Foraminifera taxon details
Neoiraqia Danilova, 1963 †
739380 (urn:lsid:marinespecies.org:taxname:739380)
accepted
Genus
Neoiraqia convexa Danilova, 1963 † (type by original designation)
Naupliella Decrouez & Moullade, 1974 † · unaccepted (Subjective junior synonym Opinion...)
Subjective junior synonym Opinion of Schroeder and Neumann (1985), Yazdi-Moghadam and Schlagintweit (2021)
- Species Neoiraqia convexa Danilova, 1963 †
- Species Neoiraqia insolita (Decrouez & Moullade, 1974) †
- Species Neoiraqia cuvillieri Moullade in Moullade et al., 1972 † accepted as Conicorbitolina cuvillieri (Moullade in Moullade et al., 1972) † (Opinion of Simmons et al. (2000), Yazdi-Moghadam and Schlagintweit (2021))
marine, brackish, fresh, terrestrial
fossil only
feminine
Danilova, A. (1963). Neoiraqia convexa -- nov foraminifer iz cenoman-turona Kosova polja - Neoiraqia convexa -- un nouveau foraminifère du Cénomanien-Turonien de Kosovo Polje - Neoiraqia convexa -- a new foraminifer from the Cenomanian-Turonian of Kosovo Polje. <em>Zavod za Geološka i Geofizička Istraživanja, Vesnik, Beograd, (Serija A).</em> 20[1962]: 223-239.
page(s): p. 226 [details] Available for editors
[request]
page(s): p. 226 [details] Available for editors

Diagnosis Test conical, apex rounded, with embryonic apparatus, subdivided supraembryonic area and incompletely divided subembryonal...
Diagnosis Test conical, apex rounded, with embryonic apparatus, subdivided supraembryonic area and incompletely divided subembryonal area, later chambers uniserial and discoidal with narrow cellular subepidermal marginal zone formed by intersecting primary and second order exoskeletal radial beams that alternate rather than being aligned from one chamber to the next, and the horizontal exoskeletal rafters, radial zone much reduced or absent but central reticulate zone is wide, occupying most of the test diameter, radial partitions wider near the chamber floor and taper upward toward the chamber roof but may be incomplete; wall of imperforate microgranular calcite, with insignificant amount of fine agglutinated material; numerous obliquely arranged intercameral pores present, in addition to pores connecting chamberlets of a single chamber. U. Cretaceous (U. Cenomanian); Yugoslavia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Neoiraqia Danilova, 1963 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=739380 on 2025-05-23
Date
action
by
original description
Danilova, A. (1963). Neoiraqia convexa -- nov foraminifer iz cenoman-turona Kosova polja - Neoiraqia convexa -- un nouveau foraminifère du Cénomanien-Turonien de Kosovo Polje - Neoiraqia convexa -- a new foraminifer from the Cenomanian-Turonian of Kosovo Polje. <em>Zavod za Geološka i Geofizička Istraživanja, Vesnik, Beograd, (Serija A).</em> 20[1962]: 223-239.
page(s): p. 226 [details] Available for editors
[request]
original description (of Naupliella Decrouez & Moullade, 1974 †) Decrouez, D.; Moullade, M. (1974). Orbitolinidés nouveaux de I'Albo-Cénomanien de Grèce. <em>Archives des Sciences, Genève.</em> 27: 75-92., available online at http://doi.org/10.5169/seals-739298
page(s): p. 87 [details] Available for editors
[request]
additional source Moullade, M., Pybernès, J., Rey, J. (1979). Révision et intérêt stratigraphique du genre Neoiraqia Danilova, 1962, Orbitolinidé du Mésocrétacé mésogéen. <em>Comptes Rendus de l'Académie des Sciences, Sér D 288: 939-942.</em> [details] Available for editors
[request]
page(s): p. 226 [details] Available for editors

original description (of Naupliella Decrouez & Moullade, 1974 †) Decrouez, D.; Moullade, M. (1974). Orbitolinidés nouveaux de I'Albo-Cénomanien de Grèce. <em>Archives des Sciences, Genève.</em> 27: 75-92., available online at http://doi.org/10.5169/seals-739298
page(s): p. 87 [details] Available for editors

additional source Moullade, M., Pybernès, J., Rey, J. (1979). Révision et intérêt stratigraphique du genre Neoiraqia Danilova, 1962, Orbitolinidé du Mésocrétacé mésogéen. <em>Comptes Rendus de l'Académie des Sciences, Sér D 288: 939-942.</em> [details] Available for editors





From editor or global species database
Diagnosis Test conical, apex rounded, with embryonic apparatus, subdivided supraembryonic area and incompletely divided subembryonal area, later chambers uniserial and discoidal with narrow cellular subepidermal marginal zone formed by intersecting primary and second order exoskeletal radial beams that alternate rather than being aligned from one chamber to the next, and the horizontal exoskeletal rafters, radial zone much reduced or absent but central reticulate zone is wide, occupying most of the test diameter, radial partitions wider near the chamber floor and taper upward toward the chamber roof but may be incomplete; wall of imperforate microgranular calcite, with insignificant amount of fine agglutinated material; numerous obliquely arranged intercameral pores present, in addition to pores connecting chamberlets of a single chamber. U. Cretaceous (U. Cenomanian); Yugoslavia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]