Foraminifera name details

Iranella Leven, 2004 †

1062412 (urn:lsid:marinespecies.org:taxname:1062412)

 unaccepted > junior homonym (Invalid: Junior homonym (see note))
Genus
Iranella bella Leven, 2004 † accepted as Leveniranella bella (Leven, 2004) † (type by original designation)

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  1. Species Iranella bella Leven, 2004 † accepted as Leveniranella bella (Leven, 2004) † (unaccepted > superseded combination, Type species of Leveniranella)
  2. Species Iranella longa Leven, 2004 † accepted as Leveniranella longa (Leven, 2004) † (unaccepted > superseded combination, Opinion of Vachard and Le Coze (2024))
  3. Species Iranella orbiculata Leven, 2004 † accepted as Leveniranella orbiculata (Leven, 2004) † (unaccepted > superseded combination, Opinion of Vachard and Le Coze (2024))
  4. Species Iranella pauca Leven, 2004 † accepted as Leveniranella pauca (Leven, 2004) † (unaccepted > superseded combination, Opinion of Vachard and Le Coze (2024))
marine, brackish, fresh, terrestrial
fossil only
feminine
Leven, E.; Vaziri Mohaddam, H. (2004). Carboniferous-Permian stratigraphy and fusulinids of eastern Iran. The Permian stage in the Bag-e-Vang section (Shirgesht area). <em>Rivista Italiana di Paleontologia e Stratigrafia.</em> 110: 441-465., available online at https://doi.org/10.13130/2039-4942/5816
page(s): p. 453 [details] Available for editors  PDF available [request]
Homonymy Junior homonym of Iranella Uvarov, 1922 [Insecta] and Iranella Hupé, 1955 [Trilobita]  
Homonymy Junior homonym of Iranella Uvarov, 1922 [Insecta] and Iranella Hupé, 1955 [Trilobita] [details]

Original description Description. Shell of moderate to large size, inflated fusiform to subcylindrical, with straight axis and sharply to...  
Original description Description. Shell of moderate to large size, inflated fusiform to subcylindrical, with straight axis and sharply to bluntly rounded poles. Mature specimens usually possess 6.5 to 8 whorls and are bilaterally symmetrical at all stages of growth. Proloculus small. First 2 to 3.5 whorls constitute tightly coiled juvenanum, which is terminated by abrupt expansion into loosely coiled adult stage. Spirotheca composed of tectum and keriotheca. Septa strongly but somewhat irregularly fluted throughout shell. Septal folds high, extending to top septa. Low cuniculi developed from four or five volutions. Phrenothecae weak or absent. Weak axial filling present only in juvenarium. Tunnel low and narrow. Small chomata sometimes present on the proloculus.
Discussion. Iranella. n. gen is very similar to Paraschwagerina Dunbar et Skinner in many aspects, but the latter has not cuniculi. Besides, the age of true Paraschwagerina is older (Asselian and Sakmarian). In addition to the species described in this article, the genus includes a specimen derived from the Bolorian deposits of Japan and referred by Morikawa & Isomi (1961) to the American species Paraschwagerina gigantea (White). All species of the genus Iranella described below are connected by transitional forms with Iranella bella n. sp., which is gradually changed to Chalaroschwagerina (Cuniculina) vulgarisiformis (Morikawa) (Fig. 4).
Distribution and age. Iran, Darvaz, Japan (?); Early Permian (Cisuralian), Bolorian.
 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Iranella Leven, 2004 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=1062412 on 2026-07-07
Date
action
by
2018-02-27 09:52:19Z
created
2019-03-04 10:06:11Z
changed
2024-03-13 13:40:50Z
changed
2024-10-23 13:08:47Z
changed

original description Leven, E.; Vaziri Mohaddam, H. (2004). Carboniferous-Permian stratigraphy and fusulinids of eastern Iran. The Permian stage in the Bag-e-Vang section (Shirgesht area). <em>Rivista Italiana di Paleontologia e Stratigrafia.</em> 110: 441-465., available online at https://doi.org/10.13130/2039-4942/5816
page(s): p. 453 [details] Available for editors  PDF available [request]
From editor or global species database
Homonymy Junior homonym of Iranella Uvarov, 1922 [Insecta] and Iranella Hupé, 1955 [Trilobita] [details]

Original description Description. Shell of moderate to large size, inflated fusiform to subcylindrical, with straight axis and sharply to bluntly rounded poles. Mature specimens usually possess 6.5 to 8 whorls and are bilaterally symmetrical at all stages of growth. Proloculus small. First 2 to 3.5 whorls constitute tightly coiled juvenanum, which is terminated by abrupt expansion into loosely coiled adult stage. Spirotheca composed of tectum and keriotheca. Septa strongly but somewhat irregularly fluted throughout shell. Septal folds high, extending to top septa. Low cuniculi developed from four or five volutions. Phrenothecae weak or absent. Weak axial filling present only in juvenarium. Tunnel low and narrow. Small chomata sometimes present on the proloculus.
Discussion. Iranella. n. gen is very similar to Paraschwagerina Dunbar et Skinner in many aspects, but the latter has not cuniculi. Besides, the age of true Paraschwagerina is older (Asselian and Sakmarian). In addition to the species described in this article, the genus includes a specimen derived from the Bolorian deposits of Japan and referred by Morikawa & Isomi (1961) to the American species Paraschwagerina gigantea (White). All species of the genus Iranella described below are connected by transitional forms with Iranella bella n. sp., which is gradually changed to Chalaroschwagerina (Cuniculina) vulgarisiformis (Morikawa) (Fig. 4).
Distribution and age. Iran, Darvaz, Japan (?); Early Permian (Cisuralian), Bolorian.
 [details]