Foraminifera taxon details
Vervilleina Groves in Groves & Boardman, 1999 †
1115585 (urn:lsid:marinespecies.org:taxname:1115585)
accepted
Genus
Dentalina bradyi Spandel, 1901 † accepted as Vervilleina bradyi (Spandel, 1901) † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
Groves, J. R.; Boardman, H. (1999). Calcareous smaller foraminifers from the lower Permian Council Grove Group near Hooser, Kansas. <em>Journal of Foraminiferal Research.</em> 29: 243-262.
page(s): p. 255 [details] Available for editors
[request]
page(s): p. 255 [details] Available for editors

Original description Test consists of a spherical proloculus followed by a rectilinear to slightly curved, uniserial succession of egg-shaped....
Original description Test consists of a spherical proloculus followed by a rectilinear to slightly curved, uniserial succession of egg-shaped. oblong, to cvlindrical chambers, Septa are short but well defined and anteriorly directed. Wall is relatively thin and two layered, consisting of an inner microgranular layer and an outer hvaline layer. Aperture is a simple terminal opening.
Occurrence: Asselian-Artinskian-?Late Permian.
(Groves and Boardman (1999)). [details]
Occurrence: Asselian-Artinskian-?Late Permian.
(Groves and Boardman (1999)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Vervilleina Groves in Groves & Boardman, 1999 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=1115585 on 2025-09-16
Date
action
by
original description
Groves, J. R.; Boardman, H. (1999). Calcareous smaller foraminifers from the lower Permian Council Grove Group near Hooser, Kansas. <em>Journal of Foraminiferal Research.</em> 29: 243-262.
page(s): p. 255 [details] Available for editors
[request]
page(s): p. 255 [details] Available for editors

From editor or global species database
Original description Test consists of a spherical proloculus followed by a rectilinear to slightly curved, uniserial succession of egg-shaped. oblong, to cvlindrical chambers, Septa are short but well defined and anteriorly directed. Wall is relatively thin and two layered, consisting of an inner microgranular layer and an outer hvaline layer. Aperture is a simple terminal opening.Occurrence: Asselian-Artinskian-?Late Permian.
(Groves and Boardman (1999)). [details]