Foraminifera taxon details

Paradunbarula Skinner, 1969 †

721782  (urn:lsid:marinespecies.org:taxname:721782)

accepted
Genus
Paradunbarula dallyi Skinner, 1969 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Skinner, J. W. (1969). Permian Foraminifera form Turkey. <em>The University of Kansas Palaeontological Contributions.</em> 36: 1-14., available online at http://hdl.handle.net/1808/3741
page(s): p. 6 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Paradunbarula Skinner, 1969 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721782 on 2024-07-06
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-11 15:49:39Z
changed
2018-02-22 09:25:50Z
changed
2018-06-04 15:39:20Z
changed

original description Skinner, J. W. (1969). Permian Foraminifera form Turkey. <em>The University of Kansas Palaeontological Contributions.</em> 36: 1-14., available online at http://hdl.handle.net/1808/3741
page(s): p. 6 [details]  Available for editors  PDF available [request] 

original description  (of Palaeofusulina (Paradunbarula) Skinner in Leven & Okay, 1996 †) Leven, E. Y.; Okay, A. I. (1996). Foraminifera from the exotic Permo-Carboniferous limestone blocks in the Karakaya Complex, northwestern Turkey. <em>Rivista Italiana di Paleontologia e Stratigrafia.</em> 102: 139-174., available online at https://doi.org/10.13130/2039-4942/5245 [details]  Available for editors  PDF available [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  PDF available [request] 
From editor or global species database
Diagnosis Test inflated fusiform to subglobular, poles bluntly rounded, proloculus tiny, followed by discoidal early whorls with short axis of coiling, later whorls expand more rapidly after a change in the axis of coiling; septa intensely fluted from pole to pole, the high folds extending to the chamber roof; wall with tectum, diaphanotheca, and inner tectorium, the latter extending over the interior of the septa as well as the outer wall, tunnel single, moderately wide, weak chomata only in the early whorls; septal pores numerous. U. Permian (Murgabian): Turkey; S. China; USSR: Pamir. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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