Foraminifera taxon details

Paraleeina Leven, 2004 †

Parafusulina postkraffti Leven, 1967
Parafusulina postkraffti Leven, 1967

1062414 (urn:lsid:marinespecies.org:taxname:1062414)

  1. Biota
  2. Chromista (Kingdom)
  3. Harosa (Subkingdom)
  4. Rhizaria (Infrakingdom)
  5. Foraminifera (Phylum)
  6. Fusulinata † (Class)
  7. Fusulinana † (Subclass)
  8. Fusulinida † (Order)
  9. Schwagerinoidea † (Superfamily)
  10. Schwagerinidae † (Family)
  11. Schwagerininae † (Subfamily)
  12. Paraleeina † (Genus)
accepted
Genus

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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. 454 [details] Available for editors  PDF available [request]
Original description Description. Shell moderate to large size, thick fusiform, nearly horizontal to slightly concave median por- tion, stright...  
Original description Description. Shell moderate to large size, thick fusiform, nearly horizontal to slightly concave median por- tion, stright to convex lateral slopes, and bluntly pointed poles. Mature individuals usually possess 7 to 8 whorls. Coiling is uniform. Spirotheca thick composed of tectum and coarsely alveolar keriotheca. Septa are rather regularly and intensely fluted throughout shell, but in median part low septa loops developed. Phrenothecae slightly developed, but may be absent. Cuniculi present. Proloculus usually large, sphaerical or subsphaerical in shape. Weak chomata present only on proloculus. Massive secondary deposits fill much of shell between tunnel area and poles except in outermost whorl. Tunnel low and not very wide.
Distribution and age. Everywhere in Tethys, Koryak Range, California; Early Permian (Cisuralian), Bolorian; Late Permian (Tethysian), Kubergandian and Murgabian.
(Leven in Leven and Vaziri Mohaddam (2004)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Paraleeina Leven, 2004 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=1062414 on 2026-07-19
Date
action
by
2018-02-27 09:52:19Z
created
Le Coze, François

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. 454 [details] Available for editors  PDF available [request]
From editor or global species database
Original description Description. Shell moderate to large size, thick fusiform, nearly horizontal to slightly concave median por- tion, stright to convex lateral slopes, and bluntly pointed poles. Mature individuals usually possess 7 to 8 whorls. Coiling is uniform. Spirotheca thick composed of tectum and coarsely alveolar keriotheca. Septa are rather regularly and intensely fluted throughout shell, but in median part low septa loops developed. Phrenothecae slightly developed, but may be absent. Cuniculi present. Proloculus usually large, sphaerical or subsphaerical in shape. Weak chomata present only on proloculus. Massive secondary deposits fill much of shell between tunnel area and poles except in outermost whorl. Tunnel low and not very wide.
Distribution and age. Everywhere in Tethys, Koryak Range, California; Early Permian (Cisuralian), Bolorian; Late Permian (Tethysian), Kubergandian and Murgabian.
(Leven in Leven and Vaziri Mohaddam (2004)). [details]
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From editor or global species database

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