Foraminifera taxon details
Robertininae Reuss, 1850
marine, fresh, terrestrial
recent + fossil
Not documented
Diagnosis Test predominantly dextrally coiled in a high trochospiral, numerous broad and low chambers subdivided by transverse...
Diagnosis Test predominantly dextrally coiled in a high trochospiral, numerous broad and low chambers subdivided by transverse partition formed by infolding of the outer wall, sutures oblique, slightly depressed; wall aragonitic, hyaline, optically radial, very finely perforate, surface smooth; aperture elongate, looplike, extending up the face of the final chamber, a small supplementary triangular opening on the opposite side of the test at the junction of the inner partition and previous septum, supplementary openings of earlier chambers closed as a new chamber is added. Paleocene to Holocene; Europe; North America; New Zealand; Atlantic; Pacific; Arctic; Antarctic. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Robertininae Reuss, 1850. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=720984 on 2024-11-19
Date
action
by
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 predominantly dextrally coiled in a high trochospiral, numerous broad and low chambers subdivided by transverse partition formed by infolding of the outer wall, sutures oblique, slightly depressed; wall aragonitic, hyaline, optically radial, very finely perforate, surface smooth; aperture elongate, looplike, extending up the face of the final chamber, a small supplementary triangular opening on the opposite side of the test at the junction of the inner partition and previous septum, supplementary openings of earlier chambers closed as a new chamber is added. Paleocene to Holocene; Europe; North America; New Zealand; Atlantic; Pacific; Arctic; Antarctic. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]