Foraminifera taxon details
Alveosepta Hottinger, 1967 †
739328 (urn:lsid:marinespecies.org:taxname:739328)
accepted
Genus
Cyclammina jaccardi Schrodt, 1894 † accepted as Pseudocyclammina jaccardi (Schrodt, 1894) † accepted as Alveosepta jaccardi (Schrodt, 1894) † (type by original designation)
- Species Alveosepta jaccardi (Schrodt, 1894) †
- Subgenus Alveosepta (Redmondellina) Banner & Whittaker, 1991 † accepted as Redmondellina Banner & Whittaker, 1991 † (Nomen translatum Opinion of Kaminski (2000))
- Species Alveosepta (Redmondellina) powersi (Redmond, 1964) † accepted as Redmondellina powersi (Redmond, 1964) † (unaccepted > superseded rank)
- Species Alveosepta powersi (Redmond, 1964) † accepted as Redmondellina powersi (Redmond, 1964) † (unaccepted > superseded combination)
marine, brackish, fresh, terrestrial
fossil only
feminine
Hottinger, L. (1967). Foraminifères imperforés du Mésozoique marocain. <em>Notes du Service Géologique du Maroc.</em> 209: 1-168.
page(s): p. 79, 84 [details] Available for editors [request]
page(s): p. 79, 84 [details] Available for editors [request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Alveosepta Hottinger, 1967 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739328 on 2024-05-05
Date
action
by
original description
Hottinger, L. (1967). Foraminifères imperforés du Mésozoique marocain. <em>Notes du Service Géologique du Maroc.</em> 209: 1-168.
page(s): p. 79, 84 [details] Available for editors [request]
page(s): p. 79, 84 [details] Available for editors [request]
From editor or global species database
Diagnosis Test coiled, microspheric early stage streptospiral, megalospheric test and microspheric adult planispiral, adult may tend to uncoil; wall agglutinated, exoskeleton with subepidermal network lining apertural face and septa as well as lateral and peripheral chamber walls, some species may have an exoskeletal projection that forms a median lamella, partially or completely bisecting the chambers; aperture consists of large openings at the base of the apertural face, supplementary areal foramina may be produced by resorption of the epidermal layer of the septum, allowing the alveoles to open into the adjacent chamber. U. Jurassic (Oxfordian to Kimmeridgian); Switzerland; France; Portugal; Morocco. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]