Schroeder, R.; Conrad, M.A. (1968). Huitième note sur les Foraminifères du Crétacé inférieur de la région genevoise. Eopalorbitolina charollaisi n.gen., n.sp., un Orbitolinidé nouveau du Barrémien à faciès urgonien. <em>Compte rendu des Sciences de la Société de Physique et d'Histoire naturelle de Genève, Nouvelle Série.</em> [1967]: 145–162., available online athttps://archive-ouverte.unige.ch/files/downloads/0/0/1/3/8/4/2/5/unige_138425_attachment01.pdf page(s): p. 149 [details] Available for editors [request]
Diagnosis Test conical, similar to Palorbitolina in structure but with embryonal apparatus at one side of the apex and consisting of...
Diagnosis Test conical, similar to Palorbitolina in structure but with embryonal apparatus at one side of the apex and consisting of globular proloculus and a lateral chamber, later uniserial and discoidal chambers with differentiated marginal zone having strongly developed vertical radial beams or septula, and central zone with more labyrinthine arrangement, rather than with pillars. L. Cretaceous (Barremian); France. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Eopalorbitolina Schroeder, 1968 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739376 on 2026-09-10
original descriptionSchroeder, R.; Conrad, M.A. (1968). Huitième note sur les Foraminifères du Crétacé inférieur de la région genevoise. Eopalorbitolina charollaisi n.gen., n.sp., un Orbitolinidé nouveau du Barrémien à faciès urgonien. <em>Compte rendu des Sciences de la Société de Physique et d'Histoire naturelle de Genève, Nouvelle Série.</em> [1967]: 145–162., available online athttps://archive-ouverte.unige.ch/files/downloads/0/0/1/3/8/4/2/5/unige_138425_attachment01.pdf page(s): p. 149 [details] Available for editors [request]
From editor or global species database
Diagnosis Test conical, similar to Palorbitolina in structure but with embryonal apparatus at one side of the apex and consisting of globular proloculus and a lateral chamber, later uniserial and discoidal chambers with differentiated marginal zone having strongly developed vertical radial beams or septula, and central zone with more labyrinthine arrangement, rather than with pillars. L. Cretaceous (Barremian); France. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]