WoRMS taxon details

Pavonina d'Orbigny, 1826

415783  (urn:lsid:marinespecies.org:taxname:415783)

accepted
Genus
Valvopavonina Hofker, 1951 · unaccepted (Isotypic junior synonym)

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marine, brackish, fresh, terrestrial
recent + fossil
feminine
Orbigny, A. D. d'. (1826). Tableau méthodique de la classe des Céphalopodes. <em>Annales des Sciences Naturelles.</em> vol. 7: 96-169, 245-314., available online at http://biodiversitylibrary.org/page/5753959
page(s): p. 260 [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Pavonina d'Orbigny, 1826. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=415783 on 2024-03-28
Date
action
by
2009-09-23 14:01:30Z
created
db_admin
2010-09-20 10:05:34Z
changed
2014-05-07 09:49:09Z
changed
2020-01-22 14:11:58Z
changed

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original description Orbigny, A. D. d'. (1826). Tableau méthodique de la classe des Céphalopodes. <em>Annales des Sciences Naturelles.</em> vol. 7: 96-169, 245-314., available online at http://biodiversitylibrary.org/page/5753959
page(s): p. 260 [details]   

original description  (of Valvopavonina Hofker, 1951) Hofker, J. (1951). The Foraminifera of the Siboga Expedition. Part 3. <em>Siboga Expeditie, monograph.</em> 4: 1-513.
page(s): p. 35 [details]  Available for editors  PDF available [request] 

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  PDF available [request] 
From editor or global species database
Diagnosis Test broadly palmate, flattened, with reduced triserial stage of only three chambers, then biserial, with rapidly broadening chambers, and finally uniserial, with very broad, low, and semicircular chambers increasing rapidly in breadth and strongly curved proximally at the margins, periphery bluntly rounded to truncate and bicarinate on the apertural face, sutures strongly arched, depressed; wall calcareous, optically radial, coarsely perforate, surface smooth to pustulose; aperture not apparent on well-preserved specimens except for coarse perforations on the apertural face like those of the remainder of the test, larger intercameral foramina formed by resorption as new chamber is added. Miocene to Holocene; Atlantic; Pacific; Africa; Madagascar; North America. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]