga (Fig. 13), where P. bifidicincta is abundant. [details]
MolluscaBase eds. (2021). MolluscaBase. Cleopatra bifidicincta. Accessed at: http://www.marinespecies.org/aphia.php?p=taxdetails&id=1066607 on 2025-09-11
Date
action
by
2018-03-08 12:11:07Z
created
2022-08-30 07:32:28Z
changed
2022-12-14 11:04:40Z
changed

Creative Commons License The webpage text is licensed under a Creative Commons Attribution 4.0 License


original description Cox, L.R. (1926). Fossil Mollusca. In: Wayland, E.J. (Ed.) The Geology and Palaeontology of the Kaiso Bone-beds. <em>Geological Survey of Uganda Occasional Paper.</em> 2: 53-71.
page(s): 65-67, pl. 8, figs 12-14 [details] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

From editor or global species database
Type locality The type material was collected by J. Coates in 1909 and described by Cox (1926) who gives ’Kazinga’ as the type locality and states in his introduction: ‘the probable locality of the Kazinga specimens is the bank of the Kazinga Channel, on the S. side, near Kazinga itself’. But the original reference on the label of Coates’ specimens is ’north-east of Lake Edward’. Since P. bifidicincta was never found in the Kazinga area during the detailed investigations by subsequent expeditions it is most likely that the real type locality is Bushabwanyama (Lake Edward, Uganda), ca 8 km south of Kazinga (Fig. 13), where P. bifidicincta is abundant. [details]
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