Foraminifera taxon details
original description
Orbigny, A. D. d'. (1839). Foraminifères, in de la Sagra R., Histoire physique, politique et naturelle de l'ile de Cuba. <em>A. Bertrand.</em> 1-224., available online at https://books.google.pt/books?id=KpVeAAAAcAAJ&pg page(s): p. 109 [details]
original description
(of Pupina d'Orbigny, 1839 †) Orbigny, A. D. d'. (1839). Foraminifères, in de la Sagra R., Histoire physique, politique et naturelle de l'ile de Cuba. <em>A. Bertrand.</em> 1-224., available online at https://books.google.pt/books?id=KpVeAAAAcAAJ&pg page(s): p. 29, 30 [details]
original description
(of Verneuilina (Chrysalidina) Brady, 1881) Brady, H. B. (1881). Notes on some of the Reticularian Rhizopoda of the "Challenger" Expedition. Part III. <em>Quarterly Journal of Microscopical Science.</em> (2) 21 (81): 31-71., available online at https://biodiversitylibrary.org/page/13808725 page(s): p. 44 [details]
additional source
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 elongate conical, triserial, with numerous low and strongly overlapping chambers, the final three occupying one-third to onehalf the test length, sutures horizontal on the faces of the test, interior of peripheral region of chambers undivided, but central area of the chamber beneath the apertural pores has short thick endoskeletal pillars projecting inward from the chamber roof, some completely crossing the chamber lumen; wall thick, finely agglutinated, largely of calcareous particles, very finely canaliculate; aperture consisting of numerous fine pores over the umbilical area and most of the upper surface of the three chambers of the final whorl, part of this porous region of the two previous chambers remaining exposed as each new chambet is added, outer row of pores in a slight groove that marks the border of the perforated region. M. Cretaceous (Cenomanian to Turonian); France; Yugoslavia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
From editor or global species database
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