Foraminifera taxon details
Dictyopsella Munier-Chalmas in Schlumberger, 1900 †
739168 (urn:lsid:marinespecies.org:taxname:739168)
accepted
Genus
Dictyopsella kiliani Munier-Chalmas in Schlumberger, 1900 † (type by subsequent designation)
- Species Dictyopsella chalmasi Schlumberger, 1900 †
- Species Dictyopsella charentensis Loeblich & Tappan, 1985 †
- Species Dictyopsella fragilis Hercogová, 1988 †
- Species Dictyopsella hofkeri Loeblich & Tappan, 1985 †
- Species Dictyopsella kiliani Munier-Chalmas in Schlumberger, 1900 †
- Species Dictyopsella libanica Saint-Marc, 1973 †
- Species Dictyopsella muretae Hottinger, 1967 †
- Species Dictyopsella cuvillieri Gendrot, 1968 † accepted as Dictyopselloides cuvillieri (Gendrot, 1968) † (Type species of Dictyopselloides)
marine, brackish, fresh, terrestrial
fossil only
feminine
Schlumberger, C. (1900). Note sur quelques Foraminifères nouveaux ou peu connus du Crétacé d'Espagne. <em>Bulletin de la Société géologique de France.</em> (3) 27 (5): 456-465., available online at https://biodiversitylibrary.org/page/31121111
page(s): p. 462 [details]
page(s): p. 462 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Dictyopsella Munier-Chalmas in Schlumberger, 1900 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739168 on 2024-08-30
Date
action
by
original description
Schlumberger, C. (1900). Note sur quelques Foraminifères nouveaux ou peu connus du Crétacé d'Espagne. <em>Bulletin de la Société géologique de France.</em> (3) 27 (5): 456-465., available online at https://biodiversitylibrary.org/page/31121111
page(s): p. 462 [details]
page(s): p. 462 [details]
From editor or global species database
Diagnosis Low conical trochospiral test, with large globular proloculus followed by about two whorls of broad low, semilunate chambers as seen from the spiral side, on the umbilical side chambers appear subtriangular with an umbilical prolongation that may spread slightly, and sutures are slightly curved and incised, interior of chambers with numerous long radial beams that arise perpendicular to the apertural face and septa and extend nearly to the center of the test, proloculus and all later chambers with shallow secondary beams that project inward from the spiral and umbilical surfaces of the test and are interconnected by rafters to produce a characteristic subepidermal network; wall finely agglutinated, surface smoothly finished; primary aperture a low interiomarginal arch, located midway between umbilicus and periphery, with smaller secondary openings present on the opposite side of the umbilical chamber flap. U. Cretaceous (Cenomanian to Maastrichtian); France; Spain. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
