Foraminifera taxon details
Cuneolinella Cushman & Bermúdez, 1941 †
721332 (urn:lsid:marinespecies.org:taxname:721332)
accepted
Genus
Cuneolinella lewisi Cushman & Bermúdez, 1941 † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
feminine
Cushman, J. A.; Bermúdez, P. J. (1941). Cuneolinella, a new genus from the Miocene. <em>Contributions from the Cushman laboratory for foraminiferal research.</em> 17(4): 101-102., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/17cclfr4.pdf
page(s): p. 101 [details] Available for editors
[request]
page(s): p. 101 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Cuneolinella Cushman & Bermúdez, 1941 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721332 on 2024-04-26
Date
action
by
original description
Cushman, J. A.; Bermúdez, P. J. (1941). Cuneolinella, a new genus from the Miocene. <em>Contributions from the Cushman laboratory for foraminiferal research.</em> 17(4): 101-102., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/17cclfr4.pdf
page(s): p. 101 [details] Available for editors [request]
basis of record Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details] Available for editors [request]
page(s): p. 101 [details] Available for editors
[request] basis of record Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details] Available for editors
[request] From editor or global species database
Diagnosis Test large, flattened, with four to five trochospirally coiled chambers in the first whorl, then biserial with broad low and compressed chambers of nearly constant height, the flat sides being parallel to the plane of biseriality as in Cuneolina, chambers increasing rapidly in breadth on the flat sides so that test becomes flabelliform, the chambers finally strongly recurved at the margins and almost cyclic; wall agglutinated, interior with subepidermal mesh, exterior smoothly finished; aperture interiomarginal, a row of low slits at the base of the final chamber face. M. Miocene; Dominican Republic. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]