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Traits name detailsEocallista (Hemicorbicula) parva (J. De C. Sowerby, 1836) †
1556586 (urn:lsid:marinespecies.org:taxname:1556586)
alternative representation
Species
marine,
fossil only
(of ) Sowerby, James de Carle. (1836). Descriptive notes respecting the shells figured in Plates XI to XXIII. In: Fitton, W.H. Observations on some of the strata between the Chalk and the Oxford Oolite, in the South-east of England. <em>Transactions of the Geological Society of London, ser. 2.</em> 4(2): 335-349 (Appendix A)., available online at https://www.biodiversitylibrary.org/page/36206436
page(s): 345, pl. 21, fig. 7 [details]
MolluscaBase eds. (2025). MolluscaBase. Eocallista (Hemicorbicula) parva (J. De C. Sowerby, 1836) †. Accessed through: Marine Species Traits editorial board (2025) Marine Species Traits at: https://www.marinespecies.org/traits/aphia.php?p=taxdetails&id=1556586 on 2025-05-10
Marine Species Traits editorial board (2025). Marine Species Traits. Eocallista (Hemicorbicula) parva (J. De C. Sowerby, 1836) †. Accessed at: https://www.marinespecies.org/traits/aphia.php?p=taxdetails&id=1556586 on 2025-05-10
Date action by
original description
(of ) Sowerby, James de Carle. (1836). Descriptive notes respecting the shells figured in Plates XI to XXIII. In: Fitton, W.H. Observations on some of the strata between the Chalk and the Oxford Oolite, in the South-east of England. <em>Transactions of the Geological Society of London, ser. 2.</em> 4(2): 335-349 (Appendix A)., available online at https://www.biodiversitylibrary.org/page/36206436
page(s): 345, pl. 21, fig. 7 [details] basis of record Huckriede, R. (1967). Molluskenfaunen mit limnischen und brackischen Elementen aus Jura, Serpulit und Wealden NW-Deutschlands und ihre paläogeographische Bedeutung. <em>Geologisches Jahrbuch, Beiheft.</em> 67: 1-263. page(s): 97 [details] Available for editors  additional source Morter, A. A. (1984). Purbeck-Wealden Beds Mollusca and their relationship to ostracod biostratigraphy, stratigraphical correlation and palaeoecology in the Weald and adjacent areas. <em>Proceedings of the Geologists' Association.</em> 95(3): 217-234. [details] Available for editors |