Taxonomy
Original description: Das sehr kleine Gehäuse besteht aus 15-16 Kammern von denen 5-6. den letzen Umgang bilden. Es ist flch trochospiral gebaut: die Kammern sind gewolbt und deutlich getrennt, sie vergrössern sich sehr allmählich. Der Nabel ist offen, aber klein. Die Apertur ist nicht gegen den Nabel gerichtet, sondern liegt in der Windungsrichtung an der Basis der letzten Kammer.
[The very small test consists of 15 to 16 chambers of which 5 to 6 form the last volution. It is flat-trochospiral, chambers are arched and distinctly separated, and enlarge only very gradually. Umbilicus is open but small. Aperture is not directed towards umbilicus, but is located at the base of the last chamber and within direction of the coil. - Translation from Chornos website]
Entries in the Catalog of original descriptions: Globigerina infracretacea, Globigerina infracretacea trochoidea, Globigerina infracretacea gargasiana, Globigerina aptica, Hedbergella beegumensis
Emended description:
Character matrix
test outline: | Subcircular | chamber arrangement: | Trochospiral | edge view: | Equally biconvex | aperture: | Extraumbilical |
sp chamber shape: | Globular | coiling axis: | Low | periphery: | N/A | aperture border: | Thin lip |
umb chbr shape: | Globular | umbilicus: | Narrow | periph margin shape: | Broadly rounded | accessory apertures: | N/A |
spiral sutures: | Moderately depressed | umb depth: | Shallow | wall texture: | Perforation cones | shell porosity: | Finely Perforate: 1-2.5µm |
umbilical or test sutures: | Moderately depressed | final-whorl chambers: | 5-5.5 | N.B. These characters are used for advanced search. N/A - not applicable |
Geological Range:
Last occurrence (top): within P. rohri zone (113.22-116.60Ma, top in Aptian stage). Data source: copied from Chronos database, but zonal name updated from T. bejaouaensis to T. rohri
First occurrence (base): within L. cabri zone (119.05-120.55Ma, base in Aptian stage). Data source: [copied from Chronos database]
Plot of range and occurrence data:
Agalarova, D. A. (1951). Studies of microfauna from Cretaceous deposits of Azerbaydzhan. Aznefteizdat, Baku. 1-128. gs Banner, F. T., Copestake, P. & White, M. R. (1993). Barremian-Aptian Praehedbergellidae of the North Sea area: a reconnaisance. Bulletin of the Natural History Museum, London (Geology). 49: 1-30. gs Glaessner, M. F. (1937a). Planktonforaminiferen aus der Kreide und dem Eozän und ihre stratigraphische Bedeutung. Etyudy po Mikropaleontologiy, Paleontologicheskaya Laboratoriya Moskovskogo Gosudarstvennogo Universiteta. 1(1): 27-46. gs Huber, B. T. & Leckie, R. M. (2011). Planktic foraminiferal species turnover across deep-sea Aptian/Albian boundary sections. Journal of Foraminiferal Research. 41: 53-95. gs Moullade, M. (1960). Sur quelques Foraminiferes du Cretace inferieur des Baronnies (Drome). Revue de Micropaléontologie. 3(2): +136+-. gs Moullade, M. (1961). Quelques foraminifères et ostracodes nouveaux du Crétacé inférieur Vocontien. Revue de Micropaléontologie. 3(4): 213-216. gsReferences:
Hedbergella infracretacea compiled by the pforams@mikrotax project team viewed: 11-9-2024
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Comments (4)
You have also in the synonymy :
Globigerina infracretacea subsp. gargasiana Moullade, 1961 an unnecessary nomen novum of Globigerina infracretacea subsp. trochoidea Moullade, 1960
why was it a superfluous name?
Moullade was considering the genus Hedbergella as useless. If it had been confirmed his subsp. would have been a junior homonym of Hedbergella trochoidea (Gandolfi)= Anomalina lorneiana (d'Orb.) trocoidea Gandolfi, 1942
this is quite complex, I think I have explained it, but I will ask Brain to take a look