Foraminifera taxon details
Archimerismus Loeblich & Tappan, 1984
415073 (urn:lsid:marinespecies.org:taxname:415073)
accepted
Genus
Hyperammina subnodosa Brady, 1884 accepted as Archimerismus subnodosus (Brady, 1884) (type by original designation)
- Species Archimerismus subnodosus (Brady, 1884)
- Species Archimerismus arenaceus (Cushman, 1927) accepted as Psammosiphonella arenacea (Cushman, 1927) (Type species of Psammosiphonella (reinstated))
- Species Archimerismus subnodosa (Brady, 1884) accepted as Archimerismus subnodosus (Brady, 1884)
marine, brackish, fresh, terrestrial
recent only
masculine
Loeblich, A. R.; Tappan, H. (1984). Some
new proteinaceous and agglutinated genera of
Foraminiferida. <em>Journal of Paleontology.</em> 58: 1158-1163.
page(s): p. 1161 [details] Available for editors
[request]
page(s): p. 1161 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Archimerismus Loeblich & Tappan, 1984. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=415073 on 2024-04-19
Date
action
by
2009-09-23 14:01:30Z
created
db_admin
original description
Loeblich, A. R.; Tappan, H. (1984). Some
new proteinaceous and agglutinated genera of
Foraminiferida. <em>Journal of Paleontology.</em> 58: 1158-1163.
page(s): p. 1161 [details] Available for editors [request]
page(s): p. 1161 [details] Available for editors
[request] 
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Diagnosis Test large, elongate, with globular proloculus followed by elongate tubular chambers, with somewhat irregular size increase, separated only by constrictions of the wall that do not form true septa; wall agglutinated, thin at the base of the proloculus, becoming thicker toward the aperture, and many grains thick in the remainder of the test, of coarse quartz grains firmly held in a small amount of cement, with inner proteinaceous layer; aperture terminal, rounded, at the somewhat constricted end of the final chamber. Holocene; N. Atlantic from 40 m to 900 m; S. Atlantic at 700 m; S. Pacific at 2,850 m to 5,200 m; N. Pacific from 4,600 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
