WoRMS taxon details

Cyclopsinella Galloway, 1933 †

738951  (urn:lsid:marinespecies.org:taxname:738951)

accepted
Genus
Cyclopsina Munier-Chalmas, 1887 † · unaccepted (Junior homonym of Cyclopsina...)  
Junior homonym of Cyclopsina Milne Edwards, 1840

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marine, brackish, fresh, terrestrial
fossil only
feminine
Galloway, J. J. (1933). A manual of Foraminifera. <em>Bloomington, Principia Press.</em> , available online at https://babel.hathitrust.org/cgi/pt?id=uc1.31822014134829
page(s): p. 138 [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Cyclopsinella Galloway, 1933 †. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=738951 on 2024-09-18
Date
action
by
2013-09-02 09:02:02Z
created
2017-11-08 11:10:51Z
changed

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original description Galloway, J. J. (1933). A manual of Foraminifera. <em>Bloomington, Principia Press.</em> , available online at https://babel.hathitrust.org/cgi/pt?id=uc1.31822014134829
page(s): p. 138 [details]   

original description  (of Cyclopsina Munier-Chalmas, 1887 †) Munier-Chalmas, E. (1887). Sur la Cyclolina et trois nouveaux genres de foraminifères des couches à rudistes: Cyclopsina, Dicyclina et Spirocyclina. <em>Compte Rendu des Séances de la Société géologique de France.</em> 4(7): 30-31.
page(s): p. xxx [details]   

additional source Neumann, M. (1964). A propos des genres Cyclolina d'Orbigny et Cyclopsinella Galloway. <em>Revue de Micropaléontologie.</em> 7(1): 47-56. [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis Test free, discoidal, large, up to 1 cm in diameter, microspheric test with early planispiral coil, rapidly becoming peneropliform, reniform, and finally with cyclic chambers, macrospheric test with protoconch and deuteroconch followed by cyclic chambers, up to fifty cyclic chambers in the adult, test up to 0.3 mm in thickness near the periphery, sutures slightly depressed, periphery broadly rounded; wall microgranular, calcareous, agglutinated, with imperforate epidermis, no exoskeletal partitions, and chamber interior undivided in early stage, later cyclic chambers with one or more endoskeletal pillars arising from a median position at the floor to extend radially from one septum to the next, pillars may bifurcate and fuse to give an irregular appearance in section (this chamber subdivision gives a superficial but erroneous appearance in section of two layers of chambers, and was so described originally; the anastomosing pillars also have been described as an undulating median partition); aperture multiple, with round openings on the peripheral surface. U. Cretaceous (Cenomanian to U. Santonian); France. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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