Foraminifera taxon details
Praesiderolites Wannier, 1983 †
722366 (urn:lsid:marinespecies.org:taxname:722366)
accepted
Genus
Praesiderolites douvillei Wannier, 1983 † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
masculine
Wannier, M. (1983). Evolution, biostratigraphie et systématique des Siderolitinae (Foraminifères). <em>Revista Española de Micropaleontología.</em> 15(1): 5-57.
page(s): p. 16 [details] Available for editors
[request]
page(s): p. 16 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Praesiderolites Wannier, 1983 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=722366 on 2024-04-24
Date
action
by
original description
Wannier, M. (1983). Evolution, biostratigraphie et systématique des Siderolitinae (Foraminifères). <em>Revista Española de Micropaleontología.</em> 15(1): 5-57.
page(s): p. 16 [details] Available for editors [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 [request]
page(s): p. 16 [details] Available for editors
[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
[request] From editor or global species database
Diagnosis Test lenticular, centrally swollen, planispirally enrolled and involute, with about three whorls and up to eighteen chambers in the final whorl, radial pillers appear as pustules at the surface, pustules larger in umbonal areas and progressively smaller toward the periphery, canal system consists of a spiral canal in the umbilical area, lateral intraseptal canals, equatorial radial canals, and a marginal canal, no lateral chamberlets such as occur in Arnaudiella, periphery angular, peripheral outline circular and may be denticulate; wall calcareous, coarsely perforate; a single row of intercameral foramina present at the base of the septa. U. Cretaceous (Santonian to Campanian); Spain; France. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]