Foraminifera taxon details

Valserina Schroeder & Conrad, 1968 †

739387  (urn:lsid:marinespecies.org:taxname:739387)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Schroeder, R., M. A. Conrad, and J. Charollais, 1968, Sixième note sur les foraminifères du Crétacé inférieur de la région genèvoise. Contribution à l'étude des Orbitolinidae: Valserina brönnimanni[ sic] Schroeder & Conrad, n. gen., n. sp.; Paleodictyoconus barremianus (Moullade) et Paleodictyoconus cuvillieri (Foury), Archives des Sciences, Genève (1967) 20:199-221. , available online at https://www.researchgate.net/profile/Marc-Conrad/publication/258049271
page(s): p. 201 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Valserina Schroeder & Conrad, 1968 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739387 on 2024-04-18
Date
action
by
2013-09-04 09:28:16Z
created
2017-11-29 15:56:23Z
changed
2019-11-29 15:23:48Z
changed

original description Schroeder, R., M. A. Conrad, and J. Charollais, 1968, Sixième note sur les foraminifères du Crétacé inférieur de la région genèvoise. Contribution à l'étude des Orbitolinidae: Valserina brönnimanni[ sic] Schroeder & Conrad, n. gen., n. sp.; Paleodictyoconus barremianus (Moullade) et Paleodictyoconus cuvillieri (Foury), Archives des Sciences, Genève (1967) 20:199-221. , available online at https://www.researchgate.net/profile/Marc-Conrad/publication/258049271
page(s): p. 201 [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis High conical test, embryonic apparatus of simple protoconch and deuteroconch, slightly eccentric in position, followed by many broad, low uniserial discoidal chambers that are subdivided into marginal, radial, and central zones, the narrow marginal zone with about three orders of radial exoskeletal beams and with horizontal exoskeletal rafters, the wider radial zone subdivided by the longer first order beams that thicken rapidly, becoming triangular in section and irregularly undulating and that continue into the central zone where they anastomose to form an irregular meshwork; aperture consisting of many small pores piercing the septa in the central zone. L. Cretaceous (M. Barremian); Europe (France). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]