Foraminifera taxon details
Angotia Cuvillier, 1963 †
722406 (urn:lsid:marinespecies.org:taxname:722406)
accepted
Genus
Angotia aquitanica Cuvillier, 1963 † (type by monotypy)
marine, brackish, fresh, terrestrial
fossil only
feminine
Cuvillier, J. (1963). Angotia aquitanica, foraminifère nouveau du Lutétien d'Aquitaine. <em>Revue de Micropaléontologie.</em> 5: 223-225.
page(s): p. 223 [details]
page(s): p. 223 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Angotia Cuvillier, 1963 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722406 on 2024-04-25
Date
action
by
original description
Cuvillier, J. (1963). Angotia aquitanica, foraminifère nouveau du Lutétien d'Aquitaine. <em>Revue de Micropaléontologie.</em> 5: 223-225.
page(s): p. 223 [details]
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]
additional source Schroeder, R. (1964). Bemerkungen zur Foraminiferen-Gattung Angotia Cuvillier 1963. <em>Neues Jahrbuch für Geologie und Paläontologie, Monatshefte.</em> (4): 193-196.
note: Possible synonym of Fabiana. [details] Available for editors [request]
page(s): p. 223 [details]
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] additional source Schroeder, R. (1964). Bemerkungen zur Foraminiferen-Gattung Angotia Cuvillier 1963. <em>Neues Jahrbuch für Geologie und Paläontologie, Monatshefte.</em> (4): 193-196.
note: Possible synonym of Fabiana. [details] Available for editors
[request] From editor or global species database
Diagnosis Test attached, conical, large thick-walled bilocular embryo followed by a series of low flat chambers forming a low to high cone with flattened base, lamellae at the base of the test may be infolded and touch the previous wall, forming what appear to be hollow pillars, similar and regularly spaced undulations or infolding of the wall in the peripheral zone produces tunnels perpendicular to the outer margin, with alternating longer and shorter radial infoldings, the longer ones commonly terminating at one of the hollow pillars; wall calcareous, finely perforate, thickened by lamellar additions, surface smooth except where abraded; aperture consists of multiple rounded pores formed by the hollow pillars in the flattened base. M. Eocene (U. Lutetian); France. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]