Foraminifera taxon details
Delosinidae Parr, 1950
- Genus Delosina Wiesner, 1931
- Genus Neodelosina McCulloch, 1977
- Genus Delosinoides McCulloch, 1977 accepted as Neodelosina McCulloch, 1977 (Opinion of Loeblich & Tappan, 1987)
marine, fresh, terrestrial
Parr, W. J. (1950). Foraminifera. <em>B.A.N.Z. Antarctic Research Expedition 1929-1931. Report.</em> Series B 5 (6): 232-392. [details] Available for editors
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Type locality contained in Antarctic Ocean
type locality contained in Antarctic Ocean [details]
Diagnosis Test triserial, high spired; primary apertural opening may be lacking and secondary sutural pores with bordering lip may be...
Diagnosis Test triserial, high spired; primary apertural opening may be lacking and secondary sutural pores with bordering lip may be present, the large sutural pores opening into subsutural canals that terminate in a spongy area of the final chamber face. Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Delosinidae Parr, 1950. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=526305 on 2025-05-07
Date
action
by
original description
Parr, W. J. (1950). Foraminifera. <em>B.A.N.Z. Antarctic Research Expedition 1929-1931. Report.</em> Series B 5 (6): 232-392. [details] Available for editors
[request]
additional source 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 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





From editor or global species database
Diagnosis Test triserial, high spired; primary apertural opening may be lacking and secondary sutural pores with bordering lip may be present, the large sutural pores opening into subsutural canals that terminate in a spongy area of the final chamber face. Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]