Foraminifera taxon details

Pseudopfenderina Hottinger, 1967 †

739304  (urn:lsid:marinespecies.org:taxname:739304)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Hottinger, L. (1967). Foraminifères imperforés du Mésozoïque marocain. <em>Notes et Mémoires du Service Géologique du Maroc.</em> 209: 1-168.
page(s): pp. 87, 89 [details] Available for editors  PDF available [request]
Diagnosis Test a high trochospiral, chambers numerous, strongly inclined with respect to the axis of coiling, the microspheric...  
Diagnosis Test a high trochospiral, chambers numerous, strongly inclined with respect to the axis of coiling, the microspheric generation becoming very high and almost rectilinear, megalospheric generation shorter and more conical in form, apertural face consists of a septal expansion covering the umbilical region, umbilical part of the chamber interior filled with numerous pillars that are continuous from chamber to chamber and form a columellar endoskeleton in the axis of coiling, axis of the juvenile whorls filled with secondary deposits, resulting in a massive central area but lacking a subcameral tunnel; wall calcareous, microgranular in structure; aperture consisting of many pores in the apertural face. L. Jurassic (M. Lias); Morocco. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Pseudopfenderina Hottinger, 1967 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=739304 on 2025-05-22
Date
action
by
2013-09-04 09:28:16Z
created
2016-12-19 06:42:07Z
changed
2017-11-27 12:58:52Z
changed

original description Hottinger, L. (1967). Foraminifères imperforés du Mésozoïque marocain. <em>Notes et Mémoires du Service Géologique du Maroc.</em> 209: 1-168.
page(s): pp. 87, 89 [details] Available for editors  PDF available [request]
From editor or global species database
Diagnosis Test a high trochospiral, chambers numerous, strongly inclined with respect to the axis of coiling, the microspheric generation becoming very high and almost rectilinear, megalospheric generation shorter and more conical in form, apertural face consists of a septal expansion covering the umbilical region, umbilical part of the chamber interior filled with numerous pillars that are continuous from chamber to chamber and form a columellar endoskeleton in the axis of coiling, axis of the juvenile whorls filled with secondary deposits, resulting in a massive central area but lacking a subcameral tunnel; wall calcareous, microgranular in structure; aperture consisting of many pores in the apertural face. L. Jurassic (M. Lias); Morocco. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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