Foraminifera taxon details

Protopeneroplis Weynschenk, 1950 †

721925  (urn:lsid:marinespecies.org:taxname:721925)

accepted
Genus
Protopeneroplis striata Weynschenk, 1950 † (type by original designation)
Ventrolamina Weynschenk, 1950 † · unaccepted (Subjective junior synonym in...)  
Subjective junior synonym in opinion of Loeblich & Tappan, 1987

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marine, brackish, fresh, terrestrial
fossil only
feminine
Weynschenk, R., 1950, Die Jura-Mikrofauna und -flora des Sonnwendgebirges (Tirol), Schlern-Schriften, Universität Innsbruck 83:1-32.  [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Protopeneroplis Weynschenk, 1950 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721925 on 2024-05-02
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-15 15:23:50Z
changed
2019-12-04 15:56:56Z
changed

original description Weynschenk, R., 1950, Die Jura-Mikrofauna und -flora des Sonnwendgebirges (Tirol), Schlern-Schriften, Universität Innsbruck 83:1-32.  [details]   

original description  (of Ventrolamina Weynschenk, 1950 †) Weynschenk, R., 1950, Die Jura-Mikrofauna und -flora des Sonnwendgebirges (Tirol), Schlern-Schriften, Universität Innsbruck 83:1-32.
page(s): p. 17 [details]   

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] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
From editor or global species database
Diagnosis Test lenticular, 0.4 mm to 0.8 mm in diameter and up to 0.42 mm in thickness, enrolled in about two rapidly enlarging and loosely coiled planispiral, oscillating, or low trochospiral whorls, final whorl with twelve to sixteen chambers, involute, periphery angular to rounded; wall calcareous, lamellar, of two layers, an inner microgranular one and an outer hyaline layer of radial structure, septa largely formed by the inner layer or may be partially covered by the outer layer, the hyaline layer rapidly thickening from the beginning of the last whorl and may appear distinctly lamellar in equatorial section, in axial section lamellae and wall layers result in alternating dark and light layers, surface may have calcareous pustules; aperture areal, in the lower part of the apertural face, and somewhat protruding. M. Jurassic (U. Dogger) to L. Cretaceous (Berriasian); Austria; Italy; France; Yugoslavia; Switzerland; Israel; Turkey. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]