Foraminifera taxon details
Geinitzinidae Bozorgnia, 1973 †
720903 (urn:lsid:marinespecies.org:taxname:720903)
accepted
Family
- Genus Frondinodosaria Sellier de Civrieux & Dessauvagie, 1965 †
- Genus Geinitzina Spandel, 1901 †
- Genus Howchinella Palmieri, 1985 †
- Genus Lunucammina Spandel, 1898 †
- Genus Omoloniella Karavaeva & Nestell, 2007 †
- Genus Praerectoglandulina Vachard in Krainer, Vachard & Schaffhauser, 2019 †
- Genus Reitlingeria Pronina in Kotlyar et al., 1989 †
- Genus Sellierina Korchagin, 2011 †
- Genus Spandelinoides Cushman & Waters, 1928 †
- Genus Geinitzella Spandel, 1898 † accepted as Geinitzina Spandel, 1901 † (Junior homonym of Geinitzella Waagen & Wentzil, 1866)
- Genus Neogeinitzina Miklukho-Maklay, 1954 † accepted as Lunucammina Spandel, 1898 † (subjective junior synonym in opinion of Loeblich & Tappan, 1987)
- Genus Spandelina Cushman & Waters, 1928 † accepted as Lunucammina Spandel, 1898 † (subjective junior synonym in opinion of Loeblich & Tappan, 1987)
marine, fresh, terrestrial
fossil only
Bozorgnia, F. (1973). Paleozoic foraminiferal biostratigraphy of central and east Alborz Mountains, Iran. <em>National Iranian Oil Company, Geological Laboratories, Publication.</em> 4: 1-185., available online at https://archive.org/details/Bozorgnia1973Searchable [details] Available for editors
[request]
Description Colanielloidea with different sagittal axial and frontal axial sections. Sagittal axial sections exhibiting geinitzinoid...
Diagnosis Test uniserial, early species rounded in section, later ones compressed, ovate to triradiate in section; wall with thicker...
Description Colanielloidea with different sagittal axial and frontal axial sections. Sagittal axial sections exhibiting geinitzinoid chambers; i.e., low, medially arched, and non-enveloping. Frontal axial sections are nodosarioid in shape. Aperture terminal, simple. Latest Pennsylvanian to Triassic.
Vachard and Le Coze (2024). [details]
Vachard and Le Coze (2024). [details]
Diagnosis Test uniserial, early species rounded in section, later ones compressed, ovate to triradiate in section; wall with thicker...
Diagnosis Test uniserial, early species rounded in section, later ones compressed, ovate to triradiate in section; wall with thicker light-colored hyaline radiate layer and thin dark granular inner layer; aperture terminal, rounded to ovate. U. Devonian (Frasnian) to U. Permian. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Geinitzinidae Bozorgnia, 1973 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=720903 on 2026-06-12
Date
action
by
original description
Bozorgnia, F. (1973). Paleozoic foraminiferal biostratigraphy of central and east Alborz Mountains, Iran. <em>National Iranian Oil Company, Geological Laboratories, Publication.</em> 4: 1-185., available online at https://archive.org/details/Bozorgnia1973Searchable [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]
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
From editor or global species database
Description Colanielloidea with different sagittal axial and frontal axial sections. Sagittal axial sections exhibiting geinitzinoid chambers; i.e., low, medially arched, and non-enveloping. Frontal axial sections are nodosarioid in shape. Aperture terminal, simple. Latest Pennsylvanian to Triassic.Vachard and Le Coze (2024). [details]
Diagnosis Test uniserial, early species rounded in section, later ones compressed, ovate to triradiate in section; wall with thicker light-colored hyaline radiate layer and thin dark granular inner layer; aperture terminal, rounded to ovate. U. Devonian (Frasnian) to U. Permian. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]