WoRMS taxon details

Faujasina d'Orbigny, 1839

722438  (urn:lsid:marinespecies.org:taxname:722438)

accepted
Genus

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marine, brackish, fresh, terrestrial
recent + fossil
feminine
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]   
Type locality contained in Cuban Exclusive Economic Zone  
type locality contained in Cuban Exclusive Economic Zone [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Faujasina d'Orbigny, 1839. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=722438 on 2024-04-25
Date
action
by
2013-03-08 13:53:47Z
created
2017-05-29 14:02:33Z
changed
2018-01-08 09:58:22Z
changed

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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]   

basis of record 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] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

From editor or global species database
Diagnosis Test trochospiral, planoconvex, partially evolute flat spiral side with numerous rapidly enlarging and strongly arched chambers and curved oblique sutures, umbilical side convex and involute, with strongly arched sutures curving forward midway from the umbilicus and then recurved toward the periphery, intraseptal canals connect the well-developed canal system on the umbilical side with the narrower one of the spiral side, periphery angular to carinate; wall calcareous, ornamentation consists of regular and closely spaced ponticuli extending into ridges and grooves that begin at the basal margin of the chambers and extend nearly to the succeeding septum, remainder of the wall surface distinctly pustulose; aperture consists of a row of pores at the base of the apertural face on the umbilical side, and a few rimmed areal pores may occur in one or two rows on the face. Pliocene to Pleistocene; England; France; Belgium; Netherlands; Japan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]