Peruvian Register of Marine Species
WoRMS taxon details
Robertinina
856670 (urn:lsid:marinespecies.org:taxname:856670)
Loeblich & Tappan, 1984
accepted
Suborder
- Superfamily Ceratobuliminoidea Cushman, 1927
- Superfamily Conorboidoidea Thalmann, 1952 †
- Superfamily Robertinoidea Reuss, 1850
marine, fresh, terrestrial
Loeblich, A. R.; Tappan, H. (1984). Suprageneric Classification of the Foraminiferida (Protozoa). <em>Micropaleontology.</em> 30(1): 1-70., available online at https://doi.org/10.2307/1485456 [details] Available for editors 
[request]
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Robertinina. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=856670 on 2024-10-30
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original description
Loeblich, A. R.; Tappan, H. (1984). Suprageneric Classification of the Foraminiferida (Protozoa). <em>Micropaleontology.</em> 30(1): 1-70., available online at https://doi.org/10.2307/1485456 [details] Available for editors [request]
additional source Rigaud, S.; Martini, R.; Vachard, D. (2015). Early evolution and new classification of the order Robertinida (Foraminifera). <em>The Journal of Foraminiferal Research.</em> 45(1): 3-28., available online at https://doi.org/10.2113/gsjfr.45.1.3 [details] Available for editors [request]
[request]additional source Rigaud, S.; Martini, R.; Vachard, D. (2015). Early evolution and new classification of the order Robertinida (Foraminifera). <em>The Journal of Foraminiferal Research.</em> 45(1): 3-28., available online at https://doi.org/10.2113/gsjfr.45.1.3 [details] Available for editors
[request]From editor or global species database
Diagnosis Test planispirally to trochospirally enrolled; chambers provided with internal partition that attaches near apertural foramen; wall of hyaline, perforate, ultrastructurally and optically radiate aragonite (orthorhombic crystal form of calcium carbonate), the hexagonal prisms with c-axis normal to the wall surface and basal pinacoid parallel to the surface, prisms in bundles surrounded by organic sheaths; extremely fine wall perforations may be localized in pore fields. M. Triassic to Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
