Catalog - Globoconusa Catalog - Globoconusa

CATALOG OF ORIGINAL DESCRIPTIONS: Globoconusa Khalilov, 1956

This page provides data from the catalog of type descriptions. The catalog is sorted alphabetically. Use the current identification link to go back to the main database.


Higher levels: pf_cat -> G -> Globoconusa
Other pages this level: << < Globigerina (Orbulina), Globigerina (Zeaglobigerina), Globigerinanus, Globigerinatella, Globigerinatheka, Globigerinella, Globigerinellita, Globigerinelloides, Globigerinita, Globigerinoides, Globigerinoidesella, Globigerinoita, Globigerinopsis, Globigerinopsoides, Globoconella, Globoconusa, Globoheterohelix, Globoquadrina, Globorotalia, Globorotalia (Acarinina), Globorotalia (Astrorotalia), Globorotalia (Clavatorella), Globorotalia (Fohsella), Globorotalia (Globoconella), Globorotalia (Globorotalia), Globorotalia (Hirsutella), Globorotalia (Menardella), Globorotalia (Morozovella), Globorotalia (Truncorotalia), Globorotalia (Truncorotaloides), Globorotalia (Turborotalia)> >>

Globoconusa conusa Khalilov 1956
= Globoconusa daubjergensis
Globoconusa daubjergensis gigantea Bang 1969
= Globoconusa daubjergensis
Globoconusa quadripartitaformis Khalilov 1956
= Acarinina subsphaerica
Globoconusa tripartita Morozova et al. 1967
= Globoconusa daubjergensis
Globoconusa victori Koutsoukos 2014
= Globoconusa victori

Globoconusa

Citation: Globoconusa Khalilov, 1956
taxonomic rank: Genus
Type species: Globoconusa conusa Khalilov, 1956
Type repository: Baku; Geological Institute, Academy of Sciences, Baku, Azerbaidzhan S.S.R.

Current identification/main database link: Globoconusa Khalilov, 1956


Original Description

Translation from the Russian. - Test high conical, turret-like, tapering toward the initial end. Dorsal side strongly convex,with a conical spire, its apex at the initial chamber. The height of the cone exceeds the diameter of its base or is nearly equal to it. On the dorsal side all whorls are visible, in general, represented by semispherical chambers; on ventral side subspherical chambers are ohserved only in the last whorl.

Lower Paleocene, Danian.

References:

Khalilov, D. M. (1956). 0 pelagicheskoy faune foraminifer Paleogenovykh otlozheniy Azerbaydzhana [Pelagic Foraminifera of the Paleogene Deposits of the Azerbaizhan SSR]. Trudy Instituta Geologii, Akademiya Nauk Azerbaidzhanskoi SSR. 17: 234-255. gs


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Globoconusa compiled by the pforams@mikrotax project team viewed: 8-12-2024

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Short stable page link: https://mikrotax.org/pforams/index.php?id=130922 Go to Archive.is to create a permanent copy of this page - citation notes



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