Foraminifera taxon details
Reissia Loeblich & Tappan, 1964
722203 (urn:lsid:marinespecies.org:taxname:722203)
accepted
Genus
Ehrenbergina hystrix Brady, 1881 accepted as Reissia hystrix (Brady, 1881) (type by original designation)
- Species Reissia hystrix (Brady, 1881)
marine, brackish, fresh, terrestrial
recent + fossil
Loeblich, A. R.; Tappan, H. (1964). Treatise on Invertebrate Paleontology, Part C: Protista 2, Sarcodina, chiefly "Thecamoebians" and Foraminiferida. <em>Geological Society of America and University of Kansas Press, Lawrence.</em> [details] Available for editors 
[request]
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Reissia Loeblich & Tappan, 1964. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722203 on 2024-06-16
Date
action
by
original description
Loeblich, A. R.; Tappan, H. (1964). Treatise on Invertebrate Paleontology, Part C: Protista 2, Sarcodina, chiefly "Thecamoebians" and Foraminiferida. <em>Geological Society of America and University of Kansas Press, Lawrence.</em> [details] Available for editors [request]
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 [request]
[request] 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
[request] From editor or global species database
Diagnosis Test with chambers biserially arranged, the plane of biseriality planispirally enrolled in the early part, then uncoiling as in Cassidulinoides but with test compressed perpendicular to the plane of biseriality as in Ehrenbergina, sutures strongly oblique, curved, slightly depressed; wall calcareous, optically radial, commonly with lateral spines and flangelike carinae that are most prominent in the early stage, later chambers nearly smooth, apertural face may have grooves radiating from the aperture; aperture a large curved opening, with broad apertural flap protruding from the inner margin of the opening, against the previous chamber. Holocene, deep water, at 3,000 m to 4,500 m; N. and S. Pacific. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
