MolluscaBase name details

Vivipara concinna J. Sowerby, 1813 †

1263096  (urn:lsid:marinespecies.org:taxname:1263096)

 unaccepted > superseded combination (genus is an incorrect subsequent spelling)
Species
marine, brackish, fresh, terrestrial
fossil only
Sowerby, J. (1812-1815). The mineral conchology of Great Britain; or coloured figures and descriptions of those remains of testaceous animals or shells, which have been preserved at various times and depths in the earth [Vol. I]. London, privately published, pp. i-vii, 9-234 + index [2 pp.], pl. 1-102., available online at http://www.biodiversitylibrary.org/bibliography/14408
page(s): 80, pl. 31, figs 4-5 [details] 
Type locality contained in Great Britain  
type locality contained in Great Britain [details]
Note New Milton (Barton on Sea) ("Barton Cliff"),...  
Type locality New Milton (Barton on Sea) ("Barton Cliff"), Hampshire, United Kingdom; Barton Group, late Lutetian to Bartonian, middle to late Eocene [details]
MolluscaBase eds. (2021). MolluscaBase. Vivipara concinna J. Sowerby, 1813 †. Accessed at: http://www.molluscabase.org/aphia.php?p=taxdetails&id=1263096 on 2025-09-11
Date
action
by
2018-07-02 12:43:57Z
created
2018-07-09 20:58:41Z
changed
2022-11-21 12:29:08Z
changed

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


original description Sowerby, J. (1812-1815). The mineral conchology of Great Britain; or coloured figures and descriptions of those remains of testaceous animals or shells, which have been preserved at various times and depths in the earth [Vol. I]. London, privately published, pp. i-vii, 9-234 + index [2 pp.], pl. 1-102., available online at http://www.biodiversitylibrary.org/bibliography/14408
page(s): 80, pl. 31, figs 4-5 [details] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

From editor or global species database
Type locality New Milton (Barton on Sea) ("Barton Cliff"), Hampshire, United Kingdom; Barton Group, late Lutetian to Bartonian, middle to late Eocene [details]
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