MolluscaBase name details
Neritina uniplicata J. De C. Sowerby, 1823 †
1052953 (urn:lsid:marinespecies.org:taxname:1052953)
unaccepted (original combination)
Species
brackish
fossil only
Sowerby, J.; Sowerby, J. De C. (1821-1823). 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. IV. Privately published by author, London, pp. 1-160, pls. 307-407., available online at https://www.biodiversitylibrary.org/page/14392771
page(s): 118, pl. 385, figs 9-10 [details]
page(s): 118, pl. 385, figs 9-10 [details]
Type locality contained in Great Britain
, Note "Between Charlton and Woolwich, [...] also...
type locality contained in Great Britain [details]
Type locality "Between Charlton and Woolwich, [...] also [...] at Plumstead, and near New Cross, on the banks of the Canal above the London Clay", London, United Kingdom; Lambeth Group/Woolwich/Blackheath Formation, late Thanetian to early Ypresian, late Paleocene to early Eocene [details]
MolluscaBase eds. (2021). MolluscaBase. Neritina uniplicata J. de C. Sowerby, 1823 †. Accessed at: https://www.molluscabase.org/aphia.php?p=taxdetails&id=1052953 on 2025-09-10
Date
action
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original description
Sowerby, J.; Sowerby, J. De C. (1821-1823). 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. IV. Privately published by author, London, pp. 1-160, pls. 307-407., available online at https://www.biodiversitylibrary.org/page/14392771
page(s): 118, pl. 385, figs 9-10 [details]
page(s): 118, pl. 385, figs 9-10 [details]




From editor or global species database
Type locality "Between Charlton and Woolwich, [...] also [...] at Plumstead, and near New Cross, on the banks of the Canal above the London Clay", London, United Kingdom; Lambeth Group/Woolwich/Blackheath Formation, late Thanetian to early Ypresian, late Paleocene to early Eocene [details]