Foraminifera taxon details
Scandonea De Castro, 1971 †
722035 (urn:lsid:marinespecies.org:taxname:722035)
accepted
Genus
Scandonea samnitica De Castro, 1971 † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
feminine
De Castro, P. (1971). Osservazioni su Raadshoovenia Van Den Bold e i suoi rapporti col nuovo genere Scandonea. <em>Bollettino della Società dei Naturalisti in Napoli.</em> 80: 161-236., available online at https://www.biodiversitylibrary.org/page/56477718
page(s): p. 163, 174 [details]
page(s): p. 163, 174 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Scandonea De Castro, 1971 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722035 on 2024-04-23
Date
action
by
original description
De Castro, P. (1971). Osservazioni su Raadshoovenia Van Den Bold e i suoi rapporti col nuovo genere Scandonea. <em>Bollettino della Società dei Naturalisti in Napoli.</em> 80: 161-236., available online at https://www.biodiversitylibrary.org/page/56477718
page(s): p. 163, 174 [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]
page(s): p. 163, 174 [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] From editor or global species database
Diagnosis Test enrolled, early stage with coiling in various planes, later planispiral and involute, increasing from about four chambers per whorl up to eight to ten in the final whorl, final stage may be uncoiled and rectilinear, with four to five subpyriform chambers of circular cross section, chamber interior subdivided by very short radial vertical partitions that may be thickened at the inner end; wall calcareous, imperforate, porcelaneous, outer wall very thick, that of septa thin; aperture multiple, cribrate. U. Cretaceous (Campanian) to L. Paleocene (Montian); Italy; Yugoslavia; Turkey. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]