WoRMS taxon details
Normanina Cushman, 1928
182838 (urn:lsid:marinespecies.org:taxname:182838)
accepted
Genus
Haliphysema confertum Norman, 1878 accepted as Normanina conferta (Norman, 1878) (type by original designation)
marine, brackish, fresh, terrestrial
Cushman, J. A. (1928). Additional genera of foraminfera. Cushman Laboratory for Foraminiferal Research. <em>Contributions.</em> 4(1): 1-8., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/4cclfr1.pdf
page(s): p. 7 [details] Available for editors
[request]
page(s): p. 7 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Normanina Cushman, 1928. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=182838 on 2024-04-26
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original description
Cushman, J. A. (1928). Additional genera of foraminfera. Cushman Laboratory for Foraminiferal Research. <em>Contributions.</em> 4(1): 1-8., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/4cclfr1.pdf
page(s): p. 7 [details] Available for editors [request]
basis of record BIOCEAN, available online at http://www.ifremer.fr/biocean/ [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]
page(s): p. 7 [details] Available for editors
[request] basis of record BIOCEAN, available online at http://www.ifremer.fr/biocean/ [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 an irregular mass of tightly branching tubules, radiating outward to terminate in globular to clublike swellings that may be internally subdivided by septa; sediment may fill the space between the tubules. Holocene; N. Pacific, at 5,588 m to 6,079 m; S. Pacific, off Chile, at 3,950 m; N. Atlantic at 3,203 m; E. Atlantic at 4,706 to 5,300 m; Caribbean at 2,920 m to 5,650 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
